Holocene precipitation δ~(18)O as an indicator of temperature history in arid central Asia: an overv

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Holocene δ~(18)O records from various archives(ice cores, cave stalagmites, and peat sediments) from the Xinjiang region of northwestern China, in arid central Asia(ACA), are all derived ultimately from local precipitation δ~(18)O(δ~(18)Op). Neverthele
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