Geologic Time Scale Imagine putting everything that has

Geologic Time Scale

Imagine putting everything that has happened on Earth into a one hour time frame!

Geologic Time in 24 Hours • 12: 00 am – Earth forms • 7: 00 am - Earliest one-celled organisms appear. • 7: 00 am-9: 00 pm- Simple, soft-bodied organisms like worms • Little past 9: 00 pm - Complex organisms evolve in oceans • Little past 10: 00 pm - Reptiles and insects first appear • Just before 11: 00 pm - Dinosaurs arrive • 11: 30 pm - Dinosaurs go extinct • 11: 59 - Humans appear one second before midnight

Geologic Time Scale Definition: A record of the life forms and geologic events in Earth’s history. Scientists placed Earth’s rocks in order by relative age to create the geologic column. We developed the scale by studying these rock layers and index fossils. Radioactive dating helped us determine the absolute date of the divisions in the scale.

NEW Geologic Time Scale OLD

Divisions of Geologic Time As they studied the fossil record, they found major changes in life forms at certain times. They used these changes to mark where one unit of geologic time ends and the next begins. Divisions of the geologic time scale depend on events in the history of life on Earth.

Divisions of Time • EON – largest division of geologic time • ERA – 2 nd largest, includes two or more periods • PERIOD – 3 rd largest, unit into which eras are divided • EPOCH – 4 th largest, the subdivision of a period EON > ERA > PERIOD > EPOCH

Why is a time scale used to represent Earth’s history instead of a calendar? Earth’s history is so long When did Geologic time begin? 4. 6 billion years ago When does Geologic time end? It doesn’t. We are now in the Quaternary Period of the Cenozoic Era. How long is a geologic period? A period doesn’t have an exact length.

EONS • Hadean – rocks from meteorites and moon • Archean – earliest rocks on earth form • Proterozoic – organisms with well developed cells • Phanerozoic – means “visible life” well represented in the fossil record

ERAS • Paleozoic – “early life” • Mesozoic – “middle life” 544 244 mya 245 66 mya • Cenozoic – “recent life” 66 mya present Which one do you live in today?

PERIODS PAST PRESENT Cambrian – Explosion of life Ordovician – 1 st Vertebrates Silurian – 1 st Land Plants Devonian – Age of Fish Mississippian – Winged insects Pennsylvanian – First reptiles Permian – Age of Amphibians Triassic – First Dinosaurs/Small mammals Jurassic – First Birds/Flowering Plants Cretaceous – Heyday of Dinosaurs Tertiary – Mammals Thrive Quaternary – Age of Man/Technology

Remember…Early Earth • Earth formed 4. 6 billion years ago. • Scientists think that Earth began as a ball of dust, rock and ice. • Gravity pulled this mass together. • As Earth grew larger, gravity increased. Pulled in nearby dust, ice and rock. • As objects hit Earth at high speeds, their energy changed into thermal energy. • Energy from collisions caused Earth’s temp to rise until planet was very hot. • Scientist believe Earth may have become so hot it melted. • Denser materials sank toward the center—formed Earth’s dense iron core. • At same time, Earth continuously lost heat to cold of space. • Less dense molten material hardened to form Earth’s outer layers. Oceans form.

Life Develops • We have fossils of single-celled organisms in rocks that formed 3. 5 billion years ago. . . probably in early ocean • Primordial Ooze – water contained the building blocks of life • Similar to present day bacteria. • About 2. 5 billion years ago, simple organisms began using energy from sun to make their own food. • Photosynthesis slowly released oxygen into air.

Cyanobacteria are some of the oldest organisms on Earth, at least 3. 5 billion years old Filamentous procaryotic microfossils from 3. 5 Billion year old black cherts of the Archean Warrawoona Group

Mass Extinction Occurs when many living things go extinct at the same time (Impacts plants and animals on land in sea) • 1 st: Between Paleozoic and Mesozoic Eras -Wiped out 90% of all life. Known as “The Great Dying” – Trilobites suddenly went extinct. Climate change from continental drift may have caused extinction. Formation of Pangaea caused deserts to expand in tropics. Sheets of ice covered land closer to South Pole. Organisms could not survive. • 2 nd: Between Mesozoic and Cenozoic Eras – Wiped out over half of all plant and animal groups on Earth. No dinosaurs survived Two Theories Asteroid hit earth. Impact threw huge amounts of dust and water into atmosphere blocking sunlight. No sun = plants died and plant eating animals starved. Clouds also caused temperatures to drop. Climate changes were caused by increased volcanic activity. Volcanic output would block sun as well and same process would follow.

Most Accepted Theory

Cambrian Period • Cambrian Explosion-so many new life forms appeared within a short time. • 1 st time organisms had hard parts-shells and outer skeletons. • All animals lived in the sea. • Many were invertebrates-jellyfish, sponges, worms drifted through the water. • Brachipods (clams) and trilobites were common in the Cambrian seas.

Ordovician Period • • Seas still cover the earth Ice cap covers what is now North Africa. Ancestors of squid and octopus appear. Jawless fish evolve—first vertebrates.

Silurian Period • Coral reefs develop. • Prior to this period, only one-celled organisms lived on land. Land plants appear. • Fish with jaws appear. • Insects and spiders appear.

Devonian Period • Often called Age of Fishes. • Every main group of fishes were present in the ocean. • Most fish had jaws, skeletons and scales on their bodies. • Sharks appeared late in the period. • Animals begin to invade land. • 1 st vertebrates on land were lungfish. 1 st amphibians evolved from the lungfish.

Carboniferous Period • Broken into Mississippian and Pennsylvanian. • Life expanded over continents. Appalachian Mountains began to form. • Small reptiles developed • Winged insects evolved-huge dragonflies and cockroaches. • Giant ferns & cone bearing plants and trees formed. “Coal forest”

Triassic Period • Fish, insects, reptiles and cone bearing trees survived Permian extinction. • 1 st dinosaurs appear. • 1 st mammals appear-size of mouse. • 1 st turtles and crocs appear. • Conifers, palm-like trees (cycads), ginko trees dominate forest. • Pangaea holds together. Hot, dry conditions dominate center of Pangaea.

Jurassic Period • Dinosaurs become dominant land animal. • Some were plant eaters, some were meat eaters. • Different types lived at different times. • 1 st birds appear. Archaeopteryx means “ancient wing thing. ” • 1 st flying reptiles-pterosaurs appear. • Pangaea breaks apart-N. America and S. America separate.

Cretaceous Period Continents moved toward present location. Widespread volcanic activity. Flying reptiles and birds competed. Birds hollow bones and feathers made them better adapted. • 1 st flowering plants. Flowering plants produce seeds that are inside fruit. Fruit helps seed survive. • Dinosaurs dominate-T-rex. • 1 st snakes appear. • •

Tertiary Period Climate was warm and mild. Rockies and Himalayas form. Continental glacier covers Antarctica. 1 st grasses appear-provide food source for grazing animals. (ancestors of cattle, deer, sheep. ) • Flowering plants thrive. • Ancestors of humans evolve. • •

Quarternary Period • Climate cooled-causing a series of ice ages. • 20, 000 years ago climate began to warm. • Modern humans-Homo sapiens evolved as early as 100, 000 years ago. 12, 000 -15, 000 humans had migrated around the world. • Mammals, flowering plants and insects dominate land. • Giant mammals of N. America and Eurasia become extinct.