Paleoclimate of southwestern China for the past 50,000 yr inferred from lake sediment records.
Long sediment cores (12.5 and 13.5 m) from two lakes in Yunnan Province were used to infer the paleoclimate of southwest China over the past 50,000 yr. During the Holocene and marine isotope stage (MIS 3), bio-induced carbonate precipitation and organic matter (OM) production was high, suggesting wa...
Main Authors: | , , , , , , , |
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Format: | Text |
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Digital Archive
1999
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Online Access: | https://digital.stpetersburg.usf.edu/fac_publications/2446 https://login.ezproxy.lib.usf.edu/login?url=http://www.sciencedirect.com/science/article/pii/S0033589499920720# |