A REVISED RADIOCARBON CHRONOLOGY OF THE ACERAMIC SHELL MIDDEN OF RA'S AL-HAMRA 6 (MUSCAT, SULTANATE OF OMAN): IMPLICATION FOR OCCUPATIONAL SEQUENCE, MARINE RESERVOIR AGE, AND HUMAN MOBILITY

Zazzo Antoine; Munoz Olivia; Badel Emilie; Beguier Irene; Genchi Francesco; Marcucci Lapo Gianni

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A REVISED RADIOCARBON CHRONOLOGY OF THE ACERAMIC SHELL MIDDEN OF RA'S AL-HAMRA 6 (MUSCAT, SULTANATE OF OMAN): IMPLICATION FOR OCCUPATIONAL SEQUENCE, MARINE RESERVOIR AGE, AND HUMAN MOBILITY

机译：RA的Al-Hamra 6（Muscat，阿曼Muscat）的Aceramic Shell Midden的修订了Radiocarbon年代学：为职业序列，海洋水库年龄和人类流动的含义

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Ra's al-Hamra 6 (RH-6) is one of the earliest stratified archaeological sites along the eastern littoral of the Arabian Peninsula. This shell midden was radiocarbon dated to the 6th-5th millennium cal BC, but the majority of the dates were obtained before the advent of accelerator mass spectrometry (AMS) C-14 dating and suffer from large uncertainties. In addition, most of these dates were obtained on marine and mangrove shells and required correction for local variations from the global average marine C-14 reservoir age (MRA). This proved difficult because no consensus value exists for this period in the area. Recent excavations at RH-6 offered the opportunity to redate this important site in order to precisely determine its occupation history and later use as a graveyard, and establish the marine reservoir effect for this time period. Thirty-eight samples of charcoal, shells, and human bone apatite were selected for C-14 dating. Bayesian modeling of the C-14 dates suggests that the formation of the shell midden spanned similar to 1 millennium, between the mid-6th and the mid-5th millennium cal BC. Positive and consistent Delta R values were calculated throughout the entire sequence, ranging from 99 +/- 27 to 207 +/- 43 C-14 yr. At the beginning of the 4th millennium cal BC, RH-6 was used as a graveyard, as suggested by the C-14 dating of a shell in strict association with an individual buried at the surface of the site. C-14 dating of human bone apatite allowed us to calculate that 89% of this individual's diet derived from marine resources. This finding confirms previous observations showing the overwhelming presence of marine and mangrove-dwelling species in the faunal and charcoal assemblage, and implies a low mobility, or mobility restricted to the coast for this population during the 4th millennium cal BC.

机译：Ra的Al-Hamra 6（RH-6）是阿拉伯半岛东部沿东尔的最早分层考古遗址之一。这壳Midden是Radiocarbon，日期为6-5千年Cal BC，但在加速器质谱（AMS）C-14的出现之前获得了大部分日期在达到了大量的不确定性。此外，大多数这些日期都在海洋和红树林壳牌上获得，并要求对全球平均海洋C-14水库年龄（MRA）的局部变化进行纠正。这证明是困难的，因为该地区的这一时期没有存在共识价值。 RH-6最近的挖掘提供了改写这个重要网站的机会，以便精确地确定其职业历史，并以后用作墓地，并为这段时间内建立海洋水库效应。选择38个样品的木炭，壳和人骨磷灰石，用于C-14约会。 C-14日期的贝叶斯建模表明，壳体MIDDEN的形成类似于6日中期和第5届千年CAL BC之间的1毫升。在整个序列中计算阳性和一致的ΔR值，范围为99 +/- 27至207 +/- 43 C-14 YR。在第4毫升Cal BC的开始时，RH-6被用作墓地，如C-14壳体的C-14在埋藏在现场埋在地表的个人的关系中。 C-14人骨磷灰石的约会使我们能够计算出于海洋资源的饮食中的89％。这一发现证实了先前的观察结果，展示了粪便和木炭组合中的海洋和美洲红树住宅的压倒性，并意味着在第四颗千年Cal BC期间妨碍了普通的流动性，或限制在海岸的流动性。

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《Radiocarbon》 |2016年第2期|共13页
作者
Zazzo Antoine; Munoz Olivia; Badel Emilie; Beguier Irene; Genchi Francesco; Marcucci Lapo Gianni;
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作者单位

Sorbonne Univ Museum Natl Hist Nat Unite Mixte Rech Archeozool Archeobot Soc Prat &

CNRS CP 56 55 Rue Buffon F-75005 Paris France;

Univ Paris 1 Pantheon Sorbonne UMR 7041 Equipe Village Etat Proche &

Moyen Orient Maison Archeol &

Ethnol Archeol &

Sci Antiquite F-92023 Nanterre France;

Univ Paris 1 Pantheon Sorbonne UMR 7041 Equipe Village Etat Proche &

Moyen Orient Maison Archeol &

Ethnol Archeol &

Sci Antiquite F-92023 Nanterre France;

Serv Dept Archeol Calvados 9 Rue St Laurent BP 20520 F-14035 Caen 1 France;

Univ Bari Dipartimento Beni Culturali &

Sci Linguaggio Piazza Umberto I 1 I-70125 Bari Italy;

Univ Paris 1 Pantheon Sorbonne UMR 7041 Equipe Village Etat Proche &

Moyen Orient Maison Archeol &

Ethnol Archeol &

Sci Antiquite F-92023 Nanterre France;

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正文语种 eng
中图分类化学;
关键词
Eastern Arabian littoral; burial; sea-level change; mangrove; Bayesian modeling;

机译：东部阿拉伯人沿岸;埋葬;海平面变化;红树林;贝叶斯造型;

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2. Variability in the marine radiocarbon reservoir effect in Muscat (Sultanate of Oman) during the 4th millennium BC: reflection of taphonomy or environment? [J] . A. Zazzoa, O. Munoz, J.-F. Saliege, Journal of Archaeological Science . 2012,第7期

机译：公元前四千年期间，马斯喀特（阿曼苏丹国）海洋放射性碳储层效应的变化：反射是环境学还是环境？
3. Continuous marine radiocarbon reservoir calibration and the ~(13)C Suess effect in the Irish Sea: Results from the first multi-centennial shell-based marine master chronology [J] . Butler P.G., Scourse J.D., Richardson C.A., Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2009,第3a4期

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7. A Revised Radiocarbon Chronology of the Aceramic Shell Midden of Ra’s Al-Hamra 6 (Muscat, Sultanate of Oman): Implication For Occupational Sequence, Marine Reservoir Age, and Human Mobility [O] . Antoine Zazzo, Olivia Munoz, Emilie Badel, 2016

机译：Ra的Al-Hamra 6（Muscat，阿曼苏丹国Muscat）的Aceramic Shell Middend的修正radiocarbon年代学：为职业序列，海洋水库年龄和人类流动的含义

A REVISED RADIOCARBON CHRONOLOGY OF THE ACERAMIC SHELL MIDDEN OF RA'S AL-HAMRA 6 (MUSCAT, SULTANATE OF OMAN): IMPLICATION FOR OCCUPATIONAL SEQUENCE, MARINE RESERVOIR AGE, AND HUMAN MOBILITY

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