225 resultados para Mecklenburg-Vorpommern


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Several geoscientific projects in the last decade led to a marked increase of radiocarbon dates in Mecklenburg-Vorpommern and in neighbouring areas. The studies were mostly focussed on the genesis of the Baltic Basin and the last termination. In this Paper, a regional collection of 271 radiocarbon dates of the late Pleistocene and early Holocene (ca. 50,000-8,000 14C yr BP) is presented. The dates were calibrated, correlate, and assessed with regard to their credibility. The evaluation of the data is focussed on problems of regional palaeogeography. The age of the last Weichselian deglaciation (deglaciation after the Mecklenburg Advance) is assumed to be around 14,000 14C yr BP through radiocarbon dates from the Pomeranian Bay. This data is ca. 1,000 years older compared to former views. On the other hand, the database allows the dating of late Pleistocene basin sequences from the Baltic coast, This indicates three stratigraphic units for basin areas 0-15 m above sea level - glaciolacustrine sedimentation in the late Pleniglacial, lacustrine and telmatic sedimentation as well as soil formation in the early Lateglacial and Alleroed and aeolian sedimentation in the Younger Dryas. The Younger Dryas in the huge Mecklenburg Bay-Darss Basin NE of Rostock is characterised by lacustrine sedimentation ca. 20 m below sea level ("Baltic Ice Lake"), and by aeolian sedimentation above sea level.

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A Late Pleistocene and Holocene sediment core from the nowadays terrestrialised portion of the Löddigsee in Southern Mecklenburg, Germany was palynologically investigated. The lake is situated in the rarely investigated Young moraine area at the transition from the Weichselian to the Saalian glaciation. The high-resolution pollen diagram contributes to the establishment of the north-eastern German Late Pleistocene pollen stratigraphy. The vegetation distribution pattern after the end of the Weichselian is in good agreement with other studies from North-eastern Germany, but also has its own characteristics. The Holocene vegetation development reveals features from the north-eastern and north-western German lowlands. A special focus was laid on the environmental history of the two settlements on an island within the lake (Late Neolithic and Younger Slavic period), which were preserved under moist conditions. Both settlements were constructed during a period of low lake level. Although there is evidence of agriculture in the area during the respective periods, the two island settlements seem to have served other purposes.

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Seit 1996 werden im Institut für Fischereitechnik (IFH) fangtechnische Untersuchungen zwecks Reduzierung des Beifangs bei der stark discardbelasteten Aalschleppnetzfischerei in der Ostsee durchgeführt. Diese Arbeiten wurden in Zusammenarbeit mit dem Institut für Fischerei der Landesforschungsanstalt für Landwirtschaft und Fischerei Mecklenburg-Vorpommern sowie dem Verein MARITEC e. V. durchgeführt (Gabriel und Thiele 1997; Gabriel et al. 1998). Nach Auswertung der bisher vorliegenden Ergebnisse und nach einer weiterführenden Beifanganalyse zur Schleppnetzfischerei auf Grundfischarten, insbesondere Plattfisch, in den Küstengewässern Mecklenburg-Vorpommerns wurden 1998 folgende technische Untersuchungen vorgesehen: • Überprüfung einer kombinierten Fischerei mit Plattfisch-Grundschleppnetzen und passiven Aalfanggeräten (Körbe, Langleinen, Korbketten) • Erprobung einer neuen Steertkonstruktion im Plattfischfang auf verbesserte Selektionseigenschaften • Blankaalfang mit einern pelagischen Tucknetz • Versuche in der passiven Fischerei mit verbesserten bzw. neuartigen Aalfanggeräten

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Berufswahlsentscheidung und die Frage nach dem Gehen oder Bleiben ist nicht nur für viele junge Menschen in ländlichen Regionen eine wichtige Frage, sondern auch für die im Übergang Schule-Beruf arbeitenden Menschen und Akteure der jeweiligen Kommune. Vor dem Hintergrund der Abwanderungstendenzen und der Optimierung der Übergänge Schule-Beruf hat die Stabsstelle Bildung des Landkreises Mecklenburgische Seenplatte repräsentativ 2800 Auszubildende des Landkreises befragt über die Einflussfaktoren für ihre Berufswahl und über ihre Entscheidung hier zu bleiben oder gehen befragt. Die z.T. überraschenden Ergebnisse werden in dieser Studie zusammen mit Handlungsempfehlungen dargestellt. (DIPF/Autor)

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We present descriptions of a new order (Ranunculo cortusifolii-Geranietalia reuteri and of a new alliance (Stachyo lusitanicae-Cheirolophion sempervirentis) for the herbaceous fringe communities of Macaronesia and of the southwestern Iberian Peninsula, respectively. A new alliance, the Polygalo mediterraneae-Bromion erecti (mesophilous post-cultural grasslands), was introduced for the Peninsular Italy. We further validate and typify the Armerietalia rumelicae (perennial grasslands supported by nutrient-poor on siliceous bedrocks at altitudes characterized by the submediterranean climate of central-southern Balkan Peninsula), the Securigero-Dasypyrion villosae (lawn and fallow-land tall-grass annual vegetation of Italy), and the Cirsio vallis-demoni-Nardion (acidophilous grasslands on siliceous substrates of the Southern Italy). Nomenclatural issues (validity, legitimacy, synonymy, formal corrections) have been discussed and clarified for the following names: Brachypodio-Brometalia, Bromo pannonici-Festucion csikhegyensis, Corynephoro-Plantaginion radicatae, Heleochloion, Hieracio-Plantaginion radicatae, Nardetea strictae, Nardetalia strictae, Nardo-Callunetea, Nardo-Galion saxatilis, Oligo-Bromion, Paspalo-Heleochloetalia, Plantagini-Corynephorion and Scorzoneret alia villosae. 

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Hintergrund und Ziel: Ausgehend von einem Forschungsdefizit im Bereich von Performance-Tests, das von der Arbeitsgruppe um Bührlen et al. (2002) gekennzeichnet wurde, war es das Ziel der Arbeit einen Performance-Tests of lower limb activities (Polla) zu validieren. Methode: In einer Längsschnittstudie wurden die Ergebnisse einer sechswöchigen physiotherapeutischen Behandlung an einem 19-75jährigem orthopädisch-traumatologisch orientierten Patientenkollektiv (n=81) mit dem Polla und dem SF-36 Fragebogen erfasst. Ergebnisse: Die Ergebnisse machen eine gute Absicherung der Teststatistik deutlich. Bei ausgezeichneter Intrarater- (n=29) sowie guter Interrater-Reliabilität (n=32) weist die Konsistenzanalyse eine zufrieden stellende Zuverlässigkeit auf. Die Kriteriumsvalidität macht moderate Zusammenhänge zwischen dem Polla und den Dimensionen Schmerz, Körperliche Rollenfunktion und Körperliche Funktionsfähigkeit des SF-36 deutlich. Über die Standardized Response Mean zeigen die Instrumente eine große Änderungssensitivität, die nur für den Polla auch zum Follow-up (n=26) gilt. Schlussfolgerung: Der Polla ist ein kostenloses Testverfahren mit hoher praktischer Relevanz, wobei aus zeitökonomischen Gründen eine modifizierte Form des Polla mit nur zehn Items und einem gemessenen Test zu empfehlen ist.

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La existencia de una red de diferentes niveles de gobernanza europea, que integre a los gobiernos locales, regionales y nacionales en el espectro supranacional, sumada al actual orden internacional globalizado, hace que algunas decisiones tomadas a nivel comunitario afecten directamente a los gobiernos que se encuentran por debajo del Estado Central. Como resultado, estos actores subnacionales han buscado la apertura de espacios para su participación en la construcción de la Unión Europea y en los procesos de toma de decisiones a escala supranacional, ya sea a través de sus gobiernos nacionales o realizando actividades internacionales no centrales. Éste es el caso de los gobiernos de Mecklemburgo-Pomerania Occidental (Mecklenburg Vorpommern), Land de la República Federal de Alemania, e Isla de Francia (Île-de-France), región de la República de Francia.

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A depression filled with Late Glacial and Holocene sediments was excavated during the geological exploration and recovery of a dump area near Tessin close to Rostock, and initiated the studies of the present paper. Pebble analysis of three exposed or respectively drilled till horizons as well as pollenanalytical, carpological and faunistical studies carried out allow the stratigraphical subdivision of the Quaternary sequence of the dump area. The basal till was probably the result of dead ice decay, and was lithostratigraphically assigned to the Pomerian Stage (qw2). The palynological results of boreholes RKS 19/93 and A/92 reveal pre-Allerod and other sediments instead of the expected interweichselian deposits. Based on the palynological and carpological findings, we correlated the beginning of the late glacial development in the locality with the end of the Meiendorf-lnterstadial sensu Menke in Bock et al. (1985, doi:10.3285/eg.35.1.18). The limnic-telmatic sedimentation could be observed pollen floristically probably starting with the Meiendorf-lnterstadial (Hippophae-Betula nana-phase) followed by the Bolling-(Betula nana-B. alba s.l.-Artemisia-Helianthemum-Poaceae-phase) and the Allerad-lnterstadial [Betula alba s.l.-(Pinus)-Cyperaceae-phase] lasting up to the Younger Dryas (Juniperus-Artemisia-Poaceae-phase). Sedimentation closed during the Younger Dryas with the accumulation of fine sands. It was reactivated later during the Holocene due to the anthropogene influence (Older and Younger Subatlantic, dampness of the depression by clearing).

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The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgression is indicated, which can be attributed to crustal movements. To determine the spatial and temporal differences since the onset of the Littorina Transgression, three relative sea-level curves have been established along a transect parallel to the gradient of upliftlsubsidence. The Wismar Bay area is one endpoint of the transect demonstrating today 10 Abb., 2 Tab. a relative sea-level rise of 1.4 mm/a. To determine the relative sea-level curve for the Wismar Bay, two sites were investigated on Rustwerder Spit (Poel) and Redentin. They provided reliable depth-age data, while the stratigraphy was additionally supported by lithological/geochemical, pollen, diatom and macrofossil data. Additional evidence was provided by archaeological submarine surveys and excavations. Comparing the new relative sea-level curve with a curve from the Vorpommern coast, it can be shown that for the period from 4000 cal BC until present, the differences between the two curves are caused by a constant neotectonic movement, while for the older periods an increasing isostatic component must be taken into account.