Isotopes of hydrogen and oxygen in nitrogen hot springs of Baikal Rift Zone in terms of interaction in the water-rock system

2012 ◽  
Vol 442 (1) ◽  
pp. 81-85 ◽  
Author(s):  
L. V. Zamana
2017 ◽  
Author(s):  
Svetlana V. Zaitseva ◽  
Elena V. Lavrentieva ◽  
Aryuna A. Radnagurueva ◽  
Olga A. Baturina ◽  
Marsel R. Kabilov ◽  
...  

Alkaline hot springs are unique extreme habitats resemble the early Earth and present a valuable resource for the discovery of procaryotic community diversity and isolation of the novel thermophilic Bacteria and Archaea. One of the model for the possible origin of biochemistry in alkaline hot springs revealed the acetyl-CoA pathway of CO2 fixation might be the most ancient form of carbon metabolism. Recent phylogenetic studies have suggested that the phylum Acetothermia is one of the deep branches of the Bacteria domain. Firstly Acetothermia (Candidate division OP1) was characterized in a culture independent molecular phylogenetic survey based on the 16S rRNA gene of the sulfide-rich hot spring, Obsidian Pool, a 75 to 95oC hot spring. Two nearly complete genomes of Acetothermia were established based on genome-resolved metagenomic analysis and its capability of implementing acetogenesis through the ancient reductive acetyl-CoA pathway by utilizing CO2 and H2 was revealed. Although genomic, proteomic and metagenomic approaches investigate basic metabolism and potentional energy conservation of uncultivated candidate phyla but ecological roles of these bacteria and general patterns of diversity and community structure stay unclear. General hydrochemical and geological characterization of alkaline thermal springs of the Baikal Rift zone with high silica concentrations and a nitrogen dominated gas phase is provided. Previous microbiogical studies based on culture-dependent methods recovered a large number of bacterial strains from thermal springs located in Baikal Rift zone. We combined microbial communities analysis by using high-throughput 16S rRNA gene sequencing, biogeochemical measurements, sediment mineralogy and physicochemical characteristics to investigate ecosystems of alkaline hot springs located in the Baikal Rift zone. Uncultivated bacteria belonging to the phylum Acetothermia, along with members of the phyla Firmicutes and Proteobacteria, were identified as the dominant group in hydrothermal sediments communities in the alkaline hot springs of Baikal Rift zone. In bottom sediments of the Alla hot spring, about 57% of all classified sequences represent this phylum. Geochemistry of fluids and sample type were strongly correlated with microbial community composition. The Acetothermia exhibited the highest relative abundance in sediment microbial community associated with alkaline thermal fluids enriched in Fe, Zn, Ni, Al and Cr.


2007 ◽  
Vol 412 (1) ◽  
pp. 101-105 ◽  
Author(s):  
E. V. Sklyarov ◽  
V. S. Fedorovskii ◽  
O. A. Sklyarova ◽  
T. M. Skovitina ◽  
Yu. V. Danilova ◽  
...  

2021 ◽  
Vol 908 (1) ◽  
pp. 012001
Author(s):  
D D Barkhutova ◽  
S P Buryukhaev ◽  
V B Dambaev ◽  
D D Tsyrenova ◽  
E V Lavrentyeva

Abstract The Baikal Rift Zone hosts many hot springs with a wide range of temperature and physical-chemical conditions, which may harbour different niches for the distribution of microbial communities. We investigated microbial community composition and their functional activity in two alkaline hot springs with a temperature range of 34.4 to 73.6°C. Comparative analysis of the composition of the dominant taxa showed significant differences depending on the collection sites. In the community of high-temperature zones with a water temperature of 55-64°C, a high proportion of thermophilic bacteria Acetothermia (up to 57.9%), Deinococcus-Thermus (up to 50%), and Aquificae (up to 10.8%). Proteobacteria (29-77%) and Firmicutes (15-26%) dominate in the sulphide-free Garga spring (73-75°C). The functional analysis of the microbial community showed that the primary producers are cyanobacteria, anoxygenic phototrophs, and chemolithotrophic bacteria. At the terminal stages of the mineralization of organic matter, sulphate-reducing bacteria are the main destructors in the microbial communities in hot springs. The cyano-bacterial and sulfidogenic microbial communities play an important role in the formation of geochemical barriers and mineral formation.


Microbiology ◽  
2018 ◽  
Vol 87 (2) ◽  
pp. 272-281 ◽  
Author(s):  
E. V. Lavrentyeva ◽  
A. A. Radnagurueva ◽  
D. D. Barkhutova ◽  
N. L. Belkova ◽  
S. V. Zaitseva ◽  
...  

2021 ◽  
Vol 44 (2) ◽  
pp. 159-166
Author(s):  
S. Kh. Pavlov

The purpose of the work is to study the effect of organic matter on the formation of ion-salt and gas composition of nitrogen-methane and methane thermal water occurring in the sedimentary rocks of deep horizons of artesian basins. The object of research is the Tunka intermountain artesian basin of the Baikal rift zone and the Tungor gas and oil field of the Okhotsk-Sakhalin basin, in the deep horizons of which soda (inversion) low- and high-mineralized groundwater is common. The study combines the results of the traditional study of the composition of natural solutions and the quantitative research of physical and chemical interactions in the “water – rock” system conducted using the Selector software package according to the degree of the hydrogeochemical process, which was set by the value of the rock/water ratio. Chemically pure water and rocks of medium chemical composition were used in interaction. With the use of physicochemical modeling the formation of thermal water composition in sedimentary rocks depending on the interaction degree between water and rock and the amount of organic matter was unravelled. As a result, it was determined that the organic matter present in the rock has the dominant influence on the intensity of the hydrogeochemical process determining the amount of mineralization, the ratio of components, and the amount of methane, nitrogen, and carbon dioxide produced. The correspondent compositions of the model and natural solutions showed the possibility to form low- and high-mineralized sodium bicarbonate groundwater of different gas-saturation degree in the conditions of deep horizons of sedimentary basins due to the internal reserves of the “water – rock” system not involving any components from external sources.


Author(s):  
Svetlana V. Zaitseva ◽  
Elena V. Lavrentieva ◽  
Aryuna A. Radnagurueva ◽  
Olga A. Baturina ◽  
Marsel R. Kabilov ◽  
...  

Alkaline hot springs are unique extreme habitats resemble the early Earth and present a valuable resource for the discovery of procaryotic community diversity and isolation of the novel thermophilic Bacteria and Archaea. One of the model for the possible origin of biochemistry in alkaline hot springs revealed the acetyl-CoA pathway of CO2 fixation might be the most ancient form of carbon metabolism. Recent phylogenetic studies have suggested that the phylum Acetothermia is one of the deep branches of the Bacteria domain. Firstly Acetothermia (Candidate division OP1) was characterized in a culture independent molecular phylogenetic survey based on the 16S rRNA gene of the sulfide-rich hot spring, Obsidian Pool, a 75 to 95oC hot spring. Two nearly complete genomes of Acetothermia were established based on genome-resolved metagenomic analysis and its capability of implementing acetogenesis through the ancient reductive acetyl-CoA pathway by utilizing CO2 and H2 was revealed. Although genomic, proteomic and metagenomic approaches investigate basic metabolism and potentional energy conservation of uncultivated candidate phyla but ecological roles of these bacteria and general patterns of diversity and community structure stay unclear. General hydrochemical and geological characterization of alkaline thermal springs of the Baikal Rift zone with high silica concentrations and a nitrogen dominated gas phase is provided. Previous microbiogical studies based on culture-dependent methods recovered a large number of bacterial strains from thermal springs located in Baikal Rift zone. We combined microbial communities analysis by using high-throughput 16S rRNA gene sequencing, biogeochemical measurements, sediment mineralogy and physicochemical characteristics to investigate ecosystems of alkaline hot springs located in the Baikal Rift zone. Uncultivated bacteria belonging to the phylum Acetothermia, along with members of the phyla Firmicutes and Proteobacteria, were identified as the dominant group in hydrothermal sediments communities in the alkaline hot springs of Baikal Rift zone. In bottom sediments of the Alla hot spring, about 57% of all classified sequences represent this phylum. Geochemistry of fluids and sample type were strongly correlated with microbial community composition. The Acetothermia exhibited the highest relative abundance in sediment microbial community associated with alkaline thermal fluids enriched in Fe, Zn, Ni, Al and Cr.


Microbiology ◽  
2016 ◽  
Vol 85 (3) ◽  
pp. 367-378 ◽  
Author(s):  
A. A. Radnagurueva ◽  
E. V. Lavrentieva ◽  
V. G. Budagaeva ◽  
D. D. Barkhutova ◽  
Y. E. Dunaevsky ◽  
...  

2010 ◽  
Vol 435 (1) ◽  
pp. 1515-1517 ◽  
Author(s):  
L. V. Zamana ◽  
Sh. A. Askarov ◽  
S. V. Borzenko ◽  
O. V. Chudaev ◽  
I. V. Bragin

2010 ◽  
Vol 430 (2) ◽  
pp. 218-222 ◽  
Author(s):  
E. V. Lazareva ◽  
A. V. Bryanskaya ◽  
S. M. Zhmodik ◽  
S. Z. Smirnov ◽  
O. P. Pestunova ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document