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Acta Botanica Brasilica

Print version ISSN 0102-3306

Acta Bot. Bras. vol.27 no.4 Feira de Santana Oct./Dec. 2013

http://dx.doi.org/10.1590/S0102-33062013000400006 

ARTICLES

 

Arbuscular mycorrhizal fungi in a semi-arid, limestone mining-impacted area of Brazil

 

 

Thaís Teixeira-RiosI; Renata Gomes de SouzaI; Leonor Costa MaiaI; Fritz OehlII; Cláudia Elizabete Pereira LimaI,*

IUniversidade Federal de Pernambuco, Centro de Ciências Biológicas, Departamento de Micologia, Recife, PE, Brazil
IIFederal Research Institute Agroscope Reckenholz-Tänikon ART, Organic Farming Systems, Zürich, Switzerland

 

 


ABSTRACT

The main goal of this study was to determine the diversity and activity of arbuscular mycorrhizal fungi (AMF) in an area degraded by limestone mining within the semi-arid region of Brazil known as the caatinga (shrublands). Near a limestone quarry, we selected two areas of caatinga (preserved and degraded) for study. The number of glomerospores did not differ significantly between the two areas. There was a trend toward the most probable number of infective propagules being higher in the degraded area. Twenty AMF taxa were identified in the two sampled areas, species richness, diversity and evenness being higher in the preserved area. Two species of Racocetra represent new records for the semi-arid region of Brazil. Glomerospore production and AMF species richness were unaffected by mining activity in the study area.

Key words: caatinga, glomerospores, infective propagules, mining activities, mycorrhiza


 

 

Introduction

Many interactions take place among the physical, chemical and biological components of soil, whose functionality depends on the environment in which it is located (Nannipieri et al. 2003). Particularly in the rhizosphere, various microbiological communities are essential for the occurrence of fundamental processes, such as biochemical cycling of the nutrients that influence the formation and maintenance of the soil and consequently the sustainability of land ecosystems (Barea et al. 2005).

The majority of plants form mycorrhizae, symbiotic associations with fungi that live in the root system. Those associations exercise an essential function for the structure and stability of plant communities. Arbuscular mycorrhizal fungi (AMF) are associated with representatives of more than 90% of the vascular plant families and, as obligate symbionts, are nutritionally dependent on the host plant (Smith & Read 2008). In exchange for plant-derived carbon, AMF facilitate plant absorption and uptake of nutrients from the soil, such as phosphorus (Jakobsen et al. 2001), and can increase plants' tolerance to toxic elements (Cumming & Ning 2003; Gattai et al. 2011), plant pathogens (Declerck et al. 2002), saline stress (Yano-Melo et al. 2003) and erosion (O'Dea 2007). The AMF can also help stabilize and aggregate soil, increasing the levels of soluble carbon and enzymes (e.g., urease, acid phosphatase and β-glucosidase), making them an important component to improve the growth of young plants under severe climate conditions (Caravaca et al. 2002).

Mining activity occurs in 26% of the municipalities within the semi-arid region of Brazil (DNPM 2009) and constitutes one of the human activities that most alters the land surface in the region. This activity can cause serious problems related to soil structure, water availability, biological activity, as well as to the supply of sulfur, phosphorus and nitrogen to plants, resulting in reduced productivity (Ferreira et al. 2007).

In arid and semi-arid regions, the generally low soil fertility makes plants highly dependent on mycorrhization (Tarafdar & Praveen-Kumar 1996), and it is therefore important to quantify the diversity of AMF in these regions, mainly in areas subject to degradation, such as those affected by mining activities. Due to the relevant role these fungi play in ecosystems, in this study we investigated the diversity, number of glomerospores and potential infectivity of AMF in an area of the Brazilian caatinga (shrublands) degraded by limestone mining, comparing the results with those obtained for a nearby preserved area.

 

Material and methods

Study areas

The investigated areas are located on a property owned by the company Cimpor Cimentos Brazil, in the municipality of Campo Formoso (10°30'27"S; 40°19'17''W), located within the São Francisco River Valley, which is in the northern part of the state of Bahia, Brazil. The climate is semi-arid, with irregular rainfall, ranging from 300 to 700 mm/year, most of the rainfall occurring between November and March. The average annual temperature is 22-23°C, and the average relative air humidity is 20%, making the region highly arid. The terrain is mostly flat, covered by spiny deciduous shrubs and bushes (typical of the caatinga), forming a generally open landscape, interspersed with a few emergent trees and virtually no herbaceous layer in the dry season (PRAD Cimpor 2004).

Data collection

Soil samples were collected in October 2008 (dry season), during which the average monthly temperature was 23.8°C and evapotranspiration was 36.4 mm. We selected two areas of caatinga vegetation for study: a preserved area; and an area degraded by limestone mining. In each area, an imaginary zig-zag line was traced and 20 soil samples (each comprising three subsamples of ca. 0.5 kg) were collected and placed in plastic bags for AMF studies. A single composite soil sample (ca. 1.0 kg) for each area was taken to the Soil Laboratory of the Pernambuco Institute of Agronomy for physical and chemical analyses (Tab. 1).

Evaluation of mycorrhizae

Glomerospores were extracted from 100 g of 20 soil samples by wet sieving (Gerdemann & Nicolson 1963), followed by centrifuging in water and sucrose at 50.0% (modified from Jenkins 1964). The glomerospores were then quantified in Petri dishes with a stereomicroscope (40×).

The most probable number (MPN) of infective propagules in the soil was evaluated according to Feldmann & Idzack (1994). For each area, we prepared a compound sample, which was diluted in washed, autoclaved sand at four dilution levels (no dilution; 1/10; 1/100; and 1/1000), with five replicates. Two corn seeds (Zea mays L.) were planted in each pot (150 ml). At 10 days after sowing, the seedlings were culled, leaving only one plant per pot. The plants were harvested at 30 days after culling. The roots were washed in running water, stained according to Phillips & Haymann (1970) and evaluated for the presence of mycorrhizal colonization.

We used the soil samples in order to quantify the glomerospores and to identify the AMF species directly or after growth in trap cultures using sorghum (Sorghum bicolor (L.) Moench) and peanut (Arachis hypogaea L.) as host plants. The trap cultures were kept in a greenhouse for three months and watered every other day. Glomerospores were extracted as described above, mounted on slides with polyvinyl-lacto-glycerol (PVLG) or with Melzer's reagent + PVLG (1:1 v/v) and observed under microscopy. For species identification, we consulted Schenck & Pérez (1990) and the International Culture Collection of (Vesicular) Arbuscular Mycorrhizal Fungi (http://invam.caf.wvu.edu), as well as new descriptions. The classification follows Oehl et al. (2011).

Data analysis

The numbers of glomerospores were analyzed by one-way ANOVA using the two areas (preserved and degraded) as variables. Means were compared by the Tukey's test (p < 0.05).

The Shannon diversity index (H') was calculated according to the following equation:

H' = − (Pi ln [Pi])

where Pi is the relative abundance (the number of individuals of the species i in relation to the total number of individuals of all species), and ln is the natural log. Pielou's evenness index (J') was obtained by the following equation:

J' = H'/log (S)

where S is the total number of species obtained with the PAleontological STatistics (PAST) program (Hammer et al. 2001). The species accumulation curve and the first-order Jackknife (Jackknife 1) index were estimated using the Primer 6.0 program (Clarke & Gorley 2006). The similarity between the two areas was estimated by the Sørensen index (Brower & Zar 1984). In accordance with Zhang et al. (2004), we defined the following categories of frequency of occurrence: dominant (> 50.0%); quite common (31.0-50.0%); common (10.0-30.0%); and rare (<10.0%).

 

Results and discussion

The number of glomerospores did not differ significantly between the preserved and degraded areas (164.0 ± 44.0/100 g−1 soil vs. 186.0 ± 47.0/100 g−1 soil). In both areas, the number of glomerospores was relatively low, as is common in arid and semi-arid regions (Requena et al. 1996). The high pH and limited availability of nutrients in the soil (Tab. 1), especially P, may have contributed to the small number of glomerospores (Entry et al. 2002). In an earlier study, Silva et al. (2001) obtained a similar result for an area of caatinga degraded by copper mining, reporting < 160.0 glomerospores/100 g−1 soil, suggesting that this response is related to host plant or soil toxicity in the area. However, in areas replanted after bauxite mining, Caproni et al. (2005) found an average of 2335.0 glomerospores/100 ml−1 soil, which can be considered a high density. More recently, Labidi et al. (2011) reported that CaCO3 has harmful effects on the colonization and number of mycorrhizal structures (arbuscules, vesicles, external mycelia and glomerospores) of Glomus irregulare Blaszk., Wubet, Renker & Buscot, with a negative impact on the fungus life cycle during the pre-symbiotic (germination) and symbiotic phases in the root systems of transformed chicory (Cichorium intybus L.). In the present study, the limestone quarry did not appear to have a negative influence on the formation of glomerospores, given that similar number was found in both areas.

We observed a trend toward the number of infective propagules being higher in the degraded area than in the preserved area (35.0/cm−3 soil vs. 13.0/cm−3 soil). The distribution and abundance of AMF propagules can also be related to the complexity of the mycorrhizal community (Ramos-Zapata et al. 2011). The number of infective propagules, together with the low number of glomerospores, can indicate that the infectivity of the AMF in the sampled areas is more dependent on colonized roots than on glomerospores, and the stressful conditions in the area surrounding the mine possibly induces lower infectivity, corroborating the results of other studies conducted in the caatinga (Lima et al. 2007; Mergulhão et al. 2007). A similar result was found in a mined area covered with molasses grass, guandu beans (pigeon peas) and native plants, where the authors observed 39.3 propagules/g−1 soil, while in a closed forest area containing tree species the number was only 11.2 propagules/g−1 soil (Melloni et al. 2003). In another area of caatinga in the state of Bahia, Silva et al. (2001) found a much lower number of propagules (0.15/cm−3 soil). Although the methods used by Melloni et al. (2003) and Silva et al. (2001) to evaluate the MPN of propagules were different from that used in the present study, the fact that the MPN of infective propagules identified here was nearly 90 times higher than that reported by Silva et al. (2001) suggests a significant difference between the two studies, underscoring the need for standardization of methods in mycorrhizal studies (Maia et al. 2010).

In the present study, we found no difference between the preserved and degraded areas in terms of AMF diversity, evenness or richness, as measured by the Shannon index (H' = 2.30 and H' = 2.12, respectively), Pielou's index (J' =0.81 and J' = 0.78, respectively) and the total number of species (17 and 15, respectively). Regarding AMF diversity, 12 species occurred in both areas, representing a 75.0% similarity, which can be related to the nonspecific nature of the AMF, independent of the local conditions (Dandan & Zhiwei 2007). In a study conducted in India, Radhika & Rodrigues (2010) compared AMF diversity between two areas with different levels of available P. The authors found that other physico-chemical conditions of the soil, such as texture and pH, also influenced AMF diversity and dominance. Although AMF are commonly found in arid regions, their diversity declines as aridity increases (Stutz & Morton 1996). In another study conducted in the caatinga of northeastern Brazil, Maia et al. (2010) identified over 70 species of AMF. In the Xingó region, located in the state of Alagoas, Souza et al. (2003) identified 24 AMF taxa, some of which were also found in this study: Acaulospora longula, Claroideoglomus etunicatum, Funneliformis mosseae and Paraglomus occultum. In the municipality of Jaguarari, in the state of Bahia, Silva et al. (2005) identified 15 AMF species, six of which were also registered in our study: Entrophospora infrequens, C. etunicatum, Glomus macrocarpum, G. microcarpum, F. mosseae and P. occultum.

In the present study, we identified a total of 20 AMF taxa (Tab. 2). We observed more AMF species in the preserved area than in the degraded area, with an overall dominance of Glomus macrocarpum, followed by Claroideoglomus etunicatum, which was dominant in the degraded area and quite common in the preserved area. The other species were classified as common or rare in both areas. The sampling effort was sufficiently efficient to recover 83.0% of the total species, as determined by the Jackknife 1 estimator (Figure 1). Species observed in the trap cultures did not differ from those found in the field.

 

 

The predominance of representatives of Glomeraceae (Glomus and Funneliformis) and Entrophosporaceae (Claroideoglomus and Entrophospora) confirms the tolerance of these individuals to soil disturbances and anthropogenic environments and acid to neutral soils (Boddington & Dodd 2000; Sieverding & Oehl 2006). Species of the genus Acaulospora have often been associated with acidic soils (Morton 1986; Abbott & Robson 1991). However, in the present study, various species of that genus were found to occur on alkaline soil, also a frequent finding in arid areas of tropical zones (Tao & Zhiwei 2005), although less so in subtropical zones and rarely in colder climates (Yang et al. 2011). Representatives of the Glomus genus are also commonly found in arid regions (Pande & Tarafdar 2004; Silva et al. 2005; Tian et al. 2009; Mello et al. 2012), where their occurrence is related to variations in the edaphic conditions, as well as to their high adaptability to varying conditions of soil and temperature, enabling them to survive in acidic and alkaline soils alike. In addition, the great quantity and small size of their glomerospores facilitate distribution in arid environments (Stutz et al. 2000).

Representatives of Ambispora and Entrophospora occurred in both of the areas evaluated in the present study, as did Acaulospora longula, Acaulospora mellea, Claroideoglomus etunicatum, Entrophospora infrequens, Funneliformis mosseae, Glomus macrocarpum, Pacispora boliviana and Paraglomus occultum. However, some species (Acaulospora morrowiae, Glomus microcarpum, Racocetra fulgida and R. verrucosa) were exclusive to the preserved area, whereas others (Acaulospora lacunosa, Acaulospora scrobiculata and Glomus brohultii) were exclusive to the degraded area.

The application of limestone to the soil did not alter the community of native AMF in degraded areas of the Brazilian savanna (Martins et al. 1999). However, soil disturbances have a large impact on the AMF community (Schnoor et al. 2011), possibly reducing the richness of sensitive species and increasing that of tolerant species. In a area of transition between open-pit copper mining and a preserved area of caatinga, Silva et al. (2005) registered Acaulospora scrobiculata, Claroideoglomus etunicatum, Glomus macrocarpum, Funneliformis mosseae and Paraglomus occultum, species also observed in this study (degraded area). Melloni et al. (2003) identified six AMF species in reclaimed areas after bauxite mining, among them A. scrobiculata and P. occultum, species that can be classified as generalists (Oehl et al. 2010; Tchabi et al. 2009), at least in tropical zones.

Information on the diversity of AMF can be used to investigate the function of these fungi in maintaining plant biodiversity and the function of the ecosystem during conservation and restoration of various natural ecosystems, especially in semi-arid zones (Dandan & Zhiwei 2007). The knowledge of the diversity and activity of AMF obtained here adds to that provided by previous studies conducted in arid areas and areas degraded by mining. New species of AMF have recently been described in the caatinga biome (Goto et al. 2010) and could be exclusive to Brazil. In the present study, the two species of Racocetra are among the first reported for the semi-arid region of Brazil. Our results indicate that the production of glomerospores is not altered by limestone mining activity. Our findings also confirm the predominance of Glomus in areas with a semi-arid climate, as well as showing that species that are more tolerant can be dominant in stressful environments, in contrast to rare species in unaltered environments. Knowledge of AMF diversity in Brazil can inform decisions related to public policies for environmental preservation and programs to produce seedlings of native plants for reclamation of degraded areas in the semi-arid region of the country.

 

Acknowledgments

This work was supported by the Brazilian Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq, National Council for Scientific and Technological Development; Grant nos. 563342/2010-2 and 562330/2010-0), the Brazilian Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES, Office for the Advancement of Higher Education) and the Cimpor Cimentos Company, which provided access for the collection of specimens.

 

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Received: 9 February, 2013
Accepted: 7 July, 2013

 

 

* Author for correspondence: claudiaeplima@gmail.com

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