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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:
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:
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:
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:
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:
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
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