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"James F. Kasting" is a Professor at Penn State University, where he holds joint appointments in the Departments of Geosciences and Meteorology and is an affiliate of the NASA Astrobiology Institute and Penn State's ESSC. He received his undergraduate degree from Harvard University in Chemistry and Physics and did his PhD in Atmospheric Sciences at the University of Michigan. Prior to coming to Penn State in 1988, he spent 7 year in the Space Science Division at NASA Ames Research Center. Dr. Kasting is a Fellow of the American Association for the Advancement of Science and of the International Society for the Study of the Origin of Life. His research focuses on the evolution of planetary atmospheres, particularly the question of why the atmospheres of Mars and Venus are so different from that of Earth. Dr. Kasting is also interested in the question of whether habitable planets exist around other stars and how we might look for signatures of life by doing spectroscopy on their atmospheres.
"Robert G. Crane" received his PhD in Geography from theUniversity of Colorado, Boulder. After working as a Research Associate in the National Snow and Ice Data Center and the World Data Center-A for Glaciology in Boulder, he spent a year teaching at the University of Saskatchewan before moving to Penn State in 1985. Dr. Crane's research has been on microwave remote sensing of sea ice, ice-climate interactions, and, more recently, regional-scale climate change, climate downscaling techniques, and climate change and variability in southern Africa. He is coeditor of a text on the applications of artificial neural networks in geography. Currently Dr. Crane holds the position of Professor in the Department of Geography and an affiliate of the ESSC. He also serves as the Associate Dean for Education in the College of Earth and Mineral Sciences at Penn State.
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Book Description Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Establishment of a well-characterized, well-dated and well-archived succession of rocks for the period of 2500-2000 Ma Documentation of the changes in the biosphere and the geosphere associated with the rise in atmospheric oxygen Development. Seller Inventory # 449138533
Book Description Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Earth's present-day environments are the outcome of a 4.5 billion year period of evolution reflecting the interaction of global-scale geological and biological processes. Punctuating that evolution were several extraordinary events and episodes that perturbed the entire Earth system and led to the creation of new environmental conditions, sometimes even to fundamental changes in how planet Earth operated.Volume 3: Global Events and the Fennoscandian Arctic Russia - Drilling Earth Project represents another kind of illustrated journey through the early Palaeoproterozoic, provided by syntheses, reviews and summaries of the current state of our understanding of a series of global events that resulted in a fundamental change of the Earth System from an anoxic to an oxic state. The book discusses traces of life, possible causes for the Huronian-age glaciations, addresses radical changes in carbon, sulphur and phosphorus cycles during the Palaeoproterozoic, and provides a comprehensive description and a rich photo-documentation of the early Palaeoproterozoic supergiant, petrified oil-field. Terrestrial environments are characterised through a critical review of available data on weathered and calichified surfaces and travertine deposits. Potential implementation of Ca, Mg, Sr, Fe, Mo, U and Re-Os isotope systems for deciphering Palaeoproterozoic seawater chemistry and a change in the redox-state of water and sedimentary columns are discussed. The volume considers in detail the definition of the oxic atmosphere, possible causes for the oxygen rise, and considers the oxidation of terrestrial environment not as a single event, but a slow-motion process lasting over hundreds of millions of years. Finally, the book provides a roadmap as to how the FAR-DEEP cores may facilitate future interesting science and provide a new foundation for education in earth-science community.Welcome to the illustrative journey through one of the most exciting periods of planet Earth! 528 pp. Englisch. Seller Inventory # 9783662522035
Book Description Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Earth's present-day environments are the outcome of a 4.5 billion year period of evolution reflecting the interaction of global-scale geological and biological processes. Punctuating that evolution were several extraordinary events and episodes that perturbed the entire Earth system and led to the creation of new environmental conditions, sometimes even to fundamental changes in how planet Earth operated.Volume 3: Global Events and the Fennoscandian Arctic Russia - Drilling Earth Project represents another kind of illustrated journey through the early Palaeoproterozoic, provided by syntheses, reviews and summaries of the current state of our understanding of a series of global events that resulted in a fundamental change of the Earth System from an anoxic to an oxic state. The book discusses traces of life, possible causes for the Huronian-age glaciations, addresses radical changes in carbon, sulphur and phosphorus cycles during the Palaeoproterozoic, and provides a comprehensive description and a rich photo-documentation of the early Palaeoproterozoic supergiant, petrified oil-field. Terrestrial environments are characterised through a critical review of available data on weathered and calichified surfaces and travertine deposits. Potential implementation of Ca, Mg, Sr, Fe, Mo, U and Re-Os isotope systems for deciphering Palaeoproterozoic seawater chemistry and a change in the redox-state of water and sedimentary columns are discussed. The volume considers in detail the definition of the oxic atmosphere, possible causes for the oxygen rise, and considers the oxidation of terrestrial environment not as a single event, but a slow-motion process lasting over hundreds of millions of years. Finally, the book provides a roadmap as to how the FAR-DEEP cores may facilitate future interesting science and provide a new foundation for education in earth-science community.Welcome to the illustrative journey through one of the most exciting periods ofplanet Earth!. Seller Inventory # 9783662522035
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