Isolierung, Charakterisierung und Nachweis methanogener Archaea aus laufenden Praxis-NawaRo-Biogasanlagen unter besonderer Beruecksichtigung der Gattung Methanobacterium

Im Verlauf der Forschungsarbeit wurden Proben aus fünf, mit nachwachsenden Rohstoffen (NawaRo) beschickten, landwirtschaftlichen Biogasanlagen (BGA) auf die Biozönose methanogener Archaea hin molekularbiologisch untersucht. Über „amplified rDNA restriction analysis“-Screening (ARDRA) von Bibliotheken auf Basis von 16S rRNA-Genfragmenten konnte anhand zweier beispielhafter BGA das Vorkommen von Vertretern der Gattungen Methanoculleus (Mcu.), Methanobacterium (Mb.), Methanosarcina (Msc.) und Methanosaeta (Mst.) nachgewiesen werden. Mittels denaturierender Gradienten-Gelelektrophorese (DGGE) wurde das Vorkommen dieser Mikroorganismen auch in den übrigen Anlagen gezeigt. Ergänzend dazu wurde in drei Anlagen Methanospirillum hungatei nachgewiesen. Nach Ausarbeitung gattungsspezifischer Isolierungsstrategien konnten insgesamt zehn Vertreter der Gattung Methanobacterium (Isolate Mb1 bis Mb10) und jeweils ein Vertreter der Gattungen Methanoculleus (Isolat Mcu(1)), Methanosarcina (Isolat NieKK) und Methanosaeta (Isolat Mst1.3) aus den BGA-Proben isoliert werden. Durch in silico-Abgleich der partiellen 16S rRNA-Gensequenzen wurden diese als Verwandte von Mb. formicicum MFT, Mcu. bourgensis MS2T, Msc. mazei S-6T und Mst. concilii FE mit einer Sequenzidentität > 97% identifiziert. Im Laufe weiterer molekularbiologischer Untersuchungen mittels DGGE und ARDRA-Analyse konnten die Isolate den Referenzstämmen zugeordnet werden. In Bezug auf die Gattung Methanobacterium ergaben sich jedoch leichte Abweichungen. Diese bestätigten sich in vergleichenden Analysen des genomischen Fingerabdrucks in der „specifically amplified polymorphic DNA“-PCR (SAPD-PCR), welche im Rahmen dieser Arbeit erstmalig erfolgreich auf archaeelle Organismen angewandt wurde. Hier zeigten die Isolate zwei von den Fingerabdrücken der untersuchten Referenzstämme verschiedene Hauptamplifikationsmuster. Aufgrund der Vielzahl der Isolate sowie dem signifikanten Vorkommen in qPCR-Analysen und Klonbibliotheken fokussierten sich die weiteren Arbeiten zur genauen Untersuchung dieser Abweichungen auf phylogenetische Analysen der Gattung Methanobacterium und die Entwicklung von Nachweissystemen. Die Aufklärung eines Großteils der 23S rRNA-Gensequenzen der Isolate und von ausgewählten Typstämmen ermöglichte ergänzende phylogenetische Untersuchungen zu durchgeführten 16S rRNA-Analysen. Dabei wurden die Isolate jeweils in einem eigenen Cluster abseits der meisten Referenzstämme aus der Gattung Methanobacterium positioniert. Analog zur Musterbildung im Rahmen der SAPD-Analyse zeigte sich eine Differenzierung in zwei Äste und ergab in Übereinstimmung mit den in silico-Sequenzabgleichen den höchsten Verwandtschaftsgrad mit Mb. formicicum MFT. Die Eignung der SAPD-PCR zur Ableitung spezifischer Primerpaare konnte erstmals auch für methanogene Archaea gezeigt werden. Die Ableitung zweier Primerpaare mit Spezifität für die Methanobacterium-Isolate Mb1 bis Mb10 sowie für den Typstamm Mb. formicicum MFT gelang und konnte im Rahmen eines Direkt-PCR-Nachweises erfolgreich auf Reinkulturen und Fermenterproben angewandt werden. Unter Einbezug der sequenzierten 23S rRNA-Genfragmente gelang die Erstellung von Oligonukleotid-Sonden für den Einsatz in Fluoreszenz in situ-Hybridisierungsexperimenten. Im Praxistest ergab sich für diese Sonden eine Spezifität für alle getesteten Vertreter der Gattung Methanobacterium sowie für Methanosphaera stadtmanae MCB-3T und Methanobrevibacter smithii PST.rnSomit konnten im Laufe der Arbeit die dominanten methanogenen Archaea in NawaRo-BGA in mehrphasigen Experimenten nachgewiesen, quantifiziert und auf nur wenige Gattungen eingegrenzt werden. Vertreter der vier dominanten Gattungen wurden isoliert und Nachweissysteme für Arten der Gattung Methanobacterium erstellt.rn

Isotopic signature of specific biomarkers derived from anaerobic methanotrophic archaea (ANME groups) and sulphate-reducing bacteria (SRB) at different cold seep provinces

Anaerobic methane-oxidizing microbial communities in sediments at cold methane seeps are important factors in controlling methane emission to the ocean and atmosphere. Here, we investigated the distribution and carbon isotopic signature of specific biomarkers derived from anaerobic methanotrophic archaea (ANME groups) and sulphate-reducing bacteria (SRB) responsible for the anaerobic oxidation of methane (AOM) at different cold seep provinces of Hydrate Ridge, Cascadia margin. The special focus was on their relation to in situ cell abundances and methane turnover. In general, maxima in biomarker abundances and minima in carbon isotope signatures correlated with maxima in AOM and sulphate reduction as well as with consortium biomass. We found ANME-2a/DSS aggregates associated with high abundances of sn-2,3-di-O-isoprenoidal glycerol ethers (archaeol, sn-2-hydroxyarchaeol) and specific bacterial fatty acids (C16:1omega5c, cyC17:0omega5,6) as well as with high methane fluxes (Beggiatoa site). The low to medium flux site (Calyptogena field) was dominated by ANME-2c/DSS aggregates and contained less of both compound classes but more of AOM-related glycerol dialkyl glycerol tetraethers (GDGTs). ANME-1 archaea dominated deeper sediment horizons at the Calyptogena field where sn-1,2-di-O-alkyl glycerol ethers (DAGEs), archaeol, methyl-branched fatty acids (ai-C15:0, i-C16:0, ai-C17:0), and diagnostic GDGTs were prevailing. AOM-specific bacterial and archaeal biomarkers in these sediment strata generally revealed very similar d13C-values of around -100 per mill. In ANME-2-dominated sediment sections, archaeal biomarkers were even more 13C-depleted (down to -120 per mill), whereas bacterial biomarkers were found to be likewise 13C-depleted as in ANME-1-dominated sediment layers (d13C: -100 per mill). The zero flux site (Acharax field), containing only a few numbers of ANME-2/DSS aggregates, however, provided no specific biomarker pattern. Deeper sediment sections (below 20 cm sediment depth) from Beggiatoa covered areas which included solid layers of methane gas hydrates contained ANME-2/DSS typical biomarkers showing subsurface peaks combined with negative shifts in carbon isotopic compositions. The maxima were detected just above the hydrate layers, indicating that methane stored in the hydrates may be available for the microbial community. The observed variations in biomarker abundances and 13C-depletions are indicative of multiple environmental and physiological factors selecting for different AOM consortia (ANME-2a/DSS, ANME-2c/DSS, ANME-1) along horizontal and vertical gradients of cold seep settings.

Soil characteristics and abundance of archaea in samples from the Ross Sea Region, Antarctica

The objective of this study was to examine the presence and diversity of Archaea within mineral and ornithogenic soils from 12 locations across the Ross Sea region. Archaea were not abundant but DNA sufficient for producing 16S rRNA gene clone libraries was extracted from 18 of 51 soil samples, from four locations. A total of 1452 clones were analysed by restriction fragment length polymorphism and assigned to 43 operational taxonomic units from which representatives were sequenced. Archaea were primarily restricted to coastal mineral soils which showed a predominance of Crenarchaeota belonging to group 1.1b (>99% of clones). These clones were assigned to six clusters (A through F), based on shared identity to sequences in the GenBank database. Ordination indicated that soil chemistry and water content determined archaeal community structure. This is the first comprehensive study of the archaeal community in Antarctic soils and as such provides a reference point for further investigation of microbial function in this environment.

Global distributions of picoheterothrophs (Bacteria and Archaea) abundance and biomass - Gridded data product (NetCDF) - Contribution to the MAREDAT World Ocean Atlas of Plankton Functional Types

We compiled a database of bacterial abundance of 39 766 data points. After gridding with 1° spacing, the database covers 1.3% of the ocean surface. There is data covering all ocean basins and depth except the Southern Hemisphere below 350 m or from April until June. The average bacterial biomass is 3.9 ± 3.6 µg l-1 with a 20-fold decrease between the surface and the deep sea. We estimate a total ocean inventory of about 1.3 - 1029 bacteria. Using an average of published open ocean measurements for the conversion from abundance to carbon biomass of 9.1 fg cell-1, we calculate a bacterial carbon inventory of about 1.2 Pg C. The main source of uncertainty in this inventory is the conversion factor from abundance to biomass.

Anaerobic methanotrophic archaea-2 and Desulfosarcina/Desulfococcus group in sediments at different stations

The anaerobic oxidation of methane (AOM) with sulfate as terminal electron acceptor is mediated by consortia of methanotrophic archaea (ANME) and sulfate-reducing bacteria (SRB). In sediment samples from Hydrate Ridge, the Isis Mud Volcano and the Gulf of Mexico, DSS cells accounted for 3-6% of all DAPI-stained single cells. Out of these, 8-17% were labelled with probe SEEP1a-1441. This translated into relative abundances of single SEEP-SRB1a cells of 0.3% to 0.7%. Contrastingly, in a sediment sample from the Gullfaks oil field, DSS cells accounted for 18% and SEEP-SRB1a for 9% of all single cells. This sediment sample also featured an unusually high abundance of single ANME-2 cells and only very few ANME-2/DSS aggregates in comparison with other AOM habitats. Considering also the nature of the sample, it is likely that the high number of single ANME-2 and SEEP-SRB1a cells were an artifact of sample preparation. Here, harsher sonication was required to remove the microorganisms from coarse sand prior to CARD-FISH analysis.

Orientation of the transcription preinitiation complex in Archaea

The basal transcription machinery of Archaea corresponds to the minimal subset of factors required for RNA polymerase II transcription in eukaryotes. Using just two factors, Archaea recruit the RNA polymerase to promoters and define the direction of transcription. Notably, the principal determinant for the orientation of transcription is not the recognition of the TATA box by the TATA-box-binding protein. Instead, transcriptional polarity is governed by the interaction of the archaeal TFIIB homologue with a conserved motif immediately upstream of the TATA box. This interaction yields an archaeal preinitiation complex with the same orientation as the analogous eukaryal complex.

Identification of a novel selD homolog from Eukaryotes, Bacteria, and Archaea: Is there an autoregulatory mechanism in selenocysteine metabolism?

Escherichia coli selenophosphate synthetase (SPS, the selD gene product) catalyzes the production of monoselenophosphate, the selenium donor compound required for synthesis of selenocysteine (Sec) and seleno-tRNAs. We report the molecular cloning of human and mouse homologs of the selD gene, designated Sps2, which contains an in-frame TGA codon at a site corresponding to the enzyme’s putative active site. These sequences allow the identification of selD gene homologs in the genomes of the bacterium Haemophilus influenzae and the archaeon Methanococcus jannaschii, which had been previously misinterpreted due to their in-frame TGA codon. Sps2 mRNA levels are elevated in organs previously implicated in the synthesis of selenoproteins and in active sites of blood cell development. In addition, we show that Sps2 mRNA is up-regulated upon activation of T lymphocytes and have mapped the Sps2 gene to mouse chromosome 7. Using the mouse gene isolated from the hematopoietic cell line FDCPmixA4, we devised a construct for protein expression that results in the insertion of a FLAG tag sequence at the N terminus of the SPS2 protein. This strategy allowed us to document the readthrough of the in-frame TGA codon and the incorporation of 75Se into SPS2. These results suggest the existence of an autoregulatory mechanism involving the incorporation of Sec into SPS2 that might be relevant to blood cell biology. This mechanism is likely to have been present in ancient life forms and conserved in a variety of living organisms from all domains of life.

Similarities between the DNA replication initiators of Gram-negative bacteria plasmids (RepA) and eukaryotes (Orc4p)/archaea (Cdc6p)

The proteins responsible for the initiation of DNA replication are thought to be essentially unrelated in bacteria and archaea/eukaryotes. Here we show that RepA, the initiator from the Pseudomonas plasmid pPS10, and the C-terminal domain of ScOrc4p, a subunit of Saccharomyces cerevisiae (Sc) origin recognition complex (ORC), share sequence similarities. Based on biochemical and spectroscopic evidence, these similarities include common structural elements, such as a winged-helix domain and a leucine-zipper dimerization motif. We have also found that ScOrc4p, as previously described for RepA-type initiators, interacts with chaperones of the Hsp70 family both in vitro and in vivo, most probably to regulate the assembly of active ORC. In evolutionary terms, our results are compatible with the recruitment of the same protein module for initiation of DNA replication by the ancestors of present-day Gram-negative bacteria plasmids, archaea, and eukaryotes.

Cloning of thermostable DNA polymerases from hyperthermophilic marine Archaea with emphasis on Thermococcus sp. 9 degrees N-7 and mutations affecting 3'-5' exonuclease activity.

Five extremely thermophilic Archaea from hydrothermal vents were isolated, and their DNA polymerases were cloned and expressed in Escherichia coli. Protein splicing elements (inteins) are present in many archaeal DNA polymerases, but only the DNA polymerase from strain GB-C contained an intein. Of the five cloned DNA polymerases, the Thermococcus sp. 9 degrees N-7 DNA polymerase was chosen for biochemical characterization. Thermococcus sp. 9 degrees N-7 DNA polymerase exhibited temperature-sensitive strand displacement activity and apparent Km values for DNA and dNTP similar to those of Thermococcus litoralis DNA polymerase. Six substitutions in the 3'-5' exonuclease motif I were constructed in an attempt to reduce the 3'-5' exonuclease activity of Thermococcus sp. 9 degrees N-7 DNA polymerase. Five mutants resulted in no detectable 3'-5' exonuclease activity, while one mutant (Glul43Asp) had <1% of wild-type activity.

Transcription in archaea: similarity to that in eucarya.

We present homologies between archaeal and eucaryal DNA-dependent RNA polymerase (RNAP) subunits and transcription factors. The sequences of the Sulfolobus acidocaldarius subunits D, E, and N and alignments with eucaryal homologs are presented here. The similarities between archaeal transcription factors and their eucaryal homologs TFIIB and TBP have been established in other laboratories. The archaeal RNAP subunits H, K, and N, respectively, show high sequence similarity to ABC27, ABC23, and ABC10 beta (found in all three eucaryal RNAPs); subunit D, to AC40 (common to polymerase II and polymerase III) and B44 (polymerase II); and subunit L, to AC19 and B12.5. The similarity of subunit D and its eucaryal homologs to bacterial alpha is limited to the "alpha-motif," which is also present in subunit L and its eucaryal homologs. Genes encoding homologs of the related eucaryal RNAP subunits A12.2/B12.6 and also homologs of eucaryal transcription elongation factors of the TFIIS family have been detected in Sulfolobus acidocaldarius and Thermococcus celer. In archaea, the protein is not an RNAP subunit. Together with the sequence similarities between archaeal box A-containing and eucaryal TATA box-containing promoters, this shows that the archaeal and eucaryal transcription systems are truly homologous and that they differ structurally and functionally from the bacterial transcription machinery. In contrast, however, a number of genes for the archaeal transcription apparatus are organized in clusters resembling the clusters of transcription-associated genes in Bacteria.

Estudo do exossomo de Archaea e de sua interação com a proteína reguladora PaNip7

O exossomo é um complexo multiproteico conservado evolutivamente de archaea a eucariotos superiores que desempenha funções celulares essenciais tais como: atividade exoribonucleolítica 3\'→5\', regulação dos níveis de mRNA, maturação de RNAs estruturais e controle de qualidade de RNAs durante os vários estágios do mecanismo de expressão gênica. Em Archaea, o exossomo é composto por até quatro subunidades diferentes, duas com domínios de RNase PH, aRrp41 e aRrp42, e duas com domínios de ligação a RNAs, aCsl4 e aRrp4. Três cópias das proteínas aRrp4 e/ou aCsl4 se associam com o núcleo hexamérico catalítico do anel de RNase PH e completam a formação do complexo. A proteína PaNip7 é um cofator de regulação do exossomo da archaea Pyrococcus abyssi e atua na inibição do complexo enzimático ligando-se simultaneamente ao exossomo e a RNAs. Neste projeto, a reconstituição in vitro do exossomo da archaea Pyrococcus abyssi formado pela proteína de topo PaCsl4 foi obtida. Para tanto foram realizadas análises de interação proteica usando as técnicas de cromatografia de afinidade, gel filtração e SDS-PAGE. Em adição à formação da isoforma PaCsl4-exossomo, um fragmento peptídico correspondente à região C-terminal da PaNip7 foi sintetizado pelo método da fase sólida, purificado por RP-HPLC e o purificado foi caracterizado por LC/ESI-MS almejando realizar futuros experimentos de interação com o exossomo.

Biodiversity of Archaea and floral of two inland saltern ecosystems in the Alto Vinalopó Valley, Spain

Background. The extraction of salt from seawater by means of coastal solar salterns is a very well-described process. Moreover, the characterization of these environments from ecological, biochemical and microbiological perspectives has become a key focus for many research groups all over the world over the last 20 years. In countries such as Spain, there are several examples of coastal solar salterns (mainly on the Mediterranean coast) and inland solar salterns, from which sodium chloride is obtained for human consumption. However, studies focused on the characterization of inland solar salterns are scarce and both the archaeal diversity and the plant communities inhabiting these environments remain poorly described. Results. Two of the inland solar salterns (termed Redonda and Penalva), located in the Alto Vinalopó Valley (Alicante, Spain), were characterized regarding their geological and physico-chemical characteristics and their archaeal and botanical biodiversity. A preliminary eukaryotic diversity survey was also performed using saline water. The chemical characterization of the brine has revealed that the salted groundwater extracted to fill these inland solar salterns is thalassohaline. The plant communities living in this environment are dominated by Sarcocornia fruticosa (L.) A.J. Scott, Arthrocnemum macrostachyum (Moris) K. Koch, Suaeda vera Forsk. ex Gmelin (Amaranthaceae) and several species of Limonium (Mill) and Tamarix (L). Archaeal diversity was analyzed and compared by polymerase chain reaction (PCR)-based molecular phylogenetic techniques. Most of the sequences recovered from environmental DNA samples are affiliated with haloarchaeal genera such as Haloarcula, Halorubrum, Haloquadratum and Halobacterium, and with an unclassified member of the Halobacteriaceae. The eukaryote Dunaliella was also present in the samples. Conclusions. To our knowledge, this study constitutes the first analysis centered on inland solar salterns located in the southeastern region of Spain. The results obtained revealed that the salt deposits of this region have marine origins. Plant communities typical of salt marshes are present in this ecosystem and members of the Halobacteriaceae family can be easily detected in the microbial populations of these habitats. Possible origins of the haloarchaea detected in this study are discussed.

Nitrogen regulation of protein–protein interactions and transcript levels of GlnK PII regulator and AmtB ammonium transporter homologs in Archaea

Gene homologs of GlnK PII regulators and AmtB-type ammonium transporters are often paired on prokaryotic genomes, suggesting these proteins share an ancient functional relationship. Here, we demonstrate for the first time in Archaea that GlnK associates with AmtB in membrane fractions after ammonium shock, thus, providing a further insight into GlnK-AmtB as an ancient nitrogen sensor pair. For this work, Haloferax mediterranei was advanced for study through the generation of a pyrE2-based counterselection system that was used for targeted gene deletion and expression of Flag-tagged proteins from their native promoters. AmtB1-Flag was detected in membrane fractions of cells grown on nitrate and was found to coimmunoprecipitate with GlnK after ammonium shock. Thus, in analogy to bacteria, the archaeal GlnK PII may block the AmtB1 ammonium transporter under nitrogen-rich conditions. In addition to this regulated protein–protein interaction, the archaeal amtB-glnK gene pairs were found to be highly regulated by nitrogen availability with transcript levels high under conditions of nitrogen limitation and low during nitrogen excess. While transcript levels of glnK-amtB are similarly regulated by nitrogen availability in bacteria, transcriptional regulators of the bacterial glnK promoter including activation by the two-component signal transduction proteins NtrC (GlnG, NRI) and NtrB (GlnL, NRII) and sigma factor σN (σ54) are not conserved in archaea suggesting a novel mechanism of transcriptional control.