Summary 241
I. INTRODUCTION: CAESIUM IN THE ENVIRONMENT 242
II. UPTAKE OF CAESIUM BY PLANT ROOTS 243
1. Evidence for multiple mechanisms of Cs+uptake by plant roots 243
2. Caesium uptake is affected by the presence of other cations 244
3. Caesium inhibits the uptake of other cations 244
III. MOLECULAR MECHANISMS CATALYSING CAESIUM UPTAKE 245
1. ‘High-affinity’ transport mechanisms 245
2. Inward-rectifying potassium (KIR) channels 245
3. Outward-rectifying potassium (KOR) channels 248
4. Voltage-insensitive cation (VIC) channels 249
5. Ca2+-permeable channels 249
IV. MODELLING CAESIUM INFLUX TO ROOT CELLS 249
1. Predicted Cs+influx through high-affinity mechanisms 250
2. Predicted Cs+influx through cation channels 250
3. Predicted dependence of Cs+influx on [Cs+]ext 252
V. PERSPECTIVE 253
Acknowledgements 254
References 254
Caesium (Cs) is a Group I alkali metal with chemical properties similar to potassium (K). It is present in solution
as the monovalent cation Cs+. Concentrations of the stable caesium isotope 133Cs in soils occur up to 25 μg g−1
dry soil. This corresponds to low micromolar Cs+ concentrations in soil solutions. There is no known role for Cs
in plant nutrition, but excessive Cs can be toxic to plants. Studies of the mechanism of Cs+ uptake are
important for understanding the implications arising from releases of radioisotopes of Cs, which are produced in
nuclear reactors and thermonuclear explosions. Two radioisotopes of Cs (134Cs and 137Cs) are of environmental
concern owing to their relatively long half-lives, emissions of β and γ radiation during decay and rapid
incorporation into biological systems. The soil concentrations of these radioisotopes are six orders of magnitude
lower than those of 133Cs. Early physiological studies demonstrated that K+ and Cs+ competed for influx to excised
roots, suggesting that the influx of these cations to root cells is mediated by the same molecular mechanism(s). The
molecular identity and/or electrophysiological signature of many K+ transporters expressed in the plasma
membrane of root cells have been described. The inward-rectifying K+ (KIR), outward-rectifying K+ (KOR) and
voltage-insensitive cation (VIC) channels are all permeable to Cs+ and, by analogy with their bacterial
counterparts, it is likely that ‘high-affinity’ K+/H+ symporters (tentatively ascribed here to KUP genes) also
transport Cs+. By modelling cation fluxes through these transporters into a stereotypical root cell, it can be
predicted that VIC channels mediate most (30–90%) of the Cs+ influx under physiological conditions and that the
KUP transporters mediate the bulk of the remainder. Cation influx through KIR channels is likely to be blocked
by extracellular Cs+ under typical ionic conditions in the soil. Further simulations suggest that the combined Cs+
influxes through VIC channels and KUP transporters can produce the characteristic ‘dual isotherm’ relationship
between Cs+ influx to excised roots and external Cs+ concentrations below 200 μM. Thus, molecular targets for
modulating Cs+ influx to root cells have been identified. This information can be used to direct future genetic
modification of plants, allowing them to accumulate more, or less, Cs and thereby to remediate contaminated sites.