<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Begill N</submitter><funding>European Union's Horizon 2020 Research and Innovation Programme</funding><pagination>e70646</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12683473</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>31(12)</volume><pubmed_abstract>Stabilized soil organic carbon (SOC) accrual plays a crucial role in long-term atmospheric CO&lt;sub>2&lt;/sub> sequestration. The organic carbon in the fine silt and clay size fraction (OC&lt;sub>fine&lt;/sub>) is typically mineral-associated and thus relatively stable. However, the SOC saturation concept suggests that the OC&lt;sub>fine&lt;/sub> has limited capacity for additional carbon (C) storage, thereby constraining further C sequestration. Low-OC and fine-textured soils are thought to have greater potential to stabilize additional OC than High-OC and coarse-textured soils due to their higher available storage space. Here, we assessed soils' potential to stabilize additional OC using 21 temperate agricultural soils, varying in SOC (0.7%-10.2%), silt + clay content (32%-92%), and OC loading of fine fr</pubmed_abstract><journal>Global change biology</journal><pubmed_title>Increased Retention of Litter-Derived Organic Carbon With Increasing Initial Carbon Content in Temperate Agricultural Soils.</pubmed_title><pmcid>PMC12683473</pmcid><funding_grant_id>862695</funding_grant_id><pubmed_authors>Poeplau C</pubmed_authors><pubmed_authors>Begill N</pubmed_authors><pubmed_authors>Don A</pubmed_authors><pubmed_authors>Hoeschen C</pubmed_authors><pubmed_authors>Schiedung M</pubmed_authors><pubmed_authors>Guggenberger G</pubmed_authors><pubmed_authors>Schweizer SA</pubmed_authors></additional><is_claimable>false</is_claimable><name>Increased Retention of Litter-Derived Organic Carbon With Increasing Initial Carbon Content in Temperate Agricultural Soils.</name><description>Stabilized soil organic carbon (SOC) accrual plays a crucial role in long-term atmospheric CO&lt;sub>2&lt;/sub> sequestration. The organic carbon in the fine silt and clay size fraction (OC&lt;sub>fine&lt;/sub>) is typically mineral-associated and thus relatively stable. However, the SOC saturation concept suggests that the OC&lt;sub>fine&lt;/sub> has limited capacity for additional carbon (C) storage, thereby constraining further C sequestration. Low-OC and fine-textured soils are thought to have greater potential to stabilize additional OC than High-OC and coarse-textured soils due to their higher available storage space. Here, we assessed soils' potential to stabilize additional OC using 21 temperate agricultural soils, varying in SOC (0.7%-10.2%), silt + clay content (32%-92%), and OC loading of fine fr</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Dec</publication><modification>2026-06-08T05:00:23.188Z</modification><creation>2026-06-08T03:08:53.857Z</creation></dates><accession>S-EPMC12683473</accession><cross_references><pubmed>41355724</pubmed><doi>10.1111/gcb.70646</doi></cross_references></HashMap>