Community CH1 degraded 1,4-dioxane efficiently and a degrader ZM13 was isolated from CH1
The microbial community CH1 enriched in this study had a highly efficient 1,4-dioxane degradation capability, which could degrade more than 98% of 50 mM 1,4-dioxane within 6 days (Additional file 1: Figure S1). With the increase of 1,4-dioxane concentrations, the growth rate initially increased and then decreased, which fitted the Haldane’s growth model well (Additional file 1: Figure S2) and the tolerance concentration was up to 190 mM (Additional file 1: Figure S1a). The maximum degradation rate of CH1 was 2.04 mg dioxane h− 1 mg protein− 1 at a cell yield of 0.38 mg protein/mg dioxane, which is higher than the most effective 1,4-dioxane degrader CB1190 (1.98 mg dioxane h− 1 mg protein− 1) [14]. An isolate that could utilize 1,4-dioxane as sole carbon and energy source was isolated from CH1, and was identified as Ancylobacter polymorphus and designated as ZM13 (Additional file 1: Figure S3).
Based on the degradation performances of CH1 at different concentrations of 1,4-dioxane (Additional file 1: Figure S1), we selected a high initial 1,4-dioxane concentration of 60 mM to conduct the microcosm experiment with five biological replicates for high consistency, which also showed enough experimental time for sampling. CH1 removed total 60 mM 1,4-dioxane to below detection levels within 8 days with a short and unobvious lag phase while 1,4-dioxane concentration in the abiotic control did not decline (Fig. 1a). Considering acidic intermediates that were continuously produced during 1,4-dioxane degradation, pH value was measured. As a result, the pH remained stable in the first two days and sharply decreased with a massive degradation of 1,4-dioxane (Fig. 1b), indicating the accumulation of acidic metabolites.
The bacterial community was affected by the addition of 1,4-dioxane and tended to stabilize with 1,4-dioxane exhaustion
To assess the change of community composition and structure during 1,4-dioxane degradation, sequencing of 16S rRNA gene amplicons was performed with a total of 13,356,940 raw reads obtained. The raw reads were then clustered at a similarity level of 99% and a total of 358 OTUs were obtained. α-diversity analysis showed that the bacterial diversity significantly (p < 0.05) increased right after the addition of 1,4-dioxane (Fig. 2a, b). Results of PCoA indicated that the samples collected from day 0 separated significantly (p < 0.05) with others (Fig. 2c), which is consistent with α-diversity analysis, and the separation degree gradually decreased with time and finally tended to be consistent. These results indicated that the high concentrations of 1,4-dioxane had a substantial impact on CH1, and the structure tended to stabilize with the exhaustion of 1,4-dioxane.
The taxonomy results were shown in Fig. 2d and Additional file 1: Figure S4. The composition of CH1 remained relatively stable during the microcosm experiment. The community was dominated by the phylum Proteobacteria and Alphaproteobacteria was the most abundant class (Additional file 1: Figure S4). Class Betaproteobacteria had a sharp increase on day 2 and gradually decreased from day 4, meanwhile class Gammaproteobacteria began to increase (Additional file 1: Figure S4). Abundances of some dominant genera had a significant (p < 0.05) change along with the 1,4-dioxane degradation processes (LSD, Additional file 1: Table S2). The relative abundance of Achromobacter sharply increased to 26.32% at day 1 and gradually decreased to 2.71% (Fig. 2d). Oligotropha was the dominant genus during the whole experiment while other dominant genera switched from Sphingopyxis (21.77–10.77%) to Aquamicrobium (6.63–18.23%) (Fig. 2d). The isolated 1,4-dioxane degrader, A. polymorphus, kept at a relative abundance of 0.5%-2% and its dynamic change seemed to be most consistent with Xanthobacter (LSD, Additional file 1: Table S2), indicating a potential cooperation between A. polymorphus and Xanthobacter. Moreover, the results of LEfSe analysis were presented in Additional file 1: Supplementary results and Figure S5.
Co-occurrence network analysis revealed a cooperation between ZM13 and 6 bacterial genera for 1,4-dioxane degradation
To investigate the interactions between ZM13 and other community members in CH1, OTUs from day 0 to day 8 were used to construct co-occurrence networks and the global network properties were listed in Additional file 1: Table S3. Totally, 113 of 358 OTUs were presented in the output network with strong (Spearman’s ρ > 0.66) and significant (p < 0.05) correlations, which generally indicated the co-occurrence patterns and the sharing niches were shaped by 1,4-dioxane degradation.
The network was divided into 7 modules with a good modularity index of 0.509, of which three distinct key modules, module Ⅰ, Ⅱ and Ⅲ, had OTUs with strong correlations with each other (Fig. 3a). The number of positive correlations (red edges) far exceeded that of negative correlations (blue edges) with a ratio of 81.83 (Fig. 3b), which implied a strong microbial cooperation outweighed competition during 1,4-dioxane degradation. Most of the negative correlations observed were between module Ⅰ and module Ⅱ (Fig. 3a). Also, OTUs belonged to Achromobacter, Sphingopyxis, Oligotropha, Rhodanobacter, Mersorhizobium, Alicycliphilus, and Hydrogenophaga had positive correlations with pH, while OTUs belonged to Aquamicrobium, Xanthomonas, Mesorhizobium, Afipia, Moheibacter, Lysobacter, Thermomonas, and Rhodopseudomonas had negative correlations with pH (Additional file 1: Figure S6). These results indicated that negative correlations might be caused by the microbial response to pH change during 1,4-dioxane degradation.
Although class Alphaproteobacteria had an overwhelming proportion to other class, Betaproteobacteria was the dominant class in the network (Additional file 1: Figure S7). Furthermore, the hubs (nodes with highest degree) were dominated by Betaproteobacteria while the bottlenecks (nodes with highest betweenness) were dominated by Alphaproteobacteria (Additional file 1: Table S4 and Table S5). Most of the hubs were identified as Achromobacter and the top 10 hubs were all affiliated with module Ⅰ (Additional file 1: Table S4), suggesting a potentially important role of the bacteria in module Ⅰ in the community assembly.
The 1,4-dioxane degrader ZM13 (OTU14) located in the position that connected the modules and did not seem to have a tight connection to any of the key modules in the network with only 7 correlations to other OTUs (Fig. 3b). A subnetwork centered on ZM13 was constructed to explore possible connections between ZM13 and other bacteria in the community (Fig. 3c). Specifically, ZM13 had positive correlations with Aquamicrobium, Mesorhizobium, Sphingopyxis, Xanthobacter, Cohnella and Achromobacter, and negative correlations with Pleomorphomonas (Additional file 1: Table S6). Nevertheless, ZM13 was recognized as one of the top-scoring bottlenecks located in the core of the network because of a high betweenness centrality of 873.55 (Additional file 1: Table S5). These results indicated that ZM13 was a keystone species in the biological network.
Identification of 1,4-dioxane-degradation-related genes in individual microbes by the combination of metagenomic and metatranscriptomic analyses
To investigate the metabolic capability and activity of individual microbes in microbial community CH1 during 1,4-dioxane degradation, an integrated analysis of metagenomic and metatranscriptomic data was applied with a total of 277,554,584 raw reads obtained from metagenomic sequencing and 540,603,556 raw reads obtained from metatranscriptomic sequencing.
We recovered 43 bins from metagenomic assemblies, from which four high-quality bins with high abundance in the community as well as high genome completeness (> 95%) and low genetic contamination (< 2%) were selected with the potential involvement in 1,4-dioxane degradation for further phylogenetic analysis and functional annotation (Table 1). The four acquired genomes were identified as genera Sphingopyxis, Mesorhizobium, Achromobacter and Xanthobacter, respectively, and a total of 87.68–89.97% of predicted ORFs of the four strains were identified using the RAST Server (Rapid Annotation using Subsystem Technology) (Table 1).
Table 1
Genomic information of species obtained from binning.
Bins
|
GTDB annotation
|
Genome size (Mbp)
|
GC%
|
Completeness (%)
|
Contamination (%)
|
No. of Scaffolds
|
No. of ORFs
|
Annotation ratio (%)
|
|
1
|
Sphingopyxis
|
3.43
|
65.27
|
99.3
|
1.76
|
12
|
3328
|
89.97
|
|
2
|
Mesorhizobium
|
4.55
|
63.43
|
96.55
|
1.78
|
131
|
4670
|
88.03
|
|
3
|
Achromobacter
|
6.73
|
67.32
|
98.6
|
0.57
|
56
|
6208
|
87.58
|
|
4
|
Xanthobacter
|
4.82
|
67.96
|
95.22
|
0.32
|
24
|
4678
|
88.68
|
|
Non-redundant gene catalogue (Unigenes) containing a total number of 297,123 genes was obtained from the predicted ORFs of metatranscriptomic sequencing with the total length of 179,797,590 bp. The overall descriptions of KEGG pathways during 1,4-dioxane degradation were presented in Additional file 1: Supplementary results and Figure S8. Further analyses were focused on the genes encoding enzymes that were possibly involved in 1,4-dioxane degradation, including monooxygenase genes, 1,4-dioxane metabolism intermediate-related genes, and glycolate and glyoxylate metabolism-related genes [18] that were expressed in ZM13 and the acquired bins. For the genome sequencing method and genome information of ZM13, see Additional file 1: Supplementary methods and Supplementary results.
All the differentially expressed genes potentially involved in 1,4-dioxane degradation were displayed in heat map and mapped to the genome of each strain (Additional file 1: Figure S9). The proposed 1,4-dioxane degradation pathway reported previously were shown in Additional file 1: Figure S10. The results indicated that CH1 possessed the genes responsible for glyoxylate metabolism pathways for 1,4-dioxane downstream metabolism (Additional file 1: Figure S9). The top expressed monooxygenase genes were all identified as toluene monooxygenase genes and were unique in ZM13 with high identities ranging from 97–100% (Additional file 1: Table S7 and Figure S9a). Moreover, ZM13 contained complete pathways for 1,4-dioxane degradation (Fig. 4a, b). These results indicated that ZM13 was a key degrader in 1,4-dioxane degradation.
The integrated meta-omics analysis revealed that although Mesorhizobium and Xanthobacter lacked monooxygenase genes for the first step of degradation, they contained upregulated genes for the degradation of 1,4-dioxane downstream metabolites (Fig. 4b, c, d and Additional file 1: Figure S9). Mesorhizobium lacked the genes responsible for converting 2-hydroxy-1,4-dioxane to 2-hydroxyethoxyacetic acid (2HEAA) (aldh), glycoaldehyde to glycolic acid (aldh) and glyoxylic acid to tartronate semialdehyde (gcl), but contained genes responsible for converting glycolate to malate (glcD, glcE, glcF, glcB, leuA) (Fig. 4b, c, d). Genes of aldh and gcl were only identified once in ZM13 and Xanthobacter, which could suggest that the dehydrogenation of aldehydes and the glyoxylate carboligase pathway might not be the main pathway for 1,4-dioxane degradation.
In conclusion, these results provided the evidence that A. polymorphus ZM13 was the key degrader that converted 1,4-dioxane to 2-hydroxy-1,4-dioxane and other intermediates that supported the growth of non-degrading populations, such as Mesorhizobium and Xanthobacter.