Article

Sessile oak forest plant community changes on the NE Iberian Peninsula over recent decades

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Abstract

Aims Our aims were 3-fold: (i) to determine whether global change has altered the composition and structure of the plant community found in the sessile oak forests on the NE Iberian Peninsula over the last decades, (ii) to establish whether the decline in forest exploitation activities that has taken place since the mid-20th century has had any effect on the forests and (iii) to ascertain whether there is any evidence of impact from climate warming. Methods We assess changes in the plant community by comparing a current survey of sessile oak forest with a historical data set obtained from previous regional studies dating from 1962 to 1977. We analyse the regional changes in the community in terms of biodiversity variables, species composition and plant traits. Furthermore, plants traits such as plant life forms and chorological groups are used to discern any effects from land-use changes and climate warming on the plant community. Important Findings There has been a loss of diversity in the community and, in the hottest region, there is also a loss of species richness. The composition of the community suggests that, although significant changes have taken place over recent decades, these changes differ between regions as a result of the low impact global change has had in the western regions. For instance, while the tree canopy cover in the western sessile oak forests remains stable, the eastern sessile oak forests are still recovering from the former exploitation that led to a loss of their rich and abundant herbaceous stratum. In fact, the recovery process in the Catalan Pre-Coastal Range has constituted an increase in the Euro-Siberian plants typical to this community. Moreover, in the eastern forests, there is evidence that climate warming has impacted the thermophilization of the sessile oak forests found on the Coastal Range.

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... The warm conditions on the NE Iberian Peninsula are increasing due to climate change (Martín Vide et al., 2016;Peñuelas et al., 2016), which, in turn, represents a dire threat to the conservation of the sessile oak forest ; for example, these conditions can change the species composition of the community (Bou & Vilar, 2019a). The preservation of these forests at their xeric limit is very important because they are better adapted than the northern forests to these dry and warm conditions (Mátyás, 2010). ...
... Moreover, these changes are ongoing because chestnut plantations are currently being replaced with stands of Douglas fir (Pseudotsuga menziessi (Mitb.) Franco) (Broncano et al., 2005;de Ribot Porta, 2016), an invasive plant that has been reported in sessile oak forests , 2019a. Although the exploitation of sessile oak forests has decreased, there are still a few cases of intensive activity that are causing a number of severe impacts . ...
... To evaluate the current conservation status of the sessile oak forests, we carried out 34 inventories of the plant community using a modified (Bou & Vilar, 2019a) Braun-Blanquet method (Braun-Blanquet, 1964) to measure only the abundance in 100 m 2 plots. Using the available habitat cartography of Catalonia (Vigo et al., 2005), we determined the distribution of the sessile oak forest in the study area, where we randomly distributed the plots. ...
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The sessile oak forests found on the northeast of the Iberian Peninsula are ascribed to the Lathyro-Quercetum petraeae association and play a key role in understanding the ecology of this habitat, as this region represents its xeric limit. For this reason, we analysed the biodiversity patterns and current conservation status of the sessile oak forests in the region. To do so, we collected Braun-Blanquet inventories of 34 plots randomly distributed throughout the sessile oak forests. The results showed a relationship between the climatic conditions and the biodiversity variables. While the richness of the community increased with decreasing temperatures, the characteristic species found within the community decreased at these same temperatures. This result was due to the presence of most companion species in the cool zones at high elevations. Sessile oaks are found close to other communities, such as silver birches and Scot pine forests. On the other hand, in the warm areas at low elevations, the sessile oak community was more established, with plants typical of this type of forest. These slightly warmer zones with sessile oaks are very important in terms of conservation and more vulnerable to climate change and the thermophilization of the community, as has been studied. As such, protecting and managing these forests is key to conserving this community. Nevertheless, as current protection measures do not safeguard most of these forests, it is essential to define a conservation strategy to preserve them. Using the conservation status, we have established criteria to improve the conservation strategy for sessile oak forest on the NE Iberian Peninsula.
... A l'Alta Garrotxa aquest patró és més evident, ja que també s'ha trobat la tendència a la pèrdua de riquesa relativa d'hemicriptòfits. Aquest patró seria comú amb els resultats observats a Catalunya, fora de la regió pirenaica (Bou and Vilar, 2019). El procés s'ha d' entendre com la recuperació del bosc davant de l'activitat humana, que un cop s'ha reduit ha permès el desenvolupament de la vegetació llenyosa que es veia limitada per la constant explotació. ...
... El procés s'ha d' entendre com la recuperació del bosc davant de l'activitat humana, que un cop s'ha reduit ha permès el desenvolupament de la vegetació llenyosa que es veia limitada per la constant explotació. Tanmateix, aquest fenomen força evident a les rouredes orientals, no ho és pas a les rouredes occidentals, on no s' observen aquests canvis (Bou and Vilar, 2019 Pel que fa a espècies introduïdes han aparegut algunes novetats puntuals; així a la Vall de Ribes hi ha la novetat de Picea abies, arbre originari del nord d'Europa, utilitzat en plantacions forestals al NE de la Península Ibèrica, mentre que a la Vall d'Aran ha aparegut Buddleja davidii, llenyosa invasora (MAPAMA, 2018), i de la qual s'hauria de fer un seguiment per veure si acaba de colonitzar el bosc, ja que en el moment de l'estudi eren plantes joves que havien colonitzat des del marge de la carretera, cap a dins el bosc. ...
... En aquest sentit les rouredes del Pirineu i Prepirineu català mostren certa estabilitat en les últimes dècades, sense canvis significatius (Taula 5), fet que no succeeix a les rouredes de localitats més càlides del territori. Així, al Montnegre s'ha pogut evidenciar la termofilització de la comunitat florística de la roureda de roure de fulla gran (Bou and Vilar, 2019). Aquest fenomen s'atribueix a l'augment de temperatura a Catalunya des del 1950 (Martín Vide et al., 2016), i degut a aquest fet s' esperaria observar la termofilització de les rouredes com a resposta a aquestes dinàmiques meteorològiques (Reif et al., 2017). ...
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The sessile oak (Quercus petraea) is a deciduous tree with a Euro‑Siberian distribution. It is widely spread throughout Europe and (as with other Euro‑Siberian species that constitute the Lathyro montani‑Quercetum petraeae plant community) its southern‑most distribution limit can be found on the Iberian Peninsula. Most of the sessile oak forests on the Iberian Peninsula are located on the Cantabrian Range and the Pyrenees. The NE Iberian Peninsula forests, in particualr, are of special ecological and conservation interest because they grow in a Mediterranean climate and, as such, are on the xeric limit for Quercus petraea. In Catalonia (Spain) the sessile oak forests cover 4,823 ha; the majority (85%) of which are in the Pre‑Pyrenees and the Pyrenees. This study has analyzed the species composition of the sessile oak forest found on the Catalan Pyrenees using plant community inventories that were carried out between 2016 and 2018. Furthermore, thanks to previous botanists’ work on the Catalan Pyrenees, the current state of the sessile oak forest has been able to be compared with their (historical) data. With a mean of 37 species per inventory, the results show that the sessile oak has a lot of biodiversity. The dominant species are Euro‑Siberian (68%) and the most common life form are the hemicryptophytes (51%); albeit with notable differences between the locations studied. The most relevant finding is that the composition of the sessile oak forest plant community on the Pyrenees has not, as a consequence of global change, altered a lot over recent decades. This result is the opposite of the patterns that have been observed in the rest of the sessile oak forests in Catalonia which, in turn, highlights the excellent conservation status of some of these forests in the Pyrenees and the need to continue along this path to ensure greater resistance against and resilience to climate change.
... This study analyses demographic resilience in an isolated sessile oak population located at the southernmost limit of the species distribution in the Iberian Peninsula ( Figure 1A). This forest stand is remarkable for its large extension (4 ha), maturity and conservation state, given that along rear edge Mediterranean areas well-developed stands of Q. petraea are rather uncommon due to intensive logging over the last century (Bou & Vilar, 2019 (Carnicer et al., 2014). The current forest structure is the result of a multidecadal period of rural abandonment since the 1950s and the lack of active forest management in most of the protected areas of the park. ...
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Resilience of endangered rear edge populations of cold‐adapted forests in the Mediterranean basin is increasingly altered by extreme heatwave and drought pressures. It remains unknown, however, whether microclimatic variation in these isolated forests could ultimately result in large intra‐population variability in the demographic responses, allowing the coexistence of contrasting declining and resilient trends across small topographic gradients. Multiple key drivers promoting spatial variability in the resilience of rear edge forests remain largely unassessed, including amplified and buffered thermal exposure induced by heatwaves along topographic gradients, and increased herbivory pressure on tree saplings in defaunated areas lacking efficient apex predators. Here we analysed whether indicators of forest resilience to global warming are strongly modulated by local‐scale topographic, microclimatic and biotic conditions. We studied a protected rear edge forest of sessile oak Quercus petraea, applying a suite of 20 indicators of resilience of tree secondary growth, including multidecadal and short‐term indices. We also analysed sapling recruitment success, recruit/adult ratios and sapling thermal exposure across topographic gradients. We found large within population variation in secondary growth resilience, in recruitment success and in thermal exposure of tree saplings to heatwaves, and this variability was spatially structured along small‐scale topographical gradients. Multidecadal resilience indices and curves provide useful descriptors of forest vulnerability to climate warming, complementing assessments based in the analysis of short‐term resilience indicators. Species‐specific associations of trees with microclimatic variability are reported. Biotic factors are key in determining long‐term resilience in climatically stressed rear edge forests, with strong limitation of sapling recruitment by increased roe deer and wild boar herbivory. Our results also support non‐stationary effects of climate determining forest growth responses and resilience, showing increased negative effects of warming and drought over the last decades in declining stands. Synthesis. Our findings do not support scenarios predicting spatially homogeneous distributional shifts and limited resilience in rear edge populations, and are more supportive of scenarios including spatially heterogeneous responses, characterised with contrasting intra‐population trends of forest resilience. We conclude that forest resilience responses to climate warming are strongly modulated by local‐scale microclimatic, topographic and biotic factors. Accurate predictions of forest responses to changes in climate would therefore largely benefit from the integration of local‐scale abiotic and biotic factors.
... Para poder comprobar si las hipótesis de los efectos de cambio global son ciertas, se estudian los cambios correspondientes a la evolución de los robledales en los últimos años. Trabajando a nivel de comunidad florística del robledal en el NE de la Península Ibérica (Bou & Vilar, 2019a), comparando inventarios históricos (Lapraz, 1962;Vigo, 1968Vigo, , 1996Bolòs, 1988;Viñas, 1993;Carreras et al., 1995Carreras et al., , 1997 con actuales y a su vez haciendo especial énfasis en el caso de estudio del Montseny donde se profundiza en la distribución y estructura forestal de los robledales (Bou & Vilar, 2018y Bou & Vilar, 2019b, ya que se trata de una localidad claramente en el xeric limit, es decir con una importancia estratégica en la gestión y conservación de estos bosques. ...
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El roble albar Quercus petraea se encuentra ampliamente presente en el centro de Europa. Las poblaciones del NE de la Península Ibérica se encuentran en su límite meridional de distribución y las de condiciones más mediterráneas en el xeric limit para esta especie. Los resultados de la tesis, muestran que la comunidad ha cambiado su composición de especies des de la segunda mitad del s. XX, pero de forma sensiblement diferente según cada región. La dinámica de los robledales de roble albar es su recuperación tras el cambio de los usos del bosque, y el Montseny es un buen ejemplo de este proceso. La situación es bien distinta en algunos robledales como los del Montnegre, donde los efectos del cambio climático suponen un futuro incierto. Por este motivo es importante aprovechar las localidades que se encuentran en refugios climáticos como reservorios y puntos donde poder conservar este hábitat.
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Shifts in plant species and biome distribution in response to warming have been described in past climate changes. However, reported evidence of such shifts under current climate change is still scarce. By comparing current and 1945 vegetation distribution in the Montseny mountains (Catalonia, NE Spain), we report here a progressive replacement of cold-temperate ecosystems by Mediterranean ecosystems. Beech (Fagus sylvatica) forest has shifted altitudinally upwards by ca. 70 m at the highest altitudes (1600–1700 m). Both the beech forests and the heather (Calluna vulgaris) heathlands are being replaced by holm oak (Quercus ilex) forest at medium altitudes (800–1400 m). This beech replacement has been observed to occur through a progressive isolation and degradation of beech stands. In ‘isolated’ (small and surrounded by holm oaks) beech stands, beech trees are 30% more defoliated, beech recruitment is 41% lower, and holm oak recruitment is three times higher than in ‘continental’ (large and continuous) beech stands. The progressively warmer conditions, complemented by the land use changes (mainly the cessation of traditional land management) are the apparent causes, providing a paradigmatic example of global change affecting distributions of plant species and biomes.
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Aim To assess the spatial patterns of forest expansion (encroachment and densification) for mountain pine (Pinus uncinata Ram.) during the last 50 years at a whole mountain range scale by the study of different topographic and socio-economic potential drivers in the current context of global change. Location The study area includes the whole distributional area of mountain pine in the Catalan Pyrenees (north-east Spain). This represents more than 80 municipalities, covering a total area of 6018 km2. Methods Forest cover was obtained by image reclassification of more than 200 pairs of aerial photographs taken in 1956 and 2006. Encroachment and densification were determined according to changes in forest cover, and were expressed as binary variables on a 150 × 150 m cell-size grid. We then used logistic regression to analyse the effects of several topographic and socio-economic variables on forest expansion. Results In the period analysed, mountain pine increased its surface coverage by 8898 ha (an increase of more than 16%). Mean canopy cover rose from 31.0% in 1956 to 55.6% in 2006. Most of the expansion was found on north-facing slopes and at low altitudes. Socio-economic factors arose as major factors in mountain pine expansion, as encroachment rates were higher in municipalities with greater population losses or weaker primary sector development. Main conclusions The spatial patterns of mountain pine expansion showed a good match with the main patterns of land-use change in the Pyrenees, suggesting that land-use changes have played a more important role than climate in driving forest dynamics at a landscape scale over the period studied. Further studies on forest expansion at a regional scale should incorporate patterns of land-use changes to correctly interpret drivers of forest encroachment and densification.
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Questions The 1990s were the warmest decade since the beginning of climate measurements. Based on almost 100 years of monitoring in the Swiss Alps, we asked (1) whether the extraordinary warm climatic conditions of the 1990s are reflected in the floristic composition of Alpine summit vegetation and, if so, (2) what the magnitude and rate of species change has been over the last few decades compared to the documented increase in species richness within the first 80 years of the 20th century. Location Ten high mountain summits of the Bernina area in the southeastern Swiss Alps. Methods Resurvey of the floristic composition of the uppermost altitudinal 10 m of these summits, applying the same methodology of former two surveys (1905 and 1985) and recording the presence of all vascular plant species. Results Whereas the continued increase in plant species richness of high alpine summit vegetation is confirmed, our results also suggest an acceleration of the trend in the upward shift of alpine plants. Conclusion Vegetation change in the southeastern Swiss Alps has accelerated since 1985, consistent with a climate change explanation.