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Resultats globals: 5 registres trobats en 0.01 segons.
Articles, 5 registres trobats

Articles	5 registres trobats

27 p, 1.7 MB

Fauna de Ammonites del tránsito complejo Urgoniano-Flysch negro entre Germka y Deba (Albiense medio y superior, region Vascocantábrica Septentrional) / Agirrezabala, L. M. (Universidad del País Vasco. Departamento de Estratigrafía y Paleontología) ; Martínez, R. (Universitat Autònoma de Barcelona. Departament de Geologia) ; García-Mondéjar, J. (Universidad del País Vasco. Departamento de Estratigrafía y Paleontología)
En este trabajo se describe la fauna de ammonites de los complejos Urgoniano y Supraurgoniano (Flysch Negro), entre Gernika y Deba (Bizkaia y Gipuzkoa). El Complejo Urgoniano está formado por altos carbonatados y surcos lutíticos separados por fallas activas. [...]
The fauna of ammonites from the Urgonian and Supraurgonian (Black Flysch) complexes, between Gemika and Deba (Bizkaia and Gipuzkoa), is described. The Urgonian consist of limestone horsts and lutite troughs separated by active faults. [...]
1992
Treballs del Museu de Geologia de Barcelona, Vol. 2 (1992) , p. 143-169

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29 p, 8.4 MB

Glomospirella cantabrica n. sp., and other benthic foraminifera from Lower Cretaceous Urgonian-type carbonates of Cantabria, Spain : biostratigraphic implications / Schlagintweit, F. ; Rosales, Idoia (Instituto Geológico y Minero de España) ; Najarro, M. (Instituto Geológico y Minero de España)
A new benthic foraminifer is described as Glomospirella cantabrica n. sp. from several sections of the Upper Aptian Reocín Formation and one occurrence in the lowermost Albian Las Peñosas Formation of Cantabria (northern Spain). [...]
2016 - DOI (Digital Object Identifier)

10.1344/GeologicaActa2016.14.2.3
Geologica acta, Vol. 14 Núm. 2 (June 2016) , p. 113-138 (Articles)

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13 p, 1.4 MB

Clypeina tibanai, sp. nov. (Polyphysacea, Dasycladales, Chlorophyta), mid-Cretaceous green alga from the Potiguar Basin, Brazilian margin of the young South Atlantic Ocean / Granier, B. (The University of Kansas. Department of Ecology and Evolutionary Biology) ; Dias-Brito, D. (Universidade Estadual Paulista. Center for Geosciences Applied to Petroleum) ; Bucur, I. I. (Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies)
The fossil genus Clypeina (Michelin, 1845) comprises some 40 species. We describe Clypeina tibanai, a new species from upper Albian-Cenomanian strata of the Potiguar, Brazil, characterised by closely set verticils of tubular, bended laterals. [...]
2014 - DOI (Digital Object Identifier)

10.1344/GeologicaActa2014.12.3.5
Geologica acta, Vol. 12 Núm. 3 (September 2014) , p. 227-237

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14 p, 599.5 KB

Early Cretaceous amber from south-western France : insight into the Mesozoic litter fauna / Perrichot, V. (Géosciences Rennes I)
The Albian amber of Archingeay (Charente-Maritime, SW France) shows a unique ecological feature among worldwide Cretaceous ambers: a large part of the arthropods trapped in this resin are representatives of the litter biota (i. [...]
2004 - DOI (Digital Object Identifier)

10.1344/105.000001629
Geologica acta, Vol. 2, Núm. 1 (2004) , p. 9-22

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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 - DOI (Digital Object Identifier)

10.1344/105.000001443
Geologica acta, Vol. 7, Núm. 3 (Setembre 2009) , p. 363-387

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