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Silurian

File:Mollweide_Paleographic_Map_of_Earth,_430_Ma_(Homerian_Age).png · Wikimedia Commons · See Wikimedia Commons

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Also known as Silurian Period, Silurian System

The Silurian ( ) is a geologic period and system spanning 23.5 million years from the end of the Ordovician Period, at Ma (million years ago) to the beginning of the Devonian Period, Ma. The Silurian is the third and shortest period of the Paleozoic Era, and the third of twelve periods of the Phanerozoic Eon. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera we

AI overview

The Silurian is a geologic period that lasted about 23.5 million years during the Paleozoic Era, positioned between the Ordovician and Devonian periods. It matters because studying the Silurian helps scientists understand a time marked by major extinction events and the evolution of life on Earth.

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

Key facts

Geologic timespan.name
Silurian
Geologic timespan.color
Silurian
Geologic timespan.time_start
443.1
Geologic timespan.time_start_uncertainty
0.9
Geologic timespan.time_end
419.62
Geologic timespan.time_end_uncertainty
1.36
Geologic timespan.image_map
Mollweide Paleographic Map of Earth, 430 Ma (Homerian Age).png
Geologic timespan.caption_map
A map of Earth as it appeared 430 million years ago during the Silurian Period, Wenlock Epoch
Geologic timespan.timeline
Silurian
Geologic timespan.name_formality
Formal
Geologic timespan.synonym1
Gotlandian
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.proposed_by
Roderick Murchison, 1835
Geologic timespan.timespan_formality
Formal

via Wikipedia infobox

Wikidata facts

Image
68-224-5027 Китайгородське відслонення.jpg
Show 4 more facts
Commons category
Silurian
sRGB color hex triplet
B3E1B6
start time
443100000-
end time
419620000-
Sources (2)

via Wikidata · CC0

~18 min read

Article

10 sections
Contents
  • History of study
  • Subdivisions
  • Paleogeography
  • Climate and sea level
  • Perturbations
  • Flora and fauna
  • See also
  • Notes
  • References
  • External links

The Silurian ( ) is a geologic period and system spanning 23.5 million years from the end of the Ordovician Period, at Ma (million years ago) to the beginning of the Devonian Period, Ma. The Silurian is the third and shortest period of the Paleozoic Era, and the third of twelve periods of the Phanerozoic Eon. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out.

One important event in this period was the initial establishment of terrestrial life in what is known as the Silurian-Devonian Terrestrial Revolution: vascular plants emerged from more primitive land plants, dikaryan fungi started expanding and diversifying along with glomeromycotan fungi, and three groups of arthropods (myriapods, arachnids and hexapods) became fully terrestrialized.

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On the map

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