<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Keffer JL</submitter><funding>HHS | National Institutes of Health</funding><funding>HHS | National Institutes of Health (NIH)</funding><funding>National Science Foundation (NSF)</funding><funding>NIGMS NIH HHS</funding><funding>National Science Foundation</funding><pagination>e0186524</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12016527</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>91(4)</volume><pubmed_abstract>Most of Earth's iron is mineral-bound, but it is unclear how and to what extent iron-oxidizing microbes can use solid minerals as electron donors. A prime candidate for studying mineral-oxidizing growth and pathways is &lt;i>Sideroxydans lithotrophicus&lt;/i> ES-1, a robust, facultative iron oxidizer with multiple possible iron oxidation mechanisms. These include Cyc2 and Mto pathways plus other multiheme cytochromes and cupredoxins, and so we posit that the mechanisms may correspond to different Fe(II) sources. Here, &lt;i>S. lithotrophicus&lt;/i> ES-1 was grown on dissolved Fe(II)-citrate and magnetite. &lt;i>S. lithotrophicus&lt;/i> ES-1 oxidized all dissolved Fe&lt;sup>2+&lt;/sup> released from magnetite and continued to build biomass when only solid Fe(II) remained, suggesting it can utilize magnetite as a s</pubmed_abstract><journal>Applied and environmental microbiology</journal><pubmed_title>Microbial magnetite oxidation via MtoAB porin-multiheme cytochrome complex in &amp;lt;i&amp;gt;Sideroxydans lithotrophicus&amp;lt;/i&amp;gt; ES-1.</pubmed_title><pmcid>PMC12016527</pmcid><funding_grant_id>P20 GM103446</funding_grant_id><funding_grant_id>P20 GM104316</funding_grant_id><funding_grant_id>P20GM104316</funding_grant_id><funding_grant_id>P20GM103446</funding_grant_id><funding_grant_id>BIO-1817651</funding_grant_id><pubmed_authors>Zhou N</pubmed_authors><pubmed_authors>Rushworth DD</pubmed_authors><pubmed_authors>Keffer JL</pubmed_authors><pubmed_authors>Chan CS</pubmed_authors><pubmed_authors>Yu Y</pubmed_authors></additional><is_claimable>false</is_claimable><name>Microbial magnetite oxidation via MtoAB porin-multiheme cytochrome complex in &amp;lt;i&amp;gt;Sideroxydans lithotrophicus&amp;lt;/i&amp;gt; ES-1.</name><description>Most of Earth's iron is mineral-bound, but it is unclear how and to what extent iron-oxidizing microbes can use solid minerals as electron donors. A prime candidate for studying mineral-oxidizing growth and pathways is &lt;i>Sideroxydans lithotrophicus&lt;/i> ES-1, a robust, facultative iron oxidizer with multiple possible iron oxidation mechanisms. These include Cyc2 and Mto pathways plus other multiheme cytochromes and cupredoxins, and so we posit that the mechanisms may correspond to different Fe(II) sources. Here, &lt;i>S. lithotrophicus&lt;/i> ES-1 was grown on dissolved Fe(II)-citrate and magnetite. &lt;i>S. lithotrophicus&lt;/i> ES-1 oxidized all dissolved Fe&lt;sup>2+&lt;/sup> released from magnetite and continued to build biomass when only solid Fe(II) remained, suggesting it can utilize magnetite as a s</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Apr</publication><modification>2026-06-03T04:53:05.968Z</modification><creation>2026-05-28T03:06:56.736Z</creation></dates><accession>S-EPMC12016527</accession><cross_references><pubmed>40042276</pubmed><doi>10.1128/aem.01865-24</doi></cross_references></HashMap>