{"refrec":{"BRefID":324246,"RR":"<b>Zehr, J.P.; Capone, D.G.</b> (2020). Changing perspectives in marine nitrogen fixation. <i>Science (Wash.) 368(6492)</i>: eaay9514. <a href=\"https://dx.doi.org/10.1126/science.aay9514\" target=\"_blank\">https://dx.doi.org/10.1126/science.aay9514</a>","BEntID":317722,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 368(6492)</i>: eaay9514. <a href=\"https://dx.doi.org/10.1126/science.aay9514\" target=\"_blank\">https://dx.doi.org/10.1126/science.aay9514</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Zehr, J.P.; Capone, D.G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Zehr, J.P.; Capone, D.G.","Englishabstract":"As a component of many biomolecules, nitrogen is a crucial element for life, especially in nutrient-poor environs such as the open ocean. Atmospheric dinitrogen gas (N<sub>2</sub>) is abundant but must be fixed by reduction to ammonia, a process limited to certain organisms and environments. Zehr and Capone review changes in our understanding of what marine microorganisms are fixing N<sub>2</sub>, where they live, and what environmental features influence their activity. N<sub>2</sub> fixation is more widely distributed than previously thought, and we still have much to learn about the physiology and regulation involved. We now have better estimates of global- and basin-scale inputs and outputs, but questions remain as to whether the oceanic N cycle is balanced. 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