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Paleozoic

File:Trilobite_Heinrich_Harder.jpg · Wikimedia Commons · See Wikimedia Commons

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Also known as Palaeozoic, Palaeozoic Era, Paleozoic Era, Paleozoic Erathem

The Paleozoic ( , , ; or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six geologic periods, (from oldest to youngest) Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consi

AI overview

The Paleozoic Era is the first major division of Earth's most recent 538 million years of history, spanning from about 539 to 252 million years ago and subdivided into six geological periods. It matters because it represents a foundational chapter in the history of complex life on Earth, bridging the time between the emergence of most animal groups and the rise of the age of dinosaurs.

AI-generated from the Wikipedia summary — may contain errors.

Key facts

Geologic timespan.name
Paleozoic
Geologic timespan.color
Paleozoic
Geologic timespan.top_bar
Phanerozoic
Geologic timespan.timeline
Paleozoic
Geologic timespan.name_formality
Formal
Geologic timespan.alternate_spellings
Palaeozoic
Geologic timespan.celestial_body
earth
Geologic timespan.usage
Global (ICS)
Geologic timespan.timescales_used
ICS Time Scale
Geologic timespan.chrono_unit
Era
Geologic timespan.strat_unit
Erathem
Geologic timespan.lower_boundary_def
Appearance of the Ichnofossil Treptichnus pedum
Geologic timespan.lower_gssp_location
Fortune Head section, Newfoundland, Canada
Geologic timespan.upper_boundary_def
First appearance of the Conodont Hindeodus parvus.
Geologic timespan.upper_gssp_location
Meishan, Zhejiang, China

via Wikipedia infobox

Wikidata facts

Image
Trilobite Heinrich Harder.jpg
Show 4 more facts
Commons category
Paleozoic
start time
538800000-
end time
251902000-
sRGB color hex triplet
99C08D
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~17 min read

Article

17 sections
Contents
  • Boundaries
  • Geology
  • Cambrian Period
  • Ordovician Period
  • Silurian Period
  • Devonian Period
  • Carboniferous Period
  • Permian Period
  • Climate
  • Flora
  • Fauna
  • Microbiota
  • See also
  • Footnotes
  • References
  • Further reading
  • External links

The Paleozoic ( , , ; or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six geologic periods, (from oldest to youngest) Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian.

The name Paleozoic was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Greek palaiós (παλαιός, "old") and zōḗ (ζωή, "life") meaning "ancient life".

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