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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Cited
15 citations as recorded by crossref.
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- Variations of monsoonal rain and vegetation during the past millennium in Tiangui Mountain, North China reflected by stalagmite δ18O and δ13C records from Zhenzhu Cave J. Yin et al. 10.1016/j.quaint.2017.06.039
- Large earthquakes and tsunamis recorded in limestone caves K. Yoshimura et al. 10.4116/jaqua.58.195
- Stalagmite flooding frequency record since the middle Little Ice Age from Central China L. Yuhui & L. Zhiling 10.1007/s10584-021-02977-6
- Climate change and society in the 15th to 18th centuries D. Degroot 10.1002/wcc.518
- Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071
- A new speleothem record of the penultimate deglacial: Insights into spatial variability and centennial-scale instabilities of East Asian monsoon G. Xue et al. 10.1016/j.quascirev.2019.02.023
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- Different response of trace elements in the drip-water of Kaiyuan Cave on Shandong Peninsula (coastal North China) to hydroclimatic changes from 2012 to 2014 K. Cheng et al. 10.1016/j.jhydrol.2022.127616
- The Link between ENSO-like Forcing and Hydroclimate Variability of Coastal East Asia during the Last Millennium J. Park et al. 10.1038/s41598-017-08538-1
- A comparison of growth rate of late Holocene stalagmites with atmospheric precipitation and temperature, and its implications for paleoclimatology L. Railsback 10.1016/j.quascirev.2018.03.002
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. 10.3390/quat2030026
- Speleothem‐Based Hydroclimate Reconstructions During the Penultimate Deglaciation in Northern China G. Xue et al. 10.1029/2020PA004072
- Separation of the Asian summer monsoon and local precipitation from stalagmite oxygen isotope records in Eastern China during the last millennium Z. Hu et al. 10.1016/j.quascirev.2023.108498
- Geomorphologic evolution of the shallow-buried abandoned Yellow River delta during the last 2000 years Q. Wang et al. 10.3389/fmars.2022.1073961
14 citations as recorded by crossref.
- Potential for limestone caves and their sediments as an onshore archive : A key to reading paleo-environment and human history Y. Ishihara & S. Yamasaki 10.4116/jaqua.62.2215
- Variations of monsoonal rain and vegetation during the past millennium in Tiangui Mountain, North China reflected by stalagmite δ18O and δ13C records from Zhenzhu Cave J. Yin et al. 10.1016/j.quaint.2017.06.039
- Large earthquakes and tsunamis recorded in limestone caves K. Yoshimura et al. 10.4116/jaqua.58.195
- Stalagmite flooding frequency record since the middle Little Ice Age from Central China L. Yuhui & L. Zhiling 10.1007/s10584-021-02977-6
- Climate change and society in the 15th to 18th centuries D. Degroot 10.1002/wcc.518
- Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071
- A new speleothem record of the penultimate deglacial: Insights into spatial variability and centennial-scale instabilities of East Asian monsoon G. Xue et al. 10.1016/j.quascirev.2019.02.023
- Sequence stratigraphy in the Middle Ordovician carbonate successions (Yeongheung Formation), mid-east Korea: Paleogeographic implications for a land-detached ramp-type platform Y. Kwon & Y. Kwon 10.1016/j.jseaes.2020.104263
- Different response of trace elements in the drip-water of Kaiyuan Cave on Shandong Peninsula (coastal North China) to hydroclimatic changes from 2012 to 2014 K. Cheng et al. 10.1016/j.jhydrol.2022.127616
- The Link between ENSO-like Forcing and Hydroclimate Variability of Coastal East Asia during the Last Millennium J. Park et al. 10.1038/s41598-017-08538-1
- A comparison of growth rate of late Holocene stalagmites with atmospheric precipitation and temperature, and its implications for paleoclimatology L. Railsback 10.1016/j.quascirev.2018.03.002
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. 10.3390/quat2030026
- Speleothem‐Based Hydroclimate Reconstructions During the Penultimate Deglaciation in Northern China G. Xue et al. 10.1029/2020PA004072
- Separation of the Asian summer monsoon and local precipitation from stalagmite oxygen isotope records in Eastern China during the last millennium Z. Hu et al. 10.1016/j.quascirev.2023.108498
1 citations as recorded by crossref.
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Latest update: 21 Nov 2024
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...
