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Carboniferous

   Also found in: Encyclopedia, Wikipedia, Hutchinson 0.04 sec.
Car·bon·if·er·ous  (kärb-nfr-s)
adj.
1. Of, belonging to, or denoting a geologic division of the Paleozoic Era following the Devonian and preceding the Permian, including the Mississippian Period and the Pennsylvanian Period and characterized, especially in the Pennsylvanian, by swamp formation and deposition of plant remains later hardened into coal.
2. carboniferous Producing or containing carbon or coal.
n.
The Carboniferous Period. See Table at geologic time.

carboniferous
Adjective
yielding coal or carbon

Carboniferous
Adjective
Geol of the period of geological time about 330 million years ago, during which coal seams were formed

Carboniferous  (kärb-nfr-s)
The period of geologic time from about 360 to 286 million years ago. The term is used throughout the world, although this period of time has been separated into the Mississippian (lower Carboniferous) and Pennsylvanian (upper Carboniferous) in the United States. During this time, widespread swamps formed in which plant remains accumulated and later hardened into coal. See Chart at geologic time.
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.Carboniferous - from 345 million to 280 million years ago
Paleozoic, Paleozoic era - from 544 million to about 230 million years ago
Pennsylvanian, Pennsylvanian period, Upper Carboniferous, Upper Carboniferous period - from 310 million to 280 million years ago; warm climate; swampy land
Lower Carboniferous, Lower Carboniferous period, Missippian period, Mississippian - from 345 million to 310 million years ago; increase of land areas; primitive ammonites; winged insects
Adj.1.carboniferous - of or relating to the Carboniferous geologic era; "carboniferous rock system"
2.carboniferous - relating to or consisting of or yielding carbon


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Lyell in the carboniferous strata of North America.
The main points of interest consist, first in some highly fossiliferous strata, belonging to the Devonian or Carboniferous period; secondly, in proofs of a late small rise of the land; and lastly, in a solitary and superficial patch of yellowish limestone or travertin, which contains numerous impressions of leaves of trees, together with land-shells, not now existing.
Thus conversing we followed the intricate trail toward the temple, which we came upon in a small clearing surrounded by enormous trees similar to those which must have flourished upon the outer crust during the carboniferous age.
 
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