Tree rings and ice cores reveal 14C calibration uncertainties during the Younger Dryas-Reference-Cited by-同舟云学术

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Tree rings and ice cores reveal 14C calibration uncertainties during the Younger Dryas

Published:2008-03-09 Issue:4 Volume:1 Page:263-267
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Muscheler R.,Kromer B.,Björck S.,Svensson A.,Friedrich M.,Kaiser K. F.,Southon J.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo128.pdf

Reference49 articles.

1. Dansgaard, W., White, J. W. C. & Johnsen, S. J. The abrupt termination of the younger dryas climate event. Nature 339, 532–534 (1989).

2. Björck, S. et al. An event stratigraphy for the last termination in the North Atlantic region based on the Greenland ice-core record: A proposal by the INTIMATE group. J. Quatern. Sci. 13, 283–292 (1998).

3. Litt, T. et al. Correlation and synchronisation of Lateglacial continental sequences in northern central Europe based on annually laminated lacustrine sediments. Quat. Sci. Rev. 20, 1233–1249 (2001).

4. Wang, Y. J. et al. A high-resolution absolute-dated late pleistocene monsoon record from Hulu Cave, China. Science 294, 2345–2348 (2001).

5. Hughen, K. A., Overpeck, J. T., Peterson, L. C. & Trumbore, S. Rapid climate changes in the tropical Atlantic region during the last deglaciation. Nature 380, 51–54 (1996).

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