Attached please find a publication entitled " Accurate, Direct Total Organic Carbon (TOC) Log from a New Advanced Geochemical Spectroscopy Tool: Comparison with Conventional Approaches for TOC Estimation" that covers the answer to your question.
I have copied equation 5 (see below) that depicts the correlation between the parameters of concern.
TOC = (Δ log R) × 10(2.297 – 0.1688LOM) (5)
where LOM is the level of organic maturity (Hood et al., 1975). The LOM can be determined from a variety of measurements including
vitrinite reflectance, Tmax, or Rock Eval if the type of organic matter is known. Therefore, if two formations have the same Δ log R values but
different LOM values, estimated TOC will be different. However, in over-mature shale reservoirs with LOM values greater than 10.5, the limit
of calibration of maturity to TOC is reached. In these formations, a LOM value of 10.5 should be used (Passey et al., 2010).
Carbonaceous material constitutes a major fraction of atmospheric aerosol. This fraction is thought to be responsible for adverse health effects caused by its reductive potential and the presence of specific organic species. Although a substantial part of carbonaceous material may not be readily identified, two sub fractions of total carbon (TC), n...
The present study is carried out to determine the sedimentation rate, grain size, organic matter and bathymetry of the Renuka Lake situated in the Lesser Himalaya. The 210Pb and 137Cs radioactive dating technique used for the determination of sedimentation rate indicated 0.78 cm/year and 0.51 cm/year (~0.64 cm/year) for the period of past 61 years...