Mississippian

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Related to Early Carboniferous: Upper Carboniferous period

Mississippian

the Lower CARBONIFEROUS of North America.
Collins Dictionary of Biology, 3rd ed. © W. G. Hale, V. A. Saunders, J. P. Margham 2005
References in periodicals archive ?
Early Tournasian (Early Carboniferous) shallow water communities (eastern part of the Timan-Pechora Province).
During the early Carboniferous, there wasn't anything large to eat on land.
Chronology of Devonian to Early Carboniferous rifting and igneous activity in southern Magdalen Basin based on U-Pb (zircon) dating.
Chanic synorogenic deposits of the early Carboniferous Angualasto Group (Limarino and Cesari, 1993) in Western Precordillera overlie folded and cleaved rocks of Devonian age with a strong angular unconformity (Azcuy et al., 1981; Limarino and Cesari, 1993; Lopez Gamundi and Rossello, 1993; Alonso et al., 2008; Amenabar and di Pasquo, 2008; Colombo et al., 2012; among others).
O rannekamennougolnoj ikhtiofaune Belarusi [On the Early Carboniferous ichthyofauna of Belarus].
The Chanic orogeny took place as a consequence of the accretion of the Chilenia terrane to Gondwana, in the Late Devonian early Carboniferous (Ramos et al., 1984).
We know that splays of the Minas Fault Zone both north and south of the eventual Cobequid-Chedabucto fault zone were active in the early Carboniferous (Roman Valley fault, West River St.
Early Tournaisian (Early Carboniferous) shallow water communities (Eastern part of the Timan-Pechora Province).
The continuous early Devonian to early Carboniferous sedimentation in the Arrayan basin (Charrier et al., 2007) demonstrates that the Chanic deformation did not affect the western passive margin of the Chilenia--Occidentalia terrane (Fig 10c).
Thus we characterize the Chanic structures and metamorphism of the Late Devonian and early Carboniferous, the extensional regime related to the Carboniferous basins development, as well as their later contractional deformation during the San Rafael (Gondwanan) orogeny, in early Permian times.
2003) which intruded the Guysborough Group and which could have been exposed by the Early Carboniferous. However, clasts of this distinctive granite were not noted in the section.
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