Untersuchung multimerer Proteinkomplexe mit oberflächenanalytischen und röntgenspektroskopischen Methoden

Zusammenfassung rnrnIn dieser Arbeit wurden Untersuchungen an zwei verschiedenen multimeren Proteinkomplexen durchgeführt: Zum einen am Hämocyanin aus Homarus americanus mittels Röntgen-L-Kantenspektroskopie und zum anderen am α-Toxin aus Staphylococcus aureus, hinsichtlich der Interaktion an speziellen Raft-artigen Membranabschnitten, mittels AFM.rnFür das Hämocyanin aus Homarus americanus konnte ein neuer Aspekt bezüglich der Bindung von Sauerstoff aufgezeigt werden. Ein zuvor nicht in Betracht gezogener und diskutierter Einfluss von Wassermolekülen auf diesen Vorgang konnte mittels der Methode der Röntgen-L-Kantenspektroskopie dargestellt werden. Erstmals war es möglich die beiden verschiedenen Beladungszustände (Oxy-, Deoxy-Zustand) des Hämocyanin mittels dieser Methode in physiologisch ähnlicher Umgebung zu untersuchen. Vergleiche der erhaltenen L-Kanten-Spektren mit denen anorganischer Vergleichslösungen ließen auf eine Interaktion von Wassermolekülen mit den beiden Kupferatomen des aktiven Zentrums schließen. Dadurch wurde erstmals ein möglicher Einfluss des Wassers auf den Oxygenierungsprozess des Hämocyanins auf elektronischer Ebene aufgezeigt. Vergleichende Betrachtungen von Röntgenkristallstrukturen verschiedener Typ-3-Kupferproteine bestätigten, dass auch hier ein Einfluss von Wassermolekülen auf die aktiven Zentren möglich ist. Vorgeschlagen wird dabei, dass an Stelle der Überlappung der 3d-Orbitale des Kupfers mit den 2p-Orbitalen des Sauerstoffs, wie sie im sauerstoffbeladenen Zustand auftritt, im sauerstoffunbeladenen Zustand eine Wechselwirkung der 3d-Orbitale des Kupfers mit den LUMOS der Wassermoleküle möglich wird, und ein Elektronen- bzw. Ladungstransfer von den Kupfern auf die Wassermoleküle erfolgen kann. rnAFM-Untersuchungen hinsichtlich der Interaktion des α-Toxins aus Staphylococcus aureus mit oberflächenunterstützten Modellmembranen wiesen darauf hin, dass eine bevorzugte Anbindung und zumindest teilweise Integration der α-Toxine in Raft-artige Membranbereiche stattfindet. Für verschiedene ternäre Lipidsysteme konnten phasenseparierte Modellmembranen abgebildet und die unterschiedlichen Domänenformen zugeordnet werden. Der Anbindungsprozess der Toxine an diese oberflächenunterstützte Modellmembranen erfolgte dann wahrscheinlich vornehmlich an den speziellen Raft-artigen Domänen, wohingegen die Insertion der Poren vorrangig an den Grenzbereichen zwischen den Domänen auftrat. Mögliche Ursache dafür sind die räumlichen Besonderheiten dieser Grenzflächen. Membranen weisen an den Schnittstellen zwischen zwei Domänenformen eine erhöhte Unordnung auf, was sich u.a. in einer geringeren Packungsdichte der Phospholipide und dem erhöhten Freiheitsgrad ihrer Kopfgruppen bemerkbar macht. Außerdem kommt es auf Grund der Interaktion der beteiligten Membranbestandteile Sphingomyelin und Cholesterol untereinander zu einer speziellen Ausrichtung der Phosphocholin-Kopfgruppen und innerhalb der Raft-artigen Domänen zu einer erhöhten Packungsdichte der Phospholipide. Die in dieser Arbeit präsentierten Ergebnisse unterstützten demnach die in der Literatur postulierte Vermutung der bevorzugten Interaktion und Integration der Toxin-Moleküle mit Raft-artigen Membrandomänen. Die Insertion der Pore erfolgt aber wahrscheinlich bevorzugt an den Grenzbereichen zwischen den auftretenden Domänen.rn

Propionsäureabbau in NawaRo-Biogasanlagen

Die Energiewende ist begleitet von dem Ausbau erneuerbarer Energien. Dabei spielt die Energiegewinnung aus Biomasse eine wichtige Rolle. Der optimale Betrieb einer Biogasanlage erfordert eine stabile Methanproduktion, welche jedoch durch die Akkumulation von Propionsäure nachhaltig gestört werden kann. Aus diesem Grund ist der mikrobielle Abbau dieser Substanz von besonderem Interesse. Die Thermodynamik des anaeroben bakteriellen Abbaus von Propionsäure erfordert die syntrophe Verwertung des entstehenden Wasserstoffs durch Wasserstoff-verbrauchende Mikroorganismen, beispielsweise methanogene Archaea.rnMit dem Ziel, die Erkenntnislage der Propionat-Verwertung in NawaRo-Biogasanlagen zu erweitern, sollten Propionat-verwertende Anreicherungskulturen aus NawaRo-Biogasanlagen etabliert, charakterisiert und molekularbiologisch analysiert werden.rnAus landwirtschaftlichen Biogasanlagen wurden reproduzierbar Propionat-verwertende Anreicherungskulturen mittels anaerober Kultivierungstechniken etabliert. Die anaerob Propionat-verwertende Aktivität der Kulturen blieb über Jahre erhalten und konnte unter verschiedenen Bedingungen charakterisiert werden. Die Analyse der sukzessiven Diversität von vier Anreicherungskulturen ermöglichte einen Einblick in die sich während der Propionat-Verwertung sukzessiv verändernde mikrobielle Diversität. Dabei wurden die aus der 16S rDNA-Analyse resultierenden Sequenzcluster MP-1 (Cryptanaerobacter sp./ Pelotomaculum sp.), MP-6 und MP-15 (beide ''Candidatus Cloacamonas sp. ''), sowie MP-9 (Syntrophobacter sulfatireducens) als potentiell Propionat-verwertende Schlüsselspezies identifiziert. Mit S. sulfatireducens wurde eine bekannte syntroph Propionat-verwertende Spezies gefunden. Die Sequenzen von MP-1 waren nahe verwandt mit Pelotomaculum schinkii, ebenfalls eine beschriebene syntroph Propionat-verwertende Spezies. Bei dem nächsten Verwandten der Cluster MP-6 und MP-15 handelte es sich um ''Candidatus Cloacamonas acidaminovorans'', eine bisher unkultivierbare Spezies, dessen Genom für den gesamten Abbauweg der syntrophen Propionat-Oxidation codiert. Syntrophobacter sulfatireducens kam zusammen mit Vertretern der methanogenen Gattungen Methanoculleus, Methanosaeta und Methanomethylovorans vor. Als methanogener Partner von Cryptanaerobacter sp./ Pelotomaculum sp. dominierte die Gattung Methanosarcina. Aufgrund der starken Präsenz der syntroph Acetat oxidierenden Spezies Tepidanaerobacter acetatoxydans (Sequenz-Cluster MP-3), sowie potentiell homoacetogener Arten, wurde zudem ein theoretischer Zusammenhang der Propionat-Verwertung mit der syntrophen Acetat-Oxidation und der autotrophen Homoacetogenese vorgeschlagen.rn

[Feline hemoplasmas in Switzerland: identification of a novel species, diagnosis, prevalence, and clinical importance]

Two feline hemotropic mycoplasma spp. (aka hemoplasma) have previously been recognized. We recently discovered a third novel species in a cat with hemolytic anemia, designated 'Candidatus Mycoplasma turicensis', which is closely related to rodent haemoplasmas. This novel species induced anemia after experimental transmission to two SPF cats. Three quantitative real-time PCR assays were newly designed and applied to an epidemiological study surveying the Swiss pet cat population. Blood samples from 713 healthy and ill cats were analyzed. Up to 104 parameters per cat (detailed questionnaire, case history, laboratory parameters and retroviral infections) were evaluated. 'Candidatus Mycoplasma haemominutum' infection was more prevalent (8.5%) than Mycoplasma haemofelis (0.5%) and 'Candidatus Mycoplasma turicensis' (1%). Hemoplasma infections were associated with male gender, outdoor access, and old age, but not with disease or anemia. Infections were more frequently found in the South and West of Switzerland. Several hemoplasma infected cats, some acutely infected, others co-infected with FIV or FeLV, showed hemolytic anemia indicating that additional factors might play a role in the pathogenesis of the disease.

Worldwide occurrence of feline hemoplasma infections in wild felid species

While hemoplasma infections in domestic cats are well studied, almost no information is available on their occurrence in wild felids. The aims of the present study were to investigate wild felid species as possible reservoirs of feline hemoplasmas and the molecular characterization of the hemoplasma isolates. Blood samples from the following 257 wild felids were analyzed: 35 Iberian lynxes from Spain, 36 Eurasian lynxes from Switzerland, 31 European wildcats from France, 45 lions from Tanzania, and 110 Brazilian wild felids, including 12 wild felid species kept in zoos and one free-ranging ocelot. Using real-time PCR, feline hemoplasmas were detected in samples of the following species: Iberian lynx, Eurasian lynx, European wildcat, lion, puma, oncilla, Geoffroy's cat, margay, and ocelot. "Candidatus Mycoplasma haemominutum" was the most common feline hemoplasma in Iberian lynxes, Eurasian lynxes, Serengeti lions, and Brazilian wild felids, whereas "Candidatus Mycoplasma turicensis" was the most prevalent in European wildcats; hemoplasma coinfections were frequently observed. Hemoplasma infection was associated with species and free-ranging status of the felids in all animals and with feline leukemia virus provirus-positive status in European wildcats. Phylogenetic analyses of the 16S rRNA and the partial RNase P gene revealed that most hemoplasma isolates exhibit high sequence identities to domestic cat-derived isolates, although some isolates form different subclusters within the phylogenetic tree. In conclusion, 9 out of 15 wild felid species from three different continents were found to be infected with feline hemoplasmas. The effect of feline hemoplasma infections on wild felid populations needs to be further investigated.

Aluminum toxicity to tropical montane forest tree seedlings in southern Ecuador: response of biomass and plant morphology to elevated Al concentrations

In acid tropical forest soils (pH < 5.5) increased mobility of aluminum might limit aboveground productivity. Therefore, we evaluated Al phytotoxicity of three native tree species of tropical montane forests in southern Ecuador. An hydroponic dose-response experiment was conducted. Seedlings of Cedrela odorata L., Heliocarpus americanus L., and Tabebuia chrysantha (Jacq.) G. Nicholson were treated with 0, 300, 600, 1200, and 2400 mu M Al and an organic layer leachate. Dose-response curves were generated for root and shoot morphologic properties to determine effective concentrations (EC). Shoot biomass and healthy leaf area decreased by 44 % to 83 % at 2400 mu M Al, root biomass did not respond (C. odorata), declined by 51 % (H. americanus), or was stimulated at low Al concentrations of 300 mu M (T. chrysantha). EC10 (i.e. reduction by 10 %) values of Al for total biomass were 315 mu M (C. odorata), 219 mu M (H. americanus), and 368 mu M (T. chrysantha). Helicarpus americanus, a fast growing pioneer tree species, was most sensitive to Al toxicity. Negative effects were strongest if plants grew in organic layer leachate, indicating limitation of plant growth by nutrient scarcity rather than Al toxicity. Al toxicity occurred at Al concentrations far above those in native organic layer leachate.

Aluminum toxicity in a tropical montane forest ecosystem in southern Ecuador

Aluminum phytotoxicity frequently occurs in acid soils (pH < 5.5) and was therefore discussed to affect ecosystem functioning of tropical montane forests. The susceptibility to Al toxicity depends on the sensitivity of the plant species and the Al speciation in soil solution, which can vary highly depending e.g., on pH, ionic strength, and dissolved organic matter. An acidification of the ecosystem and periodic base metal deposition from Saharan dust may control plant available Al concentrations in the soil solutions of tropical montane rainforests in south Ecuador. The overall objective of my study was to assess a potential Al phytotoxicity in the tropical montane forests in south Ecuador. For this purpose, I exposed three native Al non-accumulating tree species (Cedrela odorata L., Heliocarpus americanus L., and Tabebuia chrysantha (Jacq.) G. Nicholson) to increased Al concentrations (0 – 2400 μM Al) in a hydroponic experiment, I established dose-response curves to estimate the sensitivity of the tree species to increased Al concentrations, and I investigated the mechanisms behind the observed effects induced by elevated Al concentrations. Furthermore, the response of Al concentrations and the speciation in soil solution to Ca amendment in the study area were determined. In a final step, I assessed all major Al fluxes, drivers of Al concentrations in ecosystem solutions, and indicators of Al toxicity in the tropical montane rainforest in Ecuador in order to test for indications of Al toxicity. In the hydroponic experiment, a 10 % reduction in aboveground biomass production occurred at 126 to 376 μM Al (EC10 values), probably attributable to decreased Mg concentrations in leaves and reduced potosynthesis. At 300 μM Al, increased root biomass production of T. chrysantha was observed. Phosphorus concentrations in roots of C. odorata and T. chrysantha were significantly highest in the treatment with 300 μM Al and correlated significantly with root biomass, being a likely reason for stimulated root biomass production. The degree of organic complexation of Al in the organic layer leachate, which is central to plant nutrition because of the high root density, and soil solution from the study area was very high (mean > 99 %). The resulting low free Al concentrations are not likely to affect plant growth, although the concentrations of potentially toxic Al3+ increased with soil depth due to higher total Al and lower dissolved organic matter concentrations in soil solutions. The Ca additions caused an increase of Al in the organic layer leachate, probably because Al3+ was exchanged against the added Ca2+ ions while pH remained constant. The free ion molar ratios of Ca2+:Al3+ (mean ratio ca. 400) were far above the threshold (≤ 1) for Al toxicity, because of a much higher degree of organo-complexation of Al than Ca. High Al fluxes in litterfall (8.8 – 14.2 kg ha−1 yr−1) indicate a high Al circulation through the ecosystem. The Al concentrations in the organic layer leachate were driven by the acidification of the ecosystem and increased significantly between 1999 and 2008. However, the Ca:Al molar ratios in organic layer leachate and all aboveground ecosystem solutions were above the threshold for Al toxicity. Except for two Al accumulating and one non-accumulating tree species, the Ca:Al molar ratios in tree leaves from the study area were above the Al toxicity threshold of 12.5. I conclude that toxic effects in the hydroponic experiment occurred at Al concentrations far above those in native organic layer leachate, shoot biomass production was likely inhibited by reduced Mg uptake, impairing photosynthesis, and the stimulation of root growth at low Al concentrations can be possibly attributed to improved P uptake. Dissolved organic matter in soil solutions detoxifies Al in acidic tropical forest soils and a wide distribution of Al accumulating tree species and high Al fluxes in the ecosystem do not necessarily imply a general Al phytotoxicity.

The emergence of epitheliocystis in the upper Rhone region: evidence for Chlamydiae in wild and farm salmonid populations

We present the first study comparing epitheliocystis in a wild and farmed salmonid in Europe. Sampling three tributaries to the Lake Geneva, including one from headwaters to river mouth, revealed an unequal distribution of epitheliocystis in brown trout (Salmo trutta). When evaluated histologically and comparing sites grouped as wild versus farm, the probability of finding infected trout is higher on farms. In contrast, the infection intensities, as estimated by the number of cysts per gill arch, were higher on average and showed maximum values in the wild trout. Sequence analysis showed the most common epitheliocystis agents were Candidatus Piscichlamydia salmonis, all clustering into a single clade, whereas Candidatus Clavichlamydia salmonicola sequences cluster in two closely related sub-species, of which one was mostly found in farmed fish and the other exclusively in wild brown trout, indicating that farms are unlikely to be the source of infections in wild trout. A detailed morphological analysis of cysts using transmission electron microscopy revealed unique features illustrating the wide divergence existing between Ca. P. salmonis and Ca. C. salmonicola within the phylum Chlamydiae

Occurrence and abundance of late Early Cretaceous radiolarians at DSDP Leg 62 Holes

Well-preserved Mesozoic radiolarian faunas have been recovered at four sites of Deep Sea Drilling Project Leg 62. Late Early Cretaceous assemblages, which occur always with foraminifers or calcareous nannoplankton, allow the description of 21 new species, the introduction of a new zone scheme, and calibration of the radiolarian zones with the geochronological scale.

Cenozoic radiolaria in the western North Atlantic

Eight Cenozoic radiolarian zones were recognized in samples from two holes at Site 603, drilled on the lower continental rise off North America during Leg 93 of the Deep Sea Drilling Project. Paleocene to early Eocene radiolarian zones (Bekoma bidartensis, Buryella clinata, and Phormocyrtis striata striata zones) and early to late Miocene radiolarian zones (Calocycletta costata, Dorcadospyris alata, Diartus petterssoni, and Didymocyrtis antepenultima zones) were recognized in sediments from Holes 603 and 603B. In addition, a new Paleocene Bekoma campechensis radiolarian Zone is defined by the interval between the first morphotypic appearance of B. campechensis and the B. campechensis-B. bidartensis evolutionary transition. This zone is immediately below the B. bidartensis Zone of Foreman (1973), and has previously been discussed as a Paleocene "unnamed zone" by other investigators. A hiatus between Neogene and Paleogene sequences was also recognized in the radiolarian faunas.

Pollen and macrofossils profiles and age determination from three cores in Northeastern Kansas, U.S.A.

Two marshes near Muscotah and Arrington, Atchison County, northeastern Kansas, yielded a pollen sequence covering the last 25,000 yrs of vegetation development. The earliest pollen spectra are comparable with surface pollen spectra from southern Saskatchewan and southeastern Manitoba and might indicate a rather open vegetation but with some pine, spruce, and birch as the most important tree species, with local stands of alder and willow. This type of vegetation changed about 23,000 yrs ago to a spruce forest, which prevailed in the region until at least 15,000 yrs ago. Because of a hiatus, the vegetation changes resulting in the spread of a mixed deciduous forest and prairie, which was present in the region from 11,000 to 9,000 yrs ago, remain unknown. Prairie vegetation, with perhaps a few trees along the valleys, covered the region until about 5,000 yrs ago, when a re-expansion of deciduous trees began in the lowlands.