is the process ofdetermining an ageon a specifiedchronologyinarchaeologyandgeology. Some scientists prefer the terms, as use of the word absolute implies an unwarranted certainty of accuracy.Absolute dating provides a numerical age or range in contrast withrelative datingwhich places events in order without any measure of the age between events.

In archaeology, absolute dating is usually based on the physical, chemical, and life properties of the materials of artifacts, buildings, or other items that have been modified by humans and by historical associations with materials with known dates (coins andwritten history). Techniques includetree ringsin timbers,radiocarbon datingof wood or bones, andtrapped-charge datingmethods such asthermoluminescence datingof glazed ceramics.3Coins found in excavations may have their production date written on them, or there may be written records describing the coin and when it was used, allowing the site to be associated with a particular calendar year.

Inhistorical geology, the primary methods of absolute dating involve using theradioactive decayof elements trapped in rocks or minerals, including isotope systems from very young (radiocarbon dating with14

C) to systems such asuraniumlead datingthat allow acquisition of absolute ages for some of the oldest rocks on Earth.

Radiometric dating is based on the known and constant rate of decay ofradioactive isotopesinto theirradiogenic daughter isotopes. Particular isotopes are suitable for different applications due to the types of atoms present in the mineral or other material and its approximate age. For example, techniques based on isotopes with half lives in the thousands of years, such as carbon-14, cannot be used to date materials that have ages on the order of billions of years, as the detectable amounts of the radioactive atoms and their decayed daughter isotopes will be too small to measure within the uncertainty of the instruments.

One of the most widely used and well-known absolute dating techniques is carbon-14 (orradiocarbon) dating, which is used to date organic remains. This is a radiometric technique since it is based on radioactive decay. Cosmic radiation entering the earths atmosphere produces carbon-14, and plants take in carbon-14 as they fix carbon dioxide. Carbon-14 moves up the food chain as animals eat plants and as predators eat other animals. With death, the uptake of carbon-14 stops.

It takes 5,730 years for half the carbon-14 to change to nitrogen; this is the half-life of carbon-14. After another 5,730 years only one-quarter of the original carbon-14 will remain. After yet another 5,730 years only one-eighth will be left.

By measuring the carbon-14 inorganic material, scientists can determine the date of death of the organic matter in an artifact orecofact.

The relatively short half-life of carbon-14, 5,730 years, makes dating reliable only up to about 50,000 years. The technique often cannot pinpoint the date of an archeological site better than historic records, but is highly effective for precise dates when calibrated with other dating techniques such astree-ring dating.

An additional problem with carbon-14 dates from archeological sites is known as the old wood problem. It is possible, particularly in dry, desert climates, for organic materials such as from dead trees to remain in their natural state for hundreds of years before people use them as firewood or building materials, after which they become part of the archaeological record. Thus dating that particular tree does not necessarily indicate when the fire burned or the structure was built.

For this reason, many archaeologists prefer to use samples from short-lived plants for radiocarbon dating. The development ofaccelerator mass spectrometry(AMS) dating, which allows a date to be obtained from a very small sample, has been very useful in this regard.

Other radiometric dating techniques are available for earlier periods. One of the most widely used ispotassiumargon dating(KAr dating).Potassium-40is a radioactive isotope of potassium that decays into argon-40. The half-life of potassium-40 is 1.3 billion years, far longer than that of carbon-14, allowing much older samples to be dated. Potassium is common in rocks and minerals, allowing many samples ofgeochronologicalorarcheologicalinterest to be dated.

Argon, a noble gas, is not commonly incorporated into such samples except when producedin situthrough radioactive decay. The date measured reveals the last time that the object was heated past theclosure temperatureat which the trapped argon can escape the lattice. KAr dating was used to calibrate thegeomagnetic polarity time scale.

Thermoluminescence testing also dates items to the last time they were heated. This technique is based on the principle that all objects absorb radiation from the environment. This process frees electrons within minerals that remain caught within the item.

Heating an item to 500 degrees Celsius or higher releases the trappedelectrons, producing light. This light can be measured to determine the last time the item was heated.

Radiation levels do not remain constant over time. Fluctuating levels can skew results for example, if an item went through several high radiation eras, thermoluminescence will return an older date for the item. Many factors can spoil the sample before testing as well, exposing the sample to heat or direct light may cause some of the electrons to dissipate, causing the item to date younger.

Because of these and other factors, Thermoluminescence is at the most about 15% accurate. It cannot be used to accurately date a site on its own. However, it can be used to confirm the antiquity of an item.

Optically stimulated luminescence (OSL) dating constrains the time at which sediment was last exposed to light. During sediment transport, exposure to sunlight zeros the luminescence signal. Upon burial, the sediment accumulates a luminescence signal as natural ambient radiation gradually ionises the mineral grains.

Careful sampling under dark conditions allows the sediment to be exposed to artificial light in the laboratory which releases the OSL signal. The amount of luminescence released is used to calculate the equivalent dose (De) that the sediment has acquired since deposition, which can be used in combination with the dose rate (Dr) to calculate the age.

Dendrochronologyortree-ring datingis the scientific method of dating based on the analysis of patterns oftree rings, also known asgrowth rings. Dendrochronology can date the time at which tree rings were formed, in many types of wood, to the exact calendar year.

Dendrochronology has three main areas of application:paleoecology, where it is used to determine certain aspects of pastecologies(most prominently climate);archaeology, where it is used to date old buildings, etc.; andradiocarbon dating, where it is used to calibrate radiocarbon ages (see below).

In some areas of the world, it is possible to date wood back a few thousand years, or even many thousands. Currently, the maximum for fully anchored chronologies is a little over 11,000 years from present.4

Amino acid datingis adating technique56789used to estimate the age of a specimen inpaleobiologyarchaeologyforensic sciencetaphonomysedimentary geologyand other fields. This technique relates changes inamino acidmolecules to the time elapsed since they were formed. All biological tissues containamino acids. All amino acids exceptglycine(the simplest one) areoptically active, having an asymmetriccarbonatom. This means that the amino acid can have two different configurations, D or L which are mirror images of each other.

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 calledracemization. Thus, measuring the ratio of D to L in a sample enables one to estimate how long ago the specimen died.10

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Articles needing additional references from July 2013

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