Magnesium/Calcium ratios and sea surface temperature estimation for sediments of the Timor Sea

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Auteurs principaux: Xu, Jian, Kuhnt, Wolfgang, Holbourn, Ann E, Andersen, Nils, Bartoli, Gretta
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2006
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author Xu, Jian
Kuhnt, Wolfgang
Holbourn, Ann E
Andersen, Nils
Bartoli, Gretta
author_facet Xu, Jian
Kuhnt, Wolfgang
Holbourn, Ann E
Andersen, Nils
Bartoli, Gretta
collection Datos científicos de ciencias marinas y ambientales
contents We use a multiproxy approach to monitor changes in the vertical profile of the Indonesian Throughflow as well as monsoonal wind and precipitation patterns in the Timor Sea on glacial-interglacial, precessional, and suborbital timescales. We focus on an interval of extreme climate change and sea level variation: marine isotope (MIS) 6 to MIS 5e. Paleoproductivity fluctuations in the Timor Sea follow a precessional beat related to the intensity of the Australian (NW) monsoon. Paired Mg/Ca and d18O measurements of surface- and thermocline-dwelling planktonic foraminifers (G. ruber and P. obliquiloculata) indicate an increase of >4°C in both surface and thermocline water temperatures during Termination II. Tropical sea surface temperature changed synchronously with ice volume (benthic d18O) during deglaciation, implying a direct coupling of high- and low-latitude climate via atmospheric and/or upper ocean circulation. Substantial cooling and freshening of thermocline waters occurred toward the end of Termination II and during MIS 5e, indicating a change in the vertical profile of the Indonesian Throughflow from surface- to thermocline-dominated flow.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_760657
institution PANGAEA
language en
publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle Magnesium/Calcium ratios and sea surface temperature estimation for sediments of the Timor Sea
Xu, Jian
Kuhnt, Wolfgang
Holbourn, Ann E
Andersen, Nils
Bartoli, Gretta
Giant piston corer; GIK18460-2; GIK18462-2; GIK18480-2; GPC; IMAGES; IMAGES VII - WEPAMA; Indian Ocean; International Marine Global Change Study; Marion Dufresne (1995); MD012378; MD01-2378; MD122; MD122-MC01; MD122-MC02; MD122-MC03; MUC; MultiCorer; SO185; Sonne; Timor Sea; VITAL
We use a multiproxy approach to monitor changes in the vertical profile of the Indonesian Throughflow as well as monsoonal wind and precipitation patterns in the Timor Sea on glacial-interglacial, precessional, and suborbital timescales. We focus on an interval of extreme climate change and sea level variation: marine isotope (MIS) 6 to MIS 5e. Paleoproductivity fluctuations in the Timor Sea follow a precessional beat related to the intensity of the Australian (NW) monsoon. Paired Mg/Ca and d18O measurements of surface- and thermocline-dwelling planktonic foraminifers (G. ruber and P. obliquiloculata) indicate an increase of >4°C in both surface and thermocline water temperatures during Termination II. Tropical sea surface temperature changed synchronously with ice volume (benthic d18O) during deglaciation, implying a direct coupling of high- and low-latitude climate via atmospheric and/or upper ocean circulation. Substantial cooling and freshening of thermocline waters occurred toward the end of Termination II and during MIS 5e, indicating a change in the vertical profile of the Indonesian Throughflow from surface- to thermocline-dominated flow.
title Magnesium/Calcium ratios and sea surface temperature estimation for sediments of the Timor Sea
topic Giant piston corer; GIK18460-2; GIK18462-2; GIK18480-2; GPC; IMAGES; IMAGES VII - WEPAMA; Indian Ocean; International Marine Global Change Study; Marion Dufresne (1995); MD012378; MD01-2378; MD122; MD122-MC01; MD122-MC02; MD122-MC03; MUC; MultiCorer; SO185; Sonne; Timor Sea; VITAL
url https://doi.org/10.1594/PANGAEA.760657