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Essential processes necessary for the establishment and maintenance of rock biofilms include photosynthesis, production of extracellular polymeric substances, substrate penetration and nutrient enrichment from the atmosphere. This natural functional diversity is supported by a complex biofilm community consisting of heterotrophic and phototrophic microorganisms. While heterotrophic rock biofilm-formers are dominated by stress-tolerant microcolonial ascomycetes, phototrophs might be represented by diverse algae and cyanobacteria. Reduction of model systems to the genetically tractable minimum, a proven successful experimental strategy in different symbiotic systems, is now applied to rock biofilms. These complex and important natural systems are simulated in the lab using genetic methods coupled with continuous microscopic and analytical (microscopic as well as geochemical and biochemical) observations. Our in vitro bipartite model includes free-living and symbiosis-competent, genetically tractable microorganisms – a rock-inhabiting fungus Knufia petricola A95 and a cyanobacterium Nostoc punctiforme strain ATCC 29133. To accurately reflect the development of a rock biofilm, contacts of these two genetically tractable partners are studied under well-controlled laboratory conditions. This experimental strategy is strongly supported by the knockout mutants of Knufia petricola which have been recently created and will be compared in their action on mineral surfaces. An impact of Knufia petricola strain A95 with or without protective pigments on mineral adhesion and alteration will be presented.
Methanogenic Archaea
(2017)
Different environmental samples reveal that methanogenic Archaea are part of a multi-species biofilm on corroding metallic structures. Studies on microbial influenced corrosion (MIC) focus mainly on sulphate reducing Bacteria (SRB), leading to the assumption that they are exclusively responsible for metal corrosion. In fact, methanogenic Archaea are known to be involved in metal corrosion as well (e.g. Methanococcus maripaludis DSM 2067). In some cases SRB and methanogenic Archaea have comparable high corrosion rates. However, the underlying mechanisms causing corrosion are still unknown.
The goal of this study is to develop suitable methods for analyzing two environmental isolates (M. maripaludis DSM 2067, M. maripaludis KA1) and two human-related isolates (Methanobrevibacter oralis and Methanobrevibacter smithii) for their ability to deteriorate/transform metals, which are relevant for technical and clinical applications. Moreover, the studies will provide essential information on the interaction mechanisms of human-related Archaea, which are frequently found in peri-implantitis, with dental material such as implants, crowns and bridges leading to their degradation and transformation.
Renewable resources become more and more relevant to maintain energy demands for an increasing global population. Biosynthetic fuels like biodiesel might replace conventional petrochemical fuels. In this study the influence of microbial growth on biodiesel and diesel on the storage tank systems were investigated. Polymeric fuel storage tanks for diesel and biodiesel provide suitable environmental conditions for a broad spectrum of fungi and various bacteria, including cyanobacteria and aerobic heterotrophic, and even anaerobic, fermentative Bacteria. However, the questions whether and how ageing of the materials is affected by biofouling processes have not been answered so far. Therefore, a model system for biofilm formation was established to study the initial attachment phase of bacteria in dependency of ageing, quality and surface modification of thermoplastic polymers used for storage tank systems. The microbial survey is closely connected with a detailed characterization of the material’s properties and its ageing processes.
A widely applied plastic used for fuel storage tanks is high-density polyethylene (PE-HD), which is available with various additives to increase UV-light stability and even for the storage of biodiesel. These materials were aged under UV-light and temperature using a defined climate chamber set-up. Further, the repeated filling of fuels was mimicked for such storage tanks, as this has an important impact on the life-cycle length for the storage Container. The aged polymers showed a significant change in the material’s characteristics, including surface characteristics (e.g. hydrophobicity) and carbonyl groups. The effect of the changed material properties on the biofilm formation are studied using bacterial isolates, previously obtained from a “dieselpest”, and as a model-reference E. coli. The unaged polymers showed already some significant differences for the initial attachment of E. coli K12. Polyethylene with additives was colonized faster than the reference material (without additives) although the final biofilm coverage was not impaired. Likewise, the settlement of a kerosene-isolated Bacillus species on the unaged materials independently of additives was only minor interfered.
In future, our results should give stakeholders in industry and public authorities a better estimation of the life-cycle security for fuel storage tank systems and on the fuel quality. Further, our results could help to test and develop new materials or additives to prevent biofouling processes.
Different environmental samples reveal that methanogenic Archaea are part of a
multi-species biofilm on corroding metallic structures (Fig. 1). Studies on microbial
influenced corrosion (MIC) focus mainly on sulphate reducing Bacteria (SRB),
leading to the assumption that they are exclusively responsible for metal corrosion.
In fact, methanogenic Archaea are known to be involved in metal corrosion as well
(e.g.Methanococcus maripaludis DSM 2067). In some cases SRB and methanogenic
Archaea have comparable high corrosion rates. However, the underlying
mechanisms causing corrosion are still unknown. The goal of this study is to
analyse two environmental isolates (M. maripaludis DSM 2067, M. maripaludis
KA1) and two human-related isolates (Methanobrevibacter oralis and
Methanobrevibacter smithii) for their ability to deteriorate/transform metals,
which are relevant for technical and clinical applications. Moreover, the studies will
provide essential information on the interaction mechanisms of human-related
Archaea, which are frequently found in peri-implantitis, with dental material such
as implants, crowns and bridges leading to their degradation/transformation.
Soil formation on weathering rock surfaces is intrinsically connected with the development of primary microbial colonization at the atmosphere-lithosphere interface. A great number and variety of microorganisms is involved in these microbial communities, which are dominated by fungi, algae, cyanobacteria and heterotrophic bacteria. Rock-inhabiting life is ubiquitous on rock surfaces all around the world, but the laws of its establishment, and more important, quantification of its biodeterioration and geological input are possible only in well-controlled and simplified laboratory models. Here we would like to compare two model rock biofilm consisting of the heterotrophic and the phototrophic interacting partners. In the present work the growth of these model biofilms on diverse materials with different physical and chemical properties was investigated under well-controlled laboratory conditions. To clarify the role of environmental factors, the parameters temperature, light intensity and relative humidity were varied in growth test series. For an accelerated substrate colonization and to increase the biomass yield different flow-through chambers systems with semi-continuous cultures have been applied, simulating weathering conditions like flooding, desiccation and nutrient input. The biofilm development was studied by (i) confocal laser scanning and electron microscopy and (ii) qualitatively and quantitatively with respect to cell forms and biomass. A correlation between the presence of the model biofilm and mineral surface alteration as well as geochemical tracers of weathering were followed on various rock substrates (with differing geochemistry, porosity etc) exposed in another flow-through chamber, filled with crushed rock material. Under mentioned environmental conditions different types of flow-through chambers have been used and will be compared.
Simple, microbial biofilms have prevailed since life began on Earth. Biofilms form at the interfaces of solids with gases or liquids and have multiple effects on Substrate and element cycles. In geobiological terms, the most interesting microbial communities are those that form on solids exposed to air (subaerial). Microbial colonisers of the atmosphere-lithosphere interface include algae, cyanobacteria, fungi as well as heterotrophic bacteria and they have colonised virtually every rock surface throughout the entire geological history of the Earth. In addition to sequestering carbon, sub-aerial biofilms (SABS) actively participate in rock weathering. Rock-inhabiting SABs are the primary settlers on lava following volcanic eruptions and on rocks following the retreat of glaciers. SABs especially dominate hostile environments in which growth of higher Vegetation is restricted especially in deserts, polar- and alpine regions. SABs are the primary colonisers of lithospheric (e.g. rocks) and anthropogenic Substrates (buildings, monuments, solar panels, etc.). Life at the solid material/atmosphere interface influences and is affected by both the underlying Substrate and the microclimate surrounding it. Although subaerial life is ubiquitous, how SABs develop and importantly degrade underlying Substrates can only be clarified in well-controlled experiments that often involve simplified model Systems, So far, biofilm development on solar panels has been studied using; (i) metagenomics; (ii) in situ microscopy; and (iii) classical microbiological methods that are both qualitative and quantitative. Here we suggest that solar panel biofilms are accessible and highly relevant objects to study microbial ecology, geobiology and biodeterioration.
Different environmental samples reveal that methanogenic Archaea are part of a multi-species biofilm on corroding metallic structures (Fig. 1). Studies on microbial influenced corrosion (MIC) focus mainly on sulphate reducing Bacteria (SRB), leading to the assumption that they are exclusively responsible for metal corrosion. In fact, methanogenic Archaea are known to be involved in metal corrosion as well (e.g. Methanococcus maripaludis DSM 2067). In some cases SRB and methanogenic Archaea have comparable high corrosion rates. However, the underlying mechanisms causing corrosion are still unknown. The goal of this study is to analyse two environmental isolates (M. maripaludis DSM 2067, M. maripaludis KA1) and two human-related isolates (Methanobrevibacter oralis and Methanobrevibacter smithii) for their ability to deteriorate/transform metals, which are relevant for technical and clinical applications. Moreover, the studies will provide essential information on the interaction mechanisms of human-related Archaea, which are frequently found in peri-implantitis, with dental material such as implants, crowns and bridges leading to their degradation/ transformation.
Materials are subject to environmental constraints that include biological, chemical and physical factors. To gain confidence about durability and long-term performance of any material, environmental resistance testing procedures have to be amended with modern simulation procedures that include biological components. In fact, any environmentally exposed surface at temperatures lower than 121 °C will be home to microbial growth, even at high salt concentrations, extreme pH, environmental pollution, low water potential, and intense irradiation – everywhere where water is liquid and available. As a consequence, complex microbial ecosystems called biofilms are self-sufficient and found on almost all solid-air-water interfaces. Obviously, environmental changes perturb biofilm development but over a number of seasons, these changes result in relatively stable microbial communities peculiar and adapted to a particular niche and material. Certain microbial settlers are indicative of, and in a real sense mark, a particular biofilm and can, thus, be considered as “reference organisms”. Characteristic reference organisms’ peculiar to specific material-inhabiting communities can be isolated, identified, characterised and used in standard test procedures as well as research into materials science (materials improvement). In this presentation classical microbiological, genetic and molecular methods for studying reference organisms and their roles in materials deterioration will be presented. We will present a set of different reference organisms that are currently in focus of our research and testing development.