M. Bregante et al., EFFECTS OF MONOVALENT AND MULTIVALENT CATIONS ON THE INWARD-RECTIFYING POTASSIUM CHANNEL IN ISOLATED PROTOPLASTS FROM MAIZE ROOTS, European biophysics journal, 26(5), 1997, pp. 381-391
Transport properties mediated by ionic channels were studied by the pa
tch-clamp technique in protoplasts from cortical parenchyma cells of m
aize roots (CPMR). While outward currents could be seen only occasiona
lly, macroscopic voltage-and time-dependent potassium-selective inward
currents (I-Kin(+)) were frequently observed in the whole-cell config
uration. These currents increased continuously as a function of K+ con
centration (in the range 3-200 mM) and the slow-saturating macroscopic
chord-conductance was fitted by a Michaelis-Menten function with K-m
= 195 +/- 39 mM. Other ions, like sodium and lithium, did not permeate
at all through the maize root inward-channel, or like ammonium (P-NH4
(+)/ PK+ = 0.16 divided by 0.25) and rubidium (PRb+/PK+ approximate to
0.10) displayed a very low permeability ratio. Up to 5 mM Rb+ did not
induce any inhibition of the K+ inward current, whereas submillimolar
concentrations of Cs+ were sufficient to block, in a voltage-dependen
t manner, the inward currents. A decrease of the external potassium co
ncentration favoured Cs+ inhibition (K-m = 89 +/- 6 mu M and 26 +/- 2
mu M in 200 and 100 mM KCl, respectively). The potassium inward-curren
ts were reversibly and consistently inhibited by submillimolar externa
l concentrations of the metal ions Ni2+, Zn2+ and Co2+, while 1 mM La3
+ only slightly decreased (approximate to 10%) both the single channel
conductance (9.2 +/- 1.2 pS in 100 mM potassium) and the macroscopic
current. In contrast to the case with Cs+, inhibition induced by other
metal ions did not show any voltage dependence. These results suggest
that, as with animal potassium channels, the inward channel of maize-
root cortical cells has a narrow pore of permeation and metal ions dec
rease the K+ current, possibly by acting on binding sites located outs
ide the pore.