Calcitic foraminiferal data confirmed by cadmium in aragoniticHoeglundina: Application to the Last Glacial Maximum in the northern Indian Ocean

1995 ◽  
Vol 10 (5) ◽  
pp. 881-900 ◽  
Author(s):  
Edward A. Boyle ◽  
Laurent Labeyrie ◽  
Jean-Claude Duplessly
1980 ◽  
Vol 14 (3) ◽  
pp. 309-336 ◽  
Author(s):  
Warren L. Prell ◽  
William H. Hutson ◽  
Douglas F. Williams ◽  
Allan W.H. Bé ◽  
Kurt Geitzenauer ◽  
...  

AbstractA seasonal reconstruction of the Indian Ocean during the last glacial maximum (∼18,000 yr B.P.) reveals that its surface circulation and sea surface temperature patterns were significantly different from the modern Indian Ocean. This reconstruction is based on the planktonic foraminiferal biogeography and estimated sea surface temperatures in 42 Indian Ocean samples. Compared to modern conditions, the polar front was 5° to 10° latitude further north during the last glacial maximum; the Subtropical Convergence was 2° to 5° latitude further north. The West Australian Current was more intense as part of the West Wind Drift was deflected northward along the coast of Australia. The Agulhas Current was cooler and weaker during the summer and more saline and subtropical during the winter. In general, the low latitudes underwent little temperature change. The western Arabian Sea was warmer which implies less upwelling and a weaker Southwest Monsoon. On the average, the Indian Ocean was 1.9°C cooler in February and 1.7°C cooler in August during the last glacial maximum.


Geology ◽  
2017 ◽  
Vol 45 (5) ◽  
pp. 435-438 ◽  
Author(s):  
Enlou Zhang ◽  
Cheng Zhao ◽  
Bin Xue ◽  
Zhonghui Liu ◽  
Zicheng Yu ◽  
...  

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