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The Geologic Time Scale A History of Earth and Life
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Geologic Time Scale Division of Earth’s history into blocks of time
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Ideas about time… Processes & Forces that are occurring now occurred in Earth’s past But how do we tell how old things are…
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1. Relative Dating Trying to determine which rock units formed first, second, third, & so on… Forming a sequence of time…no dates!
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Rules for Relative Dating 1. Rocks on the bottom are older than rocks on top Law of Superposition
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2. Principle of Original Horizontality Layers of rock are generally deposited in a horizontal positions
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3. Rock that cuts through is younger than the rock it cuts Principle of Cross-Cutting
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Matching Rock Layers Correlation To make a time scale we have to be able to find similar rock in different areas
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Fossils also help… What are fossils? Remains or traces of an organism that have been preserved
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Types of fossils 1. MOLD – created when an organism is buried in sediments & is dissolved by underground water
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Types of fossils 2. CAST – Created when the hollow spaces of a mold are filled with mineral matter
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Types of fossils 3. CARBONIZATION – occurs when an organism is buried under fine sediment. Pressure causes only a thin residue of carbon to be left. Best for preserving leaves & delicate animals
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Types of fossils 4. Impression – a replica of the surface that occurs when the carbon film is lost.
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5. Amber – Created when organisms are preserved in tree sap (resin) Types of fossils
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6. Petrified – Occurs when minerals from water replace the organism “turned to stone”
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2. Absolute Dating Radiometric Dating & Radiocarbon Dating Radioactive decay is used to date fossils. This gives us a specific time that the organism died.
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So lets look at what this showed us…
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Earth is about 4.6 billon years old
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Pre-Cambrian Era 4.6-540 mya 3.6 bya life appears - Single celled organisms First prokaryotes (bacteria)
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Paleozoic Era (Cambrian Period) 540 mya Explosion of multi-cellular life in oceans
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Paleozoic Era (Ordovician Period) 490 mya Many new invertebrates in seas; first land plants
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Paleozoic Era (Silurian Period) 443 mya Fish dominant; first insect fossils; land plants diversify
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Paleozoic Era (Devonian Period) 417 mya Fish dominate seas; First amphibians
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Paleozoic Era (Carboniferous Period) 354 mya Amphibians and insects dominate land; first reptiles
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Paleozoic Era (Permian Period) 290 mya Mammal -like reptiles
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Mass Extinction 248 mya 95% Marine species extinct; 70% land species extinct
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Mesozoic Era (Triassic Period) 248 mya Small reptiles and mammals; First dinosaurs
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Mesozoic Era (Jurassic Period) 206 mya Dinosaurs dominant; first birds appear
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Mesozoic Era (Cretaceous Period) 144 mya Dinosaurs dominate; first flowering plants
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Mass Extinction 65 mya 85% of all species extinct
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Cenozoic Era (Tertiary Period) 65 mya Mammals and birds dominate
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Cenozoic Era (Quaternary Period) 1.8 mya - today Mammals abundant; Humans appear == holla ==
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You know the history of life!
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