From Simple English Wikipedia, the free encyclopedia
Jump to navigation Jump to search

Palaeontology or Paleontology is the study of fossils of living things, and their phylogeny (evolutionary relationships).[1] It depends on basic sciences such as zoology, botany and historical geology. The term palaeobiology implies that the study will investigate the palaeoecology of the groups in question.

In palaeozoology, the evolution of those phyla with fossil records are studied: see List of animal phyla. In palaeobotany, fossil plants are studied. In historical geology the formation, sequence and dating of rock strata give information about past environments.

A fossil is any kind of life that is more than ten thousand years old and preserved in any form that we can study today.[2] The fossil record is always incomplete, and later discoveries may extend the known survival of a group. See Lazarus taxon.

Some palaeontologists study fossils of microorganisms, living things that are too small to see without a microscope, while other palaeontologists study fossils of giant dinosaurs.

  • Vertebrate palaeontology: the palaeontology of vertebrate animals
  • Invertebrate palaeontology: the palaeontology of invertebrate animals

Related pages[change | change source]

References[change | change source]

  1. Prothero, Donald R. 2007. Evolution: what the fossils say and why it matters. Columbia University Press, New York. ISBN 978-0-231-13962-5
  2. Levin, Harold L. 2005. The Earth through time. 8th ed, Wiley, N.Y. Chapter 4: The fossil record.