The inorganic ion content of native aquatic bacteria.
In this study we have quantified the ionic content and volume of native aquatic, and two cultured bacteria, by X-ray microanalysis (XRMA) in the transmission electron microscope (TEM). The cellular concentrations of magnesium (means of 630 and 710 mM) were more than an order of a magnitude higher than the outside concentrations. The internal concentrations of sodium were on average 50-180 mM, and the [K+]/[Na+] ratios were in the range of 0.1-0.5; lowest for apparently nonactive bacteria. Magnesium and chloride probably act as the major components of cell turgor, since no other inorganic ions were present in comparable amounts. Our carbon and nitrogen measurements indicated that organic solutes are not likely to be present at significant concentrations. The estimated charge of inorganic ions (Na, Mg, P, Cl, K, and Ca) gave a positive net internal charge for most cells. However, in cultures of Vibrio natriegens, the high internal chloride concentration made the net inorganic charge negative in these cells. Our results suggest that growing marine bacterioplankton have an internal environment in which magnesium is the dominating cation. These results suggest that actively growing marine bacteria are physiologically adapted to high internal concentrations of both magnesium and chloride.
Department of Microbiology, University of Bergen, Norway. kjell.fagerbakke@im.uib.no
K M
KM
Fagerbakke
S
S
Norland
M
M
Heldal
D001419:Bacteria / Q000737:chemistry*; D004577:Electron Probe Microanalysis; D005618:Fresh Water; D006090:Gram-Negative Bacteria / Q000737:chemistry; D006217:Halobacterium / Q000737:chemistry; D007477:Ions; D008274:Magnesium / Q000032:analysis; D008854:Microscopy, Electron; D012623:Seawater; D013291:Streptococcus / Q000737:chemistry; D014871:Water Microbiology; D014882:Water-Electrolyte Balance
D007477:Ions; D008274:Magnesium