The anthropogenic delta(13)C change for the time period 1968 to 1991 was de
termined based on calculations of the preformed C-13/C-12 of dissolved inor
ganic carbon (DIC) distributions on isopycnal surfaces in the main thermocl
ine of the Pacific, North Atlantic and South Indian Oceans. The time rate o
f change of preformed delta(13)C (the C-13 Suess effect) along isopycnals w
as calculated using CFC-derived water ages and yields a time history of the
surface water delta(13)C change at the isopycnal outcrop location. The sur
face ocean Suess effect recorded on isopycnals decreased with increasing ou
tcrop latitude from approximately -0.2 parts per thousand decade(-1) within
the subtropics to around -0.1 parts per thousand decade(-1) in the subpola
r oceans. In the Pacific Ocean these surface delta(13)C change rate reconst
ructions agree, both in magnitude and meridional trend, with direct observa
tions of surface ocean delta(13)C changes reported from time series measure
ments and from comparisons of surface water delta(13)C of DIC measurements
in 1970 and 1993, A global ocean average surface delta(13)C rate of change
of -0.15 +/- 0.04 parts per thousand decade(-1) is determined, which is sli
ghtly smaller than a previous time series data and model-based estimate (-0
.171 parts per thousand decade(-1), [Bacastow et al., 1996]). Depth integra
tions of the C-13 reconstructions in the Pacific, Indian, and Atlantic Ocea
ns, when combined with these previous individual depth profile comparisons
and Geochemical Ocean Sections Study bomb C-14 inventories [Quay et al., 19
92], imply a global depth-integrated delta(13)C change rate of -9.7 +/- 2.4
parts per thousand m yr(-1) over the time period 1970-1990. These results
imply a net oceanic CO2 uptake rate of 1.9 +/- 0.9 Gt C yr(-1) over the tim
e period 1970-1990 when applied to an atmospheric (CO2)-C-13 and (CO2)-C-12
budget.