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It was established that the same type of organic matter was accumulated in ancient salts independently of their ages and mineralogical compositions. The origin of hydrocarbons of salt bitumoids was aquagennic organic matter, which accumulated in restore conditions. Data of alkane, sterane and triterpane distributions in conjunction with other geochemical and geological information were used here.
Svetlana N. Shanina
"Biomarkers in organic matter of the ancient salt deposits", Proc. SPIE 4939, Instruments, Methods, and Missions for Astrobiology VI, (30 January 2003); https://doi.org/10.1117/12.486692
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Svetlana N. Shanina, "Biomarkers in organic matter of ancient salt deposits," Proc. SPIE 4939, Instruments, Methods, and Missions for Astrobiology VI, (30 January 2003); https://doi.org/10.1117/12.486692