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The geological time scale

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The Geologic Time Scale 4.6 Billion Years of Earth History
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Page 1: The geological time scale

The Geologic Time Scale

4.6 Billion Years of Earth History

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What is the Earth’s time scale?

• The Geological time scale is a record of the life forms and geological events in Earth’s history.

• Scientists developed the time scale by studying rock layers and fossils world wide.

• Radioactive dating helped determine the absolute divisions in the time scale.

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Divisions of Geologic Time• Eras are subdivided into periods...periods

are subdivided into epochs.Era

Period

Epoch

E + P = EP

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Divisions of Geologic Time

• Geological time begins with Precambrian Time. Precambrian time covers approximately 88% of Earth’s history.

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One Super Eon and Four Eras• PRE-CAMBRIAN Super Eon – 88% of earth’s

history

• Paleozoic (ancient life)– 544 million years ago…lasted 300 million yrs

• Mesozoic (middle life)– 245 million years ago…lasted 180 million yrs

• Cenozoic (recent life)– 65 million years ago…continues through present day

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Today…• Today we are in the Holocene Epoch of

the Quaternary Period of the Cenozoic Era.

Which unit is the largest?

Which unit is the smallest?

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Paleozoic Era (Ancient Life)• “The Age of Fish”• Starts: Cambrian period is the 1st period of the

Paleozoic Era. • “Explosion” of life in the oceans began during this era. • Most of the continents covered in warm, shallow seas.

– Invertebrates were dominant - Trilobites– Fish emerged during this time– Fish led to the arrival of amphibians – Early land plants including mosses, ferns and cone-bearing

plants.– The coal forming forests grew during this time

(Carboniferous Period)

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Paleozoic Era Con’t• The Appalachian mountains were formed during this

time.• The formation of Pangaea, as the Earth's continents

came together once again.

• Ends: Permian Period• the largest mass extinction in history wiped out up to

97% of all life on Earth.– Possible causes of this Mass Extinction Event

• Lowering of sea levels when the continents were rejoined as Pangaea (convergent boundary)

• Increased volcanic activity (ash and dust)• Climate changes – cooler climate

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Trilobites

• Lived in Earths ancient seas• Extinct before the dinosaurs

came into existence• Cambrian Period is know as

the “Age of the Trilobites”

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Eurypterids (New York State Fossil)Giant Sea Scorpion- largest known arthropods to ever live

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Brachiopods

• Marine animals that resemble bivalves such as clams.

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Early Fish

Early fish did not have jaws.

Some species of sharks were in existence at this time.

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Frilled Shark that was found in Japan in January 2007. This shark was considered a “living fossil”

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Early Land Plants

Cone bearing plants

Ferns

Mosses

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Mesozoic Era (Middle Life)• “The Age of Reptiles”• Start: Triassic Period

• Pangaea is still joined together, broke up around the middle of this era.

• Reptiles became the most abundant animals because of their ability to adapt to the drier climate of the Mesozoic Era.– Skin maintains body fluids– Embryos live in shells

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Mesozoic Era• Dinosaurs were very active in this era.

– First small dinosaurs appeared in the Triassic Period.

– Larger and more abundant dinosaurs appeared in the Jurassic Period.

• Small mammals and birds also appeared during this era.– The mammals were small, warm-blooded

animals. Hair covering their bodies.• These characteristics help them survive in

changing environments.

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Mesozoic Era• The main plant life of this time were Gymnosperms

or plants that produce seeds, but no flowers. – Pine Trees

• Flowering plants appeared during the END of this era.

• End: Cretaceous Period• This era ended with a mass extinction event about

65 million years ago.– Many groups of animals, including the dinosaurs

disappeared suddenly at this time.

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Mesozoic Reptiles

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Mesozoic Mammals

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Mesozoic Plants

Flowering plants evolved towards the end of the Mesozoic Era.

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Cenozoic Era (Modern Life)• “Age of Mammals”• Start: Paleocene Period• Starts 65 million years ago and continues today!!!!!

– Climate was warm and mild.– Marine animals such as whales and dolphins evolved.

• Mammals began to increase and evolve adaptations that allowed them to live in many different environments – land, air and the sea.– Grasses increased and provided a food source for grazing

animals• Many mountain ranges formed during the Cenozoic

Era– Alps in Europe and Himalayas in India; Rocky Mountains in

the USA

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Cenozoic Era• Ice Ages occurred late in the Cenozoic Era

(Quaternary Period).• As the climate changed, the animals had to

adapt to the rise and fall of the oceans caused by melting glaciers.

• Marine animal examples:– Algae, Mollusks, Fish and Mammals

• Land animal examples:• Bats, Cats, Dogs, Cattle and Humans

• End: ??? TBD

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Cenozoic Mammals

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Flowering Plants were common during the Cenozoic Era


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