%0 Journal Article
%T Permian bivalves of the Taciba Formation, Itarar¨¦ Group, Paran¨¢ Basin, and their biostratigraphic significance
%A Marcello Guimar£¿es Sim£¿es
%A Jacqueline Peixoto Neves
%A Luiz Eduardo Anelli
%A Luiz Carlos Weinsch¨¹tz
%J Geologia USP : S¨¦rie Cient¨ªfica
%D 2012
%I Instituto de Geoci¨ºncias da USP
%X A small and poorly diversified bivalve fauna from Taciba Formation, Itarar¨¦ Group, Paran¨¢ Basin (State of Santa Catarina,Mafra Municipality), is described in this paper for the first time, based on new findings. The fauna is recorded in a 30 cmthick interval of fine sandstone locally at the top of Taciba Formation, in the Buti¨¢ quarry. The studied fossil-bearing sandstonebed is a marine intercalation recording a brief eustatic rise in sea-level, probably following glacier retreat and climateamelioration at the end of a broad glacial scenario. The fauna is mainly dominated by productid brachiopods, which are notdescribed here, and rare mollusk shells (bivalves and gastropods). Two bivalve species were identified: Myonia argentinensis(Harrington, 1955), and Aviculopecten multiscalptus (Thomas, 1928). The presence of Myonia argentinensis is noteworthysince this species is also present in the Baitaca assemblage found in marine siltstones (Baitaca assemblage) of theRio do Sul Formation, cropping out at the Teixeira Soares region, Paran¨¢ State. This species is also recorded in the bivalvefauna from the Bonete Formation, Pillahinco Group, Sauce Grande Basin, Buenos Aires Province, in Argentina. Hence, themarine bivalves of the Taciba Formation are associated with the transgressive event that characterizes the Eurydesma fauna,indicating a Late Asselian-Sakmarian age for the bivalve fauna. Presence of the Myonia argentinensis megadesmid speciesreinforces the Gondwanic nature of the studied fauna.
%K Bivalvia
%K Megadesmidae
%K Permian
%K Paran¨¢ Basin
%K Taciba Formation
%K Eurydesma fauna
%U http://ppegeo-local.igc.usp.br/pdf/guspsc/v12n1/a06v12n1.pdf