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Article: A compendium of geochemical information from the Saanich Inlet water column

TitleA compendium of geochemical information from the Saanich Inlet water column
Authors
Issue Date2017
Citation
Scientific Data, 2017, v. 4, article no. 170159, p. 1-10 How to Cite?
Abstract© The Author(s) 2017. Extensive and expanding oxygen minimum zones (OMZs) exist at variable depths in coastal and open ocean waters. As oxygen levels decline, nutrients and energy are increasingly diverted away from higher trophic levels into microbial community metabolism, resulting in fixed nitrogen loss and production of climate active trace gases including nitrous oxide and methane. While ocean deoxygenation has been reported on a global scale, our understanding of OMZ biology and geochemistry is limited by a lack of time-resolved data sets. Here, we present a historical dataset of oxygen concentrations spanning fifty years and nine years of monthly geochemical time series 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 geochemical framework for evaluating long-term trends in biogeochemical cycling in OMZ waters.
Persistent Identifierhttp://hdl.handle.net/10722/269771
ISSN
2017 Impact Factor: 5.311

 

DC FieldValueLanguage
dc.contributor.authorTorres-Beltrán, Mónica-
dc.contributor.authorHawley, Alyse K.-
dc.contributor.authorCapelle, David-
dc.contributor.authorZaikova, Elena-
dc.contributor.authorWalsh, David A.-
dc.contributor.authorMueller, Andreas-
dc.contributor.authorScofield, Melanie-
dc.contributor.authorPayne, Chris-
dc.contributor.authorPakhomova, Larysa-
dc.contributor.authorKheirandish, Sam-
dc.contributor.authorFinke, Jan-
dc.contributor.authorBhatia, Maya-
dc.contributor.authorShevchuk, Olena-
dc.contributor.authorGies, Esther A.-
dc.contributor.authorFairley, Diane-
dc.contributor.authorMichiels, Céline-
dc.contributor.authorSuttle, Curtis A.-
dc.contributor.authorWhitney, Frank-
dc.contributor.authorCrowe, Sean A.-
dc.contributor.authorTortell, Philippe D.-
dc.contributor.authorHallam, Steven J.-
dc.date.accessioned2019-04-30T01:49:32Z-
dc.date.available2019-04-30T01:49:32Z-
dc.date.issued2017-
dc.identifier.citationScientific Data, 2017, v. 4, article no. 170159, p. 1-10-
dc.identifier.issn2052-4463-
dc.identifier.urihttp://hdl.handle.net/10722/269771-
dc.description.abstract© The Author(s) 2017. Extensive and expanding oxygen minimum zones (OMZs) exist at variable depths in coastal and open ocean waters. As oxygen levels decline, nutrients and energy are increasingly diverted away from higher trophic levels into microbial community metabolism, resulting in fixed nitrogen loss and production of climate active trace gases including nitrous oxide and methane. While ocean deoxygenation has been reported on a global scale, our understanding of OMZ biology and geochemistry is limited by a lack of time-resolved data sets. Here, we present a historical dataset of oxygen concentrations spanning fifty years and nine years of monthly geochemical time series 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 geochemical framework for evaluating long-term trends in biogeochemical cycling in OMZ waters.-
dc.languageeng-
dc.relation.ispartofScientific Data-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.titleA compendium of geochemical information from the Saanich Inlet water column-
dc.typeArticle-
dc.description.naturepublished_or_final_version-
dc.identifier.doi10.1038/sdata.2017.159-
dc.identifier.pmid29087371-
dc.identifier.scopuseid_2-s2.0-85032618629-
dc.identifier.volume4-
dc.identifier.spagearticle no. 170159, p. 1-
dc.identifier.epagearticle no. 170159, p. 10-

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