Journal
SCIENTIFIC DATA
Volume 4, Issue -, Pages -Publisher
NATURE PUBLISHING GROUP
DOI: 10.1038/sdata.2017.160
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Funding
- US Department of Energy (DOE)
- Office of Science of the U.S. Department of Energy [DE-AC02- 05CH11231]
- G. Unger Vetlesen Foundation
- Ambrose Monell Foundation
- Tula Foundation
- Canadian Institute for Advanced Research
- NSERC
- W.R Wiley Environmental Molecular Sciences Laboratory (EMSL)
- US DOE's Office of Biological and Environmental Research
- Consejo Nacional de Ciencia y Tecnologia (CONACyT)
- Natural Sciences and Engineering Research Council of Canada
- Genome British Columbia
- Canada Foundation for Innovation
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Marine oxygen minimum zones (OMZs) are widespread regions of the ocean that are currently expanding due to global warming. While inhospitable to most metazoans, OMZs are hotspots for microbial mediated biogeochemical cycling of carbon, nitrogen and sulphur, contributing disproportionately to marine nitrogen loss and climate active trace gas production. Our current understanding of microbial community responses to OMZ expansion is limited by a lack of time-resolved data sets linking multi-omic sequence information (DNA, RNA, protein) to geochemical parameters and process rates. Here, we present six years of time-resolved multi-omic observations in Saanich Inlet, a seasonally anoxic fjord on the coast of Vancouver Island, British Columbia, Canada that undergoes recurring changes in water column oxygenation status. This compendium provides a unique multi-omic framework for studying microbial community responses to ocean deoxygenation along defined geochemical gradients in OMZ waters.
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