Palaeontology of the upper Turonian paralic deposits of the Sainte-Mondane Formation, Aquitaine Basin, France

The upper Turonian lignite deposits of Sainte-Mondane, Dordogne (Aquitaine Basin, SW France), consist of clays bearing translucent, orange to red, amber micrograins. The amber exhibits different types of microbial inclusions. The clays contain several conifers including the genera Brachyphyllum,Fren...

ver descrição completa

Detalhes bibliográficos
Autores: Néraudeau, D., Saint Martin, S., Batten, D. J., Colin, Jean-Paul, Daviero-Gomez, V., Girard, V., Gomez, Bernard|||0000-0003-1691-0634, Nohra, Y. A., Polette, F., Platel, J. P., Saint Martin, J. P., Vullo, R.
Tipo de documento: artigo
Data de publicação:2016
País:España
Recursos:Universitat Autònoma de Barcelona
Repositório:Dipòsit Digital de Documents de la UAB
Idioma:inglês
OAI Identifier:oai:ddd.uab.cat:148097
Acesso em linha:https://ddd.uab.cat/record/148097
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2016.14.1.5
Access Level:Acceso aberto
Palavra-chave:Amber
Plants
Palynomorphs
Turonian
Cretaceous
France
Descrição
Resumo:The upper Turonian lignite deposits of Sainte-Mondane, Dordogne (Aquitaine Basin, SW France), consist of clays bearing translucent, orange to red, amber micrograins. The amber exhibits different types of microbial inclusions. The clays contain several conifers including the genera Brachyphyllum,Frenelopsis and Glenrosa, and a few leaf fragments of eudicot angiosperms. Among the plant meso-fossils the occurrence of Costatheca, Spermatites and abundant, diverse megaspores, including species of Ariadnaesporites, Bacutriletes, Echitriletes, Erlansonisporites, Maexisporites, Minerisporites andVerrutriletes, is noteworthy. Pollen grains of the Normapolles group are important components of the palynomorph assemblage. The clays were deposited in a calm, estuarine or lagoonal, muddy environment. The overlying lignitic sands contain large fossil wood pieces of the coniferAgathoxylon, small solitary corals, fragmentary oysters and pectinids, echinoid spines, a few teeth of marine selachians and bony fishes, but no amber is present. These sands were deposited in a high-energy coastal marine environment.