Prokaryotic community in Pleistocene ice wedges of Mammoth Mountain.

Ice wedges differ from other types of surface and underground glacial bodies and are widely spread in perennially frozen sub-Arctic regions, but the bacterial and archaeal diversity in these permafrost features remains poorly studied. Here, we compared the prokaryotic community composition in the active layer and ancient, 13-19 kyr BP and ~ 40 kyr BP, ice wedge horizons from the same exposure profile of the Mammoth Mountain, using pyrosequencing 16S rRNA gene. The most abundant OTUs in the active layer were affiliated with Acidobacteria (31.81%) followed by Actinobacteria (18.29%), Proteobacteria (18.14%), Gemmatimonadetes (7.3%), Parcubacteria (7.13%) and Bacteroidetes (6.49%). The prokaryotic community in 13-19 kyr BP ice wedge differed at the phylum level by the predominance of Actinobacteria (29.15%) over Acidobacteria (19.52%), Proteobacteria (18.45%), Verrumicrobia (5.88%), Firmicutes (2.98%) and Gemmatimonadetes (2.87%). In contrast, the oldest (~ 40 kyr BP) ice wedge prokaryotic community was rather poor, and only three phyla Firmicutes (54.48%), Proteobacteria (31.42%) and Bacteroidetes (7.92%) constituted the major fraction of reads. Archaeal sequences contributed with no more than 0.6% to total reads in all studied samples. Apparently, the Mammoth Mountain exposure profile harbors insular microbial communities with specific structure that reflects the stratigraphy, properties and age.