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Tree growth is more limited by drought in rear-edge forests most of the times

Abstract

Background

Equatorward, rear-edge tree populations are natural monitors to estimate species vulnerability to climate change. According to biogeographical theory, exposition to drought events increases with increasing aridity towards the equator and the growth of southern tree populations will be more vulnerable to drought than in central populations. However, the ecological and biogeographical margins can mismatch due to the impact of ecological factors (topography, soils) or tree-species acclimation that can blur large-scale geographical imprints in trees responses to drought making northern populations more drought limited.

Methods

We tested these ideas in six tree species, three angiosperms (Fagus sylvatica, Quercus robur, Quercus petraea) and three gymnosperms (Abies alba, Pinus sylvestris and Pinus uncinata) by comparing rear-edge tree populations subjected to different degrees of aridity. We used dendrochronology to compare the radial-growth patterns of these species in northern, intermediate, and southern tree populations at the continental rear edge.

Results and conclusions

We found marked variations in growth variability between species with coherent patterns of stronger drought signals in the tree-ring series of the southern populations of F. sylvatica, P. sylvestris, and A. alba. This was also observed in species from cool-wet sites (P. uncinata and Q. robur), despite their limited responsiveness to drought. However, in the case of Q. petraea the intermediate population showed the strongest relationship to drought. For drought-sensitive species as F. sylvatica and P. sylvestris, southern populations presented more variable growth which was enhanced by cool-wet conditions from late spring to summer. We found a trend of enhanced vulnerability to drought in these two species. The response of tree growth to drought has a marked biogeographical component characterized by increased drought sensitivity in southern populations even within the species distribution rear edge. Nevertheless, the relationship between tree growth and drought varied between species suggesting that biogeographical and ecological limits do not always overlap as in the case of Q. petraea. In widespread species showing enhanced vulnerability to drought, as F. sylvatica and P. sylvestris, increased vulnerability to climate warming in their rear edges is forecasted. Therefore, we encourage the monitoring and conservation of such marginal tree populations.

Background

Climate warming impacts the productivity and functioning of forest ecosystems worldwide with consequences on the services they provide for human wellbeing (Anderegg et al. 2013; Hartmann et al. 2018). Recent warming trends have accelerated tree growth in temperature-limited forests (Serreze and Barry 2011), while they have caused widespread drought-related mortality in most biomes (Allen et al. 2010; Choat et al. 2018). Drought is becoming a major driver of tree growth globally (Babst et al. 2019) revealing a temporal instability in its impacts on forests over the last decades (Peltier and Ogle 2020; Wilmking et al. 2020). Along with this, the role of drought in determining tree growth is also spatially variable (Anderegg et al. 2015), with tree populations located near the equatorward distribution limit being more vulnerable to drought (e.g., Sánchez-Salguero et al. 2017; but see Cavin and Jump 2017). Therefore, when trees are not adapted to harshening environmental conditions, widespread dieback and mortality occur leading to the range contraction of the species distribution limit (Anderegg and HilleRisLambers 2016; Anderegg et al. 2019). However, recent studies have demonstrated that populations on the equatorward limit display adaptations to drought (Dorado-Liñán et al. 2019; Muffler et al. 2020) and that ecological factors can blur or override geographical patterns of greater vulnerability to drought as latitude decreases (Vilà-Cabrera and Jump 2019). In other words, marginality has different components (i.e., geographical, ecological, and genetic) and geographical range margins do not always dictate population performance (Vilà-Cabrera et al. 2019).

According to biogeographical expectations, as climate becomes warmer and drier, rear-edge tree populations of temperate or mountain species may become vulnerable to drought and show productivity and growth reductions preceding dieback events (Camarero et al. 2017). Several Eurasian tree species reach their southern distribution limit in Spain (de Vries et al. 2015), where drought-limitations on species performance and vitality have been already reported and are expected to increase (Lindner et al. 2010; Camarero et al. 2015). Even within Spain, southern or low altitudinal forests of some species such as Scots pine can be more vulnerable to drought than forests located at higher elevations or latitudes in the rear edge (Marqués et al. 2016; Serra-Maluquer et al. 2019). These reasons make some Spanish forests a valuable proxy of drought impacts on European rear-edge tree populations.

Tree populations of species such as silver fir (Abies alba Mill.) present lower growth rates in some Pre-Pyrenean sites of northern Spain than in other wetter regions of Central Europe (Gazol et al. 2015). Similarly, Scots Pine (Pinus sylvestris L.) and European beech (Fagus sylvatica L.) populations show greater sensitivity to drought in dry regions of Spain than in northern or wetter areas (Serra-Maluquer et al. 2019; Bose et al. 2020). However, local ecological conditions can affect the growth responsiveness of these species and populations to climate making rear-edge populations less vulnerable to drought than their northern counterparts (Dorado-Liñán et al. 2019). This contingency on site conditions has been shown in silver fir forests in the Spanish Pyrenees (Camarero et al. 2011), Scots pine in southern Spain (Herrero et al. 2013), or European beech forests in north eastern Spain (Vilà-Cabrera and Jump 2019). Thus, the growth response to drought of rear-edge tree populations can deviate from biogeographical predictions due to the influence of local ecological factors or genetic adaptations to drought (Vilà-Cabrera et al. 2019).

Several factors can contribute to the strong variability in tree growth response to drought between populations decoupling biogeographical and ecological margins (Vilà-Cabrera et al. 2019). Thus, population performance may depend on the interaction between different ecological factors, climate-competition trade-offs (e.g., Jump et al. 2017; Anderegg and HilleRisLambers 2019), or phenotypic plasticity and genetic variability (Hampe 2004; Valladares et al. 2015). For example, Herrero et al. (2013) and Marqués et al. (2016) found that Scots pine rear-edge populations were vulnerable to drought at low elevations, where the evapotranspiration demand increases, while at high elevations growth was less constrained by water shortage. Altitudinal variations can decouple local microclimate conditions from regional macroclimatic patterns affecting tree growth response to climate but also competitive interactions (Anderegg and HilleRisLambers 2019). That is, within the rear edge those populations at lower elevations were more vulnerable to drought. Muffler et al. (2020) found that European beech rear-edge populations did not respond to drought as compared to central populations and attributed this effect to the cooling effects of local fog events or high elevation mitigating drought impacts (see also Rozas et al. 2015; Barbeta et al. 2019). In such situations, plant-soil interactions, and the capacity of trees to compete within their neighbourhood may play an important role in enhancing or limiting drought impacts (Leuschner 2020). Marqués et al. (2018) found that the response of growth of Scots pine to drought in rear-edge populations was modulated by stand density, pointing to the impact of past forest management on recent growth vulnerability, as has been found for other species (Camarero et al. 2011; Pérez-Luque et al. 2020). Rubio-Cuadrado et al. (2020) found competition due to the cessation of traditional management as the main driver of growth in a rear edge, mixed broadleaved forest. These variations between populations can be even more apparent when different species are considered given the contrasted sensitivity to drought between drought-sensitive species such as European beech and Scots pine or tolerant species such as pedunculate oak (Quercus robur L.) (Vitasse et al. 2019). These results question the universal validity of the hypothesis of a greater vulnerability of tree growth to drought near their rear edge (Vilà-Cabrera et al. 2019; Muffler et al. 2020). Further, they indicate that regional studies over geographically and climatically contrasting tree populations are required to decipher if rear-edge populations are the most vulnerable to drought across a species distribution range. In this sense, it is expected that if tree populations are climatically different or geographically distant, rear-edge populations will be consistently more constrained by drought events as they face harsher environmental conditions (Anderegg and HilleRisLambers 2019). However, genetic adaptations can make rear-edge populations less vulnerable to drought (Vilà-Cabrera et al. 2019).

Here we tested the hypothesis that even within the rear edge those tree populations located in southern sites are subjected to drier conditions and thus display greater growth vulnerability to drought than populations located in intermediate or northern sites. Alternatively, tree populations of a species in intermediate and northern sites have not experienced an equally strong selection for drought resistance because they are less adapted to experience severe drought than those towards the species’ moisture-limited range margin. Therefore, one would expect southern, equatorward populations would be less impacted by drought of a given severity than would be poleward populations. To test these ideas, we selected six species widely distributed in Europe that found their rear-edge distribution limit in Spain. The species were three gymnosperms (Pinus sylvestris, Abies alba and Pinus uncinata Ram.) and three angiosperms (Fagus sylvatica, Quercus robur and Quercus petraea (Mattuschka) Liebl.) forming rear-edge populations in north-eastern Spain (Fig. 1). For each species in each site, we used dendrochronology to reconstruct past radial-growth patterns by accurately dating tree-ring width records. We expected: (i) higher growth variability, and lower mean growth, in southern as compared to intermediate and northern populations; (ii) stronger coupling between growth variability and drought stress in southern populations; and (iii) an increasing growth sensitivity to drought in southern populations during the last decades.

Fig. 1
figure1

Distribution maps of the studied species across Europe. For each species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea) the green area represents the distribution of the species in Europe. The dots in the graph indicate the location of the northern (blue triangle), intermediate (black circle) and southern or rear-edge (red squares)

Methods

Studied sites and tree species

We studied six common European tree species (three Pinaceae and three Fagaceae) widely distributed in Europe (Figs. 1 and S1) namely: P. uncinata, A. alba, P. sylvestris, F. sylvatica, Q. robur and Q. petraea. Mountain pine (P. uncinata) is a species distributed in central and southwestern European mountains finding its southern distribution limit in the Iberian System, eastern Spain (Camarero et al. 1998). Silver fir (A. alba) is an economically profitable species widely distributed in central and southwestern Europe with rear-edge populations in north-eastern Spain mountains as the Pre-Pyrenees (Gazol et al. 2015). Scots pine (P. sylvestris) and European beech (F. sylvatica) also find their south-western distribution limits in Spain where drought-induced dieback has been reported for both species (Camarero et al. 2015, 2017). Pedunculate (Q. robur) and sessile (Q. petraea) oaks are widely distributed from northern to southern Europe and they form pure or mixed stands, where they can hybridize, in wet sites (e.g. valley bottoms) or mountain sites of north-eastern Spain (Caudullo et al. 2017).

Field sampling and laboratory work

Three sites with contrasting climatic conditions, and always including a drier rear-edge site, were selected for each species (Table 1; Figs. 1 and 2). In each species, the driest, rear-edge site presented lower precipitation than the other two sites (Figs. 2 and S2). We quantified radial growth because this is a reliable proxy of tree vigour changes in response to drought (Dobbertin 2005). We sampled at least 15 dominant trees for each species and site. All sites form mixed stands excepting the pure Betato and Poyales F. sylvatica sites, and the Tessó del Son P. uncinata site situated near the alpine treeline. The diameter at breast height of each tree (Dbh) was measured at 1.3 m using a metric tape. Two cores (see Table 1) were extracted per tree at 1.3 m using 5-mm increment borers, and perpendicular to the main stem and the slope. Then, cores were air-dried, glued, and polished using a series of sand-paper grits until tree-ring boundaries were clearly visible. These samples were visually cross-dated and measured to the nearest 0.01 mm using a LINTAB measuring device (Rinntech, Heidelberg, Germany). Cross-dating accuracy was checked by using the software COFECHA (Holmes 1983).

Table 1 Main characteristics of each site and mean tree-ring width (and standard deviation) and dendrochronological statistics for the period 1950–2000
Fig. 2
figure2

Representation of each studied species in the climatic space (Worldclim data; Fick and Hijmans 2017) The green dots represent values of mean annual temperature and total precipitation where the species are present in Europe (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). Climate data was downloaded for the distribution of the species in Europe (http://www.euforgen.org/species/). Grey dots represent values of temperature and precipitation where the species are not found in Europe. The dots in the graph indicate the location of the tree populations of each species

Mean growth series or chronologies were created for each site and species by detrending tree-ring width measures (Fritts 1976). Individual tree-ring width series were detrended using a cubic smoothing spline with a 50% frequency response cut-off at 30 years (Cook and Peters 1981). The ring width index (RWI) for each series was obtained by dividing the observed and fitted tree-ring width values. Pre-whitened RWI series were calculated by removing temporal autocorrelation using autoregressive models. The resulting standardized, pre-whitened individuals RWI series were averaged into mean site chronologies for each species using bi-weight robust means.

To characterize the species’ chronologies of each site for the common period 1950–2000 we calculated the following tree-ring statistics: mean, standard deviation and coefficient of variation (CV) of tree-ring width; mean correlation between indexed, individual series (rbar); and the Expressed Population Signal (EPS), a measure of replication and internal coherence of each chronology (Fritts 1976). The Dunnett’s modified Tukey-Kramer pairwise multiple comparison test (Dunnett 1980) was used to compare tree-ring width of individuals between southern, intermediate and northern populations for each species.

Climatic and distribution data

For each species, distribution maps were downloaded from the EUFORGEN website (http://www.euforgen.org/species/; de Vries et al. 2015) and they were completed using recent distribution data across Europe (Caudullo et al. 2017). The European distribution maps of each species were compared with climate data to describe the climatic niche of each species. To this end, maps of mean annual temperature (MAT) and mean annual precipitation (MAP) were downloaded from the WorldClim database (https://www.worldclim.org/; Fick and Hijmans 2017). These maps represent averages over the period 1970–2000 and show global patterns in climate. Then, we plotted each site in a MAT vs. MAP graph considering the European distribution area of the study species, i.e. between 12° W–60° E, and 32°–72° N (Fig. 2).

To quantify climate-growth relationships, monthly mean temperature and precipitation data from the E-OBS database v. 20.0e (Haylock et al. 2008) were downloaded at 2.5° resolution for the period 1950–2018 using the Climate Explorer webpage (https://climexp.knmi.nl/start.cgi). To quantify drought impact, we used the Standardized Evapotranspiration Precipitation Index (SPEI; Vicente-Serrano et al. 2010). The SPEI is a multi-scalar index that quantifies drought intensity based on the difference between precipitation and the atmospheric evaporative demand for different periods, with negative values indicating water scarcity. We used 1–48 month SPEI timescales for the period 1962–2016 for the sampled forest sites from a high spatial resolution gridded dataset for Spain based on quality controlled and homogenised meteorological series (Vicente-Serrano et al. 2017).

Statistical analyses

The relationships between tree growth (RWI) and monthly mean temperature and precipitation (deviations with respect to the mean temperature and precipitation values at a site) were quantified for the best-replicated period 1950–2006 using bootstrapped Pearson correlations (Meko et al. 2011). These analyses were performed from September in the year before the tree-ring was formed to September of the year of tree-ring formation (hydrological year). Moving correlation functions were applied to assess the dynamic nature of the relationships between RWI and relevant climate variables (precipitation, temperature and July SPEI) and considering 30-year moving windows. We used July SPEI as tree growth for many tree species in north-eastern Spain, where most of our studied populations are located, have been found to respond to drought from June up to August (Pasho et al. 2011). Analyses were performed using the “dplR” (Bunn 2008), the “treeclim” (Zang and Biondi 2015), and the “visreg” libraries (Breheny and Burchett 2017) of the R statistical software (R Core Team 2020).

Results

The “climatic space” plot allowed to characterize the climate conditions of geographically southern populations from the other species sites (Fig. 2). This differentiation was clear in the case of A. alba, and less evident in P. sylvestris, and Q. robur. In P. uncinata and F. sylvatica intermediate and southern sites shared similar annual climatic conditions (Fig. S2). Lastly, in Q. petraea the warmest and driest conditions (highest MAT and lowest MAP) were observed in the intermediate site, and not in the southern site.

We found marked growth differences across populations for some species (Table 1). Lower growth rates in the southern sites were more evident for drought-sensitive species such as F. sylvatica and P. sylvestris (Table 1; Fig. S3). Growth rates of A. alba individuals were higher in the intermediate and southern sites than in the northern site, and the largest growth rates in the case of Q. petraea were found in the southern site (Table 1; Fig. S3). Growth variability varied considerably between species. Tree species inhabiting cold and wet sites (A. alba, Q. robur), but not P. uncinata, displayed lower growth variability (Fig. 3 and Table 1) than P. sylvestris and F. sylvatica. Q. petraea was the only exception in which growth variability was stronger in the central than in the rear-edge site (Fig. 3). In this respect, the average correlation between series (rbar) and the coefficient of variation in TRW were higher in its intermediate site than in the other two populations (Table 1). This result contrasts with species such as P. sylvestris and A. alba that showed the highest rbar values but either higher or lower growth variability in their respective southern sites.

Fig. 3
figure3

Mean series of ring-width indices (RWI) of the six species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea) studied in the northern (blue), intermediate (black) and southern (brown) tree populations for the period 1950–2006

The relationship between growth and climate displayed different patterns between species and sites (Fig. 4). In the case of A. alba and Q. robur we found a greater dependency of growth on summer precipitation in southern sites than in the other two populations. In A. alba and P. sylvestris warmer summer temperatures negatively impacted tree growth in southern sites (Fig. 4). This negative correlation was also observed in the northern P. sylvestris site, and particularly in the intermediate Q. petraea site which depended on prior-winter and spring precipitation. This dependency on the amount of rainfall received before or early in the growing season was also observed in southern F. sylvatica and P. sylvestris sites. The growth of P. uncinata and A. alba in southern populations, and P. uncinata and P. sylvestris in intermediate populations, was negatively related to temperature of September in the year prior to tree-ring formation. In the A. alba and F. sylvatica southern populations, prior-winter temperatures were positively correlated with growth.

Fig. 4
figure4

Correlations (Pearson coefficients) calculated between mean site series of ring-width indices and precipitation (left) and temperature (right) deviations. Dots indicate significant coefficients according to bootstrapping tests. Colours represent: northern (blue), intermediate (black), and southern (brown) populations of the six tree species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea)

For all species except Q. robur, the negative impact of summer temperatures on growth has increased over the last decades (Figs. 5 and S4). This was evident at the southern sites of some species (P. uncinata, A. alba, F. sylvatica), whereas in others it was observed in all sites (P. sylvestris). In Q. petraea, growth decreased in response to increasingly warmer summer conditions in the intermediate site. The temporal evolution of the correlation between growth and precipitation was less clear, but spring precipitation gained importance in the intermediate sites of F. sylvatica, P. sylvestris and Q. petraea (Figs. 5 and S5).

Fig. 5
figure5

Moving window correlations calculated between mean site series of ring-width indices and monthly temperature (T.) and precipitation (P.) data from May to August. Moving correlations were obtained for 30-year intervals shifted by one year and the middle year of the interval is shown in x axes for each species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). The colour scale (right side) shows the Pearson correlation coefficients

Unexpectedly, the strongest correlation between the SPEI and growth was found for Q. petraea in the intermediate population (Fig. 6). According to our expectations, we found a stronger correlation between SPEI and growth in the southern than in the other two sites for three out of the six species studied. This was the case of the drought-sensitive species F. sylvatica and P. sylvestris, and A. alba. Differences between populations were less evident in Q. robur and P. uncinata. The temporal evolution of the correlation between growth and SPEI showed that in the southern P. sylvestris population there was a marked increase in the vulnerability of growth to long droughts (12- to 18-month SPEI values; Figs. 7 and S6). In the rear-edge A. alba site, there was a persistence influence of short- and mid-term droughts on growth, and, again, this influence was more evident in the intermediate Q. petraea site.

Fig. 6
figure6

Correlations between mean site series of ring-width indices and the SPEI drought index calculated at 1- to 48-month temporal resolution (x axes) and from January to December (y axes). Northern, intermediate and southern populations are represented for the six species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). The colour scale shows the Pearson correlations

Fig. 7
figure7

Moving window correlations calculated by relating mean site series of ring-width indices and the July SPEI drought index at 1-, 3-, 6-, 9-, 12-, 15-, 18-, and 21-month temporal resolutions (y axes). Moving correlations were obtained for 30-year intervals shifted by 1 year and the middle year of the interval is shown in x axes for each species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). The colour scale shows the Pearson correlation coefficients

Discussion

We found that drought is a major factor limiting tree growth for most of the studied species and sites near the rear edge of their distribution range. According to our expectations, drought-sensitivity increased towards the equatorial border of the species distribution range for most of the species studied. That is, populations located in southern sites were in general more vulnerable to drought than populations located in intermediate or northern sites. In accordance, growth sensitivity to drought varied markedly among tree populations within each species (Fig. 6). For drought-sensitive species as Scots pine, the results showed that tree growth is more limited by drought in the southern site (Figs. 6 and 7). This negative impact has been exacerbated due to the increase in growing-season temperatures, and probably evapotranspiration rates, over the past decades (Vicente-Serrano et al. 2015). Our findings evidence the drought vulnerability of tree species such as silver fir, European beech and Scots pine (see also Vitasse et al. 2019; Bose et al. 2020). There is a notable exception in the case of sessile oak, a drought-sensitive species (Aranda et al. 2000), whose growth is more impacted by drought in intermediate than in southern populations, pointing to the importance of other ecological or local factors modulating tree growth sensitivity to drought (Cavin and Jump 2017). The intermediate and southern sites are separated by 120 km (Fig. S1) and the highest responsiveness to drought was observed in the climatic limit or most xeric site (Monsomero). This site was also formerly exploited as a coppice forest about 60 years ago (JJ Camarero, pers. observ.), which could have exacerbated its current sensitivity to drought due to competition among stems of the same individual (Corcuera et al. 2006; Pérez-Luque et al. 2020). The case of Q. petraea shows that other ecological factors besides climate can constrain the growth responsiveness to drought and can modify latitudinal patterns of drought sensitivity. Recent studies have pointed out that discrepancies between micro and macroclimate conditions, interactions between ecological factors, species interactions and genetic adaptations can play an important role in driving growth response to drought, despite biogeographical differences being important (Vilà-Cabrera et al. 2019). The lack of reliable information on local conditions only allows us to speculate on the factors that make intermediate and northern populations less vulnerable to drought than southern populations in some cases. Solving this question will require a more holistic approach to understand the interactions between geographical, ecological and historical factors. Overall, the presented results enlighten that rear-edge populations are, most of the times, reliable monitors of the long-term response of drought-sensitive tree species to climate change and show that most tree populations are more vulnerable to drought southwards.

The six studied species are widely distributed in Europe, excepting the mountain pine (P. uncinata), and find their southwestern distribution limit in Spain. However, as occurs with the geographical and climatic extents of their distribution ranges (Figs. 1 and 2), the drought sensitivity of each species varies notably (Fig. 6). In the mountain pine we found that its growth in the region is controlled by late-spring and early-summer temperatures (Fig. 4a), in line with previous studies (e.g., Camarero et al. 1998; Tardif et al. 2003), but we also found a low drought susceptibility in the rear edge which could be explained by ontogenic or genetic differences (Galván et al. 2014; González-Díaz et al. 2020). This contrast with what was found for Scots pine, a widely distributed drought-sensitive species (Dorado-Liñán et al. 2019; Bose et al. 2020). Despite growth positively responded to summer precipitation and negatively to summer temperature in all studied Scots pine sites, the response occurred earlier (in the case of temperature) and was more intense in the southern site. In this site, an acute dieback episode started after the severe 2012 drought and resulted in the death of many Scots pine trees (Camarero et al. 2015; Gazol et al. 2018). The significantly lower growth rates and the larger vulnerability of tree populations to drought and warmer conditions in this region as compared to other populations, together with the observed lack of recruitment of Scots pine, point towards major compositional changes and the replacement of that species by more drought-tolerant oak and juniper species (Gazol et al. 2018).

Our results also highlighted the drought sensitivity of European beech in line with previous research (Serra-Maluquer et al. 2019; Vitasse et al. 2019; Wilmking et al. 2020). Both, Scots pine and European beech have been recognized as drought-sensitive species in terms of growth loss (Dorado-Liñán et al. 2019) despite their marked differences in functional traits including stomatal control in response to drought (Klein 2014). Scots pine is a species with a tight stomata regulation (Klein 2014), and thus very vulnerable to early summer droughts, which is corroborated in our study by the earlier sensitivity of growth to precipitation and SPEI in the southern site (Figs. 4 and 6). It has been found that the stomatal control over water loss and the leaf area / sapwood area ratio change along gradients of dryness in Scots pine (Martínez-Vilalta et al. 2009), which can also explain the lower growth rates found in the southern site. The sensitivity of European beech to drought increased also notably in the southern site, but no clear changes in temperature-growth couplings were found in this species (Fig. 4). European beech presents large geographical differences in drought-response across its distribution area since southern populations are located in mountain areas, which allow mitigating Mediterranean drought stress, and present local adaptations related to leaf phenology (Peaucelle et al. 2019; Vilà-Cabrera et al. 2019; Wilmking et al. 2020; Leuschner 2020). However, we found that the growth rates were lower and the vulnerability of European beech growth to drought was stronger in the southern as compared to the other two populations (Fig. 6), suggesting that the tightest responses to drought occur in the driest site (Fig. 2), and pointing to the importance of geographical differences in climate as drivers of European beech growth (Dorado-Liñán et al. 2019).

Special attention should be paid to silver fir, a species that has been found to be resistant and resilient to spring droughts (Vitasse et al. 2019), but that has showed drought-induced dieback in some Spanish Pyrenean populations over the last decades (e.g., Camarero et al. 2011; Gazol et al. 2015, 2020). The large difference in growth rates found between the northern and the other two populations can be explained by the matureness of the old-growth Gamueta site (Molina-Valero et al. 2021). Thus, site conditions modulated growth rates but not the vulnerability to drought, which increased in the southern sites. Silver fir displayed larger sensitivity of tree growth to drought in the southern site, in line with the observed vulnerability of the species to drought in the Pyrenees (Camarero et al. 2011). In central Europe, silver fir is one of the most productive tree species (Vitasse et al. 2019). However, this contrasts with the observed growth reductions and loss of vitality observed in some Pyrenean sites (Gazol et al. 2015). In this region, low-altitude forests are suffering exacerbated growth sensitivity to drought and warmer conditions in comparison with other colder sites located at higher elevations. The prevalence of the species in rear-edge sites is extremely contingent on sufficient precipitation during the summer months (Fig. 4), but also on the existence of a positive water balance in the year before tree-ring formation (Fig. 6) which depends on summer temperatures (Vicente-Serrano et al. 2015). Over the last decades, the dependency of silver fir growth on summer temperature has increased (Fig. 5) suggesting that the occurrence of hotter summers as a consequence of climate change may negatively impact the species rear-edge (Sánchez-Salguero et al. 2017). We cannot obviate the fact that Iberian populations of silver fir are genetically differentiated from core populations situated in Central Europe (Gazol et al. 2015).

Pedunculate oak (Q. robur) showed no clear responses to drought at the rear edge as it can be expected for this drought-tolerant species (Vitasse et al. 2019). Climate-growth correlations showed that growth depended on wet conditions during the growing season, with a negative signal of March temperatures in the southern site. This signal can be due to a shift in the use of stored carbohydrates allowing an earlier expenditure and reducing its availability to produce new leaves and earlywood vessels, thus decreasing hydraulic conductivity (Alla and Camarero 2012). The response of pedunculate oak growth to precipitation during summer (Fig. 4) is in line with the response of the species to drought in nearby sites (Rozas 2001; Granda et al. 2017).

The response of pedunculate oak to drought contrasts with the response of sessile oak (Q. petraea) that showed a marked reaction of growth to temperature, precipitation, and drought (Figs. 4, 5 and 6), particularly in the intermediate site. Wet-warm prior winter and cool-wet spring-summer conditions improved its growth in the drought-sensitive, intermediate site. This represents the only example in which we found a greater vulnerability of tree growth to drought in a site different from the geographical rear edge (i.e., southernmost site). Previous studies have found that site-specific conditions can alter broad biogeographical patterns resulting in mismatches between the geographical and the ecological rear edges for oak forests (Pérez-Luque et al. 2020). In this respect, the rear-edge population (Valdemeca) is located at a relatively high elevation (Table 1) which can milder climate conditions thus reducing negative drought impacts (Herrero et al. 2013). Further, it is a mixed forest, composed of scattered stands with Scots pine, which could reduce the evaporative demand of oak canopies thus modulating the sensitivity of trees to drought (Rubio-Cuadrado et al. 2020). In other words, altitudinal changes decouple micro- from the macroclimate conditions thus modulating the vulnerability of tree growth to drought.

Finally, the distributions of many tree species are out of equilibrium with climate at their range margins (Talluto et al. 2007). The high longevity and limited dispersal ability of trees explain their extinction debts near the warmer, equatorward margins of their distribution ranges. Thus, rear-edge tree populations could persist under unsuitable climate conditions despite of increasing climate-distribution disequilibrium (Svenning and Sandel 2013). We show that tree-ring data are suitable monitors of rapid forest responses to climate and drought and could complement other variables (e.g., recruitment and mortality rates). Since tree species rear edges are predicted to experience contraction in response to climate warming (Talluto et al. 2007), conservation and management strategies could use retrospective growth assessments to quantify how trees respond to climate warming and increasing drought stress. This would be a first step towards accounting for lags between climate change, tree performance and distribution shifts.

Conclusions

Our findings demonstrate that the growth of major European tree species is constrained by drought in the rear edge, but genetic adaptations, ecological interactions and discrepancies between micro- and macroclimate conditions can alter the expected increase in aridity as we move southwards. We studied representative Pinaceae and Fagaceae species and found that they presented greater growth sensitivity to drought in southern than intermediate or northern sites within the rear edge. This was the case of Scots pine, European beech and silver fir. Given the great sensitivity to drought of some of the tree species studied in the rear-edge of their distribution and the expected increase in aridity as climate keeps warming, monitoring and conserving such populations is a fundamental tool to understand their resilience capacity. Dendrochronology provides tools to identify vulnerable populations based on their long-term responsiveness to drought. However, deciphering whether increased drought responsiveness results in enhanced forest vulnerability, including increased dieback and tree mortality rate, requires a more holistic approach. We combined dendrochronology with biogeography, but we lacked reliable information on the historical and ecological characteristics of each site allowing us to draw strong conclusions on why some intermediate or northern sites are equally or even more vulnerable to drought than their southern counterparts. Further studies will be improved by a better characterization of each site in terms of local features and potential genetic adaptations.

Availability of data and materials

The datasets used and/or analysed during the current study are available from the corresponding author on reasonable request.

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Acknowledgements

We thank the logistical support of Government Aragón Forest Service and the help for tree sampling of Rubén Camarero Jiménez and David Cuesta Redondo at Poyales and Valdemeca sites, respectively.

Funding

We acknowledge funding by project RTI2018–096884-B-C31 (Spanish Ministry of Science). G. S-B. is supported by a Spanish Ministry of Economy, Industry, and Competitiveness Postdoctoral grant (FJCI 2016–30121; FEDER funds).

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JJC designed the study and developed the main hypotheses, GSB, JJC, SMVS collected and prepared the data, AG analyzed the data and drafted the manuscript. All authors commented preliminary versions of the manuscript and contributed to improve the final version. The author(s) read and approved the final manuscript.

Corresponding author

Correspondence to J. Julio Camarero.

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The authors declare that they have no competing interests.

Supplementary Information

Additional file 1: Figure S1.

Latitude of the studied sites showing different symbols which correspond to poleward or northern (blue triangles), intermediate (black circles) and equatorward or southern (red squares) sites. Figure S2. Temperature and precipitation trends of the six species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea) studied in the northern (blue lines and symbols), intermediate (black lines and symbols) and southern (brown lines and symbols) tree populations for the period 1950–2006. Figure S3. Mean tree-ring width series of the six species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea) studied in the northern (blue lines), intermediate (black lines) and southern or rear-edge (brown lines) populations considering the period 1900–2018. Figure S4. Significance of the moving window correlations calculated between mean site series of ring-width indices of north, intermediate and south tree populations and monthly temperature data from previous September to September in the year of tree-ring formation. Previous and current months are abbreviated by lower- and upper-case letters, respectively. Moving correlations were obtained for 30-year intervals shifted by one year and the middle year of the interval is shown in x axes for each species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). The colour scale shows the significance (p < 0.05) of the Pearson correlation coefficients (blue, significant negative values; red, significant positive values). Figure S5. Significance of the moving window correlations calculated between mean site series of ring-width indices of north, intermediate and south tree populations and monthly precipitation data from previous September to September in the year of tree-ring formation. Moving correlations were obtained for 30-year intervals shifted by one year and the middle year of the interval is shown in x axes for each species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). The colour scale shows the significance (p < 0.05) of the Pearson correlation coefficients (blue, significant negative values; red, significant positive values). Figure S6. Significance of the moving window correlations calculated between mean site series of ring-width indices of north, intermediate and south tree populations and the June SPEI drought index at 1-, 3-, 6-, 9-, 12-, 15-, 18-, and 21-month temporal resolutions (y axes). Moving correlations were obtained for 30-year intervals shifted by one year and the middle year of the interval is shown in x axes for each species (a, Pinus uncinata; b, Abies alba; c, Fagus sylvatica; d, Pinus sylvestris; e, Quercus robur; f, Quercus petraea). The colour scale shows the significance (p < 0.05) of the Pearson correlation coefficients (red, significant positive values).

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Camarero, J.J., Gazol, A., Sangüesa-Barreda, G. et al. Tree growth is more limited by drought in rear-edge forests most of the times. For. Ecosyst. 8, 25 (2021). https://doi.org/10.1186/s40663-021-00303-1

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Keywords

  • Climate change
  • Dendroecology
  • Latitudinal gradient
  • Mediterranean forests
  • Standardized evapotranspiration precipitation index (SPEI)