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    Tytuł:
    Późnoplejstoceński rozwój doliny Niemna w rejonie Grodna na Białorusi
    Late Pleistocene evolution of the Niemen River valley near Grodno in Belarus. Prz. Geol.
    Autorzy:
    Lindner, L.
    Sańko, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074560.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Białoruś
    dolina rzeki Niemen
    zlodowacenie poozierskie
    Belarus
    Niemen River valley
    Poozerian Glaciation
    river terraces
    Opis:
    Based on geological and paleobotanic data, the oldest valley system of the Niemen River is linked in the study area with a river located southward of Grodno, within a parallel valley from the Alexandrian (Mazovian) Interglacial. The foundations of the present-day, almost meridian course of the Niemen River valley, are connected with a system of post-glacial lakes from the Sozhian (Wartanian) Stadial of the Pripethian (Odranian) Glaciation, later filled with organic deposits of the Muravian (Eemian) Interglacial. Analysis of six sites with these deposits (Pyszki, Rumlówka, Poniemuń, Żukiewicze, Bohatyrowicze and Kniażewodce) indicates that they represent three lakes located at different altitudes. During the maximal range of the Dvinian (Main) Stadial of the Poozerian (Vistulian) Glaciation, the lakes were beyond the range of the ice-sheet. At this time, the highest located deposits of the Poniemuń-Żukiewicze lake were covered by sander sediments, whereas the Bohatyrowicze-Kniażewodce and Pyszki-Rumlówka lakes that were located at lower levels, were covered by fluvio-periglacial deposits and varved clays of the Skidel ice-dammed lake. Retreat of the ice-sheet of the Dvinian Stadial, resulting in outflow of water from the Skidel ice-dammed lake through the area with the two lower interglacial lakes, triggered the formation of a system of the Niemen River supra-flood terraces above them. Accumulation of the highest of these terraces (VI), during the first phase of the Skidel lake outflow, marks the beginning of the present-day Niemen River valley formation that probably began in the younger phases of the Dvinian ice-sheet retreat. Further evolution of the valley is linked with the Late Glacial formation of the middle (III-V) supra-flood terraces and with the Holocene formation of the lower (II, I) supra-flood terraces.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 1; 73-80
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Stanowisko osadów jeziornych interglacjału murawińskiego (eemskiego) w Rumlówce koło Grodna (Białoruś)
    A locality with lacustrine deposits representing the Muravian (Eemian) Interglacial in Rumlówka near Grodno (Belarus)
    Autorzy:
    Marciniak, B.
    Jełowiczewa, J.
    Lindner, L.
    Sańko, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2063179.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    zlodowacenie poozierskie (wisły)
    pollen
    diatom and faunal studies
    Muravian (Eemian) Interglacial
    Poozerian (Vistulian) Glaciation
    palinologia
    okrzemki
    fauna
    interglacjał murawiński (eemski)
    Opis:
    Przedstawiono główne wyniki badań interdyscyplinarnych osadów jeziornych w Rumlówce koło Grodna. Osady te reprezentowane są przez kredę i mułki ilaste, a przykryte są przez piaski i piaski ze żwirem stanowiące osady fluwioperyglacjalne i deluwialne najwyższego (VI) tarasu Niemna. Badaniami palinologicznymi objęto górną część kredy i mułku ilastego w profilu Rumlówka 2. Obejmują one młodszą część (od fazy Carpinus do fazy Betula+Pinus+NAP) interglacjału murawińskiego (eemskiego) i najstarszą część zlodowacenia poozierskiego (wisły). Badania diatomologiczne młodszej części osadów interglacjału murawińskiego pozwoliły na wydzielenie w nich pięciu lokalnych poziomów okrzemkowych (Local Assemblage Zones L DAZ DR-1 do DR-5), a na ich podstawie pięciu stadiów rozwoju ówczesnego jeziora, od głębokiego, oligotroficznego przez oligomezotroficzne, z często zmieniającym się poziomem wody, do eutroficznego, wyraźnie się wypłycającego. Analiza licznych szczątków malakofauny oraz zębów i kości ssaków, zachowanych zarówno w wymienionych osadach jeziornych, jak i przykrywających je osadach rzecznych, wykazała wzajemne przenikanie się form ciepło- i zimnolubnych. Jest to zjawisko typowe dla schyłkowej części ostatniego interglacjału (murawińskiego, eemskiego) i początkowej części ostatniego zlodowacenia (poozierskiego, wisły) na obszarze środkowej Europy.
    The paper presents results of multi-disciplinary studies of the lacustrine deposits from Rumlówka near Grodno. Geological studies show that the strata are represented by marls and clayey silts and are covered by sands and sands with gravel representing of the fluvioperiglacial and deluvial accumulation of the highest (VI) terrace of Niemen. Pollen analyses were conducted in the upper part of the marls and clayey silts in the Rumlówka 2 section. These deposits correspond to the younger part (from the Carpinus to the Betula+Pinus+NAP phase) of the Muravian (Eemian) Interglacial and the oldest part of the Poozerian (Vistulian) Glaciation. Diatom analyses of the younger part of the Muravian Interglacial allowed distinguishing five Local Assemblage Zones L DAZ DR-1 to DR-5, and as a result, also five stages of the lake evolution, from deep basin (oligotrophic lake), through a reservoir with oscillating water level (oligo-mesotrophic lake), to a distinctly shallowing environment (eutrophic lake). The analysis of abundant malacofauna along with teeth and bones of mammals preserved both in the lake deposits as well as in the overlying fluvial deposits indicated intermingling of thermo- and cryophilous forms. This phenomenon is typical of the terminal part of the last interglacial (Muravian, Eemian) and the initial part of the last slaciation (Poozerian, Vistulian) in Central Europe.
    Źródło:
    Biuletyn Państwowego Instytutu Geologicznego; 2007, 425; 75-86
    0867-6143
    Pojawia się w:
    Biuletyn Państwowego Instytutu Geologicznego
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Palaeoenvironmental and climatic changes during the early pleistocene recorded in the lacustrine-boggy-fluvial sediments at Komorniki, NE Poland
    Autorzy:
    Khursevich, G.
    Nita, M.
    Ber, A.
    Sanko, A.
    Fedenya, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/1186080.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    lithology
    pollen analysis
    diatoms
    malacofauna
    palaeoenvironment
    Lower Pleistocene
    NE Poland
    Opis:
    The lacustrine-boggy-fluvial sequence at Komorniki, NE Poland was subject to complex (geological, palynological, diatomological and malacological) investigations. These sediments occur between the Narevian and Nidanian glaciations tills and belong to the Augustovian Interglacial of Poland correlated with the Cromerian 1 Interglacial of the Netherlands. Two cold stages of a glacial rank and one warm stage of interglacial rank (with dominant pollen of Quercus, Ulmus, Carpinus, Alnus, Tilia and Corylus in sediments corresponding to the climatic optimum) have been distinguished in the pollen succession. The latter is similar to that known from the Augustovian Interglacial profiles at Szczebra, Kalejty and Czarnucha. Diatom succession from the Komorniki section includes certain unidentified, apparently new small species of Stephanodiscus, Staurosirella and Pseudostaurosira side be side with the Pleistocene extinct taxon of Stephanodiscus niagarae var. insuetus and a relatively widespread species of S. rotula characterizing by some morphological peculiarities. In the composition of the malacofauna the fluvial extinct species of Fagotia wuesti and Sphaerium cf. rivicola are the most important molluscs for the biostratigraphy. Among them, Sphaerium cf. rivicola is known from the late Tiglian in the Netherlands. Fagotia wuesti is characteristic of the Bavel Interglacial in the Netherlands, as well as of the Borntal and Artern interglacials in Germany.
    Źródło:
    Polish Geological Institute Special Papers; 2005, 16; 35--44
    1507-9791
    Pojawia się w:
    Polish Geological Institute Special Papers
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The age of the oldest Scandinavian glaciations in mid-eastern Poland and southwestern Belarus
    Autorzy:
    Lindner, L.
    Marciniak, B.
    Sanko, A. F.
    Khursevich, G. K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059317.pdf
    Data publikacji:
    2001
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Polska
    Belarus
    Early Pleistocene
    Scandinavian glaciations
    stratigraphic correlation
    Opis:
    Analysis of type localities of Pleistocene deposits from mid-eastern Poland (Kozi Grzbiet, Łuków, Biała Podlaska and Wilczyn) and southwestern Belarus (Smolarka and Postolovo) has provided a new view on the age, limits and correlation of the oldest Scandinavian glaciations in the area. Integration of palaeontological data with determination of the Brunhes/Matuyama boundary (780 ka) at Kozi Grzbiet and Smolarka suggests that the first glaciation (Narevian) preceded this boundary and had a slightly smaller extent in SW Belarus than hitherto considered. The second glaciation (Nidanian) occurred slightly above or at this palaeomagnetic boundary. In Poland it is the first South Polish Glaciation, a till of which can be traced as far as the Holy Cross Mts. In SW Belarus it is represented by a till to the south of Brest and Bereza, and connected there with the oldest glaciation.
    Źródło:
    Geological Quarterly; 2001, 45, 4; 373-396
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    From Individual Heroes to National Performers: The Shift in Taekwondos Peace Promotion Activities
    Autorzy:
    Johnson, John A.
    Lewis, Sanko
    Powiązania:
    https://bibliotekanauki.pl/articles/1922298.pdf
    Data publikacji:
    2020-11-04
    Wydawca:
    PPHU Projack Jacek Wąsik
    Tematy:
    sports diplomacy
    cultural exchange
    karate
    Republic of Korea (ROK)
    People’s Democratic Republic of Korea (DPRK)
    Opis:
    The writings of early taekwondo pioneers promote peace through the practice of the martial art and, later, the combat sport. These pioneers charged taekwondo practitioners with a duty to contribute to justice, defend the weak, and build a more peaceful world. National and international taekwondo organizations such as the Kukkiwon, World Taekwondo (WT), and the International Taekwon-Do Federation (ITF) have taken up the charge of peace promotion through taekwondo by means of transnational events, such as goodwill tours and joint taekwondo demonstrations by adversarial states (e.g., South and North Korea). These activities are soft diplomacy initiatives and have seen some level of success. While these soft diplomacy activities are in line with the goal of peace promotion that the early pioneers advocated, they are qualitatively different from what the pioneers advocated. Originally, the responsibility of peace promotion was on the individual taekwondo practitioner, who ought to cultivate moral character, courage, and martial art skill in order to uphold justice and defend the weak. With the current use of taekwondo for soft diplomacy, the responsibility of peace promotion has shifted from the individual practitioner to the governing bodies, such as WT and the ITF. Instead of focusing on issues surrounding justice and the protection of the weak, these national and international organizations focus on geopolitical cooperation, which is mediated through cultural exchange activities in the form of taekwondo demonstrations. These events involve activities such as acrobatic performances, dance routines, and board breaking that require little combat skill and may not pose the risk of serious injury to the individual practitioners, mainstays of the individual heroes of old. The charge to safeguard justice and physically defend the weak, which are acts of true courage as was envisioned by the taekwondo pioneers, is mostly ignored.
    Źródło:
    Physical Activity Review; 2020, 2, 8; 64-71
    2300-5076
    Pojawia się w:
    Physical Activity Review
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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