Magnesium/calcium and stable isotope ratios of planktonic foraminifera from the Timor Sea

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Autores principales: Zuraida, Rina, Holbourn, Ann E, Nürnberg, Dirk, Kuhnt, Wolfgang, Dürkop, Anke, Erichsen, A
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2009
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author Zuraida, Rina
Holbourn, Ann E
Nürnberg, Dirk
Kuhnt, Wolfgang
Dürkop, Anke
Erichsen, A
author_facet Zuraida, Rina
Holbourn, Ann E
Nürnberg, Dirk
Kuhnt, Wolfgang
Dürkop, Anke
Erichsen, A
collection Datos científicos de ciencias marinas y ambientales
contents We present sea surface and upper thermocline temperature records (60-100 yr temporal resolution) spanning Marine Isotope Stage 3 (~24-62 kyr BP) from IMAGES Core MD01-2378 (121°47.27'E and 13°04.95'S; 1783 m water depth) located in the outflow area of the Indonesian Throughflow within the Timor Sea. Stable isotopes and Mg/Ca of the near surface dwelling planktonic foraminifer Globigerinoides ruber (white) and the upper thermocline dwelling Pulleniatina obliquiloculata reveal rapid changes in the thermal structure of the upper ocean during Heinrich Events. Thermocline warming and increased delta18Oseawater (P. obliquiloculata record) during Heinrich Events 3, 4, and 5 reflect weakening of the relatively cool and fresh thermocline flow and reduced export of less saline water from the North Pacific and Indonesian Seas to the tropical Indian Ocean. Three main factors influenced Indonesian Throughflow variability during Marine Isotope Stage 3: (1) global slow-down in thermohaline circulation during Heinrich Events triggered by northern hemisphere cooling; (2) increased freshwater export from the Java Sea into the Indonesian Throughflow controlled by rising sea level from ~60 to 47 ka and (3) insolation related changes in Australasian monsoon with associated migration of hydrological fronts between Indian Ocean and Indonesian Throughflow derived water masses at ~46-40 ka.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_712515
institution PANGAEA
language en
publishDate 2009
publisher PANGAEA
record_format pangaea
spellingShingle Magnesium/calcium and stable isotope ratios of planktonic foraminifera from the Timor Sea
Zuraida, Rina
Holbourn, Ann E
Nürnberg, Dirk
Kuhnt, Wolfgang
Dürkop, Anke
Erichsen, A
Giant piston corer; GPC; IMAGES; IMAGES VII - WEPAMA; International Marine Global Change Study; Marion Dufresne (1995); MD012378; MD01-2378; MD122; Timor Sea
We present sea surface and upper thermocline temperature records (60-100 yr temporal resolution) spanning Marine Isotope Stage 3 (~24-62 kyr BP) from IMAGES Core MD01-2378 (121°47.27'E and 13°04.95'S; 1783 m water depth) located in the outflow area of the Indonesian Throughflow within the Timor Sea. Stable isotopes and Mg/Ca of the near surface dwelling planktonic foraminifer Globigerinoides ruber (white) and the upper thermocline dwelling Pulleniatina obliquiloculata reveal rapid changes in the thermal structure of the upper ocean during Heinrich Events. Thermocline warming and increased delta18Oseawater (P. obliquiloculata record) during Heinrich Events 3, 4, and 5 reflect weakening of the relatively cool and fresh thermocline flow and reduced export of less saline water from the North Pacific and Indonesian Seas to the tropical Indian Ocean. Three main factors influenced Indonesian Throughflow variability during Marine Isotope Stage 3: (1) global slow-down in thermohaline circulation during Heinrich Events triggered by northern hemisphere cooling; (2) increased freshwater export from the Java Sea into the Indonesian Throughflow controlled by rising sea level from ~60 to 47 ka and (3) insolation related changes in Australasian monsoon with associated migration of hydrological fronts between Indian Ocean and Indonesian Throughflow derived water masses at ~46-40 ka.
title Magnesium/calcium and stable isotope ratios of planktonic foraminifera from the Timor Sea
topic Giant piston corer; GPC; IMAGES; IMAGES VII - WEPAMA; International Marine Global Change Study; Marion Dufresne (1995); MD012378; MD01-2378; MD122; Timor Sea
url https://doi.org/10.1594/PANGAEA.712515