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Hopanoids aromatic/aromatization

Fig. 4. Scheme for the alteration of hopenoids to aromatic hopanoids and hopane (namtal product examples are boxed). [Pg.85]

Aromatization of hopanoids, when derived from bacterial detritus in sediments, is inferred to proceed via diagenetic alteration or bonding of the precursors to organic matter (e.g. diploptene to neohopene. [Pg.85]

In contrast, hopanoidal precursors have no removable functional group at C-3 and aromatization begins... [Pg.192]

Aromatic hopanoids with the same carbon-number distributions as the hopanes are sometimes observed, although they are usually minor components. They must arise from the same precursors as the hopanes. [Pg.193]

The greatest abundances of higher plant derived aromatic triterpenoids and their degradation products are, not surprisingly, found in brown coals. However, aromatic hopanoids and related compounds can also be... [Pg.196]

Hussler G., Connan J., Albrecht P. (1984) Novel families of tetra- and hexacyclic aromatic hopanoids predominant in carbonate rocks and crude oils. Org. Geochem. 6, 39—49. [Pg.340]


See other pages where Hopanoids aromatic/aromatization is mentioned: [Pg.582]    [Pg.85]    [Pg.452]    [Pg.614]    [Pg.932]    [Pg.83]    [Pg.34]    [Pg.193]    [Pg.193]    [Pg.196]    [Pg.196]    [Pg.180]    [Pg.40]    [Pg.622]   
See also in sourсe #XX -- [ Pg.196 ]




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