Abstract
Although stone surfaces seem unlikely to be habitable, they support microbial life. Life on these surfaces are subjected to many varying harsh conditions and require the inhabitants to exhibit resistance to environmental factors including UV irradiation, toxic metal exposure, and fluctuating temperatures and humidity. Here we report the effect of hosting stone geochemistry on the microbiome of stone ruins found in Tamil Nadu, India. The microbial communities found on the two lithologies, granite and granodiorite, hosted distinct populations of bacteria. Geochemical composition analysis of sampled stones revealed quartz mineral content as a major driver of microbial community structure, particularly promoting community richness and proportions of Cyanobacteria and Deinococcus-Thermus. Other geochemical parameters including ilmenite, albite, anorthite, and orthoclase components or elemental concentrations (Ti, Fe, Mn, Na, and K) also influenced community structure to a lesser degree than quartz. Core members of the stone microbiome community found on both lithologies were also identified and included Cyanobacteria (Chroococcidiopsaceae and Dapisostemonum CCIBt 3536), Rubrobacter, and Deinococcus. A cluster of taxa including Sphingomonas, Geodermatophilus, and Truepera were mostly found in the granodiorite samples. Community diversity correlated with quartz mineral content in these samples may indicate that the microbial communities that attach to quartz surfaces may be transient and regularly changing. This work has expanded our understanding of built-stone microbial community structure based on lithology and geochemistry.
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Data availability
All sequence data (16S rRNA gene datasets) presented in this article is available in the repository of NCBI under Bioproject number PRJNA545121.
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Acknowledgments
Sequencing was performed on an Illumina HiSeq2500 purchased with an NSF MRI Grant: DBI-1229361 to WK Thomas. We thank Florencia Fahnestock for assistance in preparing the samples for geochemical study and Michael Rhodes at the University of Massachusetts for assistance acquiring the X-ray fluorescence data.
Funding
This study was funded in part by an award from the University of New Hampshire CoRE program (JB, LST), the University of New Hampshire Summer Teaching Assistant Fellowship (NJE), the University Grants Commission Raman Postdoctoral Fellowship of India (DD), and the College of Life Science and Agriculture at the University of New Hampshire-Durham.
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NJE, DD, and LST conceived the original idea for the study; NJE, DD, and LST jointly designed the approach and experimental plan; NJE and DD performed the sampling and DNA isolation; NJE prepared the sequenced libraries and analyzed the sequence data; NJE and JB designed the geochemical studies, prepared the samples for analyses, and interpreted and modeled the resulting data; and LST, NJE, JB, and DD wrote the manuscript. All authors read and approved the final manuscript.
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Figure S1
Photographs of the stones from the sampling locations in Tamil Nadu, India DF- Fort Dindigul; PS- Valikandapuram Sivan Temple, Perambalur; PR- Fort Ranjankudi temple foundation , Perambalur; PRA- Fort Ranjankudi temple wall, Perambalur; TB- Thanjavur Big Temple; TM- Fort Thirumayam, TMA- Fort Thirumayam temple; TF- Fort Tiruchirappalli temple foundation; , TFA- Fort Tiruchirappalli temple wall; PV- Sittanavasal Cave interior; PVA- Sittanavasal Cave exterior. (PDF 306 kb)
Figure S2
Alpha Diversity of Indian Samples Grouped by Stone Type. The Shannon Diversity Index was used to measure alpha diversity of each sample stone type. The diversity of all stone type groupings was not considered significantly different from each other according to the Student’s T test (p > 0.05). (PDF 129 kb)
Figure S3
Major Actinobacteria and Cyanobacteria families in Indian stone microbial communities. Average 16S amplicon data documents the relative abundance of each Actinobacteria (A) and Cyanobacteria (B) family after rarefying. Most Actinobacteria families were present at low abundance in both lithologies, except for Rubrobacteriaceae, which was most prominent in granodiorite. The Cyanobacteria families were generally more prominent in granodiorite, but Nostocaceae was present at low abundance in both lithologies. (PDF 120 kb)
Figure S4
Unweighted Pair Group Method with Arithmetic Mean (UPGMA) Consensus Tree of Indian Stone Microbial Communities. The UPGMA consensus tree was built using the unweighted UniFrac distance matrix of the rarefied feature table. This was done by creating 100 trees from 100 randomly subsampled sequences from each sample. Node labels represent the percentage of the 100 trees that conform to this final consensus configuration. Samples do not clearly cluster by lithology and are color-labeled as granite (red) or granodiorite (blue). (PDF 107 kb)
Table S1
Sampling Climate Data. (PDF 13 kb)
Table S2
Indian Stone Geochemical Analysis. (PDF 17 kb)
Table S3
Summary of Sequencing Data (PDF 8 kb)
Table S4
PCoA Axes Correlations with Environmental Variables. Correlations between PCoA axes and quantitative environmental variables are represented by Pearson’s correlation coefficient (r, r2) and Kendall’s rank correlation (Tau). (PDF 123 kb)
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Ennis, N.J., Dharumaduri, D., Bryce, J.G. et al. Metagenome Across a Geochemical Gradient of Indian Stone Ruins Found at Historic Sites in Tamil Nadu, India. Microb Ecol 81, 385–395 (2021). https://doi.org/10.1007/s00248-020-01598-3
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DOI: https://doi.org/10.1007/s00248-020-01598-3