Constraining the Rate of Ocean Deoxygenation Leading to the End-Permian Mass Extinction: Toward a Multi-Isotope Tracer Approach
The 5th International Conference of Geobiology
Zhang Feifei Nanjing University
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Active shelf H2S oxidation after the Marinoan glaciation
The 5th International Conference of Geobiology
Zhao Kun Chengdu University of Technology
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Enzyme-like activities of ferrihydrite and birnessite and their supportive role in microorganism s tolerating ROS in iron-rich ancient ocean.
The 5th International Conference of Geobiology
Deng Haipeng 中国地质大学（武汉）,环境学院
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Biomechanical simulations unravel eumetazoans-type tissues from Ediacaran fronds
The 5th International Conference of Geobiology
Wang Zekun Natural History Museum
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Tempo of the Late Ordovician mass extinction controlled by the rate of climate change
The 5th International Conference of Geobiology
Yang Chuan Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences
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Microbial-dominated carbon burial: Insight from biomarker and isotopic studies in the Jiufotang Formation (NE China) during OAE1a
The 5th International Conference of Geobiology
ziyi Tang University of Chinese Academy of Sciences,Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
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Rethinking Microbialites in Extinction Events: Geochemical Modelling of Biomineralization in Extinctions
The 5th International Conference of Geobiology
Jia Tianyi Peking University
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Mineral-mediated Microbial Nutrient Acquisition: Insights from Biological Nitrogen Fixation and Enzymatic Organic Matter Decomposition
The 5th International Conference of Geobiology
Sheng Yizhi China University of Geosciences, Beijing
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The Great Unconformity in the Eastern North China Craton
The 5th International Conference of Geobiology
Wang Jiayue Nanjing University
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Preservation of Organic Matter Within Primary Fluid Inclusions in Late Middle Pleistocene Halite From the Mars Analog Qaidam Basin
The 5th International Conference of Geobiology
Huang Tongtong Institue of Geology and Geophysics, Chinese Academy of Scien
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