Paleontologists can radioactively date a fossil by determining the amount of carbon-14 isotopes remaining in the specimen. Elements decay by half-lives, meaning that after one half-life, half of the sample's radioactive particles are gone.
The age of a plant or animal in a fossil is determined by radiocarbon dating. This means scientists measure the amount of a special type of carbon in the fossil, to determine the date.
By using radiometric or radiocarbon dating.
Radiocarbon dating is a technique that uses the decay of carbon-14.
Scientists can use carbon dating to determine the age of a fossil.
Carbon14 dating (isotopic dating)
Radiocarbon testing.
carbon dating
Radiocarbon dating is useful for determining the age of organic materials such as fossils because it measures the decay of carbon-14 isotopes. Carbon-14 has a half-life of about 5,730 years, making it suitable for dating organic remains up to around 50,000 years old. By comparing the ratio of carbon-14 to stable carbon isotopes in a sample, scientists can calculate its age.
Stratigraphy is the common method for dating fossils. The fossil will be younger than layers below it, and older than layers above it, provided the fossil beds have not been disturbed. Radioactive dating of fossils is more problematic, because of infiltration of fluids from elsewhere, and the carbonate circulation in the ocean is immeasurable long compared with its circulation rate in the atmosphere. So a shellfish could construct its shell from radiocarbon that was already centuries old, or from recycled old carbonate. In some circumstances it can be done however.
It allows scientists to organize the fossil record.
It tells us the absolute age of something, It is used when scientists want to see how old a fossil is.
It involves determining the age of an ancient fossil or specimen by measuring its carbon-14 content. Carbon-14, or radiocarbon, is a naturally occurring radioactive isotope that forms when cosmic rays in the upper atmosphere strike nitrogen molecules, which then oxidize to become carbon dioxide.