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Sample records for program iodp expedition

  1. IODP expedition 347: Baltic Sea basin paleoenvironment and biosphere

    NARCIS (Netherlands)

    Andrén, T.; Barker Jorgensen, B.; Cotterill, C.; Green, S.; Slomp, C.

    2015-01-01

    The Integrated Ocean Drilling Program (IODP) expedition 347 cored sediments from different settings of the Baltic Sea covering the last glacial–interglacial cycle. The main aim was to study the geological development of the Baltic Sea in relation to the extreme climate variability of the region with

  2. IODP expedition 347: Baltic Sea basin paleoenvironment and biosphere

    DEFF Research Database (Denmark)

    Andrén, T; Jørgensen, Bo Barker; Cotterill, Carol

    2015-01-01

    The Integrated Ocean Drilling Program (IODP) expedition 347 cored sediments from different set- tings of the Baltic Sea covering the last glacial–interglacial cycle. The main aim was to study the geological development of the Baltic Sea in relation to the extreme climate variability of the region...... with changing ice cover and major shifts in temperature, salinity, and biological communities. Using the Greatship Manisha as a European Consortium for Ocean Research Drilling (ECORD) mission-specific platform, we recovered 1.6 km of core from nine sites of which four were additionally cored for microbiology...... degassing upon core recovery. The depth distributions of conservative sea water ions still reflected the transition at the end of the last glaciation from fresh-water clays to Holocene brackish mud. High-resolution sampling and analyses of interstitial water chemistry revealed the intensive mineralization...

  3. Coccolithophore and benthic foraminifera distribution patterns in the Gulf of Cadiz and Western Iberian Margin during Integrated Ocean Drilling Program (IODP) Expedition 339

    Science.gov (United States)

    Balestra, B.; Grunert, P.; Ausin, B.; Hodell, D.; Flores, J.-A.; Alvarez-Zarikian, C. A.; Hernandez-Molina, F. J.; Stow, D.; Piller, W. E.; Paytan, A.

    2017-06-01

    For the first time during an Integrated Ocean Drilling Program (IODP) Expedition (Exp. 339, Mediterranean Outflow) water samples for living coccolithophore distributions and mudline samples for coccoliths, benthic foraminifera, and geochemical analyses in the underlying surface sediments were collected. In total, 14 water samples (from 5 to 20 m water depth) and 7 mudline samples were gathered at the drill sites. Coccolithophore distributions show spatial variations in species diversity. In particular, assemblages that characterize the Western Iberian Margin differ from those in the Gulf of Cadiz, indicative of oceanographic and environmental controls on the community in the upper ocean (0-20 m depth). Comparison of the living assemblages to those in surface sediments shows differences in the presence of some species, suggesting the influence of post deposition sedimentary processes. Other factors such as the season of sampling and the limited sampling depth may also have a role in the differences recorded. Benthic foraminiferal assemblages seem to be primarily determined by source, quantity and quality of available food. Sites in the Gulf of Cadiz are bathed by Mediterranean Outflow Water (MOW) and characterized by a considerable amount of advected food particles. Elevated epibenthic foraminifera exploit this niche, while arborescent epifaunal and infaunal taxa thrive on food particles falling out of MOW. The combined data suggest different flow speeds and settling of MOW suspension load in the Gulf of Cadiz. In contrast, assemblages from the Western Iberian Margin located farthest from or outside of MOW are determined by local export productivity and mirror trophic conditions in the surface waters. Both assemblages reveal variation in the composition at intermediate and deep water depths along the southern and western Iberian Margins with distance from the Strait of Gibraltar.

  4. IODP expedition 334: An investigation of the sedimentary record, fluid flow and state of stress on top of the seismogenic zone of an erosive subduction margin

    Digital Repository Service at National Institute of Oceanography (India)

    Vannucchi, P.; Ujiie, K.; Stroncik, N.; IODP Exp. 334 Scientific Party; Yatheesh, V.

    The Costa Rica Seismogenesis Project (CRISP) is an experiment to understand the processes that control nucleation and seismic rupture of large earthquakes at erosional subduction zones. Integrated Ocean Drililng Program (IODP) Expedition 334 by R...

  5. Particle sizes of Pliocene and Pleistocene core sediments from IODP Expedition 323 in the Bering Sea

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This data compilation includes the results of grain size analyses of core sediment collected by IODP during Expedition 323 in the Bering Sea. One dataset is included...

  6. Magnetic Susceptibility as a Tool for Investigating Igneous Rocks—Experience from IODP Expedition 304

    Directory of Open Access Journals (Sweden)

    Roger C. Searle

    2008-07-01

    Full Text Available Continuous measurements of magnetic susceptibility have been commonly used on Ocean Drilling Program (ODP and Integrated Ocean Drilling Program (IODPexpeditions to study minor lithological variations (forexample, those related to climatic cycles in sedimentary rocks, but they have been less frequently used on igneous rocks, although important post-cruise studies have utilized them (e.g., Ildefonse and Pezard, 2001. Here I report its use (and that of the closely related electrical conductivity on IODP Expedition 304 to examine igneous crustal rocks. Expedition 304/305 targeted the Atlantis Massif, an oceanic core complex on the Mid-Atlantic Ridge, and recovered a suite of igneous rocks comprising mainly gabbros, troctolites, and some diabases (Blackman et al., 2006; Ildefonse et al., 2006, 2007; IODP Expeditions 304 and 305 Scientists, 2005. Shipboard measurements (on D/V JOIDES Resolution of physical properties were made to characterize lithological units and alteration products, to correlate cored material with down-hole logging data, and to interpret broader-scale geophysical data.

  7. Archive of Core and Site/Hole Data and Photographs from the Integrated Ocean Drilling Program (IODP)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The US Science Operator for the Integrated Ocean Drilling Program (IODP) operated the drilling vessel JOIDES Resolution from 2004-2013 for worldwide expeditions...

  8. Raman Spectroscopy: an essential tool for future IODP expeditions

    Science.gov (United States)

    Andò, Sergio; Garzanti, Eduardo; Kulhanek, Denise K.

    2016-04-01

    The scientific drilling of oceanic sedimentary sequences plays a fundamental part in provenance studies, paleoclimate recostructions, and source-to-sink investigations (e.g., France-Lanord et al., 2015; Pandey et al., 2015). When studying oceanic deposits, Raman spectroscopy can and does represent an essential flexible tool for the multidisciplinary approach necessary to integrate the insight provided by different disciplines. This new user-friendly technique opens up an innovative avenue to study in real time the composition of detrital mineral grains of any origin, complementing traditional methods of provenance analysis (e.g., sedimentary petrography, heavy minerals; Andò and Garzanti, 2014). Raman spectra can readily reveal the chemistry of foraminiferal tests, nannofossils and other biogenic debris for the study of ecosystem evolution and paleoclimate, or the Ca/Mg ratio in biogenic or terrigenous carbonates for geological or marine biological applications and oil exploration (Borromeo et al., 2015). For the study of pelagic or turbiditic muds, which represent the bulk of the deep-marine sedimentary record, Raman spectroscopy allows us to identify silt-sized grains down to the size of a few microns with the same precision level required in quantitative provenance analysis of sand-sized sediments (Andò et al., 2011). Silt and siltstone also represent a very conspicuous part of the stratigraphic record onshore and usually preserve original mineralogical assemblages better than more permeable interbedded sand and sandstone (Blatt, 1985). Raman spectra can be obtained on sample volumes of only a few cubic microns by a confocal micro-Raman coupled with a standard polarizing light microscope using a 50× objective. The size of this apparatus can be easily placed onboard an IODP vessel to provide crucial information and quickly solve identification problems for the benefit of a wide range of scientists during future expeditions. Cited references Andò, S., Vignola

  9. IODP Expedition 333: Return to Nankai Trough Subduction Inputs Sites and Coring of Mass Transport Deposits

    Directory of Open Access Journals (Sweden)

    Michael Strasser

    2012-09-01

    Full Text Available Integrated Ocean Drilling Program (IODP Expedition 333 returned to two sites drilled during IODP Expedition 322 on the ocean side of the Nankai Trough to pursue the characterization of the inputs to the Nankai subduction and seismogenic zone, as part of the Nankai Trough Seismogenic Experiment (NanTroSEIZE multi-expedition project. SiteC0011 is located at the seaward edge of the trench and Site C0012 on a basement high, Kashinozaki Knoll (Fig. 1. The main objectives of drilling again at these sites were to fill coring gaps in the upper part (<350 m of the sedimentary sequence, to measure heat flow, and to core the oceanic basement to a greater depth on the Knoll. New results include the observation of a diagenetic boundary within the Shikoku Basin sediments that may be compared to one documented further west by ODP Legs 131, 190 and 196 but occurs here at a lower temperature. Borehole heat flow measurements confirm spatial variations in the Shikoku Basin that were indicated by short probe surveys. Heat flow variations between topographic highs and lows may be related to fluid convection within the basement. This expedition also included the objectives of the Nankai Trough Submarine LandSLIDEhistory (NanTroSLIDE Ancillary Project Letter (APL and cored at Site C0018 a pile of mass transport deposits on the footwall of the megasplay fault, a major out of sequence thrust that presumably slips coseismically during large subduction earthquakes. This brought newinsight on the timing of these mass wasting events and on the deformation within the sliding slope sediments.

  10. IODP Expedition 360: Analyzing the Media Coverage of a High Profile Research Project

    Science.gov (United States)

    Kavanagh, L.; Martinez, A. O.; Burgio, M.; Zhang, J.; Expedition 360 Scientists, I.

    2016-12-01

    During Expedition 360 of the International Ocean Discovery Program (IODP), the JOIDES Resolution drilled 789 meters of lower crustal gabbro in the Southwest Indian Ocean. This hole began a multi-expedition project with the goal of one day drilling across the crust-mantle boundary for the first time. This simplified narrative of the research objectives struck a chord with media and the project received worldwide coverage in the form of over 50 stories with a total audience in the millions. This expedition is presented as a case study in science communication. A four-member education and outreach team onboard the ship acted as the point of contact for interested reporters. Major outlets that ran stories include the Australian Broadcasting Corporation, British Broadcasting Corporation, Boston Globe, Daily Express, Fox News, Nature, Smithsonian, and Chinese based Xinhua News Agency who sailed a reporter on the ship for the duration of the expedition. The majority of stories published provided accurate and favourable coverage of the project; however, a few contained critical errors and cast the expedition in a less positive light. Public reaction varied greatly depending on the article. Positive themes include interest in the scientific outcomes and encouragement of human exploration. Negative themes include the project being an inefficient use of money and a perceived risk of the drilling triggering an earthquake or volcano. Through a review of published articles and online comments, the successes and challenges faced by Expedition 360 are identified. Despite minimal preparation for media relations, the team successfully maintained a public profile while working in one of the most remote locations on Earth. Interviews were facilitated and videos, articles, and podcasts were produced onboard the ship. A simple, catchy narrative resulted in a large volume of coverage; however, this simplicity also formed the root of a number of misconceptions and issues of public concern.

  11. IODP Expedition 331: Strong and Expansive Subseafloor Hydrothermal Activities in the Okinawa Trough

    Directory of Open Access Journals (Sweden)

    the IODP Expedition 331 Scientists

    2012-04-01

    Full Text Available Integrated Ocean Drilling Program (IODP Expedition 331 drilled into the Iheya North hydrothermal system in the middle Okinawa Trough in order to investigate active subseafloor microbial ecosystems and their physical and chemical settings. We drilled five sites during Expedition 331 using special guide bases at three holes for reentry, casing, and capping, including installation of a steel mesh platformwith valve controls for postcruise sampling of fluids. At Site C0016, drilling at the base of the North Big Chimney (NBCmound yielded low recovery, but core included the first Kuroko-type black ore ever recovered from the modern subseafloor. The other four sites yielded interbedded hemipelagic and strongly pumiceous volcaniclastic sediment, along with volcanogenic breccias that are variably hydrothermally altered and mineralized. At most sites, analyses of interstitial water and headspace gas yielded complex patterns withdepth and lateral distance of only a few meters. Documented processes included formation of brines and vapor-rich fluids by phase separation and segregation, uptake of Mg and Na by alteration minerals in exchange for Ca, leaching of K at high temperature and uptake at low temperature, anhydrite precipitation, potential microbial oxidation of organic matter and anaerobic oxidation of methane utilizing sulfate, and methanogenesis. Shipboard analyses have found evidence for microbial activity in sediments within the upper 10–30 m below seafloor (mbsf where temperatures were relativelylow, but little evidence in the deeper hydrothermally altered zones and hydrothermal fluid regime.

  12. Overpressure, Flow Focusing, Compaction and Slope Stability on the continental slope: Insights from IODP Expedition 308

    Science.gov (United States)

    Flemings, P. B.

    2010-12-01

    Integrated Ocean Drilling Program Expepedition 308 used direct measurements of pore pressure, analysis of hydromechanical properties, and geological analysis to illuminate how sedimentation, flow focusing, overpressure, and slope stability couple beneath the seafloor on the deepwater continental slope in the Gulf of Mexico. We used pore pressure penetrometers to measure severe overpressures (60% of the difference between lithostatic stress and hydrostatic pressure) that extend from the seafloor for 100’s of meters. We ran uniaxial consolidation experiments on whole core and found that although permeability is relatively high near the seafloor, the sediments are highly compressible. As a result, the coefficient of consolidation (the hydraulic diffusivity) is remarkably constant over a large range of effective stresses. This behavior accounts for the high overpressure that begins near the seafloor and extends to depth. Forward modeling suggests that flow is driven laterally along a permeable unit called the Blue Unit. Calculations suggest that soon after deposition, lateral flow lowered the effective stress and triggered the submarine landslides that we observe. Later in the evolution of this system, overpressure may have pre-conditioned the slope to failure by earthquakes. Results from IODP Expedition 308 illustrate how pore pressure and sedimentation control the large-scale form of continental margins, how submarine landslides form, and provide strategies for designing stable drilling programs.

  13. IODP Expedition 324: Ocean Drilling at Shatsky Rise Gives Clues about Oceanic Plateau Formation

    Directory of Open Access Journals (Sweden)

    Jörg Geldmacher

    2011-09-01

    Full Text Available Integrated Ocean Drilling Program (IODP Expedition 324 cored Shatsky Rise at five sites (U1346–U1350 to study processes of oceanic plateau formation and evolution. Site penetrations ranged from 191.8 m to 324.1 m with coring of 52.6 m to 172.7 m into igneous basement at four of the sites. Average recovery in basement was 38.7%–67.4%. Cored igneous sections consist mainly of variably evolved tholeiiticbasalts emplaced as pillows or massive flows. Massive flows are thickest and make up the largest percentage of section on the largest and oldest volcano, late Jurassic age Tamu Massif; thus, it may have formed at high effusion rates. Such massive flows are characteristic of flood basalts, and similar flows were cored at Ontong Java Plateau. Indeed, the similarity of igneous sections at Site U1347 with that cored on Ontong Java Plateau implies similar volcanic styles for these two plateaus. On younger, smaller Shatsky Rise volcanoes, pillow flows are common and massive flows thinner andfewer, which might mean volcanism waned with time. Cored sediments from summit sites contain fossils and structures implying shallow water depths or emergence at the time of eruption and normal subsidence since. Summit sites also show pervasive alteration that could be due to high fluid fluxes. A thick section of volcaniclastics cored on Tamu Massif suggests that shallow, explosive submarine volcanism played a significant role in the geologic development of the plateau summit. Expedition 324 results imply that Shatsky Risebegan with massive eruptions forming a huge volcano and that subsequent eruptions waned in intensity, forming volcanoes that are large, but which did not erupt with unusually high effusionrates. Similarities of cored sections on Tamu Massif with those ofOntong Java Plateau indicate that these oceanic plateaus formed insimilar fashion.

  14. IODP Expeditions 309 and 312 Drill an Intact Section of Upper Oceanic Basement into Gabbros

    Directory of Open Access Journals (Sweden)

    Douglas S. Wilson

    2007-03-01

    Full Text Available The Integrated Ocean Drilling Program’s (IODP Expeditions 309 and 312 successfully completed the first sampling of an intact section of upper oceanic crust, through lavas and the sheeted dikes into the uppermost gabbros. Hole 1256D, which was initiated on the Ocean Drilling Program’s (ODP Leg 206, now penetrates to >1500 mbsf and >1250 m sub-basement. The first gabbroic rocks were encountered at 1407 mbsf. Below this, the hole penetrates ~100 m into a complex zone of fractionated gabbros intruded into contact metamorphosed dikes.

  15. IODP Expedition 323—Pliocene and Pleistocene Paleoceanographic Changes in the Bering Sea

    Directory of Open Access Journals (Sweden)

    Carlos Alvarez Zarikian

    2011-03-01

    Full Text Available High-resolution paleoceanography of the Plio-Pleistocene is important in understanding climate forcing mechanisms and the associated environmental changes. This is particularly true in high-latitude marginal seas such as the Bering Sea, which has been very sensitive to changes in global climate during interglacial and glacial or Milankovitch time scales. This is due to significant changes in water circulation, land-ocean interaction, and sea-ice formation. With theaim to reveal the climate and oceanographic history of the Bering Sea over the past 5 Ma, Integrated Ocean Drilling Program (IODP Expedition 323 cored a total of 5741 meters of sediment (97.4% recovery at seven sites covering three different areas: Umnak Plateau, Bowers Ridge, and the Bering slope region. Four deep holes range from 600 m to 745 m spanning in age from 1.9 Ma to 5 Ma. The water depths (819 m to 3173 m allow characterization of past verticalwater mass distribution such as the oxygen minimum zone (OMZ. The results highlight three key points. (1 The first is an understanding of long-term evolution of surface-water mass distribution during the past 5 Ma including past sea-ice distribution and warm and less eutrophic subarctic Pacific water mass entry into the Bering Sea. (2 We characterized relatively stagnant intermediate water mass distribution imprinted as laminated sediment intervals that have beenubiquitously encountered. Today, the OMZ impinges upon the sediments at ~700–1600 m water depths. In the past, the OMZ appears to have occurred mainly during interglacial periods. Changes in low oxygen-tolerant benthic foraminiferal faunas clearly concur with this observation. (3 We also characterized significant changes between glacial episode of terrigenous sedimentary supply and interglacialepisode of diatom flux.

  16. Methane hydrate formation in turbidite sediments of northern Cascadia, IODP Expedition 311

    Science.gov (United States)

    Torres, M.E.; Trehu, A.M.; Cespedes, N.; Kastner, M.; Wortmann, U.G.; Kim, J.-H.; Long, P.; Malinverno, A.; Pohlman, J.W.; Riedel, M.; Collett, T.

    2008-01-01

    Expedition 311 of the Integrated Ocean Drilling Program (IODP) to northern Cascadia recovered gas-hydrate bearing sediments along a SW-NE transect from the first ridge of the accretionary margin to the eastward limit of gas-hydrate stability. In this study we contrast the gas gas-hydrate distribution from two sites drilled ~ 8??km apart in different tectonic settings. At Site U1325, drilled on a depositional basin with nearly horizontal sedimentary sequences, the gas-hydrate distribution shows a trend of increasing saturation toward the base of gas-hydrate stability, consistent with several model simulations in the literature. Site U1326 was drilled on an uplifted ridge characterized by faulting, which has likely experienced some mass wasting events. Here the gas hydrate does not show a clear depth-distribution trend, the highest gas-hydrate saturation occurs well within the gas-hydrate stability zone at the shallow depth of ~ 49??mbsf. Sediments at both sites are characterized by abundant coarse-grained (sand) layers up to 23??cm in thickness, and are interspaced within fine-grained (clay and silty clay) detrital sediments. The gas-hydrate distribution is punctuated by localized depth intervals of high gas-hydrate saturation, which preferentially occur in the coarse-grained horizons and occupy up to 60% of the pore space at Site U1325 and > 80% at Site U1326. Detailed analyses of contiguous samples of different lithologies show that when enough methane is present, about 90% of the variance in gas-hydrate saturation can be explained by the sand (> 63????m) content of the sediments. The variability in gas-hydrate occupancy of sandy horizons at Site U1326 reflects an insufficient methane supply to the sediment section between 190 and 245??mbsf. ?? 2008 Elsevier B.V.

  17. Carbon-isotope stratigraphy from terrestrial organic matter through the Monterey event, Miocene, New Jersey margin (IODP Expedition 313)

    DEFF Research Database (Denmark)

    Fang, Linhao; Bjerrum, Christian J.; Hesselbo, Stephen P.

    2013-01-01

    The stratigraphic utility of carbon-isotope values from terrestrial organic matter is explored for Miocene siliciclastic sediments of the shallow shelf, New Jersey margin, USA (Integrated Ocean Drilling Program [IODP] Expedition 313). These shallow marine strata, rich in terrestrial organic matter...... consistently in palynological preparation residues, concentrated woody phytoclasts, and individually picked woody phytoclasts obtained from the New Jersey sediments. A bulk organic matter curve shows somewhat different stratigraphic trends but, when corrected for mixing of marine-terrestrial components...... as environmental factors affecting vegetation in the sediment source areas. These possible factors are assessed on the basis of pyrolysis data, scanning electron microscope observations, and comparison to palynological indices of environmental change. Some evidence is found for localized degradation and...

  18. Gamma radiation-based astronomical timescale for the Maldives: Preliminary results from IODP Expedition 359, Maldives Monsoon and Sea Level

    Science.gov (United States)

    Slagle, Angela; Wright, James; Kroon, Dick; Lanci, Luca; Betzler, Christian; Eberli, Gregor; Alvarez Zarikian, Carlos; 359 Scientists, Expedition

    2017-04-01

    Many of the attributes that characterize the modern ocean-atmosphere system developed during the Neogene. In the Indian Ocean, strengthening of the monsoon, development of the oxygen minimum zone, and spin up of the equatorial currents occurred during this interval. International Ocean Discovery Program (IODP) Expedition 359 drilled a series of eight sites across two transects in the Maldives archipelago, capturing records of carbonate platform and drift sedimentation through this critical time period. Sites U1467 (middle Miocene to present) and U1468 (Oligocene/Miocene boundary to middle Miocene) provide the opportunity to construct a complete Neogene record of sedimentation in the depositional center of the region, the Maldives Inner Sea. Downhole logging data provide continuous, in situ measurements of physical properties but are limited to the logged interval (typically only deeper than 100 meters below seafloor) and by borehole conditions; core data are higher resolution but limited by core recovery and quality. Integration of these two data sets is a powerful tool for interpreting the complete drilled interval collected during Expedition 359. Natural gamma radiation measured both in boreholes and on recovered sediments is the primary measurement used for core-log data integration. Spectral gamma radiation data from downhole logging reveals that the gamma radiation signal is dominated by uranium at all Expedition 359 sites, indicating that its variations and cycles are likely controlled by changes in organic matter. This study of gamma radiation cycles will contribute to expedition efforts to assemble an integrated cyclo-magneto-biostratigraphic age model, allowing for further refinement of the age assignments for the Maldivian events. Ultimately, a final age model for the Maldives drift sites can be integrated with the regional seismic stratigraphic framework to establish ages for a series of critical sequence boundaries, allowing for a detailed

  19. IODP Expeditions 303 and 306 Monitor Miocene- Quaternary Climate in the North Atlantic

    Directory of Open Access Journals (Sweden)

    Carlos Alvarez-Zarikian

    2006-03-01

    Full Text Available Introduction The IODP Expeditions 303 and 306 drilling sites were chosen for two reasons: (1 to capture Miocene-Quaternary millennial-scale climate variability in sensitive regions at the mouth of the Labrador Sea and in the North Atlantic icerafted debris (IRD belt (Ruddiman et al., 1977, and (2 to provide the sedimentary and paleomagnetic attributes, including adequate sedimentation rates, for constructinghigh-resolution isotopic and magnetic stratigraphies.High accumulation rates, reaching 20 cm ky-1, permit the study of millennial-scale variations in climate and in the Earth's magnetic fi eld over the past several million years, when the amplitude and frequency of climate variability changed substantially. Shipboard logging and scanning data (magnetic susceptibility and remanence, density, natural gamma radiation, digital images and color refl ectance and post-expedition x-ray fl uorescence (XRF scanning datahave revealed that the sediment cores recovered on Expeditions 303 and 306 contain detailed histories of millennial-scale climate and geomagnetic fi eld variability throughout the late Miocene to Quaternary epochs. The climate proxies will be integrated with paleomagnetic data to place the records of millennial-scale climate change into a high resolution stratigraphy based on oxygen isotope andrelative paleomagnetic intensity (RPI. The paleomagnetic record of polarity reversals, excursions and RPI in these cores is central to the construction of the stratigraphic template and will provide detailed documentation of geomagnetic fi eld behavior.

  20. Studies on thermophysical properties at New Jersey Shallow Shelf (IODP Expedition 313)

    Science.gov (United States)

    Fehr, A.; Pechnig, R.; Inwood, J.; LOFI, J.; Bosch, F. P.; Clauser, C.

    2011-12-01

    The IODP drilling expedition 313 New Jersey Shallow Shelf was proposed for obtaining deep sub-seafloor samples and downhole logging measurements in the crucial inner shelf region.The inner to central shelf off-shore New Jersey is an ideal location for studying the history of sea-level changes and its relationship to sequence stratigraphy and onshore/offshore groundwater flows. The region features rapid depositional rates, tectonic stability, and well-preserved, cosmopolitan age control fossils suitable for characterizing the sediments of this margin throughout the time interval of interest. Past sea-level rise and fall is documented in sedimentary layers deposited during Earth's history. In addition, the inner shelf is characterised by relatively fresh pore water intervals alternating vertically with saltier intervals (Mountain et al., 2010). Therefore, three boreholes were drilled in the so-called New Jersey/Mid-Atlantic transect during IODP Expedition 313 New Jersey Shallow Shelf. Numerous questions have arisen concerning the age and origin of the brackish waters recovered offshore at depth. Here we present an analysis of thermophysical properties to be used as input parameters in constructing numerical models for future groundwater flow simulations. Our study is based mainly on Nuclear Magnetic Resonance (NMR) measurements for inferring porosity and permeability, and thermal conductivity. We performed NMR measurements on samples from boreholes M0027A, M0028A and M0029A and thermal conductivity measurements on the whole round cores prior to the Onshore Party. These results are compared with data from alternative laboratory measurements and with petrophysical properties inferred from downhole logging data.

  1. Variations of marine pore water salinity and chlorinity in Gulf of Alaska sediments (IODP Expedition 341)

    Science.gov (United States)

    März, Christian; Mix, Alan C.; McClymont, Erin; Nakamura, Atsunori; Berbel, Glaucia; Gulick, Sean; Jaeger, John; Schneider (LeVay), Leah

    2014-05-01

    Pore waters of marine sediments usually have salinities and chlorinities similar to the overlying sea water, ranging around 34-35 psu (Practical Salinity Units) and around 550 mM Cl-, respectively. This is because these parameters are conservative in the sense that they do not significantly participate in biogeochemical cycles. However, pore water studies carried out in the frame of the International Ocean Discovery Program (IODP) and its predecessors have shown that salinities and chlorinities of marine pore waters can substantially deviate from the modern bottom water composition in a number of environmental settings, and various processes have been suggested to explain these phenomena. Also during the recent IODP Expedition 341 that drilled five sites in the Gulf of Alaska (Northeast Pacific Ocean) from the deep Surveyor Fan across the continental slope to the glaciomarine shelf deposits, several occurrences of pore waters with salinities and chlorinities significantly different from respective bottom waters were encountered during shipboard analyses. At the pelagic Sites U1417 and U1418 (~4,200 and ~3,700 m water depth, respectively), salinity and chlorinity maxima occur around 20-50 m sediment depth, but values gradually decrease with increasing drilling depths (down to 30 psu in ~600 m sediment depth). While the pore water freshening at depth is most likely an effect of clay mineral dehydration due to increasing burial depth, the shallow salinity and chlorinity maxima are interpreted as relicts of more saline bottom waters that existed in the North Pacific during the Last Glacial Maximum (Adkins et al., 2002). In contrast, the glaciomarine slope and shelf deposits at Site U1419 to U1421 (~200 to 1,000 m water depth) are characterised by unexpectedly low salinitiy and chlorinity values (as low as 16 psu and 295 mM Cl-, respectively) already in very shallow sediment depths (~10 m), and their records do not show systematic trends with sediment depth. Freshening

  2. Paleolatitudinal Constraints from Eocene to Recent Sediments Cored in the Equatorial Pacific on IODP Expeditions 320 and 321

    Science.gov (United States)

    Acton, G.; Richter, C.; Yamamoto, Y.; Ohneiser, C.; Yamazaki, T.; Channell, J. E. T.; Evans, H. F.; Petronotis, K. E.; Guidry, E. P.

    2016-12-01

    Sediments cored along a Pacific Equatorial Age Transect (PEAT) during Integrated Ocean Drilling Program (IODP) Expeditions 320 and 321 record the paleomagnetic field with high fidelity, providing new paleolatitudinal constraints for the Pacific Plate. A total of 6,141 m of core was recovered from 23 holes cored at 8 sites (Sites U1331 through U1338), which are currently located at latitudes between 2.5°N and 12.1°N. Paleomagnetic data were collected from discrete samples (7 cm3 cubes) that were subjected to progressive alternating field (AF) and thermal demagnetization and were collected every 1 cm along U-channel samples (2 cm x 2 cm x 150 cm) and every 5 cm or less along split-core sections that were subjected to progressive AF demagnetization. The age of the sediment is well constrained from unambiguous magnetostratigraphies and from biostratigraphic data, as well as by subsequent astronomical tuning using cyclic variations in the physical, chemical, and magnetic properties of the sediments. The large amount of paleomagnetic data collected within each magnetic chron makes it possible to compute the change in paleolatitude with high temporal resolution and to investigate polarity asymmetries, overprints, and other possible biases. The good spatial (latitudinal) distribution of the sites along with the general northward motion of the Pacific Plate provide observations that help resolve possible biases caused by flattening, which is inherently small for near equatorial sites but, even so, possibly resolvable given the large number of paleomagnetic data.

  3. Stress magnitude and orientation in deep coalbed biosphere off Shimokita ~IODP Expedition337 drilling project

    Science.gov (United States)

    Wu, H. Y.; Lin, W.; Yamada, Y.

    2015-12-01

    One of IODP expedition (Borehole C0020A) is located in the forearc basin formed by the subducting between Pacific plate and Eurasian plate off Shimokita Peninsula. This ~2.5km deep scientific drilling collected the high-resolution wire-line resistivity logging, caliper data, Dipole Sonic waveforms; geophysical properties measurements and core samples. The riser drilling operations produced one good conditions borehole even this drilling operation was applied right after 311 Tohoku earthquake. Based on the high-resolutions Formation Micro Imager (FMI) images, both breakout and tensile fractures along the borehole wall indicating the in-situ stress orientation are detected in the unwrapped resistivity images. In this research, a reasonable geomechanical model based on the breakout width and physical properties is constructed to estimate the stress magnitude profile in this borehole. Besides, the openhole leak-off test revealed the information of Shmin magnitude. In general, stress direction along the borehole is slight rotated to east with drilling to the bottom of the borehole. Geomechanical model constarined the principal stresses in Strike-slip stress regime to satisfy the occurrences of borehole enlargements and tensile fractures. Some blank zones with no borehole wall failure and vertical fractures indicated the stress anomaly might be controlled by local lithological facies. Comparing to the JFAST drilling, this site is out of Japan trench slip zone and shows almost parallel stress direcion to the trench (~90 degree apart of Shmin with Site C0019).

  4. Downhole Logging Measurements from IODP Expedition 313: an Overview and Future Directions

    Science.gov (United States)

    Inwood, J.; Lofi, J.; Scienceparty, E.

    2009-12-01

    Downhole geophysical measurements and images allow the characterization of the lithology and physical properties of the subsurface, thus making a powerful contribution to the evaluation of facies and sediment composition and to the recognition of key surfaces in siliciclastic successions. The mission-specific IODP Expedition 313 (May-July 2009) cored and logged sequences deposited on the New Jersey continental margin during the post-Eocene ice-house world. One of the aims of the Expedition is to evaluate sequence stratigraphic facies models that predict depositional environments, sediment compositions, and stratal geometries in response to sea-level change. 5800 m of wireline logging data were collected in three boreholes drilled to a composite total of 2062 m; here we present an overview of these data. Continuous through-pipe spectral gamma ray logs were acquired in each borehole and repeated in open hole intervals for calibration. Magnetic susceptibility, resistivity, sonic and acoustic image logs were obtained in open hole at key intervals and/or where borehole conditions allowed. Due to space limitations on the offshore platform, Exp313 cores were not split. Samples from core catchers, whole-round multi-sensor track measurements, vertical seismic profiles and these logging data comprise the full data set at the time of this writing. Preliminary analysis shows lateral and vertical changes in the physical properties of the sediments that enable us to distinguish depositional intervals at several scales (cms - tens of meters). Medium to high resolution acoustic images of the borehole walls reveal sedimentary characteristics even within intervals of low core recovery, and provide an accurate core-depth positioning of some key surfaces. Likewise, the continuous spectral gamma logs allow assessment of lithologies in intervals with incomplete core recovery, and show great promise of providing excellent log-core-seismic correlations once the cores are split and fully

  5. Rhizon Sampling of Pore Waters on Scientific Drilling Expeditions: An Example from the IODP Expedition 302, Arctic Coring Expedition (ACEX

    Directory of Open Access Journals (Sweden)

    Luzie Schnieders

    2007-03-01

    Full Text Available For more than 35 years, interstitial water (IW samples have been collected from sediment recovered during marine scientific coring expeditions. Pioneering work of DSDP and ODP quickly demonstrated that pore water chemistry differed from that of overlying seawater and from one location to another for myriad reasons (Sayles and Manheim, 1975. Extraction and analysis of IW samples has now becomeroutine on deep-sea drilling cruises; the ensuing pore water profiles are being used to understand a range of processes, such as subsurface fluid flow (e.g., Brown et al., 2001; Saffer and Screaton, 2003, mineral diagenesis (e.g., Rudnicki et al., 2001; Malone et al., 2002, microbial reactions (e.g., Böttcher and Khim, 2004; D’Hondt et al., 2004, gas hydrate dissociation (e.g., Egeberg and Dickens, 1999; Tréhu et al., 2004, and glacial to interglacial changes in the composition of bottom water (e.g., Paul et al., 2001; Adkins and McIntyre, 2002.

  6. IODP Expedition 339 in the Gulf of Cadiz and off West Iberia: Decoding the environmental significance of the Mediterranean outflow water and its global influence

    NARCIS (Netherlands)

    Hernández-Molina, F.J.; Stow, D.A.V.; Alvarez-Zarikian, C.; Acton, G.; Bahr, A.; Balestra, B.; Ducassou, E.; Flood, R.; Flores, J.-A.; Furota, S.; Grunert, P.; Hodell, D.; Jimenez-Espejo, F.; Kim, J.K.; Krissek, L.; Kuroda, J.; Li, B.; Llave, E.; Lofi, J.; Lourens, L.|info:eu-repo/dai/nl/125023103; Miller, M.; Nanayama, F.; Nishida, N.; Richter, C.; Roque, C.; Pereira, H.; Sanchez Goñi, M.F.; Sierro, F.J.; Singh, A.D.; Sloss, C.; Takashimizu, Y.; Tzanova, A.; Voelker, A.; Williams, T.; Xuan, C.

    2013-01-01

    IODP Expedition 339 drilled five sites in the Gulf of Cadiz and two off the west Iberian margin (November 2011 to January 2012), and recovered 5.5 km of sediment cores with an average recovery of 86.4%. The Gulf of Cadiz was targeted for drilling as a key location for the investigation of

  7. Detachment Faulting, Serpentinization, Fluids and Life: Preliminary Results of IODP Expedition 357 (Atlantis Massif, MAR 30°N)

    Science.gov (United States)

    Fruh-Green, G. L.; Orcutt, B.; Green, S.; Cotterill, C.

    2016-12-01

    We present an overview of IODP Expedition 357, which successfully used two seabed rock drills to core 17 shallow holes at 9 sites across Atlantis Massif (Mid-Atlantic Ridge 30°N). A major goal of this expedition is to investigate serpentinization processes and microbial activity in the shallow subsurface of highly altered ultramafic and mafic sequences that have been uplifted to the seafloor along a major detachment fault zone. More than 57 m of core were recovered, with borehole penetration ranging from 1.3 to 16.4 meters below seafloor, and core recovery as high as 75% of total penetration. The cores show highly heterogeneous rock type, bulk rock chemistry and alteration that reflect multiple phases of magmatism and fluid-rock interaction within the detachment fault zone. In cores along an E-W transect of the southern wall, recovered mantle peridotites are locally intruded by gabbroic and doleritic dikes and veins. The proportion of mafic rocks are volumetrically less than the amount of mafic rocks recovered previously in the central dome at IODP Site U1309, suggesting a lower degree of melt infiltration into mantle peridotite at the ridge-transform intersection. New technologies were developed and successfully applied for the first time: (1) an in-situ sensor package and water sampling system on each seabed drill measured real-time variations in dissolved methane, oxygen, pH, oxidation reduction potential, temperature, and conductivity during drilling and took water samples after drilling; (2) a borehole plug system to seal the boreholes was successfully deployed at two sites to allow access for future sampling; and (3) delivery of chemical tracers into the drilling fluids for contamination testing. We will provide an overview of the drilling strategy and preliminary results of Expedition 357, and highlight the role of serpentinization in sustaining microbial communities in a region of active serpentinization and low temperature hydrothermal alteration.

  8. A brittle (normal?) shear zone cored in Site C0002 of Nankai Trough Seismogenic Zone Experiment (IODP Expedition 348)

    Science.gov (United States)

    Crespo-Blanc, Ana; Sample, James; Brown, Kevin; Otsubo, Makoto; Yamamoto, Yuzuru

    2016-04-01

    Integrated Ocean Discovery Program (IODP) Expedition 348, which belongs to the Nankai Trough Seismogenic Zone Experiment, conducted riser-drilling to make deeper an existing hole at Site C0002, up to 3058.5 meters below seafloor (mbsf). This site is located 80 km SE of the Kii Peninsula (Japan) in the Kumano forearc basin, in turn situated on top of the Nankai accretionary prism. Cuttings (875.5-3058.5 mbsf) and cores (2163.0-2217.5 mbsf) were collected in the upper Miocene to Pliocene turbiditic silty claystone with few intercalations of sandstone which characterize the accretionary prism lithological units. A remarkably preserved fault zone has been cored around 2205 mbsf (core section Hole C0002P-348-5R-4). It is characterized by 34 cm of fault breccia, in which an anastomosed cataclastic foliation is present. The rocks of the damaged zone are formed by silty claystone with an incipient scaly fabric and scarce levels of sandstones. Extra-large thin sections were made along the whole core section. In the brittle shear zone, they reveal a catalogue of deformation structures characteristic of a high structural level. In particular, almond-type structures and arrays of microfaults cutting the stratification are the most common structures and outline the cataclastic foliation. The occurrence of calcite veins in the recovered cores is limited to this fault zone, which is indicative of its role as fluid path, accompanied by carbonate cementation. Generally fault veins have lower δ18O values than carbonate cements in the sedimentary matrix, consistent with veins forming at higher temperatures and/or from a fluid more strongly depleted in 18O. A continuum of the relationships between calcite veins and cataclastic deformation is observed, from veins that precipitated early in the fault history, with calcite grains broken during subsequent deformation, to late veins which seal the almond-type structures within the claystones. The geometry of the calcite grains within the

  9. The First D/V Chikyu IODP Operations: Successful Logging and Coring During NanTroSEIZE Stage 1 Expeditions

    Directory of Open Access Journals (Sweden)

    Moe Kyaw Thu

    2008-07-01

    Full Text Available The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE is a multi-expedition IODP drilling project aimed at drilling, coring, logging, and instrumenting the seismogenic zone of an active subduction margin , in a region thought to generate megathrust earthquakes of magnitude >8.0 on the moment-magnitude scale (Tobin and Kinoshita, 2006. The Nankai Trough, offshore of the Kii Peninsula, Honshu, Japan (Fig. 1 was chosen as the location for thisproject based on a number of scientific drilling proposals to IODP. These reviewed existing drilling data in the region, the long-term historical and recent record of great earthquakes, the social and societal relevance of the area, and the accessibility of the seismogenic zone to present drilling technology. The first stage of this multi-stage project was intended to accomplish a broad characterization of the shallow geology, geophysics, physical properties, heat flow, and fluid flow in a transect across the downgoing Philippine Sea Plate, the toe of the Nankai accretionary prism, the megasplay fault zone region on the continental slope, and the Kumano Basin that lies between the accretionary prism and the KiiPeninsula, on the continental shelf (Fig. 2.

  10. Fluid inclusion petrology and microthermometry of the Cocos Ridge hydrothermal system, IODP Expedition 344 (CRISP 2), Site U1414.

    Science.gov (United States)

    Brandstätter, Jennifer; Kurz, Walter; Krenn, Kurt; Micheuz, Peter

    2016-04-01

    In this study, we present new data from microthermometry of fluid inclusions entrapped in hydrothermal veins along the Cocos Ridge from the IODP Expedition 344 Site U1414. The results of our study concern a primary task of IODP Expedition 344 to evaluate fluid/rock interaction linked with the tectonic evolution of the incoming Cocos Plate from the Early Miocene up to recent times. Aqueous, low saline fluids are concentrated within veins from both the Cocos Ridge basalt and the overlying lithified sediments of Unit III. Mineralization and crosscutting relationships give constraints for different vein generations. Isochores from primary, reequilibrated, and secondary fluid inclusions crossed with litho/hydrostatic pressures indicate an anticlockwise PT evolution during vein precipitation and modification by isobaric heating and subsequent cooling at pressures between ∼210 and 350 bar. Internal over and underpressures in the inclusions enabled decrepitation and reequilibration of early inclusions but also modification of vein generations in the Cocos Ridge basalt and in the lithified sediments. We propose that lithification of the sediments was accompanied with a first stage of vein development (VU1 and VC1) that resulted from Galapagos hotspot activity in the Middle Miocene. Heat advection, either related to the Cocos-Nazca spreading center or to hotspot activity closer to the Middle America Trench, led to subsequent vein modification (VC2, VU2/3) related to isobaric heating. The latest mineralization (VC3, VU3) within aragonite and calcite veins and some vesicles of the Cocos Ridge basalt occurred during crustal cooling up to recent times. Fluid inclusion analyses and published isotope data show evidence for communication with deeper sourced, high-temperature hydrothermal fluids within the Cocos Plate. The fluid source of the hydrothermal veins reflects aqueous low saline pore water mixed with invaded seawater.

  11. Fluid inclusion petrology and microthermometry of the Cocos Ridge hydrothermal system, IODP Expedition 344 (CRISP 2), Site U1414

    Science.gov (United States)

    Brandstätter, Jennifer; Kurz, Walter; Krenn, Kurt; Micheuz, Peter

    2016-04-01

    In this study, we present new data from microthermometry of fluid inclusions entrapped in hydrothermal veins along the Cocos Ridge from the IODP Expedition 344 Site U1414. The results of our study concern a primary task of IODP Expedition 344 to evaluate fluid/rock interaction linked with the tectonic evolution of the incoming Cocos Plate from the Early Miocene up to recent times. Aqueous, low saline fluids are concentrated within veins from both the Cocos Ridge basalt and the overlying lithified sediments of Unit III. Mineralization and crosscutting relationships give constraints for different vein generations. Isochores from primary, reequilibrated, and secondary fluid inclusions crossed with litho/hydrostatic pressures indicate an anticlockwise PT evolution during vein precipitation and modification by isobaric heating and subsequent cooling at pressures between ˜210 and 350 bar. Internal over and underpressures in the inclusions enabled decrepitation and reequilibration of early inclusions but also modification of vein generations in the Cocos Ridge basalt and in the lithified sediments. We propose that lithification of the sediments was accompanied with a first stage of vein development (VU1 and VC1) that resulted from Galapagos hotspot activity in the Middle Miocene. Heat advection, either related to the Cocos-Nazca spreading center or to hotspot activity closer to the Middle America Trench, led to subsequent vein modification (VC2, VU2/3) related to isobaric heating. The latest mineralization (VC3, VU3) within aragonite and calcite veins and some vesicles of the Cocos Ridge basalt occurred during crustal cooling up to recent times. Fluid inclusion analyses and published isotope data show evidence for communication with deeper sourced, high-temperature hydrothermal fluids within the Cocos Plate. The fluid source of the hydrothermal veins reflects aqueous low saline pore water mixed with invaded seawater.

  12. IODP Expedition 301 Installs Three Borehole Crustal Observatories, Prepares for Three-Dimensional, Cross-Hole Experiments in the Northeastern Pacific Ocean

    Directory of Open Access Journals (Sweden)

    Adam Klaus

    2005-09-01

    , determine how fluidpathways are distributed within an active hydrothermalsystem, and elucidate relations between fluid circulation,alteration, microbiology, and seismic properties. Thecomplete experimental program will comprise two IODPexpeditions (the first having been Expedition 301, thesecond to be scheduled, an offset seismic experiment, andlong-term monitoring and cross-hole tests facilitated withsubmersible and remotely operated vehicle (ROV expeditionsextending 6–10 years after the first IODP expedition.The experimental program will also take advantage ofopportunities related to a plate-scale network of long-termobservatories (NEPTUNE currently being planned.

  13. NanTroSEIZE Stage 1 Expeditions 314, 315, and 316: First Drilling Program of the Nankai Trough Seismogenic Zone Experiment

    Directory of Open Access Journals (Sweden)

    Hideki Masago

    2009-09-01

    Full Text Available Integrated Ocean Drilling Program (IODP Expeditions 314, 315, and 316 were carried out as a unified program of drilling collectively known as Stage 1 of the Nankai Trough Seismogenic Zone Experiment, or NanTroSEIZE, the first multi-stage complex drilling project in IODP and the most ambitious effort in scientific ocean drilling to date (Tobin and Kinoshita, 2006b; Kinoshita et al., 2006. The first of four planned operational stages, the Stage 1 expeditions were conducted aboard the new riser-capable drilling vessel Chikyu from September 2007 to February 2008, and were Chikyu’s inaugural IODP expeditions. Seventy-one scientists from twelve countries took part in the three expeditions as shipboard participants, and thirty-three holes in total were drilled at eight sites, to as much as 1400 meters below the sea floor (Table 1, Fig. 1.

  14. One Dimensional Backstripping Results from IODP Expedition 318, Site U1356: Tectonic Implications for the Wilkes Land Margin of Antarctica

    Science.gov (United States)

    Hayden, T. G.; Kominz, M. A.; González, J. J.; Escutia, C.; Brinkhuis, H.; Scientific Party of IODP Expedition 318

    2011-12-01

    The Wilkes Land margin of Antarctica is the conjugate margin of the Great Australian Bight, which underwent extension, thinning and rifting from ~160 Ma until breakup at ~83 Ma. Both Wilkes Land and the Great Australian Bight are considered passive margins, and were thought to be tectonically inactive since breakup at 83 Ma. We have backstripped the U1356 Core recovered from the continental rise off Wilkes Land, Antarctica by IODP Expedition 318. Backstripping input included lithological and sedimentary analysis, paleo-environmental indicators, combined paleomagnetic and biostratigraphic chronologies, and physical properties measurements. Tectonic subsidence shows a major event between 50 and 33.6 Ma, a time represented by a hiatus in the U1356 core. The magnitude of subsidence requires it to be tectonic in origin, and the timing matches with a reorganization of plate motions that represents the transition from slow spreading to fast spreading between Antarctica and Australia, which occurred at approximately 43 Ma. Coupled with a regional seismic framework, and using other Expedition 318 site analyses, the Wilkes Land margin is shown to be far more complex then the simple passive margin currently assumed. We explore several possible mechanisms for the subsidence and erosion observed; including thermal uplift due to continental insulation of the asthenosphere and it's interaction with a recently rifted margin, asthenospheric convection, transtensional or transpressional basin development and loading, and edge-driven asthenospheric convection.

  15. Gas hydrate drilling transect across northern Cascadia margin - IODP Expedition 311

    Science.gov (United States)

    Riedel, M.; Collett, T.; Malone, M.J.; Collett, T.S.; Mitchell, M.; Guerin, G.; Akiba, F.; Blanc-Valleron, M.; Ellis, M.; Hashimoto, Y.; Heuer, V.; Higashi, Y.; Holland, M.; Jackson, P.D.; Kaneko, M.; Kastner, M.; Kim, J.-H.; Kitajima, H.; Long, P.E.; Malinverno, A.; Myers, Gwen E.; Palekar, L.D.; Pohlman, J.; Schultheiss, P.; Teichert, B.; Torres, M.E.; Trehu, A.M.; Wang, Jingyuan; Worthmann, U.G.; Yoshioka, H.

    2009-01-01

    A transect of four sites (U1325, U1326, U1327 and U1329) across the northern Cascadia margin was established during Integrated Ocean Drilling Program Expedition 311 to study the occurrence and formation of gas hydrate in accretionary complexes. In addition to the transect sites, a fifth site (U1328) was established at a cold vent with active fluid flow. The four transect sites represent different typical geological environments of gas hydrate occurrence across the northern Cascadia margin from the earliest occurrence on the westernmost first accreted ridge (Site U1326) to the eastward limit of the gas hydrate occurrence in shallower water (Site U1329). Expedition 311 complements previous gas hydrate studies along the Cascadia accretionary complex, especially ODP Leg 146 and Leg 204 by extending the aperture of the transect sampled and introducing new tools to systematically quantify the gas hydrate content of the sediments. Among the most significant findings of the expedition was the occurrence of up to 20 m thick sand-rich turbidite intervals with gas hydrate concentrations locally exceeding 50% of the pore space at Sites U1326 and U1327. Moreover, these anomalous gas hydrate intervals occur at unexpectedly shallow depths of 50-120 metres below seafloor, which is the opposite of what was expected from previous models of gas hydrate formation in accretionary complexes, where gas hydrate was predicted to be more concentrated near the base of the gas hydrate stability zone just above the bottom-simulating reflector. Gas hydrate appears to be mainly concentrated in turbidite sand layers. During Expedition 311, the visual correlation of gas hydrate with sand layers was clearly and repeatedly documented, strongly supporting the importance of grain size in controlling gas hydrate occurrence. The results from the transect sites provide evidence for a structurally complex, lithology-controlled gas hydrate environment on the northern Cascadia margin. Local shallow

  16. Geomagnetic Excursions recorded from a sediment core from the Great Barrier Reef, IODP Expedition 325, Australia

    Science.gov (United States)

    Lau, J. K.; Herrero-Bervera, E.; Jovane, L.

    2010-12-01

    At the end of the Expedition 325, “Great Barrier Reef Environmental Changes” (GBREC), of the Integrated Ocean Drilling Program, a core 40 m long collected fine sediments from seaward of Noggin Reef, Queensland, Australia. Initial uranium-thorium and radiocarbon measurements give relative ages of ~10 to ~30 ka. The main aim of the expedition was an investigation of the magnitude and nature of sea-level changes in relation to the Last Glacial Maximum. Paleoenvironmental analyses will study the sea-level changes in relation to the glacial-interglacial phases. Recent modeling of the geodynamo and studies of the geomagnetic field show that the inner core imposes a physical constraint on fluid motions in the outer core. As a result, this complex vortex could provoke anomalies in the geomagnetic configuration that might also include complete and “aborted” reversals of the geomagnetic field. These “aborted” reversals can last for a few thousand years, and are called excursions. We present preliminary measurements of the magnetic susceptibility and NRM of U-channels and of discrete samples from Exp. 325 hole M0058A drilled in April 2010 in front of Noggin Reef in a water depth of 172 m. The magnetic susceptibility shows two zones of high susceptibility with respect to the rest of the base values. The first zone is located between 8.63 and 14.80 mbsf and the second one is located from ¬27.00 to 32.60 mbsf with a maximum value of 277.78 x 10-8 m3/kg. Natural remanent magnetization (NRM) and stepwise a.f. demagnetization have been measured for the 40 m long U-channels and for high-resolution 1-cc discrete samples. Some anomalies of the inclination of the NRM at 17-18 and 23-24 mbsf are related to increased intensity of NRM, but there is no variation in the magnetic susceptibility for these intervals. Alternating field (a.f.) stepwise demagnetization shows that these features are recognizable along the demagnetization steps, showing a consistent Characteristic

  17. Microstructural analysis and calcite piezometry on hydrothermal veins: Insights into the deformation history of the Cocos Plate at Site U1414 (IODP Expedition 344)

    Science.gov (United States)

    Brandstätter, Jennifer; Kurz, Walter; Rogowitz, Anna

    2017-08-01

    In this study we present microstructural data from hydrothermal veins in the sedimentary cover and the igneous basement recovered from Hole U1414A, Integrated Ocean Drilling Program (IODP) Expedition 344 (Costa Rica Seismogenesis Project), to constrain deformation mechanism operating in the subducting Cocos Plate. Cathodoluminescence studies, mechanical e-twin piezometry and electron backscatter diffraction (EBSD) analyses of carbonate veins were used to give insights into the deformation conditions and to help to understand the tectonic deformation history of the Cocos Plate offshore Costa Rica. Analyses of microstructures in the sedimentary rocks and in the basalt of the igneous basement reveal brittle deformation, as well as crystal-plastic deformation of the host rock and the vein material. Cathodoluminescence images showed that in the basalt fluid flow and related precipitation occurred over several episodes. The differential stresses, obtained from two different piezometers using the same parameter (twin density), indicate various mean differential stresses of 49 ± 11 and 69 ± 30 MPa and EBSD mapping of calcite veins reveals low-angle subgrain boundaries. Deformation temperatures are restricted to the range from 170°C to 220°C, due to the characteristics of the existing twins and the lack of high-temperature intracrystalline deformation mechanisms (>220°C). The obtained results suggest that deformation occurred over a period associated with changes of ambient temperatures, occurrence of fluids and hydrofracturing, induced differential stresses due to the bending of the plate at the trench, and related seismic activity.

  18. Sediment classification using neural networks: An example from the site-U1344A of IODP Expedition 323 in the Bering Sea

    Science.gov (United States)

    Ojha, Maheswar; Maiti, Saumen

    2016-03-01

    A novel approach based on the concept of Bayesian neural network (BNN) has been implemented for classifying sediment boundaries using downhole log data obtained during Integrated Ocean Drilling Program (IODP) Expedition 323 in the Bering Sea slope region. The Bayesian framework in conjunction with Markov Chain Monte Carlo (MCMC)/hybrid Monte Carlo (HMC) learning paradigm has been applied to constrain the lithology boundaries using density, density porosity, gamma ray, sonic P-wave velocity and electrical resistivity at the Hole U1344A. We have demonstrated the effectiveness of our supervised classification methodology by comparing our findings with a conventional neural network and a Bayesian neural network optimized by scaled conjugate gradient method (SCG), and tested the robustness of the algorithm in the presence of red noise in the data. The Bayesian results based on the HMC algorithm (BNN.HMC) resolve detailed finer structures at certain depths in addition to main lithology such as silty clay, diatom clayey silt and sandy silt. Our method also recovers the lithology information from a depth ranging between 615 and 655 m Wireline log Matched depth below Sea Floor of no core recovery zone. Our analyses demonstrate that the BNN based approach renders robust means for the classification of complex lithology successions at the Hole U1344A, which could be very useful for other studies and understanding the oceanic crustal inhomogeneity and structural discontinuities.

  19. Linking Active Serpentinization with Volatiles and Life: Constraints from IODP Expedition 357 (Atlantis Massif, MAR 30°N)

    Science.gov (United States)

    Fruh-Green, G. L.; Rouméjon, S.; Lilley, M. D.; Orcutt, B.

    2016-12-01

    The Atlantis Massif (MAR, 30°N) is one of the best-studied oceanic core complexes, and recently the target of IODP Expedition 357 (late 2015). This expedition successfully used two seabed rock drills to core 17 shallow holes at 9 sites to study serpentinization processes and microbial activity in the shallow subsurface of highly altered ultramafic and mafic rocks that have been uplifted to the seafloor along a major detachment fault zone. An in situ sensor and water sampling system mounted on the drills recorded real-time variations in dissolved methane, oxygen, pH, oxidation reduction potential, temperature and conductivity during drilling and sampled bottom water after drilling, providing evidence for active serpentinization at all sites. The cores have highly heterogeneous rock types, bulk rock chemistry, and alteration that reflect multiple phases of magmatism and fluid-rock interaction. Recovered ultramafic rocks are dominated by harzburgite with intervals of dunite and minor pyroxenite veins; gabbroic rocks occur as melt impregnations and veins. Dolerite dikes and basaltic rocks represent the latest magmatic activity. The ultramafic rocks show a high degree of serpentinization, with a metasomatic talc-amphibole-chlorite overprint and local rodingitization. Serpentinization textures vary between sites and holes, but are characterized by lizardite mesh textures after olivine, recrystallization textures into chrysotile-polygonal serpentine or antigorite, and veins. Monitoring of borehole fluids during drilling recorded numerous excursions in methane, temperature and redox potential that often correlated with each other. The fact that the excursions occurred both while drilling as well as when no coring operations were taking place implies that horizons of hydrogen- and methane-rich fluids must exist in the basement rocks, and that volatiles are continuously being expelled during active serpentinization at Atlantis Massif.

  20. IODP Expedition 317: Exploring the Record of Sea-Level Change off New Zealand

    Directory of Open Access Journals (Sweden)

    Peter Blum

    2011-09-01

    Full Text Available Expedition 317 investigated the record of global sea-level change (eustasy within continental margin sedimentary sequences and how eustasy interacts with local forcing to produce preserved sedimentary architectures. The Canterbury Basin, on the eastern margin of the South Island of New Zealand, was selected to study these complex interactions because of high rates of Neogene sediment supply fromthe uplifting Southern Alps. This sediment input results in a high-frequency (~0.1–0.5 My periods record of depositional cyclicity that is modulated by the presence of strong ocean currents. The expedition recovered sediments as old as Eocene but focused on the sequence stratigraphy of the late Miocene to Recent, when global sea-level change was dominated by glacioeustasy. A transect of three sites was drilled on the continental shelf (Sites U1353, U1354, and U1351, plus one on the continental slope (Site U1352. The transectsamples the shallow-water environment most directly affected by relative sea-level change. Lithologic boundaries, provisionally correlative with seismic sequence boundaries, have been identified in cores from each site. Continental slope Site U1352 provides a record of ocean circulation and fronts during the last ~35 My. The early Oligocene (~30 MaMarshall Paraconformity was the deepest target ofExpedition 317 and is hypothesized to represent intensified current erosion or non-deposition associated with the initiation of thermohaline circulation in the region. Expedition 317 involved operational challenges for JOIDES Resolution, including shallow-water, continental-shelf drilling and deep penetrations. Despitethese challenges, Expedition 317 set a number of records for scientific ocean drilling penetration and water-depth.

  1. Microstructural observations on hydrothermal veins of Site U1414, IODP Expedition 344 (CRISP 2)

    Science.gov (United States)

    Brandstätter, Jennifer; Kurz, Walter; Rogowitz, Anna

    2017-04-01

    The erosive active margin offshore Osa Peninsula (Costa Rica) is characterized by the subducting Cocos Plate with its topographic height, the aseismic Cocos Ridge, which has lifted the seismogenic zone in the reach of scientific drilling. To understand the processes occurring in the subducting Cocos Plate in the vicinity to the Middle America Trench, we investigated microstructures in hydrothermal veins, transecting the lithified sediments and the igneous basement of IODP Hole U-1414A. Mechanical e-twinning occurred mainly in the blocky calcite veins in the lithified sediments, rather than in the fibrous calcite veins within the Cocos Ridge basalt. The differential stress, obtained from two different piezometers, indicate mean differential stresses of approximately 53 and 82 MPa. The majority of the twins show a significant thickness (up to 120 µm), straight twin boundaries and are indicative for deformation temperatures between 150 to 300°C. The presence of additional deformation structures, such as undulose extinction and subgrain boundaries, indicates intracrystalline-plastic deformation by dislocation creep. The comparison of the EBSD data from two samples within the lithified sedimentary unit indicates diverse deformation temperatures. Variation in subgrain size observed for the different samples can be related to local variations in differential stress. The results of different microstructural observations showed, that the deformational history of Site 344-U1414 is characterized by distinct tectonic phases, occurring during the movement of the Cocos Ridge from its location of origin (the Galapagos hotspot) to the convergent margin offshore Costa Rica. The causes for these changes in deformation mechanisms in the studied rocks are ascribed to magmatic advection resulting in an increase of temperature and decrease of critical resolved shear stresses, as well as the bending of the Cocos plate adjacent to the Middle American trench.

  2. IODP Expedition 302, Arctic Coring Expedition (ACEX: A First Look at the Cenozoic Paleoceanography of the Central Arctic Ocean

    Directory of Open Access Journals (Sweden)

    the IODP Expedition 302 Scientists

    2005-09-01

    Full Text Available Introduction The behavior and inf luence of the A rct ic Oceanthroughout the course of the global Cenozoic climateevolution have been virtually unknown. Only the uppermostfew meters of the Arctic’s sediment record, representingHolocene and late Pleistocene times, have been retrievedfrom ridges through a limited number of short piston,gravity, and box cores. Even less of the thick sedimentsequences, ~6 km in the Canada Basin and ~3 km in theNansen Basin(Grantz et al., 1990; Jokat et al., 1995, restingon the Arctic Ocean’s abyssal plains, have been cored.Prior to the Arctic Coring Expedition (ACEX, informationon Neogene or Paleogene conditions in the central Arcticwas limited to a 1.6-m interval in a 3.6-m-long T-3 gravitycore raised from the Alpha Ridge (Clark, 1974, providingthe sole evidence for marine conditions no older than themiddle Eocene in the central Arctic (Bukry, 1984.

  3. Thermophysical properties derived from lab measurements and downhole logging at New Jersey Shallow Shelf (IODP Expedition 313)

    Science.gov (United States)

    Fehr, A.; Pechnig, R.; Inwood, J.; Lofi, J.; Bosch, F. P.; Clauser, C.

    2012-04-01

    The IODP drilling expedition 313 New Jersey Shallow Shelf was proposed for obtaining deep sub-seafloor samples and downhole logging measurements in the crucial inner shelf region. The inner to central shelf off-shore New Jersey is an ideal location for studying the history of sea-level changes and its relationship to sequence stratigraphy and onshore/offshore groundwater flows. The region features rapid depositional rates, tectonic stability, and well-preserved, cosmopolitan age control fossils suitable for characterizing the sediments of this margin throughout the time interval of interest. Past sea-level rise and fall is documented in sedimentary layers deposited during Earth's history. In addition, the inner shelf is characterised by relatively fresh pore water intervals alternating vertically with saltier intervals (Mountain et al., 2010). Therefore, three boreholes were drilled in the so-called New Jersey/Mid-Atlantic transect during IODP Expedition 313 New Jersey Shallow Shelf. Numerous questions have arisen concerning the age and origin of the brackish waters recovered offshore at depth. Here we present an analysis of thermophysical properties to be used as input parameters in constructing numerical models for future groundwater flow simulations. Our study is based mainly on Nuclear Magnetic Resonance (NMR) measurements for inferring porosity and permeability, and thermal conductivity. We performed NMR measurements on samples from boreholes M0027A, M0028A and M0029A and thermal conductivity measurements on the whole round cores prior to the Onshore Party. These results are compared with data from alternative laboratory measurements and with petrophysical properties inferred from downhole logging data. We deduced petrophysical properties from downhole logging data and compared them with results obtained with laboratory measurements. In water saturated samples, the number of spins in the fluid is proportional to sample porosity. NMR porosities were calculated

  4. Towards an improved understanding of Baltic Sea hypoxia during the Holocene: preliminary results from IODP Expedition 347

    Science.gov (United States)

    Slomp, Caroline; Dijkstra, Nikki; Egger, Matthias; Gustafsson, Bo; Ash, Jeanine; Bauersachs, Thorsten; Hardisty, Dalton; Martin, Ellen; Riedinger, Natascha; Andren, Thomas; Barker Jorgensen, Bo

    2015-04-01

    The Baltic Sea is a restricted brackish-marine basin that is highly sensitive to changes in climate and anthropogenic activity. Due to its salinity stratification, the Baltic Sea is particularly vulnerable to hypoxia (oxygen concentrations Medieval Climate Anomaly (MCA), ca. 1-0.7 ka (Zillen et al., 2008; Jilbert and Slomp, 2013). While changes in salinity, temperature and the input and recycling of nutrients all may contribute to the development of hypoxia in the Baltic Sea, their relative importance in driving the hypoxia during the MCA and HTM is still incompletely understood. Here, we use porewater and sediment geochemical data obtained during the IODP Expedition 347: Baltic Sea Paleoenvironment (September 13 - November 1, 2013) to obtain further insight into the role of changes in salinity and phosphorus recycling during the HTM. We focus on three sites along the modern salinity gradient in the Baltic Sea, Sites M0059, M0063 and M0065. Our results indicate that bottom water salinity in the Baltic Proper was higher during the HTM than at present, confirming previous studies that increased salinity stratification may have contributed to the development of hypoxia during the HTM. We also discuss evidence for temporal changes and spatial differences in primary productivity and phosphorus burial and recycling in the Baltic Sea and their potential role in contributing to the development of hypoxia during the HTM and MCA. References: Jilbert, T., and Slomp, C.P. (2013). Rapid high-amplitude variability in Baltic Sea hypoxia during the Holocene. Geology 41, 1183-1186. doi: 10.1130/g34804.1. Zillén, L., Conley, D.J., Andrén, T., Andrén, E., and Björck, S. (2008). Past occurrences of hypoxia in the Baltic Sea and the role of climate variability, environmental change and human impact. Earth-Science Reviews 91, 77-92. doi: 10.1016/j.earscirev.2008.10.001.

  5. IODP Expedition 321T: Cementing Operations at Holes U1301A and U1301B, Eastern Flank of the Juan de Fuca Ridge

    Directory of Open Access Journals (Sweden)

    Andrew T. Fisher

    2010-04-01

    Full Text Available IODP Expedition 301 (Fisher et al., 2005a was part of a series of expeditions and experiments to quantify hydrogeologic, lithologic, biogeochemical, and microbiological properties, processes, and linkages on the eastern flank of the Juan de Fuca Ridge, North Pacific (Fig. 1. Operations during Expedition 301 included replacement of one existing subseafloor borehole observatory (“CORK”, Hole 1026B, drilling two basement holes and installing two new long-term observatories (Holes U1301A and U1301B, coring the upper ~300 m of basement and shallow sediments above basement, and collection of in situ hydrogeologic and geophysical data from basement. Subsequent expeditions using a remotely operated vehicle (ROV and submersible have serviced borehole observatories, collected pressure and temperature data and fluid and microbiological samples, and replaced components as needed to maintain these systems for futureuse. Another drilling expedition is planned for 2010 (see backcover for schedule to emplace three more borehole observatories and initiate cross-hole tests, and additional ROV and submersible ex-peditions will conduct long-term experiments and recover subseafloor data and samples.

  6. Fluid inclusion petrography and microthermometry of the Cocos Ridge hydrothermal system, IODP Expedition 344 (CRISP 2), Site U1414

    Science.gov (United States)

    Brandstätter, J.; Kurz, W.; Krenn, K.; Micheuz, P.

    2015-12-01

    We present new data from microthermometric analyses of fluid inclusions entrapped in hydrothermal veins within lithified sediments and Cocos Ridge (CCR) basalt from IODP Expedition 344 site U1414 (Costa Rica) and concern on a primary task of Expedition 344, i.e. to evaluate fluid/rock interaction, the hydrologic system, and the geochemical processes (indicated by composition and volume of fluids) active within the incoming Cocos Plate. Mineralization of the veins and crosscutting relationships gives constraints for the different generation of veins. Calcium carbonate, commonly aragonite in the upper part and calcite in the lower part of the igneous basement, is usually present in veins as a late phase following the quartz precipitation and the clay minerals formation. The sequence of vein generations in the lithified sediments close to the contact within the CCR basalt is characterized by smaller veins filled by quartz, followed by massive intersecting calcite veins. A high fluid pressure can be concluded, due to wall rock fragments embedded within the filling and fractured mineral grains in the ground mass, which are close to the veins. This requires that the magmatic basement and the lithified sediments were covered by sequences of low permeability sediments forming a barrier that enabled build up elevated fluid pressure. The investigation of fluid inclusions in the lowest units of borehole 344-U1414, give clues about the source of the fluids and about the vein evolution within the incoming Cocos Plate close to Middle American Trench. The microthermometric analyses of the primary, almost aqueous, inclusions indicate a temperature range during entrapment between 200 and 420°C. The data indicate that seawater within the Cocos Ridge aquifer communicated with high-temperature fluids and/or were modified by heat advection. We consider the Galapagos hotspot and/ or the Cocos-Nazca spreading center as heat source. Fluids originated from mobilized sediment pore water

  7. Archive of Core and Site/Hole Data and Photographs from the International Ocean Discovery Program (IODP)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Texas A&M University operates the drilling vessel JOIDES Resolution for the International Ocean Discovery Program (IODP). The International Ocean Discovery...

  8. Microstructural analysis and calcite piezometry on hydrothermal veins: Insights into the deformation history of the Cocos Plate at Site U1414 (IODP Expedition 344).

    Science.gov (United States)

    Brandstätter, Jennifer; Kurz, Walter; Rogowitz, Anna

    2017-08-01

    In this study we present microstructural data from hydrothermal veins in the sedimentary cover and the igneous basement recovered from Hole U1414A, Integrated Ocean Drilling Program (IODP) Expedition 344 (Costa Rica Seismogenesis Project), to constrain deformation mechanism operating in the subducting Cocos Plate. Cathodoluminescence studies, mechanical e-twin piezometry and electron backscatter diffraction (EBSD) analyses of carbonate veins were used to give insights into the deformation conditions and to help to understand the tectonic deformation history of the Cocos Plate offshore Costa Rica. Analyses of microstructures in the sedimentary rocks and in the basalt of the igneous basement reveal brittle deformation, as well as crystal-plastic deformation of the host rock and the vein material. Cathodoluminescence images showed that in the basalt fluid flow and related precipitation occurred over several episodes. The differential stresses, obtained from two different piezometers using the same parameter (twin density), indicate various mean differential stresses of 49 ± 11 and 69 ± 30 MPa and EBSD mapping of calcite veins reveals low-angle subgrain boundaries. Deformation temperatures are restricted to the range from 170°C to 220°C, due to the characteristics of the existing twins and the lack of high-temperature intracrystalline deformation mechanisms (>220°C). The obtained results suggest that deformation occurred over a period associated with changes of ambient temperatures, occurrence of fluids and hydrofracturing, induced differential stresses due to the bending of the plate at the trench, and related seismic activity.

  9. Mineralogical influences on porosity-depth trends of shelf deposits (Miocene-Pleistocene) along the northwest shelf of Australia (IODP Expedition 356)

    Science.gov (United States)

    Knierzinger, Wolfgang; Lee, Eun Young; Wagreich, Michael

    2017-04-01

    Porosity in sediments is influenced by various factors such as mineralogical composition, burial depth, connate fluids, and stratigraphic layering. This work focuses on processes underlying porosity anomalies in carbonate shelf deposits along the northwest shelf of Australia by using different techniques (polarization microscopy, electron microscopy, XRD, XRF). IODP expedition 356 recovered cored seven sites (U1458-U1464), covering a latitudinal range of 29°S-18°S on the northwest shelf. Strong negative deviations from general porosity-depth trends for these carbonate rich sediments are clear for samples with higher contents of dolomite, calcium sulfates, and non-skeletal calcite. No significant influence of aragonite on porosity values has yet been detected. However, it is likely that the occurrence of high amounts of aragonite is a crucial element with regard to porosity values in these carbonate rich deposits, since elongated aragonite needles commonly enhance interparticle porosity. Further insight might be gained through the application of electron microscopy. In general, sediments in the northern part of the study area (Sites U1462, U1463, U1464) tend to show slightly higher porosity values compared to sediments form the south (Sites U1459, U1460). This may reflect the influence of calcium sulfate, because mineralogical analyses show, calcium sulfate is relatively rare at the southern sites, whereas higher amounts of calcium sulfates occur in the north. The lack of detrital particles in calcium sulfate components indicates an evaporitic origin. Deposits at Site U 1461 differ from other analyzed sediments insofar as higher amounts of feldspars and micas are apparent. *This research is conducted within the frame of the 'International Ocean Discovery Program', funded by the Ministry of Oceans and Fisheries, Korea.

  10. IODP Expedition 334: An Investigation of the Sedimentary Record, Fluid Flow and State of Stress on Top of the Seismogenic Zone of an Erosive Subduction Margin

    Directory of Open Access Journals (Sweden)

    Paola Vannucchi

    2013-03-01

    Full Text Available The Costa Rica Seismogenesis Project (CRISP is an experiment to understand the processes that control nucleation and seismic rupture of large earthquakes at erosional subduction zones. Integrated Ocean Drililng Program (IODP Expedition 334 by R/V JOIDES Resolution is the first step toward deep drilling through the aseismic and seismicplate boundary at the Costa Rica subduction zone offshore the Osa Peninsula where the Cocos Ridge is subducting beneath the Caribbean plate. Drilling operations included logging while drilling (LWD at two slope sites (Sites U1378 and U1379 and coring at three slope sites (Sites U1378–1380and at one site on the Cocos plate (Site U1381. For the first time the lithology, stratigraphy, and age of the slope and incoming sediments as well as the petrology of the subducting Cocos Ridge have been characterized at this margin.The slope sites recorded a high sediment accumulation rate of 160–1035m m.y.-1 possibly caused by on-land uplift triggered by the subduction of the Cocos Ridge. The geochemical data as well as the in situ temperature data obtained at the slope sites suggest that fluids are transported from greater depths. The geochemical profiles at Site U1381 reflect diffusional communication of a fluid with seawater-likechemistry and the igneous basement of the Cocos plate (Solomon et al., 2011; Vannucchi et al., 2012a. The present-day in situ stress orientation determined by borehole breakouts at Site U1378 in the middle slope and Site U1379 in the upper slope shows a marked change in stress state within ~12 km along the CRISP transect; that maycorrespond to a change from compression (middle slope to extension (upper slope.

  11. Preliminary results of three-dimensional stress orientation determined by anelastic strain recovery (ASR) measurements of core samples retrieved from IODP Expedition 343

    Science.gov (United States)

    Lin, W.; Yamamoto, Y.; Tanikawa, W.

    2013-12-01

    Integrated Ocean Drilling Program (IODP) Expedition 343, Japan Trench Fast Drilling Project (JFAST) penetrated to ~850 meter below seafloor (mbsf) in a water depth of 6890 m and passed through the plate boundary fault of the overriding North American Plate and the subducting Pacific plate witch. The fault locates at ~820 mbsf and is preliminarily considered to be the source fault of the 2011 Tohoku-oki Mw 9.0 earthquake. Area of JFAST drilling site (C0019) was in the largest coseismic slip zone where the fault slipped more than 50 m during the earthquake. Hole C0019E dedicated to coring retrieved a total of 21 cores having a total of 51 m long cores from both the hanging wall and the footwall of the plate boundary fault. To determine three-dimensional stress state after the huge earthquake, we collected four whole round core samples and measured anelastic strain recovery (ASR) also called 'relaxation' of the core samples onboard D/V Chikyu. The principle idea behind the ASR method is that stress-induced elastic strain is released first instantaneously (i.e., as time-independent elastic strain), followed by a more gradual or time-dependent recovery of anelastic strain. The ASR method takes advantage of the time-dependent strain and has been successfully applied in IODP expeditions (e.g. Byrne et al., 2009; Yamamoto et al., 2013). The four core samples used for ASR measurements were taken from C0019E-1R1 (~177 mbsf), C0019E-5R1 (~697 mbsf)), C0019E-13R1 (~802 mbsf) and C0019E-19R2 (~828 mbsf). The three core samples at shallower depths were in the hanging wall of the fault; and the deepest one was in the footwall. We started ASR measurements approximate three hours after the core was 'on deck', that is approximate six hours from the in situ stress was released, and keep the measurements for about two weeks. The anelastic strains measured in nine directions including six independent directions were extensional; all of the curves varied smoothly and similarly with

  12. Thermal evolution of Site U1414 by stable isotopes δ13C and δ18O, 87Sr/86Sr and fluid inclusion analyses, IODP Expedition 344

    Science.gov (United States)

    Brandstätter, Jennifer; Kurz, Walter; Krenn, Kurt; Richoz, Sylvain

    2017-04-01

    IODP Expedition 344 is the second expedition in course of the Costa Rica Seismogenesis Project (Program A), that was designed to reveal processes that effect nucleation and seismic rupture of large earthquakes at erosional subduction zones. Site 344-U1414, located 1 km seaward of the deformation front offshore Costa Rica, serves to evaluate fluid-rock interaction and geochemical processes linked with the tectonic evolution of the incoming Cocos Plate from the Early Miocene up to recent times. Combined isotope analyses and microthermometric analyses of fluid inclusions of hydrothermal veins within lithified sediments and the igneous basement (Cocos Ridge basalt), was used to reveal the thermal history of Site 344-U1414. Veins in the sedimentary rocks are mainly filled by coarse-grained calcite and subordinately by quartz. Veins within the basalt show polymineralic filling of clay minerals, calcite, aragonite and quartz. Blocky veins with embedded wall rock fragments, appearing in the sediments and in the basalt, indicate hydraulic fracturing. The carbon isotopic composition of the vein calcite suggest the influence of a CO2 -rich fluid mixed with seawater (-3.0 to -0.4‰ V-PDB) and the δ18O values can be differentiated in two groups, depending on the formation temperature (-13.6 to -9.3‰ and -10.8 to -4.7‰ V-PDB). 87Sr/86Sr ratios from the veins confirm the results of the stable isotope analyses, with a higher 87Sr/86Sr ratio close to seawater composition and lower ratios indicating the influence of basalt alteration. The hydrothermal veins contain different types of fluid inclusions with high and low entrapment temperatures and low saline fluids. The occurrence of decrepitated fluid inclusions, formed by increased internal overpressure, is related to isobaric heating. Elongated fluid inclusion planes, arc-like fluid inclusions and low homogenization temperatures suggest subsequent isobaric cooling. The stable isotopic content, strontium isotopic composition

  13. A shape and compositional analysis of ice-rafted debris in cores from IODP Expedition 323 in the Bering Sea

    Science.gov (United States)

    Dadd, Kelsie; Foley, Kristen

    2016-03-01

    Sediment cores recovered during IODP Expedition 323 in the Bering Sea, northern Pacific, contained numerous ice-rafted debris (IRD) clasts up to 85 mm in length. The physical properties (including roundness and sphericity) of 136 clasts from the working half of the cores, a subsample of the total clast number, were analysed and their composition determined using standard petrographic techniques. After removal of pumice and possible fall-in derived material from the clast population, a total of 86 clasts from the original collection were considered to be IRD. While roundness and sphericity vary greatly in the clast population, the IRD are predominately discoid in shape with oblate/prolate indices typically between -5 and 5. There are four time periods over the approximately 4.5 Ma sample interval, 0.36-0.67 Ma, 0.82-1.06 Ma 1.54-1.77 Ma and >3.28 Ma, where there are no IRD in the sample set for sites of the Bering slope, suggesting that these times may have been ice-free. Most clasts show some rounding and are likely to have spent time on beaches with wave action. Wave action on beaches suggests periods of no ice or only seasonal sea-ice. The low roundness values of other clasts, however, suggest they underwent little working and, therefore, the presence of glaciers or more permanent sea-ice at times in those locations. The abundance of rounded and unfaceted clasts as IRD suggests a lack of large ice sheets in the area during cool periods. Clast composition of the IRD is divided into four broad groups, basalt and andesite, granite and metamorphic, sedimentary, and felsic volcanic. The granite and metamorphic and more mature sedimentary lithologies are most likely derived from the Alaskan continental margin, while the extrusive igneous clasts could be derived from a variety of volcanic sources surrounding the Bering Sea, both emergent now or emergent at times of lower sea level. There is only a poor correlation with IRD abundance and marine isotope stages (MIS) for

  14. Biogenic opal production changes in the Gulf of Alaska (IODP Expedition 341 Site U1417) during the Pliocene to Miocene

    Science.gov (United States)

    Khim, B. K.; Kim, S.; Asahi, H.

    2016-12-01

    IODP Expedition 341 Site U1417 (56o57.59'N, 147o6.59'W, 4200 m) is located in the distal Surveyor Fan in the Gulf of Alaska, Northeast Pacific. In this study, we documented biogenic opal content and its mass accumulation rate using a total of 445 sediments from Hole U1417D (below core 43X, 275 CSF-A m) and from Hole U1417E (below core 14R, 465 CSF-A m) which were assigned to Pliocene-Miocene epoch on the basis of shipboard age model. Biogenic opal content and MAR were generally low (<10% and 0.5 g/cm2/kyr, respectively) throughout the core. A significant offset of biogenic opal contents between Site U1417 and Site 887 (54o21.9'N, 148o26.8'W, 3633 m) is observed; much lower at Site U1417. However, biogenic opal content was distinctively high (20 to 40%) at 23 Ma, 15 Ma, 12 Ma, and 8 Ma, which correspond to the lithologic unit changes. These intervals are also characterized by low NGR, MS, and linear sedimentation rate (LSR), indicating the sediment deposition under warm climate/less glacier influence. Thus, the intervals seem to correspond to climatic optimums during the Miocene. Based on terrigenous MAR at Site 887, terrigenous materials supplied by glacial denudation increased greatly since the Northern Hemisphere Glaciation (NHG; 3.5-2.5 Ma). However, Site U1417 shows that high MS representing the terrestrial input occurred far earlier since 8 Ma. It may imply that the formation of glacier in the Gulf of Alaska began earlier or that terrestrial material input was enhanced by sea-ice or turbidite. Intermittent peaks of biogenic opal content and MAR after 8 Ma coincided with the occurrence of cold water/littoral and neritic diatoms and deep cold water radiolarian species, which is likely related to gradual glaciation. Biogenic opal productivity was high during the early Pliocene (5-3.5 Ma), and then it decreased during the NHG.

  15. A "tropical" Early Eocene marine environment on the Antarctic margin: TEX86 results from IODP expedition 318

    Science.gov (United States)

    Bendle, J. A.; Bijl, P.; Toney, J. L.; Pross, J.; Contreras, L.; Schouten, S.; Roehl, U.; Tauxe, L.; Huber, M.; Brinkhuis, H.; Scientific Team of IODP Drilling Leg 318

    2011-12-01

    The early Eocene was characterised by high pCO2 (ca.1,000 to more than 2,000ppm) and mean global temperatures that reached a long-term maximum. Relative to the present day, meridional temperature gradients were unusually low, with warmer equatorial regions and much warmer subtropical Arctic and mid-latitude climates. Yet global climatic conditions during this pre-glacial interval have remained poorly constrained, as only a few temperature records are available portraying the Cenozoic climatic evolution of the high southern latitudes. Here we present dinoflagellate cyst assemblages and organic geochemical tetraether based sea-surface temperature estimates from IODP expedition 318, extracted from bio- and magnetostratigraphically dated, late early to early middle Eocene sediments recovered at Site U1356. For the first time, we reconstruct marine temperatures and ecological conditions from the Eocene Greenhouse world in direct proximity to the Antarctic continent. Early Eocene dinocyst assemblages are dominated by tropical dinocyst genus Apectodinium, whilst TEX86 results indicate persistent and remarkable warmth, with the magnitude of the reconstructed SSTs dependent on the applied calibration: TEX86-L = 20 - 26°C (Av. 23°C); TEX86-H = 27 - 33°C (Av. 32°C). Our marine based proxies are just several strands from multiple independent lines of evidence emerging from the Early Eocene of the Wilkes Land Antarctic margin, including: pollen, terrestrial biomarkers (e.g. MBT/CBT-MAT estimates of 22 - 27°C , Av. 26°C), compound specific plant wax D/H measurements and clay minerals. Taken together, this evidence of very high temperatures, thermophilic fauna, an invigorated hydrological cycle, chemically weathered soils and well developed wetlands gives a very compelling picture of environmental conditions comparable to the modern tropics. These results confirm that exceptionally warm polar-regions are a feature common to reconstructed Greenhouse periods. Such

  16. Oligocene-Miocene Transition in the North Atlantic Interrupted by Warming: New Records from the Newfoundland Margin, IODP Expedition 342

    Science.gov (United States)

    Smith, R.; Liebrand, D.; van Peer, T. E.; Bohaty, S. M.; Friedrich, O.; Bornemann, A.; Blum, P.; Wilson, P. A.

    2016-12-01

    The beginning and end of the Oligocene epoch were marked by major Antarctic glaciation events. While the Eocene-Oligocene transition is known to have initiated sustained major ice sheets on Antarctica, the intensification of glaciation associated with the Oligocene-Miocene Transition (OMT) 23 Ma appears to have been ephemeral. The inference of rapid growth and then retreat of large Antarctic ice sheets on orbital time scales is difficult to reconcile with the strong hysteresis seen in the results of numerical ice sheet model experiments and the modest variability seen in published records of atmospheric CO2. A number of benthic foraminiferal proxy records have been generated at orbital resolution across the OMT, but high-resolution sea-surface records are sparse, particularly in the mid to high latitudes of the northern hemisphere, with none yet produced in the Atlantic Ocean. IODP Site 1406 (40°N, 3799 m water depth, Expedition 342: Newfoundland Sediment Drifts) recovered an interval spanning the OMT in the North Atlantic. We present planktic foraminiferal stable isotope data from this interval (23.5-22.5 Ma) with an average sample spacing of 2 kyrs. Our high-fidelity sea surface record benefits from exceptional `glassy' preservation of clay-hosted foraminifera. Variability in our record shows prominent 100 kyr eccentricity pacing (cycle amplitude typically >1.0 ‰ in δ18O and >0.6‰ in δ13C) and a strong precessional influence. Intriguingly, while the rise in δ18O associated with the OMT is fairly smooth in benthic records, our planktic data show that after over two-thirds of the total 1.6‰ rise in δ18O had already taken place, a 50 kyr recovery to pre-OMT δ18O values occured, preceeding a rapid transition to the OMT δ18O maximum. Our results demonstrate for the first time the North Atlantic sea surface response to OMT events. The structure in our new planktic stable isotope record differs markedly from that seen in published benthic records

  17. IODP Expedition 322 Drills Two Sites to Document Inputs to The Nankai Trough Subduction Zone

    Directory of Open Access Journals (Sweden)

    Yu’suke Kubo

    2010-09-01

    Full Text Available Ocean Drilling Program were to sample and log the incoming sedimentary strata and uppermost igneous basement of the Shikoku Basin, seaward of the Nankai Trough (southwestern Japan. Characterization of these subduction inputs is one piece of the overall science plan for the Nankai Trough Seismogenic Zone Experiment. Before we can assess how various material properties evolve down the dip of the plate interface, and potentially change the fault’s behavior from stable sliding to seismogenic slip, we must determine the initial pre-subduction conditions. Two sites were drilled seaward of the trench to demonstrate how facies characterand sedimentation rates responded to bathymetric architecture. Site C0011 is located on the northwest flank of a prominent basement high (Kashinosaki Knoll, and Site C0012 is located near the crest of the seamount. Even though significant gaps remain in the coring record, and attempts to recover wireline logs at Site C0012 failed, correlations can be made between stratigraphic units at the two sites.Sedimentation rates slowed down throughout the condensed section above the basement high, but the seafloor relief was never high enough during the basin’s evolution to prevent the accumulation of sandy turbidites near the crest of the seamount. We discovered a new stratigraphic unit, the middle Shikoku Basin facies, which is typified by late Miocene volcaniclastic turbidites. The sediment-basalt contact was recovered intact at Site C0012, giving a minimumbasement age of 18.9 Ma. Samples of interstitial water show a familiar freshening trend with depth at Site C0011, but chlorinity values at Site C0012 increase above the values for seawater toward the basement contact. The geochemical trends at Site C0012 are probably a response to hydration reactions in the volcaniclastic sediment and diffusional exchange with seawater-like fluid in the upper igneous basement. These data are important because they finallyestablish an

  18. Textures of water-rich mud sediments from the continental margin offshore Costa Rica (IODP expeditions 334 and 344)

    Science.gov (United States)

    Kuehn, Rebecca; Stipp, Michael; Leiss, Bernd

    2017-04-01

    During sedimentation and burial at continental margins, clay-rich sediments develop crystallographic preferred orientations (textures) depending on the ongoing compaction as well as size distribution and shape fabrics of the grains. Such textures can control the deformational properties of these sediments and hence the strain distribution in active continental margins and also the frictional behavior along and around the plate boundary. Strain-hardening and discontinuous deformation may lead to earthquake nucleation at or below the updip limit of the seismogenic zone. We want to investigate the active continental margin offshore Costa Rica where the oceanic Cocos plate is subducted below the Caribbean plate at a rate of approximately 9 cm per year. The Costa Rica trench is well-known for shallow seismogenesis and tsunami generation. As it is an erosive continental margin, both the incoming sediments from the Nazca plate as well as the slope sediments of the continental margin can be important for earthquake nucleation and faulting causing sea-floor breakage. To investigate texture and composition of the sediments and hence their deformational properties we collected samples from varying depth of 7 different drilling locations across the trench retrieved during IODP expeditions 334 and 344 as part of the Costa Rica Seismogenesis Project (CRISP). Texture analysis was carried out by means of synchrotron diffraction, as only this method is suitable for water-bearing samples. As knowledge on the sediment composition is required as input parameter for the texture data analysis, additional X-ray powder diffraction analysis on the sample material has been carried out. Samples for texture measurements were prepared from the original drill cores using an internally developed cutter which allows to produce cylindrical samples with a diameter of about 1.5 cm. The samples are oriented with respect to the drill core axis. Synchrotron texture measurements were conducted at the

  19. The use of amino acid indices for assessing organic matter quality and microbial abundance in deep-sea Antarctic sediments of IODP Expedition 318

    Science.gov (United States)

    Carr, Stephanie A; Mills, Christopher T.; Mandernack, Kevin W

    2016-01-01

    The Adélie Basin, located offshore of the Wilkes Land margin, experiences unusually high sedimentation rates (~ 2 cm yr− 1) for the Antarctic coast. This study sought to compare depthwise changes in organic matter (OM) quantity and quality with changes in microbial biomass with depth at this high-deposition site and an offshore continental margin site. Sediments from both sites were collected during the International Ocean Drilling (IODP) Program Expedition 318. Viable microbial biomass was estimated from concentrations of bacterial-derived phospholipid fatty acids, while OM quality was assessed using four different amino acid degradation proxies. Concentrations of total hydrolysable amino acids (THAA) measured from the continental margin suggest an oligotrophic environment, with THAA concentrations representing only 2% of total organic carbon with relative proportions of non-protein amino acids β-alanine and γ-aminobutyric acid as high as 40%. In contrast, THAA concentrations from the near-shore Adélie Basin represent 40%–60% of total organic carbon. Concentrations of β-alanine and γ-aminobutyric acid were often below the detection limit and suggest that the OM of the basin as labile. DI values in surface sediments at the Adélie and margin sites were measured to be + 0.78 and − 0.76, reflecting labile and more recalcitrant OM, respectively. Greater DI values in deeper and more anoxic portions of both cores correlated positively with increased relative concentrations of phenylalanine plus tyrosine and may represent a change of redox conditions, rather than OM quality. This suggests that DI values calculated along chemical profiles should be interpreted with caution. THAA concentrations, the percentage of organic carbon (CAA%) and total nitrogen (NAA%) represented by amino acids at both sites demonstrated a significant positive correlation with bacterial abundance estimates. These data suggest that the selective degradation of amino acids, as

  20. Multi-proxy geochemical analyses of Indus Submarine Fan sediments sampled by IODP Expedition 355: implications for sediment provenance and palaeoclimate reconstructions

    Science.gov (United States)

    Bratenkov, Sophia; George, Simon C.; Bendle, James; Liddy, Hannah; Clift, Peter D.; Pandey, Dhananjai K.; Kulhanek, Denise K.; Andò, Sergio; Tiwari, Manish; Khim, Boo-Keun; Griffith, Elizabeth; Steinke, Stephan; Suzuki, Kenta; Lee, Jongmin; Newton, Kate; Tripathi, Shubham; Expedition 355 Scientific Party

    2016-04-01

    The interplay between the development of the Asian summer monsoon and the growth of mountains in South and Central Asia is perhaps the most compelling example of the relationship between climate and the solid Earth. Understanding this relationship is crucial in the context of understanding past changes and for predicting future impacts in the Monsoon region. Both rapid and gradual mountain uplift influence the surrounding environments and regional climate. The sedimentary record of the Indus Fan offers a unique opportunity to study the climatic changes that occurred in South Asia and their link to the intensity of the erosion during the late Cenozoic. Although some paleoclimate reconstructions in the region can be partly addressed by studies onshore, the dominance of erosional processes in such a mountainous region ensures such records are fragmentary and limited in coverage. Thus ocean drilling is the best way to recover long sequences and to test the possible relations among mountain uplift, erosion, sediment deposition and climate (including carbon burial, chemical weathering and CO2 drawdown). The sediments and sedimentary rocks from the Indian continental margin, adjoining the Arabian Sea, were drilled during the International Ocean Discovery Program (IODP) Expedition 355. Drilling operations at Site U1456 penetrated through 1109.4 m of sediment and sedimentary rocks. The oldest sediment recovered at this site is dated to 13.5-17.7 Ma, with about 390 m of mass transport deposit. This study provides a multiproxy approach for palaeoenvironmental reconstructions in the Arabian Sea area. We use a wide variety of organic geochemical data coupled with inorganic chemistry, mineralogy, and isotopic analyses. For direct comparison among various data sets, we divided whole round residue from the interstitial water samples among different laboratories, with each receiving 50-300 g (dry mass). The preliminary results include initial sediment provenance data based on bulk

  1. Palaeobathymetric Interpretations using Foraminiferal Data from the North-west Continental Shelf off Western Australia, IODP Expedition 356

    Science.gov (United States)

    Mamo, B. L.; Renema, W.; Auer, G.; Groeneveld, J.; Gallagher, S. J.; Fulthorpe, C.; Bogus, K.; Expedition 356 Scientists, I.

    2016-12-01

    In 2015, Integrated Ocean Discovery Program Expedition 356 drilled along the passive margin off the West Australian coast to investigate the history of the Indonesian Throughflow (ITF) and its integral role in the development of global thermohaline circulation and climate. Throughout the expedition, a suite of foraminiferal analyses were employed to assess stratigraphy and benthic environments. Planktic foraminifera were primarily used for biostratigraphy and an incredibly diverse benthic fauna ( 260 species) yielded information regarding palaeobathymetric settings and variable conditions at the sediment-water interface. Benthic foraminiferal biofacies are particularly sensitive to changes in environmental conditions and have rapid turnover making them ideal proxies for monitoring physical and chemical changes in marine environments. When these data are combined with a multi-proxy approach incorporating lithostratigraphic and other microfossil data, a robust understanding of past environments can be realised. Stretching from the Northern Carnarvon Basin north to the Roebuck Basin, several distinct biofacies were isolated at sites U1461-U1464 that reveal an array of marine settings and events that span from the Miocene through to the Pleistocene. These features include water depths ranging from Miocene shallows (including larger benthic foraminifera) to Pliocene bathyal depths ( 1000 m), the occurrence of key indicator species for both the Leeuwin Current and the West Pacific Warm Pool (Asterorotalia and Pseudorotalia), and episodes of downslope sediment transport. Here we present the main isolated biofacies, their associated lithofacies and their implications for reconstructing fluctuating sea-level, thermohaline circulation and sediment transport in a changing marine landscape.

  2. IODP Expedition 319, NanTroSEIZE Stage 2: First IODP Riser Drilling Operations and Observatory Installation Towards Understanding Subduction Zone Seismogenesis

    Directory of Open Access Journals (Sweden)

    Sean Toczko

    2010-09-01

    Full Text Available The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE is a major drilling project designed to investigate fault mechanics and the seismogenic behavior of subduction zone plate boundaries. Expedition 319 is the first riser drilling operation within scientific ocean drilling. Operations included riser drilling at Site C0009 in the forearc basin above the plate boundary fault, non-riser drilling at Site C0010 across the shallow part of the megasplay faultsystem—which may slip during plate boundary earthquakes—and initial drilling at Site C0011 (incoming oceanic plate for Expedition 322. At Site C0009, new methods were tested, including analysis of drill mud cuttings and gas, and in situ measurements of stress, pore pressure, and permeability. These results, in conjunction with earlier drilling, will provide a the history of forearc basin development (including links to growth of the megasplay fault system and modern prism, b the first in situ hydrological measurements of the plate boundary hanging wall, and c integration of in situ stress measurements (orientation and magnitude across the forearc and with depth. A vertical seismic profile (VSP experiment provides improved constraints on the deeper structure of the subduction zone. At Site C0010, logging-while-drilling measurements indicate significantchanges in fault zone and hanging wall properties over short (<5 km along-strike distances, suggesting different burial and/or uplift history. The first borehole observatory instruments were installed at Site C0010 to monitor pressure and temperature within the megasplay fault zone, and methods of deployment of more complex observatoryinstruments were tested for future operations.

  3. Rock Magnetic Characterization Through an Intact Sequence of Oceanic Crust, IODP Hole 1256D

    NARCIS (Netherlands)

    Herrero-Bervera, E.; Acton, G.; Krasá, D.; Rodriguez, S.; Dekkers, M.J.

    2011-01-01

    Coring at Site 1256 (6.736◦N, 91.934◦W, 3635 m water depth) during Ocean Drilling Program (ODP) Leg 206 and Integrated Ocean Drilling Program (IODP) Expeditions 309 and 312 successfully sampled a complete section of in situ oceanic crust, including sediments of Seismic Layer 1, lavas and dikes of

  4. IODP Expedition 362: Initial results from drilling the Sumatra subduction zone - the role of input materials in shallow seismogenic slip and forearc plateau development

    Science.gov (United States)

    McNeill, L. C.; Dugan, B.; Petronotis, K. E.; Expedition 362 Scientists, I.

    2016-12-01

    IODP Expedition 362, August-October, 2016, plans to drill two boreholes within the input section of the Indian oceanic plate entering the North Sumatran subduction zone. In 2004, a Mw 9.2 earthquake ruptured the Sunda subduction zone from North Sumatra to the Andaman Islands, a length of 1500 km. The earthquake and tsunami devastated coastal communities around the Indian Ocean. This earthquake and the 2011 Tohoku-Oki Mw 9.0 earthquake showed unexpectedly shallow megathrust slip. In the case of North Sumatra, this shallow slip was focused beneath a distinctive plateau of the accretionary prism. This intriguing seismogenic behavior and forearc structure are not explained by existing models or by observations at other margins where seismogenic slip typically occurs farther landward. Expedition 362 will use core and log data in conjunction with in situ temperature and pressure measurements to document the lithology, structures, and physical and chemical properties of the input sediments. The input materials of the North Sumatran subduction zone are a distinctive, thick (up to 4-5 km) sequence of primarily Bengal-Nicobar Fan-related sediments. This sequence geophysically shows strong evidence for induration and dewatering and has probably reached the temperatures required for sediment-strengthening diagenetic reactions, and input materials may be key to driving the distinctive slip behavior and long-term forearc structure. The plate boundary fault (décollement) originates within the lower pelagic and submarine fan sediments so sampling this interval will help determine what controls décollement development and how its properties evolve. Initial results from the Expedition and plans for post-expedition experiments and modeling will be presented. These methods will be used to predict physical, thermal, fluid, and mechanical properties and diagenetic evolution of the sediments as stresses and temperatures increase due to burial and subduction. Results will be used to

  5. The first microbiological contamination assessment by deep-sea drilling and coring by the D/V Chikyu at the Iheya North hydrothermal field in the Mid-Okinawa Trough (IODP Expedition 331

    Directory of Open Access Journals (Sweden)

    Katsunori eYanagawa

    2013-11-01

    Full Text Available During the Integrated Ocean Drilling Program (IODP Expedition 331 at the Iheya North hydrothermal system in the Mid-Okinawa Trough by the D/V Chikyu, we conducted microbiological contamination tests of the drilling and coring operations. The contamination from the drilling mud fluids was assessed using both perfluorocarbon tracers (PFT and fluorescent microsphere beads. PFT infiltration was detected from the periphery of almost all whole round cores. By contrast, fluorescent microspheres were not detected in hydrothermally active core samples, possibly due to thermal decomposition of the microspheres under high-temperature conditions. Microbial contamination from drilling mud fluids to the core interior subsamples was further characterized by molecular-based evaluation. The microbial 16S rRNA gene phylotype compositions in the drilling mud fluids were mainly composed of sequences of Beta- and Gammaproteobacteria, and Bacteroidetes and not archaeal sequences. The phylotypes that displayed more than 97% similarity to the sequences obtained from the drilling mud fluids were defined as possible contaminants in this study and were detected as minor components of the bacterial phylotype compositions in 13 of 37 core samples. The degree of microbiological contamination was consistent with that determined by the PFT and/or microsphere assessments. This study suggests a constructive approach for evaluation and eliminating microbial contamination during riser-less drilling and coring operations by the D/V Chikyu.

  6. Carbonate and silicate cementation of siliciclastic sediments of the New Jersey shelf (IODP Expedition 313): relation with organic matter diagenesis and submarine groundwater discharge

    Science.gov (United States)

    Pierre, Catherine; Blanc-Valleron, Marie-Madeleine; Boudouma, Omar; Lofi, Johanna

    2017-12-01

    The New Jersey continental shelf extends 150 km off the shoreline. During IODP Expedition 313, siliciclastic deposits of late Eocene to late Pleistocene age were drilled down to 631, 669 and 755 m below seafloor at sites 27A, 28A and 29A respectively in very shallow waters (33.5 to 36 m depth). Pore water salinities display multilayered brackish-salty-brine units 10 to 170 m thick, where low-salinity water is preferentially stored in fine-grained sediments. The sharp boundaries of these buried aquifers are often marked by cemented layers a few centimetres thick. The mineralogy and scanning electron microscope observations of these layers show two phases of cementation by authigenic minerals: (1) the early carbonate cement is frequently associated with pyrite, and (2) the late silicate cement infills the residual porosity. The isotopic compositions of the carbonate cements vary widely: -2.4 weathering of reactive silicate minerals by the CO2-rich pore waters issued from organic matter diagenesis that released bicarbonate, cations and dissolved silica, which were further precipitated as carbonate and silicate cements. The estimated range of temperature (18±4 °C) during carbonate precipitation is consistent with carbonate cementation at moderate burial depths; however, silicate cementation occurred later during diagenesis at deeper burial depths.

  7. Geochemistry of Fast-Spreading Lower Oceanic Crust: Results from Drilling at the Hess Deep Rift (ODP Leg 147 and IODP Expedition 345; East Pacific Rise)

    Science.gov (United States)

    Godard, M.; Falloon, T.; Gillis, K. M.; Akizawa, N.; de Brito Adriao, A.; Koepke, J.; Marks, N.; Meyer, R.; Saha, A.; Garbe-Schoenberg, C. D.

    2014-12-01

    The Hess Deep Rift, where the Cocos Nazca Ridge propagates into the young, fast-spread East Pacific Rise crust, exposes a dismembered, but nearly complete, lower crustal section. The extensive exposures of the plutonic crust were drilled at 3 sites during ODP Leg 147 (Nov. 1992-Jan. 1993) and IODP Expedition 345 (Dec. 2012-Feb. 2013). We report preliminary results of a bulk rock geochemical study (major and trace elements) carried out on 109 samples representative of the different drilled lithologies. The shallowest gabbroic rocks were sampled at ODP Site 894. They comprise gabbronorite, gabbro, olivine gabbro and gabbronorite. They have evolved compositions with Mg# 39-55, Yb 4-8 x chondrite and Eu/Eu* 1-1.6. Olivine gabbro and troctolite were dominant at IODP Site U1415, with minor gabbro, gabbronorite and clinopyroxene oikocryst-bearing troctolite and gabbro. All U1415 gabbroic rocks have primitive compositions except for one gabbronorite rubble that is similar in composition to the shallow gabbros. Olivine gabbro, gabbro and gabbronorite overlap in composition: they have high Mg# (79-87) and Ni (130-570 ppm), low TiO2 (0.1-0.3 wt.%) and Yb (1.3-2.3 x chondrite) and positive Eu anomaly (Eu/Eu*=1.9-2.7). Troctolite has high Mg# (81-89), Ni (260-1500 ppm) and low TiO2 (4). ODP Site 895 recovered sequences of highly depleted harzburgite, dunite and troctolite (Yb down to <0.1xchondrite) that are interpreted as a mantle-crust transition zone. Basalts were recovered at Sites 894 and U1415: they have low Yb (0.5-0.9xN6MORB) and are depleted in the most incompatible elements (Ce/Yb=0.6-0.9xN-MORB). The main geochemical characteristics of Site U1415 and 894 gabbroic rocks are consistent with formation as a cumulate sequence from a common parental MORB melt; troctolites are the most primitive end-member of this sequence. They overlap in composition with the most primitive of slow and fast spread crust gabbroic rocks.

  8. Ecosystem reconstructions for the hinterland of the Atlantic Coastal Plain during the late Mid-Miocene Climatic Optimum (IODP Expedition 313)

    Science.gov (United States)

    Prader, Sabine; Kotthoff, Ulrich; McCarthy, Francine; Greenwood, David

    2016-04-01

    During IODP Expedition 313, cores from three Sites (313-M0027, M0028, and M0029) from the New Jersey shallow shelf (water depth approximately 35 m) were retrieved in 2009. We have investigated the palynology of sediment cores from Site M0027, 45 km off the present-day coast of New Jersey in order to reconstruct environmental and climate change in the region during the second half of the Mid-Miocene Climatic Optimum (MMCO) and the subsequent transition to cooler conditions (ca. 15 to 13 million years before present). Transport-caused bias of the pollen assemblages was identified via the analysis of the terrestrial/marine palynomorph ratio and these results were considered when interpreting palaeo-vegetation from the pollen data. Pollen preservation in the interval analyzed herein was generally very good. Pollen grains were analyzed via both light and scanning electron microscopy. In the analyzed samples, angiosperm tree pollen grains were most abundant and probably formed the main vegetation zone in the lowland during the MMCO. The pollen-based results point to the presence of a deciduous-evergreen mixed forest that was characterised by e.g. Quercus, Carya, Liquidambar, Juglans, Pterocarya, Tilia, Engelhardia. Frequent conifer pollen grains indicate that highland forests with e.g. Pinus, Cathaya, and Picea were present the hinterland of the New Jersey shelf. Typical wetland elements like Nyssa and Taxodium as well as herbal taxa like Polygonum and Polygala were generally rare. The pollen-based climate reconstructions for the hinterland oft the New Jersey shallow shelf document a warm temperate climate without winterfrost and relatively high precipitation through the year during this time. Our results imply that the vegetation and regional climate in the hinterland of the New Jersey shelf did not react as sensitively to the cooling phase following the MMCO as other regions in North America or Europe.

  9. IODP Expedition 339 in the Gulf of Cadiz and off West Iberia: decoding the environmental significance of the Mediterranean outflow water and its global influence

    Science.gov (United States)

    Hernández-Molina, F. J.; Stow, D.; Alvarez-Zarikian, C.

    2013-11-01

    IODP Expedition 339 drilled five sites in the Gulf of Cadiz and two off the west Iberian margin (November 2011 to January 2012), and recovered 5.5 km of sediment cores with an average recovery of 86.4%. The Gulf of Cadiz was targeted for drilling as a key location for the investigation of Mediterranean outflow water (MOW) through the Gibraltar Gateway and its influence on global circulation and climate. It is also a prime area for understanding the effects of tectonic activity on evolution of the Gibraltar Gateway and on margin sedimentation. We penetrated into the Miocene at two different sites and established a strong signal of MOW in the sedimentary record of the Gulf of Cadiz, following the opening of the Gibraltar Gateway. Preliminary results show the initiation of contourite deposition at 4.2-4.5 Ma, although subsequent research will establish whether this dates the onset of MOW. The Pliocene succession, penetrated at four sites, shows low bottom current activity linked with a weak MOW. Significant widespread unconformities, present in all sites but with hiatuses of variable duration, are interpreted as a signal of intensified MOW, coupled with flow confinement. The Quaternary succession shows a much more pronounced phase of contourite drift development, with two periods of MOW intensification separated by a widespread unconformity. Following this, the final phase of drift evolution established the contourite depositional system (CDS) architecture we see today. There is a significant climate control on this evolution of MOW and bottom-current activity. However, from the closure of the Atlantic-Mediterranean gateways in Spain and Morocco just over 6 Ma and the opening of the Gibraltar Gateway at 5.3 Ma, there has been an even stronger tectonic control on margin development, downslope sediment transport and contourite drift evolution. The Gulf of Cadiz is the world's premier contourite laboratory and thus presents an ideal testing ground for the contourite

  10. The Pacific Equatorial Age Transect, IODP Expeditions 320 and 321: Building a 50-Million-Year-Long Environmental Record of the Equatorial Pacific Ocean

    Directory of Open Access Journals (Sweden)

    Kusali Gamage

    2010-04-01

    Full Text Available In March 2009, the R/V JOIDES Resolution returned to operations after its extended refit and began with a drilling program ideally suited to its drilling strengths, the Pacific Equatorial Age Transect (PEAT, IODP Exp 320/321; Fig. 1A. The PEAT drilling program was developed to understand how a major oceanic region evolved over the Cenozoic Era(65–0 Ma and how it interacted with global climate. It specifically targeted the interval between 52 Ma and 0 Ma and drilled a series of sites that originated on the paleoequator. These sites have since been moved to the northwest by plate tectonics.The equatorial Pacific is an important target for paleocean ographic study because it is a significant ‘cog’ in the Earth’s climate machine, representing roughly half of the total tropical oceans that in turn represent roughly half of the total global ocean area. Prior drilling in both the Deep Sea Drilling Project (DSDP and the Ocean Drilling Program (ODP outlined the changes that have occurred through the Cenozoic (e.g., van Andel et al., 1975; Pisias et al., 1995. Not only did the earlier work fail to cover sufficient timeintervals but also many of the sites were cored with ‘first-generation’ scientific drilling technology with incomplete and disturbed sediment recovery and thus cannot be used for detailed studies.

  11. Interactions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: Results from IODP Expedition 316 Sites C0006 and C0007

    Science.gov (United States)

    Screaton, E.; Kimura, G.; Curewitz, D.; Moore, G.; Chester, F.; Fabbri, O.; Fergusson, C.; Girault, F.; Goldsby, D.; Harris, R.; Inagaki, F.; Jiang, T.; Kitamura, Y.; Knuth, M.; Li, C.-F.; Liljedahl, L. Claesson; Louis, L.; Milliken, K.; Nicholson, U.; Riedinger, N.; Sakaguchi, A.; Solomon, E.; Strasser, M.; Su, X.; Tsutsumi, A.; Yamaguchi, A.; Ujiee, K.; Zhao, X.

    2009-12-01

    Integrated Ocean Drilling Program (IODP) Expedition 316 Sites C0006 and C0007 examined the deformation front of the Nankai accretionary prism offshore the Kii Peninsula, Japan. In the drilling area, the frontal thrust shows unusual behavior as compared to other regions of the Nankai Trough. Drilling results, integrated with observations from seismic reflection profiles, suggest that the frontal thrust has been active since ˜0.78-0.436 Ma and accommodated ˜13 to 34% of the estimated plate convergence during that time. The remainder has likely been distributed among out-of-sequence thrusts further landward and/or accommodated through diffuse shortening. Unlike results of previous drilling on the Nankai margin, porosity data provide no indication of undercompaction beneath thrust faults. Furthermore, pore water geochemistry data lack clear indicators of fluid flow from depth. These differences may be related to coarser material with higher permeability or more complex patterns of faulting that could potentially provide more avenues for fluid escape. In turn, fluid pressures may affect deformation. Well-drained, sand-rich material under the frontal thrust could have increased fault strength and helped to maintain a large taper angle near the toe. Recent resumption of normal frontal imbrication is inferred from seismic reflection data. Associated décollement propagation into weaker sediments at depth may help explain evidence for recent slope failures within the frontal thrust region. This evidence consists of seafloor bathymetry, normal faults documented in cores, and low porosities in near surface sediments that suggest removal of overlying material. Overall, results provide insight into the complex interactions between incoming materials, deformation, and fluids in the frontal thrust region.

  12. Reconstructing Holocene palaeo-environmental conditions in the Baltic: A multi-proxy comparison from the Little Belt (IODP Expedition 347, Site M0059)

    Science.gov (United States)

    Kotthoff, Ulrich; Andrén, Elinor; Andrén, Thomas; Ash, Jeanine; Bauersachs, Thorsten; Fanget, Anne-Sophie; Granoszewski, Wojciech; Groeneveld, Jeroen; Krupinski, Nadine; Peyron, Odile; Slomp, Caroline; Stepanova, Anna; Warnock, Jonathan; van Helmond, Niels; Expedition 347 Science Party

    2016-04-01

    Some of the largest marine environmental impacts from ongoing global climate change are occurring in continental shelf seas and enclosed basins, including severe oxygen depletion, intensifying stratification, and increasing temperatures. In order to predict future changes in water mass conditions, it is essential to reconstruct how these conditions have changed in the past against the background of climate changes. The brackish Baltic Sea is one of the largest semi-enclosed basins worldwide, and its sediment records provide a unique opportunity to analyse palaeo-environmental and climate change in central and northern Europe. IODP Expedition 347 recovered an exceptional set of sediment cores from the Baltic Sea which allow high-resolution reconstructions in unprecedented quality. We present a comparison of commonly-used proxies to reconstruct palaeoecosystems, -temperatures, and -salinity from IODP Site M0059 in the Little Belt over the past ˜8000 years. Our aim is to reconstruct the development of the terrestrial and marine ecosystems in the research area and the related environmental conditions, and to identify potential limitations of individual proxies. The age model for Site M0059 is based on 14Cdating, biostratigraphic correlation with neighbouring terrestrial pollen records, and sediment stratigraphy. Sedimentary organic carbon content and the bulk elemental composition have been measured, and can be used to determine the depositional environment and degree of oxygen depletion (e.g., Mo, Corg/Ptot). Pollen is used as proxy for vegetation development in the hinterland of the southern Baltic Sea and as a land/air-temperature proxy. Comparison with dinoflagellate cysts, insect remains, and green algae remains from the same samples provides a direct land-sea comparison. The application of the modern analogues technique to pollen assemblages has previously yielded precise results for late Pleistocene and Holocene datasets, including specific information on

  13. Deep-sea trace fossil and benthic foraminiferal assemblages across glacial Terminations 1, 2 and 4 at the "Shackleton Site" (IODP Expedition 339, Site U1385)

    Science.gov (United States)

    Rodríguez-Tovar, Francisco J.; Dorador, Javier; Grunert, Patrick; Hodell, David

    2015-10-01

    Numerous studies focused on the transitions between glacial and interglacial periods, the so-called terminations, due to the associated significant reorganizations of the ocean-atmosphere system. However, analyses combining macro- and micropaleontological information are near absent. In this research, an integrative study of trace fossils and benthic foraminiferal assemblages is conducted in order to improve the characterization of Terminations 1, 2 and 4, as revealing the response of the macro-and microbenthic habitats to the involved paleoenvironmental changes. For this purpose, selected cores from Site U1385 (IODP Expedition 339) located off the western Iberian Margin, have been studied. Changes in trace fossils and benthic foraminifera related to both long-term variations at the glacial/interglacial scale, and short-term millennial-scale climatic events. Food and oxygen availability have been identified as the main factors determining variations in the macro- and microbenthic community structure across glacial terminations in the context of changes in water mass distribution and productivity in the NE Atlantic. A deep-sea multi-tiered tracemaker community, consisting of biodeformational structures, Chondrites, ?Nereites, Palaeophycus, Planolites, Thalassinoides, and Zoophycos, suggest generally well-oxygenated bottom and pore-water conditions during interglacial as well as glacial intervals, with punctual decreases in oxygenation. Short-climatic events registered during Terminations 1, 2, and 4 induce a similar response of trace fossil and benthic foraminifera communities to the variable incidence of food and oxygen availability. Termination 1 shows a severe deterioration of oxic conditions and increasing food availability during the YD and HS 1, favoring appearance/dominance of Zoophycos, together with the lowest miliolid and the highest deep infaunal taxa abundances. Short-term climatic events (HS 11, IRE 10.1) associated with Terminations 2 and 4 are

  14. IODP: Facilitating Multidisciplinary Collaboration in Subseafloor Investigations

    Science.gov (United States)

    Meth, C. E.; Koppers, A. A.; Screaton, E.

    2012-12-01

    The Integrated Ocean Drilling Program (IODP) is an international marine research program that brings to the surface new insights into climate and environmental change, tectonics and earthquake genesis, and the nature of life in extreme environments. The program crosses disciplines, international boundaries, and generations in a collaborative effort to collect subseafloor cores and data for studying the planet. A recent survey of the U.S. scientific ocean drilling community defines the breadth and research diversity of the scientists involved in this innovative program. In total, 433 scientists responded, representing 117 universities, institutions, businesses, and government agencies located in 39 states and Washington, DC. A particularly striking statistic is that 44% of the respondents are students or early career researchers who finished their Ph.D. within the past 10 years. Respondents were asked to identify with which of the main IODP research themes they most closely identified. With 31% selecting more than one theme, it is clear that many are taking a truly interdisciplinary approach to their research. More than half (51%) of the respondents have never sailed on an expedition, showing that the use and impact of scientific ocean drilling data reaches far beyond the confines of one expedition and the scientists directly involved therein. These data paint a picture of a broad community that is engaged and ready to embrace future research challenges. By understanding the demographics and interests of a research community - especially diverse communities focused on large research programs - program managers can better develop mechanisms to facilitate collaborations and use resources efficiently.

  15. Refining the Bengal Fan stratigraphy - A first correlation of IODP Expedition 354 results and seismic data from the Bay of Bengal

    Science.gov (United States)

    Schwenk, Tilmann; Spiess, Volkhard; Bergmann, Fenna; France-Lanord, Christian; Klaus, Adam

    2016-04-01

    The Bengal Fan covers the floor of the entire Bay of Bengal from the continental margins of India and Bangladesh to the sediment-filled Sunda Trench off Myanmar and the Andaman Islands, and along the west side of the Ninetyeast Ridge. The deposition and progradation of the Bengal Fan started in the Eocene after the collision of India with Asia resulting in the build-up of the Himalaya and the formation of a large proto-Bay of Bengal. Continued convergence of the Indian and Australian plates with the Southeast Asian plate reduced the size of the bay and focused the source of turbidites finally into the present Bengal Basin, Bangladesh shelf, and the shelf canyon "Swatch of no Ground". Today, the Bengal Fan is mainly fed by the sediment load of the Ganges and Brahmaputra rivers, which drain the Himalayas at its southern and northern slope, respectively, and deliver their load to the delta in the Bengal Basin, to the Bengal Shelf and to the deep sea fan. Thus the Bengal Fan is a suitable recorder to study interactions among the growth of the Himalaya and Tibet, the development of the Asian monsoon, and processes affecting the carbon cycle and global climate. Because sedimentation in the Bengal Fan responds to both, climate and tectonic processes, its terrigenous sediment records the past evolution of both the Himalaya and regional climate. This evolution is also expressed in the stratigraphy of the fan in terms of unconformities and key horizons, average sedimentation rates as a function of distance from the basement ridges at 85°E and 90°E and the presence or absence of channel-levee systems. The histories of the Himalaya/Tibetan system and the Asian monsoon require sampling different periods of time with different levels of precision. Therefore IODP Expedition 354 drilled in February-March 2015 a seven site, 320 km-long transect across the Bengal Fan at 8°N. This strategy has been chosen because sediment transport took place by turbidity currents following

  16. New insights into the radiocarbon calibration based on 14C and U-Th dating of corals drilled offshore Tahiti (IODP Expedition #310)

    Science.gov (United States)

    Durand, Nicolas; Deschamps, Pierre; Bard, Edouard; Hamelin, Bruno; Camoin, Gilbert; Thomas, Alexander L.; Henderson, Gideon M.; Yokoyama, Yusuke

    2010-05-01

    Beyond the high-precision tree-ring calibration, the fossil corals are the most reliable archive that can be used to calibrate the radiocarbon time scale. In this contribution, we present a new radiocarbon dataset based on paired 14C and U-Th dating of fossil shallow-water tropical corals drilled offshore Tahiti during the IODP Expedition 310 'Tahiti Sea-Level'. Before 14C and U-Th analyses, rigorous screening criteria have been applied in order to select pristine aragonitic coral skeletons and avoid those displaying any post-mortem diagenesis that alters original ages. In particular, we made a significant effort to improve detection and quantification of very small amount of secondary calcite in the aragonitic coral lattice using X-ray diffraction measurements [1]. In addition, we apply a strict screening criterion based on δ234U. However, the new Tahiti dataset allow to refine the previous tolerance ranges previously adopted. More than 60 radiocarbon dates were processed at the Laboratoire de Mesure du Carbone 14 (Saclay, France) with the ARTEMIS AMS facility. This new Tahiti record provides new data to the radiocarbon calibration for two distinct time windows: for the interval between 29,200 and 36,200 years BP and for the last deglaciation period, with especially, a higher resolution (40 data) for the 14,000 - 16,000 years BP time interval. These new data extend the previous Tahiti record beyond 13,900 years BP which was the oldest U-Th age obtained on cores drilled onshore in the modern Tahiti barrier reef [2, 3]. These new results are compared with 14C chronologies from other corals, those of Barbados [4, 5] and those from other Pacific islands (Mururoa, Vanuatu, Marquesas, Christmas), and from the Cariaco Basin sediment [6, 7], the Iberian Margin sediment [8, 9] and the Bahamian speleothem [10] records. The new 14C dataset from the corals drilled offshore Tahiti allows to validate the precision and accuracy of other records either directly dated by U-Th or

  17. ECORD-IODP new opportunities in sub-seafloor investigation

    Science.gov (United States)

    Camoin, G.; Mevel, C.; Gatliff, R.; McInroy, D.

    2012-04-01

    Scientific ocean drilling has traditionally been conducted within a framework of international programmes. The current phase, IODP (Integrated Ocean Drilling Program), started in 2004. As opposed to its predecessors, IODP has a multiplatform approach allowing to encompass most oceanic environments and therefore expands the scientific opportunities. USA operates the non-riser vessel JOIDES Resolution. Japan operates the Chikyu, a vessel specially built for scientific purposes and equipped with a riser system that allows drilling in unstable formation and down to ~6 km beneath the seafloor. The creation of ECORD (European Consortium for Ocean Research Drilling), consortium of 16 (now 17) European countries and Canada that joined IODP as a single member, made possible the development of the concept of Mission Specific Platforms (MSPs). MSPs are platforms of opportunity contracted on a case by case basis that have allowed scientific ocean drilling to recover cores from ice-covered and shallow water targets that are generally inaccessible to the two dedicated IODP platforms. The current phase of IODP is ending in September 2013 and the new phase of ocean drilling is being prepared. A new science plan, elaborated by the international science community, was released in June 2011: http://www.iodp.org/Science-Plan-for-2013-2023/. The three current major players (USA, Japan and ECORD) are willing to participate in the next phase and continue providing access to all three platforms, although final funding decisions are still pending at the national level. The new organizational framework for scientific ocean drilling will be streamlined for a more efficient proposal review system and a better use of resources. An international evaluation for drilling proposals will be maintained, but the platforms will be operated independently by the country/consortia providing them. At the ECORD level, the new organisation may secure more funding for MSP operations and the goal is to

  18. Benthic Biotic Response to Climate Changes over the Last 700,000 Years, the Sea of Japan: Ostracode Assemblages from Site U1427, IODP Expedition 346

    Science.gov (United States)

    Huang, H. H. M.; Yasuhara, M.; Iwatani, H.; Alvarez Zarikian, C. A.; Bassetti, M. A.; Sagawa, T.

    2016-12-01

    The Sea of Japan is a marginal sea, semi-enclosed by the Eurasian Continent, Korean Peninsula, Japanese Islands, and shallow straits (water depth influence of TWC. Here we present 700,000-year record of benthic biotic response to the paleoceanographic changes in the southern Sea of Japan based on ostracode assemblage reconstruction at IODP Site U1427. Five local extinction events were caused by extreme bottom conditions (mainly oxygen depletion) during the Ice Age Terminations I, II, IV, V, and VII. Primary and secondary ostracode assemblages were revealed by Q-mode k-means clustering, CABFAC factor analysis, and non-metric multidimensional scaling. The primary ostracode components, characterized by Krithe sawanensis and Cytheropteron hyalinosa, broadly reflect glacial/interglacial and high-latitude insolation cycles. In contrast, a faunal shift determined by the secondary faunal components was driven by the TWC enhancement at 300 ka.

  19. IODP New Ventures in Exploring Scientific Targets (INVEST: Defining the New Goals of an International Drilling Program

    Directory of Open Access Journals (Sweden)

    Fumio Inagaki

    2010-04-01

    Full Text Available The INVEST conference, an international meeting to define the scientific goals and required technology for a new ocean drilling program, was held at the University of Bremen on 22–25 September 2009. Based on the large attendance and vigorous engagement of scientists in the discussion of new science/technology ideas, INVEST was extremely successful. Initially 400 participants were expected, but the INVEST steering and organization committees were thrilled to see a much larger number of scientists flock to Bremen to demonstrate their support and enthusiasm for the continuation of an international scientific ocean drilling program. In all, 584 participants, including sixty-four students, from twenty-one nations and >200 institutions and agencies attended the INVEST conference. Contributions to INVEST included 103 submitted white papers that were posted on the INVEST webpage (http://www.marum.de/iodp-invest. html, and breakout discussions in fifty working groups that focused on a range of topics during the course of the conference. In addition, students and early career scientists, as well as national funding agency managers and platform providers, presented a total of eighty-six posters. Interspersed with the working group and plenary sessions were twelve keynote lectures, chosen to highlight overarching themes and new directions in research and technology.

  20. Proceedings of the Integrated Ocean Drilling Program Vol. 341: Expedition reports Southern Alaska margin

    Digital Repository Service at National Institute of Oceanography (India)

    Jaeger, J.M.; Gulick, S.P.S.; Le; Asahi, H.; Bahlburg, H.; Belanger, C.L.; Berbel, G.B.B.; Childress, L.B.; Cowan, E.A.; Drab, L.; Forwick, M.; Fukumura, A.; Ge, S.; Gupta, S.M.; et

    ). Deposition of the eroded sediments in the outer part of an orogen can, in J.M. Jaeger et al. Expedition 341 summary Proc. IODP | Volume 341 4 turn, suppress deformation due to loading (e.g., Simpson, 2010; Worthington et al., 2010). A critical question... al., 1994; En- kelmann et al., 2008; Perry et al., 2009; Witmer et al., 2009). Physical and oceanographic setting The morphology of the Gulf of Alaska shelf has been strongly influenced by active tectonics and glacial deposition overprinted by glacial...

  1. Expeditions to Drill Atlantic, Gulf of Mexico, and Pacific Sites

    Science.gov (United States)

    Coffin, Millard F.

    2005-04-01

    The Integrated Ocean Drilling Program (IODP), an international collaboration of Earth, ocean, and life scientists that began in 2003, offers scientists worldwide unprecedented opportunities to address a vast array of scientific problems in all submarine settings. Recently, the scientific advisory structure of the proposal-driven IODP scheduled drilling expeditions, targeting critical scientific problems in the Atlantic Ocean, Gulf of Mexico, and Pacific Ocean, for 2005 and early 2006 (Figure 1, Table 1). The IODP, which is co-led by Japan and the United States, with strong contributions from the European Consortium for Ocean Research Drilling (ECORD) and China, is guided by an initial science plan, ``Earth, Oceans, and Life'' (www.iodp.org). For the first time, through the IODP, scientists have at their disposal both a riser (drilling vessel which has a metal tube surrounding the drill pipe that enables the return of drilling fluid and cuttings to the drill ship; the ``riser'' is attached to a ``blow-out preventer'' or shut-off device at the seafloor) and riserless drilling vessel (which lacks a riser pipe and blow-out preventer), as well as mission-specific capabilities such as drilling barges and jack-up rigs for shallow-water and Arctic drilling.

  2. Phosphorus burial and diagenesis in the central Bering Sea (Bowers Ridge, IODP Site U1341): Perspectives on the marine P cycle

    OpenAIRE

    März, C; Poulton, SW; Wagner, T; Schnetger, B; Brumsack, H-J

    2014-01-01

    To reconstruct the cycling of reactive phosphorus (P) in the Bering Sea, a P speciation record covering the last ~4Ma was generated from sediments recovered during Integrated Ocean Drilling Program (IODP) Expedition 323 at Site U1341 (Bowers Ridge). A chemical extraction procedure distinguishing between different operationally defined P fractions provides new insight into reactive P input, burial and diagenetic transformations. Reactive P mass accumulation rates (MARs) are ~20-110μmol/cm/ka, ...

  3. Occurrences of Orthopyroxene in the "Multi-textured" Layered Gabbros from the Hess Deep Rift, East Pacific Rise (the Site U1415P, IODP Expedition 345)

    Science.gov (United States)

    Hoshide, T.; Machi, S.; Maeda, J. I.

    2015-12-01

    IODP Exp.345 drilled three main holes (Holes U1415 I, J & P) from the lowermost plutonic crust exposed at the Hess Deep Rift, East Pacific Rise and primitive layered gabbroic rocks were newly discovered from these holes (Gillis et al., 2014). One of the mysteries about the layered gabbros is the fact that Opx, which is considered to appear in the late stage of crystallization on the basis of crystallization experiments of MORB, occurs as a dominant phase in many of the layered gabbros. In this presentation, we report the occurrence of Opx from the Hole U1415P and consider the significance of Opx in the origin of the layered gabbros. Hole U1415P (about 100m in thickness) is divided into two units, the upper Multi-textured Layered Gabbro Series (MLGS) and lower Troctolite Series (TS). Gabbroic rocks from the MLGS contain Opx (< 4 vol%) and are macroscopically classified into Opx-bearing olivine gabbro. However, these rocks are mesoscopically (on cm scale) inhomogeneous and have a great variation of mode, grain size and texture. On the other hand, TS consists of homogeneous troctolites and Opx rarely occurs in the series. The occurrences of Opx from the MLGS are as follows: (i) coarse-grained Opx+Cpx+Pl vein parallel to the layered structure of the surrounding troctolite (ii) undeformed Opx+Pl veinlets in kinked Ol (iii) Opx in the concave of anhedral Ol (iv) Opx rimming Cr-spl crystals in contact with Ol. The occurrence of Opx like (ii) and (iii) resembles the texture which is considered to be formed by the reaction between mantle peridotite and a SiO2-saturated melt (e.g, Piccardo et al., 2007). The facts that Opx is often found in association with Cr-spl and Cr-spl lamellae occur in pyroxenes of the Opx+Cpx+Pl vein suggest that the SiO2-saturated melt which reacted with Ol was rich in chromium. In addition, Cr-spl crystals rimmed by Opx contain multiphase-solid inclusions. The inclusions should be key in understanding the chemical composition of the reacted melt.

  4. Using DSDP/ODP/IODP core photographs and digital images in the classroom

    Science.gov (United States)

    Pereira, Hélder; Berenguer, Jean-Luc

    2017-04-01

    Since the late 1960's, several scientific ocean drilling programmes have been uncovering the history of the Earth hidden beneath the seafloor. The adventure began in 1968 with the Deep Sea Drilling Project (DSDP) and its special drill ship, the Glomar Challenger. The next stage was the Ocean Drilling Program (ODP) launched in 1985 with a new drill ship, the JOIDES Resolution. The exploration of the ocean seafloor continued, between 2003 and 2013, through the Integrated Ocean Drilling Program (IODP). During that time, in addition to the JOIDES Resolution, operated by the US, the scientists had at their service the Chikyu, operated by Japan, and Mission-Specific-Platforms, funded and implemented by the European Consortium for Ocean Research Drilling. Currently, scientific ocean drilling continues through the collaboration of scientists from 25 nations within the International Ocean Discovery Program (IODP). Over the last 50 years, the scientific ocean drilling expeditions conducted by these programmes have drilled and cored more than 3500 holes. The numerous sediment and rock samples recovered from the ocean floor have provided important insight on the active biological, chemical, and geological processes that have shaped the Earth over millions of years. During an expedition, once the 9.5-meter long cores arrive from the seafloor, the technicians label and cut them into 1.5-meter sections. Next, the shipboard scientists perform several analysis using non-destructive methods. Afterward, the technicians split the cores into two halves, the "working half", which scientists sample and use aboard the drilling platform, and the "archive half", which is kept in untouched condition after being visually described and photographed with a digital imaging system. The shipboard photographer also takes several close-up pictures of the archive-half core sections. This work presents some examples of how teachers can use DSDP/ODP/IODP core photographs and digital images, available

  5. Variability of the intensity of the Tsushima Warm Current and bottom water ventilation in western North Pacific marginal seas during the Pleistocene: Preliminary results from IODP Expedition 346 (Sites U1427 and U1428) based on ostracod assemblages

    Science.gov (United States)

    Alvarez Zarikian, Carlos A.; Bassetti, Maria-Angela; Toucanne, Samuel; Sagawa, Takuya; Holbourn, Ann; Yasuhara, Moriaki; Tada, Ryuji; Murray, Richard W.

    2015-04-01

    IODP Expedition 346 drilled Sites U1427 and U1428 in ideal locations to monitor changes in (i) the intensity of the influx of the Tsushima Warm Current (TWC), and (ii) the intermediate bottom water ventilation from a few hundred thousand years to over a million years in the western North Pacific marginal seas. Site U1427 is located at 330 m water depth in the marginal sea bordered by the Eurasian continent, the Korean peninsula and the Japanese Islands. This semi-enclosed marginal sea has an average water depth of 1350 m and is connected with other marginal seas in the region by shallow, narrow straits. Site U1428 is located at 724 m in the East China Sea and this region is more influenced by continental freshwater runoff derived from the Yangtze River. Both sites are in the path of the TWC, a branch of the Kuroshio Current, the only warm current flowing into the marginal sea west of Japan. The TWC carries both water originating from the subtropical North Pacific and fresher runoff water derived from East China Sea continental shelf. The northerly flow of the TWC through the shallow Tsushima Strait is ultimately controlled by relative sea level variations over time. The Japan Sea Intermediate Water (JSIW), found below the TWC between 200 and 400-500 m water depth, corresponds to a vertical salinity minimum, and has relatively high oxygen concentration related to the deep-water convection in winter and linked to fresh water supply during winter monsoon intervals. Recent observations point to variations in the intensity of deep and intermediate water currents during glacials and interglacials, and millennial scale climate cycles, but the mechanisms of such variations are not fully known. Here we present preliminary results based on microfossil faunal (ostracods) and sedimentological (sortable silt) proxies that show variability in the intensity of bottom water circulation and environmental conditions during the Pleistocene. Ostracods (benthic microcrustaceans known

  6. Arctic Ocean Paleoceanography and Future IODP Drilling

    Science.gov (United States)

    Stein, Ruediger

    2015-04-01

    Although the Arctic Ocean is a major player in the global climate/earth system, this region is one of the last major physiographic provinces on Earth where the short- and long-term geological history is still poorly known. This lack in knowledge is mainly due to the major technological/logistical problems in operating within the permanently ice-covered Arctic region which makes it difficult to retrieve long and undisturbed sediment cores. Prior to 2004, in the central Arctic Ocean piston and gravity coring was mainly restricted to obtaining near-surface sediments, i.e., only the upper 15 m could be sampled. Thus, all studies were restricted to the late Pliocene/Quaternary time interval, with a few exceptions. These include the four short cores obtained by gravity coring from drifting ice floes over the Alpha Ridge, where older pre-Neogene organic-carbon-rich muds and laminated biosiliceous oozes were sampled. Continuous central Arctic Ocean sedimentary records, allowing a development of chronologic sequences of climate and environmental change through Cenozoic times and a comparison with global climate records, however, were missing prior to the IODP Expedition 302 (Arctic Ocean Coring Expedition - ACEX), the first scientific drilling in the central Arctic Ocean. By studying the unique ACEX sequence, a large number of scientific discoveries that describe previously unknown Arctic paleoenvironments, were obtained during the last decade (for most recent review and references see Stein et al., 2014). While these results from ACEX were unprecedented, key questions related to the climate history of the Arctic Ocean remain unanswered, in part because of poor core recovery, and in part because of the possible presence of a major mid-Cenozoic hiatus or interval of starved sedimentation within the ACEX record. In order to fill this gap in knowledge, international, multidisciplinary expeditions and projects for scientific drilling/coring in the Arctic Ocean are needed. Key

  7. Geothermal policy development program: expediting the local geothermal permitting process

    Energy Technology Data Exchange (ETDEWEB)

    1981-07-01

    For a number of years, concerns have been raised about the length of time and the complexity involved in obtaining required permits in order to develop the geothermal resource at the Geysers. Perhaps the most important factor is jurisdiction. At the Geysers, all three levels of government - local, state, and federal - exercise significant authority over various aspects of geothermal development. In addition, several agencies within each governmental level play an active role in the permitting process. The present study is concerned primarily with the local permitting process, and the ways in which this process could be expedited. This report begins by looking at the local role in the overall permitting process, and then reviews the findings and conclusions that have been reached in other studies of the problem. This is followed by a case study evaluation of recent permitting experience in the four Geysers-Calistoga KGRA counties, and the report concludes by outlining several approaches to expediting the local permitting process.

  8. Development of a glacially dominated shelf-slope-fan system in tectonically active southeast Alaska: Results of IODP Expedition 341 core-log-seismic integrated studies at glacial cycle resolution

    Science.gov (United States)

    Gulick, Sean; Jaeger, John; Mix, Alan; Swartz, John; Worthington, Lindsay; Reece, Robert

    2014-05-01

    Collision of the Yakutat microplate with North American formed the St. Elias Mountains in coastal Gulf of Alaska. While the tectonic driver for orogenesis has been ongoing since the Miocene, results from the Integrated Ocean Drilling Program Expedition 341 suggests that direct climatic perturbation of active orogenesis through glacial erosion is non-linear. Geophysical studies of the glaciated continental margin, slope, and adjacent deep-sea Surveyor Fan allow examination of the glaciated orogen from source to sink. Using high-resolution and crustal-scale seismic data and through comparison with other glaciated margins, we can identify key diagnostic seismic morphologies and facies indicative of glacial proximity and sediment routing. Expedition drilling results calibrated these images suggesting a timeline for initial advances of the Cordilleran ice sheet related glacial systems onto the shelf and a further timeline for the development of ice streams that reach the shelf edge. Comparisons can be made within this single margin between evolution of the tectonic-glacial system where erosion and sediment transport are occurring within a fold and thrust belt versus on a more stable shelf region. Onshore the Bering-Bagley glacial system in the west flows across the Yakataga fold and thrust belt, allowing examination of whether glacial erosion can cause tectonic feedbacks, whereas offshore the Bering-Bagley system interacts with the Pamplona Zone thrusts in a region of significant sediment accommodation. Results from Expedition 341 imply that timing of glacial advance to the shelf edge in this region may be driven by the necessity of filling up the accommodation through aggradation followed by progradation and thus is autogenic. In contrast the Malaspina-Hubbard glacial system to the east encountered significantly less accommodation and more directly responded to climatic forcing including showing outer shelf glacial occupation since the mid-Pleistocene transition-MPT to

  9. Drilling Polar Oceans with the European Research Icebreaker AURORA BOREALIS: the IODP Context

    Science.gov (United States)

    Lembke-Jene, Lester; Wolff-Boenisch, Bonnie; Azzolini, Roberto; Thiede, Joern; Biebow, Nicole; Eldholm, Olav; Egerton, Paul

    2010-05-01

    -European partners), a multidisciplinary platform for studies ranging from the sub-seafloor into the atmosphere. AURORA BOREALIS was planned for her role in deep-sea drilling in consultation with engineers and technical experts familiar with the program and the operation of these vessels. All techniques currently deployed on IODP expeditions can be implemented onboard the vessel under polar weather and ice conditions, including the full range of re-entry, casing and cementing, and instrumentation options and the entire suite of downhole logging tools. Due to sufficient laboratory space, a full analytical workflow can be easily established comparable to existing permanent platforms, including clean rooms, diverse scanning and logging or incubation facilities. While the vessel is equipped with a dedicated deep-sea drilling rig, other coring and drilling techniques can be employed if needed (e.g. Rockdrill, MEBO, large diameter Kasten cores). AURORA BOREALIS is fitted to operate a CALYPSO Piston Coring System in polar waters. Future mud-return systems under consideration and testing for IODP to provide controlled borehole conditions in difficult facies are compatible with the layout of AURORA BOREALIS. The berthing capacity of 120 personnel total (scientists, technical support and crew) allows to accommodate a sufficient number of science party members offshore. The present scientific implementation documents plan for about one polar scientific drilling expedition per year in a to-be-determined configuration. As the vessel is a multi-dsiciplinary platform, operations for the entire year are not dependant on drilling operations alone. While principal access to the vessel will be based on a competitive proposal review and evaluation system, the allocation of timeslots specifically for drilling would preferably be given over to IODP handling and planning systems in a cooperative mode using the strengths and capacitites of the future program. Depending on interests and needs of the

  10. Historical Overview of ODP/IODP CORK Hydrological Observatories

    Science.gov (United States)

    Becker, K.; Davis, E. E.; Fisher, A. T.; Wheat, C. G.; Jannasch, H. W.; Pettigrew, T.

    2011-12-01

    Since 1991, the Ocean Drilling Program (ODP) and Integrated Ocean Drilling Program (IODP) have instrumented 24 holes drilled beneath the seafloor with long-term sealed-hole hydrological observatories called "CORKs." We present a historical summary of the designs of and experiences with the CORK observatories, starting from the 1989 concept sketch on a dinner napkin and continuing through three new installations planned in young Atlantic crust during IODP Expedition 336 during autumn of 2011. Understanding subseafloor hydrology in a variety of type environments has been a prime objective of scientific ocean drilling since the late 1970's. However, early experience indicated that holes that penetrated through marine sediments into underlying oceanic basement often allowed open exchange between formation fluids and ocean water, perturbing if not totally disturbing the in-situ hydrogeological state. This motivated the CORK approach to seal select holes with long-term sensor strings and data loggers, to record the recovery from drilling disturbances to the in-situ state and monitor natural hydrological signals. The original design included a single seal at the seafloor, and later designs have allowed for monitoring multiple zones in a single hole sealed by packers. The sensor strings have always included pressure and temperature monitoring, and many have included self-contained fluid samplers driven by osmotic pumps ("OsmoSamplers") that can be tuned for a variety of geochemical and microbiological sampling objectives. Typically, data and samplers have been recovered and/or exchanged at average intervals of ~1-3 years using manned or unmanned research submersibles. One CORK is now connected to the NEPTUNE Canada cable network; this allows 1 Hz sampling frequency and eliminates demand on battery power and the need for submersible visits to collect data. Cable connections to other holes are now planned in both the Juan de Fuca and Nankai regions. Nearly all installations

  11. Mid to late Holocene oceanographic changes offshore Adélie Land, Antarctica: Ultra-high resolution foraminiferal assemblage and isotopic records from IODP Expedition 318 Site U1357

    Science.gov (United States)

    Hendricks, E.; Salman, F. I.; Pekar, S. F.; Dunbar, R. B.; DeCesare, M.

    2014-12-01

    Foraminiferal biofacies as well as δ18O and δ13C records from IODP Site U1357 reveal significant changes in deep and surface water properties that include temperature, ventilation, and productivity during the mid to late Holocene. Site U1357 is located in the Adélie Trough, a glacially scoured valley on the continental shelf ~50km off the coast of East Antarctica. Sediment samples were taken at 10cm intervals resulting in an approximate time step for each sample of 7yr resolution based on extensive C14 dating and visible band counting exercises. As part of a collaborative effort between Queens College and Stanford University, samples from the upper part of the core were used in this study, which spanned from near Recent to 6kyr BP. Neogloboquadrina pachyderma make up nearly 50% of all foraminifers counted and was used to construct pelagic stable isotope records. From nearly 10,000 foraminifers counted, ~34 foraminiferal species were identified. The highest δ18O values occur from ~3.0 to ~6.1kyr and ~1kyr to Recent, with the lowest occurring from ~1.4 to ~3.8kyr. The highest δ13C values occur when δ18O are low. Total benthic foraminiferal abundances are highest during two intervals: Recent to ~1.4kyr and ~3.6 to ~6.1kyr. For ~2 to ~3.6kyr, the agglutinated species are the most dominant with calcareous benthic foraminifers being mainly absent. The higher δ18O values observed are consistent with lower surface water temperatures and decreased melt water from icebergs, with lower δ18O values ascribed to increased melt waters and possibly higher surface water temperatures. Previous studies indicate that cooler waters occurred when we observe lower foraminiferal δ18O values. This suggests that the N. pachyderma δ18O record was influenced primarily by the δ18O of seawater (e.g., iceberg melt waters), with temperature being a minor control. Higher δ13C values are associated with lower δ18O, which implies increased water column stratification coupled with high

  12. Exploring Links Between Global Climate and Explosive Arc Volcanism in Tephra-Rich Quaternary Sediments: A Pilot Study from IODP Expedition 350 Site 1437B, Izu Bonin Rear-Arc Region

    Science.gov (United States)

    Corry-Saavedra, K.; Straub, S. M.; Bolge, L.; Schindlbeck, J. C.; Kutterolf, S.; Woodhead, J. D.

    2015-12-01

    Fallout tephra in marine sediment provide an excellent archive of explosive arc volcanism that can be directly related to the other parameters of climate change, such as ice volume data, IRD (ice-rafted debris) input, etc. Current studies are based on 'discrete' tephra beds, which are produced by major eruptions and visible with the naked eye. Yet the more common, but less explosive arc eruptions that are more continuous through time produce 'disperse' tephra, which is concealed by the non-volcanic host sediment and invisible to the eye. The proportion of disperse tephra in marine sediments is known to be significant and may be critical in elucidating potential synchronicity between arc volcanism and glacial cycles. We conducted a pilot study in young sediments of IODP Hole 1437B drilled at 31°47.3911'N and 139°01.5788'E at the rear-arc of the Izu Bonin volcanic arc. By means of δ18O (Vautravers, in revision), eleven climatic cycles are recorded in uppermost 120 meter of carbonate mud that is interspersed by cm-thick tephra fallout layers. We selected six tephra layers, ranging from 0.2 to 1.16 million years in age, and sampled those vertically, starting from carbonate mud below the basal contact throughout the typical gradational top into the carbonate mud above. From each tephra bed, volcanic particles (>125 micrometer) were handpicked. All other samples were powdered and leached in buffered acetic acid and hydroxylamine hydrochloride to remove the carbonate and authigenous fraction, respectively. Major and trace element abundances (except for SiO2) from all samples were determined by ICP-MS and ICP-OES methods. Strong binary mixing trends are revealed between the pure tephra end member, and detrital sediment component. The tephra is derived from the Izu Bonin volcanic front and rear-arc, while the sediment component is presumably transported by ocean surface currents from the East China Sea. Our data show that mixing proportions change systematically with

  13. Expedited Programs for Serious Conditions: An Update on Breakthrough Therapy Designation.

    Science.gov (United States)

    Kwok, Martin; Foster, Theresa; Steinberg, Michael

    2015-09-01

    Our aim was to describe the regulatory pathways made available by the US Food and Drug Administration (FDA) to expedite the drug development and approval process, with a focus on the benefits and limitations of the Breakthrough Therapy Designation (BTD) pathway. Published materials consisting of journal articles, press releases, government documents, and news articles from pharmaceutical publishers were identified through online databases (ie, Medline and Scopus), the FDA website, and Internet search engines (eg, Google). To encourage pharmaceutical innovation and increase the number of products being approved each year, the FDA has introduced 4 expedited regulatory pathways to accelerate the drug development and approval process. The most recent program, enacted in July 2012, was BTD that is given to drugs that treat a serious or life-threatening disease or condition; and preliminary clinical evidence suggests the potential for these drugs to provide a substantial improvement over the current standard of care. The primary basis for the creation of BTD is to provide patients with serious conditions with earlier access to FDA-approved medications. In 2014, 22% of the new molecular entities approved within the Center for Drug Evaluation and Research had BTD status, as opposed to only 11% in 2013, which indicates both the popularity and success of this expedited pathway. Additionally, the creation of BTD has produced a more collaborative working relationship between the pharmaceutical industry and the FDA because both parties have a vested interest in the drug's success. Some of the more notable concerns surrounding these approved breakthrough therapies have been the abbreviated tolerability and efficacy evidence available from accelerated clinical development programs, ensuring the manufacturing aspects keep pace with these accelerated clinical programs, and finally, managing the strain on resources for both the pharmaceutical companies and the FDA. BTD has already

  14. Student Experiences: the 2013 Cascadia Initiative Expedition Team's Apply to Sail Program

    Science.gov (United States)

    Mejia, H.; Hooft, E. E.; Fattaruso, L.

    2013-12-01

    During the summer of 2013, the Cascadia Initiative Expedition Team led six oceanographic expeditions to recover and redeploy ocean bottom seismometers (OBSs) across the Cascadia subduction zone and Juan de Fuca plate. The Cascadia Initiative (CI) is an onshore/offshore seismic and geodetic experiment to study questions ranging from megathrust earthquakes to volcanic arc structure to the formation, deformation and hydration of the Juan de Fuca and Gorda plates with the overarching goal of understanding the entire subduction zone system. The Cascadia Initiative Expedition Team is a team of scientists charged with leading the oceanographic expeditions to deploy and recover CI OBSs and developing the associated Education and Outreach effort. Students and early career scientists were encouraged to apply to join the cruises via the Cascadia Initiative Expedition Team's Apply to Sail Program. The goal of this call for open participation was to help expand the user base of OBS data by providing opportunities for students and scientists to directly experience at-sea acquisition of OBS data. Participants were required to have a strong interest in learning field techniques, be willing to work long hours at sea assisting in OBS deployment, recovery and preliminary data processing and have an interest in working with the data collected. In total, there were 51 applicants to the Apply to Sail Program from the US and 4 other countries; 21 graduate students as well as a few undergraduate students, postdocs and young scientists from the US and Canada were chosen to join the crew. The cruises lasted from 6 to 14 days in length. OBS retrievals comprised the three first legs, of which the first two were aboard the Research Vessel Oceanus. During each of the retrievals, multiple acoustic signals were sent while the vessel completed a semi-circle around the OBS to accurately determine its position, a final signal was sent to drop the seismometer's anchor, and finally the ship and crew

  15. South African Climates: Highlights From International Ocean Discovery Program Expedition 361

    Science.gov (United States)

    Hemming, S. R.; Hall, I. R.; LeVay, L.

    2016-12-01

    International Ocean Discovery Program Expedition 361 drilled six sites on the southeast African margin and in the Indian-Atlantic ocean gateway, southwest Indian Ocean, from 30 January to 31 March 2016. In total, 5175 m of core was recovered, with an average recovery of 102%, during 29.7 days of on-site operations. The sites, situated in the Mozambique Channel, at locations directly influenced by discharge from the Zambezi and Limpopo River catchments, the Natal Valley, the Agulhas Plateau, and the Cape Basin were targeted to reconstruct the history of the Greater Agulhas Current System over the past 5 Ma. The Agulhas Current transports 70 Sv of warm and saline surface waters from the tropical Indian Ocean along the East African margin to the tip of Africa. Exchanges of heat and moisture with the atmosphere influence southern African rainfall patterns. Recent ocean model and paleoceanographic data further point at a potential role of the Agulhas Current in controlling the strength and mode of the Atlantic Meridional Overturning Circulation (AMOC) during the Late Pleistocene. The main objectives of the expedition were to document the oceanographic properties of the Agulhas Current through tectonic and climatic changes during the Plio-Pleistocene, to determine the dynamics of the Indian-Atlantic gateway circulation during this time, to examine the connection of the Agulhas leakage and AMOC, to address the influence of the Agulhas Current on African terrestrial climates and potential links to Human evolution. Additionally, the Expedition set out to fulfill the needs of the Ancillary Project Letter, consisting of high-resolution interstitial water samples that will, and to constrain the temperature and salinity profiles of the ocean during the Last Glacial Maximum. Here we highlight some of the expedition successes and show how it has made major strides toward fulfilling each of these objectives. The recovered sequences allowed complete spliced stratigraphic sections

  16. Active subsurface cellular function in the Baltic Sea Basin, IODP Exp 347

    Science.gov (United States)

    Reese, B. K.; Zinke, L. A.; Bird, J. T.; Lloyd, K. G.; Marshall, I.; Amend, J.; Jørgensen, B. B.

    2016-12-01

    The Baltic Sea Basin is a unique depositional setting that has experienced periods of glaciation and deglaciation as a result of global temperature fluctuations over the course of several hundred thousand years. This has resulted in laminated sediments formed during periods with strong permanent salinity stratification. The high sedimentation rates (100-500 cm/1000 y) make this an ideal setting to understand the microbial structure of a deep biosphere community in a high-organic matter environment. The responses of deep sediment microbial communities to variations in conditions during and after deposition are poorly understood. Samples were collected through scientific drilling during the International Ocean Discovery Program (IODP) Expedition 347 on board the Greatship Manisha, September-November 2013. We examined the active microbial community structure using the 16S rRNA gene transcript and active functional genes through metatranscriptome sequencing. Major biogeochemical shifts have been observed in response to the depositional history between the limnic, brackish, and marine phases. The microbial community structure in the BSB is diverse and reflective of the unique changes in the geochemical profile. These data further define the existence life in the deep subsurface and the survival mechanisms required for this extreme environment.

  17. High-Resolution Magnetic Properties and Cyclicity of Contourites from IODP Site U1389 (West Iberian Margin)

    Science.gov (United States)

    Richter, C.; Adesiyun, O.; Acton, G.; Sidorovskaia, N.; Sierro, F. J.; Xuan, C.; Verosub, K. L.

    2015-12-01

    We present high-resolution paleomagnetic and rock magnetic results from the lower part of the APC-cored section (36 - 107 meters composite depth) of Integrated Ocean Drilling Program (IODP) Site U1389 (36º 25.515'N; 7º 16.683'W, 644 m water depth). This site was cored as part of the IODP Mediterranean Outflow Expedition to address paleoceanographic questions about the evolution of the North Atlantic Mediterranean and climate system over the past 6 million years. The recovered section at Site U1389 consists of a thick, rapidly accumulated (~40 cm/kyr), and very uniform series of contouritic sediment. Ages were obtained by tuning the planktonic foraminifer oxygen isotope data to the NGRIP ice core record. We collected rock magnetic and paleomagnetic measurements at 1-cm resolution on 71-m of U-channel samples (representing ~145 k.yr.), with the goal of extracting a high-resolution record of paleoenvironmental variability, relative geomagnetic paleointensity, and paleosecular variation. Stepwise demagnetization of the natural remanence (NRM) demonstrates the successful removal of a secondary, predominantly drill-string induced, magnetization and identification of a stable and strong primary magnetization carried by the sediment samples (average MAD calculated by principal component analysis: ~1º). Excellent behavior of the samples during alternating field demagnetization and isothermal remanent magnetization (IRM) acquisition suggest magnetite as the main carrier of magnetic remanence. Relative paleointensity estimates were determined by normalizing the NRM by the ARM, IRM, and magnetic susceptibility. Time-frequency analyses of high-resolution concentration and grain-size dependent paleomagnetic proxy data for the entire 107-m (200 k.yr.) long APC section of Site U1389 will be presented with the goal of identifying the driver of cyclic changes in the sedimentary section.

  18. Geologic implications of gas hydrates in the offshore of India: results of the National Gas Hydrate Program Expedition 01

    Science.gov (United States)

    Collett, Timothy S.; Boswell, Ray; Cochran, J.R.; Kumar, Pushpendra; Lall, Malcolm; Mazumdar, Aninda; Ramana, Mangipudi Venkata; Ramprasad, Tammisetti; Riedel, Michael; Sain, Kalachand; Sathe, Arun Vasant; Vishwanath, Krishna

    2014-01-01

    The Indian National Gas Hydrate Program Expedition 01 (NGHP-01) is designed to study the occurrence of gas hydrate along the passive continental margin of the Indian Peninsula and in the Andaman convergent margin, with special emphasis on understanding the geologic and geochemical controls on the occurrence of gas hydrate in these two diverse settings. The NGHP-01 expedition established the presence of gas hydrates in the Krishna-Godavari and Mahanadi Basins, and the Andaman Sea. The expedition discovered in the Krishna-Godavari Basin one of the thickest gas hydrate accumulations ever documented, in the Andaman Sea one of the thickest and deepest gas hydrate stability zones in the world, and established the existence of a fully developed gas hydrate petroleum system in all three basins.

  19. Bridging the Gap Between Scientists and Classrooms: Scientist Engagement in the Expedition Earth and Beyond Program

    Science.gov (United States)

    Graff, P. V.; Stefanov, W. L.; Willis, K. J.; Runco, S.

    2012-01-01

    Teachers in today s classrooms need to find creative ways to connect students with science, technology, engineering, mathematics (STEM) experts. These STEM experts can serve as role models and help students think about potential future STEM careers. They can also help reinforce academic knowledge and skills. The cost of transportation restricts teachers ability to take students on field trips exposing them to outside experts and unique learning environments. Additionally, arranging to bring in guest speakers to the classroom seems to happen infrequently, especially in schools in rural areas. The Expedition Earth and Beyond (EEAB) Program [1], facilitated by the Astromaterials Research and Exploration Science (ARES) Directorate Education Program at the NASA Johnson Space Center has created a way to enable teachers to connect their students with STEM experts virtually. These virtual connections not only help engage students with role models, but are also designed to help teachers address concepts and content standards they are required to teach. Through EEAB, scientists are able to actively engage with students across the nation in multiple ways. They can work with student teams as mentors, participate in virtual student team science presentations, or connect with students through Classroom Connection Distance Learning (DL) Events.

  20. 45 CFR 303.101 - Expedited processes.

    Science.gov (United States)

    2010-10-01

    ... 45 Public Welfare 2 2010-10-01 2010-10-01 false Expedited processes. 303.101 Section 303.101... STANDARDS FOR PROGRAM OPERATIONS § 303.101 Expedited processes. (a) Definition. Expedited processes means... intrastate cases, expedited processes as specified under this section to establish paternity and to establish...

  1. Inspiring the Next Generation of Explorers: Scientist Involvement in the Expedition Earth and Beyond Program

    Science.gov (United States)

    Graff, P. V.; Stefanov, W. L.; Willis, K.; Runco, S.

    2012-12-01

    Scientists, science experts, graduate and even undergraduate student researchers have a unique ability to inspire the next generation of explorers. These science, technology, engineering, and mathematics (STEM) experts can serve as role models for students and can help inspire them to consider future STEM-related careers. They have an exceptional ability to instill a sense of curiosity and fascination in the minds of students as they bring science to life in the classroom. Students and teachers are hungry for opportunities to interact with scientists. They feel honored when these experts take time out of their busy day to share their science, their expertise, and their stories. The key for teachers is to be cognizant of opportunities to connect their students with scientists. For scientists, the key is to know how to get involved, to have options for participation that involve different levels of commitment, and to work with educational specialists who can help facilitate their involvement. The Expedition Earth and Beyond (EEAB) Program, facilitated by the Astromaterials Research and Exploration Science (ARES) Directorate at the NASA Johnson Space Center, is an Earth and planetary science education program designed to inspire, engage, and educate teachers and students by getting them actively involved with NASA exploration, discovery, and the process of science. One of the main goals of the program is to facilitate student research in the classroom. The program uses astronaut photographs, provided through the ARES Crew Earth Observations (CEO) payload on the International Space Station (ISS) as the hook to help students gain an interest in a research topic. Student investigations can focus on Earth or involve comparative planetology. Student teams are encouraged to use additional imagery and data from Earth or planetary orbital spacecraft, or ground-based data collection tools, to augment the astronaut photography dataset. A second goal of the program is to provide

  2. Inspiring the Next Generation of Explorers: Scientist Involvement in the Expedition Earth and Beyond Program

    Science.gov (United States)

    Graff, Paige; Stefanov, William; Willis, Kim; Runco, Susan

    2012-01-01

    Scientists, science experts, graduate and even undergraduate student researchers have a unique ability to inspire the next generation of explorers. These science, technology, engineering, and mathematics (STEM) experts can serve as role models for students and can help inspire them to consider future STEM-related careers. They have an exceptional ability to instill a sense of curiosity and fascination in the minds of students as they bring science to life in the classroom. Students and teachers are hungry for opportunities to interact with scientists. They feel honored when these experts take time out of their busy day to share their science, their expertise, and their stories. The key for teachers is to be cognizant of opportunities to connect their students with scientists. For scientists, the key is to know how to get involved, to have options for participation that involve different levels of commitment, and to work with educational specialists who can help facilitate their involvement. The Expedition Earth and Beyond (EEAB) Program, facilitated by the Astromaterials Research and Exploration Science (ARES) Directorate at the NASA Johnson Space Center, is an Earth and planetary science education program designed to inspire, engage, and educate teachers and students by getting them actively involved with NASA exploration, discovery, and the process of science. One of the main goals of the program is to facilitate student research in the classroom. The program uses astronaut photographs, provided through the ARES Crew Earth Observations (CEO) payload on the International Space Station (ISS) as the hook to help students gain an interest in a research topic. Student investigations can focus on Earth or involve comparative planetology. Student teams are encouraged to use additional imagery and data from Earth or planetary orbital spacecraft, or ground-based data collection tools, to augment the astronaut photography dataset. A second goal of the program is to provide

  3. Linking downhole logging data with geology and drilling /coring operations - Example from Chicxulub Expedition 364.

    Science.gov (United States)

    Lofi, Johanna; Smith, Dave; Delahunty, Chris; Le Ber, Erwan; Mellet, Claire; Brun, Laurent; Henry, Gilles; Paris, Jehanne

    2017-04-01

    faults, as evidenced from borehole wall images. Both form conduits probably open at a large scale as suggested by associated anomalies in the borehole fluid temperature profiles. When coring the basement, pieces of metal trapped outside the drill bit apparently led to an increase of the borehole tilt as well as to an enlargement of the hole, although this later remained sub-circular. In the post impact carbonates, 6-7 m long apparent cyclic oscillations in the magnetic field coupled to a spiral shape trajectory of the same wavelength suggest drilling induced artifacts and formation re-magnetization. Acknowledgements: Expedition 364 was funded by IODP with co-funding from ICDP and implemented by ECORD, with contributions and logistical support from the Yucatán state government and Universidad Nacional Autónoma de México. Drilling Services were provided by DOSECC Exploration Services. The downhole logging program was coordinated by EPC, as part of ESO. Expedition 364 Scientists: S. Gulick, J.V. Morgan, E. Chenot, G. Christeson, P. Claeys, C. Cockell, M.J. L. Coolen, L. Ferrière, C. Gebhardt, K. Goto, H. Jones, D.A. Kring, J. Lofi, X. Long, C. Lowery, C. Mellett, R. Ocampo-Torres, L. Perez-Cruz, A. Pickersgill, M. Poelchau, A. Rae, C. Rasmussen, M. Rebolledo-Vieyra, U. Riller, H. Sato, J. Smit, S. Tikoo, N. Tomioka, M. Whalen, A. Wittmann, J. Urrutia-Fucugauchi, K.E. Yamaguchi, W. Zylberman.

  4. Quiet eye training expedites motor learning and aids performance under heightened anxiety: the roles of response programming and external attention.

    Science.gov (United States)

    Moore, Lee J; Vine, Samuel J; Cooke, Andrew; Ring, Christopher; Wilson, Mark R

    2012-07-01

    Quiet eye training expedites skill learning and facilitates anxiety-resistant performance. Changes in response programming and external focus of attention may explain such benefits. We examined the effects of quiet eye training on golf-putting performance, quiet eye duration, kinematics (clubhead acceleration), and physiological (heart rate, muscle activity) responses. Forty participants were assigned to a quiet eye or technical trained group and completed 420 baseline, training, retention, and pressure putts. The quiet eye group performed more accurately and displayed more effective gaze control, lower clubhead acceleration, greater heart rate deceleration, and reduced muscle activity than the technical trained group during retention and pressure tests. Thus, quiet eye training was linked to indirect measures of improved response programming and an external focus. Mediation analyses partially endorsed a response programming explanation. Copyright © 2012 Society for Psychophysiological Research.

  5. “Core on deck!” The End of SODV and the Return of the JOIDES Resolution as the IODP Riserless Vessel

    Directory of Open Access Journals (Sweden)

    Sean Higgins

    2009-09-01

    Full Text Available In February 2009, after a 3-year operational hiatus in order to undergo a major retrofit, the JOIDES Resolution (or simply the JR, as it has been called since 1985 reverberated with the trademark phrase, “Core on deck!”. For the crew and technical staff aboard during the JR’s sea trials cruise in January–February 2009, it brought shouts of joy and tears of relief from years of rebuilding the JR in a Singapore shipyard, and a realization that we were “really” going back to carrying out international expeditions. But what does the phrase mean to marine geoscientists around the world?For most scientists, it means that one of the only tools to explore sediments and rocks in the deep sub-seafloor throughout the world’s oceans is finally available again. This unique research facility is our community’s equivalent to the Hubble telescope and provides the access we need to the deep ocean. Accumulating an impressive array of accomplishments, the JR (Fig. 1 has served as the sole scientificdrilling vessel for the Ocean Drilling Program (ODP, 1985–2003 and for the initial phase of riserless drilling for the Integrated Ocean Drilling Program (IODP, 2003–2006. Over 120 expeditions since 1985 have retrieved samples encompassing a latitudinal range from 80.5°N to 70.8°S, a water depth range from 85 m to nearly 6000 m, sub-bottomdepths as deep as 2.1 km, and a total depth range (water depth plus penetration over 6.9 km.

  6. [Expedition medicine].

    Science.gov (United States)

    Donlagić, Lana

    2009-01-01

    Expedition and wildeness medicine is a term that combines rescue medicine, sport medicine as well as more specific branches as polar or high altitude medicine. It is being intensively studied both at the reaserch institutes and on expeditions. Ophtalmologists are concentrated on the reaserch of HARH (High Altitude Retinal Hemorrhage), neurologists on HACE reaserch (High Altitude Cerebral Edema), psychologists are developing tests to decsribe cognitive functions and many physicians are being trained to work in extreme enviroment. The result of all this effort are numerous new findings in pathophysiology and therapy of altitude illness, increased security on expedition and further development of expeditionism.

  7. Expedition sol

    DEFF Research Database (Denmark)

    Jacobsen, Aase Roland

    2006-01-01

    Tag på expedition sol rundt i museet. Er der nogen, der har taget en bid af solen? Hvorfor bliver der solformørkelse? Kan vi undvære Solen?......Tag på expedition sol rundt i museet. Er der nogen, der har taget en bid af solen? Hvorfor bliver der solformørkelse? Kan vi undvære Solen?...

  8. Neogene paleoceanography of the eastern equatorial Pacific based on the radiolarian record of IODP drill sites off Costa Rica

    Science.gov (United States)

    Sandoval, María. I.; Boltovskoy, Demetrio; Baxter, Alan T.; Baumgartner, Peter O.

    2017-03-01

    The Integrated Ocean Drilling Program (IODP) Expedition 344 drilled cores following a transect across the convergent margin off Costa Rica. Two of the five sites (U1381 and U1414) are the subject of the present study. Major radiolarian faunal breaks and characteristic species groups were defined with the aid of cluster analysis, nodal analysis, and discriminant analysis of principal components. A middle-late Miocene to Pleistocene age (radiolarian zones RN5 to RN16) was determined for the sites, which agrees with the nannofossil zonations and 40Ar/39Ar and tephra layers. Considering the northward movement of the Cocos plate (˜7.3 cm/yr), and a paleolatitude calculator, it is assumed that during the Miocene the two sites were located ˜1000 km to the southwest of their current position, slightly south of the equator. The radiolarian faunas retrieved were thus seemingly formed under the influence of different oceanic currents and sources of nutrients. Changes in the radiolarian assemblages at Site U1414 point at dissimilar environmental settings associated with the colder South Equatorial Current and the warmer Equatorial Countercurrent, as well as to coastal upwelling. These differences are best reflected by changes in the abundance of the morphotype Spongurus spp., with noticeably higher values during the Miocene, than in the Pliocene and the Pleistocene. Because Spongurus spp. is generally associated with cooler waters, these abundance variations (as well as those of several other species) suggest that during the Miocene the area had a stronger influence of colder waters than during younger periods. During the Pliocene and the lowermost Pleistocene, biogenic remains are scarce, presumably due to the terrigenous input, which could have diluted and affected the preservation of pelagic fossils, as well as to the displacement of the site to warmer waters. A typically tropical fauna characterized the Pleistocene, yet with widespread presence of colder water species

  9. Relative Geomagnetic Paleointensity, Environmental Magnetism, and Cyclicity of Contourites from the West Iberian Margin (IODP Site U1389)

    Science.gov (United States)

    Richter, C.; Horton, L. B.; Acton, G.; Sidorovskaia, N.; Sierro, F. J.; Xuan, C.; Verosub, K. L.

    2014-12-01

    The Mediterranean Outflow Expedition provides an outstanding opportunity to address paleoceanographic questions about the evolution of the Mediterranean and North Atlantic climate system over the past 6 million years. As part of the overall project, we present high-resolution paleomagnetic and rock magnetic results from the top ~36 meters composite depth (mcd) of Integrated Ocean Drilling Program (IODP) Site U1389 (36º 25.515'N; 7º 16.683'W, 644 m water depth) located approximately 90 km west of Cádiz. The sedimentary section is represented by a thick, rapidly accumulated (mean sediment accumulation rate of ~40 cm/kyr), and very uniform series of contouritic sediment. The age model was obtained by tuning the planktonic foraminifer oxygen isotope data to the NGRIP ice core record. Paleomagnetic and rock magnetic measurements were collected at 1-cm interval resolution on U-channel samples covering the top ~36 mcd, with the goal of extracting a high-resolution record of paleosecular variation, relative geomagnetic paleointensity change, and the variability of the paleoenvironmental conditions. Detailed demagnetization of the natural remanence (NRM) reveals the successful removal of a secondary magnetization and identification of a stable and strong primary magnetization carried by the sediment samples (average MAD associated with principal component analysis: 0.97º). Isothermal remanent magnetization (IRM) acquisition curves and excellent behavior of the samples during alternating field demagnetization suggest magnetite as the main magnetic remanence carrier. Relative paleointensity estimates were calculated by normalizing NRM with ARM, IRM, as well as magnetic susceptibility. Time-frequency analyses of high-resolution concentration and grain-size dependent paleomagnetic proxy data and other physical properties are in progress and will be presented with the goal of identifying the driver of cyclic changes in the sedimentary section.

  10. Trials at Sea: Successful Implementation of a Unique Two-Month Professional Development Program

    Science.gov (United States)

    Peart, L. W.; Orcutt, B. N.; Fisher, A. T.; Tsuji, T.; Petronotis, K. E.; Iodp Expedition 327 Participants

    2010-12-01

    During the summer of 2010, Integrated Ocean Drilling Program (IODP) Expedition 327 conducted coring and observatory installations on the Juan de Fuca Plate to characterize the hydrogeology of ridge-flank ocean crust. Due to the nature of the expedition, a smaller science party than usual was needed. IODP took this opportunity to expand education, outreach, and communication (EOC) activities with a previously untested model. Up to now, the IODP U.S. Implementing Organization had sailed either individual teachers on regular (2-month long) expeditions or groups of teachers and informal educators during short (2-week long) transits (School of Rock workshops). After two shipboard (Expeditions 312 and 321T) and two shore-based (Gulf Coast Repository) programs, we have recognized that sailing a group of educators is a beneficial model for IODP and the participants. What has been unavoidable is that these workshops took place outside typical expedition activities. Expedition 327 provided a unique opportunity to sail a diverse group of outreach officers on a regular expedition with a full range of scientific activities. The group included individuals with a wide variety of skills and backgrounds. US participants included a late-career high school physics teacher, a visualization graduate student, an undergraduate engineering student from an historically black university, and an artist. French participants included two middle and high school earth and life science teachers. This diversity made the group more dynamic but it also posed a challenge. Numerous scientific and technical staff also participated in EOC activity design and leadership, including development of dedicated web sites and blogs. After a seminar on constructivist and inquiry-based methods, we spent the first few weeks investigating earth science concepts so EOC participants could gain a basic understanding of the regional geology and the scientific objectives of the expedition. Close to the beginning of the

  11. The Natural Classroom: A Directory of Field Courses, Programs, and Expeditions in the Natural Sciences.

    Science.gov (United States)

    Edelman, Jack R.

    The purpose of this book is to increase awareness of the numerous seminars, short courses, field courses, workshops, and programs for teachers, students, naturalists, and independent scholars. These programs emphasize the natural sciences including general biology, botany, zoology, ecology, marine biology, ichthyology, microbiology, natural…

  12. Deformation microstructures and timing of a large submarine landslide drilled offshore Martinique (IODP Exp. 340)

    Science.gov (United States)

    Guyard, H.; Le Friant, A.; Brunet, M.; Boudon, G.; Emmanuel, L.; Caron, B.; Villemant, B.; Feuillet, N.

    2015-12-01

    Flank-instabilities constitute a recurrent process in the long-term evolution of many volcanoes. A very large submarine landslide deposit (~2100 km2, ~300 km3) drilled southwest Martinique island during the IODP Exp. 340 in 2012 is likely associated with one (or more) major volcanic flank collapse of Mount Pelée during the Late Pleistocene. A recent study revealed that this D1/D2 deposit is emergent in its central part, frontally confined, and mainly comprises remobilized seafloor sediments rather than debris avalanche material from the volcanic edifice (Brunet et al., subm). Here, we investigate the sedimentary microstructures and timing of deformation from the central (Hole 1400B, ~37 km from the coastline) and distal (Hole 1399A, ~70 km from the coastline) units of the D1/D2 deposit, in order to better understand the emplacement dynamics of such potentially tsunamigenic submarine landslides. High resolution CT-Scan analyses were continuously performed on more than 300 m of sediment cores, in order to characterize and distinguish the internal architecture and the complex deformation features of the sediments at each drilling site. The establishment of the stratigraphy, based on δ18O measurements and AMS 14C dating, is still in progress and may confirm the possible link between the submarine landslide deposits and the flank collapse scars observed on the subaerial part of Martinique. These new insights into the timing and emplacement processes of this large submarine landslide will have important implications for tsunami hazards. ReferenceBrunet, M., Le Friant, A., Boudon, G., Lafuerza, S., Talling, P., Hornbach, M., Lebas, E., Guyard, H., and IODP Expedition 340 science party, submitted. Composition, geometry and emplacement dynamics of a large volcanic island landslide offshore Martinique: from volcano flank-collapse to seafloor sediment failure? Geochemistry, Geophysics, Geosystems.

  13. Insights into magmatic processes and hydrothermal alteration of in situ superfast spreading ocean crust at ODP/IODP site 1256 from a cluster analysis of rock magnetic properties

    NARCIS (Netherlands)

    Dekkers, Mark J.; Heslop, David; Herrero-Bervera, Emilio; Acton, Gary; Krasa, David

    We analyze magnetic properties from Ocean Drilling Program (ODP)/Integrated ODP (IODP) Hole 1256D (6°44.1' N, 91°56.1' W) on the Cocos Plate in ∼15.2 Ma oceanic crust generated by superfast seafloor spreading, the only drill hole that has sampled all three oceanic crust layers in a tectonically

  14. Early-middle Eocene transition in calcareous nannofossil assemblages at IODP Site U1410 (Southeast Newfoundland Ridge, NW Atlantic)

    Science.gov (United States)

    Cappelli, Carlotta; Agnini, Claudia; Yamamoto, Yuhji

    2017-04-01

    nannofossils, making this Site suitable for a comprehensive taxonomic revision of Nannotetrina and Chiasmolithus. Biohorizons related to species belonging to these two genera are used to mark middle Eocene biozone boundary, a better characterization of their taxonomy would thus improve their reliability as biostratigraphic tools. Furthermore, during the early middle Eocene a new evolutionary lineage, which includes S. kempii - S. perpendicularis- S. furcatholitoides morph. A - S. cuniculus - S. furcatholitoides morph. B occurred among sphenoliths. This plexus is characterized by progressive morphological changes which, if correctly identify, will allow for a very detailed subdivision of this interval. Even more interestingly, we would assess if there is any relationship between this evolutionary trend and the surrounding abiotic conditions. Agnini, C., Fornaciari, E., Raffi, I., Catanzariti, R., Pälike, H., Backman, J., and Rio, D., Newslett. Stratigr., 47, 131-181 (2014). Martini E., in: Farinacci, A. (Ed.), Proceedings 2nd International Conference Planktonic Microfossils Roma: Rome (Ed. Tecnosci.) 2, 739-785 (1971). Norris R.D., Wilson P.A., Blum P. and the IODP Expedition 342 Scientists, Proceedings of the Integrated Ocean Drilling Program, 342, 1-148 (2012). Zachos J., Pagani M., Sloan L., Thomas E., Billups K., Science, 292, 686-693 (2001).

  15. Hundreds of Cruises, Thousands of People, Endless Discoveries - Education and Outreach in the Integrated Ocean Drilling Program

    Science.gov (United States)

    Peart, L.; Niemitz, M.; Boa, S.; Corsiglia, J.; Klaus, A.; Petronotis, K.; Iturrino, G.

    2005-12-01

    For 37 years, scientific ocean drilling programs have sponsored hundreds of expeditions, drilled at over 1,800 sites and recovered over 200 miles of core. The discoveries of these programs have led to important realizations of how our earth works. Past expeditions have validated the theory of plate tectonics, provided unparalleled ancient climate records and recovered evidence of the asteroid impact that wiped out the dinosaurs 65 million years ago - and new discoveries occur with every expedition. By producing education materials and programs and encouraging mass media journalists' interest in our news, we strive to fulfill our commitment to communicate our programs' scientific discoveries to the public, in a way that people - not just other scientists - understand. With the advent of the Integrated Ocean Drilling Program (IODP), education and outreach efforts have expanded to pursue new opportunities and engage wider audiences. Through our strategy of Teaching for Science, Learning for LifeTM, our education efforts seek to utilize the interdisciplinary nature of scientific ocean drilling to teach career awareness, scientific methods, teamwork, and problem solving techniques for a lifetime of learning, decision making and good citizenship. In pursuit of this goal, we have implemented professional and resource development programs and expanded our outreach at education-focused conferences to help teachers use IODP science to satiate the student's need to learn the methods of science that apply to everyday life. We believe that this message also applies to life-long learners and thus we have focused our efforts on news media outreach and education opportunities surrounding ports of call of the JOIDES Resolution, permanent and traveling museum exhibits. In addition, our outreach to undergraduate and graduate audiences, through a lecture series, research fellowships and internships, helps to create future generations of science leaders.

  16. Last deglacial paleoceanography in equatorial Pacific reconstructed from boron isotopes on Tahitian fossil corals obtained from IODP Exp 310

    Science.gov (United States)

    Kubota, K.; Yokoyama, Y.; Ishikawa, T.; Inoue, M.; Suzuki, A.

    2012-12-01

    Antarctic ice cores have revealed close relations between surface temperature and atmospheric pCO2 in the past in accord with glacial and interglacial cycles for the last 800 kyrs. The deep ocean is thought as responsible for approximately 80-100 ppm changes in its magnitude since it is the largest carbon reservoir on surface of the Earth. Several attempts have been made to identify exact locations of those carbon pools and routes during the climate change in the ocean though the outcomes are still inconclusive. Pacific ocean is the one of the main candidates for this path of CO2 purge during the deglaciation because there is the largest CO2 source in the world ocean at present in the equatorial Pacific, and Tahiti locates in the margin of the equatorial upwelling (cold tongue) region as is sensitive to its past changes. In this study, we measured Boron isotopes (δ11B) to reconstruct paleo pH on Tahitian fossil corals (Porites spp.) recovered during the Integrated Ocean Drilling Program (IODP) expedition 310 'Tahiti Sea level'. U-series dated corals precisely can provide the timing of changes as is able to compare the record directly with ice core pCO2. Local marine radiocarbon reservoir ages are also calculated using previously published datasets in the region. The result shows large pH depletions in surface of equatorial Pacific associated with much older water intrusions during the last deglatiation, in particular during H1 and YD. This is consistent with previous pH reconstructions using δ11B of marine carbonates in Marquesas Island (coral) and off Papua New Guinea (planktonic foraminifera). Thus low pH and radiocarbon depleted surface water distribution during the millennial scale climate event was persisted not only in Tahiti but other surface equatorial Pacific. This suggests close relations Pacific oceanography with global climate via ocean circulation as is recorded as either stronger upwelling or subsurface water chemical characteristic changes in wider

  17. Embark students on geosciences expeditions, across the oceans …

    Science.gov (United States)

    Burgio, Marion; Darrieu, Michele; Pointu, Agnes; Maruejol, Patricia; Cooper, Sharon

    2017-04-01

    As teachers we can live and share a fabulous experience of science and research on the scientific drilling vessels and platforms of IODP-ECORD and JAMSTEC consortiums. ECORD offered us the opportunity to embark on the IODP 359, 360 and 362 expeditions as Education Officers. Our task was to communicate about science with the general public and students from 7 to 25 years-old. In this presentation, we will focus on the 360 expedition, South West Indian Ridge-lower crust and Moho. We explain the three steps of the "teacher at sea" experience from the very first idea to the real pedagogical work during and after the expedition. -Apply, get ready and leave… for two months: From the difficulties you may encounter to the most efficient ways to prepare the pedagogical tasks. -Work, live onboard and get back: We will describe the main activities of the Education officers among the Science party and the way all this can become a highly changing-life experience. -Use data, share and inspire: We will detail some strategies we used to catch the attention of the students. They could participate to "live" science and have a better idea of the job of researcher. Now, we have to inspire others teachers to use our data and pedagogical documents, or to get the opportunity to embark ! What gets out of these crossed experiences is that the quality of the human relationships, and the way the students can get closer to the scientists during the interactions, are the keys to motivate students and give them a new vision of the scientific research.

  18. Using giant piston coring within IODP to track past earthquakes in the sedimentary record along the Japan Trench

    Science.gov (United States)

    Strasser, Michael

    2017-04-01

    "Submarine paleoseismology" is a promising approach to investigate deposits from the deep sea, where earthquakes leave traces preserved in stratigraphic succession. The concept of studying sedimentary event deposits for reconstructing past earthquake history and related impacts to the marine environment is increasingly being applied in various settings. However, at present we lack comprehensive data sets that allow conclusive distinctions between quality and completeness of the paleoseismic archives, as they may relate to different sediment transport, erosion and deposition processes vs. variability of intrinsic seismogenic behavior across different segments. Nevertheless, many recent studies, which are mostly based on conventional 10-m-long cores, demonstrate the potential of the research concept. With ECORD opening their mission specific platform approach to include giant piston coring within IODP, a new horizon has opened up for multi-coring expeditions fully dedicated to the rapidly growing field of submarine paleoseismology. IODP is uniquely positioned to address the complex feedback mechanisms between earthquake shaking and its manifestation in the marine archive, decipher related mass fluxes from the shallow to the deep see and to eventually provide longer records to constrain earthquake recurrence far beyond historical catalogues. Initially building on what sedimentary deposits were generated from the 2011 M9 Tohoku-oki earthquake, the Japan Trench is a promising study area to investigate earthquake-triggered sediment remobilization processes and how they become embedded in the stratigraphic record, and has thus been identified as a primary target for proposing giant piston coring within IODP. In this presentation we summarize recent results and available site survey data collected since the 2011 earthquake, comprising >50, 5-10m long piston and gravity cores from (i) trench-fill and graben-fill basin across the entire trench axis from 36° to 40.3° N (ii

  19. CaCO3 dissolution in the Eastern Equatorial Pacific during the Mid-Miocene: A study using IODP PEAT cores

    Science.gov (United States)

    Shackford, J. K.; Lyle, M. W.

    2013-12-01

    X-ray Fluorescence (XRF) scan data from Integrated Ocean Drilling Program (IODP) Expedition 320/321 in the Eastern Equatorial Pacific show evidence of carbonate dissolution occurring at multiple times during the Cenozoic. Specifically, at sites U1335, U1336, and U1337, the characteristic variations in sedimentary calcium carbonate content that results in the common seismic stratigraphy found throughout the equatorial Pacific east of Hawaii. Large-scale changes in the carbon cycle are reflected in changes of the carbonate compensation depth, those changes subsequently being recorded in deep sea sediments. We have identified a number of carbonate dissolution events throughout the Cenozoic, primarily focusing on a major carbonate dissolution cycle during the early to mid-Miocene (~18-16 Ma). Previously, inadequate core recovery within this time interval has hindered study of this event, however we have completed analysis of three nearly continuous sediment records of the early Miocene allowing much more detailed study. These three IODP Leg 320/321 sites in the study provide a matrix of sedimentation rates and latitude for the early Miocene since they were all at roughly the same depth (~4 km) at 17 Ma, and formed a transect of paleolatitude from the equator, through 1°N to 3.5°N. Since the magnitude of productivity depends heavily on latitude in the equatorial Pacific, these three sites can be used to distinguish between dissolution events and productivity transients. XRF scan data from Sites U1335, U1336, and U1337 over the 18-16 Ma interval are used to better constrain the timing and structure of the event, as well as provide understanding of how productivity and changes in ocean carbon cycling affect carbonate preservation in sediments. The major dissolution event at 17 Ma lasted ~1 million years and CaCO 3 analyses indicate cyclicity on an approximately 100,000 year time scale. The cycling is strongly influenced by orbital insolation changes. Core sections from

  20. Oxygen minimum zone dynamics and anammox in the Gulf of Alaska (IODP Site U1419)

    Science.gov (United States)

    Zindorf, Mark; März, Christian; Rush, Darci; Talbot, Helen; Crawford, Alexandra; Wagner, Thomas; van der Land, Cees; Sidgwick, Frances

    2017-04-01

    In the modern northeast Pacific Ocean, an oxygen minimum zone (OMZ) occurs in depths of 700 to 1300 metres. Under current climatic conditions, this OMZ extends northwards into the Gulf of Alaska and is most pronounced during spring and autumn and disappears during winter. While its modern behaviour is well constrained, the extent of this OMZ in the past, especially in the Gulf of Alaska, is not well understood. Anaerobic ammonium oxidation (anammox) only takes place under suboxic to anoxic conditions. With the BHT-isomer (bacteriohopanetetrol-stereoisomer) the involved microorganisms leave a distinct biomarker trace in sedimentary organic matter. This biomarker is well preserved compared to other anammox biomarkers (e.g., ladderanes) and while BHT is produced by a broad range of microbes, the BHT-isomer is only produced by anammox bacteria. The ratio between BHT and BHT-isomer can, therefore, be used as a reliable proxy for suboxic-anoxic conditions in the overlying water column at the time of deposition. We present the application of this BHT-isomer at a new high-resolution record at the continental shelf off Alaska (IODP Expedition 341 Site U1419) that provides a 60 ka record of paleo-environmental conditions. The BHT-isomer displays significant variability and partly very high concentrations, indicating periods of sub- or anoxic conditions in the overlying water column. Elemental ratios such as Cu/Al, Mo/Al, S/Al and U/Al, which are commonly used as inorganic proxies for water column oxygenation do not show the same pattern in the respective intervals. However, these proxies can be affected by authigenic mineral formation in the course of early diagenesis, redistributing elements in the sediment column which impact their usefulness as paleo-redox-proxies. In contrast, the BHT-isomer ratio appears to be a robust proxy for water column oxygenation and not sensitive to early diagenesis.

  1. Teaching Marine Geoscience at Sea: Integrated Ocean Drilling Program's School of Rock Explores Cascadia Subduction Zone - Cores, Logs, and ACORKs

    Science.gov (United States)

    Reagan, M.; Collins, J.; Ludwig, K. A.; Slough, S.; Delaney, M. L.; Hovan, S. A.; Expedition 328 Scientists

    2010-12-01

    For twelve days this past September, seventeen formal and informal educators from the US, UK, and France joined six instructors and a small science party on the scientific drillship JOIDES Resolution for the Integrated Ocean Drilling Program (IODP)’s Cascadia ACORK Expedition. The educators were part of the annual “School of Rock (SOR)” education program. SOR is coordinated by the U.S. Implementing Organization (USIO) of IODP and is designed to engage participants in seagoing Earth systems research and education workshops onboard the JOIDES Resolution and on shore at the Gulf Coast Core Repository in Texas. The scientific objective of the Cascadia ACORK expedition was to install a new permanent hydrologic observatory at ODP Site 889 to provide long-term monitoring of the pressure at the frontal part of the Cascadia accretionary prism. This year’s SOR workshop focused on how cores, logs, and ACORKs shed light on the hydrology and geology of the Cascadia subduction zone in the Northeast Pacific. In addition to observing the deployment of the ACORK, the SOR participants conducted daily hands-on analyses of archived sediment and hard-rock cores with scientists and technicians who specialize in IODP research using the lab facilities on the ship. Throughout the expedition, participants engaged in different activities and lessons designed to explore the deep biosphere, methane hydrates, paleoceanography, sedimentology, biostratigraphy, seafloor spreading, and drilling technology. The workshop also provided participants with “C3” time; time to communicate their experience using the successful joidesresolution.org website and other tools, make connections to their prior knowledge and expertise, and to be creative in developing and planning new education and outreach activities based on their new knowledge and research. As part of participating in the expedition, participants committed to further developing and testing their education and outreach products after

  2. Mapping of rock types using a joint approach by combining the multivariate statistics, self-organizing map and Bayesian neural networks: an example from IODP 323 site

    Science.gov (United States)

    Karmakar, Mampi; Maiti, Saumen; Singh, Amrita; Ojha, Maheswar; Maity, Bhabani Sankar

    2017-07-01

    Modeling and classification of the subsurface lithology is very important to understand the evolution of the earth system. However, precise classification and mapping of lithology using a single framework are difficult due to the complexity and the nonlinearity of the problem driven by limited core sample information. Here, we implement a joint approach by combining the unsupervised and the supervised methods in a single framework for better classification and mapping of rock types. In the unsupervised method, we use the principal component analysis (PCA), K-means cluster analysis (K-means), dendrogram analysis, Fuzzy C-means (FCM) cluster analysis and self-organizing map (SOM). In the supervised method, we use the Bayesian neural networks (BNN) optimized by the Hybrid Monte Carlo (HMC) (BNN-HMC) and the scaled conjugate gradient (SCG) (BNN-SCG) techniques. We use P-wave velocity, density, neutron porosity, resistivity and gamma ray logs of the well U1343E of the Integrated Ocean Drilling Program (IODP) Expedition 323 in the Bering Sea slope region. While the SOM algorithm allows us to visualize the clustering results in spatial domain, the combined classification schemes (supervised and unsupervised) uncover the different patterns of lithology such of as clayey-silt, diatom-silt and silty-clay from an un-cored section of the drilled hole. In addition, the BNN approach is capable of estimating uncertainty in the predictive modeling of three types of rocks over the entire lithology section at site U1343. Alternate succession of clayey-silt, diatom-silt and silty-clay may be representative of crustal inhomogeneity in general and thus could be a basis for detail study related to the productivity of methane gas in the oceans worldwide. Moreover, at the 530 m depth down below seafloor (DSF), the transition from Pliocene to Pleistocene could be linked to lithological alternation between the clayey-silt and the diatom-silt. The present results could provide the basis for

  3. Oceanographic and meteorological data collected on expeditions of vessels in the academic fleet since 1994, submitted by the Rolling Deck to Repository (R2R) program

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This collection includes oceanographic and meteorological data collected during expeditions of vessels in the academic fleet. The data have been managed using the...

  4. Campanian agglutinated foraminifera from the Lomonosov Ridge, IODP Leg 302 (ACEX): implications for Arctic Late Cretacous paleogeography

    Science.gov (United States)

    Setoyama, E.; Kaminski, M. A.; Tyszka, J.

    2012-04-01

    The biotic history of the Eurasian side of the early Arctic Ocean is known from precious few localities, and these are mainly boreholes drilled along the Arctic margins by the petroleum industry. Most of our knowledge on the foraminiferal record of the Late Cretaceous Arctic Ocean comes from studies of the Canadian and North American Arctic margins in the Mackenzie Delta region. In the Eurasian Arctic region, the Upper Cretaceous is represented by a major hiatus in Spitsbergen and the Northern and Eastern Barents Sea. We document the occurrence of agglutinated foraminifera in Upper Cretaceous (Campanian) sediments recovered during the Arctic Coring Expedition (ACEX), IODP Leg 302. One of the primary drilling objectives of Expedition 302 was to penetrate the post-rift sedimentary cover of the Lomonosov Ridge to determine the age of the break-up unconformity observed in seismic sections. This goal was achieved in Hole M0004A, which recovered two cores of Cretaceous sediments beneath the unconformity. Foraminiferal assemblages consist entirely of agglutinated taxa with 29 taxa including three new species. The agglutinated assemblage from the Lomonosov Ridge represents a shallow, probably restricted, brackish environment, and displays some taxonomic affinity to Late Cretaceous assemblages described from the Beaufort-Mackenzie basin. Comparison of the Lomonosov Ridge assemblages with coeval faunas from the southwestern Barents Sea and Western Siberia reveals that there are no species in common with coeval assemblages described from the southwestern Barents Sea or Western Siberia, and only several cosmopolitan species are in common between the later two regions. Therefore, we suggest that the Arctic Ocean was probably isolated from the North Atlantic faunal province during the Late Cretaceous, with very limited or no marine connections between the Arctic, North Atlantic and Western Siberia over the Barents Shelf. In our opinion the Late Cretaceous paleogeographical

  5. Progressive Curation of IODP Core Material at Kochi Core Center, Japan

    Science.gov (United States)

    Gupta, L. P.; Hisamitsu, T.; Ahagon, N.; Kuramoto, T.; Tokuyama, H.; Kinoshita, M.

    2014-12-01

    Kochi Core Center (KCC) is one of the 3 IODP core repositories in the world, and is in-charge of curating core materials collected/to be collected from most of the Indian Ocean, west Pacific Ocean and Bering Sea. Curation of IODP core material in the KCC began in 2007 as it started receiving 83 km of Legacy cores from the other IODP core repositories. Since then the KCC has not only maintained curatorial standards of the IODP, but also added many services for convenience of the IODP researchers that include curation of cuttings and deep frozen aliquots of cores, open access to logging equipment in the KCC for core measurements, virtual core library to provide quick online access to 3-D XCT images of the cores collected by the D/V Chikyu, online summary of the cores being curated in the KCC, and up-to-date online images of working half to show status of samples available for prospective users. With its existing stock of 104 km of the IODP & Legacy cores and cores to be recovered from the Indian Ocean in near future by the JOIDES Resolution, and a huge new reefer building with storage capacity of ca. 150 km core becoming part of the KCC this August, the KCC is bound to play a significant role in promoting earth and biogeo-sciences throughout the world, especially in neighboring Asian countries.

  6. Microstructure of muddy contourites from the Gulf of Cadiz (IODP Exp. 339)

    Science.gov (United States)

    Nishida, N.

    2014-12-01

    In deep-sea environments, hemipelagites/pelagites and episodic-event deposits are formed from fall out of fine-grained suspensions and from sediment-gravity flows represented by turbidity currents, respectively. In addition, contourites are also formed from bottom currents along the slope. Bottom currents are one of the major processes for the sediment transportation and deposition in deep-sea environments, and are affected by local and global factors such as climate, sea level and tectonics. Therefore, it is important to discriminate the contourites from deep-sea sediments and to clarify their spatial and temporal distribution patterns to reconstruct fluctuations of bottom currents controlled under other factors. In general, major sedimentary facies contourite are characterized by bioturbated mottled facies and bi-gradational grading. However, it is difficult to discriminate muddy contourites from hemipelagites based only on the facies. Therefore, this study focuses on the microstructure of muddy contourites, which would be an additional characteristic/ diagnostic to identify muddy contourites. This study muddy contourites collected from 6 sites are analysed mainly in the Gulf of Cadiz by IODP Expedition 339 (Mediterranean Outflow). In addition, hemipelagites collected from off the west Iberian margin were also examined. Each studied sediments were sub-sampled from the core samples using 7 cc plastic cubes generally used for paleomagnetic analysis. Mean-grain size of the samples was 7.9-25.2 μm, and major mineral components were illite, calcite, and quartz. Most of the samples were wet condition, thus these were dried for SEM observations using a t-butyl alcohol replacing method, which allow us to prepare dried sample without deformation of microstructure. Then the microstructures of the samples were observed using a SEM (JEOL JSM-6390LV). As a result, it is recognized that hemipelagites are composed mainly by calcareous nannoplankton with random orientation of

  7. Expeditions and other exploration

    NARCIS (Netherlands)

    NN,

    1964-01-01

    Previous to the 4th UNESCO Expedition, Dr H. Sleumer of the Rijksherbarium made three trips together with Mr Tem Smitinand, first to Doi Chiengdao and Doi Suthep in the North (Aug. 15-21, 1963), then to the Khao Yai National Park in Central Siam (Aug. 28-29), then to Pha Nok Khao and Phu Krading

  8. Fungal diversity from deep marine subsurface sediments (IODP 317, Canterbury Basin, New Zealand)

    Science.gov (United States)

    Redou, V.; Arzur, D.; Burgaud, G.; Barbier, G.

    2012-12-01

    Recent years have seen a growing interest regarding micro-eukaryotic communities in extreme environments as a third microbial domain after Bacteria and Archaea. However, knowledge is still scarce and the diversity of micro-eukaryotes in such environments remains hidden and their ecological role unknown. Our research program is based on the deep sedimentary layers of the Canterbury Basin in New Zealand (IODP 317) from the subsurface to the record depth of 1884 meters below seafloor. The objectives of our study are (i) to assess the genetic diversity of fungi in deep-sea sediments and (ii) identify the functional part in order to better understand the origin and the ecological role of fungal communities in this extreme ecosystem. Fingerprinting-based methods using capillary electrophoresis single-strand conformation polymorphism and denaturing high-performance liquid chromatography were used as a first step to raise our objectives. Molecular fungal diversity was assessed using amplification of ITS1 (Internal Transcribed Spacer 1) as a biomarker on 11 samples sediments from 3.76 to 1884 meters below seafloor. Fungal molecular signatures were detected throughout the sediment core. The phyla Ascomycota and Basidiomycota were revealed with DNA as well as cDNA. Most of the phylotypes are affiliated to environmental sequences and some to common fungal cultured species. The discovery of a present and metabolically active fungal component in this unique ecosystem allows some interesting first hypotheses that will be further combined to culture-based methods and deeper molecular methods (454 pyrosequencing) to highlight essential informations regarding physiology and ecological role of fungal communities in deep marine sediments.

  9. A lunar polar expedition.

    Science.gov (United States)

    Dowling, Richard; Staehle, Robert L.; Svitek, Thomas

    This paper reviews issues related to a five-person expedition to the lunar north pole which primarily addresses site selection and the requirements for transportation, power, and life support. A one-year stay on the lunar surface is proposed based on available technology, and proposals are detailed for incorporating flight-proven systems, abort or rescue options, and the use of the base as the nucleus for subsequent operations. Specific details are given regarding lunar orbital data, the characteristics of the proposed base, power and consumables requirements, and equipment such as two-person lunar roving vehicles and space suits. During the expedition: (1) water is recycled; (2) Autolanders are used to deliver equipment; (3) two rovers are included in the mass budget; (4) the lunar surface is studied in detail. A polar lunar-base site offers the advantages of unobstructed astronomy, enhanced heat rejection, and the potential for reuse.

  10. Microbial community analysis of deeply buried marine sediments of the New Jersey shallow shelf (IODP Expedition 313).

    Science.gov (United States)

    Breuker, Anja; Stadler, Susanne; Schippers, Axel

    2013-09-01

    The investigated deeply buried marine sediments of the shallow shelf off New Jersey, USA, are characterized by low organic carbon content and total cell counts of Crenarchaeota with 1%, 14%, and 85%, respectively. The typical deep subsurface sediment-associated groups MBG-B, MBG-D, MCG, and SAGMEG were represented in the sediment community. MCG was the dominant group with a high diversity of the isolated 16S rRNA gene sequences. © 2013 Federation of European Microbiological Societies. Published by John Wiley & Sons Ltd. All rights reserved.

  11. IODP Expedition 310 Reconstructs Sea Level, Climatic, and Environmental Changes in the South Pacific during the Last Deglaciation

    Directory of Open Access Journals (Sweden)

    Yasufumi Iryu

    2007-07-01

    Full Text Available The timing and course of the last deglaciation (19,000–6,000 years BP are essential components for understanding the dynamics of large ice sheets (Lindstrom and MacAyeal, 1993 and their effects on Earth’s isostasy (Nakada and Lambeck, 1989; Lambeck, 1993; Peltier, 1994, as well as the complex relationship between freshwater fluxes to the ocean, thermohaline circulation, and, hence, global climate during the Late Pleistocene and the Holocene. Moreover, the lastdeglaciation is generally seen as a possible analogue for the environmental changes and increased sea level that Earth may experience because of the greenhouse effect, related thermal expansion of oceans, and the melting of polar ice sheets.

  12. Miocene-Pliocene alkenone and coccolithophorid stable isotopic data for sea surface condition reconstructions in the Eastern Equatorial Pacific (IODP Site U1338). (Invited)

    Science.gov (United States)

    Beltran, C.; Rousselle, G.; Raffi, I.; Backman, J.; Sicre, M.; de Rafélis, M.; Iodp Expedition 320/321 Shipboard Scientific Party

    2010-12-01

    Coccolithophores play an important role in earth’s biogeochemical cycles due to their great abundance, fast turnover rates, and their ability to carry out photosynthesis and calcification. Although calcareous nannofossils are major producers of carbonates and alkenones in the ocean, the use of coccoliths as a recorder of seawater δ18O and δ13C has been limited by the difficulty of isolating them from the bulk carbonates. Here, we present temperature and δ18O reconstructions over the mid-Miocene through the Plio-Pleistocene from IODP Site U1338 of Expedition 320/321 in the Eastern Equatorial Pacific. Isotopic data were obtained from mono-specific Noealherabdaceae dominated coccolith fine fractions isolated using the granulometric separation technique developed by Minoletti et al., (2009). The nannofossil assemblage compositions and the alkenone-derived SSTs were determined in the same samples and combined to the δ18O and δ13C values measured on the alkenone producing coccoliths to evaluate past sea-surface environmental conditions prevailing in the Equatorial Pacific. These new data based on organic and inorganic compounds produced by coccolithophores offer the potential to extract environmental informations including: sea surface temperature (alkenone unsaturation ratio) and salinity and fertility conditions (coccolith isotopic ratio). Using multiple geochemical proxies derived from a single group of plankton have huge potential for paleoenvironmental reconstructions.

  13. Climate-Ocean-Ice sheet interactions across the Pliocene and Pleistocene: Preliminary Results from IODP 341 Exp (Gulf of Alaska).

    Science.gov (United States)

    Sánchez Montes, Maria Luisa; McClymont, Erin L.; Müller, Juliane; Cowan, Ellen A.; Romero, Oscar E.; Moy, Chris; Lloyd, Jerry M.

    2016-04-01

    Since the Pliocene, global climate history is distinguished by the transition into a colder world, dominated by the onset and intensification of major Northern Hemisphere glaciations which have changed in their duration and intensity. It has been argued that cooling in the surface ocean has been driven by or been conducive to continental ice-sheet growth, or that progressive sub-glacial erosion and feedbacks might explain changing ice-sheet extent and dynamics independently of climate change and/or the potential regional climate impacts of tectonic uplift. At present, isolating climate as the driver of evolving continental ice volume since the Pliocene is hindered by the limited long term data sets which directly link climate changes to evidence for ice-sheet advance/retreat, erosion, and tectonic evolution over million year timescales. IODP Expedition 341 (May-July 2013) drilled a cross-margin transect from ice-proximal sites on the continental shelf to distal sites in the deep Pacific. This study focuses on the two most distal sites (Site U1417, c. 4190 m water depth and Site U1418, c. 3667 m water depth) which extend from modern until the Miocene and Pleistocene, respectively. The sites contain a rich recorded history of climate change, glaciation and tectonics, to allow for a detailed understanding of the interaction between north-east Pacific paleoceanography and the history of the north-west Cordilleran ice sheet, neither of which are fully understood given limited data which pre-dates the Last Glacial Maximum. The focus of this research is to reconstruct sea surface temperatures (SSTs), ice rafted debris (IRD), and primary productivity inputs through the Pliocene and Pleistocene (since ca. 6 Ma). We have reconstructed SSTs using the UK37' index, and compare to the relative abundance of C37:4 alkenone (for subpolar waters), C37 alkenone concentrations (for coccolithophore production), TAR index (to identify the terrestrial or marine source of the organic

  14. Long-term variations of clay mineral composition in the Andaman Sea (IODP Exp. 353 Site U1447): preliminary result

    Science.gov (United States)

    Lee, J.; Khim, B. K.; Cho, H. G.; Kim, S.; 353 Scientists, I. E.

    2016-12-01

    Clay mineral studies in the Bengal Fan have allowed the reconstruction of the erosional history of the Himalayan-Tibetan complex since the Early Miocene. Several factors such as climate change and tectonic activity are important for the erosion rate of the Himalaya-Tibet complex. IODP Expedition 353 Site U1447 (10°47.4'N, 93°00'E; 1391 mbsl) was drilled on a ridge 45 km offshore Little Andaman Island in the Andaman Sea, penetrating to total depths of 738 m. Riverine sediments supplied mainly by the Irrawaddy and Salween (draining the Indo-Burman Ranges; smectite-rich) and the Ganga/Brahmaputra (draining the Himalaya; illite-rich) via the surface currents have been known to deposit in the Andaman Sea. We measured clay minerals of 38 sediment samples collected from 150 to 737 m CSF-A at Site U1447 in order to reveal long-term variation patterns of clay minerals and their controlling factors. Age reconstruction of Site U1447 aided by shipboard biostratigraphic and paleomagnetic data defined the study interval spanning from the Late Miocene ( 10 Ma) to Early Pleistocene ( 1.25 Ma). At this interval, clay minerals consist mainly of smectite (28-61% with an average of 47%) followed by illite (20-41% with an average of 29%), kaolinite (9-19% with an average of 14%), and chlorite (5-15% with an average of 10%). Variation of clay mineral compositions is divided into three stages; almost consistent variations of all clay minerals (from 750 to 570 m CSF-A; 10.0 to 7.5 Ma), gradual decrease of smectite and increase of illite and chlorite (from 570 to 400 m CSF-A; 7.5 to 4.5 Ma), and great fluctuation of all clay minerals (from 400 to 150 m CSF-A; 4.5 to 1.1 Ma). Such long-term clay mineral changes may be related to provenance switches, tectonic evolution of the source regions, climatic variations, degree of volcanism with basin evolution, sedimentation history by sea level changes or some combination of these factors.

  15. Crystallographic preferred orientations and melt-rock interactions : olivine-rich troctolites from IODP Hole U1309D

    Science.gov (United States)

    Drouin, M.; Ildefonse, B.; Hirth, G.; Waters, C. L.; Godard, M.

    2010-12-01

    IODP Expeditions 304-305 sampled the Atlantis Massif, an oceanic core complex located at 30°N in the inside corner of the intersection of the Mid-Atlantic Ridge with the Atlantis Fracture Zone. The most primitive end-members of the recovered gabbroic sequence, olivine-rich troctolites (ol > ~70%), have textures and geochemical compositions intermediate between those of mantle peridotites and primitive cumulates, indicative of melt impregnation processes (Drouin et al., 2009). Olivine-rich troctolites from Hole U1309D (about 5% of recovered rocks) display poikilitic textures, with olivine ranging from coarse-grained subhedral crystals, commonly containing well-developed subgrains, to medium-grained rounded crystals with fewer or no substructures. Olivine substructures reveal dislocation creep that is consistent with activation of the main high-temperature slip systems, dominantly (010)[100]. Olivine crystallographic preferred orientation is very weak, but generally shows a relatively stronger, uncommon [001] concentration (Drouin et al., 2010). These unusual olivine fabrics are interpreted as resulting from dunitisation and melt impregnation of a previously deformed olivine matrix; the solid olivine framework is eventually disrupted by olivine corrosion along grain and subgrain boundaries, and the high-temperature plastic fabric is modified in a liquid-dominated regime. Similar fabrics are described in impregnated peridotites from the mantle/crust transition zone in the Oman ophiolite. A reduction of fabric strength in the presence of melt is also documented in deformation experiments performed in a gas-medium high-pressure high-temperature vessel. Experiments were conducted with olivine + melt (10 to 30 wt%) isostatically hot-pressed initial material. The olivine crystallographic preferred orientation is weaker in deformed sampled than in the undeformed hot pressed material. We propose that very weak fabrics such as those measured in the Atlantis Massif olivine

  16. 12 CFR 347.118 - Expedited processing.

    Science.gov (United States)

    2010-01-01

    ... 12 Banks and Banking 4 2010-01-01 2010-01-01 false Expedited processing. 347.118 Section 347.118... INTERNATIONAL BANKING § 347.118 Expedited processing. (a) Expedited processing of branch applications. An... foreign country, after complying with the expedited processing requirements contained in § 303.182(b) and...

  17. A lunar polar expedition

    Science.gov (United States)

    Dowling, Richard; Staehle, Robert L.; Svitek, Tomas

    1992-01-01

    Advanced exploration and development in harsh environments require mastery of basic human survival skill. Expeditions into the lethal climates of Earth's polar regions offer useful lessons for tommorrow's lunar pioneers. In Arctic and Antarctic exploration, 'wintering over' was a crucial milestone. The ability to establish a supply base and survive months of polar cold and darkness made extensive travel and exploration possible. Because of the possibility of near-constant solar illumination, the lunar polar regions, unlike Earth's may offer the most hospitable site for habitation. The World Space Foundation is examining a scenario for establishing a five-person expeditionary team on the lunar north pole for one year. This paper is a status report on a point design addressing site selection, transportation, power, and life support requirements.

  18. Educational expeditions - et norsk perspektiv

    Directory of Open Access Journals (Sweden)

    Andre Horgen

    2015-06-01

    Full Text Available AbstractThe topic of this article is the Norwegian concept of “friluftsliv” (outdoor life, used as a pedagogical tool to support personal growth. While supporting personal growth appears to be a central pedagogical strategy within Anglo-American and British youth expeditions and adventure programming, this does not appear to be case in the Norwegian outdoor tradition. My research question is: Do Norwegian Outdoor Education students experience a learning outcome related to personal growth, and to their abilities as leaders/mentors, during ski expeditions? I have collected data through a three-year period, after three ski expeditions with Outdoor Education students from an outdoor bachelor-programme at Telemark University College.The students have given written answers to questions regarding personal growth in which several informants’ express thoughts about experiences related to “self” and “identity”. They reflect upon experiences related to “mastering” and “performing”, to acceptance of their own strengths and weaknesses, and about developing self-confidence. They also reflect upon learning outcomes related to interpersonal relations and abilities, self-control, communication and caregiving. The informants have experienced, as leaders/mentors, that it is important to be able to, to “read” situations, to make good assessments of the situations, and to make good decisions related to the situations. As a follow up to this, the informants highlight the importance of being aware of each individual in the group, the importance of encouragement, being positive and caregiving. This study has shown that ski expeditions in “a Norwegian tradition” may have a potential when it comes to encouraging reflections related to personal growth and leadership abilities. Hopefully this study can contribute to increased awareness of the pedagogical potential, for personal growth, within the Norwegian concept of

  19. Magnetic excursions in the late Matuyama Chron (Olduvai to Matuyama-Brunhes boundary) from North Atlantic IODP sites

    Science.gov (United States)

    Channell, J. E. T.

    2017-02-01

    The sedimentary record of late Matuyama magnetic excursions, between the end of the Olduvai Subchron and the Matuyama-Brunhes boundary, has relied on North Atlantic Ocean Drilling Program (ODP) Sites 983/984, and individual recordings at ODP Site 1021 from the California Margin, and Core MD972143 from the west Philippine Sea. North Atlantic IODP Sites U1305, U1306, U1307 (Eirik Drift, off SE Greenland), and Site U1308 (central Atlantic) provide new records from u-channel samples and discrete (8 cm3) cubic samples, collected from multiple holes drilled at each site. The results confirm the existence of the Intra-Jaramillo, Punaruu, Bjorn, Gardar, and Gilsa excursions and possibly the Kamikatsura excursion. These excursions are not recorded at all sampled sites, although they do correspond to excursions recorded at ODP Sites 983/984 and to relative paleointensity minima recorded at all studied sites. For some records, including that of the Bjorn excursion (1251 ka), antipodal magnetization directions yield virtual geomagnetic poles that reach high northern latitudes, implying that the excursion involved reversal of the main axial dipole field. On the other hand, excursions are often partially and inadequately recorded, attributable to a combination of the brevity of geomagnetic excursions, bioturbation, and filtering of the magnetization signal by the detrital remanent magnetization acquisition process, nonuniform sedimentation rates at millennial/centennial scales, and possibly unrecognized drilling/sampling disturbance.

  20. Potato germplasm collecting expedition to Mexico in 1997 : taxonomy and new germplasm resources

    NARCIS (Netherlands)

    Spooner, D.M.; Rivera-Pena, A.; Berg, van den R.G.; Schueler, K.

    2000-01-01

    Wild potato (Solanum sect. Petota) germplasm has been collected in Mexico on nine major expeditions, as determined by 20 collections or more from each expedition currently at the United States potato genebank, the National Research Support Program-6 (NRSP-6). These have resulted in 609 accessions

  1. ISS Expedition 33 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 33 from 07/2012-11/2012. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  2. ISS Expedition 37 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 37 from 05/2013-11/2013. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  3. ISS Expedition 01 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 01 from 10/2000-03/2001. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  4. ISS Expedition 23 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 23 from 12/2009-09/2010. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  5. ISS Expedition 24 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 24 from 04/2010-11/2010. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  6. ISS Expedition 09 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 09 from 04/2004-10/2004. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  7. ISS Expedition 11 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 11 from 04/2005-10/2005. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  8. ISS Expedition 06 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 06 from 11/2002-05/2003. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  9. ISS Expedition 16 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 16 from 10/2007-04/2008. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  10. ISS Expedition 28 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 28 from 04/2011-11/2011. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  11. ISS Expedition 03 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 03 from 08/2001-12/2001. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  12. ISS Expedition 10 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 10 from 10/2004-04/2005. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  13. ISS Expedition 07 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 07 from 04/2003-10/2003. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  14. ISS Expedition 39 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 39 from 11/2013-05/2014. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  15. ISS Expedition 08 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 08 from 10/2003-04/2004. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  16. ISS Expedition 15 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 15 from 04/2007-10/2007. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  17. ISS Expedition 12 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 12 from 10/2005-04/2006. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  18. ISS Expedition 05 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 05 from 06/2002-12/2002. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  19. ISS Expedition 04 Press Kit

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    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 04 from 12/2001-06/2002. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  20. ISS Expedition 42 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 42 from 09/2014-03/2015. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  1. ISS Expedition 38 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 38 from 09/2013-03/2014. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  2. ISS Expedition 43 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 43 from 11/2014-06/2015. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  3. ISS Expedition 19 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 19 from 03/2009-05/2009. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  4. ISS Expedition 14 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 14 from 09/2006-04/2007. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  5. ISS Expedition 36 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 36 from 03/2013-09/2013. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  6. ISS Expedition 34 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 34 from 12/2012-03/2013. Press kits contain information about each mission overview, crew, mission timeline, benefits, and media...

  7. Ultra-High Resolution Late Pleistocene Paleomagnetic Secular Variation Records From the Gulf of Alaska (IODP Exp. 341 Sites U1418 and U1419)

    Science.gov (United States)

    Velle, J. H.; St-Onge, G.; Stoner, J. S.; Mix, A. C.; Walczak, M.; Asahi, H.; Forwick, M.

    2016-12-01

    IODP Expedition 341 in the Gulf of Alaska drilled the upper Surveyor Fan on the continental rise at Site U1418 (58°46.6'N 144°29.6'W; 3667 m water depth) and the continental slope at Site U1419 (59°319'N 144°8'W; 684 m water depth). U-channel paleomagnetic data has so far been collected to depths of 65 m (CCSF-A) at Site U1418 and 112 m (CCSF-A) at Site U1419. The preliminary oxygen isotope (U1418 and U1419) and radiocarbon-based age models (U1419) constrain the studied sequences to approximately 30,000 and 50,000 years, respectively. Sedimentation rates > 300 cm/kyr were resolved in some intervals, and these exceptionally expanded records allow paleomagnetic secular variation (PSV) from the northeastern Pacific to be studied in high-resolution. Alternating field (AF) demagnetization of u-channel samples and hysteresis data from Site U1418 reveal a low coercivity magnetization consistent with pseudo-single domain (PSD) magnetite with only slight down-core variations, resulting in a strong, well-defined (MAD <5°), single component magnetization being preserved. U-channel measurements of Site U1419 display a weaker, but still stable, low coercivity magnetization, also consistent with PSD magnetite as the primary remanence carrier. Inclination patterns can be correlated between Site U1418 and U1419, as well as to other regional records, suggesting that these features are geomagnetic in origin, and that the Gulf of Alaska sedimentary sequences have captured regional scale paleomagnetic secular variations. Normalization of the natural remanent magnetization (NRM) at Site U1418 with anhysteretic remanent magnetization (ARM) over 7 AF demagnetization steps are consistent with relative paleointensity, suggesting the potential for a NE Pacific regional template for stratigraphic correlation through the Late Pleistocene.

  8. Expedition 308 synthesis: overpressure, consolidation, and slope stability on the continental slope of the Gulf of Mexico

    OpenAIRE

    Flemings, P. B.; John, C.; Behrmann, Jan

    2012-01-01

    Integrated Ocean Drilling Program Expedition 308 quantified the coupling between sedimentation, consolidation, overpressure, fluid flow, and slope instability in continental margin settings. We summarize and synthesize peer-reviewed hydrogeologic studies published since the end of Expedition 308 that focus on Expedition 308 sites drilled in Ursa Basin: Sites U1322, U1323, and U1324. There is a rich stratigraphic complexity in the Ursa Basin, deepwater Gulf of Mexico. The ...

  9. NanTroSEIZE: The IODP Nankai Trough Seismogenic Zone Experiment

    Directory of Open Access Journals (Sweden)

    Harold J. Tobin

    2006-03-01

    Full Text Available The IODP Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE will, for the fi rst time ever, attempt to drill into, sample, and instrument the seismogenic portion of a plate-boundary fault or megathrust within a subduction zone. Access to the interior of active faults where in situ processes can be monitored and fresh fault zone materials can be sampled is of fundamental importance to the understanding of earthquake mechanics. As the December 2004 Sumatraearthquake and Indian Ocean tsunami so tragically demonstrated,large subduction earthquakes represent one of the greatest natural hazards on the planet. Accordingly, drilling into and instrumenting an active interplate seismogenic zone is a very high priority in the IODP Initial Science Plan (2001. Through a decade-long series of national and international workshops, a consensus emerged that the Nankai Trough is an ideal place to attempt drilling and monitoring of the seismogenic plate interface. The fi rst phase of NanTroSEIZE drilling operations has now been scheduled for the late summer of 2007. It involves parallel deployment of both the new U.S. Scientifi c Ocean Drilling Vessel (SODV, this volume and the riser drilling vessel Chikyu.

  10. 21 CFR 1401.6 - Expedited process.

    Science.gov (United States)

    2010-04-01

    ... 21 Food and Drugs 9 2010-04-01 2010-04-01 false Expedited process. 1401.6 Section 1401.6 Food and Drugs OFFICE OF NATIONAL DRUG CONTROL POLICY PUBLIC AVAILABILITY OF INFORMATION § 1401.6 Expedited process. (a) Requests and appeals will be given expedited treatment whenever ONDCP determines either: (1...

  11. 7 CFR 1.9 - Expedited processing.

    Science.gov (United States)

    2010-01-01

    ... 7 Agriculture 1 2010-01-01 2010-01-01 false Expedited processing. 1.9 Section 1.9 Agriculture... processing. (a) A requester may apply for expedited processing at the time of the initial request for records. Within ten calendar days of its receipt of a request for expedited processing, an agency shall decide...

  12. 21 CFR 20.44 - Expedited processing.

    Science.gov (United States)

    2010-04-01

    ... 21 Food and Drugs 1 2010-04-01 2010-04-01 false Expedited processing. 20.44 Section 20.44 Food and... Procedures and Fees § 20.44 Expedited processing. (a) The Food and Drug Administration will provide expedited processing of a request for records when the requester demonstrates a compelling need, or in other cases as...

  13. 28 CFR 802.8 - Expedited processing.

    Science.gov (United States)

    2010-07-01

    ... 28 Judicial Administration 2 2010-07-01 2010-07-01 false Expedited processing. 802.8 Section 802.8... DISCLOSURE OF RECORDS Freedom of Information Act § 802.8 Expedited processing. (a) Requests and appeals will... basis. (b) If you seek expedited processing, you must submit a statement, certified to be true and...

  14. Copper and zinc isotope systematics of altered oceanic crust at IODP Site 1256 in the eastern equatorial Pacific

    Science.gov (United States)

    Huang, Jian; Liu, Sheng-Ao; Gao, Yongjun; Xiao, Yilin; Chen, Sha

    2016-10-01

    This paper presents the first combined Cu and Zn isotopic study of altered oceanic crust at Integrated Ocean Drilling Program (IODP) Hole 1256D that penetrates a volcanic section, a lava-dyke transition zone, a sheeted dyke complex, and a plutonic complex. In the volcanic section, all but one rocks have Cu and Zn isotopic compositions similar to fresh mid-ocean ridge basalt (MORB), reflecting restricted seawater circulation and low oxygen fugacity. Rocks in the transition zone have MORB-like δ65Cu and δ66Zn, indicating the dominant influence of basalt-derived Cu and Zn during alteration. Rocks in the dyke complex have more variable δ65Cu (-0.50-0.90‰) and δ66Zn (0.19-0.55‰) and those in the plutonic complex have δ65Cu of -0.43 to 0.20‰ and δ66Zn of 0.21 to 0.41‰. The rocks with heavier δ66Zn and heavier or lighter δ65Cu relative to MORB are characterized by Cu-Zn depletions, low Li/Yb (<1.0) and low δ18O (<5‰), suggesting that hydrothermal extraction during high temperature alteration of oceanic crust can result in significant Cu and Zn isotope fractionation. Such large Cu and Zn isotopic variations are the results of redox transformation of Cu as well as Cu and Zn isotope fractionation between altered basaltic rocks and dissolved Cu and Zn species in hydrothermal fluids (e.g., [CuCl3]1-, Zn(HS)42-). This work is the first to define the distribution of Cu and Zn isotopes in an intact oceanic crust with concentration-weighted averages of δ65Cu (0.05 ± 0.03‰) and δ66Zn (0.27 ± 0.01‰). The potential implications of these new observations are discussed.

  15. Microbial community stratification controlled by the subseafloor fluid flow and geothermal gradient at the Iheya North hydrothermal field in the Mid-Okinawa Trough (Integrated Ocean Drilling Program Expedition 331).

    Science.gov (United States)

    Yanagawa, Katsunori; Breuker, Anja; Schippers, Axel; Nishizawa, Manabu; Ijiri, Akira; Hirai, Miho; Takaki, Yoshihiro; Sunamura, Michinari; Urabe, Tetsuro; Nunoura, Takuro; Takai, Ken

    2014-10-01

    The impacts of lithologic structure and geothermal gradient on subseafloor microbial communities were investigated at a marginal site of the Iheya North hydrothermal field in the Mid-Okinawa Trough. Subsurface marine sediments composed of hemipelagic muds and volcaniclastic deposits were recovered through a depth of 151 m below the seafloor at site C0017 during Integrated Ocean Drilling Program Expedition 331. Microbial communities inferred from 16S rRNA gene clone sequencing in low-temperature hemipelagic sediments were mainly composed of members of the Chloroflexi and deep-sea archaeal group. In contrast, 16S rRNA gene sequences of marine group I Thaumarchaeota dominated the microbial phylotype communities in the coarse-grained pumiceous gravels interbedded between the hemipelagic sediments. Based on the physical properties of sediments such as temperature and permeability, the porewater chemistry, and the microbial phylotype compositions, the shift in the physical properties of the sediments is suggested to induce a potential subseafloor recharging flow of oxygenated seawater in the permeable zone, leading to the generation of variable chemical environments and microbial communities in the subseafloor habitats. In addition, the deepest section of sediments under high-temperature conditions (∼90°C) harbored the sequences of an uncultivated archaeal lineage of hot water crenarchaeotic group IV that may be associated with the high-temperature hydrothermal fluid flow. These results indicate that the subseafloor microbial community compositions and functions at the marginal site of the hydrothermal field are highly affected by the complex fluid flow structure, such as recharging seawater and underlying hydrothermal fluids, coupled with the lithologic transition of sediments. Copyright © 2014, American Society for Microbiology. All Rights Reserved.

  16. PREFACE: Ocean and climate changes in polar and sub-polar environments: proceedings from the 2010 IODP-Canada/ECORD summer school

    Science.gov (United States)

    St-Onge, Guillaume; Veiga-Pires, Cristina; Solignac, Sandrine

    2011-05-01

    IODP logoECORD logo The European Consortium for Ocean Drilling Program (ECORD), the Canadian Consortium for Ocean Drilling (CCOD), the Network of the Universités du Québec (UQ), the Université du Québec à Montréal (UQAM) and GEOTOP sponsored, in 2010, a summer school entitled 'Ocean and climate changes in polar and sub-polar environments'. This summer school took place from 27 June to 12 July in Rimouski, Québec city and Montréal (Quebec, Canada) and was attended by nineteen students and postdoctoral fellows from seven countries: Canada, France, Germany, UK, Serbia, Portugal and the USA. Lectures, hands-on laboratory exercises and laboratory visits were conducted at the Institut des Sciences de la Mer de Rimouski (ISMER), Institut National de la Recherche Scientifique - Centre Eau Terre Environnement (INRS-ETE) and UQAM, in addition to two field trips and a short geological and geophysical cruise on board the R/V Coriolis II in the St Lawrence Estuary and Saguenay Fjord. During the summer school, more than twenty researchers gave lectures on the use of several paleoceanographic and geophysical techniques to reconstruct ocean and climate changes in polar and sub-polar environments. Some of these lectures are presented as short review papers in this volume. They are intended to portray a brief, but state-of-the-art overview of an array of techniques applied to Arctic and sub-Arctic environments, as well as the geological background information needed by the summer school participants to put the scientific expedition and fieldwork into context. The volume begins with a view on the great challenges and key issues to be addressed in the Arctic Ocean (Stein) in the forthcoming years and is followed by a review (O'Regan) on Late Cenozoic paleoceanography of the Central Arctic. The two subsequent papers (St-Onge et al and de Vernal et al) deal with the oceanographic, paleoceanographic and geological context of the Saguenay Fjord, and St Lawrence Estuary and Gulf

  17. The "DREAM" IODP project to drill the Mediterranean Salt Giant on the Balearic Promontory

    Science.gov (United States)

    Lofi, Johanna; Camerlenghi, Angelo; Aloisi, Giovanni; Maillard, Agnès; Garcia-Castellanos, Daniel; Huebscher, Christian; Kuroda, Junichiro

    2017-04-01

    Salt giants preserving kilometer-thick evaporite layers are the sedimentary expression of extreme environmental events of global relevance. Despite their global occurrence and general importance on Earth, there is currently no complete stratigraphic record through an un-deformed salt giant of marine origin. Similarly, there is a significant lack of knowledge about the factors controlling salt giants deposition, their early evolution, the impact they exert on the isostatic response of continental margins and on sub-salt formations, and the unprecedented deep biosphere they may harbor. The Mediterranean Messinian salt giant, which formed 5.5 Myrs ago, is one of the youngest salt giant on Earth and is currently lying below the Plio-Quaternary cover in a relatively un-deformed state close to its original depositional configuration. This salt giant is thus accessible by drilling and forms an ideal case study that could be used as a reference for older salt giants. However, since its discovery in 1970 during the DSDP Leg XIII, and despite 40 years or multi-disciplinary researches, this salt giant is still not fully understood and remains one of the longest-living controversies in Earth Science. In this context, the IODP DREAM project aims at exploring the Mediterranean salt giant by drilling with the JOIDES Resolution a transect of 4 sites on the southern margin of the Balearic promontory (Western Mediterranean). We identified this area as likely the only place in the Mediterranean where we could implement a shallow-to-deep transect of non-riser drilling sites. Due to the geological history and pre-structuration of the Promontory, MSC deposits are found preserved in a series of sedimentary basins lying at different water depths between the present-day coastline and the deep central salt basins. DREAM thus offers a unique opportunity to sample several hundred of meters of material forming the Mediterranean salt giant in varied water depths. This unique sedimentary record

  18. Okeanos Explorer 2014 Gulf of Mexico Expedition: engaging and connecting with diverse and geographically dispersed audiences

    Science.gov (United States)

    Russell, C. W.; Elliott, K.; Lobecker, E.; McKenna, L.; Haynes, S.; Crum, E.; Gorell, F.

    2014-12-01

    From February to May 2014, NOAA Ship Okeanos Explorer conducted a telepresence-enabled ocean exploration expedition addressing NOAA and National deepwater priorities in the U.S. Gulf of Mexico. The community-driven expedition connected diverse and geographically dispersed audiences including scientists from industry, academia, and government, and educators, students, and the general public. Expedition planning included input from the ocean science and management community, and was executed with more than 70 scientists and students from 14 U.S. states participating from shore in real time. Training the next generation permeated operations: a mapping internship program trained undergraduate and graduate students; an ROV mentorship program trained young engineers to design, build and operate the system; and undergraduate through doctoral students around the country collaborated with expedition scientists via telepresence. Online coverage of the expedition included background materials, daily updates, and mission logs that received more than 100,000 visits by the public. Live video feeds of operations received more than 700,000 views online. Additionally, professional development workshops hosted in multiple locations throughout the spring introduced educators to the Okeanos Explorer Educational Materials Collection and the live expedition, and taught them how to use the website and education resources in their classrooms. Social media furthered the reach of the expedition to new audiences, garnered thousands of new followers and provided another medium for real-time interactions with the general public. Outreach continued through live interactions with museums and aquariums, Exploration Command Center tours, outreach conducted by partners, and media coverage in more than 190 outlets in the U.S. and Europe. Ship tours were conducted when the ship came in to port to engage local scientists, ocean managers, and educators. After the expedition, data and products were

  19. ISS Potable Water Quality for Expeditions 26 through 30

    Science.gov (United States)

    Straub, John E., II; Plumlee, Debrah K.; Schultz, John R.; McCoy, J. Torin

    2012-01-01

    International Space Station (ISS) Expeditions 26-30 spanned a 16-month period beginning in November of 2010 wherein the final 3 flights of the Space Shuttle program finished ISS construction and delivered supplies to support the post-shuttle era of station operations. Expedition crews relied on several sources of potable water during this period, including water recovered from urine distillate and humidity condensate by the U.S. water processor, water regenerated from humidity condensate by the Russian water recovery system, and Russian ground-supplied potable water. Potable water samples collected during Expeditions 26-30 were returned on Shuttle flights STS-133 (ULF5), STS-134 (ULF6), and STS-135 (ULF7), as well as Soyuz flights 24-27. The chemical quality of the ISS potable water supplies continued to be verified by the Johnson Space Center s Water and Food Analytical Laboratory (WAFAL) via analyses of returned water samples. This paper presents the chemical analysis results for water samples returned from Expeditions 26-30 and discusses their compliance with ISS potable water standards. The presence or absence of dimethylsilanediol (DMSD) is specifically addressed, since DMSD was identified as the primary cause of the temporary rise and fall in total organic carbon of the U.S. product water that occurred in the summer of 2010.

  20. Variations of the Indian summer monsoon over the Mio-Pliocene recorded in the Bengal Fan (IODP Exp354): implications for the evolution of the terrestrial biosphere.

    Science.gov (United States)

    Galy, Valier; Feakins, Sarah; Karkabi, Elias; Ponton, Camilo; Galy, Albert; France-Lanord, Christian

    2017-04-01

    A pressing challenge in climate research is understanding the temporal evolution of the Indian monsoon system; its response to global and regional climatic controls (including warming); as well as implications in terms of vegetation (C4 expansion), erosion of the Himalaya and carbon sequestration in the Bengal Fan. Studies on climate dynamics have recently offered new insights into the mechanistic controls on the monsoon: the tectonic boundary of the Himalaya is implicated as the major control on Indian summer monsoon dynamics today. Since this region has been uplifted since at least the late Oligocene, it is possible to test the response of monsoon precipitation to global and regional climate change, and also understand feedbacks on the climate system via carbon sequestration in the Bengal Fan. The evidence for monsoon intensity changes across the Miocene and Pliocene is currently incomplete given temporal uncertainty and diagenesis in terrestrial records; biases in the records reconstructed from the distal fan; and conflicting evidence from wind speed and aridity metrics for a stronger or weaker monsoon. Our alternative approach is therefore to study the basin-wide hydrological changes recorded in a multi-proxy, multi-site study of the marine sediments of the Bengal Fan recovered during IODP expedition 354. In turbiditic sediments of Himalayan origin, the late Miocene C4 expansion was found in all three long records recovered during expedition 354 (i.e. at sites U1451, U1450 and U1455, from East to West) based on stable carbon isotope composition of terrestrial leaf-wax compounds. Cores from sites U1455 (a reoccupation of DSDP Leg 22 Site 218) provide the highest resolution record of the C4 transition, which appears to occur abruptly within a relatively continuous series of turbiditic sequences. Bio- and magneto-stratigraphic dating of these records by members of Expedition 354 science party is underway and will provide the best stratigraphic constraint of the C4

  1. Intermediate to deep water hydrographic changes of the Japan Sea over the past 10 Myr, inferred from radiolarian data (IODP Exp. 346, Site U1425)

    Science.gov (United States)

    Matsuzaki, Kenji M.; Itaki, Takuya; Tada, Ryuji; Kurokawa, Shunsuke

    2017-04-01

    The Japan Sea is a back-arc basin opened under a continental rifting during the Early to Middle Miocene (ca. 25-13 Ma). This area is characterized by active tectonism, which drastically modified the Japan Sea paleogeography such as the sill depth of its key straits. In modern condition, the Japan Sea is connected to adjacent marginal seas and the Pacific Ocean by four straits shallower than 130 m. These straits are the Tsushima Strait connecting to the East China Sea, the Tsugaru Strait connecting to the Pacific, and the Soya and Mamiya Straits connecting to the Sea of Okhotsk. Therefore, the intermediate and deep water of the Japan Sea is isolated, leading the formation of a unique and regional deep sea water, known as the Japan Sea Proper Water. However, past studies show that during the late Miocene and Pliocene, only the Tsugaru Strait connecting to the North Pacific was opened. This strait was deeper during Plio-Miocene and have likely enable inflow of deep to intermediate water of the North Pacific in the Japan Sea. Radiolarians are one of the planktic micro-organisms group bearing siliceous skeletons. Their species comprise shallow to deep water dwellers, sensitive to changes in sea water physical/ecological properties forced by climate changes. Their fossils are known for be well preserved in the deep-sea sediments of the North Pacific. Therefore, in this study we propose to monitor changes in intermediate to deep water hydrography of the Japan Sea since the late Miocene, using radiolarian as an environmental proxy. In 2013 the IODP Expedition 346 retrieved sediment cores at different sites in the Japan Sea. In this study, we have analyzed 139 core sediments samples collected at Site U1425. This site is situated in the middle of the Yamato Bank. We selected this site because the past 10 Myr could be recovered continuously without hiatuses. Changes in radiolarian assemblages reveal that the oceanographic setting of the Japan Sea changed drastically at ca. 2

  2. Links Between Eustatic History, Sequence Architecture, and Lithofacies Associations Put to the Test: IODP Exp313 Drilling on the NJ Margin

    Science.gov (United States)

    Mountain, G. S.; Proust, J.; McInroy, D.; Scienceparty, E.

    2009-12-01

    The New Jersey continental margin is a natural laboratory for tracking the history of global sea level during the post-Eocene ice-house world. In May-July 2009, IODP Expedition 313 used a "mission-specific" jack-up platform in 35 m of water, 45-65 km off the coast of New Jersey to core and log Paleogene-Neogene sequences. The goal was to: (1) compare ages of the unconformities bracketing these sequences with the ages of sea-level lowerings predicted by the δ18O glacio-eustatic proxy; (2) estimate the corresponding amplitudes, rates and mechanisms of sea-level change; and (3) evaluate sequence stratigraphic lithofacies models that predict depositional environments, sediment compositions, and stratal geometries in response to sea-level change. Despite the difficulties of coring the sandy shallow NJ shelf, we collected 612 cores with 80% recovery totaling 1311 m in length. The deepest hole was 757 mbsf; the oldest sediment was late Eocene. Slim-line logs at each site gathered spectral gamma ray, resistivity, magnetic susceptibility, sonic and acoustic televiewer measurements. A vertical seismic profile was run at each location. There was no facility to split and examine the cores offshore. Instead, we did basic sedimentological analyses of core catcher samples and through-liner descriptions were conducted. These observations, together with log and multi-sensor track measurements of unsplit core sections, revealed patterns of fluvial, coastal plain, shoreface and open marine lithofacies that appear to closely track sequences in seismic profiles through each drill site. We cored regressive sediment bodies that were not present in onshore boreholes, and we expect final analysis will reveal the record of roughly ten complete cycles of relative sea-level fall and rise that we will compare to the global record. Pore water extracted from unsplit cores revealed chlorinity values significantly above and below that of seawater, distributed in spatial patterns that are clearly

  3. Changing sediment physical properties at the Agulhas Plateau (IODP Site U1475): indications for the long-term variability of deepwater circulation over the last 7 Ma

    Science.gov (United States)

    Gruetzner, Jens; Lathika, Nambiyathodi; Jimenez Espejo, Francisco J.; Uenzelmann-Neben, Gabriele

    2017-04-01

    The gateway south of South Africa constitutes an integral inter-ocean link in the global thermohaline circulation (THC) since it allows the exchange of shallow- and deepwater masses between the Indian and the Atlantic. Thus understanding past variations of this current system is important for improving our knowledge of the global climate. The long-term changes in deepwater flow in the Atlantic-Indian gateway during the Cenozoic have been initially studied using reflection seismic profiles. But in many cases the seismic stratigraphy is poorly constrained and not further resolved within the time period from the late Miocene to present. In particular, there are limited Pliocene records that can be used to investigate the influence of climatic (e.g. Antartic ice volume) and tectonic (e.g. closure of the central American seaway) on the deep-water variability. Here we focus on the bottom water flow around the Agulhas Plateau, a location proximal to the entrance of North Atlantic Deep Water (NADW) to the Southern Ocean and South Indian Ocean. IODP Expedition 361 (SAFARI) Site U1475 was drilled in 2669 m water depth into a sediment drift that is deposited on the southwestern flank of Agulhas Plateau and comprises a complete stratigraphic section of the last 7 Ma. We present cleaned, edited, and spliced high-resolution data sets of sediment physical properties measured at Site U1475. Synthetic seismograms generated from the velocity and bulk density core scanning records allow a detailed correlation oft the drilling results with the Site survey seismic reflection profiles. Seismic reflectors at 3.75 and 3.87 s (two-way-traveltime) correspond to major increases in acoustic impedance at 110 and 216 meters below seafloor. Based on the preliminary shipboard biostratigraphic age model sediments at these depths have ages of 4.0 and 5.1 Ma, respectively. Furthermore spectral analyses of physical property records such as natural gamma radiation and colour reflectance reveal climate

  4. IODP workshop: developing scientific drilling proposals for the Argentina Passive Volcanic Continental Margin (APVCM) - basin evolution, deep biosphere, hydrates, sediment dynamics and ocean evolution

    Science.gov (United States)

    Flood, Roger D.; Violante, Roberto A.; Gorgas, Thomas; Schwarz, Ernesto; Grützner, Jens; Uenzelmann-Neben, Gabriele; Hernández-Molina, F. Javier; Biddle, Jennifer; St-Onge, Guillaume; Workshop Participants, Apvcm

    2017-05-01

    The Argentine margin contains important sedimentological, paleontological and chemical records of regional and local tectonic evolution, sea level, climate evolution and ocean circulation since the opening of the South Atlantic in the Late Jurassic-Early Cretaceous as well as the present-day results of post-depositional chemical and biological alteration. Despite its important location, which underlies the exchange of southern- and northern-sourced water masses, the Argentine margin has not been investigated in detail using scientific drilling techniques, perhaps because the margin has the reputation of being erosional. However, a number of papers published since 2009 have reported new high-resolution and/or multichannel seismic surveys, often combined with multi-beam bathymetric data, which show the common occurrence of layered sediments and prominent sediment drifts on the Argentine and adjacent Uruguayan margins. There has also been significant progress in studying the climatic records in surficial and near-surface sediments recovered in sediment cores from the Argentine margin. Encouraged by these recent results, our 3.5-day IODP (International Ocean Discovery Program) workshop in Buenos Aires (8-11 September 2015) focused on opportunities for scientific drilling on the Atlantic margin of Argentina, which lies beneath a key portion of the global ocean conveyor belt of thermohaline circulation. Significant opportunities exist to study the tectonic evolution, paleoceanography and stratigraphy, sedimentology, and biosphere and geochemistry of this margin.

  5. 31 CFR 10.82 - Expedited suspension.

    Science.gov (United States)

    2010-07-01

    ... 31 Money and Finance: Treasury 1 2010-07-01 2010-07-01 false Expedited suspension. 10.82 Section... INTERNAL REVENUE SERVICE Rules Applicable to Disciplinary Proceedings § 10.82 Expedited suspension. (a... suspension. A suspension under this section will commence on the date that written notice of the suspension...

  6. Book Review Expedition Field Techniques: Small Mammals ...

    African Journals Online (AJOL)

    Book Review. Expedition Field Techniques: Small. Mammals (excluding bats) Second Edition. A. Barnett and J. Dutton. Published and distributed 1995 by the Expedition Advisory. Cenlre, Royal Geographic Society, 1 Kensington Gore,. London, SW7 2AR. 126 pages. Price: £8.50 (softcover). ISBN 0-907649-68-8.

  7. Cobb Mountain Subchron recorded at IODP Site U1306 (Eirik Drift, off SE Greenland)

    Science.gov (United States)

    Channell, J. E. T.

    2017-06-01

    The Cobb Mountain Subchron (CMS) is recorded over ∼5 m of core at ∼180 metres composite depth in the sediment sequence recovered at IODP Site U1306, in an interval where sedimentation rates are estimated at ∼15 cm kyr-1. The relatively high-resolution record of the CMS was acquired from u-channel samples from multiple core sections from four holes drilled at the site. Large-scale swings in magnetization directions at the onset of the subchron lead to virtual geomagnetic poles (VGPs) looping over the Indian Ocean, followed by a looping transit northward through the central Pacific Ocean, a ∼10 kyr (∼1.7 m) interval of VGPs at high northern latitudes particularly in the North Atlantic and NW Pacific Oceans, followed by an abrupt normal to reverse transition as VGPs track southward through Africa. Although the VGP paths are intricate and complex, they can be compared with other CMS VGP paths from Pacific and Atlantic sites, including ODP Sites 983 and 984. The age model for Site U1306 places the CMS in the 1178-1215 ka interval (∼37 kyr duration) which bridges marine isotope stages 35-36.

  8. Utilizing the International GeoSample Number Concept during ICDP Expedition COSC

    Science.gov (United States)

    Conze, Ronald; Lorenz, Henning; Ulbricht, Damian; Gorgas, Thomas; Elger, Kirsten

    2016-04-01

    The concept of the International GeoSample Number (IGSN) was introduced to uniquely identify and register geo-related sample material, and make it retrievable via electronic media (e.g., SESAR - http://www.geosamples.org/igsnabout). The general aim of the IGSN concept is to improve accessing stored sample material worldwide, enable the exact identification, its origin and provenance, and also the exact and complete citation of acquired samples throughout the literature. The ICDP expedition COSC (Collisional Orogeny in the Scandinavian Caledonides, http://cosc.icdp-online.org) prompted for the first time in ICDP's history to assign and register IGSNs during an ongoing drilling campaign. ICDP drilling expeditions are using commonly the Drilling Information System DIS (http://doi.org/10.2204/iodp.sd.4.07.2007) for the inventory of recovered sample material. During COSC IGSNs were assigned to every drill hole, core run, core section, and sample taken from core material. The original IGSN specification has been extended to achieve the required uniqueness of IGSNs with our offline-procedure. The ICDP name space indicator and the Expedition ID (5054) are forming an extended prefix (ICDP5054). For every type of sample material, an encoded sequence of characters follows. This sequence is derived from the DIS naming convention which is unique from the beginning. Thereby every ICDP expedition has an unlimited name space for IGSN assignments. This direct derivation of IGSNs from the DIS database context ensures the distinct parent-child hierarchy of the IGSNs among each other. In the case of COSC this method of inventory-keeping of all drill cores was done routinely using the ExpeditionDIS during field work and subsequent sampling party. After completing the field campaign, all sample material was transferred to the "Nationales Bohrkernlager" in Berlin-Spandau, Germany. Corresponding data was subsequently imported into the CurationDIS used at the aforementioned core storage

  9. 29 CFR 1404.20 - Proper use of expedited arbitration.

    Science.gov (United States)

    2010-07-01

    ... 29 Labor 4 2010-07-01 2010-07-01 false Proper use of expedited arbitration. 1404.20 Section 1404... ARBITRATION SERVICES Expedited Arbitration § 1404.20 Proper use of expedited arbitration. (a) FMCS reserves the right to cease honoring request for Expedited Arbitration if a pattern of misuse of this becomes...

  10. ISS Expedition 21/22 Press Kit

    Data.gov (United States)

    National Aeronautics and Space Administration — Press kit for ISS mission Expedition 21/22 from 10/2009-03/2010. Press kits contain information about each mission overview, crew, mission timeline, benefits, and...

  11. The Igneous Architecture of IODP Hole U1309D: Constructing Oceanic Crust from Multiple Sills

    Science.gov (United States)

    Christofferson, C. A.; John, B. E.; Cheadle, M. J.; Swapp, S. M.; Grimes, C. B.

    2010-12-01

    Gabbroic rocks comprise a significant portion of the footwall of many oceanic core complexes. The decreasing age of these gabbros from the breakaway to the termination suggests that they are continuously accreted as the bounding detachment fault slips. But, questions remain; how are these large (>1 km diameter) gabbroic bodies constructed and at what scale and frequency is melt added to the system? Here we report a detailed lithologic analysis of IODP Hole U1309D drilled into the Atlantis Massif core complex (30° N, MAR). We present new, high resolution (1m scale) downhole lithological diagrams, compiled from observations of the archive core, refined using other available data including magnetic susceptibility. These data show that the thickness of the individual magmatic units is on the order of 1 to a few 10’s of m. Contacts between many of these units are sharp; many of the units are interpreted to result from small injections of melt as opposed to in-situ fractionation. However, these units are often disaggregated by later intrusive bodies and hence, it is likely that individual gabbro units were initially somewhat thicker. Downhole plots of magmatic fabric dip from both shipboard data and new electron backscatter diffraction (EBSD) data are consistent with the units having initially been intruded as sills, and subsequently rotated by ~40-50°, as constrained by paleomagnetic data (Morris et al., 2009). Using all of the available data, we propose the IODP Hole 1309D gabbro section is a composite body that grew episodically by relatively small (10’s m) repeated sill-like injections of melt. We conclude that the melt lens that formed these gabbros was relatively small at any one time. The EBSD data also provide textural constraints on the model for crustal accretion. Gabbroic samples analyzed so far show a moderate to weak plagioclase and clinopyroxene foliation, similar to those in continental mafic intrusions and are thus interpreted to be magmatic fabrics

  12. A foraminiferal study on Middle Eocene-Oligocene break-up unconformity in northern Taiwan and its correlation with IODP Site U1435 to constrain the onset event of South China Sea opening

    Science.gov (United States)

    Huang, Chi-Yue; Shea, Kai-Hsuan; Li, Qianyu

    2017-05-01

    Taiwan is situated in the SE Asian continental margin where lower Cenozoic strata are well exposed. Its geological and tectonic setting provides a unique opportunity to study the time constraint of the break-up unconformity relevant to the opening of the South China Sea. A detailed foraminiferal study on four land sections and a deep core across the boundary between the Upper and Lower Wulai Groups in the Hsüehshan Range, northern Taiwan, was conducted. Results show remarkable changes of depositional environment and lithology from the amalgamated fluvial dominant sandstones (>2000 m) of Middle Eocene in the Lower Wulai Group to the overlying inner neritic shales and siltstones (>2000 m) of Oligocene in the Upper Wulai Group. Integrated sedimentological and foraminiferal data further suggest an occurrence of a depositional hiatus between 32 ∼33 and 40 Ma across the boundary between the Kankou Formation of the Upper Wulai Group and the Szeleng Sandstone of the Lower Wulai Group in the northern Hsüehshan Range, as same as the scenario seen in the Western Foothills (25-39 Ma) of central Taiwan and the Penghu Basin (25-40 Ma) in the Taiwan Strait. This stratigraphic hiatus in the Taiwan mountain belt marks a regional break-up unconformity between the Middle Eocene syn-rift strata and the overlying Oligocene post-rift sequences in the NE South China Sea. The break-up unconformity can be correlated with those commonly recognized in the seismic profiles of the Pearl River Mouth Basin and drilling of the IODP site U1435 (Expedition 349) in the northern shelf-slope of the South China Sea. The upper time limit of the breakup unconformity 32 Ma could mark the tectonic change from rifting to depression in the Paleogene Asian continental margin which eventually led to opening of the deep South China Sea in the Early Oligocene (∼33 Ma).

  13. Metagenomics of the subsurface Brazos-Trinity Basin (IODP site 1320): comparison with other sediment and pyrosequenced metagenomes.

    Science.gov (United States)

    Biddle, Jennifer F; White, James Robert; Teske, Andreas P; House, Christopher H

    2011-06-01

    The Brazos-Trinity Basin on the slope of the Gulf of Mexico passive margin was drilled during Integrated Ocean Drilling Progam Expedition 308. The buried anaerobic sediments of this basin are largely organic-poor and have few microbial inhabitants compared with the organic-rich sediments with high cell counts from the Peru Margin that were drilled during Ocean Drilling Program Leg 201. Nucleic acids were extracted from Brazos-Trinity Basin sediments and were subjected to whole-genome amplification and pyrosequencing. A comparison of the Brazos-Trinity Basin metagenome, consisting of 105 Mbp, and the existing Peru Margin metagenome revealed trends linking gene content, phylogenetic content, geological location and geochemical regime. The major microbial groups (Proteobacteria, Firmicutes, Euryarchaeota and Chloroflexi) occur consistently throughout all samples, yet their shifting abundances allow for discrimination between samples. The cluster of orthologous groups category abundances for some classes of genes are correlated with geochemical factors, such as the level of ammonia. Here we describe the sediment metagenome from the oligotrophic Brazos-Trinity Basin (Site 1320) and show similarities and differences with the dataset from the Pacific Peru Margin (Site 1229) and other pyrosequenced datasets. The microbial community found at Integrated Ocean Drilling Program Site 1320 likely represents the subsurface microbial inhabitants of turbiditic slopes that lack substantial upwelling.

  14. Video at Sea: Telling the Stories of the International Ocean Discovery Program

    Science.gov (United States)

    Wright, M.; Harned, D.

    2014-12-01

    Seagoing science expeditions offer an ideal opportunity for storytelling. While many disciplines involve fieldwork, few offer the adventure of spending two months at sea on a vessel hundreds of miles from shore with several dozen strangers from all over the world. As a medium, video is nearly ideal for telling these stories; it can capture the thrill of discovery, the agony of disappointment, the everyday details of life at sea, and everything in between. At the International Ocean Discovery Program (IODP, formerly the Integrated Ocean Drilling Program), we have used video as a storytelling medium for several years with great success. Over this timeframe, camera equipment and editing software have become cheaper and easier to use, while web sites such as YouTube and Vimeo have enabled sharing with just a few mouse clicks. When it comes to telling science stories with video, the barriers to entry have never been lower. As such, we have experimented with many different approaches and a wide range of styles. On one end of the spectrum, live "ship-to-shore" broadcasts with school groups - conducted with an iPad and free videoconferencing software such as Skype and Zoom - enable curious minds to engage directly with scientists in real-time. We have also contracted with professional videographers and animators who offer the experience, skill, and equipment needed to produce polished clips of the highest caliber. Amateur videographers (including some scientists looking to make use of their free time on board) have shot and produced impressive shorts using little more than a phone camera. In this talk, I will provide a brief overview of our efforts to connect with the public using video, including a look at how effective certain tactics are for connecting to specific audiences.

  15. 42 CFR 8.28 - Expedited procedures for review of immediate suspension.

    Science.gov (United States)

    2010-10-01

    ... GENERAL PROVISIONS CERTIFICATION OF OPIOID TREATMENT PROGRAMS Procedures for Review of Suspension or Proposed Revocation of OTP Certification, and of Adverse Action Regarding Withdrawal of Approval of an Accreditation Body § 8.28 Expedited procedures for review of immediate suspension. (a) Applicability. When the...

  16. Rock magnetic and geochemical evidence for authigenic magnetite formation via iron reduction in coal-bearing sediments offshore Shimokita Peninsula, Japan (IODP Site C0020)

    Science.gov (United States)

    Phillips, Stephen C.; Johnson, Joel E.; Clyde, William C.; Setera, Jacob B.; Maxbauer, Daniel P.; Severmann, Silke; Riedinger, Natascha

    2017-06-01

    Sediments recovered at Integrated Ocean Drilling Program (IODP) Site C0020, in a fore-arc basin offshore Shimokita Peninsula, Japan, include numerous coal beds (0.3-7 m thick) that are associated with a transition from a terrestrial to marine depositional environment. Within the primary coal-bearing unit (˜2 km depth below seafloor) there are sharp increases in magnetic susceptibility in close proximity to the coal beds, superimposed on a background of consistently low magnetic susceptibility throughout the remainder of the recovered stratigraphic sequence. We investigate the source of the magnetic susceptibility variability and characterize the dominant magnetic assemblage throughout the entire cored record, using isothermal remanent magnetization (IRM), thermal demagnetization, anhysteretic remanent magnetization (ARM), iron speciation, and iron isotopes. Magnetic mineral assemblages in all samples are dominated by very low-coercivity minerals with unblocking temperatures between 350 and 580°C that are interpreted to be magnetite. Samples with lower unblocking temperatures (300-400°C), higher ARM, higher-frequency dependence, and isotopically heavy δ56Fe across a range of lithologies in the coal-bearing unit (between 1925 and 1995 mbsf) indicate the presence of fine-grained authigenic magnetite. We suggest that iron-reducing bacteria facilitated the production of fine-grained magnetite within the coal-bearing unit during burial and interaction with pore waters. The coal/peat acted as a source of electron donors during burial, mediated by humic acids, to supply iron-reducing bacteria in the surrounding siliciclastic sediments. These results indicate that coal-bearing sediments may play an important role in iron cycling in subsiding peat environments and if buried deeply through time, within the subsequent deep biosphere.

  17. Expedition Two crew arrives at KSC

    Science.gov (United States)

    2001-01-01

    Astronaut James Voss (right) stands with astronaut John Young on the tarmac at the KSC Shuttle Landing Facility. Voss is flying on mission STS-102, launching March 8, as part of the Expedition Two crew going to the International Space Station. Young made his fifth flight as Spacecraft Commander of STS-1, the first flight of the Space Shuttle, April 12-14, 1981. His sixth and final flight was as Spacecraft Commander of STS-9, the first Spacelab mission, Nov. 28-Dec. 8, 1983. The other members of the Expedition Two crew are Susan Helms and Yury Usachev. STS-102 will be Helms' and Voss's fifth Shuttle flight, and Usachev's second. They will be replacing the Expedition One crew (Bill Shepherd, Yuri Gidzenko and Sergei Krikalev), who will return to Earth March 20 on Discovery along with the STS-102 crew.

  18. Greenland Expeditions by Alfred Wegener - A photographic window to past

    Science.gov (United States)

    Leitner, M.; Tschürtz, S.; Kirchengast, G.; Kranzelbinder, H.; Prügger, B.; Krause, R. A.; Kalliokoski, M.; Thórhallsdóttir, E.

    2012-04-01

    On several expeditions to Greenland, Alfred Wegener (1880-1930) took pictures on glass plates from landscapes and glaciers, the expedition equipment, the people and animals taking part on the expeditions as well as physical phenomena as dust storm, clouds or spherical light phenomena. Chronologically the plates show the Danmark Expedition 1906-1908, the crossing of Greenland expedition with stop in Iceland 1912-1913, and the German Greenland Expedition 1929-1930. Until the tragic end of the expedition in 1930, Wegener was professor at the University of Graz, and such a stock of about 300 glass plates stayed there. The aim of our work is to digitize all plates for further studies. We present a first selection of Wegener's Greenland expedition pictures. For those made at Iceland in 1912 we will present a comparison of the past with pictures from the same viewing point made in 2011.

  19. Expedition Three Crew Onboard Photograph of Sunset

    Science.gov (United States)

    2001-01-01

    The setting sun and the thin blue airglow line at Earth's horizon was captured by the International Space Station's (ISS) Expedition Three crewmembers with a digital camera. Some of the Station's components are silhouetted in the foreground. The crew was launched aboard the Space Shuttle Orbiter Discovery STS-105 mission, on August 10, 2001, replacing the Expedition Two crew. After marning the orbiting ISS for 128 consecutive days, the three returned to Earth on December 17, 2001, aboard the STS-108 mission Space Shuttle Orbiter Endeavour.

  20. 20 CFR 404.926 - Agreement in expedited appeals process.

    Science.gov (United States)

    2010-04-01

    ... DISABILITY INSURANCE (1950- ) Determinations, Administrative Review Process, and Reopening of Determinations and Decisions Expedited Appeals Process § 404.926 Agreement in expedited appeals process. If you meet... 20 Employees' Benefits 2 2010-04-01 2010-04-01 false Agreement in expedited appeals process. 404...

  1. 7 CFR 1703.112 - Expedited telecommunications loans

    Science.gov (United States)

    2010-01-01

    ... 7 Agriculture 11 2010-01-01 2010-01-01 false Expedited telecommunications loans 1703.112 Section... § 1703.112 Expedited telecommunications loans RUS will expedite consideration and determination of an application submitted by an RUS telecommunications borrower for a loan under the Act or an advance of such...

  2. Using the Expedition Leader Style Analysis.

    Science.gov (United States)

    Phipps, Maurice L.; Phipps, Cynthia A.

    The Expedition Leader Style Analysis (ELSA) is an inventory designed to measure leadership style adaptability and effectiveness in terms of the situational leadership model. Situational leadership arose from the Experiential Leadership Education model, which is used in business and management, by replacing management jargon and phrases with…

  3. 49 CFR 385.105 - Expedited action.

    Science.gov (United States)

    2010-10-01

    ... Safety Monitoring System for Mexico-Domiciled Carriers § 385.105 Expedited action. (a) A Mexico-domiciled... driver who tests positive for controlled substances or alcohol or who refuses to submit to required controlled substances or alcohol tests. (6) Operating within the United States a motor vehicle that is not...

  4. Expedition medicine: A southern African perspective

    African Journals Online (AJOL)

    the death of a celebrity and lack of helicopter rescue during the night on. Mount Kilimanjaro illustrates a pervasive lack of understanding of the local rescue capabilities in that area. The expedition medic must be au fait with available facilities on the ground, and help potential participants to understand the risks in relation to ...

  5. Expedition: Yellowstone! A Cooperative School Outreach Project.

    Science.gov (United States)

    de Golia, Jack; And Others

    Designed to help upper elementary school teachers prepare for a class expedition to Yellowstone National Park, this workbook presents environmental learning activities that are also useful in schools too distant for an actual visit. Either way, the workbook aims to develop student appreciation of Yellowstone, the life in it, and the park's value…

  6. Strategies and Procedures for Expediting Election Petitions

    African Journals Online (AJOL)

    Mofasony

    Strategies and Procedures for Expediting Election Petitions and Appeals. 323. In order to achieve expeditious resolution of electoral disputes, various attempts have been made using the rules of court to fast track election petitions. The most significant of all is the Practice Direction issued by the then president of the. Court of ...

  7. Expedition 8 Crew Interviews: Alexander Y. Kaleri - FE

    Science.gov (United States)

    2003-01-01

    Russian cosmonaut Alexander Y. Kaleri, Flight Engineer on Expedition 8 to the International Space Station (ISS), answers interview questions on this video, either himself or with the help of an interpreter. The questions cover: 1) The goal of the expedition; 2) The place in history of Mir; 3) The reaction to the loss of Columbia in Houston; 4) Why the rewards of spaceflight are worth the risks; 5) Why he decided to become a cosmonaut; 6) His memory of Yuri Gagarin's first flight; 7) What happens on a Soyuz capsule during launch and flight; 8) Are Soyuz maneuvers automatic or manual; 8) How the ISS science mission will be advanced during his stay; 9) The responsibilities of a Flight Engineer onboard the ISS; 10) Extravehicular activity (EVA) plans at that time; 11) The Shuttle Return to Flight and his preference for a Shuttle or Soyuz landing; 12) Why the last Soyuz landing was too rough; 13) The most valueable contribution of the ISS program.

  8. The Second International Indian Ocean Expedition (IIOE-2)

    Science.gov (United States)

    Cowie, Greg; Hood, Raleigh

    2015-04-01

    The International Indian Ocean Expedition (IIOE) was one of the greatest international, interdisciplinary oceanographic research efforts of all time. Planning for the IIOE began in 1959 and the project officially continued through 1965, with forty-six research vessels participating under fourteen different flags. The IIOE motivated an unprecedented number of hydrographic surveys (and repeat surveys) over the course of the expedition covering the entire Indian Ocean basin. And it was an interdisciplinary endeavor that embraced physical oceanography, chemical oceanography, meteorology, marine biology, marine geology and geophysics. The end of 2015 will mark the 50th Anniversary of the completion of the IIOE. SCOR and the IOC are working to stimulate a new phase of coordinated international research focused on the Indian Ocean for a 5-year period beginning in late 2015 and continuing through 2020. The goal is to help to organize ongoing research and stimulate new initiatives in the 2015-2020 time frame as part of a larger expedition. Several International programs that have research ongoing or planned in the Indian Ocean during this time period and many countries are planning cruises in this time frame as well. These programs and national cruises will serve as a core for the new Indian Ocean research focus, which has been dubbed "IIOE-2." The overarching goal of the IIOE-2 is to advance our understanding of interactions between geological, oceanic and atmospheric processes that give rise to the complex physical dynamics of the Indian Ocean region, and to determine how those dynamics affect climate, extreme events, marine biogeochemical cycles, ecosystems and human populations. This understanding is required to predict the impacts of climate change, pollution, and increased fish harvesting on the Indian Ocean and its nations, as well as the influence of the Indian Ocean on other components of the Earth System. New understanding is also fundamental to policy makers for

  9. Expedition Two crew inspects airlock in SSPF

    Science.gov (United States)

    2001-01-01

    Inside the air lock in the Space Station Processing Facility, the Expedition Two crew look at equipment. Seen from left are cosmonaut Yury Usachev, a technician, and astronauts Susan Helms and James Voss. At far right is astronaut John Young, who flew on mission STS-1. Usachev, Helms and Voss will be flying on mission STS-102, launching March 8. The air lock will be carried to the Station during their tenure in space. STS-102 will be Helms' and Voss's fifth Shuttle flight, and Usachev's second. They will be replacing the Expedition One crew (Bill Shepherd, Yuri Gidzenko and Sergei Krikalev), who will return to Earth March 20 on Discovery along with the STS-102 crew.

  10. Repeated occurrences of methanogenic zones, diagenetic dolomite formation and linked silicate alteration in southern Bering Sea sediments (Bowers Ridge, IODP Exp. 323 Site U1341)

    Science.gov (United States)

    Wehrmann, L. M.; Ockert, C.; Mix, A. C.; Gussone, N.; Teichert, B. M. A.; Meister, P.

    2016-03-01

    Diagenetic precipitates, such as dolomite, and the chemistry of residual deeply buried porewater often represent the only traces of past biogeochemical activity in marine sediments. A 600 m thick sedimentary section, recently drilled at Integrated Ocean Drilling Program (IODP) Site U1341 on Bowers Ridge (southern Bering Sea), provides insight into such a 4.3 Ma old paleo-diagenetic archive. Hard-lithified calcite-dolomite layers, and laminae of disseminated carbonate, were recovered in diatom-rich sediments over a depth range of 400 m. Carbon isotope values of the diagenetic carbonates between -16.6 and -14.4‰ (VPDB) and strontium isotope ratios of dolomites close to past seawater values suggest carbonate precipitation induced by the production of dissolved inorganic carbon (DIC) during elevated rates of organic carbon mineralization, primarily via sulfate reduction, at shallow sediment depth below the paleo-seafloor. Diagenetic carbonates at 280-440 m below seafloor were likely also produced by the intermittent onset of sulfate reduction coupled to the anaerobic oxidation of methane (AOM) at sulfate-methane transition zones (SMTZ). These microbially mediated processes do not occur in the sediment at this site at present but were likely connected to the presence of a methanogenic zone at 2.58-2.51 Ma. A minimum in sulfate concentrations in modern porewaters and low sedimentary Ba/Al ratios resulting from former sulfate depletion are reminiscent of the presence of this large methanogenic zone. The minimum in sulfate concentrations is reflected in a minimum in magnesium concentrations, less radiogenic strontium and isotopically light calcium in the porewater. It is proposed that magnesium was removed from the porewater during carbonate precipitation and volcanic ash alteration which occurred in the former methanogenic zone and also released strontium with a less radiogenic isotope ratio and isotopically light calcium into the porewater. The isotopic composition of

  11. Reconstruction of recent 10Ma thermal structure seaward of updip limit of Nankai seismogenic zone off Kumano inferred from IODP NanTroSEIZE geothermal data and time-dependent numerical model

    Science.gov (United States)

    Kinoshita, Masataka; Araki, Eiichiro; Kimura, Toshinori; Kopf, Achim; Saffer, Demian; Toczko, Sean

    2017-04-01

    Understanding the slip behavior of the seismogenic faults in subduction zones requires accurate estimates on the present & past thermal structures. Some geochemical processes that affect the effective fault strength (such as clay mineral dehydration) require a knowledge on the thermal history of sediment particles since its deposition. To depict the thermal history, we need to know the tectonics and thermal regime of the Philippine Sea plate (PHS), which may have stopped subduction until 6MaBP, and restarted afterwards. Our purpose here is to test if such subduction tectonics can affect the 'present' thermal regime, which can be constrained by the heat flow measured at the seafloor or by the borehole measurements. During the IODP NanTroSEIZE expeditions, we deployed 2 borehole observatories containing 5 thermistors. In 2012, the first observatory was deployed at Site C0002 above the updip limit of locked portion of megathrust, and the temperature and heat flow at 900 m below seafloor is determined as 37.8 degC and 57 mW/m2, respectively (Sugihara et al., 2014). In 2016, we deployed the second observatory at Sites C0010 across the shallow portion of megasplay fault zone. Thermistors are located between 400 mbsf (crossing the fault zone) and 562.72 mbsf, and the temperature at 562.7 mbsf is 26.7 degC. With core thermal conductivity data, average heat flow is determined as 60 mW/m2. It is slightly higher than the heat flow at the nearby Site C0004 (54 mW/m2; Harris et al., 2011). This high heat flow may be attributed wither to pore fluid flow or transient phenomena (e.g., burial due to thrust faulting). Using these heat flow data, a thermal structure model around the updip zone of Nankai seismogenic zone is constructed for 2 end-member models; subduction of 12Ma-old Shikoku Basin (SB) started at 6MaBP, vs. subduction of 5Ma-old SB continued since 13MaBP. To account for the high heat flow seaward of trough axis, we followed the effective thermal conductivity model

  12. John Murray / MABAHISS expedition versus the International Indian Ocean Expedition (IIOE) in retrospect

    Science.gov (United States)

    Aleem, A. A.; Morcos, S. A.

    In addition to its scientific achievements, the John Murray/Mabahiss Expedition was a unique experiment in technology transfer and it pioneered bilateral relations in the field of oceanography, at a time when the Law of the Sea was not even an embryonic concept. The Expedition will be remembered for its profound influence on the development of oceanography in Egypt, and subsequently in several Arab and African countries, as well as for its socio-economic impact in Egypt. The International Indian Ocean Expedition (IIOE) was an elaborate exercise involving both the most sophisticated developments in oceanography of the day and the full complexity of international relations which necessitated the scientific, coordinating and supporting mechanisms of SCOR, IOC and Unesco combined. Each exercise separated by 25 years represented a significant event in the development of oceanography. Each was a natural product of the prevailing state of the art and the international climate. Oceanography had made a quantum jump in technology in the intervening quarter of a century, which had put the cost of deep sea oceanography quite beyond the financial capabilities of many developing countries, an important factor to bear in mind when comparing the impact of the John Murray/Mabahiss Expedition on Egypt with that of the IIOE, on the Indian Ocean countries.

  13. Biological results of the Snellius expedition. XXIV. Pelagic Tunicates of the Snellius expedition

    NARCIS (Netherlands)

    Tokioka, T.

    1974-01-01

    Eleven samples of pelagic tunicates were found in the material collected during the Snellius Expedition 1929-30. In these, seven species, viz., two pyrosomas and five salpas, are included. In addition, a few old specimens of another species of Pyrosoma were found in the collection of the Leiden

  14. 8 CFR 235.3 - Inadmissible aliens and expedited removal.

    Science.gov (United States)

    2010-01-01

    ... 8 Aliens and Nationality 1 2010-01-01 2010-01-01 false Inadmissible aliens and expedited removal. 235.3 Section 235.3 Aliens and Nationality DEPARTMENT OF HOMELAND SECURITY IMMIGRATION REGULATIONS INSPECTION OF PERSONS APPLYING FOR ADMISSION § 235.3 Inadmissible aliens and expedited removal. (a) Detention...

  15. 12 CFR 229.55 - Expedited recredit for banks.

    Science.gov (United States)

    2010-01-01

    ... 12 Banks and Banking 3 2010-01-01 2010-01-01 false Expedited recredit for banks. 229.55 Section 229.55 Banks and Banking FEDERAL RESERVE SYSTEM (CONTINUED) BOARD OF GOVERNORS OF THE FEDERAL RESERVE... Expedited recredit for banks. (a) Circumstances giving rise to a claim. A bank that has an indemnity claim...

  16. Insights on the Formation and Evolution of the Upper Oceanic Crust from Deep Drilling at ODP/IODP Hole 1256D

    Science.gov (United States)

    Teagle, D. A. H.

    2009-04-01

    Deep drilling of Hole 1256D on ODP Leg 206 and IODP Expeditions 309/312 provides the first complete section of intact upper oceanic crust down to gabbros. Site 1256 is located on ocean crust of the Cocos Plate that formed at the East Pacific Rise (EPR) 15 million years ago during an episode of superfast rate ocean spreading in excess of 200 mm/yr. Past deep drilling of intact ocean crust has been fraught with difficulties due to the highly fractured nature of oceanic lavas. Site 1256 was specifically chosen because the observed relationship between spreading rate and the depth to axial seismic low velocity zones at modern mid-ocean ridges (thought to be magma chambers), suggests that gabbroic rocks should occur at the shallowest levels in ocean crust formed at the highest spreading rates. In line with pre-drilling predictions, gabbroic rocks were first encountered 1157 m into the basement. Hole 1256D penetrates 754 m of lavas, a 57-m thick transition zone and a thin (346 m) sheeted dike complex. The lower ~60 m of the sheeted dikes are contact metamorphosed to granoblastic textures. After encountering gabbros the hole was deepened a further 100 m before the cessation of drilling operations and the plutonic section comprises two gabbroic sills, 52 and 24 m-thick, intruded into a 24 m screen of granoblastic dikes. The gabbro sills have chilled margins and compositions similar to the overlying lavas and dikes, precluding formation of the cumulate lower oceanic crust from the melt lenses so far penetrated by Hole 1256D. A vertical seismic experiment conducted in Hole 1256D indicates that the bottom of the Hole is still within seismic layer 2 despite gabbroic rocks having been recovered. These data together with 1-D and imaging wire-line logs, have been used to construct a continuous volcano-stratigraphy for Site 1256. Comparison of this data with the recovered cores and the styles of eruption occurring at the modern EPR indicate that ~50% of lava sequences were formed

  17. Social interaction and pain: An arctic expedition.

    Science.gov (United States)

    Block, Per; Heathcote, Lauren C; Burnett Heyes, Stephanie

    2017-11-08

    Complex human behaviour can only be understood within its social environment. However, disentangling the causal links between individual outcomes and social network position is empirically challenging. We present a research design in a closed real-world setting with high-resolution temporal data to understand this interplay within a fundamental human experience - physical pain. Study participants completed an isolated 3-week hiking expedition in the Arctic Circle during which they were subject to the same variation in environmental conditions and only interacted amongst themselves. Adolescents provided daily ratings of pain and social interaction partners. Using longitudinal network models, we analyze the interplay between social network position and the experience of pain. Specifically, we test whether experiencing pain is linked to decreasing popularity (increasing isolation), whether adolescents prefer to interact with others experiencing similar pain (homophily), and whether participants are increasingly likely to report similar pain as their interaction partners (contagion). We find that reporting pain is associated with decreasing popularity - interestingly, this effect holds for males only. Further exploratory analyses suggest this is at least partly driven by males withdrawing from contact with females when in pain, enhancing our understanding of pain and masculinity. Contrary to recent experimental and clinical studies, we found no evidence of pain homophily or contagion in the expedition group. Copyright © 2017 The Author(s). Published by Elsevier Ltd.. All rights reserved.

  18. Arctic Collaboration: Developing a Successful Researcher/Teacher Expedition

    Science.gov (United States)

    Skotnicki, S.; Loranty, M. M.

    2016-12-01

    Are you a researcher working in the polar regions of the world or a K-12 science teacher who would like to be part of a field research expedition in the polar regions? Researchers and K-12 science teachers can apply for funding from PolarTREC, a program that pairs researchers and teachers to conduct field science in Antarctica and the Arctic. Our poster presentation will offer details of one such successful researcher/teacher partnership. During the summer of 2016, Science Teacher Stan Skotnicki (Cheektowaga Central Middle School in Buffalo, NY) was teamed up with Assistant Professor Mike Loranty (Colgate University) to study vegetation and ecosystem impacts on permafrost vulnerability. Stan joined Mike and his research team in Northeastern Siberia preparing field sites, collecting data, processing samples, discussing methods, and planning daily activities. In order to raise awareness and broaden the impact of the research being conducted, Stan communicated the science through a series of journals on the PolarTREC website with his students, staff, and members of the community. Additionally, Mike and Stan held a live webinar from Siberia discussing the content of the research, the nature of the fieldwork, and why it was important to travel so far for this information. This expedition allowed Stan to experience working with a field research team for an extended period of time. Mike benefited from having a team member dedicated to learning about and communicating project details that also provided valuable field assistance. Stan gets to bring his hands-on experience back to his classroom in Buffalo and Mike has the opportunity to share his research with a new and different audience, including presenting to students at Cheektowaga Central with the help of his undergraduate students. This model of collaboration provides a number of valuable benefits for both teachers and researchers. While the PolarTREC program provides necessary logistics and funding to conduct these

  19. Mathematics in narratives of Geodetic expeditions.

    Science.gov (United States)

    Terrall, Mary

    2006-12-01

    In eighteenth-century France, geodesy (the measure of the earth's shape) became an arena where mathematics and narrative intersected productively. Mathematics played a crucial role not only in the measurements and analysis necessary to geodesy but also in the narrative accounts that presented the results of elaborate and expensive expeditions to the reading public. When they returned to France to write these accounts after their travels, mathematician-observers developed a variety of ways to display numbers and mathematical arguments and techniques. The numbers, equations, and diagrams they produced could not be separated from the story of their acquisition. Reading these accounts for the interplay of these two aspects--the mathematical and the narrative--shows how travelers articulated the intellectual and physical difficulties of their work to enhance the value of their results for specialist and lay readers alike.

  20. Spectroscopic studies of terrestrial impact materials: Preparation for Popigai expedition

    Science.gov (United States)

    Evdokimova, N. A.; Rodin, A. V.; Masaitis, V. L.; Timofeev, I. S.; Roste, O. Z.; Korablev, O. I.; Dolnikov, G. G.

    2011-10-01

    Terrestrial craters give us an excellent opportunity of direct analisys as opposed to craters out of the E arth. However, on the Earth there are only few sites where traces of strong impacts event could be studied in the fi eld. The traces of ancient impacts are better preserved in the frozen subsoil at subpolar latitudes. One of such sites is Popigai crater, located in subpolar Siberia, Russia, presumably caused by a giant impactor 35 Ma ago. This astrobleme gives a good chance to observe in situ the asteroid crater, impact materials and other consequenses of great energy deposition. T he crater was thoroughly studied during last few decades due to impact diamond inventories associated with it [1]. However a number of problems remain unresolved and wait for further studies: the physics and chemistry of impactites and impact breccias; mineral components with metamorphic rocks affected by great shock and impactites; material ejecta; structural forms invoked by crater formation; problems of remote sensing studies and problems related to comparative planetology. In the framework o f Europlanet program, we plan the expedition to Popigai site scheduled to 2012.

  1. The Twelfth Indian Scientific Expedition to Antarctica: Events and achievements

    Digital Repository Service at National Institute of Oceanography (India)

    Dhargalkar, V.K.

    The twelfth Indian Scientific Expedition to Antarctica comprising 56 members coming from different scientific organisations/institutions and the logistic contingent from three wings of defense services was flagged off by Shri Ravi Naik, Honourable...

  2. Biological results of the Snellius expedition : XXIX. Echinodermata, Asteroidea

    NARCIS (Netherlands)

    Jangoux, M.

    1978-01-01

    Twenty-eight species of starfish were collected during the Snellius Expedition (19291930). The collection contains seven rare or uncommon species, i.e., Astropecten novaeguineae, A. sumbawanus, Celerina heffernani, Fromia eusticha, Disasterina abnormalis, Nepanthia briareus and Echinaster

  3. Field Science Ethnography: Methods For Systematic Observation on an Expedition

    Science.gov (United States)

    Clancey, William J.; Clancy, Daniel (Technical Monitor)

    2001-01-01

    The Haughton-Mars expedition is a multidisciplinary project, exploring an impact crater in an extreme environment to determine how people might live and work on Mars. The expedition seeks to understand and field test Mars facilities, crew roles, operations, and computer tools. I combine an ethnographic approach to establish a baseline understanding of how scientists prefer to live and work when relatively unemcumbered, with a participatory design approach of experimenting with procedures and tools in the context of use. This paper focuses on field methods for systematically recording and analyzing the expedition's activities. Systematic photography and time-lapse video are combined with concept mapping to organize and present information. This hybrid approach is generally applicable to the study of modern field expeditions having a dozen or more multidisciplinary participants, spread over a large terrain during multiple field seasons.

  4. Problems in the Optimization of Manned Interplanetary Expeditions

    Science.gov (United States)

    Kiforenko, B. N.; Vasil'Ev, I. Yu.

    Within the scope of the unified variation problem the authors discuss the optimization of parameters, choosing flight trajectories and optimal flight control as well as control of life support systems in spacecraft in manned interplanetary expeditions. They examine the efficiency of ejecting the life support systems waste by jets from high-thrust rocket engines as compared to partial waste regeneration. They confirm the possibility of manned expeditions to Mars before efficient life support systems based on biological regeneration are developed.

  5. Temporal changes in Quaternary paleoenvironment and ostracode fauna in the eastern Indian Sea off Western Australia (IODP, Exp. 356, site U1461)

    Science.gov (United States)

    Iwatani, H.; Yasuhara, M.; Angue Minto'O, C. M.; Bassetti, M. A.; Expedition 356 Scientists, I.

    2016-12-01

    The International Ocean Discovery Program Expedition 356 drilled on seven sites off Western Australia to reveal the history of the Indonesian throughflow, the effects of the Australian monsoon, and the subsidence of the northwest shelf of Australia. To achieve these objectives, we investigated paleoenvironmental evolutions in this region during the Quaternary period using high-resolution statistical analyses of the fossil Ostracoda (Crustacea) as an effective environmental indicator. For the investigation, we used a sediment core obtained from an area off Western Australia in the eastern Indian Sea (site: U1461; water depth: 128 m; latitude: 20°, 12.85' S; longitude: 115°, 03.94' E). The upper part of the core mainly comprises alternating beds of darker-colored packstone/wackestone and light-colored wackestone/mudstone. The light-colored wackestone/mudstone beds often contain fecal pellets and well-preserved molluscan fossils. We investigated fossil ostracode faunal composition and species diversity changes during the deposition of the study site. Many well-preserved ostracodes were recorded in the studied cores. Many of collected species are extant taxa that inhabit the upper sublittoral regions as reported from around the recent Indian Ocean off northwestern Australia. Ostracode assemblages, abundance, and diversity drastically changed during the deposition, and they are concordant with sedimentary facies. Here we will discuss the relationships between these paleo-communities changes and paleoenvironmental conditions.

  6. Recognizing magnetostratigraphy in overprinted and altered marine sediments: Challenges and solutions from IODP Site U1437

    Science.gov (United States)

    Musgrave, Robert J.; Kars, Myriam

    2016-08-01

    Core disturbance, drilling overprints, postdepositional acquisition of remanence, authigenic growth of magnetic iron sulfides, and alteration all contribute challenges to recognizing the primary magnetostratigraphy in marine sediments. We address these issues in a sequence of tuffaceous muds and volcaniclastics at International Ocean Discovery Program Site U1437 and produce the longest continuous magnetic polarity stratigraphy in the history of scientific ocean drilling. Remanence measurements were filtered to remove intervals affected by fluidization, plastic sediment disturbance, and core biscuiting. Drilling overprints are concentrated in the disturbed annulus surrounding intact core material. Bioturbation was limited to a vertical extent of at most 15 cm. Changes in sediment color, stiffness, and magnetic hysteresis all suggest that remanence was locked in within a few meters of the sediment-water interface. We did not observe any systematic offset between magnetostratigraphic and biostratigraphic datums. Authigenic growth of greigite, in response to both initial sulfate reduction in the upper 50 m of the sediment column and to deeper resupply of sulfate, has led to magnetic overprinting. Anomalous polarity artefacts, extending acquired by greigite produced during early diagenesis. Diagenetic magnetic mineral alteration resulted in the progressive loss of fine-grained magnetite, which enhanced susceptibility to drilling and postdrilling overprints and increased the resistance of these overprints to removal by conventional demagnetization. We recovered the magnetostratigraphic record from many samples with resistant overprints through low-temperature demagnetization through the Verwey transition.

  7. The German-Tanzanian Tendaguru Expedition 2000

    Directory of Open Access Journals (Sweden)

    W.-D. Heinrich

    2001-01-01

    Full Text Available The celebrated fossil locality of Tendaguru (Tanzania, East Africa has been well known for its unique Late Jurassic dinosaur assemblages since the early decades of the 20th century. Recently, within the scope of the German-Tanzanian Tendaguru project, an expedition returned to Tendaguru with the aim of collecting microvertebrates, micro- and macroinvertebrates, plant fossils and new sedimentological and stratigraphical data. Applying a multidisciplinary research approach, the data collected were used to address various controversial issues regarding the Tendaguru Beds. These include their exact age, depositional environments and reconstructions of the palaeoecosystems in which the dinosaurs lived. Field work resulted in a new standard section for the Tendaguru Beds. Preliminary biostratigraphic results, based on ammonites, charophytes and palynomorphs, support a Late Kimmeridgian age for the Nerinea Bed, an early Tithonian age for the Trigonia smeei Bed, and an Early Cretaceous (possibly Valanginian to Hauterivian age for the Trigonia schwarzi Bed. Facies analysis of the Tendaguru Beds indicates environments ranging from storm- and tide-influenced, siliciclastic coastal barrier systems, ooid sand bar complexes and backbarrier tidal flats to sabkha-like coastal plains with brackish lakes and pools. Sedimentological indicators of palaeoclimate and palynological data point to a subtropical to tropical climate with pronounced dry seasons. In concert with sedimentological data, quantitative palaeoecological analysis of macroinvertebrates helped to finetune understanding of environmental factors such as substrate conditions, salinity, sedimentation rate and water depth. Along with abundant microvertebrate remains and fragments of fusain and cuticles, these new data have considerably improved our knowledge of the fauna and flora found in the Tendaguru Beds, and provide a solid basis for developing a better understanding of the Late Jurassic and Early

  8. Sodium dichromate expedited response action assessment

    Energy Technology Data Exchange (ETDEWEB)

    1993-09-01

    The US Environmental Protection Agency (EPA) and Washington Department of Ecology (Ecology) recommended that the US Department of Energy (DOE) perform an expedited response action (ERA) for the Sodium Dichromate Barrel Disposal Landfill. The ERA lead regulatory agency is Ecology and EPA is the support agency. The ERA was categorized as non-time-critical, which required preparation of an engineering evaluation and cost analysis (EE/CA). The EE/CA was included in the ERA proposal. The EE/CA is a rapid, focused evaluation of available technologies using specific screening factors to assess feasibility, appropriateness, and cost. The ERA goal is to reduce the potential for any contaminant migration from the landfill to the soil column, groundwater, and Columbia River. Since the Sodium Dichromate Barrel Disposal Landfill is the only waste site within the operable unit, the removal action may be the final remediation of the 100-IU-4 Operable Unit. This ERA process started in March 1992. The ERA proposal went through a parallel review process with Westinghouse Hanford Company (WHC), DOE Richland Operations (RL), EPA, Ecology, and a 30-day public comment period. Ecology and EPA issued an Action Agreement Memorandum in March 1993 (Appendix A). The memorandum directed excavation of all anomalies and disposal of the collected materials at the Hanford Site Central Landfill. Primary field activities were completed by the end of April 1993. Final waste disposal of a minor quantity of hazardous waste was completed in July 1993.

  9. N Springs expedited response action proposal

    Energy Technology Data Exchange (ETDEWEB)

    1994-01-01

    Since signing the Hanford Federal Facility Agreement and Consent Order (Tri-Party Agreement) in 1989, the parties to the agreement have recognized the need to modify the approach to conducting investigations, studies, and cleanup actions at Hanford. To implement this approach, the parties have jointly developed the Hanford Past-Practice Strategy. The strategy defines a non-time-critical expedited response action (ERA) as a response action ``needed to abate a threat to human health or welfare or the environment where sufficient time exists for formal planning prior to initiation of response. In accordance with the past-practice strategy, DOE proposes to conduct an ERA at the N Springs, located in the Hanford 100 N Area, to substantially reduce the strontium-90 transport into the river through the groundwater pathway. The purpose of this ERA proposal is to provide sufficient information to select a preferred alternative at N Springs. The nature of an ERA requires that alternatives developed for the ERA be field ready; therefore, all the technologies proposed for the ERA should be capable of addressing the circumstances at N Springs. A comparison of these alternatives is made based on protectiveness, cost, technical feasibility, and institutional considerations to arrive at a preferred alternative. Following the selection of an alternative, a design phase will be conducted; the design phase will include a detailed look at design parameters, performance specifications, and costs of the selected alternative. Testing will be conducted as required to generate design data.

  10. Rescuing biogeographic legacy data: The "Thor" Expedition, a historical oceanographic expedition to the Mediterranean Sea.

    Science.gov (United States)

    Mavraki, Dimitra; Fanini, Lucia; Tsompanou, Marilena; Gerovasileiou, Vasilis; Nikolopoulou, Stamatina; Chatzinikolaou, Eva; Plaitis, Wanda; Faulwetter, Sarah

    2016-01-01

    This article describes the digitization of a series of historical datasets based οn the reports of the 1908-1910 Danish Oceanographical Expeditions to the Mediterranean and adjacent seas. All station and sampling metadata as well as biodiversity data regarding calcareous rhodophytes, pelagic polychaetes, and fish (families Engraulidae and Clupeidae) obtained during these expeditions were digitized within the activities of the LifeWatchGreece Research Ιnfrastructure project and presented in the present paper. The aim was to safeguard public data availability by using an open access infrastructure, and to prevent potential loss of valuable historical data on the Mediterranean marine biodiversity. The datasets digitized here cover 2,043 samples taken at 567 stations during a time period from 1904 to 1930 in the Mediterranean and adjacent seas. The samples resulted in 1,588 occurrence records of pelagic polychaetes, fish (Clupeiformes) and calcareous algae (Rhodophyta). In addition, basic environmental data (e.g. sea surface temperature, salinity) as well as meterological conditions are included for most sampling events. In addition to the description of the digitized datasets, a detailed description of the problems encountered during the digitization of this historical dataset and a discussion on the value of such data are provided.

  11. Increasing Shore-based Participation of Scientists & Students in Telepresence-enabled Nautilus Expeditions

    Science.gov (United States)

    Bell, K. L. C.; Raineault, N.; Carey, S.; Eberli, G. P.; John, B. E.; Cheadle, M. J.; German, C. R.; Mirmalek, Z.; Pallant, A.

    2016-02-01

    As the US oceanographic research fleet shrinks, reducing seagoing opportunities for scientists and students, remote participation in cruises via telepresence will become increasingly vital. The Nautilus Exploration Program is improving the experience of shoreside participants through the development of new tools and methodologies for connecting them to expeditions in real time increasing accessibility to oceanographic cruises. The Scientist Ashore Program is a network of scientists around the world who participate in Exploration Vessel Nautilus expeditions from their own labs or homes. We have developed a suite of collaboration tools to allow scientists to view video and data in real time, as well as to communicate with ship-based and other shore-based participants to enable remote participation in cruises. Post-cruise, scientists and students may access digital data and biological and geological samples from our partner shore-based repositories: the University of Rhode Island Inner Space Center, Harvard Museum of Comparative Zoology, and URI Marine Geological Samples Lab. We present examples of successful shore-based participation by scientists and students in Nautilus expeditions. In 2013, Drs. Cheadle and John stood watch 24/7 with ten undergraduate and graduate students at the University of Wyoming, recording geologic features and samples, during a cruise to the Cayman Rise. The Straits of Florida & Great Bahama Bank cruise was co-led by Dr. Eberli at the University of Miami in 2014, greatly complementing existing data. That same year, the ISC hosted four early career scientists and their twelve undergraduate students who led dives from shore in collaboration with Dr. Carey, Lead Scientist at sea on the Kick'em Jenny Volcano & the Barbados Mud Volcanoes cruise. In 2015, 12 Scientists Ashore worked in collaboration with the ship-based team on the exploration of Galapagos National Park, and more than 20 are working with OET on post-cruise data & sample analysis.

  12. University of Maine's Follow a Researcher Program™, Expedition 3: Antarctica, Using Graduate Student Fieldwork Experiences as a framework to Incorporate Next Generation Science Standard Practices in the Classroom

    Science.gov (United States)

    Kaluzienski, L. M.; Kranich, G.; Wilson, L.; Hamley, C.

    2016-12-01

    For the past three years the University of Maine Cooperative Extension 4-H has connected K-12 students in Maine and around the country to UMaine researchers in the field as part of its Follow a Researcher (FAR) Program™. This program aims to provide middle and high school students with a look into future science career paths. FAR™ selects one student engaged in university level research per year to showcase their work. Previous years have selected graduate students with field-work intensive research. During the graduate student's field expedition, a weekly education science video is released based on the Next Generation Science Standards. Similarly, classroom students are encouraged to ask questions during weekly Twitter session hosted live from the field. Past expeditions have taken students to the Quelccaya Ice Cap in Peru as well as the Falkland Islands. This year's expedition shared graduate student Lynn Kaluzienski's expedition to the Ross Ice Shelf in Antarctica. Highlights include obtaining GPS observations in a remote setting using helicopter support, as well acquiring scientific measurements from a heavily crevassed area through the use of robotically towed ground penetrating radar (GPR). Future program plans include connecting K-12 students with graduate students with a focus in lab-intensive research as well as engineering. We also are developing a training program for university outreach staff and a Follow a Researcher™ network that would allow other universities to host their own program while tapping into a larger national K-12 audience.

  13. Joint Antarctic School Expedition - An International Collaboration for High School Students and Teachers on Antarctic Science

    Science.gov (United States)

    Botella, J.; Warburton, J.; Bartholow, S.; Reed, L. F.

    2014-12-01

    The Joint Antarctic School Expedition (JASE) is an international collaboration program between high school students and teachers from the United States and Chile aimed at providing the skills required for establishing the scientific international collaborations that our globalized world demands, and to develop a new approach for science education. The National Antarctic Programs of Chile and the United States worked together on a pilot program that brought high school students and teachers from both countries to Punta Arenas, Chile, in February 2014. The goals of this project included strengthening the partnership between the two countries, and building relationships between future generations of scientists, while developing the students' awareness of global scientific issues and expanding their knowledge and interest in Antarctica and polar science. A big component of the project involved the sharing by students of the acquired knowledge and experiences with the general public. JASE is based on the successful Chilean Antarctic Science Fair developed by Chile´s Antarctic Research Institute. For 10 years, small groups of Chilean students, each mentored by a teacher, perform experimental or bibliographical Antarctic research. Winning teams are awarded an expedition to the Chilean research station on King George Island. In 2014, the Chileans invited US participation in this program in order to strengthen science ties for upcoming generations. On King George Island, students have hands-on experiences conducting experiments and learning about field research. While the total number of students directly involved in the program is relatively small, the sharing of the experience by students with the general public is a novel approach to science education. Research experiences for students, like JASE, are important as they influence new direction for students in science learning, science interest, and help increase science knowledge. We will share experiences with the

  14. Land - Ocean Climate Linkages and the Human Evolution - New ICDP and IODP Drilling Initiatives in the East African Rift Valley and SW Indian Ocean

    Science.gov (United States)

    Zahn, R.; Feibel, C.; Co-Pis, Icdp/Iodp

    2009-04-01

    The past 5 Ma were marked by systematic shifts towards colder climates and concomitant reorganizations in ocean circulation and marine heat transports. Some of the changes involved plate-tectonic shifts such as the closure of the Panamanian Isthmus and restructuring of the Indonesian archipelago that affected inter-ocean communications and altered the world ocean circulation. These changes induced ocean-atmosphere feedbacks with consequences for climates globally and locally. Two new ICDP and IODP drilling initiatives target these developments from the perspectives of marine and terrestrial palaeoclimatology and the human evolution. The ICDP drilling initiative HSPDP ("Hominid Sites and Paleolakes Drilling Project"; ICDP ref. no. 10/07) targets lacustrine depocentres in Ethiopia (Hadar) and Kenya (West Turkana, Olorgesailie, Magadi) to retrieve sedimentary sequences close to the places and times where various species of hominins lived over currently available outcrop records. The records will provide a spatially resolved record of the East African environmental history in conjunction with climate variability at orbital (Milankovitch) and sub-orbital (ENSO decadal) time scales. HSPDP specifically aims at (1) compiling master chronologies for outcrops around each of the depocentres; (2) assessing which aspects of the paleoenvironmental records are a function of local origin (hydrology, hydrogeology) and which are linked with regional or larger-scale signals; (3) correlating broad-scale patterns of hominin phylogeny with the global beat of climate variability and (4) correlating regional shifts in the hominin fossil and archaeological record with more local patterns of paleoenvironmental change. Ultimately the aim is to test hypotheses that link physical and cultural adaptations in the course of the hominin evolution to local environmental change and variability. The IODP initiative SAFARI ("Southern African Climates, Agulhas Warm Water Transports and Retroflection

  15. Outreach Aboard the JOIDES Resolution During IODP Exp. 360: Bringing Cutting Edge Research on Mid Ocean Ridge Processes to Classrooms Worldwide

    Science.gov (United States)

    Kavanagh, L.; Martinez, A. O.; Burgio, M.; Zhang, J.; Expedition 360 Scientists, I.

    2016-12-01

    In order to increase classroom engagement for the next generation of scientists, teachers must include current research in their curriculum. The JOIDES Resolution offers this opportunity to teachers worldwide. We recently served as four Education and Outreach Officers during Exp. 360: Southwest Indian Ridge Lower Crust and Moho. Our aim was to communicate the goals of the expedition to students and the general public through webcasts, social media, videos, and interviews. Prior to the expedition, I visited a number of schools in Texas and shared my upcoming experience with 800 teachers and students. Webcasts hosted during the expedition were tailored to the teacher's specifications of subject area and grade level. Students and teachers were able to witness cutting edge science during a tour of the ship and ask questions of those directly involved in the research. Lessons, resources, and videos featuring the scientific activities taking place and highlighting the workings of a research vessel were developed and will be featured at science teacher conferences at the state and national level. Upon my return home I visited schools that participated in webcasts and provided samples of peripheral rock material for instructional purposes. This expedition has also led to post cruise collaboration with some of the Expedition 360 scientists. My students will have the opportunity to do research with the microbiologists along the Rio Grande River and at Texas A&M University. Expedition 360 has opened up a multitude of opportunities for my students and those around the world that participated in the live webcasts. I was able to reach out to the same students multiple times during this experience which made it possible for them to connect with the science before, during, and after the expedition. These types of opportunities will inspire the next generation of scientists who will make advances towards new understandings of Earth's processes.

  16. Lessons from Previous Expeditions for the Human Exploration of Mars

    Science.gov (United States)

    Stuster, J.

    Anecdotal comparisons frequently are made between expeditions of the past and future space missions. From an engineering perspective, the differences between future and past expeditions are considerable. Spacecraft are far more complex than sailing ships, and one of the factors that drives the complexity is the requirement to support the crew in the hostile environment of space. The technological differences are significant, but from a behavioral perspective, are the differences really that great between confinement in a small wooden ship locked in the polar ice cap and confinement in a small high-technology ship hurtling through interplanetary space? The psychological differences probably are few. This paper discusses some of the most salient behavioral and technical lessons from previous expeditions that can be applied to facilitate the human explora- tion of Mars.

  17. Ship Sensor Observations for Expedition to the Deep Slope 2007 - Office of Ocean Exploration

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Hourly measurements made by selected ship sensors on the NOAA Ship Ronald H. Brown during the "Expedition to the Deep Slope 2007" expedition sponsored by the...

  18. Dive Activities for Expedition to the Deep Slope 2006 - Office of Ocean Exploration

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Information about dive activities were recorded by personnel during the "Expedition to the Deep Slope 2006" expedition, May 7 through June 2, 2006. Additional...

  19. Dive Activities for Expedition to the Deep Slope 2007 - Office of Ocean Exploration

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Information about dive activities were recorded by personnel during the "Expedition to the Deep Slope 2007" expedition, June 4 through July 6, 2007. Additional...

  20. 77 FR 12724 - International Postal Service-Global Expedited Package Services (GEPS) Contracts

    Science.gov (United States)

    2012-03-02

    ... Part 20 International Postal Service--Global Expedited Package Services (GEPS) Contracts AGENCY: Postal... change for the international competitive product Global Expedited Package Services (GEPS) Contracts. The... States Postal Service, International Mail Manual (IMM ) to incorporate a change concerning the...

  1. Outcome of Expedited Rotator Cuff Surgery in Injured Workers: Determinants of Successful Recovery

    Science.gov (United States)

    Razmjou, Helen; Boljanovic, Dragana; Lincoln, Sandra; Holtby, Richard; Gallay, Stephen; Henry, Patrick; Macritchie, Iona; Borthwick, Cheryl; Mayer, Lauren; Roknic, Carolyn; Shore, Deborah; Kamino, Allison; Grossman, Julie; Hill, Joanne; Singh, Gargi; Travers, Niki; Yanofsky, Loraine; Wilson, Marni; Sumar, Shellina; Savona, Alicia; De Medeiros, Filomena; Mann, Helen; Champsi, Aisha; Chau, Stefanie; Medeiros, Danielle; Richards, Robin R.

    2017-01-01

    Background: Work-related rotator cuff injuries are a common cause of disability and employee time loss. Purpose: To examine the effectiveness of expedited rotator cuff surgery in injured workers who underwent rotator cuff decompression or repair and to explore the impact of demographic, clinical, and psychosocial factors in predicting the outcome of surgery. Study Design: Case series; Level of evidence, 4. Methods: Injured workers who were seen at a shoulder specialty program and who underwent expedited arthroscopic rotator cuff decompression or repair were observed for a period of 6 to 12 months based on their type of surgery and recovery trajectory. The primary outcome measure was the American Shoulder and Elbow Surgeons (ASES) Standardized Shoulder Assessment Form. The impact of surgery was assessed by whether the change in the ASES score exceeded the minimal clinically important difference (MCID) of 17 points. Secondary outcomes were range of motion (ROM), medication consumption, and work status. Results: One hundred forty-six patients (43 women [29%], 103 men [71%]; mean age, 52 years; SD, 8 years) completed the study. Sixty-seven (46%) patients underwent rotator cuff repair. The mean time between the date the patient consented to have surgery and the date of surgery was 82 (SD, 44) days. There was a statistically significant improvement in ASES score and ROM and work status (52 returned to regular duties and 59 to modified duties) (P MCID of 17 points. Individual factors that affected patient overall disability were preoperative ASES, work status prior to surgery, access to care, and autonomy at work. Achieving a minimal clinically meaningful change was influenced by perceived access to care, autonomy and stress at work, and overall satisfaction with the job. Conclusion: Expedited rotator cuff surgery improved disability, ROM, and work status in injured workers. Successful recovery after work-related shoulder injuries may further be facilitated by improving

  2. Outcome of Expedited Rotator Cuff Surgery in Injured Workers: Determinants of Successful Recovery.

    Science.gov (United States)

    Razmjou, Helen; Boljanovic, Dragana; Lincoln, Sandra; Holtby, Richard; Gallay, Stephen; Henry, Patrick; Macritchie, Iona; Borthwick, Cheryl; Mayer, Lauren; Roknic, Carolyn; Shore, Deborah; Kamino, Allison; Grossman, Julie; Hill, Joanne; Singh, Gargi; Travers, Niki; Yanofsky, Loraine; Wilson, Marni; Sumar, Shellina; Savona, Alicia; De Medeiros, Filomena; Mann, Helen; Champsi, Aisha; Chau, Stefanie; Medeiros, Danielle; Richards, Robin R

    2017-05-01

    Work-related rotator cuff injuries are a common cause of disability and employee time loss. To examine the effectiveness of expedited rotator cuff surgery in injured workers who underwent rotator cuff decompression or repair and to explore the impact of demographic, clinical, and psychosocial factors in predicting the outcome of surgery. Case series; Level of evidence, 4. Injured workers who were seen at a shoulder specialty program and who underwent expedited arthroscopic rotator cuff decompression or repair were observed for a period of 6 to 12 months based on their type of surgery and recovery trajectory. The primary outcome measure was the American Shoulder and Elbow Surgeons (ASES) Standardized Shoulder Assessment Form. The impact of surgery was assessed by whether the change in the ASES score exceeded the minimal clinically important difference (MCID) of 17 points. Secondary outcomes were range of motion (ROM), medication consumption, and work status. One hundred forty-six patients (43 women [29%], 103 men [71%]; mean age, 52 years; SD, 8 years) completed the study. Sixty-seven (46%) patients underwent rotator cuff repair. The mean time between the date the patient consented to have surgery and the date of surgery was 82 (SD, 44) days. There was a statistically significant improvement in ASES score and ROM and work status (52 returned to regular duties and 59 to modified duties) ( P work status prior to surgery, access to care, and autonomy at work. Achieving a minimal clinically meaningful change was influenced by perceived access to care, autonomy and stress at work, and overall satisfaction with the job. Expedited rotator cuff surgery improved disability, ROM, and work status in injured workers. Successful recovery after work-related shoulder injuries may further be facilitated by improving the psychosocial work environment and increasing access to care.

  3. 12 CFR 1202.10 - Will FHFA expedite my request or appeal?

    Science.gov (United States)

    2010-01-01

    ... 12 Banks and Banking 7 2010-01-01 2010-01-01 false Will FHFA expedite my request or appeal? 1202... FREEDOM OF INFORMATION ACT § 1202.10 Will FHFA expedite my request or appeal? (a) Applications for... application must be in writing. FHFA will grant expedited processing, and give the request or appeal priority...

  4. 20 CFR 404.925 - How to request expedited appeals process.

    Science.gov (United States)

    2010-04-01

    ... DISABILITY INSURANCE (1950- ) Determinations, Administrative Review Process, and Reopening of Determinations and Decisions Expedited Appeals Process § 404.925 How to request expedited appeals process. (a) Time... 20 Employees' Benefits 2 2010-04-01 2010-04-01 false How to request expedited appeals process. 404...

  5. Technical procedures for aeromagnetic surveys in Antarctica during the Italian expeditions (1988-1992

    Directory of Open Access Journals (Sweden)

    D. Damaske

    1994-06-01

    Full Text Available For most of Antarctica, the geophysical data now available are those of aeromagnetic surveys performed there from 1950 to 1960. Until 1984, the inaccurate positioning and insufficient monitoring of geomagnetic time variations allowed the investigation of the geomagnetic residual field only along profiles. The Ganovex IV aeromagnetic survey, performed by BGR-USGS over the Ross Sea and the Northern Victoria Land, and the geophysical investigations of BAS on the Southern Antarctic peninsula and the Ronne ice shelf region corresponds to the recent advancement of these techniques in Antarctica. The first experiments of aeromagnetic measurements, during the Italian expeditions in Antarctica were made during the 1988-1989 field season. Some geomagnetic helicopter borne profiles were accomplished with a Proton Precession Magnetometer (PPM in the Terra Nova Bay-Gerlache Inlet area. In the 1989-1990 ItaliAntartide expedition some profiles were flown over the suture between the Wilson and Bower terranes, in Northern Victoria Land. During the 1991-1992 expedition, in cooperation with researchers of BGR (Bundesanstalt fur Geowissenschaften und Rohstoffe of Hannover, the GITARA I (German ITalian Aeromagnetic Rescarch Antarctica program, as part of the LIRA (Litospheric Investigation in the Ross Sea Area project, was carried out. The investigated area lies between the latitudes 74°18' S and 75°18' S and the longitudes 160°30' E and 164°30'E and it corresponds to a portion of the North Victoria Land, located between the Eisenhower Range and the, DrygaIski Ice Tongue. The survey was made with a Cesium vapour magnetometer. The positioning system was of the “Range-Range” type, it consisted of three transmitters (beacons, installed inside the investigated area and located with GPS measurements. The line spacing was 4.4 km, with tie lines every 22 km. The survey covered an area of 6500 km2 . Four PPM base stations for the determination of the time variation

  6. 8 CFR 1235.3 - Inadmissible aliens and expedited removal.

    Science.gov (United States)

    2010-01-01

    ... 8 Aliens and Nationality 1 2010-01-01 2010-01-01 false Inadmissible aliens and expedited removal. 1235.3 Section 1235.3 Aliens and Nationality EXECUTIVE OFFICE FOR IMMIGRATION REVIEW, DEPARTMENT OF JUSTICE IMMIGRATION REGULATIONS INSPECTION OF PERSONS APPLYING FOR ADMISSION § 1235.3 Inadmissible aliens...

  7. Zoological results of the Dutch Scientific Expedition to Central Borneo

    NARCIS (Netherlands)

    Jentink, F.A.

    1898-01-01

    In a paper dated April 1897 (Notes from the Leyden Museum, 1897, p. 25) Dr. Büttikofer stated that the work of the expedition was still being continued in Borneo, Dr. Nieuwenhuis having once more started for the Upper-Mahakkam with a staff of collectors, and that, according to the latest news he

  8. Jean-Baptiste Charcot, the French Antarctic expedition and scurvy

    Directory of Open Access Journals (Sweden)

    Hélio Afonso Ghizoni Teive

    2014-07-01

    Full Text Available During the second expedition to the South Pole, Commander Jean-Baptiste Charcot and some members of the crew of “Pourquoi Pas?” developed symptoms suggestive of scurvy. The clinical picture was totally reversed after dietary changes.

  9. Strategies and Procedures for Expediting Election Petitions and ...

    African Journals Online (AJOL)

    Justice delayed, they say, is justice denied. Delay in the dispensation of electoral disputes in Nigeria has become an albatross to the Nigerian nation. It has become a sour point in our electoral process. In this article, the writer meticulously looked at the various strategies and procedures for expediting election petitions and ...

  10. Recognizing and Developing Adaptive Expertise within Outdoor and Expedition Leaders

    Science.gov (United States)

    Tozer, Mark; Fazey, Ioan; Fazey, John

    2007-01-01

    Adaptive expertise, an individual's ability to perform flexibly and innovatively in novel and unstructured situations, could have particular relevance for expedition and outdoor leaders. This element may be recognized in leadership practitioners who are able to act more effectively when problem-solving in complex, ambiguous and unpredictable…

  11. Joint pricing and inventory replenishment decisions with returns and expediting

    NARCIS (Netherlands)

    Zhu, Stuart X.

    2012-01-01

    We study a single-item periodic-review model for the joint pricing and inventory replenishment problem with returns and expediting. Demand in consecutive periods are independent random variables and their distributions are price sensitive. At the end of each period, after the demand is realized, a

  12. 8 CFR 287.10 - Expedited internal review process.

    Science.gov (United States)

    2010-01-01

    ... Immigration and Customs Enforcement, 425 I Street NW., Washington, DC, 20536. (c) Expedited processing of... Section 287.10 Aliens and Nationality DEPARTMENT OF HOMELAND SECURITY IMMIGRATION REGULATIONS FIELD... enforcement activities. Alleged violations of the standards for enforcement activities established in...

  13. The Construction of Shared Knowledge in an Internet-based Shared Environment for Expeditions (iExpeditions).

    Science.gov (United States)

    Wang, Minjuan; Laffey, James; Poole, Melissa J.

    2001-01-01

    Investigates how participants (39 teenagers and 10 college-age online mentors) interacted and constructed shared knowledge of concepts, goals, tasks, procedures, and solutions when solving a real-world problem in an Internet-mediated project-based learning environment (iExpeditions). The main focus of the study was on how different patterns of…

  14. Spiral Survey Expedition: A proposal to organize for the Survey, exploration and eventual colonization of the Milky Way Galaxy

    Science.gov (United States)

    Galloway, Scott

    1993-12-01

    This paper details a plan to explore the galaxy. Areas of interest to an era of cyberspace include the Tech-Index information system for the expedition and the role cyberspace has in increasing expedition productivity and increasing the capabilities of cyberspace by expanding the goals and data set. The paper offers lists of projects for the cybermarket pool. The expedition is described also as a developers tool for cyberspace to acknowledge the scope of the human mind far surpasses present engineering yet guides our direction of energies and materials. Maintaining the biological capability to reproduce the Terran biosphere via Evolution park conservation areas is discussed. The ecological repair of Spaceship Earth and the build up of an interstellar industrial base from simple recyling and educational programs is meshed with a proposed 'reverse engineering cyberspace' plan. A set of constructive contests are proposed with 3 new currencies offered as prizes. The Planet, The Solar System, The Galaxy are 3 areas of focus. Each of these areas are considered in a cyberspectrum of (1) Sentience; (2) Biological diversity; and (3) Energy/Matter resources.

  15. Saba Bank research expedition 2011 - Progress Report

    NARCIS (Netherlands)

    Beek, van I.J.M.; Meesters, H.W.G.

    2013-01-01

    The Saba Bank is a large submerged carbonate platform of approximately 2,200 km2 in the Caribbean Sea which lies partially within the Exclusive Economic Zone of the Netherlands and partially within the territorial waters of Saba and St. Eustatius. The Saba Bank research program aims to obtain

  16. The Koster Expedition and the New Archeology

    Science.gov (United States)

    Struever, Stuart

    1975-01-01

    Describes archeology as a discipline and explains the interdisciplinary approach being used to explore the Koster excavations in Illinois. Four programs involving direct student participation in archeological research are outlined as well as the major findings at Koster and their contribution to interdisciplinary archeology. (BR)

  17. Early Science Results from the Williams College Eclipse Expedition

    Science.gov (United States)

    Pasachoff, Jay M.; Person, Michael J.; Dantowitz, Ron; Lockwood, Christian A.; Nagle-McNaughton, Tim; Meadors, Erin N.; Perez, Cielo C.; Marti, Connor J.; Yu, Ross; Rosseau, Brendan; Daly, Declan M.; Ide, Charles A.; Davis, Allen B.; Lu, Muzhou; Sliski, David; Seiradakis, John; Voulgaris, Aris; Rusin, Vojtech; Peñaloza-Murillo, Marcos A.; Roman, Michael; Seaton, Daniel B.; Steele, Amy; Lee, Duane M.; Freeman, Marcus J.

    2018-01-01

    We describe our first cut of data reduction on a wide variety of observations of the solar corona and of the effect of the penumbra and umbra on the terrestrial atmosphere, carried out from our eclipse site on the campus of Willamette University in Salem, Oregon. Our team of faculty, undergraduate students, graduate students, and other colleagues observed the eclipse, taking images and spectra with a variety of sensors and telescopes. Equipment included frame-transfer cameras observing at 3 Hz in 0.3 nm filters at the coronal green and red lines to measure the power spectrum of oscillations in coronal loops or elsewhere in the lower corona; 3 spectrographs; a variety of telescopes and telephotos for white-light imaging; a double Lyot system tuned at Fe XIV 530.3 nm (FWHM 0.4 nm) and Fe X 637.4 nm (FWHM 0.5 nm); and a weather station to record changes in the terrestrial atmosphere. We are comparing our observations with predictions based on the previous mapping of the photospheric magnetic field, and preparing wide-field complete coronal imaging incorporating NOAA/NASA GOES-16 SUVI and NRL/NASA/LASCO for the corona outside our own images (which extend, given the completely clear skies we had, at least 4 solar radii), and NASA SDO/AIA and NOAA/NASA GOES-16 SUVI for the solar disk. One of our early composites appeared as Astronomy Picture of the Day for September 27: https://apod.nasa.gov/apod/ap170927.htmlOur expedition was supported in large part by grants from the Committee for Research and Exploration of the National Geographic Society and from the Solar Terrestrial Program of the Atmospheric and Geospace Sciences Division of the National Science Foundation, with additional student support from the STP/AGS of NSF, the NASA Massachusetts Space Grant Consortium, the Sigma Xi honorary scientific society, the Clare Booth Luce Foundation studentship and the Freeman Foote Expeditionary Fund at Williams College, other Williams College funds, and U. Pennsylvania funds.

  18. Sediment compaction and pore pressure prediction in deepwater basin of the South China Sea: Estimation from ODP and IODP drilling well data

    Science.gov (United States)

    Xie, Yangbing; Wu, Tuoyu; Sun, Jin; Zhang, Hanyu; Wang, Jiliang; Gao, Jinwei; Chen, Chuanxu

    2018-02-01

    Overpressure in deepwater basins not only causes serious soft sediment deformation, but also significantly affects the safety of drilling operations. Therefore, prediction of overpressure in sediments has become an important task in deepwater oil exploration and development. In this study, we analyze the drilling data from ODP Leg 184 Sites 1144, 1146, and 1148, and IODP Leg 349 Sites U1431, U1432, U1433, and U1435 to study the sediment compaction and controls in the northern South China Sea. Sedimentation rate, sediment content, distribution area, and buried depth are the factors that influence sediment compaction in the deepwater basin of the South China Sea. Among these factors, the sediment content is the most important. The fitted normal compacted coefficients and mudline porosity for an interval of 50 m shows disciplinary variation versus depth. The pore pressure predicted from different fitted results shows varying overpressure situations. The normal compaction trend from Site 1144 reflects the porosity variation trend in stable deposition basins in the northern South China Sea. The predicted pore pressure shows overpressure at Site 1144, which is attributed to compaction disequilibrium. Nevertheless, the mixed lithology column may influence the predicted over-pressure at Site 1148, which is responsible for the confusing result. Above all, we find that sediment compaction should serve as a proxy for pore pressure in the deepwater basin of the South China Sea.

  19. The Arctic Ocean Then and Now: Preliminary Hydrographic Data from the 2015 US GEOTRACES Arctic Expedition

    Science.gov (United States)

    Swift, J. H.; Kadko, D. C.; Smethie, W. M., Jr.; Becker, S. M.; Barna, A.; Cummiskey, J.; Gum, J.; Miller, M. T.; Schatzman, C.

    2016-02-01

    The US GEOTRACES Arctic Expedition on USCGC Healy, August-October 2015, offers the opportunity to compare high-quality, full water column temperature, salinity, dissolved oxygen, and nutrient data from the Canadian sector of the Arctic Ocean with data from the 1994 Makarov Basin crossing from CCGS Louis S. St-Laurent (working with USCGC Polar Sea) and the 2005 Canada Basin transect from Icebreaker Oden (working with the Healy). Supplementary 2015 cruise funding for full-depth profiles for the US Global Ocean Carbon and Repeat Hydrography program and deployment of XCTDs and XBTs are being used to improve lateral resolution along the GEOTRACES track. This will allow identification of mesoscale features (e.g. eddies), improving interpretation of hydrographic and chemical data. The GEOTRACES track overlaps with those of the two previous cruises, thus, in addition to presenting the new hydrographic data, we will show and discuss the differences over the 10- and 20-year intervals between the cruises.

  20. The Hawaii Undersea Research Laboratory's 25th Anniversary Expedition to the South Pacific

    Science.gov (United States)

    Smith, J. R.; Wiltshire, J. C.; Malahoff, A.

    2005-12-01

    The Hawaii Undersea Research Laboratory (HURL) was established by NOAA at the University of Hawaii 25 years ago as part of its National Undersea Research Program. HURL's mission is to study deep water marine processes in the Pacific Ocean through a competitive proposal and review process. The dual Pisces IV and Pisces V 2000-meter manned submersibles, an RCV-150 1000-meter ROV, and multibeam equipped support ship R/V Ka'imikai-o-Kanaloa ( KoK) were largely acquired from the petroleum industry then adapted and upgraded to carry out cutting edge scientific expeditions. These studies range from active submarine volcanoes, delicate precious coral gardens, endangered marine mammal and fisheries management, to engineering surveys and deployment of observatory systems. HURL successfully completed a major 5-month expedition to the South Pacific during March-August 2005, working in the waters of New Zealand, Tonga, American Samoa, and the U.S. Line Islands covering a distance of nearly 14,500 nautical miles. This mission was significant in both the scientific merit and scope of operations, consisting of 8 different cruise legs at 21 study sites, with 12 chief and co-chief scientists, 58 total science team participants, and completing 61 out of 56 scheduled Pisces science dives, 17 ROV dives, 5 multibeam survey areas, 6 CTD rosette deployments, and 7 instrument mooring recoveries. The $3.5 million expedition was funded by an international partnership with New Zealand agencies (GNS & NIWA) and the University of Kiel in Germany along with the NOAA Office of Exploration and National Undersea Research Program. While most of the individual cruise legs focused on active submarine volcanoes of the Tonga-Kermadec Islands Arc and the Samoan hot spot chain with their hydrothermal systems and associated biological communities, others concentrated on marine protected areas including those of American Samoa and the remote atolls of the Line Islands of the Central Pacific. These studies

  1. Science at the ends of the Earth: astrobiology field expeditions as outreach tools

    Science.gov (United States)

    Billings, Linda

    martian meteorite, evidence of past and perhaps even present liquid water on Mars, the likelihood of a liquid water ocean on Europa, the possibility of liquid water beneath the surface of Titan, observations of a growing number of extrasolar planets, and identification of new forms of microbial life in an ever-widening range of extreme Earth environments. Consequently, in the 21st century the pace of robotic planetary exploration is speeding up and scientific and public attention is increasingly focusing on astrobiology research, especially the search for signs of life on Mars and in other environments in our solar system. NASA's ASTEP program is sponsoring field campaigns to test science strategies and robotic technologies that could be useful in conducting astrobiological investigations in planetary environments, focusing on Mars and Europa. Public interest in astrobiology research is substantial, and advances in the field are rapid. Thus the NASA Astrobiology Program encourages Principal Investigators to incorporate communication, education, and public outreach initiatives in their research plans. NASA ASTEP projects provide especially good opportunities for communication, education, and outreach. The work of ASTEP projects takes place in remote terrestrial environments, places typically inaccessible to "civilians": the Norwegian protectorate of Svalbard, above the Arctic Circle; the far-northern reaches of the Arctic Ocean; the dry valleys of Antarctica; deep-sea hydrothermal vent systems and other unmapped underwater environments. ASTEP projects involve human researchers working with robotic adjuncts. ASTEP teams often combine include senior and student researchers. Some have even included "embedded" journalists and public affairs officers. ASTEP expeditions typically unfold in visually interesting, sometimes stunning, physical environments. ASTEP expeditions are virtually always intensive learning experiences for their researchers, and thus they provide good

  2. Expedition 8 Crew Interviews: C. Michael Foale - CDR

    Science.gov (United States)

    2003-01-01

    C. Michael Foale, Commander of the Expedition 8 crew to the International Space Station (ISS), answers interview questions in this video. The questions cover: 1) The goals of the Expedition; 2) How his Mir experience prepared him for long-duration spaceflight; 3) The reaction the Columbia accident where he was training in Star City, Russia; 4) Why the rewards of spaceflight are worth the risks; 5) Why he wanted to become an astronaut; 6) His career path; 7) His influences; 8) His path of study; 9) His responsibilities on a mission; 10) What a Soyuz capsule is like; 11) What the oncoming and offgoing ISS crews will do together; 12) How the ISS science mission will be advanced during his stay; 13) Training and plans for extravehicular activity (EVA); 14) Return to Flight of Shuttle; 15) What is needed to make his mission a success; 16) The most valuable contribution of the ISS.

  3. Medical Operational Challenges in the Expedition 16 Landing and Recovery

    Science.gov (United States)

    Moynihan, S.; Johnston, S. L.; Ilcus, L. S.; Shevchenko, V.

    2009-01-01

    On April 19, 2008 the crew of Expedition 16 left the International Space Station and returned to earth via their Soyuz TMA-11 capsule after 192 days on orbit. Their capsule experienced the second consecutive and third ballistic reentry in the last 10 TMA recoveries and landed approximately 260 miles (420 km) from the prime landing site. Issues: The purpose of this presentation will be to describe, not only the typical medical operational challenges faced by Flight Surgeons recovering a long duration crew from space, but also address the unique challenges that existed with the Expedition 16 landing and crew recovery. Nominal Soyuz recovery challenges include remote recovery sites with crew exposures to sleep shifting and fatigue, dehydration, hypothermia and hyperthermia, and rotational, sustained, and impact g-forces. These environmental factors coupled with the patho-physiologic neuro-vestibular and orthostatic intolerance changes that occur secondary to the crews reintroduction into the earth s gravity field will be detailed. Additional challenges that were unique to this expedition included a ballistic reentry with higher g-loads, the presence of fire outside of the capsule on landing, a contingency medical event of a ground support personnel, and loss of communications with the crew just prior to landing and during recovery operations. Conclusions: In spite of these unique challenges the Russian Search and Rescue Forces and Medical Support personnel along with U.S. Medical Support performed well together. Possible improvements in training and coordination will be discussed.

  4. Early scientific expeditions and local encounters: new perspectives on Carsten Niebuhr and 'The Arabian Journey'

    DEFF Research Database (Denmark)

    scholarly expeditions and voyages from the eighteenth and early nineteenth century, placing the Danish expedition in a broad context of early scientific expeditions. This was a time when the coastlines of continents, except in the Pacific and the Polar regions, were reasonably well known. Yet scientific...... and longer encounters with local populations. Most studies in this volume focus on expeditions that involved contacts between local people and travelling European scientists and scholars. Others examine the scholarly questions which the scientific expeditions and travellers were sent out to solve and how......, the papers in these proceedings paint a varied picture of eighteenth and early nineteenth century scientific expeditions and scholarly travel. In the eighteenth century the considerate and careful approach of Niebuhr and Forsskål in their dealing with local people was new or at least not so common...

  5. North Atlantic Climate Changes During the Last 100 ky as Reflected in Deep Sea Ostracod Assemblages at IODP Site U1314

    Science.gov (United States)

    Alvarez Zarikian, C. A.; Stepanova, A. Y.

    2006-12-01

    Changes in the North Atlantic climate have influenced surface water productivity and deep-sea bottom water circulation patterns, thus affecting deep sea benthic assemblages. This study examines the ostracod assemblage composition over the last 100 ky in sediments drilled at IODP Site U1314 to establish the effects of climate change from the Late Pleistocene to Holocene. Site U1314 is located on the southern Gardar Drift at a water depth of 2820 m. At present, the location of the drill site lies under the influence of the lower portion of the relatively warm, highly saline and well oxygenated North Atlantic Deep Water (NADW), whereas during glacial times this water mass may have been replaced by the northward flowing nutrient-rich and low oxygen Southern Ocean Water [1]. The age model for the studied interval is based on an existent benthic oxygen isotope-based stratigraphy from Site 983 ODP Leg 162 in the northern Gardar Drift [2] and derived from the correlation of reflectance and magnetic susceptibility data from ODP Site 983 and IODP Site U1314 [3]. High amplitude fluctuations in ostracod abundance and diversity were observed at Site U1314. Krithe is the dominant genus in both glacial and interglacial assemblages (40-90 %), but exhibits slightly lower abundance during glacial intervals. Other common genera, such as Oxycythereis and Echinocythereis, display their highest relative abundances during interglacial times, whereas Rockallia and Cytheropteron seem to have their highest relative abundances during glacial and cooling conditions. Besides dominant taxa typical for colder climate, some other glacial-indicative genera (Nannocythere, ?Rhombobythere, Pseudocythere and Polycope) are usually present, although their relative abundances are low. The transition from Marine Isotope Stage 3 (MIS 3) to MIS 2 and the subsequent deglaciation are characterized by the highest ostracod abundance and diversity, although most of the species present exhibit very low abundance

  6. The GOLD IODP Project: Global Climate Changes, Extreme Events, Margins formation and the Limits of Life in the Gulf of Lion

    Science.gov (United States)

    Rabineau, M.

    2009-12-01

    Miocene and older sediments the drilling combined to seismic reflexion data, will give the nature, the paleoenvironments and dating of deposits enabling early history of margin formation and subsidence understanding and an Astronomically Tuned Neogene Time Scale to be established. 4) The messinian extreme event represents a unique sedimentological, hydrological, oceanographic, biological and climatological crisis in earth history. It is a unique case to study and quantify the impact of an outstanding sea-level drop (more than 1500 m, one order of magnitude greater than Late Quaternary glaciations) on sedimentary river behavior, deltaic and evaporitic deposition. Furthermore, the amount of messinian deposits reaches more than 3000 m. Such important erosion and sedimentation must provide crucial information on margin vertical dynamic. So far, DSDP and IODP drillings have reached the upper part of the evaporites only, the beginning of the crisis is still a matter of intense debate and conjectures. We invite all interested participants to join this drilling project and let you know that we have proposed an IODP Magellan Workshop in Banyuls in early March 2010.

  7. Sea-surface dynamics changes in the North Atlantic Ocean (IODP Site U1314) during late Pliocene deduced from calcareous nannofossil observation

    Science.gov (United States)

    Jatiningrum, R. S.; Sato, T.; Effendi, R.

    2016-12-01

    Calcareous nannofossils were analyzed on the late Pliocene sediments (2.55 to 2.88 Ma) from the southern Gardar Drift, in the subpolar North Atlantic IODP Site U1314 (56°21.9'1N, 27°53.3'W) at an average resolution of 3 kyr. In this study, a total 131 samples were analyzed and a total of 24 species from 14 genera were identified by polarizing microscope observation. In general, the coccolith assemblage is dominated by Reticulofenestra spp., whilst significant changes in paleoceanographic conditions are mainly shown by the ratio of Reticulofenstra morphometric and several subordinate species. Top of D. tamalis found at 272.81 mcd, which dates to an age of 2.756 Ma. The age is based on correlation with the age model established by Hayashi et al. (2012) and modified partly by Sato et al. (2015). The presence of abundant large reticulofenestrids and lower abundance of C. pelagicus characterized the interval through G12 to G10, indicate oligotrophic surface waters and northward heat transport by intensified NAC. During G9/G8 transition the abundance of large reticulofenestrids decreased abruptly and alternating with small reticulofenestrids. Above G9/G8 transition is characterized by abundance of small reticulofenestrids, higher abundance of P. lacunosa and the cold-water species C. pelagicus, suggesting higher surface water productivity and the prevalence of cold waters over the site. Thus, reflecting a weakened influence of the NAC and southward position of AF that is characterized by high eddy activity in correspondence with cooler and nutrient-rich waters.

  8. What Aims, what Motives? Determining Research Priorities in the International Indian Ocean Expedition, 1960-1965

    Science.gov (United States)

    Doel, R.

    2016-12-01

    Fundamental tensions affected planning for United States involvement in the International Indian Ocean Expedition (IIOE). At the highest levels of the US state, science advisors and State Department officials praised the proposed Indian Ocean research plan—loosely modeled on the recently completed International Geophysical Year of 1957-58—as a way of promoting scientific internationalism, seeing this undertaking as a way to help bring India more firmly within the Western sphere amid Cold War East-West conflicts. Dwight D. Eisenhower's presidential science advisor, George Kistiakowsky, had the IIOE in mind when he advised the National Security Council that a key role science could play in American foreign relations lay "in relation with the neutral and less-developed countries." At the same time, American scientists invited to take part in the Indian Ocean Expedition—while generally sympathetic with U.S. foreign policy aims—prioritized research programs in the physical branches of the environmental sciences. While policy-makers hoped to encourage biological research, with the aim of encouraging fisheries and protein production to aid Indian citizens, earth scientists—better-funded, better-organized, supported by military agencies because their studies were crucial to national security—came to dominate the IIOE. While the IIOE was later judged a success, for it extended long-running research programs in physical and chemical oceanography into a less-explored ocean, hopes to advance biological programs on an equal footing proved premature.

  9. Dynamic mobility applications, program evaluation : national-level impacts and costs estimation : final report.

    Science.gov (United States)

    2016-07-01

    The vision of the Dynamic Mobility Applications (DMA) program is to expedite the development, testing, and deployment of innovative mobility applications that maximize system productivity and enhance mobility of individuals within the surface transpo...

  10. Ozone Hole Airborne Arctic Stratospheric Expedition (Pre-Flight)

    Science.gov (United States)

    1989-01-01

    The first segment of this video gives an overview of the Ozone Hole Airborne Arctic Stratospheric Expedition, an international effort using balloon payloads, ground based instruments, and airborne instruments to study ozone depletion and the hole in the ozone over Antarctica which occurs every spring. False color imagery taken from NASA's Nimbus 7 satellite which documents daily changes in ozone is also shown. The second segment of this video shows actual take-off and flight footage of the two aircraft used in the experiment: the DC-8 Flying Laboratory and the high flying ER-2.

  11. Community College's CAN do Research A Decade of Eclipse Expeditions

    Science.gov (United States)

    Saken, Jon M.

    2006-12-01

    Gale force winds, ravenous Tsetse flies and duct-tape equipment repairs. Now that's science! This talk will describe the triumphs and disasters over almost a decade of world-wide astronomical expeditions involving community college students, faculty and K-12 teachers chasing one of nature's most spectacular shows a total solar eclipse. The impact of this kind of field science on the participants and the wider community, along with other lessons learned along the way, will also be discussed, as we present ideas to encourage others to join in the fun.

  12. Composites Manufacturing Education and Technology Facility Expedites Manufacturing Innovation

    Energy Technology Data Exchange (ETDEWEB)

    2017-01-01

    The Composites Manufacturing Education and Technology facility (CoMET) at the National Wind Technology Center at the National Renewable Energy Laboratory (NREL) paves the way for innovative wind turbine components and accelerated manufacturing. Available for use by industry partners and university researchers, the 10,000-square-foot facility expands NREL's composite manufacturing research capabilities by enabling researchers to design, prototype, and test composite wind turbine blades and other components -- and then manufacture them onsite. Designed to work in conjunction with NREL's design, analysis, and structural testing capabilities, the CoMET facility expedites manufacturing innovation.

  13. Did opening of the South China Sea impact development of the Asian Monsoon? Results from Oligocene microfossils, IODP Site U1435, northern South China Sea

    Science.gov (United States)

    Kulhanek, Denise K.; Su, Xin; Li, Qianyu; Gregory, Mitch; Warny, Sophie; Clift, Peter D.

    2016-04-01

    Development of the Asian Monsoon is linked to uplift of the Himalayas and Tibetan Plateau in the Cenozoic, with good evidence for a strong monsoon system by the late Oligocene to early Miocene (e.g., Guo et al., 2002; Clift et al., 2008). However, Licht et al. (2014) suggested the presence of an Asian Monsoon in the late Eocene. Recent scientific ocean drilling in the Indian Ocean and surrounding marginal seas gives us the opportunity to test this hypothesis with newly recovered Paleogene sediment cores. International Ocean Discovery Program Expedition 349 to the South China Sea recovered a 30 m section of primarily lower Oligocene nannofossil-rich claystone at Site U1435, located near the northern continent/ocean boundary. A thick sandstone unit devoid of typical marine microfossils underlies the marine claystone. The sandstone is interpreted as a deltaic or restricted marine deposit and is dated to the Eocene based on the presence of organic-walled palynomorphs, suggesting that a hiatus of several million years likely separates the sandstone below from the Oligocene marine claystone. This hiatus is interpreted as the breakup unconformity, with paleodepths in the South China Sea increasing during the Oligocene. Thus, this claystone should record if opening of the South China Sea during the early Oligocene influenced development of the Asian Monsoon. Combined calcareous nannofossil and planktonic foraminifer biostratigraphy indicates that the 30 m section is primarily early Oligocene in age (~33.5-30 Ma) and was deposited on the middle slope, with paleodepths >500 m. Stable oxygen isotopes from planktonic foraminifers become heavier up-hole, suggestive of cooling/deepening in the region, whereas carbon isotopes record variable conditions with no distinct maxima or minima. Calcareous nannoplankton primarily live in the upper 50 m of the ocean and are sensitive to sea-surface temperature and nutrient conditions, thus making them useful recorders of paleoceanographic

  14. Non-Dive Activities for Expedition to the Deep Slope 2006 - Office of Ocean Exploration and Research

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Non-dive activities reported to the NOAA Office of Ocean Exploration and Research for the "Expedition to the Deep Slope 2006" expedition, May 7 through June 2, 2006....

  15. Results of the Rumphius Biohistorical Expedition to Ambon . Part 1. General Account and List of Stations

    NARCIS (Netherlands)

    Strack, H.L.

    1993-01-01

    This report gives a general account of the Rumphius Biohistorical Expedition to Ambon (Moluccas, Indonesia) held in 1990. The primary objective of the expedition was to collect marine invertebrates on the localities mentioned by Rumphius (1627-1702) in his book "D'Amboinsche Rariteitkamer" (1705).

  16. The Indigo V Indian Ocean Expedition: a prototype for citizen microbial oceanography

    DEFF Research Database (Denmark)

    Lauro, Frederico; Senstius, Svend Jacob; Cullen, Jay

    2014-01-01

    sample acquisition. The ultimate goal of the Indigo V Expedition is to create a working blue-print for ’citizen microbial oceanography’.We will present the preliminary outcomes of the first Indigo V expedition, from Capetown to Singapore, highlighting the challenges and opportunities of such endeavours....

  17. Zoological results of the Dutch Scientific Expedition to Central-Borneo

    NARCIS (Netherlands)

    Lidth de Jeude, van Th.W.

    1905-01-01

    The following pages contain an enumeration of the lizards collected in Borneo by the Dutch Borneo-Expedition, of which expedition Mr. J. Büttikofer was the zoologist, and also of the lizards collected by Dr. A. W. Nieuwenhuis during his travels in the interior of this island. The collections made

  18. Zoological results of the Dutch New Guinea expedition, 1939. No. 51) The Birds

    NARCIS (Netherlands)

    Junge, G.C.A.

    1953-01-01

    The present paper is the report on a collection of birds brought together during the expedition of the "Koninklijk Nederlandsch Aardrijkskundig Genootschap" to the Wissel Lake area in 1939. The zoologist of this expedition Prof. Dr. H. Boschma collected with the assistance of two mantris of the

  19. 42 CFR 422.572 - Timeframes and notice requirements for expedited organization determinations.

    Science.gov (United States)

    2010-10-01

    ..., Organization Determinations and Appeals § 422.572 Timeframes and notice requirements for expedited organization... 42 Public Health 3 2010-10-01 2010-10-01 false Timeframes and notice requirements for expedited organization determinations. 422.572 Section 422.572 Public Health CENTERS FOR MEDICARE & MEDICAID SERVICES...

  20. 42 CFR 423.572 - Timeframes and notice requirements for expedited coverage determinations.

    Science.gov (United States)

    2010-10-01

    ... and notice requirements for expedited coverage determinations. (a) Timeframe for determination and... 42 Public Health 3 2010-10-01 2010-10-01 false Timeframes and notice requirements for expedited coverage determinations. 423.572 Section 423.572 Public Health CENTERS FOR MEDICARE & MEDICAID SERVICES...

  1. 75 FR 17453 - International Product Change-Global Reseller Expedited Package Contracts

    Science.gov (United States)

    2010-04-06

    ... From the Federal Register Online via the Government Publishing Office POSTAL SERVICE International Product Change--Global Reseller Expedited Package Contracts AGENCY: Postal Service TM . ACTION: Notice... Global Reseller Expedited Package Contracts to the Competitive Products List pursuant to 39 U.S.C. 3642...

  2. 78 FR 33452 - International Product Change-Global Reseller Expedited Package Contracts 2

    Science.gov (United States)

    2013-06-04

    ... From the Federal Register Online via the Government Publishing Office POSTAL SERVICE International Product Change--Global Reseller Expedited Package Contracts 2 AGENCY: Postal Service\\TM\\. ACTION: Notice... Commission to add Global Reseller Expedited Package Contracts 2 to the Competitive Products List. DATES...

  3. Syllidae (Annelida: Polychaeta) from Indonesia collected by the Siboga (1899-1900) and Snellius II expeditions

    NARCIS (Netherlands)

    Aguado, M.T.; San Martín, G.; ten Hove, H.A.

    2008-01-01

    Twenty seven samples of syllids (Annelida: Polychaeta) from Indonesia collected during the Siboga Expedition (1899-1900) and five during the Snellius II Expedition (1984) have been examined. Material from several other museums and Institutions has also been included. Unpublished identifications of

  4. 75 FR 26343 - Request for Expedited Certification and Type Approval of Amtrak Advanced Civil Speed Enforcement...

    Science.gov (United States)

    2010-05-11

    ... Federal Railroad Administration Request for Expedited Certification and Type Approval of Amtrak Advanced... for expedited certification and type approval of the Amtrak ACSES. ACSES has been deployed on the... party seeking certification and type approval of ACSES, the regulatory provisions involved, the nature...

  5. Early scientific expeditions and local encounters: new perspectives on Carsten Niebuhr and 'The Arabian Journey'

    DEFF Research Database (Denmark)

    scholarly expeditions and voyages from the eighteenth and early nineteenth century, placing the Danish expedition in a broad context of early scientific expeditions. This was a time when the coastlines of continents, except in the Pacific and the Polar regions, were reasonably well known. Yet scientific...... knowledge about natural history and detailed geography of the interior of the continents other than Europe, as well as scholarly understanding of foreign cultures, both ancient and contemporary, was still limited. Increasing focus on land-based travels in the eighteenth century and onwards meant more...... and longer encounters with local populations. Most studies in this volume focus on expeditions that involved contacts between local people and travelling European scientists and scholars. Others examine the scholarly questions which the scientific expeditions and travellers were sent out to solve and how...

  6. Polar poisons: did Botulism doom the Franklin expedition?

    Science.gov (United States)

    Horowitz, B Zane

    2003-01-01

    In 1845 the Franklin expedition left London with 2 ships and 134 men on board in an attempt to find the route through the Northwest Passage. The ships were built with state-of-the-art technology for their day, but provisioned with supplies from the lowest bidder. After taking on fresh provisions in the Whalefish Islands, off the coast of Greenland, the entire crew was never heard from again. Graves found on remote Beechey Island indicate that three able-bodied seamen died during the first winter. A note written on a ship's log, later found in a cairn, indicate that the expedition's leader, Sir John Franklin, died during the second winter entrapped on the ice, by which time 24 men had also perished. The remaining crew failed in their attempt to walk out of the Arctic by an overland route. In 1981 Owen Beattie, from the University of Alberta, exhumed the remains of the sailors from the three graves on Beechey Island. Elevated lead levels were found in all three sailors. While lead poisoning has been a leading theory of the cause of the crew's deaths, blamed on the crudely tinned provisions the ships carried with them from England, chronic lead exposure may only have weakened the crew, not necessarily killed them. One of three exhumed sailors also had in his intestine the spores of an unspecified Clostridium species. The theory put forth by this article is that Botulism, type E, which is endemic in the Arctic, may have been responsible for their deaths.

  7. A Cenozoic record of the equatorial Pacific carbonate compensation depth

    Digital Repository Service at National Institute of Oceanography (India)

    Palike, H.; Lyle, M.W.; Nishi, H.; Raffi, I.; Ridgwell, A.; Gamage, K.; Klaus, A.; Acton, G.; Anderson, L.; Backman, J.; Baldauf, J.; Beltran, C.; Bohaty, S.M.; Bown, P.; Busch, W.; Channell, J.E.T.; Chun, C.O.J.; Delaney, M.; Dewangan, P.; et al.

    an important role in climate regulation1. Integrated Ocean Drilling Program (IODP) Expeditions 320/321, the "Pacific Equatorial Age Transect" (PEAT), exploited the northward Pacific plate trajectory during the Cenozoic to recover a continuous sediment... the locus of carbonate deposition between shelf and deep ocean. Therefore, increasing solute supply should be coupled to increased weathering, a warmer climate, and higher CO2, unless changes in orbital configuration significantly enhance or reduce...

  8. 21 CFR 56.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-04-01

    ... categories of research that may be reviewed by the IRB through an expedited review procedure. The list will... uses an expedited review procedure shall adopt a method for keeping all members advised of research... 21 Food and Drugs 1 2010-04-01 2010-04-01 false Expedited review procedures for certain kinds of...

  9. 49 CFR 11.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-10-01

    ... Expedited review procedures for certain kinds of research involving no more than minimal risk, and for minor... an expedited review procedure shall adopt a method for keeping all members advised of research... 49 Transportation 1 2010-10-01 2010-10-01 false Expedited review procedures for certain kinds of...

  10. Zircon U-Pb Ages of Tuffs and Volcaniclastic Sandstone of the Core Sample of IODP Exp. 322 at the Northern Part of the Shikoku Basin.

    Science.gov (United States)

    Shinjoe, H.; Nakajima, T.; Orihashi, Y.; Saito, S.; Oda, H.; Danhara, T.

    2014-12-01

    We determined U-Pb ages of zircons from core samples of IODP Exp. 322 using the laser abrasion ICP-MS (VG Plasma Quad 3 with New Wave Research UP-213). Zircon crystals were separated from four felsic tuffs from the Unit V of Site C0011, and a volcaniclastic turbidite sandstone of the lowermost horizon of the Unit V of Site C0012. Both of the drilling sites are located off the Nankai trough on the Shikoku Basin of the Philippine Sea plate, southwest Japan. Zircons from two felsic tuffs from Site C0011 are euhedral crystals, and most of their 238U-206Pb ages range 13 - 16 Ma. Weighted means of the 238U-206Pb ages of these samples are ca. 14.3 Ma. The other two felsic tuffs include zircon grains with older ages (80 - 260 Ma), however, weighted means of the 238U-206Pb ages of population with young ages ranges 14.5 - 14.7 Ma. These ages are coincide with those of the intense felsic magmatism occurred in the forearc region of southwest Japan (14 - 15 Ma) just after the opening of the Japan Sea and consequent clockwise rotation of the southwest Japan. Some of the felsic igneous bodies of the middle Miocene southwest Japan ejected large amount of felsic materials resulting caldera formation. So the provenance of felsic tuffs from the core of the Site C0011 are presumed to be one of the felsic igneous bodies of the forearc region of southwest Japan. Turbidite sandstone from Site C0012 also includes Miocene zircon grains of which their weighted mean of the 238U-206Pb ages is ca. 14.2 Ma. Moreover turbidite sandstone contains zircons with various ages (19 - 2500 Ma). One of the possible origin of such old zircon grains is reworking from sediments of the accretionary complex in the forearc of southwest Japan. If we assume the present rate of convergence of the Philippine sea plate (ca. 4 cm/y) is invariant, the turbidite including both clastic sediment and coeval felsic igneous materials traveled ca. 600 km across the trench.

  11. Sulfur isotope geochemistry of the central Japan Sea sediments (IODP Exp. 346) 20 150 kyr ago: Implications for the evolution of Asian Monsoon climate system

    Science.gov (United States)

    Oshio, S.; Yamaguchi, K. E.; Takahashi, S.; Naraoka, H.; Ikehara, M.

    2016-12-01

    Asian monsoon climate system has started about 50 Ma, after the collision of the Indian and Eurasian continents followed by uplift of the Himalaya and Tibetan Plateau. It has influenced sediments in the Japan Sea, where cm-scale alternation of Corg-rich dark layers and Corg-poor light layers occurs. This is most likely due to temporal changes in the nutrient status and/or oceanic redox conditions, which are likely caused by the fluctuations in the intensity of continental weathering and ocean currents, both of which were ultimately caused by the variable monsoon system. In order to obtain insights into the evolving oceanic redox state and the monsoon system, we conducted sulfur speciation and isotope study for the marine sediment core samples recovered in the central Japan Sea by IODP Exp. 346. The light layers have lower Spy (0.03-0.25 wt.%) contents when compared to the dark layers (0.26-1.49 wt.%). The Corg contents have similar distribution (0.34-1.10 wt.% for light layers and 1.16-3.38 wt.% for dark layers). However, the SSO4 contents (0.02-.64 wt.%) and the δ34S values (-34 to -38‰) did not show such light-dark distinction. Elevated Spy/Corg ratios (0.03-1.00) in the dark layers are interpreted to represent sulfide formation in the anoxic water column by bacterial sulfate reduction. During deposition of light layers, oxidation of sulfide minerals could have resulted in formation of sulfate minerals without significant isotope fractionation, as observed in this study. Regardless of the type of the sediments (dark vs. light), sulfate was not limiting during bacterial sulfate reduction, as reflected in the sulfur isotope compositions. We speculate that, during deposition of dark layers, enhanced summer monsoon activity caused heavy rainfall and increased source-rock weathering, runoff of the Yangtze River, and nutrient input into the East China Sea and the Tsushima Warm Current. Inflow of nutrient-rich and less salty water into the Japan Sea triggered

  12. Activities of the summer operation of the 52nd Japanese Antarctic Research Expedition (JARE-52 in 2010–2011

    Directory of Open Access Journals (Sweden)

    Takashi Yamanouchi

    2011-11-01

    Full Text Available This report describes the activities of the 52nd Japanese Antarctic Research Expedition (JARE-52 during the 2010-2011 austral summer. JARE-52, as the first year of the"VIIIth JARE 6-year program", carried out various research projects and logistical plans. Basic observations, composed of routine observations and monitoring observations, were continued as part of long-term observations, and a newly established prioritized research program"Global Warming Investigated from the Antarctic"was started, comprising three sub-targets:"Global Environmental Changes from the Antarctic Middle and Upper Atmosphere","Responses of Southern Ocean Ecosystems in Global Warming"and"Current and Future Global Environment seen from Glacial-Interglacial Cycles". Ten projects of the ordinary research observations program, including astronomy in Antarctica, were also carried out. The largest tasks of the expedition were the setting of the large atmospheric MST/IS radar (PANSY and the construction of a building for harnessing natural energy and providing garage space. The main summer activities involved the transportation of materials, the maintenance of facilities at Syowa Station, and observations from on board the icebreaker RV Shirase and in the field, including an inland trip to Dome Fuji Station. Given the extensive sea ice in Lutzow-Holm Bay following the 51st expedition, we expected difficult conditions during the 2010-2011 season and possibly challenges to overcome in accomplishing the entire program. Our predictions proved to be accurate, as we encountered thick fast ice covered by a thick snow layer, and severe ice conditions in the pack ice area with folded ice. The weather conditions were relatively calm in December but challenging in January, with long periods of strong wind, snowfall, and blowing snow, as well as record low sunshine hours. Despite the conditions, we managed to accomplish most of the large-scale construction projects and observations that

  13. Implementation and Operational Research: Expedited Results Delivery Systems Using GPRS Technology Significantly Reduce Early Infant Diagnosis Test Turnaround Times.

    Science.gov (United States)

    Deo, Sarang; Crea, Lindy; Quevedo, Jorge; Lehe, Jonathan; Vojnov, Lara; Peter, Trevor; Jani, Ilesh

    2015-09-01

    The objective of this study was to quantify the impact of a new technology to communicate the results of an infant HIV diagnostic test on test turnaround time and to quantify the association between late delivery of test results and patient loss to follow-up. We used data collected during a pilot implementation of Global Package Radio Service (GPRS) printers for communicating results in the early infant diagnosis program in Mozambique from 2008 through 2010. Our dataset comprised 1757 patient records, of which 767 were from before implementation and 990 from after implementation of expedited results delivery system. We used multivariate logistic regression model to determine the association between late result delivery (more than 30 days between sample collection and result delivery to the health facility) and the probability of result collection by the infant's caregiver. We used a sample selection model to determine the association between late result delivery to the facility and further delay in collection of results by the caregiver. The mean test turnaround time reduced from 68.13 to 41.05 days post-expedited results delivery system. Caregivers collected only 665 (37.8%) of the 1757 results. After controlling for confounders, the late delivery of results was associated with a reduction of approximately 18% (0.44 vs. 0.36; P GPRS printers) that reduce delays.

  14. After-effects of a high altitude expedition on blood.

    Science.gov (United States)

    Böning, D; Maassen, N; Jochum, F; Steinacker, J; Halder, A; Thomas, A; Schmidt, W; Noé, G; Kubanek, B

    1997-04-01

    The aim of the study was to investigate blood alterations caused by altitude acclimatization which last more than few days after return and might play a role for exercise performance at sea level. Measurements were performed in 12 mountaineers before, during and either 7/8 or 11/12 days after a Himalaya expedition (26-29 days at 4900 to 7600 m altitude). [Erythropoietin] rose only temporarily at altitude (max. +11 +/- 1 [SE] mu/ml serum). After return hemoglobin mass (initially 881 +/- 44 g, CO-Hb method) was increased by 14% (p training, partly in the Alps, and the stay in the Himalaya influenced O2-affinity for a prolonged time. The adaptations might reduce the loss of physical performance capacity at altitude and be part of altitude training effects.

  15. Physiologic adaptation changes of the "Bering Bridge" expedition participants.

    Science.gov (United States)

    Aidaraliyev, A A; Maximov, A L; Mala, T

    1993-04-01

    Cardiorespiratory measurements were repeatedly performed on indigenous and Caucasian Soviet and American male team members of the Bering Bridge expedition which covered approximately 1280 km over a 61 day period. Significant baseline differences in cardiorespiratory functions at rest and during submaximal cycle ergometer exercise were noted between racial groups. Indigenous members had significantly lower mean vital lung capacity and oxygen consumption levels during submaximal exercise, but a greater systolic blood pressure response to exercise. The energy cost during submaximal work decreased during the trek in both groups, but was marked in the Caucasians, suggesting that the indigenous subjects were better adapted at baseline to the Arctic environment. Overall, there was stabilization of functional responses in four of seven parameters studied, although differences between racial groups remained the same.

  16. ISS Expedition 1 Crew Interviews: Sergei K. Krikalev

    Science.gov (United States)

    2000-01-01

    Live footage of a preflight interview with Flight Engineer Sergei K. Krikalev is seen. The interview addresses many different questions including why Krikalev became a cosmonaut, the events that led to his interest, the transition from being an engineer to being selected as a Russian cosmonaut. Other interesting information that this one-on-one interview discusses are the main goals of the first Expedition Crew, their scheduled docking with the International Space Station (ISS), making the ISS ready for human inhabitance, and all the specifics that will make his living arrangements difficult. Krikalev mentions his responsibilities during the much-anticipated two-day flight to the ISS, as well as the possibility of his space-walk. Krikalev also discusses the crew's first tasks upon entrance including other scheduled tasks for the first week, docking from cargo ships, and spacecraft delivering equipment or performing Extra Vehicular Activities (EVA). He explains his opinion of the implications of having human beings in space.

  17. Expedited Demolition Notification for 2nd Quarter CY 2012 Structures

    Energy Technology Data Exchange (ETDEWEB)

    Juarez, Catherine L. [Los Alamos National Laboratory

    2012-06-18

    The National Nuclear Security Administration and Los Alamos National Security, LLC (LANS) (collectively the Permittees) are informing the New Mexico Environment Department Hazardous Waste Bureau (NMED-HWB) of the need to expedite the demolition of structures summarized in the enclosures. These structures have been identified to receive funding and be demolished prior to the 3rd Quarter Demolition Notification (June 30, 2012). This letter is a follow up to the email that was sent to the NMED-HWB on April 17, 2012. The enclosures attached to this letter satisfy the reporting requirements as outlined in Section 1.17 of the LANL Hazardous Facility Waste Permit (Permit). Demolition of buildings that appear on this list will not occur until 30 days after NMED has received this notification.

  18. Expediting the transfer of evidence into practice: building clinical partnerships*

    Science.gov (United States)

    Rader, Tamara; Gagnon, Anita J.

    2000-01-01

    A librarian/clinician partnership was fostered in one hospital through the formation of the Evidence-based Practice Committee, with an ulterior goal of facilitating the transfer of evidence into practice. The paper will describe barriers to evidence-based practice and outline the committee's strategies for overcoming these barriers, including the development and promotion of a Web-based guide to evidence-based practice specifically designed for clinicians (health professionals). Educational strategies for use of the Web-based guide will also be addressed. Advantages of this partnership are that the skills of librarians in meeting the needs of clinicians are maximized. The evidence-based practice skills of clinicians are honed and librarians make a valuable contribution to the knowledgebase of the clinical staff. The knowledge acquired through the partnership by both clinicians and librarians will increase the sophistication of the dialogue between the two groups and in turn will expedite the transfer of evidence into practice. PMID:10928710

  19. The Paran\\'a Ra'anga expedition

    CERN Document Server

    Gangui, Alejandro; Vena, Pablo

    2013-01-01

    Paran\\'a Ra'anga (the image of Paran\\'a, in Guaran\\'i) is the name of a cultural and scientific expedition that traveled the rivers: R\\'io de la Plata, Paran\\'a and Paraguay, from Buenos Aires to Asunci\\'on, during March 2010. The project brought together some forty scientists and artists from three countries in a slow and enriching cruise, putting in active contact actors from different backgrounds and disciplines -which usually run separately- in the framework of an unusual space-time experience. The project recovers the historical tradition of the trip as an instrument of knowledge and collaboration between the arts and sciences, necessary to build new ways of seeing and understanding the river and its banks. This article reports on the motivations of this project and its projection.

  20. Expedited partner treatment for sexually transmitted infections: an update.

    Science.gov (United States)

    Kissinger, Patricia; Hogben, Matthew

    2011-04-01

    To date, seven randomized trials have evaluated the efficacy of expedited partner treatment (EPT). These trials have included heterosexual men and women and examine EPT for Chlamydia trachomatis, Neisseria gonorrhoea, and Trichomonas vaginalis. These studies demonstrated either superiority for percentage of partners being treated, for a reduction in repeat infections, or cost benefit for EPT compared to the standard partner referral method and reported no adverse events. In the United States, although the number of states where EPT is legal continues to grow, adoption of EPT remains low. Provider concerns about liability and payment issues continue to be a barrier to implementation of EPT. More translational research is needed to improve adoption by the players involved: index patients, partners, providers, and payers.

  1. Activity report of the 40th Japanese Antarctic Research Expedition wintering party in 1999-2000

    Directory of Open Access Journals (Sweden)

    Hiroshi Miyaoka

    2011-03-01

    Full Text Available The 40th Japanese Antarctic Research Expedition (JARE-40 wintering party, with 40 members, has successfully conducted the third-year project of the Vth five-year JARE program, over the period from 1st February 1999 to 31st January 2000, at Syowa Station, Antarctica.The framework of the JARE-40 wintering party program was the same as those of JARE-38 and JARE-39, comprising three routine observation programs and project/monitoring research observation programs in upper atmospheric physics, atmospheric sciences and glaciology, geophysics, and biology. In addition to many continuing projects, several new observations were started: 50MHz/112MHz aurora radars and a VLF wave receiver as part of the ionosphere program, aerosol sonde observations of Polar Stratospheric Clouds (PSCs as part of the meteorological program, HF/MF radars as part of the upper atmospheric physics program, frequent VLBI experiments as part of the geophysics program, and biological field surveys (including two dives, including monitoring of the undersea behavior of Weddell seals using bio-logging devices.In terms of inland field surveys, two parties were organized: fuel transportation and glaciological/meteorological observations along the route to Mizuho Station in August-September and to Dome Fuji/Yamato air-basecamp in November-January. These surveys involved snow sampling, precise GPS positioning, and sub-glacial surveys using three types of ice radar.Logistical activities, conducted in cooperation with the JARE-40 summer party, included the construction of a second summer lodge, the startup of a second 300 kVA generator and co-generator system, the development of a sewage plant, solar power panels, an access road to the A-heliport, and the cleanup of disused buildings. During the wintering period, efforts were directed towards the maintenance of all facilities at Syowa Station, safety management, and practical support for field operations.The Antarctic Environmental

  2. Antarctic Porifera database from the Spanish benthic expeditions

    Directory of Open Access Journals (Sweden)

    Pilar Rios

    2014-04-01

    Full Text Available The information about the sponges in this dataset is derived from the samples collected during five Spanish Antarctic expeditions: Bentart 94, Bentart 95, Gebrap 96, Ciemar 99/00 and Bentart 2003. Samples were collected in the Antarctic Peninsula and Bellingshausen Sea at depths ranging from 4 to 2044 m using va­rious sampling gears.The Antarctic Porifera database from the Spanish benthic expeditions is unique as it provides in­formation for an under-explored region of the Southern Ocean (Bellingshausen Sea. It fills an information gap on Antarctic deep-sea sponges, for which there were previously very few data.This phylum is an important part of the Antarctic biota and plays a key role in the structure of the Antarctic marine benthic community due to its considerable diversity and predominance in different areas. It is often a dominant component of Southern Ocean benthic communities.The quality of the data was controlled very thoroughly with GPS systems onboard the R/V Hesperides and by checking the data against the World Porifera Database (which is part of the World Register of Marine Species, WoRMS. The data are therefore fit for completing checklists, inclusion in biodivers­ity pattern analysis and niche modelling. The authors can be contacted if any additional information is needed before carrying out detailed biodiversity or biogeographic studies.The dataset currently contains 767 occurrence data items that have been checked for systematic reliability. This database is not yet complete and the collection is growing. Specimens are stored in the author’s collection at the Spanish Institute of Oceanography (IEO in the city of Gijón (Spain. The data are available in GBIF.

  3. Inspiring students through an authentic polar science expedition: the RESEt Project

    Science.gov (United States)

    Cattadori, Matteo

    2016-04-01

    RESEt (Research and Education Svalbard Experience www.resetsvalbard.it) is an ongoing educational project focusing mainly on polar and climate system topics. It started in 2014 and will end in 2017 with the high school diploma of the 22 students (16 y. o.) making the participant class. This class attend a school (Liceo Filzi, Rovereto, Trento. Italy) with a primary focus on disciplines like philosophy and education, rather then STEM (Science, Technology, Engineering, and Mathematics). Nevertheless their science curricula include climate topics that are rather challenging to grasp and, at the same time, crucial for their scientific citizenship. Some questions arise: How to foster their interest in geosciences topics? How to engage them in authentic scientific knowledge? How to increase their interest in scientific university courses during their post-secondary career? RESEt project will attempt to answer these questions through the development of integrated activities distributed over the last three years of their high school cycle. The most important moment will be an educational scientific expedition at the Svalbard, an archipelago located in the Arctic. The expedition be entirely organized, planned, and directed by students. In Svalbard, students will visit the main scientific facilities devoted to climate studies including those of Italian CNR (National Research Council) and they will perform some environmental measurement using data-loggers. Students are even involved in the fundraising process to raise more than ten thousand Euros needed to for travel expenses. This work is aimed mainly at presenting some of the preliminary data collected during the RESEt project, including the fundraising aspects. The management of the RESEt project strongly relies on the experience and network gained by the abstract author during the participation to the Education and Public Outreach (EPO) program of International Polar Year (IPY) 2007-2009 as well as the support of Polar

  4. Effects of an Arctic Ocean Ski Traverse on the Protective Capabilities of Expedition Footwear

    National Research Council Canada - National Science Library

    Endrusick, Thomas; Frykman, Peter; O'Brien, Catherine; Giblo, Joseph

    2005-01-01

    A traverse of the Arctic Ocean during a 2000-km unsupported ski expedition provided an opportunity to assess the impact of an extreme cold environment on the protective capabilities of a specialized footwear system (FS...

  5. ASTER Expedited L1A Reconstructed Unprocessed Instrument Data V003

    Data.gov (United States)

    National Aeronautics and Space Administration — The ASTER Expedited L1A Reconstructed Unprocessed Instrument Data is produced with the express purpose of providing the ASTER Science Team members and others, data...

  6. ASTER Expedited L1B Registered Radiance at the Sensor V003

    Data.gov (United States)

    National Aeronautics and Space Administration — The Expedited ASTER Level-1B Registered Radiance at the Sensor data set is produced with the express purpose of providing ASTER Science Team members data of their...

  7. Australian solar eclipse expeditions: the voyage to Cape York in 1871

    Science.gov (United States)

    Lomb, Nick

    2016-04-01

    Techniques such as photography and spectroscopy only became available to study solar eclipses in the 1860s. The first subsequent total eclipse of the Sun to be visible from Australia was one in December 1871 that was visible from far north Queensland. Initiated by the Royal Society of Victoria, astronomers in Melbourne and Sydney cooperated to organise the Australian Eclipse Expedition aboard the steamship Governor Blackall to a suitable observing location. Though on the day of the eclipse clouds prevented viewing, this was an important expedition that was complex to organise and involved dealings with colonial Governments and with relatively large sums of money that Australian scientists had not previously experienced. With a newspaper reporter as part of the expedition along with two photographers the expedition was well recorded and provides a clear insight into the activities of late nineteenth century astronomers and other scientists.

  8. Expediting Clinician Adoption of Safety Practices: The UCSF Venous Access Patient Safety Interdisciplinary Education Project

    National Research Council Canada - National Science Library

    Donaldson, Nancy E; Plank, Rosemary K; Williamson, Ann; Pearl, Jeffrey; Kellogg, Jerry; Ryder, Marcia

    2005-01-01

    ...) Venous Access Device (VAD) Patient Safety Interdisciplinary Education Project was to develop a 30-hour/one clinical academic unit VAD patient safety course with the aim of expediting clinician adoption of critical concepts...

  9. Investigating the role of virtual reality in geography via Google Expeditions

    OpenAIRE

    Tilling, Steve; Tudor, Ana-Despina; Kitchen, Becky; Minocha, Shailey

    2017-01-01

    This workshop-session explored the use of Google Expeditions (GEs), virtual reality-based field trips, to support and encourage outdoor fieldwork and facilitate visualisation of processes and locations. Participants had the opportunity to trial GEs and were invited to discuss and evaluate the outcomes (particularly the educator’s perspective) of a project investigating the role of virtual reality in geography education.\\ud \\ud We first showed several Expeditions to the educators, such as Rio ...

  10. Antarctic Starfish (Echinodermata, Asteroidea) from the ANDEEP3 expedition

    Science.gov (United States)

    Danis, Bruno; Jangoux, Michel; Wilmes, Jennifer

    2012-01-01

    Abstract This dataset includes information on sea stars collected during the ANDEEP3 expedition, which took place in 2005. The expedition focused on deep-sea stations in the Powell Basin and Weddell Sea. Sea stars were collected using an Agassiz trawl (3m, mesh-size 500µm), deployed in 16 stations during the ANTXXII/3 (ANDEEP3, PS72) expedition of the RV Polarstern. Sampling depth ranged from 1047 to 4931m. Trawling distance ranged from 731 to 3841m. The sampling area ranges from -41°S to -71°S (latitude) and from 0 to -65°W (longitude). A complete list of stations is available from the PANGAEA data system (http://www.pangaea.de/PHP/CruiseReports.php?b=Polarstern), including a cruise report (http://epic-reports.awi.de/3694/1/PE_72.pdf). The dataset includes 50 records, with individual counts ranging from 1-10, reaching a total of 132 specimens. The andeep3-Asteroidea is a unique dataset as it covers an under-explored region of the Southern Ocean, and that very little information was available regarding Antarctic deep-sea starfish. Before this study, most of the information available focused on starfish from shallower depths than 1000m. This dataset allowed to make unique observations, such as the fact that some species were only present at very high depths (Hymenaster crucifer, Hymenaster pellucidus, Hymenaster praecoquis, Psilaster charcoti, Freyella attenuata, Freyastera tuberculata, Styrachaster chuni and Vemaster sudatlanticus were all found below -3770m), while others displayed remarkable eurybathy, with very high depths amplitudes (Bathybiaster loripes (4842m), Lysasterias adeliae (4832m), Lophaster stellans (4752m), Cheiraster planeta (4708m), Eremicaster crassus (4626m), Lophaster gaini (4560m) and Ctenodiscus australis (4489m)). Even if the number of records is relatively small, the data bring many new insights on the taxonomic, bathymetric and geographic distributions of Southern starfish, covering a very large sampling zone. The dataset also brings

  11. Antarctic Starfish (Echinodermata, Asteroidea from the ANDEEP3 expedition

    Directory of Open Access Journals (Sweden)

    Bruno Danis

    2012-04-01

    Full Text Available This dataset includes information on sea stars collected during the ANDEEP3 expedition, which took place in 2005. The expedition focused on deep-sea stations in the Powell Basin and Weddell Sea.Sea stars were collected using an Agassiz trawl (3m, mesh-size 500µm, deployed in 16 stations during the ANTXXII/3 (ANDEEP3, PS72 expedition of the RV Polarstern. Sampling depth ranged from 1047 to 4931m. Trawling distance ranged from 731 to 3841m. The sampling area ranges from -41°S to -71°S (latitude and from 0 to -65°W (longitude. A complete list of stations is available from the PANGAEA data system (http://www.pangaea.de/PHP/CruiseReports.php?b=Polarstern, including a cruise report (http://epic-reports.awi.de/3694/1/PE_72.pdf.The dataset includes 50 records, with individual counts ranging from 1-10, reaching a total of 132 specimens.The andeep3-Asteroidea is a unique dataset as it covers an under-explored region of the Southern Ocean, and that very little information was available regarding Antarctic deep-sea starfish. Before this study, most of the information available focused on starfish from shallower depths than 1000m. This dataset allowed to make unique observations, such as the fact that some species were only present at very high depths (Hymenaster crucifer, Hymenaster pellucidus, Hymenaster praecoquis, Psilaster charcoti, Freyella attenuata, Freyastera tuberculata, Styrachaster chuni and Vemaster sudatlanticus were all found below -3770m, while others displayed remarkable eurybathy, with very high depths amplitudes (Bathybiaster loripes (4842m, Lysasterias adeliae (4832m, Lophaster stellans (4752m, Cheiraster planeta (4708m, Eremicaster crassus (4626m, Lophaster gaini (4560m and Ctenodiscus australis (4489m.Even if the number of records is relatively small, the data bring many new insights on the taxonomic, bathymetric and geographic distributions of Southern starfish, covering a very large sampling zone. The dataset also brings to light

  12. Antarctic Starfish (Echinodermata, Asteroidea) from the ANDEEP3 expedition.

    Science.gov (United States)

    Danis, Bruno; Jangoux, Michel; Wilmes, Jennifer

    2012-01-01

    This dataset includes information on sea stars collected during the ANDEEP3 expedition, which took place in 2005. The expedition focused on deep-sea stations in the Powell Basin and Weddell Sea.Sea stars were collected using an Agassiz trawl (3m, mesh-size 500µm), deployed in 16 stations during the ANTXXII/3 (ANDEEP3, PS72) expedition of the RV Polarstern. Sampling depth ranged from 1047 to 4931m. Trawling distance ranged from 731 to 3841m. The sampling area ranges from -41°S to -71°S (latitude) and from 0 to -65°W (longitude). A complete list of stations is available from the PANGAEA data system (http://www.pangaea.de/PHP/CruiseReports.php?b=Polarstern), including a cruise report (http://epic-reports.awi.de/3694/1/PE_72.pdf).The dataset includes 50 records, with individual counts ranging from 1-10, reaching a total of 132 specimens.The andeep3-Asteroidea is a unique dataset as it covers an under-explored region of the Southern Ocean, and that very little information was available regarding Antarctic deep-sea starfish. Before this study, most of the information available focused on starfish from shallower depths than 1000m. This dataset allowed to make unique observations, such as the fact that some species were only present at very high depths (Hymenaster crucifer, Hymenaster pellucidus, Hymenaster praecoquis, Psilaster charcoti, Freyella attenuata, Freyastera tuberculata, Styrachaster chuni and Vemaster sudatlanticus were all found below -3770m), while others displayed remarkable eurybathy, with very high depths amplitudes (Bathybiaster loripes (4842m), Lysasterias adeliae (4832m), Lophaster stellans (4752m), Cheiraster planeta (4708m), Eremicaster crassus (4626m), Lophaster gaini (4560m) and Ctenodiscus australis (4489m)).Even if the number of records is relatively small, the data bring many new insights on the taxonomic, bathymetric and geographic distributions of Southern starfish, covering a very large sampling zone. The dataset also brings to light six

  13. Gender, culture, and astrophysical fieldwork: Elizabeth Campbell and the Lick Observatory-Crocker eclipse expeditions.

    Science.gov (United States)

    Pang, A. S.-K.

    The article is organized as follows. It begins with an overview of women in nineteenth-century American science. It then describes the culture of mountaintop observatories and life on Mount Hamilton. Elizabeth Campbell's unique role in the Crocker-Lick expeditions drew upon her equally unique role in the observatory, and also on the meaning given to women's work in general on the mountain. The bulk of the article focuses on the Campbells and their expeditions to India in 1898, Spain in 1905, and the South Pacific in 1908. The third section compares the Lick Observatory expeditions to those conducted by David Todd of Amherst College. Todd's wife, Mabel Loomis Todd, went into the field several times with her husband, but her place in the field was radically different from Elizabeth Campbell's, a difference that can be ascribed to a combination of local culture and personality. Finally, it compares American expeditions to British expeditions of the period, to see what the absence of British women on expeditions can tell us about the way national scientific styles and cultures affected gender roles in science.

  14. The expedition to Peru and Chile (1777-1788): inventory of scientific production.

    Science.gov (United States)

    Bueno, A G; Rodríguez Nozal, R

    1996-01-01

    The aim of this work is to provide an inventory of the scientific corpus produced by the Spanish members of the Expedition to Peru and Chile (1777-1788). This material is divided into six large sections. The first section covers the different versions of the diary of the journey taken by the Expedition. The second section covers the drafts and workbooks used by the Expedition members for the writing of "Flora Peruviana et Chilensis," the manuscripts and published editions of this work, the materials used in the preparation of both the "Prodromus" and the "Systema Vegetabilium," the contributions of the assistants on the Expedition and some monographs of taxonomic interest. The third section is dedicated to quinological studies and other pharmacological works undertaken by Hipólito Ruiz López and José Pavón Jiménez. The fourth section includes the writings concerning Ruiz's dispute with Antonio José Cavanilles. The fifth section contains texts which set forth the botanical thought of the members of the Expedition. The sixth and final section includes the Expedition members' writings on various subjects, from anthropology and ethnography to others of a purely historical nature.

  15. DAN-IODP-SEIS Project

    DEFF Research Database (Denmark)

    Bendixen, Carina; Boldreel, Lars Ole; Jensen, Jørn Bo

    . The data will be integrated with already existing archive data. The data is to be processed and interpreted using state of the art interpretation software (Petrel). Seismic examples are shown to illustrate aspects of the geological development of the Kattegat. This PhD project is funded by Geocenter...... Denmark and is a collaboration project between IGN, GEUS and IGG. Further information regarding the cruise that took place in June-July will be available in issue no. 3 2013 of Geoviden....

  16. Antibacterial Compounds from Marine Vibrionaceae Isolated on a Global Expedition

    Directory of Open Access Journals (Sweden)

    Lone Gram

    2010-12-01

    Full Text Available On a global research expedition, over 500 bacterial strains inhibitory towards pathogenic bacteria were isolated. Three hundred of the antibacterial strains were assigned to the Vibrionaceae family. The purpose of the present study was to investigate the phylogeny and bioactivity of five Vibrionaceae strains with pronounced antibacterial activity. These were identified as Vibrio coralliilyticus (two strains, V. neptunius (two strains, and Photobacterium halotolerans (one strain on the basis of housekeeping gene sequences. The two related V. coralliilyticus and V. neptunius strains were isolated from distant oceanic regions. Chemotyping by LC-UV/MS underlined genetic relationships by showing highly similar metabolite profiles for each of the two V. coralliilyticus and V. neptunius strains, respectively, but a unique profile for P. halotolerans. Bioassay-guided fractionation identified two known antibiotics as being responsible for the antibacterial activity; andrimid (from V. coralliilyticus and holomycin (from P. halotolerans. Despite the isolation of already known antibiotics, our findings show that marine Vibrionaceae are a resource of antibacterial compounds and may have potential for future natural product discovery.

  17. Europa’s lost expedition a scientific novel

    CERN Document Server

    Carroll, Michael

    2017-01-01

    This classically styled, chilling murder mystery about an expedition under the ice of Jupiter’s ocean moon Europa, backed up by the latest scientific findings on this icy satellite. The science fiction premise explores real possibilities of exploring other bodies in the Solar System, including probing their possible astrobiology. Now that the most recent world war has concluded on Earth, human explorers are returning to exploration, carrying out a full-court press to journey into the alien abyss using tele-operated biorobotics and human-tended submersibles. Nine scientists head out to Jupiter’s icy ocean-moon. But at Europa’s most remote outpost, one by one, the team members who shared the cruise out begin to die under suspicious circumstances. All was well until humans begin diving into Europa’s subsurface ocean. The deaths have all the symptoms of some sort of plague, despite Europa’s seemingly sterile environment. Besides providing thrills, a science section covers the very latest in undersea rob...

  18. Sampling and Chemical Analysis of Potable Water for ISS Expeditions 12 and 13

    Science.gov (United States)

    Straub, John E. II; Plumlee, Deborah K.; Schultz, John R.

    2007-01-01

    The crews of Expeditions 12 and 13 aboard the International Space Station (ISS) continued to rely on potable water from two different sources, regenerated humidity condensate and Russian ground-supplied water. The Space Shuttle launched twice during the 12- months spanning both expeditions and docked with the ISS for delivery of hardware and supplies. However, no Shuttle potable water was transferred to the station during either of these missions. The chemical quality of the ISS onboard potable water supplies was verified by performing ground analyses of archival water samples at the Johnson Space Center (JSC) Water and Food Analytical Laboratory (WAFAL). Since no Shuttle flights launched during Expedition 12 and there was restricted return volume on the Russian Soyuz vehicle, only one chemical archive potable water sample was collected with U.S. hardware and returned during Expedition 12. This sample was collected in March 2006 and returned on Soyuz 11. The number and sensitivity of the chemical analyses performed on this sample were limited due to low sample volume. Shuttle flights STS-121 (ULF1.1) and STS-115 (12A) docked with the ISS in July and September of 2006, respectively. These flights returned to Earth with eight chemical archive potable water samples that were collected with U.S. hardware during Expedition 13. The average collected volume increased for these samples, allowing full chemical characterization to be performed. This paper presents a discussion of the results from chemical analyses performed on Expeditions 12 and 13 archive potable water samples. In addition to the results from the U.S. samples analyzed, results from pre-flight samples of Russian potable water delivered to the ISS on Progress vehicles and in-flight samples collected with Russian hardware during Expeditions 12 and 13 and analyzed at JSC are also discussed.

  19. Mission Specific Platforms: Past achievements and future developments in European led ocean research drilling.

    Science.gov (United States)

    Cotterill, Carol; McInroy, David; Stevenson, Alan

    2013-04-01

    Mission Specific Platform (MSP) expeditions are operated by the European Consortium for Ocean Research Drilling (ECORD). Each MSP expedition is unique within the Integrated Ocean Drilling Program (IODP). In order to complement the abilities of the JOIDES Resolution and the Chikyu, the ECORD Science Operator (ESO) must source vessels and technology suitable for each MSP proposal on a case-by-case basis. The result is that ESO can meet scientific requirements in a flexible manner, whilst maintaining the measurements required for the IODP legacy programme. The process of tendering within EU journals for vessels and technology means that the planning process for each MSP Expedition starts many years in advance of the operational phase. Involvement of proposal proponents from this early stage often leads to the recognition for technological research and development to best meet the scientific aims and objectives. One example of this is the planning for the Atlantis Massif proposal, with collaborative development between the British Geological Survey (BGS) and MARUM, University of Bremen, on suitable instruments for seabed drills, with the European Petrophysics Consortium (EPC) driving the development of suitable wireline logging tools that can be used in association with such seabed systems. Other technological developments being undertaken within the European IODP community include in-situ pressure sampling for gas hydrate expeditions, deep biosphere and fluid sampling equipment and CORK technology. This multi-national collaborative approach is also employed by ESO in the operational phase. IODP Expedition 302 ACEX saw vessel and ice management support from Russia and Sweden to facilitate the first drilling undertaken in Arctic sea ice. A review of MSP expeditions past, present and future reveal the significant impact of European led operations and scientific research within the current IODP programme, and also looking forward to the start of the new International

  20. Discoveries From the Cross-Disciplinary, Multi-Institutional South Seas Expedition from Hawaii to New Zealand and Back

    Science.gov (United States)

    Malahoff, A.; Wiltshire, J. C.; Smith, J. R.

    2005-12-01

    The Hawaii Undersea Research Laboratory organised an international research team to explore the chemistry, geology, biology, hydrothermal venting processes, mineral deposition, and biodiversity of seamounts extending south from Hawaii to New Zealand, including the submarine volcanoes of the Tonga-Kermadec Island Arc. Research team members came from a Consortium comprising of principal investigators from the NOAA Pacific Marine Environment Lab and VENTS program, the Inst of Geological and Nuclear Sciences and the National Inst of Water and Atmospheric Research both of New Zealand, the Univ of Kiel in Germany, the Univ of Mississippi, Univ of Hawaii, the NOAA Marine Fisheries Service, Scripps Institution of Oceanography, Univ of Oregon, Oregon State Univ, Stanford Univ, and the U.S. Fish and Wildlife Service. Funding came from the member organizations of the Consortium and the NOAA Office of Ocean Exploration and National Undersea Research Program. The expedition left Hawaii on 18 March 2005 and returned on 05 August, aboard the R/V Ka`imikai-o-Kanaloa with the submersibles Pisces IV and Pisces V and the ROV RCV-150. Sixty-one science dives were executed during the eight legs of the expedition. Twelve active volcanoes in the Samoa to New Zealand legs, one in the Samoan hot spot chain and the flanks of five islands and atolls on the legs between Samoa and Hawaii were investigated. Hundreds of specimens of new and unusual marine life, corals and other benthic organisms, extremophile micro- and macro-organisms, water samples for chemical analysis, polymetallic sulfides and rock samples were collected during the expedition. Unusual processes were observed at the Kermadec submarine volcanoes, including the oozing of liquid sulphur onto the seafloor and profuse carbon dioxide venting into seawater. Extensive submarine hydrothermal venting, black smoker activity and extraordinary chimney formations were studied in the caldera of Brothers Volcano. In addition, extensive

  1. North Slope (Wahluke Slope) expedited response action cleanup plan

    Energy Technology Data Exchange (ETDEWEB)

    1994-02-01

    The purpose of this action is to mitigate any threat to public health and the environment from hazards on the North Slope and meet the expedited response action (ERA) objective of cleanup to a degree requiring no further action. The ERA may be the final remediation of the 100-I-3 Operable Unit. A No Action record of decision (ROD) may be issued after remediation completion. The US Department of Energy (DOE) currently owns or administers approximately 140 mi{sup 2} (about 90,000 acres) of land north and east of the Columbia River (referred to as the North Slope) that is part of the Hanford Site. The North Slope, also commonly known as the Wahluke Slope, was not used for plutonium production or support facilities; it was used for military air defense of the Hanford Site and vicinity. The North Slope contained seven antiaircraft gun emplacements and three Nike-Ajax missile positions. These military positions were vacated in 1960--1961 as the defense requirements at Hanford changed. They were demolished in 1974. Prior to government control in 1943, the North Slope was homesteaded. Since the initiation of this ERA in the summer of 1992, DOE signed the modified Hanford Federal Agreement and Consent Order (Tri-Party Agreement) with the Washington Department of Ecology (Ecology) and the US Environmental Protection Agency (EPA), in which a milestone was set to complete remediation activities and a draft closeout report by October 1994. Remediation activities will make the North Slope area available for future non-DOE uses. Thirty-nine sites have undergone limited characterization to determine if significant environmental hazards exist. This plan documents the results of that characterization and evaluates the potential remediation alternatives.

  2. Development and validation of an expedited 10 g protein counter (EP-10) for dietary protein intake quantification.

    Science.gov (United States)

    Lim, Su-Lin; Lye, Jamie; Shen, Liang; Miller, Michelle; Chong, Yap-Seng

    2012-11-01

    Precise protein quantification is essential in clinical dietetics, particularly in the management of renal, burn, and malnourished patients. The expedited 10 g protein counter (EP-10) was developed to expedite the estimation of dietary protein for nutritional assessment and recommendation. The main objective of this study was to compare the validity and efficacy of the EP-10 with the American Dietetic Association's "Exchange List for Meal Planning" (ADA-7 g) in quantifying dietary protein intake, against computerized nutrient analysis (CNA). Protein intake of 197 food records kept by healthy adult subjects in Singapore was determined thrice using 3 different methods: (1) EP-10, (2) ADA-7 g, and (3) CNA using SERVE program (Version 4.0). Assessments using the EP-10 and ADA-7 g were performed by 2 assessors in a blind crossover manner while a third assessor performed the CNA. All assessors were blind to each other's results. Time taken to assess a subsample (n = 165) using the EP-10 and ADA-7 g was also recorded. Mean difference in protein intake quantification when compared with the CNA was statistically nonsignificant for the EP-10 (1.4 ± 16.3 g, P = .239) and statistically significant for the ADA-7 g (-2.2 ± 15.6 g, P = .046). Both the EP-10 and ADA-7 g had clinically acceptable agreement with the CNA, as determined via Bland-Altman plots, although it was found that EP-10 had a tendency to overestimate with protein intakes above 150 g. The EP-10 required significantly less time for protein intake quantification than the ADA-7 g (mean time of 65 ± 36 seconds vs. 111 ± 40 seconds, P valid clinical tools for protein intake quantification in an Asian context, with EP-10 being more time efficient. However, a dietician's discretion is needed when the EP-10 is used on protein intakes above 150 g. Copyright © 2012 National Kidney Foundation, Inc. All rights reserved.

  3. [The real philanthropic expedition of the smallpox vaccine: monarchy and modernity in 1803].

    Science.gov (United States)

    Rigau-Pérez, José G

    2004-09-01

    Smallpox resulted in the death of 30 % of those who acquired it, so the preventive method discovered by Edward Jenner (London, 1798) spread very quickly. At the request in 1803 of Carlos IV, king of Spain, his government evaluated offers to carry smallpox vaccine to the colonies. The selected proposal, by doctor Francisco Xavier de Balmis, sought to take the lymph to America and Asia in a chain of arm to arm vaccination of foundlings. The Expedition set sail from Corunna on November 30, 1803, stopped in the Canary Isles, Puerto Rico, and Venezuela and after Caracas (1804) split in two groups. Balmis led some members of the Expedition to Cuba and Mexico. For the trip to the Philippines, in 1805, parents lent their children in exchange for economic compensation and the promise that the boys would be returned home. The Expedition returned to Mexico in August, 1807, but Balmis separately took vaccine to China and returned to Spain. Another contingent of the Expedition, under vice-director José Salvany, took vaccine to what we know as Colombia, Ecuador, Peru and Bolivia. His assistant Manuel Grajales reached the Chilean Patagonia in 1811. This article also comments on three principal themes - the institutional management of the scientific project, the conflicts that characterized its course, and the children's experience. The Vaccine Expedition was a brave and humanitarian endeavor, but also an extraordinary sanitary and administrative success. It was not until the twentieth century that a global eradication campaign eliminated smallpox in the world.

  4. Revisiting J.M. Gilliss' astronomical expedition to Chile in 1849‒1852

    Science.gov (United States)

    Hermosilla, Germán Hidalgo

    2017-08-01

    Between 1849 and 1852 the U.S. astronomer J.M. Gilliss led an expedition to Santiago, Chile, aimed at improving the accepted value for the solar parallax. Although this particular research project was not a success, the astronomers did make other useful astronomical contributions, and the expedition was the catalyst that led directly to the founding of the Chilean National Observatory. Meanwhile, Gilliss later went on to achieve further prominence as Superintendent of the U.S. Naval Observatory in Washington, D.C. The results of the Chilean expedition were published by Gilliss in a six-volume work titled The U.S. Naval Astronomical Expedition to the Southern Hemisphere during the Years 1849-50-51-52 that was issued over a 40-year period. In Volume I (published in 1855) Gilliss presented a 'warts-and-all' account of Chile, its politics and its people, which at the time—and subsequently—created considerable controversy. In this paper, after briefly reviewing Gilliss' Southern Hemisphere expedition we focus on the extensive non-astronomical narrative that Gilliss presents in this first volume.

  5. Expedition Earth and Beyond: Using NASA Data Resources and Integrated Educational Strategies to Promote Authentic Research in the Classroom

    Science.gov (United States)

    Graffi, Paige Valderrama; Stefanov, William; Willis, Kim; Runco, Sue

    2009-01-01

    Teachers in today s classrooms are bound by state required skills, education standards, and high stakes testing. How can they gain skills and confidence to replace units or individual activities with curriculum that incorporates project and inquiry-based learning and promotes authentic research in the classroom? The key to promoting classroom authentic research experiences lies in educator professional development that is structured around teacher needs. The Expedition Earth and Beyond Program is a new geosciences program based at the NASA Johnson Space Center designed to engage, inspire and educate teachers and students in grades 5-14. The program promotes authentic research experiences for classrooms and uses strategies that will help NASA reach its education goals while still allowing educators to teach required standards. Teachers will have access to experts in terrestrial and planetary remote sensing and geoscience; this will enhance their use of content, structure, and relevant experiences to gain the confidence and skills they need to actively engage students in authentic research experiences. Integrated and powerful educational strategies are used to build skills and confidence in teachers. The strategies are as follows: 1) creating Standards-aligned, inquiry-based curricular resources as ready-to-use materials that can be modified by teachers to fit their unique classroom situation; 2) providing ongoing professional development opportunities that focus on active experiences using curricular materials, inquiry-based techniques and expanding content knowledge; 3) connecting science experts to classrooms to deepen content knowledge and provide relevance to classroom activities and real world applications; 4) facilitating students sharing research with their peers and scientists reinforcing their active participation and contributions to research. These components of the Expedition Earth and Beyond Education Program will be enhanced by providing exciting and

  6. Microarray Я US: a user-friendly graphical interface to Bioconductor tools that enables accurate microarray data analysis and expedites comprehensive functional analysis of microarray results

    Directory of Open Access Journals (Sweden)

    Dai Yilin

    2012-06-01

    Full Text Available Abstract Background Microarray data analysis presents a significant challenge to researchers who are unable to use the powerful Bioconductor and its numerous tools due to their lack of knowledge of R language. Among the few existing software programs that offer a graphic user interface to Bioconductor packages, none have implemented a comprehensive strategy to address the accuracy and reliability issue of microarray data analysis due to the well known probe design problems associated with many widely used microarray chips. There is also a lack of tools that would expedite the functional analysis of microarray results. Findings We present Microarray Я US, an R-based graphical user interface that implements over a dozen popular Bioconductor packages to offer researchers a streamlined workflow for routine differential microarray expression data analysis without the need to learn R language. In order to enable a more accurate analysis and interpretation of microarray data, we incorporated the latest custom probe re-definition and re-annotation for Affymetrix and Illumina chips. A versatile microarray results output utility tool was also implemented for easy and fast generation of input files for over 20 of the most widely used functional analysis software programs. Conclusion Coupled with a well-designed user interface, Microarray Я US leverages cutting edge Bioconductor packages for researchers with no knowledge in R language. It also enables a more reliable and accurate microarray data analysis and expedites downstream functional analysis of microarray results.

  7. Microarray Я US: a user-friendly graphical interface to Bioconductor tools that enables accurate microarray data analysis and expedites comprehensive functional analysis of microarray results.

    Science.gov (United States)

    Dai, Yilin; Guo, Ling; Li, Meng; Chen, Yi-Bu

    2012-06-08

    Microarray data analysis presents a significant challenge to researchers who are unable to use the powerful Bioconductor and its numerous tools due to their lack of knowledge of R language. Among the few existing software programs that offer a graphic user interface to Bioconductor packages, none have implemented a comprehensive strategy to address the accuracy and reliability issue of microarray data analysis due to the well known probe design problems associated with many widely used microarray chips. There is also a lack of tools that would expedite the functional analysis of microarray results. We present Microarray Я US, an R-based graphical user interface that implements over a dozen popular Bioconductor packages to offer researchers a streamlined workflow for routine differential microarray expression data analysis without the need to learn R language. In order to enable a more accurate analysis and interpretation of microarray data, we incorporated the latest custom probe re-definition and re-annotation for Affymetrix and Illumina chips. A versatile microarray results output utility tool was also implemented for easy and fast generation of input files for over 20 of the most widely used functional analysis software programs. Coupled with a well-designed user interface, Microarray Я US leverages cutting edge Bioconductor packages for researchers with no knowledge in R language. It also enables a more reliable and accurate microarray data analysis and expedites downstream functional analysis of microarray results.

  8. An Exploration of Canadian Identity in Recent Literary Narratives of the Franklin Expeditions

    Directory of Open Access Journals (Sweden)

    Victor Kennedy

    2006-06-01

    Full Text Available Sir John Franklin’s three expeditions to the high Arctic in 1819, 1825, and 1845 have become the stuff of Canadian legend, enshrined in history books, songs, short stories, novels, and web sites. Franklin set out in 1845 to discover the Northwest Passage with the most advanced technology the British Empire could muster, and disappeared forever. Many rescue explorations found only scant evidence of the Expedition, and the mystery was finally solved only recently. This paper will explore four recent fictional works on Franklin’s expeditions, Stan Rogers’ song “Northwest Passage”, Margaret Atwood’s short story “The Age of Lead”, Rudy Wiebe’s A Discovery of Strangers, and John Wilson’s North with Franklin: the Lost Journals of James Fitzjames, to see how Franklin’s ghost has haunted the hopes and values of nineteenth-century, as well as modern, Canada.

  9. The social event of the season. Solar eclipse expeditions and Victorian culture.

    Science.gov (United States)

    Pang, A. S.-K.

    1993-06-01

    The purpose of this article is to examine the construction of eclipse expeditions in Victorian and Edwardian Britain. (American expeditions will also be discussed to highlight national styles in organization and fieldwork.) The author begins by examining how expeditions were planned and how choices about observing sites, observers, and travel plans were made. He then follows parties out into the field. He argues that eclipse expeditons were powerfully affected by the practices and culture of tourism and were further shaped by expectations surrounding the encounter of "civilized" and "uncivilized" peoples. Finally, the author examines the crafting of observing practices used during totality. The evolution of astrophotography, the rise of big instruments, and battles between amateurs and professionals all had their effect on eclipse observation, but a close examination of observing practices and instrument design will show that the tools of empire were as important as cameras and telescopes for the production of reliable knowledge about the Sun.

  10. On the Turn of Two Millennia (60 Years of the Mari Archaeological Expedition

    Directory of Open Access Journals (Sweden)

    Nikitin Valeriy V.,

    2017-03-01

    Full Text Available The article is dedicated to the 60th Anniversary of the Mari Archaeological Expedition and summarizes the two decades of its studies (1996-2016 into the early cultures of the Mari region, starting from the era of the original settlement (Mesolithic, through the Neolithic-Eneolithic, Bronze Age, Early Iron Age and up to the Middle Ages. The expedition studied stations and settlements of primitive cultures, as well as unfortified and fortified settlements and necropolises. Special studies focused on formation and development of the early Mari culture, as well as the material and spiritual culture of the medieval Mari. The expedition continues its survey exploration in order to identify new archaeological sites. During the reported period, twelve monographs were published and three monographs prepared based on the expedition’s materials.

  11. Not Just About the Science: Cold War Politics and the International Indian Ocean Expedition

    Science.gov (United States)

    Harper, K.

    2016-12-01

    The International Indian Ocean Expedition broke ground for a series of multi-national oceanographic expeditions starting in the late 1950s. In and of itself, it would have been historically significant—like the International Geophysical Year (1957-58)—for pulling together the international scientific community during the Cold War. However, US support for this and follow-on Indian Ocean expeditions were not just about the science; they were also about diplomacy, specifically efforts to bring non-aligned India into the US political orbit and out of the clutches of its Cold War enemy, the Soviet Union. This paper examines the behind-the-scenes efforts at the highest reaches of the US government to extract international political gain out of a large-scale scientific effort.

  12. Temperature and salinity profile data from CTD casts from the icebreaker ODEN during the Lomonosov Ridge off Greenland (LOMROG) expedition in 2007 (NODC Accession 0093533)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The CTD data were taken during the expedition "Lomonosov Ridge off Greenland" (LOMROG) in summer 2007 with the Swedish icebreaker Oden. The LOMROG expedition...

  13. 15 CFR 27.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-01-01

    ... HUMAN SUBJECTS § 27.110 Expedited review procedures for certain kinds of research involving no more than... 15 Commerce and Foreign Trade 1 2010-01-01 2010-01-01 false Expedited review procedures for certain kinds of research involving no more than minimal risk, and for minor changes in approved research...

  14. 40 CFR 26.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-07-01

    ... EPA § 26.110 Expedited review procedures for certain kinds of research involving no more than minimal... 40 Protection of Environment 1 2010-07-01 2010-07-01 false Expedited review procedures for certain kinds of research involving no more than minimal risk, and for minor changes in approved research. 26...

  15. 45 CFR 46.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-10-01

    ... SUBJECTS Basic HHS Policy for Protection of Human Research Subjects § 46.110 Expedited review procedures... list of categories of research that may be reviewed by the IRB through an expedited review procedure... reviewers may not disapprove the research. A research activity may be disapproved only after review in...

  16. 34 CFR 97.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-07-01

    ...) § 97.110 Expedited review procedures for certain kinds of research involving no more than minimal risk... 34 Education 1 2010-07-01 2010-07-01 false Expedited review procedures for certain kinds of research involving no more than minimal risk, and for minor changes in approved research. 97.110 Section 97...

  17. 7 CFR 1c.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-01-01

    ... review procedures for certain kinds of research involving no more than minimal risk, and for minor... an expedited review procedure shall adopt a method for keeping all members advised of research... 7 Agriculture 1 2010-01-01 2010-01-01 false Expedited review procedures for certain kinds of...

  18. 38 CFR 16.110 - Expedited review procedures for certain kinds of research involving no more than minimal risk...

    Science.gov (United States)

    2010-07-01

    ... AFFAIRS PROTECTION OF HUMAN SUBJECTS § 16.110 Expedited review procedures for certain kinds of research... 38 Pensions, Bonuses, and Veterans' Relief 1 2010-07-01 2010-07-01 false Expedited review procedures for certain kinds of research involving no more than minimal risk, and for minor changes in...

  19. Studioantarctica: Embedding Art in a Geophysics Sea Ice Expedition

    Science.gov (United States)

    O'Connor, Gabby; Stevens, Craig

    2017-04-01

    Here we report on a six year collaboration developing new modes of communication using the interconnections between art and science in the context of climate science. We use the polar regions as a context for the collaboration in part because it holds a special place in the imaginations of many people. Not only is it is a part of the planet likely to be never visited be the viewer but there is a growing understanding of the role the poles play in the planet's climate. Motivated by the potential for cross-disciplinary outcomes, an artist was embedded in a science expedition to the fast sea ice around Antarctica. Both the science and art focused on ice crystal formation. Most elements of the art process had three phases, pre, during and post - as with the science. The environment largely dominated the progress and evolution of ideas. The results were multi-material and multiscale and provide a way to entrain a wide range of audiences, while also making non-didactic connections around global climate - and producing art. This built on a continuum of approaches where we have evolved from consideration and debate about synergies in approach, through to cross-fertilisation of ideas, shared labour, trial remote controlling and finally shared field experimentation. Certainly this is ground-breaking in an academic sense, but beyond this, it is proving a powerful attractor in engaging primary school students. In a class room setting we describe our work and experiences, both separately and in combination, as well as our recent experiences seeking to bridge the disciplinary divide. We then ask the students to contribute to the process of creating science-inspired art. There are complementary perspectives on the evolving process, their associated communication strands and how this drives a suite of communication and education outcomes. The need to understand how these systems are changing as the human species modifies its planet is urgent. Science around the connection between

  20. Medical supplies for the expeditions of the heroic age of Antarctic exploration: introduction.

    Science.gov (United States)

    Guly, H R

    2012-06-01

    During the heroic age of Antarctic exploration (1895-1922) there were at least 18 expeditions to the Antarctic lasting between 18 and 30 months. This is an introduction to a series of articles about the drugs taken and used in the Antarctic at this time. Most of the information relates to the expeditions of Robert Scott and Ernest Shackleton and the main supplier of medical equipment was Burroughs Wellcome and Co. This article also describes the medical cases that were taken to the Antarctic.

  1. Expeditions to Komsomolets in 1993 and 1994; Tokt til Komsomolets i 1993 og 1994

    Energy Technology Data Exchange (ETDEWEB)

    Kolstad, A.K.

    1995-09-01

    The Russian nuclear submarine Komsomolets went down about 180 km southwest of the Bear Island in the Norwegian Sea on April 7, 1989. According to Russian information the submarine contains one nuclear reactor and two torpedoes with nuclear warheads. The Norwegian Radiation Protection Authority has taken part in the Russian expeditions to the accident site since 1991. This is a report from the expeditions in 1993 and 1994. It includes sampling, analysis and results obtained by the Norwegian part. 5 refs., 4 figs., 5 tabs.

  2. The Visible Empire: The Expert View and Images in the Scientific Expeditions of the Enlightenment

    Directory of Open Access Journals (Sweden)

    Daniela BLEICHMAR

    2010-06-01

    Full Text Available This essay examines the Spanish natural history expeditions to Latin America in the late 18th Century —particularly the Real Expedición Botánica a Nueva Granada, directed by José Celestino Mutis— as an approach to an analysis of the importance of visual culture in European natural history, especially in imperial contexts. It explains the connections between economic botany and taxonomic botany, and highlights the role of visual epistemology in bringing them together. It proposes that the scientific expeditions constituted visualization projects that, through the circulation of images and collections, transformed locally rooted natures into global natures in motion.

  3. Expedition Earth and Beyond: Engaging Classrooms in Student-Led Research Using NASA Data, Access to Scientists, and Integrated Educational Strategies

    Science.gov (United States)

    Graff, P. V.; Stefanov, W. L.; Willis, K. J.; Runco, S.; McCollum, T.; Baker, M.; Lindgren, C.; Mailhot, M.

    2011-01-01

    Classroom teachers are challenged with engaging and preparing today s students for the future. Activities are driven by state required skills, education standards, and high-stakes testing. Providing educators with standards-aligned, inquiry-based activities that will help them engage their students in student-led research in the classroom will help them teach required standards, essential skills, and help inspire their students to become motivated learners. The Astromaterials Research and Exploration Science (ARES) Education Program, classroom educators, and ARES scientists at the NASA Johnson Space Center created the Expedition Earth and Beyond education program to help teachers promote student-led research in their classrooms (grades 5-14) by using NASA data, providing access to scientists, and using integrated educational strategies.

  4. Silent film: The Carlsberg Foundation’s Oceanographic Expedition Round the World, 1928–30

    DEFF Research Database (Denmark)

    Poulsen, Bo

    2016-01-01

    Danish marine scientist, Johannes Schmidt was also a pioneer when it comes to popularizing deep-sea marine research through the use of mass media. When Schmidt headed the Carlsberg Foundation’s Oceanographical Expedition Round the World, 1928-1930, he brought along a film camera, documenting...

  5. Seaweeds of the Snellius-II Expedition. Chlorophyta: Caulerpales (except Caulerpa and Halimeda)

    NARCIS (Netherlands)

    Coppejans, E.; Prud’homme van Reine, W.F.

    1989-01-01

    In the present paper a survey is given of species belonging to the genera Avrainvillea, Chlorodesmis, Rhipilia, Rhipiliopsis, Tydemania, and Udotea collected during the Indonesian-Dutch Snellius- II Expedition (1984) in the Banda, Sawu and Flores Seas. The morphology and anatomy of these seaweeds

  6. Chitons (Mollusca: Polyplacophora) procured by the CANCAP I-VII expeditions, 1976-86

    NARCIS (Netherlands)

    Kaas, P.

    1991-01-01

    The 327 specimens of chitons captured during six out of seven CANCAP Expeditions have been examined. They belong to 26 species, including two recently described ones: Ischnochiton (Stenosemus) substriatus Kaas & Van Belle, 1990 and Ischnochiton (Ischnochiton nicklesi Kaas & Van Belle, 1990.

  7. 42 CFR 405.1206 - Expedited determination procedures for inpatient hospital care.

    Science.gov (United States)

    2010-10-01

    ... Hospital Discharges § 405.1206 Expedited determination procedures for inpatient hospital care. (a... discharge, or at any time for good cause. The QIO will issue a decision in accordance with paragraph (d)(6... hospital to demonstrate that discharge is the correct decision, either on the basis of medical necessity...

  8. 77 FR 10774 - Silicon Metal From China; Scheduling of an Expedited Five-Year Review

    Science.gov (United States)

    2012-02-23

    ... From the Federal Register Online via the Government Publishing Office ] INTERNATIONAL TRADE COMMISSION Silicon Metal From China; Scheduling of an Expedited Five-Year Review AGENCY: United States...)) (the Act) to determine whether revocation of the antidumping duty order on silicon metal from China...

  9. 77 FR 43492 - Expedited Vocational Assessment Under the Sequential Evaluation Process

    Science.gov (United States)

    2012-07-25

    ... use the same assessment of your residual functional capacity at step five of the sequential evaluation... ADMINISTRATION 20 CFR Parts 404 and 416 RIN 0960-AH26 Expedited Vocational Assessment Under the Sequential Evaluation Process AGENCY: Social Security Administration. ACTION: Final rules. SUMMARY: We are revising our...

  10. 76 FR 56357 - Expedited Vocational Assessment Under the Sequential Evaluation Process

    Science.gov (United States)

    2011-09-13

    ... assessment of your residual functional capacity at step five of the sequential evaluation process to decide... ADMINISTRATION 20 CFR Parts 404 and 416 RIN 0960-AH26 Expedited Vocational Assessment Under the Sequential Evaluation Process AGENCY: Social Security Administration. ACTION: Notice of proposed rulemaking (NPRM...

  11. Species of Caulerpa (Chlorophyceae) collected on the International Indian Ocean Expedition

    NARCIS (Netherlands)

    Taylor, Wm. Randolph

    1967-01-01

    One of the major scientific efforts of the decade has been the International Indian Ocean Expedition of 1960—64, involving several institutions and ships and numerous scientists. With an oceanographic focus, not only physical and biological open sea oceanographic studies were carried on, but

  12. Expedition agroparks : research by design into sustainable development and agriculture in network society

    NARCIS (Netherlands)

    Smeets, P.J.A.M.

    2010-01-01

    This book is the result of several years of expedition into the development of metropolitan FoodClusters. The authors fascination for the agricultural landscapes in and around metropolises led him to the conclusion that improving the efficiency of agriculture is the most effective way to safeguard

  13. 77 FR 33254 - Expediting Transition of Government Performed and Sponsored Aeronautics Research and Development

    Science.gov (United States)

    2012-06-05

    ... TECHNOLOGY POLICY Expediting Transition of Government Performed and Sponsored Aeronautics Research and... improve future national aeronautics R&D plans and progress assessments, the Council seeks public comment on the utility of certain national aeronautics R&D planning documents for providing transparency of...

  14. 75 FR 8745 - Expedited Review Scheduling Notice; Hand Trucks and Certain Parts Thereof From China

    Science.gov (United States)

    2010-02-25

    ... COMMISSION Expedited Review Scheduling Notice; Hand Trucks and Certain Parts Thereof From China AGENCY... concerning the antidumping duty order on hand trucks and certain parts thereof from China. SUMMARY: The... duty order on hand trucks and certain parts thereof from China would be likely to lead to continuation...

  15. Results of the CERPOLEX/Mammuthus Expeditions on the Taimyr Peninsula, Arctic Siberia, Russian Federation

    NARCIS (Netherlands)

    Mol, D.; Tikhonov, A.; van der Plicht, J.; Kahlke, R.D.; Debruyne, R.; van Geel, B.; van Reenen, G.B.A.; Pals, J.P.; de Marliave, C.; Reumer, J.W.F.

    2006-01-01

    Abstract During a series of expeditions organized by CERPOLEX/Mammuthus to the Taimyr region in northern Siberia several mammoth (Mammuthus primigenius) carcasses were discovered and subsequently excavated and studied. The oldest specimen is the Arilakh Mammoth (ca. 55,800 BP). Much younger are the

  16. Results of the CERPOLEX/Mammuthus expeditions on the Taimyr peninsula, Arctic Siberia, Russian federation

    NARCIS (Netherlands)

    Mol, D; Tikhonov, A; van der Plicht, J; Kahlke, RD; Debruyne, R; van Geel, B; van Reenen, G; Pals, JP; de Marliave, C; Reumer, JWF; Kahlke, Ralf-Dietrich; Pals, Jan Peter; Reumer, Jelle W.F.

    During a series of expeditions organized by CERPOLEX/Mammuthus to the Taimyr region in northern Siberia several mammoth (Mammuthus primigenius) carcasses were discovered and subsequently excavated and studied. The oldest specimen is the Arilakh Mammoth (ca. 55,800 BP). Much younger are the Jarkov

  17. 76 FR 30176 - Expedited Review for New Animal Drug Applications for Human Pathogen Reduction Claims; Withdrawal...

    Science.gov (United States)

    2011-05-24

    ... animal drug applications, in support of the review of animal drug products. As a result of these... From the Federal Register Online via the Government Publishing Office DEPARTMENT OF HEALTH AND HUMAN SERVICES Food and Drug Administration (Formerly Docket No. 2001D-0107) Expedited Review for New...

  18. Satellite Eye for the Galathea 3 ship expedition: Global tour 2006-2007

    DEFF Research Database (Denmark)

    Hasager, Charlotte Bay; Badger, Merete; Sørensen, Peter

    2007-01-01

    Islands, New Zealand, Antarctica, Chile, Galapagos, the Caribbean, the Northeastern USA and finishing in Denmark 25 April 2007. During the entire expedition satellite images were ordered along the ship track, downloaded, processed, archived and used for education. The satellite images are displayed...

  19. 76 FR 78694 - Fresh Garlic From China; Scheduling of an expedited five-year review

    Science.gov (United States)

    2011-12-19

    ... COMMISSION Fresh Garlic From China; Scheduling of an expedited five-year review AGENCY: United States...)) (the Act) to determine whether revocation of the antidumping duty order on fresh garlic from China... Commission has found the response submitted by the Fresh Garlic Producers Association and its individual...

  20. Starvation Resulting From Inadequate Dietary Planning for a 50-Day Rowing Expedition.

    Science.gov (United States)

    Reid, Hamish A B; Dennison, Nicholas C; Quayle, Jonathan; Preston, Tom

    2017-09-01

    Meeting the energy demands of prolonged arduous expeditions and endurance sport may be a significant barrier to success. Expedition rowing is associated with high levels of body-mass loss, reflecting the challenge of meeting energy expenditure in this exacting environment. To use the doubly labeled water (DLW) technique to calculate the total energy expenditure (TEE) and body-composition changes of two 28-y-old healthy male athletes during a 50-d continuous and unsupported row around Great Britain. A measured dose of DLW was taken at the start of 2 separate study periods (days 5-19 and 34-48) followed by sequential urine collection, which was analyzed on return to land. Mean TEE was 15.3 MJ/d: athlete 1, 16.4 MJ/d; athlete 2, 14.9 MJ/d. Athlete 1 lost 11.2 kg and athlete 2 lost 14.9 kg of body mass during the row. Average energy provision was 19.1 MJ per 24-h ration pack. These results highlight the difficulty of maintaining energy balance during expedition rowing. A starvation state was observed despite dietary provision in excess of estimated energy expenditure, indicating that nutritional strategy rather than caloric availability was at fault. The authors recommend that future expeditions prioritize thorough testing and the individualization of rations to ensure that they are both palatable and practical during the weeks to months at sea.

  1. MITAS-2009 Expedition, U.S. Beaufort Shelf and Slope—Lithostratigraphy Data Report

    Energy Technology Data Exchange (ETDEWEB)

    Rose, K.; Johnson, J.E.; Phillips, S.C.; Smith, J.; Reed, A.; Disenhof, C.; Presley, J.

    2012-09-17

    The volume of methane released through the Arctic Ocean to the atmosphere and its potential role in the global climate cycle have increasingly become the focus of studies seeking to understand the source and origin of this methane. In 2009, an international, multi-disciplinary science party aboard the U.S. Coast Guard icebreaker Polar Sea successfully completed a trans-U.S. Beaufort Shelf expedition aimed at understanding the sources and volumes of methane across this region. Following more than a year of preliminary cruise planning and a thorough site evaluation, the Methane in the Arctic Shelf/Slope (MITAS) expedition departed from the waters off the coast of Barrow, Alaska in September 2009. The expedition was organized with an international shipboard science team consisting of 33 scientists with the breadth of expertise necessary to meet the expedition goals. NETL researchers led the expedition’s initial core processing and lithostratigraphic evaluations, which are the focus of this report. This data report is focused on the lithostratigraphic datasets from the recovered vibra cores and piston cores. Operational information about the piston and vibra cores such as date acquired, core name, total length, water depth, and geographic location is provided. Once recovered, gas samples were immediately collected from cores. In addition, each core was run through the Geotek multi-sensor core logger for magnetic susceptibility, P-wave velocity, resistivity, and gamma-density measurements (Rose et al., 2010). After the samples and measurements were completed, the cores were split into working and archive halves. Visual core descriptions of the archive half was completed for each core. Samples for shipboard smear slides, coarse fractions, and XRD analyses were collected, as well as corresponding samples for post-cruise grain size analysis from the working half of each core. Line scan images of the split core surfaces were collected post-expedition. The methods used to

  2. Framing the Arctic: Reconsidering Roald Amundsen’s Gjøa Expedition Imagery

    Directory of Open Access Journals (Sweden)

    Ingeborg Høvik

    2015-04-01

    Full Text Available In 1906 Roald Amundsen’s Gjøa Expedition returned to Norway after three years in the Arctic. The first to complete a Northwest Passage by sea, the expedition also brought back a substantial amount of ethnographic material concerning the Netsilik Inuit, with whom Amundsen and his crew had been in sustained contact during their stay on King William Island in Nunavut between 1903 and 1905. This material included a large number of photographs, forty-two of which were included as illustrations in his expedition narrative, titled Nordvest-passagen and first released in Norwegian in 1907. Focusing on a selection of published and unpublished photographs from Amundsen’s voyage and their interrelationships, this article examines the degree to which the Gjøa Expedition’s use of photography formed part of a planned project that intersected with anthropological concerns and practices of its time. My purpose is further to demonstrate that there is a discernible change in the representation of indigeneity that occurs when particular photographs were selected and then contextually reframed as illustrations in Nordvest-passagen. On the one hand, the extensive body of photographs taken in the field elaborates the close interaction between crew and Inuit recorded in Amundsen’s personal diary and published narrative, testifying to the existence of an active and dynamic contact zone. In this regard, the original photographs could arguably be read as a dialogic portrayal of the unique individuals Amundsen’s crew met while in the Arctic. On the other hand, a peculiar distancing seems to have taken place as the Gjøa Expedition’s photographs were selected and reproduced as illustrations for Amundsen’s expedition narrative. Likely connected to a desire to match his expedition narrative to existing scientific visual and literary conventions, this shift suggests Amundsen’s attempts through textual and visual means to deny the Netsilik Inuit

  3. [The journey of the vaccine against smallpox: one expedition, two oceans, three continents, and thousands of children].

    Science.gov (United States)

    Tuells, José; Duro-Torrijos, José Luis

    2015-01-01

    Spain encouraged, during the Bourbon dynasty, the formation of scientific expeditions, among which was the Royal Philanthropic Vaccine Expedition, an example of biopolitics applied by the state in order to protect health. The expedition went all over the world, using children as a reservoir to transport the vaccine fluid. Francisco Xavier Balmis established a human chain that arm-to-arm materialized the success of the mission. The characteristics and difficulties which children had to pass through and their contribution to the spread of the smallpox vaccine are analyzed.

  4. Activities of the summer operations of the 43rd Japanese Antarctic Research Expedition (JARE-43 in 2001-2002

    Directory of Open Access Journals (Sweden)

    Fumihiko Nishio

    2013-03-01

    Full Text Available The activities in the 2001-2002 austral summer of the 43rd Japanese Antarctic Research Expedition (JARE-43 are reported. JARE-43 consisted of 60 personnel including 20 summer and 40 wintering personnel. In addition, 7 observers joined the voyage of R/V Shirase. She left Harumi on Nov. 14 in 2001, and the 56 personel and 7 observers went on boad in Freemantle of Western Australia for Syowa Station, other 4 personel for another ship as mentioned below. R/V Shirase left the ground on Dec. 3 and arrived at the ice edge on Dec. 14, after carrying out marine observations on the cruise. She anchored at Syowa Station on Dec. 23, after the first flight on Dec. 18. All the cargo and fuel necessary for the wintering program of JARE-43 were unloaded and the missions for the summer party were forced to finish by the last flight on Feb. 12 in 2002. The helicopter, chartered by JARE-43, moved to Syowa Station from R/V Shirase on Dec. 23 and supported the observation programs until Feb. 3, including the inland areas of ice sheets. The observation on the Mizuho Ice Plateau for the seismic exploration programs was especially supported by air during the traverse. Constructions with engineering works and facilities update were conducted in the several areas in Syowa Station, and most of them were accomplished, some, however, left for the wintering party. In addition, 4 summer members carried out other marine observations using R/V Tangaroa chartered by JARE-43.

  5. Corganiser: a web-based software tool for planning time-sensitive sampling of whole rounds during scientific drilling

    DEFF Research Database (Denmark)

    Marshall, Ian

    2014-01-01

    Corganiser is a software tool developed to simplify the process of preparing whole-round sampling plans for time-sensitive microbiology and geochemistry sampling during scientific drilling. It was developed during the Integrated Ocean Drilling Program (IODP) Expedition 347, but is designed to work...... with a wide range of core and section configurations and can thus be used in future drilling projects. Corganiser is written in the Python programming language and is implemented both as a graphical web interface and command-line interface. It can be accessed online at http://130.226.247.137/....

  6. Dive Data from Expedition Information System (EIS) for Islands in the Stream 2002 - Deep Reef Habitat - Office of Ocean Exploration

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The Expeditions Information System (EIS) contains information recorded by the NOAA Office of Ocean Exploration's data manager during the 2002 "Islands in the Stream...

  7. 77 FR 38523 - Expedited Approval of Alternative Test Procedures for the Analysis of Contaminants Under the Safe...

    Science.gov (United States)

    2012-06-28

    ... afforded by the revised method include: Use of solid preservation reagents (ascorbic acid...: Differential Interference Contrast EDTA: Ethylenediaminetetraacetic Acid EPA: Environmental Protection Agency... site at http://water.epa.gov/scitech/drinkingwater/labcert/analyticalmethods_expedited.cfm . B. What is...

  8. Drilling Deep Into STEM Education with JOIDES Resolution Education and Outreach Officers

    Science.gov (United States)

    Christiansen, E. A.

    2015-12-01

    During International Ocean Discovery Program (IODP) expeditions, IODP scientists and Education/Outreach (E/O) Officers enter classrooms and informal science venues via live Internet video links between the JOIDES Resolution (JR) and land-based learning centers. Post-expedition, E/O Officers, serving as JR Ambassadors, deepen and broaden the learning experience by bringing STEM from the JR to the general public through targeted outreach events at those land-based sites. Youth and adult learners participate in scientific inquiry through interactive activities linked directly to the video broadcast experience. Outreach venues include museums, summer camps, and after-school programs; classroom visits from E/O Officers encompass kindergarten to undergraduate school groups and often include professional development for educators. Events are hands-on with simulations, expedition samples, core models, and equipment available for interaction. This program can serve as a model for linking virtual and real experiences; deepening the educational value of virtual field trip events; and bringing cutting edge science into both classrooms and informal science venues.

  9. Relationship of psychological and physiological parameters during an arctic ski expedition

    Science.gov (United States)

    Bishop, Sheryl L.; Grobler, Lukas C.; SchjØll, Olaf

    2001-08-01

    Considerable data (primarily physiological) have been collected during expeditions in extreme environments over the last century. Physiological measurements have only recently been examined in association with the emotional or behavioral state of the subject. Establishing this psychophysiological relationship is essential to understanding fully the adaptation of humans to the stresses of extreme environments. This pilot study investigated the simultaneous collection of physiological, psychological and behavioral data from a two-man Greenland expedition in order to model how specific relationships between physiological and psychological adaptation to a polar environment may be identified. The data collected describes changes in adrenal and other hormonal activity and psychological functioning. Levels of cortisol and testosterone were calculated. Factors influencing the plasma profiles of the aforementioned included 24-hour sunlight, high calorific intake of more than 28 000 kJ/day and extreme physical exercise. There was a difference between individual psychological profiles as well as self-report stress and physiological stress.

  10. The Last Expedition of the Siberian A.V. Adrianov (Tuva, 1915–1916

    Directory of Open Access Journals (Sweden)

    Olga B. Belikova

    2014-12-01

    Full Text Available The article presents the results of the examination of archaeological activity of Siberian public figure and scientist A.V. Adrianov (1854–1920 in his last expedition. It took place in the upstream basin of the Yenisei River – in Tuva (Uryankhaysky Kray / Tannu Uryankhay in 1915–1916. The archaeologist could not summarize and publish the results of his successful field research – he died in 1920 due to the unjustified sentence of the Bolsheviks. The expedition prehistory, the content of the archaeological excavations and exploration, the history of the materials deposition to the storage, scientist's last years have been restored. The information, concerning 23 ancient Old Turkic manuscripts, examined by A.V. Adrianov has been identified and summarized. The data on new sources have been introduced into scientific use.

  11. Haughton-Mars Project Expedition 2005: Interplanetary Supply Chain Management & Logistics Architectures

    Science.gov (United States)

    deWeck, Olivier; Simchi-Levi, David

    2006-01-01

    The 2005 expedition to the Haughton-Mars Project (HMP) research station on Devon Island was part of a NASA-funded project on Space Logistics. A team of nine researchers from MIT went to the Canadian Arctic to participate in the annual HMP field campaign from July 8 to August 12, 2005. We investigated the applicability of the HMP research station as an analogue for planetary macro- and micro-logistics to the Moon and Mars, and began collecting data for modeling purposes. We also tested new technologies and procedures to enhance the ability of humans and robots to jointly explore remote environments. The expedition had four main objectives. We briefly summarize our key findings in each of these areas.

  12. ISS Expeditions 16 Thru 20: Chemical Analysis Results for Potable Water

    Science.gov (United States)

    Straub, John E., II; Plumlee, Debrah K.; Schultz, John R.

    2010-01-01

    This slide presentation reviews the results of the chemical analysis of the potable water supply from the International Space Station (ISS) expeditions 16 thru 20. Both Russian ground water and shuttle-transferred water are available for the use of the ISS crew's requirements. This is supplemented with condensate water and water form the Water Recovery System (WRS). An overview of the condensate H2O recovery system is given and the WRS is described and diagrammed. The water quality requirements, the handling, and analytical methods for the inorganic and organic tests are reviewed. The chemical analysis results for expeditions 16-20 archival water samples collected from the various water sources indicate that all of the ISS potable water supplies were acceptable for crew consumption.

  13. Striking balance between expedited review and expecting efficacious anticancer drug and biologics: An ongoing challenge.

    Science.gov (United States)

    Chary, Krishnan Vengadaragava; Ramesh, Anita

    2017-01-01

    The objective of this study is to assess the postmarketing status: Efficacy and safety drugs and biologics related with cancer approved under expedited review. This observational, analytical study was carried between January and April 2016 by the Department of Pharmacology and Medical Oncology, Saveetha Medical College. Drugs approved under expedited review, fast-track status and its association with anti-cancer effects, postmarketing efficacy and safety, propensity to induce the second tumor was noted. Drug approval status and average time of review process were obtained from the United States-Food and Drug Administration (FDA), Center for Drugs and Biologics Center (Center for Drug Evaluation and Research and Center for Biologics Evaluation and Research). Postmarketing adverse events and safety issues were collected FDA adverse effects reporting system. Further, evidence efficacy and safety of drugs were taken from various meta-analysis, reports on BioMed journals, and Cochrane systematic reviews. In the last 5 years, 166 products were approved by expedited review. Out of 166, 48 (28.9%) drugs/biologics are anticancer drugs and drugs used in precancerous conditions. The average time of review varies from19 months to 8.2 months. Out of these 48 molecules, 37 (77%) molecules received serious adverse event alert. Positive correlation is seen between average time of review and number of adverse events reported. Seven (14.5%) drugs were proven to induce second tumor among receivers. Although expedited review facilitates faster approval of drugs; selection and assessment criteria should be stringent to prevent clinical failure, serious adverse effects of such drugs exposed to many individuals. Focus should be given developing chemosensitizing molecule and evaluation of metronomic regimen which is being more optimistic in current cancer therapeutics.

  14. Striking balance between expedited review and expecting efficacious anticancer drug and biologics: An ongoing challenge

    Directory of Open Access Journals (Sweden)

    Krishnan Vengadaragava Chary

    2017-01-01

    Full Text Available Objective: The objective of this study is to assess the postmarketing status: Efficacy and safety drugs and biologics related with cancer approved under expedited review. Methods: This observational, analytical study was carried between January and April 2016 by the Department of Pharmacology and Medical Oncology, Saveetha Medical College. Drugs approved under expedited review, fast-track status and its association with anti-cancer effects, postmarketing efficacy and safety, propensity to induce the second tumor was noted. Drug approval status and average time of review process were obtained from the United States-Food and Drug Administration (FDA, Center for Drugs and Biologics Center (Center for Drug Evaluation and Research and Center for Biologics Evaluation and Research. Postmarketing adverse events and safety issues were collected FDA adverse effects reporting system. Further, evidence efficacy and safety of drugs were taken from various meta-analysis, reports on BioMed journals, and Cochrane systematic reviews. Results: In the last 5 years, 166 products were approved by expedited review. Out of 166, 48 (28.9% drugs/biologics are anticancer drugs and drugs used in precancerous conditions. The average time of review varies from19 months to 8.2 months. Out of these 48 molecules, 37 (77% molecules received serious adverse event alert. Positive correlation is seen between average time of review and number of adverse events reported. Seven (14.5% drugs were proven to induce second tumor among receivers. Conclusion: Although expedited review facilitates faster approval of drugs; selection and assessment criteria should be stringent to prevent clinical failure, serious adverse effects of such drugs exposed to many individuals. Focus should be given developing chemosensitizing molecule and evaluation of metronomic regimen which is being more optimistic in current cancer therapeutics.

  15. MATERIALS OF EXPEDITIONS F. A. SCHERBINA AND MAPPING OF CULTURAL LANDSCAPES EARLIER DEVELOPED REGIONS

    Directory of Open Access Journals (Sweden)

    S. A. Teslenok

    2013-01-01

    Full Text Available  Considered some mapping materials reports of expeditions to research steppe areas of Russia (1896 - 1903 led by an outstanding scientist and political figure, founder of budget statistics F. A. Scherbina. Presented methodology and results of the use these materials in the geoinformation mapping of cultural landscapes earlier developed areas in process of studying processes agrolandshaftogenez (genesis agrolandscape, shaping agricultural landscape, agricultural formation landscape.    

  16. Notes on caridean shrimps collected during the Snellius-II expedition. I. Associates of Anthozoa

    Science.gov (United States)

    Fransen, C. H. J. M.

    During the Snellius-II Expedition to Indonesian waters in 1984, ten species of shrimp were collected associated with Anthozoa (Actiniaria: 6 species; Corallimorpharia: 1 species; Scleractinia: 3 species). These species are: Thor amboinensis (Hippolytidae), Periclimenes brevicarpalis, P. aff. inornatus, P. ornatus, P. holthuisi, P. magnificus, Pliopontonia furtiva, Paratypton siebenrocki, Philarius gerlachei and Jocaste japonica (all Palaemonidae, Pontoniinae). Four new associations and four new records for Indonesian waters were established. Biogeographical aspects, as well as taxonomic problems in some groups are discussed.

  17. The Australasian Antarctic Expedition 2013-2014: Practicing 'Citizen-Science' in a Changing World

    Science.gov (United States)

    Fogwill, C. J.; Turney, C. S.

    2014-12-01

    Government funding is the cornerstone of modern science. But with declining investment in science across most of the Western World, a major challenge for society is where best to place what little resource we have. Which research questions should have the greatest priority? Nowhere are these issues more pressing than in the Antarctic, where bases have and continue to play host to 'big-science', multi-year programmes of research, locking up logistical support and costs. But in a warming world, the areas with the greatest effects of climate change aren't always near government research stations. With this in mind, in 2012 a plan was formed to visit Commonwealth Bay, a remote area off the East Antarctic Ice Sheet, where in 2010, an iceberg the size of Rhode Island, known as B09B, dramatically knocked a 60-mile long tongue of ice off the Mertz Glacier into the Southern Ocean, setting off a cascade of change. Inspired by the expeditions of the past, we advertised berths for sale to take citizen scientists south with us, harnessing their interest, experience and investment. People responded far and wide. We were oversubscribed, and the Australasian Antarctic Expedition 2013-2014 was born. With the Russian-owned MV Akademik Shokalskiy as the expedition vessel, we set out south from the New Zealand port of Bluff in late November 2013. During our journey south and on the ice we undertook a number of scientific firsts for the region actively engaging the volunteer scientists on board in projects ranging from oceanography, biology, ecology, geology and glaciaology. The expedition demostrated how private funding could support targeted programmes of research and communicate it to the wider world. Small-science research can capture the public's imagination and also reap real scientific outputs. Although it is a funding model developed in the Antarctic a hundred years ago, the beauty is it can applied anywhere in the world.

  18. Want of Proper Spirit and Energy: The Penobscot Expedition of 1779

    Science.gov (United States)

    2011-06-10

    her men. Shirley appealed to Admiral Peter Warren operating in the Carribean to support the operation, but he could not offer his support until...WANT OF PROPER SPIRIT AND ENERGY: THE PENOBSCOT EXPEDITION OF 1779 A thesis presented to the Faculty of the U.S. Army...Command and General Staff College in partial fulfillment of the requirements for the degree MASTER OF MILITARY ART AND SCIENCE Military History

  19. Behavioral Issues Associated With Long Duration Space Expeditions: Review and Analysis of Astronaut Journals

    Science.gov (United States)

    Struster, Jack

    2010-01-01

    Personal journals maintained by NASA astronauts during six-month expeditions onboard the International Space Station were analyzed to obtain information concerning a wide range of behavioral and human factors issues. Astronauts wrote most about their work, followed by outside communications (with mission control, family, and friends), adjustment to the conditions, interactions with crew mates, recreation/leisure, equipment (installation, maintenance), events (launches, docking, hurricanes, etc.), organization/management, sleep, and food. The study found evidence of a decline in morale during the third quarters of the missions and identified key factors that contribute to sustained adjustment and optimal performance during long-duration space expeditions. Astronauts reported that they benefited personally from writing in their journals because it helped maintain perspective on their work and relations with others. Responses to questions asked before, during, and after the expeditions show that living and working onboard the ISS is not as difficult as the astronauts anticipate before starting their six-month tours of duty. Recommendations include application of study results and continuation of the experiment to obtain additional data as crew size increases and operations evolve.

  20. The Inaugural SHALDRIL Expedition to the Weddell Sea, Antarctica

    Directory of Open Access Journals (Sweden)

    S. W. Wise,

    2005-09-01

    Full Text Available Introduction In 1994, a group of scientists began discussing a number of important scientific questions that could be addressed by drilling a series of short cores on the Antarctic continental shelf. The group adopted the name SHALDRIL, for SHALlow DRILling, and soon learned that the technology for high-quality sampling of the upper few hundred metersof the stratigraphic column was still lacking.After more than a decade of discussion and several years of detailed planning, SHALDRIL sailed from Punta Arenas, Chile, in March 2005. The objectives of this first SHALDRIL cruise are to demonstrate the feasibility of drilling from an icebreaker platform into the Antarctic continental shelf and to obtain cores from three different sedimentary sequences that previously have not been sampled.The principal objective of SHALDRIL originally was to monitor technological developments in shallow drilling from conventional icebreaking research vessels. In 2000, the SHALDRIL steering committee learned about new and improved drilling systems that can core through gravelly glacial deposits in water depths of several hundred meters and to subbottom depths of a few hundred meters(SHALDRIL Steering Committee, 2001. These systems can be operated from the icebreaking research vessel Nathaniel B. Palmer (Fig. 1; thus, the long-term project has now entered the next phase of testing this proven drilling technology aboard a U. S. Antarctic Program vessel.

  1. A “radically new method”: balloon buoy communications of the Baldwin–Ziegler Polar Expedition, Franz Josef Land, June 1902

    OpenAIRE

    Capelotti, P.J.

    2008-01-01

    The history of lighter-than-air operations in the Arctic between 1896 and 1930 has focused almost exclusively upon four expeditions. These are the balloon voyage of the Swede Salomon Andrée in 1896–97, and the dirigible expeditions of the American Walter Wellman in 1906–09, the Norwegian Roald Amundsen with the Italian Umberto Nobile in 1926 and the Nobile expedition of 1928. Largely invisible in this lineage are the aeronautical operations of the Baldwin–Ziegler Polar Expedition on Alger Isl...

  2. 75 FR 29366 - ``Homeless Veterans' Reintegration Program (HVRP) National Technical Assistance Center...

    Science.gov (United States)

    2010-05-25

    ... of the Assistant Secretary for Veterans' Employment and Training ``Homeless Veterans' Reintegration... the Homeless Veterans' Reintegration Program (HVRP) to include the Homeless Female Veterans and... to expedite the reintegration of homeless Veterans into the labor force. In order to assist the USDOL...

  3. Geophysical and geochemical evidence of large scale fluid flow within shallow sediments in the eastern Gulf of Mexico, offshore Louisiana

    OpenAIRE

    A. Gay; Y. Takano; W. P. Gilhooly III; C. Berndt; Katja Heeschen; N. Suzuki; S. Saegusa; F. Nakagawa; U. Tsunogai; S. Y. Jiang; M. Lopez

    2011-01-01

    We analyse the fluid flow regime within sediments on the Eastern levee of the modern Mississippi Canyon using 3D seismic data and downhole logging data acquired at Sites U1322 and U1324 during the 2005 Integrated Ocean Drilling Program (IODP) Expedition 308 in the Gulf of Mexico. Sulphate and methane concentrations in pore water show that sulphate–methane transition zone, at 74 and 94 m below seafloor, are amongst the deepest ever found in a sedimentary basin. This is in part due to a basinwa...

  4. Operational Review of the First Wireline In Situ Stress Test in Scientific Ocean Drilling

    Directory of Open Access Journals (Sweden)

    Casey Moore

    2012-04-01

    Full Text Available Scientific ocean drilling’s first in situ stress measurement was made at Site C0009A during Integrated Ocean Drilling Program (IODP Expedition 319 as part of Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE Stage 2. The Modular Formation Dynamics Tester (MDT, Schlumbergerwireline logging tool was deployed in riser Hole C0009A to measure in situ formation pore pressure, formation permeability (often reported as mobility=permeability/viscosity, and the least principal stress (S3 at several isolated depths (Saffer et al., 2009; Expedition 319 Scientists, 2010. The importance of in situ stress measurements is not only for scientific interests in active tectonic drilling, but also for geomechanical and well bore stability analyses. Certain in situ tools were not previously available for scientific ocean drilling due to the borehole diameter and open hole limits of riserless drilling. The riser-capable drillship, D/V Chikyu,now in service for IODP expeditions, allows all of the techniques available to estimate the magnitudes and orientations of 3-D stresses to be used. These techniques include downhole density logging for vertical stress, breakout and caliper log analyses for maximum horizontal stress, core-based anelastic strain recovery (ASR, used in the NanTroSEIZE expeditions in 2007–2008, and leak-off test (Lin et al., 2008 and minifrac/hydraulic fracturing (NanTroSEIZE Expedition319 in 2009. In this report, the whole operational planning process related to in situ measurements is reviewed, and lessons learned from Expedition 319 are summarized for efficient planning and testing in the future.

  5. Terrigenous Grain-size Record of the Newfoundland Ridge Contourite Drift, IODP Site U1411: The First Physical Proxy Record of North Atlantic Abyssal Current Intensity during the Eocene-Oligocene Transition

    Science.gov (United States)

    Chilton, K.; Romans, B.; Spray, J.; Wilson, P. A.; Bohaty, S. M.; Sanchez, T.

    2016-12-01

    Atlantic Meridional Ocean Circulation (AMOC) is a vital process that helps to regulate global climate and support marine ecosystems. The timing and nature of the shift to modern AMOC, and especially to deep-water formation in the North Atlantic, has been a topic of ongoing study, with the Eocene-Oligocene Transition (EOT, 34 Ma) being a potential focal point of this shift. However, the role played by abrupt EOT cooling in North Atlantic circulation remains unclear. Improved constraints on Paleogene circulation will provide insight into the sensitivity of AMOC to perturbations in global climate. We obtained grain-size data from the terrigenous fraction of the mud-dominated sediments of the Southeast Newfoundland Ridge contourite drift complex at IODP Site U1411, which is interpreted to have formed under the influence of the Deep Western Boundary Current. We analyzed 195 samples that span 150 m of stratigraphy from 36-26 Ma. The main objective was to use the `sortable silt' fraction (10-63 µm) to generate a record of relative change in bottom-current velocity. These data are complemented with a record of the abundance and size of lithogenic sand (>63 µm). Here we present U1411 sortable silt data as the first physical proxy record of abyssal current intensity in the North Atlantic, from late Eocene to mid Oligocene. Invigoration of North Atlantic deep circulation occurred gradually (over Myr timescales). We infer that deep circulation in the North Atlantic was not sensitive to the abrupt global cooling and Antarctic glaciation associated with the EOT. Rather, our data suggest that changes in North Atlantic circulation were likely governed by longer-term processes related to the opening of key tectonic gateways (i.e., the Greenland-Scotland-Faeroes Ridge in the North Atlantic, and the Drake and Tasman Passages in the Southern Ocean). Lithogenic sand is nearly absent in the Eocene and then systematically increases in abundance from the earliest Oligocene through the

  6. In-Situ Sampling and Characterization of Naturally Occurring Marine Methane Hydrate Using the D/V JOIDES Resolution

    Energy Technology Data Exchange (ETDEWEB)

    Frank R. Rack

    2006-09-20

    Cooperative Agreement DE-FC26-01NT41329 between Joint Oceanographic Institutions and DOE-NETL was divided into two phases based on successive proposals and negotiated statements of work pertaining to activities to sample and characterize methane hydrates on ODP Leg 204 (Phase 1) and on IODP Expedition 311 (Phase 2). The Phase 1 Final Report was submitted to DOE-NETL in April 2004. This report is the Phase 2 Final Report to DOE-NETL. The primary objectives of Phase 2 were to sample and characterize methane hydrates using the systems and capabilities of the D/V JOIDES Resolution during IODP Expedition 311, to enable scientists the opportunity to establish the mass and distribution of naturally occurring gas and gas hydrate at all relevant spatial and temporal scales, and to contribute to the DOE methane hydrate research and development effort. The goal of the work was to provide expanded measurement capabilities on the JOIDES Resolution for a dedicated hydrate cruise to the Cascadia continental margin off Vancouver Island, British Columbia, Canada (IODP Expedition 311) so that hydrate deposits in this region would be well characterized and technology development continued for hydrate research. IODP Expedition 311 shipboard activities on the JOIDES Resolution began on August 28 and were concluded on October 28, 2005. The statement of work for this project included three primary tasks: (1) research management oversight, provided by JOI; (2) mobilization, deployment and demobilization of pressure coring and core logging systems, through a subcontract with Geotek Ltd.; and, (3) mobilization, deployment and demobilization of a refrigerated container van that will be used for degassing of the Pressure Core Sampler and density logging of these pressure cores, through a subcontract with the Texas A&M Research Foundation (TAMRF). Additional small tasks that arose during the course of the research were included under these three primary tasks in consultation with the DOE

  7. MaNIDA: Integration of marine expedition information, data and publications: Data Portal of German Marine Research

    Science.gov (United States)

    Koppe, Roland; Scientific MaNIDA-Team

    2013-04-01

    The Marine Network for Integrated Data Access (MaNIDA) aims to build a sustainable e-infrastructure to support discovery and re-use of marine data from distinct data providers in Germany (see related abstracts in session ESSI 1.2). In order to provide users integrated access and retrieval of expedition or cruise metadata, data, services and publications as well as relationships among the various objects, we are developing (web) applications based on state of the art technologies: the Data Portal of German Marine Research. Since the German network of distributed content providers have distinct objectives and mandates for storing digital objects (e.g. long-term data preservation, near real time data, publication repositories), we have to cope with heterogeneous metadata in terms of syntax and semantic, data types and formats as well as access solutions. We have defined a set of core metadata elements which are common to our content providers and therefore useful for discovery and building relationships among objects. Existing catalogues for various types of vocabularies are being used to assure the mapping to community-wide used terms. We distinguish between expedition metadata and continuously harvestable metadata objects from distinct data providers. • Existing expedition metadata from distinct sources is integrated and validated in order to create an expedition metadata catalogue which is used as authoritative source for expedition-related content. The web application allows browsing by e.g. research vessel and date, exploring expeditions and research gaps by tracklines and viewing expedition details (begin/end, ports, platforms, chief scientists, events, etc.). Also expedition-related objects from harvesting are dynamically associated with expedition information and presented to the user. Hence we will provide web services to detailed expedition information. • Other harvestable content is separated into four categories: archived data and data products, near

  8. Arctic Expedition of the Frozen Five: an Alternative way of Education and Outreach During the International Polar Year

    Science.gov (United States)

    Senger, K.; Björkman, M.; Garny, H.; Girard, L.; Lichteneger, J.

    2006-12-01

    In March 2007, a group of international students of the geosciences will embark on a two month expedition across the wilderness of Svalbard. The journey will involve traversing up to 1000 km of high Arctic glaciers between 76° an 80°N, reaching both the southernmost and northernmost capes of Spitsbergen, Svalbard's largest island. We expect to be frequently camping at -30°C, as well as having a high probability of encountering polar bears, crevasses and arctic storms during the expedition. Through this expedition, we wish to promote the multi-disciplinary approach required in successful Arctic science. Our team, young and energetic, has already demonstrated a strong research interest in the Arctic and is ready to share their passion with the general public. Presentations by the various team members focus on the enhanced climate change and related processes witnessed at high latitudes. The concept of alternative energy, including solar power and kites used while en route, is given a high priority throughout. Here we present the education and outreach framework of the project, as well as introducing the research background of the team. We highlight current progress on the integration of this expedition in high schools around the world. The Frozen Five expedition runs in close collaboration with New Zealand's Youth Steering Committee, a major IPY project, aiming to network young polar researchers and promote the study of the polar regions to potential scientists.

  9. Assessing the Impacts of the First Five Years of School of Rock On-Board and On-Shore Professional Development Program for Educators: Lessons for Other Teacher Professional Development Programs

    Science.gov (United States)

    Collins, J.; Peart, L. W.; Cooper, S. K.; St John, K. K.; Leckie, R. M.; Hovan, S. A.; Firth, J. V.

    2011-12-01

    School of Rock (SoR) is an immersive professional development program run by the Deep Earth Academy (DEA) of the Consortium for Ocean Leadership. The program offers formal and informal educators an opportunity to utilize the laboratories, cores, smear slides, and other data on the JOIDES Resolution research vessel and Texas A&M Gulf Coast Repository to investigate Earth science topics aligned with the IODP science goals. Participants acquire content and skills through inquiry explorations facilitated by scientist instructors and lab technicians, and are exposed to the culture of onshore and offshore science by interacting with experts from a range of scientific and non-scientific disciplines. Since 2005, the School of Rock program has hosted over 60 participants from 33 states and four countries. Several of the SoR programs had on-board experiences, while others were held on-shore at the IODP's Gulf Coast Repository. The participant demographics varied in each cohort as did some of science content focus and pedagogical approach. To assess the impact of the SoR experience on participants and their classrooms, and inform DEA about how to proceed with future SoR programs, past participants recently completed two online surveys. Data were analyzed in the context of three guiding questions: What important qualities have been consistent across the years?, What are some key differences between the SoR programs?, What are the key differences between shore-based and onboard experiences?. Additionally, participants documented the number of activities they developed, workshops given, and other efforts that share their SoR experience with their respective audiences. The survey results and ensuing discussions with a focus group of program participants representing each of the cohorts suggest to our surprise, that participants in on-shore experiences were similarly satisfied and enthusiastic about their learning experience as those that participated in shipboard SoRs, even

  10. Sleep during an Antarctic summer expedition: new light on "polar insomnia".

    Science.gov (United States)

    Pattyn, Nathalie; Mairesse, Olivier; Cortoos, Aisha; Marcoen, Nele; Neyt, Xavier; Meeusen, Romain

    2017-04-01

    Sleep complaints are consistently cited as the most prominent health and well-being problem in Arctic and Antarctic expeditions, without clear evidence to identify the causal mechanisms. The present investigation aimed at studying sleep and determining circadian regulation and mood during a 4-mo Antarctic summer expedition. All data collection was performed during the continuous illumination of the Antarctic summer. After an habituation night and acclimatization to the environment (3 wk), ambulatory polysomnography (PSG) was performed in 21 healthy male subjects, free of medication. An 18-h profile (saliva sampling every 2 h) of cortisol and melatonin was assessed. Mood, sleepiness, and subjective sleep quality were assessed, and the psychomotor vigilance task was administered. PSG showed, in addition to high sleep fragmentation, a major decrease in slow-wave sleep (SWS) and an increase in stage R sleep. Furthermore, the ultradian rhythmicity of sleep was altered, with SWS occurring mainly at the end of the night and stage R sleep at the beginning. Cortisol secretion profiles were normal; melatonin secretion, however, showed a severe phase delay. There were no mood alterations according to the Profile of Mood States scores, but the psychomotor vigilance test showed an impaired vigilance performance. These results confirm previous reports on "polar insomnia", the decrease in SWS, and present novel insight, the disturbed ultradian sleep structure. A hypothesis is formulated linking the prolonged SWS latency to the phase delay in melatonin.NEW & NOTEWORTHY The present paper presents a rare body of work on sleep and sleep wake regulation in the extreme environment of an Antarctic expedition, documenting the effects of constant illumination on sleep, mood, and chronobiology. For applied research, these results suggest the potential efficiency of melatonin supplementation in similar deployments. For fundamental research, these results warrant further investigation of the

  11. A New Era of Multidisciplinary Expeditions: Recent Opportunities and Progress to Advance the Telepresence Paradigm

    Science.gov (United States)

    Cantwell, K. L.; Kennedy, B. R.; Malik, M.; Gray, L. M.; Elliott, K.; Lobecker, E.; Drewniak, J.; Reser, B.; Crum, E.; Lovalvo, D.

    2016-02-01

    Since it's commissioning in 2008, NOAA Ship Okeanos Explorer has used telepresence technology both as an outreach tool and as a new way to conduct interdisciplinary science expeditions. NOAA's Office of Ocean Exploration and Research (OER) has developed a set of collaboration tools and protocols to enable extensive shore-based participation. Telepresence offers unique advantages including access to a large pool of expertise on shore and flexibility to react to new discoveries as they occur. During early years, the telepresence experience was limited to Internet 2 enabled Exploration Command Centers, but with advent of improved bandwidth and new video transcoders, scientists from anywhere with an internet connection can participate in a telepresence expedition. Scientists have also capitalized on social media (Twitter, Facebook, Reddit etc.) by sharing discoveries to leverage the intellectual capital of scientists worldwide and engaging the general public in real-time. Aside from using telepresence to stream video off the ship, the high-bandwidth satellite connection allows for the transfer of large quantities of data in near real-time. This enables not only ship - shore data transfers, but can also support ship - ship collaborations as demonstrated during the 2015 and 2014 seasons where Okeanos worked directly with science teams onboard other vessels to share data and immediately follow up on features of interest, leading to additional discoveries. OER continues to expand its use of telepresence by experimenting with procedures to offload roles previously tied to the ship, such as data acquisition watch standers; prototyping tools for distributed user data analysis and video annotation; and incorporating in-situ sampling devices. OER has also developed improved tools to provide access to archived data to increase data distribution and facilitate additional discoveries post-expedition.

  12. The legal aspects of expedited partner therapy practice: do state laws and policies really matter?

    Science.gov (United States)

    Cramer, Ryan; Leichliter, Jami S; Stenger, Mark R; Loosier, Penny S; Slive, Lauren

    2013-08-01

    Expedited partner therapy (EPT) is a potential partner treatment strategy. Significant efforts have been devoted to policies intended to facilitate its practice. However, few studies have attempted to evaluate these policies. We used data on interviewed gonorrhea cases from 12 sites in the STD Surveillance Network in 2010 (n = 3404). Patients reported whether they had received EPT. We coded state laws relevant to EPT for gonorrhea using Westlaw legal research database and the general legal status of EPT in STD Surveillance Network sites from Centers for Disease Control and Prevention's Web site in 2010. We also coded policy statements by medical and other boards. We used χ tests to compare receipt of EPT by legal/policy variables, patient characteristics, and provider type. Variables significant at P < 0.10 in bivariate analyses were included in a logistic regression model. Overall, 9.5% of 2564 interviewed patients with gonorrhea reported receiving EPT for their partners. Receipt of EPT was significantly higher where laws and policies authorizing EPT existed. Where EPT laws for gonorrhea existed and EPT was permissible, 13.3% of patients reported receiving EPT as compared with 5.4% where there were no EPT laws and EPT was permissible, and 1.0% where there were no EPT laws and EPT was potentially allowable (P < 0.01). Expedited partner therapy was higher where professional boards had policy statements supporting EPT (P < 0.01). Receipt of EPT did not differ by most patient characteristics or provider type. Policy-related findings were similar in adjusted analyses. Expedited partner therapy laws and policies were associated with higher reports of receipt of EPT among interviewed gonorrhea cases.

  13. Delayed-Start Analyses in the Phase 3 Solanezumab EXPEDITION3 Study in Mild Alzheimer's Disease.

    Science.gov (United States)

    Liu-Seifert, H; Case, M G; Andersen, S W; Holdridge, K C; Aisen, P S; Kollack-Walker, S; Siemers, E

    2018-01-01

    A delayed-start design has been proposed to assess a potential disease-modifying effect in investigational drugs for Alzheimer's disease that target the underlying disease process. We extended this methodology to recently obtained data from the EXPEDITION3. EXPEDITION3 was a Phase 3, double-blind study with participants randomized to solanezumab (400 mg) or placebo every 4 weeks for 80 weeks, with an optional extension of active treatment. The delayed-start analysis was designed to determine if a statistically significant treatment difference established during the placebo-controlled period is maintained (at predefined level) during the delayed-start period, which would suggest the active drug has a disease-modifying effect. The delayed-start analysis was assessed across multiple efficacy measures, and includes data from baseline in the placebo-controlled period and up to 9 months in the delayed-start period. No significant difference was observed between the placebo and solanezumab treatment groups at the end of the placebo-controlled period for the Alzheimer's Disease Assessment Scale-Cognitive 14-item subscale. A significant treatment difference was observed at the end of the placebo-controlled period for the Alzheimer's Disease Cooperative Study-Activities of Daily Living instrumental items, an effect also seen at 6 months in the delayed-start period, and the noninferiority criterion was met. No other efficacy measures met these criteria. Delayed-start statistical methodology was used to understand the longitudinal outcomes in EXPEDITION3 and its extension. The small treatment differences observed at the end of the placebo-controlled phase prevented adequate assessment of any putative disease modifying effect.

  14. In-Situ Sampling and Characterization of Naturally Occurring Marine Methane Hydrate Using the D/V JOIDES Resolution

    Energy Technology Data Exchange (ETDEWEB)

    Frank Rack

    2005-06-30

    The primary accomplishments of the JOI Cooperative Agreement with DOE/NETL in this quarter were to refine budgets and operational plans for Phase 2 of this cooperative agreement based on the scheduling of a scientific ocean drilling expedition to study marine methane hydrates along the Cascadia margin, in the NE Pacific as part of the Integrated Ocean Drilling Program (IODP) using the R/V JOIDES Resolution. The proposed statement of work for Phase 2 will include three primary tasks: (1) research management oversight, provided by JOI; (2) mobilization, deployment and demobilization of pressure coring and core logging systems, through a subcontract with Geotek Ltd., who will work with Fugro and Lawrence Berkeley National Laboratory to accomplish some of the subtasks; and, (3) mobilization, deployment and demobilization of a refrigerated container van that will be used for degassing of the Pressure Core Sampler and density logging of these pressure cores, through a subcontract with the Texas A&M Research Foundation (TAMRF). More details about these tasks are provided in the following sections of this report. The appendices to this report contain a copy of the scientific prospectus for the upcoming IODP Expedition 311 (Cascadia Margin Hydrates), which provides details of operational and scientific planning for this expedition.

  15. EXPEDITING THE PATH TO CLOSURE THE CHEMICAL WASTE LANDFILL, SANDIA NATIONAL LABORATORIES, NEW MEXICO

    Energy Technology Data Exchange (ETDEWEB)

    Young, S.G.; Schofield, D.P.; Davis, M.J.; Methvin, R.; Mitchell, M.

    2003-02-27

    The Chemical Waste Landfill (CWL) at Sandia National Laboratories, New Mexico (SNL/NM) is undergoing closure subject to the requirements of Subtitle C of RCRA. This paper identifies regulatory mechanisms that have and continue to expedite and simplify the closure of the CWL. These include (1) the Environmental Restoration (ER) Programmatic effort to achieve progress quickly with respect to the standard regulatory processes, which resulted in the performance of voluntary corrective measures at the CWL years in advance of the standard process schedule, (2) the management and disposal of CWL remediation wastes and materials according to the risks posed, and (3) the combination of multiple regulatory requirements into a single submittal.

  16. Fast 3D Net Expeditions: Tools for Effective Scientific Collaboration on the World Wide Web

    Science.gov (United States)

    Watson, Val; Chancellor, Marisa K. (Technical Monitor)

    1996-01-01

    Two new technologies, the FASTexpedition and Remote FAST, have been developed that provide remote, 3D (three dimensional), high resolution, dynamic, interactive viewing of scientific data. The FASTexpedition permits one to access scientific data from the World Wide Web, take guided expeditions through the data, and continue with self controlled expeditions through the data. Remote FAST permits collaborators at remote sites to simultaneously view an analysis of scientific data being controlled by one of the collaborators. Control can be transferred between sites. These technologies are now being used for remote collaboration in joint university, industry, and NASA projects. Also, NASA Ames Research Center has initiated a project to make scientific data and guided expeditions through the data available as FASTexpeditions on the World Wide Web for educational purposes. Previously, remote visualization of dynamic data was done using video format (transmitting pixel information) such as video conferencing or MPEG (Motion Picture Expert Group) movies on the Internet. The concept for this new technology is to send the raw data (e.g., grids, vectors, and scalars) along with viewing scripts over the Internet and have the pixels generated by a visualization tool running on the viewers local workstation. The visualization tool that is currently used is FAST (Flow Analysis Software Toolkit). The advantages of this new technology over using video format are: (1) The visual is much higher in resolution (1280x1024 pixels with 24 bits of color) than typical video format transmitted over the network. (2) The form of the visualization can be controlled interactively (because the viewer is interactively controlling the visualization tool running on his workstation). (3) A rich variety of guided expeditions through the data can be included easily. (4) A capability is provided for other sites to see a visual analysis of one site as the analysis is interactively performed. Control of

  17. TCGA Expedition: A Data Acquisition and Management System for TCGA Data.

    Science.gov (United States)

    Chandran, Uma R; Medvedeva, Olga P; Barmada, M Michael; Blood, Philip D; Chakka, Anish; Luthra, Soumya; Ferreira, Antonio; Wong, Kim F; Lee, Adrian V; Zhang, Zhihui; Budden, Robert; Scott, J Ray; Berndt, Annerose; Berg, Jeremy M; Jacobson, Rebecca S

    2016-01-01

    The Cancer Genome Atlas Project (TCGA) is a National Cancer Institute effort to profile at least 500 cases of 20 different tumor types using genomic platforms and to make these data, both raw and processed, available to all researchers. TCGA data are currently over 1.2 Petabyte in size and include whole genome sequence (WGS), whole exome sequence, methylation, RNA expression, proteomic, and clinical datasets. Publicly accessible TCGA data are released through public portals, but many challenges exist in navigating and using data obtained from these sites. We developed TCGA Expedition to support the research community focused on computational methods for cancer research. Data obtained, versioned, and archived using TCGA Expedition supports command line access at high-performance computing facilities as well as some functionality with third party tools. For a subset of TCGA data collected at University of Pittsburgh, we also re-associate TCGA data with de-identified data from the electronic health records. Here we describe the software as well as the architecture of our repository, methods for loading of TCGA data to multiple platforms, and security and regulatory controls that conform to federal best practices. TCGA Expedition software consists of a set of scripts written in Bash, Python and Java that download, extract, harmonize, version and store all TCGA data and metadata. The software generates a versioned, participant- and sample-centered, local TCGA data directory with metadata structures that directly reference the local data files as well as the original data files. The software supports flexible searches of the data via a web portal, user-centric data tracking tools, and data provenance tools. Using this software, we created a collaborative repository, the Pittsburgh Genome Resource Repository (PGRR) that enabled investigators at our institution to work with all TCGA data formats, and to interrogate these data with analysis pipelines, and associated tools

  18. TCGA Expedition: A Data Acquisition and Management System for TCGA Data.

    Directory of Open Access Journals (Sweden)

    Uma R Chandran

    Full Text Available The Cancer Genome Atlas Project (TCGA is a National Cancer Institute effort to profile at least 500 cases of 20 different tumor types using genomic platforms and to make these data, both raw and processed, available to all researchers. TCGA data are currently over 1.2 Petabyte in size and include whole genome sequence (WGS, whole exome sequence, methylation, RNA expression, proteomic, and clinical datasets. Publicly accessible TCGA data are released through public portals, but many challenges exist in navigating and using data obtained from these sites. We developed TCGA Expedition to support the research community focused on computational methods for cancer research. Data obtained, versioned, and archived using TCGA Expedition supports command line access at high-performance computing facilities as well as some functionality with third party tools. For a subset of TCGA data collected at University of Pittsburgh, we also re-associate TCGA data with de-identified data from the electronic health records. Here we describe the software as well as the architecture of our repository, methods for loading of TCGA data to multiple platforms, and security and regulatory controls that conform to federal best practices.TCGA Expedition software consists of a set of scripts written in Bash, Python and Java that download, extract, harmonize, version and store all TCGA data and metadata. The software generates a versioned, participant- and sample-centered, local TCGA data directory with metadata structures that directly reference the local data files as well as the original data files. The software supports flexible searches of the data via a web portal, user-centric data tracking tools, and data provenance tools. Using this software, we created a collaborative repository, the Pittsburgh Genome Resource Repository (PGRR that enabled investigators at our institution to work with all TCGA data formats, and to interrogate these data with analysis pipelines, and

  19. Power supplies and equipment for military field research: lessons from the British Service Dhaulagiri Research Expedition 2016.

    Science.gov (United States)

    Howard, Matt; Bakker-Dyos, J; Gallagher, L; O'Hara, J P; Woods, D; Mellor, A

    2017-12-25

    The British Service Dhaulagiri Research Expedition (BSDMRE) took place from 27 March to 31 May 2016. The expedition involved 129 personnel, with voluntary participation in nine different study protocols. Studies were conducted in three research camps established at 3600, 4600 and 5140 m and involved taking and storing blood samples, cardiac echocardiography and investigations involving a balance plate. Research in this remote environment requires careful planning in order to provide a robust and resilient power plan. In this paper we aim to report the rationale for the choices we made in terms of power supply, the equipment used and potential military applicability. This is a descriptive account from the expedition members involved in planning and conducting the medical research. Power calculations were used to determine estimates of requirement prior to the expedition. The primary sources used to generate power were internal combustion engine (via petrol fuelled electric generators) and solar panels. Having been generated, power was stored using lithium-ion batteries. Special consideration was given to the storage of samples taken in the field, for which electric freezers and dry shippers were used. All equipment used functioned well during the expedition, with the challenges of altitude, temperature and transport all overcome due to extensive prior planning. Power was successfully generated, stored and delivered during the BSDMRE, allowing extensive medical research to be undertaken. The challenges faced and overcome are directly applicable to delivering military medical care in austere environments, and lessons learnt can help with the planning and delivery of future operations, training exercises or expeditions. © Article author(s) (or their employer(s) unless otherwise stated in the text of the article) 2017. All rights reserved. No commercial use is permitted unless otherwise expressly granted.

  20. Multiple Ships and Multiple Media: A Flexible Telepresence Program

    Science.gov (United States)

    Pelz, M.; Hoeberechts, M.; Riddell, D. J.; Ewing, N.

    2016-02-01

    Ocean Networks Canada (ONC) uses a number of research and exploration vessels equipped with remotely operated vehicles (ROVs) to maintain the NEPTUNE and VENUS cabled ocean observatories off the west coast of British Columbia, Canada. Maintenance expeditions range from several days to multiple weeks and encompass a range of activities including deploying new instruments, laying cable, recovering platforms, scientific sampling and conducting multibeam and visual surveys. In order to engage the widest possible participation in at-sea work, ONC uses telepresence technology to communicate from ship to shore and back with scientists, students, teachers and online viewers. In this presentation, we explore the challenge of designing a sustainable and flexible telepresence program which can be supported across multiple ship and ROV platforms, sometimes simultaneously. To meet outreach and education objectives, onboard educators conduct presentations to K-12 and post-secondary classrooms, museums and science centres on a daily basis. Online commentary by the educators, dive chief and ROV pilots accompanies the ROV dive footage and is streamed online 24/7 during underwater operations. Sharing the sights and sounds of the expeditions with students and educators ashore, including those in remote and inland communities, creates a unique learning environment for both formal and informal education audiences. As space is always a limiting factor on expeditions, the use of telepresence and other communication media enables ONC to simultaneously achieve engineering and science priorities at sea while communicating the successes and challenges of the expedition back to shore. Scientists and engineers provide guidance for operations from shore using a variety of communication technologies. We give examples from Ocean Networks Canada's most recent expedition, Fall 2015, which involved co-ordinated operations with three vessels - the R/V Thompson, the E/V Nautilus and the C/S Wave

  1. The vegetation of the Coastal Region of Suriname. Results of the scientific expedition to Suriname 1948—49 botanical series No. 1

    NARCIS (Netherlands)

    Lindeman, J.C.

    1952-01-01

    The data on which this study is based, were gathered during a scientific expedition which lasted from September 1948 to May 1949. The author had accepted an invitation to join Prof. J. LANJOUW who on this expedition was entrusted with the botanical part of the investigations. They worked in close

  2. 50th Anniversary of Bilyar Archaeological Expedition: results and issues of Great Town investigation

    Directory of Open Access Journals (Sweden)

    Khuzin Fayaz Sh.

    2017-07-01

    Full Text Available The article outlines the main results of the investigation of Bilyar fortified settlement – a unique monument of medieval East-European archaeology located in Alexeyevsky District of the Tatarstan Republic. A small amount of information on Bilyar has remained in Ancient Russian chronicles (in which it is referred to as Great Town and the works by 10th – 14th century Arabic and Persian authors. The monument has been known to historians since 18th century, but its archaeological excavations only started in 1967. For 20 years researchers studied its fortifications, five urban burial grounds (including a necropolis of nobility in the centre of the town, discovered the ruined remains of three brick buildings and a white-stone Cathedral Mosque with a free-standing minaret, craft workshops (pottery, glass-making, blacksmithing and metallurgical, as well as tens and hundreds of common dwellings, utility structures and wells. The discoveries made by Bilyar expedition received a positive reaction from the archaeological community of the country. Since late 1980s the activity of the expedition gradually decreased due to the absence of adequate financing. Minor protective excavations were generally performed in the neighbouring villages. Investigation of the settlement it self continued in 2015. The necessity of continuing systematic excavations in Bilyar and the surrounding monuments is evident from both the scientific and practical viewpoints – application of investigation results for the purposes of tourism.

  3. The Indigo V Indian Ocean Expedition: a prototype for citizen microbial oceanography

    Science.gov (United States)

    Lauro, Federico; Senstius, Jacob; Cullen, Jay; Lauro, Rachelle; Neches, Russell; Grzymski, Joseph

    2014-05-01

    Microbial Oceanography has long been an extremely expensive discipline, requiring ship time for sample collection and thereby economically constraining the number of samples collected. This is especially true for under-sampled water bodies such as the Indian Ocean. Specialised scientific equipment only adds to the costs. Moreover, long term monitoring of microbial communities and large scale modelling of global biogeochemical cycles requires the collection of high-density data both temporally and spatially in a cost-effective way. Thousands of private ocean-going vessels are cruising around the world's oceans every day. We believe that a combination of new technologies, appropriate laboratory protocols and strategic operational partnerships will allow researchers to broaden the scope of participation in basic oceanographic research. This will be achieved by equipping sailing vessels with small, satcom-equipped sampling devices, user-friendly collection techniques and a 'pre-addressed-stamped-envelope' to send in the samples for analysis. We aim to prove that 'bigger' is not necessarily 'better' and the key to greater understanding of the world's oceans is to forge the way to easier and cheaper sample acquisition. The ultimate goal of the Indigo V Expedition is to create a working blue-print for 'citizen microbial oceanography'. We will present the preliminary outcomes of the first Indigo V expedition, from Capetown to Singapore, highlighting the challenges and opportunities of such endeavours.

  4. Antarctic station life: The first 15 years of mixed expeditions to the Antarctic

    Science.gov (United States)

    Sarris, Aspa

    2017-02-01

    This study examined the experiences of women who lived and worked on remote and isolated Antarctic stations for up to 15 months at a time. The study employed purposeful sampling and a longitudinal - processual approach to study women's experiences over the first 15 years of mixed gender Antarctic expeditions. The retrospective analysis was based on a semi-structured interview administered to 14 women upon their return to Australia. The results showed that women referred to the natural physical Antarctic environment as one of the best aspects of their experience and the reason they would recommend the Antarctic to their friends as a good place to work. In describing the worst aspect of their experience, women referred to aspects of Antarctic station life, including: (i) the male dominated nature of station culture; (ii) the impact of interpersonal conflict, including gender based conflict and friction between scientists and trades workers; and (iii) the lack of anonymity associated with living and working with the same group of individuals, mainly men, for up to 12 months or more. The results are discussed within the context of the evolution of Antarctic station culture and recommendations are made in terms of the demography of expeditions, expeditioner selection and recruitment and the ongoing monitoring of Antarctic station culture. The study presents a framework that can be applied to groups and teams living and working in analogous isolated, confined and extreme work environments, including outer space missions.

  5. Impact of a 5-Day Expedition to Machu Picchu on Persons with Multiple Sclerosis

    Directory of Open Access Journals (Sweden)

    Marie Beatrice D’hooghe

    2014-01-01

    Full Text Available Persons with multiple sclerosis (MS are less physically active than nondiseased persons and often report low self-efficacy levels. In the context of an awareness project to promote physical activity and participation in MS, we addressed the impact of training for and participation in a unique expedition. Medical events, relapses, and self-reported neurological worsening were followed from 6 months before and up to 4 months afterwards. Validated patient-reported outcome measures were used to assess fatigue, self-efficacy in exercising, walking abilities, and illness perception. Nine participants completed the training, expedition, and observational study. Minor events, relapses, and/or neurological worsening were reported in six participants. The three participants with mild disability and no cardiovascular risk factors or comorbidities were free of medical and neurological events. We found a significant reduction of motor fatigue at last when compared with the first assessment. The reduction tended to be more evident in participants with mild disability (Expanded Disability Status Scale (EDSS <4 at baseline. Cognitive fatigue, self-efficacy, and self-reported walking abilities did not change significantly. Illness perceptions tended to be reduced over time in the domains of consequences, identity, and concerns. Overall, no major adverse events occurred.

  6. Impact of a 5-day expedition to machu picchu on persons with multiple sclerosis.

    Science.gov (United States)

    D'hooghe, Marie Beatrice; Feys, Peter; Deltour, Sam; Van de Putte, Isabelle; De Meue, Jan; Kos, Daphne; O Eijnde, Bert; Van Asch, Paul

    2014-01-01

    Persons with multiple sclerosis (MS) are less physically active than nondiseased persons and often report low self-efficacy levels. In the context of an awareness project to promote physical activity and participation in MS, we addressed the impact of training for and participation in a unique expedition. Medical events, relapses, and self-reported neurological worsening were followed from 6 months before and up to 4 months afterwards. Validated patient-reported outcome measures were used to assess fatigue, self-efficacy in exercising, walking abilities, and illness perception. Nine participants completed the training, expedition, and observational study. Minor events, relapses, and/or neurological worsening were reported in six participants. The three participants with mild disability and no cardiovascular risk factors or comorbidities were free of medical and neurological events. We found a significant reduction of motor fatigue at last when compared with the first assessment. The reduction tended to be more evident in participants with mild disability (Expanded Disability Status Scale (EDSS) <4 at baseline). Cognitive fatigue, self-efficacy, and self-reported walking abilities did not change significantly. Illness perceptions tended to be reduced over time in the domains of consequences, identity, and concerns. Overall, no major adverse events occurred.

  7. Osteogenic Differentiation Capacity of In Vitro Cultured Human Skeletal Muscle for Expedited Bone Tissue Engineering

    Directory of Open Access Journals (Sweden)

    Chunlei Miao

    2017-01-01

    Full Text Available Expedited bone tissue engineering employs the biological stimuli to harness the intrinsic regenerative potential of skeletal muscle to trigger the reparative process in situ to improve or replace biological functions. When genetically modified with adenovirus mediated BMP2 gene transfer, muscle biopsies from animals have demonstrated success in regenerating bone within rat bony defects. However, it is uncertain whether the human adult skeletal muscle displays an osteogenic potential in vitro when a suitable biological trigger is applied. In present study, human skeletal muscle cultured in a standard osteogenic medium supplemented with dexamethasone demonstrated significant increase in alkaline phosphatase activity approximately 24-fold over control at 2-week time point. More interestingly, measurement of mRNA levels revealed the dramatic results for osteoblast transcripts of alkaline phosphatase, bone sialoproteins, transcription factor CBFA1, collagen type I, and osteocalcin. Calcified mineral deposits were demonstrated on superficial layers of muscle discs after an extended 8-week osteogenic induction. Taken together, these are the first data supporting human skeletal muscle tissue as a promising potential target for expedited bone regeneration, which of the technologies is a valuable method for tissue repair, being not only effective but also inexpensive and clinically expeditious.

  8. Osteogenic Differentiation Capacity of In Vitro Cultured Human Skeletal Muscle for Expedited Bone Tissue Engineering.

    Science.gov (United States)

    Miao, Chunlei; Zhou, Lulu; Tian, Lufeng; Zhang, Yingjie; Zhang, Wei; Yang, Fanghong; Liu, Tianyi; Tang, Shengjian; Liu, Fangjun

    2017-01-01

    Expedited bone tissue engineering employs the biological stimuli to harness the intrinsic regenerative potential of skeletal muscle to trigger the reparative process in situ to improve or replace biological functions. When genetically modified with adenovirus mediated BMP2 gene transfer, muscle biopsies from animals have demonstrated success in regenerating bone within rat bony defects. However, it is uncertain whether the human adult skeletal muscle displays an osteogenic potential in vitro when a suitable biological trigger is applied. In present study, human skeletal muscle cultured in a standard osteogenic medium supplemented with dexamethasone demonstrated significant increase in alkaline phosphatase activity approximately 24-fold over control at 2-week time point. More interestingly, measurement of mRNA levels revealed the dramatic results for osteoblast transcripts of alkaline phosphatase, bone sialoproteins, transcription factor CBFA1, collagen type I, and osteocalcin. Calcified mineral deposits were demonstrated on superficial layers of muscle discs after an extended 8-week osteogenic induction. Taken together, these are the first data supporting human skeletal muscle tissue as a promising potential target for expedited bone regeneration, which of the technologies is a valuable method for tissue repair, being not only effective but also inexpensive and clinically expeditious.

  9. In-Situ Sampling and Characterization of Naturally Occurring Marine Methane Hydrate Using the D/V JOIDES Resolution

    Energy Technology Data Exchange (ETDEWEB)

    Rack, Frank; Schultheiss, Peter

    2005-12-31

    The primary accomplishments of the JOI Cooperative Agreement with DOE/NETL in this quarter were the implementation of a scientific ocean drilling expedition to study marine methane hydrates along the Cascadia margin, in the NE Pacific as part of Integrated Ocean Drilling Program (IODP) Expedition 311 using the R/V JOIDES Resolution and the deployment of all required equipment and personnel to provide the required services during this expedition. IODP Expedition 311 shipboard activities on the JOIDES Resolution began on August 28 and were concluded on October 28, 2005. New ODP Pressure Coring System (PCS) aluminum autoclave chambers were fabricated prior to the expedition. During the expedition, 16 PCS autoclaves containing pressure cores were X-rayed before and after depressurization using a modified Geotek MSCL-P (multi-sensor core logger-pressure) system. These PCS cores were density scanned using the MSCL-V (multi-sensor core logger-vertical) during depressurization to monitor gas evolution. The MSCL-V was set up in a 20-foot-long refrigerated container provided by Texas A&M University through the JOI contract with TAMRF. IODP Expedition 311 was the first time that PCS cores were examined before (using X-ray), during (using MSCL-V gamma density) and after (using X-ray) degassing to determine the actual volume and distribution of sediment and gas hydrate in the pressurized core, which will be important for more accurate determination of mass balances between sediment, gas, gas hydrate, and fluids in the samples collected. Geotek, Ltd was awarded a contract by JOI to provide equipment and personnel to perform pressure coring and related work on IODP Expedition 311 (Cascadia Margin Gas Hydrates). Geotek, Ltd. provided an automated track for use with JOI's infrared camera systems. Four auxiliary monitors showed infrared core images in real time to aid hydrate identification and sampling. Images were collected from 185 cores during the expedition and processed

  10. Sequencing at sea: challenges and experiences in Ion Torrent PGM sequencing during the 2013 Southern Line Islands Research Expedition

    NARCIS (Netherlands)

    Lim, Y.W.; Cuevas, D.A.; Silva, G.G.; Aguinaldo, K.; Dinsdale, E.A.; Haas, A.F.; Hatay, M.; Sanchez, S.E.; Wegley-Kelly, L.; Dutilh, B.E.; Harkins, T.T.; Lee, C.C.; Tom, W.; Sandin, S.A.; Smith, J.E.; Zgliczynski, B.; Vermeij, M.J.; Rohwer, F.; Edwards, R.A.

    2014-01-01

    Genomics and metagenomics have revolutionized our understanding of marine microbial ecology and the importance of microbes in global geochemical cycles. However, the process of DNA sequencing has always been an abstract extension of the research expedition, completed once the samples were returned

  11. Sequencing at sea : challenges and experiences in Ion Torrent PGM sequencing during the 2013 Southern Line Islands Research Expedition

    NARCIS (Netherlands)

    Lim, Yan Wei; Cuevas, Daniel A; Silva, Genivaldo Gueiros Z; Aguinaldo, Kristen; Dinsdale, Elizabeth A; Haas, Andreas F; Hatay, Mark; Sanchez, Savannah E; Wegley-Kelly, Linda; Dutilh, Bas E; Harkins, Timothy T; Lee, Clarence C; Tom, Warren; Sandin, Stuart A; Smith, Jennifer E; Zgliczynski, Brian; Vermeij, Mark J A; Rohwer, Forest; Edwards, Robert A

    2014-01-01

    Genomics and metagenomics have revolutionized our understanding of marine microbial ecology and the importance of microbes in global geochemical cycles. However, the process of DNA sequencing has always been an abstract extension of the research expedition, completed once the samples were returned

  12. 76 FR 64107 - Uranium From Russia; Scheduling of an Expedited Five-Year Review Concerning the Suspended...

    Science.gov (United States)

    2011-10-17

    ... COMMISSION Uranium From Russia; Scheduling of an Expedited Five-Year Review Concerning the Suspended Investigation on Uranium From Russia AGENCY: United States International Trade Commission. ACTION: Notice... of the suspended investigation on uranium from Russia would be likely to lead to continuation or...

  13. 76 FR 54206 - Gray Portland Cement and Clinker From Japan: Final Results of the Expedited Third Sunset Review...

    Science.gov (United States)

    2011-08-31

    ... International Trade Administration Gray Portland Cement and Clinker From Japan: Final Results of the Expedited... review of the antidumping duty order on gray portland cement and clinker from Japan. As a result of this... duty order on gray portland cement and clinker from Japan \\1\\ pursuant to section 751(c) of the Tariff...

  14. 76 FR 50252 - Gray Portland Cement and Cement Clinker From Japan; Scheduling of an Expedited Five-Year Review...

    Science.gov (United States)

    2011-08-12

    ... COMMISSION Gray Portland Cement and Cement Clinker From Japan; Scheduling of an Expedited Five-Year Review Concerning the Antidumping Duty Order on Gray Portland Cement and Cement Clinker From Japan AGENCY: United... cement and cement clinker from Japan would be likely to lead to continuation or recurrence of material...

  15. The Operation and Impact of Participants' Trans-Expedition Reflective Practice: Structuring and Optimising the Transfer Process

    Science.gov (United States)

    Hickman, Mark; Collins, Dave

    2014-01-01

    With gap year activities, including expeditions, for young people worth an estimated £2 billion annually, the subject of transfer (or ensuring that outcomes offer positive benefits to participants' general lives) from these experiences is an important topic in outdoor education. This paper argues that many of the claims for a positive behavioural…

  16. 76 FR 31360 - Paper Clips From China; Scheduling of an Expedited Five-Year Review Concerning the Antidumping...

    Science.gov (United States)

    2011-05-31

    ... COMMISSION Paper Clips From China; Scheduling of an Expedited Five-Year Review Concerning the Antidumping Duty Order on Paper Clips From China AGENCY: United States International Trade Commission. ACTION... revocation of the antidumping duty order on paper clips from China would be likely to lead to continuation or...

  17. 75 FR 13257 - Carbazole Violet Pigment 23 from India: Final Results of the Expedited Five-year (Sunset) Review...

    Science.gov (United States)

    2010-03-19

    ... International Trade Administration Carbazole Violet Pigment 23 from India: Final Results of the Expedited Five... Pigment 23 (CVP-23) ] from India pursuant to section 751(c) of the Tariff Act of 1930, as amended (the Act... merchandise includes the crude pigment in any form (e.g., dry powder, paste, wet cake) and finished pigment in...

  18. A Preliminary Exploration of the Influence of Short-Term Adventure-Based Expeditions on Levels of Resilience

    Science.gov (United States)

    Ewert, Alan; Yoshino, Aiko

    2008-01-01

    The purpose of this study was to investigate the effect of participation in a three-week adventure-based expedition on levels and types of resiliency. Defined as an individual constellation of characteristics and capacities that mitigate the impact of biological, psychological and social factors that threaten an individual's health (Kaplan, 1999;…

  19. 78 FR 68472 - Steel Nails From China; Scheduling of an Expedited Five-Year Review Concerning the Antidumping...

    Science.gov (United States)

    2013-11-14

    ... COMMISSION Steel Nails From China; Scheduling of an Expedited Five-Year Review Concerning the Antidumping Duty Order on Steel Nails From China AGENCY: United States International Trade Commission. ACTION... revocation of the antidumping duty order on steel nails from China would be likely to lead to continuation or...

  20. 77 FR 10477 - Silicon Metal From the People's Republic of China: Final Results of the Expedited Third Sunset...

    Science.gov (United States)

    2012-02-22

    ... International Trade Administration Silicon Metal From the People's Republic of China: Final Results of the... (``the Department'') initiated the third sunset review of the antidumping duty order on silicon metal..., the Department conducted an expedited (120-day) sunset review of the antidumping duty order on silicon...

  1. 78 FR 61334 - Silicon Metal From the Russian Federation: Final Results of the Expedited Second Sunset Review of...

    Science.gov (United States)

    2013-10-03

    ... International Trade Administration Silicon Metal From the Russian Federation: Final Results of the Expedited... silicon metal from the Russian Federation.\\1\\ The Department finds that revocation of this antidumping...-0197. SUPPLEMENTARY INFORMATION: Background The antidumping duty order on silicon metal from the...

  2. Scientific Results of the Surinam Expedition 1948-1949 : Part II. Zoology. No. 1. Crustacea Decapoda Macrura

    NARCIS (Netherlands)

    Holthuis, L.B.

    1950-01-01

    During the 1948-1949 Scientific Surinam Expedition, thorough zoological, botanical and geological explorations have been made in the coastal area and in the anterior mountain region of Dutch Guiana. The number of macrurous Decapods collected is large, though the number of species represented is

  3. 77 FR 18861 - Stainless Steel Bar From Brazil, India, Japan, and Spain; Scheduling of Expedited Five-Year Reviews

    Science.gov (United States)

    2012-03-28

    ... COMMISSION Stainless Steel Bar From Brazil, India, Japan, and Spain; Scheduling of Expedited Five-Year... orders on stainless steel bar from Brazil, India, Japan, and Spain would be likely to lead to... Inc. Co., Universal Stainless & Alloy Products, Inc., and Valbruna Slater Stainless, Inc. to be...

  4. 75 FR 62103 - Stainless Steel Plate in Coils From South Africa: Final Results of Expedited Sunset Review

    Science.gov (United States)

    2010-10-07

    ... International Trade Administration Stainless Steel Plate in Coils From South Africa: Final Results of Expedited... review of the countervailing duty order (``CVD'') on stainless steel plate in coils from South Africa... review of the CVD order on stainless steel plate in coils from South Africa pursuant to section 751(c) of...

  5. 76 FR 64105 - Stainless Steel Wire Rod From India; Scheduling of an Expedited Five-Year Review Concerning the...

    Science.gov (United States)

    2011-10-17

    ... COMMISSION Stainless Steel Wire Rod From India; Scheduling of an Expedited Five-Year Review Concerning the Antidumping Duty Order on Stainless Steel Wire Rod From India AGENCY: United States International Trade... determine whether revocation of the antidumping duty order on stainless steel wire rod from India would be...

  6. 76 FR 73592 - Certain Lined Paper Products From Indonesia: Final Results of the Expedited Sunset Review of the...

    Science.gov (United States)

    2011-11-29

    ... located 2\\3/8\\'' from the top of the front plastic cover and provides pen or pencil storage. Both ends of... with the outside of the polyester spine cover to the inside back cover. Both free ends (the ends not... and 19 CFR 351.218(e)(1)(ii)(C)(2), the Department conducted an expedited sunset review of the CVD...

  7. 77 FR 59896 - Honey From the People's Republic of China: Final Results of Expedited Sunset Review of the...

    Science.gov (United States)

    2012-10-01

    ... International Trade Administration Honey From the People's Republic of China: Final Results of Expedited Sunset... the second five-year (``sunset'') review of the antidumping duty order on honey from the People's... Department finds that revocation of the antidumping duty order on honey from the PRC would be likely to lead...

  8. 77 FR 65204 - Honey From China; Scheduling of an Expedited Five-Year Review Concerning the Antidumping Duty...

    Science.gov (United States)

    2012-10-25

    ... COMMISSION Honey From China; Scheduling of an Expedited Five-Year Review Concerning the Antidumping Duty Order on Honey From China AGENCY: United States International Trade Commission. ACTION: Notice. SUMMARY... antidumping duty order on honey from China would be likely to lead to continuation or recurrence of material...

  9. Two Expeditions to Capture Fort Duquesne: A Study in Understanding the Operational Environment and Attendant Failure (1755) and Success (1758)

    Science.gov (United States)

    2013-03-27

    O’Meara. With these titles as the basis for information and research, I next used the journal database JSTOR to browse the large amount of scholarly...journals for research on either Braddock’s or Forbes’s expedition. JSTOR introduced me to the works of Stanley Pargellis, Niles Anderson, Paul

  10. 77 FR 73021 - Lemon Juice From Argentina: Final Results of the Expedited First Sunset Review of the Suspended...

    Science.gov (United States)

    2012-12-07

    ... International Trade Administration Lemon Juice From Argentina: Final Results of the Expedited First Sunset... sunset review of the suspended antidumping duty investigation on lemon juice from Argentina. The..., 2012, the Department initiated a sunset review of the suspended antidumping duty investigation on lemon...

  11. 77 FR 777 - Fresh Garlic From the People's Republic of China: Final Results of Expedited Sunset Review of the...

    Science.gov (United States)

    2012-01-06

    ... International Trade Administration Fresh Garlic From the People's Republic of China: Final Results of Expedited...) initiated the third sunset review of the antidumping duty order fresh garlic from the People's Republic of... fresh garlic from the PRC pursuant to section 751(c) of the Act. See Initiation of Five-Year (``Sunset...

  12. The Ratu River Expedition - A Case Study in Successful Outreach Using Film and Social Media

    Science.gov (United States)

    Kerlow, Isaac

    2016-04-01

    The Ratu River Expedition is a 25-minute film about earthquakes in Nepal made for a general audience and for a Nepalese audience in particular. The movie explains basic facts about seismic activity in the Himalaya region and also basic preparedness concepts. It showcases the scientific research of the Structural Geology group at the Earth Observatory of Singapore in collaboration with the Department of Mines and Geology, Nepal. A social media campaign was developed to bring the movie to a large Nepalese audience, and the Nepali-subtitled version of the movie yielded over 79,000 post Likes in a Facebook outreach campaign. This presentation reviews the development, production, and distribution of this highly successful natural hazards documentary with scientific depth but designed for a mainstream audience. The full movie is being shown at EGU's Geo-Cinema 2016. http://raturiver.com/

  13. Wellfield strategy and recommendations for the 200 West Area carbon tetrachloride expedited response action

    Energy Technology Data Exchange (ETDEWEB)

    Rohay, V.J.

    1994-04-01

    On December 20, 1990, the US Environmental Protection Agency (EPA) and the Washington State Department of Ecology (Ecology) requested the US Department of Energy (DOE), Richland Field Office (RL) to proceed with the detailed planning, including nonintrusive field work, required to implement an Expedited Response Action (ERA) for removing carbon tetrachloride contamination in the unsaturated soils in the 200 West Area of the Hanford Site. The request was based on concerns that the carbon tetrachloride residing in the soils was continuing to spread to the groundwater and, if left unchecked, would significantly increase the area of groundwater contamination. The purpose of this ERA is to minimize carbon tetrachloride migration within the unsaturated zone beneath and,away from the carbon tetrachloride disposal sites in the 200 West Area.

  14. Sea ice thickness measurements collected during the LOMROG 2007 and 2009 expeditions

    DEFF Research Database (Denmark)

    Skourup, Henriette; Forsberg, René; Hanson, Susanne

    and 2009 we have collected a unique data set of late summer sea ice thickness, freeboard height and snow depth from the high Arctic Ocean during the time of the annual minimum sea ice extent. The data were collected by on-the-ground drilling and EM measurements. Here we give a brief overview of the data....... The processes involved in the declining sea ice are not fully understood. This is primarily due to a lack of knowledge of the variety and high spatial resolution of, e.g. snow depth, ice thickness and morphology, which are difficult or impossible to obtain remotely. During the LOMROG expeditions in 2007...... collection, as well as the results including the freeboard-to-sea-ice thickness conversion factor, which is used when interpreting freeboard heights measured by remote sensing....

  15. ArCEs - A digital archive of Italian Colonial Cartography and Scientific Expeditions

    Directory of Open Access Journals (Sweden)

    Irene Calloud

    2013-02-01

    Full Text Available ArcCEs is a study for developing a digital archive on Italian scientific expeditions in Northern and Eastern Africa and the former Italian colonies (19th–20th centuries. The aim of the project is to assess, protect and enhance an important corpus of documents (historical cartographies, photographs, scientific papers and archive documents distributed among public archives and private collections. The database structure is based on the Dublin Core metadata standard. The information system is designed to integrate and make interoperable digital resources, to ensure standardized and complex indexing, and to support advanced retrieval, according to the standards in use. The geolocation of the resources in a GIS environment can display query results in the Google Earth environment.

  16. Early scientific expeditions and local encounters: new perspectives on Carsten Niebuhr and 'The Arabian Journey'

    DEFF Research Database (Denmark)

    knowledge about natural history and detailed geography of the interior of the continents other than Europe, as well as scholarly understanding of foreign cultures, both ancient and contemporary, was still limited. Increasing focus on land-based travels in the eighteenth century and onwards meant more......, the papers in these proceedings paint a varied picture of eighteenth and early nineteenth century scientific expeditions and scholarly travel. In the eighteenth century the considerate and careful approach of Niebuhr and Forsskål in their dealing with local people was new or at least not so common......, and Niebuhr and Forsskål’s methods in acquiring local knowledge seem to mark a new departure for the study of foreign cultures and their interaction with nature. A conclusion drawn by several of the papers in this symposium is that, in spite of careful preparations, elaborate apodemics and detailed...

  17. Illustrators of the New World. The Image in the Spanish Scientific Expeditions of the Enlightenment

    Directory of Open Access Journals (Sweden)

    Puig-Samper, Miguel Ángel

    2012-12-01

    Full Text Available In the Eighteenth Century, with the boom in the exploration of the Earth, most travellers and explorers had painters and illustrators at their sides who recorded their adventures, even their deaths, the exotic locations they visited, the aborigines, the landscapes or the strange creatures or plants that inhabited them. The presence of artists would increase in these types of exploration companies, sent by Spain, in order to recognise the natural resources and the imperial control of their territories. We take as a starting point Löfling’s expedition, in which naturalist artists seek to comply with the requirements of the Linnaean classification system then, looking at the case of Francisco Requena, who cartographically represented the territory and drew the activities of his own expedition members along the boundaries with the Portuguese empire. Likewise, we analyze expeditions known as “Botanical” to the different viceroyalties, which attempted to transmit the American nature idealized in a few “types” that were drawn and recorded to make the new species and the wealth of the Empire known, until finally arriving at the expedition of Malaspina, in which there is a step towards the depiction of the imperial landscape.

    En el siglo XVIII, con la explosión de la exploración de la Tierra, la mayoría de los viajeros y expedicionarios llevan a su lado a pintores y dibujantes que dejan constancia de sus aventuras, incluso de su muerte, de los lugares exóticos visitados, los aborígenes, el paisaje o las extrañas criaturas vegetales o animales que las habitan. La presencia de artistas irá incrementándose en este tipo de empresas de exploración enviadas por España para el reconocimiento de los recursos naturales y el control imperial de sus territorios. Tomamos como punto de partida la expedición de Löfling, en la que los dibujantes naturalistas buscan cumplir con los requisitos del sistema linneano de clasificación, pasando

  18. caNanoLab: data sharing to expedite the use of nanotechnology in biomedicine

    Science.gov (United States)

    Gaheen, Sharon; Hinkal, George W.; Morris, Stephanie A.; Lijowski, Michal; Heiskanen, Mervi

    2014-01-01

    The use of nanotechnology in biomedicine involves the engineering of nanomaterials to act as therapeutic carriers, targeting agents and diagnostic imaging devices. The application of nanotechnology in cancer aims to transform early detection, targeted therapeutics and cancer prevention and control. To assist in expediting and validating the use of nanomaterials in biomedicine, the National Cancer Institute (NCI) Center for Biomedical Informatics and Information Technology, in collaboration with the NCI Alliance for Nanotechnology in Cancer (Alliance), has developed a data sharing portal called caNanoLab. caNanoLab provides access to experimental and literature curated data from the NCI Nanotechnology Characterization Laboratory, the Alliance and the greater cancer nanotechnology community. PMID:25364375

  19. Sustainable Foods and Medicines Support Vitality, Sex and Longevity for a 100-Year Starship Expedition

    Science.gov (United States)

    Edwards, M. R.

    Extended space flight requires foods and medicines that sustain crew health and vitality. The health and therapeutic needs for the entire crew and their children for a 100-year space flight must be sustainable. The starship cannot depend on resupply or carry a large cargo of pharmaceuticals. Everything in the starship must be completely recyclable and reconstructable, including food, feed, textiles, building materials, pharmaceuticals, vaccines, and medicines. Smart microfarms will produce functional foods with superior nutrition and sensory attributes. These foods provide high-quality protein and nutralence (nutrient density), that avoids obesity, diabetes, and other Western diseases. The combination of functional foods, lifestyle actions, and medicines will support crew immunity, energy, vitality, sustained strong health, and longevity. Smart microfarms enable the production of fresh medicines in hours or days, eliminating the need for a large dispensary, which eliminates concern over drug shelf life. Smart microfarms are adaptable to the extreme growing area, resource, and environmental constraints associated with an extended starship expedition.

  20. Early scientific expeditions and local encounters: new perspectives on Carsten Niebuhr and 'The Arabian Journey'

    DEFF Research Database (Denmark)

    knowledge about natural history and detailed geography of the interior of the continents other than Europe, as well as scholarly understanding of foreign cultures, both ancient and contemporary, was still limited. Increasing focus on land-based travels in the eighteenth century and onwards meant more...... observations were brought back to Europe and communicated both to other scholars and to the general reading public. The contrasts between the “gentleman travellers” or the authors of entertaining travelogues and the scholarly approach of the Danish expedition are also apparent in several accounts. Together......, and Niebuhr and Forsskål’s methods in acquiring local knowledge seem to mark a new departure for the study of foreign cultures and their interaction with nature. A conclusion drawn by several of the papers in this symposium is that, in spite of careful preparations, elaborate apodemics and detailed...

  1. World as The Biggest Clasroom. Travel as The Best Lesson. Independent Scientific School Expeditions.

    Science.gov (United States)

    Oleksik, Ireneusz; Lorek, Grzegorz; Dacy-Ignatiuk, Katarzyna

    2013-04-01

    We are a group of teachers from Poland who think that classroom lessons are not enough for our pupils to understand the world. We had a dream to take our students and show them the most beautiful places and phenomena on the Earth. But how to do it? Though today's travelling is so easy as never before, there are still some problems for young Poles - not only funding but also philosophy of travelling. It looks that we found a solution a few years ago - why not to organise quite independent school scientific expeditions? Without travel agencies and agents we can reduce costs of travelling 2-3 times! And we did it! We buy cheap flight tickets, fly to our destination and then... we must manage with all problems ourselves. We sleep in tents or budget hostels, use local means of transport and eat food from cheap markets or street eating places. Our motto is: "To see as much as possible for the minimum money". There are many more advantages - we decide where to go and how much time we spend in one area, we can change our route in every moment if something appears worth seeing. Our small groups are very mobile, sometimes local people invite us to visit their houses (like in Iran or Morocco). Expeditions allow students to watch, feel, touch, taste and smell phenomena, places and organisms which they could only read about in a classroom and to understand people from other cultures and religions. The list of nature and culture jewels that we have already seen is still growing - sands and oasis of Sahara, snow peaks of Himalayas, salt waters of Caspian Sea in Iran, geysers, volcanoes and glaciers of Iceland, the biggest sea birds colonies and whales in the North Atlantic, ancient cities - Fez, Marrakesh, Esfahan, Varanasi and Yazd.

  2. Attempt of Serendipitous Science During the Mojave Volatile Prospector Field Expedition

    Science.gov (United States)

    Roush, T. L.; Colaprete, A.; Heldmann, J.; Lim, D. S. S.; Cook, A.; Elphic, R.; Deans, M.; Fluckiger, L.; Fritzler, E.; Hunt, David

    2015-01-01

    On 23 October a partial solar eclipse occurred across parts of the southwest United States between approximately 21:09 and 23:40 (UT), with maximum obscuration, 36%, occurring at 22:29 (UT). During 21-26 October 2014 the Mojave Volatile Prospector (MVP) field expedition deployed and operated the NASA Ames Krex2 rover in the Mojave desert west of Baker, California (Fig. 1, bottom). The MVP field expedition primary goal was to characterize the surface and sub-surface soil moisture properties within desert alluvial fans, and as a secondary goal to provide mission operations simulations of the Resource Prospector (RP) mission to a Lunar pole. The partial solar eclipse provided an opportunity during MVP operations to address serendipitous science. Science instruments on Krex2 included a neutron spectrometer, a near-infrared spectrometer with associated imaging camera, and an independent camera coupled with software to characterize the surface textures of the areas encountered. All of these devices are focused upon the surface and as a result are downward looking. In addition to these science instruments, two hazard cameras are mounted on Krex2. The chief device used to monitor the partial solar eclipse was the engineering development unit of the Near-Infrared Volatile Spectrometer System (NIRVSS) near-infrared spectrometer. This device uses two separate fiber optic fed Hadamard transform spectrometers. The short-wave and long-wave spectrometers measure the 1600-2400 and 2300-3400 nm wavelength regions with resolutions of 10 and 13 nm, respectively. Data are obtained approximately every 8 seconds. The NIRVSS stares in the opposite direction as the front Krex2.

  3. The aircraft energy efficiency active controls technology program

    Science.gov (United States)

    Hood, R. V., Jr.

    1977-01-01

    Broad outlines of the NASA Aircraft Energy Efficiency Program for expediting the application of active controls technology to civil transport aircraft are presented. Advances in propulsion and airframe technology to cut down on fuel consumption and fuel costs, a program for an energy-efficient transport, and integrated analysis and design technology in aerodynamics, structures, and active controls are envisaged. Fault-tolerant computer systems and fault-tolerant flight control system architectures are under study. Contracts with leading manufacturers for research and development work on wing-tip extensions and winglets for the B-747, a wing load alleviation system, elastic mode suppression, maneuver-load control, and gust alleviation are mentioned.

  4. Microbial diversity in Cenozoic sediments recovered from the Lomonosov Ridge in the Central Arctic basin.

    Science.gov (United States)

    Forschner, Stephanie R; Sheffer, Roberta; Rowley, David C; Smith, David C

    2009-03-01

    The current understanding of microbes inhabiting deeply buried marine sediments is based largely on samples collected from continental shelves in tropical and temperate latitudes. The geographical range of marine subsurface coring was expanded during the Integrated Ocean Drilling Program Arctic Coring Expedition (IODP ACEX). This expedition to the ice-covered central Arctic Ocean successfully cored the entire 428 m sediment stack on the Lomonosov Ridge during August and September 2004. The recovered cores vary from siliciclastic sediment low in organic carbon (deep (> 200 m below sea floor) sulfate reduction zone. The diversity of microbes within each zone was assessed using 16S rRNA phylogenetic markers. Bacterial 16S rRNA genes were successfully amplified from each of the biogeochemical zones, while archaea was only amplified from the deep sulfate reduction zone. The microbial communities at each zone are phylogenetically different and are most closely related to those from other deep subsurface environments.

  5. Underway Sampling of Marine Inherent Optical Properties on the Tara Oceans Expedition as a Novel Resource for Ocean Color Satellite Data Product Validation

    Science.gov (United States)

    Werdell, P. Jeremy; Proctor, Christopher W.; Boss, Emmanuel; Leeuw, Thomas; Ouhssain, Mustapha

    2013-01-01

    Developing and validating data records from operational ocean color satellite instruments requires substantial volumes of high quality in situ data. In the absence of broad, institutionally supported field programs, organizations such as the NASA Ocean Biology Processing Group seek opportunistic datasets for use in their operational satellite calibration and validation activities. The publicly available, global biogeochemical dataset collected as part of the two and a half year Tara Oceans expedition provides one such opportunity. We showed how the inline measurements of hyperspectral absorption and attenuation coefficients collected onboard the R/V Tara can be used to evaluate near-surface estimates of chlorophyll-a, spectral particulate backscattering coefficients, particulate organic carbon, and particle size classes derived from the NASA Moderate Resolution Imaging Spectroradiometer onboard Aqua (MODISA). The predominant strength of such flow-through measurements is their sampling rate-the 375 days of measurements resulted in 165 viable MODISA-to-in situ match-ups, compared to 13 from discrete water sampling. While the need to apply bio-optical models to estimate biogeochemical quantities of interest from spectroscopy remains a weakness, we demonstrated how discrete samples can be used in combination with flow-through measurements to create data records of sufficient quality to conduct first order evaluations of satellite-derived data products. Given an emerging agency desire to rapidly evaluate new satellite missions, our results have significant implications on how calibration and validation teams for these missions will be constructed.

  6. Dive Data from Expedition Information System (EIS) for Islands in the Stream 2002 - Pharmaceutical Discovery, Vision, and Bioluminescence - Office of Ocean Exploration

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The Expeditions Information System (EIS) contains information recorded by the NOAA Office of Ocean Exploration's data manager during the 2002 "Islands in the Stream...

  7. Investigation of environmental radioactivity in waste dumping areas of the far eastern seas. JAERI`s activities in the 1st Japanese-Korean-Russian joint expedition 1994

    Energy Technology Data Exchange (ETDEWEB)

    Amano, Hikaru; Matsunaga, Takeshi [Japan Atomic Energy Research Inst., Tokai, Ibaraki (Japan). Tokai Research Establishment; Yabuuchi, Noriaki

    1996-10-01

    Large quantities of radioactive waste have been dumped in the Far Eastern Sea by the former USSR and Russia. In order to survey marine radioactive contamination in the Far Eastern Sea, the first Japanese-Korean-Russian joint expedition was conducted according to the governmental agreement. The joint expedition was conducted at the areas of the Russian radioactive waste dumping site from March 18 1994 to April 6, 1994. JAERI participated in this expedition according to the request from STA Japan, and conducted mainly on-board measurement of marine radioactivities. The results showed that the radionuclides concentrations in seawater and seabed sediment samples from the study site were not different from those in the western North Pacific. This report summarises JAERI`s activities in the expedition. Final report by Japanese-Korean-Russian government and IAEA is annexed. (author)

  8. Integrated ocean drilling program expedition 341 Preliminary report: Southern Alaska margin- Interactions of tectonics, climate, and sedimentation

    Digital Repository Service at National Institute of Oceanography (India)

    Jaeger, J.M.; Asahi, H.; Gulick, S.S.; Bahlburg, H.; LeVay, L.J.; Belanger, C.L.; Slagle, A; Berbel, G.B.B.; Drab, L.; Childress, L.B.; Cowan, E.A; Konno, S.; Forwick, M.; Marz, C.E.; Fukumura, A; Matsuzaki, K.M.; Ge, S.; McClymont, E.L.; Gupta, S.M.; et al.

    Global climate during the Neogene is distinguished by the transition into a colder, more variable world dominated by the onset and intensification of major Northern Hemisphere glaciations. This transition to the icehouse world corresponds with a...

  9. Geologic implications of gas hydrates in the offshore of India: Results of the National Gas Hydrate Program Expedition 01

    Digital Repository Service at National Institute of Oceanography (India)

    Collett, T.S.; Boswell, R.; Cochran, J.R.; Kumar, P.; Lall, M.; Mazumdar, A.; Ramana, M.V.; Ramprasad, T.; Riedel, M.; Sain, K.; Sathe, A.V.; Vishwanath, K.; NGHP Expedition 01 Scientific Party

    hours and assisted by mammal watchers posted at both the bow and stern of the ship. No mammals were observed during any of the VSP operations. 2.4.5. NGHP-01 operational summary For organizational purposes, NGHP-01 was divided into five operational...

  10. CRITICALITY SAFETY LIMIT EVALUATION PROGRAM (CSLEP) & QUICK SCREENS, ANSWERS TO EXPEDITED PROCESSING LEGACY CRITICALITY SAFETY LIMITS & EVALUATIONS

    Energy Technology Data Exchange (ETDEWEB)

    TOFFER, H.

    2006-02-21

    Since the end of the cold war, the need for operating weapons production facilities has faded. Criticality Safety Limits and controls supporting production modes in these facilities became outdated and furthermore lacked the procedure based rigor dictated by present day requirements. In the past, in many instances, the formalism of present day criticality safety evaluations was not applied. Some of the safety evaluations amounted to a paragraph in a notebook with no safety basis and questionable arguments with respect to double contingency criteria. When material stabilization, clean out, and deactivation activities commenced, large numbers of these older criticality safety evaluations were uncovered with limits and controls backed up by tenuous arguments. A dilemma developed: on the one hand, cleanup activities were placed on very aggressive schedules; on the other hand, a highly structured approach to limits development was required and applied to the cleanup operations. Some creative approaches were needed to cope with the limits development process.

  11. Of Images, Archives, and Anonymity: Glacier Photographs from Louise Arner Boyd's East Greenland Expeditions, 1933, 1937, and 1938

    Science.gov (United States)

    Nelson, F. E.; Peschel, S. M.; Hall, D. K.

    2010-12-01

    Louise A. Boyd (1887-1972) was raised to wealth and privilege in San Raphael, CA. Her inherited fortune allowed unlimited travel, and in 1924 she arrived in Spitsbergen as a tourist. Infatuated by Arctic landscapes, Boyd resolved to return north in a more assertive role and ran three "preliminary" expeditions to Greenland, in 1926, 1928, and 1931. Boyd’s expeditions to East Greenland in 1933, 1937, and 1938 were predictive of the type of campaign that after WWII would characterize government-sponsored and international scientific efforts. “Planned as a unit,” these campaigns, sponsored by the American Geographical Society (AGS), were thoroughly integrated scientific expeditions incorporating glaciology, periglacial and glacial geomorphology, bedrock geology, botany, hydrography, topographic surveys, tides and currents, and magnetic observations within representative areas. The goal of the expeditions was to provide comprehensive characterization of the physical environment. The volumes resulting from this work contain many large-scale hydrographic and topographic maps, photomosaics, glacier maps, and chapters on the geology, glacial history, botany, and hydrology of the region. Boyd received extensive publicity for her Arctic expeditions, although much of it was concerned with the novelty of expeditions to remote locations being led by a woman. Boyd’s expeditions employed scientists who eventually became highly influential in their respective fields. Boyd employed, among others, the earth scientists J.H. Bretz, R.F. Flint, and A.L. Washburn. Other important personnel on these expeditions included AGS cartographer/surveyor O.M. Miller and his assistant, W.A. Wood, who employed novel ground-based photogrammetric techniques to construct a series of glacier maps at scales as large as 1:5000. The maps featured detailed error analyses, and are probably the first large-scale maps of known accuracy to be made of the Greenland Ice Sheet’s outlet glaciers. Boyd

  12. Scientific travel in the Atlantic world: the French expedition to Gorée and the Antilles, 1681-1683.

    Science.gov (United States)

    Dew, Nicholas

    2010-03-01

    Although historians have long recognized the importance of long-range scientific expeditions in both the practice and culture of eighteenth- and nineteenth-century science, it is less well understood how this form of scientific organization emerged and became established in the seventeenth and early eighteenth centuries. In the late seventeenth century new European scientific institutions tried to make use of globalized trade networks for their own ends, but to do so proved difficult. This paper offers a case history of one such expedition, the voyage sponsored by the French Académie royale des sciences to Gorée (in modern Senegal) and the Caribbean islands of Guadeloupe and Martinique in 1681-3. The voyage of Varin, Deshayes and de Glos reveals how the process of travel itself caused problems for instruments and observers alike.

  13. Pb distribution in bones from the Franklin expedition: synchrotron X-ray fluorescence and laser ablation/mass spectroscopy

    Science.gov (United States)

    Martin, Ronald Richard; Naftel, Steven; Macfie, Sheila; Jones, Keith; Nelson, Andrew

    2013-04-01

    Synchrotron micro-X-ray Fluorescence has been used to map the metal distribution in selected bone fragments representative of remains associated with the Franklin expedition. In addition, laser ablation mass spectroscopy using a 25 μm diameter circular spot was employed to compare the Pb isotope distributions in small regions within the bone fragments. The X-ray Fluorescence mapping shows Pb to be widely distributed in the bone while the Pb isotope ratios obtained by laser ablation within small areas representative of bone with different Pb exchange rates do not show statistically significant differences. These results are inconsistent with the hypothesis that faulty solder seals in tinned meat were the principle source of Pb in the remains of the expedition personnel.

  14. Earth Expeditions: Telling the stories of eight NASA field campaigns by focusing on the human side of science

    Science.gov (United States)

    Bell, S.

    2016-12-01

    NASA's Earth Right Now communication team kicked off an ambitious multimedia campaign in March 2016 to tell the stories of eight major field campaigns studying regions of critical change from the land, sea and air. Earth Expeditions focused on the human side of science, with live reporting from the field, behind-the-scenes images and videos, and extended storytelling over a six-month period. We reported from Greenland to Namibia, from the eastern United States to the South Pacific. Expedition scientists explored ice sheets, air quality, coral reefs, boreal forests, marine ecosystems and greenhouse gases. All the while the campaign communications team was generating everything from blog posts and social media shareables, to Facebook Live events and a NASA TV series. We also participated in community outreach events and pursued traditional media opportunities. A massive undertaking, we will share lessons learned, best practices for social media and some of our favorite moments when science communication touched our audience's lives.

  15. Comparison and significance of auroral studies during the Swedish and Russian bilateral expedition to Spitsbergen in 1899–1900

    Directory of Open Access Journals (Sweden)

    S. Chernouss

    2008-05-01

    Full Text Available Results of measurements and visual observations of aurora at Spitsbergen, carried out by the joint Swedish-Russian expedition during 1899–1900, are described. Auroral observations took place during the great bilateral Arc-of-Meridian expedition, which was patronized by the Swedish Royal Family and the Russian Imperial Family. The Russian-Swedish Arc-of-Meridian measurements were closely coordinated but auroral measurements from the two sites in the Spitsbergen Archipelago were almost independent of each other. The basic auroral data for our presentation are reports of the Russian astronomer Josef Sykora and the Swedish geophysicist Jonas Westman. Both scientists used similar types of photo cameras and spectrographs, which were the best at that time and were made in Potsdam by Toepfer. Detailed descriptions of the optical devices and the system of spectral calibration are presented. A Toepfer spectrograph, possibly the one used by Westman, is still kept at IRF in Kiruna. We present a comparative analysis of auroral data from the Russian and Swedish stations on three themes: visual observations of aurora, describing features of auroral forms and giving us statistical data on aurora occurrence and the heights of aurora, photos of aurora, and auroral spectra. It is shown that the observations contain enough data to construct an auroral oval and to determine the heights of aurora. The expedition obtained the first photographic observations of the aurora in the Arctic. The auroral spectra demonstrate a high spectral resolution and show not only the main auroral emissions in the blue-green spectral range but also some weak emissions in the violet and ultraviolet region. All data are interpreted from a modern point of view. The Russian-Swedish 1899–1900 expedition carried out the first complex auroral investigations in the Arctic using optical instruments and presented well documented data and new results.

  16. A short note on the cephalopods sampled in the Angola Basin during the DIVA I-expedition

    OpenAIRE

    Piatkowski, Uwe; Diekmann, Rabea

    2005-01-01

    Five cephalopods, all belonging to different species, were identified from deep-sea trawl samples conducted during the DIVA 1-expedition of RV “Meteor” in the Angola Basin in July 2000. These were the teuthoid squids Bathyteuthis abyssicola, Brachioteuthis riisei, Mastigoteuthis atlantica, Galiteuthis armata, and the finned deep-sea octopus Grimpoteuthis wuelkeri. The present study contributes information on size, morphometry, biology and distribution of the species form this unique cephalopo...

  17. The health of nine Royal Naval Arctic crews, 1848 to 1854: implications for the lost Franklin Expedition

    OpenAIRE

    Millar, Keith; Bowman, Adrian W.; Battersby, William; Richard R. Welbury

    2016-01-01

    Medical factors including tuberculosis, scurvy, lead poisoning and botulism have been proposed to explain the high death rate prior to desertion of the ships on Sir John Franklin's expedition of 1845–1848 but their role remains unclear because the surgeons’ Sick books which recorded illness on board have eluded discovery. In their absence, this study examines the Sick books of Royal Naval search squadrons sent in search of Franklin, and which encountered similar conditions to his ships, to co...

  18. FROM THE LEWIS AND CLARK EXPEDITION TO IBM, DELL, AND SOUTHWEST AIRLINES: TEACHING HISTORY AND LEADERSHIP TO BUSINESS STUDENTS

    OpenAIRE

    Jeffrey J. Matthews

    2006-01-01

    History is not a tomb of dead facts but a resource that can inform and improve everyday decision making. Experience as an analytical tool is invaluable for solving problems in changing and competitive environments. “From the Lewis and Clark Expedition,” which coincides with the National Lewis & Clark Bicentennial Commemoration (2003—2006), demonstrates how contemporary business concepts of visionary leadership, systematic planning, and organizational climate were instrumental to the succe...

  19. Sequencing at sea: challenges and experiences in Ion Torrent PGM sequencing during the 2013 Southern Line Islands Research Expedition

    Directory of Open Access Journals (Sweden)

    Yan Wei Lim

    2014-08-01

    Full Text Available Genomics and metagenomics have revolutionized our understanding of marine microbial ecology and the importance of microbes in global geochemical cycles. However, the process of DNA sequencing has always been an abstract extension of the research expedition, completed once the samples were returned to the laboratory. During the 2013 Southern Line Islands Research Expedition, we started the first effort to bring next generation sequencing to some of the most remote locations on our planet. We successfully sequenced twenty six marine microbial genomes, and two marine microbial metagenomes using the Ion Torrent PGM platform on the Merchant Yacht Hanse Explorer. Onboard sequence assembly, annotation, and analysis enabled us to investigate the role of the microbes in the coral reef ecology of these islands and atolls. This analysis identified phosphonate as an important phosphorous source for microbes growing in the Line Islands and reinforced the importance of L-serine in marine microbial ecosystems. Sequencing in the field allowed us to propose hypotheses and conduct experiments and further sampling based on the sequences generated. By eliminating the delay between sampling and sequencing, we enhanced the productivity of the research expedition. By overcoming the hurdles associated with sequencing on a boat in the middle of the Pacific Ocean we proved the flexibility of the sequencing, annotation, and analysis pipelines.

  20. Sequencing at sea: challenges and experiences in Ion Torrent PGM sequencing during the 2013 Southern Line Islands Research Expedition.

    Science.gov (United States)

    Lim, Yan Wei; Cuevas, Daniel A; Silva, Genivaldo Gueiros Z; Aguinaldo, Kristen; Dinsdale, Elizabeth A; Haas, Andreas F; Hatay, Mark; Sanchez, Savannah E; Wegley-Kelly, Linda; Dutilh, Bas E; Harkins, Timothy T; Lee, Clarence C; Tom, Warren; Sandin, Stuart A; Smith, Jennifer E; Zgliczynski, Brian; Vermeij, Mark J A; Rohwer, Forest; Edwards, Robert A

    2014-01-01

    Genomics and metagenomics have revolutionized our understanding of marine microbial ecology and the importance of microbes in global geochemical cycles. However, the process of DNA sequencing has always been an abstract extension of the research expedition, completed once the samples were returned to the laboratory. During the 2013 Southern Line Islands Research Expedition, we started the first effort to bring next generation sequencing to some of the most remote locations on our planet. We successfully sequenced twenty six marine microbial genomes, and two marine microbial metagenomes using the Ion Torrent PGM platform on the Merchant Yacht Hanse Explorer. Onboard sequence assembly, annotation, and analysis enabled us to investigate the role of the microbes in the coral reef ecology of these islands and atolls. This analysis identified phosphonate as an important phosphorous source for microbes growing in the Line Islands and reinforced the importance of L-serine in marine microbial ecosystems. Sequencing in the field allowed us to propose hypotheses and conduct experiments and further sampling based on the sequences generated. By eliminating the delay between sampling and sequencing, we enhanced the productivity of the research expedition. By overcoming the hurdles associated with sequencing on a boat in the middle of the Pacific Ocean we proved the flexibility of the sequencing, annotation, and analysis pipelines.

  1. Viral to metazoan marine plankton nucleotide sequences from the Tara Oceans expedition.

    Science.gov (United States)

    Alberti, Adriana; Poulain, Julie; Engelen, Stefan; Labadie, Karine; Romac, Sarah; Ferrera, Isabel; Albini, Guillaume; Aury, Jean-Marc; Belser, Caroline; Bertrand, Alexis; Cruaud, Corinne; Da Silva, Corinne; Dossat, Carole; Gavory, Frédérick; Gas, Shahinaz; Guy, Julie; Haquelle, Maud; Jacoby, E'krame; Jaillon, Olivier; Lemainque, Arnaud; Pelletier, Eric; Samson, Gaëlle; Wessner, Mark; Acinas, Silvia G; Royo-Llonch, Marta; Cornejo-Castillo, Francisco M; Logares, Ramiro; Fernández-Gómez, Beatriz; Bowler, Chris; Cochrane, Guy; Amid, Clara; Hoopen, Petra Ten; De Vargas, Colomban; Grimsley, Nigel; Desgranges, Elodie; Kandels-Lewis, Stefanie; Ogata, Hiroyuki; Poulton, Nicole; Sieracki, Michael E; Stepanauskas, Ramunas; Sullivan, Matthew B; Brum, Jennifer R; Duhaime, Melissa B; Poulos, Bonnie T; Hurwitz, Bonnie L; Pesant, Stéphane; Karsenti, Eric; Wincker, Patrick

    2017-08-01

    A unique collection of oceanic samples was gathered by the Tara Oceans expeditions (2009-2013), targeting plankton organisms ranging from viruses to metazoans, and providing rich environmental context measurements. Thanks to recent advances in the field of genomics, extensive sequencing has been performed for a deep genomic analysis of this huge collection of samples. A strategy based on different approaches, such as metabarcoding, metagenomics, single-cell genomics and metatranscriptomics, has been chosen for analysis of size-fractionated plankton communities. Here, we provide detailed procedures applied for genomic data generation, from nucleic acids extraction to sequence production, and we describe registries of genomics datasets available at the European Nucleotide Archive (ENA, www.ebi.ac.uk/ena). The association of these metadata to the experimental procedures applied for their generation will help the scientific community to access these data and facilitate their analysis. This paper complements other efforts to provide a full description of experiments and open science resources generated from the Tara Oceans project, further extending their value for the study of the world's planktonic ecosystems.

  2. A Genetic Algorithm Approach for Expedited Crossing of Emergency Vehicles in Connected and Autonomous Intersection Traffic

    Directory of Open Access Journals (Sweden)

    Qiang Lu

    2017-01-01

    Full Text Available This paper proposes an intersection control algorithm which aims to determine an efficient vehicle-passing sequence that allows the emergency vehicle to cross an intersection as soon as possible while the travel times of other vehicles are minimally affected. When there are no emergency vehicles within the intersection area, the vehicles are controlled by the DICA that we proposed in our earlier work. When there are emergency vehicles entering the communication range, we prioritize emergency vehicles through optimal ordering of vehicles. Since the number of possible vehicle-passing sequences increases rapidly with the number of vehicles, finding an efficient sequence of vehicles in a short time is the main challenge of the study. A genetic algorithm is proposed to solve the optimization problem which finds the optimal vehicle sequence that gives the emergency vehicles the highest priority. The efficiency of the proposed approach for expedited crossing of emergency vehicles is validated through comparisons with DICA and a reactive traffic light algorithm through extensive simulations. The results show that the proposed genetic algorithm is able to decrease the travel times of emergency vehicles significantly in light and medium traffic volumes without causing any noticeable performance degradation of normal vehicles.

  3. State-level gonorrhea rates and expedited partner therapy laws: insights from time series analyses.

    Science.gov (United States)

    Owusu-Edusei, K; Cramer, R; Chesson, H W; Gift, T L; Leichliter, J S

    2017-06-01

    In this study, we examined state-level monthly gonorrhea morbidity and assessed the potential impact of existing expedited partner therapy (EPT) laws in relation to the time that the laws were enacted. Longitudinal study. We obtained state-level monthly gonorrhea morbidity (number of cases/100,000 for males, females and total) from the national surveillance data. We used visual examination (of morbidity trends) and an autoregressive time series model in a panel format with intervention (interrupted time series) analysis to assess the impact of state EPT laws based on the months in which the laws were enacted. For over 84% of the states with EPT laws, the monthly morbidity trends did not show any noticeable decreases on or after the laws were enacted. Although we found statistically significant decreases in gonorrhea morbidity within four of the states with EPT laws (Alaska, Illinois, Minnesota, and Vermont), there were no significant decreases when the decreases in the four states were compared contemporaneously with the decreases in states that do not have the laws. We found no impact (decrease in gonorrhea morbidity) attributable exclusively to the EPT law(s). However, these results do not imply that the EPT laws themselves were not effective (or failed to reduce gonorrhea morbidity), because the effectiveness of the EPT law is dependent on necessary intermediate events/outcomes, including sexually transmitted infection service providers' awareness and practice, as well as acceptance by patients and their partners. Published by Elsevier Ltd.

  4. Ames expedited site characterization demonstration at the former manufactured gas plant site, Marshalltown, Iowa

    Energy Technology Data Exchange (ETDEWEB)

    Bevolo, A.J.; Kjartanson, B.H.; Wonder, J.D.

    1996-03-01

    The goal of the Ames Expedited Site Characterization (ESC) project is to evaluate and promote both innovative technologies (IT) and state-of-the-practice technologies (SOPT) for site characterization and monitoring. In April and May 1994, the ESC project conducted site characterization, technology comparison, and stakeholder demonstration activities at a former manufactured gas plant (FMGP) owned by Iowa Electric Services (IES) Utilities, Inc., in Marshalltown, Iowa. Three areas of technology were fielded at the Marshalltown FMGP site: geophysical, analytical and data integration. The geophysical technologies are designed to assess the subsurface geological conditions so that the location, fate and transport of the target contaminants may be assessed and forecasted. The analytical technologies/methods are designed to detect and quantify the target contaminants. The data integration technology area consists of hardware and software systems designed to integrate all the site information compiled and collected into a conceptual site model on a daily basis at the site; this conceptual model then becomes the decision-support tool. Simultaneous fielding of different methods within each of the three areas of technology provided data for direct comparison of the technologies fielded, both SOPT and IT. This document reports the results of the site characterization, technology comparison, and ESC demonstration activities associated with the Marshalltown FMGP site. 124 figs., 27 tabs.

  5. Meteorological observations at Syowa Station, Antarctica, 2008 by the 49th Japanese Antarctic Research Expedition

    Directory of Open Access Journals (Sweden)

    Hideshi Yoshimi

    2013-07-01

    Full Text Available This report describes the result of meteorological observations at Syowa Station by the Meteorological Observation Team of the 49th Japanese Antarctic Research Expedition (JARE-49 during the period 1 February 2008 to 27 January 2009. The observation methods, instruments, and statistical methods used by the JARE-49 team are nearly the same as those used by the JARE-48 observation team. Remarkable weather phenomena observed during the period of JARE-49 are as follows. 1 On 1 September 2008, the record minimum temperature for September was observed in the upper atmosphere (pressure greater than 175 hPa. 2 The monthly mean temperature at Syowa Station during October 2008 was -17.5°C; this is the lowest monthly mean October temperature recorded at Syowa Station. 3 The total ozone over Syowa Station was less than or equal to 220 m atm-cm during the period from late August to late November, and was close to minimum levels during the period from mid-September to mid-October. The lowest total ozone in 2008, recorded on 16 October 2008, was 140 m atm-cm.

  6. Spatial Distribution of Methanesulphonic Acid in the Arctic Aerosol Collected during the Chinese Arctic Research Expedition

    Directory of Open Access Journals (Sweden)

    Peipei Ye

    2015-05-01

    Full Text Available Methanesulphonic acid (MSA, mainly derived from marine biogenic emissions has been frequently used to estimate the marine biogenic contribution. However, there are few reports on MSA over the Arctic Ocean, especially the central Arctic Ocean. Here, we analyzed MSA in aerosol samples collected over the ocean and seas during the Chinese Arctic Research Expedition (CHINARE 2012 using ion chromatography. The aerosol MSA concentrations over the Arctic Ocean varied considerably and ranged from non-detectable (ND to 229 ng/m3, with an average of 27 ± 54 ng/m3 (median: 10 ng/m3. We found the distribution of aerosol MSA exhibited an obvious regional variation, which was affected by biotic and abiotic factors. High values were generally observed in the Norwegian Sea; this phenomenon was attributed to high rates of phytoplankton primary productivity and dimethylsulfide (DMS fluxes in this region. Concentrations over the pack ice region in the central Arctic Ocean were generally lower than over the open waters at the ice edge in the Chukchi Sea. This difference was the mainly caused by sea ice. In addition, we found that higher MSA concentrations were associated with warmer sea surface temperature (SST.

  7. Life-Cycle Cost/Benefit Assessment of Expedite Departure Path (EDP)

    Science.gov (United States)

    Wang, Jianzhong Jay; Chang, Paul; Datta, Koushik

    2005-01-01

    This report presents a life-cycle cost/benefit assessment (LCCBA) of Expedite Departure Path (EDP), an air traffic control Decision Support Tool (DST) currently under development at NASA. This assessment is an update of a previous study performed by bd Systems, Inc. (bd) during FY01, with the following revisions: The life-cycle cost assessment methodology developed by bd for the previous study was refined and calibrated using Free Flight Phase 1 (FFP1) cost information for Traffic Management Advisor (TMA, or TMA-SC in the FAA's terminology). Adjustments were also made to the site selection and deployment scheduling methodology to include airspace complexity as a factor. This technique was also applied to the benefit extrapolation methodology to better estimate potential benefits for other years, and at other sites. This study employed a new benefit estimating methodology because bd s previous single year potential benefit assessment of EDP used unrealistic assumptions that resulted in optimistic estimates. This methodology uses an air traffic simulation approach to reasonably predict the impacts from the implementation of EDP. The results of the costs and benefits analyses were then integrated into a life-cycle cost/benefit assessment.

  8. Going with the Floe? An Analysis of the Epic Expeditions of Fridtjof Nansen and Sir Ernest Shackleton

    Science.gov (United States)

    Pfirman, S.; Tremblay, B.; Fowler, C.

    2007-12-01

    One hundred years ago, the heroic age of polar exploration was underway. At first glance the Arctic-based Fridtjof Nansen and Antarctic-based Sir Ernest Shackleton, and their most famous expeditions, are literally poles apart. But the expeditions wound up having much in common, including the fact that their fates were largely dependent on their drift trajectory in the sea ice pack and, in Shackleton's case, the wind and ocean currents. These are natural forces, outside the control of the expedition leaders. Were Nansen and Shackleton lucky that the ice and ocean delivered them and their crew to locations from which they could return? Or were their fates more or less inevitable, within the normal range of natural conditions? While we cannot reconstruct the wind and ocean patterns that actually existed 100 years ago to answer this question, we looked at variability over the past three decades to explore potential alternate fates of these expeditions. Our analysis indicates that Nansen and Shackleton were both lucky and unlucky in the natural conditions that they encountered during their expeditions. Most years since 1979, Nansen would have gotten much closer to the North Pole - his goal -- than his ship did in 1895, so he was unlucky in that respect. On the other hand, he was lucky with the relatively short drift duration of his ship in the Arctic pack ice. Shackleton was also lucky in the rapid pace of drift within the pack. The fact that his trajectory was so far to the west might have been a factor in the crushing and sinking of his ship, but it did allow him to land most of his men on Elephant Island while he went for help. Shackleton's heroic, and harrowing, boat journey to South Georgia turned out to be helped by prevailing conditions: it was within the likely ocean drift trajectory from Elephant Island. Analyses such as these, including "Nansen's Luck" by Roger Colony, and "The Coldest March" by Susan Solomon, help set history and profiles of leadership within

  9. The ``Adopt A Microbe'' project: Web-based interactive education connected with scientific ocean drilling

    Science.gov (United States)

    Orcutt, B. N.; Bowman, D.; Turner, A.; Inderbitzen, K. E.; Fisher, A. T.; Peart, L. W.; Iodp Expedition 327 Shipboard Party

    2010-12-01

    We launched the "Adopt a Microbe" project as part of Integrated Ocean Drilling Program (IODP) Expedition 327 in Summer 2010. This eight-week-long education and outreach effort was run by shipboard scientists and educators from the research vessel JOIDES Resolution, using a web site (https://sites.google.com/site/adoptamicrobe) to engage students of all ages in an exploration of the deep biosphere inhabiting the upper ocean crust. Participants were initially introduced to a cast of microbes (residing within an ‘Adoption Center’ on the project website) that live in the dark ocean and asked to select and virtually ‘adopt’ a microbe. A new educational activity was offered each week to encourage learning about microbiology, using the adopted microbe as a focal point. Activities included reading information and asking questions about the adopted microbes (with subsequent responses from shipboard scientists), writing haiku about the adopted microbes, making balloon and fabric models of the adopted microbes, answering math questions related to the study of microbes in the ocean, growing cultures of microbes, and examining the gases produced by microbes. In addition, the website featured regular text, photo and video updates about the science of the expedition using a toy microbe as narrator, as well as stories written by shipboard scientists from the perspective of deep ocean microbes accompanied by watercolor illustrations prepared by a shipboard artist. Assessment methods for evaluating the effectiveness of the Adopt a Microbe project included participant feedback via email and online surveys, website traffic monitoring, and online video viewing rates. Quantitative metrics suggest that the “Adope A Microbe” project was successful in reaching target audiences and helping to encourage and maintain interest in topics related to IODP Expedition 327. The “Adopt A Microbe” project mdel can be adapted for future oceanographic expeditions to help connect the

  10. Grain Size Analyses of Neogene-Quaternary Sediments from the Arctic Coring Expedition

    Science.gov (United States)

    Moran, K.; Lado-Insua, T.; O'Regan, M.

    2013-12-01

    The Arctic Coring Expedition (ACEX) recovered the first Cenozoic sediment sequence from the central Arctic Ocean. Results from this expedition indicate that perennial sea ice may have formed in the Arctic at or before the early mid-Miocene. Sea ice formation is an important process in the global climate system, affecting directly the Earth's albedo and indirectly the Meridional Overturning Circulation. The deep Arctic Ocean receives sediment primarily from ice-rafted debris and turbidity currents. Suspension freezing on the shallow continental shelves of the Arctic has generally been considered the major process trapping sediment within sea ice. Sea ice motion is largely driven by wind. The anticyclonic Beaufort Gyre transports sea ice over the Amerasia Basin, while the Transpolar Drift transports it across the Eurasian Basin. The Transpolar Drift is divided into a Siberian and Polar branch, both branches cross the position of the ACEX drilling sites on the Lomonosov Ridge. Grain size analyses of ACEX sediments were obtained with a Malvern Mastersizer 2000 laser diffraction particle sizing system. Preliminary analyses indicate pulses with a higher percentage of sand between 3.64 Ma ago until the end of the Gelasian (1.8 Ma). The percent sand remained relatively low during the Cenozoic with the exception of two major increases of sand occurring ~6.2 and 9.2 Ma ago and a smaller peak ~8.2 Ma ago. These intervals also show less sorting and lower values for skewness and kurtosis. Increases in the percentage of sand and less sorting at this latitude relate to ice rafted debris, indicating an increase in sea-ice melting during these periods. A Principal Components Analysis and a Maximum Correlation Factor Analysis agree on a correlation between different grain sizes that would divide the grain size in two major distributions (63 to 250 μm portion to represent glacial ice. Based on our data we hypothesize that when sediments exhibit a bimodal distribution with relatively

  11. Group dynamics in a long-term blind endeavor on Earth: An analog for space missions (Lewis & Clark Expedition group dynamic analysis)

    Science.gov (United States)

    Allner, M.; Rygalov, V.

    2008-12-01

    In 1803, President Thomas Jefferson set fourth a military expedition led by Captains M. Lewis and W. Clark (Lewis and Clark Expedition) on an exploration that would become an everlasting part of US national history and pride. Looking back at the events of this exploration, there are many similarities to the experiences future human space explorers will face as we look to colonize the Moon and travel to Mars and beyond (NASA Vision for Space Exploration, 2004): The Lewis and Clark Expedition lasted almost three years and involved a crew of 43 men traveling up the Missouri River to explore the unknown lands and a possible water route to the Pacific Ocean; The Expedition took place far away from customary comfortable environments known to European settlers in the early 18th century; The Expedition involved a remotely confined high-perceived risk environment with high levels of uncertainty providing stresses and every day challenges for the crew; Supplies brought on the mission were limited (mainly a mass/weight issue rather than cost), therefore the discovery and use of environmental resources (In-Situ Resource Utilization approach, including info-resources to mitigate uncertainty) was necessary for crew survival. The environments astronauts will encounter in space and on the Moon and Mars due to high risk and uncertainty will be in many aspects similar to what Lewis and Clark's crew experienced, as environments will be hostile and unforgiving if problems arise and aren't resolved quickly. The analysis provided in this research paper is relevant because the Lewis and Clark Expedition needed to move extensively and with minimal supplies. Polar remote settings, which were analyzed extensively, were different from this expedition due to the fact that these missions did not encompass extensive movement of crew facilities and supplies and were more like space missions orbiting the Earth. Using past space station results of performance on orbit in correlation with a

  12. Politicians, Patriots and Plotters: Unlikely Debates Occasioned by Maximilian Hell's Venus Transit Expedition of 1769

    Science.gov (United States)

    Kontler, Laszlo

    2013-05-01

    This paper discusses the cultural and political contexts and reception of the most important by-product of Maximilian Hell's famous Venus transit expedition of 1768-69, the Demonstratio. Idioma Ungarorum et Lapponum idem esse (1770) by Hell's associate Janos Sajnovics. Now considered a landmark in Finno-Ugrian linguistics, the Demonstratio addressed an academic subject that was at that time almost destined to be caught up in an ideological battlefield defined by the shifting relationship between the Habsburg government, the Society of Jesus, and the Hungarian nobility. The "enlightened absolutist" policies of the former aimed at consolidating the Habsburg monarchy as an empire, at the expense of privileged groups, including religious orders as well as the noble estates. In the situation created by the 1773 suppression of the Jesuit order (a signal of declining patronage from the dynasty), the growing preoccupation on the part of ex-Jesuits like Hell and Sajnovics with "things Hungarian" could have been part of an attempt to re-situate themselves on the Central European map of learning. At the same time, the founding document of this interest, the Demonstratio, evoked violent protests from the other target of Habsburg policies, the Hungarian nobility, because its basic assumptions - the kinship of the Hungarian and the Sami (Lappian) language - potentially undermined the noble ideology of social exclusiveness, established on the alleged "Scythian" ancestry of Hungarians. By exploring the complex motives, intentions, reactions and responses of the chief agents in this story, it is possible to highlight the extra-scientific constraints and facilitators for the practice of knowledge in late eighteenth century Central Europe.

  13. Wood-destroying soft rot fungi in the historic expedition huts of Antarctica.

    Science.gov (United States)

    Blanchette, Robert A; Held, Benjamin W; Jurgens, Joel A; McNew, Douglas L; Harrington, Thomas C; Duncan, Shona M; Farrell, Roberta L

    2004-03-01

    Three expedition huts in the Ross Sea region of Antarctica, built between 1901 and 1911 by Robert F. Scott and Ernest Shackleton, sheltered and stored the supplies for up to 48 men for 3 years during their explorations and scientific investigation in the South Pole region. The huts, built with wood taken to Antarctica by the early explorers, have deteriorated over the past decades. Although Antarctica has one of the coldest and driest environments on earth, microbes have colonized the wood and limited decay has occurred. Some wood in contact with the ground contained distinct microscopic cavities within secondary cell walls caused by soft rot fungi. Cadophora spp. could be cultured from decayed wood and other woods sampled from the huts and artifacts and were commonly associated with the soft rot attack. By using internal transcribed spacer sequences of ribosomal DNA and morphological characteristics, several species of Cadophora were identified, including C. malorum, C. luteo-olivacea, and C. fastigiata. Several previously undescribed Cadophora spp. also were found. At the Cape Evans and Cape Royds huts, Cadophora spp. commonly were isolated from wood in contact with the ground but were not always associated with soft rot decay. Pure cultures of Cadophora used in laboratory decay studies caused dark staining of all woods tested and extensive soft rot in Betula and Populus wood. The presence of Cadophora species, but only limited decay, suggests there is no immediate threat to the structural integrity of the huts. These fungi, however, are widely found in wood from the historic huts and have the capacity to cause extensive soft rot if conditions that are more conducive to decay become common.

  14. Persistent organic pollutants in biota samples collected during the Ymer-80 expedition to the Arctic

    Directory of Open Access Journals (Sweden)

    Henrik Kylin

    2015-10-01

    Full Text Available During the 1980 expedition to the Arctic with the icebreaker Ymer, a number of vertebrate species were sampled for determination of persistent organic pollutants. Samples of Arctic char (Salvelinus alpinus, n=34, glaucous gull (Larus hyperboreus, n=8, common eider (Somateria mollissima, n=10, Brünnich's guillemot (Uria lomvia, n=9, ringed seal (Pusa hispida, n=2 and polar bear (Ursus maritimus, n=2 were collected. With the exception of Brünnich's guillemot, there was a marked contamination difference of birds from western as compared to eastern/northern Svalbard. Samples in the west contained a larger number of polychlorinated biphenyl (PCB congeners and also polychlorinated terphenyls, indicating local sources. Brünnich's guillemots had similar pollutant concentrations in the west and east/north; possibly younger birds were sampled in the west. In Arctic char, pollutant profiles from lake Linnévatn (n=5, the lake closest to the main economic activities in Svalbard, were similar to profiles in Arctic char from the Shetland Islands (n=5, but differed from lakes to the north and east in Svalbard (n=30. Arctic char samples had higher concentrations of hexachlorocyclohexanes (HCHs than the marine species of birds and mammals, possibly due to accumulation via snowmelt. Compared to the Baltic Sea, comparable species collected in Svalbard had lower concentrations of PCB and dichlorodiphenyltrichloroethane (DDT, but similar concentrations indicating long-range transport of hexachlorobenzene, HCHs and cyclodiene pesticides. In samples collected in Svalbard in 1971, the concentrations of PCB and DDT in Brünnich's guillemot (n=7, glaucous gull (n=2 and polar bear (n=2 were similar to the concentrations found in 1980.

  15. Expediting Transition to Home Parenteral Nutrition With Fast-Track Cycling.

    Science.gov (United States)

    Austhof, Sandra I; DeChicco, Robert; Cresci, Gail; Corrigan, Mandy L; Lopez, Rocio; Steiger, Ezra; Kirby, Donald F

    2017-03-01

    Delivery of home parenteral nutrition (PN) is typically cycled over 12 hours. Discharge to home on PN is often delayed due to potential adverse events (AEs) associated with cycling PN. The purpose was to determine whether patients requiring long-term PN can be cycled from 24 hours to 12 hours in 1 day instead of 2 days without increasing the risk of PN-related AEs. Hospitalized patients receiving PN at goal calories infused over 24 hours without severe electrolyte or blood glucose abnormalities were eligible. Patients were randomly assigned to a 1-step "fast-track" protocol or 2-step "standard" protocol. AEs were defined as hypoglycemia or hyperglycemia, new-onset or worsening dyspnea, tachycardia, tachypnea, lower extremity or sacral edema, pulmonary edema, or abdominal ascites and were graded as minor or major. In the 63 patients studied, the most prevalent PN-related AE was hyperglycemia, occurring in 24.2% and 30.0% of patients in the fast-track and standard groups, respectively. Overall, there was no significant difference in the prevalence of PN-related minor AEs between fast-track and standard groups (33.3% and 53.3%, P = .5). No major PN-related AEs occurred in the fast-track group, while 1 major PN-related AE (pulmonary edema) occurred in the standard group. Fast-track cycling is as safe as standard cycling in patients without diabetes mellitus or major organ dysfunction requiring long-term PN. Fast-track cycling could potentially expedite hospital discharge, resulting in decreased healthcare costs and improved patient satisfaction.

  16. Kondoma Tatars and the Bloomery Process (source: the Great Northern Expedition

    Directory of Open Access Journals (Sweden)

    Evgeny V. Vodyasov

    2016-06-01

    Full Text Available The article presents for the first time the unique source for studying indigenous ironmaking in West Siberia. This is a copy of the illustration made by Johann Wilhelm Lursenius on 19 September 1734 during the Second Kamchatka Expedition (the copy is kept in the Russian State Archive of Ancient Acts. On that day, the artist together with German scientist Johann Georg Gmelin observed the iron melting process in a Tatar yurt in Gornaya Shoria, and they both documented these observations in detail, each in his own way. The synchronous description and sketching of a traditional trade technology is a most singular or even the unique phenomenon in Siberian ethnography of the early 18th century. The article features excerpts from Gmelin’s 1751 work devoted to iron ore smelting by Kondoma Tatars and provides an analysis of the illustration by Lursenius. Ferrous metallurgy of Kondoma Tatars in the 18th century involved using «small» iron-smelting furnaces (0.3 m high at the most placed at the hearths of yurts. Besides, Tatars decorated the upper part of the furnace with carving. As seen from the analysis of archaeological and ethnographic sources, the tradition of building such furnaces and smelting iron ore in dwellings existed in the Upper Parts of Ob River from the early 5th century AD to the ethnographic modernity. Ethnographic sources and archaeological experiments reveal that one small furnace could yield about 1 kg iron. According to historical sources, a few kilograms would make a year of trouble-free housekeeping for a Tatar family. This explains why «home production» of iron was so widespread, when a dwelling would be turned into a metallurgy shop to provide the family with all necessary tools and utensils.

  17. Report on expedited site characterization of the Central Nevada Test Area, Nye County, Nevada

    Energy Technology Data Exchange (ETDEWEB)

    Yuhr, L. [Technos Inc., Miami, FL (United States); Wonder, J.D.; Bevolo, A.J. [Ames Lab., IA (United States)

    1997-09-01

    This report documents data collection, results, and interpretation of the expedited site characterization (ESC) pilot project conducted from September 1996 to June 1997 at the Central Nevada Test Area (CNTA), Nye County, Nevada. Characterization activities were limited to surface sites associated with deep well drilling and ancillary operations at or near three emplacement well areas. Environmental issues related to the underground nuclear detonation (Project Faultless) and hydrologic monitoring wells were not addressed as a part of this project. The CNTA was divided into four functional areas for the purpose of this investigation and report. These areas include the vicinity of three emplacement wells (UC-1, UC-3, and UC-4) and one mud waste drilling mud collection location (Central Mud Pit; CMP). Each of these areas contain multiple, potentially contaminated features, identified either from historic information, on-site inspections, or existing data. These individual features are referred to hereafter as ``sites.`` The project scope of work involved site reconnaissance, establishment of local grid systems, site mapping and surveying, geophysical measurements, and collection and chemical analysis of soil and drilling mud samples. Section 2.0 through Section 4.0 of this report provide essential background information about the site, project, and details of how the ESC method was applied at CNTA. Detailed discussion of the scope of work is provided in Section 5.0, including procedures used and locations and quantities of measurements obtained. Results and interpretations for each of the four functional areas are discussed separately in Sections 6.0, 7.0, 8.0, and 9.0. These sections provide a chronological presentation of data collected and results obtained, followed by interpretation on a site-by-site basis. Key data is presented in the individual sections. The comprehensive set of data is contained in appendices.

  18. STIs in sex partners notified for chlamydia exposure: implications for expedited partner therapy.

    Science.gov (United States)

    van Aar, Fleur; van Benthem, Birgit H B; van den Broek, Ingrid V F; Götz, Hannelore M

    2018-01-11

    Expedited partner therapy (EPT) may reduce chlamydia reinfection rates. However, the disadvantages of EPT for chlamydia include missing the opportunity to test for other STIs and unnecessary use of antibiotics among non-infected partners. As part of a larger study that investigated the feasibility of EPT in the Netherlands, we explored the frequency of STI among a potential EPT target population of chlamydia-notified heterosexual men and women attending STI clinics for testing. Cross-sectional national STI/HIV surveillance data, which contain information on all consultations at STI clinics, were used to calculate STI positivity rates stratified by chlamydia notification and gender, and proportions of STI that were attributable to clients notified for chlamydia. Of all consultations in 2015 (n=101 710), 14 445 (14.4%) clients reported to be notified exclusively for chlamydia. Among chlamydia-notified clients, the chlamydia positivity rate was 34.2% (n=4947), and consequently 65.8% (n=9488) of them tested negative for chlamydia. Chlamydia-notified clients contributed to 10.2% of all gonorrhoea infections (n=174/1702) and 10.9% of all infectious syphilis, HIV and/or infectious hepatitis B infections (n=15/173). Implementing EPT without additional STI testing for all partners of chlamydia-infected index patients implies that STIs other than chlamydia will be missed. Although the chlamydia positivity rate was high among chlamydia-notified partners, two-thirds would unnecessarily use azithromycin. An evaluation of EPT against the current partner treatment strategy is needed to carefully weigh the potential health gains against the potential health losses and to explore the characteristics of EPT-eligible partners. © Article author(s) (or their employer(s) unless otherwise stated in the text of the article) 2018. All rights reserved. No commercial use is permitted unless otherwise expressly granted.

  19. Astronomy behind Enemy Lines: Colonial American Field Expeditions, 1761--1780

    Science.gov (United States)

    Schechner, Sara J.

    2012-09-01

    In May 1761, John Winthrop packed up two students, two telescopes, a clock, and an octant, and embarked for Newfoundland, to observe the Transit of Venus. Winthrop's departure was hasty. Only days before had the President and Fellows of Harvard College approve Professor Winthrop's request to take the college apparatus behind enemy lines during the French and Indian War, to serve the cause of science. Winthrop knew he had no time to waste if he were to reach St. Johns and properly calibrate his equipment before the Transit. In 1761 Winthrop was the sole North American astronomer in a global network helping to determine the distance from the Earth to the Sun. The expedition was a major achievement for colonial astronomy, especially in time of war. Winthrop, however, looked forward to a second chance to observe a transit in 1769. Benjamin Franklin urged him to go to Lake Superior, but preparations for the transit were thwarted by two events: the loss of Harvard's apparatus in a 1764 fire; and pre-Revolutionary War politics in the American colonies. In the end, Winthrop was forced to content himself with observations in Cambridge. In 1780 Winthrop's successor at Harvard, Samuel Williams, risked the college apparatus once again. During the American War of Independence, he received permission to go behind British enemy lines in order to observe a total solar eclipse in Penobscot Bay, Maine. Limitations placed on his encampment led him to be slightly outside totality, but able to observe what would later be known as Baily's beads. This paper will examine the challenges of observational science in provincial America, especially when one had to negotiate with enemies to have access to the best apparatus and field sites.

  20. An evaluation of NASA's program for improving aircraft fuel efficiency

    Science.gov (United States)

    1980-01-01

    The report provides commentary and recommendations where appropriate on each of the major elements of the program. Key findings of the committee included a recommendation that closer ties be established between NASA and the FAA to expedite the use and acceptance of the new technology. The committee also cited the potential for fuel savings through an imporved air traffic control system and recommended that the management of NASA and the FAA discuss ways and means to work together to exploit more effectively the capabilities and responsibilities of each to develop air traffic control.

  1. Structural mode significance using INCA. [Interactive Controls Analysis computer program

    Science.gov (United States)

    Bauer, Frank H.; Downing, John P.; Thorpe, Christopher J.

    1990-01-01

    Structural finite element models are often too large to be used in the design and analysis of control systems. Model reduction techniques must be applied to reduce the structural model to manageable size. In the past, engineers either performed the model order reduction by hand or used distinct computer programs to retrieve the data, to perform the significance analysis and to reduce the order of the model. To expedite this process, the latest version of INCA has been expanded to include an interactive graphical structural mode significance and model order reduction capability.

  2. Framing the transit: expeditionary culture and identities in Lieutenant E.J.W. Noble's caricatures of the 1874 transit of Venus expedition to Honolulu.

    Science.gov (United States)

    Higgitt, Rebekah

    2017-07-01

    Making use of a source previously unknown to historians, this article sheds new light on the British expedition to the Sandwich Islands to observe the 1874 transit of Venus. This source, a series of caricature drawings that follow the expedition from departure to return, gives insight into expeditionary culture and the experience of a previously unremarked member of this astronomical expedition, Evelyn J.W. Noble, a career officer of the Royal Marine Artillery. It also reveals overlapping military, scientific and masculine identities, developed in dialogue with, and often deliberately subverting, more public accounts. The article explores this unique source as a product of naval, imperial and expeditionary cultures; as a contribution to the wide textual and visual culture that surrounded the transit expeditions; and as a series of drawings that united the expedition members through the use of humour and irony, by differentiating the group from others they encountered, and by reflecting or rejecting ideas about the nature of scientific work and personae. The artist represented himself not as a serving officer but as part of a (mostly) united group, dedicated to but humorously self-deprecating about their contribution to the scientific effort.

  3. The Arctic Gakkel Vents (AGAVE) Expedition: Technology Development and the Search for Deep-Sea Hydrothermal Vent Fields Under the Arctic Ice Cap

    Science.gov (United States)

    Reves-Sohn, R. A.; Singh, H.; Humphris, S.; Shank, T.; Jakuba, M.; Kunz, C.; Murphy, C.; Willis, C.

    2007-12-01

    Deep-sea hydrothermal fields on the Gakkel Ridge beneath the Arctic ice cap provide perhaps the best terrestrial analogue for volcanically-hosted chemosynthetic biological communities that may exist beneath the ice-covered ocean of Europa. In both cases the key enabling technologies are robotic (untethered) vehicles that can swim freely under the ice and the supporting hardware and software. The development of robotic technology for deep- sea research beneath ice-covered oceans thus has relevance to both polar oceanography and future astrobiological missions to Europa. These considerations motivated a technology development effort under the auspices of NASA's ASTEP program and NSF's Office of Polar Programs that culminated in the AGAVE expedition aboard the icebreaker Oden from July 1 - August 10, 2007. The scientific objective was to study hydrothermal processes on the Gakkel Ridge, which is a key target for global studies of deep-sea vent fields. We developed two new autonomous underwater vehicles (AUVs) for the project, and deployed them to search for vent fields beneath the ice. We conducted eight AUV missions (four to completion) during the 40-day long expedition, which also included ship-based bathymetric surveys, CTD/rosette water column surveys, and wireline photographic and sampling surveys of remote sections of the Gakkel Ridge. The AUV missions, which lasted 16 hours on average and achieved operational depths of 4200 meters, returned sensor data that showed clear evidence of hydrothermal venting, but for a combination of technical reasons and time constraints, the AUVs did not ultimately return images of deep-sea vent fields. Nevertheless we used our wireline system to obtain images and samples of extensive microbial mats that covered fresh volcanic surfaces on a newly discovered set of volcanoes. The microbes appear to be living in regions where reducing and slightly warm fluids are seeping through cracks in the fresh volcanic terrain. These discoveries

  4. Vertical thermodynamic structure of the troposphere during the Norwegian young sea ICE expedition (N-ICE2015)

    Science.gov (United States)

    Kayser, Markus; Maturilli, Marion; Graham, Robert M.; Hudson, Stephen R.; Rinke, Annette; Cohen, Lana; Kim, Joo-Hong; Park, Sang-Jong; Moon, Woosok; Granskog, Mats A.

    2017-10-01

    The Norwegian young sea ICE (N-ICE2015) expedition was designed to investigate the atmosphere-snow-ice-ocean interactions in the young and thin sea ice regime north of Svalbard. Radiosondes were launched twice daily during the expedition from January to June 2015. Here we use these upper air measurements to study the multiple cyclonic events observed during N-ICE2015 with respect to changes in the vertical thermodynamic structure, moisture content, and boundary layer characteristics. We provide statistics of temperature inversion characteristics, static stability, and boundary layer extent. During winter, when radiative cooling is most effective, we find the strongest impact of synoptic cyclones. Changes to thermodynamic characteristics of the boundary layer are associated with transitions between the radiatively "clear" and "opaque" atmospheric states. In spring, radiative fluxes warm the surface leading to lifted temperature inversions and a statically unstable boundary layer. Further, we compare the N-ICE2015 static stability distributions to corresponding profiles from ERA-Interim reanalysis, from the closest land station in the Arctic North Atlantic sector, Ny-Ålesund, and to soundings from the SHEBA expedition (1997/1998). We find similar stability characteristics for N-ICE2015 and SHEBA throughout the troposphere, despite differences in location, sea ice thickness, and snow cover. For Ny-Ålesund, we observe similar characteristics above 1000 m, while the topography and ice-free fjord surrounding Ny-Ålesund generate great differences below. The long-term radiosonde record (1993-2014) from Ny-Ålesund indicates that during the N-ICE2015 spring period, temperatures were close to the climatological mean, while the lowest 3000 m were 1-3°C warmer than the climatology during winter.

  5. Scleractinian corals recorded in the Argentinean Antarctic expeditions between 2012 and 2014, with comments on Flabellum (Flabellum areum Cairns, 1982

    Directory of Open Access Journals (Sweden)

    Laura Schejter

    2016-07-01

    Full Text Available In this contribution, we provide a list of the scleractinian corals recorded during the Argentinean Antarctic expeditions on board the oceanographic vessel Puerto Deseado (Argentina in the austral summers in 2012, 2013 and 2014. The identified taxa consist of six solitary species (Flabellum impensum, F. flexuosum, F. areum, Caryophyllia antarctica, Paraconotrochus antarcticus and Javania antarctica, recorded from 19 sampling sites located off the Antarctic Peninsula and South Shetland and South Orkney islands. We also update the information of F. areum, previously known only from south-west Atlantic waters, extending its distribution range to Antarctic waters and its upper bathymetric range to 218 m.

  6. FROM THE LEWIS AND CLARK EXPEDITION TO IBM, DELL, AND SOUTHWEST AIRLINES: TEACHING HISTORY AND LEADERSHIP TO BUSINESS STUDENTS

    Directory of Open Access Journals (Sweden)

    Jeffrey J. Matthews

    2006-01-01

    Full Text Available History is not a tomb of dead facts but a resource that can inform and improve everyday decision making. Experience as an analytical tool is invaluable for solving problems in changing and competitive environments. “From the Lewis and Clark Expedition,” which coincides with the National Lewis & Clark Bicentennial Commemoration (2003—2006, demonstrates how contemporary business concepts of visionary leadership, systematic planning, and organizational climate were instrumental to the success of Thomas Jefferson's “Corps of Discovery” and shows how a mastery of these concepts contributed to the successes of the pioneering US corporations IBM, Southwest Airlines, and Dell.

  7. Spatial distribution of Delta(CO2)-C-14 across Eurasia: measurements from the TROICA-8 expedition

    OpenAIRE

    Turnbull, J.C.; Miller, J.B.; Lehman, S.J.; Hurst, D.; Peters, W.

    2009-01-01

    Because fossil fuel derived CO2 is the only source of atmospheric CO2 that is devoid of 14C, atmospheric measurements of delta14CO2 can be used to constrain fossil fuel emission estimates at local and regional scales. However, at the continental scale, uncertainties in atmospheric transport and other sources of variability in delta14CO2 may influence the fossil fuel detection capability. We present a set of delta14CO2 observations from the train-based TROICA-8 expedition across Eurasia in Mar...

  8. The Expedition of Ilya G. Voznesensky to Russian America in 1839–1849 and the Formation of the American Collections in St. Petersburg Academic Museums

    Directory of Open Access Journals (Sweden)

    Tatyana Yurievna Feklova

    2014-10-01

    Full Text Available Expeditions were an integral part of the activity of the Russian Academy of Sciences, promoting its further development and prosperity. Expeditions also helped assemble data for future scientific development. In the first half of the 19th century, the territory of the Russian Empire included some regions of North America (Alaska, North California and the Aleutian Islands. The study of these areas was carried out with the participation of the Russian-American Company. The greatest merit for the scientific study of these regions belongs to a scientist from the Russian Academy of Sciences, Ilya G. Voznesensky. In this article, for the first time, attention will be paid to the analysis of organizational and documentary aspects of this expedition.

  9. Physical, chemical and biological data, Tasaday Expedition, Legs I, II, III and IV : Leg I, 5 June-1 July 1973; Leg II, 8-15 July 1973; Leg III, 22 July-4 August 1973; Leg IV, 13 August-6 September 1973 (NODC Accession 9200047)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Tasaday expedition aboard RV Thomas Washington was a multidisciplinary oceanographic expedition in the Pacific and Indian Ocean during 1973-1974. This report...

  10. Program specialization

    CERN Document Server

    Marlet, Renaud

    2013-01-01

    This book presents the principles and techniques of program specialization - a general method to make programs faster (and possibly smaller) when some inputs can be known in advance. As an illustration, it describes the architecture of Tempo, an offline program specializer for C that can also specialize code at runtime, and provides figures for concrete applications in various domains. Technical details address issues related to program analysis precision, value reification, incomplete program specialization, strategies to exploit specialized program, incremental specialization, and data speci

  11. The expedition ARCTIC `96 of RV `Polarstern` (ARK XII) with the Arctic Climate System Study (ACSYS). Cruise report; Die Expedition ARCTIC `96 des FS `Polarstern` (ARK XII) mit der Arctic Climate System Study (ACSYS). Fahrtbericht

    Energy Technology Data Exchange (ETDEWEB)

    Augstein, E.

    1997-11-01

    The multinational expedition ARCTIC `96 was carried out jointly by two ships, the German RV POLARSTERN and the Swedish RV ODEN. The research programme was developed by scientists from British, Canadian, Finish, German, Irish, Norwegian, Russian, Swedish and US American research institutions and universities. The physical programme on POLARSTERN was primarily designed to foster the Arctic Climte System Study (ACSYS) in the framework of the World Climate Research Programme (WCRP). Investigations during the recent years have provided substantial evidence that the Arctic Ocean and the adjacent shelf seas play a significant role in the thermohaline oceanic circulation and may therefore have a distinct influence on global climate. Consequently the main ACSYS goals are concerned with studies of the governing oceanic, atmospheric and hydrological processes in the entire Arctic region. (orig.) [Deutsch] Die Expedition ARCTIC `96 wurde von zwei Forschungsschiffen, der deutschen POLARSTERN und der schwedischen ODEN unter Beteiligung von Wissenschaftlern und Technikern aus Deutschland, Finnland, Grossbritannien, Irland, Kanada, Norwegen, Russland, Schweden und den Vereinigten Staaten von Amerika durchgefuehrt. Die physikalischen Projekte auf der POLARSTERN dienten ueberwiegend der Unterstuetzung der Arctic Climate System Study (ACSYS) des Weltklimaforschungsprogramms, die auf die Erforschung der vorherrschenden ozeanischen, atmosphaerischen, kryosphaerischen und hydrologischen Prozesse der Arktisregion ausgerichtet ist. (orig.)

  12. The Transient Tracers in the Ocean (TTO) program: The North Atlantic Study, 1981; The Tropical Atlantic Study, 1983

    Science.gov (United States)

    Brewer, Peter G.; Sarmiento, Jorge L.; Smethie, William M.

    1985-01-01

    The scientific papers here collected result from the Transient Tracers in the Ocean (TTO) program. The two parts of this major geochemical and physical oceanographie expedition took place in the North Atlantic Ocean in 1981 and in the Tropical Atlantic in 1983 on the research vessel Knorr of the Woods Hole Oceanographie Institution. The expeditions, sponsored by the National Science Foundation and the U.S. Department of Energy (North Atlantic only), were designed to observe the passage of man-made geochemical tracers into the interior of the ocean. The foundations for such an experiment were laid in the 1972-1978 GEOSECS program. Here, for the first time, a systematic survey revealed the penetration into the thermocline and deep ocean of the products of man's military/industrial activities, principally tritium and carbon-14 resulting from atmospheric testing of nuclear weapons, which terminated with the nuclear test ban treaty in 1962.

  13. From Geocaching to Virtual Reality: Technology tools that can transform courses into interactive learning expeditions

    Science.gov (United States)

    Moysey, S. M.; Lazar, K.; Boyer, D. M.; Mobley, C.; Sellers, V.

    2016-12-01

    Transforming classrooms into active learning environments is a key challenge in introductory-level courses. The technology explosion over the last decade, from the advent of mobile devices to virtual reality, is creating innumerable opportunities to engage students within and outside of traditional classroom settings. In particular, technology can be an effective tool for providing students with field experiences that would otherwise be logistically difficult in large, introductory earth science courses. For example, we have created an integrated platform for mobile devices using readily accessible "off the shelf" components (e.g., Google Apps, Geocaching.com, and Facebook) that allow individual students to navigate to geologically relevant sites, perform and report on activities at these locations, and share their findings through social media by posting "geoselfies". Students compete with their friends on a leaderboard, while earning incentives for completing extracurricular activities in courses. Thus in addition to exposing students to a wider range of meaningful and accessible geologic field experiences, they also build a greater sense of community and identity within the context of earth science classrooms. Rather than sending students to the field, we can also increasingly bring the field to students in classrooms using virtual reality. Ample mobile platforms are emerging that easily allow for the creation, curation, and viewing of photospheres (i.e., 360o images) with mobile phones and low-cost headsets; Google Street View, Earth, and Expeditions are leading the way in terms of ease of content creation and implementation in the classroom. While these tools are an excellent entry point to show students real-world sites, they currently lack the capacity for students to interact with the environment. We have therefore also developed an immersive virtual reality game that allows students to study the geology of the Grand Canyon using their smartphone and Google

  14. Spatial distribution of Δ14CO2 across Eurasia: measurements from the TROICA-8 expedition

    Directory of Open Access Journals (Sweden)

    J. W. Elkins

    2009-01-01

    Full Text Available Because fossil fuel derived CO2 is the only source of atmospheric CO2 that is devoid of 14C, atmospheric measurements of Δ14CO2 can be used to constrain fossil fuel emission estimates at local and regional scales. However, at the continental scale, uncertainties in atmospheric transport and other sources of variability in Δ14CO2 may influence the fossil fuel detection capability. We present a set of Δ14CO2 observations from the train-based TROICA-8 expedition across Eurasia in March–April 2004. Local perturbations in Δ14CO2 are caused by easily identifiable sources from nuclear reactors and localized pollution events. The remaining data show an increase in Δ14CO2 from Western Russia (40° E to Eastern Siberia (120° E, consistent with depletion in 14CO2 caused by fossil fuel CO2 emissions in heavily populated Europe, and gradual dispersion of the fossil fuel plume across Northern Asia. Other trace gas species which may be correlated with fossil fuel CO2 emissions, including carbon monoxide, sulphur hexafluoride, and perchloroethylene, were also measured and the results compared with the Δ14CO2 measurements. The sulphur hexafluoride longitudinal gradient is not significant relative to the measurement uncertainty. Carbon monoxide and perchloroethylene show large-scale trends of enriched values in Western Russia and decreasing values in Eastern Siberia, consistent with fossil fuel emissions, but exhibit significant spatial variability, especially near their primary sources in Western Russia. The clean air Δ14CO2 observations are compared with simulated spatial gradients from the TM5 atmospheric transport model. We show that the change in Δ14CO2 across the TROICA transect is due almost entirely to emissions of fossil fuel CO2, but that the magnitude of this Δ14CO2 gradient is relatively insensitive to modest uncertainties in the fossil fuel flux. In contrast, the Δ14CO2 gradient is more sensitive to the modeled representation of vertical

  15. The Sorcerer II Global Ocean Sampling Expedition: metagenomic characterization of viruses within aquatic microbial samples.

    Directory of Open Access Journals (Sweden)

    Shannon J Williamson

    Full Text Available Viruses are the most abundant biological entities on our planet. Interactions between viruses and their hosts impact several important biological processes in the world's oceans such as horizontal gene transfer, microbial diversity and biogeochemical cycling. Interrogation of microbial metagenomic sequence data collected as part of the Sorcerer II Global Ocean Expedition (GOS revealed a high abundance of viral sequences, representing approximately 3% of the total predicted proteins. Cluster analyses of the viral sequences revealed hundreds to thousands of viral genes encoding various metabolic and cellular functions. Quantitative analyses of viral genes of host origin performed on the viral fraction of aquatic samples confirmed the viral nature of these sequences and suggested that significant portions of aquatic viral communities behave as reservoirs of such genetic material. Distributional and phylogenetic analyses of these host-derived viral sequences also suggested that viral acquisition of environmentally relevant genes of host origin is a more abundant and widespread phenomenon than previously appreciated. The predominant viral sequences identified within microbial fractions originated from tailed bacteriophages and exhibited varying global distributions according to viral family. Recruitment of GOS viral sequence fragments against 27 complete aquatic viral genomes revealed that only one reference bacteriophage genome was highly abundant and was closely related, but not identical, to the cyanomyovirus P-SSM4. The co-distribution across all sampling sites of P-SSM4-like sequences with the dominant ecotype of its host, Prochlorococcus supports the classification of the viral sequences as P-SSM4-like and suggests that this virus may influence the abundance, distribution and diversity of one of the most dominant components of picophytoplankton in oligotrophic oceans. In summary, the abundance and broad geographical distribution of viral

  16. The Sorcerer II Global Ocean Sampling expedition: northwest Atlantic through eastern tropical Pacific.

    Directory of Open Access Journals (Sweden)

    Douglas B Rusch

    2007-03-01

    Full Text Available The world's oceans contain a complex mixture of micro-organisms that are for the most part, uncharacterized both genetically and biochemically. We report here a metagenomic study of the marine planktonic microbiota in which surface (mostly marine water samples were analyzed as part of the Sorcerer II Global Ocean Sampling expedition. These samples, collected across a several-thousand km transect from the North Atlantic through the Panama Canal and ending in the South Pacific yielded an extensive dataset consisting of 7.7 million sequencing reads (6.3 billion bp. Though a few major microbial clades dominate the planktonic marine niche, the dataset contains great diversity with 85% of the assembled sequence and 57% of the unassembled data being unique at a 98% sequence identity cutoff. Using the metadata associated with each sample and sequencing library, we developed new comparative genomic and assembly methods. One comparative genomic method, termed "fragment recruitment," addressed questions of genome structure, evolution, and taxonomic or phylogenetic diversity, as well as the biochemical diversity of genes and gene families. A second method, termed "extreme assembly," made possible the assembly and reconstruction of large segments of abundant but clearly nonclonal organisms. Within all abundant populations analyzed, we found extensive intra-ribotype diversity in several forms: (1 extensive sequence variation within orthologous regions throughout a given genome; despite coverage of individual ribotypes approaching 500-fold, most individual sequencing reads are unique; (2 numerous changes in gene content some with direct adaptive implications; and (3 hypervariable genomic islands that are too variable to assemble. The intra-ribotype diversity is organized into genetically isolated populations that have overlapping but independent distributions, implying distinct environmental preference. We present novel methods for measuring the genomic

  17. [Improved program maintenance of the CIRCIS dosimetric planning system].

    Science.gov (United States)

    Sevast'ianov, A I; Liutova, N A; Ratner, T G

    1983-03-01

    A special computer complex CIRCIS (Informatique, France) is used in the All-Union Cancer Research Center, USSR AMS, for the dosimetric planning of radiotherapy on 5 gamma-beam units and electron accelerator. Mathematical maintenance of the complex includes programs of the calculation of dose distribution for gamma-, inhibition and electron radiation but has no program of the calculation of the time of irradiation. The authors have devised and introduced into the complex such a program in the Fortran language that makes it possible to calculate within 2-3 min the time of irradiation for multifield rotation therapy using several units as a time, thus expediting the dosimetric planning for patients' irradiation.

  18. Annual report of the Wind Characteristics Program Element, October 1979-September 1980

    Energy Technology Data Exchange (ETDEWEB)

    Wendell, L.L.; Barchet, W.R.; Connell, J.R.; Miller, A.H.; Pennell, W.T.; Renne, D.S.

    1981-09-01

    This annual report briefly describes the technical progress within each segment of the WCPE from October 1979 through September 1980. It includes the progress accomplished directly by the Pacific Northwest Laboratory (PNL) and by subcontractors funded directly by DOE or through PNL. To expedite the management of the activities to produce the required information, the WCPE has been divided into three program areas: Wind Energy Prospecting, Support for Design and Operations, and Site Evaluation. Accomplishments in each of these program areas provide a highlight of WCPE activities in FY 1980.

  19. New Programming Environments for Uncertainty Analysis

    Science.gov (United States)

    Hill, M. C.; Poeter, E. P.; Banta, E. R.; Christensen, S.; Cooley, R. L.; Ely, D. M.; Babendreier, J.; Leavesley, G.; Tonkin, M.; Julich, R.

    2005-12-01

    We live in a world of faster computers, better GUI's and visualization technology, increasing international cooperation made possible by new digital infrastructure, new agreements between US federal agencies (such as ISCMEM), new European Union programs (such as Harmoniqua), and greater collaboration between US university scientists through CUAHSI. These changes provide new resources for tackling the difficult job of quantifying how well our models perform. This talk introduces new programming environments that take advantage of these new developments and will change the paradigm of how we develop methods for uncertainty evaluation. For example, the programming environments provided by COSU API, JUPITER API, and Sensitivity/Optimization Toolbox provide enormous opportunities for faster and more meaningful evaluation of uncertainties. Instead of waiting years for ideas and theories to be compared in the complex circumstances of interest to resource managers, these new programming environments will expedite the process. In the new paradigm, unproductive ideas and theories will be revealed more quickly, productive ideas and theories will more quickly be used to address our increasingly difficult water resources problems. As examples, two ideas in JUPITER API applications are presented: uncertainty correction factors that account for system complexities not represented in models, and PPR and OPR statistics used to identify new data needed to reduce prediction uncertainty.

  20. Quantifying K, U and Th contents of marine sediments using shipboard natural gamma radiation spectra measured on DV JOIDES Resolution

    Science.gov (United States)

    De Vleeschouwer, David; Dunlea, Ann G.; Auer, Gerald; Anderson, Chloe H.; Brumsack, Hans; de Loach, Aaron; Gurnis, Michael C.; Huh, Youngsook; Ishiwa, Takeshige; Jang, Kwangchul; Kominz, Michelle A.; März, Christian; Schnetger, Bernhard; Murray, Richard W.; Pälike, Heiko; Expedition 356 shipboard scientists, IODP

    2017-04-01

    During International Ocean Discovery Program (IODP) expeditions, shipboard-generated data provide the first insights into the cored sequences. The natural gamma radiation (NGR) of the recovered material, for example, is routinely measured on the ocean drilling research vessel DV JOIDES Resolution. At present, only total NGR counts are readily available as shipboard data, although full NGR spectra (counts as a function of gamma-ray energy level) are produced and archived. These spectra contain unexploited information, as one can estimate the sedimentary contents of potassium (K), thorium (Th), and uranium (U) from the characteristic gamma-ray energies of isotopes in the 40K, 232Th, and 238U radioactive decay series. Dunlea et al. [2013] quantified K, Th and U contents in sediment from the South Pacific Gyre by integrating counts over specific energy levels of the NGR spectrum. However, the algorithm used in their study is unavailable to the wider scientific community due to commercial proprietary reasons. Here, we present a new MATLAB algorithm for the quantification of NGR spectra that is transparent and accessible to future NGR users. We demonstrate the algorithm's performance by comparing its results to shore-based inductively coupled plasma-mass spectrometry (ICP-MS), inductively coupled plasma-emission spectrometry (ICP-ES), and quantitative wavelength-dispersive X-ray fluorescence (XRF) analyses. Samples for these comparisons come from eleven sites (U1341, U1343, U1366-U1369, U1414, U1428-U1430, U1463) cored in two oceans during five expeditions. In short, our algorithm rapidly produces detailed high-quality information on sediment properties during IODP expeditions at no extra cost. Dunlea, A. G., R. W. Murray, R. N. Harris, M. A. Vasiliev, H. Evans, A. J. Spivack, and S. D'Hondt (2013), Assessment and use of NGR instrumentation on the JOIDES Resolution to quantify U, Th, and K concentrations in marine sediment, Scientific Drilling, 15, 57-63.