Resultats globals: 2 registres trobats en 0.02 segons.
Articles, 2 registres trobats
Articles 2 registres trobats  
1.
17 p, 4.6 MB Palaeontology of the upper Turonian paralic deposits of the Sainte-Mondane Formation, Aquitaine Basin, France / Néraudeau, D. (Université Rennes 1) ; Saint Martin, S. (Université Rennes 1) ; Batten, D. J. (University of Manchester. School of Earth, Atmospheric and Environmental Sciences) ; Colin, Jean-Paul ; Daviero-Gomez, V. (Université Lyon 1) ; Girard, V. (Université Montpellier 2) ; Gomez, Bernard (Université Lyon 1) ; Nohra, Y. A. (Université Rennes 1) ; Polette, F. (Université Rennes 1) ; Platel, J. P. ; Saint Martin, J. P. (Sorbonne Universités) ; Vullo, R. (Université Rennes 1)
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. [...]
2016 - 10.1344/GeologicaActa2016.14.1.5
Geologica acta, Vol. 14 Núm. 1 (March 2016) , p. 53-69 (Articles)  
2.
25 p, 5.7 MB Unusual concentration of Early Albian arthropod-bearing amber in the Basque-Cantabrian Basin (El Soplao, Cantabria, Northern Spain) : palaeoenvironmental and palaeobiological implications / Najarro, M. (Instituto Geológico y Minero de España) ; Peñalver, Enrique (Instituto Geológico y Minero de España) ; Rosales, Idoia (Instituto Geológico y Minero de España) ; Pérez, de la Fuente, R. (Universitat de Barcelona. Departament d'Estratigrafia, Paleontologia i Geociències Marines) ; Daviero-Gomez, V. (Université Claude-Bernard. UMR 5125 (PEPS) CNRS, Paléobotanique) ; Gomez, Bernard (Université Claude-Bernard. UMR 5125 (PEPS) CNRS, Paléobotanique) ; Martínez-Delclòs, Xavier (Universitat de Barcelona. Departament d'Estratigrafia, Paleontologia i Geociències Marines)
The El Soplao site is a recently-discovered Early Albian locality of the Basque-Cantabrian Basin (northern Spain) that has yielded a number of amber pieces with abundant bioinclusions. The amber-bearing deposit occurs in a non-marine to transitional marine siliciclastic unit (Las Peñosas Formation) that is interleaved within a regressive-transgressive, carbonate-dominated Lower Aptian-Upper Albian marine sequence. [...]
2009 - 10.1344/105.000001443
Geologica acta, Vol. 7, Núm. 3 (Setembre 2009) , p. 363-387  

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