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    Tytuł:
    Acritarch assemblages from the Silurian Pomeranian Caledonides and their foreland
    Autorzy:
    Jachowicz, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059448.pdf
    Data publikacji:
    2000
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Pomeranian Caledonides
    Silurian
    acritarch assemblages
    Opis:
    Comprehensive palynological studies of the Silurian rocks of the Pomeranian Caledonides are described, the first since Eisenack's (1972) work. 250 clastic rock samples were analysed, all from deep boreholes. Three of these boreholes (Lębork IG 1, Gdańsk IG 1 and Kościerzyna IG 1) are located NE of the Teisseyre-Tornquist Zone (TTZ) and contain horizontal successions of the western, marginal part of the East European Craton. Other boreholes studied (Bydgoszcz IG 1, Klosnowo IG 1 and Stobno 1) penetrated folded Lower Palaeozoic sediments, and lie SE of the TTZ. The investigations included a complete Silurian profile from the Llandovery to the Poidoli, which is documented in detail by graptolites. Associations of microflora (Acritarcha, Prasinophyceae, Sporites) and microfauna (Chitinozoa, Scolecodonta) varied in quality and quantity. There was considerable variability in the preservation and thermal maturity of the organic-walled microfossils. Detailed investigations of the acritarchs are described. 7 characteristic acritarch assemblages have been distinguished, and these are correlated with the graptolite biozones. Llandovery rocks contain assemblages with Domasia, Ammonidium and Tylotopalla genera. Wenlock deposits include Tylotopalla, Leptobrachion and Cymbosphaeridium. The Upper Ludlow deposits contain well preserved assemblages with Visbysphaera, Veryhachium, Onondagella and Leoniella, accompanied by Neoveryhachium carminae, Geron gracilis, and some Deflandrastrum and Visbysphaera species generally considered characteristic of Gondwana. Throughout the Silurian profile, individual specimens of typical Ordovician genera such as Acanthodiacrodium, Frankea, Striatotheca and Coryphidium occur. The acritarch assemblages overall show mixed characters, typical of both Baltica and Gondwana.
    Źródło:
    Geological Quarterly; 2000, 44, 3; 317-331
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Molluscs in Eemian-Vistulian deposits of the Kolodiiv section, Ukraine (East Carpathian Foreland) and their palaeoecological interpretation
    Autorzy:
    Alexandrowicz, W.P.
    Dmytruk, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059489.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Ukraine
    Halye Basin
    Vistulian
    loess
    molluscan assemblages
    Opis:
    A profile of loess several metres thick with palaeosoils, underlain by calcareous gyttja, out crops in Kolodiiv, Ukraine. Rich and diverse assemblages of molluscs have been found in these deposits. Three types of mollusc communities can be distinguished. The oldest is dominated by freshwater taxa and corresponds to calcareous gyttja of Eemian age. The next two assemblages contain only snails typical of loess. The first of these indicates a cold and dry climate and open environment of arctic steppe type, with rapid accumulation of loess; the second assemblage represents a cold and humid climate and a relatively moist, open environment of tundra type.
    Źródło:
    Geological Quarterly; 2007, 51, 2; 173-178
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Palynomorph assemblages from the Upper Ordovician in northern and central
    Autorzy:
    Stempień-Sałek, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/191654.pdf
    Data publikacji:
    2011
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    palynological assemblages
    palynostratigraphy
    palaeotemperatures
    Upper Ordovician
    Polska
    Opis:
    Palynological studies have been done to compare the Upper Ordovician strata in various geological units of northern and central Poland (epi-Caledonian Platform, East European Platform, Małopolska Block and Holy Cross Mountains–Łysogóry Fold Zone and Kielce Fold Zone). Two distinct palynological assemblages have been distinguished in the studied material: the Caradoc assemblage I and the Ashgill assemblage II (with two sub-assemblages IIa and IIb), thus demonstrating usefulness of the Upper Ordovician palynomorphs for biostrati- graphy. Thermal maturity of organic matter was studied using the TAI method. The palynological analysis, palynostratigraphy, and estimates of thermal maturity were done with the aim at palynological characterization of three ancient units: the Avalonia, Baltica and the Małopolska Block, all now participating in structures of the present-day geological units of northern and central Poland.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2011, 81, No 1; 21-61
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Diversity of cyanobacteria and microalgae in hydro-terrestrial habitatsin Svalbard and its ecological evaluation
    Autorzy:
    Richter, Dorota
    Powiązania:
    https://bibliotekanauki.pl/articles/2042113.pdf
    Data publikacji:
    2018
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Arctic
    Svalbard
    phycoflora
    assemblages
    ecological features
    trophic status
    Źródło:
    Polish Polar Research; 2018, 39, 2; 255-311
    0138-0338
    2081-8262
    Pojawia się w:
    Polish Polar Research
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Criteria to discriminate between proglacial and paraglacial environments
    Autorzy:
    Slaymaker, O.
    Powiązania:
    https://bibliotekanauki.pl/articles/294984.pdf
    Data publikacji:
    2007
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    proglacial ststems
    paraglacial systems
    sediment-landform associations
    landform assemblages
    Źródło:
    Landform Analysis; 2007, 5; 72-74
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Effects of location of Norway spruce (Picea abies) stumps on their colonisation by insects in the mountains
    Autorzy:
    Skrzecz, Iwona
    Bulka, Maria
    Ukalska, Joanna
    Powiązania:
    https://bibliotekanauki.pl/articles/2044136.pdf
    Data publikacji:
    2019
    Wydawca:
    Instytut Badawczy Leśnictwa
    Tematy:
    mountains
    altitude
    exposure
    insect assemblages
    Coleoptera
    Picea abies stump
    Opis:
    Tree stumps provide habitat for insect assemblages, which are influenced by various factors. Among these factors, physical and chemical changes of the stumps, fungi developing in the dead wood and stump size are most often reported. However there is limited information about the abundance of insects in stumps that are located on mountains where there are different microclimatic conditions. The studies pointed at the determination whether the location of Picea abies stumps in mountains at different altitudes above sea level and on mountainsides with different sun exposure has an impact on the frequency of insects colonising them. The study was carried out in the Eastern Sudety Mountains situated in south-western Poland. The stumps were in clearcuts located at the altitudes 600–700 m and 900–1000 m above sea level and on southern and northern mountainsides. The insects were collected from 0.05 m2 of bark from each stump and identified to the family, order or species level. The numbers of insects in the stumps were modelled with the use of the Poisson distribution or the negative binomial distribution and the generalised linear models. Picea abies stumps were colonised by insects from 16 families in 3 orders (Coleoptera, Diptera, Hymenoptera) in which the Coleoptera was most frequently represented by the families Cerambycidae, Curculionidae (with the sub-family Scolytinae). In the stumps located at the elevation of 900–1000 m there were 28% more insects than in the stumps at 600–700 m. The stumps located on mountainsides with northern exposure were colonised more abundantly by Cerambycidae. Numbers of Curculionidae in the stumps were affected by altitude. Most Curculionidae were found in the stumps located at the elevation 900–1000 m above sea level. The interaction of altitude and mountainside exposure showed more insects in the stumps at higher altitude, regardless of the mountainside exposure. The results showed that the total number of insects in the stumps was influenced by their location in mountains.
    Źródło:
    Folia Forestalia Polonica. Series A . Forestry; 2019, 61, 1; 64-77
    0071-6677
    Pojawia się w:
    Folia Forestalia Polonica. Series A . Forestry
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Natural and anthropogenic changes in the environment during the Holocene at the Kraków region (Southern Poland) from study of mollusc assemblages
    Autorzy:
    Alexandrowicz, Witold Paweł
    Powiązania:
    https://bibliotekanauki.pl/articles/2058731.pdf
    Data publikacji:
    2021
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    mollusc assemblages
    environmental changes
    anthropogenic pressure
    Holocene
    Southern Poland
    Opis:
    Malacological analysis was used to reconstruct Holocene environmental changes from profiles of calcareous tufa and fluvial deposits exposed in the Kobylanka stream valley, several kilometres west of Kraków in southern Poland. The abundant and diversified mollusc fauna was characterized by clear variability within the vertical succession where five types of molluscan assemblages were distinguished. The pattern of sedimentary and molluscan facies allowed characterization of two main intervals of environmental change during Holocene. In the lower interval, until the end of the Middle Holocene, human activity was not detected and environmental processes were controlled by natural factors. In the upper interval, corresponding to the Late Holocene, human impact can be seen, in the form of rapid deforestation and agricultural development. Anthropogenic impact has been particularly evident during the last millennium. The mollusc assemblages studied allowed accurate reconstruction of natural and anthropogenic factors affecting the natural environment.
    Źródło:
    Geological Quarterly; 2021, 65, 1; 9
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Freshwater diatoms of the Ecology Glacier foreland, King George Island, South Shetland Islands
    Autorzy:
    Kochman-Kędziora, Natalia
    Noga, Teresa
    Olech, Maria
    Van De Vijver, Bart
    Powiązania:
    https://bibliotekanauki.pl/articles/2042083.pdf
    Data publikacji:
    2018
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Antarctic
    King George Island
    Ecology Glacier
    diatoms
    freshwater assemblages
    Źródło:
    Polish Polar Research; 2018, 39, 3; 393-412
    0138-0338
    2081-8262
    Pojawia się w:
    Polish Polar Research
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Molluscan assemblages in sediments of a landslide on Majerz Hill near Niedzica (Inner Carpathians, Southern Poland) – phases of development and environmental changes
    Autorzy:
    Alexandrowicz, Witold Paweł
    Powiązania:
    https://bibliotekanauki.pl/articles/2055854.pdf
    Data publikacji:
    2022
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    landslide
    molluscan assemblages
    environmental changes
    Holocene
    Podhale Basin
    Southern Poland
    Opis:
    A detailed malacological analysis was made of sediments associated with a small landslide which had developed on the north-eastern slope of Majerz Hill near Niedzica (Inner Carpathians, Southern Poland). The age of the development and environmental changes associated with particular phases of the landslide was determined by means of radiocarbon dating. The analyses made it possible to distinguish two periods of landslide activation falling on the turn of the Early/Middle Holocene and on the Late Holocene (probably on the Iron Age Cold Period). These phases are closely related to periods of increased mass movements, both of landslides and debris flows in other European mountains, stages of glacial advance in the Alps, periods of increased fluvial activity in rivers and elevated water levels in European lakes. The molluscan assemblages also enabled the reconstruction of environmental conditions before the landslide formation, during periods of dormancy, and after the end of its activity.
    Źródło:
    Geology, Geophysics and Environment; 2022, 48, 1; 51--68
    2299-8004
    2353-0790
    Pojawia się w:
    Geology, Geophysics and Environment
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Dinoflagellate cyst and spore−pollen spectra from the Lower Oligocene Krabbedalen Formation at Kap Brewster, East Greenland
    Autorzy:
    Birkenmajer, Krzysztof
    Gedl, Przemysław
    Worobiec, Elżbieta
    Powiązania:
    https://bibliotekanauki.pl/articles/2051607.pdf
    Data publikacji:
    2010
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Greenland
    Kap Brewster
    Early Oligocene
    biostratigraphy
    palynology
    dinoflagellate cyst assemblages
    Źródło:
    Polish Polar Research; 2010, 2; 103-140
    0138-0338
    2081-8262
    Pojawia się w:
    Polish Polar Research
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Molluscan assemblages in Late Holocene tufa cones in the Pieniny Mountains (southern Poland)
    Autorzy:
    Alexandrowicz, W. P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059741.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    calcareous tufa
    molluscan assemblages
    historic period
    Pieniny Mts.
    South Poland
    Opis:
    Limestone rock walls of various inclination form a favourable substrate for the deposition of calcareous tufas that form cone-shaped structures located at the foot of slopes or fill niches within them. Such carbonate deposits usually contain rich and diversified molluscan assemblages, whose composition and structure closely correspond to the ambient environmental conditions in the immediate vicinity. The study of the Pieniny Mountains area revealed 10 sites with such deposits. The identified malacofouna was subjected to detailed analysis. It enabled identification of three types of faunistic assemblages (Bythinella austriaca assemblage, Pyramidula pusilla assemblage, and a shade-loving species assemblage), which are related to the conditions prevailing during the deposition. Tufa cones found in the Pieniny Mountains represent the historic period (Late Holocene). The deposits provide a record of two climatic phases: warmer and colder. The former (Medieval Warm Period) involved the intensified deposition of carbonate material and the rapid growth of tufa cones. The latter – the Little Ice Age – entailed the slow degradation of cones and slower sedimentation of tufas, while the intensified physical weathering led to the increase in the clast material proportion (sharp-edged limestone fragments). Tufas accumulated in the zone unaffected by high anthropogenic pressure and thus represent a record of natural environmental changes during the historic period
    Źródło:
    Geological Quarterly; 2014, 58, 2; 269--280
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Molluscs of the Eemian Interglacial in Poland
    Autorzy:
    Alexandrowicz, S. W.
    Alexandrowicz, W. P.
    Powiązania:
    https://bibliotekanauki.pl/articles/191962.pdf
    Data publikacji:
    2010
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Eemian Interglacial
    basic and supplementary sections
    molluscan assemblages
    malacostratigraphy
    Polska
    Opis:
    Shells of subfossil snails and bivalves commonly noted in deposits of the Eemian Interglacial were used by several authors as more or less important stratigraphic indicators. In Poland, they have been noted in 35 sections, 20 of which are described as basic ones. Molluscan assemblages found at these sites include 60 species of freshwater molluscs and 58 species of land snails, the former being dominant. Climatic tolerance of particular species is the main attribute deciding on their stratigraphic values. Cold-tolerant snails are typical of the preceding Late Glacial and some of them occur also in early phases of the interglacial, while species connected with moderate climate and warm-demanding ones characterise the middle part of the Eemian Interglacial. The freshwater snail Belgrandia marginata is typical of the climatic optimum of this interglacial. Particular species of molluscs were related to regional pollen assemblage zones of the Eemian Interglacial in Poland.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2010, 80, No 1; 69-87
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Stratigraphy and geological structure of the Magura Nappe in the south-western part of the Gorce Mountains, Outer Carpathians, Poland
    Autorzy:
    Szczęch, Mateusz
    Waśkowska, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/24201044.pdf
    Data publikacji:
    2023
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Late Cretaceous–Early Miocene
    stratigraphy
    foraminiferal assemblages
    tectonics
    highresolution DEM
    Opis:
    The south-western part of the Gorce Mts (Outer Carpathians) is composed of flysch deposits of the Krynica and Bystrica subunits of the Magura Nappe. The Krynica Subunit includes the Late Cretaceous–Paleocene Ropianka Fm, the Early Eocene Beloveža Fm, the Early Eocene–Oligocene Magura Fm and the Oligocene–Early Miocene Malcov Fm, while the Bystrica Subunit includes the Middle Eocene–?Oligocene Magura Fm, represented mainly by the thick-bedded Magura Sandstone. Thin- and medium-bedded sandstone-shale turbidites predominate in the other formations. The lithostratigraphic units are dated on the basis of foraminifers. The studied deposits accumulated in the southern part of the Magura Basin. Their detrital material was derived from a ridge, bounding the basin in the south. In the study area, the Krynica Subunit overthrusts the Bystrica Subunit. The studied deposits are folded, thrust and cut by numerous faults. The Turbacz Thrust Sheet and the newly identified Kudłoń Thrust Sheet were distinguished in the Krynica Subunit. Faults of different lengths and throws are transverse or oblique. Some of them form complex dislocation zones with lengths of up to several km. In general, the high-resolution digital elevation model DEM contributed significantly to progress in the geological and geomorphological research.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2023, 93, 2; 103--136
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Bentonitized tuffites in the Lower Eocene deposits of the Subsilesian Unit (Western Outer Carpathians, Poland): lithology, stratigraphic position and mineral composition
    Zbentonityzowane tufity w dolnoeoceńskich osadach jednostki podśląskiej (polskie Zachodnie Karpaty Zewnętrzne): litologia, pozycja stratygraficzna i skład mineralny
    Autorzy:
    Cieszkowski, M.
    Środoń, J.
    Waśkowska-Oliwa, A.
    Leśniak, T.
    Powiązania:
    https://bibliotekanauki.pl/articles/191629.pdf
    Data publikacji:
    2006
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Polish Outer Carpathians
    Subsilesian unit
    Early Eocene
    bentonitized tuffites
    foraminiferal assemblages
    Opis:
    New occurrences of bentonitized tuffites were described from numerous outcrops of the Lower Eocene flysch rocks of the Subsilesian Unit. These deposits crop out in the Żywiec tectonic window and in the tectonic windows of the Lanckorona - Żegocina Structural Zone. The bentonitized tuffites, composed of almost pure dioctahedral motmorillonite, form numerous thin layers and laminae, only occasionally exceeding 5 cm. The age of the tuffites is estimated as the Early Eocene (Glomospira div. sp. and Saccamminoides carpathicus zones) on the basis of foraminiferal assemblages. They occur in the upper part of green shales and in the lower part of the Lipowa beds that consist mainly of muddy turbidites represented by green or green-brownish shales with rare intercalations of sandstones. The sedimentary sequences with the tuffite intercalations form a lithostratigraphic level in the Subsilesian Unit called in the present paper "the Glichów Tuffite Horizon". This tuffite horizon could probably be correlated with deposits of similar age containing tuffites which are known from the Magura, Silesian and Skole nappes.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2006, 76, No 2; 197-214
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Influence of palaeoclimate and the green house effect on Hettangian clay mineral as sem blages (Holy Cross Mts. area, Polish Basin)
    Autorzy:
    Brański, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059218.pdf
    Data publikacji:
    2009
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Hettangian
    Holy Cross Mountains
    margin
    clay mineral assemblages
    palaeoclimate
    greenhouse effect
    Opis:
    Hettangian clay mineral assemblages from the Holy Cross Mts. margin (south eastern part of the epicontinental Polish Basin) were mostly controlled by climaticcon ditions and weathering regime. Hettangian claystones and mudstones were deposited in continental and marine-margin palaeoenvironments in a warm climate, mostly with year-round humidity. The pronounced, long-term green house conditions intensified chemical weathering in the hinterland. Reworking and redeposition of ancient sediments caused by tectonics and/or by sea-level changes and early diagenesis may have modified the clay mineral content in the earliest Hettangian. Burial diagenesis and telodiagenesis changed the clay mineral composition only locally.
    Źródło:
    Geological Quarterly; 2009, 53, 3; 363-368
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Charakterystyka jurajskich mszywiołów południowej Polski w aspekcie warunków paleooerodowiska i biogeografii
    Characteristics of Jurassic bryozoans from southern Poland in palaeoecological and biogeographical aspects
    Autorzy:
    Hara, U.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074500.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    jura
    mszywioły
    różnorodność
    paleośrodowisko
    biogeografia
    Jurassic
    bryozoan assemblages
    cyclostomes
    diversity
    palaeoecology
    biogeography
    Opis:
    A few distinctive bryozoan assemblages have been recognized in the Middle and Upper Jurassic sediments of southern Poland. The biota moderately rich in bryozoan taxa are generally restricted to a few cyclostome genera and dominated respectively by tubuloporines among which the majority form a fan-shaped or discoidal [bereniciform], encrusting colonies previously called "Berenieca", a bryozoan ubiquitous in the Jurassic. The Lower and Upper Callovian epifaunal bryozoan community of the vicinity of Cracow at Zalas in the Cracow Upland is represented by well-known Jurassic Stomatopora Bronn, Hyporosopora Canu & Bassler and Microeciella Taylor & Sequeiros, genera, as well as the other undeterminated, numerous bereniciform colonies. In terms of the species richness the most diversified is the Early Oxfordian bryozoan assemblage of the Ćmielów area [NW margin of the Holy Cross Mts], associated with an open shelf biohermal sedimentation, which was replaced later [during the transversarium and bifurcatues zones] by the shallow-water, soft-bottom coral buildups, among which the bryozoans are well-represented and described from Bałtów. The presence of the ?Late Tithonian–Berriasian bryozoan fauna has been documented in the thin-sections of the Stramberk limestones of the Polish Flysch Carpathians. Palaeoecological aspects of the studied bryozoan biotas are related to the nature and relative abundance of the colonial growth forms, the substrate type and other ecological factors. The moderately rich occurrence of the bryozoans in the Late Middle and Upper Jurassic sequences of Poland shows a different pattern of distribution than the biotas of the northwestern Europe which display the greatest species diversity in the Middle Jurassic [Bathonian]. The taxonomical and biogeographical studies of the Jurassic bryozoan biotas of Poland, in spite of the great patchiness in the global distribution of the Jurassic cyclostomes, has a key significance for the evolutionary radiation pattern and may add new data, whether this fauna originated and started to radiate in the Late Middle or the Upper Jurassic, or this event was mostly connected with the facies migration from west to east.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 1; 54-60
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Late Glacial and Holocene molluscan assemblages in deposits filling palaeolakes in northern Poland
    Autorzy:
    Alexandrowicz, W.P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2027032.pdf
    Data publikacji:
    2013
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    lacustrine chalk
    calcareous gyttja
    palaeolakes
    molluscan assemblages
    Late Glacial
    Holocene
    northern
    Po land
    Opis:
    Late Gla cial and Ho lo cene car bon ate lac us trine de pos its de vel oped as lac us trine chalk and cal car e ous gyttja are fairly wide spread across north ern Po land. They form fill ings of palaeolakes which de vel oped dur ing the deglaciation. These for ma tions are usu ally cov ered by peat. Rich and di ver si fied malacofauna has been found in the afore men tioned sed i -ments. The pro files from 154 sites de scribed and pub lished by var i ous au thors were sub jected to malacological anal y -sis. In the whole ma te rial, 18 mol lus can as sem blages were dis tin guished, rep re sent ing three types of hab i tats: terrestrial,of tem po rary wa ter bod ies, and of per ma nent wa ter bod ies. The com po si tion and struc ture of these as sem blages al lows char ac ter iz ing cli mate and dif fer en ti at ing hab i tats. The time-se quences of malacological as sem blages pro videdpos si bil ity to de fine three types of malacological se quences. On the ba sis of these suc ces sions, a scheme of the lakewa ter bod ies evo lu tion dur ing Late Gla cial and in north ern Po land was elab o rated.
    Źródło:
    Studia Quaternaria; 2013, 30; 5-17
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Prejudices behind Algorithms: Automated Surveillance Systems as Tools of Segregation and Discrimination
    Autorzy:
    Gurtowski, Maciej
    Waszewski, Jan
    Powiązania:
    https://bibliotekanauki.pl/articles/1985830.pdf
    Data publikacji:
    2018-12-31
    Wydawca:
    Wydawnictwo Adam Marszałek
    Tematy:
    Big Data
    data doubles
    dataveillance
    invisible hand
    new surveillance
    perverse effect
    racism
    surveillant assemblages
    Opis:
    The aim of this paper is to describe the emerging phenomenon of new racism brought by the development of automated surveillance tools. We would like to show that this new system of discrimination is a byproduct of some general transformations in the field of social control. For this purpose, we will refer to invisible hand type of explanation, and the concept of perverse effect in particular. We will also relate widely to some cases and concepts from the “new surveillance” and social control literature and we will try to summarize it.
    Źródło:
    Kultura i Edukacja; 2018, 4(122); 94-109
    1230-266X
    Pojawia się w:
    Kultura i Edukacja
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Possibilities and restrictions of heavy-mineral analysis for the reconstruction of sedimentary environments and source areas
    Autorzy:
    Derkachev, A.N.
    Nikolaeva, N. A.
    Powiązania:
    https://bibliotekanauki.pl/articles/94357.pdf
    Data publikacji:
    2013
    Wydawca:
    Uniwersytet im. Adama Mickiewicza w Poznaniu
    Tematy:
    heavy-mineral assemblages
    sedimentary environments
    ODP cores
    Mesozoic folded belts
    złoża ciężkich minerałów
    środowiska sedymentacyjne
    Opis:
    The possible reconstruction of ancient sedimentary environments on the basis of heavy-minerals assemblages is presented by means of discriminant lithogeodynamic diagrams that compare modern and ancient sedimentary environments. This is exemplified by Mesozoic-Cenozoic deposits recovered from ODP cores obtained from the Philippine and Japan Seas, the Japan Trench and the North Atlantic, as well as by deposits from folded areas onshore. On the basis of the comparative analysis, it can be deduced that the main tendencies in mineral assemblages of modern deposits that depend on the structural-tectonic conditions, are fairly well preserved in Cenozoic deposits (including the deposits recovered by ODP drilling). On the other hand, the environmental reconstruction of folded and faulted pre-Cenozoic continental areas on the basis of their heavy-mineral assemblages, by comparing them with supposed modern analogs, is not always possible with much certainty. The main reasons may be either a considerable change in the composition of the initial (primary) mineral assemblages as a result of intralayer solution or the absence, at the time of deposition, of geodynamic environments that closely resembled modern ones.
    Źródło:
    Geologos; 2013, 19, No. 1-2; 147-158
    1426-8981
    2080-6574
    Pojawia się w:
    Geologos
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The Middle Miocene of the Fore-Carpathian Basin (Poland, Ukraine and Moldova)
    Autorzy:
    Wysocka, A.
    Radwański, A.
    Górka, M.
    Bąbel, M.
    Radwańska, U.
    Złotnik, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/138689.pdf
    Data publikacji:
    2016
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Lithofacies
    fossil assemblages
    Middle Miocene
    Fore-Carpathian Basin
    Polska
    Ukraine
    Litofacje
    miocen
    zbiornik przedkarpacki
    Polska
    Ukraina
    Opis:
    Studies of Miocene sediments in the Fore-Carpathian Basin, conducted by geologists from the University of Warsaw have provided new insights on the distribution of the facies infilling the basin, particularly in the forebulge and back-bulge zones. The origin of the large-scale sand bodies, evaporitic deposits and large-scale organic buildups is discussed, described and verified. These deposits originated in variable, shallow marine settings, differing in their water chemistry and the dynamics of sedimentary processes, and are unique with regard to the fossil assemblages they yield. Many years of taxonomic, biostratigraphic, palaeoecologic and ecotaphonomic investigations have resulted in the identification of the fossil assemblages of these sediments, their age, sedimentary settings and post-mortem conditions. Detailed studies were focused on corals, polychaetes, most classes of molluscs, crustaceans, echinoderms, and fishes.
    Źródło:
    Acta Geologica Polonica; 2016, 66, 3; 351-401
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ekologia polityczna powietrza: o uwidzialnianiu miejskiego ryzyka
    The Political Ecology of the Air: Making Urban Risk Visible
    Autorzy:
    Bojadżijewa, Iwona
    Powiązania:
    https://bibliotekanauki.pl/articles/1373328.pdf
    Data publikacji:
    2016-05-23
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    actor-network theory
    risk
    agency of things
    urban conflicts
    assemblages
    teoria aktora-sieci
    ryzyko
    sprawczość rzeczy
    konflikty miejskie
    asamblaże
    Opis:
    In this text the author attempts to reconstruct contemporary disputes about air quality in Poland using the language of actor-network theory (ANT). The purpose is to show the process of making urban risk visible—in this instance, the risk of polluted air—through the development of hybrid alliances and the formulation of translations aimed at the final elimination of air pollution. The article consists of three parts and a theoretical introduction in which the author discusses the basic tools and concepts of ANT, as well as Latour’s programme of political ecology. In the first part, the author sketches the map of actors and actants involved in air-pollution discussions. Then she examines the role of things—material objects—in air pollution conflicts, with special emphasis on the agency of these non-human actants. Finally, she focuses on alternative translations, which are attempts to negotiate smog’s place in the hierarchy of the collective.
    Źródło:
    Kultura i Społeczeństwo; 2016, 60, 2; 35-53
    2300-195X
    Pojawia się w:
    Kultura i Społeczeństwo
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ewolucja jezior przybrzeżnych Niziny Gardzieńsko - Łebskiej na tle rozwoju środkowego wybrzeża Bałtyku w świetle badań malakologicznych
    Evolution of coastal lakes of the Gardno - Łeba Lowland in the light of malacological research
    Autorzy:
    Wojciechowski, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/295242.pdf
    Data publikacji:
    2008
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    jeziora przybrzeżne
    Nizina Gardzieńsko-Łebska
    wybrzeże południowego Bałtyku
    zespoły mięczaków
    coastal lakes
    Gardno-Łeba Lowland
    South Baltic Coast
    molluscs assemblages
    Opis:
    Wartykule przedstawiono syntezę dotychczasowego stanu wiedzy o rozwoju jezior przybrzeżnych Niziny Gardzieńsko- Łebskiej i środkowego wybrzeża Bałtyku, bazującą na wynikach badań malakologicznych. Analizy zespołów mięczaków z osadów limnicznych i morskich pozwoliły na wyróżnienie czterech faz rozwojowych jezior: wczesnoholoceńskiej fazy limniczno-bagiennej (trwającej od późnego glacjału do około 7500 lat 14C BP), fazy lagunowej (około 7500–6600 lat 14C BP), fazy przejściowej, słonawowodno-limnicznej (6600–4000 lat 14C BP) oraz fazy jeziornej (młodszej od 4000 lat 14C BP).W artykule wykazano, iż sukcesja malakofauny jest odzwierciedleniem regionalnych przemian środowiska, zarejestrowanych podobnymi zmianami zespołów fauny na całym wybrzeżu południowego Bałtyku.
    The papers presents the synthesis of the current understanding of the evolution of coastal lakes in the Gardno-Łeba Lowland. Particular emphasis has been placed upon the influence of pre-Holocene surface topography on lake basin evolution and water level changes caused by the transgression of southern Baltic. Malacological analysis reveals four phases in lake environmental history: limnic-swampy phase, lagoon phase, transitional brackish-limnic phase, and limnic phase. The oldest, early Holocene limnic-swampy phase in the Gardno-Łeba Lowland area is represented by Preboreal and Boreal assemblages with freshwater fauna, described as Planorbis phase. It is characterized by rich assemblages, in terms of both number of individuals and species, composed of members of Planorbis, accompanied by Bithynia tentaculata, Valvata piscinalis and Pisidium. The lagoon-marine phase, described as Scrobicularia phase (7500–6000 BP), is defined by a homogeneous assemblage of malacofauna, consisting entirely of brackish and marine species, such as Hydrobia ulvae, H. ventrosa, Cerastoderma glaucum, Macoma baltica, Mytilus edulis and indicative Lusitanian and Lower Boreal species for the Mesoholocene of the southern Baltic, including Scrobicularia plana, Rissoa membranaea, R. inconspicua, Parvicardium exiguum and Mysella bidentata. The transitional brackish-limnic phase Cardium (6600–4000 BP) is correlated with late Littorina transgressive phases. It is dominated by Cardium glaucum, with minor percentage of Hydrobia ventrosa, Mytilus edulis, and sporadic freshwater species. The limnic Lymnaea phase corresponds with the post-Littorina period (4000 BP–1900 AD). The onset of this phase is marked by an assemblage with dominating Theodoxus fluviatilis, the optimum – by Lymnea peregra assemblages, whereas frequent Bithynia tentaculata indicate the end of the phase. The youngest Potamopyrgus phase includes recent lake sediments from the last 100 years and is marked by the first appearance of a new mollusc species in the coastal zone of the Baltic – Potamopyrgus antipodarium. The malacofauna succession identified in the coastal lakes in the Gardno-Łeba Lowland reflects regional environmental change, recorded by similar faunal assemblages throughout the southern coast of the Baltic.
    Źródło:
    Landform Analysis; 2008, 7; 154-171
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zgrupowania epigeicznych mrówek w drzewostanach sosnowych opryskanych inhibitorami syntezy chityny
    Autorzy:
    Głowacka, B.
    Mazur, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/1022200.pdf
    Data publikacji:
    2005
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    mrowki
    drzewostany sosnowe
    inhibitory biosyntezy chityny
    zgrupowania zwierzat
    srodki ochrony roslin
    lesnictwo
    owady epigeiczne
    pest control
    acylureas
    epigeic ants assemblages
    Opis:
    This paper is an attempt to find the changes which undergo in ants assemblages after using acylureas pine foliophagous pest.
    Źródło:
    Sylwan; 2005, 149, 03; 34-41
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Malakofauna górnoholoceńskich martwic wapiennych w Beskidach Zachodnich (południowa Polska)
    Malacofauna of Upper Holocene calcareous tufa in the Western Beskidy Mts (Southern Poland)
    Autorzy:
    Alexandrowicz, W. P.
    Powiązania:
    https://bibliotekanauki.pl/articles/183928.pdf
    Data publikacji:
    2009
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    martwice wapienne
    malakofauna
    zespoły mięczaków
    górny holocen
    Beskidy Zachodnie
    południowa Polska
    calcareous tufa
    malacofauna
    molluscan assemblages
    Upper Holocene
    Western Beskidy Mts.
    southern Poland
    Opis:
    Górnoholoceńskie martwice wapienne występują pospolicie na obszarze Beskidów Zachodnich. Często, choć nie zawsze, zawierają one miej lub bardziej bogate zespoły mięczaków. Analiza malakologiczna przeprowadzona została na podstawie materiału pochodzącego z 33 stanowisk reprezentowanych przez 59 próbek. Pozwoliła ona na opis najbardziej charakterystycznych zespołów mięczaków. Zostały wydzielone cztery typy i trzy podtypy fauny różniące się między sobą strukturą i składem gatunkowym. Malakofauna rozpoznana w omawianych osadach węglanowych jest ściśle uzależniona od lokalnych warunków. Spośród 68 rozpoznanych gatunków tylko kilka występowało licznie i w wielu profilach, podczas gdy pozostałe miały znaczenie akcesoryczne. Badania nad górnoholoceńskimi martwicami wapiennymi mają duże znaczenie dla rozpoznania mechanizmów tworzenia takich osadów węglanowych i zróżnicowania zespołów fauny. Stanowią one także podstawę rozważań aktuopaleontologicznych istotnych dla interpretacji paleogeograficznych i paleoekologicznych martwic holocenu oraz późnego glacjału występujących w południowej Polsce.
    Upper Holocene calcareous tufa occur commonly in the Western Beskidy Mts. Often, at least not always they contain more or less rich and differentiated molluscan assemblages. Malacological analysis was carried out on the basis of material collected from 33 localities represented by 59 samples. The most typical communities of snails and bivalves were characterized. Four types and three subtypes of fauna differing oneself in structure and species composition have been distinguished. Malacofauna recognized in discussed calcareous deposits is closely depended on local conditions. The whole material comprises 68 species, but only a few of them occur in large numbers and in many profiles, while the remaining ones had only accesorical importance. Malacological investigations of Upper Holocene calcareous tufa are important for recognizing mechanisms of deposition such calcareous sediments and differentiation of molluscan assemblages. They can be useful for actuopelaeontological analysis essential for palaeogeographical and palaeoecological interpretations of tufas of Holocene and Late Glacial age occurred in Southern Poland.
    Źródło:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2009, 35, 2; 175-200
    0138-0974
    Pojawia się w:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Holoceńska ewolucja torfowiska w Zatoce Słupiańskiej (jezioro Wigry, NE Polska) w świetle analizy malakologicznej
    Holocene evolution of the peat-bog in Słupiańska Bay (Wigry Lake, NE Poland) in the light of malacological analysis
    Autorzy:
    Alexandrowicz, W. P.
    Żurek, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2061609.pdf
    Data publikacji:
    2018
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    gytia wapienna
    zespoły mięczaków
    zmiany środowiska
    wahania poziomu jezior
    holocen
    jezioro Wigry
    calcareous gyttja
    assemblages of molluscs
    environmental changes
    lake-level fluctuations
    Holocene
    Wigry lake
    Opis:
    W profilach wierceń wykonanych na obszarze torfowiska w Zatoce Słupiańskiej rozpoznano trzy typy zespołów mięczaków. Liczne skorupki mięczaków występowały w obrębie serii gytii wapiennych i drobnodetrytusowych o miąższości 5,35 m. Malakofauna była reprezentowana głównie przez ślimaki wodne i małże. Taksony lądowe pojawiały się rzadko, a największe liczebności osiągały w stropowej części analizowanej sekwencji. Wydzielone zespoły mięczaków charakteryzowały odmienne typy siedlisk. Występujący w spągowej części profilu zespół z Gyraulus laevis zawiera liczne taksony zimnolubne i wiekowo odpowiada wczesnemu holocenowi. Młodsza fauna (zespół z Gyraulus albus) cechuje się znacznym udziałem form ciepłolubnych, a jego obecność wskazuje na fazę atlantycką. Zespół z gatunkami lądowymi występuje w stropowej części analizowanego profilu. Zespoły mięczaków reprezentują różne typy środowisk: strefę litoralną jeziora, okresowe zbiorniki wodne oraz podmokłe siedliska lądowe. Zmienność zespołów mięczaków oraz zróżnicowany udział skorupek i wieczek Bithynia tentaculata wskazuje na obecność faz obniżenia poziomu wody w jeziorze Wigry, które przypadają na fazę borealną, środkową część fazy atlantyckiej oraz schyłek fazy subborealnej i fazę atlantycką. Z tym ostatnim okresem wiąże się początek depozycji torfu.
    Three types of molluscan assemblages have been identified in a profile of calcareous gyttja and peat penetrated by drilling within the raised peat-bog of the Słupiańska Bay. Numerous shells of molluscs have been identified within the 5.35 m thick intervals of fine detritus of the calcareous gyttja. The shells belonged primarily to the bivalves and water snails. Terrigenous species appeared only rarely and have been more frequent in the upper part of the penetrated interval. The three distinguished molluscan assemblages have been described and interpreted in terms of representing different environmental conditions. Assemblage with Gyraulus laevis that occurs within the lower part of the interval consists of the cold-loving forms representing early Holocene. Assemblage with Gyraulus albus that occurs in the middle part of the interval consists of warm-loving species linked to the Atlantic Phase. Assemblage with terrigenous species, mainly snails, occurs in the upper part of the interval. The distinguished types of molluscan assemblages are composed of species characteristic of littoral habitat of ephemeral lakes and some of terrestrial habitats. Lake-level fluctuations are expressed by changing of molluscan fauna. Variable proportions of Bithynia tentaculata shells and opercula indicates low-level water stages of the Wigry Lake that took place during the Boreal Phase, the middle part of the Atlantic Phase and during the termination of the Sub Boreal and Sub Atlantic phases. The completion of gyttja accumulation and the beginning of peat deposition are associated with the latter period.
    Źródło:
    Biuletyn Państwowego Instytutu Geologicznego; 2018, 473; 1--12
    0867-6143
    Pojawia się w:
    Biuletyn Państwowego Instytutu Geologicznego
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Biegaczowate jako zooindykatory regeneracji drzewostanów sosnowych zaburzonych przez huragan w 2002 roku - wyniki obserwacji z lat 2003-2011
    Carabids as bioindicators of regeneration of Scots pine stands disturbed by a hurricane in 2002 - results of observations from 2003-2011
    Autorzy:
    Skłodowski, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/993268.pdf
    Data publikacji:
    2013
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    lesnictwo
    drzewostany pokleskowe
    drzewostany sosnowe
    drzewostany pohuraganowe
    regeneracja
    bioindykatory
    chrzaszcze
    biegaczowate
    Carabidae
    zgrupowania zwierzat
    struktura zgrupowan
    struktura gatunkowa
    ground beetles
    assemblages
    species diversity
    forest species
    mib
    Opis:
    During the period from 2003 to 2011 observations of carabid community regression and selected habitat indicators were conducted on 15 plots in stands that had been disturbed by a hurricane and on 15 plots in control stands. Regression of carabid communities delayed 3−4 years was observed, consisting in increases in the number of species and the proportion of xerophilous species and reductions in the percentage of forest fauna and in mean individual biomass. Only after 7 years did these indicators begin to show a tendency in the reverse direction, albeit not very strong, indicating that carabid communities had begun to regenerate.
    Źródło:
    Sylwan; 2013, 157, 05; 376-384
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rethinking Polish assemblages of the 1960s: The (re)turn to things
    Autorzy:
    Błotnicka-Mazur, Elżbieta
    Powiązania:
    https://bibliotekanauki.pl/articles/1806875.pdf
    Data publikacji:
    2019-10-23
    Wydawca:
    Katolicki Uniwersytet Lubelski Jana Pawła II. Towarzystwo Naukowe KUL
    Tematy:
    polskie asamblaże; zwrot materialny; przedmioty w sztuce; polska sztuka lat 60. XX wieku
    Polish assemblages; material turn; objects in art; Polish art of the 1960s
    Opis:
    Przemyśleć na nowo polskie asamblaże z lat 60. XX wieku: powrót do rzeczy Celem artykułu jest analiza statusu obiektu w praktykach neoawangardowych wybranych polskich artystów w latach 60. XX wieku, z perspektywy „zwrotu materialnego”, zainicjowanego przez kryzys reprezentacji postrukturalizmu w naukach społecznych i humanistycznych. Chęć wyjścia poza tradycyjne dzieło malarskie, pojmowane w kategoriach płaskiej, dwuwymiarowej powierzchni, sprawiła, że artyści zaczęli wprowadzać do sztuki przedmioty z prawdziwego życia, dzięki czemu dzieło zyskiwało nowe życie i „osobowość”. Artykuł koncentruje się na pracach czterech wybitnych polskich artystów neoawangardowych: Erny Rosenstein, Włodzimierza Borowskiego, Tadeusza Kantora i Aliny Szapocznikow. Biorąc pod uwagę różnice między ich postawami artystycznymi i osobistymi doświadczeniami, można zaobserwować wspólne zainteresowanie materialnością świata, które zaowocowało różnorodnymi interpretacjami przedmiotów (Rosenstein, Borowski, Kantor), a także reifikacją ciała (Szapocznikow). Odniesienie do teorii aktora-sieci Latoura tworzy także nową perspektywę dla badań nad rolą obiektów w dziełach sztuki (Kantor).
    The article aims to analyse the status of the object in the neo-avantgarde practice of selected Polish artists in 1960s assemblages, from the perspective of the ‘material turn’, initiated by postructuralism’s crisis of representation in the social sciences and humanities. Trespassing on the intellectual ground associated with traditional painting, which was conceived as a flat two-dimensional surface, led the artists to introducing objects from real life into their art, this gave the artwork containing objects new life and ‘personality’. The paper focuses on the works by four prominent modernist Polish artists: Erna Rosenstein, Włodzimierz Borowski, Tadeusz Kantor and Alina Szapocznikow. Taking into account the differences between their artistic attitudes and personal experiences, one may observe a common interest in the materiality of the world that resulted in a variety of object interpretations (Rosenstein, Borowski, Kantor) as well as the reification the body (Szapocznikow). Reference to Latour’s Actor-Network-Theory also creates a new perspective for research on the objects in works of art (Kantor).
    Źródło:
    Roczniki Humanistyczne; 2018, 66, 4; 131-150
    0035-7707
    Pojawia się w:
    Roczniki Humanistyczne
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zgrupowania biegaczowatych jako zooindykatory różnych sposobów przygotowania gleby na zrębach oraz ich zagospodarowania
    Carabid communities as zooindicators of soil scarification techniques applied in clear-cutted forest stands and the further used management practices
    Autorzy:
    Skłodowski, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/1009276.pdf
    Data publikacji:
    2010
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    lesnictwo
    zreby
    zrab zupelny
    zagospodarowanie lasu
    gleby lesne
    przygotowanie gleby
    bioindykacja
    bioindykatory
    owady
    biegaczowate
    Carabidae
    zgrupowania zwierzat
    clear cut area
    soil preparation
    carabidae
    structure of assemblages
    regeneration
    Opis:
    In this paper the effect of different methods of soil scarification in a clear−cut area were studied. The following soil preparation techniques were applied: the soil cutter, the active soil plough, the traditional method with use of LPz plough, and the manual scarification of soil in circles surrounding the stem of the future young tree. The effect of management of the residual heaps of branches was also tested. Branches were either put in prisms in the original shape or, having been previously chipped, equally distributed over the entire area of the clear−cut. Additional studies focused on the effect of the time of clear−cut execution (winter or summer) on the condition of epigeic carabid communities. The least regressive effect to analysed communities was observed after the application of the point manual soil scarification. The clear−cuts carried out during the winter season, to a greater degree, favours the forest carabid fauna, preserving them in a structure more resembling the forest communities. More distinctive positive effect on the carabids is observed after putting the residual heaps of branches in prisms; the latter gives shelter for the carabid fauna and constitutes the refuge spots for it.
    Źródło:
    Sylwan; 2010, 154, 09; 625-638
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zgrupowania wciornastków (Thysanoptera) pni drzew w różnowiekowych lasach dębowych Słowacji
    Assemblages of bark-dwelling thrips [Thysanoptera] of uneven-aged oak forests in Slovakia
    Autorzy:
    Dubovsky, P.
    Fedor, P.
    Kucharczyk, H.
    Masarovic, R.
    Balkovic, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/1009045.pdf
    Data publikacji:
    2010
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    lesnictwo
    drzewostany debowe
    drzewa lesne
    dab
    Quercus
    pnie drzew
    owady
    wciornastki
    Thysanoptera
    zgrupowania zwierzat
    sklad gatunkowy
    struktura zgrupowan
    drzewostany roznowiekowe
    Slowacja
    thysanoptera
    oak woods
    assemblages
    diversity
    corticolous species
    bark
    Opis:
    The paper refers to the research on bark−dwelling thrips (Thysanoptera) on oaks (Quercus sp.) in the area of ‘Martinský les' wood that is a rare isolated refuge of natural oak wood stands Aceri tatarici−Quercetum Zólyomi 1957 being situated in lowland close to the town Senec in SW Slovakia. Arboreal photoeclectors were used for sampling corticolous arthropods at 6 various sites during the vegetation periods 2007 and 2008 in three−week intervals. Totally 1544 specimens of 35 Thysanoptera species were collected. Six of the species: Kakothrips dentatus, Thrips calcaratus, Phlaeothrips bispinoides, Hoplothrips corticis, Megathrips nobilis and Poecilothrips albopictus were observed for the first time in Slovakia. The statistic analysis PPCA was used for finding the relation between the assemblage's species composition and the age of oak trees on researched sites.
    Źródło:
    Sylwan; 2010, 154, 10; 659-668
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zmiany zgrupowań biegaczowatych zamieszkujących drzewostany zaburzone przez huragan – wyniki pierwszych 6 lat obserwacji w Puszczy Piskiej
    Changes in ground beetle assemblages inhabiting forest stands disturbed by the hurricane - the results of the first 6 years of the observations in Puszcza Piska Forest
    Autorzy:
    Skłodowski, J.
    Garbalińska, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/1009397.pdf
    Data publikacji:
    2010
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    lesnictwo
    Puszcza Piska
    drzewostany pokleskowe
    drzewostany pohuraganowe
    owady
    biegaczowate
    Carabidae
    zgrupowania zwierzat
    liczebnosc
    zmiany skladu gatunkowego
    hurricane
    disturbance
    post−hurricane stands
    carabidae
    ground beetles
    assemblages structure
    mib
    spc/mib model
    Opis:
    A survey on the structure and species composition of ground beetle assemblages inhabiting forest stands disturbed by the hurricane was carried out. During the first 6 years after the hurricane two distinct phases of carabids response to the disturbance could be observed. The first 3 years were characterised by relatively minor, although mostly statistically significant changes in carabids abundance, mean individual biomass and assemblages structure. In the 4th year after the hurricane, the second phase started comprising profound changes in all analysed parameters. The state of development of ground beetle assemblages inhabiting disturbed stands worsened considerably, however it did not reach the very low level recorded in assemblages inhabiting clear−cuts. The study revealed that the regression of carabid assemblages in post−hurricane stands occurred with a time lag of 3 years after the hurricane. Moreover, no symptoms of carabid assemblages regeneration could be observed.
    Źródło:
    Sylwan; 2010, 154, 08; 552-568
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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