The Vardar Zone is a product of the Triassic-Jurassic opening Neotethys, Jurassic obduction, Late Cretaceous/Paleogene consumption oceanic crust and continental collision. During last process, Eastern was thrust over Central eventually both onto Western Zone. present paleomagnetic structural study provided new results from first two zones in Belgrade area. younger set data, together with publis...

Abstract The Cenozoic history of the Tibetan Plateau topography is critical for understanding evolution Indian‐Eurasian collision, climate, and biodiversity. However, long‐term growth landscape remain ambiguous, it remains unclear if plateau uplift occurred soon after India‐Asia collision in Paleogene (∼50–25 Ma) or later Neogene (∼20–5 Ma). Here, we reproduce southeastern using a 2D model, whi...

The Fayum Depression of Egypt has yielded fossils of hystricognathous rodents from multiple Eocene and Oligocene horizons that range in age from ∼37 to ∼30 Ma and document several phases in the early evolution of crown Hystricognathi and one of its major subclades, Phiomorpha. Here we describe two new genera and species of basal phiomorphs, Birkamys korai and Mubhammys vadumensis, based on rost...

1 Albrecht-von-Haller-Institut f r Pflanzenwissenschaften, Abteilung Systematische Botanik, Georg-August-Universit t G ttingen, Untere Karsp le 2, 37073 G ttingen, Germany 2 Department of Botany, The Field Museum, 1400 South Lake Shore Drive, Chicago, IL, U.S.A. 3 Nachtigallenweg 9, 29342 Wienhausen, Germany 4 Courant Research Centre Geobiology, Georg-August-Universit t G ttingen, Goldschmidtst...