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Helium isotopic evidence for episodic mantle melting and crustal growth

Abstract

The timing of formation of the Earth’s continental crust is the subject of a long-standing debate1,2, with models ranging from early formation with little subsequent growth, to pulsed growth, to steadily increasing growth. But most models do agree that the continental crust was extracted from the mantle by partial melting3. If so, such crustal extraction should have left a chemical fingerprint in the isotopic composition of the mantle. The subduction of oceanic crust and subsequent convective mixing, however, seems to have largely erased this record in most mantle isotopic systems (for example, strontium, neodymium and lead). In contrast, helium is not recycled into the mantle because it is volatile and degasses from erupted oceanic basalts. Therefore helium isotopes may potentially preserve a clearer record of mantle depletion than recycled isotopes. Here I show that the spectrum of 4He/3He ratios in ocean island basalts appears to preserve the mantle’s depletion history, correlating closely with the ages of proposed continental growth pulses4,5. The correlation independently predicts both the dominant 4He/3He peak found in modern mid-ocean-ridge basalts, as well as estimates of the initial 4He/3He ratio of the Earth6. The correspondence between the ages of mantle depletion events and pulses of crustal production implies that the formation of the continental crust was indeed episodic and punctuated by large, potentially global, melting events. The proposed helium isotopic evolution model does not require a primitive, undegassed mantle reservoir, and therefore is consistent with whole mantle convection.

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Figure 1: Globally recurring 4 He/ 3 He peaks in oceanic basalts.
Figure 2: Correspondence of OIB and MORB 4 He/ 3 He peaks with continental crust zircon age peaks.

References

  1. Taylor, S. R. & McLennan, S. M. The geochemical evolution of the continental crust. Rev. Geophys. 33, 241–265 (1995)

    Article  ADS  Google Scholar 

  2. Bowring, S. A. & Housh, T. The Earth’s early evolution. Science 269, 1535–1540 (1995)

    Article  ADS  CAS  Google Scholar 

  3. Hofmann, A. W. Chemical differentiation of the Earth — the relationship between mantle, continental crust, and oceanic crust. Earth Planet. Sci. Lett. 90, 297–314 (1988)

    Article  ADS  CAS  Google Scholar 

  4. Condie, K. C. Episodic continental growth and supercontinents: a mantle avalanche connection? Earth Planet. Sci. Lett. 163, 97–108 (1998)

    Article  ADS  CAS  Google Scholar 

  5. Kemp, A. I. S., Hawkesworth, C. J., Paterson, B. A. & Kinny, P. D. Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon. Nature 439, 580–583 (2006)

    Article  ADS  CAS  Google Scholar 

  6. Mahaffy, P. R., Donahue, T. M., Atreya, S. K., Owen, T. C. & Niemann, H. B. Galileo probe measurements of D/H and 3He/4He in Jupiter’s atmosphere. Space Sci. Rev. 84, 251–263 (1998)

    Article  ADS  CAS  Google Scholar 

  7. Allègre, C. J. & Moreira, M. Rare gas systematics and the origin of oceanic islands: the key role of entrainment at the 670 km boundary layer. Earth Planet. Sci. Lett. 228, 85–92 (2004)

    Article  ADS  Google Scholar 

  8. Kurz, M. D., Jenkins, W. J. & Hart, S. R. Helium isotopic systematics of oceanic islands and mantle heterogeneity. Nature 297, 43–47 (1982)

    Article  ADS  CAS  Google Scholar 

  9. Moreira, M., Breddam, K., Curtice, J. & Kurz, M. D. Solar neon in the Icelandic mantle: new evidence for an undegassed lower mantle. Earth Planet. Sci. Lett. 185, 15–23 (2001)

    Article  ADS  CAS  Google Scholar 

  10. Porcelli, D. & Ballentine, C. J. Models for the distribution of terrestrial noble gases and evolution of the atmosphere. Rev. Mineral. Geochem. 47, 411–480 (2002)

    Article  CAS  Google Scholar 

  11. Allègre, C. J., Hofmann, A. & O’Nions, K. The argon constraints on mantle structure. Geophys. Res. Lett. 23, 3555–3557 (1996)

    Article  ADS  Google Scholar 

  12. Brooker, R. A. et al. The ‘zero charge’ partitioning behaviour of noble gases during mantle melting. Nature 423, 738–741 (2003)

    Article  ADS  CAS  Google Scholar 

  13. Parman, S. W., Kurz, M. D., Hart, S. R. & Grove, T. L. Helium solubility in olivine and implications for high 3He/4He in ocean island basalts. Nature 437, 1140–1143 (2005)

    Article  ADS  CAS  Google Scholar 

  14. Class, C. & Goldstein, S. L. Evolution of helium isotopes in the Earth’s mantle. Nature 436, 1107–1112 (2005)

    Article  ADS  CAS  Google Scholar 

  15. Stuart, F. M., Lass-Evans, S., Fitton, J. G. & Ellam, R. M. High 3He/4He ratios in picritic basalts from Baffin Island and the role of a mixed reservoir in mantle plumes. Nature 424, 57–59 (2003)

    Article  ADS  CAS  Google Scholar 

  16. Graham, D., Lupton, J., Albarède, F. & Condomines, M. Extreme temporal homogeneity of helium isotopes at Piton de la Fournaise, Réunion Island. Nature 347, 545–548 (1990)

    Article  ADS  CAS  Google Scholar 

  17. Kurz, M. D. Mantle heterogeneity beneath oceanic islands — some inferences from isotopes. Phil. Trans. R. Soc. Lond. 342, 91–103 (1993)

    Article  ADS  CAS  Google Scholar 

  18. Seta, A., Matsumoto, T. & Matsuda, J. Concurrent evolution of 3He/4He ratio in the Earth’s mantle reservoirs for the first 2 Ga. Earth Planet. Sci. Lett. 188, 211–219 (2001)

    Article  ADS  CAS  Google Scholar 

  19. Stein, M. & Hofmann, A. W. Mantle plumes and episodic crustal growth. Nature 372, 63–68 (1994)

    Article  ADS  CAS  Google Scholar 

  20. Armstrong, R. L. Radiogenic isotopes — The case for crustal recycling on a near-steady-state no-continental-growth Earth. Phil. Trans. R. Soc. Lond. 301, 443–472 (1981)

    Article  ADS  CAS  Google Scholar 

  21. Burke, K. & Torsvik, T. H. Derivation of large igneous provinces of the past 200 million years from long-term heterogeneities in the deep mantle. Earth Planet. Sci. Lett. 227, 531–538 (2004)

    Article  ADS  CAS  Google Scholar 

  22. Courtillot, V., Davaille, A., Besse, J. & Stock, J. Three distinct types of hotspots in the Earth’s mantle. Earth Planet. Sci. Lett. 205, 295–308 (2003)

    Article  ADS  CAS  Google Scholar 

  23. Wen, L. X. A compositional anomaly at the Earth’s core-mantle boundary as an anchor to the relatively slowly moving surface hotspots and as source to the DUPAL anomaly. Earth Planet. Sci. Lett. 246, 138–148 (2006)

    Article  ADS  CAS  Google Scholar 

  24. Allègre, C. J. & Turcotte, D. L. Implications of a two-component marble-cake mantle. Nature 323, 123–127 (1986)

    Article  ADS  Google Scholar 

  25. Helffrich, G. R. & Wood, B. J. The Earth’s mantle. Nature 412, 501–507 (2001)

    Article  ADS  CAS  Google Scholar 

  26. Hofmann, A. W. & White, W. M. Mantle plumes from ancient oceanic crust. Earth Planet. Sci. Lett. 57, 421–436 (1982)

    Article  ADS  CAS  Google Scholar 

  27. Davies, G. F. Stirring geochemistry in mantle convection models with stiff plates and slabs. Geochim. Cosmochim. Acta 66, 3125–3142 (2002)

    Article  ADS  CAS  Google Scholar 

  28. Zindler, A. & Hart, S. Chemical geodynamics. Annu. Rev. Earth Planet. Sci. 14, 493–571 (1986)

    Article  ADS  CAS  Google Scholar 

  29. Butler, S. L., Peltier, W. R. & Costin, S. O. Numerical models of the Earth’s thermal history: Effects of inner-core solidification and core potassium. Phys. Earth Planet. Inter. 152, 22–42 (2005)

    Article  ADS  CAS  Google Scholar 

  30. Davies, G. F. Punctuated tectonic evolution of the earth. Earth Planet. Sci. Lett. 136, 363–379 (1995)

    Article  ADS  CAS  Google Scholar 

  31. Abedini, A. A., Hurwitz, S. & Evans, W. C. USGS-NoGaDat — A global dataset of noble gas concentrations and their isotopic ratios in volcanic systems. (US Geological Survey Digital Data Series, 202) 〈http://pubs.usgs.gov/ds/2006/202〉 (2006)

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Acknowledgements

I thank G. Pearson, P. Martin and T. Grove for informal reviews, M. Kurz, S. Hart, M. Walter and J. Blundy for discussions, and A. Abedini for compiling the He isotope database. This research was supported by the Nuffield Foundation.

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Correspondence to S. W. Parman.

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Supplementary information

Supplementary Information

The file contains a Supplementary Table 1 of the corresponding 4He/3He and zircon age peaks used in the regression in the text and in Figure 2. It also contains Supplementary Figure 1 which is a more comprehensive version of Figure 1, showing all of the ocean islands for which there are more than 10 analyses, separating out various ridge systems and also showing the underlying histograms for the probability distribution functions. (PDF 301 kb)

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Parman, S. Helium isotopic evidence for episodic mantle melting and crustal growth. Nature 446, 900–903 (2007). https://doi.org/10.1038/nature05691

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