Cosmogenic 10Be concentrations in Antarctic ice during the past 30,000 years

Raisbeck, G. M.; Yiou, F.; Fruneau, M.; Loiseaux, J.M.; Lieuvin, M.; Ravel, J. C.; Lorius, C.

doi:10.1038/292825a0

Cited by 126 publications

(54 citation statements)

References 14 publications

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“…Ocean. This can be ascribed to the melting of the Antarctic ice which may have at least 50 times higher "Be concentrations than those of the average Pacific surface water (Raisbeck et al, 1981). As the 9Be profile here is almost identical to those in the Pacific, the surface "Be/ 'Be ratio of 3 x 10-' is the highest among the values measured thus far.…”

Section: Resultssupporting

confidence: 52%

Beryllium isotopes in the ocean.

Kusakabe

Southon

et al. 1990

Geochem. J.

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Vertical profiles of 9Be and "Be have been determined in the ocean. The nutrient-like recycling behavior for both Be isotopes, involving surface scavenging and deep-water regeneration, is manifested by their vertical profiles in the borderland basin off southern California, in the Pacific and in the Bering Sea. In contrast, in the western N. Atlantic, the concentrations of 9Be are almost vertically constant (or slightly higher in the surface than in the deep), and the concentrations of "Be generally show minor sur face depletion and are lower than those of the Pacific. The 9Be profiles in the S. Atlantic are generally similar to those of the Pacific except for a station close to the plume of Saharan desert dust, which shows surface enrichment. We interpret the vertical distributions and their differences among stations in terms of intense surface 9Be input (especially\eolian input) to the Atlantic, a relatively uniform ocean wide pluvial input of "Be, the particle reactive nature of Be, and the oceanic residence time of Be. Material balance calculations using a two-box (coastal and open oceans) model point to the importance of coastal ocean as a sink for both Be isotopes and eolian dusts as a source of oceanic 9Be.

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Section: Resultssupporting

confidence: 52%

Beryllium isotopes in the ocean.

Kusakabe

Southon

et al. 1990

Geochem. J.

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“…As we show in the following, these different records lead to a different normalization of the 14 C-based solar-modulation records, but do not strongly affect the inferred relative changes in solar modulation. (Nishiizumi and Finkel, 2007), South Pole (Raisbeck et al, 1990), Dome Fuji (Horiuchi et al, 2008), Dome C (Beer, Raisbeck, and Yiou, 1991;Raisbeck et al, 1981), Milcent (Beer, Raisbeck, and Yiou, 1991), Dye-3 (Beer et al, 1990), Camp Century (Beer et al, 1988), GRIP (Muscheler et al, 2004;Yiou et al, 1997), and NGRIP (Berggren et al, 2009). The bottom panel indicates the temporal coverage of each record.…”

Section: Neutron-monitor Datamentioning

confidence: 99%

The Revised Sunspot Record in Comparison to Cosmogenic Radionuclide-Based Solar Activity Reconstructions

et al. 2016

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Recent revisions in the sunspot records illustrate the challenges related to obtaining a 400-year-long observational record of past solar-activity changes. Cosmogenic radionuclides offer the possibility of obtaining an alternative and completely independent record of solar variability. Here, we illustrate that these records offer great potential for quantitative solar-activity reconstructions far back into the past, and we provide updated radionuclide-based solar-activity reconstructions for the past 2000 years. However, cosmogenic-radionuclide records are also influenced by processes independent of solar activity, leading to the need for critical assessment and correction for the non-solar influences. Independent of these uncertainties, we show a very good agreement between the revised sunspot records and the 10 Be records from Antarctica and, in particular, the 14 C-based solar-activity reconstructions. This comparison offers the potential of identifying remaining non-solar processes in the radionuclide-based solar-activity reconstructions, but it also helps identifying remaining biases in the recently revised sunspot records.

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“…The large peak at 31,000 calBP is attributed to a magnetic excursion (Kitagawa and Van der Plicht 1998a). Such excursions (known as Mono Lake and/or Laschamp) have also been observed in other cosmogenic isotope records: 10 Be in the ice cores Vostok (at 35,000 cal BP, Raisbeck et al, 1987) and GRIP (at 41,000 cal BP, Yiou et al, 1997), 10 Be in marine sediments from the Mediterranean Sea (at 37,000 cal BP, Castagnoli et al, 1995), the Gulf of California (at 32,000 cal BP, McHargue et al, 1995) and the Caribbean Sea (at 37,000 cal BP, Aldahan and Possnert, 1998), and 36 C1 in the GRIP ice core (at 38,000 cal BP, Baumgartner et al, 1998; at 32.000 cal BP, Wagner et al, 2000).…”

Section: Discussion Of the Oldest Part Of The Scale 4 C Timementioning

confidence: 96%

Calibration of the ¹⁴C time scale: towards the complete dating range

Plicht

2002

Netherlands Journal of Geosciences

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Radiocarbon calibration based on dendro-chronology and U-series dated corals yield a calibration curve (INTCAL98) well into the Late Glacial, back to ca. 15,600 calendar years ago. Beyond this limit, various calibration curves are produced, mainly based on laminated sediments and various carbonates dated by U-series isotopes. Such calibration curves now cover the complete "C dating range of about 45,000 years, but are not consistent with each other. Each calibration method (other than dendro-chronology) has its own assumptions and pitfalls. Thus far, the calibration curve obtained from Lake Suigetsu laminated sediments is the only terrestrial (atmospheric) one.

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Cosmogenic 10Be concentrations in Antarctic ice during the past 30,000 years

Cited by 126 publications

References 14 publications

Beryllium isotopes in the ocean.

Beryllium isotopes in the ocean.

The Revised Sunspot Record in Comparison to Cosmogenic Radionuclide-Based Solar Activity Reconstructions

Calibration of the ¹⁴C time scale: towards the complete dating range

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Cosmogenic 10Be concentrations in Antarctic ice during the past 30,000 years

Cited by 126 publications

References 14 publications

Beryllium isotopes in the ocean.

Beryllium isotopes in the ocean.

The Revised Sunspot Record in Comparison to Cosmogenic Radionuclide-Based Solar Activity Reconstructions

Calibration of the 14C time scale: towards the complete dating range

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Product

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Calibration of the ¹⁴C time scale: towards the complete dating range