{"refrec":{"BRefID":321632,"RR":"<b>Nayak, A.R.; Twardowski, M.S.</b> (2020). “Breaking” news for the ocean's carbon budget. <i>Science (Wash.) 367(6479)</i>: 738-739. <a href=\"https://dx.doi.org/10.1126/science.aba7109\" target=\"_blank\">https://dx.doi.org/10.1126/science.aba7109</a>","BEntID":315072,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 367(6479)</i>: 738-739. <a href=\"https://dx.doi.org/10.1126/science.aba7109\" target=\"_blank\">https://dx.doi.org/10.1126/science.aba7109</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Nayak, A.R.; Twardowski, M.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Nayak, A.R.; Twardowski, M.S.","Englishabstract":"Oceans play a critical role in Earth's carbon cycle. Quantifying essential processes in carbon cycling and extending these to future predictions remain great scientific challenges. Nearly 30% of anthropogenic carbon is absorbed from the atmosphere into the ocean, where sempiternal, ubiquitous populations of microscopic particles transport carbon into the isolated deep sea (1). This complex pathway is driven by various biophysical and chemical interactions, including phytoplankton productivity, zooplankton grazing, oceanic mixing and turbulence, advection, and the sinking of particles and aggregates (2) (see the figure). On page 791 of this issue, Briggs et al. 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