carboniferous system

Omphalophloios is a genus of fossil lycopsid trees in the Carboniferous system.

It is a subdivision of the Carboniferous system or period and the regional Silesian series.

Dinantian is the name of a series or epoch from the Lower Carboniferous system in Europe.

Vast swaths of forest covered the land, which would eventually be laid down and become the coal beds characteristic of the Carboniferous system.

New genera of batrachian footprints of the Carboniferous System in eastern Canada.

The Warwickshire Group is a lithostratigraphic unit of rock strata defined within the British Carboniferous system.

The Coal Measures is a lithostratigraphical term for the coal-bearing part of the Upper Carboniferous System.

Palaeontology - contributions to The Carboniferous System (biostratigraphy, biogeography, geochronology, and magnetostratigraphy)

The Carboniferous system, Permian System and Triassic systems are seen in the western Himalayas.

Palaeontology, The Carboniferous System, Palaeozoic Ostracoda, Fossil Conchostraca, The Geological Timescale.

Monografia do gênero Dicranophillum (Sistema Carbónico) (Monograph of the genus Dicranophillum [Carboniferous System])

Hainaut small granite, or Arquennes, Feluy and Soignies bluestone is a limestone that is a natural grey-blue colour composed of approximately 96% calcite, from the secondary era (Carboniferous system).

The Cretaceous system is for example divided into the Upper Cretaceous and Lower Cretaceous series; while the Carboniferous system is divided in the Pennsylvanian and Mississippian series.

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.

In geology, Bernician Series was a term proposed by Samuel Pickworth Woodward in 1856 (Manual of Mollusca, p. 409) for the lower portion of the Carboniferous System, below the Millstone Grit.

In Europe, the Mississippian and Pennsylvanian are one more-or-less continuous sequence of lowland continental deposits and are grouped together as the Carboniferous system, and sometimes called the Upper Carboniferous and Lower Carboniferous instead.

The base of the Tournaisian (which is also the base of the Carboniferous system) is at the first appearance of the conodont Siphonodella sulcata within the evolutionary lineage from Siphonodella praesulcata to Siphonodella sulcata.