A Pulsed Oxygenation in Terminal Paleoproterozoic Ocean: Evidence From the Transition Between the Chuanlinggou and Tuanshanzi Formations, North China

Abstract The mid‐Proterozoic (ca. 1.8–0.8 Ga) witnessed a period of stable carbon cycling and long stasis in eukaryotic evolution, which was commonly ascribed to the persistently low oxygen levels in the atmosphere‐ocean system. Recently, several pulsed marine oxygenations were identified from diffe...

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Bibliographic Details
Main Authors: Beilei Wei, Dongjie Tang, Xiaoying Shi, Maxwell Lechte, Limin Zhou, Xiqiang Zhou, Huyue Song
Format: Article
Language:English
Published: Wiley 2021-05-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2020GC009612