PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
2013 | 58 | 3 |

Tytuł artykułu

Morphological variability of the Paratethyan Oligocene–Miocene small reticulofenestrid coccolites and its paleoecological and paleogeographical implications

Autorzy

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
The analysis of size changes (length of placoliths, their width, length of central opening and its width) in elliptical reticulofenestrids from the NP25–NN5 zonal interval of the Central Paratethys allowed to dicriminate two size categories of placoliths: (i) small Reticulofenestra minuta (< 3.5 μm); (ii) Reticulofenestra haqii–pseudoumbilicus group (4–10.0 μm). The latter group appeared for the first time (FO, first occurrence) in the upper Egerian (size 4–7 μm) with the size of placoliths in this plexus increasing gradually. The FO of R. pseudoumbilicus > 8.0 μm has been established in the Zone NN2 while its FCO (first common occurrence) in the Zone NN5. This study shows that the FOs of size−defined morphotypes of the R. haqii–pseudoumbilicus group differ in the Central Paratethys and oceanic realm. Blooms of R. minuta at the Oligocene–Miocene boundary and in the Early Middle Miocene may be correlated with the incoming of warm water into the higher latitude Central Paratethys basins during connection with the Mediterranean Sea. Transgression favored the expansion of near−shore areas associated probably by some short−time oscillations of salinity. The FO of R. haqii–pseudoumbilicus group and the FO of R. pseudoumbilicus > 8.0 μm can be correlated with the opening of new pathways between the Mediterranean and the Central Paratethys. Gradual size changes in the R. haqii–pseudoumbilicus group probably reflect climatic changes: the decrease of coccolith size in the late Egerian may reflect cooling (Mi1 event) while the increase in coccolith size in the interval from the FO of Helicosphaera ampliaperta to the FO of Sphenolithus heteromorphus occurred due to warming. Two size categories of placoliths in the R. haqii–pseudoumbilicus group (3.5–6 μm and 6–8 μm) recorded in the interval from Zone NN1 to the lower part of the Zone NN2 may represent seasonal populations.

Wydawca

-

Rocznik

Tom

58

Numer

3

Opis fizyczny

p.651-668,fig.,ref.

Twórcy

autor
  • Department of Geology and Paleontology, Charles University in Prague, Albertov 6, 128 43 Praha 2, Czech Republic

Bibliografia

  • Andreyeva−Grigorovich, A.S., Kulchytsky, Y.O., Gruzman, A.D., Lozonyak, P.Y., Petrashkevich, M.I., Portnyagina, L.O., Ivanina, A.V., Smirnov, S.E., Trofimovich, N.A., and Savitskaya, N.A. 1997. Regional stratigraphic scheme of Neogene formations of the Central Paratethys of Ukraine. Geologica Carpathica 48: 123–136.
  • Andreyeva−Grigorovich, A.S., Oszczypko, N., Slaczka, A., Oszczypko-Clowes, M., Savitskaya, N.A., and Trofimovich, N.A. 2008. New data on the stratigraphy of the folded Miocene Zone at the front of the Ukrainian Outer Carpathians. Acta Geologica Polonica 58: 325–354.
  • Backman, J. 1978. Late Miocene–Early Pliocene nannofossil biochronology and biogeography in the Vera Basin, SE Spain. Stockholm Contributions in Geology 32: 93–114.
  • Backman, J. 1980. Miocene–Pliocene nannofossils and sedimentation rates in the Hatton−Rockall Basin, NE Atlantic Ocean. Stockholm Contributions in Geology 36: 1–91.
  • 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 Science (Geologische Rundschau) 95: 119–142.
  • Báldi T. 1986. Mid−tertiary Stratigraphy and Paleogeographic Evolution of Hungary. 201 pp. Akademiai Kiado, Budapest.
  • Beaufort, L. and Aubry, M.−P. 1992. Palaeoceanographic implications of a 17 m.y. long record of high−latitude Miocene calcareous nannoplankton fluctuations. Proceeding of Ocean Drilling Program, Scientific Results 120: 530–549.
  • Berggren, W.A., Kent, D.V., Swisher III., C.C., and Aubry, M.−P. 1995. A revised cenozoic geochronology and chronostratigraphy. In: W.A. Berggren, D.V. Kent, and J. Hardenbol (eds.), Geochronology, Time Scale and Global Stratigraphic Correlations: A Unified Temporal Framework for an Historical Geology. Society of Economic Paleontologists and Mineralogists, Special Publication 54: 129–212.
  • Bicchi, E., Ferrero, E., and Gonera, M. 2003. Palaeoclimatic interpretation based on Middle Miocene planktonic Foraminifera: the Silesia Basin (Paratethys) and Monferrato (Tethys) records. Palaeogeography, Palaeoclimatology, Palaeoecology 196: 265–303.
  • Böhme, M. 2003. The miocene climatic optimum: evidence from ectothermic vertebrates of Central Europe. Palaeogeography, Palaeoclimatology, Palaeoecology 195: 389–401.
  • Bollmann, J., Baumann, K.H., and Thierstein, H.R. 1998. Global dominance of Gephyrocapsa coccoliths in the late Pleistocene: Selective dissolution, evolution, or global environmental change? Paleoceanography 13: 517–529.
  • Brzobohatý, R. 1987. Contribution to paleogeography of the Miocene basins of the Central Paratethys from otolith fauna. Miscellanea Micropalaeontologica II/2, Knihovnička zemního plynu a nafty 6b: 101–111.
  • Chira, C. 2004. Early Miocene calcareous nannofossils assemblages from Transylvania. Acta Paleontologica Romaniae 4: 81–88.
  • Chlupáč, I., Brzobohatý, R., Kovanda, J., and Stráník, Z. 2002. Geologická minulost České republiky. 436 pp. Academia, Praha.
  • Cita, M.B., Wright, R.C., Ryan, W.B.F., and Longinelli, A. 1978. Messinian paleoenvironments, Initial Reports of the Deep Sea Drilling Project 42A: 1003–1035.
  • Ćorić, S. and Hohenegger, J. 2008. Quantitative analyses ofcalcareous nannoplankton assemblages from the Baden−Sooss section (Middle Miocene of Vienna Basin, Austria). Geologica Carpathica 59: 447–460.
  • Ćorić, S. and Rögl, F. 2004. Roggendorf−1 borehole, a key−section for Lower Badenian transgressions and the stratigraphic positin of the Grund Formation (Molasse Basin, Lower Austria).Geologica Carpathica 55: 165–178.
  • Ćorić, S. and Švábenická, L. 2004. Calcareous nannofossil biostratigraphy of the Grund Formation (Molasse Basin, Lower Austria). Geologica Carpathica 55: 147–155.
  • Flores, J.A., Sierro, F.S., Francés, G., Vasquez, A., and Zamarreno, I. 1997. The last 100,000 years in the western Mediterranean: Sea surface water and frontal dynamics as revealed by coccolithophores. Marine Micropaleontology 29: 351–366.
  • Fornaciari, E. and Rio, D. 1996. Latest Oligocene to early middle Miocene quantitative calcareous nannofossil biostratigraphy in the Mediterranean region. Micropaleontology 42: 1–36.
  • Fornaciari, E., Di Stefano, A., Rio, D., and Negri, A. 1996. Middle Miocene quantitative calcareous nannofossil biostratigraphy in the Mediterranean region. Micropaleontology 42: 37–63.
  • Gartner, S., Chen, M.P., and Stanton, R.J. 1983. Late Neogene nanofossil biostratigraphy and paleoceanography of the northeastern Gulf of mexico and adjacent areas. Marine Micropaleontology 8: 17–50.
  • Gonera, M., Peryt, T.M., and 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.
  • Halásová, E., Hudáčková , N., Holcová, K., Vass, D., Elečko, M., and Pereszlényi, M. 1996. Sea ways connecting the Fiľakovo−Pétervasara Basin with the Eggenburgian/Burdigalian open sea. Slovak Geological Magazine 2: 125–136.
  • Hallock, P. 1987. Fluctuations in the trophic resource continuum: a factor in global diversity cycles? Paleooceanography 2: 457–471.
  • Haq, B.U. 1980. Biogeographic history of the Miocene calcareous nannoplankton and paleoceanography of the Atlantic Ocean. Micropaleontology 26: 414–443.
  • Haq, B.U., Hardenbol, J., and Vail, P.R. 1988. Mesozoic and Cenozoic chronostratigraphy and cycles of sea−level change. Society of Economic Paleontologists and Mineralogists, Special Publication 42: 71–108.
  • Harzhauser, M. and Piller, W.E. 2007. Benchmark data of a changing sea—palaeogeograpgy, palaebiogeography and events in the Central Paratethys during the Miocene. Palaeogeography, Palaeoclimatology, Palaeoecology 253: 8–31.
  • Hohenegger, J., Andersen, N., Báldi, K., Ćorić, S,, Pervesler, P., Rupp, C., and Wagreich, M. 2008. Paleoenvironment of the Early Badenian (Middle Miocene) in the southern Vienna Basin (Austria)—multivariate analysis of the Baden−Sooss section. Geologica Carpathica 59: 461–487.
  • Hohenegger, J., Coric, S., Khatun, M., Pervesler, P., Rögl, F., Rupp, Ch., Selge, A., Uchman, A., and Wagreich, M. 2009. Cyclostratigraphic dating in the Lower Badenian (Middle Miocene) of the Vienna Basin (Austria)—the Baden−Sooss core. International Journal of Earth Sciences 98: 915–930.
  • Holcová, K. 2001. New methods in foraminiferal and calcareous nannoplankton analysis and evolution of Oligocene and Miocene basins of the Southern Slovakia. Slovak Geological Magazine 7: 19–41.
  • Holcová, K. 2002. Calcareous nannoplankton from the Eggenburgian stratotypes (Lower Miocene, Central Paratethys). Geologica Carpathica 53: 381–390.
  • Holcová, K. 2005. Quantitative calcareous nannoplankton biostratigraphy of the Oligocene/Miocene boundary interval in the northern part of the Buda Basin (Central Paratethys). Geological Quarterly 49: 263–274.
  • Holcová, K. 2008. Foraminiferal species diversity in the Central Paratethys—a reflection of global or local events?Geologica Carpathica 59: 71–85.
  • Howe, R.W. and Sblendorio−Levy, J. 1998. Calcareous nannofossil biostratigraphy and sediment accumulation of turbidite sequences on the Madeira abyssal plain, sites 950–952. In: P.P.E. Weaver, H.U. Schmincke, and J.V. Firth (eds.), Proceeding of the Ocean Drilling Program, Scientific Results 157: 501–520.
  • Jamrich, M. and Halásová, E. 2010. The evolution of the Late Badenian calcareous nannofossil assemblages as a reflexion of the palaeoenvironmental changes of the Vienna Basin (Devínska Nová Ves−clay pit). Acta Geologica Slovaca 2: 123–140.
  • Kameo, K. 2002. Late Pliocene Caribbean surface water dynamics and climatic changes based on calcareous nannofossil records. Palaeogeography, Palaeoclimatology, Palaeoecology 179: 211–226.
  • Kováč, M. 2000. Geodynamic, Paleogeographical and Structural Development of the Carpathian–Pannonian Region During the Miocene. 202 pp. Veda, Bratislava.
  • Kroh, A. and Harzhauser, M. 1999. An echinoderm fauna from the Lower Miocene of Austria: Paleoecology and implications for Central Paratethys paleogeography. Annalen des Naturhistorischen Museums in Wien 101A: 145–191.
  • Kürschner, W.M., Kvaček, Z., and Dilcher, D.L. 2008. The impact of Miocene atmospheric carbon dioxine fluctuations on climate and the evolution of terrestrial ecosystems. Proceedings of the National Academy of Sciences of the United States of America 105: 449–453.
  • Kvaček, Z. and Teodoridis, V. 2007. Tertiary macrofloras of the Bohemian Massif: a review with correlations within Boreal and Central Europe. Bulletin of Geosciences 82: 383–408.
  • Lehotayová, R. 1975. Reticulofenestra excavata n. sp. from the Eggenburgian to Karpatian of Central Slovakia. Západné Karpaty, séria paleontológia 2: 39–40.
  • Lehotayová, R. 1982. Miocene nannoplankton zones in west Carpathians. Západné Karpaty, séria paleontológia 8: 91–110.
  • Lehotayová, R. 1984. Lower Miocene calcareous nannoflora of the West Carpathians. Západné Karpaty, séria paleontológia 9: 99–110.
  • Lourens, L., Hilgen, F., Shackleton, N.J., Laskar, J., and Wilson, D. 2004. The Neogene period. In: F. Gradstein, J. Ogg, and A. Smith (eds.), A Geological Time Scale, 409–440. Cambridge University Press, Cambridge.
  • Mandic, O. and Steininger, F.F. 2003. Computer−based mollusc stratigraphy—a case study from the Eggenburgian (Lower Miocene) type region (NE Austria). Palaeogeography, Palaeoclimatology, Palaeoecology 197: 263–291.
  • Martini, E. 1971. Standard Tertiary and Quaternary calcareous nanoplankton zonation. In: A. Farinacci (ed.), Proceeding of 2nd Planktonic Conference, Roma 1970, Roma, 739–785. Tecnoscienza, Rome.
  • Márton, E., Vass, D., and Túnyi, I. 1995. The Late Tertiary rotation of the megaunit Pelsö and the adjecent West Carpathians area. Knihovnička Zemní Plyn a Nafta 16: 97–108.
  • Marunteanu, M. 1992. Distribution of the Miocene calcareous nannofossils in the Intra− and Extra− Carpathian areas of Rumania. Knihovnička Zemní Plyn Nafta 14b (2): 247–262.
  • Marunteanu, M. 1999. Litho−and biostratigraphy (calcareous nannoplankton) of the Miocene deposits from the Outer Moldavides. Geologica Carpathica 50: 313–324.
  • McIntyre, A. and Be, A.W.H. 1967. Coccolithus neohelis sp.n. a coccolith fossil type in contemporary seas. Deep−Sea Research 14: 369–371.
  • Molčíková, V. 1983. The Karpatian and Lower Badenian Calcareous nannoflora of the Carpathian Foredeep in Moravia. Knihovnička Zemní Plyn a Nafta 4: 283–304.
  • Molčíková, V. and Straník, Z. 1987. Calcareous nannoplankton from the Ždánice−Hustopeče Formation and their relation to underlying formations. Knihovnička Zemní Plyn a Nafta 6b: 59–76.
  • Piller, W.E., Harzhauser, M., and Mandic, O. 2007. Miocene Central Paratethys stratigraphy—current status and future directions. Stratigraphy 4: 151–168.
  • Planderová, E. 1990. Miocene Microflora of Slovak Central Paratethys and its Biostratigraphical Significance. 144 pp. Geologický Ústav Dionýza Štúra, Bratislava.
  • Popov, S.V., Rögl, F., Rozanov, A.Y., Steininger, F.F., Shcherba, I.G., and Kováč, M. 2004. Lithological−Paleogeographic maps of Paratethys. Courier Forschungsinstitut Senckenberg 250: 1–46.
  • Pujos, A. 1985. Cenozoic nannofossils, central equatorial Pacific, deep sea Drilling Project Leg 85. In: L. Mayer and F. Theyer (eds.), Initial Reports of the Deep Sea Drilling Project 85: 581–608.
  • Raffi, I. and Flores, J.A. 1995. Pleistocene through Miocene calcareous nannofossils from Eastern Equatorial Pacific Ocean (Leg 138). In: N.G. Pisias, L.A. Mayer, T.R. Janecek, A. Palmer−Julson, and T.H. van Andel (eds.), Proceedings of the Ocean Drilling Program, Scientific Results 138: 233–286.
  • Raffi, I., Rio, D., d`Atri, A., Fornaciari, E., and Rochetti, S. 1995. Quantitative distribution patterns and biomagnetostratigraphy of middle and late Miocene calcareous nannofossils from western equatorial Indian and Pacific Oceans (Legs 115, 130, and 138). In: N.G. Pisias, L.A. Mayer, T.R. Janecek, A. Palmer−Julson, and T.H. van Andel (eds.), Proceeding of Oceanic Drilling Project, Scientific Results 138: 479–502.
  • Rahman, A. and Roth, P.H. 1990. Late Neogene paleoceanography and paleoclimatology of the Gulf of Aden region based on calcareous nannofossils. Paleoceanography 5: 91–107.
  • Rio, D., Fornaciari, E., and Raffi, I. 1990. Late Oligocene through early Pleistocene calcareous nannofossils from western equatorial Indian Ocean (Leg 115). Proceedings of the Ocean Drilling Program, Scientific Results 115: 175–221.
  • Rögl, F. 1998. Paleogeographic considerations for Mediterranean and Paratehys seaways (Oligocene to Miocene). Annalen des Naturhistorische Museum in Wien 99A: 279–310.
  • Rögl, F. 1999. Mediterranean and Paratethys. facts and hypotheses of an Oligocene to Miocene paleogeography (short overview). Geologica Carpathica 50: 339–349.
  • Rögl, F. and Steininger, F.F. 1983. Vom Zerfall der Tethys zu Mediterran und Paratethys—Die neogene Palaegeographie and Palinspastik des zirkummediterranen Raumes. Annalen des Naturhistorische Museum in Wien 85/A: 135–164.
  • Rögl, F., Ćorić, S., Daxner−Höck, G., Harzhauser, M., Mandić, O., Švábenická, L., and Zorn, I. 2003. Correlation of the Karpatian Stage. In: R. Brzobohatý, I. Cicha, M. Kováč, and F. Rögl (eds.), The Karpatian—a Lower Miocene Stage of the Central Paratethys, 27—35. Masaryk University, Brno.
  • Seneš, J. 1961. Paläogeographie des Westkarpatischen Raumes in Beziehung zur übringen Paratethys in Miozän. Geologické práce 60: 160–194.
  • Spezzaferri, S. and Ćorić, S. 2001. Ecology of Karpatian (Early Miocene) foraminifera and calcareous nannoplankton from Laa an der Thaya, Lower Austria: a statistical approach. Geologica Carpathica 52: 361–374.
  • Spezzaferri, S., Ćorić, S., and Stingl, K. 2009. Palaeoenvironmental reconstruction of the Karpatian–Badenian (Late Burdigalian–Early Langhian) transition in the Central Paratethys. A case study from theWagna Section (Austria). Acta Geologica Polonica 59: 523–544.
  • Švábenická, L. 2002. Calcareous nannofossils of the Upper Karpatian and Lower Badenian Deposits in the Carpathian Foredeep, Moravia (Czech Republic). Geologica Carpathica 53: 197–210.
  • Švábenická, L., Coric, S., Andreyeva−Grigorovich, A.S., Halásová, E., Marunteanu, M., Nagymarosi, A., and Oszcypko−Clowes, M. 2003. Central Paratethys Karpatian Calcareous Nannofossils. R. Brzobohatý, I. Cicha, M. Kováč, and F. Rögl (eds.), The Karpatian—a Lower Miocene Stage of the Central Paratethys, 151–168. Masaryk University, Brno.
  • Teodoridis, V. 2007. Overview of macrofloras from the Most Basin (Czech Republic) and their phytostratigraphical correlation within Central and Boreal Europe. In: Organizing Committee in Bonn (eds.), Terra Nostra 2, IPC−XII /IOPC−VIII Bonn, Germany 2008, Abstract Volume, 280. GeoUnion Alfred−Wegener−Stiftung, Berlin.
  • Teodoridis, V. and Kvaček, Z. 2006. Palaeobotanical research of the Early Miocene deposits overlying the main coal seam (Libkovice and Lom Mbs.) in the Most Basin (Czech Republic). Bulletin of Geosciences 81: 93–113.
  • Teodoridis, V., Mazouch, P., Spicer, R.A., and Uhl, D. 2011. Refining CLAMP—Investigations towards improving the Climate Leaf Analysis Multivariate Program. Palaeogeography, Palaeoclimatology, Palaeoecology 299: 39–48.
  • Tomanová Petrová, P. and Švábenická, L. 2007. Lower Badenian biostratigraphy and paleoecology: a case study from the Carpathian Foredeep (Czech Republic). Geologica Carpathica 58: 333–352.
  • Váňová, M. 1975. Lepidocyclina and Miogypsina from the facistratotype localities Budikovany and Bretka (South Slovakia). In: T. Báldi and J. Seneš (eds.), OM—Egerien, Chronostratigraphie und Neostratotypen, 315–339. Slovak Academy of Sciences, Bratislava.
  • Vass, D. 1995. Global sea level changes reflected on Northern margin of the Hungarian Paleogene the Filakovo and Novohrad (Nograd) Lower Miocene Basin (South Slovakia). Mineralia slovaca 27: 193–206.
  • Vass, D. 1996. The origin and disappearance of Hungarian Paleogene Basins and short−term Lower Miocene Basin in Northern Hungary and Southern Slovakia. Slovak Geological Magazine 1: 81–95.
  • Vass, D. and Elečko, M. 1982. Litostratigraphic units of the Kiscellian-Eggenburgian of the Rimava Basin and Cerová Upland. Geologické Práce, Správy 77: 111–124.
  • Vass, D., Elečko, M., Pristaš, J., Lexa, J., Hanzel, V., Mordlitba, I., Jánová, V., Bodnár, J., Husák, Ľ., Filo, M., Májovský, J., and Linkeš, V. 1989. Geology of the Rimavska Kotlina Depression. 160 pp. Geologický Ústav Dionýza Štúra, Bratislava.
  • Vass, D., Hók, J., Kováč, P., and Elečko, M. 1993. Succesion of the Paleogene and Neogene tectonic events in the light of tectonical analysis. Mineralia Slovaca 25: 79–82.
  • Vass, D., Konečný, V., and Šefara, J. 1979. Geology of the Ipeľ basin and Krupinská Planina Upland. 227 pp. Geologický Ústav Dionýza Štúra, Bratislava.
  • Vass, D., Elečko, M., Konečný, V., Krippel, M., Kubeš, P., Lexa, J., Pristaš, J., Zakovič, M., Vozár, J., Vozárová, A., Bodnár, J., Husák, Ľ., Filo, M., Lacika, J., and Linkeš, V. 2007. Geology of Lučenecká kotlina Depression and Cerová vrchovina Upland. 284 pp. Geologický Ústav Dionýza Štúra, Bratislava.
  • Vávra, N. 1979. Die Bryozoenfaunen des österreichischen Tertiärs. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 157: 366–392.
  • Wade, B.S. and Bown, P.R. 2006. Calcareous nannofossils in extreme environments: the Messinian Salinity Crisis, Polemi Basin, Cyprus. Palaeogeography, Palaeoclimatology, Palaeoecology 233: 271–286.
  • Wells, P. and Okada, H. 1997. Response of nannoplankton to major changes in seasurface temperatrure and movements of hydrological fronts over site DSDP 594 (south Chatham Rise, southeastern New Zealand), during the last 130 kyr. Marine Micropalaeontology 32: 341–363.
  • Young, Y.R. 1990. Size variations of neogene Reticulofenestra coccoliths from Indian DSDP cores. Journal of Micropaleontology 9: 71–86.
  • Young, Y. 1999. Neogene. In: P.R. Bown (ed.), Calcareous Nannofossil Biostratigraphy, 225–265. Cambridge University Press, Cambridge.
  • Zachos, J.M., Pagani, L., Sloan, E.T., and Billups, K. 2001. Trends, rhythms, and aberrations in global climate 65 Ma to present. Science 292: 686–693.
  • Zágoršek, K., Holcová, K., and Trasoň, T. 2008. Bryozoan event from Middle Miocene (Early Badenian) lower neritic sediments from the locality Kralice nad Oslavou (Central Paratethys, Moravian part of the Carpathian Foredeep). International Journal of Earth Sciences (Geologische Rundschau) 97: 835–850.
  • Zágoršek, K., Nehyba, S., Holcová, K., Hladiková, Š., and Kroh A. 2009. Fauna from the Middle Miocene (Early Badenian) sediments from the section Kralice nad Oslavou (Central Paratethys, Moravian part of the Carpathian Foredeep). Bulletin of Geosciences 84: 465–496.
  • Zágoršek, K. and Holcová, K. 2009: The oldest Early Badenian Bryozoa event in the Carpathian Foredeep from the Přemyslovice (PY−1, PY−2) boreholes. Přírodovědné Studie Muzea Prostějovska 10–11: 53–59.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-29eefed0-d522-41d0-9db5-8dbb24a5c808
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.