Long-term carbon cycle models are critical for understanding the levels and underlying controls of atmospheric CO 2 over geological time-scales. We have refined the …
A Pedrera, J García-Senz, EL Pueyo, B López-Mir… - Earth-Science …, 2023 - Elsevier
The kinematic evolution of the Pyrenees was largely controlled by structural and thermal heterogeneities inherited from a precursor rift system, resulting in complex along-strike …
Abstract In the northern Iberian Peninsula, the Pyrenean-Cantabrian orogenic belt extends EW for ca. 1000 km between the Atlantic Ocean and Mediterranean Sea. This orogen …
Sedimentary successions provide direct evidence of climate and tectonics, and these give clues about the causes of the mass extinction around the Permian–Triassic boundary …
S Opluštil, JW Schneider - 2023 - pubs.geoscienceworld.org
Abstract In Europe, North Africa and Asia Minor, the remains of Pennsylvanian sedimentary basins bearing continental deposits either intimately mixed with shallow-marine strata or …
In recent years photogrammetry has become an essential tool in the study of tetrapod footprints. Morphological analyses of footprints are interpretative; thus, researchers should …
Intramontane late Carboniferous–Permian basins of western Europe developed during the latest orogenic stages of the Variscan Mountain Belt in eastern Pangaea, at equatorial …
A Tosal, J Pàmies, C Martín-Closas - Palaeogeography, Palaeoclimatology …, 2022 - Elsevier
The Pennsylvanian flora from the intramontane Erillcastell Basin in the eastern Pyrenees (Catalonia, Spain) is described in a palaeoenvironmental context based on a combined …
Palaeo-loess and silty aeolian-marine strata are well recognized across the Carboniferous– Permian of equatorial Pangaea. Aeolian-transported dust and loess appear in the Late …