simulations and observations of patchy stomatal behavior in leaves of quercus crispula, a...
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REGULAR PAPER
Simulations and observations of patchy stomatal behaviorin leaves of Quercus crispula, a cool-temperate deciduousbroad-leaved tree species
Mai Kamakura • Yoshiko Kosugi • Kanako Muramatsu •
Hiroyuki Muraoka
Received: 20 June 2011 / Accepted: 23 September 2011
� The Botanical Society of Japan and Springer 2011
Abstract We investigated the occurrence of patchy sto-
matal behavior in leaves of saplings and a forest canopy
tree of Quercus crispula Blume. Through a combination of
leaf gas-exchange measurements and numerical simulation,
we detected patterns of stomatal closure (either uniform or
patchy bimodal) coupled with depression of net assimila-
tion rate (A). There was a clear inhibition of A associated
with stomatal closure in leaves of Q. crispula during the
day, but the magnitude of inhibition varied among days and
growing conditions. Comparisons of observed and simu-
lated A values for both saplings and the canopy tree iden-
tified patterns of stomatal behavior that shifted flexibly
between uniform and patchy frequency distributions
depending on environmental conditions. Bimodal stomatal
closure explained severe depression of A in saplings under
conditions of relatively high leaf temperature and vapor
pressure deficit. Model simulations of A depression through
bimodal stomatal closure were corroborated by direct
observations of stomatal aperture distribution using Su-
zuki’s Micro-Printing method; these demonstrated that
there was a real bimodal frequency distribution of stomatal
apertures. Although there was a heterogeneous distribution
of stomatal apertures both within and among patches,
induction of heterogeneity in intercellular CO2 concentra-
tion among patches, and hence severe depression of A,
resulted only from bimodal stomatal closure among pat-
ches (rather than within patches).
Keywords Bimodal stomatal closure � Leaf gas exchange �Midday depression � Leaf temperature �Vapor pressure deficit
Introduction
Gas exchange rates between plants and atmosphere are
determined by adjustment of photosynthetic capacity and
changes in the apertures of stomata on the leaf epidermis.
Photosynthesis and transpiration rates in individual leaves
vary in response to environmental factors such as light,
temperature, water and nutrient supplies. High light, coin-
cident with high leaf temperature or water deficit, often
causes midday depression of net assimilation rate (A),
which is coupled with stomatal closure (Tenhunen et al.
1984; Epron et al. 1995; Valladares and Pearcy 1997; Pathre
et al. 1998; Muraoka et al. 2000). Stomatal closure, induced
by increased leaf-to-air vapor pressure deficit (VPD) and/or
low leaf water potential (Maier-Maercker 1983; Mott and
Parkhurst 1991; Brodribb and Holbrook 2004), decreases
CO2 concentration within intercellular spaces (Ci). The
reduction of A at midday is the result of both an increase in
stomatal limitation and a reduction in the photochemical
process (Ishida et al. 1999; Muraoka et al. 2000).
Patterns of stomatal closure in canopy leaves of tropical
trees may be patchy during severe midday depression
(Ishida et al. 1999). Patchy stomatal behavior occurs in
M. Kamakura (&) � K. Muramatsu
KYOUSEI Science Center for Life and Nature,
Nara Women’s University, Kita-uoya Higashimachi,
Nara 630-8506, Japan
e-mail: [email protected]
Y. Kosugi
Laboratory of Forest Hydrology, Division of Environmental
Science and Technology, Graduate School of Agriculture,
Kyoto University, Kitashirakawa Oiwake-cho, Sakyo-ku,
Kyoto 606-8502, Japan
H. Muraoka
Institute for Basin Ecosystem Studies, Gifu University,
1-1 Yanagido, Gifu 501-1193, Japan
123
J Plant Res
DOI 10.1007/s10265-011-0460-8
plants with heterobaric leaves. In these leaves, vertical
extensions of bundle sheath cells delimit the mesophyll and
restrict CO2 diffusion (Mott and Buckley 1998, 2000; West
et al. 2005; Kenzo et al. 2007). Patchy stomatal behavior
occurs in response to low humidity (Loreto and Sharkey
1990; Beyschlag et al. 1992; Mott et al. 1993), water stress
(Sharkey and Seemann 1989; Gunasekera and Berkowitz
1992) and increased internal abscisic acid (ABA) concen-
tration (Downton et al. 1988; Terashima et al. 1988).
Because uniform stomatal behavior is assumed in leaf gas-
exchange calculations based on the Farquhar–von Caem-
merer–Berry model (von Caemmerer and Farquhar 1981;
Warren et al. 2003), the effect of patchy stomatal closure
on depression of A may well have been underestimated.
Although, the importance of patchy stomatal closure
effects on leaf gas-exchange rates is recognized, only a few
studies have evaluated the pattern of stomatal behavior
(uniform or patchy bimodal) associated with A depression
in tree leaves under natural conditions (Takanashi et al.
2006; Kosugi et al. 2009; Kamakura et al. 2011).
By combining a numerical analysis that calculated
simulated A at a given stomatal conductance (gs) for both
uniform and patchy stomatal behavior with a pressure-
infiltration method, Takanashi et al. (2006) demonstrated
that patchy stomatal closure with a bimodal pattern
explains midday A depression in top-canopy leaves of a
tropical rainforest. Direct observation of stomatal aperture
distributions using Suzuki’s Universal Micro-Printing
(SUMP) method showed a real patchy bimodal distribution
of stomatal apertures during midday depression in leaves of
mid- and upper-layers in tropical tree vegetation. Further-
more, there was a heterogeneous distribution of stomatal
apertures among adjacent stomata rather than among
compartments delimited by bundle sheath extensions (Ka-
makura et al. 2011). By numerical analysis, we also found
that patchy bimodal stomatal behavior occurs only during
midday depression, suggesting that stomatal aperture dis-
tribution varies flexibly within single days. On the basis of
these procedures, there have been arguments for the
occurrence of patchy stomatal closure that leads to midday
A depression in tropical trees growing in natural environ-
ment. However, there are few reported studies on quanti-
tative effects of such stomatal behavior on gas-exchange
characteristics of heterobaric tree species in other climatic
regions. Moreover, the question of whether or not patchy
stomatal behavior depends on plant species, growth envi-
ronment, or weather conditions.
The objectives of this study were to (1) describe changes
in pattern of stomatal behavior within and among days, (2)
determine factors that induce patchy bimodal stomatal
behavior, and (3) determine the scale of heterogeneity in
frequency distributions of stomatal apertures within leaves
of Quercus crispula Blume, a dominant cool-temperate,
deciduous, broad-leaf tree with heterobaric leaves. Midday
depression of A occurs in leaves of several top-canopy tree
species in cool-temperate forests (Iio et al. 2004). Because
changes in hydraulic architecture through ontogeny affect
photosynthetic capacity (Cavender-Bares and Bazzaz
2000), it is possible that leaf stomatal behavior under high
light differs between saplings and canopy trees. Thus, we
studied both life stages of Q. crispula.
We measured and numerically simulated CO2 exchange
associated with patterns of stomatal behavior under various
photosynthetic photon flux densities (PPFD), leaf temper-
atures (Tleaf), and VPD conditions in a nursery and in a
cool-temperate deciduous broadleaf forest. To predict
A values by numerical simulation, we assumed uniform and
patchy bimodal stomatal behaviors, which are the most
extreme patterns of stomatal aperture frequency distribu-
tion in leaves. Because maximum depression of A is caused
by patchy stomatal closure with a bimodal frequency dis-
tribution (Takanashi et al. 2006), we simulated largest
effects of patchy stomatal behavior on A by assuming
bimodal stomatal closure. Our comparison of observed and
simulated A detected fluctuations in A values caused by
stomatal behavior. Moreover, corroborative data on real
stomatal aperture distribution were provided by SUMP
method observations. We predicted that (1) observed
A would fluctuate between simulated A values calculated
under assumptions of uniform and bimodal stomatal
behaviors within and among days and (2) stomatal aperture
distribution with a bimodal pattern would occur among
adjacent compartments delimited by bundle sheath exten-
sions in leaves under severe environmental conditions that
cause midday depression associated with patchy bimodal
stomatal closure.
Materials and methods
Site and materials
Saplings were studied in a nursery at Kyoto University,
Kyoto, Japan (35�010N, 135�460E). Three-year-old saplings
of Quercus crispula were planted into pots (18 cm diam-
eter, 20 cm deep) filled with soil (Akadama soil:leaf
mold = 7:3, by vol.) on April 7, 2010. The leaves flushed
1–2 weeks after planting. Plants were watered daily and
treated with a Hyponex solution (Hyponex Japan, Osaka,
Japan; N:P:K = 6:10:5 at 1 g l-1) once per week. We
measured in situ leaf gas exchange and observed stomatal
apertures on 1, 7 and 24 June, 2010. Three leaves from
different saplings were used. Mean leaf number was
39 ± 3 (±SD).
We studied a full-sized tree in a cool-temperate decid-
uous broadleaf forest (36�080N, 137�250E, 1,420 m a.s.l.)
J Plant Res
123
on the north-western slope of Mt. Norikura, Japan. At the
nearby (500 m from the study site) ‘‘Takayama (TKY)
AsiaFlux site’’, annual mean air temperature and precipi-
tation from 1994 to 2008 were 7.2�C and 2,075 mm,
respectively; mean air temperature in the forest we studied
was 6.6�C. The forest canopy was dominated by Q.
crispula, Betula platyphylla Sukatchev var. japonica Hara
and B. ermanii Cham. Betula ermanii is a pioneer species
with a thin crown in the multispecies deciduous forest.
Quercus crispula is a late-successional species that forms a
multi-layered crown that often occupies space down to the
forest shrub layer. Leaf flush in all of these deciduous tree
species occurs after snow-melt. Measurements were made
on leaves collected in top layer of a Q. crispula canopy tree
using a canopy access tower (10 9 10 m on the base and
18 m tall) on 30, 31 July and 2 August, 2010. Three leaves
were collected from a single adult tree.
Measurement of leaf gas exchange
Diurnal changes in net assimilation rate (A, lmol m-2 s-1)
and stomatal conductance for water vapor (gs,
mol m-2 s-1) in intact leaves were measured under natural
photosynthetic photon flux density (PPFD, lmol pho-
tons m-2 s-1) using a LI-6400 gas-exchange measurement
system (Li-Cor Inc., Lincoln, NE, USA) with a 2 9 3 cm
clear-top chamber. Incident PPFD beside the leaf chamber
was measured with a photon sensor (LI-190SA, Li-Cor
Inc.). CO2 concentration, temperature, and relative
humidity of the air in the chamber were adjusted to
ambient levels. Ambient air temperature and relative
humidity were measured with thermo-hygrometers (HOBO
ProV2, Onset Computer corp., Bourne, MA, USA). Leaf-
to-air VPD was calculated from air temperature and rela-
tive humidity in the chamber. Air entered the chamber at a
flow rate of 500 lmol s-1. Gas exchange measurements
were made at about 15-min intervals.
Model description
To obtain normalized maximum rates of carboxylation at
25�C (Vcmax25, lmol m-2 s-1), we used the one-point
method (Wilson et al. 2000; Kosugi et al. 2003; Grassi
et al. 2005; Kosugi and Matsuo 2006); this is an inverse
method based on the Farquhar–von Caemmerer–Berry
model, and it can be used to determine actual responses of
leaves in the field. With the one-point method, apparent
partial pressure of CO2 within the intercellular space
(p(Ci)*) is estimated from variables measured with gas-
exchange methodology, and the ‘apparent’ normalized
maximum carboxylation rate at 25�C (Vcmax25*) is calcu-
lated from values of A, p(Ci)*, and Tleaf. We calculated
Vcmax25* assuming that the infinite internal conductance
(gi = ?), and thus the CO2 concentration in the chloro-
plast (p(Cc)), was identical to p(Ci)*. Hence, Vcmax25* was
calculated as follows:
Vc max 25� ¼ Aþ Rdð ÞpðCcÞ þ Kc 1þ pðOÞ
Ko
� �
pðCcÞ � pðOÞ2s
�1þ exp
DSðVc maxÞðTleafþ273Þ�DHdðVc maxÞRðTleafþ273Þ
h i
expDHaðVc maxÞðTleaf�25Þ
298RðTleafþ273Þ
h i ð1Þ
where Rd is the non-photorespiratory respiration rate
(lmol m-2 s-1); s is the specificity factor of Rubisco;
p(O) (21,000 Pa) is the partial pressure of O2 at the sites of
oxygenation; Kc and Ko are the Rubisco Michaelis–Menten
constants for CO2 and O2, respectively; Tleaf is leaf tem-
perature (�C); R is the gas constant (8.31 J K-1 mol-1);
DHa (Vcmax) is the activation energy for Vcmax; DHd (Vcmax)
is the deactivation energy for Vcmax; and DS (Vcmax) is an
entropy term. Values of Kc and Ko, s and their activation
energies used to calculate temperature dependence were
obtained from Harley et al. (1992). The Arrhenius function
was used to estimate temperature dependence of parame-
ters Kc, Ko, s, Vcmax and Rd (detailed in Kosugi et al. 2003;
Kosugi and Matsuo 2006; Takanashi et al. 2006). Vcmax25
was estimated from Vcmax25* at maximum gs (gsmax)
because Vcmax25 is the intrinsic value that represents car-
boxylation ability of leaves and is not always identical to
the apparent value (Vcmax25*), which has significant diurnal
fluctuations coupled with patchy stomatal closure (Takan-
ashi et al. 2006).
To determine the fluctuations in observed A values
between simulated A values calculated under assumptions
of uniform and patchy bimodal stomatal behaviors within
and among days, we performed simulations to predict net
assimilation rates at a given stomatal conductance for both
uniform and non-uniform stomatal behaviors using photo-
synthetic parameters obtained by the one-point method.
Uniform stomatal behavior indicates that whole-leaf con-
ductance reflects uniform change in stomatal conductance.
For non-uniform stomatal behavior, we assumed a patchy
bimodal frequency distribution of stomata, which indicates
that whole-leaf conductance reflects either open or closed
stomatal conductance. In heterobaric leaves, the bundle
sheath extensions separate mesophyll into many compart-
ments, and we termed each compartment a ‘patch’. For
patchy bimodal distribution, stomatal conductances for
open and closed patches were maximum and minimum gs
(gsmax and gsmin), and the open/closed patch ratio (roc) was
determined from the observed gs for a whole leaf. Net
assimilation rate and intercellular CO2 concentration for
each patch were estimated with the Farquhar–von Caem-
merer–Berry model used for determining patch stomatal
conductance values. We assumed uniform photosynthetic
J Plant Res
123
parameters for each patch, and average net assimilation
rate for the whole leaf was calculated by integrating net
assimilation rates of individual patches. In model simula-
tions, the net assimilation rate of each patch was calculated
following Kosugi et al. (2003), Kosugi and Matsuo (2006),
and Takanashi et al. (2006). Briefly, A values of open (Aop)
and closed (Acl) patches were determined from the mini-
mum difference between the RuBP-saturated rate or car-
boxylation-limited net assimilation rate (Ac) and the
electron transport- or RuBP regeneration-limited net
assimilation rate (Aj) calculated as follows:
Ac ¼ Vc max 25
expDHaðVc maxÞðT1�25Þ
298RðT1þ273Þ
h i
1þ expDSðVc maxÞðT1þ273Þ�DHdðVc maxÞ
RðT1þ273Þ
h i
�pðCcÞ � pðOÞ
2s
pðCcÞ þ Kc 1þ pðOÞKo
� �� Rd ð2Þ
Aj ¼J
4
pðCcÞ � pðOÞ2s
pðCcÞ þ pðOÞs
� Rd: ð3Þ
The partial pressure of CO2 in the chloroplasts of open
patches (p(Cc)op) was determined from Aop and gsmax, and
that for closed patches (p(Cc)cl) was determined from Acl
and gsmin. A J value was required to estimate the influence
of depression in the electron transport rate on net
assimilation rate. To estimate J, we used optimal Jmax
values estimated from the relationship between Vcmax and
Jmax as follows:
Jmax ¼ kjVc max: ð4Þ
Net assimilation rate (Aleaf) and CO2 concentration in
the chloroplasts (p(Cc)leaf) of the whole leaf were
calculated by multiplying the open and closed patch ratio
in a leaf by A or p(Cc) values for open and closed patches.
The equations were as follows:
Aleaf ¼ rocAop þ ð1� rocÞAcl ð5Þ
pðCcÞleaf ¼ rocpðCcÞop þ ð1� rocÞpðCcÞcl: ð6Þ
The estimated maximum rate of carboxylation at 25�C
(Vcmax25*) was determined by substituting values of Aleaf
and p(Cc)leaf into Eq. 1.
For uniform photosynthetic parameters, we used the
observed optimal values of Vcmax25 (lmol m-2 s-1) and
gsmax (mol m-2 s-1), i.e., 41.1 and 0.19 in saplings and
40.3 and 0.19 in the canopy tree, respectively. We also
used values of 0.005 mol m-2 s-1 for gsmin and 2.2 for kj
following Takanashi et al. (2006). Based on the average
line or median value listed by Kosugi and Matsuo (2006),
we used the following parameterizations: 55,200 J mol-1
for DHa (Vcmax), 220,000 J mol-1 for DHd (Vcmax),
650 J mol-1 for DS (Vcmax), and 41,500 lmol m-2 s-1 for
DHa (Rd). Other parameters were taken from Table 2 of
Takanashi et al. (2006).
Observation of stomatal aperture frequency distribution
To determine real stomatal behavior distributions, we cal-
culated the frequency distribution of stomatal apertures for
single leaves from saplings and the canopy tree using the
SUMP method (Kamakura et al. 2011). Immediately fol-
lowing leaf gas exchange measurements, we made
impressions of the surface of one of the three experimental
leaves by fastening thin celluloid plate (2 cm in diameter,
SUMP Laboratory, Tokyo, Japan) dissolved in amyl ace-
tate to the abaxial leaf surface (the site at which gas
exchange rate was measured). Individual stomatal aper-
tures distributed within a patch were observed in a field of
vision under a digital microscope (Model VH-Z450; Key-
ence, Osaka, Japan). Stomatal numbers per patch were
28 ± 5 in saplings and 25 ± 5 in the canopy tree,
respectively (mean ± SD). We examined 40 microscope
fields per leaf for both saplings and the canopy tree. The
widths of individual stomatal pores were determined from
static images using NIH image software (National Insti-
tutes of Health, Bethesda, MD, USA). Because the leaves
used for making impressions were destroyed, we used
adjacent leaves with similar photosynthetic rates for sub-
sequent leaf gas exchange measurements.
Results
Diurnal patterns of leaf gas exchange and stomatal
distribution in Q. crispula saplings
Observed and simulated plots of diurnal changes in gas
exchange rates of Q. crispula saplings are depicted in Fig. 1.
The ratios of simulated A values calculated under assump-
tions of bimodal versus uniform stomatal behaviors (ratios of
gray-dash lines versus gray-solid lines of net assimilation
rate graphs in Fig. 1) were 0.67 ± 0.26, 0.46 ± 0.11, and
0.69 ± 0.08 on 1, 7, and 24 June, respectively
(mean ± SD). These values indicate the maximum effect of
patchy stomatal closure on A. Plots of observed A values fell
between plots of simulated A values calculated under
assumptions of uniform and bimodal stomatal behaviors.
The ratios of observed to simulated A under the assumption
of uniform stomatal behavior were 1.01 ± 0.17,
0.82 ± 0.02, and 0.61 ± 0.15 (mean ± SD). These values
indicate the actual effect of patchy stomatal closure on A,
with maximum depression occurring on 24 June. On 1 and 24
June, observed A and gs reached their maxima in the morn-
ing, and then decreased during the day as PPFD
([1,500 lmol m-2 s-1), Tleaf, and VPD increased to highest
J Plant Res
123
values. Observed A and gs values were rather constant during
7 June when PPFD, Tleaf, and VPD were more moderate. Net
assimilation and transpiration rates (TR) during midday
hours of 24 June were more depressed than those on 1 June.
A plot of observed A values through the day on 1 June fell on
the simulated A line calculated under assumption of uniform
stomatal behavior. On 24 June, however, the plot of observed
A values shifted to the simulated A line calculated under the
assumption of bimodal stomatal behavior (with PPFD, Tleaf,
and VPD increasing to maximum values), suggesting
changes in patterns of stomatal behavior.
Relationships between observed and simulated A values
for three leaves measured on each day demonstrate that
uniform stomatal behavior largely explained observed
trends in A through the day on 1 June (Fig. 2). This was not
the case for 7 June, when neither nor bimodal stomatal
behaviors explained observed trends in A. On 24 June,
uniform stomatal behavior explained only higher values of
observed A in the morning, but patchy stomatal behavior
with a bimodal distribution explained depressed values of
A during midday hours. Thus, there was probably a shift in
stomatal behavior pattern (from uniform to patchy bimo-
dal) during the day on 24 June. A comparison of data for 1
and 24 June also suggests that uniform and bimodal sto-
matal behavior largely explained the magnitude of the
severe depression of A on 24 June and the moderate
depression on 1 June.
Figure 3 depicts images (captured by SUMP method)
and plots of stomatal aperture frequency distributions
within a patch (a, d, g), and pooled frequency distribution
data for both stomatal apertures (b, e, h) and mean stomatal
apertures of patches (c, f, i) within single leaves of Q.
crispula saplings. On 1 June, most of stomata were wide
open at 0900 hours (Fig. 3a, b, c), following which, there
was a depression of stomatal openings at 1100 hours
(Fig. 3d, e, f). On 24 June, however, we observed open
(most stomata were wide open, Fig. 3g-1) and closed pat-
ches (most stomata were closed, Fig. 3g-2) on a single leaf
at 1200 hours (Fig. 3h). We detected heterogeneity of
individual stomatal pores within a patch at each observa-
tion time (Fig. 3a, d, g). However, two peaks in the fre-
quency distribution plots of mean stomatal apertures of
patches within a leaf observed at 1200 hours on 24 June
(Fig. 3i) indicate that there was a natural patchy bimodal
distribution of stomatal apertures among patches rather
than within patches during midday depression. The actual
scale of patchiness coincided with the theoretical scale of
patchy bimodal stomatal closure assuming a bimodal fre-
quency distribution of ‘closed’ and ‘open’ patches.
Fig. 1 Plots of observed and simulated (through numerical analysis
based on the Farquhar–von Caemmerer–Berry model) diurnal
changes in gas exchange rates in three Q. crispula sapling leaves.
Measurements were made on 1, 7 and 24 June, 2010. Net assimilation
rates (A), stomatal conductances (gs), transpiration rates (TR),
photosynthetically active photon flux densities (PPFD), leaf temper-
atures (Tleaf), and leaf to air vapor pressure deficits (VPD) are plotted
against time of day. Comparisons were made between observed
A values and simulations assuming uniform and patchy bimodal
patterns of stomatal behavior. Solid vertical lines indicate times when
impressions were made from abaxial leaf surfaces using the SUMP
method
c
J Plant Res
123
Diurnal patterns of leaf gas exchange and stomatal
distribution in a Q. crispula canopy tree at the TKY site
The ratios of simulated A values of the canopy tree of Q.
crispula calculated under assumptions of bimodal versus
uniform stomatal behaviors were 0.47 ± 0.03, 0.55 ±
0.04, and 0.51 ± 0.03 (mean ± SD) on 30 July, 31 July,
and 2 August, respectively (Fig. 4). These values indicate
the maximum effect of patchy stomatal closure on A. The
ratios of observed to simulated A under the assumption of
Fig. 2 Plots of observed and simulated net assimilation rates
(A) calculated by numerical analysis based on the Farquhar–von
Caemmerer–Berry model for three Q. crispula sapling leaves.
Simulated A was calculated assuming uniform stomatal closure
(a) or patchy bimodal stomatal closure (b). Close fits of observed data
to the line calculated under the assumption of uniform stomatal
behavior explained A. A close fit of observed data to the line
calculated under the assumption of patchy bimodal stomatal closure
indicates that patchy stomatal behavior with a bimodal distribution
explained A
Fig. 3 Images (captured by the SUMP method) and frequency
distribution plots of stomatal apertures within a patch (a, d, g), and
pooled frequency distribution plots for stomatal apertures (b, e, h) and
mean stomatal apertures for patches (c, f, i) within single Q. crispulasapling. Data were captured at 0900 and 1100 hours on 1 June, and at
1200 hours on 24 June
J Plant Res
123
uniform stomatal behavior were 1.02 ± 0.06, 1.04 ± 0.02,
and 0.81 ± 0.02 (mean ± SD). Thus, the effect of patchy
stomatal closure on A in canopy tree leaves was smaller
than in sapling leaves. On cloudy days (30 and 31 July),
A and gs were not depressed during midday hours, and
plotted observed A values fell on the simulated A line
calculated under the assumption of uniform stomatal
behavior through the day. On 2 August, however, gs
decreased during midday hours under higher PPFD
([1,200 lmol m-2 s-1), Tleaf, and VPD, indicating mod-
erate depression of A. On this day, observed A moved
between simulated A lines calculated under assumptions of
(1) uniform or (2) bimodal stomatal behaviors.
The relationships between observed and simulated
A values for three tree leaves on each day indicate that
uniform stomatal behavior explained optimum A through
the days of 30 and 31 July (Fig. 5). On the other hand, it
was difficult to determine whether either uniform or
bimodal stomatal behavior explained A through the day on
2 August.
Figure 6 depicts the distribution of leaf stomatal aper-
tures in the Q. crispula canopy tree on 2 August. Most
stomata were wide open at 0930 hours (Fig. 6a, b, c); there
was a depression of stomatal opening was shown at
1200 hours (Fig. 6d, e, f). At 1530 hours, however, open
and closed patches were observed within the leaf (Fig. 6g,
h). Two peaks in the frequency distributions of mean sto-
matal apertures of patches within the leaf (Fig. 6i) indicate
that there was a natural bimodal stomatal closure in late
afternoon hours.
Discussion
Changes in pattern of stomatal behavior by day
and growing condition
Patchy stomatal closure occurs with midday depression of
A in tree species with heterobaric leaves (Beyschlag and
Pfanz 1990; Beyschlag et al. 1992; Takanashi et al. 2006;
Kamakura et al. 2011). We showed a clear inhibition of
A coupled with stomatal closures in leaves of both saplings
and a canopy tree of Q. crispula during the daytime hours
on clear days (1 and 24 June in the nursery, and 2 August at
the TKY site), but the magnitude of inhibition varied by
day and growing conditions (Figs. 1, 3). By comparing
observed and simulated A values at a given gs for both
uniform and bimodal stomatal behaviors and observing
stomatal distribution directly (Figs. 2, 3), we demonstrated
Fig. 4 Plots of observed and simulated diurnal changes in gas
exchange rates in three leaves from a Q. crispula canopy tree at the
TKY site. Measurements were made on 30, 31 July, and 2 August,
2010. Net assimilation rates (A), stomatal conductances (gs), transpi-
ration rates (TR), photosynthetically active photon flux densities
(PPFD), leaf temperatures (Tleaf), and leaf to air vapor pressure
deficits (VPD) are plotted against time of day. Comparisons were
made between observed A values and simulations assuming uniform
and patchy bimodal patterns of stomatal behavior. Solid vertical linesindicate times when impressions were made from abaxial leaf
surfaces using the SUMP method
c
J Plant Res
123
that patchy bimodal stomatal closure explained severe
depression of A during midday hours of 24 June; moderate
midday depression of A was coupled with uniform stomatal
closure in Q. crispula saplings on 1 June. Thus, midday
depression of A did not always occur with bimodal sto-
matal closure. Numerical analysis indicated that uniform
stomatal behavior in leaves of the canopy tree best
explained A through cloudy days at the TKY site (30 and
31 July, Fig. 5). However, neither uniform nor bimodal
stomatal behaviors explained A in leaves of either saplings
Fig. 5 Comparisons between observed and simulated net assimila-
tion rates (A) calculated by numerical analysis based on the Farquhar–
von Caemmerer–Berry model for three Q. crispula canopy tree leaves
collected at the TKY site. Simulated A was calculated assuming
uniform stomatal closure (a) or patchy bimodal stomatal closure (b).
Close fits of observed data to the line calculated under the assumption
of uniform stomatal behavior explained A. A close fit of observed data
to the line calculated under the assumption of patchy bimodal
stomatal closure indicates that patchy stomatal behavior with a
bimodal distribution explained A
Fig. 6 Images (captured by the SUMP method) and frequency
distribution plots of stomatal apertures within a patch (a, d, g), and
pooled frequency distributions of stomatal apertures (b, e, h) and
mean stomatal aperture of patches (c, f, i) within a Q. crispula canopy
tree leaf at the TKY site. Data were captured at 0930, 1200, and
1530 hours on 2 August
J Plant Res
123
or the canopy tree through the days of 7 June and 2 August
(Figs. 2, 5). Thus, on sunny days with high temperature and
VPD, the pattern of stomatal closure shifts to a bimodal
frequency distribution and induces severe midday
A depression. In contrast, the patterns of stomatal opening
and closing show a uniform frequency distribution (in some
cases, neither uniform nor bimodal frequency distribution)
on cool, cloudy days. These results suggest that patterns of
stomatal behavior shifted in a flexible manner between
uniform and bimodal frequency distributions depending on
micrometeorological conditions. Different patterns of sto-
matal behavior between saplings and the canopy tree
indicate that growing conditions would also affect stomatal
opening and closing pattern.
Effects of biotic factors on leaf gas exchange
Our numerical simulation predicted that gi was infinite;
thus p(Cc) and p(Ci)* were identical. However, diurnal
change in gi might have been caused by aquaporin, which
affects photosynthetic CO2 diffusion (Terashima et al.
2006). Figure 7 depicts the sensitivity of simulated A under
assumption of uniform stomatal closure (a) and patchy
bimodal stomatal closure (b) to changes in gi. In each
graph, observed A varied much more than the gi range.
Thus, changes in stomatal behavior were more susceptible
to leaf gas exchange than gi.
The SUMP-based analysis demonstrated that ‘‘closed
patches’’ assumed in a numerical simulation might in reality
be rather open (Figs. 3, 6). Hence, the real gsmin might have
been higher than the value we used (0.005). Figure 8 depicts
the sensitivity of simulated A to changes in gsmin. Simulated
A values under the assumption of bimodal stomatal closure
decreased with gsmin. If bimodal stomatal closure with a
higher value of gsmin ([0.005) is assumed, simulated
A values under the assumption of bimodal stomatal closure
would be higher than those of this study (Figs. 1, 4). If
bimodal stomatal behavior with a higher value of gsmin were
to occur in nature, bimodal stomatal behavior might have
explained A on 7 June and/or 2 August since A on those two
dates were not explained neither by uniform nor bimodal
stomatal behavior (Figs. 2, 5).
Which factors induce bimodal stomatal behavior?
Because the saplings used in this study were well watered
before measurements, midday stomatal closure on 1 and 24
June might have been caused by increased transpirational
demand (Maier-Maercker 1983; Mott and Parkhurst 1991)
rather than decreased leaf water potential. Comparisons of
gas exchange data for 1 and 24 June indicate that magni-
tude of midday depression in Q. crispula saplings was
correlated with Tleaf and VPD, which are strongly related to
transpirational demand (Fig. 1), as reported previously
(Lange 1988; Muraoka et al. 2000). Indeed, Tleaf and VPD
increased rapidly by midday on 24 June, and depression of
A began earlier than on 1 June. Moreover, TR decreased
with severe depression of gs during midday hours of 24
June (Fig. 1). Hence, the pattern of stomatal behavior,
which varied flexibly with Tleaf and VPD, appeared to
determine the magnitude of midday depression. In other
words, bimodal stomatal closure may occur when Tleaf and
VPD exceed certain threshold values even though tree
species with heterobaric leaves would not show bimodal
stomatal behavior at sub-threshold values of these two
parameters.
The effect of patchy stomatal closure on A in the canopy
tree leaves was smaller than in saplings (Figs. 1, 4). Sap-
lings generally have smaller and shallower root systems
Fig. 7 Sensitivity of simulated A under assumption of uniform
stomatal closure (a) and patchy bimodal stomatal closure (b) to
changes in internal conductance (gi). Data from 24 June (leaf 3)
Fig. 8 Sensitivity of simulated A under the assumption of patchy
bimodal stomatal closure to changes in minimum stomatal conduc-
tance (gsmin). Data from 24 June (leaf 3)
J Plant Res
123
than canopy trees, which are able to develop root systems
into deeper soil layers where water may be more abundant
(Lyford 1980). Canopy trees also have great biomass
allocated to storage tissues that may hold reserve water
(Holbrook and Putz 1996). Thus, different age classes of
trees use different strategies when responding to water
stress under high light; saplings resist water stress by
closing stomata, whereas canopy trees avoid water deficit
by accessing deeper water reserves (Cavender-Bares and
Bazzaz 2000). Although Tleaf and VPD values of the can-
opy tree during 2 August were lower than those in saplings
during 24 June (Figs. 1, 3), it is also possible that a dif-
ference in stomatal sensitivity between saplings and can-
opy trees under high light may affect pattern of stomatal
behavior during midday hours.
On 2 August, Tleaf and VPD of the canopy tree reached
maxima during midday hours, and then decreased with
light reduction (Fig. 4). Nevertheless, we assumed
depression of A coupled with bimodal stomatal closure in
Q. crispula leaves during late afternoon hours. Kosugi et al.
(2009) reported that depression of A coupled with bimodal
stomatal closure occurs in tropical rainforest top-canopy
leaves during late afternoon even under relatively moderate
PPFD, Tleaf and VPD. Thus, bimodal stomatal closure may
be cued by circadian rhythms as well as by transpirational
demand (Doughty et al. 2006; Kosugi et al. 2009).
Scale differences in the heterogeneity of stomatal
aperture distribution
Our direct observation of stomatal aperture frequency
distribution in Q. crispula leaves using the SUMP method
agreed with simulated depression of A caused by bimodal
stomatal closure, indicating real occurrence of patchy
bimodal distribution in stomatal apertures (Figs. 3g, 6g).
We detected bimodal distributions of stomatal apertures
among patches by the presence of two peaks in the fre-
quency distributions of mean stomatal apertures of patches
within single leaves (Figs. 3i, 6i); we also observed het-
erogeneity of individual stomatal pores within a patch.
Hence, bimodal stomatal closure occurred among patches
rather than within patches in Q. crispula leaves. Theoret-
ically, the bimodal distribution of stomatal apertures
among patches rather than within patches would lead to Ci
heterogeneity among patches and, hence, to severe
depression of A (Terashima et al. 1988). Our results for Q.
crispula were concordant with this theoretical manner of
‘patchy bimodal stomatal closure’. We reported previously
that a bimodal distribution of stomatal aperture occurs
within patches in top-canopy leaves of several tropical
rainforest species, and we observed that this scale of
patchiness is coincident with severe depression of A (Ka-
makura et al. 2011). In theory, CO2 absorbed from open
stomata diffuses uniformly within a patch and the occur-
rence of patchy bimodal stomatal behavior within patches
rather than between them would not cause heterogeneity of
Ci. However, the effects of real distributions of stomatal
apertures within and between patches on the distribution of
Ci, and hence A, may be more complicated. Further anal-
yses are necessary to determine which scales of hetero-
geneity in the frequency distribution of stomatal apertures
regulate leaf gas exchange capacity.
Acknowledgments We thank Dr. Hibiki Noda of the University of
Tsukuba for her support of field investigations at the Takayama site.
We also thank Mr. Kenji Kurumado and Yasunori Miyamoto at the
Takayama field station, Gifu University, for their arrangement of field
investigations.
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