Abstract
Abandoned tailing dumps (ATDs) offer an opportunity to identify the main physicochemical filters that determine colonization of vegetation in solid mine wastes. The current study determined the soil physicochemical factors that explain the compositional variation of pioneer vegetal species on ATDs from surrounding areas in semiarid Mediterranean-climate type ecosystems of north-central Chile (Coquimbo Region). Geobotanical surveys—including physicochemical parameters of substrates (0–20 cm depth), plant richness, and coverage of plant species—were performed on 73 ATDs and surrounding areas. A total of 112 plant species were identified from which endemic/native species (67%) were more abundant than exotic species (33%) on ATDs. The distribution of sampling sites and plant species in canonical correspondence analysis (CCA) ordination diagrams indicated a gradual and progressive variation in species composition and abundance from surrounding areas to ATDs because of variations in total Cu concentration (1.3%) and the percentage of soil particles <2 μm (1.8%). According to the CCA, there were 10 plant species with greater abundance on sites with high total Cu concentrations and fine-textured substrates, which could be useful for developing plant-based stabilization programs of ATDs in semiarid Mediterranean-climate type ecosystems of north-central Chile.
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Introduction
Mineral residues from metal mine operations, such as mine tailings, are discharged into the environment, becoming a source of hazardous metals that are transported to soils and surface waters, affecting the surrounding ecosystem (Johnson et al. 2016; Yu et al. 2016). Mine tailings are disposed of in artificial dumps. Once they enter the post-operational phase, surface tailings dry out at a speed that is dependent on the climatic conditions of the site, leaving a fine and non-cohesive material that is exposed to wind and water erosion and dispersion (Dold and Fontboté 2001). The erosion of abandoned tailing dumps (ATDs) is accentuated in arid and semiarid environments because of the high rate of water evaporation, which rapidly dries out surface tailings, resulting in the risk of metal pollution in surrounding areas (Conesa et al. 2007; Mendez and Maier 2008).
A range of physical, chemical, and biological remediation techniques are available for ATDs for different mining systems (Li 2006). Among them, well-developed revegetation (i.e., assisted or natural phytostabilization) can assure long-term and self-sustainable remediation (Tordoff et al. 2000; Mendez and Maier 2008). Once plants have successfully established on ATDs, they can readily accumulate organic matter, aid nutrient cycling (Ottenhof et al. 2007), improve the physical properties of the soil, and add nutrients to the mineral substrate (Verdugo et al. 2011). Spontaneous vegetation cover developed on metal-enriched substrates and ATDs offers a valuable ecological opportunity to look for plants capable of growing in such stressful environments, which could reduce both the erosive processes and the risks of environmental metal pollution (Salt et al. 1995). For example, diverse plant species that spontaneously colonize metal-enriched substrates have been identified, studied, and tested in different metalliferous habitats worldwide for plant-based remediation purposes (Whiting et al. 2004; Baker et al. 2010; Solís-Domínguez et al. 2012; Cuevas et al. 2013; Tapia et al. 2013). In particular, spontaneous pioneer plant species represent key stress-tolerant genetic resources that can be used in the remediation of ATDs in semiarid environments (Salt et al. 1995; Ginocchio and Baker 2004).
Abandoned tailing dumps are similar to strongly natural disturbed sites, such as lava fields, rockslides, and landslides, where spontaneous primary successional processes begin following disturbance (Pickett and White 1985). Particularly, primary succession occurs on mineral substrates that lack in situ plant propagules (Tilman 1988) and correspond to long-term vegetation changes and the transformation of mineral substrates into soil (Pickett and White 1985; Tilman 1988). After primary spontaneous plant colonization and establishment, pioneer plants modify the microenvironment so as to reduce the frequency and/or intensity of some physical disturbances or stresses, allowing further colonization by less-tolerant species; this creates habitats for other organisms and eventually increases biological diversity with time (Parraga-Aguado et al. 2014). In the case of ATDs, spontaneous colonization is limited, generally with small patches of vegetation distributed mainly on their edges (dump walls) (Conesa et al. 2007; Das and Maiti 2007). Therefore, a large portion of them remained bare and exposed to erosion agents. For example, it was reported that even 18 years after abandonment plant cover only accounts for <3% of the total area (Shu et al. 2005).
The study of the early stages of primary vegetational succession on mineral substrates of ATDs could identify the physicochemical characteristics that determine their spontaneous colonization (Conesa et al. 2006; Horáčková et al. 2016; Żołnierz et al. 2016). ATD substrate is characterized as being toxic and unsuitable for plant growth because of its elevated metal (i.e., Cu, Ni, Pb, Cd, and Zn) concentrations (Ginocchio et al. 2006), low organic matter content (Ottenhof et al. 2007), low soil nutrients availability (Verdugo et al. 2011), restrictive soil cation exchange capacity (CEC), and limited microbiological activity (De La Iglesia et al. 2006). Their poor soil physical properties, such as low porosity and a fine homogeneous texture, reduce water infiltration and root development and promote compaction (Mendez and Maier 2008; Verdugo et al. 2011). Depending on their metal sulfide content and the climatic conditions of the site, secondary acidification of ATD substrate can also occur (Dold and Fontboté 2001), further increasing toxicity (Ginocchio et al. 2009). Therefore, it has been assumed that metal toxicity, extreme acidity, and/or low nutritional availability of the substrate are the main factors restricting plant colonization and establishment in ATDs (Mendez and Maier 2008; Schippers et al. 2000; Li and Huang 2015). Hence, it is generally thought that plants able to colonize and establish on ATDs are metal-tolerant species or metallophytes (Whiting et al. 2004; Baker et al. 2010). However, in water-limited environments, such as semiarid Mediterranean-climate type ecosystems, the establishment of a plant cover on ATDs could be more difficult because of extreme temperatures at the tailing surface and low precipitation throughout the year, resulting in high salt concentrations (up to 18 dS m−1) and high compaction levels (Pérez-Sirvent et al. 2015). Therefore, physical, chemical, nutritional, and/or microbiological limiting conditions of tailings would be other edaphic factors controlling plant colonization on ATDs at early successional stages, in addition to acidity and/or metal toxicity.
Although several studies have reported the occurrence of spontaneous pioneer plant species on metal-enriched soils and ATDs in different semiarid Mediterranean-climate type regions worldwide (Conesa et al. 2006; Mendez and Maier 2008; Cuevas et al. 2013; Tapia et al. 2013), the soil physicochemical factors that restrict spontaneous vegetation early establishment in ATDs are still poorly understood. Therefore, in the current study, we carried out an edaphic and botanical survey of 73 ATDs in a semiarid Mediterranean-climate type area of north-central Chile (Coquimbo Region, latitude 29° 00′ to 32° 10′ S and longitude 70° 00′ to 71° 50′ W) to explore the physicochemical factors of tailings that determine the compositional variation in pioneer plant species growing on ATDs. We used the Coquimbo Region as a case study area, as it holds 67% (Casale et al. 2011) of ATDs registered in north and central areas of Chile (SERNAGEOMIN 2015).
Methods
Study area
Climate of the Coquimbo Region ranges from arid Mediterranean-type in the north (Elqui province) to semiarid Mediterranean-type towards the southern end (Limarí and Choapa provinces). Mean annual temperatures and precipitation vary from 14.8 °C and 127.4 mm in the north to 14.2 °C and 334.3 mm in the south, respectively (Di Castri and Hajek 1976). Plant communities are characterized by high endemism and diversity of xerophytic shrubs, cacti, and a seasonal herbaceous cover. Small and medium-sized Cu and Au mine operations have been common in the area since the nineteenth century, leaving more than 300 ATDs scattered throughout the region (Casale et al. 2011). Cu tailings in the region came from mines that processed porphyry Cu, characterized by a high mineral Cu (chalcopyrite) content, using alkaline foam flotation processes (Dold and Fontboté 2001).
Seventy-three ATDs throughout the Coquimbo Region were selected for the present study (Table 1), according to the following criteria: (1) minimal disturbance after abandonment; (2) no or low introduction of exotic plants (revegetation or forestation); (3) no incorporation of foreign substrates or soil amendments; and (4) year of abandonment ideally documented.
Geobotanical surveys
Geobotanical surveys were performed in selected ATDs (Table 1) and their surrounding areas according to Baker and Brooks (1989); each ATD was only visited for 1 week (spring for good representation of flora and vegetation) and all surveys were done from March 2005 to December 2007. At each ATD, composite samples were made of five subsamples of surface tailings (0–20 cm depth) collected both from dam walls and the consolidated tailings (Fig. 1). Composite soil samples (eight subsamples at 0–20 cm depth) were also collected up to 80–100 m away from each ATD. All substrate samples were transported to the laboratory to be physicochemically characterized, as described below.
Spontaneous vegetation established on ATDs and surrounding areas was characterized in terms of plant richness (number of plant species) and coverage (projection of aerial biomass of plants onto the ground, expressed as a fraction of the total area), according to methods described by Mueller-Dombois and Ellenberg (1974). All vascular plants were registered, herborized, and taxonomically identified; total plant coverage was estimated from five 30-m-long linear transects evenly and radially distributed along ATDs and selected sites in surrounding areas. Aerial tissue samples (last growth season for perennial plants and whole shoots for herbs and/or grasses) of dominant plant species were collected for at least three randomly selected individual plants. Tissue samples were stored in clean paper bags and transported to the laboratory for further processing, as described below. The Spatz index (Mueller-Dombois and Ellenberg 1974) was calculated from plant species composition and abundance to analyze the floristic similarity of vegetation present on ATDs and surrounding areas. It ranges from null (0%) to complete similitude (100%); this index is more sensitive to changes in plant abundance than other similarity indexes. The Spatz index was calculated using the Ginkgo program version 1.5.0 (Bouxin 2005).
Physicochemical characterization of substrates
Substrate samples were oven dried at 30 °C, sieved to 2 mm, and stored. Fractions less than 2 μm were determined by granulometry using the method of Bouyoucos (USDA 2004). The substrate pH, electrical conductivity (EC), CEC, organic matter (OM), and sulfate content were determined using USDA protocols (USDA 2004). Total concentrations of metals (Cu, Zn, and Fe) and Ca were determined by atomic absorption spectrophotometry, after acid (HNO3/HF/H2O2) digestion and extraction in a microwave oven, using method 3051 of the US EPA (1995); duplicate samples, blank samples, and certified reference material (B-Loam from High-Purity Standard, Charleston, SC, USA) were also analyzed to meet the criteria for quality assurance and quality control.
Determination of metals in aerial tissues
Aerial tissue samples were sequentially washed with tap water and ultrapure water (>18 MΩ cm−1) to eliminate external contamination. Shoots were air dried at 30 °C to a constant weight, pulverized in a grinder with stainless steel blade, and placed in clean polyethylene containers (US EPA 1995). Metals (Cu, Zn, and Fe) were analyzed as described previously. The standard reference material sample used was SRM 1573a tomato leaves (National Institute of Standards and Technology, Gaithersburg, MD, USA).
Statistical analyses
One- and two-way analyses of variance were used to test for differences in physicochemical characteristics and metal concentrations in aerial tissues among substrate types (soils from surroundings, consolidated tailings, dam wall tailings) and/or geographic location (Elqui, Limarí and Choapa provinces). Fisher’s least-significant difference test was used for a posteriori comparison. When required, characteristics were corrected for non-normality using logarithmic transformations (x′ = log10 [x]). Simple linear regressions were used to evaluate statistical relations between the physicochemical characteristics of tailings and floristic similarity of ATDs and surrounding soils with either time since abandonment or surface area. The InfoStat program (Grupo InfoStat, Universidad Nacional de Córdoba, Argentina), version 2010p, was used to perform the statistical analyses. Canonical correspondence analyses (CCAs; Leps and Šmilauer 2003) were conducted to determine whether selected physicochemical characteristics of substrates (soils and tailings) explained the compositional variation of vegetation on ATDs at a regional level. To obtain a CCA ordination model that only included those physicochemical characteristics of substrates that contribute significantly to species composition, a forward selection of explanatory variables was made. The statistical significance of the contribution of physicochemical variables of substrate was assessed using a partial Monte Carlo permutation test with 1000 permutations. In this test, the candidate physicochemical variable of the substrate was used as the only explanatory variable (ordination model with just one canonical axis), considering the other physicochemical variables already selected as co-variables. The statistical significance of the CCA model was evaluated using a permutation test of Monte Carlo based on the sum of all canonical eigenvalues and considering 1000 permutations. To isolate the effect of physicochemical variables of the substrate on species abundance from latitude, partial CCA tests were conducted, considering latitude as a co-variable. CANOCO 4.5 (Microcomputer Power, Ithaca, NY, USA) was used to conduct the CCA.
Results
Physicochemical characteristics of substrates
Physicochemical characteristics of consolidated tailings, dam wall tailings, and surrounding soils by provinces (Elqui, Limarí, and Choapa) are shown in Table 2. A significant difference according to geographic location was only found for OM while significant differences according to substrate type were found for texture, CEC, OM, sulfate, total Cu, and total Fe. The interaction factor among geographic location × substrate type was only significant for OM and textural fractions <2 μm and 50–2000 μm (Table 2). OM significantly increased from north to south of the study area (0.3% Elqui < 0.5% Limarí < 0.6% Choapa), following the arid to semiarid gradient; it was also an order of magnitude higher in soils than in tailings (1.0 ± 0.8% soils and 0.3 ± 0.3% tailings). According to the USDA textural classification chart for soil (Soil Survey Staff 1993), both soils and dam wall tailings were sandy loam, whereas consolidated tailings were silt loam. The CEC was one order of magnitude lower in tailings than in soils, whereas sulfate, total Cu, and total Fe were one order of magnitude higher in tailings than in soils. No significant differences were found for these characteristics among consolidated tailings and dam wall tailings, with the exception of sulfate content, which was 1.8 times higher on consolidated tailings. Even though total Cu and Fe concentrations were higher in tailings than in surrounding soils, there was high variability among ATDs for these characteristics (Table 2).
Flora and vegetation
A total of 195 plant species were identified on both ATDs and surrounding soils, belonging to 50 families. For ATDs, mean plant richness was 7 and a total of 112 spontaneous plant species, belonging to 37 families, were found. Native/endemic species were more abundant than exotics (67 and 33%, respectively) and the main families were Asteraceae (27%) and Poaceae (11%). Most plant species (80%) were only present in less than 10% of ATDs, but 10 plant species were frequently (>20% of ATDs) found on ATDs. A mean plant coverage of 4 ± 6% was found in ATDs, with a range of 0.1–26%; there was a significant and positive (R = 0.82, P < 0.01) relation between coverage of plant species and percentage of occurrence on ATDs (Fig. 2). Dominant species (coverage >10% and percentage of occurrence >20%) on ATDs were Baccharis linearis, Baccharis marginalis, Bromus berterianus, Erodium cicutarium, Muehlenbeckia hastulata, Pleocarphus revolutus, Schinus molle, Schinus polygama, Schismus arabicus, and Tessaria absinthioides. On surrounding areas, the same general trends were found; most species belonged to the Asteraceae (25%) and Poaceae (11%), and native/endemic species were more abundant than exotics (68 versus 32%). However, plant richness and coverage of dominant species were higher than on ATDs. Floristic similarities among ATDs and surrounding areas varied from 0 to 36%, with a mean of 3.3%. Therefore, pioneer plants on ATDs represented a subgroup of the plant species present in surrounding areas. Floristic similarity significantly increased (R = 0.49, P < 0.01) with time of abandonment of ATDs (Fig. 2), but was independent of surface area (R = 0.02, P = 0.863). Plant changes with time were slow and variable; after 31 years of abandonment, the floristic similarities of vegetation on tailings versus the surrounding area ranged from 1.6 to 13.3% (Fig. 2).
Metal concentrations in aerial tissues
Table 3 shows the shoot metal concentrations (Cu, Zn, and Fe) of pioneer plants (percentage of occurrence >5%) growing on both ATDs and surrounding soils. Mean Cu, Zn, and Fe concentrations in aerial tissues broadly varied among plant species, and in general, no significant differences were found among substrates (Table 3). The exceptions were Haplopappus parvifolius and Senecio bridgesii for Cu, H. parvifolius and S. molle for Zn, and B. linearis, B. marginalis, Haplopappus macraeanus, and P. revolutus for Fe, which showed higher metal concentrations when they were on tailings than on soils (Table 3). Mean shoot Cu and Zn concentrations of common spontaneous plant species growing on tailings ranged from 11 mg to 804 mg Cu kg−1 (dry weight basis) and from 17 mg to 191 mg Zn kg−1, respectively (Table 3). However, metal concentrations in aerial tissues of plants growing on tailings and surrounding soils did not differ statistically (Table 3), even though total metal concentrations were higher in tailings than in surrounding soils (Table 2). Only Cu concentrations were significantly and positively correlated to Zn and Fe levels in tissues of plants growing on tailings (R = 0.22 for P = 0.01 and R = 0.64 for P = 0.01, respectively) and on surrounding soils (R = 0.33 for P = 0.01 and R = 0.62 for P = 0.01, respectively).
Relations among physicochemical characteristics of substrates and abundance of plant species
Only 2 (total Cu concentration and the percentage of particles in the substrate that were <2 μm; Fig. 3) out of the 12 physicochemical parameters considered (Table 2) significantly contributed to the CCA ordination model (P ≤ 0.05; partial Monte Carlo permutation test; Table 4). The relation between the variation in floristic composition and the total Cu concentration and the percentage of particles <2 μm was statistically significant (F ratio = 2.010, P = 0.001). The CCA ordination diagram (Fig. 3) shows the distribution of sites (ATDs and surrounding areas) according to the weighted average of species present in each site, in direct relation to the substrate characteristics determined for each site. A 100% of the total variation of the species–substrate relation was explained by the first two axes of the ordination model (Fig. 3) and the total inertia that was constrained corresponded to 3.1%. The percentage of particles <2 μm (canonical r = 0.78) was the variable most correlated with the first canonical ordination axis, whereas total Cu concentration (canonical r = 0.72) was the variable most correlated to the second canonical ordination axis (Table 4), both of which explained the distribution of sites in the study area. The distribution of sites in the CCA ordination diagram (Fig. 3) indicated that there was a gradual and progressive variation in species composition from surrounding areas to ATDs because of variation in total Cu concentrations of substrates and percentage of particles <2 μm. Plant species present at the sites (tailings plus surrounding areas) are displayed in the ordination diagram of Fig. 4. In this diagram, the orthogonal projection of the plant species (stars) on any physicochemical vector indicates approximately the relative value on a weighted average for each species regarding the vector. Thus, the plant species Haplopappus bezanillanus, Baccharis paniculata, Sphacele salviae, Atriplex numularia, Rapistrum rugosum, Bromus catharticus, Gymnophyton robustum, and Senecio adenotrichius had the highest weighted averages in terms of the total Cu concentration and the percentage of particles <2 μm, suggesting that their greater coverage (%) occurred in sites with the highest total Cu concentration and finer substrates. Latitudinal variation of the study area was large; therefore, a partial CCA was conducted considering latitude as a co-variable, for determining the contribution to the model of every physicochemical parameter that could not be explained by latitude (Table 5). Total Cu concentration in the substrate explained 1.3% of the total variation in plant species abundance, whereas the percentage of particles <2 μm explained 1.8% of the total variance. When latitude was considered as a co-variable in the CCA ordination model, constrained inertia was only reduced by 1.8% and the significance of the model remained (F-ratio = 1.995; P = 0.001). This suggested that the effect of both physicochemical parameters selected on plant species composition was independent of latitude (Table 1).
Discussion
Acidity, metal toxicity, and/or low nutritional availability (Mendez and Maier 2008; Schippers et al. 2000; Li and Huang 2015) have been generally considered the main factors restricting spontaneous plant colonization and establishment on ATDs. However, our study demonstrate that from 12 physicochemical characteristics considered (Table 2), content of fine particles (percentage of particles <2 μm) and total Cu content of tailings are the main factors restricting spontaneous colonization of ATDs in semiarid Mediterranean-climate type ecosystems in north-central Chile. Under both conditions, high percentage of fine particles and total Cu concentration found in tailings (particularly on consolidated tailings), only a subset of plant species (H. bezanillanus, B. paniculata, S. salviae, A. nummularia, R. rugosum, B. catharticus, G. robustum, and S. adenotrichius) was able to establish and growth, as shown by the CCA ordination model obtained in the present study (Fig. 4). On one hand, elevated content of fine particles in ATDs results in substrate compaction (high bulk density) with time (Lottermoser 2007), which may restrict root growth and therefore plant establishment as it has been shown for soils (Chen et al. 2014). On the other hand, total Cu content strongly varied among ATDs (range of 100 to 18,127 mg kg−1) and with surrounding soils (mean values of 3252 and 905 mg kg−1, respectively), as expected from literature (Lottermoser 2007). However, Cu toxicity to plants in tailings is only expected under high bioavailability of this element. Previous studies of our research group have demonstrated that Cu bioavailability in alkaline tailings is low as metals occurs in mineral form which are rather insoluble (Badilla-Ohlbaum et al. 2001; Ginocchio et al. 2006; Ginocchio et al. 2009; Verdugo et al. 2011). Weathering of tailings occurs when exposed to external environmental conditions (e.g., rain, presence of iron- and sulfur-oxidizing bacteria), leading to substrate acidification and dissolution of metals from primary minerals (Dold and Fontboté 2001; Lottermoser 2007). However, secondary acidification of tailings was a rare phenomenon in studied ATDs (Table 2), particularly due to semiarid climatic conditions of the area and elevated calcium contents of tailings (Table 2). Under semiarid climatic conditions, high evapotranspiration rates contribute to the development of calcium carbonate (gypsum) and metal carbonate forms at tailings surface (Lottermoser 2007), thus reducing metal solubility (Dold and Fontboté 2001). Therefore, further studies on Cu bioavailability and thus phytotoxicity have to be performed in selected tailings, as Cu speciation studies were not included in the present study.
A number (112) of spontaneous plant colonizers were found in selected ATDs of north-central Chile, 10 of them being dominant (coverage >10% and percentage of occurrence on ATDs >20%). None of them was exclusively established on ATDs, unlike metalliferous habitats where strongly distinctive plant communities resulting from deterministic species selection by environmental filters have been described (Conesa et al. 2007; Parraga-Aguado et al. 2013). It is interesting to note that some dominant pioneer species (e.g., B. linearis) found on selected ATDs has been already described as pioneer and nurse plant species in highly disturbed sites of north-central Chile (Bustamante 1991), including abandoned mine tailings (Cuevas et al. 2013). Native/endemic plants were more successful (67%) than exotics (Table 5) as pioneer species. This response could be explained by the adaptation of native/endemic plant species to local site conditions (e.g., drought, high radiation, nutrient availability, soil depth) and conditions of semiarid Mediterranean-climate type environments. For example, low-nutrient soils are commonly found in semiarid Mediterranean-climate type areas, whereas exotic weedy species have higher nitrogen requirements (Dallman 1998). Low colonization success by exotic weedy species has been also described on primary successions on disused gravel-sand pits (Rehounková and Prach 2010; Šebelíková et al. 2016). In agreement with our results, Asteraceae and/or Poaceae have been described as the most represented families on ATDs in other places like southern China (Shu et al. 2005), southern Spain (Conesa et al. 2007), and India (Das and Maiti 2007). Initial plant colonization success is related to seed traits that determine the dispersal ability of the species, such as anemochory and wind dispersal, common in Asteraceae ( Table 5) and the production of light diasporas (small seeds, common in Poaceae), which are generally advantageous for long-distance dispersal (Rehounková and Prach 2010).
Species richness increased with time since abandonment in studied ATDs of north-central Chile. However, plant changes with time were slow and variable among ATDs of similar abandonment time, leading to a maximum coverage of 26% after 31 years after abandonment. Changes in ATDs have been described as being very slow and very limited in terms of species richness and plant colonization (Shooner et al. 2015). For example, after 18 years, ATDs might still have limited plant colonization, with total plant covers being <3% (Shu et al. 2005). It is interesting to note that an increment of species richness with time was independent of the surface area of ATDs (Fig. 2). It has been reported that the succession process can depend more on the physicochemical parameters of tailings than on their surface area, at least during the early revegetation stages (Shu et al. 2005). In the present study, percentage of fine particles (<2 μm) and total Cu concentration in the substrate were found to be the main physicochemical parameters that explained the changes in spatial variation of plant species across ATDs and surrounding soils (31% of variation was explained by these factors). However, a large percentage of variation (69%) of the plant species–substrate relation remained unexplained, indicating the need to explore other environmental (e.g., microtopography of tailings, precipitation, wind speed) and microenvironment (substrate aggregation, presence of heterotrophic microbial communities) parameters in future studies, as it has been stated in the literature (Mendez and Maier 2008; Moreno-de las Heras 2009). For example, spontaneous plant colonization of ATDs has been described to be limited and unevenly distributed, being generally restricted to small patches in dam walls and on the edges of platforms on consolidated tailings (Conesa et al. 2007; Das and Maiti 2007; Moreno-de las Heras et al. 2008). Spontaneous plant colonization is also found in favorable microsites of consolidated tailings, such as cracks and manure deposits or sites below nurse pioneer shrubs with relatively higher OM and nutrient contents, and better water retention and infiltration (Shu et al. 2005; Cuevas et al. 2013). For ATDs in north-central Chile, this pattern could be explained in part by changes in the physicochemical parameters across dam wall tailings and consolidated tailings. Indeed, consolidated tailings appear to be harsher substrates than dam wall tailings for plant establishment and growth, because the percentage of particles <2 μm, sulfate concentration, and EC values were higher for the former. Mean EC values for consolidate tailings (provincial level) were all above 4 dS m−1, rendering them saline substrates. Elevated sulfate concentrations in consolidated tailings (and, consequently, high EC values) could be explained by the occurrence of secondary metal sulfide oxidation (i.e., pyrite and FeS2), with the formation of sulfuric acid and reduction in pH (acid mine drainage) (Dold 2017). In arid and semiarid climates, where evaporation exceeds precipitation, the secondary sulfide oxidation phenomenon is restricted to upper tailings (oxidation zone); therefore, because the migration of water is upwards via capillary forces, super saturation controls the precipitation of mainly water-soluble secondary sulfates and strong salt enrichment at the top of consolidated tailings (Dold and Fontboté 2001).
Shoot metal concentrations of pioneer plants on ATDs have been frequently described as elevated (Shu et al. 2005; Conesa et al. 2007; Das and Maiti 2007). However, this was not a general finding in the current study; with few exceptions (H. parvifolius, H. macraeanus, S. bridgesii, S. molle, B. linearis, B. marginalis, and P. revolutus) (Table 6), the shoot metal concentrations of pioneer species were similar to concentrations found for the same species in surrounding soils. This finding could be interpreted as a shoot metal exclusion strategy (Baker et al. 2010), a positive characteristic expected for the phytostabilization of ATDs (Solís-Domínguez et al. 2012); however, we did not determine root metal concentrations. This finding might also result from shoot exposure to air-borne tailing particulates. Plant tissues were thoroughly washed before metal determination, but the possibility exists that persistent external contaminants on the aerial tissues could not be completely removed, particularly because of the presence of trichomes and/or resin glands in the leaves of these drought-tolerant plants (Dallman 1998). By contrast, similarities in terms of the lowest metal levels might also result from the low bioavailability to plants of these metals on tailings (Ginocchio et al. 2006; Das and Maiti 2007).
Our findings highlight the interesting potential of native/endemic species for use in plant-based remediation technologies (phytostabilization or phytoextraction) for stabilizing ATDs located in semiarid Mediterranean-climate type environments of north-central Chile. Dominant plant species identified on studied ATDs are able to tolerate multiple environmental stresses, both substrate (e.g., poor nutritional content, low OM content) and climate (e.g., water stress) based. However, further studies are needed to determine the metal tolerance of pioneer plant species and their propagation requirements, among other autecological characteristics.
Conclusions
The present study showed that acidity, metal toxicity, and/or low nutrient levels are not the only and/or the main factors limiting spontaneous plant colonization of ATDs. From all physicochemical characteristics evaluated in the present study (e.g., pH, OM, EC, sulfate), content of fine particles (percentage of particles <2 μm) and total Cu concentration of tailings are the main factors restricting spontaneous colonization of ATDs in semiarid Mediterranean-climate type areas of north-central Chile. However, further studies are needed to verify Cu bioavailability and thus plant toxicity of these tailings. Unlike other studies that stated tailing acidity as a relevant factor restricting spontaneous plant colonization, secondary acidification of tailings was rare on studied ATDs due to semiarid climatic conditions and their elevated Ca content.
Ten plant species were identified as dominant pioneer species of ATDs in semiarid Mediterranean-climate type areas of north-central Chile (B. linearis, B. marginalis, B. berterianus, E. cicutarium, M. hastulata, P. revolutus, S. molle, S. polygama, S. arabicus, and T. absinthioides). None of them is exclusively found on ATDs, but most of them are native/endemic species adapted to local climatic and edaphic conditions of semiarid environments, in which seeds are spread out at large distances by the wind or animals. Few (e.g., B. linearis) have been previously described as pioneer and nurse species of highly disturbed sites in the area. These findings highlight the interesting potential of pioneer native/endemic species for being used in plant-based remediation technologies (phytostabilization or phytoextraction) for proper stabilization of ATDs located in north-central Chile.
References
Badilla-Ohlbaum R, Ginocchio R, Rodríguez PH, Céspedes A, González S, Allen HE (2001) Relationship between soil copper content and copper content of selected crop plants in central Chile. Env Tox and Chem 20:2749–2757
Baker AJM, Brooks RR (1989) Terrestrial higher plants which hyperaccumulate metallic elements: a review of their distribution, ecology and phytochemistry. Biorecovery 1:81–126
Baker A, Ernst W, Van der Ent A, Malaisse F, Ginocchio R (2010) Metallophytes: the unique biological resource, its ecology and conservational status in Europe, central Africa and Latin America. In: Batty L, Hallberg K (eds) Ecology of industrial pollution. Cambridge University Press, Cambridge, pp 7–40
Bouxin G (2005) Ginkgo, a multivariate analysis package. J Veg Sci 16:355–359. doi:10.1111/j.1654-1103.2005.tb02374.x
Bustamante R (1991) Clonal reproduction and succession: the case of Baccharis linearis in the Chilean matorral. Medio Ambiente 11:43–47
Casale JF, Ginocchio R, León-Lobos P (2011) Guía N°4: Marco ambiental y legal de relaves mineros abandonados en la Región de Coquimbo. In: INIA and CIMM (ed) Fitoestabilización de depósitos de relaves en Chile. Santiago de Chile, pp 41.
Chen G, Weil RR, Hill RL (2014) Effects of compaction and cover crops on soil least limiting water range and air permeability. Soil Tillage Res 136:61–69. doi:10.1016/j.still.2013.09.004
Conesa HM, Faz Á, Arnaldos R (2006) Heavy metal accumulation and tolerance in plants from mine tailings of the semiarid Cartagena-La Union mining district (SE Spain). Sci Total Environ 366:1–11. doi:10.1016/j.scitotenv.2005.12.008
Conesa HM, García G, Faz Á, Arnaldos R (2007) Dynamics of metal tolerant plant communities development in mine tailings from the Cartagena-La Unión Mining District (SE Spain) and their interest for further revegetation purposes. Chemosphere 68:1180–1185. doi:10.1016/j.chemosphere.2007.01.072
Cuevas JG, Silva SI, León-Lobos P, Ginocchio R (2013) Nurse effect and herbivory exclusion facilitate plant colonization in abandoned mine tailings storage facilities in north-central Chile. Rev Chil Hist Nat 86:63–74. doi:10.4067/S0716-078X2013000100006
Dallman PR (1998) Plant life in the world’s Mediterranean climates. California, Chile, South Africa, Australia, and the Mediterranean Basin. University of California Press, CA
Das M, Maiti SK (2007) Metal accumulation in 5 native plants growing on abandoned Cu-tailings ponds. Appl Ecol Environ Res 5:27–35
De La Iglesia R, Castro D, Ginocchio R, Van Der Lelie D, González B (2006) Factors influencing the composition of bacterial communities found at abandoned copper-tailings dumps. J Appl Microbiol 100:537–544. doi:10.1111/j.1365-2672.2005.02793.x
Di Castri F, Hajek E (1976) Bioclimatología de Chile. Ediciones Universidad Católica de Chile, Santiago de Chile
Dold B (2017) Acid rock drainage prediction: a critical review. J Geochemical Explor 172:120–132. doi:10.1016/j.gexplo.2016.09.014
Dold B, Fontboté L (2001) Element cycling and secondary mineralogy in porphyry copper tailings as a function of climate, primary mineralogy, and mineral processing. J Geochemical Explor 74:3–55. doi:10.1016/S0375-6742(01)00174-1
Ginocchio R, Baker AJM (2004) Metallophytes in Latin America: a remarkable biological and genetic resource scarcely known and studied in the region. Rev Chil Hist Nat 77:185–194. doi:10.4067/S0716-078X2004000100014
Ginocchio R, Sánchez P, de la Fuente LM, Camus I, Bustamante E, Silva Y, Urrestarazu P, Torres JC, Rodríguez PH (2006) Agricultural soils spiked with copper mine wastes and copper concentrate: implications for copper bioavailability and bioaccumulation. Environ Toxicol Chem 25:712–718. doi:10.1897/05-105R.1
Ginocchio R, de la Fuente LM, Sanchez P, Bustamante E, Silva Y, Urrestarazu P, Rodriguez PH (2009) Soil acidification as a confounding factor on metal phytotoxicity in soils spiked with copper-rich mine wastes. Environ Toxicol Chem 28:2069–2081. doi:10.1897/08-617.1
Horáčková M, Řehounková K, Prach K (2016) Are seed and dispersal characteristics of plants capable of predicting colonization of post-mining sites? Environ Sci Pollut Res 23:13617–13625. doi:10.1007/s11356-015-5415-5
Johnson AW, Gutiérrez M, Gouzie D, McAliley LR (2016) State of remediation and metal toxicity in the Tri-State Mining District, USA. Chemosphere 144:1132–1141. doi:10.1016/j.chemosphere.2015.09.080
Li MS (2006) Ecological restoration of mineland with particular reference to the metalliferous mine wasteland in China: a review of research and practice. Sci Total Environ 357:38–53. doi:10.1016/j.scitotenv.2005.05.003
Li X, Huang L (2015) Toward a new paradigm for tailings phytostabilization—nature of the substrates, amendment options, and anthropogenic pedogenesis. Crit Rev Environ Sci Technol 45:813–839. doi:10.1080/10643389.2014.921977
Lottermoser B (2007) Mine wastes. Characterization, treatment and environmental impacts. Second Edition. Springer, Berlin
Mendez MO, Maier RM (2008) Phytostabilization of mine tailings in arid and semiarid environments—an emerging remediation technology. Environ Health Perspect 116:278–283. doi:10.1289/ehp.10608
Moreno-de las Heras M (2009) Development of soil physical structure and biological functionality in mining spoils affected by soil erosion in a Mediterranean-Continental environment. Geoderma 149:249–256. doi:10.1016/j.geoderma.2008.12.003
Moreno-de las Heras M, Nicolau JM, Espigares T (2008) Vegetation succession in reclaimed coal-mining slopes in a Mediterranean-dry environment. Ecol Eng 34:168–178. doi:10.1016/j.ecoleng.2008.07.017
Mueller-Dombois D, Ellenberg P (1974) Aims and methods of vegetation ecology. Wiley, New York
Ottenhof CJM, Faz Cano Á, Arocena JM, Nierop KGJ, Verstraten JM, van Mourik JM (2007) Soil organic matter from pioneer species and its implications to phytostabilization of mined sites in the Sierra de Cartagena (Spain). Chemosphere 69:1341–1350. doi:10.1016/j.chemosphere.2007.05.032
Parraga-Aguado I, Gonzalez-Alcaraz MN, Alvarez-Rogel J, Jimenez-Carceles FJ, Conesa HM (2013) The importance of edaphic niches and pioneer plant species succession for the phytomanagement of mine tailings. Environ Pollut 176:134–143. doi:10.1016/j.envpol.2013.01.023
Parraga-Aguado I, Querejeta J, González-Alcaraz M, Jiménez-Cárceles FJ, Conesa HM (2014) Usefulness of pioneer vegetation for the phytomanagement of metal(loid)s enriched tailings: grasses vs shrubs vs trees. J Environ Manag 133:51–58. doi:10.1016/j.jenvman.2013.12.001
Pérez-Sirvent C, Hernández-Pérez C, Martínez-Sánchez MJ, García-Lorenzo ML, Bech J (2015) Geochemical characterisation of surface waters, topsoils and efflorescences in a historic metal-mining area in Spain. J Soils Sediments 16:1238–1252. doi:10.1007/s11368-015-1141-3
Pickett STA, White PS (1985) The ecology of natural disturbance and patch dynamics. Academic Press, San Diego, CA
Rehounková K, Prach K (2010) Life-history traits and habitat preferences of colonizing plant species in long-term spontaneous succession in abandoned gravel-sand pits. Basic Appl Ecol 11:45–53. doi:10.1016/j.baae.2009.06.007
Salt DE, Blaylock M, Kumar NP, Dushenkov V, Ensley BD, Chet I, Raskin I (1995) Phytoremediation: a novel strategy for the removal of toxic metals from the environment using plants. Nat Biotechnol 13:468–474. doi:10.1038/nbt0595-468
Schippers A, Jozsa PG, Sand W, Kovacs ZM, Jelea M (2000) Microbiological pyrite oxidation in a mine tailings heap and its relevance to the death of vegetation. Geomicrobiol J 17:151–162. doi:10.1080/01490450050023827
Šebelíková L, Řehounková K, Prach K (2016) Spontaneous revegetation vs. forestry reclamation in post-mining sand pits. Environ Sci Pollut Res 23:13598–13605. doi:10.1007/s11356-015-5330-9
SERNAGEOMIN (2015) Catastro de depósitos de relaves en Chile. Ministerio de Minería, Santiago de Chile
Shooner S, Chisholm C, Davies TJ (2015) The phylogenetics of succession can guide restoration: an example from abandoned mine sites in the subarctic. J Appl Ecol 52:1509–1517. doi:10.1111/1365-2664.12517
Shu WS, Ye ZH, Zhang ZQ, Lan CY, Wong MH (2005) Natural colonization of plants on five lead/zinc mine tailings in southern China. Restor Ecol 13:49–60. doi:10.1111/j.1526-100X.2005.00007.x
Soil Survey Staff (1993) Soil survey manual. USDA, Washington DC
Solís-Domínguez FA, White SA, Hutter TB, Amistadi MK, Root RA, Chorover J, Maier RM (2012) Response of key soil parameters during compost-assisted phytostabilization in extremely acidic tailings: effect of plant species. Environ Sci Technol 46:1019–1027. doi:10.1021/es202846n
Tapia Y, Diaz O, Pizarro C, Segura R, Vines M, Zúñiga G, Moreno-Jiménez E (2013) Atriplex atacamensis and Atriplex halimus resist As contamination in Pre-Andean soils (northern Chile). Sci Total Environ 450–451:188–196. doi:10.1016/j.scitotenv.2013.02.021
Tilman D (1988) Plant strategies and the structure and dynamics of plant communities. Princeton University Press, NJ
Tordoff GM, Baker AJM, Willis AJ (2000) Current approaches to the revegetation and reclamation of metalliferous mine wastes. Chemosphere 41:219–228. doi:10.1016/S0045-6535(99)00414-2
US Environmental Protection Agency (1995) Laboratory methods for soil and foliar analysis in long-term environmental monitoring programs. Cincinnati, OH.
USDA (2004) Soil survey laboratory methods manual. National Soil Survey Center, Natural Resources Conservation Service, Soil Survey Investigations Report 42, version 4.0. United States Department of Agriculture, Washington DC
Verdugo C, Sánchez P, Santibáñez C, Urrestarazu P, Bustamante E, Silva Y, Gourdon D, Ginocchio R (2011) Efficacy of lime, biosolids, and mycorrhiza for the phytostabilization of sulfidic copper tailings in Chile: a greenhouse experiment. Int J Phytoremediation 13:107–125. doi:10.1080/15226510903535056
Whiting SN, Reeves RD, Richards D, Johnson MS, Cooke JA, Malaisse F, Paton A, Smith JAC, Angle JS, Chaney RL, Ginocchio R, Jaffré T, Johns R, McIntyre T, Purvis OW, Salt DE, Schat H, Zhao FJ, Baker AJM (2004) Research priorities for conservation of metallophyte biodiversity and its sustainable uses in ecological restoration and site remediation. Restor Ecol 12:106–116
Yu Y, Wang H, Li Q, Wang B, Yan Z, Ding A (2016) Exposure risk of rural residents to copper in the Le’an river basin, Jiangxi Province, China. Sci Total Environ 548–549:402–407. doi:10.1016/j.scitotenv.2015.11.107
Żołnierz L, Weber J, Gilewska M, Strączyńska S, Pruchniewicz D (2016) The spontaneous development of understory vegetation on reclaimed and afforested post-mine excavation filled with fly ash. Catena 136:84–90. doi:10.1016/j.catena.2015.07.013
Acknowledgements
This study was funded by the INNOVA-Chile CORFO-04CR9IXD and the Comisión Nacional de Investigación Científica y Tecnológica—CONICYT FB 0002-2014. The authors would like to thank Claudio Canut de Bon, Universidad de La Serena; Jaime G. Cuevas, Sergio I. Silva, Ismael Jiménez, and Marcelo Rosas, INIA-Intihuasi; and Luz María de la Fuente and Elena Bustamante, Centro de Investigación Minera y Metalúrgica for their support with the field and laboratory works and taxonomical determinations of plant species.
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Ginocchio, R., León-Lobos, P., Arellano, E.C. et al. Soil physicochemical factors as environmental filters for spontaneous plant colonization of abandoned tailing dumps. Environ Sci Pollut Res 24, 13484–13496 (2017). https://doi.org/10.1007/s11356-017-8894-8
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DOI: https://doi.org/10.1007/s11356-017-8894-8