The partitioning of stable isotopes of carbon between coexisting calcite and graphite is sensitive to temperature and, as a pressure-independent system, is a useful geothermometer in metamorphic rocks.  Differing versions of the calcite-graphite thermometer strongly diverge below temperatures of 600° C.  This study investigates the calcite-graphite exchange in marble subjected to regional metamorphism at temperatures of 450-500° C based on calcite-dolomite geothermometry.  The study area lies in southern Ontario, in the Belmont Domain of the Elsevier Terrane, Grenville Province—an area also referred to as the Hastings Low, which includes the lowest grade of metamorphism in the southern Grenville.  Samples taken for this study are from outcrops located at least 2 km from mapped igneous intrusions in an effort to avoid thermal aureoles.

To date, calcite in 29 samples and graphite in 14 samples have been analyzed.  The d¹⁸O values of the calcite range from 18.09 to 29.76 ‰, while d¹³C values of carbonates range from -1.17 to 5.48 ‰ and d¹⁶C values of bulk graphite range from -0.18 to -3.75 ‰ (one outlier at +3.32 ‰ is not considered further).  ∆_cc-gr values (∆_cc-gr=d¹³C_calcite - d¹³C_graphite) for 12 samples are in the range of 6.1 to 11.3 ‰.  These correspond to temperatures of 490 to 290°C, respectively, using the formulation of Dunn & Valley (1992).  The lower ∆_cc-gr values yield reasonable temperatures for this area, but we believe the larger values represent incomplete exchange of the isotopically light organic matter precursor with surrounding calcite due to sluggish self-diffusion within graphite grains.  We are attempting to examine different size fractions of graphite within single samples to determine if isotopic zoning is present.  Graphite grains <5 μm in one sample are 2.5 ‰ lighter (d¹³C=-13.55 ‰) than graphite grains 5-10 and 10-15 μm (d¹³C=-11.02 and -11.04 ‰, respectively).  If confirmed in additional samples, this suggests that coarsening promotes isotopic exchange and that the finest graphite fraction is furthest from isotopic equilibrium.