Pd. Erskine et al., WATER AVAILABILITY - A PHYSIOLOGICAL CONSTRAINT ON NITRATE UTILIZATION IN PLANTS OF AUSTRALIAN SEMIARID MULGA WOODLANDS, Plant, cell and environment, 19(10), 1996, pp. 1149-1159
Nitrate was found to be the predominant form of available nitrogen in
mulga soils. Nitrate reductase activities on a fresh mass basis of a r
ange of plants from eastern (Queensland) mulga ecosystems 2 weeks afte
r partial relief from drought were uniformly low for both herbaceous s
pecies (165 +/- 25 pkat g(-1)) and woody perennials (77 +/- 14 pkat g(
-1)). Supply of nitrate for 24 h to cut transpiring shoots of woody sp
ecies or application of nitrate solution to the rooting zone of herbac
eous species promoted little further increase in mean shoot nitrate re
ductase activities. Most species exhibited high tissue nitrate concent
rations during water stress and soluble organic N profiles were in man
y cases dominated by the osmoprotective compounds, proline or glycine
betaine. Species with low levels of proline or glycine betaine showed
high foliar concentrations of other compatible osmotica such as polyol
s or sugars. Effects of relieving water stress on nitrate reductase ac
tivity, proline, glycine betaine and nitrate levels were followed over
3 d of irrigation. Available soil nitrate rose 10-fold immediately an
d, following rapid restoration of leaf water status of the eight study
species, a 4-fold increase occurred in mean nitrate reductase activit
y together with progressive decreases in mean tissue concentrations of
nitrate, proline and glycine betaine over the 3 d period. Similar cha
nges in soil nitrate, nitrate reductase activity, proline and tissue n
itrate were observed in the same ecosystem following a natural rainfal
l event and in western (S.W. Australia) mulga following irrigation. It
is concluded that, although nitrate nitrogen is present at high conce
ntrations and is the predominant inorganic nitrogen source in soils of
the mulga biogeographic region, its assimilation by perennial and eph
emeral vegetation is limited primarily by water availability. A scheme
is presented depicting interrelated physiological and biochemical eve
nts in typical mulga species following a rain event and subsequent dry
ing out of the habitat.