Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed but, as today, polar day length added a hostile element to this otherwise tranquil climate. With the aid of scientists from all the countries close to the Arctic Circle, this book describes the palaeontology, the statistical analysis of vegetational features, comparisons with atmospheric, marine, and geological features and some of the first models of plant migration developed from newly constructed databases.Proceeidngs of the NATO Advances Research Workshop on Reconstruction of North Atlantic Climate Change Using Extinct Plant Data, held in London, UK, November 11-16, 1993Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed but, as today, polar day length added a hostile element to this otherwise tranquil climate. With the aid of scientists from all the countries close to the Arctic Circle, this book describes the palaeontology, the statistical analysis of vegetational features, comparisons with atmospheric, marine, and geological features and some of the first models of plant migration developed from newly constructed databases.Section 1: Introduction.- Towards a Review of Tertiary Palacobotany in the Boreal Realm.- Fossil Plants as Palaeoenvironmental Indicators.- Section 2: The Atmosphere, Tectonics and the Marine Realm.- Palaeo-Ecophysiological Studies on Cretaceous and Tertiary Fossil Floras.- Cenozoic Tectono-Magmatic Events in the North Atlantic: Potential Palaeo-Environmental Implications.- Cenozoic Dinoflagellate Palaeoecology Elucidated, and Used for Marine-Terrestrial Biological CorrelatiolӜ