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400 million hp: Fossil bony fish in the Green River Formation
Main article: The history of the Earth before the appearance of hominids
Bony fish. At a junction called Fossil, near Kemmerer (Wyoming, USA), cliffs of marl limestones and clay shales are exposed. These are deposits of Eocene age that accumulated in one of the numerous lakes that extended into southwestern Wyoming and neighboring states of Utah and Colorado. These deposits are part of the Green River Formation. They are famous for the perfectly preserved fossil fish found in them in large numbers.
The group of fish to which the finds belong in the Green River Formation had the same skin structure as in sharks, but the inner skeleton of these fish has changed. Their complex inner skeleton was not built from cartilage, but from real bones, and more skin bones were added to the skull, jaws and shoulder girdle. Their caudal fins changed, and in more advanced shapes the tail took on a bilaterally symmetrical shape. After the Devonian extinction, when placoderms died out, bony and cartilaginous fish began to dominate the seas, having no competitors.

