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The δ18O and δ13C records of a 230Th/U dated, 2.2-m long stalagmite from Fengyu Cave in south China provide a continuous decadal-resolution (with 3698 measurements) proxy for regional climatic and environmental conditions during 4–65 ka. This single stalagmite reveals all Heinrich cold events, most Dansgaard-Oeschger warm events, deglaciation and Holocene Optimum, generally supporting the Hulu and...
A total of 117 water samples, including cave water, ground water, spring water and river water, collected from the monsoonal area of China have been analyzed for their H- and O-isotope composition. Overall, a δ 18 O–δD correlation is observed of δD=−4.45+6.6δ 18 O (R 2 =0.90) and a significant evaporation effect observed for the southern sites. Average δ 18 O and δD...
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