Xenolithic corundum aggregates in Cretaceous mafic pyroclastics from Mount Carmel contain pockets of silicate melts with mineral assemblages (SiC (moissanite), TiC, Ti 2 O 3 (tistarite), Fe-Ti-Zr silicides/phosphides) indicative of magmatic temperatures and oxygen fugacity (fO 2 ) at least 6 log units below the Iron-Wüstite buffer (IW≤-6). Microstructural evidence indicates that immiscible, carbon-rich metallic (Fe-Ti-Zr-Si-P) melts separated during the crystallization of the silicate melts. The further evolution of these metallic melts was driven by the crystallization of two main ternary phases (FeTiSi and FeTiSi 2 ) and several near-binary phases, as well as the separation of more evolved immiscible melts.Reconstructed melt compositions fall close to cotectic curves in the Fe-Ti-Si system, consistent with trapping as metallic liquids. Temperatures estimated from comparisons with experimental work range from ≥1500 °C to ca 1150 °C; these probably are maximum values, due to the solution of C, H, P and Zr. With decreasing temperature (T), the Si, Fe and P contents of the Fe-Ti-Si melts increased, while contents of Ti and C decreased. The increase in Si with declining T implies a corresponding decrease in fO 2 , probably to ca IW-9. The solubility of P in the metallic melts declined with T and fO 2 , leading to immiscibility between Fe-Ti-Si melts and (Ti,Zr)-(P,Si) melts. Decreasing T and fO 2 also reduced the solubility of C in the liquid metal, driving the continuous crystallization of TiC and SiC during cooling. The lower-T metallic melts are richer in Cr, and to some extent V, as predicted by experimental studies showing that Cr and V become more siderophile with decreasing fO 2 .These observations emphasise the importance of melt-melt immiscibility for the evolution of magmas under reducing conditions. The low fO 2 and the abundance of carbon This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.