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Hypoxia (environmental): Difference between revisions

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→‎Aquatic hypoxia: Consensus phrasing that most fish rely on "both nutrients and oxygen for their chemical energy".
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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 both nutrients and oxygen forto their chemicalderive energy.<ref name="Schmidt-Rohrfrom 20">their Schmidt-Rohr, Knutrients. (2020). "Oxygen Is the High-Energy Molecule Powering Complex Multicellular Life: Fundamental Corrections to Traditional Bioenergetics". ''ACS Omega'' '''5''': 2221-2233. http://dx.doi.org/10.1021/acsomega.9b03352. </ref> Hypoxia leads to impaired reproduction of remaining fish via [[endocrine disruptor|endocrine disruption]].<ref>Wu, R. et al. 2003. [https://www.researchgate.net/publication/231277909_Aquatic_Hypoxia_Is_an_Endocrine_Disruptor_and_Impairs_Fish_Reproduction Aquatic Hypoxia Is an Endocrine Disruptor and Impairs Fish Reproduction]</ref> A "healthy" aquatic environment should seldom experience less than 80% saturation. The '''exaerobic''' zone is found at the boundary of anoxic and hypoxic zones.
 
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>