Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.jas.2012.01.043 |
Variability in the marine radiocarbon reservoir effect in Muscat (Sultanate of Oman) during the 4th millennium BC: reflection of taphonomy or environment? | |
Zazzo, A.1; Munoz, O.2; Saliege, J-F.1; Moreau, C.3 | |
通讯作者 | Zazzo, A. |
来源期刊 | JOURNAL OF ARCHAEOLOGICAL SCIENCE
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ISSN | 0305-4403 |
EISSN | 1095-9238 |
出版年 | 2012 |
卷号 | 39期号:7页码:2559-2567 |
英文摘要 | Radiocarbon (C-14) dating of archaeological coastal sites in arid areas is challenging because of the relative rarity of datable terrestrial artefacts. Marine artefacts provide an abundant source of carbon, which is technically easy to date but radiocarbon dates need to be corrected for local variations from the global average marine C-14 reservoir age (Delta R). In archaeological sites, this is usually done by the comparison of the C-14 age measured between coeval pairs of terrestrial and marine samples that have no inbuilt age. Here, we present the results of a study that aims to determine the local C-14 marine reservoir effect (MRE) along the Eastern coast of the Arabic Peninsula during the 4th millennium BC, a period of important cultural, demographic and social changes in this region. Previous estimates of the MRE based on associated shells and charcoal vary by about 400 C-14 yr and this is a serious limitation to the establishment of a precise chronology in the area based on marine material. In order to maximize the chances to obtain contemporaneous terrestrial-marine pairs for a new assessment of the MRE in this region we dated charcoal, shells, fish and turtle bones as well as human bones found in three recently and carefully excavated graves from Ra’s al-Hamra RH5. A large variability was found between charcoals (up to 240 C-14 yr) and marine specimens (up to 785 C-14 yr) present in the same grave. This variability was attributed to inbuilt ages, diagenesis and possibly environmental factors although taphonomic processes cannot be excluded. We discarded the oldest charcoals and used the C-14 ages obtained on human apatite as a cut-off value to remove the marine outliers. Two out of the three graves provided terrestrial and marine assemblages which did not differ statistically and were used to calculate an average MRE of 645 +/- 40 C-14 yr (Delta R = 255 +/- 55 C-14 yr). This value is consistent with previous estimates based on the C-14 dating of marine sediments off Pakistan and suggests stability of the MRE in the Arabian Sea since the 4th millennium BC. (C) 2012 Elsevier Ltd. All rights reserved. |
英文关键词 | Radiocarbon dating Marine reservoir effect Diagenesis Inbuilt age Mangrove Sultanate of Oman |
类型 | Article |
语种 | 英语 |
国家 | France |
收录类别 | SCI-E ; SSCI ; AHCI |
WOS记录号 | WOS:000305849400063 |
WOS关键词 | AGE CALIBRATION ; ARABIAN SEA ; COASTAL ; CHRONOLOGY ; HOLOCENE ; CARBONATE ; MONSOON ; OCEAN ; DATES |
WOS类目 | Anthropology ; Archaeology ; Geosciences, Multidisciplinary |
WOS研究方向 | Anthropology ; Archaeology ; Geology |
来源机构 | French National Research Institute for Sustainable Development |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/173171 |
作者单位 | 1.Museum Natl Hist Nat, Dep EGB, CNRS, UMR 7209, F-75005 Paris, France; 2.Univ Paris 01, CNRS UMR 7041, F-92023 Nanterre, France; 3.CEA Saclay, UMS 2572, LMC14, F-91191 Gif Sur Yvette, France |
推荐引用方式 GB/T 7714 | Zazzo, A.,Munoz, O.,Saliege, J-F.,et al. Variability in the marine radiocarbon reservoir effect in Muscat (Sultanate of Oman) during the 4th millennium BC: reflection of taphonomy or environment?[J]. French National Research Institute for Sustainable Development,2012,39(7):2559-2567. |
APA | Zazzo, A.,Munoz, O.,Saliege, J-F.,&Moreau, C..(2012).Variability in the marine radiocarbon reservoir effect in Muscat (Sultanate of Oman) during the 4th millennium BC: reflection of taphonomy or environment?.JOURNAL OF ARCHAEOLOGICAL SCIENCE,39(7),2559-2567. |
MLA | Zazzo, A.,et al."Variability in the marine radiocarbon reservoir effect in Muscat (Sultanate of Oman) during the 4th millennium BC: reflection of taphonomy or environment?".JOURNAL OF ARCHAEOLOGICAL SCIENCE 39.7(2012):2559-2567. |
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