The origin and implications of primordial helium depletion in the Afar mantle plume

Abstract

Abstract Mantle plumes are responsible for the Earth’s largest volcanic provinces. In the prevailing paradigm, the deep mantle is less degassed than convecting shallow mantle, implying that plume-derived lavas have higher concentrations of primordial volatiles such as helium (He). Demonstrating this has led to explanations that question the established Earth model. Here, we show that the 3He/4He of basalts from the Red Sea display coherent relationships with trace elements, allowing the helium concentration of the Afar plume to be calculated. Contrary to the prevailing model it appears the helium concentration of the Afar plume is 10-25% of the upper mantle. This contradiction is resolved if the plume material itself is a mixture of helium-rich high-3He/4He deep mantle with helium-depleted low-3He/4He recently subducted oceanic crust. This implies that helium-depleted domains may exist in convecting mantle and that moderately high 3He/4He plumes likely do not contain a notable contribution of the deep mantle.