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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- Triple oxygen isotope evidence for limited mid-Proterozoic primary productivity P. Crockford et al. 10.1038/s41586-018-0349-y
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- Proterozoic seawater sulfate scarcity and the evolution of ocean–atmosphere chemistry M. Fakhraee et al. 10.1038/s41561-019-0351-5
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25 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
- Mesoproterozoic paleo-redox changes during 1500–1400 Ma in the Yanshan Basin, North China X. Chen et al. 10.1016/j.precamres.2020.105835
- 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
- The Mesoproterozoic Oxygenation Event S. Zhang et al. 10.1007/s11430-020-9825-x
- Decoupled Cr, Mo, and U records of the Hongshuizhuang Formation, North China: Constraints on the Mesoproterozoic ocean redox X. Wang et al. 10.1016/j.marpetgeo.2021.105243
- Shallow-marine ironstones formed by microaerophilic iron-oxidizing bacteria in terminal Paleoproterozoic Y. Lin et al. 10.1016/j.gr.2019.06.004
- 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
- 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
- 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
- The formation of marine red beds and iron cycling on the Mesoproterozoic North China Platform D. Tang et al. 10.2138/am-2020-7406
- The environmental context of carbonaceous compressions and implications for organism preservation 1.40 Ga and 0.63 Ga F. Zhang et al. 10.1016/j.palaeo.2021.110449
- Highly fractionated chromium isotopes in Mesoproterozoic-aged shales and atmospheric oxygen D. Canfield et al. 10.1038/s41467-018-05263-9
- The Biomarkers in the Mesoproterozoic Organic‐rich Rocks of North China Craton: Implication for the Precursor and Preservation of Organism in the Prokaryotic Realm S. MA et al. 10.1111/1755-6724.14773
- Contrasting Mo–U enrichments of the basal Datangpo Formation in South China: Implications for the Cryogenian interglacial ocean redox Y. Ye et al. 10.1016/j.precamres.2018.07.013
- Manganese-rich deposits in the Mesoproterozoic Gaoyuzhuang Formation (ca. 1.58 Ga), North China Platform: Genesis and paleoenvironmental implications H. Fang et al. 10.1016/j.palaeo.2020.109966
- A transient swing to higher oxygen levels in the atmosphere and oceans at ~1.4 Ga W. Wei et al. 10.1016/j.precamres.2020.106058
- A paleosol record of the evolution of Cr redox cycling and evidence for an increase in atmospheric oxygen during the Neoproterozoic D. Colwyn et al. 10.1111/gbi.12360
- A Pulsed Oxygenation in Terminal Paleoproterozoic Ocean: Evidence From the Transition Between the Chuanlinggou and Tuanshanzi Formations, North China B. Wei et al. 10.1029/2020GC009612
- Heterogeneous oxygenation coupled with low phosphorus bio-availability delayed eukaryotic diversification in Mesoproterozoic oceans: Evidence from the ca 1.46 Ga Hongshuizhuang Formation of North China Q. Shi et al. 10.1016/j.precamres.2020.106050
- Mesoproterozoic oxygenated deep seawater recorded by early diagenetic carbonate concretions from the Member IV of the Xiamaling Formation, North China A. Liu et al. 10.1016/j.precamres.2020.105667
- Proterozoic seawater sulfate scarcity and the evolution of ocean–atmosphere chemistry M. Fakhraee et al. 10.1038/s41561-019-0351-5
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