In: Palaeobiodiversity and Palaeoenvironments, 2019, vol. 99, no. 3, p. 527–543
Simplomys, a dormouse with a simple dental morphology compared to other glirids, shows a continuous evolution in Spain during the end of the Ramblian and up to the middle Aragonian, the stratigraphic frame considered in this work. In contrast, the record of the genus in Central Europe is reduced to a few localities spanning from the early to the middle Miocene. We review the record from the...
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Porrentruy : Office de la culture, Paléontologie A16, 2018
(Catalogues du patrimoine paléontologique jurassien - A16)
ISBN: 9782884360555
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Porrentruy : Office de la culture, Paléontologie A16, 2018
(Catalogues du patrimoine paléontologique jurassien - A16)
ISBN: 9782884360548
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In: Swiss Journal of Geosciences, 2013, vol. 106, no. 2, p. 291-301
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In: International Journal of Earth Sciences, 2005, vol. 94, no. 4, p. 697-710
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In: PLoS ONE, 2015, vol. 10, no. 10, p. e0140223
Cold-water coral (CWC) ecosystems occur worldwide and play a major role in the ocean's carbonate budget and atmospheric CO2 balance since the Danian (~65 m.y. ago). However their temporal and spatial evolution against climatic and oceanographic variability is still unclear. For the first time, we combine the main macrofaunal components of a sediment core from a CWC mound of the Melilla Mounds...
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In: Paläontologische Zeitschrift, 2016, vol. 90, p. 101-123
Excavations of two fossiliferous layers in the Wallenried sand- and marl pit produced a very diversified vertebrate fauna. New material allows the reassessment of the taxonomic position of the ruminant taxa Andegameryx andegaviensis and endemic Friburgomeryx wallenriedensis. An emended diagnosis for the second species is provided and additional material of large and small mammals, as well as...
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In: Journal of African Earth Sciences, 2014, vol. 100, p. 586–597
A detailed sedimentary section of the marine Chouabine Formation in the palaeogeographic Gafsa Basin, south-western Tunisia, was investigated in order to characterize environmental and depositional conditions focusing on the interval that spans the Paleocene–Eocene transition. We did stable isotope analyses of bulk sediments. Both phosphorite and carbonate yielded relatively similar isotopic...
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In: Deep Sea Research Part II: Topical Studies in Oceanography, 2014, vol. 99, p. 249–269
Cold-water coral (CWC) settlement in northern Norway is strongly related to the outlet-glaciers of the Fennoscandian Ice-sheet, and dating of known CWC structures show clearly post-glacial ages. Two gravity cores (POS391 559/2,277 cm long and POS391 559/3,282 cm long) were recovered on a CWC reef in the area of Lopphavet, northern Norway. Detailed investigations on lithology (sediment structures...
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In: Swiss Journal of Geosciences, 2013, vol. 106, no. 2, p. 291–301
This study analyses the regressive phase of the marine Froidefontaine Subgroup and the subsequent fluvio-lacustrine Niederroedern formation in the southern Upper Rhine Graben during the Late Rupelian and the position of the Rupelian/Chattian boundary. The study is based on the sedimentary record and several microfossil groups from two boreholes, with a focus on new records of fish otoliths,...
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