Abstract
Determining the origin of light oil presents a significant challenge due to the diversity of genetic types and the limitation of conventional biomarkers. Diamondoid hydrocarbons, characterized by their thermal stability and enrichment in high maturity oil, are considered effective indicators for elucidating generation mechanisms and secondary alteration processes of light oils. In this study, the diamondoid distributions are examined in light oil samples from various regions (i.e., Wushi, Bozi, Dabei, Keshen, Kela, Dina, Dibei, Tuzi, Tudong, Yangtake, Yingmai, Hongqi, and Yaha) in the Kuqa Depression of the Tarim Basin, Northwest China, to discern the origin of the oils. Diamondoids concentrations and ratios in the Kuqa oils show significant variations, indicating two dominant source rock types and various maturity levels. Total diamondoid concentrations (including adamantanes, diamantanes, and triamantanes) vary from 141 to 19,137 ppm. Notably, the light oils from the Kela and Tuzi regions exhibit unusually high diamondoid concentrations (> 9000 ppm), while those from Yingmai, Hongqi, Yaha, Wushi, Keshen, and Tudong regions have relatively lower concentrations (< 2000 ppm). Employing our previously developed source facies discriminant model based on multivariate statistical analysis of multiple diamondoid indices, we suggest that the light oils from the Kela, Keshen, Yangtake, and Yaha regions are originated from lacustrine shales. In contrast, the other studied samples are inferred to primarily derive from coaly source rocks. Meanwhile, our maturity prediction model indicates that the maturity of the Kuqa oils ranges from 0.81 to 2.44 EASY%Ro. The highest maturity is found in the Kela light oils (2.3–2.5 EASY%Ro), while the lowest maturity is observed in the samples from the Wushi, Yingmai, and Hongqi areas (0.8–1.1 EASY%Ro). The formation mechanisms for some samples with anomalous diamondoid distributions are also explored. The Kela light oils, distinguished by their high maturity, abundant diamondoids, and relatively high biomarker concentrations, demonstrate a mixed origin with a notable contribution from highly mature condensates derived from the maturation of lacustrine kerogens. The Tuzi coal-derived oils, exhibiting moderate maturity (1.25% EASYRo) and characterized by elevated adamantane concentrations coupled with inconsistently relatively lower diamantane concentrations, are inferred to be condensates underwent evaporative (or migration) fractionation during upward migration from deeper reservoirs. Our findings corroborate the potential application of diamondoids as previously suggested. In summary, the diamondoid hydrocarbons provide a robust methodology for elucidating the origins, thermal maturity, and formation mechanisms of light oils, particularly within highly mature systems.
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The datasets generated and/or analysed during the current study are available from the corresponding author on reasonable request.
References
Peters, K. E., David, J. C. & Marek, K. An overview of basin and petroleum system modeling: Definitions and concepts. In Basin Modeling: New Horizons in Research and Applications: AAPG Hedberg Series, vol. 4 (eds. Peters, K. E. et al.) 1–16 (2012).
Thompson, K. F. M. Fractionated aromatic petroleums and the generation of gas condensates. Org. Geochem. 11, 573–590 (1987).
Meulbroek, P., Cathles, L. & Whelan, J. Phase fractionation at South Eugene Island block 330. Org. Geochem. 29, 223–239 (1998).
van Graas, G. W., Gilje, A. E., Isom, T. P. & Tau, L. A. The effects of phase fractionation on the composition of oils, condensates and gases. Org. Geochem. 31, 1419–1439 (2000).
Losh, S., Cathles, L. & Meulbroek, P. Gas washing of oil along a regional transect, offshore Louisiana. Org. Geochem. 33, 655–663 (2002).
Losh, S. & Cathles, L. Phase fractionation and oil-condensate mass balance in the South marsh Island block 208–239 area, offshore Louisiana. Mar. Pet. Geol. 27, 467–475 (2010).
Zhang, S. C. et al. Geochemistry of palaeozoic marine petroleum from the Tarim Basin, NW china: part 3. Thermal cracking of liquid hydrocarbons and gas washing as the major mechanisms for deep gas condensate accumulations. Org. Geochem. 42, 1394–1410 (2011).
Peng, P. & Jia, C. Z. Evolution of deep source rock and resource potential of primary light oil and condensate. Acta Petrolei Sinica. 42, 1543–1555 (2021).
Zhang, S. C., Su, J., Zhang, B., Wang, X. M. & He, K. Genetic mechanism and controlling factors of deep marine light oil and condensate oil in Tarim basin. Acta Petrolei Sinica. 42, 1566–1580 (2021).
Wingert, W. S. GC-MS analysis of diamondoid hydrocarbons in smackover petroleums. Fuel 71, 37–43 (1992).
Chen, J. H., Fu, J. M., Sheng, G. Y., Liu, D. H. & Zhang, J. J. Diamondoid hydrocarbon ratios: novel maturity indices for highly mature crude oils. Org. Geochem. 25, 179–190 (1996).
Dahl, J. E. et al. Diamondoid hydrocarbons as indicators of natural oil cracking. Nature 399, 54–57 (1999).
Wei, Z. B., Moldowan, J. M., Jarvie, D. M. & Hill, R. The fate of diamondoids in coals and sedimentary rocks. Geology 34, 1013–1016 (2006).
Li, J. G., Philp, P. & Cui, M. Z. Methyl Diamantane index (MDI) as a maturity parameter for lower palaeozoic carbonate rocks at high maturity and overmaturity. Org. Geochem. 31, 267–272 (2000).
Zhang, S. C., Huang, H. P., Xiao, Z. Y. & Liang, D. G. Geochemistry of palaeozoic marine petroleum from the Tarim Basin, NW China. Part 2: maturity assessment. Org. Geochem. 36, 1215–1225 (2005).
Wei, Z. B. et al. Diamondoid hydrocarbons as a molecular proxy for thermal maturity and oil cracking: geochemical models from hydrous pyrolysis. Org. Geochem. 38, 227–249 (2007).
Wei, Z. B., Moldowan, J. M. & Paytan, A. Diamondoids and molecular biomarkers generated from modern sediments in the absence and presence of minerals during hydrous pyrolysis. Org. Geochem. 37, 891–911 (2006).
Fang, C. C. et al. The origin and evolution of Adamantanes and Diamantanes in petroleum. Geochim. Cosmochim. Acta. 120, 109–120 (2013).
Li, Y. et al. Origin of Adamantanes and Diamantanes in marine source rock. Energy Fuels. 29, 8188–8194 (2015).
Schulz, L. K., Wilhelms, A., Rein, E. & Steen, A. S. Application of diamondoids to distinguish source rock facies. Org. Geochem. 32, 365–375 (2001).
Moldowan, J. M., Dahl, J., Zinniker, D. & Barbanti, S. M. Underutilized advanced geochemical technologies for oil and gas exploration and production-1. The diamondoids. J. Pet. Sci. Eng. 126, 87–96 (2015).
Li, Y. et al. The application of diamondoid indices in the Tarim oils. AAPG Bull. 102, 267–291 (2018).
Esegbue, O., Jones, D. M., van Bergen, P. F. & Kolonic, S. Quantitative diamondoid analysis indicates oil cosourcing from a deep petroleum system onshore Niger delta basin. AAPG Bull. 104, 1231–1259 (2020).
Spaak, G. et al. Identifying multiple sources of petroleum fluids in browse basin accumulations using diamondoids and semi-volatile aromatic compounds. Mar. Pet. Geol. 113, 104091 (2020).
Atwah, I., Moldowan, J. M., Koskella, D. & Dahl, J. Application of higher diamondoids in hydrocarbon mudrock systems. Fuel 284, 118994 (2021).
Forkner, R., Fildani, A., Ochoa, J. & Moldowan, J. M. Linking source rock to expelled hydrocarbons using diamondoids: an integrated approach from the Northern Gulf of Mexico. J. Pet. Sci. Eng. 196, 108015 (2021).
Walters, C. C., Sun, X. & Zhang, T. Geochemistry of oils and condensates from the lower eagle Ford formation, South Texas. Part 4: diamondoids. Mar. Pet. Geol. 154, 106308 (2023).
Grice, K., Alexander, R. & Kagi, R. I. Diamondoid hydrocarbon ratios as indicators of biodegradation in Australian crude oils. Org. Geochem. 31, 67–73 (2000).
Wei, Z. B., Moldowan, J. M., Peters, K. E., Wang, Y. & Xiang, W. The abundance and distribution of diamondoids in biodegraded oils from the San Joaquin valley: implications for biodegradation of diamondoids in petroleum reservoirs. Org. Geochem. 38, 1910–1926 (2007).
Cheng, X., Hou, D. J. & Xu, C. G. The effect of biodegradation on Adamantanes in reservoired crude oils from the Bohai Bay Basin, China. Org. Geochem. 123, 38–43 (2018).
Chang, X. et al. Biodegradation levels of oils from the chepaizi Uplift, Junggar basin (NW China) evaluated by a full-range biodegradation index as constrained by adamantane, Diamantane homologs and carboxylic acids. Mar. Pet. Geol. 146, 105939 (2022).
Sassen, R. & Post, P. Enrichment of diamondoids and 13C in condensate from Hudson Canyon, US Atlantic. Org. Geochem. 39, 147–151 (2008).
Zhu, G. Y. et al. Diamondoids as tracers of late gas charge in oil reservoirs: example from the Tazhong area, Tarim Basin, China. Fuel 253, 998–1017 (2019).
Chai, Z. & Chen, Z. Biomarkers, light hydrocarbons, and diamondoids of petroleum in deep reservoirs of the Southeast Tabei Uplift, Tarim basin: implication for its origin, alteration, and charging direction. Mar. Pet. Geol. 147, 106019 (2023).
Atwah, I., Azzouni, A. & Alalawi, W. Time-lapse diamondoid analysis in unconventional reservoirs: A new frontier in production monitoring. SPE/AAPG/SEG Unconventional Resources Technology Conference (URTeC), D021S037R003 (2024).
AlSaif, M. et al. Diamondoids, biomarkers, and chemofacies: uniting insights on hydrocarbon maturation and migration in the Cline Shale, Midland basin. Org. Geochem. 203, 104953 (2025).
Atwah, I., Mohammadi, S., Moldowan, J. M. & Dahl, J. Episodic hydrocarbon charge in tight Mississippian reservoirs of central Oklahoma, USA: insights from oil inclusion geochemistry. Mar. Pet. Geol. 123, 104742 (2021).
Chakhmakhchev, A., Sanderson, J., Pearson, C. & Davidson, N. Compositional changes of diamondoid distributions caused by simulated evaporative fractionation. Org. Geochem. 113, 224–228 (2017).
Zhu, G. Y. et al. Deepest oil in asia: characteristics of petroleum system in the Tarim basin, China. J. Pet. Sci. Eng. 199, 108246 (2021).
Qi, Y., Sun, P., Cai, C., Wang, D. & Peng, Y. Phase fractionation controlling regional distribution of diamondoids: A case study from the Halahatang oil field, Tarim Basin, China. Mar. Pet. Geol. 140, 105674 (2022).
Liang, D. G., Zhang, S. C., Chen, J., Wang, F. & Wang, P. Organic geochemistry of oil and gas in the Kuqa depression, Tarim Basin, NW China. Org. Geochem. 34, 873–888 (2003).
Zhu, G. Y. et al. Geochemistry, origin and accumulation of continental condensate in the ultra-deep-buried cretaceous sandstone reservoir, Kuqa Depression, Tarim Basin, China. Mar. Pet. Geol. 65, 103–113 (2015).
Zhu, G. Y. et al. The complexity, secondary geochemical process, genetic mechanism and distribution prediction of deep marine oil and gas in the Tarim Basin, China. Earth-Sci. Rev. 198, 102930 (2019).
Yang, H. J. et al. Accumulation conditions, key exploration and development technologies for Keshen gas field in Tarim basin. Acta Petrolei Sinica. 42, 399–414 (2021).
Wang, Q. H. et al. Major breakthrough and exploration significance of well Ketan 1 in Kuqa Depression, Tarim basin. China Pet. Explor. 28, 1–10 (2023).
Zhao, W. Z. et al. Gas systems in the Kuche depression of the Tarim basin: source rock distributions, generation kinetics and gas accumulation history. Org. Geochem. 36, 1583–1601 (2005).
Bao, J., Zhu, C., Zhang, Q., Li, M. & Lu, Y. Geochemical characteristics of crude oil from frontal uplift in Kuqa depression. J. Oil Gas Tech. 29, 40–44 (2007).
Zhang, S. C., Zhang, B., Zhu, G., Wang, H. & Li, Z. Geochemical evidence for coal-derived hydrocarbons and their charge history in the Dabei gas Field, Kuqa thrust Belt, Tarim Basin, NW China. Mar. Pet. Geol. 28, 1364–1375 (2011).
Bao, J., Zhu, C. & Shen, X. Study on diamondoids and genetic mechanism of condensates from the Kela 2 structure in the Kuche depression. Nat. Gas Geosci. 29, 1217–1230 (2018).
Deng, H. et al. Geochemical characteristics of light crude oils/condensates from the Kelasu structural belt of the Kuqa depression in the Tarim Basin, Northwest China. Geochimica 53, 668–680 (2024).
Ji, H., Huang, G., Cheng, D. & Xu, S. Geochemical application of light hydrocarbons in Kuqa depression of Tarim basin: case study of Dawanqi-Dabei areas. Nat. Gas Geosci. 28, 965–974 (2017).
Zhu, G. Y. et al. Composition and origin of molecular compounds in the condensate oils of the Dabei gas field, Tarim Basin, NW China. Pet. Explor. Dev. 46, 482–495 (2019).
Chai, Z. et al. Light hydrocarbons and diamondoids of light oils in deep reservoirs of shuntuoguole low Uplift, Tarim basin: implication for the evaluation on thermal maturity, secondary alteration and source characteristics. Mar. Pet. Geol. 117, 104388 (2020).
Chai, Z. et al. Light hydrocarbons and diamondoids in deep oil from Tabei of Tarim basin: implications on petroleum alteration and mixing. Mar. Pet. Geol. 138, 105565 (2022).
Zhou, C. et al. Oil maturities, mixing and charging episodes in the cratonic regions of the Tarim Basin, NW china: insight from biomarker and diamondoid concentrations and oil bulk properties. Mar. Pet. Geol. 126, 104903 (2021).
Huang, W. et al. Diamondoid fractionation and implications for the Kekeya condensate field in the Southwestern depression of the Tarim Basin, NW China. Mar. Pet. Geol. 138, 105551 (2022).
Huang, W., Zhang, H., Xiao, Z., Yu, S. & Pan, C. Generation, expulsion and accumulation of diamondoids, aromatic components and gaseous hydrocarbons for gas fields in Kuqa depression of the Tarim Basin, NW China. Mar. Pet. Geol. 145, 105893 (2022).
Qiao, R., Li, M., Zhang, D. & Xiao, H. Distribution and origin of higher diamondoids in the ultra-deep paleozoic condensates of the Shunbei oilfield in the Tarim Basin, NW China. Org. Geochem. 197, 104883 (2024).
Qiao, R., Li, M., Zhang, D. & Xiao, H. Geochemistry and accumulation of the ultra-deep ordovician oils in the Shunbei oilfield, Tarim basin: coupling of reservoir secondary processes and filling events. Mar. Pet. Geol. 167, 106959 (2024).
Guo, X. et al. Effects of tectonic compression on petroleum accumulation in the Kelasu thrust belt of the Kuqa Sub-basin, Tarim Basin, NW China. Org. Geochem. 101, 22–37 (2016).
Lei, G. et al. Structural features and natural gas exploration in the Kelasu structural belt, Kuqa depression. Oil Gas Geol. 28, 816–820 (2007).
Liang, Q. Y., Xiong, Y. Q., Fang, C. C. & Li, Y. Quantitative analysis of diamondoids in crude oils using gas chromatography–triple quadrupole mass spectrometry. Org. Geochem. 43, 83–91 (2012).
Xuan, Y., Wang, W., Li, Y., Xiong, Y. & Jiang, W. M. Absolute quantitative analysis and thermal evolution of Trimantanes and tetramantanes in crude oil and source rock. Geochimica 53, 643–654 (2024).
Atwah, I. & Alsaif, M. Novel diamondoid detection technique using pMRM (GC-MS/MS): enabling source rock-oil-condensate correlations. Org. Geochem. 213, 105125 (2026).
Jiang, W. M., Li, Y., Fang, C. C., Yu, Z. Q. & Xiong, Y. Q. Diamondoids in petroleum: their potential as source and maturity indicators. Org. Geochem. 160, 104298 (2021).
Sweeney, J. J. & Burnham, A. K. Evaluation of a simple model of vitrinite reflectance based on chemical kinetics. AAPG Bull. 74, 1559–1570 (1990).
Gong, D. Y. et al. Geochemical characteristics and origins of the oils in Wushi Sag, Ratim basin. Nat. Gas Geosci. 25, 62–69 (2014).
Zhu, G. Y. et al. The geological feature and origin of Dina 2 large gas field in Kuqa Depression, Tarim basin. Acta Petrolei Sinica. 28, 2479–2492 (2012).
Li, J. et al. Source and exploration direction of tight oil and gas in the Dibei section of Northern Kuqa depression. China Pet. Explor. 24, 485–497 (2019).
Zhao, S. F., Chen, W. & Gao, Y. Analysis of fluid geochemical characteristics and accumulation process of Dibei condensate gas reservoir in Kuqa depression. J. Xi’an Shiyou Univer (Nat. Sci. Ed). 37, 1–10 (2022).
Liu, R. H. et al. Geochemical characteristics and implication for gas and oil source correlation in the tugeerming area of the Kuqa Depression, Tarim basin. Nat. Gas Geosci. 30, 574–581 (2019).
Xiao, Z. Y., Huang, G., Lu, Y., Wu, Y. & Zhang, Q. Rearranged Hopanes in oils from the quele 1 Well, Tarim Basin, and the significance for oil correlation. Pet. Explor. Dev. 31, 35–37 (2004).
Liu, C. et al. Geochemical tracer of hydrocarbon migration path of Middle-Cenozoic in the South slope of the Kuqa foreland basin. Acta Geol. Sinica. 94, 3488–3502 (2020).
Jiang, W. M., Li, Y. & Xiong, Y. Q. The effect of organic matter type on formation and evolution of diamondoids. Mar. Pet. Geol. 89, 714–720 (2018).
Gordadze, G. N. Geochemistry of cage hydrocarbons. Pet. Chem. 48, 241–253 (2008).
Okui, A., Nishizuka, T. & Okamoto, S. Petroleum potential of Norwegian sedimentary basins revealed by detailed petroleum system analysis. J. Jpn. Assoc. Pet. Technol. 80, 38–49 (2015).
Fang, C. C., Xiong, Y. Q., Li, Y., Chen, Y. & Tang, Y. J. Generation and evolution of diamondoids in source rock. Mar. Pet. Geol. 67, 197–203 (2015).
Huang, W. Y. & Meinschein, W. G. Sterols as ecological indicators. Geochem. Cosmochim. Acta. 43, 739–745 (1979).
Fang, C. C., Xiong, Y. Q., Liang, Q. Y. & Li, Y. Variation in abundance and distribution of diamondoids during oil cracking. Org. Geochem. 47, 1–8 (2012).
van der Ploeg, R., Pureveen, J. B. M., van den Boorn, S. H. J. M. & van Bergen, P. F. Novel diamondoid-based maturity models using naturally occurring petroleum fluids. AAPG Bull. 107, 1799–1810 (2023).
Burnham, A. K. & Sweeney, J. J. A chemical kinetic model of vitrinite maturation and reflectance. Geochim. Cosmochim. Acta. 53, 2649–2657 (1989).
Jiang, W. M., Li, Y. & Xiong, Y. Q. Source and thermal maturity of crude oils in the Junggar basin in Northwest China determined from the concentration and distribution of diamondoids. Org. Geochem. 128, 148–160 (2019).
Berner, U. & Faber, E. Empirical carbon isotope/maturity relationships for gases from algal kerogens and terrigenous organic matter, based on dry, open-system pyrolysis. Org. Geochem. 24, 947–955 (1996).
Acknowledgements
This work is financially supported by the National Science and Technology Major Project (Grant No. 2025ZD1400500), National Natural Science Foundation of China (Grant No. 42272164), Natural Science Foundation of Guangdong Province (Grant No. 2025A1515010879), and Basic and Applied Basic Research Project of Guangzhou City (Grant No. 2024A04J4751).
Funding
This work is financially supported by the National Science and Technology Major Project (Grant No. 2025ZD1400500), National Natural Science Foundation of China (Grant No. 42272164), Natural Science Foundation of Guangdong Province (Grant No. 2025A1515010879), and Basic and Applied Basic Research Project of Guangzhou City (Grant No. 2024A04J4751).
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H. Z. Z.: Data curation, investigation, validation, resources, writing- original draft, writing-review and editing. Y.W.S.: Data curation, investigation. Y.L.: Conceptualization, funding acquisition, methodology. Y.F.Z.: Data curation, investigation. Y.Q.X.: Conceptualization, funding acquisition, supervision. K.Z.: Data curation, investigation. B.C.L.: Data curation, investigation. W.M.J.: Data curation, funding acquisition, methodology, visualization, writing- original draft, writing-review and editing. All authors reviewed the manuscript.
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Zhang, H., Sun, Y., Li, Y. et al. Application of diamondoids in source and maturity evaluation of light oil: a case study from the Kuqa Depression of the Tarim Basin, NW China. Sci Rep (2026). https://doi.org/10.1038/s41598-026-38619-z
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DOI: https://doi.org/10.1038/s41598-026-38619-z


