PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

A unique habitat of endolithic biota: hurricane-induced limestone rubble in an Albian sand-mass of the Cracow Upland, southern Poland

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Peculiarly shaped, relatively large (up to 30 cm in diameter) concretions of quartzitic sandstone occur in a single horizon of Upper Albian loose sands in the Cracow Upland, southern Poland. They are characterized by hollow interiors adorned with mass-aggregated moulds of the borings of diverse sponges, polychaetes and bivalves. These moulds represent the siliceous filling of borings in limestone clasts that had been subject to dissolution, leaving a hollow within the concretion that had formed around them. Synsedimentary block-faulting and jointing affected the Jurassic limestone-basement, causing the uplift of a local horst (the Glanow Horst), to within the littoral zone so that it became exposed to abrasion. It is inferred that a hurricane or catastrophic storm surge swept limestone debris fallen from the cliff out to the sandy offshore, where nucleation of soluble silica was presumably favoured by the decay of the soft tissue of live or dead rock-borers. After filling the emptyo borings and solution of the limestone clasts, the nucleation progressed intensely, finally completed by precipitation of siliceous sinter in the hollow interiors of some of the concretions during subsequent diagenesis and/or epigenesis.
Rocznik
Strony
505--521
Opis fizyczny
Bibliogr. 41 poz.,Fot., rys.,
Twórcy
  • Institute of Geology, University of Warsaw; Al. Żwirki i Wigury 93, PL-02-089 Warsaw, Poland
Bibliografia
  • Alexandrowicz, S.W. 1954. Turonian of the southern part of the Cracow Upland. Acta Geologica Polonica, 4, 361–390. [In Polish]
  • Aurell, M., Bosence, D.W.J. and Waldham, D. 1995. Carbonate ramp depositional systems from a Late Jurassic epeiric platform (Iberian Basin, Spain): a combined computer modeling and outcrop analysis. Sedimentology, 42, 75–94.
  • Barczyk, W. 1956. On the Upper Chalk deposits on Bonarka near Cracow. Studia Societatis Scientiarum Torunensis, Sectio C (Geographia et Geologia), 3, 1–26. [In Polish with English Summary]
  • Bromley, R.G. 1970. Borings as trace fossils and Entobia cretacea Portlock, as an example. In: T.P. Crimes and J.C. Harper (Eds), Trace fossils (Geological Journal Special Issue), 3, 49–90. Liverpool.
  • Bromley, R.G. and D’Alessandro, A. 1983. Bioerosion in the Pleistocene of southern Italy: ichnogenera Caulostrepsis and Meandropolydora. Rivista Italiana di Paleontologia e Stratigrafia, 89, 283–309.
  • Bromley, R.G. and D’Alessandro, A. 1984. The ichnogenus Entobia from the Miocene, Pliocene and Pleistocene of southern Italy. Rivista Italiana di Paleontologia e Stratigrafia, 90, 227–296.
  • Bromley, R.G. and D’Alessandro, A. 1987. Bioerosion of the Plio-Pleistocene transgression of southern Italy. Rivista Italiana di Paleontologia e Stratigrafia, 93, 379–442.
  • Bromley, R.G. and D’Alessandro, A. 1989. Ichnological study of shallow marine endolithic sponges from the Italian coast. Rivista Italiana di Paleontologia e Stratigrafia, 95, 279–314.
  • Dżułyński, S. 1953. Tectonics of the southern part of the Cracow Upland. Acta Geologica Polonica, 3, 325–440. [In Polish]
  • Gibert, J.M. De and Martinell, J. 1998. Ichnofabrics of the Pliocene marginal marine basins of the northwestern Mediterranean. Revista de la Sociedad Geológica España, 11, 43–56.
  • Gibert, J.M. De, Martinell, J. and Domènech, R. 1998. Entobia ichnofacies in fossil rocky shores, Lower Pliocene, northwestern Mediterranean. Palaios, 13, 476–487.
  • Głazek, J., Marcinowski, R. and Wierzbowski, A. 1971. Lower Cenomanian trace fossils and transgressive deposits in the Cracow Upland. Acta Geologica Polonica, 21, 433–448.
  • Handford, C.R. 1986. Facies and bedding sequences in shelfstorm deposited carbonates. Fayettville Shale and Pitkin Limestone (Mississippian) Arkansas. Journal of Sedimentary Petrology, 56, 123–137.
  • Kelly, S.R.A. and Bromley, R.G. 1984. Ichnological nomenclature of clavate borings. Palaeontology, 27, 793–807.
  • Marcinowski, R. 1970a. The Cretaceous transgressive deposits east of Częstochowa (Polish Jura Chain). Acta Geologica Polonica, 20, 413–449.
  • Marcinowski, R. 1970b. Turbidites in the Upper Oxfordian Limestones at Jaskrów in the Polish Jura Chain. Bulletin de l’Académie Polonaise des Sciences, Série des Sciences Géologiques et Géographiques, 18, 219–235.
  • Marcinowski, R.1974. The transgressive Cretaceous (Upper Albian through Turonian) deposits of the Polish Jura Chain. Acta Geologica Polonica, 24, 117–217.
  • Marcinowski, R. and Radwański, A. 1983. The mid-Cretaceous transgression onto the Central Polish Uplands. Zitteliana, 10, 65–96.
  • Marcinowski, R. and Radwański, A. 1989. A biostratigraphic approach to the mid-Cretaceous transgressive sequence of the Central Polish Uplands. Cretaceous Research, 10, 153–172.
  • Marcinowski, R. and Szulczewski, M. 1972. Condensed Cretaceous sequence with stromatolites in the Polish Jura Chain. Acta Geologica Polonica 22, 515–539.
  • Marcinowski, R. and Wiedmann, J. 1988. Paleogeographic implications of the Albian ammonite faunas of Poland. In: J. Wiedmann and J. Kullmann (Eds), Cephalopods Present and Past – O.H. Schindewolf Symposium Tübingen 1985, pp. 491–504. Schweizerbart’sche Verlagsbuchhandlung (Nägele u. Obermiller); Stuttgart.
  • Marques Da Silva, C., Hindson, R. and Andrade, C. 1996. Bioerosion evidence of extreme marine flooding of Algarve region (Southern Portugal) associated with the tsunami of the AD 1755 Lisbon earthquake: taphonomic and (paleo) ecological analyses. Communicación de la II Reunión de Tafonomia y Fosilizatión, pp. 371–378. Zaragoza.
  • Martinell, J. and Domènech, R. 1995. Bioerosive structures on the Pliocene rocky shores of Catalonia (Spain). Revista Española de Paleontologia, 10, 37–44.
  • Matyszkiewicz, J. 1966. The significance of Saccocoma-calciturbidites for the analysis of the Polish Epicontinental Late Jurassic Basin: an example from the Southern Cracow-Wieluń Upland. Facies, 34, 23–40.
  • Matyszkiewicz, J. 1997.Microfacies, sedimentation and some aspects of digenesis of Upper Jurassic sediments from the elevated part of the Northern peri-Tethyan shelf: a comparative study on the Lochen area (Schwäbische Alb) and the Cracow area (Cracow-Wieluń Upland, Poland). Berliner geowissenschaftliche Abhandlungen, E21, 1–111.
  • McAdoo, B.G. and Watts, P. 2004. Tsunami hazard from submarine landslides on the Oregon continental slope. Marine Geology, 203, 235–245.
  • Pleydell, S.M. and Jones, B. 1988. Boring of various faunal elements in Oligocene-Miocene Bluff Formation of Grand Cayman, British West Indies. Journal of Paleontology, 62, 348–367.
  • Radwański, A. 1964. Boring animals in Miocene littoral environments of Southern Poland. Bulletin de l’Académie Polonaise des Sciences, Série des Sciences Géologiques et Géographiques, 12, 57–62.
  • Radwański, A. 1968. Lower Tortonian transgression onto Miechów and Cracow Uplands. Acta Geologica Polonica, 18, 387–445.
  • Radwański, A.1 969. Lower Tortonian transgression onto the southern slopes of the Holy Cross Mountains. Acta Geologica Polonica, 19, 1–164.
  • Radwański, A. 1970. Dependence of rock-borers and burrowers on the environmental conditions within the Tortonian littoral zone of Southern Poland. In: T.P. Crimes and J.C. Harper (Eds), Trace fossils (Geological Journal Special Issue), 3, 371–390. Liverpool.
  • Radwański, A. 1977. Present-day types of trace in the Neogene sequence; their problems of nomenclature and preservation. In: T.P. Crimes and J.C. Harper (Eds), Trace fossils (Geological Journal Special Issue), 9, 227–264. Liverpool.
  • Reading, H.G. and Levell, B.K. 1996. Controls on the sedimentary rock record. In: H.G. Reading (Ed.). Sedimentary Environments: Processes, Facies and Stratigraphy, pp. 5–36. Blackwell Scientific Publications Inc; Cambridge.
  • Röder, H. 1977. Zur Beziehung zwischen Konstruktion und Substrat bei mechanisch bohrenden Bohrmuscheln (Pholadidae, Teredinidae). Senckenbergiana Maritima, 9, 105–213.
  • Rützler, K. and Bromley, R.G. 1981. Cliona rhodensis, new species (Porifera: Hadromerida) from Mediterranean. Proceedings of the Biological Society of Washington, 94, 1219–1225.
  • Spalletta, C. and Vai, G.B. 1984. Upper Devonian intraclast parabreccias interpreted as seismites. Marine Geology, 55, 133–144.
  • Stephenson, L.W. 1952. Large invertebrate fossils of the Woodbine Formation (Cenomanian) of Texas. United States Geological Survey Professional Paper, 242, 1–226.
  • Voigt, E. 1965. Über parasitische Polychaeten in Kreide-Austern sowie einige andere in Muschelschalen bohrende Würmer. Paläontologische Zeitschrift, 39, 193–211.
  • Volz, P. 1939. Die Bohrschwämme (Clioniden) der Adria. Thalassia, 3, 1–64.
  • Walaszczyk, I. 1992. Turonian through Santonian deposits of the Central Polish Uplands; their facies development, inoceramid paleontology and stratigraphy. Acta Geologica Polonica, 42, 1–122.
  • Ziółkowski, P. 2007. Stratigraphy and the facial variability of Upper Jurassic in the eastern part of the Cracow Upland. Tomy Jurajskie, 4, 25–38. [In Polish]
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-2718-0616
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.