Articles | Volume 14, issue 8
https://doi.org/10.5194/bg-14-2133-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-2133-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The oxic degradation of sedimentary organic matter 1400 Ma constrains atmospheric oxygen levels
Shuichang Zhang
CORRESPONDING AUTHOR
Key Laboratory of Petroleum Geochemistry, Research Institute of
Petroleum Exploration and Development, China National Petroleum Corporation,
Beijing 100083, China
Xiaomei Wang
Key Laboratory of Petroleum Geochemistry, Research Institute of
Petroleum Exploration and Development, China National Petroleum Corporation,
Beijing 100083, China
Huajian Wang
Key Laboratory of Petroleum Geochemistry, Research Institute of
Petroleum Exploration and Development, China National Petroleum Corporation,
Beijing 100083, China
Emma U. Hammarlund
Villum Investigator, Department of Biology and
NordCEE, University of Southern Denmark, Campusvej 55, 5230 Odense M,
Denmark
Jin Su
Key Laboratory of Petroleum Geochemistry, Research Institute of
Petroleum Exploration and Development, China National Petroleum Corporation,
Beijing 100083, China
Yu Wang
Key Laboratory of Petroleum Geochemistry, Research Institute of
Petroleum Exploration and Development, China National Petroleum Corporation,
Beijing 100083, China
Donald E. Canfield
Villum Investigator, Department of Biology and
NordCEE, University of Southern Denmark, Campusvej 55, 5230 Odense M,
Denmark
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44 citations as recorded by crossref.
- Paleoenvironmental proxies and what the Xiamaling Formation tells us about the mid‐Proterozoic ocean S. Zhang et al. 10.1111/gbi.12337
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- A transient oxygen increase in the Mesoproterozoic ocean at ∼1.44 Ga: Geochemical evidence from the Tieling Formation, North China Platform Y. Yu et al. 10.1016/j.precamres.2021.106527
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- Did high temperature rather than low O2 hinder the evolution of eukaryotes in the Precambrian? F. Zhang et al. 10.1016/j.precamres.2022.106755
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- Linking the rise of atmospheric oxygen to growth in the continental phosphorus inventory G. Cox et al. 10.1016/j.epsl.2018.02.016
- A Mesoproterozoic iron formation D. Canfield et al. 10.1073/pnas.1720529115
- Mineralogy of the 1.45 Ga Wafangzi manganese deposit in North China: Implications for pulsed Mesoproterozoic oxygenation events H. Yan et al. 10.2138/am-2022-8919
- Triple oxygen isotope evidence for limited mid-Proterozoic primary productivity P. Crockford et al. 10.1038/s41586-018-0349-y
- Petrographic carbon in ancient sediments constrains Proterozoic Era atmospheric oxygen levels D. Canfield et al. 10.1073/pnas.2101544118
- Hydrocarbon generation characteristics and exploration prospects of Proterozoic source rocks in China W. Zhao et al. 10.1007/s11430-018-9312-4
- A pulse of oxygen increase in the early Mesoproterozoic ocean at ca. 1.57–1.56 Ga M. Shang et al. 10.1016/j.epsl.2019.115797
- Vanadium Speciation in Ancient Shales Revealed through Synchrotron-Based X-ray Spectroscopy W. Bennett et al. 10.1021/acsearthspacechem.2c00308
- Growth mechanisms and environmental implications of carbonate concretions from the ~ 1.4 Ga Xiamaling Formation, North China A. Liu et al. 10.1186/s42501-019-0036-4
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- The formation of marine red beds and iron cycling on the Mesoproterozoic North China Platform D. Tang et al. 10.2138/am-2020-7406
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