Planktonic Foraminiferal and Alkenone Records of the Last Deglaciation from the Eastern Arabian Sea

The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief δ18O transient event. In the tropics, this δ18O maximum could correspond to a cooling or to a change in the δ18O content of sea water. In this stu...

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Published inQuaternary research Vol. 52; no. 3; pp. 337 - 342
Main Authors Cayre, Olivia, Bard, Edouard
Format Journal Article
LanguageEnglish
Published New York, USA Cambridge University Press 01.11.1999
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Abstract The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief δ18O transient event. In the tropics, this δ18O maximum could correspond to a cooling or to a change in the δ18O content of sea water. In this study, past sea-surface temperature (SST) and primary production (PP) are reconstructed from foraminiferal transfer functions and compared to values estimated from alkenone measurements. SST and PP records from both proxies indicate a 1.5–2.5°C deglacial warming, coupled with a PP decrease, and a 0.5–1°C cooling during the Younger Dryas (YD). A detailed comparison between independent micropaleontological and geochemical proxies helps us identify potential biases and thus strengthen the paleo-reconstructions.
AbstractList The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief δ18O transient event. In the tropics, this δ18O maximum could correspond to a cooling or to a change in the δ18O content of sea water. In this study, past sea-surface temperature (SST) and primary production (PP) are reconstructed from foraminiferal transfer functions and compared to values estimated from alkenone measurements. SST and PP records from both proxies indicate a 1.5–2.5°C deglacial warming, coupled with a PP decrease, and a 0.5–1°C cooling during the Younger Dryas (YD). A detailed comparison between independent micropaleontological and geochemical proxies helps us identify potential biases and thus strengthen the paleo-reconstructions.
The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief δ 18 O transient event. In the tropics, this δ 18 O maximum could correspond to a cooling or to a change in the δ 18 O content of sea water. In this study, past sea-surface temperature (SST) and primary production (PP) are reconstructed from foraminiferal transfer functions and compared to values estimated from alkenone measurements. SST and PP records from both proxies indicate a 1.5–2.5°C deglacial warming, coupled with a PP decrease, and a 0.5–1°C cooling during the Younger Dryas (YD). A detailed comparison between independent micropaleontological and geochemical proxies helps us identify potential biases and thus strengthen the paleo-reconstructions.
The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief delta super(18)O transient event. In the tropics, this delta super(18)O maximum could correspond to a cooling or to a change in the delta super(18)O content of sea water. In this study, past sea-surface temperature (SST) and primary production (PP) are reconstructed from foraminiferal transfer functions and compared to values estimated from alkenone measurements. SST and PP records from both proxies indicate a 1.5-2.5 degree C deglacial warming, coupled with a PP decrease, and a 0.5-1 degree C cooling during the Younger Dryas (YD). A detailed comparison between independent micropaleontological and geochemical proxies helps us identify potential biases and thus strengthen the paleo-reconstructions.
Author Cayre, Olivia
Bard, Edouard
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DocumentTitleAlternate CAYRE AND BARD
THE LAST DEGLACIATION FROM THE EASTERN ARABIAN SEA
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Issue 3
Keywords last deglaciation
Arabian Sea
planktonic foraminifera
alkenones
Marine quaternary
Methodology
Oxygen 18
Palaeo-ecology
Marine sediment
Foraminifera
Surface temperature
Palaeo-environment
Deglaciation
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Snippet The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief δ18O...
The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief δ 18...
The oxygen isotope record of planktonic foraminifera from tropical core MD77194 (Eastern Arabian Sea) exhibits a clear two-step deglaciation with a brief delta...
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SubjectTerms alkenones
Arabian Sea
Bgi / Prodig
last deglaciation
Marine
Marine quaternary
Palaeogeography
Physical geography
planktonic foraminifera
Title Planktonic Foraminiferal and Alkenone Records of the Last Deglaciation from the Eastern Arabian Sea
URI https://www.cambridge.org/core/product/identifier/S0033589400025941/type/journal_article
https://dx.doi.org/10.1006/qres.1999.2083
https://search.proquest.com/docview/17391674
Volume 52
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