Vevel Ya.A.
Graduated from the Department of Paleontology of the Geological Faculty of the A.A. Zhdanov Leningrad State University (1992), specialization “geologist-surveyor-prospecting worker”.
Junior Researcher of the Laboratory of Oil and Gas Basins, Institute of Geology, Komi Scientific Center, Ural Branch of the Russian Academy of Sciences.
Area of scientific interests: Lower Carboniferous foraminifera, stratigraphy.
Author of 24 publications.
Stratigraphy and lithology
| Article # 24_2023 | submitted on 06/02/2023 displayed on website on 06/30/2023 |
| 20 p. | Vevel Ya.A., Ivanova R.M., Gruzdev D.A., Zhuravlev A.V. |
| Calcareous algae of the Visean-Serpukhovian boundary beds in the Izyayu River section (south of the Chernyshev Uplift) | |
| We consider changes in the composition of the algaflora in the Visean-Serpukhovian boundary interval in the Izyayu River section. A transgressive trend in changing sedimentation conditions - from extremely shallow water at the end of the Visean to moderately deep water at the end of the Early and early Late Serpukhovian - is observed for the section as a whole. This change in sedimentation conditions led to a consistent reduction in the abundance and diversity of calcareous algae. In general, the composition of the Late Visean-Early Serpukhovian algaflora in the Izyayu River section corresponds to warm shallow-water conditions. Keywords: calcareous algae, changing sedimentation conditions, Lower Carboniferous, Chernyshev Uplift. |
|
| article citation | Vevel Ya.A., Ivanova R.M., Gruzdev D.A., Zhuravlev A.V. Vodorosli pogranichnykh otlozheniy vizeyskogo i serpukhovskogo yarusov v razreze na r. Iz"yayu (yug podnyatiya Chernysheva) [Calcareous algae of the Visean-Serpukhovian boundary beds in the Izyayu River section (south of the Chernyshev Uplift)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 2, available at: http://www.ngtp.ru/rub/2023/24_2023.html EDN: ZSZTYM |
References
Bogush O.I., Ivanova R.M., Luchinina V.A. Izvestkovye vodorosli verkhnego famena i nizhnego karbona Urala i Sibiri [Calcareous algae of the Upper Famennian and Lower Carboniferous of the Urals and Siberia]. Novosibirsk: Nauka: Sib. otd., 1990, 160 p.
Boucot A.J., Chen X., Scotese C.R. Phanerozoic Paleoclimate: An Atlas of Lithologic Indicators of Climate. SEPM Concepts in Sedimentology and Paleontology, 2013, no. 11, 478 p.
Eliseev A.I. Formatsii zon ogranicheniya severo-vostoka Evropeyskoy platformy (pozdniy devon i karbon) [Formations of the North-Eastern European Platform limitation zones (Late Devonian and Carboniferous)]. Leningrad: Nauka, 1978, 192 p.
Eliseev A.I. Stratigrafiya i litologiya kamennougol'nykh otlozheniy gryady Chernysheva [Stratigraphy and lithology of the Carboniferous strata of the Сhernyshev Ridge]. Moscow-Leningrad: Nauka, 1963, 168 p.
Elliott G.F. Dasycladalean Algae of the Palaeozoic and Mesozoic. Calcareous Algae and Stromatolites. R. Riding (Ed.). Berlin: Springer-Verlag, 1991, pp. 125-130.
Fielding C.R., Frank T.D., Isbell J.L. The late Paleozoic ice age - A review of current understanding and synthesis of global climate patterns. Resolving the Late Paleozoic Ice Age in Time and Space: Geological Society of America Special, 2008, vol. 441, pp. 343-354. DOI: 10.1130/2008.2441(24)
Goddéris Y., Donnadieu Y., Carretier S., Aretz M., Dera G., Macouin M., Regard V. Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering. Nature Geoscience, 2017, vol. 10, pp. 382-386. DOI: 10.1038/ngeo2931
Gruzdev D.A. Pozdnedevonsko-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [Late Devonian-Early Carboniferous isolated platform in the Circumpolar Urals (Bolshaya Nadota River)]. Vestnik Instituta geologii, 2017, no. 4, pp. 16-23.
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol., 1965, no. 49, pp. 445-459.
Ivanova R.M. Izvestkovye vodorosli karbona Urala [Calcareous algae of the Carboniferous Urals]. Ekaterinburg: RIO UrO RAN, 2013, 244 p.
Kossovaya O.L., Vevel Y.A., Zhuravlev A.V. Fauna and sedimentation near the Visean/Serpukhovian boundary (Izyayu River section, Tchernyshev Swell, Subpolar Urals). Newsletter on Carboniferous Stratigraphy, 2001, no. 19, p. 29-31.
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf DOI: 10.17353/2070-5379/27_2016
Richards B.C. Current status of the International Carboniferous Time Scale. New Mexico Museum of Natural History and Science, 2013, bull. 60, pp. 348-353.
Sevastopulo G.D., Barham M. Correlation of the base of the Serpukhovian Stage (Mississippian) in NW Europe. Geological Magazine, 2014, no. 152, pp. 244-253.
Timonin N.I. Tektonika gryady Chernysheva (Severnoe Priural'e) [Tectonics of the Сhernyshev Ridge (Northern Pre Urals)]. Leningrad: Nauka, 1975, 130 p.
Vevel Y.A., Zhuravlev A.V., Kossovaya O.L., Sobolev D.B. Lochriea cruciformis Zone (Lower Carboniferous) and its correlation with foraminifer and coral subdivisions (North of Urals, Izyayu section). Abstracts. Geological Society of Australia, 2000, 61, p. 61.
Vevel' Ya.A. Foraminifery pogranichnykh vizeysko-serpukhovskikh otlozheniy v razreze na r. Iz"yayu (gryada Chernysheva) [Foraminifers of the Visean-Serpukhovian boundary level in the Izyayu River section (Chernyshev Ridge)]. Geologiya i mineral'nye resursy Evropeyskogo severo-vostoka Rossii: materialy XIV geol. s"ezda Respubliki Komi. Syktyvkar, 2004, vol. III, pp. 308-310.
Vevel' Ya.A., Zhuravlev A.V., Gruzdev D.A. Nizhniy serpukhov (nizhniy karbon) v basseyne r. Kozhim (Pripolyarnyy Ural)[Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 4, available at: http://www.ngtp.ru/rub/2018/35_2018.html DOI: 10.17353/2070-5379/35_2018
Zhuravlev A.V. Konodonty verkhnego devona - nizhnego karbona severo-vostoka Evropeyskoy Rossii Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St. Petersburg, VSEGEI, 2003, 85 p.
Zhuravlev A.V. Mestnaya stratigraficheskaya skhema verkhnego devona - nizhnego karbona yugo-zapada Lyzhsko-Kyrtael'skogo vala (vostok Pechorskoy plity) [Stratigraphy of the Upper Devonian - Lower Carboniferous of south-west of Lyzha-Kyrtael swell (Pechora Plate eastward)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 1, available at: http://www.ngtp.ru/rub/2023/8_2023.html DOI: 10.17353/2070-5379/8_2023
Zhuravlev A.V., Sobolev D.B. Konodonty pogranichnykh vizeysko-serpukhovskikh otlozheniy yuzhnoy chasti gryady Chernysheva (r. Iz"yayu) [Conodonts of the Visean-Serpukhovian boundary level of the southern part of the Сhernyshev Ridge (Iz'yayu River)]. Syktyvkarskiy paleontologicheskiy sbornik, 2000, no. 4, pp. 84-89.
Zhuravlev A.V., Vevel Y.A., Gruzdev D.A., Erofeevsky A.V. Late Mississippian (early Serpukhovian) carbon isotope record of northern Laurussia: A proposal for the Visean / Serpukhovian boundary. Revista Mexicana de Ciencias Geológicas, 2023, vol. 40, no. 1, pp. 35-43. DOI: 10.22201/cgeo.20072902e.2023.1.1722
Boucot A.J., Chen X., Scotese C.R. Phanerozoic Paleoclimate: An Atlas of Lithologic Indicators of Climate. SEPM Concepts in Sedimentology and Paleontology, 2013, no. 11, 478 p.
Eliseev A.I. Formatsii zon ogranicheniya severo-vostoka Evropeyskoy platformy (pozdniy devon i karbon) [Formations of the North-Eastern European Platform limitation zones (Late Devonian and Carboniferous)]. Leningrad: Nauka, 1978, 192 p.
Eliseev A.I. Stratigrafiya i litologiya kamennougol'nykh otlozheniy gryady Chernysheva [Stratigraphy and lithology of the Carboniferous strata of the Сhernyshev Ridge]. Moscow-Leningrad: Nauka, 1963, 168 p.
Elliott G.F. Dasycladalean Algae of the Palaeozoic and Mesozoic. Calcareous Algae and Stromatolites. R. Riding (Ed.). Berlin: Springer-Verlag, 1991, pp. 125-130.
Fielding C.R., Frank T.D., Isbell J.L. The late Paleozoic ice age - A review of current understanding and synthesis of global climate patterns. Resolving the Late Paleozoic Ice Age in Time and Space: Geological Society of America Special, 2008, vol. 441, pp. 343-354. DOI: 10.1130/2008.2441(24)
Goddéris Y., Donnadieu Y., Carretier S., Aretz M., Dera G., Macouin M., Regard V. Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering. Nature Geoscience, 2017, vol. 10, pp. 382-386. DOI: 10.1038/ngeo2931
Gruzdev D.A. Pozdnedevonsko-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [Late Devonian-Early Carboniferous isolated platform in the Circumpolar Urals (Bolshaya Nadota River)]. Vestnik Instituta geologii, 2017, no. 4, pp. 16-23.
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol., 1965, no. 49, pp. 445-459.
Ivanova R.M. Izvestkovye vodorosli karbona Urala [Calcareous algae of the Carboniferous Urals]. Ekaterinburg: RIO UrO RAN, 2013, 244 p.
Kossovaya O.L., Vevel Y.A., Zhuravlev A.V. Fauna and sedimentation near the Visean/Serpukhovian boundary (Izyayu River section, Tchernyshev Swell, Subpolar Urals). Newsletter on Carboniferous Stratigraphy, 2001, no. 19, p. 29-31.
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf DOI: 10.17353/2070-5379/27_2016
Richards B.C. Current status of the International Carboniferous Time Scale. New Mexico Museum of Natural History and Science, 2013, bull. 60, pp. 348-353.
Sevastopulo G.D., Barham M. Correlation of the base of the Serpukhovian Stage (Mississippian) in NW Europe. Geological Magazine, 2014, no. 152, pp. 244-253.
Timonin N.I. Tektonika gryady Chernysheva (Severnoe Priural'e) [Tectonics of the Сhernyshev Ridge (Northern Pre Urals)]. Leningrad: Nauka, 1975, 130 p.
Vevel Y.A., Zhuravlev A.V., Kossovaya O.L., Sobolev D.B. Lochriea cruciformis Zone (Lower Carboniferous) and its correlation with foraminifer and coral subdivisions (North of Urals, Izyayu section). Abstracts. Geological Society of Australia, 2000, 61, p. 61.
Vevel' Ya.A. Foraminifery pogranichnykh vizeysko-serpukhovskikh otlozheniy v razreze na r. Iz"yayu (gryada Chernysheva) [Foraminifers of the Visean-Serpukhovian boundary level in the Izyayu River section (Chernyshev Ridge)]. Geologiya i mineral'nye resursy Evropeyskogo severo-vostoka Rossii: materialy XIV geol. s"ezda Respubliki Komi. Syktyvkar, 2004, vol. III, pp. 308-310.
Vevel' Ya.A., Zhuravlev A.V., Gruzdev D.A. Nizhniy serpukhov (nizhniy karbon) v basseyne r. Kozhim (Pripolyarnyy Ural)[Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 4, available at: http://www.ngtp.ru/rub/2018/35_2018.html DOI: 10.17353/2070-5379/35_2018
Zhuravlev A.V. Konodonty verkhnego devona - nizhnego karbona severo-vostoka Evropeyskoy Rossii Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St. Petersburg, VSEGEI, 2003, 85 p.
Zhuravlev A.V. Mestnaya stratigraficheskaya skhema verkhnego devona - nizhnego karbona yugo-zapada Lyzhsko-Kyrtael'skogo vala (vostok Pechorskoy plity) [Stratigraphy of the Upper Devonian - Lower Carboniferous of south-west of Lyzha-Kyrtael swell (Pechora Plate eastward)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 1, available at: http://www.ngtp.ru/rub/2023/8_2023.html DOI: 10.17353/2070-5379/8_2023
Zhuravlev A.V., Sobolev D.B. Konodonty pogranichnykh vizeysko-serpukhovskikh otlozheniy yuzhnoy chasti gryady Chernysheva (r. Iz"yayu) [Conodonts of the Visean-Serpukhovian boundary level of the southern part of the Сhernyshev Ridge (Iz'yayu River)]. Syktyvkarskiy paleontologicheskiy sbornik, 2000, no. 4, pp. 84-89.
Zhuravlev A.V., Vevel Y.A., Gruzdev D.A., Erofeevsky A.V. Late Mississippian (early Serpukhovian) carbon isotope record of northern Laurussia: A proposal for the Visean / Serpukhovian boundary. Revista Mexicana de Ciencias Geológicas, 2023, vol. 40, no. 1, pp. 35-43. DOI: 10.22201/cgeo.20072902e.2023.1.1722
Stratigraphy and lithology
| Article # 13_2022 | submitted on 06/04/2021 displayed on website on 06/03/2022 |
| 31 p. | Zhuravlev A.V., Vevel Ya.A. |
| Biostratigraphy of conodonts and foraminifera of Upper Devonian - Lower Permian of the Padimey Area (north-east of Timan-Pechora petroleum Province) - new data | |
| The article considers new data on the biostratigraphy of the Upper Devonian Lower Permian of the Padimey Area (Vorkuta transverse uplift of the Cis-Uralian depression). Conodont Alteration Index allows reconstruct paleogeothermal gradient of 50°C per kilometer (20°C per kilometer accounting sediment compaction). The Lower Permian possesses thermal maturity of PK-MK1 grade, but the Upper Devonian has thermal maturity of MK1-2 grade. Keywords: biostratigraphy, Upper Devonian, Lower Permian, thermal maturation, Padimey Area, Timan-Pechora petroleum Province. |
|
| article citation | Zhuravlev A.V., Vevel Ya.A. Biostratigrafiya verkhnego devona – nizhney permi Padimeyskoy ploshchadi (severo-vostok Timano-Pechorskoy neftegazonosnoy provintsii) po konodontam i foraminiferam [Biostratigraphy of conodonts and foraminifera of Upper Devonian - Lower Permian of the Padimey Area (north-east of Timan-Pechora petroleum Province) – new data]. Neftegazovaya Geologiya. Teoriya I Praktika, 2022, vol. 17, no. 2, available at: http://www.ngtp.ru/rub/2022/13_2022.html |
| DOI | https://doi.org/10.17353/2070-5379/13_2022 |
References
Burnett R.D. Regional maturation patterns for Late Visean (Carboniferous, Dinantian) rocks of northern England based on mapping of conodont colour. Irish Journal of Earth Sciences, 1987, no. 8, pp. 165-185.
Danilov V.N. Perspektivy neftegazonosnosti verkhnedevonskikh otlozheniy severnoy chasti Kos'yu-Rogovskoy vpadiny [Prospects for the oil and gas potential of the Upper Devonian strata in the northern part of the Kosyu-Rogov depression]. Geologiya nefti i gaza, 1992, no. 8, http://geolib.narod.ru/Journals/OilGasGeo/1992/08/Stat/01/stat01.html
Durkina A.V. Foraminifery serpukhovskogo yarusa Timano-Pechorskoy provintsii [Foraminifers of the Serpukhov Formation of the Timan-Pechora Province]. St. Petersburg: Izd-vo Sankt-Peterburgskoy kartograficheskoy fabriki VSEGEI, 2002, 198 p.
Epstein A.G., Epstein J.B., Harris L.D. Conodont Color Alteration - an Index Organic Metamorphism. U.S. Geological Survey Professional Paper, 1977, no. 995, pp. 1-27.
Grigor'ev M.N. Analiz struktury resursnoy bazy mineral'no-syr'evykh tsentrov nefti kontinental'noy chasti Nenetskogo avtonomnogo okruga [Analysis of the structure of the resource base of mineral resource centers of oil in the continental part of the Nenets Autonomous Okrug]. Neftyanoe khozyaystvo, 2014, no.5, pp. 12-18.
Jones G.L. Irish Carboniferous conodonts record maturation levels and the influence of tectonisn, igneous activity and mineralization. Terra Nova, 1992, no. 4(4), pp. 238-244.
Kirkinskaya V.Η, Smekhov Ε.Μ. Karbonatnye porody - kollektory nefti i gaza [Carbonate rocks as oil and gas reservoirs]. Leningrad: Nedra, 1981, 255 p.
Kostygova P.K. Pechorskiy paleobasseyn v vizeyskom i serpukhovskom vekakh i foraminifery nizhnego vize [Pechora paleobasin in the Visean and Serpukhovian and Foraminifera of the lower Visean]. St. Petersburg: Izd-vo St-Peterburgskoy kartograficheskoy fabriki VSEGEI, 2004, 204 p.
Nikitin D.S, Khutorskoy M.D., Ivanov D.A. Vertikal'naya katageneticheskaya zonal'nost' osadochnogo chekhla severo-vostochnoy chasti Barentsevomorskogo shel'fa [Vertical catagenetic zonality of the sedimentary cover of the northeastern part of the Barents Sea shelf]. Litologiya i poleznye iskopaemye, 2020, no. 5, pp. 438-460.
Zhuravlev A.V. Dinamika taksonomicheskogo raznoobraziya konodontov v pozdnem devone-rannem karbone (famenskiy-serpukhovskiy veka) [Dynamics of taxonomic diversity of Conodonts in the Late Devonian-Early Carboniferous (Famenian-Serpukhovian Age)]. Litosfera, 2019, no. 1, pp.81-91.
Zhuravlev A.V. Otsenka stepeni termal'nogo katageneza paleozoyskikh otlozheniy severa Pay-Khoyskogo paravtokhtona po indeksam okraski konodontov [Estimation of the degree of thermal catagenesis of Paleozoic in the north of the Pay-Khoy paraautochthon based on the color indices of Conodonts]. Litosfera, 2017, no. 1, pp.44-52.
Danilov V.N. Perspektivy neftegazonosnosti verkhnedevonskikh otlozheniy severnoy chasti Kos'yu-Rogovskoy vpadiny [Prospects for the oil and gas potential of the Upper Devonian strata in the northern part of the Kosyu-Rogov depression]. Geologiya nefti i gaza, 1992, no. 8, http://geolib.narod.ru/Journals/OilGasGeo/1992/08/Stat/01/stat01.html
Durkina A.V. Foraminifery serpukhovskogo yarusa Timano-Pechorskoy provintsii [Foraminifers of the Serpukhov Formation of the Timan-Pechora Province]. St. Petersburg: Izd-vo Sankt-Peterburgskoy kartograficheskoy fabriki VSEGEI, 2002, 198 p.
Epstein A.G., Epstein J.B., Harris L.D. Conodont Color Alteration - an Index Organic Metamorphism. U.S. Geological Survey Professional Paper, 1977, no. 995, pp. 1-27.
Grigor'ev M.N. Analiz struktury resursnoy bazy mineral'no-syr'evykh tsentrov nefti kontinental'noy chasti Nenetskogo avtonomnogo okruga [Analysis of the structure of the resource base of mineral resource centers of oil in the continental part of the Nenets Autonomous Okrug]. Neftyanoe khozyaystvo, 2014, no.5, pp. 12-18.
Jones G.L. Irish Carboniferous conodonts record maturation levels and the influence of tectonisn, igneous activity and mineralization. Terra Nova, 1992, no. 4(4), pp. 238-244.
Kirkinskaya V.Η, Smekhov Ε.Μ. Karbonatnye porody - kollektory nefti i gaza [Carbonate rocks as oil and gas reservoirs]. Leningrad: Nedra, 1981, 255 p.
Kostygova P.K. Pechorskiy paleobasseyn v vizeyskom i serpukhovskom vekakh i foraminifery nizhnego vize [Pechora paleobasin in the Visean and Serpukhovian and Foraminifera of the lower Visean]. St. Petersburg: Izd-vo St-Peterburgskoy kartograficheskoy fabriki VSEGEI, 2004, 204 p.
Nikitin D.S, Khutorskoy M.D., Ivanov D.A. Vertikal'naya katageneticheskaya zonal'nost' osadochnogo chekhla severo-vostochnoy chasti Barentsevomorskogo shel'fa [Vertical catagenetic zonality of the sedimentary cover of the northeastern part of the Barents Sea shelf]. Litologiya i poleznye iskopaemye, 2020, no. 5, pp. 438-460.
Zhuravlev A.V. Dinamika taksonomicheskogo raznoobraziya konodontov v pozdnem devone-rannem karbone (famenskiy-serpukhovskiy veka) [Dynamics of taxonomic diversity of Conodonts in the Late Devonian-Early Carboniferous (Famenian-Serpukhovian Age)]. Litosfera, 2019, no. 1, pp.81-91.
Zhuravlev A.V. Otsenka stepeni termal'nogo katageneza paleozoyskikh otlozheniy severa Pay-Khoyskogo paravtokhtona po indeksam okraski konodontov [Estimation of the degree of thermal catagenesis of Paleozoic in the north of the Pay-Khoy paraautochthon based on the color indices of Conodonts]. Litosfera, 2017, no. 1, pp.44-52.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 37_2019 | submitted on 08/12/2019 displayed on website on 11/05/2019 |
| 20 p. | Zhuravlev A.V., Vevel Ya.A., Plotitsyn A.N., Erofeevskiy A.V., Lukin V.Yu. |
| Late Tournaisian shallow-water sequenses of the eastern part of Timan-Pechora Province (Kozhva River) | |
| The shallow-water Upper Tournaisian sequences of the eastern part of Timan-Pechora petroleum Province were studied with biostratigraphical (based on foraminifers, conodonts, and brachiopods) and isotope stratigraphical methods. Poor conodont associations containing Siphonodella obsoleta Hass and S. cooperi Hass are characteristic of this stratigraphic interval in the shallow-water facies. Foraminifer associations are very variable: some of them are composed of numerous late Tournaisian species (Kozhva River section), but some associations comprise just species of wide stratigraphic range. The prominent global positive shift in the carbonate carbon isotope record marks the upper Tournaisian in the region. This shift is considered as reliable stratigraphical marker. Keywords: shallow-water sequence, Lower Carboniferous, Upper Tournaisian, biostratigraphy, isotope stratigraphy, Timan-Pechora petroleum Province. |
|
| article citation | Zhuravlev A.V., Vevel Ya.A., Plotitsyn A.N., Erofeevsky A.V., Lukin V.Yu. Pozdneturneyskie melkovodnye otlozheniya vostoka Timano-Pechorskoy provintsii (r. Kozhva) [Late Tournaisian shallow-water sequenses of the eastern part of Timan-Pechora Province (Kozhva River)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 4, available at: http://www.ngtp.ru/rub/2019/37_2019.html |
| DOI | https://doi.org/10.17353/2070-5379/37_2019 |
References
Chernov G.A. Nizhniy karbon Pechorskoy gryady [Lower Carboniferous of the Pechora Swell]. Sbornik trudov po geologii i paleontologii, Syktyvkar, 1960, pp. 56–93.
Durkina A.V. O zonal'nom raschlenenii pogranichnykh otlozheniy nizhne-verkhneturneyskogo pod"yarusov po foraminiferam i o granitse mezhdu nimi v Timano-Pechorskoy provintsii [About foraminiferal zonation and boundary of the lower-upper Tournaisian of the Timan-Pechora province]. Biostratigrafiya neftegazonosnykh basseynov: Tr. 1-go Mezhdunarodnogo simpoziuma. St. Petersburg: VNIGRI, 1997, pp. 70–75.
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Razrez verkhnego devona – nizhnego karbona na r. Talota (Timano-Pechorskaya provintsiya) - rezul'taty litologicheskikh, biostratigraficheskikh i paleomagnitnykh issledovaniy [Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 4, available at: http://www.ngtp.ru/rub/2/45_2009.pdf
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Razrez verkhnego devona – nizhnego karbona na r. Talota (Timano-Pechorskaya provintsiya) - rezul'taty litologicheskikh, biostratigraficheskikh i paleomagnitnykh issledovaniy / Prilozhenie [Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 4, available at: http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf
Howard C., Brunton C., Lazarev S.S., Grant R.E., Jin Yu-gan. Productidina. Treatise on Invertebrate Paleontology / Editor Pt.H. Revis. Brachiopoda, 2000, vol. 3, pp. 424–609.
Hudson R.G.S., Clarke M.J., Sevastopulo G.D. A detailed account of the fauna and age of a Waulsortian Reef Knoll Limestone and associated shales. Scientific Proceedings of the Royal Dublin Society, 1966, ser. A2, no. 16, pp. 251–272.
Kulagina E.I., Stepanova T.I., Zaytseva E.L., Gorozhanina E.N., Gibshman N.B., Ivanova R.M., Vevel' Ya.A., Ponomareva G.Yu., Filimonova T.V. Atlas foraminifer i mikrofatsiy verkhnedevonskikh i nizhnekamennougol'nykh otlozheniy Severnoy Evrazii. Famenskiy i turneyskiy yarusy [Atlas of foraminifers and microfacies of the Upper Devonian and Lower Carboniferous depososits of the Northern Eurasia. Famennian and Tournaisian stages]. Moscow: PIN RAN, 2018, 220 p.
Muir-Wood H., Cooper G. Morphology, Classification and Life Habits of the Productoidea (Brachiopoda). Geol. Soc. America, 1960, mem. 81, 447 p.
Nikonov N.I., Bogatskiy V.I., Martynov A.V., Larionova Z.V., Laskin V.M., Galkina L.V., Dovzhikova E.G., Ermakova O.L., Kostygova P.K., Kuranova T.I., Moskalenko K.A., Pankratov Yu.A., Petrenko E.L., Popova E.V., Surina A.I., Shabanova G.A. Timano-Pechorskiy sedimentatsionnyy basseyn kart [Timan-Pechora sedimentary basin. Atlas of geological maps]. Atlas geologicheskikh kart, Ukhta, 2000, 67 p.
Qie W.K., Zhang X.H., Du Y.S., Zhang Y. Lower Carboniferous carbon isotope stratigraphy in South China: Implications for the Late Paleozoic glaciation. Sci. China Earth Sci., 2011, 54, pp. 84–92. DOI: https://doi.org/10.1007/s11430-010-4062-4
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in δ13C: an example from the lower Mississippian. Paleogeography, Paleoclimatology, Paleoecology, 2004, no. 213, pp. 359–377.
Sarycheva T.G., Sokol'skaya A.N., Beznosova G.A., Maksimova S.V. Brakhiopody i paleogeografiya karbona Kuznetskoy kotloviny [Brachiopods and Paleogeography of the Carboniferous of the Kuznetsk Basin]. Moscow, 1963, 547 p. (Trudy PIN, vol. 65).
Sokol'skaya A.N. Brahiopody osnovaniya Podmoskovnogo karbona i perekhodnyh devonsko-kamennougol'nyh otlozhenij (Chernyshinskie, Upinskie i Malevsko-Muraevninskie sloi) [Brachiopods of the base of the Carboniferous of the Moscow region and transitional Devonian-Carboniferous boundary deposits (Chernysh, Upian and Malevska-Muraevna levels)]. Patr. 1. Spiriferidae. Moscow: Izd-vo AN SSSR, 1941, 138 p. (Trudy Paleontologicheskogo instituta, vol. 12, no. 2).
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Zhuravlev A.V. Tafonomiya konodontovykh elementov v usloviyakh melkovodnogo karbonatnogo shel'fa na primere nizhnego karbona vostochnoy chasti Timano-Pechorskogo basseyna [Taphonomy of conodont elements in the environments of shallow-water Carbonate shelf – the Lower Carboniferous of the eastern part of Timan-Pechora basin as example]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 1, available at: http://www.ngtp.ru/rub/2019/5_2019.html. DOI: https://doi.org/10.17353/2070-5379/5_2019
Zhuravlev A.V., Vevel Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) ]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf. DOI: https://doi.org/10.17353/2070-5379/3_2018
Durkina A.V. O zonal'nom raschlenenii pogranichnykh otlozheniy nizhne-verkhneturneyskogo pod"yarusov po foraminiferam i o granitse mezhdu nimi v Timano-Pechorskoy provintsii [About foraminiferal zonation and boundary of the lower-upper Tournaisian of the Timan-Pechora province]. Biostratigrafiya neftegazonosnykh basseynov: Tr. 1-go Mezhdunarodnogo simpoziuma. St. Petersburg: VNIGRI, 1997, pp. 70–75.
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Razrez verkhnego devona – nizhnego karbona na r. Talota (Timano-Pechorskaya provintsiya) - rezul'taty litologicheskikh, biostratigraficheskikh i paleomagnitnykh issledovaniy [Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 4, available at: http://www.ngtp.ru/rub/2/45_2009.pdf
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Razrez verkhnego devona – nizhnego karbona na r. Talota (Timano-Pechorskaya provintsiya) - rezul'taty litologicheskikh, biostratigraficheskikh i paleomagnitnykh issledovaniy / Prilozhenie [Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 4, available at: http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf
Howard C., Brunton C., Lazarev S.S., Grant R.E., Jin Yu-gan. Productidina. Treatise on Invertebrate Paleontology / Editor Pt.H. Revis. Brachiopoda, 2000, vol. 3, pp. 424–609.
Hudson R.G.S., Clarke M.J., Sevastopulo G.D. A detailed account of the fauna and age of a Waulsortian Reef Knoll Limestone and associated shales. Scientific Proceedings of the Royal Dublin Society, 1966, ser. A2, no. 16, pp. 251–272.
Kulagina E.I., Stepanova T.I., Zaytseva E.L., Gorozhanina E.N., Gibshman N.B., Ivanova R.M., Vevel' Ya.A., Ponomareva G.Yu., Filimonova T.V. Atlas foraminifer i mikrofatsiy verkhnedevonskikh i nizhnekamennougol'nykh otlozheniy Severnoy Evrazii. Famenskiy i turneyskiy yarusy [Atlas of foraminifers and microfacies of the Upper Devonian and Lower Carboniferous depososits of the Northern Eurasia. Famennian and Tournaisian stages]. Moscow: PIN RAN, 2018, 220 p.
Muir-Wood H., Cooper G. Morphology, Classification and Life Habits of the Productoidea (Brachiopoda). Geol. Soc. America, 1960, mem. 81, 447 p.
Nikonov N.I., Bogatskiy V.I., Martynov A.V., Larionova Z.V., Laskin V.M., Galkina L.V., Dovzhikova E.G., Ermakova O.L., Kostygova P.K., Kuranova T.I., Moskalenko K.A., Pankratov Yu.A., Petrenko E.L., Popova E.V., Surina A.I., Shabanova G.A. Timano-Pechorskiy sedimentatsionnyy basseyn kart [Timan-Pechora sedimentary basin. Atlas of geological maps]. Atlas geologicheskikh kart, Ukhta, 2000, 67 p.
Qie W.K., Zhang X.H., Du Y.S., Zhang Y. Lower Carboniferous carbon isotope stratigraphy in South China: Implications for the Late Paleozoic glaciation. Sci. China Earth Sci., 2011, 54, pp. 84–92. DOI: https://doi.org/10.1007/s11430-010-4062-4
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in δ13C: an example from the lower Mississippian. Paleogeography, Paleoclimatology, Paleoecology, 2004, no. 213, pp. 359–377.
Sarycheva T.G., Sokol'skaya A.N., Beznosova G.A., Maksimova S.V. Brakhiopody i paleogeografiya karbona Kuznetskoy kotloviny [Brachiopods and Paleogeography of the Carboniferous of the Kuznetsk Basin]. Moscow, 1963, 547 p. (Trudy PIN, vol. 65).
Sokol'skaya A.N. Brahiopody osnovaniya Podmoskovnogo karbona i perekhodnyh devonsko-kamennougol'nyh otlozhenij (Chernyshinskie, Upinskie i Malevsko-Muraevninskie sloi) [Brachiopods of the base of the Carboniferous of the Moscow region and transitional Devonian-Carboniferous boundary deposits (Chernysh, Upian and Malevska-Muraevna levels)]. Patr. 1. Spiriferidae. Moscow: Izd-vo AN SSSR, 1941, 138 p. (Trudy Paleontologicheskogo instituta, vol. 12, no. 2).
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Zhuravlev A.V. Tafonomiya konodontovykh elementov v usloviyakh melkovodnogo karbonatnogo shel'fa na primere nizhnego karbona vostochnoy chasti Timano-Pechorskogo basseyna [Taphonomy of conodont elements in the environments of shallow-water Carbonate shelf – the Lower Carboniferous of the eastern part of Timan-Pechora basin as example]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 1, available at: http://www.ngtp.ru/rub/2019/5_2019.html. DOI: https://doi.org/10.17353/2070-5379/5_2019
Zhuravlev A.V., Vevel Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) ]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf. DOI: https://doi.org/10.17353/2070-5379/3_2018
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 32_2019 | submitted on 07/24/2019 displayed on website on 09/05/2019 |
| 24 p. | Gruzdev D.A., Kotik I.S., Vevel Ya.A., Zhuravlev A.V., Kotik O.S. |
| Lithofacial characteristics and organic matter geochemistry of the Devonian-Carboniferous section оf folded and thrust belt area of the Kosyu-Rogov Depression southeastern part (using Levogrubeyu-1 well data as reference source) | |
| The results of study of the Middle-Upper Palaeozoic bioherm-shoal association in the east of the Timan-Pechora petroleum Basin (based on the Levogrubeyu-1 well description) are presented. The core lithological study allows distinguishing the facial analogues with the succession types of the Bolshaya Nadota carbonate association. It is supposed that the bioherm-shoal association demonstrates similar architecture along the all shelf border. Foraminifera and Conodont studies allow as to improve the biostratigraphic subdivision of the succession discovered by the borehole. The geochemical investigations reveal that the Devonian-Carboniferous rocks in the core samples disclose low hydrocarbon generation potential. On the other hand high hydrocarbon potential is supposed for the clayey-carbonate units of Middle-Late Frasnian age. Rock-Eval pyrolysis and the Conodont Alteration Index indicate a high level maturity of organic matter corresponding to the main gas generation zone (Ro > 1.5 %). Keywords: lithofacial study, organic matter, hydrocarbons, Upper Palaeozoic, Kosyu-Rogov Depression, Timan-Pechora petroleum basin. |
|
| article citation | Gruzdev D.A., Kotik I.S., Vevel Ya.A., Zhuravlev A.V., Kotik O.S., Priymak P.I. Litologo-fatsial'naya kharakteristika i geokhimiya organicheskogo veshchestva devonsko-kamennougol'nykh otlozheniy skladchato-nadvigovoy zony yugo-vostoka Kos'yu-Rogovskoy vpadiny (po dannym skvazhiny Levogrubeyuskaya-1) [Lithofacial characteristics and organic matter geochemistry of the Devonian-Carboniferous section оf folded and thrust belt area of the Kosyu-Rogov Depression southeastern part (using Levogrubeyu-1 well data as reference source)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 3, available at: http://www.ngtp.ru/rub/2019/32_2019.html |
| DOI | https://doi.org/10.17353/2070-5379/32_2019 |
References
Antoshkina A.I. Rifoobrazovanie v paleozoe (sever Urala i sopredel'nye oblasti) [Paleozoic reef formation (northern Urals and adjacent areas)]. Ekaterinburg: UrO RAN, 2003, 303 p.
Danilevskiy S.A., Sklyarova Z.P., Trifachev Yu.M. Geoflyuidal'nye sistemy Timano-Pechorskoy provintsii [Geo-fluid system of the Timan-Pechora Province]. Ukhta, 2003, 298 p.
Eliseev A.I. Karbon Lemvinskoy zony severa Urala [Carboniferous Lemva area of Northern Urals]. Leningrad: Nauka, 1973, 95 p.
Geologicheskoe stroenie i perspektivy gazonosnosti zapadnogo sklona Polyarnogo i Pripolyarnogo Urala (po rezul'tatam geologorazvedochnykh rabot) [Geological structure and gas potential of the western slope of the Polar and Subpolar Urals (according to the results of exploration study)]. Editor V.N. Danilova, St. Petersburg: FGUP «VNIGRI», 2015, 264 p.
Gruzdev D.A. Pozdnedevonskaya-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [The Late Devonian-Early Carboniferous isolated carbonate platform in the Subpolar Urals (Bol'shaya Nadota River)]. Vestnik IG Komi NTs UrO RAN, 2017, no. 4, pp.16-23.
Ivanova R.M. Izvestkovye vodorosli karbona Urala [The calcareous algae of the Carboniferous of the Urals]. Ekaterinburg: RIO UrO RAN, 2013, 244 p.
Khant D. Geologiya i geokhimiya nefti i gaza [Geology and oil and gas geochemistry]. Moscow: Mir, 1982, 703 p.
Peters K.E. Guidelines for evaluating petroleum source rock using programmed pyrolysis. Am. Assoc. Petrol. Geol. Bull., 1986, vol. 70, pp.318–329.
Peters K.E., Cassa M.R. Applied sourse rock geochemistry / The petroleum system – from source to trap. AAPG Memoir 60. Tulsa, Oklahoma, U.S.A, 1994, pp. 93–117. Prishchepa O.M., Bogatskiy V.I., Makarevich V.N., Chumakova O.V., Nikonov N.I., Kuranov A.V., Bogdanov M.M. Novye predstavleniya o tektonicheskom i neftegazogeologicheskom rayonirovanii Timano-Pechorskoy neftegazonosnoy provintsii [The Timan-Pechora oil-bearing province – new tectonical insight]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 4, available at: http://www.ngtp.ru/rub/4/40_2011.pdf
Priymak P.I., Nikonov N.I., Kuranova T.I. Perspektivy neftegazonosnosti rifogennykh otlozheniy zony sochleneniya Kos'yu-Rogovskoy vpadiny i Zapadno-Ural'skoy skladchato-nadvigovoy zony [Petroleum potential of Middle - Upper Devonian reef section in the junction zone of Kosyu-Rogow Depression and the Western Ural fold-thrust zone]. Neftegazovaya Geologiya. Teoriya I Praktika, 2013, vol. 8, no. 3, available at: http://www.ngtp.ru/rub/4/36_2013.pdf. DOI: https://doi.org/10.17353/2070-5379/36_2013
Skompski S., Paszkowski M., Krobicki M., Kokovin K., Korn D., Tomas A. & Wrzolek T. Depositional setting of the Devonian/Carboniferous biohermal Bol'shaya Nadota Carbonate Complex, Subpolar Urals. Acta Geologica Polonica, 2001, no. 3, pp. 217-235.
Spravochnik po geokhimii nefti i gaza [Handbook of oil and gas geochemistry]. St. Petersburg: Nedra, 1998, 576 p.
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of North Urals and Pay-Khoy]. RAN, Ural. otd-nie, Komi nauch. tsentr, In-t geologii, Ekaterinburg: Nauka, 1994, 284 p.
Zhukova T.V., Petrenko E.L. Stroenie i perspektivy ranne-sredne-pozdnedevonskogo rifa v skv. 1-Levogrubeyuskaya [The structure and prospects concerning the Early-Middle-Late Devonian reef in the well 1-Levogrubeyu]. Geologiya rifov: materialy Vserossiyskogo litologicheskogo soveshchaniya. Syktyvkar: IG Komi NTs UrO RAN, 2015, pp. 45-47.
Zhuravlev A.V. Otsenka stepeni termal'nogo katageneza paleozoyskikh otlozheniy severa Pay-Khoyskogo paravtokhtona po indeksam okraski konodontov [Estimation of Palaeozoic sedimentary rocks thermal maturity of Northern Pay-Khoy parautochthone on the basis of Conodont colour alteration index]. Litosfera, 2017, no. 1, pp. 44–52.
Zhuravlev A.V. Sedimentatsionnaya model' oblasti sochleneniya Eletskoy i Lemvinskoy formatsionnykh zon Pripolyarnogo Urala v pogranichnom devonsko-kamennougol'nom intervale [Sedimentation model of the transitional zone from the Elets to Lemva formation belts (Devonian-Carboniferous boundary, Cis-Polar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 4, available at: http://www.ngtp.ru/rub/2/59_2012.pdf
Danilevskiy S.A., Sklyarova Z.P., Trifachev Yu.M. Geoflyuidal'nye sistemy Timano-Pechorskoy provintsii [Geo-fluid system of the Timan-Pechora Province]. Ukhta, 2003, 298 p.
Eliseev A.I. Karbon Lemvinskoy zony severa Urala [Carboniferous Lemva area of Northern Urals]. Leningrad: Nauka, 1973, 95 p.
Geologicheskoe stroenie i perspektivy gazonosnosti zapadnogo sklona Polyarnogo i Pripolyarnogo Urala (po rezul'tatam geologorazvedochnykh rabot) [Geological structure and gas potential of the western slope of the Polar and Subpolar Urals (according to the results of exploration study)]. Editor V.N. Danilova, St. Petersburg: FGUP «VNIGRI», 2015, 264 p.
Gruzdev D.A. Pozdnedevonskaya-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [The Late Devonian-Early Carboniferous isolated carbonate platform in the Subpolar Urals (Bol'shaya Nadota River)]. Vestnik IG Komi NTs UrO RAN, 2017, no. 4, pp.16-23.
Ivanova R.M. Izvestkovye vodorosli karbona Urala [The calcareous algae of the Carboniferous of the Urals]. Ekaterinburg: RIO UrO RAN, 2013, 244 p.
Khant D. Geologiya i geokhimiya nefti i gaza [Geology and oil and gas geochemistry]. Moscow: Mir, 1982, 703 p.
Peters K.E. Guidelines for evaluating petroleum source rock using programmed pyrolysis. Am. Assoc. Petrol. Geol. Bull., 1986, vol. 70, pp.318–329.
Peters K.E., Cassa M.R. Applied sourse rock geochemistry / The petroleum system – from source to trap. AAPG Memoir 60. Tulsa, Oklahoma, U.S.A, 1994, pp. 93–117. Prishchepa O.M., Bogatskiy V.I., Makarevich V.N., Chumakova O.V., Nikonov N.I., Kuranov A.V., Bogdanov M.M. Novye predstavleniya o tektonicheskom i neftegazogeologicheskom rayonirovanii Timano-Pechorskoy neftegazonosnoy provintsii [The Timan-Pechora oil-bearing province – new tectonical insight]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 4, available at: http://www.ngtp.ru/rub/4/40_2011.pdf
Priymak P.I., Nikonov N.I., Kuranova T.I. Perspektivy neftegazonosnosti rifogennykh otlozheniy zony sochleneniya Kos'yu-Rogovskoy vpadiny i Zapadno-Ural'skoy skladchato-nadvigovoy zony [Petroleum potential of Middle - Upper Devonian reef section in the junction zone of Kosyu-Rogow Depression and the Western Ural fold-thrust zone]. Neftegazovaya Geologiya. Teoriya I Praktika, 2013, vol. 8, no. 3, available at: http://www.ngtp.ru/rub/4/36_2013.pdf. DOI: https://doi.org/10.17353/2070-5379/36_2013
Skompski S., Paszkowski M., Krobicki M., Kokovin K., Korn D., Tomas A. & Wrzolek T. Depositional setting of the Devonian/Carboniferous biohermal Bol'shaya Nadota Carbonate Complex, Subpolar Urals. Acta Geologica Polonica, 2001, no. 3, pp. 217-235.
Spravochnik po geokhimii nefti i gaza [Handbook of oil and gas geochemistry]. St. Petersburg: Nedra, 1998, 576 p.
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of North Urals and Pay-Khoy]. RAN, Ural. otd-nie, Komi nauch. tsentr, In-t geologii, Ekaterinburg: Nauka, 1994, 284 p.
Zhukova T.V., Petrenko E.L. Stroenie i perspektivy ranne-sredne-pozdnedevonskogo rifa v skv. 1-Levogrubeyuskaya [The structure and prospects concerning the Early-Middle-Late Devonian reef in the well 1-Levogrubeyu]. Geologiya rifov: materialy Vserossiyskogo litologicheskogo soveshchaniya. Syktyvkar: IG Komi NTs UrO RAN, 2015, pp. 45-47.
Zhuravlev A.V. Otsenka stepeni termal'nogo katageneza paleozoyskikh otlozheniy severa Pay-Khoyskogo paravtokhtona po indeksam okraski konodontov [Estimation of Palaeozoic sedimentary rocks thermal maturity of Northern Pay-Khoy parautochthone on the basis of Conodont colour alteration index]. Litosfera, 2017, no. 1, pp. 44–52.
Zhuravlev A.V. Sedimentatsionnaya model' oblasti sochleneniya Eletskoy i Lemvinskoy formatsionnykh zon Pripolyarnogo Urala v pogranichnom devonsko-kamennougol'nom intervale [Sedimentation model of the transitional zone from the Elets to Lemva formation belts (Devonian-Carboniferous boundary, Cis-Polar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 4, available at: http://www.ngtp.ru/rub/2/59_2012.pdf
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 25_2019 | submitted on 06/18/2019 displayed on website on 08/02/2019 |
| 27 p. | Plotitsyn A.N., Vevel Ya.A. |
| Conodonts of the Devonian-Carboniferous boundary deposits of the Kozhim River key section (Subpolar Urals) | |
| A new version of conodont biostratigraphy (based on compilation of new author’s and published materials) of Tournaisian part of the Kozhim River key section is given. The zones/subzones expansa, sulcata, Lower duplicata, Upper duplicata-sandbergi, quadruplicata and isosticha are characterized. The bases of all zonal subdivisions except for sulcata and duplicata Zones are shifted (compared to the latest versions of zonal biostratigraphy). The most reliably diagnosed zones (the base of the sulcata, duplicata, and quadruplicata Zones) are established in carbonate graded cycles (calciturbidites). The deposits of the terminal Famennian are very conditionally compared with the Lower and lower part of the Middle praesulcata Zones according to the position in the section. Absence of deposits of the upper part of the Middle and Upper praesulcata Zones suggests the presence of erosion on the D/C boundary interval. The presence of erosion on the D/C boundary interval doesn’t allow using the Kozhim River section as a key section of the stratigraphic boundary (in accordance with the tasks and rules of studying and describing the key stratigraphic sections developed by an interdepartmental stratigraphic committee). However, formally this section can be used as a key section of the structural-facial zone due to the fact that it is the most studied, and by the availability of outcrops, it exceeds all sections within the development of deep-shelf deposits of the Kozhim intra-shelf palaeodepression. Keywords: conodonts, biostratigraphy, Famennian, Tournaisian, key section, Subpolar Urals. |
|
| article citation | Plotitsyn A.N., Vevel Ya.A. Biostratigrafiya verkhnedevonsko-nizhnekamennougol'nykh otlozheniy opornogo razreza na r. Kozhim (Pripolyarnyy Ural) po konodontam [Conodonts of the Devonian-Carboniferous boundary deposits of the Kozhim River key section (Subpolar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 3, available at: http://www.ngtp.ru/rub/2019/25_2019.html |
| DOI | https://doi.org/10.17353/2070-5379/25_2019 |
References
Becker R.T., Kaiser S.I., Aretz M. Review of chrono-, litho- and biostratigraphy across the global Hangenberg Crisis and Devonian–Carboniferous Boundary // Devonian Climate, Sea Level and Evolutionary Events; Editors R.T. Becker, P. Konigshof, C.E. Brett. Geological Society, 2016, no. 423, pp. 355–386.
Brenckle P.L. Late Tournaisian (Lower Carboniferous) foraminifers from the Middle Urals and their use in Russian Horizon Definition // Late Paleozoic Foraminifera; their biostratigraphy, evolution, and paleoecology; and the Mid-Carboniferous boundary; Editors C.A. Ross, J.R.P. Ross, P.L. Brenckle. Cushman Found. Foram. Res. Special Publication 36, 1997, pp. 5–9.
Chermnykh V.A. Stratigrafiya karbona severa Urala [Stratigraphy of the Carboniferous of the North of the Urals]. Leningrad, 1976, 302 p.
Chermnykh V.A., Kochetkova N.M., Pazukhin V.N., Lipina O.A. Pogranichnye devonsko-kamennougol'nye otlozheniya Severnogo i Pripolyarnogo Urala [Devonian-Carboniferous boundary deposits of the Northern and Subpolar Urals]. Granitsa devona i karbona na territorii SSSR, Minsk, 1988, pp. 145–151.
Chermnykh V.A., Kononova L.I., Pazukhin V.N., Cheusova G.N. Tri tipa razrezov otlozheniy, perekhodnykh mezhdu devonom i karbonom na severe Ural'skoy skladchatoy oblasti [Three types of sections of transitional deposits between the Devonian and Carboniferous in the North Ural folded region]. Biostratigrafiya pogranichnykh otlozheniy devona i karbona SSSR, Magadan, 1980, pp. 1–18.
Corradini C., Barca S., Spalletta C. Late Devonian-Early Carboniferous conodonts from the «Clymeniae limestones» of SE Sardinia (Italy) // Courier Forschungs-Institut Senckenberg, 2003, no.245, pp. 227–253.
Corradini C., Spaletta C., Mossoni A., Matyja H., Over D.J. Conodonts across the Devonian/Carboniferous boundary: a review and implication for the redefinition of the boundary and a proposal for an updated conodont zonation // Geological Magazine, 2016, no. 1, pp. 1–15.
Deulin Yu.V. Konodonty i korrelyatsiya produktivnykh na neft' verkhnedevonskikh otlozheniy severa Timano-Pechorskoy provintsii [Conodonts and correlation of oil-producing Upper Devonian deposits in the north of the Timan-Pechora province]. Arhangel'sk: Pravda Severa, 2006, 253 p.
Ivanov K.S. Sovremennye metodiki vydeleniya konodontov (obzor) [Modern methods for isolating conodonts (review)]. Problemy sovremennoy mikropaleontologii, Leningrad: Nauka, 1990, pp. 149–156.
Kaiser S.I. Mass Extinctions, Climatic and Oceanographic Changes at the Devonian-Carboniferous Boundary: Ph. D. Dissertation. Germany: Ruhr-University Bochum, 2005, 156 p. Kochetkova N.M., Reytlinger E.A., Pazukhin V.N., Avkhimovich V.I. Granitsa devona i karbona na Yuzhnom Urale [The Devonian-Carboniferous boundary in the Southern Urals]. Granitsa devona i karbona na territorii SSSR. Minsk: Nauka i tekhnika, 1988, pp. 157–166.
Kondratenko-Zav'yalova E.A. Verkhneturneyskie foraminifery L'vovsko-Volynskogo ugol'nogo basseyna [Upper Tournaisian Foraminifera of the Lviv-Volyn coal basin]. Paleontologicheskiy sbornik, 1974, vol. 1, no. 10, pp. 11–15.
Kulagina E.I., Stepanova T.I., Zaytseva E.L., Gorozhanina E.N., Gibshman N.B., Ivanova R.M., Vevel' Ya.A., Ponomareva G.Yu., Filimonova T.V. Atlas foraminifer i mikrofatsiy verkhnedevonskikh i nizhnekamennougol'nykh otlozheniy Severnoy Evrazii. Famenskiy i turneyskiy yarusy [Atlas of foraminifers and microfacies of the Upper Devonian and Lower Carboniferous depososits of the Northern Eurasia. Famennian and Tournaisian stages]. Moscow: PIN RAN, 2018, 220 p.
Nemirovskaya T.I., Chermnykh V.A., Kononova L.I., Pazukhin V.N. Conodonts of the Devonian-Carboniferous boundary section, Kozhim, Polar Urals, Russia // Annales de la Societe geologique de Belgique, 1992, vol. 115, pp. 629–647.
Nikolaeva S.V., Gatovskiy Yu.A., Kulagina E.I., Zaytseva E.L. Granitsa devona i karbona: novye resheniya staroy problemy (soveshchanie mezhdunarodnoy rabochey gruppy v Monpel'e, 20-22 sentyabrya 2016 g.) [The Devonian–Carboniferous boundary: new solutions of old problem (meeting of the international working group in Montpellier, September 20-22, 2016)]. Bulletin of Moscow society of naturalists. Geological series, 2016, vol. 91, no. 6, pp. 66–74.
Palmatolepis-based revision of upper part of standart Late Devonian conodont zonation // Conodont biofacies and provincialism / Editor D.L. Clark. Geological Society of America, 1984, no. 196, pp. 179–194.
Plotitsyn A.N. Konodonty i stratigrafiya verkhnefamensko-turneyskikh otlozheniy severa Urala i gryady Chernysheva [Conodonts and stratigraphy of the Upper Famennian–Tournaisian of the North Urals and Tchernyshev Swell]. Avtoreferat dissertatsii na soiskanie uchenoy stepeni kandidata geologo-mineralogicheskikh nauk. Syktyvkar: Geoprint, 2016a, 19 p.
Plotitsyn A.N. Korrelyatsionnye urovni v verkhnem famene i turne severa Urala i gryady Chernysheva [Correlation levels in Upper Famennian-Tournaisian of the North Urals and Tchernyshev Swell]. Vestnik IG Komi SC UB RAS, 2016b, no. 7, pp. 46–53.
Plotitsyn A.N., Gruzdev D.A. Granitsa devonskoy i kamennougol'noy sistem na r. Iz"yael' (yug gryady Chernysheva) [Devonian-Carboniferous boundary in the Izyayel River section (south of the Tchernyshev Swell)]. Geologiya. geoekologiya i resursnyy potentsial Urala i sopredelnykh territoriy: Proceedings of the VI All-Russian youth conf. Ufa, 2016, pp. 102–107.
Plotitsyn A.N., Gruzdev D.A., Zhuravlev A.V. Vliyanie tafonomii na biostratigrafiyu glubokovodno-shel'fovykh otlozheniy po konodontam [Taphonomical influence on the biostratigraphy of the deep-water deposits]. Trudy XVII Vserossiyskogo mikropaleontologicheskogo soveshchaniya «Sovremennaya mikropaleontologiya – problemy i perspektivy». Moscow: PIN RAS, 2018, pp. 339–343.
Plotitsyn A.N., Sobolev D.B., Gruzdev D.A. Novye dannye o pogranichnykh otlozheniyakh devona i karbona na Pripolyarnom Urale (r. Syv"yu) [New data on the Devonian and Carboniferous boundary deposits in the Subpolar Urals (Syvyu River)]. Vestnik IG Komi SC UB RAS, 2014, no. 6, pp. 13–20.
Postanovleniya Mezhvedomstvennogo stratigraficheskogo komiteta i ego postoyannykh komissiy [Resolutions of the Interdepartmental Stratigraphic Committee and its standing committees]. St. Petersburg: Izd-vo VSEGEI, 2003, vol. 34, 48 p.
Predtechenskiy N.N. Zadachi i pravila izucheniya i opisaniya opornykh stratigraficheskikh razrezov [Tasks and rules for studying and describing key stratigraphic sections]. Leningrad, 1983, 33 p. (M-vo geologii SSSR. Vsesoyuz. ordena Lenina nauch.-issled. Geol. in-t im. A.P. Karpinskogo. Mezhved. stratigraf. kom. SSSR).
Sandberg C.A., Ziegler W., Leuteritz K., Brill S.M. Phylogeny, speciation, and zonation of Siphonodella (Conodonta, Upper Devonian and Lower Carboniferous) // Newsletters on Stratigraphy, 1978, vol. 7, no. 2, pp. 102–120.
Sedaeva K.M., Ryabinkina N.N., Kuleshov V.N., Valyaeva O.V. Otrazhenie Khangenbergskogo global'nogo geologicheskogo sobytiya rubezha devona i karbona v razrezakh zapadnogo sklona Pripolyarnogo (r. Kozhim) i Yuzhnogo (r. Sikaza) Urala [The Hangenberg global geological event on the Devon-Carbon boundary strata on the western slope of Prepolar (the Kozhim riser) and Southern (the Sikaza River) Urals]. Litosfera, 2010, no. 6, pp. 25–37. Sobolev D.B., Zhuravlev A.V., Tsyganko V.S. Stop 3. Upper Devonian-Lower Carboniferous succession on the Kozhym River // Geology of the Devonian System. Subpolar Urals Field Trip Guidebook. Syktyvkar, 2002, pp. 21–40.
Sobolev D.B., Zhuravlev A.V., Tsyganko V.S. Stop 8. Upper Devonian-Lower Carboniferous succession on the Kozhym River // Pan-Arctic Palaeozoic Tectonics, Evolution of Basins and Faunas. Subpolar Urals Field Trip Guidebook. Syktyvkar, 2000, pp. 101–111. (IGCP406 Special Publication 6).
Sostoyanie izuchennosti stratigrafii dokembriya i fanerozoya Rossii. Zadachi dal'neyshikh issledovaniy: Postanovleniya Mezhvedomstvennogo stratigraficheskogo komiteta i ego postoyannykh komissiy [The state of knowledge of Precambrian and Phanerozoic stratigraphy of Russia. Tasks for further research: Decisions of the Interdepartmental Stratigraphic Committee and its standing committees]. St. Petersburg: Izd-vo VSEGEI, 2008, vol. 38, 131 p.
Stratigraficheskie skhemy Urala (dokembriy, paleozoy) [Stratigraphic schemes of the Urals (Precambrian, Paleozoic)]. Mezhved. strat. komitet Rossii. Ekaterinburg, 1993, 151 p. of schemes.
Stratigraficheskiy kodeks Rossii. Izdanie tret'e [Stratigraphic code of Russia. Third Edition.]. St. Petersburg: Izdatelstvo VSEGEI, 2006, 96 p. (Mezhvedomstvennyy stratigraficheskiy komitet Rossii. VSEGEI).
Walliser O.H. Global events in the Devonian and Carboniferous // Global Events and Event Stratigraphy in the Phanerozoic // Editor O.H. Walliser. Berlin: Springer, 1996, pp. 225–250.
Zhuravlev A.V. Dinamika taksonomicheskogo raznoobraziya konodontov v pozdnem devone – rannem karbone (famenskiy-serpukhovskiy veka) [Dynamics of the conodont diversity in the Late Devonian–Early Carboniferous (Famennian–Serpukhovian)]. Litosfera, 2019, vol. 19, no. 1, pp. 81–91.
Zhuravlev A.V. Fatsial'no-stratigraficheskie analogi slantsev i izvestnyakov Khangenberg na Pripolyarnom Urale [Facial-stratigraphic analogs of Hangenberg shales and Hangenberg limestones in the Subpolar Urals]. Izvestiya vuzov. Geologiya i razvedka, 1990, no. 8, pp. 121–123.
Zhuravlev A.V. Pozdnedevonskoe (Khangenbergskoe) sobytie [Late Devonian Hangenberg event]. Ispol'zovanie sobytiyno-stratigraficheskikh urovney dlya mezhregional'noy korrelyatsii fanerozoya Rossii: Metod. posobie. St. Petersburg: Izd-vo VSEGEI, 2000, pp. 41–46.
Zhuravlev A.V. Sedimentatsionnaya model' oblasti sochleneniya Eletskoy i Lemvinskoy formatsionnykh zon Pripolyarnogo Urala v pogranichnom devonsko-kamennougol'nom intervale [Sedimentation model of the transitional zone from the Elets to Lemva formation belts (Devonian-Carboniferous boundary, Cis-Polar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 4, available at: http://www.ngtp.ru/rub/2/59_2012.pdf
Zhuravlev A.V. Tafonomiya konodontovykh elementov v pozdnedevonsko-rannekamennougol'nykh turbiditakh severa Urala i Pay-Khoya [Conodont element taphonomy in the Late Devonian-Early Carboniferous turbidities of the north of Urals and Pay-Khoy]. Litosfera, 2012b, no 3, pp. 14–21.
Zhuravlev A.V., Tolmacheva T.J. Ecological recovery of conodont communities after Cambrian/Ordovican and Devonian/Carboniferous events // Cour. Forsch.-Inst. Senckenberg, 1995, no. 182, pp. 313–324.
Ziegler W. Taxionomie und Phylogenie Oberdevonischer Conodonten und ihre stratigraphische Bedeutung // Abhandlunghen des Hessisches Landesamt für Bodenforschung, 1962, no. 38, pp. 1–166.
Ziegler W., Sandberg C. The Late Devonian Standard Conodont Zonation // Cour. Forsch.-Inst. Senckenberg, 1990, no. 121, 115 p.
Brenckle P.L. Late Tournaisian (Lower Carboniferous) foraminifers from the Middle Urals and their use in Russian Horizon Definition // Late Paleozoic Foraminifera; their biostratigraphy, evolution, and paleoecology; and the Mid-Carboniferous boundary; Editors C.A. Ross, J.R.P. Ross, P.L. Brenckle. Cushman Found. Foram. Res. Special Publication 36, 1997, pp. 5–9.
Chermnykh V.A. Stratigrafiya karbona severa Urala [Stratigraphy of the Carboniferous of the North of the Urals]. Leningrad, 1976, 302 p.
Chermnykh V.A., Kochetkova N.M., Pazukhin V.N., Lipina O.A. Pogranichnye devonsko-kamennougol'nye otlozheniya Severnogo i Pripolyarnogo Urala [Devonian-Carboniferous boundary deposits of the Northern and Subpolar Urals]. Granitsa devona i karbona na territorii SSSR, Minsk, 1988, pp. 145–151.
Chermnykh V.A., Kononova L.I., Pazukhin V.N., Cheusova G.N. Tri tipa razrezov otlozheniy, perekhodnykh mezhdu devonom i karbonom na severe Ural'skoy skladchatoy oblasti [Three types of sections of transitional deposits between the Devonian and Carboniferous in the North Ural folded region]. Biostratigrafiya pogranichnykh otlozheniy devona i karbona SSSR, Magadan, 1980, pp. 1–18.
Corradini C., Barca S., Spalletta C. Late Devonian-Early Carboniferous conodonts from the «Clymeniae limestones» of SE Sardinia (Italy) // Courier Forschungs-Institut Senckenberg, 2003, no.245, pp. 227–253.
Corradini C., Spaletta C., Mossoni A., Matyja H., Over D.J. Conodonts across the Devonian/Carboniferous boundary: a review and implication for the redefinition of the boundary and a proposal for an updated conodont zonation // Geological Magazine, 2016, no. 1, pp. 1–15.
Deulin Yu.V. Konodonty i korrelyatsiya produktivnykh na neft' verkhnedevonskikh otlozheniy severa Timano-Pechorskoy provintsii [Conodonts and correlation of oil-producing Upper Devonian deposits in the north of the Timan-Pechora province]. Arhangel'sk: Pravda Severa, 2006, 253 p.
Ivanov K.S. Sovremennye metodiki vydeleniya konodontov (obzor) [Modern methods for isolating conodonts (review)]. Problemy sovremennoy mikropaleontologii, Leningrad: Nauka, 1990, pp. 149–156.
Kaiser S.I. Mass Extinctions, Climatic and Oceanographic Changes at the Devonian-Carboniferous Boundary: Ph. D. Dissertation. Germany: Ruhr-University Bochum, 2005, 156 p. Kochetkova N.M., Reytlinger E.A., Pazukhin V.N., Avkhimovich V.I. Granitsa devona i karbona na Yuzhnom Urale [The Devonian-Carboniferous boundary in the Southern Urals]. Granitsa devona i karbona na territorii SSSR. Minsk: Nauka i tekhnika, 1988, pp. 157–166.
Kondratenko-Zav'yalova E.A. Verkhneturneyskie foraminifery L'vovsko-Volynskogo ugol'nogo basseyna [Upper Tournaisian Foraminifera of the Lviv-Volyn coal basin]. Paleontologicheskiy sbornik, 1974, vol. 1, no. 10, pp. 11–15.
Kulagina E.I., Stepanova T.I., Zaytseva E.L., Gorozhanina E.N., Gibshman N.B., Ivanova R.M., Vevel' Ya.A., Ponomareva G.Yu., Filimonova T.V. Atlas foraminifer i mikrofatsiy verkhnedevonskikh i nizhnekamennougol'nykh otlozheniy Severnoy Evrazii. Famenskiy i turneyskiy yarusy [Atlas of foraminifers and microfacies of the Upper Devonian and Lower Carboniferous depososits of the Northern Eurasia. Famennian and Tournaisian stages]. Moscow: PIN RAN, 2018, 220 p.
Nemirovskaya T.I., Chermnykh V.A., Kononova L.I., Pazukhin V.N. Conodonts of the Devonian-Carboniferous boundary section, Kozhim, Polar Urals, Russia // Annales de la Societe geologique de Belgique, 1992, vol. 115, pp. 629–647.
Nikolaeva S.V., Gatovskiy Yu.A., Kulagina E.I., Zaytseva E.L. Granitsa devona i karbona: novye resheniya staroy problemy (soveshchanie mezhdunarodnoy rabochey gruppy v Monpel'e, 20-22 sentyabrya 2016 g.) [The Devonian–Carboniferous boundary: new solutions of old problem (meeting of the international working group in Montpellier, September 20-22, 2016)]. Bulletin of Moscow society of naturalists. Geological series, 2016, vol. 91, no. 6, pp. 66–74.
Palmatolepis-based revision of upper part of standart Late Devonian conodont zonation // Conodont biofacies and provincialism / Editor D.L. Clark. Geological Society of America, 1984, no. 196, pp. 179–194.
Plotitsyn A.N. Konodonty i stratigrafiya verkhnefamensko-turneyskikh otlozheniy severa Urala i gryady Chernysheva [Conodonts and stratigraphy of the Upper Famennian–Tournaisian of the North Urals and Tchernyshev Swell]. Avtoreferat dissertatsii na soiskanie uchenoy stepeni kandidata geologo-mineralogicheskikh nauk. Syktyvkar: Geoprint, 2016a, 19 p.
Plotitsyn A.N. Korrelyatsionnye urovni v verkhnem famene i turne severa Urala i gryady Chernysheva [Correlation levels in Upper Famennian-Tournaisian of the North Urals and Tchernyshev Swell]. Vestnik IG Komi SC UB RAS, 2016b, no. 7, pp. 46–53.
Plotitsyn A.N., Gruzdev D.A. Granitsa devonskoy i kamennougol'noy sistem na r. Iz"yael' (yug gryady Chernysheva) [Devonian-Carboniferous boundary in the Izyayel River section (south of the Tchernyshev Swell)]. Geologiya. geoekologiya i resursnyy potentsial Urala i sopredelnykh territoriy: Proceedings of the VI All-Russian youth conf. Ufa, 2016, pp. 102–107.
Plotitsyn A.N., Gruzdev D.A., Zhuravlev A.V. Vliyanie tafonomii na biostratigrafiyu glubokovodno-shel'fovykh otlozheniy po konodontam [Taphonomical influence on the biostratigraphy of the deep-water deposits]. Trudy XVII Vserossiyskogo mikropaleontologicheskogo soveshchaniya «Sovremennaya mikropaleontologiya – problemy i perspektivy». Moscow: PIN RAS, 2018, pp. 339–343.
Plotitsyn A.N., Sobolev D.B., Gruzdev D.A. Novye dannye o pogranichnykh otlozheniyakh devona i karbona na Pripolyarnom Urale (r. Syv"yu) [New data on the Devonian and Carboniferous boundary deposits in the Subpolar Urals (Syvyu River)]. Vestnik IG Komi SC UB RAS, 2014, no. 6, pp. 13–20.
Postanovleniya Mezhvedomstvennogo stratigraficheskogo komiteta i ego postoyannykh komissiy [Resolutions of the Interdepartmental Stratigraphic Committee and its standing committees]. St. Petersburg: Izd-vo VSEGEI, 2003, vol. 34, 48 p.
Predtechenskiy N.N. Zadachi i pravila izucheniya i opisaniya opornykh stratigraficheskikh razrezov [Tasks and rules for studying and describing key stratigraphic sections]. Leningrad, 1983, 33 p. (M-vo geologii SSSR. Vsesoyuz. ordena Lenina nauch.-issled. Geol. in-t im. A.P. Karpinskogo. Mezhved. stratigraf. kom. SSSR).
Sandberg C.A., Ziegler W., Leuteritz K., Brill S.M. Phylogeny, speciation, and zonation of Siphonodella (Conodonta, Upper Devonian and Lower Carboniferous) // Newsletters on Stratigraphy, 1978, vol. 7, no. 2, pp. 102–120.
Sedaeva K.M., Ryabinkina N.N., Kuleshov V.N., Valyaeva O.V. Otrazhenie Khangenbergskogo global'nogo geologicheskogo sobytiya rubezha devona i karbona v razrezakh zapadnogo sklona Pripolyarnogo (r. Kozhim) i Yuzhnogo (r. Sikaza) Urala [The Hangenberg global geological event on the Devon-Carbon boundary strata on the western slope of Prepolar (the Kozhim riser) and Southern (the Sikaza River) Urals]. Litosfera, 2010, no. 6, pp. 25–37. Sobolev D.B., Zhuravlev A.V., Tsyganko V.S. Stop 3. Upper Devonian-Lower Carboniferous succession on the Kozhym River // Geology of the Devonian System. Subpolar Urals Field Trip Guidebook. Syktyvkar, 2002, pp. 21–40.
Sobolev D.B., Zhuravlev A.V., Tsyganko V.S. Stop 8. Upper Devonian-Lower Carboniferous succession on the Kozhym River // Pan-Arctic Palaeozoic Tectonics, Evolution of Basins and Faunas. Subpolar Urals Field Trip Guidebook. Syktyvkar, 2000, pp. 101–111. (IGCP406 Special Publication 6).
Sostoyanie izuchennosti stratigrafii dokembriya i fanerozoya Rossii. Zadachi dal'neyshikh issledovaniy: Postanovleniya Mezhvedomstvennogo stratigraficheskogo komiteta i ego postoyannykh komissiy [The state of knowledge of Precambrian and Phanerozoic stratigraphy of Russia. Tasks for further research: Decisions of the Interdepartmental Stratigraphic Committee and its standing committees]. St. Petersburg: Izd-vo VSEGEI, 2008, vol. 38, 131 p.
Stratigraficheskie skhemy Urala (dokembriy, paleozoy) [Stratigraphic schemes of the Urals (Precambrian, Paleozoic)]. Mezhved. strat. komitet Rossii. Ekaterinburg, 1993, 151 p. of schemes.
Stratigraficheskiy kodeks Rossii. Izdanie tret'e [Stratigraphic code of Russia. Third Edition.]. St. Petersburg: Izdatelstvo VSEGEI, 2006, 96 p. (Mezhvedomstvennyy stratigraficheskiy komitet Rossii. VSEGEI).
Walliser O.H. Global events in the Devonian and Carboniferous // Global Events and Event Stratigraphy in the Phanerozoic // Editor O.H. Walliser. Berlin: Springer, 1996, pp. 225–250.
Zhuravlev A.V. Dinamika taksonomicheskogo raznoobraziya konodontov v pozdnem devone – rannem karbone (famenskiy-serpukhovskiy veka) [Dynamics of the conodont diversity in the Late Devonian–Early Carboniferous (Famennian–Serpukhovian)]. Litosfera, 2019, vol. 19, no. 1, pp. 81–91.
Zhuravlev A.V. Fatsial'no-stratigraficheskie analogi slantsev i izvestnyakov Khangenberg na Pripolyarnom Urale [Facial-stratigraphic analogs of Hangenberg shales and Hangenberg limestones in the Subpolar Urals]. Izvestiya vuzov. Geologiya i razvedka, 1990, no. 8, pp. 121–123.
Zhuravlev A.V. Pozdnedevonskoe (Khangenbergskoe) sobytie [Late Devonian Hangenberg event]. Ispol'zovanie sobytiyno-stratigraficheskikh urovney dlya mezhregional'noy korrelyatsii fanerozoya Rossii: Metod. posobie. St. Petersburg: Izd-vo VSEGEI, 2000, pp. 41–46.
Zhuravlev A.V. Sedimentatsionnaya model' oblasti sochleneniya Eletskoy i Lemvinskoy formatsionnykh zon Pripolyarnogo Urala v pogranichnom devonsko-kamennougol'nom intervale [Sedimentation model of the transitional zone from the Elets to Lemva formation belts (Devonian-Carboniferous boundary, Cis-Polar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 4, available at: http://www.ngtp.ru/rub/2/59_2012.pdf
Zhuravlev A.V. Tafonomiya konodontovykh elementov v pozdnedevonsko-rannekamennougol'nykh turbiditakh severa Urala i Pay-Khoya [Conodont element taphonomy in the Late Devonian-Early Carboniferous turbidities of the north of Urals and Pay-Khoy]. Litosfera, 2012b, no 3, pp. 14–21.
Zhuravlev A.V., Tolmacheva T.J. Ecological recovery of conodont communities after Cambrian/Ordovican and Devonian/Carboniferous events // Cour. Forsch.-Inst. Senckenberg, 1995, no. 182, pp. 313–324.
Ziegler W. Taxionomie und Phylogenie Oberdevonischer Conodonten und ihre stratigraphische Bedeutung // Abhandlunghen des Hessisches Landesamt für Bodenforschung, 1962, no. 38, pp. 1–166.
Ziegler W., Sandberg C. The Late Devonian Standard Conodont Zonation // Cour. Forsch.-Inst. Senckenberg, 1990, no. 121, 115 p.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 35_2018 | submitted on 07/11/2018 displayed on website on 10/17/2018 |
| 17 p. | Vevel Ya.A., Zhuravlev A.V., Gruzdev D.A. |
| Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals) | |
| Results of study of the Visean-Serpukhovian boundary beds of the Kozhym River basin (Nizhniy Nortnichayol’ Creek) are considered. Biostratigraphy based on conodonts, foraminifers, and algae is described. The early Serpukhovian transgression led to sequential environment changes from quite-water shallow inner shoal to active-water shoal border. Correlation of the study section with sequences of the Kosyu-Rogovaya Depression allows elaborating facial model of the Lower Serpukhovian. Keywords: Subpolar Urals, Serpukhovian, conodonts, foraminifers, algae, environments. |
|
| article citation | Vevel Ya.A., Zhuravlev A.V., Gruzdev D.A. Nizhniy serpukhov (nizhniy karbon) v basseyne r. Kozhim (Pripolyarnyy Ural) [Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 4, available at: http://www.ngtp.ru/rub/2018/35_2018.html |
| DOI | https://doi.org/10.17353/2070-5379/35_2018 |
References
Gerasimova A.I., Gruzdev D.A., Zhuravlev A.V. Modeli razvitiya otmeley kraya shel'fa na severe Paleoural'skogo basseyna v srednem paleozoe [Models of development of the shoals ofthe shelf margin in the North of Palaeo-Uralian basin in the Middle Palaeozoic]. Materialy V Mezhdunarodnoy konferentsii molodykh uchenykh i spetsialistov pamyati akademika A.P. Karpinskogo (St. Petersburg, 28 Feb – 3 Mar 2017). SPb.: Izd-vo VSEGEI, 2017, p. 35-37. 1-CD-R (DVD-ROM).
Gruzdev D.A. Pozdnedevonsko-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [The Late Devonian-Early Carboniferous isolated carbonate platform in the Subpolar Urals (Bol'shaya Nadota River)] Vestnik Instituta geologii. - 2017, no. 4, pp.16-23.
Ivanova R.M. Izvestkovye vodorosli karbona Urala [Calcareous algae carbon Urals]. Ekaterinburg: RIO UrORAN, 2013, 244 p.
Ivanova R.M. Nekotorye izvestkovye vodorosli karbona Urala [Some calcareous algae carbon Urals]. Paleontologicheskii zhurnal, 1999, no. 6, pp. 76-79.
Kulagina E.I., Gibshman N.B. Obshchaya zonal'naya shkala nizhnego karbona Rossii po foraminiferam [General foraminiferal zonation of Lower Carboniferous in Russia]. Byul. MOIP. Otd. geol, 2005, issue 80, vol. 2. pp. 33–59.
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian sediments (Lower Carboniferous) from the south of Chernyshev uplift and Kosyu-Rogovsky depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/27_2016
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny // Neftegazovaya geologiya. Teoriya i praktika. - 2016. - T.11. - №3. - http://www.ngtp.ru/rub/2/27_2016.pdf. DOI: 10.17353/2070-5379/27_2016
Ponomareva G.Yu. Sostoyanie i problemy foraminiferovoy shkaly verkhnevizeyskikh i serpukhovskikh otlozheniy Zapadnogo Urala [The state and the problems of the foraminiferal scale for the upper Visean and Serpukhovian in the western Urals]. Materialy mezhdunarodnogo polevogo soveshchaniya (Ufa–Sibay, 13-18 Aug 2009). Ufa: DizaynPoligrafServis, 2009, p. 220–224.
Richards B.C., Aretz M., Barnett A., Barskov I., Blanco-Ferrera S., Brenckle P.L., Clayton G., Dean M., Ellwood B., Gibshman N., Hecker M., Konovalova V.A., Korn D., Kulagina E., Lane R., Mamet B., Nemyrovska T., Nikolaeva S.V., Pazukhin V., Qi Y.-P., Sanz-López J., Saltzman M.R., Titus A., Utting J. & Wang X. Report of the Task Group to establish a GSSP close to the existing Visean-Serpukhovian boundary. Newsletter on Carboniferous Stratigraphy, 2011, 29, p. 26–30.
Skompski S., Alekseev A., Meischner D., Nemirovskaya T., Perret M.-F. & Varker W.J. Conodont distribution across the Viséan/Namurian boundary. Courier Forschungsinstitut Senckenberg 188, 1995, p. 177-209.
Skompski S., Paszkowski M., Krobicki M., Kokovin K., Korn D., Tomas A. & Wrzolek T. Depositional setting of the Devonian/Carboniferous biohermal Bol'shaya Nadota Carbonate Complex, Subpolar Urals. Acta Geologica Polonica, 2001, vol. 51, no. 3, p. 217-235.
Sobolev D.B., Zhuravlev A.V., Popov V.V., Vevel' Ya.A. Depressionnyy tip razreza verkhnego vize–serpukhova na Pripolyarnom Urale [The depression type of the Upper Visean-Serpukhovian succession in the Subpolar Urals]. Litosfera, 2015, no. 4, pp. 62-72.
Vevel' Ya.A., Gruzdev D.A., Zhuravlev A.V. Foraminifery i konodonty melkovodnykh otlozheniy ranneserpukhovskogo vozrasta v razreze na r. Kamenka (yug Pechoro-Kozhvinskogo megavala) [Foraminifers and conodonts from the early Serpukhovian shallow-water deposits of the Kamenka river section (south of the Pechora-Kozhva swell)]. Syktyvkarskiy paleontologicheskiy sbornik (Trudy Instituta geologii Komi nauchnogo tsentra UrO RAN), 2017, vol. 130, no 8, p. 14-23.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St-Petersburg: VSEGEI, 2003, 85 p.
Gruzdev D.A. Pozdnedevonsko-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [The Late Devonian-Early Carboniferous isolated carbonate platform in the Subpolar Urals (Bol'shaya Nadota River)] Vestnik Instituta geologii. - 2017, no. 4, pp.16-23.
Ivanova R.M. Izvestkovye vodorosli karbona Urala [Calcareous algae carbon Urals]. Ekaterinburg: RIO UrORAN, 2013, 244 p.
Ivanova R.M. Nekotorye izvestkovye vodorosli karbona Urala [Some calcareous algae carbon Urals]. Paleontologicheskii zhurnal, 1999, no. 6, pp. 76-79.
Kulagina E.I., Gibshman N.B. Obshchaya zonal'naya shkala nizhnego karbona Rossii po foraminiferam [General foraminiferal zonation of Lower Carboniferous in Russia]. Byul. MOIP. Otd. geol, 2005, issue 80, vol. 2. pp. 33–59.
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian sediments (Lower Carboniferous) from the south of Chernyshev uplift and Kosyu-Rogovsky depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/27_2016
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny // Neftegazovaya geologiya. Teoriya i praktika. - 2016. - T.11. - №3. - http://www.ngtp.ru/rub/2/27_2016.pdf. DOI: 10.17353/2070-5379/27_2016
Ponomareva G.Yu. Sostoyanie i problemy foraminiferovoy shkaly verkhnevizeyskikh i serpukhovskikh otlozheniy Zapadnogo Urala [The state and the problems of the foraminiferal scale for the upper Visean and Serpukhovian in the western Urals]. Materialy mezhdunarodnogo polevogo soveshchaniya (Ufa–Sibay, 13-18 Aug 2009). Ufa: DizaynPoligrafServis, 2009, p. 220–224.
Richards B.C., Aretz M., Barnett A., Barskov I., Blanco-Ferrera S., Brenckle P.L., Clayton G., Dean M., Ellwood B., Gibshman N., Hecker M., Konovalova V.A., Korn D., Kulagina E., Lane R., Mamet B., Nemyrovska T., Nikolaeva S.V., Pazukhin V., Qi Y.-P., Sanz-López J., Saltzman M.R., Titus A., Utting J. & Wang X. Report of the Task Group to establish a GSSP close to the existing Visean-Serpukhovian boundary. Newsletter on Carboniferous Stratigraphy, 2011, 29, p. 26–30.
Skompski S., Alekseev A., Meischner D., Nemirovskaya T., Perret M.-F. & Varker W.J. Conodont distribution across the Viséan/Namurian boundary. Courier Forschungsinstitut Senckenberg 188, 1995, p. 177-209.
Skompski S., Paszkowski M., Krobicki M., Kokovin K., Korn D., Tomas A. & Wrzolek T. Depositional setting of the Devonian/Carboniferous biohermal Bol'shaya Nadota Carbonate Complex, Subpolar Urals. Acta Geologica Polonica, 2001, vol. 51, no. 3, p. 217-235.
Sobolev D.B., Zhuravlev A.V., Popov V.V., Vevel' Ya.A. Depressionnyy tip razreza verkhnego vize–serpukhova na Pripolyarnom Urale [The depression type of the Upper Visean-Serpukhovian succession in the Subpolar Urals]. Litosfera, 2015, no. 4, pp. 62-72.
Vevel' Ya.A., Gruzdev D.A., Zhuravlev A.V. Foraminifery i konodonty melkovodnykh otlozheniy ranneserpukhovskogo vozrasta v razreze na r. Kamenka (yug Pechoro-Kozhvinskogo megavala) [Foraminifers and conodonts from the early Serpukhovian shallow-water deposits of the Kamenka river section (south of the Pechora-Kozhva swell)]. Syktyvkarskiy paleontologicheskiy sbornik (Trudy Instituta geologii Komi nauchnogo tsentra UrO RAN), 2017, vol. 130, no 8, p. 14-23.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St-Petersburg: VSEGEI, 2003, 85 p.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 32_2018 | submitted on 06/29/2018 displayed on website on 08/28/2018 |
| 34 p. | Plotitsyn A.N., Ponomarenko E.S., Vevel Ya.A. |
| Tournaisian deep-water deposits of the Usa River basin (Polar Urals) | |
| The article presents new data of detailed lithological and paleontological study, and results of stratigraphical investigations of the Tournaisian deep-water deposits of the Malaya Usa River section (Polar Urals). The section is biostratigraphically characterized by conodonts, foraminifers, fishes, and corals. The traces of the Mid-Tournaisian (Lower Alum Shale) Global Event are distinguished. The lithological marker (transgressive clayey beds), biostratigraphical data (FAD of Siphonodella crenulata conodonts), and isotope anomaly (negative shift of б13С) allowed to confidently recognize the Event. The new data fill the gap in the stratigraphical characteristics of the deposits of the base of the Carboniferous System of the Polar Urals and are important for detailing correlation of the tectonically complex sections within the Vorkuta oil and gas bearing complex of the eastern part of the Timan-Pechora Basin. In addition, there are quite rare taxa in the complex of conodonts, which justify the additional paleontological interest to the present work. Keywords: biostratigraphy, event stratigraphy, conodonts, foraminifers, Tournaisian, Polar Urals. |
|
| article citation | Plotitsyn A.N., Ponomarenko E.S., Vevel Ya.A. Turneyskie glubokovodnye otlozheniya basseyna r. Usa (Polyarnyy Ural) [Tournaisian deep-water deposits of the Usa River basin (Polar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 3, available at: http://www.ngtp.ru/rub/2/32_2018.pdf |
| DOI | https://doi.org/10.17353/2070-5379/32_2018 |
References
Becker R.T. Anoxia, eustatic changes, and Upper Devonian to lowermost Carboniferous global ammonoid diversity. The Ammonoidea: Environment, Ecology and Evolutionary Change. Oxford: Systematic Association, 1993а, p. 115 163.
Becker R.T. Analysis of ammonoid palaeobiogeography in relation to the global Hangenberg (terminal Devonian) and Lower Alum Shale (Middle Tournaisian) events. Ann. Soc. Geol. Belg, 1993б, no. 115, p. 459–473.
Becker R.T. New faunal records and holostratigraphic correlation of the Hasselbachtal D/C-boundary auxiliary stratotype (Germany). Ann. Soc. Geol. Belg, 1996, no. 117, p. 19–45.
Chernov G.A. Devonskiye otlozheniya vostochnoy chasti Bolshezemelskoy tundry [Devonian of the Bolshezemelskaya tundra eastern part]. Moscow-Leningrad: AN SSSR, 1962, 118 p.
Chernov G.A. Paleozoy Bolshezemelskoy tundry i perspektivy ego neftegazonosnosti [Paleozoic of the Bolshezemelskaya tundra and prospects of its oil and gas potential]. Moscow: Nauka, 1972, 315 p.
Chizhova V.A. Razvitiye ostrakod v famene i turne i granitsa devona-karbona [Ostracods evolution in the Famennian and Tournaisian, and the Devonian-Carboniferous boundary]. Granitsa devona i karbona na territorii SSSR. Minsk: Nauka i tekhnika, 1988, p. 271 286.
Chizhova V.A., Stashkova E.K., Zvereva E.V., Stukova T.V., Akulova N.N. Sootnosheniye verkhnefransko-nizhnevizeyskikh biostratigraficheskikh podrazdeleniy po konodontam. foraminiferam. ostrakodam i sporam v razrezakh vostoka Russkoy platformy [The ratio of the Upper Frasnian – Lower Viasean conodont, foraminiferal, ostracodes and spores biostratigraphic subdivisions in the sections of the Eastern part of the Russian platform]. Biostratigrafiya i mikroorganizmy fanerozoya Evrazii: proceedings of the XII All-Russian micropaleontological conference. Moscow: GEOS, 1997, p. 61 70.
Draganits E., Mawson R., Talent J.A., Krystyn L. Lithostratigraphy, conodont biostratigraphy and depositional environment of the Middle Devonian (Givetian) to Early Carboniferous (Tournaisian) Lipak Formation in the Pin Valley of Spiti (NW India). Rivista Italiana di Paleontologia e Stratigrafia, 2002, no. 108, p. 7–35.
Durkina A.V. O zonalnom raschlenenii pogranichnykh otlozheniy nizhne-verkhneturneyskogo podyarusov po foraminiferam i o granitse mezhdu nimi v Timano-Pechorskoy provintsii [About zonal subdivision of the lower-upper Tournaisian boundary sections using foraminifers and the boundary between Tournasian substages in the Timan-Pechora province]. Biostratigrafiya neftegazonosnykh basseynov: proceedings of the First International Symposium. St. Petersburg: VNIGRI, 1997, p. 70 75.
Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii [State Geological Map of the Russian Federation]. Scale 1:200000 (second edition). Series Polar Ural – Sheet Q-41-XI (Eletskiy). Explanatory letter. Saint-Petersburg MF VSEGEI, 2004, 216 p.
Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii [State Geological Map of the Russian Federation]. Scale 1:200000 (second edition). Series Polar Ural – Sheet Q-41-V, VI (Vorkuta). Explanatory letter. St. Petersburg: MF VSEGEI, 2005, 262 p.
Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii [State Geological Map of the Russian Federation]. Scale 1:1000000 (third edition). Series Ural – Sheet Q-41 (Vorkuta). Explanatory letter. St. Petersburg: KF VSEGEI, 2007, 541 p.
Gosudarstvennaya geologicheskaya karta SSSR [State Geological Map of the USSR]. Scale 1:200000. Series North Ural – Sheet Q-41-VI. Explanatory letter. Moskow, 1981, 120 p.
Habibi T., Corradini C., Yazdi M. Conodont biostratigraphy of the Upper Devonian–Lower Carboniferous Shahmirzad section, central Alborz, Iran. Geobios, 2008, no. 41, p. 763–777.
Ivanov K.S. Sovremennyye metodiki vydeleniya konodontov (obzor) [Modern methods of isolating conodonts (review)]. Problemy sovremennoy mikropaleontologii. Leningrad: Nauka, 1990, p. 149 156.
Kaiser S.I., Becker R.T. The required revision of the Devonian-Carboniferous boundary. Journal of Stratigraphy, 2007, v. 31, supplement 1, p. 95.
Kaiser S.I., Corradini C. Should the Devonian-Carboniferous boundary be redefined? Subcomission on Devonian Stratigraphy. Newsletter, 2008, no. 23, p. 55 56.
Kalvoda J. Sedimentological and evolutionary cycles in the Upper Devonian and Lower Carboniferous / Acta Universitatis Carolinae. Geologica, 1989, v. 1, no. 1, p. 29 45.
Kolesnik L.S. Verkhniy devon i nizhniy karbon verkhovyev r. Kary (zapadnyy sklon Polyarnogo Urala) [Upper Devonian – Lower Carboniferous of the Kara river upstream (Western slope of the Polar Urals)]. Byul. MOIP. Otd. geol, 1993, vol. 68, no. 1, p. 15 20.
Kulagina E.I., Gibshman N.B. Obshchaya zonalnaya shkala nizhnego karbona Rossii po foraminiferam [Foraminiferal zonal standard of the Lower Carboniferous of the Russia]. Byull. MOIP. Otd. geol , 2005, vol. 80, no. 2, p. 33–59.
Mizens G.A., Kuleshov V.N., Stepanova T.I., Kucheva N.A. Otrazheniye globalnykh geologicheskikh sobytiy famenskogo i turneyskogo vekov v razreze izolirovannoy karbonatnoy platformy na vostoke Urala [Evidence for Global Famennian and Tournaisian geologic events in the section of an isolated carbonate platform in the Eastern Urals]. Russian geology and geophysics, 2015, vol. 56, no. 11, p. 1945 1960.
Prishchepa O.M., Bogatskiy V.I., Makarevich V.N., Chumakova O.V., Nikonov N.I., Kuranov A.V., Bogdanov M.M. Novyye predstavleniya o tektonicheskom i neftegazogeologicheskom rayonirovanii Timano-Pechorskoy neftegazonosnoy provintsii [The Timan-Pechora oil-bearing province – new tectonical insight]. Neftegazovaya geologiya. Teoriya i praktika, 2011, vol. 6, no. 4, http://www.ngtp.ru/rub/4/40_2011.pdf
Prishchepa O.M., Orlova L.A., Chumakova O.V. Napravleniya geologorazvedochnykh rabot na neft i gaz v severo-vostochnoy chasti Timano-Pechorskoy neftegazonosnoy provintsii [Directions of exploration for oil and gas in the North-Eastern part of the Timan-Pechora petroleum province]. Neftegazovaya geologiya. Teoriya i praktika, 2008, v. 3, no. 3, http://www.ngtp.ru/rub/4/40_2008.pdf
Plotitsyn A.N. Nizhneturneyskiye konodonty r. Malaya Usa (Polyarnyy Ural) [Lower Tournaisian conodonts of the Small Usa River section (Polar Urals)]. Struktura. veshchestvo. istoriya litosfery Timano-Severouralskogo segmenta: materials of the 23-rd youth scientific conference. Syktyvkar: Geoprint, 2014, p. 105 109.
Plotitsyn A.N. Korrelyatsionnyye urovni v verkhnem famene i turne severa Urala i gryady Chernysheva [Correlation levels in Upper Famennian – Tournaisian deposits of the North of Urals and Chernishev Swell]. Vestnik IG Komi SC UB RAS, 2016, no. 7, p. 46 53.
Plotitsyn A.N., Beznosov P.A. Conodont and vertebrate assemblages from the Early Carboniferous section of Malaya Usa River (Polar Urals, Russia). Abstracts of the XVIII International Congress on the Carboniferous and Permian. Kazan, 2015, p. 146.
Plotitsyn A.N., Zhuravlev A.V. Novyye vidy konodontov rodov Neopolygnathus i Polygnathus iz turneyskikh otlozheniy severa Urala i gryady Chernysheva [The new species of Neopolygnathus and Polygnathus from the Tournaisian of the North Urals and Chernyshev Ridge]. Syktyvkar palaeontological miscellany № 8, Syktyvkar, 2017, p. 24 30 (Proceedings of Institute of Geology of Komi Science Centre UB RAS, v. 130).
Plotitsyn A.N., Zhuravlev A.V. A new species of the conodont genus Polygnathus from the Tournaisian of the Northern Urals, Chernyshev Ridge and Pai-Khoi. Paleontological Journal, 2017, v. 51, no. 3, p. 304 307.
Plotitsyn A.N.. Zhuravlev A.V.. Vevel Ya.A.. Gruzdev D.A. Sredneturneyskoye sobytiye na severe Urala i v Priuralye [Mid-Tournaisian event on the North of the Urals and Cis-Urals]. Fundamentalnaya i prikladnaya paleontologiya: materials of the LXIV session of the Paleontological society. St. Petersburg, 2018, p. 89 90.
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in ?13С: an example from the lower Mississippian. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, v. 213, p. 359–377.
Sandberg C.A., Morrow J.R., Ziegler W. Late Devonian sea-level changes, catastrophic events, and mass extinctions. Geological Society of America, 2002, Special Paper 356, p. 473–487.
Sandberg C.A., Ziegler W., Leuteritz K., Brill S.M. Phylogeny, speciation, and zonation of Siphonodella (Conodonta, Upper Devonian and Lower Carboniferous). Newsletters on Stratigraphy, 1978, vol. 7, no. 2, p. 102–120.
Stevens C.H., Klingman D.S., Sandberg C.A., Stone P., Belasky P., Poole F.G., Snow K. Mississippian stratigraphic framework of east-central California and southern Nevada with revision of Upper Devonian and Mississippian stratigraphic units in Inyo County, California: U.S. Geological Survey, 1996, bull. 1988–J, p. 1–39.
Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracodes and biostratigraphy of the Tournaisian of the North of the Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
Sobolev D.B. Evolyutsiya i bioraznoobraziye rannekamennougolnykh ostrakod na sobytiynykh urovnyakh [Evolution and biodiversity of Early Carboniferous ostracods at the several event levels]. Biogeologiya. evolyutsiya organizmov i bioraznoobraziya v geologicheskoy istorii Timano-Severouralskogo regiona, modelirovaniye paleoekosistem. paleontologicheskiye i stratigraficheskiye geokorrelyatsii. Syktyvkar: Geoprint, 2011, p. 102 108.
Timonin N.I. Pechorskaya plita: istoriya geologicheskogo razvitiya v fanerozoye [Pechora plate: the history of geological development in the Phanerozoic.]. Ekaterinburg: UrO RAN, 1998, 239 p.
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang B., Wang X. The TICE event: Perturbation of carbon–nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse–icehouse transition. Chemical Geology, 2015, v. 401, p. 1 14.
Zhuravlev A.V. The Mid-Tournaisian Event in the Northern Urals and conodont dynamics. Proceedings of Geologists Association, 1998, no. 109, p. 161 168.
Zhuravlev A.V. Sredneturneyskoye sobytiye [Mid-Tournaisian event]. Ispolzovaniye sobytiyno-stratigraficheskikh urovney dlya mezhregionalnoy korrelyatsii fanerozoya Rossii: toolkit. St. Petersburg: VSEGEI, 2000, p. 46 48.
Zhuravlev A.V., Vevel Ya.A., Iosifidi A.G., Tomsha V.A. Razrez verkhnego devona – nizhnego karbona na myse Kostyanom ostrova Vaygach [Upper Devonian – Lower Carboniferous of the Kostyanoy cape of the Vaygach island]. Neftegazovaya geologiya. Teoriya i praktika, 2011, vol. 6, no 1, available at: http://www.ngtp.ru/rub/2/6_2011.pdf.
Zhuravlev A.V., Plotitsyn A.N. Stratotip vazhkhanoveyskoy svity v kanone reki Bolshaya Usa kak geologicheskiy pamyatnik prirody regionalnogo znacheniya [Stratotype of the Vashkhan Formation in the canyon of the Big Usa river as a geological natural monument of the regional significance]. Prirodnoye geologicheskoye naslediye Evropeyskogo Severa Rossii: materials of the All-Russian Scientific Conference. Syktyvkar: IG Komi SC UB RAS, 2017, p. 41 43.
Zhuravlev A.V., Plotitsyn A.N. The symmetry of the rostrum as a key to taxonomy of advanced Siphonodella (Conodonta, Early Carboniferous). Stratigraphy, 2017, vol. 14, no. 1 4, p.457 474.
Becker R.T. Analysis of ammonoid palaeobiogeography in relation to the global Hangenberg (terminal Devonian) and Lower Alum Shale (Middle Tournaisian) events. Ann. Soc. Geol. Belg, 1993б, no. 115, p. 459–473.
Becker R.T. New faunal records and holostratigraphic correlation of the Hasselbachtal D/C-boundary auxiliary stratotype (Germany). Ann. Soc. Geol. Belg, 1996, no. 117, p. 19–45.
Chernov G.A. Devonskiye otlozheniya vostochnoy chasti Bolshezemelskoy tundry [Devonian of the Bolshezemelskaya tundra eastern part]. Moscow-Leningrad: AN SSSR, 1962, 118 p.
Chernov G.A. Paleozoy Bolshezemelskoy tundry i perspektivy ego neftegazonosnosti [Paleozoic of the Bolshezemelskaya tundra and prospects of its oil and gas potential]. Moscow: Nauka, 1972, 315 p.
Chizhova V.A. Razvitiye ostrakod v famene i turne i granitsa devona-karbona [Ostracods evolution in the Famennian and Tournaisian, and the Devonian-Carboniferous boundary]. Granitsa devona i karbona na territorii SSSR. Minsk: Nauka i tekhnika, 1988, p. 271 286.
Chizhova V.A., Stashkova E.K., Zvereva E.V., Stukova T.V., Akulova N.N. Sootnosheniye verkhnefransko-nizhnevizeyskikh biostratigraficheskikh podrazdeleniy po konodontam. foraminiferam. ostrakodam i sporam v razrezakh vostoka Russkoy platformy [The ratio of the Upper Frasnian – Lower Viasean conodont, foraminiferal, ostracodes and spores biostratigraphic subdivisions in the sections of the Eastern part of the Russian platform]. Biostratigrafiya i mikroorganizmy fanerozoya Evrazii: proceedings of the XII All-Russian micropaleontological conference. Moscow: GEOS, 1997, p. 61 70.
Draganits E., Mawson R., Talent J.A., Krystyn L. Lithostratigraphy, conodont biostratigraphy and depositional environment of the Middle Devonian (Givetian) to Early Carboniferous (Tournaisian) Lipak Formation in the Pin Valley of Spiti (NW India). Rivista Italiana di Paleontologia e Stratigrafia, 2002, no. 108, p. 7–35.
Durkina A.V. O zonalnom raschlenenii pogranichnykh otlozheniy nizhne-verkhneturneyskogo podyarusov po foraminiferam i o granitse mezhdu nimi v Timano-Pechorskoy provintsii [About zonal subdivision of the lower-upper Tournaisian boundary sections using foraminifers and the boundary between Tournasian substages in the Timan-Pechora province]. Biostratigrafiya neftegazonosnykh basseynov: proceedings of the First International Symposium. St. Petersburg: VNIGRI, 1997, p. 70 75.
Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii [State Geological Map of the Russian Federation]. Scale 1:200000 (second edition). Series Polar Ural – Sheet Q-41-XI (Eletskiy). Explanatory letter. Saint-Petersburg MF VSEGEI, 2004, 216 p.
Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii [State Geological Map of the Russian Federation]. Scale 1:200000 (second edition). Series Polar Ural – Sheet Q-41-V, VI (Vorkuta). Explanatory letter. St. Petersburg: MF VSEGEI, 2005, 262 p.
Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii [State Geological Map of the Russian Federation]. Scale 1:1000000 (third edition). Series Ural – Sheet Q-41 (Vorkuta). Explanatory letter. St. Petersburg: KF VSEGEI, 2007, 541 p.
Gosudarstvennaya geologicheskaya karta SSSR [State Geological Map of the USSR]. Scale 1:200000. Series North Ural – Sheet Q-41-VI. Explanatory letter. Moskow, 1981, 120 p.
Habibi T., Corradini C., Yazdi M. Conodont biostratigraphy of the Upper Devonian–Lower Carboniferous Shahmirzad section, central Alborz, Iran. Geobios, 2008, no. 41, p. 763–777.
Ivanov K.S. Sovremennyye metodiki vydeleniya konodontov (obzor) [Modern methods of isolating conodonts (review)]. Problemy sovremennoy mikropaleontologii. Leningrad: Nauka, 1990, p. 149 156.
Kaiser S.I., Becker R.T. The required revision of the Devonian-Carboniferous boundary. Journal of Stratigraphy, 2007, v. 31, supplement 1, p. 95.
Kaiser S.I., Corradini C. Should the Devonian-Carboniferous boundary be redefined? Subcomission on Devonian Stratigraphy. Newsletter, 2008, no. 23, p. 55 56.
Kalvoda J. Sedimentological and evolutionary cycles in the Upper Devonian and Lower Carboniferous / Acta Universitatis Carolinae. Geologica, 1989, v. 1, no. 1, p. 29 45.
Kolesnik L.S. Verkhniy devon i nizhniy karbon verkhovyev r. Kary (zapadnyy sklon Polyarnogo Urala) [Upper Devonian – Lower Carboniferous of the Kara river upstream (Western slope of the Polar Urals)]. Byul. MOIP. Otd. geol, 1993, vol. 68, no. 1, p. 15 20.
Kulagina E.I., Gibshman N.B. Obshchaya zonalnaya shkala nizhnego karbona Rossii po foraminiferam [Foraminiferal zonal standard of the Lower Carboniferous of the Russia]. Byull. MOIP. Otd. geol , 2005, vol. 80, no. 2, p. 33–59.
Mizens G.A., Kuleshov V.N., Stepanova T.I., Kucheva N.A. Otrazheniye globalnykh geologicheskikh sobytiy famenskogo i turneyskogo vekov v razreze izolirovannoy karbonatnoy platformy na vostoke Urala [Evidence for Global Famennian and Tournaisian geologic events in the section of an isolated carbonate platform in the Eastern Urals]. Russian geology and geophysics, 2015, vol. 56, no. 11, p. 1945 1960.
Prishchepa O.M., Bogatskiy V.I., Makarevich V.N., Chumakova O.V., Nikonov N.I., Kuranov A.V., Bogdanov M.M. Novyye predstavleniya o tektonicheskom i neftegazogeologicheskom rayonirovanii Timano-Pechorskoy neftegazonosnoy provintsii [The Timan-Pechora oil-bearing province – new tectonical insight]. Neftegazovaya geologiya. Teoriya i praktika, 2011, vol. 6, no. 4, http://www.ngtp.ru/rub/4/40_2011.pdf
Prishchepa O.M., Orlova L.A., Chumakova O.V. Napravleniya geologorazvedochnykh rabot na neft i gaz v severo-vostochnoy chasti Timano-Pechorskoy neftegazonosnoy provintsii [Directions of exploration for oil and gas in the North-Eastern part of the Timan-Pechora petroleum province]. Neftegazovaya geologiya. Teoriya i praktika, 2008, v. 3, no. 3, http://www.ngtp.ru/rub/4/40_2008.pdf
Plotitsyn A.N. Nizhneturneyskiye konodonty r. Malaya Usa (Polyarnyy Ural) [Lower Tournaisian conodonts of the Small Usa River section (Polar Urals)]. Struktura. veshchestvo. istoriya litosfery Timano-Severouralskogo segmenta: materials of the 23-rd youth scientific conference. Syktyvkar: Geoprint, 2014, p. 105 109.
Plotitsyn A.N. Korrelyatsionnyye urovni v verkhnem famene i turne severa Urala i gryady Chernysheva [Correlation levels in Upper Famennian – Tournaisian deposits of the North of Urals and Chernishev Swell]. Vestnik IG Komi SC UB RAS, 2016, no. 7, p. 46 53.
Plotitsyn A.N., Beznosov P.A. Conodont and vertebrate assemblages from the Early Carboniferous section of Malaya Usa River (Polar Urals, Russia). Abstracts of the XVIII International Congress on the Carboniferous and Permian. Kazan, 2015, p. 146.
Plotitsyn A.N., Zhuravlev A.V. Novyye vidy konodontov rodov Neopolygnathus i Polygnathus iz turneyskikh otlozheniy severa Urala i gryady Chernysheva [The new species of Neopolygnathus and Polygnathus from the Tournaisian of the North Urals and Chernyshev Ridge]. Syktyvkar palaeontological miscellany № 8, Syktyvkar, 2017, p. 24 30 (Proceedings of Institute of Geology of Komi Science Centre UB RAS, v. 130).
Plotitsyn A.N., Zhuravlev A.V. A new species of the conodont genus Polygnathus from the Tournaisian of the Northern Urals, Chernyshev Ridge and Pai-Khoi. Paleontological Journal, 2017, v. 51, no. 3, p. 304 307.
Plotitsyn A.N.. Zhuravlev A.V.. Vevel Ya.A.. Gruzdev D.A. Sredneturneyskoye sobytiye na severe Urala i v Priuralye [Mid-Tournaisian event on the North of the Urals and Cis-Urals]. Fundamentalnaya i prikladnaya paleontologiya: materials of the LXIV session of the Paleontological society. St. Petersburg, 2018, p. 89 90.
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in ?13С: an example from the lower Mississippian. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, v. 213, p. 359–377.
Sandberg C.A., Morrow J.R., Ziegler W. Late Devonian sea-level changes, catastrophic events, and mass extinctions. Geological Society of America, 2002, Special Paper 356, p. 473–487.
Sandberg C.A., Ziegler W., Leuteritz K., Brill S.M. Phylogeny, speciation, and zonation of Siphonodella (Conodonta, Upper Devonian and Lower Carboniferous). Newsletters on Stratigraphy, 1978, vol. 7, no. 2, p. 102–120.
Stevens C.H., Klingman D.S., Sandberg C.A., Stone P., Belasky P., Poole F.G., Snow K. Mississippian stratigraphic framework of east-central California and southern Nevada with revision of Upper Devonian and Mississippian stratigraphic units in Inyo County, California: U.S. Geological Survey, 1996, bull. 1988–J, p. 1–39.
Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracodes and biostratigraphy of the Tournaisian of the North of the Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
Sobolev D.B. Evolyutsiya i bioraznoobraziye rannekamennougolnykh ostrakod na sobytiynykh urovnyakh [Evolution and biodiversity of Early Carboniferous ostracods at the several event levels]. Biogeologiya. evolyutsiya organizmov i bioraznoobraziya v geologicheskoy istorii Timano-Severouralskogo regiona, modelirovaniye paleoekosistem. paleontologicheskiye i stratigraficheskiye geokorrelyatsii. Syktyvkar: Geoprint, 2011, p. 102 108.
Timonin N.I. Pechorskaya plita: istoriya geologicheskogo razvitiya v fanerozoye [Pechora plate: the history of geological development in the Phanerozoic.]. Ekaterinburg: UrO RAN, 1998, 239 p.
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang B., Wang X. The TICE event: Perturbation of carbon–nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse–icehouse transition. Chemical Geology, 2015, v. 401, p. 1 14.
Zhuravlev A.V. The Mid-Tournaisian Event in the Northern Urals and conodont dynamics. Proceedings of Geologists Association, 1998, no. 109, p. 161 168.
Zhuravlev A.V. Sredneturneyskoye sobytiye [Mid-Tournaisian event]. Ispolzovaniye sobytiyno-stratigraficheskikh urovney dlya mezhregionalnoy korrelyatsii fanerozoya Rossii: toolkit. St. Petersburg: VSEGEI, 2000, p. 46 48.
Zhuravlev A.V., Vevel Ya.A., Iosifidi A.G., Tomsha V.A. Razrez verkhnego devona – nizhnego karbona na myse Kostyanom ostrova Vaygach [Upper Devonian – Lower Carboniferous of the Kostyanoy cape of the Vaygach island]. Neftegazovaya geologiya. Teoriya i praktika, 2011, vol. 6, no 1, available at: http://www.ngtp.ru/rub/2/6_2011.pdf.
Zhuravlev A.V., Plotitsyn A.N. Stratotip vazhkhanoveyskoy svity v kanone reki Bolshaya Usa kak geologicheskiy pamyatnik prirody regionalnogo znacheniya [Stratotype of the Vashkhan Formation in the canyon of the Big Usa river as a geological natural monument of the regional significance]. Prirodnoye geologicheskoye naslediye Evropeyskogo Severa Rossii: materials of the All-Russian Scientific Conference. Syktyvkar: IG Komi SC UB RAS, 2017, p. 41 43.
Zhuravlev A.V., Plotitsyn A.N. The symmetry of the rostrum as a key to taxonomy of advanced Siphonodella (Conodonta, Early Carboniferous). Stratigraphy, 2017, vol. 14, no. 1 4, p.457 474.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 19_2018 | submitted on 05/14/2018 displayed on website on 06/18/2018 |
| 21 p. | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. |
| Local stratigraphy of the Upper Devonian – Carboniferous of the north of Pay-Khoy | |
| Analyses of stratigraphical data on Upper Devonian and Carboniferous of the north of Pay-Khoy allow elaborating a new stratigraphic scheme comprising the Pechora and Pay-Khoy formation belts. Correlation of the local stratigraphical units of the belts is based on biostratigraphical and event-stratigraphical methods. A number of interfacial correlative levels corresponding to global eustatic events are detected, namely: Middlesex, Kellwasser, Dasberg, Hangenberg, Late Tournaisian-Early Visean, Mid-Visean, and Mid-Carboniferous.
Keywords: stratigraphical data, Upper Devonian, Carboniferous, interfacial correlative level, eustatic events, Pay-Khoy. |
|
| article citation | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. Mestnaya stratigraficheskaya skhema verkhnego devona i karbona severa Pay-Khoya [Local stratigraphy of the Upper Devonian – Carboniferous of the north of Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 2, available at: http://www.ngtp.ru/rub/2/19_2018.pdf |
| DOI | https://doi.org/10.17353/2070-5379/19_2018 |
References
Barskov I.S., Kononova L.I. O konodontakh kamennougol’nykh otlozheniy mysa Chayka (Yugo-Zapadnyy Pay-Khoy) [About conodonts of the Carboniferous deposits of the Chayka Cape (South-Western Pay-Khoy)]. Izvestiya AN SSSR. Geologiya, 1983, p. 1163-1167.
Becker R.T. Anoxia, evolutionary changes, and Upper Devonian to lowermost Carboniferous global ammonoid diversity. In: M.R. House (ed.), The Ammonoidea: Environment, Ecology, and Evolutionary Change, 1993, Systematic Association Special Volume 47, p. 115–163.
Becker R.T., Kaiser S.I., Aretz M. Review of chrono-, litho- and biostratigraphy across the global Hangenberg Crisis and Devonian–Carboniferous Boundary. Geological Society, 2016, no. 423, p. 355-386.
Belyaev A.A. Ftanitovaya verkhnedevonsko-nizhnekamennougol’naya formatsiya Pay-Khoya [Ftanite Upper Devonian-Lower Carboniferous formation of the Pay-Khoy]. Osadochnye paleozoiskie formatsyi Pai-Khoia. Trudy IG KFAN SSSR, 1986, vyp. 56, p. 27-37.
Belyaev A.A., Semenov G.F. Geneticheskie osobennosti serpukhovskikh karbonatnykh otlozheniy slantsevoy zony Pai-Khoia [Genetical peculiarities of the Serpukhovian deposits of the shale zone of Pay-Khoy]. Litologiya karbonatnykh porod severa Urala, Pai-Khoia i Timana. Trudy IG Komi NC UrO AN SSSR, 1988, vyp. 67, p. 51-61.
Belyaev A.A., Semenov G.F. Tolerovaya verkhnedevonsko-srednekamennougol’naya formatsiya Pay-Khoya [Tolerovaya Upper Devonian – Middle Carboniferous formation of the Pay-Khoy]. Osadochnye paleozoiskie formatsyi Pay-Khoya. Trudy IG KFAN SSSR, 1986, vyp. 56, p. 38-48.
Dmitrieva T.V., Zhuravlev A.V., Nikolaev A.I., Eremenko N.M. Fatsial'no-stratigraficheskaya model' devonsko-kamennougol'nykh otlozheniy Korotaikhinskoy vpadiny TPP [Facial-stratigraphic model of Devonian-Carboniferous deposits of Korotaikha depression, Timan-Pechora province]. Razvedka i okhrana nedr, 2011, no. 4, p. 22-27.
Enokyan S.V. Paleozoiskie otlozheniya i istoriya geologicheskogo razvitiya territorii zapadnogo Pai-Khoia i ostrova Vaygach [Palaeozoic deposits and history of geological development of the territory of the western Pay-Khoy and Vaigach Island]. Kand.geol.-min.nauk thesises. Moscow: MGRI, 1971, 26 p.
Kalashnikov N.V., Mikhaylova Z.P., Cheusova G.N. Stratigrafiya kamennougol’nukh otlozheniy reki Peschanoy (Severo-Vostochnyy Pay-Khoy) [Stratigraphy of the Carboniferous of the Peschanaya River (North-Eastern Pay-Khoy)]. Stratigrafia paleozoya severo-vostoka evropeiskoy chasti SSSR. Trudy IG KFAN SSSR, 1981, vyp. 37, p. 53-57.
Krylova A.K. K stratigrafii srednego i verkhnego paleozoya yugo-zapadnogo Pay-Khoya [The stratigraphy of the Middle and Upper Paleozoic southwest of Pay-Khoy]. Zap.VMO, 1940, part 69, chapter 2, vol. 2-3, p. 418-427.
Romanov A.A., Zhuravlev A.V. Vzaimootnosheniya karbonatnogo paravtokhtona i slancevogo allokhtona Pai-Khoia (Yugorskiy poluostrov) [The relationship of the shale allochton and carbonate parautochton of Pay-Khoy (Ugra Peninsula)]. Vestnik IG Komi SC UrB RAS, 2017, no. 1, p. 22-28.
Sandberg C.A., Morrow J.R., Ziegler W. Late Devonian sea-level changes, catastrophic events, and mass extinctions. In: C. Koeberl, K.G. MacLeod (eds), Catastrophic Events and Mass Extinctions: Impacts and Beyond. Geol. Soc. Am., Spec. Pap., 2002, vol. 356, p. 473–487. DOI: https://doi.org/10.1130/0-8137-2356-6.473
Schindler E. Die Kellwasser-Krise (hohe Frasne-Stufe, Ober-Devon). Gottinger Arbeiten zur Geologie und Palaontologie, 1990, no. 46, p. 1–115.
Solov'eva M.N. Nizhnyaya granitsa verkhnego karbona po faune foraminifer Yugorskogo poluostrova [Lower boundary of the Upper Carboniferous based on foraminifer fauna of the Yugra Peninsula]. Verkhniy karbon SSSR. Moscow: Nauka, 1984, p. 121-155.
Stepanov D.L., Sultanaev A.A., Grozdilova L.P., Degtyarev D.D., Kruchinina O.N., Lapina N.N., Muromtseva V.A., Nikolaev A.I., Popov A.V., Simakova M.A., Tkacheva I.D. Novoe o srednem karbone Yugo-Zapadnogo Pay-Khoya [New data on the Middle Carboniferous of South-Western Pay-Khoy]. Vestnik LGU, 1977, no. 24, p. 25-32.
Timonin N.I. Geologicheskoe stroenie severo-zapadnoi chasti Pay-Khoya [Geological composition of north-western Pay-Khoy]. In A.M.Pystin (ed.) Problemy geologii i mineralogii. Syktyvkar: Geoprint, 2006, p. 117-127.
Timonin N.I., Yudin V.V., Belyaev A.A. Paleogeodinamika Pay-Khoya [Pay-Khoy Paleogeodynamics]. Ekaterinburg: UrO RAN, 2004, 223 pp.
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of North Urals and Pay-Khoy]. RAN, Ural. otd-nie, Komi nauch. tsentr, In-t geologii. Ekaterinburg: UIF "Nauka", 1994, 285 p.
Yushkin N.P., Kunts A.F., Timonin N.I. Minerageniya Pay-Khoya [Pay-Khoy minerageny]. Ekaterinburg: UrO RAN, 2007, 292 pp.
Zhuravlev A. Conodont response to middle Visean (Early Carboniferous) ecological event – preliminary data. Cour. Forcb.-lnst, Senchenbery, 2003, no. 245, p. 255-259.
Zhuravlev A.V. Novaya hengurseyskaya svita verkhnego devona yugo-zapadnogo Pay-Khoya [A new Hengurse Formation of the Upper Devonian of the south-western slope of Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2010, vol. 5, no. 2, available at: http://www.ngtp.ru/rub/2/20_2010.pdf
Zhuravlev A.V. Stroenie i usloviya formirovaniya franskikh otlozheniy severo-zapadnogo Pay-Khoya [Structure and formation conditions of Frasnian section, northwest Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 4, available at: http://www.ngtp.ru/rub/2/38_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/38_2016
Zhuravlev A.V., Gerasimova A.I. Stroenie razreza i konodonty karskoy svity (nizhniy karbon) Amderminskogo raiona severnogo Pay-Khoya [Sequence composition and conodonts of the Kara Formation (Lower Carboniferous) of the Amderma District of the northern Pay-Khoy]. Vestnik IG Komi SC UrB RAS, 2016, no.1, p. 3. DOI: 10.19110/2221-1381-2016-1-3-10
Zhuravlev A.V., Gerasimova A.I., Vevel Y.A. Mestnaya stratigraficheskaya skhema verkhnedevonsko-srednekamennougol’nogo intervala severa Paykhoyskogo karbonatnogo paravtokhtona[Local stratigraphical map of Upper Devonian - Middle Carboniferous interval of Northern Pay-Khoy carbonate parautochthone]. Vestnik IG Komi SC UrB RAS, 2015, no. 4, p. 8-13.
Zhuravlev A.V., Vevel' Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf. DOI: https://doi.org/10.17353/2070-5379/3_2018
Zhuravlev A.V., Vevel' Y.A. Srednekamennougol'naya granitsa na severe Pay-Khoya – korrelyatsiya melkovodnykh i glubokovodnykh razrezov [The Middle Carboniferous boundary in the north of Pay-Khoy – correlation between the shallow-and deep-water sequences]. Uchenye Zapiski Kazanskogo Universiteta. Seriya Estestvennye Nauki, 2017, vol. 159, no.1, p. 152–163.
Zhuravlev A.V., Vevel' Y.A., Iosifidi A.G., Tomsha V.A., Chermnykh V.A. Razrez verkhnego devona – nizhnego karbona na myse Kostyanom ostrova Vaigach [Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 1, available at: http://www.ngtp.ru/rub/2/6_2011.pdf
Becker R.T. Anoxia, evolutionary changes, and Upper Devonian to lowermost Carboniferous global ammonoid diversity. In: M.R. House (ed.), The Ammonoidea: Environment, Ecology, and Evolutionary Change, 1993, Systematic Association Special Volume 47, p. 115–163.
Becker R.T., Kaiser S.I., Aretz M. Review of chrono-, litho- and biostratigraphy across the global Hangenberg Crisis and Devonian–Carboniferous Boundary. Geological Society, 2016, no. 423, p. 355-386.
Belyaev A.A. Ftanitovaya verkhnedevonsko-nizhnekamennougol’naya formatsiya Pay-Khoya [Ftanite Upper Devonian-Lower Carboniferous formation of the Pay-Khoy]. Osadochnye paleozoiskie formatsyi Pai-Khoia. Trudy IG KFAN SSSR, 1986, vyp. 56, p. 27-37.
Belyaev A.A., Semenov G.F. Geneticheskie osobennosti serpukhovskikh karbonatnykh otlozheniy slantsevoy zony Pai-Khoia [Genetical peculiarities of the Serpukhovian deposits of the shale zone of Pay-Khoy]. Litologiya karbonatnykh porod severa Urala, Pai-Khoia i Timana. Trudy IG Komi NC UrO AN SSSR, 1988, vyp. 67, p. 51-61.
Belyaev A.A., Semenov G.F. Tolerovaya verkhnedevonsko-srednekamennougol’naya formatsiya Pay-Khoya [Tolerovaya Upper Devonian – Middle Carboniferous formation of the Pay-Khoy]. Osadochnye paleozoiskie formatsyi Pay-Khoya. Trudy IG KFAN SSSR, 1986, vyp. 56, p. 38-48.
Dmitrieva T.V., Zhuravlev A.V., Nikolaev A.I., Eremenko N.M. Fatsial'no-stratigraficheskaya model' devonsko-kamennougol'nykh otlozheniy Korotaikhinskoy vpadiny TPP [Facial-stratigraphic model of Devonian-Carboniferous deposits of Korotaikha depression, Timan-Pechora province]. Razvedka i okhrana nedr, 2011, no. 4, p. 22-27.
Enokyan S.V. Paleozoiskie otlozheniya i istoriya geologicheskogo razvitiya territorii zapadnogo Pai-Khoia i ostrova Vaygach [Palaeozoic deposits and history of geological development of the territory of the western Pay-Khoy and Vaigach Island]. Kand.geol.-min.nauk thesises. Moscow: MGRI, 1971, 26 p.
Kalashnikov N.V., Mikhaylova Z.P., Cheusova G.N. Stratigrafiya kamennougol’nukh otlozheniy reki Peschanoy (Severo-Vostochnyy Pay-Khoy) [Stratigraphy of the Carboniferous of the Peschanaya River (North-Eastern Pay-Khoy)]. Stratigrafia paleozoya severo-vostoka evropeiskoy chasti SSSR. Trudy IG KFAN SSSR, 1981, vyp. 37, p. 53-57.
Krylova A.K. K stratigrafii srednego i verkhnego paleozoya yugo-zapadnogo Pay-Khoya [The stratigraphy of the Middle and Upper Paleozoic southwest of Pay-Khoy]. Zap.VMO, 1940, part 69, chapter 2, vol. 2-3, p. 418-427.
Romanov A.A., Zhuravlev A.V. Vzaimootnosheniya karbonatnogo paravtokhtona i slancevogo allokhtona Pai-Khoia (Yugorskiy poluostrov) [The relationship of the shale allochton and carbonate parautochton of Pay-Khoy (Ugra Peninsula)]. Vestnik IG Komi SC UrB RAS, 2017, no. 1, p. 22-28.
Sandberg C.A., Morrow J.R., Ziegler W. Late Devonian sea-level changes, catastrophic events, and mass extinctions. In: C. Koeberl, K.G. MacLeod (eds), Catastrophic Events and Mass Extinctions: Impacts and Beyond. Geol. Soc. Am., Spec. Pap., 2002, vol. 356, p. 473–487. DOI: https://doi.org/10.1130/0-8137-2356-6.473
Schindler E. Die Kellwasser-Krise (hohe Frasne-Stufe, Ober-Devon). Gottinger Arbeiten zur Geologie und Palaontologie, 1990, no. 46, p. 1–115.
Solov'eva M.N. Nizhnyaya granitsa verkhnego karbona po faune foraminifer Yugorskogo poluostrova [Lower boundary of the Upper Carboniferous based on foraminifer fauna of the Yugra Peninsula]. Verkhniy karbon SSSR. Moscow: Nauka, 1984, p. 121-155.
Stepanov D.L., Sultanaev A.A., Grozdilova L.P., Degtyarev D.D., Kruchinina O.N., Lapina N.N., Muromtseva V.A., Nikolaev A.I., Popov A.V., Simakova M.A., Tkacheva I.D. Novoe o srednem karbone Yugo-Zapadnogo Pay-Khoya [New data on the Middle Carboniferous of South-Western Pay-Khoy]. Vestnik LGU, 1977, no. 24, p. 25-32.
Timonin N.I. Geologicheskoe stroenie severo-zapadnoi chasti Pay-Khoya [Geological composition of north-western Pay-Khoy]. In A.M.Pystin (ed.) Problemy geologii i mineralogii. Syktyvkar: Geoprint, 2006, p. 117-127.
Timonin N.I., Yudin V.V., Belyaev A.A. Paleogeodinamika Pay-Khoya [Pay-Khoy Paleogeodynamics]. Ekaterinburg: UrO RAN, 2004, 223 pp.
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of North Urals and Pay-Khoy]. RAN, Ural. otd-nie, Komi nauch. tsentr, In-t geologii. Ekaterinburg: UIF "Nauka", 1994, 285 p.
Yushkin N.P., Kunts A.F., Timonin N.I. Minerageniya Pay-Khoya [Pay-Khoy minerageny]. Ekaterinburg: UrO RAN, 2007, 292 pp.
Zhuravlev A. Conodont response to middle Visean (Early Carboniferous) ecological event – preliminary data. Cour. Forcb.-lnst, Senchenbery, 2003, no. 245, p. 255-259.
Zhuravlev A.V. Novaya hengurseyskaya svita verkhnego devona yugo-zapadnogo Pay-Khoya [A new Hengurse Formation of the Upper Devonian of the south-western slope of Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2010, vol. 5, no. 2, available at: http://www.ngtp.ru/rub/2/20_2010.pdf
Zhuravlev A.V. Stroenie i usloviya formirovaniya franskikh otlozheniy severo-zapadnogo Pay-Khoya [Structure and formation conditions of Frasnian section, northwest Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 4, available at: http://www.ngtp.ru/rub/2/38_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/38_2016
Zhuravlev A.V., Gerasimova A.I. Stroenie razreza i konodonty karskoy svity (nizhniy karbon) Amderminskogo raiona severnogo Pay-Khoya [Sequence composition and conodonts of the Kara Formation (Lower Carboniferous) of the Amderma District of the northern Pay-Khoy]. Vestnik IG Komi SC UrB RAS, 2016, no.1, p. 3. DOI: 10.19110/2221-1381-2016-1-3-10
Zhuravlev A.V., Gerasimova A.I., Vevel Y.A. Mestnaya stratigraficheskaya skhema verkhnedevonsko-srednekamennougol’nogo intervala severa Paykhoyskogo karbonatnogo paravtokhtona[Local stratigraphical map of Upper Devonian - Middle Carboniferous interval of Northern Pay-Khoy carbonate parautochthone]. Vestnik IG Komi SC UrB RAS, 2015, no. 4, p. 8-13.
Zhuravlev A.V., Vevel' Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf. DOI: https://doi.org/10.17353/2070-5379/3_2018
Zhuravlev A.V., Vevel' Y.A. Srednekamennougol'naya granitsa na severe Pay-Khoya – korrelyatsiya melkovodnykh i glubokovodnykh razrezov [The Middle Carboniferous boundary in the north of Pay-Khoy – correlation between the shallow-and deep-water sequences]. Uchenye Zapiski Kazanskogo Universiteta. Seriya Estestvennye Nauki, 2017, vol. 159, no.1, p. 152–163.
Zhuravlev A.V., Vevel' Y.A., Iosifidi A.G., Tomsha V.A., Chermnykh V.A. Razrez verkhnego devona – nizhnego karbona na myse Kostyanom ostrova Vaigach [Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 1, available at: http://www.ngtp.ru/rub/2/6_2011.pdf
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 3_2018 | submitted on 01/31/2018 displayed on website on 02/14/2018 |
| 10 p. | Zhuravlev A.V., Vevel Ya.A. |
| The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) | |
| The late Tournaisian Event (Mid-Aikuanian Event) appearing as significant changes in marine and terrestrial biota is considered as consequence of the beginning of the Early Carboniferous phase of the Gondwana glaciation and transition from the greenhouse climate to icehouse climate. The event caused one of the highest Palaeozoic shift in the carbon isotope ratio. This shift was traced in the sections of the Kosyu-Rogovaya Depression and adjacent areas: 1-Kochmes borehole, the Izyayu River section, and the Kozhym River section. The isotope shift is dated by conodonts of the Siphonodella isosticha and Gnathodus typicus zones, foraminifers Eoforschia gigantea and Dainella, and algae Exvotarisella. The traces of the late Tournaisian Event are considered as reliable stratigraphic tool for the eastern part of the Timan-Pechora Province.
Keywords: Lower Carboniferous, Tournaisian, isotopic anomaly, late Tournaisian Event, Timan-Pechora Province, Kosyu-Rogovaya Depression. |
|
| article citation | Zhuravlev A.V., Vevel Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) ]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf |
| DOI | https://doi.org/10.17353/2070-5379/3_2018 |
References
Kostygova P.K. Pechorskiy paleobasseyn v vizeyskom i serpukhovskom vekakh i foraminifery nizhnego vize [Pechora palaeobasin in the Visean and Serpukhovian, and foraminifers of the Lower Visean]. St. Petersburg: VSEGEI, 2004, 204 p.
Nikonov N.I., Bogatskiy V.I., Martynov A.V., Larionova Z.V., Laskin V.M., Galkina L.V., Dovzhikova E.G., Ermakova O.L., Kostygova P.K., Kuranova T.I., Moskalenko K.A., Pankratov Yu.A., Petrenko E.L., Popova E.V., Surina A.I., Shabanova G.A. Timano-Pechorskiy sedimentatsionnyy basseyn. Atlas geologicheskikh kart [Timan-Pechora sedimentary basin. Atlas of geological maps]. Ukhta, 2000, 67 p.
Saltzman M.R. Carbon and oxygen isotope stratigraphy of the Lower Mississippian (Kinderhookian–early Osagean), western United States: implications for seawater chemistry and glaciation. Geological Society of America Bulletin, 2002, no. 114, p. 96–108. DOI: https://doi.org/10.1130/0016-7606(2002)114%3C0096:CAOISO%3E2.0.CO;2
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in б13C: an example from the lower Mississippian. Paleogeography, Paleoclimatology, Paleoecology, 2004, vol. 213, p. 359–377. DOI: https://doi.org/10.1016/S0031-0182(04)00389-X
Scotese C.R. PALEOMAP PaleoAtlas for GPlates and the PaleoDataPlotter program Geological Society of America Abstracts with Programs. 2016, vol. 48, no. 5. DOI: https://doi.org/10.1130/abs/2016NC-275387
Yao L., Qie W., Luo G., Liu J., Algeo T. J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian – Lower Carboniferous of north-east of European Russia]. St. Petersburg: VSEGEI, 2003, 85 p.
Nikonov N.I., Bogatskiy V.I., Martynov A.V., Larionova Z.V., Laskin V.M., Galkina L.V., Dovzhikova E.G., Ermakova O.L., Kostygova P.K., Kuranova T.I., Moskalenko K.A., Pankratov Yu.A., Petrenko E.L., Popova E.V., Surina A.I., Shabanova G.A. Timano-Pechorskiy sedimentatsionnyy basseyn. Atlas geologicheskikh kart [Timan-Pechora sedimentary basin. Atlas of geological maps]. Ukhta, 2000, 67 p.
Saltzman M.R. Carbon and oxygen isotope stratigraphy of the Lower Mississippian (Kinderhookian–early Osagean), western United States: implications for seawater chemistry and glaciation. Geological Society of America Bulletin, 2002, no. 114, p. 96–108. DOI: https://doi.org/10.1130/0016-7606(2002)114%3C0096:CAOISO%3E2.0.CO;2
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in б13C: an example from the lower Mississippian. Paleogeography, Paleoclimatology, Paleoecology, 2004, vol. 213, p. 359–377. DOI: https://doi.org/10.1016/S0031-0182(04)00389-X
Scotese C.R. PALEOMAP PaleoAtlas for GPlates and the PaleoDataPlotter program Geological Society of America Abstracts with Programs. 2016, vol. 48, no. 5. DOI: https://doi.org/10.1130/abs/2016NC-275387
Yao L., Qie W., Luo G., Liu J., Algeo T. J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian – Lower Carboniferous of north-east of European Russia]. St. Petersburg: VSEGEI, 2003, 85 p.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 17_2017 | submitted on 02/10/2017 displayed on website on 05/16/2017 |
| 13 p. | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. |
| Characteristic of the pore space in the Upper-Devonian - Carboniferous Carbonate section of the Pai-Khoy Parautochthone unit | |
| The characteristics of intergrain pore space in the carbonate deposits of the Upper Devonian - Carboniferous Pai-Khoy carbonate parautochtone unit are given. The total and open porosity of carbonate rocks is characterized by low values; however, small pores with an average diameter predominate in the pore space. The main factors controlling the values of intergranular porosity of the Upper Devonian - Carboniferous carbonates are rock texture and the degree of secondary transformations: the porosity is proportional to the detritus size and decreases in thermally matured rocks.
Keywords: intergranular porosity, carbonates, Late Devonian – Carboniferous, Pai-Khoy Carbonate Parautochtone. |
|
| article citation | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. Kharakteristika porovogo prostranstva v porodakh verkhnedevonsko-kamennougol'nogo karbonatnogo kompleksa Pay-Khoyskogo paravtokhtona [Characteristic of the pore space in the Upper-Devonian - Carboniferous Carbonate section of the Pai-Khoy Parautochthone unit]. Neftegazovaya Geologiya. Teoriya I Praktika, 2017, vol. 12, no. 2, available at: http://www.ngtp.ru/rub/2/17_2017.pdf |
| DOI | https://doi.org/10.17353/2070-5379/17_2017 |
References
|
|
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 21_2012 | submitted on 02/21/2012 displayed on website on 04/19/2012 |
| 9 p. | Zhuravlev A.V., Vevel Ya.A. |
| Possibilities of computed microtomography application in micropalaeontological and lithological studies* | |
| *The article is presented in two languages, Russian and English. Possibilities of the computed X-ray and optic tomography in the micropalaeontological and lithological studies are considered. X-ray microtomography allows determining phosphate microfossils (conodonts) avoiding special sample preparation; evaluate the total porosity and concentration of sulfides. The optic microtomography promises results in histological study of conodont elements. Key words: tomography, micropalaeontology, conodonts, foraminifers, lithology, carbonates, silicites. |
|
| article citation | Zhuravlev A.V., Vevel’ Ya.A. Vozmozhnosti ispol'zovaniya vychislitel'noy mikrotomografii v mikropaleontologicheskikh i litologicheskikh issledovaniyakh [Possibilities of computed microtomography application in micropalaeontological and lithological studies]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 2, available at: http://www.ngtp.ru/rub/2/21_2012.eng.pdf |
References
|
Zhuravlev A.V. Gistologiya i mikroskul'ptura pozdnepaleozoyskikh konodontovykh elementov [Late Palaeozoic conodont element histology and micro-ornamentation]. Saint Petersburg.: Geoservis Plyus, 2002, 94 p. |
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 6_2012 | submitted on 10/26/2011 displayed on website on 01/25/2012 |
| 19 p. | Vevel Ya.A., Zhuravlev A.V., Popov V.V. |
| Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province) | |
| The article deals with the Devonian-Carboniferous boundary in the shallow-water strata (the Kamenka River section as example) on the basis of cyclostratigraphy (maximum of regression) controlled by biostratigraphical data (conodonts and foraminifera). Facial control on the foraminifer and conodont associations is considered. Dependence of the magnetic suscessibility of the rocks on the sea-level changes is detected. The dependence is probably caused by variations of the terrigenous content in the carbonate rocks.
Keywords: conodonts, foraminifera, cyclostratigraphic method, magnetic susceptibility of rocks, Devonian-Carboniferous boundary strata, Timan-Pechora province.
Key words: Devonian/Carboniferous boundary, Timan-Pechora Province, conodonts, foraminifers, cyclostratigraphy, biostratigraphy, palaeomagnitology. |
|
| article citation | Vevel' Ya.A., Zhuravlev A.V., Popov V.V. Pogranichnye otlozheniya devonskoy i kamennougol'noy sistem v razreze na r. Kamenka (Pechoro-Kozhvinskiy megaval, Timano-Pechorskaya provintsiya) [Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/6_2012.pdf |
References
Barskov I.S., Kononova L.I., Migdisova A.V. Konodonty nizhneturneyskikh otlozheniy podmoskovnogo basseyna [Conodonts of the Lower Tournaisian deposits of the Pre-Moscow Basin]. Paleontologicheskaya kharakteristika stratotipicheskikh i opornykh razrezov karbona Moskovskoy sineklizy. Editor V.V. Menner. Moscow: Moskow State University, 1984, pp. 3-33.
Eremenko N.M., Vevel' Ya.A., Zhuravlev A.V. Interfatsial'naya korrelyatsiya morskikh ranneturneyskikh otlozheniy severa Urala i vostoka Timano-Pechorskoy plity – litostratigraficheskiy podkhod [Inter-facial correlation of the Lower Tournaisian marine deposits, northern Urals and eastern Timan-Pechora plate - lithostratigraphic approach]. Proceedings of the International Scientific Conference “Litologicheskie i geokhimicheskie osnovy prognoza neftegazonosnosti” [Lithological and geochemical basis of oil and gas potential forecast]. Saint Petersburg: VNIGRI, 2008, pp. 600-605.
Fauna i biostratigrafiya pogranichnykh otlozheniy devona i karbona Berchogura (Mugodzhary) [Fauna and biostratigraphy of the Devonian and Carboniferous deposits, Berchogur (Mugodzhary)]. Moscow: Nauka, 1987, 121 p.
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol. 49, 1965, pp. 445-459.
Kulagina E.I., Gibshman N.B. Obshchaya zonal'naya shkala nizhnego karbona Rossii po foraminiferam [Total zonal scale of the Lower Carboniferous of Russia in view of foraminifera]. Byulleten’ MOIP. Otdelenie geologicheskoe, 2005, vol. 80, no. 2, pp. 60-67.
Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. Saint Petersburg: Saint Petersburg State Mining University, 2010, 276 p.
Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracoda and biostratigraphy of the Tournaisian stage, north of the Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
Vevel' Ya.A. Nakhodka foraminifer Tournayellina beata pseudobeata Reitlinger et Kulagina v nizhnem karbone Pechorskoy gryady [Discovery of foraminifera Tournayellina beata pseudobeata Reitlinger et Kulagina in the Lower Carboniferous Pechora ridge]. Neftegazovaya geologiya. Teoriya i praktika, 2009, vol. 4, no. 2, available at: http://www.ngtp.ru/rub/2/17_2009.pdf
Zhuravlev A. Biogeography of the Early Carboniferous conodont genus Patrognathus. In: Wong, Th. E. (Ed.): Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy. Utrecht, the Netherlands, 10–16 August 2003. Royal Netherlands Academy of Arts and Sciences, 2007, pp. 325-329.
Zhuravlev A.V. Gistologiya i mikroskul'ptura pozdnepaleozoyskikh konodontovykh elementov [Histology and microsculpture the Late Paleozoic conodont elements]. Saint Petersburg: Geoservis Plyus, 2002, 94 p.
Zhuravlev A.V. Konodontovaya zonal'nost' nizhnego karbona dlya melkovodnykh otlozheniy [Conodont zonation of the Lower Carboniferous for shallow-water deposits]. Proceedings of the All-Russia meeting “Zonal'nye podrazdeleniya karbona obshchey stratigraficheskoy shkaly Rossii” [Zonal subdivision of the Carboniferous common stratigraphic scale of Russia]. Ufa: Gilem, 2000, pp. 42-43.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous north-east of European Russia]. Saint Petersburg: VSEGEI, 2003, 85 p.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Biostratigraphy of the Lower Tournaisian (Lower Carboniferous) shallow-water deposits of the Eastern Part of the Timan-Pechora Province. Newsletter on Carboniferous Stratigraphy, 1999, no. 17, pp. 22-26.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Early Tournasian (Early Carconiferous) Shallow water Communities (Eastern part of the Timan-Pechora Province). Ichthyolith Issues special Publication 4, 1998, pp. 60-62.
Eremenko N.M., Vevel' Ya.A., Zhuravlev A.V. Interfatsial'naya korrelyatsiya morskikh ranneturneyskikh otlozheniy severa Urala i vostoka Timano-Pechorskoy plity – litostratigraficheskiy podkhod [Inter-facial correlation of the Lower Tournaisian marine deposits, northern Urals and eastern Timan-Pechora plate - lithostratigraphic approach]. Proceedings of the International Scientific Conference “Litologicheskie i geokhimicheskie osnovy prognoza neftegazonosnosti” [Lithological and geochemical basis of oil and gas potential forecast]. Saint Petersburg: VNIGRI, 2008, pp. 600-605.
Fauna i biostratigrafiya pogranichnykh otlozheniy devona i karbona Berchogura (Mugodzhary) [Fauna and biostratigraphy of the Devonian and Carboniferous deposits, Berchogur (Mugodzhary)]. Moscow: Nauka, 1987, 121 p.
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol. 49, 1965, pp. 445-459.
Kulagina E.I., Gibshman N.B. Obshchaya zonal'naya shkala nizhnego karbona Rossii po foraminiferam [Total zonal scale of the Lower Carboniferous of Russia in view of foraminifera]. Byulleten’ MOIP. Otdelenie geologicheskoe, 2005, vol. 80, no. 2, pp. 60-67.
Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. Saint Petersburg: Saint Petersburg State Mining University, 2010, 276 p.
Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracoda and biostratigraphy of the Tournaisian stage, north of the Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
Vevel' Ya.A. Nakhodka foraminifer Tournayellina beata pseudobeata Reitlinger et Kulagina v nizhnem karbone Pechorskoy gryady [Discovery of foraminifera Tournayellina beata pseudobeata Reitlinger et Kulagina in the Lower Carboniferous Pechora ridge]. Neftegazovaya geologiya. Teoriya i praktika, 2009, vol. 4, no. 2, available at: http://www.ngtp.ru/rub/2/17_2009.pdf
Zhuravlev A. Biogeography of the Early Carboniferous conodont genus Patrognathus. In: Wong, Th. E. (Ed.): Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy. Utrecht, the Netherlands, 10–16 August 2003. Royal Netherlands Academy of Arts and Sciences, 2007, pp. 325-329.
Zhuravlev A.V. Gistologiya i mikroskul'ptura pozdnepaleozoyskikh konodontovykh elementov [Histology and microsculpture the Late Paleozoic conodont elements]. Saint Petersburg: Geoservis Plyus, 2002, 94 p.
Zhuravlev A.V. Konodontovaya zonal'nost' nizhnego karbona dlya melkovodnykh otlozheniy [Conodont zonation of the Lower Carboniferous for shallow-water deposits]. Proceedings of the All-Russia meeting “Zonal'nye podrazdeleniya karbona obshchey stratigraficheskoy shkaly Rossii” [Zonal subdivision of the Carboniferous common stratigraphic scale of Russia]. Ufa: Gilem, 2000, pp. 42-43.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous north-east of European Russia]. Saint Petersburg: VSEGEI, 2003, 85 p.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Biostratigraphy of the Lower Tournaisian (Lower Carboniferous) shallow-water deposits of the Eastern Part of the Timan-Pechora Province. Newsletter on Carboniferous Stratigraphy, 1999, no. 17, pp. 22-26.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Early Tournasian (Early Carconiferous) Shallow water Communities (Eastern part of the Timan-Pechora Province). Ichthyolith Issues special Publication 4, 1998, pp. 60-62.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 16_2011 | submitted on 04/06/2011 displayed on website on 04/27/2011 |
| 18 p. | Zherlygin A.L., Shishlov S.B., Zhuravlev A.V., Vevel Ya.A. |
| Structure and genesis history of Kara-Silovoyahsky devonian organogenic complex (southeastern Pai-Khoi) | |
| New data about the size, shape, composition and structural features of the Devonian organogenic complex (Kara Silova-Yakha interfluve, southeastern Pai-Khoi) are presented. The interpretation of these features is related together with reconstruction of genesis history of this organogenic complex, under the influence of the transgressive-regressive phases of the paleobasin evolution. The study results can be used in geological mapping and in core analysis of wells of the Pre-Urals Trough, where prospective hydrocarbon reservoirs are related to the brecciated aprons, produced by crushing and fracturing of such organogenic structures.
Key words: Pai-Khoi, the Devonian period, conodonts, organogenic complex, lithotypes, genesis history, morpho-litho-stratigraphic unit. |
|
| article citation | Zherlygin A.L., Shishlov S.B., Zhuravlev A.V., Vevel Ya.A. Stroenie i istoriya formirovaniya Kara-Silovoyakhskogo devonskogo organogennogo massiva (yugo-vostochnyy Pay-Khoy) [Structure and genesis history of Kara-Silovoyahsky devonian organogenic complex (southeastern Pai-Khoi)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 2, available at: http://www.ngtp.ru/rub/2/16_2011.pdf |
References
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 6_2011 | submitted on 02/08/2011 displayed on website on 02/22/2011 |
| 31 p. | Zhuravlev A.V., Vevel Ya.A., Iosifidi A.G., Tomsha /Mikhaylova/ V.A., Chermnykh V.A. |
| Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island | |
| Results of multidisciplinary study of the Upper Devonian – Lower Carboniferous succession of the NE of the Vaygach Island are described. T-R cycles,
biostratigraphical units based on foraminifers and conodonts, and magnitostratigraphic zones have been identified in the section for a first time. Due
to complete carbonate succession of the Middle Famennian – Upper Visean, the section is considered as a key one of the NW of the Pay-Khoy – Vaygach
region and the east of Barents Sea shelf.
Key words: stratigraphy, Upper Devonian, Lower Carboniferous, Foraminifera, Conodonta, palaeomagnetism, Vaygach Island. |
|
| article citation | Zhuravlev A.V., Vevel’ Ya.A., Iosifidi A.G., Tomsha V.A., Chermnykh V.A. Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island // Neftegazovaya Geologiya. Teoriya I Praktika. – 2011. -V.6. - #1.- http://www.ngtp.ru/rub/2/6_2011.pdf |
References
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 45_2009 | submitted on 12/10/2009 displayed on website on 12/14/2009 |
| 20 p. | Otmas (Eremenko) N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. |
| Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches | |
| The results of complex studying the Upper Devonian - Lower Carboniferous key sequence on the Talota river (north of the Vashutkino-Talota zone of overthrusts, Timan-Pechora province) are presented. The tectonic twinning of the sequence on the zone of overthrusts is proved by biostratigraphy data. The parautochthonous and allochthonous parts of the sequence are dated by foraminifera and conodonts. The first part contains Early Famenian-Late Visean deposits, the second part - Late Famenian-Serpukhovsk deposits. Breaks in sedimentations are established in the Lower Tournaisian and Lower Visean. The presence of an ancient secondary prefolded component of magnetization, confined to the definite parts of the sequence and caused by tectonic and hypergene processes, is established. The direction of this magnetization allowed reconstructing the prefolded (Middle Paleozoic) position of the allochthone and parautochthone. Key words: Upper Devonian, Lower Carboniferous, key sequence, Timan-Pechora province, stratigraphy, paleomagnetology, tectonics. Sequence description by Eremenko N.M. and Zhuravlev A.V. is provided in the Annex 1. |
|
| article citation | Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45_2009.pdf Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf |
References
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
| Article # 17_2009 | submitted on 03/27/2009 displayed on website on 04/30/2009 |
| 15 p. | Vevel Ya.A. |
| The find of the foraminifera Tournayellina beata pseudobeata Reitlingerer et Kulagina in the Lower Carboniferous of the Pechora ridge | |
| It is said about the find of the Tournayellina beata pseudobeata Reitlingerer et Kul. in the Lower Carboniferous of the Pechora ridge (Timan-Pechora province). This taxon is known only in some localities of the world: southern Urals, northern France, Czechia. The finds located in the Patrognathus crassus conodont zone and characterizing the upper part of the taxon stratigraphic range are considered. Facies control on distribution of the T. beata pseudobeata is also considered. This subspecies occurs in the peloidal pack- and grainstones of the Y facies zone and transition to the Z facies zone by Irvin (1965). Key words: Upper Devonian, Lower Carboniferous, Foraminifers, biostratigraphy, Timan-Pechora province |
|
| article citation | Vevel Ya.A. The find of the foraminifera Tournayellina beata pseudobeata Reitlingerer et Kulagina in the Lower Carboniferous of the Pechora ridge // Neftegazovaya Geologiya. Teoriya I Praktika. – 2009. - V.4. - #2.- http://www.ngtp.ru/rub/2/17_2009.pdf |
References