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Das vorliegende Arbeitspapier ist die unveränderte Fassung einer Diplomarbeit, die von Michael Grimm während einer Dauer von vier Monaten am Institut für Konjunktur, Wachstum und Verteilung der Universität Frankfurt a. M. geschrieben wurde. Die Ergebnisse der Analyse halte ich für so interessant, daß mir eine Veröffentlichung als Arbeitspapier im Rahmen des von mir geleiteten EVS-Projektes, dessen Daten die Grundlage der Arbeit bilden, als lohnend erscheint. Dadurch kann sichergestellt werden, daß die Untersuchungsergebnisse Interessierten zur weiteren Nutzung, sei es als reine Informationsgrundlage oder als Ausgangspunkt weiterer Analysen, zur Verfügung stehen. Die Studie beleuchtet die Verteilung von Geld- und Grundvermögen auf sozioökonomische Gruppen in der Bundesrepublik Deutschland. Als Datenbasis wurde eine Datenbank mit (anonymisierten) Individualdaten der Einkommens- und Verbrauchsstichprobe 1988 der Universität Frankfurt a. M. genutzt. Anknüpfend an frühere Arbeiten, die zu diesem Themenkomplex im Rahmen des Sonderforschungsbereichs 3 "Mikroanalytische Grundlagen der Gesellschaftspolitik" angefertigt wurden sowie durch Berücksichtigung von Daten zur EVS 1993, die zum Untersuchungszeitpunkt allerdings nur in tabellierter Form vorlagen, skizziert die Analyse eindrucksvoll die Entwicklung der Vermögensverteilung bis in die neunziger Jahre hinein. Dabei zeigt sich, daß die Verteilung des Vermögens, im Vergleich zur Verteilung der Einkommen, einen weiterhin sehr hohen Konzentrationsgrad aufweist. Insbesondere auf der Personenebene hat sich der Grad der Konzentration im Laufe der achtziger Jahre sogar noch verstärkt. Auch die Betrachtung der Verteilung auf sozio-ökonomische Gruppen zeigt viele interessante und neue Ergebnisse, so daß die Analyse ein echter Erkenntnisfortschritt ist. Es bleibt zu hoffen, daß weitere Arbeiten auf Basis der Einkommens- und Verbrauchs stichproben 1993 und 1998 sich der Entwicklung der Vermögensverteilung, insbesondere auch in den neuen Bundesländern, widmen und so eine langfristige Informationsgrundlage für Wirtschafts- und Sozialpolitik schaffen. Frankfurt am Main, im März 1998 (Richard Hauser)
Methanogenic archaea are a group of strictly anaerobic microorganisms characterized by their strict dependence on the process of methanogenesis for energy conservation. Among the archaea, they are also the only known group synthesizing proteins containing selenocysteine or pyrrolysine. All but one of the known archaeal pyrrolysine-containing and all but two of the confirmed archaeal selenocysteine-containing protein are involved in methanogenesis. Synthesis of these proteins proceeds through suppression of translational stop codons but otherwise the two systems are fundamentally different. This paper highlights these differences and summarizes the recent developments in selenocysteine- and pyrrolysine-related research on archaea and aims to put this knowledge into the context of their unique energy metabolism.
A new artificial regulatory system for essential genes in yeast is described. It prevents translation of target mRNAs upon tetracycline (tc) binding to aptamers introduced into their 5'UTRs. Exploiting direct RNA–ligand interaction renders auxiliary protein factors unnecessary. Therefore, our approach is strain independent and not susceptible to interferences by heterologous expressed regulatory proteins. We use a simple PCR-based strategy, which allows easy tagging of any target gene and the level of gene expression can be adjusted due to various tc aptamer-regulated promoters. As proof of concept, five differently expressed genes were targeted, two of which could not be regulated previously. In all cases, adding tc completely prevented growth and, as shown for Nop14p, rapidly abolished de novo protein synthesis providing a powerful tool for conditional regulation of yeast gene expression.
The magnetic field sensors enabling birds to extract orientational information from the Earth’s magnetic field have remained enigmatic. Our previously published results from homing pigeons have made us suggest that the iron containing sensory dendrites in the inner dermal lining of the upper beak are a candidate structure for such an avian magnetometer system. Here we show that similar structures occur in two species of migratory birds (garden warbler, Sylvia borin and European robin, Erithacus rubecula) and a non-migratory bird, the domestic chicken (Gallus gallus). In all these bird species, histological data have revealed dendrites of similar shape and size, all containing iron minerals within distinct subcellular compartments of nervous terminals of the median branch of the Nervus ophthalmicus. We also used microscopic X-ray absorption spectroscopy analyses to identify the involved iron minerals to be almost completely Fe III-oxides. Magnetite (Fe II/III) may also occur in these structures, but not as a major Fe constituent. Our data suggest that this complex dendritic system in the beak is a common feature of birds, and that it may form an essential sensory basis for the evolution of at least certain types of magnetic field guided behavior.
Experimental results are presented for 180 in silico designed octapeptide sequences and their stabilizing effects on the major histocompatibility class I molecule H-2Kb. Peptide sequence design was accomplished by a combination of an ant colony optimization algorithm with artificial neural network classifiers. Experimental tests yielded nine H-2Kb stabilizing and 171 nonstabilizing peptides. 28 among the nonstabilizing octapeptides contain canonical motif residues known to be favorable for MHC I stabilization. For characterization of the area covered by stabilizing and non-stabilizing octapeptides in sequence space, we visualized the distribution of 100,603 octapeptides using a self-organizing map. The experimental results present evidence that the canonical sequence motives of the SYFPEITHI database on their own are insufficient for predicting MHC I protein stabilization.
Linear-implicit versions of strong Taylor numerical schemes for finite dimensional Itô stochastic differential equations (SDEs) are shown to have the same order as the original scheme. The combined truncation and global discretization error of an gamma strong linear-implicit Taylor scheme with time-step delta applied to the N dimensional Itô-Galerkin SDE for a class of parabolic stochastic partial differential equation (SPDE) with a strongly monotone linear operator with eigenvalues lambda 1 <= lambda 2 <= ... in its drift term is then estimated by K(lambda N -½ + 1 + delta gamma) where the constant K depends on the initial value, bounds on the other coefficients in the SPDE and the length of the time interval under consideration.
AMS subject classifications: 35R60, 60H15, 65M15, 65U05.
Alternative education or teaching radicalism? New literature on Islamic education in Southeast Asia
(2009)
This review article focuses on three recent publications on Islamic education in Southeast Asia. While two are monographs on South Thailand and Myanmar/ Burma, one is a collection of essays on Indonesia, Malaysia, South Thailand, Cambodia, and the Southern Philippines. All works highlight local, regional and international educational networks, as well as their connections to the Indian subcontinent and the Middle East. Based chiefly on first-hand fieldwork, the works deliver an up-to-date and detailed picture of current discussions and developments regarding Islamic education in Southeast Asia. Key words Education ; Islam ; Southeast Asia ; Indonesia ; Malaysia ; Thailand ; Myanmar
Samples of freshly fallen snow were collected at the high alpine research station Jungfraujoch, Switzerland, during the Cloud and Aerosol Characterization Experiments (CLACE) 5 in February and March 2006. Sampling was carried out on the Sphinx platform. Headspace-solid-phase-dynamic extraction (HS-SPDE) combined with gas chromatography/mass spectrometry (GC/MS) was used to quantify C6–C10 n-aldehydes in the snow samples. The most abundant n-aldehyde was n-hexanal (median concentration 1.324 micro g L -1) followed by n-nonanal, n-decanal, n-octanal and n-heptanal (median concentrations 1.239, 0.863, 0.460, and 0.304 micro g L -1, respectively). A wide range of concentrations was found among individual snow samples, even for samples taken at the same time. Higher median concentrations of all n-aldehydes were observed when air masses reached Jungfraujoch from the north-northwest in comparison to air masses arriving from the southeast-southwest. Results suggest that the n-aldehydes detected most likely are of direct and indirect biogenic origin, and that they entered the snow through the particle phase.
Both, gas and particle scavenging contribute to the transport of organic compounds by ice crystals in the troposphere. To simulate these processes an experimental setup was developed to form airborne ice crystals under atmospheric conditions. Experiments were performed in a wall independent reactor (WIR) installed in a walk-in cold chamber maintained constantly at -20°C. Aerosol particles were added to the carrier gas of ambient air by an aerosol generator to allow heterogeneous ice formation. Temperature variations and hydrodynamic conditions of the WIR were investigated to determine the conditions for ice crystal formation and crystal growth by vapour deposition. In detail, the dependence of temperature variations from flow rate and temperature of the physical wall as well as temperature variations with an increasing reactor depth were studied. The conditions to provide a stable aerosol concentration in the carrier gas flow were also studied. The temperature distribution inside the reactor was strongly dependent on flow rate and physical wall temperature. At an inlet temperature of -20°C, a flow rate of 30 L•min exp -1 and a physical wall temperature of +5°C turned out to provide ideal conditions for ice formation. At these conditions a sharp and stable laminar down draft "jet stream" of cold air in the centre of the reactor was produced. Temperatures measured at the chamber outlet were kept well below the freezing point in the whole reactor depth of 1.0 m. Thus, melting did not affect ice formation and crystal growth. The maximum residence time for airborne ice crystals was calculated to at 40 s. Ice crystal growth rates increased also with increasing reactor depth. The maximum ice crystal growth rate was calculated at 2.82 mg• exp -1. Further, the removal efficiency of the cleaning device for aerosol particles was 99.8% after 10 min. A reliable particle supply was attained after a preliminary lead time of 15 min. Thus, the minimum lead time was determined at 25 min. Several test runs revealed that the WIR is suitable to perform experiments with airborne ice crystals.