PL
 |
EN
Preferencje help
Polish version English version Język
Widoczny [Schowaj] Abstrakt
Liczba wyników

Znaleziono wyników: 8

Liczba wyników na stronie
first rewind previous Strona / 1 next fast forward last
Wyniki wyszukiwania
help Sortuj według:

help Ogranicz wyniki do:
first rewind previous Strona / 1 next fast forward last
1
Content available remote The Neolithization of eastern Croatia and southern Transdanubia – lithic perspective
Klindžić R. Š., Kaczanowska M., Kozłowski J. K., Karavanić I.
Folia Quaternaria
|
2018
|
nr 86
159--189
EN
The objective of this paper is to show the complexity of Neolithization processes on the basis of lithic industries structure in eastern Croatia and southern Transdanubia. The location of major deposits of siliceous rocks is presented and the procurement systems of these rocks at the most important sites of the Starčevo Culture and of the LBK Formative Phase in the territories in question is discussed. The data obtained in the raw materials and techno-morphological analyses is compared with the taxonomic and socio-economic diversity of the Early Neolithic Cultures.
2
Content available remote The Mesolithic lithic industries of the eastern Adriatic zone
Kaczanowska M., Kozłowski J. K.
Folia Quaternaria
|
2018
|
nr 86
191--215
EN
In the Mesolithic, specific traits of the environment of the eastern Adriatic coast resulted in the emergence of a local cultural province, different from the Central Balkans and open to trans-Adriatic influences. This province was distinguished by the blending of three different cultural traditions: Epigravettian, Sauveterian, and Castelnovian.
3
Content available remote The evolution of chipped stone industries in the “Polgár Island” from the Middle Neolithic to the Early Copper Age
Kaczanowska M., Kozłowski J. K.
Folia Quaternaria
|
2016
|
nr 84
67--84
EN
“Polgár Island” is a natural elevation delimited by river banks; its flat area covers 70 sq.km The “Polgár Island” is of particular importance for the study of interregional contacts as raw materials deposits are absent in this territory. The settlement in the “Polgár Island” can be seen from the Middle Neolithic to the Early Copper Age (ALP I-IV, Late Neolithic and Tiszpolgár Culture). In this time-span changes in raw material supply, technology and organization of lithic production took place. In the Early Phase obsidian played the most important role, and contacts developed along the north-south axis. In the Late Neolithic horizon (Polgár-Csöszhálom-dűlő) the flow of obsidian was smaller, replaced by limnoquartzites. A major change in the systems of raw material supply occured at the beginning of the Copper Age, Simultaneously with changes in the direction of raw material supply, diachronic changes took place in the organization of lithic production.
4
Content available remote Chipped and ground stone implements from the Middle Neolithic site of Polgár 31 (north-east Hungary)
Kaczanowska M., Kozłowski J. K., Sümegi P.
Folia Quaternaria
|
2016
|
nr 84
5--66
EN
The site of Polgár 31 (Ferenci-hát) is situated on the left bank of the Upper Tisza, within the so-called “Polgár Island”. The site consists of single features dated at the Alföld Linear Pottery Culture (ALP) I-III, while the majority of features belong to the youngest phase (ALP IV) attached to the Bükk Culture. Our analysis focuses on both the chipped stone and the ground stone implements. The most important raw material used for the chipped stone industry of ALP IV phase was obsidian, followed by limno-hydroquartzites. Extra local raw materials played a minor role. Both in the case of obsidian as well as limnohydroquartzites on-site production was limited, while most artefacts were produced off-site. The structure of retouched tools shows that end-scrapers dominate slightly over marginally retouched blades. The most commonly exploited raw material in the ground stone industry were various types of rhyolites deriving from the areas 40 to 50 km north of the site. Among tools predominate implements related to food preparation such as a variety of grinding stones, pestles, grinders etc. As part of rituals these tools were destroyed. Sometimes the fragments were used for crushing mineral dyes. Both: fragments of ground stone as well as chipped stone tools occur also in the graves.
5
Content available remote Mesolithic occupations and environments on the Island of Ikaria, Aegean, Greece
Sampson A., Kaczanowska M., Kozłowski J. K., Athanassas C., Bassiakos Y., Liritzis I., Laskaris N., Tsermegas I.
Folia Quaternaria
|
2012
|
nr 80
1--87
EN
The most important Mesolithic site on the Island of Ikaria, Kerame 1, extends 80 m along the sloping edge of the cliff and is up to 40 m wide. The site is a sum of repeated sojourns of Mesolithic groups that had left behind concentrations of lithic artefacts, which were subsequently displaced by post-depositional agents, first of all by erosion. As a result, the site reveals now a large concentration of finds in Trenches E, C, and G. Moreover, post-depositional agents caused the destruction of permanent features such as the hearths associated with the various khsemenitsas, or — possibly — stone rings surrounding the dwelling structures. Only in trenches D, B and E the remains of a circular stone rings, probably around hearths, were registered. The lithic industry of Kerame 1 displays considerable similarity to the site of Maroulas on Kythnos; the techno-morphological differences are, probably, the effect of differing raw materials structure at Kerame 1 and at Maroulas. At Kerame 1, the distant interregional contacts and the influx of extralocal raw materials (documented by the flow of obsidian nodules from Melos and Yali) caused that production in a full cycle was carried out on-site. Thus, there was no specialization of lithic production, and unworked nodules of raw material were exploited in the particular social clusters in a full cycle, whose outcome were tools to be used by a given unit. Regretfully, because organic materials (also bones) have not been preserved we have no data to determine seasonality at Kerame l. Nevertheless, we can say with all certainty that Mesolithic groups visiting Kerame 1 were mobile, which is evidenced by the network of interregional contacts. The most noticeable similarity between Kerame 1 and Maroulas can be accounted for by the chronological closeness of the two sites. The AMS determinations from Maroulas concentrate in the first half of the 9th millenium cal. BC (Facorellis et a1. 2010). Similarly, the dates from obsidian dehydration from Kerame 1 (if their broad standard deviation is overlooked) correspond to the first half of the 9th millenium cal. BC.
6
Content available remote The formation of mammoth bone accumulation at the Gravettian site Kraków-Spadzista B+B1
Kalicki T., Kozłowski J. K., Krzemińska A., Sobczyk K., Wojtal P.
Folia Quaternaria
|
2007
|
nr 77
5-30
EN
The subject of this paper is sector B+B1 of the Upper Palaeolithic site Kraków-Spadzista. In this sector, situated on the rocky elevation above the Rudawa River valley in the loess deposit (layer 6), an accumulation of mammoth bones was partially excavated and provided some evidence of activities of Gravettian hunters (hearths, lithic artefacts, rare modified bones). The accumulation of mammoth bones is a result of several occupational episodes dated between 24,000 and 23,000 years BP; in every episode some mammoths were killed and butchered. Postdepositional factors, such as solifluction (forming a sequence of lobes), human and carnivore activities, and animal trampling disturbed the original structure of killing and butchering areas, particularly in the filling of the karstic depression in the bedrock. Some in situ structures have only been preserved on the platform surrounding the depression.
7
Content available remote Les origines de la recolonisation de la partie septentrionale de l'Europe centrale apres le Pleniglaciaire
Kozłowski J. K.
Folia Quaternaria
|
1999
|
nr 70
317-331
8
Content available remote An overview of the conference
Kobusiewicz M., Kozłowski J. K.
Folia Quaternaria
|
1999
|
nr 70
393-395
first rewind previous Strona / 1 next fast forward last
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.