In This Article Fossils

  • Introduction
  • General Overviews
  • Texts Organized around Specific Lineages or Fossil Types
  • Texts Organized around Earth History

Evolutionary Biology Fossils
by
Kevin Boyce
  • LAST MODIFIED: 21 January 2016
  • DOI: 10.1093/obo/9780199941728-0070

Introduction

Fossils represent the remnants of biological activity preserved over thousands, millions, or billions of years. Those remnants range from direct preservation of organic matter and original biominerals, to replacement with sediment or secondarily precipitated minerals, to various forms of more or less indirect preservation of organism behavior. Long before Darwin described the mechanism of natural selection, fossils were central to the recognition of the biological reality of evolution and the immensity of geologic time. Fossils remain central to the investigation of evolutionary processes over temporal scales too large for direct observation, under environmental circumstances that no longer exist, such as anoxic atmospheres or aggregated continents, and across singular historical events, such as mass extinctions. Mammoths and tyrannosaurs may be the most common ambassadors providing entry into awareness of fossils, but at least twenty other animal phyla have contributed to the fossil record in addition to those vertebrates. The paleontological history of life spans both prokaryote and eukaryote—the latter including plants and animals, but also fungi and forams, algae and amoebae. The fossil record preserves the separate evolution of complex multicellularity in at least six different lineages and of robust skeletal elements in dozens.

General Overviews

Fossils played a foundational role in the recognition of biotic evolution and of geological time (Lyell 1830–1833, Darwin 1845, Darwin 1859), as recently reviewed by Rudwick 2014. Beginning with the utility of fossil succession for telling time via biostratigraphy (Berry 1968), paleontology has gone on to play a central role in understanding macroevolutionary patterns and processes (Gould 2002, Foote and Miller 2007), and it has diversified into considerations of form and function, radiation and extinction, development and physiology, and ecosystem and environment (Briggs and Crowther 2001).

  • Berry, William B. N. 1968. Growth of a prehistoric time scale, based on organic evolution. San Francisco: W. H. Freeman.

    E-mail Citation »

    Fascinating account of the rapid establishment of biostratigraphy and the geologic timescale in the years immediately after William Smith’s recognition that evolutionary turnover in the fossil record can be used to tell time in rocks.

  • Briggs, Derek E. G., and Peter R. Crowther, eds. 2001. Palaeobiology II. London: Blackwell Science.

    DOI: 10.1002/9780470999295E-mail Citation »

    Short essays from leading experts covering the broad diversity of paleontological research. This is a second volume, rather than a second edition, to Palaeobiology, published eleven years earlier. Where there is overlap in content, comparison demonstrates the impact of the intervening years of research.

  • Darwin, Charles R. 1845. Journal of researches into the natural history and geology of the countries visited during the voyage of H.M.S. Beagle round the world, under the command of Capt. Fitz Roy, R.N. 2d ed. London: John Murray.

    E-mail Citation »

    Commonly shortened to Voyage of the Beagle. The second edition represents an extraction of the popular Darwin volume from a multivolume set covering the voyages. The best immersion into the new intellectual possibilities opened up in natural history when the advances of Smith, Hutton, and Lyell are applied to the world by a curious and observant mind.

  • Darwin, Charles R. 1859. On the origin of species by means of natural selection. London: Murray.

    E-mail Citation »

    Nothing in biology makes sense except in the light of evolution (a truth first so phrased by Theodosius Dobzhansky).

  • Foote, Michael, and Arnold I. Miller. 2007. Principles of paleontology. 3d ed. New York: W. H. Freeman.

    E-mail Citation »

    A renewal of the classic text by David M. Raup and Steven M. Stanley. The best student text covering analytical paleobiology.

  • Gould, Stephen Jay. 2002. The structure of evolutionary theory. Cambridge, MA: Belknap Press of Harvard Univ. Press.

    E-mail Citation »

    The summary statement from one of the great thinkers of paleontology and evolution.

  • Lyell, Charles. 1830–1833. Principles of geology: Being an attempt to explain the former changes of the Earth’s surface, by reference to causes now in operation. London: John Murray.

    DOI: 10.5962/bhl.title.50860E-mail Citation »

    The first great modern synthesis of geology, based on John Hutton’s principle of uniformitarianism—the concept that the geologic record of the distant past must have been formed via the same natural processes seen in the modern world. Extremely influential; Darwin read it on the Beagle.

  • Rudwick, Martin J. S. 2014. Earth’s deep history. Chicago: Univ. of Chicago Press.

    DOI: 10.7208/chicago/9780226204093.001.0001E-mail Citation »

    Insight from decades of work from a leading historian of the scientific discipline of paleontology.

back to top

Users without a subscription are not able to see the full content on this page. Please subscribe or login.

How to Subscribe

Oxford Bibliographies Online is available by subscription and perpetual access to institutions. For more information or to contact an Oxford Sales Representative click here.

Purchase an Ebook Version of This Article

Ebooks of the Oxford Bibliographies Online subject articles are available in North America via a number of retailers including Amazon, vitalsource, and more. Simply search on their sites for Oxford Bibliographies Online Research Guides and your desired subject article.

If you would like to purchase an eBook article and live outside North America please email onlinemarketing@oup.com to express your interest.

Article

Up

Down