product and the synthetic (16S)-epimer were, with the one excep-
tion noted, remarkably consistent.
Acknowledgements
We thank UTM Skudai for support to N.B. and Novartis for
support to H. L. We are grateful for a Commonwealth Fellowship
to D. S. N. and we would like to thank Professor W. Kitching for
exchange of 13C NMR data.
Fig. 1 Chemical shift differences in parts per billion between (16S)-2
and the natural product.
Notes and references
1 (a) M. T. Fletcher, S. Chow, L. K. Lambert, O. P. Gallagher, B. W. Cribb,
P. G. Allsopp, C. J. Moore and W. Kitching, Org. Lett., 2003, 5, 5083;
(b) S. Chow, M. T. Fletcher, L. K. Lambert, O. P. Gallagher, C. J. Moore,
B. W. Cribb, P. G. Allsopp and W. Kitching, J. Org. Chem., 2005, 70,
1808.
2 (a) C. Herber and B. Breit, Angew. Chem., Int. Ed., 2005, 44, 5267;
(b) C. Herber and B. Breit, Eur. J. Org. Chem., 2007, 3512; (c) J. Zhou,
Y. Zhu and K. Burgess, Org. Lett., 2007, 9, 1391; (d) G. Zhu, B. Liang
and E.-i. Negishi, Org. Lett., 2008, 10, 1099.
3 S. Donnelly, E. J. Thomas and E. A. Arnott, Chem. Commun., 2003,
1460.
4 S. Donnelly, M. Fielding and E. J. Thomas, Tetrahedron Lett., 2004, 45,
6779.
Fig. 2 Chemical shift differences in parts per billion between (16R)-2
and the natural product.
5 E. J. Thomas, Chem. Rec., 2007, 7, 115.
Having prepared the pentamethyldocosanes (16S)- and (16R)-
2, it remained to establish which diastereoisomer corresponded
to the natural product. Unfortunately, no sample of the natural
product was available and its optical rotation was unknown, and
so it was necessary to compare the 13C NMR data of the two
epimers (16S)-2 and (16R)-2 with the data available for the
natural product. As the 13C NMR spectra of the two epimers
were very similar indeed,1 a quantitative comparison was used.
Fortunately the original data were measured at high field (17.6
T) and reported to 1 ppb precision, so spectra measured at 9.4 T
were processed with Gaussian weighting and extensive zero
filling to allow detailed comparison.
6 N. Basar, S. Donnelly, H. Liu and E. J. Thomas, Synlett, 2010, 575.
7 Synthesized from (S)-citronellol, for an alternative route see ref. 8.
8 D. R. Williams, A. L. Nold and R. J. Mullins, J. Org. Chem., 2004, 69,
5374.
9 M. Wada, H. Ohki and K.-Y. Akiba, Bull. Chem. Soc. Jpn., 1990, 63,
1738.
10 (a) D. A. Evans and M. M. Morrissey, J. Am. Chem. Soc., 1984, 106,
3866; (b) D. A. Evans, M. M. Morrissey and R. L. Dow, Tetrahedron
Lett., 1985, 26, 6005.
11 Spectroscopic data, in particular its 13C NMR spectrum, of alcohol 15
corresponded to those in the literature (ref. 2).
12 As the bromide 3 had an e.e. of ca. 90% (Mosher’s on the corresponding
alcohol), another minor impurity at the 5% level was the diastereoisomer
resulting from the reaction of the enantiomer of bromide 3 with the alde-
hyde 7.
Fig. 1 shows the differences in the chemical shifts between
those listed1 for the natural product and our data for the (16S)-
epimer (16S)-2. Apart from the peak assigned to C(19),19 all the
peaks correspond to within less 5 ppb once the small difference
in referencing is corrected for, with an rms error of 1.4 ppb (less
than the instrumental linewidth).
In contrast, the differences between the chemical shifts listed
for the natural product and our data for the (16R)-epimer (16R)-
2, are much larger, with an rms error of 10 ppb (see Fig. 2).
Based on this comparison, the natural product was identified as
(4S,6R,8R,10S,16S)-4,6,8,10,16-pentamethyldocosane (16S)-2.20
Of interest in this work is the use of the allyl organobismuth
chemistry for the stereoselective synthesis of the undecenol 8,
the confirmation of the relative stereochemistry of the
naturally occurring 4,6,8,10,16-pentamethyldocosane as the
(4S,6R,8R,10S,16S)-epimer (16S)-2, and the unusually detailed
numerical comparison of the 13C spectra of the natural product
and the (16S)- and (16R)-epimers which allowed the assignment
of stereochemistry to be made. Indeed the spectra of the natural
13 K. Mori, Tetrahedron, 2008, 64, 4060.
14 S. E. Denmark, C. S. Regens and T. Kobayashi, J. Am. Chem. Soc., 2007,
129, 2774.
15 D. Raederstorff, A. Y. L. Shu, J. E. Thompson and C. Djerassi, J. Org.
Chem., 1987, 52, 2337.
16 E. Hedenström, H. Edlund, S. Lund, M. Abersten and D. Persson,
J. Chem. Soc., Perkin Trans. 1, 2002, 15, 1810.
17 Y. S. Chow, J. H. Williams, Q. Huang, S. Nanda and I. A. Scott, J. Org.
Chem., 2005, 70, 9997.
18 E. Hedenström, B. V. Nguyen and L. A. Silks, Tetrahedron: Asymmetry,
2002, 13, 835.
19 In the 13C NMR spectrum of the natural product, the peak at δ 29.712
was originally assigned to both C(4) and C(19) but C(19) has since been
reassigned to a peak at δ 29.697 although this peak was partly obscured
by an impurity in the natural product. (Personal communication from Pro-
fessor W. Kitching.) However, it remains slightly more than 5 ppb differ-
ent from the peak at δ 29.6987 assigned to C(19) in (16S)-2 and from the
peak at δ 29.6951 assigned to C(19) in the 13C NMR spectrum of (16R)-
2.
20 This work establishes the relative configuration of the natural 4,6,8,10,16-
pentamethyldocosane. As the optical rotation of the natural hydrocarbon
is unknown, the absolute configuration shown was provisionally assigned
by analogy with that of the naturally occurring 4,6,8,10,16,18-hexam-
ethyldocosane 1 (see ref. 2).
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