In this study, organic matter content, type and maturity as well as some petrographic and physical characteristics of the Jurassic coals exposed in the eastern Taurus were investigated and their depositional environments were interpreted. The total organic carbon (TOC) contents of coals in the Feke-Akkaya, Kozan-Gedikli and Kozan-Kizilinc areas are 24.54, 66.78 and 49.15%, respectively. The Feke-Akkaya and Kozan-Kizilinc coals have low Hydrogen Index (HI) values while the Kozan-Gedikli coals show moderate HI values. All coal samples display very low Oxygen Index (01) values. The Kozan-Gedikli coals contain Type 11 organic matter (OM), the Feke-Akkaya coals contain a mixture of type II and type III OM; and the Kozan-Kizilinc coals are composed of Type III OM. Sterane distribution was calculated as C-27>C-29>C-28 from the m/z 217 mass chromatogram for all coal samples. T-max values for the Feke-Akkaya, Kozan-Gedikli and Kozan-Kizilinc coals are 439, 412 and 427 degrees C. Vitrinite reflectance values (%R-o) for the Feke-Akkaya and Kozan-Kizilinc coal samples were measured as 0.65 and 0.51 and these values reveal that the Feke-Akkaya and Kozan-Kizilinc coals are at subbituminous A or high volatile C bituminous coal stage. On the basis of biomarker maturity parameters, these coals have a low maturity. The pristane/phytane (Pr/Ph) ratios for the Feke-Akkaya, Kozan-Gedikli and Kozan-Kizilinc coals are 1.53, 1.13 and 1.25, respectively. In addition, all coals show a homohopane distribution which is dominated by low carbon numbers, and C-35 homohopane index is very low for all coal samples. All these features may indicate that these coals were deposited in a suboxic environment. The high sterane/hopane ratios with high concentrations of steranes, low Pr/Ph ratios and C-25/C-26 tricyclic ratios >1 may indicate that these coals formed in a swamp environment were temporarily influenced by marine conditions. (C) 2006 Elsevier B.V All rights reserved.