https://doi.pangaea.de/10.1594/PANGAEA.993418Baumann, Karl-HeinzKarl-HeinzBaumann0000-0003-2109-5179PANGAEA2026coccolith abundancesCoccolithsEquatorial AtlanticDEPTH, sediment/rockAGECoccoliths, totalCalciosolenia spp.Calcidiscus leptoporusCoccolithus braarudiiEmiliania huxleyiFlorisphaera profundaGephyrocapsa caribbeanicaGephyrocapsa ericsoniiGephyrocapsa muelleraeGephyrocapsa oceanicaGladiolithus flabellatusHayaster perplexusHelicosphaera carteriOolithotus fragilisReticulofenestra sessilisRhabdosphaera clavigeraRhabdosphaera spp.Syracosphaera pulchraSyracosphaera spp.Umbilicosphaera hulburtianaUmbilicosphaera sibogaeUmbellosphaera irregularisUmbellosphaera tenuisCoccoliths, otherGravity corer (Kiel type)Scanning electron microscope (SEM), Zeiss, DSM 940AM29/3Meteor (1986)1994-08-24T00:00:00Dataset2184 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThe calcareous nannofossil assemblages from sediment core GeoB2908-7 from the equatorial Atlantic were examined to document oceanographic changes in surface waters during the last 365 ka. Coccolith counts were made manually on filtered samples using a Zeiss DSM 940A scanning electron microscope at 3,000x or 5,000x magnification. The surface water circulation of the equatorial Atlantic has changed drastically, as can be seen from changes in the coccolithophore species composition and absolute coccolith abundances.-23.3266666666670.10666666666667Western Equatorial Atlantic