World Library  
Flag as Inappropriate
Email this Article

Index fossil


Index fossil

Examples of index fossils

Index fossils (also known as guide fossils, indicator 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 minor.[1]

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.

The series of deposits that spans the occurrence of a particular index fossil, is often referred to as that fossil's zone, enabling to relate different faunas through time. An example would be to say that Mesolenellus hyperborea occurs in the late Nevadella-zone.

How index fossils are used

"Imagine an E.L. Doctorow novel in which Alfred Tennyson, William Tweed, Abner Doubleday, Jim Bridger, and Martha Jane Canary sit down to a dinner prepared by Rutherford B. Hayes. ... a geologist could quickly decide -- as could anyone else -- that the dinner must have occurred in the middle 1870s, because Canary was 18 when the decade began, Tweed becam extinct in 1878, and the biographies of the others do not argue with these limits." -- John McPhee, Basin and Range (1981). [2]

List of common index fossils [3]

Fossil Scientific Name Time Period Million Years Ago

Calico Scallop
Pecten gibbus
Argopecten gibbus
Quaternary Period
Neptunea tabulata Quaternary Period
Viviparus glacialis Tiglian (Early Pleistocene)
Calyptraphorus velatus Tertiary Period
Venericardia planicosta Eocene

Scaphites hippocrepis Cretaceous Period

Inoceramus labiatus Cretaceous Period
Perisphinctes Perisphinctes tiziani Jurassic Period
Nerinea trinodosa Jurassic Period
Tropites subbullatus Triassic Period
Monotis subcircularis Triassic Period

Leptodus americanus Permian Period
Parafusulina Parafusulina bosei Permian Period
Dictyoclostus americanus Pennsylvanian Period
Lophophyllidium proliferum Pennsylvanian Period
Cactocrinus multibrachiatus Mississippian Period
Prolecanites gurleyi Mississippian Period

Mucrospirifer mucronatus Devonian Period
Palmatolepis unicornis Devonian Period
Silurian Period
Tetragraptus fructicosus Ordovician Period
Paradoxides Cambrian Period
Billingselia corrugata Cambrian Period
Archeocyathids Lower Cambrian


  1. ^ Ghosh, v D. (2006). "Index fossils - Evidences from plant sources". Resonance: 69–77. Retrieved 7 November 2013. 
  2. ^ John McPhee, Basin and Range. 1981, Farrar, Straus & Giroux. ISBN 0-374-10914-1 . Reprinted in the omnibus Annals of the Former World, ISBN 0-374-10520-0
  3. ^ Index Fossils, from the US Geological Survey. Updated July 31, 1997.
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.