Abstract
Key message
Defoliation followed by water deficit showed time-dependent effects on plant water status and growth in black spruce ( Picea mariana (Mill.) B.S.P.). Biotic stress negatively (during active defoliation by growing instars) and positively (after defoliation) affected plant water relations. However, water deficit, alone or combined with defoliation, prevails over defoliation-related stress for radial growth and sapling vitality.
Context
Tree vitality is influenced by multiple factors such as insect damage, water deficit, and the timing of these stresses. Under drought, positive feedback via the reduction of leaf area may improve the water status of defoliated trees. However, the effect on tree mortality remains largely unknown.
Aims
We investigated the effects of defoliation followed by a water deficit on tree growth, plant water status, and mortality in black spruce (Picea mariana (Mill.) B.S.P.) saplings.
Methods
In a controlled greenhouse setting, saplings were submitted to combined treatments of defoliation and water stress. To assess the impact of these stresses and their interaction, we measured phenology, twig development, secondary growth of the stem, water potential, and mortality of the saplings.
Results
Both defoliation and water deficits reduced growth; however, the effect was not additive. During active defoliation, we observed a higher evaporative demand and a lower midday leaf water potential Ψmd. We observed an opposite pattern of response post-stress. Drought alone increased sapling mortality immediately after the stress period, but after c.a. 20 days, mortality rates remained similar following combined drought and defoliation.
Conclusion
Our results highlight two key periods during which defoliation affects plant water relations either negatively (during active defoliation) or positively (after defoliation). Mortality in defoliated saplings was reduced immediately following drought because available internal water increased in the stem.
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1 Introduction
The assessment of tree vitality must consider the effect of multiple stress factors that vary in terms of their timing, frequency, intensity, and interactions (Mitchell et al. 2013). Developing an understanding of the effects of multiple stress responses (i.e., additive, synergistic, or antagonistic effects, see Bansal et al. (2013)) remains a major challenge, although it is crucial to understand the physiological mechanisms of interactive effects. Indeed, the boreal forest faces increasing challenges linked to both drought and defoliating insects, co-occurring events that increase tree mortality (De Grandpré et al. 2019). Outbreaks of the eastern spruce budworm (Choristoneura fumiferana Clemens) are currently one of the major natural disturbances in the boreal forest (Bergeron et al. 1995; Rossi and Morin 2011; Simard et al. 2012). These events cause marked reductions in tree growth and increased stand mortality (Bouchard et al. 2005; Zhang et al. 2014). Drought is another important stress with rates of tree mortality in Canada’s boreal forest increasing by 1.9% year−1 in the eastern part to 4.9% year−1 in the western portion between 1963 and 2008 (Peng et al. 2011). A recent study on trembling aspen in a mixed boreal forest of western Canada indicated that drought had a greater impact on decreasing growth than defoliation (Chen et al. 2017b). Do these multiple stress factors (defoliation followed by a water deficit) make spruce more or less susceptible to water stress and increase/decrease mortality?
Several studies have reported that xylem growth can be reduced under conditions of drought or severe drought (Chen et al. 2017a; Fernández-de-Uña et al. 2017; Forner et al. 2018; Giovannelli et al. 2007; Gruber et al. 2010; Oberhuber et al. 2011; Rossi et al. 2009). However, contrasting responses have been observed for the effects of both drought and defoliation on growth. No significant changes in height and diameter growth were observed in defoliated Eucalyptus globulus Labill. (Eyles et al. 2009; Quentin et al. 2012). Jacquet et al. (2014) showed that the radial growth of young Mediterranean conifers was reduced by defoliation. However, the interaction of drought and defoliation did not limit radial growth in Pinus pinaster Aiton (Jacquet et al. 2014). Experimental research on young trees is necessary to elucidate the simultaneous impacts of drought and defoliation on growth.
The ecophysiological responses to defoliation at the canopy level versus the leaf level are complex. Soil-to-leaf hydraulic conductance and leaf area play key roles in regulating water transport and gas exchange (Mencuccini 2003; Tyree 2003). Defoliation can improve tree water relations at the canopy level (Páez et al. 1995; Quentin et al. 2012), because the reduction in leaf area changes the water balance, increasing transpiration rates and the leaf-specific hydraulic conductance (Quentin et al. 2011). Similarly, whole-plant water relations show a less negative midday leaf water potential (Quentin et al. 2011; Salleo et al. 2003). In contrast, after 2–3 years of spruce budworm outbreaks, the relative water content of twigs can be reduced by an average of 8% in heavily defoliated mature balsam fir (Abies balsamea (L.) Mill.) (Deslauriers et al. 2015), indicating that the water status at the whole-plant level is reduced.
Under conditions of decreased soil water availability, a reduced stomatal conductance postpones or avoids dehydration during periods of water deficit (Bréda et al. 2006; Choat et al. 2018; Cochard et al. 2002). This efficient stomatal control prevents water loss and decreases of leaf water potential at a critical threshold for xylem dysfunction (Bond and Kavanagh 1999; Delzon and Cochard 2014; Tyree and Zimmermann 2002). Moreover, stomatal control occurs in black spruce at low leaf water potentials as high as − 1.0 MPa to − 1.5 (Bernier 1993; Stewart et al. 1995). More negative water potential has been linked to tree mortality after drought due to loss of hydraulic conductivity with a xylem air entry pressure (P12) of − 2.9 MPa (Balducci et al. 2015). Xylem vulnerability to water stress is associated with leaf water potential where 50% of xylem tracheids are not working (Brodribb and Cochard 2009). Thus, the risk of hydraulic failure could be heightened under defoliation, as trees can maintain a high level of gas exchange, even during drought periods, to increase carbon gain at the cost of reducing water potential and thus loss of hydraulic conductivity (Salmon et al. 2015). Nevertheless, studies of plant water status can add significant knowledge regarding transpiration dynamics and tree vitality under conditions of both defoliation and drought.
Here, we investigate the effects of defoliation by the eastern spruce budworm followed by a water deficit on growth, plant water status, and mortality of black spruce saplings within a controlled greenhouse experiment. We expected the following responses:
-
(1)
Plant water status is expected to decrease (negative effect) following a water deficit. Under defoliation, plant water status is expected to improve (positive effect) because of reduced transpiration in the defoliated saplings. The combined effect of a water deficit and defoliation should therefore be less negative than that of a water deficit alone because of an additive effect (the sum of the negative and positive effects of both water deficit and defoliation, respectively);
-
(2)
Both defoliation and water deficit will cause growth reductions, and their combined effects will be additive (the sum of) or synergistic (greater than the sum of the separate effects of defoliation and water deficit);
-
(3)
Mortality rates are expected to follow a pattern similar to that of water status (Hypothesis 1), with higher mortality rates under conditions of water deficit and lower rates under the combined effect of a water deficit and defoliation.
2 Materials and methods
2.1 Experimental design
The experiment ran from May to September 2014 in a greenhouse at the Université du Québec à Chicoutimi (QC, Canada, 48° 25′ N, 71° 04′ W). The plants were 6-year-old black spruce saplings placed in plastic pots (11.4 L) filled with perlite and peat moss vermiculite. The plants’ mean stem base diameter was 18.0 ± 3.2 mm, and the mean height was 73.5 ± 13.1 cm. Each sapling received a single dose of 1 L of 20–20–20 fertilizer at 6 g L−1 at the beginning of the experiment. The saplings were grown under natural daylight and local photoperiod conditions. The average temperature was 20.2 °C throughout the experiment. The average maximum temperature was 26.3 °C, while the average minimum temperature was 13.9 °C.
The experimental design consisted of 192 saplings in four fully replicated blocks (compartments), each with of 48 plants, divided into four treatments according to a split-split-plot design. Each block was split into two defoliation treatments (24 plants for each treatment), one with spruce budworm (named defoliated) and one without spruce budworm (named undefoliated). All treatment plots were surrounded by border plants. The 24 plants in each defoliation treatment were further subdivided into two irrigation treatments, i.e., irrigated (I) and non-irrigated (NI), and were set out as 12 plots having two plants each. Enclosures were placed over the plants to avoid the migration of larvae; they were made of a wooden frame (288 cm high × 183 cm wide × 173 cm high) covered with a fine textile net (proteknet 60 g; mesh size of 1.9 × 0.95 mm) that allowed the passage of 93% of light. For the spruce budworm defoliation treatment, 125 larvae at the L2 stage (standard code Glfc:IPQL:Cfum01 to Cfum16, Roe et al. (2018)) were applied in groups of 25 onto the first whorls of each sapling when more than 50% of the apical buds had reached a stage 3 (see description of bud phenology). Each pot was irrigated via drip watering. All plants received 1.2 L of water per day during the initial part of the experiment up to the day of the year (DOY) 160. For the NI treatment, irrigation ceased for 23 days (from DOY 160 to DOY 182) during the phase of active primary growth (Zhai et al. 2012). When the pre-dawn water potential (Ψpd) dropped under − 3 MPa in NI plants, irrigation was resumed from DOY 183 until the end of the experiment.
2.1.1 Bud phenology and growth
We measured phenology and growth twice per week for 48 randomly selected trees (12 trees × 2 defoliation treatments × 2 irrigation regimes). The observation of bud stages followed Dhont et al. (2010) and Rossi and Isabel (2017) and corresponded to the following: 1, open bud; 2, elongated bud; 3, swollen bud; 4, translucent bud; 5, split bud; 6, exposed shoot. Two branches of the first whorl were selected for lateral growth measurements, and an electronic caliper (mm) was used to record this growth. The stem radius (mm) of 18 saplings was measured using automatic point dendrometers (LVDT, Macro Sensor PR750, Pennsauken, NJ). Dendrometers were appositely constructed to fit on small stems with a sensing rod held by a constant force against the outer surface of the bark and at about 5 cm above the collar. The stem size was recorded every 15 min and was averaged over each day (Deslauriers et al. 2007).
2.1.2 Spruce budworm
Spruce budworm development stages (phenological instar stages L2 to L6 and pupae stage 7) were determined based on the size of the head capsule of the larvae according to the insect’s life history (Deslauriers et al. 2019; Pureswaran et al. 2015). Instar phenology was monitored on three larvae twice per week, randomly picked from 48 randomly selected trees (12 trees × 2 defoliation treatments × 2 irrigation regimes) and then put back onto the sapling. An overall plant defoliation level was determined visually on saplings branches, according to the shoot-count method (Maclean and Lidstone 1982; Piene et al. 1981). We used six defoliation classes that correspond to a median percentage of defoliation (Deslauriers et al. 2019).
2.1.3 Plant water status
The measurements of plant water status involved destructive samplings and used 16 different saplings (4 trees × 2 defoliation treatments × 2 irrigation regimes). The pre-dawn leaf water potential (ψpd) and midday leaf water potential (ψmd) were measured using a pressure chamber (PMS Instruments, Corvalis, OR, USA). We took ψpd measurements between 2:00 AM and 4:00 AM and ψmd measurements between 9:00 AM and 11:00 AM. The relative soil water content (VWC) was monitored using a TDR probe (time domain reflectometer, Fieldscout 300). The measurements were taken at 7-cm depth in each pot and replicated twice (Topp et al. 1984).
2.1.4 Plant mortality
Sapling mortality was determined by considering the main damaged structural components: complete needle wilting, cambium collar, and stem necrosis (Balducci et al. 2013). Every week, following the stress period, we calculated the mortality rate (percentage, %) from the total number of saplings that had died within each of the defoliation and irrigation treatments.
2.2 Statistical analysis
Bud and larvae phenology were analyzed as qualitative variables. The average date (\( \overline{x} \)) and standard deviation (\( {s}_{\overline{x}} \)) at which the Ei stage (from 1 to 6) occurred were determined according to:
where xi is the date expressed in DOY, \( {f}_{E_i} \) is the frequency of the Ei stage, and k is the number of sampling dates [adapted from Scherrer 2007]. To compare the progression of the phenological stages between treatments, we developed ordinal regression models using the LOGISTIC procedure in SAS (SAS Institute, Cary, NC, USA). Differences between defoliation treatments and irrigation regimes were identified using the LSMEANS option with a Bonferroni multiple test comparison.
A Gompertz function (NonLINear regression, SAS) was fitted to apical and lateral growth to determine the total growth achieved and growth rate (Deslauriers et al. 2003). The Gompertz function was defined as:
where y is weekly cumulative growth (mm), t the time computed in DOY, I is the initial growth value (mm) at bud burst, A the upper asymptote β the x-axis placement parameter, and κ the rate of change of the shape (Rossi et al. 2003). A weighted mean absolute cell formation rate (r, cell·day−1) was also calculated (Deslauriers et al. 2003):
Repeated mixed-effect models (MIXED procedure in SAS) evaluated the effects of defoliation treatment and irrigation regimes on defoliation (%), apical and lateral growth (mm), soil relative water content (%), and water potential (Ψpd and Ψmd, MPa). Defoliation and irrigation treatments were the fixed factors while compartment and tree (nested in compartment × defoliation treatment irrigation regime) were the random factors. The DOY effect was considered as the repetitive factor with tree as subject (nested in compartment × defoliation treatment × irrigation regime). We ran the VCIRY option (MIXED procedure in SAS) to test the distribution of the data, and we plotted the model residuals to verify their distribution.
3 Results
3.1 Phenology, defoliation, and growth
The phases of budburst proceeded similarly among the different treatments (Fig. 1, Table 1). The bud development phases varied significantly between the different dates (Wald = 513, P < 0.001, Table 1) showing a linear trend. No differences were found between the defoliation treatments and irrigation regimes, although their interaction was significant (P = 0.001, Table 1). For all treatments, buds began their development on DOY 135 and ended 4 weeks later on DOY 162–163 (Fig. 1). The transition from one stage to another took 4.66 days on average.
Spruce budworm development took approximately 25 days (4.16 days per stage) with a linear trend over time. Development was not affected by the irrigation regime, as instar development was almost complete when the treatments began (Table 1). The L5–L6 instars were able to feed on split buds (bud stage 5, exposed shoots) after DOY 160. Thus, defoliation began when the new shoots and needles started to grow, and defoliation stopped increasing when pupas were observed (Fig. 1). Afterward, defoliation varied according to the different sampled trees. Defoliation was already high at DOY 164, and it did not differ between the irrigated (37.5%) and non-irrigated saplings (39.2%) (Table 2).
Apical and lateral shoot growth had already stopped in the defoliated plants by the fifth instar stage, around the time that defoliation began (Fig. 2). From that moment onward, primary growth slowed significantly in the defoliated plants compared to the undefoliated plants (Table 3). Apical and lateral growth were affected more strongly by the defoliation treatments than by the irrigation treatments as half of the total primary growth had occurred when irrigation ceased (Tables 2 and 3, Fig. 2).
In the defoliated–irrigated saplings, radial growth slowed as a result of defoliation (Fig. 3), and this reduction was significant by the end of September (P < 0.001). The largest differences in the patterns of stem radial variation were observed between the irrigated and non-irrigated saplings (P < 0.001) with a mean radial growth 0.6 mm less in the latter. The radial growth stopped soon after the irrigation ceased (DOY 160). Minimal increase in stem radius was detected in the defoliated saplings following the water deficit period (Fig. 3). A typical downward wave was observed in the undefoliated–non-irrigated saplings with minimal growth afterward, indicative of elevated stem shrinking. However, this stem shrinking was not observed in the defoliated–non-irrigated saplings. At the end of September (DOY 273), both undefoliated–non-irrigated and defoliated–non-irrigated saplings had similar radial growths (P = 0.58).
3.2 Soil water status and water relations
We examined soil moisture and water relations by delineating three different periods based on the treatment effects: (1) the pre-stress period (DOY < 162), i.e., no visible defoliation (instar stage 4 at most) and no water deficit; (2) the stress period (DOY 163–184) beginning with the peak in defoliation and growth damage (instar stages 5 and 6) and ending at the peak of water deficit—this period also covered the lowest levels of the volumetric water content; (3) the post-stress period beginning when irrigation was resumed (DOY > 182).
In the pre-stress period, the mean soil moisture varied from 32 to 42% and showed no difference between the irrigation treatments (Table 4, Fig. 4). The plants reflected optimal water conditions, with pre-dawn (Ψpd) water potential ranging between − 0.2 and − 1.0 MPa and midday (Ψmd) water potential ranging between − 0.1 and − 1.4 MPa in both the irrigated and non-irrigated saplings having similar defoliation and irrigation treatments.
During the stress period, soil moisture decreased markedly in the non-irrigated pots after DOY 162. Minimum soil moisture was recorded in DOY 175–184 with levels < 10% to c.a. zero in the non-irrigated pots. Similarly, both Ψpd and Ψmd were significantly lower in the non-irrigated saplings relative to the irrigated saplings (P < 0.01, Table 4, Fig. 4). The water potential of non-irrigated plants reached Ψpd and Ψmd levels of − 2.5 and − 2.7 MPa, respectively. The midday water potential (Ψmd) was not significantly affected by the defoliation treatment, but a significant interaction was found for defoliation × irrigation (P < 0.05, Table 4). Differences of least squares means (LSM) revealed that the midday water potential of undefoliated–irrigated saplings (LSM Ψmd = − 1.20 MPa) was significantly less negative than all other treatment combinations, including the defoliated–irrigated saplings (LSM Ψmd = − 1.51 MPa). The non-irrigated saplings had similar Ψmd (− 1.71 and − 1.56 MPa for the undefoliated and defoliated treatments, respectively), which did not differ from the defoliated–irrigated saplings.
In the post-stress period, the soil moisture increased rapidly but only returned to levels similar to that of the irrigated pots after DOY 191, producing a significant difference during the post-stress period (P < 0.01, Table 4). After resuming irrigation, the pre-dawn water potential Ψpd increased and returned to levels similar to those observed prior to the stress period. However, after the stress period, the Ψmd of the defoliated saplings was less negative than that of the undefoliated saplings (Fig. 4).
3.3 Sapling mortality
All saplings in the undefoliated–irrigated and defoliated–irrigated treatments survived (data not shown). Mortality was observed, however, in the non-irrigated saplings after the stress period but differed between the undefoliated and defoliated plants; undefoliated–non-irrigated saplings had higher mortality rates during the first 2 weeks after resuming irrigation (0.3 dead·sampling·day−1) compared to defoliated–non-irrigated plants (0 dead·sampling·day−1) (Fig. 5). After these 2 weeks, mortality rates were similar (0.05–0.1 dead·sampling·day−1).
4 Discussion
4.1 Plant water status
Leaf water status was more affected by the amount of irrigation than defoliation in black spruce saplings exposed to spruce budworm defoliation immediately followed by a water deficit. Most previous studies investigating combined stresses have had the abiotic stress followed by a biotic stress; these studies concluded that drought stress predisposes trees to pathogen attacks (see review in Niinemets (2010)). Here, we assessed the reverse effects—biotic and then abiotic stressors—because spruce budworm outbreaks are cyclical (Morin et al. 1993). Thus, we could test the effect of drought on plant water status, growth, and mortality in trees weakened by defoliation. In contrast to the prediction for defoliation (first hypothesis), all non-irrigated saplings (defoliated or not) reached a similar water status in the nighttime (Ψpd) and daytime (Ψmd) during the stress period. Therefore, under situations of coupled defoliation and water stress, defoliation did not have a positive effect on water potential. In black spruce, significant decreases in soil water content and water potential have been reported under scenarios of water deficit (Balducci et al. 2013; Tan and Blake 1997), with leaf Ψpd fluctuating between − 2.2 and − 2.9 MPa (Balducci et al. 2013; Stewart and Bernier 1995; Zine El Abidine et al. 1994). At the end of the stress period, all non-irrigated saplings had a limited ability to take up water from the soil as Ψpd dropped when the relative water content reached zero. This placed all the saplings in a physiological state of water stress (Bernier 1993; Grossnickle and Blake 1987; Stewart and Bernier 1995).
Contradictory responses were found in other studies where the leaf Ψmd of defoliated plants was either higher (Quentin et al. 2011; Vanderklein and Reich 2000; Wiley et al. 2013) or similar (Quentin et al. 2012) to undefoliated plants. This pattern can be related to the timing of measurements. In this study, we observed two different responses of Ψmd: a detrimental effect during defoliation and the opposite pattern during the post-stress period, thus partially confirming our first hypothesis. In irrigated plants, Ψmd was significantly lower in defoliated plants relative to the undefoliated plants. This indicates a higher evaporative demand during or immediately following defoliation (Salmon et al. 2015). Eyles et al. (2013) also report a decrease in Ψmd for saplings subjected to different levels of defoliation (50% or 100% apical bud damage). We explained this lower Ψmd by the mechanical chewing action of larvae during active defoliation (i.e., Fig. 1). Budworm feeding habits damage many growing needles, resulting in a loss of turgor or even localized cavitation because of the entry of air into the damaged needles. This likely decreases the water potential. The opposite pattern was observed during the post-stress period: leaf Ψmd was less negative in the defoliated saplings than in the undefoliated saplings. These results are similar to patterns observed in Larix decidua Mill., Pinus strobus L., and Quercus velutina Lam. (Vanderklein and Reich 2000; Wiley et al. 2013). In the post-stress period, direct defoliation ceased, but the reduced leaf area of defoliated saplings led to a lower leaf transpiration surface (Schmid et al. 2017; Wiley et al. 2013). From DOY 190–230, a greater gradient of leaf Ψmd was observed in undefoliated saplings due to persistently higher growth temperatures. These lower Ψmd values could indicate higher transpiration occurred during the day and reduced the optimal water status.
4.2 Plant growth
Apical shoot and twig growth were reduced primarily by defoliation but without additive or synergistic effects from the combined stresses (second hypothesis). Although black spruce is considered as a secondary host (Hennigar et al. 2008; Pureswaran et al. 2015), the L2 instars deposited on the branch rapidly colonized the plants and began growing quickly, defoliating the growing buds and shoots when larvae reached stage 4. While the opened buds of the defoliated plants stopped growing as defoliation proceeded, the buds of non-irrigated saplings continued to grow but more slowly as the water content decreased in the pots. Expansive growth of leaves depends heavily on water availability (Tardieu et al. 2011; Tardieu et al. 2014). In the non-irrigated saplings, apical shoot and lateral twig growth were reduced by about 30% and 20%, respectively, relative to the undefoliated saplings. As the physiological water deficit began when half of the primary growth was already completed, twig growth was less affected by the water deficit.
Radial growth at the base of the stem was reduced more by water deficit than by defoliation. Cambium division in the stem and tracheid enlargement stop earlier than usual during a period of water stress (Balducci et al. 2013; Steppe et al. 2015; Zweifel et al. 2006). According to Deslauriers et al. (2016), the number of xylem cells produced by the cambium is explained more strongly by water availability than by carbon supply. Under water deficit conditions, a sink growth limitation rules over source (C) limitation (Muller et al. 2011). This could explain why no additive or synergistic effects were found in the radial growth when the stresses were combined.
At the intra-annual level, however, we observed a divergent pattern in the defoliated–non-irrigated saplings. This suggests a positive effect of defoliation on the stem water reservoir. As the soil dries due to low water availability, transpiration causes stem dehydration. As a consequence, the stem water reservoir is progressively depleted (Bréda et al. 2006; Salomón et al. 2017), such as illustrated by the pronounced reversible stem shrinking observed in our non-irrigated trees. The use of water stored within stem tissues that are closer to the sites of evaporation may buffer temporary imbalances in the soil (Goldstein et al. 1998). In the non-irrigated-defoliated saplings, surprisingly, we did not observe any reversible stem shrinking. Therefore, the amount of water withdrawn from stem storage, substantially contributing to the total daily water loss for transpiration, was refilled on a daily basis (Steppe et al. 2015), avoiding strong stem contraction under drought conditions (Giovannelli et al. 2007; Salomón et al. 2017).
4.3 Sapling mortality
In agreement with our third hypothesis, the mortality rate in the post-stress period was caused primarily by a water deficit, although only during the first 2 weeks. Afterward, the mortality rate was constant and ranged between 0.05 and 0.1 dead saplings·day−1. It is widely reported that drought is responsible for tree mortality (Allen et al. 2010; Park Williams et al. 2013). The temporal scale of drought-induced tree mortality strongly depends on the physiological mechanisms that act as thresholds. In the black spruce stem, we determined the xylem tension that induces 50% loss of conductivity (P50): − 4.26 MPa and the xylem air entry pressure (P12) of − 2.9 MPa (Balducci et al. 2015).
In non-irrigated defoliated trees, however, the mortality rate was very low for 14 days following the water stress period. Moreover, none of the non-irrigated, defoliated saplings died during the first week following the resumption of irrigation. Since no stem dehydration was observed under water-stress conditions (see previous section), we propose that drought mortality in defoliated saplings could be temporarily reduced because of more readily available internal water when transpiration resumes after the water deficit. In other words, reduced foliar biomass would consequently decrease the transpiration flux, and as such, the stem water reservoir and root absorption would be more similar to water demand during the drought event.
5 Conclusion
The defoliation and water deficit effects (alone or in combination) were highly time dependent. Our results on sapling water status and growth point to two key periods during which defoliation negatively (1) or positively (2) affects plant water relations. First (1), a more negative water balance, observed during active defoliation, could favor branches (Deslauriers et al. 2015; Salmon et al. 2015) or even tree mortality, independent of drought. We observed a large difference in twig water potential between the undefoliated (optimal) and defoliated trees (suboptimal), which reflects a negative effect of defoliation. Under a combined stress, however, the effects of water stress prevail over defoliation-related stress. Second (2), it is only after the developing instars had begun to transform into moths that the detrimental effects of defoliation became positive for tree water balance (above optimal). Then, for the remainder of the study period, the water potential of defoliated saplings became less negative—including at the peak of drought—indicating a reduced transpiration demand and therefore a reduced post-drought mortality.
Data availability
Data are available upon request to the corresponding authors.
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We thank S. Rivest for his help in collecting the data.
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This study was funded by the “Programme de soutien à la recherche, volet Soutien à des initiatives internationales de recherche et d’innovation (PSR-SIIRI),” the Ministère du Développement économique, Innovation et Exportation du Québec (MDEIE), and the Natural Sciences and Engineering Research Council of Canada (Discovery Grant of A. Deslauriers).
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Contribution of the co-authors All authors have contributed directly to the content of this work (study design, interpretation of the data, writing, and critical revision). H. Bouzidi, A. Deslauriers, and L. Balducci participated in the data analysis. J. Mackay and A. Deslauriers participated in the funding of the study.
This article is part of the topical collection on Wood formation and tree adaptation to climate
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Bouzidi, H.A., Balducci, L., Mackay, J. et al. Interactive effects of defoliation and water deficit on growth, water status, and mortality of black spruce (Picea mariana (Mill.) B.S.P.). Annals of Forest Science 76, 21 (2019). https://doi.org/10.1007/s13595-019-0809-z
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DOI: https://doi.org/10.1007/s13595-019-0809-z