Challenges in 14C dating towards the limit of the method inferred from anchoring a floating tree ring radiocarbon chronology to ice core records around the Laschamp geomagnetic field minimum

Riamund Muscheler, Florian Adolphi, Anders Svensson

22 Citationer (Scopus)

Abstract

The 14C dating method is the cornerstone for inferring age estimates for natural archives covering the last 50000 yrs. However, 14C age calibration for the last ice age relies mostly on records that only indirectly reflect the atmospheric 14C concentrations. In consequence, calendar age estimates are significantly more uncertain for the period of the last ice age compared to the past 14000 yrs where tree-ring based calibration records exist. Here we connect a 14C tree-ring chronology from Kauri trees in New Zealand to ice core 10Be records via the common signal in the galactic cosmic ray flux around the period of the Laschamp geomagnetic field minimum (ca. 41000 yrs BP). Synchronous changes of modelled 14C and 14C inferred from U/Th-dated speleothems support the ice core chronology independently and suggest that the published ice core time scale errors are rather conservative for this period. Our analysis puts 14C age determinations directly into the context of ice core climate records and it shows that the 14C records underlying the 14C calibration curve overestimate the atmospheric 14C concentration by more than 200‰. Consequently, 14C age calibration presently yields too old calendar age estimates by about 1200 yrs for this period.

OriginalsprogEngelsk
TidsskriftEarth and Planetary Science Letters
Vol/bind394
Sider (fra-til)209-215
ISSN0012-821X
DOI
StatusUdgivet - 15 maj 2014

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