{"refrec":{"BRefID":69963,"RR":"<b>LaRoche, J.; Breitbarth, E.</b> (2005). Importance of the diazotrophs as a source of new nitrogen in the ocean. <i>J. Sea Res. 53(1-2)</i>: 67-91. <a href=\"https://dx.doi.org/10.1016/j.seares.2004.05.005\" target=\"_blank\">https://dx.doi.org/10.1016/j.seares.2004.05.005</a>","BEntID":66029,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>J. Sea Res. 53(1-2)</i>: 67-91. <a href=\"https://dx.doi.org/10.1016/j.seares.2004.05.005\" target=\"_blank\">https://dx.doi.org/10.1016/j.seares.2004.05.005</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"LaRoche, J.; Breitbarth, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"LaRoche, J.; Breitbarth, E.","Englishabstract":"Nitrogen fixation is one of the important biochemical pathways that play a role in controlling the oceanic nitrogen inventory. Here we review nitrogen fixation in the ocean, with a particular emphasis on <i>Trichodesmium</i>, one of the dominant marine diazotrophs. Distribution data for diazotrophs are scarce, except in specific regions where <i>Trichodesmium</i> is known to bloom. Although some regions are clearly under-sampled, <i>Trichodesmium</i> can generally be found in tropical regions where temperature is at least 20 °C, except in the North Atlantic, where drift to higher latitudes is possible via the Gulf Stream. Likewise, biomass estimates are problematic because of the colony-forming habit of this organism. <i>Trichodesmium</i> grows slowly with reported maximum growth rates of approximately 0.14 d-1. Studies of the photosynthetic physiology indicate that <i>Trichodesmium</i> can tolerate high light intensity with Ik and Ic values of 300 and 140 μmole photons m<sup>−2</sup> s<sup>−1</sup>, respectively. Review of the elemental composition of <i>Trichodesmium</i> indicates that the C:N molar ratio of 6.3:1 does not depart significantly from the predicted Redfield stoichiometry of 6.6:1. Overall, measured N:P ratios from the field and the laboratory were around 50, a significant departure from the Redfield stoichiometry of 16:1. Whether this indicates phosphorus limitation is not clear at present. The iron requirements of diazotrophs in general and of <i>Trichodesmium</i> in particular have been the subject of debate, but some recent laboratory studies have converged on Fe:C (μmole:mole) of approximately 50 at 70% of the maximum growth rates (μmax) to 250 at μmax for this species. There is a noticeable lack of information on growth rate as a function of phosphorus and fixed nitrogen sources. Although <i>Trichodesmium</i> is a non-heterocystous cyanobacterium, carbon and nitrogen fixation co-occur during the light period, indicating that light energy is required for both of these processes. This is likely to be achieved through cellular differentiation of the trichomes and a tight control of the temporal expression of many biochemical pathways. A summary table presents a set of values for the initial parameterisation of parameters relevant to the incorporation of nitrogen fixation in biological and biogeochemical models.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Importance of the diazotrophs as a source of new nitrogen in the ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-04 01:30:54.242140","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"marine diazotrophs; Trichodesmium; biogeochemical modelling; iron","OtherDescriptors":"Marine diazotrophs; Trichodesmium; Biogeochemical modelling; Iron","Notes":null,"AnaPub":2005,"MonPub":null,"DateUpdate":"2021-02-19","DateCreate":"2005-01-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000226392000005","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.seares.2004.05.005"},"refs":null,"anarec":{"AnaID":69963,"PubliDate":2005,"Pagination":"67-91","XtraPublOfAnaID":null,"ISBN":null,"Volume":"53","Issue":"1-2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43261,"SerRR":"Journal of Sea Research. Elsevier/Netherlands Institute for Sea Research: Amsterdam; Den Burg.  ISSN 1385-1101; e-ISSN 1873-1414","StandardTitleSer":"Journal of Sea Research","ISSN":"1385-1101","AbbrevSer":"J. Sea Res.","StandardTitleMon":null,"StartPage":67,"Pages":25,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":[{"YBRefID":69946,"RefStrFull":"<b>Veldhuis, M.J.W. (Ed.)</b> (2005). Iron resources and oceanic nutrients: advancement of global environmental simulations. <i>Journal of Sea Research</i>, 53(1-2). 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