Ratios of Sulfur Isotopes (32S, 33S, 34S, and 36S) in Archean Rocks of Karelia: Evidence of Microbial Life and the Anoxic Atmosphere

被引：1

作者：

Velivetskaya, T. A. ^{[1
]}

Ignatiev, A. V. ^{[1
]}

Vysotskiy, S. V. ^{[1
]}

Aseeva, A. V. ^{[1
]}

机构：

[1] Russian Acad Sci, Far Eastern Branch, Far Eastern Geol Inst, Pr 100 Letiya Vladivostoka 159, Vladivostok 690022, Russia

来源：

RUSSIAN GEOLOGY AND GEOPHYSICS | 2024年 / 65卷 / 06期

基金：

俄罗斯科学基金会;

关键词：

sulfur isotope ratios; Archean atmosphere; sedimentary sulfides; bacteria; Karelia; MASS-INDEPENDENT FRACTIONATION; BACTERIAL SULFATE REDUCTION; 125; DEGREES-C; PYRITE FORMATION; GREENSTONE-BELT; AQUEOUS-SOLUTIONS; ELEMENTAL SULFUR; SO2; PHOTOLYSIS; IRON-FORMATION; BALTIC SHIELD;

D O I：

10.2113/RGG20234602

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

--We have studied sulfur isotope ratios (S-32, S-33, S-34, and S-36) archived in the volcanic and ferruginous rocks of the Sumozero-Kenozero (ca. 2.9 Ga) and Kostomuksha (ca. 2.7 Ga) greenstone belts of the Fennoscandian Shield. The obtained data provide new arguments for developing ideas of the bacterial activity in the Archean ocean and the involvement of sulfur in the biogenic cycle and also indicate no free oxygen in the Archean Earth's atmosphere. The isotope data on S-34 and S-33 show a high activity of sulfate-reducing and sulfur-disproportionating bacteria in the surface environments of Archean sedimentary rocks. The discovery of S-33 and S-36 anomalies in the studied rocks is the main evidence for the anoxic atmosphere during the formation of Meso- and Neoarchean deposits in Karelia.

引用

页码：689 / 698

页数：10

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