Abstract
The use of chlorate as an analogue for NO3 during nitrate uptake into Chara corallina cells has been investigated. NO3 inhibits 36C1O3 influx into Chara over the concentration range 0–1000 mmol m−3. Lineweaver-Burke plots of the data are characteristic of competitive inhibition by NO−3 in the low concentration range (0–300 mmol m−3 ClO3) and apparent KINO3 is 140 mmol m−3 which is of a similar order of magnitude as apparent KmCIO3- 180 mmol m−3. At higher substrate concentrations the inhibition by NO3 was not characteristic of competitive or uncompetitive inhibition. 36C1O3/NO3 influx was dependent on K+ and Ca2+ in the external medium and inhibited by FCCP. NO3 pretreatment or N starvation increased subsequent 36C1O3/NO3 influx into Chara. A comparison between rates of net NO3 uptake and 36C1O3/NO3 influx supported the previous hypothesis that NO3 efflux is an important component in the determination of overall uptake rates.