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DOI10.1016/j.quascirev.2019.02.021
Can we detect centennial sea-level variations over the last three thousand years in Israeli archaeological records?
Dean S.; Horton B.P.; Evelpidou N.; Cahill N.; Spada G.; Sivan D.
发表日期2019
ISSN0277-3791
起始页码125
结束页码135
卷号210
英文摘要Archaeological remains are valuable relative sea-level (RSL) indicators in Israel, a tectonically stable coast with minor isostatic inputs. Previous research has used archaeological indicators to argue for centennial sea-level fluctuations. Here, we place archaeological indicators in a quality-controlled dataset where all indicators have consistently calculated vertical and chronological uncertainties, and we subject the data to statistical analysis. We combine the archaeological data with bio-construction data from Dendropoma petraeum colonial vermetids. The final dataset consists of 99 relative sea-level index points and 12 limiting points from the last 4000 a. The temporal distribution of the index points is uneven; Israel has only four index points before 2000 a BP. We apply an Errors-In-Variables Integrated Gaussian Process (EIV IGP) to the index points to model the evolution of RSL. Results show RSL in Israel rose from −0.8 ± 0.5 m at ∼2750 a BP (Iron Age) to 0.0 ± 0.1 m by ∼1850 a BP (Roman period) at 0.8 mm/a, and continued rising to 0.1 ± 0.1 m until ∼1600 a BP (Byzantine Period). RSL then fell to −0.3 ± 0.1 m by 0.5 mm/a until ∼650 a BP (Late Arab period), before returning to present levels at a rate of 0.4 mm/a. The re-assessed Israeli record supports centennial-scale RSL fluctuations during the last 3000 a BP, although the magnitude of the RSL fall during the last 2000 a BP is 50% less. The new Israel RSL record demonstrates correspondence with regional climate proxies. This quality-controlled Israeli RSL dataset can serve as a reference for comparisons with other sea-level records from the Eastern Mediterranean. © 2019 Elsevier Ltd
英文关键词Eastern Mediterranean; Israel; Late Holocene; Maritime archaeology; Middle East; Sea level changes
语种英语
scopus关键词Glacial geology; Quality control; Uncertainty analysis; Eastern Mediterranean; Israel; Late Holocene; Maritime archaeology; Middle East; Sealevel change; Sea level; archaeological evidence; archaeology; biochronology; data set; Holocene; proxy climate record; sea level change; snail; statistical analysis; temporal distribution; temporal variation; uncertainty analysis; Israel; Mediterranean Sea; Mediterranean Sea (East); Dendropoma petraeum; Vermetidae
来源期刊Quaternary Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/151973
作者单位Dept. of Maritime Civilizations, L. Charney School of Marine Sciences and The Leon Recanati Institute for Maritime Studies, University of Haifa, Haifa, 3498838, Israel; Earth Observatory of Singapore, Nanyang Technological University, Singapore, 639798, Singapore; Asian School of the Environment, Nanyang Technological University, Singapore, 639798, Singapore; National & Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Greece; Department of Mathematics and Statistics, Maynooth University, Kildare, Ireland; Dipartimento di Scienze Pure e Applicate (DiSPeA), Urbino University ‘’Carlo Bo’’, Via Santa Chiara, 27, Urbino, PU I-61029, Italy
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Dean S.,Horton B.P.,Evelpidou N.,et al. Can we detect centennial sea-level variations over the last three thousand years in Israeli archaeological records?[J],2019,210.
APA Dean S.,Horton B.P.,Evelpidou N.,Cahill N.,Spada G.,&Sivan D..(2019).Can we detect centennial sea-level variations over the last three thousand years in Israeli archaeological records?.Quaternary Science Reviews,210.
MLA Dean S.,et al."Can we detect centennial sea-level variations over the last three thousand years in Israeli archaeological records?".Quaternary Science Reviews 210(2019).
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