“…However, as the concentrations of Al 3+ in the mantle are too low to meet this entire need, iron in the olivine disproportionates, with Fe 3+ deputizing for the lacking Al 3+ , while the native iron Fe 0 tends to gravitate to the core [ 61 , 62 , 63 , 85 ]. The result is a relatively oxidized volatisphere comprising CO 2 > H 2 O >> N 2 [ 85 , 124 , 125 , 126 , 127 , 128 , 129 , 130 , 131 , 132 , 133 , 134 , 135 , 136 , 137 , 138 , 139 ].…”