Stable isotope analysis of foraminifera from sediment core V23-81 (Table 2)

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Hauptverfasser: Jansen, Eystein, Veum, T
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Sprache:en
Veröffentlicht: PANGAEA 1990
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author Jansen, Eystein
Veum, T
author_facet Jansen, Eystein
Veum, T
collection Datos científicos de ciencias marinas y ambientales
contents Oxygen and carbon isotope records from benthic and planktonic foraminifera are presented for the past 35,000 years in the northeastern Atlantic. The results support the idea that the last deglaci-ation took place in two major steps (Duplessy et al., 1981 doi:10.1016/0031-0182(81)90096-1; Mix and Ruddiman, 1985 doi:10.1016/0277-3791(85)90015-0; Ruddiman, 1987; Fairbanks, 1989 doi:10.1038/342637a0), and conflict with theories calling for a strong reduction in North Atlantic deep-water formation to explain the abrupt cooling of the Younger Dryas cold period (Broecker et al., 1985 doi:10.1038/315021a0; Rind et al., 1986 doi:10.1007/BF01277044; Broecker et al., 1988 doi:10.1029/PA003i001p00001).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_106768
institution PANGAEA
language en
publishDate 1990
publisher PANGAEA
record_format pangaea
spellingShingle Stable isotope analysis of foraminifera from sediment core V23-81 (Table 2)
Jansen, Eystein
Veum, T
Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; DEPTH, sediment/rock; Glacial Atlantic Ocean Mapping; GLAMAP; GLAMAP2000; Isotope ratio mass spectrometry; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; PC; Piston corer; V23; V23-81; Vema
Oxygen and carbon isotope records from benthic and planktonic foraminifera are presented for the past 35,000 years in the northeastern Atlantic. The results support the idea that the last deglaci-ation took place in two major steps (Duplessy et al., 1981 doi:10.1016/0031-0182(81)90096-1; Mix and Ruddiman, 1985 doi:10.1016/0277-3791(85)90015-0; Ruddiman, 1987; Fairbanks, 1989 doi:10.1038/342637a0), and conflict with theories calling for a strong reduction in North Atlantic deep-water formation to explain the abrupt cooling of the Younger Dryas cold period (Broecker et al., 1985 doi:10.1038/315021a0; Rind et al., 1986 doi:10.1007/BF01277044; Broecker et al., 1988 doi:10.1029/PA003i001p00001).
title Stable isotope analysis of foraminifera from sediment core V23-81 (Table 2)
topic Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; DEPTH, sediment/rock; Glacial Atlantic Ocean Mapping; GLAMAP; GLAMAP2000; Isotope ratio mass spectrometry; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; PC; Piston corer; V23; V23-81; Vema
url https://doi.org/10.1594/PANGAEA.106768