No description available.

Köln, University, Diss., 1998.

University, Diss., 2004--Heidelberg.

No description available.

No description available.

Brandenburgische Techn. Universiẗat, Diss., 2004--Cottbus.

Abstract not available

The present study investigated aspects of the biology of the cestode, Proteocephalus filicollis from the three-spined stickleback Gasterosteus aculeatus from Airthrey Loch, Scotland. The population biology study demonstrated that the parasite has an annual cycle of recruitment, which occur mostly in late summer and early autumn. The cestode did not show preference for any sex of the host. Maturation of the cestode also showed a seasonal cycle with the majority of worms maturing in late spring and early summer, but this period may be extended in different generations. Proteocephalus filicollis was overdispersed throughout the year in all sizes of fish, moreover variance to mean ratio always exceeded unity. No severe pathology was observed due to attachment of the worm to the intestine of the fish. The worm population in different sections of the intestine varied according to season and maturity stage. The P. filicollis migrate from the rectum to the anterior intestine as they mature and it is suggested that growth and maturation of the worm is a major stimulus for this migration. Proteocephalus filicollis has a high fecundity as indicated by the higher number of eggs per mm of gravid portion of the strobila and high fertility. Infrapopulation size did not show any relationship with length of worm, percentage gravid portion, number of gravid segments or mean length of gravid segments. Numbers of eggs are correlated to length of the worm, but not to infrapopulation size. Numbers of eggs per mm of the gravid portion are not correlated to length of worm or infrapopulation size. Acanthocyclops robustus was used as an experimental intermediate host. 15-16°C was the optimum experimental temperature for growth and a fully developed larva was formed in 23-27 days at this temperature. No growth was observed at 4°C, growth was slow at 10°C, but rapid at 21-22°C. The eggs are infective for 25 days at 4°C, 10°C and 15-16°C, but for only 15 days at 21-22°C. Prevalence and mortality of copepods are significantly correlated to their exposure time to parasite eggs, but mean intensity of infection did not show any relationship to the exposure time to the eggs. Ultrastructural studies demonstrated that a mature egg is surrounded by at least four embryonic envelopes, the capsule, the outer envelope, the inner envelope, and the oncospheral membrane. All these envelopes originate differently and undergo definite changes during their development.

No description available.

The Loch Lomond Advance limits and raised marine shorelines in N. W. Argyll have been mapped and surveyed. Radiocarbon dated Lateglacial and Postglacial pollen sites at Salen and Loch Shiel provide the vegetational history and chronology for the area. 14 Loch Lomond Advance glacier termini and associated limits were mapped using the distribution of hummocky and fluted moraine, together with a survey of erratic boulders. 83% of the reconstructed former glaciers had a southerly aspect relating to southerly snow-bearing winds. The average firnline gradient was 7.5m/km increasing in altitude towards the north-east; the average firnline height for the area was 369m. The Main Lateglacial Shoreline, formed during the Loch Lomond Stadial, slopes towards 270 with a gradient of 0.15m/km from 9m in the east to Om in the west of the area. It was formed by freeze-thaw action operating under exceptional conditions, and its formation was influenced by rock type. Two Postglacial shorelines are recognized : the Main Postglacial shoreline that slopes towards 270, from 14m to 8m with a gradient of 0.06m/km, and a lower shoreline at approximately 5m which has no definite gradient. An absolute Lateglacial pollen site at Salen, Ardnamurchan, shows an early pioneer community of Rumex, Salix, Gramineae and Cyperaceae species being replaced by an Empetrum heath during the Lateglacial Interstadial. Subsequent stadial conditions are reflected by open herb communities and the onset of coarse minerogenic sedimentation. This minerogenic influx ceased around 10,000 to 9,700 B.P. with a rapid recolonization of the surrounding area by pioneer herbs, then dwarf shrub and finally deciduous woodland. Middle and Late Postglacial vegetational development is recorded by lacustrine sediments from Loch Shiel where the fossil pollen record shows that a mixed deciduous woodland of Quercus, Alnus, Betula and Corylus was progressively cleared by man. Palaeomagnetic and chemical records were obtained from the site. The Main Postglacial Transgression flooded Loch Shiel resulting in the deposition of shells of the marine bivlave Thyasira flexonosa.