1 / 18

Earth History: Geologic Time

Earth History: Geologic Time. Geologic Time. Geologic Time: It is very, very long. Earth is estimated to be around 4.7 billion years old based on the rock and fossil record. Geologic time is broken up into sections based on major changes in Earth. Divisions of Geologic Time.

jennad
Download Presentation

Earth History: Geologic Time

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Earth History: Geologic Time

  2. Geologic Time • Geologic Time: It is very, very long. • Earth is estimated to be around 4.7 billion years old based on the rock and fossil record. • Geologic time is broken up into sections based on major changes in Earth .

  3. Divisions of Geologic Time Largest Division: Eons • Eons divided into Eras: • PreCambrian, Paleozoic, Mesozoic, Cenozoic • Ceno - recent • Meso - middle • Paleo - ancient • Zoic - life • Eras are divided into Periods

  4. PreCambrian543 million years ago to ~ 4 billion years ago (?) • “Age of Bacteria” • Oldest Era • Longest era because we know so little about the earth that long ago • Life: Very little life: only basic forms including bacteria, the oldest fossils ever found, seaweed, jellyfish, and worms • Photosynthesis of the seaweed added oxygen to the early atmosphere, paving the way for land life.

  5. First Life One celled plants (algae) entered the fossil record approximately 3 b.y. ago (Precambrian). Large colonies of this algae are called stromatolites.

  6. More Atmospheric Changes Through photosynthesis, O2 was released into the atmosphere and ocean allowing animals to eventually evolve.

  7. Paleozoic543 million years ago to 248 million years ago • “Age of the Fish” • Explosion of life in the sea: trilobites, shellfish, Fish • Life appears on land: Ferns, Amphibians • Pangaea formed • Largest mass extinction ever at the end of the Paleozoic. 90% of species became extinct.

  8. Paleozoic Organisms

  9. Carboniferous Time In Europe the Mississippian and Pennsylvanian periods are together called the Carboniferous period. Vast swamps and forests from that time created the huge coal beds found throughout eastern United States.

  10. Mesozoic248 mya- 65mya • “Age of the Reptiles” • Life: Reptiles are the dominant life on land. Dinosaurs exist. Birds appear. Forests of trees appear • Pangeabroke apart during this peroid. • Dinosaurs become extinct in a mass extinction at the end of the Mesozoic.

  11. Reptiles: …until Dinosaurs took over. Appeared in the Permian and quickly became the dominant life form. They ruled the planet throughout the Mesozoic era (the “Age of Dinosaurs”).

  12. Birds Some of the dinosaurs are thought to have evolved into birds. Archaeopteryx is the oldest fossil bird found to date.

  13. Dinosaur Extinction 2.Meteoriteimpact causes multiple natural disasters 1. Volcanoeserupt and fill the atmosphere with CO2 and gasses that BLOCK the sun light preventing plant life…….

  14. Evidence of a Meteorite • Layer of Iridium in rock layers

  15. Cenozoic65 mya- present • “Age of the Mammals” • Life: Large mammals appear, Humans appear • Ice Ages occur and ice sheets advance

  16. Mammals Mammals first appeared in the Mesozoic as small rodents. After the dinosaurs were erased at the end of the Mesozoic, Mammals quickly evolved to become the dominant life form. The Cenozoic is the “Age of Mammals”.

  17. Present We live in the Holoceneepoch, of the Quaternaryperiod, of the Cenozoicera.

More Related