Cited by 247Archaeology and ancient environmental studiesAncient Egypt and ArchaeologyTree-ring climate responses

Radiocarbon-Based Chronology for Dynastic Egypt

Ramsey, Christopher Bronk, Dee, Michael W., Rowland, Joanne M., Higham, Thomas F. G., Harris, Stephen A., Brock, Fiona, Quiles, Anita, Wild, Eva M. +2 more·2010·Science

Abstract

Date with the Pharaohs: Ancient Egypt dominated the Mediterranean world for several thousand years. However, the absolute chronology of this civilization has been uncertain, even though the sequence of rulers is well documented. Bronk Ramsey et al. (p. 1554 ; see the Perspective by Bruins ) now provide a detailed radiocarbon-based record using more than 200 samples that spans much of this time and reduces uncertainties in some cases to less than 20 years. To avoid artifacts, the authors dated only short-lived plant remains from known contexts (i.e., that were associated with specific reigns). They then used the known reign lengths as a further constraint to obtain a final chronology. The final dates agree most closely with the previous older chronology but force some revisions to the timing of events in the Old Kingdom, the period in the third millennium B.C.E. when Egypt attained its first continuous peak of civilization.

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Crossref · 10.1126/science.1189395

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  • Class 1 dates included samples on short-lived plant remains and terrestrial avian eggshell, all of which have been shown to produce consistent and reliable ages in the Pacific relative to the target event.

    “Class 1 dates included samples on short-lived plant remains (e.g., twig charcoal or wood, bark, seeds, leaves) and terrestrial avian eggshell, all of which have been shown to produce consistent and reliable ages in the Pacific relative to the target event, i.e., human activity (4, 6, 7, 32).”
  • The precise dendro-14C-based timescale enables a robust historical synthesis of Ancient Near Eastern civilization in the earlier second millennium BCE; in particular, it facilitates comparison with the coherent historical and 14C-based timescale recently available from Egypt.

    “Our precise dendro-14C-based timescale enables a robust historical synthesis of Ancient Near Eastern civilization in the earlier second millennium BCE; in particular, it facilitates comparison with the coherent historical and 14C-based timescale recently available from Egypt [50].”
  • The end of the EB III cultural horizon is traditionally seen as contemporaneous with the reign of Pepi I, variously dated by Egyptologists to 2321-2287 BC or 2289-2255 BC, and recently by 14C to 2399-2310 BC (1σ) or 2389-2349 BC (2σ).

    “The end of the EB III cultural horizon is traditionally seen as contemporaneous with the reign of Pepi I (de Miroschedji 2012), variously dated by Egyptologists to 2321-2287 BC (Shaw 2000) or 2289-2255 BC (Baines and Malek 1980), and recently by 14 C to 2399-2310 BC ( 1σ) or 2389-2349 BC (2σ) (Bronk Ramsey et al. 2010).”
  • Bayesian modelling can generate decadal or annual precision.

    “Bayesian modelling can generate this sort of precision (Bronk Ramsey et al. 2010; Dee et al. 2013)”

    From Radiocarbon dating and the Naqada relative chronology (2014) · cites this paper as Bronk Ramsey et al. 2010

  • The growth period of tree rings in central and northern Europe and northern America that comprise the Holocene IntCal record is spring through summer, whereas many plants in the Mediterranean and Near East grow in winter to early summer.

    “An example of the latter is the difference between the growth period of tree rings in central and northern Europe and northern America that comprise the Holocene IntCal record (spring through summer), versus those of many plants in the Mediterranean and Near East (winter to early summer)5–8,10.”

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Research works printed but not linked: 3

  1. K. A. Kitchen in ( 5 ) pp. 163–171.
  2. Franke D., Zur Chronologie des Mittleren Reiches (12. – 18. Dynastie). Teil I: Die 12. Dynastie. Orientalia 57, 113 (1988).
  3. M. Bietak F. Höflmayer in The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium BC III M. Bietak E. Czerny Eds. (Verlag der Österreichischen Akademie der Wissenschaften Vienna 2007) pp. 13–23. · DOI

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Authors
Ramsey, C. B., Dee, M. W., Rowland, J. M., Higham, T. F. G., Harris, S. A., Brock, F., Quiles, A., Wild, E. M., Marcus, E. S., & Shortland, A. J.
Affiliations
  • University of Oxford (GB)
  • Laboratoire de Mesure du Carbone 14, bat 450 Porte 4E, Commissariat à l’Energie Atomique (CEA)–Saclay, France-Université Paris VII-Diderot, 91191 Gif-Sur-Yvette, France.
  • University of Vienna (AT)
  • University of Haifa (IL)
  • Cranfield University (GB)
Corresponding author
Ramsey, Christopher Bronk
Venue
Science
Published
2010-06-18
Volume
328
Issue
5985
Pages
1554-1557
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2032787368
Cited by
246
References
27
Citations by year
2025: 13 · 2024: 13 · 2023: 17 · 2022: 17 · 2021: 14 · 2020: 15 · 2019: 21 · 2018: 19 · 2017: 15 · 2016: 16 · 2015: 15 · 2014: 21 · 2013: 16 · 2012: 19
FWCI
11.34
Type
journal article
Language
en
Open access
closed
Locations
  • Science (publishedVersion)
  • PubMed (publishedVersion)
  • INRIA a CCSD electronic archive server (submittedVersion)
Funders
  • Sight Research UK (NRCF010002)
  • Natural Environment Research Council (NRCF010002)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
  • Social Sciences › Arts and Humanities › Archeology › Ancient Egypt and Archaeology
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tree-ring climate responses
Keywords
dynastic Egypt, radiocarbon chronology, New Kingdom, Old Kingdom, Djoser, Bayesian model, floating chronology, Nile Valley, ancient Egyptian chronology

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