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                <identifier>oai:data.mendeley.com/74jvszf5km.1</identifier>
                <datestamp>2025-12-19T15:33:04Z</datestamp>
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            <metadata><oai_dc:dc xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
    <dc:creator>Wu, Xinyue</dc:creator>
    <dc:title>Depth-dependent fate of antimony in sediment is governed by microbially driven iron transformation under redox fluctuation</dc:title>
    <dc:publisher>Mendeley Data</dc:publisher>
    <dc:description>Antimony (Sb) is a highly ecotoxic metalloid that frequently coprecipitates with hydroxyl ferric sulfate minerals (e.g., schwertmannite) in mining environments. The depth-dependent release patterns and governing mechanisms of Sb in sediments under redox fluctuation are not yet clear, which limits a systematic understanding of its biogeochemical behavior and associated environmental risks. This study constructed sediment column systems with different Sb doping levels, and simulated a cycle of 40-day flooding and 20-day drying treatment. Results showed that Sb migration was controlled by a microbial-mediated Fe-Sb coupling cycle with distinct vertical differentiation. During flooding, strong deep-layer reducing conditions drove reductive dissolution and Sb(III) accumulation. Consequently, dissolved Sb increased with depth, reaching 59.0 μg/L (16.3% Sb(III)) in deep layer (15 cm) in high-Sb treatment (0.10Sb_Sch: 674 mg Sb/kg sediment). This process was dominated by iron-reducing bacteria (Bacteroidales), with specific taxa like Acidimicrobiia facilitating Sb(V) reduction. After drying, surface aerobic conditions triggered the proliferation of iron-oxidizing bacteria (Gallionellaceae), promoting Fe oxidation and Sb re-fixation. In contrast, deep sediments (15 cm) maintained high Sb mobility (18.91 μg/L in 0.10Sb_Sch treatment) due to persistent reducing bacteria (Bacillota, Thermodesolufobacteria). This study revealed the hierarchical regulation of microbial-mediated Fe-Sb coupling mechanism under hydrological fluctuation, deepened the understanding of Sb environmental behavior, and provided theoretical basis for the prevention, control and restoration of Sb pollution risk in mining areas.</dc:description>
    <dc:subject>Sedimentary Geochemistry</dc:subject>
    <dc:subject>Antimony</dc:subject>
    <dc:subject>Microorganism</dc:subject>
    <dc:type>Dataset</dc:type>
    <dc:identifier>doi:10.17632/74jvszf5km.1</dc:identifier>
    <dc:identifier>oai:data.mendeley.com/74jvszf5km.1</dc:identifier>
    <dc:rights>Creative Commons Attribution 4.0 International</dc:rights>
    <dc:rights>http://creativecommons.org/licenses/by/4.0</dc:rights>
    <dc:relation>https://data.mendeley.com/datasets/74jvszf5km</dc:relation>
    <dc:date>2025-12-19T15:33:04Z</dc:date>
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