Michał Zatorski, Krzysztof Buczek and Paweł Franczak
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Joanna Pszonka, Katarína Žecová and Marek Wendorff
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Piotr Strzeboński, Justyna Kowal-Kasprzyk and Barbara Olszewska
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Włodzimierz Margielewski, Adam Michczyński and Andrzej Obidowicz
landslide (Beskid Średni Range, Outer Carpathians). Studia Geomorphologica Carpatho-Balcanica 35: 63-79
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Włodzimierz Margielewski, Piotr Kołaczek, Adam Michczyński, Andrzej Obidowicz and Anna Pazdur
deposits of the Beskid Makowski and Beskid Wyspowy Mts. area (Polish Outer Carpathians). Folia Quaternaria 76: 1–149.
 Margielewski W, 2006b. Structural control and types of movements of rock mass in anisotropic rocks: case studies in the Polish FlyschCarpathians. Geomorphology 77(1–2): 47–68, DOI 10.1016/j.geomorph.2006.01.003. http://dx.doi.org/10.1016/j.geomorph.2006.01.003
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Nestor Oszczypko, Dorota Salata and Patrik Konečný
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Miroslav Bubík, Juraj Franců, Helena Gilíková, Jiří Otava and Lilian Švábenická
Type sections/areas for all four formations distinguished in the sedimentary succession of the Subsilesian Unit on Czech territory were revisited and described. New data on lithology, sedimentology, fossil record, biostratigraphy, heavy-minerals and geochemical proxies are based on observations and analysis of these sections. The historical type section of the Frýdek Formation was destroyed during railway construction in 19th century. Outcrops of Campanian to Maastrichtian marls and sandstones on the southwestern slope of “Castle hill” at Frýdek, are proposed as a new type section. The Ostravice riverbed in Frýdlant nad Ostravicí was originally designated as the type area, not mentioning the particular section. This area, even when supplemented with Sibudov Creek, does not show all typical facies of the formation. The outcrops range from lowermost Eocene to Eocene-Oligocene transition. In the original description of the Menilite Formation Glocker mentioned several localities in the area covering the Ždanice, Subsilesian and Silesian units, not mentioning the principal one. The single sections, each not exceeding a thickness of 2 m, are not sufficient to be a type section. Instead of that, we propose the area between Paršovice and Bystřice pod Hostýnem, covering the historical localities, as the type area. The type locality of the Ženklava Formation is an outcrop in an unnamed creek in Ženklava according to the original definition. It seems to be reasonable to extend the type section to the whole 500 m long section of the creek with the outcrops that better illustrate the lithological variability of the formation. New biostratigraphic data allow assignment to late Egerian (Eggenburgian?).
Anna Bucała, Włodzimierz Margielewski, Leszek Starkel, Krzysztof Buczek and Valentina Zernitskaya
FlyschCarpathians (Czech Republic/Slovakia). Quaternary Research 80(1): 33–46, DOI 10.1016/j.yqres.2013.03.009. http://dx.doi.org/10.1016/j.yqres.2013.03.009
 Parczewski M, 1988. Najstarsza faza kultury wczesnosłowiańskiej w Polsce (The oldest phase of the Early Slavonic Culture in Poland). Rozprawy habilitacyjne 141, Jagiellonian University Kraków.
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Krystyna Żbikowska-Zdun, Krzysztof Piksa and Anna Smaczyńska
Variation of selected morphological characters of the cave mite Oribella cavatica Kunst, 1962 (Acari, Oribatida)
Two populations of Oribella cavatica were examined. The mites were isolated from bat guano collected in February 2006 in Zbójecka Cave in Mount Łopień and in the cave Czarci Dół, which are situated in the Beskid Wyspowy Mountains, within the Flysch Carpathians in southern Poland. Coefficients of variation of body length and width, lamella length, and sensillus length of this species under stenotopic conditions were compared with those of two eurytopic species. The stable variation of sensillus length of O. cavatica, like differences in the variation of Heminothrus peltifer in various soil habitats, may have bioindicative significance.
BOYD S.A., MORTLAND M.M., CHIOU C.T., 1988: Sorption characteristics of organic compounds on hexadecyltrimethylammonium smectite. Soil Science Society of America Journal 52, 652-657.
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FRANUS W., 2002: Studium geologiczno-mineralogiczne skaŁ ilastych formacji pstrych Łupków jednostki skolskiej. Prace Mineralogiczne PAN 92, 1-60.