Index fossil
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Index fossils (also known as guide fossils or zone fossils) are fossils used to define and identify geologic periods (or faunal stages). They work on the premise that, although different sediments may look different depending on the conditions under which they were laid down, they may include the remains of the same species of fossil. If the species concerned were short-lived (in geological terms, lasting a few hundred thousand years), then it is certain that the sediments in question were deposited within that narrow time period. The shorter the lifespan of a species, the more precisely different sediments can be correlated, and so rapidly evolving types of fossils are particularly valuable. The best index fossils are common, easy-to-identify at species level, and have a broad distribution—otherwise the likelihood of finding and recognizing one in the two sediments is low.
Ammonites fit these demands well, and are the best-known fossils that have been widely used for this. Other important groups that provide index fossils are the corals, graptolites, brachiopods, trilobites, and echinoids (sea urchins). Conodonts may be identified by experts using light microscopy such that they can be used to index a given sample with good resolution. Fossilized teeth of mammals, have also been used.
Geologists use both large fossils (called macrofossils) and microscopic fossils (called microfossils) for this process, known as biostratigraphy. Macrofossils have the advantage of being easy to see in the field, but they are rarer, and microfossils are very commonly used by oil prospectors and other industries interested in mineral resources when accurate knowledge of the age of the rocks being looked at is needed.
[edit] Common Index Fossils
Fossil | Scientific Name | Time Period | Million Years Ago |
---|---|---|---|
Calico Scallop |
Pecten gibbus Argopectin gibbus |
Quaternary Period | |
Neptunea tabulata | Quaternary Period | ||
Calyptatraphorus velatus | Tertiary Period | ||
Venericardia planicosta | Tertiary Period | ||
Scaphites |
Scaphites hippocrepis | Cretaceous Period | |
Inoceramus | Inoceramus labiatus | Cretaceous Period | |
Perisphinctes | Perisphinctes tiziani | Jurassic Period | |
Nerinea trinodosa | Jurassic Period | ||
Trophites subbullatus | Triassic Period | ||
Monotis subcircularis | Triassic Period | ||
Leptodus americanus | Permian Period | ||
Parafusulina | Parafusulina bosei | Permian Period | |
Dictyocostus americanus | Pennsylvanian Period | ||
Lophophyllidium proliferum | Pennsylvanian Period | ||
Cactocrinus multibrachiatus | Mississippian Period | ||
Prolecanites gurleyi | Mississippian Period | ||
Mucrospirifer |
Mucrospirifer mucronatus | Devonian Period | |
Palmatolepus unicornis | Devonian Period | ||
Ammonite |
Ammonite jeletzkytes | Late Silurian to Early Devonian | |
Cystiphyllum niagarense | Silurian Period | ||
Hexamoceras hertzeri | Silurian Period | ||
Trilobite | Bathyurus extans | Ordovician Period | |
Tetragraptus fructicosus | Ordovician Period | ||
Paradoxides pinus | Cambrian period | ||
Trilobite |
See list of trilobites | Cambrian Period | |
Billingselia corrugata | Cambrian Period |
[edit] In Popular Culture
Musical Group Bad Religion have a song titled "Part IV (The Index Fossil)" on their 1988 album Suffer. The song suggests that one day humanity will be "an index fossil buried in [its] own debris".
[edit] References and Links
- ^ Index Fossils, from the US Geological Survey. Updated July 28, 1997.