First Land Plants: How Plants Colonised the Land
Plants evolved from freshwater green algae, colonised the land and began to create soils, alter the atmosphere and form the basis of land ecosystems.
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Plants evolved from freshwater green algae, colonised the land and began to create soils, alter the atmosphere and form the basis of land ecosystems.
Eurypterids flourished for more than 200 million years, produced the largest known arthropods, and died out in the end-Permian extinction.
An estimated 85% of marine species died out in two pulses, but the main Paleozoic groups survived and recovered in the Silurian.
Roughly three-quarters of marine species disappeared in several pulses; the great Devonian reef systems collapsed and the armoured placoderm fishes died out.
Buried peat from swamp forests turned into thick coal seams that later fuelled the Industrial Revolution.
All major continents were joined for over 100 million years before rifting apart in the Jurassic to form the Atlantic Ocean and today's continents.
Glossopteris fossils on all the southern continents became one of the strongest early arguments that they had once formed a single landmass.
CT scans in 2013 showed the tooth whorl sat inside the lower jaw and that Helicoprion was related to ratfishes rather than true sharks.
An estimated 80 to 90 percent or more of marine species and around two-thirds or more of land vertebrate species died out, ending the Paleozoic Era and reshaping life for the Mesozoic.
Roughly three-quarters of marine species and many land reptile groups died out, leaving dinosaurs as the dominant large land animals of the Jurassic.
Pangaea split into the northern landmass Laurasia and the southern landmass Gondwana, the Central Atlantic Ocean opened, and the continents began moving towards their modern positions.
A global mass extinction wiped out the non-avian dinosaurs and around three-quarters of plant and animal species, ending the Cretaceous Period.