WorldWideScience

Sample records for bogs

  1. Bog bodies

    DEFF Research Database (Denmark)

    Lynnerup, Niels

    2015-01-01

    In northern Europe during the Iron Age, many corpses were deposited in bogs. The cold, wet and anaerobic environment leads in many cases to the preservation of soft tissues, so that the bodies, when found and excavated several thousand years later, are remarkably intact. Since the 19th century th...

  2. Fra bog til film

    DEFF Research Database (Denmark)

    Schepelern, Peter

    2010-01-01

    Efter en historisk oversigt over samspillet mellem film og litteratur i dansk film, opstilles en råkke begreber, som filmatiseringer kan analyseres ud fra. Der ses pa det litteråre vårks status — evt. som klassiker eller bestseller. Der ses pa de centrale filmatiseringsproblemer, forhold som pråger...... adaptionsprocessen fra bog til film. De kan opdeles dels i forhold, der udspringer af filmsprogets specifikke sys- tem, dels forhold, der udspringer af filmens status som massemedium. Den färste kategori er pråget af, at filmsproget generelt fremstiller handling snarere end refleksion, noget konkret snarere end...... noget abstrakt, en scene snarere end et resume og det ydre snarere det indre. Den anden kategori kan forklare filmens tilbäjelighed til åndring af forlågget, til forkortelse, forenkling og modernisering. Eksemplerne er en råkke centrale danske film/romaner...

  3. Iron from Zealandic bog iron ore -

    DEFF Research Database (Denmark)

    Lyngstrøm, Henriette Syrach

    2011-01-01

    og geologiske materiale, metallurgiske analyser og eksperimentel arkæologiske forsøg - konturerne af en jernproduktion med udgangspunkt i den sjællandske myremalm. The frequent application by archaeologists of Werner Christensen’s distribution map for the occurrence of bog iron ore in Denmark (1966...... are sketched of iron production based on bog iron ore from Zealand....

  4. The systime iBog

    DEFF Research Database (Denmark)

    Ebbesen, Toke Riis

    2016-01-01

    This article proposes a method for critical analysis of design contributions and the material properties of digital textbooks aimed at tertiary schools, in the transition to digital publishing and from paper-based books to digitally available learning materials. The suggested method, adapted from...... an analytic methodology proposed by design semiotician Proni(Proni, 2002; Proni, 2010), is grounded in a material and cultural interdisciplinary perspective on books as designed artifacts. The method, combining close descriptions of material properties, prodution, use and cultural framing, is shown...... to be sufficient for predictive and practical design purposes in an analysis of the digital textbook the iBog by the Danish publisher Systime....

  5. "Den lille havfrue" som digital pop op-bog

    DEFF Research Database (Denmark)

    Mygind, Sarah

    2017-01-01

    Anmeldelse af: DIGITAL POP OP-BOG H. C. ANDERSEN OG BOOKS & MAGIC DEN LILLE HAVFRUE Bog og App til iOS & Android 5......Anmeldelse af: DIGITAL POP OP-BOG H. C. ANDERSEN OG BOOKS & MAGIC DEN LILLE HAVFRUE Bog og App til iOS & Android 5...

  6. [Metagenomics and biodiversity of sphagnum bogs].

    Science.gov (United States)

    Rusin, L Yu

    2016-01-01

    Biodiversity of sphagnum bogs is one of the richest and less studied, while these ecosystems are among the top ones in ecological, conservation, and economic value. Recent studies focused on the prokaryotic consortia associated with sphagnum mosses, and revealed the factors that maintain sustainability and productivity of bog ecosystems. High-throughput sequencing technologies provided insight into functional diversity of moss microbial communities (microbiomes), and helped to identify the biochemical pathways and gene families that facilitate the spectrum of adaptive strategies and largely foster the very successful colonization of the Northern hemisphere by sphagnum mosses. Rich and valuable information obtained on microbiomes of peat bogs sets off the paucity of evidence on their eukaryotic diversity. Prospects and expectations of reliable assessment of taxonomic profiles, relative abundance of taxa, and hidden biodiversity of microscopic eukaryotes in sphagnum bog ecosystems are briefly outlined in the context of today's metagenomics.

  7. Field Simulation of Global Change: Transplanting Northern Bog Mesocosms Southward

    NARCIS (Netherlands)

    Breeuwer, A.J.G.; Heijmans, M.M.P.D.; Robroek, B.J.M.; Berendse, F.

    2010-01-01

    A large proportion of northern peatlands consists of Sphagnum-dominated ombrotrophic bogs. In these bogs, peat mosses (Sphagnum) and vascular plants occur in an apparent stable equilibrium, thereby sustaining the carbon sink function of the bog ecosystem. How global warming and increased nitrogen

  8. Mining under kalina and Selisoo Bogs

    OpenAIRE

    Otsmaa, Merle

    2015-01-01

    Continuous developing of Estonian power engineering on the basis of oil shale requires ever taking into use of new exploration fields. When the reserve of Estonia mine is depleted, mining of the exploration field of Seli has to be started. But that field is located under the Selisoo bog which is defined as a region of the Natura 2000 network and is planned become a nature preserve. Conservationists are interested for what extent oil shale mining under the Selisoo bog and in its immediate near...

  9. Sphagnum bogs of Kelantan, Peninsular Malaysia

    NARCIS (Netherlands)

    Yao, T.L.; Kamarudin, S.; Chew, M.Y.; Kiew, R.

    2009-01-01

    Sphagnum bog, a unique plant community for Peninsular Malaysia was encountered on Padang Ragut, Kelantan. Its topographical features and flora are described, and compared with padang and upper montane floras. It is postulated that the community is derived from upper montane forest and is the result

  10. An ombrotrophic bog as a methane reservoir

    Science.gov (United States)

    Brown, Ann; Mathur, S. P.; Kushner, D. J.

    1989-09-01

    The distribution of methane in an ombrotrophic bog was examined by extracting the gas from different depths, using evacuated bottles and sampling tubes. Methane was extracted during 75 min, from 60 cm, 90 cm and 120 cm depths at 25 stations in a 24 meter-square area. The amount of methane extracted varied widely between samples, and this variation was greater within each depth than between the different depths. Approximately two and a half times as much methane was found at 90 cm and 120 cm depths as at 60 cm. The amount of methane from sites more than 60 cm below the surface can be correlated with the methane microbially produced from peat from the same site during laboratory incubations. Much less methane could be extracted from near-surface peat than from deeper levels, but laboratory incubations of peat from this level produced 10-fold more methane. Our results show that there is a considerable amount of methane trapped below 50 cm depth within an ombrotrophic bog, which we calculate in the bog studied to be 1.7 Gg. We suggest this entrapped methane reduces the hydraulic conductivity in the lower layers of the peat by blocking the soil pore spaces and preventing fluid movement; this in turn generates an elevated water table allowing the formation of a raised bog. We further suggest that if this peat is disturbed by mining or farming, the entrapped methane could be released into the atmosphere and add to the atmospheric pollution by greenhouse gases.

  11. [Methanotrophic bacteria of acid sphagnum bogs].

    Science.gov (United States)

    Dedysh, S N

    2002-01-01

    Acid sphagnum bogs cover a considerable part of the territory of Russia and are an important natural source of biogenic methane, which is formed in their anaerobic layers. A considerable portion of this methane is consumed in the aerobic part of the bog profile by acidophilic methanotrophic bacteria, which comprise the methane filter of sphagnum bogs and decrease CH4 emission to the atmosphere. For a long time, these bacteria escaped isolation, which became possible only after the elucidation of the optimal conditions of their functioning in situ: pH 4.5 to 5.5; temperature, from 15 to 20 degrees C; and low salt concentration in the solution. Reproduction of these conditions and rejection of earlier used media with a high content of biogenic elements allowed methanotrophic bacteria of two new genera and species--Methylocella palustris and Methylocapsa acidophila--to be isolated from the peat of sphagnum bogs of the northern part of European Russia and West Siberia. These bacteria are well adapted to the conditions in cold, acid, oligotrophic sphagnum bogs. They grow in a pH range of 4.2-7.5 with an optimum at 5.0-5.5, prefer moderate temperatures (15-25 degrees C) and media with a low content of mineral salts (200-500 mg/l), and are capable of active nitrogen fixation. Design of fluorescently labeled 16S rRNA-targeted oligonucleotide probes for the detection of Methylocella palustris and Methylocapsa acidophila and their application to the analysis of sphagnum peat samples showed that these bacteria represent dominant populations of methanotrophs with a density of 10(5)-10(6) cells/g peat. In addition to Methylocella and Methylocapsa populations, one more abundant population of methanotrophs was revealed (10(6) cells/g peat), which were phylogenetically close to the genus Methylocystis.

  12. Radionuclides in peat bogs and energy peat

    International Nuclear Information System (INIS)

    Helariutta, K.; Rantavaara, A.; Lehtovaara, J.

    2000-06-01

    The study was aimed at improving the general view on radionuclides contents in energy peat produced in Finland. The annual harvest of fuel peat in 1994 was studied extensively. Also thirteen peat bogs used for peat production and one bog in natural condition were analysed for vertical distributions of several radionuclides. These distributions demonstrate the future change in radioactivity of energy peat. Both natural nuclides emitting gamma radiation ( 238 U, 235 U, 232 Th, 226 Ra, 40 K) and radiocaesium ( 137 Cs, 134 Cs) origin in fallout from a nuclear power plant accident (1986) and in atmospheric nuclear weapon tests were analysed. The beta and alpha active natural nuclides of lead and polonium ( 210 Pb, 210 Po) were determined on a set of peat samples. These nuclides potentially contribute to radiation exposure through inhalation when partially released to atmosphere during combustion of peat. The activity concentrations of natural radionuclides often increased towards the deepest peat bog layers whereas the radioactive caesium deposited from atmosphere was missing in the deep layers. In undisturbed surface layers of a natural bog and peat production bogs the contents of 210 Pb and 210 Po exceeded those of the deeper peat layers. The nuclides of the uranium series in the samples were generally not in radioactive equilibrium, as different environmental processes change their activity ratios in peat. Radiation exposure from handling and utilisation of peat ash was estimated with activity indices derived from the data for energy peat harvested in 1994. Intervention doses were exceeded in a minor selection of samples due to 137 Cs, whereas natural radionuclides contributed very little to the doses. (orig.)

  13. Prospects for Sphagnum bogs subject to high nitrogen deposition

    NARCIS (Netherlands)

    Limpens, J.

    2003-01-01

    S phagnum bogs harbour a wealth of rare vascular plant and bryophyte species, preserve an amazing pollen record and are long-term sinks for atmospheric carbon. Unfortunately, the relatively low production and decomposition rates, that make these bogs such important environments,

  14. RAISED BOGS ON THE NORTH-EAST OF EUROPE

    Directory of Open Access Journals (Sweden)

    T. K. YURKOVSKAYA

    2004-01-01

    Full Text Available In the Northeastern Europe 2 types of raised bogs are distinguished: coastal (Southern White Sea raised hogs and continental (Pechora-Onega raised bogs. They have been compared as to their flora, prevailing syntaxa, characteristics of their complexes, structure of mire massifs and composition of peat deposits.

  15. RAISED BOGS ON THE NORTH-EAST OF EUROPE

    Directory of Open Access Journals (Sweden)

    T. K. YURKOVSKAYA

    2004-05-01

    Full Text Available In the Northeastern Europe 2 types of raised bogs are distinguished: coastal (Southern White Sea raised hogs and continental (Pechora-Onega raised bogs. They have been compared as to their flora, prevailing syntaxa, characteristics of their complexes, structure of mire massifs and composition of peat deposits.

  16. Radioactive fallout nuclides in a peat-bog ecosystem

    International Nuclear Information System (INIS)

    Pausch, G.; Hofmann, W.; Steger, F.; Tuerk, R.

    1996-01-01

    The Province of Salzburg belongs to the regions with the highest contamination from the Chernobyl-fallout outside the former USSR. The peat-bog investigated in this study is situated in Koppl, east of Salzburg. A peat-bog is a special example of an ecosystem, which is generally not disturbed by human activities because it is under strict nature-conservation and whose soil structure is not affected by animal activities from moles and earthworms. Peat-bogs are characterized by acidic soils which are high in organic material and low in clay mineral content. A number of previous studies have demonstrated that especially in peat-bogs and especially in the Koppl-peat-bog very high amounts of radioactive fallout nuclides from the Chernobyl accident and from the bomb-testings could be found

  17. Communities of larger fungi of ombrotrophic bogs in West Siberia

    Directory of Open Access Journals (Sweden)

    N.V. Filippova

    2014-11-01

    Full Text Available Bogs are common ecosystems in the Taiga of West Siberia. Little is known about mycological diversity in these important ecosystems. This article summarises the results of a two-year study of the macrofungi in two bogs near the town of Khanty-Mansiysk. Sporocarps were collected in 20 plots (about 300 m2 established in Mukhrino Bog as well as during random walks in Mukhrino Bog and Chistoe Bog in the late summer–autumn of 2012 and 2013. The plots were established in two common bog habitats representing the Ledo-Sphagnetum fusci (LS and Scheuchzerio palustris-Sphagnetum cuspidati (SS plant community associations. A total of 59 distinct fungal taxa were collected from the two bogs, with the LS association having a higher species richness and diversity than the SS association (50 taxa vs. 16 taxa and 30–40 taxa per 1000 m2 vs. 6–10 taxa per 1000 m2, respectively. Each of the two plant community associations has its own characteristic fungal taxa, with the LS association having 13 characteristic taxa and the SS association having five. Nearly two thirds of the fungal taxa are saprotrophic, mainly of Sphagnum spp., while others are mycorrhizal, mainly with Pinus spp. Most taxa were collected fewer than ten times during the study period and, hence, are considered rare and may need to be recognised for conservation programmes in this region.

  18. Establishing Sphagnum cultures on bog grassland, cut-over bogs, and floating mats: procedures, costs and area potential in Germany

    Directory of Open Access Journals (Sweden)

    S. Wichmann

    2017-04-01

    Full Text Available Sphagnum biomass is valued as a high-quality constituent of horticultural growing media. The cultivation of Sphagnum (peatmoss was tested successfully on peat soil and on artificial mats floating on acidic water bodies. But whether Sphagnum farming is economically feasible is unclear. Drawing on experience gained during four research projects in Germany we compared the procedures, costs and area potential for establishing large-scale Sphagnum cultures. Establishment costs were clearly lower for soil-based cultivation (€8.35 m-2 to €12.80 m 2 than for water-based cultivation (€17.34 m-2 to €21.43 m-2. Relating costs to the predicted dry mass yield over the total cultivation time resulted in values of €1,723 t-1 on cut-over bog, €2,646 t-1 on former bog grassland, €9,625 t -1 on floating mats without pre-cultivation and €11,833 t-1 on pre-cultivated Sphagnum mats. The high production costs of the mats (without pre-cultivation 54 % and with pre-cultivation 63 % of total costs resulted in the highest overall costs. In the case of soil-based Sphagnum cultures, the costs of purchasing Sphagnum diaspores were most influential (on bog grassland 46 % and on cut-over bog 71 % of total costs. The lowest costs relate to cut-over bog because of the smaller effort required for site preparation compared to taking off the topsoil of former bog grassland and the limited costs for the assumed irrigation system. In the case of former bog grassland, the high investment costs for the project-specific automatic water management boosted the establishment costs. Taking into account potential savings on the irrigation system and the high area potential, bog grassland emerges as the most promising land category for Sphagnum farming in Germany.

  19. Carbon dioxide emission from raised bog surface after peat extraction

    Directory of Open Access Journals (Sweden)

    Turbiak Janusz

    2017-12-01

    Full Text Available Research on CO2 emission from a raised bog after completion of peat extraction was performed in 2011–2013. CO2 emissions were determined by the chamber method. Twenty years after the termination of peat extraction, the bog surface was almost entirely devoid of plants. CO2 emission from the bog varied depending on temperature and water conditions and was 418 mg·m−2·h−1 on average during the research period. CO2 losses on the raised bog were on average 19.7 Mg·ha−1·year−1 during the research period which corresponded to a carbon loss of 5.37 Mg·ha−1·year−1 or mineralisation of 9.6 Mg·ha−1·year−1 of organic mass of 56% carbon content. It is possible to reduce organic mass losses and CO2 emission to the atmosphere from the bog surface after peat extraction has been terminated by reconstruction of initial water conditions, i.e. retaining a high ground water level and restoration of aquatic plant communities.

  20. Age estimation by 3D CT-scans of the Borremose Woman, a Danish bog body

    DEFF Research Database (Denmark)

    Villa, Chiara; Møller Rasmussen, Maria; Lynnerup, Niels

    2011-01-01

    Non-invasive estimation of age at death has been carried out by using 3D CT scanning of a bog body discovered in 1948 in a peat bog in Borremose (Denmark). The bog body has been dated to the 8th century BC, in the last part of the Bronze Age. The skeletal structures useful for age estimation have...

  1. {sup 137}Cs in a raised bog in central Sweden

    Energy Technology Data Exchange (ETDEWEB)

    Rosen, K. [Department of Soil and Environment, Swedish University of Agricultural Sciences, SLU, Ulls vag 17, Box 7014, SE-75007, Uppsala (Sweden)], E-mail: klas.rosen@mv.slu.se; Vinichuk, M. [Department of Soil and Environment, Swedish University of Agricultural Sciences, SLU, Ulls vag 17, Box 7014, SE-75007, Uppsala (Sweden); Department of Ecology, Zhytomyr State Technological University, 103 Cherniakhovsky Str., 10005 Zhytomyr (Ukraine); Johanson, K.J. [Department of Soil and Environment, Swedish University of Agricultural Sciences, SLU, Ulls vag 17, Box 7014, SE-75007, Uppsala (Sweden)

    2009-07-15

    The vertical distribution of {sup 137}Cs activity in peat soil profiles and {sup 137}Cs activity concentration in plants of various species was studied in samples collected at two sites on a raised bog in central Sweden. One site (open bog) was in an area with no trees and only a few sparsely growing plant species, while the other (low pine) was less than 100 m from the open bog site and had slowly growing Scots pine, a field layer dominated by some ericaceous plants and ground well-covered by plants. The plant samples were collected in 2004-2007 and were compared with samples collected in 1989 from the same open bog and low pine sites. Ground deposition of {sup 137}Cs in 2005 was similar at both sites, 23 000 Bq m{sup -2}. In the open bog peat profile it seems to be an upward transport of caesium since a clear peak of {sup 137}Cs activity was found in the uppermost 1-4 cm of Sphagnum layers, whereas at the low pine site {sup 137}Cs was mainly found in deeper (10-12 cm) layers. The migration rate was 0.57 cm yr{sup -1} at the open bog site and the migration centre of {sup 137}Cs was at a depth of 10.7, while the rate at the low pine site was 0.78 cm yr{sup -1} and the migration centre was at 14.9 cm. Heather (Calluna vulgaris) was the plant species with the highest {sup 137}Cs activity concentrations at both sites, 43.5 k Bq{sup -1} DM in 1989 decreasing to 20.4 in 2004-2007 on open bog and 22.3 k Bq kg{sup -1} DM in 1989 decreasing to 11.2 k Bq{sup -1} DM by the period 2004-2007 on the low pine site. {sup 137}Cs transfer factors in plants varied between 0.88 and 1.35 on the open bog and between 0.48 and 0.69 m{sup 2} kg{sup -1} DM at the low pine site.

  2. 137Cs in a raised bog in central Sweden

    International Nuclear Information System (INIS)

    Rosen, K.; Vinichuk, M.; Johanson, K.J.

    2009-01-01

    The vertical distribution of 137 Cs activity in peat soil profiles and 137 Cs activity concentration in plants of various species was studied in samples collected at two sites on a raised bog in central Sweden. One site (open bog) was in an area with no trees and only a few sparsely growing plant species, while the other (low pine) was less than 100 m from the open bog site and had slowly growing Scots pine, a field layer dominated by some ericaceous plants and ground well-covered by plants. The plant samples were collected in 2004-2007 and were compared with samples collected in 1989 from the same open bog and low pine sites. Ground deposition of 137 Cs in 2005 was similar at both sites, 23 000 Bq m -2 . In the open bog peat profile it seems to be an upward transport of caesium since a clear peak of 137 Cs activity was found in the uppermost 1-4 cm of Sphagnum layers, whereas at the low pine site 137 Cs was mainly found in deeper (10-12 cm) layers. The migration rate was 0.57 cm yr -1 at the open bog site and the migration centre of 137 Cs was at a depth of 10.7, while the rate at the low pine site was 0.78 cm yr -1 and the migration centre was at 14.9 cm. Heather (Calluna vulgaris) was the plant species with the highest 137 Cs activity concentrations at both sites, 43.5 k Bq -1 DM in 1989 decreasing to 20.4 in 2004-2007 on open bog and 22.3 k Bq kg -1 DM in 1989 decreasing to 11.2 k Bq -1 DM by the period 2004-2007 on the low pine site. 137 Cs transfer factors in plants varied between 0.88 and 1.35 on the open bog and between 0.48 and 0.69 m 2 kg -1 DM at the low pine site.

  3. Species identification of archaeological skin objects from Danish bogs

    DEFF Research Database (Denmark)

    Brandt, Luise Ørsted; Schmidt, Anne Lisbeth; Mannering, Ulla

    2014-01-01

    environment of peat bogs leading to morphological and molecular degradation within the samples. We compared species assignment results of twelve archaeological skin samples from Danish bogs using Mass Spectrometry (MS)-based peptide sequencing, against results obtained using light and scanning electron...... microscopy. While it was difficult to obtain reliable results using microscopy, MS enabled the identification of several species-diagnostic peptides, mostly from collagen and keratins, allowing confident species discrimination even among taxonomically close organisms, such as sheep and goat. Unlike previous...

  4. Woodcock Bog Research Natural Area: guidebook supplement 40

    Science.gov (United States)

    Reid Schuller; Susan J. Fritts; Mark Mousseaux

    2010-01-01

    This guidebook describes Woodcock Bog Research Natural Area (RNA), a 114-ha (281-ac) area located within the Klamath-Siskiyou ecoregion in southwestern Oregon. The RNA includes a hanging fen and stream segment on ultramafic rock and derived soils. Numerous plant species occur within the fens that are endemic to the Klamath-Siskiyou Mountains of southwestern Oregon and...

  5. A Species Distribution Modeling Informed Conservation Assessment of Bog Spicebush

    Science.gov (United States)

    2016-09-14

    ERDC develops innovative solutions in civil and military engineering, geospatial sciences, water resources, and environmental sciences for the Army...Natural Resources Program. This work was conducted by the Ecological Processes Branch (CNN), In- stallations Division (CN), Construction Engineering...declining number of Bog Spicebush populations, as well as limited information about the species’ ecology , indicate species distribution modeling would

  6. Atmospheric nitrogen deposition promotes carbon loss from peat bogs

    NARCIS (Netherlands)

    Bragazza, L.; Freeman, C.; Jones, T.; Rydin, H.; Limpens, J.; Fenner, N.; Ellis, T.; Gerdol, R.; Hajek, M.; Hajek, T.; Iacumin, P.; Kutnar, L.; Tahvanainen, T.; Toberman, H.

    2006-01-01

    Peat bogs have historically represented exceptional carbon (C) sinks because of their extremely low decomposition rates and consequent accumulation of plant remnants as peat. Among the factors favoring that peat accumulation, a major role is played by the chemical quality of plant litter itself,

  7. Bog bilberry phenolics, antioxidant capacity and nutrient profile

    Czech Academy of Sciences Publication Activity Database

    Colak, N.; Torun, H.; Grúz, Jiří; Strnad, Miroslav; Hermosín-Gutiérrez, I.; Hayirlioglu-Ayaz, S.; Ayaz, F. A.

    2016-01-01

    Roč. 201, JUN 15 (2016), s. 339-349 ISSN 0308-8146 R&D Projects: GA ČR GA14-34792S; GA MŠk(CZ) LO1204; GA MŠk LK21306 Institutional support: RVO:61389030 Keywords : Vaccinium uliginosum * Bog bilberry * Phenolic acid Subject RIV: EF - Botanics Impact factor: 4.529, year: 2016

  8. Dating bog bodies by means of C-14-AMS

    NARCIS (Netherlands)

    van der Plicht, J; van der Sanden, WAB; Aerts, AT; Streurman, HJ

    We have made efforts to date a substantial number of bodies from northwest European peat bogs by means of C-14. In our research, we compared materials such as skin, hair, bone, textile, leather and wood where available. Most of the bodies we investigated were found to date from the Late Iron

  9. Dating Danish textiles and skins from bog finds by means of 14C AMS

    DEFF Research Database (Denmark)

    Mannering, Ulla; Possnert, Göran; Heinemeier, Jan

    2010-01-01

    This paper presents the results of 44 new 14C analyses of Danish Early Iron Age textiles and skins. Of 52 Danish bog finds containing skin and textile items, 30 are associated with bog bodies. Until now, only 18 of these have been dated. In this paper we add dates to the remaining finds. The resu......This paper presents the results of 44 new 14C analyses of Danish Early Iron Age textiles and skins. Of 52 Danish bog finds containing skin and textile items, 30 are associated with bog bodies. Until now, only 18 of these have been dated. In this paper we add dates to the remaining finds....... The results demonstrate that the Danish custom of depositing clothed bodies in a bog is centred to the centuries immediately before and at the beginning of the Common Era. Most of these bodies are carefully placed in the bog - wrapped or dressed in various textile and/or skin garments....

  10. Metabolism of nonparticulate phosphorus in an acid bog lake

    International Nuclear Information System (INIS)

    Koenings, J.P.

    1977-01-01

    In North Gate Lake, an acid bog lake located on the northern Michigan-Wisconsin border, U.S.A., the algal nutrient inorganic phosphate (FRP) is not detectable by chemical means. Organic phosphorus (FUP) represents 100% of the detectable filterable phosphorus. The availability and cycling of this organic fraction are of considerable interest in regard to the primary productivity of this system. To clarify these relationships, the cycling of nonparticulate forms of phosphorus found in the epilimnion of this lake was studied

  11. Metabolism of nonparticulate phosphorus in an acid bog lake

    Energy Technology Data Exchange (ETDEWEB)

    Koenings, J. P.

    1977-01-01

    In North Gate Lake, an acid bog lake located on the northern Michigan-Wisconsin border, U.S.A., the algal nutrient inorganic phosphate (FRP) is not detectable by chemical means. Organic phosphorus (FUP) represents 100% of the detectable filterable phosphorus. The availability and cycling of this organic fraction are of considerable interest in regard to the primary productivity of this system. To clarify these relationships, the cycling of nonparticulate forms of phosphorus found in the epilimnion of this lake was studied.

  12. Properties and structure of raised bog peat humic acids

    Science.gov (United States)

    Klavins, Maris; Purmalis, Oskars

    2013-10-01

    Humic substances form most of the organic components of soil, peat and natural waters, and their structure and properties differ very much depending on their source. The aims of this study are to characterize humic acids (HAs) from raised bog peat, to evaluate the homogeneity of peat HAs within peat profiles, and to study peat humification impact on properties of HAs. A major impact on the structure of peat HAs have lignin-free raised bog biota (dominantly represented by bryophytes of different origin). On diagenesis scale, peat HAs have an intermediate position between the living organic matter and coal organic matter, and their structure is formed in a process in which more labile structures (carbohydrates, amino acids, etc.) are destroyed, while thermodynamically more stable aromatic and polyaromatic structures emerge as a result of abiotic synthesis. However, in comparison with soil, aquatic and other HAs, aromaticity of peat HAs is much lower. Comparatively, the raised bog peat HAs are at the beginning of the transformation process of living organic matter. Concentrations of carboxyl and phenolic hydroxyl groups change depending on the peat age and decomposition degree from where HAs have been isolated, and carboxylic acidity of peat HAs increases with peat depth and humification degree.

  13. Age estimation by 3D CT-scans of the Borremose Woman, a Danish bog body

    DEFF Research Database (Denmark)

    Villa, Chiara; Møller Rasmussen, Maria; Lynnerup, Niels

    2011-01-01

    Non-invasive estimation of age at death has been carried out by using 3D CT scanning of a bog body discovered in 1948 in a peat bog in Borremose (Denmark). The bog body has been dated to the 8th century BC, in the last part of the Bronze Age. The skeletal structures useful for age estimation have...... been visualized from CT-scans using the Mimics software from Materialise. Extensive manual editing was necessary, as is common with bog bodies, since the bones were severely degraded and the ordinary range of Hounsfield Units (HU), used for clinical work, is not suitable. Only the cranium, the left...

  14. The fungal consortium of Andromeda polifolia in bog habitats

    Directory of Open Access Journals (Sweden)

    N.V. Filippova

    2015-09-01

    Full Text Available (1 Andromeda polifolia (bog rosemary is a common plant species in northern circumboreal peatlands. While not a major peat-forming species in most peatlands, it is characterised by a substantial woody below-ground biomass component that contributes directly to the accumulation of organic matter below the moss surface, as well as sclerophyllous leaf litter that contributes to the accumulation of organic matter above the moss surface. Rather little is known about the fungal communities associated with this plant species. Hence, we investigated the fungal consortium of A. polifolia in three distinct vegetation communities of ombrotrophic bogs near Khanty-Mansiysk, West Siberia, Russia, in 2012 and 2013. These vegetation communities were forested bog (Tr = treed, Sphagnum-dominated lawn (Ln, and Eriophorum-Sphagnum-dominated hummock (Er. (2 In total, 37 fungal taxa, belonging to five classes and 16 families, were identified and described morphologically. Seven fungal species were previously known from Andromeda as host. Others are reported for the first time, thus considerably expanding the fungal consortium of this dwarf shrub. Most taxa were saprobic on fallen leaves of A. polifolia found amongst Sphagnum in the bog. Two taxa were parasitic on living plant tissues and one taxon was saprobic on dead twigs. Three taxa, recorded only on A. polifolia leaves and on no other plant species or materials, may be host-specific to this dwarf shrub. (3 A quantitative analysis of the frequency of occurrence of all taxa showed that one taxon (Coccomyces duplicarioides was very abundant, 64 % of the taxa occurred frequently, and 32 % of the taxa occurred infrequently. The mean Shannon diversity index of the community was 2.4. (4 There were no statistical differences in the fungal community composition of A. polifolia in the three vegetation communities investigated in this study. Redundancy analysis suggested that some fungal taxa were positively, and others

  15. Persistent versus transient tree encroachment of temperate peat bogs: effects of climate warming and drought events

    NARCIS (Netherlands)

    Heijmans, M.M.P.D.; Knaap, Y.A.M.; Holmgren, M.; Limpens, J.

    2013-01-01

    Peatlands store approximately 30% of global soil carbon, most in moss-dominated bogs. Future climatic changes, such as changes in precipitation patterns and warming, are expected to affect peat bog vegetation composition and thereby its long-term carbon sequestration capacity. Theoretical work

  16. 137Cs deposition in peat profiles on a raised bog in central Sweden

    International Nuclear Information System (INIS)

    Rosen, K.; Vinichuk, M.; Galan, P.R.; Johanson, K.J.

    2009-01-01

    Distribution of 137 Cs depositions within peat profiles in open bog and nearby (low pine) sites in raised bog are shown and discussed. A possible involvement of Sphagnum moss in radionuclide binding and retention in such nutrient poor ecosystem is suggested. (au)

  17. The importance of groundwater-derived carbon dioxide in the restoration of small Sphagnum bogs

    NARCIS (Netherlands)

    Patberg, Wouter; Baaijens, Gert Jan; Smolders, Alfons J. P.; Grootjans, Ab P.; Elzenga, J. Theo M.

    Essential for successful bog restoration is the reestablishment of Sphagnum mosses. High carbon dioxide availability has been shown to be of great importance for the growth of Sphagnum mosses. In well-developed Sphagnum bogs large amounts of carbon dioxide are produced by (an)aerobic decomposition

  18. Hounsfield Units ranges in CT-scans of bog bodies and mummies

    DEFF Research Database (Denmark)

    Villa, Chiara; Lynnerup, Niels

    2012-01-01

    (peat bog, cold-dry and hot-dry environment). We also analyzed the impact of different museal preservation techniques on the HU ranges, as e.g. in the Tollund Man and Grauballe Man, two bog bodies from Denmark. The HU results for mummies were compared with HU results from forensic cases, cremated...

  19. Temperature-Induced Increase in Methane Release from Peat Bogs: A Mesocosm Experiment

    NARCIS (Netherlands)

    van Winden, J.F.; Reichart, G.J.; McNamara, N.P.; Benthien, A.; Sinninghe Damsté, J.S.

    2012-01-01

    Peat bogs are primarily situated at mid to high latitudes and future climatic change projections indicate that these areas may become increasingly wetter and warmer. Methane emissions from peat bogs are reduced by symbiotic methane oxidizing bacteria (methanotrophs). Higher temperatures and

  20. Temperature-induced increase in methane release from peat bogs: A mesocosm experiment

    NARCIS (Netherlands)

    Winden, J.F. van; Reichart, G.-J.; McNamara, N.P.; Benthien, A.; Sinninghe Damsté, J.S.

    2012-01-01

    Peat bogs are primarily situated at mid to high latitudes and future climatic change projections indicate that these areas may become increasingly wetter and warmer. Methane emissions from peat bogs are reduced by symbiotic methane oxidizing bacteria (methanotrophs). Higher temperatures and

  1. Effects of elevated CO2 and vascular plants on evapotranspiration in bog vegetation

    NARCIS (Netherlands)

    Heijmans, M.M.P.D.; Arp, W.J.; Berendse, F.

    2001-01-01

    We determined evapotranspiration in three experiments designed to study the effects of elevated CO2 and increased N deposition on ombrotrophic bog vegetation. Two experiments used peat monoliths with intact bog vegetation in containers, with one experiment outdoors and the other in a greenhouse. A

  2. Persistent versus transien tree encroachment of temperate peat bogs: effects of climate warming and drought events.

    NARCIS (Netherlands)

    Heijmans, M.M.P.D.; van der Knaap, Y.A.M.; Holmgren, M.; Limpens, J.

    2013-01-01

    Peatlands store approximately 30% of global soil carbon, most in moss-dominated bogs. Future climatic changes, such as changes in precipitation patterns and warming, are expected to affect peat bog vegetation composition and thereby its long-term carbon sequestration capacity. Theoretical work

  3. Ecological networks and nature policy in central Russia : peat bogs in central and northern Meshera

    NARCIS (Netherlands)

    Butovsky, R.O.; Reijnen, R.; Otchagov, D.M.; Aleshenko, G.M.; Melik-Bagdasarov, E.

    2001-01-01

    In central and northern Meshera, Russia, the habitat of many characteristic peat bog species now show a very fragmented pattern. Peat mining and other human influences are the most important causes. As a result the potentials for viable populations ofcharacteristic peat bog species have decreased

  4. Assessing the conservation potential of damaged peat bog networks in Central and Northern Meshera (Central Russia)

    NARCIS (Netherlands)

    Butovsky, R.O.; Reijnen, M.J.S.M.; Aleshenko, G.M.; Melik-Bagdasarov, E.M.; Otchagov, D.M.

    2004-01-01

    Peat bogs are one of the most characteristic ecosystems of Central Russian landscape. Because of peat mining and transformation of peat bogs into agricultural land after drainage, suitable habitats for several characteristic species now show a very fragmented pattern. The potentials for viable

  5. Aged anthropogenic iodine in a boreal peat bog

    International Nuclear Information System (INIS)

    Maillant, S.; Sheppard, M.I.; Denys, S.; Leclerc Cessac, E.

    2004-01-01

    Iodine-129 is a radionuclide of major concern in the international safety assessments for deep geological storage and disposal of nuclear waste because it migrates quickly through the geosphere to the biosphere and then from the soil to humans through the food-chain. However, in organic soils the 129 I may be immobilized over a long time period, and so these soils represent a potential accumulation point in the biosphere. Effects of long residence times of iodine in soils are scarce. The present paper gives some insight on the aging of stable iodine, under natural conditions. Stable iodine was introduced as KI in 1987 at the base of a small natural sphagnum bog to simulate arrival of iodine via a groundwater discharge from the geosphere. Previous data revealed the spread of the iodine outwards spatially from the basal spike and also recorded its rise towards the bog surface. Fifteen years later, the groundwater, the soil and the vegetation have been sampled and analyzed for iodine. The results we will present give insight on the mobility of 'aged' iodine with time, the retention properties of the peat, and provide iodine transfer factors for native boreal plant species. The data show iodine: - continues to slowly spread from the spike after 15 years, - is more strongly retained on the solid phase at the surface than at depth, - the chemical structure of the peat may influence the retention of iodine as shown by NMR analysis, - iodine retention has become greater with time, and - herbaceous species are the greatest accumulators. This study demonstrates bogs present good sinks for iodine and limit the transfer of iodine to some of the 'wildlife' food-chains. (author)

  6. Microform-related community patterns of methane-cycling microbes in boreal Sphagnum bogs are site specific.

    Science.gov (United States)

    Juottonen, Heli; Kotiaho, Mirkka; Robinson, Devin; Merilä, Päivi; Fritze, Hannu; Tuittila, Eeva-Stiina

    2015-09-01

    Vegetation and water table are important regulators of methane emission in peatlands. Microform variation encompasses these factors in small-scale topographic gradients of dry hummocks, intermediate lawns and wet hollows. We examined methane production and oxidization among microforms in four boreal bogs that showed more variation of vegetation within a bog with microform than between the bogs. Potential methane production was low and differed among bogs but not consistently with microform. Methane oxidation followed water table position with microform, showing higher rates closer to surface in lawns and hollows than in hummocks. Methanogen community, analysed by mcrA terminal restriction fragment length polymorphism and dominated by Methanoregulaceae or 'Methanoflorentaceae', varied strongly with bog. The extent of microform-related variation of methanogens depended on the bog. Methanotrophs identified as Methylocystis spp. in pmoA denaturing gradient gel electrophoresis similarly showed effect of bog, and microform patterns were stronger within individual bogs. Our results suggest that methane-cycling microbes in boreal Sphagnum bogs with seemingly uniform environmental conditions may show strong site-dependent variation. The bog-intrinsic factor may be related to carbon availability but contrary to expectations appears to be unrelated to current surface vegetation, calling attention to the origin of carbon substrates for microbes in bogs. © FEMS 2015. All rights reserved. For permissions, please e-mail: journals.permissions@oup.com.

  7. Rain increases methane production and methane oxidation in a boreal thermokarst bog

    Science.gov (United States)

    Neumann, R. B.; Moorberg, C.; Turner, J.; Wong, A.; Waldrop, M. P.; Euskirchen, E. S.; Edgar, C.; Turetsky, M. R.

    2017-12-01

    Bottom-up biogeochemical models of wetland methane emissions simulate the response of methane production, oxidation and transport to wetland conditions and environmental forcings. One reason for mismatches between bottom-up and top-down estimates of emissions is incomplete knowledge of factors and processes that control microbial rates and methane transport. To advance mechanistic understanding of wetland methane emissions, we conducted a multi-year field investigation and plant manipulation experiment in a thermokarst bog located near Fairbanks, Alaska. The edge of the bog is experiencing active permafrost thaw, while the center of the bog thawed 50 to 100 years ago. Our study, which captured both an average year and two of the wettest years on record, revealed how rain interacts with vascular vegetation and recently thawed permafrost to affect methane emissions. In the floating bog, rain water warmed and oxygenated the subsurface, but did not alter soil saturation. The warmer peat temperatures increased both microbial methane production and plant productivity at the edge of the bog near the actively thawing margin, but minimally altered microbial and plant activity in the center of the bog. These responses indicate processes at the edge of the bog were temperature limited while those in the center were not. The compounding effect of increased microbial activity and plant productivity at the edge of the bog doubled methane emissions from treatments with vascular vegetation during rainy years. In contrast, methane emissions from vegetated treatments in the center of the bog did not change with rain. The oxygenating influence of rain facilitated greater methane oxidation in treatments without vascular vegetation, which offset warming-induced increases in methane production at the edge of the bog and decreased methane emissions in the center of the bog. These results elucidate the complex and spatially variable response of methane production and oxidation in

  8. Controls on evapotranspiration in a west Siberian bog

    Science.gov (United States)

    Shimoyama, K.; Hiyama, T.; Fukushima, Y.; Inoue, G.

    2004-04-01

    This study analyzed controls on evapotranspiration (E) from a western Siberian bog, from a perspective that surface constraints limit the E available for atmospheric evapotranspiration demands. Ratios of E to potential evapotranspiration (EP) ranged from 0.2 to 0.9, and were clearly related to changes in surface constraints represented by the bulk transfer coefficient for latent heat CE (= βCH where β is the surface moisture availability and CH is the bulk transfer coefficient for sensible heat). Both EP and equilibrium evaporation (EEQ) showed similar seasonal trends, suggesting the importance of radiation to the seasonal variation of EP. The atmospheric drying power (Ea) was a minor factor in EP and showed less seasonal change during most of the growing season. However, the presence of a dry air mass caused by synoptic scale advection (most frequently observed in May 1999) significantly enhanced Ea; consequently, the seasonal maximum of EP occurred earlier than the seasonal maximum of EEQ. Values for CH (0.004-0.011) increased with leaf area index except Sphagnum moss (LAIg), indicating that vegetation growth contributes to changes in bog roughness through canopy height changes. The β value gradually decreased with decreases in the water table position (zwt); the open water surface area and water content of Sphagnum moss depended on zwt. Furthermore, the absence of a significant relationship between β and phenology implies that changes in evaporation contribute to variations in E more than changes in transpiration. Hence roughness change created by vegetation growth and surface wetness limit evapotranspiration to less than the potential evapotranspiration.

  9. Electrocoagulation treatment of peat bog drainage water containing humic substances.

    Science.gov (United States)

    Kuokkanen, V; Kuokkanen, T; Rämö, J; Lassi, U

    2015-08-01

    Electrocoagulation (EC) treatment of 100 mg/L synthetic wastewater (SWW) containing humic acids was optimized (achieving 90% CODMn and 80% DOC removal efficiencies), after which real peat bog drainage waters (PBDWs) from three northern Finnish peat bogs were also treated. High pollutant removal efficiencies were achieved: Ptot, TS, and color could be removed completely, while Ntot, CODMn, and DOC/TOC removal efficiencies were in the range of 33-41%, 75-90%, and 62-75%, respectively. Al and Fe performed similarly as the anode material. Large scale experiments (1 m(3)) using cold (T = 10-11 °C) PBDWs were also conducted successfully, with optimal treatment times of 60-120 min (applying current densities of 60-75 A/m(2)). Residual values of Al and Fe (complete removal) were lower than their initial values in the EC-treated PBDWs. Electricity consumption and operational costs in optimum conditions were found to be low and similar for all the waters studied: 0.94 kWh/m(3) and 0.15 €/m(3) for SWW and 0.35-0.70 kWh/m(3) and 0.06-0.12 €/m(3) for the PBDWs (large-scale). Thus, e.g. solar cells could be considered as a power source for this EC application. In conclusion, EC treatment of PBDW containing humic substances was shown to be feasible. Copyright © 2015 Elsevier Ltd. All rights reserved.

  10. Regional patterns and controlling factors in plant species composition and diversity in Canadian lowland coastal bogs and laggs

    Directory of Open Access Journals (Sweden)

    S.A. Howie

    2016-11-01

    Full Text Available Inventories of natural assemblages of plant species are critical when planning ecological restoration of bogs. However, little is known about the regional variation in plant communities at the margins (laggs of bogs, even though they are an integral element of raised bog ecosystems. Therefore, we investigated the regional patterns in the plant communities of bogs and laggs, and the factors that control them, for thirteen bogs in coastal British Columbia, Canada. Species richness was significantly higher in the bogs and laggs of the cooler, wetter Pacific Oceanic wetland region. Beta Diversity analyses showed that bogs in the Pacific Oceanic wetland region often shared species with their respective laggs, whereas half of the laggs in the warmer, drier Pacific Temperate wetland region had no species in common with the adjacent bogs and were thus more ecologically distinct from the bog. Primary climatic variables, such as mean annual precipitation, mean annual temperature and latitude, as well as climate-influenced variables, such as pH, peat depth, and Na+ concentrations were the main correlates of plant species composition in the studied bogs. Site-specific factors, particularly depth to water table, and fraction of inorganic material in peat samples, were as strongly related to lagg plant communities as climate, while hydrochemistry appeared to have less influence.

  11. Enhanced sensitivity of a mountain bog to climate change as a delayed effect of road construction

    Directory of Open Access Journals (Sweden)

    P. von Sengbusch

    2015-01-01

    Full Text Available Trees of Pinus rotundata (bog pine characterise many bogs in the mid-altitude mountains of central Europe (Switzerland, East and South Germany, Czech Republic. The research described here focuses on recent changes in the growth of bog pine on the Ennersbacher Moor, a mountain mire in the Black Forest (south-west Germany. An increase in the cover of bog pine is usually caused by drainage and subsequent drawdown of the water table. However, this bog has not been drained or directly disturbed in any other way. One possible explanation is that a road constructed in 1983 along one margin of the bog has diverted part of its water supply. Even though the road was designed to conduct potentially salt-contaminated drainage water away from the bog, its construction did not cause an immediate vegetation response in the 1980s and 1990s. Therefore, I hypothesise that it enhanced the sensitivity of the bog to climatic stress, predisposing it to a succession that was eventually triggered by a series of drought years in 2009–2011. Data collected near the centre of the bog over the period 1998–2014 indicate not only a distinct change in the relationship between height and trunk circumference of the trees, but also an increase of dwarf shrub cover and changes in the composition of Sphagnum communities. Although the pH of near-surface water may have increased slightly over this period, pH and EC values remain within typical ranges for raised bogs in the Black Forest. Examination of peat profiles reveals that the peat is more highly humified now than it was in 2002, and water table records from 2012–2014 show a greater amplitude of fluctuation than water table data collected in 1998–2001. Even though its mean level is only 105 mm below the ground surface, the water table is now observed to fall rapidly to depths of at least 350 mm during both wet and dry summers. Mapping surface (mesotopography and flow lines from the adjacent slope shows that the

  12. Climate-driven expansion of blanket bogs in Britain during the Holocene

    Science.gov (United States)

    Gallego-Sala, A. V.; Charman, D. J.; Harrison, S. P.; Li, G.; Prentice, I. C.

    2016-01-01

    Blanket bog occupies approximately 6 % of the area of the UK today. The Holocene expansion of this hyperoceanic biome has previously been explained as a consequence of Neolithic forest clearance. However, the present distribution of blanket bog in Great Britain can be predicted accurately with a simple model (PeatStash) based on summer temperature and moisture index thresholds, and the same model correctly predicts the highly disjunct distribution of blanket bog worldwide. This finding suggests that climate, rather than land-use history, controls blanket-bog distribution in the UK and everywhere else. We set out to test this hypothesis for blanket bogs in the UK using bioclimate envelope modelling compared with a database of peat initiation age estimates. We used both pollen-based reconstructions and climate model simulations of climate changes between the mid-Holocene (6000 yr BP, 6 ka) and modern climate to drive PeatStash and predict areas of blanket bog. We compiled data on the timing of blanket-bog initiation, based on 228 age determinations at sites where peat directly overlies mineral soil. The model predicts that large areas of northern Britain would have had blanket bog by 6000 yr BP, and the area suitable for peat growth extended to the south after this time. A similar pattern is shown by the basal peat ages and new blanket bog appeared over a larger area during the late Holocene, the greatest expansion being in Ireland, Wales, and southwest England, as the model predicts. The expansion was driven by a summer cooling of about 2 °C, shown by both pollen-based reconstructions and climate models. The data show early Holocene (pre-Neolithic) blanket-bog initiation at over half of the sites in the core areas of Scotland and northern England. The temporal patterns and concurrence of the bioclimate model predictions and initiation data suggest that climate change provides a parsimonious explanation for the early Holocene distribution and later expansion of

  13. Persistent versus transient tree encroachment of temperate peat bogs: effects of climate warming and drought events.

    Science.gov (United States)

    Heijmans, Monique M P D; van der Knaap, Yasmijn A M; Holmgren, Milena; Limpens, Juul

    2013-07-01

    Peatlands store approximately 30% of global soil carbon, most in moss-dominated bogs. Future climatic changes, such as changes in precipitation patterns and warming, are expected to affect peat bog vegetation composition and thereby its long-term carbon sequestration capacity. Theoretical work suggests that an episode of rapid environmental change is more likely to trigger transitions to alternative ecosystem states than a gradual, but equally large, change in conditions. We used a dynamic vegetation model to explore the impacts of drought events and increased temperature on vegetation composition of temperate peat bogs. We analyzed the consequences of six patterns of summer drought events combined with five temperature scenarios to test whether an open peat bog dominated by moss (Sphagnum) could shift to a tree-dominated state. Unexpectedly, neither a gradual decrease in the amount of summer precipitation nor the occurrence of a number of extremely dry summers in a row could shift the moss-dominated peat bog permanently into a tree-dominated peat bog. The increase in tree biomass during drought events was unable to trigger positive feedbacks that keep the ecosystem in a tree-dominated state after a return to previous 'normal' rainfall conditions. In contrast, temperature increases from 1 °C onward already shifted peat bogs into tree-dominated ecosystems. In our simulations, drought events facilitated tree establishment, but temperature determined how much tree biomass could develop. Our results suggest that under current climatic conditions, peat bog vegetation is rather resilient to drought events, but very sensitive to temperature increases, indicating that future warming is likely to trigger persistent vegetation shifts. © 2013 Blackwell Publishing Ltd.

  14. Functional diversity, succession, and human-mediated disturbances in raised bog vegetation.

    Science.gov (United States)

    Dyderski, Marcin K; Czapiewska, Natalia; Zajdler, Mateusz; Tyborski, Jarosław; Jagodziński, Andrzej M

    2016-08-15

    Raised and transitional bogs are one of the most threatened types of ecosystem, due to high specialisation of biota, associated with adaptations to severe environmental conditions. The aim of the study was to characterize the relationships between functional diversity (reflecting ecosystem-shaping processes) of raised bog plant communities and successional gradients (expressed as tree dimensions) and to show how impacts of former clear cuts may alter these relationships in two raised bogs in 'Bory Tucholskie' National Park (N Poland). Herbaceous layers of the plant communities were examined by floristic relevés (25m(2)) on systematically established transects. We also assessed patterns of tree ring widths. There were no relationships between vegetation functional diversity components and successional progress: only functional dispersion was negatively, but weakly, correlated with median DBH. Lack of these relationships may be connected with lack of prevalence of habitat filtering and low level of competition over all the successional phases. Former clear cuts, indicated by peaks of tree ring width, influenced the growth of trees in the bogs studied. In the bog with more intensive clear cuts we found more species with higher trophic requirements, which may indicate nutrient influx. However, we did not observe differences in vegetation patterns, functional traits or functional diversity indices between the two bogs studied. We also did not find an influence of clear cut intensity on relationships between functional diversity indices and successional progress. Thus, we found that alteration of the ecosystems studied by neighbourhood clear cuts did not affect the bogs strongly, as the vegetation was resilient to these impacts. Knowledge of vegetation resilience after clear cuts may be crucial for conservation planning in raised bog ecosystems. Copyright © 2016 Elsevier B.V. All rights reserved.

  15. Interactions between Nitrogen Fixation and Methane Cycling in Northern Minnesota Peat Bogs

    Science.gov (United States)

    Warren, M. J.; Gaby, J. C.; Lin, X.; Morton, P. L.; Kostka, J. E.; Glass, J. B.

    2014-12-01

    Peatlands cover only 3% of the Earth's surface, yet store a third of soil carbon. Increasing global temperatures have the potential to change peatlands from a net sink to a net source of atmospheric carbon. N is a limiting nutrient in oligotrophic Sphagnum-dominated peatlands and biological N2 fixation likely supplies a significant but unknown fraction of N inputs. Moreover, environmental controls on diazotrophic community composition in N-limited peatlands are poorly constrained. Thus, improved understanding of feedbacks between the CH4 and N cycles is critical for predicting future changes to CH4 flux from peat bogs. We coupled measurements of N2 fixation activity measured by the acetylene (C2H2) reduction assay (ARA) with molecular analyses of expression and diversity of nifH genes encoding the molybdenum (Mo)-containing nitrogenase from two peat bogs in the Marcell Experimental Forest, Minnesota, USA. The top 10 cm of peat was sampled from the high CH4 flux S1 bog and the low CH4 flux Zim bog in April and June 2014. Despite similar N concentrations in the top 10 cm of both bogs (0.5-1.0 μM NO2-+NO3- and 2-3 μM NH4+), the S1 bog displayed variable ARA activity (1-100 nmol C2H4 h-1 g-1) whereas the Zim bog had consistently low ARA activity (Methylocella was the dominant diazotroph in the S1 bog based on high throughput next generation sequencing of nifH cDNA amplicons. Given previous reports of C2H2 inhibition of methanotrophy, we measured CH4 consumption in the presence or absence of 1% C2H2. Preliminary results suggest minimal effect of C2H2 on CH4 oxidation. Future measurements of 15N2 incorporation coupled to molecular analysis will elucidate whether methanotroph diazotrophy was suppressed by C2H2 in ARA incubations.

  16. Synanthropization of the Baltic-type raised bog “Roby” (NW Poland

    Directory of Open Access Journals (Sweden)

    Sotek Zofia

    2015-06-01

    Full Text Available Raised and transitional peat bogs, despite their considerable resistance to synanthropization, as a result of anthropogenic transformations are exposed to the colonisation by alien species. One of them is the peatland “Roby”, where, in the years 2007-2009 and 2014, floristic, phytosociological and soil studies were carried out in order to record the signs of ongoing synanthropization. Conducted observations and analyses indicated that the expansion of willows has taken place and at present they occupy a large part of the bog, encroaching into bog birch forest and successfully competing with Myrica gale. Progressive peat mineralisation and constructed surfaced roads within the bog, contributed to the appearance and wide distribution of synanthropic species, such as: Urtica dioica, Impatiens parviflora and Spiraea salicifolia. Raised bog communities and their characteristic species occur on a few fragments of the bog, in north-western part, where water regime is shaped mainly by precipitation and peat deposit is fairly well-preserved. At the same time, in the patches of these communities, a distinct unfavourable increase in the share of Molinia caerulea is observed.

  17. The hydrological and geochemical isolation of a freshwater bog within a saline fen in north-eastern Alberta

    Directory of Open Access Journals (Sweden)

    S.J. Scarlett

    2013-10-01

    Full Text Available In the oil sands development region near Fort McMurray, Alberta, wetlands cover ~62 % of the landscape, and ~95 % of these wetlands are peatlands. A saline fen was studied as a reference site for peatland reclamation. Despite highly saline conditions, a freshwater bog was observed in the path of local saline groundwater flow. The purpose of this study was to identify the hydrological controls that have allowed the development and persistence of a bog in this setting. The presence of bog vegetation and its dilute water chemistry suggest that saline groundwater from the fen rarely enters the bog, which functions predominantly as a groundwater recharge system. Chloride (Cl– and sodium (Na+ were the dominant ions in fen water, with concentrations averaging 5394 and 2307 mg L-1, respectively, while the concentrations in bog water were 5 and 4 mg L-1, respectively. These concentrations were reflected by salinity and electrical conductivity measurements, which in the fen averaged 9.3 ppt, and 15.8 mS cm-1, respectively, and in the bog averaged 0.1 ppt and 0.3 mS cm-1, respectively. A small ridge in the mineral substratum was found at the fen–bog margin, which created a persistent groundwater mound. Under the dry conditions experienced in early summer, groundwater flow was directed away from the bog at a rate of 14.6 mm day-1. The convex water table at the fen-bog margin impeded flow of saline water into the bog and instead directed it around the bog margin. However, the groundwater mound was eliminated during flooding in autumn, when the horizontal hydraulic gradient across the margin became negligible, suggesting the possibility of saline water ingress into the bog under these conditions.

  18. Regulation of nitrogen removal and retention in sphagnum bogs and other peatlands

    International Nuclear Information System (INIS)

    Damman, A.W.H.

    1988-01-01

    Nitrogen concentrations range from 0.3-l.3% in ombrotrophic peat of raised bogs. Within ombrogenous bogs, the N concentration of the peat increases in oceanic regions, with the highest concentrations found in blanket bogs on Southern Hemisphere islands. In minerotrophic peat, N concentrations increase with age (depth) as in upland humus. In this paper, I propose that N immobilization is truncated at low levels in ombrotrophic peat because 1) microbial activity is reduced well below that determined by environmental conditions, and 2) N is not limiting decay, in spite of low N concentrations. Consequently, net mineralization of N occurs at C:N quotients 80 to over 100 in inland raised bogs. Nutrient deficiency, probably P deficiency, appears to limit microbial activity and N immobilization. The increased N immobilization in oceanic bogs is attributed to higher Mg inputs that stimulate the biochemical release of P by enzymatic catalysis, and hence increase microbial activity. In ombrotrophi bogs, peat formed during periods of slow accumulation and long residence in the acrotelm has the highest N concentrations but, paradoxically, has also lost more of its original N content than peat that accumulated rapidly. Irregular changes in the anaerobic peat reflect conditions of decay when the peat was in the acrotelm. In a dated profile, N losses were largest during the last 2000 yr. This indicates a change in environmental conditions in the surface peat. Presumably, during this period the bog reached its maximum elevation with respect to the water mound that can be maintained in the peat under the present climatic conditions, and N losses increased as peat accumulation decreased. (author)

  19. Polyphenolic Compositions and Chromatic Characteristics of Bog Bilberry Syrup Wines

    Directory of Open Access Journals (Sweden)

    Shu-Xun Liu

    2015-11-01

    Full Text Available Phenolic compounds determine the color quality of fruit wines. In this study, the phenolic compound content and composition, color characteristics and changes during 6 months of bottle aging were studied in wines fermented with bog bilberry syrup under three different pHs. The total anthocyanins and total phenols were around 15.12–16.23 mg/L and 475.82 to 486.50 mg GAE/L in fresh wines and declined 22%–31% and about 11% in bottle aged wines, respectively. In fresh wines, eight anthocyanins, six phenolic aids and 14 flavonols, but no flavon-3-ols were identified; Malvidin-3-O-glucoside, petunidin-3-O-glucoside and delphinium-3-O-glucoside were the predominant pigments; Chlorogentic acid was the most abundant phenolic acid, and quercetin-3-O-galactoside and myricetin-3-O-galactoside accounted for nearly 90% of the total flavonols. During 6 months of bottle storage, the amounts of all the monomeric anthocyanins and phenolic acids were reduced dramatically, while the glycosidyl flavonols remained constant or were less reduced and their corresponding aglycones increased a lot. The effects of aging on blueberry wine color were described as the loss of color intensity with a dramatic change in color hue, from initial red-purple up to final red-brick nuances, while the pH of the fermentation matrix was negatively related to the color stability of aged wine.

  20. Peat Bogs as Hotspots for Organoarsenical Formation and Persistence.

    Science.gov (United States)

    Mikutta, Christian; Rothwell, James J

    2016-04-19

    Peatlands have received significant atmospheric inputs of As and S since the onset of the Industrial Revolution, but the effect of S deposition on the fate of As is largely unknown. It may encompass the formation of As sulfides and organosulfur-bound As, or the indirect stimulation of As biotransformation processes, which are presently not considered as important As immobilization pathways in wetlands. To investigate the immobilization mechanisms of anthropogenically derived As in peatlands subjected to long-term atmospheric pollution, we explored the solid-phase speciation of As, Fe, and S in English peat bogs by X-ray absorption spectroscopy. Additionally, we analyzed the speciation of As in pore- and streamwaters. Linear combination fits of extended X-ray absorption fine structure (EXAFS) data imply that 62-100% (average: 82%) of solid-phase As (Astot: 9-92 mg/kg) was present as organic As(V) and As(III). In agreement with appreciable concentrations of organoarsenicals in surface waters (pH: 4.0-4.4, Eh: 165-190 mV, average Astot: 1.5-129 μg/L), our findings reveal extensive biotransformation of atmospheric As and the enrichment of organoarsenicals in the peat, suggesting that the importance of organometal(loid)s in wetlands subjected to prolonged air pollution is higher than previously assumed.

  1. Genetic population structure of the vulnerable bog fritillary butterfly.

    Science.gov (United States)

    Vandewoestijne, S; Baguette, M

    2004-01-01

    Populations of the bog fritillary butterfly Proclossiana eunomia (Lepidoptera, Nymphalidae) occur in patchy habitat in central and western Europe. P. eunomia is a vulnerable species in the Belgian Ardennes and the number of occupied sites has significantly decreased in this region since the 1960s. RAPD (random amplified polymorphic DNA) markers were used to study the consequences of habitat loss and fragmentation on the genetic population structure of this species. Gene diversity was lower in populations with smaller population sizes. Genetic subdivision was high (Fst=0.0887) considering the small spatial scale of this study (150 km2). The most geographically isolated population was also the most genetically differentiated one. The genetic population structure and genetic differentiation detected in this study were explained by (1) differences in altitude of the sampled locations and, (2) lower dispersal propensity and dispersal rate in fragmented landscapes versus continuous landscapes. Results from the RAPD analyses were compared with a previous allozyme based study on the same populations. The results of this study suggest that increased fragmentation has lead to a greater genetic differentiation between remaining P. eunomia populations.

  2. CO2 and CH4 fluxes of contrasting pristine bogs in southern Patagonia (Tierra del Fuego, Argentina)

    Science.gov (United States)

    Münchberger, Wiebke; Blodau, Christian; Kleinebecker, Till; Pancotto, Veronica

    2015-04-01

    South Patagonian peatlands cover a wide range of the southern terrestrial area and thus are an important component of the terrestrial global carbon cycle. These extremely southern ecosystems have been accumulating organic material since the last glaciation up to now and are - in contrast to northern hemisphere bogs - virtually unaffected by human activities. So far, little attention has been given to these pristine ecosystems and great carbon reservoirs which will potentially be affected by climate change. We aim to fill the knowledge gap in the quantity of carbon released from these bogs and in what controls their fluxes. We study the temporal and spatial variability of carbon fluxes in two contrasting bog ecosystems in southern Patagonia, Tierra del Fuego. Sphagnum-dominated bog ecosystems in Tierra del Fuego are similar to the ones on the northern hemisphere, while cushion plant-dominated bogs can almost exclusively be found in southern Patagonia. These unique cushion plant-dominated bogs are found close to the coast and their occurrence changes gradually to Sphagnum-dominated bogs with increasing distance from the coast. We conduct closed chamber measurements and record relevant environmental variables for CO2 and CH4 fluxes during two austral vegetation periods from December to April. Chamber measurements are performed on microforms representing the main vegetation units of the studied bogs. Gas concentrations are measured with a fast analyzer (Los Gatos Ultraportable Greenhouse Gas Analyzer) allowing to accurately record CH4 fluxes in the ppm range. We present preliminary results of the carbon flux variability from south Patagonian peat bogs and give insights into their environmental controls. Carbon fluxes of these two bog types appear to be highly different. In contrast to Sphagnum-dominated bogs, cushion plant-dominated bogs release almost no CH4 while their CO2 flux in both, photosynthesis and respiration, can be twice as high as for Sphagnum

  3. Natural and artificial radionuclides in forest and bog soils: tracers for migration processes and soil development

    International Nuclear Information System (INIS)

    Schleich, N.; Degering, D.; Unterricker, S.

    2000-01-01

    Radionuclide distributions in undisturbed forest and bog soils, mostly situated in Saxony, Germany (Erzgebirge), were studied. Low concentrations of naturally-occurring U and Th decay series nuclides, including 210 Pb, and artificial radioisotopes ( 125 Sb, 134 Cs, 137 Cs, 241 Am) were determined using low-level γ-spectrometry. In addition, the activities of 238 Pu and 239,240 Pu were determined by radiochemical separation and α-spectrometry. 14 C and excess 210 Pb dating methods were used to date the sampled bog profiles. The different radionuclides show characteristic depth distributions in the forest and bog soil horizons, which were sub-sampled as thin slices. 125 Sb, 241 Am, 238 Pu and 239,240 Pu are strongly fixed in soil organic matter. In spruce forest soils, the influence of soil horizons with distinct properties dominates the vertical time-dependent distribution. In ombrotrophic bogs, the peak positions correlated with the year of maximum input of each nuclide. The Sb, Am and Pu ''time markers'' and the 14 C and 210 Pb dating results correspond very well. Although Cs seems to be relatively mobile in organic as well as mineral forest soil horizons, it is enriched in the organic material. In ombrotrophic bogs, Cs is very mobile in the peat deposit. In Sphagnum peat, Cs is translocated continuously towards the growing apices of the Sphagnum mosses, where it is accumulated. (orig.)

  4. Problem of a radiocapacity in a system soil-plant for bog ecosystem

    International Nuclear Information System (INIS)

    Kutlakhmedova-Vyshnyakova, V.

    1998-01-01

    The factors of the various components of a pasture bog ecosystem were evaluated on the example of the Volynsk area. Soil and water were found to contribute appreciably to the accumulation of radionuclides in plants in the bog ecosystem. Evaluation of the integral distribution of radionuclides ( 137 Cs) and the radiocapacity factors of the bog ecosystem components lead to F(soil) = 0.5, F(water) = 0.1, F(plants) = 0.25, and F(root) = 0.15. The radiocapacity factor determines the fraction of radionuclides from a general reserve concentrated in a particular component of the ecosystem. The higher values transfer factors of accumulation for plants in the bog ecosystem in comparison with terrestrial ecosystems (Tf 1.5-18) are noteworthy. Thus the contribution of soil to the formation Tf is from 60 % to 80 %, the remaining pathway in plants being from the water phase. This may be related with the high radiocapacity of soil in the bog ecosystem and (as a corollary) the rather small concentration of radionuclides in water in comparison with soil

  5. Some results on the isotope studies of water exchange in boreal raised bogs

    International Nuclear Information System (INIS)

    Sirin, A.A.; Vlasova, L.S.; Polyakov, V.A.; Trofimova, A.E.

    2002-01-01

    Raised bogs are rather common and one of the most exciting mire types of the boreal zone. They receive water and nutrients from precipitation and pore water stored in their domes (up to 10 m in height) is spaced above levels of regional ground water or streams draining them. Peatland hydrologists have long assumed that fluid flow occurs mainly in a peat layer near to the surface and water transport is negligible in deeper layers. The 'acrotelm/catotelm' paradigm on active and inert horizons for the peat above and below the lowest water level is still widely spread in peatland hydrology. However, recent studies have shown that deep water movement is much more dynamic in raised bogs than was previously thought. Based on geochemical studies and numerical simulations even temporal reverse of the vertical direction of water fluid flow through the peat as connected to climate fluctuations was assumed. Relying on isotope studies we consider only the mounded strata of the raised bogs to have relatively active water exchange. The study included two raised bogs, representing different local hydrological conditions (underlain by outwash sands and moraine clay) at the Zapadnaya Dvina Peatland Field Station of the Forest Research Institute located 400 km west of Moscow. Peatlands, among which raised bogs dominate, constitute >30% of the area, and maximum peat thickness exceeds 7 m

  6. Towards sustainable ecological networks of peat bogs in central Russia; development of local environmental action program (LEAP) as a practical tool for protection and restoration of peat bogs in Egorievsk sub region

    NARCIS (Netherlands)

    Butovsky, R.O.; Reijnen, R.; Bondartchuk, E.A.; Otchagov, D.M.; Melik-Bagdasarov, E.M.

    2001-01-01

    In central and northern Meshera the habitats for many characteristic peat bog species now show a very fragmented pattern. As a result, the potential for viable populations of characteristic peat bog species has decreased considerably. Peat-mining and other human influences are the most important

  7. The Sphagnum microbiome supports bog ecosystem functioning under extreme conditions.

    Science.gov (United States)

    Bragina, Anastasia; Oberauner-Wappis, Lisa; Zachow, Christin; Halwachs, Bettina; Thallinger, Gerhard G; Müller, Henry; Berg, Gabriele

    2014-09-01

    Sphagnum-dominated bogs represent a unique yet widely distributed type of terrestrial ecosystem and strongly contribute to global biosphere functioning. Sphagnum is colonized by highly diverse microbial communities, but less is known about their function. We identified a high functional diversity within the Sphagnum microbiome applying an Illumina-based metagenomic approach followed by de novo assembly and MG-RAST annotation. An interenvironmental comparison revealed that the Sphagnum microbiome harbours specific genetic features that distinguish it significantly from microbiomes of higher plants and peat soils. The differential traits especially support ecosystem functioning by a symbiotic lifestyle under poikilohydric and ombrotrophic conditions. To realise a plasticity-stability balance, we found abundant subsystems responsible to cope with oxidative and drought stresses, to exchange (mobile) genetic elements, and genes that encode for resistance to detrimental environmental factors, repair and self-controlling mechanisms. Multiple microbe-microbe and plant-microbe interactions were also found to play a crucial role as indicated by diverse genes necessary for biofilm formation, interaction via quorum sensing and nutrient exchange. A high proportion of genes involved in nitrogen cycle and recycling of organic material supported the role of bacteria for nutrient supply. 16S rDNA analysis indicated a higher structural diversity than that which had been previously detected using PCR-dependent techniques. Altogether, the diverse Sphagnum microbiome has the ability to support the life of the host plant and the entire ecosystem under changing environmental conditions. Beyond this, the moss microbiome presents a promising bio-resource for environmental biotechnology - with respect to novel enzymes or stress-protecting bacteria. © 2014 John Wiley & Sons Ltd.

  8. Prereservation of a rare bog pine genotypes using micropropagation techniques

    Directory of Open Access Journals (Sweden)

    Hana Vejsadová

    2008-01-01

    Full Text Available Bog pine (Pinus uncinata DC. subsp. uliginosa (Neumann Businský is a subendemic species and appears to be one of the most endangered tree species of the Czech Republic. Its rare populations are at the present time greatly endangered namely by spontaneous hybridization with the Scots pine (Pinus sylvestris L.. Regarding the fact that its protection is insufficient even in national nature reserves (NNR and the classical propagation by cuttings is problematic, modern methods were adopted for a long-term preservation of the taxon. Growth regulation conditions were investigated for the induction of organogenesis and somatic embryogenesis. Mature seeds were obtained from selected trees in the Žofinka NNR and from a locality near the village of Krajková in the Sokolov district. Cotyledon and hypocotyl segments from seedlings pregerminated in sterile conditions were used to induce the organogenesis. Bud proliferation was observed on the cotyledons after 4 weeks. The largest amount of buds was found on the medium with 1.5 mg . l−1 benzyladenine (BA and 0.5 mg . l−1 1-naphtylacetic acid (NAA after 12 weeks. The hypocotyl segments showed only the formation of green callus. Isolated mature zygotic embryos were used for the induction of somatic embryogenesis. Development of mucilaginous callus was recorded after 3 weeks of cultivation on media with different combinations of BA, NAA and 2,4-dichlorophenoxy acetic acid (2,4-D concentrations. When the callus induced on the medium with the combination of 0.56 (1.13 mg . l−1 BA and 1.86 mg.l−1 NAA was transferred on the medium with lower BA (0.113 mg . l−1 and 2,4-D (0.44 mg.l−1 concentrations, the first somatic embryos started to emerge after a period of other two weeks.

  9. Antonio Beccadellis bog om kong Alfonso I af Napoli (1455) og reformationskongen Christian III af Danmark-Norge (1550)

    DEFF Research Database (Denmark)

    Lausten, Martin Schwarz

    2016-01-01

    Præsentation af Beccadellis bog (1455) og redegørelse for, hvorledes den ukendte Erhard efter tilskyndelse fra Melanchthon kunne tilegne denne katolske humanistiske bog, ændret i lettere grad, til den lutherske konge Christian III (1550)....

  10. Dicranochaete quadriseta (Korš. Nov. and Pop. from an oligominerotrophic peat bog in Lower Silesia (South-Western Poland

    Directory of Open Access Journals (Sweden)

    Jan Matuła

    2011-01-01

    Full Text Available Dicranochaete quadriseta (Korš. Nov. and Pop. was collected during investigations of algae from mountain peat bogs of the Sudeten Mts (Poland. The paper describes the morphology, taxanomy, geographical distribution and ecological conditions of this species. This very rare species was found in an oligominerotrophic peat bog called "Topieliska-Zieleniec" near Duszniki (Orlickie Mts.

  11. Distribution of 35 Elements in Peat Cores from Ombrotrophic Bogs Studied by Epithermal Neutron Activation Analysis

    CERN Document Server

    Frontasyeva, M V

    2004-01-01

    In ombrotrophic bogs the surface peat layer is supplied with chemical substances only from the atmosphere. Peat cores from these bogs therefore can be used to study temporal trends in atmospheric deposition of pollutants. In this work epithermal neutron activation analysis was applied for the first time to study the distribution of 35 elements in peat profiles from ombrotrophic bogs. The selected examples were from Finnmark county in northern Norway: one pristine site far from any local pollution source, and another strongly affected by long-term operation of Russian copper-nickel smelters located close to the border. The elements are classified with respect to their behavior in the uppermost 40 cm of the peat, and similarities and differences between the two profiles are discussed. As compared with other more commonly used analytical techniques based on acid decomposition of the sample ENAA has the advantage of providing the total concentrations of the elements.

  12. North-West European bogs show that Little Ice Age climate changes may have been driven by changes in solar activity

    NARCIS (Netherlands)

    Mauquoy, D.; Geel, van B.; Blaauw, M.; Plicht, van der J.; Berendse, F.

    2001-01-01

    Bog mosses (Sphagnum species) are sensitive to the position of local water-tables on intact raised peat bogs. These peat bogs are rain-fed, receiving all their water through precipitation alone. After death, the mosses are remarkably well preserved, since they are resistant to decay, and

  13. Habitat and species controls on Sphagnum production and decomposition in a mountain raised bog

    Czech Academy of Sciences Publication Activity Database

    Hájek, Tomáš

    2009-01-01

    Roč. 14, č. 6 (2009), s. 947-958 ISSN 1239-6095 R&D Projects: GA AV ČR KJB600050503 Institutional research plan: CEZ:AV0Z60050516 Keywords : bog * production * decomposition Subject RIV: EF - Botanics Impact factor: 1.467, year: 2009

  14. How Phosphorus Availability Affects the Impact of Nitrogen Deposition on Sphagnum and Vascular Plants in Bogs

    NARCIS (Netherlands)

    Limpens, J.; Berendse, F.; Klees, H.

    2004-01-01

    To elucidate the impact of high nitrogen (N) deposition on intact bog vegetation, as affected by phosphorus (P) availability, we conducted a 4-year fertilization experiment with N and P at six sites, one with moderate N deposition and five with high N deposition. During the growing season, N (40 kg

  15. Iodine dispersion and effects on groundwater chemistry following a release to a peat bog, Manitoba, Canada

    International Nuclear Information System (INIS)

    Sheppard, M.I.; Thibault, D.H.; Smith, P.A.

    1989-01-01

    The migration and behaviour of I was investigated in a sphagnum bog on the precambrian Shield in eastern Manitoba, Canada. A 6 M solution of K1 was released at the base of the bog to simulate a pulse discharge of contaminated groundwater from a fracture in the granitic rock. A network of piezometer tubes was used to monitor the dispersion of the I and the groundwater chemistry over 1 year. Cores of peat were also taken for analysis to supplement the groundwater data and to investigate the sorption of I. The introduced I dispersed 2 m horizontally and 1 m vertically within a month. After this, the system stabilized and further migration was insignificant. The pattern of I dispersion indicated that the bog hydrology was very complex with flow directions changing substantially with depth. The groundwater concentrations of the major cations rose in response to the mass action effect of K displacing them from reaction sites in the peat. Humic materials in the groundwater decreased in size after the KI release and returned to their pre-release conformation one month later. The geometric mean soil distribution coefficient value, K d , for I in the bog was 1.361/kg, but it was strongly related to pore water concentration. Thus, a single K d value was insufficient for describing the system. (author)

  16. A geospatial model to quantify mean thickness of peat in cranberry bogs

    Science.gov (United States)

    Commercial cranberry (Vaccinium macrocarpon Ait.) is cultivated on peatlands, which consist of sedimentary deposits of peat capped by a 0.3-1 m of artificial sand. Despite distinct soil layering, a general paucity of information exists on the physical properties of cranberry bogs. Field measurement...

  17. Potassium limits potential growth of bog vegetation under elevated atmospheric CO2 and N deposition

    NARCIS (Netherlands)

    Hoosbeek, M.R.; Breemen, van N.; Vasander, H.; Buttlers, A.; Berendse, F.

    2002-01-01

    The free air carbon dioxide enrichment (FACE) and N deposition experiments on four ombrotrophic bogs in Finland, Sweden, the Netherlands and Switzerland, revealed that after three years of treatment: (1) elevated atmospheric CO2 concentration had no significant effect on the biomass growth of

  18. Ecology of southeastern shrub bogs (pocosins) and Carolina bays: a community profile

    Energy Technology Data Exchange (ETDEWEB)

    Sharitz, R.R.; Gibbons, J.W.

    1982-11-01

    Shrub bogs of the Southeast occur in areas of poorly developed internal drainage that typically but not always have highly developed organic or peat soils. Pocosins and Carolina bays are types or subclasses of shrub bogs on the coastal plains of the Carolinas and Georgia. They share roughly the same distribution patterns, soil types, floral and faunal species composition and other community attributes, but differ in geological formation. Carolina bays may contain pocosin as well as other communities, but are defined more by their unique elliptical shape and geomorphometry. The pocosin community is largely defined by its vegetation, a combination of a dense shrub understory and a sparser canopy. The community is part of a complex successional sequence of communities (sedge bogs, savannas, cedar bogs, and bay forests) that may be controlled by such factors as fire, hydroperiod, soil type, and peat depth. Pocosins and Carolina bays harbor a number of animal groups and may be locally important in their ecology. Although few species are endemic to these habitats, they may provide important refuges for a number of species. These communities are simultaneously among the least understood and most rapidly disappearing habitats of the Southeast. Forestry and agricultural clearage are current impacts.

  19. Dibasic Ammonium Phosphate Application Enhances Aromatic Compound Concentration in Bog Bilberry Syrup Wine.

    Science.gov (United States)

    Wang, Shao-Yang; Li, Yi-Qing; Li, Teng; Yang, Hang-Yu; Ren, Jie; Zhang, Bo-Lin; Zhu, Bao-Qing

    2016-12-29

    A nitrogen deficiency always causes bog bilberry syrup wine to have a poor sensory feature. This study investigated the effect of nitrogen source addition on volatile compounds during bog bilberry syrup wine fermentation. The syrup was supplemented with 60, 90, 120 or 150 mg/L dibasic ammonium phosphate (DAP) before fermentation. Results showed that an increase of DAP amounts accelerated fermentation rate, increased alcohol content, and decreased sugar level. Total phenol and total flavonoid content were also enhanced with the increase of DAP amounts. A total of 91 volatile compounds were detected in the wine and their concentrations were significantly enhanced with the increase of DAP. Ethyl acetate, isoamyl acetate, phenethyl acetate, ethyl butanoate, ethyl hexanoate, ethyl octanoate, ethyl decanoate, isobutanol, isoamyl alcohol, levo -2,3-butanediol, 2-phenylethanol, meso -2,3-butanediol, isobutyric acid, hexanoic acid, and octanoic acid exhibited a significant increase of their odor activity value (OAV) with the increase of DAP amounts. Bog bilberry syrup wine possessed fruity, fatty, and caramel flavors as its major aroma, whereas a balsamic note was the least present. The increase of DAP amounts significantly improved the global aroma attributes, thereby indicating that DAP supplementation could promote wine fermentation performance and enhance the sensory quality of bog bilberry syrup wine.

  20. Anmeldelse af Masood Fouroozandeh og Marianne Søndergaards bog om moskeernes mange ansigter

    DEFF Research Database (Denmark)

    Skovsgaard, Steen

    2016-01-01

    Massoud Fouroozandeh har sammen med Marianne Sønderskov skrevet en bog: ”Moskeernes mange ansigter”. Det er en bog, som er svær at komme udenom eller lægge fra sig. En frygtløs bog, som alligevel er fyldt med frygt og mange advarsler. Her advares imod islam, som vil erobre Vesten, og moskeerne, som...... for. Én, som kender islam, og én som kan forkynde evangeliet klart og forståeligt for muslimer. Og så vidt jeg har oplevet og hørt om det, så går det også rigtig godt med missionen og med menigheden: ”Church of Love”. Her samles mange muslimer, som er konverteret, til gudstjenester og undervisning i...... en levende menighed. Efter at have læst bogen: ”Moskeernes mange ansigter” sidder jeg alligevel tilbage med en følelse af, at der mangler noget. For det, som denne bog fortæller, er jo ikke nyt. Afdøde sognepræst Rolf Sloth-Henriksen skrev f.eks. allerede i 2001 bogen: ”Hellig Krig – Terror eller...

  1. Anmeldelse: Peter Gøtzsches nye bog: Big pharma = Big crime?

    DEFF Research Database (Denmark)

    Møller, Marianne

    2013-01-01

    Cochrane-lægen Peter Gøtzsche har udgivet en bog med stærk kritik af medicinalindustrien og systemet for godkendelse og kontrol af medicin. Bogen er ladet med eksempler fra mange terapeutiske områder og er - med sin usædvanligt hårde retorik - en oplagt debatskaber....

  2. Isolated peat bog habitats and their food connections: parasitoids (Hymenoptera: Ichneumonoidea) and their lepidopteran hosts

    Czech Academy of Sciences Publication Activity Database

    Lozan, Aurel; Spitzer, Karel; Jaroš, Josef

    2012-01-01

    Roč. 16, č. 3 (2012), s. 391-397 ISSN 1366-638X Institutional research plan: CEZ:AV0Z50070508 Keywords : Paleorefugia * relict peat bogs * specific Lepidoptera Subject RIV: EH - Ecology, Behaviour Impact factor: 1.801, year: 2012 http://www.springerlink.com/content/78u173hn60701033/

  3. Indicative effects of climate change on groundwater levels in Estonian raised bogs over 50 years

    Directory of Open Access Journals (Sweden)

    E. Lode

    2017-08-01

    Full Text Available Analyses of 50-year (1962–2011 monthly air temperature and precipitation data indicated substantial climate change in the locations of two raised bogs (Linnusaare and Männikjärve in central-east Estonia. During recent years the cross-year winter air temperature increased by 1.7 ºC, while the cold-season precipitation increased by 4 mm. The fluctuation amplitude of temperature and precipitation values decreased. Snow depth proved to be the most sensitive variable to winter warming, followed by groundwater levels together with mean and maximum soil frosts. Long-term groundwater levels on the domes of the bogs and in the forested/treed lagg areas were 0.3−0.4 m and 0.4−0.8 m below the soil surface, respectively. Warming caused changes in groundwater level amplitude of 3−22 cm in the bog domes and 3−14 cm in the forested lagg zones. The lowest groundwater levels in ridge-pool ecotopes at Männikjärve rose by 6−10 cm (i.e. these ecotopes became wetter; but the incidence of low groundwater levels increased in most ecotopes, indicating a more general trend towards drier conditions in the bog.

  4. Tracing decadal environmental change in ombrotrophic bogs using diatoms from herbarium collections and transfer functions

    International Nuclear Information System (INIS)

    Poulíčková, Aloisie; Hájková, Petra; Kintrová, Kateřina; Bat'ková, Romana; Czudková, Markéta; Hájek, Michal

    2013-01-01

    Central European mountain bogs, among the most valuable and threatened of habitats, were exposed to intensive human impact during the 20th century. We reconstructed the subrecent water chemistry and water-table depths using diatom based transfer functions calibrated from modern sampling. Herbarium Sphagnum specimens collected during the period 1918–1998 were used as a source of historic diatom samples. We classified samples into hummocks and hollows according to the identity of dominant Sphagnum species, to reduce bias caused by uneven sampling of particular microhabitats. Our results provide clear evidence for bog pollution by grazing during the period 1918–1947 and by undocumented aerial liming in the early 90-ies. We advocate use of herbarized epibryon as a source of information on subrecent conditions in recently polluted mires. -- Highlights: •We reconstruct the subrecent ecological variables using transfer functions. •Calibration was based on long-term averages and modern diatom sampling. •Herbarized bryophytes were used as a source of historic diatom samples. •Bogs were influenced by grazing in the period 1918–1947. •We provide clear evidence of bog pollution by aerial liming in early 90-ies. -- We provide clear evidence that the recent pH/calcium gradient appeared ca 20 years ago owing to aerial liming of forests

  5. Hvordan jøderne blev til jøder i Esters bog

    DEFF Research Database (Denmark)

    Holt, Else Kragelund

    2015-01-01

    persere, der ikke ”bliver jøder”. Denne kamp tolkes som udtryk dels for en fællesskabsskabende effervescens (Durkheim), der bedst forstås gennem Purimfestens karnevaleske karakter, dels for mimetisk rivalisering (Girard), personificeret gennem Haman og Mordokaj. Purim og Esters Bog står således i en...

  6. Some Late-Holocene pollen diagrams from the Peel raised bogs (Southern Netherlands)

    NARCIS (Netherlands)

    Janssen, C.R.; Hove, ten H.A.

    1971-01-01

    Three pollen diagrams from the Peel peatlands, a raised bog area in the southern part of The Netherlands reveal the post-Boreal vegetation history of that region. There are two or three land-occupation phases in the Neolithic and Bronze ages, that show but low values of terrestrial herbs. They are

  7. Effects of climate change and human activities on a Swedish raised bog

    NARCIS (Netherlands)

    van der Linden, M.

    2005-01-01

    We determined the effects of climate change and human activities on the species composition of ombrotrophic (rain-fed) peat bogs by analyzing pollen and macrofossils. We used 14C AMS wiggle-match dating (1) to obtain a precise chronology. Thermophilous plant species in the microfossil record provide

  8. Expansion of invasive species on ombrotrophic bogs: desiccation or high N deposition?

    NARCIS (Netherlands)

    Tomassen, H.B.M.; Smolders, A.J.P.; Limpens, J.; Lamers, L.P.M.; Roelofs, J.G.M.

    2004-01-01

    1. In many ombrotrophic bog areas the invasion of grass (e.g. Molinia caerulea) and tree (e.g. Betula pubescens) species has become a major problem. We investigated whether the invasion of such species is due to high atmospheric nitrogen (N) deposition by conducting a fertilization experiment. 2.

  9. Tracing decadal environmental change in ombrotrophic bogs using diatoms from herbarium collections and transfer functions

    Czech Academy of Sciences Publication Activity Database

    Poulíčková, A.; Hájková, Petra; Kintrová, K.; Baťková, R.; Czudková, M.; Hájek, Michal

    2013-01-01

    Roč. 179, August (2013), s. 201-209 ISSN 0269-7491 R&D Projects: GA ČR GA206/08/0389 Institutional support: RVO:67985939 Keywords : epibyon * diatoms * bogs Subject RIV: EF - Botanics Impact factor: 3.902, year: 2013

  10. A single well pumping and recovery test to measure in situ acrotelm transmissivity in raised bogs

    NARCIS (Netherlands)

    Schaaf, van der S.

    2004-01-01

    A quasi-steady-state single pit pumping and recovery test to measure in situ the transmissivity of the highly permeable upper layer of raised bogs, the acrotelm, is described and discussed. The basic concept is the expanding depression cone during both pumping and recovery. It is shown that applying

  11. Southern Hemisphere bog persists as a strong carbon sink during droughts

    Science.gov (United States)

    Goodrich, Jordan P.; Campbell, David I.; Schipper, Louis A.

    2017-10-01

    Peatland ecosystems have been important global carbon sinks throughout the Holocene. Most of the research on peatland carbon budgets and effects of variable weather conditions has been done in Northern Hemisphere Sphagnum-dominated systems. Given their importance in other geographic and climatic regions, a better understanding of peatland carbon dynamics is needed across the spectrum of global peatland types. In New Zealand, much of the historic peatland area has been drained for agriculture but little is known about rates of carbon exchange and storage in unaltered peatland remnants that are dominated by the jointed wire rush, Empodisma robustum. We used eddy covariance to measure ecosystem-scale CO2 and CH4 fluxes and a water balance approach to estimate the sub-surface flux of dissolved organic carbon from the largest remaining raised peat bog in New Zealand, Kopuatai bog. The net ecosystem carbon balance (NECB) was estimated over four years, which included two drought summers, a relatively wet summer, and a meteorologically average summer. In all measurement years, the bog was a substantial sink for carbon, ranging from 134.7 to 216.9 gC m-2 yr-1, owing to the large annual net ecosystem production (161.8 to 244.9 gCO2-C m-2 yr-1). Annual methane fluxes were large relative to most Northern Hemisphere peatlands (14.2 to 21.9 gCH4-C m-2 yr-1), although summer and autumn emissions were highly sensitive to dry conditions, leading to very predictable seasonality according to water table position. The annual flux of dissolved organic carbon was similar in magnitude to methane emissions but less variable, ranging from 11.7 to 12.8 gC m-2 yr-1. Dry conditions experienced during late summer droughts led to significant reductions in annual carbon storage, which resulted nearly equally from enhanced ecosystem respiration due to lowered water tables and increased temperatures, and from reduced gross primary production due to vapor pressure deficit-related stresses to the

  12. Decadal changes in peat carbon accrual rates in bogs in Northern Minnesota

    Science.gov (United States)

    Fissore, C.; Nater, E. A.; McFarlane, K. J.

    2017-12-01

    Throughout the Holocene, peatland ecosystems have accumulated substantial amounts of carbon (C) and currently store about one third of all soil organic carbon (SOC) worldwide. Large uncertainty still persists on whether peatland ecosystems located in northern latitudes will continue to act as C sinks, or if the effects of global warming will have greater effects on decomposition processes than on net ecosystem production. We investigated decadal C accrual rates of the top 25 cm of peats in three Sphagnum-rich peatlands located in Northern Minnesota (two ombrotrophic bogs and one fen). We used radiocarbon analysis of Sphagnum cellulose and model fitting to determine peat ages, and peat FTIR spectroscopy to determine humification indices and relative decomposition of peat samples with depth. We had the scope to detect whether recent warming has had an effect on peat decomposition and C accumulation rates. Modeled C accumulation rates in the three peatlands during the past five decades ranged between 78 and 107 g C m-2 yr-1 in the top 25 cm analyzed in this study, values that are higher than the 22 to 29 g C m-2 yr-1 obtained for long-term (millennial) accumulations for the entire bog profiles. Peat IR spectra and C:N ratios confirm low levels of decomposition across the bog sites, especially in the uppermost parts of the peat. The fen site showed very limited decomposition across the entire sampled profile. Higher rates of C accumulation, combined with low decomposition rates close to the surface provide a good estimate of net primary productivity. As substrate decomposition progresses over time, net rates of accumulation decrease. Peat decomposition was more pronounced in the lower depths of the sampled cores in the two ombrotrophic bogs than in the fen, likely an effect of larger temporal variation in water table depth in the bogs than in the fen. Some of the variation in C accumulation and decomposition observed in our bogs and fen suggests that future C

  13. Genesis of Spodic Material underneath Peat Bogs in a Danish Wetland

    DEFF Research Database (Denmark)

    Kristiansen, Søren Munch; Dalsgaard, Kristian; Thomsen, Ingrid Kaag

    2010-01-01

    features, were exclusively found in sandy material at the margins of or underneath sphagnum peat bogs, whereas Inceptisols were found on well-drained sandy deposits only. Aluminum content was very high and Fe low in spodic materials with ortstein properties. Solid-state 13C nuclear magnetic resonance (NMR......) spectra of wet sandy 2Bs horizons were dominated by alkyl C (70%) from water-insoluble OM and were clearly distinct from NMR spectra of overlying 2Bhsm material. Pollen analysis revealed that an open forest with a thick mor layer dominated until shortly after 5000 yr BP, when sphagnum was first recorded....... Radiocarbon ages of bulk soil C in the spodic horizons had mean residence times of 4500 to 4400 yr. Accordingly, the spodic B horizon was probably formed by strong in situ illuviation of Al-OM complexes before the sphagnum peat bog formation. This suggests that spodic material formation and thus strong C...

  14. Towards the identification of dyestuffs in Early Iron Age Scandinavian peat bog textiles

    DEFF Research Database (Denmark)

    Mannering, Ulla; Gleba, Margarita; Vanden Berghe, Ina

    2009-01-01

    A large systematic dye investigation of prehistoric Danish and Norwegian bog textiles was carried out using high performance liquid chromatography with photo diode array detection. After the selection of the most suitable protocol for dye extraction and HPLC analysis for this specific group...... of archaeological samples, the second part included the characterisation of the dyes detected in the whole series of the Early Iron Age textiles and the interpretation of the dyeing technology. Natural organic dyes were found from the three main categories of natural dyes, hence throwing new light on the use...... of biological dye sources in Early Iron Age Scandinavia. The results clearly indicate that most Scandinavian peat bog textiles originally were dyed and that already during the 1st millennium BC, the populations in Scandinavia were familiar with the dyeing technology....

  15. Blanket bog in Newfoundland. Part 1. The occurrence and accumulation of fog-water deposits

    Science.gov (United States)

    Price, Jonathan S.

    1992-07-01

    Fog deposition on to a blanket bog near Cape Race, Newfoundland, was measured with a fog collector and a lysimeter. Fog is most frequently produced by warm southwesterly air flow over cold offshore water, although cooler northeasterly air is also important. Between 21 June and 14 July 1989 fog deposition was 50% of rainfall, averaging 1.8 mm day -1, with a maximum daily deposition of 10.2 mm. Evaporation was also restricted during fog and rain events; evaporation on days with fog or rain averaged <1.1 mm, compared with 2.5 mm when it was not foggy or raining. The addition of water to the surface by fog, combined with low evaporation rates may be critical to the development of blanket bog in this area.

  16. Late Holocene palaeohydrological changes in a Sphagnum peat bog from NW Romania based on testate amoebae

    Directory of Open Access Journals (Sweden)

    Andrei-Cosmin Diaconu

    2016-04-01

    Full Text Available This paper investigates the possibility of reconstructing the palaeohydrological changes in an active Sphagnum peat bog from north-western Romania using testate amoebae fauna and organic matter content determined by loss on ignition (LOI. In total 28 taxa of testate amoebae were identified of which 11 were frequent enough to present a remarkable ecological significance. Based on the relative abundance of these taxa nine zones were identified, crossing from very wet to dry climate conditions. The wet periods identified are characterized by taxa like Centropyxis cassis, Amphitrema flavum and Hyalosphenia papilio, while in the dry periods Difflugia pulex and Nebela militaris thrive. We showed that combining qualitative information regarding hydrological preferences with the quantitative percentage data from the fossil record it is possible to obtain information regarding major surface moisture changes from the peat bog surface. Furthermore we identified a link between distribution of testate amoebae assemblages, organic matter variation and minerogenic material.

  17. Diet of Tollund Man. Stable isotope analyses of an Iron Age bog body from Denmark

    DEFF Research Database (Denmark)

    Helt Nielsen, Nina; Philippsen, Bente; Jensen, L. V.

    Tollund Man is one of the world’s most famous bog bodies due to his exceptionally well-preserved head. He was found in 1950 by peat cutters in a bog near Bjældskovdal, c. 10 km west of Silkeborg. During the years, several analyses have been performed on the body to shed light on the life and death...... of Tollund Man. The investigations have primarily included forensic and medical examinations, X-rays, CT-scans and microscopical analyses of e.g. the stomach content, while chemical and isotope analyses have not been conducted. In 2016, an extraordinary grant from the municipality of Silkeborg enabled Museum...... Silkeborg to initiate a range of new scientific investigations of Tollund Man and the associated finds. These include protein analysis, multi-element analysis, Sr isotope analysis and analysis of the stable isotopes of N, C and S. This presentation focuses on measurements of the stable isotopes in bone...

  18. Tracing decadal environmental change in ombrotrophic bogs using diatoms from herbarium collections and transfer functions.

    Science.gov (United States)

    Poulíčková, Aloisie; Hájková, Petra; Kintrová, Kateřina; Bat'ková, Romana; Czudková, Markéta; Hájek, Michal

    2013-08-01

    Central European mountain bogs, among the most valuable and threatened of habitats, were exposed to intensive human impact during the 20th century. We reconstructed the subrecent water chemistry and water-table depths using diatom based transfer functions calibrated from modern sampling. Herbarium Sphagnum specimens collected during the period 1918-1998 were used as a source of historic diatom samples. We classified samples into hummocks and hollows according to the identity of dominant Sphagnum species, to reduce bias caused by uneven sampling of particular microhabitats. Our results provide clear evidence for bog pollution by grazing during the period 1918-1947 and by undocumented aerial liming in the early 90-ies. We advocate use of herbarized epibryon as a source of information on subrecent conditions in recently polluted mires. Copyright © 2013 Elsevier Ltd. All rights reserved.

  19. Ground-penetrating radar study of the Rahivere peat bog, eastern Estonia

    Directory of Open Access Journals (Sweden)

    Jüri Plado

    2011-03-01

    Full Text Available The current case study presents results of the ground-penetrating radar (GPR profiling at one of the Saadjärve drumlin field interstitial troughs, the Rahivere bog, eastern Estonia. The study was conducted in order to identify the bog morphology, and the thickness and geometry of the peat body. The method was also used to describe the applicability of GPR in the evaluation of the peat deposit reserve as the Rahivere bog belongs among the officially registered peat reserves. Fourteen GPR profiles, ~ 100 m apart and oriented perpendicular to the long axis of the depression, covering the bog and its surrounding areas, were acquired. In order to verify the radar image interpretation as well as to evaluate the velocity of electromagnetic waves in peat, a common source configuration was utilized and thirteen boreholes were drilled on the GPR profiles. A mean value of 0.036 m ns–1 corresponding to relative dielectric permittivity of 69.7 was used for the time–depth conversion. Radar images reveal major reflection from the peat–soil interface up to a depth of about 4 m, whereas drillings showed a maximum thickness of 4.5 m of peat. Minor reflections appear from the upper peat and mineral soil. According to the borehole data, undecomposed peat is underlain by decomposed one, but identifying them by GPR is complicated. Mineral soil consists of glaciolimnic silty sand in the peripheral areas of the trough, overlain by limnic clay in the central part. The calculated peat volumes (1 200 000 m3 were found to exceed the earlier estimation (979 000 m3 that was based solely on drilling data. Ground-penetrating radar, as a method that allows mapping horizontal continuity of the sub-peat interface in a non-destructive way, was found to provide detailed information for evaluating peat depth and extent.

  20. Archaeological science and object biography:a Roman bronze lamp from Kavastu bog (Estonia)

    OpenAIRE

    Oras, Ester; Higham, Thomas; Cramp, Lucy; Bull, Ian

    2017-01-01

    Objects imported over long distances often have rich biographies, not least a collection of bronze objects found in a peat bog in Estonia that included an elaborate lamp of Roman origin. Combining new scientific approaches with earlier observations and traditional archaeological analysis, the authors reconstruct the provenance, possible itinerary and changing use of the lamp over half a millennium, and across thousands of kilometres. They highlight its variable roles, from luxurious illuminat...

  1. Contributions to the knowledge of flora and vegetation of peat bog from Bihorului Mountains (NW Romania

    Directory of Open Access Journals (Sweden)

    Petru BURESCU

    2010-11-01

    Full Text Available The oligotrophic peat bog of Bihorului Mountains are quartered in the valleys with northern exposure, of siliceous substrate, forming habitats with high conservation value, which are home to over 10 rare relict species. The phytocoenoses of the associations Sphagnetum magellanici, Sphagno cuspidati – Rhynchosporetum albae, Caricetum limosae were analyzed by us in terms of floristic composition, ecological spectra of the type of life forms and floristic elements, in terms of chart ecological factors: moisture, soil temperature and chemical reaction.

  2. Hydrologic cycling of mercury and organic carbon in a forested upland-bog watershed

    Science.gov (United States)

    R. K. Kolka; D. F. Grigal; E. A. Nater; E. S. Verry

    2001-01-01

    The hydrologic cyvling of total Hg (HgT) and organic C (OC) was studies for a 1-yr period in a northern Minnesota forested watershed, consisting of an upland surrounding a bog peatland with a narrow lagg at their interface. Throughfall and sternflow contributed twice as much HgT as seven times as much OC to the forested watershed than atmospheric deposition in a...

  3. Sensitivity of carbon gas fluxes to weather variability on pristine, drained and rewetted temperate bogs

    Directory of Open Access Journals (Sweden)

    Z. Urbanová

    2013-05-01

    Full Text Available Climate change is considered to alter the functioning of boreal peatland ecosystems, but the vulnerability of pristine, rewetted and drained peatlands to climate change in temperate regions is unknown. We measured carbon (C gas exchange during wet (2009 and dry (2010 growing periods in pristine, drained and rewetted sites in mountain bogs in the Bohemian Forest (Czech Republic. Wetter lawns with sedges and drier habitats dominated by ericaceous shrubs were distinguished and studied at each site. Methane (CH4 emissions, which decreased in the order pristine > rewetted > drained, were generally lower during the 2010 growing period than in 2009 as a consequence of a drought. During the drought in 2010, photosynthesis (PG in the drier habitats with shrub vegetation increased on pristine and rewetted sites, while total respiration (RECO remained the same. Communities dominated by sedges maintained similar rates of PG and RECO during both growing periods. Generally, this led to higher C accumulation during the drought on pristine and rewetted bogs. At the drained bog site, the decreased water table (WT during the drought led to increased PG and RECO, such that the net C accumulation was similar in the two years. Drained peatlands may be more threatened by future climate change than pristine or rewetted peatlands because of their limited buffering capacity for decreased WT. In the case of further decreases in WT, they could lose the peatland vegetation and functions that have partly persisted through decades of drainage.

  4. Numerical simulation and experimental investigation on suction heating of a BOG compressor

    International Nuclear Information System (INIS)

    Jia, Xiaohan; Zhao, Bin; Feng, Jianmei; Zheng, Sulu; Peng, Xueyuan

    2016-01-01

    Highlights: • An investigation focusing on suction heating of a BOG compressor is carried out. • There is frost on the cylinder cover as the compressor at lower suction temperature. • The suction and discharge flow rate decrease with rising suction temperature. • The volumetric efficiency has a maximum value with increasing suction temperature. • The temperature coefficient increased with suction temperature or rotational speed. - Abstract: One of the key components of a liquefied natural gas (LNG) receiving terminal is the boil-off gas (BOG) compressor, which is used to pump out the BOG from the LNG storage tank to ensure safety in the transportation and receiving systems. Owing to the ultra-low suction temperature, the heat exchange between the intake gas and the cylinder, piston, and cylinder cover cannot be ignored as in normal conditions. This paper presents an investigation focusing on suction heating of the BOG compressor. A finite element model with dynamic mesh was established to simulate the suction process. At the same time, a performance test rig was built to study the characteristics of the BOG compressor under low suction temperature conditions and verify the numerical model. Consequently, the results of the simulation were in good agreement with experimental results. Both results implied that the temperature of cylinder surface increased starting from the cylinder cover to the crankcase. In addition, at lower suction temperature, the temperature difference between various points on the cylinder surface and cylinder cover was much larger than that at higher suction temperature. With increasing suction temperature, the temperature coefficient increased markedly, and the difference between gas temperatures at the beginning and end of the suction process, as well as the compressor flow rate, decreased significantly; however, the volumetric efficiency increased first and then decreased. Furthermore, the temperature coefficient clearly increased

  5. The new European Competence Centre for Moor and Climate - A European initiative for practical peat bog and climate protection

    Science.gov (United States)

    Smidt, Geerd; Tänzer, Detlef

    2013-04-01

    The new European Competence Centre for Moor and Climate (EFMK) is an initiative by different local communities, environmental protection NGOs, agricultural services, and partners from the peat and other industries in Lower Saxony (Germany). The Centre aims to integrate practical peat bog conservation with a focus on green house gas emission after drainage and after water logging activities. Together with our partners we want to break new ground to protect the remaining bogs in the region. Sphagnum mosses will be produced in paludiculture on-site in cooperation with the local peat industry to provide economic and ecologic alternatives for peat products used in horticulture business. Land-use changes are needed in the region and will be stimulated in cooperation with agricultural services via compensation money transfers from environmental protection funds. On a global scale the ideas of Carbon Credit System have to be discussed to protect the peat bogs for climate protection issues. Environmental education is an important pillar of the EFMK. The local society is invited to explore the unique ecosystem and to participate in peat bog protection activities. Future generations will be taught to understand that the health of our peat bogs is interrelated with the health of the local and global climate. Besides extracurricular classes for schools the centre will provide infrastructure for Master and PhD students, as well for senior researchers for applied research in the surrounding moor. International partners in the scientific and practical fields of peat bog ecology, renaturation, green house gas emissions from peat bogs, and environmental policy are invited to participate in the European Competence Center for Moor and Climate.

  6. Peat bogs and their organic soils: Archives of atmospheric change and global environmentalsignificance (Philippe Duchaufour Medal Lecture)

    Science.gov (United States)

    Shotyk, William

    2013-04-01

    A bog is much more than a waterlogged ecosystem where organic matter accumulates as peat. Peatlands such as bogs represent a critical link between the atmosphere, hydrosphere, and biosphere. Plants growing at the surface of ombrotrophic bogs receive nutrients exclusively from the atmosphere. Despite the variations in redox status caused by seasonal fluctuations in depth to water table, the low pHof the waters, and abundance of dissolved organic matter, bogs preserve a remarkably reproducible history of atmospheric pollution, climate change, landscape evolution and human history. For example, peat cores from bogs in Europe and North America have provided detailed reconstructions of the changing rates and sources of Ag, Cd, Hg, Pb, Sb, and Tl, providing new insights into the geochemical cycles of these elements, including the massive perturbations induced by human activities beginning many thousands of years ago. Despite the low pH, and perhaps because of the abundance of dissolved organic matter, bogs preserve many silicate and aluminosilicate minerals which renders them valuable archives of atmospheric dust deposition and the climate changes which drive them. In the deeper, basal peat layers of the bog, in the minerotrophic zone where pore waters are affected bymineral-water interactions in the underlying and surrounding soils and sediments, peat serves as animportant link to the hydrosphere, efficiently removing from the imbibed groundwaters such trace elements as As, Cu, Mo, Ni, Se, V, and U. These removal processes, while incompletely understood, are so effective that measuring the dissolved fraction of trace elements in the pore waters becomes a considerable challenge even for the most sophisticated analytical laboratories. While the trace elements listed above are removed from groundwaters (along with P and S), elements such as Fe and Mn are added to the waters because of reductive dissolution, an important first step in the formation of lacustrine Fe and Mn

  7. Mites (Acari at the edges of bog pools in Orawa–Nowy-Targ Basin (S Poland, with particular reference to the Oribatida

    Directory of Open Access Journals (Sweden)

    Seniczak Anna

    2014-12-01

    Full Text Available Mites, and among them especially the Oribatida, are very abundant in bogs, being good bioindicators of various changes, but little is known about their reaction to heavy industrial exploitation of bogs. This study aimed to compare the acarofauna of the edges of small pools located in 2 bogs of Orawa-Nowy-Targ Basin (Kotlina Orawsko-Nowotarska, namely Łysa Puścizna (LP and Bór Podczerwony (BP, degraded to different degrees by peat exploitation. The area of bog LP has decreased since the end of the 19th century by 34%, while that of BP has decreased during this time drastically (by 68%. Water in both studied pools differed from that in natural bogs, reported in the literature, especially in pH, colour, and oxygen conditions (COD and BOD5, and these differences were more pronounced at BP. The abundance of mites was similar to that observed in natural bogs, and the Oribatida dominated among mites, constituting over 99% of them. The species diversity of Oribatida was low in both pools, but especially in pool BP. In both bogs the aquatic species were the most abundant due to the wet study season. The species structure of Oribatida differed, however, from that reported from natural bogs as well as from each other. At the less degraded bog LP the most abundant was Hydrozetes lacustris (D = 69%, while at bog BP, with worse water parameters, Trimalaconothrus maior highly dominated (D = 93%. This suggests that the latter species is very tolerant to water parameters, being a successful coloniser of degraded bogs.

  8. Biological N2 fixation mainly controlled by Sphagnum tissue N:P ratio in ombrotrophic bogs

    Science.gov (United States)

    Zivkovic, Tatjana; Moore, Tim R.

    2017-04-01

    Most of the 18 Pg nitrogen (N) accumulated in northern nutrient-poor and Sphagnum-dominated peatlands (bogs and fens) can be attributed to N2-fixation by diazotrophs either associated with the live Sphagnum or non-symbiotically in the deeper peat such as through methane consumption close to the water table. Where atmospheric N deposition is low (Sphagnum, suggested by the increase in tissue N:P to >16. It is unclear how Sphagnum-hosted diazotrophic activity may be affected by N deposition and thus changes in N:P ratio. First, we investigated the effects of long-term addition of different sources of nitrogen (0, 1.6, 3.2 and 6.4 g N m-2 y-1as NH4Cl and NaNO3), and phosphorus (5 g P m-2 y-1as KH2PO4) on Sphagnum nutrient status (N, P and N:P ratio), net primary productivity (NPP) and Sphagnum-associated N2fixation at Mer Bleue, a temperate ombrotrophic bog. We show that N concentration in Sphagnum tissue increased with larger rates of N addition, with a stronger effect on Sphagnum from NH4 than NO3. The addition of P created a 3.5 fold increase in Sphagnum P content compared to controls. Sphagnum NPP decreased linearly with the rise in N:P ratio, while linear growth declined exponentially with increase in Sphagnum N content. Rates of N2-fixation determined in the laboratory significantly decreased in response to even the smallest addition of both N species. In contrast, the addition of P increased N2 fixation by up to 100 times compared to N treatments and up to 5-30 times compared to controls. The change in N2-fixation was best modeled by the N:P ratio, across all experimental treatments. Secondly, to test the role of N:P ratio on N2-fixation across a range of bogs, eight study sites along the latitudinal gradient from temperate, boreal to subarctic zone in eastern Canada were selected. From each bog, two predominant microptopographies, hummocks and hollows, were tested for both N2-fixation activity in the laboratory and Sphagnum tissue concentrations of N, P and N

  9. Boreal bog plants: nitrogen sources and uptake of recently deposited nitrogen

    International Nuclear Information System (INIS)

    Nordbakken, J.F.; Ohlson, M.; Hoegberg, P.

    2003-01-01

    The main goals of this study were to determine the δ 15 N signature of quantitatively important boreal bog plants as basis for discussing their N sources, and to assess the effects of five different 3 year N treatments (i.e. 0, 5, 10, 20 and 40 kg N ha -1 year -1 ) on the bog plants and surface peat at different depths (i.e. 0, 5, 10, 20 and 40 cm) by using 15 N as tracer. Plants and peat were analyzed for N concentration, 15 N natural abundance and 15 N at.%. From the results we draw three main conclusions: First, the relative importance of different N sources is species-specific among bog plants. Second, an annual addition of 5 kg N ha -1 year -1 was sufficient to significantly increase the N concentration in Sphagnum mosses, liverworts and shallow rooted vascular plants, and an annual addition of 40 kg N ha -1 year -1 during 3 years was not sufficient to increase the N concentration in deep rooted plants, although the 15 N content increased continuously, indicating a possible longer term effect. Third, an annual addition of 40 kg N ha -1 year -1 during 3 years increased the N content in surface peat at depths of 5 and 10 cm, but not at depths of 20 and 40 cm, indicating the capacity of the living Sphagnum mosses and the surface peat to take up deposited N, and thereby function as a filter. - Living Sphagnum mosses and surface peat function as a filter for added nitrogen

  10. Investigation into perfluoroalkyl substances (PFASs) in a cranberry bog: method development and sampling results.

    Science.gov (United States)

    Genualdi, Susan; Jeong, Nahyun; deJager, Lowri; Begley, Timothy

    2017-12-01

    The contamination of groundwater and surface water from previous uses of perfluoroalkyl substances (PFASs), particularly products containing the contaminants perfluorooctane sulfonate (PFOS) and perfluorooctanoate (PFOA), has become a concern for drinking water and as a potential exposure route to the food supply. In 2016, the Food and Drug Administration (FDA) was asked to investigate a bog in Massachusetts where the surface water was believed to be contaminated with PFASs. As a result, a method was developed for the analysis of PFASs in cranberries, and water and fruit from the affected bog were evaluated. A QuEChERS method was developed and validated for PFOA, PFOS, and six additional shorter-chain PFASs. Method recoveries ranged from 60% to 115% for validation spikes performed at 10, 20 and 40 ng g -1 and method detection limits ranged from 0.2 to 5.6 ng g -1 . Bog water samples were analysed using Environmental Protection Agency (EPA) method 537 for PFOA, PFOS and four additional short-chain PFASs. Surface water concentrations for PFOS ranged from 16 to 122 ng L -1 and input water concentrations were 132 ng L -1 and 206 ng L -1 . Of the eight water samples, seven had water concentrations that exceeded the EPA health advisory level for PFOS of 70 ng L -1 . Of the 42 cranberry samples analysed, none had detects of PFOA or PFOS above their method detection limits (0.4 and 0.5 ng g -1 , respectively), nor any of the other short-chain PFASs.

  11. Unexpected differences in butterfly diversity between two peat bogs in the same area

    Directory of Open Access Journals (Sweden)

    Klimczuk Przemysław

    2017-09-01

    Full Text Available Peat bogs are listed among the most threatened habitats in central Europe, a situation that is reflected by, for example, the conservational status of stenotopic butterflies. Even so, this group remains relatively little studied and most of the available data are limited to qualitative records. The present study enabled us to gain insight into the butterfly fauna of the two largest peat bogs in the Knyszyn Forest (NE Poland, i.e. Bagno Moskal and the one in the Jesionowe Góry nature reserve. The sites, only ca 10 km apart, are characterized by similar vegetation (mainly the Ledo-Sphagnetum association. The study was carried out in 2013-2015 using the transect method, i.e. regular counts along fixed routes. A total of 37 species, including three tyrphobionts (Colias palaeno, Plebejus optilete and Boloria eunomia and two tyrphophiles (Callophrys rubi and Boloria euphrosyne, were recorded. The greatest and unexpected differences between the sites were related to the complete absence of P. optilete at Bagno Moskal, the significantly higher abundance of B. eunomia at Jesionowe Góry and the greater abundance of B. euphrosyne at Bagno Moskal. In addition, C. palaeno was observed sporadically and only at Bagno Moskal. There was some heterogeneity in the distribution and density of particular species, however. Ledum palustre was found to be the most important nectar plant, its flowers also being frequently visited by tyrphoneutrals. The present study shows that isolated island-like habitats (e.g. peat bogs may possess specific features and be subject to specific independent changes. The results provide a good basis for further research into the habitat preferences of tyrphophilous and tyrphobiontic butterflies, which is important in the context of their conservation.

  12. Pb and Cd concentrations in a southern Bavarian bog profile and the history of vegetation as recorded by pollen analysis

    Energy Technology Data Exchange (ETDEWEB)

    Kuester, H.; Rehfuess, K.-E. [Universitaet Muenchen, Muenchen (Germany). Inst. fuer Vor- und Fruehgeschichte

    1997-12-01

    In the lower part of a raised bog profile from Langegger Filz, southern Bavaria, the Pb and Cd concentrations were comparatively low while considerably higher concentrations of both elements were observed in the upper section of the profile. The peat layers with the highest concentrations of Pb and Cd were found to date from the Iron Age, the Roman Age, and the Middle Ages. The Fagus pollen curve reflects the beginning of a beech decline exactly in those peat layers in which the start of the Pb increase is visible. Therefore it appears that metal smelting caused a local release of heavy metals which were subsequently deposited in the raised bog. Metals could only be smelted when wood was cut and burned, and beech charcoal was preferred as it produces relatively high temperatures. The good agreement between the Pb concentration profile and the pollen analyses suggests that the bog provides an accurate record of atmospheric Pb deposition. 14 refs., 3 figs.

  13. Ground-penetrating radar study of the Cena Bog, Latvia: linkage of reflections with peat moisture content

    Directory of Open Access Journals (Sweden)

    Karušs, J.

    2015-12-01

    Full Text Available Present work illustrates results of the ground-penetrating radar (GPR study of the Cena Bog, Latvia. Six sub-horizontal reflections that most probably correspond to boundaries between sediments with different electromagnetic properties were identified. One of the reflections corresponds to bog peat mineral bottom interface but the rest are linked to boundaries within the peat body. The radar profiles are incorporated with sediment cores and studies of peat moisture and ash content, and degree of decomposition. Most of the electromagnetic wave reflections are related to changes in peat moisture content. The obtained data show that peat moisture content changes of at least 3 % are required to cause GPR signal reflection. However, there exist reflections that do not correlate with peat moisture content. As a result, authors disagree with a dominant opinion that all reflections in bogs are solely due to changes in volumetric peat moisture content.

  14. Comparison of Supercritical Fluid and Soxhlet Extraction Methods for the Determination of Chlorothalonil from Cranberry Bog Soils.

    Science.gov (United States)

    Erstfeld; Chen

    1998-02-16

    The development and validation of an analytical method to determine the concentration of chlorothalonil from cranberry bog soil using supercritical fluid extraction (SFE) are reported. A self-built supercritical fluid extractor using CO(2) as the supercritical fluid (SCF) was used. The recovery of chlorothalonil was optimized by varying extraction temperature, pressure, time (static and dynamic), organic modifiers, and SCF flow rate. This method was then compared to a Soxhlet extraction procedure. SFE had more consistent performance than the Soxhlet extraction method for the recovery of chlorothalonil from both fortified bog soils and field samples. SFE provided cleaner extracts, had shorter extraction times, and used less organic solvent than the Soxhlet extraction method. This result is consistent with other SFE methods for determining pesticides from various environmental matrices. Thus, SFE is a preferred method for the extraction of chlorothalonil from cranberry bog soil.

  15. Sorption of radioiodide in an acidic, nutrient-poor boreal bog: insights into the microbial impact

    International Nuclear Information System (INIS)

    Lusa, M.; Bomberg, M.; Aromaa, H.; Knuutinen, J.; Lehto, J.

    2015-01-01

    Batch sorption experiments were conducted to evaluate the sorption behaviour of iodide and the microbial impact on iodide sorption in the surface moss, subsurface peat, gyttja, and clay layers of a nutrient-poor boreal bog. The batch distribution coefficient (K d ) values of iodide decreased as a function of sampling depth. The highest K d values, 4800 L/Kg dry weight (DW) (geometric mean), were observed in the fresh surface moss and the lowest in the bottom clay (geometric mean 90 mL/g DW). In the surface moss, peat and gyttja layers, which have a high organic matter content (on average 97%), maximum sorption was observed at a pH between ∼4 and 5 and in the clay layer at pH 2. The K d values were significantly lower in sterilized samples, being 20-fold lower than the values found for the unsterilized samples. In addition, the recolonization of sterilized samples with a microbial population from the fresh samples restored the sorption capacity of surface moss, peat and gyttja samples, indicating that the decrease in the sorption was due to the destruction of microbes and supporting the hypothesis that microbes are necessary for the incorporation of iodide into the organic matter. Anoxic conditions reduced the sorption of iodide in fresh, untreated samples, similarly to the effect of sterilization, which supports the hypothesis that iodide is oxidized into I 2 /HIO before incorporation into the organic matter. Furthermore, the K d values positively correlated with peroxidase activity in surface moss, subsurface peat and gyttja layers at +20 °C, and with the bacterial cell counts obtained from plate count agar at +4 °C. Our results demonstrate the importance of viable microbes for the sorption of iodide in the bog environment, having a high organic matter content and a low pH. - Highlights: • Sorption of iodide is highest on the surface Sphagnum layer of the bog. • Sterilization of peat decreases the sorption of iodide. • Anoxic conditions decrease

  16. Peat decomposition records in three pristine ombrotrophic bogs in southern Patagonia

    Directory of Open Access Journals (Sweden)

    T. Broder

    2012-04-01

    Full Text Available Ombrotrophic bogs in southern Patagonia have been examined with regard to paleoclimatic and geochemical research questions but knowledge about organic matter decomposition in these bogs is limited. Therefore, we examined peat humification with depth by Fourier Transformed Infrared (FTIR measurements of solid peat, C/N ratio, and δ13C and δ15N isotope measurements in three bog sites. Peat decomposition generally increased with depth but distinct small scale variation occurred, reflecting fluctuations in factors controlling decomposition. C/N ratios varied mostly between 40 and 120 and were significantly correlated (R2 > 0.55, p < 0.01 with FTIR-derived humification indices. The degree of decomposition was lowest at a site presently dominated by Sphagnum mosses. The peat was most strongly decomposed at the driest site, where currently peat-forming vegetation produced less refractory organic material, possibly due to fertilizing effects of high sea spray deposition. Decomposition of peat was also advanced near ash layers, suggesting a stimulation of decomposition by ash deposition. Values of δ13C were 26.5 ± 2‰ in the peat and partly related to decomposition indices, while δ15N in the peat varied around zero and did not consistently relate to any decomposition index. Concentrations of DOM partly related to C/N ratios, partly to FTIR derived indices. They were not conclusively linked to the decomposition degree of the peat. DOM was enriched in 13C and in 15N relative to the solid phase probably due to multiple microbial modifications and recycling of N in these N-poor environments. In summary, the depth profiles of C/N ratios, δ13C values, and FTIR spectra seemed to reflect changes in environmental conditions affecting decomposition, such as bog wetness, but were dominated by site specific factors, and are further influenced by ash

  17. Eddy covariance measurements of greenhouse gases from a restored and rewetted raised bog ecosystem.

    Science.gov (United States)

    Lee, S. C.; Christen, A.; Black, T. A.; Johnson, M. S.; Ketler, R.; Nesic, Z.; Merkens, M.

    2015-12-01

    Wetland ecosystems play a significant role in the global carbon (C) cycle. Wetlands act as a major long-term storage of carbon by sequestrating carbon-dioxide (CO2) from the atmosphere. Meanwhile, they can emit significant amounts of methane (CH4) due to anaerobic microbial decomposition. The Burns Bog Ecological Conservancy Area (BBECA) is recognized as one of Canada's largest undeveloped natural areas retained within an urban area. Historically, it has been substantially reduced in size and degraded by peat mining and agriculture. Since 2005, the bog has been declared a conservancy area, and the restoration efforts in BBECA focus on rewetting the disturbed ecosystems to promote a transition back to a raised bog. A pilot study measured CH4, CO2 and N2O exchanges in 2014 and concluded to monitor CO2, CH4 fluxes continuously. From the perspective of greenhouse gas (GHG) emissions, CO2 sequestered in bog needs to be protected and additional CO2 and CH4 emissions due to land-cover change need to be reduced by wise management. In this study, we measured the growing-season (June-September) fluxes of CO2 and CH4 exchange using eddy covariance (EC). A floating platform with an EC system for both CO2 (closed-path) and CH4 (open-path) began operation in June 2015. During the growing-season, gross ecosystem photosynthesis (GEP) and ecosystem respiration (Re) averaged 5.87 g C m-2 day-1 and 2.02 g C m-2 day-1, respectively. The magnitude of GEP and Re were lower than in previous studies of pristine northern peatlands. The daily average CH4 emission was 0.99 (±1.14) g C m-2 day-1 and it was higher than in most previous studies. We also characterized how environmental factors affected the seasonal dynamics of these exchanges in this disturbed peatland. Our measurements showed that soil temperature and soil water content were major drivers of seasonal changes of GHG fluxes. The daily average GHG warming potential (GWP) of the emissions in the growing seasons (from CO2 and CH4

  18. IMPACTS OF ECOTOURISM ON THE BOG OF SERRA NEGRA - BEZERROS/ PE

    Directory of Open Access Journals (Sweden)

    Carolina Florio Castro

    2005-05-01

    Full Text Available The “Brejo da Serra Negra” ( Bog of Serra Negra has become an area of interest of manysectors of society, among them tourism in its different forms. Ecotourism is one of thepropellers of tourism and defined by the Institute of Ecotourism of Brazil as : “the practice ofrecreational, sporting or educational tourism using, in a sustainable form, natural and culturalassets, encouraging conservation, promoting environmental awareness and assuring the wellbeing of the populations involved” (Instituto de Ecoturismo do Brasil, 1995. Within thisperspective some questions such as : how does ecotourism is developed in the concernedarea? What are the impacts caused on Brejo da Serra Negra ( Bog of Serra Negra? How isenvironmental awareness being addressed? should be answered.The Brejo da Serra Negra has been the constant aim of ecotourism because of its very uniquebeauty and the fact that it is a climatic sub-humid area in the hinterlands of Pernambuco andattraction to the so-called radical sports, ecologic tours, caverns exploring as well as camping.

  19. Radiocarbon dating of Sphagnum cellulose from Mohos peat bog, East Carpathians

    Science.gov (United States)

    Hubay, Katalin; Braun, Mihály; Harangi, Sándor; Palcsu, László; Túri, Marianna; Rinyu, László; Molnár, Mihály

    2015-04-01

    This work focuses on building a high-resolution age-depth model for quantitative paleoclimate study from the Mohos peat bog, East Carpathians. Peats are important archives for Quaternary science, because they preserve environmental changes. To study the chronology of peat profiles the key is in the precise coring and reliable dating. However, many studies dealing with coring and radiocarbon dating of peat deposits they often shown problems with the proper methods and material. With our novel coring technique we reached undisturbed and uncompressed peat cores from the Mohos bog. A 10 meter deep peat profile was drilled in 2012 using a modified technique of a piston corer. The core presents a continuous peat profile from the last 11.500 cal. yr BP. The chronology was based on AMS radiocarbon analyses of the separated Sphagnum samples from different depths of the profile. The peat samples were wet sieved (40-280 μm) to avoid contamination by rootlets. Dry Sphagnum samples for AMS dating were prepared using the classical acid-base-acid (ABA) method completed with an oxidative bleaching step to get clean cellulose. Sphagnum cellulose samples were converted to CO2 and later graphite and measured by EnvironMICADAS accelerator mass spectrometry (AMS) in Hertelendi Laboratory (Debrecen, Hungary). Fine peat accumulation rate changes (sections with lowest accumulation values) were observed along the profile. Based on the chronology in further studies we want to focus special intervals to investigate environmental changes in the Holocene. Key words: peat, radiocarbon, cellulose

  20. Mid- and late Holocene human impact recorded by the Coltrondo peat bog (NE Italian Alps)

    Science.gov (United States)

    Segnana, Michela; Poto, Luisa; Gabrieli, Jacopo; Martino, Matteo; Oeggl, Klaus; Barbante, Carlo

    2016-04-01

    Peat bogs are ideal archives for the study of environmental changes, whether these are natural or human induced. Indeed, receiving water and nutrients exclusively from dry and wet atmospheric depositions, they are among the most suitable matrices for palaeoenvironmental reconstruction. The present study is focused on the Eastern sector of the Italian Alps, where we sampled the Coltrondo peat bog, in the Comelico area (ca. 1800 m a.s.l.) The knowledge of the human history in this area is rather scarce: the only pieces of archaeological evidence found in this area dates back to the Mesolithic and the absence of later archaeological finds makes it difficult to reconstruct the human settlement in the valley. With the main aim to obtain information about the human settlement in that area we selected a multi-proxy approach, combining the study of biotic and abiotic sedimentary components archived in the 7900 years-peat bog record. Pollen analysis is performed along the core registering human impacts on the area from ca. 2500 cal BP, when land-use changes are well evidenced by the presence of human-related pollen and non-pollen palynomorphs (NPPs), as well as by the increase in micro-charcoal particles. Periods of increased human impact are recorded at the end of the Middle Ages and later, at the end of the 19th century. The analysis of trace elements, such as lead, is performed by means of ICP-MS technique and its enrichment factor (EF) is calculated. A first slight increase of Pb EF during Roman Times is possibly related to mining activities carried out by the Romans. Mining activities carried out in the area are registered during the Middle Ages, while the advent of the industrialization in the 20th century is marked by the highest EF values registered on the top of the core. To help and support the interpretation of geochemical data, lead isotopes ratios are also measured using ICP-MS to discriminate between natural and anthropogenic sources of lead. The 206Pb/207Pb

  1. Nitrogen dynamics in peat bogs: Comparison of sites with contrasting pollution levels (Central Europe)

    Science.gov (United States)

    Novak, Martin; Bohdalkova, Leona; Stepanova, Marketa; Vile, Melanie A.; Wieder, Kelman R.

    2013-04-01

    Nitrogen belongs to chemical elements whose biogeochemical cycles are most heavily disturbed by human activities, and large regions worlwide experience elevated depositions of reactive N (NO3-, NH4+). Peatlands contain as much as 15 % of the world's soil N. It it is unclear whether fertilizing by anthopogenic N will lead to higher storage of C in wetlands. Elevated N input may lead to both higher net primary productivity, but will also augment microbial decomposition. Here we discuss two aspects of N cycling in Sphagnum-dominated bogs in the Czech Republic, an area characterized by a steep north-south pollution gradient and high annual N deposition (60 kg ha-1). These two aspects are N inventory in 210Pb-dated peat cores, and post-depositional mobility of N in peat. We compared the N inventory in two Czech bogs, differing in pollution, with cumulative atmospheric N input. We hypothesized that the total amount of N in the peat cores would be smaller than the cumulative N input (leaching of excess N from the bog, denitrification). The two bogs were VJ (industrial north) and CB (rural south). The investigated period was 1885-2002. The total amount of N was 4020 kg ha-1 at VJ and 1530 kg ha-1 at CB. Peat in the north contained 2.6 times more N than in the south. Historical rates of N deposition in the Czech Republic are well known (numerous papers by Kopacek). To estimate cumulative N inputs into the bogs, we also used the monthly N depositions between 1994 and 2002, measured in two nearby catchments. The estimated cumulative atmospheric N input was 1350 kg ha-1 at VJ, and 530 kg ha-1 at CB. In both cases, the amount of N found in peat was 3 times higher than the estimated atmospheric N input. Such high storage of N in peat is surprising. Post-depositional mobility of N may help to explain the discrepancies between atmospheric N inputs and N storage in peat. We found two-fold evidence for post-depositional mobility of N. Maximum N concentrations at VJ were observed in

  2. Annual greenhouse gas budget for a bog ecosystem undergoing restoration by rewetting

    Directory of Open Access Journals (Sweden)

    S.-C. Lee

    2017-06-01

    Full Text Available Many peatlands have been drained and harvested for peat mining, agriculture, and other purposes, which has turned them from carbon (C sinks into C emitters. Rewetting of disturbed peatlands facilitates their ecological recovery and may help them revert to carbon dioxide (CO2 sinks. However, rewetting may also cause substantial emissions of the more potent greenhouse gas (GHG methane (CH4. Our knowledge of the exchange of CO2 and CH4 following rewetting during restoration of disturbed peatlands is currently limited. This study quantifies annual fluxes of CO2 and CH4 in a disturbed and rewetted area located in the Burns Bog Ecological Conservancy Area in Delta, BC, Canada. Burns Bog is recognized as the largest raised bog ecosystem on North America's west coast. Burns Bog was substantially reduced in size and degraded by peat mining and agriculture. Since 2005, the bog has been declared a conservancy area, with restoration efforts focusing on rewetting disturbed ecosystems to recover Sphagnum and suppress fires. Using the eddy covariance (EC technique, we measured year-round (16 June 2015 to 15 June 2016 turbulent fluxes of CO2 and CH4 from a tower platform in an area rewetted for the last 8 years. The study area, dominated by sedges and Sphagnum, experienced a varying water table position that ranged between 7.7 (inundation and −26.5 cm from the surface during the study year. The annual CO2 budget of the rewetted area was −179 ± 26.2 g CO2–C m−2 yr−1 (CO2 sink and the annual CH4 budget was 17 ± 1.0 g CH4–C m−2 yr−1 (CH4 source. Gross ecosystem productivity (GEP exceeded ecosystem respiration (Re during summer months (June–August, causing a net CO2 uptake. In summer, high CH4 emissions (121 mg CH4–C m−2 day−1 were measured. In winter (December–February, while roughly equal magnitudes of GEP and Re made the study area CO2 neutral, very low CH4 emissions (9 mg CH4–C m−2

  3. Annual greenhouse gas budget for a bog ecosystem undergoing restoration by rewetting

    Science.gov (United States)

    Lee, Sung-Ching; Christen, Andreas; Black, Andrew T.; Johnson, Mark S.; Jassal, Rachhpal S.; Ketler, Rick; Nesic, Zoran; Merkens, Markus

    2017-06-01

    Many peatlands have been drained and harvested for peat mining, agriculture, and other purposes, which has turned them from carbon (C) sinks into C emitters. Rewetting of disturbed peatlands facilitates their ecological recovery and may help them revert to carbon dioxide (CO2) sinks. However, rewetting may also cause substantial emissions of the more potent greenhouse gas (GHG) methane (CH4). Our knowledge of the exchange of CO2 and CH4 following rewetting during restoration of disturbed peatlands is currently limited. This study quantifies annual fluxes of CO2 and CH4 in a disturbed and rewetted area located in the Burns Bog Ecological Conservancy Area in Delta, BC, Canada. Burns Bog is recognized as the largest raised bog ecosystem on North America's west coast. Burns Bog was substantially reduced in size and degraded by peat mining and agriculture. Since 2005, the bog has been declared a conservancy area, with restoration efforts focusing on rewetting disturbed ecosystems to recover Sphagnum and suppress fires. Using the eddy covariance (EC) technique, we measured year-round (16 June 2015 to 15 June 2016) turbulent fluxes of CO2 and CH4 from a tower platform in an area rewetted for the last 8 years. The study area, dominated by sedges and Sphagnum, experienced a varying water table position that ranged between 7.7 (inundation) and -26.5 cm from the surface during the study year. The annual CO2 budget of the rewetted area was -179 ± 26.2 g CO2-C m-2 yr-1 (CO2 sink) and the annual CH4 budget was 17 ± 1.0 g CH4-C m-2 yr-1 (CH4 source). Gross ecosystem productivity (GEP) exceeded ecosystem respiration (Re) during summer months (June-August), causing a net CO2 uptake. In summer, high CH4 emissions (121 mg CH4-C m-2 day-1) were measured. In winter (December-February), while roughly equal magnitudes of GEP and Re made the study area CO2 neutral, very low CH4 emissions (9 mg CH4-C m-2 day-1) were observed. The key environmental factors controlling the seasonality of

  4. Nutrient additions in pristine Patagonian Sphagnum bog vegetation : can phosphorus addition alleviate (the effects of) increased nitrogen loads

    NARCIS (Netherlands)

    Fritz, C.; Dijk, G. van; Smolders, A.J.P.; Pancotto, V.A.; Elzenga, J.T.M.; Roelofs, J.G.M.; Grootjans, A.P.

    Sphagnum-bog ecosystems have a limited capability to retain carbon and nutrients when subjected to increased nitrogen (N) deposition. Although it has been proposed that phosphorus (P) can dilute negative effects of nitrogen by increasing biomass production of Sphagnum mosses, it is still unclear

  5. The sensitivity of Sphagnum to surface layer conditions in a re-wetted bog: a simulation study of water stress

    NARCIS (Netherlands)

    Schouwenaars, J.M.; Gosen, A.M.

    2007-01-01

    The behaviour of the water table in re-wetted bogs varies widely between different locations so that recolonising Sphagnum is vulnerable to water stress, especially when the water table is drawn down in summer. It is important to understand how physical site conditions influence the occurrence of

  6. Reintroduction of salt marsh vegetation and phosphorus fertilisation improve plant colonisation on seawater-contaminated cutover bogs

    Directory of Open Access Journals (Sweden)

    C. Emond

    2016-07-01

    Full Text Available Coastal bogs that are used for peat extraction are prone to contamination by seawater during storm events. Once contaminated, they remain mostly bare because of the combination of high salinity, low pH, high water table and low nutrient availability. The goal of this research was to investigate how plant colonisation at salt-contaminated bogs can be accelerated, in order to prevent erosion and fluvial export of the peat. At two seawater-contaminated bogs, we tested the application of rock phosphate and dolomitic lime in combination with five plant introduction treatments: transplantation of Carex paleacea; transplantation of Spartina pectinata; transfer of salt marsh diaspores in July; transfer of salt marsh diaspores in August; and no treatment (control. The effects of different doses of lime on the growth of C. paleacea and S. pectinata were also investigated in a greenhouse experiment. In the field, phosphorus fertilisation improved plant growth. Transplantation of C. paleacea resulted in the highest plant colonisation, whereas salt marsh diaspore transfer led to the highest species diversity. Lime applications did not improve plant establishment in either the field or the greenhouse. To promote revegetation of seawater-contaminated cutover bogs, adding P is an asset, Carex paleacea is a good species to transplant, and the transfer of salt marsh diaspores improves plant diversity.

  7. Relative importance of local habitat complexity and regional factors for assemblages of oribatid mites (Acari: Oribatida) in Sphagnum peat bogs.

    Science.gov (United States)

    Minor, M A; Ermilov, S G; Philippov, D A; Prokin, A A

    2016-11-01

    We investigated communities of oribatid mites in five peat bogs in the north-west of the East European plain. We aimed to determine the extent to which geographic factors (latitude, separation distance), local environment (Sphagnum moss species, ground water level, biogeochemistry) and local habitat complexity (diversity of vascular plants and bryophytes in the surrounding plant community) influence diversity and community composition of Oribatida. There was a significant north-to-south increase in Oribatida abundance. In the variance partitioning, spatial factors explained 33.1 % of variability in abundance across samples; none of the environmental factors were significant. Across all bogs, Oribatida species richness and community composition were similar in Sphagnum rubellum and Sphagnum magellanicum, but significantly different and less diverse in Sphagnum cuspidatum. Sphagnum microhabitat explained 52.2 % of variability in Oribatida species richness, whereas spatial variables explained only 8.7 %. There was no distance decay in community similarity between bogs with increased geographical distance. The environmental variables explained 34.9 % of the variance in community structure, with vascular plants diversity, bryophytes diversity, and ground water level all contributing significantly; spatial variables explained 15.1 % of the total variance. Overall, only 50 % of the Oribatida community variance was explained by the spatial structure and environmental variables. We discuss relative importance of spatial and local environmental factors, and make general inferences about the formation of fauna in Sphagnum bogs.

  8. Home Turf: an interdisciplinary exploration of the long-term development, use and reclamation of raised bogs in the Netherlands

    NARCIS (Netherlands)

    Beek, van R.; Maas, G.J.; Berg, van den E.

    2015-01-01

    Raised bogs are popular research subjects in various scientific disciplines such as palaeobotany, climatology, archaeology and historical geography. However, interdisciplinary studies using a long-term cultural perspective are rare. This paper aims to make a contribution in that field by exploring

  9. Present results of vegetation and habitat monitoring in mountain bogs of the Jizerské hory Mts, 1991-1998

    Czech Academy of Sciences Publication Activity Database

    Rybníček, Kamil

    2000-01-01

    Roč. 17, - (2000), s. 101-108 ISSN 1211-3603 R&D Projects: GA AV ČR KSK2017602 Institutional research plan: CEZ:AV0Z6005908 Keywords : air pollution * bog ecosystems * the Jizerské hory Mts Subject RIV: EF - Botanics

  10. Observations and model results for water vapor and carbon dioxide fluxes above a sparsely vegetated bog area

    NARCIS (Netherlands)

    Jacobs, A.F.G.; Ronda, R.J.; Holtslag, A.A.M.

    2002-01-01

    In this study observations of water vapor and carbon dioxide fluxes above a sparsely vegetated bog area in the north of the Netherlands during the early growing season was analyzed. The observations are used to evaluate a combined assimilation photosynthesis (so-called A-gs) model on canopy scale

  11. Summertime greenhouse gas fluxes from an urban bog undergoing restoration through rewetting

    Directory of Open Access Journals (Sweden)

    A. Christen

    2016-04-01

    Full Text Available Rewetting can promote the ecological recovery of disturbed peatland ecosystems and may help to revert these ecosystems to carbon dioxide (CO2 sinks. However, rewetting of disturbed peatlands can also cause substantial emissions of methane (CH4 and possibly nitrous oxide (N2O. This study quantified summertime emissions of the three major long-lived greenhouse gases (GHGs CO2, CH4 and N2O; from undisturbed, disturbed and rewetted soils in the Burns Bog Ecological Conservancy Area (BBECA, a 20 km2 urban bog located in Delta, British Columbia, Canada. Four sites were chosen that represent different stages before or after ecological recovery in the BBECA: (i a relatively undisturbed scrub pine / Sphagnum / low shrub ecosystem; (ii a Rhynchospora alba / Sphagnum ecosystem that was disturbed by peat mining more than 65 years ago; (iii a R. alba / Dulichium arundinaceum ecosystem that was disturbed by peat mining 50 years ago and rewetted five years ago; and (iv a disturbed and rewetted surface with little vegetation cover that was cleared of vegetation 16 years ago and rewetted two years ago. The GHG fluxes from soils and ground vegetation were measured at all sites during June–August 2014, using a portable non-steady-state chamber system for CO2 and syringe sampling and laboratory analysis for CH4 and N2O fluxes. All four sites exhibited net GHG emissions into the atmosphere, dominated by CH4, which contributed 81–98 % of net CO2 equivalent (CO2e emissions. Overall, the median CH4 flux for all measurements and sites was ~74 mg m-2 day-1 (~30–410 mg m-2 day-1, 25th–75th percentiles. Fluxes in the rewetted (water-saturated sedge ecosystem were highest, with a quarter of the values higher than 3,000 mg m-2 day-1 (median 78 mg m-2 day-1. Exchange of CO2 due to photosynthesis and respiration was of secondary importance compared to soil CH4 emissions. Continuous CO2 flux measurements using the eddy covariance approach in the disturbed and rewetted R

  12. Soil data for a thermokarst bog and the surrounding permafrost plateau forest, located at Bonanza Creek Long Term Ecological Research Site, Interior Alaska

    Science.gov (United States)

    Manies, Kristen L.; Fuller, Christopher C.; Jones, Miriam C.; Waldrop, Mark P.; McGeehin, John P.

    2017-01-19

    Peatlands play an important role in boreal ecosystems, storing a large amount of soil organic carbon. In northern ecosystems, collapse-scar bogs (also known as thermokarst bogs) often form as the result of ground subsidence following permafrost thaw. To examine how ecosystem carbon balance changes with the loss of permafrost, we measured carbon and nitrogen storage within a thermokarst bog and the surrounding forest, which continues to have permafrost. These sites are a part of the Bonanza Creek Long Term Ecological Research (LTER) site and are located within Interior Alaska. Here, we report on methods used for core collection analysis as well as the cores’ physical, chemical, and descriptive properties.

  13. Effect of fire on phosphorus forms in Sphagnum moss and peat soils of ombrotrophic bogs.

    Science.gov (United States)

    Wang, Guoping; Yu, Xiaofei; Bao, Kunshan; Xing, Wei; Gao, Chuanyu; Lin, Qianxin; Lu, Xianguo

    2015-01-01

    The effect of burning Sphagnum moss and peat on phosphorus forms was studied with controlled combustion in the laboratory. Two fire treatments, a light fire (250 °C) and a severe fire (600 °C), were performed in a muffle furnace with 1-h residence time to simulate the effects of different forest fire conditions. The results showed that fire burning Sphagnum moss and peat soils resulted in losses of organic phosphorus (Po), while inorganic phosphorus (Pi) concentrations increased. Burning significantly changed detailed phosphorus composition and availability, with severe fires destroying over 90% of organic phosphorus and increasing the availability of inorganic P by more than twofold. Our study suggest that, while decomposition processes in ombrotrophic bogs occur very slowly, rapid changes in the form and availability of phosphorus in vegetation and litter may occur as the result of forest fires on peat soils. Copyright © 2014 Elsevier Ltd. All rights reserved.

  14. Mineral content in Sphagnum mosses from ombrotrophic bogs of southwestern Poland: pattern in species and elements

    Directory of Open Access Journals (Sweden)

    Bronisław Wojtuń

    2014-01-01

    Full Text Available Major elements (N, P, K, Ca, Mg, Na, Fe were analyzed in 11 Sphagnum species from ombrotrophic bogs in southwestern Poland. The material included species from wet to dry microsites. The highest levels of elements were recorded for S. lindbergii, whereas S. balticum and S. cuspidatum were poorest in elements. The microhabitat gradient from hummock to hollow species is clearly reflected by decreasing concentrations of Ca and Mg, and increasing concentration of Na. Phosphorus, K and N were much more enriched into moss tissues than the remaining elements. These three nutrients were also accumulated in the upper green parts of mosses, while the concentrations of Na and Fe were higher in the bottom brown parts. There were no differences in Ca and Mg between the green and brown segments.

  15. Deciphering the environmental and landscape evolution of Sierra Nevada (S Iberia) from bog archives

    Science.gov (United States)

    Garcia Alix, Antonio; Toney, Jaime L.; Jiménez-Moreno, Gonzalo; Ramos-Román, Maria J.; Anderson, R. Scott; Jiménez-Espejo, Francisco; Delgado Huertas, Antonio; Ruano, Patricia

    2016-04-01

    Sierra Nevada is the southernmost mountain range in the Iberian Peninsula and one of the highest in Europe. Its geomorphology was the result of Pleistocene glaciations that carved out depressions, valleys and cirques at high elevations in the metamorphic basement. Depressions gave rise to lakes and wetlands during the Holocene. Geophysical and organic geochemical analyses of biomarkers (n-alkanes) and bulk sediment (C and N ratio and isotopes) from two high elevation bogs (locally called "Borreguiles"): Borreguiles de la Virgen (BdlV) and Borreguiles de la Caldera (BdlC), have allowed us to track the hydrological evolution of the area and its relationship to climatic fluctuations of the western Mediterranean during the Holocene. Most of the bogs of this area resulted from the natural evolution of former small lakes. The records are 56 cm and 169 cm long, respectively. Geophysical data suggest that we recovered the whole sedimentary record from BdlC; however, there are some post-glacial sediments remaining below the BdlV core that we could not recover due to hard-ground conditions. During the early and middle Holocene, aquatic conditions predominated in BdlV compared to the most recent part of the record (low C/N values and high proportion of aquatic plants (Paq) deduced from the n-alkanes) suggesting a lake environment whose water level gradually decreased until ˜5.5 cal ky BP. This aridity trend is also observed in nearby records such as at Laguna de Río Seco (LdRS), a result of the African Humid Period demise. Carbon and nitrogen isotopes were higher during this interval, which might suggest more algae activity, in agreement with the highest concentrations of the algae Pediastrum in the area. There is an important development of terrestrial plants, a real bog stage (C/N higher than 20, high TOC, lower Paq) in both records from ˜5.5 to 3.5-3.0 cal ky BP. Those hydrological changes in the landscape might be related to a possible change in the source of

  16. Peat decomposition indicators of two contrasting peat bogs in the Eastern Alps, Austria

    Science.gov (United States)

    Drollinger, Simon; Kuzyakov, Yakov; Glatzel, Stephan

    2017-04-01

    Worldwide ˜612 Pg of carbon (C) is stored in peat, of which ˜270 to 370 Pg C have been removed from the atmosphere by peat growth since the last glacial period. Since C in peatlands is labile and sensitive to disturbances, peatlands entail the potential to release high amounts of C in the course of land use changes and proceeding global warming. Therefore, adequate peat decomposition indicators (PDI) are necessary to assess the peatland degradation status and potential C release of peatlands. In order to assess the degradation status of Alpine peat bogs and to evaluate the PDI, we compare PDI in two Alpine peat bogs with contrasting land-use histories located in the Enns valley, Austria. We evaluate the conventional PDI loss on ignition, bulk density, C:N ratios, water table depths (WTD) and the recently introduced PDI stable carbon isotope ratios (δ13C) and stable nitrogen isotope ratios (δ15N) at nine study sites. We detected significant differences in PDI between the two bogs and between the study sites, which vary in WTD and degree of decomposition. Moreover, we demonstrate strong relationships and similar depth profiles of the variables. Loss on ignition of strongly degraded sites decrease from the acrotelm (94.77%) to the catotelm (80.02%), but remain stable at less degraded sites (˜97.76%). Bulk density generally increases with depth, featuring lowest values in the acrotelm of the central bog area (0.05 g cm-3) and highest values in the catotelm of the former peat cutting areas (0.18 g cm-3). C:N ratios exhibit large variations at most sites, but demonstrate differences in the degree of decomposition. Regarding the δ13C and δ15N, we observed an increase in the uppermost layers down to depths of -24 to -42 cm at all study sites. In the catotelm, δ13C are significantly lower in strongly decomposed peat (-27.44 ±0.37‰) in contrast to the less degraded sites (-26.09 ±0.59‰). δ15N are significantly higher at strongly degraded sites in both

  17. Carbon balance of a boreal bog during a year with an exceptionally dry summer

    Energy Technology Data Exchange (ETDEWEB)

    Alm, J.; Silvola, J. [Univ. of Joensuu (Finland). Dept. of Biology; Schulman, L. [Univ. of Helsinki (Finland). Dept. of Ecology and Systematics; Walden, J. [Finnish Meteorological Inst., Helsinki (Finland); Nykaenen, H.; Martikainen, P.J. [National Public Health Inst., Kuopio (Finland). Lab. of Environmental Microbiology

    1999-01-01

    Northern peatlands are important terrestrial carbon stores, and they show large spatial and temporal variation in the atmospheric exchange of CO{sub 2} and CH{sub 4}. Thus, annual carbon balance must be studied in detail in order to predict the climatic responses of these ecosystems. Closed-chamber methods were used to study CO{sub 2} and CH{sub 4} in hollow, Sphagnum angustifolium lawn. S. fuscum lawn, and hummock microsites within an ombrotrophic S. fuscum bog. Micrometeorological tower measurements were used as a reference for the CH{sub 3} efflux from the bog. Low precipitation during May--August in 1994 and a warm July--August period caused the water table to drop by more than 15 cm below the peat surface in the hollows and to 48 cm below the surface in high hummocks. Increased annual total respiration exceeded gross production and resulted in a net C loss of 4--157 g/m{sup 2} in the different microsites. Drought probably caused irreversible desiccation in some lawns of S. angustifolium and S. balticum and in S. fuscum in the hummocks, while S. balticum growing in hollows retained its moisture and even increased its photosynthetic capacity during the July--August period. Seasonal (12 May--4 October) CH{sub 4} emissions ranged from 2 g CH{sub 4}-C/m{sup 2} in drier S. fuscum hummocks and lawns to 7 and 14 g/m{sup 2} in wetter S. angustifolium-S. balticum lawns and hollows, respectively.

  18. High methane emissions dominate annual greenhouse gas balances 30 years after bog rewetting

    Science.gov (United States)

    Vanselow-Algan, M.; Schmidt, S. R.; Greven, M.; Fiencke, C.; Kutzbach, L.; Pfeiffer, E.-M.

    2015-02-01

    Natural peatlands are important carbon sinks and sources of methane (CH4). In contrast, drained peatlands turn from a carbon sink to a carbon source and potentially emit nitrous oxide (N2O). Rewetting of peatlands thus implies climate change mitigation. However, data about the time span that is needed for the re-establishment of the carbon sink function by restoration is scarce. We therefore investigated the annual greenhouse gas (GHG) balances of three differently vegetated bog sites 30 years after rewetting. All three vegetation communities turned out to be sources of carbon dioxide (CO2) ranging between 0.6 ± 1.43 t CO2 ha-2 yr-1 (Sphagnum-dominated vegetation) and 3.09 ± 3.86 t CO2 ha-2 yr-1 (vegetation dominated by heath). While accounting for the different global warming potential (GWP) of the three greenhouse gases, the annual GHG balance was calculated. Emissions ranged between 25 and 53 t CO2-eq ha-1 yr-1 and were dominated by large emissions of CH4 (22 up to 51 t CO2-eq ha-1 yr-1), while highest rates were found at purple moor grass (Molinia caerulea) stands. These are to our knowledge the highest CH4 emissions so far reported for bog ecosystems in temperate Europe. As the restored area was subject to large fluctuations in water table, we conclude that the high CH4 emission rates were caused by a combination of both the temporal inundation of the easily decomposable plant litter of this grass species and the plant-mediated transport through its tissues. In addition, as a result of the land use history, the mixed soil material can serve as an explanation. With regards to the long time span passed since rewetting, we note that the initial increase in CH4 emissions due to rewetting as described in the literature is not limited to a short-term period.

  19. Microclimate of a peat bog and of the forest in different states of damage in the Šumava National Park

    Czech Academy of Sciences Publication Activity Database

    Hojdová, M.; Hais, M.; Pokorný, Jan

    2005-01-01

    Roč. 11, č. 1 (2005), s. 13-24 ISSN 1211-7420 Institutional research plan: CEZ:AV0Z60870520 Keywords : dying forest * microclimate * peat bog * remote sensing * temperature amplitude Subject RIV: EH - Ecology, Behaviour

  20. Using stable isotopes of water to re-evaluate the recharge/discharge functions of North American bogs and fens

    Science.gov (United States)

    Levy, Zeno; Siegel, Donald; Glaser, Paul; Dasgupta, Soumitri

    2014-05-01

    In North American mires hydrologists commonly find raised bog crests and low-lying fen water tracks to be focal points for groundwater recharge and discharge, respectively. To further test these observations we synoptically surveyed vertical profiles of peat pore water δ18O/δ2H and major mineral solutes from a range of bog and fen landforms across the Glacial Lake Agassiz Peatlands (GLAP) of northern Minnesota. We also sampled a detailed transect through a 150 km2 bog-fen complex in the Red Lake II peatland watershed of the GLAP. The molar ratios of Ca/Mg in the pore water beneath the Red Lake II bog crest are depleted in Mg with respect to the atmospheric average of 3.6, indicative of preferential flushing of Mg from the peat by meteoric recharge. Higher solute concentrations in the middle of the peat profile at an adjacent fen show focused groundwater discharge with Ca/Mg ratios of ~1.4, similar to that of water from local wells tapping underlying glacial till. However, contrary to expectations, we find evidence that modern recharge has penetrated throughout the peat column beneath both bog and fen landforms throughout the GLAP. Landform surface features control the isotopic recharge value. These landform-specific isotope signatures propagate through vertical pore water profiles. Pore waters deeper than 0.5 m partition into discrete ranges of δ18O according to three a priori landform classifications: 1) -11.9 ± 0.4 o for bog crests, 2) -10.6 ± 0.1 o for Sphagnum lawns, and 3) -8.8 ± 1.0 o for fen water tracks. The fen water tracks have standing water at their surface that is seasonally enriched by isotope fractionating evaporation and therefore fingerprints recharge to depths ≥3 m. Incongruities between isotope and solute mixing trends may be related to the dual porosity nature of peat and matrix diffusion, which could supply solutes to active pore spaces following flushing by meteoric recharge. This buffering of base solutes in the deep peat may

  1. Tracing of ca 800 yr old mining activity in peat bog using Pb elemental concentrations and isotope compositions.

    Science.gov (United States)

    Baron, S.; Carignan, J.; Ploquin, A.

    2003-04-01

    Sixty sites of slags have been documented on the Mont-Lozère in southern France. The petrographic analysis shows that slags are metallurgical wastes (800 to 850 yr BP) which certainly result from smelting activity for lead and silver extraction (Ploquin et al., 2001). The aims of this study are: 1) to trace the source of Pb ores which supplied the smelting sites, by using the Pb isotopic composition of several surrounding Pb deposits, 2) to evaluate the actual pollution caused by these slags, by using elemental and isotopic compositions of soils, water and vegetation, and 3) to document the pollution history of the region, by using elemental and isotopic compositions of peat bog cores collected in the neighbourhood of the historical smelting sites. The lead isotopic composition of galena collected in most surrounding ores is very similar to that of different slag samples. On the other hand, the high precision of the results allowed us to select the mineralised areas which were probably the ore sources. The Pb isotopic composition of slags is even more homogeneous: 208/206 Pb: 2.092±0.002; 206/207 Pb: 1.179±0.001; 208/204 Pb: 38.663±0.025; 207/204 Pb: 15.665±0.006; 206/204 Pb: 18.476±0.023, and will allow source tracing in the environment. The "Narses Mortes" peat bog, around which two smelting sites have been reported, is strongly minerotrophic and contains 8 to 60% ash. A 1.40 m core have been retrieved and divided into 58 individual samples. Minerotrophic peat bog records both atmospheric deposition, soils leaching and the grounwater influence. The measured metal concentrations are normalised to Al contents of peat bog samples and the metal/Al ratios are compared to that of the Mont-Lozère granite: relative excess in metal concentrations are found in peat bog samples. An increasing excess of most metals (Pb, Zn, Cd...) was measured for surface samples, from 55 cm depth to the top of the core (23 cm depth). This profil might be attributed to atmospheric

  2. Evaluation of heavy metal pollution in bogs of Tomsk region on change in biogeochemical activity of ericaceous shrubs

    Science.gov (United States)

    Gaskova, L. P.

    2018-01-01

    The article discusses the change in biogeochemical activity of plant species in bogs under the influence of various types of human impact (roads, cities, drainage of mires, fire). It has been established that ericaceous shrubs, depending on the species, react with varying degrees of intensity to anthropogenic influences. The biogeochemical activity of species increased by 2.5 to 4.8 times in polluted sites.

  3. Bottlenecks in bog pine multiplication by somatic embryogenesis and their visualization with the environmental scanning electron microscope.

    Science.gov (United States)

    Vlašínová, Helena; Neděla, Vilem; Đorđević, Biljana; Havel, Ladislav

    2017-07-01

    Somatic embryogenesis (SE) is an important biotechnological technique used for the propagation of many pine species in vitro. However, in bog pine, one of the most endangered tree species in the Czech Republic, limitations were observed, which negatively influenced the development and further germination of somatic embryos. Although initiation frequency was very low-0.95 %, all obtained cell lines were subjected to maturation. The best responding cell line (BC1) was used and subjected to six different variants of the maturation media. The media on which the highest number of early-precotyledonary/cotyledonary somatic embryos was formed was supplemented with 121 μM abscisic acid (ABA) and with 6 % maltose. In the end of maturation experiments, different abnormalities in formation of somatic embryos were observed. For visualization and identification of abnormalities in meristem development during proliferation and maturation processes, the environmental scanning electron microscope was used. In comparison to the classical light microscope, the non-commercial environmental scanning electron microscope AQUASEM II has been found as a very useful tool for the quick recognition of apical meristem disruption and abnormal development. To our knowledge, this is the first report discussing somatic embryogenesis in bog pine. Based on this observation, the cultivation procedure could be enhanced and the method for SE of bog pine optimized.

  4. Nutrient additions in pristine Patagonian Sphagnum bog vegetation: can phosphorus addition alleviate (the effects of) increased nitrogen loads.

    Science.gov (United States)

    Fritz, C; van Dijk, G; Smolders, A J P; Pancotto, V A; Elzenga, T J T M; Roelofs, J G M; Grootjans, A P

    2012-05-01

    Sphagnum-bog ecosystems have a limited capability to retain carbon and nutrients when subjected to increased nitrogen (N) deposition. Although it has been proposed that phosphorus (P) can dilute negative effects of nitrogen by increasing biomass production of Sphagnum mosses, it is still unclear whether P-addition can alleviate physiological N-stress in Sphagnum plants. A 3-year fertilisation experiment was conducted in lawns of a pristine Sphagnum magellanicum bog in Patagonia, where competing vascular plants were practically absent. Background wet deposition of nitrogen was low (≈ 0.1-0.2 g · N · m(-2) · year(-1)). Nitrogen (4 g · N · m(-2) · year(-1)) and phosphorus (1 g · P · m(-2) · year(-1)) were applied, separately and in combination, six times during the growing season. P-addition substantially increased biomass production of Sphagnum. Nitrogen and phosphorus changed the morphology of Sphagnum mosses by enhancing height increment, but lowering moss stem density. In contrast to expectations, phosphorus failed to alleviate physiological stress imposed by excess nitrogen (e.g. amino acid accumulation, N-saturation and decline in photosynthetic rates). We conclude that despite improving growth conditions by P-addition, Sphagnum-bog ecosystems remain highly susceptible to nitrogen additions. Increased susceptibility to desiccation by nutrients may even worsen the negative effects of excess nitrogen especially in windy climates like in Patagonia. © 2011 German Botanical Society and The Royal Botanical Society of the Netherlands.

  5. Non-Pollen Palynomorphs from Mid-Holocene Peat of the Raised Bog Borsteler Moor (Lower Saxony, Germany

    Directory of Open Access Journals (Sweden)

    Shumilovskikh Lyudmila S.

    2015-06-01

    Full Text Available In order to reconstruct regional vegetation changes and local conditions during the fen-bog transition in the Borsteler Moor (northwestern Germany, a sediment core covering the period be tween 7.1 and 4.5 cal kyrs BP was palynologically investigated. The pollen diagram demonstrates the dominance of oak forests and a gradual replacement of trees by raised bog vegetation with the wetter conditions in the Late Atlantic. At ~ 6 cal kyrs BP, the non-pollen palynomorphs (NPP demonstrate the succession from mesotrophic conditions, clearly indicated by a number of fun gal spore types, to oligotrophic conditions, indicated by Sphagnum spores, Bryophytomyces sphagni, and testate amoebae Amphitrema, Assulina and Arcella, etc. Four relatively dry phases during the transition from fen to bog are clearly indicated by the dominance of Calluna and associated fungi as well as by the in crease of microcharcoal. Several new NPP types are described and known NPP types are identified. All NPP are discussed in the context of their palaeoecological indicator values.

  6. Variations in the D/H and 18O/16O ratios in cellulose extracted from a peat bog core

    International Nuclear Information System (INIS)

    Brenninkmeijer, C.A.M.; Mook, W.G.; Geel, B. van

    1982-01-01

    A peat core from a raised bog covering the period 3100 to 2400 14 C years B.P. has been analysed for D/H and 18 O/ 16 O ratios. These analyses were applied to cellulose, extracted from 56 successive layers of 1 cm thickness. D/H ratios were determined for the carbon bonded hydrogen; 18 O/ 16 O analyses were performed by applying a new method. For the interpretation of the results obtained on peat, the isotopic ratios of 11 living bog plant species were measured, showing a relatively large scatter. Most pronounced is a depletion in D of about 25per mille and in 18 O of about 5per mille of the Sphagnum mosses relative to the vascular bog plants. This different isotopic composition is reflected by the deltaD and delta 18 O records of the peat core, because the abundance of the remains of non-vascular plants is variable. If this effect is taken account of, the remaining deltaD variations appear to be too large to be attributed to variations in the isotopic compositions of precipitation. As palaeoclimatic indicators the D/H and 18 O/ 16 O ratio qualitatively agree with the pollen analytical evidence for the climatic deterioration of the Subboreal-Subatlantic transition. (orig.)

  7. Large scale in-situ BOrehole and Geofluid Simulator (i.BOGS) for the development and testing of borehole technologies at reservoir conditions

    Science.gov (United States)

    Duda, Mandy; Bracke, Rolf; Stöckhert, Ferdinand; Wittig, Volker

    2017-04-01

    A fundamental problem of technological applications related to the exploration and provision of geothermal energy is the inaccessibility of subsurface processes. As a result, actual reservoir properties can only be determined using (a) indirect measurement techniques such as seismic surveys, machine feedback and geophysical borehole logging, (b) laboratory experiments capable of simulating in-situ properties, but failing to preserve temporal and spatial scales, or vice versa, and (c) numerical simulations. Moreover, technological applications related to the drilling process, the completion and cementation of a wellbore or the stimulation and exploitation of the reservoir are exposed to high pressure and temperature conditions as well as corrosive environments resulting from both, rock formation and geofluid characteristics. To address fundamental and applied questions in the context of geothermal energy provision and subsurface exploration in general one of Europe's largest geoscientific laboratory infrastructures is introduced. The in-situ Borehole and Geofluid Simulator (i.BOGS) allows to simulate quasi scale-preserving processes at reservoir conditions up to depths of 5000 m and represents a large scale pressure vessel for iso-/hydrostatic and pore pressures up to 125 MPa and temperatures from -10°C to 180°C. The autoclave can either be filled with large rock core samples (25 cm in diameter, up to 3 m length) or with fluids and technical borehole devices (e.g. pumps, sensors). The pressure vessel is equipped with an ultrasound system for active transmission and passive recording of acoustic emissions, and can be complemented by additional sensors. The i.BOGS forms the basic module for the Match.BOGS finally consisting of three modules, i.e. (A) the i.BOGS, (B) the Drill.BOGS, a drilling module to be attached to the i.BOGS capable of applying realistic torques and contact forces to a drilling device that enters the i.BOGS, and (C) the Fluid.BOGS, a geofluid

  8. Pb-210 and fly ash particles in ombrotrophic peat bogs as indicators of industrial emissions.

    Science.gov (United States)

    Vaasma, Taavi; Karu, Helen; Kiisk, Madis; Pensa, Margus; Isakar, Kadri; Realo, Enn; Alliksaar, Tiiu; Tkaczyk, Alan Henry

    2017-08-01

    Peat cores were collected from a Sphagnum-dominated Selisoo bog, which is located about 40 km from the large oil shale-fired power plants (PPs) in Estonia. These PPs have been operational from the 1960's and had the largest negative impact on the surrounding environment during the 1970's and 1980's. Nearby ombrotrophic peatlands are good indicators of atmospheric pollution due to their properties of effectively adsorbing mineral matter and pollutants. Collected peat cores (S1 and S2) from Selisoo peat bog were sliced into 1 cm thick layers and measured gamma spectrometrically. In addition, spherical fly ash particles (SFAP) originating from the combustion of the PPs were counted. The maximum concentrations (particles per cm 3 ) of the SFAP remained between 7 and 12 cm for core S1 and between 11 and 17 cm for core S2. The concentration profiles of the SFAP reflect the combustion and emission history of the PPs. Pb-210 activity concentrations have the maximum values up to 500 Bq kg -1 and 413 Bq m -2 for S1 and for the S2 the values are 441 Bq kg -1 and 535 Bq m -2 (dry weight). The unsupported 210 Pb inventory is around 4250 Bq m -2 . This represents a 210 Pb deposition flux of 133 Bq m -2  y -1 . The estimated 210 Pb deposition via fly ash from the PPs at Selisoo area remains between 0.2 and 2.2 Bq m -2  y -1 . Considering the annual 210 Pb deposition from the atmosphere (with a precipitation rate of 600 mm y -1 ) between 92 and 133 Bq m -2 , which is regarded as the natural background value, we show that the radiological burden due to the power plants at these distances is negligible. As the peat cores exhibit noticeable differences from each other (in terms of radionuclide concentration distribution), the SFAP can provide a good additional parameter to improve the validity of results obtained only from radiometric methods in the chronological studies. SFAP can also act as a possible tool to estimate the radionuclide deposition rate via fly

  9. High methane emissions dominated annual greenhouse gas balances 30 years after bog rewetting

    Science.gov (United States)

    Vanselow-Algan, M.; Schmidt, S. R.; Greven, M.; Fiencke, C.; Kutzbach, L.; Pfeiffer, E.-M.

    2015-07-01

    Natural peatlands are important carbon sinks and sources of methane (CH4). In contrast, drained peatlands turn from a carbon sink to a carbon source and potentially emit nitrous oxide (N2O). Rewetting of peatlands thus potentially implies climate change mitigation. However, data about the time span that is needed for the re-establishment of the carbon sink function by restoration are scarce. We therefore investigated the annual greenhouse gas (GHG) balances of three differently vegetated sites of a bog ecosystem 30 years after rewetting. All three vegetation communities turned out to be sources of carbon dioxide (CO2) ranging between 0.6 ± 1.43 t CO2 ha-2 yr-1 (Sphagnum-dominated vegetation) and 3.09 ± 3.86 t CO2 ha-2 yr-1 (vegetation dominated by heath). While accounting for the different global warming potential (GWP) of CO2, CH4 and N2O, the annual GHG balance was calculated. Emissions ranged between 25 and 53 t CO2-eq ha-1 yr-1 and were dominated by large emissions of CH4 (22-51 t CO2-eq ha-1 yr-1), with highest rates found at purple moor grass (Molinia caerulea) stands. These are to our knowledge the highest CH4 emissions so far reported for bog ecosystems in temperate Europe. As the restored area was subject to large fluctuations in the water table, we assume that the high CH4 emission rates were caused by a combination of both the temporal inundation of the easily decomposable plant litter of purple moor grass and the plant-mediated transport through its tissues. In addition, as a result of the land use history, mixed soil material due to peat extraction and refilling can serve as an explanation. With regards to the long time span passed since rewetting, we note that the initial increase in CH4 emissions due to rewetting as described in the literature is not inevitably limited to a short-term period.

  10. Characterization of Groundwater Flow Processes in the Cedar Creek Watershed and the Cedarburg Bog in Southeastern Wisconsin

    Science.gov (United States)

    Graham, J. P.; Han, W. S.; Feinstein, D.; Hart, D. J.

    2014-12-01

    The purpose of this study is to characterize the geology and groundwater flow of the bog as well as the surrounding area, notably the Cedar Creek Watershed, a HUC (Hydrologic Unit Code) 12 watershed. The watershed is approximately 330 km2, and borders the sub-continental divide separating the Mississippi River Basin from the Great Lakes Basin. The Cedar Creek watershed is composed of mostly agricultural and urban land with a significant stress of groundwater withdrawal for both irrigation and residential use. This watershed has importance due to the contribution to both the Milwaukee River and Lake Michigan, and is integral in the study of regional groundwater flow of Southeastern Wisconsin. Furthermore, the Cedarburg Bog, located in the northeast corner of the Cedar Creek Watershed preserves diverse ecology and is recognized by the U.S. Department of Interior as a National Landmark. Groundwater is the primary driver for the diverse and unique ecology that is contained within the bog. Within the Cedar Creek Watershed, well data and glacial geology maps (Mickelson and Syverson, 1997) were integrated to develop a 3-dimensional subsurface map and watershed-scale groundwater flow model using the LAK3 and the SFR2 package to simulate surface water-aquifer interactions. The model includes 10 zones of the glacial sediments and the weathered and consolidated Silurian Dolomite bedrock. The hydraulic conductivity and storage parameters were calibrated with 203 head targets using universal parameter estimation code (PEST). Then, a series of future climate scenarios, developed by the Wisconsin Initiative on Climate Change Impact, were implemented to the USGS Soil-Water-Balance Code (SWB) to identify variations in recharge. The simulated recharge scenarios were adopted to predict the response of groundwater resources in the watershed and the Cedarburg Bog. Preliminary results produced from the MODFLOW model indicate the bog is acting as a recharge zone under current recharge

  11. Chromobacterium sphagni sp. nov., an insecticidal bacterium isolated from Sphagnum bogs.

    Science.gov (United States)

    Blackburn, Michael B; Farrar, Robert R; Sparks, Michael E; Kuhar, Daniel; Mitchell, Ashaki; Gundersen-Rindal, Dawn E

    2017-09-01

    Sixteen isolates of Gram-reaction-negative, motile, violet-pigmented bacteria were isolated from Sphagnum bogs in West Virginia and Maine, USA. 16S rRNA gene sequences and fatty acid analysis revealed a high degree of relatedness among the isolates, and genome sequencing of two isolates, IIBBL 14B-1T and IIBBL 37-2 (from West Virginia and Maine, respectively), revealed highly similar genomic sequences. The average nucleotide identity (gANI) calculated for these two isolates was found to be in excess of 99 %, but did not exceed 88 % when comparing either isolate with genomic sequences of Chromobacterium violaceum ATCC 12472T, C. haemolyticum DSM 19808T, C. piscinae ND17, C. subtsugae PRAA4-1T, C. vaccinii MWU205T or C. amazonense CBMAI 310T. Collectively, gANI and 16S rRNA gene sequence comparisons suggested that isolates IIBBL 14B-1T and IIBBL 37-2 were most closely related to C. subtsugae, but represented a distinct species. We propose the name Chromobacterium sphagni sp. nov. for this taxon; the type strain is IIBBL 14B-1T (=NRRL B-67130T=JCM 31882T).

  12. Mycobacterium minnesotense sp. nov., a photochromogenic bacterium isolated from sphagnum peat bogs.

    Science.gov (United States)

    Hannigan, Geoffrey D; Krivogorsky, Bogdana; Fordice, Daniel; Welch, Jacqueline B; Dahl, John L

    2013-01-01

    Several intermediate-growing, photochromogenic bacteria were isolated from sphagnum peat bogs in northern Minnesota, USA. Acid-fast staining and 16S rRNA gene sequence analysis placed these environmental isolates in the genus Mycobacterium, and colony morphologies and PCR restriction analysis patterns of the isolates were similar. Partial sequences of hsp65 and dnaJ1 from these isolates showed that Mycobacterium arupense ATCC BAA-1242(T) was the closest mycobacterial relative, and common biochemical characteristics and antibiotic susceptibilities existed between the isolates and M. arupense ATCC BAA-1242(T). However, compared to nonchromogenic M. arupense ATCC BAA-1242(T), the environmental isolates were photochromogenic, had a different mycolic acid profile and had reduced cell-surface hydrophobicity in liquid culture. The data reported here support the conclusion that the isolates are representatives of a novel mycobacterial species, for which the name Mycobacterium minnesotense sp. nov. is proposed. The type strain is DL49(T) (=DSM 45633(T) = JCM 17932(T) = NCCB 100399(T)).

  13. Characterizing Early Succession Following Wildfires at Different Severities in Boreal Bog and Fen Peatlands

    Science.gov (United States)

    Ernst, E. J.; Bourgeau-Chavez, L. L.; Kane, E. S.; Wagenbrenner, J. W.; Endres, S.

    2016-12-01

    The Arctic-boreal region is experiencing changes in climate, trending toward warmer summers, resulting in a greater occurrence of wildfires with longer burning periods and higher intensities. Drought-like conditions have dried surface fuels, leading to a higher probability of ignition, even in lowland peatlands. Previous work has been done to characterize post-fire succession rates in Arctic-boreal upland sites, but much less is known of fire effects and early successional dynamics in lowlands. Wildland fires are the number one disturbance in Canada's Northwest Territories (NWT), which characteristically burn at high intensities with large flame fronts, and result in some of the biggest wildfires in the world. Areas surrounding the Great Slave Lake, NWT—including parts of the Taiga Plains, Taiga Shield, and Boreal Plains ecozones—experienced exceptional wildfire activity in 2014 and 2015. We characterized burn severity of the bog and fen peat surface and canopy layers at several burned sites. To determine if the severe ground or crown wildfires were stand-replacing events, we characterized post-fire vegetation in peatlands in 2015 and 2016 based on seedling regeneration. We stratified sites according to estimated water residence times across the three ecozones and made comparisons between data collected at the same sites across years. This work adds much needed context for post-fire succession in boreal peatland ecosystems, as the susceptibility of these systems to burning will continue to increase with a warming climate.

  14. Climate change and water table fluctuation: Implications for raised bog surface variability

    Science.gov (United States)

    Taminskas, Julius; Linkevičienė, Rita; Šimanauskienė, Rasa; Jukna, Laurynas; Kibirkštis, Gintautas; Tamkevičiūtė, Marija

    2018-03-01

    Cyclic peatland surface variability is influenced by hydrological conditions that highly depend on climate and/or anthropogenic activities. A low water level leads to a decrease of peatland surface and an increase of C emissions into the atmosphere, whereas a high water level leads to an increase of peatland surface and carbon sequestration in peatlands. The main aim of this article is to evaluate the influence of hydrometeorological conditions toward the peatland surface and its feedback toward the water regime. A regional survey of the raised bog water table fluctuation and surface variability was made in one of the largest peatlands in Lithuania. Two appropriate indicators for different peatland surface variability periods (increase and decrease) were detected. The first one is an 200 mm y- 1 average net rainfall over a three-year range. The second one is an average annual water depth of 25-30 cm. The application of these indicators enabled the reconstruction of Čepkeliai peatland surface variability during a 100 year period. Processes of peatland surface variability differ in time and in separate parts of peatland. Therefore, internal subbasins in peatland are formed. Subbasins involve autogenic processes that can later affect their internal hydrology, nutrient status, and vegetation succession. Internal hydrological conditions, surface fluctuation, and vegetation succession in peatland subbasins should be taken into account during evaluation of their state, nature management projects, and other peatland research works.

  15. Why are there few gas bubbles in deep peat in British raised and blanket peat bogs?

    Directory of Open Access Journals (Sweden)

    R.S. Clymo

    2015-08-01

    Full Text Available (1 There is evidence of gas-filled voids - ‘bubbles’ - in deep (> 50–100 cm peat in North America. (2 I used corers, designed to collect samples of accurately known volume, to sample peat profiles down to maximum depth 700 cm at five varied bog sites in northern England and southern Scotland, and measured the proportion of space apparently occupied by bubbles. (3 Of 126 samples in peat below 50 cm depth, three had bubbles occupying 12–15 % of the volume (and one of these was at only 55 cm depth. The other 123 had apparent bubbles distributed in Gaussian fashion, positively and negatively, about zero proportion of total volume and with standard deviation less than 2 %, consistent with these ‘bubbles’ being measurement error. (4 In northern England and southern Scotland, compared with North America, less variable temperature and cooler summers may lead to concentrations of dissolved gas that are generally too low to allow bubbles to form. Even where bubbles do form in summer, they may re-dissolve at winter temperatures.

  16. The Effect of Long-term Nutrient Addition on Peat Properties in an Ombrotrophic Bog

    Science.gov (United States)

    Moore, T. R.; Bubier, J. L.; Knorr, K. H.; Roy, C.

    2017-12-01

    Atmospheric inputs of nutrients, particularly N and P, to ecosystems have increased and may have a significant effect on nutrient-deficient peatlands such as bogs. At the Mer Bleue ombrotrophic bog near Ottawa, Canada, we have conducted an experiment over 10 to 20 years by adding 1.6 to 6.4 g N m-2 yr-1 (as NH4NO3), with/without 6 g P m-2 yr-1 (as K phosphate), to evaluate the effect of increased inputs on ecosystem functions. Increased N and P amendment has changed the vegetation from a mixed shrub-Sphagnum community into one dominated by shrubs with the disappearance of mosses, with changes in plant production and litter input. The largest N and P amendments have resulted in an increase in bulk density at 0-10 cm and a lowering of the peat surface by 10 to 20 cm, creating an effective rise in the water table and an increase in CH4 emission from 15 to 50 mg m-2 d-1. Peat cores to a depth of 40 cm were collected after 10 to 15 yr of amendment and showed little change in soil pH (range 4.1 to 4.5). There were substantial increases in the concentration of N and P in the peat (8 to 14 and 0.5 to 1.5 mg g-1, respectively) and general decreases in Ca and Mg concentration. The von Post humification index increased by about 1 unit in the heavily fertilized plots, with shrub leaves replacing Sphagnum as the primary litterfall. FTIR analysis of the 0-20 cm peat showed significant increases in abundance of phenolic+aliphatic, aromatic, and carboxylic relative to polysaccharide components, revealed by the following ratios of absorbance at the respective wavenumbers: 1420/1090 cm-1, 0.41 to 0.45; 1510/1090 cm-1, 0.23 to 0.30; 1630/1090 cm-1, 0.53 to 0.65; and 1720/1090 cm-1, 0.44 to 0.48, respectively. Laboratory incubations of peat samples showed that potential rates of aerobic CH4 consumption were unaffected by nutrient treatment, apart from position relative to the water table, whereas potential rates of anaerobic CH4 production near the water table increased under the P

  17. Small spatial variability in methane emission measured from a wet patterned boreal bog

    Science.gov (United States)

    Korrensalo, Aino; Männistö, Elisa; Alekseychik, Pavel; Mammarella, Ivan; Rinne, Janne; Vesala, Timo; Tuittila, Eeva-Stiina

    2018-03-01

    We measured methane fluxes of a patterned bog situated in Siikaneva in southern Finland from six different plant community types in three growing seasons (2012-2014) using the static chamber method with chamber exposure of 35 min. A mixed-effects model was applied to quantify the effect of the controlling factors on the methane flux. The plant community types differed from each other in their water level, species composition, total leaf area (LAITOT) and leaf area of aerenchymatous plant species (LAIAER). Methane emissions ranged from -309 to 1254 mg m-2 d-1. Although methane fluxes increased with increasing peat temperature, LAITOT and LAIAER, they had no correlation with water table or with plant community type. The only exception was higher fluxes from hummocks and high lawns than from high hummocks and bare peat surfaces in 2013 and from bare peat surfaces than from high hummocks in 2014. Chamber fluxes upscaled to ecosystem level for the peak season were of the same magnitude as the fluxes measured with the eddy covariance (EC) technique. In 2012 and in August 2014 there was a good agreement between the two methods; in 2013 and in July 2014, the chamber fluxes were higher than the EC fluxes. Net fluxes to soil, indicating higher methane oxidation than production, were detected every year and in all community types. Our results underline the importance of both LAIAER and LAITOT in controlling methane fluxes and indicate the need for automatized chambers to reliably capture localized events to support the more robust EC method.

  18. Investigating the internal structure of four Azorean Sphagnum bogs using ground-penetrating radar

    Directory of Open Access Journals (Sweden)

    D. Pereira

    2017-08-01

    Full Text Available This study evaluates the applicability of ground penetrating radar (GPR as a technique for determining the thickness and internal structure of four peat deposits on Terceira Island (Azores archipelago, mid-Atlantic region. The peatlands studied are all Sphagnum mires located above 500 m a.s.l., but they differ hydrogenetically and in their degree of naturalness. Radargrams for all four bogs, obtained using both 100 MHz and 500 MHz GPR antennae, are presented and compared. The radargram data were validated against peat characteristics (bulk density, von Post H, US method obtained by direct sampling (‘open cores’ across the whole peat profile at each site. A scheme of ‘soft scoring’ for degree of naturalness (DN of the peatland was developed and used as an additional validation factor. The GPR data were positively correlated with DN, and relationships between GPR data, peat bulk density and degree of humification (H were also found. From the radargrams it was possible to distinguish the interface between the peat and the mineral substratum as well as some of the internal structure of the peat deposit, and thus to derive the total thickness of the peat deposit and (in some cases the thicknesses of its constituent layers. The first evaluation of the propagation velocity of electromagnetic waves in Azorean peat yielded a value of 0.04 m ns-1 for 100 MHz and 500 MHz radar antennae. For one of the study sites, the GPR data were analysed using GIS software to produce tridimensional models and thus to estimate the volumes of peat layers. This type of analysis has potential utility for quantifying some of the ecosystem services provided by peatlands.

  19. Granulated bog iron ores as sorbents in passive (bio)remediation systems for arsenic removal

    Science.gov (United States)

    Debiec, Klaudia; Rzepa, Grzegorz; Bajda, Tomasz; Uhrynowski, Witold; Sklodowska, Aleksandra; Krzysztoforski, Jan; Drewniak, Lukasz

    2018-03-01

    The main element of PbRS (passive (bio)remediation systems) are sorbents, which act as natural filters retaining heavy metals and carriers of microorganisms involved in water treatment. Thus, the effectiveness of PbRS is determined by the quality of the (ad)sorbents, which should be stable under various environmental conditions, have a wide range of applications and be non-toxic to (micro)organisms used in these systems. Our previous studies showed that bog iron ores (BIOs) meet these requirements. However, further investigation of the physical and chemical parameters of BIOs under environmental conditions is required before their large-scale application in PbRS. The aim of this study was (i) to investigate the ability of granulated BIOs (gBIOs) to remove arsenic from various types of contaminated waters, and (ii) to estimate the application potential of gBIOs in technologies dedicated to water treatment. These studies were conducted on synthetic solutions of arsenic and environmental samples of arsenic contaminated water using a set of adsorption columns filled with gBIOs. The experiments performed in a static system revealed that gBIOs are appropriate arsenic and zinc adsorbent. Dynamic adsorption studies confirmed these results and showed that the actual sorption efficiency of gBIOs depends on the adsorbate concentration and is directly proportional to them. Desorption analysis showed that As-loaded gBIOs are characterized by high chemical stability and they may be reused for the (ad)sorption of other elements, i.e. zinc. It was also shown that gBIOs may be used for remediation of both highly oxygenated waters and groundwater or settling ponds, where the oxygen level is low, as both forms of inorganic arsenic (arsenate and arsenite) were effectively removed. Arsenic concentration after treatment was <100 µg/L, which is below the limit for industrial water.

  20. Granulated Bog Iron Ores as Sorbents in Passive (Bio)Remediation Systems for Arsenic Removal

    Science.gov (United States)

    Debiec, Klaudia; Rzepa, Grzegorz; Bajda, Tomasz; Uhrynowski, Witold; Sklodowska, Aleksandra; Krzysztoforski, Jan; Drewniak, Lukasz

    2018-01-01

    The main element of PbRS (passive (bio)remediation systems) are sorbents, which act as natural filters retaining heavy metals and carriers of microorganisms involved in water treatment. Thus, the effectiveness of PbRS is determined by the quality of the (ad)sorbents, which should be stable under various environmental conditions, have a wide range of applications and be non-toxic to (micro)organisms used in these systems. Our previous studies showed that bog iron ores (BIOs) meet these requirements. However, further investigation of the physical and chemical parameters of BIOs under environmental conditions is required before their large-scale application in PbRS. The aim of this study was (i) to investigate the ability of granulated BIOs (gBIOs) to remove arsenic from various types of contaminated waters, and (ii) to estimate the application potential of gBIOs in technologies dedicated to water treatment. These studies were conducted on synthetic solutions of arsenic and environmental samples of arsenic contaminated water using a set of adsorption columns filled with gBIOs. The experiments performed in a static system revealed that gBIOs are appropriate arsenic and zinc adsorbent. Dynamic adsorption studies confirmed these results and showed, that the actual sorption efficiency of gBIOs depends on the adsorbate concentration and is directly proportional to them. Desorption analysis showed that As-loaded gBIOs are characterized by high chemical stability and they may be reused for the (ad)sorption of other elements, i.e., zinc. It was also shown that gBIOs may be used for remediation of both highly oxygenated waters and groundwater or settling ponds, where the oxygen level is low, as both forms of inorganic arsenic (arsenate and arsenite) were effectively removed. Arsenic concentration after treatment was <100 μg/L, which is below the limit for industrial water. PMID:29616211

  1. Videographic Analysis of Eriophorum Vaginatum Spatial Coverage in an Ombotrophic Bog

    Directory of Open Access Journals (Sweden)

    Margaret Kalacska

    2013-12-01

    Full Text Available The use of Remotely Piloted Aircraft Systems (RPAS as well as newer automated unmanned aerial vehicles is becoming a standard method in remote sensing studies requiring high spatial resolution (<1 m and very precise temporal data to capture phenological events. In this study we use a low cost rotorcraft to map Eriophorum vaginatum at Mer Bleue, an ombrotrophic bog located east of Ottawa, ON, Canada. We focus on E. vaginatum because this sedge plays an important role in methane (CH4 gas exchange in peatlands. Using the remote controlled rotorcraft we were able to record, process, and mosaic 11.1 hectares of 4.5 cm spatial resolution imagery extracted from individual frames of video recordings (post georegistration RMSE 4.90 ± 4.95 cm. Our results, based on a supervised classification (96% accuracy of the red, green, blue image planes, indicate a total tussock cover of 2,417 m2. Because the basal area of the plant is more relevant for calculating its contribution to the CH4 flux, the tussock area was related to the basal area from field data (R2 = 0.88, p < 0.0001. Our final results indicate a total basal area of 1,786 ± 62.8 m2. Based on temporal measurements of CH4 flux from the peatland as a whole that vary over the growing season, we estimate the E. vaginatum contribution to range from 3.0% to 17.3% of that total. Overall, our low cost approach was an effective non-destructive way to derive E. vaginatum coverage and estimate CH4 exchange over the growing season.

  2. Small spatial variability in methane emission measured from a wet patterned boreal bog

    Directory of Open Access Journals (Sweden)

    A. Korrensalo

    2018-03-01

    Full Text Available We measured methane fluxes of a patterned bog situated in Siikaneva in southern Finland from six different plant community types in three growing seasons (2012–2014 using the static chamber method with chamber exposure of 35 min. A mixed-effects model was applied to quantify the effect of the controlling factors on the methane flux. The plant community types differed from each other in their water level, species composition, total leaf area (LAITOT and leaf area of aerenchymatous plant species (LAIAER. Methane emissions ranged from −309 to 1254 mg m−2 d−1. Although methane fluxes increased with increasing peat temperature, LAITOT and LAIAER, they had no correlation with water table or with plant community type. The only exception was higher fluxes from hummocks and high lawns than from high hummocks and bare peat surfaces in 2013 and from bare peat surfaces than from high hummocks in 2014. Chamber fluxes upscaled to ecosystem level for the peak season were of the same magnitude as the fluxes measured with the eddy covariance (EC technique. In 2012 and in August 2014 there was a good agreement between the two methods; in 2013 and in July 2014, the chamber fluxes were higher than the EC fluxes. Net fluxes to soil, indicating higher methane oxidation than production, were detected every year and in all community types. Our results underline the importance of both LAIAER and LAITOT in controlling methane fluxes and indicate the need for automatized chambers to reliably capture localized events to support the more robust EC method.

  3. Granulated Bog Iron Ores as Sorbents in Passive (BioRemediation Systems for Arsenic Removal

    Directory of Open Access Journals (Sweden)

    Klaudia Debiec

    2018-03-01

    Full Text Available The main element of PbRS (passive (bioremediation systems are sorbents, which act as natural filters retaining heavy metals and carriers of microorganisms involved in water treatment. Thus, the effectiveness of PbRS is determined by the quality of the (adsorbents, which should be stable under various environmental conditions, have a wide range of applications and be non-toxic to (microorganisms used in these systems. Our previous studies showed that bog iron ores (BIOs meet these requirements. However, further investigation of the physical and chemical parameters of BIOs under environmental conditions is required before their large-scale application in PbRS. The aim of this study was (i to investigate the ability of granulated BIOs (gBIOs to remove arsenic from various types of contaminated waters, and (ii to estimate the application potential of gBIOs in technologies dedicated to water treatment. These studies were conducted on synthetic solutions of arsenic and environmental samples of arsenic contaminated water using a set of adsorption columns filled with gBIOs. The experiments performed in a static system revealed that gBIOs are appropriate arsenic and zinc adsorbent. Dynamic adsorption studies confirmed these results and showed, that the actual sorption efficiency of gBIOs depends on the adsorbate concentration and is directly proportional to them. Desorption analysis showed that As-loaded gBIOs are characterized by high chemical stability and they may be reused for the (adsorption of other elements, i.e., zinc. It was also shown that gBIOs may be used for remediation of both highly oxygenated waters and groundwater or settling ponds, where the oxygen level is low, as both forms of inorganic arsenic (arsenate and arsenite were effectively removed. Arsenic concentration after treatment was <100 μg/L, which is below the limit for industrial water.

  4. Effects of elevated CO2 and increased N deposition on bog vegetation in the Netherlands = [Gevolgen van een verhoogde atmosferische CO2-concentratie en N-depositie voor hoogveenvegetatie in Nederland

    NARCIS (Netherlands)

    Heijmans, M.M.P.D.

    2000-01-01

    Ombrotrophic bogs are important long-term sinks for atmospheric carbon. Changes in species composition of the bog plant community may have important effects on carbon sequestration, because peat mosses ( Sphagnum ) contribute more to peat accumulation than vascular

  5. Nitrogen and sulphur deposition and the growth of Sphagnum fuscum in bogs of the Athabasca Oil Sands Region, Alberta

    Directory of Open Access Journals (Sweden)

    Melanie A. VILE

    2010-08-01

    Full Text Available One of the consequences of ongoing development of the oil sands reserve in the Athabasca Oil Sands Region (AOSR near Fort McMurray, Alberta, Canada (56° 39' N, 111° 13' W is an increase in emissions of nitrogen (N and sulphur (S, with an attendant increases in regional atmospheric N and S deposition. Regional land cover across northeastern Alberta is a mixture of Boreal Mixedwood, Boreal Highlands, and Subarctic areas. Peatlands occupy between 22 and 66% of these natural regions, and the land cover of bogs varies between 6.7% in the Mixedwood Region to 46% in the Subarctic Region. Ombrotrophic bog ecosystems may be especially sensitive to atmospheric deposition of N and S. Across 10 ombrotrophic bog sites in the AOSR over four years (2005– 2008, we found no evidence of elevated deposition of NH4 +-N, NO3 –-N, total inorganic nitrogen (TIN; NH4 +-N plus NO3 –-N, or SO4 2–-S, with values measured using ion exchange resin collectors averaging 0.61 ± 04, 0.20 ± 0.01, 0.81 ± 0.04, and 1.14 ± 0.06 kg ha–1 y–1, respectively. Vertical growth and net primary production of Sphagnum fuscum, an indicator of elevated deposition, did not differ consistently across sites, averaging 11.8 ± 0.2 mm y–1 and 234 ± 3.3 g m–2 y–1, respectively, over the four years. Neither vertical growth nor net primary production of S. fuscum was correlated with growing season atmospheric N or S deposition. Our data provide a valuable benchmark of background values for monitoring purposes in anticipation of increasing N and S deposition over a broader geographic region within the AOSR.

  6. Intercomparison of radiocarbon bomb pulse and 210Pb age models. A study in a peat bog core from North Poland

    International Nuclear Information System (INIS)

    Piotrowska, Natalia; Vleeschouwer, Francois De; Sikorski, Jaroslaw; Pawlyta, Jacek; Fagel, Nathalie; Roux, Gael Le; Pazdur, Anna

    2010-01-01

    Radiocarbon and 210 Pb were measured on the uppermost 40 cm of a Wardenaar peat core retrieved from a Baltic raised bog at Slowinskie Blota (Pomerania, North Poland). This site is the subject of ongoing multiproxy studies covering the last 1300 years. Radiocarbon age model was constructed on the basis of 14 AMS dates obtained on selected Sphagnum spp. fragments, with use of P S equence tool. We present here a comparison of this model with the age model obtained using CRS model classically applied to 210 Pb measurements.

  7. Radiometric age dating of peat cores from ombrotrophic bogs: challenges and opportunities presented by the Industrial Period

    Science.gov (United States)

    Shotyk, W.; Appleby, P.; Davies, L. J.; Froese, D. G.; Magnan, G.; Mullan-Boudreau, G.; Noernberg, T.; Bob, S.; van Bellen, S.; Zaccone, C.

    2016-12-01

    The upper layers of ombrotrophic (rain-fed) bogs are hydrologically isolated from surface waters and groundwaters and, in consequence, contaminants are supplied exclusively from the atmosphere. Peat cores from bogs have been used to reconstruct the history of heavy metal pollution since mining and metallurgy began, but the greatest changes have taken place since the start of the Industrial Revolution which was well underway by the middle of the 19th century. Dating peat, accumulated since this time has been made possible using 210Pb (t1/2 = 22.3 yr), but the validity of the age-depth relationship obtained must always be assessed using one or more chronostratigraphic markers. The post-industrial period provides an enormous range of possible time markers including various fallout radionuclides, numerous trace metals and their isotopes, and countless organic contaminants. Most of these have not yet been explored, and will be helpful only if they are immobile in the peat column; often, their fate during chemical diagenesis in anoxic, acidic bog waters is either unknown or at least poorly understood. The atmospheric bomb pulse curve of 14C for the period since AD 1950 has proved to be particularly valuable for validating 210Pb chronologies by providing accurate dates for individual plant macrofossils. Peat cores collected in northern Alberta, surrounding open pit mines and upgraders of Athabsca Bituminous Sands, were carefully dated using 210Pb and the age-depth relationship evaluated using both 241Am and 14C. The cores nearest industry (MIL, JPH4) show that atmospheric deposition of trace metals has been declining ever since industrial-scale mining and refining began in 1967. This includes all of the potentially toxic trace elements (Ag, Cd, Pb, Sb, Tl), but also the metals known for their enrichment in bitumen (V, Ni, Mo). In fact, the surface layers of these bogs today are comparable in composition to the "cleanest" peat samples ever found in the northern hemisphere

  8. Atmospheric Pb deposition in Spain during the last 4600 years recorded by two ombrotrophic peat bogs and implications for the use of peat as archive

    Energy Technology Data Exchange (ETDEWEB)

    Martinez Cortizas, A.; Garcia-Rodeja, E.; Pontevedra Pombal, X.; Novoa Munoz, J.C. [Departamento de Edafologia y Quimica Agricola, Faculdad de Biologia, Universidad de Santiago, Campus Sur E-15706, Santiago de Compostela (Spain); Weiss, D. [T.H. Huxley School, Imperial College, Prince Consort Road, SW7 2BP London (United Kingdom); Cheburkin, A. [EMMA Analytical Inc Canada, ON Elmvale (Canada)

    2002-06-20

    Two ombrotrophic peat bogs in Northwestern Spain provided a history of 4600 years of Pb accumulation. Highest Pb concentrations (84-87 {mu}g g{sup -1}) were found near the bogs' surface, but there were also other significant peaks (6-14 {mu}g g{sup -1}), indicating pre-industrial atmospheric pollution. The enrichment factors (EFs) in both cores show a remarkably similar record. Atmospheric Pb pollution dates back to at least approximately 2500 years ago, reaching a first maximum during the Roman period. For the last 300 years, Pb EFs significantly increased due to industrial development, but the uppermost samples of the bogs show decreasing Pb EFs, probably due to the phasing out of leaded gasoline. These results are also supported by 206Pb/207Pb isotope ratios, as they continuously decrease from ca. 3000 BP until 2000 BP (from 1.275 at 4070 14C years BP to 1.182), indicating the growing importance of non-radiogenic Pb released from Iberian ores by ancient mining. Peat samples at a 3-5-cm depth are even less radiogenic (206Pb/107Pb=1.157), indicating the strong influence of leaded gasoline. Despite the common history shared by the two bogs, striking differences were found for Pb enrichment, whether this was calculated by normalising to the Pb/Ti ratio of the upper continental crust or to the Pb/Ti ratios of peats from pre-anthropogenic times. This effect seems to be related to differences in Ti accumulation in both bogs, possibly due to physical fractionation of the airborne dust during wind transport. Enrichment has to be carefully considered when comparing the results obtained for different bogs, since our results suggest that normalising to crustal proportions is meaningless when the bulk of the deposition in an area is strongly influenced by short- and medium-range dust transport.

  9. Soil-to-plant transfer of 137Cs and 40K in an Atlantic blanket bog ecosystem

    International Nuclear Information System (INIS)

    Moran-Hunter, C.; O'Dea, J.

    2008-01-01

    The transfer of 137 Cs and 40 K from soil to vegetation was studied in an Atlantic blanket bog ecosystem along the Atlantic coast of Ireland where the dominant vegetation is a mixture of Calluna vulgaris, Eriophorum vaginatum and Sphagnum mosses. The impact of soil chemistry and nutritional status of vegetation on the uptake of both radionuclides was also examined. Cesium-137 transfer factors values ranged from 1.9 to 9.6 and accumulation of 137 Cs was higher in the leaves of C. vulgaris than in the stems. Transfer factors values for 137 Cs in both C. vulgaris and E. vaginatum were similar indicating that for the vegetation studied, uptake is not dependent on plant species. The uptake of 137 Cs in bog vegetation was found to be positively correlated with the nutrient status of vegetation, in particular the secondary nutrients, calcium and magnesium. Potassium-40 transfer factors ranged from 0.9 to 13.8 and uptake was higher in E. vaginatum than in C. vulgaris, however, unlike 137 Cs, the concentrations of 40 K within the leaves and stems of C. vulgaris were similar. The concentration of both 137 Cs and 40 K found in moss samples were in general lower than those found in vascular plants. (author)

  10. Sphagnum mosses from 21 ombrotrophic bogs in the athabasca bituminous sands region show no significant atmospheric contamination of "heavy metals".

    Science.gov (United States)

    Shotyk, William; Belland, Rene; Duke, John; Kempter, Heike; Krachler, Michael; Noernberg, Tommy; Pelletier, Rick; Vile, Melanie A; Wieder, Kelman; Zaccone, Claudio; Zhang, Shuangquan

    2014-11-04

    Sphagnum moss was collected from 21 ombrotrophic (rain-fed) peat bogs surrounding open pit mines and upgrading facilities of Athabasca bituminous sands in Alberta (AB). In comparison to contemporary Sphagnum moss from four bogs in rural locations of southern Germany (DE), the AB mosses yielded lower concentrations of Ag, Cd, Ni, Pb, Sb, and Tl, similar concentrations of Mo, but greater concentrations of Ba, Th, and V. Except for V, in comparison to the "cleanest", ancient peat samples ever tested from the northern hemisphere (ca. 6000-9000 years old), the concentrations of each of these metals in the AB mosses are within a factor of 3 of "natural, background" values. The concentrations of "heavy metals" in the mosses, however, are proportional to the concentration of Th (a conservative, lithophile element) and, therefore, contributed to the plants primarily in the form of mineral dust particles. Vanadium, the single most abundant trace metal in bitumen, is the only anomaly: in the AB mosses, V exceeds that of ancient peat by a factor of 6; it is therefore enriched in the mosses, relative to Th, by a factor of 2. In comparison to the surface layer of peat cores collected in recent years from across Canada, from British Columbia to New Brunswick, the Pb concentrations in the mosses from AB are far lower.

  11. [Isolation and characterization of nitrogen-fixing bacteria of the genus Azospirillum from the soil of a Sphagnum peat bog].

    Science.gov (United States)

    Doroshenko, E V; Bulygina, E S; Spiridonova, E M; Turova, T P; Kravchenko, I K

    2007-01-01

    The presence of nitrogen-fixing bacteria of the genus Azospirillum in the soils of acidic raised Sphagnum bogs is revealed for the first time. Three Azospirillum strains, B2, B21, and B22, were isolated as a component of methane-oxidizing enrichment cultures, whereas attempts to isolate them directly from peat samples have failed. The results of comparative analysis of the nucleotide sequences of 16S rRNA genes, DNA-DNA hybridization, and the analysis of the sequences of the functional genes encoding nitrogenase and ribulose-1, 5-bisphosphate carboxylase reveal that all the newly obtained strains can be classified as Azospirillum lipoferum. Yet, unlike A. lipoferum. the isolates do not require biotin and utilize sucrose, inositol, and glycerol for growth. The cell morphology of strain B2 differs from that of the type strain and strains B21 and B22. The results obtained indicate the variability of morphological, physiological, and biochemical properties in closely related Azospirillum strains and suggest the existence of metabolic relationships between methanotrophic bacteria and the representatives of the genus Azospirillum under peat bog conditions.

  12. Ebullition, Plant-Mediated Transport, and Subsurface Horizontal Water Flow Dominate Methane Transport in an Arctic Sphagnum Bog

    Science.gov (United States)

    Wehr, R. A.; McCalley, C. K.; Logan, T. A.; Chanton, J.; Crill, P. M.; Rich, V. I.; Saleska, S. R.

    2017-12-01

    Emission of the greenhouse gas methane from wetlands is of prime concern in the prediction of climate change - especially emission associated with thawing permafrost, which may drive a positive feedback loop of emission and warming. In addition to the biochemistry of methane production and consumption, wetland methane emission depends critically on the transport mechanisms by which methane moves through and out of the ecosystem. We therefore developed a model of methane biochemistry and transport for a sphagnum bog representing an intermediate permafrost thaw stage in Stordalen Mire, Sweden. In order to simultaneously reproduce measured profiles of both the concentrations and isotopic compositions of both methane and carbon dioxide in the peat pore water (Fig. 1) - as well as the surface methane emission - it was necessary for the model to include ebullition, plant-mediated transport via aerenchyma, and subsurface horizontal water flow. Diffusion of gas through the pore water was relatively unimportant. As a result, 90% of the produced methane escaped the wetland rather than being consumed by methanotrophic organisms in the near-surface pore water. Our model provides a comprehensive picture of methane emission from this bog site by quantifying the vertical profiles of: acetoclastic methanogenesis, hydrogenotrophic methanogenesis, methane oxidation, aerobic respiration, ebullition, plant-mediated transport, subsurface horizontal water flow, and diffusion.

  13. Net ecosystem exchange and energy fluxes measured with the eddy covariance technique in a western Siberian bog

    Science.gov (United States)

    Alekseychik, Pavel; Mammarella, Ivan; Karpov, Dmitry; Dengel, Sigrid; Terentieva, Irina; Sabrekov, Alexander; Glagolev, Mikhail; Lapshina, Elena

    2017-08-01

    Very few studies of ecosystem-atmosphere exchange involving eddy covariance data have been conducted in Siberia, with none in the western Siberian middle taiga. This work provides the first estimates of carbon dioxide (CO2) and energy budgets in a typical bog of the western Siberian middle taiga based on May-August measurements in 2015. The footprint of measured fluxes consisted of a homogeneous mixture of tree-covered ridges and hollows with the vegetation represented by typical sedges and shrubs. Generally, the surface exchange rates resembled those of pine-covered bogs elsewhere. The surface energy balance closure approached 100 %. Net CO2 uptake was comparatively high, summing up to 202 gC m-2 for the four measurement months, while the Bowen ratio was seasonally stable at 28 %. The ecosystem turned into a net CO2 source during several front passage events in June and July. The periods of heavy rain helped keep the water table at a sustainably high level, preventing a usual drawdown in summer. However, because of the cloudy and rainy weather, the observed fluxes might rather represent the special weather conditions of 2015 than their typical magnitudes.

  14. Contrasting species-environment relationships in communities of testate amoebae, bryophytes and vascular plants along the fen-bog gradient.

    Science.gov (United States)

    Lamentowicz, Mariusz; Lamentowicz, Lukasz; van der Knaap, Willem O; Gabka, Maciej; Mitchell, Edward A D

    2010-04-01

    We studied the vegetation, testate amoebae and abiotic variables (depth of the water table, pH, electrical conductivity, Ca and Mg concentrations of water extracted from mosses) along the bog to extremely rich fen gradient in sub-alpine peatlands of the Upper Engadine (Swiss Alps). Testate amoeba diversity was correlated to that of mosses but not of vascular plants. Diversity peaked in rich fen for testate amoebae and in extremely rich fen for mosses, while for testate amoebae and mosses it was lowest in bog but for vascular plants in extremely rich fen. Multiple factor and redundancy analyses (RDA) revealed a stronger correlation of testate amoebae than of vegetation to water table and hydrochemical variables and relatively strong correlation between testate amoeba and moss community data. In RDA, hydrochemical variables explained a higher proportion of the testate amoeba and moss data than water table depth. Abiotic variables explained a higher percentage of the species data for testate amoebae (30.3% or 19.5% for binary data) than for mosses (13.4%) and vascular plants (10%). These results show that (1) vascular plant, moss and testate amoeba communities respond differently to ecological gradients in peatlands and (2) testate amoebae are more strongly related than vascular plants to the abiotic factors at the mire surface. These differences are related to vertical trophic gradients and associated niche differentiation.

  15. Features of seasonal temperature variations in peat soils of oligotrophic bogs in south taiga of Western Siberia

    Science.gov (United States)

    Kiselev, M. V.; Dyukarev, E. A.; Voropay, N. N.

    2018-03-01

    The work presents the results of the study of the peculiarities of the temperature regime in the five basic ecosystems of oligotrophic bogs in the south taiga zone of Western Siberia in 2011-2016. The soil temperature regime was studied using the atmospheric-soil measuring complex at different depths from surface down to 240 cm. All sites were divided into two groups according to the bog water level: flooded sites (hollow and open fen) and drained sites (ridge, tall and low ryam). The waterlogged sites are better warmed in the summer period and slowly freeze in the winter period. The analysis of the annual cycle of temperature showed that the maximum surface temperature is in July. The minimum temperature on the surface is observed in February or January. The greatest temperature gradient was recorded in the upper 2 cm layer. The gradient at the open fen was -2 °C/cm in February and 1.1 °C/cm in October. The peak of formation of the seasonally frozen layer occurs at the end of autumn or in the beginning of winter. The degradation of the seasonally frozen layer was observed both from top and bottom, but the degradation rate from the top is faster.

  16. Altitude or slope position - gaseous carbon cycling on UK blanket peat bogs

    Science.gov (United States)

    Dixon, Simon; Rowson, James; Worrall, Fred

    2010-05-01

    Blanket peat accounts for 87% of Britain's total peatlands and represents one of the UK's largest terrestrial carbon stores. For peatlands to accumulate carbon the net ecosystem exchange of CO2 (NEE) must be negative with respect to the atmosphere. Unlike many other peatlands, upland blanket peat bogs in the UK are draped across hillsides and so it could be that both altitude and slope position are significant controls upon the magnitude and direction of NEE. The role that altitude and slope position play on NEE in upland blanket peat is poorly constrained on a local scale. Thus a hillslope transect was set up to measure how the gaseous exchange of CO2 varies across altitude and with slope position. The slope-transect consisted of 4 sites, in the English Peak District, with three replicates per site. The transect spanned the entire margin of peat occurrence on the hillside, from the summit (447m ASL) to the lowest occurrence of peat at (378m ASL). The sites were positioned to sample each of the distinct points of the variation in slope from the flat top, to the point of slope steepening, to the point of slope leveling to the final flattening out of the slope. Each site was located in Calluna vulgaris of similar age and in the same growth phase (degenerate). Data were gathered for a year in order to sample a complete seasonal cycle. The results of analysis by ANOVA showed that altitudinal effects were either not present or so small as to be masked by other effects. However both NER and GPP seemed to be linked to slope position. ANOVA and post hoc Tukey testing showed that only the site on the point of slope steepening was significantly different to the other sites with NER being 47% higher and GPP being 63% greater than the average of the other sites. But the elevated rates of GPP and NER cancelled each other out resulting in a non-significant 3% greater rate of overall NEE from the point of slope steepening. Another slope position effect observed was that of hill

  17. Historical accumulation rates of mercury in four Scottish ombrotrophic peat bogs over the past 2000 years

    Energy Technology Data Exchange (ETDEWEB)

    Farmer, John G., E-mail: J.G.Farmer@ed.ac.uk [School of GeoSciences, University of Edinburgh, Edinburgh, EH9 3JN, Scotland (United Kingdom); Anderson, Peter [Contaminated Land Assessment and Remediation Research Centre, University of Edinburgh, Edinburgh, EH9 3JL, Scotland (United Kingdom); Cloy, Joanna M.; Graham, Margaret C. [School of GeoSciences, University of Edinburgh, Edinburgh, EH9 3JN, Scotland (United Kingdom); MacKenzie, Angus B.; Cook, Gordon T. [Scottish Universities Environmental Research Centre, East Kilbride, G75 0QF, Scotland (United Kingdom)

    2009-10-15

    The historical accumulation rates of mercury resulting from atmospheric deposition to four Scottish ombrotrophic peat bogs, Turclossie Moss (northeast Scotland), Flanders Moss (west-central), Red Moss of Balerno (east-central) and Carsegowan Moss (southwest), were determined via analysis of {sup 210}Pb- and {sup 14}C-dated cores up to 2000 years old. Average pre-industrial rates of mercury accumulation of 4.5 and 3.7 {mu}g m{sup -2} y{sup -1} were obtained for Flanders Moss (A.D. 1-1800) and Red Moss of Balerno (A.D. 800-1800), respectively. Thereafter, mercury accumulation rates increased to typical maximum values of 51, 61, 77 and 85 {mu}g m{sup -2} y{sup -1}, recorded at different times possibly reflecting local/regional influences during the first 70 years of the 20th century, at the four sites (TM, FM, RM, CM), before declining to a mean value of 27 {+-} 15 {mu}g m{sup -2} y{sup -1} during the late 1990s/early 2000s. Comparison of such trends for mercury with those for lead and arsenic in the cores and also with direct data for the declining UK emissions of these three elements since 1970 suggested that a substantial proportion of the mercury deposited at these sites over the past few decades originated from outwith the UK, with contributions to wet and dry deposition arising from long-range transport of mercury released by sources such as combustion of coal. Confidence in the chronological reliability of these core-derived trends in absolute and relative accumulation of mercury, at least since the 19th century, was provided by the excellent agreement between the corresponding detailed and characteristic temporal trends in the {sup 206}Pb/{sup 207}Pb isotopic ratio of lead in the {sup 210}Pb-dated Turclossie Moss core and those in archival Scottish Sphagnum moss samples of known date of collection. The possibility of some longer-term loss of volatile mercury released from diagenetically altered older peat cannot, however, be excluded by the findings of this

  18. Biogeochemical indicators of peatland degradation - a case study of a temperate bog in northern Germany

    Science.gov (United States)

    Krüger, J. P.; Leifeld, J.; Glatzel, S.; Szidat, S.; Alewell, C.

    2014-12-01

    Peatlands store a great proportion of the global soil carbon pool and can loose carbon via the atmosphere due to degradation. In Germany, most of the greenhouse gas emissions from organic soils are attributed to sites managed as grassland. Here we investigated a land-use gradient from near-natural wetland (NW) to an extensively managed (GE) to an intensively managed grassland site (GI), all formed in the same bog complex in northern Germany. Vertical depth profiles of δ13C, δ15N, ash content, C/N ratio, bulk density, as well as radiocarbon ages were studied to identify peat degradation and to calculate carbon loss. At all sites, including the near-natural site, δ13C depth profiles indicate aerobic decomposition in the upper horizons. Depth profiles of δ15Ndiffered significantly between sites with increasing δ15N values in the top layers with increasing intensity of use, indicating that the peat is more decomposed. At both grassland sites, the ash content peaked within the first centimeter. In the near-natural site, ash contents were highest in 10-60 cm depth. This indicates that not only the managed grasslands, but also the near-natural site, is influenced by anthropogenic activities, most likely due to the drainage of the surrounding area. However, we found very young peat material in the first centimeter of the NW, indicating recent peat growth. The NW site accumulates carbon today even though it is and probably was influenced by anthropogenic activities in the past indicated by δ13C and ash content depth profiles. Based on the enrichment of ash content and changes in bulk density, we calculated carbon loss from these sites in retrograde. As expected land use intensification leads to a higher carbon loss which is supported by the higher peat ages at the intensive managed grassland site. All investigated biogeochemical parameters together indicate degradation of peat due to (i) conversion to grassland, (ii) historical drainage as well as recent development

  19. Formation, succession and landscape history of Central-European summit raised bogs: A multiproxy study from the Hrubý Jeseník Mountains

    Czech Academy of Sciences Publication Activity Database

    Dudová, Lydie; Hájková, Petra; Buchtová, H.; Opravilová, V.

    2013-01-01

    Roč. 23, č. 2 (2013), s. 230-242 ISSN 0959-6836 R&D Projects: GA ČR GA206/08/0389 Institutional support: RVO:67985939 Keywords : bog succession * Larix * testate amoebae Subject RIV: EF - Botanics Impact factor: 3.794, year: 2013

  20. Rates and Controls of N2 Fixation in Sphagnum spp. along the Hydrological Gradient - Beaver Pond to Bog Transition at Mer Bleue, Ontario, Canada

    Science.gov (United States)

    Zivkovic, T.; Moore, T. R.

    2014-12-01

    Many northern bogs with low atmospheric N inputs acquire N only via N2-fixation. Little is known about rates and controls on N2-fixation in bogs. The aim of this study was to: 1) test the important ecological drivers for N2-fixation, 2) investigate seasonal and temporal patterns of N2 fixation, and 3) to estimate current N2-fixation rates at Mer Bleue bog. We used acetylene reduction assay (ARA) to measure N2-fixation from June-October 2013 and 2014 (currently ongoing field season) along a hydrological gradient (beaver pond, hollows and hummocks). The highest ARA rates in 2013 growing season occurred in the pond in floating Sphagnum cuspidatum mats (50.3 ± 12.9 μmol m-2 d-1 Mean ± Std Err) which were up to 2.5 times latger than the rates found in the hummock with the lowest water table depth throughout the season. Two rain events during the summer 2013 increased ARA rates in all plots by 1 to 4 times, suggesting that moisture availability may play a crucial role on N2 fixation potential in the field. We are currently investigating the role of moisture, temperature, PAR and nutrient content (N, phosphorous and metals) on ARA along the gradient. In addition, we are using 15N2 enrichment method to estimate N2 fixation rates and compare them to ARA method at Mer Bleue bog.

  1. Plant component features of forest-bog ecotones of eutrophic paludification in the south of boreal forest zone of West Siberia

    Science.gov (United States)

    Klimova, N. V.; Chernova, N. A.; Pologova, N. N.

    2018-03-01

    Paludified forests formed in transitional forest-bog zone aren’t studied enough, inspite of its high expected diversity and large areas in the south of boreal forest zone of West Siberia. In this article wet birch (Betula pubescens) forests of forest-bog ecotones of eutrophic paludification are investigated on Vasyugan plain with nutrient-rich calcareous clays as soil-forming rocks. Species diversity and ecocoenotic structure of these phytocoenoses are discussed. They correlated with wetness and nutrient-availability of habitats evaluated with indicator values of plants. The participation of hydrophylous species is increasing as wetness of habitats increasing in the forest-to-bog direction like in mesotrophic paludification series. However the number of species is higher in the phytocoenoses of eutrophic paludification. The share of species required to nutrient availability is also higher, both in number and in abundance. A lot of these species are usual for eutrophic boreal forested swamps with groundwater input and absent in forests of mesotrophic paludification. Accordingly the nutrient-availability of habitats is also higher. All these features we connect with birch to be a forest forming species instead of dark-coniferous and with the influence of nutrient-rich parent rocks, which is evident in forest-bog ecotones of Vasyugan plain gradually decreasing together with peat horizon thickening.

  2. Differential effects of high atmospheric N and S deposition on bog plant/lichen tissue and porewater chemistry across the Athabasca Oil Sands Region

    Science.gov (United States)

    R. Kelman Wieder; Melanie A. Vile; Kimberli D. Scott; Cara M. Albright; Kelly J. McMillen; Dale H. Vitt; Mark E. Fenn

    2016-01-01

    Oil extraction and development activities in the Athabasca Oil Sands Region of northern Alberta, Canada, release NOx, SOx, and NHy to the atmosphere, ultimately resulting in increasing N and S inputs to surrounding ecosystems through atmospheric deposition. Peatlands are a major feature of the northern Alberta landscape, with bogs covering 6-10% of the land area, and...

  3. Predominant anthropogenic sources and rates of atmospheric mercury accumulation in southern Ontario recorded by peat cores from three bogs: comparison with natural "background" values (past 8000 years).

    Science.gov (United States)

    Givelet, Nicolas; Roos-Barraclough, Fiona; Shotyk, William

    2003-12-01

    Peat cores from three bogs in southern Ontario provide a complete, quantitative record of net rates of atmospheric Hg accumulation since pre-industrial times. For comparison with modern values, a peat core extending back 8000 years was used to quantify the natural variations in Hg fluxes for this region, and their dependence on climatic change and land use history. The net mercury accumulation rates were separated into "natural" and "excess" components by comparing the Hg/Br ratios of modern samples with the long-term, pre-anthropogenic average Hg/Br. The average background mercury accumulation rate during the pre-anthropogenic period (from 5700 years BC to 1470 AD) was 1.4 +/- 1.0 microg m(-2) per year (n = 197). The beginning of Hg contamination from anthropogenic sources dates from AD 1475 at the Luther Bog, corresponding to biomass burning for agricultural activities by Native North Americans. During the late 17th and 18th centuries, deposition of anthropogenic Hg was at least equal to that of Hg from natural sources. Anthropogenic inputs of Hg to the bogs have dominated continuously since the beginning of the 19th century. The maximum Hg accumulation rates decrease in the order Sifton Bog, in the City of London, Ontario (141 microg Hg m(-2) per year), Luther Bog in an agricultural region (89 microg Hg m(-2) per year), and Spruce Bog which is in a comparatively remote, forested region (54 microg Hg m(-2) per year). Accurate age dating of recent peat samples using the bomb pulse curve of 14C shows that the maximum rate of atmospheric Hg accumulation occurred during AD 1956 and 1959 at all sites. In these (modern) samples, the Hg concentration profiles resemble those of Pb, an element which is known to be immobile in peat bogs. The correlation between these two metals, together with sulfur, suggests that the predominant anthropogenic source of Hg (and Pb) was coal burning. While Hg accumulation rates have gone into strong decline since the late 1950's, Hg

  4. Holocene climate variability in the western Mediterranean through a multiproxy analysis from Padul peat bog (Sierra Nevada, Spain)

    Science.gov (United States)

    Ramos-Román, María J.; Jiménez-Moreno, Gonzalo; Camuera, Jon; García-Alix, Antonio; Anderson, R. Scott; Jiménez-Espejo, Francisco J.; Sachse, Dirk

    2017-04-01

    The Iberian Peninsula, located in the Mediterranean area, is an interesting location for paleoclimate studies due to its geographic situation between arid and humid climates. Sediments from peat bogs and lakes from Sierra Nevada, in southeastern Iberian Peninsula, have been very informative in terms of how vegetation and wetland environments were impacted by Holocene climate change. These studies are essential if we want to understand the past climate change in the area, which is the key to identify the possible environmental response of the Sierra Nevada ecosystems to future climate scenarios. Padul basin, located in the southwest of the Sierra Nevada mountain range, contains a ca. 100 m-thick peat bog sedimentary sequence that was deposited during the past 1 Ma making this area interesting for paleoenvironmental and paleoclimatic reconstructions. A new 43 m-long sedimentary record has recently been retrieved from the Padul peat bog. In this study we have developed a multiproxy analysis of the Holocene part of the Padul-15-05 core including pollen analysis, XRF-core scanner, magnetic susceptibility and organic geochemistry, supported by an age control based on AMS radiocarbon dates, providing with information about vegetation and climate variability during the past 9.9 cal ka BP. This multiproxy reconstruction of the Padul-15-05 evidences the Mediterranean as a sensitive area with respect to global-scale climate system, showing relevant climate episodes such as the ca. 8, 7.5, 6.5 and 5.5 cal ka BP events during the early and middle Holocene. The trend to aridification to the late Holocene is interrupted by more arid and humid periods as the Iberian Roman Humid Period (from ca. 3 to 1.6 cal ka BP), the Dark Ages (from ca. 1.5 to 1.1 cal ka BP), the Medieval Climate Anomaly (from ca. 1.1 to 1.3 cal ka BP) and the Little Ice Age period (from ca. 500 to 100 cal yr BP).

  5. Experimental warming delays autumn senescence in a boreal spruce bog: Initial results from the SPRUCE experiment

    Science.gov (United States)

    Richardson, Andrew; Furze, Morgan; Aubrecht, Donald; Milliman, Thomas; Nettles, Robert; Krassovski, Misha; Hanson, Paul

    2016-04-01

    Phenology is considered one of the most robust indicators of the biological impacts of global change. In temperate and boreal regions, long-term data show that rising temperatures are advancing spring onset (e.g. budburst and flowering) and delaying autumn senescence (e.g. leaf coloration and leaf fall) in a wide range of ecosystems. While warm and cold temperatures, day length and insolation, precipitation and water availability, and other factors, have all been shown to influence plant phenology, the future response of phenology to rising temperatures and elevated CO2 still remains highly uncertain because of the challenges associated with conducting realistic manipulative experiments to simulate future environmental conditions. At the SPRUCE (Spruce and Peatland Responses Under Climatic and Environmental Change) experiment in the north-central United States, experimental temperature (0 to +9° C above ambient) and CO2 (ambient and elevated) treatments are being applied to mature, and intact, Picea mariana-Sphagnum spp. bog communities in their native habitat through the use of ten large (approximately 12 m wide, 10 m high) open-topped enclosures. We are tracking vegetation green-up and senescence in these chambers, at both the individual and whole-community level, using repeat digital photography. Within each chamber, digital camera images are recorded every 30 minutes and uploaded to the PhenoCam (http://phenocam.sr.unh.edu) project web page, where they are displayed in near-real-time. Image processing is conducted nightly to extract quantitative measures of canopy color, which we characterize using Gcc, the green chromatic coordinate. Data from a camera mounted outside the chambers (since November 2014) indicate strong seasonal variation in Gcc for both evergreen shrubs and trees. Shrub Gcc rises steeply in May and June, and declines steeply in September and October. By comparison, tree Gcc rises gradually from March through June, and declines gradually from

  6. Flexibility instead of regulation. Is the Energy Transition bogged down?; Flexibilitaet statt Regulierung. Ist die Energiewende festgefahren?

    Energy Technology Data Exchange (ETDEWEB)

    Gochermann, Josef [Hochschule Osnabrueck, Lingen (Germany). Professur Marketing und Technologiemanagement

    2017-07-15

    The growth in renewable energy systems is stagnating. Is the energy transition bogged down? Is the transition to the new energy world over-regulated? In addition to the regulation of the large systems at the national level, the energy users need more scope and flexibility at regional and on individual level. The present article deals with the most important criticisms regarding the energy transition and provides references on their solution. [German] Der Zuwachs an erneuerbaren Energieanlagen stagniert. Ist die Energiewende festgefahren? Wird der Uebergang in die neue Energiewelt ueberreguliert? Neben der Regulation der grossen Systeme auf nationaler Ebene braucht die Energiewende mehr Freiraum und Flexibilitaet auf regionaler und auf individualer Ebene. Der vorliegende Artikel greift die wichtigsten Kritikpunkte in Bezug auf die Energiewende auf und gibt Hinweise zu deren Loesung.

  7. Dendrochronological assessment and radiocarbon dating of subfossil coniferous macroremains excavated from a peat bog, Maramures Mts, Romania

    Directory of Open Access Journals (Sweden)

    Matyas ÁRVAI

    2014-11-01

    Full Text Available Fifty-six subfossil samples have been collected from a peat bog located on the Vinderel plateau, Farcău massif, Maramureș Mountains (Romania. The majority of wood-remains are Norway spruce (Picea abies and Silver fir (Abies alba. The samples have been subjected to dendrochronological analysis and 7 samples were selected for AMS radiocarbon analysis. Seven floating chronologies have been developed from these subfossil samples, so far. The longest floating chronology contains 166 years and the shortest spans 47 years. Radiocarbon age obtained for the oldest and youngest samples are 1717 ± 19 yr 14C BP (255 – 388 cal AD and 1039 ± 16 yr 14C BP (985 – 1023 cal AD, respectively.

  8. Atmospheric pollutants in alpine peat bogs record a detailed chronology of industrial and agricultural development on the Australian continent.

    Science.gov (United States)

    Marx, Samuel K; Kamber, Balz S; McGowan, Hamish A; Zawadzki, Atun

    2010-05-01

    Two peat bogs from remote alpine sites in Australia were found to contain detailed and coherent histories of atmospheric metal pollution for Pb, Zn, Cu, Mo, Ag, As, Cd, Sb, Zn, In, Cr, Ni, Tl and V. Dramatic increases in metal deposition in the post-1850 AD portion of the cores coincide with the onset of mining in Australia. Using both Pb isotopes and metals, pollutants were ascribed to the main atmospheric pollution emitting sources in Australia, namely mining and smelting, coal combustion and agriculture. Results imply mining and metal production are the major source of atmospheric metal pollution, although coal combustion may account for up to 30% of metal pollutants. A novel finding of this study is the increase in the otherwise near-constant Y/Ho ratio after 1900 AD. We link this change to widespread and increased application of marine phosphate fertiliser in Australia's main agricultural area (the Murray Darling Basin). Copyright 2009 Elsevier Ltd. All rights reserved.

  9. History of atmospheric deposition of Cd, Hg, and Pb in North America: Evidence from lake and peat bog sediments

    International Nuclear Information System (INIS)

    Norton, S.A.; Dillon, P.J.; Evans, R.D.; Mierle, G.; Kahl, J.S.

    1990-01-01

    The precipitation chemistry and lake and peat sediment chemistry of three metals emitted to the atmosphere in significant amounts as a result of anthropogenic activity are reviewed. The three metals, Cd, Hg, and Pb, have contrasting source terms, atmospheric residence times, and chemical mobility. Lake and ombrotrophic peat bog sediments record increases in the concentrations and accumulation rates of the metals for most of temperate North America for the last 100 years. These increases are largely related to the burning of coal, smelting of nonferrous metals, the transportation industry, and the industrial production of chlorine. Modern atmospheric fluxes of Cd in central North America are about 1,000 times background fluxes; accumulation rates for Cd in sediments have increased two to 3 times above background, beginning about 100 years ago. Global scale Hg pollution off the atmosphere is suggested by concentrations in northern hemisphere air that are double the Hg content of southern hemisphere air. Accumulation rates of Hg in sediment have approximately doubled in the last 100 years. However, these rates are approximately an order of magnitude less than those for Cd. Modern increases in Pb concentrations are ubiquitous for all lakes examines thus far in North America. Input is from multiple sources and thus the timing of increased accumulation rates in sediment varies across the continent. Typical modern accumulation rates reach maxima at 20 to 30 mg/sq-m/yr, or 100 times that of Cd and 1,000 times that off Hg. Recent decreases in atmospheric lead are reflected in decreases in the accumulation rate of Pb in both lake and peat bog sediment in eastern North America

  10. Multi-scale hydroclimate reconstruction using co-located lake and bog records from Maine and comparison with other records from the Northeast US

    Science.gov (United States)

    Nolan, C.; Shuman, B. N.; Booth, R.; Jackson, S. T.

    2015-12-01

    Sedimentary lake-level records and ombrotrophic bog water-table depth records both document hydrologic variability over the Holocene. Lake level records have long temporal length (10,000+ years) and fidelity in preserving low-frequency trends and centennial to millennial length events. Hydrologic reconstructions based on peatland testate amoebae assemblage composition are sensitive to moisture variability at interannual to multidecadal time scales and precipitation on the bog surface is the sole moisture input. However, bog records are generally not as long as lake level records and bog development processes can confound centennial to millennial trends. In this study we present and combine new reconstructions from Giles Pond, Aurora, Maine, USA and Caribou Bog, Old Town, ME USA. The lake-level record from Giles Pond extends a network of lake-level records from southern New England that show an orbitally driven long-term trend toward wetter conditions punctuated by low-water phases in the mid- to late-Holocene that each lasted 100 to 400+ years. Some of these low lake level events appear to be synchronous across multiple sites in New England (Newby, et al. 2014 GRL). Preliminary data from Giles Pond suggest that some of these events extended all the way to Maine. Thus, there were New England-wide dry periods within the last 5000 years that lasted more than 100 years. These long low stands are unlike anything observed during the historical period and the interannual to decadal variability during these low stands is poorly understood. This leads to challenges in understanding the modern and future implications of the lake-level record alone. The Caribou Bog record also builds on a network of peatland water-table reconstructions from the Northeast, and contributes higher-resolution hydroclimate information that adds interannual to multidecadal texture to the centennial to millennial variability of the Giles Pond record. Our multiproxy approach allows us to use the

  11. Denitrification at two nitrogen-polluted, ombrotrophic Sphagnum bogs in Central Europe: Insights from porewater N2O-isotope profiles

    Czech Academy of Sciences Publication Activity Database

    Novák, M.; Gebauer, G.; Thoma, M.; Curik, J.; Štěpánová, M.; Jacková, I.; Buzek, F.; Bárta, J.; Santrucková, H.; Fottová, D.; Kuběna, Aleš Antonín

    2015-01-01

    Roč. 81, č. 1 (2015), s. 48-57 ISSN 0038-0717 Grant - others:GA ČR(CZ) GAP504/12/1782 Institutional support: RVO:67985556 Keywords : Denitrification * Nitrogen isotopes * Nitrous oxide * Ombrotrophic bog * Porewater * Sphagnum * Wetland * Engineering controlled terms * Meteorological problems Subject RIV: DD - Geochemistry Impact factor: 4.152, year: 2015 http://library.utia.cas.cz/separaty/2015/E/kubena-0439538.pdf

  12. Greenhouse gas exchange of rewetted bog peat extraction sites and a Sphagnum cultivation site in northwest Germany

    Science.gov (United States)

    Beyer, C.; Höper, H.

    2015-04-01

    During the last decades an increasing area of drained peatlands has been rewetted. Especially in Germany, rewetting is the principal treatment on cutover sites when peat extraction is finished. The objectives are bog restoration and the reduction of greenhouse gas (GHG) emissions. The first sites were rewetted in the 1980s. Thus, there is a good opportunity to study long-term effects of rewetting on greenhouse gas exchange, which has not been done so far on temperate cutover peatlands. Moreover, Sphagnum cultivating may become a new way to use cutover peatlands and agriculturally used peatlands as it permits the economical use of bogs under wet conditions. The climate impact of such measures has not been studied yet. We conducted a field study on the exchange of carbon dioxide, methane and nitrous oxide at three rewetted sites with a gradient from dry to wet conditions and at a Sphagnum cultivation site in NW Germany over the course of more than 2 years. Gas fluxes were measured using transparent and opaque closed chambers. The ecosystem respiration (CO2) and the net ecosystem exchange (CO2) were modelled at a high temporal resolution. Measured and modelled values fit very well together. Annually cumulated gas flux rates, net ecosystem carbon balances (NECB) and global warming potential (GWP) balances were determined. The annual net ecosystem exchange (CO2) varied strongly at the rewetted sites (from -201.7 ± 126.8 to 29.7± 112.7g CO2-C m-2 a-1) due to differing weather conditions, water levels and vegetation. The Sphagnum cultivation site was a sink of CO2 (-118.8 ± 48.1 and -78.6 ± 39.8 g CO2-C m-2 a-1). The annual CH4 balances ranged between 16.2 ± 2.2 and 24.2 ± 5.0g CH4-C m-2 a-1 at two inundated sites, while one rewetted site with a comparatively low water level and the Sphagnum farming site show CH4 fluxes close to 0. The net N2O fluxes were low and not significantly different between the four sites. The annual NECB was between -185.5 ± 126.9 and 49

  13. Greenhouse gas emissions from rewetted bog peat extraction sites and a Sphagnum cultivation site in Northwest Germany

    Science.gov (United States)

    Beyer, C.; Höper, H.

    2014-03-01

    During the last three decades, an increasing area of drained peatlands was rewetted. This was done with the objective to convert these sites from sources back to sinks or, at least, to much smaller sources of greenhouse gases (GHG). However, available data is still scarce, especially on the long-term climatic effects of rewetting of temperate bogs. Moreover, first field trials are established for Sphagnum cultivating (paludiculture) on wet bog sites and an assessment of the climate impact of such measures has not been studied yet. We conducted a field study on the exchange of carbon dioxide, methane and nitrous oxide at three rewetted sites with a gradient from dry to wet conditions and at a Sphagnum cultivation site in NW Germany over more than two years. Gas fluxes were measured using transparent and opaque closed chambers. The ecosystem respiration (CO2) and the net ecosystem exchange (CO2) were modelled in high time resolution using automatically monitored climate data. Measured and modelled values fit very well together (R2 between 0.88 and 0.98). Annually cumulated gas flux rates, net ecosystem carbon balances (NECB) and global warming potential (GWP) balances were determined. The annual net ecosystem exchange (CO2) varied strongly at the rewetted sites (from -201.7 ± 126.8 to 29.7 ± 112.7 g CO2-C m-2 a-1) due to different weather conditions, water level and vegetation. The Sphagnum cultivation site was a sink of CO2 (-118.8 ± 48.1 and -78.6 ± 39.8 g CO2-C m-2 a-1). The yearly CH4 balances ranged between 16.2 ± 2.2 and 24.2 ± 5.0 g CH4-C m-2 a-1 at two inundated sites, while one rewetted site with a comparatively low water level and the Sphagnum farming site show CH4 fluxes close to zero. The net N2O fluxes were low and not significantly different between the four sites. The annual NECB at the rewetted sites was between -183.8 ± 126.9 and 51.6 ± 112.8 g CO2-C m-2 a-1 and at the Sphagnum cultivating site -114.1 ± 48.1 and -75.3 ± 39.8 g CO2-C m-2 a-1

  14. Atmospheric deposition of Pb, Cu, Ni, As, Sb, V, Cr, Co, Cd and Zn recorded in the Misten peat bog (Hautes-Fagnes, Belgium) during the Industrial Revolution

    Science.gov (United States)

    Allan, M.; Le Roux, G.; De Vleeschouwer, F.; Mattielli, N.; Fagel, N.

    2012-04-01

    A 40 cm peat core was studied from ombrotrophic bog in Western Europe (Misten bog, Hautes-Fagnes, Belgium). Trace metal and metalloid content (TM) and Pb isotopes were analysed by Q-ICP-MS and MC-ICP-MS, respectively. We focused our attention to a selected number of TM according to their specific enrichment (i.e. Pb, Cu, Ni, As, Sb, Cr, Co, V, Cd and Zn). Our aims were: 1) to investigate TM mobility; 2) to determine TM accumulation rates and 3) to link TM accumulation rates with established histories of anthropogenic atmospheric emission. According to 210Pb and 14C data the studied peat core section covered the last two centuries. The general agreement in TM concentration and flux profiles suggested that all TM (except Zn and Cd), were immobile in the Misten peat bog. The temporal increase of TM fluxes between the inception of the Industrial Revolution and the present vary by a factor of 5 to 50 according to TM. The maximum fluxes of TM were found between 1991 and 1995 AD. The coal consumption and metallurgical activities were the predominant source of pollution. The historical TM profiles in the Misten peat profile are in agreement with other European records, reflecting the influence of regional European pollution.

  15. Variations in the D/H and /sup 18/O//sup 16/O ratios in cellulose extracted from a peat bog core

    Energy Technology Data Exchange (ETDEWEB)

    Brenninkmeijer, C.A.M.; Mook, W.G. (Rijksuniversiteit Groningen (Netherlands). Isotopenlaboratorium); van Geel, B. (Amsterdam Univ. (Netherlands). Hugo de Vries Lab.)

    1982-12-01

    A peat core from a raised bog covering the period 3100 to 2400 /sup 14/C years B.P. has been analysed for D/H and /sup 18/O//sup 16/O ratios. These analyses were applied to cellulose, extracted from 56 successive layers of 1 cm thickness. D/H ratios were determined for the carbon bonded hydrogen; /sup 18/O//sup 16/O analyses were performed by applying a new method. For the interpretation of the results obtained on peat, the isotopic ratios of 11 living bog plant species were measured, showing a relatively large scatter. Most pronounced is a depletion in D of about 25per mille and in /sup 18/O of about 5per mille of the Sphagnum mosses relative to the vascular bog plants. This different isotopic composition is reflected by the deltaD and delta/sup 18/O records of the peat core, because the abundance of the remains of non-vascular plants is variable. If this effect is taken account of, the remaining deltaD variations appear to be too large to be attributed to variations in the isotopic compositions of precipitation. As palaeoclimatic indicators the D/H and /sup 18/O//sup 16/O ratio qualitatively agree with the pollen analytical evidence for the climatic deterioration of the Subboreal-Subatlantic transition.

  16. The occurence of rare and protected plant species on the peat bog near Lake Bikcze (Łęczyńsko-Włodawskie Lakeland

    Directory of Open Access Journals (Sweden)

    Magdalena Pogorzelec

    2012-12-01

    Full Text Available This paper presents the results of a pilot field study, conducted in July 2007, designed to make floristic evaluation of the peat bog area adjacent to the western shore of Lake Bikcze (Łęczyńsko-Włodawskie Lakeland. The main aim of the study was to confirm the occurrence of populations of rare and legally protected plant species in this area and to identify, on a preliminary basis, habitat conditions in their stands. The occurrence of populations of the following strictly protected plant species: Betula humilis, Salix lapponum, Salix myrtilloides, Carex limosa, Drosera intermedia, Drosera rotundifolia, Dactylorhiza incarnata; and partially protected species: Menyanthes trifoliata, has been confirmed in the studied peat bog. Both an investigation of abiotic factors, conducted in situ, and an analysis of the species composition of the flora in terms of habitat preferences of particular groups of taxa have shown that the described rare plant species find suitable conditions for their growth and development in the studied peat bog.

  17. Sphagnum-dominated bog systems are highly effective yet variable sources of bio-available iron to marine waters

    International Nuclear Information System (INIS)

    Krachler, Regina; Krachler, Rudolf F.; Wallner, Gabriele; Steier, Peter; El Abiead, Yasin; Wiesinger, Hubert; Jirsa, Franz; Keppler, Bernhard K.

    2016-01-01

    Iron is a micronutrient of particular interest as low levels of iron limit primary production of phytoplankton and carbon fluxes in extended regions of the world's oceans. Sphagnum-peatland runoff is extraordinarily rich in dissolved humic-bound iron. Given that several of the world's largest wetlands are Sphagnum-dominated peatlands, this ecosystem type may serve as one of the major sources of iron to the ocean. Here, we studied five near-coastal creeks in North Scotland using freshwater/seawater mixing experiments of natural creek water and synthetic seawater based on a 59 Fe radiotracer technique combined with isotopic characterization of dissolved organic carbon by Accelerator Mass Spectrometry. Three of the creeks meander through healthy Sphagnum-dominated peat bogs and the two others through modified peatlands which have been subject to artificial drainage for centuries. The results revealed that, at the time of sampling (August 16–24, 2014), the creeks that run through modified peatlands delivered 11–15 μg iron per liter creek water to seawater, whereas the creeks that run through intact peatlands delivered 350–470 μg iron per liter creek water to seawater. To find out whether this humic-bound iron is bio-available to marine algae, we performed algal growth tests using the unicellular flagellated marine prymnesiophyte Diacronema lutheri and the unicellular marine green alga Chlorella salina, respectively. In both cases, the riverine humic material provided a highly bio-available source of iron to the marine algae. These results add a new item to the list of ecosystem services of Sphagnum-peatlands. - Highlights: • We report that peat-bogs are sources of bio-available iron to marine algae. • This iron is effectively chelated with aquatic humic acids. • The radiocarbon age of the iron-carrying aquatic humic acids was up to 550 years. • Analysis was focused on mixing experiments of iron-rich creek water with seawater. • Drained

  18. Sphagnum-dominated bog systems are highly effective yet variable sources of bio-available iron to marine waters

    Energy Technology Data Exchange (ETDEWEB)

    Krachler, Regina, E-mail: regina.krachler@univie.ac.at [Institute of Inorganic Chemistry, University of Vienna, Währingerstraße 42, 1090 Vienna (Austria); Krachler, Rudolf F.; Wallner, Gabriele [Institute of Inorganic Chemistry, University of Vienna, Währingerstraße 42, 1090 Vienna (Austria); Steier, Peter [Isotope Research and Nuclear Physics, University of Vienna, Währingerstraße 17, 1090 Vienna (Austria); El Abiead, Yasin; Wiesinger, Hubert [Institute of Inorganic Chemistry, University of Vienna, Währingerstraße 42, 1090 Vienna (Austria); Jirsa, Franz [Institute of Inorganic Chemistry, University of Vienna, Währingerstraße 42, 1090 Vienna (Austria); University of Johannesburg, Department of Zoology, P. O. Box 524, Auckland Park 2006 (South Africa); Keppler, Bernhard K. [Institute of Inorganic Chemistry, University of Vienna, Währingerstraße 42, 1090 Vienna (Austria)

    2016-06-15

    Iron is a micronutrient of particular interest as low levels of iron limit primary production of phytoplankton and carbon fluxes in extended regions of the world's oceans. Sphagnum-peatland runoff is extraordinarily rich in dissolved humic-bound iron. Given that several of the world's largest wetlands are Sphagnum-dominated peatlands, this ecosystem type may serve as one of the major sources of iron to the ocean. Here, we studied five near-coastal creeks in North Scotland using freshwater/seawater mixing experiments of natural creek water and synthetic seawater based on a {sup 59}Fe radiotracer technique combined with isotopic characterization of dissolved organic carbon by Accelerator Mass Spectrometry. Three of the creeks meander through healthy Sphagnum-dominated peat bogs and the two others through modified peatlands which have been subject to artificial drainage for centuries. The results revealed that, at the time of sampling (August 16–24, 2014), the creeks that run through modified peatlands delivered 11–15 μg iron per liter creek water to seawater, whereas the creeks that run through intact peatlands delivered 350–470 μg iron per liter creek water to seawater. To find out whether this humic-bound iron is bio-available to marine algae, we performed algal growth tests using the unicellular flagellated marine prymnesiophyte Diacronema lutheri and the unicellular marine green alga Chlorella salina, respectively. In both cases, the riverine humic material provided a highly bio-available source of iron to the marine algae. These results add a new item to the list of ecosystem services of Sphagnum-peatlands. - Highlights: • We report that peat-bogs are sources of bio-available iron to marine algae. • This iron is effectively chelated with aquatic humic acids. • The radiocarbon age of the iron-carrying aquatic humic acids was up to 550 years. • Analysis was focused on mixing experiments of iron-rich creek water with seawater. • Drained

  19. Geochemical response of a calcareous fen to road salt contamination during snow melt and precipitation events: Kampoosa Bog, Stockbridge, MA

    Science.gov (United States)

    Rhodes, A. L.; Guswa, A. J.

    2008-12-01

    Kampoosa Bog is the largest and most diverse calcareous lake-basin fen remaining in Massachusetts, and it is one of the state's elite Areas of Critical Environmental Concern (ACEC). The ground water chemistry of the fen has been greatly altered by road salt runoff (NaCl) from the Massachusetts Turnpike, which crosses the northern margin of the wetland complex. Ground water samples collected at different depths within the wetland, measurements of exchangeable Na from an eight-meter core, and hydraulic conductivity measurements suggest that ground water flow and contamination is largely a near- surface phenomenon. Detailed sampling of surface and ground waters during three spring snow melt events and one precipitation event characterizes the geochemical response of the wetland to hydrologic events. Overall, Na:Cl ratios for surface and ground water samples are less than one, and sodium and chloride imbalances suggest that 20-30% of sodium from rock salt is stored on cation exchange sites on organic material. Na:Cl ratios greater than one for fen ground water sampled during Snow Melt 2007 suggest that sodium can be released from cation exchange sites back to ground water under dilute conditions. The total mass of Na and Cl exported from the wetland is greatest under conditions of high discharge. The flux of dissolved salts at the outlet of the fen during Snow Melt 2005 accounts for ~ 24% Na and ~ 32% Cl of rock salt added to the Massachusetts Turnpike during 2004-2005. Estimates of annual fluxes of Na and Cl are on par with the amount of road salt applied, and sodium and chloride concentrations in shallow groundwater have decreased since 2002. The months of March, April and May are the primary months for salt export, accounting for more than half of the annual salt flux in 2005. Concerning the annual net export of sodium and chloride, large rain events may be more important with removing dissolved salts from the fen than snow melt because snow melt also is a time when

  20. A Holocene History of Permafrost Dynamics, Carbon Sequestration, and Hydrological Changes at Beretta Bog, Mackenzie River Basin

    Science.gov (United States)

    Von Ness, K.; Loisel, J.; Beilman, D. W.; Kaiser, K.

    2017-12-01

    The Mackenzie River Basin (MRB) is one of the world's largest permafrost peatland areas. This region contains dense soil carbon deposits and is home of the largest Canadian Arctic watershed. However, much remains to be known about the timing of permafrost initiation and the moisture changes that have affected soil development across this region throughout the Holocene. Peatland hydroclimatic conditions, which impact permafrost freezing and thawing as well as carbon sequestration rates, are relatively undocumented in peat-based paleoreconstructions. To provide further insight into the region's permafrost dynamics and the moisture changes associated with them, this study presents a permafrost initiation history and paleohydrological reconstruction of Beretta Bog, MRB that dates back to roughly 9000 cal BP. We explore the use of lichens as a bio-indicator of permafrost formation by quantifying the abundance of lichen-specific carbohydrates (mannose and galactose) in the peat profile. Testate amoebae, plant macrofossils, and carbon and oxygen isotopes (δ13C and δ18O) are also being analyzed at high resolution to reconstruct past changes in soil moisture and temperature. To our knowledge this study will constitute the first high-resolution paleohydrological reconstruction for this region. While carbohydrate analysis is underway, high C/N values from 6000 cal BP to present are temporarily used as an indicator for permafrost aggradation. Carbon accumulation rates of the core are highest prior to 6000 cal BP (during the Holocene Thermal Maximum) and relatively lower until around 1000 cal BP; we hypothesize this period of slow accumulation corresponds to permafrost aggradation. Preliminary results of our δ13C analysis corroborate testate assemblages as a proxy suitable for revealing moisture changes in permafrost peat. In the upper core, our analysis shows that more negative δ13C values, which reflect drier conditions, correlate to higher percentages of A. flavum and H

  1. Carbon dioxide fluxes over a raised open bog at the Kinosheo Lake tower site during the Northern Wetlands Study (NOWES)

    Science.gov (United States)

    Neumann, H. H.; Den Hartog, G.; King, K. M.; Chipanshi, A. C.

    1994-01-01

    Measurements of carbon dioxide concentration and flux were made above a raised open bog at Lake Kinosheo in the southern Hudson Bay lowlands during the Northern Wetlands Study (NOWES) experiment in 1990. The flux measurements were made using micrometeorological techniques. They provide the first nondisturbing, larger-scale CO2 flux measurements for this ecosystem and are the first to integrate the exchange over the whole 24 hours of the day. Continuous concentration measurements by infrared gas analyzers (IRGA) and spot flask samples were taken over the period July 1 to July 29. Afternoon CO2 values were only 5 to 7 parts per million by volume (ppmv) lower than measurements over the same period at Canadian background monitoring stations. This suggested that there was little draw-down by local photosynthetic sinks. CO2 fluxes were measured at 8 and 18 m by Bowen ratio and eddy correlation methods, respectively. The methods produced comparable results on averaged data but often diverged considerably on individual half-hour results. Fluxes were small. Daytime values averaged to -0.068 mg/sq m/s by eddy correlation and -0.077 mg/sq m/s by Bowen ratio over the period June 25 to July 28 (negative denotes downward flux), while at night, flux densities were +0.062 mg/sq m/s and +0.085 mg/sq m/s. Integration of the mean diurnal curve gave a net flux of -1.7 g/sq m/d. Comparable data for this type of ecosystem were not found. However, Coyne and Kelley (1975), measuring near Barrow, Alaska, over wet meadow tundra dominated by sedges and grasses, found net fluxes of -7.2 g/sq m/d. Typical net CO2 fluxes from other active temperature ecosystems have been found to be -10 to -20 g/sq m/d (Monteith, 1976). Mean half hourly fluxes were almost constant at +0.06 mg/sq m/s through the nighttime hours. About one half-hour after sunrise the flux reversed direction. Uptake peaked about 0900 eastern daylight time (EDT) and then gradually declined but remained downward until near sunset

  2. Holocene palaeohydrological history of the Tǎul Muced peat bog (Northern Carpathians, Romania) based on testate amoebae (Protozoa) and plant macrofossils

    Science.gov (United States)

    Cosmin Diaconu, Andrei; Feurdean, Angelica; Lamentowicz, Mariusz; Gałka, Mariusz; Tanţǎu, Ioan

    2016-04-01

    Knowledge of past local vs. regional hydro-climate variability is a priority in climate research. This is because ecosystems and human depend on local climatic conditions and the magnitude of these climate changes is more variable at local and regional rather than at global scales. Ombrotrophic bogs are highly suitable for hydro-climate reconstructions as they are entirely dependent on the water from precipitation. We used stratigraphy, radiocarbon dating, testate amoebae (TA) and plant macrofossils on a peat profile from an ombrotrophic bog (Tǎul Muced) located in the Biosphere Reserve of the Rodna National Park Romania. We performed quantitative reconstruction of the depth to water table (DWT) and pH over the last 8000 years in a continental area of CE Europe. We identified six main stages in the development of the bog based on changes in TA assemblages in time. Wet conditions and pH between 2 and 4.5 were recorded between 4600-2750 and 1300-400 cal. yr BP, by the occurrence of Archerella flavum, Amphitrema wrightianum and Hyalosphenia papilio. This was associated to a local vegetation primarily composed of Sphagnum magellanicum and S. angustifolium. Dry stages and pH of 2.5 to 5 were inferred between 7550-4600, 2750-1300 and -50 cal. yr BP, by the dominance of Nebela militaris, Difflugia pulex and Phryganella acropodia. These overall dry conditions were also connected with increased abundance of Eriophorum vaginatum. The period between 400 and -50 cal. yr BP was characterized by a rapid shift from dry to wet conditions on the surface of the bog. Vegetation shifted from Sphagnum magellanicum to Sphagnum russowii dominated community. Our reconstruction remains in relatively good agreement with other palaeohydrological records from Central Eastern Europe. However, it shows contrasting conditions to others particularly with records from NW Europe. The valuable information regarding bog hydrology offered by our record puts an accent on the need of more regional TA

  3. Mining for Nonribosomal Peptide Synthetase and Polyketide Synthase Genes Revealed a High Level of Diversity in the Sphagnum Bog Metagenome.

    Science.gov (United States)

    Müller, Christina A; Oberauner-Wappis, Lisa; Peyman, Armin; Amos, Gregory C A; Wellington, Elizabeth M H; Berg, Gabriele

    2015-08-01

    Sphagnum bog ecosystems are among the oldest vegetation forms harboring a specific microbial community and are known to produce an exceptionally wide variety of bioactive substances. Although the Sphagnum metagenome shows a rich secondary metabolism, the genes have not yet been explored. To analyze nonribosomal peptide synthetases (NRPSs) and polyketide synthases (PKSs), the diversity of NRPS and PKS genes in Sphagnum-associated metagenomes was investigated by in silico data mining and sequence-based screening (PCR amplification of 9,500 fosmid clones). The in silico Illumina-based metagenomic approach resulted in the identification of 279 NRPSs and 346 PKSs, as well as 40 PKS-NRPS hybrid gene sequences. The occurrence of NRPS sequences was strongly dominated by the members of the Protebacteria phylum, especially by species of the Burkholderia genus, while PKS sequences were mainly affiliated with Actinobacteria. Thirteen novel NRPS-related sequences were identified by PCR amplification screening, displaying amino acid identities of 48% to 91% to annotated sequences of members of the phyla Proteobacteria, Actinobacteria, and Cyanobacteria. Some of the identified metagenomic clones showed the closest similarity to peptide synthases from Burkholderia or Lysobacter, which are emerging bacterial sources of as-yet-undescribed bioactive metabolites. This report highlights the role of the extreme natural ecosystems as a promising source for detection of secondary compounds and enzymes, serving as a source for biotechnological applications. Copyright © 2015, American Society for Microbiology. All Rights Reserved.

  4. Biomass, productivity and relative rate of photosynthesis of sphagnum at different water levels on a South Swedish peat bog

    International Nuclear Information System (INIS)

    Wallen, B.; Falkengren-Grerup, U.; Malmer, N.

    1988-01-01

    The distribution pattern of Spaghnum species on bogs follows a hummock-hollow gradient. S. Sect. Acutifolia (that is in this study S. Fuscum and S. rubellum combined) dominates hummock tops, ca 20 cm above the maximum water level with a green biomass of 50 g m --2 , S. magellanicum dominates at a lower level, about 5 cm above the water level with a green biomass of 75 g m -2 and S. cuspidatum dominates in the wettest hollows with a green biomass of about 50 g m -2 . In situ measurements of length growth of S. Sect. Acutifolia and S. magelanicum using a 14 CO 2 -labelling technique during three consecutive years, revealed an unexpectedly high between-year variation in length growth of 7-23 mm yr -1 , and 16-22 mm yr -1 , respectively. Consequently the dominating producer in the transition between hummock and hollow changes from year to year, probably depending on climatic conditions. In vitro experiments on the effects of different water levels of 2, 5, 10 and 20 cm below the moss surface, on photosynthetic activity of S. Sect. Acutifolia and S. magellanicum, measured by a second 14 CO 2 -technique, indicate optimal conditions for S. magellanicum at 10 cm above water level, and for S. Sect, Acutofolia at 20 cm above water level. Differences in capillary water transport capability between the species are more important than the sensitivity of photosynthesis to water stress in explaining field patterns of productivity and distribution

  5. Chromobacterium vaccinii sp. nov., isolated from native and cultivated cranberry (Vaccinium macrocarpon Ait.) bogs and irrigation ponds.

    Science.gov (United States)

    Soby, Scott D; Gadagkar, Sudhindra R; Contreras, Cristina; Caruso, Frank L

    2013-05-01

    A large number of Gram-negative, motile, mesophilic, violacein-producing bacteria were isolated from the soils and roots of Vaccinium macrocarpon Ait. and Kalmia angustifolia L. plants and from irrigation ponds associated with wild and cultivated cranberry bogs in Massachusetts, USA. Phylogenetic analyses of 16S rRNA gene sequences placed these isolates in a clade with Chromobacterium species, but the specialized environment from which they were isolated, their low genomic DNA relatedness with Chromobacterium violaceum ATCC 12472(T) and C. subtsugae PRAA4-1(T), significant differences in fatty acid composition and colony morphology indicate that the cranberry and Kalmia isolates comprise a separate species of Chromobacterium, for which the name Chromobacterium vaccinii sp. nov. is proposed. Strain MWU205(T) ( = ATCC BAA-2314(T)  = DSM 25150(T)) is proposed as the type strain for the novel species. Phenotypic analysis of 26 independent isolates of C. vaccinii sp. nov. indicates that, despite close geographical and biological proximity, there is considerable metabolic diversity among individuals within the population.

  6. Three new species of oribatid mites of the family Punctoribatidae (Acari, Oribatida) from alpine bogs of New Zealand.

    Science.gov (United States)

    Ermilov, Sergey G; Minor, Maria A

    2016-03-15

    Three new species of oribatid mites of the family Punctoribatidae (Acari, Oribatida) are described from alpine bogs of the Central Otago region in the South Island of New Zealand. Macrogena hexasetosa sp. nov. is morphologically most similar to M. brevisensilla Ermilov & Minor, 2015, however, it differs from the latter by larger body size, the presence of six pairs of genital setae, notogastral and ano-adanal setae of medium size, setiform rostral setae, narrower tutorial cusps, the absence of antero-ventral teeth on genua I, II and femora II, and by the absence of striae on the subcapitular mentum. Porallozetes badamdorji sp. nov. differs from the type species-P. dispar (Hammer, 1973)-by larger body length, the presence of interlamellar setae, short and clavate bothridial setae, anterior notogastral margin, notogastral setae of medium size, semi-oval dorsophragmata, and by the position of notogastral porose areas A2 posteriorly to A1. Safrobates gerdi sp. nov. differs from the type species-S. miniporus Mahunka, 1989-by larger body size, the presence of setiform rostral setae, and by notogastral setae of medium length. Porallozetes and Safrobates are recorded in New Zealand for the first time. Generic diagnoses for Macrogena, Porallozetes and Safrobates are given.

  7. Atmospheric pollutants in alpine peat bogs record a detailed chronology of industrial and agricultural development on the Australian continent

    International Nuclear Information System (INIS)

    Marx, Samuel K.; Kamber, Balz S.; McGowan, Hamish A.; Zawadzki, Atun

    2010-01-01

    Two peat bogs from remote alpine sites in Australia were found to contain detailed and coherent histories of atmospheric metal pollution for Pb, Zn, Cu, Mo, Ag, As, Cd, Sb, Zn, In, Cr, Ni, Tl and V. Dramatic increases in metal deposition in the post-1850 AD portion of the cores coincide with the onset of mining in Australia. Using both Pb isotopes and metals, pollutants were ascribed to the main atmospheric pollution emitting sources in Australia, namely mining and smelting, coal combustion and agriculture. Results imply mining and metal production are the major source of atmospheric metal pollution, although coal combustion may account for up to 30% of metal pollutants. A novel finding of this study is the increase in the otherwise near-constant Y/Ho ratio after 1900 AD. We link this change to widespread and increased application of marine phosphate fertiliser in Australia's main agricultural area (the Murray Darling Basin). - Detailed records of atmospheric metal pollution accumulation in Australia are presented and are shown to trace the industrial and agricultural development of the continent.

  8. Seasonal variations in CO2 and CH4 fluxes of four different plant compositions of a Sphagnum-dominated Alpine peat bog

    Science.gov (United States)

    Drollinger, Simon; Maier, Andreas; Karer, Jasmin; Glatzel, Stephan

    2017-04-01

    Peatlands are the only type of ecosystems which have the ability to accumulate significant amounts of carbon (C) under undisturbed conditions. The amount of C sequestered in peatlands depends on the balance between gross primary production, ecosystem respiration and decomposition of plant material. Sphagnum-dominated bogs possess the greatest peat accumulation potential of all peatlands, thus in turn, feature highest C release potentials. Many studies report about the C balances of undisturbed northern peat bogs, however, little is known about the effects of peatland degradation on the C balance between different plant compositions within peat bog ecosystems. Particularly in the Alpine region, where temperature increase during the last century has been almost twice as high as the global mean. The investigated peat bog is located in the inner Alpine Enns valley in the Eastern Alps, Austria (N 47˚ 34.873' E 14˚ 20.810'). It is a pine peat bog covered by Sphagnum mosses and a present extent of about 62 ha. Due to increasing differences in surface height of the peatland compared to the surrounding areas and related lowered water retention capacity attributed to the subsidence of the adjacent intensively managed meadows on deeply drained peat soils, the function of the peatland as a carbon sink is strongly endangered. Hence, the current mean water table depth of the central peat bog area is about -12 cm. To reveal differences in peatland-atmosphere C exchanges within the peatland ecosystem, we investigated CO2 and CH4 fluxes of four different vegetation compositions (PM1-PM4) at the treeless central peat bog area. PM1 is dominated by the graminoids Rhynchospora alba and Eriophorum vaginatum. PM2 is inhabited by small individuals (< 35 cm) of the conifer Pinus mugo, whereas PM3 is dominated by the ericaceous plant Calluna vulgaris. PM4 again is populated by Pinus mugo, but higher growing (35 - 60 cm) and with corresponding higher amount of biomass. Fluxes were measured

  9. Preliminary palynological analysis of a Holocene peat bog from Apakará-tepui (Chimantá Massif, Venezuelan Guayana

    Directory of Open Access Journals (Sweden)

    Rull, V.

    2011-12-01

    Full Text Available Preliminary palynological analysis of a Holocene peat bog from Apakará-tepui (Chimantá Massif, Venezuelan Guayana.- This paper reports the preliminary palynological results, at a millennial scale, of a Holocene peat bog sequence, since around 8.0 cal kyr BP to the present, obtained in the summit of the Apakará-tepui (2170 m elevation, in the Chimantá massif, located in the neotropical Venezuelan Guayana. The early Holocene was characterized by a vegetation different to the present, in which trees and shrubs dominated and Myrica (Myricaceae was the main element of the gallery forests around a permanent water body, as indicated by the continuous presence of Isoëtes (Isoëtaceae in high percentages. Around the middle Holocene (5.3 cal kyr BP, a shift towards more herbaceous and non-flooded communities occurred, and the present day vegetation established. This has been interpreted as a shift from warmer and wetter climates to cooler and drier conditions. The first phase, from 8.0 to 5.3 cal kyr BP, falls within a warming phase widely documented worldwide, known as the Holocene Thermal Maximum. The millennial trends shown here will be refined with further studies at centennial to decadal time scales. These results support the hypothesis that the best sites to detect paleoenvironmental changes in the summits of the tabular Guayana mountains are close to altitudinal ecotones.

    Análisis palinológico preliminar de una turbera holocena del Apakará-tepui (Macizo de Chimantá, Guayana venezolana.- Este artículo presenta los resultados palinológicos preliminares, a escala de milenios, de una secuencia holocena, desde 8.0 cal kyr BP hasta la actualidad, obtenida en la cima del Apakará-tepui (2170 m de altitud, en el Macizo del Chimantá, situado en la región neotropical de la Guayana venezolana. El Holoceno temprano se caracterizó por una vegetación diferente a la actual, dominada por árboles y arbustos, en la que

  10. Sphagnum-dominated bog systems are highly effective yet variable sources of bio-available iron to marine waters.

    Science.gov (United States)

    Krachler, Regina; Krachler, Rudolf F; Wallner, Gabriele; Steier, Peter; El Abiead, Yasin; Wiesinger, Hubert; Jirsa, Franz; Keppler, Bernhard K

    2016-06-15

    Iron is a micronutrient of particular interest as low levels of iron limit primary production of phytoplankton and carbon fluxes in extended regions of the world's oceans. Sphagnum-peatland runoff is extraordinarily rich in dissolved humic-bound iron. Given that several of the world's largest wetlands are Sphagnum-dominated peatlands, this ecosystem type may serve as one of the major sources of iron to the ocean. Here, we studied five near-coastal creeks in North Scotland using freshwater/seawater mixing experiments of natural creek water and synthetic seawater based on a (59)Fe radiotracer technique combined with isotopic characterization of dissolved organic carbon by Accelerator Mass Spectrometry. Three of the creeks meander through healthy Sphagnum-dominated peat bogs and the two others through modified peatlands which have been subject to artificial drainage for centuries. The results revealed that, at the time of sampling (August 16-24, 2014), the creeks that run through modified peatlands delivered 11-15μg iron per liter creek water to seawater, whereas the creeks that run through intact peatlands delivered 350-470μg iron per liter creek water to seawater. To find out whether this humic-bound iron is bio-available to marine algae, we performed algal growth tests using the unicellular flagellated marine prymnesiophyte Diacronema lutheri and the unicellular marine green alga Chlorella salina, respectively. In both cases, the riverine humic material provided a highly bio-available source of iron to the marine algae. These results add a new item to the list of ecosystem services of Sphagnum-peatlands. Copyright © 2016 The Authors. Published by Elsevier B.V. All rights reserved.

  11. Methylocapsa acidiphila gen. nov., sp. nov., a novel methane-oxidizing and dinitrogen-fixing acidophilic bacterium from Sphagnum bog.

    Science.gov (United States)

    Dedysh, Svetlana N; Khmelenina, Valentina N; Suzina, Natalia E; Trotsenko, Yuri A; Semrau, Jeremy D; Liesack, Werner; Tiedje, James M

    2002-01-01

    A novel genus and species, Methylocapsa acidiphila gen. nov., sp. nov., are proposed for a methane-oxidizing bacterium isolated from an acidic Sphagnum peat bog. This bacterium, designated strain B2T, represents aerobic, gram-negative, colourless, non-motile, curved coccoids that form conglomerates covered by an extracellular polysaccharide matrix. The cells use methane and methanol as sole sources of carbon and energy and utilize the serine pathway for carbon assimilation. Strain B2T is a moderately acidophilic organism with growth between pH 4.2 and 7.2 and at temperatures from 10 to 30 degrees C. The cells possess a well-developed system of intracytoplasmic membranes (ICM) packed in parallel on only one side of the cell membrane. This type of ICM structure represents a novel arrangement, which was termed type III. The resting cells are Azotobacter-type cysts. Strain B2T is capable of atmospheric nitrogen fixation; it possesses particulate methane monooxygenase and does not express soluble methane monooxygenase. The major phospholipid fatty acid is 18:1omega7c and the major phospholipids are phosphatidylglycerols. The G+C content of the DNA is 63.1 mol%. This bacterium belongs to the alpha-subclass of the Proteobacteria and is most closely related to the acidophilic methanotroph Methylocella palustris KT (97.3% 16S rDNA sequence similarity). However, the DNA-DNA hybridization value between strain B2T and Methylocella palustris K(T) is only 7%. Thus, strain B2T is proposed to comprise a novel genus and species, Methylocapsa acidiphila gen. nov., sp. nov. Strain B2T (= DSM 13967T = NCIMB 13765T) is the type strain.

  12. Demographic and genetic status of an isolated population of bog turtles (Glyptemys muhlenbergii): Implications for managing small populations of long-lived animals

    Science.gov (United States)

    Pittman, Shannon E.; King, T.L.; Faurby, S.; Dorcas, M.E.

    2011-01-01

    In this study, we sought to determine the population stability and genetic diversity of one isolated population of the federally-threatened bog turtle (Glyptemys muhlenbergii) in North Carolina. Using capture-recapture data, we estimated adult survival and population growth rate from 1992 to 2007. We found that the population decreased from an estimated 36 adult turtles in 1994 to approximately 11 adult turtles in 2007. We found a constant adult survival of 0. 893 (SE = 0. 018, 95% confidence interval, 0. 853-0. 924) between 1992 and 2007. Using 18 microsatellite markers, we compared the genetic status of this population with five other bog turtle populations. The target population displayed allelic richness (4. 8 ?? 0. 5) and observed heterozygosity (0. 619 ?? 0. 064) within the range of the other bog turtle populations. Coalescent analysis of population growth rate, effective population size, and timing of population structuring event also indicated the genetics of the target population were comparable to the other populations studied. Estimates of effective population size were a proportion of the census size in all populations except the target population, in which the effective population size was larger than the census size (30 turtles vs. 11 turtles). We attribute the high genetic diversity in the target population to the presence of multiple generations of old turtles. This study illustrates that the demographic status of populations of long-lived species may not be reflected genetically if a decline occurred recently. Consequently, the genetic integrity of populations of long-lived animals experiencing rapid demographic bottlenecks may be preserved through conservation efforts effective in addressing demographic problems. ?? 2011 Springer Science+Business Media B.V.

  13. Four thousand years of atmospheric Pb, Cd and Zn deposition recorded by the ombrotrophic peat bog of Penido Vello (northwestern Spain)

    Energy Technology Data Exchange (ETDEWEB)

    Martinez-Cortizas, A.; Pontevedra-Pombal, X.; Novoa-Munoz, J.C.; Garcia-Rodeja, E. [Universidad de Santiago de Compostila, Santiago de Compostela (Spain). Dept. de Edafologia y Quimica Agricola

    1997-12-01

    The Northwest Iberian Peninsula is a mid-latitude oceanic region with areas where different types of bogs are frequent or abundant. The ombrotrophic nature of some bogs make them suitable for the study of accumulation patterns of heavy metals. One of these bogs, Penido Vello, was sampled to a depth of 2.5 m and analyzed in detail for its physico-chemical properties and Pb, Zn and Cd concentrations. Ash and organic carbon content, Ca/Mg molar ratios and a number of other characteristics support an ombrotrophic interpretation of the core. Concentrations of Pb, Zn and Cd were measured, showing important variations in the core. While Zn and Cd are concentrated mainly in the upper sections of the core with minor changes with depth, the Pb profile shows significant peaks in the deeper layers suggesting pre-industrial atmospheric pollution. Enrichment factors (EFs) calculated by normalising to Al correlated well with those calculated by normalising to Ti. Maximum EFs are 33.56 and 52 for Pb, Zn and Cd respectively. While for Pb these values are comparable to those obtained by other authors, maximum Zn EFs are greater than those mentioned in the literature and may be attributed to the emissions of a nearby coal-burning power plant. At least for Pb the accumulation pattern suggests that atmospheric pollution can be dated back some 2800 years, and that pollution increased steadily since the Iron Age to reach considerably elevated levels, up to 5 times the `background`, during the Roman Empire. Changes in Pb emissions through times are in good accord with the prehistorical and historical record of the Iberian Peninsula. 54 refs., 8 figs., 1 tab.

  14. Intercomparison of radiocarbon bomb pulse and {sup 210}Pb age models. A study in a peat bog core from North Poland

    Energy Technology Data Exchange (ETDEWEB)

    Piotrowska, Natalia, E-mail: natalia.piotrowska@polsl.p [Department of Radioisotopes, Institute of Physics, Silesian University of Technology, Krzywoustego, 2, Gliwice 44100 (Poland); Vleeschouwer, Francois De; Sikorski, Jaroslaw; Pawlyta, Jacek [Department of Radioisotopes, Institute of Physics, Silesian University of Technology, Krzywoustego, 2, Gliwice 44100 (Poland); Fagel, Nathalie; Roux, Gael Le [Clays and Palaeoclimate Unit, Department of Geology, University of Liege, Allee du 6 Aout, B18, Sart Tilman, Liege 4000 (Belgium); Pazdur, Anna [Department of Radioisotopes, Institute of Physics, Silesian University of Technology, Krzywoustego, 2, Gliwice 44100 (Poland)

    2010-04-15

    Radiocarbon and {sup 210}Pb were measured on the uppermost 40 cm of a Wardenaar peat core retrieved from a Baltic raised bog at Slowinskie Blota (Pomerania, North Poland). This site is the subject of ongoing multiproxy studies covering the last 1300 years. Radiocarbon age model was constructed on the basis of 14 AMS dates obtained on selected Sphagnum spp. fragments, with use of P{sub S}equence tool. We present here a comparison of this model with the age model obtained using CRS model classically applied to {sup 210}Pb measurements.

  15. Diatoms from a peat bog on the Pešter plateau (southwestern Serbia: New records for diatom flora of Serbia

    Directory of Open Access Journals (Sweden)

    Vidaković Danijela

    2016-01-01

    Full Text Available The distribution of diatoms was studied in three types of diatom communities (epiphytes, benthos and plankton of a peat bog on the Pešter plateau. The observed diatom flora inhabited all investigated communities, comprising in total 250 taxa in 53 genera. Among them, 45 taxa were new records for the Serbian diatom flora. Identified taxa belonged to different groups of algae, however alkaliphile diatoms were dominant. New ecological data for Encyonopsis minuta, Pinnularia isostauron and P. marchica are presented here. All the diatoms were documented by light micrographs, and brief notes on their morphology, distribution and ecology are provided. [Projekat Ministarstva nauke Republike Srbije, br. TR 037009

  16. High specificity but contrasting biodiversity of Sphagnum-associated bacterial and plant communities in bog ecosystems independent of the geographical region.

    Science.gov (United States)

    Opelt, Katja; Berg, Christian; Schönmann, Susan; Eberl, Leo; Berg, Gabriele

    2007-10-01

    Mosses represent ecological niches that harbor a hitherto largely uncharacterized microbial diversity. To investigate which factors affect the biodiversity of bryophyte-associated bacteria, we analyzed the bacterial communities associated with two moss species, which exhibit different ecological behaviors and importance in bog ecosystems, Sphagnum magellanicum and Sphagnum fallax, from six temperate and boreal bogs in Germany and Norway. Furthermore, their surrounding plant communities were studied. Molecular analysis of bacterial communities was determined by single-strand conformation polymorphism (SSCP) analysis using eubacterial and genus-specific primers for the dominant genera Burkholderia and Serratia as well as by sequence analysis of a Burkholderia 16S rRNA gene clone library. Plant communities were analyzed by monitoring the abundance and composition of bryophyte and vascular plant species, and by determining ecological indicator values. Interestingly, we found a high degree of host specificity for associated bacterial and plant communities of both Sphagnum species independent of the geographical region. Calculation of diversity indices on the basis of SSCP gels showed that the S. fallax-associated communities displayed a statistically significant higher degree of diversity than those associated with S. magellanicum. In contrast, analyses of plant communities of Sphagnum-specific habitats resulted in a higher diversity of S. magellanicum-specific habitats for all six sites. The higher content of nutrients in the S. fallax-associated ecosystems can explain higher diversity of microorganisms.

  17. Flourish or flush: effects of simulated extreme rainfall events on Sphagnum-dwelling testate amoebae in a subarctic bog (Abisko, Sweden).

    Science.gov (United States)

    Tsyganov, Andrey N; Keuper, Frida; Aerts, Rien; Beyens, Louis

    2013-01-01

    Extreme precipitation events are recognised as important drivers of ecosystem responses to climate change and can considerably affect high-latitude ombrotrophic bogs. Therefore, understanding the relationships between increased rainfall and the biotic components of these ecosystems is necessary for an estimation of climate change impacts. We studied overall effects of increased magnitude, intensity and frequency of rainfall on assemblages of Sphagnum-dwelling testate amoebae in a field climate manipulation experiment located in a relatively dry subarctic bog (Abisko, Sweden). The effects of the treatment were estimated using abundance, species diversity and structure of living and empty shell assemblages of testate amoebae in living and decaying layers of Sphagnum. Our results show that increased rainfall reduced the mean abundance and species richness of living testate amoebae. Besides, the treatment affected species structure of both living and empty shell assemblages, reducing proportions of hydrophilous species. The effects are counterintuitive as increased precipitation-related substrate moisture was expected to have opposite effects on testate amoeba assemblages in relatively dry biotopes. Therefore, we conclude that other rainfall-related factors such as increased infiltration rates and frequency of environmental disturbances can also affect testate amoeba assemblages in Sphagnum and that hydrophilous species are particularly sensitive to variation in these environmental variables.

  18. Nutrient cycling and productivity of dystrophic lake-bog systems (Part A). Technical progress report, December 1, 1972--September 30, 1975

    International Nuclear Information System (INIS)

    Hooper, F.F.

    1975-10-01

    A sampler and an analytical and characterization scheme were developed to investigate the chemical and physical state of iron in a highly stained acid bog lake. Iron fractions were chemically separated by reactivity to bathophenanthroline (BPN) after specific digestion procedures. Physical separation involved anaerobic in situ filtration (450 nm), and in situ dialysis (4.8 nm). This resulted in three size classes: particulate, colloidal, and dissolved. Unlike pH 6-8 lakes, inorganic, nonreactive species of iron [e.g., Fe(OH) 3 ] represent minor amounts of the total iron in North Gate Lake. In situ radiochemical analyses revealed that colloidal sized reactive ferric iron predominates in the oxygenated epilimnion, while dialyzable or dissolved ferrous iron increases with depth. Unlike iron, organic matter is present in a nontransient colloidal state. In acid (pH 4-5) bog lakes ferric iron is not colloidal as an inorganic complex (OH - ), but colloidal as reactive Fe + 3 by complexation with the colloidal organic acids. After thermally induced mixing with anaerobic waters, ferric iron is reduced and dissolved. However, some of the BPN reactive iron remains colloidal suggesting the presence of a residual ferrous organic complex

  19. Experimental nitrogen, phosphorus, and potassium deposition decreases summer soil temperatures, water contents, and soil CO2 concentrations in a northern bog

    Directory of Open Access Journals (Sweden)

    C. Blodau

    2011-03-01

    Full Text Available Ombrotrophic peatlands depend on airborne nitrogen (N, whose deposition has increased in the past and lead to disappearance of mosses and increased shrub biomass in fertilization experiments. The response of soil water content, temperature, and carbon gas concentrations to increased nutrient loading is poorly known and we thus determined these data at the long-term N fertilization site Mer Bleue bog, Ontario, during a two month period in summer. Soil temperatures decreased with NPK addition in shallow peat soil primarily during the daytime (t-test, p p RMANOVA, which also suggested an influence of volumetric water contents as co-variable on soil temperature and vice versa (p RMANOVA (p 2 concentrations in the near-surface peat (t-test, p < 0.05 were lower with increasing N load, suggesting more rapid soil gas exchange. The results thus suggest that changes in bog ecosystem structure with N deposition have significant ramifications for physical parameters that in turn control biogeochemical processes.

  20. Non-destructive methods for peat layer assessment in oligotrophic peat bogs: a case study from Poiana Ştampei, Romania

    Directory of Open Access Journals (Sweden)

    Iuliana F. Gheorghe

    2011-01-01

    Full Text Available Practices currently employed in the investigation and characterisation of peat deposits are destructive and may irremediable perturb peat bog development even in cases when exploitation is not carried out. We investigated the correlation between vegetation characteristics in the active area of Poiana Ştampei peat bog, Romania, and the underlying peat layer depth, aiming at establishing a non-destructive method of peat layer depth estimation. The presence of the Sphagneto-Eriophoretum vaginati association, dominated by Sphagnum fimbriatum, Eriophorum vaginatum, Andromeda polifolia, Vaccinium oxycoccos, V. myrtillus, V. vitis-idaea, Polytrichum commune, Picea excelsa, Pinus sylvestris and Betula verrucosa was found to predict the existence of the peat layer but not its depth. Out of the seven identified vegetation types, one type was associated with a very thin or no peat layer, one type was characterised by the presence of a thick (over 100 cm peat layer and five types indicated the presence of variable average depths of the peat layer. pH values correlated with peat layer depth only within the vegetation type associated with thick peat layers.

  1. Antioxidant properties, phenolic composition and potentiometric sensor array evaluation of commercial and new blueberry (Vaccinium corymbosum) and bog blueberry (Vaccinium uliginosum) genotypes.

    Science.gov (United States)

    Kraujalytė, Vilma; Venskutonis, Petras Rimantas; Pukalskas, Audrius; Česonienė, Laima; Daubaras, Remigijus

    2015-12-01

    Antioxidant properties of juices of newly bred and known blueberry (Vaccinium corymbosum) genotypes and wild bog blueberry (Vaccinium uliginosum) were evaluated by ABTS(+) scavenging capacity (RSC), ferric reducing antioxidant power (FRAP), oxygen radical absorbance capacity (ORAC), total phenolic content (TPC) and total anthocyanin content (TAC) assays. TPC varied in the range of 0.85-2.81 mg gallic acid equiv./mL, RSC, FRAP and ORAC values were 6.38-20.9, 3.07-17.8 and 4.21-45.68 μmol Trolox equiv./g, respectively. New blueberry genotypes and bog blueberry demonstrated stronger antioxidant properties and TAC than other studied genotypes. The content of quinic (203-3614 μg/mL), chlorogenic (20.0-346.8 μg/mL) acids and rutin (0.00-26.88 μg/mL) measured by UPLC/ESI-QTOF-MS varied depending on the genotype. Juices were evaluated by electronic tongue; PCA score plot showed that the method discriminates different genotypes although some juice samples were located very closely and overlapping. Significant differences were observed between L(∗), a(∗), b(∗) colour parameters of some genotypes. Copyright © 2015 Elsevier Ltd. All rights reserved.

  2. Seasonal climate manipulations have only minor effects on litter decomposition rates and N dynamics but strong effects on litter P dynamics of sub-arctic bog species.

    Science.gov (United States)

    Aerts, R; Callaghan, T V; Dorrepaal, E; van Logtestijn, R S P; Cornelissen, J H C

    2012-11-01

    Litter decomposition and nutrient mineralization in high-latitude peatlands are constrained by low temperatures. So far, little is known about the effects of seasonal components of climate change (higher spring and summer temperatures, more snow which leads to higher winter soil temperatures) on these processes. In a 4-year field experiment, we manipulated these seasonal components in a sub-arctic bog and studied the effects on the decomposition and N and P dynamics of leaf litter of Calamagrostis lapponica, Betula nana, and Rubus chamaemorus, incubated both in a common ambient environment and in the treatment plots. Mass loss in the controls increased in the order Calamagrostis Litter chemistry showed within each incubation environment only a few and species-specific responses. Compared to the interspecific differences, they resulted in only moderate climate treatment effects on mass loss and these differed among seasons and species. Neither N nor P mineralization in the litter were affected by the incubation environment. Remarkably, for all species, no net N mineralization had occurred in any of the treatments during 4 years. Species differed in P-release patterns, and summer warming strongly stimulated P release for all species. Thus, moderate changes in summer temperatures and/or winter snow addition have limited effects on litter decomposition rates and N dynamics, but summer warming does stimulate litter P release. As a result, N-limitation of plant growth in this sub-arctic bog may be sustained or even further promoted.

  3. Atmospheric lead and heavy metal pollution records from a Belgian peat bog spanning the last two millenia. Human impact on a regional to global scale

    Energy Technology Data Exchange (ETDEWEB)

    De Vleeschouwer, Francois; Gerard, Laetitia; Fagel, Nathalie [URAP, Departement de Geologie, Universite de Liege, Allee du 6 Aout B18 Sart Tilman B4000 - Liege (Belgium); Goormaghtigh, Catherine; Mattielli, Nadine [Unite de recherche: ' ' Isotopes, Petrologie et Environnement' ' , Departement des Sciences de la Terre et de l' Environnement, CP 160/02 Universite Libre de Bruxelles, Avenue FD. Roosevelt, 50, B-1050 Bruxelles (Belgium); Le Roux, Gael [Institute of Environmental Geochemistry, University of Heidelberg, Im Neuenheimer Feld 236 B-69120 Heidelberg (Germany)

    2007-05-15

    Europe has been continuously polluted throughout the last two millennia. During the Roman Empire, these pollutions were mainly from ore extraction and smelting across Europe. Then, during the Middle Ages and the Early times of Industrial revolution (i.e. 1750), these pollutions extended to coal burning and combustion engine. Belgian ombrotrophic peat bogs have proved an effective archive of these pollutants and provide the opportunity to reconstruct the history of atmospheric deposition in NW Europe. The results of recent and past trace metal accumulation and Pb isotopes from a one-meter peat core (in the Misten peat bog) have been derived using XRF and Nu-plasma MC-ICP-MS. Combined with {sup 14}C and {sup 210}Pb dates these data have enabled us to trace fluxes in anthropogenic pollution back to original Roman times. Several periods of well-known Pb pollution events are clearly recorded including the Early and Late Roman Empire, the Middle Ages and the second industrial revolution. Also recorded is the introduction of leaded gasoline, and more recently the introduction of unleaded gasoline. Lead isotopes in this site have also enabled us to fingerprint several regional and global sources of anthropogenic particles. (author)

  4. Atmospheric lead and heavy metal pollution records from a Belgian peat bog spanning the last two millenia: Human impact on a regional to global scale

    Energy Technology Data Exchange (ETDEWEB)

    Vleeschouwer, Francois de [URAP, Departement de Geologie, Universite de Liege, Allee du 6 Aout B18 Sart Tilman B4000 - Liege (Belgium)]. E-mail: fdevleeschouwer@student.ulg.ac.be; Gerard, Laetitia [URAP, Departement de Geologie, Universite de Liege, Allee du 6 Aout B18 Sart Tilman B4000 - Liege (Belgium); Goormaghtigh, Catherine [Unite de recherche: ' Isotopes, Petrologie et Environnement' , Departement des Sciences de la Terre et de l' Environnement, CP 160/02 Universite Libre de Bruxelles, Avenue FD. Roosevelt, 50, B-1050 Bruxelles (Belgium); Mattielli, Nadine [Unite de recherche: ' Isotopes, Petrologie et Environnement' , Departement des Sciences de la Terre et de l' Environnement, CP 160/02 Universite Libre de Bruxelles, Avenue FD. Roosevelt, 50, B-1050 Bruxelles (Belgium); Le Roux, Gael [Institute of Environmental Geochemistry, University of Heidelberg, Im Neuenheimer Feld 236 B-69120 Heidelberg (Germany); Fagel, Nathalie [URAP, Departement de Geologie, Universite de Liege, Allee du 6 Aout B18 Sart Tilman B4000 - Liege (Belgium)

    2007-05-15

    Europe has been continuously polluted throughout the last two millennia. During the Roman Empire, these pollutions were mainly from ore extraction and smelting across Europe. Then, during the Middle Ages and the Early times of Industrial revolution (i.e. 1750), these pollutions extended to coal burning and combustion engine. Belgian ombrotrophic peat bogs have proved an effective archive of these pollutants and provide the opportunity to reconstruct the history of atmospheric deposition in NW Europe. The results of recent and past trace metal accumulation and Pb isotopes from a one-meter peat core (in the Misten peat bog) have been derived using XRF and Nu-plasma MC-ICP-MS. Combined with {sup 14}C and {sup 210}Pb dates these data have enabled us to trace fluxes in anthropogenic pollution back to original Roman times. Several periods of well-known Pb pollution events are clearly recorded including the Early and Late Roman Empire, the Middle Ages and the second industrial revolution. Also recorded is the introduction of leaded gasoline, and more recently the introduction of unleaded gasoline. Lead isotopes in this site have also enabled us to fingerprint several regional and global sources of anthropogenic particles.

  5. Lateglacial and early Holocene palaeoenvironmental 'events' in Sluggan Bog, Northern Ireland: comparisons with the Greenland NGRIP GICC05 event stratigraphy

    Science.gov (United States)

    Walker, Mike; Lowe, John; Blockley, Simon P. E.; Bryant, Charlotte; Coombes, Paul; Davies, Siwan; Hardiman, Mark; Turney, Chris S. M.; Watson, Jenny

    2012-03-01

    A multi-proxy Lateglacial environmental record is described from Sluggan Bog in County Antrim, Northern Ireland. Pollen, plant macrofossil, charcoal, sediment chemistry, stable isotope and sedimentological data provide a multi-faceted picture of local and regional environmental changes during the transition from the Last Cold Stage to the beginning of the present interglacial, and enable a series of distinctive palaeoenvironmental 'events' to be identified. A combination of radiometric and AMS radiocarbon dates on both humic and humin sediment fractions, and on charcoal fragments and plant macrofossils, provides one of the most closely-constrained radiocarbon timescales for any Lateglacial site in the British Isles. The evidence suggests that an initial period of warm conditions, beginning in the Sluggan record around 14.2 ka b2k (before AD 2000), and when open Salix-Betula woodland was locally present, was succeeded first by a heathland phase, then by a re-establishment of wood and scrub, before this was replaced during the later part of the Lateglacial (Woodgrange) Interstadial by species-rich grassland. In terms of timing, this sequence corresponds very closely to the GI-1e, GI-1d, GI-1c series of events in the Greenland NGRIP ice core. A short-lived Betula phase towards the end of the interstadial in the Sluggan sequence may reflect the short-lived climatic warming of GI-1a, although the radiocarbon age model suggests that it occurred prior to that event. There is a similar age discrepancy between the two sequences at the end of the interstadial with the onset of the Nahanagan (Younger Dryas) Stadial in Sluggan appearing to predate that in NGRIP by up to 200 yrs. By contrast, there is a very close correspondence between the date on the onset of the Holocene inferred from the pollen record in Sluggan (11.69 ka b2k) and the age of the Pleistocene-Holocene boundary (11.7 ka b2k) in NGRIP. While uncertainties remain over the climatic signals in the later

  6. Geophysical characterization of peatlands using crosshole GPR full-waveform inversion: Case study from a bog in northwestern Germany

    Science.gov (United States)

    Schmäck, J.; Klotzsche, A.; Van Der Kruk, J.; Vereecken, H.; Bechtold, M.

    2017-12-01

    The characterization of peatlands is of particular interest, since areas with peat soils represent global hotspots for the exchange of greenhouse gases. Their effect on global warming depends on several parameters, like mean annual water level and land use. Models of greenhouse gas emissions and carbon accumulation in peatlands can be improved by including small-scale soil properties that e.g. act as gas traps and periodically release gases to the atmosphere during ebullition events. Ground penetrating radar (GPR) is well suited to non- or minimal invasively characterize and improve our understanding of dynamic processes that take place in the critical zone. It uses high frequency electromagnetic waves to image and characterize the dielectric permittivity and electrical conductivity of the critical zone, which can be related to hydrogeological properties like porosity, soil water content, salinity and clay content. In the last decade, the full-waveform inversion of crosshole GPR data has proved to be a powerful tool to improve the image resolution compared to standard ray-based methods. This approach was successfully applied to several different aquifers and was able to provide decimeter-scale resolution images including small-scale high contrast layers that can be related to zones of high porosity, zones of preferential flow or clay lenses. The comparison to independently measured e.g. logging data proved the reliability of the method. Here, for the first time crosshole GPR full-waveform inversion is used to image three peatland plots with different land use that are part of the "Ahlen-Falkenberger Moor peat bog complex" in northwestern Germany. The full-waveform inversion of the acquired data returned higher resolution images than standard ray-based GPR methods, and, is able to improve our understanding of subsurface structures. The comparison of the different plots is expected to provide new insights into gas content and gas trapping structures across different

  7. Experimental Whole-Ecosystem Warming Alters Vegetation Phenology in a Boreal Spruce Bog: Initial Results from the SPRUCE Experiment

    Science.gov (United States)

    Richardson, A. D.

    2016-12-01

    Phenology is one of the most robust indicators of the biological impacts of global change. However, the response of phenology to future environmental conditions still remains highly uncertain because of the challenges associated with conducting realistic manipulative experiments. At the SPRUCE (Spruce and Peatland Responses Under Climatic and Environmental Change) experiment in the north-central United States, experimental temperature (0 to +9°C above ambient) and CO2 (ambient and elevated) treatments are being applied to mature, and intact, Picea mariana-Sphagnum spp. bog communities in their native habitat through the use of ten large (approximately 12 m wide, 10 m high) open-topped enclosures. We are tracking vegetation green-up and senescence in these chambers using repeat digital photography. Within each chamber, images are recorded every 30 minutes and uploaded to PhenoCam (http://phenocam.sr.unh.edu), where processed to yield quantitative measures of canopy color. These data are complemented by on-the-ground phenological data collected by human observers. Air warming treatments at SPRUCE began in August 2015. We observed a delay in senescence during autumn 2015 (2-5 days per degree of warming) and an advance in onset during spring 2016 (1-4 days per degree of warming). These patterns are robust across species and methods of phenological observation (i.e. camera-based vs. human observer). And, our results show very little evidence for photoperiod acting as a constraint on the response to warming. Early spring onset and consequent loss of frost hardiness in the warmest chambers proved disadvantageous when a brief period of extreme cold (to -12°C in the control chambers, to -3°C in the +9°C chambers) followed a month of generally mild weather. Foliage mortality for both Larix and Picea was immediate and severe, although both species subsequently re-flushed. These results give support for the hypothesis that warming may enhance the likelihood of spring frost

  8. Linking major and trace element headwater stream concentrations to DOC release and hydrologic conditions in a bog and peaty riparian zone

    Science.gov (United States)

    Broder, Tanja; Biester, Harald

    2017-04-01

    Peatlands and organic-rich riparian zones are known to export large amounts of dissolved organic carbon (DOC) to surface water. In organic-rich, acidic headwater streams main carriers for element export are dissolved organic matter (DOM) and organic-iron complexes. In this environment DOM might also act as major carrier for metals, which otherwise may have a low solubility. This study examines annual and short term event-based variations of major and trace elements in a headwater catchment. Patterns are used to trace hydrological pathways and element sources under different hydrologic preconditions. Furthermore, it elucidates the importance of DOC as carrier of different elements in a bog and a peaty riparian catchment. The study was conducted in a small headwater stream draining an ombrotrophic peatland with an adjacent forested area with peaty riparian soils in the Harz Mountains (Germany). Discharge sampling was conducted weekly at two sites from snowmelt to begin of snowfall and in high resolution during selected discharge events in 2013 and 2014. Element concentrations were measured by means of ICP-MS and ICP-OES. A PCA was performed for each site and for annual and event datasets. Results show that a large number of element concentrations strongly correlate with DOC concentrations at the bog site. Even elements like Ca and Mg, which are known to have a low affinity to DOC. Congruently, the first principal component integrates the DOC pattern (element loadings > 0.8: Ca, Fe, Mg, Mn, Zn, As, Sr, Cd, DOC) and explained about 35 % of total variance and even 50 % during rain events (loadings > 0.8: Al, Ca, Fe, Mg, Mn, Zn, Li, Co, As, Sr, Cd, Pb, DOC). The study cannot verify that all correlating elements bind to DOC. It is likely that also a common mobilization pattern in the upper peat layer by plant decomposition causes the same response to changes in hydrologic pathways. Additionally, a low mineral content and an enrichment of elements like Fe and Mn in the

  9. Sphagnum-dwelling testate amoebae in subarctic bogs are more sensitive to soil warming in the growing season than in winter: the results of eight-year field climate manipulations.

    NARCIS (Netherlands)

    Tsyganov, A.N.; Aerts, R.; Nijs, I.; Cornelissen, J.H.C.; Beyens, L.

    2012-01-01

    Sphagnum-dwelling testate amoebae are widely used in paleoclimate reconstructions as a proxy for climate-induced changes in bogs. However, the sensitivity of proxies to seasonal climate components is an important issue when interpreting proxy records. Here, we studied the effects of summer warming,

  10. Chemical composition, pH, and redox state of sulfur and iron in complete vertical porewater profiles from two Sphagnum peat bogs, Jura Mountains, Switzerland

    Science.gov (United States)

    Steinmann, Philipp; Shotyk, William

    1997-03-01

    Complete porewater profiles from two peat bogs in the Jura Mountains were analysed for major and trace inorganic anions and cations. At La Tourbière des Genevez (TGe) and Etang de la Gruère (EGr), peat formation began approximately 5,000 and 10,000 years BP, respectively. The maximum depths of peat accumulation are 140 cm (TGe) and 650 cm (EGr); previous geochemical studies showed that the ombrogenic sections of the bogs extend to depths of approximately 20 cm (TGe) and 250 cm (EGr). Water samples were obtained using in situ diffusion equilibrium samplers (peepers), which allow filtered (0.2 μm) porewaters to be obtained while preventing degassing and oxidation. These samplers were found to be well suited to bog porewaters and allowed volatile (dissolved CO 2, acetate) and redox-sensitive species (HS -, Fe 2+) to be quantified without further sample preparation or treatment. Aqueous species concentrations were determined immediately afterwards using ion chromatography with either conductivity (acetate, HCO 3-, Cl -, Br -, NO 3-, HPO 42-, SO 42-, Na +, NH 4+, K +, Mg 2+, Ca 2+), amperometry (HS -), or absorbance detection (Fe(III) and Fe(II)). The comprehensive analyses of anions and cations allowed humic substances to be calculated by the difference in electrical charge balance (i.e., the anion deficit). Concentrations of total dissolved CO 2 (2-12 mM) showed that carbonate equilibria play a significant role in the acid-base chemistry throughout the profiles. In near surface, ombrogenic porewaters with pH around 4, however, protons (approx. 160 μeq/L) are contributed mainly by the dissociation of humic substances (2-7 mM DOC). In the deepest, minerogenic layers H 2CO 3 is the predominant acid at both sites. At these depths, carbonate alkalinity (up to 3 meq/L at EGr, up to 8 meq/L at TGe) arises from reaction of the pore fluids with mineral matter in the underlying sediments. In the transition zone between the ombrogenic and minerogenic extremes, organic and

  11. Comparative ecosystem-atmosphere exchange of energy and mass in a European Russian and a central Siberian bog II. Interseasonal and interannual variability of CO2 fluxes

    International Nuclear Information System (INIS)

    Arneth, A.; Kolle, O.; Lloyd, J.; Schulze, E.D.; Kurbatova, J.; Vygodskaya, N.N.

    2002-01-01

    Net ecosystem-atmosphere exchange of CO 2 (NEE) was measured in two boreal bogs during the snow-free periods of 1998, 1999 and 2000. The two sites were located in European Russia (Fyodorovskoye), and in central Siberia (Zotino). Climate at both sites was generally continental but with more extreme summer-winter gradients in temperature at the more eastern site Zotino. The snow-free period in Fyodorovskoye exceeded the snow-free period at Zotino by several weeks. Marked seasonal and interannual differences in NEE were observed at both locations, with contrasting rates and patterns. Amongst the most important contrasts were: (1) Ecosystem respiration at a reference soil temperature was higher at Fyodorovskoye than at Zotino. (2) The diurnal amplitude of summer NEE was larger at Fyodorovskoye than at Zotino. (3) There was a modest tendency for maximum 24 h NEE during average rainfall years to be more negative at Zotino (-0.17 versus -0.15 mol/m 2 /d), suggesting a higher productivity during the summer months. (4) Cumulative net uptake of CO 2 during the snow-free period was strongly related to climatic differences between years. In Zotino the interannual variability in climate, and also in the CO 2 balance during the snow-free period, was small. However, at Fyodorovskoye the bog was a significant carbon sink in one season and a substantial source for CO 2 -C in the next, which was below-average dry. Total snow-free uptake and annual estimates of net CO 2 -C uptake are discussed, including associated uncertainties

  12. Dust is the dominant source of "heavy metals" to peat moss (Sphagnum fuscum) in the bogs of the Athabasca Bituminous Sands region of northern Alberta.

    Science.gov (United States)

    Shotyk, William; Bicalho, Beatriz; Cuss, Chad W; Duke, M John M; Noernberg, Tommy; Pelletier, Rick; Steinnes, Eiliv; Zaccone, Claudio

    2016-01-01

    Sphagnum fuscum was collected from twenty-five ombrotrophic (rain-fed) peat bogs surrounding open pit mines and upgrading facilities of Athabasca Bituminous Sands (ABS) in northern Alberta (AB) in order to assess the extent of atmospheric contamination by trace elements. As a control, this moss species was also collected at a bog near Utikuma (UTK) in an undeveloped part of AB and 264km SW of the ABS region. For comparison, this moss was also collected in central AB, in the vicinity of the City of Edmonton which is approximately 500km to the south of the ABS region, from the Wagner Wetland which is 22km W of the City, from Seba Beach (ca. 90km W) and from Elk Island National Park (ca. 45km E). All of the moss samples were digested and trace elements concentrations determined using ICP-SMS at a commercial laboratory, with selected samples also analyzed using instrumental neutron activation analysis at the University of Alberta. The mosses from the ABS region yielded lower concentrations of Ag, As, Bi, Cd, Cu, Pb, Sb, Tl, and Zn compared to the moss from the Edmonton area. Concentrations of Ni and Mo in the mosses were comparable in these two regions, but V was more abundant in the ABS samples. Compared with the surface vegetation of eight peat cores collected in recent years from British Columbia, Ontario, Quebec and New Brunswick, the mean concentrations of Ag, As, Bi, Cd, Cu, Mo, Ni, Pb, Sb, Tl and Zn in the mosses from the ABS region are generally much lower. In fact, the concentrations of these trace elements in the samples from the ABS region are comparable to the corresponding values in forest moss from remote regions of central and northern Norway. Lithophile element concentrations (Ba, Be, Ga, Ge, Li, Sc, Th, Ti, Zr) explain most of the variation in trace metal concentrations in the moss samples. The mean concentrations of Th and Zr are greatest in the moss samples from the ABS region, reflecting dust inputs to the bogs from open pit mines, aggregate

  13. Natural bog pine ecosystem in southern Germany is a steady and robust sink of CO2 but a minor source of CH4

    Science.gov (United States)

    Hommeltenberg, Janina; Schmid, Hans Peter; Droesler, Matthias; Werle, Peter

    2013-04-01

    Natural peatland ecosystems sequester carbon dioxide. They do this slowly but steadily, but also emit methane in small rates. Thus peatlands have both positive and negative greenhouse gas balance impacts on the climate system due to their influence on atmospheric CO2 and CH4 concentration. We present data of net ecosystem CO2 exchange (NEE) of almost three years (July 2010 to March 2013) and of methane fluxes over a period of nine months (July 2012 to March 2013), measured by eddy covariance technique in the bog forest "Schechenfilz". The site (47°48' N; 11°19' E, 590 m a.s.l.) is an ICOS-ecosystems associate site, located in the pre-alpine region of southern Germany, where a natural Pinus mugo rotundata forest grows on an undisturbed, almost 6 m thick peat layer. The slow growing bog pines and their low rates of carbon sequestration, in combination with high water table and thus low availability of oxygen, lead to low carbon dioxide fluxes. Photosynthesis as well as soil respiration are considerably attenuated compared to upland sites. Additionally, the high soil water content is damping the impact of dry and hot periods on CO2 exchange. Thus the CO2 balance is very robust to changing environmental parameters. While the CO2 exchange is clearly related to soil temperature and photosynthetic active radiation, we have not yet identified a parameter that governs variations in methane exchange. Various environmental parameters appear to be related to methane emissions (including soil moisture, soil and air temperature and wind direction), but the scatter with respect to half hourly methane fluxes is too large to be useful for gap modeling. Analysis of daily averages reduces the scatter, but since methane exchange exhibits considerable daily variation, daily averages are not useful to fill data gaps of half hourly fluxes. In consequence, as the daily course is the summary result of all environmental parameters having influence on the methane exchange at the half

  14. Sphagnum-dwelling testate amoebae in subarctic bogs are more sensitive to soil warming in the growing season than in winter: the results of eight-year field climate manipulations.

    Science.gov (United States)

    Tsyganov, Andrey N; Aerts, Rien; Nijs, Ivan; Cornelissen, Johannes H C; Beyens, Louis

    2012-05-01

    Sphagnum-dwelling testate amoebae are widely used in paleoclimate reconstructions as a proxy for climate-induced changes in bogs. However, the sensitivity of proxies to seasonal climate components is an important issue when interpreting proxy records. Here, we studied the effects of summer warming, winter snow addition solely and winter snow addition together with spring warming on testate amoeba assemblages after eight years of experimental field climate manipulations. All manipulations were accomplished using open top chambers in a dry blanket bog located in the sub-Arctic (Abisko, Sweden). We estimated sensitivity of abundance, diversity and assemblage structure of living and empty shell assemblages of testate amoebae in the living and decaying layers of Sphagnum. Our results show that, in a sub-arctic climate, testate amoebae are more sensitive to climate changes in the growing season than in winter. Summer warming reduced species richness and shifted assemblage composition towards predominance of xerophilous species for the living and empty shell assemblages in both layers. The higher soil temperatures during the growing season also decreased abundance of empty shells in both layers hinting at a possible increase in their decomposition rates. Thus, although possible effects of climate changes on preservation of empty shells should always be taken into account, species diversity and structure of testate amoeba assemblages in dry subarctic bogs are sensitive proxies for climatic changes during the growing season. Copyright © 2011 Elsevier GmbH. All rights reserved.

  15. Stratigraphy and chronology of a 15 ka sequence of multi-sourced silicic tephras in a montane peat bog, eastern North Island, New Zealand

    International Nuclear Information System (INIS)

    Lowe, D.J.; Newnham, R.M.; Ward, C.M.

    1999-01-01

    We document the stratigraphy, composition, and chronology of a succession of 16 distal, silicic tephra layers interbedded with lateglacial and Holocene peats and muds up to c. 15 000 radiocarbon years (c. 18 000 calendar years) old at a montane site (Kaipo Bog) in eastern North Island, New Zealand. Aged from 665 + or - 15 to 14 700 + or - 95 14 C yr BP, the tephras are derived from six volcanic centres in North Island, three of which are rhyolitic (Okataina, Taupo, Maroa), one peralkaline (Tuhua), and two andesitic (Tongariro, Egmont). Correlations are based on multiple criteria: field properties and stratigraphic interrelationships, ferromagnesian silicate mineral assemblages, glass-shard major element composition (from electron microprobe analysis), and radiocarbon dating. We extend the known distribution of tephras in eastern North Island and provide compositional data that add to their potential usefulness as isochronous markers. The chronostratigraphic framework established for the Kaipo sequence, based on both site-specific and independently derived tephra-based radiocarbon ages, provides the basis for fine-resolution paleoenvironmental studies at a climatically sensitive terrestrial site from the mid latitudes of the Southern Hemisphere. Tephras identified as especially useful paleoenvironmental markers include Rerewhakaaitu and Waiohau (lateglacial), Konini (late-glacial-early Holocene), Tuhua (middle Holocene), and Taupo and Kaharoa (late Holocene). (author). 102 refs., 3 tabs., 3 figs

  16. Anthropogenic impacts in North Poland over the last 1300 years - A record of Pb, Zn, Cu, Ni and S in an ombrotrophic peat bog

    International Nuclear Information System (INIS)

    De Vleeschouwer, Francois; Fagel, Nathalie; Cheburkin, Andriy; Pazdur, Anna; Sikorski, Jaroslaw; Mattielli, Nadine; Renson, Virginie; Fialkiewicz, Barbara; Piotrowska, Natalia; Le Roux, Gael

    2009-01-01

    Lead pollution history over Northern Poland was reconstructed for the last ca. 1300 years using the elemental and Pb isotope geochemistry of a dated Polish peat bog. The data show that Polish Pb-Zn ores and coal were the main sources of Pb, other heavy metals and S over Northern Poland up until the industrial revolution. After review of the potential mobility of each element, most of the historical interpretation was based on Pb and Pb isotopes, the other chemical elements (Zn, Cu, Ni, S) being considered secondary indicators of pollution. During the last century, leaded gasoline also contributed to anthropogenic Pb pollution over Poland. Coal and Pb-Zn ores, however, remained important sources of pollution in Eastern European countries during the last 50 years, as demonstrated by a high 206 Pb/ 207 Pb ratio (1.153) relative to that of Western Europe (ca. 1.10). The Pb data for the last century were also in good agreement with modelled Pb inventories over Poland and the Baltic region.

  17. Landscape dynamics and fire activity since 6740 cal yr BP in the Cantabrian region (La Molina peat bog, Puente Viesgo, Spain)

    Science.gov (United States)

    Pérez-Obiol, R.; García-Codron, J. C.; Pèlachs, A.; Pérez-Haase, A.; Soriano, J. M.

    2016-03-01

    A lack of paleobotanic studies with adequate resolution and multiproxy approaches has limited proper discussion of vegetation dynamics in Cantabria and of the role of fires in the configuration of the plant landscape during the Holocene in the northwest part of the Iberian peninsula. The pollen diagram of La Molina peat bog in Puente Viesgo (43°15‧38″ N-3°58‧37″ W; ETRS89), located at 484 m.a.s.l., and the study of its sedimentary charcoals allowed the acquisition of a continuous and thorough fire sequence for the last 6700 cal yr BP and an understanding of its relationship to the forest. The results show the importance of human influence on the incidence and characteristics of fire activity during the different phases studied: the Neolithic, Bronze Age, Iron Age, Roman period, and Middle Ages. A synergy seems to exist between dry climate periods (especially during Bond events 3 and 4) and a greater presence of biomass. As the Holocene advances, vegetation coverage clearly tends to decrease. This study provides key elements for understanding the role of fire activity in the forest dynamics of deciduous and evergreen Quercus, Corylus, Pinus, Fagus, and Alnus and demonstrates the strongly artificialized character of the present landscape.

  18. Rapid peat accumulation favours the occurrence of both fen and bog microbial communities within a Mediterranean, free-floating peat island.

    Science.gov (United States)

    Concheri, Giuseppe; Stevanato, Piergiorgio; Zaccone, Claudio; Shotyk, William; D'Orazio, Valeria; Miano, Teodoro; Piffanelli, Pietro; Rizzi, Valeria; Ferrandi, Chiara; Squartini, Andrea

    2017-08-17

    The unique environment of a 4m-thick, free-floating peat island within the Posta Fibreno lake (Central Italy) was analyzed using DNA-based techniques to assess bacterial and fungal community members identity and abundance. Two depths were sampled at 41 and 279 cm from the surface, the former corresponding to an emerged portion of Sphagnum residues accumulated less than 30 yrs ago, and the latter mainly consisting of silty peat belonging to the deeply submerged part of the island, dating back to 1520-1660 AD. The corresponding communities were very diverse, each of them dominated by a different member of the Delta-proteobacteria class for prokaryotes. Among Eukaryotes, Ascomycota prevailed in the shallow layer while Basidiomycota were abundant in the deep sample. The identity of taxa partitioning between acidic surface layer and neutral core is very reminiscent of the differences reported between bogs and fens respectively, supporting the view of Posta Fibreno as a relic transitional floating mire. Moreover, some microbial taxa show an unusual concurrent species convergence between this sub-Mediterranean site and far Nordic or circumpolar environments. This study represents the first report describing the biotic assemblages of such a peculiar environment, and provides some insights into the possible mechanisms of its evolution.

  19. A 15 000-year record of climate change in northern New Mexico, USA, inferred from isotopic and elemental contents of bog sediments

    Science.gov (United States)

    Cisneros-Dozal, L. M.; Heikoop, J.M.; Fessenden, J.; Anderson, R. Scott; Meyers, P.A.; Allen, Craig D.; Hess, M.; Larson, T.; Perkins, G.; Rearick, M.

    2010-01-01

    Elemental (C, N, Pb) and isotopic (δ13C, δ15N) measurements of cored sediment from a small bog in northern New Mexico reveal changes in climate during the Late Pleistocene and Holocene. Abrupt increases in Pb concentration and δ13C values ca. 14 420 cal. YBP indicate significant runoff to the shallow lake that existed at that time. Weathering and transport of local volcanic rocks resulted in the delivery of Pb-bearing minerals to the basin, while a 13C-enriched terrestrial vegetation source increased the δ13C values of the sedimentary material. Wet conditions developed over a 300 a period and lasted for a few hundred years. The Younger Dryas period (ca. 12 700–11 500 cal. YBP) caused a reduction in terrestrial productivity reflected in decreasing C/N values, δ15N values consistently greater than 0‰ and low organic content. By contrast, aquatic productivity increased during the second half of this period, evidenced by increasing δ13C values at the time of highest abundance of algae. Dry conditions ca. 8 000–6 000 cal. YBP were characterised by low organic carbon content and high Pb concentrations, the latter suggesting enhanced erosion and aeolian transport of volcanic rock. The range in δ13C, δ15N and C/N values in the sedimentary record fall within the range of modern plants, except during the periods of runoff and drought. The sedimentary record provides evidence of natural climate variability in northern New Mexico, including short- (multi-centennial) and long-(millennial) term episodes during the Late Pleistocene and Holocene.

  20. Nitrogen cycling in ombrotrophic peat bogs in the Czech Republic: Is microbial N-fixation occurring at atmospheric depositions of reactive N higher than 10 kg/ha/yr?

    Science.gov (United States)

    Novak, Martin; Jackova, Ivana; Cejkova, Bohuslava; Buzek, Frantisek; Curik, Jan; Stepanova, Marketa; Prechova, Eva; Veselovsky, Frantisek; Komarek, Arnost

    2017-04-01

    Biogeochemical cycling of carbon (C) and nitrogen (N) in peat bogs are coupled. Whereas at low pollution levels, reactive nitrogen (Nr, mainly nitrate- and ammonium-N) inputs may positively affect C storage, high Nr deposition may have a detrimental effect on C storage. We have previously reported N isotope systematics at two ombrotrophic peat bogs in the Czech Republic, receiving medium levels of Nr of about 10 kg/ha/yr via atmospheric deposition. Nitrogen of living Sphagnum was systematically heavier than N of the atmospheric input (p water prior to the 15N-N2 incubation has led to a slight further increase in del15N of Sphagnum. Also in 2016, we monitored del15N of atmospheric deposition at three medium Nr-polluted peat bogs. Open-area precipitation had the following mean del 15N values: Uhlirska -6.1 per mil (NH4) and -6.2 per mil (NO3); Brumiste -1.7 per mil (NH4) and -3.4 per mil (NO3); Male Mechove Jezirko -3.3 per mil (NH4) and -3.9 per mil (NO3). At all sites, atmospheric Nr deposition was made up by NO3-N and NH4-N in a roughly 1.1 ratio. We found that N of winter-time deposition became isotopically extremely light (less than -10.0 per mil). During the growing season, del15N of total atmospheric input was higher, closer to 0.0 per mil, but still slightly lower than del15N of living Sphagnum. These data thus confirm a N isotope discrepancy between the N isotope signature of deposition and Sphagnum. In the paper, we will also discuss a mass balance discrepancy in long-term atmospheric N input and N storage at the Czech sites, determined for replicated, lead-210 dated peat cores. We took into consideration a 30 % contribution of horizontal deposition (mainly fog interception), which we had directly measured, to total Nr deposition. Still, the dated peat cores appeared to accumulate 30 to 60 % more N than the maximum estimated atmospheric Nr input (both estimates for the period 1900-2015). Preliminarily, we conclude that three independent lines of evidence

  1. Fimbriiglobus ruber gen. nov., sp. nov., a Gemmata-like planctomycete from Sphagnum peat bog and the proposal of Gemmataceae fam. nov.

    Science.gov (United States)

    Kulichevskaya, Irina S; Ivanova, Anastasia A; Baulina, Olga I; Rijpstra, W Irene C; Sinninghe Damsté, Jaap S; Dedysh, Svetlana N

    2017-02-01

    An aerobic, budding, dark pink to red-pigmented bacterium was isolated from an acidic boreal Sphagnum peat bog and designated strain SP5T. Cells of this strain were non-motile spheres that were uniformly covered with crateriform pits and fimbria, and tended to form aggregates during growth in liquid media. Strain SP5T was capable of growth between pH 4.0 and pH 6.8 (optimum at pH 5.5-6.0) and at temperatures between 10 and 30 °C (optimum at 20-25 °C). The preferred growth substrates were sugars and some heteropolysaccharides. The major fatty acids were C20 : 1ω9c, C16 : 1ω9c and C16 : 0, and the major polar lipid was trimethylornithine. Cells contained also significant amounts of bound (ω-1)OH-C30 : 1 fatty acid. The quinone was menaquinone-6, and the G+C content of the DNA was 60.7 mol%. Strain SP5T was a member of the order Planctomycetales and belonged to the phylogenetic lineage defined by the genus Gemmata. It displayed 88 and 89 % 16S rRNA gene sequence similarity to Gemmata obscuriglobusUQM 2246T and 'Gemmata massiliana' IIL30, 89 % to Zavarzinella formosa A10T and 86 % to Telmatocola sphagniphila SP2T. However, strain SP5T differed from members of these genera by cell morphology, substrate utilization pattern and fatty acid composition. Based on these data, the novel isolate should be considered as representing a novel species of a new genus of planctomycetes, for which the name Fimbriiglobus ruber gen. nov., sp. nov, is proposed. The type strain is SP5T (=LMG 29572T=VKM B-3045T). We also suggest the establishment of a novel family, Gemmataceaefam. nov., which includes the phylogenetically related genera Gemmata, Zavarzinella, Telmatocola and Fimbriiglobus.

  2. Life in Ice: Microbial Growth Dynamics and Greenhouse Gas Production During Winter in a Thermokarst Bog Revealed by Stable Isotope Probing Targeted Metagenomics

    Science.gov (United States)

    Blazewicz, S.; White, R. A., III; Tas, N.; Euskirchen, E. S.; Mcfarland, J. W.; Jansson, J.; Waldrop, M. P.

    2016-12-01

    Permafrost contains a reservoir of frozen C estimated to be twice the size of the current atmospheric C pool. In response to changing climate, permafrost is rapidly warming which could result in widespread seasonal thawing. When permafrost thaws, soils that are rich in ice and C often transform into thermokarst wetlands with anaerobic conditions and significant production of atmospheric CH4. While most C flux research in recently thawed permafrost concentrates on the few summer months when seasonal thaw has occurred, there is mounting evidence that sizeable portions of annual CO2 and CH4 efflux occurs over winter or during a rapid burst of emissions associated with seasonal thaw. A potential mechanism for such efflux patterns is microbial activity in frozen soils over winter where gasses produced are partially trapped within ice until spring thaw. In order to better understand microbial transformation of soil C to greenhouse gas over winter, we applied stable isotope probing (SIP) targeted metagenomics combined with process measurements and field flux data to reveal activities of microbial communities in `frozen' soil from an Alaskan thermokarst bog. Field studies revealed build-up of CO2 and CH4 in frozen soils suggesting that microbial activity persisted throughout the winter in soils poised just below the freezing point. Laboratory incubations designed to simulate in-situ winter conditions (-1.5 °C and anaerobic) revealed continuous CH4 and CO2 production. Strikingly, the quantity of CH4 produced in 6 months in frozen soil was equivalent to approximately 80% of CH4 emitted during the 3 month summer `active' season. Heavy water SIP targeted iTag sequencing revealed growing bacteria and archaea in the frozen anaerobic soil. Growth was primarily observed in two bacterial phyla, Firmicutes and Bacteroidetes, suggesting that fermentation was likely the major C mineralization pathway. SIP targeted metagenomics facilitated characterization of the primary metabolic

  3. How do climate and human impact affect Sphagnum peatlands under oceanic-continental climatic conditions? 2000 years of fire and hydrological history of a bog in Northern Poland

    Science.gov (United States)

    Marcisz, Katarzyna; Tinner, Willy; Colombaroli, Daniele; Kołaczek, Piotr; Słowiński, Michał; Fiałkiewicz-Kozieł, Barbara; Lamentowicz, Mariusz

    2014-05-01

    Climate change affects many natural processes and the same applies to human impact For instance climate change and anthropogenic activities may cause increased fire activity or change peatland dynamics. Currently it is still unknown how Sphagnum peatlands in the oceanic-continental transition zone of Poland may respond to combined effects of heat waves, drought and fire. The aim of the study was to reconstruct the last 2000 years palaeohydrology and fire history at Linje bog in Northern Poland. The main task was to determine the drivers of fire episodes, particularly to identify climatic and anthropogenic forcing. A two-meter peat core was extracted and subsampled with a high resolution. Micro- and macroscopic charcoal analyses were applied to determine past fire activity and the results compared with palaeohydrological reconstructions based on testate amoeba analysis. Palynological human indicators were used to reconstruct human activity. A depth-age model including 20 14C dates was constructed to calculate peat accumulation rates and charcoal influx. We hypothesised that: 1) fire frequency in Northern Poland was determined by climatic conditions (combination of low precipitation and heat waves), as reflected in peatland water table, and that 2) past fire episodes in the last millennium were intensified by human activity. Furthermore climate may have influenced human activity over harvest success and the carrying capacity. Our study shows that fire was important for the studied ecosystem, however, its frequency has increased in the last millennium in concomitance with land use activities. Landscape humanization and vegetation opening were followed by a peatland drying during the Little Ice Age (from ca. AD 1380). Similarly to other palaeoecological studies from Poland, Linje peatland possessed an unstable hydrology during the Little Ice Age. Increased fire episodes appeared shortly before the Little Ice Age and most severe fires were present in the time when

  4. Small scale soil carbon and moisture gradients in a drained peat bog grassland and their influence on CO2, CH4 and N2O fluxes

    Science.gov (United States)

    Leiber-Sauheitl, K.; Fuß, R.; Freibauer, A.

    2012-04-01

    Due to the UNFCCC report requirements of each country on the emissions of greenhouse gases from key sources the joint research project "Organic Soils" was established in Germany. The project's objective is to improve the data set on greenhousegas emissions from organic soils in Germany. Within 12 German Project Catchments emissions from different types of organic soils, e.g. under different land uses and hydrological conditions, are measured. At the location "Großes Moor" near Gifhorn (Lower Saxony) the effects of small-scale soil organic carbon and groundwater level gradients on the GHG fluxes (CO2, CH4 and N2O) are quantified. The study area is located within a former peat bog altered by drainage and peat cutting, which is currently grassland under extensive agricultural use. The focus of the study is on the acquisition of CO2, CH4 and N2O fluxes on six sites via manual closed chambers. In order to calculate the annual CO2 exchange rate, values are interpolated on a 0.5 hour scale between measurement campaigns. In combination with continually logged meteorological parameters, such as the photosynthetic active radiation as well as air and soil temperatures, we calculate the daily CO2 ecosystem exchange of the different sites. During the 2011 campaign, CO2 was determined as the most important greenhouse gas. The groundwater table was the dominant variable influencing gas emissions. Another important factor was the vegetation composition. In detail, highest CO2 emissions occurred with a water table of 40-50 cm below ground level, temperatures above 10°C and low plant biomass amounts. Due to the more complex formation of N2O by a number of processes, each being promoted by different soil conditions, the measurement of N2O fluxes in the field was complemented by a laboratory experiment. In this, the use of stable isotope tracer techniques enabled us to quantify the contribution of single biochemical pathways to the overall formation of N2O under controlled

  5. Methylocella palustris gen. nov., sp. nov., a new methane-oxidizing acidophilic bacterium from peat bogs, representing a novel subtype of serine-pathway methanotrophs.

    Science.gov (United States)

    Dedysh, S N; Liesack, W; Khmelenina, V N; Suzina, N E; Trotsenko, Y A; Semrau, J D; Bares, A M; Panikov, N S; Tiedje, J M

    2000-05-01

    A new genus, Methylocella, and a new species, Methylocella palustris, are proposed for three strains of methane-oxidizing bacteria isolated from acidic Sphagnum peat bogs. These bacteria are aerobic, Gram-negative, colourless, non-motile, straight and curved rods that utilize the serine pathway for carbon assimilation, multiply by normal cell division and contain intracellular poly-beta-hydroxybutyrate granules (one at each pole). These strains use methane and methanol as sole sources of carbon and energy and are moderately acidophilic organisms with growth between pH 4.5 and pH 7.0, the optimum being at pH 5.0-5.5. The temperature range for growth is 10-28 degrees C with the optimum at 15-20 degrees C. The intracytoplasmic membrane system is different from those of type I and II methanotrophs. Cells contain an extensive periplasmic space and a vesicular membrane system connected to the cytoplasmic membrane. The strains grew only on media with a low salt content (0.2-0.5 g l(-1)). All three strains were found to possess soluble methane monooxygenase and are able to fix atmospheric nitrogen via an oxygen-sensitive nitrogenase. No products were observed in a PCR with particulate methane monooxygenase-targeted primers; hybridization with a pmoA probe was also negative. The major phospholipid fatty acids are 18:1 acids. The G+C content of the DNA is 61.2 mol%. The three strains share identical 16S rRNA gene sequences and represent a novel lineage of methane-oxidizing bacteria within the alpha-subclass of the class Proteobacteria and are only moderately related to type II methanotrophs of the Methylocystis-Methylosinus group. The three strains are most closely related to the acidophilic heterotrophic bacterium Beijerinckia indica subsp. indica (96.5% 16S rDNA sequence similarity). Collectively, these strains comprise a new species and genus Methylocella palustris gen. nov., sp. nov.; strain KT (= ATCC 700799T) is the type strain.

  6. Turfeiras da Serra do Espinhaço Meridional - MG: I - caracterização e classificação Peat bogs of the Serra do Espinhaço Meridional - Minas Gerais, Brazil: I - characterization and classification

    Directory of Open Access Journals (Sweden)

    Alexandre Christófaro Silva

    2009-10-01

    Full Text Available As turfeiras são ambientes especiais para estudos relacionados com a dinâmica da matéria orgânica, evolução das paisagens, mudanças climáticas e ciclos de poluição atmosférica locais, regionais e globais. Elas contribuem para o sequestro global de carbono, funcionam como reservatórios de água e constituem o ambiente de uma biodiversidade endêmica. A Serra do Espinhaço Meridional (SdEM, "Reserva da Biosfera Terrestre", apresenta uma área significativa formada por diferentes tipos de turfeira, que foram descritas em três perfis, situados a 1.250 m (P1, 1.800 m (P2 e 1.350 m (P4 de altitude e classificados respectivamente como Organossolo Háplico Sáprico térrico (P1, Organossolo Háplico Fíbrico típico (P2 e Organossolo Háplico Hêmico típico (P4, de acordo com o Sistema Brasileiro de Classificação de Solos. Os três perfis foram caracterizados morfologicamente e, nas amostras coletadas, foram realizadas análises químicas, físicas e microbiológicas. Verificou-se que a localização, a altitude e a drenagem influenciaram os atributos morfológicos, físicos, químicos e microbiológicos das turfeiras da SdEM. O estádio de decomposição da matéria orgânica é mais avançado com a melhoria da drenagem nas turfeiras. O teor de metais pesados está relacionado com o teor e a composição granulométrica da fração mineral e com a localização das turfeiras. O perfil P1 apresentou os mais elevados teores médios de Ti, Zr e Pb; em P2 foram detectados os teores médios mais elevados de Mn, Zn e Cu; e o teor médio de Fe é mais elevado em P4. A intensidade da atividade microbiológica das turfeiras P2 e P4 relacionou-se com sua drenagem e com o teor de metais pesados de suas camadas.Peat bogs are a special environment for studies related with the dynamics of organic matter, landscape evolution and climatic changes and with local, regional and global cycles of atmospheric pollution. Peat bogs contribute to the global C

  7. Debatartikel om Hanne Sanders bog

    DEFF Research Database (Denmark)

    Eriksen, Sidsel

    1997-01-01

    Artiklen påpeger, at Hanne Sanders kun vanskeligt kan sammenligne de svenske og danske vækkelser uden at inddrage den angloamerikanske vækkelsesreligiøsitet, som spiller en enorm rolle for udbredelsen af de svenske vækkelser i hele 1800-tallet og bl.a. resulterede i en omfattende frikirkedannelse...

  8. Integrating the EMPD with an Alpine altitudinal training set to reconstruct climate variables in Holocene pollen records from high-altitude peat bogs

    Science.gov (United States)

    Furlanetto, Giulia; Badino, Federica; Brunetti, Michele; Champvillair, Elena; De Amicis, Mattia; Maggi, Valter; Pini, Roberta; Ravazzi, Cesare; Vallé, Francesca

    2016-04-01

    Temperatures and precipitation are the main environmental factors influencing vegetation and pollen production. Knowing the modern climate optima and tolerances of those plants represented in fossil assemblages and assuming that the relationships between plants and climate in the past are not dissimilar from the modern ones, fossil pollen records offer many descriptors to reconstruct past climate variables. The aim of our work is to investigate the potential of high-altitude pollen records from an Alpine peat bog (TBValter, close to the Ruitor Glacier, Western Italian Alps) for quantitative paleoclimate estimates. The idea behind is that high-altitude ecosystems are more sensitive to climate changes, especially to changes in July temperatures that severely affect the timberline ecotone. Meantime, we met with difficulties when considering the factors involved in pollen dispersal over a complex altitudinal mountain pattern, such as the Alps. We used the EMPD-European Modern Pollen Database (Davis et al., 2013) as modern training set to be compared with our high-altitude fossil site. The EMPD dataset is valuable in that it provides a large geographic coverage of main ecological and climate gradients (at sub-continental scale) but lacks in sampling of altitudinal gradients and high-altitude sites in the Alps. We therefore designed an independent altitudinal training set for the alpine valley hosting our fossil site. 27 sampling plots were selected along a 1700m-elevational transect. In a first step, each plot was provided with (i) 3 moss polsters collected following the guidelines provided by Cañellas-Boltà et al. (2009) and analyzed separately to account for differences in pollen deposition at small scale, (ii) morphometrical parameters obtained through a high-resolution DEM, and (iii) temperature and precipitation were estimated by means of weighted linear regression of the meteorological variable versus elevation, locally evaluated for each site (Brunetti et al

  9. Determination of (239)Pu, (240)Pu, (241)Pu and (242)Pu at femtogram and attogram levels - evidence for the migration of fallout plutonium in an ombrotrophic peat bog profile.

    Science.gov (United States)

    Quinto, Francesca; Hrnecek, Erich; Krachler, Michael; Shotyk, William; Steier, Peter; Winkler, Stephan R

    2013-04-01

    The isotopic composition of plutonium ((239)Pu, (240)Pu, (241)Pu and (242)Pu) was investigated in a ∼0.5 m long peat core from an ombrotrophic bog (Black Forest, Germany) using clean room procedures and accelerator mass spectrometry (AMS). This sophisticated analytical approach was ultimately needed to detect reliably the Pu concentrations present in the peat samples at femtogram (fg) and attogram (ag) levels. The mean (240)Pu/(239)Pu isotopic ratio of 0.19 ± 0.02 (N = 32) in the peat layers, representing approximately the last 80 years, was in good agreement with the accepted value of 0.18 for the global fallout in the Northern Hemisphere. This finding is largely supported by the corresponding and rather constant (241)Pu/(239)Pu (0.0012 ± 0.0005) and (242)Pu/(239)Pu (0.004 ± 0.001) ratios. Since the Pu isotopic composition characteristic of the global fallout was also identified in peat samples pre-dating the period of atmospheric atom bomb testing (AD 1956-AD 1980), migration of Pu within the peat profile is clearly indicated. These results highlight, for the first time, the mobility of Pu in a peat bog with implications for the migration of Pu in other acidic, organic rich environments such as forest soils and other wetland types. These findings constitute a direct observation of the behaviour of Pu at fg and ag levels in the environment. The AMS measurements of Pu concentrations (referring to a corresponding activity of (240+239)Pu from 0.07 mBq g(-1) to 5 mBq g(-1)) essentially confirm our a priori estimates based on existing (241)Am and (137)Cs data in the investigated peat core and agree well with the global fallout levels from the literature. Exclusively employing the Pu isotope ratios established for the peat samples, the date of the Pu irradiation (AD 1956, correctable to AD 1964) was calculated and subsequently compared to the (210)Pb age of the peat layers; this comparison provided an additional hint that global fallout derived Pu is not fixed in

  10. Multivariate study of trace element distribution in the geological record of Roñanzas Peat Bog (Asturias, N. Spain). Paleoenvironmental evolution and human activities over the last 8000 calyr BP.

    Science.gov (United States)

    Gallego, José Luis R; Ortiz, José E; Sierra, Carlos; Torres, Trinidad; Llamas, J F

    2013-06-01

    Trace element concentrations in the Roñanzas peat bog record reveal a contribution of natural processes but the influence of anthropogenic factors predominates in the last two millenniums, particularly aerosol deposition linked to mining and industrial activities in northern Spain. We observed that the Roñanzas record can be considered a preserved environment, suitable to search for local (major elements. Our study design represents a novel approach to assign natural vs. human contributions in peatlands. Therefore, synergies obtained by the simultaneous study of multivariate statistics and enrichment factors allow robust conclusions about paleoenvironmental evolution and human activities. Anthropogenic influence has also been reported in similar records in other parts of Europe, thereby suggesting large-scale sources for atmospheric pollution. However, here we revealed remarkable particularities, such as the association of Cd, Zn and Pb, mainly linked to regional and local factors (mining and more recently the metallurgical industry), whereas we propose that the occurrence of Hg is associated with a combination of regional factors and global atmospheric pollution. Copyright © 2013 Elsevier B.V. All rights reserved.

  11. Fate of N in a peatland, Whim bog: immobilisation in the vegetation and peat, leakage into pore water and losses as N2O depend on the form of N

    Science.gov (United States)

    Sheppard, L. J.; Leith, I. D.; Leeson, S. R.; van Dijk, N.; Field, C.; Levy, P.

    2013-01-01

    Peatlands represent a vast carbon reserve that has accumulated under conditions of low nitrogen availability. Given the strong coupling between the carbon and nitrogen cycles, we need to establish the consequences of the increase in reactive nitrogen deposition for the sustainability of peatlands, and whether the form in which the nitrogen is deposited makes a difference. We have addressed these questions using a globally unique field simulation of reactive N deposition as dry deposited ammonia and wet deposited reduced N, ammonium and oxidised N, nitrate, added as ammonium chloride or sodium nitrate, to an ombrotrophic peatland, Whim bog in SE Scotland. Here we report the fate of 56 kg N ha-1 yr-1 additions over 10 yr and the consequences. The effects of 10 yr of reactive N additions depended on the form in which the N was applied. Ammonia-N deposition caused the keystone Sphagnum species, together with the main shrub Calluna and the pleurocarpous mosses, to disappear, exposing up to 30% of the peat surface. This led to a significant increase in soil water nitrate and nitrous oxide emissions. By contrast wet deposited N, despite significantly reducing the cover of Sphagnum and Pleurozium moss, did not have a detrimental effect on Calluna cover nor did it significantly change soil water N concentrations or nitrous oxide emissions. Importantly 10 yr of wet deposited N did not bare the peat surface nor significantly disrupt the vegetation enabling the N to be retained within the carbon rich peatland ecosystems. However, given the significant role of Sphagnum in maintaining conditions that retard decomposition, this study suggests that all nitrogen forms will eventually compromise carbon sequestration by peatlands through loss of some keystone Sphagnum species.

  12. Late-Holocene hydroclimate and atmospheric circulation variability in southern Patagonia: insights from triple stable isotopes (δ18O, δ13C, δD) of peat bog Sphagnum moss

    Science.gov (United States)

    Xia, Z.; Yu, Z.; Zheng, Y.; Loisel, J.; Huang, Y.

    2017-12-01

    The Southern Hemisphere Westerly Winds (SHWWs) exert important influences on regional and global climates, but their long-term behaviors and dynamics are still poorly understood but critical for projecting future changes. Here we present a 5,500-year record from a Sphagnum-dominated peat bog located on the lee side of the Andes at 54.2 °S in southern Patagonia—based on plant macrofossils, Sphagnum cellulose δ18O and δ13C, and lipid δD data—to document and understand the variability in hydroclimate and atmospheric circulation. There is a striking negative correlation between cellulose δ18O and the Southern Annular Mode (SAM) index over the last millennium; particularly the 2.5‰ negative shift of δ18O is concurrent with the observed positive trend in the SAM over the recent decades. The interval of Medieval Climate Anomaly (MCA, 850-600 yr BP) is characterized by a 2.5‰ negative shift of δ18O and low δ13C values, while the Little Ice Age (LIA, 500-300 yr BP) is characterized by a 2.5‰ positive shift of δ18O and high δ13C values. Furthermore, we find the largest negative shift of δ18O ( 3‰) at 2,300 yr BP, suggesting a significantly positive shift in the SAM. We interpret high Sphagnum abundance and high cellulose δ13C values to reflect great moss moisture conditions, while cellulose δ18O variations primarily reflect moisture sources and atmospheric circulation. During the positive phase of SAM (e.g., the MCA and recent decades), strengthened SHWWs enhance the rain-shadow effect, resulting in dry climate and 18O-depleted precipitation (low δ18O values) in the study region. During the negative phase of SAM (e.g., the LIA), weakened SHWWs reduce rain-shadow effect, resulting in wet climate and high δ18O values caused by increases in moisture contributions from the southerly and easterly flows that do not experience strong Rayleigh distillation process during air mass transports. Furthermore, coupling cellulose δ18O and lipid δD enables

  13. Ground penetrating radar (GPR) evidence for variations in free phase carbon gas accumulation as a function of peatland landforms: a comparison between near-crest bogs and mid-slope lawns

    Science.gov (United States)

    Parsekian, A.; Slater, L.; Comas, X.; Nolan, J.; Glaser, P.

    2009-05-01

    Northern peatlands serve as atmospheric sources of biogenic free-phase gas (FPG) produced under anaerobic conditions below the water table (mostly methane and carbon dioxide). Recent evidence suggest that FPG accumulates in the subsurface under confining layers and is released during sudden ebullition events, often triggered by sudden drops in atmospheric pressure. Accurate quantification of the impact of FPG releases on the global carbon budget is needed given recent observations of increasing atmospheric methane concentrations. One important step towards understanding the dynamics of FPG in peatlands is to investigate whether certain peatland landforms (i.e. areas with significantly different vegetation patterns) may be more conducive to FPG accumulation and/or release. Additionally, it is important to determine the vertical distribution of FPG within the peat soil and the potential role of peat stratigraphy on gas accumulation and release. In this study, we used common mid-point (CMP) velocity surveys to predict vertical profiles of FPG accumulations by comparing two different peatland landforms: historically forested near-crest bogs and non- forested mid-slope lawns in the Glacial Lake Agassiz Peatland of Minnesota, USA. We show that there is a statistically significant difference in electromagnetic (EM) wave velocities calculated over gas-rich intervals in the peat strata compared to gas-poor intervals. Common-offset radar profiles identified laterally continuous woody confining layers responsible for FPG accumulation. Chaotic GPR facies containing diffraction hyperbolae at the forested near-crest sites are interpreted as deformation of the peat matrix due to FPG accumulation and/or peat fabric disturbance during FPG release events. In contrast, non-forested mid-slope lawn sites, are characterized by planar GPR facies with no evidence of peat fabric disturbance and small relative changes in interpreted EM velocity distribution along the peat column. Using the

  14. Variation in photosynthetic properties among bog plants

    Czech Academy of Sciences Publication Activity Database

    Korrensalo, A.; Hájek, Tomáš; Vesala, T.; Mehtätalo, L.; Tuittila, E. S.

    2016-01-01

    Roč. 94, č. 12 (2016), s. 1127-1139 ISSN 1916-2790 Institutional support: RVO:67985939 Keywords : CO2 * photosynthesis rate * plant functional types Subject RIV: EH - Ecology, Behaviour Impact factor: 1.224, year: 2016

  15. Bog Stvoritelj u djelu Charlesa Darwina

    OpenAIRE

    Balabanić, Josip

    2009-01-01

    U ovome članku traži se odgovor na pitanje zašto u djelu Charlesa Darwina (1809-1882) ima iznenađujuća količina izravna teološkog sadržaja i zašto je, premda pristaša znanstvenog redukcionizma, u svoja kapitalna djela Postanak vrsta (1859) i Podrijetlo čovjeka (1871) unio egzistencijalnu dimenziju vlastita religioznog stajališta o Bogu kao stvoritelju putem sekundarnih uzroka (tj. prirodnih zakona). Na temelju njegovih izjava i navoda iz Autobiografje izvodi se zaključak kako Darwin Stvoritel...

  16. Insect biodiversity of boreal peat bogs

    Czech Academy of Sciences Publication Activity Database

    Spitzer, Karel; Danks, H. V.

    2006-01-01

    Roč. 51, - (2006), s. 137-161 ISSN 0066-4170 R&D Projects: GA ČR(CZ) GA206/97/0077; GA AV ČR(CZ) IBS5007015 Institutional research plan: CEZ:AV0Z50070508 Keywords : peatlands * tyrphobiontic insect s * conservation Subject RIV: EH - Ecology, Behaviour Impact factor: 8.714, year: 2006

  17. Bedste bog om Balkans beskidte krig

    DEFF Research Database (Denmark)

    Lund, Joachim

    2018-01-01

    Anmeldelse af: "Vi troede ikke, det kunne ske her. Jugoslaviens sammenbrud 1991-1999" af Christian Axboe Nielsen. Kristeligt Dagblads Forlag, 2018. 410 sider......Anmeldelse af: "Vi troede ikke, det kunne ske her. Jugoslaviens sammenbrud 1991-1999" af Christian Axboe Nielsen. Kristeligt Dagblads Forlag, 2018. 410 sider...

  18. Medical Imaging of Mummies and Bog Bodies

    DEFF Research Database (Denmark)

    Lynnerup, Niels

    2010-01-01

    Mummies are human remains with preservation of non-bony tissue. Mummification by natural influences results in so-called natural mummies, while mummification induced by active (human) intervention results in so-called artificial mummies, although many cultures practiced burial rites which to some...... severely degraded, bone is quite readily visualized, but accurate imaging of preserved soft tissues, and pathological lesions therein, may require considerable post-image capture processing of CT data....

  19. Bog rodom iz detstva / Jelena Skulskaja

    Index Scriptorium Estoniae

    Skulskaja, Jelena, 1950-

    2007-01-01

    Eldar Rjazanovi eluloofilm muinasjutuvestja Hans Christian Anderseni elust "Andersen. Elu ilma armastuseta" ("Andersen. Zhizn bez ljubvi"): stsenarist Irakli Kvirikadze : operaatorid Jevgeni Guslinski ja Vadim Alissov : helilooja Aleksei Rõbnikov : nimiosas Vanja Haratjan, Stanislav Rjadinski, Sergei Migitsko

  20. Peat power: fuel by the bog

    Energy Technology Data Exchange (ETDEWEB)

    Aronson, R.B.

    1979-10-11

    The article reviews harvesting techniques and the use of peat in Europe, especially Russia, Ireland, and Finland. US peat reserves are estimated at 240 billion barrels of oil equivalent and DOE is researching new techniques for its harvesting and use. Advantages of peat are its low sulfur content (about 1%) and the fact that it is highly reactive, making it suitable for gasification. Disadvantages occur in reducing the water content from over 90% to below 50% and its low heating value relative to its bulk. Ash content varies from 2 to 70%. It looks at the first major attempt in the US to commercially harvest peat for fuel on about 150,000 acres near Creswell, NC.

  1. Lead atmospheric deposition rates and isotopic trends in Asian dust during the last 9.5 kyr recorded in an ombrotrophic peat bog on the eastern Qinghai-Tibetan Plateau

    Science.gov (United States)

    Ferrat, Marion; Weiss, Dominik J.; Dong, Shuofei; Large, David J.; Spiro, Baruch; Sun, Youbin; Gallagher, Kerry

    2012-04-01

    been particularly important between 3.1-2.7 kyr BP and 1.7-0.9 kyr BP, suggesting a possible strengthening of the East Asian winter monsoon, in agreement with previous reconstructions in Asia. Based on the Pb/Sc and isotopic composition profiles we do not note any evidence for anthropogenic Pb derived from the thriving mining or smelting activities in northern and eastern China in the last few millennia, suggesting that atmospheric deposition to this region of the eastern Tibetan Plateau was dominated by natural Pb fluxes. These can serve as a true Asian "background" value against which anthropogenic impacts can be quantified. Our results confirm that the combination of radiogenic isotopes (Pb) and trace elements in peat bogs enables observational reconstructions of changes in past regional atmospheric circulation. Such records will enable more refined interpretations of marine and terrestrial palaeorecords in Asia and the Pacific and consequently provide further constraints for changes in ocean and atmospheric circulation and for the testing of palaeoclimate models of circulation patterns.

  2. Turfeiras da Serra do Espinhaço Meridional - MG: II - influência da drenagem na composição elementar e substâncias húmicas Peat bogs in the Serra do Espinhaço Meridional - Minas Gerais, Brazil: II - influence of drainage on elemental humus composition and substances

    Directory of Open Access Journals (Sweden)

    Alexandre Christófaro Silva

    2009-10-01

    Full Text Available As turfeiras são Organossolos que resultam de condições ecológicas ideais ao acúmulo de material orgânico, controladas pelos sistemas geomorfológicos e processos geológicos e climáticos globais. Sua constituição física, química e biológica é pouco conhecida. No presente trabalho foi realizado um estudo sobre as turfeiras da Serra do Espinhaço Meridional (SdEM - MG, por meio da descrição e coleta de amostras em três perfis situados a 1.250 m (P1, 1.350 m (P4 e 1.800 m (P2 de altitude. Os três perfis foram caracterizados morfologicamente e, nas amostras coletadas, foram realizadas análises químicas e fracionamento da matéria orgânica em ácidos húmicos, ácidos fúlvicos e humina. A matéria orgânica dos perfis de Turfeiras da SdEM apresentou marcantes diferenças entre si em relação à sua composição química e ao teor das substâncias húmicas e à composição química dos ácidos húmicos. A variação das condições de drenagem foi preponderante para a diferenciação qualitativa e quantitativa da matéria orgânica. A turfeira P1, com moderadas condições de drenagem, apresentou matéria orgânica com maiores relações C/N e O/C, predomínio de ácidos fúlvicos entre as substâncias húmicas e ácidos húmicos e elevada relação C/N. Nas turfeiras P2 e P4, com muito más condições de drenagem, as relações C/N e O/C da matéria orgânica foram mais baixas, a humina predominou amplamente entre as substâncias húmicas e os ácidos húmicos apresentaram a mais baixa relação C/N.Peat bogs are Organosols formed under ideal ecological conditions in terms of the accumulation of organic material, controlled by geomorphological and geological processes and climate. The physical, chemistry and biological constitution of peat bogs is largely unknown. In this study the peat bogs of the Southern Serra do Espinhaço (Minas Gerais, Brazil were described and sampled from three profiles at 1,250 m (P1, 1,350 m (P4 and

  3. Degradation of Parathion by Microorganisms from Cranberry Bogs

    International Nuclear Information System (INIS)

    Gorder, G.W.; Lichtenstein, E.P.

    1981-01-01

    Full text: Oxygen concentration and different carbon sources drastically altered parathion degradation in culture media inoculated with microorganisms from Wisconsin cranberry (Vaccinium macrocarpon Ait.) growing soils. These microorganisms also grew in basal salts media utilizing parathion as a sole carbon source. 14 CO 2 was produced only from phenyl-labelled parathion while 14 C-(ethyl)-parathion derived radiocarbon remained in the stale media of the soil-free cultures. Addition of 0.05% glucose to basal salts medium inhibited 14 C-(phenyl)-parathion degradation while the addition of 0.05% yeast extract to basal salts medium also inhibited microbiological degradation of the insecticide to 14 CO 2 , but to a lesser extent. Aminoparathion and aminoparaoxon were formed only in basal salts medium with 0.05% yeast extract. Aerobic cultures produced more 14 CO 2 from 14 C-(phenyl)-parathion and less aminoparathion than anaerobic cultures. Aminoparathion was more abundant in cultures with inocula obtained from the 18- to 23-cm layer than with culture inocula obtained from the 0- to 5-cm soil layer under both aerobic and anaerobic conditions. (author)

  4. Atmospheric nitrogen deposition promotes carbon loss from peat bogs

    Czech Academy of Sciences Publication Activity Database

    Bragazza, L.; Freeman, Ch.; Jones, T.; Rydin, H.; Limpens, J.; Fenner, N.; Ellis, T.; Gerdol, R.; Hájek, Michal; Hájek, Tomáš; Iacumin, P.; Kutnar, L.; Tahvanainen, T.; Toberman, H.

    2006-01-01

    Roč. 103, č. 51 (2006), s. 19386-19389 ISSN 0027-8424 Institutional research plan: CEZ:AV0Z60050516 Keywords : peatlands * nitrogen * deposition Subject RIV: EF - Botanics Impact factor: 9.643, year: 2006

  5. SVJETOVNI BOG MARS: RAZMATRANJA O DIMENZIJAMA RATA KROZ HERAKLITSKE DVOJNOSTI

    OpenAIRE

    Hercigonja, Zoran

    2017-01-01

    Heraklit, jedan od najstarijih grčkih filozofa, od čijeg učenja su ostale sačuvane samo nepovezane izreke, rat poima kroz dvojnosti, što nam daje mogućnost za bolje razumijevanje tog negativno konotiranog pojma. Heraklitovo promišljanje rata dovodi do dimenzioniranja područja borbe. Borba ili nužnost zavade i sukoba, prema Heraklitu, neizostavni su faktor za funkcioniranje svijeta. U ovom radu razmatramo Heraklitove fragmente u kojima promišlja o ratu.

  6. Engaging Students in World History with a Bog Body Mystery

    Science.gov (United States)

    Yell, Michael M.

    2012-01-01

    Getting students involved in the process of inquiry takes much more than pointing out a problem, offering sources, and setting them on their way. Fortunately, there are a number of teaching strategies that can be instrumental in engaging students in the process of inquiry. As a teacher of world history in the seventh grade, House of Avalon, at…

  7. Birds, bogs and forestry: the peatlands of Caithness and Sutherland

    OpenAIRE

    Stroud, D.A.; Reed, T.M.; Pienkowski, M.W.; Lindsay, Richard

    1988-01-01

    NCC’s Upland Bird Survey had surveyed a significant area of the Flow Country between 1979 and 1986, and the 1987 report analysed and published the data from those surveys, together with those obtained from eight sites in Caithness surveyed by RSPB in 1985 using NCC methods. \\ud \\ud The results highlighted losses of up to 19% of the populations of Golden Plover, Greenshank and Dunlin in the Flow Country area as a result of then widespread and rapidly occurring afforestation of the peatlands. N...

  8. Methanotrophic symbionts provide carbon for photosynthesis in peat bogs

    NARCIS (Netherlands)

    Raghoebarsing, A.A.; Smolders, A.J.P.; Schmid, M.C.; Rijpstra, W.I.C.; Wolters-Arts, M.; Derksen, J.; Jetten, M.S.M.; Schouten, S.; Sinninghe Damsté, J.S.; Lamers, L.P.M.; Roelofs, J.G.M.; Op den Camp, H.J.M.; Strous, M.

    2005-01-01

    Wetlands are the largest natural source of atmospheric methane, the second most important greenhouse gas. Methane flux to the atmosphere depends strongly on the climate; however, by far the largest part of the methane formed in wetland ecosystems is recycled and does not reach the atmosphere.

  9. Emissions of biogenic sulfur gases from northern bogs and fens

    Science.gov (United States)

    Demello, William Zamboni; Hines, Mark E.; Bayley, Suzanne E.

    1992-01-01

    Sulfur gases are important components of the global cycle of S. They contribute to the acidity of precipitation and they influence global radiation balance and climate. The role of terrestrial sources of biogenic S and their effect on atmospheric chemistry remain as major unanswered questions in our understanding of the natural S cycle. The role of northern wetlands as sources and sinks of gaseous S by measuring rates of S gas exchange as a function of season, hydrologic conditions, and gradients in tropic status was investigated. Experiments were conducted in wetlands in New Hampshire, particularly a poor fen, and in Mire 239, a poor fen at the Experimental Lakes Area (ELA) in Ontario. Emissions were determined using Teflon enclosures, gas cryotrapping methods and gas chromatography (GC) with flame photometric detection. Dynamic (sweep flow) and static enclosures were employed which yielded similar results. Dissolved S gases and methane were determined by gas stripping followed by GC.

  10. Environmental factors determining spontaneous recovery of industrially mined peat bogs: A multi-site analysis

    Czech Academy of Sciences Publication Activity Database

    Konvalinková, Petra; Prach, Karel

    2014-01-01

    Roč. 69, Aug 2014 (2014), s. 38-45 ISSN 0925-8574 R&D Projects: GA ČR(CZ) GAP505/11/0256 Institutional support: RVO:67985939 Keywords : peatland * restoration * succession Subject RIV: EH - Ecology, Behaviour Impact factor: 2.580, year: 2014

  11. Ecology of some mire and bog plant communities in the Western Italian Alps

    Directory of Open Access Journals (Sweden)

    Giorgio BUFFA

    2003-02-01

    Full Text Available During a mire vegetation study, conducted mainly in the subalpine-alpine sector of the Western Italian Alps, the ecology of several plant communities and numerous moss species of this kind of vegetation was evaluated. The study area covered the Piedmontese sector of the Graian Alps, the eastern sector of the Aosta Valley as well as certain localities of the Pennine Alps, the Canavese district and the Maritime Alps. They have a rocky substratum representative of the various regional lithologies and include the main sectors characterised by the highest precipitation. Three hundred and twenty two relevées were made using the phytosociological method and the pH and the conductivity of the water table and its depth were measured directly. Cluster Analysis allowed a classification of the samples and the identification of various groups of plant communities. Ordination performed by DCA and CCA allowed us to identify the ecological features of the various plant communities by using the values of the main environmental parameters, measured directly in the field, and certain climatic parameters (altitude and mean annual precipitation available. The use of climatic parameters is an important result for identifying communities which show greater oceanicity, something that is underlined also by the presence of indicator species such as Sphagnum papillosum and S. subnitens. Furthermore the communities are arranged in a "poor-rich" gradient, and are also profoundly influenced by depth to water table which is inversely correlated to the pH. Therefore we find certain kinds of communities all with a very low water table and which are little affected by its chemistry. Other groups share the fact that the water table is outcropping or near the surface and are distinguishable for their pH values and conductivity. We discuss the different response of the bryophytes and vascular plants of these communities to the environmental parameters considered, in light of their anatomic and functional differences. Bryophytes are more sensitive to environmental and climatic parameters whilst vascular plants are mostly ubiquitous in the relevées with a greater ecological plasticity.

  12. Acrotelm pedogenesis of a Sphagnum bog is reflected in effective unsaturated hydraulic properties

    Science.gov (United States)

    Weber, Tobias K. D.; Iden, Sascha C.; Durner, Wolfgang

    2017-04-01

    In ombrotrophic peatlands, the moisture content of the vadose zone (acrotelm) controls oxygen diffusion rates, redox state, and the turnover of organic matter. Whether peatlands act as sinks or sources of atmospheric carbon thus relies on variably saturated flow processes. Modeling of these processes is crucial in assessing effects of changed environmental conditions on the future development of these ecosystems. The Richards equation (RE) is the standard model for water flow in soils, but it is not clear whether it can be applied to simulate water flow in live Sphagnum moss. To check the suitability of the RE to describe the water dynamics in drying moss and peat we conducted transient laboratory evaporation experiments on undisturbed samples from the entire acrotelm. The experimental data consisted of measured pressure heads in two depths and water fluxes, and were evaluated by inverse modelling using the RE as process model. The results showed that the measurements could be matched very well only if the soil hydraulic properties (SHPs) were represented by a suitable model. A successful parameterisation of the SHPs of the moss was based on pore-size distributions (PSD) which combine three distinct pore systems of the Sphagnum moss, reflecting an inter-, intra-, and inner-plant pore space. We had to extend the traditional van Genuchten-Mualem model to account for non-capillary water storage and flow to obtain consistent descriptions of the observations. For the deeper samples, the pedogenesis of the acrotelm, a process of compaction and biochemical degradation of the solid matrix, had considerably impact on the shape of the SHPs. The collapse of the inter-plant pores and their filling with smaller particles led gradually to bi-modal PSDs with increasing depth. This coincides with a homogenisation and a considerably reduction in horizontal variability of SHPs at greater depths. We conclude that the RE with adequate representation of SHPs is a valid process description for variably saturated moisture fluxes over a wide pressure range in peatlands, supporting the conceptualization of the living moss as part of the vadose zone.

  13. A pore-size classification for peat bogs derived from unsaturated hydraulic properties

    Science.gov (United States)

    Weber, Tobias Karl David; Iden, Sascha Christian; Durner, Wolfgang

    2017-12-01

    In ombrotrophic peatlands, the moisture content of the acrotelm (vadoze zone) controls oxygen diffusion rates, redox state, and the turnover of organic matter. Thus, variably saturated flow processes determine whether peatlands act as sinks or sources of atmospheric carbon, and modelling these processes is crucial to assess effects of changed environmental conditions on the future development of these ecosystems. We show that the Richards equation can be used to accurately describe the moisture dynamics under evaporative conditions in variably saturated peat soil, encompassing the transition from the topmost living moss layer to the decomposed peat as part of the vadose zone. Soil hydraulic properties (SHP) were identified by inverse simulation of evaporation experiments on samples from the entire acrotelm. To obtain consistent descriptions of the observations, the traditional van Genuchten-Mualem model was extended to account for non-capillary water storage and flow. We found that the SHP of the uppermost moss layer reflect a pore-size distribution (PSD) that combines three distinct pore systems of the Sphagnum moss. For deeper samples, acrotelm pedogenesis changes the shape of the SHP due to the collapse of inter-plant pores and an infill with smaller particles. This leads to gradually more homogeneous and bi-modal PSDs with increasing depth, which in turn can serve as a proxy for increasing state of pedogenesis in peatlands. From this, we derive a nomenclature and size classification for the pore spaces of Sphagnum mosses and define inter-, intra-, and inner-plant pore spaces, with effective pore diameters of > 300, 300-30, and 30-10 µm, respectively.

  14. ION EXCHANGE IN SPHAGNUM AND ITS RELATION TO BOG ECOLOGY. (U915444)

    Science.gov (United States)

    The perspectives, information and conclusions conveyed in research project abstracts, progress reports, final reports, journal abstracts and journal publications convey the viewpoints of the principal investigator and may not represent the views and policies of ORD and EPA. Concl...

  15. Herons, Frogs, and Cranberry Bogs: A Wetlands Unit for Science and Language Arts.

    Science.gov (United States)

    Pottle, Jean L.

    This book presents interesting lessons about freshwater and saltwater wetlands, the creatures that inhabit them, and individuals who have played an important role in saving them. Activities in this book give students a chance to do their own research, perform experiments, use field guides, and work with maps and diagrams. Students are asked to…

  16. The American cranberry: first insights into the whole genome of a species adapted to bog habitat.

    Science.gov (United States)

    Polashock, James; Zelzion, Ehud; Fajardo, Diego; Zalapa, Juan; Georgi, Laura; Bhattacharya, Debashish; Vorsa, Nicholi

    2014-06-13

    The American cranberry (Vaccinium macrocarpon Ait.) is one of only three widely-cultivated fruit crops native to North America- the other two are blueberry (Vaccinium spp.) and native grape (Vitis spp.). In terms of taxonomy, cranberries are in the core Ericales, an order for which genome sequence data are currently lacking. In addition, cranberries produce a host of important polyphenolic secondary compounds, some of which are beneficial to human health. Whereas next-generation sequencing technology is allowing the advancement of whole-genome sequencing, one major obstacle to the successful assembly from short-read sequence data of complex diploid (and higher ploidy) organisms is heterozygosity. Cranberry has the advantage of being diploid (2n = 2x = 24) and self-fertile. To minimize the issue of heterozygosity, we sequenced the genome of a fifth-generation inbred genotype (F ≥ 0.97) derived from five generations of selfing originating from the cultivar Ben Lear. The genome size of V. macrocarpon has been estimated to be about 470 Mb. Genomic sequences were assembled into 229,745 scaffolds representing 420 Mbp (N50 = 4,237 bp) with 20X average coverage. The number of predicted genes was 36,364 and represents 17.7% of the assembled genome. Of the predicted genes, 30,090 were assigned to candidate genes based on homology. Genes supported by transcriptome data totaled 13,170 (36%). Shotgun sequencing of the cranberry genome, with an average sequencing coverage of 20X, allowed efficient assembly and gene calling. The candidate genes identified represent a useful collection to further study important biochemical pathways and cellular processes and to use for marker development for breeding and the study of horticultural characteristics, such as disease resistance.

  17. Plant quality and local adaptation undermine relocation in a bog specialist butterfly

    NARCIS (Netherlands)

    Turlure, C.; Radchuk, V.; Baguette, M.; Meijrink, M.; Burg, van den A.; Wallis de Vries, M.F.; Duinen, G.J.

    2013-01-01

    The butterfly Boloria aquilonaris is a specialist of oligotrophic ecosystems. Population viability analysis predicted the species to be stable in Belgium and to collapse in the Netherlands with reduced host plant quality expected to drive species decline in the latter. We tested this hypothesis by

  18. Seasonal changes of microbial communities in two shallow peat bog lakes

    Czech Academy of Sciences Publication Activity Database

    Lew, S.; Koblížek, Michal; Lew, M.; Medová, Hana; Glinska-Lewczuk, K.; Owsianny, P. M.

    2015-01-01

    Roč. 60, č. 2 (2015), s. 165-175 ISSN 0015-5632 R&D Projects: GA ČR GA13-11281S; GA MŠk ED2.1.00/03.0110 Institutional support: RVO:61388971 Keywords : AEROBIC ANOXYGENIC PHOTOTROPHS * TARGETED OLIGONUCLEOTIDE PROBES * IN-SITU HYBRIDIZATION Subject RIV: EE - Microbiology, Virology Impact factor: 1.335, year: 2015

  19. Small ones and big ones: cross-taxon congruence reflects organism body size in ombrotrophic bogs

    Czech Academy of Sciences Publication Activity Database

    Hájek, Michal; Poulíčková, A.; Vašutová, Martina; Syrovátka, V.; Jiroušek, M.; Štěpánková, J.; Opravilová, V.; Hájková, Petra

    2014-01-01

    Roč. 726, č. 1 (2014), s. 95-107 ISSN 0018-8158 R&D Projects: GA ČR GA206/08/0389 Institutional support: RVO:67985939 ; RVO:67179843 Keywords : biomonitoring * multi-proxy * species richness Subject RIV: EF - Botanics; EH - Ecology, Behaviour (UEK-B) Impact factor: 2.275, year: 2014

  20. Importance of landscape heterogeneity for the conservation of aquatic macroinvertebrate diversity in bog landscapes

    NARCIS (Netherlands)

    Verberk, W.C.E.P.; Duinen, van G.A.; Brock, A.M.T.; Leuven, R.S.E.W.; Siepel, H.; Verdonschot, P.F.M.; Velde, van der G.; Esselink, H.

    2006-01-01

    Heterogeneous landscapes are biodiversity `hotspots¿. Degradation resulting from acidification, desiccation and eutrophication not only decreases habitat quality, but also causes heterogeneity to decline. While restoration measures aim at restoring habitat quality, they can further reduce

  1. Biodiversity and ecology of algae in mountain bogs (Bohemian Forest, Central Europe)

    Czech Academy of Sciences Publication Activity Database

    Lederer, F.; Papáčková, Lenka

    2002-01-01

    Roč. 144, č. 106 (2002), s. 151-183 ISSN 0342-1120 R&D Projects: GA ČR GA206/96/1115; GA ČR GA206/99/1411; GA ČR GA206/00/P063 Institutional research plan: CEZ:AV0Z6005908 Keywords : cyanobacteria * algae * patterned mires Subject RIV: EF - Botanics

  2. "Students Get Bogged Down": How Religious Israeli Elementary Teachers View Problems and Solutions in Bible Teaching

    Science.gov (United States)

    Walfish, Ruth A.; Brody, David L.

    2018-01-01

    Bible teachers in contemporary society confront serious problems related to the nature of the biblical text and the socio-cultural context of their teaching. This study, based on semi-structured interviews, examines the problems that five expert religious Israeli elementary school teachers encounter in their teaching and the solutions they employ.…

  3. Dynamics of methane fluxes from two peat bogs in the Ore Mountains, Czech Republic

    Czech Academy of Sciences Publication Activity Database

    Bohdálková, Leona; Čuřík, J.; Kuběna, A.; Bůzek, F.

    2013-01-01

    Roč. 59, č. 1 (2013), s. 14-21 ISSN 1214-1178 R&D Projects: GA MŠk(CZ) ED1.1.00/02.0073 Institutional support: RVO:67179843 Keywords : restoration * peatland * climate change * Sphagnum * Carex Subject RIV: EH - Ecology, Behaviour Impact factor: 1.113, year: 2013

  4. Håndbog i praktisk hjælp eBog

    DEFF Research Database (Denmark)

    René, Michael

    Håndbog i praktisk hjælp er en opslagsbog med masser af nyttig viden om rengøring, hygiejne og opbevaring af fødevarer. Bogen indeholder afsnit om forskellige rengøringsmidler, om rengøring af forskellige materialer og om fjernelse af pletter, og der er en beskrivelse af forholdsregler i forbinde......://michaelrene.com/forfatter/ Anmeldelse: http://www.michaelrene.com/Munksgaard/AnmeldelseHaandbogIpraktiskhjaelp.png...

  5. Håndbog i praktisk hjælp iBog

    DEFF Research Database (Denmark)

    René, Michael

    Håndbog i praktisk hjælp er en opslagsbog med masser af nyttig viden om rengøring, hygiejne og opbevaring af fødevarer. Bogen indeholder afsnit om forskellige rengøringsmidler, om rengøring af forskellige materialer og om fjernelse af pletter, og der er en beskrivelse af forholdsregler i forbinde......://michaelrene.com/forfatter/ Anmeldelse: http://www.michaelrene.com/Munksgaard/AnmeldelseHaandbogIpraktiskhjaelp.png...

  6. Estudios sonoros desde la Región Andina UIO-BOG

    OpenAIRE

    Estévez Trujillo, Mayra Patricia

    2008-01-01

    Existen un sin número de prácticas artísticas con sonido, aparentemente generadas en las vanguardias europeas y estadounidenses de inicios y mediados del siglo XX, producto de la apropiación y asimilación cultural, lingüística, musical y gráfica, de las expresiones simbólicas africanas y asiáticas, por parte de dadaístas, surrealistas, futuristas, expresionistas y minimalistas. Son estos procedimientos de apropiación y asimilación de matrices culturales no occidentales, los ...

  7. Insect biodiversity of Central European peat bogs: the habitat island concept of conservation

    Czech Academy of Sciences Publication Activity Database

    Spitzer, Karel

    2004-01-01

    Roč. 12, - (2004), s. 113-117 ISSN 0782-7784 R&D Projects: GA AV ČR IBS5007015 Institutional research plan: CEZ:AV0Z5007907 Keywords : Insects * relicts * peatbogs Subject RIV: EH - Ecology, Behaviour

  8. Skarp og præcis bog om præstationsløn

    DEFF Research Database (Denmark)

    Bukh, Per Nikolaj

    2010-01-01

    Anmeldelse af Rewarding Performance: Guiding principles, custom strategies, Robert J. Greene, Routledge......Anmeldelse af Rewarding Performance: Guiding principles, custom strategies, Robert J. Greene, Routledge...

  9. Bog burst in the eastern Netherlands triggered by the 2.8 kyr BP climate event

    NARCIS (Netherlands)

    van Geel, B.; Heijnis, H.; Charman, D.J.; Thompson, G.; Engels, S.

    2014-01-01

    The nature and cause of the so-called 2.8 kyr BP event have been a subject of much debate. Peat sequences have provided much of the evidence for this event, but the process link between climate and peatland response is not well understood. Multiproxy, high-resolution analysis of a core from

  10. Heavy metals, especially lead, deposition recorded in an ombrotrophic peat bog near Manchester, United Kingdom

    Science.gov (United States)

    Le Roux, G.; Weiss, D.; Cheburkin, A.; Rausch, N.; Grattant, J.; Krachler, M.; Shotyk, W.

    2003-05-01

    A peat monolith representing up to 4,000 years of peat accumulation near Manchester, England, was collected. Major and trace elements were analysed with XRF and for Cd and Pb in the deeper samples with GF-AAS following acid digestion. Pb isotopic composition was measured with TIMS and ICP-MS. The results show a pollution since the Roman Period due to local lead sources and an increase in lead pollution in the last century due to leaded gasoline as fingerprinted by Pb isotopic signatures.

  11. Biophysical drivers of seasonal variability in Sphagnum gross primary production in a northern temperate bog

    Science.gov (United States)

    Walker, Anthony P.; Carter, Kelsey R.; Gu, Lianhong; Hanson, Paul J.; Malhotra, Avni; Norby, Richard J.; Sebestyen, Stephen D.; Wullschleger, Stan D.; Weston, David J.

    2017-05-01

    Sphagnum mosses are the keystone species of peatland ecosystems. With rapid rates of climate change occurring in high latitudes, vast reservoirs of carbon accumulated over millennia in peatland ecosystems are potentially vulnerable to rising temperature and changing precipitation. We investigate the seasonal drivers of Sphagnum gross primary production (GPP)—the entry point of carbon into wetland ecosystems. Continuous flux measurements and flux partitioning show a seasonal cycle of Sphagnum GPP that peaked in the late summer, well after the peak in photosynthetically active radiation. Wavelet analysis showed that water table height was the key driver of weekly variation in Sphagnum GPP in the early summer and that temperature was the primary driver of GPP in the late summer and autumn. Flux partitioning and a process-based model of Sphagnum photosynthesis demonstrated the likelihood of seasonally dynamic maximum rates of photosynthesis and a logistic relationship between the water table and photosynthesizing tissue area when the water table was at the Sphagnum surface. The model also suggested that variability in internal resistance to CO2 transport, a function of Sphagnum water content, had minimal effect on GPP. To accurately model Sphagnum GPP, we recommend the following: (1) understanding seasonal photosynthetic trait variation and its triggers in Sphagnum; (2) characterizing the interaction of Sphagnum photosynthesizing tissue area with water table height; (3) modeling Sphagnum as a "soil" layer for consistent simulation of water dynamics; and (4) measurement of Sphagnum "canopy" properties: extinction coefficient (k), clumping (Ω), and maximum stem area index (SAI).

  12. Methane cycling in peat bogs: Environmental relevance of methano-Trophs revealed by microbial lipid chemistry

    NARCIS (Netherlands)

    van Winden, J.F.

    2011-01-01

    Global warming is continuing without delay and this is caused by the accumulation of greenhouse gases in the atmosphere. Methane is a strong greenhouse gas, 25 times stronger compared to CO2. The increase in methane concentrations in the atmosphere is largely the result of human influences, but

  13. The effect of increased temperature and nitrogen deposition on decomposition in bogs

    NARCIS (Netherlands)

    Breeuwer, A.J.G.; Heijmans, M.M.P.D.; Robroek, B.J.M.; Limpens, J.; Berendse, F.

    2008-01-01

    Despite their low primary production, ombrotrophic peatlands have a considerable potential to store atmospheric carbon as a result of their extremely low litter decomposition rates. Projected changes in temperature and nitrogen (N) deposition may increase decomposition rates by their positive

  14. Transpiration of Pinus rotundata on a wooded peat bog in central Europe

    Czech Academy of Sciences Publication Activity Database

    Kučerová, Andrea; Čermák, J.; Nadezhdina, N.; Pokorný, J.

    2010-01-01

    Roč. 24, č. 5 (2010), s. 919-930 ISSN 0931-1890 Institutional research plan: CEZ:AV0Z60050516 Keywords : heat field deformation method * sap flow * water table Subject RIV: EF - Botanics Impact factor: 1.444, year: 2010

  15. Decomposition patterns, nutrient availability, species identities and vegetation changes in central-European summit bogs

    Czech Academy of Sciences Publication Activity Database

    Jiroušek, M.; Tůma, I.; Záhora, J.; Holub, Petr; Kintrová, K.; Hájek, M.

    2015-01-01

    Roč. 20, č. 5 (2015), s. 571-586 ISSN 1239-6095 Institutional support: RVO:67179843 Keywords : atmospheric nitrogen deposition * boreal peatlands * nutritional constraints * litter decomposition Subject RIV: EH - Ecology, Behaviour Impact factor: 1.476, year: 2015

  16. Gene flow rise with habitat fragmentation in the bog fritillary butterfly (Lepidoptera: Nymphalidae).

    Science.gov (United States)

    Nève, Gabriel; Barascud, Bernard; Descimon, Henri; Baguette, Michel

    2008-03-17

    The main components of the spatial genetic structure of the populations are neighbourhood size and isolation by distance. These may be inferred from the allele frequencies across a series of populations within a region. Here, the spatial population structure of Proclossiana eunomia was investigated in two mountainous areas of southern Europe (Asturias, Spain and Pyrenees, France) and in two areas of intermediate elevation (Morvan, France and Ardennes, Belgium). A total of eight polymorphic loci were scored by allozyme electrophoresis, revealing a higher polymorphism in the populations of southern Europe than in those of central Europe. Isolation by distance effect was much stronger in the two mountain ranges (Pyrenees and Asturias) than in the two areas of lower elevation (Ardennes and Morvan). By contrast, the neighbourhood size estimates were smaller in the Ardennes and in the Morvan than in the two high mountain areas, indicating more common movements between neighbouring patches in the mountains than in plains. Short and long dispersal events are two phenomena with distinct consequences in the population genetics of natural populations. The differences in level of population differentiation within each the four regions may be explained by change in dispersal in lowland recently fragmented landscapes: on average, butterflies disperse to a shorter distance but the few ones which disperse long distance do so more efficiently. Habitat fragmentation has evolutionary consequences exceeding by far the selection of dispersal related traits: the balance between local specialisation and gene flow would be perturbed, which would modify the extent to which populations are adapted to heterogeneous environments.

  17. Gene flow rise with habitat fragmentation in the bog fritillary butterfly (Lepidoptera: Nymphalidae

    Directory of Open Access Journals (Sweden)

    Descimon Henri

    2008-03-01

    Full Text Available Abstract Background The main components of the spatial genetic structure of the populations are neighbourhood size and isolation by distance. These may be inferred from the allele frequencies across a series of populations within a region. Here, the spatial population structure of Proclossiana eunomia was investigated in two mountainous areas of southern Europe (Asturias, Spain and Pyrenees, France and in two areas of intermediate elevation (Morvan, France and Ardennes, Belgium. Results A total of eight polymorphic loci were scored by allozyme electrophoresis, revealing a higher polymorphism in the populations of southern Europe than in those of central Europe. Isolation by distance effect was much stronger in the two mountain ranges (Pyrenees and Asturias than in the two areas of lower elevation (Ardennes and Morvan. By contrast, the neighbourhood size estimates were smaller in the Ardennes and in the Morvan than in the two high mountain areas, indicating more common movements between neighbouring patches in the mountains than in plains. Conclusion Short and long dispersal events are two phenomena with distinct consequences in the population genetics of natural populations. The differences in level of population differentiation within each the four regions may be explained by change in dispersal in lowland recently fragmented landscapes: on average, butterflies disperse to a shorter distance but the few ones which disperse long distance do so more efficiently. Habitat fragmentation has evolutionary consequences exceeding by far the selection of dispersal related traits: the balance between local specialisation and gene flow would be perturbed, which would modify the extent to which populations are adapted to heterogeneous environments.

  18. Reconstruction of hydrology, vegetation and past climate change in bogs using fungal microfossils

    NARCIS (Netherlands)

    Yeloff, D.; Charman, D.; van Geel, B.; Mauquoy, D.S.

    2007-01-01

    Water is one of the most important environmental factors defining the niche of terrestrial fungi, and fungi preserved in ombrotrophic peat deposits have the potential to indicate past variations in surface wetness and vegetation composition. This study aimed to assess the potential of fungal

  19. Multi-omics of permafrost, active layer and thermokarst bog soil microbiomes

    DEFF Research Database (Denmark)

    Hultman, Jenni; Waldrop, Mark P.; Mackelprang, Rachel

    2015-01-01

    Over 20% of Earth's terrestrial surface is underlain by permafrost with vast stores of carbon that, once thawed, may represent the largest future transfer of carbon from the biosphere to the atmosphere(1). This process is largely dependent on microbial responses, but we know little about microbia...

  20. Thermodynamic analysis of hydrocarbon refrigerants-based ethylene BOG re-liquefaction system

    Science.gov (United States)

    Beladjine, Boumedienne M.; Ouadha, Ahmed; Addad, Yacine

    2016-09-01

    The present study aims to make a thermodynamic analysis of an ethylene cascade re-liquefaction system that consists of the following two subsystems: a liquefaction cycle using ethylene as the working fluid and a refrigeration cycle operating with a hydrocarbon refrigerant. The hydrocarbon refrigerants considered are propane (R290), butane (R600), isobutane (R600a), and propylene (R1270). A computer program written in FORTRAN is developed to compute parameters for characteristic points of the cycles and the system's performance, which is determined and analyzed using numerical solutions for the refrigerant condensation temperature, temperature in tank, and temperature difference in the cascade condenser. Results show that R600a gives the best performance, followed by (in order) R600, R290, and R1270. Furthermore, it is found that an increase in tank temperature improves system performance but that an increase in refrigerant condensation temperature causes deterioration. In addition, it is found that running the system at a low temperature difference in the cascade condenser is advantageous.

  1. Root growth of tomato seedlings intensified by humic substances from peat bogs

    Directory of Open Access Journals (Sweden)

    Alexandre Christofaro Silva

    2011-10-01

    Full Text Available Peats are an important reserve of humified carbon in terrestrial ecosystems. The interest in the use of humic substances as plant growth promoters is continuously increasing. The objective of this study was to evaluate the bioactivity of alkaline soluble humic substances (HS, humic (HA and fulvic acids (FA isolated from peats with different decomposition stages of organic matter (sapric, fibric and hemic in the Serra do Espinhaço Meridional, state of Minas Gerais. Dose-response curves were established for the number of lateral roots growing from the main plant axis of tomato seedlings. The bioactivity of HA was greatest (highest response in lateral roots at lowest concentration while FA did not intensify root growth. Both HS and HA stimulated root hair formation. At low concentrations, HS and HA induced root hair formation near the root cap, a typical hormonal imbalance effect in plants. Transgenic tomato with reporter gene DR5::GUS allowed the observation that the auxin-related signalling pathway was involved in root growth promotion by HA.

  2. Le rônier (Borassus akeassii B.O.G.) dans les parcs agroforestiers à ...

    African Journals Online (AJOL)

    SARAH

    30 avr. 2016 ... RESUME. Objectif : Le palmier rônier au Centre-ouest du Burkina Faso est méconnu bien qu'étant une composante de parcs agroforestiers. Cette étude a pour objectifs de faire une description de ces parcs ; apprécier les interactions rôniers-cultures ; identifier les modes, les contraintes de gestion et les ...

  3. Investigating carbon dynamics in Siberian peat bogs using molecular-level analyses

    Science.gov (United States)

    Kaiser, K.; Benner, R. H.

    2013-12-01

    Total hydrolysable carbohydrates, and lignin and cutin acid compounds were analyzed in peat cores collected 56.8 N (SIB04), 58.4 N (SIB06), 63.8 N (G137) and 66.5 N (E113) in the Western Siberian Lowland to investigate vegetation, chemical compositions and the stage of decomposition. Sphagnum mosses dominated peatland vegetation in all four cores. High-resolution molecular analyses revealed rapid vegetation changes on timescales of 50-200 years in the southern cores Sib4 and Sib6. Syringyl and vanillyl (S/V) ratios and cutin acids indicated these vegetation changes were due to varying inputs of angiosperm and gymnosperm and root material. In the G137 and E113 cores lichens briefly replaced sphagnum mosses and vascular plants. Molecular decomposition indicators used in this study tracked the decomposition of different organic constituents of peat organic matter. The carbohydrate decomposition index was sensitive to the polysaccharide component of all peat-forming plants, whereas acid/aldehyde ratios of S and V phenols (Ac/AlS,V) followed the lignin component of vascular plants. Low carbohydrate decomposition indices in peat layers corresponded well with elevated (Ad/Al)S,V ratios. This suggested both classes of biochemicals were simultaneously decomposed, and decomposition processes were associated with extensive total mass loss in these ombrotrophic systems. Selective decomposition or transformation of lignin was observed in the permafrost-influenced northern cores G137 and E113. Both cores exhibited the highest (Ad/Al)S,V ratios, almost four-fold higher than measured in peat-forming plants. The extent of decomposition in the four peat cores did not uniformly increase with age, but showed episodic extensive decomposition events. Variable decomposition events independent of climatic conditions and vegetation shifts highlight the complexity of peatland dynamics.

  4. Conspicuous peak of oligotrichous ciliates following winter stratification in a bog lake

    Czech Academy of Sciences Publication Activity Database

    Macek, Miroslav; Šimek, Karel; Bittl, T.

    2001-01-01

    Roč. 23, č. 4 (2001), s. 353-363 ISSN 0142-7873 R&D Projects: GA ČR GA206/99/0028; GA AV ČR KSK2005601 Keywords : ciliates * feeding rates * ice Subject RIV: EH - Ecology, Behaviour Impact factor: 1.259, year: 2001

  5. A pore-size classification for peat bogs derived from unsaturated hydraulic properties

    Directory of Open Access Journals (Sweden)

    T. K. D. Weber

    2017-12-01

    Full Text Available In ombrotrophic peatlands, the moisture content of the acrotelm (vadoze zone controls oxygen diffusion rates, redox state, and the turnover of organic matter. Thus, variably saturated flow processes determine whether peatlands act as sinks or sources of atmospheric carbon, and modelling these processes is crucial to assess effects of changed environmental conditions on the future development of these ecosystems. We show that the Richards equation can be used to accurately describe the moisture dynamics under evaporative conditions in variably saturated peat soil, encompassing the transition from the topmost living moss layer to the decomposed peat as part of the vadose zone. Soil hydraulic properties (SHP were identified by inverse simulation of evaporation experiments on samples from the entire acrotelm. To obtain consistent descriptions of the observations, the traditional van Genuchten–Mualem model was extended to account for non-capillary water storage and flow. We found that the SHP of the uppermost moss layer reflect a pore-size distribution (PSD that combines three distinct pore systems of the Sphagnum moss. For deeper samples, acrotelm pedogenesis changes the shape of the SHP due to the collapse of inter-plant pores and an infill with smaller particles. This leads to gradually more homogeneous and bi-modal PSDs with increasing depth, which in turn can serve as a proxy for increasing state of pedogenesis in peatlands. From this, we derive a nomenclature and size classification for the pore spaces of Sphagnum mosses and define inter-, intra-, and inner-plant pore spaces, with effective pore diameters of >  300, 300–30, and 30–10 µm, respectively.

  6. Bottlenecks in bog pine multiplication by somatic embryogenesis and their visualization with the environmental scanning electron microscope

    Czech Academy of Sciences Publication Activity Database

    Vlašínová, H.; Neděla, Vilém; Dordevic, B.; Havel, J.

    2017-01-01

    Roč. 254, č. 4 (2017), s. 1487-1497 ISSN 0033-183X R&D Projects: GA ČR(CZ) GA14-22777S Institutional support: RVO:68081731 Keywords : somatic embryogenesis * pinus uncinata subsp uliginosa * abnormalities * environmental scanning electron microscope Subject RIV: JA - Electronics ; Optoelectronics, Electrical Engineering OBOR OECD: Plant sciences, botany Impact factor: 2.870, year: 2016

  7. Faunistical data on the spiders (Arachnida: Araneae of the Lacul Dracului bog complex with new data for the Romanian fauna

    Directory of Open Access Journals (Sweden)

    GALLE Robert

    2006-09-01

    Full Text Available The present paper contains faunistical data obtained by the joint research of Babeş-Bolyai and Szeged University. 44 species of 15 families were identified from Lacul Dracului marsh-complex (Harghita Mountains. Meioneta similis (Kulczynski 1926 is new for the Romanian fauna. Furthermore the occurrences of two questionable species [Kaestneria pullata (O.P.-Cambridge, 1863 and Trichoncus saxicola (O.P.- Cambridge, 1861] are proved.

  8. Methanotrophic activity and diversity in different Sphagnum magellanicum dominated habitats in the southernmost peat bogs of Patagonia

    NARCIS (Netherlands)

    Kip, N.; Fritz, C.; Langelaan, E. S.; Pan, Y.; Bodrossy, L.; Pancotto, V.; Jetten, M. S. M.; Smolders, A. J. P.; den Camp, H. J. M. Op

    2012-01-01

    Sphagnum peatlands are important ecosystems in the methane cycle. Methanotrophs living inside the dead hyaline cells or on the Sphagnum mosses are able to act as a methane filter and thereby reduce methane emissions. We investigated in situ methane concentrations and the corresponding activity and

  9. Effects of peatland drainage on water quality: a case study of the shallow blanket bogs of Exmoor, UK

    Science.gov (United States)

    Grand-Clement, E.; Luscombe, D.; Le Feuvre, N.; Smith, D.; Anderson, K.; Brazier, R. E.

    2012-04-01

    Peatlands are widely represented in the South West of England (i.e. Exmoor, Dartmoor and Bodmin moors), but their existence is currently under threat due to both climate change and the impact of historical human activities. Peat cutting and intensive drainage for agricultural reclamation in the 19th and 20th century, have modified the hydrological behaviour of these shallow peats and dried out the upper layers, causing oxidation, erosion and vegetation change. Such anthropogenic impacts directly affect the storage of carbon, but also the provision of other ecosystem services, such as the supply of drinking water, and the support of specific and rare habitats. Blocking drainage ditches to restore the hydrological behaviour of peatlands has mostly been undertaken in the North of England, but to date, little is still known about the consequences of such management approaches on the overall Carbon stocks. The need to monitor restoration of peatlands in the South West of England arises due to the specific characteristics of the peat - it is often shallower than more northerly peat and dominated by Purple Moor Grass. In addition, and in part because of the shallowness of the resource, the peat has been damaged differently, often with very dense networks of hand-cut ditches which behave as highly efficient drainage networks. Most importantly, their location at the southernmost margin of the UK peatlands' geographical extent makes them extremely vulnerable to climate change, and so it is hypothesised that monitoring of these peatlands may provide an 'early warning system' for climatic impacts that affect more northerly sites in years to come. This study focuses upon the current impact of peatland degradation on water quality on Exmoor. Our experimental approach employs detailed, high resolution monitoring of selected ditches that are representative of damaged conditions on Exmoor, from small- (30 x 30cm ditches) through medium- (50x50cm), large- (1-2m ditches) and finally headwater catchment-scales. Flow monitoring has been in place at all scales since November 2010. Flow proportional water samples were collected during a range of events throughout winter 2011-2012 and analysed for Dissolved Organic Carbon (DOC), Particulate Organic Carbon (POC), pH and colour. These variables were identified as critical, both in terms of carbon cycling and for costly water treatment that currently takes place downstream. Results were examined spatially in relation to drain sizes and magnitude/frequency of event, to improve our understanding of carbon losses in streams from damaged peatlands and further estimate the potential for improvement that can be expected after restoration. Data presented here focus on the DOC and colour and demonstrate the importance of understanding across different scales of ditch and understanding the effects of the magnitude/frequency of events that are observed prior to restoration of the system.

  10. Influence of selected environmental factors on the abundance of aerobic anoxygenic phototrophs in peat-bog lakes

    Czech Academy of Sciences Publication Activity Database

    Lew, S.; Lew, M.; Koblížek, Michal

    2016-01-01

    Roč. 23, č. 14 (2016), s. 13853-13863 ISSN 0944-1344 R&D Projects: GA ČR GA13-11281S Institutional support: RVO:61388971 Keywords : BACTERIAL COMMUNITY COMPOSITION * MEDITERRANEAN SEA * PHOTOHETEROTROPHIC BACTERIA Subject RIV: EH - Ecology, Behaviour Impact factor: 2.741, year: 2016

  11. Between Bog Bodies and High Halls. Changes in Spatial Focus and Religious Conceptions in the Pre-Christian North

    DEFF Research Database (Denmark)

    Nygaard, Simon

    2015-01-01

    Abstract prepared and accepted for The Sixteenth International Saga Conference: Sagas and Space, Zürich 2015. Due to personal reasons, the actual paper was not presented at the conference, but at a Saga Seminar in Aarhus later the same year. Published in the Preprints of Abstracts for the Saga...

  12. Flight Morphology, Compound Eye Structure and Dispersal in the Bog and the Cranberry Fritillary Butterflies: An Inter- and Intraspecific Comparison.

    Directory of Open Access Journals (Sweden)

    Camille Turlure

    Full Text Available Understanding dispersal is of prime importance in conservation and population biology. Individual traits related to motion and navigation during dispersal may differ: (1 among species differing in habitat distribution, which in turn, may lead to interspecific differences in the potential for and costs of dispersal, (2 among populations of a species that experiences different levels of habitat fragmentation; (3 among individuals differing in their dispersal strategy and (4 between the sexes due to sexual differences in behaviour and dispersal tendencies. In butterflies, the visual system plays a central role in dispersal, but exactly how the visual system is related to dispersal has received far less attention than flight morphology. We studied two butterfly species to explore the relationships between flight and eye morphology, and dispersal. We predicted interspecific, intraspecific and intersexual differences for both flight and eye morphology relative to i species-specific habitat distribution, ii variation in dispersal strategy within each species and iii behavioural differences between sexes. However, we did not investigate for potential population differences. We found: (1 sexual differences that presumably reflect different demands on both male and female visual and flight systems, (2 a higher wing loading (i.e. a proxy for flight performance, larger eyes and larger facet sizes in the frontal and lateral region of the eye (i.e. better navigation capacities in the species inhabiting naturally fragmented habitat compared to the species inhabiting rather continuous habitat, and (3 larger facets in the frontal region in dispersers compared to residents within a species. Hence, dispersers may have similar locomotory capacity but potentially better navigation capacity. Dispersal ecology and evolution have attracted much attention, but there are still significant gaps in our understanding of the mechanisms of dispersal. Unfortunately, for many species we lack detailed information on the role of behavioural, morphological and physiological traits for dispersal. Our novel study supports the existence of inter- and intra-specific evolutionary responses in both motion and navigation capacities (i.e. flight and eye morphology linked to dispersal.

  13. Evidence from northwest European bogs shows ‘Little Ice Age’ climatic changes driven by variations in solar activity

    NARCIS (Netherlands)

    Mauquoy, D; van Geel, B; Blaauw, Maarten; van der Plicht, J

    2002-01-01

    Fluctuations in Holocene atmospheric radiocarbon concentrations have been shown to be due to variations in solar activity. Analyses of both Be-10 and C-14 nuclides confirm that production-rate changes during the Holocene were largely modulated by solar activity. Analyses of peat samples from two

  14. Geology, vegetation, and hydrology of the 52 bog at the MEF: 12,000 years in northern Minnesota. Chapter 4.

    Science.gov (United States)

    Elon S. Verry; Joannes. Jansenns

    2011-01-01

    A clear understanding of geology and landscape setting is fundamental to the interpretation of water and solute movement among landscape forms. This understanding allows us to assess how land use affects water, soils, and vegetation as well as assess the fate of acids, nutrients, trace metals, and organic compounds deposited from the atmosphere. Pleistocene Glaciation...

  15. Effects of human impact and climate change during the last 350 years recorded in a Swedish raised bog deposit

    OpenAIRE

    van der Linden, M.; Vickery, E.; Charman, D.J.; van Geel, B.

    2008-01-01

    A peat core from an ombrotrophic mire in central Sweden was analysed for multi-proxy indicators (plant macrofossils, pollen/non-pollen microfossils, testate amoebae, colorimetric humification, carbon/nitrogen ratios, bulk densities, loss on ignition), to evaluate the relative contributions of climate change and human impact on vegetation and peat accumulation during the last c. 350 years. 14C wiggle-match dating was applied for high precision dating. Testate amoebae assemblages were used to r...

  16. Loss of genetic diversity through spontaneous colonization in the bog fritillary butterfly, Proclossiana eunomia (Lepidoptera: Nymphalidae) in the Czech Republic

    Czech Academy of Sciences Publication Activity Database

    Néve, G.; Pavlíčko, A.; Konvička, Martin

    2009-01-01

    Roč. 106, č. 1 (2009), s. 11-19 ISSN 1210-5759 R&D Projects: GA MŠk LC06073 Institutional research plan: CEZ:AV0Z50070508 Keywords : allozyme electrophoresis * conservation * genetic polymorphism Subject RIV: EH - Ecology, Behaviour Impact factor: 0.783, year: 2009 http://www.eje.cz/scripts/viewabstract.php?abstract=1420

  17. The dynamics of lake, bog, and bay - Consequences of exposure to man related to final storage of spent nuclear fuel

    International Nuclear Information System (INIS)

    Agnedal, P.O.; Andersson, K.; Evans, S.; Sundblad, B.; Tham, G.; Wilkens, A.B.

    1984-12-01

    The natural aging of the environment, much shorter than a possible continuous release from a repository, results in uncertainties as regards to consequences of exposure to man related to final storage of spent fuel. The Phase I project summarizes the identification of such factors and parameters of predominant importance for an assessment of possible radiological consequences in a normally revolving biosphere. Three major areas are described: geomorphology and residence time such as phenomena associated with the formation of lakes in Sweden formed by the latest inland ice, lake development in terms of uptake of different elements and radionuclides as a function of the chemical composition of the water in a recipient and some aspects of sedimentation in lakes and coastal waters. The chemical environment is also studied in the evolution of a lake or a Baltic bay into farming land or peat land. The most important parameters to the behaviour of trace metal ions seem to be pH, Eh, ionic strength and content of complex formers. Finally, the human impact during the evolution of a lake or a bay is discussed. The study also includes recommendation for a reference field test area and for laboratory studies of the chemical properties of radionuclides in sediments in a Phase 2 project. (Author)

  18. Disturbances on a wooded raised bog - How windthrow, bark beetle and fire affect vegetation and soil water quality?

    Czech Academy of Sciences Publication Activity Database

    Kučerová, Andrea; Rektoris, L.; Štechová, T.; Bastl, M.

    2008-01-01

    Roč. 43, č. 1 (2008), s. 49-67 ISSN 1211-9520 R&D Projects: GA AV ČR KSK6005114 Grant - others:GA MŽP(CZ) SE/610/10/00 Program:SE Institutional research plan: CEZ:AV0Z60050516 Keywords : Czech Republic * Groundwater chemistry * Post- fire succession Subject RIV: EF - Botanics Impact factor: 0.964, year: 2008

  19. Role of Organic Solutes in the Chemistry Of Acid-Impacted Bog Waters of the Western Czech Republic

    Science.gov (United States)

    HrušKa, Jakub; Johnson, Chris E.; KráM, Pavel

    1996-04-01

    In many regions, naturally occurring organic acid anions can effectively buffer mineral acid inputs from atmospheric deposition, moderating their effect on surface water pH. We studied the effect of chronically high inputs of acid rain on the chemistry of three brown-water streams in the western Czech Republic. The dissolved organic acids in the streams were similar in character to those of other systems in Europe and North America. The site densities (the carboxyl group content per mass of C) were similar to values reported from Fenno-Scandia, and the relationship between the apparent pKa and pH conformed to those from two North American studies. Sulfate and organic acid anions (OA-) were the dominant anions in all three streams, yet despite high dissolved organic carbon and total organic acid concentrations, OA - comprised only 21-32% of total anion charge. This pattern was due to very high sulfate concentrations and, in two of the streams, a low degree of dissociation of the organic acids, probably the results of high long-term inputs of strong acids. Stream water pH was highly correlated to sulfate concentration, but uncorrelated with OA-, suggesting that free acidity is controlled by strong mineral acids rather than organic acids. Thus future reductions in strong acid inputs should result in increased pH and a return to organic control over acid-base chemistry.

  20. Leaf-spinning moths (Lepidoptera) feeding on Vaccinium uliginosum L. along an ecological gradient of central European peat bogs

    Czech Academy of Sciences Publication Activity Database

    Spitzer, Karel; Jaroš, Josef; Bezděk, Aleš

    2003-01-01

    Roč. 14, - (2003), s. 46-52 ISSN 0785-8760 R&D Projects: GA AV ČR IBS5007015 Institutional research plan: CEZ:AV0Z5007907 Keywords : Vaccinium uliginosum L. Subject RIV: EG - Zoology Impact factor: 0.246, year: 2003

  1. Peatland Woody Plant Growth Responses to Warming and Elevated CO2 in a Southern-boreal Raised Bog Ecosystem

    Science.gov (United States)

    Phillips, J. R.; Hanson, P. J.; Warren, J.; Ward, E. J.; Brice, D. J.; Graham, J.

    2017-12-01

    Spruce and Peatland Responses Under Changing Environments (SPRUCE) is an in situ warming by elevated CO2 manipulation located in a high-carbon, spruce peatland in northern Minnesota. Warming treatments combined a 12-m diameter open topped chamber with internally recirculating warm air and soil deep heating to simulate a broad range of future warming treatments. Deep below ground soil warming rates are 0, +2.25, +4.5, +6.75, and +9 °C. Deep belowground warming was initiated in June 2014 followed by air warming in August 2015. In June 2016, elevated CO2 atmospheres (eCO2 at + 500 ppm) were added to half of the warming treatments in a regression design. Our objective was to track long-term vegetation responses to warming and eCO2. Annual tree growth is based on winter measurement of circumference of all Picea mariana and Larix laricina trees within each 113 m2 plot, automated dendrometers, terrestrial LIDAR scanning of tree heights and canopy volumes, and destructive allometry. Annual shrub growth is measured in late summer by destructive clipping in two 0.25 m2 sub-plots and separation of the current year tissues. During the first year of warming, tree basal area growth was reduced for Picea, but not Larix trees. Growth responses for the woody shrub vegetation remains highly variable with a trend towards increasing growth with warming. Elevated CO2 enhancements of growth are not yet evident in the data. Second-year results will also be reported. Long-term hypotheses for increased woody plant growth under warming include potential enhancements driven by increased nutrient availability from warming induced decomposition of surface peats.

  2. The American cranberry crowned jewel of the bog at the 2014 U.S.A. Science & Engineering Festival

    Science.gov (United States)

    For researchers in Dr. Juan Zalapa’s Cranberry Genetics and Genomics Lab, part of the USDA-ARS Vegetable Crops Research Unit, cranberries are more than a side dish on their Thanksgiving tables, they are the main course in their daily studies. The majority of these little red super-fruits come from t...

  3. The role of Juncus effusus litter quality and nutrient availability on organic matter decomposition in restored cutover bogs

    Science.gov (United States)

    Agethen, Svenja; Knorr, Klaus-Holger

    2017-04-01

    More than 90% of peatlands in Europe are degraded by drainage and subsequent land use. However, beneficial effects of functioning peatlands, most of all carbon storage, have long been recognized but remain difficult to recover. Fragmentation and a surrounding of intensively used agricultural catchments with excess nutrients in air and waters further affects the recovery of sites. Under such conditions, highly competitive species such as Juncus effusus colonize restored peatlands instead of peat forming Sphagnum. While the specific stoichiometry and chemical composition makes Sphagnum litter recalcitrant in decomposition and hence, effective in carbon sequestration, we know little about dynamics involving Juncus, although this species provides organic matter in high quantity and of rather labile quality. To better understand decomposition in context of litter quality and nutrient availability, we incubated different peat types for 70 days; I) recent, II) weakly degraded fossil, and III) earthyfied nutrient rich fossil peat, amended with two 13C pulse-labelled Juncus litter types (excessively fertilized "F", and nutrient poor "NF" plants grown for three years watered with MilliQ only), respectively. We determined anaerobic decomposition rates, compared potential rates extrapolated from pure materials with measured rates of the mixtures, and tracked the 13C in the solid, liquid, and gaseous phase. To characterize the biogeochemical conditions, inorganic and organic electron acceptors, hydrogen and organic acids, and total enzyme activity were monitored. For characterization of dissolved organic matter we used UV-Vis and fluorescence spectroscopy (parallel factor analysis), and for solid organic matter elemental analysis and FTIR spectroscopy. There were two main structural differences between litter types: "F" litter and its leachates contained more proteinaceous components, the C/N ratio was 20 in contrast to 60 of the "NF" litter. However, humic components and aromaticity were higher in "F" litter. Generally, decomposition rates of litter were 5-30 times higher than of peat. Rates in batches amended with "F" were lower compared to "NF" for the respective peat, opposing typically reported observations. Nevertheless, the 13C label suggested that in case of peat I and III preferably the litter was decomposed, decomposition of peat II was apparently stimulated when "NF" was added, albeit this litter was poor in nutrients. Multiple linear regression identified specific absorption at 254 nm (SUVA), a measure of aromaticity representative for an array of inter-correlating spectroscopic features, and enzyme activity as most important predictors for C-mineralization rates. These two parameters explained 88% of the variance. Although enzyme activity and SUVA did not correlate in the mixed assays, this was the case for the pure materials (R2=0.95), suggesting an inhibitory effect of aromatic components on enzyme activity. This study confirms that generally litter quality is a major control for mineralization and hence, carbon storage in peatlands. Interestingly, in the case of Juncus effusus, high nutrient availability in peat and litter did not lead to enhanced degradation of the litter itself or priming of decomposition of the surrounding peat. Furthermore, the results underline the substantial contribution of Juncus biomass to C-cycling and potentially high C-emissions in restored peatlands.

  4. Staphylinid beetles (Coleoptera, Staphylinidae) recorded by pitfall and light trapping in Mrtvý Luh peat bog

    Czech Academy of Sciences Publication Activity Database

    Boháč, Jaroslav; Bezděk, A.

    2004-01-01

    Roč. 10, - (2004), s. 141-150 ISSN 1211-7420 R&D Projects: GA AV ČR KSK6005114 Institutional research plan: CEZ:AV0Z6087904 Keywords : Staphylinidae * flight activity * distribution Subject RIV: EH - Ecology, Behaviour

  5. Flight Morphology, Compound Eye Structure and Dispersal in the Bog and the Cranberry Fritillary Butterflies: An Inter- and Intraspecific Comparison.

    Science.gov (United States)

    Turlure, Camille; Schtickzelle, Nicolas; Van Dyck, Hans; Seymoure, Brett; Rutowski, Ronald

    2016-01-01

    Understanding dispersal is of prime importance in conservation and population biology. Individual traits related to motion and navigation during dispersal may differ: (1) among species differing in habitat distribution, which in turn, may lead to interspecific differences in the potential for and costs of dispersal, (2) among populations of a species that experiences different levels of habitat fragmentation; (3) among individuals differing in their dispersal strategy and (4) between the sexes due to sexual differences in behaviour and dispersal tendencies. In butterflies, the visual system plays a central role in dispersal, but exactly how the visual system is related to dispersal has received far less attention than flight morphology. We studied two butterfly species to explore the relationships between flight and eye morphology, and dispersal. We predicted interspecific, intraspecific and intersexual differences for both flight and eye morphology relative to i) species-specific habitat distribution, ii) variation in dispersal strategy within each species and iii) behavioural differences between sexes. However, we did not investigate for potential population differences. We found: (1) sexual differences that presumably reflect different demands on both male and female visual and flight systems, (2) a higher wing loading (i.e. a proxy for flight performance), larger eyes and larger facet sizes in the frontal and lateral region of the eye (i.e. better navigation capacities) in the species inhabiting naturally fragmented habitat compared to the species inhabiting rather continuous habitat, and (3) larger facets in the frontal region in dispersers compared to residents within a species. Hence, dispersers may have similar locomotory capacity but potentially better navigation capacity. Dispersal ecology and evolution have attracted much attention, but there are still significant gaps in our understanding of the mechanisms of dispersal. Unfortunately, for many species we lack detailed information on the role of behavioural, morphological and physiological traits for dispersal. Our novel study supports the existence of inter- and intra-specific evolutionary responses in both motion and navigation capacities (i.e. flight and eye morphology) linked to dispersal.

  6. Long-term vegetation changes in bogs exposed to high amospheric deposition, aerial liming and climate fluctuation

    Czech Academy of Sciences Publication Activity Database

    Hájková, Petra; Hájek, Michal; Rybníček, Kamil; Jiroušek, M.; Tichý, L.; Králová, Š.; Mikulášková, E.

    2011-01-01

    Roč. 22, č. 5 (2011), s. 891-904 ISSN 1100-9233 R&D Projects: GA ČR GA206/08/0389 Institutional research plan: CEZ:AV0Z60050516 Keywords : Oxycocco-Sphagnetea * permanent plot * succession Subject RIV: EF - Botanics Impact factor: 2.770, year: 2011

  7. Impact of Peat Mining and Restoration on Methane Turnover Potential and Methane-Cycling Microorganisms in a Northern Bog.

    Science.gov (United States)

    Reumer, Max; Harnisz, Monika; Lee, Hyo Jung; Reim, Andreas; Grunert, Oliver; Putkinen, Anuliina; Fritze, Hannu; Bodelier, Paul L E; Ho, Adrian

    2018-02-01

    Ombrotrophic peatlands are a recognized global carbon reservoir. Without restoration and peat regrowth, harvested peatlands are dramatically altered, impairing their carbon sink function, with consequences for methane turnover. Previous studies determined the impact of commercial mining on the physicochemical properties of peat and the effects on methane turnover. However, the response of the underlying microbial communities catalyzing methane production and oxidation have so far received little attention. We hypothesize that with the return of Sphagnum spp. postharvest, methane turnover potential and the corresponding microbial communities will converge in a natural and restored peatland. To address our hypothesis, we determined the potential methane production and oxidation rates in natural (as a reference), actively mined, abandoned, and restored peatlands over two consecutive years. In all sites, the methanogenic and methanotrophic population sizes were enumerated using quantitative PCR (qPCR) assays targeting the mcrA and pmoA genes, respectively. Shifts in the community composition were determined using Illumina MiSeq sequencing of the mcrA gene and a pmoA -based terminal restriction fragment length polymorphism (t-RFLP) analysis, complemented by cloning and sequence analysis of the mmoX gene. Peat mining adversely affected methane turnover potential, but the rates recovered in the restored site. The recovery in potential activity was reflected in the methanogenic and methanotrophic abundances. However, the microbial community composition was altered, being more pronounced for the methanotrophs. Overall, we observed a lag between the recovery of the methanogenic/methanotrophic activity and the return of the corresponding microbial communities, suggesting that a longer duration (>15 years) is needed to reverse mining-induced effects on the methane-cycling microbial communities. IMPORTANCE Ombrotrophic peatlands are a crucial carbon sink, but this environment is also a source of methane, an important greenhouse gas. Methane emission in peatlands is regulated by methane production and oxidation catalyzed by methanogens and methanotrophs, respectively. Methane-cycling microbial communities have been documented in natural peatlands. However, less is known of their response to peat mining and of the recovery of the community after restoration. Mining exerts an adverse impact on potential methane production and oxidation rates and on methanogenic and methanotrophic population abundances. Peat mining also induced a shift in the methane-cycling microbial community composition. Nevertheless, with the return of Sphagnum spp. in the restored site after 15 years, methanogenic and methanotrophic activity and population abundance recovered well. The recovery, however, was not fully reflected in the community composition, suggesting that >15 years are needed to reverse mining-induced effects. Copyright © 2018 American Society for Microbiology.

  8. Impact of peat mining, and restoration on methane turnover potentials and methane-cycling microorganisms in a northern bog

    NARCIS (Netherlands)

    Reumer, Max; Harnisz, M.; Lee, H.J.; Reim, A.; Grunert, O.; Putkinen, A.; Fritze, H.; Bodelier, P.L.E.; Ho, A.

    2018-01-01

    Ombrotrophic peatlands are a recognized global carbon reservoir. Without restoration and peat regrowth, harvested peatlands are dramatically altered, impairing its carbon sink function, with consequences for methane turnover. Previous studies determined the impact of commercial mining on the peat

  9. Plant carnivory beyond bogs: reliance on prey feeding in Drosophyllum lusitanicum (Drosophyllaceae) in dry Mediterranean heathland habitats

    Science.gov (United States)

    Gil-Cabeza, E.; Ojeda, F.

    2017-01-01

    Background and Aims In a cost–benefit framework, plant carnivory is hypothesized to be an adaptation to nutrient-poor soils in sunny, wetland habitats. However, apparent exceptions to this cost–benefit model exist, although they have been rarely studied. One of these exceptions is the carnivorous subshrub Drosophyllum lusitanicum, which thrives in Mediterranean heathlands on dry sandstone soils and has relatively well-developed, xeromorphic roots. Here, the roles of leaf (carnivory) and root (soil) nutrient uptake in growth promotion of this particular species were assessed. Methods In a greenhouse experiment, plants were fed with laboratory-reared fruit flies (Drosophila virilis) and received two concentrations of soil nutrients in a factorial design. Above-ground plant growth and final above- and below-ground dry biomass after 13 weeks were recorded. Nutrient uptake via roots was also evaluated, using stable nitrogen isotope analysis. Key Results Insect feeding resulted in significantly higher growth and above- and below-ground biomass compared with soil fertilization. No additional benefits of fertilization were discernable when plants were insect-fed, indicating that roots were not efficient in nutrient absorption. Conclusions The first evidence of strong reliance on insect prey feeding in a dry-soil carnivorous plant with well-developed roots is provided, suggesting that carnivory per se does not preclude persistence in dry habitats. Instead, the combination of carnivory and xeromorphic root features allows Drosophyllum to thrive on non-waterlogged soils. New evidence is added to recent research emphasizing the role of root systems of carnivorous plants in explaining their distribution, partly challenging the cost–benefit hypothesis. PMID:28065921

  10. Effects of human impact and climate change during the last 350 years recorded in a Swedish raised bog deposit

    NARCIS (Netherlands)

    van der Linden, M.; Vickery, E.; Charman, D.J.; van Geel, B.

    2008-01-01

    A peat core from an ombrotrophic mire in central Sweden was analysed for multi-proxy indicators (plant macrofossils, pollen/non-pollen microfossils, testate amoebae, colorimetric humification, carbon/nitrogen ratios, bulk densities, loss on ignition), to evaluate the relative contributions of

  11. Performing Translation as Practice-led Research: The Case of Carr’s “By the Bog of Cats…” in Brazil

    Directory of Open Access Journals (Sweden)

    Alinne Balduino P. Fernandes

    2015-12-01

    an individual task, originating in the complex act of reading the play-text, its final trajectory is deeply influenced by the creative insights of the production team. The overarching objectives of this article are, therefore: firstly to account for the overall process of translating for the stage, from the early drafts of the translation to the rehearsal process, and ultimately to the staged reading of the play; and secondly, to offer a narrative for how the cultural encounter between the exporting and importing cultures has taken place through translation and theatrical performance.

  12. Parasitoids (Hymenoptera) of leaf-spinning moths (Lepidoptera) feeding on Vaccinium uliginosum L. along an ecological gradient in central European peat bogs

    Czech Academy of Sciences Publication Activity Database

    Lozan, Aurel; Spitzer, Karel; Jaroš, Josef; Khalaim, A.; Rizzo, M. C.; Guerrieri, E.; Bezděk, Aleš

    2010-01-01

    Roč. 21, č. 4 (2010), s. 243-253 ISSN 0785-8760 R&D Projects: GA AV ČR 1QS500070505 Grant - others:EU Synthesys(BE) GB-TAF-4159; European Science Foundation(BE) 1667 Institutional research plan: CEZ:AV0Z50070508 Keywords : Vaccinium uliginosum L. Subject RIV: EH - Ecology, Behaviour Impact factor: 0.321, year: 2010

  13. Deciphering human-climate interactions in an ombrotrophic peat record: REE, Nd and Pb isotope signatures of dust supplies over the last 2500 years (Misten bog, Belgium)

    Science.gov (United States)

    Fagel, N.; Allan, M.; Le Roux, G.; Mattielli, N.; Piotrowska, N.; Sikorski, J.

    2014-06-01

    A high-resolution peat record from Eastern Belgium reveals the chronology of dust deposition for the last 2500 years. REE and lithogenic elements in addition to Nd and Pb isotopes were measured in a 173 cm age-dated peat profile and provide a continuous chronology of dust source and intensity. Calculated dust flux show pronounced increases c. 300 BC, 600 AD, 1000 AD, 1200 AD and from 1700 AD, corresponding to local and regional human activities combined with climate change. The Industrial Revolution samples (1700-1950 AD) are characterised by a significant enrichment in Sc-normalised REE abundance (sum REE/Sc > 25) due to intensive coal combustion. For the pre-Industrial Revolution samples, the Sc-normalised REE abundance (10 periods characterised by dominant-distal sources (c. 320 AD, 1000 AD and 1700 AD) are consistent with local wetter-than-average intervals as indicated by a lower degree of peat humification. Local erosion prevails during the drier (higher humification) intervals (100 AD, 600 AD). On a global scale, more distal supplies are driven during colder periods, in particular during the Oort and Maunder minima, suggesting a potential link between dust deposition and global climate. Combining REE abundance, fractionation between Light REE and Heavy REE and Nd isotope data in ombrotrophic peat allows one to distinguish between dust flux changes related to human and climate forcings.

  14. Growth response of downy birch (Betula pubescens) to moisture treatment at an cut-over peat bog in the Šumava Mts., Czech Republic

    Czech Academy of Sciences Publication Activity Database

    Lanta, Vojtěch; Hazuková, I.

    2005-01-01

    Roč. 42, - (2005), s. 247-256 ISSN 0003-3847 R&D Projects: GA ČR GD206/03/H034 Institutional research plan: CEZ:AV0Z6005908 Keywords : Betula pubescens * cut-over peatland * increment Subject RIV: EF - Botanics Impact factor: 0.315, year: 2005

  15. The influence of climate change on recent peat accumulation patterns of Distichia muscoides cushion bogs in the high-elevation tropical Andes of Colombia

    Science.gov (United States)

    Benavides, Juan C.; Vitt, Dale H.; Wieder, R. Kelman

    2013-12-01

    Extensive cushions of Distichia muscoides found at high elevations in the Andes form deep deposits of peat and function as peatland. The location of Distichia peatlands at the highest elevations makes them susceptible to the effects of global change including global warming. Accumulation rates of organic matter are the key function of peatland ecosystems and are highly susceptible to changes in climate. This study used 210Pb chronologies to infer the recent dynamics of three Distichia muscoides peatlands located above 4000 m in elevation. Chronological markers from dated volcanic eruptions were correlated to the 210Pb chronologies of Distichia peat and validated the 210Pb chronologies. Changes in 210Pb activity with depth indicated rapid accumulation in recent times. Organic matter had a mean accumulation rate of 1400 g m-2 yr-1 during the past 10 years, with values well above the observed regional accumulation rate of 300-400 g m-2 yr-1. The same pattern was observed in peat accretion rates, with growth rates of 1-2 cm per year during the last 10 years. Cushion plants engineer their own environment, allowing the system to be less susceptible to direct changes in climate. However, the high rates of peat accretion in recent times may be originated from increasing temperatures and excess water from nearby glacier melt. However, glaciers are predicted to disappear during the next 20 years in the northern Andes, reducing water inputs in tropical high-elevation ecosystems.

  16. No effects of experimental warming but contrasting seasonal patterns for soil peptidase and glycosidase enzymes in a sub-arctic peat bog

    NARCIS (Netherlands)

    Weedon, J.T.; Aerts, R.; Kowalchuk, G.A.; van Bodegom, P.M.

    2014-01-01

    The nature of linkages between soil C and N cycling is important in the context of terrestrial ecosystem responses to global environmental change. Extracellular enzymes produced by soil microorganisms drive organic matter decomposition, and are considered sensitive indicators of soil responses to

  17. The origin and vegetation development of the Rejvíz pine bog and the history of the surrounding landscape during the Holocene

    Czech Academy of Sciences Publication Activity Database

    Dudová, Lydie; Hájek, M.; Hájková, P.

    2010-01-01

    Roč. 82, č. 2 (2010), s. 223-246 ISSN 0032-7786 R&D Projects: GA ČR GA206/08/0389 Institutional research plan: CEZ:AV0Z60050516 Keywords : palaeoecology * peatland * pollen Subject RIV: EF - Botanics Impact factor: 2.792, year: 2010

  18. Origin of a boreal birch bog woodland and landscape development on a warm low mountain summit at the Carpathian–Pannonian interface

    Czech Academy of Sciences Publication Activity Database

    Gálová, A.; Hájková, Petra; Čierniková, M.; Petr, L.; Hájek, M.; Novák, J.; Rohovec, Jan; Jamrichová, Eva

    2016-01-01

    Roč. 26, č. 7 (2016), s. 1112-1125 ISSN 0959-6836 Institutional support: RVO:67985831 ; RVO:67985939 Keywords : charcoal * lake sediment * macrofossil * peat chemistry * phytogeography * pollen Subject RIV: DB - Geology ; Mineralogy; EH - Ecology, Behaviour (BU-J) Impact factor: 2.324, year: 2016

  19. Soil thermal dynamics, snow cover, and frozen depth under five temperature treatments in an ombrotrophic bog: Constrained forecast with data assimilation

    Science.gov (United States)

    Huang, Yuanyuan; Jiang, Jiang; Ma, Shuang; Ricciuto, Daniel; Hanson, Paul J.; Luo, Yiqi

    2017-08-01

    Accurate simulation of soil thermal dynamics is essential for realistic prediction of soil biogeochemical responses to climate change. To facilitate ecological forecasting at the Spruce and Peatland Responses Under Climatic and Environmental change site, we incorporated a soil temperature module into a Terrestrial ECOsystem (TECO) model by accounting for surface energy budget, snow dynamics, and heat transfer among soil layers and during freeze-thaw events. We conditioned TECO with detailed soil temperature and snow depth observations through data assimilation before the model was used for forecasting. The constrained model reproduced variations in observed temperature from different soil layers, the magnitude of snow depth, the timing of snowfall and snowmelt, and the range of frozen depth. The conditioned TECO forecasted probabilistic distributions of soil temperature dynamics in six soil layers, snow, and frozen depths under temperature treatments of +0.0, +2.25, +4.5, +6.75, and +9.0°C. Air warming caused stronger elevation in soil temperature during summer than winter due to winter snow and ice. And soil temperature increased more in shallow soil layers in summer in response to air warming. Whole ecosystem warming (peat + air warmings) generally reduced snow and frozen depths. The accuracy of forecasted snow and frozen depths relied on the precision of weather forcing. Uncertainty is smaller for forecasting soil temperature but large for snow and frozen depths. Timely and effective soil thermal forecast, constrained through data assimilation that combines process-based understanding and detailed observations, provides boundary conditions for better predictions of future biogeochemical cycles.

  20. Effect of disturbance on the vegetation of peat bogs with Pinus rotundata in the Třeboň Basin, Czech Republic

    Czech Academy of Sciences Publication Activity Database

    Bastl, M.; Štechová, T.; Prach, Karel

    2009-01-01

    Roč. 81, č. 2 (2009), s. 105-117 ISSN 0032-7786 R&D Projects: GA AV ČR IAA600050702 Institutional research plan: CEZ:AV0Z60050516 Keywords : succession * vascular plants * species composition Subject RIV: EH - Ecology, Behaviour Impact factor: 2.638, year: 2009

  1. Calculation of Boil-Off Gas (BOG Generation of KC-1 Membrane LNG Tank with High Density Rigid Polyurethane Foam by Numerical Analysis

    Directory of Open Access Journals (Sweden)

    Jeong Hyeonwon

    2017-03-01

    Full Text Available Recently, a new type of LNG tank named “KC-1 membrane LNG tank” has been developed by Korean Gas Corporation (KOGAS, and Samsung Heavy Industries (SHI is currently building KC-1 membrane type LNG carriers. Unlike other LNG tanks, the KC-1 membrane LNG tank has a single-insulation structure rather than a double-insulation structure. For a given tank’s boundary condition, heat transfer analysis is performed from the external to the internal environment of the LNG tank by numerical simulation for three tanks. In each tank, the main thermally resistant layer of insulation is assembled with a High density rigid Polyurethane Foam (H-PUF, which is blown with one of three different types of hydrofluorocarbons-namely-HFC-365mfc, 245fa, and 245fa-e (enhanced. Advantage of such blowing agents is that it has a lower Ozone Depletion Potential (ODP than HCFC-141b or carbon dioxide (CO2 that has been used in the past as well as having low thermal conductivity. A Reduced Order Model is utilized to a 3-dimensional section of the insulation to calculate equivalent thermal conductivity. The equivalent thermal conductivity of the insulation is then applied to the rest of LNG tank, reducing the size of tank simulation domain as well as computation time. Tank’s two external and internal boundary conditions used are those defined by the International Code for the Construction and Equipment of Ships Carrying Liquefied Gases in Bulk (IGC and the United States Coast Guard (USCG conditions. Boil-off Rate (BOR of the tank that has the insulation with H-PUF blown with HFC-245fa resulted in 0.0927 %/day and 0.0745 %/day for IGC and USCG conditions, respectively.

  2. Soil thermal dynamics, snow cover, and frozen depth under five temperature treatments in an ombrotrophic bog: Constrained forecast with data assimilation: Forecast With Data Assimilation

    Energy Technology Data Exchange (ETDEWEB)

    Huang, Yuanyuan [Department of Microbiology and Plant Biology, University of Oklahoma, Norman Oklahoma USA; Jiang, Jiang [Department of Microbiology and Plant Biology, University of Oklahoma, Norman Oklahoma USA; Key Laboratory of Soil and Water Conservation and Ecological Restoration in Jiangsu Province, Collaborative Innovation Center of Sustainable Forestry in Southern China of Jiangsu Province, Nanjing Forestry University, Nanjing China; Ma, Shuang [Department of Microbiology and Plant Biology, University of Oklahoma, Norman Oklahoma USA; Ricciuto, Daniel [Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge Tennessee USA; Hanson, Paul J. [Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge Tennessee USA; Luo, Yiqi [Department of Microbiology and Plant Biology, University of Oklahoma, Norman Oklahoma USA; Department of Earth System Science, Tsinghua University, Beijing China

    2017-08-01

    Accurate simulation of soil thermal dynamics is essential for realistic prediction of soil biogeochemical responses to climate change. To facilitate ecological forecasting at the Spruce and Peatland Responses Under Climatic and Environmental change site, we incorporated a soil temperature module into a Terrestrial ECOsystem (TECO) model by accounting for surface energy budget, snow dynamics, and heat transfer among soil layers and during freeze-thaw events. We conditioned TECO with detailed soil temperature and snow depth observations through data assimilation before the model was used for forecasting. The constrained model reproduced variations in observed temperature from different soil layers, the magnitude of snow depth, the timing of snowfall and snowmelt, and the range of frozen depth. The conditioned TECO forecasted probabilistic distributions of soil temperature dynamics in six soil layers, snow, and frozen depths under temperature treatments of +0.0, +2.25, +4.5, +6.75, and +9.0°C. Air warming caused stronger elevation in soil temperature during summer than winter due to winter snow and ice. And soil temperature increased more in shallow soil layers in summer in response to air warming. Whole ecosystem warming (peat + air warmings) generally reduced snow and frozen depths. The accuracy of forecasted snow and frozen depths relied on the precision of weather forcing. Uncertainty is smaller for forecasting soil temperature but large for snow and frozen depths. Timely and effective soil thermal forecast, constrained through data assimilation that combines process-based understanding and detailed observations, provides boundary conditions for better predictions of future biogeochemical cycles.

  3. Problem - oriented studies on plant - soil - water relations : sowing strategies for maize in rainfed agriculture in Southern Mozambique : water management in bog relicts in the Netherlands

    NARCIS (Netherlands)

    Schouwenaars, J.M.

    1990-01-01

    Plant-soil-water models are applied in two case studies. Attention is given to the desired level of accuracy in (agro-)hydrological. research when applied in problem-oriented studies. In the case studies it is shown that when decision criteria are only roughly known and when only

  4. Seasonal climate manipulations have only minor effects on litter decomposition rates and N dynamics but strong effects on litter P dynamics of sub-arctic bog species.

    NARCIS (Netherlands)

    Aerts, R.; Callaghan, T.V.; Dorrepaal, E.; van Logtestijn, R.S.P; Cornelissen, J.H.C.

    2012-01-01

    Litter decomposition and nutrient mineralization in high-latitude peatlands are constrained by low temperatures. So far, little is known about the effects of seasonal components of climate change (higher spring and summer temperatures, more snow which leads to higher winter soil temperatures) on

  5. Spatial distribution of ground beetles (Coleoptera : Carabidae) and moths (Lepidoptera) in the Mrtvy luh bog, Sumava Mts (Central Europe): A test of habitat island community

    Czech Academy of Sciences Publication Activity Database

    Bezděk, Aleš; Jaroš, Josef; Spitzer, Karel

    2006-01-01

    Roč. 15, č. 1 (2006), s. 395-409 ISSN 0960-3115 R&D Projects: GA AV ČR(CZ) IAA600070501 Institutional research plan: CEZ:AV0Z50070508 Keywords : Carabidae * central Europe * community ecology Subject RIV: EH - Ecology, Behaviour Impact factor: 1.423, year: 2006

  6. How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire

    Czech Academy of Sciences Publication Activity Database

    Hájková, Petra; Grootjans, A.B.; Lamentowicz, M.; Rybníčková, E.; Madaras, M.; Opravilová, V.; Michaelis, D.; Hájek, Michal; Joosten, H.; Wolejko, L.

    2012-01-01

    Roč. 27, č. 3 (2012), s. 233-243 ISSN 0267-8179 Institutional research plan: CEZ:AV0Z60050516 Institutional support: RVO:67985939 Keywords : Holocene * succession * mire Subject RIV: EF - Botanics Impact factor: 2.939, year: 2012

  7. Kant's Theory of virtue

    DEFF Research Database (Denmark)

    Nielsen, Carsten Fogh

    2012-01-01

    Anmeldelse af Anne Margaret Baxleys bog: "Kant's Thery of Virtue. The Value of Autocracy" (Cambridge University Press, 2010)......Anmeldelse af Anne Margaret Baxleys bog: "Kant's Thery of Virtue. The Value of Autocracy" (Cambridge University Press, 2010)...

  8. Norsk inspiration til uddannelse og job

    DEFF Research Database (Denmark)

    Skovhus, Randi Boelskifte; Thomsen, Rie; Buhl, Rita

    2017-01-01

    Anmeldelse af bog om det norske fag Utdanningsvalg - inspiration til arbejde med uddannelse og job......Anmeldelse af bog om det norske fag Utdanningsvalg - inspiration til arbejde med uddannelse og job...

  9. Flow i ledelse - det er god forretning

    DEFF Research Database (Denmark)

    Andersen, Frans Ørsted; Csikszentmihalyi, Mihaly

    2015-01-01

    Forord til den danske udgave af Mihaly Csikszentmihalyis bog "God forretning - ledelse, flow og skabelse af mening"......Forord til den danske udgave af Mihaly Csikszentmihalyis bog "God forretning - ledelse, flow og skabelse af mening"...

  10. Harriet Bjerrum Nielsen

    DEFF Research Database (Denmark)

    Hansen, Niels-Henrik Møller

    2011-01-01

    Anmeldelse i tidsskriftet Dansk Sociologi af Harriet Bjerrum Nielsens bog "Skoletid. Piger og drenge fra 1. til 9. klasse".......Anmeldelse i tidsskriftet Dansk Sociologi af Harriet Bjerrum Nielsens bog "Skoletid. Piger og drenge fra 1. til 9. klasse"....

  11. Morality, Moral Luck and Responsibility. Fortune's Web

    DEFF Research Database (Denmark)

    Nielsen, Carsten Fogh

    2011-01-01

    Anmeldelse af Nafsika Athanassoulis bog: Morality, Moral Lock and Responsibility (Palgrave MacMillian 2010)......Anmeldelse af Nafsika Athanassoulis bog: Morality, Moral Lock and Responsibility (Palgrave MacMillian 2010)...

  12. Evaluering af lokale udviklingsprocesser

    DEFF Research Database (Denmark)

    Rasbech Nielsen, Mie; Jensen, Bente

    Arbejdspapir udviklet til HPA-projektet 2007. Revideret, nyt forord, ISBN nummer og udgivet som e-bog......Arbejdspapir udviklet til HPA-projektet 2007. Revideret, nyt forord, ISBN nummer og udgivet som e-bog...

  13. Variation in hydrologic connectivity as a result of microtopography explained by discharge to catchment size relationship

    NARCIS (Netherlands)

    Oosterwoud, Marieke; Ploeg, van der Martine; Schaaf, van der Sake; Zee, van der Sjoerd

    2017-01-01

    In hydrological terms, raised bogs are often approximated by simple models as in the acrotelm-catotelm concept. However, raised bogs are often characterized by a pronounced surface topography, causing large changes in connectivity of contributing areas on the bog. In this study, daily regression

  14. Stjernebilleder I

    DEFF Research Database (Denmark)

    2012-01-01

    Valg af materiale/medie/form: iBog Valg af arbejdsform: iBog er relevant for digitale hold i læreruddannelsen Begrundelse for valg af materiale/medie/form/arbejdsform: iBog er relevant for studerende i læreruddannelsen...

  15. Characterisation of Sanguinhal Mire, Terceira Island (Azores: a protected quaking bog habitat Caracterização da Turfeira do Sanguinhal, ilha Terceira (Açores um habitat protegido de turfeira ondulante

    Directory of Open Access Journals (Sweden)

    Cândida Mendes

    2009-09-01

    Full Text Available The Azores archipelago in the North Atlantic is an important area for biodiversity because it is rich in rare species and habitats, and almost undisturbed. Sanguinhal mire was originally a lake that evolved through paludification into a peat habitat. It is located inside Nature 2000 (European Union for Protection of Nature and Biodiversity, Council Directive 92/43/EEC of 21 May 1992 on the conservation of natural habitats and of wild fauna and flora, Habitat Directive Annex I(b habitat 7140 area of Santa Bárbara and Pico Alto Mountains on the island of Terceira, and it is a good example of a basin peatland type that was first discovered in 1998. This paper provides baseline information on its flora, vegetation communities, structure, surface hydrology and chemistry. Forty-one plant species including six Sphagnum species and ten endemic vascular plants have been recorded, and eight plant communities are distinguished. The maximum peat depth is 2.5 m. The mire receives flowing water from its margins, in addition to intercepted precipitation and fog. After precipitation, water drains through several placic rupture points. Both pH and water conductivity were measured, with some ecological tendencies observed. The conservation status of the mire is good, but it is subject to increasing pressure from cattle pasture and a walking trail that constrains natural surface water movement.O Arquipélago dos Açores no Atlântico Norte é uma área importante em biodiversidade, rica em espécies e habitats raros em estado selvagem. A turfeira do Sanguinhal foi originalmente uma lagoa que evoluiu por paludificação para um habitat de turfa. Esta localiza-se na Rede Natura 2000 (União Europeia para a Proteção da Natureza e Biodiversidade, Directive do Conselho 92/43/EEC de 21 de Maio 1992 sobre a concervação de habitats naturais e da fauna e flora, Diretiva de Habitat Anexo I(b habitat 7140 da Serra de Santa Bárbara e Pico Alto e é um bom exemplo de um tipo de turfeira de bacia, descoberto pela primeira vez em 1998. Este trabalho provê informações iniciais sobre a flora, as comunidades vegetais, a estrutura, as caracteristicas químicas da água e o regime hidrológico de superfície. Foram identificadas 41 espécies vegetais, incluindo 6 espécies do género Sphagnum, e 10 espécies de plantas vasculares endêmicas, forma identificadas oito comunidades vegetais. A profundidade máxima de turfa é de 2,5 m. A turfeira recebe água superficial de suas margens, além da precipitação interceptada e da névoa. Depois das chuvas, a água é drenada por vários pontos da turfeira onde o placic se rompeu. O pH e a condutividade das água foram medidos tendo-se verificado algumas tendências. O estado de conservação da turfeira é bom embora esteja sujeita a um crescente pastoreio por gado selvagem e a abertura de trilhos de forma desordenada altera o natural movimento de água na turfeira.

  16. Sollevarsi dallo stagno afferrandosi per il codino. L’attualità della metacritica di Theodor W. Adorno (Pulling oneself out of the bog by one’s own pigtail. The legacy of Theodor W. Adorno’s metacritique

    Directory of Open Access Journals (Sweden)

    Luca BALDASSARRE

    2016-11-01

    Full Text Available n this article the author highlights some issues about Adorno’s thought that are fundamental to be acquired in the present age. It focuses on the questions most criticized in the postwar period: cultural industry, managed world, presumed snobbery about mass society, decline of aura, end of individuality, post-individual or pseudo-individuality, ticket mentality. Therefore, the author suggests to explain contemporary age starting from the Adornian model, an important interpretive antecedent to understand new media and the world that they produce. So this article underscores the similarity about many causes for reflection in Theodor W. Adorno and also H. Marcuse: in spite of oustanding differences, both theorists persist on the “power of negative thinking” and on the “feeling of the contrary”. This persistence lays the foundations of critical thought in Adorno, who shows parodying art such as the critical model par excellence. Finally, last pages are directed to remark the importance of Adorno’s thought such as metacritical philosophy, surely more fruitful than the paradigm of the “second generation” in the following decades.

  17. Free-living nematodes (Nematoda) of the Rokytská Slať and the Chalupská Slať peat bogs in the Bohemian Forest (Czech Republic)

    Czech Academy of Sciences Publication Activity Database

    Háněl, Ladislav

    2015-01-01

    Roč. 79, č. 3 (2015), s. 199-213 ISSN 1211-376X R&D Projects: GA ČR GA206/99/1416 Institutional support: RVO:60077344 Keywords : soil zoology * ecology * Nematoda * diversity * peatland Subject RIV: EH - Ecology, Behaviour

  18. Variability of Lepidoptera communities (moths and butterflies) along an altitudinal gradient of peat bogs from the Třeboň Basin up to the Bohemian Forest (South Bohemia, Central Europe)

    Czech Academy of Sciences Publication Activity Database

    Jaroš, Josef; Spitzer, Karel; Zikmundová, Hana

    2014-01-01

    Roč. 20, č. 2 (2014), s. 55-95 ISSN 1211-7420 Institutional support: RVO:60077344 Keywords : moths and butterflies * peatlands * communities Subject RIV: EH - Ecology, Behaviour http://www.npsumava.cz/ gallery /27/8381-sg_20_2_jarosetal.pdf

  19. Anmeldelse af Kristiansen, S. (2005). Kvalitativ dataanalyse og software - en introduktion til Nvivo

    DEFF Research Database (Denmark)

    Musaeus, Peter

    2005-01-01

    En anmdelse af en brugervenlig bog om Nvivo (QSR Nvivo), der er en videreudvikling af NUD*IST. Herværende bog, der er den første af sin slags på dansk, diskuteres i forhold til dens introduktion til Nvivo. Udgivelsesdato: december......En anmdelse af en brugervenlig bog om Nvivo (QSR Nvivo), der er en videreudvikling af NUD*IST. Herværende bog, der er den første af sin slags på dansk, diskuteres i forhold til dens introduktion til Nvivo. Udgivelsesdato: december...

  20. Udfordr eleverne og understøt dem i at gå fra konkret hverdagssprog til abstrakt fagsprog

    DEFF Research Database (Denmark)

    Østergren-Olsen, Dorte

    2011-01-01

    Artiklen er en anmeldelse af Pauline Gibbons bog English Learners. Academic Literacy and Thinking – Learning in the Challenging Zone......Artiklen er en anmeldelse af Pauline Gibbons bog English Learners. Academic Literacy and Thinking – Learning in the Challenging Zone...

  1. Evaluation of mitigation for acid aluminum leachate from a highway fill in Garrett County, Maryland. Research report (Final)

    International Nuclear Information System (INIS)

    Gracie, J.W.

    1992-01-01

    The effectiveness of a man-made sphagnum bog in reducing acidity and removing aluminum from an acidic leachate is evaluated. Although some effectiveness is demonstrated, the bog does not retain its ability to function as a result of physical changes due to uncontrolled sediment deposition in it

  2. Decomposition of Carex and Sphagnum litter in two mesotrophic fens differing in dominant plant species

    NARCIS (Netherlands)

    Scheffer, R.A.; Van Logtestijn, R. S P; Verhoeven, J. T A

    2001-01-01

    Peatlands can be classified into fens and bogs based on their hydrology. Development of fens to bogs is accompanied by the invasion of Sphagnum species. The purpose of this study was to determine how the decomposition process in fens is influenced by the transition from a vascular plant-dominated

  3. Distance Education Report, 2011-2012

    Science.gov (United States)

    California Community Colleges, Chancellor's Office, 2013

    2013-01-01

    This is a report on distance education in the California Community College. This is the seventh report to the California Community Colleges Board of Governors (BOG) per BOG Standing Order 409 (b) "that evaluates the effectiveness of distance education and education technology system wide and provides analysis of data demographically (by age,…

  4. Anjas univers

    DEFF Research Database (Denmark)

    Pedersen, Christine Pepke

    2017-01-01

    Anmeldelse af Anja C. Andersen, “En lille bog om Universet”, 256 sider, 165 kr. Lindhardt og Ringhof 2016 (fx saxo.com)......Anmeldelse af Anja C. Andersen, “En lille bog om Universet”, 256 sider, 165 kr. Lindhardt og Ringhof 2016 (fx saxo.com)...

  5. Hitler og Stalin arm i arm

    DEFF Research Database (Denmark)

    Bryld, Claus

    2015-01-01

    Levende fortalt bog om pagten mellem Hitler og Stalin, som udløste krigen og kastede lange skygger over Europas historie.......Levende fortalt bog om pagten mellem Hitler og Stalin, som udløste krigen og kastede lange skygger over Europas historie....

  6. Diagnosis of bacterial overgrowth of the small intestine. Comparison of the 14C-D-xylose breath test and jejunal cultures in 60 patients

    DEFF Research Database (Denmark)

    Rumessen, J J; Gudmand-Høyer, E; Bachmann, E

    1985-01-01

    the presence of BOG was ruled out (diagnoses: irritable bowel syndrome, 8; chronic diarrhoea, 6; and lactose malabsorption, 1). These patients were used as controls. The other 22 of the 60 patients could not be placed in either group owing to the presence of factors known to predispose for BOG; none of them...

  7. En verden uden ende

    DEFF Research Database (Denmark)

    Pedersen, Jens Olaf Pepke

    2017-01-01

    Multivers. Er der kun ét, eller er der utallige universer med hver sine naturlove? Det er emnet for en nyoversat bog af fysikeren Stephen Hawking og forfatteren Leonard Mlodinow.......Multivers. Er der kun ét, eller er der utallige universer med hver sine naturlove? Det er emnet for en nyoversat bog af fysikeren Stephen Hawking og forfatteren Leonard Mlodinow....

  8. Armillaria ectypa, a rare fungus of mire in Poland

    Directory of Open Access Journals (Sweden)

    Małgorzata Stasińska

    2015-08-01

    Full Text Available Armillaria ectypa is a saprotroph that occurs on active raised bogs and alkaline fens, as well as Aapa mires and transitional bogs. It is a very rare and threatened Eurasian species and one of the 33 fungal species proposed for inclusion into the Bern Convention. Its distribution in Poland, ecological notes and morphology of basidiocarp based on Polish specimens are presented.

  9. Capability Approach

    DEFF Research Database (Denmark)

    Kjeldsen, Christian Christrup; Jensen, Hans Iskov

    2010-01-01

    En kort og introducerende bog om Martha Nussbaums ti centrale kapabiliteter i relation til unge med særlige behov......En kort og introducerende bog om Martha Nussbaums ti centrale kapabiliteter i relation til unge med særlige behov...

  10. Ambiguous chair

    DEFF Research Database (Denmark)

    Manelius, Anne-Mette

    2011-01-01

    Bidrag til gør-det-selv bog, hvor det beskrives i udførlige tegninger, hvordan man bygger sin egen 'Ambiguous Chair', en tekstilforskallet stol.......Bidrag til gør-det-selv bog, hvor det beskrives i udførlige tegninger, hvordan man bygger sin egen 'Ambiguous Chair', en tekstilforskallet stol....

  11. The effect of temperature on growth and competition between Sphagnum species

    NARCIS (Netherlands)

    Breeuwer, A.J.G.; Heijmans, M.M.P.D.; Robroek, B.J.M.; Berendse, F.

    2008-01-01

    Peat bogs play a large role in the global sequestration of C, and are often dominated by different Sphagnum species. Therefore, it is crucial to understand how Sphagnum vegetation in peat bogs will respond to global warming. We performed a greenhouse experiment to study the effect of four

  12. Response of Sphagnum species mixtures to increased temperature and nitrogen availability

    NARCIS (Netherlands)

    Breeuwer, A.J.G.; Heijmans, M.M.P.D.; Berendse, F.; Gleichman, J.M.; Robroek, B.J.M.; Limpens, J.

    2009-01-01

    To predict the role of ombrotrophic bogs as carbon sinks in the future, it is crucial to understand how Sphagnum vegetation in bogs will respond to global change. We performed a greenhouse experiment to study the effects of two temperature treatments (17.5 and 21.7°C) and two N addition treatments

  13. Bag pigtråd

    DEFF Research Database (Denmark)

    Bjerre, Jacob Halvas

    2015-01-01

    BogFeature om Inger Bjørn Knudsen: Bag Pigtråd - Rom flygtningelejr 1945-1948. Udg. af Lemvig Museum, 2014. 80 sider......BogFeature om Inger Bjørn Knudsen: Bag Pigtråd - Rom flygtningelejr 1945-1948. Udg. af Lemvig Museum, 2014. 80 sider...

  14. Development and refinement of proxy-climate indicators from peats

    NARCIS (Netherlands)

    Chambers, F.M.; Booth, R.K.; De Vleeschouer, F.; Lamentowicz, M.; Le Roux, G.; Mauquoy, D.; Nichols, J.E.; van Geel, B.

    2012-01-01

    Peat, especially from acidic mires (bogs), is a natural archive of past environmental change. Reconstructions of past climate from bogs commenced in the 19th Century through examination of visible peat stratigraphy, and later formed the basis for a postglacial climatic scheme widely used in

  15. The Acid-Base Balance Between Organic Acids and Circumneutral Ground Waters in Large Peatlands

    Science.gov (United States)

    Siegel, D. I.; Glaser, P. H.; So, J.

    2006-05-01

    Organic acids supply most of the acidity in the surface waters of bogs in peatlands. Yet, the fundamental geochemical properties of peatland organic acids are still poorly known. To assess the geochemical properties of typical organic acid assemblages in peatlands, we used a triprotic analog model for peat pore waters and surface waters in the Glacial Lake Agassiz Peatlands, optimizing on charge balance and calibrated to estimates of mole site density in DOC and triprotic acid dissociation constants. Before the calibration process, all bog waters and 76% of fen waters had more than +20% charge imbalance. After calibration, most electrochemically balanced within 20%. In the best calibration, the mole site denisty of bog DOC was estimated as ~0.05 mmol/mmol C., approximately 6 times smaller than that for fen DOC or the DOC in the fen deeper fen peats that underlie bogs. The three modeled de-protonation constants were; pKa1 = ~3.0, pKa2 = ~4.5 and pKa3 = ~7.0 for the bog DOC, and; pKa1 = ~5.2, pKa2 =~ 6.5 and pKa3 = ~7.0 for the fen DOC. Bog DOC, behaves as a strong acid despite its small mole site density. The DOC in bog runoff can therefore theoretically acidify the surface waters in adjacent fens wherever these waters do not receive sufficient buffering alkalinity from active groundwater seepage.

  16. Retrofit design of a boil-off gas handling process in liquefied natural gas receiving terminals

    International Nuclear Information System (INIS)

    Park, Chansaem; Song, Kiwook; Lee, Sangho; Lim, Youngsub; Han, Chonghun

    2012-01-01

    Generation of Boil-off gas (BOG) in liquefied natural gas (LNG) receiving terminals considerably affects operating costs and the safety of the facility. For the above reasons, a proper BOG handling process is a major determinant in the design of a LNG receiving terminal. This study proposes the concept of a retrofit design for a BOG the handling process using a fundamental analysis. A base design was determined for a minimum send-out case in which the BOG handling becomes the most difficult. In the proposed design, the cryogenic energy of the LNG stream is used to cool other streams inside the process. It leads to a reduction in the operating costs of the compressors in the BOG handling process. Design variables of the retrofit design were optimized with non-linear programming to maximize profitability. Optimization results were compared with the base design to show the effect of the proposed design. The proposed design provides a 22.7% energy saving ratio and a 0.176 year payback period. -- Highlights: ► A retrofit design of the BOG handling process was proposed to maximize energy savings. ► The superstructure of the proposed design was developed based on a thermodynamic analysis. ► In the proposed design, the cryogenic energy of the LNG stream was utilized to directly cool down the BOG streams. ► The payback period of the proposed design is sufficiently short for investment in industry.

  17. Politisk marketing

    DEFF Research Database (Denmark)

    Disciplinen politisk marketing er udbredt i mange vestlige lande. Imidlertid er kendskabet til politisk marketing i Danmark bemærkelsesværdigt lavt. I det lys er denne bog Politisk Marketing: Personer, Partier & Praksis den første bog i Danmark, som -ud fra marketing- indkredser de sidste mange års...... brudflader i dansk politik. Gennem ti bidrag fra forskere og praktikere udskraber forfatterne et DNA for feltet politisk marketing. Kort sagt kan du i denne bog finde svarene på: Hvad er politisk marketing? Hvordan har det udviklet sig? Og hvilke konsekvenser har dette fænomen for vælgere, partier og...

  18. A unique guild of Lepidoptera associated with the glacial relict populations of Labrador tea (Ledum palustre Linnaeus, 1753) in Central European peatlands (Insecta: Lepidoptera)

    Czech Academy of Sciences Publication Activity Database

    Spitzer, Karel; Jaroš, Josef

    2014-01-01

    Roč. 42, č. 166 (2014), s. 319-327 ISSN 0300-5267 Institutional support: RVO:60077344 Keywords : Insecta * Lepidoptera * relict peat bogs Subject RIV: EH - Ecology, Behaviour Impact factor: 0.435, year: 2014

  19. NACP Peatland Landcover Type and Wildfire Burn Severity Maps, Alberta, Canada

    Data.gov (United States)

    National Aeronautics and Space Administration — This data set provides landcover maps of (1) peatland type (bog, fen, marsh, swamp) with levels of biomass (open, forested) and (2) Burn Severity Index (BSI)...

  20. Socialt arbejde gennem 40 år 1970 - 2010

    DEFF Research Database (Denmark)

    Bog indeholdende artikler skrevet af Therese Halskov 1984-2008, samt artikler skrevet af personer, der har samarbejdet med Therese i socialt arbejdes praksis, undervisning omkring socialt arbejde og/eller forskning i perioden 1970-2010...

  1. Испытанные временем / Тийна Кольк

    Index Scriptorium Estoniae

    Кольк, Тийна

    2011-01-01

    Ajaproovile vastupannud klassikalise disainiga toodetest: viini tool, Alvar Aalto taburet ja vaas "Savoy", Arne Jacobseni tugitool "Muna" jt. Kaidi Ploomipuu kavandatud Euroopa disainiauhinna Red Dot pälvinud vaip «Bog 4053»

  2. På Spring

    DEFF Research Database (Denmark)

    Bjørn, Michael Würtz

    Beskrivelse: Undervisningsmateriale til redskabsaktiviteter og grundlæggende springgymnastik med hensyntagen til børns forskellige aktivitetsniveau. Materialet består af en bog med tilhørende CD rom...

  3. O sallingmo'l

    DEFF Research Database (Denmark)

    Hansen, Inger Schoonderbeek

    2005-01-01

    Anmeldelsen har til formål kort at beskrive Jens Ejsings nyeste bog, som beskriver sallingmålets grammatik meget detaljeret. Anmeldelsen er informativ snarere end kritisk. Udgivelsesdato: december...

  4. Role of Acidophilic Methanotrophs in Long Term Natural Attenuation of cVOCs in Low pH Aquifers

    Science.gov (United States)

    2017-06-15

    Methylocystis bryophila sp. nov., a facultatively methanotrophic bacterium from acidic Sphagnum peat, and emended description of the genus Methylocystis (ex...dinitrogen- fixing acidophilic bacterium from Sphagnum bog. Int. J. Syst. Evol. Microbiol. 52:251–261. Dedysh S.N., Knief C., Dunfield P.F. 2005...Tiedje J.M. 1998a. Acidophilic methanotrophic communities from Sphagnum peat bogs. Appl. Environ. Microbiol. 64:922–929. Dedysh S.N., Panikov N.S

  5. Ikke ligefrem noget lysthus

    DEFF Research Database (Denmark)

    Birkholm, Klavs

    2016-01-01

    I sin bog om den amerikanske "neuropsykiater" Robert Heath (1915-99) demonstrerer videnskabsjournalisten Lone Frank nok engang sin forbundethed med den internationale transhumanisme og dens dualistiske forståelse af ånd og materie......I sin bog om den amerikanske "neuropsykiater" Robert Heath (1915-99) demonstrerer videnskabsjournalisten Lone Frank nok engang sin forbundethed med den internationale transhumanisme og dens dualistiske forståelse af ånd og materie...

  6. En alkymist fra Amerika

    DEFF Research Database (Denmark)

    Hansen, Nils Gunder

    2013-01-01

    Sean Wilentz skriver sig uden om storladne myter og smålig nyfigenhed i sin bog om Bob Dylan. Forfatteren har fantastisk godt fat i manden som kunstner og led i den amerikanske musiks kæde......Sean Wilentz skriver sig uden om storladne myter og smålig nyfigenhed i sin bog om Bob Dylan. Forfatteren har fantastisk godt fat i manden som kunstner og led i den amerikanske musiks kæde...

  7. Dynamic vertical profiles of peat porewater chemistry in a northern peatland

    Science.gov (United States)

    Natalie A. Griffiths; Stephen D. Sebestyen

    2016-01-01

    We measured pH, cations, nutrients, and total organic carbon (TOC) over 3 years to examine weekly to monthly variability in porewater chemistry depth profiles (0–3.0 m) in an ombrotrophic bog in Minnesota, USA. We also compared temporal variation at one location to spatial variation in depth profiles at 16 locations across the bog. Most solutes exhibited large...

  8. Social arv

    DEFF Research Database (Denmark)

    Jensen, Bente

    Arbejdspapir som er udarbejdet i forbindelse med HPA-projektet og brugt i en anden udgivelse fra 2007. Nu genudgivet med nyt forord og ISBN nummer, samt udgive via DPU's forlag som e-bog......Arbejdspapir som er udarbejdet i forbindelse med HPA-projektet og brugt i en anden udgivelse fra 2007. Nu genudgivet med nyt forord og ISBN nummer, samt udgive via DPU's forlag som e-bog...

  9. Compilation of 1986 Annual Reports of the Navy ELF (Extremely Low Frequency) Communications System Ecological Monitoring Program. Volume 3. TABS H-J.

    Science.gov (United States)

    1987-07-01

    chronicles the data collection and analysis activities for a monitoring project during 1986. As in the past, each report has been reviewed by four or...sediments thoroughly and re- taining the suspended animals in a 60 tm mesh soil sieve. Animals were preserved in 80% ethyl alcohol . The sediments were...Gaultheria procuinbens Hepatica Labrador Tea Hepat ia americana Ledum groenland icum Anemone Bog Laurel Anemone sp Kahnmia polifolia Blue Cohosh Bog

  10. Æstetik er tilbage som nøgle til at forstå samtiden

    DEFF Research Database (Denmark)

    Sharma, Devika

    2013-01-01

    Casper Christensen er gakket, Hello Kitty er nuttet og konceptkunsten er interessant. Her er tre nye kategorier at forstå senkapitalismen med. I anledning af Sianne Ngais bog "Our aesthetic categories: zany, cute, interesting" .......Casper Christensen er gakket, Hello Kitty er nuttet og konceptkunsten er interessant. Her er tre nye kategorier at forstå senkapitalismen med. I anledning af Sianne Ngais bog "Our aesthetic categories: zany, cute, interesting" ....

  11. Ikke overklasse, men særklasse

    DEFF Research Database (Denmark)

    Holt Larsen, Henrik

    2009-01-01

    Danske virksomheder har i stigende grad brug for videnarbejdere, men de ved for lidt om dem. En ny rapport og en ny bog sætter den fagprofessionelle specialist i fokus......Danske virksomheder har i stigende grad brug for videnarbejdere, men de ved for lidt om dem. En ny rapport og en ny bog sætter den fagprofessionelle specialist i fokus...

  12. Science og gode læringsmiljøer

    DEFF Research Database (Denmark)

    Broström, Stig; Frøkjær, Thorleif

    2018-01-01

    Science bliver ret sikkert en del af de nye, styrkede pædagogiske læreplaner. Her introducerer forfatterne begrebet, med eksempler, og med henvisninger til deres bog om samme emne......Science bliver ret sikkert en del af de nye, styrkede pædagogiske læreplaner. Her introducerer forfatterne begrebet, med eksempler, og med henvisninger til deres bog om samme emne...

  13. Ross - for altid?

    DEFF Research Database (Denmark)

    Blume, Peter Erik

    2011-01-01

    Med baggrund i Jens Ewalds bog om Alf Ross omtaler artiklen en række de problemstillinger, som bogen behandler, samt vurderer den betydning, Ross har haft og måske fortsat har. Afslutningsvis betones den juridiske biografis betydning.......Med baggrund i Jens Ewalds bog om Alf Ross omtaler artiklen en række de problemstillinger, som bogen behandler, samt vurderer den betydning, Ross har haft og måske fortsat har. Afslutningsvis betones den juridiske biografis betydning....

  14. UAV based 3D digital surface model to estimate paleolandscape in high mountainous environment

    Science.gov (United States)

    Mészáros, János; Árvai, Mátyás; Kohán, Balázs; Deák, Márton; Nagy, Balázs

    2016-04-01

    Our method to present current state of a peat bog was focused on the possible use of a UAV-system and later Structure-from-motion algorithms as processing technique. The peat bog site is located on the Vinderel Plateau, Farcǎu Massif, Maramures Mountains (Romania). The peat bog (1530 m a.s.l., N47°54'11", E24°26'37") lies below Rugasu ridge (c. 1820 m a.s.l.) and the locality serves as a conservation area for fallen down coniferous trees. Peat deposits were formed in a landslide concavity on the western slope of Farcǎu Massif. Nowadays the site is surrounded by a completely deforested landscape, and Farcǎu Massif lies above the depressed treeline. The peat bog has an extraordinary geomorphological situation, because a gully reached the bog and drained the water. In the recent past sedimentological and dendrochronological researches have been initiated. However, an accurate 3D digital surface model also needed for a complex paleoenvironmental research. Last autumn the bog and its surroundings were finally surveyed by a multirotor UAV developed in-house based on an open-source flight management unit and its firmware. During this survey a lightweight action camera (mainly to decrease payload weight) was used to take aerial photographs. While our quadcopter is capable to fly automatically on a predefined flight route, several over- and sidelapping flight lines were generated prior to the actual survey on the ground using a control software running on a notebook. Despite those precautions, limited number of batteries and severe weather affected our final flights, resulting a reduced surveyed area around peat bog. Later, during the processing we looked for a reliable tool which powerful enough to process more than 500 photos taken during flights. After testing several software Agisoft PhotoScan was used to create 3D point cloud and mesh about bog and its environment. Due to large number of photographs PhotoScan had to be configured for network processing to get

  15. Investigation and Modeling of Cranberry Weather Stress.

    Science.gov (United States)

    Croft, Paul Joseph

    Cranberry bog weather conditions and weather-related stress were investigated for development of crop yield prediction models and models to predict daily weather conditions in the bog. Field investigations and data gathering were completed at the Rutgers University Blueberry/Cranberry Research Center experimental bogs in Chatsworth, New Jersey. Study indicated that although cranberries generally exhibit little or no stomatal response to changing atmospheric conditions, the evaluation of weather-related stress could be accomplished via use of micrometeorological data. Definition of weather -related stress was made by establishing critical thresholds of the frequencies of occurrence, and magnitudes of, temperature and precipitation in the bog based on values determined by a review of the literature and a grower questionnaire. Stress frequencies were correlated with cranberry yield to develop predictive models based on the previous season's yield, prior season data, prior and current season data, current season data; and prior and current season data through July 31 of the current season. The predictive ability of the prior season models was best and could be used in crop planning and production. Further examination of bog micrometeorological data permitted the isolation of those weather conditions conducive to cranberry scald and allowed for the institution of a pilot scald advisory program during the 1991 season. The micrometeorological data from the bog was also used to develop models to predict daily canopy temperature and precipitation, based on upper air data, for grower use. Models were developed for each month for maximum and minimum temperatures and for precipitation and generally performed well. The modeling of bog weather conditions is an important first step toward daily prediction of cranberry weather-related stress.

  16. Soil microbial community composition is correlated to soil carbon processing along a boreal wetland formation gradient

    Science.gov (United States)

    Chapman, Eric; Cadillo-Quiroz, Hinsby; Childers, Daniel L.; Turetsky, Merritt R.; Waldrop, Mark P.

    2017-01-01

    Climate change is modifying global biogeochemical cycles. Microbial communities play an integral role in soil biogeochemical cycles; knowledge about microbial composition helps provide a mechanistic understanding of these ecosystem-level phenomena. Next generation sequencing approaches were used to investigate changes in microbial functional groups during ecosystem development, in response to climate change, in northern boreal wetlands. A gradient of wetlands that developed following permafrost degradation was used to characterize changes in the soil microbial communities that mediate C cycling: a bog representing an “undisturbed” system with intact permafrost, and a younger bog and an older bog that formed following the disturbance of permafrost thaw. Reference 16S rRNA databases and several diversity indices were used to assess structural differences among these communities, to assess relationships between soil microbial community composition and various environmental variables including redox potential and pH. Rates of potential CO2 and CH4 gas production were quantified to correlate sequence data with gas flux. The abundance of organic C degraders was highest in the youngest bog, suggesting higher rates of microbial processes, including potential CH4 production. In addition, alpha diversity was also highest in the youngest bog, which seemed to be related to a more neutral pH and a lower redox potential. These results could potentially be driven by increased niche differentiation in anaerobic soils. These results suggest that ecosystem structure, which was largely driven by changes in edaphic and plant community characteristics between the “undisturbed” permafrost bog and the two bogs formed following permafrost thaw, strongly influenced microbial function.

  17. Impact of long-term drainage on summer groundwater flow patterns in the Mer Bleue peatland, Ontario, Canada

    Directory of Open Access Journals (Sweden)

    B. J. Kopp

    2013-09-01

    Full Text Available Long-term impacts of drier conditions on the hydrology of northern peatlands are poorly understood. We used long-term drainage near a historic drainage ditch, separating an area from the main peatland, as an analogue for long-term drying in a northern temperate bog. The objective was to identify the impact of drier conditions on ecohydrological processes and groundwater flow patterns in an area now forested and an area that maintained a bog-like character. Groundwater flow patterns alternated between mostly downward flow and occasionally upward flow in the bog area and were mostly upward-orientated in the forested area, which suggested that there the flow pattern had shifted from bog- to fen-like conditions. Flow patterns were in agreement with changes in post-drainage hydraulic conductivities, storage capacity of the peat and water table levels. Compared to the bog, hydraulic conductivities in the forested area were one to three orders of magnitude lower in the uppermost 0.75 m of peat (paired t test, p < 0.05. Bulk density had increased and the water table level was lower and more strongly fluctuating in the forested area. Our findings suggest hydraulic gradients and flow patterns have changed due to increased evapotranspiration and interception with the emergence of a tree cover. The smaller size of the now-forested area relative to the remaining bog area appeared to be important for the hydrological change. With the main Mer Bleue bog as hinterland, enhanced runoff to the drainage channel had little effect on hydrologic and vegetation patterns. In the cut-off, smaller, now forested area pervasive changes in vegetation and hydrologic processes occurred. The difference in response to local drainage raises questions about tipping points with respect to the impact of drying on peatland ecosystems that need to be addressed in future research.

  18. Active methanotrophs in two contrasting North American peatland ecosystems revealed using DNA-SIP.

    Science.gov (United States)

    Gupta, Varun; Smemo, Kurt A; Yavitt, Joseph B; Basiliko, Nathan

    2012-02-01

    The active methanotroph community was investigated in two contrasting North American peatlands, a nutrient-rich sedge fen and nutrient-poor Sphagnum bog using in vitro incubations and (13)C-DNA stable-isotope probing (SIP) to measure methane (CH(4)) oxidation rates and label active microbes followed by fingerprinting and sequencing of bacterial and archaeal 16S rDNA and methane monooxygenase (pmoA and mmoX) genes. Rates of CH(4) oxidation were slightly, but significantly, faster in the bog and methanotrophs belonged to the class Alphaproteobacteria and were similar to other methanotrophs of the genera Methylocystis, Methylosinus, and Methylocapsa or Methylocella detected in, or isolated from, European bogs. The fen had a greater phylogenetic diversity of organisms that had assimilated (13)C, including methanotrophs from both the Alpha- and Gammaproteobacteria classes and other potentially non-methanotrophic organisms that were similar to bacteria detected in a UK and Finnish fen. Based on similarities between bacteria in our sites and those in Europe, including Russia, we conclude that site physicochemical characteristics rather than biogeography controlled the phylogenetic diversity of active methanotrophs and that differences in phylogenetic diversity between the bog and fen did not relate to measured CH(4) oxidation rates. A single crenarchaeon in the bog site appeared to be assimilating (13)C in 16S rDNA; however, its phylogenetic similarity to other CO(2)-utilizing archaea probably indicates that this organism is not directly involved in CH(4) oxidation in peat.

  19. Past processes in peats : untangling the origin of dried peat in the Australian alps

    International Nuclear Information System (INIS)

    Grover, S.P.P.; Tisdall, J.M.; Jacobsen, G.

    2005-01-01

    Peat soils form where decomposition is hindered, often by a combination of cold and wet conditions, such that production of organic matter outweighs decomposition. Such conditions are rare in the hot, dry continent of Australia. Consequently peat barely features on a map of Australian soils, though small areas are noted to occur in the alps and along the humid east coast. It is pertinent to ask several questions about the origin of peat in the alps. Is dried peat a remnant of bog peat? And if so, when did bogs drain to form dried peat? The study site, on Wellington Plains in the south-east Gippsland Alps, contains a substantial area of bog peat and extensive areas of dried peat. AMS radiocarbon dating of surface, base and, for the bog peat only, mid-profile peat samples, was carried out at ANSTO. 14 C dating enabled us to look at the initiation of peat accumulation, but the change from bog peat to dried peat is thought to have occurred more recently, since the introduction of stock to the alps. The short half-life of 210 Pb (22.6 years) and the constant supply from the upper atmosphere makes 210 Pb an appropriate technique to investigate this time frame. 5 refs., 1 fig., 2 tabs

  20. Preliminary paleoecological reconstruction of long-term relationship between human and environment in the northern part of Danube-along Plain, Hungary

    Science.gov (United States)

    Kustár, Rozália; Molnár, Dávid; Sümegi, Pál; Törőcsik, Tünde; Sávai, Szilvia

    2016-06-01

    The peat bog at Ócsa is located at the northern part of the Danube-Tisa Interfluves at the transitional zone of two landscapes with different morphological characters. At the boundary of the Danube-Tisa Interfluves and the Danube-along Plain a marshland sequence can be found from Hajós to Ócsa. We extended our research to the Ócsa peat bog to complete the environmental historical investigations in the examined area, as well. The bog is located in a former pool formed by the Danube River in which aeolian sand and thick lake sediment deposited from the Late Pleistocene. The initial oligotrophic lake became mesotrophic, therefore thick carbonate sediment deposited. Afterwards, as a consequence of the Neolithic human occupations, the natural development of the lake changed drastically and the lake choked up. The pollen and quartermalacological analysis of the area support the mentioned geological processes.

  1. Estimating exposure of piscivorous birds and sport fish to mercury in California lakes using prey fish monitoring: a predictive tool for managers

    Science.gov (United States)

    Ackerman, Joshua T.; Hartman, C. Alex; Eagles-Smith, Collin A.; Herzog, Mark P.; Davison, Jay; Ichikawa, Gary; Bonnema, Autumn

    2015-01-01

    Numerous water bodies in California are listed under the Clean Water Act as being impaired due to mercury (Hg) contamination. The Surface Water Ambient Monitoring Program (SWAMP), via the Bioaccumulation Oversight Group (BOG), has recently completed statewide surveys of contaminants in sport fish tissue from more than 250 lakes and rivers in California and throughout coastal waters. This effort focused on human health issues but did not include beneficial uses by wildlife. Many piscivorous birds such as grebes, terns, cormorants, and mergansers eat fish smaller than those that were sampled by BOG, and sport fish Hg concentrations are not always indicative of wildlife exposure to Hg; therefore, the BOG surveys could not address whether wildlife were at risk due to Hg-induced reproductive impairment in these lakes.

  2. Cranberry flowering times and climate change in southern Massachusetts

    Science.gov (United States)

    Ellwood, Elizabeth R.; Playfair, Susan R.; Polgar, Caroline A.; Primack, Richard B.

    2014-09-01

    Plants in wild and agricultural settings are being affected by the warmer temperatures associated with climate change. Here we examine the degree to which the iconic New England cranberry, Vaccinium macrocarpon, is exhibiting signs of altered flowering phenology. Using contemporary records from commercial cranberry bogs in southeastern Massachusetts in the United States, we found that cranberry plants are responsive to temperature. Flowering is approximately 2 days earlier for each 1 °C increase in May temperature. We also investigated the relationship between cranberry flowering and flight dates of the bog copper, Lycaena epixanthe—a butterfly dependent upon cranberry plants in its larval stage. Cranberry flowering and bog copper emergence were found to be changing disproportionately over time, suggesting a potential ecological mismatch. The pattern of advanced cranberry flowering over time coupled with increased temperature has implications not only for the relationship between cranberry plants and their insect associates but also for agricultural crops in general and for the commercial cranberry industry.

  3. Efecto de la disciplina deportiva sobre valores hematológicos en hombres deportistas

    Directory of Open Access Journals (Sweden)

    Daniel Arias Mutis

    2007-08-01

    Full Text Available Se establecieron los volúmenes sanguíneos y la masa de Hb (método de retoma de CO y el consumo de oxígeno máximo (VO2max en 15 individuos sedentarios de Bogotá (UT-Bog, 17 deportistas de diferentes disciplinas residentes en Bogotá (TR-Bog, divididos por deporte (marcha, cinco; patinaje, siete; triatlón, cinco y cuatro deportistas provenientes de Sao Paulo (Brasil, que permanecieron ocho semanas en Bogotá, Colombia y a los que se les efectuaron dos medidas, a las dos (Brasil 1 y a las siete (Brasil 2 semana. Hubo diferencia significativa en el VO2max entre TR-Bog (65,4 +/- 7,9, Brasil 1 y 2 (56,2 +/- 1,7, y 55,8 +/- 2,8, p

  4. Mycorrhizal colonisation of highbush blueberry and its native relatives in central Finland

    Directory of Open Access Journals (Sweden)

    A. KASURINEN

    2008-12-01

    Full Text Available Transmission electromicroscopy, trypan blue staining in combination with stereomicroscope analysis and biochemical ergosterol assay were used to study the mycorrhizal symbionts in wild bilberry (Vaccinium myrtillus, bog whortleberry (Vaccinium uliginosum and highbush blueberry (Vaccinium corymbosum roots. TEM-analysis showed that in all species ericoid mycorrhizas formed hyphae coil inside the epidermal root cells. In stereomicroscopic viewing the highest mycorrhizal colonisation was observed in the roots of wild bilberries (51%, whereas according to the ergosterol assay the highest total fungal biomass of roots was found in bog whortleberries (209 mg g-1 of root d. wt. Both ergosterol and microscopical method showed that the mycorrhizal associations in blueberry cultivars and their wild relatives growing on natural soil medium are frequent, although ericoid mycorrhiza formation of highbush blueberries was somewhat weaker than that of wild bilberries and bog whortleberries.

  5. Wood anatomy of Argyroxiphium (Asteraceae): adaptive radiation and ecological correlations

    International Nuclear Information System (INIS)

    Carlquist, S.

    1997-01-01

    Wood anatomy shows close correlation with ecology: A. kauense, A. sandwicense (stem), and A. virescens, which occur in dry localities, show xeromorphic wood patterns. The most mesomorphic woods are those of the bog species A. grayanum and root wood of A. sandwicense. The wood of A. caliginis is xeromorphic, despite the bog habitat of the species, a fact explainable if A. caliginis is a recent entrant into the bog habitat Libriform wall thickness appears correlated with habit. Quantitative features of stem woods of Argyroxiphium are comparable to woods ranging from desert to moist montane forest areas in California. The similarities to woods from each Californian habitat are correlative to the relative moisture availability of the respective Hawaiian habitats of the Argyroxiphium species. (author)

  6. THE ROLE OF THE LANDSLIDE LAKES (WETLANDS IN TRANSFORMATION OF PHYSICOCHEMICAL WATER ON THE EXAMPLE VELKE OSTURNIANSKE JAZERO, SLOVAKIA

    Directory of Open Access Journals (Sweden)

    Tadeusz Molenda

    2015-03-01

    Full Text Available In the article a role of the flow bog in the transformation of the physical-chemical properties of waters was described. They demonstrated that in the water flowing out of the bog a fall in the mineralization and concentrations of selected ions take place towards feedwaters. The species stated within the bog of plants, mainly Carex rostrata, Schoenoplectus lacustris, Equisetum fluviatile, Juncus effusus, Menyanthes trifoliata can be found the under construction application of sewage treatment plant on highlands of the Western Carpathians (to 900 m.n.p.m., the average annual air temperature > of 5 °C and the time of lying of the snowy lid of 90 days in the year.

  7. Holocen history of vegetation at “Uroczysko Mokradła” (SW Poland – paleobotanical research

    Directory of Open Access Journals (Sweden)

    Klara Tomaszewska

    2016-09-01

    Full Text Available Two peat bogs were studied in the Bory Dolnośląskie, the forest complex in Lower Silesia (Poland. An Instorf drill was used to collect two peat profiles from the deepest places. The macroremains analysis showed that after the initiation of peat-forming processes phytocoenoses responsible for the deposition of transition sphagnum peat were developed at both locations. Later on, the development of both peat bogs differed. The smaller peat bog continued to develop, whereas the big bog was shifted to ombrotrophic water regime. Therefore, phytocoenoses accumulated 1.3 m of Sphagnum peat. The peat-forming process was initiated at different times in both sites. For the smaller peat bog, it took place during the Atlantic period, while in the case of the larger peat bog – several thousand years later. The first identified forest phytocoenoses in the Atlantic period are mesophilic multi-species deciduous forests. Dry coniferous forests and mixed birch-pine forests grew in dry habitats. Riparian forests occupied lower grounds. In the Subboreal period, the oak–hazel communities initially developed and mixed coniferous forests were partially replaced by light oak forests. The encroachment of spruce, fir, hornbeam, and beech resulted in the development of dry ground forests, including beech–fir woods. The importance of riparian forests increased, whereas in dry grounds pine and mixed coniferous forests continued to occur. In the Subatlantic period, the transformations in forest communities were associated with the spread of hornbeam, beech, and fir and thereby vast fertile habitats were colonized by dry ground communities and beech woods. Pine and mixed forests as well as riparian forests were of lesser importance. Pollen records from the last 500 years showed the clear presence of humans. It was evident from the presence of cereal and weed pollen and from the disturbances in the pollen records caused by peat extraction in the Middle Ages.

  8. In vitro decomposition of Sphagnum by some microfungi resembles white rot of wood.

    Science.gov (United States)

    Rice, Adrianne V; Tsuneda, Akihiko; Currah, Randolph S

    2006-06-01

    The abilities of some ascomycetes (Myxotrichaceae) from a Sphagnum bog in Alberta to degrade cellulose, phenolics, and Sphagnum tissue were compared with those of two basidiomycetes. Most Myxotrichaceae degraded cellulose and tannic acid, and removed cell-wall components simultaneously from Sphagnum tissues, whereas the basidiomycetes degraded cellulose and insoluble phenolics, and preferentially removed the polyphenolic matrix from Sphagnum cell walls. Mass losses from Sphagnum varied from up to 50% for some ascomycetes to a maximum of 35% for the basidiomycetes. The decomposition of Sphagnum by the Myxotrichaceae was analogous to the white rot of wood and indicates that these fungi have the potential to cause significant mineralization of carbon in bogs.

  9. Iodine and microbial interactions in an organic soil

    International Nuclear Information System (INIS)

    Sheppard, M.I.; Hawkins, J.L.

    1995-01-01

    Iodine-129 in groundwater discharging from a geological disposal vault could accumulate in wetlands by chemical sorption onto low pH, highly organic solid surfaces or by direct or indirect microbial processes. Previous work indicated that saturation of anion sorption sites, microbial toxicity, or swamping of the I reduction/oxidation reaction decreased the retention of a wetland sphagnum for iodine with increased iodine porewater concentrations. Bog water and peat of an iodine-rich bog were studied to elucidate the role of micro-organisms in the retention and accumulation of iodine in a temperate wetland. (author)

  10. Om at oversætte Mead

    DEFF Research Database (Denmark)

    Willert, Søren

    2005-01-01

    George Herbert Mead har skrevet en rigtig dårlig bog, der dog også er en klassiker. "sindet, selvet og samfundet" er den blevet til i en udgivelsesklar dansk udgave- og oversættelsen er en historie i seig selv.......George Herbert Mead har skrevet en rigtig dårlig bog, der dog også er en klassiker. "sindet, selvet og samfundet" er den blevet til i en udgivelsesklar dansk udgave- og oversættelsen er en historie i seig selv....

  11. Biological peculiarities of the cranberry (Oxycoccus palustris Pers.) and ecological parameters of its environment: influence on accumulation of 137Cs by phytomass

    International Nuclear Information System (INIS)

    Orlov, A.A.; Krasnov, V.P.

    1998-01-01

    Investigation of radioecology of the cranberry in Polessye of Ukraine (N.W. of Zhitomir region) were carried out. 137 Cs specific activity in shoots and berries of cranberry, sphagnous layers and bog water was analysed. Distribution of 137 Cs specific activity in different vertical parts of sphagnous layers was rather similar. It was shown that the cranberry is an intensive accumulator of 137 Cs. During the analysed period (1991-96) decrease in specific activity of cranberry was observed. Close connection between 137 Cs specific activity and the level of exposure dose on the bog habitat was found. (authors)

  12. Duplik til Nils Hybels tredje eventyr

    DEFF Research Database (Denmark)

    Bøgh, Anders

    2005-01-01

    Andet indlæg i en debat med og om lektor, dr.phil. Nils Hybel i anledning af hans bog: Danmark og Europa 750-1300, 2003. Indlægget handler mest om kildernes status i den historiske forskningsproces.......Andet indlæg i en debat med og om lektor, dr.phil. Nils Hybel i anledning af hans bog: Danmark og Europa 750-1300, 2003. Indlægget handler mest om kildernes status i den historiske forskningsproces....

  13. Diagenesis of sulphur in a peat forming environment: a case study from Sri Lanka

    Energy Technology Data Exchange (ETDEWEB)

    Senaratne, A.; Tobschall, H.J.; Dissanayake, C.B. (Universitaet Mainz, Mainz (Germany, F.R.). Inst. fuer Geowissenschaften)

    1990-03-01

    The sulphur geochemistry of the Muthurajawela peat deposit in Sri Lanka was studied. Due to the reducing conditions prevailing within the peat bog, sulphur was mainly in the sulphide form and almost all of the iron in the peat was in the form of iron sulphide. By releasing organically bound sulphur, the organic matter contributed significantly to the content of sulphur required for pyrite formation. It was found that the pyrite distribution in the peat bog did not depend on the depth of the organic matter, but on the state of decomposition. 20 refs., 7 figs., 1 tab.

  14. Land-use history affects understorey plant species distributions in a large temperate-forest complex, Denmark

    DEFF Research Database (Denmark)

    Svenning, J.-C.; Baktoft, Karen H.; Balslev, Henrik

    2009-01-01

    spatial, and 5 historical variables, and principal components analysis (PCA), redundancy analysis (RDA) as well as indicator species analysis. The historical variables were status as ancient (1805 AD) high forest, reclaimed bogs, ≤100 m from Bronze Age burial mounds, or former conifer plantation...... dispersal and a strong literature record as ancient-forest species, were still concentrated in areas that were high forest in 1805. Among the younger forests, there were clear floristic differences between those on reclaimed bogs and those not. Apparently remnant populations of wet-soil plants were still...

  15. Contributions of palynology in the reconstruction of livestock impact on the surroundings of Rascafria (Madrid) during the recent Holocene; Aportaciones de la palinologia en la reconstruccion del impacto ganadero, en los alrededores de Rascafria (Madrid), durante el Holoceno reciente

    Energy Technology Data Exchange (ETDEWEB)

    Gomez-Gonzalez, C.; Ruiz Zapata, M. B.; Lopez-Saez, J. A.; Gil Garcia, M. J.

    2009-07-01

    We present the results obtained from the palaeocological studies about human impact on the vegetal landscape of a peat bog located in Resurface (Lozoya Valley, Madrid, Central Spain). Palynomorph analysis allows to identify the kind and intensity of human activity and its relation to the trophic changes in the peat bog during the late Holocene (2455{+-}35 BP). Pollen record reveals an anthropic Mediterranean landscape mainly composed by pastures used for grazing. Non Pollen Palynomorphs (NPP) and pH and conductivity sediment have revealed as useful tools for detection of trophic conditions and land use changes. (Author)

  16. Litteraturens huse

    DEFF Research Database (Denmark)

    2013-01-01

    Valg af materiale/medie/form: iBog Valg af arbejdsform: interaktive opgaver, foto, interaktive tidslinjer, tekster, opgaver, quizer, videoklip, kunstbilleder, skriveøvelser mv. Begrundelse for valg af materiale/medie/form/arbejdsform: iBøger dækker 80% af omsætningen i Systime......Valg af materiale/medie/form: iBog Valg af arbejdsform: interaktive opgaver, foto, interaktive tidslinjer, tekster, opgaver, quizer, videoklip, kunstbilleder, skriveøvelser mv. Begrundelse for valg af materiale/medie/form/arbejdsform: iBøger dækker 80% af omsætningen i Systime...

  17. Arkitektur og plan i den danske velfærdsby 1950-1990

    DEFF Research Database (Denmark)

    Pedersen, Poul Bæk

    2005-01-01

    Den danske arkitektur- og planhistorie fra 1950 til 1990 'genskrives' i denne bog ud fra et sammenhængende arkitektur- og byperspektiv. Afsættet er en typologisk forståelse af den danske by, der rummer både den historiske by og de nyere bydele.......Den danske arkitektur- og planhistorie fra 1950 til 1990 'genskrives' i denne bog ud fra et sammenhængende arkitektur- og byperspektiv. Afsættet er en typologisk forståelse af den danske by, der rummer både den historiske by og de nyere bydele....

  18. The cultural evolution of religion

    DEFF Research Database (Denmark)

    Bulbulia, Joseph; Geertz, Armin W.; Atkinson, Quentin D.

    2013-01-01

    I dette bidrag til en bog om kulturel evolution beskriver forfatterne religionens kulturel evolution. Kapitlet forsøger ved anvendelsen af en bred vifte af metoder og data at forklare kompleksiteten og variationen i religion inden for og på tværs of grupper gennem historien.......I dette bidrag til en bog om kulturel evolution beskriver forfatterne religionens kulturel evolution. Kapitlet forsøger ved anvendelsen af en bred vifte af metoder og data at forklare kompleksiteten og variationen i religion inden for og på tværs of grupper gennem historien....

  19. Historisierung der Energiefrage

    DEFF Research Database (Denmark)

    Czeskleba-Dupont, Rolf

    2014-01-01

    Anmeldelse af prof.em.Bent Sørensens bog, der præsenterer energiregnskaber fra Neanderthalerne til vor tid inden for det geografiske område, som Danmark dækker/har dækket. Bidrag til et kommende fag energi-historie.......Anmeldelse af prof.em.Bent Sørensens bog, der præsenterer energiregnskaber fra Neanderthalerne til vor tid inden for det geografiske område, som Danmark dækker/har dækket. Bidrag til et kommende fag energi-historie....

  20. Contributions of palynology in the reconstruction of livestock impact on the surroundings of Rascafria (Madrid) during the recent Holocene

    International Nuclear Information System (INIS)

    Gomez-Gonzalez, C.; Ruiz Zapata, M. B.; Lopez-Saez, J. A.; Gil Garcia, M. J.

    2009-01-01

    We present the results obtained from the palaeocological studies about human impact on the vegetal landscape of a peat bog located in Resurface (Lozoya Valley, Madrid, Central Spain). Palynomorph analysis allows to identify the kind and intensity of human activity and its relation to the trophic changes in the peat bog during the late Holocene (2455±35 BP). Pollen record reveals an anthropic Mediterranean landscape mainly composed by pastures used for grazing. Non Pollen Palynomorphs (NPP) and pH and conductivity sediment have revealed as useful tools for detection of trophic conditions and land use changes. (Author)

  1. Do big gods cause anything?

    DEFF Research Database (Denmark)

    Geertz, Armin W.

    2014-01-01

    Dette er et bidrag til et review symposium vedrørende Ara Norenzayans bog Big Gods: How Religion Transformed Cooperation and Conflict (Princeton University Press 2013). Bogen er spændende men problematisk i forhold til kausalitet, ateisme og stereotyper om jægere-samlere.......Dette er et bidrag til et review symposium vedrørende Ara Norenzayans bog Big Gods: How Religion Transformed Cooperation and Conflict (Princeton University Press 2013). Bogen er spændende men problematisk i forhold til kausalitet, ateisme og stereotyper om jægere-samlere....

  2. Darwin på arabisk

    DEFF Research Database (Denmark)

    Riexinger, Martin Thomas

    2014-01-01

    Det var to revolutionære spor, som i begyndelsen af 1800-talet gødede jorden for introduktionen af Darwins evolutionsteori i Mellemøsten, og muslimer spillede stort set ingen rolle for den udviklingen. Ny bog om islam og evolutionsteorien.......Det var to revolutionære spor, som i begyndelsen af 1800-talet gødede jorden for introduktionen af Darwins evolutionsteori i Mellemøsten, og muslimer spillede stort set ingen rolle for den udviklingen. Ny bog om islam og evolutionsteorien....

  3. Visuel kommunikation på digitale medier

    DEFF Research Database (Denmark)

    Thorlacius, Lisbeth

    Visuel kommunikation på digitale medier er en teoretisk forankret bog, som med afsæt i nye begrebsudviklinger og aktuel forskning inden for feltet præsenterer de væsentligste visuelle virkemidler, som indgår på de digitale medieplatforme. Derudover gennemgås de mest udbredte genrer og aktuelle st...

  4. Engineering Education in the Rapidly Changing World : Rethinking the Vision for Higher engineering Education

    NARCIS (Netherlands)

    Kamp, A.

    2016-01-01

    When drafting the first issue of this document it sometimes felt like I was manoeuvring a small canoe through a highly viscous fluid of conservatism and complacency, with everybody bogged down by today’s thinking, preparing next Tuesday’s nine o’clock lecture, aiming for the best learning experience

  5. The diversity of microfungi in peatlands originated from the White Sea

    NARCIS (Netherlands)

    Grum-Grzhimaylo, Olga A.; Debets, Fons; Bilanenko, Elena N.

    2016-01-01

    The diversity of culturable filamentous microfungi in peat and sediments of four peatlands at the coastal zone of Kandalaksha Bay of the White Sea (Murmansk region, Russia) was studied by culture methods on standard and selective media. Annually 100 samples were collected from the bogs 2007-2010.

  6. Conservation assessment for the autumn willow in the Black Hills National Forest, South Dakota and Wyoming

    Science.gov (United States)

    J. Hope Hornbeck; Carolyn Hull Sieg; Deanna J. Reyher

    2003-01-01

    Autumn willow, Salix serissima (Bailey) Fern., is an obligate wetland shrub that occurs in fens and bogs in the northeastern United States and eastern Canada. Disjunct populations of autumn willow occur in the Black Hills of South Dakota. Only two populations occur on Black Hills National Forest lands: a large population at McIntosh Fen and a small...

  7. 76 FR 77162 - Floodplain Management and Protection of Wetlands

    Science.gov (United States)

    2011-12-12

    ... CONTACT: Charles Bien, Acting Director Office of Environment and Energy, Office of Community Planning and... swamps, marshes, bogs, and similar areas such as sloughs, potholes, wet meadows, river overflows, mud... compensatory mitigation in a state or watershed, a lack of funds within the project, or other reasons that make...

  8. MATLAB syntaksen

    DEFF Research Database (Denmark)

    Skajaa, Anders; Jørgensen, Jakob Heide

    MATLAB er et matematik-program som fokuserer på anvendelsen af matricer og vektorer. Deraf navnet MATrix LABoratory. Denne bog er en praktisk vejledning i at forstår og anvende MATLAB syntaksen og fungerer som en hurtig genvej til dig, der skal i gang med at anvende MATLAB i forbindelse med fx dit...

  9. Ecology and distribution of Myriosclerotinia caricis-ampullaceae (Sclerotiniaceae, Ascomycota) in Central Europe with remarks on its world distribution

    Czech Academy of Sciences Publication Activity Database

    Holec, J.; Kučera, Tomáš; Balner, V.

    2007-01-01

    Roč. 59, č. 1 (2007), s. 57-74 ISSN 0082-0598 Institutional research plan: CEZ:AV0Z60870520 Keywords : mycogeography * raised-bogs * mountain vegetation Subject RIV: EH - Ecology, Behaviour Impact factor: 0.556, year: 2007

  10. Monitoring revitalizačních zásahů na rašeliništi Žofinka, CHKO Třeboňsko

    Czech Academy of Sciences Publication Activity Database

    Rektoris, Ladislav; Kolmanová, Andrea; Jakšičová, T.

    -, - (2003), s. 117-132 ISSN 1211-3603 R&D Projects: GA MŽP SE/610/10/00; GA ČR GA206/98/0727 Institutional research plan: CEZ:AV0Z6005908 Keywords : postfire succession * pine bog forests * soil water chemistry Subject RIV: EF - Botanics

  11. Can seasonal variation in fen water chemistry influence the reliability of vegetation-environment analyses?

    Czech Academy of Sciences Publication Activity Database

    Hájek, Michal; Hekera, P.

    2004-01-01

    Roč. 76, - (2004), s. 1-14 ISSN 0032-7786 R&D Projects: GA AV ČR KSK6005114 Institutional research plan: CEZ:AV0Z6005908 Keywords : anion and cation concentration * bog * central Europe Subject RIV: EF - Botanics

  12. Variation in the C/N-quotient of peat in relation to decomposition rate and age determination with 210Pb

    International Nuclear Information System (INIS)

    Malmer, N.; Holm, E.

    1984-01-01

    Peat profiles ca. 0.5 m in depth through bog hummocks with Sphagnum spp. have been studied on a subarctic mire in northern Sweden and on some bogs in southern Sweden. The C/N-quotient in the peat decreases with depth due to losses in C during the decay processes. As a result of decay and compaction, the annual peat volume increment at the bottom of the profiles is 4-15% of the increment in the upper parts. On the central bog areas in southern Sweden the decay processes during periods are interrupted at earlier stages which gives rise to a more rapid volumetric peat increment than in the marginal bog areas and in the north. Datings from 210 Pb activity have proved to be reliable only in the lower parts of the profiles (age>50 yr) as lead might be mobile in the upper parts. At the deposition in the catotelm layer after a period of at least 150 yr the organic matter has lost up to 80% of its original carbon. The accumulation of 210 Pb and N shows that the supply of these elements is higher in southern Sweden than in the north. (author)

  13. Microtropography and water table fluctuation in a sphagnum mire

    Science.gov (United States)

    E.S. Verry

    1984-01-01

    A detailed organic soil profile description, 22 years of continuous water table records, and a hummock-hollow level survey were examined at a small Minnesota mire (a bog with remnants of poor fen vegetation). Variation in the level survey suggests that hollows be used to minimize variation when detailed topographic information is needed and to match profile...

  14. Teologie en ekologie

    African Journals Online (AJOL)

    5 Jan 1986 ... areas oorgeneem deur 'sphagnum moss, a plant w^hich traps so much water in its large leaf cells that moss effectively drowns competition'. Hierdie wurg-mos ontbind stadig en vorm moerasturf 'insulating the bog surface from underlying soil nutrients'. Die gevolg is groot stukke grond 'too wet to farm and ...

  15. Kvantemekanik

    DEFF Research Database (Denmark)

    Mølmer, Klaus

    enorm succes, men fortolkningen af den splittede samtidig tidens største videnskabsmænd, særligt Niels Bohr og Albert Einstein. Denne bog gennemgår kvantemekanikkens og fysikkens udvikling i det 20. århundrede - og giver indblik i de nyeste opdagelser af, hvordan den atomare verden fungerer...

  16. The future of innovation serves humanity before economy

    DEFF Research Database (Denmark)

    Darsø, Lotte

    2009-01-01

    En bog med over 200 globale bidragsydere om fremtiden for innovation. Vægten i Lotte Darsøs bidrag er på den menneskelige faktor som det væsentligste omdrejningspunkt for innovation samt på menneskelige værdier, læring og ledelse som vejen til innovation. www.thefutureofinnovation.org  ...

  17. A Mechanical Image: Heinrich Hertz's Principles of Mechanics

    DEFF Research Database (Denmark)

    Lützen, Jesper

    2006-01-01

    Heinrich Hertz's bog Die Prinzipien der Mechanik in neuem Zusammenhange dargestellt var nyskabende inden for både fysik, matematik og filosofi. I fysik lagde den det første fundament til en fysik, som undgår kraftbegrebet som et basalt begreb; i matematik præsenterede den en ny geometrisering af ...

  18. Final Environmental Assessment to Implement the Defense Base Closure and Realignment Commission Recommendations for Shaw Air Force Base, South Carolina

    Science.gov (United States)

    2007-07-01

    calyculata Leatherleaf ─ SC wetlands and bogs Cyperus lecontei Leconte’s flatsedge ─ SC sand dune swales; pond margins Echinodorus parvulus Dwarf burhead...pod CIRF to support the workload. Many BRAC actions are tied together. Not performing these actions would have a ripple effect across several other

  19. Human Resources Coordinator | IDRC - International Development ...

    International Development Research Centre (IDRC) Digital Library (Canada)

    Job Summary Under the direction of the Director of Human Resources, the Administrative Assistant provides operational and administrative assistance to her ... BoG, SMC; lead the management of paper and electronic records for the Division; provide directions for the proper preparation of goods and services contracts and ...

  20. Boganmeldelse - Music Therapy Research

    DEFF Research Database (Denmark)

    Ridder, Hanne Mette Ochsner

    2006-01-01

    . Alligevel følger her en anbefaling af bogen: for musikterapeuter er det en bog, man ikke kommer uden om. Music Therapy Research, på dansk Musikterapiforskning, er en gennemrevideret, ja faktisk nyudgivelse, af bogen Music Therapy Research: Quantitative and Qualitative Perspectives, som udkom i 1995. Også...

  1. Preliminary Guide to the Onsite Identification and Delineation of the Wetlands of Alaska.

    Science.gov (United States)

    1984-02-01

    fenestratus (Western dock) Valeriana capitata (Capitate valerian) b. Riparian marsh subtype. Prevalent speciep include: Arctophila fulva (Pendent grass...Polar willow) * Valeriana capitata (Capitate valerian) * b. Riparian marsh subtype. Prevalent species include: Carex aquatilis (Water sedge) A...34 "° . Jon S 0o Sphagnum spp. (Sphagnum moss) and other mosses Vaccinium uliginosum (Bog blueberry) Vaccinium vitis-idaea (Mountain cranberry) Valeriana

  2. Innovation systems as patent networks : The Netherlands, India and nanotech

    NARCIS (Netherlands)

    Dolfsma, Wilfred; Leydesdorff, Loet

    2011-01-01

    Research in the domain of 'Innovation Studies' has been claimed to allow for the study of how technology will develop in the future. Some suggest that the National and Sectoral Innovation Systems literature has become bogged down, however, into case studies of how specific institutions affect

  3. Synopsis for klinikassistenter

    DEFF Research Database (Denmark)

    Danielsen, Bo

    2009-01-01

    Textbook for dental nurses. 426 p.ills., ISBN: 9781405175579.  Denne bog giver en gennemgang af det stof, som det er nødvendigt at besidde for, at man kan bestå den britiske eksamen til klinikassistent (Dental Nurse). Bogen dækker derfor mange emner, der omtales meget kort og meget summarisk - ofte...

  4. Searching for branched glycerol dialkyl glycerol tetraether membrane lipid producing bacteria in soil

    NARCIS (Netherlands)

    Aydin, R.

    2012-01-01

    KEYWORDS:Branched GDGTs, proxy, pH, temperature, Acidobacteria, methylotrophy, high-throughput techniques

    Bacteria present in soil and peat bog environments were previously found to produce branched glycerol dialkyl glycerol

  5. Indledning

    DEFF Research Database (Denmark)

    Jacobsen, Claus Haugaard; Thorgaard, Lars

    2006-01-01

    Tilknytning, tab og tilblivelse har en central betydning i menneskelivet, i udviklingspsykologi, i den kliniske psykologi og i den psykoanalytiske psykoterapi. Denne bog omhandler tilknytning, tab og tilblivelse i forhold til psykoterapi med børn, voksne med personlighedsforstyrrelser eller skizo...

  6. Passionate Utterance and Moral Education

    Science.gov (United States)

    Munday, Ian

    2009-01-01

    This paper explores Stanley Cavell's notion of "passionate utterance", which acts as an extension of/departure from (we might read it as both) J. L. Austin's theory of the performative. Cavell argues that Austin having made the revolutionary discovery that truth claims in language are bound up with how words perform, then gets bogged by convention…

  7. Die Geschichte von Tom Buk-Swienty

    DEFF Research Database (Denmark)

    Rønhede, Søren

    2010-01-01

    Buk-Swienty markedsfører sin seneste bog på en påstand om at have afsløret, at kongen, Christian IX, i 1864 gennem sin anmodning om optagelse i Det tyske Forbund søgte at nedlægge Danmark. Påstanden er uden hold i de historiske realiteter....

  8. Selecting parameters for the environmental interpretation of peat molecular chemistry - A pyrolysis-GC-MS study

    NARCIS (Netherlands)

    Schellekens, J.F.P.; Buurman, P.; Pontevedra Pombal, X.

    2009-01-01

    A number of samples from a deep peat bog in Tierra del Fuego were analyzed using pyrolysis-gas chromatography/mass spectrometry (Py-GC/MS) in order to extract parameters that might be used to interpret the peat chemistry in terms of vegetation change, anaerobic and aerobic decomposition, and fire

  9. Towards a universal description of cohesive-particle flows

    Science.gov (United States)

    Lamarche, Casey; Liu, Peiyuan; Kellogg, Kevin; Lattanzi, Aaron; Hrenya, Christine

    2017-11-01

    A universal framework for describing cohesive granular flows seems unattainable based on prior works, making a fundamental continuum theory to predict such flows appear unachievable. For the first time, universal behavior of cohesive-grain flows is demonstrated by linking the macroscopic (many-grain) behavior to grain-grain interactions via two dimensionless groups: a generalized Bond number BoG - ratio of maximum cohesive force to the force driving flow - and a new Agglomerate number Ag - ratio of critical cohesive energy to the granular energy. Cohesive-grain flow is investigated in several systems, and universal behavior is determined via collapse of a cohesion-dependent output variable from each system with the appropriate dimensionless group. Universal behavior is observed using BoG for dense (enduring-contact-dominated) flows and Ag for dilute (collision-dominated) flows, as BoG accounts for the cohesive contact force and Ag for increased collisional dissipation due to cohesion. Hence, a new physical picture is presented, namely, BoG dominates in dense flows, where force chains drive momentum transfer, and Ag dominates in dilute systems, where the dissipative collisions dominate momentum transfer. Apparent discrepancies with past treatments are resolved. Dow Corning Corporation.

  10. Matematik i ottende

    DEFF Research Database (Denmark)

    Hansen, Niels Jacob; Beck, Hans Jørgen; Graff, Lona

    Matematik i ottende, Kopimappe indeholder 109 kopiark samt 11 siders håndbog til regneark. De 87 kopiark er en integreret del af Matematik i ottende. Grundbogen indeholder henvisninger til Kopiarkene. Desuden indeholder Kopimappen 22 siders kopiark til færdighedsregning. Matematik i ottende omfat...... omfatter flg. komponenter: Grundbog, Kopimappe samt Lærerens Bog. Herudover er computerprogrammet SuperFunk udgivet....

  11. Mathematics as Liberal Education: Whitehead and the Rhythm of Life

    Science.gov (United States)

    Woodhouse, Howard

    2012-01-01

    In several of his works, Alfred North Whitehead (1861-1947) presents mathematics as a way of learning about general ideas that increase our understanding of the universe. The danger is that students get bogged down in its technical operations. He argues that mathematics should be an integral part of a new kind of liberal education, incorporating…

  12. Tekster til organisationsanalyse

    DEFF Research Database (Denmark)

    Bogen samler klassiske og nyere tekster om organisationer. Forfattere som Weber, Taylor, March, Schein, Mintzberg og Weick indgår mange steder som fast pensum på organisationsfag, og her er de samlet i een bog. Tilsammen tilbyder teksterne afsæt for analyser af en lang række aspekter af organisat...

  13. Thin book

    DEFF Research Database (Denmark)

    En lille bog om teater og organisationer, med bidrag fra 19 teoretikere og praktikere, der deltog i en "Thin Book Summit" i Danmark i 2005. Bogen bidrager med en state-of-the-art antologi om forskellige former for samarbejde imellem teater og organisationer. Bogen fokuserer både på muligheder og...

  14. Dyp tæerne i skriftsproget!

    DEFF Research Database (Denmark)

    Korsgaard, Klara Aalbæk

    2012-01-01

    I denne bog argumenterer forskere og erfarne praktikere for, hvorfor det lille barn bør inviteres til at udforske og kommunikere via skriftsproget. Der bliver også lagt vægt på, hvordan skrivning kan indgå i børnehaven på en legende og støttende måde....

  15. Ejeraftaler

    DEFF Research Database (Denmark)

    Kruhl, Martin Christian

    Denne bog er den første samlede og dybdegående afhandling om ejeraftaler på dansk. Ejeraftaler (tidligere 'aktionær- eller anpartsoverenskomster') spiller i praksis en væsentlig rolle som det aftalemæssige grundlag for de indbyrdes rettigheder og forpligtelser mellem kapitalejere i små og mellems...

  16. Algae of the Bohemian Forest. 1. Specieses richness

    Czech Academy of Sciences Publication Activity Database

    Lederer, F.; Lukavský, Jaromír

    2001-01-01

    Roč. 6, - (2001), s. 97-104 ISSN 1211-7420 R&D Projects: GA AV ČR IA60504; GA ČR GA206/99/1411 Institutional research plan: CEZ:AV0Z6005908 Keywords : Bohemian Forest * species richness * biodiversity * algae * cyanobacteria * lakes * brooks * rivers * bogs Subject RIV: EH - Ecology, Behaviour

  17. "A Scrapbook of You + Me"

    DEFF Research Database (Denmark)

    Tanderup, Sara

    2017-01-01

    Artiklen læser det eksperimentende bog-værk S. (2013), af Doug Dorst og J.J. Abrams, som en refleksion over, og et udtryk for den trykte romans forandrede status i en digital tidsalder. Som en eksperimenterende roman med gulnede sider og håndskrift i marginen synes S. at reflektere en materiel ve...

  18. Velkommen til gældens hus

    DEFF Research Database (Denmark)

    Lunde, Jens

    2015-01-01

    De amerikanske professorer, Atif Mian og Amir Sufi, udgav i år den udmærkede og noget oversete bog »House of Debt«, der vender fortællingen om finanskrisen på hovedet. Anmeldelse af: Atif Mian og Amir Sufi: "House of Debt. How They (and You) Caused the Great Recession, and How We Can Prevent...

  19. "Hvem er som jeg blandt Guder?"

    DEFF Research Database (Denmark)

    Holst, Søren

    2004-01-01

    En hymne fra Dødehavsrullerne beskriver en persons opstigning til himlen, hvor den pågældende får tildelt overmenneskelig indsigt, som giver ham autoritet til at belære sine tilhængere på jorden. Hymnen analyseres, og der foretages en kritisk gennemgang af Israel Knohls bog "The Messiah Before Je...

  20. En dronning kom til byen

    DEFF Research Database (Denmark)

    Storm, Rasmus K.

    2009-01-01

    Det er ganske rigtig et af dansk håndbolds mest dramatiske kapitler Dan Philipsen beskriver i sin bog om Anja Andersens eventyr i Slagelse: 'En dronning kom til byen'. Bogen er velskrevet, og er i sin form en velsignet god gang underholdning til natbordet. Problemet er bare, at man kan have svært...

  1. Important physical properties of peat materials

    Science.gov (United States)

    D.H. Boelter

    1968-01-01

    Peat materials from 12 bogs in northern Minnesota, U.S.A., showed significant differences in physical properties. It is pointed out that 1) these properties can be related to the hydrology of organic soils only if the soils represent undisturbed field conditions, and 2) volumetric expressions of water content are necessary to correctly evaluate the amount of water in a...

  2. How to DO Projects? A Nordic Flavour to Managing Projects

    DEFF Research Database (Denmark)

    Geraldi, Joana; Thuesen, Christian; Oehmen, Josef

    Hvis du mangler inspiration til alternative måder at lede projekter på, så hjælper denne bog dig med at udvikle din egen "opskrift" på projektledelse. Bogen viser dig, hvordan du bruger de velkendte projektledelsesteorier i praksis, og hvordan du i samarbejde med andre kan skabe meningsfulde form...

  3. Ambient UV-B radiation decreases photosynthesis in high arctic Vaccinium uliginosum

    DEFF Research Database (Denmark)

    Albert, Kristian Rost; Mikkelsen, Teis Nørgaard; Ro-Poulsen, H.

    2008-01-01

    An UV-B-exclusion experiment was established in high arctic Zackenberg, Northeast Greenland, to investigate the possible effects of ambient UV-B on plant performance. During almost a whole growing season, canopy gas exchange and Chl fluorescence were measured on Vaccinium uliginosum (bog blueberry...

  4. Acidic precipitation and forest vegetation

    Science.gov (United States)

    Carl Olof Tamm; Ellis B. Cowling

    1976-01-01

    Most plants can take up nutrients from the atmosphere as well as from the soil solution. This capacity is especially important in natural ecosystems such as forests and bogs where nutrients from other sources are scarce and where fertilization is not a normal management procedure. Trees develop very large canopies of leaves and branches that extend high into the air....

  5. Lake acidification in the Adirondack Mountains of New York causes and consequences

    Science.gov (United States)

    Carl L. Schofield

    1976-01-01

    Current and historic geographic distributions of acidity in Adirondack lakes were examined in relation to regional edaphic, climatic, and physiographic features. Acid conditions are currently predominant in high elevation drainage lakes having small watershed/surface area ratios. Comparable levels of acidity were found only in small seepage lakes and bog ponds during...

  6. Short Review

    DEFF Research Database (Denmark)

    Lynnerup, Niels; Rühli, Frank

    2015-01-01

    X-raying is arguably the most well-known, non-invasive technique for visualising the internal structures of ancient mummies and bog bodies. There are several factors such as the easy availability, the relative cheapness as well as the high spatial resolution, which speaks for this diagnostic moda...

  7. Sociale medier i gymnasiet

    DEFF Research Database (Denmark)

    Tække, Jesper; Paulsen, Michael

    Denne bog rapporterer om første år af Socio Media Education eksperimentet, der tematiserede den konkrete udfordring det er at etablere en god it-kultur i en gymnasieklasse. Baseret på resultaterne undersøger bogen, både hvordan man kan skabe en god it-kultur i en klasse, og hvordan man kan forbed...

  8. Use of lignocellulosic materials as sorbents for pesticide and phosphate residues

    Science.gov (United States)

    Mandla A. Tshabalala

    2006-01-01

    We previously reported results from limited field trials of a bark-based filtration unit designed to remove phosphorus from cranberry bog tail water. In that report we also identified some barriers that needed to be overcome to improve the performance of such a filtration unit. One barrier was lack of a cost effective process for large-scale conversion of bark to an...

  9. Dansk selskabsret 3

    DEFF Research Database (Denmark)

    Friis Hansen, Søren; Krenchel, Jens Valdemar

    Dansk selskabsret er et værk i 3 bind, der giver et samlet overblik over de forskellige selskabsformer, den erhvervsdrivende kan vælge som juridisk ramme for sin virksomhed. Denne tredje bog i serien gennemgår interessentskabet, der omfatter en række forskellige former for erhvervsdrivende virkso...

  10. Elementær Teori for Plane Bjælker

    DEFF Research Database (Denmark)

    Byskov, Esben

    Denne bog er skrevet med henblik på introduktion og benyttelse af de mest basale teorier for strenger og bjælker, hvor hovedvægten er lagt på retliniede, plane bjælker. Bogens indhold dækker mere end et enkelt semesters pensum ved bygningsingeniøruddannelsen ved Aalborg Universitet. Ideen er, at ...

  11. Computer Cache. Wildlife on the Web: Connections to Animals, Biomes, Environments, and Habitats

    Science.gov (United States)

    Byerly, Greg; Brodie, Carolyn S.

    2004-01-01

    Follow the migration of monarch butterflies, explore Yellowstone National Park, find out about endangered species in the Everglades, or learn about the wildlife dependent upon a bog for existence. This article describes how students can learn these things and many more through the numerous resources available on the World Wide Web that feature…

  12. Berlins Alexanderplatz mellem opbrud og erindring

    DEFF Research Database (Denmark)

    Post, Hans Christian

    Denne bog undersøger den byarkitektoniske idékonkurrence i 1993 for Berlins Alexanderplatz. I hidtidige arkitekturfaglige og videnskabelige artikler og værker er konkurrencen blevet udlagt som en bestræbelse på at annullere DDR-tiden og vende tilbage til den byrumlige situation, der herskede i fø...

  13. Byg og hold bøtte!

    DEFF Research Database (Denmark)

    Munch, Anders V.

    2009-01-01

    Anmeldelse af en bog, der gennemgår forskellige receptioner af Ludwig Mies van der Rohes arkitektur ud fra forskellige filosofiske og kulturkritiske vinkler. Bogen har som særlig dagsorden af genoverveje den kritiske teoris status på feltet mellem arkitektur og kulturkritik og følger de rene...

  14. Do big gods cause anything?

    DEFF Research Database (Denmark)

    Geertz, Armin W.

    2014-01-01

    Dette er et bidrag til et review symposium vedrørende Ara Norenzayans bog Big Gods: How Religion Transformed Cooperation and Conflict (Princeton University Press 2013). Bogen er spændende men problematisk i forhold til kausalitet, ateisme og stereotyper om jægere-samlere....

  15. Mediejura for journalister og andre mediearbejdere

    DEFF Research Database (Denmark)

    Sandfeld Jakobsen, Søren; Schaumburg-Müller, Sten

    denne frihed hører også et ansvar, og medierettens omdrejningspunkt, som derfor også er denne bogs omdrejningspunkt, er at afdække den helt centrale balance mellem frihed og ansvar. En balancegang, der ikke er blevet nemmere i det digitale informationssamfund med mange nye medier og medieplatforme og...

  16. Geomorphology and landscape organization of a northern peatland complex

    Science.gov (United States)

    Richardson, M. C.

    2012-12-01

    The geomorphic evolution of northern peatlands is governed by complex ecohydrological feedback mechanisms and associated hydro-climatic drivers. For example, prevailing models of bog development (i.e. Ingram's groundwater mounding hypothesis and variants) attempt to explicitly link bog dome characteristics to the regional climate based on analytical and numerical models of lateral groundwater flow and the first-order control of water table position on rates of peat accumulation. In this talk I will present new results from quantitative geomorphic analyses of a northern peatland complex at the De Beers Victor diamond mine site in the Hudson Bay Lowlands of northern Ontario. This work capitalizes on spatially-extensive, high-resolution topographic (LiDAR) data to rigorously test analytical and numerical models of bog dome development in this landscape. The analysis and discussion are then expanded beyond individual bog formations to more broadly consider ecohydrological drivers of landscape organization, with implications for understanding and modeling catchment-scale runoff response. Results show that in this landscape, drainage patterns exhibit relatively well-organized characteristics consistent with observed runoff responses in six gauged research catchments. Interpreted together, the results of these geomorphic and hydrologic analyses help refine our understanding of water balance partitioning among different landcover types within northern peatland complexes. These findings can be used to help guide the development of appropriate numerical model structures for hydrologic prediction in ungauged peatland basins of northern Canada.

  17. Mit barn er anbragt

    DEFF Research Database (Denmark)

    Nissen Møller, Sanne; Skytte Aalborg Universitet, Marianne

    Anbringelse af etniske minoritetsbørn og -unge udgør en voksende opgave for kommunerne. I denne bog belyses gennem 11 personlige livshistorier de særlige problemer og dilemmaer, som etniske minoritetsforældre står i, når deres barn anbringes. Livshistorierne giver et indblik i, hvordan forældrene...

  18. Kampen om erhvervslivet

    DEFF Research Database (Denmark)

    Johannsen, Carl Gustav

    2010-01-01

    På grundlag af Carl Gustav Johannsens bog "Firmabiblioteker i Danmark 1945-2007" beskriver artiklen, hvordan danske firmabibliotekers historie peger på et lavt konfliktniveau i forhold til forskningsbibliotekerne. Til gengæld rivaliserede forskningsbibliotekerne med folkebibliotekerne i slut-80'e...

  19. Social praksisteoretiske analyser af unge i partnerskaber

    DEFF Research Database (Denmark)

    Mørck, Line Lerche; Munkholm, Merete

    Denne bog analyserer lokale partnerskaber mellem produktionsskoler og virksomheder, institutioner og civilsamfund. Bogen illustrerer, hvordan vi med social praksis teori kan forstå partnerskaber som grænsefællesskaber, hvor partnerskaber arrangeres i og på tværs af forskellige fællesskaber og han...

  20. Litteraturens hus, livets værksted

    DEFF Research Database (Denmark)

    Munk, Kasper Green

    2016-01-01

    W.G. Sebalds ’Campo Santo’ er et vildt katalog over litteraturens pligt til at bringe lys og lindring i mørke tider. Forfatterens ukuelige tro på skrivekunstens nytte står tilsyneladende kun i modsætning til hans pessimistiske historiefilosofi . Nu udkommer Sebalds posthume bog også på dansk...

  1. Elevated atmospheric CO2 and increased nitrogen deposition : effects on C and N metabolism and growth of the peat moss Sphagnum recurvum P. Beauv. var. mucronatum (Russ.) Warnst

    NARCIS (Netherlands)

    van der Heijden, E; Verbeek, S.K.; Kuiper, P.J C

    Sphagnum bogs play an important role when considering the impacts of global change on global carbon and nitrogen cycles. Sphagnum recurvum P. Beauv. var. mucronatum (Russ.) was grown at 360 (ambient) and 700 mu L L-1 (elevated) atmospheric [CO2] in combination with different nitrogen deposition

  2. Normalitet og afvigelse

    DEFF Research Database (Denmark)

    Holst, Jesper

    2009-01-01

    Anmeldelse ad Ivar Morkens bog:" Normalitet og afvigelse", der tager udgangspunkt i kontrasten mellem visionerne om inklusion, empowerment og anerkendelse og de faktiske forhold, hvor menneskelig afvig stadig diagnosticeres. Kontrasterne defineres og forsøges imødegået med forskellige former for ...

  3. Preservation status and priorities for in situ monitoring of the weapon sacrifice in Illerup Ådal, Denmark

    DEFF Research Database (Denmark)

    Tjelldén, A.K.E.; Kristiansen, S.M.; Botfeldt, Knud Bo

    2012-01-01

    in the area. Results show that the remaining artefacts are generally well preserved in a waterlogged and anaerobic environment. However, in the north-eastern part of the bog, the groundwater table is too low even in a year when net precipitation and hydrological conditions were near normal. In the centre...

  4. Alpine wetlands in the West Carpathians: vegetation survey and vegetation - environment relationships

    Czech Academy of Sciences Publication Activity Database

    Sekulová, L.; Hájek, Michal; Hájková, Petra; Mikulášková, E.; Rozbrojová, Zuzana

    2011-01-01

    Roč. 83, č. 1 (2011), s. 1-24 ISSN 0032-7786 R&D Projects: GA ČR GAP505/10/0638 Institutional research plan: CEZ:AV0Z60050516 Keywords : bogs * environmantal gradiens * fens Subject RIV: EF - Botanics Impact factor: 2.521, year: 2011

  5. Virkelighed er noget vi leger frem, når vi leger med magten

    DEFF Research Database (Denmark)

    Holm, Claus

    2008-01-01

    I ny bog analyserer professor Niels Åkerstrøm Andersen fra CBS, hvordan organisationer forsøger at bruge den ellers uskyldige leg i magtens tjeneste. Men legen er ikke kun en loyal tjener, legen laver sine egne regler og risikerer at tage magten fra magthaverne, når de mægtiggør os gennem legen....

  6. Videnskabsteori i Samfundsvidenskaberne

    DEFF Research Database (Denmark)

    2013-01-01

    Inden for samfundsvidenskaberne findes der mange forskellige og ofte modstridende antagelser om, hvordan viden opbygges, hvad samfundet er, og hvad der indgår i samfundsvidenskabelig analyse. Denne bog sigter på at give en samlende og loyal fremstilling af de mest fremherskende videnskabsteoretiske...

  7. Review of: Ancient Scandinavia: An Archaeological History from the First Humans to the Vikings (Oxford University Press, Oxford, 2016) T. Douglas Price

    DEFF Research Database (Denmark)

    Løvschal, Mette

    2017-01-01

    , barrows and megaliths that still mark the present-day landscape and bear witness to an intriguing prehistory. One of the important factors involved in the discovery of these archaeological remains is the nature of Scandinavian landscapes, riddled as they are with wet marshes, bogs, rivers and flooded...

  8. God stil i professionsopgaver

    DEFF Research Database (Denmark)

    Petersen, Kit Stender; Christoffersen, Ditte Dalum

    "God stil i professionsopgaver" er en vejledende bog, der sikrer dig en god arbejdsproces og det bedst mulige resultat. Du får hjælp fra start til slut, og information om alt fra hvordan du stiller et videnskabelige spørgsmål til hvordan du laver en analyse og sikrer korrekt formalia. "God stil i...

  9. Når aktivitetsfælden klapper

    DEFF Research Database (Denmark)

    Klindt, Mads Peter; Pedersen, Villy Hovard; Baadsgaard, Kelvin

    Med afsæt i et stort skandinavisk strukturfondsprojekt som case undersøger denne bog, hvorfor udviklingsprojekter havner i aktivitetsfælden og bliver kortsigtede. Bogen peger på at strukturfondssystemets egne regler er med til at snapore, at projektaktører retter deres opmærksomhed mod budgetter ...

  10. Recent pollen spectra from the deciduous and coniferous-deciduous forests of Northeastern Minnesota: a study in pollen dispersal

    NARCIS (Netherlands)

    Janssen, C.R.

    1966-01-01

    Pollen samples were taken along nine transects across local vegetational belts bordering bogs or ponds in overall deciduous and coniferous-deciduous forest regions. Three types of pollen rain are distinguished: local, extralocal, and regional. Local pollen rain is derived from plants that grow at or

  11. Influence of lake water pH and alkalinity on the distribution of coreand intact polar branched glycerol dialkyl glycerol tetraethers (GDGTs) in lakes

    NARCIS (Netherlands)

    Schoon, P.L.; de Kluijver, A.; Middelburg, J.J.; Downing, J.A.; Sinninghe Damsté, J.S.; Schouten, S.

    2013-01-01

    Branched glycerol dialkyl glycerol tetraethers (GDGTs) are bacterial membrane lipids, ubiquitously present in soils and peat bogs, as well as in rivers, lakes and lake sediments. Their distribution in soil is controlled mainly by pH and mean annual air temperature, but the controls on their

  12. A Mega-fire event in Central Russia: fire weather, radiative, and optical properties of the atmosphere, and consequences for subboreal forest plants

    Science.gov (United States)

    Nataly Y. Chubarova; Nickolay G. Prilepsky; Alexei N. Rublev; Allen R. Riebau

    2009-01-01

    In 2002, a major drought and prolonged high temperatures occurred in central Russia that resulted in unprecedented wildland fires. These fires occurred under extreme fire danger conditions and were impossible for the Russian authorities to extinguish. It is perhaps somewhat unique that the fires were first burning peat bogs and later forests, causing very massive smoke...

  13. Ensenanza basada en el diálogo

    DEFF Research Database (Denmark)

    Bernhardt, Nana; Dysthe, Olga; Esbjørn, Line

    Hvad er dialogbaseret undervisning, og hvordan kan den udfolde sig på et kunstmuseum? I denne bog viser forfatterne, hvordan erfarne museumsundervisere møder børn og unge på syv museer og udfordrer dem til nysgerrigt og kreativt at udforske temaer, udveksle synspunkter og udvikle nye tanker og id...

  14. Shark Bite Meetings for Creative Program Planning

    Science.gov (United States)

    Pellien, Tamara; Yergeau, Steven

    2017-01-01

    The strength of Cooperative Extension lies in the breadth of knowledge and experience of its faculty and staff. Yet those working in Extension can get so bogged down by the weight of this knowledge and become so focused on details, ownership, and process that it can be hard to respond to emerging needs or work effectively as a group. "Shark…

  15. Anmeldelse: Whitney Davis A General Theory of Visual Culture

    DEFF Research Database (Denmark)

    Michelsen, Anders Ib

    2012-01-01

    Whitney Davis bog A General Theory of Visual Culture vil utvivlsomt blive opfattet som en provokation af mange deltagere i forskningsdebatterne om visuel kultur. At basere en »generel« teori om visuel kultur – dvs. en teori, som benytter sig af termer som »visualitet« – på et kerneargument de facto...

  16. MotionsFloorball

    DEFF Research Database (Denmark)

    Vorup, Jacob; Seidelin, Kåre

    Med denne "opskriftsbog" er I nu klar til at begynde med MotionsFloorball. Ingen vellykket middagsret tilbereder som bekendt sig selv - de vigtigste ingredienser til et succesfuldt forløb er vilje og handlingskraft. Tilsættes værktøjerne og vidensdelen fra denne bog, er der dog ikke langt fra tanke...

  17. The Extended Mind Thesis and Mechanistic Explanations

    DEFF Research Database (Denmark)

    Fazekas, Peter

    2013-01-01

    The Extended Mind Thesis (EMT) is traditionally formulated against the bedrock of functionalism, and ongoing debates are typically bogged down with questions concerning the exact relationship between EMT and different versions of functionalism. In this paper, I offer a novel ally for EMT: the new...

  18. Test af spørgeskema

    DEFF Research Database (Denmark)

    Hermansen, Jonathan

    2017-01-01

    Denne bog gennemgår alle surveyarbejdets faser og giver en praktisk indføring i •design af undersøgelsen og udvælgelse af stikprøver, •formulering af spørgeskemaer samt indsamling og kodning af data, •metoder til at analysere resultaterne....

  19. Det er systemet den er gal med

    DEFF Research Database (Denmark)

    Bryld, Claus

    2014-01-01

    Anmeldelse af Klaus Buster Jensen og Jakob Mathiassen: Kamppladser. Østarbejdere og social dumping i byggeriet. Informations forlag. En fremragende bog om social dumping evner at udfolde det store problem uden at gøre hverken østeuropæerne eller arbejdsgiverne til karikerede skurke...

  20. Notes on the ecology of Natal Highland Sourveld vleis | BH | African ...

    African Journals Online (AJOL)

    The term vlei can be applied to most natural, low-lying, wet or damp areas in South Africa which may correspond with such categories as swamp, reedswamp, marsh and fen, but excluding pans and bogs. Keywords: hydromorphic soils|vlei types|valleys|plains|grassland vegetation|successional stages ...