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Biodiversity of the microbial mat of the Garga hot spring. / Rozanov, Alexey Sergeevich; Bryanskaya, Alla Victorovna; Ivanisenko, Timofey Vladimirovich et al.

In: BMC Evolutionary Biology, Vol. 17, No. Suppl 2, 254, 28.12.2017, p. 254.

Research output: Contribution to journalArticlepeer-review

Harvard

Rozanov, AS, Bryanskaya, AV, Ivanisenko, TV, Malup, TK & Peltek, SE 2017, 'Biodiversity of the microbial mat of the Garga hot spring', BMC Evolutionary Biology, vol. 17, no. Suppl 2, 254, pp. 254. https://doi.org/10.1186/s12862-017-1106-9

APA

Rozanov, A. S., Bryanskaya, A. V., Ivanisenko, T. V., Malup, T. K., & Peltek, S. E. (2017). Biodiversity of the microbial mat of the Garga hot spring. BMC Evolutionary Biology, 17(Suppl 2), 254. [254]. https://doi.org/10.1186/s12862-017-1106-9

Vancouver

Rozanov AS, Bryanskaya AV, Ivanisenko TV, Malup TK, Peltek SE. Biodiversity of the microbial mat of the Garga hot spring. BMC Evolutionary Biology. 2017 Dec 28;17(Suppl 2):254. 254. doi: 10.1186/s12862-017-1106-9

Author

Rozanov, Alexey Sergeevich ; Bryanskaya, Alla Victorovna ; Ivanisenko, Timofey Vladimirovich et al. / Biodiversity of the microbial mat of the Garga hot spring. In: BMC Evolutionary Biology. 2017 ; Vol. 17, No. Suppl 2. pp. 254.

BibTeX

@article{b4b16a63a9c8451d9503ab1096337bab,
title = "Biodiversity of the microbial mat of the Garga hot spring",
abstract = "Background: Microbial mats are a good model system for ecological and evolutionary analysis of microbial communities. There are more than 20 alkaline hot springs on the banks of the Barguzin river inflows. Water temperature reaches 75 °C and pH is usually 8.0-9.0. The formation of microbial mats is observed in all hot springs. Microbial communities of hot springs of the Baikal rift zone are poorly studied. Garga is the biggest hot spring in this area. Results: In this study, we investigated bacterial and archaeal diversity of the Garga hot spring (Baikal rift zone, Russia) using 16S rRNA metagenomic sequencing. We studied two types of microbial communities: (i) small white biofilms on rocks in the points with the highest temperature (75 °C) and (ii) continuous thick phototrophic microbial mats observed at temperatures below 70 °C. Archaea (mainly Crenarchaeota; 19.8% of the total sequences) were detected only in the small biofilms. The high abundance of Archaea in the sample from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. In the microbial mats, primary products were formed by cyanobacteria of the genus Leptolyngbya. Heterotrophic microorganisms were mostly represented by Actinobacteria and Proteobacteria in all studied samples of the microbial mats. Planctomycetes, Chloroflexi, and Chlorobi were abundant in the middle layer of the microbial mats, while heterotrophic microorganisms represented mostly by Firmicutes (Clostridia, strict anaerobes) dominated in the bottom part. Besides prokaryotes, we detect some species of Algae with help of detection their chloroplasts 16 s rRNA. Conclusions: High abundance of Archaea in samples from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. Metagenomic analysis of microbial communities of the microbial mat of Garga hot spring showed that the three studied points sampled at 70 °C, 55 °C, and 45 °C had similar species composition. Cyanobacteria of the genus Leptolyngbya dominated in the upper layer of the microbial mat. Chloroflexi and Chlorobi were less abundant and were mostly observed in the middle part of the microbial mat. We detected domains of heterotrophic organisms in high abundance (Proteobacteria, Firmicutes, Verrucomicrobia, Planctomicetes, Bacteroidetes, Actinobacteria, Thermi), according to metabolic properties of known relatives, which can form complete cycles of carbon, sulphur, and nitrogen in the microbial mat. The studied microbial mats evolved in early stages of biosphere formation. They can live autonomously, providing full cycles of substances and preventing live activity products poisoning.",
keywords = "Bacterial mats, Garga, Hot springs, Metagenome, Microbial community, Geography, Bacteria/genetics, RNA, Ribosomal, 16S/genetics, Phylogeny, Biodiversity, Russia, Hot Springs/microbiology, Likelihood Functions, Archaea/genetics, PHOTOTROPHIC BACTERIA, COMMUNITIES, METAGENOMIC ANALYSIS, ARCHAEAL, COMPLETE GENOME SEQUENCE, CYANOBACTERIA, BACTERIAL DIVERSITY, GEOTHERMAL REGION, YELLOWSTONE-NATIONAL-PARK, TENGCHONG",
author = "Rozanov, {Alexey Sergeevich} and Bryanskaya, {Alla Victorovna} and Ivanisenko, {Timofey Vladimirovich} and Malup, {Tatyana Konstantinovna} and Peltek, {Sergey Evgenievich}",
year = "2017",
month = dec,
day = "28",
doi = "10.1186/s12862-017-1106-9",
language = "English",
volume = "17",
pages = "254",
journal = "BMC Evolutionary Biology",
issn = "1471-2148",
publisher = "BioMed Central Ltd.",
number = "Suppl 2",

}

RIS

TY - JOUR

T1 - Biodiversity of the microbial mat of the Garga hot spring

AU - Rozanov, Alexey Sergeevich

AU - Bryanskaya, Alla Victorovna

AU - Ivanisenko, Timofey Vladimirovich

AU - Malup, Tatyana Konstantinovna

AU - Peltek, Sergey Evgenievich

PY - 2017/12/28

Y1 - 2017/12/28

N2 - Background: Microbial mats are a good model system for ecological and evolutionary analysis of microbial communities. There are more than 20 alkaline hot springs on the banks of the Barguzin river inflows. Water temperature reaches 75 °C and pH is usually 8.0-9.0. The formation of microbial mats is observed in all hot springs. Microbial communities of hot springs of the Baikal rift zone are poorly studied. Garga is the biggest hot spring in this area. Results: In this study, we investigated bacterial and archaeal diversity of the Garga hot spring (Baikal rift zone, Russia) using 16S rRNA metagenomic sequencing. We studied two types of microbial communities: (i) small white biofilms on rocks in the points with the highest temperature (75 °C) and (ii) continuous thick phototrophic microbial mats observed at temperatures below 70 °C. Archaea (mainly Crenarchaeota; 19.8% of the total sequences) were detected only in the small biofilms. The high abundance of Archaea in the sample from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. In the microbial mats, primary products were formed by cyanobacteria of the genus Leptolyngbya. Heterotrophic microorganisms were mostly represented by Actinobacteria and Proteobacteria in all studied samples of the microbial mats. Planctomycetes, Chloroflexi, and Chlorobi were abundant in the middle layer of the microbial mats, while heterotrophic microorganisms represented mostly by Firmicutes (Clostridia, strict anaerobes) dominated in the bottom part. Besides prokaryotes, we detect some species of Algae with help of detection their chloroplasts 16 s rRNA. Conclusions: High abundance of Archaea in samples from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. Metagenomic analysis of microbial communities of the microbial mat of Garga hot spring showed that the three studied points sampled at 70 °C, 55 °C, and 45 °C had similar species composition. Cyanobacteria of the genus Leptolyngbya dominated in the upper layer of the microbial mat. Chloroflexi and Chlorobi were less abundant and were mostly observed in the middle part of the microbial mat. We detected domains of heterotrophic organisms in high abundance (Proteobacteria, Firmicutes, Verrucomicrobia, Planctomicetes, Bacteroidetes, Actinobacteria, Thermi), according to metabolic properties of known relatives, which can form complete cycles of carbon, sulphur, and nitrogen in the microbial mat. The studied microbial mats evolved in early stages of biosphere formation. They can live autonomously, providing full cycles of substances and preventing live activity products poisoning.

AB - Background: Microbial mats are a good model system for ecological and evolutionary analysis of microbial communities. There are more than 20 alkaline hot springs on the banks of the Barguzin river inflows. Water temperature reaches 75 °C and pH is usually 8.0-9.0. The formation of microbial mats is observed in all hot springs. Microbial communities of hot springs of the Baikal rift zone are poorly studied. Garga is the biggest hot spring in this area. Results: In this study, we investigated bacterial and archaeal diversity of the Garga hot spring (Baikal rift zone, Russia) using 16S rRNA metagenomic sequencing. We studied two types of microbial communities: (i) small white biofilms on rocks in the points with the highest temperature (75 °C) and (ii) continuous thick phototrophic microbial mats observed at temperatures below 70 °C. Archaea (mainly Crenarchaeota; 19.8% of the total sequences) were detected only in the small biofilms. The high abundance of Archaea in the sample from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. In the microbial mats, primary products were formed by cyanobacteria of the genus Leptolyngbya. Heterotrophic microorganisms were mostly represented by Actinobacteria and Proteobacteria in all studied samples of the microbial mats. Planctomycetes, Chloroflexi, and Chlorobi were abundant in the middle layer of the microbial mats, while heterotrophic microorganisms represented mostly by Firmicutes (Clostridia, strict anaerobes) dominated in the bottom part. Besides prokaryotes, we detect some species of Algae with help of detection their chloroplasts 16 s rRNA. Conclusions: High abundance of Archaea in samples from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. Metagenomic analysis of microbial communities of the microbial mat of Garga hot spring showed that the three studied points sampled at 70 °C, 55 °C, and 45 °C had similar species composition. Cyanobacteria of the genus Leptolyngbya dominated in the upper layer of the microbial mat. Chloroflexi and Chlorobi were less abundant and were mostly observed in the middle part of the microbial mat. We detected domains of heterotrophic organisms in high abundance (Proteobacteria, Firmicutes, Verrucomicrobia, Planctomicetes, Bacteroidetes, Actinobacteria, Thermi), according to metabolic properties of known relatives, which can form complete cycles of carbon, sulphur, and nitrogen in the microbial mat. The studied microbial mats evolved in early stages of biosphere formation. They can live autonomously, providing full cycles of substances and preventing live activity products poisoning.

KW - Bacterial mats

KW - Garga

KW - Hot springs

KW - Metagenome

KW - Microbial community

KW - Geography

KW - Bacteria/genetics

KW - RNA, Ribosomal, 16S/genetics

KW - Phylogeny

KW - Biodiversity

KW - Russia

KW - Hot Springs/microbiology

KW - Likelihood Functions

KW - Archaea/genetics

KW - PHOTOTROPHIC BACTERIA

KW - COMMUNITIES

KW - METAGENOMIC ANALYSIS

KW - ARCHAEAL

KW - COMPLETE GENOME SEQUENCE

KW - CYANOBACTERIA

KW - BACTERIAL DIVERSITY

KW - GEOTHERMAL REGION

KW - YELLOWSTONE-NATIONAL-PARK

KW - TENGCHONG

UR - http://www.scopus.com/inward/record.url?scp=85039695879&partnerID=8YFLogxK

U2 - 10.1186/s12862-017-1106-9

DO - 10.1186/s12862-017-1106-9

M3 - Article

C2 - 29297382

AN - SCOPUS:85039695879

VL - 17

SP - 254

JO - BMC Evolutionary Biology

JF - BMC Evolutionary Biology

SN - 1471-2148

IS - Suppl 2

M1 - 254

ER -

ID: 9399369