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7. Walking in the Gondwanic Floodplains of Rio do Peixe Basins

verfasst von : Giuseppe Leonardi, Ismar de Souza Carvalho

Erschienen in: Dinosaur Tracks of Mesozoic Basins in Brazil

Verlag: Springer Nature Switzerland

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Abstract

The Rio do Peixe basins are the set of four associated basins: Sousa, Uiraúna-Brejo das Freiras (also known as Triunfo), Pombal and Vertentes. They are located in the western Paraíba State and in the Ceará State, northeastern Brazil, in a total area of ~1,280 km². The origin of these basins (Lower Cretaceous, Berriasian to lower Barremian) is related to normal and transcurrent fault movements along preexisting structural trends of the Proterozoic basement during the South and Equatorial Atlantic Ocean opening. Dinosaur footprints are the most abundant fossils in the siliciclastic continental sediments. The main tetrapod ichnofauna comprises, in at least 42 individual tracksites through approximately 96 stratigraphic levels, isolate footprints and trackways of large and small theropods, besides ornithopods, sauropods, and rare ankylosaurs. There are also invertebrate ichnofossils. The body fossils are fish scales and bone fragments, but also rare dinosaur and Crocodylomorpha bones, palynomorphs, plant fragments, ostracods and conchostracans. These basins comprise a lot of dinosaur ichnofaunas, in the same stratigraphic-time-paleogeographical context, and they represent segments of a widespread megatracksite. There are 447 theropod tracks; 90 sauropods (Total of 537 saurischians); 2 quadrupedal ornithischians (one of them an ankylosaurian); 6 small ornithopods; 30 graviportal ornithopods (total of 38 ornithischians); one track of a juvenile biped dinosaur; about 53 unclassifiable dinosaur tracks (629 dinosaurs, all together); a hand-foot set of batrachopodid prints; traces of a Crocodylomorpha; an isolate lacertoid print; and a large number of small chelonian half-swimming tracks. The environmental setting indicates an endemic biota living nearby ephemeral rivers and shallow lakes under hot climate conditions. These were preserved in alluvial fans, braided, meandering rivers and shallow lake deposits of Berriasian to lower Barremian ages. Dinosaur faunas (both as bone remains and as ichnofaunas) from the Early Cretaceous are quite rare in the world, and the material discovered in these basins is important to the knowledge of the dinosaur diversity during the Cretaceous.

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Vorheriges Kapitel The Cretaceous Araripe Basin Dinosaur Tracks and Their Paleoenvironmental Meaning

Nächstes Kapitel Tracking Dinosaurs During the Equatorial and South Atlantic Opening

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Titel: Walking in the Gondwanic Floodplains of Rio do Peixe Basins
verfasst von: Giuseppe Leonardi
Ismar de Souza Carvalho
Verlag: Springer Nature Switzerland
Buch: Dinosaur Tracks of Mesozoic Basins in Brazil
Print ISBN: 978-3-031-56354-6

Electronic ISBN: 978-3-031-56355-3

Copyright-Jahr: 2024
DOI: https://doi.org/10.1007/978-3-031-56355-3_7