Issue 10, 1990

Biosynthesis of mangostin. Part 1. The origin of the xanthone skeleton

Abstract

The biosynthesis of mangostin (3) has been studied by wick-feeding of 14C- and 13C-labelled precursors to young Garcinia mangostana plants. Radioactive mangostin was isolated as 3,6-di-O-methylmangostin (4), which was subsequently degraded to phloroglucinol and isovaleric acid to aid location of the label. Although results from feeding of 14C-labelled precursors suggested two alternative malonate–shikimate routes to compound (3), experiments with 13C-labelled compounds clearly demonstrated that mangostin (3) originates from a C6C1 unit (benzoate) and three C2 units (malonates). [1,2,3-13C3]malonic acid was incorporated solely into ring A of compound (4) and two different arrangements of C2 units in compounds (17a and b) were evident, indicating that mangostin (3) derives via ring closure of a symmetrical intermediate (18).

Article information

Article type
Paper

J. Chem. Soc., Perkin Trans. 1, 1990, 2671-2676

Biosynthesis of mangostin. Part 1. The origin of the xanthone skeleton

G. J. Bennett, H. Lee and N. P. Das, J. Chem. Soc., Perkin Trans. 1, 1990, 2671 DOI: 10.1039/P19900002671

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