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Geologic Time Scale (Earth is 4.6 billion years old)

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Presentation on theme: "Geologic Time Scale (Earth is 4.6 billion years old)"— Presentation transcript:

1 Geologic Time Scale (Earth is 4.6 billion years old)
The Earth’s Past Geologic Time Scale (Earth is 4.6 billion years old)

2 Geologic Time Scale Time scale that outlines the development of Earth and of life on Earth Time scale divisions based on major changes in the Earth’s surface, climate, or types of organisms Time scale divisions usually based on dominant life forms

3 Geologic Time Units Eon Largest unit of time 4 eons Precambrian time
Hadean, Archean, Proterozoic, & Phanerozoic Precambrian time Hadean + Archean + Proterozoic Covers about first 4 billion years of the Earth

4 Geologic Time Units (continued)
Eons broken into Eras Phanerozoic  Paleozoic, Mesozoic, & Cenozoic Eras broken into Periods Periods broken into Epochs Epochs can be broken into Ages

5 Geologic Units Eons Eras Periods Smaller time units Epochs Ages

6 Eons and Eras

7

8

9 Geologic Columns An ordered arrangement of rock layers that is based on the relative ages of the rocks in which the oldest rocks are at the bottom Layers are distinguished by the type of rock and types of fossils in the rock

10 Grand Canyon Geologic Column

11 Grand Staircase Region
X X

12

13 X X X

14 Precambrian Time 4.6 Ga (Billion years) – 542 Ma (million years)
88% of Earth’s history Little known about this time Rocks are deformed and altered by tectonic activity

15 Precambrian Rocks & Life
Shields – large exposed Precambrian rocks Nearly ½ of valuable mineral deposits found in shields Life Very few fossils Stromatolites – blue-green algae deposits

16 Paleozoic Era 542 Ma – 251 Ma Land masses started out apart but ended up together (Pangaea) Rocks have lots of fossils Plant & animal species increase dramatically at beginning of era 7 Periods

17 Cambrian Period Marine life forms
Warm shallow seas cover much of the continents No evidence of land dwelling plants or animals

18 Ordovician Period Primitive fish Lots of invertebrates
First vertebrates (mostly fish) appear No plant life on land

19 Silurian Period Vertebrate and invertebrate marine life dominate
Land plants & animals evolve near end of period

20 Devonian Period “Age of Fishes” Amphibians
Land plants and seed bearing plants evolve

21 Carboniferous Period Includes Mississippian and Pennsylvanian Periods
Climate was warm and humid Forests and swamps responsible for coal deposits Amphibians, fish, large insects

22 Permian Period Appalachian Mountains created
Shallow inland seas disappear Mass extinction Many invertebrates die out Reptiles & amphibians survive

23 Mass Extinctions Used to indicate end of an era
Permian mass extinction 90% of marine organisms 70% of land organisms Plenty of resources for other species to begin to dominate

24 Mesozoic Era 251 Ma – 65.5 Ma Pangaea breaks apart to form continents
Mountain ranges form Sierra Nevadas, Andes “Age of Reptiles” Includes Triassic, Jurassic, & Cretaceous Periods

25 Triassic Period Dinosaurs – mostly 16 feet long Reptiles in the oceans
Ammonites – Mesozoic index fossil First mammals appear

26 Jurassic Period Dinosaurs become dominant life form
2 major groups of dinosaurs Saurischians – lizard hipped Herbivores & Carnivores Ornithischians – bird hipped Herbivores Flying reptiles First birds

27 Cretaceous Period Dinosaurs still dominate T Rex
Horned and duck-billed dinosaurs First flowering plants (angiosperms) Magnolias, willows, oaks, maples, walnuts

28 Cretaceous-Tertiary Mass Extinction
C-T Extinction End of Cretaceous Period No dinosaur fossils found in rocks formed after Cretaceous Period Due to environmental changes from continental movement or volcanic activity

29 C-T Extinction (continued)
Impact hypothesis Giant meteorite crashed into the Earth Produces dust that blocks the sun Planet cools, plant life dies off, animals die off Iridium near suspected impact site (Iridium is common in meteorites, but not Earth rocks

30 Cenozoic Era 65.5 Ma to present day
Continents move to present day position Alps and Himalayas form Ice ages Mammals become dominant

31 Cenozoic Era (continued)
Divided into 2 periods Tertiary Period Time before the last Ice Age Quaternary Period From last ice age to present day Divided into 7 epochs

32 Cenozoic Epochs Paleocene & Eocene Primates evolve
Whales, flying squirrels, bats Still lots of small reptiles Worldwide temp drops about 4oC at end of Eocene

33 Cenozoic Epochs (Continued)
Oligocene Uplifting of Himalayas World climate becomes much cooler & drier Grasslands favored Miocene Antarctic ice caps begin to form Mediterranean Sea fills and empties several times Large land mammals Earliest human ancestors(?)

34 Cenozoic Epochs (Continued)
Pliocene Dramatic climate changes Ice caps grow, water levels fall Alaska and Russia connected by Bering land bridge North and South America become connected Species migrate into different continents

35 Cenozoic Epochs (Continued)
Pleistocene Ice ages Fossils of earliest modern humans Holocene 11500 years ago as last ice age ends Sea level rises 140 m Great Lakes take their shape Humans develop agriculture and begin to use tools


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