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Документ Baymouth barrier of Dniestrovsky liman (DLBB)(Astroprint, 2006) Konikov, Yevhenii G.; Kravchuk, Anna O.The baymouth barrier varies in width from 1 km, where it is attached to the east side of the mainland coast, to 70-100 m.A natural inlet,called Tsaregradsky Girlo,occurs in the western part of the barrier,where it acts as a connection between the liman and the sea.The surface of the barrier consists of sandy beach and dune deposits.The absolute elevation of the barrier ranges from 0.5 to 4.5 m. At present,its natural landscape is altered by extensive development.Numerous boreholes reveal deposits of Middle-Late Pleistocene and Holocene age (Fig. 29).The erosional downcutting of the Dniester River valley penetrated 74 m of Neogene deposits. Thickness of the Middle-Late Pleistocene alluvium averages 20-30 m. The Late Pleistocene alluvium (Antsky horizon) corresponds to one of the stages of the Neoeuxinian regression.Based on radiocarbon dating,the age of the alluvium is 17,050 yrs BP (borehole #221).Higher on the outcrop, on the reworked surface of the Neoeuxinian alluvium (-20 to -30 m),lies a layer of the transgressive series of the Neoeuxinian basin. It is 1-2 m thick and consists of organic liman clays with large amounts of plant fragments and peat horizons. The radiocarbon age of these deposits is 9,500 yrs BP.This point marks the beginning of the formation of the modern liman and the mouth of the Dniester River.Документ Bol'shaya Akkarzha(Astroprint, 2006) Smyntyna, Olena V.; Сминтина, Олена Валентинівна; Смынтына, Елена ВалентиновнаThis late Palaeolithic settlement was a base camp for bison hunters. It is located on the right bank of the small Akkarzha River (or Akkarzhanskaya ravine),6 km from the shore and 1.5 km to the southwest of Velikodolinskoye village (Ovidiopol district of Odessa region). The settlement was discovered by Kraskovsky in 1955 and excavated later by Boriskovsky (1963), Kraskovsky (1978),and Sapozhnikov (2003). Palynological,stratigraphic,and paleontological analysis of the settlement supplemented by radiocarbon dating enabled researchers to attribute it to the Last Glacial Maximum [19- 18 ky BP] (Sapozhnikov, 2003).Four household complexes (each 15-23 m2) have been uncovered consisting of hearths and,concentrated around them,flint artifacts (about 57,000 pieces in total)and faunal remains(represented exclusively by Bison priscus with only some horse teeth).Peculiarities of the flint industry and lifeways of this site have become the background for delineating a special Akkarzhanskaya Culture of the LGM related to the circle of Gravettian cultures of Europe.Документ Il'inka(Astroprint, 2006) Smyntyna, Olena V.; Сминтина, Олена Валентинівна; Смынтына, Елена ВалентиновнаSituated on the northeastern outskirts of the eponymous village (Belyaevka district, Odessa region), the karst cave in the mouth of short deep girder on the right bank of Kuyalnik Liman was discovered by Gritsay and A. Roschin (Gritsay, 1939). It is an archaeological as well as paleontological location, the most striking feature of which being its connection with cave bears procurement and worship. It was the subject of repeated studies in the middle of the 20th century (Zamyatnin, 1950; Boriskovsky and Kraskovsky, 1961; Kraskovsky, 1978), which have been renewed through the collaboration of the Paleontological Museum of Odessa I.I. Mechnikov National University with the University of Vienna, Austria.Документ Luzanovka(Astroprint, 2006) Smyntyna, Olena V.; Сминтина, Олена Валентинівна; Смынтына, Елена ВалентиновнаThe ancient Greek site of the 5th-beginning of the 4th century ВСЕ known as the 'Harbor of Istrians' is located on the left bank of the mouth of Kuyalnitsky Liman (Fig. 1b) (Diamant, 1980;Sinitsyn, 1955, 1957). Minimally excavated in the 1920s-1930s, this site is now totally destroyed by abrasive processes and human activity.According to written tradition, Istrians' Harbor was tightly connected with Isiaks' Harbor located within the contemporary port of Odessa and adjacent plateau between Devolanovskiy spusk and Voennyi spusk (names of two modern streets of Odessa).During the 5th - 3rd centuries ВСЕ, the settlement of Luzanovka was connected with nomadic Scythians and maintained broad-based contacts with neighboring Greek poleis.Документ Parutino(Astroprint, 2006) Konikov, Yevhenii G.; Chepalyga, A. L.The stratotype of the Bugsky horizon (Veklich, Sirenko, 1972)is located near the northern outskirts of Parutino and represents a natural outcrop on the erosional shore of Dniepero-Bugsky Liman. The slope reaches 17-20 min height.The stratigraphic section reveals the Upper Pleistocene loess-paleosol formations overlying Pliocene-Quaternary fluvio-lacustrine sediments (Fig. 6).It, in turn,is overlain by Dofinophinovskaya or Bryanskaya (Velichko, 1990)soil with a date of 26-30 ky BP.Документ Right (western) shore of Berezansky liman(Astroprint, 2006) Konikov, Yevhenii G.The accumulative terrace is located on the eastern shore of Berazansky Liman at 1 km from the mouth (Fig.41).The terrace is 1.5-2.0 m in height and 30 m in width.Based on the trenches along the coastal bluff, the following deposits are described after Gozhik (1984):Section 1 (depth, m): 0.00-0.30 modern soil 0.30-1.15 brown-gray sandy mud, diluvial (sharp lower contact) 1.15-1.70 moderately sorted sand with large amounts of Cardium edule, Mytilus sp., and Hydrobia sp. shells (beach facies).The age of shells from this layer is 4500 14C yrs BP.Документ Series of accumulative terraces from Dneprovskoe village to Ochakov Cape(Astroprint, 2006) Konikov, Yevhenii G.; Kravchuk, Anna O.Accumulative terraces (beach ridges) are located sporadically along the mainland shore over a distance of about 10 km.Their width ranges from 20-30 m to 300-500 m at the Adzhigol'skaya spit and Ochakov cape (Fig. 22).The geological structure of these terraces is essentially similar (Fig. 23). Near the cliff of the mainland coast, they have elevations 1.5-2.3 m above the liman level. Here, the sandy deposits of beach facies are covered by a layer of modern muddy diluvium averaging 0.3-0.7 m in thickness. Closer to the water line, the diluvium pinches out, and the upper unit consists of shellrich sandy deposits of the modern beach.Underlying the aforementioned sequence are moderately sorted sands with layers of shells and shell detritus.According to sediment cores, their thickness at the Adzhigol'skaya spit and Ochakov cape is 3.5-5.0 m and 10-11 m, respectively.Based on molluscan assemblages, the age of these deposits is Kalamitian- Dzhemetinian.The upper sequence of layers with typical Kalamitian molluscs is located at absolute elevations ranging from -5 to 0.2 m.The typical Kalamitian-Dzhemetinian waveformed(beach facies) deposits are underlain by muddy sands of Vityazevian ageДокумент Slobodka-Romanovka(Astroprint, 2006) Smyntyna, Olena V.; Сминтина, Олена Валентинівна; Смынтына, Елена ВалентиновнаAn Eneolithic barrow situated on the hill between Krivaya Balka and Slobodka- Romanovka (nowadays on the outskirts of the central part of the city of Odessa) which gradually descends to the sea, ending by the famous Odessa Peresyp (Fig. 1b). Most probably, a series of barrows was constructed there, and only one has survived.This barrow is interpreted as the first polyethnic cemetery within the territory of the contemporary city of Odessa. Its thousand-year history involved many reshapings through burials and refillings as a ritual place used by Usatovo, Pit-Grave, Kemi-Oba, Catacomb, and Sabatinovka populations (Sinitsyn, 1955). Stratigraphically traced by Dobrovolsky (1950), this barrow is regarded as the most detailed reference point for barrow graves of prehistoric inhabitants of NWBS region.Документ Zhevakhova Gora(Astroprint, 2006) Smyntyna, Olena V.; Сминтина, Олена Валентинівна; Смынтына, Елена ВалентиновнаThis high cape dividing Khadzhibeisky and Kuyalnitsky Limans on the high bank of the northern part of Odessa Bay contains a series of archaeological monuments and single finds of different periods.Most of them (a Late Bronze Age barrow,two diachronic barrows,a settlement of the 2nd - beginning of the 5th century CE) have only been located without further investigations.Other finds are represented by scarce numismatics, among which Roman coins (a denarium of Antonin Pius II and a copper coin of Theodosius minted in Nikomedia in the 4th century ВСЕ)and a silver eastern coin were discovered (Fabritsius, 1951; Diamant and Kuzmenko, 1978).The settlement of the 5th-3rd century ВСЕ that was discovered and studied by Mikhail Sinitsyn(1955) in the 1950s and 1960s is widely known. He uncovered houses, a pit for grain storage,red-figure vessels, and other objects.In 2006, fieldwork at this settlement resumed.