The discussion focuses on the difficulty of finding comprehensive data on the Earth's composition by compounds rather than elements. It highlights that the mantle, which constitutes two-thirds of Earth's mass, is primarily composed of silicates, particularly SiO2, which is significantly more abundant than water (H2O) in terms of total mass. The crust and mantle are complex, with many minerals existing as solid solutions rather than distinct compounds. The ocean, while covering a large portion of the Earth's surface, contributes minimally to the planet's overall mass. The conversation also touches on the role of the atmosphere and the presence of noble gases, although these do not significantly alter the overall composition.