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Article

Prunus lusitanica L.: An Endangered Plant Species Relict in the Central Region of Mainland Portugal

by
Mauro A. M. Raposo
1,2,*,
Leonel J. R. Nunes
3,
Ricardo Quinto-Canas
4,
Sara del Río
5,
Francisco M. Vázquez Pardo
6,
Ana Galveias
7 and
Carlos J. Pinto-Gomes
1,2
1
Department of Landscape, Environment and Planning, School of Science and Technology, University of Évora, 7000-671 Évora, Portugal
2
Mediterranean Institute for Agriculture, Environment and Development (MED), University of Évora, 7000-671 Évora, Portugal
3
PROMETHEUS—Unidade de Investigação em Materiais, Energia e Ambiente para a Sustentabilidade, Escola Superior Agrária, Instituto Politécnico de Viana do Castelo, Rua da Escola Industrial e Comercial de Nun’Alvares, 4900-347 Viana do Castelo, Portugal
4
Centre of Marine Sciences (CCMAR), Faculty of Sciences and Technology, Campus de Gambelas, University of Algarve, 8005-139 Faro, Portugal
5
Departamento de Biodiversidad y Gestión Ambiental (Área de Botánica), Instituto de Ganadería de Montaña (CSIC-ULE), Facultad de Ciencias Biológicas y Ambientales, Campus de Vegazana s/n, Universidad de León, E-24071 León, Spain
6
Departamento de Producción Florestal y Pastos, Centro de Investigación Finca La Orden-Valdesequera (CICYTEX), 06187 Guadajira, Spain
7
Department of Chemistry, ICT—Institute of Earth Sciences, School of Sciences and Technology & IIFA, University of Évora, 7000-671 Évora, Portugal
*
Author to whom correspondence should be addressed.
Diversity 2021, 13(8), 359; https://doi.org/10.3390/d13080359
Submission received: 5 July 2021 / Revised: 20 July 2021 / Accepted: 31 July 2021 / Published: 4 August 2021
(This article belongs to the Section Plant Diversity)
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Versions Notes

Abstract

:
Prunus lusitanica L. is a paleotropical relic species with an Ibero-Maghrebian distribution, which is presently considered as an endangered species, recognized by the Natura 2000 Network (92/43/EEC) as a priority habitat for conservation in Europe. The mountains in the Portuguese mainland central region offer the best location for this species to occur. The main objective of this study is to measure the current conservation status of the communities of P. lusitanica, through the collection of field data, such as the number of existing individuals of each population and their location, which will then be comparatively analyzed based on the previous literature, published at least 15 years ago. Soil characterization analysis was carried out and the main threats to conservation were identified. As a result, a decline of approximately 40% was observed in the number of individuals and in the quality of their habitat. The main threats to their conservation were found to be the seasonal occurrence of rural fires and the expansion of invasive species, such as Acacia dealbata Link and Ailanthus altissima (Mill.) Swingle. Finally, we present the main management methodologies that should be considered for the valorization of this important vegetational relic in the central region of mainland Portugal.

1. Introduction

The communities of Prunus lusitanica L. are true paleotropical relics that had their optimal ecological apogee during the Paleogene period [1,2]. Since then, with the evolution of the Mediterranean climate conditions to actual standards in the Iberian Peninsula, characterized mainly by the accentuation of a summer drought period, the Laurissilva forest has undergone a sharp reduction in its occupation area throughout southern Europe and, particularly, in the Mediterranean basin [3,4,5]. For this reason, the communities of P. lusitanica are currently refugees in certain specific locations with very particular conditions, where the orography allows for a greater atmospheric humidity and mild temperatures to occur [6,7]. This forest can be characterized by exhibiting persistent leafy vegetation, similar to what happens today in some well-preserved slopes in the north of the Island of Madeira (Portugal) and in the Canary Islands (Spain) [8]. Although much of the typical Laurissilva flora has disappeared from the European continent, several other species, such as Rhododendron ponticum L., Laurus nobilis L., Ilex aquifolium L. and Myrica faya Aiton, still persist as relic vegetation [1,9].
Evaluated as an Endangered species using the IUCN criteria established in 1998 [10], it is in Portugal that the most well-preserved and extensive communities of P. lusitanica still persist throughout its entire distribution area, with more than 19,000 individuals registered at a national level in 2005, corresponding to approximately 62% of the total global population [11]. Their communities are also recognized as a priority habitat for conservation in Europe through the Sectoral Plan of the Natura 2000 Network (92/43/EEC), called Laurus nobilis arborescent shrubs, of the Azereirais subtype (5230*pt2). However, due to the permanent threats that menace these habitats, a significant reduction in the number of individuals occurred [6]. Among all the threats identified in the Habitat File, the invasion of exotic plants that progressively colonize new areas and the recurrence and severity of rural fires can be highlighted [12,13,14]. In fact, at this moment, the impact of fires is, probably, the major concern for the reduction in the number of individuals and loss of the area occupied by this habitat, particularly in the central region of mainland Portugal [15]. An example of this is the rural fire that occurred in October 2017 and destroyed a significant part of the largest population of P. lusitanica, located in Mata da Margaraça (Arganil, Portugal). As can be seen in Figure 1, the entire area that surrounds the habitat was burnt and is slowly recovering 1 year after the rural fire.
Thus, it is necessary to study and monitor, in detail, the evolution of P. lusitanica nuclei to reverse this situation of decline. The analysis of the edaphoclimatic conditions, as well as the anthropic action, allows us to understand and facilitate the adoption of adequate management methodologies for the valorization of the remaining populations of the continental Laurissilva. Based on these concerns, the main objectives of the present article are to update the population census of P. lusitanica in Serra da Estrela; to identify the main threats to its conservation; to identify management strategies to value this relict habitat.

2. Materials and Methods

2.1. Characterization of the Area under Study

The area under study is located on the reliefs of the central region of mainland Portugal, covering the area occupied by Serra da Estrela, Serra da Lousã, Serra de Alvéolos, Serra Vermelha and Serra do Açor. The lower altitude found in the region is around 220 m and the highest altitude is around 1300 m (Figure 2). In biogeographic terms, the areas under study belong to the Montemuro and Estrela Sierran Sector and the Oretania and Tejo Sector [16]. The geology of the region is mostly formed by Precambrian and Cambrian metasediments that form the schist–greywacke complex, which is intercepted by a set of granitic rocks of hercynian origin [17]. Although a varied mineralogical composition can be found from granodiorites to leucogranites [18], the areas of occurrence of P. lusitanica are dominated by the schist soils, as well as fluvial sedimentary deposits with wavy and pronounced reliefs. These schists are part of the Malpica do Tejo formation and are dated from 500 to 650 million years ago [19]. Most of the soils in the area under study are lithosols, while some of which have evolved into cambisols over the years [20].
At the bioclimatic level, the area is located in the transition from the mediterranean to the temperate macrobioclimate (Table 1). The municipality of Mação represents the southern limit of the natural distribution area of P. lusitanica in mainland Portugal and is under the influence of a humid thermomediterranean bioclimate [21]. The northern limit of the area is part of the municipality of Seia and is influenced by a humid mesotemperate bioclimate (Figure 3).
These conditions are favorable for the presence of Quercus robur subsp. broteroana O. Schwartz that constituted the potential climatophilic vegetation of much of the area under study, of the association Viburno tini-Quercetum broteroanae (Br.Bl., P. Silva, and Rozeira, 1955) J.C. Costa, Capelo, Honrado, Aguiar and Lousã 2002 corr. J.C. Costa and Monteiro-Henriques 2012. The communities of Alnus lusitanica Vít, Douda and Mandák, from the association Scrophulario scorodoniae-Alnetum glutinosae Br.-Bl., P. Silva and Rozeira 1955, appear in an edafo-hygrophilic position. In a secondary position, or as an edaphoxerophilous vegetation, are communities of Quercus pyrenaica Willd., Q. suber L. and Q. rotundifolia Lam., from the associations Arbuto unedonis-Quercetum pyrenaicae (Rivas-Goday in Rivas-Goday, Esteve, Galiano, Rigual and Rivas-Martínez, 1960) Rivas-Martínez 1987, Sanguisorbo hybridae-Quercetum suberis Rivas-Goday in Rivas-Goday, Borja, Esteve, Galiano, Rigual and Rivas-Martínez 1960 and Teucrium salviastri-Quercetum rotundifoliae Pinto-Gomes, Ladero, Cano, Meireles, Aguiar and P. Ferreira 2010, respectively [22].
However, the landscape is quite altered, dominating the stands of maritime pine (Pinus pinaster Aiton) and eucalyptus (Eucalyptus globulus Labill.). The communities of P. lusitanica in the Portuguese central region are ecologically positioned between the amyals of Scrophulario scorodoniae-Alnetum glutinosae and the oak trees of Viburno tini-Quercetum broteroanae, integrating with the slopes or as the first stage of replacement of these forests. Thus, the association Frangulo alni-Prunetum lusitanicae C. Lopes, J.C. Costa, Lousã and Capelo in J.C. Costa, C. Lopes, Capelo and Lousã 2000 often occupies a tempori-hygrophilic position or a climatophilic position, with water being compensated at a ground level or at an atmospheric level by the fog.

2.2. Data Collection

The interpretation of plant communities followed the phytosociological information based on the landscape and sigmatist approach presented by the Zurich-Montpellier Phytosociology School, as proposed by Braun-Blanquet [23], Géhu and Rivas-Martínez [24] and updated by Rivas-Martínez [25]. Taxonomic and sintaxonomic nomenclature followed the work of Rivas-Martínez et al. [26] and was complemented by more recent works, namely those by Costa et al. [22], Mucina et al. [27] and Taleb and Fennane [28]. For the identification of plant material, the works presented by Castroviejo et al. [29], Coutinho [30], Franco [31] and Franco and Rocha Afonso [32] were used. The biogeographical and bioclimatic framework followed the work presented by Rivas-Martínez et al. [16] and Rivas-Martínez et al. [21].
To count the number of individuals of P. lusitanica, field trips were conducted from 2018 to 2020, during which their geographical coordinates were recorded using GPS equipment with a precision of 1 m, as well as the number of individuals observed in each nucleus. These individuals were separated into two groups: more than 1.5 m and less than 1.5 m height. Regeneration over the year itself was not taken into account due to its small size. Although pollen crossing between individuals can occur at a distance of several kilometers, in this study, each population nuclei was differentiated when any specimen was more than 100 m away.
For the characterization of the pollen, scanning electron microscopy was carried out on a Phenom Pro X instrument. The P. lusitanica L. pollen was deposited on carbon adhesive tabs with a diameter of 12 mm. For the hydration of pollen grains, the carbon adhesive was placed in a humid chamber overnight. The pollen samples were photographed in high resolution (10 kV).
In order to understand the different existing soil conditions, five sampling points were randomly selected in four different zones: P1—habitat in good condition; P2—degraded habitat; P3—areas surrounding the habitat; P4—areas dominated by acacias. This approach resulted in the selection and collection of composite samples, separated into three depth horizons: 0–5 cm; 5–15 cm; 15–30 cm. In the sampling points with shallow soil, it was possible to collect only the first two most superficial horizons. The determination of the organic matter (OM) content was achieved using the muffle method following the procedure established by Goldin [33], with some modifications: beforehand, the samples were dried in an oven at 105 °C for a period of 24 h to eliminate all the water present in the samples [34]. After this period, the ceramic crucibles with the samples were placed in a muffle furnace and incinerated at a temperature of 550 °C for 3 h. Subsequently, the set (crucible + waste) was placed in a desiccator and then weighed. The organic matter content was determined due to the mass loss of the incinerated residue, considering the material lost by burning in the temperature range of from 105 °C to 550 °C, according to the formula (P = weight of the sample (g) after heating to 105 °C; C = tare of the crucible (g); T = weight of ash + crucible (g)), as presented in Equation (1):
OM   ( % ) = ( P − ( T − C ) ) × 100 P ,
Diversity 13 00359 g003 550
Figure 3. Thermopluviometric graphics of the areas under study: (a) Mação; (b) Seia; (c) Lousã; (d) Arganil (data acquired at Portal do Clima web platform, available at www.portaldoclima.pt, accessed on 14 June 2021, in accordance with the methodology presented by Walter and Lieth (1967) and Walter (2012) [34,35]).
Figure 3. Thermopluviometric graphics of the areas under study: (a) Mação; (b) Seia; (c) Lousã; (d) Arganil (data acquired at Portal do Clima web platform, available at www.portaldoclima.pt, accessed on 14 June 2021, in accordance with the methodology presented by Walter and Lieth (1967) and Walter (2012) [34,35]).
Diversity 13 00359 g003

2.3. Ecological Modeling

Based on prior knowledge of the ecological conditions of P. lusitanica, modeling was carried out using the Maxent 3.4.4 program for the area under study [11,35]. This information was complemented with field data collected during the period from 2018 to 2020. Eight climate variables from WorldClim (version 2.1) were used for ecological modeling: Tavg—average temperature; Tmax—maximum temperature; Tmin—minimum temperature; elev—elevation; prec—precipitation; srad—solar radiation; vapr—water vapor pressure; wind—wind speed [36]. The bioclimatic variables (1970–2000) used to calculate the current distribution have a spatial resolution of 30 s (~1 km2).

3. Results and Discussion

The fieldwork resulted in the observation of almost 10,000 individuals of P. lusitanica in the central region of mainland Portugal (Table 2). Despite the rural fire that occurred in October 2017, Serra do Açor continues to have the greatest representativeness of this species, corresponding to approximately 50% of the individuals in the area under study. With almost 3000 individuals, the União de Freguesias de Vide e Cabeça faces serious problems with the invasion of exotic species, such as Acacia dealbata Link., Acacia melanoxylon R. Br. and Ailanthus altissima (Mill.) Swingle. In the municipality of Mação, which includes the lowest number of cherry trees, with around 70 individuals, constitutes the southernmost territory in Portugal, where the presence of thermophilic elements can still be detected, such as Pistacia lentiscus, Myrtus communis and Smilax aspera in the Ribeira do Aziral and Ribeira do Fraguedo.
These data show a reduction of approximately 6500 individuals in the area under study, corresponding to a loss of approximately 40% in comparison with the results published by Calleja [11]. In general, in the well-preserved areas, there were no problems with the pollination of flowers, or with the seed production, or with the natural germination (Figure 4). However, we verified a low survival of young plants. Occasionally, there were problems with the presence of herbivorous animals, such as deer, namely in Ribeira do Gondufo (Seia), where it is possible to observe some of the oldest cherry trees in Portugal, although the natural regeneration is practically nil.
At the infraspecific and even specific levels, the pollen of the genus Prunus is one of the most difficult to differentiate due to its morphological similarities [11,37]. According to the present research, pollen from P. lusitanica is rarely studied, and there is only one database with its typification [38]. Through our analyzes we confirm that Prunus lusitanica L. pollen is monad, tricolporate (three apertures furrows, pores indistinct or obscure) and isopolar. In polar view is circular or triangular and subprolate in equatorial view (Figure 5). In equatorial view the apertures are visible. The exine is strongly striate with some puncta between the striae. Furrows are wide, with irregular margins, granulate ornamentation with saliente intine. The size of this pollen type is average, around 36-40 µm. The pollen of several taxa of the genus Prunus is heavy, which is why pollination by the honeybee (Apis mellifera Linneus) is important for the development of a high number of fruits, as is the case with the cultivation of the cherry trees [39,40].
The strong mortality of young plants may be associated with climatic or edaphic factors. In the different sampled areas, the horizon A (0–5 cm) of the soil showed a high organic matter content, while the second sampled horizon (5–15 cm) showed a significant reduction in organic matter content (Figure 6). Although some samples from the third horizon (15–30 cm) were not taken due to the weak thickness of the soil, this was the horizon that showed the lowest accumulated values. Although the areas P2 and P3 were sometimes presented as clearings between the shrub cover, the areas dominated by A. dealbata showed an even lower organic matter content in horizon A. This fact is mainly due to the lack of other flora, kept away by the physical and allelopathic competition effect of the acacias, as well as the reduced amount of organic matter produced by A. dealbata stands [41].
Several nuclei of P. lusitanica from the central region of mainland Portugal are currently in regression due to the strong expansion of exotic plants with an invasive character. Table 3 presents the main species identified in the area under study, as well as the most appropriate control method for each species [42]. Of all species, A. dealbata can be highlighted, which occurs inside or in the vicinity of all the areas under study, occupying the slopes and margins of the water lines (Figure 7a). Another identified aspect was the formation of seeds in Hakea sericea Schrader from plants that germinated 1 year after the occurrence of a rural fire (Figure 7b). On the other hand, although E. globulus does not have an invasive behavior in much of the national territory, in territories with high humidity and after the passage of fire, it presents a high dispersion and germination of seeds, resulting in plant densities which sometimes completely cover the soil (Figure 7c).
In addition to the urgent need to control invasive plants in the region under study, it is necessary to avoid the introduction of other species that could invade new areas, as has happened in other areas of Europe [43,44]. Rural fires promote the appearance of heliophilous shrubs, which increases the risk of rural fires recurring in short time periods [45]. In this sense, selective control with vegetation cover is proposed, in order to promote the growth of the characteristic species of habitat 5230, such as Laurus nobilis, Rhododendron ponticum, Myrica faya, Arbutus unedo, Viburnum tinus, Ilex aquifolium, Rosa sempervirens and Smilax aspera, among others, avoiding the negative impacts of chemical control [46].
On the other hand, to create buffer zones and fire breaks in a landscape marked by forest production stands, discontinuities must be created through the promotion of native forest species, such as Q. robur subsp. broteroana, Q. pyrenaica, Q. suber or even Castanea sativa, Prunus avium and Arbutus unedo. The landscape mosaic contributes not only to lowering the risk of fires but also to the greater sustainability and resilience of the landscape. Thus, planting native forests in the areas surrounding habitat 5230 will contribute significantly to reducing the risk of fire, when compared to the high rates of flammability of resinous species and species with high essential oil content, such as P. pinaster and E. globulus, respectively [47,48]. Although the strong contribution of the analyzed threats to the decrease in the number of individuals of P. lusitanica, recolonization through plantations is an effective method and has already been tested and used with other species [49,50]. To meet the potential area of occurrence of the species, a model was created using current ecological data, presented in Figure 8.
According to the results obtained, the most determining factor in the geographic distribution of P. lusitanica in the central region of mainland Portugal is precipitation. Other noteworthy factors are solar radiation and the average annual temperature (Figure 9). These results are in accordance with the ecological characterizations carried out in previous works, namely on the north-facing slopes, with mild temperatures and higher humidity [51,52,53,54]. Following the achievements of the present research, however, the aim is to identify integrative policies with local communities instead of on a restrictive basis, as is the case in other places in the Mediterranean basin with lush vegetation [55].

4. Conclusions

The communities of P. lusitanica in the central region of mainland Portugal are in sharp decline, with the loss of approximately 40% of individuals in 15 years. Several conservation projects have contributed to recovering this species and avoiding aggravating the evaluation criteria to Critically Endangered. Thus, it is expected that, in the near future, the assessment of Endangered will be maintained due to the adequacy of the A2c criterion. However, stricter conservation policies and replication actions are needed based on the experiences that were already carried out, such as the Life-Relict Project (NAT/PT/000754). Thus, it is not enough to conserve the species, but instead, its habitat and the surrounding areas must be conserved, allowing better flow between plants and animals. This study shows the need for the rapid integration of P. lusitanica in the Red List of Vascular Plants of Mainland Portugal, thus allowing a better transmission of the value of this species to the instruments of territorial management.

Author Contributions

Conceptualization, M.A.M.R. and C.J.P.-G.; methodology, M.A.M.R., A.G. and L.J.R.N.; software, S.d.R. and R.Q.-C.; validation, S.d.R., F.M.V.P. and C.J.P.-G.; formal analysis, M.A.M.R. and A.G.; investigation, M.A.M.R., L.J.R.N. and R.Q.-C.; data curation, M.A.M.R., S.d.R., R.Q.-C., L.J.R.N. and C.J.P.-G.; writing—original draft preparation, M.A.M.R.; writing—review and editing, S.d.R. and F.M.V.P.; visualization, A.G. and M.A.M.R.; supervision, S.d.R., F.M.V.P. and C.J.P.-G. All authors have read and agreed to the published version of the manuscript.

Funding

This work is funded by National Funds through the Foundation for Science and Technology (FCT) under the Project UIDB/05183/2020. L.J.R.N. was supported by Prometheus—Research Unit on Energy, Materials and Environment for Sustainability, UIDP/05975/2020, funded by national funds through FCT.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

The data presented in this study are available on request to the corresponding author.

Acknowledgments

This research received a contribution from the European Commission’s LIFE program, through the Life-Relict Project (NAT/PT/000754), to the municipalities of Mação, Pampilhosa da Serra and Freguesia de Vide e Cabeça for their collaboration in the fieldwork. We would like to thank researcher Helena Ribeiro from the Department of Geosciences, Environment and Spatial Plannings of the Faculty of Sciences University of Porto for her contributions to pollen characterization.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Mata da Margaraça (Arganil, Portugal) after the rural fire that occurred in October 2017 (picture taken in 2018).
Figure 1. Mata da Margaraça (Arganil, Portugal) after the rural fire that occurred in October 2017 (picture taken in 2018).
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Figure 2. Location of the areas under study.
Figure 2. Location of the areas under study.
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Figure 4. Details of P. lusitanica. From left to right: flowering; fruiting; natural regeneration.
Figure 4. Details of P. lusitanica. From left to right: flowering; fruiting; natural regeneration.
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Figure 5. P. lusitanica pollen grains under the Scanning Electron Microscope (SEM), collected in Mata da Margaraça. (a) Tricolpate pollen in polar view on the left side and equatorial view on the right side. (b) Tricolpate pollen in polar view—detail of the exine sculpturing with some puncta between the striae.
Figure 5. P. lusitanica pollen grains under the Scanning Electron Microscope (SEM), collected in Mata da Margaraça. (a) Tricolpate pollen in polar view on the left side and equatorial view on the right side. (b) Tricolpate pollen in polar view—detail of the exine sculpturing with some puncta between the striae.
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Figure 6. Percentage of organic matter per plot and depth of sampling (P1—habitat with good conservation status; P2—habitat with poor conservation status; P3—periphery of habitat 5230*pt2; P4—areas dominated by A. dealbata).
Figure 6. Percentage of organic matter per plot and depth of sampling (P1—habitat with good conservation status; P2—habitat with poor conservation status; P3—periphery of habitat 5230*pt2; P4—areas dominated by A. dealbata).
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Figure 7. Exotic plants with invasive behavior in the areas under study. (a) Invasion of the banks of the River Alvôco with A. dealbata; (b) H. sericea fruiting near Ribeira do Aziral (Mação); (c) aggressive seminal regeneration of E. globulus in Serra da Estrela. (These photographs are by Mauro Raposo).
Figure 7. Exotic plants with invasive behavior in the areas under study. (a) Invasion of the banks of the River Alvôco with A. dealbata; (b) H. sericea fruiting near Ribeira do Aziral (Mação); (c) aggressive seminal regeneration of E. globulus in Serra da Estrela. (These photographs are by Mauro Raposo).
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Figure 8. Map of the potential occurrence area of P. lusitanica in the central region of mainland Portugal.
Figure 8. Map of the potential occurrence area of P. lusitanica in the central region of mainland Portugal.
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Figure 9. Importance of ecological factors in modeling the potential occurrence area of P. lusitanica in Serra da Estrela (Tavg—average temperature; Tmax—maximum temperature; Tmin—minimum temperature; elev—elevation; prec—precipitation; srad—solar radiation; vapr—water vapor pressure; wind—wind speed).
Figure 9. Importance of ecological factors in modeling the potential occurrence area of P. lusitanica in Serra da Estrela (Tavg—average temperature; Tmax—maximum temperature; Tmin—minimum temperature; elev—elevation; prec—precipitation; srad—solar radiation; vapr—water vapor pressure; wind—wind speed).
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Table
Table 1. Bioclimatic data of the area under study: T—annual average temperature in Celsius degrees; P—average annual rainfall in millimeters; Tp—positive annual temperature in Celsius degrees; Pp—positive rainfall in millimeters; Io—annual ombrothermic index; It—thermicity index; Ic—simple continentality index (index based on Rivas-Martínez et al. [21]).
Table 1. Bioclimatic data of the area under study: T—annual average temperature in Celsius degrees; P—average annual rainfall in millimeters; Tp—positive annual temperature in Celsius degrees; Pp—positive rainfall in millimeters; Io—annual ombrothermic index; It—thermicity index; Ic—simple continentality index (index based on Rivas-Martínez et al. [21]).
LocationTPTpPpIoItIc
Mação14.87816.30178.40816.304.58316.6714.00
Lousã14.031270.00168.401270.007.54324.339.10
Mata da Margaraça13.531157.50162.401157.507.13277.3313.90
Seia13.03906.90156.40906.905.80264.3314.00
Average13.871037.68166.401037.686.26295.6712.75
Table
Table 2. Size of the population nuclei of P. lusitanica.
Table 2. Size of the population nuclei of P. lusitanica.
Geographical AreaAdult Individuals (>1.5 m)Young
Individuals
(<1.5 m)		Total
Individuals		Natural
Regeneration
(%)		Total Population (%)
Vide and Cabeça (Seia)2494469296318.8130.3
Serra da Lousã2162824412.962.49
Serra do Açor3905831473621.2848.40
Pampilhosa da Serra1229162139113.1814.22
Ribeira do Aziral (Mação)672692.990.71
Serra dos Alvéolos245142595.712.65
Orvalho (Oleiros)11491237.891.26
Total82701515978511.83100
Table
Table 3. Main exotic plants with invasive behavior identified in the areas under study.
Table 3. Main exotic plants with invasive behavior identified in the areas under study.
Scientific NameFamilyOccurrencesControl Method
Acacia dealbata Link.FABACEAEAçor, Estrela, Lousã, Mação, Oleiros, Orvalho, Pampilhosa da SerraTo peel
Acacia melanoxylon R. Br.FABACEAELousã, Estrela, Pampilhosa da SerraTo peel
Hakea sericea SchraderPROTEACEAEEstrela, Lousã, Mação, Orvalho, Pampilhosa da SerraCut + burn
Ailanthus altissima (Miller) SwingleSIMAROUBACEAEEstrela, Lousã, Pampilhosa da SerraTo peel
Robinia pseudoacacia L.FABACEAELousã, estrelaTo peel
Eucalyptus globulus Labill.MYRTACEAEAçor, Lousã, EstrelaTo peel
Paulownia tomentosa (Thunb.) Steud.PAULOWNIACEAEEstrelaTo peel
Arundo donax L.POACEAEEstrela, LousãCut + grazing
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Raposo, M.A.M.; Nunes, L.J.R.; Quinto-Canas, R.; del Río, S.; Pardo, F.M.V.; Galveias, A.; Pinto-Gomes, C.J. Prunus lusitanica L.: An Endangered Plant Species Relict in the Central Region of Mainland Portugal. Diversity 2021, 13, 359. https://doi.org/10.3390/d13080359

AMA Style

Raposo MAM, Nunes LJR, Quinto-Canas R, del Río S, Pardo FMV, Galveias A, Pinto-Gomes CJ. Prunus lusitanica L.: An Endangered Plant Species Relict in the Central Region of Mainland Portugal. Diversity. 2021; 13(8):359. https://doi.org/10.3390/d13080359

Chicago/Turabian Style

Raposo, Mauro A. M., Leonel J. R. Nunes, Ricardo Quinto-Canas, Sara del Río, Francisco M. Vázquez Pardo, Ana Galveias, and Carlos J. Pinto-Gomes. 2021. "Prunus lusitanica L.: An Endangered Plant Species Relict in the Central Region of Mainland Portugal" Diversity 13, no. 8: 359. https://doi.org/10.3390/d13080359

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