PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Late Wenlock biostratigraphy and the Pristiograptus virbalensis group (Graptolithina) in Lithuania and the Holy Cross Mountains

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Graptolites from Lithuania and the Holy Cross Mountains comprise a succession of the lundgreni, parvus (except for the Holy Cross Mts.), nassa, praedeubeli, deubeli and ludensis biozones of the upper Wenlock, the parvus, praedeubeli and deubeli biozones being recognized for the first time in Lithuania, where a graptolite-free interval may also be distinguished. P. virbalensis Paskevicius, 1974 and the virbalensis group are not widely known, and are discussed here. Analysis of P. virbalensis shows this to be an independent taxon, closely related to P. auctus. There are three species - P. virbalensis, P.jaegeri and P. auctus - in the virbalensis group.
Rocznik
Strony
333--344
Opis fizyczny
fot., mapki, tab., bibliogr. 40 poz.
Twórcy
  • Department of Geology and Mineralogy, Vilnius University, M. K. Ćiurlionio 21/27, Vilnius, LT03I0I, Lithuania; Institute of Geology, University of Tartu, Vanemuise 46, Tartu 51014, Estonia, sigitas.radzevicius@gf.vu.lt
Bibliografia
  • BRAZAUSKAS A. and PASKEVICIUS J. (1981) - Correlation of the graptolitic zones with the complexes of the conodonts of the Silurian rocks in the geological section of the well Vidukle-61 (Middle Lithuania). Geologija, 2: 41-52.
  • CALNER M. and SALL E. (1999) - Transgressive oolites onlapping a Silurian rocky shoreline unconformity, Gotland, Sweden. GFF, 121 (2): 91-100.
  • CALNER M. and JEPPSSON L. (2003) - Carbonate platform evolution and conodont stratigraphy during the middle Silurian Mulde Event, Gotland, Sweden. Geol. Magaz., 140 (2): 173-2003.
  • GAILITE L., RYBNIKOVA M. and ULST R. (1967) - Stratigraphy, fauna and formation conditions of Silurian rock in the Middle Baltic State. Riga, Zinatne.
  • GAILITE L., ULST R. and JAKOVLEVA V. (1987) - Silurian stratigraphy and typical section in Latvia. Riga, Sojuzmoringeologia: 162-164.
  • HOLLAND C. H., RICKARDS R. B. and WARREN P. T. (1969) - The Wenlock graptolites of the Ludlow district, Shropshire, and their stratigraphical significance. Palaeontology, 12 (4): 663-683.
  • JAEGER H. (1991) - Neue Standard - Graptolihenzonenfolge nach der "Grossen Krise" an der Wenlock/Ludlow - Grenze (Silur)". Neues Jahrbuch fur Geologie und Palaeontologie, Abhandlungen, 182: 303-354.
  • JAWOROWSKI K. (1965) - Top of the Pasłęk Beds in the Lithuanian Depression and the Venlockian-Ludlovian boundary. Geol. Quart., 9 (3): 511-528.
  • KOREN' T. N. and URBANEK A. (1994) - Adaptive radiation of monograptids after the Late Wenlock crisis. Acta Palaeont. Pol., 39 (2): 137-167.
  • KOREN' T. N. and SUYARKOVA A. A. (1994) - Monograptus deubeli and praedeubeli (Wenlock, Silurian) in the Asian part of the former Soviet Union. Alcheringa, 18: 85-101.
  • KOZŁOWSKA-DAWIDZIUK A. (1990) - The genus Gothograptus (Graptolithina) from the Wenlock of Poland. Acta Palaeont. Pol., 35 (3-4): 191-209.
  • KOZŁOWSKA-DAWIDZIUK A. (1997) - Retiolitid graptolite Spinograptus from Poland and its membrane structures. Acta Palaeont. Pol., 42 (5): 391-412.
  • KOZŁOWSKA-DAWIDZIUK A. (1999) - Retiolitids (Graptolithina) development after Cyrtograptus lundgreni Event in the East European Platform (in Polish with English summary). Prz. Geol., 47 (4): 354-358.
  • LAPINSKAS P. (2000) - Structure and petroliferosity of the Silurian in Lithuania. Inst. Geol., Vilnius.
  • LENZ A. C. and KOZŁOWSKA-DAWIDZIUK A. (2002) - Upper Homerian (Upper Wenlock, Silurian) graptolites from Arctic Canada. J. Paleont., 76: 321-346.
  • MASIAK M., PODHALAŃSKA T. and STEMPIEŃ-SAŁEK M. (2003) - Ordovician-Silurian boundary in the Bardo Syncline, Holy Cross Mountains, Poland-new data on fossil assemblages and sedimentary succession. Geol. Quart., 47 (4): 311-330.
  • NAWROCKI J. (2000) - Late Silurian paleomagnetic pole from the Holy Cross Mountains: constraints for the post-Caledonian tectonic activity of the Trans-European Suture Zone. Earth Planet. Sc. Lett., 179: 325-334.
  • PASKEVICIUS J. (1965) - Lietuvos apatinio siluro zoninis suskirstymas. Pietn Pabaltyjo paleozojaus geologija ir naftingumas, 1: 40-49.
  • PASKEVICIUS J. (1974) - Graptolites and zonal subdivision of the Lud-low deposits in the Pribaltica (East Baltic). In: Graptolites of the USSR (ed. A. Obut ): 122-134. Novosibirsk, Nauka.
  • PASKEVICIUS J. (1979) - Biostratigraphy and graptolites of the Lithuanian Silurian. Vilnius, Mokslas.
  • PASKEVICIUS J. (1991) - Principles of integration of the Silurian grap-tolitic zones and of fauna complexes. Geologija, 12: 29-46.
  • PASKEVICIUS J. (1997) - The geology of the Baltic republics. Geol. Surv. Lithuania. Vilnius.
  • PORĘBSKA E. (1998) - Cyrtograptus lundgreni Event recorded in an upwelling sequence in the Sudetes (SW Poland). In: Proceedings of the Sixth International Graptolite Conference of the GWG (IPA) and the 1998, Field Meeting of the International Subcommision on Silurian Stratigraphy (ICS-IUGS) (eds. J. C. Gutierrez-Marco and I. Rabano). Temas Geologico-Mineros, 23: 248-251.
  • PORĘBSKA E. KOZŁOWSKA-DAWIDZIUK A. and MASIAK M. (2004) - The lundgreni event in the Silurian of the East European Platform, Poland. Palaeogeogr., Palaeoclimat., Palaeoecol., 213: 271-294.
  • PRIBYL A. (1943) - Revise zastupcu rodu Pristiograptus ze skupiny P dubius a P vulgaris z ceskeho a ciziho siluru. Rozpravy II. Tridy Ceske Akad., 53 (4): 1-40.
  • RADZEVICIUS S. (2003a) - Monograptids (Graptoloidea) from Holy Cross Mountains at the Wenlock Ludlow boundary. Geologija, 41: 44-51.
  • RADZEVICIUS S. (2003b) - Pristiograptus (Graptoloidea) from the perneri-lundgreni biozones (Silurian) of Lithuania. Carnets de Geologie/Notebooks on Geology, Article 2003/07 (CG2003_A07_SR): 1-14.
  • RADZEVICIUS S. (2004) - Gothograptus nassa biozona Lietuvoje. Mokslas gamtos moksll fakultete, 244-249.
  • RADZEVICIUS S. and PASKEVICIUS J. (2000) - Pristiograptids (Graptolites) and their adaptive types of the Wenlock (Silurian) in Lithuania. Geologija, 32: 88-109.
  • RADZEVICIUS S. and PASKEVICIUS J. (2005) - Pristiograptus (Graptoloidea) from the Upper Wenlock of the Baltic Countries. Sratigr. Geol. Correl., 13 (2): 47-56.
  • RICKARDS R. B. (1965) - New Silurian graptolites from the Howgill Fells (Northern England). Palaeontology, 8 (2): 248-271.
  • RICKARDS R. B. and WRIGHT A. J. (2003) - The Pristiograptus dubius (Suess, 1851) species group and iterative evolution in the Mid- and Late Silurian. Scottish J. Geol., 39 (1): 61-69.
  • SZYMAŃSKI B. and TELLER L. (1998) - The Silurian stratigraphy of the Zawiercie-Żarki area (NE margin of the Upper Silesian Coal Basin). Geol. Quart., 42 (2): 183-200.
  • TELLER L. (1972) - Biostratygrafia osadów sylurskich z profilu otworu Szczawno 1. Acta Geol. Pol., 22 (4): 677-688.
  • TELLER L. (1997) - The subsurface Silurian in the East European platform. Palaeont. Pol., 56: 7-21.
  • TOMCZYK H. (1962) - Outer Sudety monocline stratigraphy problems (in Polish with English summary). Prace Inst. Geol., 35: 3-134.
  • TRELA W. (2004) - Ordovician sea-level changes in the Małopolska Block (south-eastern Poland). In: WOGOGOB-2004 Conference Materials (eds. O. Hints and L. Ainsaar): 96-97. Tartu University Press.
  • TSEGELNJUK P. D. (1988) - Graptolites of Monograptus lundgreni (Murchison, 1839) group fromVolhyniaandPodolia. In: Graptolites in the Earth history (ed. J. Paskevicius): 81-83. Abstracts 5th Symposium on Investigation on Graptolites in USSR, Vilnius,
  • ULST R. (1974) - The early sequence of pristiograptids inconterminous deposits of Wenlock and Ludlow of the Middle Pribaltic. In: Graptolites of the USSR (ed. A. Obut): 90-105. Novosibirsk, Nauka.
  • WINCHESTER J. A. and the PACE TMR Network Team (contract ERBFMRXCT97-0136) (2002) - Palaeozoic amalgamation of Central Europe: new results from recent geological and geophysical investigations. Tectonophysics, 360 (1-4): 5-21.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS2-0011-0018
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.