The Mantel test showed the relationships between the microbial community structure and environmental variables (Fig. 3). Bacterial community structure in bulk soil was significantly correlated with available magnesium while fungal community structure was not significantly affected by any of the soil physicochemical properties. Bacterial communities in the endosphere of leaf and fruit were not significantly correlated with nutrient contents in leaves and fruits, but fungal communities in those two compartments were affected by iron and total nitrogen content.
The Spearman correlation analysis was conducted between the phyla at higher relative abundance with the environmental variables such as soil physicochemical properties, leaf nutrients content and fruit nutrients content (Fig. 4). In bulk soil and endosphere of leaves and fruits, there were significant correlations between microbial taxa at different phylum and soil physicochemical properties, as well as nutrient contents of leaves. In bulk soil, The phylum of Proteobacteria, Firmicutes, Chloroflexi, Actinobacteriota, Bacteroidota, Bdellovibrionota, Gemmatimonadota, Myxococcota and Dependentiae was significantly correlated with soil physicochemical properties. Among them, the relative abundance of Bdellovibrionota was positively correlated with soil pH, available P, available Mg and Fe, total carbon and C/N ratio while the relative abundance of Gemmatimonadota was negatively correlated with soil pH, available magnesium, available zinc, total carbon and C/N ratio. Eight fungal phyla were affected by soil physicochemical properties. The relative abundance of Aphelidiomycota was negatively correlated with available P and SOM while the relative abundance of GS01 was positively correlated with SOM, available zinc and total carbon. However, compared to that in bulk soil, the relative abundance of bacteria and fungi in leaf and fruit endosphere was less susceptible to plant and soil variables. In leaf and fruit endosphere, two bacterial phyla and 2 fungal phyla were significantly affected by nutrient contents of leaves and fruits. The relative abundance of Firmicutes was positively correlated with available Ca, Mg, Mn, and that of the Bacteroidota was positively correlated with total carbon and negatively with total P. The relative abundance of Basidiomycota was affected by nearly all the variables.
Core microbiomes and functional annotations
To define core microbiomes in rhizosphere soil, we first selected those OTUs shared by all samples of each variety, then we used Venn diagrams to find those OTUs which were common to five varieties (Fig. 5). Then the relative abundance of core bacterial taxa or core fungal taxa must be more than 1% in whole bacterial or fungal dataset, respectively. Subsequently, 97 OTUs were regarded as core and 29 OTUs were as core fungi. Taken together, 5 bacterial OTUs and 172 fungal OTUs were defined as core microbiomes of endosphere.
The taxonomic analysis showed that the core bacteria in rhizosphere soil belonged to 9 phyla, 40 families and 43 generas (Supplementary file1). Subsequently, core bacteria (relative abundance > 1%) in rhizosphere soil mainly belonged to Proteobacteria, Actinobacteriota, and Firmicutes (Fig. 6A). Taken together, the relative abundance of core bacteria belonging to Enterobacteriaceae, Rhizobiaceae, Comamonadaceae, Sphingomonadaceae, Streptomycetaceae, Steroidobacteraceae, Bacillaceae, Methylophilaceae, Xanthomonadaceae, Paenibacillaceae, Microbacteriaceae, Nocardioidaceae were all more than 1%. Core fungi in rhizosphere soil belonged to 5 phyla, 15 families and 20 generas, and mainly belonged to Ascomycota, Basidiomycota, Mortierellomycota with relative abundance > 1% (Fig. 6C). The core fungi mainly belong to Ceratobasidiaceae, Lasiosphaeriaceae, Nectriaceae, Mortierellaceae, Stachybotryaceae, Bionectriaceae, Morosphaeriaceae and Chaetomiaceae.
Endophytic core bacteria all belonged to Proteobacteria (Fig. 6B). The endophytic core bacteria belong to Burkholderiaceae, Enterobacteriaceae and Mitochondria, respectively. Endophytic core fungi were belonged to Ascomycota, Rozellomycota, Basidiomycota, Mortierellomycota, Monoblepharomycota and others (Fig. 6D). Chaetomiaceae, Nectriaceae, Ascobolaceae, Phaeosphaeriaceae, Lasiosphaeriaceae, Onygenales fam Incertae sedis, Gymnoascaceae, Aspergillaceae and Metschnikowiaceae were main families of endophytic core fungi (relative abundance > 1%).
To gain further insights into the potential functioning of core microbiomes, the functional annotations according to FunGuild database were also displayed (Supplementary file2). There were 78 functional annotations for bacteria in rhizosphere soil and 8 annotations in endosphere (Supplementary file2). The predicted functions in rhizosphere soil were mainly associated with methanol oxidation, methylotrophy, chitinolysis, nitrogen fixation, aerobic chemoheterotrophy, aromatic compound degradation, nitrate reduction, predatory, ureolysis and chemoheterotrophy. The functions for endophytic core bacteria were mainly associated with fermentation, forming symbionts with plants, nitrate reduction, intracellular parasites, chemoheterotrophy. Furthermore, the major trophic modes of core fungi in rhizosphere soil were saprotroph, followed by pathotroph and symbiotroph. Core fungi in endosphere were mainly putative pathotroph, followed by saprotroph and symbiotroph.