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The Characterization of Microbiome and Interactions on Weathered Rocks in a Subsurface Karst Cave, Central China

Karst caves are a natural oligotrophic subsurface biosphere widely distributed in southern China. Despite the progress in bacterial and fungal diversity, the knowledge about interactions between bacteria, fungi, and minerals is still limited in caves. Hence, for the first time, we investigated the interaction between bacteria and fungi living on weathered rocks in the Heshang Cave via high-throughput sequencing of 16S rRNA and ITS1 genes, and co-occurrence analysis. The mineral compositions of weathered rocks were analyzed by X-ray diffraction. Bacterial communities were dominated by Actinobacteria (33.68%), followed by Alphaproteobacteria (8.78%), and Planctomycetia (8.73%). In contrast, fungal communities were dominated by Sordariomycetes (21.08%) and Dothideomycetes (14.06%). Mineral substrata, particularly phosphorus-bearing minerals, significantly impacted bacterial (hydroxyapatite) and fungal (fluorapatite) communities as indicated by the redundancy analysis. In comparison with fungi, the development of bacterial communities was more controlled by the environmental selection indicated by the overwhelming contribution of deterministic processes. Co-occurrence network analysis showed that all nodes were positively linked, indicating ubiquitous cooperation within bacterial groups and fungal groups, as well as between bacteria and fungi under oligotrophic conditions in the subsurface biosphere. In total, 19 bacterial ASVs and 34 fungal OTUs were identified as keystone taxa, suggesting the fundamental role of fungi in maintaining the microbial ecosystem on weathered rocks. Ascomycota was most dominant in keystone taxa, accounting for 26.42%, followed by Actinobacteria in bacteria (24.53%). Collectively, our results confirmed the highly diverse bacterial and fungal communities on weathered rocks, and their close cooperation to sustain the subsurface ecosystem. Phosphorus-bearing minerals were of significance in shaping epipetreous bacterial and fungal communities. These observations provide new knowledge about microbial interactions between bacteria, fungi, and minerals in the subterranean biosphere.


INTRODUCTION
Karst caves are thought to be barren with few microorganisms and a weak reflection of the microbiology of surface soils due to oligotrophic conditions (Hess, 1900;Høeg, 1946;Caumartin, 1963;Palmer, 1991). Autotrophic microorganisms in caves usually obtain energy by chemosynthesis using inorganic energy sources (reduced Fe, Mn, and S compounds), organic and inorganic nutrients in host rocks, cave sediments, groundwater, and atmosphere (Jones and Macalady, 2016;Tomczyk-Żak and Zielenkiewicz, 2016;Hershey and Barton, 2018). The occurrence of various metabolic pathways is concurrent in cave microbiota (Kováč, 2018). In consideration of the oligotrophic conditions in caves, the microbial diversity encountered is surprisingly higher than expected as indicated by the application of molecular technology (routinely 10 6 cells/g; Hershey and Barton, 2018).
Surfaces of various materials have been demonstrated to serve as important niches for microbial communities in diverse ecosystems, such as the surface of the painted murals, heritage buildings, petroglyph panels, and rock surfaces (Ma et al., 2015;Brewer and Fierer, 2018;Zhang et al., 2018;Irit et al., 2019;Ren et al., 2019;He et al., 2021). Rock surfaces are subjected to weathering by physical, chemical, and biological processes, thus offering special niches for microorganisms (Cañveras et al., 2001;Lian et al., 2008). Abundant radiation-resistant bacteria on the surface of limestone outcrops were detected, which were associated with lichens and grew under neutral to alkaline pH conditions (Brewer and Fierer, 2018). Usually, bacterial communities living on outcrop carbonate rocks exposed to sunlight and rainfall were dominated by Actinobacteria, Proteobacteria, Chloroflexi, Bacteroidetes, and Acidobacteria, whereas fungal communities consisted of Eurotiomycetes, Lecanoromycetes, Dothideomycetes, and Leotiomycetes (Choe et al., 2018). Microbial communities inhabiting the surfaces of carbonate rocks in permanently dark caves (Man et al., 2015;Yun et al., 2016;Zhu et al., 2021) are far less studied than those associated with outcrop rocks. Rock surfaces in subsurface caves are directly exposed to air, aerosol, and water vapor (high humidity), as well as a variety of physicochemical and biological dissolutionprecipitation and oxidation-reduction reactions, leading with time to weathering and the formation of various secondary minerals (Aloisi et al., 2006;Gallagher et al., 2012). Rock walls act as surface biofilms for exchanges between the bedrock and the atmosphere. Microorganisms can use many minerals as sources of nutrients, carbon, and energy (Tomczyk-Żak et al., 2013). Nevertheless, the current knowledge is ambiguous on microbial communities in relation to mineral substrates and secondary minerals formed during rock weathering in subsurface caves.
Studies have shown that microbial communities in caves are affected by a variety of physical and chemical parameters. Studies in the Heshang Cave, a karst dolomite cave, have shown that pH and TOC are important drivers of the variations in bacterial communities among sediments, overlying soils, dripping water, and weathered rocks (Yun et al., 2016;Cheng et al., 2021). The underlying factors resulting in differences in bacterial and fungal communities living on rocks in caves are poorly understood. The physical properties and chemical compositions of minerals can profoundly impact the composition of microbial communities. Mineral phases in rocks serve as nutrients, substrates, and habitats for microbial communities (Shi L. et al., 2016). Some microbes use conductive mineral particles as conduits of interspecies electron transfer and cooperative catabolism (Kato et al., 2012). Actinobacteria are prevalent in Ca carbonate environments, and alpha-, beta-, and gamma-Proteobacteria are typically associated with complex minerals in cave environments (Barton et al., 2007).
Metabolic activities of microorganisms have important effects on the dissolution and formation of minerals. Moderately halophilic bacteria in liquid media cause the precipitation of calcite, Mg-calcite, and struvite (Arias et al., 2019). Carbonate biomineralization can be enhanced by ureolytic bacteria (Dhami et al., 2013;Arias et al., 2019). Paracoccus versutus XT0.6 isolated from the Xikuangshan antimony mine could dissolve stibnite and oxidize released Sb(III) to Sb(V), subsequently resulting in the formation of secondary Sb(V)-bearing minerals (Loni et al., 2020).
Highly diverse bacterial communities were detected from the weathered rocks in caves with the dominance of Proteobacteria, Actinomycetes, and Firmicutes (Yun et al., 2016;Zhu et al., 2019Zhu et al., , 2021Ma et al., 2021). In contrast, the diversity of fungi is relatively low due to the limited input of organic matter by photosynthesis in caves (Lee et al., 2012;Man et al., 2015). It was estimated that the content of organic matter in caves is three orders of magnitude less than that on the surface (Lavoie et al., 2010). Sunlight penetrates into the cave via the cave entrance to a limited distance and thus divides the cave into three zones: the photic zone with relatively strong light, the twilight zone with weak light, and the totally dark aphotic zone (Yun et al., 2016;Zhao et al., 2018). Due to the different light intensities, physical and chemical conditions vary in the three zones, resulting in different geochemical gradients and biological distribution patterns (Bonacci et al., 2009). In the photic zone, algae and green plants are visible on the rock surface and ground. Light is sufficient to support photosynthesis, thereby supporting CO 2 fixation and primary production . The availability of organic matter in the twilight and aphotic zones is extremely limited as it mainly depends on the input of exogenous organic matter via airflow, bat feces, and external organic matter excreted by burrowing animals such as cave rats (Pape and OConnor, 2014;Pfendler et al., 2019). Due to the differences in light, mineral components, and organic matter from different light zones, we hypothesize that (1) microbial communities living on the rocks vary with the zones, and mineral substrates significantly contribute to the variation; (2) bacterial and fungal communities interact intensively to sustain the microbial ecosystem on the rock; and (3) different ecological processes would contribute to the community assembly of bacteria and fungi, respectively.
To test these hypotheses, we collected weathered rock samples from different light zones in the Heshang Cave and subjected them to high-throughput sequencing of bacterial 16S rRNA and fungal ITS1 genes to investigate microbial communities. Variations in microbial communities and the driving forces responsible for these changes would be elucidated via the redundancy analysis. Interactions between bacterial and fungal communities were studied via co-occurrence network analysis to decipher how microbes interact with other microorganisms and sustain the ecosystem. Ecological processes and their contributions to the bacterial and fungal community assembly will be conducted to help understand how the specific microbial communities are established in caves. Our results will provide new insights into the interactions between bacteria and fungi living on carbonate rocks and the ecological processes responsible for microbial communities within subsurface caves.

Site Description and Sample Collection
The Heshang Cave, a dolomite karst cave, is 250 m long, 20-30 m wide, and 15-20 m high. It is located on the steep south bank of the Qingjiang River, northwest Hubei province, central China, with an elevation of 194 m above sea level (Supplementary Figure 1). An intermittent stream develops inside the cave during the rainy season, and dripping water is frequently observed from the ceiling of the cave all year round. The humidity is above 90% till saturated (Hu et al., 2008).
Weathered rock samples from the cave walls were collected along the cave from the entrance to the end on October 25, 2015. In total, nine sites were selected for sampling, with triplicates at each site (Supplementary Figure 1D), and the samples were designated as R1 to R9 accordingly. Green microbial mats were present on the surface of the cave walls close to the cave entrance ( Supplementary Figure 2). At each sampling site, weathered rock samples were carefully scraped off with a sterilized scalpel and stored in 50 mL centrifuge tubes. The samples were placed on ice and transported to the Geomicrobiology Laboratory of China University of Geosciences (Wuhan) within 24 h and stored at -80 • C upon arrival until analysis. The wind speed and relative humidity were measured in situ with a handheld weather station (XYZ06E, Dalian Hede Technologies Corporation, China; Supplementary Figures 3A,B). The wind speed and relative humidity at each sampling site were continuously monitored for over 10 min. Values at 3, 6, and 9 min were read, and the mean values were used.

Mineralogical Analysis
The weathered rock samples were freeze-dried (ALPHA 1-2 LD, Christ, Germany) and fully ground into powder. Mineral phases were analyzed by X-ray powder diffraction (XRD, Shimadzu XRF-1800) at a scanning speed of 0.05 s per step, with a step scan of 0.02 • (10 • ≤ 2 θ ≤ 90 • ) via a Cu target Kα radiation source (Ni filter, 40 kV, 40 mA). The phase composition and content of minerals in the samples were qualitatively and semiquantitatively analyzed by Jade7 and X-powder software.

DNA Extraction and Sequencing
Genomic DNA was extracted using a FastDNA TM SPIN Kit for soil DNA extraction (MP Biomedicals) in accordance with the instructions. The concentration and quality of extracted DNA were detected by using a micro-nucleic acid protein detector (Nanodrop 2000, Thermo Fisher). The primer set of 520F (5'-AYTGGGYDTAAAGNG-3') and 802R (5'-TACNVGGGTATCTAATCC-3') targeting the bacterial 16S rRNA V4 region (Claesson et al., 2009(Claesson et al., , 2010 and the primer set of ITS5F (5'-GGAAGTAAAAGTCGTAACAAGG-3') and ITS1R (5'-GCTGCGTTCTTCATCGATGC-3') targeting the fungal internal transcribed spacer (ITS1) region (Chang et al., 2001) were used for bacterial and fungal sequencing, respectively. All the sequences were conducted using an Illumina MiSeq PE250 platform (Shanghai Personal Biotechnology Co., Shanghai, China). All data are accessible via BioProject IDs of PRJNA337918 and PRJNA821722 for bacteria and fungi, respectively, on the NCBI.

Data Processing and Statistical Analysis
FLASH (v1.2.7) 1 was used for quality checking the original readings with Q30 and sequence assembly. Chimeras were removed by a DADA2 plugin in QIIME2 (2019.7, Quantitative Insight into Microbial Ecology). A table of bacterial amplicon sequence variants was constructed from the clean sequences with a 100% similarity, and the representative sequence of each ASV was obtained. Fungal OTUs were identified with a 97% similarity using Vsearch (2.15.1) software. All samples were resampled to the same sequencing depth. Bacterial annotation was carried out against the SILVA database, 2 and fungal annotation was based on the UNITE database 3 (Nilsson et al., 2019).
The microbial diversity index was calculated by a diversity plugin of QIIME2. The one-way analysis of variance (ANOVA) and Pearson correlation analysis were carried out using SPSS (v10.0). The heatmap analysis was performed using the OmicShare tools, a free online platform for data analysis. 4 The vegan package of R software was used for NMDS analysis and output of rarefaction curves (Dixon, 2003), and the box diagram and stacked bar chart were visualized by the ggplot2 package of R software (Wickham et al., 2016). The Venn diagram was drawn using the plotrix package (Lemon et al., 2021). The redundancy analysis (RDA) of bacterial communities and physicochemical parameters was conducted by Canoco5 software. Indicator groups in the different light zones were obtained online with the interactive web pages 5 by using the least discriminant analysis effect size (LEfSe) method, in which the linear discriminant analysis (LDA) threshold was set to 3.0. To reduce the network complexity, bacterial ASVs and fungal OTUs detected in at least three samples were selected. The relative abundance of retained bacterial ASVs accounted for > 36.6%, and the numbers of ASVs accounted for 6.6% of the total. The relative abundance of retained fungal OTUs accounted for > 94.4%, and the numbers of OTUs accounted for 15.2% of the total. The Gephi software (v.0.9.2) was used to visualize the co-occurrence network of bacteria and fungi. The ecological roles of each node were determined based on within-module connectivity (Zi) and among-module connectivity (Pi; Guimera and Amaral, 2005). Highly associative "hubs" in the microbiome can be identified from the network and are considered keystone taxa (Banerjee et al., 2018). Node topologies were classified as module hubs (highly connected nodes within modules, Zi ≥ 2.5 and Pi ≤ 0.62), network hubs (highly connected nodes within the entire network, Zi ≥ 2.5 and Pi > 0.62), connectors (nodes that connect modules, Zi < 2.5 and Pi ≥ 0.62), and peripherals (nodes connected in modules with few outside connections, Zi < 2.5 and Pi < 0.62; Deng et al., 2012;Shi S. et al., 2016). The assessment of ecological processes was performed with a mature workflow from the published literature (Stegen et al., 2012(Stegen et al., , 2013. The nearest taxon index (NTI), mean nearest taxon distance (MNTD), weighted β-mean nearest taxon distance (βMNTD), and weighted β-nearest taxon index (βNTI) were utilized to measure the phylogenic turnover using the theory of null model analyses across samples using the picante package (Kembel et al., 2010). Ecological processes were divided into deterministic processes with a |βNTI| > 2 and stochastic processes with a |βNTI| < 2. If βNTI values are above 2, variable selection is the crucial assembly process in the microbial community; otherwise, homogeneous selection dominates (βNTI < -2). To further specify the stochastic processes, the Raup-Crick matrix (RC bray ) based on the Bray-Curtis matrix of microbial community was calculated using the vegan package. Dispersal limitation acting with the drift, undominated processes, and homogenizing dispersal were, respectively, dominant in bacterial communities under the conditions of RC bray values > 0.95, | RC bray | < 0.95, and RC bray < -0.95 (Stegen et al., 2012(Stegen et al., , 2013.

Mineralogy, Wind Speed, and Relative Humidity in Heshang Cave
Minerals of the weathered rocks in the photic zone were dolomite, calcite, Mg-calcite, quartz, and amorphous materials (Supplementary Table 1). More minerals were detected in samples collected in the twilight zone, with the dominance of dolomite and quartz and a minor proportion of amorphous materials (Supplementary Table 1). Phosphate minerals (hydroxyapatite and fluorapatite), gypsum, and illite were also observed in twilight zone samples. Samples in the aphotic zone harbored eight minerals with Mg-calcite (18.6%) and phosphate minerals as the most abundant.
The average wind speed decreased from the cave entrance inward to the cave throughout the year. It was relatively stable

Bacterial and Fungal Communities on the Weathered Rocks
A total of 6,885 bacterial ASVs and 5,320 fungal OTUs were obtained in this study, and 511 bacterial ASVs and 1,269 fungal OTUs were found in samples from photic, twilight, and aphotic zones as indicated by the Venn diagram (Supplementary Figure 4). The rarefaction curves of bacterial communities were leveled off across all sampling sites, whereas those of fungal communities at the R5 sampling site were rather steeper (Supplementary Figure 5).
No significant differences were observed in the alpha diversity of bacterial communities among different zones. The Shannon indices varied between 7.56 and 8.12, and ACE values ranged between 4.18 and 10.60 (Figures 1A,B and Supplementary Table 4). The alpha diversity of fungi showed significant differences in the Shannon indices but not in ACE values between the three zones ( Figures 1C,D and Supplementary Table 4).
The NMDS analysis showed poor interpretation of bacterial communities between the three light zones (stress > 0.2; Figure 1E), but clearly separated the fungal communities between the photic zone and the aphotic zone, while those in the twilight zone were scattered around ( Figure 1F).

The Correlation Between Microbial Communities and Mineral Substrate
RDA was conducted to investigate the relationship between mineral phases and microbial communities living on the weathered rock. All minerals such as quartz, carbonate minerals (including dolomite, calcite, Mg-calcite, and aragonite), gypsum, illite, phosphate minerals (including white apatite, hydroxyapatite, and fluorapatite), and amorphous materials were included to elucidate their impact on bacterial and fungal communities. The results showed that hydroxyapatite and fluorapatite significantly affected bacterial and fungal communities with an explanation of 22.9% (P = 0.018) and 31.2% (P = 0.006), respectively (Figures 3A,B).

Microbial Community Assembly on the Weathered Rocks
The median of the βNTI matrix was below -2, indicating that the deterministic process controlled the assembly of bacterial communities ( Figure 4A). Bacterial community assembly was overwhelmingly dominated by the homogeneous selection, with a contribution from 71.43 to 92.86% (Figure 4C). By contrast, the median of the βNTI matrix of fungal communities was between -2 and 2, indicating the dominance of the stochastic process in fungal community assembly ( Figure 4B). Thus, ecological processes responsible for fungal community assembly were more complex than those for bacterial communities. Variable selection contributed 42.86 and 47.62% in the photic and twilight zones, respectively, but decreased to 10% in the aphotic zone, which was dominated by homogeneous selection (40%; Figure 4C). The contribution of dispersal limitation decreased inward to the cave from 23.81% in the photic zone, 19.05% in the twilight zone, to no contribution in the aphotic zone ( Figure 4C).

Interactions Between Bacterial and Fungal Communities Living on Weather Rocks
In total, 924 nodes and 7,425 links were observed in the cooccurrence network of bacteria and fungi with good modularity (0.788). Among the links, 800 connected fungal and bacterial nodes, 2,776 connected bacterial nodes, and 3,849 connected fungal nodes, respectively ( Figure 5A). All nodes were positively linked. The average path length, diameter, and clustering coefficient were 5.634, 14, and 0.618, respectively.
Totally 28 modules were observed in the fungal-bacterial interaction network, and nine of the modules had a node relative abundance of over 4%, which were subject to further analysis ( Figure 5B). Module 14 had the most nodes, accounting for 20.56% of the total nodes in the network. Nodes in modules 6, 18, and 22 mainly originated from PZ and TZ, whereas those in module 7 were mainly from AZ ( Figure 5C). Nodes in modules 13 and 14 were evenly contributed by the three zones. Fungi dominated in modules 6, 13, 14, 18, and 22 (Figure 5D), and nodes in these modules were mainly affiliated with Ascomycetes. By contrast, bacteria dominated in modules 7, 9, 11, and 17 ( Figure 5D), with the dominance of Actinobacteria. Actinobacteria and Ascomycota accounted for 19.59 and 16.99% of the total nodes, respectively.
Microbial keystone taxa were highly connected taxa that individually or in a guild exerted a considerable influence on the microbiome structure and functioning (Banerjee et al., 2018). Overall, 53 keystone taxa were identified (Figure 5E), five of them were module hubs (0.54% of all nodes), and the rest were connectors (5.19% of the total nodes). The module hubs and connectors accounted for 35.85, and 64.15% of all keystone taxa, respectively. Among 53 keystone taxa, 34 were affiliated with fungi and 19 were from bacteria. Ascomycota was the most dominant in keystone taxa, accounting for 26.42%, of which the  The contribution of each ecological process to microbial community assembly in different zones in the Heshang Cave (C). PZ_B, TZ_B, and AZ_B indicate the ecological processes responsible for bacterial community assembly in the photic zone, twilight zone, and aphotic zone, respectively, whereas those PZ_F, TZ_F, and AZ_F denote fungal community assembly.

Variation of Microbial Communities on Weathered Rocks Along the Cave Passage
Proteobacteria and Actinomycetes were previously reported to dominate bacterial communities living on the weathered rocks (Tomczyk-Żak and Zielenkiewicz, 2016), which matched well with our observation of the dominance of Actinomycetes (37.66%) and Proteobacteria (12.68%) in the Heshang Cave. Actinomycetes can interact with a variety of mineral phases (Abdulla, 2009;Cuezva et al., 2012) and metals (Manimaran and Kannabiran, 2017) and are capable of degrading various organic compounds (Ningthoujam et al., 2012), which enables them to survive in extreme environments like caves. Proteobacteria (12.68%) ranked the second most abundant linage in the Heshang Cave, indicating highly diverse metabolic capabilities and important roles in the global carbon (Huügler et al., 2005;Kang et al., 2019;Schada von Borzyskowski et al., 2019), nitrogen (Shapleigh, 2011;De Mandal et al., 2017;Delmont et al., 2017), and sulfur cycles (Campbell et al., 2006;Marshall and Morris, 2013). The relative abundance of Planctomycetes (8.92%) in the Heshang Cave was relatively higher than that previously reported for other caves (<5%; Ortiz et al., 2013;Ma et al., 2015;Wu et al., 2015;Gulecal-Pektas, 2016), suggesting the uniqueness of bacterial communities in our study. The dominance of Ascomycetes (40%) in the Heshang Cave was consistent with previous reports on fungal communities in many other caves (Ogórek et al., 2013;Vaughan et al., 2015). Some of the fungal top 15 fungal genera observed in our study were also common in other caves, such as Acremonium, Aspergillus, Cladosporium, and Penicillium (Popović et al., 2015;Zhang et al., 2017;Zhang and Cai, 2019). Parengyodontium (13.66%) was the most abundant genus, which was frequently observed in other caves (Leplat et al., 2017(Leplat et al., , 2019. Parengyodontium album had often been the most abundant detected species when salt efflorescence was present (Ponizovskaya et al., 2019;Trovão et al., 2019). The high abundance of Penicillium (3.42%) may be related to bat activity (Karkun et al., 2012). The species Penicillium janczewskii is characterized by habitation in dry substrates depleted in organic matter, which is partially consistent with its presence in the cave . Neodevriesia (2.37%) was reported as a dominant group on mural paintings in North Thai temples (Suphaphimol et al., 2022).
Alpha diversities and bacterial community compositions on the rocks did not show significant differences as indicated by Shannon and ACE indices and NMDS analysis in the sampling zones (the photic zone, twilight zone, and aphotic zone), suggesting a fundamental role of the rock substrate (carbonate especially), rather than sunlight in the shaping of bacterial communities. In contrast, the alpha diversity of fungal communities in the aphotic zone was significantly lower than that in the other two zones, which may be related to the isolation of the aphotic zone from light and plants. Fungal communities are known to be tightly associated with plant communities (Tedersoo et al., 2014;Purahong et al., 2018;Adamczyk et al., 2019), and almost 20% of total fungal species are symbiotic with lichens (Kirk et al., 2001;Honegger, 2009). Our results also found high fungal diversity at the entrance of the Heshang Cave, where lichens were observed on the rock surface. The decrease in fungal diversity inward to the cave may result from the impediment in the transfer of fungal spores due to the slow wind speed inside the cave (Supplementary Figure 3A). In fact, our observation of the significant positive correlations between the relative abundances of fungal classes such as Wallemiomycetes, Agaricomycetes, Tremellomycetes, Lecanoromycetes, Exobasidiomycetes, and the wind speed (Supplementary Figure 3C) also supported the decrease in the fungal diversity inward to the cave.
Despite small differences in bacterial communities, indicator groups were distinct in three light zones. The indicator groups in the photic zone were Cyanobacteria, Gemmatimonas, Nitrolancea, Brevundimonas, and Zavarzinella, which are closely related to light-dependent metabolism. Many cyanobacterial species can survive on soil and other terrestrial habitats and play important roles in the carbon and nitrogen cycles (Wegener et al., 2010;Forchhammer and Selim, 2020). Some species in Gemmatimonas such as Gemmatimonas aurantiaca can accumulate polyphosphate (Zhang et al., 2003), and other species like Gemmatimonas phototrophica are able to use light as an energy source (Zeng et al., 2015). Nitrolancea spp. are obligately aerobic, which are chemolithoautotrophic nitriteoxidizers (Sorokin et al., 2014). Flavisolibacter are aerobic chemoheterotrophs in the phylum Bacteroidetes (Lee J. J. et al., 2016). The main indicator groups in the twilight zone were Aquisphaera, Gimesia, and Streptomyces. Aquisphaera and Gimesia belong to the phylum Planctomycetes. Aquisphaera forms large visible cell aggregates during growth, which may affect the survival of other microorganisms (Bondoso et al., 2011). Isolates of Gimesia chilikensis are salt-and alkalitolerant (Kumar et al., 2020). Many Streptomyces species produce multiple antibiotics or other secondary metabolites, which act synergistically or contingently against biological competition (Challis and Hopwood, 2003). Conexibacter, Actinomadura, Aciditerrimonas, Planctopirus, and Chthonomonas were the indicator groups in the aphotic zone. They can survive in extreme environments, which is consistent with the lack of organic matter in the depths of the cave. Conexibacter, Actinomadura, and Aciditerrimonas all belong to class Actinobacteria and have been frequently isolated from extreme environments. For example, Conexibacter stalactiti was isolated from samples of stalactites collected from a lava cave (Lee, 2017), and Actinomadura namibiensis was isolated from desert sandy soil in Namibia (Wink et al., 2003). Chthonomonas calidirosea was thermophilic and isolated from geothermal soil (Lee K. C. et al., 2016;Compton et al., 2020). Microbes in the aphotic zone can also be involved in iron reduction. For example, Aciditerrimonas ferrireducens is capable of reducing ferric iron aerobically or anaerobically (Itoh et al., 2011;Hu et al., 2014).
The indicator groups of fungi also varied in the zones. In the photic zone, Lecanoromycetes, Hypocreales, Bionectriaceae, and Cladosporiaceae were identified as indicator groups. Lecanoromycetes is the largest class of lichenized fungi and includes most of the lichen-forming fungal species (> 13,500 species; Miadlikowska et al., 2006;Hofstetter et al., 2007). The majority of lichenized fungi in Lecanoromycetes are obligate mutualists, which can obtain organic nutrients from photosynthetic symbiotes and N compounds fixed by cyanobacteria (Gueidan et al., 2015;Jüriado et al., 2017). The Bionectriaceae is a family in the order Hypocreales, which tends to grow on plant materials (Khodosovtsev et al., 2012), and some species are related to algae (Khodosovtsev et al., 2012), bryophytes (Döbbeler et al., 2015), or other fungi. Cladosporiaceae is also associated with plants (Alghuthaymi, 2017) and is dominant in highly saline environments (Yang and Sun, 2020). The indicator groups in the twilight zone were Nectriaceae and Zasmidium. Numerous members in the family Nectriaceae (Hypocreales) are plant and human pathogens, and several species belonging to this family are used extensively in industrial and commercial applications for biodegradation and as biocontrol agents (Lombard et al., 2014(Lombard et al., , 2015. Zasmidium cellare has been reported in the Mammoth Cave, Kentucky (Barr, 1968), and is a strain known for living in dark and ethanol-rich environments (Cailhol et al., 2020). The indicator groups in the aphotic zone included Cutaneotrichosporon and Wardomycopsis inopinata. Cutaneotrichosporon oleaginosus is an oleaginous yeast with fast growth and also grows as filamentous fungus in the soil and leaf litter (Bracharz et al., 2017). Information on the function of Wardomycopsis inopinata in the environment is not available.

The Impact of Mineral Substrate on Microbial Communities and Ecological Processes in Community Assembly
RDA indicated that bacterial communities were significantly affected by hydroxyapatite, mainly due to phosphatesolubilizing bacteria Streptomyces and Pseudomonas. An isolate of Pseudomonas fluorescens from the Heshang Cave has been demonstrated to solubilize fluorapatite, making phosphate bioavailable for microorganisms . Fungal communities were positively impacted by fluorapatite, attributed to phosphorus-solubilizing soilborne fungi Aspergillus niger and Penicillium spp. (Reyes et al., 2007;Farhat et al., 2009;Li et al., 2016). The mechanism of phosphorus-solubilizing microorganisms is generally attributed to organic acid metabolites produced by bacteria and fungi (Kavanagh, 2005;Jones and Oburger, 2011). Phosphate is a common minor element in many silicate, sulfide, and carbonate minerals. Under phosphate-limited conditions in soil environments, microorganisms colonizing minerals may acquire bioavailable phosphate as it solubilizes from the mineral phase (Rogers and Bennett, 2004). Our observation of the significant impact of phosphate-bearing minerals on bacterial and fungal communities on the weathered rocks substantiates the development of microbial communities nutritionally dependent on the mineral-phase substrate.
Ecological processes responsible for the development of microbial communities were also investigated in the Heshang Cave. The assembly of bacterial communities is mainly a deterministic process, with the dominance of homogeneous selection across different sampling zones, indicating a spatial homogeneity in environmental conditions and the convergence in bacterial communities (Dini-Andreote et al., 2015). This conclusion is also consistent with the result of the NMDS (Figure 1E). In contrast, different ecological processes contributed to fungal assembly in sampling zones. Variable selection dominated the assembly of fungal communities in both the photic and twilight zones, indicating the strong environmental selection of fungal communities partially due to sunlight. Many fungal groups were associated with algae, cyanobacteria, and plant debris, all of which were highly dependent on sunlight. Homogeneous selection only dominated the fungal assembly in the aphotic zone, indicating that a homogeneous environmental condition resulted in the convergence in fungal communities. The occurrence of dispersal limitation in the aphotic zone indicates a weakening selection, which may have resulted from slow wind speed and high relative humidity toward the end of the cave entrance (Supplementary Tables 3,4). Slow airflow is known to decrease airborne transmission of fungal spores (Quintero et al., 2010), and fungal survival increases with relative humidity (Oliveira et al., 2005;Hameed et al., 2012). The relative abundances of fungal classes Wallemiomycetes, Agaricomycetes, Tremellomycetes, Lecanoromycetes, and Exobasidiomycetes showed significant positive correlations with the wind speed (Supplementary Figure 3C), and similar phenomena in air have also been reported (Begerow and Kemler, 2018;Els et al., 2019).

Interaction Between Bacteria and Fungi Living on Weathered Rocks
The co-occurrence network of bacteria and fungi showed good modularity and positive links between nodes, indicating that the bacterial and fungal communities formed a close organization through cooperation among different species. Their interactions increased the complexity of the community structure and the stability of the ecosystem (Chen et al., 2018).
In total, 53 keystone taxa were identified, which usually interact with many other groups, thus promoting the exchange and flow of energy, information, metabolites, and nutrients among different species and maintaining the balance of microbial communities (Berry and Widder, 2014;Ma et al., 2016). There are many unknown functions of the keystone taxa in this study, but some clues can be garnered from the previous investigations. The fungal keystone taxa mainly belonged to classes of Sordariomycetes, Dothideomycetes, and Eurotiomycetes. Members of Sordariomycetes are ubiquitous in natural environments (Zhang and Wang, 2015). They participate in the decomposition of organic matter and nutrient cycling as saprotrophs in almost all ecosystems, and they include endophytes and pathogens of plants (Arnold and Lutzoni, 2007), arthropods (Samuels and Blackwell, 2001), and mammals (O'Donnell et al., 2010), and even as mycoparasites attacking other fungi (Broberg et al., 2021). Sordariomycetes also contain species known to produce secondary metabolites such as potent mycotoxins (Zhang and Wang, 2015). Dothideomycetes is the largest class of Ascomycetes, which includes numerous rock-inhabiting fungi, adapted well to nutrient-poor and dry habitats on rock surfaces (Ruibal et al., 2009;Haridas et al., 2020). Eurotiomycetes can degrade a wide variety of organic substrates and can tolerate high salinity, complete darkness, and oligotrophic conditions (Greiner et al., 2014;Zhang and Wang, 2015), which favor their survival in caves.
Nocardioidaceae, Planctomycetaceae, and Rubrobacteraceae were keystone taxa of bacterial classes in the network. Nocardioidaceae uses a wide range of carbon and nitrogen sources, including unusual organic compounds and toxic environmental pollutants, and has versatile metabolic pathways . Like many other actinomycetes, Nocardioidaceae can survive under extreme conditions such as desiccation, low and high temperatures, UV damage, and toxic compounds (Kirby et al., 2006;Brodie et al., 2007;Griffin, 2007;Polymenakou et al., 2008). Members of the Nocardioidaceae are symbiotic with plants and may exist as reciprocal endophytes. They can also occur in association with lichens (Li et al., 2007) and fungi (Lauer et al., 2007). Marmoricola is a genus of Nocardioidaceae, which are found in different environments, such as marble, beach sediments, and agricultural soil (Lee, 2007;Freed et al., 2019). Some species are alkalitolerant or display alkaliphilic properties (Evtushenko, 2015). The family Planctomycetaceae is distributed in both soil and water (Wiegand et al., 2018) and shows strong tolerance to seawater, acid peat bog, hot springs, and low temperature (Kulichevskaya et al., 2007(Kulichevskaya et al., , 2008Fuerst and Sagulenko, 2011). It can use a special mechanism to absorb and digest complex polysaccharides, which may help it compete for nutrients in natural habitats (Boedeker et al., 2017;Schubert et al., 2020). The family Rubrobacteraceae is usually represented by its thermophilic and radiation-resistant types (Albuquerque et al., 2014). The genus Rubrobacter of Rubrobacteraceae is involved in chlorophyll biosynthesis (Gupta and Khadka, 2016). These keystone bacteria and fungi impact microbial community composition and symbiotic or parasitic relationships on rock walls. Some of their secondary metabolites have antibiotic or toxin properties that can promote or inhibit effector species and modulate interactions in microbial communities.
The co-occurrence network analysis provides us with a new way to find potential symbiotic or parasitic associations between bacteria and fungi. Bacteria can be endosymbiotic with fungi (termed endohyphal bacteria), which are phylogenetically and ecologically widespread. Endohyphal bacteria recently have been documented in diverse Ascomycota, including members of multiple classes (Pezizomycetes, Eurotiomycetes, Dothideomycetes, and Sordariomycetes; Hoffman and Arnold, 2010;Shaffer et al., 2016Shaffer et al., , 2017. Our network analysis found that many unannotated groups within Eurotiomycetes, Dothideomycetes, and Sordariomycetes serve as keystone taxa in the network, which are also tightly connected with bacteria. For example, Betaproteobacteria has a connection with unidentified fungi, and related studies have demonstrated that some genera of Betaproteobacteria can parasitize as endosymbionts in fungal hyphae (Hoffman and Arnold, 2010). Xanthomonadaceae has been found to subsist in fungal hyphae (Hoffman and Arnold, 2010), as also notices for unidentified fungi in our network. The observation of the connection between Caldiline and unidentified fungi in our study is consistent with a previous report of a negative correlation between Caldiline and an unclassified fungus of Pezizomycotina (Fouts et al., 2012). Gammaproteobacteria in the network are linked to many OTUs in Dothideomycetes, Sordariomycetes, and unidentified fungi. Arendt et al. (2016) demonstrated that some species of Gammaproteobacteria can be successfully introduced into Dothideomycetes and Sordariomycetes, thus substantiating their symbiotic relationships.
It should be emphasized that co-occurrence networks visualize the correlations between microbial groups, including real ecological interactions (such as reciprocity), and also include non-random processes (such as niche overlap). They do not, therefore, necessarily reflect direct interactions between the groups. Future experiments will assess whether the identified key species directly affect other members of the microbiome or indirectly affect the performance and fitness of the host, thus affecting other community members.

CONCLUSION
We studied the ecological processes responsible for the community assembly, endeavoring to provide new insights into microbial interactions and establishment of microbial communities under extreme conditions in the subsurface cave biosphere.
1. Microbial indicator groups varied with different light zones, indicating functional changes in response to the light variation in karst caves. Phosphate minerals such as hydroxyapatite and fluorapatite significantly influenced bacterial and fungal communities living on weathered rock surfaces. 2. The co-occurrence network analysis showed that bacteria and fungi on rock surfaces were mainly positively linked, indicating extensive, close cooperations among microbial groups across different domains connected under stark environmental conditions to maintain the microbial ecosystem. The co-occurrence network may also provide us with a new robust way to decipher symbiosis and parasitism between bacterial and fungal groups. 3. Homogeneous selection dominated bacterial community assembly throughout the cave, resulting in the convergence of bacterial communities. Variable selection contributed most to the fungal community assembly in the photic and twilight zones, whereas homogeneous selection with dispersal limitation contributed more to fungal assembly in the dark zone.

DATA AVAILABILITY STATEMENT
The datasets presented in this study can be found in online repositories. The names of the repository/repositories and accession number(s) can be found below: https://www.ncbi.nlm.n ih.gov/bioproject/337918, http://www.ncbi.nlm.nih.gov/bioproje ct/821722.

AUTHOR CONTRIBUTIONS
YW, JZ, and XL completed the sample collection. JZ finished DNA extraction. YW and XC completed data analysis, visualization, and original draft preparation. HW designed this experiment, supervised data analysis, acquired funding, and wrote and edited this manuscript. OT participated in data discussion and manuscript drafting. All authors contributed to the article and approved the submitted version.

FUNDING
This work was supported by the National Natural Science Foundation of China (91951208 and 41130207).