Intensified chemical weathering during the Permian-Triassic transition recorded in terrestrial and marine successions
Volume: 519, Pages: 166 - 177
Published: Apr 1, 2019
Abstract
Global warming is inferred to have been one of the main causes of the Permian-Triassic (P-Tr) boundary mass extinction. Although a strong temperature rise in tropical sea-surface temperatures during the latest Permian has been documented, coeval climate changes in terrestrial sections are less well-known. Here, we analyzed multiple weathering indexes (including CIA, CIW, and PIA) for two terrestrial sections in North China (Shichuanhe and Yima),...
Paper Details
Title
Intensified chemical weathering during the Permian-Triassic transition recorded in terrestrial and marine successions
Published Date
Apr 1, 2019
Volume
519
Pages
166 - 177
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