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Science 29 May 1998: Vol. 280. no. 5368, pp. 1421 - 1424 DOI: 10.1126/science.280.5368.1421
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Reports
Eclogitic Diamond Formation at Jwaneng: No Room for a Recycled Component
Pierre Cartigny,
*
Jeffrey W. Harris,
Marc Javoy
Eclogitic diamonds have a large range of 13C values,
whereas peridotitic diamonds do not. Paired
15N- 13C-N variations in 40 eclogitic
diamonds from the Jwaneng kimberlite in Botswana show that neither the
influence of recycled biogenic carbon nor the global and primordial
heterogeneity of mantle carbon are likely for the origin of the large
13C range; the data instead support a fractionation
process. It is proposed that carbonatitic mantle melts from which
diamonds crystallize undergo different evolutions before diamond
precipitation, when percolating through either a peridotite or an
eclogite. These different evolutions, reflecting the presence or
absence of olivine, can account for their respective 13C
distributions.
P. Cartigny and M. Javoy, Laboratoire de
Géochimie des Isotopes Stables, Université de Paris VII,
Institut de Physique du Globe de Paris (IPGP), 4 Place Jussieu, 75251 Paris Cedex 05, France.
J. W. Harris, Department of Geology and Applied
Geology, University of Glasgow, Glasgow G12 8QQ, Scotland, UK.
*
To whom correspondence should be addressed. E-mail:
cartigny{at}ipgp.jussieu.fr
Read the Full Text
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