2021
DOI: 10.1089/ast.2019.2086
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Hot Spring Microbial Community Elemental Composition: Hot Spring and Soil Inputs, and the Transition from Biocumulus to Siliceous Sinter

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Cited by 11 publications
(8 citation statements)
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“…Nitrate was detectable in both samples (14.3 µM), while ammonium was below detection limit in 18WCA1 and 6.0 µM in 18WCA2 (Supplementary File 1). Micromolar concentrations of nitrate and/or ammonia have been previously reported LGB springs (Havig et al, 2021;Holloway et al, 2011), and thus we expect 2017 samples would have had similar concentrations. It is possible that unmeasured parameters and/or biogeography are primary predictors of the characteristic extremely thermophilic green filaments in these springs.…”
Section: (Fig 1 Tablementioning
confidence: 70%
“…Nitrate was detectable in both samples (14.3 µM), while ammonium was below detection limit in 18WCA1 and 6.0 µM in 18WCA2 (Supplementary File 1). Micromolar concentrations of nitrate and/or ammonia have been previously reported LGB springs (Havig et al, 2021;Holloway et al, 2011), and thus we expect 2017 samples would have had similar concentrations. It is possible that unmeasured parameters and/or biogeography are primary predictors of the characteristic extremely thermophilic green filaments in these springs.…”
Section: (Fig 1 Tablementioning
confidence: 70%
“…Nitrate was detectable in both samples (14.3 μM), while ammonium was below detection limit in 18WCA1 and 6.0 μM in 18WCA2 ( Data Set S1 ). Micromolar concentrations of nitrate and/or ammonia have been previously reported in Lower Geyser Basin springs ( 31 , 32 ), and thus we expect that 2017 samples would have had similar concentrations. It is possible that unmeasured parameters and/or biogeography are primary predictors of the characteristic extremely thermophilic green filaments in these springs.…”
Section: Resultsmentioning
confidence: 69%
“…For the ∼500 geysing hot springs in YNP ( 9 , 10 ), eruption periodicities range from regular (e.g., Old Faithful is ∼91 to 93 min) to chaotic (e.g., Steamboat Geyser can vary from 3 days to 50 years [ 11 ]). Here, we examined phototrophic community composition coupled to rates of light-dependent C assimilation (via 13 C-labeled bicarbonate microcosms) in the outflow channels of two eruptive hot springs with similar geochemical profiles ( 12 ) (see Table S1 in the supplemental material): Flat Cone (FC) and an unnamed feature we colloquially named “The Jolly Jelly” (JJ; YNP Thermal Feature Inventory ID LFMNN010) in LGB, YNP ( Fig. 1 ; Fig.…”
Section: Observationmentioning
confidence: 99%