1887
PDF

Abstract

Summary

Δ2-sterenes have long been postulated to represent the precursors of 3β-alkylsteranes, although this relationship has remained speculative in the absence of proven intermediates. The observed prevalence of C5 and C6 alkyl moieties has also prompted the suggestion that 3β-alkylsteranes may derive from precursors with a sugar substituent at C-3. Recognition of the presence of both Δ2-sterenes and methylated Δ2-sterenes in a Cenomanian-Turonian sediment sequence deposited during OAE2 provides convincing evidence that validate a potential pathway for formation of 3-methylsteranes. The similarity in the proportions of corresponding homologs (C27, C28, and C29 versus C28, C29, and C30) for both series of sterenes supports their assignment as precursor and product. In addition, the carbon number distributions of the methylated Δ2-sterenes are wholly distinct from those of co-occurring 4-methylsteroidal hydrocarbons refuting the possibility that the former are 4-methylster-2-enes. The relative retention times of the methylated Δ2-sterenes are uniform among the three series and consistent with expectations for methylation at C-3, which was confirmed by the presence of 3-methylsteranes after hydrogenation.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.202533250
2025-09-07
2026-02-09
Loading full text...

Full text loading...

/deliver/fulltext/2214-4609/2025/imog-2025/250.html?itemId=/content/papers/10.3997/2214-4609.202533250&mimeType=html&fmt=ahah

References

  1. Schlanger & Jenkyns, 1976. Geologie en mijnbouw55, 179–184.
    [Google Scholar]
  2. Arthur et al., 1987. doi:10.1144/GSL.SP.1987.026.01.25
    https://doi.org/10.1144/GSL.SP.1987.026.01.25
  3. TurgeonBrumsack, 2006. doi:10.1016/j.chemgeo.2006.05.008
    https://doi.org/10.1016/j.chemgeo.2006.05.008
  4. Mort et al., 2007. doi:10.1016/j.cretres.2006.09.003
    https://doi.org/10.1016/j.cretres.2006.09.003
  5. Jenkyns et al., 2007. doi:10.1029/2006PA001355
    https://doi.org/10.1029/2006PA001355
  6. Gambacorta et al., 2015. doi:10.1127/nos/2015/0066
    https://doi.org/10.1127/nos/2015/0066
  7. Owens et al., 2016. doi:10.1016/j.epsl.2016.05.046
    https://doi.org/10.1016/j.epsl.2016.05.046
  8. Brassell, 1984. doi:10.2973/dsdp.proc.75.133.1984
    https://doi.org/10.2973/dsdp.proc.75.133.1984
  9. Brassell & Farrimond, 1986. Mitt. Geol.-Palaontol. Inst. Univ. Hamburg, 60, 311–338.
    [Google Scholar]
  10. Farrimond et al., 1986. doi:10.1144/GSL.SP.1986.021.01.25
    https://doi.org/10.1144/GSL.SP.1986.021.01.25
  11. Rullkötter et al., 1987. doi:10.2973/dsdp.proc.93.148.1987
    https://doi.org/10.2973/dsdp.proc.93.148.1987
  12. Forster et al., 2004. doi:10.2973/odp.proc.ir.207.110.2004
    https://doi.org/10.2973/odp.proc.ir.207.110.2004
  13. Forster et al., 2008. doi:10.1016/j.palaeo.2008.07.006
    https://doi.org/10.1016/j.palaeo.2008.07.006
  14. Sepúlveda et al., 2009. doi:10.1016/j.orggeochem.2009.02.009
    https://doi.org/10.1016/j.orggeochem.2009.02.009
  15. French et al., 2019. doi:10.1016/j.orggeochem.2019.02.007
    https://doi.org/10.1016/j.orggeochem.2019.02.007
  16. Forkner et al., 2021. doi:10.1038/s41598‑021‑92817‑5
    https://doi.org/10.1038/s41598-021-92817-5
  17. Robinson et al., 2024. doi:10.1016/j.palaeo.2023.111496
    https://doi.org/10.1016/j.palaeo.2023.111496
  18. Dastillung & Albrecht, 1977. doi:10.1038/269678b0
    https://doi.org/10.1038/269678b0
  19. Gagosian & Farrington, 1978. doi:0016‑7037/78/0801‑1091
    https://doi.org/0016-7037/78/0801-1091
  20. Summons & Capon, 1988. doi:10.1016/0016-7037(88)90042-7
  21. Killops & Abbott, 2022. doi:10.1016/j.chemgeo.2022.121014
    https://doi.org/10.1016/j.chemgeo.2022.121014
  22. Riboulleau et al., 2023. doi:10.5802/crgeos.233
    https://doi.org/10.5802/crgeos.233
/content/papers/10.3997/2214-4609.202533250
Loading
/content/papers/10.3997/2214-4609.202533250
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error