Avaliação das condições bióticas e abióticas em um viveiro neotropical impactado

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

HIV-assoziierte Neuritis des Nervus vestibulocochlearis. Fallbeschreibung und systematische Literaturanalyse der HIV-assoziierten Polyneuropathien

Die Polyneuropathien sind Komplikationen der Infektion mit dem Human- Immunodeficiency-Virus (HIV). Dazu gehören Polyradikulopathien, distale (sensible) Polyneuropathien, Mono- und Oligoneuropathien und brachiale Neuritiden. Selten gibt es Formen, die sich nicht kategorisieren lassen. In dieser Dissertation präsentieren wir einen aussergewöhnlichen Fall einer bilateralen Neuritis des Nervus vestibulo-cochlearis (N. vestibulocochlearis). In einer ausgedehnten Literaturrecherche ist das erst der dritte beschriebene Fall. Gleichzeitig wurde die Literaturrecherche genutzt, um epidemiologische, klinische und laborchemische Parameter der HIV-assoziierten Polyneuropathien zu analysieren. Dazu wurden Daten von 539 Patientinnen aus 67 Publikationen extrahiert und ausgewertet. Die Daten wurden bezüglich ihrer Qualität gewertet, um den Schlussfolgerungen eine Gewichtung zu geben. Die Literaturanalyse ergab, dass die meisten Daten zu HIVassoziierten – und bezüglich antiretroviraler Therapie (ART) naiven – Polyneuropathien von afrikanischen Patienten stammen. Die meisten europäischen und nordamerikanischen Studien zu diesem Thema wurden vor 1996 publiziert. Polyradikulopathien präsentieren sich typischerweise früh und distale (sensible) Polyneuropathien spät in der HIV-Krankheit. Das Guillain-Barré-Syndrom war das häufigste Krankheitsbild der Polyradikulopathien. Die häufigste Präsentation distaler Polyneuropathien sind Sensibilitätsausfälle an den unteren Extremitäten. Bei den Mono- und Oligoneuropathien hat ein Grossteil der Personen Mononeuropathien, wobei der N. facialis am häufigsten betroffen ist. Die Rolle der ART zur Erholung der Neuropathien konnte nicht beurteilt werden. Unter den HIV-assoziierten Polyneuropathien haben die distalen (sensiblen) Polyneuropathien die schlechtere und die Polyradikulopathien und Mono- oder Oligoneuropathien die bessere Prognose bezüglich Erholung

Abundance and biomass of zooplankton from 1986-1994 collected in front of Constanta city, Black Sea

The Est Constanta 1986-1994 dataset contains zooplankton data collected allong a 5 station transect in front of the city Constanta (44°10'N, 28°41.5'E - EC1; 44°10'N, 28°47'E - EC2; 44°10'N, 28°54'E - EC3; 44°10'N, 29°08'E - EC4; 44°10'N, 29°22'E - EC5). Zooplankton sampling was undertaken at 5 stations where samples were collected using a Juday closing net in the 0-10, 10-25, 25-50m layer (depending also on the water masses). The dataset includes samples analysed for mesozooplankton species composition and abundance. Sampling volume was estimated by multiplying the mouth area with the wire length. Taxon-specific mesozooplankton abundance was count under microscope. Total abundance is the sum of the counted individuals. Total biomass Fodder, Rotifera , Ctenophora and Noctiluca was estimated using a tabel with wet weight for each species an stage.

Pollen profiles from 8 sediment cores from the Degersee, Southern Germany

The discovery of a neolithic pile field in the shallow water near the eastern shore of the Degersee confirmed earlier palynological and sedimentological studies stating that early man was active in the region since more than 6000 years. The already available off-site data were freshly assessed, completed by additional data from old and new cores and the interpretations revised. A common time scale for the off-site data and the on-site data was obtained by AMS dating of terrestrial macro remains of the neolithic section of off-site core De_I+De_H. The ages can thus be parallelled with AMS ages of construction timber on-site. Pollen analyses from all cores provide a further time scale. The continuously and densely sampled pollen profile of the profundal zone embracing the entire Late glacial and Holocene serves as a reference. From the Boreal onwards the relative ages are transformed by AMS ages and varve counts into calibrated and absolute. A transect cored close to the neolithic pile field across the lake marl-platform demonstrates its geological architecture in the shallow water since the Lateglacial. Studies of the microfabric of thin sections of drilled cores and of box cores from the excavations demonstrate that neolithic settlements now at 2-3,5 m water depth had been erected on lake marl freshly fallen dry, thus indicating earlier lake levels dropped by 1.5-2 m. The neolithic section of the highly resolved off-site profile in the lake=s profundal zone has laminated and calcareous zones alternating with massive ones. Assemblages of diatoms and concentrations of trace elements changing simultaneously characterise the calcareous sections as deposits of low lake levels that lasted between some 40 and more than 300 years. The ages of discovered lake shore dwellings fall into calcareous segments with low lake levels. From the end of the Upper Atlantic period (F VII) appear Secondary Forest Cycles in the beech forest, a man-made sequence of repeated vegetational development with an identical pattern: With a decrease of beech pollen appear pollen of grasses, herbs and cultural indicators. These are suppressed by the light demanding hazel and birch, those again by ash, and finally by the shade demanding beech forming a new pollen peak. Seven main Forest Cycles are identified In the upper Neolithic period each comprising some 250, 450 or 800 years. They are subdivided into subcycles that can be broken down by very dense sampling in even shorter cycles of decadal length. Farming settlers have caused minor patchy clearances of the beech-mixed-forest with the use of fire. The phases of clearance coincide with peaks of charcoal and low stands of the lake levels. The Secondary Forest Cycles and the continuous occurrence of charcoal prove a continued occupation of the region. Together with the repeated restoration of the beech climax forest they point to pulsating occupation probably associated with dynamic demography. The synchronism of the many palynological, sedimentological and archaeological data point to an external forcing as the climate that affects comprehensively all these proxies. The fluctuations of the activity of the sun as manifested in the residual d14C go largely along with the proxies. The initial clearances at the begin of the forest cycles are linked to low lake levels and negative values of d14C that point to dry and warm phases of a more continental climate type. The subcycles exist independent from climatic changes, indicating that early man acted largely independent from external forces.

Pollen record from Blankensee, Germany

Lake Blankensee is filled with 14 m of late- and postglacial deposits, Lake Siethener See with 22,5 m. The lacustrine sedimentation begins in Lake Siethener See in the middle of the Alleröd with annual lamination which partly continues in the Younger Dryas. A 2 cm thick layer of the Laacher See tephra was found in both lakes, the Saksunarvatn tephra only in Lake Siethener See where the cool Rammelbeek-phase (Preboreal) could be shown. The youngest part of the sediment profiles is suspended drifting mud. Masses of Pediastrum (algae) indicate an increasing shoaling of Lake Blankensee after the Subboreal.

Pollen record from Muggesfelder See and Plussee in Germany

A basaltic tephra layer consisting of brownish-olive glass shards. and about 0.2 mm thick. was found in cores from four lakes in northwest Germany. According to pollen analysis it was deposited during the early Boreal period (corresponding to about 8700 BP). The petrographic properties. the geochemical composition and the age agree with those of the Saksunarvatn tephra. which was first found on the Faroe Islands. The position of the tephra layer in the pollen stratigraphy and in the absolute time-scale is discussed. Procedures for locating the tephra in other cores are suggested.