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Summer oxygen depletion in a diked New England estuary

January 1, 1991

The diked and freshened Herring River estuary (Wellfleet, Massachusetts) experiences regular summer hypoxia and one- to three-week periods of main stream anoxia, often accompanied by fish kills. Stream hypoxia results from the temperature-dependent increase in oxygen demand of organic matter released by diked salt marsh deposits; periods of total anoxial are induced by heavy rains which increase the runoff of wetland organic matter. Historic reductions in tidal flushing have extended the low salinity region of the estuary normally characterized by high organic loads and minimal flushing. Recurrent main stream anoxia has depressed both migratory and resident aquatic fauna.

Publication Year 1991
Title Summer oxygen depletion in a diked New England estuary
DOI 10.2307/1351685
Authors J. W. Portnoy
Publication Type Article
Publication Subtype Journal Article
Series Title Estuaries
Index ID 5223270
Record Source USGS Publications Warehouse
USGS Organization Patuxent Wildlife Research Center