Gorstian
Sixth stage of the Silurian / From Wikipedia, the free encyclopedia
In the geologic timescale, the Gorstian is an age of the Ludlow Epoch of the Silurian Period of the Paleozoic Era of the Phanerozoic Eon that is comprehended between 427.4 ± 0.5 Ma and 425.6 ± 0.9 Ma (million years ago), approximately. The Gorstian Age succeeds the Homerian Age and precedes the Ludfordian Age.[5] The age is named after Gorsty village southwest of Ludlow. The base of the age is marked by Graptolites tumescens and Graptolites incipiens. The type section is located in a quarry in the Elton Formation at Pitch Coppice, Shropshire, United Kingdom.[6]
Quick Facts Chronology, Etymology ...
Gorstian | |||||||||||||
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427.4 ± 0.5 – 425.6 ± 0.9 Ma | |||||||||||||
Chronology | |||||||||||||
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Etymology | |||||||||||||
Name formality | Formal | ||||||||||||
Name ratified | 1980[4] | ||||||||||||
Usage information | |||||||||||||
Celestial body | Earth | ||||||||||||
Regional usage | Global (ICS) | ||||||||||||
Time scale(s) used | ICS Time Scale | ||||||||||||
Definition | |||||||||||||
Chronological unit | Age | ||||||||||||
Stratigraphic unit | Stage | ||||||||||||
Time span formality | Formal | ||||||||||||
Lower boundary definition | FAD of the graptolite Saetograptus (Colonograptus) varians | ||||||||||||
Lower boundary GSSP | Pitch Coppice, Ludlow, U.K. 52.3592°N 2.7772°W / 52.3592; -2.7772 | ||||||||||||
Lower GSSP ratified | 1980[4] | ||||||||||||
Upper boundary definition | Imprecise. Near FAD of the graptolite Saetograptus leintwardinensis | ||||||||||||
Upper boundary definition candidates | None | ||||||||||||
Upper boundary GSSP candidate section(s) | None | ||||||||||||
Upper boundary GSSP | Sunnyhill, Ludlow, England 52.3592°N 2.7772°W / 52.3592; -2.7772 | ||||||||||||
Upper GSSP ratified | 1980[4] |
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