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    Tytuł:
    Evidence of soils and paleosols in the Poznań Formation (Neogene, Polish Lowland)
    Autorzy:
    Duczmal-Czernikiewicz, A. M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059716.pdf
    Data publikacji:
    2013
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Poznań clays
    Neogene
    Polish Lowland
    pedostructures
    Opis:
    A succession of stacked paleosol profiles was recognized in open pits in the western Wielkopolska region (Poland). Field observations and micromorphological studies made it possible to distinguish the following pedostructures, formed in contrasting environments: soil horizons, crystallaria, concretions, redoximorphic structures, Fe-Mn globulae and slickensides. In both soils (Holocene) and paleosols (Pleistocene or/and Pliocene?), surface horizons are present (horizon A), marked by rhizocretions. There are two separate carbonate soils. One of them contains calcite concretions and gypsum pedofeatures, presumably formed in arid or semi-arid conditions. Two of the soil profiles are probably truncated, and only subsurface horizons are present (horizon B). In some cases, paleosols are separated by sediment layers slightly influenced by pedogenesis (horizon BC). Carbonate soils (Bk) indicate water deficit during their formation. The presence of horizons with slickensides (Bss) indicates intervals with contrasting seasonal climates (wet and dry cycles). The profiles were influenced by gleying processes which caused redistribution of iron oxides and formation of iron and iron-manganese concretions. The pedostructures recognised reflect different climatic conditions as well as humidity changes during the time of their formation.
    Źródło:
    Geological Quarterly; 2013, 57, 2; 189--204
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Fennoscandian erratics in glacial deposits of the polish lowland - Methodical aspects
    Autorzy:
    Górska, Maria
    Powiązania:
    https://bibliotekanauki.pl/articles/2027069.pdf
    Data publikacji:
    2006
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    indicator and statistical erratics
    glacial deposits
    Polish Lowland
    Vistulian
    Opis:
    In the gla cial de pos its of the Pol ish Low land, there are er ratic boul ders drifted with the last con ti nen tal ice sheet. Their out crops are situ ated in the Bal tic Shield area as well as south of it, in the bot tom of the cen tral and south ern Bal tic Sea. In di ca tor er rat ics, sta tis ti cal er rat ics and the oth ers can be dis tin guished in coarse- gravels as so cia tions. The stud ies on iden ti fi ca tion of the in di ca tor er rat ics are de signed for speci fi ca tion of the Scan di na vian and Bal tic ali men ta tion cen - tres of gla cial tills of dif fer ent age and their flu vio gla cial coun ter parts; they are also aimed at de ter min ing the di rec tion of the dis tant trans port as well as the ice- sheet and its streams’ trans gres sion routes to the depo si tion places. Ef fec tive - ness of the analy sis de pends to a large ex tent on the cor rect clas si fi ca tion of er rat ics, and this abil ity hap pens in turn to be bur dened with a sub jec tive evalua tion of the clearly visi ble fea tures of an er ratic. In the pres ent pa per, an at ten tion is paid to ad van tages and dis ad van tages of the analy sis on the in di ca tor boul ders of the gla cial de pos its.
    Źródło:
    Studia Quaternaria; 2006, 23; 11-15
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Freshwater lichens on submerged stones and alder roots in the Polish lowland
    Słodkowodne porosty na zanurzonych kamieniach i korzeniach olsz na Niżu Polskim
    Autorzy:
    Hachulka, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/67531.pdf
    Data publikacji:
    2011
    Wydawca:
    Polskie Towarzystwo Botaniczne
    Tematy:
    aquatic lichen
    lichen
    submerged stone
    stone
    Polish lowland
    lowland
    freshwater habitat
    tree root
    Opis:
    The article presents the results of the studies of lichens in streams and spring areas of the escarpment zone of Wzniesienia Łódzkie Heights in Central Poland. The boulders, stones and roots of Alnus glutinosa, situated in 3 inundated zones in the streams: submerged zone, fluvial mesic zone and fluvial xeric zone, were examined in the streams. The studies have shown 23 species connected with these streams. Six species of freshwater lichens: Verrucaria aquatilis, V. hydrela, Hydropunctaria rheitrophila, V. margacea, V. praetermissa and V. madida, occupied stones in 3 different zones. Verrucaria aquatilis and Hydropunctaria rheitrophila colonized also secondary substrates – the bark of alder roots incrusted with sand grains and silt.
    W rzekach i strumieniach Parku Krajobrazowego Wzniesień Łódzkich, w Polsce Środkowej, odnotowano 23 gatunki porostów wodnych (Tab. 2), z którymi konkuruje o podłoże 7 gatunków mszaków. Sześć ściśle wodnych gatunków naskalnych znajduje się na czerwonej liście porostów zagrożonych Polski (Cieśliński et al. 2006). Większość porostów wodnych rośnie w odcinkach początkowych rzek i strumieni, co prawdopodobnie wynika z korzystnych warunków fizykochemicznych wód (Tab. 1) i wzrostu zanieczyszczenia w dalszym biegu rzek. Badania porostów wodnych wykazały ich rozmieszczenie w trzech strefach: 1 − całkowicie zatopionej, 2 − często zatapianej i 3 − sporadycznie zatapianej lub spryskiwanej wodą (Fig. 2). W drugiej i trzeciej strefie zanurzenia, w towarzystwie Coenogonium pineti, Arthonia spadicea i Absconditella lignicola (Tab. 2) rośnie Bacidina sulphurella (Fig. 5), rzadki porost w Polsce. W badanych rzekach obligatoryjne epility wodne rosną na głazach i kamieniach, jedynie Hydropunctaria rheitrophila (Figs 3 A, B) i Verrucaria aquatilis zasiedlają także korę korzeni olsz często pokrytych ziarnami piasku i mułem. Kolonizowanie podłoży zastępczych przez epility wodne obserwowano w Alpach (Thüs and Schultz 2009), w północno-wschodniej i wschodniej Europie (Motiejūnaitė 2003, 2009; Pykälä 2006; Motiejūnaitė, Czyżewska 2008), również w Polsce Północno-Wschodniej (Czyżewska et al. 2001).
    Źródło:
    Acta Mycologica; 2011, 46, 2
    0001-625X
    2353-074X
    Pojawia się w:
    Acta Mycologica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Polymorphism of insulin-like growth factor (IGF-1) gene in Polish Lowland sheep from Podlaskie voivodship
    Polimorfizm genu czynnika insulinopodobnego IGF-1 u polskich owiec nizinnych utrzymywanych w województwie podlaskim
    Autorzy:
    Niznikowski, R.
    Czub, G.
    Kaminski, J.
    Nieradko, M.
    Swiatek, M.
    Glowacz, K
    Slezak, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2890.pdf
    Data publikacji:
    2014
    Wydawca:
    Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie
    Tematy:
    gene polymorphism
    insulin-like growth factor
    Polish Lowland breed
    sheep
    Podlasie voivodship
    Opis:
    Research was carried out on 432 Polish Lowland Sheep (405 ♀ and 27♂) of three varieties: Corriedale, Żelaźnieńska Sheep and Polish Lowland Sheep of Podlasie region. All animals were subjected to gene identifi cation factor insulin – IGF-1, in the assessment of alleles C and T. In conclusion it should be noted that in the three examined varieties of Polish Lowland Sheep showed no polymorphism in exon 3 of the insulin-like growth factor (IGF-1) gene, limiting its scope to determine the allele C, respectively genotype CC. This result indicates the need for further research in this area in “culture” sheep imported and adapted to Polish conditions and the production environment.
    Polimorfizm genu czynnika insulinopodobnego IGF-1 u polskich owiec nizinnych utrzymywanych w województwie podlaskim. Badania przeprowadzono na materiale 432 polskich owiec nizinnych (405 ♀ i 27♂) trzech odmian: corriedale, owcy żelaźnieńskiej i polskiej owcy nizinnej regionu podlaskiego. Wszystkie zwierzęta były poddane identyfikacji genu czynnika insulinopodobnego IGF-1, w zakresie oceny występowania alleli C i T. Podsumowując, należy stwierdzić, iż u badanych trzech odmian polskich owiec nizinnych nie wykazano polimorfizmu występowania alleli i genotypów genu czynnika insulinopodobnego IGF-1, ograniczając jego zakres do ustalenie jedynie do allelu C i genotypu CC. Wynik ten wskazuje na potrzeby przeprowadzenia dalszych badań z tego zakresu u owiec kulturowych pochodzących z importu i adaptowanych do polskich warunkach środowiska produkcyjnego.
    Źródło:
    Annals of Warsaw University of Life Sciences - SGGW. Animal Science; 2014, 53
    1898-8830
    Pojawia się w:
    Annals of Warsaw University of Life Sciences - SGGW. Animal Science
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Sorption of Pb and Cd by sediments of the polygenetic river valleys of the eastern part of the Polish Lowland
    Autorzy:
    Falkowska, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059178.pdf
    Data publikacji:
    2003
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Polish Lowland
    river valleys
    sorption of Pb and Cd
    contamination
    sorption isotherms
    Opis:
    Sediments, filling the polygenetic, melt-out river valleys of the eastern part of the Polish Lowland and adjacent areas are characterised by various sorption capacities in relation to Pb and Cd. Valley bottoms and ice-dammed basins within the morainic plateau are built of peats, mucks and warps, which bond 98% of the added heavy metals from the input solution with concentrations of 1 to 20 mg/dm3. These sediments, occurring also in the form of horizontal and continuous layers, form natural isolation barriers protecting the groundwaters against pollution with lead and cadmium. Deposits which build the adjacent morainic plateau and which contain over 20% of clay fraction also possess very high sorption capacities in relation to Pb and Cd. Sandy sediments of kames and kame terraces are characterised by the lowest sorption capacities to lead and cadmium. The content of organic matter and to a lesser extent the clay mineral composition determines the sorption capacities of lacustrine and marsh sediments. In the case of the clastic deposits of the morainic plateau, the value of this parameter depends on the quantity and composition of the clay fraction, and on the presence of CaCO3 and oxides and hydroxides of Fe, Al and Mn. The sorption of lead by peats and warps for delivered input solutions (5–100 mg/dm3), in most cases, are described by Henry’s isotherms whereas the sorption of cadmium is described by Freundlich’s isotherms. The sorption of lead as well as cadmium by mineral and organic-mineral sediments are described by Freundlich’s isotherms.
    Źródło:
    Geological Quarterly; 2003, 47, 2; 169-186
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Baeothryon alpinum (L.) T.V. Egorova (Cyperaceae) in the Polish Lowlands: distribution, population decrease and implications for conservation
    Autorzy:
    Pawlikowski, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/57279.pdf
    Data publikacji:
    2010
    Wydawca:
    Polskie Towarzystwo Botaniczne
    Tematy:
    Baeothryon alpinum
    Cyperaceae
    Polish Lowland
    plant distribution
    plant population
    plant conservation
    threatened plant
    locality
    Opis:
    A total of 47 localities of Baeothryon alpinum, hosting population of more than 100 000 shoots, were recorded in the lowland part of Poland during field surveys in the years 2003-2009. Among them were 25 populations discovered for the first time. Out of 57 sites of the species known from literature and unpublished (including herbarium) sources, 35 were not confirmed during the survey, 27 of them being definitely extinct. B. alpinum shows a clear pattern of distribution in Poland, with three main areas of occurrence: 1) the north-easternmost Poland (Lithuanian Lake District with the adjacent parts of the Masurian Lake District and the upper Biebrza river valley in North Podlasie Lowlands), which is part of the species boreal main range; 2) scattered localities in north-western Poland; 3) mountain mires at higher altitudes in the Sudetes and Tatra mountains and the adjacent part of southern Poland. The main aggregation of localities is found in Augustów Forest (including the Sejny Lakeland and Wigry National Park), and in the Góry Sudawskie region with adjacent areas. The biggest Polish population in the "Kobyla Biel" fen near Augustów consisted of several dozens of thousands of shoots. The Lithuanian Lake District is an area of general importance for the conservation of B. alpinum in Poland. The species is threatened, first of all, due to secondary succession (mires overgrowing with shrubs, trees and reed) and requires conservation measures as well as establishing nature reserves in places where it occurs. The degree that B. alpinum decreases in number is strikingly different in particular regions of Poland - it has lost most of its localities in north-western Poland and in Masurian Lake District, while in the Lithuanian Lake District and the upper Biebrza valley there are minor losses only. Depending on the region (from the west to the east and from the south-west to the north-east), the species should be given extinct or critically endangered (regions of north-western and southern Poland), endangered (Masurian Lake District), vulnerable (North Podlasie Lowlands) and near threatened (Lithuanian lake District) status. Although the disappearance of the populations beyond the species main range is a common phenomenon, the presented pattern is man-related and connected with differences in land management.
    Źródło:
    Acta Societatis Botanicorum Poloniae; 2010, 79, 3
    0001-6977
    2083-9480
    Pojawia się w:
    Acta Societatis Botanicorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Transformation from natural (thermal contraction) to anthropogenic (resource exploitation) depressions in the Krotoszyn-Koźmin-Raszków area (Polish Lowland)
    Autorzy:
    Stankowski, Wojciech
    Powiązania:
    https://bibliotekanauki.pl/articles/94711.pdf
    Data publikacji:
    2012
    Wydawca:
    Uniwersytet im. Adama Mickiewicza w Poznaniu
    Tematy:
    geomorphology
    periglacial relief
    anthropogenic relief
    thermal-contraction structures
    Polish Lowland
    geomorfologia
    antropogeniczna rzeźba
    Niż Polski
    Opis:
    An exceptional concentration of almost identical depressions exist near the small towns of Krotoszyn, Koźmin and Raszków (southern Wielkopolska). Their origin is, however, different from that of the typical post glacial-relief: they are Man-made enlarged thermal-contraction structures that developed at the very end of the Middle Polish (Warthian) glaciation and during the North Polish (Weichselian) glaciation, most probably under periglacial conditions.
    Źródło:
    Geologos; 2012, 18, 1; 43-50
    1426-8981
    2080-6574
    Pojawia się w:
    Geologos
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Unionid clams and the zebra mussels on their shells (Bivalvia: Unionidae, Dreissenidae) as hosts for trematodes in lakes of the Polish lowland
    Autorzy:
    Marszewska, A.
    Cichy, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/83142.pdf
    Data publikacji:
    2015
    Wydawca:
    Uniwersytet Mikołaja Kopernika. Wydział Biologii i Ochrony Środowiska. Stowarzyszenie Malakologów Polskich
    Tematy:
    unionid clam
    zebra mussel
    shell
    Bivalvia
    Unionidae
    Dreissena polymorpha
    Dreissenidae
    Digenea
    Aspidogastrea
    Rhipidocotyle
    Phyllodistomum
    Aspidogaster
    prevalence
    host
    trematode
    lake
    lowland
    Polish lowland
    Źródło:
    Folia Malacologica; 2015, 23, 2
    1506-7629
    Pojawia się w:
    Folia Malacologica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Soil environment of Pulsatilla vernalis (L.) Mill. at selected sites in the Polish lowland
    Autorzy:
    Grzyl, A.
    Niewiadomski, A.
    Woziwoda, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/58134.pdf
    Data publikacji:
    2013
    Wydawca:
    Polskie Towarzystwo Botaniczne
    Tematy:
    soil environment
    Pulsatilla vernalis
    site
    Polish lowland
    lowland
    relict population
    rare plant
    distribution
    soil property
    ecological indicator value
    active conservation
    plant conservation
    Polska
    Opis:
    The paper presents soil conditions of Pulsatilla vernalis in the Polish lowland. There were determined species preferences in relation to physical and chemical properties, grain size composition and the type of soil. It has been found that P. vernalis prefers very poor sandy, acid, dry and permeable soils, with small water capacity. The range of habitat parameters at the lowland sites differs, however, from the conditions at the mountain sites. Due to specific habitats of the species, new ecological indicator values were proposed for the lowland sites of P. vernalis. The results of soil analysis presented in this paper, as well as other data related to biology of the species, should be accounted for in the active protection plan, including the processes of reintroduction and introduction of the species.
    Źródło:
    Acta Societatis Botanicorum Poloniae; 2013, 82, 4
    0001-6977
    2083-9480
    Pojawia się w:
    Acta Societatis Botanicorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Milk yield and chemical composition in ewes kept in pasture and indoor system of maintenance
    Wydajność i skład chemiczny mleka owiec utrzymywanych w systemie pastwiskowym i alkierzowym
    Autorzy:
    Pięta, M
    Patkowski, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2197187.pdf
    Data publikacji:
    2009
    Wydawca:
    Uniwersytet Przyrodniczy w Lublinie. Wydawnictwo Uniwersytetu Przyrodniczego w Lublinie
    Tematy:
    milk yield
    chemical composition
    ewe
    pasture
    indoor system
    maintenance
    sheep
    milk
    somatic cell
    genotype
    Polish Lowland sheep
    synthetic line
    lactation
    Źródło:
    Annales Universitatis Mariae Curie-Skłodowska. Sectio EE: Zootechnica; 2009, 27, 2; 1-11
    0239-4243
    2083-7399
    Pojawia się w:
    Annales Universitatis Mariae Curie-Skłodowska. Sectio EE: Zootechnica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Exploration and exploitation of oil and gas fields in Poland: a historical outline
    Autorzy:
    Karnkowski, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2066017.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    historia przemysłu naftowego
    pola naftowe i gazowe
    Karpaty
    zapadlisko przedkarpackie
    nizina polska
    history of petroleum industry
    oil and gas fields in Poland
    Carpathians
    Carpathian Foredeep
    Polish Lowland
    Opis:
    Petroleum industry began in Galicia region, the former part of Poland which was in 1772-1918 a province of the Austro-Hungarian Empire. The birth of this industry was connected with petroleum distillation made by two pharmacists: Ignacy Łukasiewicz and Jan Zeh, who persistently were working to get a liquid without both light and heavy factions of hydrocarbons, i.e. a liquid paraffin of oil. This aim was reached in spring of 1853. That time also a kerosene lamp was constructed by Adam Bratkowski under direction of I. Łukasiewicz. The set of these lamps was used in the Lviv municipal hospital during the serious surgical operation on 31 July 1853. This date was accepted as the beginning of the world oil industry. Next year I. Lukasiewicz established the oil mine in the Bóbrka village near Krosno. Oil wells then were frequently the open ones dug out to the depth of 60 m and from them oil was extracted with wooden buckets by usage of gin. When petroleum deliveries were assured I. Łukasiewicz founded in 1856 the first petroleum distillery in Ulaszowice near Jasło, the second one in 1858 in Kleczany, and the third one in Polanka near Krosno in 1861. In 1890s in the Carpathians the new oil deposits were discovered in the Gorlice-Jasło-Sanok region. In 1888 the Bergheim Mac Garvey Company found the new oil fields in Weglówka near Krosno and the Galician Oil Mining Company discovered oil-rich deposits in Potok, Turaszówka, Iwonicz, Stara Wieś, Rudawka Rymanowska and Wankowa. Discoveries were also along the Carpathians thrust front where exists the zone of deep-seated folds covered by the Miocene deposits. Oil fields are here located at depth of 800-2000 m. In the Borislav vicinity a few very efficient oil fields were documented in 1896. In 1908 the highly productive "Oil City" well with oil production 2500 t/d was drilled. Exploitation in this region of the Carpathians in 1909 was 2x10exp.6 t, i.e. 5%of the world oil production and Galicia was the third producer in the world. During 150 years of exploration, in this part of Polish Carpathians, 67 oil and 17 gas fields were discovered. In the Carpathian Foredeep 50 gas fields and 10 oil fields were documented. The biggest success was the Jaksmanice-Przemyśl gas field with 75x 10exp.9 m3 of resources. In the Polish Lowland in 1946, just after the Second World War, basing on gravimetric and magnetic data, the first drilling was located on the Kłodawa structure and the Zechstein salts at depth of 300 m were found. Later this drill was a base for foundation of Kłodawa salt mine. In 1961 in the Fore-Sudetic Monocline the first oil field Rybaki was discovered in the Zechstein Main Dolomite formation, and three years later, in 1964, the first gas field discovery - Bogdaj-Uciechów was found within the Rotliegend sandstone and the Zechstein Limestone unit. Until now a dozen of oil and gas fields were documented not only in the Permian formations but also in the Devonian and the Carboniferous deposits in the Lublin Petroleum Province and in the Cambrian sandstones in the Gdansk Petroleum Province. Exploration works, initiated after the Second World War, both in the Carpathians as well as in the Carpathian Foreland and the Polish Lowland give premises of new oil and gas filed discoveries there also in the future.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 12/1; 1049-1059
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Sorption properties of gypsic rendzinas from the Niecka Nidzianska area
    Autorzy:
    Ciarkowska, K
    Powiązania:
    https://bibliotekanauki.pl/articles/1450782.pdf
    Data publikacji:
    2001
    Wydawca:
    Polska Akademia Nauk. Instytut Agrofizyki PAN
    Tematy:
    soil profile
    glacial cover
    rendzina soil
    Polish lowland
    soil protection
    arable soil
    semispherical gypsic hill
    soil
    turf soil
    gypsum deposit
    sorption property
    gypsic rendzina soil
    Niecka Nidzianska area
    gypsic rock
    terrestrial ecosystem
    Nida area
    Opis:
    In order to estimate sorption properties of gypsic rendzinas from the Niecka Nidziańska area as well as compare a composition of exchangeable cations in arable and turf soils 24 profiles have been investigated which represented following subtypes: initial, proper, chernozemic and brown ones, and derived from 3 types of miocene gypsum: selenite, shaly and compact gypsum. On the basis of the investigations it has been found that sorption properties of gypsic rendzinas were formed under influence of lithological factor and depend on the activity of the parent rock which is expressed by a content of the active calcium in the rock. Humous horizons of the arable soils characterised of a slightly lower complex exchange capacity and a higher contribution of potassium and magnesium in the composition of exchangeable ions in comparison with analogous horizons of the turf soils. A content of exchangeable cations permitted to count investigated soils among the soils with saturated complex of exchangeable cations. In their complex dominated calcium and the contribution of acid cations was small.
    Źródło:
    Acta Agrophysica; 2001, 50; 71-79
    1234-4125
    Pojawia się w:
    Acta Agrophysica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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