Titlebook: Carbon in the Geobiosphere; - Earth‘s Outer Shel Fred T. Mackenzie,Abraham Lerman Book 2006 Springer Science+Business Media B.V. 2006 Bioge

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BILIO

Carbon Dioxide in Natural Waters,s surface environment. It would be an understatement to say that the literature on this subject is extensive—it is prodigious! In Chapter 2 we dealt with the Earth’s atmosphere in the past and present that is based mostly on the model of an ideal gas. However, CO. on the Earth’s surface interacts wi

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Isotopic Fractionation of Carbon: Inorganic and Biological Processes,ances of isotopic species measured by their ratios provide indications of the origin of various materials and differences in the abundance ratios that develop in different processes make it possible to identify the mechanisms behind a variety of phenomena in extraterrestrial space, within the solid

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Carbon in the Oceanic Coastal Margin,nd sediment accumulation occur. At present, the coastal zone is more or less synonymous with the continental shelf that is covered by ocean water as a result of ice melting and sea level rise of 120 meters since the end of the Last Glacial Maximum about 18,000 years ago. In some intervals of the geo

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Natural Global Carbon Cycle through Time,tion and climatic change relevant to that behavior. A discussion of glacial-interglacial changes in the carbon cycle follows to provide background of carbon system behavior prior to major human interference in the carbon cycle. We utilize and emphasize portions of the previous chapters to present a