Metagenome of a Versatile Chemolithoautotroph from Expanding Oceanic Dead Zones

Life in Dead Zones Oxygen minimum zones, or oceanic “dead zones,” are expanding. Marine dead zone expansion and intensification results in amplification of biological nitrogen and greenhouse gas production, with implications for marine fisheries' productivity and for climate balance. Little is known about the microbial communities mediating the underlying biogeochemistry of dead zones. Walsh et al. (p. 578) present metagenomic analyses of a ubiquitous, abundant, and uncultivated bacterium in oceanic dead zones. Similar bacteria, related to chemoautotrophic gill symbionts of deep-sea clams and mussels, play a role in sulfide detoxification in African shelf waters. Reconstruction of the carbon and energy metabolism of this enigmatic lineage revealed a metabolic repertoire mediating carbon sequestration, sulfur-detoxification, and biological nitrogen loss in oxygen-deficient oceanic waters. An abundant microbe in oxygen-deficient oceanic waters reveals its redox-driven niche specialization. Oxygen minimum zones, also known as oceanic “dead zones,” are widespread oceanographic features currently expanding because of global warming. Although inhospitable to metazoan life, they support a cryptic microbiota whose metabolic activities affect nutrient and trace gas cycling within the global ocean. Here, we report metagenomic analyses of a ubiquitous and abundant but uncultivated oxygen minimum zone microbe (SUP05) related to chemoautotrophic gill symbionts of deep-sea clams and mussels. The SUP05 metagenome harbors a versatile repertoire of genes mediating autotrophic carbon assimilation, sulfur oxidation, and nitrate respiration responsive to a wide range of water-column redox states. Our analysis provides a genomic foundation for understanding the ecological and biogeochemical role of pelagic SUP05 in oxygen-deficient oceanic waters and its potential sensitivity to environmental changes.

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