Abstract

The biosynthetic origins of amphidinolides G ( 1) and H ( 2) were investigated on the basis of 2D NMR data of 13C-enriched samples obtained by feeding experiments with [1- 13C], [2- 13C], and [1,2- 13C 2] sodium acetates in cultures of a marine dinoflagellate Amphidinium sp. These incorporation patterns suggested that 1 and 2 were generated from three unusual C 2 units derived only from C-2 of acetates in addition to three successive polyketide chains. Furthermore, it is noted that six oxygenated carbons of C-1, C-18, C-20, C-21, C-22, and C-26 in 1 and 2 were not derived from the C-1 carbonyl but from the C-2 methyl of acetates.

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