Nannofossil absolute abundances of sediment core GeoB1117-2

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Auteurs principaux: Baumann, Karl-Heinz, Kinkel, Hanno
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2025
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author Baumann, Karl-Heinz
Kinkel, Hanno
author_facet Baumann, Karl-Heinz
Kinkel, Hanno
collection Datos científicos de ciencias marinas y ambientales
contents The present study was initiated to ascertain the significance of coccolithophores as a proxy for paleoceanographic and paleoproductivity studies in the equatorial Atlantic. Data from a range of different samples, from the plankton, surface sediments as well as sediment cores are shown and compared with each other. During the past 140,000 years the surface water circulation of the equatorial Atlantic has changed drastically, as can be seen from changes in the coccolithophore species composition, absolute coccolith numbers. Significant increases in coccolith numbers and accumulation rates is observed in the southern equatorial Atlantic during the last glacial interval (oxygen isotope stages 2–4), which we attribute to enhanced upwelling intensities and advection of cool nutrient-rich waters at this site. In the western equatorial Atlantic we observe an opposite trend with decreasing numbers of coccoliths during glacial periods, which probably is caused by a deepening of the thermocline.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_974789
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Nannofossil absolute abundances of sediment core GeoB1117-2
Baumann, Karl-Heinz
Kinkel, Hanno
AGE; Brazil Basin; Calcidiscus leptoporus; Calculated, see reference(s); Center for Marine Environmental Sciences; Coccoliths; Coccoliths, total; coccolith species abundances; Counted; DEPTH, sediment/rock; Emiliania huxleyi; Equatorial Atlantic; Florisphaera profunda; GeoB1117-2; Gephyrocapsa ericsonii; Gephyrocapsa muellerae; Gephyrocapsa oceanica; Gravity corer (Kiel type); M9/4; MARUM; Meteor (1986); SL; Umbilicosphaera sibogae
The present study was initiated to ascertain the significance of coccolithophores as a proxy for paleoceanographic and paleoproductivity studies in the equatorial Atlantic. Data from a range of different samples, from the plankton, surface sediments as well as sediment cores are shown and compared with each other. During the past 140,000 years the surface water circulation of the equatorial Atlantic has changed drastically, as can be seen from changes in the coccolithophore species composition, absolute coccolith numbers. Significant increases in coccolith numbers and accumulation rates is observed in the southern equatorial Atlantic during the last glacial interval (oxygen isotope stages 2–4), which we attribute to enhanced upwelling intensities and advection of cool nutrient-rich waters at this site. In the western equatorial Atlantic we observe an opposite trend with decreasing numbers of coccoliths during glacial periods, which probably is caused by a deepening of the thermocline.
title Nannofossil absolute abundances of sediment core GeoB1117-2
topic AGE; Brazil Basin; Calcidiscus leptoporus; Calculated, see reference(s); Center for Marine Environmental Sciences; Coccoliths; Coccoliths, total; coccolith species abundances; Counted; DEPTH, sediment/rock; Emiliania huxleyi; Equatorial Atlantic; Florisphaera profunda; GeoB1117-2; Gephyrocapsa ericsonii; Gephyrocapsa muellerae; Gephyrocapsa oceanica; Gravity corer (Kiel type); M9/4; MARUM; Meteor (1986); SL; Umbilicosphaera sibogae
url https://doi.org/10.1594/PANGAEA.974789