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    Wyświetlanie 1-12 z 12
    Tytuł:
    Older and Younger Holsteinian climate oscillations in the palaeobotanical record of the Brus profile (SE Poland)
    Autorzy:
    Hrynowiecka, A.
    Pidek, I. A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060592.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    pollen analysis
    macrofossil remains analysis
    Mazovian Interglacial
    Holsteinian Interglacial
    palaeoecological reconstruction
    climate reconstruction
    Eastern Poland
    Opis:
    A pollen sequence of Holsteinian/Mazovian age known since the 1980s in Brus (Western Polesie) is the second site with a plant macrofossil record in eastern Poland. High sedimentation rates in a palaeolake that functioned in this area have allowed a detailed climate reconstruction that enabled to trace the Older and Younger Holsteinian oscillations and to outline the water-level changes in the water body. Climate reconstructions, based on full palaeobotanical analyses (pollen and macroremains), were compared with those from Nowiny Żukowskie (Lublin Upland), revealing regional climatic patterns. The two Holsteinian climate oscillations were correlated with those detected in the Dethlingen section of Germany (Koutsodendris et al., 2010), providing more information on the spatial scale of these events.
    Źródło:
    Geological Quarterly; 2017, 61, 4; 723--737
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Nowe stanowiska interglacjalne w rejonie dolin Wilgi i Okrzejki na Wysoczyźnie Żelechowskiej (Polska południowo-wschodnia)
    New interglacial sites in the region of the Wilga and Okrzejka river valleys at the Żelechów Upland (SE Poland)
    Autorzy:
    Żarski, M.
    Nita, M.
    Winter, H.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074384.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    interglacjał mazowiecki
    interglacjał eemski
    stratygrafia
    palinostratygrafia
    Wysoczyzna Żelechowska
    Mazovian Interglacial
    Eemian Interglacial
    stratigraphy
    palynostratigraphy
    Żelechów Plateau
    Opis:
    Lake sediments of the Mazovian Interglacial were found in boreholes Kasyldów and Wola Okrzejska 48, and deposits of the Eemian Interglacial were discovered in Wola Okrzejska 49 and Szczepaniec bore-holes. The pollen succession recorded in the lacustrine sediments in the pro-files Kasyldów and Wola Okrzejska 48 is characteristic for the Mazovian Interglacial, and those from the profiles Wola Okrzejska 49 and Szczepaniec typical for the Eemian Interglacial. The biogenic sediments in the Kasyldów and Wola Okrzejska (48) were accumulated in lakes, formed after meltdown of the Sanian 2 (Wilgian) ice-sheet. These sites are located within the Mazovian Lakeland, in the south-east of the Żelechów Upland. The glacial horizon of the Sanian 2 (Wilgian) Glaciation occurs under Mazovian sediments. The fluvioglacial deposits of the Wartanian Glaciation cover the lacustrine sediments. The Eemian sites at Wola Okrzejska 49 and Szczepaniec are located in the Okrzejka River valley, which was formed after the Wartanian Glaciation. The silts of the Wartanian Glaciation occur below Eemian deposits. The sands of the Vistulian Glaciation and peats of the Holocene cover the lacustine deposits of the Eemian Interglacial. These sites are important for stratigraphy of sediments, which fill the Okrzejka, Wilga and Mała Bystrzyca valleys.
    Źródło:
    Przegląd Geologiczny; 2005, 53, 2; 137--144
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Kilka uwag o interglacjale mazowieckim we wschodniej Polsce
    Some remarks on the Mazovian Interglacial in Eastern Poland
    Autorzy:
    Winter, H.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074575.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    palinologia
    Parrotia
    skrzydłorzech
    interglacjał mazowiecki
    wschodnia Polska
    palynology
    Pterocarya
    Mazovian Interglacial
    eastern Poland
    Opis:
    Eastern Poland is a region, where a lot of sites with detailed palynological records of the Mazovian (Holsteinian) Interglacial are located. The pollen succession of this interglacial in Eastern Poland has specific features: high proportions of Pterocarya pollen, the occurrence of Parrotia pollen and a distinct share of pollen of other exotic taxa, among others: Juglans, Ilex, Celtis, Buxus and Vitis. Palynological studies reveal variability proportions of Taxus in the Ma IV Taxus-Picea-Alnus zone. The presence of intra-interglacial cooling is distinct in sediments of this age.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 3; 225-231
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Nowe stanowisko interglacjału mazowieckiego w Gajcu - Pojezierze Łagowskie [zachodnia Polska]
    New Mazovian Interglacial site at Gajec - Łagowskie Lakeland [western Poland]
    Autorzy:
    Winter, H.
    Urbański, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074544.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    analiza pyłkowa
    interglacjał mazowiecki
    litostratygrafia
    Pojezierze Łagowskie
    pollen analysis
    Mazovian Interglacial
    litostratigraphy
    Łagowskie Lakeland
    Opis:
    Gajec [Rze-1] borehole was drilled for needs of detailed geological mapping of Poland at the scale 1 : 50 000 (sheet Rzepin ). A deep tunnel valley was recognized in this borehole. It was eroded to 120 m below a see level in the Lower Miocene sediments. The tunnel was filled with 85 m thick series of sands, mud and dusty till deposited during the San Glaciation [the Elsterian Glaciation]. The sediments from the depth interval of 67,9 m - 57,1 m have been examined by palinological analysis. The data obtained indicate that the pollen succession from the Gajec section has features characteristic of the Mazovian [Holsteinian] pollen succession. These features are the high proportion of coniferous trees [Pinus, Picea, Taxus, Abies], and the association of Alnus with Picea and Carpinus with Abies, Quercus and Corylus as well the most abundant thermophilous elements. Warmth-demanding taxa are represented by pollen of Pterocarya, Celtis, Juglans, Buxus, Ilex aquifolium and Vitis.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 4; 330-335
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Environmental changes of the Mazovian (Holsteinian /~MIS 11) palaeolake near Szymanowo (eastern Poland) in the light of malacological analysis
    Autorzy:
    Szymanek, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/138661.pdf
    Data publikacji:
    2014
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    molluscs
    Palaeolakes
    Mazovian (Holsteinian) Interglacial
    palaeoecology
    mięczaki
    paleojeziora
    interglacjał mazowiecki
    paleoekologia
    Opis:
    The malacofauna of the palaeolake deposits at Szymanowo (eastern Poland) was investigated. It represents the younger part of the climatic optimum of the Mazovian (Holsteinian) Interglacial (~MIS 11) and possibly the postoptimal period. The mollusc assemblage is composed of both standing and running water species, mostly connected with temperate climate. The presence of biostratigraphical indicators of the Mazovian, Viviparus diluvianus (Kunth, 1865), Lithoglyphus jahni Urbański, 1975 and Pisidium clessini Neumayr, 1875, is noteworthy. Variability in the structure and composition of the assemblage enables palaeoecological reconstruction. Changes in the water-level, vegetation and energy conditions are inferred from the malacological succession. Three stages of the lake development were distinguished. The first one is connected with deeper conditions and predominance of V. diluvianus and L. jahni. The second one, dominated by Bithynia tentaculata (Linnaeus, 1758), records a fall of the water-level and the growth of aquatic plants, evidenced by high frequencies of Valvata cristata Müller, 1774 and Acroloxus lacustris (Linnaeus, 1758). The third stage corresponds to another rise of the water-level and an increase in V. diluvianus, L. jahni, Valvata piscinalis Müller, 1774 and Pisidium henslowanum (Sheppard, 1823), which evidence some higher energy conditions.
    Źródło:
    Acta Geologica Polonica; 2014, 64, 2; 249-260
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The rank of climatic oscillations during MIS 11c (OHO and YHO) and post-interglacial cooling during MIS 11b and MIS 11a in eastern Poland
    Autorzy:
    Hrynowiecka, Anna
    Żarski, Marcin
    Drzewicki, Wojciech
    Powiązania:
    https://bibliotekanauki.pl/articles/2058672.pdf
    Data publikacji:
    2019
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    substages of MIS 11
    Mazovian interglacial
    Holsteinian Interglacial
    MIS 12 and MIS 10 glaciation range
    palaeoclimate changes
    E Poland palaeolakeland
    Carbon isotope
    Opis:
    Lacustrine sediments representing Marine Isotope Stage 11 (MIS 11) were found in Hermanów (SE Poland) in a present-day closed depression under a thin cover of Weichselian and Holocene deposits (1.4 m). These sediments filled a palaeolake created as a result of melting of a dead-ice block at the end of MIS 12. Geological research has excluded the presence of an ice sheet during MIS 12 in this area. The lobe of the ice sheet of this glaciation was located several kilometres to the west of Hermanów. The palaeolake was part of a larger palaeolakeland in southeastern Poland, formed during MIS 11. The palaeomorphology of this interglacial is evident in the contemporary relief of the area and the outline of the lakes corresponds to the pattern of the closed palaeodepressions. Based on the record of sediments from Hermanów, a new perspective regarding the sub-division of MIS 11 is presented. Two regressive phases are observed in the Holsteinian Interglacial (MIS 11c) - OHO and YHO. The subsequent substages with five cold fluctuations according to the newest stratigraphic standards should be assigned to MIS 11b with a very clear cooling and a slightly warmer MIS 11a. Carbon isotopic composition of organic matter corroborates geological and environmental analysis. The isotopic composition suggests two cooling periods: OHO and MIS 11b. Stable climatic conditions with little temperature fluctuations persisted between the cooling periods.
    Źródło:
    Geological Quarterly; 2019, 63, 2; 375--394
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Palinologiczne i diatomologiczne badania osadów interglacjału mazowieckiego z odsłonięcia w kopalni Bełchatów
    Pollen and diatom analysis of the Mazovian Interglacial deposits from the open-cast mine “Bełchatów” (Central Poland)
    Autorzy:
    Balwierz, Z.
    Goździk, J.
    Marciniak, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074419.pdf
    Data publikacji:
    2006
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    plejstocen
    analiza palinologiczna
    analiza diatomologiczna
    intergracjał mazowiecki
    pollen stratigraphy
    diatom stratigraphy
    palynology
    Mazovian Interglacial
    Middle Pleistocene
    Central Poland
    Opis:
    The thickness of Pleistocene deposits in the Kleszczów Graben reach 300 m. Data from these deposits are important for stratigraphic schemes of the Pleistocene of Poland. However, up to now the Mazovian Interglacial deposits were recognized from boreholes only, not from the exposures in the open-cast mine and they comprise incomplete interglacial successions. The present analysis of organic deposits from closed depression exposed on the escarpment of the mine,reveals almost the full pollen succession of the Mazovian Interglacial. The succession started with dominance of birch forest followed by birch-pine and afterwards birch-pine forest with increasing share of alder, spruce and thermophilous trees that led to development of mixed forest which corresponded to climatic interglacial optimum. First there were forests with share of yew which later were replaced by hornbeam and fir. The fir-hornbeam phase closed the climatic optimum. The distinctly colder pine phase following fir-hornbeam phase ended the interglacial succesion of plants in Folwark 93K site. On the basis of changes in diatom composition and relative (percentage) diatom frequency in this site it was determined that the fossil lake sediments represent the diatom succession of the Mazovian Interglacial. The diatom succession from Folwark has been divided into 7 local diatom assemblage zones (LDAZ Fd 1–Fd7). These zones represent four stages of paleolake development and correspond to the local and regional pollen assemblage zones of the Mazovian Interglacial. The Mazovian Interglacial age of the organic deposits from the site Folwark 93K implies the revision of the stratigraphical position of some lithostratigraphic units from the Middle Pleistocene in the Kleszczów Graben. The obtained results indicate also that at least some intensive deformations of the Lower Pleistocene deposits were completed before the Mazovian Interglacial.
    Źródło:
    Przegląd Geologiczny; 2006, 54, 1; 61-67
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Analiza pyłkowa osadów interglacjału mazowieckiego w Malicach (Wyżyna Woźnicko-Wieluńska)
    Pollen analysis of Mazovian deposits in Malice (Woźniki-Wieluń Upland)
    Autorzy:
    Nita, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074579.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    analiza pyłkowa
    kolejność pyłkowa
    interglacjał mazowiecki
    Wyżyna Woźnicko-Wieluńska
    pollen analysis
    pollen succession
    Mazovian Interglacial
    Woźniki-Wieluń Upland
    Opis:
    The paper shows results of pollen analysis of organic sediments from the site Malice (M1). The diagram includes 11 local pollen zones representing Mazovian Interglacial. Forest landscape in the vicinity of the site has changed together with the climate amelioration. In the beginning of the interglacial, birch and pine forests predominated in this area. Later, they were replaced by alder, spruce and yew communities, and next by multispecies deciduous forests and fir woods. Warm and humid climate of this interglacial is indicated for instance by high percentage of Taxus pollen (49%). According to Janczyk-Kopikowa, 1991 at the beginning of the pollen period III the pollen curves show that an intrainterglacial climate cooling might have taken place what has also been recorded in many pollen diagrams of this interglacial in Poland. Pollen succession from Malice, apart from features characteristic for the succession of Mazovian Interglacial, also shows many local features caused by differentiation of habitats, and various hydrological and microclimatic conditions. Similar features are also revealed from the succession at the site Konieczki located nearby. Despite the fact that the influence of oceanic climate in Mazovian Interglacial reached farther eastwards than it is now, the forest landscape of Poland was also regionally differentiated, although not as distinctly as it is today.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 12; 1061-1066
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Wyniki analizy pyłkowej osadów organicznych z Katowic-lokalna i regionalna stratygrafia pyłkowa (interglacjał mazowiecki)
    Results of pollen analysis of organic sediments from Katowice - local and regional pollen stratigraphy (Mazovian Interglacial)
    Autorzy:
    Nita, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074777.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    analiza pyłkowa
    sukcesja pyłkowa
    interglacjał mazowiecki
    regionalnaj strefa zbioru pyłku
    pollen analysis
    pollen succession
    Mazovian Interglacial
    regional pollen assemblage zone
    Opis:
    The paper presents results of pollen analysis of organic sediments from the site Katowice 2. Six local pollen assemblage zones identified in the section represent the youngest part of Mazovian Interglacial. The pollen spectra of the basal part of the section display some changes indicative of intra-interglacial cooling, well recorded in many profiles of this interglacial in Poland. The forest landscape was subsequently dominated by hornbeam-fir communities which were replaced later by those of pine forests. In turn, taxa of thermophilous aquatic plants, represented by pollen Trapa and microsporangia Azolla filiculoides and Salvinia evidence of lacustrine environment. The results of pollen analysis of sediments from the Katowice site and those hitherto obtained from some other localities in western and central part of the Polish Uplands (Malice, Raków, Wielki Bór, Konieczki i Białe Ługi) became the basis for distinguishing seven regional pollen zones for this area. As compared to pollen succession from Podlasie and eastern Poland, the most significant differences concern the course of pollen curves of Carpinus and Abies and the sequence of their pollen culmination.
    Źródło:
    Przegląd Geologiczny; 2010, 58, 6; 516-521
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Comparison of diatom successions from Mazovian (Poland) and Alexandrian (Belarus) lacustrine interglacial deposits
    Autorzy:
    Marciniak, B.
    Khursevich, G. K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059912.pdf
    Data publikacji:
    2002
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Polska
    Belarus
    Mazovian/Alexandrian (Likhvinian, Holsteinian) Interglacial
    diatoms
    succession
    lake development.
    Opis:
    Comparative analysis of two profiles (Gvoznitsa, Malorita district, southwestern Belarus and Krępiec, Lublin Upland, eastern Poland) of Alexandrian and/or Mazovian (=Likhvinian, Holsteinian) age shows different diatom successions which are correlated with pollen data. Various species of Cyclotella, Stephanodiscus and Aulacoseira predominate at Gvoznitsa, while the diatom flora at Krępiec is more diverse and includes also Synedra, Asterionella, and Fragilaria taxa. Certain apparently extinct taxa of Cyclotella (C. comta var. lichvinensis (Jousé) Loginova, C. comta var. pliocaenica Krasske, C. temperiana (Loginova) Loginova, C. michiganiana var. parvula Loginova (C. parvula Loginova), are typical of the Mazovian and/or Alexandrian Interglacial.
    Źródło:
    Geological Quarterly; 2002, 46, 1; 59-68
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Malacofauna of the Masovian interglacial from the locality Hrud II near Biala Podlaska
    Autorzy:
    Szymanek, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/83408.pdf
    Data publikacji:
    2012
    Wydawca:
    Uniwersytet Mikołaja Kopernika. Wydział Biologii i Ochrony Środowiska. Stowarzyszenie Malakologów Polskich
    Tematy:
    malacofauna
    interglacial
    locality
    Biala Podlaska town
    Mazovia region
    Mazovian interglacial
    Hrud village
    Valvata piscinalis
    Viviparus diluvianus
    Lithoglyphus jahni
    Armiger crista f.nautilus
    Acroloxus lacustris
    Pisidium lilljeborgii
    Pisidium amnicum
    Pisidium nitidum
    Unio pictorum
    water body
    Źródło:
    Folia Malacologica; 2012, 20, 1
    1506-7629
    Pojawia się w:
    Folia Malacologica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    How to resolve Pleistocene stratigraphic problems by different methods? A case study from eastern Poland
    Autorzy:
    Terpiłowski, S.
    Zieliński, T.
    Kusiak, J.
    Pidek, I.A.
    Czubla, P.
    Hrynowiecka, A.
    Godlewska, A.
    Zieliński, P.
    Małek, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059725.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    chronostratigraphy
    geochronology
    interglacial meandering river
    Pleistocene
    Mazovian/Holsteinian
    Eastern Poland
    Opis:
    Different methods have been used to determine the stratigraphic position of Pleistocene alluvial deposits, particularly fluvial interglacial deposits. Near-surface deposits of a meandering river, developed in point-bar and oxbow lake facies, in the Samica River valley (near Łuków, eastern Poland) have been investigated. The fossil valley is incised into the till plain and the outwash. The fluvial succession is locally overlain by solifluction deposits. All the deposits underwent sedimentological analysis. The petrographic composition of basal till occurring in the vicinity of a fossil valley was determined with the method of indicator erratics. Fluvial deposits were examined by pollen analysis and plant macrofossil analysis of oxbow lake facies. Absolute dating methods were applied to the deposits (thermoluminescence methods: TL and additionally IRSL). Lithological differences between fluvial and the surrounding glaciofluvial deposits were identified and their lithostratigraphic position assigned. Petrographic analysis of till and palaeobotanical analyses of oxbow lake facies gave compatible results. Fluvial deposits were formed after the Sanian 2/Elsterian Glaciation, during the Mazovian/Holsteinian Interglacial. Luminescence dating of the fluvial deposits by the TLMAX method yielded the most relevant results (412-445 ka), which indicate that these deposits were formed during the end of the MIS 12 and beginning of the MIS 11 stage.
    Źródło:
    Geological Quarterly; 2014, 58, 2; 235--250
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-12 z 12

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