The contribution of Asian dust in the pedogenesis of ultisols in Southeastern China determined by soil grain size-Reference-Cited by-同舟云学术

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The contribution of Asian dust in the pedogenesis of ultisols in Southeastern China determined by soil grain size

Published:2018-05-24 Issue:1 Volume:19 Page:232-240
ISSN:1439-0108
Container-title:Journal of Soils and Sediments
language:en
Short-container-title:J Soils Sediments

Author:

Li Jianwu,Song Zhaoliang,Ruan Li,Yang Lihui,Van Zwieten Lukas,Hu Zhongchen,He Shengjia,Chenwu Wentao,Wang Hailong

Publisher

Springer Science and Business Media LLC

Subject

Stratigraphy,Earth-Surface Processes

Link

http://link.springer.com/article/10.1007/s11368-018-2012-5/fulltext.html

Reference52 articles.

1. An ZS (2000) The history and variability of the East Asian monsoon. Quat Sci Rev 19:171–187

2. Borg LE, Banner JL (1996) Neodymium and strontium isotopic constraints on soil sources in Barbados, West Indies. Geochim Cosmochim Acta 60:4193–4206

3. Chadwick OA, Derry LA, Vitousek PM, Huebert BJ, Hedin LO (1999) Changing sources of nutrients during four million years of ecosystem development. Nature 397:491–497

4. Chinese Soil Taxonomy Research Group (2001) Chinese soil taxonomy. Science Press, Beijing

5. Ding ZL, Xiong SF, Sun JM, Yang SL, Gu ZY, Liu TS (1999) Pedostratigraphy and paleomagnetism of a 70 Ma eolian loess–red clay sequence at Lingtai, loess plateau, north-central China and the implications for paleomonsoon evolution. Paleogeogr Paleoclimatol Paleoecol 152:49–66

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3. Loess in eastern equatorial Pangea archives a dusty atmosphere and possible upland glaciation;GSA Bulletin;2020-06-19

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