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Tytuł:
Mesozoic thickness pattern in the Mid-Polish Trough
Autorzy:
Dadlez, R.
Powiązania:
https://bibliotekanauki.pl/articles/2058886.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
western and central Poland
Mid-Polish Trough
Mesozoic thickness
tectonics
palaeogeography
Opis:
The Mid-Polish Trough (MPT) is well recorded in the distribution of thickness of the Mesozoic sediments. Its shape was most distinctly delineated in the Early Triassic, and Early to Middle Jurassic, when thickness gradients attaining 100 m/km were reached. However, because the regional faults bordering the MPT were not active throughout its history, the existence of Mid-Polish Rift has not been confirmed. The strongest thickness gradients may have been caused by the periodical activity of the sub-Zechstein faults, which did not penetrate the Mesozoic strata due to the damping effect of plastic Zechstein salts. On the contrary, local faults, forming (mainly during the Late Triassic) syn-sedimentary grabens, are a common feature in the MPT and its surroundings. Transversal subdivision of the MPT and its slopes into at least two segments (Pomeranian and Kuiavian) is clearly visible in the thickness pattern. It is expressed by the presence of separate depocentres, reversal of asymmetry, differences in stratigraphical sequences observed on the palaeomorphological terraces south-west of the MPT, and by the structural variations after the inversion. The scale of inversion, which transformed the MPT into the Mid-Polish Swell (MPS), is unclear and needs further investigations. Estimation of the thickness of the Upper Cretaceous sediments removed by erosion is a key problem in this respect. It should take into account both, the effects of the regional inversion and the local changes resulting from the last stage of strong salt displacements.
Źródło:
Geological Quarterly; 2003, 47, 3; 223-240
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Populations of Cepaea Hortensis (O. F. Muller, 1774) polymorphic for the colour of shell lip in north-western Poland and north-central Germany
Autorzy:
Ozgo, M.
Powiązania:
https://bibliotekanauki.pl/articles/84682.pdf
Data publikacji:
2010
Wydawca:
Uniwersytet Mikołaja Kopernika. Wydział Biologii i Ochrony Środowiska. Stowarzyszenie Malakologów Polskich
Opis:
In Cepaea hortensis (O. F. Müller), the shell lip (peristome) is usually white. In most areas the lip colour allows us to reliably distinguish this species from C. nemoralis (Linnaeus) in which the lip is usually dark brown. Populations polymorphic for lip colour are rare and occur only locally. Here I report on populations of C. hortensis containing dark-lipped individuals in north-western Poland and in north-central Germany. The frequency of dark-lipped individuals ranged from 3% to 31%. It was common in brown and pink shells, but occurred only sporadically in yellow shells. No selective factors promoting dark-lipped C. hortensis are evident. The occurrence of this phenotype is likely to reflect random events.
Źródło:
Folia Malacologica; 2010, 18, 2
1506-7629
Pojawia się w:
Folia Malacologica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Stan obecny i perspektywy rozwoju populacji rysia euroazjatyckiego w środkowej i zachodniej Polsce
Current status and prospects of development of Eurasian lynx population in central and western Poland
Autorzy:
Kwiatkowska, I.
Myslajek, R.W.
Powiązania:
https://bibliotekanauki.pl/articles/880192.pdf
Data publikacji:
2019
Wydawca:
Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Leśny Zakład Doświadczalny. Centrum Edukacji Przyrodniczo-Leśnej w Rogowie
Tematy:
zwierzeta chronione
drapiezniki
rys euroazjatycki
Lynx lynx
wystepowanie
populacje zwierzat
dyspersja
bariery ekologiczne
Polska Srodkowa
Polska Zachodnia
Źródło:
Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej; 2019, 21, 2[59]
1509-1414
Pojawia się w:
Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Phosphorus and its Fractionation in Bottom Sediments of Selected Lakes of Wielkopolskie Lakeland in Central and Western Poland
Fosfor i jego frakcje w osadach dennych wybranych jezior Pojezierza Wielkopolskiego w środkowej i zachodniej Polsce
Autorzy:
Bryl, Łukasz
Sobczyński, Tadeusz
Powiązania:
https://bibliotekanauki.pl/articles/1812061.pdf
Data publikacji:
2019
Wydawca:
Politechnika Koszalińska. Wydawnictwo Uczelniane
Tematy:
lake
bottom sediments
phosphorus
fractionation of phosphorus
organic matter
iron
aluminium
calcium
jezioro
osady denne
fosfor
frakcjonowanie fosforu
materia organiczna
żelazo
glin
wapń
Opis:
The role of phosphorus contained in bottom sediments of water reservoirs is crucial in the whole eutrophication process. It is an element responsible for the proper functioning of aquatic ecosystems, and its excess leads to deterioration of water quality. The release of phosphorus from bottom sediments directly into the water depends on many factors. This process is particularly intensified at the moment of anaerobic conditions occurring in the bottom layer, or the phenomenon of resuspension of sediments due to external factors, such as intense waving. The persistence of phosphorus deposition in sediments also depends on the nature of chemical connections and changing oxidation-reduction conditions, temperature and pH. Bottom sediments from eight selected lakes of Wielkopolskie Lakeland were investigated for their total phosphorus content and the possibility of its rerelease into water. The subject of the study were the following lakes: Wolsztyńskie, Winiary, Jelonek, Siekiera, Pniewskie, Umultowskie, Góreckie, Strykowskie. The investigated water reservoirs are glacial lakes, usually shallow and characterized by large variations in water level. The samples of bottom sediments were collected from profundal zone with a tube probe from the surface layer of 10 cm thickness, i.e. the layer that exchanges matter with the surrounding water. The collected sediments were placed in sealed, plastic containers to their full capacity. Before proceeding to carry out detailed laboratory analyzes, samples were prepared accordingly. First, the bottom sediments were thoroughly homogenized. Then, they were dried and subjected to further testing. The obtained results were statistically analyzed in the program Statistica 6 PL. Phosphorus was fractionated by means of a sequential extraction described by Psenner. The sediments were also analyzed for the content of phosphorus binding components such as organic matter, iron, aluminium and calcium. Phosphorus was found to be bound mostly to organic matter, aluminium and calcium – the fractions from which it was difficult to release into water. The share of exchangeable and most mobile and bioavailable iron-bound fraction of phosphorus was the lowest but it was still high enough to cause phytoplankton blooms. No clear relationships between the content of individual phosphorus-binding components and the share of phosphorus fractions related to them in total phosphorus pool were identified. Total content of phosphorus in the sediments of the investigated lakes was analogue and similar to that determined in bottom sediments of other eutrophic lakes of Wielkopolskie Lakeland. The content of aluminium, calcium, iron and organic matter were much more variable.
Rola fosforu zawartego w osadach dennych zbiorników wodnych jest kluczowa w całym procesie ich eutrofizacji. Jest pierwiastkiem odpowiedzialnym za prawidłowe funkcjonowanie ekosystemów wodnych, a jego nadmiar prowadzi do pogorszenia się jakości wody. Uwalnianie się fosforu z osadów dennych bezpośrednio do toni wodnej zależy od wielu faktorów. Szczególnie proces ten intensyfikuje się w momencie pojawienia się w warstwie naddennej warunków beztlenowych, czy też zjawiska resuspensji osadów na skutek oddziaływania czynników zewnętrznych, np. intensywnego falowania. Trwałość deopozycji fosforu w osadach zależy również od charakteru połączeń chemicznych oraz zmiennych warunków oksydacyjno-redukcyjnych, temperatury, a także pH. Badano osady denne z ośmiu wybranych jezior Pojezierza Wielkopolsko-Kujawskiego pod kątem całkowitej zawartości fosforu i potencjalnej możliwości jego ponownego uwalniania do toni. Przedmiotem badań były następujące jeziora: Wolsztyńskie, Winiary, Jelonek, Siekiera, Pniewskie, Umultowskie, Strykowskie, Góreckie. Badane zbiorniki wodne to jeziora polodowcowe, zwykle płytkie, charakteryzujące się dużymi wahaniami poziomu wody. Próbki osadów dennych pobierano za pomocą sondy rurowej z powierzchniowej warstwy osadu o miąższości 10 cm, czyli warstwy, która uczestniczy w wymianie materii z tonią. Pobrany osad umieszczano w szczelnych, plastikowych pojemnikach napełniając je do pełna. Przed przystąpieniem do przeprowadzania szczegółowych analiz laboratoryjnych próbki zostały odpowiednio przygotowane. W pierwszej kolejności osady denne dokładnie zhomogenizowano. Następnie wysuszono oraz przeprowadzono kolejne analizy. Uzyskane wyniki badań poddano analizie statystycznej w programie Statistica 6 PL. Frakcjonowanie fosforu realizowano na drodze ekstrakcji sekwencyjnej wg schematu zaproponowanego przez Psennera. Dodatkowo w osadach oznaczano materię organiczną oraz żelazo, glin i wapń, czyli składniki osadu wiążące fosfor. Stwierdzono, że w ogólnej puli fosforu poszczególnych osadów największy udział miały frakcje związane z materią organiczną i glinem oraz z wapniem, czyli stosunkowo trudniej uwalniane do toni. Udział frakcji wymiennej i związanej z żelazem, czyli frakcji najbardziej mobilnych, biodostępnych, był mniejszy co jednak było wystarczające, aby w wodach tych jezior występowały zakwity fitoplanktonu. Nie zaobserwowano natomiast wyraźnych zależności pomiędzy zawartością w osadach poszczególnych składników wiążących fosforany, a udziałem frakcji fosforu z nimi związanych w ogólnej jego puli. Łączna zawartość fosforu w osadach badanych jezior była analogiczna i podobna do tej stwierdzonej w osadach dennych innych eutroficznych jezior Pojezierza Wielkopolskiego. Zawartość glinu, wapnia, żelaza i materii organicznej była znacznie bardziej zmienna.
Źródło:
Rocznik Ochrona Środowiska; 2019, Tom 21, cz. 2; 1515-1532
1506-218X
Pojawia się w:
Rocznik Ochrona Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Phases of Palaeogene and Neogene tectonic evolution of selected grabens in the Wielkopolska area, central-western Poland
Autorzy:
Widera, M.
Powiązania:
https://bibliotekanauki.pl/articles/191603.pdf
Data publikacji:
2004
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
tectonic phases
grabens
Palaeogene
Neogene
Wielkopolska area
central-western Poland
Opis:
In the Wielkopolska (Great Poland) area, there occur numerous tectonic grabens which were active in the Palaeogene and Neogene. The similarities and differences between their development are presented on the example of the Czempiń, Szamotuły, Lubstów, and Władysławów Grabens. Using various methods of palaeotec- tonic analysis, the stages of accelerated subsidence of the grabens, i.e. tectonic phases, were indicated. The extent of vertical movement in the studied grabens were compared and it was affirmed that there is a connection between the occurrence of older dislocations and salt structures in the deep basement. From among the examined grabens, the Lubstów Graben is the deepest one, and shows the most complex geological structure. The Czempiń and Szamotuły Grabens are characterized by relatively simple geological structure, where the stratigraphic complete- ness and tectonic style are very legible. These three grabens were active in different tectonic stages from the turn of the Eocene/Oligocene till the end of the Neogene, and perhaps also in the Prepleistocene. The Władysławów Graben is a very shallow tectonic structure and its evolution lasted for the shorter period of time. The time of its development extended from the Early through the Middle Miocene. These grabens provide a good example of the relationship between the fault throw and graben location. The Czempiń, Szamotuły, and Lubstów Grabens, connected with deeply-rooted dislocations, came to existence in the Pyrenean phase (latest Eocene - Early Oligocene). However, the Władysławów Graben was affected mainly by salt structure activity. Thus, its first stage of tectonic evolution took place in the Savian phase (Early Miocene).
Źródło:
Annales Societatis Geologorum Poloniae; 2004, 74, No 3; 295-310
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Cepaea vindobonensis (Ferussac, 1821) (Gastropoda: Pulmonata: Helicidae) in Central, Northwestern and Western Poland
Autorzy:
Mierzwa, D.
Powiązania:
https://bibliotekanauki.pl/articles/83727.pdf
Data publikacji:
2009
Wydawca:
Uniwersytet Mikołaja Kopernika. Wydział Biologii i Ochrony Środowiska. Stowarzyszenie Malakologów Polskich
Opis:
Cepaea vindobonensis (Fér.), occurring in south-eastern Europe, is a xerothermophile associated with carbonate or carbonate-silica substratum. In Poland it has natural localities in the south-east. Its distribution in the other parts of the country was studied and up-dated based on literature data and museum materials. Its presence on the flood plains of the Vistula and Odra river systems in C., NW. and W. Poland is a result of water dispersal from sites with mainly carbonate substratum. Its further spread from there may be due to accidental dispersal by humans.
Źródło:
Folia Malacologica; 2009, 17, 4
1506-7629
Pojawia się w:
Folia Malacologica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Variability and temporal structure of concentrations of carbon monoxide in Poznan (central-western Poland)
Autorzy:
Kalbarczyk, E.
Kalbarczyk, R.
Powiązania:
https://bibliotekanauki.pl/articles/962863.pdf
Data publikacji:
2017
Wydawca:
Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Opis:
Carbon monoxide, in addition to CO2 and CH4, constitutes the largest source of carbon in the atmosphere and. by reacting with the hydroxyradical OH, it indirectly contributes to the increase in the concentration of methane and ozone in the atmosphere. The aim of the study was to determine the temporal variation of CO concentrations and its dependence on the weather course in an urban area situated in Wielkopolska, a region in central-western Poland. The research used data from the State Environmental Monitoring Station in the north-western part of Poznań (Hs = 84 m above sea level) in the immediate vicinity of a residential and recreational area. The data included hourly concentrations of CO and hourly values of atmospheric pressure, air temperature, total solar radiation, relative air humidity and wind velocity in 2005-2014. To measure the concentration of carbon monoxide, a Horiba APMA 360 analyzer and TELEDYNE API T400 were used. The measurement method was infrared spectroscopy. The time distribution of CO concentrations was considered by years, half years, months and hours. Relationships between the analyzed variables were confirmed using the Spearman’s correlation coefficient at the level of p ≤ 0.01. It was found that in the years of research the average concentration of CO in central-western Poland had a negative trend, as well as higher values in the heating season than in the warm half of year, and on week days than at weekends. Two concentration maxima, morning and evening ones, both in warm and cool half-year and on working days, were observed. On non-working days, there was one evening maximum. The variability of CO was mostly affected by air temperature (rs = -0.45) and solar radiation (rs = 0.32). The highest concentrations of CO were accompanied by the lowest values of solar radiation, air temperature and wind velocity, and highest values of the atmospheric pressure, as well as higher than average relative air humidity.
Źródło:
Journal of Elementology; 2017, 22, 2
1644-2296
Pojawia się w:
Journal of Elementology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Variability and temporal structure of concentrations of carbon monoxide in Poznan (central-western Poland)
Autorzy:
Kalbarczyk, E.
Kalbarczyk, R.
Powiązania:
https://bibliotekanauki.pl/articles/1190148.pdf
Data publikacji:
2017
Wydawca:
Uniwersytet Warmińsko-Mazurski w Olsztynie / Polskie Towarzystwo Magnezologiczne im. Prof. Juliana Aleksandrowicza
Tematy:
gas pollution
meteorological factor
weekday
Wielkopolska region
Opis:
Carbon monoxide, in addition to CO2 and CH4, constitutes the largest source of carbon in the atmosphere and. by reacting with the hydroxyradical OH, it indirectly contributes to the increase in the concentration of methane and ozone in the atmosphere. The aim of the study was to determine the temporal variation of CO concentrations and its dependence on the weather course in an urban area situated in Wielkopolska, a region in central-western Poland. The research used data from the State Environmental Monitoring Station in the north-western part of Poznań (Hs = 84 m above sea level) in the immediate vicinity of a residential and recreational area. The data included hourly concentrations of CO and hourly values of atmospheric pressure, air temperature, total solar radiation, relative air humidity and wind velocity in 2005-2014. To measure the concentration of carbon monoxide, a Horiba APMA 360 analyzer and TELEDYNE API T400 were used. The measurement method was infrared spectroscopy. The time distribution of CO concentrations was considered by years, half years, months and hours. Relationships between the analyzed variables were confirmed using the Spearman’s correlation coefficient at the level of p ≤ 0.01. It was found that in the years of research the average concentration of CO in central-western Poland had a negative trend, as well as higher values in the heating season than in the warm half of year, and on week days than at weekends. Two concentration maxima, morning and evening ones, both in warm and cool half-year and on working days, were observed. On non-working days, there was one evening maximum. The variability of CO was mostly affected by air temperature (rs = -0.45) and solar radiation (rs = 0.32). The highest concentrations of CO were accompanied by the lowest values of solar radiation, air temperature and wind velocity, and highest values of the atmospheric pressure, as well as higher than average relative air humidity.
Źródło:
Journal of Elementology; 2017, 22, 2; 697-711
1644-2296
Pojawia się w:
Journal of Elementology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Various genetic types of end moraines in the city of Poznań and its close vicinity, central-western Poland
Autorzy:
Widera, Marek
Chomiak, Lilianna
Powiązania:
https://bibliotekanauki.pl/articles/396069.pdf
Data publikacji:
2019
Wydawca:
Uniwersytet Zielonogórski. Oficyna Wydawnicza
Tematy:
Pleistocene of central-western Poland
accumulative moraines
push end moraines
depositional processes
deformational processes
Scandinavian ice sheet
Plejstocen
Polska środkowo-zachodnia
moreny akumulacyjne
moreny pchające
procesy depozytowe
procesy deformacyjne
Skandynawskie pokrywy lodowe
lodowiec skandynawski
Opis:
The current research focuses on explaining the origin of end moraines running through the northernmost districts of the city of Poznań. The highest hills, that is, the Moraska Hill and the Dziewicza Hill, are a stagnation record of the Vistulian Glaciation of the Poznań Phase. These two hills represent terminal moraines of similar height and age, but the mechanism of their formation is diametrically opposed. The Dziewicza Hill is a typical accumulative end moraine, where Pleistocene deposits over 70 m thick are undisturbed. On the other hand, the Moraska Hill is a classic example of a push end moraine with a relatively thin cover of Pleistocene sediments and glaciotectonically elevated (up to 130 m a.s.l.) upper Neogene deposits. In the latter case, these strongly deformed sediments are the so-called "Poznań Clays" that underlie the Quaternary deposits in the vast area of the Polish Lowlands.
Źródło:
Civil and Environmental Engineering Reports; 2019, 29, 3; 218-227
2080-5187
2450-8594
Pojawia się w:
Civil and Environmental Engineering Reports
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Early and Middle Jurassic tectonically controlled deposition in the High-Tatric succession (Tatricum), Tatra Mountains, southern Poland : a review
Autorzy:
Łuczyński, Piotr
Powiązania:
https://bibliotekanauki.pl/articles/2058707.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Central Western Carpathians
Vahic Ocean
Jurassic
High-Tatric series
synsedimentary tectonics
Opis:
The High-Tatric succession of the Tatra Mountains represents the Tatricum domain of the Central Western Carpathians, which in the Jurassic was located on the southern margin of the incipient and expanding Vahic Ocean – a branch of Western Tethys. This paper describes the various depositional consequences of extensional tectonic activity as it impacted on sedimentation in the High-Tatric succession of the Tatra Mountains during the Early and Middle Jurassic. Evidence of such impacts on depositional style and facies development are present within the Dudziniec, Smolegowa and Krupianka formations, in all the High-Tatric tectonic units. These impacts also include erosional surfaces and sedimentary gaps separating particular formations, commonly associated with minor angular unconformities. The Lower Jurassic, pre-Bajocian, Dudziniec Formation of the Kominy Tylkowe (autochthonous) Unit is developed in mixed carbonate-clastic facies. The occurrence and proportion of sand-dominated and carbonate-dominated facies, as well as their thickness differences, were controlled by syndepositional tilt-block tectonics, taking place both in depositional and in neighbouring source areas. The Smolegowa and Krupianka formations (Bajocian–Bathonian) occur in all High-Tatric tectonic units, but in the Czerwone Wierchy and Giewont units they are represented mainly by laterally discontinuous bodies of crinoidal limestone of very limited thickness. The preservation of these deposits only in some areas, as well as their thickness reductions, are effects of differentiated subsidence and uplift of isolated blocks taking place in an extensional regime. Moreover, the Krupianka Formation abounds in condensed facies with ferruginous crusts and stromatolites – a feature characteristic of rapidly drowning ocean margins. Deposits of the Dudziniec, Smolegowa and Krupianka formations are also preserved as infills of extensive systems of neptunian dykes penetrating mainly the Triassic substrate, which is yet another classic symptom of synsedimentary extension. The dominant influence of tectonics on sedimentary development ceased with the onset of deposition of the Raptawicka Turnia Formation in the Callovian.
Źródło:
Geological Quarterly; 2021, 65, 1; 16
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Effect of Maintenance Works on Ichthyofauna in the Context of Hydrochemical Conditions of Small Watercourses of Central and North-Western Poland
Autorzy:
Brysiewicz, Adam
Czerniejewski, Przemysław
Powiązania:
https://bibliotekanauki.pl/articles/123175.pdf
Data publikacji:
2019
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
dredging
watercourse
fish
habitat preferences
biodiversity
Opis:
The studies were conducted in the summers of 2017 and 2018 on three watercourses in Central and North-Western Poland, the where maintenance works involving disposal of sediment and silt were performed in the autumn of 2017. Monitoring of the ichthyofauna in the Rurzyca River and the Tywa River before (year 2017) and after the maintenance works (year 2018) indicated a decrease in the number of species. Altogether, 23 fish species were caught in all the watercourses. Out of these, 12 species were not recorded after the studied rivers had been dredged. A slight decrease in the number of fish species was observed in each studied river after the maintenance works. The values of physicochemical parameters obtained for each watercourse indicate a low quality of the waters. After silt had been removed from the watercourses, lower N-NO3values were observed at most research sites, whereas the N-NH4+ values increased significantly (except for one site on the Kanał Habdziński). Additionally, high volumes of P-PO43-were observed (except for sites 2 and 3 on the Kanał Habdziński and site 2 on the Rurzyca River). Maintenance works performed on small watercourses have a negative impact on the quality of waters and a less significant impact on the number of fish and biodiversity. This appears to be connected with migration of fish in the river during the maintenance works and avoidance of the consequent unfavourable conditions to gradually return to their habitats afterwards.
Źródło:
Journal of Ecological Engineering; 2019, 20, 8; 82-89
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Recharge and drainage of lakes in the Powidzki Landscape Park in conditions of increased anthropogenic and environmental pressure (central-western Poland)
Autorzy:
Nowak, Bogumił Michał
Przybyłek, Jan
Powiązania:
https://bibliotekanauki.pl/articles/2058553.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
surface resources
groundwater resources
hydraulic contacts
water level changes
mining dewatering
evapotranspiration
Gniezno Lakeland
Opis:
The lakes of the Powidzki Landscape Park (Gniezno Lakeland) are known for their natural and recreational values. The majority of them are located within two large glacial tunnel valleys, that in many places cut through several levels of till and inter-till aquifers. Regional hydraulic linkage systems are developed where surface water and groundwater remain in direct contact. Smaller water bodies occur between the lakes, in other tunnel valleys, in isolated meltwater basins, or in river valleys. These water bodies constitute local drainage bases. The existence in the area of such morphologically diverse lakes with different flow rates, varied morphology, and heterogeneous geological structure permitted tracing of the hydrodynamic dependencies of lake catchments of various types. Hydrogeological cross-sections, comparative analyses of structural maps for successive aquifers, bathymetric plans of lakes, and piezometric contour maps were prepared. Surface and groundwater level fluctuations were investigated, as well as their response to changing atmospheric conditions. Water balances of lakes were also determined for selected lake catchments. The study showed that all the lakes analysed are closely related to groundwater, and that the deepest ones reach lower aquifers. The majority of the lakes drain the aquifers, but some of the lakes feed them. Such a situation was documented in coastal wetlands and in the eastern part of the Park, affected by a depression cone associated with a nearby lignite opencast mine. The study showed that the deepest of the lakes analysed have a very wide catchment area of groundwater recharge, expanding beyond the boundaries of their surface catchment areas. This is important for the development of their resources, especially in periods of hydrogeological low flow.
Źródło:
Geological Quarterly; 2020, 64, 1; 205--219
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Deformacje osadów kenozoicznych w zachodniej ścianie odkrywki Koźmin KWB „Adamów”
Deformations of Cenozoic sediments in the western face of Koźmin outcrop KWB ,,Adamów”
Autorzy:
Stępień, B.
Powiązania:
https://bibliotekanauki.pl/articles/294348.pdf
Data publikacji:
2015
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
glacitektonika
analiza strukturalno-litofacjalna
centralna Polska
glaciotectonics
structural and lithofacies analysis
Central Poland
Opis:
Deformacje osadów kenozoicznych w odsłonięciu w Koźminie znajdują się pomiędzy drugim poziomem nadkładu a poziomem eksploatacyjnym. Wśród zaburzeń wyróżniono mezostruktury o wielkości od kilkunastu do kilku metrów oraz drobne struktury deformacyjne o rozmiarach od kilku do kilkudziesięciu centymetrów. Pomiary strukturalne zostały zestawione w formie sferycznych diagramów wraz z rekonstrukcją kierunku lokalnego nacisku lądolodu. Analiza lokalnych pól naprężeń w oparciu o pomiary orientacji i wergencji struktur deformacyjnych pozwoliła wyznaczyć kierunki głównego nacisku (transportu glacitektonicznego) skierowanego z NNE–NE ku SSW–SW w przedziale azymutów 5–42°. Analizowane struktury deformacyjne związane są z nasunięciem lądolodu zlodowacenia Odry.
Deformations of Cenozoic sediments in Koźmin exposure are situated between the second level of overlayer and a brown coal bench. In registered disturbances mesostructures in size from several to couple meters and fine structures in size from few to several dozen centimetres. The structural analysis was compiled in the spherical diagrams with the reconstruction of local ice flow. The examination of local stress poles on the basis of orientations and vergences measurements allowed to evaluate the main stress directions (glaciotectonic transport) from NNE–NE to SSW–SW (5–42° azimuth). Deformation structures are connected with ice-sheet of Odranian Glaciation.
Źródło:
Landform Analysis; 2015, 30; 29-40
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Changes in paleo-circulation and the distribution of ammonite faunas at the Coniacian–Santonian transition in central Poland and western Ukraine
Autorzy:
Remin, Z.
Gruszczyński, M.
Marshall, J. D.
Powiązania:
https://bibliotekanauki.pl/articles/139412.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Coniacian–Santonian transition
paleogeography
paleo-circulation
ammonites
carbon stable isotopes
oxygen stable isotopes
paleogeografia
amonity
izotopy węgla
izotop tlenu
Opis:
Ammonite distribution patterns and carbon and oxygen stable isotopes from the Lipnik-Kije (Poland) and Dubovcy (Ukraine) sections allow us to propose a model of sea water paleo-circulation in central Europe for the Coniacian-Santonian interval. The tectonic evolution of the south-eastern part of Poland, and expansion of the Krukienic Island areas, appears to have been one of the most important factors affecting paleotemperatures and the distribution of ammonite faunas in the shallow, epicontinental sea in this part of Europe. In the Lipnik-Kije section, low-latitude Tethyan ammonites, especially of the genera Nowakites, Parapuzosia and Saghalinites, are mixed with the cold water loving ammonite genus Kitchinites in the Lower Santonian. In the Dubovcy section (western Ukraine), Tethyan ammonites disappear abruptly in the earliest Santonian, giving place to temperate ammonites of the Kitchinites group in the early Early Santonian and to Boreal belemnites of the genus Gonioteuthis in the Middle and Late Santonian. Despite evidence for the effects of diagenesis in both sections, bulk-rock δ18O records from the limestones support higher seawater paleotemperatures in the Polish sea and cooler conditions in the western Ukraine. The proposed paleo-circulation model and paleotemperature distribution across Europe is supported independently by changes in faunal and nannoflora evidence (ammonites, foraminifera and nannoplankton), and rather unexpectedly with the bulk δ18O data. These data allow the recognition of the end-Coniacian–Early Santonian cooling event, resulting from cold currents flowing from the north, which is traceable, with different magnitude, in several European sections. Facies changes in both sections are related to the input of terrigenous material, and linked to Subhercynian tectonic movements which affected the eastern (Ukrainian) and central (Holy Cross) segment of the Mid Polish Trough at different times. Uplift and sediment input moved westwards through time. Clastic input is detectable at the Coniacian–Santonian boundary in the Ukrainian segment. Similar facies changes reached the Holy Cross segment in Poland distinctly later, somewhen in the Middle Santonian. It is likely that tectonics together with paleo-circulation changes markedly restricted or even cut-off the western Ukraine area from Tethyan ocean influences in the Early Santonian.
Źródło:
Acta Geologica Polonica; 2016, 66, 1; 107-124
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Early Miocene residual flysch basin at the front of the Central Western Carpathians and its palaeogeographic implications (Magura Nappe, Poland)
Autorzy:
Oszczypko-Clowes, M.
Oszczypko, N.
Piecuch, A.
Soták, J.
Boratyn, J.
Powiązania:
https://bibliotekanauki.pl/articles/2060420.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Outer Carpathians
Magura Nappe
residual flysch basin
Early Miocene
calcareous nannoplankton
palaeogeography
Opis:
In the Polish sector of the Magura Nappe, along the front of the Pieniny Klippen Belt, strongly tectonized calcareous flysch up to 1000 m thick is exposed. Previously these deposits, composed of thin- to thick-bedded flysch, with a packet of Łącko-type marls, have been included into several Paleocene/Eocene formations, e.g., the Szczawnica Formation. This formation contains a poor assemblage of agglutinated foraminifera and a relatively rich assemblage of calcareous nannoplankton, with abundant reworked species. The youngest species give evidence of the NN2 Zone (Lower Miocene). Additionally, in three profiles (Szlachtowa, Knurów and Waksmund) of the Kremna Fm., Early Miocene foraminifera have been recognized. This research documented that during the Burdigalian, at the front of Central Western Carpathians, there still existed a residual marine basin probably up to 100 km wide. These deposits also contain thick packages of exotic carbonate conglomerates derived from the SE, previously regarded as the Jarmuta Formation.
Źródło:
Geological Quarterly; 2018, 62, 3; 597--619
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 21

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