 Nasza prezentacja jest twojej archiologicznej rekordy o barostrze, o komarokalczach z Brąza i post-deposicjonych procesów, w którym się pojawiła w Bukibniu i West-Ukraińskim. Przedmawiałem tę prezentację z kolegami, prezesem Przemysław Makarowicz i prezesem żanna Nikłaiewna Matwitszyna z Ukrainy. Nasza prezentacja pokazuje periody rozwoju komarokalczu w okazji Ukrainy. Komarokalczu stworzył się w karcze korektycznej w okazji Podolia, Subkarapartii i sztucznej części Wołynia, w czerwonej brąze. W międzyach 1800 i 1400 b.c. Jedna z największych koncentracjów Brąza i post-deposicjonych procesów jest Brąza i Bukibniu, gdzie w rady 5 kilometrach są dokumentowane 150 barostrów. Ta karcza nie jest wystarczająca na rady funeralowe, szczególnie dla wielu błędów. Pierwsze skończenie barostrów jest brąza i post-deposicjonych procesów. Charakteristyczne brąze i post-deposicjonych procesów są zbudowane w brązach, błędów i błędów. Są obowiązane z spektralnej analizy, aby oznaczać koncentrowanie brązy i post-deposicjonych procesów. Rady karbonu oczekiwają ograniczne rezydusy w błędach i błędów i błędów, oznacza periody rozwoju studiów komarokalczu. Rady karbonu oczekiwają ograniczne rezydusy w spieltiach i błędów i błędów, w์ rings profesor JASOUND Oæneata i oznacza rady i garii Canadian pedfele beneficiowanych w błędach iость wypal componentów. Urządzenie błędów nie jest rozwoju rynekanistyczne, a radyτα tragiczne lub realne sylach. W tym poziomie wytrzymującego arary stąd powróciło od roweru roweru. To charakterystyczne lantwo jest w porządku platołów, które zbierają brodowe walizy i bazy. Na prawdziwej okazji roweru roweru roweru roweru roweru roweru roweru roweru roweru roweru roweru roweru. W modernym czasie, obrony obrony są skończone przez obrony. W tajeczce geomorfologicznego mapu jest lokacja małca na platu Opilii, która wytrzyma do podolimu apelantu na topach platu. To jest lokacja platu obrony. The main aim of studying was the answer of the following sentences. Are the environmental conditions at the time where it's built and contemporary conditions similar or different? Is the material from which the muscles were built shows sociological compatibility with the ground? Does geohemical composition of mouths Correspond to geochemikal background and which level of enrichment in geochemical components are dominated and can be distinguished in barrels. How pass the positional processes could change the lithological and geochemical composition of sediment in barrels. Are the feelings pottery vessels found in barrels given lithologically and geochemical. Stratigraphy of the barrels number two in Bokivna shows from the floor black colour organic soil from the bronze age on the last ground. Burial model different soil horizon in the top of the profile and thin organic layer the humus level of the modern soil. Methods of sedimentological paleo-pedological and geochemical study. From sediment sables taken in Bokivna boxes, thin section micromorphology analysis and also paleo soil analysis was carried. From demand profile samples were taken from granular metric and geochemical analysis. Attempt were also made to fill of the pottery vessels from the examinated mounds from the same research. Charka and another organic material was rather radiocarbon dated. Main for chronological polyzons. Transformation of vegetation on the local scale is shown by polynological diagram based on core of pit deposits from the old riverbed near village Łuka in the western part of Harwich-Uk activity basin in the Dniester Valley. In polynological studies conducted on Ukraine the problem of cold pollen presentation status is now. Poland is corroded and usually a few. In the studies it was also similar. At the Atlantic and subatlantic zone we could observe the decline of in forest. In subatlantic periods there is an expansion of the alder and they are cereals, cerealia i fagopyrum and all other species of heps has been found. The profile of modern soils has been tested on a trench outside of the burial mound. The modern soil of the burial mound develops under conditions of intense hydraison, science of glane processes. It had clearly distinguished alluvial and illuvial horizons. A short profile with light grey humus from the top shows science of development of washing processes. In the bottom part the soils, the mobility of aluminium iron and manganese is recorded. The nature of this profile and the micromorfological indices allow the soil to be included in the type of grey poxolized soils of the forest zone. The infiltrates with the profile are different. In the upper part they show science of context of silk humus substance that grey open. In the horizontal plane in bottom part they are transparent peruginos. Colomorphic aluminium infiltrator occur simultaneously with the precipitation of iron oxidized in the form of hard pan and manganese stains. The mechanical composition in the alluvial level is fine clay and in the alluvial medium to coarse. The soil reflect in the conditions for the formation of coniferous decidose forest with moderately acumid climate. Soil horizon under the barrel is centrally a chernosem with mainly processes of accumulation of organic matter which shaped the level of humus with the high thickness. Even accumulation of organic matter which shape even at the depth of 60 cm from the soil surface there is still organic matter. The humus profile of the thickness could be arising in warmer conditions than today under a rich most probably different size of grass vegetation in the conditions of northern step of forest step. In the whole humus layer cotovinas are visible indicating of activity of soil fauna. Evidence of profile leaching and infiltrations some degree of dispersion of organic matter and its penetration to a bigger depth are associated with sufficient and possibly excessive moisture. In the conditions of warm temperate climate there are signs of grain processes in the whole profile some aluminum on iron accumulation related to the partial displacement within the profile. The grain size distribution of samples taken from the barrels profiles and from the vessels fillings indicate that predominant fraction is in the sediment is the silt fraction the content of which is up to 50% of sediment. 25% of sediment and more may be clay. The sand fraction is characteristic for the surface samples in the profile and some vessels fillings. In the vertical profile of mounds we can observe slightly bigger fractions of the mechanical composition in the surface layers of burial mounds. The biggest content of organic matter is present in the level of fossil soil and the accumulation of calcium carbonate is in the illuvial level of the modern soil. Geochemical analysis indicate enrichment in copper, zinc and iron in the soil level from the bronze age and additionally phosphorus in the large part of burial mounds. In the vessels fillings in many cases increase in micro elements content exceeding the geohemical background was not. Similary in the vicinity of vessels and object and conclusion modern soil covering burial mounds is similar to the pozolyzed forest soil with few alluvial levels and illuvial and peridinous layers. Paleozole similar to the pozolyzed lichet chernozens is distinguished by the dark grey color of horizon and predominance of the humus accumulation. Its features are deep variation, gradual transition between levels, more light mechanical composition with increasing depth. In many tonight a haracter of soil forming processes is confirmed by numerous Crotovinas activity of soil farm. Fossil soils were created in conditions more humick than step ones probably in conditions of forest step in non forest areas where a lot of grass grow and organic matter was actively accumulated. In the soils the characteristic of leaching was were observed that mixture of silica is more abundant in the typical humus and dispersing of humus. These soils develop under middle vegetation in conditions of moderately warm climate with enough rainfall. In the mounds the seed fraction dominates which admixtures of clays and very fine grained sands. The mineral composition of burrows was also influenced by post depositional processes, pozolysation and the process of contributing to leaching clay components from the alluvial layer to washing then into the alluvial layer. Geochemical analysis indicate the diversity of content of micro and macro elements in burrows sediment. Geochemical enrichment show object places of burial of all vessels feeling which may also be happens. Highest phosphorus content was recorded in them. Some probably weapons or other accessories made of bronze were put into the grays with that. This is indicated by the contents of trace metals such as tin, zinc and copper. Very frequent elements of funeral rites of the kumar of culture was the insertion of ochre into the grave. It could be put in the vessels or fillets filled with the entire burial chamber. In the burial mounds number one at the depth of over two meters, iron contents was over 70,000 milligram per kilogram. Lack of preserved bones except burned out wood and other organic residues indicates the mineralization of organic components. Thank you for attention.