Carbon and Oxygen Isotopic Data from the Clino core

Abstract: This dataset reports δ13C and δ18O data of limestone collected from the Clino core located in the shallow sub-surface of the Bahamas from the Bahama Drilling Project in 1990.

Other Description: Swart, P.K. and Oehlert, A.M. (2018) Revised interpretations of stable C and O patterns in carbonate rocks resulting from meteoric diagenesis. Sedimen. Geol. 364, 14-23.

Oehlert, A.M. and Swart, P.K. (2019) Rolling window regression of δ13C and δ18O values in carbonate sediments: Implications for source and diagenesis. The Depositional Record 5, 613-630.

Melim, L.A., Swart, P.K. and Maliva, R.G. (2001) Meteoric and marine-burial diagenesis in the subsurface of Great Bahama Bank, in: Ginsburg, R.N. (Ed.), Subsurface geology of a prograding carbonate platform margin, Great Bahama Bank: results of the Bahama Drilling Project. Society of Economic Paleontologists and Mineralogists, Tulsa, pp. 137-161.

Melim, L.A., Swart, P.K. and Eberli, G.P. (2004) Mixing-zone diagenesis in the subsurface of Florida and The Bahamas. J. Sed. Res. 74, 904-913.