Coral skeletons are natural archives whose geochemical signatures provide insights into the tropical ocean history beyond the instrumental record. Carbon stable isotopes from coral skeletons (δ 13 Ccoral) have been used as a proxy for multiple variables on a seasonal basis. Long-term changes in coral δ 13 C relate to the changing isotopic composition of the dissolved inorganic carbon (δ 13 CDIC). δ 13 CDIC in turn reflects changes in the δ 13 C of atmospheric CO2, which in the modern Earth system is governed primarily by anthropogenic injection of CO2 into the atmospherea process known as the Suess Effect.Here we report three δ 13 C coral-based records of Siderastrea stellata from the tropical South Atlantic. U-series dating for the colonies 12SFB-1, 13SS-1 and 13SS-2 suggests these corals lived 13, 57 and 65 years, respectively. Short-term δ 13 C variations in their skeletal aragonite are dominated by inter-annual variation. All three δ 13 C records additionally exhibit an overall decreasing trend, with a depletion of about −0.0243 ± 0.0057 ‰.yr −1 (12SFB-1), −0.0208 ± 0.0007 ‰.yr −1 (13SS-1) and −0.0214 ± 0.0013 ‰.yr −1 (13SS-2). These rates of the coral records from Rocas Atoll are similar to the reported trend for the δ 13 C of atmospheric CO2 over the years 1960-1990 (−0.023 to −0.029 ‰.yr −1 ), and to the estimated decreasing rates of global δ 13 CDIC.Our findings suggest that multiple δ 13 C coral-based records are required for confidently identifying local changes in the δ 13 CDIC of the ocean. This information, in turn, can be used to infer changes in the δ 13 C of the atmospheric CO2 composition and provide valuable information about recent changes on the carbon biogeochemical cycle during the Anthropocene epoch.