Abstract
As part of the ongoing effort to improve the Northern Hemisphere radiocarbon (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 C measurements. In this age range, IntCal13 was constructed largely from German and Irish oak as well as Californian bristlecone pine C dates, with most samples measured with a 10-yr resolution. The new data presented here is the first atmospheric 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.
| Original language | English |
|---|---|
| Pages (from-to) | 919-937 |
| Number of pages | 19 |
| Journal | Radiocarbon |
| Volume | 62 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 2020 |
Subject classification (UKÄ)
- Geology
Free keywords
- calibration
- IntCal
- radiocarbon
- tree rings
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Dive into the research topics of 'Single-Year German oak and Californian Bristlecone Pine C Data at the Beginning of the Hallstatt Plateau from 856 BC to 626 BC'. Together they form a unique fingerprint.Infrastructure
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Radiocarbon Dating Laboratory
Muscheler, R. (Manager) & Rundgren, M. (Manager)
Department of Earth and Environmental Sciences (MGeo)Infrastructure
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