Literature DB >> 28154485

Community Structures of Arbuscular Mycorrhizal Fungi in Soils and Plant Roots Inhabiting Abandoned Mines of Korea.

Hyeok Park1, Eun-Hwa Lee1, Kang-Hyeon Ka2, Ahn-Heum Eom1.   

Abstract

In this study, we collected rhizosphere soils and root samples from a post-mining area and a natural forest area in Jecheon, Korea. We extracted spores of arbuscular mycorrhizal fungi (AMF) from rhizospheres, and then examined the sequences of 18S rDNA genes of the AMF from the collected roots of plants. We compared the AMF communities in the post-mining area and the natural forest area by sequence analysis of the AMF spores from soils and of the AMF clones from roots. Consequently, we confirmed that the structure of AMF communities varied between the post-mining area and the natural forest area and showed significant relationship with heavy metal contents in soils. These results suggest that heavy metal contamination by mining activity significantly affects the AMF community structure.

Entities:  

Keywords:  Arbuscular mycorrhizal fungi; Community; DNA cloning; Diversity; Mycorrhizae

Year:  2016        PMID: 28154485      PMCID: PMC5287160          DOI: 10.5941/MYCO.2016.44.4.277

Source DB:  PubMed          Journal:  Mycobiology        ISSN: 1229-8093            Impact factor:   1.858


Arbuscular mycorrhizal fungi (AMF) are symbiotic fungi associated with more than 80% of terrestrial plants [1]. AMF increase the fitness of host plants by allowing increased uptake of soil nutrients and water, increased tolerance to plant pathogens and environmental stresses such as drought, salts, and heavy metals [2345]. These symbiotic associations function as an important biological factor in disturbed soil ecosystems [67]. Symbiotic associations between host plants and AMF play an important role in soil ecosystems that are disturbed naturally by forest fires and earthquakes, or artificially by forest thinning, mining, and farming [7]. There are approximately 5,000 mining sites in Korea, and approximately 40% of these are metal mines. Most of the metal mines were abandoned without adequate environmental habilitation and have therefore affected the surrounding ecosystems. Soil contamination is a serious condition because of the heavy metals contained in the abandoned mining equipment, the mullocks remaining from the ore dressing process, and the waste water discharged during ore smelting [89]. It has been reported that the AMF community in disturbed areas shows different species composition from that in undisturbed soil [10]. AMF communities in soil contaminated with heavy metals vary significantly according to the kinds and contents of the heavy metals because different AMF species show varying degrees of tolerance to heavy metals [11]. AMF spore analysis has been used in previous studies on AMF in the rhizosphere soil of host plants [121314]. However, it is difficult to understand the origin of spore formation using AMF spore analysis in soil alone, which has limited the study of AMF communities that form mycorrhizae in the roots of host plants [15]. To confirm the relationships between host plants and AMF accurately, it is necessary to investigate the AMF colonizing the roots of host plants. In this study, we investigated AMF communities colonizing the roots as well as the spores in the rhizosphere soil from an abandoned metal mine in Korea.

MATERIALS AND METHODS

The soils and roots used in this study were collected from a mine (128°12'50'' E, 37°04'05'' N) located in Jecheon, Korea. The mine was closed in 1981 after about 20 years of mining molybdenum and other heavy metals [16]. Ten samples of soils and roots were randomly collected within a radius of 20 m from the mine-tail. A natural forest area located at 200 m from the mine-tail was selected as a control site, and another 10 samples were randomly collected within a radius of 20 m. The collected samples were packed into polyethylene bags and transported to the laboratory. Root samples for molecular analysis were stored at −80℃, and the root samples for mycorrhizal root colonization rate and the soils for spore analysis were stored at 4℃. The heavy metal concentration in the soil samples was analyzed in a soil analysis laboratory (Jeil Analysis Center, Seoul, Korea). AMF spores were extracted from 10 g of dried soil samples using wet decanting and sucrose density gradient methods [17]. The morphological characteristics of the extracted spores were observed under light microscopes. Spores were identified by the morphological characteristics of spore walls, such as number, thickness, color, structure, and surface ornamentations. In addition, each species was identified morphologically. DNA was extracted from spores, and small subunit ribosomal DNA fragments were amplified by nested PCR [18]. The first PCR was performed using the universal primers NS1 and NS4, and the product was used as template for the second amplification using AMFspecific primers, AML1 and AML2 [19]. The second PCR product was then sequenced (Solgent Co., Daejeon, Korea). A sequence-similarity search of the National Center for Biotechnology Information (NCBI) database was conducted using the Basic Local Alignment Search Tool (BLAST) algorithm. The sequences were aligned, and a phylogenetic tree was obtained using MEGA5 [20]. The obtained sequences were submitted to Genbank with the accession numbers KX879056~KX879063. Six roots of Lespedeza cyrtobotrya were selected from 20 root samples for mycorrhizal colonization and community analysis. To examine the AMF colonization rates, the plant roots were washed and stained with trypan blue according to the methods described by Koske and Gemma [21]. The roots were observed under a microscope (AXIO Imager; Carl Zeiss, Jena, Germany), and root colonization rates were measured by the previously described magnified intersects technique. DNA was extracted from surface-sterilized root samples using the DNeasy Plant Mini Kit (Qiagen, Venlo, Netherlands) with 30% H2O2 solution. Nested PCR was performed to amplify the small subunit rDNA using primers NS1 and NS4 for the first PCR and AML1 and AML2 for the second PCR as previously described for spores. The PCR product was purified using Solgent PCR purification kit and cloned using T-blunt PCR cloning kit following the manufacturer's instructions [22]. The nucleotide sequence of 20 clones from each sample was determined using an automated sequencer, and identified through BLAST and phylogenetic sequence analysis. Only the sequences belonging to Glomeromycota were included in the analysis. In order to determine the phylogenetic relationships among operational taxonomic units (OTUs), representative sequences for each OTU were selected and aligned with the closest matches obtained from GenBank by BLAST using the ClustalX algorithm in MEGA5. Neighbor-joining phylogenetic analysis was conducted in MEGA5 using a bootstrap analysis with 1,000 replicates. The obtained sequences were submitted to Genbank with the accession numbers KX879064~KX879070. Relative abundances for AMF communities in soils and roots were estimated based on the molecular and morphological identification data for each root sample. Shannon diversity indices were also calculated [21]. Univariate analysis of variance (ANOVA) was used to evaluate the fixed effect of the sampling site on the percent mycorrhizal root colonization rates and the species diversity of AMF communities. Pearson correlation analysis was performed to test the effects of heavy metals on AMF communities using the statistical package, SPSS-WIN ver. 12 (SPSS Inc., Chicago, IL, USA).

RESULTS AND DISCUSSION

Soil chemical analysis for heavy metals (As, Pb, Cd, Ni, and Zn) showed that the concentrations of As and Zn were significantly higher in the abandoned mines than in the natural forest (Table 1). Pb was not detected in both the soils collected in this study, and Cd was detected in the soil at both sites but showed no significant difference between locations.
Table 1

Heavy metal contents in soils of post-mining areas and natural forest areasa

Values are presented as mean ± SE.

aDifferent letters indicate significant difference between sites at p < 0.05.

Morphological and molecular analysis of spores in rhizosphere soils showed that 8 species of 7 genera were found in the post-mining area, and 6 species of 5 genera of AMF were found in the natural forest area (Table 2, Fig. 1). Relative abundance showed that Claroideoglomus etunicatum was the most dominant species in the post-mining area and that Rhizophagus irregularis was dominant in the natural forest area (Table 2). Acaulospora longula and Ambispora leptoticha were found only in the mine area. The total spore numbers were higher in the mining area than those in the natural forests. Shannon's index and species evenness were also higher in the mining area than that in the natural forest but were not statistically significant. Correlation analysis of heavy metal concentration with relative abundance of spores showed that A. longula has a strong positive relationship with the heavy metals As and Zn, which were significantly higher in the mining area (Table 3). The accumulation of heavy metals significantly influenced the AMF spore communities in the soil for a long period.
Table 2

Relative abundance of arbuscular mycorrhizal fungi spores in in soils of post-mining areas and natural forest areas

Values are presented as mean ± SE.

aSignificant difference between sites at p < 0.05.

Fig. 1

Neighbor-joining phylogenic tree for partial 18S rDNA sequence of arbuscular mycorrhizal fungal spores in soils. Rhodotorula hordea was used as an outgroup and bootstrap values (> 50) were shown at the nodes (●, mining area; ○, natural forest).

Table 3

Correlations between heavy metal contents and the relative abundance of arbuscular mycorrhizal fungi (AMF) species

aSignificant difference between sites at p < 0.05.

Mycorrhizal root colonization rates were significantly higher in the mine area (81.33 ± 2.67%) than in the natural forest area (61.67 ± 2.85) at p < 0.05, suggesting that significantly high concentrations of heavy metals affect mycorrhizal symbiosis with host plants at the mining sites. Cloning results for AMF-colonizing roots allowed identification of 7 OTUs in the mine area and 5 OTUs in the species of the forest area (Table 4, Fig. 2). Relative abundance showed that Glo6 was dominant in both the mine and the natural forest areas. Glo2, Glo5, and Glo7 were found only in the mine area, and Glo4 was found only in the forest area. In this study, more diverse AMF sequence types were found in the roots of plants in the mining area with high concentration of heavy metals. However, some previous studies showed that OTU number and root colonization rates were decreased with increasing concentrations of heavy metals [23]. Thus, it is considered that diversity of AMF could be increased or decreased according to the intensity of the heavy metals which act as a disturbance. Shannon indices were not significantly different between the two areas (Table 4), and correlation analysis showed no significant relationship between the relative abundances of AMF species and heavy metal concentrations. Significantly, higher heavy metal concentrations, especially of Zn, might be the reason for the higher colonization rates in the mining area.
Table 4

Relative abundance of arbuscular mycorrhizal fungi colonizing roots of post-mining areas and natural forest areas

Values are presented as mean ± SE.

OTU, operational taxonomic unit.

Fig. 2

Neighbor-joining phylogenic tree for partial 18S rDNA sequence of arbuscular mycorrhizal fungi colonizing roots. Rhodotorula hordea was used as an outgroup and bootstrap values (> 50) were shown at the nodes (●, mining area; ○, natural forest).

It has been reported that high accumulation of Zn stressed the host plants and increased AMF colonization in their roots [24]. The reason might be that though some AMF species are sensitive to heavy metals, other species are tolerant of high heavy metal concentration in soil [25]. Previous studies show that AMF species belonging to Claroideoglomus are often tolerant to heavy metals [26], and the results of this study showed that species of Claroideoglomus were significantly more in the mine area. Additionally, A. longula showed a strong positive correlation with As and Zn and is consistent with previous results [27] that the frequency of A. longula is higher in higher concentrations of Zn. In addition, A. leptoticha, which was found only in the mining area in this study, was also frequently found in contaminated soil containing Zn [28]. However it have been reported that AMF communities in soil contaminated by heavy metals more affected by other chemicals in the soil than heavy metals [29]. Thus, the diversity of AMF communities in abandoned mine area should be considered with factors of the soil environments as well as the intensity of the disturbance. The species mainly found in abandoned mines with a long period of ecological disturbance belonged to Glomaceae [2330]. Previous studies showed that the Glomaceae species were dominant under stress conditions such as ecological disturbances, suggesting that Glomaceae species are better adapted to disturbed environments than other species [3132]. In this study, AMF species, C. etunicatum, R. irregularis, R. intraradices in Glomaceae were species having a high relative abundance common to both abandoned and natural forest area. The result was consistent with previous studies of heavy metal contaminated areas [33], suggesting that the emergence of these species would be the results of strong selection pressure in the settlement process of plants than the intensity of the disturbance. In conclusion, this study showed that the anthropogenic disturbance of mining activities affects the AMF communities.
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