Abstract:Although a broad diversity of eukaryotic and bacterial taxa reside on rock surfaces where they can influence the weathering of rocks and minerals, these communities and their contributions to mineral weathering remain poorly resolved. To build a more comprehensive understanding of the diversity, ecology and potential functional attributes of microbial communities living on rock, we sampled 149 tombstones across three continents and analysed their bacterial and eukaryotic communities via marker gene and shotgun… Show more
“…Similarly, the observed dominance of Gemmatimonadetes in the edaphic niche, supported by previous findings by Niederberger et al (2008) and Babalola et al (2009), may be linked to their important role in soil biogeochemical processes through phosphorous metabolism (Zhang et al, 2003), hence assisting early ecosystem development in this deglaciated area (Knelman et al, 2014), as confirmed by the observed increases in soil phosphate availability with time. In contrast, the phylum Deinococcus-Thermus and the Sphingomonadales (Alphaproteobacteria) were significantly more abundant on rocks, where they may benefit from using sugar alcohols and organic acids released by lichenized fungi, molds and algae (Siebert and Hirsch, 1988;Brewer and Fierer, 2018).…”
Glacier forefields provide a unique chronosequence to assess microbial or plant colonization and ecological succession on previously uncolonized substrates. Patterns of microbial succession in soils of alpine and subpolar glacier forefields are well documented but those affecting high polar systems, including moraine rocks, remain largely unexplored. In this study, we examine succession patterns in pioneering bacterial, fungal and algal communities developing on moraine rocks and soil at the Hurd Glacier forefield (Livingston Island, Antarctica). Over time, changes were produced in the microbial community structure of rocks and soils (ice-free for different lengths of time), which differed between both substrates across the entire chronosequence, especially for bacteria and fungi. In addition, fungal and bacterial communities showed more compositional consistency in soils than rocks, suggesting community assembly in each niche could be controlled by processes operating at different temporal and spatial scales. Microscopy revealed a patchy distribution of epilithic and endolithic lithobionts, and increasing endolithic colonization and microbial community complexity along the chronosequence. We conclude that, within relatively short time intervals, primary succession processes at polar latitudes involve significant and distinct changes in edaphic and lithic microbial communities associated with soil development and cryptogamic colonization.
“…Similarly, the observed dominance of Gemmatimonadetes in the edaphic niche, supported by previous findings by Niederberger et al (2008) and Babalola et al (2009), may be linked to their important role in soil biogeochemical processes through phosphorous metabolism (Zhang et al, 2003), hence assisting early ecosystem development in this deglaciated area (Knelman et al, 2014), as confirmed by the observed increases in soil phosphate availability with time. In contrast, the phylum Deinococcus-Thermus and the Sphingomonadales (Alphaproteobacteria) were significantly more abundant on rocks, where they may benefit from using sugar alcohols and organic acids released by lichenized fungi, molds and algae (Siebert and Hirsch, 1988;Brewer and Fierer, 2018).…”
Glacier forefields provide a unique chronosequence to assess microbial or plant colonization and ecological succession on previously uncolonized substrates. Patterns of microbial succession in soils of alpine and subpolar glacier forefields are well documented but those affecting high polar systems, including moraine rocks, remain largely unexplored. In this study, we examine succession patterns in pioneering bacterial, fungal and algal communities developing on moraine rocks and soil at the Hurd Glacier forefield (Livingston Island, Antarctica). Over time, changes were produced in the microbial community structure of rocks and soils (ice-free for different lengths of time), which differed between both substrates across the entire chronosequence, especially for bacteria and fungi. In addition, fungal and bacterial communities showed more compositional consistency in soils than rocks, suggesting community assembly in each niche could be controlled by processes operating at different temporal and spatial scales. Microscopy revealed a patchy distribution of epilithic and endolithic lithobionts, and increasing endolithic colonization and microbial community complexity along the chronosequence. We conclude that, within relatively short time intervals, primary succession processes at polar latitudes involve significant and distinct changes in edaphic and lithic microbial communities associated with soil development and cryptogamic colonization.
“…We used both high‐throughput amplicon (targeting the 16S rRNA gene) and whole metagenome shotgun sequencing on stone ruins from three distinct climates in Tunisia and Algeria to achieve our objectives. Although climate has been shown to have an impact on stone microbes of the Mediterranean basin (Macedo et al ., ), most previous research on the microbiome of stone structures of Europe, North America, and South America has instead focused on stone geochemistry as drivers of diversity and functional variation (Cockell et al ., ; Krakova et al ., ; Chimienti et al ., ; Brewer and Fierer, ; Gaylarde et al ., ,b). In this study, we aimed to determine what aspects of the climate, including precipitation, temperature and others, were associated with specific microbial community variation, particularly in representation of Actinobacteria and Cyanobacteria colonizers.…”
Summary
Stone surfaces are extreme environments that support microbial life. This microbial growth occurs despite unfavourable conditions associated with stone including limited sources of nutrients and water, high pH and exposure to extreme variations in temperature, humidity and irradiation. These stone‐dwelling microbes are often resistant to extreme environments including exposure to desiccation, heavy metals, UV and Gamma irradiation. Here, we report on the effects of climate and stone geochemistry on microbiomes of Roman stone ruins in North Africa. Stone microbiomes were dominated by Actinobacteria, Cyanobacteria and Proteobacteria but were heavily impacted by climate variables that influenced water availability. Stone geochemistry also influenced community diversity, particularly through biologically available P, Mn and Zn. Functions associated with photosynthesis and UV protection were enriched in the metagenomes, indicating the significance of these functions for community survival on stones. Core members of the stone microbial communities were also identified and included Geodermatophilaceae, Rubrobacter, Sphingomonas and others. Our research has helped to expand the understanding of stone microbial community structure and functional capacity within the context of varying climates, geochemical properties and stone conditions.
“…Li et al [41] considered Sphingomonas a major player in the deterioration of monuments because of its high relative abundance and frequency on heritage stone [42]. However, this genus has been also retrieved in dust samples which may explain its global presence on stone substrata [43,44]. Indeed, Sphingomonas and Quadrisphaera, a recently identified actinobacterium [45], were isolated from Antarctic samples [46].…”
Despite the massive presence of biofilms causing aesthetic alteration to the façade of the Monza Cathedral, our team in a previous work proved that the biocolonization was not a primary damaging factor if compared to chemical-physical deterioration due to the impact of air pollution. Nonetheless, the conservators tried to remove the sessile dwelling microorganisms to reduce discolouration. In this research, two nearby sculpted leaves made of Candoglia marble were selected to study the effects of a chemical treatment combining the biocides benzalkonium chloride, hydrogen peroxide and Algophase® and mechanical cleaning procedures. One leaf was cleaned with the biocides and mechanically, and the other was left untreated as control. The impact of the treatment was investigated after 1 month from the cleaning by digital microscopy, environmental scanning electron microscopy, confocal microscopy and molecular methods to determine the composition and the functional profiles of the bacterial communities. Despite the acceptable aesthetic results obtained, the overall cleaning treatment was only partially effective in removing the biofilm from the colonized surfaces and, therefore, not adequately suitable for the specific substrate. Furthermore, the cleaning process selected microorganisms potentially more resistant to biocides so that the efficacy of future re-treatment by antimicrobial agents could be negatively affected.
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