Some Anthropic Aspects in Meridional Region of Sebdou ( Oran-Algeria )

Relying essentially on human data (social structure, demography, population repartitions, migratory movements, agro-pastural activities), the authors, from their studies, note that these regions are an extension of hamlets and other groups. Highlands gather a small population that seems to settle. Responsible human disturbance (clearings, cultures, urbanization, etc.) modified a large part of the actual state of vegetation structures. The results also show that most of the population is concentrated in the main towns. This concentration causes consumption of pre-forest land and rangelands. The average annual extension can sometimes reach 2.4 Ha. Hamlets, home grouping seem to impose a lifestyle approaching that of centers located in the North. At the bioclimatic level, the results show that the cold thermal variations promote contact between woody vegetation and steppe formations with thermal determinism (formation often in xerophytes thorny pads). Droughts often advocate regressive dynamics of these plant formations which are quite degraded. On the other hand, stressing continuity issues related to human actions, the authors present the floristic composition, detailing the botanical plant species including biological and morphological types. The therophyte type predominates in all areas explored and their percentage can reach 73% in the steppe and 49% in Beni-Snous.


Introduction
After independence in 1962, the Algerian forest has gradually found its hangouts, but it is certain that the impact of human action on the natural landscape remains present and uncontrolled.
Recovery and development of this heritage can not be conceived in a purely ecological context, only if the socio-economic aspect contributes effectively in the state of ecosystem stability.
Mountain societies, all over the world, have always used ingenuity to enhance their profit, resources often limited in hard environment.
In general, the Mediterranean region, and in particular that of Beni-Snous and El-Bayadh remain submitted to a strong destruction of ecosystems which can be the consequences of human activities pressure which is exercised with intensity on the natural environment.
Barbero, et al. [1] reported changes that occurred for certain climatic parameters.Amplification of the summer drought in the suboréal-Subatlantic hinge contributed to a seasonal aridity of climate which, at least for Mediterranean coastal and coastal juxta areas, could influence a restructuring of biological material of forest ecosystems, by modifying interspecific competition processes and promoting the establishment of mixed forests, as it is the case today in the old population growth.The arrival of herbaceous species is not compatible in the ecosystem with maintaining some sclerophyllous species and the development of pink laurel (Nerium oleander) species of meso-thermal which have been limited by the repeated human use of forest ecosystems.Stages of further degradation of these formations distinguish very open landscapes.
Anthropogenic disturbances are for a large part responsible for the current state of vegetation structures in the Maghreb Barbero, et al. [2].
The ecological study of the vegetation is primarily a study of the action of man on vegetation Long [3].Demography is one of the main causes of degradation of these environments.It has been exploded since the beginning of the century.The population almost doubles every 20 to 30 years, depending on the country, 25 years on average, especially since the 50s.Therefore, more land must be cultivated, more animals must be adopted, and more wood must be cut for heating.
In addition most countries experience a significant improvement in living standards and a certain urbanization.Demand for meat and cereal products has increased even faster than population, which further exacerbates the pressures on land.
Pastoral societies especially in steppe areas have faced the mounted state, introduced by colonization.It is the state that holds the power.As a result, traditional institutions have become unnecessary and disappeared.Young states have pursued the same policy of consolidation of state structures.The semi-nomadic societies, considered retrograde, are forced to settle down in the steppe because of the problem of political control Regagba [4].
To capture the effect of human action and threats that significantly affect our study area (mountain and steppic areas), we found it necessary to study the population evolution, bioclimate, agricultural activities, the state of vegetation, and overgrazing charged on the environment.

Geographic Situation (Figure 1, Table 1)
Administratively, the region of Beni-Snous including the surrounding high lands, is split between the wilaya of

Mountain Ranges of Beni-Snous
The geological approach that we are going to deal with is related to the works of Benest and Elmi [5], this one says that the mountains are formed of cracked limestone.The rocks of these mountains are based on porous sand stone, lying themselves on clays and marls.Their tops, always flat, are lime stone lands, as those located in im-mediate vicinity of Tlemcen: Lalla Setti, Ain Fezza.It is a formation consisting mainly of limestone and dolomite alternating with beds of marl and sand stone.The primary bed rock forms the base of the High Plains, which consist of conglomerate sand lacustrine limestones in a collapsed compartment of secondary land.Mountains of Sidi-Djilali correspond to a northern advanced of high plains of the high lands Benest [6].Furthernorth the Jurassic Mountains of Tell separates the plain of Moulouya (situated in Moroccan territories).
Lithology briefly presented in this study can have some preponderant influence on the pedogenesis in semiarid place, in one hand, and on some conditions of plant life on the other hand.

Depression of the High Lands (El-Aricha, El-Bayadh)
This depression is full largely by quaternary material of alluvial origin.In his study of the plain of Moulouya, Ruellan [7], reports the relationship which exists between ground types in the one hand and shapes and deposits on the other hand.Quaternary formation are organized in nested terraces along the wadis, in particular the glaze terraces.These formation contain calcareous brown soil with calcareous accumulation, localized on quaternary glaze, they are characterized by a small deepness (20 to 50 cm) a sandy loam texture, a rate of organic matter under 2%, an absorbent complex saturated in magnesium and calcium and a vegetation based on Stipa tenacissima, Artemisia herba-alba, Lygeum spartum… Steppic ground are significant in the majority of plains from Sebdou to El-Bayadh via El-Aricha till semi-arid valley, by the number of their characters, they can remind of chestnut ground, brown ground and the Sierozems of Russia Aubert [8].However, Duchaufour [9] precised that all soils of the steppe belong to the iso-humic soils.In these steppes and the steppe of El-Bayadh region, we find a considerable area occupied by shallow soils, these are: • Raw mineral soils and little evolved of erosion on the mountains and outcrop of geologic substratum.
• Calcimagnesic soils with slab, calcareous crust or crusting on encrusted glaze of old or middle quaternary.
In steppic environment of North Africa, we often find grounds with salinity, either on source rocks containing a high content in salts, or in the endorheic depressions (Chotts and Sebkhas).Halophytic vegetation can cover larges areas.

Bioclimate
In order to know the bioclimatology of our place of study, we referred to the data of Seltzer [10] and that of national office of meteorology of Oran for the period of 1980-2008.
The combination of climatic parameters (precipitations and temperature).They constitute the hinge of climate because they influence vegetation by giving its typology Bary-Lenger, et al. [11].These parameters helped many authors for the development of several indices which indicate the climate and existant vegetation, especially the classification of Debrach, the theombrothermic diagrams and pluviothermic Emberger Quotient.
According to the classification of Debrach [12], the climate of Beni-Snous is semi-continental (M-m = 28˚C), that of the high lands is continental (El-Aricha M-m = 35.77˚C).

Ombrothermic Diagrammes.
They are used to determine the length of the dry period of the year, by considering the dry month when P = 2T, P = average rainfall in mm, T = middle temperatures of the same year in ˚C.In order to visualize these diagrams, Bagnouls et Gaussen [13] propose a method which consists of focusing on the same graph the temperature and the pluviometry so that the scale of temperatures doubles that of precipitations, by considering the drought when the curve of precipitations goes under the curve of temperatures.The region of Beni-Snous presents a period more or less dry during the year, it lasts 6 months, that of the central land exceeds ten months of the year.These periods of drought coincide with the summer period, including, sometimes a part of spring and another part of autumn.The duration of drought is strongly influenced by the altitude, the temperatures increase tardily at the level of these mountainous slopes and increase earlier on the coastline.

Pluviothermic Emberger Quotient
Used in northern Africa and in the Mediterranean countries, this quotient remains an essential tool for characterizing the bioclimate of a region.By using a two-dimensional diagram in which the value of quotient of a determined locality is in ordinate and the average of the coldest month of the year in abscisse.
This quotient allows you to view the position of the meteorological stations and to delimit the bioclimatic period of plant species or a vegetal group and to make any comparison.It was formulated as follows: • The climagramme shows that the mountainous bioclimate of Beni-Snous is semi-arid and higher with a tempered winter, only in high altitude where it is sub-humid lower with tempered winter variant (Q 2 = 66.51 et m = 5.4 C˚).The fresh semi-arid appears in places of more than 400 m of altitude and spreads until the steppe.In steppic area, the bioclimate differs from the Saharan bioclimatic stage higher than arid bioclimatic stage with cold winter variant (Q 2 = 36.51and m = −1 ˚C).We conclude (that the climate of the region is typically Mediterranean, where there are essentially two bioclilmatic stages, the semi-arid which is the most spread, and the arid, with a hot and dry season in contrast with a cold rainy season.The actual rainfall precipitations on the mountains vary between 350 mm and 480 mm, this is what explains rusticity of vegetal species (Pinus halepensis, Olea europea, Ziziphus lotus, Juniperus oxycedrus) of the region.The climate parameters have a certain and direct influence on the development of vegetal species.Two principal parameters were always taken into consideration; rainfall precipitations and the temperature.

Sampling Methods (Flora)
Vegetation surveys are realized according to classical methods, by establishing a list of all the species on an area unit set beforehand within a homogeneous station, by giving two indices to every species: abundance, dominance, and sociability.
In order to know the floristic composition of the area of study, twenty phytoecologic surveys were respectively realized at the level of pre forest mountains around Beni-Snous and in steppic areas during the lasts years (2011 to 2014), when everyone has the woody species list accompanied with a set of ecologic and physionomic information.The number of inventoried species rises to 158 in Beni-Snous and to 60 at the level of the steppe.
Taxa identification was made from the flora of Maire [14], that of Quézel and Santa [15] and of Bonnier [16].After they have been classified by family, the inventoried species were characterized botanically.
The inventoried species were subjected to characterization.The species counting is made on the totality of inventoried species in each station of the two regions.
• Morphologic, distinguishing wood types, perennial types and annual herbaceous.

Anthropic Actions
In our study, we devoted an important part to anthropization, this is how the data related to population, human activities of two regions as the social structure, demography, migratory movements, overgrazing, of town hall, from magister works of Benabadji Bouchenak [18] of Boukhoza [19] and Bourdieu [20] and the investigations made on sites of study from population after many missions made.

Population of the Region
A small berber islet in western Algeria, situated between Tlemcen and Moroccan border.Linguistically, as mentioned by Salem Chaker [21], Beni-Snous can be related to the rifain set, and more particularly Beni-Iznassen, with whom they share many particularities.Roger Bellissant [22] mentioned that the population of Beni-Snous belonged to the Azail who occupy this picturesque region.In the past, it was composed of four tribes Azaïls, El-Khémis and its surroundings, Kef and Béni-Bou Saïd.Whereas now, it is composed of El-Khemis and its dependances and Azail.Every social structure, has its own name referring to its ancestor.The group members considered themselves as the ancestor descendants of whom they often take the noun.El-Khemis is the capital of the region and the noun of the tribe.Built on the edge of wadi El-Khemis, Beni-Snous possesses an uphill and below a suburb of many villages of which it is the economic center, because it is in El-Khemis where the only market is held.And it is the political center because this is where the caîd lives.These villages are, from douwn stream to upstream: the Wadi, Beni Hammou, Oulad Moussa, Oulad Arbi, Béni Achir, Dehar Ayed, Béni Zidaz, and further Sidi Larbi et Mazzer.All these villages exist thanks to the presence of wadi El-Khemis.It brought the small alluvial that the berbers cultivate in these wild places.Below toward meridional zone, particularly on the steppic plains, there are two kinds of populations; Ouled Nehar Ghoraba who occupy the western part of the region (Magoura, Sidi Djilali), Ouled Nehar Cheragua occupy Aricha areas.According to the kind of life, we can distinguish between the nomads and semi-nomadic people; desert for the firsts and steppe for the seconds who seem to oppose the old sedentary townsfolk.However, between the two a series of continuous transitions exists.

Population Distribution
The great majority of population tends to occupy southern piedmonts of mountain ranges of Tlemcen, where life conditions (climate, soil quality, level of natural resources, etc) are more or less favorable.They are also concentrated next highways (trunk roads, wilaya paths) leading to El-Aricha, Sebdou, Tlemcen).A part from the sparse populations and the watershed, we can say that the high plains are uninhabited.The average density rises to 7 inhabitants in Km 2 El-Gor, El-Aricha and El-Bayadh.Everywhere else communal density seems lower because of strong dispersion of populations.Densities don't exceed 3 to 4 inhabitants in Km 2 (El-Aouedj, El-Aricha, El-Bayadh), they remain very scattered in the territory.Agglomerated populations represent higher densities: • Whether in real urban structures, • In old colonisation centers, • Or, firmly, in hamlets.Distribution of lower density zones displays a contrasted situation and opposes clearly two part separated by trunk road 22.
In the steppic plain, El-Aricha, Naama, El-Bayadh, Sebdou grew on the surface.The average annual extension can, sometimes reach 2.4 Ha.Hamlets, housing grouping seem to impose a lifestyle approaching that of agglomerations situated in the north.The extension of these hamlets and other groupings is, sometimes, rising more than the agglomerations.Highlands gather a weak population which seems to settle.
In the west, in the township of Beni-Snous, Azail, densities are, often between 6 to 9 inhabitants in Km 2 .The number is never below 5 inhabitants in Km 2 .The high plains till Ras El-Ma, El-Bayadh, are completely differents.Areas of settlement represent lower densities.Densities, rarely, exceed 3 inhabitants in Km 2 (El-Aouedj, El-Aricha, El-Bayadh), especially in lower and flood places of the plain.

Migratory Movements (Figure 2)
Migratory phenomenon seems to affect all towns from Beni-Snous to El-Bayadh via El-Aricha and Mechria.
It is very difficult to know the migratory movements, their origin, and their rhythm.Census mention very little indications.So we did not consider places of birth or successive residences of inventoried persons.Partial and heterogeneous information are at our disposal.Before arriving to the desirable precision, some facts can be established, the outlines of migratory movements can be identified.
We notice that the population movements, generally, occur towards the agglomerations of the north, as Sebdou, Tlemcen, Sidi-Bel-Abbès.Migrants leave searching for an employment or an occupation.This happens, particularly with young people who remain residents in rural area but work in urban one.These movements often, caused troubles in revenues and consumption habits in rural environment and resulted in abandonment of agro-pastoral employment.
Some migrations find obstacles.The state borders of young countries remain obstacles for traditional movements.The same tribe can have its different lineages scattered among several countries and cut from these traditional corridors of semi-nomadic movements.
Many semi-nomadic people are attracted by the standard of modern life and are themselves settled.Schooling as among the main reasons for this settlement because the educated youth do no more want to run after the sheep [4].

Evolution of the Population
Census data show that growth rate is rising through the years.Between 1987 and 2002, the population in Tlemcen (chief place of the region) increased from 111,588 to 137,578, which represents an increase of 18.89%.In Sidi Djilali, the population rised significantly from 9504 to 11,433 between 1977 and 1987.The population densities seem to experience changes from one region to another.In the piedmonts of Sebdou and Sidi Djillali, the whole population reaches 13 inhabitants in Km 2 , and the dispersed population amounts to 5 inhabitants in Km 2 .Tlemcen and Beni-Snous have a high rate, 59 inhabitants in Km 2 .
Figure 3 shows a rise in population of El-Aricha, which increased from 4200 (1966) to 8500 (2008).From 1977 to 1987, the region experienced a significant decline of population from 6200 (1977) to 6050 (1987).This decrease may be the consequence of migrations searching for survival jobs (Figure 2).The largest majority of the population is concentrated in the main towns.This concentration causes a consumption of pre-forest land and rangelands.Population growth in regions concerned led to uncontrolled exploitation of the environment and inappropriate agricultural practices that leave no possibility for space regeneration.4 and Figure 5)

Biological Types
These biological types, in these formations, remain very heterogeneous.These spectra show a reduction, and a total absence of phanerophytes du, essentially, to degradation phenomena and to an increase of therophytes, especially at the level of some exploited stations.
The steppe is dominated by therophytes (73%, Alyssum campestre, Atractylis carduus, Centaurea pullata, Herniaria hirsuta…), the chamaephytes are in second position with 19% (Astragalus armatus, Eryngium matritimum, Echinops spinosus, Artemisia herba-alba, Stipa tenacissima…).Hemicryptophytes (7%) are represented by Dactylis glomerata, Paronychia argentea… Hemicryptophytes are very weak, represented by number 2 in Sidi-Djilali and 3 in Nedroma, this can be explained by a soil poor in organic matter.This phenomenon was confirmed by Barbero [31]: "Indeed, the abundance of hemicryptophytes reflects a wealth of organic matter in forests and a high altitude".Despite the importance of therophytes, the chamaephytes keep an important place in psammophile vegetal formation.They are better adapted to aridity.The harsh climate and structural instability of the ground support the development of short-cycle species, more or less demanding in water and trophic needs.

Morphological Types
There are three morphological types: In Beni-Snous these morphological types are distributed as follows: • Annual herbaceous (49%) as Avena sterilis, Arsarum vulgare… • Perennial herbaceous (31%) as Juncus maritimus, Allium nigrum • Perennial woody (20%) as Pinus halepensis, Quercus suber Vegetal formations are marked by their heterogeneity between woody and herbaceous, in one hand, and perennial and annual in another hand.Perennial annual species dominate with 46%.
In the steppic region (El-Aricha and El-Bayadh), these morphological types are distributed as follows:  which constitute about 30% of natural rangeland, which results in overgrazing, soil compaction, lack of regeneration, aging plantations, can rise from three to four times according to the regions.In these mountains, the pastoral charge, always, remains worrying and may cause environmental degradation.Herd composition shows an overwhelming predominance of small livestock, particularly sheep which occupy about 75% of the number of herds Aidoud Lounis [32].These lasts are more and more concentrated in very small spaces exercising a strong pressure on the environment.Figure number 6 also shows strong domination by sheep (88%), goats (8%), and finally cattle (4%).
The steppes of North Africa occupy more than 63 million hectares of low and sparse vegetation submitted to very old human exploitation.The above ranching of sheep and goats has been the historical vocation of the steppes.This situation has endured for centuries until the mid 20th century Aidoud, et al. [33].Cultures seem to stretch on surfaces where the forest has existed and where grazing pressure has significantly increased.This is generally based on extensive livestock transhumance and breeders who are at the same time farmers.Courses are exploited by a very important charge of animals.Open to public (pickers, walkers, etc.) these matorrals, by the succeeding of continual population growth of agglomerations, trampling, and degradations multiply.
Clearing of pre-forest lands for the benefit of cultures (cereal and food) affects more than 20% of areas and tends to make them very vulnerable.Sometimes as a result of reductions in rangeland, anthropogenic pressure causes overgrazing in these silvo pastoral ecosystems.Despite its important economic role, the agricultural sector still faces structural problems (land structures) and natural ones.
Transformations of vegetation are related to the evolution and extension of cultures, loss of forest areas, changing rural landscapes, anarchic recolonisation of environments through infrastructure (urbanization matorrals).Thinning forests are recovered for agriculture and procurement of firewood.
The slow regeneration of perennial species also causes a change of vegetation.These perennials are marked by heterogeneity between the woody and herbaceous and between perennials and annuals, but also by the harsh climate promoting the development of herbaceous species of short cycle at the expense of perennial woody generally more demanding in water and trophic needs.Disturbances which affect the mountains of our regions (Tlencen, Béni-Snous, Sebdou and Sidi Djilali) caused diversification of the floristic procession (4.Vegatation and activites).

Fire
By its floristic composition, the area of study could not escape the fires.The annual average of burned areas represents 120 hectares for the period between 1992 and 2004.Most of these fires are due to human negligence related to pyromania.The causes of forests fires are known and the works of Amouric [34] are applied for giving summary review, among the most recent, we mention: • Increases in frequency tend to accelerate in the summer during critical periods; • The penetration routes of most forests; • Pyromania; Climatic conditions play an important role first in the fires and their inter-annual and inter-regional irregularities.
It seems that, apart from pyrophytiques formation represented by Pinus halepensis, Cistus ladaniferus, Cistus villosus, Thymus ciliatus, the presence of the Lamiaceae, Papilionaceae and Cistacées can also accelerate fires.

Threats of Ecosystem
Among the formation corresponding to further stages of degradation, before the bare earth, we can mention: • the ermes with Ampelodesma mauritanicum, Asphodelus microcarpus and Urginea maritima, presenting sometimes release of green oak and some species of matorrals • Lawns with Filago pyramidata et Plantago lagopus • Lawns with Bromus rubens, etc.
The actual human pressure (overgrazing and cultures) do not allow them to reconstruct forestry or pre-forest groups to which they belong.It seems that the actual climatic conditions are not a favorable factor in this reconstruction.
At matorralisation resulting from foresty and pre-forest structures, rapidly succeed a dematorralisation with a complete extinction of woody other than softwood and the appearance of some species which announce the steppisation (phenomenon observed in the steppe of El-Aricha and El-Bayadh).This last is characterized in the

Figure 1 .
Figure 1.Location of pre-forest and steppic areas.
medium precipitations in mm; M = Average of maxima of the hottest month in (Kelvin); m = Average of minimas of the coldest month in (Kelvin).

.
Location of study areas.