Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
Nummulites-Discocyclina bioclastic packstone and Discocyclina rudstone occur in the transgressive sequence of the Middle–Upper Eocene deposits in the Tatra Mts. The succession of the studied facies is a direct response to a rapid environmental change, related to progressive deepening. Facies transition from Nummulites- Discocyclina bioclastic packstone of proximal mid-ramp to Discocylina rudstone of distal mid- and outer-ramp is an exemplary record of a deposition during deepening conditions. Increasing of diversity of the genus Discocyclina, decreasing of diversity of other foraminifera up the section and vertical variation of orthophragminid mor- photypes from the ovate- through saddle- to the disc-shaped tests are related to deepening and shadowing of the depositional environment.
Wydawca
Czasopismo
Rocznik
Tom
Strony
199--205
Opis fizyczny
Bibliogr. 51 poz., rys., tab., wykr.
Twórcy
autor
autor
autor
- Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland, elżbieta.machaniec@uj.edu.pl
Bibliografia
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- 3.Aigner, T., 1985. Biofabrics as dynamic indicators in nummulite accumulations. Journal of Sedimentary Petrology, 55: 131- 134.
- 4.Alexandrowicz, S. W. & Geroch, S., 1963. Association de petits Foraminiferes dans FEocene de la Tatra. (In Polish, French summary). Rocznik Polskiego Towarzystwa Geologicznego, 33: 219-228.
- 5.Bac-Moszaszwili, M., Burchart, J., Głazek, J., Iwanow, A., Jaroszewski, W., Kotański, Z., Lefeld, J., Mastella, L., Ozimkowski, W., Roniewicz, P., Skupiński, A. & Westwalewicz-Mogilska, E., 1979. Geological map of the Polish Tatra Mountains 1:30 000. (In Polish, English summary). Wydawnictwa Geologiczne, Warszawa.
- 6.Bartholdy, J., Bellas, S. M., Ćosović, V., Fućek, V. P. & Keupp, H., 1999. Process controlling Eocene mid-latitude larger foraminifera accumulations: modeling of the strati graphic architecture of a forearc basin (Podhale Basin, Poland). Geologica Carpathica, 50: 435-448.
- 7.Bartholdy, J., Bellas, S. M., Mertmann, D., Machaniec, E. & Manutsoglu, E., 1995. Fazies-Entwicklung und Biostratigraphie einer Sequenz eozäner Sedimente im Steinbruch Pod Capkami, Tatra Gebirge, Polen. Berliner Geowissenschaftlische Abhandlungen, 16: 409-425.
- 8.Bassi, D., 2005. Larger foraminiferal and coralline algal facies in an Upper Eocene storm influenced, shallowwater carbonate platform (Colli Berici, north-eastern Italy). Palaeogeography, Palaeoclimatology, Palaeoecology, 226: 17-35.
- 9.Beavington-Penney, S. J., 2004. Analysis of the effects of abrasion on the test of Palaeonummulites venosus: Implications for the origin of nummulithoclastic sediments. Palaios, 19: 143- 155.
- 10.Beavington-Penney, S. J. & Racey, A., 2004. Ecology of extant nummulitids and other larger benthic foraminifera: application in palaeonvironmnetal analysis. Earth-Science Reviews, 67: 219-265.
- 11.Beavington-Penney, S. J., Wright, V. P. & Racey, A., 2006. The Middle Eocene Seeb Formation of Oman; an investigation of a cyclicity, stratigraphic completeness and accumulation rates in shallow marine carbonate settings. Journal of Sedimentary Research, 76: 1137-1161.
- 12.Bieda, F., 1963. Larger Foraminifers of the Tatra Eocene. (In Polish, English summary). Prace Instytutu Geologicznego, 37: 3-215.
- 13.Ćosović, V. & Drobne, K., 1995. Palaeoecological significance of morphology of orthophragminids from the Istrian Peninsula (Croatia and Slovenia). Geobios, 18: 93-99.
- 14.Ćosović, V., Drobne, K. & Moro, A., 2004. Palaeoenvironmental model of Eocene foraminiferal limestones of the Adriatic carbonate platform (Istrian Peninsula). Facies, 50: 61-75.
- 15.Fermont, W. J. J., 1982. Discocyclinidae from Ein Avedat (Istrael). Utrecht Micropaleontological Bulletins, 27: 1-173.
- 16.Ferrandez-Cañadell, C., 1998. Morphostructure and paleobiology of Mesogea orthophragminids (Discocyclinidae and Orbito-clipeidae Foraminifera). Acta Geologica Hispanica, 31: 183-189.
- 17.Ferrandez-Cañadell, C. & Serra-Kiel, J., 1992. Morphostructure and paleobiology of Discocyclina Gümbel, 1870. Journal of Foraminiferal Research, 22: 147-165.
- 18.Geel, T., 2000. Recognition of stratigraphic sequences in carbonate platform and slope deposits: empirical models based on microfacies analysis of Paleogene deposits in of Cenozoic carbonate depositional facies. Palaios, 1: 55-64.
- 19.Hallock, P., 1979. Trends in test shape with depth in large, symbiont-bearing Foraminifera. Journal of Foraminiferal Research, 9: 61-69.
- 20.Hallock, P., 1985. Why are Larger Foraminifera large? Paleobiology, 11: 195-208.
- 21.Hallock, P., 1999. Symbiont-bearing Foraminifera. In: Sen Gupta, B. K. (ed.), Modern Foraminifera. Kluwer, Dordrecht: 123-139.
- 22.Hallock, P., Forward, L. B. & Hansen, H. J., 1986. Environmental influence of test shape in Amphistegina. Journal of Foraminiferal Research, 16: 224-231.
- 23.Hallock, P. & Glenn, C. E., 1986. Larger Foraminifera: A tool for paleoenvironmental analysis of Cenozoic carbonate depositional facies. Palaios, 1: 55-64.
- 24.Hallock, P. & Pomar, L., 2008. Cenozoic Evolution of Larger Benthic Foraminifers: Paleoceanographic Evidence for Changing Habitats. In: Proceedings of the 11th International Coral Reef Symposium, Ft. Lauderdale, Florida, 7-11 July 2008. Session number 1: 16-20.
- 25.Hohenegger, J., 2004. Depth coenoclines and environmental considerations of Western Pacific larger foraminifera. Journal of Foraminiferal Research, 34: 9-33.
- 26.Hohenegger, J., 2005. Estimation of environmental paleogradient values based on presence/absence data: a case study using benthic foraminifera for paleodepth estimation. Palaeogeography, Palaeoclimatology, Palaeoecology, 217: 115-130.
- 27.Hohenegger, J., 2009. Functional shell geometry of symbiont-bearing benthic Foraminifera. Galaxea, Journal of Coral Reef Studies, 11:81-89.
- 28.Hohenegger, J. & Yordanova, E., 2001. Displacement of larger foraminifera at the western slope of Motobu Peninsula (Okinawa, Japan). Palaios, 16: 53-72.
- 29.Hottinger, L., 1983. Processes determining the distribution of larger foraminifera in space and time. Utrecht Micropaleontological Bulletins, 30: 239-253.
- 30.Hottinger, L., 1997. Shallow benthic foraminiferal assemblages as signals for depth of their deposition and their limitations. Bulletin de la Société Géologique de France, 168: 491-505.
- 31.Jach, R., Machaniec, E., Uchman, A., in press. The trace fossil Nummipera eocenica from the Eocene nummulitic limestones, Tatra Mts., Poland: morphology and palaeoenvironmental implications. Lethaia.
- 32.Jorry, J. S., Hasler, C. A. & Davaud, E., 2006. Hydrodynamic behavior of Nummulites: implications for depositional models. Facies, 52: 221-235.
- 33.Kulka, A., 1985. Arni sedimentological model in the Tatra Eocene. Kwartalnik Geologiczny, 29: 31-64.
- 34.Larsen, A. R., 1976. Studies of recent Amphistegina: taxonomy and some ecological aspects. Israel Journal of Earth Sciences, 25: 1- 26.
- 35.Larsen, A. R. & Drooger, C. W., 1977. Relative thickness of the test in Amphistegina species from the Gulf of Elat. Utrecht Micropaleontological Bulletins, 15: 225-239.
- 36.Less, G., 1987. Paleontology and stratigraphy of the European Orthophragminae. Geologica Hungarica, Series Palaeontologica, 51: 1-373.
- 37.Nebelsick, J. H., Rasser, M. W. & Bassi, D., 2005. Facies dynamics in Eocene to Oligocene circum alpine carbonates. Facies, 51: 197-216.
- 38.Neumann, M., 1958. Revision des Orbitoidides du Cretacé et de l'Eocene en Aquitaine Occidentale. Mémoires de la Société Géologique de France, 38, 1-174.
- 39.Olempska, E., 1973. The genus Discocyclina (Foraminiferida) from the Eocene of the Tatra Mts, Poland. Acta Palaeontologica Polonica, 18: 71-98.
- 40.Olszewska, B., 2009. Small foraminifera of "Nummulitic Eocene" of the Tatra Mts. - stratigraphy and palaeoenvironment. (In Polish, English abstract). Przegląd Geologiczny, 57: 703-713.
- 41.Olszewska, B. W. & Wieczorek, J., 1998. The Paleogene of the Podhale Basin (Polish Inner Carpathians) - micropaleontological perspective. Przegląd Geologiczny, 46: 721-728.
- 42.Papazzoni, C. A., 1994. Macroforaminifers and paleoenviron-ments near the Middle-Upper Eocene boundary in the Mos-sano section (Berici Mts., Vicenza, northern Italy). In: Matteucci, R., Carboni, M. G. & Pignatti, J. S. (eds), Studies on Ecology and Paleoecology of Benthic Communities. Bollettino della Societf Paleontologica Italiana Special Volume, 2: 203-212.
- 43.Passendorfer, E., 1959. Eocene palaeogeography of the Tatra Island. (In Polish, English summary). Biuletyn Instytutu Geologicznego, 149:259-271.
- 44.Pomar, L., 2001. Types of carbonate platforms, a genetic approach. Basin Research, 13: 313-334.
- 45.Racey, A., 2001. A review of Eocene nummulite accumulations: Structure, formation and reservoir potential. Journal of Petroleum Geology, 24: 79-100.
- 46.Radomski, A., 1959. Podhale flysch sedimentation. (In Polish, English summary). Acta Geologica Polonica, 8: 335409.
- 47.Reiss, Z. & Hottinger, L., 1984. The Gulf of Aqaba; Ecological Micropaleontology. Springer, Berlin, 354 pp.
- 48.Renema, W., 2005. Depth estimation using diameterthickness ratios in larger benthic foraminifera. Lethaia 38: 137-141.
- 49.Roniewicz, P., 1969. Sedimentation of the Nummulite Eocene in the Tatra. (In Polish, English summary). Acta Geologica Polonica, 19: 503-608.
- 50.Serra-Kiel, J., Hottinger, L., Caus, E., Drobne, K., Ferrandez, C., Kumar Jauhri, A., Less, G., Pavlovec, R., Pignatti, J., Samso, J. M., Schaub, H., Sire, E., Strougo, A., Tambareau, Y., Tosquella, Y. & Zakrevskaya, E., 1998. Larger foraminiferal biostratigraphy of the Tethyan Paleocene and Eocene. Bulletin de la Société Géologique de France, 169: 281-299.
- 51.Yordanova, E. K. & Hohenegger, J., 2002. Taphonomy of larger foraminifera: Relationships between living individuals and empty tests on flat reef slopes (Sesoko Island, Japan). Facies, 46: 169-203.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS6-0036-0036