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Rusophycus inexpectus isp. nov. from the Furongian (Upper Cambrian) of the Holy Cross Mountains (Poland

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Języki publikacji
EN
Abstrakty
EN
A new trace fossil Rusophycus inexpectus isp. nov. is described from the Furongian (Upper Cambrian) strata of the Holy Cross Mountains. This ichnospecies is probably non-trilobite in origin and is commonly preserved as an undertrace. This preservation style resembles that of Rusophycus ramellensis Legg, an index fossil of the Cambrian Series 3. Therefore, previous workers misinterpreted material from the Wiśniówka Sandstone Formation as Rusophycus ramellensis Legg (recorded by them as Cruziana barbata) and put the Cambrian Series 3 and Furongian boundary within this unit. Rusophycus inexpectus isp. nov differs from Rusophycus ramellensis Legg: 1) in having a smooth trapezoidal area behind the lobes; 2) in the presence of a direct contact between the endopodal lobes and cephalic margin imprints and 3) in the restriction of the occurrence of the endopodal lobes and scratches to the cephalic region of the trace fossil. Care must be taken, when dealing with the undertrace preservation style of Rusophycus ramellensis Legg in other assemblages, as it may represent Rusophycus inexpectus isp. nov.
Rocznik
Strony
143--151
Opis fizyczny
Bibliogr. 36 poz., rys.
Twórcy
autor
  • Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, PL- 00-818 Warszawa, Poland
Bibliografia
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  • 5. Dżułyński, S. & Żak, C., 1960. Sedcmentary environment of the Cambrian quartzites in the Holy Cross Mountains, Central Potand, and their relationship to the flysch facies. Rocznik Polskiego Towarzystwa Geologicznego, 30: 213 241.
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  • 7. Hughes, N. C., 2003a. Trilobite body patterning and the evolution of arthropod tagmosis. BioEssays, 25: 386-395.
  • 8. Hughes, N. C., 2003b. Tritobite tagmosis and body patterning from morphological and developmental perspectives. Integrative and Comparative Biology, 43: 185-206.
  • 9. Jaworowski, K. & Sikorska, M., 2006. Łysogóry Unit (Central Poland) versus East European Craton - application of sedimentological data from Cambrian siliciclastic associat ion. Geological Quarterly, 50: 77-88.
  • 10. Jensen, S., 1997. Trace fossils from the Lower Cambrian Mickwitzia sandstone, south-central Sweden. Fossils and Strata, 42: 1-111.
  • 11. Jensen, S., Bogolepova, O. K. & Gubanov, A. P., 2011. Cruziana semiplicata from the Furongian (Late Cambrian) of Severnaya Zemlya Archipelago, Arctic Russia, with a review of the spatial and temporal distribution of this ichnospecies. Geological Journal, 46: 26-33.
  • 12. Keighley, D. G., & Pickerill, R. K., 1996. Small Cruziana, Rusophycus, and related ichnotaxa from eastern Canada: The nomenclatural debate and systematic ichnology. Ichnos, 4: 261-285.
  • 13. Kowalczewski, Z., 1995. Fundamental stratigraphic probtem of the Cambrian in the Holy Cross Mts. Geological Quarterly, 39: 449-470.
  • 14. Kowalczewski, Z., Żylińska, A. & Szczepanik, Z., 2006. Kambr w Górach Świętokrzyskich. In: Skompski, S. & Żylińska, A. (eds), Procesy i zdarzenia w historii geologicznej Gór Świętokrzyskich, LXXVII Zjazd Naukowy Polskiego Towarzystwa Geologicznego, Ameliówka k. Kielc, 28-30 czerwca 2006 r., Materiały Konferencyjne. Polskie Towarzystwo Geologiczne, Państwowy Instytut Geologiczny, Wydział Geologii Uniwersytetu Warszawskiego, Warszawa, pp. 14-27. [In Polish.]
  • 15. Legg, I. C., 1985. Trace fossils from a Middle Cambrian deltaic sequence, north Spain. In: Curran, A. H. (ed.), Biogenic Structures: Their Use in Interpreting Depositional Environments. Society of Economic Paleontologists and Mineralogists Special Papers, 35: 151-165.
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  • 18. Nagtegaal, P. J. C., 1978. Sandstone-framework instabiltty as a function of burial diagenesis. Journal of the Geological Society, 135: 101-105.
  • 19. Orłowski, S., 1992. Trilobite trace fossils and their stratigraphical signiftcance in the Cambrian sequence of the Holy Cross Mountains, Poland. Geological Journal, 27: 15-34.
  • 20. Orłowski, S., Radwański, A. & Roniewicz, P., 1970. The trilobite ichnocoenoses in the Cambrian sequence of the Holy Cross Mountains. In: Crimes. T. P. & Harper, J. C. (eds), Trace Fossils. Geological Journal, Special Issue, 3: 345-360.
  • 21. Orłowski, S., Radwański, A. & Roniewicz, P., 1971. Ichnospecific variability of the Upper Cambrian Rusophycus from the Holy Cross Mts. Acta Geologica Polonica, 21: 341-348.
  • 22. Orłowski, S. & Żylińska, A., 1996. Non-arthropod burrows from the Middle and Late Cambrian of the Holy Cross Mountains, Poland. Acta Palaeontologica Polonica, 41: 385-409.
  • 23. Radwański, A. & Roniewicz, P., 1960. Ripple marks and other sedimentary structures of the Upper Cambrian at Wielka Wiśniówka (Holy Cross Mts.). Acta Geologica Polonica, 10: 371-400.
  • 24. Radwański, A. & Roniewicz, P., 1972. A long trilobite trackway, Cruziana semiplicata Salter, from the Upper Cambrian of the Holy Cross Mts. Acta Geologica Polonica, 22: 439-447.
  • 25. Sadlok, G., 2010. Trace fossil Cruziana tenella from the Furongian (Upper Cambrian) depostts of Potand. Acta Geologica Polonica, 60: 349-355.
  • 26. Sadlok, G., 2011. Arthropod tracks from the Furongian (Upper Cambrian) of the Wiśniówka Wielka (Holy Cross Mountains) and their taphonomy: a prelimtnary report. Przegląd Geologiczny, 59: 82-90. [In Polish, with English abstract].
  • 27. Sadlok, G. & Machalski, M., 2010. The trace fossil Rusophycus versans from the Furongian (Upper Cambrian) of central Po- land - an example of behavtoural convergence amongst arthropods. Acta GeologicaPolonica, 60: 119-123.
  • 28. Schlirf, M., Uchman, A. & Kümmel, M., 2001. Upper Triassic (Keuper) non-marine trace fos s ils from the Haßberge area (Franconia, south-eastern Germany). Paläontologische Zeitschrift, 75: 71-96.
  • 29. Seilacher, A., 1970. Cruziana stratigraphy of “non-fossiliferous” Palaeozoic sandstones. In: Crimes. T. P. & Harper, J. C. (eds), Trace Fossils. Geological Journal, Special Issue, 3: 447-475.
  • 30. Seilacher, A. 1985. Trilobite palaeobiology and substrate relationships. Transactions of the Royal Society of Edinburgh. Earth Sciences, 76: 231-237.
  • 31. Seilacher, A., 1994. How valid is Cruziana stratigraphy? Geologische Rundschau, 83: 752-758.
  • 32. Seilacher, A., 2007. Trace Fossil Analysis. Springer, Berlin. 226 pp.
  • 33. Sikorska, M., 2000. Silification history of Cambrian sandstones in the Wiśniówka area, Holy Cross Mts (Central Poland). Przegląd Geologiczny, 48: 251-258. [In Polish, with English abstract].
  • 34. Whittington, H. B., 1980. Exoskeleton, moult stage, appendage morphology, and habits of the Middle Cambrian trilobite Olenoides serratus. Palaeontology, 23: 171-204.
  • 35. Żylińska, A., 2002. Stratigraphic and biogeographic signiftcance of Late Cambrian trilobites from Łysogóry (Holy Cross Mountains, central Potand). Acta Geologica Polonica, 52: 217-238.
  • 36. Żylińska, A., Szczepanik, Z. & Salwa, S., 2006. Cambrian of the Holy Cross Mountains, Poland; biostratigraphy of the Wiśniówka Hill succession. Acta Geologica Polonica, 56: 443461.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-fef8d261-0208-40df-bc60-d68f0f5979b8
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