4.5 Article

Insights into community of photosynthetic microorganisms from permafrost

期刊

FEMS MICROBIOLOGY ECOLOGY
卷 96, 期 12, 页码 -

出版社

OXFORD UNIV PRESS
DOI: 10.1093/femsec/fiaa229

关键词

cyanobacteria; green algae; metagenome; permafrost; cryosol; Arctic

资金

  1. National Science Foundation [DEB-1442262, 1460058]
  2. Russian Federal Target Program [0191-2019-0044]
  3. Russian Foundation for Basic Research (RFBR) [19-04-01240, 19-29-05003mk]
  4. U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research, Genomic Science Program [DE-SC0020369]
  5. Office Of Internatl Science &Engineering
  6. Office Of The Director [1460058] Funding Source: National Science Foundation

向作者/读者索取更多资源

This work integrates cultivation studies of Siberian permafrost and analyses of metagenomes from different locations in the Arctic with the aim of obtaining insights into the community of photosynthetic microorganisms in perennially frozen deposits. Cyanobacteria and microalgae have been described in Arctic aquatic and surface soil environments, but their diversity and ability to withstand harsh conditions within the permafrost are still largely unknown. Community structure of photosynthetic organisms in permafrost sediments was explored using Arctic metagenomes available through the MG-RAST. Sequences affiliated with cyanobacteria represented from 0.25 to 3.03% of total sequences, followed by sequences affiliated with Streptophyta (algae and vascular plants) 0.01-0.45% and Chlorophyta (green algae) 0.01-0.1%. Enrichment and cultivation approaches revealed that cyanobacteria and green algae survive in permafrost and they could be revived during prolonged incubation at low light intensity. Among photosynthetic microorganisms isolated from permafrost, the filamentous Oscillatoria-like cyanobacteria and unicellular green algae of the genus Chlorella were dominant. Our findings suggest that permafrost cyanobacteria and green algae are expected to be effective members of the re-assembled community after permafrost thawing and soil collapse.

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