Download presentation
Presentation is loading. Please wait.
Published byGarey Barnett Modified over 6 years ago
2
Cambrian period, ~525mya. Gondwana (southern continent) beginning to form.
3
Permian period, ~275mya. Continents collide, forming Pangaea
Permian period, ~275mya. Continents collide, forming Pangaea. Lava flows, ash cools the atmosphere, huge glaciers, sea level drops, oceans turn over, toxic gases released. Result: Mass extinction.
4
Cretaceous period, ~140mya
Cretaceous period, ~140mya. Pangaea separates into southern (Gondwana) and northern (Laurasia) continents.
6
Dominant life forms of the past: some very broad generalizations
Precambrian: prokaryotes Cambrian-Ordovician: marine invertebrates, algae Silurian-Devonian: fish diversify, and remain the dominant group in the seas; land colonized Carboniferous-Permian: amphibians, insects, forests of ferns and seedless vascular plants. Mesozoic era: reptiles (inc. dinosaurs), gymnosperms Cenozoic era: mammals, flowering plants, new insects
7
BUT… These are dangerously broad generalizations, and only a starting point. Most groups originated long before they became dominant. (e.g. 1st reptiles in Carboniferous, 1st mammals in Triassic)
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.