“…[9] In simple ionic compounds, Fe typically coordinates with 4 or 6 anions, such as carbon, [10] pnictogens, [11] chalcogens, [12] and halogens, [13] with notable exceptions being Fe 7 O 10 and Fe 2 O 3 , [12a] which exhibit mixed coordination, [14] and 8-coordinated δ-Fe 3 O 4 [15] under high pressures. Numerous theoretical studies have proposed 8-coordinated Fe in two-dimensional FeB 6 and other highly compressed Fe-bearing solids, such as FeCl@300 GPa, [16] FeF 4 @116 GPa, [17] FeF 6 @274 GPa, [17] FeN 4 @250 GPa, [18] and FeOOHe@120 GPa, [19] among others. However, these configurations have not been experimentally confirmed, likely due to the challenges in preparing unconventional stoichiometric compounds and the technical limitations at ultra-high pressures.…”