Abstract
The reported source rocks for the abundant petroleum in the Tarim Basin, China range from Cambrian to Lower Ordovician and/or Upper Ordovician in age. However, the difference between the two groups of source rocks is not well characterized. In this study, pyrite was removed from eleven mature to over mature kerogen samples from source rocks using the method of CrCl 2 reduction and grinding. The kerogen and coexisting pyrite samples were then analyzed for δ 34S values. Results show that the kerogen samples from the Cambrian have δ 34S values between +10.4‰ and +19.4‰. The values are significantly higher than those from the Lower Ordovician kerogen ( δ 34S of between +6.7‰ and +8.7‰), which in turn are generally higher than from the Upper Ordovician kerogen samples ( δ 34S of between −15.3 and +6.8‰). The associated pyrite shows a similar trend but with much lower δ 34S values. This stratigraphically controlled sulfur isotope variation parallels the evolving contemporary marine sulfate and dated oil δ 34S values from other basins, suggesting that seawater sulfate and source rock age have an important influence on kerogen and pyrite δ 34S values. The relatively high δ 34S values in the Cambrian to Lower Ordovician source rocks are associated with abundant aryl isoprenoids, gammacerane and C 35 homohopanes in the extractable organic matter, indicating that these source rocks were deposited in a bottom water euxinic environment with water stratification. Compared with the Upper Ordovician, the Cambrian to Lower Ordovician source rocks show abundance in C 28 20R sterane, C 23 tricyclic terpanes, 4,23,24-trimethyl triaromatic dinosteroids and depletion in C 24 tetracyclic terpane, C 29 hopane. Thus, δ 34S values and biomarkers of source rock organic matter can be used for distinguishing the Cambrian and Upper Ordovician source rocks in the Tarim Basin.
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