T102 Lacustrine Systems across Space and Time I
Monday, 23 October 2017
8:00 AM - 12:00 PM
Room 307/308
THE OSCILLATING FRINGE OF THE EAST ASIAN MONSOON
Paper number: T102-16
Program: Technical Sessions
Time: 11:45 AM – 12:00 PM
Authors
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Hai XuChinese Academy of Sciences, Xi'an
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Pratigya J. PolissarLamont Doherty Earth Observatory, Palisades, NY
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Wallace BroeckerNew York, NY
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Peter deMenocalColumbia University, New York, NY
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Jianghu LanChinese Academy of Sciences, Xi'an
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Peng ChengInstitute of Earth Environment,Chinese Academy of Sciences, Xi'an
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Weijian ZhouInstitute of Earth Environment, Chinese Academy of Sciences, Xi'an
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Zhisheng AnXi'an
Abstract
Lake-levels were 60 m higher than present during the early and middle Holocene. A mean annual rainfall increase of at least two times higher than today and a ~400 km northward expansion is required to sustain the high stand lake levels. Rainfall amount and the northern extent of the EAM alternated abruptly between wet and dry periods on time scales of a few centuries. Both the onset (~60 m rise at 11.5 ka BP) and termination (~35 m drop at 5.5 ka BP) of the Holocene humid period occurred abruptly, within centuries. δDwax from samples where both age and lake level are well constrained (n=5) show a significant correlation with lake level. In addition, lake level is correlated with both North and South Chinese stalagmite records, indicating that in North China changes in δp are associated with real rainfall changes.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-304574
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