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Fossils
preserved remains and traces of organisms
Mould Fossil
Impression of an organism has been left on the rock, creating a cavity where the organism decayed
Cast fossil
minerals can be fit into the cavity where an impression of an organism was left
petrified fossil
When organic material has been replaced with minerals and rock, most bone fossils are petrified
Trace fossils
Evidence of an organisms activity, more frequent than petrified fossils
Transitional fossils
Rare fossils depicting the intermedeol phase of evolution between an organisms ancestral form and its descendants.
gradualism
The theory that evolution is a steady, gradual divergence of lineages
Punctuated equilibrium
The theory that evolution can be both stable, and rapid if there is a sudden change in environment
fossil dating methods
Absolute dating, Comparative dating methods, stratigraphic correlation, index fossils
Absolute Dating
Assigning a numerical age to the fossil via the physical and chemical properties of the rock
Radiometric Dating
Determines the predictable rate of decay of naturally occurring radioactive isotopes for Absolute dating.
half life
measures time taken for half of the radioactive isotope to decay
Carbon Dating
type of Radioactive dating that measures the decay of carbon-14 into nirtogen-14, accurate for samples up to about 50 000 years old
Comparative Dating Techniques
Determining the age of a rock relative to other similar rocks nearby based mostly on their stratum.
Stratigraphic Correlation
Comparative dating technique that estimates the relative age of a fossil using similar igneous rock
igneous rock
Rock that can be dated with uranium or potassium
index fossils
fossil found used in stratigraphic dating that can be date due to being found in igneous rock. it is easily identifiable and abundant.