2: Overview of Plant Evolution Flashcards
Cambrian to Ordovician (544-541 MYA
Tectonic activity Reorganisation of continental plates (volcanoes brought new soil Ordovician started & ended with an extinction event Time of dramatic sea level changes
Sea Level Changes
1) Rises
2) Falls
1) warmed it gets the more ice melts on the poles and sea level rises
2) cooler more ice gets taken more water turns into ice at the poles and sea level falls
Silurian (444-419 MYA
Dramatic sea level changes
First land plants emerged (Cooksonia
Devonian (419 - 360 MYA
Laurasia & Gondwana drew closer together (plants spread)
Sea level high
Spore bearing trees by the end of period
Emergence of clubmosses, ferns, horsetails & progymnosperms
Lycophytes / Lycopsids
(Identify
Clubmosses
Pterophyta / Filicopsids
(Identify
Ferns
Equisetales / Sphenopsids
(Identify
Horsetails
Carboniferous (360 - 300 MYA
Pangea formed
Rise in sea level created inland seas and swamps (became coal deposits
Permian (300 - 252 MYA
Seed plants dominated Emergence of ginkgos, cycads & glossopteridaceae Conifers evolved & started to radiate Early (ice age), Late (Dried out) Pangea 80% vegetative
Triassic (252 - 200 MYA
Pangea drifted into Gondwana & Laurasia (mid period)
Period started & ended with mass extinction
Seed plants start to dominated (high atmos CO2)
Jurassic (255 - 145 MYA
Laurasia (north)
Gondwana (south)
Arid continental conditions (no ice)
Confers flourished
Creataceous (145 - 66 MYA
Angiosperms, (flowering plants), emerged at 140 MYA
Within 60 million year they attain ecological dominance due to their adaptive behaviour
What drives evolution in plants
Changes in environmental conditions