Abstract
A new type of kerogen, defined as Type I-S with an atomic H/C ratio > 1.5 and an atomic S (sub org) /C ratio > 0.04 is reported from two lacustrine deposits in fault-bounded basins of E Iberia. The morphology and chemical structure of the kerogens are described. The Ribesalbes kerogen is mainly composed of fossilized organic matter of the freshwater alga Botryococcus braunii. The results indicate the large variability in palaeodepositional conditions in lacustrine environments.