INVESTIGATION OF THE IMPORTANCE OF STARUNIA PALEONTOLOGICAL LOCATION OF THE PLEISTOCENE FAUNA OF THE RHINOCEROSES AND THE MAMMOTHS FOR QUATERNARY GEOLOGY

Kateryna Radlovska, Sofiia Kachala

Abstract


The first finds of mummified carcasses of the hairy rhino, mammoth, horse, roe deer and other animals were carried out at a depth of 12 m when passing the mines for the production of ozokerite near the village. The expedition of the Academy of Skill from Krakow, when passing a mine at a depth of 17 m, found the remains of 3 more hairy rhinos. There were also numerous bones of small vertebrates (rodents), artichokes, numerous insects, beetles, parasitic worms, slag, butterflies, spiders, snails, vascular plants, seeds and branches of dwarf birch, alder, and other representatives of tundra flora. After the earthquake in the Vrancha Mountains (Romania), the first and still unique mud volcano in the Carpathians, which gave the Starunia paleontological location a new "sound", arose on the ozokerite deposit.

An important result was the discovery of the most desirable area, where the remains of giant mammals and even the Cro-Magnon Pleistocene could still be found at the depths. All the numerous interdisciplinary traces of Polish and Ukrainian scientists confirm the uniqueness of Starunia on a global scale, requiring the preservation and further study of paleontological finds and the only mud volcano in the Carpathians. Such findings can only be made by organizing the Starunia geodynamic ground International Ecological and Tourist Center «Geopark Ice Age».


Keywords


upper Pleistocene; hairy rhino; mammoth; tundra; natural-human-made geosystems; paleoclimate; Starunia area; Geopark

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References


Adamenko, O. (2016). Our Future House is Ekoeurope the System of Ecological Security of the European Union, Carpathian Euroregion and Ukraine. Scientific Bulletin Series D: Mining, Mineral Processing, Non-Ferrous Metallurgy, Geology and Environmental Engineering, 30 (2), 7–20.

Kyrpach, Yu. V. (2009). Geological structure of south-west part Predkarpatian foredeep (Rozsilna - Dzvinjach - Starunja area) and structural-lithological model of salt deposits. Collection of scientific works of the IGS NAS of Ukraine, 2, 78–81.

Matyszkiewicz, J., Kotarba, M., Krzak, M., Wendorff, M. (2016). Department of Environmental Analyses, Geological Mapping and Economic Geology. Geology, Geophysics & Environment, 42 (2), 226. doi: https://doi.org/10.7494/geol.2016.42.2.226

Аdamenko, O. M. (2019). The Upper Pleistocene stratigraphy of the Starunya site as a “bridge” between the stratigraphical frameworks of Western Europe and the plain area of Ukraine. Journal of Geology, Geography and Geoecology, 28 (2), 213–220. doi: https://doi.org/10.15421/111922

Adamenko, O. M., Kryzhanivsky, Y. I., Vekeryk, V. I. et. al. (2005). A concept of an International "Ice-Age Yepark" as an ecological-tourist center in Starunia former ozokerite mine, fore- Carpatian region, Ukraine In. Polish and Ukrainian geological studies (2004-2005) at Starunia-the area Discoveries of Wolly Rhinoceroses. Warszawa; Krakow, 205–209.

Menshov, O., Kuderavets, R., Vyzhva, S., Maksymchuk, V., Chobotok, I., Pastushenko, T. (2016). Magnetic studies at Starunia paleontological and hydrocarbon bearing site (Carpathians, Ukraine). Studia Geophysica et Geodaetica, 60 (4), 731–746. doi: https://doi.org/10.1007/s11200-016-0621-2

Woch, M. W., Trzcińska-Tacik, H. (2014). High occurrence of rare inland halophytes on post-mining sites in western Ukraine. Nordic Journal of Botany, 33 (1), 101–108. doi: https://doi.org/10.1111/njb.00607

Ziemianin, K., Brzuszek, P., Słoczyński, T., Jankowski, L. (2015). Dispersed organic matter in shales from Menilite Beds within Polish Outer Carpathians – preliminary diagnosis. Nafta-Gaz, 71 (9), 615–623.

Palmer, D. (2005). Earth. Kyiv: Entsyklopediya, 847.

Gębica, P., Jacyszyn, A., Krąpiec, M., Budek, A., Czumak, N., Starkel, L. et. al. (2016). Stratigraphy of alluvia and phases of the Holocene floods in the valleys of the Eastern Carpathians foreland. Quaternary International, 415, 55–66. doi: https://doi.org/10.1016/j.quaint.2015.11.088




DOI: http://dx.doi.org/10.21303/2585-6847.2019.001035

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ISSN 2585-6847 (Online), ISSN 2585-6839 (Print)