Articles | Volume 12, issue 4
Clim. Past, 12, 871–881, 2016
Clim. Past, 12, 871–881, 2016

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 et al.

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Manuscript not accepted for further review
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Cited articles

Baker, A., Smart, P. L, and Edwards, R. L.: Annual growth banding in a cave stalagmite, Nature, 364, 518–520, 1993.
Baker, A., Proetor, C. J., and Barnes, W. L.: Variations in stalagmite luminescence laminae structure at Pool's Cave, England, AD 1910–1996: Calibration of a palaeo precipitation proxy, The Holocene, 9, 683–688, 1999.
Baldini, J. U. L.: Cave atmosphere controls on stalagmite growth rate and palaeoclimate records. Geological Society, London, Special Publications, 336, 283–294, 2010.
Baldini, J. U. L., McDermott, F., Baker, A., Baldini, L. M., Mattey, D. P., and Railsback, L. B.: Biomass effects on stalagmite growth and isotope ratios: A 20th century analogue from Wiltshire, England, Earth Planet. Sci. Lett., 240, 486–494, 2005.
Ban, F. M., Pan, G. X., and Wang, X. Z.: Timing and possible mechanism of organic substances formation in stalagmites liminae from Beijing Shihua Cave, Quaternary Sci., 25, 265–268, 2005 (in Chinese with English Abstract).
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.