Introduction
Identifying the important factors that determine ecosystem function is a major challenge, and devising strategies to effectively manipulate them in order to obtain biological benefits is even more demanding
[1]. The soil microbiome is among the most complex systems for humans to manipulate and is directly connected with plant growth and health
[2]. Intensive agricultural practices characterized by the use of chemical fertilizers and pesticides are known to alter soil biology by disrupting biotic interactions
[3]. This can lead to the development of damaging soilborne diseases caused by an unbalanced proliferation of a subset of harmful microbes that encompass a set of plant pathogenic fungi and bacteria
[4,5]. Among these, Fusarium wilt disease, mainly caused by pathogenic
Fusarium oxysporum, is a major factor limiting several cropping systems
[6]. This pathogen can survive in soil over decades as chlamydospores, and effective methods of control or prevention remain to be developed
[7]. Thus, the exploration of efficient and practical strategies for
F. oxysporum control, such as developing strategies that benefit from indigenously developed soil suppressiveness, is urgently needed.
Soil disease suppression is a phenomenon essentially mediated by soil microbiota that has been divided into two categories: general and specific suppression
[2]. General suppression is associated with the biomass, activity and diversity of the soil microbiome
[2], and specific suppression is directly associated with a particular microbe (or a consortium of microbes) that directly antagonizes the pathogen in the system
[8]. Recently, there has been a growing consensus that soil suppressiveness is stimulated by agricultural practices associated with organic matter manipulation
[8,9]. Hence, a better understanding of abiotic factors structuring disease-suppressive soils is key to developing alternative practices to promote soil health.
The rhizosphere is the zone where a complex microbial network interacts with pathogens and influences the outcome of infection
[8]. The composition of the resident microbial community in the rhizosphere is of critical importance and has a vital role to the success of pathogen invasion
[5,8,10]. Previous studies showed that application of a biofertilizer consisting of
Bacillus amyloliquefaciens and compost resulted in the control of Fusarium wilt disease by changing the composition and activity of the resident rhizosphere microbes
[4,11]. It is also important to note that changes imposed in bulk soil, for instance by agricultural practices, have a major role in the composition of rhizosphere communities
[12]. However, numerous studies have focused on determining suppressive bulk soil microbiomes via integrated soil amendments and there is little information on the relationship between the bulk and rhizosphere microbiomes with respect to disease suppression.
In banana crops worldwide, a particular strain of the fungus
Fusarium (
F. oxysporum f. sp.
cubense) causes Fusarium wilt (or Panama disease)
[13]. Here, we investigated the biological basis of Fusarium disease suppression induced by organic amendments in banana stands. We hypothesized that the enhanced soil suppressiveness induced by management practices was initially related to bulk soil microbial communities that subsequently determined the suppressive rhizosphere microbiota. A better knowledge of the mechanisms that trigger the immune response of soils can lead to optimized crop management strategies that enhance disease suppression with the goal of improving plant health and securing future crop yields.
Materials and methods
Experimental system
The experimental site is located in Chengmai County (19°65′ N, 109°92′ E), Hainan Province, one of the major areas of banana production in China. This region has been recently impacted by banana Fusarium wilt. The soil is a Acric Ferralsol with a pH of 4.83 (1:5 soil:water), organic matter content of 10.2 g·kg
−1, total nitrogen content of 0.79 g·kg
−1, electrical conductivity of 20.9 μs·cm
−1, available phosphorus of 31.8 mg·kg
−1, and available potassium of 64.6 mg·kg
−1. The field experiment was conducted over two consecutive years, 2012 and 2013. In February 2012, one area covered with
Eucalyptus and
Acacia mangium was converted into a banana plantation. Two management regimes in areas of 0.65 ha were established. These regimes were (1) a bio-organic system (BIO), soil amended with bio-organic fertilizer at 12000 and 8000 kg·ha
−1 for the first and second seasons, respectively, lime (Ca-Mg powder) at 3750 kg·ha
−1 each season, and essential mineral fertilizers; and (2) an organic system (CF), soil amended with chicken manure and essential mineral fertilizers. The bacterium
Bacillus
amyloliquefaciens strain NJN-6 was part of the bio-organic fertilizer treatment and acts as a biocontrol agent against Fusarium wilt
[4] at a concentration ˃ 1 × 10
8 CFU·g
−1 dry weight (at the end of the fermentation). In the first year the field was planted with banana tissue culture plantlets (
Musa acuminata AAA Cavendish cv. Brazil) at a density of 2400 seedlings ha
−1. All mother banana plants and unnecessary suckers were cut down two months after harvest, leaving the best sucker per plant for the cropping cycle. Information about the production of the bio-organic fertilizer, other management practices applied in the field and methods of identifying the disease incidence and banana yield has been published previously
[7].
Sample collection and soil DNA isolation
Soil samples were collected in September 2013 before harvest. A systematic sampling approach
[14] was adopted to collect 10 individual soil samples from each field treatment (Supplementary materials, Fig. S1). Briefly, each field was divided into plots of 10 m × 10 m in a grid and 10 plots 10 m apart were selected in a W shape for sampling. Within each plot, five banana plants at least 4 m apart were randomly selected and five soil cores (25 cm deep × 2.5 cm diameter) around a 0.5 m radius of each banana plant were collected and pooled as composite bulk soil samples. Rhizosphere soils were obtained as previously described
[7]. The soil samples were immediately stored at
-80°C for further DNA isolation. A total of 20 bulk and 20 rhizosphere soil samples were collected (2 fertilizer treatments × 10 replicates per treatment). DNA was isolated using a PowerSoil DNA Isolation Kit (Mobio Laboratories, Carlsbad, CA) following the manufacturer’s instructions. The concentration and quality of the extracted DNA were determined using a NanoDrop 2000 spectrophotometer (Thermo Scientific, Waltham, MA).
Quantitative PCR analysis
Copy numbers of marker genes accounting for bacteria
[15], fungi
[15],
B.
amyloliquefaciens NJN-6
[4] and
F.
oxysporum[16] were determined using gene-specific primers (Supplementary materials, Table S1) and SYBR
Premix Ex TaqTMII (Takara Bio Inc., Kusatsu, Japan) following the manufacturer’s instructions.
Pseudomonas was detected using a combination of primers and probes (Supplementary materials, Table S1) as described by Bergmark et al.
[17]. The results are expressed as lg values (target copy number g
−1 soil).
MiSeq sequencing and sequence data processing
The V4 region of the bacterial 16S rRNA gene was amplified from the soil genomic DNA using the primer sets 515F and 806R
[18]. For fungi the first internal transcribed spacer (ITS) region was amplified by the primer set ITS1F/ITS2
[19] (Supplementary materials, Table S2). PCR conditions and the protocol for library preparation were conducted as previously described
[11]. The libraries were sequenced on an Illumina MiSeq platform at Novogene Bioinformatics Technology Co., Ltd. (Beijing, China). The resulting raw sequences were processed using QIIME (1.8.0) to demultiplex and remove adaptor and primer sequences
[20]. Sequences were then paired using FLASH v1.2.7. Merged sequences were filtered and clustered using USEARCH, UPARSE, and Perl scripts to remove low-quality sequences
[21]. OTU tables were generated using 97% nucleotide identity and sequences were annotated using the RDP naïve Bayesian classifier for bacteria
[22] and UNITE for fungal sequences
[23]. All sequence data are available through accession number SRP072164 in the NCBI Sequence Read Archive.
Statistical analysis
All statistical tests were conducted in R v3.2.0
[24] and considered significant at
P<0.05. Non-normal data were square-root or log-transformed to meet test assumptions. Significant differences between samples were determined by two-tailed Student’s or Welch’s
t-tests or the Wilcoxon rank sum test. Prior to statistical tests and community metrics inferences the original OTU tables were rarefied at depths of 8397 sequences for bacteria and 8955 sequences for fungi per sample.
α- and β-diversity metrics
α-diversity (the number and abundance of taxa within communities) and β-diversity (compositional dissimilarity between communities) metrics were adopted to characterize the soil microbiomes. The number of observed OTUs (S
obs) and Faith’s phylogenetic diversity (PD) index were determined using Mothur
[25]. β-diversity of both bacterial and fungal communities was determined using non-metric multidimensional scaling (NMDS) analysis based on the Bray-Curtis distance matrices in Mothur
[25]. Analysis of similarity (ANOSIM)
[26] and permutational multivariate analysis of variance (PERMANOVA, 999 permutations) were conducted to test for significant differences among microbial composition of samples using the “vegan” package in R. Multiple regression tree (MRT) analysis, based on the Bray-Curtis distance metric, was conducted to evaluate the relative influences of management and the soil compartment on the microbiome using “vegan”, “mvpart”, and “MVPARTwrap” packages in R. Differences in the relative abundance of bacterial and fungal genera between BIO and CF were conducted using STAMP
[27].
P-values were calculated using a two-sided Welch’s
t-test and confidence intervals were calculated using Welch’s inverted method. The false discovery rate (FDR) was calculated using Benjamini-Hochberg with
q<0.05. Spearman correlations were used to relate the relative abundance of specific bacterial taxa with copy numbers of
F.
oxysporum using the package “stat” in R.
Structural equation modeling
Structural equation modeling (SEM) was constructed to tease apart indirect and direct effects of bulk soil microbiota on rhizosphere microbiota in a multivariate approach using the packages “sem” and “lavaan” in R. The first axis of NMDS analysis comprising Pseudomonas, Duganella, Gp6, Terrimonas, Cupriavidus, and Ohtaekwangia was used to quantify rhizosphere-responsive OTUs. We quantified F. oxysporum and NJN-6 abundances using targeted gene copy numbers. The bacterial and fungal community composition was quantified using the third and second axes of the NMDS, respectively. All variables were standardized using the scale function in R. Goodness-of-fit was evaluated on the basis of a c2 test (P>0.05 indicates a good model fit).
Results
Effects of soil management on Fusarium wilt disease incidence and fruit yield
We observed an overall increase in Fusarium wilt disease incidence in the second year in both BIO and CF systems. However, the rate of disease increase differed between systems. The rate of disease in the BIO treatment increased from 2.9% to 13.2% while the rate in CF increased from 10.1% to 50.3% (Fig. 1(a)). These results indicate that the BIO system greatly contributed to a lower disease incidence in the newly converted banana fields. In addition, the BIO system significantly enhanced the average banana yield per plant compared to the yield from the CF system (the BIO system yield was 16.0% higher than that in the CF system in the first year and 18.9% higher in the second year) (Fig. 1(b)).
Differences in community abundance and α-diversity
qPCR results showed that significantly more bacteria (Welch’s t-test, P<0.001) and fewer fungi were detected in BIO bulk soil (BIOB) than in the bulk soil from CF (CFB), and results from rhizosphere soil samples showed a similar tendency (Fig. 2). The BIO system led to significantly higher bacterial diversity (Faith’s PD) (Student’s t-test, P<0.05) in BIOB compared to that found in CFB, however there were no significant trends observed for bacteria in rhizosphere soil and fungi in bulk and rhizosphere soils (Fig. 2). Furthermore, a significantly higher bacterial richness (Sobs) was observed in soils collected from BIO compared to CF (Welch’s t-test, P<0.01). Fungal results showed the opposite trends, with rhizosphere soils showing a significant difference (Fig. 2).
Changes in microbiome β-diversity
As shown in Fig. 3(a) and 3(b), NMDS plots showed differences in the bacterial and fungal community composition in BIO and CF (PERMANOVA, P<0.001; ANOSIM, P<0.001; Supplementary materials, Table S3). BIO was distinctly separated from CF along the NMDS1-NMDS2 plane and NMDS1-NMDS3 plane, respectively, for bacteria and fungi. The fertilization scheme and soil compartment explained 28% and 14% of the variation, respectively, for bacteria and 14% and 16% for fungi (Supplementary materials, Table S3). MRT analysis showed similar trends in which the fertilization scheme accounted for the largest proportion of variation explaining the microbiome composition, followed by the soil compartment (Fig. 3(c) and 3(d)).
Depicting microbial taxa potentially associated with disease suppression
After STAMP analysis, significant differences in bulk and rhizosphere soil microbial composition between BIO and CF were observed (Supplementary materials, Fig. S2 and Fig. S3). Significant increases were observed in OTUs associated with Cupriavidus, Duganella, Terrimonas, Gp6, Gp4, Nitrospira, Ohtaekwangia, Pseudomonas, Gemmatimonas, Flavobacterium, and Planctomyces (Benjamini-Hochberg FDR, q<0.05) in rhizosphere samples in the BIO system. Of these, Terrimonas, Pseudomonas, Cupriavidus, Gp6, Ohtaekwangia, and Duganella were also enriched in the bulk soil (Benjamini-Hochberg FDR, q<0.05) (Supplementary materials, Fig. S2). Regarding the fungi, only one unidentified genus belonging to Sordariomycetes differed in relative abundance between BIOB and CFB (Supplementary materials, Fig. S3). However, in the rhizosphere, significantly higher relative abundances of two taxa, Sordariomycetes (unidentified) and Microascaceae (unidentified), and significantly lower relative abundances of Aspergillus, Sordariaceae (unidentified), Fusarium, Penicillium, Retroconis, Purpureocillium, Trichocomaceae (unidentified), Humicola, Clonostachys, Chaetomiaceae (unidentified), Chaetomium, Acaulospora, Mortierella, Calonectria, Trichocladium, Scedosporium and Sordariales (unidentified) (Benjamini-Hochberg FDR, q<0.05), were found in BIO than in CF. Moreover, significantly lower abundance of F. oxysporum (Student’s t-test, P<0.001) and higher abundance of Pseudomonas (Welch’s t-test, P<0.001) in BIO rhizosphere samples were validated using qPCR (Supplementary materials, Fig. S4). Although a higher relative abundance of Bacillus was not observed, the biocontrol agent B. amyloliquefaciens NJN-6 was successfully detected in both bulk and rhizosphere soil samples (Supplementary materials, Fig. S4).
Spearman correlations were conducted between F. oxysporum copy number and the relative abundances of specific bacterial genera that significantly responded to BIO management. These were potentially associated with wilt disease suppression (Fig. 4). As shown in Fig. 4, the F. oxysporum copy number was negatively correlated with Pseudomonas (r = -0.81, P<0.0001), Duganella (r = -0.75, P = 0.0003), Gp6 (r = -0.65, P = 0.03), Terrimonas (r = -0.74, P = 0.0003), Cupriavidus (r = -0.81, P<0.0001) and Ohtaekwangia (r = -0.57, P = 0.01).
Discussion
A practical fertilization strategy, namely application of BIO in the newly reclaimed fields, gave highly efficient biocontrol efficacy in the pre-control of Fusarium wilt disease. Our results are consistent with previous studies in which the continuous application of BIO to recently established agricultural sites or continuous plantation with banana both produced enhanced suppression of Fusarium wilt disease
[4,10]. The field results provide a unique opportunity to explore in more detail the relationships between the disease-suppressive bulk soil and rhizosphere microbiomes.
Higher bacterial abundance (qPCR), diversity (Faith’s PD), and richness (S
obs) and lower fungal abundance, diversity, and richness were observed in biofertilizer-amended soil, and results from rhizosphere soil samples showed trends similar to those in bulk soil. These results are in line with a previous study in which, compared to the control, the α-diversity of bacteria significantly increased whereas fungal diversity decreased after two years of biofertilizer application
[10]. This illustrates the potential boost of soil bacterial activity by novel fertilization strategies which was ultimately reflected in its variation. Higher bacterial diversity has been observed to be advantageous in soil disease suppression
[28], and microbial diversity is becoming progressively recognized as a property that hinders pathogen establishment in soils
[29]. Thus, our findings indicate that higher bacterial community abundance, diversity and richness in the rhizosphere may have created a more phylogenetically diverse community that occupies the majority of the available niches in soil, thus restricting the further multiplication and development of the pathogen in the system.
NMDS and MRT both revealed significant differences in bulk soil bacterial and fungal community composition between the different fertilization strategies. This finding indicates that different soil amendments induce differences in microbial composition
[30], and PGPR-containing bio-organic fertilizers have been broadly confirmed to have a significant effect in shaping soil microbial communities
[5,10]. Importantly, we found similar variation in bacterial and fungal communities in rhizosphere and bulk soil samples. As previously shown
[31,32], we also found that the rhizosphere microbial composition was largely dependent on the composition of the bulk soil microbiota. In addition, fertilization and the soil compartment had important roles in determining the composition of the microbiome. Consistent with our results, fertilization has been reported to influence microbial composition (structure) in the soil and rhizosphere in different crop systems
[4,33,34]. Hence, we show that the fertilization pattern initially altered the community composition of the bulk soil microbiome and this further resulted in changes to their respective rhizosphere microbiomes.
The abundance of the pathogen was negatively correlated with bacteria belonging to the genera
Pseudomonas,
Duganella,
Cupriavidus,
Terrimonas,
Ohtaekwangia, and
Gp6, all of which were enriched in both bulk soil and rhizosphere samples in BIO.
Pseudomonas has been described as having a wide spectrum of biological activities
[35] such as antibiosis, induced systemic resistance and plant growth promotion, and this genus has already been noted to be associated with the suppression of Fusarium wilt on banana
[36].
Duganella, a member of the family Oxalobacteraceae, is well-known for its antifungal effects including against
Fusarium, and the antifungal activity is most likely induced by the synthesis of chitinases
[37]. Although no antagonistic activity against
F.
oxysporum was observed, interplay of
Cupriavidus with some other non-antagonistic bacteria can significantly contribute to the development of suppression against
F.
oxysporum both
in vitro and
in planta[38]. Furthermore,
Cupriavidus can produce lipopeptide siderophores such as taiwachelin
[39] which may mediate in competition for iron and induced resistance to suppress pathogenic fungi
[40]. Although there has been no report that the genera
Terrimonas and
Ohtaekwangia possess specific biocontrol activity against
F. oxysporum, these two genera were identified as key groups that confer soil disease-suppressiveness against Fusarium wilt pathogen invasion
[41]. In addition, species in the Chitinophagaceae and Cytophagales were reported to be producers of chitinolytic enzymes which are involved in fungal cell wall lysis and chitin degradation
[42]. The
Gp6 group was reported to occur in higher relative abundance in potato common scab and banana Fusarium wilt disease-suppressive soils than in disease-conducive soils
[4,41,43]. Despite this indication, the actual role of
Gp6 influencing disease suppression is still unknown. Only one unidentified genus belonging to the Sordariomycetes differed in relative abundance between BIO and CF. However, in the rhizosphere, a significantly lower relative abundance of
Fusarium was observed in BIO compared to CF. Moreover, the abundance of
Pseudomonas was further detected by qPCR and demonstrated a similar trend as that observed in the sequencing results. Hence, in addition to the microbes amended with the biofertilizers (
B.
amyloliquefaciens), which can be detected both in BIO bulk and rhizosphere soils, the increased relative abundances of these indigenous (and potentially antagonistic) species may likely be involved in Fusarium wilt disease suppression, for instance through taxa-specific mechanisms.
Conclusions
Here, we have demonstrated efficient Fusarium wilt disease suppression capacity in newly converted fields with the application of bio-organic fertilizer. As a summary of the variation in the SEM model (Fig. 5), the changes in bulk soil bacterial community determined its induced rhizosphere bacterial community, and serves as an important and direct factor in restraining the pathogen. In addition, biocontrol agents and responsive bacterial genera both act as direct disease suppression indicators. Collectively, understanding how different organic amendments affect the assembly and functioning of microbiomes is the basis for exploring robust soil practices to manipulate bulk and rhizosphere soil systems. We also propose that the beneficial effects of taxa-specific suppression should be considered in the design of bio-organic fertilizers and their use in sustainable strategies for plant protection against diverse disease agents.
The Author(s) 2020. Published by Higher Education Press. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0)