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...
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 |
Similar Items
-
Patterns of diversification in early eukaryotes
by: Javaux Emmanuelle J.
Published: (2007-03-01) -
Growth mechanisms and environmental implications of carbonate concretions from the ~ 1.4 Ga Xiamaling Formation, North China
by: An-Qi Liu, et al.
Published: (2019-05-01) -
East Greenland Caledonides: stratigraphy, structure and geochronology: The Neoproterozoic Rivieradal Group of Kronprins Christian Land, eastern North Greenland
by: Smith, M. Paul, et al.
Published: (2004-12-01) -
Chromium Isotope Systematics in Modern and Ancient Microbialites
by: Sylvie Bruggmann, et al.
Published: (2020-10-01) -
Age, geochemistry, and origin of the mid-Proterozoic Häme mafic dyke swarm, southern Finland
by: Arto Luttinen, et al.
Published: (2022-06-01)