Geologic time scale_1

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Geologic Time Scale

Transcript of Geologic time scale_1

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Geologic Time Scale

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Imagine putting everything that has happened on Earth into a

one hour time frame!

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Geologic Time in 24 Hours

• 12:00am – Earth forms

• 7:00am - Earliest one-celled organisms appear.

• 7:00am-9:00 pm- Simple, soft-bodied organisms like worms

• Little past 9:00pm - Complex organisms evolve in oceans

• Little past 10:00pm - Reptiles and insects first appear

• Just before 11:00pm - Dinosaurs arrive

• 11:30pm - Dinosaurs go extinct

• 11:59:59 - Humans appear one second before midnight

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Geologic Time ScaleA record of the life forms and geologic events in

Earth’s history.

Scientists placed Earth’s rocks in order by relative ageto create the geologic column.

We developed the scale by studying these rock layersand index fossils.

Radioactive dating helped us determine the absolutedate of the divisions in the scale.

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Geologic Time Scale

OLD

NEW

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Divisions of Geologic TimeAs 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.

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Divisions of Time• EON – largest division of geologic time

• ERA – 2nd largest, includes two or more periods

• PERIOD – 3rd largest, unit into which eras are divided

• EPOCH – 4th largest, the subdivision of a period

EON > ERA > PERIOD > EPOCH

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Why is a time scale used to represent Earth’shistory 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 ofthe Cenozoic Era.

How long is a geologic period?A period doesn’t have an exact length.

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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

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ERAS

• Paleozoic – “early life” 544 244 mya

• Mesozoic – “middle life” 245 66 mya

• Cenozoic – “recent life” 66mya present

Which one do you live in today?

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PERIODSCambrian – Explosion of lifeOrdovician – 1st Vertebrates

Silurian – 1st Land PlantsDevonian – Age of Fish

Mississippian – Winged insectsPennsylvanian – First reptilesPermian – Age of Amphibians

Triassic – First Dinosaurs/Small mammalsJurassic – First Birds/Flowering Plants

Cretaceous – Heyday of DinosaursTertiary – Mammals Thrive

Quaternary – Age of Man/Technology

PAST

PRESENT

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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.

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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.

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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

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Mass ExtinctionOccurs when many living things go extinct at the same time (Impacts

plants and animals on land and in sea)

• Only happened twice in Earth’s history.

• 1st: Between Paleozoic and Mesozoic Eras– Trilobites suddenly went extinct. Think 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.

• 2nd: Between Mesozoic and Cenozoic Eras– Wiped out over half of all plant and animal groups on Earth. No dinosaurs survived

Two TheoriesAsteroid 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.

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Most Accepted Theory

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Cambrian Period• Cambrian Explosion-so many new life forms

appeared within a short time.• 1st 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.

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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.

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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.

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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.• 1st vertebrates on land were lungfish. 1st

amphibians evolved from the lungfish.

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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”

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Triassic Period• Fish, insects, reptiles and cone bearing trees

survived Permian extinction.• 1st dinosaurs appear.• 1st mammals appear-size of mouse.• 1st turtles and crocs appear.• Conifers, palm-like trees (cycads), ginko trees

dominate forest.• Pangaea holds together. Hot, dry conditions

dominate center of Pangaea.

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Jurassic Period• Dinosaurs become dominant land animal.• Some were plant eaters, some were meat

eaters.• Different types lived at different times.• 1st birds appear. Archaeopteryx means

“ancient wing thing.”• 1st flying reptiles-pterosaurs appear.• Pangaea breaks apart-N. America and S.

America separate.

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Cretaceous Period• Continents moved toward present location.• Widespread volcanic activity.• Flying reptiles and birds competed.• Birds hollow bones and feathers made them better

adapted.• 1st flowering plants. Flowering plants produce

seeds that are inside fruit. Fruit helps seed survive.

• Dinosaurs dominate-T-rex.• 1st snakes appear.

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Tertiary Period• Climate was warm and mild.• Rockies and Himalayas form.• Continental glacier covers Antarctica.• 1st grasses appear-provide food source

for grazing animals. (ancestors of cattle, deer, sheep.)

• Flowering plants thrive.• Ancestors of humans evolve.

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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.