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The Asturian and Cantabrian floral assemblages with Cordaites from the Plzeň Basin (Czech Republic)

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EN
The macrofloras of the Nýřany Member (late Asturian - early Cantabrian age) were studied at five localities and two boreholes in the Plzeň Basin (Western Bohemia). The floras were mostly dominated by Cordaites, and seven species were recognised based mainly on cuticular evidence. Cordaites dobranensis Šimůnek was the most common species and occurred in most of the Asturian-age localities. In addition, an outcrop near Heřmanova Huď yielded C. blazkovicensis Šimůnek, C. wilkischensis Šimůnek and C. pilsensis Šimůnek; and borehole Krašovice Kš 1 yielded C. krasovicensis Šimůnek and C. touskovensis Šimůnek. Cordaites radcicensis nov. sp. was only found in the Cantabrian part of the succession, at the Radčice locality, and shows characters suggesting adaptation to somewhat drier conditions, namely thick cutinisation and proximally oriented projection of the anticlinal cell walls. The most diversified assemblage with 29 species was found at the Dobřany locality, but most other localities yielded only 12 to 18 species. The species-spectrum of individual localities varied according to type of locality, sedimentology and method of collecting. In most localities, cordai- taleans made up 40 to 67% of the macroflora, the only notable exception being the Krimich II mine at Tlučná that yielded only 5% cordaitaleans. The next important plant group was the sphenopsids, which usually comprised about 30% of the macrofloras, with the exception of Heřmanova Huď locality where there were only 3% sphenopsids. The proportion of fern remains varied between localities from 8 to 35%. Lycopsids were usually very rare, except at the Heřmanova Huď locality where 30% of the flora consisted of allochthonous lycopsid fragments. Pteridosperms were very rare and never exceeded 10% of the macroflora. The Westphalian rain forest was not monotonous, but was diversified into several floral assemblages. My work supports the conclusion of previous workers in the area (Šetlík, 1980), that the five most common species in the Nýřany Member of the Plzeň Basin are Pecopteris polypodioides (Presl in Sternberg) Němejc, Sphenophyllum emarginatum (Brongniart) Brongniart, Pecopteris unita, Dicksonites plukenetii and Annularia stellata (Schlotheim) Wood.
Rocznik
Tom
Strony
51--80
Opis fizyczny
bibliogr. 37 poz., fot., tab., wykr.
Twórcy
autor
  • Czech Geological Survey, Klárov 3, 118 21 Praha 1, Czech Republic
Bibliografia
  • Behrensmeyer, A. K., Damuth, J. D., DiMichele, W. A., Potts R. Sues, H.-D. & Wing, S. L., 1992. Terrestrial ecosystems through time. Evolution ary paleoecology of Terrestrial plants and animals. The Universityof Chicago Press, 568 pp. Chicago and London.
  • Cleal, C. J., Dimitrova, T. Kh. & Zodrow, E. L., 2003. Macrofloral and palynological criteria for recognising the Westphalian - Stephanian boundary. News letters on Stratigraphy, 39: 181-208.
  • Čtveráček, B., 1984. Geologická stavba karbonu mezi Radčicemi a Plzní v plzeòské pánvi (Geology of the Carboniferous between Radčice and Plzeòin the Plzeò Basin), Diplomathesis, Charles University, 59 p. Praha.
  • Drábková, J., Lojka, R. & Šimùnek, Z., 2005. Paleoekologie a biostratigrafie jemnozrnných poloh de file u Radčic, Kantábr, Plzeòská pánev (Palaeoecology and biostratigraphy of the fine-grained deposits from the Radčice section, Cantabrian, Plzeò Basin - in Czech). Geoscience Research Reports for 2004: 30-33.
  • Feistmantel, O., 1870. Ueber Pflanzenpetrefacte aus dem Nürschaner Gasschiefer, sowie seine Lagerung und sein Verhältnis zu den übrigen Schichten. Sitzunsberichte der Königl. Böhmischen Gesellschaft der Wissenschaften in Prag, 12: 56-73.
  • Franke, F. 1912. Beiträge zur Kenntnis der paläozoischen Arten von Alethopteris und Callipteridium. Inaugural-Disertation, Philosophischen Fakultät, Friedrich-Wilhelms-Universität zu Berlin, 123 pp.
  • Gastaldo, R. A., 1996. Flöznah and Flözfern assemblages: potential predictors of Late Carbon iferous biome replacement. Patterns in Paleobotany, Proceedings of a Czech-U.S. Carboniferous Palaeobotany Workshop. In: R. L. Leary (ed.), Illinois State Museum Scientific Papers, 26: 19-27.
  • Gastaldo, R. A., Pfefferkorn, H. W. & DiMichele, W. A., 1995. Taphonomic and sedimentologic characterisation of roof-shale floras. In: P. Lyons, R. H. Wagner & E. Morey (eds), Historical perspective of early twentieth century Carboniferous paleobotany in North America. Geological Society of America Memoir 185: 341-350.
  • Kalibová-Kaiserová, M., 1964. Výzkum megaspor oblasti mezi Všeruby, Horní Bìlou, Horní Boízoua Chotíkovem v severní části plzeòské kamenouhelné pánve (Megasporenforschung im Gebiet zwischen Všeruby, Horní Bìlá, Horní Boíza und Chotíkov im Nördlichen Teil des Pilsener-Steinkohlenbeckens, Plzeò - in Czech, German summary). Časopis pro mineralogii a geologii, 8: 151-158.
  • Kerp, H., 1990. The study of fossil gymnosperms by means of cuticu ar analysis. Palaios, 5: 548-549.
  • Korous, K. & Zelenka, R., 1981. Západočeské uhelné doly Zbùch, Dùl Ant. Uxa-Tlučná, Vrtné profily. (West Bohemian Coal Mines Zbùch, Tlučná, Ant.Uxa Coal Mine, Borehole logs - in Czech). Mining Archive ZUD, Zbùch.
  • Leary, R. L. & Pfefferkorn, H. W., 1977. An Early Pennsylvanian flora with Megalopteris and Noeggerathiales from West-Central Illinois. Illinois State Geological Survey Circular, 500: 1-77. Urbana.
  • Mergl, M. & Vohradský, O., 2000. Vycházky za geologickými zajímavostmi Plznì a okolí (Trips to Geological interests of Plzeò and surrounding - in Czech). KOURA publishing - Ludìk Bartoš, Mariánské Láznì: 1-270.
  • Nìmejc, F., 1929. O nìkterých nových nálezech ve stoedočeských uhelných pánvích (On some discoveries of fossil plant remains in the Carboniferous district of Central Bohemia, II - in Czech, English summary). Rozpravy II. toídy České akademie (Bulletin International de l'Academie des Sciences de Boheme), 39 (33): 1-8 (1-8).
  • Nìmejc, F., 1933. Stratigrafické výzkumy konané z hlediska paleobotanického v uhelných revírech jižní části plzeòské kamenouhelné pánve v letech 1928-1932 (Stratigraphical research made from palaeobotanical point of view in the coal districts of the Southern part of the Plzeò Basin in years 1928-1932 - in Czech, English summary). Hornický vìstník, 14 (1932): 1-20.
  • Nìmejc, F., 1937. O stratigrafické poíslušnosti uhelné sloje v oblasti mezi Rochlovou, Poehýšovem, Vlkýší a Heomanovou Hutí (On the stratigraphical level of the coal measure in the region between Rochlová, Poehýšov, Vlkýše and Heomanova Huï - in Czech, English summary). Vìstník Státního Geologického ústavu, 13 (6): 278-283.
  • Nìmejc, F., 1941. Paleontologicko-stratigrafické poíspìvky k poznání uhelných revírù severovýchodního okraje plzeòské uhelné pánve (Paläontologisch-stratigrapische Beiträge zur Kenntnis der Kohlereviere am Nordostrande des Pilsener Permokarbonbeckens - in Czech, German summary). Zprávy Geologického ústavu pro Čechy a Moravu (Mitteilungen der geologischen Anstalt für Böhmen and Mähren). 17: 184-214.
  • Nìmejc, F., 1953. Úvod do floristické stratigrafie kamenouhelných oblastí ČSR. (An introduction to the floral Stratigraphy of the bituminous coal regions of the CSR - in Czech), Academia, Praha, 173 pp.
  • Nìmejc, F., 1958. Biostratigrafické studie v plzeòské pánvi (Studies in the biostratigraphy of the Plzeò Coal Basin). Rozpravy Československé akademie vìd, Oada matematických a poírodních vìd. 68 (4): 1-58.
  • Opekar, L. et al., 1994. Kaznìjov - Hydrogeologický prùzkum. Kaznìjov (Hydrogeological exploration - in Czech). MS. Archiv Geofond, Praha.
  • Opluštil, S., 2005. Peat-forming plant assemblages of volcanoclastics of the Radnice Basin. Excursion Guide, The 16th International Plant Taphonomy Meeting, Plzeò, Septem ber 2005: 3-13.
  • Opluštil, S., Martínek, K. & Tasáryová, Z. 2005. Facies and architectonical analysis of fluvial deposits of the Nýoany Member and the Týnec Formation (Westphalian D-Barruelian) in the Kladno-Rakovník and Pilsen basins. Bulletin of Geosciences, 80 (1) 45-66.
  • Opluštil, S., Pšenička, J., Libertín, M. & Šimùnek, Z., 2007. Vegetation patterns of Westphalian and Lower Stephanian mire assemblages preserved in tuff beds of the continental basins of Czech Republic. Review of Palaeobotany and Palynology, 143: 107-154.
  • Pešek, J., 1975. Notes on the geology of Plzeò Carboniferous of the Dobré štìstí Mine. Acta Universitatis Carolinae - Geologica, 2: 139-147.
  • Pešek, J., 1994. Carboniferous of Central and Western Bohemia. Czech Geological Survey, Prague, 1-64.
  • Purkynì, C., 1913. Geologie Okresu Plzeòského (Geology of the Plzeò County - in Czech). Okresní Výbor v Plzni, Plzeò: 140 pp.
  • Remy, W. & Remy, R. 1975. Lesleya weillerbachensis n. sp. aus dem höheren Westphal C des Saar-Karbons. Argumenta Palaeobotanica 4: 1-11.
  • Salisbury, E. J., 1928. On the causes and ecolog ical significance of stomatal frequency, with Special reference to the Wood land Flora. Philosophical Transactions of the Royal Society of London, Series B, 216: 1-65.
  • Šetlík, J., 1968: Fytopaleontologie nýoanských vrstev (Palaeobotany of the Nýoany Member - in Czech). MS archiv ČGS, Praha: 43 pp.
  • Šetlík, J., 1980. Makrofytopaleontologie (Macrophytopalaeontology - in Czech). In: Malán O. et al. Plzeòská pánev - černé uhlí - studie (Plzeò Basin - bituminous coal - a study - in Czech). MS Geofond. Praha.
  • Šimùnek, Z., 1994. Megaflora of tuffaceous interbeds in coal seams of the Nýoany Mem ber (Westphalian D) at the Dobré štìstí Mine in the Plzeò Basin (Czech Republic). Vìstník Českého Geologického ústavu, 69 (2): 31-41.
  • Šimùnek, Z., 2007. New classification of the genus Cordaites from the Carboniferous and Permian of the Bohemian Massif based on micromorphology of its cuticle. Acta Musei nationalis, Pragae, Series B., Historia Naturalis, 62 (3-4): 97-210.
  • Vávra, J., 1988. Zpráva o výsledcích geologicko-prùzkumných prací - úkol Nýoany-Tesla (Report on re sults of the geology-explorational work, Task Nýoany-Tesla - in Czech). Stavební geologie, n.p. MS archiv Geofond, Praha, 25 pp. 12 supl.
  • Wagner, R. H., 1969. Proposal for the recognition of a new 'Cantabrian' Stage at the base of Stephanian Series. Compte Rendu 6e CongrÀs International de Stratigraphphie et de Géologie du Carbonifere 1967, Sheffield: 139-150.
  • Wagner, R. H. & Winkler Prins, C. F., 1985. The Cantabrian and Barruelian stratotypes: A sumary of basin development and biostratigraphic information. In: Lemos de Sousa, M. J. & Wagner, R. H. (eds), 1983. Papers on the Carboniferous of the Iberian Peninsula (Sedimentology, Stratigraphy, Palaeontology, Tectonics nad Geochronology), 64: 359-410.
  • Zeiller, R., 1899. Étude sur la flore fossile du Bassin Houiller d' Héraclée (Asie Mineure). Mémoires de la Société Géologique de France, Paléontologie. Mémoire, 21: 1-91.
  • Zodrow, E. L., Šimùnek, Z. & Bashforth, A. R., 2000. New cuticular morphotypes of "Cordaites principalis (Germar) Geinitz" from the Canadian Carboniferous Maritimes Basin. Canadian Journal of Botany, 78 (2): 135-148.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0020-0011
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