Extinction and recovery patterns of the vegetation across the Cretaceous-Palaeogene boundary - a tool for unravelling, the causes of the end-Permian mass-extinction
High-resolution palynofloral signatures through the Cretaceous-Palaeogene boundary succession show several features in common with the Permian-Triassic transition but there are also important differences. Southern Hemisphere Cretaceous-Palaeogene successions, to date studied at high resolution only in New Zealand, reveal a diverse palynoflora abruptly replaced by fungi-dominated assemblages that a
