The effects of summer exposure to ozone on the frost hardiness after the vegetation period of Norway
and Sitka spruce seedlings
P. W. Lucas
Institute of Environmental and
Biological Sciences, (Division
ofBiological Sciences), University
of Lancaster, Lancaster, LA1 4YQ. U.K.Introduction
No single
causehas
beenidentified
toexplain the decline of coniferous
trees in somehigh-elevation forests
inEurope
andparts of the USA, but
a consensusview
among researchers is that the observedchanges
are associatedwith
airpollutants.
Air
pollutants
are,however, only
one of avariety
ofenvironmental
stresses which may affect thephysiology
of trees andwhich could
predispose
or incitedamage.
In those areas where
forest declines
areoccurring, daily
mean ozone concentra-tions
are often above 100!g-nrr3. Expo-
sure to
elevated concentrations
of ozone isknown
todamage cell membranes
(Heath, 1980). Since loss of
membraneintegrity is thought
tobe the major
causeof frost injury (Levitt, 1980), there
aregood physiological
reasons tobelieve that
ozone
could
increase thesensitivity
ofplants
tofreezing injury.
The objectives
of thepresent study
were to
investigate whether long-term
ex-posure to ozone
during
the summeraf-
fected the frost
hardening
anddeharden- ing of Norway
spruce(Picea abies
L.Karst)
andSitka
spruce(P sitchensis [Bong] Carr) such that their susceptibility
to
frost damage
wasincreased.
Materials
andMethods
Ozone fumigafion
andgrowth
measure-ments
At the
beginning
ofMay
1987, 25 2 yr old seed-lings
of eachspecies
wereassigned randomly
to each of 4
large-scale fumigation chambers,
described
previously by
Lucas et al.(1987).
Fumigation
of theeseedlings began
on 1 June1987 and continued until 11
September
1987.In two of the
chambers,
trees wereexposed
toozone for 7 h each
day (08:00-15:00)
for 5 d per wk at an averagehourly
concentration of 140μg·m- 3 ;
theremaining
chambers received charcoal-filtered air and acted as controls.Frost
hardening and freezing
testsAt the end of the
fumigation,
the trees remainedin the chambers to frost harden until lateral shoot
elongation
had ended and minimum airtemperatures
had fallen below 10°C. The firstfreezing
test was therefore not carried out untilthe 20 October 1987.
On each
sampling occasion,
currentyear’s
lateral shoots were detached from each of 5 trees of eachspecies
and from each chamber.Two
shoots, approximately
4 cm inlength,
fromeach tree were frozen in an unlit
programmable freezing
cabinet as describedby
Lucas et al.(1988). Separate
batches of shoots were sub-jected
toseparate freezing
tests in the range -5 to-25°C,
withcooling
andwarming
rates of 5°Ch- 1
and 10°C
h-!, respectively.
Thepreset
tar-get temperature
was held for 3 h. Afterfreezing,
the middle
portion
of each shoot wasplaced
ina 20 ml
polypropylene
vial and 15 ml of deion- ised water were added. The vial wascapped,
shaken and stored at 6°C. Solution
conductivity
was measured after 24 h
using
aplatinum
elec-trode. The
samples
were stored at 6°C for a fur-ther 5 d and the
conductivity
wasagain
mea-sured. After this second
reading,
the shootswere stored at 6°C and after 14 d scored for visual
damage (0
= nodamage,
1 = <50%damaged,
2 = >50%damaged,
3 = shootbrown,
assumeddead).
The shoots + vials werethen autoclaved and the total
conductivity (C-)
of the solution determined. Based on the
assumption
that the rate ofleakage
of electro-lytes
from a detached shoot is controlledby
dif-fusion,
theconductivity
of the solution at any time(C,)
can be describedby
a first-order reac-tion
equation: C t
=G {1 e-’&dquo;). ).
By logarithmic
transformation of the aboveequation
and substitution of the measuredconductivity values,
the rate ofchange
inconductivity
or normalisedleakage
rate(k)
wascalculated. A
comparison
of k values with visibledamage
showed for bothspecies
ofspruce that shoots with k values >0.35% h-I would be killed.
Results
By the time of the first freeze
test on 20October
1987(Fig. 1 the Norway spruce had hardened
to atemperature
ofabout - 19°C, although there
was adelay in hardening in those shoots that had been
exposed
to ozone.For the Sitka
spruce, there was noeffect of pollutant exposure
on
the timing of frost hardiness attained by
the
shoots but, compared
to theNorway
shoots at this
time,
there was aquite
marked difference
(approximately 12°C)
inthe
depth
of hardiness attained.Between
20October and
24November, the Norway shoots hardened
at a rateof
ca
0.3°C d- 1 compared
tothe Sitka
whichhardened at a rate
of
ca0.2°C d- 1 and had acquired
at least afurther 5-6°C of hardiness.
TheNorway shoots
may,how-
ever,have
hardened tomuch lower
tem-peratures,
asthe
minimumtemperature
which could be
attained by the freezing
chamber was
only -25°C.
For thissecond freezing
testand for the
testsmade
at laterdates, there
were nosignificant
effects of
ozone on thefreezing sensitivity
of shoots
fromeither species of spruce.
Over the period
24November-20
January, there
was nochange
inthe leak-
age rate of
the Norway
spruceshoots
and it isprobable
thatthey
werehardy
totemperatures considerably
in excess ofthe minimum
freezing temperature shown (Fig. 2).
Incontrast,
theSitka shoots had only
attained a further3°C
ofhardiness during
this time.By mid-May, bud burst had occurred
inall the
trees and a freezer test atthis time
showed that shoots of bothspecies
haddehardened
totemperatures between
-5and
-10°C (Fig. 3).
Discussion and Conclusions
Exposure
to ozonedelayed
the frosthard- ening of Norway spruce shoots during
mid-autumn. Similar results for Norway
spruce have also been observed by other researchers, both with
ozone(Barnes and Davison, 1988) with S0 2 and N0 2 in
com-bination (Freer-Smith and Mansfield,
1987) and with acid
mist(Cape
etal.,
1988). The results of the present study,
therefore, appear
tosupport
thehypothe-
sis that air pollutants may predispose
Nor-way spruce trees to
damage by
frosts.For
Sitka
spruce,however, there
wereno
effects
of ozone ondelayed
frosthard- ening and the
resultsdiffer from those
reported previously by Lucas et al. (1988),
in
which spruce seedlings
wereexposed
to a
similar concentration of
ozoneusing
the
samefumigation system. In this
case,although there
was noeffect of the pollu-
tant on
the attainment of deep winter hard- iness, the sensitivity of detached shoots
to autumn frosts wasfound
tobe increased.
At present
it isdifficult
tooffer
anexplana-
tion for
the different
results betweenthe
two
experiments, but other environmental
factors may
beinvolved
inmodifying the
plant’s response
tothe
ozone.Acknowledgments
This work was
supported
inpart by
the UKDepartment
of theEnvironment,
the Commis- sion of theEuropean Communities,
the NE ForestExperiment
Station of the USDA Forest Service and the US Environmental ProtectionAgency,
aspart
of the National AcidPrecipita-
tion Assessment
Program.
References
Barnes J.D. & Davison A.W.
(1988)
The influ-ence of ozone on the winter hardiness of Nor- way spruce.
New Phytol. 108, 159-166 Cape J.N., Sheppard L.J.,
LeithI.D., Murray M.B.,
Deans J.D. & Fowler D.(1988)
The effects of acid mist on the frost hardiness of red spruceseedlings. Aspects Appl.
Biol.17,
141- 149Freer-Smith P.H. & Mansfield TA.
(1987)
The combined effects of low
temperature
andS0 2
+N0 2 pollution
on the new season’sgrowth
and water relations of Picea sitchensis.New Phytot. 1 O6,
225-237Heath R.L.
(1980)
Initial events ininjury
toplants by
airpollutants.
Annu. Rev. PlantPhy
sioL
31,
395-401Levitt J.
(1980) Responses
ofplants
to environ-mental stresses. In:
Physiological Ecology
Series.(2nd
edn. Vol.1) Chilling, Freezing
andHigh Temperature
Stresses. AcademicPress,
NewYork,
pp. 254-262Lucas
P.W.,
Cottam D.A. & Mansfield TA.(1987)
Alarge-scale fumigation system
forinvestigating
interactions between airpollution
and cold stress on
plants.
Environ. Pollut.43,
15-28Lucas
P.W.,
CottamD.A., Sheppard
L.J. &Francis B.J.
(1988)
Growth responses anddelayed
winterhardening
in Sitka spruce fol-lowing
summer exposure to ozone. NewPhy-
tol.