Distinctive microbial communities in subzero hypersaline brines from Arctic coastal sea ice and rarely sampled cryopegs. Issue 12 (18th October 2019)

• Record Type: Journal Article
• Authors: Cooper, Zachary S; Rapp, Josephine Z; Carpenter, Shelly D; Iwahana, Go; Eicken, Hajo; Deming, Jody W
• Is Part Of: FEMS microbiology ecology. Volume 95:Issue 12(2020)
• Publication Date: 2019-10-18
• Subjects: cryopeg -- sea ice -- Arctic -- Marinobacter -- subsurface microbiology -- bacterial diversity; Microbial ecology -- Periodicals; Microbiology -- Periodicals; 579.17
• DOI: 10.1093/femsec/fiz166
• Languages: English
• ISSNs: 0168-6496

Abstract

ABSTRACT: Hypersaline aqueous environments at subzero temperatures are known to be inhabited by microorganisms, yet information on community structure in subzero brines is very limited. Near Utqiaġvik, Alaska, we sampled subzero brines (–6°C, 115–140 ppt) from cryopegs, i.e. unfrozen sediments within permafrost that contain relic (late Pleistocene) seawater brine, as well as nearby sea-ice brines to examine microbial community composition and diversity using 16S rRNA gene amplicon sequencing. We also quantified the communities microscopically and assessed environmental parameters as possible determinants of community structure. The cryopeg brines harbored surprisingly dense bacterial communities (up to 10 8 cells mL –1 ) and millimolar levels of dissolved and particulate organic matter, extracellular polysaccharides and ammonia. Community composition and diversity differed between the two brine environments by alpha- and beta-diversity indices, with cryopeg brine communities appearing less diverse and dominated by one strain of the genus Marinobacter, also detected in other cold, hypersaline environments, including sea ice. The higher density and trend toward lower diversity in the cryopeg communities suggest that long-term stability and other features of a subzero brine are more important selective forces than in situ temperature or salinity, even when the latter are extreme. Abstract : An ice cave in Arctic permafrost yields subzero brines, likely ancient relic seawater, inhabited by robust microbial communities (dominated by a single strain of Marinobacter ) distinctive from modern sea-ice brines.