Phosphatidylinositol, a phospholipid of ice-nucleating bacteria

Abstract

The nature of the phospholipids of the various bacteria that have ice nucleation activity in supercooled water has been determined. The seven bacteria studied included Pseudomonas syringae, Erwinia herbicola, three Escherichia coli K-12 strains that are phenotypically Ice+ because they contain plasmids with different amounts of either P. syringae or E. herbicola cloned DNA, and two E. coli K-12 strains without cloned ice gene DNA. All five Ice+ bacterial strains contained small amounts (0.1 to 1.0% of the total phospholipids) of phosphatidylinositol (PI), a phospholipid not previously detected in E. coli, Pseudomonas, or Erwinia species. The Ice- E. coli strains also contained trace level of PI that amounted to 2 to 30% of the level found in the Ice+ E. coli strains. Extracts of Ice+ strains contained low but measurable activities of PI synthase, while the activities in Ice- strains amounted to only 8 to 12% or less of that found in extracts of Ice+ bacteria. The functioning of the ice gene apparently increased both the PI synthase activity and the PI content of Ice+ strains from low endogenous levels. The relative ice nucleation activity at -4 degrees C or above (class A nucleation activity) of all Ice+ strains was found to be proportional to their PI content. The addition of myo-inositol (5 x 10(-4) M) to synthetic culture media increased the class A nucleation activity of both Ice+ E. coli strains and P. syringae up to sevenfold but had no stimulating effect on ice nucleation at lower temperatures (class B and class C nucleation activities). If these cells after fusion with PI vesicles were incubated with an energy source, the class A nucleation activity increased 70-fold over that present before fusion. These results indicate that PI plays an important role in ice nucleation at warm temperatures and is a likely precursor or component of the class A structure.