Abstract
Since ancient time, magnificence and beauty have been the goals of architecture. Artists and architects used high strength, durable and beautiful stones like marble and limestone for the construction of monuments like Taj Mahal, Milan Cathedral, Roman Catacombs and Necropolis in Rome etc. These historic monuments are exposed to open air which allows the invading army of algae, cyanobacteria, fungi etc. to easily access them. The invasion of microorganisms and their subsequent interaction with mineral matrix of the stone substrate under varied environment conditions fosters deterioration of stones by multiple mechanisms resulting in loss of strength, durability, and aesthetic appearance. The review details about the major routes and mechanisms which led to biodeterioration, discusses current remedial methodologies and suggests future directions.
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Review
Introduction
Biodeterioration can be defined as a geophysical and geochemical process that causes undesirable physical, chemical, mechanical and aesthetic alterations and damages to historic monuments and artworks. It is a complex process that illustrates the interaction of micro-organisms with its substratum and environment[1–3]. These stone structures are highly susceptible to damage by weathering and atmospheric conditions (such as light, temperature, humidity, pollutants and acid rain)[1, 4–6] because of their chemical nature and petrologic properties (texture, high porosity etc). The high porosity allows penetration of water along with corrosive ions, acids and salts inside the porosity of the stone and cause severe damage to them. Besides this, stone surface supports the growth of some characteristic group of microorganisms which includes alkaliphiles, halophiles, epiliths and endoliths[7–10] which cause deterioration in many ways (Table1). These micro-organisms through different known mechanisms of deterioration cause harm to the stone surfaces of monuments and artworks resulting in an irreversible and irreparable loss of their physical strength, aesthetic appearance, value and information[1, 6, 10–16] (Table2).
Impact of environment conditions and pollutants on rate of biodeterioration
Since the time, industrial revolution began the deterioration and weathering of heritage monuments and artworks became noticeable. Environmental conditions like relative humidity, temperature, wind, light and rainfall plays a crucial role in colonization and establishment of microbial communities on the stone surfaces of monuments and artworks[1, 4, 5]. The problem is more pronounced in tropical areas where the high temperature, high relative humidity and high annual rainfall favor the growth of diverse group of microorganisms. Microbial growth and activity is a function of the environment that surrounds them. For instance, seepage of the rain water and subsequent dampening and moistening of the vertical walls of the monuments favor the colonization of diverse groups of organisms such as cyanobacteria, algae, fungi and lichens, which foster deterioration. Similarly, oxides of nitrogen and suspended particles are affecting the lichen diversity in some cities of Italy[68]. Increasing industrial activities and pollution had also modified the composition of atmosphere and consequently favored the invasion of some aggressive species of lichens such as Dirina massiliensis forma sorediata, Lecanora muralis and Xanthoria parietina whose presence became apparent in past two decades in various monuments of Italy, Spain and Portugal[52, 53]. The mineral matrix of the stone serves as a suitable substratum for the growth of microorganisms. The mineral composition, nature of stone substrate and surrounding environmental conditions are the major determinants of the type and extent of microbial colonization. Nevertheless, the atmosphere contains abundant of pollutants of different origin (industrial and automobiles) which have also immense biodeterioration potential. Persistent air pollutants of urban environment like oxides of sulfur, nitrogen and other carbonaceous particles, fly ash, particulate matters upon settling on the surface of the monumental stones destroy their aesthetic and artistic beauty[4–6]. Oxides of nitrogen and sulfur combine with the rain water making it acidic and showers as acid rain on the monuments. These oxides may be oxidized into their corresponding acids by the humid air or moisture present on the damp stone surfaces of monuments further worsening their physical strength and durability. Crystallization of soluble salts like sulfates and black crust formation is also considered as one of the major causes of damage to the surfaces of monumental stones and artworks[23, 69, 70].
Monumental stones and their bioreceptivity
During historic time, people used different stones (limestones, granites, marbles etc) for the construction of magnificent monuments and for making beautiful artworks. These historic building and artworks are our heritage which tells us about the past art, architecture and enriches us with cultural values. Stones used in making these sculptural monuments were highly consolidated and durable and were obtained from naturally occurring sedimentary rocks which are composed of one or more minerals. These monuments and artworks exposed to polluted air and corrosive acid rain water and are now at risk of degradation and deterioration. Varieties of microbes are getting an open access and are now enjoying their royal stay in historic monuments, viewing intricately designed painting and artwork for which visitors need to pay. Microbial presence on monumental stones and artworks does not imply that the biodeterioration is associated with their growth. Microbial ability to colonize stone surface depends up on numerous factors like mineral composition, nutrient availability, pH, salinity, surface texture, moisture content, porosity, permeability, climatic and micro-environmental conditions[23]. The mineralogical nature of stone together with its surface properties and environmental conditions synergistically controls the bioreceptivity of a stone (an ability of stone to be colonized by microorganisms) while the intensity of colonization is influenced by the surrounding environment conditions (including pollutants concentration and micro-climatic conditions) and by anthropogenic eutrophication of the atmosphere[71, 72].
Major routes to biodeterioration
Microbes play a geoactive role in the biosphere. They can initiate, support and accelerates some geochemical and geophysical reactions which lead to biodeterioration of historic monuments[1]. The biodeterioration of historic monuments and stone works occurs as a consequence of biofilm production, secretion and deposition of organic and inorganic compounds (salt encrustation and efflorescence), physical intrusion/penetration of microbes and redox processes on cations from the mineral lattice ([23, 73] ). The growth and activity of the microorganisms on monuments or stone surface results in five major alterations: bioweathering (stone dissolution), staining or color alteration, surface alterations (pitting, etching, stratification etc), biocorrosion and transformation of crystal into small size one[25].
Bioweathering or stone dissolution
Weathering is a process induced by microbial communities secreting corrosive organic and inorganic acids, metal binding ligands, resulting in progressive weathering or dissolution of superficial mineral surface of rock. Microbial-mineral interaction serves as a good ground for studying the role of microbes in the process of geochemical transformation of monumental stones and artworks. This interaction represents different methods which microbes utilize for the extraction of nutrients from the mineral surface[23, 27, 69, 74, 75]. The dissolution of stone provides essential trace-metals, phosphate, sulfate and metabolites to the inhabiting microbial communities which are crucial for the growth and development of inhabiting microbial consortia[76]. Fungi perform stone dissolution in two ways: by forming secondary minerals and metabolism independent binding of metals on their cell wall or other external surfaces[51, 77]. The release of highly corrosive inorganic acids, organic acids and chelating agents by fungi and lichens on stone surface of monuments are among those methods which are inadvertently involved in the promotion of bioweathering process[23]. Biofilm formation though conspicuous on monumental stones and artworks but very little is documented in literature regarding their role in extraction of minerals from the stone substrates[23, 30, 69].
Biocorrosion: release of corrosive inorganic and organic acids
Biogenic secretion or release of inorganic and organic acids by a great number of microorganisms is considered as the probable cause of biocorrosion of monumental stone surfaces. The destruction processes induced by the released inorganic and organic acids are respectively known as acidolysis and complexolysis[70]. The process of acidolysis is associated with the chemolithotrophic bacteria like nitric and sulfuric acid producing bacteria. Apart from this, the release of carbon dioxide produced during cellular respiration by lichens and mosses is also a potent corrosive agent[24, 78]. The formation of organic acids like oxalic acids, citric acids etc by certain chemoorganotrophs and lichens have strong corrosive property.
Stone encrustation: deposition of corrosive organic and inorganic compounds
Increasing industrialization and combustion of the fossil fuel has increased the concentration of SO2 and NO2 in the atmosphere. Both NO2 and SO2 have bioweathering effect[36, 38]. SO2 together with other dark particles (particulate matters) settles down and get deposited on the stone surfaces rendering darkened and yellowish color to them[6, 36]. There is a special class of bacteria, called sulfur-oxidizing bacteria and nitrifying bacteria (chemoautotrophs) which can colonize marble surface and oxidize the nitrogen compounds including atmospheric ammonia (Nitrosomonas sp. and Nitrobacter sp.) and sulfur compounds (Thiobacillus sp.) into nitric and sulfuric acid respectively[38]. These acids are highly corrosive and accelerate the dissolution of the stone surface (biocorrosion) and changes. This acids react with the stone carbonates and results in the formation of nitrate and sulfate salts. The sulfation is stone carbonates is known to be prompted by the presence of humidity and fossil fuel derived particulate matters[37, 40]. Upon coming in contact with rain water these sulfates get dissolved forming hydrated salts like gypsum[35]. The formation of gypsum is often accompanied by the entrapment of carbonaceous particles (fly ash), diesel particulate matters and dust, leading to the formation of black and brown sulfated crust over the stone[37, 39]. The affects of encrustation of marble stones with sulfates is not limited to the aesthetic problems, these sulfates can precipitates inside the pores of the stones and upon recrystallization exerts considerable stress inside the pore walls resulting in structural damage to the marble stones. The chemical composition of these sulfated crusts varies and is dependent on the age of the crusts and particular airborne pollutants in individual areas[79]. Quite often sulfur-oxidizing bacteria are also benefited by the presence of sulfur-reducing bacteria at the base of the stone. These bacteria reduce the sulfates to sulfides, which is an excellent source of energy for the sulfur-oxidizing bacteria. The presence of extremely and moderate halophiles on the monumental stone and stone works of art is also reported. Halophiles are abundantly found on the surface of the stones and art works which are laden with the deposits of hygroscopic salts. These depositions are formed as a result of drying of salt containing water on the exposed surfaces of the stone by a process commonly known as efflorescences.
Secondary mineral formation: calcium oxalate or patina formation
Calcium oxalate formation on sculptural monuments and artworks is prominent feature of several lichens and fungal species which stains the stone surfaces with various colored patina[29]. Calcium oxalates (whewellite-CaC2O4.H2O and weddellite-CaC2O4.2H2O) widely occur in nature mainly as patina on the stones of historic monuments and artifacts. Calcium oxalates are formed as a result of precipitation of calcium carbonate by oxalic acid which is produced as a metabolic byproduct by lichens and fungi. Raman spectra analysis showed the presence of calcium oxalate monohydrate (by Lecanora sulfurea and Aspicilia calcarea) and dihydrate (Dirina massiliensis f. sorediata, D. massiliensis f. massiliensis and Tephromela atra) in the biomineral product of lichen bioweathering[80]. Earlier the precipitation of calcium in the form of oxalate was assumed to be less common in other organism like algae and fungi. During recent year several experimental demonstration were presented regarding their biogenesis[54]. The evidence of fungal biogenesis of calcium oxalate formation was also reported in literature[54]. Additionally, the origin of patina is partially attributed to past stonemasonry treatments and to atmospheric pollution[29].
Biofilm formation
Algae, microalgae and cyanobacteria are considered as the pioneering inhabitants of a stone surface hence their presence can be easily identifiable on the stones surface[2, 3, 48]. Cyanobacteria are often present in association with red algae, green algae and lichens[48]. These are the one on the major threats to the monumental and ornamental stone works of art. Due to their phototrophic nature, they easily grow on the stone forming colored patinas and incrustations[22]. Their association with substrate in the presence of water makes their growth predominates over other organisms and accelerates the formation of biofilms which facilitates attachment and serves as a mechanism for resisting adverse abiotic conditions[17, 81]. Biofilm act as precursor for the physical damage to the stone leading to its biodeterioration[21, 48] and discoloration[20]. It is believed that under certain conditions almost all substrate both natural and man-made can be colonized by microorganisms enclosed within a three dimensional extracellular polysaccharides matrices called biofilm[23, 73]. Biofilm composition and distribution mainly depend up on the resulting spatial and temporal variation in a number of abiotic and physico-chemical factors, including micro-environment. Biofilm production on outdoor monuments that are continuously exposed to light tends to contain pleothora of phototrophic microorganisms[21]. Biofilm formation by cyanobacteria represents a mechanism to resist changes in environment like extremes of temperature, drought and prolonged exposure to light[82, 83]. Other survival strategies which include use of water stored within substrate[84], formation of compounds conferring resistance to drought[85] and synthesis of protective UV shield[84, 86] are also known. Cyanobacteria have capability of extraction and mobilization of ions like calcium and potassium present on artworks for their own nutrition[81]. The biofilm is composed of cells and extracellular polymeric substance that facilitates the attachment of the biofilm on the solid substratum. Further, the biofilms enhanced N and P availabilities when inoculated in the soil[87]. The biofilm formation makes the stone lose its property of cohesion. Some genera of the microalgae such as Cosmarium, Phormidium and Symploca are the major destructors of ornamental stones collected from the fountain of Bibatauin at Granada in Spain[31]. The constant presence of water also favors the growth of some endolithic green algae and cyanobacteria which forms black crust on the Robba’s fountain statues, Ljubljana (Slovenia). The stratification of biofilm is controlled by a number of factors, including the quality of light. Low light conditions tend to reduce the stratification and affect species diversity and permit only certain species to survive[88]. Biofilms can be both detrimental and beneficial, depending on the substratum and microorganisms involved. While biofilms and the inhabiting organisms accelerate the deterioration process[89], some communities have a more protective role[90]. In later case, the removal of biofilm layer may fasten the deterioration of stones by making them susceptible to atmospheric pollutants and to the attacks of salts[91, 92].
Redox processes on cations from the mineral lattice
Some protein compounds called “Siderophores” are involved in the process of cation transfer from mineral matrix of the stone to microbial cells. Besides this, active ion uptake followed by accumulation of cation on microbial cell wall is another mechanism for this process. The leached cations are immobilized by the degradation of metal organic transport complexes and metal organic chelates. Subsequently the redox process is favored upon liberation of oxygen by cohabitant photosynthetic cyanobacterial and algae[23]. Several chemoorganotrophic bacteria and fungi (Acidithiobacillus ferrooxidans, Bacillus spp., Leptospirillum spp., Aureobasidium spp.) are facilitate the removal of cations, in particular, iron and manganese cations from the mineral lattice by oxidation and consequently contributing to deterioration of stone[23].
Physical penetration of microbes
Physical intrusion and penetration of bacterial and fungal hyphae inside the gaps, pores, cracks and boundaries of the stones has also posed a big threat to biophysical and biomechanical damage to monuments and artworks[25, 27, 48, 74]. The physical intrusion by hyphae along the crystal plane destabilizes the stone texture and increases the porosity which causes biomechanical deterioration of stones and artworks[25, 27, 48, 74]. Besides bacteria and fungi, some photosynthetic microorganisms such as mosses are known to possess rhizoids which physically intrude inside the stone but biomechanical damage caused as a result of their rhizoids intrusion is less documented in literature[48].
Microorganisms involved in biodeterioration
Bacteria
Bacteria involved in deterioration of monuments and artworks mainly belong to three nutritional groups: Photoautotrophs, Chemolithoautotrophs and Chemoorganotrophs. Among phototrophs and chemolithoautotrophs are mainly cyanobacteria, sulfur-oxidizing and nitrifying bacteria were reported from the heritage sites. Due to their simpler nutritional (like inorganic minerals, atmospheric ammonia etc.) and ecological needs (like presence of light, CO2 and water) these bacteria easily develop on outdoor monuments. Among these organisms, cyanobacteria have the ability to survive under the conditions of repeated drying and rehydration occurring on exposed monument’s surfaces[48] and to protect themselves by the harmful UV radiation by producing protective pigments[48]. However, their presence was also conspicuous in interior works of art[20, 93, 94] (hypogean environments of Roman Catacombs) which were subjected to inappropriate natural or artificial illumination during visitor’s hours[81, 95]. The colonization of these photosynthetic microorganisms on external surface of monuments is related to biofilm formation, corrosive inorganic and organic acid secretion resulting in mechanical deterioration (due to alternate shrinking and swelling cycles of biofilm) undesirable unaesthetic staining of the monuments (by secreted acids, pigments and metabolic bioproducts), enlargment of pore (due to hyphal penetration), alteration in pore size, distribution and water permeability of the minerals (by deposition of surfactants) and weathering (as a consequences of uptake of calcium, precipitation of calcium salt and secondary mineral formation)[18, 19]. Chemoorganotrophs and chemoheterotrophs bacteria found associated with deterioration process are mainly sulfur-reducing bacteria and actinomycetes respectively. Population of these heterotrophic bacteria and actinomycetes prevail in hypogean environment characterized by stable microclimatic conditions (high relative humidity <90%, constant temperature throughout year and low photon influx)[42, 96]. These bacteria are mainly responsible for the irreversible damage to the indoor artworks (wall painting, frescos, stuccoes etc) and are less involved in the deterioration of outdoor monuments. Some species belonging to order Actinomycetales like Geodermatophilaceae strains[97] and also some Micromonospor a strains[98] were also isolated from monumental stones. Actinomycetes species mainly, Streptomyces (S. julianum) may form intimate association with cyanobacterial partner as found in the hypogean environment of Roman Catacombs. Actinomycetes preferred to grow where there exist the growth of algae and chemosynthetic nitrogen fixer bacteria. Invasion and damage to the Caves of Lascaux by fungi Fusarium and associated bacterium Pseudomonas Fluorescens was mainly ascribed to the perturbations induced by illumination and visitor’s breath[57, 99].
Two archaebacteria were detected and isolated from two ancient wall painting namely Catherine Chapel of the Castle Herberstein (Styria) from Austria and Roman Necropolis of Carmona from Spain. These archaeal communities were subjected to 16s rRNA sequencing and denaturing gradient gel electrophoresis and are characterized and found related to Halococcus (halophilic) and Halobacterium (alkaliphilic)[9].
Fungi
Fungi are ubiquitously present microorganisms representing the group of chemoheterotrophs characterized by the presence of unicellular or multicellular hyphae[58]. Fungi are metabolically more versatile than other biodeteriogens in the microbial kingdom. This versatility allows them to colonize on wide variety of substrates including wood, stones, and metals and enhances their biodeterioration potential. Their ability to grow on variety of substrate, endure extremes of environmental conditions, establishing mutualistic association with cyanobacteria and algae as lichens[51] and adopting various structural, morphological and metabolic strategies further enhances their versatility and adaptability[46, 100]. The biodeterioration of inorganic substrate (like carbonate) by fungi entirely follow a different mechanism. Being heterotrophic, fungi are unable to consume the inorganic carbonate substrate to supports its growth, but can grow on the waste product or dead cells of previous communities and deposits of organic nitrogenous matters of birds excretes, decayed leaves and aerosols[51] present on rock surface, fissures, cracks, subaerial and subsoil environment. Their capability to grow as oligotrophs and scavenge nutrient material from atmospheric and rain water permits their growth on inhospitable environments of rocks[100]. The presence of fungi on the stone surface of the heritage monuments and stoneworks is often associated with the process of biodeterioration. Fungi are known to harm the monumental stones and artworks in numerous ways. Their growth on stone surface can alter it severely by the excreting inorganic and organic acids as a result of their own metabolism. These metabolically generated organic acids (like oxalic acid and citric acid) have chelating properties by which it weaken the metal-oxygen bond, increases the solubility of some metals and forms complexes with the mineral cations present on the surface matrix[45, 49, 60, 61]. Intrusion of fungal hyphae along the crystal plane by some fungi is known to destabilize the stone texture resulting in its mechanical deterioration ([100]; Gadd 2005). Another mean of mechanical damage results from the alternate contraction and expansion of the thallus under fluctuating environmental humidity conditions. Some endolithic fungi by biochemical mean cause "pitting", of the stone surface that appears to have many small holes. This alteration has been found on historic monuments such as the gate of the Cathedral of Huesca in Spain. Species of fungi of different genera such as Cladosporium herbarum, Aspergillus niger, Stachybotrys sp. and Alternaria have been found on these supports. Scanning electron microscopy also revealed the presence of ‘etch marks’ beneath the microorganism which is a form of biochemical weathering[24, 101]. Fungi can transform and weather the mineral surface of the stone by precipitating calcium carbonate into calcium oxalate by the actions of secreted oxalic acid using the process of secondary mineral formation (or neogenesis)[44, 47]. Formation of oxalate film on carrara marble from Pisa Tower is also attributed to the growth of fungal species Sporotrichum[50].
Fungal diagenesis
It is a complex process of biochemical[46] and biomechanical alterations[47, 51] of carbonate substrates induced by fungus resulting in the formation of different secondary minerals. Carbonate stones mainly consisted of limestone or dolomite serves as an unusual niche for the fungal communities. These substrates are highly susceptible to fungi and their interaction promotes extensive microbial diagenesis of these substrates. Extensive diagenesis results in the dissolution (or bioweathering) of the carbonate substrate due to exuded organic acids (oxalic, citric and malic acid) and transformation of the original minerals of the substrate with new one as consequences of fungal biomineralization process[76].
Lichens
Lichens grow as a visible film on the stone surface and due to their macroscopic structure, their presence on stones is visibly evident. Lichens represent the symbionts of fungi (mainly ascomycete) and algae (mainly green algae) or fungi and cyanobacteria (less common)[28]. Lichens are comparatively more resistant to extreme temperature and desiccation which allows them to flourish and grow in wide variety of habitats some of them may be hostile to other forms of lives[102, 103]. Lichens are among the pioneer organisms which inhabits the exposed stone surfaces. Their growth may be favored by the presence of organic nitrogen rich excretes of birds (crows and pigeons). They have significant contribution in biogeophysical and biogeochemical deterioration of the monumental stone. The CO2 produced during respiration is transformed into carbonic acid (a potent weathering agent) inside the thallus[28]. With the help of their specialized devices like hyphae (crustose lichens) and rhizoids (foliose and fructicose lichens) lichens gain attachment and penetrates into the pores, cracks and fissures of the stones leading to structural and physical damage[26]. Their metabolic activities are often associated with the release of highly corrosive organic carboxylicx acids (like oxalic acid etc) and chelating compounds by which they form complexes with the mineral cations of the substratum[24, 78]. Nitrogen fixation by them is also known to improve the bioweathering potential[30]. Recently documented lichen acids, a group of polyphenolic compounds such as anthraquinones[24] having polar moiety that chelates metallic cations by donating electron pair cause chemical deterioration of the monumental stones through the process of bioweathering. After death, lichens leave behind a pitting corrosion with etch mark due to their metabolic activity and to the incorporation of mineral fragments into the thallus. The contraction-expansion of the lichens as a consequence of desiccation and rehydration results in peeling and detachment of superficial mineral layer[28]. Their presence was also suspected for the formation of oxalate layer on patinas[24, 28].
Fungi within lichens are known to secrete several hundred compounds known as lichen substance. Lichen substances include simple aliphatic organic acids, aromatic polyphenol compounds (such as depsides, depsidones, depsones and carotenoids)[27, 74] and chelating agents (such as norstictic, psoromic, iso-usnic, and usnic acid)[27]. It was believed that some of these lichen substances have got role in extraction of nutrients from the mineral surface of stone[27, 74]. The Lichen-stone mineral interaction was demonstrated in few studies where the presences of some lichen substances like usnic acid, zeroin, and leucotylin (in Lecanora muralis), divaricatic and usnic acid (in Ophioparma ventosa), parietina and rhizocarpic acid (in Xanthoria elegans) and thamnolic acid (in Ophioparma ventosa and Pertusaria corallina) were not reported to be linked with any sort of biodeterioration[52, 104].
Mosses and liverworts
Mosses and liverworts are bryophytes which develop and grow on the surface with abundance of humus deposits. Accumulation of atmospheric particles and dead microorganisms (algae) constitutes the major portion of humus. These are photosynthetic organisms with characteristic pigments but lacking vascular tissues. Their presence is most evident with algae in tropical environment and damp surfaces of monuments. The damage caused by them (usually green-grey patches) is mainly associated with aesthetic appearance but other damages are also known. The carbonic acid produced by them as a result of cellular respiration cause damage to stone over an extended period of time. The extraction of mineral cations from the stones by them is well documented[33, 60, 61, 70]. There are literatures that had also showed the ability of mosses (Grimmia pulvinata (Hedw.) Sm.) to uptake calcium and established their role in biodeterioration but their role in biodeterioration of monuments and art works is still considered as negligible[33]. They possess structures called rhizoids which physical intrude the stone surface but any mechanical damages caused by them is not reported yet. Death on mosses causes indirect damage to monuments and stones by enriching and increasing the humus content which supports the growth of successive species higher plant.
Microbial succession and monuments deterioration: relation Do exist
The colonization of microbial communities on the bare surface of monuments and artworks is mainly determined by the nature and properties of stone surface (surface texture, mineral composition, percentage of different minerals, pH, moisture content and salinity etc.) and surrounding environment conditions (Figure1). The exposed inorganic mineral surface of the monumental stones and artworks serves as a suitable niche for the growth and development of the pioneer microorganisms which includes photoautotrophs, lithophiles and chemolithotrophs (Figure1). Microbial colonization on bare stone surface is thought to be initiated by pioneering phototrophic cyanobacteria and algae, probably followed by lichens, and then general heterotrophs, as heterotrophic communities have ability to grow on rocks having initial phototrophic biomass[41] (Figure1). Phototrophic microorganism which mainly includes cyanobacteria, green algae and lichens are reported to harm the stone surface aesthetically by their secreted pigments. However, secreted organic acids, polyphenolic compounds such as anthraquinones[24] cause chemical deterioration through the process of bioweathering. In tropical climate, (high temperature, high relative humidity and high annual rainfall) these organisms may secrete carbohydrates and growth factors which helps in the formation of biofilm (a three-dimensional structure regulating temperature and humidity) and consequently facilitates the growth of diverse microbial communities within it. The lithophiles population is principally consisted of epilithic (dwelling on surface) and endolithic (residing few mm inside the stone pores) bacteria which promote the breakdown of crystalline structure contributing towards pedogenesis[8, 10]. Biological and metabolic activities and death of these organisms and photosynthetic biomass often fertilizes the surface with organic matters and growth factors which support the growth of successive microbial communities which is predominated by heterotrophic bacteria and fungi. Some organisms are also benefited by the accumulation of ammonia and phosphates coming the atmosphere. Phototrophic algae, lichens and heterotrophic bacteria are also found to be mutually interacts with each other where organic acids produced by phototrophs serves as carbon source for the heterotrophs and both grow unrestricted over a periods of several months[55]. Some of these microorganisms also show pedogenetic actions, making the stone surface powdery and pave the path for succession of mosses and liverwort. Mosses and liverwort occur on substrate with high humus content and contain deposits of dead algal cells. Progressive accumulation of humus and death of mosses favor the emergence of higher plant species.
A Brief demonstration of the relationship between ecological succession and biodeterioration of monuments.
Conclusions
The current research in the field of geomicrobiology has extended our knowledge and understanding of the role of microbes in biodeterioration of historic monuments and artworks. Subsequently, it was felt that the field although maturing needs to unravel the underlying mechanism and cause of destruction to monuments and artworks. Merely, identification and characterization of the biodeteriogens cannot solve the problem of biodeterioration. Additional investigation of various biogeochemical and biogeophysical alterations brought about by action of microorganisms on stone surfaces and the mechanistic studies of alterations is equally worthy to be researched out. Besides this, as certain bacterial and fungal species have inherent capability to act upon the applied protective resins and other covering and use them as source of energy[56], stone surfaces once treated should also looked thereafter routinely so as to check reoccurrence of microbial growth. Moreover, some species of microorganism had acquired resistance to applied biocides[64], which has led intensive research towards formulation of potent biocides.
Evaluation of the factors promoting microbial activity (microbial adherence, growth and survival) on stone surface and understanding the mechanism of deterioration caused to stone surface by them is very essential for designing an appropriate conservation and restoration strategy[70]. Additionally the knowledge of bioreceptivity, which is defined as the totality of materials properties that contribute to the adherence, establishment and colonization of fauna and/or flora on the stone surface of monuments and artworks[72] may be exploited as an important tool for recognizing the biodeterioration process induced by microorganisms and for developing conservation and restoration campaigns. After identification of microorganism and type of deterioration associated with monuments and artworks, the next step is to employ the molecular strategies like Scanning Electron Microscopy (SEM), 16s-RNA Sequencing[9], Denaturing DNA Gel Electrophoresis[9], Temperature Gradient Gel Electrophoresis, Terminal Restriction Fragment Length Polymorphism, X-ray Diffraction (XRD), Laser Induced Fluorescence, Bioinformatics tools, for instance, BLAST, NJ etc. and physical techniques such as Raman Spectroscopy, FT-IR, Mössbauer Spectrometry, Induction Coupled Plasma-Mass Spectrometry, Thermal Analysis, Laser Induced Fluorescence, Fluorescence LIDAR, Thin-layer Petrography, Mercury Intrusion Porosimetry etc. to gain more insight into the cause and mechanism of deterioration processes.
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We would like to thank the Director, Institute of Microbial Technology (CSIR, Govt. of India) for providing the facility for writing this review paper.
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Dakal, T.C., Cameotra, S.S. Microbially induced deterioration of architectural heritages: routes and mechanisms involved. Environ Sci Eur 24, 36 (2012). https://doi.org/10.1186/2190-4715-24-36
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DOI: https://doi.org/10.1186/2190-4715-24-36