<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>15(1)</volume><submitter>Sanchez-Roman M</submitter><pubmed_abstract>Microbial impacts on early carbonate diagenesis, particularly the formation of Mg-carbonates at low temperatures, have long eluded scientists. Our breakthrough laboratory experiments with two species of halophilic aerobic bacteria and marine carbonate grains reveal that these bacteria created a distinctive protodolomite (disordered dolomite) rim around the grains. Scanning Electron Microscopy (SEM) and X-ray Diffraction (XRD) confirmed the protodolomite formation, while solid-state nuclear magnetic resonance (NMR) revealed bacterial interactions with carboxylated organic matter, such as extracellular polymeric substances (EPS). We observed a significant carbon isotope fractionation (average δ&lt;sup>13&lt;/sup>C = 11.3‰) and notable changes in Mg/Ca ratios throughout the experiments. Initial med</pubmed_abstract><journal>Scientific reports</journal><pagination>561</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC11696100</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>The hidden role of heterotrophic bacteria in early carbonate diagenesis.</pubmed_title><pmcid>PMC11696100</pmcid><pubmed_authors>Sanchez-Roman M</pubmed_authors><pubmed_authors>Reijmer J</pubmed_authors><pubmed_authors>Vahrenkamp V</pubmed_authors><pubmed_authors>Areias C</pubmed_authors><pubmed_authors>Chandra V</pubmed_authors><pubmed_authors>Mulder S</pubmed_authors></additional><is_claimable>false</is_claimable><name>The hidden role of heterotrophic bacteria in early carbonate diagenesis.</name><description>Microbial impacts on early carbonate diagenesis, particularly the formation of Mg-carbonates at low temperatures, have long eluded scientists. Our breakthrough laboratory experiments with two species of halophilic aerobic bacteria and marine carbonate grains reveal that these bacteria created a distinctive protodolomite (disordered dolomite) rim around the grains. Scanning Electron Microscopy (SEM) and X-ray Diffraction (XRD) confirmed the protodolomite formation, while solid-state nuclear magnetic resonance (NMR) revealed bacterial interactions with carboxylated organic matter, such as extracellular polymeric substances (EPS). We observed a significant carbon isotope fractionation (average δ&lt;sup>13&lt;/sup>C = 11.3‰) and notable changes in Mg/Ca ratios throughout the experiments. Initial med</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Jan</publication><modification>2025-04-22T08:59:30.685Z</modification><creation>2025-04-05T22:52:27.441Z</creation></dates><accession>S-EPMC11696100</accession><cross_references><pubmed>39747618</pubmed><doi>10.1038/s41598-024-84407-y</doi></cross_references></HashMap>