<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>13</volume><submitter>Yang Y</submitter><pubmed_abstract>Soil dissolved organic matter (DOM) plays a vital role in biogeochemical processes. Global warming leads to increased freeze-thaw cycles (FTCs) in boreal forest soils, which can change DOM production and consumption. However, the interactions between the chemical composition of DOM molecules and the microbial communities that drive C decomposition in the context of freeze-thaw are poorly understood. Here, a FTCs incubation experiment was conducted. Combined with pyrolysis gas chromatography-mass spectrometry and high-throughput sequencing techniques, the relationships between DOM chemodiversity and microbial community structure were assessed. Results indicated that both low-frequency (2FTCs) and high-frequency freeze-thaw cycles (6FTCs) significantly increased soil dissolved organic carbon</pubmed_abstract><journal>Frontiers in microbiology</journal><pagination>1012512</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9868181</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Linkages between the molecular composition of dissolved organic matter and soil microbial community in a boreal forest during freeze-thaw cycles.</pubmed_title><pmcid>PMC9868181</pmcid><pubmed_authors>Cheng S</pubmed_authors><pubmed_authors>Fang H</pubmed_authors><pubmed_authors>Li Y</pubmed_authors><pubmed_authors>Yang Y</pubmed_authors><pubmed_authors>Guo Y</pubmed_authors><pubmed_authors>Vancampenhout K</pubmed_authors><pubmed_authors>Shi F</pubmed_authors><pubmed_authors>Zhou Y</pubmed_authors></additional><is_claimable>false</is_claimable><name>Linkages between the molecular composition of dissolved organic matter and soil microbial community in a boreal forest during freeze-thaw cycles.</name><description>Soil dissolved organic matter (DOM) plays a vital role in biogeochemical processes. Global warming leads to increased freeze-thaw cycles (FTCs) in boreal forest soils, which can change DOM production and consumption. However, the interactions between the chemical composition of DOM molecules and the microbial communities that drive C decomposition in the context of freeze-thaw are poorly understood. Here, a FTCs incubation experiment was conducted. Combined with pyrolysis gas chromatography-mass spectrometry and high-throughput sequencing techniques, the relationships between DOM chemodiversity and microbial community structure were assessed. Results indicated that both low-frequency (2FTCs) and high-frequency freeze-thaw cycles (6FTCs) significantly increased soil dissolved organic carbon</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022</publication><modification>2026-05-27T22:44:56.879Z</modification><creation>2025-02-19T04:45:48.27Z</creation></dates><accession>S-EPMC9868181</accession><cross_references><pubmed>36699583</pubmed><doi>10.3389/fmicb.2022.1012512</doi></cross_references></HashMap>