{"refrec":{"BRefID":364010,"RR":"<b>Yamashita, Y.; Mori, Y.; Ogawa, H.</b> (2023). Hydrothermal-derived black carbon as a source of recalcitrant dissolved organic carbon in the ocean. <i>Science Advances 9(6)</i>: eade3807. <a href=\"https://dx.doi.org/10.1126/sciadv.ade3807\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.ade3807</a>","BEntID":361730,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Science Advances 9(6)</i>: eade3807. <a href=\"https://dx.doi.org/10.1126/sciadv.ade3807\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.ade3807</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Yamashita, Y.; Mori, Y.; Ogawa, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Yamashita, Y.; Mori, Y.; Ogawa, H.","Englishabstract":"Deep-sea hydrothermal vents are a possible source of thermogenic dissolved black carbon (DBC), which is a component of recalcitrant dissolved organic carbon, but little is known about the distribution of hydrothermal DBC in the deep ocean. Here, we show basin-scale distributions of DBC along two transects in the eastern Pacific Ocean, which are located outside the jet-like hydrothermal plumes from the East Pacific Rise. The DBC concentration in the deep waters did not show a strong linear relationship with apparent oxygen utilization (AOU), as previously observed in the central and western Pacific Ocean. Deviations in DBC concentration from the DBC-AOU relationship observed in the central and western Pacific Ocean were quantified. The deviation was linearly correlated with excess 3He, a tracer for hydrothermal input, indicating that a fraction of the DBC in the deep ocean is transported long distances from hydrothermal systems.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Hydrothermal-derived black carbon as a source of recalcitrant dissolved organic carbon in the ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2023,"MonPub":null,"DateUpdate":"2023-05-04","DateCreate":"2023-05-04","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000937229100005","VABBcode":null,"OpenAcc":1,"DOI":"10.1126/sciadv.ade3807"},"refs":null,"anarec":{"AnaID":364010,"PubliDate":2023,"Pagination":"eade3807","XtraPublOfAnaID":null,"ISBN":null,"Volume":"9","Issue":"6","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":248966,"SerRR":"Science Advances. 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