Increased precipitation and weathering across the Paleocene-Eocene Thermal Maximum in central China-Reference-Cited by-同舟云学术

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Increased precipitation and weathering across the Paleocene-Eocene Thermal Maximum in central China

Published:2016-06 Issue:6 Volume:17 Page:2286-2297
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Chen Zuoling¹,Ding Zhongli¹,Yang Shiling¹,Zhang Chunxia¹,Wang Xu¹

Affiliation:

1. Key Laboratory of Cenozoic Geology and Environment; Institute of Geology and Geophysics, Chinese Academy of Sciences; Beijing China

Funder

the Strategic Priority Research Program of the Chinese Academy of Sciences

the (973) National Basic Research Program of China

the China Postdoctoral Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference83 articles.

1. Late Cretaceous to early Paleocene climate and sea-level fluctuations: the Tunisian record;Adatte;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2002

2. Mineralogy and sedimentation of recent deep-sea clay in the Atlantic ocean and adjacent seas and oceans;Biscaye;Geol. Soc. Am. Bull.,1965

3. Palaeocene-early Eocene climatic evolution in the Tethyan realm: Clay mineral evidence;Bolle;Clay Miner.,2001

4. Persistent environmental change after the Paleocene-Eocene Thermal Maximum in the eastern North Atlantic;Bornemann;Earth Planet. Sci. Lett.,2014

5. Mechanisms of PETM global change constrained by a new record from central Utah;Bowen;Geology,2008

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