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Unit 6 Geologic Time. Chapter 21 Fossils and the Rock Record. 21.1 The Rock Record. The geologic time scale - the Earth is 4.6 billion years old. - in order to break up this vast amount of time, scientists divide it into Eons. Eons.
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Unit 6 Geologic Time Chapter 21 Fossils and the Rock Record
21.1 The Rock Record The geologic time scale - the Earth is 4.6 billion years old. - in order to break up this vast amount of time, scientists divide it into Eons
Eons The three earliest eons are grouped into the “Precambrian” Hadean – The formation of the earth 542 Hadean
Eons Archaen – Continental plates begin to form and earliest fossils 542 Hadean
Eons Proterozoic – multicellular life cyanobacteria increases oxygen levels 542 Hadean
Eons Phanerozoic– “visible life” Most of the fossils with hard parts 542 Hadean
Eons are divided into Eras • Phanerozoic is divided into three Eras • Paleozoic – ancient life • Mesozoic – middle life • Cenozoic – recent life 542 Hadean
Eras are divided into Periods • Mesozoic is divided into three Periods • Triassic • Jurassic • Cretaceous 542 Hadean
Periods are divided into Epochs Eons Eras Periods Epochs
You were born 15 seconds ago
If 1 Second was 1 year The Revolutionary War was 4 minutes ago
The First Christmas was 33 minutes ago
The pyramids were built 1.5 hours ago
The Last Ice Age Was 2 hours and 12 minutes ago
Dinosaurs were wiped out 2 years ago
Pangaea broke apart • 6 years and 4 months ago
Dinosaurs showed up (Triassic) • 8 years ago
Cambrian began 17 years ago
Earth formed • 145 years ago
21.2 Relative-Age Dating • What happened first? • Oldest and newest?
James Hutton • Geologist and Physician • Proposed that the earth was millions of years old based on geologic evidence
Sir Charles Lyell • Geologist • Proposed that geologic changes occur slowly over long periods of time.
Uniformitarianism • The idea that the same processes occurring today have been the same throughout time • This idea replaced the idea of catastophism which suggested major changes by sudden catastrophic events
Principles for Determining Relative Age • Original horizontality – sedimentary rocks are deposited in horizontal layers
Superposition The deeper strata (layers) were deposited first. Fossils found in lower layers are older than in higher layers.
Cross cutting relationships Plutons are younger than the rocks they are found in
Principle of Inclusions Fragments of a rock included in a rock layer are older than the rock layer
Unconformities • Signs of surface erosion that are buried show a gap in the rock record
Disconformities • Signs of surface erosion that are buried between sedimentary layers
Nonconformities • Signs of erosion that are found between a sedimentary layer and metamorphic or igneous layers
Angular Unconformity Nonhorizontal rock layers indicate uplifting
Correlation • Matching of a unique rock layer or fossil in one area to similar layers in another area.
Key Bed A rock layer used as a marker
Fossil Correlation Using index fossils to compare ages of rock layers
21.3 Absolute-Age Dating So how old is it? Absolute-age dating gives the numerical age of rocks.
Radioactive Isostopes Isotopes are atoms of an element with more or less neutrons Carbon – has 6 protons Carbon-12 has 6 protons and 6 neutrons
Nucleus C-12
Radioactive Isostopes Isotopes are atoms of an element with more or less neutrons Carbon – has 6 protons Carbon-12 has 6 protons and 6 neutrons Carbon-14 has 6 protons and 8 neutrons
Nucleus C-14
Radioactive Isostopes Isotopes are atoms of an element with more or less neutrons Carbon – has 6 protons Carbon-12 has 6 protons and 6 neutrons Carbon-14 has 6 protons and 8 neutrons Carbon-14 decays into Nitrogen-14
Nucleus N-14
Radioactive Decay The decay of radioactive isotopes into the daughter product
Half life The time required for ½ of the isotopes to decay