Globorotaliid intervals of the sub-evaporite Badenian (Middle Miocene) in the Upper Silesia Basin (Central Paratethys, Poland)

• Autorzy: Gonera M.
• Języki publikacji: EN

Abstrakty

EN

Globorotaliids of the Skawina Formation (Badenian) come from deposits representing CPN 7 (Orbulina suturalis Zone) and CPN 8 sub-evaporite Wielician (Globigerina druryi–G. decoraperta Zone alias Uvigerina costai Zone) age. There are two taxonomic groups of globorotaliids in the studied material: globoconellids (Globoconella bykovae and G. minoritesta) and jenkinsellids (Jenkinsella mayeri and J. transsylvanica). There are five stratigraphically-rank intervals of these foraminifers prior to the Middle Badenian salinity crisis in Central Paratethys. The investigated Badenian begins with G. bykovae–J. mayeri association followed by the first occurence (FO) of J. transsylvanica. The closing member of the CPN 7 biozone is the G. bykovae–J. transsylvanica assemblage. The jenkinsellids disappear during CPN 7: J. mayeri first and J. transsylvanica after. Since the base of CPN 8 in situ jenkinsellids have not been noted in the Badenian deposits. The CPN 8 begins with a stratigraphic interval barren of globorotaliids (biozone IIC in the Polish Paratethys). It is followed by episodic appearances of globoconellids (G. bykovae and G. minoritesta) in the sub-evaporite Wielician (IID biozone in Poland). G. minoritesta has been found in only one case so far. The globorotaliid stratigraphic units are distinct and well-correlated with changes in climate and the circulation of water masses in Paratethys. This study provides additional data on Mi3 in Paratethys. It documents a cryptic cooling event in the late Orbulina suturalis Zone (mid CPN 7) located at the late IIA–B assemblage (alias upper lagenide zone) in regional biostratigraphic scale. The event is recorded by J. transsylvanica Acme, matching with circa 1‰VPDB δ¹⁸O positive excursion. The event must have resulted in a considerable sea level drop – a trigger of the Moravian ecosystem demolition in the Paratethys environment.

Słowa kluczowe

EN

Middle Miocene; Badenian; foraminifers; Globorotaliidae; Paratethys

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2013
• Tom: Vol. 57, No. 4
• Strony: 757–--768
• Opis fizyczny: Bibliogr. 46 poz., rys., tab.

Twórcy

autor

Gonera M.

• Academy of Sciences, Institute of Nature Conservation, Al. A. Mickiewicza 33, 31-120 Kraków, Poland

Bibliografia

• 1. Alexandrowicz S.W. (1963) Stratigraphy of the Miocene deposits in the Upper Silesian basin (in Polish with English summary). Prace Instytutu Geologicznego, 39.
• 2. Alexandrowicz S.W. (1997) Lithostratigraphy of the Miocene deposits in the Gliwice area (Upper Silesia, Poland). Bulletin of the Polish Academy of Sciences, Earth Sciences, 45: 167-179.
• 3. Baldi K. (2006) Paleoceanography and climate of the Badenian (Middle Miocene, 16.4-13.0 Ma) in the central Paratethys based on foraminifera and stable isotope (S18O and S13C) evidence. International Journal of Earth Sciences (Geologische Rundschau), 95: 119-142.
• 4. Barwicz-Piskorz W. (1997) Badenian (Miocene) radiolaria from the Gliwice area (Upper Silesia, Poland). Bulletin of the Polish Academy of Sciences, Earth Sciences, 45: 87-95.
• 5. Bé A.W.H. (1977) An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera. In: Oceanic Micropaleontology (ed. A.T.S. Ramsay): 1-100. Academic Press, London.
• 6. Berggren W.A., Kent D.U., Swisher C. III , Aubry M.P. (1995) A revised Cenozoic geochronology and chronostratigraphy. SEPM Special Publication, 54: 129-212.
• 7. Bicchi E., Ferrero E., Gonera M. (2003) Paleoclimatic interpretation based on Middle Miocene planktonic foraminifera: the Silesia Basin (Paratethys) and Monferrato (Tethys) record. Palaeogeography, Palaeoclimatology, Palaeoecology, 196: 265-303.
• 8. Blow W.H. (1959) Age, correlation, and biostratigraphy of the Upper Tocuyo (San Lorenzo) and Puzon formations, Eastern Falcon, Venezuela. Bulletins of American Paleontology, 39: 67-251.
• 9. Bolli H.M., Saunders J.B. (1982) Globorotalia mayeri and its reIationship to Globorotalia siakensis and Globorotalia continuosa. Journal of Foraminiferal Research, 12: 39-50.
• 10. Cicha I., Čtyroká J., Jiřiček R., Zapletalová I. (1975) Principal biozones of the Late Tertiary in East Alps and West Carpathians. In: Biozonal division of the Upper Tertiary bas I ns of the Eastern Alps and West Carpathians (ed. I. Cicha): 19-34. IUGS Proccedings of the VI Congress, Bratislava.
• 11. Cicha I., Rögl F., Rupp Ch., Čtyroká J. (1998) Oligocene-Miocene foraminifera of the Central Paratethys. Abhandlungen der Senckenbergischen Naturforschenden Gesellschaft, 549: 1-325.
• 12. Cushman J.A., Ellisor A.C. (1939) New species of Foraminifera from the Oligocene and Miocene. Contributions to the Cushman Laboratory of Foraminiferal Research, 15: 1-14.
• 13. Durakiewicz T., Gonera M., Peryt T.M. (1997) Oxygen and carbon isotopic changes in the Middle Miocene (Badenian) foraminifera of the Gliwice area (SW Poland). Bulletin of the Polish Academy of Sciences, Earth Sciences, 45: 145-156.
• 14. Garlicki A. (1979) Sedimentation of Miocene salts in Poland (in Polish with English summary). Prace Geologiczne, 119.
• 15. Gonera M. (2001) Foraminiferida and plaeonevironment of the Badenian formations (Middle Miocene) in Upper Silesia (Poland) (in Polish with English summary). Studia Naturae, 48: 1-211.
• 16. Gonera M., Bukowski K. (2012) Isotopic events in the Early/Middle Badenian (Miocene) of the Upper Silesia Basin (Central Paratethys). Geological Quarterly, 56 (3): 561-568.
• 17. Gonera M., Peryt T.M., Durakiewicz T. (2000) Biostratigraphical and paleoenvironmental implications of isotopic studies (18O, 13C) of middle Miocene (Badenian) foraminifers in the Central Paratethys. Terra Nova, 12: 231-238.
• 18. Gonera M., Peryt T.M., Durakiewicz T. (2003) Coiling direction in Globigerina bulloides of Middle Miocene age. Journal of Micropaleontology, 22: 141-146.
• 19. Gonera M., Bukowski K., d'Obyrn K., Wiewiorka J. (2012) Foraminifera in slump deposits of the Badenian (Middle Miocene) Green Stratified Salt in Wieliczka, Poland. Geological Quarterly, 56 (4): 869-880.
• 20. Harzhauser M., Piller W.E., Müllegger S., Grunert P., Micheels A. (2011) Changing seasonality patterns in Central Europe from Miocene Climate Optimum to Miocene Transition deduced from the Crassostrea isotope archive. Global and Planetary Change, 76: 166-169.
• 21. Hemleben Ch., Spindler M., Anderson O. R. (1989) Modern Planktonic Foraminifera. Springer, New York.
• 22. Iaccarino S. (1985) Mediterranean Miocene and Pliocene planktic foraminifera. In: Planktonic Stratigraphy (eds. H. M. Bolli, J. B. Saunders and K. Perch-Nielsen): 263-282. Cambridge University Press.
• 23. Jenkins D.G. (1960) Planktonic Foraminifera from the Lakes Entrance oil shaft, Victoria, Australia. Micropaleontology, 6: 345-371.
• 24. Kennett J.P., Srinivasan M.S. (1983) Neogene Planktonic Foraminifera. A Phylogenetic Atlas. Hutchinson Ross Publishing Company, Stroudsburg.
• 25. Key M.M., Zágoršek K., Patterson W.P. (2013) Paleoenvironmental reconstruction of the Early to Middle Miocene Central Paratethys using stable isotopes from bryozoan skeletons. International Journal of Earth Sciences, 102: 305-318.
• 26. Kovačová P., Hudáčková N. (2009) Late Badenian foraminifers from the Vienna Basin (Central Paratethys): stable isotope study and paleoecological implications. Geologica Carpathica, 60: 59-70.
• 27. Laskarev V. (1924) Sur les equivalents du Sarmatian superieur en Serbie. In: Recueil de travaux offert a M. Jovan Cvijie per ses amis et collaborateurs (ed. P. Vujevic), Belgrade: 73-85.
• 28. Leeuw A. de, Bukowski K., Krijgsman W., Kuiper K.F. (2010) The age of the Badenian Salinity Crisis; impact of Miocene climate variability on the Circum-Mediterranean region. Geology, 38: 715-718.
• 29. Loeblich A.R. Jr., Tappan H. (1988) Foraminiferal genera and their classification. Van Nostrand Reinhold Company, NewYork.
• 30. Łuczkowska E. (1964) The micropaleontological stratigraphy of the Miocene in the region of Tarnobrzeg-Chmielnik (in Polish with English summary). Prace Geologiczne, 20.
• 31. Oszczypko N., Krzywiec P., Popadyuk I., Peryt T. (2006) Carpathian Foredeep Basin (PoIand and Ukraine): its sedimentary, structural, and geodynamic evolution. AAPG Memoir, 84: 293-350.
• 32. Papp A., Cicha I., Seneš J. (1978a) Gliederung des Badenian, Faunenzonen und Unterstufen. In: Chronostratigraphie und Neostratotypen: Miozän der Zentralen Paratethys (ed. E. Brestenská): 49-52. Bd. VI. M4 Badenian (Moravien, Wielicien, Kosovien). VEDA SAV, Bratislava.
• 33. Papp A., Rögl F., Cicha I., Čtyroká J., Pishvanova L.S. (1978b) Planktonische Foraminiferen im Badenian. In: Chronostratigraphie und Neostratotypen. Miozan der Zentralen Paratethys (ed. E. Brestenská): 268-278. Bd. VI Bratislava, VEDA.
• 34. Peryt D. (2013) Foraminiferal record of the Middle Miocene climate transition prior to the Badenian salinity crisis in the Polish Carpathians Foredeep basin (Cenlral Paratethys). Geological Quarterly, 57 (1): 141-164.
• 35. Peryt D., Gedl P. (2010) Palaeoenvironmental changes preceding the Middle Miocene Badenian salinity crisis in the northern Polish Carpathian Foredeep Basin (Borków Quarry) inferred from foraminifers and dinoflagellate cysts. Geologlcal Quarterly, 54 (4): 487-508.
• 36. Popescu G. (1970) Planktonic foraminiferal zonation in the Dej Tuff Complex. Revue Roumaine de Géologie, Géophysique, et Géographie, Série de Géologie, 14: 189-203.
• 37. Rögl F. (1998) Palaeogeographic considerations for Mediterranean and Paratethys seaways (Oligocene to Miocene). Annalen des Naturhistorischen Museums in Wien, 99A: 279-310.
• 38. Rögl F., Steininger F.F. (1984) Neogene Paratethys, Mediterranean and Indo-Pacific seaways. In: Fossils and Climate (ed. P. Branchley): 171-200. Wiley.
• 39. Rupp Ch., Hochenegger J. (2008) Paleoecology of planktonic foraminifera from the Baden-Sooss section (Middle Miocene, Badenian, Vienna Basin, Auslria). Geologica Carpathica, 59: 425-445.
• 40. Seneš J. (1959) Súcasné znalosti o stratigrafii centralnej Paratétydy. Geologické Práce, 55.
• 41. Seneš J. (1971) Korrelation des Miozans der Zentralen Paratethys (stand 1970). Geologicky Zbornik, 22: 3-9.
• 42. Srinivasan M.S., Kennett J.P. (1981) Neogene planktonic foraminiferal biostratigraphy: Equatorial to subantarctic, South Pacific. Marine Micropaleontology, 6: 499-534.
• 43. Steininger F.F., Seneš J., Kleeman K., Rögl F., eds. (1985) Neogene of the Medlterranean Tethys and Paratethys. Stratigraphic correlation tables and sediment distribution maps. Univ. Vienna Inst. Paleont.
• 44. Subbotina N.N., Pishvanova L.S., Ivanova L.V. (1960) Stratigrafia oligotsenovikh i miotsenovikh otlozheniy Predkarpatya po foraminiferam. Trudy VNIGRI, 153: 5-127.
• 45. Szczechura J. (1982) Middle Miocene foraminiferal biochronology and ecology of SE Poland. Acta Palaeontologica Polonica, 27: 3-44.
• 46. Witkowski A., Gonera M. (1997) Miocene diatom flora from Central Paratethys (Carpathian Foredeep, Upper Silesia) - preliminary results. Bulletin of the Polish Academy of Sciences, Earth Sciences, 45: 181-190.