Das etwa 20 000 Jahre alte Pulvermaar in der Westeifel besitzt einen 72 m tiefen, zentral liegenden See und einen stellenweise mindestens 45 m mächtigen Tuffwall. Durch seinen außergewöhnlich guten Erhaltungszustand nimmt es eine Sonderstellung ein. Um auch den Tiefbau dieser Struktur besser kennenzulernen, wurden geophysikalische Messungen mit dem Ziel einer dreidimensionalen Modellierung durchgeführt. Über beides wird in dieser Arbeit berichtet. Den Schwerpunkt der geophysikalischen Untersuchungen bildet ein Gravimetrieprogramm mit der Erstellung einer Schwerekarte des Pulvermaars und seiner Umgebung. Im Rahmen dieser Schweremessungen hat der Einsatz des GPS-Systems zur Vermessung ein besonderes Gewicht. Die Magnetfeldmessungen der Totalintensität konzentrieren sich mit einem dichten Meßnetz auf den Seebereich (Messungen im Boot). Mit Widerstands-Tiefensondierungen der Geoelektrik wird versucht, zu einer präziseren Bestimmung der Tuffmächtigkeiten zu gelangen. Die gewonnene Schwerekarte dient einer dreidimensionalen Modellierung auf der Basis der Freiluftanomalie mit dem Programm IGMAS. Die verhältnismäßig kleine (negative) Schwere-anomalie von 1 - 2 mGal über dem Pulvermaar läßt vermuten, daß ein Basaltkörper in das Diatrem eingebettet ist und zur kleinen Amplitude beiträgt. Die Magnetfeldmessungen er-härten diese Vorstellung; das Ergebnis einer einfachen Modellierung für ein diametrales Profil ist mit einem 40 m mächtigen Basaltkörper grob 120 m unter Seeoberfläche ver-träglich. Die Ergebnisse der gravimetrischen und magnetischen Modellierung, die Mächtigkeitsab-schätzungen für die pyroklastischen Ablagerungen aufgrund der Geoelektrik-Messungen sowie die Einbeziehung einer Volumenkalkulation für die Pyroklastika führen zu einem detaillierten Modell für das Pulvermaar, das sich insbesondere durch ein 2000 m tief reichendes Diatrem auszeichnet. Eine Bearbeitung des Schwerefeldes mit der Berechnung von Gradientenfeldern führt zu einem bisher von Maaren nicht bekannten Ergebnis: Um das Pulvermaar herum existiert ein Hof erniedrigter Dichte mit einem Durchmesser von grob 2 km. Als Ursache wird eine Auf-lockerung des Gesteins durch Streß-Wellen angenommen, die ihren Ursprung in den wiederholten starken Eruptionen der Maar-Entstehung haben. Ebenfalls die Gradienten-felder der Gravimetrie zeigen Zusammenhänge zwischen der Struktur des Maares und der regionalen Tektonik auf. / The Pulvermaar is located in the Westeifel volcanic field. It is roughly 20000 years old and contains a 72 m deep, centrally situated maar lake as well as a partially at least 45 m thick tuff-rim. The Pulvermaar is very exceptional due to its good state of preservation. To learn more about the underground body of this structure, geophysical investigations were carried out aiming at a three-dimensional modeling. The core of the geophysical investigations represented a gravimetrical program in order to create a gravitational anomaly map of the Pulvermaar and its surroundings. The use of the GPS-system was of special importance for the gravimetrical measurements. The magnetic field measurements of the total intensity were mainly conducted in a fine pattern all over the lake-side (measurements on a boat). With the help of geoelectrical resistivity soundings one tried to precisely determine the thickness of the tuff deposits. The resulting gravity anomaly map serves a three-dimensional modeling based on free air anomaly with the software-program IGMAS. The relatively small (negative) gravitational anomaly of 1-2 mGal above the Pulvermaar leads to the assumption that a basaltic body is embedded in the diatreme and contributes to the small amplitude. The magnetic field measurements support this conception. The result of a simple modeling of a diametrical profile fits to a 40 m thick basaltic body located in about 120 m below the surface of the lake. The gravimetric and magnetic modeling, the estimation of the thickness of the pyroclastic deposits based on geoelectrical measurements, and the calculation of the volumina of the pyroclastic rocks lead to a detailled model for the Pulvermaar. This is espeacially characterized by a 2000 m deep diatreme. The processing of the gravity field by a calculation of its gradient fields leads to a result which is yet unknown for maarvolcanoes: the Pulvermaar is surrounded by a 2 km-diameter halo of reduced density. This can be explained by a relaxation of the rocks caused by stress-waves which originate from the repeatedly heavy eruptions during the formation of maarvolcanoe. Also, the gradients fields of the gravity show correlations between the structure of the maarvolcanoe and the regional tectonic.

The plant pathogen, Phytophthora dnnamomi, is a cause of dieback disease observed in sclerophyll vegetation in Australia, The effects of P. dnnamomi on flora and fauna were studied at two locations in heathland vegetation near the coastal town of Anglesea, Victoria. The pathogen was isolated from soils beneath diseased heathland plants. The extent of diseased vegetation was assessed by the presence and absence of highly sensitive indicator species, Xanthorrhoea australis and hopogon ceratophyllus. The characteristics of heathland vegetation exhibiting dieback disease associated with the presence of P. dnnamomi were investigated. Plant species richness was similar between diseased and non-diseased areas however diseased areas were characterised by significant declines in the cover and frequency of susceptible species, increases in resistant species and increases in percent cover of open ground. Compared to non-diseased areas, diseased areas exhibited fewer shrub species and decreased shrub cover. The percentage cover and number of species of sedges, lilies and grasses were higher in diseased areas. Structural differences were significant between 0-0.6 m with decreased cover of vegetation in diseased areas. Differences in structure between diseased and non-diseased areas were not as great as expected due to increases in the cover of resistant species. A number of regenerating X australis were observed in post-disease areas. Cluster analysis of floristic data could clearly separate diseased and non-diseased trap stations. The population dynamics and habitat use of eight small mammal species present were compared in diseased and non-diseased areas using trapping and radio-tracking techniques. The number of small mammal species captured in post-disease areas was significantly lower than non-diseased areas. Mean captures of Antechinus stuartii and Rattus fiisdpes were significantly lower in diseased areas on Grid B. Mean captures of Rattus lutreolus were significantly lower in diseased areas on both study grids. Significant differences were not observed in every season over the two year study period. Radio tracking revealed more observations of Sminthopsis leucopus in non-diseased vegetation than in diseased. Cercartetus nanus was frequently observed to utilise the disease susceptible X. australis for nesting. At one location, the recovery of vegetation and small mammal communities in non-diseased and diseased vegetation after fuel reduction burning was monitored for three years post-fire. Return of plant species after fire in both disease classes were similar, reaching 75% of pre-fire richness after three years. Vegetation cover was slower to return after fire in diseased areas. Of the seven small mammal species captured pre-fire, five were regularly captured in the three years after fire. General linear model analysis revealed a significant influence of disease on capture rates for total small mammals before fire and a significant influence of fire on capture rates for total small mammals after fire. After three years, the influence of fire on capture rates was reduced no significant difference was detected between disease classes. Measurements of microclimate indicate that diseased, burnt heathland was likely to experience greater extremes of temperature and wind speed. Seeding of diseased heathland with X. australis resulted in the establishment of seedlings of this sensitive species. The reported distributions of the mamma] species in Victoria were analysed to determine which species were associated with the reported distribution of dieback disease. Twenty-two species have more than 20% of their known distribution in diseased areas. Five of these species, Pseudomys novaehollandiae, Pseudomys fumeust Pseudomys shortridgei, Potorous longipes and Petrogale pencillata are rare or endangered in Victoria. Four of the twenty-two species, Sminthopsis leucopus, Isoodon obesulus, Cercartetus nanus and Rottus lutreolus am observed in Victorian heathlands. Phytophthora cinnamomi changes both the structure and floristics of heathland vegetation in the eastern Qtway Ranges. Small mammals respond to these changes through decreased utilisation of diseased heathland. The pathogen threatens the diversity of species present and future research efforts should be directed towards limiting its spread and rehabilitating diseased areas.

<p>Dispersal is an important factor in animal ecology. Anurans (frogs and toads) are often philopatric (home loving) but some specimens in a population usually have the capacity to disperse relatively long distances. In this study I investigated the colonization of newly constructed ponds in the southwest of Sweden by three anuran species: The common toad (Bufo bufo), the moor frog (Rana arvalis) and the common frog (Rana temporaria). The ponds were constructed between two and five years ago and were now as frequently occupied as older source ponds in the area. For the common toad and the common frog there was no correlation between distance to source populations and degree of colonization. The moor frog was more common in ponds that were situated in the vicinity of older source ponds with ample populations. The main impression was that these species rapidly colonize newly constructed ponds, at least within moderate distances from source populations. There were some differences between the species though and it seems like the moor frog have more limited dispersal abilities than the other two species.</p>

Dispersal is an important factor in animal ecology. Anurans (frogs and toads) are often philopatric (home loving) but some specimens in a population usually have the capacity to disperse relatively long distances. In this study I investigated the colonization of newly constructed ponds in the southwest of Sweden by three anuran species: The common toad (Bufo bufo), the moor frog (Rana arvalis) and the common frog (Rana temporaria). The ponds were constructed between two and five years ago and were now as frequently occupied as older source ponds in the area. For the common toad and the common frog there was no correlation between distance to source populations and degree of colonization. The moor frog was more common in ponds that were situated in the vicinity of older source ponds with ample populations. The main impression was that these species rapidly colonize newly constructed ponds, at least within moderate distances from source populations. There were some differences between the species though and it seems like the moor frog have more limited dispersal abilities than the other two species.

Growth rate is an important life history trait, which impacts fitness indirectly through its effect on the age and size at maturity, as well as directly through costs associated with accelerated growth such as increased predation risk. Genetic variation and plasticity in growth are widespread in nature, and local adaptation of growth rate may evolve due to divergent selection in different environments, for example related to predation risk, temperature or time constraints. I studied local adaptation of larval life history in the moor frog Rana arvalis, in a local network of ponds close to Uppsala. Local adaptation of growth rate and survival was studied in a reciprocal transplant experiment between ponds with different habitat characteristics. Meanwhile, differences among the populations in intrinsic growth, activity and response to predation were studied in a common garden experiment in the laboratory, where tadpoles were raised in the presence or absence of a predator and tested in direct predation trials. In the field, differences in growth among populations were found, independent of which pond the tadpoles were raised in, indicating that the ponds were similar growth environments. Survival differences among the populations depended on the pond, but local populations did not do better than foreign ones. In the laboratory, similar patterns in growth rate were found. All populations were highly plastic in their response to predation, having lower growth and activity in the predator-induced treatment and decreased mortality in the predation trials. Tadpole size was an important factor in escaping predation. One population clearly grew faster than the others in the field and in the lab, which could be explained in terms of its habitat of origin but was most likely related to the relatively late hatching of this population. Future studies are necessary concerning the possible costs of this accelerated growth and the importance of breeding phenology. Apart from the one differential population, I did not find evidence of local adaptation in the field or in the laboratory. The influence of habitat characteristics on tadpole life history was difficult to study, due to the limited number of ponds and many environmental differences among them. However, this thesis was a valuable pilot study concerning the design of experiments to study factors promoting and constraining local adaptation in landscape mosaics. An understanding of local adaptation at the scale at which gene flow occurs is important for the conservation of populations in fragmented landscapes as well as for the study of ecological speciation.

第18回名古屋大学年代測定総合研究センターシンポジウム平成17(2005)年度報告 Proceedings of the 18th symposiumon on Chronological Studies at the Nagoya University Center for Chronological Research in 2005 日時:平成18 (2006)年1月17日(火)､18日(水) 会場:名古屋大学シンポジオン Date:Januaryl7th and 18th, 2006 Venue:Nagoya Uhiversity Symposion Hall

The functional hydrological components of the ombrotrophic mire water balance are, considered in terms of their ecological relevance. It is proposed that numerical models provide a suitable framework for mire hydro-systems and their potential as quantitative tools for mire restoration and conservation management is demonstrated. Existing models previously applied to mires are reviewed. The USGS 3-D groundwater model MODFLOW is selected and a new shallow surface and groundwater model GSHAW5 is developed for application to mires. Extensive ecohydrological case studies are undertaken at two mire sites and the models are tested using data collected at the sites. Field studies at Wedholme Flow, Cumbria, extended over four years and the data collected were combined with historical records to form a 10-year hydrological data set. Studies at Trough End Bog, Northumbria, extended over a 3-year period. Topographic, soil and vegetation surveys were carried out at both sites. Watertable fluctuation was recorded manually on a weekly basis and electronically at a 20-minute interval along with automatic meteorological records. New hydrometric techniques were developed in the Surface Water Monitoring Plot, SWaMP, constructed at Trough End to record hydrological exchanges within the hummock-hollow complex of the mire acrotelm. The models operate on very different spatial and temporal scales. GSHAW5 is applied to reproduce ground and surface exchanges in the acrotel. MODFLOW is used to simulate large-scale exchanges in undisturbed areas and between regenerating and active peat cutting areas. Predictive MODFLOW simulations are used to examine the impact of different peat cutting regimes on mire hydrology and potential regeneration. Both models produce simulations strongly correlated to observed hydrological exchanges. The usefulness of numerical models as tools for mire management is considered in light of the model test results from both case studies. It is concluded that both models provide insight and quantitative estimates of hydrological exchanges not possible by other means. MODFLOW simulations reveal considerable water loss from the Wedholme Flow mire reserve to an active peat cutting area. Simulations of Trough End bog reveal hydrological acrotelm processes strongly related to vegetation assemblages. An extensified GSHAW5 acrotelm model is recommended for the simulation of intact ombrotrophic mires.

In Shakespeare’s Othello, Othello faces societal pressures of racism as he marries Senator Brabantio’s White daughter Desdemona. This creates the main plot, and the villain of the play, Iago, plots against him which leads to the destruction of Othello’s reputable character. Othello is transformed into a violent, murderous husband by Iago’s villainous ploy fueled by using racial slurs, and Othello’s final form matches the name his enemies assign him. Stripping Othello of his name and portraying him as “the Moor”, a term used to describe a category of Black persons viewed as barbaric, is a tactic used throughout time and is rooted in historical strategies for identity destruction and racism. The reader witnesses this tactic in a play written some 400 years in the past, but the problem still lingers in America where racism is commonly expressed through “Speech Acts”. Just a short time ago, Paul Robeson, a famous actor of Othello, faced these same problems while pursuing his spot on the stage. In consideration of today’s time, the movement “Say His Name” started following the death of George Floyd only two years ago, and this signifies the persistence of racism alongside the importance of names. Using slurs or refusing to use a person’s rightful name is a form of racial identity destruction witnessed from Shakespeare’s time, to Paul Robeson’s portrayal of the character, and into America’s now as the phrase “Say His Name” has become a staple in the fight against police brutality on Black persons in America.

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