482
M. L. Jimeno et al.
columnchromatography [silicagel deactivatedwith10% H2O(w/v),
light petroleum–EtOAc (7 : 3) as eluent], yielding 60 fractions (15 ml
each). Fractions 28–37 contained isabelin (3) (320 mg, 32% yield) and
1024 ð 256 matrix with a spectral width of 5000 Hz and a
2 s recycle delay. The data were linear predicted forward to
512 points in the t1 dimension and zero-filled to 1024 points.
Inverse proton detected heteronuclear 2D spectra, gHSQC
and gHMBC, were acquired in the phase-sensitive mode.
Data were collected in a 4096 ð 128 matrix with a spec-
tral width of 8000 Hz in the proton domain and 25000 Hz
in the carbon domain. The data were linear predicted for-
ward to 256 points in the t1 dimension and zero-filled to
512 points. The gHSQC experiment was optimized for a
one-bond heteronuclear coupling constant of 145 Hz. The
gHMBC experiment was optimized for long-range coupling
constants of 8 Hz.
fractions 52–59 provided 4 (270 mg, 27% yield).
20
°
°
Isabelin (3): m.p. 168–170 C (Me2CO–pentane), [˛]D ꢀ 56.7
25
2
°
°
(CHCl3; c 0.213); literature: m.p. 169–170 C, [˛]D ꢀ57.2 (CHCl3; c
0.87). IR and UV spectra were identical to those reported previously.2
EIMS: m/z (relative intensity, %) 260 [M]C (3), 231 (4), 215 (4), 164
(17), 149 (14), 135 (24), 124 (59), 96 (100), 77 (41), 68 (77), 55 (44),
43 (78), 39 (74). For 1H and 13C NMR spectra, see Tables 2 and 3,
respectively.
6˛-Hydroxy-15-oxogermacra-1(10)E,4Z,11(13)-trien-12,8˛-olide
20
°
°
(4): m.p. 153–156 C (EtOAc–n-hexane), [˛]D ꢀ63.9 (CHCl3; c
0.668); IR, ꢃmax: 3435, 2935, 2862, 1762, 1687, 1635, 1312, 1252, 1144,
1103, 1072, 1040, 1007, 970, 934, 893, 817, 763 cmꢀ1; UV (MeOH),
ꢄmax (log ε): 223 (3.55); EIMS: m/z (relative intensity, %) 262 [M]C
(12), 244 (4), 233 (31), 215 (13), 187 (12), 159 (13), 148 (39), 137 (25),
123 (69), 105 (30), 97 (65), 91 (84), 69 (94), 68 (100), 67 (82), 53 (44), 41
(88), 39 (73). Found: C, 68.49; H, 6.98. C15H18O4 requires C, 68.68; H,
6.92%. For 1H and 13C NMR spectra, see Tables 2 and 3, respectively.
Molecular modeling
Semi-empirical calculations were performed using the
HyperChem package.8 The computations were carried out
on a Windows 2000 workstation with a Pentium III PC. The
starting structures were generated according to previous
molecular mechanics calculations and to NMR restrictions.
Final geometries were optimized using the AM1 method.
X-ray crystallography of artemisiifolin (1)
Crystals of artemisiifolin (1) suitable for x-ray diffraction
analysis were obtained by recrystallization from EtOAc. A
colourless prism of 1 (0.47 ð 0.36 ð 0.08 mm) was selected
for the data collection. Crystal data: C15 H20 O4; Mr
D
264.32 g molꢀ1; trigonal a D 11.0254(3) A, b D 11.0254(3) A,
˚
˚
Plant material
˚
°
°
°
c D 9.7614(5) A, ˛ D 90 , ˇ D 90 , ꢀ D 120 , V D
Aerial parts of Staehelina dubia L. were collected in August
2000, near Ciruelos del Pinar, Guadalajara province, Spain.
A voucher specimen (No. 479/2000) is deposited in the
Herbarium of the Department of Pharmacognosy, Faculty of
Pharmacy, Complutense University, Madrid, Spain.
1027.6(1) A , space group P31, Z D 3, Dcal D 1.2813 Mg mꢀ3
.
3
˚
Data collection: Seifert XRD 3000S diffractometer, 273.(2)
K; 1289 independent reflection intensities were collected
°
between 4.63 and 66.80 in Â, in the ω/2Â scan mode, with
˚
Cu K˛ monochromated radiation (ꢄ D 1.54180 A). No decay
was observed in two reference reflections measured every
150 min, and 1284 reflections were considered as observed
at the 2ꢅ(I) level.
Extraction and isolation of artemisiifolin (1)
Dried and powdered aerial parts of the plant (1.5 kg) were extracted
with Me2CO (3 ð 10 l) at room temperature for 1 week. Filtration
and evaporation of the solvent yielded a residue (86 g) which was
subjected to column chromatography [silica gel 1080 g, deactivated
The structure was solved by direct methods using
SHELX-9717 and difference Fourier techniques; no absorption
correction was applied (ꢆ D 0.251 mmꢀ1). The structure
was refined using full-matrix least-squares on F2 through
SHELXL-97.17 All non-H atoms were refined with anisotropic
thermal parameters. Since 1 crystallizes in a polar space
group, polar axis restraints were applied.18 The H atoms
were assigned geometrically and treated using appropriate
riding models. The refinement converged to R final indices
[I > 2ꢅ(I)] R1 D 0.036, ωR2 D 0.100 and R indices (all data)
R1 D 0.036, ωR2 D 0.100. All calculations were done with the
program SHELX-97.17 All the geometric calculations were
performed with the program PARST,19 and scattering factors,
anomalous dispersion and absorption coefficients were
taken from International Tables for X-ray Crystallography.20
Crystallographic data for the structure reported in this paper
have been deposited with the Cambridge Crystallographic
Data Centre (CCDC 193230).
°
with 10% (w/v) H2O], eluting with light petroleum (b.p. 60–70 C)
and then with a light petroleum–EtOAc gradient from 9 : 1 to 1 : 1.
The chromatographic fractions eluted with light petroleum–EtOAc
(3 : 2) furnished a crystalline residue, which was recrystallized
from EtOAc, giving pure artemisiifolin (1) (27 g, 1.8% on dry
22
°
°
plant material): m.p. 135–137 C, [˛]D C 58.9 (CHCl3; c 1.557);
25
literature:1 m.p. 131 C, [˛]D C 54.6 (MeOH). IR, UV and mass
spectra were identical with those reported previously.1 For 1H and
13C NMR spectra, see Tables 1 and 3, respectively.
°
°
Sodium borohydride reduction of 1 to give
11,13-dihydroartemisiifolin (2)
A stirred solution of 1 (330 mg) in MeOH (20 ml) was treated with
an excess of NaBH4 (200 mg) for 30 min at room temperature.
Then water (50 ml) was added and the reaction mixture was
extracted with CH2Cl2 (4 ð 25 ml). The combined extracts were
dried (Na2SO4), filtered and evaporated to dryness, giving a residue
(328 mg, 98.6% yield), which was crystallized from EtOAc: m.p.
20
1
°
°
175–177 C, [˛]D C 89.6 [CHCl3 –MeOH (1 : 1); c 0.556]; literature:
25
°
°
m.p. 183–185 C, [˛]D C 94 (MeOH). IR and UV spectra were
identical with those reported previously.1 EIMS: m/z (relative
intensity, %) 266 [M]C (1), 248 (5), 235 (14), 219 (15), 217 (17),
121 (45), 107 (67), 93 (65), 79 (100), 69 (65), 55 (36), 53 (36), 41 (64).
Found: C, 67.72; H, 8.60. C15H22O4 requires C, 67.64; H, 8.33%. For
1H and 13C NMR spectra, see Tables 2 and 3, respectively.
Acknowledgements
The authors thank the Spanish Direccio´n General de Investigacio´n
´
Cientıfica y Te´cnica (DGICYT) (grant No. BQU 2000-0868) and
´
Comisio´n Interministerial de Ciencia y Tecnologıa (CICYT) (grant
No. AGL 2001-1652) for financial support.
Pyridinium dichromate oxidation of 1: isabelin (3)
and compound 4
Pyridinium dichromate (PDC) (2.25 g) was added to a solution of
1 (1.01 g) in anhydrous THF (55 ml) under argon. The mixture was
stirred for 48 h at room temperature. Then Et2O (25 ml) was added
and the mixture was filtered through a pad of Celite. Evaporation
of the solvents gave a residue (630 mg), which was subjected to
REFERENCES
1. Porter TH, Mabry TJ, Yoshioka H, Fischer NH. Phytochemistry
1970; 9: 199.
Copyright 2004 John Wiley & Sons, Ltd.
Magn. Reson. Chem. 2004; 42: 474–483