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.
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.
the Creative Commons Attribution 3.0 License.
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
CORRESPONDING AUTHOR
Coast Institute of Ludong University, Yantai 264025,
China
School of Geography, South China Normal University,
Guangzhou 510631, China
Ke Cheng
Coast Institute of Ludong University, Yantai 264025,
China
Hong Chi
Coast Institute of Ludong University, Yantai 264025,
China
Chuan-Chou Shen
High-precision Mass Spectrometry and Environment Change
Lab (HISPEC), Department of Geosciences, National Taiwan University, Taipei
10617, Taiwan, ROC
Changshan Wang
Coast Institute of Ludong University, Yantai 264025,
China
Qianqian Ma
Coast Institute of Ludong University, Yantai 264025,
China
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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.
The upper part of stalagmite ky1 (from top to 42.769 mm depth), consisting of 678 laminae, was...
