The base of the Telychian Stage is defined in an abandoned quarry forming part of the Cefn-cerig Road section, Wales, UK, and is just above the highest record of the brachiopod Eocoelia intermedia and below the earliest record of the succeeding species Eocoelia intermedia .
The GSSP is located in an abandoned quarry forming part of the Cefn-cerig Road section, just below the top of the Wormwood Formation, Wales, UK.
The GSSP lies within the bioturbated sandstones and siltstones of the Wormwood Formation.
The base of the Telychian Stage is defined at a point just above the highest record of the brachiopod Eocoelia intermedia and below the earliest record of the succeeding species Eocoelia curtisi.
Acritarchs:
The boundary horizon corresponds with the base of the Biozone 4 acritarch fauna of Hill (1974). It is characterized by the incoming of Deunffia monospinosa, Domasia bispinosa and Pterospermella cf. foveolata.
Just above Brachiopod LAD Eocoelia intermedia and below FAD of Eocoelia curtisi
See:
Holland, C. H. and Bassett, M. G., 1989 (eds.). A global standard for the Silurian System. National Museum of Wales, Geological Series 9, Cardiff.
Holland, C. H., 1985. Series and Stages of the Silurian System. Episodes 8/2, p. 101-103.
Cocks, L. R. M., 1989. The Llandovery Series in the Llandovery Area. In: Holland, C. H. and Bassett, M. G. (eds.). A global standard for the Silurian System. National Museum of Wales, Geological Series 9, p. 36 - 50, Cardiff.