(Appendix A) Abundance of calcareous dinoflagellates of sediment core GeoB2204-2

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Main Authors: Höll, Christine, Karwath, Britta, Rühlemann, Carsten, Zonneveld, Karin A F, Willems, Helmut
Format: Dataset Open Access
Language:en
Published: PANGAEA 1999
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author Höll, Christine
Karwath, Britta
Rühlemann, Carsten
Zonneveld, Karin A F
Willems, Helmut
author_facet Höll, Christine
Karwath, Britta
Rühlemann, Carsten
Zonneveld, Karin A F
Willems, Helmut
collection Datos científicos de ciencias marinas y ambientales
contents The environmental preferences of calcareous dinoflagellates have been investigated over the last 140 ka by comparing material from two sediment cores: one from the highly productive equatorial divergence of the eastern Atlantic Ocean and the other from the low productivity western tropical Atlantic Ocean. Pronounced differences in palaeoproductivity between the two sediment cores are indicated by high and variable organic carbon accumulation rates in the east, in contrast to relatively constant and low values in the west. Calcareous dinoflagellates show just the opposite pattern: high accumulation rates in the west and lower in the east. At the equatorial divergence, temporal variations of calcareous dinoflagellate and organic carbon accumulation rates show, for the most part, an inverse relationship. High calcareous dinoflagellate content coincides with low organic carbon accumulation rates and vice versa. In the investigated region and time interval, enhanced production of calcareous dinoflagellates can be correlated to periods of reduced palaeoproductivity probably related to relatively stratified conditions of the upper water column.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_55382
institution PANGAEA
language en
publishDate 1999
publisher PANGAEA
record_format pangaea
spellingShingle (Appendix A) Abundance of calcareous dinoflagellates of sediment core GeoB2204-2
Höll, Christine
Karwath, Britta
Rühlemann, Carsten
Zonneveld, Karin A F
Willems, Helmut
Brazil Basin; Calciodinellum albatrosianum; Calciodinellum levantinum; Counting, dinoflagellate cysts; DEPTH, sediment/rock; GeoB2204-2; Gravity corer (Kiel type); Leonella granifera; M23/3; Meteor (1986); Rhabdothorax spp.; Sample mass; Sample volume; see reference(s); SFB261; SL; Slide volume; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Thoracosphaera heimii
The environmental preferences of calcareous dinoflagellates have been investigated over the last 140 ka by comparing material from two sediment cores: one from the highly productive equatorial divergence of the eastern Atlantic Ocean and the other from the low productivity western tropical Atlantic Ocean. Pronounced differences in palaeoproductivity between the two sediment cores are indicated by high and variable organic carbon accumulation rates in the east, in contrast to relatively constant and low values in the west. Calcareous dinoflagellates show just the opposite pattern: high accumulation rates in the west and lower in the east. At the equatorial divergence, temporal variations of calcareous dinoflagellate and organic carbon accumulation rates show, for the most part, an inverse relationship. High calcareous dinoflagellate content coincides with low organic carbon accumulation rates and vice versa. In the investigated region and time interval, enhanced production of calcareous dinoflagellates can be correlated to periods of reduced palaeoproductivity probably related to relatively stratified conditions of the upper water column.
title (Appendix A) Abundance of calcareous dinoflagellates of sediment core GeoB2204-2
topic Brazil Basin; Calciodinellum albatrosianum; Calciodinellum levantinum; Counting, dinoflagellate cysts; DEPTH, sediment/rock; GeoB2204-2; Gravity corer (Kiel type); Leonella granifera; M23/3; Meteor (1986); Rhabdothorax spp.; Sample mass; Sample volume; see reference(s); SFB261; SL; Slide volume; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; Thoracosphaera heimii
url https://doi.org/10.1594/PANGAEA.55382