Title: History of life Cont The Phanerozoic Eon
1History of life Cont The Phanerozoic Eon
- Paleozoic Era "time of ancient life" (544 and
245 mya) - spread of animals with hard preservable parts
such as shells and exoskeletons.
2The Paleozoic Era
- Cambrian
- Ordovician
- Silurian
- Devonian
- Carboniferous
- Mississippian
- Pennsylvanian
- Permian
3Cambrian Period 550 505 mya
- Cambrian Explosion sudden appearance of a
stupendous array of animal life, most not closely
related to modern forms. - The Burgess Shale best fossil assemblage
showing cambrian explosion. - Ancestors of almost all major groups of life
developed. - Trilobites primitive ex of exoskeleton -
4End of Cambrian Period
- Glaciation in parts of the world
- ended in the greatest mass extinction in world
history. - nearly 96 of all marine species went extinct.
- Unknown cause
5Ordovocian Period - 505 to 440 mya
- Following the extinctions at the close of the
cambrian period, diversification occurred among
the survivors. - Corals become dominant reef-building animals -
(How old are our coral reefs then)? - First land plants.
- First fish
6The Silurian period 440 410 mya
- Eukaryotic life colonized terrestrial
environments. - adaptive radiation The development of a
variety of species from a single ancestral form - Major flooding of continents as glaciers melt
- Vascular plants (transport tissue allowed for
height
7Crinoids common in midwest
- stems were so common in some areas of the U.S.
midwest that native peoples used them as a form
of currency. - significant elements of the marine fauna until
they nearly went extinct at the close of the
Permian period. - Echinoderms (same group as starfish sand
dollars).
8Devonian period 410 to 360 mya
- diversification of life on land,
- first terrestrial vertebrates, the amphibians
(frogs) - first forests of trees
- Invertebrates such as crinoids, coral, and
brachiopods thrived in shallow seas - Brachiopods primitive clam-like animals
9Devonian Rhynie Chert
- Scotland - groups of early vascular land plants
have been discovered in excellent condition in
specimens where silicification of the plants
occurred while they were still alive and growing. - minute detail preserved showing reproduction
- diverse fossils of fungi
10Devonian cont
- Ferns
- New forms of arthopods
- Global cooling
- Devonian extinction of crinoids, most coral,
triolobites, primitive fish
11The Carboniferous period 360 to 286 mya
- Coal laid down - Swamps
- Known in North America as the Mississippian
period and the Pennsylvanian period due to
receeding seas - Both Mississippian Pennsylvanian in IL
12Carboniferous cont
- Sharks, bony fish (I.e. blue-gill, perch)
- Gymnosperms (pine trees)
- Amphibians, reptiles
- insects
- Glaciation stopped swamp creation no more coal
forming
13The Permian period 286 to 245 - mya
- Reptiles gaining dominance
- Another mass extintion
- 90 of all species eliminated
- Cleared the way for the dinosaur age
- Pangea
14The Mesozoic Era 245 65 mya
- Triassic period
- Jurassic period
- Cretaceous period
15Triassic Period 245-208 mya
- Octopus
- Ginko
- Iythosaurus marine dinosaur
- Crocodiles, Modern turtles
- Gondwana in the south (composed of the future
continents of South America, Africa, India,
Antarctica, and Australia) and Laurasia in the
north (Asia and North America).
16Jurassic period 208 to 146 mya
- Dinosaurs
- Atlantic ocean formed
- New coral reefs emerged
- New plant species Angiosperms
- Swimming, walking, flying reptiles
- Giant reptiles
17Jurassic cont
- Archaeopteryx, once considered the first bird.
The fossil is from the Solnhoefen Limestone
(Jurassic) of Germany. - China bird-reptile fossils support
18Cretaceous period 144 to 65 mya
- Temperate climate
- Ended with mass extinction of dinosaurs and much
other life - Current theory asteroids cooling climate
-Chicxulub in Yucatan, Mexico
19Cenozoic Era 65 mya to present
- Age of mammals birds
- Glaciation alters species
- 7 continents form