@book{OPUS4-7110, title = {Isaac Euchel}, series = {Aufkl{\"a}rung und Moderne}, journal = {Aufkl{\"a}rung und Moderne}, number = {15}, editor = {Aptroot, Marion and Kennecke, Andreas and Schulte, Christoph}, publisher = {Wehrhahn}, address = {Hannover}, isbn = {978-3-86525-215-9}, publisher = {Universit{\"a}t Potsdam}, pages = {380}, year = {2010}, abstract = {Isaac Euchel (1756-1804) war lange Zeit einer der zu Unrecht vergessenen j{\"u}dischen Aufkl{\"a}rer. Das hat sich erst seit wenigen Jahren ge{\"a}ndert: Seine bedeutende Rolle innerhalb der Haskala, der j{\"u}dischen Aufkl{\"a}rungsbewegung, wurde in der Forschung erkannt, seine wichtigen Schriften in hebr{\"a}ischer und jiddischer Sprache wiederentdeckt, {\"u}bersetzt und ediert. Euchel war ein vielseitiger Aufkl{\"a}rer: Er war Verleger und Kaufmann, Autor, Herausgeber und {\"U}bersetzer, schrieb in Deutsch, Hebr{\"a}isch und Jiddisch; er war zugleich in der j{\"u}dischen und in der christlichen Gesellschaft zu Hause, war Student Kants und Biograph Mendelssohns. In K{\"o}nigsberg und Berlin wurde er zum Organisator und Vernetzer der {\"u}ber halb Europa verstreuten Anh{\"a}nger der Haskala, die nach seiner Vorstellung durch die Erneuerung der hebr{\"a}ischen Sprache eine aufgekl{\"a}rte und moderne j{\"u}dische Kultur hervorbringen sollte. Anl{\"a}sslich seines 250. Geburtstags trafen sich Historiker, Hebraisten, Jiddisten, Judaisten und Literaturwissenschaftler aus Deutschland, {\"O}sterreich, Israel und den USA in Potsdam, um auf einer internationalen Tagung unter dem Titel »Vom Nutzen der Aufkl{\"a}rung oder: Woß tut me damit« sein Leben und Werk zu ehren und umfassend zu diskutieren. Der vorliegende Tagungsband b{\"u}ndelt die Fr{\"u}chte dieser Diskussionen und bietet einen {\"U}berblick {\"u}ber den Stand der Forschung.}, subject = {Euchel, Isaac Abraham}, language = {de} } @book{Homolka2010, author = {Homolka, Walter}, title = {Jesus von Nazareth : im Spiegel j{\"u}discher Forschung}, series = {J{\"u}dische Miniaturen}, volume = {85}, journal = {J{\"u}dische Miniaturen}, publisher = {Hentrich \& Hentrich}, address = {Berlin}, isbn = {978-3-942271-01-1}, pages = {135 S.}, year = {2010}, abstract = {Jesu Wahrnehmung im Judentum war vielgestaltig. Rabbiner Walter Homolka zeichnet eine Geschichte von Abgrenzung und Auseinandersetzung. Im 19. Jahrhundert fuehrte die "Heimholung Jesu" ins Judentum zu einer heute selbstbewussten Position. War Jesus aus juedischer Sicht Pharisaeer und Schriftgelehrter? Vielleicht. War er bedeutend? Ohne Zweifel. War er der Messias oder gar Gottes eigener Sohn? Nach juedischem Verstaendnis nein. Homolkas Buch laedt dazu ein, die zentrale Gestalt des Christentums aus der Perspektive des juedischen Glaubens zu betrachten. Besonders interessant sind die von Homolka aufgezeigten vielfaeltigen Versuche juedischer Wissenschaftler, die Lehre Jesu als "integralen Bestandteil der juedischen Tradition und Geschichte zu begreifen"; Versuche, die auch das christliche Jesus-Bild bereichern koennen - auch wenn juedisches und christliches Jesus-Bild letztlich doch auf entscheidende Weise different bleiben. (ORF Buchtipp)}, language = {de} } @book{HomolkaHafnerKosmanetal.2010, author = {Homolka, Walter and Hafner, Johann Evangelist and Kosman, Admiʾel and Karakoyun, Ercan}, title = {Muslime zwischen Tradition und Moderne : die G{\"u}len-Bewegung als Br{\"u}cke zwischen den Kulturen}, publisher = {Herder}, address = {Freiburg im Breisgau}, isbn = {978-3-451-30380-7}, pages = {240 S.}, year = {2010}, language = {de} } @article{CaliendoFossenKritikos2010, author = {Caliendo, Marco and Fossen, Frank and Kritikos, Alexander}, title = {The impact of risk attitudes on entrepreneurial survival}, issn = {0167-2681}, doi = {10.1016/j.jebo.2010.02.012}, year = {2010}, abstract = {Risk attitudes influence the complete life cycle of entrepreneurs. Whereas recent research underpins the theoretical proposition of a positive correlation between risk attitudes and the decision to become self-employed, the effects on survival are not as straightforward. Psychological research posits an inverse U-shaped relationship between risk attitudes and entrepreneurial survival. On the basis of experimentally validated data of the German Socio-Economic Panel (SOEP), we examine the extent to which risk attitudes influence survival rates in self-employment in Germany. The empirical results confirm that persons whose risk attitudes are in the medium range survive significantly longer as entrepreneurs than do persons with particularly low or high risk attitudes.}, language = {en} } @article{HeisterBartelsHeideetal.2010, author = {Heister, Julian and Bartels, Luise and Heide, Judith and W{\"u}rzner, Kay-Michael}, title = {Analysemethode und Datengrundlage k{\"o}nnen die Ergebnisse beeinflussen : selektiver Einfluss der Stammfrequenzen f{\"u}r ver-pr{\"a}figierte Verben}, year = {2010}, language = {de} } @article{TrauthMaslinDeinoetal.2010, author = {Trauth, Martin H. and Maslin, Mark A. and Deino, Alan L. and Junginger, Annett and Lesoloyia, Moses and Odada, Eric O. and Olago, Daniel O. and Olaka, Lydia A. and Strecker, Manfred and Tiedemann, Ralph}, title = {Human evolution in a variable environment : the amplifier lakes of Eastern Africa}, issn = {0277-3791}, doi = {10.1016/j.quascirev.2010.07.007}, year = {2010}, abstract = {The development of rise Cenozoic East African Rift System (EARS) profoundly re-shaped the landscape and significantly increased the amplitude of short-term environmental response to climate variation. In particular, the development of amplifier lakes in rift basins after three million years ago significantly contributed to this exceptional sensitivity of East Africa to climate change compared to elsewhere on the African continent. Amplifier lakes are characterized by tectonically-formed graben morphologies in combination with an extreme contrast between high precipitation in the elevated parts of the catchment and high evaporation in the lake area. Such amplifier lakes respond rapidly to moderate, precessional-forced climate shifts, and as they do so apply dramatic environmental pressure to the biosphere. Rift basins, when either extremely dry or lake-filled, form important barriers for migration, mixing and competition of different populations of animals and hominins. Amplifier lakes link long-term, high-amplitude tectonic processes and short-term environmental fluctuations. East Africa may have become the place where early humans evolved as a consequence of this strong link between different time scales. (C) 2010 Elsevier Ltd. All rights reserved.}, language = {en} } @article{WichuraBousquetOberhaenslietal.2010, author = {Wichura, Henry and Bousquet, Romain and Oberh{\"a}nsli, Roland and Strecker, Manfred and Trauth, Martin H.}, title = {Evidence for middleUocene uplift of the East African Plateau}, issn = {0091-7613}, doi = {10.1130/G31022.1}, year = {2010}, abstract = {Cenozoic uplift of the East African Plateau has been associated with fundamental climatic and environmental changes in East Africa and adjacent regions. While this influence is widely accepted, the timing and the magnitude of plateau uplift have remained unclear. This uncertainty stems from the lack of datable, geomorphically meaningful reference horizons that could record surface uplift. Here, we document the existence of significant relief along the East African Plateau prior to rifting, as inferred from modeling the emplacement history of one of the longest terrestrial lava flows, the similar to 300-km-long Yatta phonolite flow in Kenya. This 13.5 Ma lava flow originated on the present-day eastern Kenya Rift flank, and utilized a riverbed that once routed runoff from the eastern rim of the plateau. Combining an empirical viscosity model with subsequent cooling and using the Yatta lava flow geometry and underlying paleotopography (slope angle), we found that the prerift slope was at least 0.2 degrees, suggesting that the lava flow originated at a minimum elevation of 1400 m. Hence, high paleotopography in the Kenya Rift region must have existed by at least 13.5 Ma. We infer from this that middle Miocene uplift occurred, which coincides with the two-step expansion of grasslands, as well as important radiation and speciation events in tropical Africa.}, language = {en} } @article{HintersbergerThiedeStreckeretal.2010, author = {Hintersberger, Esther and Thiede, Rasmus Christoph and Strecker, Manfred and Hacker, Bradley R.}, title = {East-west extension in the NW Indian Himalaya}, issn = {0016-7606}, doi = {10.1130/B26589.1}, year = {2010}, abstract = {Explaining the presence of normal faults in overall compressive settings is a challenging problem in understanding the tectonics of active mountain belts. The Himalayan-Tibetan orogenic system is an excellent setting to approach this problem because it preserves one of the most dramatic records of long-term, contemporaneous shortening and extension. Over the past decades, several studies have described extensional features, not only in the Tibetan Plateau, but also in the Himalaya. For a long time, the favored model explained the function of the Southern Tibetan detachment system, a major fault zone in the Himalaya, as a decoupling horizon between the regime of crustal shortening forming the Himalayan wedge to the south and the extensional regime of the Tibetan Plateau to the north. However, in recent years, increasing evidence has shown that N-S-trending normal faults in the Central Himalaya crosscut not only the Southern Tibetan detachment system, but also the Main Central thrust. Here, we present new structural data and geologic evidence collected within the NW Indian Himalaya and combine them with previously published seismicity data sets in order to document pervasive E-W extension accommodated along N-S-trending faults extending as far south as the footwall of the Main Central thrust. We conducted a kinematic analysis of fault striations on brittle faults, documented and mapped fault scarps in Quaternary sedimentary deposits using satellite imagery, and made field observations in the Greater Sutlej region (Spiti, Lahul, Kinnaur) and the Garhwal Himalaya. Studies of extensional features within the regionally NW- SE-trending NW Indian Himalaya provide the advantage that arc-parallel and E-W extension can be separated, in contrast to the Central Himalaya. Therefore, our observations of E-W extension in the Indian NW Himalaya are well suited to test the applicability of current tectonic models for the whole Himalaya. We favor the interpretation of E-W extension in the NW Indian Himalaya as a propagation of extension driven by collapse of the Tibetan Plateau.}, language = {en} } @article{ToeroekBergerKliem2010, author = {T{\"o}r{\"o}k, Tibor and Berger, Mitch A. and Kliem, Bernhard}, title = {The writhe of helical structures in the solar corona}, issn = {0004-6361}, doi = {10.1051/0004-6361/200913578}, year = {2010}, abstract = {Context. Helicity is a fundamental property of magnetic fields, conserved in ideal MHD. In flux rope geometry, it consists of twist and writhe helicity. Despite the common occurrence of helical structures in the solar atmosphere, little is known about how their shape relates to the writhe, which fraction of helicity is contained in writhe, and how much helicity is exchanged between twist and writhe when they erupt. Aims. Here we perform a quantitative investigation of these questions relevant for coronal flux ropes. Methods. The decomposition of the writhe of a curve into local and nonlocal components greatly facilitates its computation. We use it to study the relation between writhe and projected S shape of helical curves and to measure writhe and twist in numerical simulations of flux rope instabilities. The results are discussed with regard to filament eruptions and coronal mass ejections (CMEs). Results. (1) We demonstrate that the relation between writhe and projected S shape is not unique in principle, but that the ambiguity does not affect low- lying structures, thus supporting the established empirical rule which associates stable forward (reverse) S shaped structures low in the corona with positive (negative) helicity. (2) Kink-unstable erupting flux ropes are found to transform a far smaller fraction of their twist helicity into writhe helicity than often assumed. (3) Confined flux rope eruptions tend to show stronger writhe at low heights than ejective eruptions (CMEs). This argues against suggestions that the writhing facilitates the rise of the rope through the overlying field. (4) Erupting filaments which are S shaped already before the eruption and keep the sign of their axis writhe (which is expected if field of one chirality dominates the source volume of the eruption), must reverse their S shape in the course of the rise. Implications for the occurrence of the helical kink instability in such events are discussed. (5) The writhe of rising loops can easily be estimated from the angle of rotation about the direction of ascent, once the apex height exceeds the footpoint separation significantly. Conclusions. Writhe can straightforwardly be computed for numerical data and can often be estimated from observations. It is useful in interpreting S shaped coronal structures and in constraining models of eruptions.}, language = {en} } @article{ValoriKliemToeroeketal.2010, author = {Valori, Gherardo and Kliem, Bernhard and T{\"o}r{\"o}k, Tibor and Titov, Viacheslav S.}, title = {Testing magnetofrictional extrapolation with the Titov-Demoulin model of solar active regions}, issn = {0004-6361}, doi = {10.1051/0004-6361/201014416}, year = {2010}, abstract = {We examine the nonlinear magnetofrictional extrapolation scheme using the solar active region model by Titov and Demoulin as test field. This model consists of an arched, line-tied current channel held in force-free equilibrium by the potential field of a bipolar flux distribution in the bottom boundary. A modified version with a parabolic current density profile is employed here. We find that the equilibrium is reconstructed with very high accuracy in a representative range of parameter space, using only the vector field in the bottom boundary as input. Structural features formed in the interface between the flux rope and the surrounding arcade - "hyperbolic flux tube" and "bald patch separatrix surface" - are reliably reproduced, as are the flux rope twist and the energy and helicity of the configuration. This demonstrates that force-free fields containing these basic structural elements of solar active regions can be obtained by extrapolation. The influence of the chosen initial condition on the accuracy of reconstruction is also addressed, confirming that the initial field that best matches the external potential field of the model quite naturally leads to the best reconstruction. Extrapolating the magnetogram of a Titov-Demoulin equilibrium in the unstable range of parameter space yields a sequence of two opposing evolutionary phases, which clearly indicate the unstable nature of the configuration: a partial buildup of the flux rope with rising free energy is followed by destruction of the rope, losing most of the free energy.}, language = {en} } @article{CarrapaHauerSchoenbohmetal.2010, author = {Carrapa, Barbara and Hauer, Joern and Schoenbohm, Lindsay M. and Strecker, Manfred and Schmitt, Axel K. and Villanueva, Arturo and Gomez, Jos{\´e} Sosa}, title = {Dynamics of deformation and sedimentation in the northern Sierras Pampeanas : an integrated study of the Neogene Fiambal{\´a} basin, NW Argentina ; reply}, issn = {0016-7606}, doi = {10.1130/B30134.1}, year = {2010}, language = {en} } @article{FoxWakkerSmokeretal.2010, author = {Fox, Andrew J. and Wakker, Bart P. and Smoker, Jonathan V. and Richter, Philipp and Savage, Blair D. and Sembach, Kenneth R.}, title = {Exploring the origin and fate of the Magellanic stream with ultraviolet and optical absorption}, issn = {0004-637X}, doi = {10.1088/0004-637x/718/2/1046}, year = {2010}, abstract = {We present an analysis of ionization and metal enrichment in the Magellanic Stream (MS), the nearest gaseous tidal stream, using Hubble Space Telescope/STIS and FUSE ultraviolet spectroscopy of two background active galactic nuclei. The targets are NGC 7469, lying directly behind the MS with log N(H I)(MS) = 18.63 +/- 0.03(stat) +/- 0.08(syst), and Mrk 335, lying 24 degrees.7 away with log N(H I)(MS) = 16.67 +/- 0.05. For NGC 7469, we include optical spectroscopy from VLT/UVES. In both sight lines, the MS is detected in low-ion (O I, C II, C III, Si II, Si III, Al II, Ca II) and high-ion (O VI, C IV, Si IV) absorption. Toward NGC 7469, we measure an MS oxygen abundance [O/H](MS) = [O I/ H I]= -1.00 +/- 0.05(stat) +/- 0.08(syst), supporting the view that the Stream originates in the Small Magellanic Cloud rather than the Large Magellanic Cloud. We use CLOUDY to model the low-ion phase of the Stream as a photoionized plasma using the observed Si III/Si II and C III/C II ratios. Toward Mrk 335, this yields an ionization parameter between log U= -3.45 and -3.15, a gas density log (n(H)/cm(-3)) between-2.51 and -2.21, and a hydrogen ionization fraction of 98.9\%- 99.5\%. Toward NGC 7469, we derive sub-solar abundance ratios for [Si/O], [Fe/O], and [Al/O], indicating the presence of dust in the MS. The high-ion column densities are too large to be explained by photoionization, but also cannot be explained by a single-temperature collisional ionization model (equilibrium or non-equilibrium). This suggests that the high-ion plasma is multi-phase, with an Si IV region, a hotter O VI region, and C IV potentially contributing to each. Summing over the low-ion and high-ion phases, we derive conservative lower limits on the ratio N(total H II)/N(H I) of greater than or similar to 19 toward NGC 7469 and greater than or similar to 330 toward Mrk 335, showing that along these two directions the vast majority of the Stream has been ionized. The presence of warm-hot plasma together with the small-scale structure observed at 21 cm provides evidence for an evaporative interaction with the hot Galactic corona. This scenario, predicted by hydrodynamical simulations, suggests that the fate of the MS will be to replenish the Galactic corona with new plasma, rather than to bring neutral fuel to the disk.}, language = {en} } @article{EichlerGuettaPohl2010, author = {Eichler, David and Guetta, Dafne and Pohl, Martin}, title = {The high energy budget allocations in shocks and gamma ray bursts}, issn = {0004-637X}, doi = {10.1088/0004-637x/722/1/543}, year = {2010}, abstract = {The statistical distribution of energies among particles responsible for long gamma-ray burst (GRB) emission is analyzed in light of recent results of the Fermi Observatory. The all-sky flux, F., recorded by the Gamma-Ray Burst Monitor (GBM) is shown, despite its larger energy range, to be not significantly larger than that reported by the Burst and Transient Explorer, suggesting a relatively small flux in the 3-30MeV energy range. The present-day energy input rate in gamma-rays recorded by the GBM from long GRBs is found, assuming star formation rates in the literature, to be W(0) = 0.5F gamma H/c = 5x10(42) erg Mpc(-3) yr(-1). The Large Area Telescope fluence, when observed, is about 5\%-10\% per decade of the total, in good agreement with the predictions of saturated, nonlinear shock acceleration. The high- energy component of long GRBs, as measured by Fermi, is found to contain only similar to 10-2.5 of the energy needed to produce ultrahigh-energy cosmic rays (UHECRs) above 4 EeV, assuming the latter to be extragalactic, when various numerical factors are carefully included, if the cosmic-ray source spectrum has a spectral index of -2. The observed. - ray fraction of the required UHECR energy is even smaller if the source spectrum is softer than E-2. The AMANDA II limits rule out such a GRB origin for UHECRs if much more than 10(-2) of the cosmic-ray energy goes into neutrinos that are within, and simultaneous with, the gamma-ray beam. It is suggested that "orphan" neutrinos out of the gamma-ray beam might be identifiable via orphan afterglow or other wide angle signatures of GRBs in lieu of coincidence with prompt gamma-rays, and it is recommended that feasible single neutrino trigger criteria be established to search for such coincidences.}, language = {en} } @misc{Botsch2010, author = {Botsch, Gideon}, title = {Puschner, M., Antisemitismus im Kontext der politischen Romantik; T{\"u}bingen, Niemeyer, 2008}, issn = {0044-2828}, year = {2010}, language = {de} } @article{TomasZitzmannHomannetal.2010, author = {Tomas, Sara and Zitzmann, Max and Homann, Martin and Rumpf, Michael and Amour, Frederic and Benisek, Merle-Friederike and Betzler, Christian and Mutti, Maria}, title = {From ramp to platform : building a 3D model of depositional geometries and facies architectures in transitional carbonates in the Miocene, northern Sardinia}, issn = {0172-9179}, doi = {10.1007/s10347-009-0203-7}, year = {2010}, abstract = {The depositional geometry and facies distribution of an Early Miocene (Burdigalian) carbonate system in the Perfugas Basin (NW Sardinia) comprise a well-exposed example of a transition from a ramp to a steep-flanked platform. The carbonate succession (Sedini Limestone Unit) is composed of two depositional sequences separated by a major erosional unconformity. The lower (sequence 1) records a ramp dominated by heterozoan producers and the upper (sequence 2) is dominated by photozoan producers and displays a gradual steepening of the depositional profile into a steep- flanked platform. This paper shows the process of creating a digital outcrop model including a facies model. This process consists of combining field data sets, including 17 sedimentary logs, and a spatial dataset consisting of differential global positioning system data points measured along key stratigraphic surfaces and sedimentary logs, with the goal of locking traditional field observations into a 3D spatial model. Establishing a precise geometrical framework and visualizing the overall change in the platform geometry and the related vertical and lateral facies variations of the Sedini carbonate platform, allows us to better understand the sedimentary processes leading to the geometrical turn- over of the platform. Furthermore, a detailed facies modeling helps us to gain insight into the detailed depositional dynamics. The final model reproduces faithfully the depositional geometries observed in the outcrops and helps in understanding the relationships between facies and architectural framework at the basin scale. Moreover, it provides the basis to characterize semiquantitatively regional sedimentological features and to make further reservoir and subsurface analogue studies.}, language = {en} } @article{SiliverstovsOetschKemfertetal.2010, author = {Siliverstovs, Boriss and {\"O}tsch, Rainald and Kemfert, Claudia and Jaeger, Carlo and Haas, Armin and Kremers, Hans}, title = {Climate change and modelling of extreme temperatures in Switzerland}, issn = {1436-3240}, doi = {10.1007/s00477-009-0321-3}, year = {2010}, abstract = {This study models maximum temperatures in Switzerland monitored in twelve locations using the generalised extreme value (GEV) distribution. The parameters of the GEV distribution are determined within a Bayesian framework. We find that the parameters of the underlying distribution underwent a substantial change in the beginning of the 1980s. This change is characterised by an increase both in the level and the variability. We assess the likelihood of the heat wave of the summer 2003 using the fitted GEV distribution by accounting for the presence of a structural break. The estimation results do suggest that the heat wave of 2003 is not that statistically improbable if an appropriate methodology is used for dealing with nonstationarity.}, language = {en} } @article{WilkeO'BrienGerdesetal.2010, author = {Wilke, Franziska Daniela Helena and O'Brien, Patrick J. and Gerdes, Axel and Timmerman, Martin Jan and Sudo, Masafumi and Khan, M. Ahmed}, title = {The multistage exhumation history of the Kaghan Valley UHP series, NW Himalaya, Pakistan from U-Pb and Ar-40/Ar- 39 ages}, issn = {0935-1221}, doi = {10.1127/0935-1221/2010/0022-2051}, year = {2010}, abstract = {Amphibole and mica Ar-40/Ar-39 ages as well as zircon, rutile and titanite U-Pb geochronology of eclogites and associated host rocks from the Higher Himalayan Crystalline Nappes (Indian Plate) in the Upper Kaghan Valley, Pakistan allow distinction of a multistage exhumation history. An Eocene age for peak-pressure metamorphism has been obtained by phengite Ar-40/Ar-39 (47.3 +/- 0.3 Ma) and zircon U-Pb (47.3 +/- 0.4 and 47.4 +/- 0.3 Ma) ages from cover and basement gneisses. A very short-lived metamorphic peak and rapid cooling is documented by an amphibole Ar-40/Ar-39 age of 46.6 +/- 0.5 Ma and a rutile U-Pb age of 44.1 +/- 1.3 Ma from eclogites. Phengite and biotite ages from cover and basement sequences metamorphosed during the Himalayan orogeny are 34.5 +/- 0.2 to 28.1 +/- 0.2 Ma whereas youngest biotites, yielding 23.6 +/- 0.1 and 21.7 +/- 0.2 Ma, probably reflect argon partial resetting. The amphibole age, together with those derived from phengite and zircon demonstrate a rate of initial exhumation of 86-143 mm/a i.e. an extremely rapid transport of the Indian Plate continental crust from ultra-high pressure (UHP) conditions back to crustal levels (47-46 Ma for transport from 140 to 40 km depth). Subsequent exhumation (46-41 Ma, 40-35 km) slowed to about 1 mm/a at the base of the continental crust but increased again later towards slightly higher exhumation rates of ca. 2 mm/a (41-34 Ma, 35- 20 km). This indicates a change from buoyancy-driven exhumation at mantle depths to compression forces related to continent-continent collision and accompanied crustal folding, thrusting and stacking that finally exposed the former deeply-buried rocks.}, language = {en} } @article{VasquezAltenbergerRomeretal.2010, author = {Vasquez, M{\´o}nica and Altenberger, Uwe and Romer, Rolf L. and Sudo, Masafumi and Moreno-Murillo, Juan Manuel}, title = {Magmatic evolution of the Andean Eastern Cordillera of Colombia during the Cretaceous : Influence of previous tectonic processes}, issn = {0895-9811}, doi = {10.1016/j.jsames.2009.02.003}, year = {2010}, abstract = {The Eastern Cordillera of the Colombian Andes represents an inverted Cretaceous basin where Cretaceous magmatism is characterized by rare mafic dykes and sills. We use Ar-40/Ar-39, Sr-Nd-Pb isotopes, as well as major and trace elements analyses of Cretaceous intrusions from both flanks of the Eastern Cordillera in combination with structural data to document the complex evolution of the basin. Magmatism, which is diachronous and geochemically diverse, seems to be related to mantle melting beneath the most subsiding segments of each sub-basin during enhanced extensional tectonics. The mafic intrusions display two different compositional series: an alkaline one with OIB-like pattern and a tholeiitic one with MORB-like features. This indicates at least two diverse mantle sources. Trace-element patterns suggest that the intrusions were emplaced in an extensional setting. Ar-40/Ar-39 dating on primary plagioclase and hornblende provides plateau ages between similar to 136 and similar to 74 Ma. The geochemical and temporal diversities show that the emplacement of the magmas was tectonically controlled, each sub-basin reflecting an individual subsidence event.}, language = {en} } @article{SobelSeward2010, author = {Sobel, Edward and Seward, Diane}, title = {Influence of etching conditions on apatite fission-track etch pit diameter}, issn = {0009-2541}, doi = {10.1016/j.chemgeo.2009.12.012}, year = {2010}, abstract = {The temperature range of the apatite fission-track partial annealing zone (PAZ) varies as a function of the kinetic characteristics of the apatite crystal as well as the cooling rate. These kinetic characteristics are controlled largely by the chemical composition of the apatites; fission-track etch pit diameter (D-par) has been shown to be a proxy for quantifying these characteristics. Since some annealing models explicitly use D-par as a kinetic indicator, the question of whether D-par varies according to either operator variability or etching conditions has serious implications. The influence of etching conditions includes both minor variations in temperature and etch time as well as larger variations between the three popular concentrations of nitric acid that are presently in use within the fission- track community: 5 and 5.5 M HNO3 at 21 degrees C for 20 s, and 1.6 M (7 vol.\%) HNO3 at 21 degrees C for 45 or 50 s. We have conducted a systematic study of D-par in two widely used apatite age standards: Durango and Fish Canyon Tuff (FCT). Samples were analyzed by at least 2 operators in 2 laboratories; over 15,000 etch pits were measured. Operator imprecision is small compared to other effects both within and between operators. The measured D-par parameters depend primarily on etching conditions including concentration of etchant, and the time and temperature of etching. D-par size increases linearly with time but non-linearly with temperature. Differences between D-par size of Durango and FCT are significantly smaller for the 1.6 M etch compared to the other two etches, implying that the weak etch has less resolving power for D-par measurements. In addition, when etching conditions are changed, confined track lengths for different apatite compositions and D-par values co-vary in a complex fashion. Therefore, the 5 or 5.5 M etch is recommended for studies that employ D-par as a proxy for chemistry; the 1.6 M etch and other weak etches are not recommended. We propose a linear correction for D-par based on measuring D-par in two widely available AFT age standards, Durango and FCT, and cross-plotting the results with those obtained by R. Donelick. The slope of the resulting curve, which passes through the origin, provides a correction factor. This system yields reasonably good corrected values for 3 test samples using the 5 M and 5.5 M HNO3 etches.}, language = {en} } @article{SobelSeward2010, author = {Sobel, Edward and Seward, Diane}, title = {Erratum to "Influence of etching conditions on apatite fission-track etch pit diameter by E.R. Sobel and D. Seward" [Chem. Geol. 271 (2010) 59-69]}, issn = {0009-2541}, doi = {10.1016/j.chemgeo.2010.08.005}, year = {2010}, language = {en} } @article{FilimonKopfBalloutetal.2010, author = {Filimon, Marlena and Kopf, Ilona and Ballout, Fuad and Schmidt, Dietrich A. and Bruendermann, Erik and R{\"u}he, J{\"u}rgen and Santer, Svetlana and Havenith, Martina}, title = {Smart polymer surfaces : mapping chemical landscapes on the nanometre scale}, issn = {1744-683X}, doi = {10.1039/C0sm00098a}, year = {2010}, abstract = {We show that Scattering Infrared Near-field Microscopy (SNIM) allows chemical mapping of polymer monolayers that can serve as designed nanostructured surfaces with specific surface chemistry properties on a nm scale. Using s- SNIM a minimum volume of 100 nm x 100 nm x 15 nm is sufficient for a recording of a "chemical'' IR signature which corresponds to an enhancement of at least four orders of magnitudes compared to conventional FT-IR microscopy. We could prove that even in cases where it is essentially difficult to distinguish between distinct polymer compositions based solely on topography, nanophase separated polymers can be clearly distinguished according to their characteristic near-field IR response.}, language = {en} } @article{ChinagliaGregorioStefanelloetal.2010, author = {Chinaglia, Dante Luis and Gregorio, Rinaldo and Stefanello, Josiani Cristina and Altafim, Ruy Alberto Pisani and Wirges, Werner and Wang, Feipeng and Gerhard, Reimund}, title = {Influence of the solvent evaporation rate on the crystalline phases of solution-cast poly(vinylidene fluoride) films}, issn = {0021-8995}, doi = {10.1002/App.31488}, year = {2010}, abstract = {The influence of the solvent-evaporation rate on the formation of of. and P crystalline phases in solution-cast poly(vinylidene fluoride) (PVDF) films was systematically investigated. Films were crystallized from PVDF/N,N- dimethylformamide solutions with concentrations of 2.5, 5.0, 10, and 20 wt \% at different temperatures. During crystallization, the solvent evaporation rate was monitored in situ by means of a semianalytic balance. With this system, it was possible to determine the evaporation rate for different concentrations and temperatures of the solution under specific ambient conditions (pressure, temperature, and humidity). Fourier-Transform InfraRed spectroscopy with Attenuated Total Reflectance revealed the P-phase content in the PVDF films and its dependence on previous evaporation rates. Based on the relation between the evaporation rate and the PVDF phase composition, a consistent explanation for the different amounts of P phase observed at the upper and lower sample surfaces is achieved. Furthermore, the role of the sample thickness has also been studied. The experimental results show that not only the temperature but also the evaporation rate have to be controlled to obtain the desired crystalline phases in solution-cast PVDF films.}, language = {en} } @article{FloresSuarezGanesanWirgesetal.2010, author = {Flores Su{\´a}rez, Rosaura and Ganesan, Lakshmi Meena and Wirges, Werner and Gerhard, Reimund and Mellinger, Axel}, title = {Imaging liquid crystals dispersed in a ferroelectric polymer matrix by means of thermal-pulse tomography}, issn = {1070-9878}, doi = {10.1109/TDEI.2010.5539683}, year = {2010}, abstract = {A new arrangement of the optical elements in a Thermal-Pulse-Tomography (TPT) setup allows to scan micrometer structures in composite and heterogeneous samples such as polymer-dispersed liquid crystals (PDLCs). The non-destructive TPT technique allows the determination of three-dimensional profiles of polarization and space charge in dielectrics. The samples under study were 12 mu m thick films of a copolymer of vinylidene fluoride with trifluoroethylene P(VDF- TrFE) (65/35) with embedded liquid-crystal droplets. The poling process was performed in direct contact well above the coercive field of the copolymer. The 3D map obtained from scanning with a 10 mu m wide spot shows elliptically shaped areas with liquid-crystal droplets. Considering the droplets as oblate spheroids, their major axis lies in the x-y plane, while their minor axis in the z direction measures 0.5 mu m or more. This result is in good agreement with scanning electron micrographs. It is believed that the major axis is overestimated due to imaging of liquid-crystal clusters.}, language = {en} } @article{GrecoWangWegener2010, author = {Greco, Tonino and Wang, Feipeng and Wegener, Michael}, title = {Multifunctional silver poly(vinylidene fluoride) nanocomposites : nanoparticle synthesis, film processing, and structural characterization}, issn = {0015-0193}, doi = {10.1080/00150193.2010.482896}, year = {2010}, abstract = {Scope of this work was the synthesis of homogeneously dispersed silver nanoparticles in the ferroelectric polymer poly(vinylidene fluoride) (PVDF) and the study of the resulting properties affecting both the electro-active matrix and the optically-active nanofiller. In the nanocomposites surface plasmon resonances can be tuned across the UV- vis to the NIR spectral range. From IR spectra and DSC measurements it is concluded that the - to -phase transformation is observed and no degradation of the polymer matrix occurs. Finally, electrical poling was performed in order to investigate the influence of the embedded silver particles on the polarization behavior of the ferroelectric polymer.}, language = {en} } @article{FangQiuWirgesetal.2010, author = {Fang, Peng and Qiu, Xunlin and Wirges, Werner and Gerhard, Reimund and Zirkel, Larissa}, title = {Polyethylene-naphthalate (PEN) ferroelectrets : cellular structure, piezoelectricity and thermal stability}, issn = {1070-9878}, doi = {10.1109/TDEI.2010.5539678}, year = {2010}, abstract = {Cellular polyethylene-naphthalate (PEN) ferroelectrets are useful as soft and flexible electromechanical transducer materials. Improved cellular PEN foams are prepared by means of a "voiding + inflation + stretching" process and investigated with respect to their structure and their applications-relevant properties. It is found that most of the cellular voids have heights below 8 mu m. The polymer walls do not allow sufficient gas exchange between the voids and the ambient atmosphere, when the cellular films are exposed to atmospheric pressures between a millibar and a few bars. As expected for ferroelectrets, a threshold voltage for charging is observed: A reasonable piezoelectric coefficient d(33) is only found when the charging voltage is higher than 4 kV. Furthermore, d(33) increases with charging voltage and reaches saturation at approximately 8 kV. Annealing after charging or charging at elevated temperatures may enhance the thermal stability of the PEN ferroelectrets. The d(33) of properly annealed samples is stable up to the respective annealing temperatures, but the annealing process reduces the piezoelectric activity of charged ferroelectret films to some extent. Samples charged at suitable elevated temperatures show much better thermal stability than those charged at room temperature, but the charging temperature should be limited to values below the material's glass-transition temperature T-g. Furthermore, the relevant elastic modulus c(33) of PEN ferroelectrets may decrease upon thermal treatment.}, language = {en} } @article{XieJelicicWangetal.2010, author = {Xie, Zai-Lai and Jelicic, Aleksandra and Wang, Feipeng and Rabu, Pierre and Friedrich, Alwin and Beuermann, Sabine and Taubert, Andreas}, title = {Transparent, flexible, and paramagnetic ionogels based on PMMA and the iron-based ionic liquid 1-butyl-3- methylimidazolium tetrachloroferrate(III) [Bmim][FeCl4]}, issn = {0959-9428}, doi = {10.1039/C0jm01733g}, year = {2010}, abstract = {The iron-containing ionic liquid (IL) 1-butyl-3-methylimidazolium tetrachloroferrate(III) [Bmim][FeCl4] has been used as a building block in the synthesis of transparent, ion-conducting, and paramagnetic ionogels. UV/Vis spectroscopy shows that the coordination around the Fe(III) ion does slightly change upon incorporation of the IL into PMMA. The thermal stability of the PMMA increases significantly with IL incorporation. In particular, the onset weight loss observed at ca. 265 degrees C for pure PMMA is completely suppressed. The ionic conductivity shows a strong temperature dependence and increases with increasing IL weight fractions. The magnetic properties are similar to those reported for the pure IL and are not affected by the incorporation into the PMMA matrix. The resulting ionogel is thus an interesting prototype for soft, flexible, and transparent materials combining the mechanical properties of the matrix with the functionality of the metal-containing IL, such as magnetism.}, language = {en} } @article{DaskalowBoisguerinJandrigetal.2010, author = {Daskalow, Katjana and Boisguerin, Prisca and Jandrig, Burkhard and van Landeghem, Frank K. H. and Volkmer, Rudolf and Micheel, Burkhard and Schenk, J{\"o}rg A.}, title = {Generation of an antibody against the protein phosphatase 1 inhibitor KEPI and characterization of the epitope}, issn = {0250-7005}, year = {2010}, abstract = {A monoclonal antibody against the potential tumor suppressor kinase-enhanced protein phosphatase 1 (PP1) inhibitor KEPI (PPP1R14C) was generated and characterized. Human KEPI was expressed in Escherichia coli and used to immunize Balb/c mice. Using hybridoma technology, one clone, G18AF8, was isolated producing antibodies which bound specifically to the KEPI protein in ELISA, immunoblotting and flow cytometry. The antibody was also successfully applied to stain KEPI protein in paraffin sections of human brain. The epitope was mapped using peptide array technology and confirmed as GARVFFQSPR. This corresponds to the N-terminal region of KEPI. Amino acid substitution analysis revealed that two residues, F and Q, are essential for binding. Affinity of binding was determined by competitive ELISA as 1 mu M. In Western blot assays testing G18AF8 antibody on brain samples of several species, reactivity with hamster, rat and chicken samples was found, suggesting a broad homology of this KEPI epitope in vertebrates. This antibody could be used in expression studies at the protein level e.g. in tumor tissues.}, language = {en} } @article{WartenburgerKuehnSassenbergetal.2010, author = {Wartenburger, Isabell and K{\"u}hn, Esther and Sassenberg, Uta and Foth, Manja and Franz, Elisabeth A. and van der Meer, Elke}, title = {On the relationship between fluid intelligence, gesture production, and brain structure}, issn = {0160-2896}, doi = {10.1016/j.intell.2009.11.001}, year = {2010}, abstract = {Individuals scoring high in fluid intelligence tasks generally perform very efficiently in problem solving tasks and analogical reasoning tasks presumably because they are able to select the task-relevant information very quickly and focus on a limited set of task-relevant cognitive operations. Moreover, individuals with high fluid intelligence produce more representational hand and arm gestures when describing a geometric analogy task than individuals with average fluid intelligence. No study has yet addressed the relationship between intelligence, gesture production, and brain structure, to our knowledge. That was the purpose of our study. To characterize the relation between intelligence, gesture production, and brain structure we assessed the frequency of representational gestures and cortical thickness values in a group of adolescents differing in fluid intelligence. Individuals scoring high in fluid intelligence showed higher accuracy in the geometric analogy task and produced more representational gestures (in particular more movement gestures) when explaining how they solved the task and showed larger cortical thickness values in some regions in the left hemisphere (namely the pars opercularis, superior frontal, and temporal cortex) than individuals with average fluid intelligence. Moreover, the left pars opercularis (a part of Broca's area) and left transverse temporal cortex showed larger cortical thickness values in participants who produced representational and in particular movement gestures compared to those who did not. Our results thus indicate that cortical thickness of those brain regions is related to both high fluid intelligence and the production of gestures. Results are discussed in the gestures-as-simulated-action framework that states that gestures result from simulated perception and simulated action that underlie embodied language and mental imagery.}, language = {en} } @article{vanderMeerBeyerHornetal.2010, author = {van der Meer, Elke and Beyer, Reinhard and Horn, Judith and Foth, Manja and Bornemann, Boris and Ries, Jan and Kramer, J{\"u}rg and Warmuth, Elke and Heekeren, Hauke R. and Wartenburger, Isabell}, title = {Resource allocation and fluid intelligence ; insights from pupillometry}, issn = {0048-5772}, year = {2010}, language = {en} } @article{Wartenburger2010, author = {Wartenburger, Isabell}, title = {Gehirn und Sprache : wie wir Sprache(n) erlernen und verarbeiten}, isbn = {978-3-8340-0654-7}, year = {2010}, language = {de} } @article{SellrieBeckHildebrandtetal.2010, author = {Sellrie, Frank and Beck, Michael and Hildebrandt, Niko and Micheel, Burkhard}, title = {A homogeneous time-resolved fluoroimmunoassay (TR-FIA) using antibody mediated luminescence quenching}, issn = {1759-9660}, doi = {10.1039/C0ay00306a}, year = {2010}, abstract = {The determination of low-molecular weight substances (haptens) is demonstrated with a homogeneous time-resolved immunoassay using antibody-induced luminescence quenching. Our novel assay technology uses the newly developed monoclonal antibody (G24-BA9) to quench the luminescence of europium trisbipyridine (EuTBP). We performed a competitive biotin immunoassay including an EuTBP-biotin conjugate, the anti-EuTBP antibody G24-BA9 and streptavidin as assay components. Steric hindrance allows only the binding of either G24-BA9 (to the EuTBP moiety) or streptavidin (to the biotin moiety) to the EuTBP-biotin conjugate. Addition of the analyte biotin resulted in the binding of streptavidin to biotin and a concomitant preferred binding of G24-BA9 to EuTBP-biotin. Since G24-BA9 quenches the luminescence of EuTBP within the conjugate, the luminescence signal could be used to indicate and quantify the presence of free biotin in the system. All experiments were carried out in solution in the presence of 5\% serum demonstrating the possibility of using our novel assay for a very fast determination of low molecular weight substances in biological fluids.}, language = {en} } @article{SchmidtHennkeKnocheletal.2010, author = {Schmidt, Marco and Hennke, Thomas and Knochel, Mira and Kurten, Achim and Hierholzer, Johannes and Daniel, Peter and Bittmann, Frank}, title = {Can chronic irritations of the trigeminal nerve cause musculoskeletal disorders?}, issn = {1021-7096}, doi = {10.1159/000315338}, year = {2010}, abstract = {In this article, five cases of odontogenous dysfunctions and musculoskeletal complaints are presented. A common finding in all patients of this study was that the presence of joint complaints was related to deficits in the corresponding muscular function. These deficits were determined by manual muscle tests as described by Kendall et al. [Muscles - Testing and Function, ed 4. Baltimore, Williams and Wilkins, 1993] and were eliminated immediately by a neural therapeutic test injection into the disturbed dental region. The therapy provided solely aimed to eliminate the odontogenous dysfunction. No other therapeutic measures were carried out with regard to the patients' respective muscle, tendon, or joint complaints.}, language = {en} } @article{CacaceKaiserLewerenzetal.2010, author = {Cacace, Mauro and Kaiser, Bjoern Onno and Lewerenz, Bjoern and Scheck-Wenderoth, Magdalena}, title = {Geothermal energy in sedimentary basins : what we can learn from regional numerical models}, issn = {0009-2819}, doi = {10.1016/j.chemer.2010.05.017}, year = {2010}, abstract = {Understanding the interactions between the different processes that control the geothermal and fluid flow fields in sedimentary basins is crucial for exploitation of geothermal energy. Numerical models provide predictive and feasible information for a correct assessment of geothermal resources especially in areas where data acquisition is demanding. Here, we present results from numerical efforts to characterize the thermal structure and its interaction with the fluid system for the area of the North East German Basin (NEGB). The relative impact of the different (diffusive and advective) processes affecting the hydrothermal setting of the basin are investigated by means of three- dimensional numerical simulations. Lithospheric-scale numerical models are evaluated to understand the specific thermal signature of the relevant factors influencing the present-day conductive geothermal field in the NEGB. Shallow and deep structural controls on the thermal configuration of the basin are addressed and quantified. Interaction between the resulting thermal field and the active fluid system is investigated by means of three-dimensional simulations of coupled fluid flow and heat transport. Factors influencing stability and reliability of modeling predictions are discussed. The main effort is to build a physically consistent model for the basin which integrates the impacts of thermal gradients on the regional fluid regime and their coupling with the main geological units defining the basin.}, language = {en} } @article{BloecherCacaceLewerenzetal.2010, author = {Bloecher, Mando Guido and Cacace, Mauro and Lewerenz, Bjoern and Zimmermann, G{\"u}nter}, title = {Three dimensional modelling of fractured and faulted reservoirs : framework and implementation}, issn = {0009-2819}, doi = {10.1016/j.chemer.2010.05.014}, year = {2010}, abstract = {Modelling of coupled physical processes in fractured and faulted media is a major challenge for the geoscience community. Due to the complexity related to the geometry of real fracture networks and fault systems, modelling studies have been mainly restricted either to two dimensional cases or to simplified orthogonal fracture systems consisting of vertical and horizontal fractures. An approach to generate three dimensional meshes for realistic fault geometries is presented. The method enables representation of faults in an arbitrary incline as two dimensional planes within a three dimensional, stratified porous matrix of a generic geometry. Based on a structural geological model, the method creates three dimensional unstructured tetrahedral meshes. These meshes can be used for finite element and finite volume numerical simulations. A simulation of a coupled fluid flow and heat transport problem for a two layered porous medium cut by two crossing faults is presented to test the reliability of the method.}, language = {en} }