14 S. Sakuda, M. Ono, K. Furihata, J. Nakayama, A. Suzuki and
for 1 h. The mixture was filtered and the solid washed with HCl
(5%; 1 cm3). The filtrate was concentrated by azeotropic distil-
lation from ethanol, and the residue triturated twice with acet-
one, then dried (in vacuo over phosphorus pentoxide) to give the
product 7c (48.7 mg, 100% of hydrochloride), [α]D28 10.0 (c 1,
H2O); TLC: single spot on CHIRALPLATE at lower Rf
A. Isogai, J. Am. Chem. Soc., 1996, 118, 7855; M. Ono, S. Sakuda,
H. Ikeda, K. Furihata, J. Nakayama, A. Suzuki and A. Isogai,
J. Antibiot., 1998, 51, 1019.
15 A. G. M. Barrett, J. Head, M. L. Smith and N. S. Stock, Chem.
Commun., 1999, 133; A. G. M. Barrett, J. Head, M. L. Smith, N. S.
Stock, A. J. P. White and D. J. Williams, J. Org. Chem., 1999, 64,
6005.
16 O. Spavold and J. Bremer, Biochim. Biophys. Acta, 1989, 1003, 72;
For application in biosynthetic studies, see: Z. Li, F. M. Martin and
J. C. Vederas, J. Am. Chem. Soc., 1992, 114, 1531; Y. Liu, Z. Li and
J. C. Vederas, Tetrahedron, 1998, 54, 15937.
17 J. M. Behan, R. A. W. Johnstone and M. J. Wright, J. Chem. Soc.,
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524.
19 T. J. Simpson, in Biosynthesis: Polyketides and Vitamins, ed. F. J.
Leeper and J. C. Vederas, Springer, Berlin, 2000, pp. 1–48. For a
review of the use of oxygen-18 and deuterium isotope shifts, oxygen
exchange with medium and effects of pulsed feeding on spectra, in
biosynthetic studies, see: J. C. Vederas, Nat. Prod. Rep., 1987, 4, 277.
20 For magnitudes of deuterium and oxygen-18 isotope shifts, see:
P. E. Hansen, Annu. Rep. NMR Spectrosc., 1983, 15, 106.
21 D. E. Cane, T.-C. Liang and H. Hasler, J. Am. Chem. Soc., 1982,
104, 7274.
1
than the -enantiomer (above); H NMR, 13C NMR, CI-MS
and EI-MS gave results that were identical to those for the
-enantiomer.
DL-[1-13C,18O2]Serine 11
-[1-13C]Serine (106 mg), H218O (0.09 cm3) and conc. HCl (0.1
cm3) were sealed into a flame-dried glass tube under a nitrogen
atmosphere. The tube was heated at 90 ЊC in an oil-bath for
5 days. After cooling, the mixture was neutralised with NaOH
and lyophilised. The resulting material containing the product
and sodium chloride was used without further purification. 1H
NMR (D2O; 200 MHz) spectrum was indistinguishable from
that for -[1-13C]serine; 13C NMR (D2O; 50 MHz) spectrum
was as for the starting material but the C᎐O resonance at
᎐
δC 172.4 was enhanced and exhibited 3 peaks, ∆δ 0.027 ppm
per 18O; 24% 18O2, 48% 18O16O, 28% 16O2, corresponding to 70
atom% 18O per site.
22 For an example, see: A. K. Demetriadou, E. D. Laue and
J. Staunton, J. Chem. Soc., Chem. Commun., 1985, 764, 1125.
23 L. R. Kass and D. J. H. Brock, Methods Enzymol., 1969, 14, 696.
24 M. J. Robins, S. D. Hawrelak, T. Kanai, J.-M. Siefert and R. Mengel,
J. Org. Chem., 1979, 44, 1317.
Acknowledgements
25 E. W. Miles and P. McPhie, J. Biol. Chem., 1974, 249, 2852.
26 C. A. Townsend, A. M. Brown and L. T. Nguyen, J. Am. Chem. Soc.,
1983, 105, 919.
27 A. I. P. M. de Kroon, J. W. Timmermans, J. A. Killian and B. de
Kruijff, Chem. Phys. Lipids, 1990, 54, 33.
28 L. Velluz, G. Amiard and R. Heymes, Bull. Soc. Chim. Fr., 1954,
1015.
29 H. Gorissen, C. van der Maesen, A. Mockel, G. Journee and
V. Libert, in Synthesis and Applications of Isotopically Labelled
Compounds 1991, ed. E. Buncel and G. W. Kabalka, Elsevier,
New York, 1992, pp. 588–591.
Financial support from the Natural Sciences and Engineering
Research Council of Canada (NSERC) is gratefully acknow-
ledged. Cambridge Isotopes is thanked for a grant of isotopic-
ally labelled compounds. H218O was a generous gift from
Professor J. C. Vederas, University of Alberta. We thank
Professor A. D. Bain at McMaster for assistance with the
spectral simulation.
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