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Main Authors: Wien, Katharina, Kölling, Martin, Schulz, Horst D
Format: Dataset Open Access
Language:en
Published: PANGAEA 2005
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.711655
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author Wien, Katharina
Kölling, Martin
Schulz, Horst D
author_facet Wien, Katharina
Kölling, Martin
Schulz, Horst D
collection Datos científicos de ciencias marinas y ambientales
contents High-resolution records of Ca and Sr were obtained from shipboard XRF analyses of bulk sediments in five gravity cores from the southern Cape Basin, South Atlantic Ocean. Sr/Ca ratios display regular glacial/interglacial variations of 14-40% and reveal a close correlation with the SPECMAP record, minimum Sr/Ca ratios appearing during glacial (delta18 O) maxima, distinct increases during periods of deglaciation, and highest ratios in interstadials. Shifts in carbonate-producing phytoplankton and/or zooplankton assemblages over glacial/interglacial cycles are suggested to be the main cause for the observed variations in Sr/Ca patterns. Quick assessment of the relationship between Sr/Ca ratios and the SPECMAP record made it possible to easily transfer an age model to the newly collected cores already during the cruise.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_711655
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle Element concentrations of bulk sediment from the Southern Cape Basin
Wien, Katharina
Kölling, Martin
Schulz, Horst D
GeoB2004-3; GeoB8301-6; GeoB8307-6; GeoB8310-2; GeoB8315-6; Gravity corer (Kiel type); M23/1; M57/1; Meteor (1986); SL; South African margin
High-resolution records of Ca and Sr were obtained from shipboard XRF analyses of bulk sediments in five gravity cores from the southern Cape Basin, South Atlantic Ocean. Sr/Ca ratios display regular glacial/interglacial variations of 14-40% and reveal a close correlation with the SPECMAP record, minimum Sr/Ca ratios appearing during glacial (delta18 O) maxima, distinct increases during periods of deglaciation, and highest ratios in interstadials. Shifts in carbonate-producing phytoplankton and/or zooplankton assemblages over glacial/interglacial cycles are suggested to be the main cause for the observed variations in Sr/Ca patterns. Quick assessment of the relationship between Sr/Ca ratios and the SPECMAP record made it possible to easily transfer an age model to the newly collected cores already during the cruise.
title Element concentrations of bulk sediment from the Southern Cape Basin
topic GeoB2004-3; GeoB8301-6; GeoB8307-6; GeoB8310-2; GeoB8315-6; Gravity corer (Kiel type); M23/1; M57/1; Meteor (1986); SL; South African margin
url https://doi.org/10.1594/PANGAEA.711655