Author Correction: Sampling the volatile-rich transition zone beneath Bermuda.

An Amendment to this paper has been published and can be accessed via a link at the top of the paper.

Sampling the volatile-rich transition zone beneath Bermuda.

Intraplate magmatic provinces found away from plate boundaries provide direct sampling of the composition and heterogeneity of the Earth's mantle. The chemical heterogeneities that have been observed in the mantle are usually attributed to recycling during subduction, which allows for the addition of volatiles and incompatible elements into the mantle. Although many intraplate volcanoes sample deep-mantle reservoirs-possibly at the core-mantle boundary-not all intraplate volcanoes are deep-rooted, and reservoirs in other, shallower boundary layers are likely to participate in magma generation.