last of four internationally defined stages of the Pennsylvanian Subsystem (Pennsylvanian Subperiod), Carboniferous System (Carboniferous Period), encompassing all rocks deposited during the Gzhelian Age (303.9 to 299 million years ago). The name is taken from the Russian city of Gzhel, which lies just southeast of Moscow in the Moscow Basin. Gzhelian strata are cyclic but consist mainly of dolomite, dolomitic marls (marl), and intercalated siltstones (siltstone).

The base of the stage has been historically drawn at the appearance of the advanced fusulinid (single-celled amoeba-like organisms with complex shells) species Rauserites rossicus, R. stuckenbergi, Jigulites jigulensis, and Daixina sokensis. However, working groups of the International Commission on Stratigraphy (ICS) now believe that using the first appearances of the conodont (primitive chordates with tooth-shaped fossil remains) Idiognathodus simulator is more useful for the global correlation of basal Gzhelian strata. To date, no Global Stratotype Section and Point (GSSP) section for the base of this stage has been submitted to the ICS.

In contrast, the top of the Gzhelian, and thus the Carboniferous-Permian boundary, has been demarcated by a GSSP at the Aidaralash Creek section in northern Kazakhstan. This section was ratified by the ICS in 1996. The Gzhelian Stage lies above the Kasimovian Stage of the Pennsylvanian Subsystem, Carboniferous System, and is overlain by the Asselian Stage of the Permian System (Permian Period).