Δ2-Triterpenes: Early intermediates in the diagenesis of terrigenous triterpenoids

HL Ten Haven, TM Peakman, J Rullkötter - Geochimica et Cosmochimica …, 1992 - Elsevier
HL Ten Haven, TM Peakman, J Rullkötter
Geochimica et Cosmochimica Acta, 1992Elsevier
A series of Δ 2-triterpenoids (oleana-2, 12-diene, oleana-2, 13 (18)-diene, oleana-2, 18-
diene, ursa-2, 12-diene, and taraxera-2, 14-diene) has been identified in Holocene buried
mangrove sediments (Florida, USA) by comparison of the mass spectra of and by co-
injections with authentic standards. In the Oligocene Brandon lignite (Vermont, USA) oleana-
2, 12-diene and oleana-2, 13 (18)-diene were also identified, along with two A-ring
contracted amyrin derivatives. By comparison with the sedimentary occurrence of related …
Abstract
A series of Δ2-triterpenoids (oleana-2,12-diene, oleana-2,13(18)-diene, oleana-2,18-diene, ursa-2, 12-diene, and taraxera-2,14-diene) has been identified in Holocene buried mangrove sediments (Florida, USA) by comparison of the mass spectra of and by co-injections with authentic standards. In the Oligocene Brandon lignite (Vermont, USA) oleana-2,12-diene and oleana-2,13(18)-diene were also identified, along with two A-ring contracted amyrin derivatives. By comparison with the sedimentary occurrence of related analogues of oxyallobetulin and betulin and the demonstrated diagenetic formation of lup-2-ene from lupan-3-one, these novel terrigenous biological markers are considered diagenetic products formed by dehydration of precursor molecules, such as α- and β-amyrin, and taraxerol. The identification of these early intermediates brings us one step closer to the full understanding of the diagenetic fate of terrigenous triterpenoids.
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