Preliminary study on climatic signals of stable isotopes from Holocene speleothems under monsoon condition

Stalagmite East Asian Monsoon
DOI: 10.1007/bf02883822 Publication Date: 2008-04-04T15:29:57Z
ABSTRACT
Within the East Asian monsoon zone the change in oxygen isotope of Holocene stalagmite is mainly related to monsoon rain rather than to temperature. And carbon isotope can be taken as a comprehensive signal which contains the natural information and the information of anthropogenic activity. Isotopic analysis is also compared with the annual layer records.
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