<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Deng Y</submitter><funding>Special Funds of Scientific and Technological Innovation for Carbon Peak and Neutrality in Jiangsu Province</funding><funding>Youth Innovation Promotion Association of CAS</funding><funding>National Natural Science Foundation of China</funding><funding>Second Tibetan Plateau Scientific Expedition and Research Program</funding><pagination>ycae032</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC10960969</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>4(1)</volume><pubmed_abstract>Methane (CH&lt;sub>4&lt;/sub>), an important greenhouse gas, significantly impacts the local and global climate. Our study focused on the composition and activity of methanotrophs residing in the lakes on the Tibetan Plateau, a hotspot for climate change research. Based on the field survey, the family &lt;i>Methylomonadaceae&lt;/i> had a much higher relative abundance in freshwater lakes than in brackish and saline lakes, accounting for ~92% of total aerobic methanotrophs. Using the microcosm sediment incubation with &lt;sup>13&lt;/sup>CH&lt;sub>4&lt;/sub> followed by high throughput sequencing and metagenomic analysis, we further demonstrated that the family &lt;i>Methylomonadaceae&lt;/i> was actively oxidizing CH&lt;sub>4&lt;/sub>. Moreover, various methylotrophs, such as the genera &lt;i>Methylotenera&lt;/i> and &lt;i>Methylophilu</pubmed_abstract><journal>ISME communications</journal><pubmed_title>&lt;i>Methylomonadaceae&lt;/i> was the active and dominant methanotroph in Tibet lake sediments.</pubmed_title><pmcid>PMC10960969</pmcid><funding_grant_id>BK20220015</funding_grant_id><funding_grant_id>41401075</funding_grant_id><funding_grant_id>2019QZKK0503</funding_grant_id><funding_grant_id>U2102216</funding_grant_id><funding_grant_id>2014273</funding_grant_id><funding_grant_id>41971077</funding_grant_id><funding_grant_id>92251304</funding_grant_id><funding_grant_id>2021QZKK0100</funding_grant_id><pubmed_authors>Liang C</pubmed_authors><pubmed_authors>Pan H</pubmed_authors><pubmed_authors>Tao Y</pubmed_authors><pubmed_authors>Chen L</pubmed_authors><pubmed_authors>Xun F</pubmed_authors><pubmed_authors>Zhu X</pubmed_authors><pubmed_authors>Deng Y</pubmed_authors><pubmed_authors>Xing P</pubmed_authors></additional><is_claimable>false</is_claimable><name>&lt;i>Methylomonadaceae&lt;/i> was the active and dominant methanotroph in Tibet lake sediments.</name><description>Methane (CH&lt;sub>4&lt;/sub>), an important greenhouse gas, significantly impacts the local and global climate. Our study focused on the composition and activity of methanotrophs residing in the lakes on the Tibetan Plateau, a hotspot for climate change research. Based on the field survey, the family &lt;i>Methylomonadaceae&lt;/i> had a much higher relative abundance in freshwater lakes than in brackish and saline lakes, accounting for ~92% of total aerobic methanotrophs. Using the microcosm sediment incubation with &lt;sup>13&lt;/sup>CH&lt;sub>4&lt;/sub> followed by high throughput sequencing and metagenomic analysis, we further demonstrated that the family &lt;i>Methylomonadaceae&lt;/i> was actively oxidizing CH&lt;sub>4&lt;/sub>. Moreover, various methylotrophs, such as the genera &lt;i>Methylotenera&lt;/i> and &lt;i>Methylophilu</description><dates><release>2024-01-01T00:00:00Z</release><publication>2024 Jan</publication><modification>2025-04-26T12:06:31.167Z</modification><creation>2024-11-13T04:46:53.647Z</creation></dates><accession>S-EPMC10960969</accession><cross_references><pubmed>38524764</pubmed><doi>10.1093/ismeco/ycae032</doi></cross_references></HashMap>