Early-Holocene monsoon instability and climatic optimum recorded by Chinese stalagmites/ (Record no. 12829)
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| 000 -LEADER | |
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| fixed length control field | 02562nab a2200325 4500 |
| 005 - DATE & TIME | |
| control field | 20220817200415.0 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| 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. |
| 650 ## - Subject | |
| Subject | climatic optimum, |
| 650 ## - Subject | |
| Subject | early Holocene, |
| 650 ## - Subject | |
| Subject | East Asia, |
| 650 ## - Subject | |
| Subject | millennial-scale events, |
| 650 ## - Subject | |
| Subject | Stalagmite δ18O, |
| 650 ## - Subject | |
| Subject | summer monsoon |
| 700 ## - Added Entry Personal Name | |
| Added Entry Personal Name | Yang, Hong |
| 700 ## - Added Entry Personal Name | |
| Added Entry Personal Name | Wang, Baoyan |
| 700 ## - Added Entry Personal Name | |
| Added Entry Personal Name | Huang, Li-Jung |
| 700 ## - Added Entry Personal Name | |
| 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 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Koha item type | Articles |
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| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| -- | ddc |
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