The fossil record is one piece of fossil evidence that supports the theory of continental drift. In rocks with a similar age, scientists have discovered fossils of related plant and animal species. The coastlines of many continents were home to these rocks.
Similar creature fossils discovered on wildly dissimilar continents supported the ground-breaking notion of continental drift. One of the earliest hypotheses put up by geologists for how continents might migrate through time is called continental drift. The preserved remnants of plants and animals that were submerged in sediments like sand and mud beneath ancient seas, lakes, and rivers are known as fossils. Any preserved sign of life that is typically older than 10,000 years is considered a fossil. Any surviving remains, impression, or evidence of a once-living thing from a previous geological epoch is referred to as a fossil. Examples include fossilized bones, shells, exoskeletons, animal or microbe imprints in stone, amber-preserved artifacts, hair, petrified wood, oil, coal, and DNA traces. The fossil record is the collection of all fossils. A geological timeline and the relative ages of various fossils were recognized in the 19th century as a result of the discovery that specific fossils were linked to specific rock strata. Scientists are now able to quantitatively determine the absolute ages of rocks and the fossils they contain thanks to the introduction of radiometric dating methods in the early 20th century. Permineralization, casts and molds, authigenic mineralization, replacement and recrystallization, adpression, carbonization, and bioimmuration are just a few of the numerous processes that result in fossilization.
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