Neoselachians and Chimaeriformes (Chondrichthyes) from the latest CretaceousePaleogene of Sierra Baguales, southernmost Chile. Chronostratigraphic, paleobiogeographic and paleoenvironmental implications
Artículo
Open/ Download
Publication date
2013Metadata
Show full item record
Cómo citar
Otero, Rodrigo A.
Cómo citar
Neoselachians and Chimaeriformes (Chondrichthyes) from the latest CretaceousePaleogene of Sierra Baguales, southernmost Chile. Chronostratigraphic, paleobiogeographic and paleoenvironmental implications
Author
Abstract
This paper discusses a well-represented fossil record of cartilaginous fishes (Chondrichthyes) from
southern South America. The recovered samples allow the recognition of three assemblages with
chronostratigraphic and paleogeographic value: i) typical Maastrichtian sharks and rays with affinities to
eastern Pacific fauna, including the taxa Ischyrhiza chilensis, Serratolamna serrata, Centrophoroides sp.
associated to Carcharias sp., and Dasyatidae indet.; ii) a scarce reworked assemblage of PaleoceneeEarly
Eocene age including the taxa Otodus obliquus and Megascyliorhinus cooperi; iii) a rich assemblage with
reworked taxa of Early to Middle Eocene age, together with autochthonous deposited Middle to Late
Eocene taxa with close affinities to paleoichthyofaunas recovered from the North Atlantic, represented by
Carcharias ‘hopei’, Odontaspis winkleri, Carcharoides catticus, Macrorhizodus praecursor, Carcharocles
auriculatus, Striatolamia sp., Striatolamia macrota, Hexanchus agassizi, Notorhynchus sp., Myliobatis sp.,
Abdounia sp., Pristiophorus sp., Squatina sp., cf. Rhizoprionodon sp., Ischyodus sp., and one new species,
Jaekelotodus bagualensis sp. nov. The studied samples include for the first time taxa with well established
chronostratigraphic resolutions as well as taphonomic information that help clarifying the age of the
fossil-bearing units. In addition, they provide relevant information about the evolution of the Magallanes
(¼Austral) Basin from the Upper Cretaceous to the Paleogene, suggesting a probable connection with the
Quiriquina Basin of south-central Chile during the latest Cretaceous. Finally, the studied assemblages
indicate a latitudinal pattern of distribution that provides valuable data on the environmental evolution
and temperature of southern South America during the Paleogene.
General note
Artículo de publicación ISI
Identifier
URI: https://repositorio.uchile.cl/handle/2250/119675
DOI: DOI: 10.1016/j.jsames.2013.07.013
Quote Item
Journal of South American Earth Sciences 48 (2013) 13e30
Collections