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Migracje zarobkowe Ukraińców do Polski a zasady zrównoważonego rozwoju

Skoczyńska-Prokopowicz B.

Zeszyty Naukowe. Organizacja i Zarządzanie / Politechnika Śląska

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2018

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z. 117

531--546

PL

Zjawisko migracji w tym zarobkowych do krajów UE rośnie w szybkim tempie. Migranci zarobkowi korzystają z ciągle modernizowanych rozwiązań prawnych umożliwiających im pracę na terenie państw UE. Do Polski przyjeżdżają głównie obywatele Ukrainy, zapełniają lukę na rynku pracy oraz w zakresie usług edukacyjnych szkolnictwa wyższego. Autorka przytacza ilustrację statystyczną zjawiska oraz omawia efekty dla polskiej gospodarki oraz formułuje postulaty dotyczące polityki społecznej wobec migrantów zarobkowych w Polsce. Ich realizacja wpisuje się w założenia zrównoważonego rozwoju umożliwiające ewolucję społeczeństwa i wzrost gospodarczy kraju.

EN

The phenomenon of migration, including labour migration, to EU countries, has been growing rapidly. Migrants who go abroad for financial reasons, benefit from constantly-modernised legal solutions enabling them to work in EU countries. Poland is mainly visited by Ukrainian citizens, who fill a gap in the labour market and who take advantage of Poland’s higher education services. The author of this article provides a statistical illustration of the phenomenon, discusses its effects on the Polish economy and proposes ways of developing social policy towards migrant workers in Poland. The realisation of these would fit into assumptions of sustainable development, allowing for the evolution of society and the economic growth of the country.

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MET System in Ukraine

Miyusov M. V., Zhukov D. S.

TransNav : International Journal on Marine Navigation and Safety of Sea Transportation

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2010

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Vol. 4, no. 4

465--470

EN

It is believed that Ukraine is one of the largest seafarers’ suppliers to the world maritime fleet. The vast and diverse system of waterways and lakes in addition to the tradition of seafaring and maritime history which dates back more than 200 years create the necessary basis for the government which considers it more important to provide graduates with the full education rather than merely to produce 'vocational' specialists. Moreover Ukraine has already made some major steps on the road to Euro integration having taken part in the Bologna process. Therefore it’s not surprising that on 15 January 2005 a new resolution of the Cabinet of Ministers of Ukraine was approved. The Odessa National Maritime Academy(ONMA) was the first to visualize it by means of the new-presented system of MET.

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Plant macrofossils and malacocoenoses of Quaternary mineral-organic sediments at Starunia palaeontological site and vicinity (Carpathian region, Ukraine)

Stachowicz-Rybka R., Gałka M., Alexandrowicz W. P., Alexandrowicz S. W.

Annales Societatis Geologorum Poloniae

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2009

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Vol. 79, No 3

297-313

EN

The unique nature of the Starunia palaeontological site, where near-perfectly preserved large mammals were discovered at the beginning of the 20th century, and incomplete knowledge on the development of palaeoenvironment in the Velyky Lukavets River valley in the Late Pleistocene and Holocene were the reasons for undertaking new comprehensive palaeobotanical and malacological studies. Starunia is also one of the sites bearing Pleistocene fossil flora, rare in this part of Europe. The results of plant macrofossil analysis show that in the Weichselian Middle Pleniglacial the landscape was dominated by steppe and tundra plant communities, being represented mostly by various grass and sedge species. Areas of higher humidity were covered with shrub tundra with Betula nana. The temperature requirements of taxa which are cool climate indicators show that the minimum July temperature amounted to at least 10°C. The record of Late Weichselian malacofauna confirms the dominance of an open landscape, mostly with steppe and steppe-tundra communities, as well as the presence of a dry, continental climate. At the beginning of the Holocene, an improvement of climatic and humidity conditions led to a fast local expansion of plant communities of the low and transition peat bog type, in the surroundings of shallow, periodically drying-up water pools. From the Middle Pleniglacial up to the present day, the area has been characterized by the presence of species tolerating an increased amount of salt in the environment. Their presence should be associated with natural brine effluences derived from Miocene strata in the bedrock.