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Showing 1 to 19 of 19 for “"Planktic foraminifera"”.

  1. Climate proxies in planktic foraminifera: Environmental or biomineralisation controls?

    The calcite shells (or ‘tests’) of foraminifera are among the best archives of Earth’s past climate. Numerous trace elements and isotopes in foraminiferal fossils have been applied as proxies to reconstruct ocean environments over geological time. However, the proxy-environment correlations often …

    cambridge Repository record for Climate proxies in planktic foraminifera: Environmental or biomineralisation controls? (opens in a new tab)

  2. Sodium-Calcium Ratios in the Planktic Foraminifera <i>Trilobatus Sacculifer</i> as a Proxy for Sea Surface Salinity

    … salinity and the incorporation of sodium into foraminiferal calcite, suggesting a potential new proxy for reconstructing past changes in sea surface salinity (SSS) (Mezger et al., 2016 and Bertlich et al., 2018). In order to test the applicability of this new proxy in an open-ocean setting, …

    odu Repository record for Sodium-Calcium Ratios in the Planktic Foraminifera <i>Trilobatus Sacculifer</i> as a Proxy for Sea Surface Salinity (opens in a new tab)

  3. Nitrogen cycling in the subtropical southeast Atlantic and southwest Indian Oceans as recorded by the nitrogen isotopes of modern planktic foraminifera

    … and the long history of using fossil foraminifera to reconstruct past ocean conditions, it is only in recent years, due to methodological advances, that the nitrogen isotope ratio (δ15N) of foraminifera has become a viable proxy for past marine nutrient cycling. Organic N trapped …

    cape-town Repository record for Nitrogen cycling in the subtropical southeast Atlantic and southwest Indian Oceans as recorded by the nitrogen isotopes of modern planktic foraminifera (opens in a new tab)

  4. Abrupt climate change in the Atlantic Ocean during the last 20,000 years : insights from multi-element analysis of benthic and planktic foraminifera and coupled OA-GCM

    Minor and trace element records of planktic and benthic foraminifera from Atlantic sediment cores, as well as output from a coupled OAGCM, were used to investigate the magnitude and distribution of the oceanic response to abrupt climate events of the past 20 kyr. The study addressed three major …

    mit Repository record for Abrupt climate change in the Atlantic Ocean during the last 20,000 years : insights from multi-element analysis of benthic and planktic foraminifera and coupled OA-GCM (opens in a new tab)

  5. Abrupt climate change in the Atlantic Ocean during the last 20,000 years : insights from multi-element analysis of benthic and planktic foraminifera and a coupled OA-GCM

    Minor and trace element records from planktic and benthic foraminifera from Atlantic sediment cores, as well as outputfrom a coupled OA·GCM, were used to investigate the magnitude and distribution of the oceanic response to abrupt Climate events.of the past 20,000 years. The study addressed three …

    woods-hole Repository record for Abrupt climate change in the Atlantic Ocean during the last 20,000 years : insights from multi-element analysis of benthic and planktic foraminifera and a coupled OA-GCM (opens in a new tab)

  6. FORAMINIFERAL DISTRIBUTION AND SEQUENCE STRATIGRAPHY OF OXFORDIAN SUCCESSIONS IN THE WESSEX/ANGLO-PARIS BASIN

    … South Dorset and Normandy were obtained, and foraminifera extracted. Examination of the fauna revealed representatives from 23 families, comprising 36 genera and 126 species. All species were identified and the taxonomy of each studied and described. The abundance and distribution patterns of …

    plymouth Repository record for FORAMINIFERAL DISTRIBUTION AND SEQUENCE STRATIGRAPHY OF OXFORDIAN SUCCESSIONS IN THE WESSEX/ANGLO-PARIS BASIN (opens in a new tab)

  7. Response of pteropod and related faunas to climate change and ocean acidification

    … Sea and Indian Ocean. Pteropods, heteropods and planktic foraminifera were picked from samples to provide palaeoenvironmental data for each core. Determination of pteropod calcification was made using the Limacina Dissolution Index (LDX) and the average shell size of Limacina inflata specimens. …

    plymouth Repository record for Response of pteropod and related faunas to climate change and ocean acidification (opens in a new tab)

  8. Reconstructing Surface Water Carbonate Ion Concentration Changes in the Eastern Equatorial Pacific Across Glacial Transitions

    … climate changes. I measured B/Ca ratios in the planktic foraminifera Globigerina bulloides from core MV1014-17JC (00º10.83’S, 85º52.00’W; 2846 m water depth) as a proxy for changes in surface water carbonate ion concentration ([CO<sub>3</sub><sup>2-</sup>]) in the EEP across both climate …

    odu Repository record for Reconstructing Surface Water Carbonate Ion Concentration Changes in the Eastern Equatorial Pacific Across Glacial Transitions (opens in a new tab)

  9. Diffraction and Spectroscopy of Marine Calcite Biominerals: Insights into Structure and Geochemistry

    … produced by marine organisms. Organisms such as foraminifera and coccolithophores provide an unparalleled 'proxy’ archive of past marine conditions. The way in which these organisms record these proxy archives is largely unknown, and is a fundamental question in applying and interpreting …

    cambridge Repository record for Diffraction and Spectroscopy of Marine Calcite Biominerals: Insights into Structure and Geochemistry (opens in a new tab)

  10. The centennial and millennial variability of the IndoPacific warm pool and the Indonesian Throughflow

    … Mg/Ca and [delta]¹⁸0 of calcite of the calcitic planktic foraminifera Globigerinoides ruber (G. ruber) were used to estimate the sea surface temperature and [delta]¹⁸0 of water, an indicator of hydrologic conditions, over the past 20,000 years. I also attempted to estimate thermocline structure …

    mit Repository record for The centennial and millennial variability of the IndoPacific warm pool and the Indonesian Throughflow (opens in a new tab)

  11. Early Palaeogene planktic foraminiferal assemblages in Australasian sequences: links to past changes in climate and carbon cycling

    … μm), benthic foraminifer abundance (BENTH), and planktic foraminifer fragmentation ratio (FRAG) were measured to create a record of dissolution. There are three intervals where dissolution parameters indicate prominent dissolution episodes for both holes between 65 and 33.7 Ma: during the middle …

    jamescook Repository record for Early Palaeogene planktic foraminiferal assemblages in Australasian sequences: links to past changes in climate and carbon cycling (opens in a new tab)

  12. Neogene to quaternary foraminifera from the western margin of southern Africa

    … how the margin evolved. Fossil shells (tests) of foraminifera (singlecelled protists) from twenty cores from the Namibian shelf (199 to 309 m water depth) and three cores from the western slope (874 to 3631 m water depth) of South Africa were studied to determine the middle Miocene to Quaternary …

    cape-town Repository record for Neogene to quaternary foraminifera from the western margin of southern Africa (opens in a new tab)

  13. Benthic foraminiferal change and depositional history across the Cretaceous – Paleogene (K/Pg) boundary in the Brazos River area, Texas

    … impact or multiple impacts. The benthic foraminiferal data generated indicates significant changes in palaeoecology of the benthic foraminifera across the K/Pg boundary. The benthic foraminifera do not experience a mass extinction, unlike the planktic foraminifera, which were …

    plymouth Repository record for Benthic foraminiferal change and depositional history across the Cretaceous – Paleogene (K/Pg) boundary in the Brazos River area, Texas (opens in a new tab)

  14. Aspects of Neogene palaeoceanography in the southern Tasman Sea (DSDP site 593)

    … are nannofossil ooze changing upcore to foraminifera-bearing nannofossil ooze. This change in texture has been attributed to intermittent winnowing at the site and experimentally determined to be due to selective removal of grains sized 3-13 ηm, which comprise nannofossil placoliths. The …

    waikato-masters Repository record for Aspects of Neogene palaeoceanography in the southern Tasman Sea (DSDP site 593) (opens in a new tab)

  15. The Role of the Ocean in MIS 4 Climatic Changes and Atmospheric CO₂ Variability: a Geochemical Fingerprinting Approach

    … in the future. High resolution planktonic foraminifera Mg/Ca-based SST reconstructions from the Iberian Margin during MIS 4 show that certain aspects of the surface ocean response may not always track Greenland temperature and that Greenland ice core records do not serve as a universal …

    cambridge Repository record for The Role of the Ocean in MIS 4 Climatic Changes and Atmospheric CO₂ Variability: a Geochemical Fingerprinting Approach (opens in a new tab)

  16. Characteristics and evolution of a dynamic prograding continental margin: the late Neogene Giant Foresets Formation, northern Taranaki Basin, New Zealand

    … and the paleoenvironmental interpretation of foraminiferal data derived from well cuttings samples. Outbuilding of the modem continental shelf-slope margin began during the Early Miocene as the regressive phase of a 1ˢᵗ-order megacycle. Four 2ⁿᵈ-order cycles superimposed on this megacycle have …

    waikato-masters Repository record for Characteristics and evolution of a dynamic prograding continental margin: the late Neogene Giant Foresets Formation, northern Taranaki Basin, New Zealand (opens in a new tab)