Ch 10 Geologic Time Scale

Ch 10 Notes
August 21, 2013
Ch 10 Geologic Time Scale
Sec 1­Life and Geologic Time
Geologic time­ earth's history is divided into time units that make up the GEOLOGIC TIME SCALE.
Time units on the scale are based on the appearance or disappearance of types of organisms such as trilobites, index fossils that lived during specific periods of time and over vast regions of the world..
Geologic Time is divided into 4 major subdivisions.
A. Eons­ longest subdivision of time
B. Eras­ marked by significant changes in types of fossils
C. Periods­ based on types of existing life
D. Epochs­ characterized by different regional life­forms
Organic Evolution­ Organisms have changed over time, most likely due to environmental changes.
Darwin's theory of Natural Selection
Species only reproduce with their own kind
Survival of the fittest
Artifical selection­ same as selective breeding where man chooses traits they want
New species evolve from natural selection
Trilobites­ have an exoskeleton with 3 lobes (this never changed); lived in oceans for more than 200 million years. Their eye position changed depending upon where they lived. Bodies and tails changed depending on environment. Changes in the trilobite exoskeleton can be attributed to changing environments and competition for survival.
Continental collisions formed giant landmass Pangaea near the end of the Paleozoic Era. This caused sea levels to drop causing the extinction of trilobites.
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Ch 10 Notes
August 21, 2013
Sec 2­ Early Earth History
Precambrain time­ from 4 billion to about 544 MYA (million years ago)
Very little fossils from this time, probably because of 1.the rocks being deeply buried, 2.lots of heat and pressure and 3.the organisms were soft­bodied so they didn't become fossils.
Cyanobacteria­ blue green algae. Earliest life form. Added oxygen to atmosphere by photosynthesis (contained chlorophyll).This made it possible the development of complex life forms because it help the atmosphere to have oxygen and an ozone layer.
Invertebrates and Edicaran animals appeared late in Precambrian time.
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Ch 10 Notes
August 21, 2013
Paleozoic Era­ Era of Ancient Life, 544 mya to 245 mya
Cambrian Period­ 544 mya
1st Trilobites
Ordovician Period­ 505 mya
1st Fish
Silurian Period­ 440 mya
1st land plants
Devonian Period­ 410 mya
1st Amphibians
Missippian Period­ 360 mya
1st Reptiles
Pennsylvannian Period­ 325 mya
Permian Period­ 286 mya
Many organisms with shells
Amphibians evolved to survive in water and on land. Might have evolved from fish. They used gills or lungs.
Reptiles evolved from amphibians to survive away from water.
Appalachian Mountains formed because of plate collisions.
Volcanoes very active
Some organisms of the Paleozoic era were fish, trilobites, and reptiles.
Most marine and land species became extinct at the end of the Paleozoic Era ( 245 mya). The change in environments that may have occurred at the end of the Paleozoic Era may have been caused by plate tectonics.
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Ch 10 Notes
August 21, 2013
Mesozoic Era­ Era of Middle Life, 245 mya to 65 mya
Triassic Period­ 245 mya
Pangaea breaks into 2 large pieces, climate became drier
1st dinosaurs
Reptiles most common animal
Mammals 1st appeared (but different than today) Small, mouse­like creatures
Jurassic Period­ 213 mya
1st Birds They evolved from small dinosaurs
Dinosaurs were dominant
Cretaceous Period­ 145 mya
Gymnosperms were dominant land plant (pine trees)
Angiosperms were flowering plants w/seeds that have hard outer shells (oak tree)
Some organisms during the Mesozoic Era were Angiosperms, reptiles, birds, and dinosaurs
Mesozoic Era ended 65 mya with a mass extinction.
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Ch 10 Notes
August 21, 2013
Cenozoic Era­ Era of Recent Life, 65 mya to today
Tertiary Period­ 65 mya
Paleocene Epoch­ 65mya
Eocene Epoch­ 55.5mya
Oligocene Epoch­ 33.7mya
Miocene Epoch­ 23.8mya
Pliocene Epoch­ 5.3mya
Only Era with Epochs that have been given specific names.
Quaternary Period­ 1.8 mya
Pleistocene Epoch­ 1.8mya
Holocene epoch­ 0.008mya
Mountain building period with cooler climates (1st Ice Age) Alps and Himalayas Mountains were formed
Mammals became dominant with many new life forms appearing after the dinosaur became extinct.
Mammals evolved and some species became isolated as the continents continued to separate.
Some organisms during the Cenozoic era were humans, reptiles, marine mammals, and birds.
Humans also appeared about 400,000 years ago.
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