Search results for "Neodymium isotopes"

showing 5 items of 5 documents

Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the co…

2013

11 pages; International audience; The Neodymium(Nd) isotope composition of fish remains has beenwidely used to track past changes in oceanic circulation. Although the number of published Nd isotope data for the Cretaceous has markedly increased in the last years, no consensus has been reached on the structure of the oceanic circulation and its evolution during the Late Cretaceous. Yet this period is characterised bymajor geodynamical and climatic changes andmarked by the disappearance of global oceanic anoxic events inwhich changes in oceanic circulation modesmay have played a significant role. In this study we present the first record of Nd isotopic composition of fish remains from contine…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousIsotopic signaturePaleontologyContinental marginJapanGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryoceanic circulation14. Life underwater[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesRadiogenic nuclide[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySeafloor spreadingCretaceous[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPeriod (geology)Seawaterneodymium isotopesGeology
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Rare earth element and neodymium isotope tracing of sedimentary rock weathering

2020

Chemical weathering plays an important role in sequestering atmospheric CO2, but its potential influence on global climate over geological timescales remains debated. To some extent, this uncertainty arises from the difficulty in separating the respective contribution of sedimentary and crystalline silicate rocks to past weathering rates in the geological record; two types of rocks having presumably different impact on the long-term carbon cycle. In this study, we investigate the use of rare earth element (REE) and neodymium isotopes (εNd) in leached iron oxide fractions of river sediments for tracing the origin of weathered rocks on continents. A new index, called ‘concavity index’ (CI), i…

010504 meteorology & atmospheric sciencessub-01Mid-REE enrichmentGeochemistrySilicate weatheringWeatheringConcavity indexengineering.materialStructural basin010502 geochemistry & geophysicsGeologic record01 natural sciencesIron oxideschemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[CHIM]Chemical Sciences0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySulphide weatheringNeodymium isotopesGeology15. Life on landWorld riversSilicateCratonchemistry13. Climate actionCarbonate weatheringengineeringCarbonateSedimentary rockPyriteGeology
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Water mass exchange and variations in seawater temperature in the NW Tethys during the Early Jurassic: evidence from neodymium and oxygen isotopes of…

2009

10 pages; International audience; Oxygen and neodymium isotope analyses performed on biostratigraphically well-dated fish remains recovered from the Hettangian to Toarcian of the Paris Basin were used to reconstruct variations of Early Jurassic seawater temperature and to track oceanographic changes in the NW Tethys. Our results indicate a strong correlation between δ18O trends recorded by fish remains and belemnites, confirming the paleoenvironmental origin of oxygen isotope variations. Interestingly, temperatures recorded by pelagic fishes and nektobenthic belemnites and bottom dwelling fishes are comparable during the Late Pliensbachian sea-level lowstand but gradually differ during the …

010506 paleontologyWater mass[SDE.MCG]Environmental Sciences/Global ChangesToarcian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologyWater columnGeochemistry and PetrologyPaleoceanography[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrypaleoclimateEarth and Planetary Sciences (miscellaneous)14. Life underwater0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRadiogenic nuclidebiologyoxygen isotopesPelagic zonebiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphypaleoceanographyfish toothSeawaterneodymium isotopes[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyBelemnitesGeology
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Evolution de la circulation oécanique profonde durant le Crétacé : apport des isotopes du néodyme

2014

The Cretaceous is depicted as the warmest period of the last 300 Ma. The oceanic circulation and location of the source zones of deep-waters are essential to understand the role of oceans in the evolution of the climate during the Cretaceous, yet they remain unclear for this period. The neodymium (Nd) isotopes are used to track oceanic circulation and exchanges between water masses, in both past and modern oceans. The Nd isotope composition (εNd) in the ocean is related to the nature of the surrounding continental landmasses. The oceanic currents transport this isotopic signature, thus every oceanic basin acquires a singular εNd. Unequivocal interpretations of the Cretaceous seawater εNd va…

Oceanic circulationCrétacéNeodymium isotopesIsotopes du néodyme[SDU.STU] Sciences of the Universe [physics]/Earth SciencesCirculation océanique[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesRare earth elementsClimate modelModélisation climatiqueCretaceousTerres rares
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Evolution of neodymium isotopic signature of seawater during the Late Cretaceous: implications for intermediate and deep circulation.

2016

20 pages; International audience; Neodymium isotopic compositions (εNd) have been largely used for the last fifty years as a tracer of past ocean circulation, and more intensively during the last decade to investigate ocean circulation during the Cretaceous period. Despite a growing set of data, circulation patterns still remain unclear during this period. In particular, the identification of the deep-water masses and their spatial extension within the different oceanic basins are poorly constrained. In this study we present new deep-water εNd data inferred from the Nd isotope composition of fish remains and Fe–Mn oxyhydroxide coatings on foraminifera tests, along with new εNd data of resid…

Water mass010504 meteorology & atmospheric sciences010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousBottom waterPaleontologyOcean circulation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterSouthern Ocean0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryNeodymium isotopesNorth Atlantic Deep WaterOcean currentAbyssal plainGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousOceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyThermohaline circulationOceanic basinGeology
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