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Cunninghamia publishes original research papers on all aspects of plant ecology with particular emphasis on the vegetation and flora of eastern Australia. Descriptive, experimental and historical studies of plant communities, populations, individuals, their interactions with other organisms and their management are acceptable. Cunninghamia is a fully open-access online scientific journal published on the Web by the National Herbarium of New South Wales, Royal Botanic Gardens & Domain Trust, Sydney.
Aerial photo interpretation of high resolution airborne imagery (ADS40) was used in a three-dimensional (3-D) digital Geographic Information System (GIS) environment to map native plant communities defined in the NSW Vegetation Classification and Assessment (NSW VCA) in central-southern New South Wales. NSW VCA plant community types form part of the NSW BioMetric vegetation type dataset underpinning NSW natural resource management (NRM) planning frameworks. This region was previously devoid of detailed vegetation mapping. In addition to developing a novel method for mapping plant communities, the use of ADS40 imagery allowed for capture of multiple attributes in each map polygon including attributes pertaining to dominant species and vegetation condition. Such data informs multi-attribute models used in conservation planning, providing utility beyond that of a singular plant community map.
A total of 546,150 hectares of native vegetation in 100 native plant communities was mapped across the study area (Coolamon, Cootamundra, Junee, Lockhart, Narrandera, Tarcutta, Urana, Wagga Wagga and Yanco 1:100,000 mapsheets and Ariah Park, Wallaroobie Range and Yoogali 1:50,000 mapsheets). Exotic pine plantations and native species plantings were also mapped. Remnants of greater than one hectare were captured through on-screen GIS digitising at scales of approximately 1:4,000. The plant community type mapping was independently assessed using random blind validation points as having a user accuracy of 87%. This level of accuracy demonstrates the applicability of the methodology for mapping open forests, woodlands and open woodlands of south-eastern Australia and probably other vegetation elsewhere. Such accurate mapping provides end users with confidence when using vegetation maps in environmental assessment and land use planning.
This thesis presents various algorithms which have been developed for on-line event reconstruction in the CBM experiment at GSI, Darmstadt and the ALICE experiment at CERN, Geneve. Despite the fact that the experiments are different — CBM is a fixed target experiment with forward geometry, while ALICE has a typical collider geometry — they share common aspects when reconstruction is concerned.
The thesis describes:
— general modifications to the Kalman filter method, which allows one to accelerate, to improve, and to simplify existing fit algorithms;
— developed algorithms for track fit in CBM and ALICE experiment, including a new method for track extrapolation in non-homogeneous magnetic field.
— developed algorithms for primary and secondary vertex fit in the both experiments. In particular, a new method of reconstruction of decayed particles is presented.
— developed parallel algorithm for the on-line tracking in the CBM experiment.
— developed parallel algorithm for the on-line tracking in High Level Trigger of the ALICE experiment.
— the realisation of the track finders on modern hardware, such as SIMD CPU registers and GPU accelerators.
All the presented methods have been developed by or with the direct participation of the author.
Schulkinder mit einem türkischen Migrationshintergrund zeigen im deutschen Bildungssystem einen spezifischen Leistungsnachteil: Während der Leistungsnachteil von Schulkindern mit einem Migrationshintergrund aus anderen Ländern durch Hintergrundvariablen wie beispielsweise dem SES aufklärbar ist, ist der Leistungsabstand zwischen Schulkindern mit einem türkischen Migrationshintergrund und Schulkindern ohne Migrationshintergrund nicht nur stärker ausgeprägt, sondern zudem nicht durch die bisher betrachteten Hintergrundvariablen aufklärbar. Daher erscheint die Suche nach Gründen für diesen spezifischen Leistungsnachteil bei Prozessen des vorschulischen Kompetenzerwerbs notwendig.
Eine Voraussetzung für schulischen Erfolg ist Selbstkontrolle, also die Fähigkeit, eine Handlungstendenz für das Erreichen eines anderen Zieles zu unterdrücken. Kinder, die bereits im Kindergartenalter eine gut ausgeprägte Selbstkontrolle aufweisen, zeigen in ihrem späteren Leben bessere Schulleistungen als Kindergartenkinder mit einer geringeren Fähigkeit zur Selbstkontrolle. Die Fähigkeit zur Selbstkontrolle könnte bei Kindern mit einem türkischen Migrationshintergrund durch kultur- und/oder migrationsspezifische Faktoren geringer sein als die von Kindern ohne Migrationshintergrund. Als kulturspezifischer Faktor ist beispielsweise eine geringere Bewertung von Selbstkontrolle im türkischen Erziehungssystem möglich; als migrationsspezifischer Faktor kommt eine Verminderung der Selbstkontrolle durch migrationsbedingte Stressoren in Betracht.
Daher war die zentrale Frage der vorliegenden Dissertation, ob Kindergartenkinder mit einem türkischen Migrationshintergrund eine geringere Selbstkontrolle zeigen als Kindergartenkinder ohne Migrationshintergrund. Ein bewährtes Paradigma zur Erfassung von Selbstkontrolle bei Kindergartenkindern ist der Belohnungsaufschub, die Fähigkeit auf eine sofortige, kleinere Belohnung zugunsten einer späteren aber größeren Belohnung zu verzichten. In einer Literaturübersicht (Artikel 1) wurde sich mit verschiedenen Paradigmen zur Erfassung des Belohnungsaufschubes beschäftigt. Dabei wurden Probleme in der konvergenten Validität der bestehenden Methoden festgestellt. Das Warteparadigma scheint den Belohnungsaufschub im Kindergartenalter am adäquatesten zu erfassen, zeigt jedoch nur eine geringe Re-Test Reliabilität. Aus diesem Grund wurde eine neue Variante der klassischen Warteaufgabe, die Sanduhraufgabe, auf ihre prognostische Validität und Re-Test Reliabilität geprüft (Artikel 2). Die Sanduhraufgabe, gemessenen im Kindergartenalter, besitzt eine ausreichende Re-Test Reliabilität und Vorhersagekraft für mathematische Kompetenzen und Verhaltensauffälligkeiten am Ende der ersten Klasse.
Mit dieser Aufgabe wurde die zentrale Frage der vorliegenden Dissertation, ob Kindergartenkinder mit einem türkischen Migrationshintergrund eine geringere Selbstkontrolle zeigen als Kindergartenkinder ohne Migrationshintergrund, untersucht (Artikel 3). Zur Differenzierung zwischen kultur- und migrationsspezifischen Faktoren wurde hierbei die Selbstkontrollfähigkeit von Kindergartenkindern mit unterschiedlichem Migrationshintergrund (türkisch vs. andere) verglichen sowie die von deutschen und türkischen Kindern ohne Migrationshintergrund. Die in Deutschland untersuchten Gruppen (ohne Migrationshintergrund, türkischer Migrationshintergrund und Migrationshintergrund aus anderen Ländern) unterschieden sich nicht in ihrer Selbstkontrolle. Damit scheint der spezifische Leistungsnachteil von Kindern mit einem türkischen Migrationshintergrund im deutschen Bildungssystem nicht durch vorschulische Unterschiede in der Fähigkeit zur Selbstkontrolle erklärbar zu sein. Allerdings wiesen die türkischen Kinder ohne Migrationshintergrund eine geringere Selbstkontrolle auf als die deutschen Kinder ohne Migrationshintergrund. Die Ergebnisse wurden bezüglich ihrer Aussagekraft über mögliche kultur- und migrationsspezifische Einflussfaktoren auf die Selbstkontrolle von Kindergartenkindern diskutiert.
Nicht nur literarische Werke und Figuren, Schriftsteller und Festschriftempfänger – auch Verben können zu Grenzgängern werden. Während das Grenzgängertum in der ersten Gruppe meist äußeren Umständen wie z.B. Migration geschuldet ist, gibt es bei Verben eigentlich keinen Grund, zu Grenzgängern zu werden. Dennoch kommt es immer wieder zu solchen Phänomenen. Dies impliziert, dass es überhaupt Grenzen gibt, die die Verben in bestimmte Rubriken verweisen; dies sind üblicherweise die sog. Flexionsklassen, etwa in Gestalt der starken und schwachen Klasse. Dieser Beitrag befasst sich mit Grenzen im Verbalbereich, illustriert anhand einiger skandinavischer Verben. In einem weiteren Schritt sollen auch Grenzziehungen, Grenzveränderungen und Grenzauflösungen beleuchtet werden. Dabei stellt sich die Frage, wie unverbrüchlich Grenzen sind, und insbesondere, warum es überhaupt Flexionsklassen gibt und warum sie sich oft so hartnäckig erhalten. Solche Fragen wurden bisher viel zu selten gestellt. Schließlich werden temporäre und dauerhafte Grenzüberschreitungen von Verben beleuchtet. Dabei verharren bestimmte Verben über Jahrhunderte hinweg als Grenzgänger zwischen wohletablierten Klassen. Speziell solche Phänomene verlangen eine Begründung, denn Grenzen, so steht zu vermuten, sollten dazu dienen, eine gewisse Ordnung zu garantieren.
Touroultia, a new genus of Onciderini Thomson, 1860 (Coleoptera: Cerambycidae: Lamiinae) is described and illustrated. Five new species of Onciderini are also described and illustrated: Jamesia ramirezi from Costa Rica; Peritrox marcelae from French Guiana; Touroultia swifti from Ecuador; Touroultia lordi from French Guiana; Trestoncideres santossilvai from Brazil. Keys to the known species of Peritrox Bates, 1865; Touroultia gen. nov.; and Trestoncideres Martins and Galileo, 1990 are provided. The following new synonymies are proposed: Calliphenges Waterhouse, 1880 (Colobotheini) = Malthonea Thomson, 1864 (Desmiphorini); Paraclytemnestra Breuning, 1974 (Onciderini) = Jamesia Jekel, 1861 (Onciderini); Orteguaza Lane, 1958 (Apomecynini) = Clavidesmus Dillon and Dillon, 1946 (Onciderini). The following new combinations are proposed: Clavidesmus funerarius (Lane, 1958) (Onciderini); Clavidesmus lichenigerus (Lane, 1958) (Onciderini); Ischiocentra insulata (Rodrigues and Mermudes, 2011); Malthonea cuprascens (Waterhouse, 1880) (Desmiphorini); Touroultia obscurella (Bates, 1865) (Onciderini). The following species is restored to original combination: Jamesia lineata Fisher, 1926 (Onciderini). The following 13 new country records are reported: Ataxia hovorei Lingafelter and Nearns, 2007 (Pteropliini) (Haiti); Carterica soror Belon, 1896 (Colobotheini) (Ecuador); Colobothea lunulata Lucas, 1859 (Colobotheini) (Colombia); Curius punctatus (Fisher, 1932) (Curiini) (Haiti); Cyclopeplus lacordairei Thomson, 1868 (Anisocerini) (Colombia); Iarucanga mimica (Bates, 1866) (Hemilophini) (Ecuador); Pirangoclytus latithorax (Martins and Galileo, 2008) (Clytini) (Costa Rica); Porangonycha princeps (Bates, 1872) (Hemilophini) (Colombia); Trestonia lateapicata Martins and Galileo, 2010 (Onciderini) (Brazil); Tulcus dimidiatus (Bates, 1865) (Onciderini) (Colombia); Unaporanga cincta Martins and Galileo, 2007 (Hemilophini) (Colombia); Zeale dubia Galileo and Martins, 1997 (Hemilophini) (Colombia); Zonotylus interruptus (Olivier, 1790) (Trachyderini) (Colombia).
The American species belonging to the genus Gonaphodiellus Schmidt (Coleoptera: Scarabaeidae: Aphodiinae) are redescribed and figured. Two new genera are described: Gonaphodioides and Gonaphodiopsis. Fourteen new species are described: Gonaphodiellus arcanus, G. cerropuntanus, G. manantlanicus, G. martinpierai, G. omiltemicus, G. sacatepequezis, Gonaphodioides newtoni, G. ratcliffei, G. skelleyi, Gonaphodiopsis deloyai, G. hypogea, G. montesdeocai, G. pachecoi, G. teopiscaensis. The lectotype of Aphodius columbicus (Harold, 1880) is designated. The following new combinations are proposed: Gonaphodiellus nigrinus (Schmidt, 1916), Gonaphodioides acutecernans (Balthasar, 1960), Gonaphodioides chapini (Hinton, 1934), Gonaphodioides columbicus (Harold, 1880), Gonaphodioides sincerus (Petrovitz, 1973). Aphodius (Gonaphodiellus) xalapensis Galante, Stebnicka and Verdú, 2003 is placed as a junior synonym of Gonaphodiellus bimaculosus (Schmidt, 1909), new synonymy. Aphodius ataenioides Hinton, 1938 and Aphodius (Blackburneus) castanescens Petrovitz, 1973 are placed as junior synonyms of Gonaphodioides chapini (Hinton, 1934), new synonymies.
We conducted a morphological and mtDNA analysis of Cicindela decemnotata Say (Coleoptera: Carabidae: Cicindelinae) populations from throughout its geographic range to determine the extent of variation within the species and to assess the validity of subspecific names. The morphological study included an analysis of traditional subspecific characters including elytral color and maculations. These results provided evidence for the recognition of four subspecies of C. decemnotata, three of which are new: 1. C. d. decemnotata Say usually with green to dark green dorsal coloration and complete elytral maculations; it is widely distributed from Canada south to northern New Mexico and west into southern Utah and Idaho; 2. C. d. meriwetheri n. ssp. is distinguished by its bright green to green dorsal coloration, elytral maculation characterized by a thin middle band, a lack of humeral maculations, and a small number of genal setae; it has a restricted distribution from eastern Washington north to south central British Columbia; 3. C. d. bonnevillensis n. ssp. is distinguished by a combination of green to green-purple dorsal coloration and its greatly reduced elytral maculations; it is restricted to the area of ancient Lake Bonneville in north central Utah; 4. C. d. montevolans n. ssp. is distinguished by a predominately red-purple dorsal color and greatly reduced elytral maculations; its distribution is restricted to high elevations of the Bear River Mountains of northeastern Utah and southeastern Idaho. We also analyzed the mitochondrial haplotypes for cob and cox1 genes for one to six individuals from each of the six populations. This molecular analysis indicated recently diverged but discrete groups within C. decemnotata that are compatible with the subspecies distinctions postulated from morphology. These shallow molecular divergences within C. decemnotata are best explained by rapid phylogenetic radiation in the recent geological past in the wake of postglacial recession.
Ziel dieser Arbeit war es erstmals durch eine Kombination aus chemischer Mutagenese und gezielter genetischer Modifikation (hier: „metabolic engineering“) einen Phaffia-Stamm herzustellen, welcher über die Mutagenese hinaus über eine weiter verstärkte Astaxanthin-Synthese verfügt.
Die von „DSM Nutritional Products“ bereitgestellten chemischen Mutanten wurden analysiert und über einen Selektionsprozess auf Pigmentstabilität und Wachstum hin optimiert, da die Stämme aus cryogenisierter Dauerkultur starke Pigmentinstabilitäten und ein verzögertes Wachstum aufwiesen.
Über eine exploratorische Phase wurde die Carotinoidsynthese analysiert und festgestellt, dass in den Mutanten keine Einzelreaktionen betroffen sind, welche für die Heraufregulierung der Carotinoidsynthese in den Mutanten verantwortlich sind. Hierbei wurden Limitierungen identifiziert und diese durch Transformation von Expressionsplasmiden mit geeigneten Genen aufgehoben, um damit eine noch effizientere Metabolisierung von Astaxanthin-Vorstufen hin zu Astaxanthin zu erreichen. Eine Überexpression der Phytoensynthase/Lycopinzyklase crtYB resultierte in einem gesteigerten Carotinoidgehalt bei gleichbleibendem Astaxanthin- Anteil. Durch eine zweite Transformation mit einer Expressionskassette für die Astaxanthin-Synthase asy konnte der Carotinoidgehalt weiter gesteigert und zusätzlich eine Limitierung der Metabolisierung von Astaxanthin-Vorstufen behoben werden, sodass die Transformante nahezu alle Intermediate der Astaxanthinsynthese zu Astaxanthin metabolisieren konnte (Gassel et al. 2013). Es konnte gezeigt werden, dass auch in den Mutanten, aus Experimenten mit dem Wildtyp bekannte, Limitierungen identifiziert und ausgeglichen werden konnten.
Manfred Moritz 60 Jahre alt
(1991)
Am 12. September 1991 beging der Arachnologe Dr. Manfred MORITZ (Berlin) seinen 60. Geburtstag. Sein langjähriges Wirken als Kustos am Museum für Naturkunde der Humboldt-Universität zu Berlin, das seinen Niederschlag auch in zahlreichen wissenschaftlichen Publikationen und umfangreicher
Korrespondenz fand, wird aus der Sicht des Gratulanten dargestellt.
"... die werdent ouch Helmbrehtel!" : Zu den Prager und Wiener "Helmbrechten" im Spätmittelalter
(1987)
Man kann voraussetzen, daß einem Hörer oder Leser nach seiner Bekanntschaft mit der Erzählung vom 'Helmbrecht' der Name des Helden etwas anderes als ein beliebiger Rufname bedeutet haben wird. Jeder reale Namensträger ist für einen Rezipienten der Geschichte auffällig, und der Name wird eine gewisse Distanz hervorrufen. Vom Zeitpunkt der Erstaufführung der Erzählung Wernhers des Gartenaeres an konnotiert der Name Gewalt gegen Bauern, Strauchrittertum und Wegelagerei, Gottlosigkeit, Standesverrat und andere Bedeutungen mehr, deren Glieder eine ganze Kette negativer Besetzungen bilden. Man wird als Kenner der Materie seine Kinder nicht Helmbrecht nennen und auch Freunden von der Namensgebung abraten: nomen est omen. In der Meidung eines nunmehr besetzten Eigennamens artikuliert sich die Angst, durch die enge Relation von Zeichen und Bezeichnetem könne einer so werden wie jener Helmbrecht.
Hoffmanns erstaunliche Erzählung "Der Zusammenhang der Dinge" beginnt mit einer Grundsatzdiskussion zwischen den Freunden Ludwig und Euchar. [...] Mit den beiden Protagonisten sind zugleich zwei Bilder über den Zusammenhang der Dinge einander gegenübergestellt: Uhrwerk (Ludwig) und roter Faden (Euchar). Beiden gemeinsam ist offenbar die Weigerung, den Lauf der Welt als blindes Geschehen, als disparate Folge von Zufällen anzusehen. Worin aber ihre positive Doktrin besteht, in welchem Sinn der Lauf der Dinge als zweckhaft eingerichtetes Ganzes aufzufassen sei, das bleibt zunächst, bei Ludwig wie bei Euchar, undeutlich.
Arachnology and the Internet
(1995)
Das Editorial informiert über einige Veränderungen, die sich bei der Herausgabe der Zeitschrift Arachnologische Mitteilungen in jüngster Zeit ergeben haben (bspw. die Online-Verfügbarkeit betreffend). Wenngleich sich der Anteil der englischsprachigen Beiträge in letzten Jahren auf ca. 50 % erhöht hat, möchte die Zeitschrift auch künftig die Möglichkeit bieten auf Deutsch zu publizieren.
2008 konnte erstmals in der Erft ein überwinterndes Vorkommen von Pistia stratiotes beobachtet werden, das sich seitdem immer weiter ausbreitet, in der Erft und in angrenzenden Gewässern dichte Massenbestände ausbildet und die Gewässeroberfläche teilweise vollständig bedeckt. Die Bestände blühen reichlich von Juni bis in den November hinein und bilden viele Samen aus, die eine hohe Keimungsrate aufweisen. Aufgrund der bereits bestehenden Problematik der Beschattung ganzer Nebengewässer und Seitenarme und des durch die Verdriftung von Pflanzen und Samen in den Rhein bestehenden hohen Ausbreitungspotenzials der Art für den Rhein und angrenzende Gewässer erscheint ein Management der Art notwendig.
Subvisible cirrus clouds (SVCs) may contribute to dehydration close to the tropical tropopause. The higher and colder SVCs and the larger their ice crystals, the more likely they represent the last efficient point of contact of the gas phase with the ice phase and, hence, the last dehydrating step, before the air enters the stratosphere. The first simultaneous in situ and remote sensing measurements of SVCs were taken during the APE-THESEO campaign in the western Indian ocean in February/March 1999. The observed clouds, termed Ultrathin Tropical Tropopause Clouds (UTTCs), belong to the geometrically and optically thinnest large-scale clouds in the Earth's atmosphere. Individual UTTCs may exist for many hours as an only 200–300 m thick cloud layer just a few hundred meters below the tropical cold point tropopause, covering up to 105 km2. With temperatures as low as 181 K these clouds are prime representatives for defining the water mixing ratio of air entering the lower stratosphere.
Mechanisms by which subvisible cirrus clouds (SVCs) might contribute to dehydration close to the tropical tropopause are not well understood. Recently Ultrathin Tropical Tropopause Clouds (UTTCs) with optical depths around 10−4 have been detected in the western Indian ocean. These clouds cover thousands of square kilometers as 200–300 m thick distinct and homogeneous layer just below the tropical tropopause. In their condensed phase UTTCs contain only 1–5% of the total water, and essentially no nitric acid. A new cloud stabilization mechanism is required to explain this small fraction of the condensed water content in the clouds and their small vertical thickness. This work suggests a mechanism, which forces the particles into a thin layer, based on upwelling of the air of some mm/s to balance the ice particles, supersaturation with respect to ice above and subsaturation below the UTTC. In situ measurements suggest that these requirements are fulfilled. The basic physical properties of this mechanism are explored by means of a single particle model. Comprehensive 1-D cloud simulations demonstrate this stabilization mechanism to be robust against rapid temperature fluctuations of +/−0.5 K. However, rapid warming (ΔT>2 K) leads to evaporation of the UTTC, while rapid cooling (ΔT<−2 K) leads to destabilization of the particles with the potential for significant dehydration below the cloud.
Balloon-borne measurements of CFC-11 (on flights of the DIRAC in situ gas chromatograph and the DESCARTES grab sampler), ClO and O3 were made during the 1999/2000 winter as part of the SOLVE-THESEO 2000 campaign. Here we present the CFC-11 data from nine flights and compare them first with data from other instruments which flew during the campaign and then with the vertical distributions calculated by the SLIMCAT 3-D CTM. We calculate ozone loss inside the Arctic vortex between late January and early March using the relation between CFC-11 and O3 measured on the flights, the peak ozone loss (1200 ppbv) occurs in the 440–470 K region in early March in reasonable agreement with other published empirical estimates. There is also a good agreement between ozone losses derived from three independent balloon tracer data sets used here. The magnitude and vertical distribution of the loss derived from the measurements is in good agreement with the loss calculated from SLIMCAT over Kiruna for the same days.
Turbulent fluxes of carbonyl sulfide (COS) and carbon disulfide (CS2) were measured over a spruce forest in Central Germany using the relaxed eddy accumulation (REA) technique. A REA sampler was developed and validated using simultaneous measurements of CO2 fluxes by REA and by eddy correlation. REA measurements were conducted during six campaigns covering spring, summer, and fall between 1997 and 1999. Both uptake and emission of COS and CS2 by the forest were observed, with deposition occurring mainly during the sunlit period and emission mainly during the dark period. On the average, however, the forest acts as a sink for both gases. The average fluxes for COS and CS2 are -93 ± 11.7 pmol m -2 s -1 and -18 ± 7.6 pmol m -2 s -1, respectively. The fluxes of both gases appear to be correlated to photosynthetically active radiation and to the CO2 and H2O fluxes, supporting the idea that the air-vegetation exchange of both gases is controlled by stomata. An uptake ratio COS / CO2 of 10 ± 1.7 pmol mmol -1 has been derived from the regression line for the correlation between the COS and CO2 fluxes. This uptake ratio, if representative for the global terrestrial net primary production, would correspond to a sink of 2.3 ± 0.5 Tg COS yr-1.
Measurements of OH, the sum of peroxy radicals (ROx), non-methane hydrocarbons (NMHCs) and various other trace gases were made at the Meteorological Observatory Hohenpeissenberg in June 2000. The data from an intensive measurement period characterised by high solar insolation (18-21 June) are analysed. The maximum midday OH concentration ranged between 4.5 x 106 molecules cm-3 and 7.4 x 106 molecules cm-3. The maximum total ROx mixing ratio increased from about 55 pptv on 18 June to nearly 70 pptv on 20 and 21 June. A total of 64 NMHCs, including isoprene and monoterpenes, were measured every 1 to 6 hours. The oxidation rate of the NMHCs by OH was calculated and reached a total of over 14 x 106 molecules cm-3 s-1 on two days. A simple photostationary state balance model was used to simulate the ambient OH and ROx concentrations with the measured data as input. The model was able to reproduce the main features of the diurnal profiles of both OH and ROx. The model results proved to be most sensitive to assumptions about the mixing ratio of formaldehyde (HCHO), which was included as a proxy for carbonyl compounds, and about the partitioning between HO2 and RO2. The measured OH concentration and ROx mixing ratios were reproduced well by assuming the presence of 3 ppbv HCHO and a ratio HO2/RO2 between 1:1 and 1:2. The most important source of OH, and conversely the greatest sink for ROx, was the recycling of HO2 radicals to OH. This reaction was responsible for the recycling of more than 45 x 106 molecules cm-3 s-1 on two days. The most important sink for OH, and the largest source of ROx, was the oxidation of NMHCs, in particular, of isoprene and the monoterpenes.
A new, two-channel instrument for simultaneous NO3 and N2O5 monitoring was used to make the first comprehensive set of nocturnal NOx measurements (NO, NO2, NO3 and N2O5) at the Taunus Observatory, a rural mountain site (Kleiner Feldberg) in South-western Germany. In May 2008, NO3 and N2O5 mixing ratios were well above the instrumental detection limit (a few ppt) on all nights of the campaign and were characterised by large variability resulting from inhomogeneously distributed sinks. The concentrations of NO3, N2O5 and NO2 were consistent with the equilibrium constant, K2, defining the rates of formation and thermal dissociation of N2O5. A steady-state lifetime analysis showed that nocturnal NOx losses were generally dominated by reaction of NO3 with volatile organic compounds in this forested region, with N2O5 uptake to aerosols of secondary importance. Analysis of a limited dataset obtained at high relative humidity indicated that the loss of N2O5 by reaction with water vapour is less efficient (> factor 3) than derived using laboratory kinetic data. The fraction of NOx present as NO3 and N2O5 reached ≈20% on some nights, with night-time losses of NOx competing with daytime losses.
In this work we present the setup and first tests of our new BIO IN detector. This detector is designed to classify atmospheric ice nuclei (IN) for their biological content. Biological material is identified via its auto-fluorescence (intrinsic fluorescence) after irradiation with UV radiation. Ice nuclei are key substances for precipitation development via the Bergeron–Findeisen process. The level of scientific knowledge regarding origin and climatology (temporal and spatial distribution) of IN is very low. Some biological material is known to be active as IN even at relatively high temperatures of up to –2°C (e.g. pseudomonas syringae bacteria). These biological IN could have a strong influence on the formation of clouds and precipitation. We have designed the new BIO IN sensor to analyze the abundance of IN of biological origin. The instrument will be flown on one of the first missions of the new German research aircraft ''HALO'' (High Altitude and LOng Range).
During the second part of the TROCCINOX campaign that took place in Brazil in early 2005, chemical species were measured on-board of the high altitude research aircraft Geophysica (ozone, water vapor, NO, NOy, CH4 and CO) in the altitude range up to 20 km (or up to 450 K potential temperature), i.e. spanning the TTL region roughly extending between 350 and 420 K.
Analysis of transport across TTL is performed using a new version of the Chemical Lagrangian Model of the Stratosphere (CLaMS). In this new version, the stratospheric model has been extended to the earth surface. Above the tropopause, the isentropic and cross-isentropic advection in CLaMS is driven by ECMWF winds and heating/cooling rates derived from a radiation calculation. Below the tropopause the model smoothly transforms from the isentropic to hybrid-pressure coordinate and, in this way, takes into account the effect of large-scale convective transport as implemented in the ECMWF vertical wind. As with other CLaMS simulations, the irreversible transport, i.e. mixing, is controlled by the local horizontal strain and vertical shear rates.
Stratospheric and tropospheric signatures in the TTL can be seen both in the observation and in the model. The composition of air above ≈350 K is mainly controlled by mixing on a time scale of weeks or even months. Based on CLaMS transport studies where mixing can be completely switched off, we deduce that vertical mixing, mainly driven by the vertical shear in the outflow regions of the large-scale convection and in the vicinity of the subtropical jets, is necessary to understand the upward transport of the tropospheric air from the main convective outflow around 350 K up to the tropical tropopause around 380 K. This mechanism is most effective if the outflow of the mesoscale convective systems interacts with the subtropical jets.
In dieser Dissertation wird die diskursive Konstruktion der Übersetzer bzw. der Übersetzung in ausgewählten Chroniken der Eroberung Lateinamerikas untersucht, welche von Autoren unterschiedlicher Herkunft im ungefähren Zeitraum zwischen 1515 bis 1615 verfasst wurden. Im Rahmen einer historisch-deskriptiven Analyse wird erforscht, welchem Zweck die vorgefundenen sprachlichen Aussagen zur Übersetzungsthematik in den verschiedenen Chroniken dienen. Die Analyse zeigt deutlich, dass nicht nur die Erwähnung, sondern auch die Omission der Aussagen zu den Übersetzern bzw. den Übersetzungsprozessen eine wichtige Rolle einnimmt und Brüche und Widersprüche in den einzelnen Darstellungen hervortreten lässt. Es wird deutlich, dass Übersetzer und Übersetzung, aber auch deren Omission, nicht nur der Legitimierung bzw. Humanisierung der Eroberungen dienen, sondern dass vor allem auch die Figur des Übersetzers zum Zweck der Identitätskonstruktion (sowohl der eigenen als auch der des anderen), der Herstellung sowie Aufrechterhaltung asymmetrischer Dominanzverhältnisse und der Konstruktion bzw. Bestätigung bereits bestehender Geschlechterrollen funktionalisiert wird. Es wird gezeigt, dass „Übersetzung“, welche oftmals als völkerverbindendes Mittel der Kommunikation dargestellt wird, vor allem im Kontext der Eroberung nicht unbedingt ein friedliches Instrument darstellt, sondern enormes Macht- und Gewaltpotential in sich birgt. Außerdem gehen aus den Analysen die Konturen einer Forschungslücke hervor, die noch weitere Untersuchen ermöglicht, nicht nur in Bezug auf den Bereich des oralen Übersetzungsprozesses, sondern vor allem auch, was den Bereich der kulturellen Übersetzung betrifft.
Die Autoren geben in ihrem umfangreichen Werk für 384 häufige Spinnenarten eine graphische Darstellung der von diesen besiedelten Makrolebensräume. Weitere 554 seltenere Arten werden mit den zugeordneten Lebensraumkürzeln und den Quellen als Anhang tabellarisch aufgelistet. Eine Auswertung mikroökologischer/autökologischer Daten ist ausdrücklich nicht einbezogen. Dies wird zwar in der Einleitung deutlich gemacht - geht aber aus dem Titel nicht hervor.
1795 erschien ein Werk unter dem Titel "Sur la Decouverte du Rapport Constant, entre I'apparition ou la disparition, le travail ou le non travail, le plus ou le moins d'etendue des toiles ou des fils d'attache des Araignees des differentes especes; et les Variations AthmospMriques du beau temps a la pluye, du sec a I'humide, mais principalement du chaud - au - froid, & de la gelee a glace au veritable digel: par le Citoyen QuatremereD'lsjonval". Das Buch, aber auch seine Entstehungsgeschichte und das bewegte Leben des Autors schienen es mir wert zu sein, 200 Jahre nach Erscheinen einige Worte darüber zu verlieren. Dabei stütze ich mich auf die Übersetzung ins Deutsche (QUATREMÈRE-D'ISJONVAL 1799).
Ein motorangetriebenes Vakuumsauggerät kann eingesetzt werden, um die Anzahl Arthropoden pro Einheitsvolumen in der Vegetation zu ermitteln (MÜHLENBERG 1993) oder um einzelne Arthropoden schnell einzufangen. Für meine Untersuchungen an Spinnen, Weberknechten und deren potentieller Beute benutze ich für diesen Zweck ein kleines elektrisches Vakuumgerät, mit dem ich Arthropoden unbeschädigt einfangen kann, ohne dabei allzu viel unerwünschtes Streumaterial mit aufzunehmen. Ich beschreibe im Folgenden die Anpassung des von mir verwendeten Modells an meine Arbeitsanforderungen.
Aus dem Gebiet der Tschechischen Republik sind derzeit 21 Pseudoskorpion-Arten bekannt (DUCHAC 1994, VERNER 1971). Diese Liste kann nun um eine weitere Species erweitert werden. Während einer Exkursion im Rahmen des 15. Europäischen Arachnologenkolloquiums in Ceske Budejovice gelang es dem Verfasser, die Art Chernes (Toxochernes) nigrimanus ELLlNGSEN nachzuweisen.
The seasonality of transport and mixing of air into the lowermost stratosphere (LMS) is studied using distributions of mean age of air and a~mass balance approach, based on in-situ observations of SF6 and CO2 during the SPURT (Spurenstofftransport in der Tropopausenregion, trace gas transport in the tropopause region) aircraft campaigns. Combining the information of the mean age of air and the water vapour distributions we demonstrate that the tropospheric air transported into the LMS above the extratropical tropopause layer (ExTL) originates predominantly from the tropical tropopause layer (TTL). The concept of our mass balance is based on simultaneous measurements of the two passive tracers and the assumption that transport into the LMS can be described by age spectra which are superposition of two different modes. Based on this concept we conclude that the stratospheric influence on LMS composition is strongest in April with tropospheric fractions (α1) below 20% and that the strongest tropospheric signatures are found in October with (α1 greater than 80%. Beyond the fractions, our mass balance concept allows to calculate the associated transit times for transport of tropospheric air from the tropics into the LMS. The shortest transit times (<0.3 years) are derived for the summer, continuously increasing up to 0.8 years by the end of spring. These findings suggest that strong quasi-horizontal mixing across the weak subtropical jet from summer to mid of autumn and the considerably shorter residual transport time-scales within the lower branch of the Brewer-Dobson circulation in summer than in winter dominates the tropospheric influence in the LMS until the beginning of next year's summer.
Das Vorkommen von Collinsia submissa (L. KOCH, 1879; Nomenklatur nach ESKOV 1994; Synonym zu C. inerrans in PLA TNICK 1993) ist bislang nur für wenige Fundorte in Deutschland belegt. Diese Daten sind bis jetzt meist unveröffentlicht geblieben. Zur Autökologie der Art ist wenig bekannt. So findet sich z. B. bei HEIMER & NENTWIG (1991) (sub Milleriana inerrans) die Angabe: " ... selten gefunden, in Mooren nahe dem Boden" (S. 218), während MAURER & HÄNGGI (1990) Auenwald und Mähwiesen als Habitat angeben. HANGGI et al. (1995) führen in ihrer Auswertung nur wenige Einzelnachweise von C. submissa an. Diese stammen aus der Schweiz, aus den Niederlanden und aus Großbritannien. Als Habitate werden Äcker, eine Weide und ein Schilfrohricht genannt. Im Rahmen dieses Aufsatzes sollen alle uns verfügbaren Fundmeldungen dieser Art in Deutschland dokumentiert werden, wobei die Angaben aus dem Drachenfelser Landchen neu sind (vgl. Tab. 1). Auch soll an hand der von C. submissa vorläufig grob zu umreißen.
Das vorliegende Buch richtet sich primär an Vogelspinnenhalter. Aus verschiedenen Gründen soll eine kurze Vorstellung an dieser Stelle nicht versäumt werden. Zum einen, weil die exzellenten Farbfotos als Orientierung bei einer Artidentifikation auch Wissenschaftlern helfen können, zum anderen, weil Peter Klaas Beobachtungen auch von generellem wissenschaftlichem Interesse schildert. Zum Beispiel konnte er nachweisen und fotografisch dokumentieren, dass sich Spinnenlarven noch im Kokon bereits von Geschwister-Eiern ernähren. Eine Nahrungsaufnahme war bisher erst ab dem Nymphenstadium postuliert werden. Erstmalig wird die unter Vogelspinnen einmalige Konstruktion eines hängenden(!) Eikokons von Citharischius crawshayi gezeigt, bzw. wie ein Weibchen von Poecilotheria ornata die Häute ihres Nachwuchses einsammelt und aus der ,Kinderstube' entfernt.
Die biogeographische Sonderstellung der Berchtesgadener Alpen im deutschen Alpenraum ist hinlänglich bekannt. Zahlreiche Endemiten der (Nord-)Ostalpen erreichen an der Saalach ihre (nord-)westliche Verbreitungsgrenze (MERXMULLER 1952, HUBL 2001). Unter den Arachniden konnten solche Arten bereits bei Weberknechten (HAMMELBACHER 1987, BLICK & HAMMELBACHER 1994) und Spinnen (MUSTER 2000, 2001) nachgewiesen werden. Mit Chthonius (C.) alpicola wird erstmals ein Pseudoskorpion dieses Arealtyps vorgestellt.
In this third supplement to the Catalogue of Swiss spiders of MAURER & HANGGI (1990) 9 species are recorded for the first time for Switzerland. 4 additional species already published elsewhere are added to the list of Swiss spiders. 5 other earlier published species are listed, which are only known from greenhouses or under similar eusynanthropic conditions. The list of spiders known to Switzerland today comprises 944 species.
Die Sackspinne Clubiona similis L. Koch, 1867 wird in der älteren Literatur aus den verschiedensten Gebieten und Lebensraumtypen Mittel- und Osteuropas erwähnt. Nach HEIMER & NENTWIG (1991) ist sie "in feuchtem Gelände auf niedriger Vegetation" zu finden. Bei HANGGI et al. (1995) werden überwiegend Nachweise aus Küstendünen, daneben einzelne aus Wäldern und extensiv oder ungenutzten Lebensraumtypen des Offenlandes genannt.
Untersuchungen über die Spinnenbesiedlung des Pimpinellenberges, eines xerothermen Biotops in Brandenburg, erbrachten zum Teil überraschende Nachweise von Arten mit süd- bzw. südosteuropäischem Verbreitungsschwerpunkt (v.BROEN&JAKOBITZ2002). Während solche Arten für das südliche Deutschland und die südlichen und südostlichen Nachbarländer als Besiedler von Xerothermstandorten seit längerer Zeit dokumentiert sind (z.B. BUCHAR & ZDAREK 1960, MILLER & VALESOVA 1964, BRAUN 1969, CASEMIR 1975, THALER 1985, BAUCHHENSS 1988, STEINBERGER 1988), liegen aus den nord- und nordostdeutschen Bundesländern kaum Verbreitungsangaben vor oder Fundmeldungen fehlen gänzlich.
BUCHAR, Jan & Vlastimil Růžička (2002): Catalogue of spiders of the Czech Republic [Rezension]
(2003)
Das Ausmaß des ökofaunistischen Schrifttums über die Spinnen von Mitteleuropa hat es längst unmöglich gemacht, ohne großen Aufwand die für konkrete Fragen relevante Literatur angemessen und ausgewogen zu berücksichtigen. Zudem sind vie1e in regionalen bzw. lokalen Organen veröffentlichte Arbeiten nicht unmittelbar zuganglich, sowohl wegen des Erscheinungsortes wie aus sprachlichen Gründen. Umso wichtiger sind nun regionale Datenbanken und Kataloge, die das Schrifttum über ein bestimmtes Gebiet bzw. die Information über die regionale Verbreitung und das Auftreten der Arten zusammenfassen und erschließen. Die Aussagekraft einer solchen Zusammenschau hangt wesentlich ab von Art und Umfang der Datenbasis, also der Verläßlichkeit der Daten und Arbeiten sowie von Grad und Ausmaß der Durchforschung von Lebensraumen und Landesteilen.
Noch ein Vogelspinnenbuch ... ? Dachte ich auch erst, als ich ein Besprechungsexemplar zugesandt bekam, zugegeben. Beim ersten Durchblättern stellte sich heraus, dass es sich von anderen Vogelspinnenzuchtbüchern unterscheidet und eine Vorstellung an dieser Stelle lohnenswert ist. Steven B. Reichling beschreibt die Vogelspinnenfauna von Belize vor dem Hintergrund seiner achtjährigen Untersuchungszeit in dem kleinen mittelamerikanischen Land. Dabei ist das Genre des Buches nicht eindeutig zu bestimmen: Reichling inkludiert ökologische, biologische und taxonomische Aspekte, wobei der Schreibstil in einigen Kapiteln mehr an einen Abenteuerbericht als an eine wissenschaftliche Publikation erinnert. Ansprechen will der Autor aber ausdrücklich drei Lesergruppen: Wissenschaftler, Hobbyforscher und Naturliebhaber.
In den Arachn. Mitt. 23. wurde bereits ein Spinnenbuch aus Korea besprochen, welches wegen der koreanischen Schrift weniger für den europäischen Markt geeignet schien. Erst jetzt wurde ein weiteres koreanisches Bestimmungsbuch verfügbar, mit dem es sich deutlich anders verhält, obwohl es ebenfalls beinahe durchgehend in Koreanisch verfasst ist. Alle 546 Arten aus 220 Gattungen und 43 Familien werden mit Farbfotos (im Schnitt 2 pro Art) und Genitalzeichnungen (mindestens Palpus und Epigyne) vorgestellt.
Erste Freilandpopulationen von Theridion hannoniae DENIS, 1944 in Deutschland (Araneae: Theridiidae)
(2003)
In drei saarländischen Melaphyr-Steinbrüchen des Naturraumes Saar-Nahe-Bergland (Untereinheit Prims-Blies-Hügelland) wurde vom Autor im Jahr 1991 eine Theridion-Art festgestellt, die zunächst unbestimmt blieb, da sie damals in der Standard-Bestimmungsliteratur nicht aufgeführt war. Hinweise von T. BLICK, Hummeltal, auf die Meldung einer für Deutschland neuen Theridion-Art am Köln-Bonner Flughafen durch P. JÄGER (KLOID 1994, JÄGER 1996) ermöglichten schließlich die Determination der Tiere als Theridion hannoniae DENIS, 1944.
Caused by the similarity with the type species Aculepeira packardi and with A. ceropegia we confirm the combination Aculepeira lapponica for the arctic araneid Aranea lapponica Holm, 1945.
In den Jahren 1998, 2000 und 2001 wurde in Thüringen, Hessen und Niedersachsen an zehn Mittelgebirgsbachen, die einer erh6hten eigendynamischen Entwicklung unterliegen, die Spinnenfauna mit Bodenfallen entlang eines Gradienten von ufernahem zu uferfernem Bereich im Vergleich zu begradigten Referenzabschnitten untersucht. Ergänzend 34 wurden zeit- und flächenbezogene Handaufsammlungen auf vegetationslosen Uferbanken durchgeführt sowie die Besiedlung neu entstandener Uferstrukturen untersucht. Dabei wurden insgesamt 164 Arten nachgewiesen. In den Bodenfallen wurden 138 Arten erfasst, von denen 75 Arten (54%) sowohl im Grünland als auch in anderen Biotoptypen der Aue zu finden waren. 19 Arten kamen ausschließlich auf vegetationslosen Uferbanken vor. 12 Arten waren an den "dynamischen" Abschnitten signifikant häufiger als an den "statischen" Abschnitten und profitierten damit möglicherweise von der Förderung der Eigendynamik gegenüber keiner einzigen Art, die an den "statischen" Abschnitten signifikant häufiger als an den "dynamischen" Abschnitten war. Als Spezialisten für die Uferbänke im Mittelgebirgsbereich werden Oedothorax agrestis, Pirata knorri und Pirata latitans eingeschätzt.
Results are presented with respect to faunistics and are briefly discussed. Notes concerning Bavarian faunistics are added for the following remarkable species: Arctosa perita, Centromerus capucinus, Collinsia inerrans, Haplodrassus dalmatensis, Haplodrassus minor, Meioneta foscipalpa, Talavera aperta.
'Savaria' nannten die alten Römer diesen Ort - das hatte ich noch hinbekommen, aber als mich der ungarische Grenzer nach meinem Reiseziel fragte, konnte ich nur hilflos auf 'Szombathely' auf meiner Fahrkarte deuten. Ungarisch scheint eine zum Sprechen wenig geeignete Sprache, brauchen die Magyaren doch ganze fünf Silben um 'Prost' zu sagen: egeszsegere. Mehr ungarisch war aber auch gar nicht nötig, wurden wir doch von der Ankunft bis zur Abfahrt von unseren Gastgebern perfekt umsorgt.
Die Briten setzen, wie schon bei Bestimmungsbüchern, nun auch für Kartenwerke neue Maßstäbe. Dieses Werk hat eine lange Entstehungsgeschichte. Seit 1987 gibt es das "National Spider Recording Scheme", das seither drei "National Organisers" hatte: Clifford SMITH (1987-1993), David NELLIST (1993-1999) und Peter HARVEY (seit 1999). In den Atlas wurden die Spinnen-Nachweise (ähnlich wie seit vergleichsweise kurzer Zeit in Deutschland) im 10x10km-Raster erfasst.
Es wird ein Fall einer Gnaphoside (Scotophaeus scutulatus) geschildert, bei dem ein adultes Weibchen ein ebenfalls adultes Weibchen von Tegenaria atrica in deren Netz überwältigt. Ein Netzeindring-Verhalten ist von 4 weiteren Gnaphosiden-Arten bekannt (Poecilochroa senilis, Poecilochroa pugnax, Scotophaeus blackwalli, Taieria erebus), ein araneophages Verhalten ebenfalls bei 4 Arten (Drassodes lapidosus, Poecilochroa senilis (auspex), Scotophaeus scutulatus, Taieria erebus). Die Frage, ob ein Netzeindring-Verhalten bzw. ein araneophages Verhalten ein typischer Bestandteil des Verhaltensrepertoires epigäisch lebender Gnaphosiden ist, kann erst nach weiteren Beobachtungen und Versuchen beantwortet werden.
Balkan populations of Rafalskia olympica (KULCZYNSKI, 1903) are distinguished as separate subspecies Rafalskia olympica bulgarica ST ARI::GA, 1963 novo stat. Certain novel details of the R. olympica female body structure are presented. It is stated that Metaplatybunus drenskii SILHAVY, 1965 is not a synonym of R. olympica.
A comprehensive evaluation of seasonal backward trajectories initialized in the Northern Hemisphere lowermost stratosphere (LMS) has been performed to investigate the origin of air parcels and the main mechanisms determining characteristic structures in H2O and CO within the LMS. In particular we explain the fundamental role of the transit time since last tropopause crossing (tTST) for the chemical structure of the LMS as well as the feature of the extra-tropical tropopause transition layer (ExTL) as identified from CO profiles. The distribution of H2O in the background LMS above Θ=320 K and 340 K in northern winter and summer, respectively, is found to be governed mainly by the saturation mixing ratio, which in turn is determined by the Lagrangian Cold Point (LCP) encountered by each trajectory. Most of the backward trajectories from this region in the LMS experienced their LCP in the tropics and sub-tropics. The transit time since crossing the tropopause from the troposphere to the stratosphere (tTST) is independent of the H2O value of the air parcel. TST often occurs 20 days after trajectories have encountered their LCP. CO, on the other hand, depends strongly on tTST due to its finite lifetime. The ExTL as identified from CO measurements is then explained as a layer of air just above the tropopause, which on average encountered TST fairly recently.
The way we perceive the visual world depends crucially on the state of the observer. In the present study we show that what we are holding in working memory (WM) can bias the way we perceive ambiguous structure from motion stimuli. Holding in memory the percept of an unambiguously rotating sphere influenced the perceived direction of motion of an ambiguously rotating sphere presented shortly thereafter. In particular, we found a systematic difference between congruent dominance periods where the perceived direction of the ambiguous stimulus corresponded to the direction of the unambiguous one and incongruent dominance periods. Congruent dominance periods were more frequent when participants memorized the speed of the unambiguous sphere for delayed discrimination than when they performed an immediate judgment on a change in its speed. The analysis of dominance time-course showed that a sustained tendency to perceive the same direction of motion as the prior stimulus emerged only in the WM condition, whereas in the attention condition perceptual dominance dropped to chance levels at the end of the trial. The results are explained in terms of a direct involvement of early visual areas in the active representation of visual motion in WM.
his study aims at a detailed characterization of an ultra-fine aerosol particle counting system for operation on board the Russian high altitude research aircraft M-55 "Geophysica" (maximum ceiling of 21 km). The COndensation PArticle counting Systems (COPAS) consists of an aerosol inlet and two dual-channel continuous flow Condensation Particle Counters (CPCs).
The aerosol inlet, adapted for COPAS measurements on board the M-55 "Geophysica", is described concerning aspiration, transmission, and transport losses. The counting efficiencies of the CPCs using the chlorofluorocarbon FC-43 as the working fluid are studied experimentally at two pressure conditions, 300 hPa and 70 hPa. Three COPAS channels are operated with different temperature differences between the saturator and the condenser block yielding smallest detectable particle sizes (dp50 – as 50% detection "cut off" diameters) of 6 nm, 11 nm, and 15 nm, respectively, at ambient pressure of 70 hPa. The fourth COPAS channel is operated with an aerosol heating line (250°C) for a determination of the non-volatile number of particles. The heating line is experimentally proven to volatilize pure H2SO4-H2O particles for a particle diameter (dp) range of 11 nm<dp<200 nm.
Additionally this study includes investigation to exclude auto-nucleation of the working fluid inside the CPCs. An instrumental inter-comparison (cross-correlation) has been performed for several measurement flights and mission flights in the Arctic and the Tropics are discussed. Finally, COPAS measurements are used for an aircraft plume crossing analysis.
During SPURT (Spurenstofftransport in der Tropopausenregion, trace gas transport in the tropopause region) we performed measurements of a wide range of trace gases with different lifetimes and sink/source characteristics in the northern hemispheric upper troposphere (UT) and lowermost stratosphere (LMS). A large number of in-situ instruments were deployed on board a Learjet 35A, flying at altitudes up to 13.7 km, at times reaching to nearly 380 K potential temperature. Eight measurement campaigns (consisting of a total of 36 flights), distributed over all seasons and typically covering latitudes between 35° N and 75° N in the European longitude sector (10° W–20° E), were performed. Here we present an overview of the project, describing the instrumentation, the encountered meteorological situations during the campaigns and the data set available from SPURT. Measurements were obtained for N2O, CH4, CO, CO2, CFC12, H2, SF6, NO, NOy, O3 and H2O. We illustrate the strength of this new data set by showing mean distributions of the mixing ratios of selected trace gases, using a potential temperature – equivalent latitude coordinate system. The observations reveal that the LMS is most stratospheric in character during spring, with the highest mixing ratios of O3 and NOy and the lowest mixing ratios of N2O and SF6. The lowest mixing ratios of NOy and O3 are observed during autumn, together with the highest mixing ratios of N2O and SF6 indicating a strong tropospheric influence. For H2O, however, the maximum concentrations in the LMS are found during summer, suggesting unique (temperature- and convection-controlled) conditions for this molecule during transport across the tropopause. The SPURT data set is presently the most accurate and complete data set for many trace species in the LMS, and its main value is the simultaneous measurement of a suite of trace gases having different lifetimes and physical-chemical histories. It is thus very well suited for studies of atmospheric transport, for model validation, and for investigations of seasonal changes in the UT/LMS, as demonstrated in accompanying and elsewhere published studies.
Kann man Wahlaussagen verstehen? : Über die Sprache der Parteiprogramme zur Bundestagswahl 2009
(2009)
Die Sprache der Politik hat nicht den besten Ruf. Als Ergebnis von innerparteilichen Expertenrunden entstehen oft Texte in einer von Bürokratismen durchzogenen Fachsprache. Unverständlich vor allem für die, an die sie gerichtet sind: die Wähler. Wie ist es konkret um die Verständlichkeit der Wahlprogramme 2009 bestellt? Eine Analyse.
Active chlorine species play a dominant role in the catalytic destruction of stratospheric ozone in the polar vortices during the late winter and early spring seasons. Recently, the correct understanding of the ClO dimer cycle was challenged by the release of new laboratory absorption cross sections (Pope et al., 2007) yielding significant model underestimates of observed ClO and ozone loss (von Hobe et al., 2007). Under this aspect, Arctic stratospheric limb emission measurements carried out by the balloon version of the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS-B) from Kiruna (Sweden) on 11 January 2001 and 20/21 March 2003 have been reanalyzed with regard to the chlorine reservoir species ClONO2 and the active species, ClO and ClOOCl (Cl2O2). New laboratory measurements of IR absorption cross sections of ClOOCl for various temperatures and pressures allowed for the first time the retrieval of ClOOCl mixing ratios from remote sensing measurements. High values of active chlorine (ClOx) of roughly 2.3 ppbv at 20 km were observed by MIPAS-B in the cold mid-winter Arctic vortex on 11 January 2001. While nighttime ClOOCl shows enhanced values of nearly 1.1 ppbv at 20 km, ClONO2 mixing ratios are less than 0.1 ppbv at this altitude. In contrast, high ClONO2 mixing ratios of nearly 2.4 ppbv at 20 km have been observed in the late winter Arctic vortex on 20 March 2003. No significant ClOx amounts are detectable on this date since most of the active chlorine has already recovered to its main reservoir species ClONO2. The observed values of ClOx and ClONO2 are in line with the established chlorine chemistry. The thermal equilibrium constants between the dimer formation and its dissociation, as derived from the balloon measurements, are on the lower side of reported data and in good agreement with values recommended by von Hobe et al. (2007). Calculations with the ECHAM/MESSy Atmospheric Chemistry model (EMAC) using established kinetics show similar chlorine activation and deactivation, compared to the measurements in January 2001 and March 2003, respectively.
Chemical ozone loss in winter 1991–1992 is recalculated based on observations of the HALOE satellite instrument, ER-2 aircraft measurements and balloon data. HALOE satellite observations are shown to be reliable in the lower stratosphere below 400 K, at altitudes where profiles are most likely disturbed by the enhanced sulfate aerosols, as a result of the Mt. Pinatubo eruption in June 1991. Very large chemical ozone loss was observed below 400 K from Kiruna balloon observations between December and March 1992. Additionally, for the two winters after the Mt. Pinatubo eruption, HALOE satellite observations show a stronger extent of chemical ozone loss at lower altitudes compared to other Arctic winter between 1991 and 2003. In stipe of already occurring deactivation of chlorine in March 1992, Mipas-B and LPMA balloon observations indicate still chlorine activation at lower altitudes, consistent with observed chemical ozone loss occurring between February and March and April. Enhanced chemical ozone loss in the Arctic winter 1991–1992 as calculated in earlier studies is corroborated here.
On the observation of mesospheric air inside the arctic stratospheric polar vortex in early 2003
(2005)
During several balloon flights inside the Arctic polar vortex in early 2003, unusual trace gas distributions were observed, which indicate a strong influence of mesospheric air in the stratosphere. The tuneable diode laser (TDL) instrument SPIRALE (Spectroscopie InFrarouge par Absorption de Lasers Embarqués) measured unusually high CO values (up to 600 ppb) on 27 January at about 30 km altitude. The cryosampler BONBON sampled air masses with very high molecular Hydrogen, extremely low SF6 and enhanced CO values on 6 March at about 25 km altitude. Finally, the MIPAS (Michelson Interferometer for Passive Atmospheric Sounding) Fourier Transform Infra-Red (FTIR) spectrometer showed NOy values which are significantly higher than NOy* (the NOy derived from a correlation between N2O and NOy under undisturbed conditions), on 21 and 22 March in a layer centred at 22 km altitude. Thus, the mesospheric air seems to have been present in a layer descending from about 30 km in late January to 25 km altitude in early March and about 22 km altitude on 20 March. We present corroborating evidence from a model study using the KASIMA (KArlsruhe Simulation model of the Middle Atmosphere) model that also shows a layer of mesospheric air, which descended into the stratosphere in November and early December 2002, before the minor warming which occurred in late December 2002 lead to a descent of upper stratospheric air, cutting of a layer in which mesospheric air is present. This layer then descended inside the vortex over the course of the winter. The same feature is found in trajectory calculations, based on a large number of trajectories started in the vicinity of the observations on 6 March. Based on the difference between the mean age derived from SF6 (which has an irreversible mesospheric loss) and from CO2 (whose mesospheric loss is much smaller and reversible) we estimate that the fraction of mesospheric air in the layer observed on 6 March, must have been somewhere between 35% and 100%.
The Match method for quantification of polar chemical ozone loss is investigated mainly with respect to the impact of mixing across the vortex edge onto this estimate. We show for the winter 2002/03 that significant mixing across the vortex edge occurred and was accurately modeled by the Chemical Lagrangian Model of the Stratosphere. Observations of inert tracers and ozone in-situ from HAGAR on the Geophysica aircraft and sondes and also remote from MIPAS on ENVISAT were reproduced well. The model even reproduced a small vortex remnant that was isolated until June 2003 and was observed in-situ by a balloon-borne whole air sampler. We use this CLaMS simulation to quantify the impact of cross vortex edge mixing on the results of the Match method. It is shown that a time integration of the determined vortex average ozone loss rates as performed in Match results in larger ozone loss than the polar vortex average ozone loss in CLaMS. Also, the determination of the Match ozone loss rates can be influenced by mixing. This is especially important below 430 K, where ozone outside the vortex is lower than inside and the vortex boundary is not a strong transport barrier. This effect and further sampling effects cause an offset between vortex average ozone loss rates derived from Match and deduced from CLaMS with an even sampling for the entire vortex. Both, the time-integration of ozone loss and the determination of ozone loss rates for Match are evaluated using the winter 2002/03 CLaMS simulation. These impacts can explain the differences between CLaMS and Match column ozone loss. While the investigated effects somewhat reduce the apparent discrepancy in January ozone loss rates, a discrepancy between simulations and Match remains. However, its contribution to the accumulated ozone loss over the winter is not large.
Strong perturbations of the Arctic stratosphere during the winter 2002/2003 by planetary waves led to enhanced stretching and folding of the vortex. On two occasions the vortex in the lower stratosphere split into two secondary vortices that re-merged after some days. As a result of these strong disturbances the role of transport in and out of the vortex was stronger than usual. An advection and mixing simulation with the Chemical Lagrangian Model of the Stratosphere (CLaMS) utilising a suite of inert tracers tagging the original position of the air masses has been carried out. The results show a variety of synoptic and small scale features in the vicinity of the vortex boundary, especially long filaments peeling off the vortex edge and being slowly mixed into the mid latitude environment. The vortex folding events, followed by re-merging of different parts of the vortex led to strong filamentation of the vortex interior. During January, February, and March 2003 flights of the Russian high-altitude aircraft Geophysica were performed in order to probe the vortex, filaments and in one case the merging zone between the secondary vortices. Comparisons between CLaMS results and observations obtained from the Geophysica flights show in general good agreement.
Ground inhabiting spiders were investigated during the vegetation periods of 1996, 1998 and 2000 in four pine forests of Brandenburg, Germany. 1995 three of them were managed in different ways and one area served as a control. In total 105 different species were found and the lowest number of species was found on the control area. Due to the management the pine forests got opened and xerophilous species could settle the areas. In total a heterogeneous species community was found on each area. From year to year high rates of species turnover were measured even for the dominant species (> 5 % of all collected individuals per area and year). Some endangered species in Brandenburg were collected as well.
wo different single particle mass spectrometers were operated in parallel at the Swiss High Alpine Research Station Jungfraujoch (JFJ, 3580 m a.s.l.) during the Cloud and Aerosol Characterization Experiment (CLACE 6) in February and March 2007. During mixed phase cloud events ice crystals from 5 μm up to 20 μm were separated from large ice aggregates, non-activated, interstitial aerosol particles and supercooled droplets using an Ice-Counterflow Virtual Impactor (Ice-CVI). During one cloud period supercooled droplets were additionally sampled and analyzed by changing the Ice-CVI setup. The small ice particles and droplets were evaporated by injection into dry air inside the Ice-CVI. The resulting ice and droplet residues (IR and DR) were analyzed for size and composition by two single particle mass spectrometers: a custom-built Single Particle Laser-Ablation Time-of-Flight Mass Spectrometer (SPLAT) and a commercial Aerosol Time of Flight Mass Spectrometer (ATOFMS, TSI Model 3800). During CLACE 6 the SPLAT instrument characterized 355 individual ice residues that produced a mass spectrum for at least one polarity and the ATOFMS measured 152 particles. The mass spectra were binned in classes, based on the combination of dominating substances, such as mineral dust, sulfate, potassium and elemental carbon or organic material. The derived chemical information from the ice residues is compared to the JFJ ambient aerosol that was sampled while the measurement station was out of clouds (several thousand particles analyzed by SPLAT and ATOFMS) and to the composition of the residues of supercooled cloud droplets (SPLAT: 162 cloud droplet residues analyzed, ATOFMS: 1094). The measurements showed that mineral dust particles were strongly enhanced in the ice particle residues. 57% of the SPLAT spectra from ice residues were dominated by signatures from mineral compounds, and 78% of the ATOFMS spectra. Sulfate and nitrate containing particles were strongly depleted in the ice residues. Sulfate was found to dominate the droplet residues (~90% of the particles). The results from the two different single particle mass spectrometers were generally in agreement. Differences in the results originate from several causes, such as the different wavelength of the desorption and ionisation lasers and different size-dependent particle detection efficiencies.
We present the analysis of the impact of convection on the composition of the tropical tropopause layer region (TTL) in West-Africa during the AMMA-SCOUT campaign. Geophysica M55 aircraft observations of water vapor, ozone, aerosol and CO2 during August 2006 show perturbed values at altitudes ranging from 14 km to 17 km (above the main convective outflow) and satellite data indicates that air detrainment is likely to have originated from convective cloud east of the flights. Simulations of the BOLAM mesoscale model, nudged with infrared radiance temperatures, are used to estimate the convective impact in the upper troposphere and to assess the fraction of air processed by convection. The analysis shows that BOLAM correctly reproduces the location and the vertical structure of convective outflow. Model-aided analysis indicates that convection can influence the composition of the upper troposphere above the level of main outflow for an event of deep convection close to the observation site. Model analysis also shows that deep convection occurring in the entire Sahelian transect (up to 2000 km E of the measurement area) has a non negligible role in determining TTL composition.
We present the analysis of the impact of convection on the composition of the tropical tropopause layer region (TTL) in West-Africa during the AMMA-SCOUT campaign. Geophysica M55 aircraft observations of water vapor, ozone, aerosol and CO2 show perturbed values at altitudes ranging from 14 km to 17 km (above the main convective outflow) and satellite data indicates that air detrainment is likely originated from convective cloud east of the flight. Simulations of the BOLAM mesoscale model, nudged with infrared radiance temperatures, are used to estimate the convective impact in the upper troposphere and to assess the fraction of air processed by convection. The analysis shows that BOLAM correctly reproduces the location and the vertical structure of convective outflow. Model-aided analysis indicates that in the outflow of a large convective system, deep convection can largely modify chemical composition and aerosol distribution up to the tropical tropopause. Model analysis also shows that, on average, deep convection occurring in the entire Sahelian transect (up to 2000 km E of the measurement area) has a non negligible role in determining TTL composition.
Tracer measurements in the tropical tropopause layer during the AMMA/SCOUT-O3 aircraft campaign
(2009)
We present airborne in situ measurements made during the AMMA (African Monsoon Multidisciplinary Analysis)/SCOUT-O3 campaign between 31 July and 17 August 2006 on board the M55 Geophysica aircraft, based in Ouagadougou, Burkina Faso. CO2 and N2O were measured with the High Altitude Gas Analyzer (HAGAR), CO was measured with the Cryogenically Operated Laser Diode (COLD) instrument, and O3 with the Fast Ozone ANalyzer (FOZAN). We analyze the data obtained during five local flights to study the dominant transport processes controlling the tropical tropopause layer (TTL) above West-Africa: deep convection up to the level of main convective outflow, overshooting of deep convection, horizontal inmixing across the subtropical tropopause, and horizontal transport across the subtropical barrier. Except for the flight of 13 August, distinct minima in CO2 indicate convective outflow of boundary layer air in the TTL. The CO2 profiles show that the level of main convective outflow was mostly located between 350 and 360 K, and for 11 August reached up to 370 K. While the CO2 minima indicate quite significant convective influence, the O3 profiles suggest that the observed convective signatures were mostly not fresh, but of older origin. When compared with the mean O3 profile measured during a previous campaign over Darwin in November 2005, the O3 minimum at the main convective outflow level was less pronounced over Ouagadougou. Furthermore O3 mixing ratios were much higher throughout the whole TTL and, unlike over Darwin, rarely showed low values observed in the regional boundary layer. Signatures of irreversible mixing following overshooting of convective air were scarce in the tracer data. Some small signatures indicative of this process were found in CO2 profiles between 390 and 410 K during the flights of 4 and 8 August, and in CO data at 410 K on 7 August. However, the absence of expected corresponding signatures in other tracer data makes this evidence inconclusive, and overall there is little indication from the observations that overshooting convection has a profound impact on TTL composition during AMMA. We find the amount of photochemically aged air isentropically mixed into the TTL across the subtropical tropopause to be not significant. Using the N2O observations we estimate the fraction of aged extratropical stratospheric air in the TTL to be 0.0±0.1 up to 370 K during the local flights, increasing above this level to 0.2±0.15 at 390 K. The subtropical barrier, as indicated by the slope of the correlation between N2O and O3 between 415 and 490 K, does not appear as a sharp border between the tropics and extratropics, but rather as a gradual transition region between 10 and 25° N latitude where isentropic mixing between these two regions may occur.
In-situ measurements of ice crystal size distributions in tropical upper troposphere/lower stratosphere (UT/LS) clouds were performed during the SCOUT-AMMA campaign over West Africa in August 2006. The cloud properties were measured with a Forward Scattering Spectrometer Probe (FSSP-100) and a Cloud Imaging Probe (CIP) operated aboard the Russian high altitude research aircraft M-55 ''Geophysica'' with the mission base in Ouagadougou, Burkina Faso. A total of 117 ice particle size distributions were obtained from the measurements in the vicinity of Mesoscale Convective Systems (MCS). Two or three modal lognormal size distributions were fitted to the average size distributions for different potential temperature bins. The measurements showed proportionate more large ice particles compared to former measurements above maritime regions. With the help of trace gas measurements of NO, NOy, CO2, CO, and O3, and satellite images clouds in young and aged MCS outflow were identified. These events were observed at altitudes of 11.0 km to 14.2 km corresponding to potential temperature levels of 346 K to 356 K. In a young outflow (developing MCS) ice crystal number concentrations of up to 8.3 cm−3 and rimed ice particles with maximum dimensions exceeding 1.5 mm were found. A maximum ice water content of 0.05 g m−3 was observed and an effective radius of about 90 μm. In contrast the aged outflow events were more diluted and showed a maximum number concentration of 0.03 cm−3, an ice water content of 2.3 × 10−4 g m−3, an effective radius of about 18 μm, while the largest particles had a maximum dimension of 61 μm.
Close to the tropopause subvisual cirrus were encountered four times at altitudes of 15 km to 16.4 km. The mean ice particle number concentration of these encounters was 0.01 cm−3 with maximum particle sizes of 130 μm, and the mean ice water content was about 1.4 × 10−4 g m−3. All known in-situ measurements of subvisual tropopause cirrus are compared and an exponential fit on the size distributions is established in order to give a parameterisation for modelling.
A comparison of aerosol to ice crystal number concentrations, in order to obtain an estimate on how many ice particles result from activation of the present aerosol, yielded low activation ratios for the subvisual cirrus cases of roughly one cloud particle per 30 000 aerosol particles, while for the MCS outflow cases this resulted in a high ratio of one cloud particle per 300 aerosol particles.
Processes occurring in the tropical upper troposphere and lower stratosphere (UT/LS) are of importance for the global climate, for the stratospheric dynamics and air chemistry, and they influence the global distribution of water vapour, trace gases and aerosols. The mechanisms underlying cloud formation and variability in the UT/LS are of scientific concern as these still are not adequately described and quantified by numerical models. Part of the reasons for this is the scarcity of detailed in-situ measurements in particular from the Tropical Transition Layer (TTL) within the UT/LS. In this contribution we provide measurements of particle number densities and the amounts of non-volatile particles in the submicron size range present in the UT/LS over Southern Brazil, West Africa, and Northern Australia. The data were collected in-situ on board of the Russian high altitude research aircraft M-55 "Geophysica" using the specialised COPAS (COndensation PArticle counting System) instrument during the TROCCINOX (Araçatuba, Brazil, February 2005), the SCOUT-O3 (Darwin, Australia, December 2005), and SCOUT-AMMA (Ouagadougou, Burkina Faso, August 2006) campaigns. The vertical profiles obtained are compared to those from previous measurements from the NASA DC-8 and NASA WB-57F over Costa Rica and other tropical locations between 1999 and 2007. The number density of the submicron particles as function of altitude was found to be remarkably constant (even back to 1987) over the tropical UT/LS altitude band such that a parameterisation suitable for models can be extracted from the measurements. At altitudes corresponding to potential temperatures above 430 K a slight increase of the number densities from 2005/2006 results from the data in comparison to the 1987 to 2007 measurements. The origins of this increase are unknown. By contrast the data from Northern hemispheric mid latitudes do not exhibit such an increase between 1999 and 2006. Vertical profiles of the non-volatile fraction of the submicron particles were also measured by a COPAS channel and are presented here. The resulting profiles of the non-volatile number density fraction show a pronounced maximum of 50% in the tropical TTL over Australia and West Africa. Below and above this fraction is much lower attaining values of 10% and smaller. In the lower stratosphere the fine particles mostly consist of sulphuric acid which is reflected in the low numbers of non-volatile residues measured by COPAS. Without detailed chemical composition measurements the reason for the increase of non-volatile particle fractions cannot yet be given. The long distance transfer flights to Brazil, Australia and West-Africa were executed during a time window of 17 months within a period of relative volcanic quiescence. Thus the data measured during these transfers represent a "snapshot picture" documenting the status of a significant part of the global UT/LS aerosol (with sizes below 1 μm) at low concentration levels 15 years after the last major (i.e., the 1991 Mount Pinatubo) eruption. The corresponding latitudinal distributions of the measured particle number densities are also presented in this paper in order to provide input on the UT/LS background aerosol for modelling purposes.
Current atmospheric models do not include secondary organic aerosol (SOA) production from gas-phase reactions of polycyclic aromatic hydrocarbons (PAHs). Recent studies have shown that primary semivolatile emissions, previously assumed to be inert, undergo oxidation in the gas phase, leading to SOA formation. This opens the possibility that low-volatility gas-phase precursors are a potentially large source of SOA. In this work, SOA formation from gas-phase photooxidation of naphthalene, 1-methylnaphthalene (1-MN), 2-methylnaphthalene (2-MN), and 1,2-dimethylnaphthalene (1,2-DMN) is studied in the Caltech dual 28-m3 chambers. Under high-NOx conditions and aerosol mass loadings between 10 and 40 μg m, the SOA yields (mass of SOA per mass of hydrocarbon reacted) ranged from 0.19 to 0.30 for naphthalene, 0.19 to 0.39 for 1-MN, 0.26 to 0.45 for 2-MN, and constant at 0.31 for 1,2-DMN. Under low-NOx conditions, the SOA yields were measured to be 0.73, 0.68, and 0.58, for naphthalene, 1-MN, and 2-MN, respectively. The SOA was observed to be semivolatile under high-NOx conditions and essentially nonvolatile under low-NOx conditions, owing to the higher fraction of ring-retaining products formed under low-NOx conditions. When applying these measured yields to estimate SOA formation from primary emissions of diesel engines and wood burning, PAHs are estimated to yield 3–5 times more SOA than light aromatic compounds. PAHs can also account for up to 54% of the total SOA from oxidation of diesel emissions, representing a potentially large source of urban SOA.
Detailed knowledge of reaction mechanisms is key to understanding chemical, biological, and biophysical processes. For many reasons, it is desirable to comprehend how a reaction proceeds and what influences the reaction rate and its products.
In biophysics, reaction mechanisms provide insight into enzyme and protein function, the reason why they are so efficient, and what determines their reaction rates. They also reveal the relationship between the function of a protein and its structure and dynamics.
In chemistry, reaction mechanisms are able to explain side products, solvent effects, and the stereochemistry of a product. They are also the basis for potentially optimizing reactions with respect to yield, enhancing the stereoselectivity, or for modifying reactions in order to obtain other related products.
A key step to investigate reaction mechanisms is the identification and characterization of intermediates, which may be reactive, short-lived, and therefore only weakly populated. Nowadays, the structures of those can in most cases only be hypothesized based on products, side products, and isolable intermediates, because intermediates with a life time of less than a few microseconds are not accessible with the commonly used techniques for structure determination such as X-ray crystallography and nuclear magnetic resonance (NMR) spectroscopy.
In this thesis, two-dimensional infrared (2D-IR) spectroscopy is shown to be a powerful complement to the existing techniques for structure determination in solution. 2D-IR spectroscopy uses a femtosecond laser setup to investigate interactions between vibrations - analogous to 2D-NMR, which investigates the interactions between spins. Its ultrafast time resolution makes 2D-IR spectroscopy particularly well suited for the two topics investigated in this thesis: Structure Determination of Reactive Intermediates and Conformational Dynamics of Proteins.
Structure Determination of Reactive Intermediates: The focus of this thesis is using polarization-dependent 2D-IR (P2D-IR) spectroscopy for structure determination of N-crotonyloxazolidinone (referred to as 1), a small organic compound with a chiral oxazolidinone, known as Evans auxiliary, and its reactive complexes with the Lewis acids SnCl4 and Mg(ClO4)2. Chiral oxazolidinones in combination with Lewis acids have frequently been used in stereoselective synthesis for over 30 years. Nevertheless, the detailed mechanisms are in many cases xvi ABSTRACT still mere hypotheses and have not yet been experimentally proven. By accurately measuring the angles between the transition dipole moments in the molecules using an optimized P2D-IR setup and comparing the results to DFT calculations, the conformation of 1 and the conformation and coordination of the main complexes with SnCl4 and Mg(ClO4)2 are unequivocally identified and analyzed in depth. Structural details, such as a slight twist in the solution structure of 1, are detected using P2D-IR spectroscopy; these cannot be inferred from NMR spectroscopy or DFT calculations. In addition to the main Lewis acid complexes, complexes in low concentration are detected and tentatively assigned to different conformations and complexation geometries. The knowledge of those structures is essential for rationalizing the observed stereoselectivities. Additionally, a method is introduced that enables structure determination of molecules in complex mixtures and even in the presence of molecules with similar spectral properties and in high concentration. This work sets the stage for future studies of other substrate-catalyst complexes and reaction intermediates for which the structure determination has not been possible to date.
Conformational Dynamics of Proteins: Exchange 2D-IR spectroscopy allows the investigation of fast dynamics without disturbing the equilibrium of the exchanging species. It is therefore well suited to investigate fast dynamics of proteins and to reveal the speed limit of those. The temperature dependence of the conformational dynamics between the myoglobin substates A1 and A3 in equilibrium is analyzed. The various substates of myoglobin can be detected with FTIR spectroscopy, if carbon monoxide is bound to the heme. From previous studies it is known that the exchange rates at room temperature are in the picosecond time range, well suited to be investigated by 2D-IR spectroscopy. In the temperature range between 0 °C and 40 °C only a weak temperature dependence of the exchange rate in the myoglobin mutant L29I is observed in the present study. The exchange rate approximately doubles from 15 ns-1 at 0 °C to 31 ns-1 at 40 °C. It turned out that the conformational dynamics correlates linearly with the solvent viscosity, which itself is temperature dependent. Comparing our results to measurements at cryogenic temperatures, the linear relation between exchange time constant for this process and the viscosity is shown for the temperature range between -100 °C and 40 °C (corresponding to a viscosity change of 14 orders of magnitude). Thus, it is proven that the dynamics of the conformational switching are mainly determined by solvent dynamics, i.e., the protein dynamics are slaved to the solvent dynamics. This is the first time slaving is observed for such fast processes (in the picosecond time range). The observation implies a long-range structural rearrangement between the myoglobin substates A1 and A3. In addition, the exchange for other mutants and wild type myoglobin is analyzed qualitatively and found to agree with the conclusions drawn from L29I myoglobin.
Significant reductions in stratospheric ozone occur inside the polar vortices each spring when chlorine radicals produced by heterogeneous reactions on cold particle surfaces in winter destroy ozone mainly in two catalytic cycles, the ClO dimer cycle and the ClO/BrO cycle. Chlorofluorocarbons (CFCs), which are responsible for most of the chlorine currently present in the stratosphere, have been banned by the Montreal Protocol and its amendments, and the ozone layer is predicted to recover to 1980 levels within the next few decades. During the same period, however, climate change is expected to alter the temperature, circulation patterns and chemical composition in the stratosphere, and possible geo-engineering ventures to mitigate climate change may lead to additional changes. To realistically predict the response of the ozone layer to such influences requires the correct representation of all relevant processes. The European project RECONCILE has comprehensively addressed remaining questions in the context of polar ozone depletion, with the objective to quantify the rates of some of the most relevant, yet still uncertain physical and chemical processes. To this end RECONCILE used a broad approach of laboratory experiments, two field missions in the Arctic winter 2009/10 employing the high altitude research aircraft M55-Geophysica and an extensive match ozone sonde campaign, as well as microphysical and chemical transport modelling and data assimilation. Some of the main outcomes of RECONCILE are as follows: (1) vortex meteorology: the 2009/10 Arctic winter was unusually cold at stratospheric levels during the six-week period from mid-December 2009 until the end of January 2010, with reduced transport and mixing across the polar vortex edge; polar vortex stability and how it is influenced by dynamic processes in the troposphere has led to unprecedented, synoptic-scale stratospheric regions with temperatures below the frost point; in these regions stratospheric ice clouds have been observed, extending over >106km2 during more than 3 weeks. (2) Particle microphysics: heterogeneous nucleation of nitric acid trihydrate (NAT) particles in the absence of ice has been unambiguously demonstrated; conversely, the synoptic scale ice clouds also appear to nucleate heterogeneously; a variety of possible heterogeneous nuclei has been characterised by chemical analysis of the non-volatile fraction of the background aerosol; substantial formation of solid particles and denitrification via their sedimentation has been observed and model parameterizations have been improved. (3) Chemistry: strong evidence has been found for significant chlorine activation not only on polar stratospheric clouds (PSCs) but also on cold binary aerosol; laboratory experiments and field data on the ClOOCl photolysis rate and other kinetic parameters have been shown to be consistent with an adequate degree of certainty; no evidence has been found that would support the existence of yet unknown chemical mechanisms making a significant contribution to polar ozone loss. (4) Global modelling: results from process studies have been implemented in a prognostic chemistry climate model (CCM); simulations with improved parameterisations of processes relevant for polar ozone depletion are evaluated against satellite data and other long term records using data assimilation and detrended fluctuation analysis. Finally, measurements and process studies within RECONCILE were also applied to the winter 2010/11, when special meteorological conditions led to the highest chemical ozone loss ever observed in the Arctic. In addition to quantifying the 2010/11 ozone loss and to understand its causes including possible connections to climate change, its impacts were addressed, such as changes in surface ultraviolet (UV) radiation in the densely populated northern mid-latitudes.
Language and transnationalism : language discourse in transnational Salsa communities of practice
(2013)
Language ideologies in contemporary Western societies are characterised by a strong influence of the idea that one language ‘pertains’ to one culture. Yet, cultural developments of globalisation, such as migration, the construction of transnational networks or global mass media, question national frameworks of culture and language.
In this thesis, after reviewing the field of language ideology and discussing historical examples of the development of national language discourse, language ideologies in a transnational context are examined. Using ethnographic research methods and a discursive approach to interview data, concepts and ideas revolving around language of transnational Communities of Practice constituted through Salsa dancing are analysed. Due to its connections to the Latin American cultural space, the practice of Salsa dancing in non-Latin contexts intrinsically constructs transnational ties. Different Salsa Communities of Practice are studied in Sydney, Australia, and Frankfurt, Germany. Interestingly, different local communities show very different ideologies concerning the role of language, multilingualism, concepts of authenticity or influences of capitalist discourse. The cross-national approach allows studying the influence of different national discourses on the formation of local ideologies in transnational contexts.
Thus, next to scrutinising the traditional concept of a ‘language’ and its relevance in a transnational age, the theoretical aim of this study is to analyse the interaction of discourses from different realms – local, regional, national, transnational – in the formation of contemporary discourses on language. These construct new symbolic meanings of language that co-exist next to the national concept of the relationship of language and culture, so that a multiplication of language boundaries can be considered to be a characteristic trait of contemporary language discourse.
Sulphuric acid, ammonia, amines, and oxidised organics play a crucial role in nanoparticle formation in the atmosphere. In this study, we investigate the composition of nucleated nanoparticles formed from these compounds in the CLOUD chamber experiments at CERN. The investigation is carried out via analysis of the particle hygroscopicity, ethanol affinity, oxidation state, and ion composition. Hygroscopicity was studied by a hygroscopic tandem differential mobility analyser and a cloud condensation nuclei counter, ethanol affinity by an organic differential mobility analyser and particle oxidation level by a high-resolution time-of-flight aerosol mass spectrometer. The ion composition was studied by an atmospheric pressure interface time-of-flight mass spectrometer. The volume fraction of the organics in the particles during their growth from sizes of a few nanometers to tens of nanometers was derived from measured hygroscopicity assuming the Zdanovski-Stokes-Robinson relationship, and compared to values gained from the spectrometers. The ZSR-relationship was also applied to obtain the measured ethanol affinities during the particle growth, which were used to derive the volume fractions of sulphuric acid and the other inorganics (e.g. ammonium salts). In the presence of sulphuric acid and ammonia, particles with a mobility diameter of 150 nm were chemically neutralised to ammonium sulphate. In the presence of oxidation products of pinanediol, the organic volume fraction of freshly nucleated particles increased from 0.4 to ∼0.9, with an increase in diameter from 2 to 63 nm. Conversely, the sulphuric acid volume fraction decreased from 0.6 to 0.1 when the particle diameter increased from 2 to 50 nm. The results provide information on the composition of nucleated aerosol particles during their growth in the presence of various combinations of sulphuric acid, ammonia, dimethylamine and organic oxidation products.
During the APE-THESEO mission in the Indian Ocean the Myasishchev Design Bureau stratospheric research aircraft M55 Geophysica performed a flight over and within the inner core region of tropical cyclone Davina. Measurements of total water, water vapour, temperature, aerosol backscattering, ozone and tracers were made and are discussed here in comparison with the averages of those quantities acquired during the campaign time frame.
Temperature anomalies in the tropical tropopause layer (TTL), warmer than average in the lower part and colder than average in the upper TTL were observed. Ozone was strongly reduced compared to its average value, and thick cirrus decks were present up to the cold point, sometimes topped by a layer of very dry air. Evidence for meridional transport of trace gases in the stratosphere above the cyclone and the perturbed water distribution in the TTL is illustrated and discussed.
Number concentrations of total and non-volatile aerosol particles with size diameters >0.01 µm as well as particle size distributions (0.4–23 µm diameter) were measured in situ in the Arctic lower stratosphere (10–20.5 km altitude). The measurements were obtained during the campaigns European Polar Stratospheric Cloud and Lee Wave Experiment (EUPLEX) and Envisat-Arctic-Validation (EAV). The campaigns were based in Kiruna, Sweden, and took place from January to March 2003. Measurements were conducted onboard the Russian high-altitude research aircraft Geophysica using the low-pressure Condensation Nucleus Counter COPAS (COndensation PArticle Counter System) and a modified FSSP 300 (Forward Scattering Spectrometer Probe). Around 18–20 km altitude typical total particle number concentrations nt range at 10–20 cm−3 (ambient conditions). Correlations with the trace gases nitrous oxide (N2O) and trichlorofluoromethane (CFC-11) are discussed. Inside the polar vortex the total number of particles >0.01 µm increases with potential temperature while N2O is decreasing which indicates a source of particles in the above polar stratosphere or mesosphere. A separate channel of the COPAS instrument measures the fraction of aerosol particles non-volatile at 250°C. Inside the polar vortex a much higher fraction of particles contained non-volatile residues than outside the vortex (~24% outside vortex). This is most likely due to a strongly increased fraction of meteoritic material in the particles which is transported downward from the mesosphere inside the polar vortex. The high fraction of non-volatile residual particles gives therefore experimental evidence for downward transport of mesospheric air inside the polar vortex. It is also shown that the fraction of non-volatile residual particles serves directly as a suitable experimental vortex tracer. Nanometer-sized meteoritic smoke particles may also serve as nuclei for the condensation of gaseous sulfuric acid and water in the polar vortex and these additional particles may be responsible for the increase in the observed particle concentration at low N2O. The number concentrations of particles >0.4 µm measured with the FSSP decrease markedly inside the polar vortex with increasing potential temperature, also a consequence of subsidence of air from higher altitudes inside the vortex. Another focus of the analysis was put on the particle measurements in the lowermost stratosphere. For the total particle density relatively high number concentrations of several hundred particles per cm3 at altitudes below ~14 km were observed in several flights. To investigate the origin of these high number concentrations we conducted air mass trajectory calculations and compared the particle measurements with other trace gas observations. The high number concentrations of total particles in the lowermost stratosphere are probably caused by transport of originally tropospheric air from lower latitudes and are potentially influenced by recent particle nucleation.
The ambient and laboratory molecular and ion clusters were investigated. Here we present data on the ambient concentrations of both charged and uncharged molecular clusters as well as the performance of a pulse height condensation particle counter (PH-CPC) and an expansion condensation particle counter (E-CPC). The ambient molecular cluster concentrations were measured using both instruments, and they were deployed in conjunction with ion spectrometers and other aerosol instruments in Hyytiälä, Finland at the SMEAR II station during 1 March to 30 June 2007. The observed cluster concentrations varied and were from ca. 1000 to 100 000 cm−3. Both instruments showed similar concentrations. The average size of detected clusters was approximately 1.8 nm. As the atmospheric measurements at sub 2-nm particles and molecular clusters are a challenging task, and we were most likely unable to detect the smallest clusters, the reported concentrations are our best estimates for minimum cluster concentrations in boreal forest environment.
ucleation experiments starting from the reaction of OH radicals with SO2 have been performed in the IfT-LFT flow tube under atmospheric conditions at 293±0.5 K for a relative humidity of 13–61%. The presence of different additives (H2, CO, 1,3,5-trimethylbenzene) for adjusting the OH radical concentration and resulting OH levels in the range (4–300)·105 molecule cm−3 did not influence the nucleation process itself. The number of detected particles as well as the threshold H2SO4 concentration needed for nucleation was found to be strongly dependent on the counting efficiency of the used counting devices. High-sensitivity particle counters allowed the measurement of freshly nucleated particles with diameters down to about 1.5 nm. A parameterization of the experimental data was developed using power law equations for H2SO4 and H2O vapour. The exponent for H2SO4 from different measurement series was in the range of 1.7–2.1 being in good agreement with those arising from analysis of nucleation events in the atmosphere. For increasing relative humidity, an increase of the particle number was observed. The exponent for H2O vapour was found to be 3.1 representing a first estimate. Addition of 1.2·1011 molecule cm−3 or 1.2·1012 molecule cm−3 of NH3 (range of atmospheric NH3 peak concentrations) revealed that NH3 has a measureable, promoting effect on the nucleation rate under these conditions. The promoting effect was found to be more pronounced for relatively dry conditions. NH3 showed a contribution to particle growth. Adding the amine tert-butylamine instead of NH3, the enhancing impact for nucleation and particle growth appears to be stronger.
During a 4-week run in October–November 2006, a pilot experiment was performed at the CERN Proton Synchrotron in preparation for the CLOUD1 experiment, whose aim is to study the possible influence of cosmic rays on clouds. The purpose of the pilot experiment was firstly to carry out exploratory measurements of the effect of ionising particle radiation on aerosol formation from trace H2SO4 vapour and secondly to provide technical input for the CLOUD design. A total of 44 nucleation bursts were produced and recorded, with formation rates of particles above the 3 nm detection threshold of between 0.1 and 100 cm−3s−1, and growth rates between 2 and 37 nm h−1. The corresponding H2SO4 concentrations were typically around 106 cm−3 or less. The experimentally-measured formation rates and H2SO4 concentrations are comparable to those found in the atmosphere, supporting the idea that sulphuric acid is involved in the nucleation of atmospheric aerosols. However, sulphuric acid alone is not able to explain the observed rapid growth rates, which suggests the presence of additional trace vapours in the aerosol chamber, whose identity is unknown. By analysing the charged fraction, a few of the aerosol bursts appear to have a contribution from ion-induced nucleation and ion-ion recombination to form neutral clusters. Some indications were also found for the accelerator beam timing and intensity to influence the aerosol particle formation rate at the highest experimental SO2 concentrations of 6 ppb, although none was found at lower concentrations. Overall, the exploratory measurements provide suggestive evidence for ion-induced nucleation or ion-ion recombination as sources of aerosol particles. However in order to quantify the conditions under which ion processes become significant, improvements are needed in controlling the experimental variables and in the reproducibility of the experiments. Finally, concerning technical aspects, the most important lessons for the CLOUD design include the stringent requirement of internal cleanliness of the aerosol chamber, as well as maintenance of extremely stable temperatures (variations below 0.1°C).
River flow regimes, including long-term average flows, seasonality, low flows, high flows and other types of flow variability, play an important role for freshwater ecosystems. Thus, climate change affects freshwater ecosystems not only by increased temperatures but also by altered river flow regimes. However, with one exception, transferable quantitative relations between flow alterations and ecosystem responses have not yet been derived. While discharge decreases are generally considered to be detrimental for ecosystems, the effect of future discharge increases is unclear. As a first step towards a global-scale analysis of climate change impacts on freshwater ecosystems, we quantified the impact of climate change on five ecologically relevant river flow indicators, using the global water model WaterGAP 2.1g to simulate monthly time series of river discharge with a spatial resolution of 0.5 degrees. Four climate change scenarios based on two global climate modelsand two greenhouse gas emissions scenarios were evaluated.
We compared the impact of climate change by the 2050s to the impact of water withdrawals and dams on natural flow regimes that had occurred by 2002. Climate change was computed to alter seasonal flow regimes significantly (i.e. by more than 10%) on 90% of the global land area (excluding Greenland and Antarctica), as compared to only one quarter of the land area that had suffered from significant seasonal flow regime alterations due to dams and water withdrawals. Due to climate change, the timing of the maximum mean monthly river discharge will be shifted by at least one month on one third on the global land area, more often towards earlier months (mainly due to earlier snowmelt). Dams and withdrawals had caused comparable shifts on less than 5% of the land area only. Long-term average annual river discharge is predicted to significantly increase on one half of the land area, and to significantly decrease on one quarter. Dams and withdrawals had led to significant decreases on one sixth of the land area, and nowhere to increases.
Thus, by the 2050s, climate change will have impacted ecologically relevant river flow characteristics much more strongly than dams and water withdrawals have up to now. The only exception refers to the decrease of the statistical low flow Q90, with significant decreases both by past water withdrawals and future climate change on one quarter of the land area. Considering long-term average river discharge, only a few regions, including Spain, Italy, Iraq, Southern India, Western China, the Australian Murray Darling Basin and the High Plains Aquifer in the USA, all of them with extensive irrigation, are expected to be less affected by climate change than by past anthropogenic flow alterations. In some of these regions, climate change will exacerbate the discharge reduction. Emissions scenario B2 leads to only slightly reduced alterations of river flow regimes as compared to scenario A2 even though emissions are much smaller. The differences in alterations resulting from the two applied climate models are larger than those resulting from the two emissions scenarios. Based on general knowledge about ecosystem responses to flow alterations and data related to flow alterations by dams and water withdrawals, we expect that the computed climate change induced river flow alterations will impact freshwater ecosystems more strongly than past anthropogenic alterations.
Global-scale information on natural river flows and anthropogenic river flow alterations is required to identify areas where aqueous ecosystems are expected to be strongly degraded. Such information can support the identification of environmental flow guidelines and a sustainable water management that balances the water demands of humans and ecosystems. This study presents the first global assessment of the anthropogenic alteration of river flow regimes by water withdrawals and dams, focusing in particular on the change of flow variability. Six ecologically relevant flow indicators were quantified using an improved version of the global water model WaterGAP. WaterGAP simulated, with a spatial resolution of 0.5 degree, river discharge as affected by human water withdrawals and dams, as well as naturalized discharge without this type of human interference. Mainly due to irrigation, long-term average river discharge and statistical low flow Q90 (monthly river discharge that is exceeded in 9 out of 10 months) have decreased by more than 10% on one sixth and one quarter of the global land area (excluding Antarctica and Greenland), respectively. Q90 has increased significantly on only 5% of the land area, downstream of reservoirs. Due to both water withdrawals and dams, seasonal flow amplitude has decreased significantly on one sixth of the land area, while interannual variability has increased on one quarter of the land area mainly due to irrigation. It has decreased on only 8% of the land area, in areas with little consumptive water use that are downstream of dams. Areas most affected by anthropogenic river flow alterations are the western and central USA, Mexico, the western coast of South America, the Mediterranean rim, Southern Africa, the semi-arid and arid countries of the Near East and Western Asia, Pakistan and India, Northern China and the Australian Murray-Darling Basin, as well as some Arctic rivers. Due to a large number of uncertainties related e.g. to the estimation of water use and reservoir operation rules, the analysis is expected to provide only first estimates of river flow alterations that should be refined in the future.
Pollen-based climate reconstructions were performed on two high-resolution pollen – marines cores from the Alboran and Aegean Seas in order to unravel the climatic variability in the coastal settings of the Mediterranean region between 15 000 and 4000 cal yrs BP (the Lateglacial, and early to mid-Holocene). The quantitative climate reconstructions for the Alboran and Aegean Sea records focus mainly on the reconstruction of the seasonality changes (temperatures and precipitation), a crucial parameter in the Mediterranean region. This study is based on a multi-method approach comprising 3 methods: the Modern Analogues Technique (MAT), the recent Non-Metric Multidimensional Scaling/Generalized Additive Model method (NMDS/GAM) and Partial Least Squares regression (PLS). The climate signal inferred from this comparative approach confirms that cold and dry conditions prevailed in the Mediterranean region during the Heinrich event 1 and Younger Dryas periods, while temperate conditions prevailed during the Bølling/Allerød and the Holocene. Our records suggest a West/East gradient of decreasing precipitation across the Mediterranean region during the cooler Late-glacial and early Holocene periods, similar to present-day conditions. Winter precipitation was highest during warm intervals and lowest during cooling phases. Several short-lived cool intervals (i.e., Older Dryas, another oscillation after this one (GI-1c2), Gerzensee/Preboreal Oscillations, 8.2 ka event, Bond events) connected to the North Atlantic climate system are documented in the Alboran and Aegean Sea records indicating that the climate oscillations associated with the successive steps of the deglaciation in the North Atlantic area occurred in both the western and eastern Mediterranean regions. This observation confirms the presence of strong climatic linkages between the North Atlantic and Mediterranean regions.
Abrupt climate changes of the last deglaciation detected in a western Mediterranean forest record
(2009)
Abrupt changes in Western Mediterranean climate during the last deglaciation (20 to 6 cal ka BP) are detected in marine core MD95-2043 (Alboran Sea) through the investigation of high-resolution pollen data and pollen-based climate reconstructions by the modern analogue technique (MAT) for annual precipitation (Pann) and mean temperatures of the coldest and warmest months (MTCO and MTWA). Changes in temperate Mediterranean forest development and composition and MAT reconstructions indicate major climatic shifts with parallel temperature and precipitation changes at the onsets of Heinrich stadial 1 (equivalent to the Oldest Dryas), the Bölling-Allerød (BA), and the Younger Dryas (YD). Multi-centennial-scale oscillations in forest development occurred throughout the BA, YD, and early Holocene. Shifts in vegetation composition and (Pann reconstructions indicate that forest declines occurred during dry, and generally cool, episodes centred at 14.0, 13.3, 12.9, 11.8, 10.7, 10.1, 9.2, 8.3 and 7.4 cal ka BP. The forest record also suggests multiple, low-amplitude Preboreal (PB) climate oscillations, and a marked increase in moisture availability for forest development at the end of the PB at 10.6 cal ka BP. Dry atmospheric conditions in the Western Mediterranean occurred in phase with Lateglacial events of high-latitude cooling including GI-1d (Older Dryas), GI-1b (Intra-Allerød Cold Period) and GS-1 (YD), and during Holocene events associated with high-latitude cooling, meltwater pulses and N. Atlantic ice-rafting. A possible climatic mechanism for the recurrence of dry intervals and an opposed regional precipitation pattern with respect to Western-central Europe relates to the dynamics of the westerlies and the prevalence of atmospheric blocking highs. Comparison of radiocarbon and ice-core ages for well-defined climatic transitions in the forest record suggests possible enhancement of marine reservoir ages in the Alboran Sea by 200 years (surface water age 600 years) during the Lateglacial.
Die in diesem Aufsatz entfaltete Analyse der kurzen Passage aus Vitruvs Traktat (VI, praef., 1), die eine erbauliche Anekdote über schiffbrüchigen Philosophen Aristippus darstellt und dabei eine sinngeladene plastisch-symbolische Bildlichkeit in sich verhüllt, erlaubt festzustellen, dass ein die klassisch-antiken ästhetischen Äußerungen bestimmendes Prinzip der Statuarität auch dort seine entscheidende Rolle spielt.
Bibliotheken sind im Erwerbungsalltag mit einer Vielzahl unterschiedlichster Lizenzverträge für die Beschaffung von elektronischen Medien konfrontiert. Dabei nimmt die Komplexität durch das Anwachsen der Zahl der Marktteilnehmer aus Buchhandel und Agenturen, Verlagen und auch der verschiedenen Konsortien sowohl auf nationaler als auch auf internationaler Ebene wie durch die immer größer werdende Vielzahl der Produkte und Lizenzmodelle ständig zu. Die Transaktionskosten bei der Lizenzierung neuer Produkte, aber auch die Aktivitäten zur Verlängerung bestehender Lizenzverträge, steigen proportional mit der Zunahme der Bedeutung und Gewichtung, die elektronische Medienangebote einnehmen. Geschäftsgangmodelle, die ein Verfahren ohne Reibungsverluste garantieren, sind nicht vorhanden - wenn denn ein entsprechendes Problembewusstsein für die Bedeutung und den Wirkungsgrad bestimmter Lizenzvertragsklauseln existiert. Aufgrund der prinzipiell vorhandenen Vertragsfreiheit steht es den Partnern im Grunde frei, einen Vertrag entsprechend den Wünschen und Vorstellungen auszuhandeln. Dies wird in bestimmten Fällen von Vorteil sein, wenn es sich z.B. um Verträge von Konsortien mit Produkteanbietern handelt. Wie aber verhält es sich mit individuell abzuschließenden Lizenzverträgen einzelner Institutionen, z.B. beim Nachkauf von E-Books oder Ergänzungen von weiteren Datenbankprodukten des gleichen Anbieters. In vielen Fällen ist jedesmal ein Lizenzvertrag neu abzuschließen, wobei die minutiöse Lektüre aller Klauseln dringend angeraten sei. Hier würde sich anbieten, den Geschäftsverkehr der Vertragspartner zu vereinfachen, wenn nur schon die Vertragstexte soweit standardisiert wären, dass einheitliche Definitionen und Formulierungen für die einzelnen Regelungspunkte Verwendung fänden und lediglich Sonderabsprachen oder -vereinbarungen als Addenda beizufügen wären.
1996 und 1997 wurde die Spinnenfauna stehender abgestorbener Baumstämme in zwei Auenwäldern Südmährens (Tschechische Republik) untersucht. Einer der Standorte hatte ein naturnahes Überschwemmungsregime und wurde im Sommer 1997 von einem Sommerhochwasser überschwemmt. Die Spinnen wurden mittels Baumeklektoren gefangen. Von den 1714 gefangenen Individuen konnten 924 Adulti und 50 Jungtiere bis zur Art bestimmt werden. Dies ergab 82 Arten aus 17 Fami1ien. 13 Arten waren Erstnachweise für das erweiterte Biospharenreservat Palava, Tmarus stellio ein Erstnachweis für die Tschechische Republik und Midia midas für Mähren. Linyphiidae und Theridiidae waren die dominanten Familien sowohl bezüglich Individuen- als auch Artenzahl. Am überschwemmungsexponierten Standort wurden mehr Arten und Individuen gesammelt, insbesondere 1997 (mit höchsten Fangzahlen während des Sommerhochwassers: Oedothorax retusus stellte hier 97 % der Adulti in diesem Zeitraum). 35 Arten sind nach PLATEN et al. (1991) als obligatorisch bis fakultativ arborikol zu betrachten. Als weitere arborikole Arten sind Diaea livens, Midia midas, Philodromus praedatus, Pseudicius encarpatus, Theridion blackwalli und Tmarus stellio anzusehen. Auf einige besonders seltene Arten wird bezüglich Verbreitung und Lebensraum näher eingegangen.
Wolf spiders (Araneae: Lycosidae) on the overgrowing peat bog in Dubravica (north-western Croatia)
(2002)
The peat bog in Dubravica is of spread interest due to its overgrowing by the process of natural succession, causing the habitat to become dryer and shadier. The dominance structure and phenology of wolf spiders on the Dubravica bog was studied. The spiders were collected during the period 09.04.-9.10.1995, using 20 pitfall traps. Altogether 10 lycosid species were found among 723 adult individuals. For six more abundant species phenology graphs are presented. Three species are found to be eudominant: Pardosa lugubris, Trochosa spinipalpis and Hygrolycosa rubrofasciata. The lycosids habitat preferences and dominance structure according the habitat condition and species occurrences on some other European bogs are discussed. 55,2 % caught specimens are hygrophilous species, and only 7,6 % are photophilous. The lycosid fauna and dominance structure does reflect the habitat condition. As overgrowing is not fully progressed yet, the lycosid fauna of this bog is still relatively bog-characteristic.
Mit Hilfe von lnsektizidbenebelungen wurden die Spinnengemeinschaften von Eichen in Bayern (Deutschland) gesammelt und mit Gemeinschaften verglichen, in denen Formica polyctena-Ameisen numerisch dominierten. Von den mit Ameisen belaufenen Baumen wurden signifikant mehr Spinnen gesammelt und das Verhältnis von Adulten zu Juvenilen war zu den Juvenilen hin verschoben. Die Spinnengemeinschaften zeigten deutliche Unterschiede auf dem Niveau der Familien- und Artenzusammensetzung. Insbesondere wurden bei Anwesenheit von Ameisen mehr Clubioniden, Salticiden, Araneiden und Linyphiiden gesammelt. Dagegen wurden weniger Theridiiden (insbesondere Enoplognatha ovata) und Anyphaeniden auf den „Ameisenbäumen“ gefunden. Innerhalb der abundanz- und artenmäßig dominanten Linyphiiden wurde Linyphia triangularis in sehr viel höherer Anzahl aus den Bäumen mit Ameisen gesammelt.
Nach einigen Büchern zur chinesischen und japanischen Spinnenfauna ist aus dem ostasiatischen Raum nun ein Buch über Spinnen Koreas verfügbar. Obwohl wahrscheinlich nur wenige Europäer des Koreanischen mächtig sind, in dem das vorliegende Buch ausschließlich verfasst ist, soll eine kurze VorstelIung nicht versäumt werden.
Der stabil gebundene Band, gedruckt auf Hochglanzpapier im A5-Format, wirkt schon auf den ersten Blick recht ansprechend. Der Katalog umfasst ein riesiges Areal: Rußland vom Ural bis zum Pazifik, die Mongolei, beide Teile Koreas, sowie den Norden von Kasachstan, China und Japan (Hokkaido) - das Gebiet ist also in erster Linie geografisch definiert. Ein Blick auf einen Atlas/Globus zeigt, dass es (bis auf das flache sumpfige Westsibirien) in weiten Teilen Mittel- und vor allem Hochgebirgsareale enthalt. Dazu kommen natürlich noch Habitate an Küsten, Fluss- und Seeufem, Sümpfe, usw.
An anomaly of chaetotaxy of pedipalpal chela in Neobisium carcinoides (Arachnida: Pseudoscorpiones)
(2002)
Observations of anomalies in the trichobothrial pattern in pseudo scorpions are rare. Some aberrations in Neobisiidae have been described by CURCle (1992): irregular distribution of some trichobothria on both pedipalpal chelae although normal setal count is maintained; reduction in the number of trichobothria due to reduced size or some other anomaly of one or both pedipalpal chelae; and the occurrence of a supernumerary trichobothrium at a normal length of both pedipalpal chelae. One similar anomaly of chaetotaxy in Neobisium carcinoides (HERMANN, 1804) has been observed within our study of the pseudo-scorpion fauna in the Czech republic. The specimen was collected on the "Mrtvy luh" peat bog in the Sumava mountains (Bohemia or.), 740 m altitude, in October 1993 (leg. 1. BUCHAR).
Specimens of T. vulgaris were recently introduced in Germany with cricket boxes from southern United States. The species has been sent within Germany with post packages to different pet dealers. These samples represent probably the first confirmed records of T. vulgaris for Germany. Further observation could show, whether the populations are stabile in synanthropic habitats, especially inside buildings. Female genitalia are illustrated. One structure is recognized as a glandular part of the spermathecae. Terminology of female genitalia is given in comparison of terms used in the past by different authors.
Bei der ersten systematischen Aufnahme des Spinnenbestandes auf dem Trockenhügel "Pimpinellenberg" bei Oderberg, einem Refugium für viele xerotherme Wirbellose Ostbrandenburgs, gelangen Nachweise einiger Webspinnenarten, die eine gesonderte Mitteilung rechtfertigen. Sie haben überregionale Bedeutung, da sie wahrscheinlieh an bzw. nahe der Nordgrenze des Verbreitungsgebietes liegen.
In Deutschland kommen große aggregative Netze verschiedener Spinnenarten vor. Die Netze entstehen zufällig und bestehen wahrscheinlich aus den Sicherheitsfäden der einzelnen Individuen. Zwei Hauptursachen könnten für das Entstehen solcher Gewebe verantwortlich sein: 1. Das Ballooning Verhalten von Spinnen, die bei optimalen Bedingungen in Massen zu einer aeronautischen Verbreitung aufbrechen und so mit ihren einzelnen Sicherungsfaden Vegetationsstrukturen mit einem Gewebe überziehen können, und 2. Spinnen, die sich bei einer Störung in ihrem Habitat (z.B. das Fällen von Bäumen) aufmachen, um in höhere, früher bewohnte Straten zurück zu gelangen. Eine aktive Aggregation oder ein parasoziales Verhalten kann grundsätzlich nicht ausgeschlossen werden, scheint aber durch die vorliegenden Ergebnisse und Beobachtungen eher unwahrscheinlich. Detaillierte faunistisch-ökologische Untersuchungen von Baumwipfeln könnten zur Klärung dieses Phänomens beitragen. Eine Sammlung von Daten ähnlicher Fälle ist wünschenswert.
It has been widely accepted that the biology of Drapetisca socialis includes a pronounced stratum change of this species from the forest soil into the crowns of beech trees. On old pine trees, however, D. socialis never exceeded its activity range to heights greater than 10 metres. These results lead to an re-examination of existing results, and to a review of several studies on tree-dwelling spiders. A synopsis of all data revealed that D. socialis changes stratum along stems of trees into greater heights in forests, but only very seldom, and then obviously only by chance, reaches high tree crowns. Earlier results of a stratum change into the crowns of old beech are only assumptions. The requirement for studies including samples from the bottom to the top of trees is proposed.
Faunistische Untersuchungen an Spinnen wurden in den letzten Jahrzehnten überwiegend mit Barberfallen durchgeführt, da die Probennahme gut standardisierbar ist und vor allem unabhängig von der Witterung erfolgen kann. Die Kenntnisse über die Spinnenbesiedlung höherer Straten sind nach wie vor lückenhaft. Systematische Untersuchungen an Gebüschen mit Hilfe des Klopfschirms liegen nur von HARTMANN (1984) aus Oberfranken und von NAHRlG (1987) aus dem Kraichgau vor. In der vorliegenden Untersuchung wurde ein thermophiles Waldmantelgebüsch in Mittelfranken regelmassig beklopft. Um die Besiedlung unterschiedlicher Straten vergleichen zu können, wurde zusätzlich die epigäische Spinnenfauna des Waldmantels mit Barberfallen erfasst.
Die Arbeit von Oliver-D. FINCH gliedert sich in zwei große Bereiche: die zönologische und die parasitologische Erforschung der Spinnenfauna niedersächsischer Waldstandorte. Der Autor spielt dabei gekonnt mit unterschiedlichen Statistikmethoden, um dem Leser einen Lebensraum vorzustellen, der bisher nur unzureichend arachnologisch und parasitologisch bearbeitet ist. Er schafft dabei die Gratwanderung zwischen einer "trockenen" statistischen Arbeit und einem lesenswerten Buch, das dem Leser viele detaillierte Einblicke gewährt, ohne langatmig zu werden.
400 Millionen Jahre hatten die Spinnen Zeit, "formidable Biosensoren" zu entwickeln, so Barth in der Einleitung zum vorliegenden Buch. Er selbst nahm sich 30 Jahre Zeit, jene Sensoren sowie das Verhalten der Spinnen gründlich zu erforschen. Anfang diesen Jahres erschien das Buch, das den neuesten Stand aller Aspekte zu diesem Thema zusammenfasst. Vorweg, wer glaubt, dass es sich bei den untersuchten Objekten nur um eine Spinne - nämlich Cupiennius salei - handelt, wie im Titel angedeutet, liegt nur teilweise richtig, denn es werden immer wieder interessante Vergleiche zu anderen Spinnen- bzw. Insektengruppen gezogen. Zum anderen sei auch vorweggenommen, dass es Barth gelungen ist, eben nicht nur physiologische Details auf eindrucksvolle Weise zu präsentieren, sondern morphologische, verhaltensbiologische und andere Gesichtspunkte so einzuarbeiten, dass sich daraus ein Überaus lesenswertes und abgerundetes exemplarisches Gesamtbild einer Spinnenart ergibt.
On the distribution of Astrobunus laevipes CANESTRINI, 1872 (Arachnida: Opiliones) in Central Europe
(2001)
Published data and unpublished communications show that the range of Astrobunus laevipes in Central Europe is much larger than previously believed. The present review extends the list of records to the German states of Baden-Württemberg, Hessia, Rhineland Palatinate, Bavaria, Northrhine-Westfalia, Saxony, and Lower Saxony and provides a map of the present distribution in Germany. Furthermore, it lists new findings of A. laevipes in the Czech Republic and Hungary (Rakaca/Serehat Valley). Records of A. laevipes in Austria are not included in this review.
Im Folgenden möchte ich eine kleine Studie zum Beutespektrum unserer heimischen Pholcus-Arten und zur Arachnofauna in einem Wohnhaus im Frankenwald (Bayern) zum Besten geben. Während eines Aufenthalts bei meinen Schwiegereltern fielen mir bei der Benutzung der Toilette die auf dem Fußboden Iiegenden eingesponnenen Beutepakete der unter der Decke hängenden Zitterspinnen auf. Bei einer ersten Sichtung der in einem Schnappdeckelgläschen gesammelten Beutereste zeigte sich schon, dass ein großer Teil aus eingesponnenen Spinnen bestand. Nun ist ja bekannt, dass die einheimischen Pholcus Arten regelmäßig Spinnen, insbesondere aber die großen in Gebäuden lebenden Tegenaria-Arten erbeuten, die von mir eingesammelten Beutereste stammten jedoch zumindest teilweise offensichtlich von Individuen anderer Arten.