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Qualitative observations of owls were carried out in the Polish Tatra Mts, S Poland in the years 1998-2003. The following six species were recorded: Eagle Owl, Tawny Owl, Ural Owl, Pygmy Owl, Tengmalm’s Owl and Long-eared Owl. The distribution of particular owl species in the Tatra Mts is clearly associated with changes in the habitat according to the altitude. Records of the Tawny Owl predominate in the lower montane zone, those of Tengmalm’s Owl in the upper montane zone, and of Long-eared Owl at higher altitudes (timberline and above).
This paper reports a study of the visitation of bats to Great Litworowa Cave (1,907 m a.s.l., Tatra Mts., southern Poland) during summer and autumn 1999–2005. A total 5,608 bats representing 11 of Poland's 25 species were captured. Myotis mystacinus predominated. Its activity at all times was high. However, the species composition and number of other bats changed seasonally. Swarming activity lasted between July and November, peaking in late July and August. Nightly activity peaked between 22.00 and 02.00 hrs and then gradually decreased toward dawn. Strong male bias was observed. Myotis mystacinus showed regular changes in sex and age ratios. Rare species such as M. bechsteinii, M. emarginatus, and Vespertilio murinus were recorded. This cave is the highest locality of M. bechsteinii and M. brandtii in Europe. Some behavioural observations including copulation, drinking and daylight activity were recorded. The role of swarming activity is discussed in light of the findings. Some observations suggest that this activity of bats is connected with mating; some other observations provide evidence that the function of swarming is also to facilitate the location of mates and/or to assess suitable hibernacula.
A new stand of H. pilosum, a species not reported before from the territory of Poland, was found in the Polish Western Tatra Mts. It grows in numerous stands on limestone rocks on the slopes of Upłaziańska Kopka, at ca. 1400 m a.s.l. Moreover, typical form of this species, collected in the Polish Western Tatra Mts, was also found in herbaria of KRA and KRAM. These data indicate that H. pilosum is a widespread species in the described region but it was unrecognized from H. villosum so far.
The results of faunistic studies on Orthoptera fauna of the Tatra Mountains and the Podhale region in Poland are presented. The material of Orthoptera collected in 2008 and 2009 contained 24 species. The review of the material from the earlier collections stored in MIZ PAS in Warsaw and ISEA PAS in Cracow as well as the field notes made in the 1950's and 1960's by Polish entomologist Władysław Bazy luk, showed that 32 Orthoptera species were noted in total from the study regions. Comparison of data collected at different times spanning more than a century shows the dynamics of change in the Polish part of theTatra National Park fauna.
This paper is a review of fundamental information on bark beetles and their interactions with several predisposing factors (air pollution, drought/temperature interactions, windthrows, management activities) that are thought to contribute to the outbreaks in the High Tatra Mountains. The findings of many research projects indicate that the impact of air pollution on bark beetle populations is indirect and complex and that the disturbances in the physiology and natural resistance of trees may be of crucial importance to bark beetle population dynamics. An active forest protection approach is needed to be applied to the secondary Norway spruce forests affected in the past by human activity. Bark beetle populations in natural and near-natural forests (mainly in the upper montane zone) are regulated by natural mechanisms; bark beetles are therefore a natural factor contributing to forest development, including the transition of future generations of spruce.
The article describes the research into the impact of deforestation on the values of physicochemical traits and chemical composition of waters which drain the catchments covered with forest, and those that have been deforested, in the western part of Polish Carpathians. The research was carried out in independent catchments in the Skrzyczne massif in the Beski Śląski (Silesian Beskidy Range) in 2013–2014, and in the Kościeliska Valley in the Western Tatras in 2015–2016. During field studies, water samples were collected monthly in catchments with various degrees of deforestation, and the physicochemical characteristics of water were measured (pH, PEW, Tw). In the laboratory, the chemical composition of water, specifically the content of 14 ions (Ca²⁺, Mg²⁺, Na⁺, K⁺, NH₄⁺, Li⁺, HCO₃⁻ , SO₄²⁻, Cl⁻, NO2 ⁻, NO₃⁻ , PO₄³⁻ , Br⁻, F⁻), was determined by means of ion chromatography (DIONEX 2000). The conducted research has shown the impact of deforestation on the value of physical and chemical traits and chemical composition of water. Deforestation of the slopes caused changes in the structure of the chemical composition of water, especially in the area of correlations between anions. In the Tatras, in the basins deforested as a result of windfall, a significant increase in the proportion of NO₃⁻ (% mval ∙ dm⁻³) in the anionic element of the chemical composition of water was observed, and in the Beskid Śląski, in catchments deforested due to the tree stand decay associated with the imission of pollutants, a significant increase in SO₄²⁻ (% mval ∙ dm⁻³) and a significant decrease in HCO₃⁻ (% mval ∙ dm⁻³) in the anionic structure of the chemical composition of waters was observed. These examples document the extremely important role played by forests, which cover mountain slopes, in the hydrochemical functioning of the catchment. In the spatial aspect, there is an unusual phenomenon of hydrochemical mosaicism consisting in the occurrence of different relationships between anions, especially hydrogen carbonates, sulphates and nitrates.
We report cyrtocrinid (Crinoidea) ossicles from the Rhaetian (Late Triassic) of the Tatra Mountains (southern Poland). The columnals are high, the facets are covered with thick crenulae and the latera are concave. Such features of symplectial articulation and latera distinguish them from the columnals of other Triassic crinoids (i.e., millericrinids and encrinids) and therefore we consider they belong to Cyrtocrinida. The oldest representatives of cyrtocrinids were known from the Early Jurassic, therefore the presented material constitutes the oldest world record of these crinoids to date. We speculate that perturbations related to the global mid−Carnian extinction combined with predation intensity observed in the Middle– Late Triassic have been involved in early origin of Cyrtocrinida.
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