OCEANIC C-13 C-12 OBSERVATIONS - A NEW WINDOW ON OCEAN CO2 UPTAKE/

Equations are developed describing the rate of change of carbon isotop ic ratios in the atmosphere and oceans in terms of deltaC-13 quantitie s. The equations enable one to perform calculations directly with delt a and epsilon quantities commonly reported in the literature. The main cause of the change occurring today is the combustion of fossil fuel carbon with lower deltaC-13 values. The course of this isotopic anomal y in atmosphere and oceans can provide new constraints on the carbon b udgets of these reservoirs. Recently published deltaC-13 isotopic data of total inorganic carbon in the oceans [Quay et al., 1992] appear to lead to incompatible results with respect to the uptake of fossil fue l CO2 by the oceans if two different approaches Lo the data are taken. Consideration of the air-sea isotopic disequilibrium leads to an upta ke estimate of only a few tenths of a gigaton C (Gt, for 10(15) g) per year, whereas the apparent change in the ocean deltaC-13 inventory le ads to an estimate of more than 2 Gt C yr-1. Both results are very unc ertain with presently available data. The isotopic ratio has the advan tage that the signal-to-noise ratio for the measurement of the uptake of the isotopic signal by the oceans is better than for the uptake of total carbon. The drawback is that isotopic exchange with carbon reser voirs that are difficult to characterize introduces uncertainty into t he isotopic budget. The accuracy requirements for the measurements are high, demanding careful standardization at all stages.