Detriral flux of sediment cores in the southeast Indian Ocean ...

Because of a close relationship between detrital flux variations and magnetic susceptibility (MS) flux (MS cm**3 of bulk sediment multiplied by the linear sedimentation rate) variations in the southeast Indian basin of the southern ocean, MS flux profiles have been used to examine the spatial and te...

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Main Authors: Bareille, Gilles F, Grousset, Francis E, Labracherie, Monique, Labeyrie, Laurent D, Petit, Jean Robert
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1994
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.733896
https://doi.pangaea.de/10.1594/PANGAEA.733896
id ftdatacite:10.1594/pangaea.733896
record_format openpolar
spelling ftdatacite:10.1594/pangaea.733896 2024-09-30T14:26:55+00:00 Detriral flux of sediment cores in the southeast Indian Ocean ... Bareille, Gilles F Grousset, Francis E Labracherie, Monique Labeyrie, Laurent D Petit, Jean Robert 1994 application/zip https://dx.doi.org/10.1594/pangaea.733896 https://doi.pangaea.de/10.1594/PANGAEA.733896 en eng PANGAEA https://dx.doi.org/10.1029/94pa01946 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Piston corer MD38 APSARA4 KERSIMAG RC11 Marion Dufresne 1972 Robert Conrad Collection Supplementary Publication Series of Datasets article 1994 ftdatacite https://doi.org/10.1594/pangaea.73389610.1029/94pa01946 2024-09-02T08:40:50Z Because of a close relationship between detrital flux variations and magnetic susceptibility (MS) flux (MS cm**3 of bulk sediment multiplied by the linear sedimentation rate) variations in the southeast Indian basin of the southern ocean, MS flux profiles have been used to examine the spatial and temporal detrital flux changes in this basin during the last climatic cycle. Results indicate a general increase in detrital material input during the coldest periods, suggesting a widespread phenomenon, at least on the basin scale. Mineralogical data, geochemical data, and 87Sr/86Sr isotopic ratios have been used to determine the origin and transport mechanisms responsible for increased detrital flux during glacial periods. Mineralogical and geochemical data show that these glacial 'highs' are due to increases in both Kerguelen-Crozet volcanic and Antarctic detrital inputs. The 87Sr/86Sr isotopic composition of the >45-µm fraction indicates that the Kerguelen-Crozet province contributes to at least 50% of the ... : Supplement to: Bareille, Gilles F; Grousset, Francis E; Labracherie, Monique; Labeyrie, Laurent D; Petit, Jean Robert (1994): Origin of detrital fluxes in the southeast Indian Ocean during the last climatic cycles. Paleoceanography, 9(6), 799-820 ... Article in Journal/Newspaper Antarc* Antarctic Southern Ocean DataCite Antarctic Indian Kerguelen Monique ENVELOPE(70.250,70.250,-49.517,-49.517) Southern Ocean
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Piston corer
MD38
APSARA4
KERSIMAG
RC11
Marion Dufresne 1972
Robert Conrad
spellingShingle Piston corer
MD38
APSARA4
KERSIMAG
RC11
Marion Dufresne 1972
Robert Conrad
Bareille, Gilles F
Grousset, Francis E
Labracherie, Monique
Labeyrie, Laurent D
Petit, Jean Robert
Detriral flux of sediment cores in the southeast Indian Ocean ...
topic_facet Piston corer
MD38
APSARA4
KERSIMAG
RC11
Marion Dufresne 1972
Robert Conrad
description Because of a close relationship between detrital flux variations and magnetic susceptibility (MS) flux (MS cm**3 of bulk sediment multiplied by the linear sedimentation rate) variations in the southeast Indian basin of the southern ocean, MS flux profiles have been used to examine the spatial and temporal detrital flux changes in this basin during the last climatic cycle. Results indicate a general increase in detrital material input during the coldest periods, suggesting a widespread phenomenon, at least on the basin scale. Mineralogical data, geochemical data, and 87Sr/86Sr isotopic ratios have been used to determine the origin and transport mechanisms responsible for increased detrital flux during glacial periods. Mineralogical and geochemical data show that these glacial 'highs' are due to increases in both Kerguelen-Crozet volcanic and Antarctic detrital inputs. The 87Sr/86Sr isotopic composition of the >45-µm fraction indicates that the Kerguelen-Crozet province contributes to at least 50% of the ... : Supplement to: Bareille, Gilles F; Grousset, Francis E; Labracherie, Monique; Labeyrie, Laurent D; Petit, Jean Robert (1994): Origin of detrital fluxes in the southeast Indian Ocean during the last climatic cycles. Paleoceanography, 9(6), 799-820 ...
format Article in Journal/Newspaper
author Bareille, Gilles F
Grousset, Francis E
Labracherie, Monique
Labeyrie, Laurent D
Petit, Jean Robert
author_facet Bareille, Gilles F
Grousset, Francis E
Labracherie, Monique
Labeyrie, Laurent D
Petit, Jean Robert
author_sort Bareille, Gilles F
title Detriral flux of sediment cores in the southeast Indian Ocean ...
title_short Detriral flux of sediment cores in the southeast Indian Ocean ...
title_full Detriral flux of sediment cores in the southeast Indian Ocean ...
title_fullStr Detriral flux of sediment cores in the southeast Indian Ocean ...
title_full_unstemmed Detriral flux of sediment cores in the southeast Indian Ocean ...
title_sort detriral flux of sediment cores in the southeast indian ocean ...
publisher PANGAEA
publishDate 1994
url https://dx.doi.org/10.1594/pangaea.733896
https://doi.pangaea.de/10.1594/PANGAEA.733896
long_lat ENVELOPE(70.250,70.250,-49.517,-49.517)
geographic Antarctic
Indian
Kerguelen
Monique
Southern Ocean
geographic_facet Antarctic
Indian
Kerguelen
Monique
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation https://dx.doi.org/10.1029/94pa01946
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73389610.1029/94pa01946
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