Toward the Origins of Quadruple Sulfur Isotope Anomalies in Modern Sulfate: A Multitracer Approach and Implications for Paleo- and Planetary Atmospheres-Reference-Cited by-同舟云学术

Toward the Origins of Quadruple Sulfur Isotope Anomalies in Modern Sulfate: A Multitracer Approach and Implications for Paleo- and Planetary Atmospheres

Published:2023-02-28 Issue:4 Volume:7 Page:800-811
ISSN:2472-3452
Container-title:ACS Earth and Space Chemistry
language:en
Short-container-title:ACS Earth Space Chem.

Author:

Yin Binyan¹²³,Yu Xiaoxiao¹²,Lin Xiaomin¹²,Zhang Zhisheng⁴,Zhang Yanli²⁵^ORCID,Lin Mang¹²³^ORCID

Affiliation:

1. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

2. CAS Center for Excellence in Deep Earth Science, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

3. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100039, China

4. South China Institute of Environmental Sciences, Ministry of Ecology and Environment, Guangzhou 510530, China

5. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Guangdong Pearl River Talents Program

Publisher

American Chemical Society (ACS)

Subject

Space and Planetary Science,Atmospheric Science,Geochemistry and Petrology

Link

https://pubs.acs.org/doi/pdf/10.1021/acsearthspacechem.2c00360

Reference61 articles.

1. Atmospheric Influence of Earth's Earliest Sulfur Cycle

2. The rise of oxygen in Earth’s early ocean and atmosphere

3. Use of Isotope Effects To Understand the Present and Past of the Atmosphere and Climate and Track the Origin of Life

4. Photochemistry of Sulfur Dioxide and the Origin of Mass-Independent Isotope Fractionation in Earth's Atmosphere

5. Observation of wavelength-sensitive mass-independent sulfur isotope effects during SO2photolysis: Implications for the early atmosphere

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