paleozoic and moving continents
how wind and ocean affect climate
land masses move via:
continental drift
- plate techtonics
- drive movement of layer on top
- due to major intersection of pacific and ()
- himilayas –> indian subcontinent colllieded into an asian subcontinent
- euramerica — present day north america/greenland/europe
paleozoic climates
devonian
what was the first major evolutionary innovation
amniotic split of the tetrapods
late devonian extinction
permian extinction
late paleozoic extinction
series of volcanic eruptions
- yes, there was a large section of terresterial earth that was covered in lava, but what really causes the mass extinction was that the volcanos were releasing various types of greenhouses gases –> raised atmosphere by 6 degrees celcius –> major greenhouse effect –> causes a warming that thawed previously frzen gases –> runaway positive feedback loop
mechanism of greenhouse effect
^^ gasses are like the window
- allow for light to come in but the wavelength changes when the light bounces off of earth and various objectes in earth