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A discontinuity in mantle composition beneath the southwest Indian ridge


The composition of mid-ocean-ridge basalt is known to correlate with attributes such as ridge topography1,2 and seismic velocity in the underlying mantle3, and these correlations have been interpreted to reflect variations in the average extent and mean pressures of melting during mantle upwelling. In this respect, the eastern extremity of the southwest Indian ridge is of special interest, as its mean depth of 4.7 km (ref. 4), high upper-mantle seismic wave velocities5 and thin oceanic crust of 4–5 km (ref. 6) suggest the presence of unusually cold mantle beneath the region. Here we show that basaltic glasses dredged in this zone, when compared to other sections of the global mid-ocean-ridge system, have higher Na8.0, Sr and Al2O3 compositions, very low CaO/Al2O3 ratios relative to TiO2 and depleted heavy rare-earth element distributions. This signature cannot simply be ascribed to low-degree melting of a typical mid-ocean-ridge source mantle, as different geochemical indicators of the extent of melting1 are mutually inconsistent. Instead, we propose that the mantle beneath 1,000 km of the southwest Indian ridge axis has a complex history involving extensive earlier melting events and interaction with partial melts of a more fertile source.

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We thank the Service d'Analyse des Roches et des Minéraux (SARM) and J. Carignan for their help in the laboratory. We also thank D. Sauter for helpful discussions. Funding was provided by CNRS-INSU, and the IFRTP provided access to the Marion Dufresne II for sampling.

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Correspondence to Catherine Mével.

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The authors declare that they have no competing financial interests.

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Supplementary Tables 1-4 (DOC 214 kb)

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Figure 1: Topographic map of the southwest Indian ridge (SWIR), showing sample locations used in this study (circles).
Figure 2: Characteristics of the major-element chemistry of SWIR lavas compared to those from other mid-ocean ridges.
Figure 3: Variations of major- and trace-element chemistry of SWIR lavas compared to those from other mid-ocean ridges.
Figure 4: Rare-earth element systematics of glasses from zones B and A.


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