Controlling factors in stalagmite oxygen isotopic composition and the paleoprecipitation record for the last 1,100 years in Northeast Japan-Reference-Cited by-同舟云学术

Controlling factors in stalagmite oxygen isotopic composition and the paleoprecipitation record for the last 1,100 years in Northeast Japan

Published:2016 Issue:2 Volume:50 Page:e1-e6
ISSN:0016-7002
Container-title:GEOCHEMICAL JOURNAL
language:en
Short-container-title:Geochem. J.

Author:

Kato Hirokazu¹,Yamada Tsutomu¹

Affiliation:

1. Graduate School of Science, Tohoku University

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Link

https://www.jstage.jst.go.jp/article/geochemj/50/2/50_2.0417/_pdf

Reference29 articles.

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2. Baker, A., Asrat, A., Fairchild, I. J., Leng, M. J., Wynn, P. M., Bryant, C., Genty, D. and Umer, M. (2007) Analysis of the climate signal contained within δ¹⁸O and growth rate parameters in two Ethiopian stalagmites. Geochim. Cosmochim. Acta 71, 2975–2988.

3. Cai, B., Pumijumnong, N., Tan, M., Muangsong, C., Kong, X., Jiang, X. and Nan, S. (2010) Effects of intraseasonal variation of summer monsoon rainfall on stable isotope and growth rate of a stalagmite from northwestern Thailand. J. Geophys. Res. 115, D21104, doi:10.1029/2009JD013378.

4. Dansgaard, W. (1964) Stable isotopes in precipitation. Tellus 16, 436–468.

5. Fairchild, I. J. and Baker, A. (2012) Speleothem Science. Wiley-Blackwell, 432 pp.

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