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dc.contributor.authorColman, Daniel R.
dc.contributor.authorPoudel, Saroj
dc.contributor.authorHamilton, Trinity L.
dc.contributor.authorHavig, Jeff R.
dc.contributor.authorSelensky, Matthew J.
dc.contributor.authorShock, Everett L.
dc.contributor.authorBoyd, Eric S.
dc.date.accessioned2018-02-16T19:34:18Z
dc.date.available2018-02-16T19:34:18Z
dc.date.issued2017-10
dc.identifier.citationColman, Daniel R, Saroj Poudel, Trinity L Hamilton, Jeff R Havig, Matthew J Selensky, Everett L Shock, and Eric S Boyd. "Geobiological feedbacks and the evolution of thermoacidophiles." The ISME journal (October 2017). DOI:https://dx.doi.org/10.1038/ismej.2017.162.en_US
dc.identifier.issn1751-7362
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/14382
dc.description.abstractOxygen-dependent microbial oxidation of sulfur compounds leads to the acidification of natural waters. How acidophiles and their acidic habitats evolved, however, is largely unknown. Using 16S rRNA gene abundance and composition data from 72 hot springs in Yellowstone National Park, Wyoming, we show that hyperacidic (pH<3.0) hydrothermal ecosystems are dominated by a limited number of archaeal lineages with an inferred ability to respire O2. Phylogenomic analyses of 584 existing archaeal genomes revealed that hyperacidophiles evolved independently multiple times within the Archaea, each coincident with the emergence of the ability to respire O2, and that these events likely occurred in the recent evolutionary past. Comparative genomic analyses indicated that archaeal thermoacidophiles from independent lineages are enriched in similar protein-coding genes, consistent with convergent evolution aided by horizontal gene transfer. Because the generation of acidic environments and their successful habitation characteristically require O2, these results suggest that thermoacidophilic Archaea and the acidity of their habitats co-evolved after the evolution of oxygenic photosynthesis. Moreover, it is likely that dissolved O2 concentrations in thermal waters likely did not reach levels capable of sustaining aerobic thermoacidophiles and their acidifying activity until ~0.8Ga, when present day atmospheric levels were reached, a time period that is supported by our estimation of divergence times for archaeal thermoacidophilic clades.en_US
dc.description.sponsorshipNASA Exobiology and Evolutionary Biology grant (NNX13AI11G); NSF grant EAR-1529963; Montana Space Grant Consortium grant; NASA Astrobiology Institute is supported by grant NNA15BB02A;en_US
dc.rightsCC BY-NC-SAen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/legalcodeen_US
dc.titleGeobiological feedbacks and the evolution of thermoacidophilesen_US
mus.citation.journaltitleThe ISME journalen_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1038/ismej.2017.162en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentMicrobiology & Immunology.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.data.thumbpage4en_US


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