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Oligochaetes constituted 91-98% of the numbers and 78-97% of the biomass of the macrofauna, the remaining part were Chironomidae, while Chaoboridae, Sphaeridae, Ephemeroptera, and Coleoptera occurred sporadically. The highest density (14.5 thous. indiv. m-2) and biomass (13 g m-2) were observed near the dam. 14 species of the Oligochaetes (the most numerous being Potamothrix hammoniensis, Limnodrilus claparedeanus, and L. hoffmeisteri) and 5 taxa of Chironomidae were determined in the samples.
The majority of oligochaete species living in springs are ubiquitous and widely distributed taxa but cold stenothermic, semiaquatic and rare ones are also found. In Poland about 50 species are known from springs among 185 aquatic and semi-aquatic species found in whole country. Gianius aquaedulcis (Hrabĕ 1960) (Tubificidae, Phallodrilinae) is reported for the first time from Poland from two karstic springs situated in Kraków – Częstochowa Upland (South Poland). Both springs are hillside, fissure, descending, rheocrenes, with discharge about 30– 40 L s⁻¹. Spring no 1 is situated in banked pond, spring no 2 has natural character. Their bottom is sandy or sandy-gravely, with patches of detritus, mud and plants. The conductivity, concentration of main cations (Ca, Mg) and anions (Cl, SO₄) were typical for spring waters of this limestone area; only concentration of nitrate is slightly elevated. The samples of bottom fauna (a polyethylene corer and a bottom scraper) and water for chemical analysis were taken seasonally. This species was more numerous in a banked spring than in the natural one (maximal density about 1600 ind. m⁻²) and seasonal changes of its density were similar in both springs. Mature specimens formed only 5–8% of the population and were present in all sampling data. G. aquaedulcis is known from a few localities only (Germany, France, Spain and USA). It lives in underground and surface waters, with slightly alkaline pH on sandy or stony bottom. Maybe this species forms a few relictic populations which persist in subterranean (cave or hyporheic) waters of some geographic regions at least since the last glacial epoch. The existence of small anatomical differences (for example various thickness of the muscular lining of the atria and changeable shape of penial setae) among the studied populations from various countries seems to confirm this hypothesis.
The highest density of macrofauna was recorded in a muddy habitat, and the highest biomass (d.w.) in a stony one. Only Naididae, Hydracarina, young larvae of Trichoptera, and large specimens of Gammarus spp. preferred a transitional habitat (mud-covered stones). Of the 25 identified species of Oligochaeta especially three dominant species (Nais bretscheri, N. pardalis, and N. communis) were most numerous in the transitional habitat. Downstream the species diversity of Oligochaeta increased and the composition of the community changed.
Studies were performed on 25 karstic springs located in Southern Poland (50º10’ – 50º46’ N, 19º17’ – 19º54’E). They are natural or encased, differing also in discharge rate (0.01– 15 l s⁻¹ in the southern part of KrakówCzęstochowa Upland while 20 – 1440 l s⁻¹ in its northern part) and kind of bottom sediments (fine or coarse). 27 species and 1 genus representing 5 families were determined, among them Enchytraeidae were represented by the highest number of species whereas Tubificidae (mainly juvenile forms) were the most abundant. Among oligochaetes no crenobionts were found while crenophiles: Rhyacodrilus falciformis Bretscher and Stylodrilus heringianus Claparède were present in a half of the studied springs. In the majority of the studied springs the density of oligochaetes was significantly higher in fine sediments (ranges 200 – 13 200 ind. m⁻²) than in coarse ones (ranges 22–7900 ind. m⁻²) (P <0.05). The species diversity (H’) was also higher in fine sediments, especially in springs of the southern part of Upland. Oligochaeta were more abundant and diversified in encased springs than in natural ones and they inhabited preferably fine sediments. The discharge and springs localization (in southern or northern part of the studied area) were found to be not of importance for oligochaete composition and abundance.
Zooseston of the Vistula River section almost 340 km long was investigated in the years 1997/98. In 99 samples collected 90 species of rotifers, 16 cladocerans, 9 copepods and other animals belonging to: Harpacticoidea, Oligochaeta, Nematoda, Chironomidae, Odonata, Simulidae, Tardigrada and Coelenterata were found. Multiple regression analysis showed that the number of rotifers is significantly correlated with basic chemical indicators of water trophic state - phosphate, nitrate and nitrite as well as with the number of copepods which are usually predators. The numbers of copepods depends on the availability of possible prey, i.e. rotifers and cladocerans. Multiple regression confirmed known dependence of cladocerans from trophic conditions. Clustering of similarity matrices showed complex structure of sestonic assemblages on rhitral-potamal gradient additionally modified by hydrotechnical constructions. These constructions broke old river continuum. Ordination of sites gave complex pattern not only representing a simple gradient rithral - potamal but also all transient stages caused by hydrotechnical construction (large dam reservoir) or by inflows of polluted waters from the tributaries. Ecological meaning of principal component ordination (PC) for river zooseston assemblages is not simple and might be susceptible of various interpretations.
W badanych jaskiniach skład fauny naściennej różnił się nieco, co prawdopodobnie spowodowane było drobnymi różnicami mikroklimatycznymi (temperatura, wilgotność i przepływ powietrza) między jaskiniami. Skład fauny osadów obu jaskiń był podobny, natomiast wyraźne zmniejszenie i wahania liczebności bezkręgowców w Jaskini Towarnej były skutkiem antropopresji. W obu obiektach stwierdzono utrzymywanie się populacji troglobiontycznego chrząszcza Speonomus hydrophilus – introdukowanego do Jaskini Dzwonnica ponad 30 lat temu z jaskiń Pirenejów
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