{"refrec":{"BRefID":37583,"RR":"<b>Peelen, R.</b> (1974). Changes in the plankton of the estuarine area of the Haringvliet-Hollands Diep-Biesbosch in the S.W. Netherlands caused by the dams through Volkerak and Haringvliet. <i>Hydrobiol. Bull. 8(1-2)</i>: 190-200. <a href=\"https://dx.doi.org/10.1007/BF02254919\" target=\"_blank\">https://dx.doi.org/10.1007/BF02254919</a>","BEntID":37583,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Hydrobiol. Bull. 8(1-2)</i>: 190-200. <a href=\"https://dx.doi.org/10.1007/BF02254919\" target=\"_blank\">https://dx.doi.org/10.1007/BF02254919</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":1,"TerrestrialFlag":0,"Authorstring":"Peelen, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Peelen, R.","Englishabstract":"(1) Owing to its, partially, man-made character, the former Hollands Diep-Haringvliet area was a digital estuary with rather unique characters. The ß-mesohaline protruded beyond the coast line. The fairly large, glacier-fed Rhine discharge in summer reduces the residual times in this estuary to low values, with a poor development of the plankton as a result. 2) After the closure of the Volkerak and the Haringvliet (1970) residual times increased to 30–40 days in summer and in 1971 a diatom plankton, with <i>Asterionella Formosa</i> and <i>Fragillaria crotonensis</i> developed. In 1972 the blue-green algae <i>Microcystis aeruginosa</i> and <i>Aphanizomenon flos-aquae</i> made their entrance. (3) Developments of biota within the biotope are in full progress at the moment, and, in view of the heavy phosphate level, blue-green algae stand a good chance to dominate the plankton, as they already do in Lake Brielle.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Changes in the plankton of the estuarine area of the Haringvliet-Hollands Diep-Biesbosch in the S.W. 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