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References

  • Aisenverg, D. E., et al. (1963), Carboniferous Stratigraphy of the Donets Basin, 183 pp., Publ. House of Ukrainian Acad. of Sci., Kiev.
  • Aisenverg, D. E., et al. (1971), Atlas of Fauna of Carboniferous Deposits of Donets Basin, 327 pp., Nauk. Dumka, Kiev.
  • Aisenverg, D. E., et al. (1975), Field excursion guide book for the Donets Basin (in Russian), in Compte Rendu of the 8th International Congress on Carboniferous Stratigraphy and Geology, pp. 1360, edited by D. E. Aisenverg et al., Nauka, Moscow.
  • Aizenverg, D. E., et al. (1979), Pervyye nakhodki goniatitov v otlozheniyakh svit C11A i C13C Donetskogo basseyna (The first goniatite findings in the C11A and C13C suites of the Donets Basin), Geol. Zh., 39(6), 3240.
  • Aizenverg, D. E., et al. (1983), Verkhneserpukhovskiy Pod'yarus Donetskogo Basseyna (Paleontologicheskaya Kharakteristika), 163 pp., Akad. Nauk Ukrainskoy SSR, Inst. Geol. Nauk, Nauk. Dumka, Kiev.
  • Alekseev, A. S., and N. V. Goreva (2006), Kasimovian and Gzhelian (Upper Pennsylvanian) conodont zonation in Russia, Newsl. Carboniferous Stratigr., 24, 4043.
  • Algeo, T. J., and B. H. Wilkinson (1988), Periodicity of mesoscale Phanerozoic sedimentary cycles and the role of Milankovitch orbital modulation, J. Geol., 96(3), 313322, doi:10.1086/629222.
  • Barrick, J. E., et al. (2004), Pennsylvanian conodont zonation for midcontinent North America, Rev. Esp. Micropaleontol., 36, 231250.
  • Barrick, J. E., et al. (2008), Revision of the conodont Idiognathodus simulator (Ellison 1941), the marker species for the base of the Late Pennsylvanian global Gzhelian Stage, Micropaleontology, 54, 125137.
  • Barskov, I. S., and A. S. Alekseyev (1975), Konodonty srednego i verkhnego karbona Podmoskov'ya (Conodonts of the middle and upper Carboniferous from the vicinity of Moscow), Izv. Akad. Nauk SSSR, Ser. Geol., 6, 8499.
  • Belka, Z., and J. Lehmann (1998), Late Visean/early Namurian conodont succession from the Esla area of the Cantabrian Mountains, Spain, Acta Geol. Pol., 48(1), 3141.
  • Birgenheier, L. P., et al. (2009), Evidence for dynamic climate change on sub-106-year scales from the late Paleozoic glacial record, Tamworth Belt, New South Wales, Australia, J. Sediment. Res., 79, 5682, doi:10.2110/jsr.2009.013.
  • Black, L., et al. (2003), TEMORA 1: A new zircon standard for Phanerozoic U–Pb geochronology, Chem. Geol., 200(1–2), 155170, doi:10.1016/S0009-2541(03)00165-7.
  • Boardman, D. R.II, and P. H. Heckel (1989), Glacial-eustatic sea-level curve for early Late Pennsylvanian sequence in north-central Texas and biostratigraphic correlation with curve for midcontinent North America, Geology, 17(9), 802805, doi:10.1130/0091-7613(1989)017<0802:GESLCF>2.3.CO;2.
  • Brazhnikova, N. E., et al. (1967), Mikrofaunisticheskiye markiruyushchiye gorizonty kamennougol'nykh i permskikh otlozheniy Dneprovsko-Donetskoy vpadiny (Microfaunal Marker Horizons in the Carboniferous and Permian Deposits of the Dnieper-Donets Basin), 285 pp., Akad. Nauk Ukr. SSR, Inst. Geol. Nauk, Kiev.
  • Briand, C., et al. (1998), Stratigraphy and sequence stratigraphy of the Moscovian, Kasimovian and Gzhelian in the Moscow Basin, Bull. Soc. Geol. Fr., 169(1), 3552.
  • Burger, K., et al. (1997), Tephrochronologie mit Kaolin-Kohlentonsteinen: Mittel zur Korrelation paralischer und limnischer Ablagerungen des Oberkarbons, Geol. Jahrb., Reihe A, 147, 339.
  • Chekunov, A. V. (1994), The geodynamics of the Dniepr-Donets rift syneclise (in Russian), Geophysics, 16(3), 313.
  • Chernov'yants, M. G. (1992), Tonshteyni i ikh ispol'zovanie pri izuchenii uglenosnykh formatsyi (Tonsteins and Their Utilization in Coal-Bearing Deposits Study), 130 pp., Nedra, Moscow.
  • Chernykh, V. V. (2002), Zonal scale of the Gzhelian and Kasimovian stages based on conodonts of genus Streptognathodus (in Russian), in Stratigraphy and Paleogeography of Carboniferous of Eurasia, edited by B. I. Chuvashov, and E. A. Amon, pp. 302306, Inst. of Geol. and Geochem., Uralian Branch, Russ. Acad. of Sci., Ekaterinburg.
  • Chernykh, V. V. (2005), Zonal Method in Biostratigraphy: Zonal Conodont Scale of the Lower Permian in the Urals (in Russian), 217 pp., Inst. of Geol. and Geochemistry, Uralian Branch, Russ. Acad. of Sci., Ekaterinburg.
  • Chernykh, V. V., and N. P. Reshetkova (1987), The Biostratigraphy and Conodonts From Carboniferous-Permian Boundary Deposits on the West Slope of the Central and Southern Urals (in Russian), 53 pp., Uralian Branch, USSR Acad. of Sci., Sverdlovsk.
  • Chernykh, V. V., B. I. Chuvashov, V. I. Davydov, M. D. Schmitz, and W. S. Snyder (2006), Usolka section (southern Urals, Russia): A potential candidate for GSSP to define the base of the Gzhelian Stage in the global chronostratigraphic scale, Geologija, 49(2), 205217.
  • Chesnut, D. R. (1996), Geologic framework for the coal-bearing rocks of the Central Appalachian Basin, Int. J. Coal Geol., 31, 5566.
  • Condon, D., et al. (2007), EARTHTIME: Isotopic tracers and optimized solutions for high-precision U-Pb ID-TIMS geochronology, Eos Trans. AGU, 88(52), Fall Meet. Suppl., Abstract V41E–06.
  • Cozar, P., et al. (2008), Late Visean-Serpukhovian foraminiferans and calcareous algae from the Adarouch region (central Morocco), North Africa, Geol. J., 43(4), 463485, doi:10.1002/gj.1119.
  • Davydov, V. I. (1986), Precise definition of the Carboniferous-Permian boundary in Donets Basin and the northern Caucasus based on paleomagnetic criteria, Sov. Geol., no. 12, 7476.
  • Davydov, V. I. (1990), Zonal fusilinid subdivisions of Gzhelian in Donets Basin and Pre-Donets Trough, in Problems of Modern Micropaleontology, pp. 5269, Nauka, Saint Petersburg, Russia.
  • Davydov, V. I. (1992), Subdivision and correlation of Upper Carboniferous and Lower Permian deposits in Donets Basin according to fusulinid data (in Russian), Sov. Geol., no. 5, 5361.
  • Davydov, V. I. (1997), Middle/Upper Carboniferous boundary: The problem of definition and correlation, in Proceeding of the XIII International Congress on the Carboniferous and Permian, edited by M. Podemski et al., pp. 113122, Pol. Geol. Inst., Warsaw.
  • Davydov, V. I. (2009), Bashkirian-Moscovian transition in Donets Basin: The key for Tethyan-Boreal correlation, in The Carboniferous Type Sections in Russia, Potential and Proposed Stratotypes: Proceedings of the International Conference, pp. 188192, Inst. of Geol., Bashkirian Acad. of Sci., Ufa, Russia.
  • Davydov, V. I., and R. Khodjanyazova (2009), Moscovian-Kasimovian transition in Donets Basin: Fusulinid taxonomy, biostratigraphy correlation and paleobiogeography, in The Carboniferous Type Sections in Russia, Potential and Proposed Stratotypes: Proceedings of the International Conference, pp. 193196, Inst. of Geol., Bashkirian Acad. of Sci., Ufa, Russia.
  • Davydov, V. I., and A. V. Popov (1991), The Carboniferous system (in Russian), in Zonal Stratigraphy of the Phanerozoic of the U.S.S.R., pp. 6476, Nedra, Moscow.
  • Davydov, V. I., et al. (1992), The Carboniferous-Permian boundary in the former USSR and its correlation, Int. Geol. Rev., 34(9), 889906, doi:10.1080/00206819209465643.
  • Davydov, V. I., et al. (2004), The Carboniferous period, in A Geologic Time Scale 2004, edited by F. M. Gradstein et al., pp. 222248, Cambridge Univ. Press, Cambridge, U. K.
  • Davydov, V. I., et al. (2008), Faunal assemblage and correlation of Kasimovian-Gzhelian transition at Usolka section, southern Urals, Russia (a potential candidate for GSSP to define base of Gzhelian Stage), Stratigraphy, 5(2), 113135.
  • Devuyst, F.-X., and J. Kalvoda (2007), Early evolution of the genus Eoparastaffella (Foraminifera) in Eurasia; the “interiecta group” and related forms, late Tournaisian to early Visean (Mississippian), J. Foraminiferal Res., 37(1), 6989, doi:10.2113/gsjfr.37.1.69.
  • Devuyst, F.-X., et al. (2003), A proposed global stratotype section and point for the base of the Visean Stage (Carboniferous): The Pengchong Section, Guangzi, south China, Episodes, 26(2), 105115.
  • Dickinson, W. R., et al. (1994), Glacio-eustatic origin of Permo-Carboniferous stratigraphic cycles; evidence from the southern Cordilleran foreland region, in Concepts in Sedimentology and Paleontology, vol. 4, edited by J. M. Dennison, and F. R. Ettensohn, pp. 2534, Soc. for Sediment. Geol., Tulsa, Okla.
  • Ellison, S. P.Jr. (1941), Revisions of Pennsylvanian conodonts, J. Paleontol., 15, 107143.
  • Fisunenko, O. P. (2000), On the Problem of the Moscovian Stage, 115 pp., Lugansk Pedagogical Inst., Lugansk, Ukraine.
  • Fohrer, B., et al. (2007), The Pennsylvanian (Moscovian) Izvarino section, Donets Basin, Ukraine: A multidisciplinary study on microfacies, biostratigraphy (conodonts, foraminifers, and ostracodes), and paleoecology, J. Paleontol., 81(5), 185.
  • Gastaldo, R. A., et al. (2009), Ecological persistence in the Late Mississippian (Serpukhovian -Namurian A) megafloral record of the Upper Silesian Basin, Czech Republic, Palaios, 24(6), 336350, doi:10.2110/palo.2008.p08-084r.
  • Gavrish, V. K. (Ed.) (1989), Geology and Oil and Gas Potential of the Dniepr-Donets Depression, Depth Structure and Geotectonic Evolution (in Russian), 208 pp., Nauk. Dumka, Kiev.
  • Gerstenberger, H., and G. Haase (1997), A highly effective emitter substance for mass spectrometric Pb isotope ratio determinations, Chem. Geol., 136, 309312, doi:10.1016/S0009-2541(96)00033-2.
  • Goreva, N. V., and A. S. Alekseev (2007), Correlation of upper Carboniferous (Pennsylvanian) deposits in the Moscow Syneclise and Donets Basin by conodonts, in Paleontological Investigations in Ukraine: History, Current Status and Perspectives, edited by P.F. Gozhik et al., pp. 110114, Nauk. Dumka, Kiev.
  • Grozdilova, L. P. (1966), Foraminifery verkhnego karbona severnogo Timana (Foraminifera of the upper Carboniferous of the northern Timan range), in Trudy Vsesoyuznogo Neftyanogo Nauchno-Issledovatel'skogo Geologorazvedochnogo Instituta, pp. 254331, Nedra, Leningrad.
  • Haq, B. U., and S. R. Schutter (2008), A chronology of Paleozoic sea-level changes, Science, 322(5898), 6468, doi:10.1126/science.1161648.
  • Heckel, P. H. (1986), Sea-level curve for Pennsylvanian eustatic marine transgressive-regressive depositional cycles along midcontinent outcrop belt, North America, Geology, 14(4), 330334, doi:10.1130/0091-7613(1986)14<330:SCFPEM>2.0.CO;2.
  • Heckel, P. H. (1994), Evaluation of evidence for glacio-eustatic control over marine Pennsylvanian cyclothems in North America and consideration of possible tectonic events, in Concepts in Sedimentology and Paleontology, edited by J. M. Dennison, and F. R. Ettensohn, pp. 6587, Soc. for Sediment. Geol., Tulsa, Okla.
  • Heckel, P. H. (2002), Overview of Pennsylvanian cyclothems in midcontinent North America and brief summary of those elsewhere in the world, Can. Soc. Pet. Geol. Mem., 19, 7998.
  • Heckel, P. H. (2008), Pennsylvanian cyclothems in midcontinent North America as far-field effects of waxing and waning of Gondwana ice sheets, Spec. Pap. Geol. Soc. Am., 441, 275289.
  • Heckel, P. H., et al. (2007), Cyclothem [“digital”] correlation and biostratigraphy across the global Moscovian-Kasimovian-Gzhelian stage boundary interval (Middle-Upper Pennsylvanian) in North America and eastern Europe, Geology, 35(7), 607610, doi:10.1130/G23564A.1.
  • Heckel, P. H., et al. (2008), Choice of conodont Idiognathodus simulator (sensu stricto) as the event marker for the base of the global Gzhelian stage (Upper Pennsylvanian series, Carboniferous system), Episodes, 31(3), 319325.
  • Hess, J. C., and H. J. Lippolt (1986), 40Ar/39Ar ages of tonstein and tuff sanidines: New calibration points for the improvement of the Upper Carboniferous time scale, Chem. Geol., 59, 143154.
  • Hess, J. C., et al. (1999), High-precision 40Ar/39Ar spectrum dating on sanidine from the Donets Basin, Ukraine: Evidence for correlation problems in the Upper Carboniferous, J. Geol. Soc., 156, 527533, doi:10.1144/gsjgs.156.3.0527.
  • Inosova, K. I., et al. (1976), Atlas of Microspores and Pollen of the Upper Carboniferous and Lower Permian of the Donets Basin, 334 pp., Nedra, Moscow.
  • Isakova, T. N., and K. Ueno (2007), About lectotype Rauserites rossicus (Schellwien) 1908 [Foraminifera] from the Gzhelian stage of the Donets and Moscow basins, in Zbirnik Naukovikh Prats Institutu Geologichnikh Nauk NAN Ukraini: Biostratigraphy and Paleontology, pp. 105109, Nauk. Dumka, Kiev.
  • Ivanova, E. A., and I. V. Khvorova (1955), Stratigraphy of the Middle-Upper Carboniferous of the Western Part of the Moscow Syneclise, 279 pp., Russ. Acad. of Sci., Moscow.
  • Izart, A., et al. (1996), Stratigraphy and sequence stratigraphy of the Moscovian in the Donets Basin, Tectonophysics, 268(1–4), 189209, doi:10.1016/S0040-1951(96)00224-7.
  • Izart, A., et al. (2002), Sequence stratigraphy of the Serpukhovian, Bashkirian and Moscovian in Gondwanaland, western and eastern Europe and USA, Can. Soc. Pet. Geol. Mem., 19, 144157.
  • Izart, A., et al. (2003), Sequence stratigraphy and correlation of Late Carboniferous and Permian in the CIS, Europe, Tethyan area, North Africa, Arabia, China, Gondwanaland and the USA, Palaeogeogr. Palaeoclimatol. Palaeoecol., 196(1–2), 5984, doi:10.1016/S0031-0182(03)00313-4.
  • Izart, A., et al. (2006), Stratigraphic distribution of macerals and biomarkers in the Donets Basin: Implications for paleoecology, paleoclimatology and eustacy, Int. J. Coal Geol., 66(1–2), 69107, doi:10.1016/j.coal.2005.07.002.
  • Jaffey, A. H., et al. (1971), Precision measurement of half-lives and specific activities of 235U and 238U, Phys. Rev. C, 4, 18891906, doi:10.1103/PhysRevC.4.1889.
  • Kabanov, P. B., et al. (2006), Biotic changes in a eustatic cyclothem: Domodedovo Formation (Moscovian, Carboniferous) of Peski quarries, Moscow region, Paleontol. J., 40(4), 351368, doi:10.1134/S0031030106040010.
  • Kagarmanov, A. K., and L. M. Donakova (1990), Carboniferous system, in Decisions of the Regional Stratigraphic Conference on the Middle and Upper Paleozoic of the Russian Platform, edited by A. K. Kagarmanov, and L. M. Donakova, pp. 195, Nedra, Saint Petersburg, Russia.
  • Khodjanyazova, R., and V. I. Davydov (2008), Late Paleozoic foraminiferal diversity record in Donets Basin, Ukraine as a proxy of global climate dynamics, Geol. Soc. Am. Abstr. Programs, 40(6), 259.
  • Kireeva, G. D. (1951), Stratigraficheskoe polozhenie moskovskogo yarusa v razreze Donetskogo basseyna (na osnove raspredeleniya fuzulinidy), Byull. Mosk. Ova, Ispyt. Prir. Otd. Geol., 26(3), 3551.
  • Klein, G. d., and D. A. Willard (1989), Origin of the Pennsylvanian coal-bearing cyclothems of North America, Geology, 17(2), 152155, doi:10.1130/0091-7613(1989)017<0152:OOTPCB>2.3.CO;2.
  • Klein, G. d. (1990), Pennsylvanian time scales and cycle periods, Geology, 18(5), 455457, doi:10.1130/0091-7613(1990)018<0455:PTSACP>2.3.CO;2.
  • Kozitskaya, R. I., et al. (1978), Konodonty karbona Donetskogo Basseyna (Conodonts From the Carboniferous of the Donets Basin), 138 pp., Nauk. Dumka, Kiev.
  • Krogh, T. E. (1973), A low-contamination method for hydrothermal decomposition of zircon and extraction of U and Pb for isotopic age determinations, Geochim. Cosmochim. Acta, 37(3), 485494, doi:10.1016/0016-7037(73)90213-5.
  • Kuiper, K. F., et al. (2008), Synchronizing rock clocks of Earth history, Science, 320(5875), 500504, doi:10.1126/science.1154339.
  • Kulagina, E. I., et al. (2006), The Dombar Limestone in the south Urals and the Visean-Serpukhovian boundary, Newsl. Carboniferous Stratigr., 24, 911.
  • Kullmann, J., et al. (2008), Goniatites et conodontes du Viseen/Serpukhovien dans les Pyrenees centrales et occidentales, France (Visean/Serpukhovian goniatites and conodonts from the central and western Pyrenees, France), Geobios, 41(5), 635656, doi:10.1016/j.geobios.2007.09.003.
  • Lebedev, N. I. (1924), Materials for Donets Basin geology (in Russian), News Ekaterinoslav Min. Inst., 14(2), 1114.
  • Levenshtein, M. L. (1963), Synonymic of coals and limestone in Donets Basin, in Ugolnye basseiny i mestorozhdeniya yuga Evropeiskoi chasti SSSR (Donetskii bassein, Dneprovskii bassein, Lvovsko-Volynskii bassein, mestorozhdeniya zapadnykh oblastei Ukrainy i Moldavii, Belorussii, severnogo Kavkaza i Zakavkazya), edited by I. A. Kuznetsov, pp. 4556, Gosgeolizdat, Moscow.
  • Ludwig, K. R. (2003), User's manual for Isoplot 3.00, 70 pp., Berkeley Geochronol. Cent, Berkeley, Calif.
  • Lutugin, L. I., and P. I. Stepanov (1913), Donets coal basin, in Coal Minings in Russia, pp. 112143, Geol. Comm., Saint Petersburg, Russia.
  • Makhlina, M. K., et al. (1979), Stratigraphy, biostratigraphy and paleogeography of Upper Carboniferous of the Moscow Syneclise (in Russian), in Stratigraphy, Paleontology and Paleogeography of Carboniferous of the Moscow Syneclise. Transactions of Geological Foundation of Ministry of Geology of Russian Federation, edited by M. K. Makhlina, and C. M. Shik, pp. 2569, Geol. Found. of Russ. Fed., Moscow.
  • Makhlina, M. K., et al. (2001), Sredniy karbon Moskovskoy sineklizy (yuzhnaya chast'); v 2 tomakh, vol. 1, Stratigrafiya (Middle Carboniferous of Southern Moscow Syneclise, vol. 1, Stratigraphy), 244 pp., Rossiyskaya Akad. Nauk, Paleontol. Inst., Moscow.
  • Mattinson, J. M. (2005), Zircon U-Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages, Chem. Geol., 220, 4766, doi:10.1016/j.chemgeo.2005.03.011.
  • Menning, M., et al. (2006), Global time scale and regional stratigraphic reference scales of central and west Europe, east Europe, Tethys, south China, and North America as used in the Devonian-Carboniferous-Permian Correlation Chart 2003 (DCP 2003), Palaeogeogr. Palaeoclimatol. Palaeoecol., 240(1–2), 318372, doi:10.1016/j.palaeo.2006.03.058.
  • Milanovsky, E. E. (1992), Aulacogens and aulacogeosynclines: Regularities in setting and evolution, Tectonophysics, 215(1–2), 5568, doi:10.1016/0040-1951(92)90074-G.
  • Min, K., et al. (2000), A test for systematic errors in 40Ar/39Ar geochronology through comparison with U/Pb analysis of a 1.1-Ga rhyolite, Geochim. Cosmochim. Acta, 64(1), 7398, doi:10.1016/S0016-7037(99)00204-5.
  • Montanez, I. P., et al. (2007), CO2-forced climate and vegetation instability during late Paleozoic deglaciation, Science, 315(5808), 8791, doi:10.1126/science.1134207.
  • Mundil, R., et al. (2004), Age and timing of the end Permian mass extinctions: U/Pb geochronology on closed-system zircons, Science, 305, 17601763, doi:10.1126/science.1101012.
  • Nemirovskaya, T. I., et al. (1990), The Kal'mius section, Donbass, Ukraine, U.S.S.R.: A Soviet proposal for the Mid-Carboniferous boundary stratotype, Courier Forsch. Senckenberg, 130, 247272.
  • Nemirovskaya, T. I., et al. (1994), Lochriea ziegleri and Lochriea senckenbergica—New conodont species from the latest Visean and Serpukhovian in Europe, Courier Forsch. Senckenberg, 168, 311317.
  • Nemyrovska, T. I. (1999), Bashkirian conodonts of the Donets Basin, Ukraine, Scr. Geol., 119, 1115.
  • Nemyrovska, T. I., et al. (1999), On Moscovian (Late Carboniferous) conodonts of the Donets Basin, Ukraine, Neues Jahrb. Geol. Palaeontol. Abh., 214(1–2), 169194.
  • Nikitin, S. N. (1890), Kamennougol'nye otlozheniya podmoskovnogo kraya i artesianskie vody pod Moscvoi (Carboniferous Deposits of Moscow Basin and Artesian Water Around Moscow), 138 pp., Geol. Comm. of Russ., Saint Petersburg.
  • Nikolaeva, S. V., L. Z. Akhmetshina, V. A. Konovalova, V. F. Korobkov, and G. F. Zainakaeva (2009), The Carboniferous carbonates of the Dombar Hills (western Kazakhstan) and the problem of the Viséan-Serpukhovian boundary, Palaeoworld, 18(2–3), 8093.
  • Pazukhin, V. N., A. S. Aleksev, N. V. Goreva, and E. I. Kulagina (2006), Discovery of potential Bashkirian-Moscovian boundary marker conodont Declinognathodus donetzianus in south Urals, Newsl. Carboniferous Stratigr., 24, 1819.
  • Poletaev, V. I. (1981), Lithostratigraphic Subdivisions the Carbonate Sequences of Lower Carboniferous in Donets Basin, 49 pp., Geol. Inst., Ukrainian Acad. of Sci., Kiev.
  • Poletaev, V. I., et al. (1991), Local zones and major Lower Carboniferous biostratigraphic boundaries of the Donets Basin (Donbass), Ukraine, U.S.S.R. Courier Forsch. Senekenberg, 130, 4759.
  • Popov, A. V. (1979), Kamennougol'nyye ammonoidei Donbassa i ikh stratigraficheskoye znacheniye (Carboniferous Ammonoidea of the Donets Basin and Their stratigraphic significance), Tr. Vses. Ordena Lenina Nauchno Issled. Geol. Inst. im A.P. Karpinskogo, Novaya Ser., 220, 106 pp.
  • Poty, E., et al. (2006), Upper Devonian and Mississippian foraminiferal and rugose coral zonations of Belgium and northern France: A tool for Eurasian correlations, Geol. Mag., 143(6), 829857, doi:10.1017/S0016756806002457.
  • Poulsen, C. J., et al. (2007), Late Paleozoic tropical climate response to Gondwanan deglaciation, Geology, 35(9), 771774, doi:10.1130/G23841A.1.
  • Putrja, F. S. (1948), Protriticites—A new genus of fusulinids (in Russian), Trans. L'vov Geol. Soc., Ser. Paleontol., 1, 8996.
  • Ramezani, J., et al. (2007), High-precision U-Pb zircon age constraints on the Carboniferous-Permian boundary in the southern Urals stratotype, Earth Planet. Sci. Lett., 256(1–2), 244257, doi:10.1016/j.epsl.2007.01.032.
  • Rasbury, E. T., et al. (1998), U-Pb dates of paleosols: Constraints on late Paleozoic cycle durations and boundary ages, Geology, 26, 403406, doi:10.1130/0091-7613(1998)026<0403:UPDOPC>2.3.CO;2.
  • Rauser-Chernousova, D. M. (1941), New Upper Carboniferous stratigraphic data from the Oksko-Tsninskyi Dome (in Russian), Rep. Acad. Sci. USSR, 30(5), 434436.
  • Rauser-Chernousova, D. M., and E. A. Reitlinger (1954), Biostratigraphic distribution of foraminifers in Middle Carboniferous depositis of southern limb of Moscow Syneclise (in Russian), in Regional Stratigraphy of the U.S.S.R., vol. 2, Stratigraphy of Middle Carboniferous Deposits of Central and Eastern Parts of Russian Platforms (Based on Foraminifers Study). 1. Moscow Syneclise, edited by D. V. Nalivkin, and V. V. Menner, Tr. Akad. Nauk SSSR Geol. Inst., 7120.
  • Renne, P. R., et al. (1998), Intercalibration of standards, absolute ages and uncertainties in 40Ar/39Ar dating, Chem. Geol., 145, 117152, doi:10.1016/S0009-2541(97)00159-9.
  • Ritter, S. M. (1995), Upper Missourian-Lower Wolfcampian (Upper Kasimovian-Lower Asselian) conodont biostratigraphy of the midcontinent, USA, J. Paleontol., 69, 11391154.
  • Ross, C. A., and J. R. P. Ross (1988), Late Paleozoic transgressive-regressive deposition, in Sea-Level Changes—An Integrated Approach, edited by C. K. Wilgus et al., Spec. Publ. Soc. Econ. Paleontol. Mineral., 42, 227247.
  • Rotai, A. P. (1975), Donets Basin (in Russian), in Main Features of Carboniferous of USSR, edited by A. P. Rotai, pp. 80101, Nauka, Saint Petersburg, Russia.
  • Rozovskaya, S. E. (1950), Rod Triticites, ego razvitie i stratigraficheskoe znachenie (Triticites Genus: Its Evolution and Stratigraphic Significance), 80 pp., Tr. Paleontol. Inst., 26, 80 pp.
  • Savchuk, S. V. (1957), K voprosu o promyshlennoi klassifikatsii nizhnekarbonovykh uglei Donbassa, Izv. Dnepropetr. Gorn. Inst., 29, 4765.
  • Schellwien, E. (1908), Monographie der Fusulinen. Tell I: Die Fusulinen des russisch-arktischen Meeresgebietes, Palaeontographica, 55, 145194.
  • Schmitz, M. D., and B. Schoene (2007), Derivation of isotope ratios, errors, and error correlations for U-Pb geochronology using 205Pb-235U- (233U)-spiked isotope dilution thermal ionization mass spectrometric data, Geochem. Geophys. Geosyst., 8, Q08006, doi:10.1029/2006GC001492.
  • Schmitz, M. D., et al. (2005), New ID-TIMS U-Pb zircon ages for the Carboniferous-Permian boundary sections of the southern Urals–Russia, Kazaskhstan, Geochim. Cosmochim. Acta, 69(10), suppl., 326.
  • Shchegolev, A. K. (1975), Die Entwicklung der Pflanzenbedeckung im Sueden des Europaeischen Teils der UdSSR, vom Ende des Mittelkarbons bis zum Perm; Umfang und Gliederung des oberen Karbons (Stefan) (The evolution of the vegetation in the south of the European USSR, from the end of the middle Carboniferous to the Permian: Extent and stratigraphic divisions of the upper Carboniferous or Stephanian), C. R. Congr. Int. Stratigr. Geol. Carbonifere, 4(7), 275280.
  • Shchegolev, A. K., and R. I. Kozitskaya (1984), The paleontological basis of the project of the Upper Carboniferous standard scale in the Europe and the central Asia (in Russian), in The Upper Carboniferous of the USSR, edited by V. V. Menner, and A. D. Grigor'yeva, pp. 107113, Nauka, Moscow.
  • Skompski, S., et al. (1995), Conodont distribution across the Viséan/Namurian boundary, Courier Forsch. Senckenberg, 188, 177209.
  • Somerville, I. D. (2008), Biostratigraphic zonation and correlation of Mississippian rocks in western Europe: Some case studies in the late Visean/Serpukhovian, Geol. J., 43(2–3), 209240, doi:10.1002/gj.1097.
  • Soreghan, G. S., and W. R. Dickinson (1994), Generic types of stratigraphic cycles controlled by eustasy, Geology, 22(8), 759761, doi:10.1130/0091-7613(1994)022<0759:GTOSCC>2.3.CO;2.
  • Soreghan, G. S., and K. A. Giles (1999), Amplitudes of Late Pennsylvanian glacioeustasy, Geology, 27(3), 255258, doi:10.1130/0091-7613(1999)027<0255:AOLPG>2.3.CO;2.
  • Stovba, S. M., and R. A. Stephenson (1999), The Donbas Foldbelt: Its relationships with the uninverted Donets segment of the Dniepr-Donets Basin, Ukraine, Tectonophysics, 313(1–2), 5983, doi:10.1016/S0040-1951(99)00190-0.
  • Stovba, S. M., et al. (1996), Structural features and evolution of the Dnieper-Donets Basin, Ukraine, from regional seismic reflection profiles, Tectonophysics, 268, 127147, doi:10.1016/S0040-1951(96)00222-3.
  • Tschernyshev, F. N., and L. I. Lutugin (1897), Donets Basin (in Russian), News Soc. Min. Eng., no. 11–12, 1540.
  • Vdovenko, M. V. (1954), New species of Foraminifers from the Lower Viséan of the Donets Basin (in Russian), Sci. Notes Kiev Univ., 13(4), 6376.
  • Vdovenko, M. V. (2001), Atlas of foraminifera from the upper Visean and lower Serpukhovian (Lower Carboniferous) of the Donets Basin (Ukraine), Abh. Ber. Nat., 23, 93178.
  • Vdovenko, M. V., et al. (1990), An overview of Lower Carboniferous biozones of the Russian Platform, J. Foraminiferal Res., 20(3), 184194, doi:10.2113/gsjfr.20.3.184.
  • Villa, E. and the Task Group (2008), Progress Report of the Task Group to establish the Moscovian-Kasimovian and Kasimovian-Gzhelian boundaries, Newsl. Carboniferous Stratigr., 26, 1213.
  • Villeneuve, M., et al. (2000), A method for intercalibration of U-Th-Pb and 40Ar-39Ar ages in the Phanerozoic, Geochim. Cosmochim. Acta, 64(23), 40174030, doi:10.1016/S0016-7037(00)00484-1.
  • Wang, Z., et al. (2007), Conodont sequence across Bashkirian-Moscovian boundary in the Nashui Section, Luodian, Guizhou, south China, J. Stratigr., 31(1), 102103.
  • Wanless, H. R., and F. P. Shepard (1936), Sea level and climatic changes related to late Paleozoic cycles, Geol. Soc. Am. Bull., 47(8), 11771206.
  • Wardlaw, B. R., et al. (2004), The Permian period, in A Geologic Time Scale 2004, edited by F. M. Gradstein et al., pp. 249270, Cambridge Univ. Press, Cambridge, U. K.
  • Zaritskiy, P. V. (1977), Kaolinite partings in coal of the Donets Basin, Lithol. Miner. Resour., 12(6), 725729.
  • Zhemchuzhnikov, Y. A., and V. S. Yablokov (1956), Fatsialno-tsiklicheskii metod izucheniya uglenosnykh otlozhenii (in Russian), Tr. Lab Geol. Uglya Akad. Nauk SSSR, 5, 161170.