Hauke was invited to present the group’s recent work at the fall meeting of the American Geophysical Union (AGU) in San Francisco. The talk entitled “Deformation of (Mg,Fe)O Ferropericlase to Temperatures of 1150 K and Pressures of 96 GPa: Implications for Mantle Flow and Seismic Anisotropy” was scheduled in the session „The Role of Transition Elements in the Geophysical and Geochemical Processes in the Deep Earth“.