Journal
EARTH AND PLANETARY SCIENCE LETTERS
Volume 274, Issue 1-2, Pages 179-188Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.epsl.2008.07.021
Keywords
ocean island basalt; continental crust; helium isotopes; zircon age; density estimation
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Funding
- NSF [OCE-0452457]
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Parman [Nature (2007) 446, 900-903] has recently suggested that a correlation exists between peaks in the ocean island basalt (OIB) He-4/He-3 distribution and peaks in crustal zircon ages. This correlation is based on matching peaks seen in smooth kernel density estimates. Kernel density estimation is a very useful technique, but care is required when choosing the smoothing bandwidth as spurious peaks can be produced if the bandwidth is too small. Here I provide an introduction to a general statistical technique for determining whether peaks in density estimates are significant, know as SiZer, focusing on its application to the He-4/He-3 data. SiZer identifies only two statistically significant peaks in the OIB He-4/He-3 distribution, compared with the eight peaks identified by Parman, The helium-continental crust correlation does not seem to be supported by the current data. (C) 2008 Elsevier B.V. All rights reserved.
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