The 13C Suess effect in scleractinian corals mirror changes in the anthropogenic CO2 inventory of the surface oceans

Swart, Peter K., Lisa Greer, Brad E. Rosenheim, Chris S. Moses, Amanda J. Waite, A. Winter, Richard E. Dodge, and Kevin Helmle. 2010. The (13)C suess effect in scleractinian corals mirror changes in the anthropogenic CO(2) inventory of the surface oceans RID A-1675-2011 RID B-5241-2011. Geophysical Research Letters 37 (MAR 12): L05604.

Abstract: 
Newd13C data are presented from 10 coral skeletons collected from Florida and elsewhere in the Caribbean (Dominica, Dominican Republic, Puerto Rico, and Belize). These corals range from 96 to 200 years in age and were collected between 1976 and 2002. The change in the d13C of the skeletons from these corals between 1900 and 1990 has been compared with 27 other published coral records from the Atlantic, Pacific, and Indian Oceans. The new data presented here make possible, for the first time, a global comparison of rates of change in the d13C value of coral skeletons. Of these records, 64% show a statistically significant (p < 0.05) decrease in d13C towards the modern day (23 out of 37). This decrease is attributable to the addition of anthropogenically derived CO2 (13C Suess effect) to the atmosphere. Between 1900 and 1990, the average rate of change of the d13C in all the coral skeletons living under open oceanic conditions is approximately −0.01‰ yr−1. In the Atlantic Ocean the magnitude of the decrease since 1960,−0.019 yr−1 ±0.015‰, is essentially the same as the decrease in the d13C of atmospheric CO2 and the d13C of the oceanic dissolved inorganic carbon (−0.023 to −0.029‰ yr−1), while in the Pacific and Indian Oceans the rate is more variable and significantly reduced (−0.007‰ yr−1 ±0.013). These data strongly support the notion that (i) the d13C of the atmosphere controls ambient d13C of the dissolved inorganic carbon which in turn is reflected in the coral skeletons, (ii) the rate of decline in the coral skeletons is higher in oceans with a greater anthropogenic CO2 inventory in the surface oceans, (iii) the rate of d13C decline is accelerating. Superimposed on these secular variations are controls on the d13C in the skeleton governed by growth rate, insolation, and local water masses. Citation: Swart, P. K., L. Greer, B. E. Rosenheim, C. S. Moses, A. J. Waite, A. Winter, R. E. Dodge, and K. Helmle (2010), The 13C Suess effect in scleractinian corals mirror changes in the anthropogenic CO2 inventory of the surface oceans, Geophys. Res. Lett., 37, L05604, doi:10.1029/2009GL041397.