TY - JOUR
T1 - The effect of O2 and pressure on thiosulfate oxidation by Thiomicrospira thermophila
AU - Houghton, Jennifer L.
AU - Foustoukos, Dionysis I.
AU - Fike, David A.
N1 - Funding Information:
We thank Costa Vetriani for generously providing us strain EPR 85. The authors thank several anonymous reviewers for thoughtful and constructive comments on an earlier version of this manuscript. This research was supported by funding to D.A.F. and J.L.H. from NSF (OCE-1155346; EAR-1124389) and to D.F. from NSF (OCE-1155246; MCB-1517560) and from Venture Grant #10877 from CIW. This manuscript is C-DEBI contribution 477 for DF.
Publisher Copyright:
© 2019 John Wiley & Sons Ltd
PY - 2019
Y1 - 2019
N2 - Microbial sulfur cycling in marine sediments often occurs in environments characterized by transient chemical gradients that affect both the availability of nutrients and the activity of microbes. High turnover rates of intermediate valence sulfur compounds and the intermittent availability of oxygen in these systems greatly impact the activity of sulfur-oxidizing micro-organisms in particular. In this study, the thiosulfate-oxidizing hydrothermal vent bacterium Thiomicrospira thermophila strain EPR85 was grown in continuous culture at a range of dissolved oxygen concentrations (0.04–1.9 mM) and high pressure (5–10 MPa) in medium buffered at pH 8. Thiosulfate oxidation under these conditions produced tetrathionate, sulfate, and elemental sulfur, in contrast to previous closed-system experiments at ambient pressure during which thiosulfate was quantitatively oxidized to sulfate. The maximum observed specific growth rate at 5 MPa pressure under unlimited O2 was 0.25 hr−1. This is comparable to the μmax (0.28 hr−1) observed at low pH (<6) at ambient pressure when T. thermophila produces the same mix of sulfur species. The half-saturation constant for O2 ((Formula presented.)) estimated from this study was 0.2 mM (at a cell density of 105 cells/ml) and was robust at all pressures tested (0.4–10 MPa), consistent with piezotolerant behavior of this strain. The cell-specific (Formula presented.) was determined to be 1.5 pmol O2/cell. The concentrations of products formed were correlated with oxygen availability, with tetrathionate production in excess of sulfate production at all pressure conditions tested. This study provides evidence for transient sulfur storage during times when substrate concentration exceeds cell-specific (Formula presented.) and subsequent consumption when oxygen dropped below that threshold. These results may be common among sulfur oxidizers in a variety of environments (e.g., deep marine sediments to photosynthetic microbial mats).
AB - Microbial sulfur cycling in marine sediments often occurs in environments characterized by transient chemical gradients that affect both the availability of nutrients and the activity of microbes. High turnover rates of intermediate valence sulfur compounds and the intermittent availability of oxygen in these systems greatly impact the activity of sulfur-oxidizing micro-organisms in particular. In this study, the thiosulfate-oxidizing hydrothermal vent bacterium Thiomicrospira thermophila strain EPR85 was grown in continuous culture at a range of dissolved oxygen concentrations (0.04–1.9 mM) and high pressure (5–10 MPa) in medium buffered at pH 8. Thiosulfate oxidation under these conditions produced tetrathionate, sulfate, and elemental sulfur, in contrast to previous closed-system experiments at ambient pressure during which thiosulfate was quantitatively oxidized to sulfate. The maximum observed specific growth rate at 5 MPa pressure under unlimited O2 was 0.25 hr−1. This is comparable to the μmax (0.28 hr−1) observed at low pH (<6) at ambient pressure when T. thermophila produces the same mix of sulfur species. The half-saturation constant for O2 ((Formula presented.)) estimated from this study was 0.2 mM (at a cell density of 105 cells/ml) and was robust at all pressures tested (0.4–10 MPa), consistent with piezotolerant behavior of this strain. The cell-specific (Formula presented.) was determined to be 1.5 pmol O2/cell. The concentrations of products formed were correlated with oxygen availability, with tetrathionate production in excess of sulfate production at all pressure conditions tested. This study provides evidence for transient sulfur storage during times when substrate concentration exceeds cell-specific (Formula presented.) and subsequent consumption when oxygen dropped below that threshold. These results may be common among sulfur oxidizers in a variety of environments (e.g., deep marine sediments to photosynthetic microbial mats).
KW - hydrothermal
KW - oxygen
KW - Thiomicrospira thermophila
KW - thiosulfate
UR - https://www.scopus.com/pages/publications/85067413188
U2 - 10.1111/gbi.12352
DO - 10.1111/gbi.12352
M3 - Article
C2 - 31180189
AN - SCOPUS:85067413188
SN - 1472-4677
VL - 17
SP - 564
EP - 576
JO - Geobiology
JF - Geobiology
IS - 5
ER -