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Status report of the Heidelberg Radiocarbon Laboratory

Precision and application in Mauritanian cold-water corals over the last 30,000 years

Datos Bibliográficos

ID6447993
AutoresE Beisel (0009-0006-4439-5675, autor de correspondencia), Steffen Therre (0000-0001-5411-4749), Claudia Wienberg (0000-0001-9870-5495), Ronny Friedrich (0000-0001-5199-1957), Norbert Frank (0000-0002-0416-9546)
Año2025
Volumen67
Número3
Páginas450-460
Fecha de publicación2025-03-14
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaRadiocarbon (JOURNAL)
Identificadores de la revistaISSN: 0033-8222 • E-ISSN: 1945-5755
EditorialCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/rdc.2025.7
OpenAlexW4408460198
IdiomaEN
Referencias citadas40

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

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