Overview

The Phanerozoic eon is the most recent interval of geological time, beginning roughly 541 million years ago and continuing to the present. It is defined by a rich fossil record that documents the appearance, diversification and extinction of complex multicellular animals and plants. For a general reference see Phanerozoic. The first interval of the eon is the Cambrian, a period notable for a rapid increase in the variety of hard-bodied organisms.

Major subdivisions

The Phanerozoic is conventionally divided into three eras, each containing multiple periods and epochs that mark major evolutionary, climatic and tectonic changes:

  • Paleozoic Era — early complex marine life, the rise of fishes, arthropods and early land plants.
  • Mesozoic Era — often called the age of dinosaurs; includes the development of modern groups of reptiles and the first birds and flowering plants.
  • Cenozoic Era — the most recent era, characterized by the diversification of mammals and the appearance of humans.

Characteristics and fossil record

The Phanerozoic is distinguished by abundant, readily fossilized hard parts such as shells, teeth and bones. These fossils provide the backbone of biostratigraphy and allow scientists to correlate rock layers across continents. Major biological innovations recorded in Phanerozoic rocks include complex body plans, sophisticated ecological interactions and repeated episodes of continental reconfiguration driven by plate tectonics.

Origins and the preceding eons

Before the Phanerozoic lay what was traditionally called the Precambrian; that time is now subdivided into the Hadean, Archaean and Proterozoic eons. These earlier eons record the formation of Earth, the origin of life, early microbial ecosystems and the buildup of oxygen in the atmosphere, setting the stage for later animal-dominated ecosystems. The term Precambrian still appears in many summaries as a convenient label for everything older than the Phanerozoic.

Significant events and scientific importance

The Phanerozoic history includes dramatic turnovers such as mass extinctions, the Cambrian diversification often called an "explosion," and repeated shifts in climate and sea level. These events shaped modern biological diversity and influence natural resources — for example, many hydrocarbon reservoirs are associated with Phanerozoic sedimentary basins. Paleontologists and geologists study Phanerozoic rocks to reconstruct past environments, evolutionary pathways and the interactions between life and Earth systems.

Further reading

For introductions and stratigraphic summaries consult overview resources and period descriptions: Phanerozoic overview, Cambrian and general period pages, as well as background on the Precambrian and its subdivisions (Hadean, Archaean, Proterozoic).