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As organisms exist at the same time period throughout the world, their presence or sometimes absence may be used to provide a relative age of the formations in which they are found. If sufficient sedimentary material is available, it will be deposited up to the limits of the sedimentary basin. For example, in sedimentary rocks, it is common for gravel from an older formation to be ripped up and included in a newer layer. The principle becomes quite complex, however, given the uncertainties of fossilization, the localization of fossil types due to lateral changes in habitat facies change in sedimentary strataand that not all fossils may be found globally at the same time.
Finding the key bed in these situations may help determine off the fault is a normal fault or a thrust fault. In geology, when an igneous intrusion cuts across a formation of sedimentary rockit can be determined that the igneous intrusion is younger than the sedimentary rock. Many of the same principles are applied.