Early Cretaceous bivalves of the Romualdo Formation, Araripe Basin, northeastern Brazil.

dc.contributor.authorGuerrini, Vitor Bonatto
dc.contributor.authorMatos, Suzana Aparecida
dc.contributor.authorFürsich, Franz Theodor
dc.contributor.authorRodrigues, Mariza Gomes
dc.contributor.authorVarejão, Filipe Giovanini
dc.contributor.authorWarren, Lucas Veríssimo
dc.contributor.authorAssine, Mario Luis
dc.contributor.authorSimões, Marcello Guimarães
dc.date.accessioned2024-09-13T21:53:32Z
dc.date.available2024-09-13T21:53:32Z
dc.date.issued2024
dc.description.abstractThe fossil-rich Romualdo Formation (late Aptian/early Albian), Araripe Basin, northeastern Brazil, contains world-renowned Fossillagerstatten characterized by exceptionally preserved fossils. Macro- € invertebrates in this formation are primarily represented by mollusks, echinoids, and decapod crustaceans. Mollusk shells are abundant in certain stratigraphic intervals, forming coquinas or shell pavements. Despite recent advances in our understanding of the taxonomy of certain groups, compre-hensive taxonomic studies are lacking for almost the entire bivalve fauna. Therefore, a detailed taxonomic analysis is presented here. The described bivalves include four new genera (Araripenomia, Ciceromya, Inversatella, Australoeocallista), and six new species (Araripenomia infirma, Inversatella cearensis, Ciceromya edentulosa, Australoeocallista juazeiroi, Legumen kaririense, and Corbulomima delicata), in addition to Musculus maroimensis, Crassatella maroimensis, “Myrtea” sp. and “Tellina” sp. This bivalve fauna mainly consists of cosmopolitan and endemic brackish/marine genera, with Tethyan affinities. The fauna is not homogeneously distributed in the sedimentary succession of the Romualdo Formation, but is constrained to the third order highstand systems tract. Bivalves recorded from muddy facies are strongly dominated by infaunal and semi-infaunal suspension feeders. Assemblages of the sand-dominated facies, with dense shell accumulations of semi-infaunal to epifaunal byssate and infaunal suspension feeders, were formed under shallow, higher energy conditions. Despite the degree of generic endemicity, the mytilids, anomiids, crassateliids, astartids, tellinids, and corbulids are related to the bivalve fauna of the Early Cretaceous Riachuelo Formation of the Sergipe-Alagoas Basin, as previously demonstrated for the bakevelliids and echinoids. Indeed, the Romualdo bivalve fauna is, in part, a modified and impoverished brackish/marine fauna of the Riachuelo Formation.
dc.identifier.citationGUERRINI, V. B. et al. Early Cretaceous bivalves of the Romualdo Formation, Araripe Basin, northeastern Brazil. Cretaceous Research, v. 161, artigo 105910, 2024. Disponível em: <https://www.sciencedirect.com/science/article/pii/S0195667124000831>. Acesso em: 15 ago. 2024.
dc.identifier.doihttps://doi.org/10.1016/j.cretres.2024.105910
dc.identifier.issn0195-6671
dc.identifier.urihttps://www.repositorio.ufop.br/handle/123456789/18664
dc.identifier.uri2https://www.sciencedirect.com/science/article/pii/S0195667124000831
dc.language.isoen
dc.rightsrestrito
dc.subjectBivalve mollusks
dc.subjectSantana group
dc.subjectAraripe basin
dc.subjectSobradinho
dc.subjectEstiva
dc.titleEarly Cretaceous bivalves of the Romualdo Formation, Araripe Basin, northeastern Brazil.
dc.typeArtigo publicado em periodico
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