Seismic stratigraphy of the Blue Hole (Lighthouse Reef, Belize), a late Holocene climate and storm archive

Five seismic units may be identified in the similar to 8 m thick Holocene sediment package at the bottom of the Blue Hole, a 120 m deep sinkhole located in the atoll lagoon of Lighthouse Reef, Belize. These units may be correlated with the succession of an existing 5.85-m-long sediment core that reaches back to 1385 kyrs BP. The identification of seismic units is based on the fact that uniform, fine-grained background sediments show weak reflections while alternating background and coarser-grained event (storm) beds exhibit strong reflections in the seismic profiles. The main source of sediments is the marginal atoll reef and adjacent lagoon area to the east and north. Northeasterly winds and storms transport sediment into the Blue Hole, as seen in the eastward increase in sediment thickness, i.e., the eastward shallowing of the Blue Hole. Previous assumptions of much thicker Holocene sediment packages in the Blue Hole could not be confirmed. So far, close to 6-m-long cores were retrieved from the Blue Hole but the base of the sedimentary succession remains to be recovered. The nature of the basal sediments is unknown but mid-Holocene and possibly older, Pleistocene sinkhole deposits can be expected. The number of event beds identified in the Blue Hole (n = 37) during a 1.385 kyr-long period and the number of cyclones listed in historical databases suggest that only strong hurricanes (categories 4 and 5) left event beds in the Blue Hole sedimentary succession. Storm beds are numerous during 13-0.9 kyrs BP and 0.8-0.5 kyrs BP.

Der öffentliche Vertrieb von kollektiven Kapitalanlagen - Illustration am Beispiel des vertraglichen Anlagefonds

Der vorliegende Beitrag befasst sich mit der rechtlichen Analyse des im Recht der kollektiven Kapitalanlagen geregelten Fondsvertriebs aus aufsichts- und privatrechtlicher Sicht. Es werden dabei die Rahmenbedingungen des Vertriebs anhand der wichtigsten kollektiven Kapitalanlage, des vertraglichen Anlagefonds, aufgezeigt. Beim Direktvertrieb und beim Vertrieb durch Dritte besteht ein Geflecht von gewerbepolizeilichen Vorschriften und privatrechtlichen Normen, die von den involvierten Parteien beachtet werden müssen. Der Fokus des Beitrags liegt deshalb sowohl auf der gewerbepolizeilichen Aufsicht über die kollektiven Kapitalanlagen als auch auf den (vertraglichen) Rechtsbeziehungen zwischen den Anbietern von kollektiven Kapitalanlagen und deren Erfüllungsgehilfen einerseits und den Anlegern andererseits. Entsprechend der Behandlung des Themas in dieser Zeitschrift werden auch die Grundlagen der kollektiven Kapitalanlagen dargestellt.

Matrix pore water in low-permeable crystalline bedrock: An archive for the palaeohydrogeological evolution of the Olkiluoto Investigation Site

Matrix pore water in the connected inter- and intragranular pore space of low-permeable crystalline bedrock interacts with flowing fracture groundwater predominately by diffusion. Based on the slow exchange between the two water reservoirs, matrix pore water acts as an archive of past changes in fracture groundwater compositions and thus of the palaeohydrological history of a site. Matrix pore water of crystalline bedrock from the Olkiluoto investigation site (SW Finland) was characterised using the stable water isotopes (δ18O, δ2H), combined with the concentrations of dissolved chloride and bromide as natural tracers. The comparison of tracer concentrations in pore water and present-day fracture groundwater suggest for the pore water the presence of old, dilute meteoric water components that infiltrated into the fractures during various warm climate stages. These different meteoric components can be discerned based on the diffusion distance between the two reservoirs and be brought into context with the palaeohydrological evolution of the site.

Drivers of collaboration to mitigate climate change: An illustration of Swiss climate policy over 15 years

Climate change mitigation policy is driven by scientific knowledge and involves actors from the international, national and local decision-making levels. This multi-level and cross-sectoral context requires collaborative management when designing mitigation solutions over time and space. But collaboration in general policymaking settings, and particularly in the complex domain of climate mitigation, is not an easy task. This paper addresses the question of what drives collaboration among collective actors involved in climate mitigation policy. We wish to investigate whether common beliefs or power structures influence collaboration among actors. We adopt a longitudinal approach to grasp differences between the early and more advanced stages of mitigation policy design. We use survey data to investigate actors’ collaboration, beliefs and power, and apply a Stochastic Actor-oriented Model for network dynamics to three subsequent networks in Swiss climate policy between 1995 and 2012. Results show that common beliefs among actors, as well as formal power structures, have a higher impact on collaboration relations than perceived power structures. Furthermore, those effects hold true for decision-making about initial mitigation strategies, but less so for the implementation of those measures.

A global radiosonde and tracked balloon archive on 16 pressure levels (GRASP) back to 1905 – Part 1: Merging and interpolation to 00:00 and 12:00 GMT

Many observed time series of the global radiosonde or PILOT networks exist as fragments distributed over different archives. Identifying and merging these fragments can enhance their value for studies on the three-dimensional spatial structure of climate change. The Comprehensive Historical Upper-Air Network (CHUAN version 1.7), which was substantially extended in 2013, and the Integrated Global Radiosonde Archive (IGRA) are the most important collections of upper-air measurements taken before 1958. CHUAN (tracked) balloon data start in 1900, with higher numbers from the late 1920s onward, whereas IGRA data start in 1937. However, a substantial fraction of those measurements have not been taken at synoptic times (preferably 00:00 or 12:00 GMT) and on altitude levels instead of standard pressure levels. To make them comparable with more recent data, the records have been brought to synoptic times and standard pressure levels using state-of-the-art interpolation techniques, employing geopotential information from the National Oceanic and Atmospheric Administration (NOAA) 20th Century Reanalysis (NOAA 20CR). From 1958 onward the European Re-Analysis archives (ERA-40 and ERA-Interim) available at the European Centre for Medium-Range Weather Forecasts (ECMWF) are the main data sources. These are easier to use, but pilot data still have to be interpolated to standard pressure levels. Fractions of the same records distributed over different archives have been merged, if necessary, taking care that the data remain traceable back to their original sources. If possible, station IDs assigned by the World Meteorological Organization (WMO) have been allocated to the station records. For some records which have never been identified by a WMO ID, a local ID above 100 000 has been assigned. The merged data set contains 37 wind records longer than 70 years and 139 temperature records longer than 60 years. It can be seen as a useful basis for further data processing steps, most notably homogenization and gridding, after which it should be a valuable resource for climatological studies. Homogeneity adjustments for wind using the NOAA-20CR as a reference are described in Ramella Pralungo and Haimberger (2014). Reliable homogeneity adjustments for temperature beyond 1958 using a surface-data-only reanalysis such as NOAA-20CR as a reference have yet to be created. All the archives and metadata files are available in ASCII and netCDF format in the PANGAEA archive

Palaeoenvironmental changes in Central Europe (NE Poland) during the last 6200 years reconstructed from a high-resolution multi-proxy peat archive

Peat deposits from an ombrotrophic bog (north-eastern Poland) were analysed to reconstruct peatland development and environmental changes. This paper presents reconstructions of hydrological changes and plant succession over the last 6000 years. The methods included the high-resolution analysis of plant macrofossils, pollen and testate amoebae, supported by radiocarbon dating. Three main phases were identified in the history of the bog and surrounding woodland vegetation: 4000–400 BC, 400 BC–AD 1700 and AD 1700–2011. Except for terrestrialisation and the fen-to-bog transition phase, the development of bog vegetation was mainly dependent on the climate until approximately AD 1700. The dominant taxon in Gązwa bog was Sphagnum fuscum/rubellum. Woodland development was significantly affected by human activity at several time periods. The most visible human activity, manifested by the decline of deciduous species, occurred ca. 350 BC, ca. AD 250, ca. AD 1350 and after AD 1700. These events correspond to phases of human settlement in the area. During 400–300 BC, the decline of deciduous trees, primarily Carpinus, coincided with an increase in indicators of human activity and fire frequency. At ca. AD 200, Carpinus and Tilia abundance decreased, corresponding to an increased importance of cereals (Secale and Triticum). Since ca. AD 1350, the impact of Teutonic settlement is apparent, and after AD 1700, deciduous forests largely disappeared.

Shakespeare, the Middle Ages and the Luck of the British: Medievalism and National Identity in The Hollow Crown (2012)

Images of the medieval past have long been fertile soil for the identity politics of subsequent periods. Rather than “authentically” reproducing the Middle Ages, medievalism therefore usually tells us more about the concerns and ideological climate of its own time and place of origin. To dramatise the nascent nation, Shakespeare resorts to medievalism in his history plays. Centuries later, the BBC-produced television mini-serial The Hollow Crown – adapting Shakespeare’s second histories tetralogy – revamps this negotiation of national identity for the “Cultural Olympiad” in the run-up to the 2012 London Olympics. In this context of celebratory introspection, The Hollow Crown weaves a genealogical narrative consisting of the increasingly “glorious” medieval history depicted and “national” Shakespearean heritage in order to valorise 21st-century “Britishness”. Encouraging a reading of the histories as medieval history, the films construct an ostensibly inclusive, liberal-minded national identity grounded in this history. Moreover, medieval kingship is represented in distinctly sentimentalising and humanising terms, fostering emotional identification especially with the no longer ambivalent Hal/Henry V and making him an apt model for present-day British grandeur. However, the fact that the films in return marginalise female, Scottish, Irish and Welsh characters gives rise to doubts as to whether this vision of Shakespeare’s Middle Ages really is, as the producers claimed, “for everybody”.

Frauenbewegung - Die Schweiz seit 1968. Analysen, Dokumente, Archive

Sie kämpften nicht nur gegen die kapitalistische, sondern auch gegen die männlich dominierte Gesellschaft: Die Aktivistinnen der Frauenbewegung nach 1968. Diese verband die Suche nach einer anderen Gesellschaft mit neuen Auffassungen von Sexualität. Bestehende Machtverhältnisse wurden kritisch hinterfragt. Eine feministische Gegenkultur prägte sich aus, die sich als Gegenstück zur männlich dominierten Gesellschaft verstand. Basierend auf den Resultaten eines mehrjährigen Forschungsprojekts, bietet diese Überblicksdarstellung erstmals umfassend Einblick in Mobilisierung, Formen der Aktion sowie Kontroversen im feministischen Milieu von 1968 bis 2011. Neben Schlüsseldokumenten enthält der Band auch eine Übersicht über zentrale Quellenbestände in allen Landesteilen sowie eine umfassende Chronologie und Bibliografie.

Ein Update zur "Neuropsychotherapie" und Illustration aus der laufenden Forschung zum Einsatz emotionsfokussierter Vorgehensweisen

Während es fast trivial erscheint, dass erfolgreiche Psychotherapien – also Veränderungen im Erleben und Verhalten – prinzipiell mit funktionellen und strukturellen Veränderungen des Gehirns zusammenhängen, erweist es sich als deutlich anspruchsvoller, spezifischeren Fragestellungen nachzugehen und aus ihnen Implikationen für die Psychotherapie zu abzuleiten: Welche neuronalen Mechanismen sind an psychotherapeutisch relevanten Veränderungen im Erleben und Verhalten beteiligt? Wodurch werden diese neuronalen Wirkmechanismen beeinflusst? Und wie werden diese Erkenntnisse für die Psychotherapie praktisch nutzbar gemacht? Anhand aktueller Forschungsbefunde und konzeptueller Überlegungen in Anlehnung an Grawes “Neuropsychotherapie” wird in diesem Beitrag zu solchen und verwandten Fragen Stellung genommen. Eine laufende Studie an der Schnittstelle zwischen Psychotherapieprozessforschung und Neurowissenschaften illustriert, wie neuronale Wirkmechanismen erforscht und in bestehende psychologisch-psychotherapeutische Theorien eingebunden werden können. Untersucht werden hierbei die Effekte einer emotionsfokussierten Mikrointervention auf das subjektive emotionale Erleben und neurophysiologische Parameter. Solche neuronalen korrelate emotionaler Veränderungsprozesse werden vor dem theoretischen Hintergrund emotionsfokussierter und allgemeiner Psychotherapie interpretiert.