<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Ray AE</submitter><funding>Department of Education and Training | Australian Research Council</funding><funding>Department of Education and Training | Australian Research Council (ARC)</funding><funding>Department of Health | National Health and Medical Research Council (NHMRC)</funding><funding>Department of Health | National Health and Medical Research Council</funding><pagination>2547-2560</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9561532</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>16(11)</volume><pubmed_abstract>Cold desert soil microbiomes thrive despite severe moisture and nutrient limitations. In Eastern Antarctic soils, bacterial primary production is supported by trace gas oxidation and the light-independent RuBisCO form IE. This study aims to determine if atmospheric chemosynthesis is widespread within Antarctic, Arctic and Tibetan cold deserts, to identify the breadth of trace gas chemosynthetic taxa and to further characterize the genetic determinants of this process. H&lt;sub>2&lt;/sub> oxidation was ubiquitous, far exceeding rates reported to fulfill the maintenance needs of similarly structured edaphic microbiomes. Atmospheric chemosynthesis occurred globally, contributing significantly (p &lt; 0.05) to carbon fixation in Antarctica and the high Arctic. Taxonomic and functional analyses were per</pubmed_abstract><journal>The ISME journal</journal><pubmed_title>Atmospheric chemosynthesis is phylogenetically and geographically widespread and contributes significantly to carbon fixation throughout cold deserts.</pubmed_title><pmcid>PMC9561532</pmcid><funding_grant_id>FT170100341</funding_grant_id><funding_grant_id>APP5191146</funding_grant_id><pubmed_authors>Zaugg J</pubmed_authors><pubmed_authors>Ray AE</pubmed_authors><pubmed_authors>Montgomery K</pubmed_authors><pubmed_authors>Bay S</pubmed_authors><pubmed_authors>Ji M</pubmed_authors><pubmed_authors>Terauds A</pubmed_authors><pubmed_authors>Ferrari BC</pubmed_authors><pubmed_authors>Benaud N</pubmed_authors><pubmed_authors>Wong HL</pubmed_authors><pubmed_authors>Greening C</pubmed_authors><pubmed_authors>Cowan DA</pubmed_authors><pubmed_authors>Williams TJ</pubmed_authors><pubmed_authors>Leung PM</pubmed_authors><pubmed_authors>Chelliah DS</pubmed_authors><pubmed_authors>Hugenholtz P</pubmed_authors><pubmed_authors>Kong W</pubmed_authors></additional><is_claimable>false</is_claimable><name>Atmospheric chemosynthesis is phylogenetically and geographically widespread and contributes significantly to carbon fixation throughout cold deserts.</name><description>Cold desert soil microbiomes thrive despite severe moisture and nutrient limitations. In Eastern Antarctic soils, bacterial primary production is supported by trace gas oxidation and the light-independent RuBisCO form IE. This study aims to determine if atmospheric chemosynthesis is widespread within Antarctic, Arctic and Tibetan cold deserts, to identify the breadth of trace gas chemosynthetic taxa and to further characterize the genetic determinants of this process. H&lt;sub>2&lt;/sub> oxidation was ubiquitous, far exceeding rates reported to fulfill the maintenance needs of similarly structured edaphic microbiomes. Atmospheric chemosynthesis occurred globally, contributing significantly (p &lt; 0.05) to carbon fixation in Antarctica and the high Arctic. Taxonomic and functional analyses were per</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022 Nov</publication><modification>2026-05-31T09:58:05.873Z</modification><creation>2024-11-07T03:11:21.208Z</creation></dates><accession>S-EPMC9561532</accession><cross_references><pubmed>35933499</pubmed><doi>10.1038/s41396-022-01298-5</doi></cross_references></HashMap>