New Anthracene Derivatives from Coussarea
J ournal of Natural Products, 2003, Vol. 66, No. 7 907
derivatives by contact with methanol.9-11 In the present
investigation, compounds 5 and 6 were not exposed to
MeOH; therefore, we consider the two anthraquinones as
naturally occurring metabolites of C. macrophylla. An-
thracene derivatives 1-4 belong to a rare class of natural
products; as far as we know, oruwal and oruwalol (5- or
8-hydroxyoruwal) are the only related compounds isolated
so far from the plant kingdom and occur in Morinda lucida
Benth., another member of the Rubiaceae.14 The oxidation
pattern of the two groups of anthraquinols is, however,
significantly different; compounds 1-4 exhibit two OMe
substituents at C-1 and C-4 of the anthracene nucleus,
whereas these positions are unsubstituted in oruwal
derivatives. It has been suggested that the isolation of
anthracene derivatives such as oruwal is of biogenetic
interest, since it may indicate the operation of the shikimic
acid-mevalonate pathway15 in the biosynthesis of co-
occurring anthraquinones.14 The isolation of the six com-
pounds 1-6 from C. macrophylla strongly corroborates this
hypothesis and indicates that oxidation of the ring A of
anthracene derivatives may occur at a later step of the
biosynthesis.
Compounds 1, 2, and 5 were tested in standard filter
paper disk assays16 against Staphylococcus aureus and
Escherichia coli; only aldehyde 1 showed an inhibition zone
against S. aureus (inhibition diameter ) 12 mm for 19 µg/
disk). In addition, compounds 1 and 5 were inactive (LC50
> 280 ppm) in the brine shrimp (Artemia salina) lethality
assay.17 By contrast, the triterpene 3-epi-pomolic acid has
been shown by Xu et al. to exhibit a significant anti-HIV-1
protease activity.18 Compounds 3, 4, and 6 were not
obtained in sufficient quantity for testing.
in vacuo to give 9.5 and 2.2 g of oily materials, extracts A and
B, respectively.
Extract A was partitioned between MeCN and hexane to
give 4.5 g of the MeCN extract (A1) and 3.7 g of the hexane
extract (A2) after evaporation in vacuo. A quantity (1.1 g) of
insoluble material (A3) was also recovered. A sample of A1 (4
g) was chromatographed on a silica gel (250 g) column, eluted
with a hexane-EtOAc mixture (gradient of increasing polarity
from 70:30 to 100% EtOAc) followed by EtOAc-MeOH, 4:1.
The eluted fractions (15-20 mL each) were evaluated by TLC
to give nine main fractions, CMA1-1 to CMA1-9.
Chromatography of fraction CMA1-2 (50 mg) on a silica gel
column (3.5 g, hexane-EtOAc, 93:7) yielded 15 mg of com-
pound 1. Chromatography of fraction CMA1-3 (110 mg) on a
silica gel column (10 g, hexane-EtOAc, 95:5) gave 10 major
subfractions, CMA1-3-1 to CMA1-3-10. CMA1-3-5 corresponded
to compound 3, while yellow fine crystals of anthraquinone 5
(4 mg) slowly separated from an EtOAc-hexane solution of
CMA1-3-3 kept at -20 °C. Chromatography of fraction CMA1-4
(216 mg) on two consecutive silica gel columns (15 and 7 g,
respectively), each eluted with hexane-EtOAc mixtures (gra-
dient of increasing polarity from 85:15 to 0:100), afforded 3-epi-
pomolic acid (16.4 mg). Chromatography of fraction CMA1-5
(670 mg) on a silica gel column (50 g, hexane-EtOAc, gradient
of increasing polarity from 40% to 100% EtOAc) yielded 15
mg of compound 2. Chromatography of fraction CMA1-9 (1.18
g) on a silica gel column (70 g, hexane-EtOAc + 1% AcOH,
gradient of increasing EtOAc from 50% to 100%) yielded 12
major subfractions. Separation of fraction CMA1-5-9 (6 mg) on
a
RP-18 column (MeOH-H2O, 4:1) afforded scopoletin
(1.8 mg).
Extract B was dissolved in Et2O (200 mL) and extracted
with four portions (50 mL each) of saturated aqueous Na2CO3.
The basic layers were collected, acidified to pH 2 with 20%
aqueous H2SO4, and extracted with three portions (50 mL
each) of EtOAc. The organic layers were collected, washed with
brine, and dried with anhydrous Na2SO4. Removal of solvent
in vacuo afforded a sticky residue (165 mg), which was
chromatographed on a silica gel (15 g) column. Elution with a
hexane-EtOAc mixture (gradient of increasing polarity from
50:10 to 0:100), followed by an EtOAc-MeOH mixture (gradi-
ent of increasing polarity from 90:10 to 85:15), yielded five
major fractions, CMB-1 to CMB-5. The first one (4.3 mg)
corresponded to anthraquinone 6, while fraction CMB-4 (44.2
mg) was further separated on a silica gel (12 g) column. Elution
with CH2Cl2-EtOAc, 2:1, yielded five subfractions, CMB-4-1
to CMB-4-5. Chromatography of CMB-4-4 (2.8 mg) on a
RP-18 column (eluent: MeCN-H2O, 1:1) finally afforded
compound 4 (0.8 mg).
1,4,10-Tr im eth oxya n th r a cen e-2-ca r ba ld eh yd e (1): pale
yellow crystals (CH2Cl2-hexane); mp 145 °C; UV (EtOH) λmax
(log ꢀ) 243 (4.51), 266 (4.75), 299 (4.44), 360 (3.62), 379 (3.76),
411 (3.75), 433 (3.78) nm; IR (KBr) νmax 1675 (CdO), 1612,
1458, 1400, 1357, 1212, 1143, 1067, 976 cm-1; 1H and 13C NMR
data, see Tables 1 and 2, respectively; EIMS m/z 296 (M+, 100),
281 (72), 253 (24), 238 (20), 221 (6), 209 (15); HREIMS [M+]
m/z 296.1046 (calcd for C18H16O4, 296.1049).
Exp er im en ta l Section
Gen er a l Exp er im en ta l P r oced u r es. Melting points were
determined on a Fisher-J ohns hot-stage apparatus and are
uncorrected. UV (in 95% EtOH) and IR (neat or in mini KBr
disks) spectra were recorded on a Kontron Uvikon 941 and
an FT-IR Perkin-Elmer Paragon 1000 PC spectrometer, re-
spectively. 1H and 13C NMR spectra (CDCl3) were determined
on a Bruker CXP 300 spectrometer at 300 MHz (1H) and 75.47
MHz (13C), respectively. 1H and 13C chemical shifts (δ, ppm)
are relative to residual CHCl3 signals [δH 7.26, δC (central line
of t) 77.1, respectively); the abbreviations s ) singlet, d )
doublet, t ) triplet, q ) quartet, m ) multiplet, and br ) broad
are used throughout; coupling constants (J ) are reported in
Hz. The spectra were interpreted by the aid of the standard
FGCOSY, FGHMBC, and FGHMQC techniques. EIMS and
HREIMS were recorded using a Finnigan MAT 8222 spec-
trometer, with ionization being induced by electron impact at
70 eV. Thin-layer chromatography was performed on silica gel
60 F254 Al sheets (Merck) and RP-18 HPTLC F254 glass-backed
plates (Merck). Compounds were visualized under UV light
(254 and 366 nm) and by spraying with 0.5% vanillin solution
in H2SO4-EtOH (4:1) followed by heating. Flash column
chromatography was performed with Merck Kieselgel 60 (40-
63 µm) and Merck LiChroprep RP-18 (25-40 µm).
P la n t Ma ter ia l. A sample of the bark of C. macrophylla
was collected and identified by one of the authors (X.C.) in
May 1998 in a tropical damp forest at an altitude of 250 m
near the village Santa Ana, in the Provincia de Sucumbios,
district Cascales, Ecuador. The material was dried, ground,
and kept in the dark at room temperature. A voucher speci-
men, registered as Efrain Freire no. 2242, has been deposited
in the Nacional Herbarium of Quito, Ecuador.
Extr a ction a n d Isola tion . The plant material, 750 g of
bark, was extracted with EtOAc (2 L) at room temperature
three times with occasional stirring and filtered. The macerate
was then extracted three times with 96% EtOH (2 L each) for
24 h each time. The extracts were combined and evaporated
(1,4,10-Tr im eth oxya n th r a cen -2-yl)-m eth a n ol (2): pale
yellow crystals (CH2Cl2-hexane); mp 116 °C; UV (EtOH) λmax
(log ꢀ) 244 (4.50), 260 (4.62), 354sh (3.50), 370 (3.72), 384 (3.60),
402sh (3.53) nm; IR (KBr) νmax 3392 (OH), 2916 (C-H), 1621,
1454, 1348, 1137, 1036 cm-1); 1H and 13C NMR data, see Tables
1 and 2, respectively; EIMS m/z 298 (M+, 100), 283 (33), 268
(40), 255 (35), 239 (28), 224 (26), 211 (20); HREIMS [M+] m/z
298.1206 (calcd for C18H18O4, 298.1205).
The same compound was obtained by reduction of aldehyde
1 with NaBH4 according to a standard procedure.19
1,4,8,10-Te t r a m e t h oxya n t h r a ce n e -2-ca r b a ld e h yd e
(3): pale yellow sticky solid; UV (EtOH) λmax (log ꢀ) 238 (4.62),
268 (4.81), 298sh (4.50), 344 (3.76), 364 (3.91), 382 (4.06), 422sh
(4.02), 440 (4.06) nm; IR (film) νmax 2933 (C-H), 1673 (CdO),
1613, 1459, 1353, 1067 cm-1; 1H and 13C NMR data, see Tables
1 and 2, respectively; EIMS m/z 326 (M+, 100), 311 (60), 296
(13), 283 (22), 268 (28), 253 (15); HREIMS [M]+ m/z 326.1156
(calcd for C19H18O5, 326.1154).