Links to help understand the immensity of the Geologic Time Scale http://www.bonnechere.ca/naturalhistory.htm http://comp.uark.edu/~sboss/geotime.htm http://www.britannica.com/EBchecked/media/1650/The-geologic-time-scale-from-650-million-years-ago-to http://science.nationalgeographic.com/science/prehistoric-world/prehistoric-time-line/ http://www.geology.wisc.edu/~museum/hughes/TimeScale.pdf http://www.rocksinmyheadtoo.com/TimeLine.htm http://www.bbc.co.uk/nature/history_of_the_earth http://geology.com/time.htm https://www.youtube.com/watch?v=r10oh1NHKv4&safe=active https://www.youtube.com/watch?v=7PQURsc2SYs http://www.classzone.com/science_book/mls_grade7_FL/473_479.pdf http://www.ucmp.berkeley.edu/education/explorations/tours/geotime/index.html http://www.bgs.ac.uk/discoveringGeology/time/timeline/home.html http://archive.fieldmuseum.org/evolvingplanet/POST/EP_V8.swf https://www.youtube.com/watch?v=bxDxDE666vw&safe=active http://www.pbs.org/wgbh/nova/evolution/brief-history-life.html http://www.earthsciweek.org/classroom-activities/geologic-time-scale-analogy http://www.uh.edu/~jbutler/physical/chap9mult.html Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Knowing the Acronyms b.y.a.. = __________________________ m.y.a. = _________________________ Things to know about the Geologic Time Scale Beginning of the Earth ________________ b.y.a. ➜ The beginning of the Hadean Eon was _________________ b.y.a. ➜ The beginning of the Archeozioc Eon was ___________________ b.y.a. ➜ The beginning of the Proterozoic Eon was ________________ b.y.a. ➜ The beginning of the Phanerozoic Eon was _________________ m.y.a. ✱ The beginning of the Paleozoic Era was ___________________ m.y.a. ✱ The beginning of the Mesozoic Era was _________________ m.y.a. ✱ The beginning of the Cenozoic Era was ___________________ m.y.a. ✦ The last Period of the Cenozoic Era is the quarternary period which began ___________________ m.y.a ✧ The last epoch of the Cenozoic Era was the Holocene epoch which began ____________________ years ago. Examples ➜ Trilobite Found in the _________________ era and first appeared ________________m.y.a. ➜ First appearance of fish Found in the ________________ era and first appeared ___________________ m.y.a. ➜ Tyrannosaurus rex Found in the _________________ era and first appeared _______________ m.y.a. ➜ Homo sapiens (humans) Found in the __________________ era and first appeared _______________ years ago Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons Attribution-NonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA. Eon Era Period Mesozoic Era Paleozoic Era Phanerozoic Eon Cenozoic Era Neogene Millions of years ago Today – 23 Paleogene 23 – 65 Cretaceous 65 – 145 Jurassic 145 – 200 Triassic 200 – 251 Permian 251 – 299 Carboniferous 299 – 359 Devonian 354 – 417 Silurian 417 – 443 Ordovician 443 – 488 Cambrian 488 – 543 Proterozoic Eon 543 – 2,500 Archean Eon 2,500 – 3,800 Hadean Eon 3,800 – 4,570 Major biological events The beginning of the Neogene is when the first hominids (early humans) appeared. Modern humans appeared and developed civilization by the end of this period. Mammoths, sabre-toothed cats, and giant camels dominated until 10,000 years ago when many large mammals went extinct. Rise of the mammals and birds. Rodents, primates, pigs, cats, dogs, bears and whales appear. Flowering plants spread across the globe. Dinosaurs continue to dominate the land. Marsupials, modern sharks, bees and butterflies appear. Flowering plants appear. Period ends with the mass extinction of the dinosaurs and many plants. Dinosaurs dominate the land. Mammals are common but small. Feathered dinosaurs and birds appear. The most common land plants are ferns, palm-like trees called cycads, and grasses. The few survivors of the Permian extinction go on to populate the land and oceans. New species like mammals, dinosaurs and crocodiles appear. Amphibians dominate the land. Early cone-bearing plants like pine trees appear. Period ends with the largest mass extinction known with 95% of all marine species and 50% of all animals going extinct. Many swamps on land and sponge reefs in the oceans. Reptiles appear. Early winged insects and cockroaches appear. Fish spread across the oceans. Amphibians appear. The first trees and other plants spread across the land creating the first forests. Spiders, scorpions, insects, complex plants, and fish with bony jaws appear. Fish adapt to living in rivers and fresh water for the first time. First land plants appear. Primitive fungi and sea weed appears. The oceans are full of corals, mollusks, worms, primitive fish, and echinoderms like starfish. A large number of new animal species appear in a relatively short time. First fish appear. No known life on land yet. First multi-celled organisms like sponges appear. Earliest complex life forms are algae from 1.4 billion years ago. Oxygen begins to accumulate in the atmosphere. Earliest life on Earth are bacteria from 3.5 billion years ago. Earth is very different from today. The atmosphere is mostly methane and ammonia. The continents only just have begun to form. No known life. The Earth’s crust cools and solidifies. The moon forms. Assembled from the International Commission on Stratigraphy 2004 report A Geologic Time Scale and from information on the Univeristy of California Museum of Paleontology website (http://www.ucmp.org). This work is licensed under the Creative Commons AttributionNonCommercial License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/2.5/ or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA.