| Literature DB >> 30504850 |
Puleng Letuma1,2,3,4, Yasir Arafat3,5, Muhammad Waqas1,2,3, Feifan Lin3,5, Weiwei Lin3,5, Yiyang Zhang1,2,3, Mamello Masita5,4, Kai Fan3,5, Zhaowei Li6,7, Wenxiong Lin8,9,10,11.
Abstract
Generally, plant roots shape the rhizosphere fungal community but how individual plant genes involved in senescence affect this shaping is less studied. We used an early senescence leaf (esl) mutant rice and compared it with its isogenic wild type variety to evaluate the effect of the vacuolar H+-ATPase (VHA-A1) gene mutation on the rhizosphere fungal community structure and composition using a metagenomic pyrosequencing approach. The most predominate fungal phyla identified for both isogenic lines belonged to Ascomycota, Basidiomycota and Glomeromycota, where Ascomycota were more prevalent in the esl mutant than the wild type variety. Real-time quantitative PCR analysis confirmed a significant rise in the richness of Cladosporium cladosporioides in esl mutant rice than the wild type variety. Correlation analysis revealed four most abundant genera identified for the esl mutant and their close association with yield and biomass decline, lipid peroxidation, lower root vitality, chlorophyll degradation and limited VHA activity. Higher K+ efflux, H+ and a lower Ca2+ influx was also observed in the esl mutant which could be the reason for abnormal functioning of mutant plants. These results illustrate that besides the well-known effect of senescence on plant physiology and yield decline, it can further shape the rhizosphere fungal community.Entities:
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Year: 2018 PMID: 30504850 PMCID: PMC6269515 DOI: 10.1038/s41598-018-35578-y
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Effect of senescence on rice biomass, yield and physiological parameters of esl mutant rice (Mut) and its isogenic wild type (WT) variety.
| Parameter | WT | Mut |
|---|---|---|
| Root to shoot ratio | 0.2519a | 0.1937b |
| Panicle number/plant | 14.667a | 6.33b |
| 1,000-seed weight (g) | 26.587a | 16.10b |
| Filled grain (g) | 2679.3a | 364.7b |
| % filled grain | 88.133a | 73.667b |
| Chlorophyll content | 43.883a | 30.933b |
| Electrolyte leakage % (r) | 44.93b | 67.10a |
| Electrolyte leakage % (l) | 20.37b | 30.93a |
| MDA(r) (nmol g−1 FW) | 0.1364b | 0.2284a |
| MDA(l) (nmol g−1 FW) | 0.1713b | 0.2392a |
| % Root oxidizability | 38.54a | 26.65b |
| VHA activity (r) (µmol pi mg−1 protein h−1) | 0.3845a | 0.2974b |
| VHA activity (l) (µmol pi mg −1 protein h−1) | 0.4152a | 0.293b |
Means followed by different letters in a row are significantly different (P ≤ 0.05, n = 4). *Significant at 1% level of probability. *Significant at 5% level of probability; Tchl, Total chlorophyll; MDA(r), (l), Malondialdehyde in roots and leaves, respectively; E.L. % (r), (l), electrolyte leakage percentage in roots and leaves respectively; % R.O., percentage Root oxidizability; VHA (r), (l), Vacuolar H+-ATPase activity in roots and leaves, respectively.
Figure 1Rarefaction curves of fungal communities based on observed OTUs at 3% dissimilarity for soil samples.
Figure 2Estimates of α-diversity indices including (a) abundance-based coverage estimators (ACE), (b) Chao1, (c) Shannon, and (d) Simpson in wild type (WT) and esl mutant (Mut) soil samples.
Figure 3Biplot ordination of (a) UniFrac-weighted principal coordinate analysis (PCoA) and (b) Unweighted UniFrac (UUF) PCoA for the tested soil samples, WT represents an isogenic wild type variety, while Mut represents esl mutant. (c) UPGMA/hierarchical clustering analysis based on weighted UniFrac distances displaying the relative abundance of the most abundant fungal phylum of WT and Mut soil samples. (d) β-diversity heat map based on weighted (WUF) and unweighted (UUF) UniFrac distances. Values in the upper and lower corners represented the WUF and UUF distances.
Figure 4Heat map displaying the distribution of the 35 most abundant fungal genera and their Pearson’s correlation coefficients with yield (1,000-seed weight). Data are mean values of n = 3; significant correlation coefficients are noted in asterisks where P ≤ 0.05.
Top genera with 50% cumulative contribution to the dissimilarity amongst the samples.
| Genus | Class | Phylum | % Contribution | % Relative Abundance | |
|---|---|---|---|---|---|
| WT | Mut | ||||
| Cladosporium | Dothidiomycetes | Ascomycota | 4.9 | 0.3000b | 9.5667a |
| Thielavia | Sordoriomycetes | Ascomycota | 4.3 | 6.300a | 2.300b |
| Zopfiella | Sordoriomycetes | Ascomycota | 3.8 | 5.900a | 1.8b |
| Giberella | Sordoriomycetes | Ascomycota | 1.9 | 0.3333b | 3.4667a |
| Fusarium | Sordoriomycetes | Ascomycota | 1.3 | 1.6333a | 0.9333b |
| Westerdykella | Dothidiomycetes | Ascomycota | 1.3 | 1.7000a | 1.000b |
| Hongkongmyces | Dothidiomycetes | Ascomycota | 1.3 | 1.600a | 1a |
| Taeniolla | Dothidiomycetes | Ascomycota | 1.1 | 2.033a | 0.2333b |
| Humicola | Sordoriomycetes | Ascomycota | 1.0 | 0.8667b | 1.2333a |
Means followed by different letters in a row are significantly different (P ≤ 0.05, n = 3).
Figure 5Venn diagram showing the number of shared and unique OTUs in different sample groups. (a) Unique OTUs (442) in the samples of wild type rhizhosphere soil (b) Venn diagram figure for fungal OTUs in the two rhizospheric soil samples (c) Unique OTUs (171) in the samples of esl mutant rice (Mut) rhizosphere soil. (d) OTUs (685) shared by mutant and wild type variety at grain-filling stage.
Figure 6The net H+, Ca2+ and K+ flux in rice roots from esl mutant and the wild type variety at grain-filling stage. The positive values in the figures represent the net efflux and negative value represents the net influx. Each point represents the mean value of four individual roots and bars represent the SE of the mean. The mean fluxes of H+, K+ and Ca2+ within the measuring periods are shown alongside and different letters indicates a significant difference at P ≤ 0.05.