Jd. Trent et al., ECOPHYSIOLOGY OF THE TEMPERATE DESERT HALOPHYTES - ALLENROLFEA-OCCIDENTALIS AND SARCOBATUS-VERMICULATUS, The Great Basin naturalist, 57(1), 1997, pp. 57-65
Numerous basins of the intermountain area often have extensive playa s
urfaces that are nearly devoid of vegetation. Margins of these playas
support sparse communities dominated by the chenopod shrubs Allenrolfe
a occidentalis (iodine bush) and Sarcobatus vermiculatus (black grease
wood). These plants establish and persist in an environment where halo
morphic soils induce extreme osmotic stress and atmospheric precipitat
ion is very low and erratic and occurs largely during the winter when
temperatures are too low for growth. We measured net CO2 assimilation
rates, leaf conductances, transpiration rates, water-use efficiencies,
and stem xylem potentials for these two C3 species. Data were collect
ed in above-average (1991) and below-average (1992) precipitation year
s. Net CO2 assimilation rates for Allenrolfea were statistically simil
ar in 1991 and 1992 but in general declined for Sarcobatus in 1992. Fo
r both species, leaf conductances and leaf transpiration rates decline
d significantly from 1991 to 1992, with the decline significantly grea
ter for Sarcobatus. Water-use efficiencies doubled from 1991 to 1992 f
or both plant species. Predawn xylem water potentials were -2.2 and 3.
3 MPa for Allenrolfea and -1.8 and -2.6 MPa for Sarcobatus beginning i
n May 1991 and 1992, respectively, and dropped to 3.8 and -4.2 MPa for
Allenrolfea and -1.8 and -2.8 MPa for Sarcobatus by September 1991 an
d 1992, respectively. Afternoon xylem water potentials were 3.1 and -2
.0 MPa for Allenrolfea and -2.6 and -2.2 MPa for Sarcobatus beginning
in May 1991 and 1992, respectively. Xylem water potentials dropped to
-5.0 MPa for Allenrolfea and -3.4 MPa for Sarcobatus by September of b
oth 1991 and 1992. For Allenrolfea in general, the total soil water po
tential within the zone of maximum root activity is more negative than
the plant's predawn xylem potential, which suggests that the plant is
partially phreatophytic and/or has a large capacitance due to its ext
ensive woody root system.