Remnants of Gondwanan continental lithosphere in oceanic upper mantle: Evidence from the South Atlantic Ridge

Dredged glass from the southern Mid-Atlantic Ridge near the Bouvet Triple J unction has unique major element, trace element, and isotopic composition, distinct from typical mid-ocean ridge basalts, It is a high-Mg (Mg# 67.8), high-Ni (NiO 290 ppm) andesite depleted in highly incompatible and heavy ra re-earth elements with an isotopic signature of ancient continental lithosp here (i.e., low (206)pb/(204)pb and Nd-143/Nd-144 and high Sr-87/Sr-86 and delta O-18). The origin of this glass is attributed to melting of a Precamb rian garnet-bearing, mafic lithology, possibly related to lower crustal blo cks stranded in the upper mantle during breakup of Gondwana and opening of the Atlantic. This composition can be used to explain anomalous geochemical features of oceanic rocks in the Southern Hemisphere.