A Dicynodont-Theropod Association in the Latest Triassic of Poland

By J. Dzik, T. Sulej, G. Niedźwiedzki. 2008

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It is generally accepted that during the Triassic the composi− tion of tetrapod faunas underwent a series of fundamental transformations, mainly as a result of diversification of archosaurs and decline of therapsids (Benton 1994, 2004, 2006). The last herbivorous basal synapsids, dicynodonts, disappeared from the record in the early Norian of the Americas, about 220 Ma (Langer et al. 2007), being un− known from the Late Triassic of Europe. Here, we report a partially articulated skeleton and isolated bones of a giant rhino−size dicynodont in the Upper Triassic fluvial sedi− ments at Lisowice (Lipie Śląskie clay−pit) in southern Po− land. Paleobotanical data indicate an early Rhaetian age for the fauna (Dzik et al. 2008; Niedźwiedzki and Sulej 2008). The dicynodont bones are associated with bones of carnivo− rous dinosaurs, pterosaurs, as well as capitosaur and plagio− saur amphibians. Dicynodonts were represented in the Ger− manic Basin throughout the Late Triassic, as proven by findings of smaller dicynodonts in older deposits in the same area, associated there with temnospondyl amphibians. It ap− pears, thus, that the fossil record of tetrapod succession in the Late Triassic was strongly controlled by ecological fac− tors and biased by uneven representation of particular envi− ronments. The Lisowice assemblage proves that faunas dominated by dicynodonts did not entirely disappear at least until the end of the Triassic.

Subfields: Nature and Landscape Conservation, Paleontology

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In Nature and Landscape Conservation

  1. S. Nesbitt
  2. R. Butler
  3. R. Irmis
  4. Michael Benton
  5. S. Brusatte
  6. M. Norell
  7. M. Langer
  8. Paul M. Barrett

In Paleontology

  1. S. Nesbitt
  2. R. Butler
  3. Michael Benton
  4. R. Irmis
  5. S. Brusatte
  6. M. Norell
  7. M. Langer
  8. Jorge Ferigolo

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