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Titlebook: Carbon and Nutrient Fluxes in Continental Margins; A Global Synthesis Kon-Kee Liu,Larry Atkinson,Liana Talaue-McManus Book 2010 Springer-Ve

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O. Büyüköztürk,R. Haupt,C. Tuakta,J. Chenon budget and for developing and testing our understanding of processes that ultimately control these budgets. Continental margins are composed of the continental slope, shelf, and rise. These coastal regions are a crucial boundary between land and ocean, a focal point for the accumulation and trans
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Progress in Theoretical Computer Science, hydrosphere, lithosphere, and the biosphere. In the natural carbon cycle, the time period for the atmosphere–biosphere exchange is the shortest with a range of just a few months to a few decades. The atmosphere–hydrosphere exchange of CO., on the other hand, takes several 100 years if the interior
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Isaac Elishakoff,Lova Andriamasyution, the continental shelf sedimentation patterns formed during the Holocene period and the related processes are examined, the impact of sedimentary processes on carbon burial on the continental shelf is evaluated, and the scientific problems that need solutions for the future trends of sediment
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https://doi.org/10.1007/978-3-540-92735-8Biogeochemical fluxes; Carbon cycle; Coast; Coastal ocean; Continental shelves; Global change; IGBP; Indian
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978-3-662-51787-1Springer-Verlag Berlin Heidelberg 2010
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Carbon and Nutrient Fluxes in Continental Margins978-3-540-92735-8Series ISSN 1619-2435
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