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Schleper, C.

Publications and source records attributed to Schleper, C..

At least 19 recordsLinked to original sources

Emergence of histone-based chromatin complexity in Asgard archaea

The emergence of the eukaryotes coincided with the diversification of histone proteins and their post-translational modifications by enzymes that constitute the core of eukaryotic chromatin. Yet the evolutionary origins of this regulatory machinery are unknown. Here, we show that the key molecular components of histone-based chromatin regulation are present in the Asgard archaea, the closest prokaryotic relatives of eukaryotes. Asgard histones are abundant and have extended N-terminal tails rich in lysine residues that can be post-translationally modified, all of which are features shared with eukaryotic histones. In line with these findings, we identify enzymes from Asgard archaea that deposit or remove lysine acetylation on histone tails in vitro. Moreover, Asgard sirtuin deacetylases (SIR2 proteins) restore chromatin silencing in yeast, demonstrating the functional compatibility of Asgard enzymes with eukaryotic histone substrates. Our findings establish that the foundations of histone-based chromatin predate eukaryogenesis and place Asgard archaea as an evolutionary intermediate in the emergence of eukaryotic chromatin.

evolutionary biology↗

Biofilm Lifestyle Drives Ecophysiological Niche Expansion in an Archaeal Soil Nitrifier

As key drivers of nitrification, ammonia-oxidizing archaea (AOA) play a central role in the global nitrogen cycle and contribute significantly to the emissions of the potent greenhouse gas nitrous oxide (N2O). However, the ecological implications of AOA growth as biofilms, remain poorly understood. Since nitrite production can be used to follow cellular activities directly we were able to compare biofilms with planktonic cells of the terrestrial model AOA Nitrososphaera viennensis at ecologically and agriculturally relevant conditions. Biofilms were more resistant across nearly all tested conditions and remained active at lower temperatures, acidic pH, and high ammonium concentrations. Collectively, activities in biofilm help reconcile discrepancies between earlier laboratory and environmental observations of soil AOA. Additionally, biofilms showed a high general resilience and lowered sensitivities to nitrification inhibitors. Although in situ biofilms grown in microrespiratory chambers exhibited activity and ammonia affinity similar to planktonic cells, biofilm cultures produced only half as much N2O. The enhanced fitness of biofilms across all tested conditions vastly expands the potential ecophysiological niche of AOA and supports the hypothesis that biofilm growth represents the in situ phenotype of AOA in soil environments.

microbiology↗

Common nitrification inhibitors exhibit varied physiological mechanisms on an ammonia-oxidizing microorganism

Microbial ammonia oxidation, the first and rate-limiting step of nitrification, plays a central role in soil nitrogen cycling. It is most relevant in agricultural soils as nitrifiers compete with crops for ammonia-based fertilizers. Therefore, synthetic nitrification inhibitors are widely used alongside fertilizers to reduce the activities of dominant drivers of this process, i.e. ammonia-oxidizing archaea (AOA) and bacteria (AOB). However, the physiological responses of ammonia oxidizers remain poorly resolved. Here the response of the AOA Nitrososphaera viennensis to the nitrification inhibitors 3,4-dimethylpyrazole phosphate (DMPP) and allylthiourea (ATU) were investigated using a combination of functional genomics, physiological assays, and relief experiments. The results overturn earlier assumptions that DMPP and ATU act by chelating free copper. Both compounds affected ammonia oxidation and triggered broader shifts in energy metabolism and stress-response pathways, which diverged markedly between the two inhibitors. We propose a competitive inhibition of the ammonia monooxygenase complex with DMPP as it can be alleviated by additional ammonia and elicits activation of urea acquisition, while ATU acted as a non-competitive inhibitor generally inducing quiescence. Both modes of inhibition were associated with clear transcriptomic and proteomic signals that will be advantageous for the identification of mechanisms of other nitrification inhibitors in the future. Key word: Ammonia-oxidizing archaea, nitrification, nitrification inhibitors, archaea, nitrogen cycle

microbiology↗

Active virus-host system in a Lokiarchaeon culture

Asgard archaea are considered the closest prokaryotic relatives of eukaryotes and having a crucial role in eukaryogenesis. Only few organisms have been cultivated from this group and their viruses were previously described only through metagenomic reconstructions. Here, we report the first successful cultivation of an Asgard archaeal virus infecting a novel strain of Ca. Lokiarchaeum ossiferum B36. The 16 kbp integrated provirus is capable to excise and replicate independently leading to the formation of virus particles. Network analysis of shared protein clusters with other archaeal viruses places it in a new family, Fylgjaviridae. The host encodes a distinctive repertoire of antiviral defense systems, including Septu, Wadjet, and type II CBASS system, all different from the defense systems of the related strain Ca. L. ossiferum B35. Our cultures provide the first opportunity to study interactions of a virus-host system in Asgards and hold significant potential for developing genetic tools.

microbiology↗

Oxygen production as an electron overflow pathway in ammonia-oxidizing archaea

Ammonia-oxidizing archaea (AOA) are widespread in nature and contribute to global carbon and nitrogen cycling. Although their energy production is an aerobic process, AOA occur in environments of low oxygen and in fully anoxic zones. Recently, oxygen production under anoxic conditions was demonstrated, raising the hypothesis that this activity can sustain oxygen dependent ammonia oxidation. In the work presented here, Nitrososphaera viennensis produces high amounts of oxygen in anoxia in dependence of nitrite but not ammonia. Rather than conferring a physiological benefit, oxygen production impaired recovery from anoxia. Produced oxygen is mostly not consumed and therefore cannot sustain ammonia oxidation in the absence of external oxygen. Instead, it is tightly linked to the amount of available redox equivalents. These observations indicate that oxygen production represents a general physiological strategy for alleviating the potential accumulation of reactive intermediates in the ammonia oxidation pathway, analogous to nitrifier denitrification in ammonia-oxidizing bacteria. TeaserOxygen production in ammonia-oxidizing archaea is not an adaptation to anoxia, but rather an electron overflow pathway that is detectable in anoxic conditions.

microbiology↗

Dynamic protrusions mediate unique crawling motility in Asgard Archaea (Promethearchaeota)

Crawling motility is a hallmark of eukaryotic cells and requires a dynamic actin cytoskeleton, regulated adhesion, and spatially organized signalling pathways1-3. Asgard archaea (phylum Promethearchaeota) which are considered the closest known prokaryotic relatives of eukaryotes potentially encode these functions within their large set of eukaryotic signature proteins4-9. The few cultivated members show a complex cell morphology, consisting of a central cell body from which several protrusions extend, filled with an actin-based cytoskeleton10,11. Here, live cell microscopy of two organisms of the Loki- and Hodarchaea lineages10,12 showed that they dynamically and drastically change their cell shape on a minute time scale and grow and retract their extensive protrusions with a speed of 1.5 to 5.3 {micro}m/min, respectively. After adhering to a glass surface, cells employ their protrusions to undergo active crawling motion. In the presence of selected actin inhibitors however, the observed dynamics were arrested, suggesting a central role of actin in these processes. The observed cellular plasticity and motility are unique features among prokaryotes and might have been crucial for the emergence of the first eukaryotic cells that are thought to have formed through the association of a member of the Promethearchaeota and an alphaproteobacterium, the ancestor of mitochondria.

microbiology↗

Metabolic Response of a Chemolithoautotrophic Archaeon to Carbon Limitation

The ubiquitously distributed ammonia-oxidizing archaea generate energy from ammonia and build cell mass from inorganic carbon sources, thereby contributing to both the global nitrogen and carbon cycles. However, little is known about the regulation of their predicted core carbon metabolism. A thermodynamic model for Nitrososphaera viennensis was developed to estimate the consumption of inorganic carbon in relation to ammonia consumed for energy and was tested experimentally by growing cells in carbon-limited and excess conditions. A combined proteomic and metabolomic approach of the experimental conditions revealed distinct metabolic adaptation depending on the amount of carbon supplied, either in a catalase or pyruvate background as a reactive oxygen species scavenger. Integration of protein and metabolite dynamics revealed a cellular strategy under carbon limitation to maintain a pool of amino acids and an upregulation of proteins necessary for translation initiation to stay primed for protein synthesis. The combination of modelling and functional genomics fills gaps in the understanding of the central metabolism and its regulation in a chemolithoautotrophic, ammonia-oxidizing archaeon even in the absence of available genetic tools.

microbiology↗

A fast-track, high-throughput screening platform for biological nitrification inhibitors discovery based on soil relevant ammonia oxidizing strains

Nitrogen cycling is critical for ecosystem functioning, with nitrification playing a central role. Excessive nitrification, triggered by heavy nitrogen fertilisation, contributes to reduced nitrogen use efficiency, nitrate leaching, and nitrous oxide emissions. While synthetic nitrification inhibitors (SNIs) help reduce these impacts, their erratic performance and environmental risks have shifted focus to biological nitrification inhibitors (BNIs) as sustainable alternatives. In vitro bioassays with ammonia-oxidising microorganisms (AOM) are valuable for BNI discovery and research, but often have low throughput and rely on a limited number of mostly non-soil-relevant or genetically modified ammonia-oxidizing bacteria (AOB) strains, lacking validation with established BNIs. We present a refined fast-track, high-throughput assay for BNI screening, utilizing soil-relevant, ecophysiologically and phylogenetically diverse AOB (Nitrosospira multiformis, Nitrosomonas ureae, Nitrosomonas communis) and ammonia-oxidizing archaea (AOA) strains (Nitrososphaera viennensis, "Ca. Nitrosocosmicus franklandianus"), achieving consistent cellular activity and density. The assay was validated with established SNIs and BNIs, showing differences in inhibition efficacy and strain sensitivity, consistent with literature. As a proof of concept, root exudates from diverse wheat genotypes were screened, demonstrating distinct inhibition profiles. The proposed system advances previously available screening systems and, when integrated with realistic soil tests, will facilitate the discovery of novel BNIs and BNI-producing plant genotypes.

microbiology↗

Biofilm lifestyle as a common trait of ammonia-oxidizing archaea

Although widespread in nature, growth in biofilms has been relatively little explored in the globally distributed ammonia oxidizing archaea (AOA). Here we investigated six representatives of three different terrestrial and marine clades of AOA in a longitudinal and quantitative study for their ability to form biofilm and studied gene expression patterns of three representatives. While all strains grew on a solid surface, soil strains exhibited the highest capacity for biofilm formation. Based on microscopic and gene expression data, two different colonization strategies could be distinguished. S-layer containing AOA (from both soil and marine habitats) initialized attachment as single cells and subsequently formed denser layers and three-dimensional structures, while the S-layer free species of the Nitrosocosmicus clade attached as suspended aggregates to the surface and henceforth showed fastest establishment of biofilm. Transcription profiles were significantly different between planktonic and biofilm growth in all strains and revealed individual reactions, often fulfilling shared functions. In particular the strong expression of different types of multicopper oxidases was observed in all strains indicating modifications of their cell coats. S-layer carrying AOA each additionally expressed a set of adhesion proteins supporting attachment. Detoxification of nitrous compounds, copper acquisition as well as the expression of transcription factor B were also shared reactions among biofilm producing strains. However, the majority of differentially expressed protein families was distinct among the three strains illustrating that individual solutions have evolved for the shared growth mode of biofilm formation in AOA, probably driven by the different ecological niches.

microbiology↗

The type III-B CRISPR-Cas System Affects Energy Metabolism and Adaptation in the Archaeon Saccharolobus solfataricus

Type III CRISPR-Cas immune systems that recognize and cleave extrachromosomal RNA when active, are particularly widespread in archaea. Mechanistically, these systems have the potential to regulate gene expression of host genes on a post-transcriptional level, but very little is known about any potential accessory roles of type III-B systems beyond immunity. We have created knockout mutants of a type III-B CRISPR-Cas complex in the thermoacidophilic archaeon Saccharolobus solfataricus to investigate potential secondary functions of the type III-B system. Deletion mutants exhibited an accelerate growth but were less quickly adaptable to changes in carbon sources in their growth media. In line with this phenotype, upregulated genes were significantly enriched in functional categories of energy production and conversion, as well as with carbohydrate or amino acid transport and metabolism in RNAseq studies. Generally, a significant accumulation of genes encoding transmembrane proteins in the upregulated proportion of the transcriptome suggests interconnections between the type III-B CRISPR-Cas system and various membrane-associated processes. Notably, the deletion mutants did not lose their general virus- or plasmid defense activities indicating that this particular system might have been partially adopted for cellular regulatory roles.

microbiology↗

Molecular Tracking and Cultivation Reveal Ammonia Oxidizing Archaea as Integral Members of the Human Skin Microbiome

BackgroundAmmonia-oxidizing archaea (AOA) have repeatedly been detected on human skin, yet their persistence, physiological traits, and adaptations remain poorly understood. Here, we identify Nitrosocosmicus species as integral members of the healthy skin microbiome using two complementary approaches. ResultsThrough cultivation, we enriched two autotrophic strains, Candidatus Nitrosocosmicus epidermidis and Ca. Nitrosocosmicus unguis, from human skin samples. Genomic analyses revealed specific adaptations for skin colonization, including genomic islands and expanded gene families linked to interactions with host proteins and signaling pathways, distinguishing these AOA from their soil-dwelling relatives. Parallel molecular profiling in cross-sectional and longitudinal cohorts (n=47) consistently detected Nitrosocosmicus particularly in sebaceous areas. Co-occurrence patterns with specific bacterial taxa reinforce their role as stable components of the skin microbiome. ConclusionsThese findings indicate that Nitrosocosmicus species are emerging commensals, evolutionarily capable of transitioning from soil to human skin, where they likely play a critical role in the skin ecosystem.

microbiology↗

Targeted metagenomics using probe capture detects a larger diversity of nitrogen and methane cycling genes in complex microbial communities than traditional metagenomics

Microorganisms are key players in the global cycling of nitrogen (N) and carbon (C), controlling their availability and fluxes, including the emissions of the powerful greenhouse gases nitrous oxide (N2O) and methane (CH4). Characterizing the microbial functional guilds driving these processes is crucial for understanding ecosystem functioning and predicting their responses to environmental changes. Standard sequence-based characterization methods often reveal only a limited fraction of their diversity in nature because of their low relative abundance, the insufficient sequencing depth of traditional metagenomes of complex communities, and limitations in coverage of PCR-based assays. Here, we developed and tested a targeted metagenomics approach based on probe capture and hybridization to simultaneously characterize the diversity of multiple key metabolic genes involved in inorganic N and CH4 cycling. We designed comprehensive probe libraries for each of the 14 target marker genes comprising 264,000 unique probes. These probes were used to selectively enrich the target genes in shotgun metagenomic libraries. In validation experiments with the mock communities of known microorganisms, targeted metagenomics yielded gene profiles similar to those of the original communities. Only GC content had a small effect on probe efficiency, as low GC targets were less efficiently detected than those with high GC, within the mock communities. Furthermore, the relative abundances of the marker genes obtained using targeted or traditional shotgun metagenomics from agricultural and wetland soils were significantly correlated, indicating that the targeted approach did not introduce significant quantitative bias. In addition, using archaeal amoA genes as a case-study, targeted metagenomics identified substantially higher taxonomic diversity and a larger number of sequence reads per sample, yielding diversity estimates 28 or 1.24 times higher than shotgun metagenomics or amplicon sequencing, respectively. Notably, shotgun metagenomics detected only three out of the 84 amoA gene phylotypes detected using targeted metagenomics. Our results show that targeted metagenomics complements current approaches to characterize key microbial populations and functional guilds in biogeochemical cycles in different ecosystems, enabling more detailed, simultaneous characterization of multiple functional genes. Manuscript contribution to the fieldMetagenomic sequencing often yields limited numbers of sequences of rare microbial taxa or functional genes, preventing in-depth analyses of specific populations and functional groups. Amplicon-based approaches enable the higher diversity coverage of target populations, but the drawback is the difficulty in designing unbiased primers that cover the highest intra-group diversity. Targeted metagenomics overcomes these challenges and results in similar community structure as traditional amplicon sequencing, while expanding the sequence space in a less biased metagenomic-based approach. Therefore, targeted metagenomics is an invaluable tool for studying the diversity of specific populations within complex natural microbiomes. Here, we present and evaluate a probe library designed for targeted metagenomics of nitrogen and methane cycling genes in complex communities.

microbiology↗

Unexpected Complexity of the Ammonia Monooxygenase in Archaea

Ammonia oxidation as the first step of nitrification constitutes a critical process in the global nitrogen cycle. However, fundamental knowledge of its key enzyme, the copper-dependent ammonia monooxygenase is lacking, in particular for the environmentally abundant ammonia oxidizing archaea (AOA). Here, the structure of the enzyme is investigated by blue-native gel electrophoresis and proteomics from native membrane complexes of two AOA. Beside the known AmoABC subunits and the earlier predicted AmoX, two new protein subunits, AmoY and AmoZ, were identified. They are unique to AOA, highly conserved and co-regulated, and their genes are linked to other AMO subunit genes in streamlined AOA genomes. Modelling and in gel cross-link approaches support an overall protomer structure similar to the distantly related bacterial particulate methane monooxygenase indicating that AmoY and AmoZ serve an important structural and functional role. These data open avenues for further structure-function studies of this ecologically important key nitrification complex.

microbiology↗

Comparative proteogenomics deciphers the origin and evolution of eukaryotic chromatin

Histones and associated chromatin proteins have essential functions in eukaryotic genome organization and regulation. Despite this fundamental role in eukaryotic cell biology, we lack a phylogenetically-comprehensive understanding of chromatin evolution. Here, we combine comparative proteomics and genomics analysis of chromatin in eukaryotes and archaea. Proteomics uncovers the existence of histone post-translational modifications in Archaea. However, archaeal histone modifications are scarce, in contrast with the highly conserved and abundant marks we identify across eukaryotes. Phylogenetic analysis reveals that chromatin-associated catalytic functions (e.g., methyltransferases) have pre-eukaryotic origins, whereas histone mark readers and chaperones are eukaryotic innovations. We show that further chromatin evolution is characterized by expansion of readers, including capture by transposable elements and viruses. Overall, our study infers detailed evolutionary history of eukaryotic chromatin: from its archaeal roots, through the emergence of nucleosome-based regulation in the eukaryotic ancestor, to the diversification of chromatin regulators and their hijacking by genomic parasites.

evolutionary biology↗

Ancestral reconstructions decipher major adaptations of ammonia oxidizing archaea upon radiation into moderate terrestrial and marine environments

Unlike all other archaeal lineages, ammonia oxidizing archaea (AOA) of the phylum Thaumarchaea are widespread and abundant in all moderate and oxic environments on Earth. The evolutionary adaptations that led to such unprecedented ecological success of a microbial clade characterized by highly conserved energy and carbon metabolisms have, however, remained underexplored. Here we reconstructed the genomic content and growth temperature of the ancestor of all AOA as well as the ancestors of the marine and soil lineages based on 39 available complete or nearly complete genomes of AOA. Our evolutionary scenario depicts an extremely thermophilic autotrophic, aerobic ancestor from which three independent lineages of a marine and two terrestrial groups radiated into moderate environments. Their emergence was paralleled by (I) a continuous acquisition of an extensive collection of stress tolerance genes mostly involved in redox maintenance and oxygen detoxification, (II) an expansion of regulatory capacities in transcription and central metabolic functions and (III) an extended repertoire of cell appendages and modifications related to adherence and interactions with the environment. Our analysis provides insights into the evolutionary transitions and key processes that enabled the conquest of the diverse environments in which contemporary AOA are found.

microbiology↗

Genomes of Thaumarchaeota from deep sea sediments reveal specific adaptations of three independently evolved lineages

Marine sediments represent a vast habitat for complex microbiomes. Among these, ammonia oxidizing archaea (AOA) of the phylum Thaumarchaeota are one of the most common, yet little explored inhabitants, that seem extraordinarily well adapted to the harsh conditions of the subsurface biosphere. We present 11 metagenome-assembled genomes of the most abundant AOA clades from sediment cores obtained from the Atlantic Mid-Ocean ridge flanks and Pacific abyssal plains. Their phylogenomic placement reveals three independently evolved clades within the order Ca. Nitrosopumilales, of which no cultured representative is known yet. In addition to the gene sets for ammonia oxidation and carbon fixation known from other AOA, all genomes encode an extended capacity for the conversion of fermentation products that can be channeled into the central carbon metabolism, as well as uptake of amino acids probably for protein maintenance or as an ammonia source. Two lineages encode an additional (V-type) ATPase and a large repertoire of gene repair systems that may allow to overcome challenges of high hydrostatic pressure. We suggest that the adaptive radiation of AOA into marine sediments occurred more than once in evolution and resulted in three distinct lineages with particular adaptations to this extremely energy limiting and high-pressure environment.

microbiology↗

In situ growth of anammox bacteria in subseafloor sediments

The deep biosphere buried in marine sediments was estimated to host an equal number of microbes as found in the above oceans 1. It has been debated if these cells are alive and active 2, and their per cell energy availability does not seem to allow for net population growth 3. Here, we report the growth of anammox bacteria in [~]80,000 year old subsurface sediments indicated by their four orders of magnitude abundance increase in the nitrate-ammonia transition zone (NATZ). Their growth coincides with a local increase in anammox power supply. The genome of the dominant anammox bacterium from the NATZ was reconstructed and showed an increased index of replication confirming in situ active growth. The genome belongs to a new Scalindua species so far exclusively found in marine environments, which has the genetic capacity of urea and cyanate utilization and is enriched in genes allowing it to cope with external environmental stressors, such as energy limitation. Our results suggest that specific microbial groups are not only able to survive over geological timescales, but also thrive in the deep subsurface when encountering favorable conditions.

microbiology↗

Inter- and intra-domain functional redundancy in the rumen microbiome during plant biomass degradation

BackgroundRuminant livestock is a major source of the potent greenhouse gas methane (CH4), produced by the complex rumen microbiome. Using an integrated approach, combining quantitative metatranscriptomics with gas- and volatile fatty acid (VFA) profiling, we gained fundamental insights into temporal dynamics of the cow rumen microbiome during feed degradation.\n\nResultsThe microbiome composition was highly individual and remarkably stable within each cow, despite similar gas emission and VFA profiles between cows. Gene expression profiles revealed a fast microbial growth response to feeding, reflected by drastic increases in microbial biomass, CH4 emissions and VFA concentrations. Microbiome individuality was accompanied by high inter- and intra-domain functional redundancy among pro- and eukaryotic microbiome members in the key steps of anaerobic feed degradation. Methyl-reducing but not CO2-reducing methanogens were correlated with increased CH4 emissions during plant biomass degradation.\n\nConclusionsThe major response of the rumen microbiome to feed intake was a general growth of the whole community. The high functional redundancy of the cow-individual microbiomes was possibly linked to the robust performance of the anaerobic degradation process. Furthermore, the strong response of methylotrophic methanogens is suggesting that they might play a more important role in ruminant CH4 emissions than previously assumed, making them potential targets for CH4 mitigation strategies.

microbiology↗