 Atmospheric Lifetime of Fossil Fuel Carbon Dioxide by David Archer and others

Annual Review of Earth and Planetary Sciences 37, 117–134. The physical ocean and solid-Earth portions distinguish fast exchange, slow ocean equilibration and a long carbonate/weathering tail. Biological mechanisms are outside the present expansion.

Author-hosted text: climatemodels.uchicago.edu/geocarb/archer.2009.ann_rev_tail.pdf

Cited physical-chemistry passages: Table 1, p. 119, and physical ocean/solid-Earth conclusions, p. 131.