Topic
Paleoceanography
About: Paleoceanography is a research topic. Over the lifetime, 1405 publications have been published within this topic receiving 46519 citations. The topic is also known as: palaeoceanography.
Papers published on a yearly basis
Papers
Book•
1 Jan 1999
TL;DR: In this paper, a tool for the reconstruction of surface water Stratification using Pteropod Shells as a record of sub-surface water conditions is presented. But the tool is limited to the South Atlantic and the Southern Ocean.
Abstract: Clues to Ocean History: a Brief Overview of Proxies.- Surface Water Circulation.- Sea-Surface Temperature Estimations Using a Modern Analog Technique with Foraminiferal Assemblages from Western Atlantic Quaternary Sediments.- The Distribution of Living Planktic Foraminifera in Relation to Southeast Atlantic Oceanography.- Coccolithophores as Indicators of Ocean Water Masses, Surface-Water Temperature, and Paleoproductivity - Examples from the South Atlantic.- Calcareous Dinoflagellate Cysts as Paleo-Environmental Tools.- Oxygen Isotope Values of Planktic Foraminifera: A Tool for the Reconstruction of Surface Water Stratification.- Stable Isotopes of Pteropod Shells as Recorders of Sub-Surface Water Conditions: Comparison to the Record of G. ruber and to Measured Values.- On the Reconstruction of Paleosalinities.- Bottom- and Deep Water Circulation.- Stable Carbon Isotopes in Benthic Foraminifera: Proxies for Deep and Bottom Water Circulation and New Production.- Carbonate Dissolution in the Deep-Sea: Methods, Quantification and Paleoceanographic Application.- Kaolinite and Chlorite as Tracers of Modern and Late Quaternary Deep Water Circulation in the South Atlantic and the Adjoining Southern Ocean.- Paleoproductivity and Nutrients.- Organic Carbon and Carbonate as Paleoproductivity Proxies: Examples from High and Low Productivity Areas of the Tropical Atlantic.- Biogenic Barium as a Proxy for Paleoproductivity: Methods and Limitations of Application.- Variability in Export Production Documented by Downward Fluxes and Species Composition of Marine Planktic Diatoms: Observations from the Tropical and Equatorial Atlantic.- Reliability of the 231Pa/230 Th Activity Ratio as a Tracer for Bioproductivity of the Ocean.- Sediment Redistribution, 230Thex - Normalization and Implications for the Reconstruction of Particle Flux and Export Paleoproductivity.- The South Atlantic Carbon Isotope Record of Planktic Foraminifera.- Reconstruction of Surface Ocean Nitrate Utilization Using Stable Nitrogen Isotopes in Sinking Particles and Sediments.- CO2 in Oceans and Atmosphere.- Alkenone ?13C as a Proxy for Past PCO2 in Surface Waters: Results from the Late Quaternary Angola Current.- Reassessing Foraminiferal Stable Isotope Geochemistry: Impact of the Oceanic Carbonate System (Experimental Results).- Implications of a Carbonate Ion Effect on Shell Carbon and Oxygen Isotopes for Glacial Ocean Conditions.- Atmospherical Circulation.- Pollen and Spores in Marine Sediments from the East Atlantic - A View from the Ocean into the African Continent.- Terrestrial Organic Matter in Marine Sediments: Analytical Approaches and Eolian-Marine Records in the Central Equatorial Atlantic.- Environmental Magnetism.- The Magnetic View on the Marine Paleoenvironment: Parameters, Techniques, and Potentials of Rock Magnetic Studies as a Key to Paleoclimatic and Paleoceanographic Changes.- Using Rock Magnetic Proxy Records for Orbital Tuning and Extended Time Series Analyses into the Super- and Sub-Milankovitch Bands.- Geomagnetic Events and Relative Paleointensity Records - Clues to High-Resolution Paleomagnetic Chronostratigraphies of Late Quaternary Marine Sediments?.- Modelling.- Simulation of Oxygen Isotopes in a Global Ocean Model.- Reconstructing and Modelling the Last Glacial Maximum: Beyond CLIMAP.- Data Management.- Data Management of Proxy Parameters with PANGAEA.
677 citations
TL;DR: In this paper, the authors examined U-Mo covariation in organic-rich sediments deposited mostly in the western Tethyan region during oceanic anoxic events (OAEs) of Early Jurassic to Late Cretaceous age.
641 citations
TL;DR: The radiogenic isotope composition of dissolved trace metals in the ocean represents a set of relatively new and not yet fully exploited tracers with a large potential for oceanographic and paleoceanographic research on timescales from the present back to at least 60 Ma.
Abstract: The radiogenic isotope composition of dissolved trace metals in the ocean represents a set of relatively new and not yet fully exploited tracers with a large potential for oceanographic and paleoceanographic research on timescales from the present back to at least 60 Ma. The main topic of this review are those trace metals with oceanic residence times on the order of or shorter than the global mixing time of the ocean (Nd, Pb, Hf, and, in addition, Be). Their isotopic composition in the ocean has varied as a function of changes in paleocirculation, source provenances, style and intensity of weathering on the continents, as well as orogenic processes. The relative importance of these processes for each trace metal is evaluated, which is a prerequisite for reliable interpretation of their time series in terms of changes in paleocirculation or weathering inputs. This analysis of processes includes a discussion of the long-term isotopic evolution of Sr and Os, which are well mixed in the ocean and have thus not been influenced by circulation changes. The radiogenic isotope evolution of those trace metals with intermediate oceanic residence times can be used as paleoceanographic proxies to reconstruct paleocirculation and weathering inputs into the ocean. This is demonstrated by studies from different ocean basins, mainly carried out on ferromanganese crusts, which show that radiogenic trace metal isotopes provide important new insights and can complement results obtained by other well-established paleoceanographic tracers such as carbon isotopes.
568 citations
TL;DR: In this paper, high-precision isotope ratios of dissolved Mo in seawater from different ocean basins and depths show a homogeneous isotope composition (MOMO), as expected from its long ocean residence time (800 kyr).
541 citations
TL;DR: Comparisons of carbon isotopic data on benthic foraminifera from Deep Sea Drilling Project sites 502 and 503 suggest that modern circulation patterns in the Caribbean and eastern Pacific developed by 3 million years ago in concert with changing tectonic, climatic, and biogeographic patterns.
Abstract: Comparisons of carbon isotopic data on benthic foraminifera from Deep Sea Drilling Project sites 502 (western Caribbean) and 503 (eastern Pacific) indicate that the difference between the Atlantic and the Pacific in the per mil enrichment in carbon-13 of total dissolved carbon dioxide increased about 6 million years ago and again 3 million years ago, when the difference reached the modern level (1 per mil). Comparisons of planktonic foraminiferal oxygen isotopic data for the Caribbean and the Pacific suggest that the salinity of Caribbean surface waters began increasing 4 million years ago, possibly in response to shoaling of the Panama isthmus. These results suggest that modern circulation patterns in the Caribbean and eastern Pacific developed by 3 million years ago in concert with changing tectonic, climatic, and biogeographic patterns.
532 citations
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Performance Metrics
| Year | Papers |
|---|---|
| 2025 | 12 |
| 2024 | 30 |
| 2023 | 61 |
| 2022 | 82 |
| 2021 | 43 |
| 2020 | 45 |