{"refrec":{"BRefID":209327,"RR":"<b>Krylov, A.; Khlystov, O.; Zemskaya, T.; Minami, H.; Hachikubo, A.; Nunokawa, Y.; Kida, M.; Shoji, H.; Naudts, L.; Poort, J.; Pogodaeva, T.</b> (2008). First discovery and formation process of authigenic siderite from gas hydrate–bearing mud volcanoes in fresh water: Lake Baikal, eastern Siberia. <i>Geophys. Res. Lett. 35(5)</i>: 6 pp. <a href=\"http://dx.doi.org/10.1029/2007GL032917\" target=\"_blank\">dx.doi.org/10.1029/2007GL032917</a>","BEntID":201312,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 35(5)</i>: 6 pp. <a href=\"https://dx.doi.org/10.1029/2007GL032917\" target=\"_blank\">https://dx.doi.org/10.1029/2007GL032917</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Krylov, A.; Khlystov, O.; Zemskaya, T.; Minami, H.; Hachikubo, A.; Nunokawa, Y.; Kida, M.; Shoji, H.; Naudts, L.; Poort, J.; Pogodaeva, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Krylov, A. <i>et al.</i>","Englishabstract":"We report on the first authigenic siderite (FeCO<sub>3</sub>) concretions recovered from near-bottom sediments at gas hydrate-bearing mud volcanoes in fresh water (Lake Baikal, Eastern Siberia). The carbonates appear as firm ‘plate-type’ formations at the Malenky mud volcano (Southern Baikal Basin) and as soft nodules at the K-2 mud volcano (Central Baikal Basin). Calcium is the main divalent component which substitutes iron in the carbonate lattice (7 to 20 mol%). The d<sup> 13</sup>C values of the carbonates (+3.3 to +6.8‰ at Malenky, and +16.5 to +21.9‰ PDB at K-2) indicate that their formation is due to methanogenesis. The latter was most likely caused by the microbial methyl-type (acetate) fermentation that is suggested from the isotopic composition of the accompanying methane hydrates and dissolved methane. General depletion of the siderites in <sup>18</sup>O (-11.6 to -9.9 ‰ at Malenky, and -13.9 to -12.3‰ PDB at K-2) is mainly inherited from the isotope composition of pore water (-15.2 to -15.4‰ SMOW) at ambient temperature (3.5°C).","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"First discovery and formation process of authigenic siderite from gas hydrate–bearing mud volcanoes in fresh water: Lake Baikal, eastern Siberia","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":2008,"MonPub":null,"DateUpdate":"2014-11-06","DateCreate":"2011-11-07","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000254165000005","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2007GL032917"},"refs":null,"anarec":{"AnaID":209327,"PubliDate":2008,"Pagination":"6 pp.","XtraPublOfAnaID":null,"ISBN":null,"Volume":"35","Issue":"5","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42920,"SerRR":"Geophysical Research Letters. 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