Microbial adaptation to iron: a possible role of phosphatidylethanolamine in iron mineral deposition

Abstract

Pseudomonas fluorescens multiplied in a minimal mineral medium supplemented with iron(III) (5 mm) complexed to citrate, the sole source of carbon, with no apparent diminution in cellular mass. Atomic absorption studies of different cellular fractions and supernatant at various growth intervals revealed that the trivalent metal was initially internalized. At approximately 41 h of incubation, the soluble cellular extract contained 9.5% of the iron originally found in the growth medium. However, as bacterial multiplication progressed, most of the metal was deposited as an extracellular insoluble gelatinous residue. Phosphatidylethanolamine appeared to be an important organic constituent of this precipitate. X-ray fluorescence and diffraction studies revealed that iron(III) was deposited as amorphous hydrated oxide. Scanning electron microscopy and energy dispersive X-ray microanalysis of the pellet aided in the identification of irregular shaped bodies rich in iron and oxygen that were associated with carbon-containing elongated structures. Examination of the bacterial cells by a transmission electron microscope equipped with an electron energy loss spectrometer indicated the deposition of iron within the cells.