1678
J . Nat. Prod. 1999, 62, 1678-1681
Ocea n a p isid e, a n An tifu n ga l Bis-r,ω-a m in o Alcoh ol Glycosid e fr om th e Ma r in e
Sp on ge Ocea n a pia ph illipen sis
Gillian M. Nicholas, Tamilyn W. Hong, Tadeusz F. Molinski,* Melissa L. Lerch, Mark T. Cancilla, and
Carlito B. Lebrilla
Department of Chemistry, One Shields Avenue, University of California, Davis, California 95616
Received April 23, 1999
The structure of oceanapiside, an antifungal R,ω-bis-aminohydroxylipid glycoside from the temperate
marine sponge Oceanapia sp., was elucidated by a combination of 2D NMR, chemical degradation/
correlation, and MALDI MS-MS spectrometry. Oceanapiside exhibits antifungal activity against Candida
glabrata at 10 µg/mL (MIC).
The structures of sphingolipids from marine inverte-
brates share features of sphingolipids derived from plants
and animals. In higher animals, the base is sphingosine
(erythro-D-E-2-amino-4-octadecene-1,3-diol), while sphin-
ganine (D-2-amino-octadecan-1,3-diol) is most common in
plant sphingolipids.1 A significant departure from this
motif is found in the structures of dimeric amino alcohol
bases from certain calcareous sponges. Leucettamols A (1)
and B, from Leucetta sp.;2 compound BRS1, from an
unidentified sponge;3 rhizochalin (2), from Rhizochalina
incrustata,4 and related compounds; coriacenins, from the
Mediterranean Clathrina coriacea;5 and rhapsamine, from
the Antarctic Leucetta leptorhapsis,6 are all aminolipids
composed of symmetrical, or almost symmetrical, very long
hydrocarbon chains (C28-C30) functionalized at both ter-
minii as vicinal amino alcohols. We report here a new
glycosidic amino alcohol lipid, oceanapiside (3) from a
temperate-water, non-calcareous sponge, Oceanapia phil-
lipensis Dendy, 1895 (Haplosclerida, Phloeodictyidae) col-
lected in Southern Australia. Oceanapiside is a naturally
occurring “bolaamphiphile”sa term coined7 to describe
amphiphilic lipids with polar functionality at both termini
whose structures suggest a resemblance to the bola, a
weapon fashioned from two leather balls tethered to the
ends of a string. Oceanapiside exhibits significant antifun-
gal activity against the pathogenic, Fluconazole-resistant
yeast, Candida glabrata.
The n-BuOH-soluble portion of a MeOH extract of
Oceanapia phillipensis was fractionated by reversed-phase
(C18) chromatography to afford a highly polar amino lipid,
(-)-oceanapiside (3), C34H68N2O9 (HRFABMS (MH+
649.5003, ∆ mmu ) -1.3), which gave a positive ninhydrin
test. Oceanapiside was insoluble in CHCl3 and EtOAc, but
soluble in MeOH and water. The UV spectrum of 3 showed
no absorbance above λ 210 nm. Interestingly, the base peak
in the ESIMS of 3 was the doubly charged ion at m/z 325
(z ) 2) that corresponds to [M + H2]2+. Taken together with
the positive ninhydrin reaction, this suggested a readily
protonated diamine. The presence of a keto group was
indicated by FT-IR (ν 1712 cm-1, CdO stretch) and 13C
NMR spectra (δ 214.3, s). Although it was later confirmed
that 3 contains two free primary amines, treatment of 3
with t-BOC carbonate (THF-MeOH-Et3N) gave only a
mono-t-BOC derivative 4 (C39H75N2O11, ESIMS, m/z 748,
M+), presumably because the second NH2 group was
hindered by the glycosyl group (see below). Oceanapiside
gave no precipitate with AgNO3 (absence of Cl-), so we
formulated 3 as the free base, but cannot exclude a salt
with other anions.
Interpretation of the 1H and 13C NMR spectra of 3 in
CD3OD (Table 1) revealed one acetal group (δ 4.30, d, J )
7.6 Hz; δC 104.5 d), seven additional methines attached to
oxygen (δ 80.1, 78.1, 77.7, 74.8, 73.1, 71.6), and a lipid chain
(CH2 envelope, δ 1.28, br s). Six of the 13C signals were
consistent with the presence of a sugar, which was identi-
fied as D-glucose as follows. Methanolysis of 3 (2M HCl in
MeOH, 80 °C, 16 h) gave two fractions, separable by Si gel
chromatography. The first fraction was a mixture of
anomeric methyl glycosides (C7H14O6, m/z 180, MH+ - Me),
identified as an R:â mixture of 1-O-methyl-D-glucopyrano-
sides by high-performance TLC and comparison with an
authentic sample (obtained by methylation of D-glucose,
HCl, MeOH, 80 °C, 2 h). Glycoside 3 has the â-configuration
at the anomeric carbon as shown by the coupling constant
for the anomeric proton signal (δ 4.30, d, J ) 7.6 Hz).8 The
second fraction eluted from the column with NH3-MeOH-
CHCl3 and was identified as the novel polar aglycon 5
(FABMS; m/z 487.5, MH+).
A downfield 13C signal (δ 214.3, s) for a keto group and
the glycopyranosyl ring accounted for all of the degrees of
unsaturation required by the formula of 3. The remainder
of the formula was attributed to a linear aminolipid chain.
Interpretation of COSY, gHMQC, and gHMBC data re-
vealed the two terminal sequences of oceanapiside algycon
as -CH(OH)CH(NH2)CH3 and -CH(O-)CH(NH2)CH2OH-
and enabled assignment of the corresponding two sets of
13C NMR signals: CH2-O (δ 58.9, t, C-1), CH-N (57.2, d,
C-2), CH-O (80.1, d, C-3) and CH3 (16.0, q, C-28), CH-N
(53.5, d, C-27), and CH-O groups (73.1, d, C-26). The two
CH2 groups (δ 2.43, t, J ) 6.5 Hz, 4H; δC 43.4, t) R to the
ketone carbonyl were clearly resolved and readily assigned
by comparison with 3-heptanone (δ 2.37, t, J ) 7 Hz; δC
44.9, t).9 The methyl terminus (δΗ ∼1.3, d, δC 16.0, q) was
obscured in the 1H NMR spectrum of 3 by the CH2
envelope, but inferred from observation of the expected
COSY and HMQC cross-peaks together with DEPT data,
and conveniently revealed in the 1H NMR spectrum (CDCl3,
Table 1) of the octaacetyl derivative 6 (δ 1.05, d, J ) 6.7
Hz) or the t-BOC derivative 4 (CDCl3, δ 1.14, d, J ) 6.5
Hz).
Oceanapiside (3) gave an octaacetyl derivative, 6 (Ac2O,
pyridine, 16 h, 25 °C). The COSY spectrum (500 MHz) of 6
1
revealed downfield shifts (∆δ ∼0.5-1 ppm) of carbinol H
* To whom correspondence should be addressed. Tel: (530) 752-6358.
Fax: (530) 752-8995. E-mail: tfmolinski@ucdavis.edu.
signals due to acetylation of the OH groups, including both
10.1021/np990190v CCC: $18.00
© 1999 American Chemical Society and American Society of Pharmacognosy
Published on Web 10/23/1999