Deglacial changes in ocean circulation from an extended radiocarbon calibration

Konrad A. Hughen, Jonathan T. Overpeck, Scott J. Lehman, Michaele Kashgarian, John Southon, Larry C. Peterson, Richard B. Alley, Daniel M. Sigman

Research output: Contribution to journalArticle

292 Citations (Scopus)

Abstract

Temporal variations in the atmospheric concentration of radiocarbon sometimes result in radiocarbon-based age-estimates of biogenic material that do not agree with true calendar age. This problem is particularly severe beyond the limit of the high-resolution radiocarbon calibration based on tree-ring data, which stretches back only to about 11.8 kyr before present (BP), near the termination of the Younger Dryas cold period. If a wide range of palaeoclimate records are to be exploited for better understanding the rates and patterns of environmental change during the last deglaciation, extending the well-calibrated radiocarbon timescale back further in time is crucial. Several studies attempting such an extension, using uranium/thorium- dated corals and laminae counts in varved sediments, show conflicting results. Here we use radiocarbon data from varved sediments in the Cariaco basin, in the southern Caribbean Sea, to construct an accurate and continuous radiocarbon calibration for the period 9 to 14.5 kyr BP, nearly 3,000 years beyond the tree-ring based calibration. A simple model compared to the calculated atmospheric radiocarbon concentration and palaeoclimate data from the same sediment core suggests that North Atlantic Deep Water formation shut down during the Younger Dryas period, but was gradually replaced by an alternative mode of convection, possibly via the formation of North Atlantic Intermediate Water.

Original languageEnglish (US)
Pages (from-to)65-68
Number of pages4
JournalNature
Volume391
Issue number6662
DOIs
StatePublished - Jan 1 1998

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Younger Dryas
calibration
tree ring
paleoclimate
biogenic material
deep water formation
last deglaciation
North Atlantic Deep Water
intermediate water
thorium
sediment
sediment core
uranium
coral
environmental change
temporal variation
convection
timescale
basin
ocean circulation

All Science Journal Classification (ASJC) codes

  • General

Cite this

Hughen, K. A., Overpeck, J. T., Lehman, S. J., Kashgarian, M., Southon, J., Peterson, L. C., ... Sigman, D. M. (1998). Deglacial changes in ocean circulation from an extended radiocarbon calibration. Nature, 391(6662), 65-68. https://doi.org/10.1038/34150
Hughen, Konrad A. ; Overpeck, Jonathan T. ; Lehman, Scott J. ; Kashgarian, Michaele ; Southon, John ; Peterson, Larry C. ; Alley, Richard B. ; Sigman, Daniel M. / Deglacial changes in ocean circulation from an extended radiocarbon calibration. In: Nature. 1998 ; Vol. 391, No. 6662. pp. 65-68.
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Hughen, KA, Overpeck, JT, Lehman, SJ, Kashgarian, M, Southon, J, Peterson, LC, Alley, RB & Sigman, DM 1998, 'Deglacial changes in ocean circulation from an extended radiocarbon calibration', Nature, vol. 391, no. 6662, pp. 65-68. https://doi.org/10.1038/34150

Deglacial changes in ocean circulation from an extended radiocarbon calibration. / Hughen, Konrad A.; Overpeck, Jonathan T.; Lehman, Scott J.; Kashgarian, Michaele; Southon, John; Peterson, Larry C.; Alley, Richard B.; Sigman, Daniel M.

In: Nature, Vol. 391, No. 6662, 01.01.1998, p. 65-68.

Research output: Contribution to journalArticle

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Hughen KA, Overpeck JT, Lehman SJ, Kashgarian M, Southon J, Peterson LC et al. Deglacial changes in ocean circulation from an extended radiocarbon calibration. Nature. 1998 Jan 1;391(6662):65-68. https://doi.org/10.1038/34150