Department of Ethnology and Archaeology

ABSTRACTThis article discusses the absolute chronology of collective burials of the Trzciniec Cultural Circle communities of the Middle Bronze Age in East Central Europe. Based on Bayesian modeling of 91 accelerator mass spectrometry radiocarbon (AMS 14C) dates from 18 cemeteries, the practice of collective burying of individuals was linked to a period of 400–640 (95.4%) years, between 1830–1690 (95.4%) and 1320–1160 (95.4%) BC. Collective burials in mounds with both cremation and inhumation rites were found earliest in the upland zone regardless of grave structure type (mounded or flat). Bayesian modeling of 14C determinations suggests that this practice was being transmitted generally from the southeast to the northwest direction. Bayesian modeling of the dates from the largest cemetery in Żerniki Górne, Lesser Poland Upland, confirmed the duration of use of the necropolis as ca. 140–310 (95.4%) years. Further results show the partial contemporaneity of burials and allow formulati...

There is no consensus on the origins of Boykos, Hutsuls, and Lemkos, partly because of the scarceness of historical sources of information in the region. Documented information about Carpathian highlanders is virtually absent before the 14th century (Zakrevska 1997). Their ethnocultural identities are also not well established within the respective jurisdictions where these groups reside. Although in Slovakia Lemkos are considered a distinct ethnic minority, Lemkos, Boykos, and Hutsuls living in Ukraine are considered part of the Ukrainian nationality. In Poland, Lemkos only recently began to enjoy some ethnic recognition (Mihalasky 1997). Yet each group has its own linguistic dialect as well as distinctive cultural attributes, including a rich oral history, in which each group claims to have distinct ethnocultural roots (Chopovsky 2003; Domashevsky 2001).

Barrows play an important role in paleoenvironmental studies. This research, conducted on macromorphology (descriptive), micromorphology (thin-section), physical and chemical properties of a burial mound necropolis located in the western part of Ukraine (near Bukivna village), aimed to reconstruct the climatic conditions and landscape of the area during the Late Neolithic and Middle Bronze Ages, when they were erected. The analysis of pedogenic and post-depositional processes has made it possible to determine the evolution of soils beginning around 4000 BP. Three phases of change in vegetation, climate, and soil conditions have been distinguished. Between 6000 and 4200 BP, the brown forest soil formed at the beginning of Subboreal period. Later, the formation of chernozems (Chernozems) took place between 4200 and 3300 BP, chernozems (Chernozems) formed, at an increasing rate as meadow and meadow-forest which led to the continental climate spread through the area, while in the Forecarpahians forest areas their transformation into gray forest soils (Luvic Phaeozems) is visible, and podzolized brown soils (Dystric or Haplic Cambisols) developed about 150 BP in a cooler and much more humid climate conditions than were present in the beginning of the Subboreal period. From the present study it was concluded that post-depositional processes, such as podzolization, lessivage, and illimerization, change the original properties of soils, while others, like the activity of fauna, result in krotovinas filled with original humus, and makes it easier to recognize fossil soils.

The aim of this article is to view the spatial distribution of Upper Dniester Basin’s (Western Ukraine) barrows and to interpret their location principles. These monuments were often situated on the flattened summits of watershed ridges or hills. It appeared also that some of them were located on upper parts of gentle slopes of not more than 8° of inclination. Mounds appear within linear and group-linear arrangements and were rarely observed as clusters, while more specific adjustments to their location were dependant on local terrain morphology. Barrow alignments run along the elevated ridges, while clustered groups were situated in places where erosive indentations or denudation cavities prevented barrows from stretching in a linear pattern. It can be noted that during the spatial development of barrow alignments, more attention was paid to the intervisibility between the mounds, than to their visibility from other places in the landscape. The potential of observing at least one o...