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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

Findings from an in-Depth Annual Tree-Ring Radiocarbon Intercomparison

Radiocarbon Cambridge University Press (CUP) 62:4 (2020) 873-882

Authors:

L Wacker, EM Scott, A Bayliss, D Brown, E Bard, S Bollhalder, M Friedrich, M Capano, A Cherkinsky, D Chivall, BJ Culleton, MW Dee, R Friedrich, GWL Hodgins, A Hogg, DJ Kennett, TDJ Knowles, M Kuitems, TE Lange, F Miyake, M-J Nadeau, T Nakamura, JP Naysmith, J Olsen, T Omori, F Petchey, B Philippsen, C Bronk Ramsey, GV Ravi Prasad, M Seiler, J Southon, R Staff, T Tuna

Abstract:

ABSTRACTThe radiocarbon (14C) calibration curve so far contains annually resolved data only for a short period of time. With accelerator mass spectrometry (AMS) matching the precision of decay counting, it is now possible to efficiently produce large datasets of annual resolution for calibration purposes using small amounts of wood. The radiocarbon intercomparison on single-year tree-ring samples presented here is the first to investigate specifically possible offsets between AMS laboratories at high precision. The results show that AMS laboratories are capable of measuring samples of Holocene age with an accuracy and precision that is comparable or even goes beyond what is possible with decay counting, even though they require a thousand times less wood. It also shows that not all AMS laboratories always produce results that are consistent with their stated uncertainties. The long-term benefits of studies of this kind are more accurate radiocarbon measurements with, in the future, better quantified uncertainties.
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Marine20—The Marine Radiocarbon Age Calibration Curve (0–55,000 cal BP)

Radiocarbon Cambridge University Press (CUP) 62:4 (2020) 779-820

Authors:

Timothy J Heaton, Peter Köhler, Martin Butzin, Edouard Bard, Ron W Reimer, William EN Austin, Christopher Bronk Ramsey, Pieter M Grootes, Konrad A Hughen, Bernd Kromer, Paula J Reimer, Jess Adkins, Andrea Burke, Mea S Cook, Jesper Olsen, Luke C Skinner
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SHCal20 Southern Hemisphere Calibration, 0–55,000 Years cal BP

Radiocarbon Cambridge University Press (CUP) 62:4 (2020) 759-778

Authors:

Alan G Hogg, Timothy J Heaton, Quan Hua, Jonathan G Palmer, Chris SM Turney, John Southon, Alex Bayliss, Paul G Blackwell, Gretel Boswijk, Christopher Bronk Ramsey, Charlotte Pearson, Fiona Petchey, Paula Reimer, Ron Reimer, Lukas Wacker
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Testing and Improving the IntCal20 Calibration Curve with Independent Records

Radiocarbon Cambridge University Press (CUP) 62:4 (2020) 1079-1094

Authors:

Raimund Muscheler, Florian Adolphi, Timothy J Heaton, Christopher Bronk Ramsey, Anders Svensson, Johannes van der Plicht, Paula J Reimer
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Are there enormous age-trends in stable carbon isotope ratios of oak tree rings?

Holocene SAGE Publications 30:11 (2020) 1637-1642

Abstract:

We test a recent prediction that stable carbon isotope ratios from UK oaks will display age-trends of more than 4‰ per century by measuring >5400 carbon isotope ratios from the late-wood alpha-cellulose of individual rings from 18 modern oak trees and 50 building timbers spanning the 9th to 21st centuries. After a very short (c.5 years) juvenile phase with slightly elevated values, the number of series that show rising and falling trends is almost equal (33:35) and the average trend is almost zero. These results are based upon measuring and averaging the trends in individual time-series; the ‘mean of the slopes’ approach. We demonstrate that the more conventional ‘slope of the mean’ approach can produce strong but spurious ‘age-trends’ even when the constituent series are flat, with zero slope and zero variance. We conclude that it is safe to compile stable carbon isotope chronologies from UK oaks without de-trending. The isotope chronologies produced in this way are not subject to the ‘segment length curse’, which applies to growth measurements, such as ring width or density, and have the potential to retain very long-term climate signals.
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