Ecological Engineering 85 (2015) 132–143 Contents lists available at ScienceDirect Ecological Engineering journal homepage: www.elsevier.com/locate/ecoleng Biophysical and anthropogenous determinants of landscape patterns and degradation of plant communities in Mo hilly basin (Togo) Badabate Diwediga a,b,∗ , Kperkouma Wala b , Fousseni Folega b , Marra Dourma b , Yao A. Woegan b , Koffi Akpagana b , Quang Bao Le c a West African Science Service Centre on Climate Change and Adapted Land Use (WASCAL) Graduate Research Programme, Department of Civil Engineering, Kwame Nkrumah University of Science and Technology, Kumasi, Ghana b Laboratory of Botany and Plant Ecology, University of Lomé, 01 BP, 1515 Lomé 01, Togo c CGIAR Research Program in Dryland Systems, International Centre for Agricultural Research in Dry Areas (ICARDA), Amman 11195, Jordan a r t i c l e i n f o Article history: Received 14 April 2015 Received in revised form 8 September 2015 Accepted 13 September 2015 Keywords: Landscape patterns DCA Eco-edaphical factors Human disturbances Ecological conservation Mo basin Togo West Africa a b s t r a c t In mountainous areas, biophysical settings and human disturbances strongly influence landscape patterns and dynamics requiring a permanent understanding of their combined influence. In this study, we investigated the diversity and patterns of wild landscapes in relation to ecological factors, human disturbances and land protection regime in the Mo river basin (Central Togo). First, we used geographical information systems (GIS) and remote sensing techniques to quantify and spatially explicit the major land cover types occurring in the area. We performed a supervised classification of Landsat 8 image from 2014. Next, we used vegetation ordination and classification methods to detect vegetation group types and their similarity level from forest inventory data collected at 75 sites. Data from soil samples at the 75 sites and DEM-based topographical indices were used as biophysical variables to analyze factors of current landscape structure. Both satellite image classification and the outputs from ordination methods indicated that three major vegetation types (forestlands, woodlands and savannahs/shrubs) occurred in protected (PA) and unprotected (UPA) areas. Image classification showed that savannahs/shrubs are the most widespread vegetation types (54.4%) while forestlands and woodlands cover 10.4% and 26.4% of the total area, respectively. UPA showed high rates of human disturbances that shaped the occurrence of a fourth vegetation type made up mainly by degraded savannahs and woodlands. Along the land protection gradient, the landscapes are driven by soil nutrients and moisture, in combination with the influence of topography and human disturbances. In both PA and UPA, and along protection gradient, majority of features exhibited significant differences among plant communities. The spatial analyses combined with the field data providing information on vegetation cover, species richness, and human footprint indices suggested that some areas outside protection still exhibit high potentials for land conservation. In multifunctional landscapes of Mo basin, conservation strategies could also be encouraged in the wild landscapes of community common lands to promote both biodiversity conservation and sustainable provision of ecosystem services. © 2015 Elsevier B.V. All rights reserved. 1. Introduction Diverse landscapes are host of biodiversity and provide a wide range of ecosystem services, requiring knowledge on the socialecological interactions. Understanding the interactions between human imprints and biophysical components defining the landscape heterogeneity has been considered as a fundamental for ∗ Corresponding author at: 01 P.O. Box, 1515 Lomé 01, Togo. E-mail addresses: diwedigaba@gmail.com, diwedigaba@yahoo.fr (B. Diwediga), kpwala75@yahoo.fr (K. Wala), q.le@cgiar.org, q.le@alumini.ethz.ch (Q.B. Le). http://dx.doi.org/10.1016/j.ecoleng.2015.09.059 0925-8574/© 2015 Elsevier B.V. All rights reserved. landscape management and biological conservation (Ali et al., 2014). In tropical regions, natural landscapes, especially woodlands and forests provide many functions and services, such as biodiversity conservation, climate regulation and livelihood support to millions of people (Zeleke and Hurni, 2001; Shackleton et al., 2007; Tindan, 2015). In majority, population depend on these natural resources that they manage and conserve according to their usage and resources (Appiah et al., 2009; Pare et al., 2010; Pouliot et al., 2012; Ouedraogo et al., 2013; Steele et al., 2015). This situation led to management options through protected areas and community forest zones in order to serve as guards for landscape conservation. Unfortunately, increasing human pressures on land resources B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 affect these protected areas, aggravating the failure of their biological conservation role (Folega et al., 2010a; Wala et al., 2012; Damnyag et al., 2013; Dimobe et al., 2014; Folega et al., 2014b). It hence appears that human disturbances are taking over natural ecological factors in shaping and changing the functions, structure and aesthetics of the landscapes. This broad-scale human-related disturbance and destruction of native vegetation is considered as landscape fragmentation and degradation (Bennett and Saunders, 2010). Globally, landscape fragmentation and heterogeneity changes are primarily induced by increasing human disturbances, especially agriculture, wood extraction of timber and charcoal production (Pare et al., 2009b; Norris et al., 2010; Pare et al., 2010; Onojeghuo and Blackburn, 2011; Wale et al., 2012; Vu et al., 2014; Wampembe et al., 2014). Landscape heterogeneity is most often driven by complex mechanisms being the result of a natural dynamic phenomenon influenced by human imprints, policy response, climate change, market, and poverty (Appiah et al., 2009; Zhang and Zang, 2011; Appiah, 2013) at a given time and location. In Togo, especially in the Central region covered by mountainous ecosystems, numerous human pressures are shaping and disturbing the landscape patterns, even in protected areas. In these areas, intensive wood extraction of timber, firewood and charcoal production, and small scale farming system strongly affect the landscape structure and induce degradation of natural ecosystems (Dourma et al., 2009; Wala et al., 2012). In this context, land resource availability and location are changing following these human footprint gradients, calling for the spatial mapping of the landscape patterns in order to provide an understanding of how certain factors influence these changes at landscape level. While earth observation technology provides insights to assess the spatial patterns of the landscapes, field surveys are required to provide stand characteristics of each landscape component, especially vegetation types and soils. Interestingly, a combination of both methods could provide more understanding of the factors governing landscape structure for targeting options of sustainable use and management of resources (N’da et al., 2008; Hoffmann et al., 2012). Such information on intrinsic and exogenous factors can contribute to managing a more sustainable the landscapes considered as commons that are life-support systems on which people undeniably depend (Shackleton et al., 2007; Thondhlana et al., 2012; Tieguhong and Nkamgnia, 2012). Landscape planning needs not only knowledge of the nature of factors causing the dynamic of land cover, but also necessitate spatial information to target areas likely or not to undergo changes. Mo river basin, embedded in one of the richest landscapes in Togo covering three protected areas, is undergoing continuous transformation. Despite its importance, the ecological status and appropriate conservation management remain poorly understood. Furthermore, as in the whole Togo, there is no master plan aiming at promoting the sustainable allocation of land resources. Though protected areas are erected in the region to ensure biological conservation, the public policies failed due to weaknesses in law enforcement and illegal incursions (Wala et al., 2012). Attempts to propose pathways for sustainable management of landscapes were undertaken fundamentally on the characterization of vegetation structure and floristic composition in relation to environmental variables and human disturbances (Woegan, 2007; Dourma, 2008). Acute attention has only been paid to the use of species composition, and vegetation stand structure as evaluation indicators of land performance and landscape heterogeneity. No insight is provided on the spatial patterns of the evaluated land resources in order to inform about the potential resource availability. Furthermore, potentials of the soils in terms of chemical contents are not well understood, although correlations between soil conditions and vegetation influence the landscape patterns (Galal and Fahmy, 2012). 133 In the context of insufficient information to tackle landscape fragmentation issues, further researches that integrate spatial dimensions still need to be undertaken at local and national levels. Therefore, in this study, we used an approach that integrates geographical information systems and remote sensing combined with field measurements in order to spatially explicit landscape patterns and assist the sustainable management of the multifunctional landscapes of the Mo river basin. The specific objectives of the study were to (i) provide a spatially explicit map of the current landscape heterogeneity in natural and semi-natural landscapes of both protected and unprotected areas of Mo basin; (ii); analyze biophysical and human disturbances prevailing at the landscape level, and (iii) determine the stand characteristics as well as soil chemical conditions in each vegetation type. By hypothesizing that protected areas exhibit better indicators of land conservation performance than unprotected areas, we investigated on the structure and stand characteristics as well as edaphic-ecological variables according to land protection regimes. The outputs of the study are suggested as potential indicators of landscape configuration, threats to land conservation and land characteristics that could help in re-addressing poor land management issues and landscape planning in the Central Togo. 2. Methodology 2.1. Study area Mo watershed is a sub-unit of the Volta basin (West Africa) located in the Central Region of Togo (Fig. 1). With a total area of 148,592 ha, the basin is particularly sensitive as it contains great parts of the Fazao-Malfakassa National Park (FMNP), the Aledjo Wildlife reserve, and Kemeni Forest reserve. Due to the increasing demand for land resources, these protected areas are likely to undergo more human pressures (Woegan, 2007; Wala et al., 2012). The Mo basin is embedded in the Ecological Zone 2 of Togo, characterized by a mosaic of dry and riparian forests, woodlands, guinea-soudanian savannahs. Dominant land uses within the human-dominated landscapes (non-protected zones) are small scale agro-systems (Woegan, 2007). The predominant plant species in the area are Isoberlinia doka Craib & Stapf, Isoberlinia tomentosa (Harms) Craib & Stapf, Monotes kerstingii Gilg, Detarium microcarpum Juss. and Uapaca togoensis Pax., etc. (Woegan, 2007; Dourma, 2008; Dourma et al., 2009). The climate is tropical subhumid characterized by a rainy season from April to October (Petit, 1981). Mean annual rainfall is between 1200 and 1300 mm with an irregular spatial-temporal distribution. Mean minimal and maximal temperatures reach respectively 19 ◦ C in January with the Harmattan winds and 30 ◦ C in April. Evapotranspiration is generally high, especially during dry season and can reach 1600 mm per annum. Some parts of the hilly lands have elevation above sea level higher than 800 m, especially in Aledjo Mounts. Other mounts are of variable heights, comprising the massifs of Mazela (704 m), mount Akitili (861 m), mounts Kouzé (625 m) and Kpeya (652 m). Mounts Malfakassa composed of Ouassi (568 m), Zandebou, Tchakouya, Timbou et Balankan (Woegan, 2007). The rivers/streams network is heavily developed in accordance with the mountainous relief. Mo, Loukoulou, Kamasse, and Bouzalo are the most important streams of the basin. On morpho-structural angle, the Mo basin is dominated by sericite and muscovite dominant quartzites. Lithosoils and ferruginous tropical soils are the dominant soil types with some patches of ferralitic soils (Lamouroux, 1969). Foremost of the land uses in the area is small-scale subsistence farming, pasture lands, protected areas and built-up areas. The prominent environmental issues are land degradation due to overgrazing, unsustainable agricultural land use, fuel wood harvesting 134 B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 Fig. 1. Location of the study area. and charcoal production (Fontodji et al., 2009; Fontodji et al., 2011; Aboudou, 2012). Illicit incursions for hunting and tree logging in protected areas are also concerns that cause conflicts between land users and state agencies protecting lands. In addition, protection enforcement regarding the protected areas is weak and non-inclusive. The catchment is relatively important for tourism and one of the breadbaskets (crop production) of the country. The population is mainly composed of rural farm households and cattle herders living in villages and hamlets interlinked by a poor network of rural tracks serving in transportation of goods and other services. 2.2. Deriving Mo landscape patterns based on land use/cover mapping In order to provide a spatial glimpse of the different vegetation types in both protected and unprotected landscapes of Mo basin, this study relied on the use of Landsat 8 satellite image of March 2014. This data was downloaded from https://earthexplorer.usgs.gov. Land cover classification followed the Yangambi’s vegetation nomenclature system defined based on tree heights, canopy cover density, and grassy layer coverage (Aubreville, 1957). We defined six land use cover types (hereafter, LUC) based on landscape features that were depicted during reconnaissance field works and previous studies in the same area (Woegan, 2007; Dourma, 2008). Namely, these LUC are (1) forested lands (riparian and dry forests), (2) woodlands (open canopy forests and woody savannahs), (3) savannahs (tree savannahs and shrubs, and scattered grasslands), (4) cultivated lands (farms, young fallows, and parklands), (5) residential areas (built up areas including urban constructions and rural settlements), and (6) water bodies (rivers and reservoirs). Paved surfaces and bare rocks are mostly confused among settlements and agricultural lands since they reflect in the quite similar range. We used ENVI 4.7 and ArcGIS 10.0 software to perform the maximum likelihood classification. Since the focus of the study is vegetation-related analyses, Normalized Difference Vegetation Index (NDVI) is selected among many other vegetation indices for it is widely used as a powerful indicator of vegetation greenness, and less sensitive to topographic factors in mountainous areas (Matsushita et al., 2007). Original bands and NDVI layer were stacked in a multilayer image. Analyses were pixel-based using on-screen digitizing procedure to produce training areas for each LUC on an RGB colour composite image. Though topography is a common source of biases in land cover classification in mountainous areas (Vanonckelen et al., 2013), elevation data were not integrated during the classification process. The main reason is that the maximal elevation above sea level in the study area is around 850 m and does not really provide significant hill shade effect at the sensor passing time (Diallo et al., 2010). Image classification relied on 177 ground truth points collected during forest inventory, based on random sampling within the different vegetation cover types. Since the number of field-registered points was insufficient to serve as training and validation data, we generated training sites for each class based on Google Earth images of the same date combined with a topographical map of Togo and other field knowledge. As the acquired image corresponds to the dry season, there was sharp distinctions between the different cover types, especially vegetation and lands under crops. At least 60 training pixels were selected for each LUC from homogeneous large areas (Zhai et al., 2013). Finally, all the 177 geo-located points were used to assess the accuracy of the classified image through a confusion matrix. 2.3. Collection of vegetation data and ecological variables Since topography was the main constraint during the sampling, we set 75 forest inventory plots along a topographical gradient from valleys to top-hill or summits without any predefined plot number for each location. Thus, we randomly set these plots according to the accessibility, the representativeness of flora biodiversity B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 and the vegetation homogeneity in such a way to represent the different vegetation types in the landscape. In total, the number of plots varied according to protection regime (39 and 36 plots in protected and unprotected areas, respectively) and vegetation types (9 in dry forests, 19 in riparian forests, 10 in shrubs, 19 in tree savannahs, and 18 in woodlands). Squared plots of 20 m × 20 m and 30 m × 30 m were set in dry forests and savannahs, respectively. Meanwhile, plot dimensions were about 50 × 10 m in riparian forests in order to match the linear shape and the width of these ecosystems in savannah-dominated landscapes (Folega et al., 2010a; Wala et al., 2012; Dimobe et al., 2014). In each plot, we focused on woody plant species and recorded the following attributes for each tree: species name, total height, diameter at breast height (DBH), crown diameters (North-South and West-East directions), crown height, and trunk height. In addition, the geographical variables (longitude, Latitude, Altitude above sea level) were collected using a GPS Garmin 62S. Human disturbances, i.e., fire occurrence, grazing, selective tree logging and charcoal production, were recorded as the presence/absence (1 = presence, 0 = absence). Other ecological attributes such as vegetation type, soil type, soil submersion (0 = No, 1 = Yes), canopy cover density (coded as 0 = very low, 1 = low, 2 = medium, and 3 = high) and protection status (1 = protected, 0 = free-access) were collected as well. For data processing purpose, six major topographical positions have been defined (i.e., flat terrain, hill-foot, mid-hills, hill summits, riverbank, and inland valleys) and coded from 1 to 6, respectively. In addition to the aforementioned ecological characteristics, soil samples were collected at two depths (0–10 cm and 10–30 cm) to provide soil chemical properties of each forest inventory plot. For each depth at each site, five sub-samples were mixed thoroughly before collecting one representative composite sample. For both depth, 150 samples were collected and air-dried for chemical analyses. Three basic chemical properties were determined: soil organic carbon (SOC, in %), total nitrogen (TN, in %), and pH water. SOC was determined using Walkley-Black method, which consists of titration of excess potassium dichromate used with sulphuric acid to react with 3 g of dried soil. SOM was derived from the SOC using the Van Bemmelen conversion factor (1.724) commonly used for the estimation of organic matter content (Sebastia et al., 2008; Fontodji et al., 2009; Agboadoh, 2011). The total nitrogen was analyzed using Total Kjeldahl Nitrogen method. The potential of hydrogen (pH), which measures the acidity or alkalinity of a solution, was determined using 1/2.5 soil/water ratio. The pH of the solution is electronically and directly measured using a glass electrode pHmetre. Furthermore, to assess the potential influence of topography on vegetation types in Mo basin, other biophysical indices were derived from the DEM-SRTM 1 arc-second (approx. 30 m) downloaded from earthexplorer.usgs.gov. These indices included terrain attributes such as slope, Topographic Wetness Index (TWI), and mean altitude above the channel level (Alt a.c.l.). The TWI is a topographic variable indicating the spatial distribution of soil moisture conditions, a potential indicator of species preference to moisture. Alt a.c.l. is used to indicate the potential depth to groundwater/free water for plant species, and therefore to moisture content in the substratum. Maps of slope, TWI and Alt a.c.l were derived using SAGA GIS 2.0.8 platform that embeds the algorithms for computing these variables. Soil texture was obtained from HWSD but was not considered in detailed analyses for no difference existed in soil properties according to soil types. The various maps were then exported to ArcGIS 10 that helped in extracting values of the variables to geographical coordinates of the 75 plots. IBM SPSS 20 and Microsoft Excel served in data preparation for further analyses. 135 2.4. Vegetation and ecological data analyses The ordination method was used to identify environmental gradients defining species distribution and landscape patterns. Among the various multivariate methods used for this purpose in plant community analyses, the indirect gradient algorithms (DCA), cluster analyses (CA) and two ways indicator of species analysis (TWINSPAN) were used to analyze the variation of plant communities and their relationships with environmental variables. The first reason is that they are commonly used for plant community analyses (Dourma et al., 2009; Tavili and Jafari, 2009; Folega et al., 2010b; Zhang and Zhang, 2010; Folega et al., 2011; Wala et al., 2012; Wale et al., 2012; Kebede et al., 2013; Dimobe et al., 2014; Folega et al., 2014a). The second reason is that the dataset was too heterogeneous and too many species deviated from the assumed model of linear response (Leps and Smilauer, 2003), for the length of gradients (which measures the beta diversity in community composition, i.e., the extent of species turnover along the individual independent ordination axes) obtained during trials exhibited values between 3 and 4. In such cases, it was compelling to select unimodal method using the indirect detrended DCA method by segments down-weighting rare species without any transformation of the initial information. DCA methods summarize variation in the relative frequencies of the response variables (species). An important implication is that these methods cannot work with ‘empty’ samples, i.e. records in which no species is present (Leps and Smilauer, 2003). The DCA were performed in CANOCO 4.5 and CanoDraw 4.1 for Windows. TWINSPAN in CAP 2.15 (Community Analysis Package) clustered plant communities according to their level of similarity. First, a matrix of 75 plots × 142 plant species subjected to a DCA ordination did not help in depicting plant communities along any gradient. Therefore, the data were split into 36 unprotected relevés and 39 relevés in PA. The two matrices, 39 relevés × 121 species and 36 relevés × 100 species were subject separately to partial ordination, respectively for PA and UPA. Three measures of species diversity, i.e. species richness (S), Shannon-Wiener’s species diversity index (H ), and Pielou equitability index (E), were computed to characterize each plant community. Species richness (S) was computed for each plant community as the total number of woody species recorded in the relevés of the community. Because of different plot sizes, mean species richness at plot level was calculated as the number of species in a plot divided by the log of the area sampled (White et al., 2014). Shannon-Wiener’s species diversity index (H ) is calculated using the formula of the form: S H = − (Pi)log 2(Pi) i=1 where Pi = Ni/N with Ni is the number of individuals of species i and N is the total number of individual of all recorded species. Pielou equitability index (E) is calculated based on H and S as: E=− H log 2(S) Plot basal area at breast height (G in m2 ha−1 , sum of crosssectional area of all trees with DBH ≥10 cm in a given plot) and mean values of several other features were calculated for each plant community according to protection status: 0.0001sqr(di) 4A n G= i=1 where n is the number of trees recorded in the plot, A is the sampled plot area (plot size, in ha), and di is the DBH (in cm) of the ith tree. 136 B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 5 Protection status Fire occurrence Soil submersion Cattle grazing Axis 2 Canopy density Topography Tree logging -1 -2 Axis 1 5 Fig. 3. DCA of 75 relevés × 142 woody species in protected (green diamonds) and free-access areas (black circles). (For interpretation of the references to color in figure legend, the reader is referred to the web version of the article.) Fig. 2. Current spatial patterns of land cover types in Mo landscape. In addition, vegetation stands were characterized by computing their tree (DBH ≥ 10 cm) density. Regeneration of all mixed species was also calculated to overview landscape dynamics. Mean soil chemical properties (pH, SOC, and TN), and stand conditions (mean indices of soil submersion, fire occurrence, canopy cover, selective tree logging, and Alt a.c.l.) were calculated for the various plant communities in both free-access lands and protected areas. Similarity between plant communities was assessed using Jaccards’s index (Sij) and plotted using TWINSPAN in CAP 2.15. The performance of Jaccards’s Similarity was used to compare the plant communities under the different protection status: Sij = C A+B−C where A is the number of species belonging to the plant community i, B is the number of species belonging to the plant community j, and C the number of species belonging to both plant communities i and j. If Sij ≥ 50%, communities exhibit similarity; otherwise (i.e. Sij ≤ 50%), there is no similarity (Woegan, 2007). Supplementary statistical analyses were performed through analysis of variance to compare characteristics of the different plant communities, assuming equality of variance and normality in data distribution. Outputs from analyses of variance were contrasted using post hoc multiple comparison of Fisher and Tukey at p < 0.05. Pairwise correlation was performed to depict the relationship between biophysical and ecological variables within the vegetation types. northeast parts of the basin (Fig. 2). The spatial analysis showed that Mo basin is a heterogeneous landscape where small-scale farming, pasture, wood extraction and charcoal production dominate unprotected areas. Areas under protected status are relatively greener though human incursions are noticeable, especially at the edges. Overall, woodlands and savannahs/shrubs are the two dominant land cover types at the landscape level. Built up areas made up essentially by rural settlements covered about 0.3% of the areas outside PA. Water bodies showed the lowest coverage due to roughness that do not favour the occurrence of water bodies though the river network is highly developed. Overall, the southern and southwestern parts of Mo basin present wilder landscapes attributable to protection status and the increasing distance from settlements as well. However, these factors in combination with biophysical and soil conditions could provide explanations on the spatial patterns of the landscape. 3.2. Discrimination of plant communities and biophysical conditions in natural landscapes 3.1. Current landscape patterns from satellite image The outputs from the ordination of 75 relevés × 142 woody species (see species list in Table S8) in relation to human disturbances, protection status and other biophysical factors are shown in Fig. 3. Axis 1 of the DCA plot correlated positively with protection status (0.58) and topography (0.63) but negatively correlated to human footprints (−0.53 for tree logging and −0.63 for fire occurrence) (Tables S2 and S3). Meanwhile, axis 2 showed a positive correlation with protection status (0.64). These results indicate that the most important ecological factors determining landscape patterns are protection status and topography, in opposition to human disturbances. However, the ordination plot does not allow a net discrimination of the different vegetation types in the overall landscape. Hence, the 75 relevés were split into free access landscapes (36 relevés, black circles) and protected areas (39 relevés, green diamonds) for further partial ordination. The overall accuracy of the land cover classification was 83.1% with a kappa index of agreement of 0.79 (Table S1). Statistics on the areal distribution of the classification showed that the mosaic savannahs/shrubs are the most widespread vegetation types (80,836 ha) while forestlands covered 15,459 ha (10.4% of the total area) (Table S1). Human-made landscapes (croplands and fallows) occupying about 8.5%, dominated the central and the 3.2.1. Partial ordination of relevés of free-access landscapes The partial ordination of the 36 relevés × 100 species in unprotected areas (Fig. 4a) showed four vegetation types (U1, U2, U3, U4, U stands for unprotected areas; see supplemental file). Tables S4 and S5 showed that the first two axes of Fig. 4b defined gradients of soil moisture conditions and topographical positions. Axis 1 defines plant communities of moist and finer soils in lowlands (U1) versus 3. Results B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 2.0 a 3.5 R66 R96 U4 (a) R67 R54 R4 P3 Axis 2 (5.4 % of variance) Axis 2 (6.3 % of variance) R89 R28 R46 R37 R12 R14 R30 R10 R59 R25 U1 U2 R13 R48 R65 R63 R7 R19 R5 R57 R21 R11 R9 R97 U3 R8 R87 R95 R72 R71 R33 R27 R84 R91 R90 R78 R81 R92 R62 R47 R68 R70 R50 R55 R34 R85 R76 R69 R39 R3 R56 137 R80 R75 R52 R58 R45 R74 R16 R77 P1 R88 R43 R1 R73 R86 R60 R18 R83 R15 R6 R64 R20 R79 R82 P2 -0.5 -0.5 b Axis 2 (7.4 % of variance) -0.5 -1.0 0.2 5.0 Axis 1 (8.9 % of variance) (b) Grazing Fire occurence pH10 Soil texture SOC20 SOC10 Soil submersion Canopy cover density TN10 pH20 Soil texture Alt.a.c.l Slope Axis 2 (9.1 % of variance) 0.20 3.5 Axis 1 (13.6 % of variance) Alt_a.c.l. TN20 TWI Topography Fire occurrence Grazing SOC10 Soil submersion pH20 Slope pH10 Wetness index SOC20 Tree logging -0.20 -0.40 Axis 1 (18.9 % of variance) TN10 TN20 Topography Tree logging 0.30 Canopy cover density -0.3 Fig. 4. (a) DCA ordination of 36 relevés and 100 woody species taken from freeaccess landscapes showing the four plant communities. (b) DCA plots showing biophysical and soil properties under the 36 samples in free access landscape areas. those of dry and rocky soils located on relatively high lands (U2, U3 and U4). The DCA plot of environmental variables indicated a gradient of canopy cover density related to increasing soil moisture content and topographical position (axis 1) while axis 2 denoted mostly the effects of anthropogenic factors. From the combined analysis of the above-mentioned DCA plots in UPA, it is highlighted that U1 occurs more on richer soils in organic matter in topsoil. High density of canopy coverage, low slope and high soil moisture (TWI) characterize the community U1 though human pressures tend to modify the natural patterns (both variables are located at antipode sides of the DCA plot). The horizontal axis denotes a gradient of human pressures increasing from the left to the right side. Groups U1 and U4 are antipodes, with U1 in lowlands and U4 at hill summits. The relative high number of plots occurring in the right part of the DCA indicates that the majority of the vegetation types experienced human pressures such as illegal logging and grazing, and bush fires. 3.2.2. Partial ordination of relevés of protected areas The DCA ordination biplot (Fig. 5a) showed three groups of relevés clustered by axis 1 (8.9%), and axis 2 (5.4%) (Tables S6 and S7). The DCA plot (Fig. 5; see supplemental file). Combined analyses of above DCA plots in PA showed the coexistence of the biophysical and human threats that shape landscape composition. Indeed, P1 regroups sites in which species prefer richer soils in organic matter and TN in topsoils, and richer subsoils in TN. Releves of P1 are often in low topographic with high soil moisture (high TWI). Meanwhile, P2 occurs on soil with high pH and rich sublayers. They often experience more tree logging because of their relative low slope and their canopy cover density. -0.4 0.4 Axis 1 (12.3 % of variance) Fig. 5. (a) DCA ordination of 39 relevés and 121 woody species taken from protected areas exhibiting 3 communities (P1, P2, and P3). (b) DCA plot showing biophysical and soil properties under the 39 samples in protected areas. However, because of the relative low canopy cover density in P3, fire and grazing do occur often in these plots because of their richness in grasses and fodder herbaceous. In sum, the horizontal axis (axis 1) is comparable to an increasing gradient of topsoil nutrients and soil moisture from the right to the left side (summits and mid-hills versus lowlands and river banks). A combined effect of increasing gradient of human pressures from right to left is also interpreted from this plot (highly disturbed vegetation versus less disturbed vegetation). However, the second axis indicates mostly a decreasing gradient of vegetation physiognomy, which is denser from negative to positive canonical axes. Though groups exhibited low similarity, P2 and P3 are more similar (0.46) than P1. 3.3. Structural and dendrometric characteristics of plant communities of Mo basin Tables 1–3 show the stand characteristics and diversity indices of the various plant communities in free-access lands, protected areas, and merged analyses for PA versus UPA, respectively. In free-access landscapes, features exhibited significant differences among groups (ANOVA, p < 0.05), except for mean species richness (ANOVA, p = 0.362), tree density with saplings (ANOVA, p = 0.580), and sapling density (ANOVA, p = 0.509). Forested stands clustered in group U1 showed the highest mean values of tree height (10.5 ± 6.3 m), diameter (28.0 ± 17.4 cm), and density (947 ± 328 stems ha−1 ). With a mean basal area of 58.8 ± 14.1 m2 ha−1 , U1 exhibited the highest record, compared to U2, U3, and U4 with 18.6 ± 6.2 m2 ha−1 , 15.9 ± 7.7 m2 ha−1 , and 138 B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 Table 1 Stand characteristics in the four plant communities within none-protected areas. Characteristics Cluster U1 (8 relevés) Cluster U2 (7 relevés) Cluster U3 (11 relevés) Cluster U4 (10 relevés) ANOVA (˛ = 0.05) Species richness Mean species richness (per plot) Mean height (m) Mean DBH (cm) Mean diameter with saplings (cm) Basal area (m2 ha−1 ) Tree density (trees ha−1 ) Density without saplings (trees ha−1 ) Sapling density (saplings ha−1 ) Shannon index (unitless) Pielou evenness index (unitless) 58 19 ± 5aA 10.5 ± 6.3aA 28.0 ± 17.4aA 21.8 ± 17.6aA 58.80 ± 14.07aA 947 ± 328aA 678 ± 217aA 269 ± 219aA 5.04 ± 0.08 0.9 51 20 ± 6aA 6.7 ± 4.2bB 19.3 ± 8.7bB 13.2 ± 9.1bB 18.58 ± 6.19bB 921 ± 490aA 487 ± 167abB 433 ± 445aA 4.56 ± 0.10 0.8 66 19 ± 5aA 5.4 ± 3.7cC 18.3 ± 9.3bB 10.6 ± 8.1cC 15.93 ± 7.69bB 846 ± 432aA 311 ± 142bcC 534 ± 484aA 5.07 ± 0.07 0.8 49 16 ± 4aA 5.0 ± 3.5cC 19.4 ± 11.2bB 8.8 ± 7.9dD 7.66 ± 3.33bC 692 ± 428aA 156 ± 101cD 537 ± 444aA 4.65 ± 0.09 0.8 na p = 0.362 ns p = 0.000 ss p = 0.000 ss p = 0.000 ss p = 0.000 ss p = 0.580 ns p = 0.000 ss p = 0.509 ns na na Note: Outputs of one-way ANOVA: na, not available; ns, not statistically significant; ss, statistically significant (p < 0.05). Values that do not share a letter are significantly different at 95% confidence internal (CI) using ANOVA with post hoc test (p < 0.05). Capitalized letters are the outputs from Tukey comparison test whereas small letters are the results of Fisher comparison method. Group U1, Mosaic of riparian and dry forests; Cluster U2, Open forests/woodlands; Cluster U3, Tree savannahs/degraded woodlands; Cluster U4, Shrubs. Table 2 Stand characteristics in the three plant communities within protected areas. Characteristics Cluster P1 (10 relevés) Cluster P2 (10 relevés) Cluster P3 (19 relevés) ANOVA (at ˛ = 0.05) Species richness Mean species richness (per plot) Mean height (m) Mean DBH (cm) Mean diameter with saplings (cm) Basal area (m2 ha−1 ) Tree density (trees ha−1 ) Density without saplings (trees ha−1 ) Sapling density (saplings ha−1 ) Shannon index (unitless) Pielou evenness index (unitless) 68 14 ± 4aA 15.5 ± 6.5aA 28.0 ± 16.6aA 26.3 ± 16.9aA 46.26 ± 31.77aA 604 ± 301aAB 560 ± 280aA 50 ± 72aA 4.38 ± 0.10 0.78 70 16 ± 3aA 10.6 ± 5.4bB 24.0 ± 14.7bB 20.8 ± 14.9aB 32.55 ± 18.97abA 712 ± 533aA 553 ± 297aA 163 ± 282aA 4.61 ± 0.09 0.79 70 15 ± 4aA 9.5 ± 4.1cC 20.5 ± 10.1cC 18.7 ± 10.6cC 15.09 ± 7.99bB 407 ± 201aB 356 ± 156aB 51 ± 97aA 5.02 ± 0.08 0.86 na p = 0.245 ns p = 0.000 ss p = 0.000 ss p = 0.000 ss p = 0.001 ss p = 0.065 ns p = 0.036 ss p = 0.176 ns na na Note: Outputs of one-way ANOVA: na, not available; ns, not statistically significant; ss, statistically significant. Values that do not share a letter are significantly different at 95% CI using ANOVA with post hoc test (p < 0.05). Capitalized letters are the outputs from Tukey comparison test whereas small letters are the results of Fisher comparison method. Group P1, Mosaic of riparian and dry forests; Cluster P2, Open forests/woodlands; Cluster P3, Tree savannahs/shrubs. 7.7 ± 3.3 m2 ha−1 , respectively. Meanwhile, U3 is the species-richer group (66 woody species), exhibiting then high values of diversity features (5.07 and 0.84, for H and E, respectively) close to the values obtained for U1. The high values of H and E are indicators of stability and homogeneity in studied landscapes. U4 which is the record of low values was dominated by saplings which density is the highest (537 ± 444 saplings ha−1 ). In this group U4, species richness is about 49 species with mean diameter and height of 19.4 ± 11.2 cm and 5.0 ± 3.5 m, respectively. Saplings had a strong effect on mean diameters in all clusters resulting in mean basal areas that decreased from U1 to U4. In the other hand, plant communities in PA are characterized by relative high values of the stand and diversity features compared to those in free-access lands. An exception was observed for sapling density and diversity indices H and E. Apart from the average species richness per plot and the sapling density, all other features varied significantly according to plant communities. Mean DBH was about 28.0 ± 16.6 cm, 24.0 ± 14.7 cm, and 20.5 ± 10.1 cm in P1, P2 and P3, respectively. This trend in tree diameters resulted in similar trend in the basal areas with highest value in P1 (46.3 ± 31.8 m2 ha−1 ) and lowest in P3 (15.1 ± 8.0 m2 ha−1 ). Though the basal area and the tree density were the lowest in P3, this plant community exhibited high diversity of species (5.02 and 0.86 for H and E, respectively). With a density of 712 ± 533 trees ha−1 , P2 is the most dense plant communities compared to P1 (604 ± 301 trees ha−1 ) and P3 (407 ± 201 trees ha−1 ). Basal areas in these protected areas are more shaped by the large contribution of mature individuals than saplings which exhibited low densities, especially in P1 (50 saplings ha−1 ) and P3 (51 saplings ha−1 ). A broad analysis showed that most stand features and diversity differed significantly between PA and UPA. PA showed higher Table 3 Stand characteristics according to land protection status. Characteristics Protected landscapes (39 relevés) Free-access landscapes (36 relevés) ANOVA (at ˛ = 0.05) Species richness Mean species richness (per plot) Mean height (m) Mean DBH (cm) Mean diameter with saplings (cm) Basal area (m2 ha−1 ) Tree density (trees ha−1 ) Density without saplings (trees ha−1 ) Sapling density (saplings ha−1 ) 121 15 ± 4aA 11.2 ± 5.6aA 23.2 ± 13.5aA 21.0 ± 13.8aA 27.56 ± 23.04aA 536 ± 354bB 459 ± 247aA 79 ± 164aA 100 18 ± 5bB 6.4 ± 4.6bB 21.3 ± 12.6bB 12.5 ± 11.1bB 23.67 ± 21.10aA 840 ± 416aA 384 ± 247aA 456 ± 416bB na p = 0.000 ss p = 0.000 ss p = 0.001 ss p = 0.000 ss p = 0.450 ns p = 0.001 ss p = 0.192 ns p = 0.000 ss Note: Outputs of one-way ANOVA: na, not available; ns, not statistically significant; ss, statistically significant. Values that do not share a letter are significantly different at 95% CI using ANOVA with post hoc test (p < 0.05). Capitalized letters are the outputs from Tukey comparison test whereas small letters are the results of Fisher comparison method. B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 139 Table 4 Woody species-based similarity between discriminated vegetation stands. Groups of vegetation stands P1 P2 P3 U1 U2 U3 P2 P3 U1 U2 U3 U4 0.366 0.289 0.326 0.202 0.186 0.206 0.458 0.438 0.441 0.447 0.368 0.333 0.407 0.432 0.384 0.473 0.333 0.372 0.539 0.493 0.456 values of stand features, except tree density and sapling density. Only basal area and tree density without saplings did not display statistical significant differences between the two supra-groups. There were 122 woody species counted in PA while 100 were recorded in free-access landscapes. Mean sapling density is very low in PA (79 ± 164) compared to those in UPA (456 ± 416). This is probably due to low potential of vegetative multiplication through natural process (suckering and seedlings) in PA. On average, trees in PA are taller (11.2 ± 5.6 m) and bigger (23.2 ± 13.5 cm) than those in free-access lands (6.4 ± 4.6 m and 21.3 ± 12.6 cm, respectively for mean height and diameter). Based on stand characteristics, no significant similarity existed between the seven groups, except between U2 and U3 (Sij = 0.539) (Table 4 and Fig. 6). Closest groups in similarity were P2–P3 (Sij= 0.458), U1–U2 (Sij = 0.473), U2–U4 (Sij = 0.493), and U3–U4 (Sij = 0.456). However, the obtained similarity values indicated substantial common characteristics among groups (Sij ≥ 0.333 for most of them). 3.4. Ecology and human disturbances within plant communities The analyses of ecological features and human impacts in the different plant communities (Table 5) indicated differences related to in situ conditions. In general, soils of the seven plant communities are acidic (pH <7) with relative high chemical properties in topsoil (0–10 cm). Though pH and SOC in the lower 20 cm did not vary significantly among groups (p > 0.05), other ecological variables characterized the plant communities. Based on ecology and human footprints, similarity dendrogramme (Fig. 7) indicates four clusters of plant communities: (1) U1 and P1 are sites of riparian/dry forests developed on nutrient-rich soils (high contents of SOC and TN) located on riverbanks and inland valleys where floods often occurred (soil submersion higher than 30%). For both U1 and P1, there is negligible traces of grazing with low tree logging rate. On average, U1 is closer to the riverbed than P1 (mean altitude above the channel level of 7.2 m versus 11.2 m, respectively) resulting in high density of canopy in U1 (coefficient of 3.00 versus 2.10). (2) Relevés of U2 are particular stands as despite the high human disturbances, they exhibited nutrient-rich soils with less moisture content (33.2 m above channel). (3) U3 and P2 develop on soils with medium nutrient contents associated with high rate of illegal tree logging (0.70 in P2) and fire occurrence (0.70 and 0.91 in P2 and U3, respectively). This group is the timber-rich stands, explaining the high rate of tree logging, even in protected areas. However, cattle herders do not make incursions in P2. Their soils have low potential of submersion related to their relatively high locations above channel levels (24.4 m for U3 and 25.1 m for P2). (4) U4 and P3 are relevés with less nutrient contents experiencing moderate human disturbances, especially in U4. On average, they occur at the same altitude above the channel (19 m). Soils are less submersible with low canopy density favourable to grazing (coefficients of 0.70 and 0.79) but not to tree logging. The number of plant communities in UPA is due to the vegetation is less disturbed and allow an easy demarcation of the three vegetation types. Meanwhile, in UPA, human effects changed the physiognomy of some stands increasing the patterns defining vegetation types. In sum, though each relevés or each plant community denotes its intrinsic ecological and biophysical features, some levels of similarity are observable related to certain undeniable common points (topography and protection status). Further, broad analyses of soil conditions in protected areas versus free-access landscapes showed significant differences for TN and SOC at both depths, and cattle grazing. Plant communities under land protection status exhibited high chemical values and low coefficients of human disturbances. Though there were no statistical differences, fire occurrence has a coefficient of 0.78 in free-access landscapes versus 0.62 in protected areas. Coefficients of grazing was quite high Fig. 6. Dendrogramme of similarity between the seven plant communities based on stand characteristics. Fig. 7. Dendrogramme of similarity between the seven plant communities based on ecology of and human disturbances. Mean altitude above channel level (Alt .a.c.l) (in m) Site level 7.17 33.15 24.36 19.52 11.24 25.07 19.36 0.543 ns 20.90 18.74 0.733 ns Site level 0.00 0.14 0.36 0.60 0.00 0.00 0.16 0.001 ss 0.31 0.08 0.011 ss B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 Grazing 140 in UPA compared to PA (0.30 versus 0.08). The same comparison was observed for tree logging coefficients (0.42 in UPA versus 0.26 in PA). These human footprint coefficients in PA indicate the weakness of protection laws, especially at the edges of protected lands. 4. Discussion 0.13 0.57 0.64 0.30 0.10 0.70 0.11 0.001 ss 0.42 0.26 0.145 ns 3.00 1.86 1.45 1.30 2.10 2.40 2.00 0.004 ss 1.83 2.13 0.207 ns 6.19 ± 0.58abA 6.03 ± 0.13abAB 6.16 ± 0.57abA 6.03 ± 0.45abAB 5.70 ± 0.28bB 6.29 ± 0.50aA 6.01 ± 0.34abAB 0.086 ns 6.10 ± 0.47 6.00 ± 0.42 0.325 ns 6.41 ± 0.39abA 6.31 ± 0.26abAB 6.23 ± 0.23abAB 6.48 ± 0.49aA 5.95 ± 0.45bB 6.35 ± 0.17abA 6.36 ± 0.37abA 0.047 ss 6.35 ± 0.37 6.25 ± 0.39 0.247 ns 36 39 Note: Outputs of one-way ANOVA: na, not computed; ns, not statistically different; ss, statistically significant difference at the indicated ˛ value. 0.75aA 0.14abB 0.09bB 0.10bB 0.30abB 0.20abB 0.37abB 0.024 ss 0.25 0.31 0.584 ns 2.31 ± 0.77aA 2.05 ± 0.53aAB 1.93 ± 0.57aAB 2.11 ± 0.99aAB 1.72 ± 0.43aB 1.84 ± 0.46aAB 1.72 ± 0.39aB 0.242 ns 2.09 ± 0.73 1.75 ± 0.42 0.015 ss 2.44 ± 1.29abBC 3.09 ± 0.96abAB 2.21 ± 0.69bC 2.40 ± 0.71abBC 3.63 ± 1.46aA 3.01 ± 0.68bAB 2.55 ± 0.56abBC 0.010 ss 2.48 ± 0.92 2.94 ± 0.98 0.041 ss 0.071 ± 0.04abBC 0.074 ± 0.01abBC 0.057 ± 0.02bBC 0.052 ± 0.02bC 0.101 ± 0.04aA 0.077 ± 0.04abAB 0.062 ± 0.02bBC 0.002 ss 0.062 ± 0.02 0.076 ± 0.03 0.038 ss 8 7 11 10 10 10 19 U1 U2 U3 U4 P1 P2 P3 Anova at p = 0.05 Overall U Overall P Anova at p = 0.05 0–10 cm 0.133 ± 0.08bB 0.119 ± 0.02bBC 0.081 ± 0.03bC 0.077 ± 0.04bC 0.215 ± 0.09aA 0.129 ± 0.05bB 0.104 ± 0.04bBC 0.000 ss 0.099 ± 0.05 0.139 ± 0.07 0.009 ss 10–30 cm 0–10 cm 10–30 cm Site level 10–30 cm 0.50abBC 1.00aA 0.91aA 0.70abAB 0.20bC 0.70abAB 0.79aAB 0.002 ss 0.78 0.62 0.131 ns Mean ± standard deviation Site level Mean ± standard deviation 0–10 cm Soil organic carbon (SOC in %) Total nitrogen (TN in %) Potential of hydrogen (pH) Nb plots Plant communities Table 5 Soil conditions and human disturbance rates in the seven plant communities of both free-access lands and protected areas. Soil submersion Fire occurrence Canopy cover Site level Tree logging Site level 4.1. Vegetation patterns, structure and dynamics At landscape level, Mo basin composes of wide types of natural and human-influenced ecosystems. Indeed, apart from productive managed landscapes (farms, fallows, and pastures), dry forests, gallery forests, woodlands, tree/shrub savannahs are the common cover types, defined according to soil conditions in relation to topography as well as species composition. These biophysical variables determine the physiognomy of the vegetation types which stand characteristics and soil conditions significantly differed (Dourma, 2008; Wala et al., 2012). Along the topographical gradient denoting soil moisture conditions, canopy cover is denser in lowlands (inland valleys, hill foots and river banks) than midhills and hill summits, indicating that the wetness index plays an important role in species composition and vegetation growth (Aynekulu, 2011). Though the stand charactersitics do not really help in defining the vegetation types, it was evident that larger trees barely occurred in top-hills dominated by tree savannah and shrubs, as a consequence of the coarser and rocky soil conditions which do not favour soil moisture for plant growth. These consequently resulted in the stand basal area values which showed a decreasing trend from lowlands to upper lands (top-hills dominated by shrubs/tree savannahs). Along the protection status gradient, mean basal area (27.6 m2 ha−1 ) is higher than that of the unprotected areas (23.7 m2 ha−1 ) but included in the range of values recorded by studies in other similar landscapes made up of subtropical dry forests and woodlands (23.8–78.8 m2 ha−1 ) (Dourma et al., 2009; Folega et al., 2012; Wala et al., 2012). These results are the evidence of an over-exploitation of the landscape resources, especially of tree species. A broad analysis showed that most stand features and diversity differed significantly between PA and UPA. PA showed higher values of stand features, except sapling density, which is in contrast with the findings of Dourma et al. (2009) who found high stand characteristics in protected dry forests compared to UPA. PA showed a higher woody species-diversity with very low sapling density probably due to low potential of vegetative multiplication through natural process (suckering and seedlings). In general, the poor representation of saplings could be due to the rocky nature of the soils that do not favour quick germination of seeds, and to landscape roughness inducing seeds transportation downward in lowland and their carrying away by water. This could explain the high density of saplings in unprotected areas, which lie, mostly on less rough landscapes. On the other hand, the prevalence of tall and big trees in protected lands compared to UPA suggested the effects of intensive and selective tree logging, charcoal production and mortar making on vegetation structure. These mentioned human impacts often target specifically high and big trees, inducing the loss of trees of big size (Appiah et al., 2009; Dourma et al., 2009; Appiah, 2013). Subsequently, human pressures convert tree-rich stands into tree-less and induce svananisation process. The protected lands showed a more stable landscape with the bell-shaped distribution of tree densities. This can be resulted from the fact that trees of these sizes are subject to tree logging for wood and charcoal production. In non-protected areas, the high rate of human threats stimulate multiplication of trees through clonal propagation, suckers and seedlings (Pare et al., 2009a). These stressing B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 factors induce an increase in stem density in unprotected areas compared to protected lands undergoing less threat, especially tree cutting. This study assumed that disturbances in unprotected areas induced local vanishing of plant species due to their replacement by direct economic plant species such as Tectona grandis, Eucalptus spp., Anacardium occidentale, Eleais guinensis, etc. However, several studies (Zhai et al., 2013; Zhai et al., 2015) found that disturbed natural forests are more vulnerable to invasion by exotic plant species compared to undisturbed forests, which tend to exhibit more homogeneous and monospecific stands, and therefore less species diversity. Pare et al. (2009b) reported in Burkina Faso that unprotected forests were most diverse compared to protected areas, due to the low population density in unprotected lands. 4.2. Relationships between vegetation types and environment Ecology and biophysical factors usually define vegetation types which often contribute to the maintenance of these factors, especially edapho-ecological variables. As shown by previous studies, the distribution of plant community or vegetation types is defined along environmental gradients such as topography, soil conditions, microclimate, and human disturbances. In this study, whatever the protection status, vegetation types were mostly defined according to topographical gradient inducing different soil conditions (moisture and nutrient contents). As reported by several authors, topography is a factor that defines vegetation patterns, especially in mountainous landscapes. Riparian and dry forests and woodlands occurred on moist soils with finer particles and high nutrient contents. These findings aligned with those former authors (Woegan, 2007; Dourma, 2008; Wala et al., 2012) who worked in the same zones. Regarding soil nutrients and particles, the flow gradient from top-hills to hill-foots and inland valleys induces a typical gradient of soil conditions. From top to bottom, the soils are finer and nutrient-richer downwards (Ofori et al., 2013). Naturally, each land cover occurs on particular soil physico-chemical properties which highly vary spatially, even within the same LUC type (Wiesmeier et al., 2014). Accordingly, landscape positions and elevation induced the spatial variability of soil conditions (Solon et al., 2007; Jabeen and Ahmad, 2009; Zhang and Zhang, 2010). On the second hand, the general trend of soil chemicals is sharply shaped by the landscape positions and the hydrological processes occurring at the various sites. Based on previous findings in similar landscapes of the same study area, topography in relation with soil conditions is the most determinant factor of vegetation physiognomy and patterns in Mo basin. Topography and somehow elevation have significant effects on the vegetation patterns through their determinant effects on soil conditions (Aynekulu, 2011). Soils in lowlands and hill-foots do have deeper profiles with high moisture and nutrient content favourable the growth of plant species. In contrast, on hill summits and hillsides with steep slopes, the soil conditions are drier, rockier, and less deep. These ecological indicators explain the occurrence of forests along riversides and lowland soils, even in savannah-dominated landscapes. Besides, environmental factors, anthropogenic disturbances affect species diversity, size classes and land cover types through habitat loss and fragmentation. Studies evidenced that human disturbances usually have substantial effects on ecosystem functioning, and therefore their structure, physiognomy and species composition (Paré, 2006; Dourma et al., 2009; Folega et al., 2010a; Ouedraogo, 2010; Appiah, 2013). Human footprints caused by grazing, tree logging, wildfire, and cropping have been reported as negative drivers changing habitat fragmentation with less tree species diversity and loss of landscape functions and aesthetics, even in protected areas (Appiah, 2013; Tchabsala and Mbolo, 2013). 141 Fires in forest and wild lands are cited as a threat that affect forest structure and biodiversity (Bowman and Murphy, 2010), and contribute significantly to atmospheric CO2 and nitrogen emissions as well (Slik et al., 2008; Kugbe, 2012). The induced land degradation also has subsequent effects on soil conditions, especially nutrient flow, carbon and nitrogen cycles (Traoré et al., 2015). 4.3. Land management, human disturbances and implications for sustainable management Along land protection status, three and four vegetation types were identified in PA and UPA respectively. In both landscapes, topography and soil conditions were the most prominent variables defining the landscape patterns. This indicates that topographical conditions (i.e. elevation, slope, Alt a.c.l, and soil submersion) in combination with human disturbances (i.e. fire, logging, grazing) determine species composition and vegetation structure and dynamics. It often appears that landscape fragmentation and deforestation largely occur in accessible areas such as lowlands. In these easy accessible areas, the transformation of wild landscapes (forests and woodlands) into other land-use types (farms and pastures, plantations) is a result of people livelihood support (Appiah et al., 2009; Pare et al., 2010). It is suggested that land conservation measures should target these vulnerable areas of the landscapes in order to ensure effectiveness and efficiency of implementation. As the PA showed somehow their weakness in land resource conservation due to inefficiency of management regime and law enforcement (Folega et al., 2010a; Damnyag et al., 2013; Folega et al., 2014b), it is important to investigate on alternatives for better management (Pare et al., 2009a; Pare et al., 2009b; Wala et al., 2012; Appiah, 2013; Damnyag et al., 2013). Besides, wild unprotected lands, especially in rural areas with low population density, could be of great importance in biological conservation, even if an explicit role of conservation is not devoted to them. The lack of properties/rights over lands, the weakness of policy/laws regarding resource conservation, and the inefficiency in PA managements are among the sources of unsustainable land management (Wala et al., 2012; Folega et al., 2014b). In this regard, land management in the basin should evolve adapted strategies that define clearly property rights, reinforce laws and policies, and involve all stakeholders. These strategies involving all stackholders compel to a rethinking of collective management of common resource pools, especially forests and lands, to avoid “tragedy of commons”. The main issues in the innovative forms of adapted land use and planning in multifunctional landscapes are the participatory resource allocation and incentives for perennial ecosystem conservation. Governance and management systems combined with socioeconomic conditions of people being of the underlying factors in decision-making regarding land use (Ellis and Porter-Bolland, 2008; Kaye-Zwiebel and King, 2014; Specht et al., 2015), law enforcement for protected areas without any implication of local stakeholders will guarantee failure in sustainable conservation strategies. The role of landscapes and other social-ecological systems in ensuring people livelihood while mitigating climate change is still a crucial issue to be solved. In such conditions, agroforestry appears to be of great potential for sustainable development and climate mitigation (Mbow et al., 2014), especially using native tree species of local economic importance such as V. paradoxa and Isoberlinia spp. (Dourma et al., 2009). The quasi-stability of human-affected landscapes and ecosystems is an indicator that lands outside PA can gain more attention to ensure adapted land use/conservation in production landscapes (Ellis and PorterBolland, 2008; Ellis, 2013; Gu and Subramanian, 2014). 142 B. Diwediga et al. / Ecological Engineering 85 (2015) 132–143 5. Conclusions Diversity and status of plant species as biodiversity-related indicator of landscape stability is studied in Mo landscapes. This helped in the identification of the linkage between social-ecological systems, and the configuration of landscape patterns under different land protection status. In total, 142 woody species were identified within four plant communities in unprotected areas (UPA) and three vegetation types in protected areas (PA). The analyses of ecological features and human impacts in the different plant communities indicated differences related to in situ conditions and land protection status. In general, the soils of the seven plant communities are acidic (pH <7) with high contents of chemical properties in topsoil (0–10 cm). Land management/protection status is an important factor impacting and shaping the vegetation physiognomy in Mo basin. Accordingly, the common environmental threats were the high level of wood extraction (firewood, charcoal production and tree logging), bush fires, and cattle grazing. Though the natural biophysical factors shape landscape physiognomy, human disturbances affect the structure and composition of plant communities through the provided multiple and valuable ecosystem services to local people. As a limitation of the study, the sampling approach could have drawn an equal number of plots in PA and UPA in order to draw conclusions based on more comparable results. However, the study showed that biological conservation should not only target landscapes in protected areas but also on some wild landscapes located in inaccessible and low populated areas. This could promote both biological conservation and livelihood support to riparian population. In connivance with local resource users, their capacity for effective management of common resource pools should be strengthened by increasing people awareness of the land degradation phenomenon. Acknowledgements The authors are grateful to the German Federal Ministry of Education and Research (BMBF), which supported this research through WASCAL research programme. Special thanks to WASCAL Graduate Research Programme in Climate Change and Land Use (Kwame Nkrumah University of Science and Technology – KNUST, Ghana). We also thank the Ministry of Environment and Forest Resources of Togo, and the Central Region office of Environment in Togo. We gratefully acknowledge the technical support from the Foundation Franz Weber of Fazao-Malfakassa National Park during our field-works. The CGIAR Research Program in Dryland Systems (CRP-DS), Overarching Cluster of Integrated Systems Analysis and Modelling (budget code 910101) funded for Quang Bao Le’s contribution. Thanks to the anonymous reviewers for their valuable comments to the quality of the work. Appendix A. Supplementary data Supplementary data associated with this article can be found, in the online version, at http://dx.doi.org/10.1016/j.ecoleng.2015.09. 059. References Aboudou, M., 2012. Etat des lieux de l’occupation du sol dans et autour du parc national Fazao-Malfakassa. MERF-Togo/Fondation Franz Weber, 19 pp. Agboadoh, M.Y.D., 2011. Estimation and Mapping of Soil Organic Carbon in Croplands of the Bechem Forest District, Ghana. 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