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Today's knowledge of fossil ages comes primarily from radiometric dating, also known as radioactive dating. Radiometric dating relies on the properties of isotopes. These are chemical elements, like carbon or uranium, that are identical except for one key feature -- the number of neutrons in their nucleus.
Scientists combine several well-tested techniques to find out the ages of fossils. The most important are Relative Dating, in which fossils and layers of rock are placed in order from older to younger, and Radiometric Dating, which allows the actual ages of certain types of rock to be calculated.
To discover how organisms lived in the past, paleontologists look for clues preserved in ancient rocks the fossilized bones, teeth, eggs, footprints, teeth marks, leaves, and even dung of ancient organisms. Fossilized jaws, teeth, and dung provide important clues about what non-avian dinosaurs ate.
The field in which people study things like dinosaur guts and feces is known by some as “paleontology”. It's a discipline which essentially asks how ancient plants and animals actually lived and functioned millions of years ago. For decades there was little evidence we could use to understand dinosaur paleontology.
Early estimates of 300-year lifespans for the largest sauropods were based on comparisons with crocodiles and turtles, which have much slower metabolisms. The consensus is now that Apatosaurus and Diplodocus dinosaurs probably only lived for 70 or 80 years, which is about the same as an elephant today.
Radiometric dating is a method used to date rocks and other objects based on the known decay rate of radioactive isotopes. Radiocarbon dating is a method used to determine the age of organic material by measuring the radioactivity of its carbon content.
The best estimate for Earth's age is based on radiometric dating of fragments from the Canyon Diablo iron meteorite. From the fragments, scientists calculated the relative abundances of elements that formed as radioactive uranium decayed over billions of years.
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