Arid
DOI10.1016/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
ISSN0305-4403
EISSN1095-9238
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
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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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