Stable isotopic evidence for microbial ethane in Lake Baikal gas hydrates

Авторы

  • A. Hachikubo 1
  • H. Kimura 1
  • R. Kamata 1
  • H. Sakagami 1
  • H. Minami 1
  • S. Yamashita 1
  • O. Khlystov 2
  • G. Kalmychkov 3
  • M. De Batist 4
  • 1 Kitami Institute of Technology, 165 Koen-cho, Kitami 090-8507, Japan
  • 2 Limnological Institute, Siberian Branch of the Russian Academy of Sciences, Ulan-Batorskaya Str., 3, Irkutsk 664033, Russia
  • 3 Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences, Favorsky Str., 1-a, Irkutsk 664033, Russia
  • 4 Renard Centre of Marine Geology, Ghent University, Krijgslaan 281s8, 9000, Ghent, Belgium

DOI:

https://doi.org/10.31951/2658-3518-2020-A-4-918

Ключевые слова:

gas hydrate, ethane, microbial gas, isotopic fractionation, gas origin

Аннотация

In the framework of Multi-phase Gas Hydrate Project, near-surface gas hydrates were retrieved from the southern and central Baikal basins. In this report, we summarize characteristics of hydrate-bound hydrocarbons retrieved at Lake Baikal and focus on hydrate-bound ethane and its gas origin. The information of molecular composition of volatile hydrocarbons and their stable isotopes showed that the origin of hydrate-bound gas distributes in the fields of microbial, thermogenic, and their mixed-gas. As for stable isotope of ethane, 13C and D distribute from 69 to 23 V-PDB, and from 313 to 185 V-SMOW, respectively. Light ethane in 13C also depleted in D, indicating that the isotopically light ethane depleted in 13C and D is generated by a microbial process, and the origin of hydrogen in ethane molecules is thought to be lake water, same as methane.

Опубликован

07.09.2020

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