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Environmental Controls on Crenarchaeol Distributions in Hydrothermal Springs

dc.contributor.authorCalhoun, Amanda
dc.contributor.authorBlewett, Jerome
dc.contributor.authorColman, Daniel R.
dc.contributor.authorAmenábar, Maximiliano J.
dc.contributor.authorHarris, Carolynn M.
dc.contributor.authorBoyd, Eric S.
dc.contributor.authorPearson, Anne
dc.contributor.authorLeavitt, William D.
dc.date.accessioned2026-08-26T19:35:53Z
dc.date.issued2026-02
dc.description.abstractThermophilic archaea synthesise cellular membranes composed primarily of isoprenoid glycerol dibiphytanyl glycerol tetraethers (iGDGTs). Cells can adjust the packing of their lipids by increasing cyclopentyl ring production, thereby decreasing membrane permeability and fluidity to maintain cellular function at high temperature, acidic pH, or nutrient limitation. Archaea of the class Nitrososphaeria synthesise crenarchaeol, an iGDGT with four cyclopentyl rings and a cyclohexyl ring, the function of which is unknown. Structural modelling suggests the cyclohexyl ring may increase membrane fluidity, potentially optimising membranes for mesophilic conditions. To investigate the role of crenarchaeol in archaeal membranes in natural settings, we quantify iGDGT compositions of forty-one thermal springs in Yellowstone National Park (YNP), USA, and contextualise these within a global compilation of thermal spring iGDGTs spanning pH values of 1.1–10.1 and temperatures of 16°C–95°C. Spring pH is the strongest predictor of both crenarchaeol relative abundance and the number of cyclopentyl rings per iGDGT. Crenarchaeol relative abundance exhibits a nonlinear relationship with pH and temperature, with highest relative abundances at pH 7.4 and 46°C, decreasing above and below these values. These observations indicate that the cyclohexyl ring of crenarchaeol optimises archaeal cellular membranes for circumneutral and moderate temperature environmental conditions.
dc.identifier.citationCalhoun, A. N., J. Blewett, D. R. Colman, et al. 2026. “ Environmental Controls on Crenarchaeol Distributions in Hydrothermal Springs.” Environmental Microbiology 28, no. 2: e70248. https://doi.org/10.1111/1462-2920.70248.
dc.identifier.doi10.1111/1462-2920.70248
dc.identifier.issn1462-2920
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/20105
dc.language.isoen_US
dc.publisherWiley
dc.rightscc-by
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectaqueous geochemistry
dc.subjectarchaeal lipids
dc.subjectbiomarkers
dc.subjectthermal springs
dc.titleEnvironmental Controls on Crenarchaeol Distributions in Hydrothermal Springs
dc.typeArticle
mus.citation.extentfirstpage1
mus.citation.extentlastpage15
mus.citation.issue2
mus.citation.journaltitleEnvironmental Microbiology
mus.citation.volume28
mus.relation.collegeCollege of Agriculture
mus.relation.departmentMicrobiology & Cell Biology
mus.relation.universityMontana State University - Bozeman

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