{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,12]],"date-time":"2026-04-12T07:56:33Z","timestamp":1775980593848,"version":"3.50.1"},"reference-count":100,"publisher":"Wiley","issue":"3","license":[{"start":{"date-parts":[[2024,5,3]],"date-time":"2024-05-03T00:00:00Z","timestamp":1714694400000},"content-version":"vor","delay-in-days":2,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"funder":[{"DOI":"10.13039\/100022938","name":"Rocky Mountain Association of Geologists","doi-asserted-by":"publisher","id":[{"id":"10.13039\/100022938","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":["onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["Geobiology"],"published-print":{"date-parts":[[2024,5]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>\n                    Lehman Caves is an extensively decorated high desert cave that represents one of the main tourist attractions in Great Basin National Park, Nevada. Although traditionally considered a water table cave, recent studies identified abundant speleogenetic features consistent with a hypogenic and, potentially, sulfuric acid origin. Here, we characterized white mineral deposits in the Gypsum Annex (GA) passage to determine whether these secondary deposits represent biogenic minerals formed during sulfuric acid corrosion and explored microbial communities associated with these and other mineral deposits throughout the cave. Powder X\u2010ray diffraction (pXRD), scanning electron microscopy with electron dispersive spectroscopy (SEM\u2010EDS), and electron microprobe analyses (EPMA) showed that, while most white mineral deposits from the GA contain gypsum, they also contain abundant calcite, silica, and other phases. Gypsum and carbonate\u2010associated sulfate isotopic values of these deposits are variable, with \u03b4\n                    <jats:sup>34<\/jats:sup>\n                    S\n                    <jats:sub>V\u2010CDT<\/jats:sub>\n                    between +9.7\u2030 and +26.1\u2030, and do not reflect depleted values typically associated with replacement gypsum formed during sulfuric acid speleogenesis. Petrographic observations show that the sulfates likely co\u2010precipitated with carbonate and SiO\n                    <jats:sub>2<\/jats:sub>\n                    phases. Taken together, these data suggest that the deposits resulted from later\u2010stage meteoric events and not during an initial episode of sulfuric acid speleogenesis. Most sedimentary and mineral deposits in Lehman Caves have very low microbial biomass, with the exception of select areas along the main tour route that have been impacted by tourist traffic. High\u2010throughput 16S rRNA gene amplicon sequencing showed that microbial communities in GA sediments are distinct from those in other parts of the cave. The microbial communities that inhabit these oligotrophic secondary mineral deposits include OTUs related to known ammonia\u2010oxidizing\n                    <jats:italic>Nitrosococcales<\/jats:italic>\n                    and Thaumarchaeota, as well as common soil taxa such as Acidobacteriota and Proteobacteria. This study reveals microbial and mineralogical diversity in a previously understudied cave and expands our understanding of the geomicrobiology of desert hypogene cave systems.\n                  <\/jats:p>","DOI":"10.1111\/gbi.12594","type":"journal-article","created":{"date-parts":[[2024,5,3]],"date-time":"2024-05-03T09:29:06Z","timestamp":1714728546000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":8,"title":["Origin and modern microbial ecology of secondary mineral deposits in Lehman Caves, Great Basin National Park,\n                    <scp>NV<\/scp>\n                    ,\n                    <scp>USA<\/scp>"],"prefix":"10.1111","volume":"22","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-9037-5206","authenticated-orcid":false,"given":"Zo\u00eb E.","family":"Havlena","sequence":"first","affiliation":[{"name":"Earth and Environmental Science New Mexico Institute of Mining and Technology  Socorro New Mexico USA"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-3668-9458","authenticated-orcid":false,"given":"Louise D.","family":"Hose","sequence":"additional","affiliation":[{"name":"Department of Geological Sciences and Engineering University of Nevada  Reno Nevada USA"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0009-0009-1588-0577","authenticated-orcid":false,"given":"Harvey R.","family":"DuChene","sequence":"additional","affiliation":[{"name":"Karst Waters Institute  Lake City Colorado USA"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0009-0008-7171-3338","authenticated-orcid":false,"given":"Gretchen M.","family":"Baker","sequence":"additional","affiliation":[{"name":"Great Basin National Park  Baker Nevada USA"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0009-0006-6005-4723","authenticated-orcid":false,"given":"J. 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