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in organic matter were to increase from the average value at present, then the net new flux of carbon to depth would also increase. Fourth, a reduction in the biological formation of particulate inorganic carbon in the surface ocean would increase surface alkalinity and enhance ocean carbon sequestration. Finally, most of the organic matter The hottest product firefighter 343 never forget september 11th flagproduced by plankton is respired in the upper few hundred meters of the water column, with only a small fraction reaching the mid-depth to deep ocean where the respired CO2 is isolated from the atmosphere for many decades to centuries because of the relatively slow overturning circulation of the ocean. In model simulations, increasing the depth where sinking particles are respired back to CO2 results in increased ocean carbon sequestration (Kwon et al., 2009). These scenarios are not mutually exclusive and could arise because of changes in ocean circulation, external nutrient and trace-metal inputs, and plankton food-web dynamics. One perturbation will be climate change forced by the combustion of fossil fuels. point-source emissions are typically several orders of magnitude greater than the total available industrial byproduct alkalinity in locations across the country.
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