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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 ...

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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
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TL;DR: Aerophytic phototrophs, colonizers of different substrates exposed to air, among which are rock substrates in cave habitats, are in general not sufficiently investigated and studied as discussed by the authors.
Abstract: Aerophytic phototrophs, colonizers of different substrates exposed to air, among which are rock substrates in cave habitats, are in general not sufficiently investigated and studied. From the ecolo...

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TL;DR: The findings better define the ecological range of this species, suggesting a wider biogeographic distribution, and adding information on morphological features and genetic data.
Abstract: The colonisation of building material by photosynthetic organisms is highly dependent on the environmental conditions and the nature of the substrate. The growths of red-orange phototrophic biofilms have been widely reported in the literature and have commonly been associated with the order Trentepohliales, whose ecological and taxonomical information needs to be improved. Considering the recurrent presence of such biofilms throughout the Lazio region, we would identify the occurring species and define their favourable environmental conditions, through morphological, genetic and ecological analyses. Biofilms were collected across an altitude range of 0 to 860 m asl, occurring from the coast to 60-km inland. A dominant presence of the filamentous terrestrial green alga Trentepohlia umbrina (Kutzing) Bornet was confirmed in all sites sometimes mixed with cyanobacteria of the genus Gloeocapsa. The distribution of Trentepohliales is generally given as pan-tropical, but some species, such as T. umbrina, are also distributed in temperate climates. Here, it is reported for the first time a Mediterranean occurrence of the species. Low humidity and light conditions, such as those occurring on vertical surfaces with mainly northern aspects, are the preferred environmental conditions. Coastal areas were more favourable for its growth, probably due to the higher nocturnal condensation that occurs here. Concrete and mortars were particularly bioreceptive to T. umbrina, but marble and trachyte were also colonised under favourable conditions. The findings better define the ecological range of this species, suggesting a wider biogeographic distribution, and adding information on morphological features and genetic data.

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

  • ...…Caneva et al. 2005; Macedo et al. 2009; Zucconi et al. 2012; OrtegaMorales et al. 2012; Bartoli et al. 2014) and T. aurea (Noguerol-Seoane and Rifon-Lastra 1996; Ramirez et al. 2010), whereas records of T. umbrina are only limited to Tropical areas (Gaylarde et al. 2006; Samad and Adhikary 2008)....

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  • ...Apart from the aesthetical impact of phototrophic biofilms, in some cases, they can also be considered as bioprotective of stone materials, even if this role has not been comprehensively demonstrated (Cutler and Viles 2010; Ramirez et al. 2010; Pinna 2014)....

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  • ...…been well documented and detailed described for some tropical areas, such East Asia (Wee and Lee 1980; Lee and Wee 1982; Ho et al. 1983; Bartoli et al. 2014) and Mesoamerica (Caneva et al. 2005; Gaylarde and Gaylarde 2005; Gaylarde et al. 2006; Ramirez et al. 2010; Ortega-Morales et al. 2012)....

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TL;DR: This comprehensive review provides an overview of biocolonization and potential changes during the 21st Century and focuses on their capabilities to alter natural building stones, to better understand the role of bacteria and archaea.

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TL;DR: In this study some building materials were inoculated with a microbial consortium of 14 microorganisms, subjected to alternate wetting/drying cycles for six months, and left to rest for eight years, which indicate a remarkable preservation of the DNA.

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TL;DR: A review of the current state of knowledge regarding the mechanisms of biodeterioration, examines the role played by green algae as a result of their adaptation to a terrestrial environment, presents methods that can be used to prevent the development of green algal biofilms and indicate future prospects in the assessment of algal deterioration studies as discussed by the authors.

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References
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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)....

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  • ...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)....

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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)....

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