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Fossils and Geologic Time Vocabulary

AB
fossilpreserved remains or evidence of organsims
trace fossilevidence of an organism's activities
petrifactionprocess in which minerals replace an organsim's tissues
permineralizatioonprocess in which the pores in an organism's hard tissue is filled with minerals
replacementprocess in which minerals take the place of all of an organism's tissue
amberhardened tree sap
asphaltthick, oily, petroleum substance
burrowunderground shelters
coprolitepetrified feces
trailimprint left by animals such as slugs, snail
moldcavity made in a sediment surface after an organism decays
castsolid outer replica of an organsim formed when sediments or minerrals fill in a cavity
index fossilsfossils that are widely distributed geographically and lived during a brief period
ammonitesindex fossil similar to a modern squid that lived between 230 and 208 million years ago
trilobiteindex fossil that lived about 400 million years ago
geologic time scalestandard division of Earth's history based on geologic events and life forms
eonlargest division of geologic time
erasecond-largest division of geologic time; includes two or more periods
periodthird-largest division of geologic time
epochsmallest division of geologic time; subdivision of a period
Cenozoic Erameans recent life
Paleozoic Erameans ancient life
Mesozoic Erameans middle life
Cenozoic EraAge of Mammals
Mesozoic EraAge of Reptiles
Paleozoic EraAge of Amphibians
Paleozoic EraAge of Invertebrates
Paleozoic EraAge of Fishes
extinctiondeath of every member of a species
ice coretubular or cylinder-shaped sample of ice
Phanerozoicmost recent eon
Phanerozoicmeans visible light
Holocenethe current epoch
Quaternarythe current period
principle of superpositionwhen rock layers are undisturbed, the oldest are on the bottom
principle of cross cutting relationsfeatures such as intrusions, folding, faulting are always younger than the rocks through which they cut
principle of horizontalityrock layers are deposited parallel to Earth's surface
intrusionigneous rock that cuts through rock layers beneath Earth's surface
half-lifethe amount of time required for half of a radioactive isotope to decay to daughter isotope
radiometric decaythe process by which unstable isotopes (parent) break down into stable isotopes (daughter)
radioactive datingfinding ages of rocks and fossils based on the ratio of parent to daughter isotopes in rock or fossils
absolute datingfinding the age in years
relative datingcomparison of an object or event to another object or event to determine age from oldest to youngest


High School Science
Sequatchie County High School
TN

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