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Past and present of sediment and carbon biogeochemical cycling models

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Fig. 1, they are implicit in the diagram as the main transportagents that are responsible for the chemically reactive andphysical material flows within the system.
Fig. 2. Organic and inorganic carbon cycles in the coastal zone and open ocean, fluxes in units of 10 Figure 212 mol C yr−1 (1 Gton C = 83.3×1012mol C; modified from Wollast, 1998; Rabouille et al., 2001; Wollast, 1994; Morse and Mackenzie, 1990; Milliman 19
Fig. 3.Figure 3 Simplified two-box model of the coupled organic and in-organic carbon cycles in the coastal zone (from Mackenzie et al.,1998)
Fig. 4.Figure 4 Carbon changes in the atmosphere and surface ocean in thelast 300 years of industrial time
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