Paleomagnetic and stable isotope measurements and distribution of benthic foraminifera in sediment core PS1388-3 from the Antarctic continental margin in the eastern Weddell Sea

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Main Authors: Mackensen, Andreas, Grobe, Hannes, Hubberten, Hans-Wolfgang, Spieß, Volkhard, Fütterer, Dieter K
Format: Dataset Open Access
Language:en
Published: PANGAEA 1989
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author Mackensen, Andreas
Grobe, Hannes
Hubberten, Hans-Wolfgang
Spieß, Volkhard
Fütterer, Dieter K
author_facet Mackensen, Andreas
Grobe, Hannes
Hubberten, Hans-Wolfgang
Spieß, Volkhard
Fütterer, Dieter K
collection Datos científicos de ciencias marinas y ambientales
contents A stable isotope record from the eastern Weddell Sea from 69°S is presented. For the first time, a 250,000-yr record from the Southern Ocean can be correlated in detail to the global isotope stratigraphy. Together with magnetostratigraphic, sedimentological and micropalaeontological data, the stratigraphic control of this record can be extended back to 910,000 yrs B.P. A time scale is constructed by linear interpolation between confirmed stratigraphic data points. The benthic d18O record (Epistominella exigua) reflects global continental ice volume changes during the Brunhes and late Matuyama chrons, whereas the planktonic isotopic record (Neogloboquadrina pachyderma) may be influenced by a meltwater lid caused by the nearby Antarctic ice shelf and icebergs. The worldwide climatic improvement during deglaciations is documented in the eastern Weddell Sea by an increase in production of siliceous plankton followed, with a time lag of approximately 10,000 yrs, by planktonic foraminifera production. Peak values in the difference between planktonic and benthic d13C records, which are 0.5 per mil higher during warm climatic periods than during times with expanded continental ice sheets, also suggest increased surface productivity during interglacials in the Southern Ocean.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_549061
institution PANGAEA
language en
publishDate 1989
publisher PANGAEA
record_format pangaea
spellingShingle Paleomagnetic and stable isotope measurements and distribution of benthic foraminifera in sediment core PS1388-3 from the Antarctic continental margin in the eastern Weddell Sea
Mackensen, Andreas
Grobe, Hannes
Hubberten, Hans-Wolfgang
Spieß, Volkhard
Fütterer, Dieter K
ANT-IV/3; Atka Bay; AWI_Paleo; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS08; PS08/366; PS1388-3; SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
A stable isotope record from the eastern Weddell Sea from 69°S is presented. For the first time, a 250,000-yr record from the Southern Ocean can be correlated in detail to the global isotope stratigraphy. Together with magnetostratigraphic, sedimentological and micropalaeontological data, the stratigraphic control of this record can be extended back to 910,000 yrs B.P. A time scale is constructed by linear interpolation between confirmed stratigraphic data points. The benthic d18O record (Epistominella exigua) reflects global continental ice volume changes during the Brunhes and late Matuyama chrons, whereas the planktonic isotopic record (Neogloboquadrina pachyderma) may be influenced by a meltwater lid caused by the nearby Antarctic ice shelf and icebergs. The worldwide climatic improvement during deglaciations is documented in the eastern Weddell Sea by an increase in production of siliceous plankton followed, with a time lag of approximately 10,000 yrs, by planktonic foraminifera production. Peak values in the difference between planktonic and benthic d13C records, which are 0.5 per mil higher during warm climatic periods than during times with expanded continental ice sheets, also suggest increased surface productivity during interglacials in the Southern Ocean.
title Paleomagnetic and stable isotope measurements and distribution of benthic foraminifera in sediment core PS1388-3 from the Antarctic continental margin in the eastern Weddell Sea
topic ANT-IV/3; Atka Bay; AWI_Paleo; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS08; PS08/366; PS1388-3; SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
url https://doi.org/10.1594/PANGAEA.549061