Biodeterioration of Mayan buildings at uxmal and tulum,Mexico

Uxmal and Tulum are two important Mayan sites in the Yucatan peninsula. The buildings are mainly composed of limestone and grey/black discoloration is seen on exposed walls and copious greenish biofilms on inner walls. The principal microorganisms detected on interior walls at both Uxmal and Tulum were cyanobacteria; heterotrophic bacteria and filamentous fungi were also present. A dark‐pigmented mitosporic fungus and Bacillus cereus, both isolated from Uxmal, were shown to be acidogenic in laboratory cultures. Cyanobacteria belonging to rock‐degrading genera Synechocystis and Gloeocapsa were identified at both sites. Surface analysis previously showed that calcium ions were present in the biofilms on buildings at Uxmal and Tulum, suggesting the deposition of biosolubilized stone. Apart from their potential to degrade the substrate, the coccoid cyanobacteria supply organic nutrients for bacteria and fungi, which can produce organic acids, further increasing stone degradation.     

Sulfur bacteria promote dissolution of authigenic carbonates at marine methane seeps

Carbonate rocks at marine methane seeps are commonly colonized by sulfur-oxidizing bacteria that co-occur with etch pits that suggest active dissolution. We show that sulfur-oxidizing bacteria are abundant on the surface of an exemplar seep carbonate collected from Del Mar East Methane Seep Field, USA. We then used bioreactors containing aragonite mineral coupons that simulate certain seep conditions to investigate plausible in situ rates of carbonate dissolution associated with sulfur-oxidizing bacteria. Bioreactors inoculated with a sulfur-oxidizing bacterial strain, Celeribacter baekdonensis LH4, growing on aragonite coupons induced dissolution rates in sulfidic, heterotrophic, and abiotic conditions of 1773.97 (±324.35), 152.81 (±123.27), and 272.99 (±249.96) μmol CaCO₃ • cm⁻² • yr⁻¹, respectively. Steep gradients in pH were also measured within carbonate-attached biofilms using pH-sensitive fluorophores. Together, these results show that the production of acidic microenvironments in biofilms of sulfur-oxidizing bacteria are capable of dissolving carbonate rocks, even under well-buffered marine conditions. Our results support the hypothesis that authigenic carbonate rock dissolution driven by lithotrophic sulfur-oxidation constitutes a previously unknown carbon flux from the rock reservoir to the ocean and atmosphere.Subject terms: Microbial ecology, Water microbiology, Biogeochemistry, Biogeochemistry, Biofilms     

Comparison of the potential of coastal materials loaded with bacteria for bioremediating oily sea water in batch culture

The objective of this paper was to study whether the bioremediation potential of coastal materials for oil-polluted sea water depended on the numbers of hydrocarbon-utilizing bacteria they naturally harbor. Inshore water of the Arabian Gulf was found to contain only about one thousand hydrocarbon-utilizing bacteria per ml. Coastal sand, cyanobacterial mats and epilithic biomass were much richer in these bacteria, with numbers ranging between several thousand fold to several million fold than in the water body. The predominant bacterium in all samples was Acinetobacter calcoaceticus, next in predominance were nocardioforms and Micrococcus sp. Inoculation, in batch cultures, of oily sea water or sea water containing pure hydrocarbons with fresh sea water, coastal sand, cyanobacterial mats or epilithic biomass harboring significantly different numbers of hydrocarbon-utilizing bacteria brought bioremediation effects that depended on fertilizing with KNO₃. In the absence of KNO₃, the bioremediation effect increased with numbers of hydrocarbon-utilizing bacteria in the inoculum. In the presence of KNO₃ similar bioremediation effects were found irrespective of the inoculated materials. The reason may be that bacteria reproduce quickly in closed cultures provided with nitrogen, reaching equal maximum numbers, irrespective of the inoculum size. This information could be useful in constructing technologies for oily sea water bioremediation.     

Comparison of the Phenotypes and Genotypes of Biofilm and Solitary Epiphytic Bacterial Populations on Broad-Leaved Endive

The discovery that biofilms are ubiquitous among the epiphytic microflora of leaves has prompted research about the impact of biofilms on the ecology of epiphytic microorganisms and on the efficiency of strategies to manage these populations for disease control and to ensure food safety. Biofilms are likely to influence the microenvironment and phenotype of the microorganisms they harbor. However, it is also important to determine whether there are differences in the types of bacteria within biofilms compared to those outside of biofilms so as to better target microorganisms via disease control strategies. Broad-leaved endive (Cichorium endivia var. latifolia) harbors biofilms containing fluorescent pseudomonads. These bacteria can cause considerable post-harvest losses when this plant is used for manufacturing minimally processed salads. To determine whether the population structure of the fluorescent pseudomonads in biofilms is different from that outside of biofilms on the same leaves, bacteria were isolated quantitatively from the biofilm and solitary components of the epiphytic population on leaves of field-grown broad-leaved endive. Population structure was determined in terms of taxonomic identities of the bacteria isolated, in terms of genotypic profiles, and in terms of phenotypic traits related to surface colonization and biofilm formation. The results illustrate that there are no systematic differences in the composition and structure of biofilm and solitary populations of fluorescent pseudomonads, in terms of either genotypic profiles or phenotypic profiles of the strains. However, Gram-positive bacteria tended to occur more frequently within biofilms than outside of biofilms. We suggest that leaf colonization by fluorescent pseudomonads involves a flux of cells between biofilm and solitary states. This would allow bacteria to exploit the advantages of these two types of existence; biofilms would favor resistance to stressful conditions, whereas solitary cells could foster spread of bacteria to newly colonizable sites on leaves as environmental conditions fluctuate.     

CTC staining and counting of actively respiring bacteria in natural stone using confocal laser scanning microscopy

A method was established for staining and counting of actively respiring bacteria in natural stone by using the tetrazolium salt 5-cyano-2,3-ditolyltetrazolium chloride (CTC) in combination with confocal laser scanning microscopy (CLSM). Applying 5 mM CTC for 2 h to pure cultures of representative stone-inhabiting microorganisms showed that chemoorganotrophic bacteria and fungi-in contrast to lithoautotrophic nitrifying bacteria-were able to reduce CTC to CTF, the red fluorescing formazan crystals of CTC. Optimal staining conditions for microorganisms in stone material were found to be 15 mM CTC applied for 24 h. The cells could be visualized on transparent and nontransparent mineral materials by means of CLSM. A semi-automated method was used to count the cells within the pore system of the stone. The percentage of CTC-stained bacteria was dependent on temperature and humidity of the material. At 28 degrees C and high humidity (maximum water holding capacity) in the laboratory, about 58% of the total bacterial microflora was active. On natural stone exposed for 9 years at an urban exposure site in Germany, 52-56% of the bacterial microflora was active at the east, west, and north side of the specimen, while only 18% cells were active at the south side. This is consistent with microclimatic differences on the south side which was more exposed to sunshine thus causing UV and water stress as well as higher temperatures on a microscale level. In combination with CLSM, staining by CTC can be used as a fast method for monitoring the metabolic activity of chemoorganotrophic bacteria in monuments, buildings of historic interest or any art objects of natural stone. Due to the small size of samples required, the damage to these objects and buildings can be minimized.     

The influence of air pollution on the phyllosphere microflora composition of Tillandsia leaves (Bromeliaceae)

The effect of air pollution on total phyllospheric microflora from two species of the epiphytic neotropical genus Tillandsia (Bromeliaceae) was studied by comparing unpolluted plants living in a forest (Escazú, San José) with polluted ones from an urban site of Costa Rica (San José city). Dilutions of homogenized leaf samples were plated on media suitable for each microbial group. For each microorganism group, total counts were performed and purified strains of randomly chosen colonies were identified. There was a global reduction in the number of living microorganisms due to pollution effects, especially yeasts and bacteria, while nitrogen-fixing microorganisms and fungi were less affected. Our results showed that the phyllosphere microflora of Tillandsia plants living in a tropical urban environment changes in terms of number and species composition of yeasts and bacteria with respect to plants living in unpolluted environment.     

Activity of Microorganisms in Acid Mine Water I. Influence of Acid Water on Aerobic Heterotrophs of a Normal Stream

Comparison of microbial content of acid-contaminated and nonacid-contaminated streams from the same geographical area indicated that nonacid streams contained relatively low numbers of acid-tolerant heterotrophic microorganisms. The acid-tolerant aerobes survived when acid entered the stream and actually increased in number to about 2 × 10³ per ml until the pH approached 3.0. The organisms then represented the heterotrophic aerobic microflora of the streams comprised of a mixture of mine drainage and nonacid water. A stream which was entirely acid drainage did not have a similar microflora. Most gram-positive aerobic and anaerobic bacteria died out very rapidly in acidic water, and they comprised a very small percentage of the microbial population of the streams examined. Iron- and sulfur-oxidizing autotrophic bacteria were present wherever mine water entered a stream system. The sulfur-oxidizing bacteria predominated over iron oxidizers. Ecological data from the field were verified by laboratory experiments designed to simulate stream conditions.     

Deterioration of limestone structures associated with copper staining

Sixty limestone monuments in Central London, UK, with copper staining from brass or bronze attachments, were surveyed. Severe spalling was noted at some copper-stained sites. The survey suggests that copper initially protects the surface, but causes stone deterioration after around 70 years. Samples from four limestone monuments were analysed microbiologically and using ESEM/EDX. EDX analyses suggested the build-up of salts below a basic copper carbonate skin (salting) as the most probable explanation of the observed deterioration. Copper-stained stone was free of photosynthetic microorganisms and yielded relatively few other microorganisms. ESEM and EDX analyses of a well-conserved limestone monument surface free of copper showed the almost complete conversion of surface limestone to gypsum. The grey/brown biofilms consisted of actinomycetes and filamentous fungi. The results indicate that copper initially prevents and then enhances limestone deterioration, and that atmospheric pollutants are far less harmful than phototrophic biofilms, since surface areas completely converted to gypsum are well preserved after more than 100 years.     

嗜酸藻类研究进展

酸性矿山废水(acid mine drainage,AMD)是硫化矿物暴露于地表,与水、大气及微生物相互作用发生氧化性溶解而形成的,其pH通常在3.5以下,并含有高浓度的金属离子,危害十分严重。因为嗜酸原核生物可通过氧化硫化矿物获得能量,从而加速酸性矿山废水的形成过程,所以一直以来都是嗜酸微生物研究的焦点。但事实上,真核生物在酸性生态系统中往往发挥着更重要的作用。尤其是光合藻类,它们在很多酸性环境都是主要的初级生产者,对酸性矿山废水的演化和修复起着关键的推动作用。本文从嗜酸藻类的常见种类和生态分布、适应极端环境的生理机制以及它们在污染治理和工业生产中的应用3个方面,综述了该领域近30年来的研究进展,并以此为基础提出了将来需要着力加强的5个研究方向。     

Physical morphology and surface properties of unsaturated Pseudomonas putida biofilms

Unsaturated biofilms of Pseudomonas putida, i.e., biofilms grown in humid air, were analyzed by atomic force microscopy to determine surface morphology, roughness, and adhesion forces in the outer and basal cell layers of fresh and desiccated biofilms. Desiccated biofilms were equilibrated with a 75.5% relative humidity atmosphere, which is far below the relative humidity of 98 to 99% at which these biofilms were cultured. In sharp contrast to the effects of drying on biofilms grown in fluid, we observed that drying caused little change in morphology, roughness, or adhesion forces in these unsaturated biofilms. Surface roughness for moist and dry biofilms increased approximately linearly with increasing scan sizes. This indicated that the divides between bacteria contributed more to overall roughness than did extracellular polymeric substances (EPS) on individual bacteria. The EPS formed higher-order structures we termed mesostructures. These mesostructures are much larger than the discrete polymers of glycolipids and proteins that have been previously characterized on the outer surface of these gram-negative bacteria.     

Biodeterioration of natural stone with special reference to nitrifying bacteria

An evaluation of field data from historical buildings in Germany showed that chemoorganotrophic bacteria are the most numerous microorganisms in building stones, followed by fungi and nitrifying bacteria. Chemoorganotrophic bacteria and fungi were present in almost every sample. Ammonia and nitrite oxidizers were found in 55 and 62% of the samples, respectively. Within months, natural stone was colonized by chemoorganotrophic microorganisms. The highest cell numbers were usually found near the surface. The colonization of natural stone by nitrifying bacteria took several years. The highest cell numbers were in some cases found underneath the surface. Nitrifying bacteria showed a preference for calcareous material with a medium pore radius between 1 and 10 m. Cell numbers of nitrifying bacteria did not correlate to the nitrate content of the stone material. We demonstrated that the stone inhabiting microflora can cause significant loss of nitrate by denitrification. Our data strongly suggested that microbial colonization of historical buildings was enhanced by anthropogenic air pollution. Samples taken from stone material with a pore radius 1 m had significantly higher cell numbers when they were covered with black crusts. A comparison of samples taken between 1990–1995 from buildings throughout Germany showed that in eastern Germany a significantly stronger colonization with facultatively methylotrophic bacteria and nitrifying bacteria existed. The same was true for natural stone from an urban exposure site when compared to material from a rural exposure site. Data from outdoor exposure and laboratory simulation experiments indicated that the colonization of calcareous stone by nitrifying bacteria was enhanced by chemical weathering.     

Cyanobacteria cause black staining of the National Museum of the American Indian Building, Washington, DC, USA

Microbial deterioration of stone is a widely recognised problem affecting monuments and buildings all over the world. In this paper, dark-coloured staining, putatively attributed to microorganisms, on areas of the National Museum of the American Indian Building, Washington, DC, USA, were studied. Observations by optical and electron microscopy of surfaces and cross sections of limestone indicated that biofilms, which penetrated up to a maximum depth of about 1?mm, were mainly composed of cyanobacteria, with the predominance of Gloeocapsa and Lyngbya. Denaturing gradient gel electrophoresis analysis revealed that the microbial community also included eukaryotic algae (Trebouxiophyceae) and fungi (Ascomycota), along with a consortium of bacteria. Energy-dispersive X-ray spectroscopy analysis showed the same elemental composition in stained and unstained areas of the samples, indicating that the discolouration was not due to abiotic chemical changes within the stone. The dark pigmentation of the stone was correlated with the high content of scytonemin, which was found in all samples.     

Involvement of Sulfur- and Iron-Transforming Bacteria in Heaving of House Foundations

About 1,000 houses built on excavated nonweathered mudstone sediments, originally deposited in the Neogene, have been damaged by microbially induced heaving of foundations. The maximal height of the heaving was 48 cm. The presence of sulfate-reducing, sulfur-oxidizing, and acidophilic iron-oxidizing bacteria in the mudstone indicated that the joint activity of these three types of bacteria could account for the heaving. A hypothesis is presented in which, first, the temperature of the newly exposed mudstone sediments increased above 25 °C, which stimulated the sulfate-reducing bacteria in the mudstone to actively reduce sulfate to hydrogen sulfide. The mudstone sediments under the houses gradually dried, and became permeable to air. Consequently, sulfur-oxidizing bacteria oxidized the hydrogen sulfide to sulfuric acid and the environmental pH decreased to approximately 3. Next, the acidophilic iron-oxidizing bacteria actively oxidized the sulfur in pyrite to produce much more acid. The resulting sulfuric acid reacted with calcium carbonate and with ferric and potassium ions to produce gypsum and jarosite, respectively. A combination of the increased volume of gypsum and jarosite crystals and the production of CO 2 as a by-product of their formation made the mudstone sediments bulky. The end result was widespread heaving.     

Isolation, characterization, and in situ detection of a novel chemolithoautotrophic sulfur-oxidizing bacterium in wastewater biofilms growing under microaerophilic conditions

We successfully isolated a novel aerobic chemolithotrophic sulfur-oxidizing bacterium, designated strain SO07, from wastewater biofilms growing under microaerophilic conditions. For isolation, the use of elemental sulfur (S(0)), which is the most abundant sulfur pool in the wastewater biofilms, as the electron donor was an effective measure to establish an enrichment culture of strain SO07 and further isolation. 16S rRNA gene sequence analysis revealed that newly isolated strain SO07 was affiliated with members of the genus Halothiobacillus, but it was only distantly related to previously isolated species (89% identity). Strain SO07 oxidized elemental sulfur, thiosulfate, and sulfide to sulfate under oxic conditions. Strain SO07 could not grow on nitrate. Organic carbons, including acetate, propionate, and formate, could not serve as carbon and energy sources. Unlike other aerobic sulfur-oxidizing bacteria, this bacterium was sensitive to NaCl; growth in medium containing more than 150 mM was negligible. In situ hybridization combined with confocal laser scanning microscopy revealed that a number of rod-shaped cells hybridized with a probe specific for strain SO07 were mainly present in the oxic biofilm strata (ca. 0 to 100 micro m) and that they often coexisted with sulfate-reducing bacteria in this zone. These results demonstrated that strain SO07 was one of the important sulfur-oxidizing populations involved in the sulfur cycle occurring in the wastewater biofilm and was primarily responsible for the oxidation of H(2)S and S(0) to SO(4)(2-) under oxic conditions.     

Airborne microorganisms in a subterranean archaeological area of the basilica of San Lorenzo in Lucina (Rome)

The basilica of San Lorenzo in Lucina in Rome was built in the fifth century on the foundations of a Roman insula used for dwellings and commercial activities, where the first Christian communities had held their meetings. This archaeological area is still rather isolated since it can only be visited by groups for one/two hours once a month. Such a situation is ideal for studying both the quantity of microorganisms in the air under undisturbed conditions and/or conveyed by visitors. The biodeterioration of subterranean remains is determined by the development of bacteria, cyanobacteria, actinomycetes, algae and fungi. On the walls of this underground archaeological area the main form of alteration is the efflorescence. In order to compare the stone and airborne microflora, the microorganisms living on stone and the airborne ones have been detected. Air samples were taken both during the visits and under non-turbulent conditions utilizing three sampling methods: gravitational, intake by multi-stage impact and intake by single-stage impact. The results have made it possible to determine the microbial content of the air, as well as the sampling schedule required for rarely visited underground environments. Furthermore, a comparison of the three methods used showed that the adoption of one or the other sampling method gave different complementary information on airborne microflora. This revised version was published online in June 2006 with corrections to the Cover Date.     

Effects of heavy metal pollution on the microflora of pine needles

A leaf washing method was used to compare the numbers and species composition of the phylloplane microflora of corsican pine saplings (a) uncontaminated, (b) exposed to zinc, lead and cadmium pollution from a smelter and (c) artificially dosed with zinc, lead and cadmium oxides to simulate the emissions from the smelter without the complicating effects of other pollutants. There was little difference in total numbers of most groups of micro-organisms isolated from each site, although both sets of metal-contaminated saplings generally supported a higher percentage of metal tolerant isolates than the uncontaminated plants. Artificially dosed plants also supported greater numbers of Aureobasidium pullulans and orange and pink chromogenic bacteria. These particular organisms were also among the most metal-tolerant fungi and bacteria in vitro.     

In situ PCR for visualizing distribution of a functional gene "amoA" in a biofilm regardless of activity

In this study, ammonia-oxidizing bacteria present in biofilms resulting from a nitrifying reactor were detected by both a conventional FISH technique and an original in situ PCR technique. Both techniques showed that ammonia-oxidizing bacteria were found near the surface of the biofilms. However, after the biofilm had been exposed to 2 weeks of ammonia starvation, ammonia-oxidizing bacteria present in the biofilm could not be detected by fluorescence in situ hybridization (FISH) because they did not have sufficient copies of rRNA. In contrast, ammonia-oxidizing bacteria could be detected by in situ PCR with strong signal. It was thus demonstrated that a cell possessing a specific functional gene is detectable by in situ PCR regardless of its activity.     

Succession of fungi colonizing porous and compact limestone exposed to subtropical environments

Little is known about the dynamics of succession of fungi on limestone exposed in subtropical environments. In this study, the colonization of experimental blocks of compact and porous limestone by a fungal community derived from natural biofilms occurring on Structure X from the archaeological site of Becán (México), was studied using a cultivation-dependent approach after short-term (9 m) exposure in order to provide a preliminary insight of the colonization process under seminatural conditions. Microbial growth seen as the change of colour of stone surfaces to black/dark green was more abundant on the porous limestone. There was a fairly clear difference in microbial colonization between the onset of the experiment and the 6th month for both limestone types, but no significant increase in the colonization of coupons occurred between months 6 and 9. This could be related to the low rainfall expected for this period, corresponding to the dry season. A total of 977 isolates were obtained. From these, 138 sterile fungi were unidentified, 380 could only be assigned to the order Sphaeropsidales; the remaining isolates (459) were grouped into 27 genera and 99 different species. Nearly all detected fungal species belonged to the Ascomycota (90 %). Rare taxa (species represented by one to three isolates) included the recently described genus Elasticomyces, several species of genera Hyalodendron, Monodyctis, Papulospora, Curvularia, and Septoria. Other taxa were Minimedusa and Gliomastix luzulae, which have not been previously described for stone environments. Abundant fungi included several species of the common genera Cladosporium, Alternaria, and Taeniolella typical for a range of habitats. Succession of populations was observed for certain taxa, this shift in the composition of fungal communities was more evident in porous limestone. After 6 m of exposure, species of the genera Scolecobasidium, Hyalodendron, and Taeniolella were predominant, while after 9 m, the predominant species belonged to the genera Curvularia and Alternaria, particularly on porous stone. These results suggest that Curvularia and Alternaria replaced other fungi, due to a higher tolerance towards low levels of available water during the dry season. Higher levels of water within the porous stone, keep longer periods of microbial activity, minimizing the impact of desiccation. This study contributes to understand the diversity of fungal communities in stone surfaces in subtropical settings and the dynamics of colonization on limestone.     

Multiple cues from multiple habitats: Effect on metamorphosis of the Florida stone crab, Menippe mercenaria

The Florida stone crab, Menippe mercenaria, is an economically and ecologically important species that ranges from North Carolina throughout the Caribbean and the southeastern Gulf of Mexico. However, there is little known about its early life history stages as compared to other commercially important species in the region. The goal of this research was to examine effects of putative cues on metamorphosis from the megalopa stage to the first juvenile stage. Our study investigated the effect of water-soluble exudates from four substrata, as well as natural biofilms, and exudates from adult stone crabs. In addition, the influence of natural substrata was compared to that of artificial substrata. Adult exudate had no significant effect on metamorphosis, despite a wide range of tested concentrations. In contrast, there was a significant effect on mean time to metamorphosis in experimental groups exposed to multiple cues associated with the brown alga Sargassum fluitans, rubble from stone crab habitat, the eastern oyster Crassostrea virginica, and biofilms associated with the oyster. Furthermore, we provide evidence for metamorphic responses to water-soluble chemical cues, as well as biochemical and physical cues associated with different substrata. Overall results were coherent with the relevant body of previous work on metamorphosis of brachyuran crab larvae and indicate that both physical and chemical cues are important factors in facilitating the settlement and metamorphosis of M. mercenaria larvae in juvenile nursery habitat.     

Genetic characterization of microbial communities living at the surface of building stones

Aims:  The aim of the present study was to reveal the microbial genetic diversity of epilithic biofilms using a DNA-based procedure.
Methods and Results:  A DNA extraction protocol was first selected to obtain PCR-amplifiable metagenomic DNA from a limestone biofilm. Extracted DNA was used to amplify either 16S rRNA genes or ITS regions from prokaryotic and eukaryotic genomes, respectively. Amplified DNAs were subsequently cloned, amplified by colony PCR and screened by restriction analysis [restriction analyses of amplified ribosomal DNA (ARDRA)] for DNA sequencing. Phylogenetic analysis using 16S rDNA sequences showed that predominating bacteria were Alphaproteobacteria belonging to the genera Sphingomonas , Erythrobacter , Porphyrobacter , Rhodopila and Jannashia ; Cyanobacteria and Actinobacteria were also identified. Analysis of ITS rDNA sequences revealed the presence of algae of the Chlorophyceae family and fungi related either to Rhinocladiella or to a melanized ascomycete. Statistical analysis showed that the specific richness evidenced was representative of the original sampled biofilm.
Conclusions:  The molecular methodology developed here constitutes a valuable tool to investigate the genetic diversity of microbial biofilms from building stone.
Significance and Impact of the Study:  The easy-to-run molecular method described here has practical importance to establish microbiological diagnosis and to define strategies for protection and restoration of stone surfaces.