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Here we assess the abundance and composition of microbial communities that colonized defined minerals incubated for 12 months in two meltwater streams (N and S) emanating from Kaldal\u00f3nsj\u00f6kull (Kal), a basalt-hosted glacier in Iceland. The two streams shared similar meltwater geochemistry as well as bedrock and proglacial sediment elemental compositions. Yet genomic DNA and PCR-amplifiable 16S rRNA genes were detected only in Kal S. The amount of recoverable DNA was highest for hematite incubated in Kal S and the composition of 16S rRNA genes recovered from Kal S sediments was most like those recovered from hematite and magnetite, an effect driven largely by similarities in the relative abundance of the putative hydrogenotrophic iron reducer Rhodoferax. We suggest this is attributable to comminution and weathering reactions involving exposed iron silicate minerals that generate and release hydrogen and Fe(III) that can be coupled to support microbial metabolism in Kaldal\u00f3nsj\u00f6kull, and possibly other basaltic habitats. The low abundance of cells in Kal N could be due to low availability of Fe(III) or another substrate.<\/jats:p>","DOI":"10.1093\/femsec\/fiac155","type":"journal-article","created":{"date-parts":[[2022,12,24]],"date-time":"2022-12-24T00:18:55Z","timestamp":1671841135000},"source":"Crossref","is-referenced-by-count":4,"title":["Iron Minerals Influence the Assembly of Microbial Communities in a Basaltic Glacial Catchment"],"prefix":"10.1093","volume":"99","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-2883-2293","authenticated-orcid":false,"given":"Eric C","family":"Dunham","sequence":"first","affiliation":[{"name":"Department of Microbiology and Cell Biology, Montana State University , Bozeman, MT 59717, United States"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Lisa M","family":"Keller","sequence":"additional","affiliation":[{"name":"Department of Microbiology and Cell Biology, Montana State University , Bozeman, MT 59717, United 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