‘Carantanian / Köttlach’ jewellery from southwest Slovakia and from the other parts of the Carpathian Basin. In the Slovak and Hungarian archaeological literature, a small group of early medieval jewellery from southwest Slovakia was labelled as being of ‘Carantanian / Köttlach’ provenance, meaning that it originated from Eastern Alps region (today’s Austria and Slovenia). The goal of the article is a revision of the issue of provenance in the context of analogous finds from Moravia and the Carpathian Basin (i.e. today’s Hungary, western Romania and northeastern Croatia). The provenenace from the Eastern Alps region can be confirmed in the case of several Slovak finds only, the others are of local origin. Also, from the point of view of chronology, we are dealing with a relatively heterogenous group of jewellery, with a date-range from the turn of the 8th-9th centuries to the 11th century. The author tries to demonstrate that the argument in the middle of the 20th century and later about the ‘influences from the Eastern Alps region’ was dependent on the state of archaeological research at that time. It was a viewpoint that over-emphasised the importance of early medieval ‘Köttlach culture’ in Eastern Alps region, especially for the spreading of some jewellery types to other regions of middle and southeastern Europe., Šimon Ungerman., and Obsahuje seznam literatury
The third and final season of excavation on Pod Hradem Cave (Moravian Karst) reached bedrock at a maximum depth of 3.5 metres, although the bedrock in this part of the cave represents a very steeply sloping wall rather than the cave floor. Radiocarbon dates indicate that the basal layers in this part of the cave were deposited during the late Middle Palaeolithic period. The finding of amber and shell in layer 11 represents a curious discovery, but there is a possibility that these objects represent an intrusion from a different archaeological context., Ladislav Nejman, Lukáš Kučera, Petr Škrdla, Lenka Lisá, Šárka Hladilová, Miroslav Králík, Rachel Wood, Miriam Nývltová Fišáková, Duncan Wright, Marjorie E. Sullivan, Philip Hughes., and Obsahuje seznam literatury
In the southern part of the O´swi˛ecim Basin, in the Ko´nczyce Wielkie gravel-pit, we can find outcrops of Quaternary deposits with varied geological histories. The lower fluvial sequence is covered with glacigenic sediments. The glacigenic deposits occurring below the Brunhes-Matuyama boundary and interglacial sediments are older than the Cromerian Complex. This ice-sheet advance, in its maximum extent in southern Poland, is correlated with the Günz, i.e. pre-Cromerian glaciation in Western Europe. Cultural material was located within fluvial sands with fine-grained gravels, below a layer of diamikton – interpreted as till – and underneath the boulder pavement – an equivalent of diamikton. Raw materials inventory include local flint and hornstone, foreign flint, hornstone, quartzite, opalite, gneiss granite. Among the artifacts are macrolithic and microlithic cores, flakes and tools. The pebbles, flakes and microlithic-flakes were base for making the tools., Eugeniusz Foltyn ... [et al.]., and Obsahuje seznam literatury
The article presents visualization options for archaeological sites employing a manual GPS receiver and a methodology for creating maps on the basis of surface finds using the MapSource program. Sophisticated analytical databases make it possible to examine the distribution and spatial relationships of different types of archaeological finds. Spatial data from the analytical database of MapSource were treated using open source statistical package R., Martin Kuča, Petr Matějec, Lubomír Prokeš., and Obsahuje seznam literatury
1_ Analysis of chipped stone industry from Kopčany and Brehov (Slovakia). The fl ake stone assemblages (and other assemblages) which were discovered during the excavation of two archaeological sites in Eastern Slovakia – Zemplínske Kopčany and Brehov were analysed. Seventeen stone artefacts were found in object No. 24A-D/1974 at Zemplínske Kopčany. Obsidian stone, which is a local raw material, occurs at a higher frequency than imported raw materials – Jurassic fl int “G” and basalt. With the exception of two blanks (cores), the assemblage consists of fi nished tools, most of which were made on blades. Other tools present include two fl ake scrapers and a blunt drill made of Jurassic fl int “G”. One obsidian core is lightly reduced and the second obsidian core has a pyramidal shape. The remainder of the Zemplínske Kopčany assemblage includes ten fi nished products made of local (sedimentary rocks) and imported raw material (amphibolite?). Whetstones are most common and axes are less numerous. The assemblage also includes a wedge, a fragment of an axe-hammer, a globular pestle and conical byproducts from axe-hammer production., 2_ Local raw materials were used at Brehov. The local obsidian dominates and other stone materials are present in small proportions. The typological character of the fl ake industries is also different. Flakes account for 68 % of the artefacts and blades 25 %. Specifi c artefacts are the „łuszcznie“ (“Splitter” in German) though to have been used as chisels or cutting tools. The cores are very small and lightly reduced. One pebble with negative scars and one drill (borer) are also present. Other artefacts include a shaft of a fl at axe made of local hornstone and a fragment of an unfi nished granodiorite axe-hammer with a hole drilled in the middle (possibly originating from the High Tatras?). The analyzed assemblages are compared with assemblages from other Baden Culture sites in Slovakia and in particular to those from the Malopolskie Voivodship. The analyzed artefacts from Zemplínske Kopčany and Brehov correspond to two phases in the development of the Baden Culture. The older phase has stronger affi nities to the Funnel Beaker Culture, and in the case of the Brehov site, to a younger phase, which is parallel with the Pleszow-Zesławice group in the Malopolskie Voivodship., Marián Soják., and Obsahuje seznam literaruty
This arčcicle present analysis of a teat number of palaeobotanic samples from 13 historic plots, archaeologiccally excavated 1983 - 1992 in the town of Brno. On this outstandingly large archaeobtanic material changes of the pectrum of plant remains were reviewed for the high medieval ages (and Postmedieval period). For the first time in the Czech Republic this large number of sampled featrues (mainly cesspits) enabled to conclusively monitor the vaying importance of certain utility plant species during a long time span. Also changes in accompaying weed vegetation, icnicating the origins and agrotechniques of cultivated plants were observed. Spectrum of the local synanthrope vegetation fefelct improving hygienic situation within the inbuilt area of Brno town. Timbre/charcoal analysis consclusively refelcts variable sources of wood/ charcoal for the medieval (Postmedieval) town., Petr Kočár, Romana Kočárová, Emanuel Opravil, Rudolf Procházka., and Obsahuje seznam literatury
Častá změna podnázvu, Cizojazyčné soub. názvy do r. 1956, Od r. 1953 Praha : ČSAV, Od r. 1966 Praha : Academia, and 1992 Praha : Archeologický úst. ČSAV
Lase Induced Brakdown Spectroscopy (LIBS) and Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) were utilized for microspatian nallyses of a fossil bear (Ursus arctos) tooth dentine. The distribution of selected trace elemnts (Sr, Ba, Fe) was measured on a 26 mm x 15 mm large and 3 mm thick transversal cross section of canine tooth, The Na and Mg content together with the distribution of matrix elemnts (Ca, P) was aslo monitored within this area. It is shown that LIBS, similarly to LA-ICP-MS can be successfully utilized for fast, spatially-resolved analysis of fossi teeth samples. Rate of Sr and Ca, Sr and Ba tracers were recognized and it is possible to say, thet these elemnts are changing its concentration in according to the seasonal increments of dentine. The concetration is lower in winter, when the bear is in his hibernation, contrary to summe, which is affuent for its substances. Secondly,concentration of Sr. shows us a seasonal migration between the place of hibernating and territory where bear searched for feed. From measurement of concentrations it is possible to claim, that the bear was hunted in his season of searching for feed, when he was ensuring his fat reserfe for winter. From archaeological pint of iew, on the base of these measurements it was possible to reconstract the ehtology of the fossil brown bear, i.e the nutrition, health and migration., Miriam Nývltová Fišáková ... [et al.]., and Obsahuje seznam literatury