Interglacial-glacial cycles recorded in the deposit sequence at Kruzhyky on the Dniester River (East Carpathian Foreland)

Łanczont, Maria; Boguckyj, Aandrij; Mroczek, Przemysław; Zieliński, Paweł; Jacyszyn, Andrij; Pidek, Agnieszka I.; Urban, Daniel F.; Kulesza, Piotr; Hołub, Beata

doi:10.2478/v10066-011-0052-6

Cited by 8 publications

(10 citation statements)

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“…Доцільно зазначити, що в Україні використовуються різні стратиграфічні схеми четвертинного періоду: регіональна стратиграфічна схема Західної України (Bogucki, 1986; і стратиграфічна схема НСК України (Veklitch et al, 1993) та її модифікований варіант (Gerasimenko, 2004;Gozhik et al, 2000;Matviishyna et al, 2010). Стосовно кореляції стратиграфічних схем є певні розбіжності, які стосуються положення кайдацького і дніпровського кліматолітів (Rousseau et al, 2001;Gerasimenko, 2006;Lindner et al, 2006;Łanczont & Boguckyj, 2007;Łanczont et al, 2014;Haesaerts et al, 2016).…”

Section: стратиграфічна атрибуція педокомплексу іunclassified

“…Ґрунти часто розділяються кріогенними структурами або лесоподібними утвореннями. У седиментаційних пастках будова ґрунтової світи стає суттєво складнішою (Łanczont & Boguckyj, 2007). Ґрунтовий комплекс (ПК І) зі схожою будовою розкрито у розрізі Новий Тік, в якому чорнозем підстеляється підзолистим ґрунтом на давньому підвищенні та переходить у складно побудовану ґрунтову світу у седиментаційній пастці (похованій балці).…”

Section: стратиграфічна атрибуція педокомплексу іunclassified

“…(Fedorowicz et al, 2013;Kusiak et al, 2012). У найповніших розрізах Західної України (Колодіїв, Пронятин, Маріямпіль, Галич) виділено три колодіївських ґрунти, відокремлені рівнями кріогенезу та лесоподібними утвореннями (Łanczont & Boguckyj, 2007;Łanczont et al, 2015a, b;Bogucki et al, 2019). Нижній колодіївський ґрунт (Колодіїв-3) сформувався під лісостепом, тоді як молодші ґрунти (Колодіїв-1 і Колодіїв-2) є степовими (Łanczont et al, 2015a).…”

Section: стратиграфічна атрибуція педокомплексу іunclassified

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Palaeolithic site of Novyi Tik: stratigraphic and palaeogeographic aspects

Bonchkovskyi,

Kulakovska,

Usik

2021

PhGG

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The Novyi Tik loess-palaeosol sequence is characterized by a detailed stratification due to both its location on the slope of the valleys of Berestova and Styr rivers, as well as excavation of buried gullies, which serve as sediment traps. Nineteen basic stratigraphic units have been allocated in the section, grouped into 7 main units (4 loesses and 3 pedocomplexes). In 2018, a flint artefact was found in the upper pedocomplex (Pedocomplex I), which was interpreted as a Levallois bilateral-alternative sub-rectangular core nucleus. The precise stratigraphic position of the artefact and the comprehensive study of the loess-palaeosol sequence by the methods of Earth sciences (lithological and stratigraphical, palaeopedological (including micromorphological), geochemical and palynological) enable not only to establish chronostratigraphic position of the tool, but also to reconstruct the habitat of ancient humans. The Levallois core nucleus was found in the BCs horizon of the Podzol (subunit 10c). The Pedocomplex I was tentatively correlated with the Horohiv soil complex of the regional stratigraphic scheme of Western Ukraine, with the Pryluky-Kaydaky pedocomplex of the Quaternary stratigraphic framework of Ukraine and with MIS 5. The soil, which contained the artefact, probably corresponds to the lower Kolodiiv soil (Kolodiiv-3). The tentative age of the core nucleus is the end of the MIS 5d or the beginning of the MIS 5c. Thus, the studied section is currently the oldest stratified Palaeolithic site of the Volyn’ Upland. This site could be the key to exploring the Middle Palaeolithic of the region. A split Mammuthus primigenius bone found at the bottom of Bug loess (MIS 2) enhances the site’s importance.

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Section: стратиграфічна атрибуція педокомплексу іunclassified

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Palaeolithic site of Novyi Tik: stratigraphic and palaeogeographic aspects

Bonchkovskyi,

Kulakovska,

Usik

2021

PhGG

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“…Карпатська серія. Геологічна карта і карта корисних копалин дочетвертинних утворень, 2005; Яцишин і Плотніков, 2004;Яцишин, Богуцький і Плотніков, 2008;Яцишин та ін., 2011;Яцишин, 2014;Bogucki, Łanczont i Wojtanowicz, 2000;Bogucki i in., 2010;Łanczont i in., 2010;Łanczont et al, 2019;Terpiłowski i in., 2011;Zieliński i in., 2011).…”

unclassified

“…Максимальна потужність розкритих у правій (розташованій вище за течією Дністра) частині відслонення нагромаджень тераси сягає 17 м. У їхній основі залягає товща (1,7 м) гумідного (руслова і заплавна фації) алювію (Богуцький та ін., 2007;Богуцький та ін., 2011c;Łanczont i in., 2010;Łanczont et al, 2019;Zieliński i in., 2011). У центральній частині відслонення на рівні горизонту заплавного алювію збереглась лінза старичного алювію, збудованого сірими і темно-сірими суглинками з прошарками і лінзами торфу.…”

unclassified

Geo-Tourist Sites and Routes in the Territory of Sambir-Khyriv Terrace Foothills

Yatsyshyn¹,

Bogucki²,

Dmytruk³

et al. 2022

gpc

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The geological and geomorphological objects of Sambir-Khyriv terrace foothills have been characterized as natural monuments and potentially popular geo-touristic sites. The foothills cover the pre-Carpathian sections of the Stryvihor and Dniester valleys, the entire Bolozivka valley and the uplands of the interfluves. The main geomorphological elements of the study area are river valleys with a complex of river terraces of different ages. Outside the valleys, in the uplands of the interfluves, the most ancient foothill terraces and different-aged denudation leveling surfaces are spread. Relief-forming deposits of the foothills are mainly represented by Neogene and Anthropogenic accumulations. The anthropogenic depositsoverlapping the older accumulations are extremely heterogeneous in terms of genesis, age, and lithological structure. Within the foothills, the most valuable natural monuments are the following objects: sections of anthropogenic accumulations Slokhyni, Torhanovychi 1 and 2 and Kruzhyky, as well as landforms, i.e. a fragment of Krasna surfacedeveloped on the eastern macro-slope of RadychMountain and the western part of the Bolozivka valley. We identify the listed objects as stratigraphic and geochronological (sections of Slokhyni, Torhanovychi 1 and 2 and Kruzhyky), paleontological (section of Kruzhyky), geomorphological (surface of Krasna, Bolozivka valley),and scenic natural monuments (surface of Krasna). Foothill natural monuments are important in terms of research and geo-educational functions, in particular to study and illustrate stratification of sedimentary accumulations of anthropogenic age; lithological and sedimentological features of continental deposits; variability of paleogeographic conditions of anthropogenic age; cyclicityof continental morpholithogenetic processes; formation of exogenic forms of relief due to denudation shearing of uneven surface of the Earth, erosion and accretion activity of fluvial flows; soil-forming processes; and geological age of human material culture. The described natural monuments are important for the organization of events intended to popularize geological and geographical science, as well as environmental education among people, and teach the skills of careful attitude to the environment. It would befeasible to integrate them into the existing network of tourist routes inLviv region. Key words: Sambir-Khyriv terrace foothills; natural monuments; sections of anthropogenic deposits; surface of Krasna; Bolozivka valley.

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Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine

Goździk

Zieliński

2017

Geologos

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Deposits formed between the Neogene/Pleistocene transition and into the Early Pleistocene have been studied, mainly on the basis of drillings and at rare, small outcrops in the lowland part of Polish territory. At the Bełchatów lignite mine (Kleszczów Graben, central Poland), one of the largest opencast pits in Europe, strata of this age have long been exposed in extensive outcrops. The present paper is based on our field studies and laboratory analyses, as well as on research data presented by other authors. For that reason, it can be seen as an overview of current knowledge of lowermost Pleistocene deposits at Bełchatów, where exploitation of the Quaternary overburden has just been completed. The results of cartographic work, sedimentological, mineralogical and palynological analyses as well as assessment of sand grain morphology have been considered. All of these studies have allowed the distinction of three Lower Pleistocene series, i.e., the Łękińsko, Faustynów and Krzaki series. These were laid down in fluvial environments between the end of the Pliocene up to the advance of the first Scandinavian ice sheet on central Poland. The following environmental features have been interpreted: phases of river incision and aggradation, changes of river channel patterns, source sediments for alluvia, rates of aeolian supply to rivers and roles of fluvial systems in morphological and geological development of the area. The two older series studied, i.e., Łękińsko and Faustynów, share common characteristics. They were formed by sinuous rivers in boreal forest and open forest environments. The Neogene substratum was the source of the alluvium. The younger series (Krzaki) formed mainly in a braided river setting, under conditions of progressive climatic cooling. Over time, a gradual increase of aeolian supply to the fluvial system can be noted; initially, silt and sand were laid down, followed by sand only during cold desert conditions. These fluvio-periglacial conditions are identified in the foreground of the advance of the oldest ice sheet into this part of central Poland. The series studied have been compared with other fluvial successions which accumulated in the Kleszczów Graben during subsequent glaciations so as to document general changes in fluvial systems as reactions to climatic evolution. Thus, a palaeoenvironmental scenario has emerged which could be considered to be characteristic of central Poland during the Early Pleistocene.

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Interglacial-glacial cycles recorded in the deposit sequence at Kruzhyky on the Dniester River (East Carpathian Foreland)

Cited by 8 publications

References 1 publication

Palaeolithic site of Novyi Tik: stratigraphic and palaeogeographic aspects

Palaeolithic site of Novyi Tik: stratigraphic and palaeogeographic aspects

Geo-Tourist Sites and Routes in the Territory of Sambir-Khyriv Terrace Foothills

Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine

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