The effects of the recombinant YeaZ of Vibrio harveyi on the resuscitation and growth of soil bacteria in extreme soil environment

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Microbiology

Introduction

Many microorganisms inhabit the natural environments, but only 0.01–10% of these can be cultured using traditional techniques (Pace, 1997; Colwell et al., 1985; Oliver, 2010; Ding, Su & Yokota, 2011). In adverse environments, such as dry, hot and salt areas, it is difficult to isolate these bacteria by traditional techniques. Jookar et al. (2014) investigated the bacterial diversity of water, soil, sediment and salt samples from the east and western sites of Lake Urmia, Iran. The study is of great significance for exploring the extreme environmental microbial diversity, gene pool and the potential use of this information in biotechnology applications. Ma et al. (2009) studied the halophilic actinomycetes diversities of mud volcano and found that a large number of unknown microorganisms in Xinjiang, China. However, most of the bacteria in extreme environments cannot be obtained by using traditional pure cultivating method at present; most of them are in viable but non-culturable state and with low metabolic activities. But these metabolically active bacteria play an important role in soil nutrient cycling, biodegradation of pollutants, food safety, etc. (Su et al., 2013; Liu et al., 2016). These VBNC cells are intact and alive and can be resuscitated in favorable conditions.

A secreted protein, resuscitation promoting factor (Rpf) was first found in the supernatant of Micrococcus luteus, which has been considered essential for the resuscitation of dormant cells (Mukamolova et al., 1998). Rpf can resuscitate and promote the growth of Gram-positive and Gram-negative bacteria, including Mycobacterium spp., Rhodococcus spp., Arthrobacter spp., Bacillus spp., Paenibacillus spp. and Curvibacter fontanus (Ding & Yokota, 2010; Ding et al., 2012). It was also reported that the addition of the purified recombinant Rpf from M. luteus could recover the VBNC bacteria in the natural environment (Zou et al., 2014; Liu, 2007; Yu et al., 2015). Liu et al. (2016) reported that VBNC bacteria were isolated from sewage treatment systems using a culture supernatant from M. luteus containing Rpf. Puspita et al. (2015) reported the effect of Tomitella biformata-derived Rpf on the bacterial colony formation from a permafrost ice wedge, and found that the Rpf increased the number of colonies of Actinobacteria during the early stages of incubation, promoted growth of T. biformata from the permafrost ice wedge and exhibited cross species activity. In another study by Jin (2014), the total number of culturable bacteria increased from 7.5 × 106 to 2.4 × 108 cell/g of printing and dyeing wastewater samples by adding Rpf.. The number of culturable bacteria of pharmaceutical wastewater samples increased from 1.5 × 106 to 2.4 × 108 cell/g with in the presence of Rpf and the recovery rate of VBNC was (47.8–98.2)% (Zou et al., 2014).

Beside this, Rpf plays a significant role in enhancing the activity of bacterial communities in a polluted environment. Fida et al. (2017) found that a poly cyclic aromatic hydrocarbon (PAH) degrading bacterium Novosphingobium sp. LH128 of VBNC state were resuscitated by Rpf addition. A total of thirteen strains with heterotrophic nitrification ability were resuscitated by Rpf addition in a nitrogen polluted river (Su et al., 2019a). Su et al. (2019b) reported that Rpf from Micrococcus luteus may improve the degradative performance of bacterial populations and significantly enhanced phenol removal under high salinity stress. Ye et al. (2020) demonstrated that Rpf enhances PCB degradation by resuscitating PCB-degrading bacteria. Yu et al. (2020) revealed that the Rpf from Micrococcus luteus increased the abundances of Actinobacteria and Proteobacteria phyla which are involved in nutrient and phenol removal. Although there are many studies on the Rpf recovery of VBNC strains, the research on yeaZ recovery is relatively limited.

YeaZ is also a resuscitation factor like Rpf (Panutdaporn et al., 2006; Nichols et al., 2006), which has the similar stimulatory effect on bacterial resuscitation in several species, such as Vibrio parahaemolyticus, Escherichia coli and Salmonella typhimurium (Panutdaporn et al., 2006; Handford et al., 2009; Aydin et al., 2011). Previously, Li et al. (2016) cloned and expressed the yeaZ gene of Vibrio harveyi SF-1 and found that YeaZ has an indispensable effect on the resuscitation of VBNC. To investigate the promoting effect of YeaZ on the VBNC or uncultured bacteria in the extreme environment, two extreme environmental soil samples were selected, including volcanic soil and saline soil in Northwest China. The purified YeaZ of V. harveyi was prepared and added to the soil samples. The promoting effect was determined by using bacterial plate count and clone isolation methods.

Materials and Methods

Bacterial strains and culture media

V. harveyi SF-1 was isolated from diseased seabass (Lateolabrax japonicus) in China. The yea Z gene was cloned from the genomic DNA of V. harveyi SF-1, expressed in E. coli BL21 and purified by Ni2+-affinity chromatography, respectively (Li et al., 2016). The culture broth supplemented with pure activated or inactivated YeaZ protein was used for YeaZ treatment groups and the culture broth without YeaZ protein was used as the control group (Ding et al., 2012; Zou et al., 2014).

E. coli and other isolated bacteria were cultivated on Luria-Bertani (LB) nutrient agar containing 5.0 g peptone, 10 g yeast extract, 10 g sodium chloride (NaCl) and 20 g agar at pH 7.0 for 1,000 mL.

Soil sampling

The study sites were located in the volcanic land (sample 1) of Xinjiang (89°30.779 E, 42°55.476 N) and saline land of Minqin (sample 2) of Gansu (103.64°E, 39.14°N) in China. Sample 1 is located in the northern edge of the Turpan Basin with a typical continental arid desert climate and the high air temperature (47.8 °C) in China. Sample 2 is located in the saline land of Minqin, which is located in the east of Tengger Desert, north of Inner Mongolia Badain Jaran Desert and west of the Qilian Mountains. The residues and impurities on the surface of the soil were cleaned up in the sample plots of volcanic soil and saline soil. A total of 6 soil samples (three random samples per environment) were taken from the surface soil (0–20 cm) by a 5-point sampling method. The samples were divided into 2 parts and put into sterile brown paper bags and brought back to the laboratory. One fresh soil sample was passed through a 2 mm sieve to determine the number of soil microbial functional bacteria, and the other was air dried and sieved to determine the physical and chemical properties of the soil. The physical and chemical properties of the soil are determined according to soil agrochemical analysis (Institute of Soil Science and Chinese Academy of Sciences, 1978). The soil moisture content is measured by the fresh soil drying method at 105 °C, and the soil pH value is measured by the glass electrode method with a water-soil ratio of 1:1 (Saul-Tcherkas, Unc & Steinberger, 2013). DNA was extracted from the soil samples with the genomic DNA extraction kit (Sangon Biotech Co. Ltd., Shanghai, China) after the soil samples were received in the laboratory.

Bacterial plate count

The plate count method was used for determining the total number of culturable bacteria in the samples (Min et al., 2014). The LB liquid media supplemented with 10% activated or inactivated YeaZ protein (0.02 mg⋅mL−1) was used in treatment groups, and the LB liquid media without YeaZ protein was used as the control group. As previously described in Li et al. (2017), 10 g of each soil sample was suspended in 90 mL of sterile distilled water and was shaken for 20–30 min at 25 °C on a Thermostat oscillator. Soil sample solution (1%) was added to LB media with or without YeaZ protein, and was incubated at a constant temperature of 30 °C. After incubating for 12–24 h, the number of cultivable cells was detected by plate counting and spectrophotometry, and the dominant flora of different colony morphologies was selected for analysis.

16S rDNA gene sequencing and phylogenetic analysis

As previously described in Li et al. (2017), the total bacterial DNA was extracted with Ezup column bacterial genomic DNA extraction kit, and the 16S rRNA gene universal primers 27-F (5′-AGA GTT TGA TCC TGG CTC AG-3′) and 1492-R (5′-GGT TAC CTT GTT ACG CTT-3′) were used for PCR amplification. The PCR reaction system and the reaction cycle parameters refer to the description of Geetha & Manonmani (2010). The PCR products were detected by 1% agarose gel electrophoresis and sent to Shanghai Bioengineering Co., Ltd. for sequencing. The sequencing results were analyzed with the Basic Local Alignment Search Tool (BLAST) option of the National Centre for Biotechnology Information (NCBI) database (http://www.ncbi.nlm.nih.gov/). The sequences acquired in this study were deposited in the GenBank database (Accession no.: KY987120KY987153). Phylogenetic trees were constructed with MEGA 5.0 software using the neighbor-joining method (Tamura et al., 2011).

Statistical analyses

The all experimental data was processed by Origin 8.0 software (OriginLab Corp., USA). One-way ANOVA and Duncan’s test were performed to assess the statistically significant differences of the number of total bacteria in control and treatment groups by using SPSS Base Ver.13.0 Statistical software (SPSS, IL, Chicago, the United States) (P < 0.05).

Results

Culturable bacterial counts

After incubating for 13 h, the treatment groups became turbid (Fig. 1), indicated that YeaZ could promote bacterial recovery. The total bacterial populations of the volcanic land and saline land samples were shown in Table 1. The culturable bacterial counts in the volcanic land samples increased from 0.17 × 103 cfu⋅ml−1 to 1.00 × 103 cfu⋅ml−1 by addition of the activated YeaZ. Meanwhile, the culturable bacterial counts from the saline land samples increased from 2.03 × 103 to 5.55 × 103 cfu⋅ml−1 by the addition of activated YeaZ. This study defines the resurrection rates to represent the resuscitation and promoting results of recombinant YeaZ to the VBNC cells. The resurrection rates of the VBNC bacteria in volcanic and saline lands were 83.00% and 63.42%, respectively, and the recombination effect of YeaZ reached 5.88 and 2.73 times respectively in volcanic and saline lands, which showed the significant differences in bacterial populations between the treatment and the control groups (p < 0.05). The resuscitation of the VBNC bacteria with YeaZ of V. harveyi was displayed, and the number of culturable bacteria increased significantly after the addition of YeaZ in the soil samples.

Growth of control and treatment groups.

Figure 1: Growth of control and treatment groups.

(A) Control; (B) saline land+activated YeaZ; (C) volcanic land+activated YeaZ; (D) saline land+inactivated YeaZ; (E) volcanic land+inactivated YeaZ.
Table 1:
Number of total bacteria of control and treatment groups in agar plates.
Resurrection rate (%) = (Total number of bacteria in treatment group-Total number of bacteria in control group) / (Total number of bacteria in treatment group × 100). Results are expressed as the mean ± standard deviation of three independent tests. One way analysis of variance (ANOVA) and multiple comparisons of significant differences were performed using Duncan’s test. Different letters in the same line meant significant difference at 0.05 level.
Treatment group 1 (+YeaZ) Treatment group 2 (+inactivated YeaZ) Control group (-YeaZ) Resurrection rate of VBNC bacteria (%)
Volcanic land (1.00 ± 0.15) × 103 a (0.33 ± 0.15) × 103 b (0.17 ± 0.08) × 103 b 83.00
Saline land (5.55 ± 0.15) × 103 a (1.69 ± 0.10) × 103 b (2.03 ± 0.14) × 103 c 63.42
DOI: 10.7717/peerj.10342/table-1

Notes:

Resurrection rate (%) = (Total number of bacteria in treatment group-Total number of bacteria in control group) / Total number of bacteria in treatment group × 100.

Results are expressed as the mean ± standard deviation of three independent tests.

One way analysis of variance (ANOVA) and multiple comparisons of significant differences were performed using Duncan’s test. Different letters in the same line meant significant difference at 0.05 level.

Diversities of the culturable bacteria

Thirteen bacterial strains were isolated from the soil samples of volcanic land, while twenty-one bacterial strains were obtained from the soil samples of saline land (Table 2). The bacteria from volcanic land soil belonged to three phylogenetic groups of Actinobacteria, Firmicutes and Gammaproteobacteria (Fig. 2A). Only four species, including Ornithinimicrobium kibberense, Agrococcus citreus, Stenotrophomonas rhizophila and Pseudomonas zhaodongensis were found in the control group, while further species were isolated from the treatment groups. Micrococcus antarcticus, Kocuria rose, Salinibacterium xinjiangense and Planococcus antarcticus were only found in the treatment groups.

Table 2:
Genetic homology of 16S rDNA gene sequences of the isolated strains.
Volcanic Land Saline Land
Strain number Closest type strain Similarity (%) Genbank accession number Strain number Closest type strain Similarity (%) Genbank accession number
XJR1 Salinibacterium xinjiangense 98 KY987120 YHR-1 Bacillus licheniformis 99 KY987133
XJR2 Salinibacterium xinjiangense 98 KY987121 YHR-2 Planococcus rifietoensis 100 KY987134
XJR3 Salinibacterium xinjiangense 98 KY987122 YHR-3 Bacillus oceanisediminis 100 KY987135
XJR4 Pseudomonas zhaodongensis 99 KY987123 YHR-4 Brevibacillus brevis 99 KY987136
XJR5 Micrococcus antarcticus 99 KY987124 YHR-5 Bacillus litoralis 98 KY987137
XJR6 Pseudomonas zhaodongensis 99 KY987125 YHR-6 Paenibacillus xylanilyticus 99 KY987138
XJR7 Ornithinimicrobium kibberense 99 KY987126 YHR-7 Microbacterium maritypicum 99 KY987139
XJR8 Kocuria rosea 99 KY987127 YHR-8 Bacillus subtilis 100 KY987140
XJR9 Planococcus antarcticus 99 KY987128 YHR-9 Oceanimonas doudoroffii 97 KY987141
XJ1 Stenotrophomonas rhizophilo 99 KY987129 YHR-10 Zobellella taiwanensis 97 KY987142
XJ2 Agrococcus citreus 99 KY987130 YHR-11 Bacillus alcalophilus 97 KY987143
XJ3 Ornithinimicrobium kibberense 99 KY987131 YHR-12 Bacillus pumilus 99 KY987144
XJ4 Pseudomonas zhaodongensis 99 KY987132 YHR-13 Bacillus niabensis 98 KY987145
YH-1 Bacillus litoralis 99 KY987146
YH-2 Planococcus rifietoensis 100 KY987147
YH-3 Bacillus licheniformis 99 KY987148
YH-4 Photobacterium halotolerans 99 KY987149
YH-5 Rheinheimera aquimaris 98 KY987150
YH-6 Bacillus amyloliquefaciens 99 KY987151
YH-7 Bacillus litoralis 98 KY987152
YH-8 Bacillus pumilus 99 KY987153
DOI: 10.7717/peerj.10342/table-2
Phylogenetic trees of culturable bacterial communities of different soils.

Figure 2: Phylogenetic trees of culturable bacterial communities of different soils.

(A) Volcanic land; (B) saline land.

The isolated bacteria from the saline land soil also belonged to the phyla Firmicutes, Actinobacteria and Gammaproteobacteria (Fig. 2B). The majority of the bacterial species belonged to the genus Bacillus. Eight bacterial species in the control soil sample of saline land showed high similarities with Bacillus litoralis, Planococcus rifietoensis, B. licheniformis, Photobacterium halotolerans, Rheinheimera aquimaris, B. amyloliquefaciens, and B. pumilus. The culturable bacterial community in the treatment groups was more diverse than that of the control group. Nine species were only found in treatment groups, including B. oceanisediminis, Brevibacillus brevis, Paenibacillus xylanilyticus, Microbacterium maritypicum, B. subtilis, B. alcalophilus, B. niabensis, Oceanimonas doudoroffii and Zobellella taiwanensis. Among these, Bacillus species increased significantly. The abundance of each genus varied in the soil samples of volcanic land (Fig. 3A). Salinibacterium, Pseudomonas and Ornithinmicrobium were the predominant species and accounting for 23.08%, 23.08% and 15.39% in volcanic land, respectively. The distribution of different culturable bacteria from the saline land soil has shown in Fig. 3B. Bacillus was the most abundant group in the saline land, accounting for 57.15% of the total number.

Relative genus abundance of the different soils.

Figure 3: Relative genus abundance of the different soils.

(A) Volcanic land; (B) saline land.

Discussion

The microorganisms of the extreme environments (volcanic and saline lands) tend to have a unique genetic type, which can produce special metabolites and bioactive substances. These microbes have a wide range of application values. The volcanic land of Xinjiang and saline land of Minqin are located in the special geographical location with special natural environmental conditions for the growth of high temperature, salt-tolerant and drought-resistant microorganisms. However, numerous bacteria could be in the VBNC state due to the extreme environmental stresses. The Rpf has been confirmed to be directly related to the resuscitation of VBNC bacteria. It not only has an effect on Gram-positive bacteria, but also has a good growth-promoting function for some Gram-negative bacteria. Yu et al. (2015) reported that the Rpf of Gram-positive M. luteus could increase the number of bacterial species in the soil of Xinjiang. The rpf genes of M. luteus are widespread among high G+C Gram-positive bacteria, such as M. tuberculosis (contains five rpf genes) (Downing et al., 2004). Rpf protein is similar to soluble lytic transglycosylases, which digests the peptidoglycan in the bacterial cell wall and the digested peptidoglycans may function as signaling molecules for the growth initiation and resuscitation of the VBNC bacterial cells (Mukamolova et al., 2006). The Rpf of M. luteus could mainly promote the growth of the Gram-positive bacteria. However, it also promotes the growth of some Gram-negative bacteria, such as Curvibacter fontana sp.

In previous study, Rpf-homologous protein, YeaZ had the stimulatory effect on bacterial resuscitation (Li et al., 2016). In this study, two types of soils from special natural environments were chosen to investigate the promoting effect of YeaZ from V. harveyi on the the presence of culturable bacteria. Sample 1 with the low moisture content (2.04%) and alkaline pH (8.50) from the volcanic land resulted in bacterial growth difficultly. On the other hand, sample 2 with the high moisture content (24.38%) and alkaline pH (9.65) from the saline land soil resulted in the abundance of bacteria. Because the bacterial quantity was most significantly related to moisture content (Saul-Tcherkas, Unc & Steinberger, 2013). The bacterial counts of culturable bacteria from soil samples in the Turpan Basin ranged from 0.29 × 103 to 32.00 × 103 cfu⋅g−1, and the culturable bacterial counts of volcanic land were 2.4 × 103 cfu⋅g−1 (Pan, 2002). Crits-Christoph et al. (2013) reported that the number of culturable microorganisms in extreme aridity of the Atacama Desert varied from 3.1 × 103 to 101 × 103 cells⋅g−1 and the similar results were also observed in this study. As a resuscitation-promoting factor, YeaZ could resuscitate bacteria of the natural environment in the VBNC state. In this study, the culturable bacterial cell number increased significantly from 0.17 × 103 to 1.00 ×103 cells⋅g−1 in the volcanic land soils and also increased more than two times in saline soil by the addition of YeaZ (p < 0.05). Meanwhile, most of the isolated bacteria belonged to phyla Actinobacteria (61.54%) and Gamma-proteobacteria (30.77%) in the volcanic land. Similarly, previous studies also reported the prevalence of the phylum Actinobacteria in desert or cold desert ecosystem of McMurdo Dry Valleys, and Alpine and Arctic soil (Mccann et al., 2016; Horn et al., 2013; Rhodes et al., 2013). Zhang et al. (2015) reported that Gamma-proteobacteria was the most abundant group in the volcanic land of Xinjiang. Neilson et al. (2012) found that the communities were dominated by the phyla Actinobacteria and Chloroflexi in Atacama Desert, Chile. The predominant phyla were Firmicute (76.19%) and Gamma-proteobacteria (19.05%) in the saline soil and nine genera were only found in the samples by the addition of YeaZ. Abed et al. (2012) reported that Firmicutes were mostly detected in the saline lake sediments of Southern Australia. The soda lakes of the Kulunda Steppe, Russia with the highest salinity showed the poorest bacterial diversity, while Gamma-proteobacteria, Actinobacteria and Delta-proteobacteria were the dominant phyla in the lake sediments (Foti et al., 2008). The total bacterial populations were reported as (1.13–7.56) × 108 cells⋅g−1 in the sediments of a hypersaline lake in Western Australia (Weigold et al., 2016). The results were similar with the researches above.

In the current study, the number and community diversity of culturable bacteria increased in the treatment groups, which suggested that the recombinant YeaZ could effectively promote the resuscitation of the Gram-positive and Gram-negative bacteria in the natural environments. Aydin et al. (2011) analyzed the YeaZ crystal structure of Vibrio parahaemolyticus, and the results showed that YeaZ protein is part of the HSP70 actin-like fold (HALF) protein family and is essential for the resuscitation of VBNC strains. The YeaZ proteins open up a new avenue for exploring new special flora and provide a scientific basis for addressing energy crisis and environmental governance by the resuscitation of VBNC bacteria.

Conclusion

The results suggest that YeaZ can effectively promote the resuscitation and growth of the bacteria in the extreme environment. Recovering VBNC bacteria by YeaZ provides high opportunities to obtain more microorganisms with potential environmental functions.

Supplemental Information

Raw data for Table 1

DOI: 10.7717/peerj.10342/supp-1
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