St. Albelo et Ce. Domenech, CARBONS FROM CHOLINE PRESENT IN THE PHOSPHOLIPIDS OF PSEUDOMONAS-AERUGINOSA, FEMS microbiology letters, 156(2), 1997, pp. 271-274
The phospholipid composition of Pseudomonas aeruginosa grown in a mine
ral medium with choline as the carbon source was: phosphatidylethanola
mine, 71.6+/-1.4%; phosphatidylglycerol, 11.8+/-0.4%; diphosphatidylgl
ycerol, 0.8+/-0.4%; phosphatidic acid, 2.4 +/- 0.6%; lysophosphatidyle
thanolamine, 1.6 +/- 0.3%; phosphatidylcholine 7.9 +/- 0.3%; lysophosp
hatidylcholine, 3.9 +/- 0.7%. The molar ratio between the acidic and t
he neutral phospholipids was 0.18. Radiolabeling experiments with [met
hyl-C-14]choline or [1,2-C-14]choline carried out in cell suspension f
rom bacteria that were grown in the presence of choline as the sole ca
rbon source demonstrated that the carbons of the N-methyl groups of ch
oline contributed to the synthesis of fatty acids while the carbons co
mprising the backbone of choline were used for the synthesis of glycer
ol.