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Untersuchungsgebiet ist das heutige Bundesland Brandenburg. In diesem Raum werden von alters her germanische und slawische, seit dem Mittelalter a uch niederdeutsche (= plattdeutsche) und hochdeutsche Mundarten gesprochen. Mit der Industrialisierung im 19. Jahrhundert breitete sich die Stadtsprache Berlins als Umgangssprache auch in Brandenburg aus und trat vielerorts an die Stelle der alten Mundarten (= Dialekte). Dieser Vorgang dauert bis heute an. Das Forschungsprojekt soll seinen Stand Mitte der 90er Jahre erfassen und so Material für Vergleiche mit älteren und mit zukünftigen Erhebungen liefern. Untersuchungsmethode: Erhebung sprachlicher Daten und Ermittlung von Einstellungen zur Sprache mittels eines Fragebogens, der in einer Auflage von 8.000 Stück über Schulen, Pfarrämter, Heimatpfleger, freiwillige Helfer und Studierende der Universität Potsdam im ganzen Land Brandenburg verteilt wurde. Im Februar 1996 wurden zudem in ausgewählten Regionen insgesamt 20 Tonbandaufnahmen von Sprechern unterschiedlicher Mundarten und auch des Berlinischen als aktueller Umgangssprache aufgezeichnet. Erhebungszeitraum: Pilotstudie 1994, Erhebung 1995, Nacherhebung und Sprachaufnahmen 1996
Historisches Denken entwickeln am Gegenstand der altorientalischen,griechischen und römischen Antike, das ist Anliegen der didaktischen Handreichung für die gymnasiale Oberstufe. Didaktisch-methodische Überlegungen, Sachinformationen und ein handlungsorientierter Materialteil bieten für Lehrer und Schüler ein ideenreiches Angebot zur Auswahl für einen interessegeleiteten Geschichtsunterricht.
In order to predict which ecosystem functions are most at risk from biodiversity loss, meta-analyses have generalised results from biodiversity experiments over different sites and ecosystem types. In contrast, comparing the strength of biodiversity effects across a large number of ecosystem processes measured in a single experiment permits more direct comparisons. Here, we present an analysis of 418 separate measures of 38 ecosystem processes. Overall, 45 % of processes were significantly affected by plant species richness, suggesting that, while diversity affects a large number of processes not all respond to biodiversity. We therefore compared the strength of plant diversity effects between different categories of ecosystem processes, grouping processes according to the year of measurement, their biogeochemical cycle, trophic level and compartment (above- or belowground) and according to whether they were measures of biodiversity or other ecosystem processes, biotic or abiotic and static or dynamic. Overall, and for several individual processes, we found that biodiversity effects became stronger over time. Measures of the carbon cycle were also affected more strongly by plant species richness than were the measures associated with the nitrogen cycle. Further, we found greater plant species richness effects on measures of biodiversity than on other processes. The differential effects of plant diversity on the various types of ecosystem processes indicate that future research and political effort should shift from a general debate about whether biodiversity loss impairs ecosystem functions to focussing on the specific functions of interest and ways to preserve them individually or in combination.
Awards
(2013)
Supra-glacial deposition and flux of catastrophic rock-slope failure debris, south-central Alaska
(2013)
The ongoing debate over the effects of global environmental change on Earth's cryosphere calls for detailed knowledge about process rates and their variability in cold environments. In this context, appraisals of the coupling between glacier dynamics and para-glacial erosion rates in tectonically active mountains remain rare. We contribute to filling this knowledge gap and present an unprecedented regional-scale inventory of supra-glacial sediment flux and hillslope erosion rates inferred from an analysis of 123 large (> 0 center dot 1km2) catastrophic bedrock landslides that fell onto glaciers in the Chugach Mountains, Alaska, as documented by satellite images obtained between 1972 to 2008. Assuming these supra-glacial landslide deposits to be passive strain markers we infer minimum decadal-scale sediment yields of 190 to 7400tkm-2yr-1 for a given glacier-surface cross-section impacted by episodic rock-slope failure. These rates compare to reported fluvial sediment yields in many mountain rivers, but are an order of magnitude below the extreme sediment yields measured at the snouts of Alaskan glaciers, indicating that the bulk of debris discharged derives from en-glacial, sub-glacial or ice-proximal sources. We estimate an average minimum para-glacial erosion rate by large, episodic rock-slope failures at 0 center dot 5-0 center dot 7mmyr-1 in the Chugach Mountains over a 50-yr period, with earthquakes likely being responsible for up to 73% of this rate. Though ranking amongst the highest decadal landslide erosion rates for this size of study area worldwide, our inferred rates of hillslope erosion in the Chugach Mountains remain an order of magnitude below the pace of extremely rapid glacial sediment export and glacio-isostatic surface uplift previously reported from the region.