RT Journal Article
T1 New biostratigraphic data from the Callovian-Oxfordian La Manga Formation,Neuquén Basin, Argentina: Evidence from an ammonite condensed level
A1 Palma Durán, Ricardo
A1 Kietzmann, Diego A.
A1 Martín Chivelet, Javier
A1 López Gómez, José
A1 Bressan, Graciela Susana
AB The La Manga Formation constitutes most of the sedimentary record of the Callovian-Oxfordian in the Neuquén Basin. This stratigraphicunit represents the middle part of the Lotena Mesosequence, which is dominated by carbonates with interbedded shales, marls, andoccasional sandstones. Based on detailed stratigraphic work in the stratotype section (La Manga Creek, Mendoza), the depositionalenvironments and the sea-level history of the La Manga Formation have been interpreted. Petrographic and field observations led toidentification of nine facies distributed in two informal units. Unit 1 was deposited on a outer ramp setting, while deposition of unit 2 tookplace in the intertidal-supratidal environments. A condensed level close to the base of unit 1 has yielded Rehmannia sp., Rehmannia cf.paucicostata (Tornq.) and Homoeoplanulites sp., from the Lower Callovian Bodenbenderi-Proximum Zones, and Peltoceratoides sp.and Rursiceras sp. from the Upper Callovian and also in the Lower Oxfordian Peltoceratoides-Parawedekindia Zone. The condensedlevel is overlain by a Middle Oxfordian succession characterized by Perisphinctes (?Arisphinctes) sp., Perisphinctes (?Kranaosphinctes)sp., Mirosphinctes sp., Perisphinctes (?Antilloceras) cf. prophetae Gygi & Hill., Perisphinctes (?Otosphinctes) sp., Perisphinctes(?Subdiscosphinctes) sp., and Perisphinctes (?Kranaosphinctes) cf. decurrens (Buck.) of the Perisphinctes-Araucanites Zone, whichwas correlated with the upper part of the Cordatum Standard Zone to the Transversarium Standard Zone, and probably to the lower partof the Bifurcatus Standard Zone. Unit 2 has yielded small Mirosphinctes sp., indicating an Oxfordian age. The sharp contact betweenthe outer ramp facies of unit 1 and the overlying intertidal-supratidal facies of unit 2 can be interpreted as the result of an abrupt fall(forced regression) of the relative sea level during the end of Middle Oxfordian or Upper Oxfordian. These results could be used forcomparison with other localities in the Neuquén Basin providing additional data for Lower Callovian-Middle Oxfordian deposits.
PB Muséum d'histoire naturelle de Genève
SN 1661-5468
YR 2012
FD 2012
LK https://hdl.handle.net/20.500.14352/43690
UL https://hdl.handle.net/20.500.14352/43690
LA eng
DS Docta Complutense
RD 12 abr 2025