scispace - formally typeset
Search or ask a question
Journal ArticleDOI

Cyanobacteria-containing biofilms from a Mayan monument in Palenque, Mexico

TL;DR: The structural characterization and species composition of biofilms from the walls of one of the buildings at the archaeological site of Palenque, Mexico, are reported and the implications for the development and permanence of species capable of withstanding temporal heterogeneity in and on El Palacio are discussed.
Abstract: Surfaces of buildings at the archaeological site of Palenque, Mexico, are colonized by cyanobacteria that form biofilms, which in turn cause aesthetic and structural damage. The structural characterization and species composition of biofilms from the walls of one of these buildings, El Palacio, are reported. The distribution of photosynthetic microorganisms in the biofilms, their relationship with the colonized substratum, and the three-dimensional structure of the biofilms were studied by image analysis. The differences between local seasonal microenvironments at the Palenque site, the bioreceptivity of stone and the relationship between biofilms and their substrata are described. The implications for the development and permanence of species capable of withstanding temporal heterogeneity in and on El Palacio, mainly due to alternating wet and dry seasons, are discussed. Knowledge on how different biofilms contribute to biodegradation or bioprotection of the substratum can be used to develop maintenance ...

Content maybe subject to copyright    Report

SUPPLEMENTARY MATERIAL
Table 2. Species identified in sampling sites at El Palacio (Palenque).
Taxa Size Location Figure
Cyanobacteria
Chroococcales
Synechococcaceae
Aphanothecoideae
Aphanothece castagnei
(Bre
´
bisson) Rabenhorst
Cells 4.1-(5.3)76.6 mm wide and
2.6-(4.9)77.2 mm long
I
III
IV
Gloeothece cf. palea (Ku
¨
tz.)
Rabenhorst
Cells 2.3-(2.4)72.6 mm wide,
4.6-(7.9)711.2 mm with sheath and 2.6-
(4.9)77.26 long,
6.6-(9.2)711.8 mm with sheath.
I
II
III
IV
Microcystaceae
Gloeocapsa calcicola Gardner Cells 2.6-(3.3)74.2 mm wide and
9.2-(13.8)718.5 mm with sheath
I
II
III
IV
Gloeocapsa quaternata Ku
¨
tzing Cells 2.3-(2.9)73.5 mm wide and
3.2-(5.3)77.5 mm long. With sheath 5-
(5.7)76.5 mm wide and
6-(7.2)78.5 mm long
I
II
III
IV
Chroococcaceae
Asterocapsa divina Koma
´
rek Colonies 13.3-(63.9)7114.5 mm wide. Cells
6.6-(9.9)713.3 mm wide and 9.9-
(12.4)714.9 mm long. Cells with sheath
9.9-(25.7)741.5 mm wide
II
III
IV
Chroococcus cf. schizodermaticus
W. et G.S. West
Colonies de 7-(13.5)720 mm wide. Cells 4-
(8.5)713 mm wide and
5-(10.5)716 mm long
I
IV
Oscillatoriales
Pseudoanabaenaceae
Leptolyngbyoideae
Leptolyngbya cf. compacta
(Ku
¨
tzing ex Hansgirg) Koma
´
rek
et Anagnostidis
Filament diameter. Trichomes
1.3-(1.6)72 mm wide and cells
1.9-(2.6)73.3 mm long, sheath
1.5-(1.7)72 mm thick
I
IV
Schizotrichaceae
Schizothrix bosniaca (Hansgirg)
Geitler
Trichomes 2.4-(4.1)75.7 mm wide, cells 3.7-
(7.3)711 mm long
I
IV
(continued)

SUPPLEMENTARY MATERIAL
Table 2. (Continued).
Taxa Size Location Figure
Nostocales
Scytonemataceae
Scytonema guyanense (Mont.)
Bornet et Flahaut
Cells 4.9-(9.5)714.1 mm wide and
3.4714.9 mm long. Heterocysts 3.4-
(9.2)714.9 mm wide and
5.5-(10.8)716.1 mm long.
Sheath 8.3-(10.5)712.7 mm
I
IV
Nostocaceae
Nostoc commune Vaucher ex
Bornet et Flahaut
Cells 5.8-(6.6)77.4 mm wide and
4.9-(7.4)79.9 mm long. Heterocysts 6.6-
(7.4)78.3 mm wide and 7.4-(7.8)78.3 mm
long
I
IV
Chlorophyta
Trentepohliophyceae
Trentepohliales
Trentepohlia aurea (Linn) Martius Young cells: 3.9-(16.7)729.5 mm wide and
3.9-(13.6)723.2 mm long. Mature cells:
9.9-(18.2)726.5 mm wide and 18.2-
(35.2)752.1 mm long. Sporangia: 15.8-
(22.1)728. 2 mm wide and 17.8-
(25.5)733.2 mm long
III
IV
Citations
More filters
Journal ArticleDOI
TL;DR: In this paper, the authors provide an opinionated exposition of the status and utility of the bioreceptivity concept for built heritage science and conservation in the light of current knowledge, aimed to stimulate further discussion.

36 citations

Journal ArticleDOI
TL;DR: This review summarizes the current state of knowledge on aerial epilithic cyanobacterial communities on both natural and anthropogenic stone surfaces around the world and suggests further thorough research on this often neglected group of organisms is desirable.
Abstract: Terrestrial cyanobacteria dwelling on rocks and stone walls represent an important but still understudied part of global biodiversity, despite their substantial importance to the environment. Microbial biofilms, including those formed by cyanobacteria, play an essential role in the succession on rock habitats as they possess a unique ability to gradually change the biotope. In this review, we have gathered 180 research publications reporting on occurrence of 762 species of terrestrial cyanobacteria on rock surfaces worldwide. Despite the long history of phycological research in general, Europe remains the most thoroughly explored region in the field of terrestrial phycology. A total of 401 taxa records from aerial epilithic habitats have been reported from this subcontinent. With regard to the lack of comparably comprehensive studies from different areas of the world, reliable comparisons of species richness among different geographical regions and climatic zones are not available at the moment. Heterocytous and coccoid cyanobacteria prevailed on the rocks and stones in terms of biomass, however, the species richness seemed to be distributed equally among coccoid (269 taxa), simple filamentous (275 taxa), and heterocytous (218 taxa) forms. As the heterogeneity of the available data shows, further thorough research on this often neglected group of organisms is desirable. To set a starting point for such an effort, this review summarizes the current state of knowledge on aerial epilithic cyanobacterial communities on both natural and anthropogenic stone surfaces around the world.

35 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...Authors are grateful to all reviewers for their valuable comments leading to improvement of the manuscript....

    [...]

Journal ArticleDOI
TL;DR: In this paper, the main colonizer and the composition of the biogenic compounds present in a reddish biofilm located on the sandstone from the Northside of La Galea Fortress (Getxo, North of Spain).

33 citations

Journal ArticleDOI
TL;DR: For the first time in the cultural heritage field, culture-independent molecular methods were used to resolve the structure of airborne communities near discoloured surfaces, and to investigate the relationship between such communities and surface-associated biofilms.
Abstract: The study characterized the sessile microbial communities on mortar and stone in Milan University's Richini's Courtyard and investigated the relationship between airborne and surface-associated microbial communities. Active colonization was found in three locations: green and black patinas were present on mortar and black spots on stone. Confocal laser scanning microscopy, scanning electron microscopy and culture-independent molecular methods revealed that the biofilm causing deterioration was dominated by green algae and black fungi. The mortar used for restoration contained acrylic and siloxane resins that could be used by microorganisms as carbon and energy sources thereby causing proliferation of the biofilm. Epifluorescence microscopy and culture-based methods highlighted a variety of airborne microflora. Bacterial and fungal counts were quantitatively similar to those reported in other investigations of urban areas, the exception being fungi during summer (1–2 orders of magnitude higher). For the fi...

32 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...Indeed, deterioration due to microbial biofilm leads to chemical, physical and aesthetic damage, depending on the microorganisms involved, the environmental conditions and the physico-chemical properties of construction materials (Gaylarde and Morton 1999; Ramirez et al. 2010; Sanmartı̀n et al. 2010; Rossi et al. 2012)....

    [...]

  • ...…due to microbial biofilm leads to chemical, physical and aesthetic damage, depending on the microorganisms involved, the environmental conditions and the physico-chemical properties of construction materials (Gaylarde and Morton 1999; Ramirez et al. 2010; Sanmartı̀n et al. 2010; Rossi et al. 2012)....

    [...]

Journal ArticleDOI
TL;DR: Observations 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, while denaturing gradient gel electrophoresis analysis revealed that the microbial community also included eukaryotic algae and fungi, along with a consortium of bacteria.
Abstract: 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 co...

31 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...Cyanobacteria damage stone due to the production of inorganic and organic metabolic products, in particular acids, some of which have chelating abilities (Ramirez et al. 2010)....

    [...]

References
More filters
Journal ArticleDOI
TL;DR: In this paper, a comprehensive overview to the biodeterioration of stone and its practical relevance for the conservation is presented. But, the authors do not consider the effects of the microbial contamination on cleaning procedures, protective treatments as well as biocidal applications.

889 citations


"Cyanobacteria-containing biofilms f..." refers background in this paper

  • ...1991; Kumar and Kumar 1999), or favor the acceleration of weathering processes (Warscheid and Braams 2000) as observed in Sites II and III of El Palacio....

    [...]

  • ...artificial substrata can become colonized by communities of microorganisms enclosed in exopolysaccharide matrices called biofilms (Warscheid and Braams 2000; Di Pippo et al. 2009)....

    [...]

  • ...Under suitable conditions, both natural and artificial substrata can become colonized by communities of microorganisms enclosed in exopolysaccharide matrices called biofilms (Warscheid and Braams 2000; Di Pippo et al. 2009)....

    [...]

  • ...…can cause discoloration of stone surfaces (Hernández-Mariné et al. 2003) and mechanical and biochemical deterioration (Ortega-Calvo et al. 1991; Kumar and Kumar 1999), or favor the acceleration of weathering processes (Warscheid and Braams 2000) as observed in Sites II and III of El Palacio....

    [...]

Journal ArticleDOI
TL;DR: Subaerial biofilm metabolic activity centres on retention of water, protecting the cells from fluctuating environmental conditions and solar radiation as well as prolonging their vegetative life, which manifests itself as bio-weathering of rock surfaces.
Abstract: Biofilms are interface micro-habitats formed by microbes that differ markedly from those of the ambient environment. The term 'subaerial biofilm' (SAB) was coined for microbial communities that develop on solid mineral surfaces exposed to the atmosphere. Subaerial biofilms are ubiquitous, self-sufficient, miniature microbial ecosystems that are found on buildings, bare rocks in deserts, mountains, and at all latitudes where direct contact with the atmosphere and solar radiation occurs. Subaerial biofilms on exposed terrestrial surfaces are characterized by patchy growth that is dominated by associations of fungi, algae, cyanobacteria and heterotrophic bacteria. Inherent subaerial settlers include specialized actinobacteria (e.g. Geodermatophilus), cyanobacteria and microcolonial fungi. Individuals within SAB communities avoid sexual reproduction, but cooperate extensively with one another especially to avoid loss of energy and nutrients. Subaerial biofilm metabolic activity centres on retention of water, protecting the cells from fluctuating environmental conditions and solar radiation as well as prolonging their vegetative life. Atmospheric aerosols, gases and propagatory particles serve as sources of nutrients and inoculum for these open communities. Subaerial biofilms induce chemical and physical changes to rock materials, and they penetrate the mineral substrate contributing to rock and mineral decay, which manifests itself as bio-weathering of rock surfaces. Given their characteristic slow and sensitive growth, SAB may also serve as bioindicators of atmospheric and/or climate change.

520 citations

Journal ArticleDOI
Malcolm Potts1
TL;DR: Drying of cells leads to damage resulting from crowding of cytoplasmic components, condensation of the nucleoid, increases in the Tm of membrane phase transitions, and imposition of stress upon cell walls, which restricts many organisms to aqueous environments, some, including many cyanobacteria, can tolerate the air-dried state for prolonged periods.
Abstract: Drying of cells leads to damage resulting from crowding of cytoplasmic components, condensation of the nucleoid, increases in the Tm of membrane phase transitions, and imposition of stress upon cell walls. Prolonged desiccation leads to oxidation of proteins, DNA and membrane components through metal-dependent Fenton reactions, while Maillard reactions generate cross-linked products between the carbonyl groups of reducing sugars and the primary amines of nucleic acids and proteins. Although such damage restricts many organisms to aqueous environments, some, including many cyanobacteria, can tolerate the air-dried state for prolonged periods. Cyanobacteria in the Tintenstrich communities of exposed rock faces, Microcoleus and Lyngbya spp. in intertidal mats, chasmoendolithic Chroococcidiopsis spp. in the rocks of hot and cold deserts, and terrestrial epilithic crusts of Tolypothrix and Nostoc are examples that show a marked capacity to withstand the removal of their cellular water. For Nostoc commune, the ...

313 citations


"Cyanobacteria-containing biofilms f..." refers background in this paper

  • ...Survival strategies related to desiccation are well known (Potts 1999; Wynn-Williams 2000), and include the use of water retained within the substrata and the formation of protective, droughtresistant compounds (Gorbushina and Krumbein 2000)....

    [...]

  • ...During the dry season, in which conditions were unfavorable, phototrophic microorganisms were hidden under the remains from the previous wet season and were protected by their respective resilience strategies (Potts 1999)....

    [...]

Journal ArticleDOI
TL;DR: Differences in metabolic parameters and community structure between two types of crusts were consistent with a successional pattern, which could be partially explained on the basis of the microenvironments.
Abstract: We used microsensors to characterize physicochemical microenvironments and photosynthesis occurring immediately after water saturation in two desert soil crusts from southeastern Utah, which were formed by the cyanobacteria Microcoleus vaginatus Gomont, Nostoc spp., and Scytonema sp. The light fields within the crusts presented steep vertical gradients in magnitude and spectral composition. Near-surface light-trapping zones were formed due to the scattering nature of the sand particles, but strong light attenuation resulted in euphotic zones only ca. 1 mm deep, which were progressively enriched in longer wavelengths with depth. Rates of gross photosynthesis (3.4–9.4 mmol O2·m−2·h−1) and dark respiration (0.81–3.1 mmol O−2·m−2·h−1) occurring within 1 to several mm from the surface were high enough to drive the formation of marked oxygen microenvironments that ranged from oxygen supersaturation to anoxia. The photosynthetic activity also resulted in localized pH values in excess of 10, 2–3 units above the soil pH. Differences in metabolic parameters and community structure between two types of crusts were consistent with a successional pattern, which could be partially explained on the basis of the microenvironments. We discuss the significance of high metabolic rates and the formation of microenvironments for the ecology of desert crusts, as well as the advantages and limitations of microsensor-based methods for crust investigation.

310 citations


"Cyanobacteria-containing biofilms f..." refers result in this paper

  • ...These results are comparable with those of extreme habitats ranging from Antarctic communities (Büdel et al. 2008) to deserts (Garcia-Pichel and Belnap 1996; Wynn-Williams 2000)....

    [...]