Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy of the Ediacaran Lantian Formation in South China: Spatial gradient, ocean redox oscillation, and fossil distribution-Reference-Cited by-同舟云学术

Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy of the Ediacaran Lantian Formation in South China: Spatial gradient, ocean redox oscillation, and fossil distribution

Published:2017-01-06 Issue:4 Volume:15 Page:552-571
ISSN:1472-4677
Container-title:Geobiology
language:en
Short-container-title:Geobiology

Author:

Wang W.¹²,Guan C.¹,Zhou C.¹,Peng Y.³,Pratt L. M.⁴,Chen X.⁵,Chen L.⁶,Chen Z.⁵,Yuan X.⁵,Xiao S.²

Affiliation:

1. Key Laboratory of Economic Stratigraphy and Palaeogeography Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences Nanjing China

2. Department of Geosciences Virginia Tech Blacksburg VA USA

3. Department of Geology and Geophysics Louisiana State University Baton Rouge LA USA

4. Department of Geological Sciences Indiana University Bloomington IN USA

5. State Key Laboratory of Palaeobiology and Stratigraphy Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences Nanjing China

6. College of Earth Science and Engineering Shandong University of Science and Technology Qingdao Shandong China

Funder

Chinese Academy of Sciences

Ministry of Science and Technology of the People's Republic of China

National Natural Science Foundation of China

Natural Science Foundation of Jiangsu Province

National Science Foundation

National Aeronautics and Space Administration

Publisher

Wiley

Subject

General Earth and Planetary Sciences,General Environmental Science,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gbi.12226

Reference108 articles.

1. A multilayered water column in the Ediacaran Yangtze platform? Insights from carbonate and organic matter paired δ13C

2. Ocean redox structure across the Late Neoproterozoic Oxygenation Event: A nitrogen isotope perspective

3. Isotopic Tracers of the Marine Nitrogen Cycle: Present and Past

4. Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization

5. Calculation of simultaneous isotopic and trace element variations during water-rock interaction with applications to carbonate diagenesis

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