-
541 BCE
Marine life diversifies enormously
-Many marine invertebrates with external skeletons (arthropods)(Cambrian)
- Widespread marine algae(Ordovician)
-Fish without jaws(Ordovician) -
541 BCE
Rodinia breaks up
Rodinia was a supercontinent that brought together a large part of the earth's landmass, which began to break down due to magmatic movements in the earth's crust, accompanied by strong volcanic activity. -
Period: 541 BCE to 252 BCE
Paleaozoic Era
-
Period: 541 BCE to 485 BCE
Cambrian
-
Period: 485 BCE to 444 BCE
Ordovician
-
444 BCE
First great extinction
-First land plants(Silurian)
-Fish diversify(Devonian)
-First amphibians(Devonian)
-Forests of giant ferns(Carboniferous)
-First reptiles(Carboniferous)
-Reptiles diversify(Permian) -
444 BCE
Caledonian orogery
The Caledonian orogeny was a mountain-building process that occurred in Scotland, Ireland, England, Wales, and western Norway. -
Period: 444 BCE to 419 BCE
Silurian
-
Period: 419 BCE to 359 BCE
Devonian
-
359 BCE
Pangea forms
Pangea was the great supercontinent that existed at the end of the Paleozoic era and the beginning of the Mesozoic era, which included most of the landmass on the planet. -
Period: 359 BCE to 299 BCE
Carboniferous
-
Period: 299 BCE to 252 BCE
Permian
-
252 BCE
The Earth greatest extinction occurs Pangea forms
-First dinosaurs(Tirassic)
-Firs mammals(Tirassic)
-Gymnosperm plants dominate the Earth's surface(Jurassic)
-Dinosaurs diversify(Jurassic)
-First flying and aquatic reptiles(Jurassic)
-First birds(Jurassic)
-First plants with flowers(Cretaceous)
-Extinction of dinosaurs and anmonites(Cretaceous) -
Period: 252 BCE to 66 BCE
Mesozoic Era
-
Period: 252 BCE to 201 BCE
Tirassic
-
201 BCE
Pangea begins to break up
Scientists believe that Pangea broke apart for the same reason that the plates are moving today. The movement is caused by the convection currents that roll over in the upper zone of the mantle. -
Period: 201 BCE to 145 BCE
Jurassic
-
Period: 145 BCE to 66 BCE
Cretaceous
-
66 BCE
Massive extinction from meteorite impact
-Development and diversification of mammals(Tertiary and Quaternary) -
66 BCE
Alpine orogeny begins
The Alpine Orogeny is a mountain-building stage that occurred during the Cenozoic, when Africa, the Indian subcontinent, and the small Cimmerian plate collided with Eurasia. -
Period: 66 BCE to 2
Cenozoic Era
-
Period: 66 BCE to 2 BCE
Tertiary
-
Period: 2 BCE to 20
Quaternary