Does the North Atlantic influence the monsoon signal in Asian speleothems? (original) (raw)

2010

Abstract

Speleothems from Indian and Chinese caves have been broadly used to infer past monsoon strength, since the oxygen isotopic composition of the spelothems is primarily controlled by the oxygen composition of the precipitation. However, the d18O changes recorded by the speleothems could be due not only to a change in the strength of the monsoon but also to other causes,

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