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→Aquatic hypoxia: Consensus phrasing that most fish rely on "both nutrients and oxygen for their chemical energy". |
IpseCustos (talk | contribs) remove ref, claims per WP:FRINGE. See WP:COIN discussion. |
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{{see also|ocean deoxygenation}}
'''Oxygen depletion''' is a phenomenon that occurs in aquatic environments as [[oxygen|dissolved oxygen]] ('''DO'''; molecular oxygen dissolved in the water) becomes reduced in concentration to a point where it becomes detrimental to aquatic organisms living in the system. Dissolved oxygen is typically expressed as a percentage of the oxygen that would dissolve in the water at the prevailing temperature and salinity (both of which affect the solubility of oxygen in water; see [[oxygen saturation]] and [[underwater]]). An aquatic system lacking dissolved oxygen (0% saturation) is termed anaerobic, [[Reducing environment|reducing]], or '''[[Anoxic waters|anoxic]]'''; a system with low concentration—in the range between 1 and 30% saturation—is called '''hypoxic''' or '''dysoxic'''. Most fish cannot live below 30% saturation since they rely on
Hypoxia can occur throughout the water column and also at high altitudes as well as near sediments on the bottom. It usually extends throughout 20-50% of the water column, but depends on the water depth and location of pycnoclines (rapid changes in water density with depth). It can occur in 10-80% of the water column. For example, in a 10-meter water column, it can reach up to 2 meters below the surface. In a 20-meter water column, it can extend up to 8 meters below the surface.<ref>Rabalais, Nancy; Turner, R. Eugene; Justic´, Dubravko; Dortch, Quay; Wiseman, William J. Jr. Characterization of Hypoxia: Topic 1 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico. Ch. 3. NOAA Coastal Ocean Program, Decision Analysis Series No. 15. May 1999. < http://oceanservice.noaa.gov/products/hypox_t1final.pdf >. Retrieved February 11, 2009.</ref>
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