Abstract

The methanolyzed lipids of the extreme halophile, Halobacterium cutirubrum, were separated into glycerol diether and glycerol monoether fractions. The diether was shown by synthesis to be 2,3-di-O-(3'R,7'R,11'R,15'-tetramethylhexadecyl)-sn-glycerol. The monoether fraction was separated by thin-layer chromatography on boric acid-impregnated silicic acid into about equal amounts of alpha- and -isomers. The alpha-isomer was found to be identical with the synthetic 3-O-(3'R,7'R,11'R,15'-tetramethylhexadecyl)-sn-glycerol, and the -isomer was identical with the synthetic 2-O-(3'R,7'R,11'R,15'-tetramethylhexadecyl) glycerol.

Highlights

  • The methanolyzed lipids of the extreme halophile, Halobacterium cutirubrum, were separated into glycerol diether and glycerol monoether fractions

  • The acetone-insoluble lipids (4.9 g) were methanolyzed (1) in 100 ml of 2.5% anhydrous methanolic hydrogen chloride under reflux for 4-5 hr; the mixture was diluted with 10 ml of water, and the crude glycerol diether, together with small amounts of glycerol monoethers (3) was extracted with several 50-ml portions of petroleum ether

  • The chloro compound was identified by comparison of its R, values on TLC and relative retentions on Gas--liquid chromatography (GLC) with those of the authentic synthetic substance; it was probably formed from the diether during the refluxing with niethanolic HCl

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Summary

Introduction

The methanolyzed lipids of the extreme halophile, Halobacterium cutirubrum, were separated into glycerol diether and glycerol monoether fractions. The diether was shown by synthesis to be 2,3-di-O-(3‘R,7’R,ll’R,15’-tetramethylhexadecy1)-sn-glycerol. The monoether fraction was separated by thin-layer chromatography on boric acid-impregnated silicic acid into about equal amounts of a- and j3isomers. The a-isomer was found to be identical with the synthetic 3-0-(3’R,7’R,ll ’R,15’-tetramethylhexadecy1)-snglycerol, and the j3-isomer was identical with the synthetic 2-0-(3’R,7’R,11’R,15’-tetramethylhexadecyl) glycerol

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