Diatoms constitute a vital part of the oceanic ecosystem. As they are dependent on silica, they are thought to have risen to prominence alongside grasslands in the Miocene epoch, when the first large-scale weathering of grassland-derived silica took place. A new analysis of an ocean-bed database contradicts that scenario; it is shown that diatom diversity peaked at the Eocene–Oligocene boundary, long before grasslands became prominent.
- Daniel L. Rabosky
- Ulf Sorhannus