With a few important exceptions, living organisms keep all their amino acids in the "L" configuration.When an organism dies, control over the configuration of the amino acids ceases, and the ratio of D to L moves from a value near 0 towards an equilibrium value near 1, a process called racemization.This then can be used to deduce the sequence of events and processes that took place or the history of that brief period of time as recorded in the .For example, the presence of recycled bricks at an archaeological site indicates the sequence in which the structures were built.This knowledge helps to answer questions such as when did a volcano last erupt, what is the rate of crustal uplift in a specific area, are rocks at one gold prospect the same age as those at another or does the age of a dune fields align with the known climate record.Australia is an old continent and the age of much of its geology predates fossil evidence and must be dated by radiometric geochronology methods which provide absolute ages of Earth materials using radioactive decay.There is a wide variety of materials which can be analysed and Australian researchers continue to be at the forefront of developing instruments and methods for geochronology.The basis of radiometric geochronology is that a radioactive parent element, such as uranium, is incorporated as trace amounts into a mineral when it forms in the Earth’s crust.
The rate at which racemization proceeds depends on the type of amino acid and on the average temperature, humidity, acidity (p H), and other characteristics of the enclosing matrix.
However, both disciplines work together hand in hand, to the point that they share the same system of naming rock layers and the time spans utilized to classify layers within a strata.
(The terminology is given in the table on the right.) For instance, with reference to the geologic time scale, the Upper Permian (Lopingian) lasted from 270.6 /- 0.7 Ma (Ma = millions of years ago) until somewhere between 250.1 /- 0.4 Ma (oldest known Triassic) and 260.4 /- 0.7 Ma (youngest known Lopingian)—a gap in known, dated fossil assemblages of nearly 10 Ma.
Often, the most basic knowledge required for resource exploration is the age of rocks in a given area, regardless of whether the resource is mineral, petroleum or geothermal.
The rock ages provide information about how the rocks are related and what geological events of which they may have been part.