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The dissertation describes an Indigenous dream framework that underscores the significance of dreams as a mirror of trauma and a way that leads back to Indigenous knowledges. Significant differences of Western and Indigenous epistemology are exemplified by juxtaposing Western and Indigenous dream discourses. The selected prose fiction allows for a dream categorization that emphasizes the significance and meaning of dreams as a metaphorical as well as narrative device.
Nightmares/Anxiety dreams are often the result of the devastating effects of colonization and especially Residential School. Nightmares in the texts are often exact replicas of the abuse suffered in the boarding schools. They are discussed in the context of Robert Arthur Alexie’s novel Porcupines and China Dolls (2001/2009) represents dreams and traumatic nightmares and deals with the fictional Blue People First Nation. The community’s collective intergenerational trauma of Residential School experience keeps them stuck in dysfunctional dynamics dominated by suicides, sexual and physical abuse, drug and sex addictions.
Telling dreams, categorized as “instructing dreams,” and “announcing dreams,” teach the dreamer what will happen in the future. They are discussed in the context of Richard Van Camp’s short stories “On the Wings of this Prayer” and “The Fleshing” (Godless but Loyal to Heaven, 2012), which represent the category of the ecological nightmare as well as of telling dreams. Ecological nightmares display environmentally destructive effects of capitalist globalization that have come to “infect” the world. The Windigo figure in the stories serves as a manifestation of resource and in particular petro-capitalism and Western society’s constant need to subjugate nature. Ecological dreams hence call for ecological vigilance and establish Indigenous knowledges as a source of resurgence and restoration.
Existential dreams function as decolonizing tools that facilitate liberation. The thesis provides a literary analysis of Richard Wagamese’ novel Ragged Company (2008) and Cherie Dimaline’s short story “room 414” (Red Rooms, 2007) where homelessness is postulated as the manifestation of individual and tribal/communal disjointedness and isolation. Through existential dreaming, the urban lives of most of the characters dwelling in the shadows and margins of society are existentially transformed and healing seems possible. Paternalistic colonial mindsets continue to patronize Indigenous knowledges (as unreliable and unscientific) until Western “discoveries” prove what has been known for decades.
The thesis underscores dreams as an essential part of Indigenous Knowledges, i.e. as knowledge sources. Surmounting Western dream perceptions and instead valorizing Indigenous knowledges, the characters in the texts discussed in my thesis, unremittingly follow their dreams’ instruction and eventually achieve reconciliation and healing. In the fictional texts discussed, nightmares represent homelessness, trauma, stagnation, and a disconnection to one’s (Native) background, whereas dreams represent continuity through the restoration of identity, finding home, and a sense of belonging. The notion of a dream reality and a waking reality influencing and informing each other relies on sharing dreams with the community, eventually leading to an enactment of the dream or vision. Dreaming and identity are significantly linked and foster processes of intellectual self-determination. The characters’ inability to externalize their internal wishes, desires, and needs results in further denial and consequential bitterness that feed into the spiral of alcohol and drug abuse as well as metaphorical and literal homelessness. The dreams’ semantic field strongly alludes to ceremonial traditions and provides the prospect of a rooted Indigeneity. At the turning points in the lives of the characters, when dreams and visions start to appear, they are lost in translation. The characters’ own illiteracy towards Native epistemology and spirituality has them trapped in the inability to read and act on their dream messages. Strong (often female) Indigenous presences that go hand in hand with the appearance of dreams provide the protagonists with guidance and lead the way back to the “Old Ways.” Through dreaming, the spiral of colonialism is disrupted and replaced by the circle of reconciliation and relationality.
The aims of this study were to quantify the key mineralization processes and the resulting nutrient release potentials of different sediment types, their ranges of extent and dependency on varying environmental conditions such as seasonal variations or shifts in oxygen availability. Benthic phosphate fluxes and flux potentials were of particular interest as P is an essential nutrient for algal growth in marine systems and phosphate is often limiting primary production, hence strongly promotes the production of new biomass. A major P source in marine environments are mineralization products of early diagenetic processes.
To gain insight into the pathways of organic matter mineralization and subsequent secondary reactions, key reactants in the solid and the dissolved phase were considered in typical sediments of the Baltic Sea and the Black Sea. Seven study sites in the German Baltic Sea region, representative of the major depositional environments, including coarse and fine grained sediments, both rich or poor in organic carbon, were intensively studied. The investigations were conducted on a seasonal basis during ten ship-based expeditions between July 2013 and March 2016, covering spring- and autumn algal blooms, stagnation periods with bottom water hypoxia and winter dormancy. Hypoxic conditions frequently developed in the bottom waters of the Bay of Mecklenburg, Stoltera and the Arkona Basin sites, shallower stations like the Tromper Wiek, the Oder Bank and the Darss Sill were usually not affected by hypoxia. Increased nutrient concentrations in the bottom waters coincided with oxygen depletion. High salinity dynamics were observed in the bottom waters above the studied sediments, which were due to frequent salt water inflows from the North Sea. Bottom water temperature variability was seasonally conditioned.
The studied sands showed 2-3 orders of magnitude higher permeability values and about one order of magnitude lower organic matter contents compared to the studied muds. Occasionally, strongly increased organic matter contents were observed in the sands, likely induced by downward mixing of plankton bloom derived particles. The organic matter was found to be essentially supplied by marine phytoplankton, indicated by its elemental composition and isotopic signature.
Additionally, an adapted approach of the Keeling plot method was made to characterize the source material of organic matter mineralization. In marine environments, dissolved inorganic carbon concentrations often increase with depth together with an isotopic carbon signature shift to lighter values due to organic matter mineralization. The Keeling plot method was commonly used to determine the isotopic signature of carbon sources for ecosystem respiration. Conventionally, the influence of respiratory depletion of 13CO2 on the isotopic composition of the atmosphere was studied in terrestrial and limnic biogeochemistry. The same approach was applied on organic matter mineralization in sediments and the water column during this study. Mixing of bottom water derived background DIC and DIC released into the environment during organic carbon decomposition was assumed. In a modification of previous approaches, where changes in concentration and δ13C of DIC were followed over time, vertical profiles were analyzed in this study, which represent time-dependent variations superimposed by transport processes . DI13C gradients in the water column of the Black Sea and pore water profiles in the Black Sea and the Baltic Sea were used to estimate the 13C signature of the mineralized organic carbon via Keeling plot analysis. The Black Sea water column revealed a δ13C signature of the organic matter source close to the signature of typical particulate organic matter in the ocean and previously reported values for the Black Sea euphotic zone. In the pore waters of Black Sea sediments (from short and long sediment cores), Keeling plot analysis clearly demonstrates that the released DIC at depth can be derived from different sources. An isotopically very light carbon source (< –60 ‰) was associated with anaerobic oxidation of methane in the Black Sea. Marine organic matter was the principal source for DIC in the deeps of Baltic Sea basins, while the calculated carbon source isotopic signature in sediments of sand flats and bays was shifted to heavier δ13C signatures compared to marine organic matter. These shifts were attributed to potential dissolution of sedimentary carbonates or organic inputs of terrestrial C4 vascular plants like maize and other agricultural plants. The carbon source isotopic composition calculated via Keeling plot analysis correlated well with directly measured δ13C signatures of surface sediments POM.
Organic matter mineralization activity in the southern Baltic Sea sediments was studied via gross sulfate reduction rate analysis and total oxygen uptake measurements in sands and muds. Oxygen penetration depths were less than 4 mm in both, muddy and sandy sediments. Oxygen uptake rates were similar in muds (10.2 mmol m–2 d–1) and sands (10.7 mmol m–2 d–1), while significantly higher rates were measured in the coastal near sites of the Bay of Mecklenburg (about 12 mmol m–2 d–1) than in the deeper Arkona Basin (about 9 mmol m–2 d–1). Substantial sulfate reduction was measured in the muddy (about 4 mmol m–2 d–1) and the sandy (about 1 mmol m–2 d–1) study sites. Highest sulfate reduction rates (4.4 – 5 mmol m–2 d–1) were detected in the muds of the Bay of Mecklenburg during summer, about twice as high as in the Arkona Basin muds. Increased mineralization activity of the coastal near muds of the Bay of Mecklenburg is attributed to enhanced input of fresh organic matter during algal blooms.
About twofold higher oxygen consumption and sulfate reduction rates were measured in summer compared to winter in sandy and muddy sediments.
The studied sites were usually characterized by a typical biogeochemical zonation with oxic, suboxic and sulfidic zones. The concentration profiles in the muds reflected sulfate reduction and secondary redox-reactions, liberating dissolved carbon, nitrogen, phosphorus and hydrogen sulfide into the interstitial waters. Orders of magnitude lower concentrations were detected in the sands, while their top centimeters were mostly irrigated and mineralization products only accumulated below.
A several centimeter thick suboxic zone was sustained by active downward transport of oxidized material in the southern Baltic Sea coastal sediments, presumably mainly through bioturbation. Especially sulfur and iron species were involved in the secondary reactions between the metabolites of early diagenetic processes occurring in the suboxic zone. Partly high temporal variability was observed in the form of vertical migration of the sulfidic zone and a corresponding expansion and shrinking of the suboxic zone. The Arkona Basin site showed the most stable geochemical zonation over time, while the Luebeck Bight site and especially the Mecklenburg Bight site showed striking dynamics. The consequent redox-regime shifts within the surface sediments might promote mineralization of organic matter as higher sulfate reduction rates and higher total oxygen uptake were measured in these more dynamic muds. The vertical shifts of the redox-gradients can largely be explained by temporal and spatial variability of bioturbation activity, but also anthropogenic activities may play a role. Bottom trawling, may be the dominant mixing process at the Mecklenburg Bight site.
In the sands, less reactive iron and manganese contents were available compared to the studied muds, which may be due to frequent irrigation of the top centimeters leading to a loss of pore water reservoirs like dissolved Fe and Mn.
Another mixing process, storm induced sediment resuspension, was suggested to be important for the sediments in the study area. A severe sediment resuspension event at the silty Tromper Wiek site was indicated by steep gradients in pore water concentration and particulate mater content profiles in the top ∼ 5 cm sediments. Carrying out non steady state modeling (Bo Liu, IOW), the successive re-development of the pore water profiles towards a steady-state was simulated and the time span necessary to establish measured pore water profiles after the sediment disturbance event was approximated. In the predicted time span, daily average wind speeds reached an annual high of the category ‘gale’ which was probably sufficient to resuspend and irrigate the surface silt-type sediments.
This study showed that sediment mixing processes have a strong influence on early diagenetic reactions, solute release potentials and actual fluxes from the sediments. Also the sediment mixing via bottom trawl fishing can be regarded as an event-like disturbance. The newly developed approach of non-steady-state modeling of pore water sets (Bo Liu; IOW) can help to answer the question, how long it takes to reach a steady-state after a sediment disturbance event.
The concentration profiles in interstitial waters were used to calculate net transformation rates via the transport-reaction models REC and PROFILE. The calculations revealed net release of H4SiO4 and PO4 within the top 20 cm of the studied muds, while net DIC and NH+4 consumption and sulfate production was clearly evident within the top ∼ 5 cm. Intensive reoxidation of sulfide that was produced via sulfate reduction was also indicated by large deviations between the modeled net sulfate transformation rates and experimentally derived gross sulfate reduction rates. These surface near transformations were probably associated with microbial chemosynthesis.
The studied sands of the southern Baltic Sea were usually characterized by very low pore water gradients, probably due to their frequent irrigation. Accordingly, calculated transformation rates were one to two orders of magnitude lower in the studied sands compared to the muds of the southern Baltic Sea. However, during a situation with a stratified water column, substantial pore water reservoirs with the typical concentration trends were present in the sandy Darss Sill sediments. Integrated production rates of PO4, Mn2+ and H4SiO4 derived from these concentration profiles were in the same order of magnitude as in the muddy Arkona Basin.
Intensive pore water irrigation is also capable to transport fresh organic matter into the sediment as was occasionally indicated by strongly increased surface near TOC in the sands. Considerable gross sulfate reduction rates and total oxygen uptake rates were measured in the sandy Oder Bank sediments, where pore water concentration profiles rather suggested absence of diagenetic processes. The studied sands were, hence, not unreactive substrates but usually rather unable to preserve the mineralization products.
This reflects the often limited significance of pore water evaluations in irrigated sandy sites but also the high mineralization potentials of coastal sands. Early diagenetic processes and the impact of intense benthic-pelagic exchange in such shallow marine environments is still poorly understood, as they were rarely investigated in the past and are methodologically more difficult to investigate.
The Baltic Sea deeps Gotland Deep and Landsort Deep were mainly controlled by sulfate reduction and shallow anaerobic oxidation of methane. Calculated rates of net sulfate reduction and net sulfide production were equivalent, indicating a lack of sulfide re-oxidation reactions. Phosphate liberation rates were low in the surface sediments, but strong linear concentration gradients indicated liberation at depth.
The euxinic Black Sea sediments were purely controlled by sulfate reduction via anaerobic oxidation of methane at the sulfate-methane transition zone in sediment depths of up to several meters. Subsequent diffusive concentration gradients clearly dominated pore water profiles in the surface sediments.
Benthic solute reservoirs of the top 10 cm pore waters were generally higher in the muds than in the sands of the southern Baltic Sea. The smaller reservoirs in the sands were cause by intensive exchange between pore water and bottom water in these permeable sediments. The three studied muddy sites of the southern Baltic Sea showed great dissimilarities with respect to their pore water compositions. Large observed pools of dissolved Fe2+ and PO4 clearly point to reduction of reactive Fe and release of adsorbed P pools. Multi-dimensional scaling analysis showed that seasonal variability played only a minor role for the observed variability of the benthic solute reservoirs. Principal component analysis revealed that the studied sediments can be characterized by essentially two factors based on their pore water reservoirs of the top 10 cm: 1) their mineralization and accumulation efficiency and 2) their secondary reactions in the suboxic zone, reflecting fundamental differences in their sedimentation conditions and mixing processes. While the sands were similar to each other due to their overall low reservoirs, sands, silts and muds mainly differed in their mineralization and accumulation efficiency. Large variability was also observed within the studied muds regarding their predominating redox metabolites. Highest dissimilarities were evident between the neighboring sites Mecklenburg Bight (mostly suboxic) and Luebeck Bight (mostly sulfidic). Therefore, the biogeochemical state in the studied sediments were shown to be mainly controlled by their sediment type and the transport of reactive iron into the sediments. The supply of organic matter to the sea floor controlled the overall mineralization activity, while the sediment permeability determined the accumulation efficiency of the sediment. Mixing of surface sediments together with the complex relation of oxygen, sulfur, iron and phosphorus in the solid and aqueous phase is controlling benthic nutrient fixation/liberation reactions. Salinity variability showed no noticeable effects on early diagenetic processes. During four sampling occasions in the Arkona Basin, bottom water salinity showed strong variability which was also effecting pore water concentration profiles in more than 15 cm depth. However, concentration profiles of typical organic matter mineralization products remained remarkably stable. Also gross sulfate reduction rates seemed to be unaffected by the variable pore water sulfate concentrations.
Nutrient fluxes across the sediment-water interface were obtained by the interpretation of vertical pore water concentration profiles via different models (diffusive fluxes) and via incubation of intact sediment cores (total fluxes). Benthic diffusive fluxes represent potential release of solutes into the water column. They were often strongly associated with the benthic reservoirs, thus fluxes were highest in the muds, considerably lower in the organic-poorer silts, and generally close to zero in the sands. The dissimilarities between diffusive fluxes in the different sediments were mainly controlled by the sediment type. Highest variability was observed within the muds, controlled by their different diagenetic pathways due to different sediment mixing intensities.
In the muddy sediments, diffusive PO4 fluxes were much higher than mineralization of organic matter with the common element ratios of marine organic matter can provide, indicating active recycling of phosphorus within the muds due to recurring adsorption and re-release on reactive iron oxyhydroxide phases. Especially in the strongly mixed Mecklenburg Bight sediments, pore water dissolved PO4 was primarily controlled by the release of adsorbed P. Actual PO4 release into the bottom waters (determined via core incubation experiments) was only measured under extended bottom water oxygen deficiency conditions. The same applied to the redox-sensitive solutes Fe2+, Mn2+ and sulfide.
For the less redox-sensitive solutes, diffusion usually accounted only for a fraction of the total interfacial flux. The proportion of advective to diffusive transport was estimated with different methods. Bioturbation induced sediment mixing was quantified by comparing the diffusive H4SiO4 fluxes derived from pore water modeling with the total fluxes derived from the core incubations. The studied muds showed infauna induced advection proportions of about 35 – 100 %. Only when infauna was absent, diffusion became the dominant transport process across the sediment-water interface. In the studied sands, advection was the dominating transport process, since their generally low surface near reservoirs lead to diffusive fluxes close to zero. However, it remains unclear whether bioturbation or hydrodynamic irrigation are responsible for that. An attempt was made to estimate the effect of hydrodynamic irrigation for a range of reasonable bottom water velocities from the sediment bedform geometry after Neumann et al. (2017). However, resulting potential hydrodynamic irrigation was found to be rather low compared to reported values from the literature and may significantly underestimate actual irrigation of the sandy sediments.
In a new non steady-state multi-element diagenetic modeling approach (Bo Liu, IOW), vertical δ13C pore water profiles were used to estimate the significance of advective transport processes. Mixing processes at the sediment-water interface were expressed as multiple of pure diffusion (ε). By adjusting this mixing coefficient as boundary condition for best fits of predicted to measured pore water profiles, the degree of these mixing processes was estimated. In the Arkona Basin surface sediments, this approach revealed best fits assuming a mixing depth of 3.5 cm with a tenfold higher total mixing degree based on diffusional transport. The calculated mixing depths and intensities were similar to bioturbation depths and rates obtained via traditional methods (Morys, 2016). The novel modeling approach is a promising method to evaluate surface sediment mixing processes.
Increased mineralization activity during productive seasons lead to increased oxygen consumption and therefore frequent bottom water hypoxia. The effects of hypoxic bottom water conditions on the early diagenetic processes in the sediments were studied via prolonged core incubation experiments. Shifts to bottom water oxygen deficiency had various consequences for benthic reservoirs and fluxes. The oxygen consumption decreased during hypoxic incubation phases. Decreased bioturbation activity diminished advective transport so that total fluxes of redox-insensitive solutes (e.g. H4SiO4) were decreased. Reactive iron and manganese oxides act as barrier (“iron curtain”) in the suboxic zone, preventing redox-sensitive solutes from their release into the water column. After a shift to bottom water hypoxia, these reactive oxides are re-dissolved and liberated into the water column. Prolonged incubation experiments suggested that the Mn-oxide reservoirs were depleted first before the Fe-oxides with the adsorptively bound phosphate were liberated.
The release of nutrients (especially phosphorus), dissolved inorganic carbon, and redox- sensitive compounds (e.g. hydrogen sulfide) strongly varied in the different studied environments, covering coastal-near oxic, temporary hypoxic and euxinic conditions.
In environments, where advection through hydrodynamic irrigation or bioturbation do not occur, like in anoxic or euxinic systems, surface-near pore water gradients reflect total solute interfacial fluxes. They depend on the supply of organic matter to the sea floor, the mineralization rates in the sediments and the composition of the overlying bottom water. In the Black Sea, much of the organic matter mineralization was performed already in the water column and not in the sediments, leading to a decreasing export of organic matter to the sediment and increasing concentrations of mineralization products in the bottom water with increasing water depth. Accordingly, benthic fluxes across the sediment-water interface of the deep Black Sea sites were the lowest of the entire study, essentially reflecting the low mineralization rates of AOM in deeper layers. Highest fluxes in the Black Sea were observed at the continental slope at intermediate water depths, but were still lower than in the Baltic Sea deeps.
In contrast, highest DIC fluxes were detected in the oxygen depleted Baltic Sea deeps Gotland Deep and Landsort Deep. These basins are shallow enough that reactive organic matter reaches the sea floor, where it is mineralized via sulfate reduction close to the sediment surface. Strong concentration gradients and therefore high diffusive interfacial fluxes across the sediment-water interface were evident. As bioturbation was absent, these diffusive fluxes were representative for total interfacial fluxes unlike in sediments with additional advective flux components.
In more complex environments, like coastal oxic sediments, inhabited by macrofauna, overflowed by currents and affected by resuspension events, the sediment surface represents an interface between turbulent and calm conditions, high and low concentrations and/or different redox-states. Such gradients are the basis for intensive exchange processes. The surface sediments in the coastal sites of the southern Baltic Sea were characterized by active organic matter mineralization via sulfate reduction and mixing induced secondary reactions taking place in the suboxic zone. This included the removal of dissolved sulfide due to iron oxide reduction with simultaneous liberation of PO4 into the interstitial waters. High surface near P reservoirs existed due to internal P cycling within the sediments, which was in turn driven by continuous re-oxidation of the reduced iron by downwards transported oxygen. These reservoirs were only actually released into the water column during bottom water oxygen deficiency situations, when the iron re-oxidation was inhibited.
This also applies for sediments of the Gulf of Finland and the deeper Baltic Sea basins Bornholm Basin and Gdanks basin, where temporary hypoxic conditions are responsible for recurrent benthic phosphate release.
The widespread occurring phosphate adsorption on sedimentary solid iron phases is a much debated ecosystem service of marine sediments. As discussed in this work, the sedimentary P liberation rates and pools of readily bio-available dissolved phosphate can be substantial in Baltic Sea muddy sediments. Actual phosphate fluxes across the sediment-water interface, though, are relatively small because phosphate is scavenged by adsorption on iron oxyhydroxides that are usually an integral part of coastal marine sediments if overlain by oxic bottom waters. Although muddy sediments often show only an oxic layer of only few millimeters thickness, adsorption capacities of iron oxyhydroxides are large enough to substantially retain P from being liberated into the water column. Falling under reducing conditions, iron oxyhydroxides are re-dissolved, liberating high amounts of PO4 into the surrounding waters. While permanently oxic sediments will preserve adsorbed P, permanently anoxic sediments steadily release mineralized P into the water column. However, sedimentary environments of oscillating redox conditions are predestined for high, burst-like benthic P fluxes. Especially in a quasi isolated environment like the Baltic Sea, with high nutrient inputs but only few sinks, these internal recycling processes promote eutrophication in the long-term. Further expanding hypoxia and anoxia in the Baltic Sea with a subsequent loss of benthic fauna and altered nutrient dynamics in the surface sediments may be the consequence.
Estimating effects of craniofacial morphology on gingival recession and clinical attachment loss
(2017)
Objectives: Currently, evidence for the association between face morphology, attachment loss and
recession is lacking. Face type can be described by the ratio of facial width and facial length. We
hypothesize, that the facial type might be related to gingival recession (REC) and clinical attachment
loss (CAL) and that a broad face is associated with less recession and attachment loss than a long
face.
Materials and methods: Data from the 10 year follow-up of the Study of Health in Pomerania
(SHIP-2; 2008-2012; 2333 participants) were used. Periodontitis was assessed by probing depth (PD)
and clinical attachment loss (CAL). Generalized regression models were used to assess associations
between specific landmark distances extracted from magnetic resonance images (MRI) head scans
and clinically assessed gingival recession adjusting(REC) or clinical attachment loss(CAL) adjusting
for relevant confounders.
Results: Maximum cranial width was negatively associated with mean REC and mean CAL
(p<0.05). Also, higher mean REC and higher mean CAL correlate positively with long face
(B=0.361 with 95% CI), upper anterior facial height.
Conclusion: According to the results of the present study, gingival recession and clinical attachment
loss were associated with higher Prosopic face and facial length indices results.
Coastal and marginal seas – like the Baltic Sea – serve as natural reaction sites for the turnover and accumulation of land-derived inputs. The main location for the modification and deposition of the introduced material is, in most cases, not the water mass, but the sediment. Its key function as central reactor in the interaction between land and sea has so far been insufficiently studied and assessed. This study was part of the interdisciplinary SECOS project that aimed to identify and evaluate the service functions of sediments in German coastal seas in the context of human use with a focus on the Baltic Sea. One of its goals was to assess sediment functions related to the intermediate storage or final sink of imported material like nutrients and contaminants, and quantify their inventory as well as their mass accumulation rates on multi-decadal to multi-centennial time scales. For that, a detailed examination of the natural and anthropogenic processes that interfere with sediment accumulation in the south-western Baltic Sea basins is essential.
Body sensations play a crucial role in the etiology and maintenance of diverse anxiety and health problems (e.g., in panic disorder or respiratory diseases) as they may be perceived as threatening and consequently elicit anxious responses. The factors that may affect the perception of bodily sensations as a threat and thus modulate the anxious response to body sensations have so far rarely been studied. Therefore, the present thesis targeted at elucidating the effect of contextual (i.e., the predictability, expectation, and proximity of a threat) and dispositional factors (i.e., tendency to fear arousal sensations or trait fear of suffocation) on the defensive response to body sensations.
In study 1, it was investigated how a personality factor, that is, fear of suffocation, affects the acquisition of fear to body sensations (i.e., mild dyspnea induced by inspiratory resistive loads) and contexts when faced with a predictable and unpredictable respiratory threat (i.e., severe dyspnea). Study 2 aimed at examining the main and interactive effects of the tendency to fear arousal sensations, again a personality trait factor, and current arousal expectations as varied by situational variables on anxious responding to arousal sensations. In this study, expected and unexpected arousal sensations were induced by administering caffeine in coffee or bitter lemon soda, respectively. Moreover, in study 3, it was explored how subjective anxiety, bodily symptoms, and defensive respiratory responses change and might culminate into active defense behavior (i.e., escape/active avoidance) during increasing dyspnea that was evoked by inspiratory resistive loads increasing in intensity. For a detailed analysis of the factors that contribute to the initiation and maintenance of avoidance of or escape from increasing dyspnea, in study 4 changes in subjective, autonomic, somatic reflex and brain responses were analyzed during repeated avoidance of increasing dyspnea.
In study 1, it was demonstrated that only individuals who fear suffocation learned to fear mild dyspnea preceding the onset of severe dyspnea and developed anxiety during a context of unpredictable respiratory threat. Moreover, the data from study 2 indicate that individuals who fear arousal sensations show an increased attention allocation towards unexpected arousal sensations and higher threat appraisal when expecting arousal sensations. Increasing intensity of dyspnea as provoked in study 3 led to increased defensive respiratory responses that were associated with increased symptom reports in individuals with high compared to low fear of suffocation. Moreover, culminating dyspnea elicited repeated avoidance behavior preceded by increases in defensive respiratory mobilization. The analysis of repeated avoidance of increasing dyspnea in study 4 revealed that physiological fear responses might be involved in the initial initiation of this avoidance behavior while no indication of response preparation and physiological arousal was related to persistent avoidance.
Taken together, the present data suggest that the fear of suffocation, as well as the tendency to fear arousal sensations along with the predictability, expectation, or proximity of interoceptive threat, may increase the perceived threat and thus the anxious response to body sensations. Therefore, contextual and dispositional factors may set the stage for the culmination of body sensations into defensive action and might contribute to the development of pathological anxiety and fear of body sensations. The present findings are integrated into the current literature and discussed in relation to the development and maintenance of pathological anxiety and fear of body sensations.
Psychological health is a result of the effective interplay between explicit and implicit attempts to regulate ones’ emotions (Koole & Rothermund, 2011). Emotion regulation refers to processes that influence the intensity, the duration and the type of emotion experienced (Gross & Thompson, 2007). While explicit emotion regulation comprises effortful mental processes, implicit emotion regulation refers to processes that require no monitoring and terminate automatically (Gyurak, Gross, & Etkin, 2011).
In the present thesis, explicit and implicit strategies to regulate emotions were investigated. In Study 1, a well-established paradigm (Gross & Levenson, 1993) was adapted to examine the up- and down-regulation of positive and negative emotions using two different explicit emotion regulation strategies. To infer on the neurobiological correlates, blood oxygen level dependent (BOLD) brain activity was recorded using functional magnetic resonance tomography. Furthermore, as a trait marker for the individual ability to regulate emotions, heart rate variability (HRV) was acquired during rest. In Study 2, implicit emotion regulation was examined. Therefore, a well-established fear extinction paradigm was compared to a novel approach based on the integration of new information during reconsolidation (Schiller et al., 2010). Autonomic arousal was measured via the skin conductance response during fear acquisition, fear extinction and after fear reinstatement. In Study 3, two dysfunctional emotion regulation strategies —worrying and rumination— were investigated. Excessive worrying and rumination are pathogenic characteristics of psychological disorders. Behavioral, autonomic and BOLD activity was recorded during worried and ruminative thinking as well as during neutral thinking.
The results showed that explicit emotion regulation was associated with modulated BOLD activity in the amygdala according to the regulation direction independent of the applied strategy and the valence of the emotion. In addition, increased dorsolateral prefrontal cortex (dlPFC) activity was observed during regulation compared to passively viewing emotional pictures. The findings are in line with previous research (Eippert etal., 2007; Kim &Hamann, 2007; Ochsner etal., 2004) and support the key role of the dlPFC during the explicit regulation of emotions. Similarly, implicit emotion regulation was associated with a decreased autonomic fear response, which was sustained after fear extinction during reconsolidation. The findings underscore the notion, that this novel technique might alter the initial fear memory resulting in a permanently diminished fear response (Nader, Schafe, & LeDoux, 2000; Schiller et al., 2010). Dysfunctional emotion regulation was associated with increased autonomic activity and fear potentiated startle (during worry) as well as increased BOLD activity in the insula (during worry and rumination) and increased BOLD activity in the amygdala (during rumination). In addition, neural activity in brain areas associated with the default mode network was observed. These findings stress the preserved negative emotional activity and the self-referential nature of the examined dysfunctional strategies. The results of all three studies are integrated into a neuro-biological model of emotion regulation focusing on the interplay between subcortical and prefrontal brain areas.
Interoceptive sensations, that means, perceptions of the physiological body state, play an important role in the generation and expression of emotion. The focus of the research presented here is on respiratory sensations as specific interoceptive signals. Such respiratory sensations (like the feeling of dyspnea) play an important role in symptom perception in somatic (e.g., asthma) as well as in mental disorders (e.g., anxiety disorders). There are several different ways to manipulate respiratory sensations in an experimental environment, but many of them did not equal sensations in daily life. Here, stimuli (inspiratory resistive loads, caffeine) were used that trigger nearly naturally occurring interoceptive sensations. Taking into account that the elicited interoceptive experience also induces an unpleasant feeling state it is most likely that individuals show defensive physiological responding to such cues and try to avoid them. According to a bidirectional motivational system defensive behaviors are regulated by a defensive motivational system that is activated by threatening cues. From research with exteroceptive stimuli it is known that defensive responding is typically characterized by heightened autonomic arousal, increased respiration, and a potentiated startle eyeblink response. In contrast, only a few studies using interoceptive stimuli have incorporated the measurement of physiological data in their experimental designs. If included, studies show also heightened autonomic responding, whilst a heterogeneous respiratory as well as startle eyeblink responding is observed. Thus, the studies presented here were designed to clarify the factors that mediate defensive responding to interoceptive sensations. Study 1 investigated the influence of anxiety on the subjective, respiratory, and autonomic response to an individually determined inspiratory resistive load, while study 2 focuses on the effect of attentional modulation of the startle eyeblink response to a mild respiratory threat. In study 3 the modulation of subjective, respiratory and autonomic reactions by arousal expectations was examined. Therefore, caffeine, a respiratory stimulant, or a placebo were administered without the participants’ knowledge. The fourth study examined the influence of the process of worrying, a strategy to deal with unpleasant body symptoms, on defensive responding. Depending on the study design subjective, respiratory and autonomic (skin conductance level, heart rate) parameters were assessed as marker for defensive mobilization. In study 2 and 4 the startle eyeblink response was measured as further index of defensive activation. Besides that in study 2 also the P3 component of the event-related potential, as an index for attentional allocation, was recorded. The main findings of the presented dissertation are the following: Study 1 revealed that 1) only high anxiety sensitive individuals reporting also high suffocation fear respond to lower stimulus intensities with stronger defensive responding, and 2) that this group demonstrated a maladaptive compensatory breathing pattern. Additionally, study 2 exhibited that 1) the startle eyeblink response is relatively inhibited during a mild interoceptive threat, and 2) this inhibition corresponds to an attention allocation towards breathing as indicated by a reduced P3 amplitude to the startle noise as well as subjective report. Furthermore, highly anxiety sensitive individuals showed a more pronounced defensive responding if the interoceptive sensations were unexpected (study 3). Recently, study 4 demonstrated that worry led to an increased defensive response mobilization. All studies are discussed in the context of the theoretical background of the defensive response modulation to exteroceptive and interoceptive sensations with respect to mediating factors. Showing exaggerated defensive responding and maladaptive adaptation processes in high anxious individuals the results point towards the important role of interoceptive sensations in the etiology, maintenance and therapy of mental disorders, especially the anxiety disorders.
Introduction: Antiseptics are used for the prophylaxis of infections of acute wounds and for the treatment of critically colonized chronic wounds as well as localized infections of acute and chronic wounds. If an antiseptic with too much tissue toxicity and/or too little efficacy is used, the wound healing can be delayed.
Objective: The aim was to compare the irritation potency of frequently used wound antiseptics by using the hen's egg test on the chorioallantoic membrane (HET-CAM). Additionally, the influence of antiphlogistic active additives which might increase the tolerability was examined. To allow a more extensive comparison, antiseptics classified as obsolete such as hydrogen peroxide, creams on PVP- iodine base, silver sulfadiazine, chlorhexidine and nitrofural as well as the non-antiseptic wound treatment agents dexpanthenol and hemoglobin spray were also examined.
Method: The HET-CAM was used as a semi-in-vivo method to test the tolerability of wound antiseptics to tissues by observing the reactions that occur in the blood vessels of the highly vascularized CAM such as hemorrhage, lysis and coagulation. The irritation score (IS) was calculated and differentiated in 4 ranges according to Spielmann (1991).
Results: The vascular injuries of the CAM were considered as an indirect indicator of the tolerability. It is accepted that agents with no or low irritation potential on the CAM are to be preferred in the clinical practice if they are clinically effective.
Severe CAM reaction was observed after short-term application of octenidine based wound gel (active ingredient octenidine 0.05%) (IS: 10.3) and chlorhexidine digluconate 0.5% solution (IS: 9.5). Moderate reaction was observed for the combination of octenidine 0.05% in aqueous solution with panthenol 1.34% and allantoin 0.2% (IS: 8.7), hydrogen peroxide 1.5% in aqueous solution (IS: 6.1) and hydrogen peroxide 0.5% solution (IS: 5.5). Slight reaction was observed for hydrogen peroxide 1.5% solution in combination with sodium thiocyanate 0.698% (IS: 2.6), sodium thiocyanate 0.698% solution (IS: 2.1) and Dermacyn® (active ingredient NaOCl/HOCl each 0.004) (IS: 1.2). Polihexanide 0.04% in Ringer solution (IS: 0.9), Polihexanide 0.05% in Lipofundin, Granulox® (active agent hemoglobin 10%) (IS: 0) and dexpanthenol 5% solution (IS: 0) showed no reaction. In the long-term observation (24 hours after application), Dermacyn® showed the best results (59% of irritation remained alive after 24 hours). The addition of dexpanthenol and allantoin reduced the irritability only slightly, whereas the decrease of IS of hydrogen peroxide by addition of sodium thiocyanate was almost significant (p 0.0596).
Conclusion: It is suggested that agents with no or low irritation potential on the CAM are to be preferred in the clinical practice if they are clinically effective. It is suggested that further in vivo and in vitro studies are to be undertaken with these agents.
Solely regarding local tolerability, polihexanide and hypochlorite are the antiseptic agents of choice of the tested preparations. The wound oxygenizer hemoglobin spray is tolerated without irritation as well as the negative control 0.9% NaCl solution. Because of their other disadvantages in conjunction with their irritability, the outdated cream formulations on basis of silver sulfadiazine, PVP- iodine, chlorhexidine and nitrofural cannot be recommended for wound antisepsis.
Aiming at the goal of individualized medicine, this dissertation develops a generic methodology to individualize risk factors and phenotypes via metabolomic data from the urine. As metabolomic data can be seen as a holistic representation of the metabolism of an organism at certain time point, metabolomic data contain not only information about current life-style factors like diet and smoking but also about latent genetic traits. Utilizing this integrative attribute, the dissertation delivers a metric for biological age (the metabolic age score) which was shown to be informative beyond chronological age in three independent samples. It was associated with a broad range of age-related comorbidities in two large population-based cohorts, predicted independently of classical risk factors mortality and, moreover, it predicted weight loss subsequently to bariatric surgery in a small sample of heavily obese individuals.
Subsequently to this work, the dissertation built a definitional framework justifying the procedure underlying the metabolic age score, delivering a general framework for the construction of individualized phenotypes and thereby an operationalization of individualization in statistical terms. Conceptualizing individualization of the process of differentiation of individuals showing the same phenotype despite different underlying biological traits, it was shown formally that the prediction error of a statistical model approximating a phenotype is always informative about the underlying biology beyond the phenotype if the predictors fulfill certain statistical requirements. Thus, the prediction error facilitates the meaningful differentiation of individuals showing the same phenotype. The definitional framework presented here is not restricted to any kind of data and is therefore applicable to a broad range of medical research questions.
However, when utilizing metabolomic data, technical factors, data-preprocessing, pre-analytic features introduce unwanted variance into the statistical modeling. Thus, it is unclear whether predictive models like the metabolic age score are stable enough for clinical application. The third part of this doctoral thesis provided two statistical criteria to decide which normalization method to remove the dilution variance from urinary metabolome data performs best in terms of erroneous variance introduced by the different methods, aiding the minimization of biological irrelevant variance in metabolomic analyses.
In conclusion, this doctoral thesis developed a general, applicable, definitional framework for the construction of individualized phenotypes and demonstrated the value of the methodology for clinical phenotypes on metabolomic data, improving on the way the statistical treatment of urinary data regarding the dilution correction.
The “East German National Park Programme” of 1989/1990 was considered a coup de main, resulting in the immediate protection of 4.5% of the GDR’s territory. The authors of this programme later described the approach and its success as “using a window of opportunity during the transition phase of state and nation.” This leads to the question whether a state’s transformation period constitutes a preferred time frame and momentum for spatial conservation success.
Conservation efforts in Azerbaijan showed a similar success as the East German National Park Programme. In a country with the highest biodiversity in Europe, increasing the share of protected land from 5.0 % in 2001 to 10.3% in 2015 constitutes a remarkable achievement. Thus, the country became an interesting case study regarding the question whether “hot moments for conservation” exist in times of political and governmental changes, and if spatial success in nature conservation can be linked to political transformation. This thesis attempts to identify how the protected area (PA) network in Azerbaijan could be expanded by 100%, what achievements were made, and what conditions still need to be met for the quantitative and qualitative improvement of the PA network. To this end, I consider this increase under landscape-ecological, historical and institutional aspects. The local culture and political pre-sets in the country present additional issues for analysing the past 25 years of nature conservation in Azerbaijan.
Foot-and-mouth disease virus (FMDV) is a positive-sense RNA virus of the family Picornaviridae that comprises of seven serotypes and is distinguished by a high contagiosity with the ability of rapid spread. Strategies for abatement and control are based on an early detection, quick initiation of retaliatory actions and mass vaccinations. Therefore, aim of the study was the development of a fast and easy method for genome sequencing as well as an investigation into the causes, why some cell lines that are mainly used for vaccine production, are resistant towards FMDV infection. Finally, adaptive sequence changes in different cell culture systems and associated effects on particle stability and immunogenicity were examined.
In case of an outbreak it is of major importance to detect and rapidly characterize the circulating virus isolate to choose an appropriate vaccine to minimize the viral spread. In addition, comprehensive genome analysis of the outbreak strain provides information about the origin of the virus and allows molecular epidemiology. A universal primer set, covering most parts of the open reading frame of the viral genome, was developed to perform quick sequence analyses, independently of the viral serotype (Paper I). Especially in endemic regions, vaccination of susceptible animal species is the main action to combat foot-and-mouth disease (FMD) in an acute outbreak situation as well as a preventive measure. Reasons, why some baby hamster kidney (BHK) cell lines are resistant towards an infection with FMDV, were examined in a second study that narrowed down the cause for this phenomenon to an impaired attachment of the virus to the cell surface. Furthermore, an alternative approach could be developed to successfully adapt the virus to the resistant vaccine-production cell line by using a FMDV-sensitive “wet-nurse” cell line (Paper II). Adaptive changes in the capsid-coding region of the viral genome caused through cultivation and passaging of the virus in different BHK cell systems were the topics of the third study. It was shown that capsid alterations are rather serotype-specific and dependent on the cell line used than influenced by the cell media. Viral titers and neutralization profiles of the adapted isolates were not affected compared to the original viruses (Paper III).
Overall, this work expanded our knowledge on the control and eradication of FMD and will support the global effort to combat the disease.
Since its introduction in 2006, the NOD/scid mouse model has greatly contributed to the understanding of the pathomechanisms of antibody-mediated thrombocytopenia. This progress has however been hampered by inter-laboratory differences. With this work, we make several suggestions to minimise these differences:
We suggest that human platelets (blood group 0) be injected into the mice (age- and sex-matched, 8-16 weeks) via the tail vein. For antibody injection, scientists may choose between intraperitoneal and tail vein injection, each of which has strengths and drawbacks. In case of low antibody titer or low avidity antibodies, preincubation of the platelets with the patient serum prior to injection promotes platelet elimination where standard protocols fail. For subsequent sample preparation, we found that newly-launched ready-to-use kits present a good alternative to classical density gradient centrifugation by reducing man-hours and turnover time without affecting the quality of flow cytometry analysis.
In a second part, we used the revised mouse model to study anti-CD36 mediated thrombocytopenia in vivo. Anti-CD36 antibodies have been suggested as frequent case for FNAIT in Asia. The mechanisms behind this remain partly unclear. After injecting anti-CD36 monoclonal antibody or anti-CD36 patient immunoglobulin into the system, circulating human platelets were rapidly cleared. Interestingly, the polyclonal patient immunoglobulins used were not uniform in their anti-platelet reactivity. On further examination, we found that the anti-CD36 antibodies induce platelet activation and aggregation, which we were able to inhibit by the addition of an Fcγ-receptor blocking agent. This suggests a possible role for Fcγ-receptor in the activation and elimination process.
As our results from the experiments on the role of complement in the elimination process are however ambiguous, further studies are needed. The clinical relevance of anti-CD36 antibody-mediated platelet activation and aggregation for the high abortion rates in affected women has yet to be evaluated.
This work examines the influence of monovalent and divalent cations on tetramyristoyl cardiolipin (TMCL) monolayers. A lipid monolayer can undergo an ordering transition of the lipid alkyl chains from a disordered fluid phase (liquid-expanded (LE)) to an ordered gel phase (liquid-condensed (LC)). Compression of the lipid monolayer in a Pockels-Langmuir trough was monitored with a Wilhelmy plate tensiometer, yielding the surface pressure π in dependence of the area a molecule can occupy on average A, as a π-A-isotherm. The onset of the first order LE/LC phase transition is marked by an abrupt change in the isotherm at surface pressure πc.
These associated lipid membrane changes were characterized by variation of the compression speed, kind and concentration of the monovalent and divalent salt, pH, and temperature. The CL monolayer phase transition was found to depend on the compression speed, yielding only a small variation in the compression isotherms.
For monovalent cations on the cardiolipin monolayer, the dependence on salt concentration of the lipid liquid gel phase transition surface pressure πc was determined and a non-monotonic behavior was found, with a maximum in πc for a salt concentration of 0.1 mol/l. The maximum in πc can be shifted with pH (e.g. pH = 4.2). This behavior extended to potassium, sodium and cesium cations in the subphase. No ion specific effects were observed, which pointed to the prevalence of electrostatic interactions in the system.
Different divalent salt subphases, of either magnesium, calcium, strontium, manganese, iron or zinc salts, with fixed sodium chloride concentration of 0.15 mol/l at pH of 5.8 and 25 °C were investigated. πc decreases upon addition of divalent salts to the subphase. This points to increased screening and binding effects. Strongest binding effects were observed for calcium and manganese cations.
The electrostatic interactions of the system were modeled with a mean-field theory: Grahame’s equation, and a simple law of mass action. CL is modeled at half its molecular area and half its charge, with a proton dissociation constant of the phosphate group Ka,intrinsic(PO4) = 0.1 mol/l. The agreement with the experiment was satisfactory.
A linear dependence of πc on the temperature was found for cardiolipin monolayers on all subphases. The isothermal area compressibility modulus KA is calculated from selected isotherms. It was found that the flexibility of the monolayer decreases with temperature and the area per molecule for the cardiolipin fluid phase.
The compression speed, monovalent salt concentration, pH, and selected divalent cations were investigated with the BAM. For all a sigmoidal growth of xgel with compression was observed. For high salt concentrations non-circular and dendritic domains were observed.
A simple model for the nucleation process was introduced, yielding an estimate of 20 nm for the critical domain radius, which is below the resolution of the BAM, but a common length scale in biological systems.
The intracellular life cycle of the human immunodeficiency virus (HIV) is modelled using ordinary differential equations (ODEs). Model parameters are obtained from the literature or fitted to experimental data using parameter estimation procedures. Key steps in the life cycle are inhibited singly and in combination to show the effects on viral replication. The results validate the success of highly active antiretroviral therapy (HAART), and in addition DNA nuclear import is identified as a novel influential therapeutic target.
Lead-cluster investigations
(2017)
In this thesis, investigations on lead clusters stored in a Penning trap are presented. The measurements are performed at the ClusterTrap setup at the Institute of Physics of the University of Greifswald. A Penning trap with a superconducting magnet (B=12 Tesla) makes up the central part of the experiment. In this trap, singly positively or negatively charged lead clusters (a group of lead atoms) are stored, their amplitudes of motion are cooled, and a specific cluster size is selected. Thus, clusters of only a single size are prepared for experimental investigation. After interactions with electrons and/or photons, the trap content is extracted and analyzed by time-of-flight mass spectrometry.
In the first experiment, the size-selected clusters are excited by a frequency-doubled Nd:YAG laser, which leads to fragmentation processes. The preferred fragmentation pathway, which is observed to be break-off of a seven-atom neutral cluster is unusual for metal clusters, which typically evaporate monomers. Furthermore, the already known magic cluster sizes are observed.
In a subsequent experiment, positively charged lead clusters with 31 atoms are irradiated with laser light and fragmentation processes are time resolved investigated. The assumption that lead clusters fragment by break-off of neutral heptamers is confirmed.
In the following experiment, an electron beam is guided through the Penning trap to ionize pulsed-in argon atoms. While the positive argon ions leave the trap, the secondary electrons are trapped together with the selected lead clusters. This allows the electrons to attach to the singly charged lead clusters, which leads to multiply negatively charged lead clusters. The relative abundance of multiply-charged clusters is measured with respect to the cluster size, from which the appearance sizes of di- and trianions can be calculated. In addition to the attachment of electrons, fragmentation products similar to those of the photoexcitation measurements are observed. Furthermore, the cluster sizes 10 and 12 are observed regardless of the investigated precursor size, together with clusters of the precursor size reduced by 10 and 12. This is a first hint for a fission process of doubly negatively charged lead clusters into two singly charged products. In a following measurement, doubly charged lead clusters are produced and photoexcited. The observed abundance spectra confirm this assumption.
Certain basal Teleostei from the Early Jurassic of Mecklenburg-Western Pomerania (Germany) and the Late Jurassic of the Franconian Alb (Bavaria, Germany), the Swabian Alb (Baden-Württemberg, Germany) and the western Jura-Mountains (Ain, France) are described. The present doctoral dissertation includes four studies, dealing with representatives of “Pholidophoriformes”, Leptolepidae and Orthogonikleithridae. These studies include anatomical descriptions of new taxa and reviews of poorly known fishes. Furthermore, the stratigraphic and palaeobiogeographical distributions of the examined taxa are discussed.
There is multiple evidence that emotionally arousing events are preferentially processed, and better remembered than neutral events. In the present dissertation I investigated whether those strong emotional memories are affected by acute and chronic stress. Moreover, I was interested in whether already established emotional memories can be changed by behavioral intervention. According to the modulation hypothesis, emotionally arousing events promote attention and memory processes via noradrenergic and glucocorticoid actions. Recent models suggest that stress hormones differentially impact mnemonic processing, namely encoding, (re-) consolidation and memory retrieval, depending on timing and duration of the stressor relative to the learning experience. Acute stress around the time of encoding has been found to enhance memory, whereas chronic stress has been associated with memory impairments. Furthermore, consolidated memories are not resistant to modifications. Following reactivation, memories can turn into an unstable state and undergo a process called reconsolidated in order to persist. During this vulnerable state, memories are prone to modification, for instance by pharmacological blockade or interference learning. Here, the modulation of newly formed emotional and neutral memories as well as existing emotional and neutral memories was investigated in a well-established picture viewing and recognition memory paradigm using behavioral and neurophysiological measures (event-related potential, ERPs). More elaborative processing of emotional, relative to neutral stimuli has been related to the late positive potential (LPP). During encoding of emotional and neutral pictures, enhanced LPPs (starting at about 400 ms after stimulus onset) are usually observed for emotionally arousing relative to neutral pictures, indicating preferential attention allocation and processing. During recognition, correctly recognized old items evoke larger ERP amplitudes than correctly identified new items. This difference, the ERP old/new effect, was used to measure mnemonic processing during retrieval. The ERP old/new effect over centro-parietal sensor sites (400-800 ms) has been associated with recollection processes, and is enhanced for emotional, compared to neutral materials. Three studies are presented, that investigated 1) the influence of acute stress prior to encoding on long-term memory and its neural correlates, 2) the impact of chronic stress on encoding and memory, and 3) the influence of interference on already established memories (reconsolidation), always contrasting emotionally arousing and neutral scenes. Study 1 investigated subsequent recognition memory after encoding following acute stress using a socially evaluated cold pressure test, while study 2 tested the influence of chronic stress investigating breast cancer survivors about two years after cancer treatment. In study 3, one day after encoding, reconsolidation of the reactivated picture memory was targeted with an interfering learning task. In all three studies, recognition memory was tested one week later. High-density electroencephalograms (EEGs; 257 electrodes) were recorded to measure brain potentials. The results showed, in line with previous research, that emotionally arousing scenes were preferentially processed, as indicated by larger LPPs, and were better remembered than neutral scenes, as indicated by enhanced memory performance and larger ERP old/new differences. Experiencing acute stress prior to encoding enhanced the centro-parietal ERP old/new effect for emotionally arousing pictures at recognition, corroborating that acute stress facilitates memory for emotional scenes (Study 1). In contrast, attenuated LPPs for unpleasant pictures and impaired memory performance for arousing pictures were observed in breast cancer survivors (Study 2), indicating altered attention to emotion and subsequent emotional memory storage in chronically stressed individuals. When memory reactivation was followed by an interfering learning task, recognition memory and ERP old/new differences were attenuated for emotionally arousing scenes, selectively, showing the possibility that emotional memories might be modulated by behavioral interventions (Study 3). The results of all three studies are discussed and integrated into a model of memory modulation by stress and interference. The results highlight the importance of understanding the role of emotional arousal in the processes of memory formation, retrieval and reconsolidation. Moreover, shedding light on the differential effects of acute and chronic stress, interference and their possible interactions might help to prevent and even modify impairing memories that are one of the major concerns in stress- and fear-related mental disorders.
Costs of reproduction. A demographical approach to examine life-history trade-offs ─ Abstract. Resource-allocation trade-offs are fundamental constraints of life-history evolution. In particular the trade-offs between reproduction and longevity and between present and future reproduction are expected to form reproductive patterns. Unfortunately, exploring such trade-offs in natural populations is complicated and may not be possible. In face of several limitations, zoo data appear to be useful to better understand the reproductive biology of endangered, rare or cryptic species. In the first step, it was sought after with a data-mining, comparative multi-species approach for broad patterns of correlations between lifespan and variables in bird-eating spiders (Theraphosidae). The subfamily Eumenophoriinae on average lived longest, followed by the Theraphosinae, Ornithoctinae, Grammostolinae, Selenocosmiinae, Ischnocolinae and finally the Avicularinae. Species inhabiting tropical, more humid and/or low-altitude environments lived longer, suggesting that more predictable environments favour the evolution of longer lifespans. Furthermore, large range size, low abundance, sub-terrestrial life-style, and aggressive behaviour were all linked with longer lifespans. An argument for resource allocation trade-offs was found as larger spiderling and prosoma size were negatively related to longevity. In the second step, a demographical approach has been applied for two old-world deer species (Vietnamese sika deer Cervus nippon pseudaxis, Mesopotamian fallow deer Dama dama mesopotamica). In both species, births peaked right before the onset of the rainy season in natural environments. Females reached high reproductive output earlier in life and had (in one species only) higher survival rates than males. Offspring number covaried positively rather than negatively with longevity. In females, the length of the reproductive phase correlated positively with longevity, birth rate within the entire lifespan, and offspring number, while it was negatively correlated to the birth rate during the reproductive phase (in one species). The length of the post-reproductive phase was positively related to longevity and negatively to birth rate during the entire lifespan. In the third section, life-histories of Asiatic (Equus hemionus ssp.) and African wild asses (Equus africanus ssp.) have been anlaysed in a comparative way with another demographical long-term approach. All taxa showed even in captivity peak birth rates during the periods of highest food availability in their natural environments. Sex-specific survival rates with females living longer than males were evident in Kulan and Onager but not in Kiang and Somali wild ass, pointing towards different life-history strategies even among closely related taxa. Females achieved their highest reproductive output earlier than males, which is typical for polygynous mating systems. Offspring number and longevity were rather positively correlated than negatively. Taken together evidence for reproductive trade-offs was weak, though the length of the reproductive period was negatively related to birth rates within the reproductive period. Birth intervals increased with female age, probably reflecting detrimental effects of senescence.
Quang Xuong is considered as one of the most developed districts in Thanh Hoa Province in terms of agricultural. The major purpose of this research is to find good places to suggest for annual crops production in the case study. Therefore, the assessment of land potential productivity, land suitability, and land cover/land use change in different periods is essential for making strategies of sustainable agricultural development as this will help land-users and land managers to discover the potential and limitations of the current existing land conditions to make appropriate policies and plans for future land use. Its results will provide basic information to make reasonable decisions for investments and rational reclamations of cultivated land before and after each crop season in order to meet the objectives of sustainable development in terms of economic efficiency, social acceptability, and environmental protection. The research site is located at latitudes 19 degree 34 minute N - 19 degree 47 minuteN and at longitudes 105 degree 46 minute E - 105 degree 53 minute E. The total area is about 227km2; in which 128km2 is in use for agricultural activities. Based on soil classification methods by FAO-UNESCO (1988), the agricultural land is classified into six main soil groups, including Arenosols, Salic Fluvisols, Fluvisols, Gleysols, Acrisols, and Leptosols, 12 soil units and 18 sub-units. The largest area belongs to the Fluvisols group with 9358.29ha and the smallest area is identified as the Leptosol group with 219.33ha. Most of the soil in this district has low to moderate nutrition, but in general, they are still suitable for agricultural production. There are 42 land units defined in the land mapping, which can be different from each other by one or more land characteristics. The land mapping unit is created from the overlay of all thematic maps of soil chemicals, soil physical characteristics, and relative topography together by application of GIS techniques. It presents land characteristics and properties in this case study and will be used in comparasion with a particular crop requirement for growth in land suitability evaluation process. A certain land unit may be suitable for one or more types of different land use. It is also classified as highly suitable for a specific land utilization type, but less suitable or unsuitable for other crops. For example, in this study, land unit 26 is determined as highly suitable (S1) for growing paddy rice and maize, but it falls into moderately suitability (S2) for groundnut crop by using parametric (square root) method used in this thesis. Depending on the kind of crops need to be evaluated and its requirement for development compared with each land unit characteristics, land-users will determine the best suitable place for crop production. Identification of land use change in different periods of time has become a central key to monitoring of land resources. It is relatively important for effective land management to protect the land resources, especially the land used for agricultural production from overuse and environmental changes. The sprawl of inhabitant areas, development of rural infrastructures, and industrialization are responsible for serious losses of agricultural land. In this study, remote sensing techniques were applied to studying the trends of land cover change in the abovementioned district in a period of about 24 years from 1989 to 2013. ArcGIS software was adopted to develop the land cover and the change of land use maps from 1989 to 2013. Two satellite images with moderate resolution were collected from USGS Earth Explorer website, Landsat5 TM for 1989 and Landsat8 OLI & TIRS for 2013. After image geo-processing, the images were classified into six land cover categories by applying supervised classification method (Maximum Likelihood). The six main obtained land cover types were built-up areas, agricultural land, forest land, water surface area, salty land, and unused land. The overall accuracies of land cover maps for 1989 and 2013 were 94.08% and 92.91%, respectively. The results of change detection analysis indicate that the cultivated, water surface and unused lands decreased by 22%, 17%, and 91%, respectively. In other side, the built-up and salty land increased by 78%, 58%, respectively and forest land increased from 52.69ha in 1989 to 395.76ha in 2013. The assessment of land potential productivity for agricultural production and land suitability for selected annual crops was based on FAO guidelines for land evaluation (FAO, 1976, 1985, and 1993) which were adopted and slightly modified for compatibility with Vietnamese conditions. All related data were stored, analyzed, mapped and presented in ArcGIS software. Weighted Linear Combination Method developed by Hopkins (1977) and GIS techniques were used to analyze and determine the land potential for agricultural use in the study area. The results show that 5.26%, 83.10%, 10.06%, and 1.57% of the investigated areas were assessed as high potential, moderate potential, low potential and very low potential for growing crops. Regarding land suitability evaluation, the simple limitation, parametric (square root), and AHP methods were used to evaluate the suitability levels for selected crops, including paddy rice, sweet potato, groundnut, maize, potato, sesame, soybean, and green pepper. The obtained results indicate that each applied method provides different results of land suitability level for a specific crop in certain land units compared to the other two methods, and OM, soil pH, soil texture, and relative topography were found out as the main limitation factors which affected land suitability level. The study also suggests that three different methods as abovementioned can be expanded and applied in other places with the appropriate factors used for land suitability evaluation according to particular area conditions.
This thesis highlights the impact of surface charges and negative ions on the pre-ionization, breakdown mechanism, and lateral structure of dielectric barrier discharges operated in binary mixtures of helium with nitrogen or electronegative oxygen. Sophisticated diagnostic methods, e.g., non-invasive optical emission spectroscopy and the electro-optic Pockels effect as well as invasive laser photodetachment and laser photodesorption, were applied at one plane-parallel discharge configuration to investigate both relevant volume and surface processes. Moreover, the experimental findings were supported by numerical fluid simulations of the discharge. For the first time, the memory effect of the measured surface charge distribution was quantified and its impact on the local self-stabilization of discharge filaments was pointed out. As well, it turned out that a few additional seed electrons, either desorbed from the charged dielectric surface or detached from negative ions in the volume, significantly contribute to the pre-ionization resulting in a reduced voltage necessary for discharge breakdown. Finally, effective secondary electron emission coefficients of different dielectrics were estimated from the measured breakdown voltage using an analytical model.