The road system under investigation climbs up Monte Pellegrino (606 m a.s.l.), a well-known limestone mountain that rises to the northwest of Palermo in the northern coastal belt of Sicily (Hutchinson 1959). It has an elongated shape, with its major axes oriented from southeast to northwest, toward the Palermo plain. The topography is characterized by steep slopes and subvertical cliffs associated with subhorizontal planes (Fig. 1).

In terms of the geological setting, the study area is part of the Apennine–Maghrebian chain (Grasso, 2001). The lithostratigraphy is characterized by different formations described by Basilone (2018) within the Panormide carbonate platform successions (Upper Triassic to Lower Miocene), in particular, the following outcrops: a) the Pellegrino Formation (along the western side), that consists of massive rudistid boundstones and floatsones alternating with blackish laminated mudstone, stromatolitic and loferitic packstone, and bioclastic packstone; b) the Capo Gallo limestone formation (on the central part), that consists of well-stratified grey limestone (wackestone/packstone) alternating with blackish oolitic grainstone; c) the Piano Battaglia limestone formation (along the eastern and southern sides) that consists of massive grey reef limestones, calcareous breccias, and oolite grainstone; the Cozzo di Lupo formation that consists of Spongid reef limestones alternating with calcareous breccias and calcarenites (grainstone-packstone); d) scree and debris flow mainly concentrated along the sides of mountains (Basilone 2018).

In terms of climate, the study published by Duro et al. (1996) shows an average annual daytime temperature of 18.1 °C, while the average annual maximum temperature is 22.5 °C, and the average annual minimum temperature is 13.7 °C. The coldest month of the year is January (monthly mean minimum = 7.8 °C, monthly mean maximum = 15.7 °C), and the warmest month is August (monthly mean minimum = 20.8 °C, monthly mean maximum = 29.9 °C). Mean annual precipitation data (mm) on the Palermo plain, measured at different weather stations, show 679.4 mm (Istituto Castelnuovo), 643.7 mm (Servizio Idrografico) and 584.1 mm (Osservatorio Astronomico), corresponding to, respectively, 78, 73, and 71 rain days (Gianguzzi et al. 2013, 2015a).

Bioclimatic indices of the area, calculated according to Rivas-Martínez et al. (2011), allowed the definition of different thermotypes and ombrotypes in relation to land elevation as follows: a) Upper Thermomediterranean Lower Dry; b) Upper Thermomediterranean Upper Dry; c) Upper Thermomediterranean Lower Subhumid; d) Lower Mesomediterranean Lower Subhumid (Bazan et al. 2015; Gianguzzi et al. 2015b).

On the northern slopes, the local bioclimate tends to be Thermo-Mesomediterranean, from sub-humid to humid, due to the high cliffs shaped like a north-facing theater. Here, the vegetation consists of Rhamno alaterni-Querco ilicis pistacio terebinthi sigmetosum. In this vegetation series, the mature formation is a wood dominated by Quercus ilex and characterized by the presence of thermophilous deciduous broadleaves such as Pistacia terebinthus and Rhus coriaria. The seral stages are more frequently represented by maquis, dominated by the above-mentioned deciduous broadleaves and by perennial dry grasslands o Helictotricho-Ampelodesmetum mauritanici (Gianguzzi et al. 1996).

On the western and southwestern sides of Monte Pellegrino, contrasting microclimatic conditions, created by different slope aspects and steepness, result in a tendency towards the Thermomediterranean lower dry (also verging on the Inframediterranean). Climatophilous vegetation can be referred to the oleaster series (Ruto chalepensis-Oleo sylvestris sigmetum), whose head of series is the Olea europaea var. sylvestris xerophilous wood (Gianguzzi and Bazan 2019, 2020; Gianguzzi et al. 2020). The successional stages of the series are represented by Euphorbia dendroides garrigue (Rhamno-Euphorbietum dendroidis s.l.) and xerophilous Hyparrhenia hirta grassland (Hyparrhenietum hirto-pubescentis s.l.) which, in recent years, tends to be replaced by the alien invasive grassland Pennisetum setaceum (Penniseto setacei-Hyparrenietum hirtae), probably due to climate warming (Pasta et al. 2010). Communities dominated by therophytes (e.g. Thero-Sedetum caerulei, Stipellula capensis micro-communities, etc.) also belong to the same vegetation series.

On the eastern sides, the bioclimate is Thermomediterranean and ranges from upper dry to lower subhumid (north-east). Climatophilous vegetation is represented by a more xerophilous holm oak series (Rhamno alaterni-Querco ilicis pistacio lentisci sigmetosum) in which Hyparrhenia hirta grassland (Hyparrenietum hirtae s.l.) is the most significant and widespread degradation aspect.

The three climatophilous series come into contact with the microgeosigmeta of the inland cliff communities of the alliance Dianthion rupicolae (Asplenietea trichomanis), such as Scabioso creticae-Centaureetum ucriae (Gianguzzi et al. 1996).

Monte Pellegrino’s vegetation mosaic hosts a rich flora, counting 741 infrageneric taxa (Raimondo et al. 1996), which includes some rupicolous endemic species and taxa of biogeographic interest, such as: Iberis semperflorens, Glandora rosmarinifolia, Centaurea panormitana, Helichrysum panormitanum, Seseli bocconei, Micromeria fruticulosa and Brassica rupestris.

Archaeological evidence in the Allaura caves (on the northern slopes of the mountain) dates the human presence in the area back to the Upper Paleolithic period (Mannino et al. 2011), testifying to a thousand-year-old exploitation of Monte Pellegrino’s natural resources. Despite the historical land-use of the territory, the area has maintained a high level of biodiversity as a result of a long-term interaction between humans and nature, as has also been pointed out for other areas of Sicily (Guarino and Pasta 2017; Bazan et al. 2019, 2020; Musarella et al. 2018; Todaro et al. 2020).

However, due to its proximity to the city of Palermo, the protected area has been affected by anthropic disturbances, such as recurring fires, a prevalence (in terms of biomass) of exotic species over native ones, and waste dumping that afflicts even the most inaccessible areas, which damage the site’s natural heritage.

The road system of Monte Pellegrino is located within the administrative area of the City of Palermo and, consequently, the roads are named following the toponyms of the urban streets. It is divided in four parts (Fig. 1), as follows: 1) via Pietro Bonanno, located on the southwestern side, connects the city of Palermo to the Sanctuary of Santa Rosalia; 2) via Monte Ercta (also called “Panoramica”), on the northwestern side, connects the Sanctuary of Santa Rosalia to the Mondello area; 3) via Giordano Cascini is the road between the Sanctuary and the panoramic lookout on the northeastern slope of the mountain; 4) a (nameless) service road that climbs from the Sanctuary to the antennas (578 m a.s.l.) on the top of the mountain.

The first two stretches of the road system, with a total length of 16 km, are the historical part of the road system. Via Pietro Bonanno is 9 km long and was named after the mayor who promoted its construction. It was designed at the end of the 19th century by the engineer Giuseppe Damiani Almeyda, who started construction in 1903 (Fundarò 1974; Barbera 2008), though it proceeded extremely slowly. After Almeyda’s death in 1911, management was assigned to the engineer Carlo De Stefani who completed the work in 1924 (Bonanno 2002).

Due to the rugged morphology of the area, it was necessary to carry out large excavations in order to adapt the rocky terrain to the planned road layout. To level the road cross section, it was necessary to cut the rock and raise the lower part of the slopes using substantial masonry retaining walls along the entire route.

The second part of the road – via Monte Ercta – was built from Gabriele Ascione’s design. The excavation works began in 1949, and the construction work was initiated in July 1952, lasting five years. The road was made following the same construction methods as the first part. However, being on the northwestern part of the mountain where the slopes are steeper, it was necessary to build even higher retaining walls, especially in the tight curves above Mondello.

At the same time, the area was reforested with non-native species, especially conifers from the genus Pinus (P. halepensis, P. pinea, etc.) and Cupressus (C. sempervirens, C. arizonica, etc.), as well as broad-leaved trees of the genus Eucalyptus (E. camaldulensis, E. globulus, E. gomphocephala, etc.) and other species (Robinia pseudacacia, Ailanthus altissima, etc.).

In some cases, reforestation influenced the vegetation colonizing the base of the retaining walls by creating shady conditions. In the period between 1927 and 1933, other exotic species were also introduced into the area, such as Agave americana, A. sisalana, Opuntia ficus-indica, and O. maxima, which spontaneously spread between the escarpments and the reforested parts, sometimes forming hedges along the road margins, especially on the xeric slopes facing south/southwest, such as near Castello Utveggio.

The ecological conditions of the anthropogenic micro-habitats created by the construction of the road system reflect the adaptive specialization of the species and plant communities that have settled in them. The studied plant communities were distributed in relation to the following drivers: a) topographical characteristics of the surfaces (horizontal on the road margins, more or less vertical on the walls and rock walls); b) nature of the substrate (stone walls with mortar, asphalt, rocky outcroppings), which generally presents soil poverty, alkaline pH (given the nature of the lithic materials), a lack of nutrients, poor humidity; c) various climatic stresses (e.g., daily and annual temperature ranges, etc.).

Figure 2 shows a cross-section of the roadway on Monte Pellegrino with the different habitats within which the vegetation surveys were carried out. Specifically, these were masonry retaining walls, downhill-side road margins (parapets/guardwalls), uphill-side road margins, artificial rock cuts. For each of the habitats presented in the figure, the main structural and ecological characteristics are defined below, also in relation to the eco-morphological and physiological characteristics of the species and coenoses located there.

1) Retaining walls – These continuously delimit the downhill side of the entire road route, with a height ranging from a few meters up to about 20 m (along the hairpin bends near Mondello). They are made of stone blocks cemented with mortar, built with a (a) base plinth, (b) sloping face, (c) and vertical face. Here lithophilous species, whose roots penetrate the cracks and cavities between the stone blocks, have different settling difficulties, depending on the topographical location (Lisci and Pacini 1993a, 1993b). Cavities at ground level in the base plinth allow the establishment of numerous species, facilitated by the rainwater that flows down the walls, favoring the accumulation of nutrients and moisture needed by plants. Cavities on the sloping faces of the walls also facilitate the germination of seeds thanks to the rainwater that runs down the walls. Cavities on the vertical faces, instead, present greater settling difficulties – in particular on the higher parts and on homogeneous material – given the lower availability of water and nutrients.

2) Masonry guardwalls (downhill side of the road) – Here vegetation finds space in two different types of cavities in which accumulations of soil and humidity are generated. They are respectively located: a) on the upper surface of the guardwalls, following the crumbling of the materials due to the weather; b) at the base of the guardwall, at the interface between two types of construction materials (both inside and outside the road surface) which generates a certain water availability in the interstices.

3) Road margins (uphill side) – This habitat is located beyond the rainwater collection canals which have more nitrophilic and cooler ecological characteristics than the previous habitat. In fact, vegetation finds more favorable conditions here as there is more shade as well as a greater supply of nutrients and humidity thanks to the rainwater that flows down the slopes and walls above.

4) Rock cut slopes – These delimit the uphill part of the road margins and were created by excavating the limestone substrate. They are up to about 15 meters high (on some curves on the Mondello side), giving space to typically rocky communities that develop along the rock walls, according to ecological gradients that can be attributed to purely natural environments. In the upper part, they are true chasmophytic communities dominated by species of the Asplenietea trichomanis class, replaced towards the base of the walls by elements attributable to the Parietarietea judaicae class.

5) Natural slopes – This habitat, completely unrelated to the road profile, is colonized by phytocenotic vegetation linked to the different vegetation series that characterize the Monte Pellegrino promontory (Gianguzzi et al. 1996), not examined in this work.

The vegetation was studied according to the phytosociological method (Braun-Blanquet 1964), as later modified by other authors (e.g., Rivas-Martínez 2005; Biondi 2011; Guarino et al. 2018). Species identifications were made using Pignatti (1982) and Pignatti et al. (2017-2018). Taxonomic nomenclature follows “Flora d'Italia” (Pignatti et al. 2017-2018), with the exception of Pennisetum setaceum, which follows the online database “The Plant List” (2013). The life forms and chorotypes follow Pignatti (1982).

The syntaxonomical nomenclature follows the “International Code of Phytosociological Nomenclature” (Theurillat et al. 2020). For the definition of the syntaxa, the “Vegetation Prodrome of Italy” (Biondi et al. 2014) was followed (see the specific interactive site: http://www.prodromo-vegetazione-italia.org/), with reference to the Vegetation Prodrome of Europe (Mucina et al. 2016) for the classes Cymbalario-Parietarietea diffusae, Stipo-Trachynietea distachyae and the order Elytrigio repentis-Dittrichietalia viscosae.

The survey, carried out between 2016 and 2019, was based on stratified random sampling. The study area was divided into different homogeneous ecological contexts based on both construction typology (masonry retaining wall, guardwall, uphill-side road margin, artificial rock cut slope) and exposition (north, west/southwest), and random sampling was conducted within each of these habitats (Michalcová et al. 2011). Plot size was determined as minimum area (sensu Braun-Blanquet 1964) and ranged between 5 and 50 m2 in the different vegetation types. The number of relevés was defined on the basis of the micro-habitat's surface area. In the case of some groupments with a very small range on homogeneous surfaces, only 2-4 relevés were done.

To evaluate the distribution pattern of the habitats studied in terms of their specific composition, we used detrended correspondence analysis (DCA; Hill and Gauch 1980) using the RStudio (Version 1.1.463) free software and some functions of the vegan package (Oksanen 2015). The choice of this ordination method was confirmed by the measure of the so-called turnover (or SD units) of DCA, which corresponds to the length of its first ordination axes. Moreover, turnover represents a measure of a community’s beta diversity. According to Lepš and Šmilauer (2003), it is preferable to use a unimodal method like DCA for values of turnover units greater than 3.7.

Similarity among different phytocoenoses was evaluated using the “Jaccard Index” (Jaccard 1908). Nestedness was calculated as the average co-occurrence of species, the ‘a’ component of the “Jaccard Index” (Tsakalos et al. 2018).

The life form analysis of the data in the phytosociological table was made by establishing: the percentage distribution of presence in the species list (flora); the percentage distribution of presence in the relevés (frequency), the percentage distribution of the coverage value in the relevés (cover).

Cl.: CYMBALARIO-PARIETARIETEA DIFFUSAE Oberd. 1969

Perennial vegetation with hemicryptophytes, nitrophilous and synanthropic, chasmo-comophytic, found on rocky walls and cliffs.

Ord.: TORTULO-CYMBALARIETALIA Segal 1969

Chasmo-nitrophilous and thermophilous vegetation of built-up areas of the Mediterranean and Atlantic, mild winter to subcontinental regions of temperate Europe, the Middle East, and North Africa.

All.: GALIO VALANTIAE-PARIETARION JUDAICAE Rivas-Mart. ex O. de Bolòs 1967

Thermomediterranean chasmophytic vegetation of limestone walls of the Iberian Peninsula and the western Tyrrhenian archipelago.

1) CREPIDO BURSIFOLIAE-PARIETARIETUM JUDAICAE ass. nov.

Phytosociological data: Table 1.

Holotypus: Rel. 6, Table 1.

Diagnostic species: Parietaria judaica (dom.), Mercurialis annua, Oxalis pes-caprae, Crepis bursifolia, Erigeron bonariensis.

Floristic-syntaxonomical notes : Based on the interpretation of various authors (Bartolo and Brullo 1986; Brullo and Guarino 2002), similar characteristics of wall vegetation have been attributed to the Oxalido corniculatae-Parietarietum judaicae association (Br.-Bl. 1952) Segal 1969 [= Parietarietum judaicae (Arènes 1928) Oberd. 1977]. This syntaxon has been indicated for different areas of the Mediterranean region (Braun-Blanquet and Tüxen). 1952; de Bolós 1967; Rivas-Martínez 1960, 1969; Horvatić 1963; Bartolo and Brullo 1986; Oberdorfer 1977; Brullo and Guarino 1998, 2002; Brullo et al. 2020) as corresponding to the concept of “phytocoenon”. In fact, Oxalis corniculata – one of the species that gives the name to the association – is a plant linked to trampled environments (Brullo and Guarino 2002). Therefore, we think that Oxalido corniculatae-Parietarietum judaicae should be subdivided into multiple geographic synvariants (“races géographiques”) with more limited distribution. This is the case for the two associations proposed here in which, in their typical combinations, high-frequency local differential species were identified, though transgressive from the contiguous phytocoenoses.

Description: It is a hemicryptophytic, sciophilous-nitrophilous, paucispecific formation clearly dominated by Parietaria judaica, located on the lower part of walls. It tends to form a more or less continuous and lush belt of vegetation 40-60 (80) cm tall, that normally has coverage between 75-100% with a minimum area of 6-8 m2. The phytocoenosis is subjected to high levels of eutrophication that occurs in wall cracks and interstices between materials (rocks, mortar, concrete, soil, etc.) of different chemical composition. Here, small accumulations of well-humidified and nitrified soil are created from the flow of rainwater on the wall, as well as from the contributions of internal circulation within the wall. Other associated species can be frequent but with low coverage values, some of which have their vegetative optimum in the winter-spring period (e.g., Oxalis pes-caprae) while others have it in the spring-summer period (es. Erigeron bonariensis, Crepis bursifolia, Mercurialis annua, etc.). In particular, Oxalis pes-caprae, a South-African species in expansion in the Mediterranean area, is an element of the Stellarietea mediae class; Mercurialis annua is a paleotemperate species, typical of manured fields and belonging to the Stellarietea mediae class; Erigeron bonariensis is native to tropical America and has almost become a cosmopolite species belonging to the Chenopodion (Sisymbrietalia, Stellarietea mediae) alliance; Crepis bursifolia is an endemic Italian species that is rather widespread in the Tyrrhenian area, typical of pavements, trampled environments, and road margins, and is also an element of the Trisetario-Crepidetum bursifoliae association (Polygono-Poetea annuae).

Syndynamism: This phytocoenosis plays a pioneering role at the base of masonry and rock walls and takes part in the shady-mesic geosigmetum (north-northwestern-facing slope) of the road system in question (Fig. 3A). It is rarer on the southern part of Monte Pellegrino where it is located on the north-facing walls of via Bonanno (Fig. 4A).

The association is in contact with: (a) the vegetation of horizontal surfaces, such as trampled areas (cl. Polygono-Poetea annuae), flower beds, cultivated areas (cl. Stellarietea mediae), as well as serial aspects of the slope vegetation of Rhamno-Querco ilicis sigmetum; (b) vegetation on the tops of walls, dominated by Parietaria judaica (Athamanto siculae-Parietarietum judaicae ass. nov.), Hypochaeris laevigata (Helichryso panormitanae-Hypochaeridetum laevigatae ass. nov.), and Lomelosia cretica (Scabioso-Centauretum ucriae).

Synchorology: The association, quite common in the study area, probably has a wider distribution in Sicily and the Tyrrhenian area.

2) ATHAMANTO SICULAE-PARIETARIETUM JUDAICAE ass. nov.

Phytosociological data: Table 2.

Holotypus: Rel. 3, Table 2.

Diagnostic species: Parietaria judaica (dom.), Athamanta sicula, Antirrhinum siculum, Campanula erinus.

Description: It is a hemicryptophytic, sciophilous-nitrophilous, paucispecific formation, clearly dominated by Parietaria judaica, typical of cool and shady upper parts of walls (Fig. 3B). The association prefers the parts of walls with less eutrophication which mainly benefit from humidity and humus generated by percolation inside the embankment. Very few other species of Parietarietea (Ceterach officinarum, Antirrhinum siculum, etc.) are associated, except for Athamanta sicula (an endemic chasmophyte of the class Asplenietea trichomanis) and Campanula erinus (a therophyte species of the alliance Valantio-Galion muralis, order Geranio-Cardaminetalia), all with very sporadic presence. The elements of trampled areas, ruderal areas, and road margins (classes Polygono-Poetea annuae, Stellarietea mediae and alliance Bromo-Oryzopsion) that characterize the vegetation developing at the bases of walls (described above), are missing.

Syndynamism: The association plays a pioneer role in the colonization of walls and takes part in the shady-mesic geosigmetum of the Monte Pellegrino road system where it is north-facing.

It establishes the following contacts: a) Crepido bursifoliae-Parietarietum judaicae ass. nov. (lower parts of the walls); b) Diantho siculae-Helichrysetum panormitani ass. nov. (exposed parts of older, higher walls).

Synchorology: The phytocoenosis is frequent in the study area and probably has a wider distribution in Sicily and the Tyrrhenian area.

3) HELICHRYSO PANORMITANAE-HYPOCHAERIDETUM LAEVIGATAE ass. nov.

Phytosociological data: Table 3.

Holotypus: Rel. 3, Table 3.

Diagnostic species: Hypochaeris laevigata (dom.), Helichrysum panormitanum, Antirrhinum siculum.

Description: It is a chamaephytic-hemicryptophytic, sciophilous-nitrophilous formation dominated by Hypochaeris laevigata and associated, among other species, with the endemic Helichrysum panormitanum and Antirrhinum siculum, which are differentials of the phytocoenosis (Fig. 3C). In its typical aspect, the association is widespread mainly in the first 4-6 meters of rock and masonry walls, in cool and shaded areas of north-facing surfaces.

Syndynamism: The association plays a pioneer role in the colonization of walls and takes part in the shady-mesic geosigmetum of the road system. It establishes catenal contacts with the following coenoses: a) Athamanto siculae-Parietarietum judaicae ass. nov. (middle part of walls); b) Centranthetum rubri (less exposed vertical parts of walls); c) Diantho siculae-Helichrysetum panormitani ass. nov. (exposed parts of old higher walls).

Synchorology: The association was observed along the northern slope of Monte Pellegrino, but presumably it is present in other similar contexts of the mountains of the Palermo area.

4) CENTRANTHETUM RUBRI Oberd. 1969

Phytosociological data: Table 4.

Lectotypus: Rel. 16, Table 1, Oberdorfer (1969).

Diagnostic species: Centranthus ruber (dom.).

Description: It is a chasmo-nitrophilous heliophilous coenosis dominated by Centranthus ruber and located in the upper parts of less exposed walls and other masonry structures. The association prefers cooler habitats where it benefits from a certain amount of edaphic humidity due to water percolation inside the embankment.

Syndynamism: In the local area, this phytocoenosis belongs to the shady-mesic geosigmetum of the north-facing slope of the promontory located, in particular, on the more sheltered walls of the hairpin bends of Contrada Allaura. The association establishes catenal contacts with the following coenoses: a) Helichryso panormitanae-Hypochaeridetum laevigatae ass. nov. (near the base of old walls shaded by tree foliage); b) Diantho siculae-Helichrysetum panormitani ass. nov. (exposed upper parts of old walls, above 6-8 m); c) groupment with Rhamnus alaternus and Pistacia terebinthus (upper parts of walls at 4-6 m).

Synchorology: The association is spread across the Mediterranean area in the thermomediterranean and lower mesomediterranean bioclimatic belts, and is present in Sicily to some extent (Brullo and Guarino 2002). It is not frequent in the study areas, where it is only located on the northern slopes.

5) ANTIRRHINETUM SICULI Bartolo & Brullo 1986

Phytosociological data: Table 5.

Holotypus: Rel. 2, Table 3, Bartolo & Brullo (1986).

Diagnostic species: Antirrhinum siculum (dom.).

Description: It is a chasmo-nitrophilous paucispecific formation with an open structure, heliophilous and thermo-xerophilous, dominated by Antirrhinum siculum (Fig. 4B), an endemic species of Sicily and southern Italy, adapted to growing on masonry structures. The phytocoenosis mainly colonizes the upper parts of xeric stone, where it is located in poorly humified cracks.

Syndynamism: The phytocoenosis belongs to the more xeric geosigmetum of the study areas, where it is found mostly on the southern and western slopes. It comes into catenal contact with the following associations: a) Olopto miliacei-Pennisetetum setacei ass. nov. (both at the base of the walls and on the upper parts, in particular on guardwalls); b) Capparidetum rupestris (in the upper parts of some walls); Rhamno alaterni-Euphorbietum dendroidis Géhu and Biondi 1997 artemisietosum arborescentis subass. nov. (guardwalls of sunny and sheltered walls).

Synchorology: The association is endemic in the southern parts of the Italian Peninsula (Brullo et al. 2001; Brullo and Guarino 2002), Sicily (Bartolo and Brullo 1986; Gianguzzi 2007), and Malta (Brullo et al. 2020).

All.: ARTEMISIO ARBORESCENTIS-CAPPARIDION SPINOSAE Biondi, Blasi et Galdenzi in Biondi et al. 2014

Thermomediterranean chasmophytic vegetation of limestone walls of the Apennine Peninsula, Corsica, Sardinia, Sicily, and Malta.

6) CAPPARIDETUM RUPESTRIS O. Bolòs et Molinier 1958

Lectotypus: Rel. 1, Table 18, Bolòs & Molinier (1958).

Phytosociological data: Table 6.

Diagnostic species: Capparis spinosa (dom.).

Description: It is a chasmo-nitrophilous paucispecific formation with an open structure, heliophilous and xerophilous, dominated by large bushes of Capparis spinosa, typical of calcareous rocks and masonry walls (Fig. 4C). The phytocoenosis occupies the upper parts of old masonry walls and rock walls where it is located in sunny and xeric positions which are more or less sheltered and nitrified. In the road system investigated, it has mostly colonized the artificial rock slopes created by cutting into the limestone, in particular in the upper parts, over 4-5 m high on south-facing aspects.

Syndynamism: The phytocoenosis is a mature, permanent vegetation that grows on the most xeric geosigmetum of walls, located mostly on the southern slopes of the promontory. Here, it establishes catenal contacts with the following coenoses: a) Olopto miliacei-Pennisetetum setacei ass. nov. (both at the base of the walls and on the upper parts, in particular on the guardwalls); b) Antirrhinetum siculi (on the upper parts of some walls); c) Rhamno alaterni-Euphorbietum dendroidis Géhu & Biondi 1997 artemisietosum arborescentis subass. nov. (on sunny and sheltered guardwalls).

Synchorology: The association, described by De Bolós and Molinier (1958), is widespread in the Mediterranean area (Brullo and Guarino 2002) and, as reported by several authors, specifically in Sicily (Bartolo and Brullo 1986; Brullo et al. 1993; Gianguzzi 2007) and on the islands of Lampedusa (Bartolo et al. 1990) and Pantelleria (Gianguzzi 1999). In the study areas, it is frequently found along the roads on the slope of Contrada Arenella (Gianguzzi et al. 1996).

Cl.: ASPLENIETEA TRICHOMANIS (Br.-Bl. in Meier et Br.-Bl. 1934) Oberd. 1977

Chasmophytic vegetation of crevices, rocky ledges and faces of rocky cliffs and walls of Europe, North Africa, the Middle East, Arctic archipelagos and Greenland.

Ord.: ASPLENIETALIA GLANDULOSI Br.-Bl. in Meier & Br.-Bl. 1934

Thermo-mesomediterranean chasmophytic vegetation of sunny calcareous rock faces and crevices of the western Mediterranean.

All.: DIANTHION RUPICOLAE Brullo & Marcenò 1979

Siculo-Calabrian Tyrrhenian coasts and the islands of Malta.

7) DIANTHO SICULAE-HELICHRYSETUM PANORMITANI Gianguzzi ass. nov.

Phytosociological data: Table 7.

Holotypus: Rel. 5, Table 7.

Diagnostic species: Helichrysum panormitanum subsp. panormitanum (dom.), Dianthus rupicola, Micromeria fruticulosa, Antirrhinum siculum.

Floristic-syntaxonomical notes: Helichrysum panormitanum Guss. subsp. panormitanum (= H. rupestre (Raf.) DC. var. panormitanum (Guss.) Lojac.) is an endemic chasmophyte of the coastal capes to the west of Palermo, from Mt. Pellegrino to Castellammare del Golfo (Iamonico et al. 2016), which is linked to rupicolous environments in which it is considered an element of the Dianthion rupicolae alliance. The phytocoenosis in question is framed in the latter alliance, given the general physiognomy of vegetation clearly influenced by rupicolous species of the class Asplenietea. This is evident, above all, on the oldest walls which provide high and exposed cliff-like habitats.

Description: It is a chasmophilous, paucispecific, heliophilous, and mesophilous formation dominated by Helichrysum panormitanum subsp. panormitanum, typical of the highest parts of old walls, above 4-6 m. The association is located in sunny and xeric places which are not well nitrified, mainly on the north-facing walls and rarely on natural or artificial rocky cliffs. Species of the class Parietarietea judaicae (Ceterach officinarum, Parietaria judaica, Antirrhinum siculum, Capparis spinosa), with low coverage values, as well as several elements of the class Asplenietea trichomanis (Dianthus rupicola, Lomelosia cretica, Matthiola incana subsp. rupestris, Seseli bocconei, etc.) are associated with it. The community forms dense vegetation belts due to thick patches of the dominant species covering the cracks between the stone blocks.

Syndynamism: The association is well represented in the shady-mesic geosigmetum of the road stretches located in the north/northwest-facing slopes of the promontory. It establishes contacts with the following phytocoenoses: a) Helichryso panormitanae-Hypochaeridetum laevigatae ass. nov. (at the base of walls shaded by the crowns of trees); b) Centranthetum rubri (at the base of sunny walls); c) Rhamnus alaternus and Pistacia terebinthus groupment (upper parts of the highest walls).

Synchorology: The phytocoenosis is spread along the entire road system of Monte Pellegrino, especially on the highest and most exposed stretches of the northern and western sides (via Monte Ercta).

8) SCABIOSO CRETICAE-CENTAURETUM UCRIAE Brullo et Marcenò 1979 subass. TYPICUM

Phytosociological data: Table 8.

Holotypus: Rel. p. 139, in Brullo et Marcenò (1979).

Diagnostic species: Lomelosia cretica (dom.), Helichrysum panormitanum, Euphorbia bivonae subsp. bivonae, Centaurea panormitana (= C. ucriae Lacaita), Convolvulus cneorum, Dianthus rupicola, Seseli bocconei, Silene fruticosa, Iberis semperflorens.

Description: It is a chasmophilous, heliophilous, and mesophilous formation, widespread on the upper parts of cliffs and rocky cut slopes, more or less shaded, dominated by Lomelosia cretica.

Syndynamism: Pioneer vegetation that plays an edaphoclimatic role in the colonization processes of fresh and humid artificial rocky cut slopes and natural cliffs. In fact, on slopes shaped by the excavation of limestone that have been left undisturbed, the chasmophytic association appears naturally restored. It is in catenal contact with the following associations: a) Helichryso panormitanae-Hypochaeridetum laevigatae ass. nov. (at the base of shady and nitrified walls); b) Olopto miliacei-Pennisetetum setacei ass. nov. (at the base of sunny and xeric walls); grasslands associated with Penniseteto setacei-Hyparrhenietum hirtae and aspects of the Ruto-Oleo sylvestris sigmetum located on the slopes above the road system (Fig. 4D).

Synchorology: This phytocoenosis is frequent on the cliffs and cut slopes of Monte Pellegrino. It is also widespread in the mountains of Palermo and Trapani areas (up to 900 m a.s.l.) and has been reported for small and isolated locations in the Nebrodi Mountains at Rocche del Crasto (Brullo and Marcenò 1979).

Cl.: STIPO-TRACHYNIETEA DISTACHYAE S. Brullo in S. Brullo et al. 2001

Mediterranean calciphilous annual and ephemeroid swards and grasslands

Ord.: BRACHYPODIETALIA DISTACHYI Rivas-Mart. 1978

Western Mediterranean ephemeral winter pastures on shallow sandy and loamy soils over limestone, dolomite, and gypsum.

All.: HYPOCHOERIDION ACHYROPHORI Biondi & Guerra 2008

Annual community, xerophytic, pioneer, basiphilous, of the European Central Mediterranean area in the thermomediterranean and mesotemperate bioclimatic belts. It is part of the Trachynion distachyae alliance of the western Mediterranean, and reaches its western distribution limit in the Mediterranean area around Provence.

9) Groupment with STIPELLULA CAPENSIS

Phytosociological data: Table 9.

Diagnostic species: Stipellula capensis (dom.).

Description: Therophytic heliophilous and xerophilous formation, with spring phenology, growing in the soil accumulated on the tops of old guardwalls on the road margin (parapets) due to deterioration caused by weathering events. The phytocoenosis is physiognomically dominated by Stipellula capensis, which is associated with other ephemeral species.

Syndynamism: Pioneer vegetation mainly related to the more xeric geosigmetum of the road system. It is in catenal contact with ruderal and wall formations, such as the Olopto miliacei-Pennisetetum setacei ass. nov.

Synchorology: Stipellula capensis vegetation is quite widespread in Sicily (Brullo et al. 2000; Gianguzzi and La Mantia 2008), although it has been little investigated from a phytosociological point of view.

Cl.: ARTEMISIETEA VULGARIS Lohmeyer et al. in Tx. Ex von Rochow1951

Perennial (sub)xerophilous ruderal vegetation of the temperate and submediterranean regions of Europe.

Ord. : ELYTRIGIO REPENTIS-DITTRICHIETALIA VISCOSAE Mucina in Mucina et al. 2016

Anthropogenic sub-ruderal and ruderal grasslands and herblands of submediterranean and Mediterranean Southern Europe.

All.: BROMO-ORYZOPSION MILIACEAE O. Bolòs 1970

Thermomediterranean sub-ruderal perennial grasslands on disturbed road margins of the Mediterranean.

10) OLOPTO MILIACEI-PENNISETETUM SETACEI Gianguzzi ass. nov.

Phytosociological data: Table 21 in Gianguzzi et al. 1996.

Synonym: Penniseto setacei-Hyparrhenietum hirtae var. with Oryzopsis miliacea (L.) Asch. & Schweinf (in Gianguzzi et al. 1996).

Holotypus : Rel. 1, Table 21, in Gianguzzi et al. (1996, p. 104).

Diagnostic species: Pennisetum setaceum (dom.), Oloptum miliaceum (= Oryzopsis miliacea), Lobularia maritima, Foeniculum vulgare subsp. piperitum, Sixalis atropurpurea subsp. maritima.

Floristic-syntaxonomical notes: Pennisetum setaceum, native of the Middle East and the Arabian Peninsula, has now become thermo-cosmopolite (EPPO 2020) and an invasive alien species that is widespread in the Mediterranean area (D’Amico and Gianguzzi 2006; Pasta et al. 2010). In Sicily, the first record of Pennisetum setaceum referred precisely to Monte Pellegrino (Pignatti-Wikus 1963), followed by numerous others that highlighted a constant increase in its distribution across the region (Gianguzzi et al. 1996; D’Amico and Gianguzzi 2006). On the carbonate outcrops of the study area, nowadays it forms large and stabilized grasslands (Fig. 4E) related to the Penniseto setacei-Hyparrhenietum hirtae association (Gianguzzi et al. 1996) – of the Hyparrhenion hirtae alliance, order Cymbopogono-Brachypodietalia ramosi, class Lygeo-Stipetea that belongs to the oleaster series (Gianguzzi and Bazan 2019, 2020; Gianguzzi et al. 2020). Over time, it has replaced the vegetation with Hyparrhenia hirta, mostly in the thermomediterranean bioclimatic belt (Gianguzzi et al. 1996). In fact, Pennisetum setaceum is a strongly competitive species and creates a linear aspect of vegetation along the road margins, previously ascribed to a variant with Oloptum miliaceum (sub Oryzopsis miliacea; Gianguzzi et al. 1996) of the above-mentioned association. However, this second case consists of a nitrophilous-ruderal coenosis ascribable to the Bromo-Oryzopsion miliaceae alliance. As highlighted by Mucina et al. (2016), "... the position of this alliance is contentious. Rivas-Martínez et al. (1999) placed this alliance in the Agropyretalia repentis and only three years later Rivas-Martínez (2002) re-classified this unit within the Carthametalia lanati. Biondi et al. (2001) gave preference to the Brachypodio ramosi-Dactylidetalia. In any case, these conflicting opinions have been obviously motivated by the transitional character of the unit that straddles the border between pseudosteppes and ruderal grass-rich vegetation". On this basis, the description of the new syntaxon in question is deemed appropriate (art. 24b, code of phytosociological nomenclature).

Description: It is a hemicryptophytic, thermo-xerophilous and paucispecific formation, whose physiognomy is dominated by Pennisetum setaceum which forms a continuous vegetation belt located along the road margins in the more xeric and sunny parts (Figs 3D, 4E). Compared to Penniseto setacei-Hyparrhenietum hirtae – related to rocky limestone slopes – the phytocoenosis in question is different in its poorer floristic composition and the frequency of the above-mentioned ruderal species that are indicated among the typical characteristics (Gianguzzi et al. 1996).

Syndynamism: The association belongs to the more xeric geosigmetum of the road system. In the absence of maintenance works, it tends to colonize the edges of walls that act as parapets, where it is located both inside and outside the road surface, and sometimes also on top. The association is in catenal contact with the following coenoses: a) Trachynia distachya groupment (therophytic grassland located in the soil accumulations among the clumps); b) Capparidetum rupestris (chasmo-nitrophilous vegetation of the upper parts of sunny and sheltered walls); c) Rhamno alaterni-Euphorbietum dendroidis Géhu & Biondi 1997 artemisietosum arborescentis subass. nov. (guardwalls of sunny and sheltered parts of the road system).

Synchorology: The phytocoenosis is widespread in the study area, especially along the most xeric parts of the southern and western slopes of the promontory. It is booming in Sicily, mostly along the roads and railways of the coastal belt and, in some cases, in the interior (Gianguzzi et al. 1996, D’Amico and Gianguzzi 2006). This is due to the peculiarity of the seeds (high quantity and high germinability), the anemophilous dissemination (spread over long distances), the biological characteristics of the plant (thick clumps resistant to fires that take space and light from other herbaceous plants) and, in addition – probably – climatic changes.

Cl.: QUERCETEA ILICIS Br.-Bl. in Br.-Bl., Roussine & Nègre 1952

Thermo-mesomediterranean pine and oak forests and associated Mediterranean maquis.

Ord.: PISTACIO LENTISCI-RHAMNETALIA ALATERNI Rivas-Martínez 1975

Thermo-mesomediterranean low-growth matorral, maquis, and garrigue of the Mediterranean Basin.

All.: OLEO SYLVESTRIS-CERATONION SILIQUAE Br.-Bl. ex Guinochet et Drouineau 1944

Thermomediterranean calcicolous maquis of the Liguro-Tyrrhenian seaboards.

11) RHAMNO ALATERNI-EUPHORBIETUM DENDROIDIS Géhu & Biondi 1997 ARTEMISIETOSUM ARBORESCENTIS subass. nov.

Phytosociological data: Table 10.

Holotypus: Rel. 5, Table 10.

Diagnostic species: Euphorbia dendroides (dom.), Artemisia arborescens, Pennisetum setaceum.

Syntaxonomic notes: The scrub vegetation with Euphorbia dendroides of Sicily is referred to the association Rhamno alaterni-Euphorbietum dendroidis Géhu & Biondi 1997 (= Oleo-Lentiscetum euphorbietosum Molinier 1954; Oleo-Euphorbietum dendroidis Trinajstic 1974; Oleo-Euphorbietum dendroidis Trinajstic 1975), divided into the following subassociations, to be considered as geographic vicariants: a) subass. typicum; b) subass. phlomidetosum fruticosae (Brullo & Marcenò 1985) Gianguzzi et al. 2016 (with Phlomis fruticosa L.), on gypsic substrates of the hinterland of Sicily; c) euphorbietosum bivonae (Gianguzzi, Ilardi & Raimondo 1996) Gianguzzi et al. 2016 (with Euphorbia bivonae), on limestone-dolomitic rocks of Palermo area, Trapani area and near Sciacca; d) rhamnetosum oleoidis (Brullo & Marcenò 1985) Gianguzzi et al. 2016 [with Rhamnus lycioides L. subsp. oleoides (L.) Jahand and Maire], on calcareous, marly and calcarenitic substrates of Trapani and Agrigento are and Egadi Islands (Gianguzzi et al. 2006); e) celtidetosum aetnensis (Brullo & Marcenò 1985) Gianguzzi et al. 2016 [Celtis tournefortii Lam. subsp. aetnensis (Tornab.) Raimondo & Schicchi], on calcareous debris cones of the Sicani Mountains (Gianguzzi et al. 2014a, 2014b). A further xero-nitrophilic vicariant was detected in the study area and diversified by the frequency of Artemisia arborescens, proposed as a new subassociation.

Description: Thermo-xerophilous, heliophilous, and nitrophilous, paucispecific maquis formations, clearly dominated by Euphorbia dendroides, associated with Artemisia arborescens and Pennisetum setaceum, with high cover values. The phytocoenosis is typical of warm, sunny, and xeric slopes on carbonate substrata and tends generally to colonize anthropogenic habitats. In particular, it is spread on old walls and ruins.

Syndynamism: In the road system in question, the phytocoenosis takes part in the more xeric geosigmetum, related to the road margins of the southern and western slopes of the promontory (Fig. 4F). It forms nitrophilous-xerophilous maquis vegetation located on the upper parts of guardwalls, sometimes covering them. The association is catenal with the following: a) Olopto miliacei-Pennisetetum setacei ass. nov. (road margin vegetation of Pennisetum setaceum); b) Antirrhinetum siculi (on not very high walls); c) Capparidetum rupestris (upper parts of sunny and sheltered walls).

Synchorology: The phytocoenosis was mainly detected along the more xeric parts of the road system on the southern and western sides of the promontory.

12) TEUCRIO FLAVI-RHOETUM CORIARIAE Gianguzzi ass. nov.

Phytosociological data: Table 11.

Synonym: Groupment with Rhus coriaria (in Gianguzzi et al. 1996); Clematido cirrhosae-Rubetum ulmifolii subass. rhoetosum coriariae Gianguzzi & La Mantia 2008 (in Gianguzzi and La Mantia 2008).

Holotypus: Rel. 2, Table 11.

Diagnostic species: Rhus coriaria (dom.), Teucrium flavum subsp. flavum, Bituminaria bituminosa.

Floristic-syntaxonomical notes: Rhus coriaria is a species with a southern range (Pignatti 1982; Pignatti et al. 2017) that is widespread from the Canary Islands to the Middle East (Davis 1967; Tutin et al. 1968; Kurucu et al. 1993; Bloshenko and Letchamo 1995). It is quite common in Italy, as well as in Sicily, as a residue of ancient crops for the extraction of tannins. In the interior of Italy, it is widespread in the thermo-mesomediterranean belt where it forms frutescent formations, more or less dense, tendentially monospecific, related to arid slopes, screes, hedges, and abandoned structures (Gianguzzi and La Mantia 2008). From a phytosociological point of view, it is little studied and not well known. Some shrubby aspects, spread across the coastal slopes of Palermo and Trapani areas, have been attributed to the order Prunetalia spinosae Tx. 1952 (Gianguzzi et al. 1996; Gianguzzi and La Mantia 2008). A specific association (Cercido siliquastri-Rhoetum coriariae Biondi, Allegrezza & Guitian 1988) was described for the central Apennines (Biondi et al. 1988) and ascribed to the same order of the class Crataego-Prunetea Tx. 1962 (Cytision sessilifolii Biondi 1988). The association in question – according to other authors (Varol et al. 2006; Karaer et al. 2010; Donmez et al. 2015) who have recognized the structural role of Rhus coriaria in the xeric shrubby vegetation of Anatolian Peninsula – has been linked to the order Pistacio-Rhamnetalia alaterni of the class Quercetea ilicis.

Description: It is a shrubby, paucispecific, xerophilous, heliophilous formation, sometimes shady, dominated by Rhus coriaria, which is associated with other elements of the Oleo-Ceratonion alliance (Euphorbia dendroides, Olea europaea var. sylvestris, and Teucrium fruticans) and other sporadic species of the order Pistacio-Rhamnetalia alaterni. On this basis, it is here proposed as a new association belonging to these syntaxa. The coenosis is related to rocky slopes with poor soil, screes, and outcrops of carbonate nature (limestone, dolomite, marl, etc.). In the study area, it extends to the road margins and road cut slopes (Fig. 3E).

Syndynamism: The phytocoenosis covers the detritic slopes of the reliefs of carbonate nature. It is a secondary aspect of the holm oak series of Rhamno alaterni-Querco ilicis pistacio terebinthi sigmetosum (Brullo and Marcenò 1985; Gianguzzi et al. 1996; Brullo et al. 2008).

Along the road system of Monte Pellegrino, it belongs to the shady-mesic geosigmetum related to the slopes above the roads. Here, it comes in catenal contact with the following coenoses: a) Helictotricho convoluti-Ampelodesmetum mauritanici Minissale 1994 (Ampelodesmos mauritanicus grassland); b) Rhamno alaterni-Quercetum ilicis Brullo and Marcenò 1985 subass. pistacietosum terebinthi Gianguzzi et al. 1996 (chasmo-nitrophilous vegetation of the upper parts of walls in sunny locations, sheltered from cold winds).

Synchorology: This vegetation is frequent on the northern and western sides of Monte Pellegrino, in the Allaura area (Gianguzzi et al. 1996). Other similar aspects are widespread along the northern slopes of the mountains of Palermo area, up to Monte Cofano in the province of Trapani (Gianguzzi and La Mantia 2008).

13) Groupment with RHAMNUS ALATERNUS and PISTACIA TEREBINTHUS

Phytosociological data: Table 12.

Diagnostic species: Rhamnus alaternus (dom.), Pistacia terebinthus.

Description: It is a maquis or scrub formation dominated by Rhamnus alaternus and Pistacia terebinthus, associated with other species of the order Pistacio-Rhamnetalia alaterni. This vegetation is linked to the upper parts of old walls (5-10 m high) located on the cool and shady slopes of Contrada Allaura, whose toponym refers to the presence of Laurus nobilis, a species quite widespread in Sicily (Marino et al. 2014). Thanks to the lack of maintenance work, it tends to colonize the downhill-side of the roads. It creates a border 2-3 meters high, which in some cases overhangs the same walls that act as guardwalls. In fact, the roots of woody plants penetrate through the base of the walls into the fill slopes and road bed (Fig. 3F).

Syndynamism: It belongs to the shady-mesic geosigmetum of the road system linked to the northern face of Monte Pellegrino. It is in catenal contact with the following coenoses: a) Helichryso panormitanae-Hypochaeridetum laevigatae ass. nov. (on lower shady walls); b) Centranthetum rubri (on stretches of cool and sheltered walls); c) Diantho siculae-Helichrysetum panormitani ass. nov. (on the upper parts of the highest walls).

Synchorology: The vegetation was identified on the northern slopes of Monte Pellegrino, where it forms vegetation strips linked to the upper parts of old retaining walls. Although the phytocoenosis is not very abundant in the area, it has an important documentary value.

The resulting dataset is composed of 185 taxa divided into 95 samples (relevés). The mean value of the floristic richness is 30 taxa for the retaining wall communities. The most species-rich of the wall communities are the Diantho rupicolae-Helichrysetum panormitani (58 taxa), Crepido bursifoliae-Parietarietum judaicae (38 taxa), and Helichryso panormitanae-Hypochaeridetum laevigatae (36 taxa). These are followed by Capparidetum rupestris, Antirrhinetum siculi, Athamanto siculae-Parietarietum judaicae, and Centranthetum rubri, with 25, 19, 16, and 15 taxa, respectively.

The Stipellula capensis guardwall groupment includes 28 taxa. In the road margins, the richest communities are the Rhamno alaterni-Euphorbietum dendroidis (52 taxa) and Olopto miliacei-Pennisetetum setacei (49 taxa), while the Rhamno alaterni-Euphorbietum dendroidis and the groupment with Rhamnus alaternus and Pistacia terebinthus have 22 and 18 taxa, respectively. The overall mean value for the road margin communities is 35 taxa. The Scabioso creticae-Centaureetum ucriae of the road cut slopes is the phytocoenosis with the highest species richness (61 taxa), comparable only to Diantho rupicolae-Helichrysetum panormitani.

Species nestedness (the average co-occurrence of species, Table 13) is 8.3 among all the communities of the road system, 8.6 among the retaining wall species, and 10 among the road margin species.

The “Jaccard similarity Index” (Table 14) shows a clear differentiation among phytocoenoses (mean value = 0.15). The mean index values of the vegetation is 0.23 for wall vegetation and 0.19 for road margin vegetation. High values of nestedness (45) and Jaccard’s Index (0.61) are observed for Diantho rupicolae-Helichrysetum panormitani and Scabioso creticae-Centauretum ucriae.

The results obtained from detrended correspondence analysis show a clear distribution of communities. The ordination plot (Fig. 5) shows 95 plots grouped in 13 clusters which are quite distinct from floristic and ecological points of view. The compositional turn-over (the measure of beta diversity; Whittaker 1960) across relevés is 6.51. The wall vegetation plots (phytocoenoses 1-7) are spread over the right part of the ordination diagram. The cluster Diantho rupicolae-Helichrysetum panormitani (7) overlaps with the cluster of Scabioso creticae-Centauretum ucriae (8) of the road cut slopes. The road margin vegetation (from 10 to 13) is placed on the left part of the diagram, while the guardwall vegetation is on the opposite extreme (9). The distribution of communities in the ordination diagram shows an ecological gradient in term of environmental nitrophilia along the second axis.

From a structural point of view, the life form analysis (Table 15) shows the dominance of Hemicryptophytes in the communities linked to the shaded parts of the walls (Crepido-Parietarietum, Athamanto-Parietarietum, Helichryso-Hypochaeridetum) and the vegetation of the road margins (Olopto-Pennisetetum and groupment with Rhamnus and Pistacia). Chamaephytes are dominant in the communities on exposed parts of the walls (Centranthetum, Antirrhinetum and Diantho-Helichrysetum) and the vegetation of road cut slopes (Scabioso-Centauretum). Nanophanerophytes are dominant in Capparidetum and Teucrio-Rhoetum, while phanerophytes are dominant in Rhamno-Euphorbietum. The guardwall groupment with Stipellula is physiognomized by therophytes.