Abstract

Hydrogen peroxide (H2O2), superoxide (O2•-), and hydroxyl radicals (OH•) are produced in natural waters via ultraviolet (UV) light-induced reactions between dissolved oxygen (O2) and organic carbon, and further reaction of H2O2 and Fe(II) (i.e., Fenton chemistry). The temporal and spatial dynamics of H2O2 and other dissolved compounds (Fe(II), Fe(III), H2S, O2) were measured during a diel cycle (dark/light) in surface waters of three acidic geothermal springs (Beowulf Spring, One Hundred Springs Plain, and Echinus Geyser Spring; pH = 3-3.5, T = 68-80 °C) in Norris Geyser Basin, Yellowstone National Park. In situ analyses showed that H2O2 concentrations were lowest (ca. 1 μM) in geothermal source waters containing high dissolved sulfide (and where oxygen was below detection) and increased by two-fold (ca. 2-3 μM) in oxygenated waters corresponding to Fe(III)-oxide mat formation down the water channel. Small increases in dissolved oxygen and H2O2 were observed during peak photon flux, but not consistently across all springs sampled. Iron-oxide microbial mats were sampled for molecular analysis of ROS gene expression in two primary autotrophs of acidic Fe(III)-oxide mat ecosystems: Metallosphaera yellowstonensis (Archaea) and Hydrogenobaculum sp. (Bacteria). Expression (RT-qPCR) assays of specific stress-response genes (e.g., superoxide dismutase, peroxidases) of the primary autotrophs were used to evaluate possible changes in transcription across temporal, spatial and/or seasonal samples. Data presented here documented the presence of H2O2 and general correlation with dissolved oxygen. Moreover, two dominant microbial populations expressed ROS response genes throughout the day, but showed less expression of key genes during peak sunlight. Oxidative stress response genes (especially external peroxidases) were highly-expressed in microorganisms within Fe(III)-oxide mat communities, suggesting a significant role for these proteins during survival and growth in situ.

Highlights

  • Hydrogen peroxide (H2O2) is a central reactive oxygen species (ROS) in the global cycle of oxygen (O2), and is thought to have been a precursor to O2 via abiotic reactions in early Earth (Slesak et al, 2012)

  • Spatial and temporal changes in H2O2 and other dissolved chemical species were assessed over diel cycles in 2014 and 2015, and provide the first insight regarding concentrations of H2O2 in acidic Fe(III)-oxide depositing geothermal springs of YNP

  • The observed range in H2O2 values in acidic geothermal systems is higher than previously observed in a limited set of thermal systems supporting phototrophic activity (

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Summary

Introduction

Hydrogen peroxide (H2O2) is a central reactive oxygen species (ROS) in the global cycle of oxygen (O2), and is thought to have been a precursor to O2 via abiotic reactions in early Earth (Slesak et al, 2012). Once hydrogen peroxide is formed, hydroxyl radicals (OH) are produced via the reaction of H2O2 and ferrous iron [Fe(II)], (i.e., Fenton reaction, Equation 3), which can lead to the precipitation of highly-insoluble ferric iron [Fe(III)]oxyhydroxides (Winterbourn, 1995; Wilson et al, 2000a; Kocar and Inskeep, 2003)

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