Late Visean (Mississippian) vegetation of the north-western part of Russia according to palaeobotanical and palynological data

References

• BalmeBE. 1995. Fossil in situ spores and pollen grains: an annotated catalogue. Rev Palaeobot Palynol.87:81–323.
   Web of Science ®Google Scholar
• BekJ. 2008. Late Mississippian–early Pennsylvanian (Serpukhovian–Bashkirian) miospore assemblages of Bohemian part of the Upper Silesian Basin, Czech Republic. Rev Palaeobot Palynol.152:40–57.
   Web of Science ®Google Scholar
• BekJ, LearyRL. 2012. Porostrobus nathorstii (Leary & Mickle) emend. and its spores from the Namurian of Illinois, USA. Bull Geosci.87(1):45–52.
   Web of Science ®Google Scholar
• BekJ, OpluštilS. 2004. Palaeoecological constraints of some Lepidostrobus cones and their parent plants from the Late Palaeozoic continental basins of the Czech Republic. Rev Palaeobot Palynol.131:49–89.
   Web of Science ®Google Scholar
• BekJ, PsenickaJ. 2001. Senftenbergia plumosa (Artis.) emend. and its spores from the Carboniferous of the Kladno Pilsen Basins, Bohemian Massif and some related and synonymous taxa. Rev Paleobot Palynol.116:213–232.
   Web of Science ®Google Scholar
• ByvshevaTV. 1985. Spores from deposits of the Tournaisian and Visean stages from Russian Plate. Atlas of spore and pollen of Phanerozoic oil and gas-bearing strata of the Russian and Thuranian Plates. Trans VNIGNI. 253:80–158 (In Russian).
   Google Scholar
• ChalonerWG. 1962. A Sporangiostrobus with Densoporites microspores. Paleontology.5:73–85.
   Google Scholar
• DaviesSJ, McLeanD. 1996. Spectral gamma-ray and palynological characterization of Kinderscoutian marine bands in the Namurian of the Pennine Basin. Proc Yorkshire Geol Soc.51:103–114.
   Google Scholar
• DiMicheleWA, PhillipsTL. 1985. Arborescent lycopod reproduction and paleoecology in a coal-swamp environment of Late Middle Pennsylvanian Age (Herrin Coal, Illinois, USA). Rev Paleobot Palynol.44:1–26.
   Web of Science ®Google Scholar
• DiMicheleWA, PhillipsTL. 2002. The ecology of Paleozoic ferns. Rev Paleobot Palynol.9:143–159.
   Web of Science ®Google Scholar
• DiMicheleWA, PhillipsTL, PfefferkornHW. 2006. Paleoecology of Late Paleozoic pteridosperms from tropical Euramerica. J Torrey Bot Soc.133:83–118.
   Web of Science ®Google Scholar
• EichwaldEI. 1840. Die Tier- und Planzenreste des alten Rothen Sandsteins und Bergkalks in Novogrodischen Gouvernement. Bull Sci Acad Imp Sci St-Peterb. 7:78–91.
   Google Scholar
• EichwaldEI. 1841. On fossil remains of animals and plants enclosed in ancient red sandstones and limestones which are quite widespread in Novgorod Province. Gorn Zh.1:27–53 (in Russian).
   Google Scholar
• EichwaldEI. 1860. Lethaea Rossica ou paléontologie de la Russie. Vol. 1. Stuttgart: Librairie et imprimerie de E. Schweizerbat 681 S.
   Google Scholar
• Falcon-LangHJ. 2005. Adpressed tree-fern trunks from the Early Pennsylvanian Joggins Formation of Nova Scotia. Atlantic Geol.41:169–172.
   Google Scholar
• GordenkoNV, OrlovaOA, SnigirevskySM. 2006. A new Lycopod Novgorodendron conophorum gen. et sp. nov., from the Lower Carboniferous of the Moscow syneclise. Paleontol J.40:215–223.
   Web of Science ®Google Scholar
• Gorecka-NowakA. 2002. Palynological record of palaeoclimatic changes in Late Carboniferous – an example from the Intraudetic Basin (SW Poland). Rev Paleobot Palynol.118:101–114.
   Web of Science ®Google Scholar
• Gorecka-NowakA, MajewskaM. 2003. The palynostratigraphy and palynofacies of the Namurian Walbrzych Formation in the northern part of the Intrasudetic Basin (SW Poland). In: Proceedings of the XVth international congress on Carboniferous and Permian stratigraphy. Utrecht (the Netherlands): Royal Netherlands Acad. Arts Press; p. 333–343.
   Google Scholar
• GrebSF, DiMicheleWA, GastaldoRA. 2006. Evolution and importance of wetlands in earth history. In: GrebSF, DiMicheleWA, editors. Wetlands through time. Geological Society of America. Special Paper, 399. p. 1–40.
   Google Scholar
• JagerH, McLeanD. 2008. Palynofacies and spore assemblage variations of Upper Viséan (Mississippian) strata across the southern North Sea. Rev Paleobot Palynol.148:136–153.
   Web of Science ®Google Scholar
• JasperK, Hartkopf-FröderC, FlajsG, LittkeR. 2010. Palaeoecological evolution of Duckmantian wetlands in the Ruhr Basin (western Germany): a palynological and coal petrographical analysis. Rev Paleobot Palynol.162:143–165.
   Web of Science ®Google Scholar
• KarczewskaJ. 1969. Microsporangia and pollen of Paracalathiops stachei Remy, 1953 from Chelm I bore-hole, Eastern Poland. Acta Palaeontol Pol.14(2):343–363.
   Google Scholar
• LibertínM, BekJ, DrábkováJ. 2008. Two new Carboniferous fertile sphenophylls and their spores from the Czech Republic. Acta Palaeontol Pol.53(4):723–732.
   Web of Science ®Google Scholar
• LibertinM, DaskovaJ, OplustilS, BekJ, EdressN. 2009. A palaeoecological model for a vegetated early Westphalian intramontane valley (Intra-Sudetic Basin, Czech Republic). Rev Paleobot Palynol.155:175–203.
   Web of Science ®Google Scholar
• LindstromS. 2003. Carboniferous palynology of the Loppa High, Barents Sea, Norway. Norwegian J Geol.83:333–349.
   Web of Science ®Google Scholar
• MakhlinaMKh, VdovenkoMV, AlekseevAS, ByvshevaTV, DonakovaLM, ZhulitovaVE, KononovaLI, UmnovaNI, ShickEM. 1993. Lower Carboniferous of Moscow Syneclise and Voronezh Anteclise. Moscow (Russia). (in Russian)Nauka Press.
   Google Scholar
• NaugolnykhSV, OrlovaOA. 2006. Moscvostrobus - a new genus of the Carboniferous lycopsids from the Moscow Region (Russia). Palaeobotanist.55:1–14.
   Google Scholar
• OpluštilS, BekJ, SchultkaS. 2010. Re-examination of the genus Omphalophloios White, 1898 from the Upper Silesian Coal Basin. Bull Geosci.85:39–52.
   Web of Science ®Google Scholar
• Orlova OA. 2001. Viséan Flora of the Moscow Syneclise. Extended abstract of candidate's dissertation. Moscow. 24 p. (in Russian).
   Google Scholar
• OrlovaOA, MamontovDA, SnigirevskySM. 2012. The Late Visean plant communities of the north-western wing of the Moscow syneclise. Palaezoic of Russia: regional stratigraphy, palaeontology, geo- and bioevents. Saint-Petersburg: VSEGEI; p. 167–169.
   Google Scholar
• OrlovaOA, RasskazovaNB. 2005. Age of locality of the Late Visean plants “Porog Vittsa No 2” (village of Putlino, Novgorod region) based on palynological data. In: Paleobiology and detailed stratigraphy of the Phanerozoic time. Moscow: RAEN (in Russian) p. 64–79.
   Google Scholar
• OrlovaOA, SnigirevskySM. 2003. Late Viséan Lyginopteridophytes from the Vicinity of the Town of Borovichi (Novgorod Region). 1.Calamopityales. Paleontol J.37:665–671.
   Web of Science ®Google Scholar
• OrlovaOA, SnigirevskySM. 2004. Late Viséan Lyginopteridophytes from the Vicinity of the Town of Borovichi (Novgorod Region). 2.Lyginopteridales and Medullosales. Paleontol J.38:458–464.
   Web of Science ®Google Scholar
• OrlovaOA, ZavialovaNE, Meyer-MelikyanNR. 2009. A new microsporangiate organ of the Lower Carboniferous deposits of the Novgorod Region, Russia. Paleontol J.43:1316–1329.
   Web of Science ®Google Scholar
• OshurkovaMV. 2003. Morphology, classification and description of form-genera of Late Paleozoic miospores. Sankt-Petersburg (Russia): VSEGEI Press (in Russian).
   Google Scholar
• PšeniČkaJ, BekJ, ClealCJ, WittryJ, ZodrowEL. 2009. Description of synangia and spores of the holotype of the Carboniferous fern Lobatopteris miltoni, with taxonomic comments. Rev Paleobot Palynol.155:133–144.
   Web of Science ®Google Scholar
• RaevskayaEG, ShurekovaOV. 2011. Actual technology and equipment in preparation of carbonate-terrigenous rocks for palynological analysis. Materials of 13th Russian Palynological conference “Problems of modern palynology”. Syktyvkar. Komi Institute of Geology Press; p. 103–107. (in Russian).
   Google Scholar
• SavitskyYV, KossovayaOL, VevelYA, EvdokimovaIO. 2012. Lower Carboniferous key-section of the Msta river. In: 3rd all-Russia conference «Upper Paleozoic of Russia: regional stratigraphy, paleontology, geo- and bioevents». Guidebook of pre-conference field trip. St. Petersburg. p. 18–24. (in Russian).
   Google Scholar
• SimunekZ, BekJ. 2003. Noeggerathiaceae from the Carboniferous basins of the Bohemian Massif. Rev Paleobot Palynol.125:249–284.
   Web of Science ®Google Scholar
• SnigirevskySM. 1994. Porog Vittsa. The Lower Carboniferous deposits. In: Localities of fossil plants that need protection. Proceeding of Komarov's Botanical Institute RAS; p. 59–60. (in Russian).
   Google Scholar
• VanderflitEK. 1968. Paleopalynological background of the Lower Carboniferous deposits from the north-west part of the Moscow basin. In: Paleopalynological method in stratigraphy. Proceedings of the 2nd international palynological conference; Sep 1996The Netherlands. Leningrad (USSR): VSEGEI Press; p. 11–22.
   Google Scholar
• ZalesskyMD. 1905. Plant remains from Lower Carboniferous deposits of the Msta River basin. Zap Imp Miner O-va.42:313–342. (in Russian).
   Google Scholar