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\The fossil history of animal life in India is central to our understanding of the tectonic evolution of Gondwana, dispersal of India, its northward journey, and its collision with Asia. This book provides the only detailed overview of the paleobiogeographic, tectonic, and paleoclimatic evolution of the Indian plate from Gondwana to Asia. This thorough, up-to-date volume is a must-have reference for researchers and students in Indian geology, paleontology, plate tectonics, and collision of continents.
This publication combines the interpretations of two major sets of data. One if the geophysical data that is used to interpret the position of the tectonic plates through geologic time. The other is based on a long time search of the geological literature to find, record, and evaluate the lithologic descriptions of countless reports around the globe; paying careful attention to those lithologies that have climatic implications. The introduction to this volume includes a detailed discussion of the lithologies, mineralogies and biogeographies that are considered to be the most reliable in identifying the climatic conditions existing during their formation and how they are used or not used in this compilation. Global paleoclimatic zones based on the climatically interpreted data points are identified during the twenty-eight time periods from Cambrian to Miocene using paleotectonic reconstructed maps. The paleoclimate of each time period is summarized and includes a discussion of the specific referenced data points that have been interpreted to be the most reliable available for that time period and location.
Provides an introduction to global warming that explains why and how it occurs and the accuracy and inaccuracy of the media type that accompanies it.
In the Palaeozoic Era, the best evidence for estimating the positions of continents and oceans comes from palaeomagnetism and from the geographical distribution of fossils. This memoir contains contributions from eminent palaeomagnetists and palaeontologists from America, Asia, Australiasia and Europe. The information presented includes the most recent palaeomagnetic and biogeographic data from all major Palaeozoic continents. From this information, a new set of world maps has been produced illustrating successive positions of the continents and oceans throughout the Palaeozoic Era.
"This volume summarizes new developments in understanding the longest-lived icehouse period in Phanerozoic Earth history, the late Paleozoic ice age. Resolving the Late Paleozoic Ice Age in Time and Space provides summaries of existing and new data from the various Gondwanan continental relics, and also reviews stratigraphic successions from the paleotropical and temperate regions of Laurussia that preserve an indirect record of glaciation. It addresses the extent to which records of glaciation indicate protracted, long-term climatic austerity, as opposed to fluctuating, more dynamic climate, and provides new constraints on the timing of glaciation. Additionally, it tackles questions of synchroneity of glaciation across the various Gondwanan continental relics, and timing relationships between near-field and far-field records at greater levels of resolution than has been possible previously. Results point toward a dynamic icehouse regime that is comparable to the Cenozoic icehouse, and away from traditional interpretations of the late Paleozoic ice age as a single, protracted event that involved stable, long-lived ice centers."--Publisher's website.
A collection of extended abstracts of papers presented at two workshops on the title subject.