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Charakterystyka geochemiczna poziomów z fauną słodkowodną formacji z Lublina z Lubelskiego Zagłębia Węglowego

Krzeszowska E., Kokowska-Pawłowska M.

Gospodarka Surowcami Mineralnymi

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2017

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T. 33, z. 1

151--162

PL

Formacja z Lublina zaliczana do górnego westfalu A i westfalu B stanowi główną formację węglonośną Lubelskiego Zagłębia Węglowego (LZW). Osady westfalu B należą do serii limnicznej, w obrębie której występują nieregularnie wykształcone poziomy z fauną słodkowodną. W artykule przedstawiono charakterystykę poziomów zawierających szczątki fauny słodkowodnej z otworów wiertniczych: Borowo, Syczyn 7, Kulik, Kopina 1 (LZW). Poziomy te budują iłowce z wkładkami lub konkrecjami syderytu ilastego. Dla analizowanych poziomów oznaczono zawartości pierwiastków śladowych: U, Th, V, Cr, Rb, K (ICP-MS) oraz tlenki: Al2O3, SiO2, P2O5, K2O, MgO, CaO, Na2O, MnO, TiO2, Cr2O3 (XRF), a następnie obliczono wskaźniki geochemiczne stosowane do identyfikacji paleośrodowiska sedymentacji (Th/U, Th/K2O, V/Cr, P2O5/Al2O3, Rb/K). Stwierdzono, że zawartość pierwiastków U, Th, V, Cr, Rb, K wykazała bardzo podobne wartości dla iłowców z otworów wiertniczych : Borowo, Syczyn 7, Kulik, natomiast w próbce z otworu Kopina 1 obserwowano wyraźnie niższe ich wartości. Analiza wartości wskaźników geochemicznych dla wszystkich próbek wykazała, że wskaźniki takie jak: U, Th, Th/U, P2O5/Al2O3, V/Cr, Rb/K mogą być stosowane do identyfikacji środowisk sedymentacyjnych i korelacji geochemicznych sekwencji skalnych LZW.

EN

The most important part of the coal-bearing Carboniferous series is the Lublin formation (Lublin beds) (Westphalian A and B), where the main multi-seam coal deposits occur. Westphalian B is represented by a limnic series with are irregularly formed horizons of freshwater faunal. The paper presents the characteristics of horizons containing the remains of freshwater faunal from the boreholes: Borowo, Syczyn 7, Kulik, Kopina 1 (LCB). These horizons build claystones with layers or clay siderite concretions. For the analyzed horizons the content of the following elements: U, Th, V, Cr, Rb, K (ICP-MS) and oxides: Al2O3, SiO2, P2O5, K2O, MgO, CaO, Na2O, MnO, TiO2, Cr2O3 (XRF) were determined. The most commonly ratios used in the identification of palaeoenvironment sedimentary were calculated (Th/U, Th/K2O, V/Cr, P2O5/Al2O3, Rb/K). It was found that the content of elements U, Th, V, Cr, Rb K showed very similar values for claystones from borehole: Borowo, Syczyn 7, Kulik, while the sample from borehole Kopina 1 clearly lower value was observed. The research for all samples showed that those ratios such as: U, Th, Th/U, P2O5/Al2O3, V/Cr, Rb/K may be used to identify sedimentary environment and to geochemical correlations of the sedimentary rock sequences in the LCB.

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Badania faunistyczne wód polskiej części Tatr w latach 1919-1939

Kownacki A., Ślusarczyk J. M.

Kwartalnik Historii Nauki i Techniki

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2015

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R. 60, nr 3

67--77

EN

This work constitutes a continued presentation of the history of Polish research in the fauna of the Tatra waters and covers the inter-war period. During the years 1919-1939 these studies were still conducted but on a smaller scale than before the 1st World War. Many publications were based on earlier research done before 1914, which were broader works concerning the territory of the whole country, including also the Tatra waters, such as a monograph on the leeches of Poland by Michał Giedroyć, lacewing insects by Józef Dzięgielewicz, or juxtaposition of Heteroptera (true bugs) of “Galicia” by Adam Krasucki. Alfred Lityński summed up his many years’ research on the fauna of Cladocera (water fleas) conducted in 120 ponds, both on the Polish and Slovak sides of the Tatra Mountains. Unpublished materials of deceased scientists were used as well. Professor Kazimierz Simm, the disciple of professor Antoni Wierzejewski who died in 1916, published his monograph on Spongaria, in which he mentioned Spongaria from the Toporowy Pond and included notes about the winter fauna in the outflow of Morskie Oko. Museum collections were also used. Edward Schechtel worked out feed for trouts caught in Morskie Oko in 1900. New research on the fauna of the Tatra Mountains were conducted both as part of broader studies in the Polish fauna but also presented results of studies pursued only in the Tatras. Numerous researchers continued earlier studies of zooplankton crustacea in the waters of the Tatra Mountains during the inter-war period. Monographic study on Phyllopoda and Copepoda complexes of the Toporowy Pond was presented by Kazimierz Gajl. Several works of Zygmunt Koźmiński were devoted to population and taxonomic studies on plankton crustacean Cyclops strennus. Tadeusz Wolski found in the bog-spring on Kalatówki a new Tatra species of water flea (Cladocera) – Moina rectirostris. Meaningful from the scientific point of view and, at the same time, controversial, was the work of Gajl on Branchinecta paludosa. Using an enormous amount of materials coming from the Dwoisty Pond, as well as comparative material from Scandinavia, arctic European and Asian parts of Russia, Greenland, Alasca, and on the basis of differences in anatomical features, he came to a conclusion that the population of the Polish Tatras was a separate species Branchinecta polonica. This distinction was questioned later by scientists. It remained unsolved, however, because the population of this species in the Dwoisty Pond died out. At that time, for much broader scale studies were performed on flatworms (Dendrocoelum lacteum). They were started by Władysław Poliński with his monograph on the distribution of two species of Acoela – Crenobia alpina i Dugesia gonocephala – in Poland, and continued by W. Tomaszewski. Yet much greater achievements in learning about this group were made by Marian Gieysztor, who not only named several new species from the Tatras but on the basis of the materials coming from there also described species quite new to science: Macrostomum catarractae and Dalyellia tatrica. His research were on the global scale and later scientists named one species Gieysztor. From the world-science point of view, equally important were studies conducted by Witold Stefański on nematodes living freely in pond mosses and the lakes of the Tatra Mountains. In addition to the register of species, majority of which were found for the first time in the Tatra waters, he described three species new to science: Tripyla tatrica, Steratocephalus demani and Bunonema steineri. One of the greatest achievements of inter-war hydrobiology were studies concerning biology of the inshore sands, the so-called psammon, conducted by Jerzy Wiśniewski all over Poland, including the territory of the Tatra Mountains. In the Tatras Wiśniewski studied the fauna of rotifers occurring in the psammon on the shores of lakes and streams and the fauna of underwater sand. Briofile rotifers in Poland were studied by Leszek Kazimierz Pawłowski and in his research materials from the Tatra Mountains were also included. Similarly, Władysław Rydzewski in his review of Polish water mites from the Tatras named 9 species. On a smaller scale studies were conducted on the insects living in the Tatra waters. In his key to mayflies, based on the archive materials, Józef Stanisław Mikulski listed 7 species from the Tatra Mountains. A note on morphologic differences of mayflies from Baetis alpinus group was published by Anna Steinberg. Publishing his findings of many-years’ studies on lacewings in Poland from the area of the Tatra Mountains, Jan Zaćwilichowski named only one species Sialis flavilateratafrom Stawy Gąsiennicowe. In a thorough monograph by Tadeusz Jaczewski on water boatmen (Heteroptera) in Poland, there is only one mention of aquatic bug Glaenocorisa cavifrons occurring in the Toporowy Staw. In his subsequent work (Jaczewski), another species from Toporowy Staw was mentioned – Notonecta lutea. Of fundamental importance were only the studies on Tatra dragonflies conducted by Józef Fudakowski. He found 39 species of dragonflies in the area of the Tatra Mountains, occurring in lower water bodies: Toporowy Staw Niżny, Toporowy Staw Wyżny, Smreczyński Staw, at Capki bog-spring, on Siwa Polana, in Dolina Kondratowa, Dolina Pyszna, and the high-situated bog-spring near Morskie Oko. A popular-science review of studies on the Tatra lakes, which included also fauna research, were presented by Jerzy Młodziejowski i J. Rzóska.

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Fauna interglacjału ferdynandowskiego z Podgórza koło Wyśmierzyc nad Pilicą

Skompski F.

Przegląd Geologiczny

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2004

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Vol. 52, nr 6

516-–518

EN

The profile of the borehole Podgórze B1, which at first was reconed among the Mazovian Interglacial was revealed by palynological analyses to represent the Ferdynandów Interglacial. Additional paleozoological studies confirmed presence of diverse faunal remains: Ostracoda, Pisces, Mollusca and Coleoptera, which allow to better recognize the character of environment of the interglacial sediments in Podgórze.