Biology subjects

Pelikan, C.

Publications and source records attributed to Pelikan, C..

8 recordsLinked to original sources

bioRxiv2022

Conservation of energetic pathways for electroautotrophy in the uncultivated candidate order Tenderiales

Electromicrobiology can be used to understand extracellular electron uptake in previously undescribed chemolithotrophs. Enrichment and characterization of the uncultivated electroautotroph "Candidatus Tenderia electrophaga" using electromicrobiology led to the designation of the order Tenderiales. Representative Tenderiales metagenome assembled genomes (MAGs) have been identified in a number of environmental surveys, yet a comprehensive characterization of conserved genes for extracellular electron uptake has thus far not been conducted. Using comparative genomics we identified conserved orthologous genes within the Tenderiales and nearest neighbor orders important for extracellular electron uptake based on a previously proposed pathway from "Ca. Tenderia electrophaga". The Tenderiales contained a conserved cluster we designated uetABCDEFGHIJ, which encodes proteins containing features that would enable transport of extracellular electrons to cytoplasmic membrane bound energy transducing complexes such as two conserved cytochrome cbb3 oxidases. For example, UetJ is predicted to be an extracellular undecaheme c-type cytochrome that forms a heme wire. We also identified clusters of genes predicted to facilitate assembly and maturation of electron transport proteins, as well as cellular attachment to surfaces. Autotrophy among the Tenderiales is supported by the presence of carbon fixation and stress response pathways that could allow cellular growth by extracellular electron uptake. Key differences between the Tenderiales and other known neutrophilic iron oxidizers were revealed, including very few Cyc2 genes in the Tenderiales. Our results reveal a possible conserved pathway for extracellular electron uptake and suggests the Tenderiales have an distribution unlimited ecological role coupling metal or mineral redox chemistry and the carbon cycle in marine and brackish sediments. ImportanceElectromicrobiology enables enrichment and identification of chemolithotrophic bacteria capable of extracellular electron uptake to drive energy metabolism and CO2 fixation. The recently described order Tenderiales contains the uncultivated electroautotroph "Candidatus Tenderia electrophaga". The "Ca. Tenderia electrophaga" genome contains genes proposed to make up a previously undescribed extracellular electron uptake pathway. Here we use comparative genomics to show that this pathway is well conserved among Tenderiales spp. recovered by metagenome assembled genomes. This conservation extends to near neighbors of the Tenderiales, but not to other well-studied chemolithotrophs including iron and sulfur oxidizers. Our findings suggest that extracellular electron uptake may be pervasive among the Tenderiales and the geographic location from which metagenome assembled genomes were recovered offers clues to their natural ecological niche.

microbiology↗

bioRxiv2020

Anaerobic microbial degradation of protein and lipid macromolecules in subarctic marine sediment

Microorganisms in marine sediments play major roles in marine biogeochemical cycles by mineralizing substantial quantities of organic matter from decaying cells. Proteins and lipids are abundant components of necromass, yet microorganisms that degrade them remain understudied. Here, we revealed identities, trophic interactions and genomic features of microorganisms that degraded 13C-labelled proteins and lipids in cold anoxic microcosms with sulfidic subarctic marine sediment. Supplemented proteins and lipids were rapidly fermented to various volatile fatty acids within five days. DNA-stable isotope probing (SIP) suggested Psychrilyobacter atlanticus was an important primary degrader of proteins, and Psychromonas members were important primary degraders of both proteins and lipids. Closely related Psychromonas populations, as represented by distinct 16S rRNA gene variants, differentially utilized either proteins or lipids. DNA-SIP also showed 13C-labeling of various Deltaproteobacteria within ten days, indicating trophic transfer of carbon to putative sulfate-reducers. Metagenome-assembled genomes revealed the primary hydrolyzers encoded secreted peptidases or lipases, and enzymes for catabolism of protein or lipid degradation products. Psychromonas were prevalent in diverse marine sediments, suggesting they are important players in organic carbon processing in situ. Together, this study provides an improved understanding of the metabolic processes and functional partitioning of necromass macromolecules among microorganisms in the seafloor.

microbiology↗

bioRxiv2019

Glacial runoff promotes deep burial of sulfur cycling-associated microorganisms in marine sediments

Marine fjords with active glacier outlets are hot spots for organic matter burial in the sediments and subsequent microbial mineralization, and will be increasingly important as climate warming causes more rapid glacial melt. Here, we investigated controls on microbial community assembly in sub-arctic glacier-influenced (GI) and non-glacier-influenced (NGI) marine sediments in the Godth[a]bsfjord region, south-western Greenland. We used a correlative approach integrating 16S rRNA gene and dissimilatory sulfite reductase (dsrB) amplicon sequence data over six meters of depth with biogeochemistry, sulfur-cycling activities, and sediment ages. GI sediments were characterized by comparably high sedimentation rates and had young sediment ages of <500 years even at 6 m sediment depth. In contrast, NGI stations reached ages of approximately 10,000 years at these depths. Sediment age-depth relationships, sulfate reduction rates, and C/N ratios were strongly correlated with differences in microbial community composition between GI and NGI sediments, indicating that age and diagenetic state were key drivers of microbial community assembly in subsurface sediments. Similar bacterial and archaeal communities were present in the surface sediments of all stations, whereas only in GI sediments were many surface taxa also abundant through the whole sediment core. The relative abundance of these taxa, including diverse Desulfobacteraceae members, correlated positively with sulfate reduction rates, indicating their active contributions to sulfur-cycling processes. In contrast, other surface community members, such as Desulfatiglans, Atribacteria and Chloroflexi, survived the slow sediment burial at NGI stations and dominated in the deepest sediment layers. These taxa are typical for the energy-limited marine deep biosphere and their relative abundances correlated positively with sediment age. In conclusion, our data suggests that high rates of sediment accumulation caused by glacier runoff and associated changes in biogeochemistry, promote persistence of sulfur-cycling activity and burial of a larger fraction of the surface microbial community into the deep subsurface.\n\nContribution to the Field StatementIn most coastal marine sediments organic matter turnover and total energy flux are highest at the surface and decrease significantly with increasing sediment depth, causing depth-dependent changes in the microbial community composition. Glacial runoff in arctic and subarctic fjords alters the composition of the microbial community at the surface, mainly due to different availabilities of organic matter and metals. Here we show that glacial runoff also modifies microbial community assembly with sediment depth. Sediment age was a key driver of microbial community composition in six-meter-long marine sediment cores from the Godth[a]bsfjord region, south-western Greenland. High sedimentation rates at glacier-influenced sediment stations enabled a complex community of sulfur-cycling-associated microorganisms to continuously thrive at high relative abundances from the surface into the sediment subsurface. These communities consisted of putative fermenters, sulfate reducers and sulfur oxidizers, which likely depended on high metal concentrations in the relatively young, glacier-influenced sediments. In non-glacier-influenced sediments with lower sedimentation rates, these sulfur-cycling-associated microorganisms were only present near the surface. With increasing sediment depth these surface microorganisms were largely replaced by other surface microorganisms that positively correlated with sediment age and belong to known taxa of the energy-limited, marine deep biosphere.

microbiology↗

bioRxiv2019

DNA-foraging bacteria in the seafloor

Extracellular DNA is a major macromolecule in global element cycles, and is a particularly crucial phosphorus as well as nitrogen and carbon source for microorganisms in the seafloor. Nevertheless, the identities, ecophysiology and genetic features of key DNA-foraging microorganisms in marine sediments are completely unknown. Here we combined microcosm experiments, stable isotope probing and genome-centric metagenomics to study microbial catabolism of DNA and its sub-components in anoxic marine sediments. 13C-DNA added to sediment microcosms was degraded within ten days and mineralised to 13CO2. Stable isotope probing showed that diverse Candidatus Izemoplasma, Lutibacter, Shewanella, Fusibacteraceae and Nitrincolaceae incorporated DNA-derived 13C-carbon. Genomes representative of the 13C-labelled taxa were recovered and all encoded enzymatic repertoires for catabolism of DNA. Comparative genomics indicated that DNA can be digested by diverse members of the order Candidatus Izemoplasmatales (former Tenericutes), which appear to be specialised DNA-degraders that encode multiple extracellular nucleases. Fusibacteraceae lacked genes for extracellular nucleases but utilised various individual purine- and pyrimidine-based molecules, suggesting they cheated on liberated sub-components of DNA. Close relatives of the DNA-degrading taxa are globally distributed in marine sediments, suggesting that these poorly understood taxa contribute widely to the key ecosystem function of degrading and recycling DNA in the seabed.

microbiology↗

bioRxiv2019

Diversity decoupled from sulfur isotope fractionation in a sulfate reducing microbial community

The extent of fractionation of sulfur isotopes by sulfate reducing microbes is dictated by genomic and environmental factors. A greater understanding of species-specific fractionations may better inform interpretation of sulfur isotopes preserved in the rock record. To examine whether gene diversity influences net isotopic fractionation in situ, we assessed environmental chemistry, sulfate reduction rates, diversity of putative sulfur metabolizing organisms by 16S rRNA and dissimilatory sulfite reductase (dsrB) gene amplicon sequencing, and net fractionation of sulfur isotopes along a sediment transect of a hypersaline Arctic spring. In situ sulfate reduction rates yielded minimum cell-specific sulfate reduction rates <0.3 x 10-15 moles cell-1 day-1. Neither 16S rRNA nor dsrB diversity indices correlated with relatively constant (38 to 45{per thousand}) net isotope fractionation ({varepsilon}34Ssulfide-sulfate). Measured {varepsilon}34S values could be reproduced in a mechanistic fractionation model if 1-2% of the microbial community (10-60% of Deltaproteobacteria) were engaged in sulfate respiration, indicating heterogeneous respiratory activity within sulfate-metabolizing populations. This model indicated enzymatic kinetic diversity of Apr was more likely to correlate with sulfur fractionation than DsrB. We propose that, above a threshold alpha diversity value, the influence of the specific composition of the microbial community responsible for generating an isotope signal is overprinted by the control exerted by environmental variables on microbial physiology.\n\nSubject categoriesO_LIIntegrated genomics and post-genomics approaches in microbial ecology\nC_LIO_LIMicrobial ecology and functional diversity of natural habitats\nC_LI

microbiology↗

bioRxiv2018

Growth arrest in the active rare biosphere

Microbial diversity in the environment is mainly concealed within the rare biosphere, which is arbitrarily defined as all species with <0.1% relative abundance. While dormancy explains a low-abundance state very well, the cellular mechanisms leading to rare but active microorganisms are not clear. We used environmental systems biology to genomically and metabolically characterize a cosmopolitan sulfate reducer that is of low abundance but highly active in peat soil, where it contributes to counterbalance methane emissions. We obtained a 98%-complete genome of this low-abundance species, Candidatus Desulfosporosinus infrequens, by metagenomics. To test for environmentally relevant metabolic activity of Ca. D. infrequens, anoxic peat soil microcosms were incubated under diverse in situ-like conditions for 36 days and analyzed by metatranscriptomics. Compared to the no-substrate control, transcriptional activity of Ca. D. infrequens increased 56- to 188-fold in incubations with sulfate and acetate, propionate, lactate, or butyrate, revealing a versatile substrate use. Cellular activation was due to a significant overexpression of genes encoding ribosomal proteins, dissimilatory sulfate reduction, and carbon-degradation pathways, but not of genes encoding DNA or cell replication. We show for the first time that a rare biosphere member transcribes metabolic pathways relevant for carbon and sulfur cycling over prolonged time periods while being growth-arrested in its lag phase.\n\nSignificanceThe microbial rare biosphere represents the largest pool of biodiversity on Earth and constitutes, in sum of all its members, a considerable part of a habitats biomass. Dormancy or starvation are typically used to explain a low-abundance state. We show that low-abundance microorganisms can be highly metabolically active while being growth-arrested over prolonged time periods. We show that this is true for microbial keystone species, such as a cosmopolitan but low-abundance sulfate reducer in wetlands that is involved in counterbalancing greenhouse gas emission. Our results challenge the central dogmas \"metabolic activity translates directly into growth\" as well as \"low abundance equals little ecosystem impact\" and provide an important step forward in understanding rare biosphere members relevant for ecosystem functions.

microbiology↗

bioRxiv2017

Peatland Acidobacteria with a dissimilatory sulfur metabolism

Sulfur-cycling microorganisms impact organic matter decomposition in wetlands and consequently greenhouse gas emissions from these globally relevant environments. However,their identities and physiological properties are largely unknown. By applying a functional metagenomics approach to an acidic peatland, we recovered draft genomes of seven novel Acidobacteria species with the potential for dissimilatory sulfite (dsrAB, dsrC, dsrD, dsrN, dsrT, dsrMKJOP) or sulfate respiration (sat, aprBA, qmoABC plus dsr genes). Surprisingly, the genomes also encoded dsrL, a unique gene of the sulfur oxidation pathway. Metatranscriptome analysis demonstrated expression of acidobacterial sulfur-metabolism genes in native peat soil and their upregulation in diverse anoxic microcosms. This indicated an active sulfate respiration pathway, which, however, could also operate in reverse for sulfur oxidation as recently shown for other microorganisms. Acidobacteria that only harbored genes for sulfite reduction additionally encoded enzymes that liberate sulfite from organosulfonates, which suggested organic sulfur compounds as complementary energy sources. Further metabolic potentials included polysaccharide hydrolysis and sugar utilization, aerobic respiration, several fermentative capabilities, and hydrogen oxidation. Our findings extend both, the known physiological and genetic properties of Acidobacteria and the known taxonomic diversity of microorganisms with a DsrAB-based sulfur metabolism, and highlight new fundamental niches for facultative anaerobic Acidobacteria in wetlands based on exploitation of inorganic and organic sulfur molecules for energy conservation.

microbiology↗

bioRxiv2017

Bottled aqua incognita: Microbiota assembly and dissolved organic matter diversity in natural mineral waters

BackgroundNon-carbonated natural mineral waters contain microorganisms that regularly grow after bottling despite low concentrations of dissolved organic matter (DOM). Yet, the compositions of bottled water microbiota and organic substrates that fuel microbial activity, and how both change after bottling, are still largely unknown.\n\nResultsWe performed a multifaceted analysis of microbiota and DOM diversity in twelve natural mineral waters from six European countries. 16S rRNA gene-based analyses showed that less than ten species-level operational taxonomic units (OTUs) dominated the bacterial communities in the water phase and associated with the bottle wall after a short phase of post-bottling growth. Members of the betaproteobacterial genera Curvibacter, Aquabacterium, and Polaromonas (Comamonadaceae) grew in most waters and represent ubiquitous, mesophilic, heterotrophic aerobes in bottled waters. Ultrahigh-resolution mass spectrometry of DOM in bottled waters and their corresponding source waters identified thousands of molecular formulae characteristic of mostly refractory, soil-derived DOM.\n\nConclusionsThe bottle environment, including source water physicochemistry, selected for growth of a similar low-diversity microbiota across various bottled waters. Relative abundance changes of hundreds of multi-carbon molecules were related to growth of less than ten abundant OTUs. We thus speculate that individual bacteria cope with oligotrophic conditions by simultaneously consuming diverse DOM molecules.

microbiology↗