The ranges of vitrinite reflectance values, defining zones in which oil andgas generation occur, are examined from severalpoints of view. Geochemical consideration of coalification reactions, kerogen compositions, iso-reflectance lines, spore colour and fluorescence, electron-spin resonance, extract data and reservoir temperatures point to the following approximate ranges: oil generation 1.0-2.0% R,, wet gas and condensate 1.5-3.0% R,, methane2.0-5.0% R,. Biogenicmethanecan beformedat < 0.6 % R, and hydrogen generation from kerogen appears to be possible above 5.0% R,. These results point to hydrocarbon generation under hotter, deeper conditions than thoseproposed in mostprevious schemes. A s a consequence, reflectance ranges are broadened for traces of vitrinite in possible reservoirs: oil < 0.4-1.3% R,, methane < 0.4-3.0% R,.