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Extraction of In Situ Cosmogenic 14C from Olivine

Published online by Cambridge University Press:  18 July 2016

Jeffrey S Pigati ,
Nathaniel A Lifton ,
A J Timothy Jull  and
Jay Quade
Jeffrey S Pigati*
Affiliation:
Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
Nathaniel A Lifton
Affiliation:
Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
A J Timothy Jull
Affiliation:
Arizona-NSF AMS Facility, Physics Department, University of Arizona, Tucson, Arizona 85721, USA
Jay Quade
Affiliation:
Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
*
Corresponding author. Email: jpigati@usgs.gov
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Abstract

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Chemical pretreatment and extraction techniques have been developed previously to extract in situ cosmogenic radiocarbon (in situ14C) from quartz and carbonate. These minerals can be found in most environments on Earth, but are usually absent from mafic terrains. To fill this gap, we conducted numerous experiments aimed at extracting in situ14C from olivine ((Fe,Mg)2SiO4). We were able to extract a stable and reproducible in situ14C component from olivine using stepped heating and a lithium metaborate (LiBO2) flux, following treatment with dilute HNO3 over a variety of experimental conditions. However, measured concentrations for samples from the Tabernacle Hill basalt flow (17.3 ± 0.3 ka4) in central Utah and the McCarty's basalt flow (3.0 ± 0.2 ka) in western New Mexico were significantly lower than expected based on exposure of olivine in our samples to cosmic rays at each site. The source of the discrepancy is not clear. We speculate that in situ14C atoms may not have been released from Mg-rich crystal lattices (the olivine composition at both sites was ∼Fo65Fa35). Alternatively, a portion of the 14C atoms released from the olivine grains may have become trapped in synthetic spinel-like minerals that were created in the olivine-flux mixture during the extraction process, or were simply retained in the mixture itself. Regardless, the magnitude of the discrepancy appears to be inversely proportional to the Fe/(Fe+Mg) ratio of the olivine separates. If we apply a simple correction factor based on the chemical composition of the separates, then corrected in situ14C concentrations are similar to theoretical values at both sites. At this time, we do not know if this agreement is fortuitous or real. Future research should include measurement of in situ14C concentrations in olivine from known-age basalt flows with different chemical compositions (i.e. more Fe-rich) to determine if this correction is robust for all olivine-bearing rocks.

Type
Sample Preparation
Information
Radiocarbon , Volume 52 , Issue 3: 20th Int. Radiocarbon Conference Proceedings , 2010 , pp. 1244 - 1260
Copyright
Copyright © 2010 by the Arizona Board of Regents on behalf of the University of Arizona 

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