Skocz do pozycji: 1.

Tytuł:

Variability of clutch size in Cormorant (Phalacrocorax carbo sinensis) at the Jeziorsko Reservoir (Central Poland) in 2004

Autorzy:

Minias, Piotr
Kaczmarek, Krzysztof
Kleszcz, Anna
Rakowski, Maciej
Janiszewski, Tomasz

Powiązania:

https://bibliotekanauki.pl/articles/764922.pdf

Data publikacji:

2008

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

clutch size
Cormorant
Central Poland

Opis:

The analysis of the clutch size variability in Cormorant (P. carbo sinensis) was based on study results in colony at the “Jeziorsko Reservoir” (central Poland) in 2004. There were used 328 broods controlled 3-5 times in the season. Number of eggs in a single clutch ranged from 1 to 7, although Cormorants mostly laid 3 to 5 eggs. Mean clutch size was 3.80 (SD = 1.0 0). The size of clutch depended on time of laying eggs and the part of colony where the nest with brood was localised. The clutch size was bigger for pairs that started laying eggs earlier and lower for birds bred in the part of colony where the number of nests and their density were low.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2008, 4
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 2.

Tytuł:

Strategia Rozwoju Polski Centralnej 2020 z perspektywą do 2030 – jako przykład zintegrowanego planowania na poziomie ponadregionalnym
Strategy for the development of Polish Central 2020 with a view to 2030-as an example of integrated planning at the level of supra-regional

Autorzy:

Paturalska-Nowak, Ewa

Powiązania:

https://bibliotekanauki.pl/articles/461280.pdf

Data publikacji:

2016-06

Wydawca:

Mazowieckie Biuro Planowania Regionalnego w Warszawie

Tematy:

rozwój Polski Centralnej
Makroregion Polski Centralnej
development of Central Poland
Macroregion of Central Poland

Opis:

Strategia Rozwoju Polski Centralnej do roku 2020 z perspektywą 2030 jest czwartą strategią ponadregionalną przyjętą przez Radę Ministrów. Prace nad jej przygotowaniem zainicjowały w 2012r. władze samorządowe województw łódzkiego i mazowieckiego, podpisując porozumienie o współpracy międzyregionalnej. Efektem porozumienia było opracowanie Koncepcji Strategii Rozwoju Makroregionu Polski Centralnej 2030, która w oparciu o zdiagnozowane potencjały obu województw określiła pola współpracy i cele rozwoju makroregionu. Stała się ona podstawą do opracowania Strategii Rozwoju Polski Centralnej przez Ministerstwo Infrastruktury i Rozwoju. Wizja rozwoju Polski Centralnej – MAKROREGION POLSKI CENTRALNEJ AWANGARDĄ EUROPY XXI WIEKU – przedstawia pożądany obraz makroregionu i jest odpowiedzią na potrzeby budowania najbardziej dynamicznego, konkurencyjnego, kreatywnego i innowacyjnego obszaru Polski, rozpoznawalnego w skali europejskiej i globalnej. Za cel główny uznano: WZROST ZNACZENIA POLSKI CENTRALNEJ W SKALI MIĘDZYNARODOWEJ JAKO PRZESTRZENI PRZYJAZNEJ GENEROWANIU ORAZ TRANSFEROWI WIEDZY I INNOWACJI. Unikatowe potencjały rozwojowe, które mają stać się motorem wzrostu konkurencyjności makroregionu, to: nauka, badania i rozwój, sektor kreatywny, medycyna i farmacja, rolnictwo i przetwórstwo rolno-spożywcze oraz transport i logistyka. Dla tych pięciu strategicznych potencjałów zostały sformułowane cele szczegółowe i kierunki działań. Ich realizację warunkują cztery kierunki interwencji o charakterze horyzontalnym: dostępność i integracja, kreatywność i innowacyjność, reindustrializacja i umiędzynarodowienie.
The Strategy for Development of Central Poland unit 2020 in the 2030 Perspective is the fourth subrargional strategy adopted by the Council of Ministers. The preparation on the Strategy has started in 2012 by self-governments of Łódzkie and Mazowieckie voivodeships by signing a memorandum on inter-regional cooperation. The memorandum has resulted a preparation of the Concept of the Development Strategy of the Macroregion of Central Poland 2030. The Concept defined the areas of cooperation, which were due from identified development potentials of both voivodeships and the development objectives of the macroregion . The document has become a base for preparation the Strategy for Development of Central Poland by the Ministry of Infrastructure and Development. The vision of the Central Poland development, which states: MACROREGION OF CENTRAL POLAND AS THE AVANT-GARDE OF THE 21st CENTURY EUROPE, presents the desirable image of the macroregion and responds to the need to build the most dynamic, competitive, creative and innovative part of Poland, recognizable in Europe and globally. The main objective has been defined as THE INCREASE OF INTERNATIONAL IMPORTANCE OF CENTRAL POLAND AS THE FRIENDLY SPACE FOR CREATION AND TRANSFER OF KNOWLEDGE AND INNOVATION. The unique development potentials, which shall be the key to increased competitiveness, have been defined as: science, research and development, creative sector, medicine and pharmacy, agriculture and agri-food processing and transport, and logistics. For these five strategic potentials were formulated the specific objectives and intervention directions. The implementation of specific objectives depends on four horizontal intervention directions: accessibility and integration, creativity and innovativeness, re-industralisation and internationalization.

Źródło:

MAZOWSZE Studia Regionalne; 2016, 18; 137-144
1689-4774

Pojawia się w:

MAZOWSZE Studia Regionalne

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 3.

Tytuł:

Buntsandstein magnetostratigraphy in Poland : new data from the Brześć Kujawski IG-1 borehole

Autorzy:

Nawrocki, Jerzy
Becker, Anna

Powiązania:

https://bibliotekanauki.pl/articles/1836254.pdf

Data publikacji:

2020

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

magnetic polarity
Lower Triassic
central Poland

Opis:

New magnetostratigraphic data from the Middle Buntsandstein section, drilled in the Brześć Kujawski IG-1 borehole (Central Poland), are presented and discussed. The chronostratigraphic positions of particular formations of the Buntsandstein are discussed as well. The magnetic polarity pattern obtained from the Brześć Kujawski IG-1 borehole matches the pattern obtained earlier in other boreholes from the Polish part of the Central European Basin. Although magnetostratigraphy and palynological evidence undoubtedly indicates that the Induan/Olenekian boundary in the Polish part of the CEB is located in the lower part of the Pomerania Formation, the placement of the Olenekian/Anisian boundary within the sedimentary sequences of the Central European Basin remains problematic. This boundary most probably is located within the upper part of the Upper Buntsandstein, as can be inferred from palynological studies.

Źródło:

Annales Societatis Geologorum Poloniae; 2020, 90, 4; 435-446
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 4.

Tytuł:

Biological research of Grabia River - fifty years of activity

Autorzy:

Siciński, Jacek
Tończyk, Grzegorz

Powiązania:

https://bibliotekanauki.pl/articles/764941.pdf

Data publikacji:

2005

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

lowland river
ecology
central Poland
literature review

Opis:

Grabia, a small still close to natural conditions lowland river, has been an object of special interest for Łódź hydrobiologists for more than 50 years. Over 100 scientific papers and over 100 master theses were produced in the Faculty of Biology and Environmental Protection University of Łódź. The initiator was Prof.L.K. Pawłowski who spent many years conducting research into the river. The ground and the first research objective was to recognize the fauna diversity. The checklist encompass almost 1000 invertebrate and 24 fish species. Taxonomy, biology and ecology of various taxa have made for many decades an essential trend of scientific activity. Special attention was dedicated to rotifers, leeches, branchiobdellids, snails and bivalves, gammarids and copepods as well as aquatic insects, fish and also diatoms. Some aspects of zoobenthos and Zooplankton communities ecology was the subject of 13 Ph.D.theses. The river with its rich animal and plant communities was also the subject of dynamics of river ecosystem research. The study on the structure of invertebrate assemblages on the background of habitat diversity has been recently conducted. The model may be treealed as a reference to the restoration of Europaean rivers and their valleys.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2005, 2
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 5.

Tytuł:

Distribution of amphibians and reptiles in central Poland: 1980-2000

Autorzy:

Zieliński, Piotr
Hejduk, Janusz
Stopczyński, Michał
Markowski, Janusz

Powiązania:

https://bibliotekanauki.pl/articles/764951.pdf

Data publikacji:

2005

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

faunistics
atlas project
amphibians
reptiles
central Poland

Opis:

Based on 3047 records from 97 recorders distribution maps were drawn for the amphibians and reptiles of central Poland (lirom 51°00’N to 52°15’N and from 18°20’E to 20°20’E). The study area was divided into 180 atlas fields based on the geographic grid. All data were gathered in 1980-2000, most of them (67%) however, in 1995-2000. 13 taxa of amphibians were found in 143 atlas fields and 6 species of reptiles were found in 121 atlas fields. The amphibians were (given with the number of atlas fields with the species found): 119 - Common frog Rana temporaria Linnaeus, 1758; 114 - Common toad Bufo bufo (Linnaeus, 1758); 97 - Moor frog Rana arvalis Nilsson, 1842; 94 - Fire-bellied toad Bomhina bombina (Linnaeus, 1761); 93 - Pool frog Rana lessonae Camerano, 1882; 87 - Tree frog Hyla arhorea (Linnaeus, 1758); 85 - Green toad Bufo viriiüs Laurenti, 1768; 72 - Smooth newt Triturus vulgaris (Linnaeus, 1758); 70 - Spadefoot Pelobales fuscus (Laurenti, 1768); 69 - Edible frog Rana kl. esculenia Linnaeus, 1758; 39 - Great crested newt Triturus cristatus (Laurenti, 1768); 30 - Marsh frog Rana ridibunda Pallas, 1771 and 28 - the Natterjack Bufo calamita Laurenti, 1768. The reptile species (given with the number o f atlas fields) were: 94 - Sand lizard Lacerta agilis Linnaeus, 1758; 72 - Slow-worm Anguis fragilis Linnaeus, 1758; 67 - Common lizard Lacerta vivipara Jacquin, 1787; 60 - Grass snake Natrix natrix (Linnaeus, 1758), 57 - Adder Vipera berus (Linnaeus, 1758) and 4 - the Smooth snake Coronella austriaca Laurenti, 1768. Six adult specimens of the European pond terrapin Emys orbicularis (Linnaeus) were also found, but breeding of this species in the area studied was not confirmed.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2005, 2
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:

Record of paraglacial environment with examples from Central Poland and its role in morphogenesis of the area

Autorzy:

Rdzany, Z.

Powiązania:

https://bibliotekanauki.pl/articles/1395721.pdf

Data publikacji:

2014

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

paraglacial environment
old glacial landscape
Central Poland

Opis:

This article analyses the characteristics of paraglacial environment that are recorded in sediments and forms, within the context of the development of views on the relief of Central Poland in the area beyond the extent of the Vistulian (Weichselian) Glaciation. The original relief of the analysed area was formed during the Warta Glaciation (Wartanian, Late Saalian). Until the 1950s, the relief was considered as glacial, when the opinion that periglacial morphogenesis had great significance was prevalent. According to the hypothesis, periglacial processes dominated the original glacial relief, until denudational periglacial plains with tors were formed. However, since the 1960s, more and more data have been documented concerning good preservation of fragments of glacial landscape, particularly within the range of kame fields. In the 1990s, a concept of polygenesis of the relief was presented, stressing the importance of periglacial environment. However, it must be noted that all views on the genesis of the area that have been presented so far still have a gap in the light of contemporary interpretation of the concept of periglacial environment. There is a need to take into account the so-called paraglacial environment, which has hardly been distinguished until now in areas of Pleistocene glaciation. According to present knowledge, the relief of the Warta belt in Central Poland should be recognised as polygenic with predominant features of old glacial relief and with elements of paraglacial, periglacial and fluvio-denudational relief from moderate periods.

Źródło:

Landform Analysis; 2014, 27; 35-43
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 7.

Tytuł:

Geomorphology, sedimentology and origin of the glacigenic Złota Góra hills near Konin (Central Poland)

Autorzy:

Widera, M.

Powiązania:

https://bibliotekanauki.pl/articles/2059142.pdf

Data publikacji:

2011

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Poland
sandur
end moraine
interlobate landform

Opis:

The Złota Góra hills (Central Poland) have been variously interpreted as a kame, a sandur and as different types of moraine. Due to their morphology and internal structure, the Złota Góra hills differ, however, from typical depositional glacigenic landforms in the European lowlands. Morphologically, the Złota Góra hills consist of numerous asymmetrical and oval hills of various sizes. The deposits show a wide variety of lithofacies, which are diagnostic for debris flows, hyperconcentrated flows, sheetfloods, braided rivers, deltas and ephemeral lakes. The combination of such deposits is characteristic of an environmental setting including both an end moraine fan (debris flows, hyperconcentrated flows, sheetfloods and ephemeral lake deposits) and a sandur (braided river, sheetfloods, and delta or ephemeral lake deposits). Therefore, these hills must be interpreted as representing an end moraine/sandur massif. The hills were probably formed subaerially by meltwater in an interlobate area of the retreating Scandinavian ice sheet.

Źródło:

Geological Quarterly; 2011, 55, 3; 253-268
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 8.

Tytuł:

Ostracods from the Purbeckian of Central Poland
Małżoraczki z purbeku Polski Środkowej

Autorzy:

Sztejn, J.

Powiązania:

https://bibliotekanauki.pl/articles/23135.pdf

Data publikacji:

1991

Wydawca:

Polska Akademia Nauk. Instytut Paleobiologii PAN

Tematy:

ostracod
Purbeckian
Central Poland
Polska
Ostracoda
paleontology

Opis:

The recent stratigraphical and paleontological research in the Jurassic/Cretaceous boundary sequence in central Poland confirmed a validity of the hitherto accepted local ostracod zonation. Six ostracod zones have been compared with the zones distinguished in England, France and Germany. From 51 ostracod species and subspecies recorded in the sequence of superposing marine-brackish and brackish-fresh-water sediments the author describes the following new species and subspecies: Limnocythere biverrucosa, Timiriasevia polonica, Cypridea aleksandrowiensis, C. wandae, C. binodosa polonica, C. dunkeri spinosa, C. granulosa polonica, C. lata polonica, C. obliqua polonica, C. prealta iuvencula and C. tumescens granulosa.
W pracy ukazano zróżnicowanie zespołów małżoraczkowych w purbeku Kujaw (figs. 1—4, tabele 1—2) oraz przedstawiono opisy i ilustracje (pls. 1—8) 4 nowych gatunków (Limnocythere biverrucosa, Timiriasevia polonica, Cypridea aleksandrowiensis, C. wandae) i 7 podgatunków (Cypridea binodosa polonica, C. dunkeri spinosa, C. granulosa polonica, C. lata polonica, C. obliqua polonica, C. prealta iuvencula, C. tumescens granulosa). Dotychczasowe badania zespołów małżoraczków purbeckich były oparte na stosunkowo niewielkiej liczbie gatunków. Znaczne powiększenie kolekcji, które się dokonało w ciągu ostatnich lat, umożliwiło przeprowadzenie rewizji uzyskanych dotąd wyników. Nowe obserwacje pozwoliły utrzymać dotychczasowy, lokalny podział stratygraficzny purbeku na 6 poziomów małżoraczkowych, określonych literami od F do A (por. Bielecka i Sztejn 1966). Na podstawie nowych danych można polskie poziomy małżoraczkowe wiązać z poziomami z Europy zachodniej. Osady purbeku w Polsce są w pełni wykształcone tylko na Kujawach i tylko tam można stwierdzić obecność wszystkich lokalnych poziomów małżoraczkowych. W poziomie F, osady facji purbeckiej tworzyły się w środowisku morskim o okresowo mniejszym lub większym zasoleniu. W poziomie E, w centralnej części zbiornika oberwuje się mikrofaunę środowiska morskiego, a wśród osadów ewaporatowych (we wkładce wapiennej) nieliczne małżoraczki, które najprawdopodobniej reprezentują środowisko hypersalinarne. Ubożenie taksonomiczne i masowy rozwój małżoraczków rodzaju Cypridea świadczą o okresowym wysładzaniu się zbiornika, które powiększało się następnie w poziomie D. W poziomach C i В środowisko stało się brakiczno-słodkowodne, a następnie w poziomie A, przez zwiększenie zasolenia, stało się środowiskiem morsko-brakicznym. Analogicznie do purbeku Anglii (por. Anderson 1985), w polskim purbeku wyróżniono zespoły małżoraczków charakterystyczne dla trzech faz ekologicznych: brakiczno-słodkowodnej fazy C, morsko-brakicznej fazy S oraz hypersalinarnej fazy E. Na Kujawach przeważają małżoraczki fazy S (fig. 2). W polskim purbeku obserwuje się zdecydowaną przewagę małżoraczków nad otwornicami. Stwierdzono tu obecność następujących nadrodzin małżoraczków. Cytheracea, Darwinulacea i Cypridacea. Szczególnie wiele rodzajów należy do Cytheracea. Niektóre małżoraczki, jak Klieana alata Martin, Rhinocypris jurassica (Martin), Cypridea prealta prealta Bielecka i C. lata polonica subsp. n. występują masowo i w kolekcji liczą od około tysiąca do kilku tysięcy skorupek. Inne są reprezentowane zaledwie przez kilka lub kilkanaście egzemplarzy, do nich należą M. (Macrodentina) maculata Malz, M. (Dictyocythere) aff. mediostricta transfuga Malz i Protocytheropteron brodiei (Jones). Otwornice, to nieliczne formy zlepieńcowate. Wśród nich najlepiej jest reprezentowany rodzaj Ammobaculites, wykazujący bardzo dużą tolerancję na zmiany zasolenia w środowisku.

Źródło:

Acta Palaeontologica Polonica; 1991, 36, 2
0567-7920

Pojawia się w:

Acta Palaeontologica Polonica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 9.

Tytuł:

Z badań nad neolityzacją polski środkowej. Pozostałości osadnictwa kultury pucharów lejkowatych ze stanowiska Polesie 1, gm. Łyszkowice

Autorzy:

Rzepecki, Seweryn

Powiązania:

https://bibliotekanauki.pl/articles/1023946.pdf

Data publikacji:

2015-01-01

Wydawca:

Uniwersytet im. Adama Mickiewicza w Poznaniu

Tematy:

Funnel Beaker culture
Neolithisation
Polesie
central Poland

Opis:

The article presents the results of the study of the Funnel Beaker culture settlement at site Polesie 1, com. Łyszkowice. There have been recognised very damaged remnants of a settlement and campsites of Neolithic communities. The author of the study links them to the process of colonisation, which had started in Kujawy or eastern Wielkopolska.

Źródło:

Folia Praehistorica Posnaniensia; 2015, 20; 429-447
0239-8524
2450-5846

Pojawia się w:

Folia Praehistorica Posnaniensia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 10.

Tytuł:

Geotectonic significance of Carboniferous deposits NW of the Holy Cross Mts. (central Poland)

Autorzy:

Jaworowski, K.

Powiązania:

https://bibliotekanauki.pl/articles/2059900.pdf

Data publikacji:

2002

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Poland
Carboniferous
debrites
turbidites
flysch
pseudoflysch

Opis:

Carboniferous sandstones and shales encountered in deep boreholes drilled in central Poland, NW of the Holy Cross Mts., represent a pseudoflysch i.e. they show facies features of flysch and, simultaneously, are of cratonic provenance. Clastic sediments were derived from a peripheral bulge formed within the East European Craton as a result of stresses exerted by the accretion/thrust wedge advancing up the marginal part of the craton. In central Poland, NW of the Holy Cross Mts., a Variscan foredeep existed. The foredeep was the depositional site of interfingering exo- and pseudoflysch which, from a geodynamic point of view, are equivalent to an outer molasse. Huge masses of Carboniferous deposits (generally corresponding to flysch) from southwestern and central Poland successively represent, moving from SW to NE, Variscan ortho-, exo- and pseudoflysch.

Źródło:

Geological Quarterly; 2002, 46, 3; 267-280
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 11.

Tytuł:

Lithological features of Vistula River channel deposits in the light of micromorphological analysis

Autorzy:

Bielawska, M.

Powiązania:

https://bibliotekanauki.pl/articles/294771.pdf

Data publikacji:

2015

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

micromorphology
alluvial sediments
Vistula river
Central Poland

Opis:

The aim of the study was to identify and assess the lithological features typical for alluvial sediments of Vistula River from the natural part of its course on 603 km of the river course. For this purpose, the micromorphological analysis was carried out for a sample taken from the surface of a tree covered island. The analysis is laborious, but its great advantage is that it allows to determine the detailed characteristics of undisturbed sediments, supplying other lithological studies. Examined thin section showed fractionation lamination within medium and fine sands, interbedded with coarser grains with some organic admixtures. Detailed analysis allows to detect gradual and sudden changes of discharge energy.

Źródło:

Landform Analysis; 2015, 29; 3-8
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 12.

Tytuł:

Impact of Land Use Changes and Dynamic Vegetation Changes on Vascular Flora Diversity in Małków–Bartochów (the Warta River Valley)

Autorzy:

Woziwoda, Beata
Michalska-Hejduk, Dorota

Powiązania:

https://bibliotekanauki.pl/articles/764831.pdf

Data publikacji:

2011

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

flora
peatland
land use
degradation
Central Poland

Opis:

The paper presents the changes of vascular plant flora in the Małków–Bartochów peatland area (the Warta River valley) which took place over a 40-year period. Vanishing, permanent and new components of the flora are presented with a special focus on valuable (protected by the law, threatened and locally rare) species. Changes in the share of ecological groups are estimated and discussed. Anthropogenic and natural factors, directly or indirectly influencing (in the past and at present) flora composition, are noted and analyzed.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2011, 7; 125-138
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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• na półce

Skocz do pozycji: 13.

Tytuł:

Adaptation of the “Herbarium” Computer Database to Archiving and Analysis of Floristic Data

Autorzy:

Zielińska, Katarzyna
Jakubowska-Gabara, Janina
Kołodziejek, Jeremi

Powiązania:

https://bibliotekanauki.pl/articles/764852.pdf

Data publikacji:

2010

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

database
floristic data
cartogram method
Central Poland

Opis:

The aim of the study was to present “Herbarium” computer database. The basic goal of construction of the database was gathering and analysing of archival and contemporary floristic data referring to the area of Central Poland. Registered information considers the stands and characteristic biological and ecological traits of particular taxa. Life forms, indices of ecological requirements, the phytogeographical elements, protection and threat status are among them. The database enables the presentation of geographical distribution of taxa in the area of Central Poland with the cartogram method based on the grid of 2 km2 according to the Distribution Atlas of Vascular Plants in Poland (ATPOL).

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2010, 6; 145-150
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 14.

Tytuł:

Isotopic and Cladocera records of climate changes of Early Eemian at Besiekierz (Central Poland)

Autorzy:

Mirosław-Grabowska, J.
Niska, M.

Powiązania:

https://bibliotekanauki.pl/articles/2059552.pdf

Data publikacji:

2005

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Poland
palaeoclimate
Eemian Interglacial
cladocera
stable isotopes

Opis:

Results of stable isotope, Cladocera and pollen analyses of lacustrine sediments from Besiekierz (Central Poland) are presented. The Besiekierz palaeolake is located about 25 km north of Łódź (Central Poland) at 130 m a.s.l. The 4 m thick deposits comprise silty sands and clayey silts, overlain by calcareous gyttja and organic silts and peat. Pollen analysis documents that these deposits accumulated during the Eemian Interglacial and the Early Vistulian. Based on the results of stable isotope analyses, nine isotopic horizons (Is) were defined and characterized, and these enabled reconstruction of both climatic and hydrological changes. A positive trend in δ18O values and constant values of δ 13 suggest gradual climatic warming, while constant values of δ 18O and δ 13C indicate stable conditions and/or a fast rate of sedimentation. The fluctuation of isotopic values in the upper part of the succession probably points to a shallowing of the lake due to sedimentary infill. The subfossil cladoceran fauna in the Besiekierz succession is represented by 11 solely littoral species belonging to 3 families. Four zones of Cladocera development were distinguished. The Besiekierz palaeolake was a shallow reservoir. The initial period of its existence probably saw its greatest depth. The Cladocera species present indicate the initial oligotrophic status of the lake and its subsequent increase in trophic status.We compare the results of the isotopic, cladoceran and published palynological analyses, to distinguish and explain the phases of evolution of the lake.

Źródło:

Geological Quarterly; 2005, 49, 1; 67--74
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 15.

Tytuł:

The provenance of erratic pebbles from a till in the vicinity of the city of Radom, central Poland

Autorzy:

Strzelecki, Piotr Jan

Powiązania:

https://bibliotekanauki.pl/articles/184706.pdf

Data publikacji:

2019

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Pleistocene
MIS 6
indicator erratics
till
Central Poland

Opis:

Petrographic analysis, including the indicator erratics count method of coarse pebbles (20–60 mm), was performed for the first subsurface layer of the glacial till in the vicinity of the city of Radom. Crystalline rocks comprise 60% of the sample, whereas carbonate and clastic sedimentary rocks total 18% and 15%, respectively. Among the crystalline rocks, 14% clasts were identified as indicator erratics. The majority of the indictor erratics originated from the Åland region (63%). Significant contributions were also derived from the central Baltic Basin (12%), Ångermanland (9%) and Uppland (9%) regions. Trace amounts are recorded from the northern Baltic, Dalarna and Småland regions. The spatial distribution of crystalline erratic source areas suggests material incorporation into an ice sheet mainly from central-eastern Fennoscandia. The indicator assemblage composition indicates the Odranian (MIS 6) origin of the till. The majority of the erratic sedimentary rocks were derived from the central and southern Baltic Basin while local rocks comprise a minor proportion. The relatively low carbonate clasts content indicates that the till was affected by partial decalcification resulting from post-depositional chemical weathering. This study supplements the results on erratic pebble provenance in the glacial tills of Middle Polish Glaciation Complex in Poland.

Źródło:

Geology, Geophysics and Environment; 2019, 45, 1; 21-29
2299-8004
2353-0790

Pojawia się w:

Geology, Geophysics and Environment

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 16.

Tytuł:

The distinctive shapes of some kame ridges in the Łódź region of Central Poland

Autorzy:

Klajnert, Z.

Powiązania:

https://bibliotekanauki.pl/articles/295044.pdf

Data publikacji:

2002

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

kame
relief
deglaciation
Łódź region of Central Poland

Opis:

In the central part of the Rawka lobe of the Warta stage ice sheet of the Middle Polish glaciation (Saalian), areal déglaciation took place in the vicinity of Łódź. This is indicated by the numerous kames here, among which ridge forms are conspicuous. Some of the ridges which are situated on the slopes of river valleys and on the slopes terrain depression possess unusual shapes which resemble „tongues" and „paws". These forms merge gently with the adjacent elevated upland, whereas their distal parts are sharply defined and may lie as much as several decametres above their bases. „Kame tongues" and „karne paws" are built from paraglaciolacustrine and glaciofluvial deposits which accumulated in water bodies between dead ice blocks during the final phases of the ice sheet downwasting. The distinctive shapes of the landforms result from the varying thickness of the dead ice masses: thinner on the elevations and significantly thicker in terrain depressions (mainly in large, subglacial pre-Wartian valleys). These characteristic kame ridges demonstrate that the more elevated parts of the subglacial surface had been ice free for a long time before the dead ice blocks eventually disappeared from the terrain depressions.

Źródło:

Landform Analysis; 2002, 3; 63-75
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 17.

Tytuł:

The results of new studies of Quaternary sediments in the Kleszczów Graben, Szczerców Outcrop, Bełchatów Lignite Opencast Mine

Autorzy:

Wieczorek, D.
Stoiński, A.
Krzyszkowski, D.
Wachecka-Kotkowska, L.
Krzymińska, J.

Powiązania:

https://bibliotekanauki.pl/articles/295132.pdf

Data publikacji:

2015

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

Quaternary
stratigraphy
Kleszczów Graben
Szczerców Outcrop
Central Poland

Opis:

The paper presents the results of new studies of Quaternary deposits filling the Kleszczów Graben in the Szczerców outcrop, Bełchatów Lignite Opencast Mine. Sedimentary successions were profiled in the fieldwork. Moreover, the borehole data were studied. Laboratory studies included: grain size analyses, analyses of shape and morphology of quartz grain (morphoscopy), analyses of anisotropy of magnetic susceptibility (AMS), palynological, malacological and ostracodological studies, as well as geochronometric (C14) and geochemical (δ18O/δ16O) measurements. The studies were carried out in 2009–2013 and resulted in discovering of some sedimentary formations as well as arranging geological cross-sections and synthetic lithostratigraphic profile. The following sedimantary formations have been distinguished: Folwark, Kuców, Czyżów, Ławki, Rogowiec, Aleksandrów, Piaski and Widawka, arranged into two structural units: the lower one – deformed, and the upper one – undeformed.

Źródło:

Landform Analysis; 2015, 29; 63-71
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 18.

Tytuł:

Medical segetal flora of Central Poland

Autorzy:

Warcholińska, Aurelia Urszula

Powiązania:

https://bibliotekanauki.pl/articles/764914.pdf

Data publikacji:

2008

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

flora
medical plants
endangered medical plants
Central Poland

Opis:

In the paper a list and general characterization of medical segetal flora of Central Poland is given. This flora consists of 300 taxa. Among the most threatened species there are 6 taxa: Adonis aestivalis, A. flam mea, Anagallis foemina, Bupleurum rotundifolium, Camelina saliva, Cuscuta europaea.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2008, 4
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

Artykuł

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Skocz do pozycji: 19.

Tytuł:

Vascular plants flora of the railway grounds of Łask

Autorzy:

Warcholińska, Aurelia Urszula
Suwara-Szmigielska, Sylwia

Powiązania:

https://bibliotekanauki.pl/articles/764991.pdf

Data publikacji:

2008

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

flora
vascular plants
railway grounds
Łask
Central Poland

Opis:

In the paper a list and general characterization of vascular plants flora recorded on railway grounds of Łask is presented. The great diversity of habitats within the railway grounds as well as their readiness to accept numerous introduced species result in high variety of vascular plants there. This flora consists of 369 taxa.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2008, 4
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 20.

Tytuł:

The Vascular Flora of the Railway Grounds of the Pabianice Town

Autorzy:

Warcholińska, Aurelia Urszula
Suwara-Szmigielska, Sylwia

Powiązania:

https://bibliotekanauki.pl/articles/764888.pdf

Data publikacji:

2009

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

flora
vascular plants
railway grounds
Pabianice
Central Poland

Opis:

In the paper a list and general characterization of vascular plants recorded on railway grounds of the town of Pabianice is presented. The great diversity o f habitats within the railway grounds as well as their inclination to be colonized by numerous introduced species resulted in high variety of vascular plants there. This flora consists of 382 taxa.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2009, 5; 21-41
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 21.

Tytuł:

Petrography of glacial tills in the szczerców out crop, central poland – problems of stratigraphic interpretation

Autorzy:

Krzyszkowski, Dariusz
Wachecka-Kotkowska, Lucyna
Wieczorek, Dariusz
Stoiński, Andrzej

Powiązania:

https://bibliotekanauki.pl/articles/2025804.pdf

Data publikacji:

2015

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

tills
petrography
lithostratigraphy
Pleistocene
central Poland
Kleszczów Graben

Opis:

The pa per pres ents re sults of petrographic anal y ses of gla cial tills in the west ern part of the Kleszczów Graben and the at tempt of their strati graphic in ter pre ta tion. Petrographic co ef fi cients have al lowed the iden ti fi ca tion of five till lithotypes: T1, T2A, T2 and T2B – as signed to the South Pol ish Com plex (Elsterian) and T4 cor re lated with the Mid dle Pol ish Com plex (Saalian). The well-ex pressed tills that rep re sent the South Pol ish Com plex, oc cur at the bot tom of the sec tion. A new till lithotype, T2B, has been dis tin guished, cor re spond ing to the Kuców For ma tion. It sup ple ments the Pleis to cene lithostratigraphic sec tion of cen tral Po land and cor re sponds to the Sanian 2 Gla ci ation. Among the younger tills, the T4 one (Odranian Gla ci ation) is well de vel oped. The up per most tills of the Wartanian cold stage have been re duced by glaciofluvial and flu vial ero sion. It is, to some ex tent a con se quence of the ex is tence of a de pres sion in this area, called the Szczerców Ba sin. The pa per high lights the in ter pre ta tional dif fi cul ties con cern ing the rank and the num ber of ice sheet ad vances dur ing the Pol ish and Mid dle Pol ish Com plexes in cen tral Poland.

Źródło:

Studia Quaternaria; 2015, 32; 99-108
1641-5558
2300-0384

Pojawia się w:

Studia Quaternaria

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 22.

Tytuł:

The Tithonian Chitinoidellidae and other microfossils from Owadów–Brzezinki quarry (central Poland)

Autorzy:

Pszczółkowski, A.

Powiązania:

https://bibliotekanauki.pl/articles/2060991.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Tithonian
microfossils
Central Poland
tyton
mikroskamieniałości
Polska Centralna

Opis:

Tithonian (= “Middle Volgian”) carbonate rocks are exposed in Owadów-Brzezinki quarry 19 km southeast of Tomaszów Ma-zowiecki, central Poland. In the upper part of the Sławno Limestone Member, chitinoidellids have been identified in thin sections from three samples, only. Therefore, the documented part of the Chitinoidella Zone in Owadów-Brzezinki quarry is about 0.3 m thick. The identified chitinoidellid taxa suggest that this assemblage represents the Upper Tithonian Boneti Subzone. The Chitinoidella Zone occurs at the top of Unit I and correlates with the uppermost interval of the Zarajskensis Horizon (Matyja, Wierzbowski, 2016). Other microfossils identified in the Chitinoidella Zone consist of Saccocoma sp. and benthic foraminifera of the genus Planularia. Calcareous dinoflagellate cysts (Cadosina semiradiata semiradiata Wanner and C. cf. semiradiata semiradiata Wanner) occur above the chitinoidellid assemblage, in the strata corresponding to the Gerassimovi Subzone of the Virgatus Zone (Matyja, Wierzbowski, 2016). Calcareous nannofossils are extremely rare in the thin sections studied; only one small specimen was seen, identified as Rhombolithion minutum (Rood et al., 1971) Young et Bown 2014. In contrast, microbial filaments are frequently observed in the studied thin sections. Their shape and pattern are reminiscent of some recent Cyanobacteria of the order Nostocales, however the Tithonian microbial filaments are much thinner.

Źródło:

Volumina Jurassica; 2016, 14, 1; 133--144
1896-7876
1731-3708

Pojawia się w:

Volumina Jurassica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 23.

Tytuł:

Palynology of biogenic sediments of the Eemian Interglacial at Bieganin near Kalisz, Central Poland

Autorzy:

Malkiewicz, M.

Powiązania:

https://bibliotekanauki.pl/articles/2058816.pdf

Data publikacji:

2003

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Poland
Eemian Interglacial
pollen analysis
history of vegetation

Opis:

The paper presents palynological data from Bieganin, a village located near Kalisz, Central Poland, where organic sediments were deposited in a subglacial trough dating from the Wartanian Glaciation. The succession of vegetation is characteristic of the Eemian Interglacial. The pollen diagram indicates six local pollen assemblages: B1-Pinus-Betula, B2-Betula-Pinus-Ulmus, B3-Quercus-Corylus, B4 -Corylus, B5-Carpinus-Tilia-Polypodiaceae, B6-Pinus-Picea which correlate well with regional pollen assemblages obtained by Mamakowa (1989b) and Tobolski (1991). The plant succession in Bieganin started in the beginning of the Eemian (zone E1) and ended with the development of coniferous forest (zone E6). The profile does not include the final zone, E7, of the interglacial.

Źródło:

Geological Quarterly; 2003, 47, 4; 367-372
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 24.

Tytuł:

Cyclic sedimentation in the Middle Jurassic of central Poland

Autorzy:

Dadlez, J.

Powiązania:

https://bibliotekanauki.pl/articles/2059894.pdf

Data publikacji:

2002

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Poland
Middle Jurassic
stratigraphy
cyclic sedimentation
salt mobility

Opis:

Nine boreholes were drilled in the late eighties in central Poland to investigate the Middle Jurassic sedimentary successions. The boreholes were arranged in three lines (Ciechocinek, Brześć Kujawski and Wojszyce lines) running across three anticlines underlain by salt pillows. Long intervals of boreholes have been cored, often with 100% core recovery, thus enabling a detailed examination of sedimentary evolution. Sequences are composed of a full range of clastic rocks, from conglomerates through sandstones and heteroliths to shales. They are arranged in sedimentary cycles, predominantly regressive (coarsening upwards). These are interpreted as deposited in a shallow, wave/storm-dominated, shelf environment, each cycle being a result of progradation of fore-shore to near-shore heteroliths and sands over the shales of an open sea. The basin was probably non-tidal or microtidal. These essential (lower order) cycles, equivalents of the IVth order cycles in the world-wide scheme, are assembled in higher order cycles which resemble the IIIrd order cycles of that scheme. The bases of the higher order cycles are good lithostratigraphic markers, three of them being probably equivalents of chronostratigraphic boundaries (bases of the upper Aalenian, upper Bajocian and Bathonian, respectively). Correlation of borehole sections points to limited salt movement of the Ciechocinek and Wojszyce salt pillows during the Middle Jurassic. These are indicated, first of all, by thickness reductions seen in boreholes located above the tops of salt pillows. In the Ciechocinek area, the upward movement of salt occurred during the latest Bajocian/earliest Bathonian while in the Wojszyce area - during the early Bathonian. Coarser clastics were shed into the basin from the south-west, north-west (along the Mid-Polish Trough) and north-east during the Aalenian, and mainly from the north-east (from the East European Craton) in later times.

Źródło:

Geological Quarterly; 2002, 46, 3; 321-336
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 25.

Tytuł:

A new Eemian Interglacial to Early Vistulian site at Łanięta, central Poland

Autorzy:

Balwierz, Z.
Roman, M.

Powiązania:

https://bibliotekanauki.pl/articles/2059929.pdf

Data publikacji:

2002

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Central Poland
Eemian Interglacial
Early Vistulian
lake sediments
palynostratigraphy

Opis:

The Łanięta site with fossil lake deposits is situated just in front of the maximum extent of Vistulian Glaciation ice. Palynological analysis shows that lake accumulation lasted through the Eemian Interglacial and almost the whole Early Vistulian, the longest record of this time interval in this part of Poland. Two warm interstadial-rank oscillations (Brörup and Odderade) and two stadials have been distinguished during the Early Vistulian. The older of these is correlated with the Herning Stadial while younger one equates with the Rederstal Stadial of the German succession.

Źródło:

Geological Quarterly; 2002, 46, 2; 207-218
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 26.

Tytuł:

Structural and textural response to dynamics of fluvioglacial processes of the Rzymsko esker sediments, Central Poland

Autorzy:

Frydrych, M.

Powiązania:

https://bibliotekanauki.pl/articles/184781.pdf

Data publikacji:

2016

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

glacifluvial sediments
clast shape
esker
Central Poland
Warta Glaciation

Opis:

The study was conducted in the Rzymsko esker, in the Eastern part of the Turek Upland Plain, within the range of the Warta Glaciation (Saalian II). The form was accumulated in a tunnel valley, which was partially filled with esker sediments. Lithofacies analysis, extended by a detailed analysis of clasts, made it possible to identify a considerable variability of sedimentation conditions. At the initial stage, transport and accumulation of sediments took place in the conditions of high energy hydraulic flows or hyperconcentrated flows. The flow energy rose cyclically, which was recorded as sediments coarsening. Deposits of boulders as well as massive and cross-bedded gravels were identified, a record of catastrophic glacial floods. During the later stage of esker formation, sandy and gravelly sediments were accumulated in an open crevasse. The strong erosional force of subglacial water is confirmed by an extremely high content of local rocks in the gravelly fraction (30–87%) and its very good roundness. Zingg shape analysis (1935) revealed a clear predominance of oblate forms among local clasts and equant fennoscandian erratics. A dependency was also found between the processing method and petrographic characteristics.

Źródło:

Geology, Geophysics and Environment; 2016, 42, 4; 411-428
2299-8004
2353-0790

Pojawia się w:

Geology, Geophysics and Environment

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 27.

Tytuł:

Vascular plants flora of the railway grounds of Zduńska Wola

Autorzy:

Warcholińska, Aurelia Urszula

Powiązania:

https://bibliotekanauki.pl/articles/764916.pdf

Data publikacji:

2008

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

flora
vascular plants
railway grounds
Zduńska Wola
Central Poland

Opis:

In the paper a list and general characterization of vascular plants flora recorded on railway grounds in the city of Zduńska W ola is presented. The great diversity of habitats within the railway grounds as well as their readiness to accept numerous introduced species result in a high variety of vascular plants there. This flora consists of 366 taxa.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2008, 4
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

Artykuł

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Skocz do pozycji: 28.

Tytuł:

Distribution of endangered and protected species of synanthropic plants in Łask

Autorzy:

Suwara-Szmigielska, Sylwia

Powiązania:

https://bibliotekanauki.pl/articles/764927.pdf

Data publikacji:

2008

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

synanthropic flora
protected and endangered species
Łask
Central Poland

Opis:

The article presents description and distribution of protected and endangered species of synanthropic plants found in the Łask area in 2001-2002. The research was carried out with the use of a cartogram method. As a result, ten species of protected plants were found in the researched area, four of which under strict protection, and six under partial protection. Eight out of the ten protected species are in the danger of extinction.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2008, 4
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 29.

Tytuł:

Plant macrofossils from the Czyżów Complex deposits of the Szczerców outcrop, central Poland

Autorzy:

Myśkow, E.
Krzyszkowski, D.
Wachecka-Kotkowska, L.
Wieczorek, D.

Powiązania:

https://bibliotekanauki.pl/articles/184237.pdf

Data publikacji:

2016

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

fluvial sediments
plant macrofossils
Holsteinian
Czyżów Complex
Central Poland

Opis:

The paper presents the results of research into the plant macrofossils found in the tectonic Kleszczów Graben, within Mesopleistocene sandy sediments. A number of samples were collected at eight locations from river sediments containing variously sized fragments of plants, mostly from greenish sands overlying Neogene sediments. The structural characteristics of the sediments show a cyclic record of the formation of point bars, their washing out at supercritical conditions, and their aggradation by fine-grained material during flow waning. Based on lithological and structural studies, it has been demonstrated that the sands accumulated in an environment of a meandering river, whose valley bottom was covered with fairly dense vegetation, inhibiting the influx of mineral material to the floodplain from the surroundings – the valley or glacial plateau slopes. The aim of further analysis was to identify the plant genera of the individual macrofossils (about 40 specimens). The most numerous macrofossils were observed in the middle layers of the profile, within sandy megaripple structures, where mostly fragments of Fraxinus and Acer wood were present. In other layers, several fragments of Pinus and three pieces of Populus wood were identified. Additionally, young stems of dicotyledonous plants and fragments of rhytidome (the outer bark of a tree) were found. The results are discussed in combination with considerations on the deposition of the Czyżów Complex in the Bełchatów outcrop, and on the occurrence of local flora.

Źródło:

Geology, Geophysics and Environment; 2016, 42, 3; 325-336
2299-8004
2353-0790

Pojawia się w:

Geology, Geophysics and Environment

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 30.

Tytuł:

NOWE STANOWISKO DIPLOSCHISTES MUSCORUM (Scop.) R. Sant. na NIZINIE WIELKOPOLSKO-KUJAWSKIEJ

Autorzy:

Zarabska–Bożejewicz, Daria

Powiązania:

https://bibliotekanauki.pl/articles/942686.pdf

Data publikacji:

2017

Wydawca:

Poznańskie Towarzystwo Przyjaciół Nauk

Tematy:

Diploschistes muscorum
distribution
lichens
rare species
west-central Poland

Opis:

Diploschistes muscorum (Scop.) R. Sant. has been found in the southern part of the Wielkopolsko-Kujawska Lowland. So far, in western and central Poland the species has been reported in few localities.

Źródło:

Badania Fizjograficzne Seria B - Botanika; 2017, 65; 129-135
2082-3339

Pojawia się w:

Badania Fizjograficzne Seria B - Botanika

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 31.

Tytuł:

Beetles (Coleoptera) of the Rogów region. Part XI – a supplement to parts I-X

Autorzy:

Borowski, Jerzy

Powiązania:

https://bibliotekanauki.pl/articles/1065178.pdf

Data publikacji:

2019

Wydawca:

Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN

Tematy:

Coleoptera
Insecta
Rogów region
bionomy
central Poland
faunistic data

Opis:

In the eleventh part of the series entitled “Beetles (Coleoptera) of the Rogów region” presents supplementary information on new or rare beetles of four families: Dermestidae, Coccinellidae, Cerambycidae and Curculionidae – Scolytinae. All species are very rare or new for the Rogów region. The faunistic data of the listed species is supplemented by bionomical information.

Źródło:

World Scientific News; 2019, 120, 2; 282-285
2392-2192

Pojawia się w:

World Scientific News

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 32.

Tytuł:

The relationship between the chemical composition and lithology of Late Glacial and Holocene biogenic deposits of the Żabieniec mire (Central Poland)

Autorzy:

Okupny, Daniel
Borówka, Ryszard Krzysztof
Forysiak, Jacek
Twardy, Juliusz
Kloss, Marek
Żurek, Sławomir

Powiązania:

https://bibliotekanauki.pl/articles/2058726.pdf

Data publikacji:

2021

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

kettle hole
limnogenic mire
geochemistry
macrofossils
denudation
Central Poland

Opis:

Geochemical and plant macrofossil analyses of the Żabieniec mire deposits and the palaeoenvironmental changes they record of the past several thousand years constitute an important source for palaeogeographical reconstruction of the Polish Lowland. We describe the phases of the basin’s development from the final part of the Plenivistulian (MIS2), through the Late Glacial and the entire Holocene, encompassing changes determined by both regional and global factors in the surrounding environment, and habitat transformations in the limnogenic mire. The kettle-hole infill of the Żabieniec mire is the only documented example in Central Poland of a succession of biogenic deposits exceeding 10 m in thickness in such a setting. Deposition initially took place in a lake environment, which led to a shallowing of the lake that persisted until the end of the Mesoholocene.

Źródło:

Geological Quarterly; 2021, 65, 1; 11
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 33.

Tytuł:

Drobne ssaki północnej części Puszczy Kozienickiej na podstawie analizy diety puszczyka Strix aluco
Small mammals of the northern part of the Kozienice Forest based on the analysis of the tawny owl Strix aluco diet

Autorzy:

Lesiński, G.
Wojtowicz, B.

Powiązania:

https://bibliotekanauki.pl/articles/2090092.pdf

Data publikacji:

2021

Wydawca:

Mazowiecko-Świętokrzyskie Towarzystwo Ornitologiczne

Tematy:

Mammalia
species composition
owl pellets
woodland
Glis glis
central Poland

Opis:

The analysis of the composition of the Tawny Owl pellets collected at a study site (Stary Chinów, 51o37’N, 21o28’E) in the northern part of the Kozienice Forest in 2019-2021 documented 18 species of small mammals. They represented three orders: Soricomorpha (4), Chiroptera (3), and Rodentia (11). The community of small mammals in the study area was relatively rich. The most frequently noted species were: Sorex araneus, Clethrionomys glareolus, Microtus agrestis and Apodemus flavicollis. The populations of rodents of the family Gliridae (Muscardinus avellanarius, Glis glis) and Microtus agrestis living on the study site are relatively abundant as compared to other areas of central Poland.

Źródło:

Kulon; 2021, 26; 69-75
1427-3098

Pojawia się w:

Kulon

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 34.

Tytuł:

Potential Values of Urban Geotourism Development in a Small Polish Town (Pruszków, Central Mazovia, Poland)

Autorzy:

Górska-Zabielska, Maria
Zabielski, Ryszard

Powiązania:

https://bibliotekanauki.pl/articles/1052447.pdf

Data publikacji:

2017-09-15

Wydawca:

Uniwersytet im. Adama Mickiewicza w Poznaniu

Tematy:

abiotic resources
geodiversity
urban geotourism
south-western Mazovia
central Poland

Opis:

The paper presents abiotic resources which are located in a small town in central Poland. They remain unknown to authorities and inhabitants. For the first time they are illustrated in a scientific paper. The objects of local geological heritage point to geodiversity of this district town in the south-western Mazovia. When the geodiversity is interpreted in a simple, an understandable way, it may become attractive for tourists. We show how abiotic resources located within an urban area can be used to support urban geotourism development. The scientific, educational and aesthetic values of these resources may create the town image in accordance with the principles of environmental protection.

Źródło:

Quaestiones Geographicae; 2017, 36, 3; 75-86
0137-477X
2081-6383

Pojawia się w:

Quaestiones Geographicae

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 35.

Tytuł:

Estimation of Population Size of Dentaria Enneaphyllos in the Vicinity of the Bełchatów Brown Coal Mine and the Attempt of Its Metaplantation

Autorzy:

Kurowski, Józef K.
Koczywąs, Ewelina
Pieńkowski, Michał

Powiązania:

https://bibliotekanauki.pl/articles/764821.pdf

Data publikacji:

2011

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

metaplantation
Dentaria enneaphyllos
Central Poland
the Bełchatów Brown Coal Mine

Opis:

The impact of anthropopressure on the flora in the vicinity of the Bełchatów Brown Coal Mine in Central Poland has been substantially strong. Consequently, certain changes in habitat conditions have been observed, leading to a decline in particular species stands. Mechanical damage, as well as the mine and power plant expansion have contributed to further species decline in the area. Ex situ conservation, e.g. metaplantation from native to secondary localities seems an efficient method of ensuring the species survival in the local flora. One of the species is to be found in Wola Wydrzyna (under the Forest District Administration of Bełchatów) is Drooping Bittercress Dentaria enneaphyllos. Its population was first recorded in the area in 1979. However, since 2009 the forest complex has undergone a regular expansion of the Bełchatów Brown Coal Mine. The forest area is to be utilised for the future Szczerców coal deposit. Therefore, in 2000 the method of Dentaria enneaphyllos metaplantation was applied.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2011, 7; 247-259
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 36.

Tytuł:

Transformation of Forest Vegetation after 40 Years of Protection in the Tomczyce Nature Reserve (Central Poland)

Autorzy:

Kiedrzyński, Marcin
Zielińska, Katarzyna
Grzelak, Paulina

Powiązania:

https://bibliotekanauki.pl/articles/764874.pdf

Data publikacji:

2011

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

forest regeneration
mixed pine-oak forest
nature protection
Central Poland

Opis:

The Tomczyce nature reserve is characterized by a degenerated forest vegetation. We assume that the regeneration process was possible to launch after the establishment of the nature reserve in 1968. The vegetation of the Tomczyce forest complex was characterized for the first time by Jakubowska-Gabara (1976) whose studies were taken as a basis of our research. The phytocenoses after 40. years of protection have a greater participation of species with higher trophic and moisture requirements. The regeneration process in communities with pine trees is caused by an expansion of broad-leaved trees and shrubs. Transformation of forest vegetation causes a decrease in cover of thermophilous and heliophilous species. On the other hand, species of oak-hornbeam forests as well as anthropophytes are in expansion. Planning of the protection activities in the nature reserve needs to include these dynamic tendencies of the vegetation.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2011, 7; 207-227
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 37.

Tytuł:

Reconstruction of the sedimentary environment of phytogenic deposits in the Tomisławice opencast mine (Konin Region, central Poland)

Autorzy:

Słodkowska, Barbara
Widera, Marek

Powiązania:

https://bibliotekanauki.pl/articles/2201200.pdf

Data publikacji:

2022

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Palynology
lignite seam
plant communities
palaeofloristic reconstruction
Neogene
central Poland

Opis:

Palynological analysis of the Tomisławice opencast mine deposits has allowed reconstruction of the plant communities and investigation of the evolution of sedimentary environments at various stages of lignite-forming marsh development, recorded in the composition of pollen assemblages from deposits of the 1st Mid-Polish lignite seam (MPLS-1). Rich pollen communities from an ~9 m thick section has enabled study of the succession of plant communities and of the evolution of phytogenic sedimentation. The pollen succession indicates that the assemblages in the whole lignite seam represent the VIII Celtipollenites verus pollen Zone. Slight differences in the composition of the communities reflect different stages of basin development, depending more on the variable water dynamics than on climatic oscillations. Lignite of the MPLS-1 developed in a continental regime on alluvial plains. Changes in the succession of plant communities in the Tomisławice section record flooding-drainage cycles caused by groundwater level oscillations. Peat bog accumulation took place in river basins, in which the lack of siliciclastic intercalations within the massive lignite seams points to weak fluvial dynamics. A rise in groundwater level and/or surface water resulted in flooding of the marshes and the formation of an extensive shallow lake basin, as shown by the presence of freshwater algae and pollen of aquatic plants. The section as a whole does not record an increased contribution of thermophilic plant taxa. The flora was generally dominated by warm-temperate and thermophilic species, without the participation of strongly thermophilic vegetation, which indicates that the lignite seam in the Tomis³awice opencast mine was formed in the generally stable conditions of a warm temperate climate.

Źródło:

Geological Quarterly; 2022, 66, 4; art. 66, no. 34
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 38.

Tytuł:

Anthropogenic Causes of Peatland Species Vanishing in the Glinno Ługi Area

Autorzy:

Woziwoda, Beata
Komperda, Agata

Powiązania:

https://bibliotekanauki.pl/articles/764896.pdf

Data publikacji:

2011

Wydawca:

Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego

Tematy:

flora
wetlands
peat bog
human impacts
nature protection
Central Poland

Opis:

The paper presents information about the occurrence and state of preservation of valuable peat-bog species as well as about the threats facing them. The anthropopressure-related changes which occurred in the habitat of the Glinno Ługi peatland and their influence on the flora are presented and discussed.

Źródło:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica; 2011, 7; 139-148
1730-2366
2083-8484

Pojawia się w:

Acta Universitatis Lodziensis. Folia Biologica et Oecologica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 39.

Tytuł:

Late Cretaceous siliceous sponges from the Middle Vistula River Valley (Central Poland) and their palaeoecological significance
Późnokredowe gąbki krzemionkowe z doliny środkowej Wisły (Polska Centralna) i ich znaczenie paleoekologiczne

Autorzy:

Świerczewska-Gładysz, E.

Powiązania:

https://bibliotekanauki.pl/articles/191690.pdf

Data publikacji:

2006

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

sponges
Hexactinosida
Lychniscosida
lithistids
taxonomy
palaeoecology
Upper Cretaceous
Central Poland

Opis:

Siliceous sponges are extremely abundant in the Upper Campanian-Maastrichtian opokas and marls of the Middle Vistula River Valley, situated in the western edge of the Lublin Basin, part of the Cretaceous German-Polish Basin. This is also the only one area in Poland where strata bearing the Late Maastrichtian sponges are exposed. The presented paper is a taxonomic revision of sponges collected from this region. Based both on existing and newly collected material comprising ca. 1750 specimens, 51 species have been described, including 18 belonging to the Hexactinosida, 15 - to the Lychniscosida and 18 - to Demospongiae. Among them, 28 have not been so far described from Poland. One new genus Varioporospongia, assigned to the family Ventriculitidae Smith and two new species Varioporospongia dariae sp. n. and Aphrocallistes calciformis sp. n. have been described. Comparison of sponge fauna from the area of Podilia, Crimea, Chernihov, and Donbas regions, as well as literature data point to the occurrence of species common in the analysed area and to the basins of Eastern and Western Europe. This in turn indicates good connections between particular basins of the European epicontinental sea during the Campanian-Maastrichtian. Analysis of the taxonomic composition of the Middle Vistula assem- blage suggests that the occurring sponge fauna is transitional between the faunas of Eastern and Western Europe, what may be linked with the central location of the Lublin Basin in the European epicontinental sea. The gradual upward decrease of taxonomic diversity of the Hexactinosida and Lychniscosida in the studied succession points to gradual basin shallowing, what is consistent with the global regressive trend by the end of the Cretaceous. The domination of the Hexactinellida over the lithistids in terms of diversity and abundance in the entire section allows us to estimate the maximum depth of the Late Campanian basin as 200-250 m and to constrain the minimum depth during the latest Maastrichtian as about 100 m.

Źródło:

Annales Societatis Geologorum Poloniae; 2006, 76, No 3; 227-296
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 40.

Tytuł:

New insights into the genesis of the “Poznań clays” – upper neogene of Poland

Autorzy:

Maciaszek, Piotr
Chomiak, Lilianna
Urbański, Paweł
Widera, Marek

Powiązania:

https://bibliotekanauki.pl/articles/395989.pdf

Data publikacji:

2020

Wydawca:

Uniwersytet Zielonogórski. Oficyna Wydawnicza

Tematy:

overbank deposits
palaeosols
palaeochannels
anastomosing river
Neogene of central Poland

Opis:

The present study focuses on the upper Neogene deposits, called the “Poznań Clays”, that cover more than 75,000 km2 of Poland. They are situated between the first midPolish lignite seam and the glaciogenic deposits of the Pleistocene age. Lithostratigraphically, the “Poznań Clays” belong to the uppermost portion of the lignite-bearing Grey Clays Member and the whole Wielkopolska Member (Poznań Formation). The examined fine-grained sediments include mud-rich floodplain deposits with palaeosol remnants and large sandy-muddy or muddy palaeochannel bodies. Therefore, taking into account facies analysis, cross-sectional geometry, and the planform of the palaeochannels, it can be stated that the “Poznań Clays” formed in the environment of a late Neogene anastomosing river.

Źródło:

Civil and Environmental Engineering Reports; 2020, 30, 1; 18-32
2080-5187
2450-8594

Pojawia się w:

Civil and Environmental Engineering Reports

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 41.

Tytuł:

Multi-proxy inferred hydroclimatic conditions at Bęczkowice fen (central Poland); the influence of fluvial processes and human activity in the stone age

Autorzy:

Płóciennik, Mateusz
Jakiel, Aleksandra
Forysiak, Jacek
Kittel, Piotr
Płaza, Dominik K.
Okupny, Daniel
Pawłowski, Dominik
Obremska, Milena
Brooks, Stephen J.
Kotrys, Bartosz
Luoto, Tomi P.

Powiązania:

https://bibliotekanauki.pl/articles/2037005.pdf

Data publikacji:

2021-12-23

Wydawca:

Łódzkie Towarzystwo Naukowe

Tematy:

peatland
palaeoecology
climate changes
Late Weichselian
Early Holocene
central Poland

Opis:

Fens have been forming in the river valleys of central Poland since the Bølling and went through a transformation from fully aquatic to semiterrestrial habitats during the Younger Dryas/Holocene transition. This drove plant and invertebrate communities and left a distinct pattern in chemical sediment composition, which is why river valley peatlands are sensitive palaeo-archives of climatic, hydrological and edaphic changes. Here we reconstruct the Late Weichselian history of the Bęczkowice fen in the upper Luciąża River valley using geochemical, pollen, Cladocera and Chironomidae proxies. Pollen-based age estimation indicates that the analysed peat sequence dates from the Bølling to Early Holocene. The layers 190-170 cm and 125-105 cm of the studied core were reworked by fluvial processes. Chironomidae and Cladocera communities indicate mostly limnetic conditions during the Allerød and early Younger Dryas. Peatland pools were supplied mostly by Luciąża River floods, but also by groundwater. Since the onset of the Holocene, the water level has dropped, eliminating aquatic midges and water fleas, and supporting taxa typical of astatic waters and wet soil.

Źródło:

Acta Geographica Lodziensia; 2021, 111; 135-157
0065-1249

Pojawia się w:

Acta Geographica Lodziensia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 42.

Tytuł:

Upper Pleistocene palaeoenvironmental changes at the Zwierzyniec site, Central Poland

Autorzy:

Kalińska-Nartiša, E.
Dzierżek, J.
Bińka, K.
Borkowski, A.
Rydelek, P.
Zawrzykraj, P.

Powiązania:

https://bibliotekanauki.pl/articles/2059945.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

pollen
plant macrofossils
glaciolacustrine
Eemian–Vistulian sequence
palaeoenvironment
Central Poland

Opis:

The paper presents the data on an Eemian–Late Glacial sedimentary sequence from the Zwierzyniec site, central Poland. A number of boreholes document one or two organic layers that occur beneath one or two horizons of clayey and silty deposits of ice-dammed lakes. This study demonstrates to which extent the Zwierzyniec site can contribute to a better understanding of the palaeoenvironmental changes during the Eemian–Vistulian time-frame in central Poland. To study it, a multi-proxy approach was applied, involving: palynological and plant macrofossil analysis, study of rounding of quartz grains and morphology of their surface, and investigations of sand mineralogy and till petrography. The results show that a till bed is overlain by a sandy series corresponding to the glacial-interglacial transition. Either one or two distinct peaks of organic accumulation are evidenced by peat horizons. The lower horizon records spectra with hazel and hornbeam, and did, therefore, accumulate in the Eemian. Observed only in some boreholes, the upper peat horizon marks the Brørup (or the lower part of the Rederstall stadial) represented by forest-steppe conditions with patchy mosaics of larch and further transition into sedges and herbaceous taxa. Localized in between the two peat sequences, the sandy horizon marks a long-lasting aeolian transformation with weathering by frost in the Early Vistulian. Again, significant changes of the palaeoenvironmental regime occurred, and are manifested in the one or two horizons of the glaciolacustrine sediments. This corresponded to the last glaciation in the region, when the ice-dammed lakes formed during the Main Stadial.

Źródło:

Geological Quarterly; 2016, 60, 3; 610--623
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 43.

Tytuł:

Nietoperze odłowione w sieci ornitologiczne w punkcie obrączkowania ptaków w Dolinie Środkowej Wisły
Bats captured in ornithological nets at a bird ringing station in the middle Vistula River Valley

Autorzy:

Lesiński, G.
Grzębkowski, M.
Rapczyński, J.

Powiązania:

https://bibliotekanauki.pl/articles/2090104.pdf

Data publikacji:

2021

Wydawca:

Mazowiecko-Świętokrzyskie Towarzystwo Ornitologiczne

Tematy:

Chiroptera
bat fauna
netting
ornithological nets
riparian habitats
central Poland

Opis:

Data on bats captured in ornithological nets during the bird ringing project were collected at the station located on the Rembeza Island (51.97oN, 21.27oE) in the Vistula river valley close to Czersk village in 2013-2014 and 2019-2021. Bat species, their sex and age were determined based on photos made by ornithologists. In total, 32 individuals of six species were recorded. The most abundant were: Plecotus auritus (13) and Myotis daubentonii (9), i.e., species foraging close to vegetation or over the water surface, and flying on relatively low height. Species common in the area but flying higher Nyctalus noctula was captured rarely. Rare and valuable species – Myotis dasycneme – was also recorded, and the presence of an adult female suggests the occurrence of a breeding colony in the vicinity of the study site.

Źródło:

Kulon; 2021, 26; 65-69
1427-3098

Pojawia się w:

Kulon

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 44.

Tytuł:

Middle Pleistocene fluvial, lacustrine and glaciolacustrine sediments of the Czyżów and Kuców Formations (Kuców 9, 10 and 16 sections), Bełchatów outcrop, central Poland – the problem of stratigraphical interpretation

Autorzy:

Krzyszkowski, Dariusz
Wachecka-Kotkowska, Lucyna
Nita, Małgorzata
Wieczorek, Dariusz

Powiązania:

https://bibliotekanauki.pl/articles/2025048.pdf

Data publikacji:

2021

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

lake deposits
fluvial deposits
oxbow
Mazovian
Ferdynandovian
Kleszczów Graben
central Poland

Opis:

The article presents results of research of three sections (Kuców 9, 10 and 16). Two of them record fluvial and lacustrine interglacial sediments and the third, cold-stage glaciolacustrine sediments. They were formed inside the Miocene – Pliocene syncline depressions in a central part of the southern horst within the Kleszczów Graben. Fluvial and lacustrine deposits of the Middle Pleistocene Interglacial (Mazovian or Ferdynandovian in the Czyżów Formation) are described from the Kuców 9 and 10 sections. Their sediments are located in marginal parts of a buried river valley and within an oxbow palaeolake, then covered by glaciofluvial deposits of the Ławki (Early Saalian) and Rogowiec (Late Saalian) Formations. The Kuców 16 section comprises ice-dam sandy lithofacies (Kuców Formation, Elsterian) of a marginal part in a proglacial lake. Two pollen diagrams of K65/15 and Kuców 9 sections represent the Mazovian (Holsteinian) succession, although in the Kuców 9 section some features are typical for the Ferdinandovian succession.

Źródło:

Studia Quaternaria; 2021, 38, 1; 53-66
1641-5558
2300-0384

Pojawia się w:

Studia Quaternaria

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 45.

Tytuł:

Disturbances of the holocene lake-bog sediment succession as revealed by pollen record from wietrzychowice (south eastern kujawy, central poland)

Autorzy:

Břízová, Eva
Roman, Małgorzata

Powiązania:

https://bibliotekanauki.pl/articles/2025780.pdf

Data publikacji:

2015

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

pollen analysis
geoarchaeology
post-depositional disturbances
human activity
Holocene
central Poland

Opis:

Re sults of geo log i cal and pol len in ves ti ga tions of the lake-bog sed i ments from the sec tion Wietrzychowice W5, located nearby the Neo lithic Fun nel Beaker Cul ture (FBC) mega liths, are pre sented. The pol len data re veal that sed imen ta tion at Wietrzychowice has be gun at the be gin ning of the Ho lo cene (Preboreal). Pol len anal y sis was used to determine stratigraphy with regard to sediment characteristics. The pollen spectrum was divided into 8 LPAZes (1-7Xa, 7Xb) which were also, where pos si ble, stratigraphically clas si fied. Ra dio car bon dat ing of 6 730 ± 90 BP (5 730–5 480 BC, MKL-702) at depth of 1.20 m con firmed the pol len anal y sis age es ti ma tion. Five set tle ment ep i sodes were found in or ganic sed i ments in the up per part of the W5 core. The first was pre sum ably dur ing the Preboreal, the sec ond in the early At lan tic, the third in the late At lan tic (prob a bly Neo lithic FBC), the fourth in the early Mid dle Ages and the last one in the late Mid dle Ages. The pol len anal y sis was use ful to point ir reg u lar i ties in sed i ment suc ces sion. Such a sit u a - tion made palaeoenvironmental in ter pre ta tion dif fi cult, but fur ther re search is still needed to en able an ac cu rate re construc tion.

Źródło:

Studia Quaternaria; 2015, 32; 91-97
1641-5558
2300-0384

Pojawia się w:

Studia Quaternaria

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 46.

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

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Skocz do pozycji: 47.

Tytuł:

Preliminary results of geodetic measurements in the Inowrocław salt dome area, central Poland

Autorzy:

Szczerbowski, Z.

Powiązania:

https://bibliotekanauki.pl/articles/191587.pdf

Data publikacji:

2004

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

geodynamics
salt geology
levelling
subsidence
mining
Inowrocław salt dome
Central Poland

Opis:

The results of geodetic measurements conducted in the Inowrocław salt dome area are presented in this paper. The main aim of these studies was to determine changes in the rock mass exerted by geological processes. These processes have led to the changes in the salt dome geometry and physical properties of surrounding rocks. Degradation of the salt-gypsum cap of the dome strongly depends on the hydrogeological conditions and, particularly, on tectonic structure which has had a bearing on the uplift of the ground surface. The principal goal of the paper is to present the results of geodetic levelling surveys in the Inowrocław area wherein the mining activity was terminated in 1991. These results point to a progressive salt uplift in some areas, showing a constant rate throughout the study period.

Źródło:

Annales Societatis Geologorum Poloniae; 2004, 74, No 3; 319-324
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 48.

Tytuł:

The morphology of fossil pebbles as a tool for determining their transport processes (Koźmin South lignite open-cast pit, central Poland)

Autorzy:

Widera, M.

Powiązania:

https://bibliotekanauki.pl/articles/191884.pdf

Data publikacji:

2010

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

pebble morphology
shape
surface texture
sediment provenance
transport processes
Central Poland

Opis:

The Koźmin South lignite open-cast pit is the southernmost exposure of Palaeogene (lower Oligocene) deposits in central Poland. This study is focused on Palaeogene pebbles of the so-called Koźmin Gravels, rede- posited in the Neogene sands. These pebbles are not known from the adjacent territory of central Poland and they vary in petrographic composition, shape and surface texture. The classification of the pebble-size particle form is determined as DI/DL (elongation ratio) and DS/DI (flatness ratio). A great number of pebbles are disc-shaped (oblate-shaped) and blade-shaped or they can be classified as platy, bladed and very bladed pebbles. The oblate-prolate index (OP) is less than -2 for 45% of the particles (typical of beach pebbles), the mean sphericity (yp) is 0.56 (typical of beach pebbles), and the mean roundness (RWt) is 0.73 (typical of beach pebbles). The data obtained from SEM analysis of quartz pebble surface micromorphology are characteristic of high mechanical energy of the littoral environment. The surface of some pebbles is excellently polished with v-shaped indentations and grooves. The average composition of the heavy mineral fraction occurring with these pebbles is marked by the predominance of zircon (exceeding 70%). All the above-mentioned data, in the light of extensive literature, indicate that more morphological features of the analysed pebbles have been inherited from the littoral/beach environment. Moreover, a detailed petrographic study was very useful for determining the prove-nance of these pebbles. The most characteristic rocks are greyish-blue quartzes. They are known only from the Sudetes Mts., situated on the NE slope of the Bohemian Massif. Thus, the rock fragments were transported at least 300 km by rivers from the Sudetes to the littoral/beach zone of the Palaeogene sea. Then, the residually-marine beach pebbles were redeposited into the Neogene debris flow and/or fluvial deposits. The present-day area of the Koźmin South lignite open-cast pit was tectonically active at that time.

Źródło:

Annales Societatis Geologorum Poloniae; 2010, 80, No 3; 315-325
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 49.

Tytuł:

Relations between present relief on the border of lowlands and highlands and geological structures of the Paleozoic Platform – a case study from central Poland

Autorzy:

Szmidt, Aleksander
Wachecka-Kotkowska, Lucyna

Powiązania:

https://bibliotekanauki.pl/articles/184142.pdf

Data publikacji:

2019

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH

Tematy:

Paleozoic Platform
sub-Quaternary surface
relief inheritance
contemporary relief
Central Poland

Opis:

The article is an attempt to find relations between geology and the dynamics of the Mesozoic surface of the Łódź Synclinorium, the Radomsko Elevation and the Bełchatów Graben and the present relief on the border of the Polish Lowlands and Uplands in its central part. Fossil relief has been compared with the present one as related to the extent of the recession phases of the Saalian (Wartanian) ice-sheet. A significant convergence has been found between the Mesozoic surface plain and the main morphologic elements. The role of elevations and fossil valleys has been stressed as stable forms in the pre-Pleistocene and contemporary landscape. Also stressed has been the meaning of grabens and elevations enforcing longer stoppages of the Wartanian stadial of the Middle Polish Glaciations.

Źródło:

Geology, Geophysics and Environment; 2019, 45, 1; 57-70
2299-8004
2353-0790

Pojawia się w:

Geology, Geophysics and Environment

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 50.

Tytuł:

Contribution to the knowledge of the fauna of Kampinos National Park: Ptiliidae (Coleoptera: Staphylinoidea)

Autorzy:

Marczak, Dawid
Karol Komosiński, Karol
Masiarz, Jakub

Powiązania:

https://bibliotekanauki.pl/articles/1179152.pdf

Data publikacji:

2017

Wydawca:

Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN

Tematy:

Central Poland
Kampinos National Park
Masovian Lowland
Ptiliidae
faunistics
new records

Opis:

The paper provides new data on 30 species of Ptiliidae (Coleoptera: Staphylinoidea). Among them 19 species are new for the studied area. The occurrence of 9 species previously mentioned in literature was confirmed. Two species known from literature (Millidium minutissimum, Ptenidium pusillum) was not confirmed, but its presence within this area is beyond doubt. Thirteen species: Acrotrichis pumila. A. silvatica, Nephanes titan, Smicrus filicornis, Ptenidium formicetorum, P. gressneri, P. intermedium, P. nitidum, Ptiliola kunzei, Ptiliolum fuscum, P. limbatum, Ptinella limbata and P. tenella has been recorded from the Mazovian Lowland for the first time. One species - Nephanes titan (NEWMAN, 1834) figure in the “Red List of Threatened Animals in Poland” in the category EN (endangered).

Źródło:

World Scientific News; 2017, 83; 1-14
2392-2192

Pojawia się w:

World Scientific News

Dostawca treści:

Biblioteka Nauki

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