Late Cretaceous oil shales, located in the Yarmouk sub-basin (North Jordan), were analysed using techniques of organic and inorganic geochemistry, coupled with a microfossil study. Results of this study were used to reconstruct the paleoenvironmental and paleoclimatic conditions during the Late Cretaceous and to investigate their influence on organic matter enrichment of the oil shale deposits. The analysed oil shales have high TOC and S-total content values in the ranges of 2.11-12.85 wt.% and 1.83-8.81 wt%, respectively. The high S-total content and its relation with TOC values indicate that the sulfur is associated with organic matter and that the oil shales were deposited in a marine environment under reducing conditions, This is shown by petrographic observation and supported by biomarker distributions. The microscopic investigation indicated that the oil shales contain abundant liptinitic materials (i.e. alginite and amorphous organic matter) and planktonic foraminifera. The presence of these sapropelic materials and planktonic foraminifera assemblages further suggests a marine origin. Biomarker distributions are also known to reflect dominantly marine plankton/algal and microorganisms source input, Water column stratification and low oxygen (reducing) conditions are indicated by narrow Pr/Ph values, relatively high V/Ni elemental ratios and the presence of gammacerane. Reducing conditions contribute to preservation of organic matter. Warm-water periods during the late Cretaceous are also indicated by dominant occurrences of warm water index microfossil taxa. The warm climate combined with elevated phosphorus (P) are the major causes of excessive algae growth, and led to enhanced biological productivity within the photic zone of the water column during deposition of the oil shale deposits. This increased bio-productivity in combination with good preservation of organic matter are the main mechanisms of organic matter enrichment within the Late Cretaceous oil shales in the north Jordan. (C) 2016 Elsevier B.V. All rights reserved.