In the geologic timescale, the Homerian is an age of the Wenlock Epoch of the Silurian Period of the Paleozoic Era of the Phanerozoic Eon that is comprehended between 430.5 ± 0.7 Ma and 427.4 ± 0.5 Ma (million years ago), approximately. The Homerian Age succeeds the Sheinwoodian Age and precedes the Gorstian Age.

Quick Facts Chronology, Etymology ...

Homerian
430.5 ± 0.7 – 427.4 ± 0.5 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Paleogeography of the Homerian, 430 Ma
Chronology
−444 — – −442 — – −440 — – −438 — – −436 — – −434 — – −432 — – −430 — – −428 — – −426 — – −424 — – −422 — – −420 — – −418 — Paleozoic O Silurian D L Llandovery Wenlock Ludlow Přídolí E Hirnantian Rhuddanian Aeronian Telychian Sheinwoodian Homerian Gorstian Ludfordian Lochkovian             ← Lau event ← Mulde event[1] ← Ireviken event[2] Subdivision of the Silurian according to the ICS, as of 2021.[3] Vertical axis scale: millions of years ago.
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 Cyrtograptus lundgreni
Lower boundary GSSP	Sheinton Brook, Homer, England 52.6156°N 2.5647°W / 52.6156; -2.5647
Lower GSSP ratified	1980[4]
Upper boundary definition	FAD of the graptolite Saetograptus (Colonograptus) varians
Upper boundary GSSP	Pitch Coppice, Ludlow, U.K. 52.3592°N 2.7772°W / 52.3592; -2.7772
Upper GSSP ratified	1980[4]

Close

The name comes from the small village of Homer, Shropshire near Much Wenlock.^[5] The defining lower boundary of Homerian rock layers (GSSP) is located within the Coalbrookdale Formation of England.