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evidence that can be obtained from fossils
changes that have occurred in the types of organisms living on this planet
supports the theory of evolution
ways the fossil record can be interpreted
time scale represents millions of years
species that are further down on the record are older
faunal succession
the principle that fossilised flora and fauna in sedimentary rock strata are arranged vertically in a specific order
index fossils
fossils with known ages that can be used to relatively date other fossils by comparison
must be distinctive, abundant, distributed worldwide and have existed for only a short period of time
transitional fossils
shows traits of both its ancestral group and its descendants, acting as evidence of an intermediate form
two main ways of dating fossils
absolute age: a precise, numerical age of a fossil
relative age: a comparative age of a fossil in relation to other fossils
process of relative dating
stratigraphic method
determining relative age by its position within rock strata
use of index fossils
process of absolute dating
radiometric dating that depends on the known rate of decay of a radioactive parent isotope to a stable daughter product, measured in half-lives (eg. carbon dating)
carbon dating
carbon 14 (parent isotope)
nitrogen 14 (daughter product)
5730 years half life
dating organic remains
only used for ages up to 50,000-60,000 years