{"refrec":{"BRefID":75740,"RR":"<b>Jordan, M.B.; Joint, I.R.</b> (1984). Studies on phytoplankton distribution and primary production in the western English Channel in 1980 and 1981. <i>Cont. Shelf Res. 3(1)</i>: 25-34. <a href=\"https://dx.doi.org/10.1016/0278-4343(84)90041-4\" target=\"_blank\">https://dx.doi.org/10.1016/0278-4343(84)90041-4</a>","BEntID":71421,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Cont. Shelf Res. 3(1)</i>: 25-34. <a href=\"https://dx.doi.org/10.1016/0278-4343(84)90041-4\" target=\"_blank\">https://dx.doi.org/10.1016/0278-4343(84)90041-4</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Jordan, M.B.; Joint, I.R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Jordan, M.B.; Joint, I.R.","Englishabstract":"The distribution of chlorophyll on a transect of the English Channel was measured during 1980 and 1981. In both years, high concentrations of chlorophyll a were measured in mid-channel in July and August and this was due to a bloom of <i>Gyrodinium aureolum</i>. At a near-shore station close to Plymouth, regular measurements of water transparency and primary production were made during 1981. Values of diffuse attenuation coefficient increased in the spring with increasing chlorophyll concentration; this was followed by a period of low attenuation coefficients when chlorophyll maxima developed on the thermocline. The attenuation coefficient was greatly increased in late summer as the result of a bloom of <i>G. Aureolum</i>. 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