Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Letter
  • Published:

Terrestrial Origin of Aluminium-26 and Oceanic Sedimentation Rate

Abstract

THE recent detection of aluminium-26 in marine sediments by Amin, Kharkar and Lal1 has posed a question about the origin of this nuclide. Lal and Venkatavaradan2 pointed out that the amount of aluminium-26 in sediments is an order of magnitude higher than expected, as a result of its production by cosmic ray interactions in the terrestrial environment. Thus they concluded that the large amount of aluminium-26 can only be explained by postulating an influx with extraterrestrial cosmic dust which has been exposed to a significant flux of energetic particles capable of producing nuclear interactions.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Similar content being viewed by others

References

  1. Amin, B. S., Kharkar, D. P., and Lal, D., Deep-Sea Res., 13, 805 (1966).

    CAS  Google Scholar 

  2. Lal, D., and Venkatavaradan, V. S., Science, 151, 1381 (1966).

    Article  ADS  CAS  Google Scholar 

  3. Yiou, F., Baril, M., Dufaure de Citres, J., Fontes, P., Gradsztajn, E., and Bernas, R., Phys. Rev. (in the press).

  4. Lal, D., and Peters, B., in Handbuch der Physik, 46/2 (Springer, Berlin, 1967).

    Google Scholar 

  5. Honda, M., and Lal, D., Nucl. Phys., 51, 363 (1964).

    Article  CAS  Google Scholar 

  6. Reeves, H., J. Physiq. (suppl.), colloque No. 1, Cl, 28 (1966).

  7. Nilsson, C., Science, 153, 1242 (1966).

    Article  ADS  CAS  Google Scholar 

  8. Goldberg, E. D., and Koide, M., Geochim. Cosmochim. Acta, 26, 417 (1962).

    Article  ADS  CAS  Google Scholar 

  9. Teh-Lung Ku, thesis, Columbia Univ. (1966).

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

YOKOYAMA, Y. Terrestrial Origin of Aluminium-26 and Oceanic Sedimentation Rate. Nature 216, 569–571 (1967). https://doi.org/10.1038/216569a0

Download citation

  • Received:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/216569a0

This article is cited by

Comments

By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing