<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Zhou G</submitter><funding>Chinese Academy of Sciences</funding><funding>National Natural Science Foundation of China</funding><pagination>746-757</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8291401</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>6(4)</volume><pubmed_abstract>Soil organic carbon (SOC) plays critical roles in stabilizing atmospheric CO&lt;sub>2&lt;/sub> concentration, but the mechanistic controls on the amount and distribution of SOC on global scales are not well understood. In turn, this has hampered the ability to model global C budgets and to find measures to mitigate climate change. Here, based on the data from a large field survey campaign with 2600 plots across China's forest ecosystems and a global collection of published data from forested land, we find that a low litter carbon-to-nitrogen ratio (C/N) and high wetness index (P/PET, precipitation-to-potential-evapotranspiration ratio) are the two factors that promote SOC accumulation, with only minor contributions of litter quantity and soil texture. The field survey data demonstrated that high</pubmed_abstract><journal>National science review</journal><pubmed_title>Climate and litter C/N ratio constrain soil organic carbon accumulation.</pubmed_title><pmcid>PMC8291401</pmcid><funding_grant_id>XDA05050000</funding_grant_id><funding_grant_id>NSFC41430529</funding_grant_id><pubmed_authors>Liu J</pubmed_authors><pubmed_authors>Ciais P</pubmed_authors><pubmed_authors>Fang J</pubmed_authors><pubmed_authors>Zhang D</pubmed_authors><pubmed_authors>Du S</pubmed_authors><pubmed_authors>Lu X</pubmed_authors><pubmed_authors>Yu G</pubmed_authors><pubmed_authors>Ma Y</pubmed_authors><pubmed_authors>Wang G</pubmed_authors><pubmed_authors>Liu S</pubmed_authors><pubmed_authors>Han S</pubmed_authors><pubmed_authors>Manzoni S</pubmed_authors><pubmed_authors>Zhang Q</pubmed_authors><pubmed_authors>Ren H</pubmed_authors><pubmed_authors>Chu G</pubmed_authors><pubmed_authors>Zhou G</pubmed_authors><pubmed_authors>Wang W</pubmed_authors><pubmed_authors>Chen X</pubmed_authors><pubmed_authors>Tang X</pubmed_authors><pubmed_authors>Yan J</pubmed_authors><pubmed_authors>Zhou P</pubmed_authors><pubmed_authors>Li Y</pubmed_authors><pubmed_authors>Li S</pubmed_authors><pubmed_authors>Huang W</pubmed_authors><pubmed_authors>Xu S</pubmed_authors><pubmed_authors>Ma K</pubmed_authors></additional><is_claimable>false</is_claimable><name>Climate and litter C/N ratio constrain soil organic carbon accumulation.</name><description>Soil organic carbon (SOC) plays critical roles in stabilizing atmospheric CO&lt;sub>2&lt;/sub> concentration, but the mechanistic controls on the amount and distribution of SOC on global scales are not well understood. In turn, this has hampered the ability to model global C budgets and to find measures to mitigate climate change. Here, based on the data from a large field survey campaign with 2600 plots across China's forest ecosystems and a global collection of published data from forested land, we find that a low litter carbon-to-nitrogen ratio (C/N) and high wetness index (P/PET, precipitation-to-potential-evapotranspiration ratio) are the two factors that promote SOC accumulation, with only minor contributions of litter quantity and soil texture. The field survey data demonstrated that high</description><dates><release>2019-01-01T00:00:00Z</release><publication>2019 Jul</publication><modification>2025-04-19T20:43:29.916Z</modification><creation>2025-04-19T20:43:29.916Z</creation></dates><accession>S-EPMC8291401</accession><cross_references><pubmed>34691930</pubmed><doi>10.1093/nsr/nwz045</doi></cross_references></HashMap>