Abundance of bacterivore species in three zones of coal mine region of district Sonebhadra Uttar Pradesh.
Abstract
This present study underscores the significance of soil nematodes as indicators of ecological health, particularly in areas affected by human activities like mining. Soil nematodes, classified into five trophic groups, play vital roles in nutrient cycling and provide insights into soil food web dynamics. Various nematode community indices, including the maturity index (MI) and trophic diversity index (TDI), are crucial for assessing soil food web diversity. Nematodes exhibit adaptability across diverse soil environments, from pristine to highly disturbed habitats, making them responsive indicators of environmental changes. Understanding nematode community structure enhances their potential as global indicators for assessing food resource availability and habitat characterization. This study compares three different zones based on anthropogenic disturbances in the coal mining region of Sonebhadra, Uttar Pradesh, representing undisturbed, moderately disturbed, and intensely disturbed sites. By analyzing nematode communities and trophic group abundance, the study assesses soil ecosystems across these zones. Human activities, especially mining, significantly impact soil nematode diversity and ecosystem health. Transition from natural forests to mining sites leads to shifts in nematode communities and species diversity, with intermediate disturbance fostering increased species diversity. Maturity index values reflect ecosystem maturity, with undisturbed and moderately disturbed zones indicating structured ecosystems, while highly disturbed zones represent degraded conditions. Faunal profiles mirror these findings, indicating shifts in decomposition pathways. This study highlights the potential of nematodes as indicators for environmental monitoring and quality assessment in coal mine areas. Further research on individual nematode species can inform biodiversity modeling and contribute to more effective ecological restoration efforts.
Keywords
- soil nematodes
- trophic groups
- mining activities
- faunal profiles
- decomposition pathways
- biodiversity modeling
- ecological restoration
1. Introduction
Nematodes have been categorized into five primary trophic groups [1, 2]. They play a significant role in nutrient mineralization through energy decomposition pathways [3, 4, 5, 6] and offer valuable insights into the structure and function of soil food webs [1, 7, 8, 9]. Nematode community indices, such as the maturity index (MI) based on c-p scaling, the plant parasitic index (PPI) (weighted mean of c-p values of plant-parasitic nematodes), species richness, evenness, the ratio of bacterivore to fungivore nematodes, and the trophic diversity index (TDI), are routinely employed to assess soil food web diversity conditions [10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20]. Furthermore, various faunal food web indices for nematodes, such as enrichment (EI), structure (SI), and decomposition channel index (CI), based on the relative weighted abundance of nematode c-p guilds, provide information on enrichment, trophic connections, structure, and prevailing decomposition in a food web [1].
Nematodes are valuable indicators as they inhabit soils ranging from pristine to highly disturbed habitats and are represented in almost all trophic groups of the soil food web. They respond quickly and specifically to environmental changes. A comprehensive understanding of nematode community structure for assessing food resource availability and characterizing different habitats would enhance the indicative capability of nematodes on a global scale [1, 21].
Although we have limited knowledge about the influence of vegetation and abiotic parameters on nematode fauna, drawing trends can be challenging due to geological, climatological, and methodological differences among various sites or studies [22]. Analyzing the soil nematode community can reveal differences between habitats [19, 21].
In the present study, three different zones with varying degrees of anthropogenic disturbances in the coal mine region of district Sonebhadra, Uttar Pradesh, were compared. Various parameters of the nematode community were used to assess the prevailing soil ecosystem in these zones. Depending on the nature and frequency of disturbances (physical, chemical, or biological), active mining land and wild forests (potential future mining sites) represent two extremes in terms of ecosystem structure and stability. The three zones identified based on the degree of human interference were: undisturbed hillocks or potential future mining sites (Zone ‘A’), moderately disturbed and managed habitat represented by abandoned reclaimed land after mining (Zone ‘B’), and intensively disturbed habitat as the active mining site (Zone ‘C’).
The objectives of the study were to compare these three selected habitats using a combination of nematode community indices and trophic group abundance and to examine substrate characteristics through nematode community measures using multivariate analyses.
2. Description of site and protocol of study
See Figure 1
The coal mine region was divided broadly into three differentiating sites on gradient of anthropogenic disturbances.
3. Materials and methods
Sampling was done using steel corer of 5 cm diam. For each Zone 30 samples were collected with each sample being a composite of five samples. Samples were then stored in plastic bags and transported to the lab for chemical analysis and nematode identification. The climatic and edaphic information were also recorded (Table 1). Geographic data like geographic coordinates, altitude, and temperature were recorded
Nematode species | Functional guild | Mean ± SD (abundance) | ||
---|---|---|---|---|
Bacterivores | Zone ‘A’ Undisturbed forest (site for advance quarry) | Zone ‘B’ Spoil of median age | Zone ‘C’ Active site of mining | |
Ba2 | 10.56 ± 3.54 | 28.24 ± 21.24 | 0.0 ± 0.0 | |
Ba2 | 14.39 ± 16.54 | 20.12 ± 15.54 | 0.0 ± 0.0 | |
Ba2 | 10.34 ± 7.45 | 12.45 ± 8.64 | 0.48 ± 0.75 | |
Ba2 | 18.15 ± 2.56 | 15.10 ± 12.10 | 0.0 ± 0.0 | |
Ba2 | 5.24 ± 3.21 | 0.63 ± 2.25 | 0.0 ± 0.0 | |
Ba3 | 18.35 ± 32.30 | 30.34 ± 44.53 | 0.0 ± 0.0 | |
Ba3 | 16.3 ± 15.53 | 13.54 ± 8.64 | 0.0 ± 0.0 | |
Ba2 | 10.4 ± 6.24 | 7.52 ± 10.25 | 0.0 ± 0.0 | |
Ba2 | 10.86 ± 7.25 | 7.81 ± 5.23 | 0.0 ± 0.0 | |
Ba2 | 9.26 ± 4.23 | 19.83 ± 25.3 | 0.0 ± 0.0 | |
Ba2 | 1.45 ± 7.59 | 0.25 ± 1.25 | 0.0 ± 0.0 | |
Ba2 | 0.50 ± 2.76 | 0.65 ± 2.54 | 0.0 ± 0.0 | |
Ba2 | 16.68 ± 18.85 | 18.25 ± 12.24 | 0.0 ± 0.0 | |
Ba2 | 12.24 ± 8.35 | 8.53 ± 12.53 | 0.0 ± 0.0 | |
Ba1 | 0.00 ± 0.00 | 0.94 ± 3.65 | 0.0 ± 0.0 | |
Ba1 | 13.51 ± 8.56 | 22.45 ± 9.45 | 0.36 ± 0.67 | |
Ba1 | 8.45 ± 6.45 | 15.53 ± 12.67 | 0.48 ± 0.84 | |
Ba2 | 11.84 ± 6.85 | 15.28 ± 14.53 | 0.0 ± 0.0 | |
Ba2 | 12.54 ± 6.44 | 9.28 ± 5.68 | 0.0 ± 0.0 | |
Ba1 | 0.00 ± 0.00 | 8.22 ± 3.25 | 0.0 ± 0.0 | |
Ba1 | 3.15 ± 1.23 | 1.75 ± 0.57 | 0.0 ± 0.0 | |
Ba2 | 15.83 ± 6.86 | 8.75 ± 6.55 | 0.0 ± 0.0 | |
Ba2 | 16.84 ± 18.24 | 18.49 ± 20.24 | 0.0 ± 0.0 | |
Ba2 | 7.42 ± 4.24 | 5.77 ± 14.99 | 0.0 ± 0.0 | |
Ba1 | 2.15 ± 0.24 | 0.55 ± 2.50 | 0.0 ± 0.0 | |
Ba3 | 12.46 ± 14.48 | 16.86 ± 12.86 | 0.0 ± 0.0 | |
Ba3 | 2.43 ± 1.75 | 1.25 ± 3.45 | 0.0 ± 0.0 | |
Ba2 | 3.26 ± 2.36 | 3.86 ± 1.67 | 0.0 ± 0.0 | |
Ba2 | 3.35 ± 1.75 | 3.55 ± 5.43 | 0.0 ± 0.0 | |
Ba2 | 2.72 ± 2.24 | 0.74 ± 2.24 | 0.0 ± 0.0 |
4. Results and observations
4.1 Nematode abundance
4.2 Nematode species diversity
4.3 Nematode trophic structure
In Zone ‘A’ there was much diversity of omnivores and predators in comparison to bacterivores and in Zone ‘B’ bacterivores and fungivores nematodes were the abundant group over omnivores and predators and Zone ‘C’ had only three bacterivore species.
4.3.1 Zone ‘A’
4.3.1.1 Trophic groups
Nematode species | Functional guild | Mean ± SD (abundance) | ||
---|---|---|---|---|
Fungivores | Zone ‘A’ Undisturbed forest (Site for advance quarry) | Zone ‘B’ Spoil of Median Age | Zone ‘C’ Active site of mining | |
Fu2 | 16.43 ± 6.05 | 16.48 ± 8.45 | 0.0 ± 0.0 | |
Fu2 | 32.04 ± 18.64 | 12.6 ± 10.35 | 0.0 ± 0.0 | |
Fu2 | 36.13 ± 20.13 | 18.74 ± 16.36 | 0.0 ± 0.0 | |
Fu5 | 9.40 ± 3.56 | 2.25 ± 1.75 | 0.0 ± 0.0 | |
Fu2 | 8.95 ± 4.31 | 6.25 ± 4.21 | 0.0 ± 0.0 | |
Fu5 | 10.42 ± 4.10 | 5.40 ± 2.50 | 0.0 ± 0.0 | |
Fu2 | 3.67 ± 1.58 | 13.43 ± 6.48 | 0.0 ± 0.0 | |
Fu3 | 12.10 ± 4.20 | 4.61 ± 2.80 | 0.0 ± 0.0 | |
Fu2 | 3.26 ± 2.05 | 11.4 ± 6.23 | 0.0 ± 0.0 | |
Fu5 | 16.82 ± 6.42 | 8.64 ± 3.56 | 0.0 ± 0.0 | |
Fu2 | 39.27 ± 20.46 | 13.45 ± 6.45 | 0.0 ± 0.0 | |
Fu2 | 22.30 ± 10.46 | 16.43 ± 8.23 | 0.0 ± 0.0 | |
Fu2 | 18.20 ± 9.65 | 15.43 ± 6.28 | 0.0 ± 0.0 | |
Fu2 | 4.85 ± 2.24 | 5.44 ± 3.24 | 0.0 ± 0.0 | |
Fu5 | 4.64 ± 3.41 | 5.53 ± 2.54 | 0.0 ± 0.0 | |
Fu4 | 28.41 ± 14.42 | 12.34 ± 6.80 | 0.0 ± 0.0 | |
Fu2 | 7.23 ± 3.54 | 10.23 ± 4.25 | 0.0 ± 0.0 |
Nematode species | Functional guild | Mean ± SD (abundance) | ||
---|---|---|---|---|
Herbivores | Zone ‘A’ Undisturbed forest (site for advance quarry) | Zone ‘B’ Spoil of median age | Zone ‘C’ Active site of mining | |
H2 | 16.80 ± 6.46 | 7.25 ± 4.23 | 0.0 ± 0.0 | |
H2 | 9.35 ± 4.05 | 3.36 ± 2.35 | 0.0 ± 0.0 | |
H2 | 6.87 ± 5.64 | 1.53 ± 2.50 | 0.0 ± 0.0 | |
H3 | 9.64 ± 4.38 | 12.68 ± 5.85 | 0.0 ± 0.0 | |
H3 | 15.38 ± 8.36 | 6.86 ± 4.25 | 0.0 ± 0.0 | |
H3 | 1.50 ± 2.35 | 1.02 ± 2.21 | 0.0 ± 0.0 | |
H3 | 2.30 ± 3.66 | 10.25 ± 6.23 | 0.0 ± 0.0 | |
H5 | 13.45 ± 8.36 | 2.52 ± 0.0 | 0.0 ± 0.0 | |
H5 | 16.84 ± 10.35 | 1.08 ± 2.50 | 0.0 ± 0.0 | |
H2 | 4.68 ± 3.45 | 1.24 ± 3.65 | 0.0 ± 0.0 | |
H3 | 3.87 ± 2.36 | 1.25 ± 0.58 | 0.0 ± 0.0 | |
H2 | 2.48 ± 2.01 | 1.20 ± 2.36 | 0.0 ± 0.0 | |
H2 | 9.85 ± 6.46 | 12.26 ± 6.58 | 0.0 ± 0.0 | |
H2 | 10.64 ± 6.68 | 0.0 ± 0.0 | 0.0 ± 0.0 | |
H3 | 4.65 ± 3.34 | 0.56 ± 1.14 | 0.0 ± 0.0 | |
H3 | 6.80 ± 4.88 | 0.26 ± 2.24 | 0.0 ± 0.0 | |
H3 | 1.54 ± 2.34 | 0.50 ± 1.54 | 0.0 ± 0.0 | |
H3 | 2.38 ± 1.36 | 0.35 ± 2.25 | 0.0 ± 0.0 | |
H4 | 8.62 ± 4.38 | 1.24 ± 2.52 | 0.0 ± 0.0 | |
H3 | 11.56 ± 8.44 | 10.23 ± 6.45 | 0.0 ± 0.0 | |
H3 | 12.56 ± 6.35 | 5.86 ± 3.54 | 0.0 ± 0.0 | |
H5 | 6.24 ± 9.25 | 9.25 ± 5.24 | 0.0 ± 0.0 |
Nematode species | Functional guild | Mean ± SD (abundance) | ||
---|---|---|---|---|
Omnivores | Zone ‘A’ Undisturbed forest (site for advance quarry) | Zone ‘B’ Spoil of median age | Zone ‘C’ Active site of mining | |
Om4 | 6.24 ± 4.36 | — | — | |
Om4 | 6.20 ± 5.48 | — | — | |
Om4 | 16.84 ± 9.65 | 4.24 ± 2.35 | — | |
Om4 | 12.86 ± 9.80 | 6.33 ± 3.26 | — | |
Om4 | 10.54 ± 5.46 | 1.56 ± 3.28 | — | |
Om4 | 8.64 ± 5.24 | 0.45 ± 1.56 | — | |
Om4 | 13.64 ± 8.30 | 5.26 ± 3.25 | — | |
Om4 | 8.64 ± 5.45 | — | — | |
Om4 | 3.58 ± 4.24 | — | — | |
Om4 | 20.42 ± 12.92 | 15.50 ± 11.54 | — | |
Om4 | 24.56 ± 18.45 | 18.35 ± 8.62 | — | |
Om4 | 31.54 ± 22.56 | 2.45 ± 3.56 | — | |
Om4 | 7.45 ± 6.52 | — | — | |
Om4 | 20.38 ± 11.36 | — | — | |
Om4 | 20.38 ± 16.36 | 23.56 ± 13.46 | — | |
Om4 | 18.45 ± 8.46 | 8.54 ± 5.64 | — | |
Om4 | 12.45 ± 6.75 | 8.65 ± 5.60 | — | |
Om4 | 16.45 ± 9.45 | — | — | |
Om4 | 19.44 ± 12.46 | — | — | |
Om5 | 10.65 ± 6.54 | — | — | |
Om5 | 8.64 ± 4.84 | — | — | |
Om4 | 15.46 ± 12.24 | — | — | |
Om4 | 9.86 ± 5.68 | — | — | |
Om4 | 12.6 ± 9.83 | 2.60 ± 1.35 | — | |
Om4 | 14.24 ± 8.38 | 13.50 ± 8.45 | — | |
Om4 | 22.54 ± 16.38 | 15.68 ± 8.54 | — |
Nematode species | Functional guild | Mean ± SD (abundance) | ||
---|---|---|---|---|
Predators | Zone ‘A’ Undisturbed forest (site for advance quarry) | Zone ‘B’ Spoil of median age | Zone ‘C’ Active site of mining | |
Ca5 | 12.22 ± 5.64 | 4.68 ± 2.52 | — | |
Ca4 | 11.22 ± 6.42 | 6.86 ± 6.36 | — | |
Ca4 | 22.60 ± 14.38 | 15.50 ± 8.46 | — | |
Ca4 | 12.68 ± 8.42 | — | — | |
Ca5 | 4.23 ± 6.69 | 9.40 ± 6.53 | — | |
Ca4 | 9.68 ± 4.38 | — | — | |
Ca5 | 16.46 ± 10.26 | 14.84 ± 5.21 | — | |
Ca5 | 12.45 ± 8.62 | 15.60 ± 8.64 | — | |
Ca4 | 10.12 ± 5.36 | 6.18 ± 2.48 | — | |
Ca4 | 15.99 ± 8.59 | 4.21 ± 3.26 | — | |
Ca4 | 18.62 ± 9.96 | 8.64 ± 4.42 | — | |
Ca4 | 16.45 ± 4.66 | — | — | |
Ca4 | 22.68 ± 6.68 | 15.21 ± 8.62 | — | |
Ca4 | 14.44 ± 8.64 | 11.64 ± 6.30 | — | |
Ca1 | — | 0.25 ± 3.36 | — | |
Ca4 | 9.66 ± 3.36 | 1.89 ± 2.06 | — | |
Ca4 | 23.45 ± 14.64 | 15.24 ± 11.42 | — | |
Ca4 | 26.20 ± 18.46 | 16.54 ± 8.44 | — | |
Ca5 | 6.48 ± 5.36 | 3.05 ± 2.58 | — | |
Ca4 | 16.28 ± 6.66 | 6.26 ± 5.88 | — | |
Ca5 | 8.35 ± 6.45 | 2.83 ± 1.26 | — | |
Ca4 | 8.32 ± 4.32 | — | — | |
Ca5 | 6.64 ± 7.38 | 4.21 ± 2.36 | — | |
Ca4 | 25.68 ± 44.61 | 10.58 ± 13.60 | — | |
Ca4 | 18.68 ± 12.68 | 5.36 ± 3.36 | — | |
Ca3 | 24.35 ± 18.38 | 32.26 ± 22.42 | — | |
Ca3 | 31.24 ± 24.24 | 20.25 ± 12.24 | — |
Type Area ‘A’ Non minning forest | Type Area ‘B’ Spoil of median age | Type Area ‘C’ Active site of mining | |
---|---|---|---|
Genera (total count) | 109 | 104 | 2 |
Species (total count) | 114 | 110 | 3 |
Individuals | 1748.63 ± 163.18 (1576–1859) | 983.80 ± 120.24 (748.57–1168.74) | 0.42 ± 0.37 (0.08–0.42) |
Margalef diversity | 16.17 ± 0.35 (15.58–16.79) | 15.11 ± 0.59 (14.23–16.23) | — |
Menhinick diversity | 3.92 ± 0.35 (3.63–3.95) | 3.43 ± 0.43 (2.85–3.98) | — |
Simpson dominance | 0.01 ± 0.00 (0.01–0.01) | 0.01 ± 0.00 (0.01–0.01) | — |
Inverse Simpson dominance | 91.14 ± 3.25 (82.25–96.35) | 67.50 ± 7.33 (54.32–76.15) | — |
Hill’s effective index | 98.23 ± 2.43 (97.24–99.89) | 75.64 ± 4.90 (65.18–77.89) | — |
Shannon diversity | 4.58 ± 0.45 (3.97–5.65) | 4.32 ± 0.44 (3.54–4.88) | — |
Simpson diversity | 0.99 ± 0.00 (0.99–0.99) | 0.99 ± 0.00 (0.99–0.99) | — |
Brillouin diversity | 4.51 ± 0.65 (3.85–5.78) | 4.19 ± 0.34 (3.50–4.60) | — |
Sheldon Index | 0.82 ± 0.00 (0.82–0.82) | 0.72 ± 0.00 (0.72–0.72) | — |
Heip Index | 0.82 ± 0.00 (0.82–0.82) | 0.72 ± 0.00 (0.72–0.72) | — |
Maturity Index (MI) | 3.46 ± 0.26 (3.36–3.87) | 2.96 ± 0.50 (2.87–3.12) | — |
Plant Parasitic Index (PPI) | 0.78 ± 0.09 (0.50–1.25) | 3.26 ± 0.23 (2.00–3.65) | — |
Trophic Diversity Index (TDI) | 1.17 ± 0.02 (1.06–1.32) | 1.09 ± 0.04 (1.04–1.25) | 1.00 ± 0.00 (1.04–1.25) |
Nematode channel ratio (NCR %) | 0.40 ± 0.02 (0.35–0.72) | 0.68 ± 0.02 (0.62–0.73) | — |
Structure Index (SI) | 68.23 ± 10.20 (58.30–77.43) | 45.1 5 ± 5.85 (40.68–52.68) | — |
Enrichment Index (EI) | 12.62 ± 4.66 (7.65–32.25) | 22.62 ± 12.58 (16.53–64.65) | 9.54 ± 1.54 (9.50–10.56) |
Basal Index (BI) | 41.28 ± 12.30 (32.04–62.05) | 57.29 ± 8.10 (44.24–67.35) | 74.46 ± 3.25 (70.13–78.16) |
Channel Index (CI) | 0.31 ± 0.40 (0.25–0.84) | 0.54 ± 0.42 (0.50–1.24) | — |
4.3.2 Zone ‘B’
4.3.2.1 Trophic groups
4.3.3 Zone ‘C’
4.3.3.1 Trophic group
4.4 Biomass
The relative biomass of different trophic groups (Figure 6) varied in three zones and are as follows:
5. Diversity indices
Diversity indices and nematode maturity indices were calculated for each zone to assess the diversity of nematode species and maturity of soil ecosystem.
5.1 Margalef index (species richness)
In Zone ‘A’ the Margalef species richness index was found to be 16.17 ± 0.35 (15.58–16.79). Zone ‘B’ was calculated to be 15.11 ± 0.59 (14.23–16.23) and in Zone ‘C’, where only two species were recorded, the index was incalculable (Table 7 and Figure 7).
Characteristics | Mining sites | ||
---|---|---|---|
Zone ‘A’ Undisturbed forest (site for advance quarry) | Zone ‘B’ Spoil of median age | Zone ‘C’ Active site of mining | |
<2.0 mm (gravel) | 9.00 ± 0.92 | 13.00 ± 1.80 | 20.00 ± 2.15 |
2.–0.2 mm (sand) | 63.00 ± 3.50 | 72.00 ± 5.24 | 88.55 ± 6.54 |
0.2–0.1 mm (silt) | 13.00 ± 1.23 | 10.00 ± 0.24 | 3.00 ± 1.26 |
<0.1 mm (clay) | 8.10 ± 1.45 | 7.80 ± 1.25 | 3.20 ± 1.56 |
pH | 6.54 ± 0.02 | 6.82 ± 0.02 | 5.45 ± 0.26 |
Bulk density | 1.25 ± 0.18 | 1.26 ± 0.08 | 1.75 ± 0.16 |
Natural moisture content (%) | 12.20 ± 2.26 | 11.60 ± 0.28 | 6.2 ± 0.25 |
Porosity | 46.27 ± 2.25 | 42.62 ± 2.65 | 33.65 ± 2.66 |
Water holding capacity | 53.00 ± 0.92 | 52.00 ± 2.65 | 24.84 ± 3.25 |
Soil organic carbon (mg C/g) | 3.45 ± 0.024 | 2.38 ± 0.028 | ND |
Total soil N (μg N/g) | 2456.63 ± 148.34 | 194.94 ± 25.46 | ND |
Exchangeable K μg P/g spoil | 271.95 ± 6.74 | 16.96 ± 2.35 | ND |
Electrical conductivity ms/cm | 0.05 ± .01 | 0.33 ± 0.01 | 0.65 ± 0.01 |
6. Evenness indices
The values for both the evenness indices (Sheldon and Heip indices) were observed to be the same for the two Zones ‘A’ and ‘B’ and calculated to be 0.82 ± 0.00 (0.82–0.82) and 0.72 ± 0.00 (0.72–0.72), respectively. For Zone ‘C’ the values were inestimable (Table 7).
7. Maturity index
In Zone ‘A’ where there was the least disturbance, the MI was highest and a mean value of 3.46 ± 0.26 (3.36–3.87) was observed representing the structured soil ecosystem. Zone ‘B’ which represented coal mine-managed spoil of 21 years period, showed an MI equal to 2.96 ± 0.50 (2.87–3.12) while in Zone ‘C’ MI was incalculable (Table 7 and Figure 7).
8. Plant parasitic index (PPI)
In Zone ‘A’ the PPI was calculated to be 0.78 ± 0.09 (0.50–1.25) whereas in Zone ‘B’ the PPI value was 3.26 ± 0.23 (2.00–3.65). The PPI and MI showed an inverse correlation (Table 7 and Figure 8).
9. Trophic diversity index
The value of trophic diversity index of Zone ‘A’ was 1.17 ± 0.02 (1.06–1.32), while those of Zone ‘B’ and Zone ‘C’ were 1.09 ± 0.04 (1.04–1.25) and 1.00 ± 0.00 (1.04–1.25), respectively (Table 8 and Figure 8).
Variables | Bac. Sp | Fung. Sp | Herb. Sp | Omi. Sp | Pred. sp. | MI | PPI | TDI | SI | EI | BI | CI | NCR | Tot. Indv. | pH | BD | Porosity | SM | WHC | ToC | TSN | Avail. K | EC |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Bac. Sp | 0.996 | 0.997 | 0.872 | 0.991 | 0.949 | 0.999 | 0.898 | 0.983 | 0.705 | −0.861 | 0.884 | 0.982 | 0.886 | 0.988 | −0.986 | −0.850 | 0.944 | 0.996 | 0.943 | 0.932 | 0.534 | −0.804 | |
Fung. Sp | 0.996 | 1.000 | 0.910 | 0.999 | 0.972 | 0.999 | 0.932 | 0.995 | 0.643 | −0.901 | 0.920 | 0.963 | 0.921 | 0.998 | −0.996 | −0.891 | 0.968 | 1.000 | 0.968 | 0.899 | 0.603 | −0.851 | |
Herb. Sp | 0.997 | 1.000 | 0.905 | 0.998 | 0.969 | 1.000 | 0.927 | 0.994 | 0.653 | −0.896 | 0.915 | 0.967 | 0.917 | 0.997 | −0.995 | −0.885 | 0.965 | 1.000 | 0.964 | 0.904 | 0.593 | −0.844 | |
Omi. Sp | 0.872 | 0.910 | 0.905 | 0.931 | 0.982 | 0.892 | 0.999 | 0.948 | 0.269 | −1.000 | 1.000 | 0.766 | 1.000 | 0.937 | −0.942 | −0.999 | 0.985 | 0.914 | 0.985 | 0.636 | 0.879 | −0.992 | |
Pred. sp. | 0.991 | 0.999 | 0.998 | 0.931 | 0.983 | 0.996 | 0.950 | 0.999 | 0.602 | −0.923 | 0.939 | 0.948 | 0.941 | 1.000 | −0.999 | −0.914 | 0.980 | 0.999 | 0.980 | 0.874 | 0.644 | −0.877 | |
MI | 0.949 | 0.972 | 0.969 | 0.982 | 0.983 | 0.961 | 0.991 | 0.991 | 0.445 | −0.978 | 0.986 | 0.873 | 0.987 | 0.986 | −0.988 | −0.973 | 1.000 | 0.974 | 1.000 | 0.770 | 0.774 | −0.951 | |
PPI | 0.999 | 0.999 | 1.000 | 0.892 | 0.996 | 0.961 | 0.916 | 0.990 | 0.675 | −0.882 | 0.903 | 0.974 | 0.905 | 0.994 | −0.992 | −0.871 | 0.957 | 0.999 | 0.956 | 0.916 | 0.569 | −0.828 | |
TDI | 0.898 | 0.932 | 0.927 | 0.999 | 0.950 | 0.991 | 0.916 | 0.964 | 0.321 | −0.997 | 1.000 | 0.800 | 1.000 | 0.955 | −0.959 | −0.995 | 0.993 | 0.935 | 0.993 | 0.678 | 0.852 | −0.984 | |
SI | 0.983 | 0.995 | 0.994 | 0.948 | 0.999 | 0.991 | 0.990 | 0.964 | 0.562 | −0.940 | 0.955 | 0.931 | 0.956 | 1.000 | −1.000 | −0.933 | 0.989 | 0.996 | 0.988 | 0.849 | 0.681 | −0.900 | |
EI | 0.705 | 0.643 | 0.653 | 0.269 | 0.602 | 0.445 | 0.675 | 0.321 | 0.562 | −0.247 | 0.291 | 0.825 | 0.295 | 0.588 | −0.576 | −0.226 | 0.432 | 0.636 | 0.429 | 0.914 | −0.223 | −0.145 | |
BI | −0.861 | −0.901 | −0.896 | −1.000 | −0.923 | −0.978 | −0.882 | −0.997 | −0.940 | −0.247 | −0.999 | −0.751 | −0.999 | −0.929 | 0.935 | 1.000 | −0.981 | −0.905 | −0.981 | −0.619 | −0.889 | 0.995 | |
CI | 0.884 | 0.920 | 0.915 | 1.000 | 0.939 | 0.986 | 0.903 | 1.000 | 0.955 | 0.291 | −0.999 | 0.781 | 1.000 | 0.945 | −0.950 | −0.998 | 0.989 | 0.923 | 0.989 | 0.654 | 0.868 | −0.989 | |
NCR | 0.982 | 0.963 | 0.967 | 0.766 | 0.948 | 0.873 | 0.974 | 0.800 | 0.931 | 0.825 | −0.751 | 0.781 | 0.783 | 0.942 | −0.937 | −0.737 | 0.866 | 0.961 | 0.864 | 0.983 | 0.367 | −0.678 | |
Tot. Indv. | 0.886 | 0.921 | 0.917 | 1.000 | 0.941 | 0.987 | 0.905 | 1.000 | 0.956 | 0.295 | −0.999 | 1.000 | 0.783 | 0.946 | −0.951 | −0.997 | 0.989 | 0.925 | 0.990 | 0.658 | 0.866 | −0.988 | |
pH | 0.988 | 0.998 | 0.997 | 0.937 | 1.000 | 0.986 | 0.994 | 0.955 | 1.000 | 0.588 | −0.929 | 0.945 | 0.942 | 0.946 | −1.000 | −0.921 | 0.983 | 0.998 | 0.983 | 0.866 | 0.657 | −0.886 | |
BD | −0.986 | −0.996 | −0.995 | −0.942 | −0.999 | −0.988 | −0.992 | −0.959 | −1.000 | −0.576 | 0.935 | −0.950 | −0.937 | −0.951 | −1.000 | 0.926 | −0.986 | −0.997 | −0.986 | −0.858 | −0.669 | 0.892 | |
Porosity | −0.850 | −0.891 | −0.885 | −0.999 | −0.914 | −0.973 | −0.871 | −0.995 | −0.933 | −0.226 | 1.000 | −0.998 | −0.737 | −0.997 | −0.921 | 0.926 | −0.976 | −0.895 | −0.977 | −0.602 | −0.899 | 0.997 | |
SM | 0.944 | 0.968 | 0.965 | 0.985 | 0.980 | 1.000 | 0.957 | 0.993 | 0.989 | 0.432 | −0.981 | 0.989 | 0.866 | 0.989 | 0.983 | −0.986 | −0.976 | 0.971 | 1.000 | 0.760 | 0.783 | −0.955 | |
WHC | 0.996 | 1.000 | 1.000 | 0.914 | 0.999 | 0.974 | 0.999 | 0.935 | 0.996 | 0.636 | −0.905 | 0.923 | 0.961 | 0.925 | 0.998 | −0.997 | −0.895 | 0.971 | 0.970 | 0.894 | 0.610 | −0.856 | |
ToC | 0.943 | 0.968 | 0.964 | 0.985 | 0.980 | 1.000 | 0.956 | 0.993 | 0.988 | 0.429 | −0.981 | 0.989 | 0.864 | 0.990 | 0.983 | −0.986 | −0.977 | 1.000 | 0.970 | 0.759 | 0.785 | −0.956 | |
TSN | 0.932 | 0.899 | 0.904 | 0.636 | 0.874 | 0.770 | 0.916 | 0.678 | 0.849 | 0.914 | −0.619 | 0.654 | 0.983 | 0.658 | 0.866 | −0.858 | −0.602 | 0.760 | 0.894 | 0.759 | 0.192 | −0.534 | |
Avail. K | 0.534 | 0.603 | 0.593 | 0.879 | 0.644 | 0.774 | 0.569 | 0.852 | 0.681 | −0.223 | −0.889 | 0.868 | 0.367 | 0.866 | 0.657 | −0.669 | −0.899 | 0.783 | 0.610 | 0.785 | 0.192 | −0.932 | |
EC | −0.804 | −0.851 | −0.844 | −0.992 | −0.877 | −0.951 | −0.828 | −0.984 | −0.900 | −0.145 | 0.995 | −0.989 | −0.678 | −0.988 | −0.886 | 0.892 | 0.997 | −0.955 | −0.856 | −0.956 | −0.534 | −0.932 |
10. Weighted faunal analysis
The indices calculated depended on weighted nematode indicator guilds [1, 12] to assess the level of organic enrichment (EI), the decomposition pathways (CI) (Table 8 and Figure 9), the basal/minimal level of resource utilization (BI) and the structured status or stability of ecosystem (SI). In Zone ‘A’ the structure index (SI) was highest i.e., 68.23 ± 10.20 (58.30–77.43), while in Zone ‘B’ the SI value was calculated to be 45.15 ± 5.85 (40.68–52.68) and in Zone ‘C’ the SI was zero. On the contrary, the enrichment index (EI) was calculated to be 12.62 ± 4.66 (7.65–32.25), 22.62 ± 12.58 (16.53–64.65) and 9.54 ± 1.54 (9.50–10.56) in Zone ‘A’, Zone ‘B’ and Zone ‘C’, respectively. The values of basal index (BI) for three different Zones were 74.46 ± 3.25 (70.13–78.16) in Zone ‘C’ followed by value of 57.29 ± 8.10 (44.24–67.35) in Zone ‘B’; lowest value of BI was observed in 41.28 ± 12.30 (32.04–62.05) in Zone ‘A’. The values of channel index (CI) in Zone ‘A’ and Zone ‘B’ were 0.31 ± 0.40 (0.25–0.84) and 0.54 ± 0.42 (0.50–1.24), respectively while CI was incalculable in Zone ‘C’ (Table 8 and Figure 10).
In faunal ordination graph between structure index and enrichment index, it was observed that in Zone ‘A’ the mean values were placed in quadrat ‘C’ whereas the mean values for Zone ‘B’ were at the interjunction of quadrat ‘A’ and quadrat ‘C’. In Zone ‘C’ the soil had almost no vegetation, low nutrient, and very little organic carbon (Figure 11).
11. Correlations among different variables
The Principal component analysis (PCA) was carried out and a correlation circle was retrieved (Figure 12), which depicted the correlations among various variables. Structure index (SI) showed a positive correlation with number of bacterivores species (r = 0.98, p < 0.05), fungivores (r = 0.99, p < 0.05), and herbivores (r = 0.99, p < 0.05), omnivores (r = 0.94, <0.05) and predators (r = 0.99, p < 0.05). Almost all the trophic groups showed a positive relationship with SI. Structure index also showed a positive correlation with PPI (r = 0.99, p < 0.05), pH (r = 1.00, p < 0.05), TDI (r = 0.96, p < 0.05), NCR (r = 0.93, p < 0.05) and MI (r = 0.99, p < 0.05). SI also depicted low positive relationship EI (r = 0.56, p < 0.05) and strong negative correlation with CI (r = 0.99, p < 0.05) and BI (r = −0.94, p < 0.05). EI showed strong negative correlation with CI and BI all at (p < 0.05). All trophic groups showed a positive correlation among themselves (p < 0.05) and also with PPI, pH, and MI. Among the trophic groups, only bacterivores showed robust positive correlation with EI (r = 0.70, p < 0.05). EI did not show any correlation with PPI, nonsignificant correlation with SI and significant positive correlation with MI. Soil organic carbon was significantly positively correlated with all trophic groups (p < 0.05) and show a negative correlation with electrical conductivity, porosity, basal index and bulk density (Table 8 and Figure 13).
In Biplot ordination graph the three Zones can be clearly differentiated with respect to biotic and abiotic variables and can be superimposed on the anthropogenic disturbances to assess its impact.
12. Discussion
Human activities disturb the soil ecosystem and affect soil nematode diversity [8, 23, 24, 25]. The effect is well reflected in present study where there is a significant impact on below-ground soil biodiversity with special reference to nematodes. The transition from aboveground plant heterogeneity in natural forests to extreme loss of vegetation due to mining activities is reflected in the changed community characteristics of soil nematodes and in their species diversity.
In Zone ‘A’, the number of species (species richness) was greater, but species dominance was low while in Zone ‘B’, an intermediate value of species richness with high species dominance of bacterial-feeders was recorded. These species
Although there was not a major difference between the total number of species of fungivores and herbivores in Zone ‘A’ and Zone ‘B’, the mean abundance of both the trophic groups was much high in Zone ‘A’. Despite the fact that stable ecosystems like Zone ‘A’ demonstrated species diversity and evenness, very often the species diversity has been reported to be greater in habitats subject to intermediate levels of disturbance because stochastic, intermediate (partial) elimination of resources by disturbance leads to species-specific mortality allowing the co-existence of competitively inferior species [33]. The combination of intermediate level of disturbance with intermediate productivity levels demonstrated a peak in species richness, not only due to periodic decreases of competitively dominant species but also to increased niche packing [34]. Structurally, complex environments thus provide more niches thereby increasing species diversity [35]. In conformity with the earlier reports on increased diversity at intermediate disturbance [36, 37, 38] and a positive relationship between habitat complexity and species diversity [39, 40, 41, 42, 43, 44], Zone B demonstrated similar status. It showed an intermediate level of disturbances and the species diversity too was somewhat closer to Zone A which represented undisturbed zone. Large mononchid and large dorylaimoid nematodes with higher
The maturity index of Zone ‘A’ Zone ‘B’ did not show much difference and could well indicate the status of Zone ‘A’ as structured and mature type of ecosystem and Zone ‘B’ as moderately structured and maturing type. Zone ‘C’ was obviously a highly disturbed region because of mining activities. These results agree well with those reported by Háněl [28] on coal mines.
The faunal profile results also corresponded with MI values of Zone ‘A’ and Zone ‘B’ as both reflected the dominant fungal decomposition pathways whereas Zone ‘C’ with disturbed and degraded food web demonstrated bacterial decomposition channels.
Although the present study has provided some pertinent information related to nematodes found in coal mine areas and the differences in nematode communities and their gradual succession in different overburdens or spoils, a detailed discussion on the role of individual species could not be done due to space constraint. Nevertheless, it is clearly evident that nematode assemblages can be evaluated and can serve as excellent tools for environmental monitoring or environment quality assessment. The study has opened up avenues for more studies to be conducted in coal mine areas using nematodes as models. Also, future studies in this direction may further vouch for comparison and may indicate any specificity or association of nematode taxa to coal mine areas. Such information may also have predictive value about the specificity and occurrence of species in degraded habitats, early successional and late successional stages to undisturbed habitats and can be used in modeling and predicting future changes in biodiversity and species interactions with land use changes.
13. Conclusion
In conclusion, this study highlights the significant impact of human activities on soil nematode diversity, particularly in the context of mining activities. The transition from natural forests to mining sites results in notable changes in soil nematode communities and species diversity.
In Zone ‘A’, which represents undisturbed natural forests, there is a higher species richness and lower species dominance among nematodes. In Zone ‘B’, which is a reclaimed coal mine spoil with some soil enrichment measures, there is an intermediate level of species richness but a higher dominance of bacterial-feeders. These nematode species in Zone ‘B’ exhibit tolerance to environmental stress and anthropogenic disturbances. On the other hand, Zone ‘C’, an actively mined area with constant disturbances and little organic matter, contains only a few nematode species, primarily enrichment opportunists with a high tolerance for mineral and industrial waste materials.
The study also suggests that intermediate levels of disturbance, as seen in Zone ‘B’, can lead to increased species diversity due to periodic decreases of dominant species and increased niche packing. Habitat complexity, as observed in both Zone ‘A’ and Zone ‘B’, also contributes to higher species diversity.
The maturity index values of Zone ‘A’ and Zone ‘B’ indicate structured and mature ecosystems, while Zone ‘C’ represents a highly disturbed and degraded region due to mining activities. The faunal profile results align with the maturity index values, with Zone ‘A’ and Zone ‘B’ dominated by fungal decomposition pathways and Zone ‘C’ characterized by bacterial decomposition channels.
While this study provides valuable insights into nematode communities in coal mine areas, further research is needed to explore the roles of individual nematode species in these ecosystems. Nematodes can serve as excellent indicators for environmental monitoring and assessing environmental quality. Future studies in this area may reveal specific associations of nematode taxa with coal mine areas, aiding in biodiversity modeling and predicting how species interactions change with land use alterations. This research opens the door to a deeper understanding of the impact of human activities on soil ecosystems and the potential for ecological restoration efforts.
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