Abstract

The discovery of large Pleistocene mammals at the Starunia ozokerite (named also earth wax) mine (the Ukrainian Carpathians) was a spectacular scientific event on a world scale. The initial discovery was made in 1907 when relics of party preserved mammoth and woolly rhinoceros were excavated. Later, in 1929, the Polish Academy of Arts and Sciences organized a scientific expedition to that site, which resulted in discovery of unique, nearly completely preserved woolly rhinoceros carcass embedded in Pleistocene sediments. A specific combination of brine, oil and clays into which the animal had sunk, is responsible for almost perfect preservation of this animal. The specimens found in 1907 are exhibited at the Natural History Museum in Lviv, Ukraine, whereas the unique specimen excavated in 1929 is displayed at the Natural History Museum in Kraków, Poland. The three sites: Starunia, a small Ukrainian village in which the geopark with the museum and the tourist centre are planned to be developed and two historical towns: Lviv and Kraków, closely connected with the discoveries of extinct large mammals, will be the key sites at the planned, Ukrainian-Polish trans-border geotourist trail “Traces of large extinct mammals, earth wax, oil and salt: from Starunia to Kraków”. The trail will also include the sites where occurrences of ozokerite, salt, brine and oil are known, i.e., the substances which preserved the animal carcasses. These are: the historical rock-salt mines in Wieliczka and Bochnia (Poland), Kalush and Stebnik (Ukraine), the Polish resorts – Iwonicz-Zdrój and Rymanów-Zdrój and the most famous Ukrainian resort – Truskavets; one of the oldest oilfields in the world – Bóbrka, where the Ignacy Łukasiewicz Memorial Open-Space Museum of Oil and Gas Industry is located and Boryslav oil and ozokerite field – the largest deposit in the Ukrainian Carpathians. The idea of Ukrainian-Polish trans-border tourist trail is strongly supported by geological, natural and cultural values of the Polish and the Ukrainian Carpathians.

Highlights

  • The discovery of large Pleistocene mammals dated at 40,000 – 35,000 years BC (Kuc et al, 2005; Kuc et al, 2011) at the Starunia ozokerite mine was a spectacular scientific event on a world scale (e.g., Alexandrowicz, 2004, 2005)

  • The three sites: Starunia – small village in the Ukrainian Carpathians and two historical cities – Kraków and Lviv (Fig. 4), closely connected with the unique palaeontological finding will be the key points at the planned UkrainianPolish trans-border geotourist trail “Traces of large extinct mammals, earth wax, oil and salt: from Starunia to Kraków” (Adamenko et al, 2009; Chornobay & Drygant, 2009; and Kubiak, 2009)

  • The flysch succession of the Boryslav-Pokuttya Unit is covered by the Lower Miocene Polyanitsya Beds (Fig. 8), which are absent from the Starunia fold, as well as the Vorotyshcha Beds, which host rock-salt and potassium salt seams as well as ozokerite veins and nests (Fig. 11)

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Summary

Introduction

The discovery of large Pleistocene mammals dated at 40,000 – 35,000 years BC (Kuc et al, 2005; Kuc et al, 2011) at the Starunia ozokerite (earth wax) mine (about 130 kilometres southeast of Lviv, Ukraine) was a spectacular scientific event on a world scale (e.g., Alexandrowicz, 2004, 2005). A unique combination of brine, oil and clays into which the animal had sunk, is responsible for almost perfect preservation of this specimen. Since this discovery the remnants of two more rhinoceroses have been found at this site. The three sites: Starunia – small village in the Ukrainian Carpathians and two historical cities – Kraków and Lviv (Fig. 4), closely connected with the unique palaeontological finding will be the key points at the planned UkrainianPolish trans-border geotourist trail “Traces of large extinct mammals, earth wax, oil and salt: from Starunia to Kraków” (Adamenko et al, 2009; Chornobay & Drygant, 2009; and Kubiak, 2009). The separate papers deal with one of the oldest oilfields exploited in Poland – the famous Bóbrka (Fig. 4), where the Ignacy Łukasiewicz Memorial Open-Space Museum of Oil and Gas Industry exists (Radwański, 2009b) and in Ukraine – Boryslav (Fig. 4) (Radwański, 2009a)

Nadvirnyanska PNIV
Outline of geology
Zgłobice Unit autochthonous Miocene strata of the Carpathian Foredeep
Shales Lgota Beds ssic
Pleistocene clays and gravels
Oil and gas occurrence
Salt mines and brines
Paleocene strata ozokerite shaft exploratory borehole
Boryslav block
Palaeocene thrust or fault
Conclusions
Full Text
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