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    Tytuł:
    Homotryblium-dominated Eocene dinoflagellate cyst assemblages from Middle Miocene (Badenian) glauconitic sands at Lipowiec (Roztocze, SE Poland)
    Autorzy:
    Gedl, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059861.pdf
    Data publikacji:
    2016
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Eocene
    Miocene
    reworking
    palaeoenvironment
    Roztocze
    SE Poland
    Opis:
    A section over 20 m thick of the basal Middle Miocene succession exposed at Lipowiec (Roztocze, SE Poland) was studied for palynology. Thirteen samples were collected from quartz and glauconitic-quartz sands and thin clay layers. Sand samples were barren but clay samples yielded dinoflagellate cysts. Their assemblages consist of reworked Paleogene specimens dominated by the Homotryblium floripes complex (H. floripes and morphologically similar H. plectilum and H. vallum). The presence of reworked Paleogene specimens indicates intense erosion of marine Paleogene strata during initial stages of the Middle Miocene transgression at Roztocze. Analysis of stratigraphical ranges of reworked dinoflagellate cysts and comparison with their occurrences in known epicontinental Paleogene sites of SE Poland suggest an Upper Eocene age of the washed-out strata. The taxonomic composition of the assemblages described suggests that the Upper Eocene deposits accumulated in a near-shore, lagoonal embayment characterized presumably by oligotrophic waters of slightly increased salinity. A high proportion of the Homotryblium floripes complex is also characteristic of reworked assemblages found in younger Miocene strata of neighbouring exposures in Roztocze, which indicates widespread Eocene lagoonal environments in this part of Roztocze. Coeval Eocene strata from the eastern part of Roztocze and from the Carpathian Foredeep show different taxonomic compositions suggesting varied sedimentary settings during Eocene transgression in this region. These differences reflect variable amounts of freshwater influence resulting in a range of environments that ranged from oligotrophic to brackish.
    Źródło:
    Geological Quarterly; 2016, 60, 2; 461--472
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Luminescence dating of ancient kilns and gothic to baroque bricks from SE Poland – a comparison with archaeomagnetic data
    Autorzy:
    Nawrocki, Jerzy
    Standzikowski, Karol
    Łanczont, Maria
    Gancarski, Jan
    Kłosowicz, Mateusz
    Leszczyński, Tomasz
    Powiązania:
    https://bibliotekanauki.pl/articles/51723225.pdf
    Data publikacji:
    2023
    Wydawca:
    Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
    Tematy:
    luminescence dating
    archaeomagnetism
    kilns
    bricks
    SE Poland
    Opis:
    The TL and OSL ages obtained from two ancient kilns and gothic to baroque bricks in the SE of Poland, were compared to their presumed historical ages and discussed. The luminescence ages of ancient kilns were also matched with the results of archaeomagnetic dating. The OSL and archaeomagnetic data indicates that the ancient kilns were last used not later than ca. 280 AD. This age corresponds well to the lower limit of the postulated age of fragments of Roman type storage vessels found in the filling of kilns. The OSL data used alone can point even to the end of the phase B2 of Roman influence in Poland. The TL ages obtained from the kilns (5297 ± 256 BC, 7092 ± 423 BC) are significantly older. These bottom parts of kilns, from which samples were taken, most probably were heated to a relatively low temperature, insufficient to reset the TL signal. Most of TL ages obtained from gothic to baroque bricks do not correlate with their historical ages. Unknown and most probably varied brick moisture contents in sampled ground floor walls and cellars does not allow to precisely date these bricks using the TL signal.
    Źródło:
    Acta Archaeologica Carpathica; 2023, LVIII; 117-133
    0001-5229
    2719-4841
    Pojawia się w:
    Acta Archaeologica Carpathica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Cambrian organic microfossils at the border area of the East- and West-European platforms (SE Poland and western Ukraine)
    Autorzy:
    Jachowicz-Zdanowska, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/191451.pdf
    Data publikacji:
    2011
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Cambrian
    palynology
    acritarchs
    stratigraphy
    SE Poland
    West Ukraine
    Opis:
    This paper contains palynological and stratigraphical characteristics of the selected Cambrian sections encountered in the basement of the north-eastern part of the Carpathian Foredeep and the Outer Carpathian margin in south-eastern Poland and western Ukraine, as well as verification of the stratigraphical position of rocks recognised so far in several sections in western Ukraine. The acritarch assemblages of the Cambrian System Series 2 are dominated by species of the characteristic early Cambrian genus Skiagia. The Cambrian Series 3 beds are documented by the assemblages with numerous specimens of the Adara alea, Cristallinium cambriense, Heliosphaeridium notatum, Eliasum llaniscum, Multiplicisphaeridium martae, and Comasphaeridium longispinosum. Furongian sediments are evidenced by strongly taxonomically diversified assemblages with large quantities of acritarchs, containing genera Timofeevia, Vulcanisphaera, Ninadiacrodium, Pirea, Leiofusa, Lusatia, or Polygonium, as well as taxa characterized by diacrodial symmetry. These assemblages are dominated by such genera, as: Dasydiacrodium or Acanthodiacrodium, and also by specimens with large polar opening of the central body, belonging to acritarchs of the “galeate” group. Within the studied Cambrian sediments, nine acritarch assemblages of differing composition were distinguished. These assemblages were correlated with faunistic zones. Ages younger than Palaeozoic, identified in some of the analysed Ukrainian sections, were determined basing on very well preserved assemblages of spores and pollen.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2011, 81, No 3; 241-267
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Reworked Eocene–Oligocene dinoflagellate cysts in the Miocene of the Carpathian Foredeep Basin : implications for Paleogene palaeogeography in SE Poland
    Autorzy:
    Gedl, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060511.pdf
    Data publikacji:
    2012
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    dinoflagellate cysts
    reworking
    epicontinental Paleogene
    palaeogeography
    SE Poland
    Opis:
    Miocene strata of the Carpathian Foredeep Basin in Poland contain reworked Eocene and Oligocene dinoflagellate cysts, which come from two sources: the Flysch Carpathians and the epicontinental basin. The occurrence of the latter is almost the only trace of the epicontinental Eocene–Oligocene sedimentary cover, which extended across southwestern Poland, and is today nearly completely eroded. The distribution of epicontinental Eocene and Oligocene taxa in the Miocene strata of the northeastern part of the Carpathian Foredeep is uneven, clearly pointing to a limited extent of the host deposits and their variable erosion intensity. Erosion of the Eocene and Oligocene platform cover took place prior the Miocene transgression and took place also during the Badenian; its intensity increased during Late Badenian–Sarmatian tectonic movements, resulting in an increased frequency of reworked specimens in strata postdating the mid-Badenian deposits.
    Źródło:
    Geological Quarterly; 2012, 56, 4; 853--868
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Eocene dinoflagellate cysts from the Sołokija Graben (Roztocze, SE Poland)
    Autorzy:
    Gedl, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060470.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    dinoflagellate cysts
    biostratigraphy
    Eocene
    epicontinental basin
    Roztocze
    SE Poland
    Opis:
    The Sołokija Graben is a tectonic structure in Roztocze, the south-eastern Poland, unique by its infill with the Eocene marine strata. The over 40 metres thick sandy succession is the only well-dated palaeontologically trace of Eocene marine transgression at Roztocze being virtually the only remains of the Eocene epicontinental sea in this part of Poland: the surrounding area is devoid of coeval marine strata, which were eroded. This makes the Sołokija Graben succession crucial for the palaeogeography reconstruction of the south-eastern Poland during Eocene as well as the tectonic history of this region. For its precise age determination, the over 30-m-thick succession of loamy sands that fill the Sołokija Graben in a borehole at Leliszka and a 4-m-thick one at Łaszczówka were sampled for dinoflagellate cysts. Samples from Łaszczówka are barren, whereas the ones from Leliszka contain rich and taxonomically diverse assemblages. Their biostratigraphical interpretation confirms previous results suggesting the Bartonian age of the most of the Sołokija Graben succession; the postulated Priabonian age of its non-calcareous part was documented in its uppermost part only. Palynological record allows reconstruction of sedimentary setting of the Leliszka succession. Basal part of the Bartonian was deposited in a shallow but relatively vast marine basin characterized by normal salinity and high energetic hydrodynamic conditions. Subsequently, marine basin underwent gradual shallowing and temporal cease of sedimentation. During the late Bartonian basin became brackish. A short-lasting early Priabonian marine basin was characterized by shallow marine conditions; it became brackish during its final stage. Comparison with neighbouring Eocene deposits of the epicontinental and Carpathian basins shows that the marine basin at Roztocze was presumably connected with both during Bartonian, and separated from the Carpathian one during early Priabonian. Factors controlling seaways pattern of the Roztocze basin were either eustatics and substratum tectonic movements, the former dominating during Bartonian, and interfingering with uplift of the Meta-Carpathian Swell during early Priabonian.
    Źródło:
    Geological Quarterly; 2014, 58, 4; 707--728
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Types of gullies and conditions of their development in silvicultural loess catchment (Szczebrzeszyn Roztocze region, SE Poland)
    Autorzy:
    Dobek, K.
    Demczuk, P.
    Rodzik, J.
    Hołub, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/294637.pdf
    Data publikacji:
    2011
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    gully in forest area
    gully types
    Roztocze region
    SE Poland
    Opis:
    The aim of this paper is to present a characteristic of loess permanent gullies, which form the branched erosion system, with the total length of almost 7.8 km, dissecting an erosion-denudation dry valley. Only 20%of the gully system catchment is cultivated as the result of steep slopes and considerable height differences up to 100 m. 80%of the catchment is covered by fir coniferous forest and Carpathian beech forest, and gully development is the result of intensive forest exploitation. Five types of gullies have been selected on the basis of the runoff directions, which are determined by the following: original relief, runoff concentration from fields, runoff concentration from fallplaces, skidding and course of forest roads used to carry a timber.
    Źródło:
    Landform Analysis; 2011, 17; 39-42
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Depositional environments of loesses from the Sandomierz section, SE Poland, based on lithological and SEM studies
    Autorzy:
    Kenig, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060219.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    SE Poland
    Sandomierz site
    loesses
    lithology
    quartz grains by SEM
    Opis:
    The litology of the Sandomierz section deposits have been examined, with SEM analysis performed on 4 quartz grain-size classes. All of the Sandomierz deposits contain predominant quartz grains with signs of aeolian transport. This refers both to morainic till and muds underlying the loess section as well to loesses them selves along with soil complexes. A much smaller, although significant contribution comprises redeposited grains with features of a high energy beach environment. Their content in creases up section. During sedimentation of the LMg (younger upper loess) deposits (later part of the Vistulian Glaciation) wind strength was in creasing. This is indicated by the upwards increasing content of coarser fractions within the interval, with simultaneously improved sorting, as well as by the increased contribution of garnets and the greater content of zircon and rutile at the top. The increasing contribution of aeolian quartz grains, the considerable content of grains redeposited from a beach environment and the decreasing amount of post-sedimentary features all suggest increased wind speed. Low variability in the shape of the 1–0.5 mm quartz grains from the LMg horizon indicates short transport and a similar nearby source of material. Alimentary areas for this horizon were composed of young Pleistocene muds and tills. A change in depositional conditions is observed at the LMs/LMg boundary (upper part of the Vistulian Glaciation). During deposition of the LMs (younger middle loess) horizon, wind strength decreased, as shown by the content of heavy minerals and the smaller mean grain-size along with the reduced content of aeolized quartz grains.
    Źródło:
    Geological Quarterly; 2008, 52, 2; 169-169
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Reservoir properties of the Palaeozoic–Mesozoic sedimentary cover in the Kraków–Lubaczów area (SE Poland)
    Autorzy:
    Kosakowski, P.
    Leśniak, G.
    Krawiec, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/191812.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    reservoir rocks
    petrophysical properties
    well logging
    Palaeozoic
    Mesozoic
    SE Poland
    Opis:
    During the 50-year-long intense petroleum exploration of the Palaeozoic–Mesozoic basement of the Carpathian Foredeep, more than 20 oil and gas accumulations have been discovered. The basic and most important oil-bearing levels in the Mesozoic section are Oxfordian carbonates and Cenomanian sandstones. The Nosówka, Zalesie, Trzebownisko–Krasne, Cetynia, Uszkowce and Lachowice hydrocarbon accumulations and numerous hydrocarbon shows have been found in the Palaeozoic horizons. This paper is focused on evaluation of reservoir properties of the entire Palaeozoic–Mesozoic basement of the Carpathian Foredeep and marginal part of the Outer Carpathians for finding new reservoir horizons. 558 rock samples from 51 wells in the Kraków–Lubaczów area were analysed. The well log results from 20 wells were additionally used for the assessment of petrophysical properties. The results of porosimetry measurements and well logs varied in all discussed Palaeozoic and Meso- zoic basement horizons of the Carpathian Foredeep. The best reservoir properties were estimated within the Jurassic–Lower Cretaceous carbonate complex. Despite great variability, the carbonate rocks display highest average porosity and good permeability values. The variability of reservoir properties is mostly a result of the character of the reservoir-porous-fracture space. Good reservoir properties were also estimated for the Upper Cretaceous carbonate rocks. However, in most of the analysed wells the potential reservoirs were watered. The Palaeozoic complex displays weaker reservoir properties and they mainly refer only to the Devonian–Lower Carboniferous horizon. The Lower Palaeozoic rocks display weak reservoir properties. Their potential is additio- nally lowered by negligible range of occurrence and a small thickness. Generally, the gas- and oil-bearing pro- perties of the analysed zone can be attributed only to the Jurassic–Cretaceous reservoir horizons. The remaining horizons, especially the Upper Palaeozoic complex, are only supplement to the reservoir potential of the area.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2012, 82, 1; 51--64
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zbiorowiska okrzemek rozwijające się na glebie uprawnej w Pogórskiej Woli koło Tarnowa
    Diatom assemblages growing on cropping soil in Pogórska Wola near Tarnów
    Autorzy:
    Stanek-Tarkowska, J.
    Noga, T.
    Kochman-Kędziora, N.
    Rybak, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/399500.pdf
    Data publikacji:
    2016
    Wydawca:
    Polskie Towarzystwo Inżynierii Ekologicznej
    Tematy:
    okrzemki glebowe
    bogactwo gatunkowe
    ekologia
    Polska SE
    soil diatoms
    species diversity
    ecology
    SE Poland
    Opis:
    Celem pracy było zbadanie różnorodności gatunkowej okrzemek rozwijających się na glebie pod uprawą pszenicy w Pogórskiej Woli koło Tarnowa oraz charakterystyka zbiorowisk okrzemek w oparciu o wybrane właściwości fizykochemiczne gleby. Badania prowadzono w okresie wegetacyjnym (od kwietnia do listopada 2011 r.), próbki powierzchniowej warstwy gleby pobierano w odstępach comiesięcznych. Badania fizykochemiczne wykazały odczyn kwaśny lub lekko kwaśny oraz niskie wartości uwilgotnienia (od około 6% w kwietniu i październiku do 1,93% w czerwcu). Łącznie oznaczono 47 taksonów okrzemek. Największym bogactwem gatunkowym charakteryzowały się rodzaje Luticola, Navicula i Mayamaea. Wyróżniono 8 gatunków dominujących, z których zdecydowaną większość stanowiły gatunki aerofityczne i glebowe. Najliczniejsze populacje tworzyły: Hantzschia amphioxys (Ehrenb.) Grunow, Luticola nivalis (Ehrenb.) D.G. Mann, Pinnularia borealis Ehrenb. var. borealis i Stauroneis borrichii (Petersen) Lund.
    Studies were conducted on a farmland located in the Pogórska Wola near Tarnów. The aim of the studies was to examine the species richness of diatoms growing on soil under wheat cropping in the Pogórska Wola and characteristic of diatoms assemblages based on selected physico-chemical parameters of soil. Studies were conducted in vegetation season (from April to November 2011). Samples were collected once a month. Soil reaction in each month was acid or slightly acid. Humidity was low and balanced between 6% in April and October down to 1.93% in June. 47 diatom taxa were recorded in total. The biggest species richness occurred in genus Luticola, Navicula and Mayamea. Eight taxa were considered as dominant from which the most was aerophytic and soli species. The biggest populations were created by: Hantzschia amphioxys (Ehrenb.) Grunow, Luticola nivalis (Ehrenb.) D.G. Mann, Pinnularia borealis Ehrenb. var. borealis and Stauroneis borrichii (Petersen) Lund.
    Źródło:
    Inżynieria Ekologiczna; 2016, 46; 128-134
    2081-139X
    2392-0629
    Pojawia się w:
    Inżynieria Ekologiczna
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Integrated biostratigraphy of Upper Maastrichtian chalk at Chełm (SE Poland)
    Autorzy:
    Dubicka, Z.
    Peryt, D.
    Powiązania:
    https://bibliotekanauki.pl/articles/191439.pdf
    Data publikacji:
    2011
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    biostratigraphy
    foraminifers
    ammonites
    belemnites
    chalk
    Upper Maastrichtian
    Border Synclinorium
    SE Poland
    Opis:
    A 40-m-thick section of chalk exposed in the Chełm quarry (SE Poland) contains a rather poor assemblage of macrofauna and a well diversified assemblage of foraminifers. The planktonic foraminifer assem- blages characterized by a considerable number of representatives of Globigerinelloides and Heterohelix and the presence of Guembelitria cretacea indicate the lowest part of the Guembelitria cretacea Zone sensu Peryt (1980). Benthic foraminifers point out that the strata of the Chełm quarry section can be attributed to the lower part of the Upper Maastrichtian: i.e., the Gavelinella danica/Brotzenella preacuta Zone of the European Boreal Province or the Anomalinoides pinguis Zone distinguished in Poland (except the Carpathians). The occurrence of ammonites, such as Hoploscaphites constrictus lviviensis Machalski, Hoploscaphites schmidi (Birkelund), and Acanthoscaphites varians blaszkiewiczi Jagt & al. indicates that the Chełm succession belongs to the lower part of the Belemnitella junior Zone, i.e., to the Belemnitella junior–Spyridoceramus tegulatus Zone sensu Schulz & Schmid (1983). The correlation of the Chełm quarry section and the Middle Vistula River Valley section indicates that the equivalent interval of the former section is not exposed in the Middle Vistula River Valley and that it would occur between the Chotcza and Lucimia villages within the lower part of the Belemnitella junior Zone, i.e., within the Belemnitella junior-Spyridoceramus tegulatus Zone distinguished in NW Germany (Schulz & Schmid,1983).
    Źródło:
    Annales Societatis Geologorum Poloniae; 2011, 81, No 2; 185-197
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Neolithic Flintworking of the Samborzec-Opatów Group in Lesser Poland in the Light of Settlement Materials from Tonie 9 Site, Kraków Commune
    Autorzy:
    Wąs, Marcin
    Powiązania:
    https://bibliotekanauki.pl/articles/38618429.pdf
    Data publikacji:
    2023
    Wydawca:
    Uniwersytet Rzeszowski. Instytut Archeologii Uniwersytetu Rzeszowskiego. Muzeum Okręgowe w Rzeszowie
    Tematy:
    Samborzec-Opatów group
    early Neolithic
    flint technology
    lithic analysis
    SE Poland
    Opis:
    The article presents flint materials obtained from settlement site of Samborzec-Opatów group from the Tonie 9 site in Lesser Poland. The flintworking of this unit is still poorly recognized. In the literature, special attention has mainly been paid to ceramic materials, especially in studies on the genesis of this group and its relations with other taxonomic units of the Neolithic in Lesser Poland (especially with the Malice culture and later groups of the Lendziel). Therefore, it is worth introducing the specificity of Samborzec-Opatów flintworking, especially since the recently arrived inventory from the Tonie 9 site is quite numerous and relatively homogeneous. Therefore, the main goal is to present materials that can be used for further studies, e.g. those of a comparative nature.
    Źródło:
    Analecta Archaeologica Ressoviensia; 2023, 18; 41-66
    2084-4409
    Pojawia się w:
    Analecta Archaeologica Ressoviensia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Early Neolithic Flint Assemblages from the Targowisko Settlement Region
    Autorzy:
    Wąs, Marcin
    Powiązania:
    https://bibliotekanauki.pl/articles/38605371.pdf
    Data publikacji:
    2021
    Wydawca:
    Uniwersytet Rzeszowski. Instytut Archeologii Uniwersytetu Rzeszowskiego. Muzeum Okręgowe w Rzeszowie
    Tematy:
    LBK
    Malice culture
    flint inustry
    early Neolithic
    Targowisko region
    SE Poland
    Opis:
    The article presents flint materials obtained from domestic facilities from the late phase of Linienbandkeramik from the Brzezie 40 and Targowisko 16 sites and the classic phase of the Malice culture from the 14–15 Targowisko site. These complexes contain relatively few monuments. Their advantage, however, is that they belong to chronologically compact groups. Since the relics of the discovered houses are spatially isolated from other settlement structures, it can be assumed that the set of flint artifacts belonging to them is relatively homogeneous. Thanks to this, they can contribute considerably to the discussion on the processes of cultural heterogenization and the origin of post-LBK cultures, including the Malice culture.
    Źródło:
    Analecta Archaeologica Ressoviensia; 2021, 16; 43-62
    2084-4409
    Pojawia się w:
    Analecta Archaeologica Ressoviensia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Archaeobotanical Macroscopic Plant Remains from the Early Neolithic Dwelling Structures at the Brzezie 40, Targowisko 16 and 14–15 Sites in Western Małopolska.
    Autorzy:
    Abramów, Joanna
    Powiązania:
    https://bibliotekanauki.pl/articles/2085869.pdf
    Data publikacji:
    2021
    Wydawca:
    Uniwersytet Rzeszowski. Instytut Archeologii Uniwersytetu Rzeszowskiego. Muzeum Okręgowe w Rzeszowie
    Tematy:
    LBK
    Malice culture
    macroscopic plant remains
    early Neolithic
    Targowisko region
    SE Poland
    Opis:
    The aim of this short article is to present the results of archaeobotanical analysis of macroscopic plant remains obtained in 2018–2019, during the test excavations carried out on three selected sites from Targowisko settlement region (Brzezie 40, Targowisko 16 and 14–15). Thanks to the field research strategy adopted, chronologically compact plant remains were obtained from objects included in the house structures, coming from narrow time horizons, equal to the operation time of individual Linienbandkeramik houses from the beginning of the Želiezovce phase (Brzezie 40 and Targowisko 16) and the phase of the classic Malice culture (Targowisko 14–15).
    Źródło:
    Analecta Archaeologica Ressoviensia; 2021, 16; 63-72
    2084-4409
    Pojawia się w:
    Analecta Archaeologica Ressoviensia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The oldest traces of human settlement in the vicinity of Ulów in Middle Roztocze (SE Poland)
    Autorzy:
    Wiśniewski, Tadeusz
    Powiązania:
    https://bibliotekanauki.pl/articles/52586550.pdf
    Data publikacji:
    2017
    Wydawca:
    Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
    Tematy:
    SE Poland
    Middle Roztocze
    Palaeolithic
    Mesolithic
    human settlement
    flint artefacts
    radiocarbon dating
    Opis:
    During the many years of archaeological research in the settlement micro-region in Ulów in Middle Roztocze, traces of human presence dated to Old and Middle Stone Ages (Palaeolithic and Mesolithic) were discovered. Most sources are flint materials, most of which lost their stratigraphic context due to subsequent settlement. At the current stage of research, their classification is possible only on the basis of a typological and comparative analysis. Most likely, the oldest traces of human occupancy in the vicinity of Ulów can be synchronized with a series of radiocarbon dating obtained for samples of charcoal from five different archaeological sites. The to-date discoveries have revealed new sources for research on the Palaeolithic and Mesolithic periods in south-eastern Poland.
    Źródło:
    Folia Quaternaria; 2017, 85; 49-64
    0015-573X
    2199-5915
    Pojawia się w:
    Folia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Petroleum processes in the Palaeozoic and Mesozoic strata between Tarnów and Rzeszów (SE Poland) : 2-D modelling approach
    Autorzy:
    Wróbel, M.
    Kosakowski, P.
    Krzywiec, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/191776.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    petroleum processes
    2D modelling
    Mesozoic
    Palaeozoic
    Tarnów–Rzeszów area
    SE Poland
    Opis:
    Two-dimensional modelling of hydrocarbon generation, expulsion, migration and accumulation pro- cesses in SE Poland between Tarnów and Rzeszów was carried out for five source rock horizons, i.e. the Ordo- vician, Silurian, Middle Devonian–Lower Carboniferous carbonates, Lower Carboniferous clastics, and Middle Jurassic. Five cross-sections in the study area allowed the reconstruction of timing and range of petroleum processes. The best source rocks related to the Ordovician and Silurian shales and mudstones reached “oil window” maturity within the entire study area and locally also reached the “gas window”. Generation of hydro- carbons was observed from all five source rocks, but the Ordovician and Silurian source rocks generated two and three times more hydrocarbons than the Lower Carboniferous and Jurassic source rocks, respectively. Expulsion took place only in case of the Lower Palaeozoic source rocks, but the volume of expelled hydrocarbons differed across the area. Hydrocarbons migrated from the Ordovician and Silurian source rocks to the Upper Jurassic (carbonates) and Upper Cretaceous (sandstones) reservoirs or to the Upper Palaeozoic carbonates in connection with the emplacement of the Carpathian thrust belt during the Miocene. Faults formed main migration pathways and hydrocarbons accumulated in structural and stratigraphic traps, located in the vicinity of faults. In places, traps are associated with a deep Miocene erosion surface. The onset of hydrocarbon generation took place during the Neogene, mainly the Miocene, but in the north, generation and expulsion started earlier – at the end of the Mesozoic.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2012, 82, 1; 81--97
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Water parameters and species composition of macrophytes in reclamation lakes in the area of a former sulphur borehole mine (SE Poland)
    Autorzy:
    Krawczyk, Rafał
    Lis, Łukasz
    Urbaniak, Jacek
    Powiązania:
    https://bibliotekanauki.pl/articles/763851.pdf
    Data publikacji:
    2016
    Wydawca:
    Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
    Tematy:
    post-mining lakes, sulphur mining, reclamation, aquatic vegetation, spontaneous succession, Jeziórko, SE Poland
    Opis:
    Macrophytes and selected physical-chemical water properties were studied in 17 post-mining lakes of Jeziórko Sulphur Mine – one of the largest borehole sulphur mines in the world. Artificial lakes were constructed in subsidence depressions during the reclamation process of mining fields. They were characterized by high mineralization – conductivity ranged from 723 to 2295 μS/cm. The reaction was near neutral, or more frequently, slightly alkaline. Concentrations of phosphorus and organic matter were low. In the group of hydrophytes, Ceratophyllum demersum, Myriophyllum spicatum, Najas marina, Utricularia vulgaris, Eleocharis acicularis, Potamogeton pectinatus, Potamogeton natans and Potamogeton pusillus were frequently dominant. In several lakes, large macroscopic algae dominated – charophytes forming large, dense Chara meadows. In marsh communities, Phragmites australis was the most expansive. Reclamation process had a positive effect on diversity, some of the species found in the study area are regionally rare, including one species which is threatened in Poland (Najas minor). No alien species were recorded.
    Źródło:
    Annales Universitatis Mariae Curie-Sklodowska, sectio C – Biologia; 2016, 71, 1
    2083-3563
    0066-2232
    Pojawia się w:
    Annales Universitatis Mariae Curie-Sklodowska, sectio C – Biologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Assessment of hydrocarbon potential of the Lower Palaeozoic strata in the Tarnogród–Stryi area (SE Poland and western Ukraine)
    Autorzy:
    Więcław, D.
    Kosakowski, P.
    Kotarba, M.J.
    Koltun, Y. V.
    Kowalski, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/191878.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    source rock
    hydrocarbon potential
    Cambrian
    Ordovician
    Silurian
    Carpathian Foredeep basement
    SE Poland
    Western Ukraine
    Opis:
    Quantity, genetic type and maturity of organic matter dispersed in the Lower Palaeozoic sequence from the Lower Cambrian to Silurian strata of the Polish and Ukrainian parts of the Carpathian Foredeep basement in the Tarnogród–Stryi area were evaluated based on the results of geochemical analyses of 475 rock samples collected from 45 wells. The best source rocks were found in the Silurian strata where the present total organic carbon (TOC) content is up to 2.6 wt%. They occur in the vicinity of Wola Obszańska, where the median of the present and the initial total organic carbon (TOC) contents in the individual wells amount to 0.98 and 1.6 wt%, respectively. The Cambrian and Ordovician strata have a poorer hydrocarbon potential and their present TOC content never exceeds 1 wt%. In all of the investigated Lower Palaeozoic strata, organic matter is represented by the oil-prone Type-II kerogen deposited in anoxic or sub-oxic conditions. The maturity of source rocks ranges from early mature (the initial phase of the low-temperature thermogenic processes) in selected zones of the Silurian strata in the vicinity of Wola Obszańska, through the middle and the final phase of “oil window” in the Ordovician and Cambrian strata in the Polish part of the study area, to the overmature stage in the Ordovician strata in the south-eastern part of the study area (Ukraine).
    Źródło:
    Annales Societatis Geologorum Poloniae; 2012, 82, 1; 65--80
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rozwój sedymentacji utworów ewaporatowych cechsztynu na obszarze rowu mazursko-lubelskiego (SE Polska)
    Development of Zechstein evaporites deposition in the area of Mazovia-Lublin Graben (SE Poland)
    Autorzy:
    Czapowski, G.
    Chełmiński, J.
    Małolepszy, Z.
    Nowacki, Ł.
    Powiązania:
    https://bibliotekanauki.pl/articles/2192086.pdf
    Data publikacji:
    2017
    Wydawca:
    Polskie Stowarzyszenie Górnictwa Solnego
    Tematy:
    ewaporaty
    cechsztyn
    model 3D
    rów mazursko-lubelski
    SE Polska
    evaporites
    Zechstein
    3D model
    Mazovia-Lublin Graben
    SE Poland
    Opis:
    Utwory ewaporatowe (siarczany i sole kamienne) cyklotemów PZ1, PZ2 i PZ3 cechsztynu występują w NW części rowu mazursko-lubelskiego (SE Polska), dla którego skonstruowano w latach 2012-2016. model 3D budowy geologicznej. Dostępne dane z otworów wiertniczych (karotaże, opisy rdzeni wiertniczych i prób okruchowych) pozwoliły ustalić warunki (głębokość, miąższość) i przypuszczalny zasięg występowania tych utworów oraz wyróżnić 8 typów facjalnych, reprezentujących różne środowiska depozycji. Opracowane mapy rozmieszczenia poszczególnych typów facji dla każdego z ewaporatowych wydzieleń litostratygraficznych oraz 3D wizualizacje rozmieszczenia głównych komponentów litologiczno- facjalnych wymienionych cyklotemów umożliwiły przedstawienie zmian środowisk depozycji w kolejnych cyklach cechsztynu w tej części rowu mazowiecko-lubelskiego.
    Evaporites (sulphates and halites) of Zechstein PZ1, PZ2 and PZ3 cyclothemes occur in the NW part of Mazovia-Lublin Graben (SE Poland), for which the 3D model of geological structure was created in 2012-2016. Available geological data from boreholes (well logs and descriptions of cores and crushed rock samples) enabled to precise the occurrence parameters (depth and thickness) and the supposed extent of studied evaporites as well as to define 8 facies types, represented various depositional settings. Several maps, illustrating facies distribution of each evaporitic lithostratigraphic unit, supported with 3D images of main lithological-facies components of mentioned cyclothemes allowed to comment the environmental changes in the Mazovia-Lublin Graben area during evaporitic periods of studied cyclotheme successions.
    Źródło:
    Przegląd Solny; 2017, 13; 75--93
    2300-9349
    Pojawia się w:
    Przegląd Solny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Diurnal variations and vertical distribution of δ13C, and concentration of atmospheric and soil CO2 in a meadow site, SE Poland
    Autorzy:
    Szaran, J.
    Dudziak, A.
    Trembaczowski, A.
    Niezgoda, H.
    Hałas, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2058901.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    SE Poland
    atmospheric CO2
    carbon dioxide concentration
    diurnal observations
    delta 13C
    soil CO2
    Opis:
    We provide the results of 24-hour observations made in a meadow site located in a small river valley in Central Europe. Samples of atmospheric air were taken from three horizons: near the soil (0.05 m), in the grass (0.5 m) and above the meadow (2 m) at two-hour intervals. At the same time, samples of soil air were collected from two horizons: -0.1 and -0.5 m. We have found a variation of δ13C above the ground from -6‰ during the day to -20‰ late at night accompanied by variations in CO2 concentration from 270 ppm during the day, to various levels late at night at different heights above the ground. The maximum concentration was 1430 ppm at the ground level. The correlation coefficient between δ 13C and reciprocal of concentration was the highest (R2 = 0.984) for the samples collected 2 m above the ground, the regression line clearly indicating CO2 mixing from the two sources: atmospheric and biogenic reservoirs. The intercept of the mixing line yields δC = -23.0‰ for the biogenic CO2. In contrast, the diurnal variations in the soil were relatively small, δ13C varied from -21.6 to -23.4‰, while CO2 concentration from 4300 to 8200 and from 24 700 to 34 500 ppm at depths of 0.1 m and 0.5 m respectively, which is less than 2-fold. Small diurnal variations are characteristic of dry soils, where δ13C is weakly correlated with CO2 concentration (in our case R2 was 0.30 and 0.54, respectively).
    Źródło:
    Geological Quarterly; 2005, 49, 2; 135--144
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ocena i przyczyny zanieczyszczenia azotanami wód podziemnych w zachodniej części Polesia Lubelskiego i Wołyńskiego
    The assessment and reasons of nitrates contamination within the uppermost aquifer in the western part of Polissia region (SE Poland)
    Autorzy:
    Kaczor-Kurzawa, D.
    Powiązania:
    https://bibliotekanauki.pl/articles/296979.pdf
    Data publikacji:
    2015
    Wydawca:
    Politechnika Częstochowska. Wydawnictwo Politechniki Częstochowskiej
    Tematy:
    pierwszy poziom wodonośny
    zanieczyszczenie azotanami
    wrażliwość wód podziemnych
    Polesie (SE Polska)
    Upper Aquifer
    nitrates contamination
    vulnerability of the groundwater
    Polissia region
    SE Poland
    Opis:
    W pracy przedstawiono stan zanieczyszczenia wód pierwszego poziomu wodonośnego azotanami na obszarze zagospodarowanym rolniczo (około 300 km2) w zachodniej części Polesia Zachodniego (Lubelskiego) i Wołyńskiego. Zawartość azotanów została zbadana w wodach podziemnych metodą fotometryczną za pomocą fotometru Slandi LF300 w 31 punktach dokumentacyjnych (studniach kopanych, studni wierconej, źródłach i sondach ręcznych). Zanieczyszczenie wód azotanami (o zawartości powyżej 50 mg NO‾3 /dm3) stwierdzono w 10 próbkach wody (32% populacji danych), a stan zagrożenia tym zanieczyszczeniem (o zawartości 25÷50 mg NO‾3 /dm3) odnotowano w 5 punktach. Stwierdzone zanieczyszczenie wód pierwszego poziomu ma charakter lokalny i związane jest głównie z nieuporządkowaną gospodarką komunalną oraz złym stanem sanitarnym gospodarstw rolnych. Migracji zanieczyszczeń transportowanych przez infiltrujące wody opadowe z powierzchni terenu do systemu wodonośnego sprzyjają dobre własności filtracyjne skał strefy aeracji i płytkie występowanie poziomu wód podziemnych (do 5 m). Naturalna podatność rozpatrywanego poziomu wodonośnego na ponad 90% powierzchni terenu badań jest wysoka i bardzo wysoka, co powoduje, że czas przenikania wód (z zanieczyszczeniami) wynosi tu odpowiednio do 5 lat (dla około 30% powierzchni terenu - podatność bardzo wysoka) i 5-25 lat (dla około 65% powierzchni terenu - podatność wysoka).
    This paper presents research concerning nitrates contamination within the Uppermost Aquifer on 300 km2 study area in Polissia region, SE Poland. The analysis of nitrate concentration was conducted with the use of field-gauges set SLANDI. 31 analyzed groundwater samples were collected from hand-dug wells, pumping wells, springs and water-sampling probes. The nitrates pollution of groundwater (NO‾3 > 50 mg/dm3) was confirmed for 10 samples (32% of population), and potential nitrate pollution hazard (NO‾3 > 50 mg/dm3) was determined for 5 groundwater samples. Such results were determined in samples coming from the following villages: Stefanów, Wólka Cycowska, Przymiarki, Kolonia Wesołówka, Sławek, Stręczyn Nowy, Buza, Chojeniec, Romanówka, Stasin Dolny, Świerszczów, Zgniła Struga, Biekiesza and Dorohucza. High nitrates concentration within the Uppermost Aquifer were confirmed only locally, nearby farms characterized by invalid sanitary condition. In such cases the nitrate pollution of groundwater was caused mostly by waste from farming production and/or leaking septic tanks. High nitrates concentration was usually connected with high content of sulfates (from 57.5 up to 267.2 mg/dm3) and chlorides (Cl‾ from 15.4 up to 97.3 mg/dm3). Relatively high rate of nitrate pollution migration, from the land surface towards the Uppermost Aquifer, resulted from the specific construction of vadose zone, which is built of permeable sands and limestone. Additionally, groundwater table is situated on the depth up to 5 m below land surface. The above mentioned conditions caused that, the greater part of the examined area is characterized by high vulnerability (65% of the area) or extremely high vulnerability (30%) to anthropogenic contamination. Vertical migration time of anthropogenic pollution, transported by infiltrating water from the land surface to the aquifer, is estimated on less than 5 years for the areas of extremely high vulnerability, and on 5 up to 25 years for the areas of high vulnerability.
    Źródło:
    Inżynieria i Ochrona Środowiska; 2015, 18, 2; 141-153
    1505-3695
    2391-7253
    Pojawia się w:
    Inżynieria i Ochrona Środowiska
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Iły krakowieckie jako wskaźnik litostratygrafii w dolinie rzeki Sopot na Roztoczu
    The Krakowiec Clays as an indicator of lithostratigraphy in the Sopot River valley in the Roztocze Region (estern Poland)
    Autorzy:
    Janiec, B.
    Czarnecka, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074422.pdf
    Data publikacji:
    2006
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    iły krakowieckie
    mikrofauna
    paleontologia
    litostratygrafia
    Roztocze
    Krakowiec clays
    microfauna
    paleontology
    residuum
    lithostratigraphy
    river valley
    Roztocze region
    SE Poland
    Opis:
    The results of micropaleonthological studies of the Sarmatian (upper Miocene) Krakowiec Clays from primary deposit as well as re-deposited ones were applied to the analysis of the stratigraphic profile of the Sopot valley fills. The study site was at the break section of the Sopot River valley in a contact zone of southern escarpment between the central part of the Roztocze and Sandomierz Basin regions (SE Poland). Species of fossil microfauna (foraminiferans, radiolarians), sponges and mollusks, as well as residual deposits were used. The documented, even if apparently small change in the lithostatigraphic profile of the Sopot valley fills, i.e., the presence of pre-Pleistocene deposits in its floor, is very important for the valley history and for interpreting other problems of river breaks and the Roztocze escarpment zone itself, e.g., sclae of the Holocene movements elevating the Roztocze Region, and their effect on expected intensity of deep fluvial erosion. In the sub-scarp zone of the Tomaszów Roztocze subregion the Krakowiec Clays occur rather shallowly. In the Sopot valley (‘Czartowe Pole’landscape preserve) they are in contact with calcareous formations. In two levels of natural clays’exposures, a dozen or so foraminiferan taxa were found. They were also below the primary deposit on the floor levels of the Sopot valley fills. The residuum of the studied strata consists of glauconite and pre-Pleistocene quartz sands, without silicate and alumosilicate, typical for postglacial formations. The Sarmatian clays present in residue were redeposited at least in the pre-Pleistocene. From the clays top up to the surface of valley fills, are Holocene deposits. The study revealed that: (1) during the Holocene and earlier the Sopot valley fills were not removed completely; (2) the floor of the valley is made not of the youngest, Holocene strata, but much older; (3) the presence of the Sarmatian microfauna in the alluvia allows to date the studied deposits as pre-Pleistocene (Pliocene?); (4) fine quartz sands and glauconite (a specific form of hydromica) both forming the residuum of the studied valley fill levels, together with the absence of other silicates and alumosilicates that are common in the Pleistocene formations, exclude the studied Krakowiec Clays from the group of glacial or fluvioglacial (Pleistocene) formations; (5) the youngest (latest Pleistocene –Holocene) movements elevating the Roztocze Region and the resulting deep fluvial erosion do not correspond with shallow occurrence of the pre-Pleistocene valley fills; this requires further discussion.
    Źródło:
    Przegląd Geologiczny; 2006, 54, 10; 913-918
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Retardacja przekształcania zasobów przyrodniczych w południowo-wschodniej Polsce w świetle wybranych dokumentów strategicznych
    The retardation of natural resources transformation in southeastern Poland in the light of selected strategic documents
    Autorzy:
    Baran-Zgłobicka, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/400072.pdf
    Data publikacji:
    2013
    Wydawca:
    Polskie Towarzystwo Inżynierii Ekologicznej
    Tematy:
    środowisko przyrodnicze
    planowanie strategiczne
    retardacja
    Polska SE
    natural environment
    strategic planning
    retardation
    Poland SE
    Opis:
    Powstrzymanie nadmiernej eksploatacji zasobów nieodnawialnych, ale w pewnym stopniu i tych odnawialnych, stanowi ogromne wyzwanie w kontekście zachowania ich dla przyszłych pokoleń. Problem retardacji zasobów przyrodniczych powinien być rozpatrywany w aspekcie: zasobów ożywionych, zasobów nieożywionych (w tym racjonalnej eksploatacji surowców mineralnych i zasobów wodnych), ograniczenia emisji szkodliwych substancji do środowiska, nadmiernej produkcji i składowania odpadów oraz zahamowania degradacji przestrzeni. Jednocześnie zakres korzystania z zasobów przyrody i ich ochrony regulują odpowiednie akty prawne oraz zapisy w dokumentach strategiczno-planistycznych. Ujęcie problemów retardacji na etapie programowania i planowania pozwala podejmować właściwe decyzje w procesie zarządzania środowiskiem na różnych poziomach podziału terytorialnego kraju. Do badań wybrano obszar południowo-wschodniej Polski. Region charakteryzuje się ogromnym zróżnicowaniem środowiska przyrodniczego, którego zasoby od wieków były intensywnie wykorzystywane i przekształcane. Prace szczegółowe prowadzono w wybranych, zróżnicowanych funkcjonalnie powiatach i gminach województwa lubelskiego, podkarpackiego i świętokrzyskiego. Analizowano, w jakim stopniu retardacja przekształcenia zasobów przyrodniczych jest uwzględniana i przedstawiana w dokumentach strategicznych.
    Stopping the overexploitation of non-renewable and, to some extent, renewable resources represents an enormous challenge in the context of preserving these resources for the future generations. The problem of mitigating the transformation of natural resources should be viewed from the perspective of animate and inanimate nature (including the rational use of mineral and water resources), reducing the emission of harmful substances to the environment, excessive production and storage of waste as well as stopping the degradation of space. At the same time, the scope of using natural resources and protecting them is regulate d by relevant legislation and provisions in strategic and planning documents. Taking into account the problems of mitigation at the programming and planning stage enables making appropriate decisions in the environment management process at various levels of local government. The area selected for study was south-eastern Poland. The region is characterised by a great diversity of its natural environment, whose resources have been intensively used and transformed for several centuries. Detailed studies were conducted in selected, functionally varied counties and municipalities of the Lubelskie, Podkarpackie and Świętokrzyskie provinces. It was analysed to what extent the retardation of natural resources transformation was taken into accountand presented in strategic documents.
    Źródło:
    Inżynieria Ekologiczna; 2013, 34; 76-88
    2081-139X
    2392-0629
    Pojawia się w:
    Inżynieria Ekologiczna
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Problemy rozwoju lokalnego Starej Kalinowszczyzny (Lublin)
    Autorzy:
    Samojedna, Edyta
    Janicki, Grzegorz
    Powiązania:
    https://bibliotekanauki.pl/articles/763289.pdf
    Data publikacji:
    2018
    Wydawca:
    Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
    Tematy:
    spatial management, problem area, historical city quarter, SWOT, Poland SE
    zagospodarowanie przestrzenne, obszar problemowy, historyczna dzielnica miasta, SWOT, Polska SE
    Opis:
    The paper analyzed the conditions of local development and showed evaluation of the current socio-economic and functional-spatial situation of the historical quarter of the Lublin City so called commonly as Stara Kalinowszczyzna. The main aims of this study was determined potential directions of development of this problem area. Based on the of detailed study (urban inventory, strategic and planning documents analysis, questionnaire research and SWOT analysis) were proposed important activities for further development of this area, such as: activation of inhabitants, improvement of the management status and use of the cultural heritage potential. Stara Kalinowszczyzna has unusual potential resulting from many historical objects, monuments and attractive scenic views of the Old City. Through to appropriate activities aimed at promoting, protecting and improving attractiveness, this area has a chance to become a leading tourist product of the city.
    W pracy przedstawiono uwarunkowania rozwoju lokalnego oraz ocenę obecnej sytuacji społeczno-ekonomicznej i funkcjonalno-przestrzennej historycznej części dzielnicy Kalinowszczyzna w Lublinie, nazywanej potocznie Starą Kalinowszczyzną. Zasadniczym celem badań było wyznaczenie głównych kierunków rozwoju tego obszaru problemowego. W wyniku przeprowadzonych badań (inwentaryzacja urbanistyczna, analiza dokumentów strategicznych i planistycznych oraz badania ankietowe i analiza SWOT) zaproponowano istotne dla dalszego rozwoju badanego obszaru działania, takie jak: aktywizacja mieszkańców, poprawa stanu zagospodarowania oraz wykorzystanie potencjału dziedzictwa kulturowego. Stara Kalinowszczyzna posiada niezagospodarowany potencjał wynikający z nagromadzenia obiektów historycznych, zabytków oraz atrakcyjnych ekspozycji widokowych na Stare Miasto.
    Źródło:
    Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; 2018, 73
    0137-1983
    Pojawia się w:
    Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Wpływ działalności przemysłowej na drzewostany sosnowe w rejonie Tarnobrzega w świetle analizy dendrochronologicznej
    The influence of industry on Scots pine stands in the Tarnobrzeg area on the basis of dendrochronological analysis
    Autorzy:
    Barniak, J.
    Krąpiec, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/1009636.pdf
    Data publikacji:
    2009
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    Tarnobrzeski Okreg Przemyslowy
    lesnictwo
    drzewostany sosnowe
    dendrochronologia
    zanieczyszczenia przemyslowe
    oddzialywanie na srodowisko
    tereny przemyslowe
    sosna zwyczajna
    przyrosty roczne
    Pinus sylvestris
    tree−ring analysis
    industrial pollution
    pinus sylvestris
    tarnobrzeg region
    se poland
    Opis:
    Tree−ring analysis has been used to evaluate the influence of industrial pollution on Scots pine (Pinus sylvestris) growing in the Tarnobrzeg region. 237 samples were taken from stands located in two profiles to picture dependence of health conditions of trees on distance from the emitter. The Tarnobrzeg Sulphur Works was the main source of pollution in that region. Factories in Mielec and Nowa Dęba as well as the Połaniec Power Plant could be additional sources of emission. Response of trees to anthropogenic stress was clearly visible in the years 1970−1990, when growth reductions occurred at the majority of the investigated trees. At the beginning of 1990s the decreasing trend stopped and wider tree−rings could be observed.
    Źródło:
    Sylwan; 2009, 153, 12; 825-835
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    „Ludowy” adwokat i obrońca wojskowy. Rzecz o Mieczysławie Maślanko (1903–1986)
    The “advocate” of the People and Military Defender. Remarks on Mieczyslaw Maslanko (1903–1986)
    Autorzy:
    Zaborski, Marcin
    Powiązania:
    https://bibliotekanauki.pl/articles/621430.pdf
    Data publikacji:
    2015
    Wydawca:
    Uniwersytet w Białymstoku. Wydawnictwo Uniwersytetu w Białymstoku
    Tematy:
    samorząd adwokacki w komunistycznej Polsce, obrońcy wojskowi, tajny wykaz obrońców, Naczelna Rada Adwokacka, procesy polityczne w komunistycz- nej Polsce, sądy wojskowe w komunistycznej Polsce, tajne procesy
    Bar association in communist Poland, Court-martial defence attorneys, Se- cret register of attorneys, Supreme Council of Attorneys, Political trials in communist Poland, Courts-martial in communist Poland, Secret trials
    Opis:
    Mieczysław (Moses) Maślanko (1903–1986) was one of the most prominent personalities among the lawyers of communist Poland between 1945 and 1956. He was born in War- saw in a Jewish family. In Warsaw, he finished his secondary education and graduated from the law department of Warsaw University in 1926. Between 1927 and 1933, he took a court and defence attorney internship and became a registered attorney. During the German occupation of Poland in 1939–1945, he was persecuted by the Ger- mans. Until 1943, he was kept prisoner in the Warsaw Ghetto where he was appointed Chairman of the Disciplinary Court at the Judenrat. Between April 1943 and May 1945, he was imprisoned in the Majdanek concentration camp, Auschwitz concentration camp, and Sachsenhausen concentration camp. Upon his return to Warsaw, he resumed his work as attorney. He specialised in criminal cases. The communist authorities allowed him to participate in the court trials of the regime opponents. He defended (participated) in political trials before military courts and before the so-called “secret courts-martial” which in fact were a travesty of justice. He was admitted to the register of court-martial attorneys and his name showed also in the “secret registers”, i.e. of attorneys who were authorised to participate in secret trials. His contribution to the most famous trials of the opponents of the communist regime was to support the statements of the prosecution. In 1946-1956, he was a member of the Supreme Council of Attorneys (Bar association) which was in fact filled by way of a decision of the Minister of Justice. After 1956, the attorneys representation bodies filed several disciplinary cases against him. After 1956, he continued to work as a criminal defence attorney.
    Źródło:
    Miscellanea Historico-Iuridica; 2015, 14, 2; 389-416
    1732-9132
    2719-9991
    Pojawia się w:
    Miscellanea Historico-Iuridica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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