The export of newly produced organic carbon from the surface ocean and its regeneration at depth account for an estimated three-quarters of the vertical£CO2 gradient shown in Fig. 1 (Volk and Hoffert, 1985). If these processes, often referred to as the" biological pump," had ...
CITATION STYLE
Sarmiento, J. L., & Siegenthaler, U. (1992). New Production and the Global Carbon Cycle. In Primary Productivity and Biogeochemical Cycles in the Sea (pp. 317–332). Springer US. https://doi.org/10.1007/978-1-4899-0762-2_18
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