Sample records for ISOTOPOS DE OXIGENO (oxygen isotopes)
from WorldWideScience.org

Sample records 1 - 20 shown. Select sample records:



1

EL USO DE ISÓTOPOS ESTABLES EN BIOLOGÍA TROPICAL

Louis S., Santiago; Silvera, Katia; Andrade, José Luis; Dawson, Todd E
2005-09-01

Resumen en portugués O uso de isótopos estáveis em biologia tem aumentado nos últimos anos devido ao grande poder que têm essas técnicas para medir processos que antes eram difícil ou impossível de quantificar utilizando outros métodos. Apesar de que a maioria dos estudos com isótopos tem-se concentrado em zonas temperadas, em anos recentes tem aumentado os estudos realizados nos trópicos, o qual ha permitido entender em detalhe processos complexos. Esta revisão enfatiza aqueles es (mas) tudos que utilizam a composição isotópica de hidrogênio, carbono, nitrogênio e oxigênio para estudar processos biogeoquímicos em ambientes tropicais, tanto a escala molecular como regional. Ao detalhar os avanços recentes sobre estudos nos trópicos, se espera estimular mais estudos nesta área. Também, com base nos resultados assombrosos que se obtêm usando isótopos em biologia tropical, se tem a certeza de que os isótopos estáveis proporcionarão avanços exitantes no futuro. Resumen en español El uso de isótopos estables en biología ha aumentado en los últimos años debido al gran poder que tienen los isótopos para medir procesos que antes eran difícil o imposible de cuantificar utilizando otros métodos. A pesar de que la mayoría de los estudios con isótopos se han concentrado en zonas templadas, en años recientes han aumentado los estudios realizados en los trópicos, lo cual ha permitido entender en detalle procesos complejos. Esta revisión enfatiza (mas) aquellos estudios que utilizan la composición isotópica de hidrógeno, carbono, nitrógeno y oxígeno para estudiar procesos biogeoquímicos en ambientes tropicales, tanto a escala molecular como regional. Al detallar los avances recientes sobre estudios en los trópicos, se espera estimular más estudios en esta área. También, con base en los resultados asombrosos que se obtienen usando isótopos en biología tropical, se tiene certeza de que los isótopos estables proporcionarán avances exitantes en el futuro. Resumen en inglés The use of stable isotopes in biology has increased in recent years because of the power of these techniques to measure processes that are difficult or impossible to quantify using other methods. Although most isotopic research has been concentrated in temperate zones, there has been an increase in isotopic studies in the tropics in recent years that have led to the understanding of detailed processes in complex ecosystems. This review highlights studies that use isotopic (mas) composition of hydrogen, carbon, nitrogen, and oxygen to study biogeochemical processes in tropical environments from molecular up to regional scales. By describing the current state of knowledge in isotopic studies in the tropics, it is hoped to stimulate more research in this area. Based on the spectacular results obtained from the use of isotopes in tropical biology, there is confidence that isotopes will lead to exciting advances in the future.

Scientific Electronic Library Online (Spanish)

2

a18o and aD opal and kaolinite from la Colilla, Avila

Antona, J. F.; Fallick, A.E.; García-Sánchez, A.; García-Talegón, Jacinta
1993-01-01

Digital.CSIC (Spain)

3

Water source partitioning among trees growing on shallow karst soils in a seasonally dry tropical climate

Querejeta Mercader, José Ignacio; Estrada Medina, Héctor; Allen, Michael F.; Jiménez-Osornio, Juan J.
2007-05-01

Digital.CSIC (Spain)

4

Vigilància ambiental de metil tert-butil èter (mtbe), un additiu de la gasolina, en aigües i sòls

Barceló, Damià; Lacorte Bruguera, Silvia; Rosell Linares, Mònica
2006-01-01

Digital.CSIC (Spain)

5

Variations in 13C/12C and D/H enrichment factors of aerobic bacterial fuel oxygenate degradation

Rosell Linares, Mònica; Barceló, Damià; Rohwerder, Thore; Breuer, Uta; Gehre, Matthias; Richnow, Hans Hermann
2007-02-03

Digital.CSIC (Spain)

7

The palaeohydrological evolution of Lago Chungara´ (Andean Altiplano, northern Chile) during the Lateglacial and early Holocene using oxygen isotopes in diatom silica

Hernández, Armand; Bao, Roberto; Giralt, Santiago; Leng, Melanie J.; Barker, Philips A.; Sáez, Alberto; Pueyo Mur, Juan José; Moreno Caballud, Ana; Valero-Garcés, Blas L.; Sloane, Hilary J.
2008-05-01

Digital.CSIC (Spain)

8

The Taravilla Lake and Tufa Deposits (Central Iberian Range, Spain) as paleohydrological and paleoclimatic indicators

Valero-Garcés, Blas L.; Moreno Caballud, Ana; Navas Izquierdo, Ana; Mata, M. Pilar; Machín Gayarre, Javier; Delgado Huertas, Antonio; González-Sampériz, Penélope; Schwalb, Antje; Morellón, Mario; Edwards, Larry
2008-03-24

Digital.CSIC (Spain)

9

The Mantos Blancos copper deposit: an upper Jurassic breccia-style hydrothermal system in the Coastal Range of Northern Chile

Ramírez, L. E.; Palacios, C.; Townley, B.; Parada, Miguel Ángel; Sial, A. N.; Fernandez-Turiel, J. L.; Gimeno, D.; García-Vallés, M.; Lehmann, B.
2006-01-01

Digital.CSIC (Spain)

11

Tectonically driven landscape development within the eastern Alpujarran Corridor, Betic Cordillera, SE Spain (Almería)

García, A. F.; Zhu, Z.; Ku, T. L.; Sanz de Galdeano, Carlos; Chadwicka, O. A.; Chacón Montero, J.
2003-02-01

Digital.CSIC (Spain)

12

Synthetic coal chars for the elucidation of NO heterogeneous reduction mechanisms

Pevida García, Covadonga; Arenillas de la Puente, Ana; Rubiera González, Fernando; Pis Martínez, José Juan
2007-01-01

Digital.CSIC (Spain)

13

Structure of neutron-rich oxygen isotopes

Cortina-Gil, D.; Fernández-Vázquez, J.; Aumann, T.; Baumann, T.; Benlliure, J.; García Borge, María José

4 pages, 1 table, 2 figures. | One-nucleon removal reactions at relativistic energies have been used as a spectroscopic tool for obtaining information about the ground state of neutron-rich oxygen isotopes. Using the FRS at GSI, the longitudinal momentum distributions of the emerging fragments after...

DRIVER (Spanish)

14

Structure of neutron-rich oxygen isotopes

Cortina-Gil, D.; Fernández-Vázquez, J.; Aumann, T.; Baumann, T.; Benlliure, J.; García Borge, María José; Chulkov, L. V.; Datta Pramanik, U.; Forssén, C.; Fraile, Luis M.; Geissel, H.; Gerl, J.; Hammache, F.; Itahashi, K.; Janik, R.; Jonson, B.; Mandal, S.; Markenroth, K.; Meister, M.; Mocko, M.; Muenzenberg, G.; Ohtsubo, T.; Ozawa, A.; Prezado, Yolanda; Riisager, K.; Scheit, H.; Schneider, R.; Schrieder, G.; Simon, H.; Sitar, B.; Stolz, A.; Strmen, P.; Suemmerer, K.; Szarka, I.; Weick, H.
2005-09-12

Digital.CSIC (Spain)

15

Structural characterization of kerogen in 3.4 Ga Archaean cherts from the Pilbara Craton, Western Australia

Marshall, Craig P.; Love, Gordon D.; Snape, Colin E.; Hill, Andrew C.; Allwood, Abigail C.; Walter, Malcolm R.; Van Kranendonk, Martin J.; Bowden, Stephen A.; Sylva, Sean P.; Summons, Roger E.
2007-05-05

Digital.CSIC (Spain)

18

Pliocene–Holocene evolution of depositional conditions in the eastern Mediterranean: Role of anoxia vs. productivity at time of sapropel deposition

Gallego-Torres, David; Martínez-Ruiz, Francisca; Paytan, Adina; Jimenez Espejo, Francisco J.; Ortega-Huertas, M.
2007-04-06

Digital.CSIC (Spain)

19

Petrográfica y Geoquímica de la dolomía hospedante de una mineralización de Zn y Pb. Puesto Gregor, Neuquén, Argentina/ Petrography and geochemistry of a Zn- Pb mineralization hosted in a dolostone, Puesto Gregor, Neuquen, Argentina

Gómez, M. Cristina; Garrido, Mirta; Cesaretti, Nora; Domínguez, Eduardo
2008-07-01

Resumen en español En la Cuenca Neuquina (Argentina) y asociada a la Formación Lajas (Jurásico) se mencionó por primera vez una mineralización de esfalerita y galena asociada a carbonatos. En el área del yacimiento Puesto Gregor, ésta Formación está constituida por una secuencia clástico carbonática. Para caracterizar el ambiente de depositación de la dolomía hospedante de la mineralización de Zn y Pb se realizaron estudios petrográficos y geoquímicos. Entre los últimos los (mas) más utilizados son los análisis e interpretación de isótopos estables (O, C), elementos mayoritarios y trazas e inclusiones fluidas. En el horizonte dolomítico de 0,90 m de espesor y 300 m de corrida se distinguen petrográficamente dos tipos de dolomita: el primer tipo es penetrativo, sin preservación de la fábrica sedimentaria original y es anterior a la mineralización, el segundo tipo está vinculado a la precipitación de sulfuros y consiste en una dolomita de tipo silla de montar (saddle). El estudio de las inclusiones fluidas en la dolomita penetrativa indica la presencia de fluidos orgánicos y fluidos acuosos. Determinaciones microtermométricas sobre inclusiones fluidas acuosas revelaron temperaturas de 140º C. Geoquímicamente la capa presenta proporciones casi estequiométricas y promedios de CaCO3 y MgCO3 iguales al 52 y 48% molar, respectivamente. En cuanto a los elementos trazas, el Sr varió entre 79 y 159 ppm y el Na entre 74 y 225 ppm. Los contenidos de Mn y Fe son mucho más altos que los valores determinados para estos elementos en rocas carbonáticas. El contenido en ETR es bajo y los diagramas de ETR muestran una anomalía negativa de Ce y de Eu. Se determinaron valores de isótopos de C y O. Los valores de ä13 C (VPDB) entre -2,9 y -9 0/00 no son coherentes con los datos informados para calizas marinas de edad jurásica mientras que los valores de ä18O(VPDB) entre -2,6 y -4 0/00 coinciden con los valores informados para carbonatos de igual edad. Los datos de ä18O indican que la interacción entre el fluido y la roca de caja fue baja. Los valores del ä18O del fluido en equilibrio con la dolomía a temperaturas de 140ºC indican que este fluido corresponde a una salmuera de cuenca. Por otro lado, los isótopos de carbono indican un aporte de carbono procedente de la diagénesis de la materia orgánica causada por un aumento de temperatura vinculada al soterramiento de la cuenca. Los resultados petrográficos y geoquímicos son consistentes con la dolomitización de un carbonato de origen marino que sufrió soterramiento. Resumen en inglés In Neuquen Basin, Argentina, a Zn-Pb mineralization was first reported by Garrido et al. (2000). The ore occurs in a carbonatic level located in Puesto Gregor, 50 km SSE from the city of Zapala at 39°11'34'' S, 69° 59'18'' W (Fig. 1). The hosting bed, a dolostone, belongs to a carbonatic-siliciclastic sequence of Lajas Formation, which is part of the Cuyo Group, Jurassic age. In the mineralization of Pb-Zn deposits associated to dolostones, the fluids that were involved (mas) in the ore precipitation process were also related to the dolomitization of the carbonatic rock (Warren, 2000). In this contribution, field, petrographic and geochemical studies were carried out in order to determine the temperature and composition of the dolimitizing fluids. The obtained results were then compared to those obtained from Carbon and Oxygen isotopes (Garrido et al., 2001) to discuss the dolimitization process. The mineralized bed, 0.90 m thick, outcrops for about 300 m along the strike (W-E) and 60 m in the dip direction (Fig. 2). This bed pinches out toward the east and toward the west it is no longer visible, it is cover by scours. Petrographic studies determined that the host rock is a dolostone with a breccia texture that becomes more siliciclastic towards the east grading thus to a fine sandstone with carbonatic cement. The hypogenic mineralization, mainly sphalerite, low quantities of galena, pyrite and marcasite is found within the small fractures. Some ghosts of fossils are still visible, but pervasive dolomitization characterizes the horizon. Two distinct dolomites are recognized by crosscutting relationships: a fine to medium grained crystalline dolomite, and a coarse grained crystalline dolomite related to the mineralization. The fomer shows dark-orange and white crystals which occur as patches or partially filled vugs. These crystals are 120-400 mm in size and exhibit subhedral to anhedral shapes (Fig. 3). According to Sibley and Gregg (1987), the texture is no planar -a- unimodal to polimodal. The latter dolomite presents well developed crystals (> 5 mm); they are translucent with pink color and pearl shine and have crystal faces that look like a pavement and is referred as "saddle" dolomite according to Radke and Mathis (1980). This "saddle" dolomite is found into dissolution cavities or as clusters of crystals located on the wall fractures; it is always associated to the mineralization. Chemical analysis of major, traces and rare earth elements are homogeneous throughout the bed. Mean values are 15% MgO, 29,66% CaO and 40,43 % CO2, with high MnO and Fe2O3 contents. The molar percentages of CaCO3 and MgCO3 indicate near stoichiometric ratio (52% and 48%) with a light excess of Ca (Table 1, Fig. 4). The trace elements Sr, Na, Fe and Mn are used to constrain dolomite evolution. Sr values varies from 79 to 159 ppm and Na from 74 to 225 ppm; Mn and Fe contents are higher than the values determined for carbonatic rocks (Turekian and Wedepohl, 1961). ÓREE and LREE contents are low, and the diagram normalized to chondrite shows a negative anomaly of Eu and a great negative anomaly of Ce. The 13C (VPDB) and 18O (VPDB) values vary from -2,9 to -9(0)/00 and from -2,6 to -4 0/00 respectively (Table 2). The 13C are incoherent with the data recorded for Jurassic marine carbonates (near 0 0/00) while 18O values can be correlated with carbonates of the same age (Veizer et al., 1999). Petrography and chemical analysis allow characterizing the depositional environment of the Zn- Pb mineralized dolostone. The xenotopic texture of the dolomite with no planar crystals, gives evidence that the temperatures of deposition should have been higher than 50-60°C (Gregg and Sibley, 1984). On the other hand, the chemical composition, near ideal dolomites (stoichiometric ratio), indicates slow crystallization at high temperature (Morrow, 1982). Morover, the destructive fabric and the homogeneous composition suggest a high temperature dolomitization (Machel, 2004). Trace element values, mainly Na and Sr, agree with burial dolomites, as well as the fluid inclusions reported for these samples by Cesaretti et al. (2002). The negative Ce anomaly indicates that these rocks were formed in a marine environment. Two different processes of carbonate precipitation can produce negative Ce anomaly (Möller, 1989; Bau and Möller, 1992): deposition from seawater or from hydrothermal solutions equilibrated with highly oxydized sediments. The latter is discarded because of the presence of framboidal pyrite and organic matter, which, along with the Eu negative anomaly indicates that the dolimitization were generated under euxinic conditions. This dolostone is in contact with anoxic mudstones (Los Molles Formation, Cuyo Group). Petrographic and geochemical criteria reflect that the dolomitization were caused by normal or modified sea water in a burial environment at temperatures above 140ºC. In burial or altered dolostones, the oxygen isotopes reflect temperature of precipitation and isotope composition of the dolomitizing fluids. The oxygen isotope values of this dolomitized bed are compatible with the isotope composition of carbonates precipitated from sea water at 25°C. The narrow range in the obtained values indicates that there was no influence of meteoric water during this process (Allan and Mathews, 1982). The homogeneous values of 18O isotope suggest that the physic-chemical conditions remained constant during dolomitization, what is in agreement with the textural and geochemical homogeneity found in the study samples. The 18O isotope values of a fluid equilibrated with carbonate at 140°C indicate that the fluid belongs to a basinal fluid. The 13C isotopes reflect an organic origin for the carbon. This carbon came from the diagenesis of organic matter caused by an increase in temperature during the burial of the basin (Garrido et al., 2001; Cesaretti et al., 2002). In contrast with other MVT deposits of the world, in Puesto Gregor, the dolomitization was slow process acting at high temperatures, what has been confirmed by the homogeneity of the fabric and the narrow range in the isotope and trace elements composition. These conditions were reached during burial of the basin where the rocks interact with the basin fluids associated to the ore minerals.

Scientific Electronic Library Online (Spanish)

20

Palynological signal of the Younger Dryas in the tropical Venezuelan Andes

Rull, Valentí; Nathan, D. Stansell; Montoya, Encarnación; Bezada, Maximiliano; Abbott, Mark B.
2010-01-01

Digital.CSIC (Spain)

21
22

Paleoclimatic variations in foraminifer assemblages from the Alboran Sea (Western Mediterranean) during the last 150 ka in ODP Site 977

Pérez-Folgado, Marta; Sierro, Francisco Javier; Flores, José Abel; Grimalt, Joan O.; Zahn, Rainer
2004-09-29

Digital.CSIC (Spain)

24

Ocean surface water response to short-term climate changes revealed by coccolithophores from the Gulf of Cadiz (NE Atlantic) and Alboran Sea (W Mediterranean)

Colmenero-Hidalgo, Elena; Flores, José Abel; Sierro, Francisco Javier; Bárcena, M.ª Ángeles; Löwemark, Ludvig; Schönfeld, Joachim; Grimalt, Joan O.
2004-02-27

Digital.CSIC (Spain)

25

Multiproxy reconstruction of the palaeoclimate and palaeoenvironment of the Middle Miocene Somosaguas site (Madrid, Spain) using herbivore dental enamel

Domingo, Laura; Cuevas-González, Jaime; Grimes, Stephen T.; Hernández Fernández, Manuel; López-Martínez, Nieves

16 pages, 11 figures, 3 tables.-- Available online Nov 17, 2008.-- This work is a contribution from the research groups UCM-CAM 910161 on Geologic Record of Critical Periods: Palaeoclimatic and Palaeonvironmental Factors, and UCM-CAM 910607 on Evolution of Cenozoic Mammals and Continental Palaeoenvi...

DRIVER (Spanish)

26

Multiproxy reconstruction of the palaeoclimate and palaeoenvironment of the Middle Miocene Somosaguas site (Madrid, Spain) using herbivore dental enamel

Domingo, Laura; Cuevas-González, Jaime; Grimes, Stephen T.; Hernández Fernández, M.; Lopez-Martinez, N.
2009-02-01

Digital.CSIC (Spain)

27

Isotopic signatures of extinct low-temperature hydrothermal chimneys in the Jaroso Mars analog

Martínez-Frías, Jesús; Delgado-Huertas, Antonio; García-Moreno, Francisco; Reyes, Emilio; Lunar, Rosario

8 pages, 5 figures.-- ISI Article Identifier: 000244984600006.-- Available online Nov 15, 2006. | The present work presents a geochemical study, focused on the oxygen and carbon isotopic signatures of shallow-marine, carbonate extinct chimneys, from Jaroso Hydrothermal System (JHS). In each chimney ...

DRIVER (Spanish)

28

Isotopic signatures of extinct low-temperature hydrothermal chimneys in the Jaroso Mars analog

Martínez-Frías, Jesús; Delgado Huertas, Antonio; García-Moreno, Francisco; Reyes, Emilio; Lunar, Rosario; Rull, Fernando
2007-03-01

Digital.CSIC (Spain)

29

Formation of natural gypsum megacrystals in Naica, Mexico

García Ruiz, Juan Manuel; Villasuso, Roberto; Ayora, Carlos; Canals, Angels; Otalora, Fermín
2007-04-01

Digital.CSIC (Spain)

30
31

Estimación del agua corporal total por deuterio en diálisis peritoneal pediátrica/ Estimation of total body water using deuterium in children undergoing peritoneal dialysis

Azócar P, Marta; Cano Sch, Francisco; Marín B, Verónica; Díaz B, Erik; Salazar R, Gabriela; Vásquez F, Loreta
2003-09-01

Resumen en español Introducción:La diálisis peritoneal (DP) en pediatría es actualmente el tratamiento más utilizado para el reemplazo de la función renal en niños portadores de insuficiencia renal crónica. El ajuste de la dosis de diálisis (Kt/V) debe ser periódico, lo cual requiere estimar el agua corporal total (ACT), lo que se puede realizar por distintas fórmulas. El método ideal de la medición del ACT se basa en el uso de isótopos marcados, H2[18O] o D2O (mas) (deuterio), no aplicables en forma rutinaria a la práctica clínica. Objetivo:Estimar el ACT con deuterio en pacientes pediátricos en DP y compararla con las fórmulas de uso clínico habitual, calcular la dosis de diálisis-Kt/V- según el ACT obtenido por las distintas fórmulas y con deuterio. Pacientes y Método:Se evaluaron 8 pacientes en diálisis peritoneal crónica ambulatoria, 6 varones, edad (mediana) 6,6 años (4-14). Se realizó la medición de agua corporal por dilución isotópica con deuterio según protocolo de Plateau, administrando una dosis 1-2 gramos de deuterio al 99,9%, y recolectando una muestra de saliva basal y post-dosis a las 2, 3 y 4 horas; se comparó el resultado de esta medición con las fórmulas de Mellits y Cheek, y (ACT= kg* 0,6). Para el análisis estadístico se utilizó test de Student y test de Bland y Altman, considerando un p significativo Resumen en inglés Paedriatric peritoneal dialysis (PD) is the most frequent form of treatment for end stage chronic renal failure. The dialysis dose (Kt/V) needs to be adjusted periodically, which requires the estimation of total body water (TBW) using different methods or formulas. The ideal method is the use of isotopes oxygen -18 or D20 (deuterium), which are difficult to apply in the routine clinical situation. Objective: To estimate the TBW in children using deuterium and compare the (mas) results with those obtained using formulas commonly used in clinical practice. To calculate the dosis of dialysis according the TBW obtained using the formulas or with deuterium. Patients and methods: 8 children, 6 boys with a mean age of 6.6 years (range 4-14) undergoing CAPD. TBW was measured using a dilution method with deuterium according to the protocol of Plateau. A dose of 1-2 gms of 99.8% deuterium was used, and saliva samples collected at 0, 2, 3 and 4 hours post administration. The results were compared with the formulas of Mellits and Cheek and TBW= kg* 0.6. Statistical analysis was carried out using the Stata 7.0 program with a p value of 0.05 being significant. Results: TBW using deuterium was 2.9% lower than the value obtained using the formula of Mellits and Cheek, and 1.6% higher than the value obtained using the weight. The average value of Kt/V using a TBW based on the different methods was 2.08, 2.08 and 1.90 respectively (p = ns). Conclusions: The estimation of the TBW using different formulas is not significantly different to that using deuterium, permiting their routine use in clinical practice with an adequate level of confidence

Scientific Electronic Library Online (Spanish)

32

Effects of sample pre-treatment on the d13C and d18O values of living benthic foraminifera

Serrano, Oscar; Serrano, Laura; Mateo, Miguel Angel

Stable carbon and oxygen isotope ratios (δ13C and δ18O) of the epibenthic foraminiferan Elphidium macellum var. aculeatum were measured and compared both in raw aliquots and after various pre-analytical treatments. We tested the effects of chemical cleaning procedures (oxygen plasma ashing, NaClO an...

DRIVER (Spanish)

34

Edelfosine-induced metabolic changes in cancer cells that precede the overproduction of reactive oxygen species and apoptosis

Selivanov, Vitaly A.; Vizán, Pedro; Mollinedo, Faustino; Fan, Teresa W. M.; Lee, Paul W. M.; Cascante, Marta
2010-10-06

Digital.CSIC (Spain)

35

Ecosystem and paleohydrological response to Quaternary climate change in the Bonneville Basin, Utah

Balch, Deborah P.; Schnurremberger, Doug; Valero-Garcés, Blas L.; Edwards, R. Lawrence
2005-05-27

Digital.CSIC (Spain)

37

Climate change and coastal hydrographic response along the Atlantic Iberian margin (Tagus Prodelta and Muros Ría) during the last two millennia

Lebreiro, S. M.; Francés, G.; Abrantes, F. F. G.; Diz, P.; Bartels-Jónsdóttir, H. B.; Stroynowski, Z. N.; Gil, I. M.; Pena, L. D.; Rodrigues, T.; Jones, P. D.; Nombela, M. A.; Alejo, I.; Briffa, K. R.; Harris, I.; Grimalt, Joan O.
2006-11-01

Digital.CSIC (Spain)

39

Ancient feeding ecology and extinction of Pleistocene horses from the Pampean Region (Argentina)

Sánchez Chillón, Begoña; Prado, José L.; Alberdi Alonso, María Teresa
2006-01-01

Digital.CSIC (Spain)

40

A high-resolution study of diatom oxygen isotopes in a Late Pleistocene to Early Holocene laminated record from Lake Chungará (Andean Altiplano, Northern Chile)

Hernández, Armand; Bao, Roberto; Giralt, Santiago; Leng, Melanie J.; Barker, Philips A.; Pueyo Mur, Juan José; Sáez, Alberto; Moreno Caballud, Ana; Valero-Garcés, Blas L.; Sloane, Hilary J.
2007-08-01

Digital.CSIC (Spain)