Late Holocene climatic changes in Garhwal Himalaya
Late Holocene climatic changes in Garhwal Himalaya
Geochemical study of a 3.55 m long lake sediment core from the Badanital Lake (Garhwal Himalaya) reveals Late Holocene centennial-scale climatic changes. The ecosystem of the tectonically formed lake seems to be controlled by natural and anthropogenic factors.
Publication Date:
10/04/2013
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7
911-919