| Literature DB >> 28163711 |
Jakson Leite1, Doreen Fischer2, Luc F M Rouws3, Paulo I Fernandes-Júnior4, Andreas Hofmann2, Susanne Kublik5, Michael Schloter5, Gustavo R Xavier3, Viviane Radl5.
Abstract
Many studies have been pointing to a high diversity of bacteria associated to legume root nodules. Even though most of these bacteria do not form nodules with legumes themselves, it was shown that they might enter infection threads when co-inoculated with rhizobial strains. The aim of this work was to describe the diversity of bacterial communities associated with cowpea (Vigna unguiculata L. Walp) root nodules using 16S rRNA gene amplicon sequencing, regarding the factors plant genotype and soil type. As expected, Bradyrhizobium was the most abundant genus of the detected genera. Furthermore, we found a high bacterial diversity associated to cowpea nodules; OTUs related to the genera Enterobacter, Chryseobacterium, Sphingobacterium, and unclassified Enterobacteriacea were the most abundant. The presence of these groups was significantly influenced by the soil type and, to a lesser extent, plant genotype. Interestingly, OTUs assigned to Chryseobacterium were highly abundant, particularly in samples obtained from an Ultisol soil. We confirmed their presence in root nodules and assessed their diversity using a target isolation approach. Though their functional role still needs to be addressed, we postulate that Chryseobacterium strains might help cowpea plant to cope with salt stress in semi-arid regions.Entities:
Keywords: Bradyrhizobium; Chryseobacterium; Vigna unguiculata (L.) Walp; endophytes; microbiome
Year: 2017 PMID: 28163711 PMCID: PMC5247471 DOI: 10.3389/fpls.2016.02064
Source DB: PubMed Journal: Front Plant Sci ISSN: 1664-462X Impact factor: 5.753
Soil chemical characteristic of the top soil of the stations is shown.
| Soils type | Haplic Vertisol | Red yellow dystrophic Ultisol |
|---|---|---|
| Organic matter (g.kg-1) | 7.2 | 6.3 |
| pH (H2O) | 6.8 | 6.3 |
| P (mg.dm3) | 44.62 | 11.92 |
| K (cmolc.dm-3) | 0.36 | 0.33 |
| Ca (cmolc.dm-3) | 20.4 | 2.0 |
| Mg2+ (cmolc.dm-3) | 5.6 | 0.4 |
| Al3+ (cmolc.dm-3) | 0.05 | 0.05 |
| H+Al3+ (cmolc.dm-3) | 4.62 | 0.66 |
| Some of bases – S (cmolc.dm-3) | 26.45 | 2.78 |
| Cation exchange capacity – CEC (cmolc.dm-3) | 31.07 | 3.44 |
| Base saturation – V (%) | 85 | 81 |
Richness estimates, alpha diversity, and evenness based on OTUs clustered at 95% similarity level.
| Source | Coverage | Chao | Shannon | |
|---|---|---|---|---|
| Diversity ( | Evenness ( | |||
| BRS Acauã Ultisol | 96.0 (±1.0) | 143.0 (±17.3) | 0.28 (±0.04) | 0.05 (±0.01) |
| BRS Acauã Vertisol | 95.0 (±1.0) | 174,2 (±19.7) | 0.14 (±0.06) | 0.10 (±0.05) |
| BRS Pujante Ultisol | 95.0 (±1.0) | 202.4 (±42.2) | 0.22 (±0.11) | 0.06 (±0.02) |
| BRS Pujante Vertisol | 95.0 (±1.0) | 200.9 (±53.0) | 0.19 (±0.05) | 0.06 (±0.02) |