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Abstract

Summary

Hopanoids are among the most common biomarkers in fossil sediments and thus serve as a tool to reconstruct paleoenvironmental conditions. Despite their high abundance and compositional variability in sediments, coals and oils, their precursor organisms are often hard to distinguish. Although the diagenetic fate of hopanoids remains partially unresolved, their distributions and degrees of isomerization are widely applied in maturity assessment and palaeoenvironmental reconstruction. To investigate sources and diagenetic pathways of a variety of hopanoids co-occurring in a single sample, we analysed immature sediments from the Early Toarcian (∼183 Ma). Here, we present a suite of hopanoids forming a diagenetic continuum comprised of hopanoid species within a sedimentary succession of identical maturity. The diverse hopanoid inventory hosts aliphatic (neohop-13(18)-enes, hop-17(21)-enes, hopanes), aromatic (benzohopanes, diaromatic 8(14)-secohopanes, tri- and tetra-aromatic hopanes) functionalized (hop-17(21)-enoic acids, hopanoic acids) and thio-hopanoids (hop-17(21)-ene thiolanes, hopane thiolanes, hopane thiophenes), several of which have not been previously reported. Most of these hopanoids are present as A-ring methylated analogues. Here, for hopanoids occurring as 2-methyl hopanoids, the C33 homologues are especially abundant and yield high 2a-methyl/(2a-methyl + desmethyl) ratios, pointing to a common precursor biohopanoid, which may be especially abundant in cyanobacteria and/or nitrogen cycle affiliated a-proteobacteria.

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/content/papers/10.3997/2214-4609.202533049
2025-09-07
2026-02-15
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