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We report high precision high field strength element (HFSE) concentrations of Italian Plio-Quaternary mafic magmas.Silica-undersaturated rocks of the Roman magmatic province show high Nb/Ta.Instead, earlier silica-oversaturated rocks of the Tuscan magmatic province have unfractionated Nb/Ta.We show evidence that the high Nb/Ta of Roman magmas reflects subduction-derived, carbonate-rich melts.Similar melts may also account for high Nb/Ta in other silica-undersaturated magmas from the circum-Mediterranean (e.g., Macedonia, Bulgaria, Turkey) and the Sunda arc, previously interpreted to reflect residual rutile.We propose a genetic link between high Nb/Ta, silica-undersaturated magmas and recycling of carbonate-rich lithologies via subduction.As such, Nb/Ta can be used to trace the recycling of subducting carbonates.
Bragagni et al. (Fri,) studied this question.