Trace fossils from the Lower-Middle Jurassic Bardas Blancas Formation, Neuquen Basin, Mendoza Province, Argentina

Czasopismo : Acta Geologica Polonica
Tytuł artykułu : Trace fossils from the Lower-Middle Jurassic Bardas Blancas Formation, Neuquen Basin, Mendoza Province, Argentina

Autorzy :
Grabowski, J.
Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland, jgra@pgi.gov.pl,
Boncheva, I.
Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev St., Bl. 24, 1113 Sofia, Bulgaria, mcgoncu@metu.edu.tr,
Hairapetian, V.
Department of Geology, Islamic Azad University, Khorasgan branch, P.O.Box 81595-158, Esfahan, Iran, vachik@khuisf.ac.ir,
Bressan, G.
Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellón II, Buenos Aires C1428 EHA, Argentina, gbressan@gl.fcen.uba.ar,
Abstrakty : Trace fossil associations from the Lower.Middle Jurassic siliciclastic succession of the northern Neuquen Basin, Argentina are described and their palaeoenvironmental interpretation is discussed. The Bardas Blancas Formation displays facies of lower foreshore to offshore environments, such as massive and laminated mudstones, laminated siltstones, hummocky cross-stratified sandstones, massive and laminated sandstones, wave-rippled sandstones, as well as fine- to medium-grained bioclastic sandstones and massive conglomerates. They contain a trace fossil assemblage low in abundance but high in diversity. The assemblage, comprising eleven ichnogenera, is dominated by Skolithos, Chondrites, Thalassinoides, Planolites, Palaeophycus, Taenidium, Gyrochorte and Arenicolites. Gordia, ?Diplocraterion and Lockeia are less abundant. These trace fossils belong to the Skolithos, Cruziana and Zoophycos ichnofacies. Their distribution is controlled mainly by hydrodynamic energy, substrate consistency and oxygen levels. Storm beds exhibit two successive stages of colonization: (1) the pioneer stage, during which Skolithos, Diplocraterion and Arenicolites (elements of the Skolithos ichnofacies), were produced; and (2) the stable environment stage, represented by Chondrites, Thalassinoides, Taenidium, Gyrochorte, Gordia, Lockeia, Palaeophycus and Planolites (elements of the Cruziana ichnofacies). deeper environments exhibit a low diversity association with Chondrites and Thalassinoides, characterizing the Zoophycos ichnofacies.

Słowa kluczowe : Argentyna, ichnofauna, jura, skamieniałości śladowe, Argentina, Ichnofacies, Ichnotaxonomy, Jurassic, Neuquen Basin, Trace fossils,
Wydawnictwo : Faculty of Geology of the University of Warsaw
Rocznik : 2009
Numer : Vol. 59, no. 2
Strony : 201 – 220
Bibliografia : Alpert, S.P. 1974. Systematic review of the genus Skolithos. Journal of Paleontology, 48, 661–669
Alpert, S.P. 1975. Planolites and Skolithos from the upper Precambrian-Lower cambrian. White-Inyo Mountains, California. Journal of Paleontology, 49, 509–521.
Arnott, R.W.C. and Southard, J.B. 1990. Exploratory flow-duct experiments on combined-flow bed configurations, and some implications for interpreting storm-event stratification. Journal of Sedimentary Petrology, 60, 211–219.
Brenchley, P.J. 1989. Storm sedimentation. Geology Today, 5, 133–137
Brenchley, P.J., Pickerill, P.K. and Stromberg, S.G. 1993. The role of wave reworking on the architecture of storm sandstone facies, Bell Island Group (Lower Ordovician), eastern Newfoundland. Sedimentology, 40, 359–382.
Bressan, G.S. and Palma, R.M. 2007. Las trazas fósiles en las areniscas con estratificación cruzada tipo hummocky de la Formación Bardas Blancas, Cuenca Neuquina. In: III Simposio Argentino Jurásico, pp. 31. Mendoza.
Bressan, G.S. and Palma, R.M. 2008. Trace fossil assemblages from lower Toarcian-lower Bajocian siliciclastic marine platform-Neuquén Basin, Argentina. In: 5th International Symposium of IGCP 506, pp. 55–56. Hammamet.
Bromley, R.G. 1996. Trace fossils. Biology, taphonomy and applications, pp. 1–361. Chapman and Hall; London.
Cantalamessa, G. and Di Celma, C. 2004. Sequence response to syndepositional regional uplift: insights from high-resolution sequence stratigraphy of late Early Pleistocene strata, Periadriatic Basin, central Italy. Sedimentary Geology, 164, 283–309.
Chacra, J. 2007. Evolución paleoambiental, ciclicidad y estratigrafía secuencial en los depósitos de la Fm. Bardas Blancas (Mesosecuencia Cuyo), Cuenca Neuquina-Mendoza. Unpublished Tesis de Licenciatura, Universidad de Buenos Aires, 125 pp., Buenos Aires.
Cheel, R.J. and Leckie, D.A. 1993. Hummocky cross-stratification. In: V. P. Wright (Ed.), Sedimentology Review 1, Blackwell Scientific Publications, 103–122.
Collinson, J.D. and Thompson, D.B. 1989. Sedimentary structures, pp. 1–207. Unwin-Hyman, London.
D´Alessandro, A. and Bromley, R.G. 1987. Meniscate trace fossils and the Muensteria-Taenidium problem. Palaeontology, 30, 743–763.
Dellapé, D.A., Mombrú, C., Pando, G., Riccardi, A.G., Uliana, M.A. and Westermann, G.E.G. 1979. Edad y correlación de la Formación Tábanos en Chacay Melehue y otras localidades de Neuquén y Mendoza. Con consideraciones sobre la distribución y significado de las sedimentitas del Lotenian. In: Obra Centenario Museo La Plata, 5, 81–105.
De Raaf, J.F.M., Boersma, J.R. and Van Gelder, A. 1977. Wave-generated structures and sequences from a shallow marine succession, Lower Carboniferous, County Cork, Ireland. Sedimentology, 24, 451–483.
Dott Jr., R.H. and Bourgeois, J. 1982. Hummocky stratification: significance of its variable bedding sequences. Geological Society of America Bulletin, 93, 663–680.
Droser, M.L. and Bottjer, D.J. 1986. A semiquantitative classification of ichnofabric. Journal of Sedimentary Petrology, 56, 558–569.
Droser, M.L. and Bottjer, D.J. 1989. Ichnofabric of sandstones deposited in high-energy nearshore environments: measurement and utilization. Palaios, 4, 598–604.
Ekdale, A.A. and Mason, T.R. 1988. Characteristic trace-fossils associations in oxygen-poor sedimentary environments. Geology, 16, 720–723.
Fillion, D. and Pickerill, R.K. 1990. Ichnology of the Lower Ordovician Bell Island and Wabana Groups of eastern Newfoundland. Palaeontographica Canadiana, 7, 1–119.
Fürsich, F.T. 1974a. Corallian (Upper Jurassic) trace fossil from England and Normandy. Stuttgarter Beträge zur Naturkunde, Serie B 13, 1–51.
Fürsich, F.T. 1974b. On Diplocraterion Torell 1870 and the significance of morphological features in vertical, spreitenbearing, U-shaped trace fossils. Journal of Paleontology, 48, 952–962.
Fürsich, F.T. and Hurst, J.M. 1974. Environmental factors determining the distribution of brachiopods. Palaeontology, 17, 879–900.
Gibert J.M. de and Benner J.S. 2002. The trace fossil Gyrochorte: ethology and paleoecology. Revista Espańola de Paleontología, 17, 1–12
Gulisano, C.A. 1981. Ciclo Cuyano en el norte de Neuquén y Sur de Mendoza. In: VIII Congreso Geológico Argentino, pp. 579–592. San Luis.
Gulisano, C.A. and Gutiérrez Pleimling, A.R. 1994. Field Trips Guidebook B, Neuquen Basin, Mendoza Province. In: 4th International Congress on Jurassic Stratigraphy and Geology, pp. 1–113. Mendoza.
Gulisano, C.A. 1984. Esquema estratigráfico de la secuencia jurásica del oeste de la provincial del Neuquén. In: IX Congreso Geológico Argentino, pp. 236–259. San Carlos de Bariloche
Gulisano, C.A., Gutiérrez Pleimling, A. and Digregorio, R.E. 1984. Esquema estratigráfico de la secuencia jurásica del oeste de la provincia de Neuquén. In: IX Congreso Geológico Argentino, pp. 236–259. Buenos Aires.
Guy, H.P., Simons, D.B. and Richardson, E.V. 1966. Summary of alluvial channel data from flume experiments, 1956–61. U.S. Geological Survey Professional Paper 462–I, pp. 1–66. Washington D.C.
Häntzschel, W. 1962. Trace fossils and problematic. In: R.C. Moore (Ed.), Treatise on invertebrate paleontology, Part W, Miscellanea. Geological Society of America and University of Kansas Press, 177–245.
Häntzschel, W. 1975. Trace fossil and problematica. In: C. Teichert (Ed.), Treatise on Invertebrate Paleontology. Part W, Misellanea, Supplement 1. Geological Society of America and University of Kansas Press, 1–269.
Hart, B.S. y Plint, A.G. 1995. Gravelly shoreface and beachface deposits. Special Publication of the International Association of Sedimentologists, 22, 75–99.
Howard, J.D., and Frey, R.W. 1984. Characteristic trace fossils in nearshore to offshore sequences, Upper Cretaceous of East-Central Utah. Canadian Journal of Earth Sciences, 21, 200–219.
Jennette, D.C. and Pryor, W.A. 1993. Cyclic alternation of proximal and distal storm facies: Kope and Fairview Formations (Upper Ordovician), Ohio and Kentuchy. Journal of Sedimentary Petrology, 63, 183–203.
Junken, E.A., 2002. Sedimentación dominada por tormentas en el Bajociano (Jurásico medio): Formación Bardas Blancas, Cuenca Neuquina, Mendoza. Unpublished Tesis de Licenciatura, Universidad de Buenos Aires, 92 pp., Buenos Aires.
Kerr, M. and Eyles, N. 1991. Storm deposited sandstones (tempestites) and related ichnofossils of the Late Ordovician Georgian Bay Formation, Southern Ontario, Canada. Canadian Journal of Earth Sciences, 28, 266–282.
Kreisa, R.D. 1981. Storm-generated sedimentary structures in subtidal marine facies with examples from the Middle and Upper Ordovician of Southwestern Virginia. Journal of Sedimentary Petrology, 51, 823–848.
Kidwell, S.M. 1991. The stratigraphy of shell concentrations. In: P.A. Allison and D.E.G. Briggs (Eds), Taphonomy: releasing the data locked in the fossil record, Plenum Press, 211–290.
Legarreta, L. and Gulisano, C.A. 1989. Análisis estratigráfico secuencial de la Cuenca Neuquina (Triásico Superior-Terciario Inferior). in: G. Chebli and L. Spalleti (Eds), Cuencas Sedimentarias Argentinas, pp. 221–243. S.M. de Tucumán.
Legarreta, L., Gulisano, C.A. and Uliana, M. 1993. Las secuencias sedimentarias jurásico-cretácicas. In: XII Congreso Geológico Argentino y II Congreso de Hidrocarburos, pp. 87–114. Mendoza.
Maceachern, J.A., Kerrie, L.B., Pemberton, S.G. and Gingras, M.K. 2008. The ichnofacies paradigm: high-resolution paleoenvironmental interpretation of the rock record. In: J.A. MAcEachern, K.L. Bann, M.K. Gingras, and S. G. Pemberton (Eds), Applied ichnology. SEPM Short Course notes, 27–64.
MacNaughton, R.B. and Pickerill, R.K. 1995. Invertebrate ichnology of the nonmarine Lepreau Formation (Triassic), southern New Brunswick, eastern Canada. Journal of Paleontology, 69, 160–171.
Moghadam, H.V. and Paul, C.R.C. 2000. Trace Fossils of the Jurassic, Blue Lias, Lyme Regis, Southern England. Ichnos, 7, 283–306.
Osgood, R.G., Jr. 1970. Trace fossils of the cincinnati area. Palaeontographica Americana, 6, 281–444.
Pemberton, S.G. and Frey, R.W. 1982. Trace fossil nomenclature and the Planolites-Palaeophycus dilemma. Journal of Paleontology, 56, 843–881.
Pemberton, S.G., Maceachern, J.A. and Ranger, M.J. 1992. Ichnology and event stratigraphy: the use of trace fossils in recognizing tempestites. In: S.G. Pemberton (Ed.), Applications of ichnology to petroleum exploration-A core workshop. Society of Economic Paleontologists and Mineralogists, Core Workshop 17: 15–118.
Pickerill, R.K. and Narbonne, G.M. 1995. Composite and compound ichnotaxa: a case example from the Ordovician of Québec, eastern Canada. Ichnos, 4, 53–69.
Pickerill, R.K., Fillion, D. and Harland, T.L. 1984. Middle Ordovician trace fossils in carbonates of the Trenton Group between Montreal and Quebec City, St. Lawrence Lowland, Eastern Canada. Journal of Paleontology, 58, 416–439.
Reading, H.G. and Collinson, J.D. 1996. Clastic coasts. In: H.G. Reading (Ed.), Sedimentary environments: processes, facies and stratigraphy. Blackwell Science, 154–231.
Reineck, H.E. and Singh, I.B. 1975. Depositional sedimentary environments, pp.1–439. Springer; Berlin-Heidelberg-New york
Rhoads, D.C. and Morse J.W. 1971. Evolutionary and ecologic significance of oxygen-deficient basins. Lethaia, 4, 413–428.
Riccardi, A.C., Leanza, H.A., Damborenea, S.E., Manceńido, M.O., Ballent, S.C. and Zeiss, A. 2000. Marine bioestratigraphy of the Neuquén Basin. In : H. Miller and F. Hervé (coordinators), Geoscientific cooperation with Latin America. 31st International Geological Congress, Zeitschrift für Angewandte Geologie. Sonderheft SH1, pp. 103–108. Río de Janeiro.
Richter, R. 1927. Die fossilen Fährten und Bauten der Würmer, ein Uberblick über ihre biologischen Grundform und deren geologische Bedeutung. Paläontologische Zeitschrift, 9, 193–240.
Sanci, R. 2005. Evolución ambiental y bioestratigrafía de las Formaciones Bardas Blancas y Tres Esquinas (Grupo Cuyo), Cuenca Neuquina. Unpublished Tesis de Licenciatura, Universidad de Buenos Aires, 115 pp., Buenos Aires.
Savrda, C.E., Bottjer, D.J. and Seilacher, A. 1991. Redox-related benthic events. In: G. Einsele, W. Ricken and A. Seilacher (Eds), Cycles and Events in Stratigraphy. Springer; Berlin, 524–541.
Schlirf, M., Uchman, A. and Kümmel, M. 2001. Upper Triassic (Keuper) non-marine trace fossils from the Haßberge area (Franconia, south-eastern Germany). Paläontologische Zeitschrift, 75, 71–96.
Spalletti, L.A. and del Valle, A. 1990. Plataformas silicoclásticas. In: G.E. Bossi (Ed.), 10° Congreso Geológico Argentino- 1° Simposio de ambientes marinos y modelos sedimentarios. Boletín Sedimentológico, 4, 161–187. San Juan.
Swinbanks, D.D. 1981. Sediment reworking and the biogenic formation of clay laminae by Abarenicolapadifica. Journal of Sedimentary Petrology, 51, 1137–1145.
Swinbanks, D.D. and Luternauer, J.L. 1987. Burrow distribution of thalassinidean shrimp on a Fraser Delta tidal flat, British Colombia. Journal of Paleontology, 61, 315–332.
Uchman, A. 1995. Taxonomy and palaeoecology of flysch trace fossils: The Mamoso-arenacea Formation and associated facies (Miocene, Northern Apennines, Italy). Beringeria, 15, 3–115.
Uchman, A. 1999. Ichnology of the Rhenodanubian Flysch (Lower Cretaceous-Eocene) in Austria and Germany. Beringeria, 25, 67–173.
DOI :
Cytuj : Grabowski, J. ,Boncheva, I. ,Hairapetian, V. ,Bressan, G. , Trace fossils from the Lower-Middle Jurassic Bardas Blancas Formation, Neuquen Basin, Mendoza Province, Argentina. Acta Geologica Polonica Vol. 59, no. 2/2009
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