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Exceptionally preserved fossils from Fossil Lagerstätten contribute greatly to resolving details on the history of life on Earth. For the first time, the “Paläontologische Gesellschaft” (PalGes) and the “Palaeontological Society of China” (PSC) combined forces to jointly present an international conference aimed to highlight and encourage the study of exceptionally well-preserved fossil sites worldwide. The conference focused on all aspects of palaeontology and geobiology, also incorporating related fields like biogeochemistry, biology, sedimentology and stratigraphy. The present volume contains the abstracts of more than 275 lectures and posters presented during the joint international conference “Palaeobiology & Geobiology of Fossil Lagerstätten through Earth History”. This year’s conference was held at the northern campus of the Georg-August University in Göttingen, Germany, from September 23-27, 2013. More than three hundred palaeontologists, biologists, geologists and other scientists and researchers from sixteen countries, mainly from Germany and the P. R. of China, participated.
The print edition is published as 2 hardback volumes, parts A and B, and sold as a set. The Carboniferous was the time of the assembly of Pangaea by the collision of the Gondwanan and Larussian supercontinents, and the principal interval of the late Paleozoic ice ages. These tectonic and climatic events caused dramatic sea-level fluctuations and climate changes and produced a Carboniferous world that was diverse topographically and climatologically, perhaps only rivalled in that diversity by the late Cenozoic world. Furthermore, the Carboniferous was a time of the accumulation of vast coal deposits of great economic and societal significance. The temporal ordering of geological and biotic ev...
The Late Pennsylvanian was a time of ice ages and associated climate dynamics. A major reduction in Gondwana ice-volume was followed by a prolonged period of relative global warmth, culminating in the last great ice age of the late Paleozoic. It also was a major turning point in the evolution of life on land, when the coal forests of the Middle Pennsylvanian gave way to new kinds of Late Pennsylvanian wetland vegetation, and new kinds of animals appeared. Changes in the terrestrial biota began during the Middle Pennsylvanian, accelerating and proceeding in a spatially complex manner throughout the Late Pennsylvanian. The Late Pennsylvanian is thus a laboratory for studying environmental changes in a glacial world, and for assessing coeval biotic changes, in part to establish the possible links between the two. No book has been dedicated to this time interval, so this volume fills a gap in our understanding of a dynamic Late Pennsylvanian world that is much like the late Cenozoic world.