Interaction of Biogeochemical Sulfur and Carbon Cycles in Marine Basins by the Example of the Black Sea
- Авторлар: Lein A.Y.1, Ivanov M.V.2
-
Мекемелер:
- Shirshov Institute of Oceanology
- Russian Federation Federal Research Centre “Fundamentals of Biotechnology” of the Russian Academy of Sciences
- Шығарылым: Том 481, № 1 (2018)
- Беттер: 939-942
- Бөлім: Geochemistry
- URL: https://journal-vniispk.ru/1028-334X/article/view/193695
- DOI: https://doi.org/10.1134/S1028334X18070243
- ID: 193695
Дәйексөз келтіру
Аннотация
The interaction of biogeochemical sulfur and carbon cycles in water bodies has been studied by the different authors and methods, including the use of 35S and 14C radioactive tracers. The main reactions of sulfur and carbon interaction by the example of the Black Sea (sulfate reduction, methanogenesis, aerobic and anaerobic methane oxidation) are considered. Based on the experimental radioisotope data, the annual microbial production of H2S and CH4 in the water column of the Black Sea is estimated. The average annual production of CH4 is 3.8% of the annual production of H2S. The share of migration methane from the bottom sediments (seeps, mud volcanoes, etc.) is approximately 2% of the total dissolved methane pool.
Авторлар туралы
A. Lein
Shirshov Institute of Oceanology
Хат алмасуға жауапты Автор.
Email: lein@ocean.ru
Ресей, Moscow, 117218
M. Ivanov
Russian Federation Federal Research Centre “Fundamentals of Biotechnology” of the Russian Academy of Sciences
Email: lein@ocean.ru
Ресей, Moscow
Қосымша файлдар
