New dyrosaurid crocodylomorph and evidences for faunal turnover at the K–P transition in Brazil

Author:

Barbosa José Antonio1,Kellner Alexander Wilhelm Armin2,Viana Maria Somália Sales3

Affiliation:

1. Department of Geology/LAGESE, Universidade Federal de PernambucoRua Acadêmico Hélio Ramos, s/n, Recife, PE 50740-530, Brazil

2. Paleovertebrate Sector, Department of Geology and Paleontology, Museu Nacional/Universidade Federal do Rio de JaneiroQuinta da Boa Vista, São Cristóvão, Rio de Janeiro, RJ 20940-040, Brazil

3. Universidade Estadual Vale do AcaraúAvenida da Universidade, 85, Betânia, Sobral, CE 62040-370, Brazil

Abstract

The discovery of a new dyrosaurid crocodylomorph from the well-dated Palaeocene deposits of northeastern Brazil sheds new light on the evolutionary history of this extinct group of marine crocodylomorphs that have survived the Cretaceous–Palaeogene (K–P) extinction crisis. Guarinisuchus munizi , the most complete member of this group collected in South America so far, is closely related to the African forms, and this fact suggests that dyrosaurids had crossed the Atlantic Ocean before the K–P boundary and dispersed from there to North America and other parts of South America. This discovery also suggests that on the coast of northeastern Brazil, dyrosaurids replaced the pre-existing Late Cretaceous fauna of diversified mosasaurs, a group of marine lizards, after the K–P extinction event, becoming the main predators, together with sharks, in shallow marine Palaeocene environments. More detailed stratigraphic records and detailed dating of the deposits with dyrosaurids are necessary to correlate this particular pattern found in the ancient northeastern Brazilian coast within the evolution of the group, especially in Africa.

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Environmental Science,General Immunology and Microbiology,General Biochemistry, Genetics and Molecular Biology,General Medicine

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