The high-temperature photochemistry (HTP) and laser photolysis-shock tube (LP-ST) techniques have been combined to study the kinetics of the reaction between ground-state oxygen atoms with CH3Cl over the temperature range, 556–1485 K. In the HTP reactor, used for the 556–1291 K range, O atoms were generated by flash photolysis of O2, CO2 or SO2, and the atom concentrations were monitored by resonance fluorescence, while with the LP-ST technique, used for the 916–1485 K range, O atoms were generated by the photolysis of either SO2 or NO with the 193 nm light from a pulsed ArF excimer laser, and atomic resonance absorption spectroscopy (ARAS) was used to monitor [O]t. In both studies, rate coefficients were derived from the [O] profiles under the pseudo-first-order condition, [O] ≪[CH3Cl]. The data obtained by the two techniques are in excellent agreement and are best represented by the expression, k(T)=2.57×10−11 (T/K)0.31 exp(−5633 K/T) cm3 molecule−1 s−1 with a 2σ precision varying from ±6 to ±22% and an estimated 2σ accuracy of ±21% to ±30%, depending on temperature. The rate coefficients for the title reaction are essentially identical to those for the O+CH4 reaction over the observed temperature range, the reasons for which are discussed.