Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...

The Indian Ocean is an important component of the global thermohaline circulation system, as its western boundary currents feed the Agulhas Current, an integral part of the Atlantic meridional overturning circulation. However, Indian Ocean intermediate to deep-water variability on glacial-interglaci...

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Main Authors: Romahn, Sarah, Mackensen, Andreas, Pätzold, Jürgen, Kuhlmann, Holger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.840864
https://doi.pangaea.de/10.1594/PANGAEA.840864
id ftdatacite:10.1594/pangaea.840864
record_format openpolar
spelling ftdatacite:10.1594/pangaea.840864 2024-03-31T07:55:26+00:00 Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ... Romahn, Sarah Mackensen, Andreas Pätzold, Jürgen Kuhlmann, Holger 2014 application/zip https://dx.doi.org/10.1594/pangaea.840864 https://doi.pangaea.de/10.1594/PANGAEA.840864 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type M75/2 Meteor 1986 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Supplementary Publication Series of Datasets article Collection 2014 ftdatacite https://doi.org/10.1594/pangaea.840864 2024-03-04T13:35:39Z The Indian Ocean is an important component of the global thermohaline circulation system, as its western boundary currents feed the Agulhas Current, an integral part of the Atlantic meridional overturning circulation. However, Indian Ocean intermediate to deep-water variability on glacial-interglacial timescales is still a matter of debate. Here we provide stable carbon and oxygen isotopes and sediment elemental compositions of a sediment core from the edge of the Somali Basin. We demonstrate that throughout the past 600 kyr the intermediate western Indian Ocean was primarily bathed by Southern Ocean sourced Upper Circumpolar Deep Water (UCDW). This Southern Ocean sourced water mass enters the Somali Basin via the Amirante Passage or the Mozambique Channel and represents a downstream equivalent of South Atlantic UCDW. We cannot clearly account for the shortterm passage of Red Sea Water (RSW) at 1500 m water depth along the African continental margin, as previously suggested, on glacial-interglacial ... : Supplement to: Romahn, Sarah; Mackensen, Andreas; Pätzold, Jürgen; Kuhlmann, Holger (in prep.): Indian Ocean Deep Water Variability of the past 600 kyr. ... Article in Journal/Newspaper Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Indian Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
M75/2
Meteor 1986
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
M75/2
Meteor 1986
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Romahn, Sarah
Mackensen, Andreas
Pätzold, Jürgen
Kuhlmann, Holger
Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...
topic_facet Gravity corer Kiel type
M75/2
Meteor 1986
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The Indian Ocean is an important component of the global thermohaline circulation system, as its western boundary currents feed the Agulhas Current, an integral part of the Atlantic meridional overturning circulation. However, Indian Ocean intermediate to deep-water variability on glacial-interglacial timescales is still a matter of debate. Here we provide stable carbon and oxygen isotopes and sediment elemental compositions of a sediment core from the edge of the Somali Basin. We demonstrate that throughout the past 600 kyr the intermediate western Indian Ocean was primarily bathed by Southern Ocean sourced Upper Circumpolar Deep Water (UCDW). This Southern Ocean sourced water mass enters the Somali Basin via the Amirante Passage or the Mozambique Channel and represents a downstream equivalent of South Atlantic UCDW. We cannot clearly account for the shortterm passage of Red Sea Water (RSW) at 1500 m water depth along the African continental margin, as previously suggested, on glacial-interglacial ... : Supplement to: Romahn, Sarah; Mackensen, Andreas; Pätzold, Jürgen; Kuhlmann, Holger (in prep.): Indian Ocean Deep Water Variability of the past 600 kyr. ...
format Article in Journal/Newspaper
author Romahn, Sarah
Mackensen, Andreas
Pätzold, Jürgen
Kuhlmann, Holger
author_facet Romahn, Sarah
Mackensen, Andreas
Pätzold, Jürgen
Kuhlmann, Holger
author_sort Romahn, Sarah
title Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...
title_short Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...
title_full Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...
title_fullStr Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...
title_full_unstemmed Stable oxygen and carbon isotopes and sediment geochemistry of sediment core GeoB12616-4 ...
title_sort stable oxygen and carbon isotopes and sediment geochemistry of sediment core geob12616-4 ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.840864
https://doi.pangaea.de/10.1594/PANGAEA.840864
long_lat ENVELOPE(-60.729,-60.729,-64.008,-64.008)
geographic Andreas
Indian
Southern Ocean
geographic_facet Andreas
Indian
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
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.840864
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