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| Late Jurassic manganese microbial carbonates of West Siberian oil and gas basin: Diagnostic features, environmental sedimentation, secondary transformations |
| Latypova Margaritaa,*, Gafurova Dinab, Churkina Valeriaa, Kalmykov Antona, Kalmykov Georgya |
aGeological Faculty, Lomonosov Moscow State University, 119991, Moscow, Russia;
bCenter for Integrative Petroleum Research, College of Petroleum Engineering and Geosciences, King Fahd University of Petroleum and Minerals, 31261, Dhahran, KSA |
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Abstract This study focuses on the investigation of Late Oxfordian—Early Tithonian manganese microbial carbonates (MC) found at the top of the Georgiev regional stage in the Western Siberian oil and gas basin. In some isolated areas, these MC are oil reservoirs. However, these rocks are still one of the least studied sediments in the carbonate interval at the boundary of the Bazhenov and Georgiev subregional stage. We have described their geochemical, lithological and mineralogical composition in detail. Based on the characteristics of MC, we assumed their formation settings. The elevated MnO content, associated with microbial processes, and the high concentration of biophilic elements, both suggest the active involvement of organic matter in the formation and development of microbial sediments. The isotopic composition of carbon in the microbial carbonates further supports a biogenic source of carbon dioxide playing an important role in the formation of these deposits. We have established that the Late Jurassic manganese MC were intensely secondary altered, partially recrystallized and calcified by catagenetic processes. Isometric pyrite crystal aggregates with kutnohorite fragments were formed at the contacts between kutnohorite and calcite zones. We suggest that the presence of caverns and high reservoir potential in the microbial carbonates from the Yem—Egovskaya field of the Krasnoleninsky arch may be attributed to intense secondary catagenetic alterations.
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Received: 18 September 2024
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Corresponding Authors:
*E—mail address: m.latypova@oilmsu.ru (L. Margarita).
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[1] Balushkina N.S., Kalmykov G.A., 2016. Cavity structure in oil-saturated Bazhenov and Abalak shale rock in the Western Siberian basin. Moscow University Geology Bulletin, 71 (1), 71-80. https://doi.org/10.3103/S0145875215050026.
[2] Belkin V.I., Efremov E.P., Kaptelinin N.D., 1983. Model of oil reservoirs of the Bazhenov Formation of the Salym field.Oil Industry, 10, 27-31.
[3] Bumagina V.A., Potapova A.S., Vilesov A.P., Chertina K.N., 2019. Typing of carbonate rocks in the interval of the Bazhen-Abalak complex for the purpose of forecasting reservoirs (Krasnoleninsky arch). In the Collection of Conference "New ideas in oil and gas geology", Moscow, pp. 63-67.
[4] Berger W.Y., Soutar A., 1970. Preservation of plankton shells in an anaerobic basin off California.Geological Society of America Bulletin, 81(1), 275-282.
[5] Burnaz L., Kalmykov A., Grohmann S., Kalmykov G., Littke R.,2022. Geochemistry and organic petrology of organic-rich shales of the Upper Jurassic-Lower Cretaceous Bazhenov Regional stage in the Frolov Region, West Siberian Basin: Implications for the reconstruction of the organic matter origin and paleoredox conditions. Marine and Petroleum Geology, 77(1), 101-113. https://doi.org/10.1016/j.marpetgeo.2022.105809.
[6] Cai C.F., Li K.K., Li H.T., Zhang B.S.,2008. Evidence for cross formational hot brine flow from integrated 87Sr/86Sr, REE and fluid inclusions of the Ordovician veins in Central Tarim. Applied Geochemistry, 23, 2226-2235. https://doi.org/10.1016/j.apgeochem.2008.03.009.
[7] Cai C.F., Li K.K., Liu D.W., John C.M., Wang D.W., Fu B., Feng L.J., Fakhraee M., Jiang L., 2021. Anaerobic oxidation of methane by Mn oxides in sulfate-poor environments. Geology, 49 (7): 761-766. https://doi.org/10.1130/G48553.1.
[8] Cai C.F., Lyons T.W., Sun P., Liu D.W., Wang D.W., Tino C.J., Luo G.M., Peng Y.Y., Jiang L.,2022. Enigmatic super-heavy pyrite formation: Novel mechanistic insights from the aftermath of the Sturtian Snowball Earth. Geochimica et Cosmochimica Acta, 334, 65-82. https://doi.org/10.1016/j.gca.2022.07.026.
[9] Cai C.F., Liu D.W., Hu Y.J., Huang T.Y., Jiang Z.W., Xu C.L.,2023. Interlinked marine cycles of methane, manganese, and sulfate in the post-Marinoan Doushantuo cap dolostone. Geochimica et Cosmochimica Acta, 346, 245-258. https://doi.org/10.1016/j.gca.2023.02.014.
[10] Carmeille M., Bourillot R., Pellenard P., Dupias V., Schnyder J., Riquier L., Mathieu O., Brunet M.F., Enay R., Grossi V., Gaborieau C., Razin P., Visscher P.T., 2020. Formation of microbial organic carbonates during the Late Jurassic from the Northern Tethys (Amu Darya Basin, Uzbekistan): Implications for Jurassic anoxic events.Global and Planetary Change, 186, 103-127.
[11] Coleman M., Fleet A., Donson P., 1982. Preliminary studies of manganese-rich carbonate nodules from leg 68, suite 503, Eastern equatorial Pacific. Deep Sea Drilling Project Reports and Publications, 68, 481-489.
[12] Dahlmann A., Lange G.J., 2003. Fluid-sediment interactions at Eastern Mediterranean mud volcanoes: A stable isotope study from ODP Leg 160. Earth and Planetary Science Letters, 212, 377-391. https://doi.org/10.1016/S0012-821X(03)00227-9.
[13] Dera G., Brigaud B., Monna F., Laffont R., Puceat E., Deconinck J.-F., Pellenard P., Joachimski M.M., Durlet C., 2011. Climatic ups and downs in a disturbed Jurassic world. Geology, 39, 215-218. https://doi.org/10.1130/G31579.1.
[14] Derkachev A.N., Nikolaeva N.A., Baranov B.V., Barinov N.N., Mozherovsky A.V., Minami H., Hachikubo A., Soji H., 2015 Manifestation of carbonate-barite mineralization around methane seeps in the Sea of Okhotsk (the western slope of the Kuril Basin). Oceanology, 55 (3), 390-399. https://doi.org/10.1134/S0001437015030029.
[15] Droste H.,1990. Depositional cycles and source rock development in an epeiric intraplatform basin: The Hanifa Formation of the Arabian peninsula. Sedimentary Geology, 69, 281-296. https://doi.org/10.1016/0037-0738(90)90054-W.
[16] Eder V.G., Follmi K.B., Zanin Yu.N., Zamirailova A.G.,2018. Manganese carbonates in the Upper Jurassic Georgiev Formation of the Western Siberian marine basin. Sedimentary Geology, 363, 221-234. https://doi.org/10.1016/j.sedgeo.2017.11.012.
[17] Eisma D.,1988. Transport and deposition of suspended matter in estuaries and the Nearshore Sea. In: Physical and chemical weathering in geochemical cycles. Dordrecht: Springer Netherlands, pp. 273-298. https://doi.org/10.1007/978-94-009-3071-1_13.
[18] Eltom H.A., Rankey E.C., Hasiotis S.T., Gonzalez L.A., Cantrell D.A.,2017. Impact of upwelling on heterozoan, biosiliceous, and organic-rich deposits: Jurassic (Oxfordian) Hanifa Formation. Saudi Arabia Journal of Sedimentary Research, 87, 1235-1258. https://doi.org/10.2110/jsr.2017.71.
[19] Emerson S., Cranston R.E., Liss P.S., 1979. Redox species in a reducing fjord: Equilibrium and kinetic considerations. Deep Sea Research Part A. Oceanographic Research Papers, 26 (8), 859-878. https://doi.org/10.1016/0198-0149(79)90101-8.
[20] Fan D., Ye J., Yin L., Zhang R., 1996. The role of microbes in the formation of Mn-carbonate during early diagenesis — Take the Gaoyan deposit as an example. Organism and Organic Matter in the Formation of Mineral Deposits. China Ocean Press, pp. 81-101.
[21] Fan D., Ye J., Yin L., Zhang R., 1999. Microbial processes in the formation of the Sinian Gaoyan manganese carbonate ore, Sichuan Province, China. Ore Geology Reviews, 15 (1-3), 79-93. https://doi.org/10.1016/S0169-1368(99)00016-5.
[22] Fu B., Aharon P., Byerly G.R., Roberts H.H., 1994. Barite chimneys on the Gulf of Mexico slope: Initial report on their petrography and geochemistry. Geo-Marine Letters, 14, 81-87. https://doi.org/10.1007/BF01203718.
[23] Gurvich E.G., Bogdanov Yu.A., Lisitsyn A.P., 1978. Behavior of barium in modern sedimentation in the Pacific Ocean.Geochemistry, 3, 410-415.
[24] Hein J.R., Koski R.A., 1987. Bacterially mediated diagenetic origin for chert-hosted manganese deposits in the Franciscan Complex, California Coast Range.Geology, 15, 722-726.
[25] Hein J.R., Bolton B.R., Nziengui P., McKirdy D., Frakes L., 1989. Chemical, isotopic and lithologic associations within the Moanda Manganese Deposit, Gabon. Abstracts. 28th International Geological Congress, Washington DC, pp. 2-47.
[26] Hu Y., Cai C., Li Y., Liu D., Wei T., Wang D., Jiang L., Ma R., Shi S., Immenhauser A., 2023. Sedimentary and diagenetic archive of a deeply-buried, upper Ediacaran microbialite reservoir, southwestern China. AAPG Bulletin, 107, 387-412. https://doi.org/10.1306/08232221122.
[27] Jones C.E., Jenkyns H.C., 2001. Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous. American Journal of Science, 301, 112-149. https://doi.org/10.2475/ajs.301.2.112.
[28] Kalin, B.A., Volkov, N.V., Polsky, V.I., 2008. Scanning Electron Microscopy. Laboratory work, pp. 1-56.
[29] Karpova E.V., Khotylev A.O., Manuilova E.A., Mayorov A.A., Krasnova E.A., Khotylev O.V., Balushkina N.S., Kalmykov G.A., Kalmykov A.G.,2021. Hydrothermal-metasomatic systems as the most important factor for the formation of elements of the oil and gas-bearing complex in the Bazhenov-Аbalak sediments. Georesources, 23 (2), 142-151. https://doi.org/10.18599/grs.2021.2.14.
[30] Kontorovich A.E., Kontorovich V.A., Ryzhkova S.V., Shurygin B.N., Vakulenko L.G., Gaideburova E.A., Danilova V.P., Kazanenkov V.A., Kim N.S., Kostyreva E.A., Moskvin V.I., Yan P.A.,2013. Jurassic paleogeography of the West Siberian sedimentary basin. Russian Geology and Geophysics, 54 (8), 747-779. https://doi.org/10.1016/j.rgg.2013.07.002.
[31] Kuleshov V.N.,2013. Manganese rocks and ores: Geochemistry of isotopes, genesis, evolution of ore genesis. GIN RAS, Scientific Publishing House, pp. 1-506.
[32] Kuleshov V.N., Dombrovskaya Zh.V., 1988. Isotopic composition and conditions of formation of Nikopol carbonate manganese ores.Isotope Geochemistry of Ore formation Process, Science, 233-258.
[33] Kuleshov V.N., Bych A.F., 2002. Isotopic composition (δ13C and δ18O) and origin of carbonate manganese ores of the Usinsk deposit (Kuznetsk Alatau).Lithology and Minerals, 4, 381-396.
[34] Kunz A.F.,2002. Hydrothermal-metasomatic ore formation in carbonate rocks (experimental models and their applications). Ekaterinburg: Ural Branch of the Russian Academy of Sciences, pp. 1-344.
[35] Lein A.Yu., Ulyanova N.V., Pimenov N.V., 2001. Black Sea “corals” A product of mineralization of microbial mats
(in Russian). Nature, 12, 48-54.
[36] Leinfelder R.R., Werner W., Nose M., Schmid D.U., Krautter M., Laternser R., Takacs M., Hartmann D., 1996. Paleoecology, growth parameters and dynamics of coral, sponge and microbolite reefs from the Late Jurassic. Global and Regional Controls on Biogenic Sedimentation: I. Reef evolution. Research Reports. Gfttinger: Arb. Geol. Paleont. Sb., 2, 227-248.
[37] Latypova M.R., Khotylev O.V., Balushkina N.S., Kalmykov A.G., Kalmykov G.A., Kopaevich L.F., Karpova E.V., Churkina V.V., 2022. The sedimentation settings of the Abalak Formation and Vogulka Sequence on the Territory of the Kamennoye Crest of the Krasnoleninsky Arch (Western Siberia). Moscow University Geology Bulletin, 77 (1), 48-60. https://doi.org/10.3103/S0145875222010094.
[38] Latypova M.R., Kalmykov A.G., Churkina V.V., Karpova E.V., Balushkina N.S., Kalmykov G.A., 2023. The geochemical features of microbial carbonates of the Abalak and Georgian Formations in Western Siberia. Moscow University Geology Bulletin, 78 (5), 603-617. https://doi.org/10.3103/S0145875223050071.
[39] Maksimov S.P.,1987. Oil and gas fields of the USSR. Moscow, Nedra, 2, p. 304.
[40] Malenkina, S.Yu., 2011. Sedimentary processes in Jurassic microbial communities of the Russian Plate. In: Shurygina, B.N., Lebedeva, N.K.,. Goryacheva, A.A., (Eds.). Paleontology, stratigraphy and paleogeography of the Mesozoic and Cenozoic boreal regions: Scientific materials. Novosibirsk: INGG SB RAS, pp. 157-162.
[41] Malenkina, S.Yu., 2013. Organomineralization in Jurassic stromatolite structures of the Russian Plate. In: Ivanova, A.V., (Eds.). Collection of Proceedings of the Conference “Problems of Geology of European Russia”. Saratov: SSTU Publishing House, pp. 124-136.
[42] Manceau A., Lanson B., Schlegel M.L., Harge J.C., Musso M., Eybert-Berard L., Hazemann J.L., Chateigner D., Lamble G.M., 2000. Quantitative Zn speciation in smelter-contanimated soils by EXAFS spectroscopy. American Journal of Science, 300 (4), 289-343. https://doi.org/10.2475/ajs.300.4.289.
[43] Marinov V.A., Meledina S.V., Dzyuba O.S., Urman O.S., Yazikova O.V., Luchinina V.A., Zamirailova A.G., Fomin A.N., 2006. Biofacies of Upper Jurassic and Lower Cretaceous sediments of Central West Siberia. Stratigraphy and Geological Correlation, 14 (4), 418-432. https://doi.org/10.1134/S0869593806040058.
[44] Martinez M., Dera G., 2015. Orbital pacing of carbon fluxes by a ~9-My eccentricity cycle during the Mesozoic. Proceedings of the National Academy of Sciences, 112 (41), 12604-12609. https://doi.org/10.1073/pnas.1419946112.
[45] Matyszkiewicz J., Kochman Al.,2016. Pressure dissolution features in Oxfordian microbial-sponge buildups with pseudonodular texture, Krakov upland, Poland. Annales Societatis Geologorum Poloniae, 86, 355-377. https://doi.org/10.14241/asgp.2016.008.
[46] Mikhalchuk N.V.,2017. Mobile forms of heavy metals and microelements in carbonate soils of southwestern Belarus.Polesie Agrarian-Ecological Institute of the National Academy of Sciences of Belarus, 3, 90-97.
[47] Monin A.S., Lisitsin A.P., 1983. Biogeochemistry of the Ocean. Nauka, pp. 1-368.
[48] Okita, P.M., Maynard, J.B., Spiker, E.C., Force, E.R., 1988. Isotopic evidence for organic matter oxidation by manganese reduction in the formation of stratiform Mn carbonate ore. Geochimica et Cosmochimica Acta, 52 (11), 2679-2685. https://doi.org/10.1016/0016-7037(88)90036-1.
[49] Okita P.M., Shanks W.C., 1988. δ13C and δ33S trends in sedimentary manganese deposit, Molango (Mexico) and Taojiang (China): Evidence for mineralization in closed system.International Association for Sedimentologists. Symposium on Sedimentology Related to Mineral Deposits, 188-189.
[50] Oliver N., Colombie C., Pittet B., Lathuiliere B., 2011. Microbial carbonates and corals on the marginal French Jura platform (Late Oxfordian, Molinges section). Facies, 57, 469-492. https://doi.org/10.1007/s10347-010-0246-9.
[51] Oliver, N, Pittet, B, Mattioli, E.,2004. Paleoenvironmental control on sponge-microbialite reefs and contemporaneous deep-shelf marl-limestone deposition (Late Oxfordian, southern Germany). Palaeogeography, Palaeoclimatology, Palaeoecology, 212, 233-263. https://doi.org/10.1016/j.palaeo.2004.06.003.
[52] Oloriz F., Reolid M., Rodriguez-Tovar F.J., 2003. A Late Jurassic Carbonate Ramp Colonized by Sponges and Benthic Microbial Communities (External Prebetic, Southern Spain). Palaios, 18 (6), 528-545. https://doi.org/10.1669/0883-1351(2003)018<0528:ALJCRC>2.0.CO;2.
[53] Oschmann W.,1990. Environmental cycles in the Late Jurassic northwest European epeiric basin: Interaction with atmospheric and hydrospheric circulations. Sediment Geology, 69, 313-332. https://doi.org/10.1669/0883-1351(2003)018<0528:ALJCRC>2.0.CO;2.
[54] Palma R., Kietzmann D.A., Comerio M., Martin-Chivelet J., Lopez-Gomez J., Bressan G.S., 2015. Oxfordian microbial laminites from La Manga Formation, Neuquen Basin, Argentina: Remarkable Nanobacteria Preservation. Journal of Iberian Geology, 41 (3), 351-363. https://doi.org/10.5209/rev_JIGE.2015.v41.n3.51568.
[55] Pearce C.R., Hesselbo S.P., Coe A.L.,2005. The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognised from fossil wood in the British Isles. Palaeogeography, Palaeoclimatology, Palaeoecology, 221, 343-357. https://doi.org/10.1016/j.palaeo.2005.03.004.
[56] Polgári M., Gyollai I., 2022. Comparative study of formation conditions of Fe-Mn ore microbialites based on mineral assemblages: A critical self-overview. Minerals, 12, 1273. https://doi.org/10.3390/min12101273.
[57] Polgári M., Hein J.R., Vigh T.,Szabó-Drubina, M., Fórizs, I., Bíró, L., Müller, A., Tóth, A.L., 2012. Microbial processes and the origin of the Úrkút manganese deposit, Hungary. Ore Geology Reviews, 47, 87-109. https://doi.org/10.1016/j.oregeorev.2011.10.001.
[58] Polgári M., Szabó Z., Szederkényi T., 2000. Manganese Ores in Hungary. In: Commemoration of Professor Gyula Grasselly. Juhász Publishing House, Szeged, pp. 1-675.
[59] Polgári M., Okita P.M., Hein J.R., 1991. Stable isotope evidence for the origin of the Úrkút manganese ore deposit, Hungary. Journal of Sedimentary Petrology, 61 (3), 384-393. https://doi.org/10.1306/D426771C-2B26-11D7-8648000102C1865D.
[60] Potapova A.S., Vilesov A.P., Chertina K.N., Emelyanov D.V., Akhmadishin A.T., 2018. Signs of the subaeral exposition at the border of Аbalak and Tutlem (Bazhenov) suite.Geology, Geophysics and Development of Oil and Gas fields, 11, 13-19.
[61] Rachold V., Brumsack H.J., 2001. Inorganic geochemistry of Albian sediments from the Lower Saxony Basin NW Germany: Palaeoenvironmental constraints and orbital cycles. Palaeogeography, Palaeoclimatology, Palaeoecology, 174 (1-3), 121-143. https://doi.org/10.1016/S0031-0182(01)00290-5.
[62] Rais P.,Louis-Schmid, B., Bernasconi, S.M., Weissert, H., 2007. Palaeoceanographic and palaeoclimatic reorganization around the Middle-Late Jurassic transition. Palaeogeography, Palaeoclimatology, Palaeoecology, 251, 527-546. https://doi.org/10.1016/j.palaeo.2007.05.008.
[63] Riding R.,2011. Microbialites, stromatolites, and thrombolites. Encyclopedia of Geobiology. Encyclopedia of Earth Science Series. Springer. Heidelberg, pp. 635-654.
[64] Rogov M.A.,2012. Latitudinal Gradient of Taxonomic Richness of Ammonites in the Kimmeridgian-Volgian in the Northern Hemisphere. Paleontological Journal, 46 (2), 148-156. https://doi.org/10.1134/S0031030112020104.
[65] Sazonova I.G., Sazonov N.T., 1967. Paleogeography of the Russian Platform in Jurassic and Early Cretaceous times. NEDRA, Leningrad, pp. 1-442.
[66] Sholkovitz E.R.,1990. Rare-earth elements in marine sediments and geochemical standards. Chemical Geology, 88 (3-4), 333-347. https://doi.org/10.1016/0009-2541(90)90097-Q.
[67] Strakhov N.M., Shterenberg L.E., Kalinenko V.V., Tikhomirova E.S., 1968. Geochemistry of sedimentary manganese ore process. Nauka, USSR, pp. 185-495
[68] Su Z.T., Zhang D.M., Tang J., Sun P.J., Luo Z.F., Ma H.,2023. Microfacies and paleoenvironment of microbialites of the Cambrian (Stage 4) Qingxudong Formation in the Huayuan area, northwestern Hunan Province, southern China. Journal of Palaeogeography, 12(4), 587-602. https://doi.org/10.1016/j.jop.2023.07.004.
[69] Gurari F.G., Mogucheva N.K., Shurygin B.N., 2004. The regional stratigraphic correlation scheme of Callovian and Upper Jurassic sediments of Western Siberia. 6th Interdepartmental Stratigraphic Meeting Awards on the Consideration and Acceptation of Specified Stratigraphic Schemes of Mesozoic Sediments of Western Siberia. SNIIGGiMS, Novosibirsk, pp. 77-113.
[70] Tikhonova M.S., Kalmykov A.G., Ivanova D.A., Vidishcheva O.V., Kalmykov G.A., Borisov R.B., 2022. The distribution model for hydrocarbon compounds in a cavitated area of the Bazhenov Formation. Moscow University Geology Bulletin, 77 (1), 101-113. https://doi.org/10.33623/0579-9406-2021-6-98-109.
[71] Torres M.E., Bohrmann G., Suess E., 1996. Authigenic barites and fluxes of barium associated with fluid seeps in the Peru subduction zone. Earth and Planetary Science Letters, 144, 469-481. https://doi.org/10.1016/S0012-821X(96)00163-X.
[72] Tribovillard N., Trentesaux A., Trichet J., Defarge C., 2000. Jurassic counterpart for modern kopara of the Pacific atolls: Lagoonal, organic matter-rich, laminated carbonate of Orbagnoux (Jura Mountains, France). Palaeogeography, Palaeoclimatology, Palaeoecology, 156, 27-288. https://doi.org/10.1016/S0031-0182(99)00145-5.
[73] Ulmishek G.F.,2003. Petroleum Geology and Resources of the West Siberian Basin, Russia. USGS,Virginia, pp. 1-53.
[74] Ushatinskiy I.N., Zaripov O.G., 1971. The mineralogy of carbonate and clay cements of the productive deposits of the shaim oil-bearing region in connection with their reservoir properties. ZapSibNIGNI, Tumen, pp. 164-190.
[75] Vahrenkamp V.C., Van Laer P., Franco B., Celentano M.A., Grelaud C., Razin P., 2015. Late Jurassic to Cretaceous source rock Prone Intra-Shelf Basins of the Eastern Arabian Plate-Interplay between Tectonism, Global Anoxic Events and Carbonate Platform Dynamics. International Petroleum Technology Conference. https://doi.org/10.2523/IPTC-18470-MS.
[76] Vedrine S., Strasser A., Hug W., 2007. Oncoid growth and distribution controlled by sea-level fluctuations and climate (Late Oxfordian, Swiss Jura Mountains). Facies, 53, 535-552. https://doi.org/10.1007/s10347-007-0114-4.
[77] Volkov I.I.,1984. Geochemistry of sulphur in ocean sediments. Nauka, pp. 1-170.
[78] Von Breymann M.T., Brumsack H.J., Emeis K.C., 1992. Deposition and diagenetic behavior of barium in the Japan Sea.Proceedings of the Ocean Drilling Program Scientific Results, 651-665.
[79] Warren J.K.,2011. Evaporitic source rocks: Mesohaline responses to cycles of “famine or feast” in layered brines.International Association of Sedimentologists, Special Publications, 43, 315-392.
[80] Weissert H., Mohr H., 1996. Late Jurassic climate and its impact on carbon cycling. Paleogeography, Paleoclimatology, Paleoecology, 122, 27-43. https://doi.org/10.1007/s10347-007-0114-4.
[81] Wittkop C., Swanner E.D., Grengs A., Lambrecht N., Fakhraee M., Myrbo A., Bray A.W., Poulton S.W., Katsev S.,2020, Evaluating a primary carbonate pathway for manganese enrichments in reducing environments. Earth and Planetary Science Letters, 538. https://doi.org/10.1016/j.epsl.2020.116201.
[82] Yakushev E., Pakhomova S., Sorenson K., Skei J.,2009. Importance of the different manganese species in the formation of water column redox zones: Observations and modeling. Marine Chemistry, 117 (1-4), 59-70. https://doi.org/10.1016/j.marchem.2009.09.007.
[83] Yasovich G.S.,1971. The formation conditions of the Jurassic deposits of the Shaim and Krasnoleninsk oil-bearing regions. In: Nesterov, I.I., (Ed.). ZapSibNIGNI, Tumen, 43, pp. 207-266.
[84] Yudovich Ya.E., Ketris M.P., 1997. Geochemistry of Black Shales. 1. Outline. 2. Bibliography and Index. Prolog, Syktyvkar, pp. 1-212.
[85] Yurchenko A.Y., Balushkina N.S., Kalmykov G.A., Khamidullin R.A., Korobova N.I., Blinova V.N., 2015. The structure and genesis of limestones at the boundary between the Abalak and Bazhenov formations in Central West Siberia. Moscow University Geology Bulletin, 70 (6), 428-435. https://doi.org/10.3103/S0145875215050129.
[86] Yurchenko A.Y., Potapova A.S., Bumagina V.A., Vilesov A.P., Chertina K.N., Balushkina N.S., Kalmykov G.A., Khotylev O.V., 2019. Morphological and lithogenetic classification of the carbonate rocks of the Abalak-Bazhenov Complex. Moscow University Geology Bulletin, 74, 372-379. https://doi.org/10.3103/S0145875219040136.
[87] Zanin Y.N., Luchinina V.A., Levchuk M.A., Pisareva G.M., 2001. Stromatolites and oncolites in Mesozoic deposits of the west Siberian plate.Russian Geology and Geophysics, 42, 1348-1352.
[88] Zanin Y.N., Zamirailova A.G., Eder V.G., Pisareva G.M., 2003. Manganese carbonates in Upper Jurassic strata of the West Siberian plate.Russian Geology and Geophysics, 44(7), 686-694.
[89] Zelenin N.I., Ozerov I.M., 1983. Handbook of Oil Shales. Leningrad, pp. 1-248.
[90] Zubkov, M.Yu., 2019. Reservoir types in the Bazhenov-Abalak series of Western Siberia and their genesis.Oil and Gas Geology, 4, 59-78.
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