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Carboniferous

File:Mollweide_Paleographic_Map_of_Earth,_330_Ma_(Serpukhovian_Age).png · Wikimedia Commons · See Wikimedia Commons

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Carboniferous

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Also known as Carboniferous System, Carboniferous Period

The Carboniferous ( ) is a geologic period and system of the Paleozoic era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth period of the Phanerozoic eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian.

AI overview

The Carboniferous is a geologic period that lasted 60 million years during the Paleozoic era, situated between the Devonian and Permian periods. It matters as a major division of Earth's history and is sometimes split into two periods in North America called the Mississippian and Pennsylvanian.

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

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Vinony's link graph records 25,831 inbound references to Carboniferous, and connects out to geologic time scale, Visean and year.

The entry is geolocated on the map, across 60 mapped points.

It sits within the topics Carboniferous and Geological periods.

Vinony links it to 86 Wikipedia language editions.

Key facts

Geologic timespan.name
Carboniferous
Geologic timespan.color
Carboniferous
Geologic timespan.time_start
358.86
Geologic timespan.time_start_uncertainty
0.19
Geologic timespan.time_end
298.9
Geologic timespan.time_end_uncertainty
0.15
Geologic timespan.image_map
Mollweide Paleographic Map of Earth, 330 Ma (Serpukhovian Age).png
Geologic timespan.caption_map
A map of Earth as it appeared 330 million years ago during the Carboniferous Period, Mississippian Subperiod
Geologic timespan.timeline
Carboniferous
Geologic timespan.name_formality
Formal
Geologic timespan.nicknames
Age of Amphibians
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
William Daniel Conybeare and William Phillips, 1822
Geologic timespan.timespan_formality
Formal

via Wikipedia infobox

Wikidata facts

Image
Mollweide Paleographic Map of Earth, 330 Ma (Serpukhovian Age).png
Show 5 more facts
Commons category
Carboniferous
sRGB color hex triplet
67A599
start time
358900000-
end time
298900000-
IPA transcription
/ˌkɑːrbəˈnɪfərəs/
Sources (5)

via Wikidata · CC0

~65 min read

Encyclopedic overview

38 sections
Contents
  • Etymology and history
  • Geology
  • Stratigraphy
  • Mississippian
  • Pennsylvanian
  • Cyclothems
  • Coal formation
  • Palaeogeography
  • Variscan-Alleghanian-Ouachita orogeny
  • Uralian orogeny
  • Laurussia
  • Gondwana
  • Siberia and Amuria
  • Central and East Asia
  • Climate
  • Temperatures
  • Atmospheric oxygen levels
  • Effects of climate on sedimentation
  • Effects of climate on biodiversity
  • Geochemistry
  • Magnesium/calcium isotope ratios in seawater
  • Strontium isotopic composition of seawater
  • Oxygen and carbon isotope ratios in seawater
  • Life
  • Plants
  • Marine invertebrates
  • Freshwater and lagoonal invertebrates
  • Terrestrial invertebrates
  • Fish
  • Tetrapods
  • Fungi
  • Extinction events
  • Romer's gap
  • Carboniferous rainforest collapse
  • See also
  • References
  • Sources
  • External links

The Carboniferous ( ) is a geologic period and system of the Paleozoic era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth period of the Phanerozoic eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian.

The name Carboniferous means "coal-bearing", from the Latin ("coal") and ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern "system" names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession.

Excerpted from Wikipedia’s “Carboniferous” article, available under the CC BY-SA 4.0 licence.

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