Anatolian Chronology and Terminology

Author(s):  
Jak Yakar

This article discusses dating techniques and the necessity of working with both material and textual evidence to develop secure chronologies for the rather daunting range of Anatolian peoples and sites. It analyzes the comparative dates and phases of Neolithic, Chalcolithic, Early Bronze Age, Modern Bronze Age, Late Bronze Age, and Iron Age sites.

2013 ◽  
Vol 1 (1) ◽  
pp. 25 ◽  
Author(s):  
Joachim Lutz ◽  
Ernst Pernicka

The rich copper ore deposits in the Eastern Alps have long been considered as important sources for copper in prehistoric Central Europe. It is, however, not so clear which role each deposit played. To evaluate the amount of prehistoric copper production of the various mining regions it was attempted to link prehistoric metal artefacts with copper ores based on the geochemical characteristics of the ore deposits that have been exploited in ancient times. More than 120 ore samples from the well known mining districts Mitterberg, Viehhofen, Kitzbühel and Schwaz/Brixlegg have been analysed so far (lead isotope ratios, trace elements). Furthermore, about 730 archaeological copper/bronze artifacts were investigated and analysed. These results were combined with analytical data generated by previous archaeometallurgical projects in order to compile a substantial database for comparative studies. In the Early Bronze Age, most metal artifacts were made of copper or bronze with fahlore impurity patterns and most finds from this period match excellently the fahlore deposits in Schwaz and Brixlegg. At the end of the Early Bronze Age, a new variety of copper with lower concentrations of impurities appeared. The impurity patterns of these finds match the ores from the Mitterberg district. In the Middle Bronze Age, this variety of copper Dominated while in the Late Bronze Age fahlores from Schwaz and Brixlegg experienced a comeback. The reason for this may be a decline of the chalcopyrite mines or a rising demand for copper which could not be covered by the chalcopyrite mines alone. The finds of the Early Iron Age are of similar composition and continue the traditions of the Late Bronze Age.


Radiocarbon ◽  
2015 ◽  
Vol 57 (2) ◽  
pp. 217-235 ◽  
Author(s):  
Dafna Langgut ◽  
Israel Finkelstein ◽  
Thomas Litt ◽  
Frank Harald Neumann ◽  
Mordechai Stein

This article presents the role of climate fluctuations in shaping southern Levantine human history from 3600 to 600 BCE (the Bronze and Iron Ages) as evidenced in palynological studies. This time interval is critical in the history of the region; it includes two phases of rise and decline of urban life, organization of the first territorial kingdoms, and domination of the area by great Ancient Near Eastern empires. The study is based on a comparison of several fossil pollen records that span a north-south transect of 220 km along the southern Levant: Birkat Ram in the northern Golan Heights, Sea of Galilee, and Ein Feshkha and Ze'elim Gully both on the western shore of the Dead Sea. The vegetation history and its climatic implications are as follows: during the Early Bronze Age I (∼3600–3000 BCE) climate conditions were wet; a minor reduction in humidity was documented during the Early Bronze Age II–III (∼3000–2500 BCE). The Intermediate Bronze Age (∼2500–1950 BCE) was characterized by moderate climate conditions, however, since ∼2000 BCE and during the Middle Bronze Age I (∼1950–1750 BCE) drier climate conditions were prevalent, while the Middle Bronze Age II–III (∼1750–1550 BCE) was comparably wet. Humid conditions continued in the early phases of the Late Bronze Age, while towards the end of the period and down to ∼1100 BCE the area features the driest climate conditions in the timespan reported here; this observation is based on the dramatic decrease in arboreal vegetation. During the period of ∼1100–750 BCE, which covers most of the Iron Age I (∼1150–950 BCE) and the Iron Age IIA (∼950–780 BCE), an increase in Mediterranean trees was documented, representing wetter climate conditions, which followed the severe dry phase of the end of the Late Bronze Age. The decrease in arboreal percentages, which characterize the Iron Age IIB (∼780–680 BCE) and Iron Age IIC (∼680–586 BCE), could have been caused by anthropogenic activity and/or might have derived from slightly drier climate conditions. Variations in the distribution of cultivated olive trees along the different periods resulted from human preference and/or changes in the available moisture.


1969 ◽  
Vol 49 (1) ◽  
pp. 22-29 ◽  
Author(s):  
C. B. Burgess

SummaryThe paper pleads for an end to persistent misuse of the traditional ‘Three Age’ terminology which still governs the Irish British Bronze Age, and for acceptance of work of the past decade which has either been ignored or misunderstood. Uniform terms of reference are needed, fitted to the new attitudes. Hawkes's Scheme of 1960 provides a framework for this, and is summarized. The Early, Middle, and Late divisions now have a techno-typological, rather than cultural, basis.Traditional cultural and ceramic concepts, based on typology, have resisted changes demanded by a new emphasis on the evidence of associated finds. The various Urn forms and the Deverel—Rimbury complex are particularly relevant here. Associations of Urns, and the few available C14 dates, are examined to demonstrate their existence in the Early Bronze Age, but, because of a remarkable ritual break at c. 1400, not in the Middle Bronze Age, let alone the Late Bronze Age. Similarly, Deverel—Rimbury is now Middle Bronze Age, not Late Bronze Age, its position after c. 1000 uncertain. Since much in our Iron Age is now thought indigenous, already apparent in Deverel—Rimbury, an awkward Late Bronze Age gap is opened up, apparently devoid of settlements and pottery. But much nominally Iron Age material may prove to be Late Bronze Age. There is a need for many more C14 dates to clarify these problems.


Author(s):  
Mikhail Krivosheev ◽  
Vladimir Moiseev

In 2018, Kurgan 2 of Gvardeyskiye 3 Kurgany (the 3rd Gvardeiskiy Kurgans) in the Nadterechny District of the Chechen Republic was studied. In the result, nine burials were found in the Kurgan which was created during the Early Bronze Age and continued to be used in the course of the Middle and Late Bronze Age. However, the three most recent burials date back to the Early Iron Age period. The burials were localized inside the existing embankment and formed a compact group. In two cases, the burial type was not identified; nevertheless in one case, the burial was constructed in a catacomb. The grave goods are mainly presented by ceramic vessels from the workshops of the sedentary population from the foothill area of Central and Eastern North Caucasus regions. The conclusion was made that the investigated Kurgans were left by the nomadic North Caucasian steppes population of the 3rd–1st centuries BC due to the feature analysis of the Early Iron Age burial complexes.


Radiocarbon ◽  
1984 ◽  
Vol 26 (3) ◽  
pp. 297-366 ◽  
Author(s):  
James M Weinstein

Radiocarbon dating provides the principal chronometric data for the Middle and Upper Palaeolithic, Epipalaeolithic, and Chalcolithic periods in the southern Levant. It is a secondary source of dating evidence for the Early Bronze age, when archaeological correlations with Syria and especially Egypt become available. For the Middle and Late Bronze age, Iron age, Persian, Hellenistic, Roman, and Byzantine periods, 14C dating has only limited value because the technique is less precise than the normally available archaeologic and historic materials.


1991 ◽  
Vol 17 (1) ◽  
pp. 39-52 ◽  
Author(s):  
Stephen Carter ◽  
Richard Tipping

Summary A concentration of archaeological features at Achnasavil, Carradale, which has been recorded since 1985, is being rapidly destroyed by river erosion. Limited excavations were carried out in 1991 in order to date and characterise the nature of the site. Four periods of activity have been identified: cultivation in the Neolithic period; an occupation in the early Bronze Age; a domestic settlement in the late Bronze Age; and an Iron Age occupation. A programme of morphological mapping and dating of valley floor terraces in lower Carradale showed that the present day flood plain of the Carra Water was created by the early Neolithic period and the morphology of the valley floor has changed little since that time.


Author(s):  
John K. Papadopoulos

This paper begins with an overview of the bronze headbands from the prehistoric (Late Bronze to Early Iron Age) burial tumulus of Lofkënd in Albania, which were found among the richest tombs of the cemetery, all of them of young females or children. It is argued that these individuals represent a class of the special dead, those who have not attained a critical rite de passage: marriage. In their funerary attire these individuals go to the grave as brides, married to death. The significance of the Lofkënd headbands is reviewed, as is their shape and decoration, but it is their context that contributes to a better understanding of Aegean examples, including the many bronze, gold, and silver headbands found in tombs from the Early Bronze Age through the Early Iron Age, as well as those dedicated as votive offerings in sanctuaries. In addition to discussing the evidence for headbands in the Aegean and much of southeast Europe, this paper also attempts to uncover the word used in this early period in Greece for these distinctive items of personal ornament. In memory of Berit Wells.


Radiocarbon ◽  
2021 ◽  
pp. 1-19
Author(s):  
Federico Manuelli ◽  
Cristiano Vignola ◽  
Fabio Marzaioli ◽  
Isabella Passariello ◽  
Filippo Terrasi

ABSTRACT The Iron Age chronology at Arslantepe is the result of the interpretation of Luwian hieroglyphic inscriptions and archaeological data coming from the site and its surrounding region. A new round of investigations of the Iron Age levels has been conducted at the site over the last 10 years. Preliminary results allowed the combination of the archaeological sequence with the historical events that extended from the collapse of the Late Bronze Age empires to the formation and development of the new Iron Age kingdoms. The integration into this picture of a new set of radiocarbon (14C) dates is aimed at establishing a more solid local chronology. High precision 14C dating by accelerator mass spectrometry (AMS) and its correlation with archaeobotanical analysis and stratigraphic data are presented here with the purpose of improving our knowledge of the site’s history and to build a reliable absolute chronology of the Iron Age. The results show that the earliest level of the sequence dates to ca. the mid-13th century BC, implying that the site started developing a new set of relationships with the Levant already before the breakdown of the Hittite empire, entailing important historical implications for the Syro-Anatolian region at the end of the 2nd millennium BC.


2021 ◽  
Vol 0 (0) ◽  
Author(s):  
Arne Verbrugge ◽  
Maaike Groot ◽  
Koen Deforce ◽  
Guy De Mulder ◽  
Wouter Van der Meer ◽  
...  

Abstract Archaeological research at Aalst – Siesegemkouter revealed several pits within a Middle to Late Bronze Age settlement. Most of them hardly contained any artefacts, but one exception showed a structured stratigraphy with an abundance of finds, including a large amount of shattered pottery, charcoal and calcined animal bone. The study of this assemblage, and comparison with two other pits showing similarities, provides strong indications of a closing deposit or another type of ‘site maintenance practice’. In the Low Countries, comparable contexts generally date from the Iron Age, suggesting that the finds from Aalst – Siesegemkouter represent early forerunners of this ritual practice. On top of this early date, the large volume of cremated animal bone represents an almost unique characteristic for which, until now, parallels from the Metal Ages have hardly been found, even on a Northwestern European scale. In general, the role played by organic remains in ritual contexts from these periods and regions is poorly understood, often due to bad preservation conditions or the lack of a multidisciplinary approach.


Author(s):  
Silvia Albizuri ◽  
Aurora Grandal-d’Anglade ◽  
Julià Maroto ◽  
Mònica Oliva ◽  
Alba Rodríguez ◽  
...  

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