Declining oxygen in the global ocean and coastal waters

Denise Breitburg, Lisa A. Levin, Andreas Oschlies, Marilaure Grégoire, Francisco P. Chavez, Daniel J. Conley, Véronique Garçon, Denis Gilbert, Dimitri Gutiérrez, Kirsten Isensee, Gil S. Jacinto, Karin E. Limburg, Ivonne Montes, S. W.A. Naqvi, Grant C. Pitcher, Nancy N. Rabalais, Michael R. Roman, Kenneth A. Rose, Brad A. Seibel, Maciej TelszewskiMoriaki Yasuhara, Jing Zhang

Research output: Journal Publications and ReviewsComment/debate

2341 Citations (Scopus)

Abstract

Oxygen is fundamental to life. Not only is it essential for the survival of individual animals, but it regulates global cycles of major nutrients and carbon. The oxygen content of the open ocean and coastal waters has been declining for at least the past half-century, largely because of human activities that have increased global temperatures and nutrients discharged to coastal waters. These changes have accelerated consumption of oxygen by microbial respiration, reduced solubility of oxygen in water, and reduced the rate of oxygen resupply from the atmosphere to the ocean interior, with a wide range of biological and ecological consequences. Further research is needed to understand and predict long-term, global-and regional-scale oxygen changes and their effects on marine and estuarine fisheries and ecosystems.
Original languageEnglish
Article numbereaam7240
JournalScience
Volume359
Issue number6371
DOIs
Publication statusPublished - 5 Jan 2018
Externally publishedYes

Bibliographical note

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Funding

We thank IOC-UNESCO for financial support and for initiating and supporting the Global Ocean Oxygen Network. We also thank R. Diaz for help with updating the list of coastal sites that have reported hypoxia (Fig. 1A); B. Michael and M. Trice of the Maryland Department of Natural Resources for help with the Maryland water quality database; and our many current and past collaborators on deoxygenation research in coastal systems, OMZs, the Black Sea, and elsewhere. Funding was provided by National Oceanic and Atmospheric Administration (NOAA)–Center for Sponsored Coastal Ocean Research grant NA10NOS4780138 and Maryland Sea Grant SA75281450-P (to D.B.), NSF-EAR grant 1324095 (to L.A.L.), the Deutsche Forschungsgemeinschaft via grant SFB754 (to A.O.), and the Fonds National de la Recherche Scientifique and the BENTHOX program grant T.1009.15 (to M.G.). This study was partly supported by the BONUS COCOA project (grant 2112932-1), funded jointly by the European Union and the Swedish Research Council for Environment, Agricultural Sciences and Spatial Planning.

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