Final answer:
To date fossils, scientists utilize relative dating to sequence events and absolute dating, like carbon-14 dating, to establish approximate ages in years. Carbon-14 is effective for dating remains up to 50,000 years old, while other isotopes are used for older fossils.
Step-by-step explanation:
To determine the age of fossils, scientists use two main methods: relative dating and absolute dating. Relative dating involves sequencing fossils and rock layers to create a chronological order without determining the specific age in years. Absolute dating, on the other hand, provides an approximate age in years for the fossil. This is frequently accomplished using radiometric techniques such as carbon-14 dating.
Carbon-14 (C-14) dating is the most well-known method for determining the absolute age of once-living materials. The premise is simple: living organisms absorb Carbon-14 from the environment, and this isotope decays at a known rate, with a half-life of 5,730 years. By measuring the amount of C-14 that remains in a fossil, scientists can estimate how long ago the organism died, up to approximately 50,000 years ago. For older fossils, other isotopes with longer half-lives, such as potassium-40, may be utilized instead.