Decoding Redox Evolution Before Oxygenic Photosynthesis Based on the Sulfur-Mass Independent Fractionation (S-MIF) Record

被引：4

作者：

Ueno, Yuichiro ^{[1
,2
,3
]}

Danielache, Sebastian ^{[4
]}

Yoshida, Naohiro ^{[2
,5
]}

机构：

[1] Tokyo Inst Technol, Dept Earth & Planetary Sci, Meguro Ku, Tokyo 1528551, Japan

[2] Tokyo Inst Technol, Earth Life Sci Inst WPI ELSI, Meguro Ku, Tokyo 1528551, Japan

[3] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Precambrian Ecosyst Lab, Yokosuka, Kanagawa 2370061, Japan

[4] Sophia Univ, Fac Sci & Technol, Chiyoda Ku, Tokyo 1028554, Japan

[5] Tokyo Inst Technol, Dept Environm Chem & Engn, Midori Ku, Yokohama, Kanagawa 2268502, Japan

来源：

ORIGINS OF LIFE AND EVOLUTION OF BIOSPHERES | 2015年 / 45卷 / 03期

关键词：

Mass Independent Fractionation; Early atmosphere; ATMOSPHERIC SULFUR; ISOTOPES; PHOTOLYSIS;

D O I：

10.1007/s11084-015-9447-0

中图分类号：

Q [生物科学];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

The isotopic anomaly of stable sulfur isotope could be a useful new tracer for decoding atmospheric chemistry of early Earth from ancient rock samples. Here, we summarize current status of the experimental works and discuss what the isotopic anomaly tells about early Earth's atmosphere.

引用

页码：371 / 374

页数：4