紀元前1700~1400年のエーゲ海後期青銅時代の年代表
Sturt W Manning1, Christopher Bronk Ramsey, Walter Kutschera
1Department of Classics, Cornell University, 120 Goldwin Smith Hall, Ithaca, NY 14853-3201, USA. sm456@cornell.edu
まとめ
放射性炭素年代測定により,サントリーニの噴火は,紀元前17世紀後半に起こったことが示されています. このエーゲー海の後期青銅時代の段階の改訂された年代順は,それらを100年延長し,地域の歴史的相関に影響を及ぼします.
科学分野:
- 考古学科学 考古学科学とは
- 放射性炭素年代測定法による年代測定
- 青銅器時代の年代表
背景:
- エーゲ海銅器時代の正確な年代を確立することは,地域間の相互作用を理解するために極めて重要です.
- 従来の年代測定法により,ミノア紀後期IA,IB,IIなどの文化段階のタイムラインが確立されました.
- サントリーニ (テラ) の噴火は,潜在的な時間的なマーカーを持つ重要なパレオ環境イベントです.
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