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Geology and taphonomy of the base of the Taquaral Member, Irati Formation (Permian, Paraná Basin), Brazil

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Języki publikacji
EN
Abstrakty
EN
The taphonomy of Early Permian vertebrates from a sandy facies at the base of the Taquaral Member, Irati Formation, was surveyed in order to acquire data for the interpretation of the sedimentary processes and paleoenvironment of deposition. Six outcrops from the Rio Claro municipality and surrounding areas, from the Brazilian State of São Paulo, were investigated. The vertebrate groups are Chondrichthyes (Xenacanthiformes, Ctenacanthiformes and Petalodontiformes), Osteichthyes (Actinopterygii and Sarcopterygii) and Tetrapodomorpha. They occur as loose teeth, scales, spines and bone remains. The sandy facies is characterized by fining upward deposition. The coarser sandstone immediately above the underlying Tatuí Formation is rich in Chondrichthyes. However, the fine sandstone above, immediately beneath the silty shale facies, is devoid of Chondrichthyes, though Osteichthyes scales, teeth and bones were present. The taphonomy is important for inferring sedimentary processes and then the paleoenvironments. The poor sorting of the sandstone and the presence of fossils that are mostly abraded or worn are indicative of a high energy environment. In contrast, the presence of fossils in a good state of preservation, some without abrasion and breakages are indicative of only limited transport. Differences of fossil spatial density, numbers of specimens and taxa may be explained by the dynamics of deposition, from details of the palaeoenvironment can be obtained.
Rocznik
Strony
379--387
Opis fizyczny
Bibliogr. 30 poz., fot., rys., tab.
Twórcy
autor
  • Universidade de São Paulo, Instituto de Geociências, Departamento de Geologia Sedimentar e Ambiental. Rua do Lago, 562. Cidade Universitária 05508-080 - São Paulo, SP – Brazil
autor
  • Universidade de São Paulo, Instituto de Geociências, Departamento de Geologia Sedimentar e Ambiental. Rua do Lago, 562. Cidade Universitária 05508-080 - São Paulo, SP – Brazil
Bibliografia
  • 1. Assine, M.L., Zacharias, A.A. and Perinotto, J.A.J. 2003. Paleocorrentes, paleogeografia e seqüências deposicionais da Formação Tatuí, centro-leste do Estado de São Paulo. Revista Brasileira de Geociências, 33, 33–40.
  • 2. Barbosa, O. and Gomes, F.A. 1958. Pesquisa de petróleo na bacia do rio Corumbataí. Rio de Janeiro, Boletim do DNPM/DGM, 171, 1–40.
  • 3. Behrensmeyer, A.K. 1982. Time resolution in fluvial vertebrate assemblages. Paleobiology, 8, 211–227.
  • 4. Behrensmeyer, A.K. 1988. Vertebrate preservation in fluvial channels. Palaeogeography, Palaeoclimatology, Palaeoecology, 63, 183–199.
  • 5. Behrensmeyer, A.K. 1990. Bones/transport-hydrodynamics, In: D.E. Briggs and P.R. Crowther (Eds), Paleobiology: A Synthesis, pp. 232–235. Blackwell; Oxford.
  • 6. Behrensmeyer, A.K. 1991. Terrestrial vertebrate accumulations. In: P.A. Allison and D.E. Briggs (Eds), Taphonomy: releasing the data locked in the fossil record, pp. 291−327. Plenum Press; New York.
  • 7. Behrensmeyer, A.K. and Kidwell, S.M. 1985. Taphonomy’s contributions to paleobiology, Paleobiology 11, 105–107
  • 8. Chahud, A., Fairchild, T.R. and Petri, S. 2010. Chondrichthyans from the base of the Irati Formation (Permian, Parana Basin), São Paulo, Brazil. Gondwana Research, 18, 528–537.
  • 9. Chahud, A., Pacheco, M.L.A.F., Meira, F.E., Romero, G.R. and Petri, S. 2012. Paleontology and depositional environments of the Tatuí and Irati formations (Permian) in the Ponte Nova Farm, Ipeúna, state of São Paulo. Revista Brasileira de Geociências, 42, 198–212.
  • 10. Chahud, A. and Petri, S. 2008a. Chondrichthyes no Membro Taquaral, base da Formação Irati, no centro-leste do Estado de São Paulo, Brasil. Revista de Geologia. Fortaleza, 21, 169–179.
  • 11. Chahud, A. and Petri, S. 2008b. Registro de Paleoniscóides na base do Membro Taquaral, Formação Irati, Permiano da Bacia do Paraná. Revista do Instituto Geológico. 29, 33–40.
  • 12. Chahud, A. and Petri, S. 2009. Novos Xenacanthidae (Chondrichthyes, Elasmobranchii) da base do Membro Taquaral, Formação Irati, Permiano da Bacia do Paraná. Revista do Instituto Geológico, 30, 19–24.
  • 13. Chahud, A. and Petri, S. 2010a. Anfíbio e Paleonisciformes da Porção Basal do Membro Taquaral, Formação Irati (Permiano), Estado de São Paulo, Brasil. Geologia USP. Série Científica. São Paulo, 10, 29–37.
  • 14. Chahud, A. and Petri, S. 2010b. O tubarão Taquaralodus albuquerquei (Silva Santos, 1946) do Membro Taquaral (Permiano, Formação Irati) no Estado de São Paulo. Acta Biologica Paranaense, 39, 1–17.
  • 15. Chahud, A. and Petri, S. 2012. Levantamento dos cladodontes sul-americanos e novos espécimes do Membro Taquaral (Formação Irati, Permiano), Bacia do Paraná. Boletim Paranaense de Geociências, 66-67, 23–29.
  • 16. Chahud, A. and Petri, S. 2013a. Paleontology of Taquaral Member silty shale in the State of São Paulo. Brazilian Journal of Geology, 43, 117–123.
  • 17. Chahud, A. and Petri, S. 2013b. The silty shale Taquaral Member of the early Permian Irati Formation (Paraná Basin, Brazil). Paleontology and paleoenvironments. Swiss Journal of Palaeontology, 132, 119–128.
  • 18. Chahud, A. and Petri, S. 2014. New chondrichthyans from the Irati Formation (Early Permian, Paraná Basin), Brazil: origin, paleoenvironmental and paleogeographical considerations. Proceedings of the Geologists’ Association, 125, 437–445.
  • 19. Davies, D.J., Powell, E.P. and Stanton, R.J., Jr. 1989. Relative rates of shell dissolution and net sediment accumulation – a commentary: Can shell beds form by the gradual accumulation of biogenic debris on the sea floor? Lethaia, 22, 207–212.
  • 20. Elder, R.L. and Smith, G.R. 1988. Fish taphonomy and environmental inference in paleolimnology. Palaeogeography, Palaeoclimatology, Palaeoecology, 62, 577–592.
  • 21. Fitzgerald, M.H., Simpson, E.L., Szajna, M.J., Fillmore, D. L., Hartline, B.W., Heness, E.A., Kraal, E.R. and Wilk, J.L. 2012. Taphonomy of lacustrine shoreline fish-part conglomerates in the Late Triassic age Lockatong Formation (Collegeville, Pennsylvania, USA): Toward the recognition of catastrophic fish kills in the rock record. Palaeogeography, Palaeoclimatology, Palaeoecology, 313–314, 234–245
  • 22. Holz, M. and Simões M.G. 2002. Elementos Fundamentais de Tafonomia. pp. 231. Editora da Universidade/UFRGS Porto Alegre.
  • 23. Kidwell, S.M. and Holland, S.M. 1991. Field description of course bioclastic fabrics. Palaios, 6, 426–434.
  • 24. Mancuso, A.C. 2003. Continental fish taphonomy: a case study in the Triassic of Argentina. Journal of South American Earth Sciences, 16, 275–286.
  • 25. Mancuso, A.C. 2012. Taphonomic analysis of fish in rift lacustrine systems: Environmental indicators and implications for fish speciation. Palaeogeography, Palaeoclimatology, Palaeoecology, 339–341, 121–131
  • 26. Milani, J. and De Wit, M.J. 2008. Correlations between the classic Paraná and Cape–Karoo sequences of South America and southern Africa and their basin infills flanking the Gondwanides: du Toit revisited. Geological Society, London, Special Publications, 294, 319–342
  • 27. Mussa, D. Carvalho, R.G. and Santos, P.R. 1980. Estudo estratigráfico e Paleoecológico em Ocorrências Fossilíferas da Formação Irati, Estado de São Paulo, Brasil. Boletim do IG/USP, 11, 31–189.
  • 28. Ragonha, E.W. 1978. Chondrichthyes do Membro Taquaral (Formação Irati) no Estado de São Paulo. Master Dissertation. Instituto de Geociências, Universidade de São Paulo, São Paulo (unpublished).
  • 29. Santos, R.V., Souza, P.A., Alvarenga, C.J.S., Dantas, E.L., Pimentel, E.L., Oliveira, C.G. and Araújo, L.M. 2006. Shrimp U-Pb zircon dating and palynology of bentonitic layers from the Permian Irati Formation Parana Basin, Brazil. Gondwana Research, 9, 456–463.
  • 30. Walker, R.G. and James, N.P. 1992. Facies Models – response to sea level change. Geological Association of Canada, pp. 409.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-bebcd7e4-867e-4df3-b616-47fb8dd3789a
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