<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Zhang J</submitter><funding>Guangdong Basic and Applied Basic Research Foundation</funding><funding>National Natural Science Foundation of China</funding><funding>National Natural Science Foundation of China (National Science Foundation of China)</funding><pagination>8994</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC11489663</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>15(1)</volume><pubmed_abstract>Mangroves can retain both autochthonous and allochthonous marine and/or terrestrial organic carbon (OC) in sediments. Accurate quantification of these OC sources is essential for the proper allocation of blue C credits. Here, we conduct a global-scale analysis of sediments autochthonous and allochthonous OC contributions in estuarine and marine mangroves using stable isotopes. Globally, mangrove-derived autochthonous OC was the main contributor to estuarine and marine mangrove top-meter soil organic carbon (SOC) (49% and 62%, respectively). Less marine allochthonous OC (21%) was deposited than terrestrial allochthonous OC (30%) in estuarine mangrove sediments. Estuarine mangroves accumulated more SOC in sediments than marine mangroves (282 ± 8.1 Mg C ha&lt;sup>-1&lt;/sup> and 250 ± 5.0 Mg C ha&lt;s</pubmed_abstract><journal>Nature communications</journal><pubmed_title>A global assessment of mangrove soil organic carbon sources and implications for blue carbon credit.</pubmed_title><pmcid>PMC11489663</pmcid><funding_grant_id>42471067，U2106209</funding_grant_id><pubmed_authors>Gan S</pubmed_authors><pubmed_authors>Saintilan N</pubmed_authors><pubmed_authors>Zhang J</pubmed_authors><pubmed_authors>Huang X</pubmed_authors><pubmed_authors>He H</pubmed_authors><pubmed_authors>Sanders CJ</pubmed_authors><pubmed_authors>Yang P</pubmed_authors><pubmed_authors>Wang F</pubmed_authors><pubmed_authors>Chen H</pubmed_authors><pubmed_authors>Zhou J</pubmed_authors></additional><is_claimable>false</is_claimable><name>A global assessment of mangrove soil organic carbon sources and implications for blue carbon credit.</name><description>Mangroves can retain both autochthonous and allochthonous marine and/or terrestrial organic carbon (OC) in sediments. Accurate quantification of these OC sources is essential for the proper allocation of blue C credits. Here, we conduct a global-scale analysis of sediments autochthonous and allochthonous OC contributions in estuarine and marine mangroves using stable isotopes. Globally, mangrove-derived autochthonous OC was the main contributor to estuarine and marine mangrove top-meter soil organic carbon (SOC) (49% and 62%, respectively). Less marine allochthonous OC (21%) was deposited than terrestrial allochthonous OC (30%) in estuarine mangrove sediments. Estuarine mangroves accumulated more SOC in sediments than marine mangroves (282 ± 8.1 Mg C ha&lt;sup>-1&lt;/sup> and 250 ± 5.0 Mg C ha&lt;s</description><dates><release>2024-01-01T00:00:00Z</release><publication>2024 Oct</publication><modification>2025-04-04T19:46:06.436Z</modification><creation>2025-04-04T19:46:06.436Z</creation></dates><accession>S-EPMC11489663</accession><cross_references><pubmed>39424813</pubmed><doi>10.1038/s41467-024-53413-z</doi></cross_references></HashMap>