{"refrec":{"BRefID":296455,"RR":"Li, W.K.W.; Dickie, P.M.; Irwin, B.D.; Wood, A.M. (1992). Biomass of bacteria, cyanobacteria, prochlorophytes and photosynthetic eukaryotes in the Sargasso Sea. Deep-Sea Res. A 39(3-4): 501-519. https://dx.doi.org/10.1016/0198-0149(92)90085-8","BEntID":288544,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". Deep-Sea Res. A 39(3-4): 501-519. https://dx.doi.org/10.1016/0198-0149(92)90085-8","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Li, W.K.W.; Dickie, P.M.; Irwin, B.D.; Wood, A.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Li, W.K.W. et al.","Englishabstract":"Bacteria, cyanobacteria, prochlorophytes and photosynthetic eukaryotes were enumerated in depth profiles at a station in the northern Sargasso Sea occupied for 9 days during September 1988. Carbon biomass of each group was inferred from cell abundance using conversion factors taken from the literature. Over the upper 200 m in the water column, carbon biomass occurred in the approximate proportion of 1:2:4:8 for cyanobacteria:prochlorophytes:photosynthetic eukaryotes:bacteria. Taken together, the three phytoplankton groups represented about the same amount of carbon biomass as the bacteria. This conclusion was validated by the independent measure of bulk chlorophyll a (Chl a) if the carbon:Chl a ratio was assumed to be about 44 in the nitrate-depleted layer and about 15 in the nitrate-rich layer. In reporting the biomass co-dominance of bacteria and phytoplankton, we do not deny that bacteria may dominate phytoplankton at other times and places in the oligotrophic ocean. Biomass co-dominance between these two trophic groups admits the possibility that oligotrophic bacterial assemblages may have high growth rates.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Biomass of bacteria, cyanobacteria, prochlorophytes and photosynthetic eukaryotes in the Sargasso Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-09 01:31:57.768626","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1992,"MonPub":null,"DateUpdate":"2018-05-30","DateCreate":"2018-05-30","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1992HR30900007","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/0198-0149(92)90085-8"},"refs":null,"anarec":{"AnaID":296455,"PubliDate":1992,"Pagination":"501-519","XtraPublOfAnaID":null,"ISBN":null,"Volume":"39","Issue":"3-4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":75243,"SerRR":"Deep-Sea Research, Part A. 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