Paleozoic Era
An age of early land plants and animals
The Paleozoic Era (539–252 Ma) is in the Phanerozoic Eon, occurring after the Neoproterozoic Era, and before the Mesozoic Era. It is a time for great plant innovation and evolution. During this time land plants evolve and emerge from water, begin as lowly moss-sized plants, and become towering trees by the end of the Devonian Period. Every major group of plants evolves during this time: mosses, liverworts, hornworts, clubmosses, ferns, horsetails, and seed plants. It is a time when plants evolve structures that are commonplace today: branching stems, roots, leaves, wood, and seeds.
Geologic Age
538.8±0.2 Ma–252 Ma million years ago
Subdivisions
Permian: 299–252 Ma
Carboniferous: 359–299 Ma
Devonian: 419–359 Ma
Silurian: 444–419 Ma
Ordovician: 485–444 Ma
Cambrian: 539–485 Ma
Eon
What happened during this time?
7% of geologic history; 53% of Phanerozoic
Diversification of eukaryotic life
Rise and diversification of algae, plants, and fungi
Macro-algae diversify
Parasitic, saprophytic fungi
Land plants originate:
Origin of vascular tissue, leaves, roots, wood, and seeds
The rapid diversification of animal phyla
Invertebrates: sponges, mollusks, worms, crustaceans
Chordates: fishes, amphibians, reptiles