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Miocene

File:Mollweide_Paleographic_Map_of_Earth,_15_Ma_(Langhian_Age).png · Wikimedia Commons · See Wikimedia Commons

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Also known as Miocene Epoch, Miocene Series

The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell and comes from Ancient Greek μείων (meíōn), , and καινός (kainós), , and thus means "less recent", because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene followed the Oligocene and preceded the Pliocene.

AI overview

The Miocene is a geological epoch that occurred roughly 23 to 5 million years ago and represents the earliest period of the Neogene, with its name deriving from the Greek words meaning "less recent" because it contains fewer modern marine invertebrates than the later Pliocene epoch. Understanding the Miocene matters because it helps scientists track how life on Earth evolved over time and how marine ecosystems changed between the older Oligocene and the newer Pliocene periods.

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

Key facts

Geologic timespan.time_start
23.04
Geologic timespan.time_end
5.333
Geologic timespan.name
Miocene
Geologic timespan.color
Miocene
Geologic timespan.image_map
Mollweide Paleographic Map of Earth, 15 Ma (Langhian Age).png
Geologic timespan.caption_map
A map of Earth as it appeared 15 million years ago during the Miocene Epoch, Langhian Age
Geologic timespan.timeline
Neogene
Geologic timespan.name_formality
Formal
Geologic timespan.celestial_body
earth
Geologic timespan.usage
Global (ICS)
Geologic timespan.timescales_used
ICS Time Scale
Geologic timespan.chrono_unit
Epoch
Geologic timespan.strat_unit
Series
Geologic timespan.timespan_formality
Formal
Geologic timespan.lower_boundary_def
Base of magnetic polarity chronozone C6Cn.2n FAD of the Planktonic foraminiferan Paragloborotalia kugleri
Geologic timespan.lower_gssp_location
Lemme-Carrosio Section, Carrosio, Italy
Geologic timespan.lower_gssp_accept_date
1996
Geologic timespan.upper_boundary_def
Base of the Thvera magnetic event (C3n.4n), which is only 96 ka (5 precession cycles) younger than the GSSP

via Wikipedia infobox

Wikidata facts

Image
Dromornis BW.jpg
Show 4 more facts
Commons category
Miocene
start time
23030000-0
end time
5333000-00
sRGB color hex triplet
FFFF00
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via Wikidata · CC0

~29 min read

Article

18 sections
Contents
  • Subdivisions
  • Paleogeography
  • Eurasia
  • South America
  • Australia
  • Climate
  • Life
  • Flora
  • Fauna
  • Oceanic
  • Microbiota
  • Oceans
  • Middle Miocene disruption
  • Impact event
  • See also
  • References
  • Further reading
  • External links

The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell and comes from Ancient Greek μείων (meíōn), , and καινός (kainós), , and thus means "less recent", because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene followed the Oligocene and preceded the Pliocene.

As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by distinct global events but by regionally defined transitions from the warmer Oligocene to the cooler Pliocene Epoch.

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