“…-free and/or thermolabile hydrocarbons, mg/g sample, evolved at 300 °C S2 -cracked hydrocarbons, mg/g sample, evolved between 300-650 °C TC -total carbon, % from sample TOC -total organic carbon, % from sample T max -temperature for maximum of surface S2, °C OI -oxygen index HI -hydrogen index BI -bitumen index RC -residual carbon E -activation energy, kJ/mol A -frequency factor FID -flame ionisation detector HC -hydrocarbons R -gas constant, 8.314 J/mol β -heating rate, °/min Rock-Eval pyrolysis [1] has been a widely used method in organic geochemistry for examining the oil and gas potential and maturity of different ancient and recent sediment samples [2][3][4][5][6][7][8]. The method was extended to biomass samples in the paper [9]. Besides, a software OPTKIN was developed [10] for description of pyrolysis kinetics using the Rock-Eval measurements.…”