scholarly journals Frequency of dental caries in children in the Early Iron Age and the Medieval populations from Ukraine

2017 ◽  
Vol 80 (4) ◽  
pp. 415-426 ◽  
Author(s):  
Nataliia Valentinovna Yanko ◽  
Andrij Vladislavovich Artemyev ◽  
Lyudmyla Fedorivna Kaskova

AbstractIn this paper we determine the caries frequency in children of the Early Iron Age (EIA) (the 9th - the 3d centuries BC) and the Medieval populations (the 8th - the beginning of the 15th century AD) from the Ukraine area, and compare the results with the data from several European populations who lived at the same time. The EIA is presented by 41 children skeletons, three of which were Cimmerian (the 9th - the 7th centuries BC) from the territory of contemporary Poltava region; 38 skulls from the territory of contemporary Poltava region and Crimea represented Scythian period (the 7th - the 3d centuries BC). Remains of 24 children from the Medieval populations were also examined, three of which were the ancient Hungarians from the Poltava region (the 8th - the 9th centuries AD), 6 Khazars from the Kharkiv region (the 8th - the 9th centuries), 1 child related the Old Rus culture from the Kyiv region (the 9th century), and 14 representatives of the nomadic populations in the Golden Horde period (the 13th - the beginning of the 15th century) from the Poltava and Zaporizhzhya regions. Taking in consideration the letter archaeobotanical studies we suggest that there were no major changes in the plants exploited during all the studied periods. The frequency of carious lesions in children from the Medieval populations (8.3% in individuals, 0.5% in deciduous teeth, and 0.4% in permanent teeth) is only slightly higher than those from the EIA period (2.4% in individuals and 0.2% in deciduous teeth). These indexes were not larger those of majority of European populations dated to the same historic period. Further isotopic, chemical and palaeobotanical studies of the additional sites, with sufficient sample sizes, allow us to learn so much more of the cariogenic factors in children of the past populations from the Ukraine area.

2018 ◽  
Vol 43 (1) ◽  
pp. 3-27
Author(s):  
Daniel Pioske

Over the past twenty years our understanding of Philistine Gath's history (Tell es-Safl) has been transformed by what has been revealed through the site's early Iron Age remains. But what has received much less attention is the effect these ruins have on how we read references to the location within the Hebrew Bible. The intent of this study is to draw on the archaeological evidence produced from Tell es-Safl as an interpretive lens by which to consider the biblical portrayal of the site rendered in the book of Samuel, where the material traces of more amicable associations between Gath and highland populations invite us to reconsider the city's depiction in this ancient literary work.


AmS-Skrifter ◽  
2021 ◽  
pp. 1-300
Author(s):  
Trond Løken

The ambition of this monograph is to analyse a limited number of topics regarding house types and thus social and economic change from the extensive material that came out of the archaeological excavation that took place at Forsandmoen (“Forsand plain”), Forsand municipality, Rogaland, Norway during the decade 1980–1990, as well as the years 1992, 1995 and 2007. The excavation was organised as an interdisciplinaryresearch project within archaeology, botany (palynological analysis from bogs and soils, macrofossil analysis) and phosphate analysis, conducted by staff from the Museum of Archaeology in Stavanger (as it was called until 2009, now part of the University of Stavanger). A large phosphate survey project had demarcaded a 20 ha settlement area, among which 9 ha were excavated using mechanical topsoil stripping to expose thehabitation traces at the top of the glaciofluvial outwash plain of Forsandmoen. A total of 248 houses could be identified by archaeological excavations, distributed among 17 house types. In addition, 26 partly excavated houses could not be classified into a type. The extensive house material comprises three types of longhouses, of which there are as many as 30–40 in number, as well as four other longhouse types, of which there are only 2–7 in number. There were nine other house types, comprising partly small dwelling houses and partly storage houses, of which there were 3–10 in number. Lastly, there are 63 of the smallest storage house, consisting of only four postholes in a square shape. A collection of 264 radiocarbon dates demonstrated that the settlement was established in the last part of the 15th century BC and faded out during the 7th–8th century AD, encompassing the Nordic Bronze Age and Early Iron Age. As a number of houses comprising four of the house types were excavated with the same methods in the same area by the same staff, it is a major goal of this monograph to analyse thoroughly the different featuresof the houses (postholes, wall remains, entrances, ditches, hearths, house-structure, find-distribution) and how they were combined and changed into the different house types through time. House material from different Norwegian areas as well as Sweden, Denmark, Germany and the Netherlands is included in comparative analyses to reveal connections within the Nordic area. Special attention has been given to theinterpretation of the location of activity areas in the dwelling and byre sections in the houses, as well as the life expectancy of the two main longhouse types. Based on these analyses, I have presented a synthesis in 13 phases of the development of the settlement from Bronze Age Period II to the Merovingian Period. This analysis shows that, from a restricted settlement consisting of one or two small farms in the Early BronzeAge, it increases slightly throughout the Late Bronze Age to 2–3 solitary farms to a significantly larger settlement consisting of 3–4 larger farms in the Pre-Roman Iron Age. From the beginning of the early Roman Iron Age, the settlement seems to increase to 8–9 even larger farms, and through the late Roman Iron Age, the settlement increases to 12–13 such farms, of which 6–7 farms are located so close together that they would seem to be a nucleated or village settlement. In the beginning of the Migration Period, there were 16–17 farms, each consisting of a dwelling/byre longhouse and a workshop, agglomerated in an area of 300 x 200 m where the farms are arranged in four E–W oriented rows. In addition, two farms were situated 140 m NE of the main settlement. At the transition to the Merovingian Period, radiocarbon dates show that all but two of the farms were suddenly abandoned. At the end of that period, the Forsandmoen settlement was completely abandoned. The abandonment could have been caused by a combination of circumstances such as overexploitation in agriculture, colder climate, the Plague of Justinian or the collapse of the redistributive chiefdom system due to the breakdown of the Roman Empire. The abrupt abandonment also coincides with a huge volcanic eruption or cosmic event that clouded the sun around the whole globe in AD 536–537. It is argued that the climatic effect on the agriculture at this latitude could induce such a serious famine that the settlement, in combination with the other possible causes, was virtually laid waste during the ensuing cold decade AD 537–546. 


Author(s):  
YU. V. BOLTRIK ◽  
E. E. FIALKO

This chapter focuses on Trakhtemirov, one of the most important ancient settlements of the Early Iron Age in the Ukraine. During the ancient period, the trade routes and caravans met at Trakhtemirov which was situated over the three crossing points of the Dneiper. Its location on the steep heights assured residents of Trakhtemirov security of settlement. On three sides it was protected by the course of the Dnieper while on the other side it was defended by the plateau of the pre-Dneiper elevation. The ancient Trakhtemirov city is located around 100 km below Kiev, on a peninsula which is jutted into the river from the west. Trakhtemirov in the Early Iron Age was important as it was the site of the Cossack capital of Ukraine. It was also the site of the most prestigious artefacts of the Scythian period and a site for various items of jewellery, tools and weaponry. The abundance of artefacts in Trakhtemirov suggests that the city is a central place among the scattered sites of the middle course of the Dneiper.


2019 ◽  
Vol 7 (2) ◽  
pp. 92-110

The archaeological landscape of the Lower Danube was changing with the importance of the Danube itself, which either became, or a cultural water¬shed, or an artery, connecting the ancient communities. In the Early Iron Age, it seems that the Danube did not become an invincible barrier for the spread of offensive weapons of Scythian origin. Moreover, Dobruja itself looks like a ter-ritory mastered by the Scythians, starting from the Archaic period. The Lower Danube group forms a separate “steppe” cultural assemblage together with the Lower Dniester, South Carpathian and South Danube groups, for which the spear became the main type of weapon. However, these preferences were re¬flected in the morphology of the Scythian akinakes. So, for this steppe or Dan-ube enclave, swords are more characteristic than daggers. Daggers are connected mainly with the forest-steppe part of the Carpathian-Dniester region and Transylvania. The warrior graves of the Lower Danube region mainly belong to the Classical Scythian period, while the only exception is related to the right bank of the Lower Danube. However, there are no burials with akinakai and even stray finds in Classical time outside the steppe.


2013 ◽  
Vol 7 (3) ◽  
pp. 181-183
Author(s):  
A Agarwal ◽  
P Gupta ◽  
M Goel ◽  
N Jindal ◽  
J Batra

ABSTRACT Odontomes arise as a result of an aberration in the tissues responsible for the formation of teeth. Though regarded as tumors or hamartomas in the past they are now usually regarded as variations in development of malformations. A 15 yr old female patient with complaint of swelling and mobility of upper anterior teeth diagnosed as complex Odontomes of anterior maxilla managed with enucleation. Odontomes are diagnosed in the second decade of life and are commonly associated with delayed eruption and displacement of related permanent teeth which is sometimes accompanied by retention of deciduous teeth and swelling. The treatment of the Odontomes is surgical removal and there is no expectancy of recurrence. Since both the ameloblastic odontoma and the ameloblastic fibro-odontoma bear great resemblance to the common Odontomes, particularly on the radiographs it is suggested that all Odontomes be sent for histopathological examination.


2009 ◽  
Vol 33 (4) ◽  
pp. 289-294 ◽  
Author(s):  
Vipin Arora ◽  
Pooja Arora ◽  
AK Munshi

Tooth derived cells are readily accessible and provide an easy and minimally invasive way to obtain and store stem cells for future use. Banking ones own tooth-derived stem cells is a reasonable and simple alternative to harvesting stem cells from other tissues. Obtaining stem cells from human exfoliated deciduous teeth (SHED) is simple and convenient, with little or no trauma. Every child loses primary teeth, which creates the perfect opportunity to recover and store this convenient source of stem cells – should they be needed to treat future injuries or ailments and presents a far better alternative to simply discarding the teeth or storing them as mementos from the past. Furthermore,using ones own stem cells poses few, if any, risks for developing immune reactions or rejection following transplantation and also eliminates the potential of contracting disease from donor cells. Stem cells can also be recovered from developing wisdom teeth and permanent teeth. Individuals have different opportunities at different stages of their life to bank these valuable cells. It is best to recover stem cells when a child is young and healthy and the cells are strong and proliferative. The purpose of this review is to discuss the present scenario as well as the technical details of tooth banking as related to SHED cells.


2018 ◽  
Vol 27 (2) ◽  
pp. 245-250
Author(s):  
O. D. Mogylov ◽  
S. V. Rudenko

The article is devoted to the publication of the materials of the settlement of the Early Iron Age near Ivanivka in the Tyasmyn river region. Archaeological reconnaissance here revealed the emergence of cultural strata, represented by animal bones, ceramic moldings and imported antique utensils, arrowheads, pins. The materials date back to the pre-Scythian and Scythian period: VIII—IV centuries BC.


2020 ◽  
Vol 72 (2) ◽  
Author(s):  
Valchak Sergey B. ◽  
Lysenko Sergey D. ◽  
Gorbol Nikolai Yu. ◽  
Razumov Sergey N. ◽  
Telnov Nikolai P. ◽  
...  

Two graves of the Pre-Scythian period (Chernogorovka culture) from barrow 1 of the “Rybkhoz” (“Fish farm”) group near Glinoe village, Slobodzeya district, on the left bank of the Lower Dniester are considered on the broad background of analogies. The issues of chronology and morphology of some categories of adornments are analyzed. Particular attention is drawn to burial 8 with two bronze temporal pendants. There are no analogies to these adornments in the materials of the Chernogorovka culture. The decorative endings of these pendants resemble the design of the backs of the eastern Mediterranean (“nodular”) fibulae, especially items with three spherical or biconical thickenings. Rings-pendants from burial 14 do not find complete matches among the adornments of the Chernogorovka culture. At the same time, these products are similar to adornments from contemporaneous North Caucasian sites due to their massiveness and non-closed ends. Both graves date back to the 9th – the first half of the 8th century BC.


Zephyrvs ◽  
2021 ◽  
Vol 87 ◽  
pp. 125-144
Author(s):  
Francisco B. Gomes

In the past few years, deeply colored black-appearing glass has garnered a growing interest in the context of research on Iron Age glass technology and trade. The numerous ‘black’ glass beads found in Early Iron Age contexts of Southern Portugal have not however been considered in this discussion, and they remain largely unsystematized. In this contribution, a typological survey of these objects is presented which highlights their unusual concentration in a well-delimited area of Southern Portugal and their relatively circumscribed chronological setting. This is particularly striking when compared with other groups of beads, namely blue beads of various types, which are much more widespread and long-lasting. The global position of these beads is also considered, with typological comparisons and the few available compositional data suggesting that they may be the product of Punic, and perhaps specifically Carthaginian trade with the Western Iberian Peninsula. Finally, the possible specific historic context in which these beads arrived in Southern Portugal is considered.  


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