Diversity of arbuscular mycorrhizal fungi (Glomeromycota) in adjacent areas of
different land use in Nepal
Kuber Baral 1, Anjana Giri 2, Pradeep Kumar Shah 1, Karl Kemmelmeier 3, Sidney Luiz Stürmer 3, Sita Gyawali 4
and Jay Kant Raut 2, *
1
Tri-Chandra Multiple Campus, Department of Microbiology, Ghantaghar, Tribhuvan University, Kathmandu, Nepal.
Nepal Academy of Science and Technology, Khumaltar, Lalitpur, Nepal.
3 Universidade Regional de Blumenau, Departamento de Ciências Naturais. 89030-903 Blumenau, SC, Brazil.
4 Central Department of Botany, Tribhuvan University, Kathmandu, Nepal.
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GSC Biological and Pharmaceutical Sciences, 2021, 15(01), 141–150
Publication history: Received on 01 March 2021; revised on 23 April 2021; accepted on 25 April 2021
Article DOI: https://doi.org/10.30574/gscbps.2021.15.1.0098
Abstract
Disturbances can affect the incidence of Arbuscular Mycorrhizal Fungi (AMF) in both agricultural and natural
ecosystems. The present study is a first attempt for the qualitative assessment of AMF diversity in adjacent areas of a
forest ecosystem with different land uses and assess levels of mycorrhizal colonization by these fungi. A total of five soil
samples were taken randomly from each of the following areas situated within the same landscape: undisturbed
coniferous forest (UF), degraded forest (DF) and cultivated land (CL). A total of 22 taxa of arbuscular mycorrhizal fungi
belonging to eight genera were identified morphologically, Glomus and Acaulospora being the most common. Species
richness ranged from 11-14 among land use areas, with 14 species in UF and 11 species in CL. Acaulospora mellea,
Gigaspora sp. and two non-identified Glomus species were detected in all areas. While species richness did not differ
significantly amongst areas, diversity at the family level was 43% less in CL than in UF. Mean mycorrhizal colonization
was higher in DF (28%) than CL (20%). We concluded that land use mainly affected fungal diversity only at the family
level and had no impact on mycorrhizal development in sampled roots. This work provides the first step to identify
native AMF species in Nepal that might be cultured for further use by small farmers in a sustainable agriculture
approach.
Keywords: Disturbance; Edaphic factors; Glomeromycota; Coniferous forest; Avena sativa; Soil properties.
1. Introduction
Arbuscular Mycorrhizal Fungi (AMF – phylum Glomeromycota) are known to have a key role in terrestrial ecosystems
as they contribute to improve plant nutrition, particularly uptake of low mobility nutrients from soil solutions such as
P, Zn, and ultimately Cu, to increase plant resistance to drought, salinity and tolerance to pathogens and to improve soil
structure [1, 2]. However, disturbances can affect several aspects of AMF communities in both agricultural and natural
ecosystems through the process of limiting organic inputs into the soil and biomass removal [3, 4]. AMF establish the
arbuscular mycorrhizal symbiotic association with 72% of vascular plants [5] and therefore are ubiquitous soil
organisms accounting for 5-36 % of the total biomass in the soil and 9-55 % of the biomass of soil microorganisms [6].
Establishing an interface between soil and plant roots, AMF are sensitive to changes in soil and plant environment.
The AMF community varies greatly in size and species composition in different habitats due to differences in edaphic,
climatic and host factors that determine sporulation and root colonization in a particular place [7]. Composition of AMF
community [8], fungal composition in plant roots [9], fungal phospholipids in soil [10], and amount of extra radical
Corresponding author: Jay Kant Raut
Nepal Academy of Science and Technology, Khumaltar, Lalitpur, Nepal.
Copyright © 2021 Author(s) retain the copyright of this article. This article is published under the terms of the Creative Commons Attribution Liscense 4.0.
GSC Biological and Pharmaceutical Sciences, 2021, 15(01), 141–150
mycelium [11] are the AMF variables which are affected by agricultural practices. Although different host plants show
differential affinities for distinct AMF species due to which wider range of host plants might promote greater AMF
diversity compared with monoculture [12], these effects are context dependent and vary across soil types, ecosystems,
and precipitation regimens, etc. [13]. Plant species distribution, land management practices and long-term application
of phosphorous fertilizer impact distribution of AM fungal species [14, 15, 16, 17]. Land use change and/or disturbance
of soil negatively affect the functionality of AM fungi reducing mycorrhizal colonization [18].
Exploiting of natural forests turning them in cultivable lands or degraded forests causes changes in which plant species,
soil organic matter, soil nutrients, soil structure, and soil fungi may be affected [1]. The cultivable land is cleared of multi
species of plants and normally planted with a single species of one age-class. This constitutes a drastic site disturbance
which alters mycorrhizal abundance and species composition in the site. Agricultural management factors in cultivable
land such as the intensity of cultivation, the quality and quantity of fertilizers applied and the plant protection strategies
used in modern agriculture have severely affected AMF community structure and plant interactions [19]. After
disturbance of some Australian sites, decrease in spore number as well as shift in species composition was occurred
[20]. Similarly, AMF species composition and abundance are affected by vegetation cover [21, 22, 23]. They also noticed
a change in species composition. The removal of host plants, the soil disturbance, and compaction associated with land
clearing are detrimental to AM propagules [24].
In Nepal, global climate change and human activities such as overgrazing, harvesting of fodder, and unsustainable
agricultural practices are causing dynamic change in the land use pattern. The land use practices affect chemical,
physical and biological properties of soil [25], however the biological properties of soil are rarely considered for
agriculture. Soil in Nepal is deficient in N, P, and K due to shortage of organic matter in the soil [26]. However, farmers
who have been using chemical fertilizer in Kathmandu valley and some of the Terai districts have started to experience
its adverse effects on soil quality [26]. Therefore, for the mitigation of these effects, farmers started using compost
manures, green manures, integration of legumes in the cropping system, use of farm yard manure (FYM), homemade
botanical pesticides, among other practices in their agricultural crops. Up to now, no investigation has been carried out
in Nepal to elucidate how AMF communities and mycorrhizal colonization varies according to changes among land use
systems within the same landscape and how these changes relate with edaphic factors. Moreover, no surveys of AMF
species have been done in Nepal, despite its territory spans biomes like tropical grasslands, tropical moist forests,
tropical and temperate conifer forest and montane grasslands. These studies are important to understand whether AMF
communities are being affected by changes from native to agricultural systems and to provide subsidies to include AMF
communities as important components to assess the effects of land use changes and as another biological tool for
farmers to improve production. Our aim in this study was to determine the variation of AMF communities and levels of
mycorrhizal colonization along distinct land use areas occupying the same landscape.
2. Material and methods
2.1. Study area
The study sites were located in Bhaktapur district, the smallest of seventy-seven districts of Nepal, with an area of 119
km2 located in the eastern part of Kathmandu valley. The average annual temperature in Bhaktapur is 17.9°C and rainfall
is about 1,583 mm. June is warmest with temperatures averaging 23.2°C and January is the coldest. Main economic
activities in the district are animal husbandry and agriculture which is accelerating land use, a special concern as
Bhaktapur is one of the top ten districts of Nepal with only 25 km2 of forest.
Three areas impacted to different degrees by human activities were selected to assess AMF community composition:
undisturbed forest (UF), degraded forest (DF), and cultivated land (CL). All of these sites were located adjacent to each
other in same landscape (Figure 1). UF is a dense coniferous forest situated at the top of the landscape where grazing
and cutting fodders for cattle were prohibited while the DF site is a disturbed forest located adjacent to the UF and
impacted by local people’s activities (e.g. extraction of timber, animal husbandry, agriculture).
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Figure 1 Sampling sites
a: Map of sampling site; b: Landscape view; c: Undisturbed forest; d: Degraded forest; e: Cultivated land
Pinus roxburghii Sarg. Alnus nepalensis D. Don, Toona ciliata M. Roem., Schima wallichii (DC.) Korth., Rhododendron
arboreum Sm., Nephrolepis exaltata (Linn.) Schott, Eupotorium adenophorum Spreng. and Arundinella nepalensis Trin.
were dominant on UF while Pinus roxburghii Sarg., Alnus nepalensis D. Don, Ilex opaca Soland. ex Ait., Arundinella
nepalensis Trin., Digitaria longiflora (Retz.) Pers, and Eupotorium adenophorum Spreng. were on DF. CL is cultivable land
located at base of the landscape which is planted with different crops according to season. Oats (Avena sativa L) were
being cropped at the sampling time. Geographical information and soil properties for each site are summarized in Table
1.
Table 1 Description of the study sites.
Land use types
Properties
UF
DF
CL
Latitude
E 85˚27ʹ13.35ʺ
1708 m
N 27˚38ʹ41.76ʺ
E 85˚27ʹ13.74ʺ
Altitude
N 27˚38ʹ20.72ʺ
E 85˚27ʹ9.78ʺ
1487 m
N 27˚38ʹ50.34ʺ
1409 m
Soil type
Clay loam
Clay loam
Clay loam
Soil moisture
22.13±2.49
14.56±3.78
12.76±1.54
Soil pH (H2O)
5.07 ± 0.088
4.83 ± 0.033
4.9 ± 0.15
EC (µS)
277.33 ± 24.86
172.90 ± 6.76
166.67 ± 4.77
Carbon %
2.08 ± 0.24
1.99 ± 0.15
1.88 ± 0.14
Nitrogen %
0.10 ± 0.01
0.10 ± 0.0058
0.09 ± 0.0067
Phosphorous (mg/ kg)
14.69 ±0.53
0.46 ± 0.0
82.89 ± 36.9
Potassium (mg/kg)
121.15 ± 12.2
93.26 ± 20.10
183.9 ± 38.2
Longitude
Data are reported as (mean ± SEM) for replicate samples; UF: undisturbed forest; DF: degraded forest;
CL: cultivated land with Oat (Avena sativa); pH: percentage of hydrogen ion; EC: electrical conductivity
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2.2. Sampling procedure
In each land area, five soil samples (ca. 1 kg) were randomly collected from January to September 2019 up to a depth of
20 cm using a soil corer (Moreira et al. 2015). Only few samples were taken in this study in spite of diverse landscape
of UF and DF since it was a preliminary work to assess diversity of AMF. Soil samples were placed in zip locked polythene
bags, labeled, transported to the laboratory and stored at 4℃ until they were processed.
Large soil aggregates were crushed gently and root pieces were picked separately using a forceps. Around half of each
preserved sample was spread separately on paper trough to allow air dry for physical and chemical analysis of soil and
other half was used for identification of AMF. Then, the samples were sieved separately through 2000 μm sieve to
discard larger soil aggregates and organic debris.
2.3. Physical and chemical analysis of soil
An aliquot of 250 g of air-dried soil sample was used to determine carbon (Walkley and Black method), total nitrogen
(Kjeldahl’s method), available phosphorous (Olsen’s method), and potassium (neutral normal ammonium acetate
method). A soil suspension of 1:2.5 (soil-water mixture) was made through intermittent stirring for measurement of pH
and electric conductivity of the soil samples [27]. Soil moisture was measured by weight after 20 g samples were
incubated at 105℃ for 24 hours in hot air oven (Table 1). Soil moisture percentage was calculated using the following
equation:
Soil moisture (M) =
mass of moist soil
2.4. Assessment of the root colonization
mass of dry soil
× 100%
Roots from each soil sample were cut into approximately 1 cm pieces and a 0.5 g subsample was placed in labeled
perforated plastic cassettes and washed. Cassettes were incubated in 10% KOH solution and autoclaved at 15 psi and
121°C for 15 min. After rinsing with tap water, pigmented root pieces were immersed in alkaline H2O2 at room
temperature for 10 to 20 min or until roots were bleached. Alkaline H2O2 was prepared by adding 3 ml of 0.5% NH4OH
to 30 ml of 10% H2O2 and 567 ml of tap water. Cassettes then were thoroughly rinsed and covered with 2% HCl for 3-4
min. Acidified roots were stained with 0.05% trypan blue in lactoglycerol solution by incubation in a water bath at 95°C
for 20 minutes. Excess stain was removed using 50% glycerol.
The stained pieces of roots (around 50 to 100) from each sample were scattered on a petri plate and observed under
stereomicroscope (OLYMPUS SZ2-ILST) at 10×10 magnification. The root pieces were counted as colonized and noncolonized and results expresses in percentage of mycorrhizal colonization.
2.5. Spore extraction, purification and identification
Spores were extracted from 100 g of air-dried soil sample by wet sieving and decanting [28] using two nested sieves of
100 μm and 45 μm openings. Material retained in these sieves were transferred to a 60% sucrose solution and
centrifuged. The layer containing spores was decanted into a petri dish. Spores were separated based on shape, size and
color under a dissecting microscope (OLYMPUS SZ2-ILST). Spores of similar phenotypes were grouped and mounted in
slides with polyvinyl lacto-glycerol (PVLG) and PVLG with Melzer’s reagent (1:1). Mounted spores were observed under
compound trinocular microscope (OPTIKA B-383PLi) and photographs were taken in different magnifications with an
OPTIKA 4083.13E HDMI Easy camera. Spores were identified by comparison with descriptions presented on webpages
of the International Culture Collection of Vesicular Arbuscular Mycorrhizal Fungi (INVAM) (www.invam.wvu.edu) and
by comparison with published descriptions. The classification of Redecker et al. [29] was followed for this analysis.
3. Results
A total of 22 spore morphotypes belonging to eight genera were extracted from the soil samples of different land use
systems, of which nine were identifiable only to genus (Table 2, Figure 2). Species richness ranged from 11-14 in
different land use systems, with 14 species registered in UF and 11 species in CL (Table 2). Acaulospora mellea,
Gigaspora sp1, Glomus sp1, and Glomus sp2 were recovered from all land use systems. Ambispora cf. leptoticha, Pacispora
sp1, and Rhizophagus intraradices were found exclusively in UF, Ambispora cf. gerdemannii, Ambispora cf. reticulata,
Acaulospora sp1, Acaulospora sp2, and Paraglomus cf. occultum were detected exclusively in DF while Acaulospora
morrowiae was identified only from the CL (Table 2).
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Figure 2 Spores of arbuscular mycorrhizal fungal species identified in three land use systems in Bhaktapur district,
Nepal, and mycorrhizal structures
a. Ambispora cf. gerdemannii; b. A. cf. reticulata; c. A. cf. leptoticha; d. Acaulospora cf. alpina; e. Ac. delicata; f. Ac. mellea; g. Ac. morrowiae;
h. Ac. scrobiculata; i. Acaulospora sp1; j. Acaulospora sp2; k. Pacispora sp1; l. Gigaspora sp1; m. Gigaspora sp2; n. Claroideoglomus etunicatum;
o. Glomus cf. ambisporum; p. Glomus sp1; q. Glomus sp2; r. Glomus sp3; s. Rhizophagus clarus; t. R. intraradices; u. Paraglomus cf. occultum;
v. Paraglomus sp1; w. Root cells with vesicle; x. Root cells with arbuscules. Bar 30 μm
The family with the highest number of species recorded was Acaulosporaceae (7) followed by Glomeraceae (6),
Ambisporaceae (3), Gigasporaceae (2), and Paraglomeraceae (2). Claroideoglomeraceae and Pacisporaceae were
represented by only one species each (Table 2). Considering the number of species per family in each land use system,
Glomeraceae predominates in UF with 27.27% while Acaulosporaceae predominated in DF and CL with 22.73%.
3.1. AM fungal root colonization
Root pieces from soil samples of all land use showed evidence of arbuscular mycorrhizal colonization by the presence
of typical structures like arbuscules, hyphae, and vesicles (Figure 2). Colonization levels were similar in DF and UF
(28%), and slightly lower in CL (20%). Mycorrhizal colonization did not differ significantly (p >0.05) amongst the land
use areas.
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Table 2 Families and species of arbuscular mycorrhizal fungi recovered from undisturbed forest (UF), degraded forest
(DF), cultivated land (CL) in Bhaktapur district, Nepal.
Family/ AMF species
UF
DF
CL
Ambisporaceae
Ambispora cf. gerdemannii (Rose, Daniels & Trappe) Walker,
Vestberg & Schüßler
×
Ambispora cf. reticulata Oehl & Sieverd.
×
Ambispora cf. leptoticha (Schenck & Sm.) Walker, Vestberg &
Schüßler
×
Acaulosporaceae
Acaulospora cf. alpina Oehl, Sýkorová & Sieverd.
×
Acaulospora delicata Walker, Pfeiffer & Trappe
Acaulospora mellea Spain & N.C. Schenck
×
×
×
×
×
×
Acaulospora morrowiae Spain & Schenck
×
Acaulospora scrobiculata Trappe
×
Acaulospora sp1
×
Acaulospora sp2
×
×
Pacisporaceae
Pacispora sp1
×
Gigasporaceae
Gigaspora sp1
×
×
×
Gigaspora sp2
×
×
×
×
Glomus cf. ambisporum Sm. & Schenck
×
×
Glomus sp1
×
×
×
Glomus sp2
×
×
×
Glomus sp3
×
×
Rhizophagus clarus
×
×
R. intraradices (Schenck & Sm.) Walker & Schüßler
×
Claroideoglomeraceae
Claroideoglomus etunicatum (Becker & Gerd.) Walker & Schüßler
Glomeraceae
Paraglomeraceae
Paraglomus cf. occultum (Walker) Morton & Redecker
×
Paraglomus sp1
×
Number of species
14
×
13
11
4. Discussion
In this study, we report species of arbuscular mycorrhizal fungi (AMF) based on spore morphology in different land
uses in Nepal. Acaulosporaceae and Glomeraceae in all land uses is not surprising since it was previously shown that
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Glomus and Acaulospora species are most abundant AMF in tropical areas [30, 31, 32]. Presence of these genera also
was reported from high elevation regions with harsh climatic condition and soil with pH lower than 5 [33]. Dominance
of Acaulosporaceae could be in all land use systems, as members of this family tend to be more prevalent in lower pH
soils [< 5.0; 34]. The distribution of Glomeraceae in all land use systems could be partly the result of high tolerance to
environmental factors and strong mycelial networks within plant communities hypothesized to be traits exhibited by
members of this family [35, 36].
In spite of some non-endomycorrhizal plants on UF and DF, the higher species richness in the forests than in cultivated
land may be associated with the presence of plant diversity in the undisturbed forest compared to DF and CL. According
to [37] a positive relationship between AMF and plant diversity was occurred. Higher diversity of rhizospheric AMF
may occur in natural habitats [38, 39] compared to that in agricultural ecosystems [40, 41, 42]. The decline of species
richness in CL compared to that in UF supports such pattern.
Sporulation is not likely representative of total AMF diversity in each community. Diversity of host plants impacts on
timing and abundance of sporulation, and the environment at the time of sampling is a huge factor. Potential drivers of
AMF diversity and community structure may include plant community composition [43] and environmental factors
such as soil organic carbon [44], soil phosphate [45], and soil texture [46]. Apart from these specific environmental
factors, direct land use-related circumstances such as land-use intensity and tillage have also been suggested as primary
determinants of AMF community composition [8, 42, 47]. Land use conversion and farming practices may impact the
occurrence of AMF in multiple ways, such as changing above-ground vegetation, altering soil properties and increasing
soil disturbance [48].
Composition of AM fungal community and mycorrhizal root colonization largely depends on content of organic matter,
pH of the soil, and water content in the soil [49]. The soil properties can have a significant effect on the population of
AMF spores in the soil, irrespective of geographical location, soil cultivation system, and plant density [50], as we found
in this study despite the small sample size (15 from three land areas). The DF lies on a steep part of the landscape, which
is favorable for erosion of the soil layer with higher phosphorous status so amount of available phosphorous in DF may
be too low compared to other land uses.
This study contributed to our knowledge on the biogeography of arbuscular mycorrhizal fungi from a country that has
not been previously surveyed for these fungi. Moreover, considering the role of AMF in improving plant growth and
nutrition and impacting soil properties, this inventory is a first step to identify potential species that can be isolated and
further used by local farmers. Using locally adapted fungi has a high potential for local farmers to reduce their
dependency on imported chemical fertilizers and pesticides, turning agriculture more sustainable and environmental
friendly.
5. Conclusion
A relatively high number of AM species were found in different land use system in Nepal. AMF species richness varied
only slightly among the different land uses, with the greatest differences at the family level. As would be expected from
the limited sampling regimen, land use or edaphic variables impacted on variation in mycorrhizal colonization.
Compliance with ethical standards
Acknowledgments
We are very much thankful to Department of Microbiology, Tri-Chandra Multiple Campus, Ghantaghar, Kathmandu and
Bioresource Lab, Nepal Academy of Science and Technology (NAST), Khumaltar, Lalitpur for providing us appropriate
facilities to complete this work. We would like to thank Dr. Buddhi Ratna Khadge and Ms. Jaishree Sijapati for kind
cooperation to initiate our work in NAST.
We also like to thank Dr. Deepa Dhital (Himalayan Seed Bank) and Dr. Tirtha Raj Ghimire (Animal Research Laboratory)
for providing microscopic facility. We also thankful to Dr. Tista Prasai Joshi (Environment Research Laboratory),
Departments of Analytical Chemistry and Molecular Biotechnology of NAST for providing equipments needed in our
work. SLS thanks the Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq, Brazil) for a Research
Assistanship (Process 307.995/2019-4).
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Disclosure of conflict of interest
The authors disclose that there is no conflict of interest.
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