CONICET | Buscador de Institutos y Recursos Humanos

We present the first integrate paleoecological study which includes both previous and new sedimentological, paleoclimate, fauna and flora analyses in the Bajo Barreal Formation (Upper Cretaceous), Golfo San Jorge Basin, Patagonia, Argentina. The study was carried out principally at the Estancia (=Ranch) Ocho Hermanos Locality, although other significant paleontological localities of the Bajo Barreal Formation are included. In the Estancia Ocho Hermanos Locality, the paleoenvironment is characterized by low sinuosity single-channelized fluvial systems, with well-developed proximal floodplains. Paleoclimate was interpreted as warm and humid with marked seasonality. This locality was dominated by dinosaurs, including sauropods (titanosaurs and rebbachisaurids) and theropods (abelisaurids and megaraptorids), but other vertebrates, such as pterosaurs, crocodyliforms, turtles and fishes were also part of the paleoecosystem. In addition, the first stable isotope analysis on Mesozoic teeth (dinosaurs and crocodyliforms) from the Golfo San Jorge Basin was conducted. This new information revealed different sources of water utilized by theropod and sauropod dinosaurs, allowed to infer preliminary modes of lyfe for crocodyliforms, and provided information about diet of these Mesozoic organisms. Ground-level and mid-height feeding are interpreted for rebbachisaurid and titanosaurid sauropods, respectively. Ferns are considered the main non-arboreal component of this ecosystem and possibly an important source of the diet of sauropods, whereas angiosperms (eudicots and monocots) would have been present as well. On the other hand, gymnosperms, mainly Araucariaceae, and in a minor proportion Podocarpaceae, and Cheirolepidiaceae, would encompass the arboreal component of this environment. Abelisaurids could be recognized as one of the top predators of this paleoecosystem, in part due to their relative abundance, in relation to other carnivores. Finally, in a broad context, this study augments our understanding of Cretaceous terrestrial ecosystems of south-central Patagonia and contributes for future comparisons with other chronologically equivalent localities, principally, from the Southern Hemisphere.

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