Increased precipitation during the Little Ice Age in northern Taiwan inferred from diatoms and geochemistry in a sediment core from a subalpine lake-Reference-Cited by-同舟云学术

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Increased precipitation during the Little Ice Age in northern Taiwan inferred from diatoms and geochemistry in a sediment core from a subalpine lake

Published:2013-01-22 Issue:4 Volume:49 Page:619-631
ISSN:0921-2728
Container-title:Journal of Paleolimnology
language:en
Short-container-title:J Paleolimnol

Author:

Wang Liang-Chi,Behling Hermann,Lee Teh-Quei,Li Hong-Chun,Huh Chih-An,Shiau Liang-Jian,Chen Su-Hwa,Wu Jiunn-Tzong

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Aquatic Science

Link

http://link.springer.com/content/pdf/10.1007/s10933-013-9679-9.pdf

Reference64 articles.

1. An Z, Porter SC, Kutzbach JE, Wu X, Wang S, Liu X, Li X, Zhou W (2000) Asynchronous Holocene optimum of the East Asian monsoon. Quat Sci Rev 19:743–762

2. Atwater B, Furukawa R, Hemphill-Haley E, Ikeda Y, Kashima K, Kawase K, Kelsey H, Moore A, Nanayama F, Nishimura Y (2004) Seventeenth-century uplift in eastern Hokkaido, Japan. Holocene 14:487

3. Bard E, Raisbeck G, Yiou F, Jouzel J (2000) Solar irradiance during the last 1200 years based on cosmogenic nuclides. Tellus B 52:985–992

4. Binford M (1990) Calculation and uncertainty analysis of 210Pb dates for PIRLA project lake sediment cores. J Paleolimnol 3:253–267

5. Birks HJB (1998) D.G. Frey and E.S. Deevey Review #1: numerical tools in palaeolimnology—progress, potentialities, and problems. J Paleolimnol 20:307–332

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