|
MYA |
EON |
ERA |
PERIOD |
EPOCH |
MAJOR EVENTS |
|
0.01 |
P |
C |
Quarternary |
Recent |
Development of agriculture and human civilization |
|
1.8 |
Pleistocene |
Appearance and world-wide spread of the genus Homo.
Repeated glaciations. Extinctions of large mammals and birds. |
|||
|
5.2 |
Tertiary |
Pliocene |
Continued diversification of modern birds, placental
mammals, snakes, teleost fish, pollinating insects, grasses and angiosperms. |
||
|
24 |
Miocene |
||||
|
34 |
Oligocene |
||||
|
56 |
Eocene |
||||
|
65 |
Paleocene |
||||
|
144 |
M |
Cretaceous |
Diversification of flowering plants, birds and mammals. |
||
|
206 |
Jurassic |
1st birds and angiosperms. Dinosaurs abundant. |
|||
|
251 |
Triassic |
1st dinosaurs and mammals. Gymnosperms become
abundant. Continents moving apart. |
|||
|
290 |
P |
Permian |
Diversification of reptiles, including mammal-like
species. Land masses form single continent, Pangea. |
||
|
354 |
Carboniferous |
1st reptiles and winged insects. Warm humid
conditions result in huge forests of primitive plants, which formed extensive
coal deposits. |
|||
|
409 |
Devonian |
1st amphibians and true insects. Atmospheric
oxygen at present levels or higher. Continents moving toward one another. |
|||
|
439 |
Silurian |
1st land plants. Atmospheric oxygen about 20
percent. |
|||
|
500 |
Ordovician |
1st fish. |
|||
|
543 |
Cambrian |
1st shelled organisms. Trilobites abundant.
Probably all metazoan phyla present, including arthropods and early
chordates. Atmospheric oxygen reaches about 2%. |
|||
|
2,500 |
PROTEROZOIC |
Abundant prokaryotic life. Eukaryotes may have appeared by
2,000 million years ago. Atmospheric oxygen about 0.2%. |
|||
|
3,600 |
ARCHEAN |
Oldest known rocks and prokaryotes. |
|||
|
4,600 |
HADEAN |
Earth forms. No geological record. |
|||
From Futuyma (1998), p. 130, using dates of Jablonski et al. (1996).