期刊
ORGANIC GEOCHEMISTRY
卷 37, 期 7, 页码 772-786出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2006.03.005
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A new series of rearranged hopanes ranging from C-29 to at least C-34 has been identified as 28-nor-spergulanes (or 21-methyl-28-nor-hopanes). The C-29 member of the series was unambiguously identified as 17 beta,18 alpha-28-nor-spergulane using NMR spectroscopy. All members of the series have typical hopane mass spectra with an m/z 191 base peak, but the m/z 369 fragment is unusually intense (70-90%). The C-29 28-nor-spergulane (29Nsp) is always the dominant member of the series and 28-nor-spergulanes having more than 31 carbon atoms are insignificant in all samples. The content of 29Nsp is often positively correlated with that of other rearranged C-29 hopanes (neohopanes and diahopanes). However, 29Nsp seems to be particularly abundant in some oils from lacustrine source rocks in South East Asia. Laboratory experiments suggest that the precursors of 28-nor-spergulanes are hop-17(21)-enes which are oxidized to hopadienes, rearranged to 28-nor-spergula-12,17-dienes and finally reduced, forming 28-nor-spergulanes. The two double bonds necessary for rearrangement might also be formed by migration of double bonds from the side chain after elimination of hydroxyl groups in biological hopanoids. A late eluting compound in the 398 -> 191 transition used for detection of 29Nsp was tentatively identified as 24-nor-gammacerane. (c) 2006 Elsevier Ltd. All rights reserved.
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