Micropaleontología, Cronoestratigrafía y Sedimentología del límite Cretácico/Terciario en el NO de Cuba

Several sections have been studied in western Cuba in order to date the sediments derived of the nearby Yucatan meteorite impact event. The sections of Peñalver, Minas, La Victoria, La Yuca, Santa Isabel, Cacarajicara and Moneada contain thick sediments along the Cretaceous-Tertiary transition, show...

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Detalhes bibliográficos
Autores: Molina, Eustoquio, Arenillas, J. I., Arz, José Antonio, Díaz, C., Garcia, D., Meléndez Hevia, Alfonso, Rojas, R.
Tipo de documento: artigo
Data de publicação:2002
País:España
Recursos:Universidad de Huelva (UHU)
Repositório:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:espanhol
OAI Identifier:oai:ariasmontano.uhu.es:10272/9359
Acesso em linha:http://hdl.handle.net/10272/9359
Access Level:Acceso aberto
Palavra-chave:Cretaceous
Tertiary
Planktic Foraminifera
Impact
Descrição
Resumo:Several sections have been studied in western Cuba in order to date the sediments derived of the nearby Yucatan meteorite impact event. The sections of Peñalver, Minas, La Victoria, La Yuca, Santa Isabel, Cacarajicara and Moneada contain thick sediments along the Cretaceous-Tertiary transition, showing clear evidence of a large meteorite impact. The Chronostratigraphy of the Via Blanca, Peñalver, Cacarajicara, Moneada and Apolo Formations have been revised, placing the K/T boundary at the base of the Peñalver, Cacarajicara and Moneada formations. Planktic foraminifera of the Via Blanca Formation allowed to date the uppermost autochtonous sediments as P. hantkeninoides Biozone (latest Maastrichtian)