I don't think that was a bug, looks like more of a sign of AI on the browser's part.

Minerals are just like any other chemical species on earth. They react with one another, and form into new and more diverse populations based on a variety of fundamental thermodynamic factors. Since the earth's processes have changed and evolved since planetary accretion, it only makes since that the assemblages of minerals we see on the earth would evolve in much the same way.
It appears that this paper focuses primarily on the biological effects on mineral speciation, but there have been a variety of geologic affects that have had equally profound impacts on the earths mineralogy (which in turns defines the variety of rocks we see). Factors such as the development of the earths core, mantle, and crust, plate tectonics, the development and evolution of our atmosphere and hydrosphere, and then of course the evolution of biota and related biogenic sedimentary rocks are all going to have an effect on the mineralogic evolution of the earth.