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Centennial-Scale Monsoon Failure During the Younger Dryas Event Record in a High-ResolutionStalagmite from Longfugong Cave,Central China(PDF)

《南京师范大学学报》(自然科学版)[ISSN:1001-4616/CN:32-1239/N]

Issue:
2017年01期
Page:
134-
Research Field:
·地理学·
Publishing date:

Info

Title:
Centennial-Scale Monsoon Failure During the Younger Dryas Event Record in a High-ResolutionStalagmite from Longfugong Cave,Central China
Author(s):
Wang Luyao12Zhao Kan12Huang Wei12Zhang Weihong3Shao Qingfeng1Wang Yongjin12
(1.MOE Key Laboratory of Virtual Geographic Environment,Nanjing Normal University,Nanjing 210023,China)(2.Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application,Nanjing 210023,China)(3.College of Geo
Keywords:
stalagmiteYounger Dryas eventmonsoon failureH1 event
PACS:
P532; P597.2
DOI:
10.3969/j.issn.1001-4616.2017.01.020
Abstract:
A 461-mm long stalagmite from Longfugong Cave in Hubei province,cenrtal China,was 230Th dated and measured with stable isotopic analysis to reconstruct a high-resolution(3 a)Asian Monsoon history over a period from 12.42 to 10.53 ka B.P.,equivalent to the Younger Dyras(YD)episode. The overall pattern of δ18O record,characterized by gradual onset but rapid end,agrees well with other high-resolution and precisely-dated speleothem records from Hulu,Yamen and Qingtian Caves. A positive shift of δ18O values from -8.6‰ to -7.9‰ at around 11.71 ka B.P.,which is also mirrored in the carbon isotope composition with δ13C values from -7.4‰ to -6.0‰,indicates a~200 a monsoon failure within the YD. The structures and transitions of YD event are equally registered by the δ18O record of the H1 event(Heinrich 1)from Hulu Cave,possibly implying the same forcing mechanism. The calcite δ18O record,which presents abrupt fluctuations and detailed instabilities in monsoon over the studied interval,shows coherence with ice-core δ18O record from Greenland,supporting the direct linkage between Greenland climate and monsoonal circulation. Based on the comparison with the bulk sedimentary titanium(Ti)records from the Cariaco Basin,we attribute the internal centennial monsoon failure to the southward displacement of the Intertropical Convergence Zone(ITCZ). The statistically significant periodicities of ~128 a(δ13C)and~200 a(δ18O)from the wavelet analysis likely indicate the role of solar activity playing in monsoon,and this is further supported by the 10Be flux record derived from ice core.

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