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Journal ArticleDOI

Crisis in Context: The End of the Late Bronze Age in the Eastern Mediterranean

A. Bernard Knapp, +1 more
- 01 Jan 2016 - 
- Vol. 120, Iss: 1, pp 99
TLDR
The authors reviewed the current state of the archaeological and historical evidence and considered the coherence of climatic explanations and overprecise chronologies in attempting to place the "crisis" in context.
Abstract
Explanations for the Late Bronze Age crisis and collapse in the eastern Mediterranean are legion: migrations, predations by external forces, political struggles within dominant polities or system collapse among them, inequalities between centers and peripheries, climatic change and natural disasters, disease/plague. There has never been any overarching explanation to account for all the changes within and beyond the eastern Mediterranean, some of which occurred at different times from the mid to late 13th throughout the 12th centuries B.C.E. The ambiguity of the evidence—material, textual, climatic, chronological—and the differing contexts involved across the central-eastern Mediterranean make it difficult to disentangle background noise from boundary conditions and to distinguish cause from effect. Can we identify the protagonists of the crisis and related events? How useful are recent explanations that focus on climate and/or chronology in providing a better understanding of the crisis? This article reviews the current state of the archaeological and historical evidence and considers the coherence of climatic explanations and overprecise chronologies in attempting to place the “crisis” in context. There is no final solution: the human-induced Late Bronze Age “collapse” presents multiple material, social, and cultural realities that demand continuing, and collaborative, archaeological, historical, and scientific attention and interpretation. This article is available as open access on (AJA Online).

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References
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Journal ArticleDOI

Absolute age range of the Late Cypriot IIC Period on Cyprus

TL;DR: An absolute date range for the main Late Cypriot IIC period on Cyprus, from c. 1340-1315 BC to c. 1200 BC, is proposed in this article.
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Seasonality variations in the Central Mediterranean during climate change events in the Late Holocene

TL;DR: In this article, the authors identify events of high and low-detrital input to the Gulf of Taranto (Central Mediterranean Sea), anticipated to be linked to humid and dry conditions, respectively and, thereby, potentially reflecting seasonal contrasts.
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