In: International journal of earth sciences, 2005, vol. 94, p. 711
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In: International Journal of Earth Sciences, 2005, vol. 94, no. 4, p. 697-710
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In: International journal of earth sciences, 2005, vol. 94, p. 697
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In: Swiss Journal of Geosciences, 2013, vol. 106, no. 2, p. 125–133
A re-analysis and new description of the incertae sedis Calcicarpinum? fallax is presented, and its Late Oligocene age and paleobiogeographical distribution is ascertained. It is identified as a nutlet of a Boraginaceae and is named Boraginocarpus fallax (Taugourdeau-Lantz & Rosset 1966) comb. nov.
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In: The Journal of Foraminiferal Research, 2011, vol. 41, no. 3, p. 248-259
Although foraminifera have been found living in inland saline lakes isolated from the sea, this phenomenon has rarely been recognized in the fossil record. This study documents the occurrence of benthic foraminifera in Holocene lake sediments located nearly 500 km inland from the Red Sea, in the Al-Mundafan region of southern Saudi Arabia. The lake formed during a regional pluvial period,...
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In: Swiss Journal of Geosciences, 2011, vol. 104, p. 115-132
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. Suppl. 1, p. 115-132
The primitive ruminant genus Iberomeryx is poorly documented, as it is essentially only known from rare occurrences of dental remains. Therefore, the phylogeny and palaeobiology of Iberomeryx remain rather enigmatic. Only two species have been described: the type species I. parvus from the Benara locality in Georgia, and the Western European species I. minor reported from France, Spain, and...
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In: Swiss Journal of Palaeontology, 2012, vol. 131, no. 1, p. 161-181
Since the first exploitation of the Huppersandstones quarry of Rickenbach (Canton Solothurn, Switzerland) in 1898, many fossils of plants, molluscs, and vertebrates have been discovered. The study of the small mammals brought this locality to international recognition as the type locality for the European mammalian reference level MP29 (latest Oligocene). Our study reviews the terrestrial...
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In: Swiss Journal of Geosciences, 2008, vol. 101, no. 2, p. 483-513
Les dépôts oligocènes marins, situés dans la partie distale du bassin molassique suisse et dans le prolongement sud du fossé rhénan, sont constitués par les groupes stratigraphiques suivants: les Conglomérats de Porrentruy, le Septarienton et le Meeressand. Cette série sédimentaire a fait l’objet d’études stratigraphiques, sédimentologiques et paléontologiques détaillées. Trois...
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