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Quaternary

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Quaternary

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Also known as Anthropogene, Quaternary Period, Quaternary System, Pleistogene

The Quaternary ( , ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the Phanerozoic eon. It follows the Neogene Period and spans from 2.6 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.6 million years ago to 12 thousand years ago) and the Holocene (12 thousand years ago to today); a proposed third epoch, the Anthropocene, was rejected in 2024 by International Union of Ge

AI overview

The Quaternary is the current geological period that began 2.6 million years ago and continues today, making it the most recent of the major divisions of Earth's history. It is important because it encompasses the Pleistocene epoch (which saw the rise of humans and ice ages) and the Holocene epoch (our current warm period), providing the geological context for understanding human evolution and modern climate.

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

Key facts

Geologic timespan.name
Quaternary
Geologic timespan.color
Quaternary
Geologic timespan.time_start
2.58
Geologic timespan.time_end
0
Geologic timespan.image_map
Mollweide.jpg
Geologic timespan.caption_map
A map of Earth as it appears during the current Quaternary period, Holocene epoch
Geologic timespan.timeline
Quaternary
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
Period
Geologic timespan.strat_unit
System
Geologic timespan.timespan_formality
Formal
Geologic timespan.lower_boundary_def
Base of magnetic polarity chronozone C2r (Matuyama) Extinction of the Haptophytes Discoaster pentaradiatus and Discoaster surculus
Geologic timespan.lower_gssp_location
Monte San Nicola Section, Gela, Sicily, Italy
Geologic timespan.lower_gssp_accept_date
2009 (as base of Quaternary and Pleistocene)
Geologic timespan.upper_boundary_def
Present day

via Wikipedia infobox

Wikidata facts

Image
Northern icesheet-fr.png
Show 4 more facts
Commons category
Quaternary
sRGB color hex triplet
F9F97F
start time
2580000-00
time of discovery or invention
1829-00-00
Sources (5)

via Wikidata · CC0

~7 min read

Article

7 sections
Contents
  • Research history
  • Geology
  • Climate
  • Flora and fauna
  • See also
  • References
  • External links

The Quaternary ( , ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the Phanerozoic eon. It follows the Neogene Period and spans from 2.6 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.6 million years ago to 12 thousand years ago) and the Holocene (12 thousand years ago to today); a proposed third epoch, the Anthropocene, was rejected in 2024 by International Union of Geological Sciences (IUGS), the governing body of the International Commission on Stratigraphy (ICS).

The Quaternary is typically defined by the Quaternary glaciation, the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused.

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On the map

3 mapped locations

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