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Emergent Cambrian Period: 541 - 486 mya

Features of the Cambrian period: 541-485 mya

1) The oldest subdivision, or "lowest system" of the Paleozoic era, "characterized by the appearance of numerous animals (metazoans) bearing mineralized skeletons" (The Geologic Time Scale, p. 438).


2) Known as the Cambrian radiation, or Cambrian explosion, "an explosion in biotic diversity", due to the relative sudden appearance of many new animal body plans, and of "most multicellular phyla that have populated the Earth" (The Geologic Time Scale, pp. 437, 466) .

5) Small, cartilaginous, vertebrate fish begin to appear, and a dominance of trilobites.

ediacaran period 635-541mya

6) Seas gradually flood the continents, with a globally warm, greenhouse climate.

4) The first chordates appear: Pikaia - worm-like, with a visible, dorsal nerve cord, from the Burgess Shale, in B.C. - first thought to be an arthropod, but lack an exoskeleton and jointed legs.

3) The Age of Marine Invertebrates (mollusks; worms; sponges; echinoderms), the trilobites are the most widely used fossil group for biostratigraphic zonation, the best known group of Paleozoic arthropods (ibid., p. 467)

(marks the end of the Proterozoic eon, the beginning of the Phanerozoic eon, and the first period of the Paleozoic era

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