Actinomycetes are well-known producers of an enormous variety of secondary metabolites, many of which have beneficial applications in the field of medicine and agriculture. More recently, endophytic actinomycetes residing in plants revealed the potential sources of biodiversity carrying a variety of bioactive metabolites and acting as potential biocontrol agents.1–3 Particularly, endophytic actinomycetes isolated from tropical plants have been examined to possess significant biosynthetic potential, particularly polyketide synthase and nonribosomal peptide synthetase genes.4 We have recently reported a new polyketide compound from an endophytic actinomycete isolated from a Thai medicinal plant collected at the Eastern Botanical Garden (Khao Hin Son), Chachoengsao province, Thailand.5 Here, we now report a new furanone-containing polyketide, linfuranone A (Figure 1), produced by an endophytic actinomycete isolated from a Thai medicinal plant collected at the same location. An endophytic Microbispora sp. GMKU363 was isolated from a root of Thai medicinal plant ‘Lin Ngu Hao’ (Clinacanthus siamensis Bremek.) according to the reported protocol.6 The strain was identified as a member of the genus Microbispora on the basis of 99.9% 16S ribosomal RNA gene sequence identity (1387 nucleotides; GenBank accession number GU459171) with the Microbispora mesophila JCM 3151T type strain (accession number AF002266). Strain GMKU363 was cultured on Bn-2 slant agar medium consisting of soluble starch 0.5%, glucose 0.5%, meat extract (Kyokuto Pharmaceutical Industrial Co., Ltd., Tokyo, Japan) 0.1%, yeast extract (Difco Laboratories, Detroit, MI, USA) 0.1%, NZ-case (Wako Pure Chemical Industries, Ltd., Osaka, Japan) 0.2%, NaCl 0.2%, CaCO3 0.1%, agar 1.5% and was inoculated into 500-ml K-1 flasks each containing 100ml of the V-22 seed medium (pH 7.0) consisting of soluble starch 1%, glucose 0.5%, NZ-case 0.3%, yeast extract 0.2%, triptone (Difco Laboratories) 0.5%, K2HPO4 0.1%, MgSO4 � 7H2O 0.05% and CaCO3 0.3%. The cultures were cultivated on a rotary shaker (200 r.p.m.) at 30 1C for 4 days. The seed culture (3ml) was transferred into 500-ml K-1 flasks each containing 100ml of the A-11M production medium (pH 7.0) consisting of soluble starch 2.5%, glucose 0.2%, yeast extract 0.5%, polypeptone (Wako Pure Chemical Industries, Ltd.) 0.5%, NZ-amine 0.5%, CaCO3 0.3% and Diaion HP-20 (Mitsubishi Chemical Co.) 1%. The cultures inoculated in flasks were cultured on a rotary shaker (200 r.p.m.) at 30 1C for 6 days, and the whole culture broth was extracted with 100ml of 1butanol on each flask by shaking for an additional hour. The organic layer was evaporated to give 3.0 g of crude extract from 1.5 l of culture. The crude extract (3.0 g) was subjected to silica gel column chromatography with a step gradient of CHCl3-MeOH (1:0, 20:1, 10:1, 4:1, 2:1, 1:1 and 0:1 v/v). The concentration of the fraction eluted with a 2:1 mixture of CHCl3-MeOH provided 0.23 g of dark viscous oil, which was further purified by preparative HPLC (Cosmosil AR-II, San Diego, CA, USA, 250� 10mm2) using 30%MeCN in distilled water at 4mlmin�1 to give linfuranone A (2.0mg, tR1⁄4 12.1min). Linfuranone A (Figure 1) was obtained as an optically active ([a]D �9.9 (c 0.16, MeOH)), colorless and amorphous compound that gave an [MþNa]þ peak at m/z 417.2257 in the high resolution electrospray ionization time-of-flight mass spectrometry appropriate for a molecular formula of C22H34O6, (calculated for C22H34O6Na, 417.2248), which was consistent with the 1H and 13C NMR data (Table 1). The IR spectrum of linfuranone A showed absorption bands for hydroxyl (3333 cm�1) and carbonyl (1691 cm�1) functionalities. The UV spectrum showed absorption maxima at 282 (e 23600) and 232 (e 75300) in MeOH. 13C NMR and HMQC spectral data confirmed the presence of 22 carbons, which were assigned to two oxygenated-quaternary sp2 carbons, seven olefinic carbons (five are proton-bearing), one quaternary sp3 carbon, four sp3 methines (three are oxygen-bearing), three sp3 methylenes and five methyl carbons. Analysis of the COSY spectrum led to the identification of four proton-bearing fragments, H-17–H-19, H-15/H-14/H-21, H-12/H-13 and H-6–H-11 (Figure 1). HMBC correlations were detected from the