Carbon dating in biology

What Is Carbon Dating?

Carbon dating is a technique used to determine the approximate age of once-living materials. It is based on the decay rate of the radioactive carbon isotope 14 C, a form of carbon taken in by all living organisms while they are alive. Before the twentieth century, determining the age of ancient fossils or artifacts was considered the job of paleontologists or paleontologists, not nuclear physicists. By comparing the placement of objects with the age of the rock and silt layers in which they were found, scientists could usually make a general estimate of their age. However, many objects were found in caves, frozen in ice , or in other areas whose ages were not known; in these cases, it was clear that a method for dating the actual object was necessary.

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You probably have seen or read news stories about fascinating ancient artifacts. An archaeologist finds a child mummy high in the Andes and says the child lived more than 2, years ago. How do scientists know how old an object or human remains are? What methods do they use and how do these methods work? Radiocarbon dating, or carbon dating for short, is a way of determining the age of certain archeological artifacts of a biological origin up to about 50, years old.

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So how do you check to see its true age? Well, one method is called Carbon dating , which is used to date organic samples. This method can be used to date artifacts like our theoretical archeologist found, but it can also date plants and animals as well. In this article, we will be learning about Carbon dating and see how this process is used to date deceased organic materials and life forms.

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Carbon Dating

Carbon , C , 14 C or radiocarbon , is a radioactive isotope of carbon with an atomic nucleus containing 6 protons and 8 neutrons. Its presence in organic materials is the basis of the radiocarbon dating method pioneered by Willard Libby and colleagues to date archaeological, geological and hydrogeological samples. Its existence had been suggested by Franz Kurie in The primary natural source of carbon on Earth is cosmic ray action on nitrogen in the atmosphere, and it is therefore a cosmogenic nuclide.

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