TY - JOUR A1 - Mallikarjun, Jhenkhar A1 - Gorbushina, Anna A1 - Kuzyakov, Yakov A1 - Koester, Moritz A1 - Castro, Rodrigo A1 - Yudina, Anna A1 - Abdallah, Khaled A1 - Matus, Francisco J. A1 - Dippold, Michaela A. T1 - Post-fire recovery of temperate and mediterranean ecosystems: An interplay between fire severity, soil nutrients, and vegetation from early-stage to decadal-scale dynamics N2 - Wildfires strongly alter soil properties, which in turn affect ecosystem recovery over extended periods, though long-term impacts are less certain. This study investigated a 14-year post-fire chronosequence in Chile’s mediterranean and temperate humid forests, revealing ecosystem-specific soil properties and nutrient recovery mechanisms. By analysing sites at successional stages, the chronosequence approach assessed temporal changes and ecosystem recovery, revealing long-term wildfire effects on soil dynamics and nutrients recovery. Wildfires raised soil bulk density to 0.9 g cm−3 in humid temperate and 1.2 g cm−3 in mediterranean ecosystems. Mediterranean soils experienced greater compaction from organic matter loss, soil aggregate destruction, ash-clogged pores, and topsoil erosion. Soil texture shifts were ecosystem-dependent: mediterranean soils increased 10–12 % in clay and silt through ash redistribution and aggregation, while temperate soils saw sand content rise by 0.74 % and 0.32 % yearly at 0–5 and 5–10 cm depths from thermal disaggregation and erosion. Ground vegetation recovers quickly, but physical soil properties like bulk density require over 14 years to return to pre-fire conditions. In humid temperate forests, ash input initially increased soil pH (4.8 to 5.8), reducing acidity, mitigating aluminium toxicity, while increasing nutrient availability. Base cation stocks increased in mediterranean woodlands (e.g., Ca: up to 0.41 Mg ha−1 y−1) due to ash retention, lower leaching, and ash infiltration into subsoil. Nutrient stocks in humid forests recovered slowly (Ca: 0.087–0.13 Mg ha−1 y−1) due to rainfall-driven leaching and low subsoil reserves. Carbon and N losses were restricted to the litter horizon in temperate forests, recovering via fire-resistant tree inputs, whereas mediterranean soils suffered severe C and N depletion from vegetation loss, erosion, and low N fixation. Fire effects and recovery are ecosystem-specific, shaped by landscape, geology, hydrology, and vegetation resilience. Understanding how fire regimes affect soil and nutrient recovery is vital for improving projections in fire-prone regions. KW - Historical fire & Wildfire KW - Nutrients Ecosystem recovery & Vegetation succession KW - Chronosequence approach KW - Losses of nutrients & Nutrients stocks KW - Wildfire PY - 2025 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-642918 DO - https://doi.org/10.1016/j.catena.2025.109431 SN - 0341-8162 VL - 260 SP - 1 EP - 13 PB - Elsevier B.V. AN - OPUS4-64291 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Martin-Sanchez, Pedro Maria A1 - Gorbushina, Anna A1 - Toepel, Jörg T1 - Quantification of microbial load in diesel storage tanks using culture- and qPCR-based approaches N2 - Microbial contamination of fuels, associated with a wide variety of bacteria and fungi, leads to decreased product quality and can compromise equipment performance by biofouling and microbiologically influenced corrosion of pipelines and storage tanks. Detection and quantification of biomass are critical in monitoring fuel systems for an early detection of microbial outbreaks. The aims of this study are (i) to quantify bacterial and fungal contamination in samples from diesel storage tanks of petrol stations, using both culture dependent- and culture independent (qPCR) approaches, and (ii) to analyse the diversity of cultivable diesel-contaminating microorganisms with the purpose to create a strain collection for further use in biodeterioration experiments. Both methodological approaches revealed a high microbial contamination in all studied samples, with the bacterial load being much higher than the fungal load. The diversity of cultivable microorganisms was rather low. Based on criteria of abundance and fuel degradation potential, the most relevant microorganisms were identified as bacteria of genera Bacillus, Citrobacter, Burkholderia and Acetobacter, the filamentous fungi Paecilomyces variotii and Pseudallescheria boydii, and a Dipodascaceae yeast. Furthermore the validity and utility of qPCR-based methods are discussed. KW - Fuel contamination KW - Biofouling KW - Cultivation KW - Real-time qPCR KW - Bacteria KW - Fungi PY - 2016 DO - https://doi.org/10.1016/j.ibiod.2016.04.009 SN - 0964-8305 SN - 1879-0208 VL - 126 SP - 216 EP - 223 PB - Elsevier Ltd. AN - OPUS4-41260 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - CONF A1 - Gorbushina, Anna T1 - Studying colonization of stone surfaces – what can we learn from model biofilms growing in flow-through chambers? N2 - 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. T2 - Technoheritage CY - Cadiz, Spain DA - 21.05.2017 KW - Biofilm KW - Biodeterioration PY - 2017 AN - OPUS4-41136 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Toepfer, I. A1 - Favet, J. A1 - Schulte, A. A1 - Schmölling, M. A1 - Butte, W. A1 - Triplett, E.W. A1 - Broughton, W.J. A1 - Gorbushina, Anna T1 - Pathogens as potential hitchhikers on intercontinental dust N2 - Desert dust seeds distant lands and waters with minerals as well as micro-organisms raising the question of whether this ancient phenomenon also spreads pathogens across the globe. Severe dust storms require strong winds blowing over land-masses that are largely devoid of vegetation, effectively limiting the scope for winds to raise pathogens into the air. Nevertheless, changing patterns of land-use, often driven by belligerency, result in refugees spreading to areas that were previously deemed barely habitable. With the help of the International Committee of the Red Cross, a number of sand/dust samples were collected from the Republic of Chad, some near refugee camps, others further removed from human influence. In parallel studies, we documented the micro-organisms present in these samples and used a number of the isolates here to test the effect of environmental constraints on their ability to survive intercontinental flight. We also added traditional pathogens to the palette of microbes and tested the effects of UV irradiation, desiccation and temperature on survival of both bacteria and fungi. A clear trend was obvious—those microbes that are coloured or able to form conidia or spores (in other words, those that are native to deserts) were well able to resist the imposed stresses. On the other hand, most pathogens were more sensitive to stresses than the environmental isolates. Toxin production in two species of Aspergillus was also investigated. Short-term desiccation (simulating environmental conditions during intercontinental travel) of sand amended with fungal spores containing sterigmatocystin leads to increased mycotoxin contents, but significant mycotoxin production was only possible under growth-permissive conditions, e.g. at higher humidity. It thus seems likely that an ever-decreasing fraction of the initial pathogen load survives as the dust recedes from its desert source and that those organisms that land on other continents are highly enriched in desert dwellers. KW - Chad KW - Desert sand KW - Sterigmatocystin KW - Aspergillus sydowii KW - A. versicolor PY - 2012 DO - https://doi.org/10.1007/s10453-011-9230-2 SN - 0393-5965 SN - 1573-3025 VL - 28 IS - 2 SP - 221 EP - 231 PB - Springer Science + Business Media B.V. CY - Dordrecht [u.a.] AN - OPUS4-24814 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - CONF A1 - Gorbushina, Anna T1 - Life on the rocks and other hard surfaces N2 - After their discovery on rock surfaces in cold and hot deserts, a polyphyletic group of ascomycetous black fungi was found to dominate a range of hostile environments – natural and man-made, from salterns to dishwashers, roofs and solar panels. Together with bacteria and algae they may establish subaerial biofilms and cause weathering of the surfaces they grow on. Their impressive survival abilities as well as their constitutive protective pigmentation and cluster-like microcolony organisation are similar in environmental isolates as well as in heat-tolerant opportunistic pathogens of animals and humans. We selected the rock-inhabiting fungus Knufia petricola (class Eurotiomycetes, order Chaetothyriales) that exhibits all the characteristics of microcolonial black fungi such as yeast-like cell growth, absence of reproductive structures and constitutive dihydroxynaphthalene (DHN) melanogenesis (Nai et al. 2013, Fungal Genet Biol). We developed protocols to efficiently generate and transform protoplasts resulting in stable homokaryotic transformants by targeting genes involved in pigment synthesis. The differences between the wild-type fungus and its melanin-deficient mutants were tested in geomicrobiological experiments and measured are now discussed in detail, with special accent on the possible effects of the mutation on EPS and other exuded substances. T2 - Departmental colloquium of the Tuscia University CY - Viterbo, Italy DA - 14.02.2020 KW - Ascomycetes KW - Fungal biofilms KW - Material surface colonisation KW - Genetics KW - Genomics KW - Extremophilic fungi PY - 2020 AN - OPUS4-50643 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Montero-Calasanz, M.C. A1 - Göker, M. A1 - Pötter, G. A1 - Rohde, M. A1 - Spröer, C. A1 - Schumann, P. A1 - Gorbushina, Anna A1 - Klenk, H.-P. T1 - Geodermatophilus arenarius sp. nov., a xerophilic actinomycete isolated from Saharan desert sand in Chad N2 - A novel Gram-positive, aerobic, actinobacterial strain, CF5/4T, was isolated in 2007 during an environmental screening of arid desert soil in Ouré Cassoni, Chad. The isolate grew best in a temperature range of 28–40 °C and at pH 6.0-8.5, with 0-1 % (w/v) NaCl, forming brown-coloured and nearly circular colonies on GYM agar. Chemotaxonomic and molecular characteristics of the isolate matched those described for members of the genus Geodermatophilus. The DNA G + C content of the novel strain was 75.9 mol %. The peptidoglycan contained meso-diaminopimelic acid as diagnostic diaminoacid. The main phospholipids were phosphatidylethanolamine, phosphatidylcholine, phosphatidylinositol, diphosphatidylglycerol and a small amount of phosphatidylglycerol; MK-9(H4) was identified as the dominant menaquinone and galactose as diagnostic sugar. The major cellular fatty acids were branched-chain saturated acids: iso-C15:0 and iso-C16:0. The 16S rRNA gene showed 96.2–98.3 % sequence identity with the three members of the genus Geodermatophilus: G. obscurus (96.2 %), G. ruber (96.5 %), and G. nigrescens (98.3 %). Based on the chemotaxonomic results, 16S rRNA gene sequence analysis and DNA–DNA hybridization with the type strain of G. nigrescens, the isolate is proposed to represent a novel species, Geodermatophilus arenarius (type strain CF5/4T = DSM 45418T = MTCC 11413T = CCUG 62763T). KW - Xerophiles KW - Actinomycetes KW - Geodermatophilaceae KW - Taxonomy KW - Sahara desert PY - 2012 DO - https://doi.org/10.1007/s00792-012-0486-4 SN - 1431-0651 SN - 1433-4909 VL - 16 IS - 6 SP - 903 EP - 909 PB - Springer CY - Tokyo AN - OPUS4-26933 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Montero-Calasanz, M.d.C. A1 - Göker, M. A1 - Pötter, G. A1 - Rohde, M. A1 - Spröer, C. A1 - Schumann, P. A1 - Gorbushina, Anna A1 - Klenk, H.-P. T1 - Geodermatophilus africanus sp. nov., a halotolerant actinomycete isolated from Saharan desert sand N2 - A novel Gram-strain positive, aerobic, actinobacterial strain, designated CF11/1T, was isolated from a sand sample obtained in the Sahara Desert, Chad. The black-pigmented isolate was aerobic and exhibited optimal growth from 25 to 35 °C at pH 6.0–8.0 and with 0–8 % (w/v) NaCl, indicating that it is a halotolerant mesophile. Chemotaxonomic and molecular characteristics of the isolate matched those described for members of the genus Geodermatophilus. The G+C content in the genome was 74.4 mol%. The peptidoglycan contained meso-diaminopimelic acid as diagnostic diaminoacid. The main phospholipids were diphosphatidylglycerol, phosphatidylcholine, phosphatidylethanolamine, phosphatidylinositol and a minor fraction of phosphatidylglycerol; MK-9(H4) was the dominant menaquinone, and galactose was detected as a diagnostic sugar. The major cellular fatty acid was branched-chain saturated acid iso-C16:0. Analysis of 16S rRNA gene sequences showed 95.3–98.6 % pairwise sequence identity with the members of the genus Geodermatophilus. Based on phenotypic and chemotaxonomic properties, as well as phylogenetic distinctiveness, the isolate represents a novel species, Geodermatophilus africanus, with the type strain CF11/1T (DSM 45422 = CCUG 62969 = MTCC 11556). KW - Actinomycetes KW - Geodermatophilaceae KW - Taxonomy KW - Osmotolerant KW - Phenotype microarray PY - 2013 DO - https://doi.org/10.1007/s10482-013-9939-8 SN - 0003-6072 SN - 1572-9699 VL - 104 IS - 2 SP - 207 EP - 216 PB - Springer CY - Dordrecht AN - OPUS4-28868 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - CONF A1 - Gorbushina, Anna T1 - Some like it on the rocks: mineral-weathering fungi with manifold protective pigments N2 - The interface between materials and the environment is populated by microorganisms which organize on surfaces to form specially adapted and resistant microbial associations, so-called biofilms. Surface-bound biofilm growth is associated with substantial secretion of metabolic products that can significantly influence material corrosion. Here, a group of material-inhabiting fungi are presented, which colonize and weather air-exposed materials such as building façades, roofs and solar systems. A selected model fungus is used to carry out genetic and molecular biology experiments, which are microbiologically cutting-edge and allow for the development of novel time-saving techniques for material testing. The degree of material damage under the influence of this model fungus shows a measure of the aggressiveness of the biofilm under defined environmental conditions - and thus explores fundamental components of the interaction between material and biofilm. T2 - GZMB-Kolloquium Mikrobiologie/Genetik CY - Göttingen, Germany DA - 05.07.2016 KW - Microcolonial fungi KW - Sub-aerial biofilms KW - Knufia petricola PY - 2016 AN - OPUS4-37381 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Catanzaro, Ilaria A1 - Gerrits, Ruben A1 - Feldmann, Ines A1 - Gorbushina, Anna A1 - Onofri, Silvano A1 - Schumacher, Julia T1 - Deletion of the polyketide synthase‐encoding gene pks1 prevents melanization in the extremophilic fungus Cryomyces antarcticus N2 - Cryomyces antarcticus, a melanized cryptoendolithic fungus endemic to Antarctica, can tolerate environmental conditions as severe as those in space. Particularly, its ability to withstand ionizing radiation has been attributed to the presence of thick and highly melanized cell walls, which—according to a previous investigation—may contain both 1,8‐dihydroxynaphthalene (DHN) and L‐3,4 dihydroxyphenylalanine (L‐DOPA) melanin. The genes putatively involved in the synthesis of DHN melanin were identified in the genome of C. antarcticus. Most important is capks1 encoding a non‐reducing polyketide synthase (PKS) and being the ortholog of the functionally characterized kppks1 from the rock‐inhabiting fungus Knufia petricola. The co‐expression of CaPKS1 or KpPKS1 with a 4′‐phosphopantetheinyl transferase in Saccharomyces cerevisiae resulted in the formation of a yellowish pigment, suggesting that CaPKS1 is the enzyme providing the precursor for DHN melanin. To dissect the composition and function of the melanin layer in the outer cell wall of C. antarcticus, non‐melanized mutants were generated by CRISPR/Cas9‐mediated genome editing. Notwithstanding its slow growth (up to months), three independent non‐melanized Δcapks1 mutants were obtained. The mutants exhibited growth similar to the wild type and a light pinkish pigmentation, which is presumably due to carotenoids. Interestingly, visible light had an adverse effect on growth of both melanized wild‐type and non‐melanized Δcapks1 strains. Further evidence that light can pass the melanized cell walls derives from a mutant expressing a H2B‐GFP fusion protein, which can be detected by fluorescence microscopy. In conclusion, the study reports on the first genetic manipulation of C. antarcticus, resulting in non‐melanized mutants and demonstrating that the melanin is rather of the DHN type. These mutants will allow to elucidate the relevance of melanization for surviving extreme conditions found in the natural habitat as well as in space. KW - Astrobiology KW - Black fungi KW - CRISPR/Cas9 KW - DHN melanin KW - Cryptoendolithism PY - 2024 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-606599 DO - https://doi.org/10.1002/iub.2895 SN - 1521-6551 VL - 76 IS - 12 SP - 1072 EP - 1090 PB - Wiley AN - OPUS4-60659 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Erdmann, Eileen A1 - Nitsche, Sarah A1 - Gorbushina, Anna A1 - Schumacher, Julia T1 - Genetic Engineering of the Rock Inhabitant Knufia petricola Provides Insight Into the Biology of Extremotolerant Black Fungi N2 - Black microcolonial fungi (Ascomycetes from Arthonio-, Dothideo-, and Eurotiomycetes) are stress-tolerant and persistent dwellers of natural and anthropogenic extreme habitats. They exhibit slow yeast-like or meristematic growth, do not form specialized reproduction structures and accumulate the black pigment 1,8-dihydroxynaphthalene (DHN) melanin in the multilayered cell walls. To understand how black fungi live, survive, colonize mineral substrates, and interact with phototrophs genetic methods are needed to test these functions and interactions. We chose the rock inhabitant Knufia petricola of the Chaetothyriales as a model for developing methods for genetic manipulation. Here, we report on the expansion of the genetic toolkit by more efficient multiplex CRISPR/Cas9 using a plasmid-based system for expression of Cas9 and multiple sgRNAs and the implementation of the three resistance selection markers genR (geneticin/nptII), baR (glufosinate/bar), and suR (chlorimuron ethyl/sur). The targeted integration of expression constructs by replacement of essential genes for pigment synthesis allows for an additional color screening of the transformants. The black-pink screening due to the elimination of pks1 (melanin) was applied for promoter studies using GFP fluorescence as reporter. The black-white screening due to the concurrent elimination of pks1 and phs1 (carotenoids) allows to identify transformants that contain the two expression constructs for co-localization or bimolecular fluorescence complementation (BiFC) studies. The co-localization and interaction of the two K. petricola White Collar orthologs were demonstrated. Two intergenic regions (igr1, igr2) were identified in which expression constructs can be inserted without causing obvious phenotypes. Plasmids of the pNXR-XXX series and new compatible entry plasmids were used for fast and easy generation of expression constructs and are suitable for a broad implementation in other fungi. This variety of genetic tools is opening a completely new perspective for mechanistic and very detailed study of expression, functioning and regulation of the genes/proteins encoded by the genomes of black fungi. KW - Microcolonial fungi KW - DHN melanin KW - Cloning vectors KW - Genetics PY - 2022 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-546192 DO - https://doi.org/10.3389/ffunb.2022.862429 SN - 2673-6128 VL - 3 PB - Frontiers Media CY - Lausanne AN - OPUS4-54619 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Abdallah, Khaled A1 - Stock, S. C. A1 - Heeger, Felix A1 - Koester, M. A1 - Nájera, F. A1 - Merino, C. A1 - Spielvogel, S. A1 - Gorbushina, Anna A1 - Kuzyakov, Y. A1 - Dippold, M. A. T1 - Nitrogen Gain and Loss Along an Ecosystem Sequence: From Semi-desert to Rainforest N2 - Plants and microorganisms, besides the climate, drive nitrogen (N) cycling in ecosystems. Our objective was to investigate N losses and N acquisition strategies along a unique ecosystem-sequence (ecosequence) ranging from arid shrubland through Mediterranean woodland to temperate rainforest. These ecosystems differ in mean annual precipitation, mean annual temperate, and vegetation cover, but developed on similar granitoid soil parent material, were addressed using a combination of molecular biology and soil biogeochemical tools. Soil N and carbon (C) contents, δ15N signatures, activities of N acquiring extracellular enzymes as well as the abundance of soil bacteria and fungi, and diazotrophs in bulk topsoil and rhizosphere were determined. Relative fungal abundance in the rhizosphere was higher under woodland and forest than under shrubland. This indicates toward plants' higher C investment into fungi in the Mediterranean and temperate rainforest sites than in the arid site. Fungi are likely to decompose lignified forest litter for efficient recycling of litter-derived N and further nutrients. Rhizosphere—a hotspot for the N fixation—was enriched in diazotrophs (factor 8 to 16 in comparison to bulk topsoil) emphasizing the general importance of root/microbe association in N cycle. These results show that the temperate rainforest is an N acquiring ecosystem, whereas N in the arid shrubland is strongly recycled. Simultaneously, the strongest 15N enrichment with decreasing N content with depth was detected in the Mediterranean woodland, indicating that N mineralization and loss is highest (and likely the fastest) in the woodland across the continental transect. Higher relative aminopeptidase activities in the woodland than in the forest enabled a fast N mineralization. Relative aminopeptidase activities were highest in the arid shrubland. The highest absolute chitinase activities were observed in the forest. This likely demonstrates that (a) plants and microorganisms in the arid shrubland invest largely into mobilization and reutilization of organically bound N by exoenzymes, and (b) that the ecosystem N nutrition shifts from a peptide-based N in the arid shrubland to a peptide- and chitin-based N nutrition in the temperate rainforest, where the high N demand is complemented by intensive N fixation in the rhizosphere. KW - Nitrogen KW - Rhizosphere KW - Microbial abundance KW - Natural abundance of 15N KW - Nitrogen fixation KW - Nitrogen uptake PY - 2022 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-543708 DO - https://doi.org/10.3389/fsoil.2022.817641 SN - 2673-8619 VL - 2 SP - 1 EP - 14 PB - Frontiers Media CY - Lausanne AN - OPUS4-54370 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Ruibal, C. A1 - Gueidan, C. A1 - Selbmann, L. A1 - Gorbushina, Anna A1 - Crous, P.W. A1 - Groenewald, J.Z. A1 - Muggia, L. A1 - Grube, M. A1 - Isola, D. A1 - Schoch, C.L. A1 - Staley, J.T. A1 - Lutzoni, F. A1 - De Hoog, G.S. T1 - Phylogeny of rock-inhabiting fungi related to Dothideomycetes N2 - The class Dothideomycetes (along with Eurotiomycetes) includes numerous rock-inhabiting fungi (RIF), a group of ascomycetes that tolerates surprisingly well harsh conditions prevailing on rock surfaces. Despite their convergent morphology and physiology, RIF are phylogenetically highly diverse in Dothideomycetes. However, the positions of main groups of RIF in this class remain unclear due to the lack of a strong phylogenetic framework. Moreover, connections between rock-dwelling habit and other lifestyles found in Dothideomycetes such as plant pathogens, saprobes and lichen-forming fungi are still unexplored. Based on multigene phylogenetic analyses, we report that RIF belong to Capnodiales (particularly to the family Teratosphaeriaceae s.l.), Dothideales, Pleosporales, and Myriangiales, as well as some uncharacterised groups with affinities to Dothideomycetes. Moreover, one lineage consisting exclusively of RIF proved to be closely related to Arthoniomycetes, the sister class of Dothideomycetes. The broad phylogenetic amplitude of RIF in Dothideomycetes suggests that total species richness in this class remains underestimated. Composition of some RIF-rich lineages suggests that rock surfaces are reservoirs for plant-associated fungi or saprobes, although other data also agree with rocks as a primary substrate for ancient fungal lineages. According to the current sampling, long distance dispersal seems to be common for RIF. Dothideomycetes lineages comprising lichens also include RIF, suggesting a possible link between rock-dwelling habit and lichenisation. KW - Arthoniomycetes KW - Capnodiales KW - Dothideomycetes KW - Evolution KW - Extremotolerance KW - Multigene phylogeny KW - Rock-inhabiting fungi PY - 2009 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-219821 DO - https://doi.org/10.3114/sim.2009.64.06 SN - 0166-0616 VL - 64 IS - 1 SP - 123 EP - 133 PB - Centraalbureau voor Schimmelcultures CY - Utrecht, The Netherlands AN - OPUS4-21982 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Gerrits, Ruben A1 - Pokharel, R. A1 - Breitenbach, Romy A1 - Radnik, Jörg A1 - Feldmann, Ines A1 - Schuessler, J.A. A1 - von Blanckenburg, F. A1 - Gorbushina, Anna A1 - Schott, J. T1 - How the rock-inhabiting fungus K. petricola A95 enhances olivine dissolution through attachment N2 - Free-living and mycorrhizal fungi are able to enhance the weathering of rock and other solid substrates. Deciphering the exact mechanisms of these natural processes requires their experimental simulation. Moreover, by performing these simulations with genetically amenable rock-weathering fungi, one can knock-out certain fungal traits and consequently identify their weathering-relevant function. Here, the effect of the rock-inhabiting fungus, Knufia petricola A95, on the dissolution kinetics of an Fe-bearing olivine (Mg1.86Fe0.19SiO4) is investigated at 25 °C and pH 6 using reproducible batch and mixed flow experiments. The availability of a melanin-deficient mutant (ΔKppks) of K. petricola A95, which produces more extracellular polymeric substances (EPS) than the wild type (WT), enables the comparative study of the role of melanin and EPS in olivine dissolution. In abiotic dissolution experiments, the olivine dissolution rate decreased considerably over time at pH 6 but not at pH 3.5. This inhibition of abiotic olivine dissolution at pH 6 was most likely caused by the in-situ oxidation of ferrous Fe and/or the precipitation of ferric hydroxides at the olivine surface. In corresponding biotic experiments at pH 6, both the wild type K. petricola and its melanin-deficient mutant ΔKppks solubilised and bound significant amounts of Fe released by olivine dissolution. Fe oxidation and precipitation were thus prevented and olivine dissolution proceeded faster than in the abiotic experiments. By sequestering Fe directly at the olivine surface, the attached wild type K. petricola cells were particularly efficient at preventing the oxidation of Fe at the mineral surface: the slowdown of olivine dissolution almost completely disappeared. The attachment capacity of these wild type cells is most likely mediated by wild type-specific EPS. Our presented experimental systems allow the oxidation of mineral-released Fe and include a rock-inhabiting fungus, thus simulating chemical, physical and biological conditions that set dissolution rates in a way that is relevant to natural ecosystems. KW - Black fungi KW - Bio-weathering KW - Forsterite KW - Knock-out mutant KW - Extracellular polymeric substances KW - Melanin Adhesion PY - 2020 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-509332 DO - https://doi.org/10.1016/j.gca.2020.05.010 VL - 282 SP - 76 EP - 97 PB - Elsevier Ltd. AN - OPUS4-50933 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - CONF A1 - Fuentes, Elsa A1 - Prieto, Beatriz A1 - Gorbushina, Anna T1 - Mixed model biofilm: interactions between algae, fungi and cyanobacteria and their effects on granite biodeterioration N2 - Granite, despite being one of the most widely used rocks for building material cultural heritage, is also one of the least studied. Previous works have shown that environmental parameters modulated by climate change will lead to changes in the microbial composition of biofilms grown on stone, but also to changes in the production of EPS, in the composition of pigments and, as a consequence, in the biodeterioration processes that this rock undergoes (Fuentes, 2023). Considering that the colonisation process is highly dynamic, small changes in climatic conditions can lead to the formation of different types of biofilms and diverse interactions between species. Knowing the contribution of the different organisms to the deterioration process is important both to anticipate the consequences that climate change will have on the deterioration of the granite, but also when addressing the processes of recolonization after cleaning, to ensure an improvement of the present situation. So, in order to continue my line of research on granite biodeterioration, the aim of this new project is to study the contribution of each type of organism (green algae, cyanobacteria and fungi) to the process of granite deterioration as well as the specific effect on each mineral, in addition to its role in the resilience and response of biofilms to environmental changes. With this main objective, the effect of the type of substrate on the composition of a model mixed biofilm formed by the fungus Knufia petricola, the algae Jaagichlorella sp. and the cyanobacterium Synechocystis sp. will be studied. The results obtained on granite will be compared with those obtained with other lithic types such as marble or limestone. Furthermore, it will be observed if the different ratios between organisms lead to changes in the capacity of these organisms to generate biodeterioration and to buffer climatic changes. Finally, the susceptibility of each mineral that makes up the granite - quartz, feldspars, micas - to biodeterioration mediated by each type of organism will be analysed. To address these questions, on the one hand, the response of the mixed biofilms as a whole will be evaluated by means of confocal microscopy, PAM, as well as the quantification of pigments and EPS, and on the other hand, the effect of these organisms on the deterioration of the substrates, through the use of SEM and TEM, which will allow the assessment of both the changes in porosity and the appearance of deterioration in the surface layers of the rock. This research will deepen the knowledge of the processes of granite deterioration, which have been limitedly studied in relation to microorganisms; but also aims to provide the scientific community with a model mixed biofilm to increase the reproducibility between experiments, one of the main limitations of this field of study. T2 - 19th International Biodeterioration and Biodegradation Symposium CY - Berlin, Germany DA - 09.09.2024 KW - Biofilm KW - Stone KW - Algae KW - Fungi KW - Cyanobacteria KW - Cultural heritage PY - 2024 AN - OPUS4-62272 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER -