ERA
|
PERIOD
|
AGE
(of start)
|
Cenozoic
|
|
1.6 my
|
|
65 my
|
Mesozoic
|
|
140 my
|
|
205 my
|
|
250 my
|
Paleozoic
|
|
290 my
|
|
355 my
|
|
410 my
|
|
438 my
|
|
510 my
|
|
540 my
|
|
Carboniferous 355 -290 million
years ago
Life
Dominant life includes:
Trees, ferns, amphibians, air-breathing
molluscs and insects
Development of amniotic egg by early reptiles
occurs
The early part of the Carboniferous, the
Mississippian, was heavily marine due to a rise in sea level.
The later part of the Carboniferous, the
Pennsylvanian, is known for its vast coal swamps that later
become the coal and petroleum that we use for energy.
The main rock types/ deposits in PA are
limestone, coal, and shale.
|