PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Coiling direction in Middle Miocene globorotaliids (Foraminiferida) : a case study in the Paratethys (Upper Silesia Basin, Poland)

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The paper deals with sub-evaporite Badenian deposits (Middle Miocene, Paratethys) that display a sudden appearance of globorotaliid taxa showing preferences in the taxonomic set and coiling direction. An interval of sinistrally coiled Jenkinsella mayeri with proportionally coiled Globoconella bykovae is at the bottom of the studied sequence. It is followed by an interval of proportionally coiled Jenkinsella transsylvanica. Proportionally coiled Globoconella bykovae with a small number of proportionally coiled Jenkinsella transsylvanica are at the top of the Moravian (CPN 7) substage (Orbulina suturalis alias Lagenidae Zone). The sub-evaporite part of the Wielician (CPN 8) substage (Uvigerina costai alias Spiroplectammina Zone) began with a globorotaliid-barren interval (IIC biozone). It is followed by biozone IID displaying three globorotallid peaks amongst globorotallid-barren deposits. Only globoconellas are present in all these three events. Proportionally coiled Globoconella bykovae appeared first. It is followed by proportionally coiled Globoconella minoritesta and sinistrally coiled Globoconella bykovae at the end of the biozone IID. Coiling preferences of globorotaliids have been compared to changes in the hydrographic regime unfolding during the CPN 7 and CPN 8 in the studied area of the Paratethys. The study discovers that the coiling of globorotaliids responded selectively to the hydrographic changes. Globoconella bykovae is highly opportunistic and can tolerate considerable temperature changes. Specimens of this taxon persist to coil proportionally during the sub-evaporite Badenian, except for the shift to sinistral coiling just prior to the Wielician evaporites. Sinistrally coiled Jenkinsella mayeri is the most sensitive to hydrographic changes. This taxon retreated at the onset of the temperature drop during the mid-Moravian cryptic cooling. This cooling is marked by the new jenkinsellid occurrence – proportionally coiled Jenkinsella transsylvanica. Proportionally coiled Globoconella minoritesta is present in the middle of the IID globorotaliid peaks. The globorotaliid coiling data, presented in this paper, has been calibrated to the global stratigraphy. The integrated data (foraminifera, nannofossils, oxygen and carbon stable isotopes, radiometric measurements) supports the view that the CPN 7/CPN 8 boundary is coeval to the Langhian/Serravalian one. In the Polish part of the Carpathian Foredeep, the boundary runs within the Skawina Formation.
Rocznik
Strony
155--171
Opis fizyczny
Bibliogr. 111 poz., rys., tab., wykr.
Twórcy
autor
  • The John Paul II Catholic University of Lublin, Off-Campus Faculty of Law and Social Sciences, Kwiatkowskiego 3A, 37-450 Stalowa Wola, Poland
  • Polish Academy of Sciences, Institute of Nature Conservation, Al. A. Mickiewicza 33, 31-120 Kraków, Poland
Bibliografia
  • Opis fizyczny: zła ilość pozycji; Bibliografia: pkt. 6 – źle wpisana liczba; pkt. 95 – brak znaków diakrytycznych w wyrazie; od pkt. 98 wprowadzona podwójna numeracja;
  • 1. Abdul Aziz, H., Di Stefano, A., Foresi, L.M., Hilgen, F.J., laccarino, S.M., Kuiper, K.F., Lirer, F., Salvatorini, G., Turco, E., 2008. Integrated stratigraphy of early Middle Miocene sediments from DSDP Leg 42A, Site 372 (eastern Mediterranean). Palaeogeography, Palaeoclimatology, Palaeoecology, 257: 123-138.
  • 2. Abels, H.A., Hilgen, F.J., Kruk, R.W., Raffi, I., Turco, E., Zachariasse, W.J., 2005. Long-period orbital control on middle Miocene global cooling: Integrated stratigraphy and astronomical tuning of the Blue Clay Formation on Malta. Paleoceanography, 20: 1-17.
  • 3. Alexandrowicz, S.W., 1963. Stratigraphy of the Miocene deposits in the Upper Silesian basin (in Polish with Englsh summary). Prace Instytutu Geologicznego, 39.
  • 4. 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.
  • 5. Alexandrowicz, S.W., Garlicki, A., Rutkowski, J., 1982. Podstawowe jednostki litostratygraficzne miocenu zapadliska przedkarpackiego. Kwartalnik Geologiczny, 26: 470-471.
  • 6. Báldi, 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 (δ18O and δ13C) evidence. International Journal of Earth Sciences, 95: 119-142.
  • 7. Báldi, K., Velledits, F., Ćorić, S., Lemberkovics, V., Lőrincz, K., Shevelev, M., 2017. Discovery of the Badenian evaporites inside the Carpathian Arc: implications for global climate change and Paratethys salinity. Geologica Carpathica, 68: 193-206.
  • 8. Bandy, O.L., 1960. The geologic significance of coiling ratios in the foraminifer Globigerina pachyderma (Ehrenberg). Journal of Paleontology, 34: 671-681.
  • 9. Bandy, O.L., 1972. Variations in Globigerina bulloides d'Orbigny as indices of water masses. Antarctic Journal, 7: 194-195.
  • 10. 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.
  • 11. Bé, A.W.H., Hutson, W.H., 1977. Ecology of planktonic foraminifera and biogeographic patterns of life and fossil assemblages in the Indian Ocean. Micropaleontology, 23: 369-414.
  • 12. Bé, A.W.H., Tolderlund, D.S., 1971. Distribution and ecology of living planktonic foraminifera in surface waters of the Atlantic and Indian Oceans. In: Micropaleontology of Oceans (eds. B.M. Funnel and W.R. Riedel): 105-149. The Cambridge University Press, Cambridge.
  • 13. Berggren, W.A., Kent, D.V., Swisser, Ill C.C., Aubry, M.P., 1995. A revised Cenozoic geochronology and chronostratigraphy. SEPM Special Publication, 54: 129-212.
  • 14. 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.
  • 15. Blow, W.H., 1969. Late Middle Eocene to Recent planktonic foraminiferal biostratigraphy. Proceedings First International Conference on Planktonic Microfossils, Genova, 1: 199-422.
  • 16. Bolli, H.M., 1950. The direction of coiling in the evolution of some Globorotaliidae. Contributions from the Cushman Foundation for Foraminiferal Research, 1: 82-89.
  • 17. Bolli, H.M., 1971. The direction of coiling in planktonic foraminifera. In: Micropaleontology of Oceans. (eds. B.M. Funnel and W.R. Riedel): 639-648. The Cambridge University Press, Cambridge.
  • 18. Bolli, H.M., Saunders, J.B., 1982. Globorotalia mayeri and its relationship to Globorotalia siakensis and Globorotalia continuosa. Journal of Foraminiferal Research, 12: 39-59.
  • 19. Bolli, H.M., Saunders, J.B., 1985. Oligocene to Holocene low latitude planktic foraminifera. In: Planktonic Stratigraphy (eds. H.M. Bolli, J.B. Saunders and K. Perch-Nielsen): 155-26l. The Cambridge University Press, Cambridge.
  • 20. Boltovskoy, E., 1962. Planktonic foraminifera as indicators of different water masses in the South Atlantic. Micropaleontology, 8: 403-408.
  • 21. Boltovskoy, E., 1973. Note on the determination of absolute surface water paleotemperature by means of the foraminifer Globigerina bulloides d'Orbigny. Paläontologische Zeitschrift, 47: 152-155.
  • 22. Boltovskoy, E., Wright, R., 1976. Recent Foraminifera. Junk, The Haque.
  • 23. Boltovskoy, E., Boltovskoy, D., Correa, N., Brandini, F., 1996. Planktonic foraminifera from the southwestern (30o-60oS): species-specific patterns in the upper 50 m. Marine Micropaleontology, 28: 53-72.
  • 24. Brunner, G.J., Kroon, D., 1988. Genetically controlled planktonic foraminiferal coiling ratios as tracers of past ocean dynamics. In: Planktonic Foraminifers as Tracers of Ocean-Climate History (eds. G.J. Brunner and D. Kroon): 131-147. Free University Press, Amsterdam.
  • 25. Bukowski, K., 2011. Badenian saline sedimentation between Rybnik and Dębica based on geochemical, isotopic and radiometric research (in Polish with English summary). Dissertations Monographs, 236.
  • 26. Bukowski, K., de Leeuw, A., Gonera, M., Kuiper, K.F., Krzywiec, P., Peryt, D., 2010. Badenian tuffite levels within the Carpathian orogenic front (Gdów-Bochnia area, Southern Poland): radio-isotopic dating and stratigraphic position. Geological Quarterly, 54 (4): 449-464.
  • 27. Chira, C., 1999. Middle Miocene calcareous nannoplankton from the western Transylvanian Basin, Romania: biostratigraphy, taxonomy and palaeoecology. Studia Univ. BabeşBolyai Cluj-Napoca, Geol.-Geogr., 44: 3-75.
  • 28. 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 basins of the Eastern Alps and West Carpathians, IUGS Proceedings of the VI. Congress, Bratislava (ed. I. Cicha): 19-34.
  • 29. Cicha, I., Rögl, F., Rupp, Ch., Čtyroká, J., 1998. Oligocene-Miocene foraminifera of the Central Paratethys. Abhandlungen der Senckenbergischen Naturforschenden Gesellschaft, 549: 1-325.
  • 30. Cita, M.B., Blow, W.H., 1969. The biostratigraphy of the Langhian, Serravalian and Tortonian stages in the type-sections in Italy. Rivista Italiana de Paleontologia, 75: 549-603.
  • 31. de Leeuw, A., Bukowski, K., Krijgsman, W., Kuiper, K.F., 2010. Age of the Badenian salinity crisis; impact of Miocene climate variability on the circum-Mediterranean region. Geology, 38: 715-718.
  • 32. Doláková, N., Holcová, K., Nehyba, S., Hladilová S., Brzobohatý, R., Zágoršek K., Hrabkovský, J., Seko, M., Utescher, T., 2014. The Badenian parastratotype at Židlachovice from the perspective of the multiproxy study. Neues Jahrbuch fur Geologie und Paläontologie Abhandlungen, 271: 169-201.
  • 33. Dudziak, J., Łuczkowska, E., 1991. Biostratigraphic correlation of foraminiferal and calcareous nannoplankton zones - Middle Badenian (Miocene), southern Poland. Bulletin of the Polish Academy of Sciences, Earth Sciences, 39: 199-214.
  • 34. 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.
  • 35. Eisenach, A.R., Kelly, D.C., 2006. Coiling preferences and evolution in the middle Miocene Fohsella chronocline. Marine Micropaleontology, 60: 243-257.
  • 36. Ericson, D.B., 1959. Coiling direction of Globigerina pachyderma as climatic index. Science, 130: 219-220.
  • 37. Ericson, D.B., Wollin, G., Wolin, J., 1954. Coiling dorection of Globorotalia truncatulinoides in deep-sea cores. Deep-Sea Research, 2: 152-158.
  • 38. Ericson, D.B., Ewing, M., Wollin, G., Heezen, B.C., 1961. Atlantic deep-sea sediment cores. GSA Bulletin, 72: 104-125.
  • 39. Filipescu, R., Filipescu, S., 2014-2015. New data on the Early-Middle Badenian transition in the NW Transylvanian Basin (Romania) revealed by the planktonic foraminiferal assemblages. Studia UBB Geologia, 59: 39-44.
  • 40. Flower, B.P., Kennett, J.P., 1994. The middle Miocene climatic transition: East Antarctic ice sheet development, deep ocean circulation and global carbon cycling. Palaeogeography, Palaeoclimatology, Palaeoecology, 108: 537-555.
  • 41. Foresi, L.C., Verducci, M., Baldassini, N., Lirer, F., Mazzei, R., Gianfranco, S., Ferraro, L., Da Prato, S., 2011. Integrated stratigraphy of St. Peter's Pool section (Malta): new age for the Upper Globigerina Limestone member and progress towards the Langhian GSSP Stratigraphy, 8: 125-143.
  • 42. Fornaciari, E., Rio, D., Ghibaudo, G., Massari, F., laccarino, S., 1997. Calcareous plankton biostratigraphy of the Serravallian (Middle Miocene) stratotype section (Piedmont Tertiary Basin, NW Italy). Memoire di Scienze Geologiche, 49: 127-144.
  • 43. Fujiwara, O., Yanagisawa, Y., Irizuki, T., Shimamoto, M., Hayashi, H., Danhara, T., Fuse, K., Iwano, H., 2008. Chronological data for the Middle Miocene to Pliocene sequence around the southwestern Sandai Plain, with special reference to the uplift history of the Ou Backbone Range. Bulletin of the Geological Survey of Japan, 59: 423-438.
  • 44. Garecka, M., 2014. Biostratigraphy of the Middle Miocene deposits in the Trojanowice 2 borehole based on calcareous nannoplankton investigation (in Polish with English summary). Biuletyn Państwowego Instytutu Geologicznego, 459: 33-44.
  • 45. Garlicki, A., 1979. Sedimentation of Miocene salts in Poland (in Polish with English summary). Prace Geologiczne, 119.
  • 46. Garlicki, A., 1994. Formal lithostratigraphic units of the Miocene - Wieliczka Formation (in Polish). Przegląd Geologiczny, 42: 26-28.
  • 47. Gaździcka, E., 1994. Nannoplankton stratigraphy of the Miocene deposits in Tarnobrzeg area (northeastern part of the Carpathian Foredeep). Geological Quarterly, 38 (3): 553-570.
  • 48. Gonera, M., 1997. Miocene foraminiferal assemblages in the Gliwice area (Upper Silesia, Poland). Bulletin of the Polish Academy of Sciences, Earth Sciences, 45: 97-105.
  • 49. Gonera, M., 2001. Foraminiferida and paleoenvironment of the Badenian formations (Middle Miocene) in the Upper Silesia (Poland) (in Polish with English summary). Studia Naturae, 48.
  • 50. Gonera, M., 2013. Globorotaliid intervals of the sub-evaporite Badenian (Middle Miocene) in the Upper Silesia Basin (Central Paratethys, Poland). Geological Quarterly, 57 (4): 757-767.
  • 51. Gonera, M., Bukowski, K., 2012. Isotopic events in the Early/Middle Badenian (Miocene) of the Upper Silesia Basin (Central Paratethys). Geological Quarterly, 56: 561-568.
  • 52. Gonera, M., Kulka, A., 1979. The age and stratigraphic position of the Heterostegina sands, Miechów and Racławice region (in Polish with English summary). Zeszyty Naukowe AGH. Geologia, 5 (3): 65-71.
  • 53. Gonera, M., Peryt, T.M., Durakiewicz, T., 2000. Biostratigraphical and paleoenvironmental implications of isotopic studies (18O, 13C) of the middle Miocene (Badenian) foraminifers in the Central Paratethys. Terra Nova, 12: 231-238.
  • 54. Gonera, M., Peryt, T.M., Durakiewicz, T., 2003. Coiling direction in Globigerina bulloides of Middle Miocene age. Journal of Micropaleontology, 22: 141-146.
  • 55. Gonera, M., Wiewiórka, J., d'Obyrn, K., Bukowski, K., 2014. Wielician (Middle Badenian) foraminifers from the stratotype area - Wieliczka Salt Mine, Poland (Paratethys, Middle Miocene) Geological Quarterly, 58 (3): 427-438.
  • 56. Hilgen, F.J., Abels, H.A., Iaccarino, S., Krijgsman, W., Raffi, I., Sprovieri, R., Turco, E., Zachariasse, W.J., 2009. The Global Stratotype Section and Point (GSSP) of the Serravallian Stage (Middle Miocene). Episodes, 32: 152-166.
  • 57. Hofker, J., 1972. Is the direction of coiling in the early stages of an evolution of planktonic foraminifera at random? (50% right and 50% left). Revista Espańola de Micropaleontología, 4: 11-17.
  • 58. Hohenegger, J., Coric, S., Wagreich, M., 2014. Timing of the Middle Miocene Badenian stage of the Central Paratethys. Geologica Carpathica, 65: 55-66.
  • 59. Holbourn, A., Kuhnt, W., Schulz, M., Flores, J.-A., Andersen, N., 2007. Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion. Earth and Planetary Science Letters, 261: 534-550.
  • 60. Holcová, K., Demeny, A., 2012. The oxygen and carbon isotopic composition of Langhian foraminiferal tests as a paleoecological proxy in a marginal part of the Carpathian Foredeep (Czech Republic). Geologica Carpathica, 63: 121-137.
  • 61. Hüsing, S.K., Cascella, A., Hilgen, F.J., Krijgsman, W., Kuiper, K.F., Turco, E., Wilson, W., 2010. Astrochronology of the Mediterranean Langhian between 15.29 and 14.17 Ma. Earth and Planetary Science Letters, 290: 254-269.
  • 62. Iaccarino, S., 1985. Mediterranean Miocene and Pliocene planktic foraminifera. In: Planktonic Stratigaphy (eds. H.M. Bolli, J.B. Saunders and K. Perch-Nielsen): 283-314. The Cambridge University Press, Cambridge.
  • 63. Jacobs, E., Weissert, H., Shields, G., 1996. The Monterey event in the Mediteranean: a record from shelf sediments of Malta. Paleoceanography, 11: 717-728.
  • 64. Jenkins, D.G., 1967. Recent distribution, origin, and coiling ratio changes in Globorotalia pachydrma (Ehrenberg). Micropaleontology, 13: 195-203.
  • 65. Kennett, J.P., 1976. Phenotypic Variation in some recent and Late Cenozoic planktonic foraminifera. In: Foraminifera (eds. R.H. Hediey and C.G. Adams), 2: 111-170. Academic Press, London.
  • 66. Kováčová, P., Hudáčková, N., 2009. Late Badenian foraminifers from the Vienna Basin (Central Paratethys): stable isotope study and paleoecological implications. Geologica Carpathica, 60: 59-70.
  • 67. Kucera, M., Kennett, J.P., 2002. Causes and consequences of a middle Pleistocene origin of the modern planktonic foraminifer Neogloboquadrina pachyderma sinistral. Geology, 30: 539-542.
  • 68. Lehotayova, R., 1982. Miocene nannoplankton zones in West Carpathians. Zapadne Karpaty Seria Paleontologia, 8: 91-100.
  • 69. Lidz, B., 1972. Globorotalia crassaformis morphotype variation in Atlantic and Caribbean deep-sea cores. Micropaleontology, 18: 194-211.
  • 70. Lirer, F., laccarino, S., 2005. Integrated stratigraphy (cyclostratigraphy and biochronology) of late Middle Miocene deposits in the Mediterranean area and comparison with the North and Equatorial Atlantic oceans: synthesis of the major results. Terra Nova, 17: 338-349.
  • 71. Little, M.G., Schneider, R.R., Kroon, D., Price, B., Bickert, T., Wefer, G., 1997. Rapid paleoceanographic changes in the Benguela Upwelling System for the last 160,000 years as indicated by abundances of planktonic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130: 135-161.
  • 72. Łuczkowska, E., 1964. The micropaleontological stratigraphy of the Miocene in the region of Tarnobrzeg-Chmielnik (in Polish with English summary). Prace Geologiczne, 20.
  • 73. Łuczkowska, E., 1998. Marine Miocene deposits of the Paratethys in Poland. Abhandlungen Senckenbergischen Naturforschenden Gesellschaft, 549: 29-34.
  • 74. Majewski, W., 2010. Planktonic foraminiferal response to Middle Miocene coolíng in the Southern Ocean (ODP Site 747, Kerguelen Plateau). Acta Palaeontologica Polonica, 55: 541-560.
  • 75. Malmgren, B., Kennett, J.P., 1976. Biometric analysis of phenotypic variation in Recent Globigerina bulloides d'Orbigny in the southern Indian Ocean. Marine Micropaleontology, 1: 3-25.
  • 76. Miller, K.G., Mountain, G.S., the Leg 150 Shipboard Party, Members of the New Jersey Coastal Plain Drilling Project, 1996. Drilling and dating New Jersey Oligocene-Miocene sequences: ice volume, global sea level, and Exxon records. Science, 271: 1092-1095.
  • 77. Miller, K.G., Wright, J.D., Fairbanks, R.G., 1991. Unlocking the Ice House: Oligocene-Miocene oxygen isotopes, eustacy and marginal erosion. Journal of Geophysical Research, 96: 6829-6848.
  • 78. Murray, J.W., 1976. A method of determining proximity of marginal seas to an ocean. Marine Geology, 22: 103-119.
  • 79. Nagappa, Y., 1957. Directionof coiling in Globorotalia as an aid in correlation. Micropaleontology, 3: 393-398.
  • 80. Naidu, P.V., Malmgren, B.A., 1996. Relationship between Late Quaternary upwelling history and coiling properties of Neogloboquadrina pachyderma and Globigerina bulloides in the Arabian Sea. Journal of Foraminiferal Research, 26: 64-70.
  • 81. Olsson, R.K., 1970. Paleocene planktonic foraminiferal biostratigraphy and paleozoogeography of new Jersey. Journal of Paleontology, 44: 589-597.
  • 82. Oszczypko, N., Krzywiec, P., Popadyuk, l., Peryt, T.M., 2006. Carpathian Foredeep Basin (Poland and Ukraine): its sedimentary, structural, and geodynamic evolution. AAPG Memoir, 84: 293-350.
  • 83. Papp, A., Cicha, l., Seneš, J., 1978a. Gliederung des Badenian, Faunenzonen und Unterstufen. In: Chronostratigraphie und Neostratotypen: Miozän der Zentralen Paratethys, 6 (ed. E. Brestenská): 49-52 M4 Badenian (Moravien, Wielicien, Kosovien). VEDA SAV, Bratislava.
  • 84. Peryt, D., 1997. Calcareous nannoplankton stratigraphyofthe Middle Miocene in the Gliwice area (Upper Silesia, Poland). Bulletin of the Polish Academy of Sciences, Earth Sciences, 45: 119-131.
  • 85. Peryt, D., 2013. Foraminiferal record of the Middle Miocene climate transition prior to the Badenian salinity crisis in the Polish Carpathian Foredeep Basin (central Paratethys). Geological Quarterly, 57 (1): 141-164.
  • 86. Peryt, T.M., 2006. The beginning, development and termination of the Middle Miocene Badenian salinity crisis in Central Paratethys. Sedimentary Geology, 188-189: 379-396.
  • 87. Peryt, T.M., Karoli, S., Peryt, D., Petrichenko, O.l., Gedl, P., Narkiewicz, W., Ďurkovičová, J., Dobieszyńska, Z., 1997. Westernmost occurrence of the Middle Miocene Badenian gypsum in central Paratethys (Kobeřice, Moravia, Czech Republic). Slovak Geological Magazine, 3: 105-120.
  • 88. Peryt, T.M., Buła, Z., Hałas, S., Olszewska, B., Pluta, I., Słodkowska, B., 2005. Non-marine evaporites in the Lower Miocene of Upper Silesia (Carpathian Foreland Basin, Poland). Geologica Carpathica, 56: 327-336.
  • 89. Pfuhl, H.A., Shackleton, N.J., 2004. Changes in coiling direction, habitat depth and abundances in two menardellid species. Marine Micropaleontology, 50: 3-20.
  • 90. Popescu, Gh., Brotea, D.,1994. Evolutionof the Transylvanian foraminiferal assemblages during Late Oligocene and Middle Miocene. The Miocene from the Transylvanian Basin, Romania, Editura Carpatica Cluj-Napoca: 119-124.
  • 91. Reynolds, L.A., Thunell, R.C., 1986. Seasonal production and morphologic variation of Neogloboquadrina pachyderma (Ehrenberg) in the northeast Pacific. Micropaleontology, 32: 1-18.
  • 92. Rio, D., Cita, M.B., laccarino, S., Gelati, R., Gnaccolini, M., 1997. Langhian, Serravalian, and Tortonian historical stratotypes. In: Miocene Stratigraphy: an integrated Approach (eds. A. Montanari, G.S. Odin and R. Coccioni): 57-87. Elsevier.
  • 93. Rögl, F., 1985. Late Oligocene and Miocene planktic foraminifera of the Central Paratethys. In: Planktonic Stratigraphy (eds. H.M. Bolli, J.B. Saunders and K. Perch-Nielsen): 315-328. The Cambridge University Press, Cambridge.
  • 94. Rögl, F., 1998. Palaeogeographic considerations for Mediterranean and Paratethys seaways (Oligocene to Miocene). Annalen des Naturhistorischen Museums in Wien, 99A: 279-310.
  • 95. Rögl, F., Müller, C., 1978. Middle Miocene salinity crisis and paleogeography of the Paratethys (Middle and Eastern Europe). Initial Reports of the Deep Sea Drilling Project, Volume Leg 42A: 985-990.
  • 96. Rögl, F., Steininger, F.F., 1984. Neogene Paratethys, Mediterranean and Indo-Pacific seaways. In: Fossils and Climate (ed. P. Branchley): 171-200. Wiley.
  • 97. Rupp, Ch., Hohenegger, J., 2008. Paleoecology of planktonic foraminifera from the Baden-Sooss section (Middle Miocene, Badenian, Vienna basin, Austria). Geologica Carpathica, 59: 425-445.
  • 98. Saito, T., Maiya, S., 1973. Planktonic foraminifera of the Nishikurosawa Formation, Northeast Honsiu, Japan. Translations and Proceedings of the Paleontological Society of Japan, New Series, 91: 113-125.
  • 99. Schiebel, R., Hemleben, Ch., 2005. Modern planktic foraminifera. Paläontologische Zeitschrift, 79: 135-148.
  • 100. Scott, G.H., Bishop, S., Burt, B.J., 1990. Guide to some Neogene Globorotalid (Foraminiferida) from New Zealand. New Zealand Geological Survey Paleontological Bulletin, 61: 1-135.
  • 101. Seneš, J., 1971. Korrelation des Miozäns der Zentralen Paratethys (Stand 1970). Geologicky Zbornik, 22: 3-9.
  • 102. Simstich, J., Sarnthein, M., Erlenkeuser, H., 2003. Paired δ18O signals of Neogloboquadrina pachyderma (s) and Turborotalita quinqueloba show thermal stratification structure in Nordic Seas. Marine Micropaleontology, 48: 107-125.
  • 103. Steininger, F.F., Seneš, J., Kleeman, K., Rögl, F. eds., 1985. Neogene of the Mediterranean Tethys and Paratethys. Stratigraphic correlation tables and sediment distribution maps. Institute of Paleontology, University of Vienna.
  • 104. Szczechura, J., 1982. Middle Miocene foraminiferal biochronology and ecology of SE Poland. Acta Palaeontologica Polonica, 27: 125-130.
  • 105. Thiede, J., 1971. Variations in coiling ratios of Holocene planktonic foraminifera. Deep-Sea Research, 18: 823-831.
  • 106. Tolderlund, D.S., Bé, A.W.H., 1971. Seasonal distribution of planktonic foraminifera in the western North Atlantic. Micropaleontology, 17: 297-329.
  • 107. Vašiček, M., 1953. Changes in the ratio of sinistral and dextral individuals of the foraminifer Globorotalia scitula (Brady), and their use in stratigraphy. Sbornik Ustředniho Ustavu Geologíckoho Instituta. Oddil Paleontologicki, 20: 401-420.
  • 108. Vella, P., 1974. Coiling ratios of Neogloboquadrina pachyderma (Ehrenberg): variations in different size fractions. GSA Bulletin, 85: 1421-1424.
  • 109. Wilke, I., Meggers, H., Bickert, T., 2009. Depth habitats and seasonal distribution of recent planktic foraminifers in the Canary Islands region (290°) based on oxygen isotopes. Deep-Sea Research I, 56: 89-106.
  • 110. Winter, C.J., Pearson, P.N., 2001. Coiling direction in some Miocene planktonic foraminifera. Journal of Micropaleontology, 20: 29-30.
  • 111. Woodruff, F., Savin S.M., 1991. Mid-Miocene isotope stratigraphy in the deep sea: high resolution correlations, paleoclimatic cycles, and sediments preservation. Paleoceanography, 6: 755-806.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-55c9fee1-adc9-49a9-b0c5-74dfebdf96f2
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.