Erosion of archaeological sites: Quantifying the threat using optically stimulated luminescence and fallout isotopes

Although visible evidence shows that erosion has damaged many archaeological sites, especially when tilled, there has hitherto been scant attention to its quantitative assessment. Accordingly, the archaeology communities lack insight into whether long-term threats to the stability and integrity of s...

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Bibliographic Details
Main Authors: de Kort, J.-W (Author), Huisman, H. (Author), Ketterer, M.E (Author), Reimann, T. (Author), Schoorl, J.M (Author), van der Heiden, M. (Author), van Egmond, F. (Author), van Soest, M. (Author)
Format: Article
Language:English
Published: John Wiley and Sons Inc. 2019
Subjects:
OSL
Pu
Online Access:View Fulltext in Publisher
LEADER 02633nam a2200397Ia 4500
001 10.1002-gea.21716
008 220511s2019 CNT 000 0 und d
020 |a 08836353 (ISSN) 
245 1 0 |a Erosion of archaeological sites: Quantifying the threat using optically stimulated luminescence and fallout isotopes 
260 0 |b John Wiley and Sons Inc.  |c 2019 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1002/gea.21716 
520 3 |a Although visible evidence shows that erosion has damaged many archaeological sites, especially when tilled, there has hitherto been scant attention to its quantitative assessment. Accordingly, the archaeology communities lack insight into whether long-term threats to the stability and integrity of soils at these sites allow these cultural repositories to be preserved for future human generations. Of the techniques that are available to measure erosion rates, few have been tested on the timescales needed. We selected three archaeological sites with high expected erosion rates. We combined optically stimulated luminescence (OSL) dating with analyses of radioactive fallout isotope distributions to assess erosion patterns and rates. An age–depth representation of OSL single-aliquot results was developed to determine past erosion, and to identify stable land surfaces on centennial to millennia timescales. Fall-out isotopes of cesium (Cs) and plutonium (Pu) were suitable for shorter timescales: The 240Pu/239Pu ratios and a correlation between activities of 239+240Pu and 137Cs demonstrated the weapons testing fallout origin of these isotopes in the ~1952–1966 timeframe. Erosion rates in recent decades ranged from 2 to 6 mm/year on the studied sites. Our results indicate that erosion is not only tied to the past, but keeps on threatening archaeological sites. © 2018 The Authors. Geoarchaeology Published by Wiley Periodicals, Inc. 
650 0 4 |a 137Cs 
650 0 4 |a archaeological evidence 
650 0 4 |a cesium 
650 0 4 |a erosion 
650 0 4 |a fallout 
650 0 4 |a fallout 
650 0 4 |a geochronology 
650 0 4 |a isotopic composition 
650 0 4 |a luminescence dating 
650 0 4 |a nuclear explosion 
650 0 4 |a optical method 
650 0 4 |a OSL 
650 0 4 |a plutonism 
650 0 4 |a Pu 
650 0 4 |a quantitative analysis 
700 1 |a de Kort, J.-W.  |e author 
700 1 |a Huisman, H.  |e author 
700 1 |a Ketterer, M.E.  |e author 
700 1 |a Reimann, T.  |e author 
700 1 |a Schoorl, J.M.  |e author 
700 1 |a van der Heiden, M.  |e author 
700 1 |a van Egmond, F.  |e author 
700 1 |a van Soest, M.  |e author 
773 |t Geoarchaeology