Mild temperature gradient => ferns in Boreal Realm
pervasive tropical conditions
Geologic record Tr and Jr mostly
continental, little deep sea.
Cr => continental and deep sea. Subduction.
| The Break-up of Pangea | What continents? | How? |
|
|
|
Tethys to the W |
|
|
N Am from S Am |
|
|
|
S Am from
____________________ |
S ____________ overflow |
Ocean overflow in rift basins + arid climate = evaporites
_____________________ mark the beginning of rifting
Cr:
Gondwana splits
Antarctica & Australia from the rest
Africa from SAm; India moves N
_______________: Part of Gondwana left attached
________________ocean opens up
Impact of Sea Level, Climate and Ocean Circulation
Cr: ______________ ____________ ____________ activity => sea
level rose
Hot Mid Cr =>______________________ => black shales; cooler Lt
Cr, floras change
Poleward migration of hypersaline water
Slow wind driven atmospheric circulation (warmer climates)
MZ Geology of Eastern North America
Tr
fault basins:
alluvial fans
arkoses
Newark
_______________ _________________ (lakes with fish)
Supergroup
inter-layered ______________& _______________(Palisades Sill)
Jr
Carbonate shelf deposits => __________________
margin
Ea Cr
Siliciclastic sediments (Appalachian erosion, until today)
Carbonate sediments (S Fla)
MZ Geology of Western North America
Complex: succession of orogenies
Tertiary
Cordilleran
_____________
Cretaceous _____________
Orogeny (Subduction Pac Pl
Nevadan
Jurassic
under NAm Pl)
Triassic
_________________
Permian
Accretion
Sonoma Orogeny: Is arc & continent ______________ (SE OR,
CA and NV)
Nevadan Orogeny:
Sevier Orogeny:
Mid Cretaceous Transgression
When sediment supply was low and transgression maximum,__________________________
deposited in the center of the Interior Seaway.
Laramide Orogeny (Lt Cr)
Interior Seaway ___________ ( No more seas in the Western interior).