Md. Cramer et Sh. Lips, ENRICHED RHIZOSPHERE CO2 CONCENTRATIONS CAN AMELIORATE THE INFLUENCE OF SALINITY ON HYDROPONICALLY GROWN TOMATO PLANTS, Physiologia Plantarum, 94(3), 1995, pp. 425-432
Our previous work indicated that salinity caused a shift in the predom
inant site of nitrate reduction and assimilation from the shoot to the
root in tomato plants. In the present work we tested whether an enhan
ced supply of dissolved inorganic carbon (DIC, CO2 + HCO3-) to the roo
t solution could increase anaplerotic provision of carbon compounds fo
r the increased nitrogen assimilation in the root of salinity-stressed
Lycopersicon esculentum (L.) Mill. cv. F144. The seedlings were grown
in hydroponic culture with 0 or 100 mM NaCl and aeration of the root
solution with either ambient or CO2-enriched air (5 000 mu mol mol(-1)
). The salinity-treated plants accumulated more dry weight and higher
total N when the roots were supplied with CO2-enriched aeration than w
hen aerated with ambient air. Plants grown with salinity and enriched
DIC also had higher rates of NO3- uptake and translocated more NO3- an
d reduced N in the xylem sap than did equivalent plants grown with amb
ient DIC. Incorporation of DIC was measured by supplying a 1-h pulse o
f (HCO3-)-C-14 to the roots followed by extraction with 80% ethanol. E
nriched DIC increased root incorporation of DIC 10-fold in both salini
zed and non-salinized plants. In salinity-stressed plants, the product
s of dissolved inorganic C-14 were preferentially diverted into amino
acid synthesis to a greater extent than in non-salinized plants in whi
ch label was accumulated in organic acids. It was concluded that enric
hed DIC can increase the supply of N and anaplerotic carbon for amino
acid synthesis in roots of salinized plants. Thus enriched DIC could r
elieve the limitation of carbon supply for ammonium assimilation and t
hus ameliorate the influence of salinity on NO3- uptake and assimilati
on as well as on plant growth.