Technique that compares age of one fossil or rock with another to determine which is older
Absolute Dating
Process of determining how old rock is by looking at radioactive material in the rocks and how it has decayed
Law of Fossil Succession
Sedimentary rock is formed by accumulation of sedimentary layers on top of each other, so fossils closer to surface must be younger than those found below them
Fossils are same age as rocks in which they are found
Sometimes the Law of Fossil Succession is not true because layers of rock have been turned upside down by movement of Earth's crust
Strata (Stratum for single layer)
Layers in which sedimentary rock form
Index Fossils
Most species only existed on Earth for a relatively short time
Each fossil species is only found in narrow band of rock strata in any location
All rocks containing a particular species of fossil should be same age as each other even if places long way apart
Index Fossils
Fossils of a known age which are used to easily determine age of unknown fossils by comparing ages of strata in different locations
Index Fossils
Have been fairly widespread
Have lived in a fairly narrow period of time
Have been abundant
Be easy to identify
Index Fossils
Ammonites (extinct group of molluscs)
Trilobites (extinct group of arthropods with external skeleton and jointed limbs, same phylum as current day insects, crabs and spiders)
Known ages of different types of Trilobites that existed in narrow periods of time, so they can be used as Index fossils
Stratigraphy
Relative dating technique of comparing strata in different locations to determine their relative ages
Fossil is labelled by the locality letter and stratum number that it is found in (e.g. A1, C1)
Strata with same types of fossils are same age
Stratigraphy: Try it yourself
1. Compare different types of fossils found in different localities to determine oldest and youngest strata overall
2. Oldest stratum will be at the bottom, youngest will be at the top