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Articles

Acacia tortilis var. raddiana communities in the northwestern Algerian Sahara

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Pages 289-306 | Received 24 Feb 2016, Accepted 25 May 2016, Published online: 19 Aug 2016

Abstract

The aim of this work is the phytoecological study of the Acacia tortilis var. raddiana desert savanna in the northwestern Algerian Sahara. Sixty-seven relevés were collected for this habitat from an area extending from the northern boundary of Béchar to the southern part of Kerzaz, a latitudinal gradient of 250 km. A detrended correspondence analysis identified two communities represented by 35 and 32 relevés. Canonical correspondence analysis highlighted the topography and the nature of the substratum as the main environmental factors explaining the distribution of the two groups. The most frequent community corresponded to the Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association Quézel 1965. It is associated with large wadi-beds and alluvial plains. This association presents two facies: a saxicolous one characterized by Farsetia occidentalis and Trichodesma calcaratum and a sandy facies with Kickxia aegyptiaca and Brocchia cinerea. The second community corresponds to the Acacia tortilis var. raddiana and Rhus tripartita association Quézel 1965, typical of narrow wadi-beds with rocky substrates. The floristic composition reveals fewer taxa of tropical origin and a reduced list of characteristic species is proposed. Details of the range of the two syntaxa identified are provided. They are compared with the other Acacia tortilis var. raddiana associations described for the Algerian central Sahara.

Introduction

The vegetation of the Algerian Sahara has long been known for its distinctiveness and phytogeographical interest and complexity. Quézel (Citation1978) indicates the existence of nine biogeographical domains for the Sahara out of 14 for North Africa. An even more detailed phytogeographical description provided by Le Houerou (Citation1990, Citation1995) which, extended to the Sahelian territories, suggests the existence of 16 domains that cover the Sahara. The limits of these phytogeographical subdivisions (zones) are outlined in Figure . The vegetation description in the present paper falls into the northwestern Saharan domain of Quézel (Citation1978), corresponding more or less to the same zone proposed by Le Houérou (Citation1990, Citation1995).

Figure 1. Sketches of the phytogeographical subdivisions of the Sahara and neighbouring territories by Le Houérou (Citation1990, Citation1995). 1: Mediterranean region (semi-arid to hyper-humid zones); 2: Western arid steppe zone; 3: Central arid steppe zone; 4: Eastern arid steppic zone; 5: Oceanic northern Sahara zone; 6: Western Northern Sahara transition zone; 7: Central Northern Sahara transition zone; 8: Oriental Northern Sahara transition zone; 9: Oceanic central Sahara; 10: Northwestern central Sahara; 11: Northern central Sahara; 12: Northeastern central Sahara; 13: Western central Sahara; 14: Central central Sahara; 15: Central Sahara highlands; 16: Eastern Sahara highlands; 17: Oceanic southern Sahara; 18: Western southern Sahara; 19: Central southern Sahara; 20: Eastern southern Sahara; 21: Oceanic Sahel; 22: Western Sahel; 23: Central Sahel; 24: Eastern Sahel; 25: Eastern Sahara, fringes of the Red Sea; 26: Soudano-Angolan region, Eastern-African domain, mountain zone.

Figure 1. Sketches of the phytogeographical subdivisions of the Sahara and neighbouring territories by Le Houérou (Citation1990, Citation1995). 1: Mediterranean region (semi-arid to hyper-humid zones); 2: Western arid steppe zone; 3: Central arid steppe zone; 4: Eastern arid steppic zone; 5: Oceanic northern Sahara zone; 6: Western Northern Sahara transition zone; 7: Central Northern Sahara transition zone; 8: Oriental Northern Sahara transition zone; 9: Oceanic central Sahara; 10: Northwestern central Sahara; 11: Northern central Sahara; 12: Northeastern central Sahara; 13: Western central Sahara; 14: Central central Sahara; 15: Central Sahara highlands; 16: Eastern Sahara highlands; 17: Oceanic southern Sahara; 18: Western southern Sahara; 19: Central southern Sahara; 20: Eastern southern Sahara; 21: Oceanic Sahel; 22: Western Sahel; 23: Central Sahel; 24: Eastern Sahel; 25: Eastern Sahara, fringes of the Red Sea; 26: Soudano-Angolan region, Eastern-African domain, mountain zone.

The special character and landscape diversity of the northwestern Sahara has attracted many botanists over the last century (Tits Citation1925; Maire Citation1938; Guinet Citation1954, 1958; Guinet and Sauvage Citation1954). Tree species are rare in the Sahara and plant communities with Acacia tortilis var. raddiana as the dominant stratum are the most widespread vegetation units in the Saharo-Arabian belt (Ozenda Citation1958; Boulos Citation1995). Acacia tortilis var. raddiana is an African (Sahelo-Sudanian) element (Ross Citation1981). This species occurs abundantly in all northern and eastern African countries and extends eastward to the Arabian Peninsula (Brenan Citation1983; Kennenni Citation1991). In this paper, we used the flora of Ozenda (Citation2004) for species identification. Nomenclature follows Dobignard and Chatelain (Citation2010–2013) for all the species of the present study.

Early descriptions of Acacia communities were provided by Guinochet and Quézel (Citation1954), Quézel and Simonneau (Citation1963), Quézel (Citation1965), Barkoudah and Van Der Sar (Citation1982). In the northwestern Sahara, the “pseudo-steppe” of Acacia tortilis var. raddiana and Panicum turgidum is the main community that occupies non-saline wadi-beds (Guinet Citation1954; Quézel Citation1965). Recently, Bensaid, Aït-Mohand, and Echaïb (Citation1996) studied the spatio-temporal dynamics of Acacia tortilis var. raddiana while Benhouhou (Citation1991) and Benghanem (Citation2009) studied the ecology and phytosociology of Acacia tortilis var. raddiana communities in the Ougarta mountains (Figure ). To date, however, although Acacia communities dominate almost all Saharan wadis, relatively few phytosociological and ecological studies of these communities have been carried out in Algeria (Barry, Celles, and Manière Citation1981; Benhouhou, Dargie, and Gilbert Citation2003; Gaci Citation2012; Boucheneb and Benhouhou Citation2012). This contrasts with some other studies performed in other parts of the Sahara (Danin Citation1983; Kenneni Citation1991; Abd El-Ghani and Amer Citation2003; Al-Atar, El-Sheikh, and Thomas Citation2012).

Figure 2. Geographical localization of the study area.

Figure 2. Geographical localization of the study area.

The aim of the present study focuses on the phytoecological and phytosociological analysis of the Acacia tortilis var. raddiana communities in the northwestern Sahara, in order to identify the main ecological gradients that structure these ecosystems and to propose a critical analysis of the phytosociological framework proposed by Quézel (Citation1965). Furthermore, a comparison of the associations described with those found in the central Sahara domain in Algeria is made to strengthen the syntaxonomic system of Acacia tortilis var. raddiana communities.

Study area and methodology

The study area is bounded in the north by a line level with the city of Béchar, while the southern limit is represented by the oasis of Kerzaz; the oasis of Béni-Abbès represents an approximately central location. The latter is located 1200 km southwest of Algiers (Figure ).

Climate

Descriptions of climate and bioclimate are based on rainfall and temperature data obtained from the nearest meteorological stations to the study area: Béchar and Béni-Abbès. Data were gathered from the National Meteorological Office (NMO) for a period of 40 years (1967 to 2007) and from Dubief (Citation1959) for an earlier period spanning 24 years (1926 to 1950) (Table ).

Table 1. Climatic data for the study area.

A study of Table shows a decrease in rainfall between the two periods for both Béchar (79.9 mm to 69.5 mm) and Béni-Abbès (32.1 mm to 29.9 mm). Similarly, a slight increase in average temperature is observed. Climatic synthesis shows that Q2 values are substantially the same for Béni-Abbès (2.70 and 2.75) for the two periods, with a slight decrease for Béchar (7.13 and 6.45).

The study area is located in the Saharan bioclimate with cold to mild winters for the first period (1926 to 1950) and milder winter for the second period (1967 to 2007).

Geology and geomorphology

The study area is located at the junction of three geomorphological units: the Great Western Erg, the Guir Hamada and the Ougarta mountains. The Great Western Erg occupies the eastern part of the study area and consists of extensive sand dunes of Quaternary origin (Nedjari Citation1995).

The Guir Hamada, located in the northwestern part of the study area, is a vast rocky platform of about 10-m thick sandstone of Plio-Quaternary origin (Conrad and Roche Citation1965). The Ougarta mountains are located in the southwestern part of the study area, covering an area of about 6000 km2 of Precambrian sandstones (Aït-Ouali and Nedjari Citation2006).

Water resources in the study area are represented by unconfined aquifers in the Quaternary terrain of the Guir Hamada and a few aquifer units in the Ougarta mountains (Roche Citation1973). Occasionally, irregular flooding of wadis in the Ougarta area results in a significant additional water source for the vegetation. Soils of the study area are raw mineral soils – the dominant substrate encountered in Saharan non-saline wadis (Dutil Citation1971). It is in these mountains that the best developed examples of the Acacia savanna community are encountered.

Sampling and data analyses

Sampling of the vegetation was carried out in March 2007 and 2008 over an area of about 50,000 km2, stretching over 250 km. During this period, 67 floristic relevés were recorded. These were obtained from various different geomorphological wadi units (topography) as well as valleys and alluvial plains. The distribution of relevés is presented in Figure .

The quadrat area for the study was 100 m2, which is the standard size for most comparable work in arid zones (Kassas Citation1953; Quézel Citation1965; Abd El-Ghani Citation1998; Benhouhou, Dargie, and Gilbert Citation2003).

The geomorphological wadi unit is the key factor in the description of these communities (Fossati, Pautou, and Peltier Citation1998; Benhouhou, Dargie, and Gilbert Citation2001; Al-Atar, El-Sheikh, and Thomas Citation2012). The geomorphological units identified and used for this study are: the primary and secondary wadi beds, different terrace levels, valleys and alluvial plains. The aim is to dissect out the relationship between the floristic variability and the various geomorphological facies of the wadi.

The floristic and ecological data collected were submitted to two kinds of multivariate analysis: detrended correspondence analysis (Hill and Gauch Citation1980) and canonical correspondence analysis (Ter Braak Citation1987). The software used was PC-ORD (McCune and Mefford Citation1999). These analyses helped to distinguish the plant communities observed in the study area and also to extract the dominant ecological gradients. Associations described are related to syntaxonomical units proposed by Quézel (Citation1965) according to the phytosociological method of Braun-Blanquet (Citation1952). Finally, a bibliographical review enabled the authors to compare the associations described in this study with all of the Acacia tortilis var. raddiana communities documented to date in the Algerian central Sahara.

Results

Ecological gradient analyses

The relevés performed in this study and distributed along the first two axes resulted into two main groups, A with 35 relevés and B with 32 relevés. Eigenvalues were 0.346 for the first axis and 0.259 for the second axis, suggesting that there are at least two gradients at work. Within group A, two sub-groups were distinguished: a1 (with six relevés) and a2 (with six relevés) (Figure ).

Figure 3. Ordination diagram of a detrended correspondence analysis of 67 relevés of the study area.

Figure 3. Ordination diagram of a detrended correspondence analysis of 67 relevés of the study area.

Analysis of the relevés and species distribution along the first axis revealed the appearance of two ecological gradients (Figure ).

Figure 4. Species scatter and main ecological factors produced by canonical correspondence analysis of the 67 relevés.

Figure 4. Species scatter and main ecological factors produced by canonical correspondence analysis of the 67 relevés.

Axis 1 corresponds to a geomorphological gradient that opposes the relevés taken from large wadi beds, bordered by alluvial terraces and fans (negative side), to relevés from narrow rocky wadi beds (positive side) (Figure ). Hence, the analysis helped to distinguish two major geomorphological units of the “wadi habitat”: (i) a unit where the wadi shows both a minor (channel) and a major wadi bed (floodplain), which is characterized by species associated with gravelly sandy substrates such as Panicum turgidum, Citrullus colocynthis and Acanthorrhinum ramosissimum, and (ii) a rocky unit epitomized by woody chasmophils such as Rhus tripartita, Maytenus senegalensis and Ceratolimon feei.

For the second axis, a clear contrast appears between relevés on sandy substrates for the negative part of the axis which feature perennial psammophilous plants such as Kickxia aegyptiaca and therophytes such as Brocchia cinerea, Neurada procumbens and Ifloga spicata. On the positive side of this axis, are located the relevés taken from coarse to gravelly substrates, with high-frequency species here including Trichodesma calcaratum, Farsetia occidentalis and Kebirita roudairei. The distinction between relevés taken from sandy substrates and those from gravelly-coarse substratum highlights the soil texture as the main environmental gradient along the second axis. The projection of two gypsophilic species: Caroxylon vermiculatum and Tetraena alba, reflects minor local edaphic affinities which have limited importance in the structure of the studied communities. The analysis also reveals that the altitudinal variations observed were not discriminative.

A topographic sequence is presented in Figures a and b to illustrate the distribution of the floristic groups identified in relation to ecological gradients.

Figure 5. Topographic sequences of (A) the Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association and its two facies; and (B) the Acacia tortilis var. raddiana and Rhus tripartita association.

Figure 5. Topographic sequences of (A) the Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association and its two facies; and (B) the Acacia tortilis var. raddiana and Rhus tripartita association.

Syntaxonomic description

The phytosociological examination of the data has led to the assigning of the vegetation to two main plant communities: (i) the association with Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii Quézel Citation1965 (group A), and (ii) the association with Acacia tortilis var. raddiana and Rhus tripartita Quézel Citation1965 (group B) (Figure ). Within the phytosociological framework established by Quézel (Citation1965) for the northwestern Sahara, these two associations are included into the Antirrhineto-Zillion macropterae alliance Quézel Citation1965, the Pergularieto-Pulicaretalia order Quézel Citation1965 and the Pergularieto-Pulicarietea class Quézel Citation1965.

The Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association Quézel Citation1965

This association is characteristic of wadi beds, terraces and sediment fans on gravelly-sandy soils, mainly in the Ougarta mountains, at altitudes between 375 and 650 m (Figure ).

Figure 6. The Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association Quézel Citation1965, Ougarta, A.N. Benghanem, 31 March 2014.

Figure 6. The Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association Quézel Citation1965, Ougarta, A.N. Benghanem, 31 March 2014.

Relevés of this association are grouped in Table and are represented by:

Table 2. The Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association (Quézel Citation1965).

The association (A), a chasmophil facies (a1) with Farsetia occidentalis and Trichodesma calcaratum and a psammophil facies (a2) with Kickxia aegyptiaca and Brocchia cinerea. Both of these facies were observed on wadi terraces.

For the relevés made in the same area, among the species proposed by Quézel (Citation1965) as characteristics of the association, seven species of tropical origin were absent from those recorded during this study: Caylusea hexagyna, Seetzenia lanata, Maerua crassifolia, Senna italica, Acacia ehrenbergiana, Astragalus akkensis and Lavandula coronopifolia. An endemic species of the southeastern Moroccan desert and the Ougarta mountains, Foleyola billotii, was similarly not recorded.

The Acacia tortilis var. raddiana and Rhus tripartita association Quézel Citation1965

This association is found on rocky terrain in narrow wadi beds and has been recorded from an altitudinal range between 500 and 690 m (Figure ). It has been observed from both rocky wadis of the southern djebel slopes in the Béchar area as well as rocky wadis in the Igli and Taghit region.

Figure 7. The Acacia tortilis var. raddiana and Rhus tripartita association Quézel Citation1965,Taghit, A.N. Benghanem, 27 March 2014.

Figure 7. The Acacia tortilis var. raddiana and Rhus tripartita association Quézel Citation1965,Taghit, A.N. Benghanem, 27 March 2014.

With regard to the syntaxonomic level, the analysis of Table shows that this association belongs to the same higher syntaxonomic units as the Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association. It is also distinguished by a large proportion of characteristic species, which are typical of the Atractylion babelii alliance Quézel Citation1965 and the Gymnocarpeto-Atractyletalia order Quézel Citation1965 of rocky terrain and hamada, with this cohort being typified by species such as: Gymnocarpos decandrus, Perralderia coronopifolia, Deverra battandieri and Ceratolimon feei.

Table 3. The Acacia tortilis var. raddiana and Rhus tripartita association Quézel Citation1965.

Again, for the relevés realized in the same region, among the characteristic species proposed by Quézel (Citation1965) for this association, two tropical species, with low frequency, were notably absent from our relevés: Cenchrus ciliaris and Tricholaena teneriffae.

Discussion

Phytoecological characterization of plant communities with Acacia tortilis var. raddiana

The differences between the two associations with Acacia tortilis var. raddiana existing in the northwestern Algerian Sahara are related to the different geomorphological characteristics of the wadi and their substrates. These gradients are closely linked to water availability, a crucial limiting factor in arid environments (Abd El-Ghani Citation1998; Fossati, Pautou, and Peltier Citation1998; Kadmon and Danin Citation1999; Ali, Dickinson, and Murphy Citation2000; Abd El-Ghani and Amer Citation2003; Brinkmann et al. Citation2009).

For the northwestern Sahara, Quézel (Citation1965) describes this savanna through three associations of which two have been identified and thoroughly described in this work.

The comparison of the floristic relevés of the Acacia raddiana, Panicum turgidum and Foleyola billotii association shows that eight characteristic species from the 12 proposed by Quézel (Citation1965) were not reported during the present investigation. Not only were many characteristic species proposed by Quézel (Citation1965), but these are all characterized by both relatively low frequencies (between 6% and 20%) and a wide geographical distribution of tropical Saharo-Arabian origin. In addition, Lavandula coronopifolia and Trichodesma africanum are typical species of rocky outcrops and therefore their identification by Quézel as characteristic species of the Acacia “pseudo-steppe” may have been mistaken, considering this ecological association.

With regard to Foleyola billotii, an endemic chamephyte of the Ougarta mountains and of southeastern Morocco, present in 35% of the relevés published by Quézel (Citation1965), was also absent from the relevés performed for the present study. The same species was also absent from the floristic lists of Quézel and Simonneau (Citation1963), Barkoudah and Van Der Sar (Citation1982), and Benhouhou, Dargie, and Gilbert (Citation2003) for this association. However, it is important to note that field investigations conducted by Benghanem and Benhouhou (personal observation, 30 March 2014) have confirmed its presence – albeit at very low frequency – in our study area. This recent observation confirms the eastern boundary of its distribution in the Ougarta mountains (Quézel Citation1964, Citation1978).

The absence of these taxa, or failure to detect them, as seems to have been the case for Foleyola billotii, could be related to the increase in the intensity of certain anthropogenic activities (grazing and wood cutting). Hence, we would hypothesize that the vegetation ascribed in this study to this association is a floristically impoverished ecological state, for which we propose to retain the following characteristic species: Acacia tortilis var. raddiana, Panicum turgidum and Cullen plicatum. Despite the floristic discrepancies between relevés published by Quézel (Citation1965) and those from the present study, a detrended correspondence analysis confirmed that they correspond to the same association. Furthermore, the ecological variability of this association is again clearly illustrated along the first axis of Ffigure where the rocky facies is at one end and the sandy facies at the other end of the axis 1 (Figure ).

Figure 8. A comparative DCA of the Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association relevés (Current study vs. Quézel Citation1965).

Figure 8. A comparative DCA of the Acacia tortilis var. raddiana, Panicum turgidum and Foleyola billotii association relevés (Current study vs. Quézel Citation1965).

The Acacia tortilis var. raddiana and Rhus tripartita association was confirmed by this study in the northwestern Algerian Sahara, as being confined to rocky wadis and was less widely distributed than the previous one. Comparison between floristic lists published by Quézel and Simonneau (Citation1963) and Quézel (Citation1965) and those from the present study clearly indicates a lower frequency of two characteristic taxa for the latter: Rhus tripartita and Maytenus senegalensis. Considering the absence of two other characteristic taxa, Cenchrus ciliaris and Tricholaena teneriffae, from our relevés, their low frequency in the original association and their multiregional biogeographical distribution (Barry and Celles Citation1972–1973), their labelling as characteristic species seems no longer to be justified. Again, this is an impoverished version of the association where two species are absent and two others have low frequency, Maytenus senegalensis (I) and Rhus tripartita (II) (Table ). The detrended correspondence analysis of the relevés published by Quézel (Citation1965) and the current study confirm that we are dealing with the same association. The distribution of the relevés within the scattergram, where relevés made by Quézel (Citation1965) are plotted at the positive end of the first axis, is due to the absence of Cenchrus ciliaris and Tricholaena teneriffae (Figure ).

Figure 9. A comparative DCA of the Acacia tortilis var. raddiana and Rhus tripartita association relevés (Current study vs. Quézel Citation1965).

Figure 9. A comparative DCA of the Acacia tortilis var. raddiana and Rhus tripartita association relevés (Current study vs. Quézel Citation1965).

Phytogeography of plant communities with Acacia tortilis var. raddiana

These present results enable us to precisely describe the geographical limits of the Acacia raddiana, Panicum turgidum and Foleyola billotii association. Its eastern boundaries correspond to the eastern fringes of the Ougarta mountains because further east, in the northern Sahara subdivision, Foleyola billotii is absent (Quézel Citation1978). Its western boundaries correspond to the eastern limits of the Acacia raddiana and Foleyola billotii association described by Quézel et al. (Citation1995) from the middle valley of the Draa in Morocco. The southern limits of the association correspond to the Kerzaz region, 100 km south of Béni-Abbès. Further south, both climatic and edaphic conditions prevent the development of well-established Acacia savanna. As for its northern limit at the northeastern area of its distribution, it is located in the Béchar region, 150 km north of Béni-Abbès. The geographical distribution of the Acacia tortilis var. raddiana and Rhus tripartita association is relatively limited in area and corresponds to zones characterized by the rocky slopes of the djebels between Béchar in the north and Kerzaz in the south.

Further south, in the central Sahara, the desertic Acacia savanna corresponds to a different type – related to the Acacio-Panicion alliance Quézel Citation1965. Above the alliance level, this unit belongs to the same higher phytosociological units as the two associations described in this study. In this alliance, six Acacia associations are described, with the most common and widespread being the Senna italica and Panicum turgidum association Quézel Citation1965 that grows on gravelly-sandy substrates. The four other associations described by Quézel (Citation1965) have smaller geographical distributions and are found on gravelly to sandy wadi beds. The sixth Acacia association, the Acacia tortilis var. raddiana and Salvadora persica Boucheneb and Benhouhou Citation2012, is closely associated with large wadi beds south of Tamanrasset and only develops where there are deep sandy compact soils (Table ).

Table 4. Acacia tortilis var. raddiana associations in the Algerian Sahara.

All of these associations, dominated by Acacia tortilis var. raddiana and Panicum turgidum, in the Algerian Sahara, share a common background flora with species such as: Heliotropium bacciferum, Asteriscus graveolens, Cymbopogon schoenanthus, Morettia canescens, Pergularia tomentosa, Farsetia aegyptiaca and Kickxia aegyptiaca (Maire Citation1940; Leredde Citation1957;Guinet Citation1958; Quézel Citation1964, Citation1965; Barry and Celles Citation1972–73; Barkoudah and Van Der Sar Citation1982; Ozenda Citation2004; Boucheneb and Benhouhou Citation2012).

This common background flora is also found elsewhere in the Saharo-Arabian region (Bornkamm and Kehl Citation1990; Quézel et al. Citation1995; Léonard Citation2001; Munzbergova and Ward Citation2002; Grouzis and Le Floc’h Citation2003; Brinkmann et al. Citation2009). These Acacia communities described by the different authors differ principally in the proportion of taxa assigned to the main biogeographical groups: Saharo-Mediterranean and Mediterranean in the west and north of the Sahara, Soudano-Deccanian in the south, Irano-Turanian in the east and Saharan endemics depending on the geographical zone considered (Zohary Citation1973; Danin Citation1983; Batanouny Citation1987; El Demerdash, Hegazy, and Zilay Citation1995; Abd El-Ghani Citation1996; Abd El-Ghani and Amer Citation2003; Anthelme, Waziri Mato, and Maley Citation2008; Al-Atar, El-Sheïkh, and Thomas Citation2012).

General conclusion

Acacia tortilis var. raddiana and Panicum turgidum constitute probably the keystone species of the Acacia savanna in the northwestern and central Sahara. Each of the main geographical subdivisions of the Sahara is distinguished by subtle ecological variations highlighted by floristic differences. From this basis, and as also suggested by recent syntaxonomical studies (Boucheneb and Benhouhou Citation2012; Abdelkrim, Zeraia, and Bensettiti Citation2014), the current phytosociological framework needed to be re-examined in order to propose a clearer syntaxonomic hierarchy of the Acacia tortilis var. raddiana communities in the Algerian Sahara, and the whole Sahara desert. For instance, as far as the third association (Acacia tortilis var. raddiana and Ziziphus lotus Quézel Citation1965) related the Antirrhineto-Zillion that Quézel (Citation1965) found in the northwestern Sahara, relevés from the present study did not confirm its existence. Results suggest merging this third association with the Acacia raddiana, Panicum turgidum and Foleyola billotii association. In other words, it may be better to rationalize the Acacia tortilis var. raddiana savanna of the northwestern Sahara into two associations within which several facies could be identified (according to local topographical and edaphic parameters). Also, is it necessary to define two different alliances, Antirrhineto-Zillion for the northwestern Sahara and Acacio-Panicion for the central Sahara, when they are so floristically similar to each other? Results of our study support this approach – but need to be confirmed by further field investigations.

Notes on contributors

Abdelkader Nabil Benghanem is a lecturer at the University of Mouloud Mammeri of Tizi-Ouzou (Algeria) since 2010. He is currently preparing his PhD thesis on Acacia tortilis var. raddiana communities in the Algerian Sahara. Contribution: data collecting, data analysis and writing the manuscript.

Nacéra Boucheneb is a researcher at the National Institute of Forestery Research (Algeria) since 1990. She worked for ten years in Tamanrasset before returning to Algiers. Contribution: her field experience and knowledge helped in the phytosociological analysis and the general discussion of the submitted paper.

Salima Benhouhou is a professor at the National High School of Agriculture (Algeria) since 1991. She gained her Saharan experience from 1987 when starting her PhD research on the vegetation in the northwestern part of the Algerian Sahara. Contribution: partly field data collection and the supervision of the general framework of the paper.

Brendan O’Hanrahan is a freelance ecologist who graduated from Aberdeen University (UK). Contribution: participated at the beginning of field data sampling, helped in the general discussion, particularly the ecological approach and his perfect mastery of the English language has facilitated the writing of this article and meeting the level of quality required by the Botany Letters.

Frédéric Médail is a professor at the Mediterranean Institute of marine and terrestrial Biodiversity and Ecology (France). Contribution: his experience in the Saharan domain helped greatly to improve the present paper with an in-depth reflection on data interpretation and the general discussion.

Disclosure statement

No potential conflict of interest was reported by the authors.

Acknowledgements

We would like to thank Benhamza Abdelmalek for providing the logistical assistance which enabled us to undertake the fieldwork. Our gratitude goes particularly to our guides Boudjemâa Bouzidi, Belkacem Telhaoui and Kebir Abdelkader.

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