Early-Holocene monsoon instability and climatic optimum recorded by Chinese stalagmites/ (Record no. 12829)

MARC details
000 -LEADER
fixed length control field 02562nab a2200325 4500
005 - DATE & TIME
control field 20220817200415.0
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fixed length control field 220817b |||||||| |||| 00| 0 eng d
100 ## - MAIN ENTRY--PERSONAL NAME
Personal name Yang, Xunlin
245 ## - TITLE STATEMENT
Title Early-Holocene monsoon instability and climatic optimum recorded by Chinese stalagmites/
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Name of publisher, distributor, etc Sage,
Date of publication, distribution, etc 2019.
300 ## - PHYSICAL DESCRIPTION
Pages Vol 29, issue 6, 2019 : (1059-1067 p.).
520 ## - SUMMARY, ETC.
Summary, etc The timing and duration of the Holocene East Asian summer monsoon (EASM) maximum and the interpretation of Chinese stalagmite δ18O records have long been disputed. Notably, interpretations of Holocene EASM variations are frequently based on a single record or study area and are often contradictory. In this study, we conducted stable isotope analyses of four Holocene stalagmites from Chongqing, southwest China. The results reveal differences in the timing of the Holocene EASM maximum and to try to resolve the inconsistency we analyzed and statistically integrated a total of 16 Holocene stalagmite records from 14 caves in the EASM region. The resulting synthesized Holocene stalagmite δ18O (δ18Osyn) record is in agreement with other EASM records and confirms that stalagmite δ18O records are a valid indicator of EASM intensity, rather of local precipitation amount. The δ18Osyn record shows that the EASM intensified rapidly from the onset of the early Holocene; notably, however, there were distinct EASM oscillations in the early Holocene, consisting of three abrupt millennial-scale events. This indicates that, contrary to several previous interpretations, the early Holocene EASM was unstable. Subsequently, during 8–6 kyr BP, the EASM was relatively stable and strong, with the strongest monsoon occurring during 8–7 kyr BP. This evidence of a stable and strong mid-Holocene EASM in eastern China is in accord with the classical view of a mid-Holocene Optimum in China.
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Subject climatic optimum,
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Subject early Holocene,
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Subject East Asia,
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Subject millennial-scale events,
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Subject Stalagmite δ18O,
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Subject summer monsoon
700 ## - Added Entry Personal Name
Added Entry Personal Name Yang, Hong
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Added Entry Personal Name Wang, Baoyan
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Added Entry Personal Name Huang, Li-Jung
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Added Entry Personal Name Shen, Chuan-Chou
700 ## - Added Entry Personal Name
Added Entry Personal Name Edwards, R Lawrence
700 ## - Added Entry Personal Name
Added Entry Personal Name Cheng, Hai
773 0# - HOST ITEM ENTRY
Host Biblionumber 12756
Host Itemnumber 16504
Place, publisher, and date of publication London: Sage Publication Ltd, 2019.
Title Holocene/
International Standard Serial Number 09596836
856 ## - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier https://doi.org/10.1177/0959683619831433
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Koha item type Articles
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