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Proceeding Paper

Diversity of Arbuscular Mycorrhizal Fungi Associated with Maize in the Eastern Part of Uganda †

by
Abdoulaye Fofana Fall
1,2,*,
Grace Nakabonge
3,
Joseph Ssekandi
4,
Hassna Founoune-Mboup
5,
Arfang Badji
6,
Issa Balde
1 and
Malick Ndiaye
2
1
African Center of Excellence in Agroecology and Livelihood Systems, Faculty of Agriculture, Uganda Martyrs University, Kampala P.O. Box 5498, Uganda
2
Department of Plant Biology, Universite Cheikh Anta Diop de Dakar (UCAD), Dakar P.O. Box 5005, Senegal
3
College of Agriculture and Environmental Sciences, Makerere University, Kampala P.O. Box 7062, Uganda
4
Department of Agricultural Sciences, Faculty of Agriculture and Environmental Sciences, Kabale University, Kabale P.O. Box 317, Uganda
5
Institut Senegalais de Recherche Agricole (ISRA_LNRPV), Laboratoire National de Recherches sur les Productions Végétales (LNRPV), Dakar P.O. Box 3120, Senegal
6
Department of Agricultural Production, Makerere University, Kampala P.O. Box 7062, Uganda
*
Author to whom correspondence should be addressed.
†
Presented at the 2nd International Electronic Conference on Diversity (IECD 2022)—New Insights into the Biodiversity of Plants, Animals and Microbes, 15–31 March 2022; Available online: https://sciforum.net/event/IECD2022.
Biol. Life Sci. Forum 2022, 15(1), 12; https://doi.org/10.3390/IECD2022-12351
Published: 14 March 2022
(This article belongs to the Proceedings of The 2nd International Electronic Conference on Diversity (IECD 2022)—New Insights into the Biodiversity of Plants, Animals and Microbes)
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Abstract

:
Improving maize yield is an objective of utmost importance for food security in Uganda. In the evaluation of soil microorganisms in crop production, it is important to assess the composition and diversity of the arbuscular mycorrhizal fungi (AMF) species in different agroecosystems. AMF play an important role in improving crop growth and yield. We present a study of the morphological diversity of native AMF species associated with the rhizosphere of maize in two locations in eastern Uganda (the Amuria and Serere districts). The effects of soil chemical properties on this diversity are also assessed. AMF diversity is assessed by the morphological identification of the spores extracted from soils samples by the wet sieving method. Spores abundance, species richness, and diversity are determined. A total of 19 AMF morphotypes distributed in 7 genera (Gigaspora, Scutellospora, Glomus, Acaulospora, Archaeospora, Entrophospora, and Paraglomus) are observed. Glomus species are abundant in all sites. Spore densities are higher in Amuria than in Serere. Soil pH, CEC, and phosphorus content influence AMF distribution. Finding the species in various agroecological environments indicates that they are adapted to the environments. Maize grown in eastern Uganda is associated with a diversity of AMF that could be selected as bio-fertilizers to improve crop production.

1. Introduction

Maize (Zea mays L.), a tropical cereal crop, is one of the most economic and nutritional cereals grown in the African continent. It is used as a staple food and as livestock feed, and also in industrial production (biofuel) [1]. In sub-Saharan Africa (SSA), particularly in the eastern region, maize is the main source of carbohydrates and protein that contribute to populations’ food security [2]. Its dry grains contain a high level of carbohydrate (73%), protein (9.1–14%), and oligo-elements such as iron and zinc [3,4]. In addition, another important beneficial attribute of this cereal is that it is particularly adapted to regions of limited rainfall (under 600 mm per year), and those that are sub-humid to semi-arid (1000–1500 mm per year). In Uganda, it is the most important cereal crop; it accounts for 16% of caloric intake and, per capita, maize consumption ranges from 28 to 125 kg per annum [5]. Maize is planted in all agroecological zones in Uganda, but more intensely in the eastern region (Mbale, Jinja, Iganga, and Teso sub-regions). More than 90% of Uganda’s maize is produced by small-hold farmers, of which about 60% of the annual production is consumed on the farm, and it is generally managed with low- or zero-input technology, due to the capacity of farmers in buying chemical fertilizers [6]. It is reported that 2.9 million tons of maize grain were produced in 2018, but this level of production is largely below the national demand [7]. Constraints limiting maize production in Uganda include pests and diseases [8], as well as low soil fertility and erratic rainfall pattern [9]. The challenge of the National Agricultural Research Organization (NARO) in Uganda is the improvement of maize production using new, affordable, and sustainable technologies, contributing to maintaining biodiversity and preserving the environment. It is proven that the soil microbiota has an important role in the development of sustainable agriculture [10]. Among the key microbial communities developing in the rhizosphere are arbuscular mycorrhizal fungi (AMF). This ancient group of fungi is composed of obligate symbionts forming associations with a large majority of plant species (about 72% of terrestrial plant species) [11]. Several studies report on their roles in mineral nutrition and water supply of plants, as well as the effects on improving plant resistance to abiotic and biotic stresses [12,13]. Thus, AMF is used in agriculture to increase crop yields while reducing the application of chemical fertilizer inputs [14]. Numerous studies in Senegal and Kenya show substantial yield increases through long-term mycorrhizal inoculation [15,16]. The selection of efficient production of biofertilizers in quality and quantity are critical issues for the application of AMF technology in agricultural production in Africa. The use of indigenous mycorrhiza from soil has many benefits in restoration schemes, such as their high level of adaptation to local conditions and low ecological risk. However, little is known about native AMF associated with annual crops in fields in Uganda. The first study on mycorrhizal symbiosis in Uganda was conducted on bananas in 2001 by Msiska [17]. One recent study helped to identify the diversity of AMF in Soroti (Uganda) based on spore morphology [18]. Spores are one of the most important and convenient characteristic features, and they can help research in the rapid identification of mycorrhizae, faster than sequence techniques. Many studies reveal that spore morphology is necessary when working on AMF. About 150 AMF species were described employing morphological features of spores. Though several studies were carried out on the use of AMF in crop yield, studies on the morphological diversity of AMF are almost missing in Uganda. To the best of our knowledge, no information is available on the morphological diversity of AMF associated with maize crops grown in East African fields. Hence, the present work was conducted to find out the morpho-types of arbuscular mycorrhizal fungi associated with maize (Zea mays) in eastern Uganda. This study is probably one of the first to assess the diversity of AMF associated with the rhizosphere of maize in East Africa. The results obtained provide background information on the indigenous AMF associated with maize, and are a necessary step towards forecasting the integration of AMF biofertilizer in improving grain yields.

2. Materials and Methods

2.1. Study Area

This study arose from the need to achieve a long-term objective: to improve maize production in Uganda by using the diversity of native arbuscular mycorrhizal fungi associated with maize rhizosphere. The study areas were the Amuria and Serere districts, as depicted in Figure 1. The Serere district is located in eastern Uganda, in the Teso sub-region, and covers approximately 1965 km2 [19], with an elevation about 1095 m above sea level [20]. The Amuria district is also situated in the Teso sub-region, and covers a surface of 2588 km2, with an elevation of 1096 m above sea level. The area experiences a humid and hot climate, receiving bimodal rainfall, with an annual average of 1350 mm, between March and May. There are decreasing light showers between June and August, and heavier rains again between September and November. The dry season begins in December and lasts until February. The climate of the sub-region is modified by the large swamp wetland area that surrounds it. The minimum temperature is 18 °C and the maximum temperature is 31.3 °C. However, extremes usually occur in February, when the temperature can exceed 35 °C. Teso land slopes from east to west, and lies at a lower altitude than the Karamoja highlands and Sebei uplands sub-regions of Uganda, thereby receiving water discharges [21]. The economic activities in the sub-region are based on subsistence agriculture and livestock rearing. Farmers grow a diversity of crops, especially legumes and cereals including millet, sorghum, rice, and maize.

2.2. Soils Sampling and Analysis

Soils were sampled from maize fields, at the end of the rainy season in December 2021. Cores were collected from 20 random points, and the soils were pooled to obtain representative bulk samples. Samples were collected from between 2–30 cm in depth by removing the top 2 cm of soil and excavating maize rhizosphere soil. The fields selected were active, experimental, conventionally managed fields in maize cultivation, and had been used for multiple seasons. The soils were then placed in a zip-lock freezer bag and kept at 4 °C until their utilization. Soil samples from the fields were analyzed in Makerere University lab (Uganda), according to the procedure described by [22]. The soil samples were air-dried and used for the determination of physical and chemical properties including soil texture, pH, organic carbon (C), total nitrogen (N), total phosphorus (P), available phosphorus (P), and the CEC.

2.3. Extraction, Enumeration, and Morphological Identification of AMF Spores

Maize rhizosphere soils collected were wet-sieved and sucrose-centrifuged to extract AMF spores, following the method described by [23]. In summary, 100 g of rhizosphere soil was suspended in 1000 mL tap water, stirred for 1 min, and the solutions were sieved sequentially through 400, 200, 100, and 50 µm sieves under flowing tap water, to separate the spores according to their size. The soil fraction in each sieve was collected into the beaker. Then, spore suspensions were transferred to 50 mL centrifugation tubes and centrifuged with a water–sucrose solution (20% and 60% w/v) for 5 min at 4000 rpm [24]. The supernatant was decanted into a 32 µm sieve, washed, and transferred to Petri dishes for quantification under binoculars, and grouped according to their morphological characteristics (spore size, color, and hyphal attachment). The spore density was expressed as the total number of spores per 100 g of soil [25]. Some spores morphotypes were mounted on slides in polyvinyl–lactic acid–glycerine (PVLG) and a mixture of PVLG with Melzer’s reagent (1:1; v/v) (Brundrett et al., 1996), to observe wall structures and other specific attributes using a compound microscope at 400× magnification (Motic, MIPLUS20). Then, the spores were identified based on descriptions and identification criteria presented on the International Culture Collection of Vesicular–Arbuscular Mycorrhizal Fungi website (http://fungi.invam.wvu.edu/the-fungi/species-descriptions.html (accessed on 20 January 2022), and on the descriptions in the literature. Morphotypes were classified to the genus level and, when possible, to the species level, according to the current valid taxonomy [26].

2.4. AMF Roots Colonization Measurement

Capillary root segments were cleaned in 10% KOH solution for 20 min at 90 °C in a bain-marie, then rinsed with water several times using mesh and forceps, and acidified with 1% HCI solution for 30 min. Finally, the root pieces were stained with 0.05% trypan blue in lactoglycerol (1:1:1 lactic acid, glycerol) for 10 min at 90 °C in a bain-marie. The stained root segments were placed in a 50% (v/v) glycerol solution for distaining. The distained root samples were then placed on slides and observed under a compound microscope. Root segments were randomly chosen from the distained root samples. Ten slides were prepared by mounting 10 root fragments on each; therefore, a total of 100 root fragments were prepared per treatment. Mycorrhizal colonization was estimated according to the method proposed by [27].

2.5. Statistical Analysis

The significance of differences between treatments concerning spore abundance, species numbers, and AMF diversity (Shannon–Weiner index) was tested using Fisher’s least significant difference at p < 0.05 after one-way ANOVA. Statistical analyses for spore abundance, species numbers, and AMF diversity (Shannon–Weiner index) were performed with Minitab software version 17. The data were subjected to an analysis of variance (ANOVA) test. The Fisher least significant difference (LSD) was used to separate the means at the 5% level of significance (p < 0.05). Linear regression clarified the influence of soil chemical parameters on communities of AMF. Principal components analysis (PCA) was performed using XlStat Excel extension 2020 to determine the relationship between soil chemical properties and spore’s abundance. The principal component analysis (PCA) analyzed species composition about soil chemical properties using XlStat.
The diversity was calculated from the Shannon–Weiner diversity index (H’) with the formula:
H ′ = − ∑ ( n i N ) ln   ( n i N )
where ni = the spore abundance for an individual species (S) and N = the total spore abundance of the population of all the species in a sample.
A low H′ value generally suggests a site with few species and a few dominant species, while a high H′ value suggests considerably more species. The more species we observe, the more diverse the area.

3. Results

3.1. Soils Chemical and Physical Characterization

The characteristics of the soils from the study sites are given in Table 1. The soil pH from Amuria is neutral (6.0 < pH < 7.5), while the soils from Serere are strongly acidic (pH < 5.5). The P content also differs, with significant variation between sites, as the levels of P contents are 9.52 mg/kg and 4.62 mg/kg for Amuria and Serere, respectively. The organic matter is moderate in Amuria (2.09%) and Serere (1.952%). The CEC is low (8.6 cmol/kg) in the sandy loam soil from Amuria, and moderate (19.9 cmol/kg) in the clay loam from Serere. Total nitrogen (TN) differs significantly between sites; it is 0.047% and 0.093% for Amuria and Serere, respectively.

3.2. Intensity of Maize Mycorrhization

The microscopic observation of maize root samples shows the presence of hyphal, vesicular, and arbuscular features of AMF, and the presence of spores within the roots. Statistical analysis of the frequency and intensity of mycorrhization shows that the site has no significant effect on the mycorrhizal colonization of roots. We notice that the roots isolated from the Amuria fields show almost a similar value for mycorrhization intensity (56%) when compared to the Serere field roots that present intensity of (55%) (Table 2).

3.3. Diversity and Abundance of AMF Spores

Seven genera of AMF are associated with maize in both sites. The genera are Gigaspora, Scutellospora, Glomus, Acaulospora, Archaeospora, Entrophospora, and Paraglomus, as described by [28]. In total, 19 AMF morphotypes are recovered. Eight species are unequivocally assigned to known species of the Glomales, namely, three species of the genus Glomus, two of the genus Acaulospora, one of the genus Gigaspora, one of the genus Scutellospora, and one of the genus Entrophospora. Eleven spore types are not distinguishable at the species level, because they lack enough distinct features. Figure 1 presents some AMF spores observed in the study area. As shown in Table 3, all of the 19 AMF species found in the present study are present in the samples from Amuria. Only 17 species are observed in the samples from Serere. Regarding relative spore abundance, most of the Glomus species show no significant differences between Amuria and Serere. Glomus and Acaulospora spores are relatively more numerous than other AMF spore types in the Amuria fields, whereas Glomus and Entrophospora spores are relatively more abundant than other AMF spore types in the Serere fields. Interestingly, spores of Paraglomus are not found in Serere. Spores of the genera Archaeospora, Gigaspora, and Scutellospora are found to be ubiquitous in all the sites, and they are: Archaeospora schenckii, Archaeospora sp., Gigaspora gigantean, Gigaspora sp., Scutellospora. Pellucida, and Scutellospora sp.
The number of AMF spores per gram of soil and the number of AMF species found per site are shown in Table 3. The highest value is observed in Amuria, with 5.1 spores g−1 of soil (p < 0.05) compared to Serere (3.7 spores g−1 of soil) (Figure 2). Likewise, the species numbers are higher in Amuria compared to Serere. The AMF species diversity, as expressed by the H′, does not show much difference between sites, with higher diversity obtained in the soils from Amuria (H’ = 1.84) compared to Serere (H′ = 1.81) (Table 3). The Shannon–Weiner diversity index (H’) shows similar values (3.35–3.38) for all soil microbial communities, and these differences between soils are not statistically significant (Table 2).

3.4. Relationship between Soil Chemical Properties and Species Diversity

A strong positive and statistically significant correlation is observed between the soil chemical parameters (pH and P) and the species (b, c, e, g, j m, o, q, s, u, and v) (Table 4). The same species are negatively correlated with the CEC. Chemical parameters (such as O.M and TN) are not correlated with the species abundance.
To understand the correlation between the AMF community structure and soil chemical parameters, principal component analysis (PCA) was undertaken (Figure 3). A large number of species occur in soils with lower CEC and sufficient available P, and tend to prefer neutral soils. The distribution of the species is mostly influenced by the pH, CEC, and P. The abundance of the majority of spores is positively correlated with P and pH, and negatively correlated with CEC. This implies that the higher the pH and available P, and the lower the CEC, the higher the species abundance, and vice versa.

4. Discussion

4.1. Intensity of Maize Mycorrhization

The intensities of the mycorrhization of maize roots observed in this study are high (about 55%), and show no significant differences between the sites. These results confirm those obtained by [29,30], who observed a mycorrhization rate of between 50% and 70%. This can be explained by the fact that maize roots are less abundant, stocky, and devoid of absorbent hairs, and are, therefore, particularly dependent on AMF [31]. The root system of maize is characterized by the presence of adventitious roots that only absorb nutrients from the superficial soil layer. Thus, AMF helps root development, and improves water and nutrient uptake from the soil.

4.2. Diversity and Abundance of AMF Spores

Taking into account all the AMF species identified directly in the field samples, 19 species are divided into 7 genera: Gigaspora, Scutellospora, Glomus, Acaulospora, Archaeospora, Entrophospora, and Paraglomus, which are observed under maize cultivation in all sites. This specific richness is higher than that obtained for the sorghum crops in Uganda by [18] and by [32] for pearl millet in Senegal, as well as by [33] for maize crop in Benin. On the other hand, this specific richness is lower than that obtained from the maize field (39 species) by [34] in South Kivu (DR Congo). This difference could be due to the period of collection of soil samples and previous crops, which are important parameters to consider in the evaluation of the density of spores in the soil. The seven genera of AMF are described by [35,36,37,38]. Acaulospora, Entrophospora, and Glomus genera constitute the dominant genera in this area. This finding is in line with the results of [39] in India. These authors demonstrate that Glomus, Gigaspora, Scutellospora, Acaulospora, Paraglomus Archaeospora, and Funneliformis are the most dominant genera associated with maize crops. The results reported in this study indicate the dominance of spores of the Glomus genus. Glomus appears to be the most dominant in croplands [32], and they are the principal maize colonizers [40]. The predominance of species of the genus Glomus in the study area suggests a better adaptation of this genus to the environmental conditions and a wide range of ecological niches [41]. In addition, ref [42,43] demonstrate that maize monoculture also reduces AMF diversity. Maize monoculture is practiced in the fields where the soils are sampled. The result reveals that the area is rich in spores of the Archaeospora and Paraglomus genera. This result is in opposition to those of [44] who observe that Archaeospora and Paraglomus genera are not colonizers of maize grown in monoculture. The results of the diversity index indicate that the AMF community is very diverse, regardless of the site. In this study, the high diversity of AMF species found associated with maize might mean that the mycorrhizal fungi host specificity is low in maize crops. Host specificity of AMF is a longtime debate among researchers. Many authors argue that AMF has no host-plant specificity [45], but several studies demonstrate the preference of some AMF genera for some plant species [46]. Thus, the maize crop has a relatively high mycorrhizal dependency [47]. This mycorrhizal dependency is characterized by the type of crop, the soil properties, and the effect of the cropping system [48]. The variation in diversity index in the area, which varies between 1.81 and 1.84, might result from the variability in soil properties and management practices observed in the study area, where most of the fields are managed in a conventional setting with a medium level of nutrient input. This is in line with the findings of [49], who observe that a high diversity of AMF species results from management practices that affect the nutrient status in the soil.
The number of AMF morphotypes identified is high, which means that eastern Uganda has a high diversity of AMF species. Some AMF species could not be identified in the field samples; the morphological features of the spores were not distinct enough and, thus, these spores could only be grouped into a species group (for example Acaulospora sp.). Using bimolecular tools, this area could reveal greater AMF diversity. Therefore, to ensure the species composition, molecular methods of analysis should be used to confirm the identification of these species.
The results from this study reveal that spore density varies between 3.7 to 5.1 spores per g of soil for all sites. This density is significantly lower than that obtained by [33] (about 1340 spores per g of soil) for maize in Benin but is higher than that observed in DR Congo (0.7 to 1.5 spores per g of soil) by [34]. This difference could be due to the period of collection of soil samples and previous crops, which are important parameters to consider in the evaluation of the density of spores in the soil. According to [50,51], the number of spores is higher in the soil after long-term stress conditions. The number of undiscovered morphotypes may be even higher, affirming that many species are yet to be discovered. Spores abundance is moderate in the field soils. Similar results of moderate abundance are reported in the Willamette Valley of western Oregon (USA) in a field evaluation of AMF fungal diversity by Cheeke et al. 2013, who recorded 15.42 and 16.05 spores g-1. Low spore abundance was discovered in South Kivu (0.6 to 1.5 spores g-1) [34].

4.3. Relationship between Soil Chemical Properties and Species Diversity

In this study, differences in the composition of AMF communities associated with maize were recorded and characterized. The difference in the composition of AMF diversity indicates that soil properties are the main factors of AMF communities associated with maize. Indeed, previous studies demonstrate the influence of soil properties on the composition of AMF communities [52,53]. The results from this study show the existence of a strong relationship between some chemical parameters and the total species diversity and density in the study area. These results are consistent with those of [33]. There is a positive and negative correlation between available P, pH, and CEC, and spore density and diversity, depending on the genus. The low number of morphotypes recovered in Serere compared to Amuria could be explained by the chemical properties of the sandy loam soils, which are neutral with a high level of available P. According to [54], AMF proliferation depends on pH, with a preference for slightly acidic conditions. This is in contradiction with the results of this study, which reveals that AMF is more abundant in neutral soil than in acidic soil. The genera Acaulospora and Glomus show a positive correlation with soil pH. This finding is consistent with the observation of [55]. In addition, AMF plays a major role in P mobilization for the host plant. Depending on the pH of the soil, this element is strongly adsorbed by iron, aluminum, or calcium, in forms that are not available for plants [56]. Phosphorus is a limiting factor for the abundance of AMF spores, whether at very high or very low concentrations [57,58]. Mycorrhizal associations play a significant role in the mineralization of organic phosphorus and mobilize nutrients for the benefit of the host plant [59]. In addition, the diversity and abundance of AMF species concerning soil chemical properties vary among species, as some species are associated with some specific soil conditions. For instance, in this study, AMF species of the genus Entrophospora prefer acidic soil, low P content, and high soil CEC, while the genus Paraglomus are only found in neutral soils with a high level of P content. Many species are found to be generalists in all the sites, especially the species from the Archaeospora, Gigaspora, Scutellospora, and Glomus genera, which are not dependent on soil chemical properties. This study reveals that maize can associate with a range of AMF; thus, a mycorrhizal-based fertilizer produced from the associated species could have a higher chance of thriving in the region.

5. Conclusions

Our study is the first report on arbuscular mycorrhizal fungi (AMF) diversity associated with maize in Uganda. The overall objective of this study was to highlight the diversity of AMF associated with maize in the eastern region of Uganda. Little is currently known about the AMF composition in the roots of other cereal or other plants in the semi-arid regions of Uganda. The results show a higher spore density and a dominance of the Glomus genus in the rhizosphere soil of maize. A total of 19 species divided into 7 genera are identified, with an abundance of the Glomus genus. However, further research is needed to identify and explore more diversity of AMF species associated with this cereal. The molecular identification of the species is recommended for accurate identification. There is a strong relationship between the chemical parameters and the total spore density in the area, as well as with the diversity. The soil pH and P contribute to the distribution of AMF species. Some of the species from the genera Gigaspora, Acaulospora, Glomus, Archaeospora, Gigaspora, and Scutellospora are found in all sites. These genera can be recommended for further research aimed at improving the agricultural benefits of indigenous AMF for enhanced root functions, and the subsequent productivity in farming systems in the region.

Author Contributions

A.F.F. contributed to the inception of the paper, research, and writing. G.N. contributed to the inception and reviews of the paper. J.S. contributed to reviews. H.F.-M. contributed to the inception of the work. A.B. contributed to the data analysis. I.B. and M.N. contributed to the write-up and review. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by Regional Academic Exchange for Enhanced Skills in Fragile Ecosystem Management in Africa (REFORM), grant number: 2017–2861.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

The data presented in this study are available on request from the corresponding author.

Acknowledgments

The authors are thankful to Keryose, Katende, Jude Ssebuwufu, and J.B. of the College of Agriculture Sciences and Biotechnology department, Makerere University for providing laboratory facilities.

Conflicts of Interest

The authors declare that they have no conflicts of interest.

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Blsf 15 00012 g001 550
Figure 1. Study area and soil sampling sites.
Figure 1. Study area and soil sampling sites.
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Blsf 15 00012 g002 550
Figure 2. AMF Spores isolated from the rhizosphere of maize in eastern Uganda. 1—Glomus intraradices. 2—Entrophospora colombiana. 3—Acaulospora foveate. 4—Gigaspora gigantean. 5—Acaulospora spinose. 6—Glomus geosporum. 7—Glomus mossae. 8—Archaeospora schenckii. 9—Scutellospora pellucida.
Figure 2. AMF Spores isolated from the rhizosphere of maize in eastern Uganda. 1—Glomus intraradices. 2—Entrophospora colombiana. 3—Acaulospora foveate. 4—Gigaspora gigantean. 5—Acaulospora spinose. 6—Glomus geosporum. 7—Glomus mossae. 8—Archaeospora schenckii. 9—Scutellospora pellucida.
Blsf 15 00012 g002
Blsf 15 00012 g003 550
Figure 3. Principal component analysis of the species occurrence related to soil chemical properties.
Figure 3. Principal component analysis of the species occurrence related to soil chemical properties.
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Table
Table 1. Physical and chemical properties of soils in the study area.
Table 1. Physical and chemical properties of soils in the study area.
SitepH%TN%O.MP (mg/kg)K (mg/kg)CECSoil Texture *
Amuria6.15 a0.047 a2.09 a9.52 a108.3 a8.6 aSandy loam
Serere5.0 b0.093 b1.952 a4.62 b73.7 b19.9 bClay loam
* according to USDA classification. TN—total nitrogen content; O.M—organic matter content. Data within a row followed by the same letter are not statistically different (p > 0.05) by Fisher’s least significant difference test.
Table
Table 2. AMF spore abundance, species richness, and intensity of mycorrhization found in the field samples of the different sites.
Table 2. AMF spore abundance, species richness, and intensity of mycorrhization found in the field samples of the different sites.
AmuriaSerereLSD
Number of AMF spores per gram of soil (average of three field replicates)5.1 a3.7 b2.34
Total number of AMF species found at the field sites (sum of three field replicates)1917-
H′1.84 a1.81 a0.16
Intensity of mycorrhization56%55%
The AMF diversity is expressed by the Shannon–Weiner diversity index (H′), calculated from the no. of spores identified. Data within a row followed by the same letter are not statistically different (p > 0.05).
Table
Table 3. Relative spore abundance (%) (mean of three field replicates) from each AMF species distinguished in the soil samples from the different sites.
Table 3. Relative spore abundance (%) (mean of three field replicates) from each AMF species distinguished in the soil samples from the different sites.
GenusMorpho-SpeciesAmuriaSerere
AcaulosporaAcaulospora spinose6.910.4
Acaulospora foveata10.26.9
Acaulospora sp.12.67.3
ArchaeosporaArchaeospora schenckii5.04.4
Archaeospora sp.13.13.1
EntrophosporaEntrophospora colombiana6.610.7
Entrophospora sp.115.36.8
Entrophospora sp.25.711.8
GigasporaGigaspora gigantean8.69.0
Gigaspora sp.12.34.6
GlomusGlomus mossae7.37.8
Glomus geosporum6.75.1
Glomus intraradices10.98.2
Glomus sp.16.34.4
Glomus sp.25.64.7
ScutellosporaScutellospora. Pellucida13.38.2
Scutellospora sp.6.07.3
ParaglomusParaglomus sp.15.10.0
Paraglomus sp.25.30.0
The total number of spores identified310226
Data within a row followed by the same letter are not statistically different (p > 0.05). LSD: Fisher’s least significant difference at the 5% level.
Table
Table 4. Pearson’s correlation coefficients between soil chemical properties and AMF community.
Table 4. Pearson’s correlation coefficients between soil chemical properties and AMF community.
Morphotypes
abcdefghijlmoqrstuv
pH−0.8060.9110.9520.4940.953−0.8290.959−0.888−0.1190.9380.0180.6730.8650.7830.5640.935−0.3830.9090.917
TN0.511−0.198−0.2990.188−0.3570.546−0.3970.5180.511−0.3140.4630.117−0.136−0.0060.105−0.2680.679−0.300−0.345
O.M−0.5000.2620.298−0.0450.361−0.4030.357−0.387−0.3920.357−0.3250.0410.0660.1450.2230.309−0.3500.3450.388
P−0.9170.8860.9330.3460.958−0.8960.951−0.938−0.3020.953−0.1710.5780.7410.7110.5180.911−0.4850.9290.947
CEC0.981−0.852−0.889−0.229−0.9400.967−0.9440.9820.447−0.9380.283−0.457−0.654−0.635−0.368−0.8670.600−0.948−0.964
The values indicated in red are a positive correlation, and those in blue are a negative correlation. Abbreviation: pH—potential hydrogen; TN—total nitrogen; O.M—organic matter; P—phosphorus; CEC—cation exchange capacity; a—Acaulospora spinose; b—Acaulospora foveata; c—Acaulospora sp.; d—Archaeospora schenckii; e—Archaeospora sp.; f—Entrophospora colombiana; g—Entrophospora sp.1; h—Entrophospora sp.2; i—Gigaspora gigantean; j—Gigaspora sp.; l—Glomus mossae; m—Glomus geosporum; o—Glomus intraradices; q—Glomus sp.1; r—Glomus sp.2; s—Scutellospora pellucida; t—Scutellospora sp.; u—Paraglomus sp.1; v—Paraglomus sp.2.
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Fall, A.F.; Nakabonge, G.; Ssekandi, J.; Founoune-Mboup, H.; Badji, A.; Balde, I.; Ndiaye, M. Diversity of Arbuscular Mycorrhizal Fungi Associated with Maize in the Eastern Part of Uganda. Biol. Life Sci. Forum 2022, 15, 12. https://doi.org/10.3390/IECD2022-12351

AMA Style

Fall AF, Nakabonge G, Ssekandi J, Founoune-Mboup H, Badji A, Balde I, Ndiaye M. Diversity of Arbuscular Mycorrhizal Fungi Associated with Maize in the Eastern Part of Uganda. Biology and Life Sciences Forum. 2022; 15(1):12. https://doi.org/10.3390/IECD2022-12351

Chicago/Turabian Style

Fall, Abdoulaye Fofana, Grace Nakabonge, Joseph Ssekandi, Hassna Founoune-Mboup, Arfang Badji, Issa Balde, and Malick Ndiaye. 2022. "Diversity of Arbuscular Mycorrhizal Fungi Associated with Maize in the Eastern Part of Uganda" Biology and Life Sciences Forum 15, no. 1: 12. https://doi.org/10.3390/IECD2022-12351

APA Style

Fall, A. F., Nakabonge, G., Ssekandi, J., Founoune-Mboup, H., Badji, A., Balde, I., & Ndiaye, M. (2022). Diversity of Arbuscular Mycorrhizal Fungi Associated with Maize in the Eastern Part of Uganda. Biology and Life Sciences Forum, 15(1), 12. https://doi.org/10.3390/IECD2022-12351

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