1. Dark biological superoxide production as a significant flux and sink of marine dissolved oxygen
- Author
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Colleen M. Hansel, Kevin M. Sutherland, and Scott D. Wankel
- Subjects
010504 meteorology & atmospheric sciences ,Oceans and Seas ,Mehler reaction ,chemistry.chemical_element ,Oxygen cycle ,Photosynthesis ,01 natural sciences ,Redox ,Oxygen ,03 medical and health sciences ,chemistry.chemical_compound ,Earth, Atmospheric, and Planetary Sciences ,Superoxides ,Seawater ,14. Life underwater ,030304 developmental biology ,0105 earth and related environmental sciences ,reactive oxygen species ,chemistry.chemical_classification ,0303 health sciences ,Reactive oxygen species ,Multidisciplinary ,Chemistry ,Superoxide ,Oxygen evolution ,microbial superoxide ,Carbon ,13. Climate action ,Environmental chemistry ,Physical Sciences ,marine dissolved oxygen ,Oxidation-Reduction - Abstract
Significance Extracellular production of the reactive oxygen species (ROS) superoxide results from the one-electron reduction of O2. Nearly all major groups of marine microbes produce extracellular superoxide. In this global estimate of marine microbial superoxide production we determine that dark extracellular superoxide production is ultimately a net sink of dissolved oxygen comparable in magnitude to other major terms in the marine oxygen cycle. This abundant source of superoxide to the marine water column provides evidence that extracellular ROS play a significant role in carbon oxidation and the redox cycling of metals in marine environments. Consideration of this significant reductive flux of dissolved oxygen is essential for field, laboratory, and modeling techniques for determining productivity and oxygen utilization in marine systems., The balance between sources and sinks of molecular oxygen in the oceans has greatly impacted the composition of Earth’s atmosphere since the evolution of oxygenic photosynthesis, thereby exerting key influence on Earth’s climate and the redox state of (sub)surface Earth. The canonical source and sink terms of the marine oxygen budget include photosynthesis, respiration, photorespiration, the Mehler reaction, and other smaller terms. However, recent advances in understanding cryptic oxygen cycling, namely the ubiquitous one-electron reduction of O2 to superoxide by microorganisms outside the cell, remains unexplored as a potential player in global oxygen dynamics. Here we show that dark extracellular superoxide production by marine microbes represents a previously unconsidered global oxygen flux and sink comparable in magnitude to other key terms. We estimate that extracellular superoxide production represents a gross oxygen sink comprising about a third of marine gross oxygen production, and a net oxygen sink amounting to 15 to 50% of that. We further demonstrate that this total marine dark extracellular superoxide flux is consistent with concentrations of superoxide in marine environments. These findings underscore prolific marine sources of reactive oxygen species and a complex and dynamic oxygen cycle in which oxygen consumption and corresponding carbon oxidation are not necessarily confined to cell membranes or exclusively related to respiration. This revised model of the marine oxygen cycle will ultimately allow for greater reconciliation among estimates of primary production and respiration and a greater mechanistic understanding of redox cycling in the ocean.
- Published
- 2020