Abstract Changes in pollen and spore assemblages across the Cretaceous–Paleogene (K–
Pg) boundary elucidate the vegetation response to a global environmental crisis triggered …

One of the most significant climate changes in the history of Earth happened during the late
Palaeozoic, with the melting of the Gondwanan ice sheets and a progressive warming that …

Nonmarine biostratigraphic/biochronologic schemes have been created for all or parts of the
late Carboniferous–Middle Triassic using palynomorphs, megafossil plants, conchostracans …

Abstract The Permian-Triassic rifting represents the first of the two Mesozoic rifting stages
recorded in the Iberian Peninsula. Its first phases of development started during the Early …

The main reservoir quality controls in Triassic Buntsandstein deposits in the Upper Rhine
Graben and surrounding outcrops in Germany and France are discussed to be authigenic …

Studies of the effects of mass extinctions on ancient ecosystems have focused on changes
in taxic diversity, morphological disparity, abundance, behaviour and resource availability as …

Well-preserved marine fossils in carbonate rocks permit detailed studies of the end-Permian
extinction event in the marine realm. However, the rarity of fossils in terrestrial depositional …

The ultimate driver of the end-Permian mass extinction is a topic of much debate. Here, we
used a multiproxy and paleoclimate modeling approach to establish a unifying theory …

Carbonate and anhydrite cement, clay clasts and inter-granular clay are the main
components that reduce reservoir quality in the studied Bunter Sandstone Formation. The …

The evolution of trees and forests through the Devonian Period fundamentally changed the
Earth's land biosphere, as well as impacting physical environments and geomorphology by …