Microsatellite Analysis of Common Bean (Phaseolus vulgaris L.) Genotypes in Tanzania for Diversity in Seed Iron and Zinc Micronutrients.

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By Yanda, FE; Tryphone, GM (2023). Greener Journal of Plant Breeding and Crop Science 11(1): 1-12.

 

Greener Journal of Plant breeding and Crop Science

ISSN: 2354-2292

Vol. 11(1), pp. 1-12, 2023

Copyright ©2023, the copyright of this article is retained by the author(s)

DOI: https://doi.org/10.5281/zenodo.7655383

https://gjournals.org/GJPBCS

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Microsatellite Analysis of Common Bean (Phaseolus vulgaris L.) Genotypes in Tanzania for Diversity in Seed Iron and Zinc Micronutrients

Yanda, Focus Edson1; Tryphone, George Muhamba2*

1Ministry of Agriculture, Manyoni District Council, P.O. Box 60, Manyoni, Tanzania.

2Department of Crop Science and Horticulture, College of Agriculture, Sokoine University of Agriculture, P. O. Box 3005, Chuo Kikuu, Morogoro, Tanzania.

ARTICLE INFO ABSTRACT
Article No.: 011723005

Type: Research

Full Text: PDF, HTML, PHP, EPUB

DOI: 10.5281/zenodo.7655383

Common bean (Phaseolus vulgaris L.) grain has big dietary role in supplying protein, energy, vitamins, dietary fibre and micronutrients for millions of people worldwide. In Tanzania, reports have shown existence of Fe and Zn micronutrient variabilities among the common bean genotypes. Eighty-four (84) genotypes were collected to study such variability by seed biochemical and leaf molecular marker analysis. The analyses revealed significant (p < 0.001) genetic variability for seed Zn and Fe nutrient contents. Highest seed Fe content was 118 ppm for genotype Kashiransoni and for seed Zn was 51.81 ppm for Imponzo 5 genotype (both were collected from NPGRC). With seven (7) SSR primers associated with Fe and Zn traits, genetic diversity was evaluated. A marker BM154 scored PIC value 0.967 mean while marker BM160 had a lowest PIC score of 0.899. Using an estimated genetic similarity value, two main clusters with sub clusters in the dendrogram were developed. To corroborate the UPGMA analysis results, a Principal Coordinate Analysis (PCoA) was performed and displayed outputs into scattered plot presentation. For Fe micronutrient improvement purposes, Inula was proposed to be crossed with Kashiransoni while Roba with Imponzo 5 for Zn micronutrient improvement. Selection was based on both concentrations of nutrients for each genotype and their genetic similarity distances.

Accepted: 20/01/2023

Published: 15/02/2023

*Corresponding Author

George Muhamba Tryphone

E-mail: muhatry@ gmail.com

Keywords: SSR, Common bean, Parent selection, Iron and Zinc micronutrients, diversity
   

1.0 INTRODUCTION

Common bean (Phaseolus vulgaris L.) is one of the principal foods and cash crop legumes grown in the tropics and most of the production takes place in developing countries (Hillocks et al. 2006). Common bean grains have big dietary role in supplying protein, energy, dietary fiber and micronutrients for millions of people worldwide although its intake, in terms of nutrient content level, does not satisfy their nutrient requirements (Hillocks et al. 2006). Although common beans are grown largely by smallholder farmers for subsistence and mainly by women, about 40% of the total production from Africa is marketed (Wortmann et al. 1998). It is estimated that over 75% of rural households in Tanzania depend on common beans for daily sustenance (CIAT, 2008).

Micronutrients like zinc and iron are among the important nutrients required in small amounts in the diet to fulfill the nutritional needs of people. Both of these micronutrients are critical to human well-being and an adequate supply of iron and zinc helps to prevent iron deficiency which may lead to reduced oxygen transportation in blood, immune function and consequently to anemia (Blair et al. 2009). Zinc deficiency may lead to reduced immune function, fetal brain cell development and child’s growth and cognitive development as well as other health problems of the developing world (Black, 2003). Zinc is also an anti-cancer element because a potential anti-oxidant. Identifying common bean with high level of these nutrients and integrating them in daily diet will help to improve the situation.

In Tanzania, Tryphone and Nchimbi-Msolla (2010) reported a large variability among common bean genotypes for Fe and Zn nutrient concentrations. Such variability is influenced by genotype environmental interaction and suggested improving climate adapted genotypes has greater potential than improving common bean based on the difference in content of Fe and Zn, for exploiting existing genetic diversity in Tanzania. Unfortunately, there is limited information on how the common bean genotypes being adopted in Tanzania vary genetically for iron and zinc. The knowledge of genetic diversity patterns increases the efficiency for conservation, utilization and genetic improvement of common beans (Beebe et al. 2000). Tremendous efforts have been made to delve deeper into the genetic diversity of these traits in several crop species, including common bean through the use of molecular markers (Talukder et al. 2010). Molecular markers used in estimating the genetic diversity and level of heterozygosity among plants and animals, thus have a great potential to help breeders develop new and improved varieties (Kumar et al., 2008). Therefore, this study will investigate the genetic diversity among germplasm collection of common bean to obtain suitable parental genotype (s) based on both genetic similarity distances and the nutrient levels of Fe and Zn.

2.0 MATERIALS AND METHOD

2.1 Location of the study

The study was conducted at Sokoine University of Agriculture (SUA) in Morogoro, Tanzania in the screen housed behind African seed building located at latitude 6.84795 S and 37.65904 E at 543 m above the sea level. The study was conducted for the period of December 2017 to October 2018.

2.2 Genotypes

Eighty-four (84) common bean genotypes seed were collected from National Plant Genetic Resource Center (NPGRC) at Arusha, Uyole National Research Institute (UNRI) at Mbeya and SUA at Morogoro. The seed was stored in a cold room (12˚C) until planting at Sokoine University of Agriculture, Department of Crop Science and Horticulture. Genotypes collected were diverse, representing a range of seed types, ranging from different seed coat colors, size and shape. During accessioning, there were no specific and strict criteria in choosing a genotype to collect. The collected accessions are as indicated in Table 1.

Table 1: Common bean (Phaseolus vulgarism L.) genotype accessions from different regions of Tanzania

S/N Accession number Genotype Classification Seed Zn (ppm) Seed Fe (ppm) Origin
1 SUA222 Beti 10 Improved 34.37m-x 43.3d Morogoro
2 NPGRC2154 Biliomunyungu Landrace 34.65n-y 53.56l-p Kagera
3 SUA501 Cal 143 Improved 31.1h-s 58.48r-u Morogoro
4 UYL5011 CalimaUyole Improved 36.69o-B 54.8m-q Mbeya
5 SUA180 Canadian Wonder Improved 34.17m-x 66.12A-E Morogoro
6 SUA6301 Cheupe Improved 43B-I 64.61z-B Morogoro
7 NPGRC 286 Chilanda 6 Landrace 27.94d-m 53.04j-o Rukwa
8 NPGRC 287 Chilanda 7 Landrace 34.1m-x 71.29G-I Rukwa
9 NPGRC 134 Chilemba 4 Landrace 33.97m-x 44.29de Rukwa
10 NPGRC 135 Chilemba 5 Landrace 31.86i-t 58.77s-v Rukwa
11 NPGRC 306 Chilemba 6 Landrace 26.9c-j 61.68w-y Rukwa
12 NPGRC 307 Chilemba 7 Landrace 25.75b-i 84.08PQ Rukwa
13 NPGRC 133 Chilemba3 Landrace 42.91A-I 75.02K-M Rukwa
14 NPGRC 401 Fibea Improved 35.66o-z 57.55q-t Morogoro
15 NPGRC 4312 FukamaOkole Landrace 41.73z-I 53.26k-o Kagera
16 NPGRC 3153 Gwezamenyo Landrace 38.77u-E 61.7w-y Kigoma
17 NPGRC 147 Ilanda / Kalinso Landrace 38.12t-D 69.76F-H Rukwa
18 NPGRC 334 Imponzo 4 Landrace 37.89t-D 64.13y-A Mbeya
19 NPGRC 335 Imponzo 5 Landrace 47.89IJ 66.72A-E Mbeya
20 NPGRC 337 Imponzo 7 Landrace 51.81J 72.4H-K Mbeya
21 NPGRC 331 Imponzo1 Landrace 46.08G-H 55n-q Mbeya
22 NPGRC 188 Imponzo8 Landrace 27.29d-l 90.57R Mbeya
23 NPGRC 198 Imponzo9 Landrace 43.16C-I 76.57LM Mbeya
24 NPGRC 4258 Inula Landrace 20.5ab 32.36a Kagera
25 SUA10 Jesca Improved 25.97b-i 66.64A-E Morogoro
26 NPGRC 70 Kablanketi Landrace 30.84h-r 56.57q-t Rukwa
27 NPGRC 3157 Kalambi Landrace 42.71A-I 107.29T Kigoma
28 NPGRC 2158 Kanyamunywa Landrace 39.26v-F 52.46i-m Kagera
29 NPGRC 3175 Kashiransoni Landrace 45.93G-I 118.24U Kigoma
30 NPGRC 69 Kasukanywele Landrace 25.57b-i 65.05z-D Rukwa
31 NPGRC 2190 Kibeho Landrace 24.03a-f 68.83E-G Kagera
32 SUA1400 Kigoma Improved 32.45j-u 48.22fg Morogoro
33 NPGRC 4336 Kiisiki Landrace 24.72b-h 66.44A-E Kagera
34 NPGRC 4265 Kisapuli Landrace 28.89d-n 50.21g-j Kagera
35 NPGRC 4259 Kya Karagwe Landrace 34.77n-y 52.82j-o Kagera
36 SUA444 Lyamungo 90 Improved 35.9n-z 65.94A-E Morogoro
37 SUA333 Lyamungu 85 Improved 24.19a-g 55.7o-r Morogoro
38 NPGRC 3511 Maharage – kienyeji Landrace 23.9a-e 49.74g-i Kigoma
39 NPGRC 3816 Maharage karanga Landrace 33.53k-w 36.92b Kigoma
40 SAU1300 Maini Improved 34.36m-x 46.71ef Morogoro
41 NPGRC 218 Malima / Ndondo Landrace 44.78E-I 67.79C-F Mbeya
42 NPGRC 4269 Maliwalinda Landrace 32.43j-u 93.63S Kagera
43 NPGRC 3164 Mamesa Landrace 30.68h-q 74.1J-L Kigoma
44 NPGRC 3141 Mbuvamutwe Landrace 34.04m-x 76.37LM Kigoma
45 SUA808 Mkanamna Improved 37.11q-C 68.37EF Morogoro
46 SUA601 Msafiri Improved 22.67a-d 52.02h-m Morogoro
47 SUA1003 Mshindi Improved 41.86z-I 59.25t-w Morogoro
48 SUA16 Msolin Improved 40.04w-G 50.86g-l Morogoro
49 NPGRC 3120 Mulembegwa Landrace 34.64n-y 85.44Q Kigoma
50 NPGRC 3150 Mutsinga Landrace 40.26x-G 67.91D-F Kigoma
51 NPGRC 2178 Mwanamwana Landrace 35.97o-z 81.93OP Kagera
52 NPGRC 3155 Mwanja Landrace 45.44F-I 66.22A-E Kigoma
53 NPGRC 3119 Mwolo -yellow Landrace 41.96z-I 62.93x-z Kigoma
54 SUA909 Nanavala Improved 39.94w-G 49.77g-i Morogoro
55 SUA800 Nanka Improved 31.03h-s 56.25p-s Morogoro
56 NPGRC 2213 Ndimila enkobe Landrace 37.52s-D 88.09R Kagera
57 NPGRC 3005 Njano ndefu Landrace 36.52o-A 66.82A-F Kigoma
58 UYL5010 Njano Uyole Improved 41y-H 50.13g-j Mbeya
59 NPGRC 3154 Nyamanza Landrace 34.88n-y 73.49I-k Kigoma
60 UYL5015 Nyeupe Uyole Improved 33.16j-v 67.98D-E Mbeya
61 UYL5018 Pasi Improved 25.36b-h 52.99j-o Mbeya
62 SAU1007 Pesa Improved 33.35k-v 56.75q-t Morogoro
63 SUA200 Roba Improved 18.23a 58.7s-v Morogoro
64 SUA1009 Rojo Improved 37.42s-D 77.76MN Morogoro
65 NPGRC 4248 Ruhondela Landrace 28.5d-n 50.33g-k Kagera
66 NPGRC 2220 Rukurulana Landrace 34.06m-x 80.1NO Kagera
67 NPGRC 4352 Ruvunja Landrace 34.83n-y 67.18B-F Kagera
68 SAU500 Selian 05 Improved 37p-C 64.86z-C Morogoro
69 SUA777 Selian 06 Improved 30.28f-o 61.54v-y Morogoro
70 SUA11 Selian 94 Improved 36.67o-B 48.23fg Morogoro
71 NPGRC 3156 Seredi Landrace 45.4F-I 51.89h-m Kigoma
72 NPGRC 4221 Shona Landrace 43.58D-I 76.88LM Kagera
73 NPGRC 4322 Shona egunia Landrace 29.15e-n 48.01fg Kagera
74 NPGRC 111 Soya nano Landrace 23.96a-f 60.7u-x Morogoro
75 SUA1010 Sua 90 Improved 33.64k-w 49.15f-h Morogoro
76 NPGRC 1604 Tichakuronza Landrace 47.23H-J 72.14H-J Kagera
77 NPGRC 3182 Ugweza Landrace 33.68l-w 40.15c Kigoma
78 UYL5017 Uyole 03 Improved 27.26d-k 57.3q-t Mbeya
79 UYL5016 Uyole 04 Improved 37.27r-D 67.85C-F Mbeya
80 UYL5012 Uyole 16 Improved 37.15q-C 67.26B-F Mbeya
81 UYL5020 Uyole 94 Improved 33.21j-v 60.81u-x Mbeya
82 UYL5013 Uyole 96 Improved 25.63b-i 38.35bc Mbeya
83 UYL5009 Uyole84 Improved 20.68a-c 34.37a Mbeya
84 SUA1001 Zawadi Improved 30.47g-p 53.37l-o Morogoro
    Mean   34.44 62.533  
    SEM   1.845 0.898  
    %CV   9.3 2.5  
    P-value   <.001 <.001  

Key: UYL – Uyole, SUA – Sokoine University of Agriculture, NPGRC- National Plant Genetic Resource Center, SEM- Standard error of means and %CV- Percentage coefficient of variation

2.3 Soil sampling and chemical analysis

Composite soil samples obtained were analysed as described by Carter (1993). Bulk soil samples were taken at a depth of 0 – 20 cm on an area of 2 × 2 m2. Composite soil constituted nine sub-samples randomly collected from forestry area covering 1.0 ha. For pot experimentation, sub-samples were thoroughly mixed, sterilized, air dried and ground to pass through an 8.0 mm mesh. Further preparations for soil analysis were carried whereby, the 2.0 mm sieved composite soil samples were used for laboratory physical and chemical analyses. Composite soil samples obtained were analysed for pH, cation exchange capacity, exchangeable bases (Ca, K, Mg and Na), micronutrients (Fe, Zn, Mn and Cu), Nitrogen (N), available phosphorus, particle size distribution and organic carbon (OC) as described by Carter (1993). The soil pH was determined in water at a soil: water ratio of 1:2.5 suspension using pH meter. Electrical conductivity was measured in 1:2.5 soil: water using the electric conductivity meter (Thomas, 1996). Cation exchange capacity (CEC) was determined by the ammonium-acetate saturation method and quantification of exchangeable bases: K, Ca, Na and Mg were determined from the ammonium-acetate filtrates following the Lindsay and Norvell (1978) methods. Exchangeable calcium (Ca) and magnesium (Mg) were determined by atomic absorption spectrophotometry whereas K and Na were extracted using ammonium acetate and analysed by flame spectrophotometry. The DTPA extractable Cu, Fe, Mn and Zn were determined by atomic absorption spectrophotometry (Lindsay and Norvell, 1978). Total nitrogen was determined by the micro-Kjeldahl digestion distillation method (Bremner and Mulvaney, 1982). Soil extractable P was determined by using the Bray-1-P method by Kuo, (1996) and colour was developed by the ascorbic acid-molybdate blue method (Murphy and Rilley, 1962). Particle size analysis was determined by the hydrometer method after dispersing the soil samples with sodium hexametaphosphate solution (Gee and Bauder, 1986). Soil textural classes were determined using the USDA textural class triangle (USDA, 1975).

2.4 Screen house experimentation and agronomical practices

Eighty-four (84) genotypes were arranged in a completely randomized design (CRD) and replicated three times. Before sowing, the 4 kg potted soil was watered and allowed to stay for one day. Four seeds were sown; thinning was done at age of 10 days after emergence. Irrigation by re-introducing trapped water (infiltrates) on bottomed trays was carried out regularly to maintain the moisture content.

2.5 Chemical analysis for iron and zinc nutrients in common bean seeds

After harvesting, bean seeds from each pod of individual plant were mixed thoroughly and taken for chemical analysis. Dry ash method of extraction was undertaken to determine iron and zinc content (Jorhem, 1993). Digested plant samples were taken for reading absorbance values using the Atomic Absorption Spectrophotometer (AAS) method. A standard curve was computed and used to determine the concentration of each sample using Microsoft excel program (version 2016).

2.6 Genomic DNA extraction

Total genomic DNA was extracted from a trifoliate leaf tissue sample of 14 days old plants by using the Quick-DNA Plant/Seed Mini-Prep Kit protocols. DNA quality and quantity were assessed on gel electrophoresis stained with safe view DNA loading dye (EZ-vision) EZ vision. Seven simple sequence repeat (SSR) markers were used to detect the polymorphisms and assess genetic diversity of 84 common bean genotypes collected from two organizations, with several sources of their origin and marker diversity as shown in Table 1and 3 respectively.

2.7 SSR markers and PCR amplification

SSR primer pairs were selected on the basis of the published genetic diversity analysis on common bean by (Talukder et al. 2010). Seven microsatellite primers with high polymorphism levels (≥0.5) were selected and used for final polymerase chain reaction (PCR) amplification (Table 10) for investigating the genetic diversity on Fe and Zn micronutrients in the dry bean accession. The DNA amplification was carried out according Talukder et al. (2010) protocol with minor modifications. A final volume of 25 μl for the PCR reaction mix included 1.5 μl genomic DNA, 0.1 μl of forward and reverse primers, 12.5 μl of 2X× TaqMaster mix and 10 μl of nucleotide free sterile double distilled water. The temperature profile in the thermocycler was of one cycle of 95 0C for 3 min; 40 cycles of 95 0C for 1 min, from 55 to 57 0C for 1 min, and 72 0C for 2 min; and one cycle of 72 0C for 10 min.

2.8 Electrophoretic separation and visualization of amplicons

Superfine agarose (2 %) gel preparation involved the addition of 150 ml of chilled 1x TBE buffer (pH 8.0) to a flask with 3g of superfine agarose powder. Twenty microlitres (20μl) of safe view DNA loading dye (EZ-vision) was added to the gel and cast on a tray to set at room temperature. A gel was then carefully placed in a tank with plenty of 1x TBE buffer and into each well, 3 μl of the samples were carefully loaded with the first well having 1 μl of DNA ladder (100 bp). Gel electrophoresis was run for 200 min at 120 volts. The bands were visualized under an ultra violet trans-illuminator and photo-shopped using the Picasa software.

2.9 Data analysis

2.9.1 Chemical analysis

Obtained absorbance values were processed using MS excel (2018) to determine the concentrations through R square value by establishment of standard curve. The treatment effects were analyzed by analysis of variance (ANOVA) using GenStat V. 25 software. In additional, Fisher’s least significant difference (LSD) was used for mean separation at 5% level of probability.

2.9.2 Genetic diversity

Gel images obtained after electrophoresis were processed using IMAGE J software to determine the molecular weight of the SSR marker bands in reference to the loaded DNA ladder. The determined molecular weights of the SSR marker bands were analyzed by POWERMARKER V.3.25 for estimating the mean number of observable alleles (Na), major allele frequency, allele frequency, observed heterozygosity, expected heterozygosity, gene diversity and the polymorphic information content (PIC).

2.9.3 Cluster analysis

Genetic diversity analyses were conducted using numerical taxonomy and the multivariate analysis system, NTSYSpc V. 2.2. Genetic similarity values were computed between all possible pairs with the SIMQUAL option and ordered in a similarity matrix. The similarity matrix was run by sequential, agglomerative, hierarchical, nested (SAHN) clustering with the unweighted pair group with arithmetic averaging (UPGMA) method as an option. The dendrogram and cluster groupings were constructed by the UPGMA clustering algorithm from the SAHN option of NTSYSpc v.2.2.

2.9.4 Principal coordinate analysis

To corroborate the interrelationships between the common bean genotypes, a scatter plot representation was built using principal coordinate analysis (PCoA) with the Nei’s similarity coefficient. The analyses were performed using GenAlEx statistical software V 6.5 (Peakall and Smouse, 2012).

3.0 RESULTS

3.1 Soil chemical analysis

The experimental forestry soils had medium to high chemical and sandy clay loam textural class as physical characteristics (Table 2). The analysed composed forestry soil based on the selected soil parameters, showed optimal condition that favour growth of common bean as described by Landon, (1991). Therefore, the forestry soils were suitable for production of common beans and other field crops like cereals.

Table 2: Physical-chemical properties of the experimental forestry soils

Soil parameter Values Remark (Landon, 1991).
pH in water 6.79 Neutral
Electrical Conductivity (EC) (µS /cm) 451 Medium 
Cationic Exchange Capacity (CEC) 32.6  High 
Organic Carbon (% OC) 2.62 High
Organic matter (% OM) 4.52 High
Nitrogen (%) 0.50 Medium
Carbon: Nitrogen ratio 9.04 Good quality of the OM
Phosphorous (mgkg-1) 9.33 Medium
Extractable K (Cmol (+) kg-1) 1.90 High
Extractable Na (Cmol (+) kg-1) 0.14 Low
Extractable Mg (Cmol (+) kg-1) 0.41 Low
Extractable Ca (Cmol (+) kg-1) 16.85 High
DTPA Extractable micronutrients (mg kg-1)    
Fe 34.96 High 
Zn 4.08 High 
Particle size analysis (PSA)    
%Clay 33.56  
%Silt 9.64  
%Sand 56.8  
Textural class Sandy clay loam (USDA, 1975)

3.2 Chemical analysis for iron and zinc contents on common bean seeds

The iron content in seed for collected genotypes of Common bean differed significantly (P<0.001) (Table 1). It varied from 32.36 to 118.24 ppm, with a mean of 62.533ppm. Genotypes of Kashiransoni, Kalambi and Maliwalinda were observed with the highest seed iron (Fe) contents of 118.24 ppm, 107.29 ppm and 93.63 ppm respectively. On the other hand, 32.36 ppm, 34.37 ppm and 36.92 ppm were the lowest contents of iron observed in genotypes of Inula, Uyole84 and Maharage-karanga respectively. The genotypes differed significantly (P<0.001) in seed zinc contents (Table 1). Values varied from 18.23 to 51.81 ppm with a mean of 34.44 ppm. Genotypes Imponzo5, Imponzo7 and Tichakuronza were observed with the highest seed zinc (Zn) contents of 51.81 ppm, 47.89 ppm and 47.23 ppm respectively meanwhile 18.23 ppm, 20.5 ppm and 20.68 ppm were the lowest contents of zinc observed in genotypes Roba, Inula and Uyole 84 respectively.

3.3 Allelic diversity of common bean accessions

The key parameters used to define genetic diversity among the common bean accessions from Tanzania are presented in Table 3. There was a high polymorphism with a mean of 24.857 alleles per locus and a range of 17 to 40 alleles in the germplasm. The frequency for the major allele ranged from 0.064 for primer BM154 to 0.208 for the primer BMd16 with mean of 0.139. In total, the 7 markers detected 174 alleles and PIC ranging from 0.892 for the primer BMd16 to 0.967 for the primer BM154 with the mean of 0.923. The overall mean for the expected heterozygosity ranged from 0.899 for BMd16 primer to 0.967 for BM154 primer. The observed heterozygosity was observed on the two primers of BM160 and BM181 with value 0.025 and 0.027 respectively.

Table 3: Genetic information for the markers used to detect the genetic diversity of 84 Common bean genotypes collected from different regions of Tanzania for the Fe and Zn traits.

S/N Marker Sample amplified Major allele frequency Allele number Gene Diversity He Ho PIC
1 BM154 78 0.064 40 0.929 0.967 0.000 0.967
2 BM160 79 0.120 24 0.940 0.939 0.025 0.936
3 BM170 75 0.107 24 0.937 0.937 0.000 0.934
4 BM181 73 0.192 23 0.901 0.900 0.027 0.893
5 BM211 68 0.147 23 0.922 0.921 0.000 0.917
6 BMd16 72 0.208 17 0.899 0.899 0.000 0.892
7 BMd33 66 0.136 23 0.927 0.927 0.000 0.922
Mean     0.139 24.86 0.922 0.927 0.007 0.923

3.4 Cluster analysis

For a better understanding of the genetic relationship among common bean genotypes, the genetic similarity (GS) values were submitted to hierarchical clustering by UPGMA. The dendrogram based on Nei’s coefficient of genetic distance suggested the existence of two clusters with sub clusters (Figure 1). The Cluster I was further subdivided into two sub clusters of A and B in total comprised of 31 and 2 genotypes of common bean respectively. Cluster II was also divided into two sub cluster designated as A and B with a total of 28 and 23 genotypes respectively (Table 4).

Table 4: Distribution of genotypes to different clusters based on the UPGMA methods

Cluster Sub

cluster

Number of genotypes Name of genotypes
I A 31 Jesca, Kibego, Uyole 90, Sua 90, Kanyamunywa, Mshindi, NyeupeUyole, Uyole 94, Maharage-kienyeji, Zawadi, Shona-Egunia, Chilemba 4, Uyole 03, Rojo, Rukurulana, Kasukanywele, Chilemba 7, Biliomunyungu, Mwolo-Yellow, Maini, Msolin, Imponzo 9, Imponzo 1, Malima/Ndondo, Calima-Uyole, Fibea, Pasi, Msafiri, Kigoma, NjanoUyole and Njanondefu
B 2 Kablanketi and Uyole 04
II A 28 Selian 94, Ruvunja, FukamaOkole, Ilanda/kalinso, Canadian wonder, Uyole 16, Maharagekaranga, Lyamungu 85, Cal 143, Inula, Ruhondela, Chilemba 6, Imponzo 8, Kiisiki, Ugweza, Imponzo 7, NdimilaEnkobe, Nyamanzi, Chilemba 3, Mwanamwana, Maliwalinda, Mamesa, Mbuvamutwe, Mwanja, Mulembegwa, Seredi and Kashiransoni
B 23 Soya Njano, Beti 10, Nanka, Roba, Lyamungu 90, Imponzo 5, Chilanda 7, Selian 06, Tichakuronza, Uyole 84, Mkanamna, Mutsinga, Shona, Selian 05, Kalambi, Chilemba 5, Chilanda 6, Kyakaragwe, Cheupe, Gwezamenyo, Nanayala, Pesa and Kisapuli.

3.5 Principal co-ordinate analysis

The common bean genotypes were represented by a scatter plot in 2-dimensions using the results of the principal coordinate analysis (PCoA) obtained by estimating the Nei’s genetic similarity distance. It revealed the global structure similar to the dendrogram analysis, but the distribution of these accessions was shown more clearly in scatter plot (Figure 2). Overall, the clustering pattern of the genotypes in the principal coordinates analysis corresponds with the dendrogram derived from UPGMA (Figure 1).

Figure 1: Dendrogram representing the genetic diversity among the 84 accessions of Common bean of Tanzania based on Dice coefficient

of similarity matrix data using UPGMA cluster analysis

Figure 2: Principal coordinate analysis (PCoA) of common bean accessions from the microsatellite diversity based on molecular weight (band sizes) of alleles.

4.0 DISCUSSION

4.1 Iron and zinc contents in common bean

The high seed Fe and Zn content were expressed with genotypes of Kashiransoni and Imponzo5. Both genotypes were sourced at the gene bank of Tanzania (NPGRC) being collected from Kigoma (Kashiransoni) and Mbeya (Imponzo 5) regions. There was no environmental contribution to the significantly (p<0.001) variability of both seed Fe and Zn content on the experimented genotypes of common bean because the study was conducted in screen-house conditions hence differences in their genetic makeup could have resulted into such variability.

4.2 Genetic diversity of common bean genotypes

The employed UPGMA clustering method divided the common bean genotypes into two main clusters. The main two branches of the dendrogram have showed a considerable range of genetic diversity of genotypes in respect to the genetic similarity distance being less than 9e-04, suggesting existence of low genetic diversity based on Fe and Zn traits. This existence could be due to either the genotypes in equation comes from the similar origin or the SSR markers used could not clearly detect large range of diversity. Similar results for the diversity of common bean genotypes for iron and zinc nutrients of Tanzania corresponds with numerous and deliberate efforts done by other researchers worldwide by using various molecular techniques including SSR marker. Talukder et al. (2010) observed low level of genetic diversity because since the GS for the common bean genotypes was more than 50%, hence suggesting low genetic variability. Low genetic variability between the two main clusters does hinder selection of parental genotypes for cross breeding programs due to significant (p<0.001) difference in variabilities of seed Fe and Zn content. Thus, it can be expected that the introgression of a desired trait would be easier for this cross without sacrificing valuable trait(s) and/or adding unwanted trait(s) as a consequence of linkage drag (Talukder et al. 2010).

4.3 Selection of genotypes for breeding programs

Selection of genotypes for breeding purpose based on micronutrient variability and genetic diversity has been suggested in many crop species including common bean by Talukder et al. (2010) and rice (Gregorio, 2000). From the current results of genetic diversity analysis, several breeding strategies can be derived; however, the interest at present is to develop populations to map Zn and Fe content traits and to breed common bean cultivars with enhanced Zn and Fe contents.

Based on seed Iron (Fe) and Zinc (Zn) contents of the genotypes and genotypic variability at molecular level, the cross-breeding program for seed Fe content was designed to cross the genotypes with high Fe content namely Kashiransoni, Kalambi and Maliwalinda while low Fe content genotypes were Inula, Uyole84 and Maharage-karanga. The high Fe contents genotypes Kashiransoni, Kalambi and Maliwalinda belonged to clusters II-A, II-B and II-A respectively and those of low Fe contents viz. Inula, Uyole 84 and Maharage-karanga belonged to clusters; II-A, II-B and II-A respectively. The genetic similarity distance values of genotypes Inula with Kashiransoni, Kalambi and Maliwalinda are 1.704e-4, 0 and 1.0116e-3 respectively and those of Uyole 84 with Kashiransoni, Kalambi and Maliwalinda are 3.91e-3, 3.31e-3 and 3.20e-3 respectively and those of Maharage-karanga with Kashiransoni, Kalambi and Maliwalinda are 8.89e-4, 2.79e-3 and 1.03e-3 respectively. These values indicate that the selected genotypes are divergent at the molecular level with significant differences in seed Fe content and could result in better segregation and recombination of the desired alleles in successive generations during population development.

For the crossing program to enhance seed Zn content, genotype Imponzo 5 with high Zn content (ppm) was selected against the genotypes of Roba and Inula with low zinc contents. The high Zn content genotype of Imponzo 5 belonged to clusters II-A and the low Zn content genotypes of Roba and Inula belonged to clusters II-B and II-A respectively. The genetic similarity distances value of genotype Roba with Imponzo 5 was 8.72e-4 and that of Inula with Imponzo 5 was 5.28e-4. These values indicate that the selected genotypes are divergent at the molecular level with significant differences in seed Zn content and could result in better segregation and recombination of the desired alleles in successive generations during population development. Crossing combinations with genotypes between and within cluster having high genetic diversity and mineral content would be expected to accumulate positive alleles derived from unique sources and generate breeding lines with even higher seed mineral contents.

Also, crossing of the selected genotypes would be of significant important for genetic studies because they’re contrasting for the observed traits. Genetic studies offer an opportunity of utilizing the genetic information like inheritance patterns of Fe and Zn, additive effect and dominance effects of gene can be determined as knowledge of heritability is crucial for decisions making concerning screening and breeding methodologies and the scale of breeding.

5.0 CONCLUSION

The variability in iron and zinc content was significant (p<0.001) across all experimented genotypes. The range of seed iron content was 32.36 for Inula to 118.24 ppm for Kashiransoni genotype with mean of 62.533 ppm. For seed zinc content it ranged from 18.23 ppm for Roba to 51.81 ppm for Imponzo 5 with a mean of 34.44 ppm. The SSR primers used in this study showed to be effective on detecting the alleles bonded to the trait of iron and zinc. The high PIC (0.967) value was shown by BM154 primer which detected 40 alleles for 78 samples of genotypes that were amplified. The overall results obtained by SSR analysis of the common bean genotypes in the present study has shown that there is genetic divergence among the collected genotypes based on the traits. The UPGMA analysis together with the scattered plot presentation (PCoA) has successfully grouped the genotypes into sense of similarity by using the estimated genetic similarity distance. It is recommended that the genotypes Kashiransoni and Inula for iron and Roba and Imponzo 5 for zinc as breeding materials as sources Fe and Zn. Introgression of gene for Fe and Zn enrichment should rely on consumer preferred common bean genotypes as a key group during participatory plant breeding (PPB) programs. Further, the inheritance patterns of Fe and Zn traits has to be studied since the knowledge of heritability is crucial for decisions making concerning screening and breeding methodologies and the scale of breeding.

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Cite this Article: Yanda, FE; Tryphone, GM (2023). Microsatellite Analysis of Common Bean (Phaseolus vulgaris L.) Genotypes in Tanzania for Diversity in Seed Iron and Zinc Micronutrients. Greener Journal of Plant breeding and Crop Science, 11(1): 1-12. https://doi.org/10.5281/zenodo.7655383

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