The Role of Climate and Topography in Shaping the Diversity of Plant Communities in Cabo Verde Islands

diversity Review The Role of Climate and Topography in Shaping the Diversity of Plant Communities in Cabo Verde Islands Carlos Neto 1, JoséCarlos Costa 2, Albano Figueiredo 3, Jorge Capelo 2, Isildo Gomes 4, Sónia Vitória 5, JoséMaria Semedo 5, António Lopes 1, Herculano Dinis 6, Ezequiel Correia 1, Maria Cristina Duarte 7and Maria M. Romeiras 2,7,* 1Centre for Geographical Studies, Institute of Geography and Spatial Planning (IGOT), Universidade de Lisboa, Rua Branca Edmée Marques, 1600-276 Lisboa, Portugal; [email protected] (C.N.); [email protected] (A.L.); [email protected] (E.C.) 2Linking Landscape, Environment, Agriculture and Food (LEAF), Instituto Superior de Agronomia (ISA), Universidade de Lisboa, 1349-017 Lisboa, Portugal; [email protected] (J.C.C.); [email protected] (J.C.) 3Centre of Studies in Geography and Spatial Planning (CEGOT), Department Geography and Tourism, University of Coimbra, Colégio de São Jerónimo, 3004-530 Coimbra, Portugal; [email protected] 4 Instituto Nacional de Investigaç ã o e Desenvolvimento Agr á rio (INIDA), Santiago, S ã o Lourenço dos Org ã os CP 84, Cape Verde; [email protected].cv 5Campus do Palmarejo, Faculdade de Ciências e Tecnologia, Universidade de Cabo Verde, CP 279, Praia, Santiago CP 279, Cape Verde; [email protected].edu.cv (S.V.); [email protected] (J.M.S.) 6 Direç ã o Nacional do Ambiente (DNA-CV) & Associaç ã o Projecto Vit ó , CP 47, Xaguate, S. Filipe, Ilha do Fogo CP47, Cape Verde; [email protected] 7 Centre for Ecology, Evolution and Environmental Changes (cE3c), Faculdade de Ci ê ncias, Universidade de Lisboa, 1749-017 Lisboa, Portugal; [email protected] *Correspondence: mmr[email protected] Received: 19 January 2020; Accepted: 15 February 2020; Published: 19 February 2020   Abstract: The flora and vegetation of the archipelago of Cabo Verde is dominated by Macaronesian, Mediterranean, and particularly by African tropical elements, resulting from its southernmost location, when compared to the other islands of the Macaronesia (i.e., Azores, Madeira, Selvagens, and Canary Islands). Very likely, such a geographical position entailed higher susceptibility to extreme climatic fluctuations, namely those associated with the West African Monsoon oscillations. These fluctuations led to a continuous aridification, which is a clear trend shown by most recent studies based on continental shelf cores. Promoting important environmental shifts, such climatic fluctuations are accepted as determinant to explain the current spatial distribution patterns of taxa, as well as the composition of the plant communities. In this paper, we present a comprehensive characterization of the main plant communities in Cabo Verde, and we discuss the role of the climatic and topoclimatic diversity in shaping the vegetation composition and distribution of this archipelago. Our study reveals a strong variation in the diversity of plant communities across elevation gradients and distinct patterns of richness among plant communities. Moreover, we present an overview of the biogeographical relationships of the Cabo Verde flora and vegetation with the other Macaronesian Islands and northwestern Africa. We discuss how the distribution of plant communities and genetic patterns found among most of the endemic lineages can be related to Africa’s ongoing aridification, exploring the impacts of a process that marks northern Africa from the Late Miocene until the present. Keywords: vegetation; aridification in NW Africa; Macaronesian islands; distribution patterns; West African Monsoon (WAM); vascular flora Diversity 2020,12, 80; doi:10.3390/d12020080 www.mdpi.com/journal/diversity Diversity 2020,12, 80 2 of 16 1. Introduction The study of deep-sea cores from the West African coast conducted in recent decades, in parallel with studies of the paleolakes that characterized the wet periods of the present Sahara desert (green Sahara Periods, or GSPs), and sedimentary structures associated with ancient rivers brought a new understanding of the history of West and North African vegetation [ 1 – 4 ]. Results from pollen sequences, which were used as proxies for flora and vegetation spatial patterns, were combined with data concerning dust carried from the Sahara desert, supporting the inference of paleoclimatic conditions, namely the influence of atmospheric circulation systems such as the West African Monsoon (WAM) and trade winds [ 5 ], and with changes in hydrology of the Sahara desert [ 6 ]. Such results are of critical importance to set the origin of Cabo Verde’s flora and vegetation and clarify their relationships with the remaining flora and vegetation of northwestern Africa and the Mediterranean Basin. The Atlantic archipelagos originated from mid-Tertiary volcanic cycles, spreading from 40 ◦ to 15 ◦ N along the coasts of Europe and Africa, are known as Macaronesia, or “the Fortunate Islands”: Azores, Madeira, Selvagens Islands, Canary Islands, and Cabo Verde (Figure 1). The almost linear geographical disposition of the archipelagos, and their approximately parallel position in relation to the African and European mainland, creating a chain of islands, are paramount to hypotheses explaining “Macaronesian” flora and vegetation features, namely colonization, dispersion, and speciation events [7]. Diversity 2019, 11, x 4 of 16 Figure 1. Cabo Verde location, with details of the Macaronesian Region. The orographic convection that occurs when the flow reaches the islands with the most vigorous reliefs reinforces the cloud thickness, which dissipates rapidly leeward due to the foehn effect, resulting in a clear dissymmetry between the northern and southern slopes. Windward areas experience a significant number of foggy days, not only at higher altitudes (e.g., Santiago Island, Serra da Malagueta, and Pico da Antónia: 1000–1300 m, about 200 days/year on average), but also in lower areas (e.g., S. Jorge dos Orgãos: 320 m, about 180 days/year). On leeward areas, there are significantly fewer foggy days (e.g., Curralinho: 950 m, 100 days/year; Assomada plateau: 550 m, 15 days/year) [21]. The high frequency of clouds, besides reducing the amount of solar radiation reaching the surface, considerably increases the water availability in these areas through the interception of cloud droplets and the increase of condensation nuclei. Since the 1960s, various cloud water-harvesting experiments have been conducted on the highest sectors of Santo Antão, São Vicente, São Nicolau, Santiago, Fogo, and the Brava islands. The results show that the horizontal precipitation far outweighs vertical precipitation, more than doubling it in some cases [23], which is a volume similar to that recorded in other Macaronesian Islands [24,25]. Although the seasonal rhythm of horizontal precipitation is similar to that of vertical precipitation, with the highest values during the rainy season, its ecological significance is greater between November and March. During the dry season, as much as 100 mm were monthly recorded at Serra da Malagueta [26], between 40 and 100 mm at Pero Dias (Santo Antão) and 176 to 1029 mm at Campo das Fontes (Brava) [27]. According to the Worldwide Bioclimatic Classification system of Rivas-Martínez et al. [28], Cabo Verde’s bioclimate ranges from tropical hyperdesertic to pluviseasonal, upper infra to low supratropical, and upper ultrahyperarid to upper dry, and it is occasionally subhumid (Supplementary Materials, Table S1). 3. Plant Communities of Cabo Verde Spatial differences in the amount of precipitation, structured by topographic determinants (altitude and aspect), become evident when comparing the flatter eastern islands (i.e., Sal, Boavista, Maio), where the climate is arid, with the most mountainous islands (Santo Antão, São Nicolau, Fogo, Santiago, Brava), where a semiarid and dry bioclimatic pattern in the south-facing slopes, dominated by African floristic elements of savannoid or predesert character, are replaced by more humid conditions on the north/northeast-facing slopes, creating a significant climatic asymmetry [28,29]. To find a reasonably effective model to understand Cabo Verde’s flora and vegetation chorology, we must add the influence of successive volcanic eruptions to the atmospheric circulation model and Figure 1. Cabo Verde location, with details of the Macaronesian Region. In the continental areas surrounding Tethys, several violent disruptive environmental events took place during the mid and late Tertiary. The orogenic events associated with the alpine tectonic cycle and the onset of a summer-dry Mediterranean climate led to dramatic changes, extinctions, and novel evolutionary pressures on plant species and vegetation of those areas [ 8 ]. In this context, a global opportunity for the establishment of new migrant floras appeared, either from central Eurasia (neomediterranean) or high northern latitudes (Artho-Tertiary deciduous flora) [ 8 ]. Oceanic islands were not significantly affected by such complex phenomena during the Tertiary period, thus retaining part of the paleo-subtropical vegetation in relatively high latitudes. However, spatial changes of distribution took place, very likely contributing to the definition of low-saturated habitats, which is a feature also triggered by volcanic events, promoting windows for colonization [ 9 , 10 ] by creating suitable conditions for new founders [ 11 ] that very often went through a process of speciation by adaptive radiation [ 12 ]. In fact, biogeographical relationships, mostly with the Mediterranean and African mainland areas, were conditioned by long-range dispersal events. Diversity 2020,12, 80 3 of 16 Meanwhile, extensive speciation phenomena were taking place, which were rooted on both the ancestors from the Tertiary elements and the later newcomers from the continental areas [ 12 ]. Traditionally, the native vegetation and high prevalence of endemic elements in these islands were interpreted as relicts [ 13 ] of the subtropical Tertiary vegetation, the ‘Geoflora vegetation’, around the archaic Tethys basin (coarsely the Mediterranean Sea, spreading eastwards to include the present Black and Aral seas, reaching the Indian Ocean). This interpretation is challenged by increasing molecular and phylogeographical evidences [ 14 , 15 ] supporting the derived neoendemic synapomorphic character. This is the case of woody endemics in taxonomical groups that normally present an herbaceous habit in continental areas, which is one of the most striking attributes in the floras of the Atlantic islands [ 14 ]. In fact, the woody habit is significant among the endemics, since several genera, subgenera, or sections underwent speciation in one or in several archipelagos, namely the Asteraceae (e.g., Asteriscus, Pericallis, Sonchus, Tolpis), Boraginaceae (Echium), Campanulaceae (Musschia in Madeira, Azorina in the Azores, Canarina in the Canary Islands, and Campanula in Cabo Verde), Scrophulariaceae (Isoplexis) and others such as Sideritis, Plantago, and Aeonium (respectively, Lamiaceae, Plantaginaceae, and Crassulaceae). These plants exhibit consistent habit and structure features, namely being rosulate, monocarpic, or candelabra-shaped, exhibiting the so-called “island-woodiness” effect [ 16 ]. Other important groups encompassing Cabo Verde vegetation are paleo-Mediterranean thermophilous sclerophylls, such as spurges Euphorbia (sect. Aphyllis) and Sideroxylon. The latter lineage has circum-Mediterranean–African–Arabic affinities (Rand Flora) and reached the islands in several cycles of colonization. Rand Flora are floristic elements of taxonomical non-sister clades that are consistently found with a correlated distribution area around the peripheral borders of the whole African continent, including areas surrounding the Mediterranean and Red Seas, with no obvious relationship with inland African continental flora [ 17 ]. Such context explains why Cabo Verde’s flora combines significant Macaronesian radiations (e.g., Aeonium, Echium, Tolpis, and Sonchus) with continental African elements (e.g., Acacia, Dichrostachys, Ficus, Ziziphus, and Andopogoneae grasses). In short, Cabo Verde’s flora can be coarsely grouped into five types: (1) Paleoendemic paleosubtropical forest flora of tethysian origin; (2) Neoendemic Macaronesian flora with island woodiness physiognomy; (3) Paleo-Mediterranean xeric to semi-desert, sclerophyllous, or succulent flora; (4) Continental African flora; and (5) Flora introduced since the human colonization of these islands, more than 500 years ago. 2. Cabo Verde Islands: Origin and Climate The Cabo Verde archipelago is composed of 10 main islands and several islets (Figure 1). The islands account for 4033 km 2 of total land area and are grouped into two main sets according to prevailing NE winds: The Windward islands—Santo Ant ã o, S ã o Vicente, Santa Luzia (the only uninhabited main island), S ã o Nicolau, Sal, and Boavista—and Leeward islands: Maio, Santiago, Fogo, and Brava. The genesis of the Cabo Verde archipelago is associated with intravolcanic plaque processes. According to some authors, who defend its origin from mantle plumes (hotspot) [ 18 ], there is a submerged crest connection between the Cabo Verde and Canary archipelagos, which also have a similar nature of volcanic episodes. Hotspot activity started around 19 to 22 Ma, resulting in a large crustal uplift zone (Cabo Verde Swell) where the Cabo Verde islands are placed [ 19 ], and volcanic activity remains until present days. The topography is generally very rugged, associated with high massifs of volcanic origin, with well-preserved volcanic apparatuses, namely cones, craters, boilers (e.g., Ch ã das Caldeiras in Fogo and Cova in Santo Ant ã o), and deep valleys. The island of Fogo reaches the highest elevation at 2829 m, followed by Santo Ant ã o, Santiago, and S ã o Nicolau with 1979 m, 1392 m, and 1304 m, respectively [ 20 ]. Due to its northern position relative to the oscillation zone of the ITCZ (Intertropical Convergence Zone), Cabo Verde has a dry tropical climate with two well-marked seasons (humid and dry) conditioning the distribution of its flora and vegetation. However, the island topography contributes to significant spatial variations with altitude and exposure to prevailing winds, leading to contrasting Diversity 2020,12, 80 4 of 16 weather conditions. South blowing wind during the few ITCZ passages north of the archipelago brings tropical humid air masses and heavy rainfall associated to the West African Monsoon (WAM); in contrast, northeast winds, mainly in the dry season, carry hot and dry air masses (Saharan): The Harmattan season [21]. For most of the year, and almost exclusively between December and June, Cabo Verde is under the influence of the eastern sector of the Azorean subtropical high-pressure cell, which is the origin of the boreal trade winds. The oceanic course of the air mass and the vertical structure is marked by a clear thermal inversion, whose base is on average between 380 and 850 m, and the top at about 1400 m [ 22 ], favors the formation of stratiform cloud banks. The persistence of cloud banks, which is prompted by trade wind inversion on the north and northeast slopes on islands of wider altitudinal ranges, smoothens the characteristic dryness of the archipelago. The orographic convection that occurs when the flow reaches the islands with the most vigorous reliefs reinforces the cloud thickness, which dissipates rapidly leeward due to the foehn effect, resulting in a clear dissymmetry between the northern and southern slopes. Windward areas experience a significant number of foggy days, not only at higher altitudes (e.g., Santiago Island, Serra da Malagueta, and Pico da Ant ó nia: 1000–1300 m, about 200 days/year on average), but also in lower areas (e.g., S. Jorge dos Org ã os: 320 m, about 180 days/year). On leeward areas, there are significantly fewer foggy days (e.g., Curralinho: 950 m, 100 days/year; Assomada plateau: 550 m, 15 days/year) [21]. The high frequency of clouds, besides reducing the amount of solar radiation reaching the surface, considerably increases the water availability in these areas through the interception of cloud droplets and the increase of condensation nuclei. Since the 1960s, various cloud water-harvesting experiments have been conducted on the highest sectors of Santo Ant ã o, S ã o Vicente, S ã o Nicolau, Santiago, Fogo, and the Brava islands. The results show that the horizontal precipitation far outweighs vertical precipitation, more than doubling it in some cases [ 23 ], which is a volume similar to that recorded in other Macaronesian Islands [ 24 , 25 ]. Although the seasonal rhythm of horizontal precipitation is similar to that of vertical precipitation, with the highest values during the rainy season, its ecological significance is greater between November and March. During the dry season, as much as 100 mm were monthly recorded at Serra da Malagueta [ 26 ], between 40 and 100 mm at Pero Dias (Santo Ant ã o) and 176 to 1029 mm at Campo das Fontes (Brava) [27]. According to the Worldwide Bioclimatic Classification system of Rivas-Mart í nez et al. [ 28 ], Cabo Verde’s bioclimate ranges from tropical hyperdesertic to pluviseasonal, upper infra to low supratropical, and upper ultrahyperarid to upper dry, and it is occasionally subhumid (Supplementary Materials, Table S1). 3. Plant Communities of Cabo Verde Spatial differences in the amount of precipitation, structured by topographic determinants (altitude and aspect), become evident when comparing the flatter eastern islands (i.e., Sal, Boavista, Maio), where the climate is arid, with the most mountainous islands (Santo Ant ã o, S ã o Nicolau, Fogo, Santiago, Brava), where a semiarid and dry bioclimatic pattern in the south-facing slopes, dominated by African floristic elements of savannoid or predesert character, are replaced by more humid conditions on the north/northeast-facing slopes, creating a significant climatic asymmetry [ 28 , 29 ]. To find a reasonably effective model to understand Cabo Verde’s flora and vegetation chorology, we must add the influence of successive volcanic eruptions to the atmospheric circulation model and spatial distribution of topoclimates [ 30 ], as well as the particularly devastating anthropic impact of 500 years of human colonization [ 31 – 33 ]. The high level of landscape disturbance on the islands, which certainly led to the extinction of some plant species, such as Stachytarpheta fallax or Habenaria petromedusa, the two formally reported extinct species [ 34 ], hinders our capacity to provide a model for the pristine vegetation. Therefore, an approach must rely on data available for other Macaronesian archipelagos and consider models of distribution of African flora and vegetation that are closest to the ones of Cabo Verde, along with historical records from navigators and/or naturalists [33,35]. Diversity 2020,12, 80 5 of 16 Based on the aforementioned contingencies, we discuss a distribution model of the vegetation of the Cabo Verde Islands, supported by published [ 28 , 29 , 36 ] and unpublished work developed by the authors during the last decades. It must be noted that annual and ruderal communities were excluded from this study, as they are mainly dominated by exotic plants that have become naturalized in Cabo Verde. Some exotic plants are invading and dominating natural communities, thus constituting one of the most serious threats to plant communities, which are nowadays very strongly affected by human actions. According to the Cabo Verde Red List [ 34 ], most of the strong anthropic disturbances were recorded between 400 and 1200 m in mountainous islands (Santo Ant ã o, S ã o Nicolau, Fogo, Santiago, Brava), whereas tourism has threatened the lowland coastal plant communities, which occur in Eastern Islands of Sal and Boavista [ 34 ]. Moreover, natural disasters, specifically recent volcanic events (in 2014), have had an impact on plant communities that occur above 1600 m on Fogo Island. In this section, we present a characterization of the main plant communities in Cabo Verde, which still constitute the dominant elements of the native vegetation of these islands [i.e., 3.1. Ficus and Sideroxylon woodlands (Figure 2A); 3.2. Acacia savannas (Figure 2B); 3.3. Other arborescent communities (Figure 2C,D); 3.4. Shrub vegetation (Figure 2E,F); 3.5. Grasslands (Figure 2G); 3.6. Halophytic and hydrophytic communities (Figure 2H); and 3.7. Chasmophytic communities (Figure 2I)]. Nomenclature follows Rivas-Martínez et al. [28] and POWO—The Plants of the World Online portal [37]. 3.1. Ficus and Sideroxylon Woodlands Speaking of forests in Cabo Verde today may seem somewhat speculative, as only a few native tree species occur, and especially in areas of higher humidity and/or less accessibility. The restriction of plant communities dominated by native trees is linked to the fact that in general, endemics are more vulnerable to the browsing of introduced herbivores (e.g., goats), as shown by Cubas et al. [ 38 ] for Tenerife. In addition, the harvesting of firewood for domestic use and human-induced fires are particularly destructive to the forest areas of island ecosystems [39]. In mountainous islands, the possible past occurrence of arboreal vegetation is based on the current existence of several native taxa that are capable of phanerophytic structure (e.g., Ficus sur and F. sycomorus (Figure 2A), Dichrostachys cinerea subsp. platycarpa, and Sideroxylon marginatum), which could form open forests or woodlands. The model considers suitable conditions for three types of woodlands, two of which are clearly dominated by tropical fig trees (F. sur and F. sycomorus) and one corresponding to open forests of Sideroxylon marginatum (Table S2), which are currently restricted to very small patches. In areas with the highest vertical and horizontal precipitation values, the potential forests (woodlands) are dominated by F. sur at higher altitudes and by F. sycomorus at lower altitudes. In both cases, the phenological regime of these fig trees is similar to that of an evergreen forest, which is an outstanding feature when compared to the deciduous response pattern to the dry season found in continental Africa [ 40 ]. Outside the fog belt, sycamore fig trees (F. sycomorus) occur at valley bottoms, where floristic elements from arid and semi-arid environments are present, such as Cocculus pendulus and Ziziphus mauritiana, as well as tropophytic savannoid elements in an edaphic hygrophilic position according to a recurring tropical dry worldwide model [ 41 ], representing a process of isolation of high water-demanding flora and vegetation [ 29 ]. Currently, there are only a few specimens of isolated fig trees, which are rarely larger than 30 cm in diameter. These tropophytic and phreatophytic figs were first observed by Diogo Gomes (ca. 1420–1500), who was a Portuguese sailor that provided the earliest explicit reference to the large number of highly productive fruiting fig trees on the island of Santiago [33]. Diversity 2020,12, 80 6 of 16 Diversity 2019, 11, x 6 of 16 sailor that provided the earliest explicit reference to the large number of highly productive fruiting fig trees on the island of Santiago [33]. Figure 2. Representative species of some of the main plant communities in Cabo Verde. Woody elements present in woodlands and savannas at lowlands: Ficus sycomorus (A), Acacia caboverdeana (B), and in mountainous slopes, Dracaena caboverdeana (C). Riparian streams, near the coast: Phoenix atlantica (D). Shrub communities: Asteriscus vogelii and Artemisia gorgonum (E) and Euphorbia tuckeyana (F). Perennial grasslands at high altitudes: Hyparrhenia caboverdeana (G). Coastal halophytic communities: Tetraena vicentina (H). Upland chasmophytic communities: Umbilicus schmidtii (I). Photos by M. Cristina Duarte (A–D) and Maria Romeiras (E–I). Another evergreen woodland described for Cabo Verde [28] is dominated by the endemic marmulano of Cabo Verde (S. marginatum), which is a small tree that, similar to the fig trees, is found only in the cracks of rocky walls, rarely with significant trunk diameters. It is a paleosubtropical paleoendemic element, which occurs in the driest parts of the fog-influenced areas, with an identical position to that of the communities of S. mirmulans in Madeira or the Canarian microforest of S. Figure 2. Representative species of some of the main plant communities in Cabo Verde. Woody elements present in woodlands and savannas at lowlands: Ficus sycomorus ( A ), Acacia caboverdeana ( B ), and in mountainous slopes, Dracaena caboverdeana ( C ). Riparian streams, near the coast: Phoenix atlantica ( D ). Shrub communities: Asteriscus vogelii and Artemisia gorgonum ( E ) and Euphorbia tuckeyana ( F ). Perennial grasslands at high altitudes: Hyparrhenia caboverdeana (G). Coastal halophytic communities: Tetraena vicentina ( H ). Upland chasmophytic communities: Umbilicus schmidtii ( I ). Photos by M. Cristina Duarte (A–D) and Maria Romeiras (E–I). Another evergreen woodland described for Cabo Verde [ 28 ] is dominated by the endemic marmulano of Cabo Verde (S. marginatum), which is a small tree that, similar to the fig trees, is found only in the cracks of rocky walls, rarely with significant trunk diameters. It is a paleosubtropical paleoendemic element, which occurs in the driest parts of the fog-influenced areas, with an identical position to that of the communities of S. mirmulans in Madeira or the Canarian microforest of S. canariense. It is an evergreen woodland that includes many deciduous nanophanerophytic elements, many of them Cabo Verde endemics [e.g., Aeonium gorgoneum, Echium stenosiphon, Euphorbia tuckeyana, Diversity 2020,12, 80 7 of 16 Lavandula rotundifolia, Lotus jacobaeus, Launaea picridioides, and Lobularia fruticosa, among others]. Although present in almost all the islands, its abundance is higher in islands with a more significant fog belt (namely, Santo Ant ã o, S ã o Nicolau, Santiago, and Fogo), where it extends beyond this fog belt [ 28 ]. Such a distribution model for S. marginatum is not only congruent with the anthropic destruction of a large part of the population [ 38 ], but also with the ecological constraints that prevent it from colonizing drier habitats: this limitation does not apply to shrubs present in the community, since their larger ecological plasticity allows them to develop in more xeric habitats. This model is consistent with the latest genetic analyses regarding the divergence between taxa usually associated with Rand Flora (Afro-Mediterranean phytogeographic pattern that evolutionarily relates floras of disjunct regions such as Macaronesia, Northwest and South Africa, and Southern Arabia, among others) [ 42 – 44 ]. Older divergences are identified in sub-humid affinity taxa [e.g., Sideroxylon—17.5 Ma (10–26.2 Ma)], and those with more affinities with arid territories diverge later [e.g., Campylanthus—7.5 Ma (3.1–14.2 Ma)] [ 17 ]. The work of Pokorny et al. [ 17 ] demonstrates that the aridification of northwestern Africa, despite successive interruptions by GSPs, caused divergences in different periods of time for different taxa, depending on their ecological requirements, which is a process that still marks current spatial distribution patterns. 3.2. Acacia Savannas Under arid, semi-arid, and dry conditions, vegetation becomes dominated by tropical Acacia savannas (Acacia caboverdeana, Figure 2B), which are an African element in the vegetation of Cabo Verde that potentially covers most of the islands. This species, recently described as new to this archipelago by Rivas-Mart í nez et al. [ 28 ], was previously identified as Faidherbia albida. This species occurs in much of Africa in forest galleries along rivers and is a frequent floristic element in open deciduous rainforests and, mainly, savannas [ 45 ], requiring a long dry season and permanent access to ground water. Under natural conditions, F. albida is found close to temporary rivers and in gullies and ravines [ 46 ] or rocky areas, similar to A. caboverdeana in Cabo Verde, extending its roots to a depth of 8 m [ 47 ]. Faidherbia albida has been greatly spread by man due to its utility for livestock feeding and for undercover agriculture because of its deciduousness in the wet season [ 47 , 48 ]. In Cabo Verde, the potential area of A. caboverdeana is occupied by plantations of Prosopis juliflora, and only sporadically, as in Ribeira da Barca (Santiago), is it possible to find a small sample of what the pristine savannas of Acacia in Cabo Verde might have been. Chevalier [ 49 ] presents some photos of A. caboverdeana near the city of Praia (on sandy soil near the sea) with logs larger than 30 cm. These tropophytic Afrotropical savannas of A. caboverdeana (Table S2) are present in all islands, and they are accompanied by other micro and mesophanerophytic elements, such as Dichrostachys cinerea subsp. platycarpa and Ziziphus mauritiana and, less frequently, in plant communities dominated by endemic shrubs. In the understory, savannas frequently present a graminoid matrix of tropical continental African flora. 3.3. Other Arborescent Communities Formerly relevant in structuring the woody communities in the Cabo Verde archipelago are the endemic elements Dracaena caboverdeana (Figure 2C) and Phoenix atlantica (Figure 2D), and the native non-endemic Tamarix senegalensis. The symbolic dragon tree Dracaena caboverdeana only occurs in small patches in Santo Ant ã o and S ã o Nicolau [ 34 ]. Palm groves of the remarkable endangered Phoenix atlantica can still be seen in the eastern and southern islands of Cabo Verde, growing on riparian streams, mostly near the coast, with temporary hydromorphy. Cocculus pendulus and Ziziphus mauritiana are some of the few species present in these restricted communities. Present in most islands of the archipelago, galleries of tamarisk grow by temporary watercourses and torrents with generally scarce intermittent flow. These communities are similar to the riparian thicket savannas with Tamarix spp. of West Africa (Sahara, Mauritania, and Senegal) [50]. Diversity 2020,12, 80 8 of 16 3.4. Shrub Vegetation The shrub formations of Cabo Verde (Figure 2E,F) are mainly found in zones of medium to high elevations above 400 m, and the levels of endemism increase with elevation, as proposed by Steinbauer et al. [ 51 ]. The shrub vegetation is dominated by endemic species, showing a comparable pattern to Canary Islands [ 52 , 53 ] with a clear spatial pattern, with hotspots of endemic rarity found at high elevations and in specific habitats, namely in northeast-facing cliffs, of the Natural Parks of Moroços, Cova, and Ribeira da Torre (Santo Ant ã o); Monte Gordo (S ã o Nicolau); Serra da Malagueta (Santiago); Monte Verde (São Vicente); and Chãdas Caldeiras (Fogo Island) [54]. Among the shrub vegetation, the endemic Euphorbia tuckeyana (Figure 2F) define a wide diversity of plant communities (Table S2) depending on each island’s endemic species and/or taxa of restricted distribution and on certain specific ecological characteristics. These communities are rich in endemic species, most of them with either a shrubby or a subshrubby habit (e.g., Aeonium gorgoneum, Artemisia gorgonum, Campylanthus glaber, Conyza feae, Echium hypertropicum, E. vulcanorum, Euphorbia tuckeyana, Globularia amygdalifolia, Lavandula rotundifolia, and Periploca chevalieri). As stated above, most of these communities occur on NE slopes above 400 m, where higher values of precipitation occur. The presence of endemic shrub formations at lower altitudes and drier areas is associated with situations of edaphic compensation, namely block accumulation at the base of basaltic rock walls. A similar model was proposed by Esler et al. [ 41 ] for the deserts of southern Africa, where shrub and succulent vegetation becomes dominant on stony soils that receive less than 200 mm of rainfall/year. 3.5. Grasslands In xeric environments, woody elements are rare, and communities are dominated by perennial or short-lived herbaceous grasses such as Bothriochloa bladhii,Enneapogon desvauxii, and Tetrapogon cenchriformis. In mountainous islands, these communities are enriched by Andropogon gayanus, Chloris pycnothrix, Heteropogon melanocarpus, Hyparrhenia caboverdeana (Figure 2G), Setaria parviflora, and Rottboellia cochinchinensis, among others. As a whole, such herbaceous communities are physiognomically and structurally close to the dry tropical West African graminoid vegetation, sharing numerous taxa with it [28]. After rainy periods, ephemeral grasslands composed of annual grasses, such as the endemics Aristida cardosoi and Brachiaria lata subsp. caboverdeana, and broad-leaved herbs, such as Cleome viscosa, C. brachycarpa and Heliotropium crispum, flourish in the lowlands of all the islands. 3.6. Halophytic and Hydrophytic Communities Halophytic communities are common in Cabo Verde, but they are particularly important in the Eastern islands of Sal, Boavista, and Maio, as well as in S. Vicente. In coastal sand dunes, the xerophilous communities are dominated by perennial rhizomatous species such as the graminoids Sporobolus spicatus and Cyperus crassipes, two widespread African species, or by the dwarf shrubs Lotus brunneri,Polycarpaea caboverdeana,Pulicaria diffusa, and Tetraena vicentina (Figure 2H). The particular topographic and hydrographic features of the eastern islands favor the occurrence of saltwater marshes. These permanent succulent halophilous communities grow on coastal sandy soils, are temporarily or occasionally flooded by sea tides, and are dominated by the succulent shrub Arthrocaulon franzii and the small forb Cressa salina. Similar communities are present in the western coasts of the African continent, mainly from Morocco to Senegal [ 51 ]. Intermingled with these woody marshes, small herbaceous communities of succulents occur, including Sesuvium portulacastrum subsp. persoonii,S. sesuvioides, and Blutaparon vermiculare. Diversity 2020,12, 80 9 of 16 3.7. Chasmophytic Communities Humid and shady basaltic walls, permanently or temporarily water-flushed, support perennial communities of chasmophytic species such as the tropical ferns Adiantum capillus-veneris subsp. trifidum, Hypodematium crenatum, and Pteris vittata. In mountainous islands, perennial rupicolous communities grow on basaltic, mafic ultramafic rocky walls and cliffs that are wetted only during the rainy season. Characteristic species vary with the island and comprise the pteridophytes Hemionitis acrostica and Cosentinia vellea and shrub or subshrub chasmophytes, including a wide diversity of endemic taxa belonging to genera such as Campylanthus, Kickxia, Launaea,Sonchus, and Umbilicus (Figure 2I). Ferns such as Adiantum incisum and A. philippense, as well as some cosmopolite rupicolous species are present in nitrogen-rich habitats in urban or rural areas. These communities develop under less humid conditions than those previously listed. 4. Aridification of Northern Africa and Its Role in Shaping the Vegetation of Cabo Verde Explanation of the current features of the archipelago’s flora and vegetation requires arguments concerning the climatic changes that have occurred in Africa since the Miocene. The early Miocene (23–16 Ma) was globally hot and humid, with rainforests extending from northern Africa to nearly southern Africa [ 17 ]. The Middle Miocene (16–11.6 Ma) marks the beginning of the change toward aridity, although this aridification began in the SW (Namib Desert, Congo Basin) 17–16 Ma earlier (lower Mid-Miocene), and in North Africa, the first evidence of Saharan aridification only appears in the Late Miocene (11.6–5.3 Ma) [ 55 ]. However, this aridification trend is marked across North and Northwest Africa by strong aridity waves interrupted by humidity episodes known as GSPs (green Sahara Periods) [ 56 , 57 ]. More than 230 GSPs since 8 Ma have been documented [ 58 ], and their importance for vegetation distribution models in North and Northwest Africa cannot be discarded [ 2 , 17 , 56 , 58 – 62 ]. The alternate episodes of humidity and aridity of the aridification trend of northern Africa since the Miocene are the keystone of the irradiation phenomena of North African flora that, depending on their ecological valence, diverged into isolated and genetically differentiated populations following a similar model, but these are temporally different due to their ecology (the most humidity demanding elements present older divergences) [ 17 , 63 , 64 ]. In the Quaternary, two of these GSPs, respectively Eemian (130–115 Ky corresponding to Marine Isotope Stage 5e) and the early Holocene (11–5 ka), are relatively well documented [ 2 , 54 , 55 , 59 , 65 , 66 ] and are of great importance for the evolution of northern and northwestern African vegetation (including the Cabo Verde archipelago). During GSPs, WAM penetrates further north, and higher precipitation than today generated a series of inland Sahara lakes and permanent rivers [ 3 , 4 ]. During the Holocene GSP, the vegetation is characterized by an advance of wooded savannas northwards, occupying what is now the arid and hyperarid Sahara Desert [ 17 ]. The currently accepted general model refers to a progressive development of forests and wooded savannas during interglacial periods as a result of the intensification and latitude rise of WAM (with increased precipitation) and a decrease in vegetation cover during glaciations with a greater influence of continental trade winds. In the continental shelf cores, dusts of terrestrial origin present a minimum concentration during the interglacial periods (higher vegetation cover) and the opposite during the glacial periods. In Cabo Verde Islands, such an oscillation is recorded in the alternation of calcrete (hot and arid conditions), sand dunes (dry and cold conditions), and paleosols (wetter periods) [67,68]. In general, the endemic shrub species have a strong ecological resilience, resulting from the filtering effect of recurrent dry periods that mark the ongoing African aridification since the terminal Miocene [ 63 ]. This aridification must have led to mass extinction phenomena, and only taxa of greater plasticity managed to survive. We can assume that episodes of dryness played a more important role in Cabo Verde than in the other islands of Macaronesia. Such an assumption is based on the fact that arid and semi-arid conditions have been expanding in altitude in southernmost Macaronesian archipelagos, in a model that inevitably leads to the restriction/disappearance of the higher humid and colder zones. Such an idea is also supported by analyses of deep-sea cores from the African west coast, some of which fall between Cabo Verde and the Canary Islands. Analyses of pollen [ 69 , 70 ] and of Saharan Diversity 2020,12, 80 16 of 16 81. 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