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First fossil frog from Antarctica: implications for Eocene high latitude climate conditions and Gondwanan cosmopolitanism of Australobatrachia

Mörs, Thomas ; Reguero, Marcelo ; Vasilyan, Davit

In: Scientific Reports, 2020, vol. 10, p. 5051

Cenozoic ectothermic continental tetrapods (amphibians and reptiles) have not been documented previously from Antarctica, in contrast to all other continents. Here we report a fossil ilium and an ornamented skull bone that can be attributed to the Recent, South American, anuran family Calyptocephalellidae or helmeted frogs, representing the first modern amphibian found in Antarctica. The two bone...

The Valais units in Savoy (France): a key area for understanding the palaeogeography and the tectonic evolution of the Western Alps

Loprieno, Andrea ; Bousquet, Romain ; Bucher, Stefan ; Ceriani, Stefano ; Dalla Torre, Florian ; Fügenschuh, Bernhard ; Schmid, Stefan

In: International Journal of Earth Sciences, 2011, vol. 100, no. 5, p. 963-992

Taphonomy and palaeoecology of the green Devonian gypidulid brachiopods from the Aferdou El Mrakib, eastern Anti-Atlas, Morocco

Tessitore, Lorena ; Schemm-Gregory, Mena ; Korn, Dieter ; Wild, Ferdinand ; Naglik, Carole ; Klug, Christian

In: Swiss Journal of Palaeontology, 2013, vol. 132, no. 1, p. 23-44

Laser ablation U/Pb age patterns of detrital zircons in the Schlieren Flysch (Central Switzerland): new evidence on the detrital sources

Bütler, Endrio ; Winkler, Wilfried ; Guillong, Marcel

In: Swiss Journal of Geosciences, 2011, vol. 104, no. 2, p. 225-236

The north-subducting Rheic Ocean during the Devonian: consequences for the Rhenohercynian ore sites

Raumer, Jürgen F. von ; Nesbor, Heinz-Dieter ; Stampfli, Gérard M.

In: International Journal of Earth Sciences, 2017, vol. 106, no. 7, p. 2279–2296

Base metal mining in the Rhenohercynian Zone has a long history. Middle-Upper Devonian to Lower Carboniferous sediment-hosted massive sulfide deposits (SHMS), volcanic-hosted massive sulfide deposits (VHMS) and Lahn-Dill-type iron, and base metal ores occur at several sites in the Rhenohercynian Zone that stretches from the South Portuguese Zone, through the Lizard area, the Rhenish Massif...

The Devonian nekton revolution

Klug, Christian

In: Lethaia : an international journal of palaeontology and stratigraphy, 2009, p. 1-13

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...

Ordovician magmatism in the external French Alps: witness of a peri-gondwanan active continental margin

Bussy, François ; Péronnet, V. ; Ulianov, A. ; Epard, J.L. ; Raumer, Jürgen F. von

In: Ordovician of the World : 11th International Symposium on the Ordovician System, Alcalá de Henares, Spain, May 9-13, 2011, 2011, p. 75-82

Devonian tetrapod trackways and trackmakers : a review of the fossils and footprints

Clack, Jennifer A

In: Palaeogeography, palaeoclimatology, palaeoecology : an international journal for the geo-sciences, 1997, vol. 130, p. 227

End-permian mass extinction pattern in the northern Peri-Gondwanan region

Zhong Shen, Shu

In: Palaeoworld, 2006, vol. 15, p. 3