Climate of the Past
Climate of the Past
CP
Articles | Volume 12, issue 4
Articles | Volume 12, issue 4
https://doi.org/10.5194/cp-12-871-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-871-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 12, issue 4
Research article
 | 
08 Apr 2016
Research article |  | 08 Apr 2016

The climate reconstruction in Shandong Peninsula, northern China, during the last millennium based on stalagmite laminae together with a comparison to δ18O

Qing Wang, Houyun Zhou, Ke Cheng, Hong Chi, Chuan-Chou Shen, Changshan Wang, and Qianqian Ma

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by Editor) (07 Dec 2015) by Dominik Fleitmann
AR by Qing Wang on behalf of the Authors (17 Dec 2015)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by Editor) (05 Jan 2016) by Dominik Fleitmann
AR by Qing Wang on behalf of the Authors (15 Jan 2016)  Author's response    Manuscript
ED: Publish as is (01 Feb 2016) by Dominik Fleitmann
AR by Qing Wang on behalf of the Authors (11 Feb 2016)  Author's response    Manuscript
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Short summary
The upper part of stalagmite ky1 (from top to 42.769 mm depth), consisting of 678 laminae, was collected from a cave in northern China, located in the East Asia monsoon area. The time of deposition ranges from AD 1217±20 to 1894±20. The analysis shows that both the variations in the thickness of the laminae themselves and the fluctuating degree of variation in the thickness of the laminae of stalagmite ky1 have obviously staged characteristics and synchronized with climate.
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