Absolute dating is used when the sediments or fossil can be directly dated. There are numerous dating methods available, using a range of elements and isotopes, and more methods are always being developed. Here are some of the most commonly used dating methods in archaeology and palaeontology.
This manner of dating relies on the constant rate of decay of certain radioactive isotopes (Isotopes are one or more forms of an element differing from each other in atomic weight and in nucleas, but not in chemical properties) within a bone, tooth or sediment.
Radio carbon dating can only date organic material which is younger than 40 000 years, AMS (Accelerator Mass Spectrometry) dating can extend this back to 75 000 years ago.
Potassium is a very abundant element in the Earth’s crust and about 0.01% of all potassium is the radio-active isotope 40K. 40K decays into 40Ar at a known rate, and the ratio between the two isotopes can be used as an indication as to how old a rock or sediment, such as a tuff or layer of volcanic ash is. Volcanic rocks and tuffs are common in east Africa and have allowed for the accurate dating of early hominid skulls, and in the case of the Laeotoli footprints, evidence for the early bipedality of hominids.
Optically Stimulated Luminescence Dating (OSL) and other such similar dating methods work by counting electrons trapped by flaws in the microscopic structure of crystals. The electrons are freed as light and the amount of escaping light can be carefully measured to estimate the time elapsed since a grain of sand was last exposed to the sun before burial. This method has become so refined that single grains of sand can be dated (TT-OSL). This method can be used to date sediments to provide relative dates for the archaeology or fossils found within them, as it dates the time they became covered by sand, and directly dates the time the sediments were last exposed to light.