Abundance of calcareous dinoflagellates of sediment cores from the South Atlantic Ocean

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Main Authors: Esper, Oliver, Zonneveld, Karin A F, Höll, Christine, Karwath, Britta, Schneider, Ralph R, Vink, Annemiek, Weise-Ihlo, Ilka, Willems, Helmut
Format: Dataset Open Access
Language:en
Published: PANGAEA 2000
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author Esper, Oliver
Zonneveld, Karin A F
Höll, Christine
Karwath, Britta
Schneider, Ralph R
Vink, Annemiek
Weise-Ihlo, Ilka
Willems, Helmut
author_facet Esper, Oliver
Zonneveld, Karin A F
Höll, Christine
Karwath, Britta
Schneider, Ralph R
Vink, Annemiek
Weise-Ihlo, Ilka
Willems, Helmut
collection Datos científicos de ciencias marinas y ambientales
contents Despite the increasing interest in the South Atlantic Ocean as a key area of the heat exchange between the southern and the northern hemisphere, information about its palaeoceanographic conditions during transitions from glacial to interglacial stages, the so-called Terminations, are not well understood. Herein we attempt to increase this information by studying the calcareous dinoflagellate cysts and the shells of Thoracosphaera heimii (calcareous cysts) of five Late Quaternary South Atlantic Ocean cores. Extremely high accumulation rates of calcareous cysts at the Terminations might be due to a combined effect of increased cyst production and better preservation as result of calm, oligotrophic conditions in the upper water layers. Low relative abundance of Sphaerodinella albatrosiana compared with Sphaerodinella tuberosa in the Cape Basin may be the result of the relatively colder environmental conditions in this region compared with the equatorial Atlantic Ocean with high relative abundance of S. albatrosiana. Furthermore, the predominance of S. tuberosa during glacials and interglacials at the observed site of the western Atlantic Ocean reflects decreased salinity in the upper water layer.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_603886
institution PANGAEA
language en
publishDate 2000
publisher PANGAEA
record_format pangaea
spellingShingle Abundance of calcareous dinoflagellates of sediment cores from the South Atlantic Ocean
Esper, Oliver
Zonneveld, Karin A F
Höll, Christine
Karwath, Britta
Schneider, Ralph R
Vink, Annemiek
Weise-Ihlo, Ilka
Willems, Helmut
Brazil Basin; Cape Basin; Equatorial Atlantic; GeoB; GeoB1105-4; GeoB1117-2; GeoB1214-1; GeoB2204-2; GeoB3603-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M12/1; M23/3; M34/1; M9/4; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Southern Cape Basin
Despite the increasing interest in the South Atlantic Ocean as a key area of the heat exchange between the southern and the northern hemisphere, information about its palaeoceanographic conditions during transitions from glacial to interglacial stages, the so-called Terminations, are not well understood. Herein we attempt to increase this information by studying the calcareous dinoflagellate cysts and the shells of Thoracosphaera heimii (calcareous cysts) of five Late Quaternary South Atlantic Ocean cores. Extremely high accumulation rates of calcareous cysts at the Terminations might be due to a combined effect of increased cyst production and better preservation as result of calm, oligotrophic conditions in the upper water layers. Low relative abundance of Sphaerodinella albatrosiana compared with Sphaerodinella tuberosa in the Cape Basin may be the result of the relatively colder environmental conditions in this region compared with the equatorial Atlantic Ocean with high relative abundance of S. albatrosiana. Furthermore, the predominance of S. tuberosa during glacials and interglacials at the observed site of the western Atlantic Ocean reflects decreased salinity in the upper water layer.
title Abundance of calcareous dinoflagellates of sediment cores from the South Atlantic Ocean
topic Brazil Basin; Cape Basin; Equatorial Atlantic; GeoB; GeoB1105-4; GeoB1117-2; GeoB1214-1; GeoB2204-2; GeoB3603-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M12/1; M23/3; M34/1; M9/4; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Southern Cape Basin
url https://doi.org/10.1594/PANGAEA.603886