IANIGLA   20881
INSTITUTO ARGENTINO DE NIVOLOGIA, GLACIOLOGIA Y CIENCIAS AMBIENTALES
Unidad Ejecutora - UE
artículos
Título:
The Chañares Formation: a window to a Middle Triassic tetrapod community
Autor/es:
MANCUSO, A.C.; GAETANO, L.C.; LEARDI, J.M.; ABDALA, F.; ARCUCCI, A.
Revista:
LETHAIA
Editorial:
WILEY-BLACKWELL PUBLISHING, INC
Referencias:
Lugar: Londres; Año: 2014 vol. 47 p. 244 - 244
ISSN:
0024-1164
Resumen:
The Chañares Formation is known worldwide for its diverse and well-preserved Ladinian non-marine tetrapod assemblage, including a wide variety of archosauriform reptiles (proterochampsids, early offshoots of the crocodilian line, and dinosaurian precursors) and synapsids represented by dicynodonts and cynodonts. This tetrapod cord offers an opportunity to evaluate, within a taphonomic context, the palaeoecology of this Middle Triassic fauna. The taphonomic analysis of the Chañares ssemblage, under precise stratigraphic control, indicates that it is a good representation of the original faunal composition allowing us to address the paleoecological interactions between its components. Mass estimations and morphology-based paleobiological inferences of Chañares tetrapods are used to reconstruct the trophic structure of the community. Chañares tetrapod fauna was numerically dominated by middle-sized herbivorous and small faunivorous cynodonts, whereas middle-sized faunivorous cynodonts and large dicynodonts were less common. In contrast to the therapsids, which show a low species richness and high abundance, the archosauriforms are less abundant but are the most taxonomically diverse group. The large paracrocodylomorphs (estimated body masses between 350 and 500 kg) are identified as the top-predators of the community and the traversodontid cynodonts and dicynodonts (estimated body masses reaching approximately 43 and 360 kg, respectively) are indentified as the base herbivores of the trophic pyramid. We conclude that the worldwide faunal composition in the Ladinian reveals two continentalassemblages: (a) an eastern Laurasian assemblage dominated by temnospondyl amphibians; and (b) a western Gondwanan assemblage dominated by therapsids but including a wide diversity of archosauriforms