Abstract

ABSTRACT As part of the ongoing effort to improve the Northern Hemisphere radiocarbon ( 14 C) calibration curve, this study investigates the period of 856 BC to 626 BC (2805–2575 yr BP) with a total of 403 single-year 14 C measurements. In this age range, IntCal13 was constructed largely from German and Irish oak as well as Californian bristlecone pine 14 C dates, with most samples measured with a 10-yr resolution. The new data presented here is the first atmospheric 14 C single-year record of the older end of the Hallstatt plateau based on an absolutely dated tree-ring chronology. The data helped reveal a major solar proton event (SPE) which caused a spike in the production rate of cosmogenic radionuclides around 2610/2609 BP. This production event is thought to have reached a magnitude similar to the 774/775 AD production event but has remained undetected due to averaging effects in the decadal calibration data. The record leading up to the 2610/2609 BP event reveals a 11-yr solar cycle with varying cyclicity. Features of the new data and the benefits of higher resolution calibration are discussed.

Keywords

Radiocarbon datingPlateau (mathematics)GermanArchaeologyGeologyGeography

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Publication Info

Year
2020
Type
article
Volume
62
Issue
4
Pages
919-937
Citations
20
Access
Closed

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Simon Fahrni, John Southon, Benjamin T. Fuller et al. (2020). Single-Year German oak and Californian Bristlecone Pine <sup>14</sup>C Data at the Beginning of the Hallstatt Plateau from 856 BC to 626 BC. Radiocarbon , 62 (4) , 919-937. https://doi.org/10.1017/rdc.2020.16

Identifiers

DOI
10.1017/rdc.2020.16