D. W. Knight et al. / Tetrahedron Letters 43 (2002) 9187–9189
9189
References
1. (a) Castro, C. E.; Gaughan, E. J.; Owsley, D. C. J. Org.
Chem. 1966, 31, 4071; (b) Castro, C. E.; Stephens, R. D.
J. Org. Chem. 1963, 28, 2163; (c) Liao, H.-Y.; Cheng,
C.-H. J. Org. Chem. 1995, 60, 3711.
2. Vasilevsky, S. F.; Schvartsberg, M. S. Izv. Akad. Nauk
SSSR, Ser. Khim. 1990, 2089 and references cited therein.
3. (a) Vasilevsky, S. F.; Shvartsberg, M. S. Izv. Akad. Nauk
SSSR, Ser. Khim. 1983, 1686; (b) Vasilevsky, S. F.;
Pozdyakov, A. V. Izv. Sib. Otd. Akad. Nauk SSSR, Ser.
Khim, 1985, 1367. See also (c) Vasilevski, S. F.;
Tretyakov, E. V. Annalen, 1995, 775; (d) Tretyakov, E.
V.; Knight, D. W.; Vasilevsky, S. F. J. Chem. Soc.,
Perkin Trans. 1, 1999, 3721.
4. Hanrahan, J.; Knight, D. W.; Salter, R. Synlett 2001,
1587.
5. Sonogashira, K.; Tohda, Y.; Hagihara, N. A. Tetra-
hedron Lett. 1975, 4467.
6. General method: Warm solutions of hydroxylamine
hydrochloride (6 eq.) in methanol (0.5 ml mmol−1) and
potassium hydroxide (9 eq.) in methanol (0.25 ml
mmol−1) were mixed and the resulting solution cooled to
below 40°C when potassium chloride precipitated. This
was filtered off and a methyl 2-alkynylbenzoate (1 equiv.)
was added. The resulting mixture was then refluxed until
the reaction appeared to be complete according to TLC
(ca. 3 h). The cooled mixture was then evaporated. Excess
ice-cold 2 M hydrochloric acid was added to the residue
and the product extracted into dichloromethane. The
combined organic extracts were washed with water and
brine then dried, filtered and evaporated. Crystallization
of the resulting residue, usually from ethyl acetate or
ethyl acetate-petrol mixtures then secured the pure prod-
ucts in the yields quoted.
Scheme 5.
which, while clearly limited to a particular substituent,
are remarkable for their selectivity in favour of either
endo or exo-cyclisation. In each case, examination of
crude material did not reveal the presence of the alter-
native product. At present we can only speculate on the
origins of this very high selectivity which may be associ-
ated with the fact that all isoindolones are formed when
the alkyne is substituted with an electron-withdrawing
group, albeit not a powerful one, while the isoquinoli-
nones 8 and 17 have electron-donating substituents.
However, these relatively weak influences of such sub-
stituents does not seem entirely sufficient to account for
such a high level of regioselectivity. Hopefully further
studies along with theoretical calculations will provide a
better insight.11
7. Moriconi, E. J.; Creegan, F. J. J. Org. Chem. 1966, 31,
2090.
8. These data have been deposited on the Cambridge Crys-
tallographic Database: Compound
8
[CCDC No.
193931], compound 11 [CCDC No. 193932].
9. Isoindolinone 14a showed lH (CDC13) 4.70 (1H, d, J 6.3)
and 5.91 (t, J 6.3) while the related protons in analogue
14b resonated at 4.58 and 5.83.
Acknowledgements
10. (a) Gabriel, S. Ber. 1883, 16, 1995; (b) Kampschmidt, L.
W; Wibaut, J. P. Rec. Trav. Chem. 1954, 73, 431; (c)
Sudoh, Y; Jin, Z.-T; Matsamura, H. J. Heterocycl. Chem.
1982, 19, 525.
11. Full analytical and spectroscopic data consistent with the
proposed structures have been obtained for all com-
pounds reported herein.
We are grateful to EPSRC for support of the X-ray
crystallographic facilities in Cardiff and also thank the
EPSRC Mass Spectrometry Service, University College,
Swansea for the provision of high resolution mass
spectra and INTAS and Cardiff University for financial
support.