From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
System Series
(NW Europe)
(NW Europe)
Permian younger
Carboniferous Silesian Stephanian Pennsylvanian Gzhelian 298.9–303.7
Westphalian Kasimovian 303.7–307.0
Moscovian 307.0–315.2
Bashkirian 315.2–323.2
Mississippian Serpukhovian 323.2–330.9
Dinantian Visean Visean 330.9–346.7
Tournaisian Tournaisian 346.7–358.9
Devonian older
Subdivisions of the Carboniferous system in Europe compared with the official ICS-stages (as of 2018)

Dinantian is the name of a series or epoch from the Lower Carboniferous system in Europe. It can stand for a series of rocks in Europe or the time span in which they were deposited.

The Dinantian is equal to the lower part of the Mississippian series in the international geologic timescale of the ICS, it also correlates with the Avonian, a name proposed by British geologist Arthur Vaughan (1905; p. 264) for certain deposits of the Lower Carboniferous system in the Avon Gorge at Bristol.[1] The Dinantian is named for the Belgian city and province of Dinant where strata of this age occur; the name is still used among European geologists.

The upper Avonian (Kidwellian) is well developed about Kidwelly in Carmarthenshire; the lower substage (Clevedonian) is well displayed near Clevedon in Somerset.[2]

See also[edit]


  1. ^ Chisholm 1911.
  2. ^  One or more of the preceding sentences incorporates text from a publication now in the public domainChisholm, Hugh, ed. (1911). "Avonian" . Encyclopædia Britannica. 3 (11th ed.). Cambridge University Press. p. 67.
  • Vaughan, A. (1905) "The Palæntological Sequence in the Carboniferous Limestone of the Bristol Area", Quarterly Journal of the Geological Society, 61 (1-4), p. 181-307 doi:10.1144/GSL.JGS.1905.061.01-04.13