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We have determined the crystal structures of two decachlorocyclopentasilanes, namely bis(tetra-n-butylammonium) dichloride decachlorocyclopentasilane dichloromethane disolvate, 2C16H36N+·2Cl−·Si5Cl10·2CH2Cl2, (I), and bis(tetraethylammonium) dichloride decachlorocyclopentasilane dichloromethane disolvate, 2C8H20N+·2Cl−·Si5Cl10·2CH2Cl2, (II), both of which crystallize with discrete cations, anions, and solvent molecules. In (I), the complete decachlorocyclopentasilane ring is generated by a crystallographic twofold rotation axis. In (II), one cation is located on a general position and the other two are disordered about centres of inversion. These are the first structures featuring the structural motif of a five-membered cyclopentasilane ring coordinated from both sides by a chloride ion. The extended structures of (I) and (II) feature numerous C—H⋯Cl interactions. In (II), the N atoms are located on centres of inversion and as a result, the ethylene chains are disordered over equally occupied orientations.
Status and restoration potential of heathlands and sand grasslands in the southwest of Luxembourg
(2017)
In Europe, semi-natural nutrient-poor ecosystems such as sand grasslands and heathlands have shown extreme declines in surface area and species richness within the last century. The remaining sites are hence of high conservation value. This study analysed the vascular plant species inventory of established and recently restored heathlands and sand grasslands in the southwest of Luxembourg. Analyses to explain differences in vegetation composition between “old” (remnant sites or sites restored a long time ago) and “new” (recently restored) sites in relation to environmental variables were carried out with DCAs and ANOVA/Mann-Whitney-U tests, respectively. The vegetation of old heathlands had few character species of typical heathland communities (Calluno-Ulicetea, Nardetalia), whereas new heathland sites were preponderantly marked by taxa of meso- or eutrophic grasslands and ruderal communities. New heathland sites mainly differed from old sites by higher soil phosphorus contents. Sand grassland vegetation was species-rich and composed by species of the Sedo-Scleranthetea and Festuco-Brometea. With increasing age of the sites, vegetation composition shifted to grass dominance with species of the Molinio-Arrhenateretea. New sand grasslands differed from old sand grasslands by higher soil pH, higher soil potassium content and lower graminoid cover. The differences between new and old sites of both habitat types could mainly be explained by successional processes or were a result of topsoil removal. In some cases, former anthropogenic impact at or in close proximity of restored sites resulted in unsuitable conditions, such as alkaline soil on former landfill sites or highly eutrophic soil due to intensive agriculture. Future management options for the study sites are discussed.
This study describes the vascular flora and community structure of grasslands occurring on heaps of waste rock left by former Zn-Pb mining in relation to the metal content in the soil and other environmental factors. The study was performed on 65 heaps scattered in agricultural land in southern Poland. The sites were described in terms of plant community characteristics, soil physicochemical properties, distance from woodland, altitude and local climate. The number of plant species and proportion of species of the Festuco-Brometea class decreased with increasing heavy metal (Cd, Pb, Zn) content in the soil, and increased with Ca content and pH of the soil. There was a negative relationship between the proportion of the later successional species and heavy metal content in the soil and a positive relationship between plants connected with the earlier stages of succession and metals. Floristic composition was also affected by distance from woodland and height above sea level. The investigated heaps were primarily colonised by native species dispersed by wind, characterised as competitive stresstolerant, ruderal and competitive strategy species. Three types of Carlino acaulis-Brometum erecti (CB) communities were distinguished: CB typicum – dominated by Brachypodium pinnatum, with the highest proportion of calcareous grassland species, CB festucetosum ovinae subass. nova – loose grassland with abundant facultative metallophytes, and the CB rubietosum caesi subass. nova with nutrientdemanding ruderal and woody plants invading from the nearby forest communities. The three subassociations represent different successional stages of Carlino acaulis-Brometum erecti, strongly dependent on both the substrate and spatial relations. The proportions of species traits, especially a high occurrence of endangered species and a very low proportion of alien species show that the post-mining habitats studied have a similar degree of ‘naturalness’ as valuable xerothermic grasslands on nonmetalliferous habitats. They thus may be considered as valuable objects for the protection of plant diversity.
This paper provides a comprehensive survey of the results of phytocoenological research into Alnus incana forests from the alliance Alnion incanae in the Dinarides. Stands from the south-eastern Dinarides (Alnetum incanae = Oxali-Alnetum incanae) were analyzed and compared with those from the north-western Dinarides (Lamio orvalae-Alnetum incanae). The comparison reveals significant differences in the floristic composition and in the degree of differentiation – and particularly in the presence of the species of the Illyrian floristic geoelement. Focus was placed on the area of western Croatia where a geographic variant of Helleborus dumetorum had previously been defined within the association Lamio orvalae-Alnetum incanae. Two of its subtypes, Salix alba and Alnus glutinosa, were determined in our research. The former subtype thrives on occasionally flooded, moist sites, where the floristic composition is dominated by hygrophytes. The latter subtype grows on elevated and drier terraces and is richer in mesophilous species from the surrounding zonal forests. A floristic-sociological comparison of the Lamio orvalae-Alnetum incanae with the related syntaxa indicates the presence of about fourty diagnostic species which accentuate its independence and the need to assess it at the level of an independent, regional association within the alliance Alnion incanae.
The aim of our study was to reveal the differences in the species composition and soil properties of open sandy grasslands dominated by different Festuca species, Festuca vaginata and F. pseudovaginata. Due to the arid conditions, sandy grasslands are generally covered by xerothermic vegetation in which F. vaginata is a typical dominant species. Festuca pseudovaginata, a species newly described by the authors, can also gain dominance in sandy grasslands. However, species composition and soil properties of grasslands dominated by this recently discovered species are still undiscovered. Based on previous coenological studies, we hypothesised that the grasslands characterised by the endemic F. vaginata are more species-rich than those with F.pseudovaginata.
Coenological sampling was carried out in May 2009 at two study sites using the Braun-Blanquet method in quadrats of 2 m × 2 m. Five relevés were sampled in stands dominated by F. vaginata and F. pseudovaginata respectively at two study sites in Central Hungary, resulting in a total of twenty relevés. Analyses were based on the cover scores of vascular plant species and cryptogam crust and values of seven soil properties (pH [KCl], pH [H2O], humus, total N, Ca, P2O5 and K2O) measured in the 0–15 and 15–30 cm soil layers. Soil properties of the grasslands dominated by F. pseudovaginata and F. vaginata (dependent variables) were compared by linear mixed models, where ‘grassland type’ was the fixed factor and ‘site nested in grassland type’ was considered as random factor. Data were analysed by cluster analysis, fusion algorithm was a combinatorial method (minimising increase of variance), and the correlation was used as comparative function. We compared the cover of subordinate species by Mann-Whitney U test. We found that F. pseudovaginata and F. vaginata samples were well separated, and grasslands dominated by F. pseudovaginata had nearly two times more species than those dominated by F. vaginata. Based on the cluster analyses using plant cover and upper 0–15 cm soil layer data, F. pseudovaginata and F. vaginata groups could be well separated. Linear mixed models revealed that F. vaginata grasslands were typical on soils with higher pH, nitrogen, phosphorous and potassium contents compared to F. pseudovaginata grasslands, which indicates a tight connection between the properties of the upper soil layer and the vegetation in sandy grasslands.
Bromus racemosus L. is a rather rare grass species of moist meadows. It has strongly decreased in the course of the 20th century due to intensification of agricultural grassland management, and is therefore included in Red Lists of several European countries. Its winter annual life-cycle is remarkable for a species of permanent grasslands.
The aim of this study is to determine the habitat preference and optimal management of B. racemosus in the Netherlands and surrounding countries. Vegetation, soil and hydrological data from 28 sites in the Netherlands have been compared with B. racemosus cover, and with vegetation data from surrounding countries. The results indicate that B. racemosus is characteristic of Molinio-Arrhenatheretea meadows with good mineralisation and aftermath grazing. The optimum lies in grasslands of the alliance Alopecurion pratensis (Deschampsion cespitosae), but the species ranges from wetter Calthion palustris meadows to drier Arrhenatherion elatioris and Cynosurion cristati grasslands. It prefers intermediate nutrient levels and hydrological conditions (mesic sites), but within this range the highest cover is found in relatively nutrient rich and dry sites. Because of the absence of a seedbank and a low dispersal capability, B. racemosus is vulnerable to changes in grassland management. A management of mowing after 15 June and aftermath grazing is most suitable, since it enables fruit ripening and the maintenance of an open sward, needed for germination and development. The risk of extinction is likely to be higher in flat polders than in floodplain sites with natural relief, where the species may shift between belts in different years.
Vegetation patterns of floodplain forests are highly variable across different habitats in European regions. Their plant communities have been well described from the phytosociological point of view, but plant species richness and composition patterns and their underlying environmental factors are still insufficiently known. Sixty-one vegetation plots of black alder-dominated floodplain forests were sampled in central Slovakia in order to find main environmental predictors affecting floristic diversity of their vegetation. For each vegetation plot with a constant size (400m2), vascular plant species and a set of topographic, climatic, soil physical and chemical characteristics were recorded. A generalized linear model was applied to explain relevance of environmental factors on changes of species richness, whereas the relationship between species composition and explanatory variables was tested using ordination methods. Main gradients of species compositional variation were soil moisture, light, elevation and soil chemistry-related variables. Vascular species richness of plots varied between 19 and 59 (mean 38). Herb-layer species richness was positively related to the soil pH, stream power index and negatively to the concentration of soil iron. These linear trends were accompanied by a hump-shaped response to sand content and a U-shaped response to elevation.
Bacteria are highly organized organisms which are able to adapt to and propagate under a multitude of environmental conditions. Propagation hereby requires reliable chromosome replication and segregation which has to occur cooperatively with other cellular processes such as transcription, translation or signaling. Several mechanisms were proposed for segregation of the Escherichia coli (E. coli) chromosome, for example a mitotic-like active segregation model or entropy-based passive chromosome segregation. Another segregation model suggests coupled transcription, translation and insertion of membrane proteins (termed "transertion"), which links the replicating chromosome (nucleoid) to the growing cell cylinder.
Fluorescence microscopy was widely used to provide evidence for a distinct segregation model. However, the dynamic nature of bacterial chromosomes, the small bacterial size and the optical resolution limit of ~ 200-300 nm impair unveiling the underlying mechanisms. With the emergence of super-resolution fluorescence microscopy techniques and advanced labeling methods, a new toolbox became available enabling scientists to visualize biomolecules and cellular processes in unprecedented detail. Single-molecule localization microscopy (SMLM) represents a set of super-resolution microscopy techniques which relies on the temporal separation of the fluorescence signal and detection of single fluorophores. Separation can be achieved using photoactivatable or -convertible fluorescent proteins (FPs) in photoactivated localization microscopy (PALM), photoswitchable organic dyes in direct stochastic optical reconstruction microscopy (dSTORM) or dynamically binding fluorescent probes in point accumulation for imaging in nanoscale topography (PAINT). In all these techniques, the fluorescence emission pattern of single fluorophores is spatially localized with nanometer-precision. An artificial image is finally reconstructed from the coordinates of all single fluorophores detected. This provides a spatial resolution of ~ 20 nm, which is perfectly suited to investigate cellular processes in bacteria. In this thesis, different SMLM techniques were applied to study fundamental processes in E. coli. This includes determination of protein copy numbers and distributions as well as the nanoscale organization of nucleic acids and lipids.
A novel labeling approach was applied and used for super-resolution imaging of the E. coli nucleoid. It is based on the incorporation of the modified thymidine analogue 5-ethynyl-2’- deoxyuridine (EdU) into the replicating chromosome. Azide-functionalized organic fluorophores can be covalently attached to the ethynyl group of incorporated EdU bases using a copper-catalyzed "click chemistry" reaction. Under the investigated growth condition, E. coli cells exhibited overlapping replication cycles, which is commonly referred to as multi-fork replication and enables cells to divide faster than they can replicate the entire chromosome. dSTORM imaging of such labeled nucleoids revealed chromosome features with diameters of 50 - 200 nm, representing highly condensed DNA filaments. Sorting single E. coli cells by length allowed visualizing structural changes of the nucleoid throughout the cell cycle. Replicating nucleoids segregated and expanded along the bacterial long axis, while constantly covering the entire width of the cell. Measuring cell and nucleoid length revealed a relative nucleoid expansion rate of 78 ± 6 %. At the same time, nucleoids populated 63 ± 8 % of the cell length, almost exclusively being localized to the cylindrical part of the cell. This value was hence normalized to the cylindrical fraction of the cell, yielding a value of 79 ± 10 % (nucleoid-populated fraction of the cell cylinder), which is in good agreement with the observed relative nucleoid expansion rate. These results therefore support a growth-mediated segregation model, in which the chromosome is anchored to the inner membrane and passively segregated into the prospective daughter cells upon cell growth. 3-dimensional dSTORM imaging of labeled nucleoids confirmed that compacted nucleoids helically wrap along the inner membrane. Similar results were obtained by imaging orthogonally aligned E. coli cells using a holographic optical tweezer approach.
In order to visualize particular proteins together with the nucleoid, several correlative imaging workflows were established, facilitating multi-color SMLM imaging in single E. coli cells. These workflows bypass prior limitations of SMLM, including destruction of FPs by reactive oxygen species in copper-catalyzed click reactions or incompatibility of PALM imaging with dSTORM imaging buffers. A sequential SMLM imaging routine was developed which is based on postlabeling and retrieval of previously imaged cells. Optimal imaging conditions can be maintained for each fluorophore, enabling to extract quantitative information from PALM measurements while correlating the protein distribution to the nucleoid ultrastructure within the highly resolved cell envelope. Applying this workflow to an E. coli strain carrying a chromosomal rpoC - photoactivatable mCherry (PAmCh) fusion, transcribing RNA polymerase (RNAP) was found to be localized on the surface of nucleoids, where active genes are exposed towards the cytosol. During growth in nutrient-rich medium, the majority of RNAP molecules was bound to the chromosome, thus ensuring that the RNAP pool is equally distributed to the daughter cells upon cell division. This work represented the first triple-color SMLM study performed in E. coli cells. ...
The East African Rift System (EARS) was initiated in the Eocene epoch between 50 and 21 Ma probably due to the influence of mantle plumes that caused volcanism, flood basalts and rifting extensions in Ethiopa and the Afar region. As a result of magmatic intrusions and adiabatic decompression melting within the lithosphere caused by the impact of the Kenya plume, there was a southward propagation of the EARS of about 30 – 15 Ma from Ethiopia to Kenya, which coincide with the occurrence of volcanism. The EARS developed towards the south along the margins of the Tanzania Craton between 15 and 8 Ma. Previous findings of low-velocity anomalies within the upper mantle and the mantle transition zone indicate an upwelling of hot mantle material in the vicinity of the Afar region and the East African Rift. This study includes the analysis of P- and S-receiver functions in order to determine further impacts on the lithosphere from below. The aim was to determine the topographic undulations of further boundary layers and to identify their variability owing to the rifting processes and the formation of the EARS. The study area included the Tanzania Craton and the surrounding rift branches of the East African Rift System.
The region of the Rwenzori Mountains can be analysed in detail because of the large dataset of the RiftLink project. The use of the P-receiver function technique and the H-K stacking method enabled to determine different vP /vS ratios depending on the tectonic setting in the Rwenzori region: Rift shoulders (vP /vS =1.74), Albert Rift segment (vP /vS =1.80), Edward Rift segment (vP /vS =1.87) and Rwenzori Mountains (vP /vS =1.86). To determine the topography of the Moho, it is necessary to take into account the thickness of the sedimentary layer, the surface topography, the azimuthal variations in crustal thickness and the impact of local anomalies. After correcting these effects on the Moho depths, significant variations in Moho topography could be determined. The Moho depths range from 29 to 39 km beneath the rift shoulders of the Albertine Rift. Within the rift valley, the crustal thickness varies between 25 – 31 km in the Edward Rift segment and 22 – 30 km in the Albert Rift segment. An averaged crustal thickness of about 26 km within the rift valley indicates the lack of the crustal root beneath the Rwenzoris. Similar variations in crustal thickness were determined by using an automatic procedure for analysing S-receiver functions that was developed in this study.
The S-receiver functions are created by applying a rotation criterion in order to rotate the Z, N and E components into the L, Q and T components. It is necessary to perform trial rotations using different incident and azimuth angles to determine the correct rotation angles. The latter are identified by the use of the rotation criterion, including the amplitude ratio of the converted Moho signal to the direct S/SKS-wave signal. The L component is rotated correctly in the direction of the incident shear wave in the case of the maximum amplitude ratio. After analysing the frequency content of the receiver functions in order to sort out harmonic and long-periodic traces, the individual Moho signals are checked for consistency in order to remove atypic signals. To increase the signal-to-noise ratios on the traces, the S-receiver functions are stacked. For this purpose, the signals of the direct shear waves must originate from similar epicenters. On the basis of similar ray paths, the receiver functions show comparable waveforms and converted signals. To perform the stacking procedure, it is necessary to merge the datasets of the adjacent stations in order to obtain a sufficient number of receiver functions. This analysis is based on the assumption that the incident seismic waves arriving at the adjacent stations penetrate to some extent the same underground structures in the case of similar wave propagation paths. This approach accounts for the fact that the converted signals do not result exclusively from the piercing points at the boundary layers. Further signals originate from the conversions at the boundary layer within the Fresnel Zone. The piercing points are derived from the significant signals in the receiver functions. Depending on the order of arrival of the converted phases on the traces, the signals are attributed to the theoretical discontinuities DIS1, DIS2, DIS3 and DIS4. However, partly due to the low signal-to-noise ratios on the traces, it is difficult to identify the real conversions on the traces and to ensure that the converted signals are attributed to the correct boundary layers. For this reason, it is necessary to check the consistency of the conversion depths among each other. In the case of inconsistent conversion depths, the corresponding signals are either adjusted to another seismic boundary layer or removed from the dataset. To verify the functionality of the automatic procedure and to determine the resolvability with respect to two boundary layers, several models are tested including horizontal and dipping discontinuities. To resolve distinct discontinuities, their depths must differ by at least 60 km, otherwise, due to similar depth ranges of the different boundary layers, the converted signals cannot be separated from each other. As a consequence, the converted signals that originate from different discontinuities are attributed to a single one. Further tests including break-off edges of seismic discontinuities are performed to check the attributions of the converted signals to the discontinuities. Owing to the varying number of boundary layers, the converted signals cannot be attributed to the discontinuities according to the order of their arrivals on the traces. It is necessary to correct their attributions to the seismic discontinuities in order to resolve the boundary layers.
The crust-mantle boundary and further discontinuities within the lithospheric mantle are investigated by applying this automatic procedure. Depending on the tectonic setting, the conversion depths of the Moho range from about 30 – 45 km beneath the western rift shoulder to 20 – 35 km within the rift valley up to 30 – 40 km beneath the eastern rift shoulder. The long wavelengths of the shear waves hamper the correct identification of the converted phases in the S-receiver functions. With respect to the relative differences in conversion depth, the topographic undulations of the crust-mantle boundary are consistent with the Moho depths derived from P-receiver functions. In contrast to the Rwenzori region, it is difficult to resolve completely the trend of the Moho in the remaining area of the East African Rift due to the small dataset provided by IRIS. The results exibit an increase in crustal thickness to up to 45 km in the region of the Cenozoic volcanics such as Virunga, Kivu, Rungwe and Kenya. The greatest Moho depths of more than 50 km are located near Mount Kilimanjaro. In addition to the Moho, the analysis of the S-receiver functions revealed two further boundary layers at depths of 60 – 140 km and 110 – 260 km, which are associated with a mid-lithospheric discontinuity and the lithosphere-asthenosphere boundary, respectively. The shallowest conversion depths of the LAB are focussed to small-scale regions within the rift branches, namely the northern Albertine Rift, the Chyulu Hills and the Mozambique Belt, which are located around the Tanzania Craton. The larger thickness of the lithosphere beneath the cratonic terrain indicates that the Tanzania Craton is not significantly eroded. However, there are indications that the lithosphere beneath the craton and the rift branches is penetrated by ascending asthenospheric melts to depths of up to 140 and 60 km, respectively. The top of the ascending melts is associated with the occurrence of the mid-lithospheric discontinuity. The shallowest conversion depths of this boundary layer (60 – 90 km) are related to the rifted areas of the EARS and the Cenozoic volcanic provinces, which are located along the Albertine Rift, the Kenya Rift and the Rukwa-Malawi rift zones. The deepest conversion depths of up to 140 km are related to the Rwenzori Belt, the Ugandan Basement Complex and the interior of the Tanzania Craton.
Ziel dieser Dissertation war es, die biologische Rolle der Autophagie für die Entwicklung, Alterung und mitochondriale Qualitätskontrolle in dem Ascomyceten Podospora anserina zu untersuchen. Folgende Ergebnisse wurden dabei erzielt:
1. Der Verlust einer funktionalen Autophagie-Maschinerie ist in P. anserina mit einem Defekt der Sporen-Entwicklung bzw. -Keimung charakterisiert.
2. Es konnten drei Methoden zur Untersuchung der Autophagie in P. anserina etabliert werden: 1) Die Verwendung eines Gfp::PaAtg8-Stamms ermöglicht die Fluoreszenzmikroskopische Bestimmung der Autophagosomen-Anzahl; 2) Die phänotypische Charakterisierung des PaAtg1-Deletionsstamms unter verschiedenen Stressbedingungen (z. B. Stickstoffmangel, Rapamycin) liefert Hinweise auf eine mögliche Autophagie-abhängige Stressadaption; 3) Die Verwendung des „GFPcleavage assays“ ermöglicht einen quantitativen Nachweis genereller und selektiver Autophagie (hier: Mitophagie).
3. In zwei voneinander unabhängigen Experimenten wurde ein altersabhängiger Anstieg der Autophagie für P. anserina demonstriert: Das Autophagie-Niveau nimmt in gealterten P. anserina-Kulturen zu. Gleichzeitig resultiert der Verlust der Autophagie in ∆PaAtg1 in eine reduzierte Lebensspanne. Unter Stressbedingungen (hier: Stickstoffmangel) wird dieser positive Einfluss der Autophagie auf die Lebensspanne im Wildtyp sogar noch verstärkt.
4. Der unerwartet „gesunde“ Phänotyp der PaSod3-Deletionsmutante ist abhängig von einer funktionalen Autophagie-Maschinerie. Der Mitophagie wurde eine besondere Rolle als Kompensationsmechanismus für den Verlust von PaSOD3 zugeteilt, da das Mitophagie-Niveau in dieser Mutante erhöht ist. Am Beispiel dieser Mutante, für die ein erhöhter Superoxid-Ausstoß nachgewiesen wurde, konnte eine Dosis-abhängige Wirkung von ROS in P. anserina identifiziert werden. Eine geringe zelluläre ROSMenge verursacht eine mitohormetische Reaktion, die eine Induktion der Mitophagie zur Folge hat und sich positiv auf den Organismus auswirkt. Übersteigt die zelluläre ROS-Dosis einen kritischen Punkt, kommt es zur Induktion des autophagischen Zelltods und damit zum vorzeitigen Tod des Individuums.
5. Der Verlust der PaCLPXP-Protease führt zu Beeinträchtigungen in der Funktion und Zusammensetzung der mitochondrialen Atmungskette. Dieses Defizit im Energiemetabolismus wird über eine Induktion der AOX, vor allem aber über eine ZUSAMMENFASSUNG 127 gesteigerte Autophagie kompensiert. Die deutlich verlängerte Lebensspanne der verschiedenen PaClpXP-Deletionsmutanten (∆PaClpX, ∆PaClpP und ∆PaClpXP) ist abhängig von einer funktionalen Autophagie-Maschinerie. Interessanterweise konnte keine kompensatorische Funktion der Autophagie oder Mitophagie für den Verlust der mitochondrialen i-AAA-Protease PaIAP in P. anserina nachgewiesen werden.
Autophagie/Mitophagie stellt einen übergeordneten Qualitätskontrollmechanismus in P. anserina dar, der den Organismus sehr effektiv vor zellulären Schäden und Dysfunktionen bewahrt und einen positiven Einfluss auf die Alterung, Entwicklung und Energieversorgung einnimmt.
Background: Isolated transient vertigo can be the only symptom of posterior circulation ischemia. Thus, it is important to differentiate isolated vertigo of a cerebrovascular origin from that of more benign origins, as patients with cerebral ischemia have a much higher risk for future stroke than do those with "peripheral" vertigo. The current study aims to identify risk factors for cerebrovascular origin of isolated transient vertigo, and for future cerebrovascular events.
Methods: From the files of 339 outpatients with isolated transient vertigo we extracted history, clinical and technical findings, diagnosis, and follow-up information on subsequent stroke or transient ischemic attack (TIA). Risk factors were analyzed using multivariate regression models (logistic or Cox) and reconfirmed in univariate analyses.
Results: On first presentation, 48 (14.2%) patients received the diagnosis "probable or definite cerebrovascular vertigo". During follow-up, 41 patients suffered stroke or TIA (event rate 7.9 per 100 person years, 95% confidence interval (CI) 5.5–10.4), 26 in the posterior circulation (event rate 4.8 per 100 person years, 95% CI 3.0–6.7). The diagnosis was not associated with follow-up cerebrovascular events. In multivariate models testing multiple potential determinants, only the presentation mode was consistently associated with the diagnosis and stroke risk: patients who presented because of vertigo (rather than reporting vertigo when they presented for other reasons) had a significantly higher risk for future stroke or TIA (p = 0.028, event rate 13.4 vs. 5.4 per 100 person years) and for future posterior circulation stroke or TIA (p = 0.044, event rate 7.8 vs. 3.5 per 100 person years).
Conclusions: We here report for the first time follow-up stroke rates in patients with transient isolated vertigo. In such patients, the identification of those with cerebrovascular origin remains difficult, and presentation mode was found to be the only consistent risk factor. Confirmation in an independent prospective sample is needed.
Functional imaging studies using BOLD contrasts have consistently reported activation of the supplementary motor area (SMA) both during motor and internal timing tasks. Opposing findings, however, have been shown for the modulation of beta oscillations in the SMA. While movement suppresses beta oscillations in the SMA, motor and non-motor tasks that rely on internal timing increase the amplitude of beta oscillations in the SMA. These independent observations suggest that the relationship between beta oscillations and BOLD activation is more complex than previously thought. Here we set out to investigate this rapport by examining beta oscillations in the SMA during movement with varying degrees of internal timing demands. In a simultaneous EEG-fMRI experiment, 20 healthy right-handed subjects performed an auditory-paced finger-tapping task. Internal timing was operationalized by including conditions with taps on every fourth auditory beat, which necessitates generation of a slow internal rhythm, while tapping to every auditory beat reflected simple auditory-motor synchronization. In the SMA, BOLD activity increased and power in both the low and the high beta band decreased expectedly during each condition compared to baseline. Internal timing was associated with a reduced desynchronization of low beta oscillations compared to conditions without internal timing demands. In parallel with this relative beta power increase, internal timing activated the SMA more strongly in terms of BOLD. This documents a task-dependent non-linear relationship between BOLD and beta-oscillations in the SMA. We discuss different roles of beta synchronization and desynchronization in active processing within the same cortical region.
Over the last several decades, spinel-structured minerals with the chemical formula AB2O4 (where A and B stand for divalent and trivalent cations, respectively) have attracted more and more attention, particularly with regards to their breakdown at high pressures and temperatures and the nature of the so-called "post-spinel" phases. Spinel-structured phases with different endmember compositions, like magnetite (Fe3O4), hercynite (FeAl2O4) or spinel (MgAl2O4), are known to breakdown differently at high pressure-temperature conditions (e.g., Akaogi et al. 1999; Schollenbruch et al. 2010; Woodland et al. 2012). Such phases are of particular interest when they incorporate ferric (Fe3+) and ferrous (Fe2+) cations as this makes their stability sensitive to redox conditions. Since magnetite and magnesioferrite (MgFe3+ 2O4) have been found as inclusions in diamond (e.g., Stachel et al. 1998; Harte et al. 1999; Wirth et al. 2014; Palot et al. 2016; Jacob et al. 2016), understanding their phase relations is important for setting constraints on the conditions of their formation.
This study aimed to experimentally investigate the phase relations of Fe-Mg spinel-structured phases at conditions of the deep upper mantle and transition zone. Exploring the stability of new post-spinel phases and their characterization were also major goals of this study. Approaching a pyrolitic mantle composition by adding amounts of SiO2 in the system allowed constraints on the relevance of Fe-Mg post-spinel phases coexisting with mantle silicates to be made. ...
Reactive oxygen species are produced transiently in response to cell stimuli, and function as second messengers that oxidize target proteins. Protein-tyrosine phosphatases are important reactive oxygen species targets, whose oxidation results in rapid, reversible, catalytic inactivation. Despite increasing evidence for the importance of protein-tyrosine phosphatase oxidation in signal transduction, the cell biological details of reactive oxygen species-catalyzed protein-tyrosine phosphatase inactivation have remained largely unclear, due to our inability to visualize protein-tyrosine phosphatase oxidation in cells. By combining proximity ligation assay with chemical labeling of cysteine residues in the sulfenic acid state, we visualize oxidized Src homology 2 domain-containing protein-tyrosine phosphatase 2 (SHP2). We find that platelet-derived growth factor evokes transient oxidation on or close to RAB5+/ early endosome antigen 1− endosomes. SHP2 oxidation requires NADPH oxidases (NOXs), and oxidized SHP2 co-localizes with platelet-derived growth factor receptor and NOX1/4. Our data demonstrate spatially and temporally limited protein oxidation within cells, and suggest that platelet-derived growth factor-dependent “redoxosomes,” contribute to proper signal transduction.
A great challenge in life sciences remains the site-specific modification of proteins with minimal perturbation for in vitro as well as in vivo studies. Therefore, different chemoselective reactions and semi-synthetic techniques such as native chemical ligation or intein-mediated protein splicing have been established. They enable a site-specific incorporation of chemical reporters into proteins, such as organic fluorophores or unnatural amino acids. In this PhD Thesis, protein trans-splicing was guided by minimal high-affinity interaction pairs to trace proteins in mammalian cells. In addition, the temporal modulation of cellular processes by photo-cleavable viral immune evasins was achieved.
Protein trans-splicing mediated by split inteins is a powerful technique for site-specific and 'traceless' protein modifications. Despite recent developments there is still an urgent need for ultra-small high-affinity intein tags for in vitro and in vivo approaches. So far, only a very few in-cell applications of protein trans-splicing are reported, all limited to C-terminal protein modifications. Here, a strategy for covalent N-terminal intein-mediated protein labeling at sub-nanomolar probe concentrations was developed. Combined with the minimalistic Ni-trisNTA/His-tag interaction pair, the affinity between the intein fragments was increased 50-fold (KD ~ 10 nM). Site-specific and efficient 'traceless' protein modification by high-affinity trans-splicing is demonstrated at nanomolar concentrations in mammalian cells.
High background originating from non-reacted, 'always-on' fluorescent probes still is a crucial issue in life sciences. Covalent labeling approaches with simultaneous activation of fluorescence are advantageous to increase sensitivity and to reduce background signal. Therefore, high-affinity protein trans-splicing was combined with fluorophore/quencher pairs for online detection of covalent N-terminal protein labeling in cellular environments. Substantial fluorescence enhancement at nanomolar probe concentrations was achieved. This ultra-small fluorogenic high-affinity split intein system is an unprecedented example for real-time monitoring of the trans-splicing reaction in cell-like environments as well as for protein labeling with fluorogenic probes at nanomolar concentrations.
To extend the field of chemical immunology and to address spatiotemporal aspects in adaptive immune response, new tools to control antigen processing are required. Therefore, synthetic photo-conditional viral immune evasins were designed to modulate antigen processing on demand. By using light, the time and dose controlled antigen translocation by the transporter associated with antigen processing (TAP) was triggered with response in the second regime. Peptide delivery and loading by the peptide-loading complex (PLC) was rendered inactive, whereas blocking was abolished in a light-controlled fashion to inactivate the synthetic viral immune evasin ICP47 along with simultaneous activation of the antigen presentation pathway. Lightresponsive peptide translocation by the TAP complex was assayed in vitro by utilizing microsomes isolated from professional antigen presenting B-cell lymphomas (Raji). To extend these studies, suppression and photo-controlled rescue of antigen presentation was examined at single-cell resolution in human primary immune cells.
Native chemical ligation interconnects peptide chemistry with recombinantly expressed proteins. This technique was applied to generate the semi-synthetic full-length ICP47. Although this approach was realized, the low product yield was not sufficient for further functional studies. Therefore, full-length ICP47 was consecutively generated by utilizing a full synthetic four-fragment ligation approach. However, this synthetic viral immune evasin was not able to block peptide translocation in a robust way.
Die vorliegende Arbeit hat das Ziel, Plasmen koaxialer Beschleuniger in Hinblick auf die Erzeugung hoher Elektronendichten sowie als intensive UV/VUV-Backlighterquelle zu untersuchen. Hierzu wurde zunächst die Geometrie eines einzelnen Beschleunigers charakterisiert und optimiert, um die bestmöglichen Voraussetzungen für die anschließend durchgeführten Untersuchungen zur Kollision und Kompression der erzeugten Plasmen zu schaffen.
Das Funktionsprinzip des verwendeten Plasmabeschleunigers basiert auf einer Lorentzkraft, die aus dem Stromfluss zwischen zwei koaxial angeordneten Elektroden und dem damit verbundenen Magnetfeld resultiert. Da weder Stromdichte noch Magnetfeld homogen sind, wirkt auch die Lorentzkraft inhomogen auf die Plasmaschicht. Unter Einbeziehung von Simulationen wurde der Abstand zwischen den Elektroden auf 2,5 mm gesetzt, sodass die Ausprägung dieser Inhomogenität möglichst gering gehalten wird. Um ein Pinchen des Plasmas am Ende der Elektroden zu vermeiden haben die Elektroden im Gegensatz zu Plasma Focus Devices die gleiche Länge. Der mit 130 nH niederinduktive elektrische Aufbau ermöglicht die zur Ausbildung einer Plasmaschicht erforderlichen Stromanstiegsraten in der Größenordnung von 10^11 A/s.
Die Messung der Geschwindigkeit der Plasmaschicht erfolgte mit einem Array aus sechs Dioden, die gleichzeitig die Geschwindigkeitsabnahme im Rezipienten dokumentieren. Zusätzlich wurden die Messungen mit Kameraaufnahmen verglichen. Bei einer Elektrodenlänge von 100 mm konnten mit dem verwendeten Heliumgas Schichtgeschwindigkeiten von bis zu (79,49 ± 7,98) km/s erreicht werden. Die Untersuchung von Elektroden mit 200 mm Länge verfolgte das Ziel, durch die größere Beschleunigungszeit höhere Geschwindigkeiten und kinetische Energien der austretenden Plasmaschicht zu erreichen. Es zeigte sich jedoch, dass es hierbei zur Ausbildung einer zweiten Entladung und einer damit verbundenen Abbremsung des Initialplasmas kommt. Die Untersuchungen ergaben, dass die optimale Elektrodenlänge dadurch gegeben ist, dass der Austritt des Plasmas aus dem Beschleuniger zum Zeitpunkt des ersten Stromnulldurchgangs erfolgt. Für die Berechnung der optimalen Elektrodenlänge wurde ein Skalierungsgesetz gefunden, die auf experimentellen Ergebnissen und Simulationen basiert.
Mit spektroskopische Messungen der Stark-Verbreiterung der Hβ-Linie konnte die Elektronendichte des Plasmas zeit- und ortsintegriert bestimmt werden. Die hierbei erzielte Maximaldichte von (6,83 ± 0,83) · 10^15 cm^-3 wurde bei 9 kV und 70 mbar gemessen. Die nach der Boltzmann-Methode zeit- und ortsintegriert bestimmten Elektronentemperaturen bewegt sich bei etwa 1 eV.
Nach ausreichender Charakterisierung des Einzelbeschleunigers wurde das Experiment um einen zweiten, baugleichen Plasmabeschleuniger erweitert, um die planare Kollision zweier Plasmen zu untersuchen. Die maximal gemessene Elektronendichte von n max e = (1,36 ± 0,21) · 10^16 cm^-3 bei 9 kV und 70 mbar stellt im Vergleich zum Einzelplasma eine Steigerung um einen Faktor von 2,48 dar und ist mit einer Temperaturerhöhung einhergehend. Diese Elektronendichteerhöhung lässt sich nicht durch einfaches Durchdringen der Schichten erklären. Vielmehr muss es in der Kollisionszone zu Wechselwirkungsprozesse in Form von Kompression, zur Erzeugung neuer Ladungsträger oder der Kombination aus beidem kommen.
Das Spektrum im UV/VUV-Bereich weist Linien von ab 85 nm auf. Dies stellt eine Verbesserung gegenüber dem Einzelbeschleuniger dar, bei dem die hochenergetischste Spektrallinie erst bei 97 nm gemessen wurde. In der Kollisionskonfiguration mit einem Beschleunigerabstand von 30 mm steigt die integrierte Gesamtintensität des Spektrums bis 300 nm zudem um einen Faktor von etwa 5,2.
Als Alternative zur Plasmakollision wurde die Kompression des Plasmas des Einzelbeschleunigers durch unterschiedliche Trichtergeometrien untersucht. Die untersuchten Trichter der ersten und zweiten Generation unterscheiden sich im Wesentlichen im Durchmesser der kleineren Öffnung. Dieser wurde basierend auf Simulationen von 5 mm auf 0,5 mm reduziert. Die Dichtediagnostik der ersten Trichtergeneration erfolgte hierbei über Hα-Linie, da die Verbreiterung der Hβ-Linie zu stark und daher nicht mehr anwendbar war. Die Auswertung der Halbwertsbreiten der Hα-Linie führt zu Elektronendichten in der Größenordnung von bis zu 1018 cm−3 bei Spannungen von 9 kV. Diese Steigerung um 1,5 bis 2,5 Größenordnungen im Vergleich zum Einzelbeschleuniger ist deutlich höher als das Verhältnis der Flächen des initialen Plasmas bzw. dem Ende des Trichters von etwa acht.
Der Trichter mit verringerter Öffnung wurde bei 5 kV und 5 mbar vermessen, um die mechanische Belastung durch den hohen Druck gering zu halten. Die Bestimmung der Elektronendichte erfolgte durch die Verbreiterung der Kupferlinie bei 479,4 nm nach den quadratischen Stark-Effekt. Trotz der im Vergleich zur ersten Trichtergeneration reduzierten Entladungsenergie und verringertem Druck sind die gemessenen Elektronendichten ebenfalls bei bis zu 10^18 cm^-3.
Durch die Kompression des Plasmas weist das Spektrum im UV/VUV-Bereich bereits Linien ab Wellenlängen etwa 53 nm auf, wobei es unter Berücksichtigung der Transmissionsgrenze von Helium bei 50 nm denkbar ist, dass das Plasma noch niedrigere Wellenlängen emittiert.
Aufgrund der gesammelten Ergebnisse lässt sich festhalten, dass sich die Elektronendichte sowohl durch die Kollision zweier Plasmen als auch durch die Kompression in Trichtergeometrien steigern lässt. Der Verdichtungseffekt der Trichterkompression ist hierbei um ein vielfaches höher, als bei der Plasmakollision. Dies spiegelt sich auch im UV/VUV-Spektrum wider. Beide Versuchsanordnungen eignen sich als Linienstrahler, allerdings weist das Spektrum der Trichterkompression Linien deutlich höherer Anregungszustände auf.
Indian Ocean came into existence with the breakup of Gondwana in the Mesozoic era. The presence of complex aseismic ridges and plateaus in the Indian Ocean makes it the least-understood of all the oceans. Mascarene Plateau, apart from Central Indian Ridge (CIR) running north-south between 2◦N and 25◦S in the Indian Ocean, is one such complex feature in the Indian Ocean that consists of Seychelles microcontinent in the north and the volcanic islands of Mauritius, La Réunion and Rodrigues in the south.
Most of the previous seismological studies on the islands of Mauritius, Rodrigues and Seychelles are restricted as each of them has only one operational permanent station. In the current study, I present the results obtained from the investigations of the seismological data obtained from the deployment of temporary seismic network on Mauritius (November, 2012–August, 2014) and Seychelles (March, 2013–March, 2015) under Réunion Hotspot and Upper Mantle–Réunions Unterer Mantel (RHUM–RUM) project and later in Rodrigues (September, 2014–June, 2016) under a collaborative project between Goethe-Universität, Frankfurt, Germany and Mauritius Oceanography Institute (MOI), Mauritius. Additional data from the permanent stations were also used in this study. The investigations and results are presented under three themes, namely: (1) crustal structure beneath Mauritius, (2) upper mantle anisotropy below Mauritius, Rodrigues and Seychelles and (3) intraplate seismicity in the Rodrigues–CIR region.
Upper mantle anisotropy in south-west Indian Ocean region are very limited, especially from the islands of Mauritius and Rodrigues. With the new data from the seismic stations deployed in Mauritius and Seychelles, under RHUM–RUM, and permanent stations in Rodrigues, I constrain the upper mantle flow pattern beneath these islands. From the joint-splitting analysis, I obtain fast-polarisation direction (φ) dominant in N80◦E and delay time (δt) of ≈0.85 s for Mauritius and φ tending east–west in Rodrigues with δt of ≈1.1 s. Parabolic asthenospheric flow model explains the orientation of the fast-polarisation direction beneath Mauritius, whereas deep mantle circulation patterns best explain the horizontal alignment of the fast-polarisation direction in Rodrigues. From Seychelles data, the results show φ trending NE and δt ≈0.74 s, even for the island close to Amirante Ridge, suggesting an asthenospheric deformation induced by relative motion between the plate and the deep mantle flow.
It has recently been suggested that the volcanic island of Mauritius may be underlain by a remnant of continental origin termed “Mauritia.” To constrain the crustal thickness beneathMauritius, I analysed data from 11 land stations, 10 of which were deployed recently under the RHUM–RUM project. From the recordings, I obtained 382 P-receiver functions. On the obtained receiver functions, I applied the H–κ stacking technique and derived the crustal thickness of ≈10–15 km. I observe a considerable variation in the VP/VS ratio caused by a lack of clear multiples. Using forward modelling of receiver functions, I show that the lack of clear multiples can be explained by a transitional Moho, where the velocity increases gradually. The modelling further indicates that the thickness of this gradient zone is estimated to be ≈10 km. I argue that my findings suggest oceanic crust thickened by crustal underplating due to the mantle plume currently located beneath La Réunion.
Seismicity around Rodrigues Island is generally associated with events recorded by the global networks along the CIR. Using seismological array techniques on the data collected by the temporary deployment of seismic array on Rodrigues Island for a period of 22 months (September, 2014–June 2016), 62 new events were located, which were not reported by any global network. Determination of backazimuth and apparent velocity were performed by applying array methods in the time-domain instead of the more conventional frequency-domain analysis. Event distances were calculated using a 1-D velocity model and the measured travel-time differences between S- and P-wave arrivals. Local magnitudes of the events were obtained by removing the velocity response from the seismographs and then convolving with Wood–Anderson transfer function to obtain ground motion in nanometers. Most of the newly-detected events are located off the ridge axis and can be classified as intraplate events. Three different seismic clusters were observed around the island. Most of the events were localised in the north-east of Rodrigues at a distance of ≈138 km from the reference station. A distinguishable swarm of earthquakes was observed on the west of the spreading segment from March to April 2015. The local magnitudes (ML) of the events varied between 1.6 and 3.7.
Steilhänge der Mittelgebirge weisen eine kleinräumige standörtliche Vielfalt auf und wurden aufgrund ihrer exponierten Lage bereits frühzeitig durch den Menschen u. a. als Befestigungsanlage genutzt. Daraus resultierte häufig eine hohe floristische und vegetationskundliche Diversität mit hohem Naturschutzwert. Durch Umwelt- und Nutzungsveränderungen hat sich aber auch an diesen Standorten in den letzten Jahrzehnten ein starker Wandel vollzogen. Durch Auswertung alter Florenlisten und Vegetationsaufnahmen und durch aktuelle Erhebungen wollen wir die Vegetationszusammensetzung der Lengder Burg, eines Steilhangs auf Unterem Muschelkalk im südlichen Göttinger Wald (Süd-Niedersachsen, Deutschland), und ihre Veränderung aufzeigen und Rückschlüsse für die zukünftige Behandlung ziehen. Dazu wurden Angaben zur Gefäßpflanzenflora aus dem Zeitraum 1950 bis 1995 mit einer aktuellen floristischen Kartierung des Gesamtgebiets von 2016 verglichen. Die Vegetationszusammensetzung wurde anhand von 37 Vegetationsaufnahmen aus dem früheren Zeitraum harakterisiert. 29 dieser Flächen wurden 2009 bis 2016 erneut aufgenommen. Räumliche und zeitliche Unterschiede in der Diversität und Artenzusammensetzung wurden hinsichtlich verschiedener standörtlicher Parameter und ökologischer Artengruppen analysiert.
Die Vegetation lässt sich zwei Gruppen zuordnen: 1. Das Carici-Fagetum und seine Kontaktgesellschaften an südlich und westlich exponierten Steilhängen. 2. Das Hordelymo-Fagetum mit verschiedenen Ausbildungen auf dem Plateau und an flacheren Süd- und Nordhangbereichen. Im Carici-Fagetum ist ein deutlicher Diversitätsverlust und eine Zunahme in der Dominanzstruktur der Krautschicht zu erkennen, der im Vergleich der Aufnahmezeiträume auf eine zunehmende Homogenisierung der Vegetation hinweist. Zurückgegangen sind dabei besonders die typischen Kenn- und Trennarten dieser Waldgesellschaft bei gleichzeitiger Zunahme der Buche in der Verjüngung. Im Hordelymo-Fagetum bewirkt neben Gehölzen in der Strauch- und Krautschicht vor allem die Zunahme von Allium ursinum eine homogenere Artenzusammensetzung, jedoch ohne Diversitätsverlust. Neben Stickstoffeinträgen, dem Klimawandel sowie einem reduzierten Rehwild-Verbiss bedingt besonders der Nutzungswandel diese Veränderungen. Vor allem im Carici-Fagetum wirkte sich der Übergang zwischen früherer Nieder- und Mittelwald-Nutzung mit Waldweide über eine fast 100jährige Hochwald-Nutzung bis zum jetzigen Schutzwald stark aus. Gleichwohl weisen die steilen Hänge weiterhin einen hohen Anteil an Rote-Liste-Arten auf und tragen wesentlich zur hohen Biodiversität des Gebiets bei. Veränderungen in der Vegetation der Lengder Burg spiegeln die Veränderungen im Göttinger Wald insgesamt wider. Kleinflächige Offenhaltungsmaßnahmen zur Erhaltung wertvoller floristischer Elemente sind teilweise erfolgreich. Kleinwüchsige, lichtbedürftige Magerkeitszeiger verschwinden jedoch zunehmend aus den sich entwickelnden, hochwüchsigen Stauden-Säumen. In den benachbarten, unbewirtschafteten Hangbuchenwäldern sorgt die fehlende Nutzung nach Jahrhunderten der Auflichtung und Aushagerung für eine Sukzession in Richtung mesophilen Kalkbuchenwalds.
In Borstgrasrasen (Nardetalia) des Werra-Meißner-Gebietes (Nordhessen, Südniedersachsen) wurden 2012 nach 25 Jahren auf möglichst gleichen Untersuchungsflächen (quasi-Dauerflächen) Wiederholungsaufnahmen angefertigt, um den gegenwärtigen Zustand bzw. Veränderungen in diesem prioritären FFH-Lebensraumtyp zu erfassen. Es wurden insgesamt 61 Flächen untersucht. Neben der Artenzusammensetzung wurden auch Bodenparameter (pH, C/N-Verhältnis, Mächtigkeit der organischen Auflage) und die Nutzung erfasst.
Bei der Wiederholungsaufnahme 2012 waren, abgesehen von einer Aufforstungsfläche, noch auf allen Flächen Arten der Borstgrasrasen vorhanden. Die Flächen wurden 2012 überwiegend genutzt oder gepflegt, während 1986/87 Brachflächen noch bei weitem dominierten. Eine Düngung der Flächen erfolgte nicht. Trotz dieser generell günstigen Nutzungssituation lässt sich ein genereller Trend zur Eutrophierung feststellen, der sich hinsichtlich Artenzahl und Deckung in einer Zunahme von Arten des Wirtschaftsgrünlandes (Molinio-Arrhenatheretea) bei gleichzeitiger Abnahme der Borstgrasrasen-Kennarten äußert. Auch die Artenzahlen der übrigen Magerkeitszeiger nahmen im Mittel ab, während Verbrachungszeiger im Allgemeinen zunahmen. Eine Veränderung der Gesamtartenzahl war nicht festzustellen. Die mittleren Zeigerwerte spiegeln die Verschiebungen im Arteninventar durch erhöhte mittlere Reaktions- und Stickstoffzahlen wider. Strukturell hat in den vergangenen 25 Jahren vor allem eine generelle Zunahme der Moosschichtdeckung und eine Ausbreitung der Sträucher auf Brachflächen stattgefunden. Bei den Bodenparametern waren 2012 eine signifikante Erhöhung der pH-Werte, eine Einengung der C/N-Verhältnisse und eine Abnahme der Mächtigkeit der organischen Auflage (Of) feststellbar. Regressionsmodelle zeigen, dass dabei die Zunahme von Arten des Wirtschaftsgrünlandes direkt mit den ansteigenden pH-Werten zusammen hing, während die Veränderungen bei den Kennarten eher vom Ausgangs-C/N-Verhältnis, teilweise auch von der Entwicklung der organischen Auflage und der Nutzung abhängig waren. Die vorgefundenen Veränderungen werden vor dem Hintergrund möglicher Gefährdungsszenarien (Brache, Eutrophierung, Bodenversauerung, Klimawandel) diskutiert. Angesichts des unerwarteten Befundes einer Eutrophierung bei gleichzeitig nachlassender Bodenversauerung, wird die Hypothese aufgestellt, dass der seit den 1990er-Jahren erfolgte Rückgang der Schwefeldepositionen mit nachfolgender Erholung der Boden-pH-Werte und nachlassender Stressbelastung, z. B. durch Ammonium-Toxizität, die Veränderungen ausgelöst haben könnte. Außerdem deuten die Ergebnisse auf eine zumindest teilweise zu geringe Nutzungs- bzw. Pflegeintensität bzw. zu späte Nutzungstermine. Möglicherweise führt der erhöhte Eutrophierungsdruck hier auch zu verstärkten Anforderungen an das Management der Flächen. Eindeutige Indizien für klimabedingte Veränderungen im Arteninventar ließen sich nicht finden. Indirekte Effekte über eine erwärmungsbedingte Förderung der Mineralisationsraten oder ein ursächlicher Zusammenhang zwischen höheren Wintertemperaturen und der Zunahme der Moosdeckung lassen sich jedoch nicht ausschließen.
Transitional between the Pannonian Basin and the Eastern Carpathians the Transcarpathian Ukraine (Transcarpathia) has a diverse geology including Quaternary sediments, volcanites, limestones and flysch, and its climate at low altitudes is relatively warm and humid. We conducted a field survey in June 2016 focusing on mesophilous forest vegetation along a transect covering almost the whole lowaltitudinal part of Transcarpathia. We recorded 54 relevés in the field and further digitized 22 relevés from literature. Using classification analysis, we distinguished three clusters of oak-hornbeam forests (alliance Carpinion betuli; 1–3) and three clusters of scree and ravine forests (alliance Tilio platyphylli-Acerion; 4–6): (1) Slightly wet Pannonian oak-hornbeam forests occurring in the lowland part of the region (Circaeo-Carpinetum); (2) Mesophilous oak-hornbeam forests (Carici pilosae-Carpinetum); (3) Xero-mesophilous oak-hornbeam forests (a drier subtype of the Carici pilosae-Carpinetum and the association Primulo veris-Carpinetum); (4) Mesophilous scree forests (Phyllitido-Aceretum); (5) Forests of steep slopes (Aceri-Tilietum) and transitions to mesophilous oak-hornbeam forests (Carici pilosae-Carpinetum); (6) Cool and wet scree and ravine forests (Arunco dioici-Aceretum pseudoplatani). Using indirect ordination analysis, three environmental variables (altitude, heat load index and slope) were identified as factors of significant influence on the species composition. These factors well distinguish oak-hornbeam forests from scree and ravine forests.