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Analyses of artificial morel soil bacterial community structure and mineral element contents in ascocarp and the
cultivated soil
Journal: Canadian Journal of Microbiology
Manuscript ID cjm-2018-0600.R2
Manuscript Type: Article
Date Submitted by the Author: 27-Apr-2019
Complete List of Authors: Zhang, Fusheng; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. ChinaLong, Li; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. ChinaZongyue, Hu; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. ChinaXiaorui, Yu; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. ChinaLiu, Qingya; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. ChinaBao, Jinku; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. ChinaLong, Zhangfu; College of Life Sciences, Sichuan University, Chengdu 610064, P.R. China,
Keyword: morel, high-throughput sequencing, soil bacterial community structure, bioconcentration factor
Is the invited manuscript for consideration in a Special
Issue? :Not applicable (regular submission)
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1 Analyses of artificial morel soil bacterial community structure and
2 mineral element contents in ascocarp and the cultivated soil
3 Fusheng Zhang1, Li Long1①, Zongyue Hu1, Xiaorui Yu1, Qingya Liu1, Jinku Bao1, Zhangfu Long1①
4 1. Key Laboratory of Bio-resources and Eco-environment (Ministry of Education), College of Life
5 Sciences, Sichuan University, Chengdu 610064, P.R. China
① The author contributed equally to the first author in this work
① Corresponding author E-mail address: [email protected]
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7 Abstract: This study explored the differences among different artificial morel cultivations and the
8 influential factors, including soil bacterial community structure, yield, and mineral element contents of
9 ascocarp and the cultivated soil. High-throughput sequencing results revealed that the dominant
10 bacterial phyla in all the samples, including Proteobacteria, Acidobacteria, Chloroflexi, Bacteroides and
11 Gemmatimonadetes, were found not only in morel soils (experimental group) but also in wheat soil
12 (control group), while the highest richness and diversity in the soil bacteria were observed during the
13 primordial differentiation stage. M6 group exhibited the highest yield (271.8g/m2) and had an
14 unexpectedly high proportion of Pseudomonas (25.30%) during the primordial differentiation stage,
15 which was 1.77 ~ 194.62 times more than the proportion of Pseudomonas in other samples.
16 Pseudomonas may influence the growth of morel. Mineral element contents of the varied soil groups
17 and ascocarp were determined using electro thermal digestion and inductively coupled plasma mass
18 spectrometry. The results revealed that morel had high enrichment effects on Phosphorus (P,
19 Bioconcentration factor = 16.83), Potassium (K, 2.18), Boron (B, 1.47), Zinc (Zn, 1.36), Copper (Cu, 1.15)
20 and Selenium (Se, 2.27). P levels were the highest followed by Se and K, and the mineral element
21 contents in ascocarp were positively correlated with the soil element contents.
22 Keywords: morel, high-throughput sequencing, soil bacterial community structure, bioconcentration
23 factor
24
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26 1. Introduction
27 Morchella spp. (morel) is a prized edible and nutritional fungus and its fruit-body (ascocarp) is rich in
28 polysaccharides, amino acids, vitamins, and other nutrients (Vieira et al. 2016; Su et al. 2013). Numerous
29 studies have demonstrated that the polysaccharides from morel extracts have great potential in medical
30 applications, such as remarkable anti-tumor, antioxidant, and immunity enhancement properties (Nitha et
31 al. 2007; Mau. 2004; Greve et al. 2010; Li et al. 2017).
32 The first indoor cultivation of morels was reported by Ower (Ower. 1982; Ower et al. 1986), and
33 outdoor cultivation of morels has been developed and practiced on a large scale in China in recent years.
34 Many studies have reported that morel mycelial growth and fruit-body formation are influenced by
35 numerous factors, including temperature, humidity, illumination, air, pH, and nutrition (Kalyoncu et al.
36 2009; Richard. 2006; Du et al. 2012). Considering that morel can only fruit in soil and the sowing process
37 needs to be covered by the soil, we speculate that certain substances in the soil may play a key role in
38 morel ascocarp formation. Microorganisms are essential components of soils which participate in the
39 transport and cycling of materials in the soils, in addition to engineering and maintaining soil structure and
40 fertility (Gans et al. 2005; Torsvik et al. 2002). Bacteria are an important component of soil
41 microorganisms and are closely related to other soil biota, which is essential for maintaining the stability
42 and balance of soil microbial community structure (Rousk et al. 2015; Liu et al. 2017; Lin et al. 2014).
43 Numerous studies have observed that there are close symbiotic relationships between plants and
44 rhizosphere soil microbes (Johansson et al. 2004; Nazir et al. 2017; Rudnick et al. 2015), with these
45 interactions also observed between fungi and bacteria (Warmink et al. 2011; Boersma et al. 2010). Pion et
46 al. (2013) in their study observed that when the mycelia of Morchella esculenta were co-cultured with
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47 Pseudomonas putida, the bacteria could spread around the mycelia and the bacterial secretions facilitated
48 mycelial growth (Pion et al. 2013). Studies have shown that Pseudomonas can stimulate the growth of
49 Agaricus bisporus mycelia, reduce the production of ethylene, and induce the formation of Agaricus
50 bispores primordia (Chen et al. 2013; Noble et al. 2009). However, little is known regarding whether the
51 formation of morel fruiting bodies is similar to Agaricus bisporus, and whether some soil bacteria or their
52 secondary metabolites could stimulate morel fruiting.
53 In a single farmland soil ecosystem, the content of elements in soil does not great fluctuate in a
54 short period of time under natural conditions. At present, there are few reports about the
55 bioconcentration of different mineral elements in soil by morel, and whether the mineral elements in soil
56 have an effect on the yields difference of different varieties of morel. Nevertheless, previous studies
57 conducted in our laboratory have observed that different elements significantly influence soil bacterial
58 community structure and morel yield (Liu et al. 2017; Li et al. 2013). Inorganic fertilizers are commonly
59 used in farmland management and every trace element has critical physiological functions that could
60 influence fungal growth rates and soil bacterial community structures (Li et al. 2013; Zhao et al. 2014;Liu
61 et al. 2017). Relevant studies also show that zinc and iron in soil trace elements are valuable nutrients to
62 promote the growth of morel(Liu et al. 2017; Liu et al. 2015). However, whether the levels of elements in
63 the soil influence the element content in fruiting bodies or growth rates of morels remains unclear.
64 Little is known to date about the key mechanism of morel ascocarp formation, which severely limits the
65 further development of the industry of Morchella. However, some studies have shown a close relationship
66 between soil habitats and morel ascocarp formation. Therefore, in the present study, we design an
67 experiment to investigate the role of soil in the growth of Morchella and its influence on yield.
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69 2. Materials and methods
70 2.1 Experimental strains
71 The experimental strains used in the present study were collected from Jinchuan County, Longzhou
72 mountain, located in Huili county, and the artificial morel base of Chongzhou. These locations are located
73 in Sichuan Province, P. R. China. The strains were identified by their ITS sequences, including Morchella
74 sp. (M2, GenBank accession No: MH100896), Morchella galilaea (M3, GenBank accession No:
75 MH100895), and Morchella sextelata (M6, GenBank accession No: MH137040). All strains were
76 preserved at 4 ˚C in the laboratory using PDA medium (200 g of potato, 20 g of glucose, 20 g of agar, and
77 1 L of ddH2O; natural pH value).
78
79 2.2 Analysis of high-throughput sequencing of soil bacterial community structure
80 2.2.1 Field experiment and soil samples collection
81 The field experiment site was in Chongzhou, Sichuan, P.R. China. Before cultivation, the field was
82 levelled and ploughed, 9 split plot was set up, the shape of each split plot was1.5m × 15m, and a drainage
83 ditch of 10cm between the two-compartments. Each experiment group selected the adjacent
84 3-compartment to cultivate the same kind of morel. The mycelia were reactivated using PDA media
85 (potato 200g/L, glucose 20g/L, agar 18g/L, nature pH value) and then were inoculated into the newly
86 sterile spawn media (70% cooked wheat, 30% vermiculite and soil sealing, sterilization 4 h under 121 oC).
87 When numerous sclerotia grew around the culture bottle, and the fungus turned yellow and brown, the
88 seeds were seeded into a ploughed field with 1.5 of these bottles per square meter. The seeds were sown in
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89 a line instead of being spread out and were then covered with soil (3 ~ 5 cm depth) to facilitate the
90 subsequent production of morels. After 10 days, nutrition bags (70% cooked wheat, 30% vermiculite) were
91 added into the soil to restore the mycelium. The soil was regularly irrigated with mist to maintain soil
92 moisture between 30%-40% under the sun-shade net.
93 Soil samples were collected on November 25, 2016 (the mycelium growth stage), January 8, 2017
94 (the primordial differentiation stage), and February 13, 2017 (the ascocarp growth stage) for the three
95 varieties at the artificial morel cultivation base in Chongzhou. Each experimental group selected
96 three sampling sites on each split, the surface soil and shallow soil with depth of 5 cm were
97 respectively collected by tweezers and about 1 g soil put into sterile plastic bags,a total of
98 about 18 g of soil was sufficiently mixed uniform as soil samples(Sig.1).Soil samples of M2
99 strain from the three growth phases were respectively marked with M2-1, M2-2 and M2-3. M3 and M6
100 strain samples were labelled similarly. The wheat field soil (non-morel cultivation,W) was selected as the
101 control and labelled W1, W2, and W3 at the corresponding stages. The collected soil samples were
102 encapsulated with sterile polyethylene plastic bags, preserved at 4°C, and DNA was extracted within 24 h.
103
104 2.2.2 Soil genomic DNA extraction
105 DNA was extracted from the fresh soil samples using the Ezup column soil DNA extraction kit (Sangon
106 Biotech, Shanghai, China), according to the manufacturer’s instructions. The universal primers 515F
107 (5’-gtgccagcmgccgcggtaa-3’) and 909R (5’-ccccgycaattcmtttragt-3’) with a 12-nt unique barcode were
108 used to amplify the V4 hyper variable regions of the 16S rRNA genes for pyrosequencing using a MiSeq
109 sequencer (Caporaso et al. 2011; Caporaso et al. 2012). Each sample was amplified in a 25 μL reaction
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110 according the protocol reported in the study by Tamaki et al. (2011). Two PCR reactions were conducted
111 for each sample and their products combined and subjected to electrophoresis using a 1.5% agarose gel.
112 The bands with the correct sizes were separately excised and were purified using AXYGEN gel recovery
113 kit (Sangon Biotech, Shanghai, China). The products were quantified using Nanodrop 2000, and the
114 samples were pooled together in equal molar amounts.
115
116 2.2.3 High-throughput sequencing and data analysis
117 The Sequencing libraries were prepared using Illumina's TruSeq Nano DNA LT Library Prep Kit
118 (Illumina, Shanghai, China) and sequenced on the Illumina MiSeq sequencing platform. Before
119 on-machine sequencing, the library was checked on an Agilent Bioanalyzer using the Agilent High
120 Sensitivity DNA Kit (Illumina, Shanghai, China). The sequencing libraries were qualified on the machine
121 after gradient dilution based on the 30% of final DNA amount, , and denatured into single chains by 0.1N
122 NaOH on-machine sequencing. The 2 × 300 bp double-stranded sequencing was performed using a MiSeq
123 sequencer with MiSeq Reagent Kit V3 (600 cycles) (Illumina, Shanghai, China), according to
124 manufacturer’s instructions.
125 Paired-end sequencing of the community DNA fragments was performed on the Illumina MiSeq platform.
126 To integrate the original two-terminal sequencing data, the two-terminal sequence in FASTQ format was
127 screened using the sliding window method one by one (the average mass of the window base ≥ Q20; the
128 length of the sequence after truncation ≥ 150bp and without Ambiguous base N). Subsequently, the
129 double-stranded sequence that passed the quality screening was paired with overlapping bases using
130 FLASH software (v1.2.7, http://ccb.jhu.edu/software/FLASH/) (Magoc et al. 2011) (Read 1 and Read 2.
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131 The overlapping length of two sequences is ≥ 10bp, and base mismatch is not allowed). Finally, all the
132 sequence reads were trimmed and assigned to each sample based on their barcodes. QIIME software
133 (Quantitative Insights into Microbial Ecology, v1.8.0, http://qiime.org/) was used to identify the query
134 sequences (Caporaso et al. 2010). USEARCH (v5.2.236, http://www.drive5.com/usearch/) was invoked
135 using QIIME software (v1.8.0, http://qiime.org/) to check and delete the chimera sequences. High quality
136 sequences (length > 150bp, without ambiguous base 'N' and an average base quality score > 30) were used
137 for downstream analysis.
138 Most 16S rRNA gene-based studies on the diversity of bacterial structures usually use 97% sequence
139 similarity as Operational Taxonomic Units (OUT) to divide the threshold (Edgar et al. 2011). We
140 conducted alpha-diversity (rarefaction curves, Alpha-diversity index calculation, and Taxonomy
141 composition analysis) and beta-diversity (PCA) analyses for the observed species. Sequences obtained
142 from the present study were submitted in the NCBI Sequence Read Archive (SRA) with accession number
143 SRP132138.
144
145 2.3 Mineral elements determination of the morel ascocarp and soil
146 When the ascocarp began to mature (in early March), the M2, M3, and M6 morels were collected
147 until there was no more fruiting on the soil (in the end of March), and the yields were calculated separately.
148 Three randomly selected ascocarp varieties and 12 soil samples were processed using electrothermal
149 digestion, Samples were dried at 55 °C for 24 h and homogenized using an agate pestle. Then, a 0.1 g
150 sample was placed into a graphite crucible and digested as described in literature (Liu et al. 2012). The
151 residue was dissolved with 0.2% (w/w) HNO3 and diluted up to 10 mLThe digestion solutions were
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152 assayed to determine the concentrations of 11 mineral elements (calcium, ferric, boron, copper, selenium,
153 potassium, magnesium, manganese, phosphorus, zinc and sodium) using inductively coupled plasma mass
154 spectrometry (ICP-MS, Shimadzu, Japan), according to in the manufacturer’s instructions.
155 The bioconcentration factor (BCF) was calculated as the ratio of the content of mineral element in the
156 samples to that in the soil. When a BCF ≤ 1, it indicates that the morel can only absorb but not accumulate
157 mineral element ; when a BCF > 1, it shows that morel can accumulate mineral element(Liu et al. 2009)
158 The mineral element concentrations and yields of each morel were analyzed using SPSS.21.
159
160 3. Results
161 3.1 Experimental morel species
162 Following the observation of the morphology of the three kinds of morel (Fig. 1a), it was observed that
163 there were major differences in their appearance, particularly with regard to ascocarp color and shape.
164 When pileus color was compared, M2 was flesh colored, M3 was yellow, and M6 was gray brown. With
165 regard to stem color, M3 stems had a light yellow color, while those of M2 and M6 were beige. In addition,
166 M3 pileus had cylindrical shape, while pileus in M2 and M6 were conical.
167 Sclerotia formation in the three morel strains after seven days inoculation in PDA medium is shown in
168 Fig. 1b. M2 did not form a sclerotium structure, and the sclerotium of M3 was concentrated near the
169 inoculation block, while the sclerotium of M6 was more and evenly dispersed on the surface of the entire
170 medium.
171
172 3.2 OTU classification and Alpha-diversity index analysis
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173 According to the mi-seq platform sequencing results, 351,303 valid sequences of the 16S rRNA genes
174 were generated from 12 samples and 27,684 OTUs were obtained. The sequence information of the
175 samples and the calculated microbial diversity indices are listed in Table 1. The rarefaction analysis was
176 used to standardize and compare the observed taxa on richness between samples, and to identify whether
177 the samples were unequally sampled (Zhang et al. 2016). The rarefaction curves (Sig. 2) of the 12 samples
178 gradually exhibited a gentle trend, which implied that the sequenced depths in the current study were
179 adequate to reflect the diversity of the samples.
180 The numbers OTUs, Ace, highest species richness (Chao 1), the Shannon-Weaver Index, and Simpson
181 Index at 3% cut-off were similar did not exhibit changes among the three stages of M2, but exhibited
182 changes in the M3-2, M6-2, and W2, among their other two stages. M3, M6, and W were significantly
183 more enriched in the primordial differentiation stage than in the mycelial growth stage and the ascocarp
184 growth stage. Among the valid sequences, M6-2 was the largest among all groups, and its valid sequences
185 were 3.55 and 4.05-fold greater than those in M6-1 and M6-3, respectively, and were 1.44 to 3.78-fold
186 greater than those in the other samples However, the OTUs of M6-2 were only 1.26 and 1.34-fold more
187 than those of M6-1 and M6-2, respectively, while they were only 0.93 and 1.34-fold more than in the other
188 samples. This could imply that the quantities of some microorganisms rapidly increase in the primordial
189 stage of M6, which results in the highest sequence and OTU numbers.
190
191 3.3 Bacterial community structure at phylum level
192 Bacterial community structure was influenced by the different stage and strains (Fig. 2). Eight dominant
193 bacterial phyla, including Proteobacteria, Acidobacteria, Chloroflexi, Bacteroides, Gemmatimonadetes,
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194 Planctomycetes, Actinomyces and Nitrospira, were observed in all groups, and their percentages ranged
195 from 71.20% to 94.92% (Table 2). The bacterial percentage was similar across all samples, ranging from
196 90.22% to 94.92%, except for in the M6-3 samples (which were only 71.20%). Proteobacteria and
197 Acidobacteria were the most dominant and the second most dominant bacterial phyla in most samples,
198 respectively. The proportions of the two bacterial phyla ranged from 43.21% (M6-3) to 61.24% (M6-1).
199 When the bacterial community structures in the four groups were compared at similar stages, the
200 proportion of Proteobacteria in M6-1 was the highest (49.84%), and was 1.15 ~ 1.79 times those
201 proportions in M2-1, M3-1 and W1. The proportion of Bacteroidetes in M6-2 (25.27%) was the highest
202 and was 3.11 ~ 3.42 times greater than the proportions of Bacteroidetes in M2-2, M3-2, and W2. In
203 addition, the proportion of Acidobacteria in M2-3 (20.62%) was the highest and was 1.10~1.69 times
204 more than those proportions of Acidobacteria in M3-3, M6-3, and W3. At different growth stages,
205 dominant bacterial phyla were varied and were distributed across different experimental samples.
206 When the three stages in each group were compared, it was found that the bacteria percentages increased
207 from the mycelia growth stage to the primordial differentiation stage, and decreased from the primordial
208 differentiation stage to the fruiting body growth stage (except in the M2 group). From the first stage to the
209 second stage, Proteobacteria exhibited an increasing trend in M2 (6.19%), M3 (52.76%) and W (12.18%),
210 but decreased in M6 (14.73%). Acidobacteria (16.69%~24.78%), Chloroflexi (10.79%~40.33%), and
211 Gemmatimonadetes (1.43%~38.29%) all decreased while Actinobacteria (37.84%~93.13%) increased in
212 all groups, except in M6 (decreased 24.21%). Bacteroidetes (28.50%~162.96%) exhibited an increasing
213 trend in all groups except in M3 (decreased 2.52%); Nitrospirae (44.89%~53.90%) showed an upward
214 trend in all groups except in M2 (decreased 59.84%). From the primordial differentiation stage to the
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215 ascocarp growth stage, the Proteobanteria (12.12% ~ 27.05%) and Actinobacteria (37.84% ~ 93.13%)
216 decreased while the Chloroflexi (2.67%~49.53%) and Gemmatimonadetes (1.60%~78.70%) increased in
217 all groups. Acidobacteria (2.03% ~66.45%) exhibited an increasing trend in all groups except in the M3
218 (decreased 26.27%). In addition, Bacteroides (1.65%~78.79%) exhibited an increasing trend in all groups
219 except in M6 (decreased 73.15%). There were minimal differences in the percentages of dominant
220 bacterial phyla in each of the groups, and the changes in each dominant bacterium were in the dynamic
221 states.
222
223 3.4 Bacterial community structure at genus level
224 The dominant genera were Pseudomonas, Pedobacter, Candidatus Solibacter, Rhodopseudomonas,
225 Geobacter, and Planctomyces (Table 3). Pseudomonas, Rhodoplanes, and Geobacter belong to
226 Proteobacteria. Candidatus Solibacter and Planctomyces belong to Acidobacteria and the Planctomycetes,
227 respectively. The proportion of Pseudomonas and Pedobacter varied considerably in different groups.
228 Through a heatmap (Fig. 3) analysis, we observed that the dominant genus varied greatly among different
229 samples, and the differences in the same stage in different groups were substantial.
230 The varying trends in dominant bacteria genera were analyzed from the mycelium growth stage to the
231 primordial differentiation stage. Pedobacter increased (80.43%~2420.00%) while Candidatus Solibacter
232 decreased (28.96%~38.52%) in all groups. The levels of Pseudomonas increased in M2 (884.61%) and
233 M3 (703.70%) but decreased in M6 (84.11%) and W (25.43%). In addition, Rhodoplanes decreased in M2
234 (18.03%) but exhibited a decrease in the other groups (8.60% ~ 29.76%). Both Planctomyces and
235 Geobacter exhibited an upward trend in M2 (21.88% and 6.48%) and M6 (188.46% and 33.33%), while
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236 they showed a downward trend in M3 (44.88% and 53.13%) and W (31.81% and 68.23%).
237 A comparison of the varying trends in the dominant bacteria genera from the primordial differentiation
238 stage to the fruiting body stage, Candidatus solibacter (18.25%~88.64%) revealed an increasing trend,
239 while Pseudomonas (64.98%~98.78%) and Pedobacter (28.90%~91.72%) showed decreasing trends in
240 all groups. Rhodoplanes and Geobacter showed a decreasing trend in M2 (61.00% and 33.91%) and M3
241 (1.87% and 38.33%), and increasing trends in M6 (2.75% and 36.11%) and W (52.48% and 176.92%).
242 Planctomyces exhibited an increase in W (73.33%), decreases in M2 (59.83%) and M6 (24.00%), and
243 remained stable in M3. The percentages of the dominant genuses in different experimental groups were in
244 dynamic states.
245
246 3.5 Principal component analysis
247 According to the map (Fig. 4), the first axis explained 53.11% of the cumulative percentage variance
248 of the species and 22.16% of the cumulative percentage variance was explained by the second axis.
249 Therefore, 75.27% variance in the species could be explained by the two axes. The results of the PCA
250 analysis suggested that there were differences in the bacterial communities in M6-1, M6-3, W1, and W2,
251 while the bacterial communities were similar among the respective three periods in M2 and M3. In
252 addition, the bacterial communities among the periods in M6 were fairly different. There were minimal
253 differences among M6-2, M2, and M3. However, the difference between M6-1 and M6-3 was considerable
254 compared with the other experimental groups, and the differences between M6-1 and M6-3 were very
255 significant. The bacterial communities in W1, W2, and W3 were distinctly different, but the difference was
256 not much greater when compared with the bacterial communities in M6. The differences in bacterial
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257 communities among W3, M2, and M3 were minimal, and there was a distinct difference between bacterial
258 communities of W1 and W2.
259
260 3.6 Mineral elements concentrations in morel ascocarp and soil
261 According to the data (Table 4), the concentrations of mineral elements in the ascocarp were proportional
262 to the concentrations in soil, with the higher contents in soil corresponding with higher concentrations in
263 the ascocarp, and lower concentrations in the soil corresponding with generally lower concentrations in the
264 ascocarp. The order of the mineral element contents in the fruiting body were as follows: Potassium (K) >
265 Phosphorus (P) > Calcium (Ca) > Magnesium (Mg) > Ferric (Fe) > Sodium (Na) > Manganese (Mn) >
266 Zinc (Zn) > Boron (B) > Copper (Cu) > Selenium (Se). The value of BCF was greater than one and the
267 fruiting body had a high enrichment effect on this kind of metal. Therefore, among the 11 mineral elements,
268 P, K, B, Zn, Cu, and Se had a high enrichment effect on the fruiting bodies. The BCF of P was the highest
269 and averaged up to 16.83, which was 6.08–14.6 times that of the other highly adsorptive metals. In
270 comparing the contents among the three groups, the nine mineral element contents in M3 ascacorps were
271 the highest (except for Fe and B) than were M2 and M6, the mineral elements BCF also were the highest
272 (except P, Fe, Na, and Mn).
273 The relative yields of artificial morels demonstrated the following trend: M6 > M3 > M2 (Fig 5). The
274 yield of M6 was the highest, up to 271.8g/m2, 6.7 times that of M2 and 3.9 times that of M3.
275
276 4. Discussion
277 Large-scale cultivation of morels in China is usually field based. The field cultivation successfully
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278 owes to simulating the habitat conditions of wild morel. Consequently, morel yields were greatly
279 influenced by numerous factors, including cultivars, natural habitats, soil properties, and soil microbes.
280 Numerous studies have reported the most suitable morel cultivation conditions (Kalyoncu, et al. 2009;
281 Richard et al. 2006; Obst et al. 2000). However, we still know little about the mechanism of morel
282 development from primordial differentiation to the fruiting body. Soil may play a critical role in the
283 process. The relationships between nutrient elements and morel yield have been explored by numerous
284 reports (Liu et al. 2017; Li et al. 2013; Liu et al. 2015), but only a few reports have specifically examined
285 what kinds of microbes and nutrient elements influence morel fruiting.
286 High-throughput sequencing results showed that the bacteria in artificial morel cultivation soil
287 underwent dynamic changes. According to the changes in bacterial community structure in each group, the
288 richness and diversity of bacterial communities during the primordial differentiation stage were almost the
289 highest in all groups, which could be due to the addition of secondary nutrition bags to the soil, which
290 supplies more energy sources for the growth of microbes. The comparison of bacteria in morel soil and
291 wheat soil revealed that there was no genus that was observed exclusively in morel soil and not in the
292 wheat field, which indicated that the bacteria that stimulated morel development were not specific. It may
293 also explain why morel species may grow in soils that have never been planted with morel, and may fruit
294 after sowing. Analysis of the dominant bacteria, Rhodoplanes and Geobacter as the dominant genus, which
295 belong to Proteobacteria, reveals that they could exploit organic compounds as carbon sources for electron
296 transfer, which is critical for the transformation of material (Bond et al. 2003; Childers et al. 2002).
297 Acidobacteria play a critical role in the maintenance of soil pH. Therefore, changes in their proportions
298 could also influence the growth of other bacteria (Long et al. 2010; Jones et al. 2009). Nitrobacter and
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299 Carbendazim have been reported to be the dominant bacterial groups in wastewater treatment systems,
300 which play a critical role in the degradation of organic chlorides and of ammonia nitrogen (An et al. 2013;
301 Nelson et al. 2011). The bacteria played critical roles in the maintenance of soil physical and chemical
302 properties, and provided a suitable environment for the growth of morels.
303 Comparing the bacterial community structure of M2, M3, and M6 reveals that the bacterial community
304 structure of the three stages in M6 were highly different from the others, especially in the proportions of
305 Pseudomonas. Pseudomonas was the predominant genus in M6-1 and accounted for the largest proportion
306 of bacteria (25.30%). It was 97.3 times more than was that in M2-1 (0.26%) and 93.7 times more than was
307 that in M3-1 (0.27%). In addition, the yield in M6 (271.6g/m2) was 6.7 times that in M2 (40.5g/m2) and 3.9
308 times that in M3 (69.6g/m2). According to the analysis of the correlation between yield and the proportion
309 of Pseudomonas, the high Pseudomonas bacteria contents could have contributed to the improvement in
310 ascocarp yield. Experiments by Pion et al. (2013) also demonstrated that morel and Pseudomonas putida
311 co-culture were beneficial for both. This is also consistent with the findings of our previous study (Liu et al.
312 2017) where Pseudomonas could promote the formation and growth of morel ascocarp. Although the
313 content of Pseudomonas increased in M2-2 (884.61%) and M3-2 (703.70%), and decreased in M6-2
314 (84.11%), the contents in M6-2 were twice more than were the contents in M2-2 and M3-2. This could be
315 because of the growth rates, and the capacity to form sclerotia in M6 was higher than was those in M2 and
316 M3. Volk (1989) observed that sclerotia formation was related to fruiting body formation. Ower (Ower,
317 1982; Ower et al. 1986) also established that sclerotia were crucial for fruit-body formation. The number
318 of sclerotia may also affect Pseudomonas content, which is why M. sextelata is widely used in morel field
319 cultivation as a cultivar. The proportions of Pseudomonas in W1 and W2 were also the highest (more than
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320 10%), and some studies have found that morel and wheat intercropping result in higher morel yields and
321 wheat secretions could promote the growth of morel (Fan et al. 2013). More growth may also be induced
322 by a similar interdependent relationship between wheat and Pseudomonas, with Pseudomonas influencing
323 morel yield.
324 The present study also revealed the bioconcentration capacity of morel, and the relationship between
325 ascocarp and soil mineral element contents. We found that the contents of trace elements in the ascocarp
326 were positively correlated with the mineral element contents in soil by analyzing data from the three
327 groups. The contents of trace elements in soil influenced the contents of trace elements in the fruiting
328 bodies (Gast et al. 1988; Ma et al. 2013). After fires, which provide abundant trace elements via the ashes
329 of trees and grasses, there are typically high yield morel harvests (Li et al. 2017; Mcfarlane et al. 2005).
330 Previous studies conducted by our laboratory also demonstrated that Zn-Fe elements greatly influenced
331 morel yield (Liu et al. 2017). K contents were the highest in the three varieties, and P contents had the
332 highest value of BCF with an average of up to 16.83. The two elements are both critical for the normal
333 development of morel. Fe is an essential element in morel, with the average value of 696.06 mg/kg that is
334 similar to that in Craterellus odoratus (Nasreddine and Parent, 2002). However, the average BCF of Fe
335 (0.02) was the lowest, which was probably due to its nonionic states in the soil. In summary, when the
336 contents of mineral elements in soil are relatively low, it affects normal morel growth. However, mineral
337 element contents in the soil in the three experimental groups exhibited minimal differences. However, the
338 fruit body yields exhibited significant differences. Therefore, mineral elements in the soil were not factors
339 influencing morel fruiting.
340 Although the role of Pseudomonas species in the differentiation of primordia and the mechanism of
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341 symbiosis between Pseudomonas and morel are still not clear, our laboratory isolated nine strains of
342 Pseudomonas that could be cultured from soils of the three M6 stages. Further studies are required to
343 investigate how the Pseudomonas strains influence morel cultivation.
344
345 Acknowledgements
346 The work was financially supported by Sichuan province scientific support program (2016KZ0006),
347 Liangshan state science and agricultural technology innovation program(16NYC0041, 17CXY0015) and
348 Guangyuan Lizhou District research program (13H0923). We also thank Sichuan Wanan Agrobiotech
349 Development Co., LTD for kindly providing morchella spawn and employees joined the field experiment
350 in this study.
351
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483 Table 1: Microbial community diversity indices in the soil samples.
Sample valid sequence OTUs chao1 ACE shannon Simpson
M2-1 29989±3101ab 4605±611d 1269±101b 1807.14±367.21ab 9.16±0.21a 1±0c
M2-2 32287±3672ab 4299±788b 1225±139ab 1836.88±301.12ab 9.17±0.41a 1±0c
M2-3 30282±3361ab 4332±669b 1209±207ab 1782.93±291.18ab 9.12±0.12a 1±0c
M3-1 37977±4191b 5495±972h 1500±241c 2644.12±477.99c 9.25±0.21a 1±0c
M3-2 37433±3771ab 5819±903i 1537±279c 2576.64±399.21c 9.42±0.71a 1±0c
M3-3 31993±3355ab 5063±793f 1336±244b 1900.04±237.73bc 9.25±0.42a 1±0c
M6-1 31918±3811ab 4316±667b 1204±124ab 1990.13±276.88bc 7.45±0.39a 0.93±0.01a
M6-2 113289±8992e 5420±523g 1369±211b 2331.33±297.81c 8.92±0.14a 0.99±0.005c
M6-3 27987±2651a 4036±677a 1103±133a 1591.28±269.93a 7.94±0.21a 0.96±0.01b
W1 68249±3121c 4491±677c 1202±270ab 1925.18±311.21bc 8.20±0.31a 0.97±0.02bc
W2 78131±5052d 4985±601e 1343±201b 2131.15±334.65c 8.41±0.27a 0.98±0.015bc
W3 3172±3519ab 4436±799b 121±219ab 1712.9±255.27ab 9.12±0.22a 1±0c
484 Note: Values sharing a common superscript letter (a-d) were not significant at P <0.05.
485
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487 Table 2: Percentages of predominant bacterial phyla in the soil samples.
488 Note: Pro-Proteobacteria; Aci-Acidobacteria; Chl-Chloroflexi; Bac-Bacteroides; Gem-Gemmatimonadetes;
489 Pla-Planctomycetes; Act-Actinomyces;Nit- Nitrospira; One-way ANOVA analysis of the same bacteria in four soils at the
490 same time; Values sharing a common superscript letter (a-c) were not significant at P <0.05.
Mycelia growth stage(%) Primordial differentiation stage(%) Ascocarp growth stage(%)Phyla
M2-1 M3-1 M6-1 W1 M2-2 M3-2 M6-2 W2 M2-3 M3-3 M6-3 W3
Pro34.27±
5.64a
27.82±
3.31a
49.84±
6.82b
43.27±
5.04b
31.98±
2.47a
34.95±
4.1a31±3.5a
36.65±
5.75a
36.39±3
.79a
42.5±4
.17ab
42.5±3
.34ab
48.54±
5.17b
Aci19.2±1.
4c
18.32±
2.26bc
11.44±
1.74a
14.73±
2.91ab
20.62±
3.21b
13.5±1.
7a
12.21±
2.13a
18.71±
1.73b
16.33±2
.39c
13.78±
1.34bc
9.01±1
.03a
11.24±
2.04ab
Chl14.59±
2.53b
15.67±
1.44b
8.58±0.
64a
9.36±1.
42a
12.58±
2.14b
9.6±1.3
4ab
7.91±0.
73a
10.79±
0.83ab
11.5±1.
65b
9.35±2
.05ab
5.29±2
.13a
8.35±2
.7ab
Bac6.21±1.
37ab
8.32±0.
68bc
9.61±1.
13c
4.1±1.0
5a
9.88±1.
36b
14.5±1.
4c
6.58±1.
46a
7.5±0.4
5ab
7.98±1.
02a
8.11±1
.43a
25.27±
3.14b
7.38±1
.46a
Gem7.24±1.
14b
7.69±1.
23b
5.09±0.
66a7±1.2b
7.32±0.
84a
9.34±1.
06a
6.08±1.
16a
6.96±0.
78a
5.35±1.
24a
7.58±1
.61a
4.09±0
.73a
4.32±1
.06a
Pla5.03±1.
06b
5.03±1.
02b
2.84±0.
74a
3.58±0.
46ab
3.7±0.4
1a
3.54±0.
77a
3.38±0.
74a
3.57±0.
47a
5.71±1.
43b
3.68±0
.76a
4.46±1
.12ab
3.18±0
.26a
Act2.22±0.
62a
3.64±0.
34b
3.18±0.
06ab
5.44±1.
33c
2.9±0.6
5a
4.37±0.
74a
1.9±0.2
5a
4.48±1.
94a
3.06±0.
82a
7.03±1
.01b
2.41±0
.34a
10.36±
1.64c
Nit2.44±0.
71a
3.97±0.
84b
2.25±0.
4a
3.15±0.
85ab
2.67±0.
74a
1.67±0.
3a
2.14±0.
34a
2.94±0.
72a3.9±0.3b
1.83±0
.21a
1.24±0
.24a
1.55±0
.6a
Total91.2±2.
64a
90.46±
2.02a
92.83±
1.79a
90.63±
1.11a
91.65±
2.7b
91.47±
1.04b
71.2±2.
8a
91.6±1.
84b
90.22±0
.74a
93.86±
1.04a
94.27±
2.24a
94.92±
2.66a
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492 Table 3: Percentages of predominant bacterial genera in soil samples.
Mycelium growth stage (%)Primordial differentiation stage
(%)Ascocarp growth stage (%)
Genus
M2-1 M3-1 M6-1 W1 M2-2 M3-2 M6-2 W2 M2-3 M3-3 M6-3 W3
Pse0.26±
0.03a
0.27±
0.09a
25.3±2
.72c
14.31±
2.11b
2.56±0
.33a
2.17±
0.41a
4.02±0
.33b
10.67±
2.03c
0.48±
0.14b
0.76±
0.18c
0.3±
0.07b
0.13
±
0.06a
Ped0.1±0
.02a
0.32±
0.08b
3.68±0
.68c
0.1±0.
01a
2.52±0
.25b
2.18±
0.3b
6.64±0
.71c
1.14±0
.11a
0.96±
0.20b
1.55±
0.25c
0.55
±
0.14a
0.72
±
0.18ab
Can1.92±
0.23b
2.44±
0.41d
1.41±0
.22a
2.21±0
.19c
1.26±0
.21ab
1.5±0.
3ab
0.96±0
.13a
1.57±0
.34ab
1.49±
0.19a
1.79±
0.39a
1.64
±
0.32a
2.25
±
0.53b
Rho
1.22±
0.18a
b
0.9±0
.25a
0.84±0
.29a
0.93±0
.22a
1±0.27a
1.07±
0.19a
1.09±0
.27a
1.01±0
.27a
0.39±
0.09a
1.05±
0.31b
1.12
±
0.16b
1.54
±
0.23c
Pla0.96±
0.31b
1.27±
0.21c
0.52±0
.09a
0.44±0
.07a
1.17±0
.21bc
0.7±0.
04b
1.5±0.
32c
0.3±0.
08a
0.47±
0.14a
0.7±0.1
3ab
1.14±
0.22b
0.52±
0.16a
Geo
1.08±
0.19b
c
1.28±
0.33c
0.27±0
.06a
0.82±0
.11b
1.15±0
.14c
0.6±0.
15b
0.36±0
.11a
0.26±0
.09a
0.76±
0.03b
0.37±0.
08a
0.49±
0.13ab
0.72±
0.21b
Total5.54±
1.02a
6.48±
1.26a
32.02±
4.13c
18.81±
2.82b
9.66±1
.57a
8.22±
1.12a
14.57±
1.89b
14.95±
2.81b
4.55±
0.85a
6.22±1.
34a
5.24±
1.17a
5.88±
1.44a
493 Note: Pse-Pseudomonas ; Ped-Pedobacter ; Can-Candidatus Solibacter ; Rho-Rhodopseudomonas; Pla-Planctomyces;
494 Geo-Geobacter; One-way ANOVA analysis of the same bacteria in four soils at the same time; Values sharing a common
495 superscript letter (a-d) were not significant at P <0.05.
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497 Table 4: Mineral element contents in morel ascocarp and in cultivated soils (mg/kg dw).
M2 M3 M6
Materials Samples
Contents (mg/kg) BCF Contents (mg/kg) BCF Contents (mg/kg) BCF
Ascocarp 28517.00±363.37e 47055.00±346.41f 33220.00±236.43f
Potassium(K)
Soil 16886.67±207.65c
1.68
17250.00±395.17c
2.727
15540.00±912.03c
2.138
Ascocarp 17566.67±692.63d 21481.67±210.08e 17660.00±271.84e
Phosphorus(P)
Soil 1089.83±124.21a
16.119
1259.83±163.63a
17.051
1020.17±125.81a
17.314
Ascocarp 3775.67±61.81c 5349.00±71.51d 3835.00±39.18d
Calcium(Ca)
Soil 8311.67±423.05b
0.454
8323.33±350.25b
0.620
7691.67±491.74b
0.498
Ascocarp 1368.33±31.92b 1617.33±21.53c 1372.17±29.47cMagnesium
(Mg) Soil 6413±244.81b
0.213
6406.00±189.49b
0.252
5875.00±375.04b
0.234
Ascocarp 876.50±6.51ab 634.17±12.43b 577.50±14.02b
Ferric(Fe)
Soil 35243±2219.6d
0.025
36910.00±2149.84d
0.017
30121.6± 2117.05d
0.019
Ascocarp 149.80±1.08a 240.50±4.57a 167.00±1.85a
Zinc(Zn)
Soil 133.90±3.27a
1.119
138.50±7.63a
1.736
135.43±13.32a
1.233
Ascocarp 743.67±8.57ab 781.67±21.53b 772.00±19.35b
Sodium(Na)
Soil 7300.00±218.30b
0.102
7065.00±253.57b
0.111
6391.67±413.37b
0.121
Ascocarp 27.50±0.63a 37.38±0.40a 30.53±0.39aManganese
(Mn) Soil 282.93±5.96a
0.097
267.28±1.01a
0.14
201.72±28.63a
0.151
Boron(B) Ascocarp 33.48±2.15a 1.262 32.73±1.52a 1.752 30.22±0.31a 1.394
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Soil 26.52±2.88a 18.68±5.13a 21.68±0.31a
Ascocarp 26.67±0.52a 40.98±0.82a 28.90±0.71a
Copper(Cu)
Soil 26.78±2.07a
0.996
28.95±5.88a
1.415
27.68±1.76a
1.044
Ascocarp 3.53±0.18a 6.40±0.15a 7.63±0.27a
Selenium(Se)
Soil 3.61±0.42a
0.978
1.51±0.06a
4.240
2.46±0.22a
3.100
498 Note: Values sharing a common superscript letter (a-f) were not significant at P <0.05.
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500 Figure captions
501
502 Figure 1: Three morel experimental profiles (a) and growth status of mycelia on PDA medium (b).
503
504 Figure 2: Community composition and abundance distribution at phylum level.
505
506 Figure 3: Cluster analysis of genus community composition.
507
508 Figure 4:Two-dimension distribution figure of PCA analysis results.
509
510 Figure 5: Morel yields among different groups.
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Fig.1: three kind experimental morel profiles (a) and growth status of mycelium on PDA medium (b).
94x28mm (300 x 300 DPI)
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Fig2. Community composition and abundance distribution of phylum level.
47x34mm (300 x 300 DPI)
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Fig3. Cluster analysis of genus community composition.
47x47mm (300 x 300 DPI)
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Fig4. Two dimensions distribution figure of PCA analysis (Each point represents a sample, the closer the distance between two points, indicating that the similarity between the two samples of the microbial
community structure, the smaller the difference).
59x53mm (300 x 300 DPI)
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Fig5. Morel yields of different groups. Values sharing a common capitalized letter (a-c) were not significant at P<0.01.
50x34mm (300 x 300 DPI)
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