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The structure and diversity of bacteria and fungi in the roots and rhizosphere soil of three different species of Geodorum

Abstract

Shepherd's crook (Geodorum) is a genus of protected orchids that are valuable both medicinally and ornamentally. Geodorum eulophioides (GE) is an endangered and narrowly distributed species, and Geodorum densiflorum (GD) and Geodorum attenuatum (GA) are widespread species. The growth of orchids depend on microorganisms. However, there are few studies on the microbial structure in Geodorum, and little is known about the roles of microorganisms in the endangered mechanism of G. eulophioides. This study analyzed the structure and composition of bacterial and fungal communities in the roots and rhizosphere soil of GE, GD, and GA. The results showed that Delftia, Bordetella and norank_f_Xanthobacteraceae were the dominant bacteria in the roots of Geodorum, while norank_f_Xanthobacteraceae, Gaiella and norank_f_norank_o_Gaiellales were the dominant bacteria in the rhizosphere soil of Geodorum. In the roots, the proportion of Mycobacterium in GD_roadside was higher than that in GD_understory, on the contrary, the proportion of Fusarium, Delftia and Bordetella in GD_roadside was lower than that in GD_understory. Compared with the GD_understory, the roots of GD_roadside had lower microbial diversity. In the endangered species GE, Russula was the primary fungus in the roots and rhizosphere soil, with fungal diversity lower than in the more widespread species. Among the widespread species, the dominant fungal genera in the roots and rhizosphere soil were Neocosmospora, Fusarium and Coprinopsis. This study enhances our understanding of microbial composition and diversity, providing fundamental information for future research on microbial contributions to plant growth and ecosystem function in Geodorum.

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Introduction

Shepherds' crooks (Geodorum), a genus of the Orchidaceae, has been listed as protected plants in China. Geodorum includes approximately ten species. There are five species of Geodorum in China, namely G. densiflorum (GD), G. recurvum, G. pulchellum, G. attenuatum (GA) and G. eulophioides (GE) [1]. Geodorum is a type of plant that is protected at a national level due to its ornamental and medicinal value. It was listed in Appendix II of the Convention on International Trade in Endangered Species of Wild Fauna and Flora (CITES), and GE was listed in the International Union for Conservation of Nature (ICUN) Red List of Endangered Species. The growth and development of plants are closely linked to soil microorganisms. Analyzing the composition of soil microorganisms can aid in promoting plant protection [2]. GE is highly valuable ornamentally, but it has a narrow area of distribution [3]. In contrast, the other species of Geodorum are distributed over a wide area. GD is the most widespread and abundant speciess within Geodorum. GD predominantly grows in areas at 1,500 m altitude, including sparse forests, roadsides, and grassy slopes, and is found in South and Southwest China, Vietnam, Laos, Cambodia, Thailand, Malaysia, and Indonesia, among other countries. GA primarily grows in the forest margin and sparse forest areas below an altitude of 800 m. It is distributed in Hainan, Yunnan and the southern Guangxi Province of China, and Vietnam, Laos and Myanmar. The range of distribution of GA is smaller than that of GD. GE is only found at the junction of Yunnan, Guizhou and Guangxi Provinces in China, and it grows at an altitude of 600 m in shrubs or medium shade forests in limited quantities; it is very narrowly distributed and found in limited quantities [1]. Since orchids thrive in specific habitats, the microorganisms in their rhizosphere soil play a crucial role in adaptation, while the soil environment influences the survival of these microorganisms [4]. For instance, orchid species growing in mining areas often contain various toxic elements. Based on 16S rRNA gene and ITS amplification and sequencing of the roots and soil of narrow-leaved helleborine (Cephalanthera longgifolia), Epipactis pontica, royal helleborine (E. atrorubens), and lesser-butterfly orchid (Platanthera bifoli), no significant difference in microbial composition was found among the orchids from different mining areas, and bacteria and fungi could reduce the damage of toxic elements to orchids [5]. In the same way, the survival and reproduction of orchids require a specific environment, and they generally grow in low altitude areas, primarily in the understory, grasses, bushes, and roadsides [1]. Like other orchids, the germination of Geodorum seeds depends on the mycorrhizal fungi associated with their roots [6]. Mycorrhizal fungi are not only essential for the germination of orchid seeds but also assist in the uptake of nutrients by their roots to promote their growth and reproduction [7]. Therefore, understanding the fungal and bacterial composition in orchids' natural environments is essential for conservation efforts of these valuable plants.

Currently, most species of orchids have been listed as key protected wild plants, particularly species of Cymbidium, Dendrobium and Paphiopedilum. Therefore, strengthening the protection of wild orchids is imperatives. Many studies have focused on various aspects of orchid reproduction, including genetic diversity [8,9,10], reproductive techniques [11] and mycorrhizal fungi [12,13,14]. Microorganisms in the plant rhizosphere soil and roots affect the decomposition of soil organic matter and the absorption of nutrients by plant roots, and some harmful bacteria can also cause plant diseases. Studying the characteristics of bacteria and fungi in orchid roots and rhizosphere soil can reveal how these microorganisms affect orchid growth and distribution across habitats. Based on an analysis of microbial composition and diversity in the rhizosphere soil of Holopogon pekinensis in different regions, the dominant bacteria and microbial community richness of H. pekinensis were found to be related to the species of trees in its habitat [15]. The composition and diversity of bacteria and fungi in different tissues and other aspects of various orchids have been studied to analyze the interaction between orchids and microbial communities and to provide reliable guidance for their cultivation [16,17,18,19].

Geodorum is an herbaceous plant in the family Orchidaceae. The studies of this genus focus on its genetic diversity and analyses of its embryology [20,21,22,23]. There has been very little research on the effect of mycorrhizal fungi on the germination and growth of Geodorum seeds. Therefore, as an endangered species, the fungal composition in the root and rhizosphere soil of GE may be related to its endangered status. The reasons for its precarious status were analyzed in terms of human factors, the morphology of GE, and population competition [3]. To date, to our knowledge, there have been no relevant studies on the link between microbial diversity in the root and rhizosphere soils of Geodorum and causes of its endangered status. There were two types of habitats for GD. One included the understory (GD_understory), while the other included roadsides (GD_roadside). However, it is not clear whether there are differences in the microbial composition of GD_understory and GD_roadside and how the rhizosphere microorganisms affect their growth. The growth of Geodorum was influenced by various factors such as soil properties and altitude, subsequently impacting its interactions with soil microorganisms. Additionally, the species' distribution range was also influenced by its specificity to certain fungi. A study on the diversity of bacteria and fungi in the roots and rhizosphere soil of Geodorum in different habitats could provide insights into the interactions between microorganisms and this genus of orchids.

In this study, the roots and rhizosphere soil of three species of Geodorum (GE, GD and GA) were studied. The bacterial and fungal diversity was investigated by 16S rRNA and ITS amplification and the sequencing of root and rhizosphere soil samples from Geodorum. Differences in the bacterial and fungal diversity in the root and rhizosphere soil between different habitats and endangered species (GE) and widespread species (GD and GA) should help to identify possible relationships between the microbial diversity and endangered species and the relationship between microorganisms and the habitats of species of Geodorum.

Materials and methods

Plant roots and soil sampling

Roots and rhizosphere soils were collected from three species of Geodorum in China. GE, GD, and GA were collected from the Yachang Orchid Nature Reserve, Baise City, Guangxi Province, and Minqiang Village, Longzhou County, Chongzuo City, Guangxi Province, China. In addition, GD was sampled from understory (GD_understory) and roadside (GD_roadside) habitats. GE and GA were both sampled from the understorey. While GE was sampled in Baise City, GA was sampled in Chongzuo City. In addition, they grew in different locations at varying altitudes. The sampling site information of Geodorum was shown in Table 1, and the habitat picture was shown in Fig. 1.

Table 1 Sampling information of three species of Geodorum
Fig. 1
figure 1

Photographs of the habitat of Geodorum. A: Geodorum eulophioides; B and C: Geodorum densiflorum (B: growing in the understory; C: growing in the roadside); D: Geodorum attenuatum

The sampling sites of Geodorum were all low-altitude areas. The sampling sites of GE have a dry climate (annual average rainfall was 1216.9–940.8 mm) and annual average temperature was 19.2–20.4 °C, and especially the growth soil type was red soil. In addition, there were trees in the upper layer of habitat of GE, including Pinus yunnanensis, and grass in the shrub layer, such as Phyllodium pulchellum, Callicarpa bodinieri and Chromolaena odorata. However, the habitat of GD_roadside lacked an upper layer of trees and was situated at an altitude of 500 m. GD_roadside thrives in full light and the soil was of a sandy composition, with an environment characterized by an admixture of gravel and soft soil. Unlike the habitat of GD_roadside, the habitat of GD_understory was characterized by its upper tree layers, which include species such as Vernicia fordii. GA grew on the periphery of wooded areas, shunning direct sunlight, in mildly acidic and soft soil, with an annual average temperature of 20–28 °C in Chongzuo City.

Three plants from GA, GD_understory, GD_roadside, and GE distributions were randomly selected as biological replicates. Three biological replicates were used for both the root and rhizosphere soil samples, and they yielded 24 samples in total. After the non-rhizosphere soil of the plants was removed by shaking, about 5 g of soil about 3 mm away from the roots was collected as rhizosphere soil samples. Roots were washed with sterile water to remove soil before sample collection. Five grams of rhizosphere soil per plant and over 20 root fragments per plant were collected after removing the rhizosphere soil. Samples were collected and stored on in -80ºC and then used for 16S rRNA and ITS sequencing.

Measurement of soil properties at sampling sites

Approximately 50 g of soil samples were collected at each sampling site and airdried outdoors for 5 days after collection. Soil pH was measured using a PHS-3C acidity meter (Shanghai INESA, Shanghai, China). Weigh 10 g of air-dried soil sample in a 50 ml beaker, add 25 ml of distilled water, stir and mix well, and let stand for 30 min. The above to be tested solution was determined, each sample was repeated three times and the average value was taken.

Soil organic matter was determined using the potassium dichromate volumetric method [24]. 0.1 g of soil sample through 60 mesh sieve was weighed into a test tube, and 10 ml of 0.136 mol/L K2Cr2O7-H2SO4 solution was added to an oil bath at 170 ºC for 5 min. After cooling, it was transferred to a 250 ml triangle flask with distilled water, and 3 drops of 1,10-Phenanthroline indicator (200–629-2, Shanghai, China) was added. The solution was titrated with 0.2 mol/L FeSO4 solution to change from yellow to green to brown–red. Quartz sand was used as blank control. The soil organic matter content was calculated according to the formula (V0: The volume of FeSO4 used to titrate the blank solution. V: The volume of FeSO4 used to titrate the sample solution. N: concentration of standard FeSO4.):

$$Organic\;matter\;content\left(\frac g{kg}\right)=\frac{\left[\left(V_0-V\right)N\ast0.003\ast1.724\ast1.1\right]\ast1000}m$$

The available nitrogen in soil was determined by potassium dichromate and sulfuric acid digestion method [24]. After air drying, 0.5 g of soil sample was weighed and placed into a 150 ml digestion tube through 60 mesh sieve. Then, 5 ml of H2SO4 was added and boiled on a digestion furnace at high temperature for 20 min. After cooling, 5 ml of K2Cr2O7 solution was added and heated on an electric furnace for 5 min. The above solution was then distilled for about 20 min to complete distillation. Steam was passed through a condensing tube into a triangular bottle containing 25 ml of 2% boric acid absorption solution and 1 drop of nitrogen-mixed indicator (Thermo Scientific, MA, USA). The resulting solution was titrated with a 0.02 mol/L standard solution of hydrochloric acid. The solution changed from blue to burgundy, and the volume of hydrochloric acid used was recorded. The available nitrogen content in soil samples was calculated by this formula(V0: The volume of hydrochloric acid used to titrate the blank solution. V: The volume of hydrochloric acid used to titrate the sample solution. N: concentration of standard hydrochloric acid.):

$$Available\;nitrogen\;content\left(\frac{mg}{kg}\right)=\frac{\text{N}\ast\left(V-V_0\right)\ast14\ast1000}m$$

The available phosphorus in soil samples was determined by sodium bicarbonate method [25]. 5 g of airdried soil samples through 18 mesh sieve were weighed into a triangular flask, 0.1 g of phosphate-free active carbon was added, and the mixture was shaken for 30 min. The filtrate was filtered and placed in triangular flask. Take 10 ml of filtrate in a 50 ml volumetric flask, add 2 drops of dinitrophenol indicator (Thermo Scientific, MA, USA), add 5 ml of molybdenum antimonium sulfate mixed color developing agent (Thermo Scientific, MA, USA) and shake thoroughly, discharge carbon dioxide and add water to scale, and then shake thoroughly. After 30 min, a spectrophotometer (Thermo Scientific, MA, USA) was used to measure the value at 600 nm, and a standard curve was drawn and the available phosphorus content in the soil was calculated.

Weigh a 0.5 g soil sample and pass it through an 18 mesh sieve into a triangular flask. Add 50 ml of 1 mol/L NH4OAc solution and shake the mixture at 20–25 ºC for 30 min. Filter the mixture through dry filter paper and use a flame photometer (FP6430, Shanghai, China) to measure the available potassium content in the soil. Draw a standard curve and calculate the available potassium content in the soil.

DNA extraction, PCR, and sequencing

Genomic DNA was extracted using an E.Z.N.A.® Soil DNA Kit (Omega Bio-tek, sNorcross, GA, USA). A NanoDrop2000 spectrophotometer (Thermo Fisher Scientific, Waltham, MA, USA) was used to determine the purity and concentration of genomic DNA, and the DNA integrity was detected by 1% agarose gel electrophoresis at 5 V/cm for 20 min. For PCR amplification, primers 515F (5'—barcode—GTGCCAGCMGCCGCGGTAA—3')/ 806R (5' – GGACTACHVGGGTWTCTAAT—3') were used to amplify the V3—V4 region of 16S rRNA genes in the rhizosphere soil samples, and primers 799F (5'—barcode – AACMGGATTAGATACCCKG—3')/1193R (5' – ACGTCATCCCCACCTTCC—3') were used to amplify the V5—V7 region of 16S rRNA genes in the root samples. In addition, ITS1F (5 ' -barcode—CTTGGTCATTTAGAGGAAGTAA—3')/ITS2R (5'—GCTGCGTTCTTCATCGATGC—3') primers were used to amplify the ITS1 gene region of fungi [26]. The PCR reaction system contained 20 μL in total, with 10 ng of DNA template, 0.5 μM primer, 0.4μL FastPfu DNA polymerase (TransGen, China), 2μL 2.5 mM dNTPs, 4μL 5 × FastPfu Buffer, and 0.2μL BSA. The PCR reaction followed these conditions: 3 min denaturation at 95 °C, 30 cycles (30 s of denaturation at 95 °C, 30 s of annealing at 56 °C, 1 min of extension at 72 °C), and a final extension step of 10 min at 72 °C. The PCR products were then identified, purified, and quantified. The PCR products were identified by electrophoresis on a 2% agarose gel, purified with an Axygen Biosciences Gel Exact kit (Axygen Biosciences, Union City, CA, USA), and quantified with a Quantus™ Fluorometer (Promega, Madison, WI, USA). According to the sequencing volume requirements of each sample, the corresponding proportions were mixed. After MiSeq library construction, sequencing was performed on a MiSeq PE300 platform (Illumina, San Diego, CA, USA).

Sequence data analysis

The raw data were obtained after Illumina sequencing. FASTP (https://github.com/OpenGene/fastp, version 0.20.0) was used to remove low-quality sequences [27], and FLASH (http://www.cbcb.umd.edu/software/flash, version 1.2.7) was used to assemble the sequences [28]. During raw data quality control, bases with quality values < 20, reads shorter than 50 bp and reads containing N bases were removed. Sequence splicing was used to merge pairs of paired-end (PE) reads into a single sequence based on the overlapping relationship between the PE reads, and the minimum overlap length was 10 bp.

Statistical analysis

Data analyses were conducted using the MegBio Cloud platform (https://cloud.majorbio.com).

OTU analysis

Operational taxonomic unit (OTU) clustering to identify species and quantify bacteria and fungi in samples was performed using UPARSE software (version 7.1, http://drive5.com/uparse/) [29]. All the optimized sequences were mapped to the OTU representative sequences, and sequences > 97% similar to the OTU representative sequences were selected to generate the OTU table (Table S2, S3). The OTUs of bacteria and fungi were compared with the Silva 16S rRNA gene database (Release138 http://www.arb-silva.de) and UNITE 8.0/ITS_fungus database (Release 8.0 http://unite.ut.ee/index.php) to annotate the classification of species by OTU, respectively [30]. Rarefaction curve analysis showed Good's coverage for observed OTUs in all samples > 97%, indicating sufficient sequencing depth for subsequent analyses (Fig. S1).

Venn diagram

During the analysis, the raw data were first subjected to the steps of quality control, clustering, and assignment of taxa, resulting in an OTU table for each sample. Next, use R (version 3.3.1) draw Venn diagram [31].

Community Composition Analysis: Bar Chart

The OTU table obtained after pre-processing the raw data was used to draw the community bar chart using R (version 3.3.1). The data were converted by percentage of relative abundance, and then the data were grouped according to the taxonomic level to draw the stacking bar chart.

α-Diversity analysis: Index group difference test

The Chao index is commonly used to estimate the total number of species, and the Shannon index is often used to reflect the diversity of species, with a higher Shannon value indicating a higher community diversity. The OTU diversity index table was first obtained by pre-processing the raw data, namely the OTU analysis described above. The choice was then made to calculate a diversity value for each sample using the Chao index, reflecting the richness and evenness of the microbes in the sample. Differences in diversity between groups were tested using the Kruskal–Wallis rank sum test to assess whether there were significant differences in diversity indices between samples (GE, GD_understory, GD_roadside and GA) [32]. The diversity differences were visualized using box plots in R (version 3.3.1).

β-Diversity analysis: NMDS analysis

A non-metric multidimensional scaling (NMDS) analysis was conducted using the Bray–Curtis distance algorithm to represent the multidimensional space as points. The difference between different samples is reflected by the distance between points, and the spatial anchor map of the samples was finally obtained. The OTU table was obtained after pre-processing the raw data, and NMDS ordination was used to reduce the dimension and visualise the similarity between samples by performing NMDS analysis based on the distance matrix. In the comparison of differences between multiple groups, multiple comparisons were corrected by false discovery rate (FDR) [33]. Finally, according to the results of difference analysis, data were visualized using scatter diagram through R (version 3.3.1).

ANOSIM analysis

Analysis of similarities (ANOSIM) was used to test whether the differences between groups (two or more groups) were significantly greater than the differences within groups. The distance between pairs of samples was calculated using the distance algorithm (Bray–Curtis), and data were visualized using box plots through R (version 3.3.1).

Species difference analysis

After preprocessing the raw data, the OTU table was used for species differentiation analysis, and differences between groups were evaluated using the Kruskal–Wallis rank sum test, with statistical significance set at P < 0.05. In the comparison of differences between multiple groups, multiple comparisons were corrected by false discovery rate (FDR) (FDR < 0.05). Finally, according to the results of difference analysis, data were visualized using bar charts through R (version 3.3.1).

Co-occurrence network analysis

Co-occurrence network analysis can be used to show the distribution between samples and species. By analyzing the species abundance information among different samples, the co-occurrence relationship of species in environmental samples can be obtained, which can highlight the similarities and differences between samples. Associations with Reads Per Kilobase Million (RPKM) ≥ 200, a P-value < 0.05 and an R-value > 0.6 were retained in the network. Co-occurrence network analysis was performed according to the OTU table after preprocessing of the raw data. The co-occurrence network analysis of species abundance information between different samples was performed using Networkx (vsesion1.11), and the abundance of different microbial species in each sample was calculated. Based on the RPKM abundance data of microbial species, a co-occurrence matrix was constructed and rare species were filtered. spearman correlation coefficient was used to calculate the symbiosis between microbial species, and significant co-occurrence associations were transformed into co-occurrence network maps according to the P-value and R-value.

Multilevel species discriminant analysis: LEfSe analysis

Linear discriminant analysis Effect Size (LEfSe) combined linear discriminant analysis (LDA) and measures of effect size to identify microbial signatures with significant differences. Analysis using LEfSe software (http://huttenhower.sph.harvard.edu/galaxy/root?tool_id=lefse_upload), LDA and effect size measure (the LDA threshold was 3) found significant differences in microbial characteristics. In LEfSe, Kruskal–Wallis test was used to identify microorganisms with significant differences, and LDA analysis was used to determine the impact of these differences on sample grouping.

RDA/CCA analysis

Redundancy Analysis (RDA) and Canonical Correspondence Analysis (CCA) were commonly used to explore the effects of environmental factors on species composition. According to the selection principle of RDA or CCA model, DCA analysis was performed with the OTU table with 97% similarity. When the first axis of Lengths of gradients in the analysis results was greater than 3.5, CCA was selected, and the Lengths of gradients were less than 3.5, RDA was selected. The R language vegan(vsesion2.4.3) was used for CCA or RDA analysis and mapping.

Results

Soil information at sampling sites for the three species of Geodorum

Soil property information, including soil pH, organic matter, available nitrogen, available phosphorus, and available potassium, was analyzed at the four sampling sites. Soil properties regarding sampling sites were shown in Table S1. GE and GA soils tended to be acidic (pH < 7) while GD_understory and GD_roadside soils tended to be alkaline (pH > 7). The content of soil organic matter content and available nitrogen in GE and GD_roadside was significantly lower than that in GD_understory and GA. The content of available potassium in GE and GD_roadside soils was significantly higher than that in GD_understory and GA. The results of RDA and CCA showed that pH, altitude, available nitrogen and organic matter were significantly correlated with the composition of the microbial community (Figure S2). The community composition of bacteria and fungi in rhizosphere soil and roots of GA was mainly correlated with altitude, available nitrogen and organic matter content. Moreover, pH was negatively correlated with available nitrogen and organic matter in the soil. Organic matter and available nitrogen in the soil were mainly correlated with the fungal composition in the roots and rhizosphere soils of GD_roadside and GD_understory(Fig. S2B).

Bacterial composition of three species of Geodorum that grow in understory and roadside areas.

A total of 1,228,959 sequence numbers were obtained with an average length of 377 base pairs (bp), the shortest sequence after 16S rRNA sequencing was 200 bp, and the longest sequence was 520 bp (Table S4). A taxonomic analysis was performed on the 97% similarity level of the OTU representative sequences, and the community species composition of each sample was then calculated. At the OTU taxonomic level, the number of OTUs for bacteria in the rhizosphere soil was higher than that in the roots of all Geodorum (Table 2). Geodorum roots shared 601 (21.05%) common 16S OTUs, with GD_understory having the highest number of unique OTUs at 389 (13.63%) (Fig. 2A). However, a total of 833 (29.29%) common 16S OTUs were found in the rhizosphere soil of Geodorum, which was higher than that in the roots, indicating that the difference of bacterial species in the roots of different Geodorum was greater than that in the rhizosphere soil (Fig. 2B). A total of 2,383 (71.86%) 16S OTUs were common between bacteria in the rhizosphere soil and roots, with 472 (14.23%) and 461 (13.90%) unique OTUs in each, respectively (Fig. 2C).

Table 2 The information on 16S OTU classification statistics in Geodorum
Fig. 2
figure 2

Bacterial composition of different Geodorum species. A, B and C: Venn diagram of different groups at the OTU level (A: in the roots of GE, GD_roadside, GD_understory and GA groups; B: in the rhizosphere soil of GE, GD_roadside, GD_understory and GA groups; C: in the root and rhizosphere soil groups in all the Geodorum species). D and E: Bar graphs of the bacterial community composition at the phylum level (D: in the roots of Geodorum; E: in the rhizosphere soil of Geodorum). F and G: Bar graphs of the bacterial community composition at the genus level (F: in the roots of Geodorum; G: in the rhizosphere soil of Geodorum)

The bacterial community composition of different species of Geodorum in the roots and rhizosphere soil varied. At the phylum level, Proteobacteria, Actinobacteriota, Acidobaceriota, Myxococcota and Bacteroidota were the top 5 most abundant bacteria in the roots (Fig. 2D). In addition, Proteobacteria, Actinobacteriota, Acidobaceriota, Myxococcota and Chloroflexi were the top 5 most abundant bacteria in the rhizosphere soil (Fig. 2E). The difference was that the proportion of Actinobacteriota in the rhizosphere soil (26%—45%) was higher than that in the roots (15%—24%) (Fig. 2D, E).

The composition and proportion of bacterial communities at the genus level in the roots and rhizosphere soil of Geodorum were analyzed (Fig. 2F, G). In the roots and rhizosphere soil of GA, the dominant bacterial genera were Delftia (16%) and Bradyrhizobium (5%). The dominant bacteria in the roots and rhizosphere soil of GD_understory were Delftia (11%) and Gaiella (7.3%), respectively. The more abundant bacterial genera in the roots and rhizosphere soil of GD_roadside were Mycobacterium (15%) and Gaiella (6.5%), respectively. In the root, the proportion of Mycobacterium in GD_roadside was higher than that in GD_understory, on the contrary, the proportion of Delftia and Bordetella in GD_roadside was lower than that in GD_understory. The dominant genera in the roots and rhizosphere soil of GE were Bordetella (10%) and Gaiella (7%), respectively. These results indicated that there were differences in the composition of bacteria in the roots and rhizosphere soil of different Geodorum.

Fungal community composition of three species of Geodorum growing in understory and roadside areas.

For fungal composition analysis in the roots and rhizosphere soil of Geodorum, ITS sequencing was performed on 24 samples, similar to the 16S rRNA approach. A total of 1,169,179 sequences numbers were obtained, with an average length of 253 bp sequences per sample (Table S5). In addition, the highest number of ITS OTUs in the GD_understory was found in both the roots and rhizosphere soil (Table 3). Similarly, there were more fungal species in the rhizosphere soil than in the roots of Geodorum. A total of 48 shared ITS OTUs were found in the roots of GE, GD_roadside, GD_understory and GA, and 79 shared ITS OTUs were found in the rhizosphere soil, which was much lower than their shared 16S OTUs (Fig. 3A, B). Overall, only 1,746 (33.23%) OTUs were shared between the roots and rhizosphere soil, which was lower than that of the bacteria (2783: 71.86%), which indicated that there were greater differences between the roots and rhizosphere soil when the fungi were analyzed (Fig. 3C).

Table 3 The information on ITS OTU classification statistics in Geodorum
Fig. 3
figure 3

Fungal composition of different Geodorum species. A, B and C: Venn diagram of different groups at the OTU level (A: in the roots of GE, GD_roadside, GD_understory and GA groups; B: in the rhizosphere soil of GE, GD_roadside, GD_understory and GA groups; C: in the root and rhizosphere soil groups in all the Geodorum species). D and E: Bar graphs of the bacterial community composition at the phylum level (D: in the roots of Geodorum; E: in the rhizosphere soil of Geodorum). F and G: Bar graphs of the bacterial community composition at the genus level (F: in roots of Geodorum; G: in rhizosphere soil of Geodorum). GA, Geoderma attenuatum; GD, Geodorum densiflorum; GE, Geodorum eulophioides; OTU, operational taxonomic unit. In the Venn diagram, the circle for each group represents a taxon, and the area of the circle represents the relative abundance of that taxon in the corresponding group. Overlapping regions represent common taxa between different groups, while non-overlapping regions represent unique taxa

A bar plot analysis of the fungal community showed the dominant fungi and their proportions in the roots and rhizosphere soil of Geodorum. At the phylum level, Ascomycota, and Basidiomycota had high proportions in the fungal community in both the roots and rhizosphere soil. In addition, the dominant fungal phyla in the roots and rhizosphere soil were basically the same. The proportion of Basidiomycota in the root and rhizosphere soil of GE was 74% and 67%, respectively (Fig. 3D, E). At the genus level, the dominant fungi in the roots of GA were Penicillium (4.5%), and in the rhizosphere soil, the dominant fungi was Trichoderma (5.3%) (Fig. 3F, G). Fusarium accounted for 25% of the roots of GD_understory. It was worth noting that the proportion of Fusarium in the root of GD_understory is higher than that in GD_roadside. Pyrenochaete (9.4%) was the dominant fungus in the rhizosphere soil of GD_understory. A high proportion of fungi included Coprinopsis (21%), Oxyporus (16%) and Neocosmospora (8.6%) in the roots of GD_roadside. Russula (51%) was the dominant fungi in the roots of GE (Fig. 3F). In the rhizosphere soil of GE, Russula was also present in the highest abundance (29%) (Fig. 3G).

Twenty-six genus-level mycorrhizal fungi, previously identified in orchids [34], were found in the three Geodorum species (Table S6). In all the root samples, the first three genera of related mycorrhizal fungi identified were Fusarium, Russula, and Penicillium. In addition, the proportion of mycorrhizal fungi in the roots of Geodorum showed that single mycorrhizal fungi (Russula and Fusarium) in GE and GD_understory accounted for more than 50%, while no such situation existed in GD_roadside and GA (Fig. S3).

α-Diversity analysis: Index group difference test

Based on the Shannon index, GD_understory had the highest level of 16S OTUs among the roots of Geodorum, but there was no significant difference compared with the other Geodorum (Fig. 4A). In contrast, the GD that grew in the understory and roadside had significantly higher levels of 16S OTUs than those in the rhizosphere soil of GA among the three species of Geodorum (Fig. 4B). It was also notable that GE had the lowest diversity in its ITS OTU Shannon diversity analysis. This was found in both its roots and rhizosphere soil (Fig. 4C, D). Low fungal diversity in GE and a high diversity of ITS OTUs were observed in GD_understory and GA.

Fig. 4
figure 4

Box plots of the Shannon indices of bacteria and fungi in the root and rhizosphere soil for GE, GD_roadside, GD_understory and GA. A: in the roots of Geodorum at the 16S OTU level; B: in the rhizosphere soil of Geodorum at the 16S OTU level; C: in the roots of Geodorum at the ITS OTU level; D: in the rhizosphere soil of Geodorum at the ITS OTU level. *P ≤ 0.05. GA, Geoderma attenuatum; GD, Geodorum densiflorum; GE, Geodorum eulophioides; ITS, internal transcribed spacer; OTU, operational taxonomic unit

NMDS and ANOSIM analysis

β-diversity was analyzed using non-metric multidimensional scaling (NMDS) to compare bacterial and fungal differences between roots, rhizosphere soil, and between endangered (GE) and widespread (GD and GA) species. At the 16S OTU level, there was no significant separation in the bacteria between the endangered species and widespread species groups, while there was a significant separation between the root and rhizosphere soil groups (Fig. 5A, B). This indicates a greater environmental than species influence on bacterial composition. In fungi, there was a significant difference between those groups of species that were endangered compared with those that were widespread (Fig. 5C, D). Analysis of similarity (ANOSIM) results revealed greater differences between root and rhizosphere soil than among Geodorum species at the bacterial 16S OTU level (R-value = 0.6409; P-value = 0.001) (Fig. 5E). As for fungi, the differences in different species of Geodorum were greater than the difference between the root and rhizosphere soil groups (R-value = 0.1154; P-value = 0.046) (Fig. 5F), which was consistent with the results of NMDS analysis.

Fig. 5
figure 5

NMDS and ANOSIM analysis. A, B, C and D: NMS analysis (A: in the endangered and widespread species groups at the 16S OTU level; B: in the root and rhizosphere soil groups at the 16S OTU level; C: in the endangered and widespread species groups at the ITS OTU level; D: in the root and rhizosphere soil groups at the ITS OTU level). E and F: ANOSIM analysis between the root and rhizosphere soil groups (E: at the 16S OTU level; F: at the ITS OTU level). ANOSIM, analysis of similarity; ITS, internal transcribed spacer; NMDS, non-metric multidimensional scaling; OTU, operational taxonomic unit

The differences in bacterial and fungal composition between the roots and rhizosphere soil and between endangered and widespread species of Geodorum

A significance test between groups identified microorganisms with significantly different abundances, aiding further analysis of the microbial composition of Geodorum. At the level of 16S OTU classification, 15 OTUs with significant differences were obtained by a Wilcoxon rank sum test. OTU2385 (g__Delftia), OTU2756 (g__Bordetella), OTU2600 (g__Bradyrhizobium), OTU2360 (g__Pseudorhodoplanes), OTU915 (g__Burkholderia-caballeronia-paraburkholderia), OTU2608 (g__norank_f__Hyphomicrobiaceae), and OTU2755 (g__Pseudomonas) were significantly more abundant in the roots than in the rhizosphere soil, and the proportion of OTU2491 (g__norank_f__Xanthobacteraceae), OTU2529 (g__norank_f__norank_o__norank_c__subgroup_22), OTU2760 (g__Gaiella), OTU1785 (g__Bacillus), OTU1762 (g__MND1), OTU2517(g__norank_f__67-14), OTU1792 (g__Gaiella) and OTU1842 (g__norank_f__norank_o__Gaiellales) in the rhizosphere soil was significantly higher than that in the roots (Fig. 6A). In fungi, only OTU4041 (g__unclassified_f__Geoglossaceae) was higher in the widespread than in the endangered species, and the other 14 OTUs were significantly higher in the endangered than in the widespread species, particularly OTU2686 (g__Russula) and OTU2488 (g__unclassified_f__Russulaceae) (Fig. 6B).

Fig. 6
figure 6

Bar graph of the species difference test. A: between the root and rhizosphere soil groups at the 16S OTU level; B: between the endangered and widespread species groups at the ITS OTU level. The positive and negative difference in mean relative abundance represents the abundance of OTUs in the corresponding group. *P ≤ 0.05. **0.01 ≤ P ≤ 0.05. ***0.001 ≤ P ≤ 0.01. ITS, internal transcribed spacer; OTU, operational taxonomic unit

LEfSe analysis

LEfSe analysis was used to identify the biomarker species in different Geodorum. In terms of bacterial composition, GE had four and GA had three dominant bacterial genera, whereas GD_roadside and GD_understory exhibited 13 and 14, respectively (Fig. 7A). Of the fungal compositions examined, GD_understory exhibited the greatest prevalence of fungi, with a count of 22. Conversely, GE had 10, GD_roadside had 9, and GA had 11 (Fig. 7B). At the bacterial phylum level, Acidobacteriota was enriched on GE, while Bacteroidota and Nitrospirota were enriched on GD_understory. At the level of the fungal phylum, the GE concentration of microorganisms comprises Basidiomycota and Mucoromycota. Chytridiomycota and Kickxellomycota exhibited GA enrichment, while Glomeromycota was enriched in GD_roadside enrichment and Ascomycota was enriched in GD_understory.

Fig. 7
figure 7

A: LEfSe analysis of bacterial composition in GA, GE,GD_understory and GD_roadside on the phylum to genus level. B: LEfSe analysis of fungal composition in GA, GE, GD_understory and GD_roadside on the phylum to genus level. ITS, internal transcribed spacer; OTU, operational taxonomic unit

Co-occurrence network analysis

The co-occurrence network map reflects the coexistence of species in different samples. By analyzing the species abundance information among different samples, the co-existence patterns of microbial species in different samples can be observed and understood (Figure S4). Twenty-two 16S OTUs were detected within the roots of at least two species of Geodorum, while 17 were found in the rhizosphere soil of at least two species of Geodorum (Figure S4A, B). Moreover, in the roots and rhizosphere soil, OTU2687 (g__Mycobacterium), OTU2666 (g__Bradyrhizobium), OTU2491 (g__norank_f__Xanthobacteraceae) and OTU2528 (g__Solirubrobacter) were their co-occurring 16S OTUs. Seven 16S OTUs detected in the rhizosphere soil of Geodorum were not found to be associated with its roots, whereas fourteen 16S OTUs detected in the roots were not associated with the rhizosphere soil (Figure S4C). Eight ITS OTUs were detected within the roots of at least two species of Geodorum, while nine were found in the rhizosphere soil of at least two species of Geodorum (Figure S4D, E). 19 of the ITS OTUs of the endangered species were not associated with the widespread species, and 38 of the widespread species were not associated with the endangered species, which also reflected the low number of highly abundant fungi in the endangered species (Figure S4F). Eight 16S OTUs were associated in the rhizosphere soil and roots of GA and eight in the rhizosphere soil and roots of GD_understory. The lowest number was 5 in GD rhizosphere soil and roots, while the highest number was 11 in the rhizosphere soil and roots of GE (Figure S5). Only two ITS OTUs were associated in the rhizosphere soil and roots of GA, whereas 12 ITS OTUs were present in the rhizosphere soil and roots of GE (Figure S6).

Discussion

The growth and development of these plants are closely linked to soil microorganisms, and analyzing the composition of these microorganisms plays a crucial role in promoting plant conservation [2]. This study analyzed the composition of bacteria and fungi in the roots and rhizosphere soil of GE, GD_roadside, GD_understory, and GA. To explore the microbial diversity of roots and rhizosphere soil of Geodorum by detecting microbial species in roots and rhizosphere soil in different habitats, and to provide reference for future conservation and breeding research of Geodorum.

Differences in the microbial composition of roots and rhizosphere soil in the roadside and understory habitats

In the 16S and ITS OTU taxonomy, the number of microorganisms in each sample at each taxonomic level was analyzed (Table 2 and 3). Although there was no clear difference in the number of 16S OTUs in the rhizosphere soil of GD_roadside and GD_understory, there were more 16S OTUs in the roots of GD_understory than in the GD_roadside. At the phylum level, Proteobacteria, Actinobacteriota, Acidobaceriota, Myxococcota were the most abundant bacteria in the roots and rhizosphere soil of Geodorum (Fig. 2D, E). In the LEfSe analysis, Acidobacteriota was enriched on GE, while Bacteroidota and Nitrospirota were enriched on GD_understory. The soil in GE was more acidic, which may have contributed to the higher abundance of Acidobacteriota in roots and rhizosphere soil of GE than that in GD_understory, GD_roadside and GA. Some studies have found that soil with low pH was more conducive to the growth and abundance of Acidobacteriota, while soil with high pH has a negative effect on Acidobacteriota [35]. The high abundance of Bacteroidota and Nitrospirota might be attributed to the high organic matter and nitrogen content in the soil of GD_understory [36].

In addition, the GD_understory had more ITS OTUs than the GD_roadside in both the roots and rhizosphere soil. This indicated that the effect of understory habitat on soil microbial structure is primarily on fungi, which was consistent with the structure of research on the influence of understory vegetation on the soil microbial community structure [37]. Soils rich in organic matter typically facilitate increased microbial abundance [38]. The soil organic matter content in GD_understory was significantly higher than that in GD_roadside, and the soil in GD_roadside was relatively poor, resulting in lower microbial abundance than that in GD_understory (Table S1).

GE, GD_roadside, GD_understory and GA had similar dominant bacterial and fungal phyla in the roots and rhizosphere soil. Proteobacteria, Actinobacteriota and Acidobacteriota were the dominant bacterial phyla of the roots and rhizosphere soil in Geodorum. These bacterial phyla promote the decomposition of organic material, aiding the plants in absorbing elements like nitrogen, phosphorus (P), and potassium (K) [39,40,41,42]. At the genus level, the dominant bacteria in the rhizosphere soil and roots were different. Delftia and Bordetella were the dominant genera in the roots of Geodorum, while Gaiella and Solirubrobacter were the dominant genera in the rhizosphere soil. In the co-occurrence analysis, 22 16S OTUs and 17 16S OTUs were identified in the roots and rhizosphere soil of at least two species Geodorum, respectively. It may reflect a wide range of adaptations of some microorganisms to environmental conditions, or it may be caused by common characteristics between samples, suggesting that these microorganisms may have a wide range of adaptive adaptations, with similar patterns of presence among Geodorum. Similarly, Ascomycota and Basidiomycota were the dominant fungal phyla in the roots and rhizosphere soils of GD_roadside, GD_understory, and GE. Additionally, orchid mycorrhizal fungi are derived from the root endophytic fungi, and many Ascomycota and Basidiomycota fungi are endophytic [43,44,45]. The growth of orchids depends on the assistance of mycorrhizal fungi in the absorption of various elements in the soil, and mycorrhizal fungi can promote the germination of orchid seeds [46, 47]. Compared with GD_roadside and GA, the roots of GD_understory and GE had relatively single mycorrhizal fungi (Table S6), which might be related to the specific selection of the fungi on the host [48], but their specificity needs to be further studied.

In the root, the proportion of Mycobacterium in GD_roadside was higher than that in GD_understory, on the contrary, the proportion of Delftia and Bordetella in GD_roadside was lower than that in GD_understory. Delftia can promote plant growth and produce siderophores, which enables it to serve as an endophyte that facilitates the absorption of iron by Geodorum [49, 50]. The root of GD_roadside had a higher proportion of Mycobacterium than the root of GD_understory, but the reason for this difference has not been determined. The dominant fungi in rhizosphere soil and roots of GD_understory and GD_roadside differed considerably at the genus level. In the roots of GD_understory and GD_roadside, their primary types of endophytic fungi also differed at the genus level with the endophytic fungi of GD_roadside primarily related to Coprinopsis, Oxyporus, and Neocosmospora. Nevertheless, the endophytic fungi in GD_understory were primarily identified as Fusarium and Neocosmospora. In recent studies, Fusarium have been found to cause root rot and stem rot in plant, resulting in poor plant growth, yellow and wilting leaves, and even death in severe cases [51]. However, Fusarium has been identified as a mycorrhizal fungus in some Orchidaceae species, including Dendrobium officinale and Paphiopedilum [52, 53]. Fusarium can improve the absorption of P, K and calcium and the activity of various antioxidant enzymes, which can enhance the adaptability of orchids to manage the external environment [54]. Since orchids often grow in environments with high humidity and temperature, these conditions are often also suitable for the propagation and infection of Fusarium in plants [55]. The high nitrogen content in the soil of GD_understory may also be one of the reasons for the growth and reproduction of Fusarium [56]. Oxyporus enhances the decomposition of organic matter, thereby improving nutrient conversion efficiency It can also repair soil to some degree and reduce the damage to plants from heavy metals in soil [57, 58]. As a orchid plant, GD_understory may have a special nutritional relationship with Fusarium, and its root may form mycorrhizal with Fusarium and rely on this fungus to provide nutrition, but this needs further study. In addition, Neocosmospora, a plant endophyte, is associated with mold in plants, thus, affecting plant growth [59]. Furthermore, α-diversity analysis reveals that both bacterial and fungal diversity in the roots of GD_understory surpass those in GD_roadside, as indicated by 16S and ITS OTU counts.

Differences in fungal composition in the roots and rhizosphere soil between endangered and widespread species

The characteristics of fungi in endangered and widespread species were analyzed to understand whether the process of GE becoming endangered was related to the fungal composition in the roots and rhizosphere soil. Analysis revealed that GE exhibited the lowest number of ITS OTUs, potentially impeding its growth. The fungal community in the soil is closely related to the growth of plants, and the diversity of soil fungi can improve the resistance of plants to the environment, which can not only promote the growth of plants but also maintain the stability of ecosystems [60]. Many mycorrhizal fungi of the Orchidaceae are members of Ascomycota, Basidiomycota and Mortierellomycota, and according to the mycorrhizal fungi identified in orchids, fewer ITS sequences associated with Ascomycota were screened in the roots of GE than in the roots of GA and GD, including Aspergillus, Penicillium and Fusarium. The diversity, abundance and composition of soil microorganisms affect the stability of soil ecosystems, the efficiency of soil nutrient cycling, and the healthy growth of plants [61]. This suggested that lower fungal diversity may be one of the reasons why GE is an endangered species. Although Basidiomycota is the most common mycorrhizal fungal phylum in orchids, the high abundance of Basidiomycota in the roots or rhizosphere soil of GE is owing to the presence of a single high abundance of Russula [62, 63]. This suggested that the fungi of GE are primarily associated with Russula, aligning with the differences observed between widespread and endangered species. Russula typically thrives in soils that are abundant in organic matter, such as forest or woodland soils. It can also grow in soils that are either acidic or neutral, although it is comparatively less well-suited to alkaline soils [64]. Therefore, acidic soils in GE habitats may contribute to the high abundance of Russula. In addition to soil pH, since GE grows in the understory, the composition of microorganisms is also affected by the upper trees, and the dominance of Russula is also affected by the composition of the tree community, especially the association of its ectomycorrhizae with tree roots. Some tree species may have a preference for a symbiotic relationship with Russula, resulting in its dominance in the mycorrhizal community [65]. Other previous research indicates a negative correlation between Russula abundance and overall fungal diversity because mycorrhizal metabolites and proteins had selective antimicrobial (anti-microbial) effects, especially against rhizosphere bacterial species, leading to a decreasing trend in the diversity of fungal and bacterial species in the mycorrhizal sphere, possibly contributing to the low fungal diversity observed in GE's root and rhizosphere soil [66]. Although heterotrophic effects that depend on Russula are suspected on violet bird's-nest (Limodorum abortivum), L. trabutianum and L. brulloi [67, 68], there is also evidence that a single mycorrhizal fungus can have a large limiting effect on plant growth and distribution [69]. Interestingly, the exclusivity of a single fungus has been reported in some orchids or other plants, particularly in mycoheterotrophic angiosperms, which could indicate that Russula is associated with low fungal diversity in the roots of GE [70,71,72]. Molecular identification studies have shown that GE has a strong specificity for fungi, and this bias is also present in other Orchidaceae plants, which may be due to the specific selection of fungi on their hosts or orchids on fungi [73, 74]. Thus, the high abundance of Russula in GE may be its specific selection for fungi. The types of colonization by mycorrhizal fungi on orchids primarily include specific colonization, extensive colonization, and specific-extensive facultative colonization. There were differences in the composition of fungal species between GD_understory and GD_roadside, particularly those that had been identified as mycorrhizal fungi in other orchids, which could indicate that there were extensive colonization types of GD and fungi.

The g_unclassified_f__Geoglossaceae abundance of GE was significantly lower than those of widespread species. Currently, it has been found that Geoglossomycetes can form hyphal coils in the root cortex of plants, which could promote the exchange of nutrients between Geoglossomycetes and their roots [75]. The abundance of Fusarium and Neocosmospora, which could support the growth, nutrient absorption and ecological adaptability of Orchidaceae, were significantly lower in the root of GE than in the root of GD and GA [76]. As a result, GE has a low abundance of fungi in its roots compared with the widespread species, which could affect its ability to reproduce. It is still controversial whether there is a relationship between the rarity of orchids and the specificity of fungi. Currently, it has been reported that the endangered grand spider orchid (Caladenia huegelii) is threatened because of its high specificity with mycorrhizal fungi, which affects its mycorrhizal establishment with other fungi [77]. Studies have also shown that GE has small seeds and a low germination rate, which prevents the population of GE from expanding [3]. The tiny seeds and lack of endosperm in orchids, such as pigeon orchids (Dendrobium crumenatum), contribute to their low fecundity, which is one of the reasons why they are endangered [78]. The endangered status of GE may be attributed to the specific symbiosis between GE and Russula, coupled with the absence of other beneficial fungi, leading to reduced growth and reproductive capabilities. Consequently, orchids require endophytic fungi to promote seed germination under natural conditions, and GE could lack the assistance of endophytic fungi to promote its growth owing to its low fungal diversity, which could further contribute to its endangered state.

Factors that affect low microbial diversity

The α-diversity analysis of bacteria and fungi in the root and rhizosphere soil of Geodorum indicated that GA had the lowest bacterial diversity in the rhizosphere soil (Figure S2). In low-altitude areas, soil carbon, N, and P contents generally rise with increasing altitude, peaking in mid-altitude regions before decreasing in higher-altitude areas. Similarly, bacterial diversity tends to increase up to a certain altitude and then decreases at higher altitudes [79,80,81]. The variation in climate and precipitation between Baise City and Chongzuo City suggests that altitude is a key factor influencing soil microbial diversity in GA, warranting further investigation. In line with the above findings, α-diversity analysis revealed the lowest ITS OTU levels in GE's roots and rhizosphere soil, suggesting minimal fungal diversity, possibly due to the dominance of the fungus Russula. The results of an NMDS analysis showed that the difference in the levels of 16S OTUs between the roots and rhizosphere soil was greater than that between the endangered and widespread species. In contrast, there was a greater difference in the levels of ITS OTUs between the endangered and widespread species than between the roots and rhizosphere soil. This indicates that there is some degree of independence of bacterial characteristics between the roots and rhizosphere soil and reflects that the fungal composition of soil may relate to the fungal species in the roots of Geodorum. According to the results of intergroup differences and co-occurrence analysis, the proportions of OTU2385 (g_Delftia), OTU2756 (g_Bordetella) and OTU2755 (g_Pseudomonas) in the roots were significantly higher than those in the rhizosphere soil (P ≤ 0.001), which may be related to soil properties, microbial relationships, microbial physiological adaptations, plant regulation, etc. [82].

Conclusions

In this study, the bacterial and fungal diversity of the roots and rhizosphere soil in GE, GD_roadside, GD_understory and GA were analyzed. The study revealed that GA's rhizosphere soil, located at the lowest altitude compared to GD and GE, exhibited the lowest 16S OTU levels. A low-altitude habitat could be one of the reasons for the low bacterial diversity in the rhizosphere soil of GA. The lower fungal and bacterial diversity in the root of GD_roadside compared to GD_understory may be related to the lower soil organic matter and nitrogen content in GD_roadside, which may hinder the growth and reproduction of Geodorum. Additionally, α-diversity analysis indicated the lowest ITS OTU levels in both the roots and rhizosphere soil of GE. In GE, the dominance of the fungus Russula in both roots and rhizosphere soil correlates with low fungal diversity, potentially contributing to its endangered status. GE growth in acidic soils and understory environments may be related to the high abundance of Russula in roots and rhizosphere soils. In contrast, there was a variety of dominant fungi in the roots and rhizosphere soil of widespread species, including Fusarium and Neocosmospora, Nectriaceae, Coprinopsis, and Oxyporus, among others, which may have some influence on the distribution and reproduction of Geodorum.

Availability of Data and Materials

The sequencing data have been deposited in the NCBI with Sequence Read Archive (SRA) accession No. PRJNA953938.

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Acknowledgements

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Funding

This study was supported by the special funds for biosafety and genetic resource management of the National Forestry and Grassland Administration (KJZXSA202307), Guangxi Forestry Science and Technology Promotion Demonstration Project (Guilinkezi [2021] No. 28), the Guangxi Academy of Sciences Scholars Innovation Team Launch Project (CQZ-C-1902), sustainable development innovation project and English course construction project for postgraduates of Guangxi Normal University (2020CX003; 2021XJQYW01), Innovation Project of Guangxi Graduate Education (YCSW2023127), and Innovation training program for university students (202210602020).

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YL and SC designed the study. JL, DZ, LZand YH performed the experiments. JL, YS, LZ and HJ analyzed the data and drafted the manuscript. YL and SX helped in sample collection. YH helped in data analysis. All authors have read and approved the final paper.

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Correspondence to Yu Liang or Shengfeng Chai.

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The authors declare no competing interests.

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All the roots and rhizosphere soils were collected from three species of Geodorum in China. GE, GD, and GA were collected from the Yachang Orchid Nature Reserve, Baise City, Guangxi Province, China; and Minqiang Village, Longzhou County, Chongzuo City, Guangxi Province. The Yachang Orchid Nature Reserve and village government permit us to collect them for scientific research.

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Liu, J., Zeng, D., Huang, Y. et al. The structure and diversity of bacteria and fungi in the roots and rhizosphere soil of three different species of Geodorum. BMC Genomics 25, 222 (2024). https://doi.org/10.1186/s12864-024-10143-2

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