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Atomic and Laser Physics
Credit: Jack Hobhouse

Prof Christopher Ramsey

Professor of Archaeological Science

Research theme

  • Accelerator physics
  • Climate physics
  • Instrumentation

Sub department

  • Atomic and Laser Physics
christopher.ramsey@physics.ox.ac.uk
Telephone: 01865285215
School of Archaeology
  • About
  • Publications

The Emergence of Extramural Cemeteries in Neolithic Southeast Europe: A Formally Modeled Chronology for Cernica, Romania

Radiocarbon Cambridge University Press (CUP) 61:1 (2019) 319-346

Authors:

Susan Stratton, Seren Griffiths, Raluca Kogălniceanu, Angela Simalcsik, Alexandru Morintz, Cristian Eduard Ştefan, Valentin Dumitraşcu, Christopher Bronk Ramsey, Olaf Nehlich, Nancy Beavan, Dušan Borić, Alasdair Whittle
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Age estimates for hominin fossils and the onset of the Upper Palaeolithic at Denisova Cave

Nature Springer Nature 565 (2019) 640-644

Authors:

Katerina Douka, V Slon, Z Jacobs, Christopher Bronk Ramsey, MV Shunkov, AP Derevianko, F Mafessoni, MB Kozlikin, L Bo, R Grun, Daniel Comeskey, Thibaut Deviese, S Brown, B Viola, L Kinsley, M Buckley, M Meyer, R Roberts, S Pääbo, J Kelso, Thomas Higham

Abstract:

Denisova Cave in the Siberian Altai (Russia) is a key site for understanding the complex relationships between hominin groups that inhabited Eurasia in the Middle and Late Pleistocene epoch. DNA sequenced from human remains found at this site has revealed the presence of a hitherto unknown hominin group, the Denisovans1,2, and high-coverage genomes from both Neanderthal and Denisovan fossils provide evidence for admixture between these two populations3. Determining the age of these fossils is important if we are to understand the nature of hominin interaction, and aspects of their cultural and subsistence adaptations. Here we present 50 radiocarbon determinations from the late Middle and Upper Palaeolithic layers of the site. We also report three direct dates for hominin fragments and obtain a mitochondrial DNA sequence for one of them. We apply a Bayesian age modelling approach that combines chronometric (radiocarbon, uranium series and optical ages), stratigraphic and genetic data to calculate probabilistically the age of the human fossils at the site. Our modelled estimate for the age of the oldest Denisovan fossil suggests that this group was present at the site as early as 195,000 years ago (at 95.4% probability). All Neanderthal fossils—as well as Denisova 11, the daughter of a Neanderthal and a Denisovan4—date to between 80,000 and 140,000 years ago. The youngest Denisovan dates to 52,000–76,000 years ago. Direct radiocarbon dating of Upper Palaeolithic tooth pendants and bone points yielded the earliest evidence for the production of these artefacts in northern Eurasia, between 43,000 and 49,000 calibrated years before present (taken as AD 1950). On the basis of current archaeological evidence, it may be assumed that these artefacts are associated with the Denisovan population. It is not currently possible to determine whether anatomically modern humans were involved in their production, as modern-human fossil and genetic evidence of such antiquity has not yet been identified in the Altai region.
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C-14 wiggle-matching of short tree-ring sequences from post-medieval buildings in England

NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS 438 (2019) 218-226
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Stable Isotope Dating of Historic Buildings

Vernacular Architecture Taylor & Francis 50:1 (2019) 78-87

Authors:

D Miles, NJ Loader, GHF Young, D McCarroll, D Davies, C Bronk Ramsey, JG James
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Stable Isotope Tree-Ring Dates: List 1

Vernacular Architecture Taylor & Francis 50:1 (2019) 88-93

Authors:

NJ Loader, D McCarroll, GHF Young, D Davies, JG James, D Miles, C Bronk Ramsey
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