Timing and structure of the 8.2 kyr B.P. event inferred from δ18 O records of stalagmites from China, Oman, and Brazil
Oxygen isotope records of stalagmites from China and Oman reveal a weak summer monsoon event, with a double-plunging struc- ture, that started 8.21 ± 0.02 kyr B.P. An identical but antiphased pattern is also evident in two stalagmite records from eastern Brazil, indicating that the South American Su...
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Digital Commons @ University of South Florida
2009
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Online Access: | https://digitalcommons.usf.edu/kip_articles/5403 https://doi.org/10.1130/G30126A |