4.5 Article

Evidence of form II RubisCO (cbbM) in a perennially ice-covered Antarctic lake

期刊

FEMS MICROBIOLOGY ECOLOGY
卷 82, 期 2, 页码 491-500

出版社

OXFORD UNIV PRESS
DOI: 10.1111/j.1574-6941.2012.01431.x

关键词

Antarctica; Dry Valley lake; RubisCO; chemolithoautotrophy; polar night

资金

  1. NSF Office of Polar Programs
  2. Molecular and Cellular Biosciences Grants [0631659, 1056396, 0631494, 432595, 1115245, 0237335]
  3. Division Of Polar Programs
  4. Directorate For Geosciences [838933] Funding Source: National Science Foundation
  5. Office of Polar Programs (OPP)
  6. Directorate For Geosciences [1056396] Funding Source: National Science Foundation

向作者/读者索取更多资源

The permanently ice-covered lakes of the McMurdo Dry Valleys, Antarctica, harbor microbially dominated food webs. These organisms are adapted to a variety of unusual environmental extremes, including low temperature, low light, and permanently stratified water columns with strong chemo- and oxy-clines. Owing to the low light levels during summer caused by thick ice cover as well as 6months of darkness during the polar winter, chemolithoautotrophic microorganisms could play a key role in the production of new carbon for the lake ecosystems. We used clone library sequencing and real-time quantitative PCR of the gene encoding form II Ribulose 1, 5-bisphosphate carboxylase/oxygenase to determine spatial and seasonal changes in the chemolithoautotrophic community in Lake Bonney, a 40-m-deep lake covered by c. 4m of permanent ice. Our results revealed that chemolithoautotrophs harboring the cbbM gene are restricted to layers just above the chemo- and oxi-cline (=15m) in the west lobe of Lake Bonney (WLB). Our data reveal that the WLB is inhabited by a unique chemolithoautotrophic community that resides in the suboxic layers of the lake where there are ample sources of alternative electron sources such as ammonium, reduced iron and reduced biogenic sulfur species.

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