- CaSiO3 perovskite in diamond indicates the recycling of oceanic crust into the lower mantle. Nature. 555:237-241.
- Source assemblage types for cratonic diamonds from X-ray synchrotron diffraction. Lithos. 265:334-338.
- Structural characterization of natural diamond shocked to 60GPa; implications for Earth and planetary systems. Lithos. 265:214-221.
- Wampenite, C18H16, a new organic mineral from the fossil conifer locality at Wampen, Bavaria, Germany. European Journal of Mineralogy. 29:511-515.