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Fossil
preserved remains, impressions or traces of any once-living organism from a past geological age
Consitions that increase change of fossilisation
Remains are rapidly buried in sediments, continued sediment deposits bury it deeper and compress original sediment layer into rock
Faunal succession
the principle that fossilised fauna and flora in sedimentary rock strata are arranged in a specific order
Index fossils
fossils of geologically short-lived species that are widely distributed but are found in a restricted depth of rock strata, identifies rocks as having the same age
Transitional fossils
fossilised remains of a life form that exhibits traits common to both an ancestal group and its descendant group, act as links
Relative dating
provides a comparative age, identified as older or younger than another known object, includes stratigraphic method of using faunal succession
Absolute dating
provides a more precise numerical age
Radiometric dating technique
depends on the known rate of decay of a radioactive parent isotope to a stable daughter product