Status report of the Heidelberg Radiocarbon Laboratory
Precision and application in Mauritanian cold-water corals over the last 30,000 years
Dados Bibliográficos
| ID | 6447993 |
|---|---|
| Autores | E Beisel (0009-0006-4439-5675, autor correspondente), Steffen Therre (0000-0001-5411-4749), Claudia Wienberg (0000-0001-9870-5495), Ronny Friedrich (0000-0001-5199-1957), Norbert Frank (0000-0002-0416-9546) |
| Ano | 2025 |
| Volume | 67 |
| Fascículo | 3 |
| Páginas | 450-460 |
| Data de publicação | 2025-03-14 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | Radiocarbon (JOURNAL) |
| Identificadores do periódico | ISSN: 0033-8222 • E-ISSN: 1945-5755 |
| Editora | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/rdc.2025.7 |
| OpenAlex | W4408460198 |
| Idioma | EN |
| Referências citadas | 40 |
Highly precise and reproducible radiocarbon ( 14 C) measurements are regularly performed at the Heidelberg Institute for Environmental Physics, Heidelberg, Germany, in collaboration with the radiocarbon laboratory of the Curt-Engelhorn-Center Archaeometry in Mannheim, Germany. Here, we report an update of the technical details, focusing on the analysis of cold-water corals (CWC), and present an improved long-term blank value with a mean of (0.190 ± 0.064) pMC (n = 138) and excellent reproducibility of the IAEA-C2 standard with a mean of (41.15 ± 0.16) pMC (n = 75), consistent with its certified consensus value. Furthermore, 33 duplicates of the CWC 14 C measurements agree within 2σ, 85% even within the 1σ range. This provides excellent conditions for accurate 14 C measurements. As an application example, we present combined 230 Th/U and 14 C ages of a coral-bearing sediment core from the upper Mauritanian slope. The resulting ventilation age record confirms decreasing ventilation between 30 and 25 kyr BP, most likely reflecting a northward propagation of a water mass originating from the south. During the LGM, we confirm a previously hypothesized southward displacement of the Cap Verde Frontal Zone. With the onset of the deglaciation, our record documents again an advance of a southern-sourced water mass into the subtropical North Atlantic. During the Bølling-Allerød warm period, strong ventilation fluctuations possibly indicate temporal influence of southern-sourced water
Accelerator mass spectrometry · Coral · Deglaciation · Geography · Holocene · Last Glacial Maximum · Physical geography · Radiocarbon dating · Water mass · Coral and Marine Ecosystems Studies · Geological formations and processes · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology
Mams – A new AMS facility at the Curt-Engelhorn-Centre for Achaeometry, Mannheim, Germany
Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
Micadas
Heidelberg Radiocarbon Lab – Establishing a New Carbon Dioxide Extraction Line for Carbonate Samples
The IAEA 14 C Intercomparison Exercise 1990
Radiocarbon Dating of Deep-Sea Corals
Development of a Semi-Automated System for Routine Preparation of Carbonate Samples
International Agreements and the Use of the New Oxalic Acid Standard
Status Report on Sample Preparation Protocols Developed at the LMC14 Laboratory, Saclay, France
Sample Preparation at the Jena 14 C Laboratory
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
| Velocidade de citação | historical |
|---|---|
| Altamente citado | Não |