O gênero Montastraea (Cnidaria, Scleractinia) do Cretáceo, Grupo Santana, nordeste do Brasil

Detalhes bibliográficos
Ano de defesa: 2023
Autor(a) principal: Santos, Jhenys Maiker
Orientador(a): Não Informado pela instituição
Banca de defesa: Não Informado pela instituição
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Não Informado pela instituição
Programa de Pós-Graduação: Não Informado pela instituição
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Link de acesso: http://repositorio.ufc.br/handle/riufc/75988
Resumo: Among the sedimentary basins in Brazil, the Araripe Basin is one of the most emblematic due to its quantity of fossils and exuberant paleobiota. It is located in the Northeast region of the country and occupies portions of the states of Piauí, Pernambuco and Ceará. In a recent paleontological incursion carried out in the Araripe Basin, more precisely in the municipality of Simões (western border of the state of Piauí), a sample of fossil coral from the Romualdo Formation (Lower Cretaceous, Santana Group) was collected, here described as a specimen belonging to the genus Montastraea Blainville, 1830, and later listed in the scientific collection of the Picos Paleontology Laboratory of the Federal University of Piauí. The genus is relatively abundant in the Tethys Sea; however this is the southernmost occurrence to date. This study presents descriptive, morphometric and phylogenetic data from the specimen and reinforces the Tethyan affinities of the Araripe biota. In comparative analysis with other specimens of Cretaceous scleractinian corals, Montastraea sp. proved to be different from the other species of the genus due to the small diameter of the colony, the hemispherical shape, the intermediate diameter of the corallites and the distances between the columellae. Despite all these differences, it was preferable not to interpret it as a new species, among other factors, due to the absence of more specimens and possible deformities of characteristics suffered during the taphonomic process. The presence of a fossil coral in the basin indicates a shallow tropical marine biota adapted to clear and probably warm waters.