{"refrec":{"BRefID":317812,"RR":"<b>Blattmann, T.M.; Liu, Z.; Zhang, Y.; Zhao, Y.; Haghipour, N.; Montluçon, D.B.; Plötze, M.; Eglinton, T.I.</b> (2019). Mineralogical control on the fate of continentally derived organic matter in the ocean. <i>Science (Wash.) 366(6466)</i>: 742-745. <a href=\"https://dx.doi.org/10.1126/science.aax5345\" target=\"_blank\">https://dx.doi.org/10.1126/science.aax5345</a>","BEntID":311249,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 366(6466)</i>: 742-745. <a href=\"https://dx.doi.org/10.1126/science.aax5345\" target=\"_blank\">https://dx.doi.org/10.1126/science.aax5345</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Blattmann, T.M.; Liu, Z.; Zhang, Y.; Zhao, Y.; Haghipour, N.; Montluçon, D.B.; Plötze, M.; Eglinton, T.I.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Blattmann, T.M. <i>et al.</i>","Englishabstract":"First-order relationships between organic matter content and mineral surface area have been widely reported and are implicated in stabilization and long-term preservation of organic matter. However, the nature and stability of organomineral interactions and their connection with mineralogical composition have remained uncertain. In this study, we find that continentally derived organic matter of pedogenic origin is stripped from smectite mineral surfaces upon discharge, dispersal, and sedimentation in distal ocean settings. In contrast, organic matter sourced from ancient rocks that is tightly associated with mica and chlorite endures in the marine realm. 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