2019
DOI: 10.1128/msystems.00498-19
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Anoxygenic Phototrophs Span Geochemical Gradients and Diverse Morphologies in Terrestrial Geothermal Springs

Abstract: There is a long and rich history of literature on phototrophs in terrestrial geothermal springs. These studies have revealed sulfide, pH, and temperature are the main constraints on phototrophy. However, the taxonomic and physiological diversity of anoxygenic phototrophs suggests that, within these constraints, specific geochemical parameters determine the distribution and activity of individual anoxygenic phototrophic taxa. Here, we report the recovery of sequences affiliated with characterized anoxygenic pho… Show more

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Cited by 28 publications
(77 citation statements)
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“…As expected based on previous studies of alkaline hot springs, more than 50% of the OTUs were classified as either Chloroflexi or Cyanobacteria (Fig. 1) (Brock, 1978;Bateson and Ward, 1988;Nübel et al, 2002;Bhaya et al, 2007;Miller et al, 2009;Rozanov et al, 2017;Alcamán-Arias et al, 2018, reviewed in Thiel et al, 2018Hamilton et al, 2019). Chloroflexi richness (OTUs per sample) did not show a linear trend with temperature ( Fig.…”
Section: Phototrophic Chloroflexi Have Unique Distributions With Tempsupporting
confidence: 80%
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“…As expected based on previous studies of alkaline hot springs, more than 50% of the OTUs were classified as either Chloroflexi or Cyanobacteria (Fig. 1) (Brock, 1978;Bateson and Ward, 1988;Nübel et al, 2002;Bhaya et al, 2007;Miller et al, 2009;Rozanov et al, 2017;Alcamán-Arias et al, 2018, reviewed in Thiel et al, 2018Hamilton et al, 2019). Chloroflexi richness (OTUs per sample) did not show a linear trend with temperature ( Fig.…”
Section: Phototrophic Chloroflexi Have Unique Distributions With Tempsupporting
confidence: 80%
“…Photosynthetic bacteria are key primary producers in alkaline, terrestrial hot springs and a rich history of research has focused on phototrophs in Yellowstone National Park (YNP) (Pierson and Castenholz, 1974;Madigan and Brock, 1977; reviewed in the study by Tank et al, 2017;Hamilton et al, 2019). Hot springs provide a framework to test the ecophysiology of phototrophs in situ because they are dynamic and complex environments with natural gradients of temperature, sulfide and pH that harbour highly adapted microbial communities.…”
Section: Introductionmentioning
confidence: 99%
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“…To examine water geochemistry including major ions, major cations, trace elements, and carbon concentration and isotopes, samples were collected and stored following previously described methods [39][40][41]. In brief, samples were collected in a 140-mL syringe, filtered through 0.8/0.2 μm polyethersulfone syringe filters, and dispensed into 15-mL polypropylene centrifuge tubes (for major anions), acid-washed 15-mL polypropylene centrifuge tubes (for major cations and trace elements), Labco Exetainers® (Labco Limited, Lampeter, UK) preflushed with He (for dissolved inorganic carbon (DIC)), and sterile 50-mL centrifuge tubes (for dissolved organic carbon (DOC)).…”
Section: Geochemical Analyses Aqueous Geochemistrymentioning
confidence: 99%
“…In situ microcosms were performed to assess the potential for inorganic carbon uptake through the addition of NaH 13 CO 3 . Sample collection and the microcosm set-up followed previously described methods [39][40][41]. In summary, samples (biofilms, filaments, etc.)…”
Section: Co 2 Assimilationmentioning
confidence: 99%