Lecture 7 Flashcards
(39 cards)
Cambrian Period
541 - 485 Ma
- complex life emerges
cambrian explosion start
538.8 Ma
when did all principal animal groups develop by
530 to 520 Ma
ordovician period
485 - 444 Ma
epeiric
shallow inland seas
ordovician queenston clastic wedge in NE recorded as
queenston shale, whirlpool sandstone, grimsby shale and thorold sandstone
silurian period
444 - 419 Ma
mid-silurian record in NE
Neahge, Reynales, Irondequoit, Rochester, and Lockport
mass extinctions
episodes of globally-significant extinctions
- more than 20% of marine genera
- 75% of all species
Five Phanerozoic mass extinctions
(Late) Ordovician, Devonian, Permian, Triassic, Cretaceous
Devonian Period
419 - 359 Ma
- age of the fishes
- life starts going to land
Mississippian
359 - 323 Ma
Pennsylvanian
323 - 299 Ma
Carboniferous period
359 - 299 Ma
- plant life propogates
- coal develops - carbon sequestration
Permian period
299 - 252 Ma
first animal to walk on land
Ichthyostega, but the tiktaalik was a transition form
when did Myria;ods start to conquer land
414 Ma
oldest sea floor
340 Ma in the Mediterranean Sea
average sea floor age
200 Ma
middle ordovician continental layout
deep ocean basin between laurentia and baltica (Iapetus ocean)
middle silurian continental layout
laurentia and baltica touching, no sea between
early devonian continental layout
euramerica being created as laurentia and baltica get pushed together. taconic mountains is being created
late carboniferous continental layout
pange has been formed from laurussia and gondwana fusing together 310 Ma, and the taconic mountains are done being created. most of the continental pieces are together
late permian continental layout
almost all of the continental pieces are together