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We study the effect of weakening creditor rights on distress risk premia via a bankruptcy reform that shifts bargaining power in financial distress toward shareholders. We find that the reform reduces risk factor loadings and returns of distressed stocks. The effect is stronger for firms with lower firm-level shareholder bargaining power. An increase in credit spreads of riskier relative to safer firms, in particular for firms with lower firm-level shareholder bargaining power, confirms a shift in bargaining power from bondholders to shareholders. Out-of-sample tests reveal that a reversal of the reform's effects leads to a reversal of factor loadings and returns.
Linear Ubiquitin chain Assembly Complex (LUBAC) is an E3 ligase complex that generates linear ubiquitin chains and is important for tumour necrosis factor (TNF) signaling activation. Mice lacking Sharpin, a critical subunit of LUBAC, spontaneously develop inflammatory lesions in the skin and other organs. Here we show that TNF receptor 1 (TNFR1)-associated death domain (TRADD)-dependent TNFR1 signaling in epidermal keratinocytes drives skin inflammation in Sharpin-deficient mice. Epidermis-restricted ablation of Fas-associated protein with death domain (FADD) combined with receptor-interacting protein kinase 3 (RIPK3) deficiency fully prevented skin inflammation, while single RIPK3 deficiency only delayed and partly ameliorated lesion development in Sharpin-deficient mice, showing that inflammation is primarily driven by TRADD- and FADD-dependent keratinocyte apoptosis while necroptosis plays a minor role. At the cellular level, Sharpin deficiency sensitized primary murine keratinocytes, human keratinocytes, and mouse embryonic fibroblasts to TNF-induced apoptosis. Depletion of FADD or TRADD in Sharpin-deficient HaCaT cells suppressed TNF-induced apoptosis, indicating the importance of FADD and TRADD in Sharpin-dependent anti-apoptosis signaling in keratinocytes.
Panama is a megadiverse country that together with Costa Rica constitutes Lower Central America (LCA). Western Panama's Cordillera Central accounts for the eastern part of the LCA highlands shared between these countries. The aim of the present study is to compile the most complete and updated picture possible of the taxonomy, diversity, and distribution of reptiles that occur from 500 m asl upwards along the Talamanca and Tabasará ranges. These two continuous mountain ridges account for the western two-thirds of the Cordillera Central between the Costa Rican border and 81°W Including specimens collected four own research travels, I morphologically examined more than 1800 specimens, analyzed 16S and/or COI barcodes of 300 specimens, and performed a thorough search in literature and databases to obtain locality records for specimens and species occurrences. My complete occurrence dataset comprises 14620 georeferenced occurrence records in three quality categories. Conceivable occurrences of species not yet documented from a given area are evaluated on the basis of existing data either as "plausible" or "possible". I provide all datasets which I generated for this study in Appendices. The previously published descriptions of Dactyloa ginaelisae Lotzkat, Hertz, Bienentreu & Köhler 2013, Norops benedikti (Lotzkat, Bienentreu, Hertz & Köhler 2011), Sibon perissostichon Köhler, Lotzkat & Hertz 2010, and Sibon noalamina Lotzkat, Hertz & Köhler 2012 are included in the present work. In the course of integrative taxonomic analyses, I classify 15 genealogical lineages revealed by DNA barcoding within 7 anole species as Deep Conspecific Lineages (DCLs) because they lack consistent morphological differences to their nominal conspecifics. I provisionally classify 18 mitochondrial lineages found within six other anole species as Unconfirmed Genealogical Lineages (UGLs) pending adequate analyses of their morphological variation. I regard the two additional UGLs Celestus sp. and Geophis sp. and the two Confirmed Genealogical Lineages (CGLs) Lepidoblepharis sp. 1 and 2 to represent undescribed species. My taxonomic analyses yield the hitherto most comprehensive survey of the variability exhibited by dozens of reptile species in western Panama. The 16S and/or COI barcodes I provide represent 65 species recognized herein and constitute the first DNA barcode reference library for LCA reptiles. The reptile fauna of Panama comprises 265 species, including the four UGLs and CGLs mentioned above and characterized for the first time in this study, as well as Dendrophidion crybelum Cadle 2012 whose presence in the country I consider plausible. My occurrence dataset reveals that 160 of these species have been documented to occur in my study area. Adding the 20 species whose occurrence therein I consider plausible, I report the total species richness of the Talamanca and Tabasará ranges as comprising 180 species representing 81 genera in 25 families. With 178.8 species per 10 000 km2, the relative species richness of the area is extremely high even in a tropical context. In view of their overall documented distribution, I regard the presence of 27 additional species in my study area as possible. For the 180 species occurring in my study area I provide standardized species accounts that, together with the taxonomic results, for the first time permit the doubtless identification of all 180 species, and illustrate 168 of these with color photographs. Concerning biogeography, my georeferenced dataset yields noteworthy distribution extensions for many species. Moreover, I present the hitherto most comprehensive, detailed, and reproducible assessments of the distribution patterns, historical origins, and conservation as well as of the occurrence among physiographic regions, climatic and altitudinal belts, political subdivisions, and protected areas, for my study area's reptile fauna. With 65 species, more than a third of the fauna is endemic to LCA. Among these, 42 Talamancan highland endemics are restricted to the LCA highlands, in the case of 16 small-scale highland endemics with documented ranges spanning less than 100 km. I assess many of these endemics as endangered. The fact that several of these species do not occur in any protected area renders the establishment of additional conservation areas necessary, especially in the central Serranía de Tabasará. Distributional range boundaries shared among different clades of highland anoles indicate physiographic and climatic barriers that may have effected in situ speciation within these lineages. As the largest study on Panamanian reptile diversity assembled to date, the present dissertation considerably increases our knowledge on the reptiles along the Cordillera Central and beyond, and thus constitutes a solid basis for future studies.
Drought stress is one of the major abiotic factors diminishing crop productivity world wide. In the course of climate change, regions which already experience dry seasons nowadays will suffer from elongated drought periods and water shortage. These climatic changes will not only have an impact on the regional flora and fauna but also on the people inhabiting these areas. It is therefore of great importance to understand the reactions of plants to drought stress to help breeding and biotechnological approaches for the benefit of new robust cereal cultures growing under low water regimes. In this dissertation four grasses of the genus Panicum, P. bisulcatum (C3), P. laetum, P. miliaceum and P. turgidum (all C4 NAD-ME) were subjected to drought stress. The plants diverse reactions were investigated on a physiological as well as on a molecular level to deepen the understanding of drought stress responses. Drought stress was imposed for a species-specific period until a relative leaf water content (RWC) of ~50 % was reached in each grass. Physiological measurements were conducted on leaves with a RWC of ~50 % investigating chlorophyll a fluorescence parameters with a Plant Efficiency Analyzer (PEA) and gas exchange parameters like the photosynthesis rate and stomatal conductance with a Gas Fluorescence Chamber (GFS-3000). Subsequent molecular analysis were conducted on leaf samples taken (RWC = 50 %) analysing different proteins and the transcriptome of the Panicum species. The physiological measurements revealed a higher photosynthesis rate for the C4 grasses under drought stress with no significant differences between the C4 species. Also the water use efficiency was significantly higher in the C4 species in comparison to the C3 species independent from the water regime supporting results from the literature. The chlorophyll a measurements revealed the strongest adaptation to water shortage in the C4 species P. turgidum followed by the C3 species P. bisulcatum. It has been shown before (GHANNOUM 2009) that the C4 photosynthesis apparatus is more prone to drought stress than the C3 apparatus – despite the higher water use efficiency. Results also suggested that the great adaptation of P. turgidum to drought stress arose from its ability to recover from drought stress (all JIP test parameters showed no significant differences between control and recovery samples). The additional down-regulation of PS II but not of PS I under drought stress also helped the plant to endure times of water shortage and facilitated the recovery when water was available again. Protein analyses on the content of PEPC, OEC and RubisCO (LSU and SSU) revealed no changes. Dehydrin 1 in contrast was strongly up-regulated under drought stress and Summary 108 recovery in all four Panicum species. The stable content of the OEC protein was therefore not the catalyst of rising K peaks measured by chlorophyll a fluorescence and a reduced OEC activity was supposed. Transcriptomic analyses revealed a myriad of differentially regulated tags. Due to unsequenced genomes, tags could only be partially (8 % maximum for P. turgidum) annotated to their specific genes. Diverse methods were therefore used to annotate the most highly regulated tags to their genes and their products. Special emphasis was put on the regulation of five gene products confirming the regulation schemata from the HT-SuperSAGE analyses. Interestingly one protein – the NCED1 – was down-regulated under stress conditions, in contrast to results from the literature. It is therefore of great importance to investigate longer lasting drought to understand the full range of drought stress adaptation. Future genome sequencing projects might also include the Panicum species investigated in this dissertation and important gene candidates with no hits (maybe completely new to the research community) might help breeding and biotechnology approaches to produce more drought resistant crop species.
This study describes the Holocene sedimentary lagoonal deposition history, including event sedimentation and benthic foraminiferal analyzes, from about 10 kyrs BP until today. This is the first study describing the sedimentation of a Maldivian atoll lagoon in such detail. Thirty-nine sediment cores have been recovered from the deep Rasdhoo Atoll lagoon of the Maldives (4°N/73°W). Seventeen sediment cores were opened, described, and 296 sediment samples have been collected and analyzed. Different methods have been used to evaluate the coarse- and fine-grained carbonate components and a total of fifty-eight samples have been dated radiometrically by Beta Analytic Inc., Miami, Florida. In general, the Rasdhoo Atoll lagoon sediments can be divided into (1) a Late Pleistocene soil, (2) an early Holocene peat layer composed of mangrove deposits which mark the beginning inundation of the atoll lagoon by the rising Holocene sea-level at 10,320 ± 100 yrs BP, and (3) carbonate sediments starting to fill up the lagoon 7850 ± 140 yrs BP until today. The transition from peat to carbonate is characterized by a considerable hiatus. Six different carbonate sediment facies are classified by statistical analyses, listed in decreasing abundance:
(1) mollusk-coral-algal floatstone to rudstone (30%)
(2) mollusk-coral-red algae rudstone (23%)
(3) mollusk-coral-algal wackestone to floatstone (23%)
(4) mollusk-coral wackestone (13%)
(5) mollusk-coral mudstone to wackestone (9%)
(6) mollusk mudstone (2%)
Based on grain-sizes in combination with coral identification, the facies represent both lagoonal background sedimentation (mostly fine-grained sediments (matrix >50%)) and event sedimentation (coarse-grained sediment layers composing reefal components).
Six coarser grained layers in muddy background sediments of the Rasdhoo Atoll lagoon were interpreted as Holocene tsunami events, based on the increase of allochthonous skeletal material with shallow-water reef affinity such as fragments of shallow-water coral species, coralline red algae, and reef-dwelling foraminifera in these layers, as well as AMS dating:
• Event 1: 420 - 890 yrs BP (655 yrs BP)
• Event 2: 890 - 1560 yrs BP (1225 yrs BP)
• Event 3: 2040 - 2340 yrs BP (2190 yrs BP)
• Event 4: 2420 - 3380 yrs BP (2900 yrs BP)
• Event 5: 3890 - 4330 yrs BP (4110 yrs BP)
• Event 6: 5480 - 5760 yrs BP (5620 yrs BP)
Five of the six layers may be correlated to previously published tsunami events at adjacent coastal research sites. The mid-late Holocene atoll lagoon archive is incomplete though based on the assumption that major earthquakes at the Indonesian subduction zone generated more than six major tsunamis during the past 6.5 kyrs.
According to Gischler (2006), the sediments of the Rasdhoo Atoll lagoon can be divided into two areas: (1) a central to marginal deep lagoon with a lateral west-to-east gradient of sediment facies distribution, visible in sections <4 kyrs BP with sedimentary facies of mudstone to wackestone in the western part (e.g., cores 16, 18, and 34) and coarse-grained coral and algal-rich sediments in the eastern part of the lagoon (e.g., cores 30 and 31). (2) A northern enclosed and shallow area between the sand apron and the sand spit accumulating “sandy” sediments of wackestone facies (cores 2, 19, 25, and 26).
Comparing the sediment accumulation data of the lagoon with two reconstructed local sea-level curves, three different sequence-stratigraphical systems tracts are visible: (1) a lowstand systems tract (LST) >10 kyrs BP. Pleistocene brownish soil superposing subaerially exposed Pleistocene reef limestone. (2) A transgressive systems tract (TST) 10-6.5 kyrs BP. A peat layer marks the beginning of the inundation, and the carbonate sedimentation starts with very low sedimentation rates of 0.02 m/kyr. (3) A highstand systems tract (HST) 6.5-0 kyrs BP, further divided into three stages (6.5-3, 3-1, 1-0 kyrs BP). The sea-level rise slowed down, sedimentation rates are increasing continuously up to a maximum of 1.4 m/kyr, the sand spit developed some 4 kyrs BP, the lagoonal circulation got restricted, and the lateral west-to-east gradient of grain-size accumulation started. From 1-0 kyrs BP the sedimentation rates slowed down to modern mean sedimentation rates of 0.6 m/kyr.
Two cores, one core from the center of the lagoon (core 16) and one core from the northern margin of the lagoon (core 19), have been analyzed on diversity and assemblages of benthic foraminifera in high-resolution. The transitions of Ammonia spp. to a more even and diverse fauna marks a significant environmental change at 7.0 kyrs BP in core 16 (onset of a stable environment in the deep lagoon after the sea-level rise slowed down at HST stage 1) and at 4.0 kyrs BP in core 19. A continuing environmental change after 1.4 kyrs BP in core 16 caused the fauna to become more even, a recovery of diversity and a permanent decline of foraminiferal accumulation rate. The changes in the faunas at 4.0 kyrs BP and at 1.4 kyrs BP could be explained with the sand spit formation in the northwestern and western lagoon. The sand spit has apparently acted as an obstacle in lagoonal circulation and might have caused unstable environmental conditions due to a more rapid circulation at the shallow marine site of core 19 and a slowdown of bottom water circulation in the main lagoon (core 16) leading to higher residence times and to lower oxygen and higher nutrient concentrations.
In the past sixty years, excessive water consumption and dam construction have significantly influenced natural flow regimes and surface freshwater ecosystems throughout China, and thus resulted in serious environmental problems. In order to balance the competing water demands between human and environment and provide knowledge on sustainable water management, assessments on anthropogenic flow alterations and their impacts on aquatic and riparian ecosystems in China are needed.
In this study, the first evaluation on quantitative relationships between anthropogenic flow alterations and ecological responses in eleven river basins and watersheds in China was performed based on the data that could be obtained from published case studies. Quantitative relationships between changes in average annual discharge, seasonal low flow and seasonal high flow and changes in ecological indicators (fish diversity, fish catch and vegetation cover, etc.) were analyzed. The results showed that changes in riparian vegetation cover as well as changes in fish diversity and fish catch were strongly correlated with the changes in flow magnitude (r = 0.77, 0.66), especially with changes in average annual river discharge. In addition, more than half of the variations in vegetation cover could be explained by changes in average annual river discharge (r² = 0.63) and roughly 50 % changes in fish catch in arid and semi-arid region and 60% changes of fish catch in humid region could be related to alterations in average annual river discharge (r² = 0.53, 0.58).
In a supplementary analysis of this study, the first estimation on quantitative relationships between decreases in native fish species richness and anthropogenic flow alterations in 34 river basins and sub-basins in China was conducted. Linear relationships between losses of native fish species and five ecologically relevant flow indicators were analyzed by single and multiple regression models. For the single regression analysis, significant linear relationships were detected for the indicators of long-term average annual discharge (ILTA) and statistical low flow Q90 (IQ90). For the multiple regressions, no indicator other than ILTA has significant relationships with changes in number of fish species mainly due to collinearity. Two conclusions emerged from the analysis: 1) losses of fish species were positively correlated with changes in ILTA in China and 2) indicator of ILTA was dominant over other flow indicators included in this research for the given dataset. These results provide a guideline for the sustainable water resources management in rivers with high risk of fish extinction in China.
Within the nucleosynthetic processes of the slow neutron-capture reaction network (called the s process) the so called branching points, unstable isotopes where different nuclear reactions are competing, are important to understand . For modeling and calculating the nucleosynthesis and compare the resulting abundances to the observed ones, it is indispensable to know the branching ratios as well as the corresponding cross sections.
A great challenge in measuring those rates in experiments may be the radioactivity of the isotopes involved, which can make it nearly impossible to manufacture the needed targets. In addition, in stellar environments the excited states of isotopes can be in equilibrium with the ground state, affecting the half-lives and the branching ratios significantly. The isotope 152Eu is such a branching point, with neutron captures and β-decays competing. Those challenges were approached in the s405 experiment performed at the GSI Helmholtzzentrum für Schwerionenforschung GmbH: the challenge the challenge of the radioactivity can be approached by experiments carried out in inverse kinematics with radioactive beams, solving the problem of unstable targets. Also a reversed reaction was used to access the excited states of the studied isotope. The performed 152Sm(p,n)152Eu is a pioneering attempt to use those methods on heavy ions. The (p,n) reaction was used as a substitute for electron capture, the focus lies on reactions with low-momentum transfers, resulting in the emission of low-energy neutrons. The new developed low-energy detector array LENA was put to test for the fist time in the s405 experiment.
Understanding major causes of biodiversity and range dynamics requires research on evolutionary processes under consideration of environmental changes. In my thesis, I investigated the spatio-temporal evolution of the Neotropical tree genus Cedrela from the Meliaceae family by studying its genetic diversity, taxonomy, colonization history, climatic niche changes and dynamics of species distributions. My results show that climatic and geological changes are major drivers of biological diversification in Cedrela.
In the interest of understanding the development of a multicellular organism, subcellular events must be seen in the context of the entire three-dimensional tissue. In addition, events that occur within a short period of time can be of great importance for the relatively long developmental process of the organ. Thus, it is required to capture subcellular events in a larger spatio-temporal scale context, which has been up to now a technical challenge. In developmental biology, light microscopy has always been an important tool. The dilemma of light microscopy, in particular fluorescence microscopy, is that molecules receive high light intensities that might change the conformation of molecules, which can have signaling or toxic effects. In Light Sheet-based Fluorescence Microscopy (LSFM), the energy required for a single recording is reduced by several orders of magnitude compared to other fluorescence microscopy techniques. During the last ten years, LSFM has emerged as a preferred tool to capture all cells during embryogenesis of the zebrafish Danio rerio, the fruit fly Drosophila melanogaster or recently the red flour beetle Tribolium castaneum for a period of several days. The motivation of this work was to gain new insights in developmental related processes of plant organs. The aim of this work was to establish a protocol for imaging plant growth over a long period of time using LSFM and perform comprehensive analyses at the cellular level. Plants have to cope with a variety of environmental conditions, therefore the conditions inside the microscope chamber had to be brought under control. The sample preparation methods and the standardized conditions at a physiological level allowed the study of gravity response, day-night rhythms, organ shape development as well as the intracellular dynamic events of the cytoskeleton and endosomal compartments in an unprecedented manner. Several of these projects were successfully published in collaborations with Prof. Jozef Šamaj (Palacký University Olomouc, Czech Republic), Prof. Niko Geldner (University of Lausanne, Switzerland), Prof. Malcom Bennett (University of Nottingham, UK) and Dr. Jürgen Kleine-Vehn (University of Natural Resources and Life Sciences, Austria). The main part of my work focused on the formation of lateral roots in Arabidopsis thaliana and was conducted in close collaboration with Dr. Alexis Maizel (University of Heidelberg, Germany). Previously, most experiments that describe lateral root formation have been performed on a small number of cells and for short periods of time. Capturing the complete process of lateral roots is an ambitious goal, because first, the primordium of a lateral root is located deep inside the primary root and imaging quality is impaired due to scattering of the overlaying tissue. Second, the process takes about 48 h, i.e. the plant has to be kept healthy for the whole period. Third, the amount of excitation light required for the spatio-temporal might have phototoxic effects that lead to a stop of growth at least in conventional microscopic techniques. In Arabidopsis embryogenesis, the sequence of cell divisions is relatively invariant. However, whether lateral root organogenesis follows particular cell division patterns has been unknown. The complete process of lateral root formation was captured from the first cell division until after the emergence from the main root. Images of a nuclei marker and a plasmamembrane marker were recorded every 5 min for a time period of up to 64 h. The positions and cell divisions of all cells were tracked manually. In collaboration with Alexander Schmitz (Goethe University Frankfurt am Main, Germany) and Dr. Jens Fangerau (University of Heidelberg, Germany), comprehensive analyses of the data were performed. A lateral root forms from initially 8-15 founder cells, arranged in a patch of 5-8 parallel files. The occurrence of new cell layers by periclinal divisions, as well as the sequence of layer generation was conserved and resembles the sequence suggested by Malamy and Benfey in 1997. Besides this stereotyped occurrence of periclinal divisions, radial divisions were found to appear stochastically, following no particular pattern. A large variability was also found in the contribution of founder cells and cell files to the final lateral root. In summary, the results suggest that a stereotyped pattern of cell divisions at particular developmental stages and a dynamically adapted control of cell divisions exist in parallel. Both properties allow a controlled but flexible development of the organ according to variations in cell topology and mechanical properties of the surrounding tissue. This work shows that LSFM, the sample preparation methods and controlled environmental conditions allow to capture and analyse the development of plants over several days at high resolution in an unprecedented manner.
This thesis presents experimental studies of proton capture and fragmentation reactions with heavy-ion storage rings. In one experiment, the 96Ru(p, γ)97Rh cross sections near the Gamow window have been measured at the ESR of GSI. In the other experiment, the measurement of the fragmentation yields has been carried out at the CSRe of IMP.
It is essential to determine the cross sections of (γ, p) or (p, γ) reactions for p-process network calculations. However, only very few of the required cross sections have been measured and thus most of them rely solely on Hauser-Feshbach model predictions. The predictions of the model have always very large uncertainties because of the not well-known input parameters. These parameters can be constrained by experiments. Compared to the traditional activation technique, a novel method using a storage ring has been developed to measure the cross sections of (p, γ) reactions in inverse kinematics.
This proton capture experiment has been performed at the ESR, where the circulating 96Ru44+ ions interacted with a hydrogen gas target at 9, 10 and 11 MeV/u. The nuclear reaction products of (p, p), (p, α), (p, n) and (p, γ) reactions were registered by position sensitive detectors. A Geant4 simulation code has been developed to distinguish the (p, γ) reaction products unambiguously from the background reactions. In this work, a relative normalization method has been utilized to accurately determine the cross sections of the (p, γ) reaction. The 96Ru(p, γ)97Rh cross section in the Gamow window of the p process is sensitive to two parameters, i.e., the γ-ray strength function and the optical model potential, while it is mainly sensitive to the γ-ray strength function in the energy region of our experiment. Therefore, our experimental (p, γ) cross sections near 10 MeV/u have been used to directly constrain the γ-ray strength function used in the model. Furthermore, the proton potential has also been constrained by combining our results with additional experimental data for this reaction in the lower energy region. The constrained model has been used to calculate the reaction rate over a wide temperature range, which is an extremely important input for astrophysical calculations.
The yields of fragments produced by 78Kr fragmentation reactions have been measured at the CSRe for the Tz = −1/2 and Tz = 1/2 nuclei along or close to the paths of αp- and rp-processes. The measured yields present a significant odd-even staggering effect for Tz = −1/2 nuclides but they are small for Tz = 1/2 nuclides.
The magnitude of this effect for four consecutive yields has been quantified using a third-order difference formula. It is found that the largest odd-even staggering is reached near the closed shells Z = 20 and Z = 28. Our experimental results could also compared with the data from other experiments with different projectile-target combinations. All these experimental data strongly support the closed shells Z = 20 and Z = 28 for the Tz = −1/2 nuclei.