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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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Biogeochemical Transformations of Silicon Along the Land–Ocean Continuum and Implications for the Glely changes as consequence of global changes. Largescale programs investigated the oceanic cycling of carbon (C) and associated biogenic elements, mainly nitrogen (N) and phosphorus (P), as limiting nutrients of the global production by marine phytoplankton (Falkowski 1997; Tyrrell 1999). However, c
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Coupled Circulation/Biogeochemical Models to Estimate Carbon Flux1on 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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Sediment and Carbon Accumulation on Continental Shelves1ution, 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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