Radiocarbon calibration/comparison records based on marine sediments from the Pakistan and Iberian margins
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We present a new record of radiocarbon ages measured by accelerator mass spectrometry (AMS) on a deep-sea core collected off the Pakistan Margin. The 14 C ages measured on the planktonic foraminifera Globigerinoides ruber from core MD04-2876 define a high and stable sedimentation rate on the order of 50 cm/kyr over the last 50 kyr. The site is distant from the main upwelling zone of the western Arabian Sea where 14 C reservoir age is large and may be variable. Many independent proxies based on elemental analyses, mineralogy, biomarkers, isotopic proxies, and foraminiferal abundances show abrupt changes correlative with Dansgaard-Oeschger and Heinrich events. It is now common knowledge that these climatic events also affected the Arabian Sea during the last glacial period through changes in the Indian monsoon and in ventilation at intermediate depths. The stratigraphic agreement between all proxies, from fine- to coarse-size fractions, indicates that the foraminiferal 14 C ages are representative of the different sediment fractions. To build a calendar age scale for core MD04-2876, we matched its climate record to the oxygen isotopic (δ 18 O) profile of Hulu Cave stalagmites that have been accurately dated by U-Th (Wang et al. 2001; Southon et al. 2012; Edwards et al., submitted). Both archives exhibit very similar signatures, even for century-long events linked to monsoonal variations. For comparison, we have also updated our previous work on core MD95-2042 from the Iberian Margin (Bard et al. 2004a,b,c), whose climate record has likewise been tuned to the high-resolution δ 18 O Hulu Cave profile. Sophisticated and novel statistical techniques were used to interpolate ages and calculate uncertainties between chronological tie-points (Heaton et al. 2013, this issue). The data from the Pakistan and Iberian margins compare well even if they come from distant sites characterized by different oceanic conditions. Collectively, the data also compare well with the IntCal09 curve, except for specific intervals around 16 cal kyr BP and from 28 to 31 cal kyr BP. During these intervals, the data indicate that 14 C is somewhat older than indicated by the IntCal09 curve. Agreement between the data from both oceanic sites suggests that the discrepancy is not due to local changes of sea-surface 14 C reservoir ages, but rather that the IntCal09 curve needed to be updated in these intervals as has been done in the framework of IntCal13 (Reimer et al. 2013a, this issue).
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For Pakistan and Iberian margin sediment cores, climate proxy records are the same as those described for IntCal13.
“For the sediment cores from the Pakistan and Iberian margins, the climate proxy records are the same as those described for IntCal13 (Bard et al. 2013).”
From The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP) (2020) · cites this paper as Bard et al. 2013
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Fagault, Y., Tuna, T., Rostek, F., & Bard, E. (2019) · Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms · doi:10.1016/j.nimb.2018.11.018 · Cited by 30 · see citing works
Self-citationTesting and Improving the IntCal20 Calibration Curve with Independent Records
Muscheler, R., Adolphi, F., Heaton, T. J., Bronk Ramsey, C., Svensson, A., van der Plicht, J., & Reimer, P. J. (2020) · Radiocarbon · doi:10.1017/rdc.2020.54 · Cited by 30 · see citing works
Self-citation
- Authors
- Bard, E., Ménot, G., Rostek, F., Licari, L., Böning, P., Edwards, R. L., Cheng, H., Wang, Y., & Heaton, T. J.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- University of Minnesota (US)
- Nanjing Normal University (CN)
- University of Sheffield (GB)
- Venue
- Radiocarbon
- Publisher
- Cambridge University Press (CUP)
- Published
- 2013
- Volume
- 55
- Issue
- 4
- Pages
- 1999-2019
- ISSN
- 0033-8222 (ISSN-L)
- 1945-5755
- OpenAlex
- W2158905005
- Semantic Scholar
- 94e68677948f8bc0f9ea9ef74e2e42cf63813750
- Cited by
- 73
- References
- 73
- Citations by year
- 2026: 2 · 2025: 2 · 2024: 1 · 2023: 9 · 2022: 7 · 2021: 18 · 2020: 7 · 2019: 5 · 2018: 3 · 2017: 4 · 2016: 3 · 2015: 6 · 2014: 1 · 2013: 3
- FWCI
- 2.82
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Radiocarbon (publishedVersion)
- HAL (submittedVersion)
- Institutional Archive of Ifremer (French Research Institute for Exploitation of the Sea) (submittedVersion, other-oa)
- EGU General Assembly Conference Abstracts
- Funders
- National Science Foundation (1211299, 41230524, 1103403, 0908792)
- Woods Hole Oceanographic Institution
- Comer Science and Education Foundation
- Equipex
- Agence Nationale de la Recherche (ANR-10-EQPX-0024)
- National Natural Science Foundation of China (1103403, 41230524)
- Centre National de la Recherche Scientifique
- Institut Polaire Français Paul Emile Victor
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
- Keywords
- radiocarbon calibration, oxygen isotopes, Dansgaard-Oeschger events, Heinrich events, planktonic foraminifera, Globigerinoides ruber, sedimentation rate, Arabian Sea, western Iberian margin, last glacial period, Indian monsoon, deep water ventilation, chronology, marine sediment
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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