Glacial to Holocene changes in the surface and deep waters of the northeast Indian Ocean

Stable carbon and oxygen isotopic investigations are carried out on planktonic and benthic foraminifera from an AMS-dated sediment core of the northeast Indian Ocean (NEIO) to infer glacial to Holocene changes in surface and deep waters. The chronology of this gravity core (SK157-14; water-depth 330...

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Veröffentlicht in:	Marine geology 2012-11, Vol.329-331, p.16-23
Hauptverfasser:	Ahmad, Syed M., Zheng, Hongbo, Raza, Waseem, Zhou, Bin, Lone, Mahjoor A., Raza, Tabish, Suseela, Gorti
Format:	Artikel
Sprache:	eng
Schlagworte:	Back propagation Deep water Foraminifera Holocene Indian Ocean Intervals Last glacial maximum Marine Northeast Northeast Indian Ocean Oxygen isotopes Sediments Surface water δ13C δ18O
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