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JOURNAL ARTICLE
Large perturbations of the carbon and sulfur cycle associated with the Late Ordovician mass extinction in South China
Tonggang Zhang
Tonggang Zhang
1
Canada Research Chairs Program in Biogeochemistry, University of Quebec at Montreal, Montreal, QC H3C 3P8, Canada
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Yanan Shen
Yanan Shen
1
Canada Research Chairs Program in Biogeochemistry, University of Quebec at Montreal, Montreal, QC H3C 3P8, Canada *E-mail: shen.yanan@uqam.ca.
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Renbin Zhan
Renbin Zhan
2
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 21008, China
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Shuzhong Shen
Shuzhong Shen
2
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 21008, China
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Xu Chen
Xu Chen
2
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 21008, China
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Geology (2009) 37 (4): 299-302.
Published:
April 01, 2009
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Tonggang Zhang, Yanan Shen, Renbin Zhan, Shuzhong Shen, Xu Chen; Large perturbations of the carbon and sulfur cycle associated with the Late Ordovician mass extinction in South China. Geology ; 37 (4): 299–302. doi: https://doi.org/10.1130/G25477A.1
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Index Terms/Descriptors
- anaerobic environment
- ancient ice ages
- Ashgillian
- Asia
- biostratigraphy
- biozones
- C-13/C-12
- carbon
- carbon cycle
- chemostratigraphy
- China
- deep-water environment
- Far East
- geochemical cycle
- geochemistry
- glaciation
- Graptolithina
- Guizhou China
- Hirnantian
- isotope ratios
- isotopes
- lithostratigraphy
- Lower Silurian
- mass extinctions
- Ordovician
- organic carbon
- paleo-oceanography
- paleoclimatology
- paleoecology
- Paleozoic
- pyrite
- S-34/S-32
- sea-level changes
- Silurian
- stable isotopes
- sulfides
- sulfur
- sulfur cycle
- Upper Ordovician
- variations
- southern China
- Tongzi China
- Honghuayuan China
Latitude & Longitude
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