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Ediacaran to Cambrian oceanic rocks of the Gondwana margin and their tectonic interpretation

von Raumer, Jürgen ; Stampfli, Gérard ; Arenas, Ricardo ; Sánchez Martínez, Sonia

In: International Journal of Earth Sciences, 2015, vol. 104, no. 5, p. 1107-1121

Oysters and oyster-like bivalves from the Middle Triassic Muschelkalk of the Germanic Basin

Hautmann, M. ; Hagdorn, H.

In: Paläontologische Zeitschrift, 2013, vol. 87, no. 1, p. 19-32

Cartographie sectorielle du paléoenvironnement de la plaine alluviale du Rhône suisse depuis la fin du Petit Age Glaciaire: la métamorphose fluviale de Viège à Rarogne et de Sierre à Sion

Laigre, Laetitia ; Reynard, Emmanuel ; Arnaud-Fassetta, Gilles

In: Bulletin de la Murithienne, 2009, p. 7-18

L’identité professionnelle en question : de l’autrui significatif en formation des enseignants

Wentzel, Bernard

In: Actes de la Recherche, 2007, no. 6, p. 91-101

Studies on continental Late Triassic tetrapod biochronology : II: The Ischigualastian and a Carnian global correlation

Cardoso Langer, Max

In: Journal of South American Earth sciences, 2005, vol. 19, p. 219-239

Sedimentology and paleoecology of a diverse early jurassic tetrapod tracksite in Lesotho, Southern Africa

Smith, Roger M.H. ; Marsicano, Claudia A. ; Wilson, Jeffrey A.

In: Palaios : international journal of the Society of Economic Paleontologists and Mineralogists, 2009, vol. 24, p. 672-684

Tetrapod postural shift estimated from Permian and Triassic trackways

Kubo, Tai ; Benton, Michael J

In: Palaeontology, 2009, vol. 52, no. 5, p. 1029-1037

Tetrapods from the Late Jurassic lithographic limestones and Plattenkalke of Western Europe : an updated comparative review

Billon-Bruyat, Jean-Paul ; Marty, Daniel ; Bocat, Loïc

In: 5th International Symposium on Lithographic Limestone and Plattenkalk : abstracts and field guides, 2009, p. 17-18

The formation of Pangea

Stampfli, G.M. ; Hochard, C. ; Vérard, C. ; Wilhem, C. ; Raumer, Jürgen F. von

In: Tectonophysics, 2013, vol. 593, p. 1-19

The making of Pangea is the result of large-scale amalgamation of continents and micro-continents, which started at the end of the Neoproterozoic with the formation of Gondwana. As pieces were added to Gondwana on its South-American, Antarctica and Australia side, ribbon-like micro-continents were detached from its African and South-Chinese side: Cadomia in the late Neoproterozoic, Avalonia...

Tithonian marine reptiles of the western Neuquén basin, Argentina : facies and palaeoenvironments

Gasparini, Zulma ; Spalletti, Luis A.

In: Geobios : paléontologie, stratigraphie, paléoécologie, 1997, vol. 30, no. 5, p. 701