Gelasian
's information is

Birth and death years unknown

The Gelasian is an age in the international geologic timescale or a stage in chronostratigraphy, being the earliest or lowest subdivision of the Quaternary Period/System and Pleistocene Epoch/Series. It spans from 2.58–1.80 million years ago, following the Piacenzian Age (from the Pliocene Epoch) and preceding the Calabrian Age.

* Calculated from Wikipedia data.
Accuracy is not guaranteed.

Gelasian
2.58 – 1.80 Ma
Chronology
−2.6 —
−2.4 —
−2.2 —
−2 —
−1.8 —
−1.6 —
−1.4 —
−1.2 —
−1 —
−0.8 —
−0.6 —
−0.4 —
−0.2 —
0 —
Cenozoic
 
 
 
 
 
 
 
 
Subdivision of the Quaternary according to the ICS, as of 2024.
Vertical axis scale: Millions of years ago
Formerly part ofTertiary Period/System
Pliocene Epoch/Series
Etymology
Name formalityFormal
Name ratifiedAugust 1996
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definition
Lower boundary GSSPMonte San Nicola Section, Gela, Sicily, Italy
37°08′49″N 14°12′13″E / 37.1469°N 14.2035°E / 37.1469; 14.2035
Lower GSSP ratifiedAugust 1996 (as base of Gelasian)
Upper boundary definitionApproximately 8 m after the end of magnetic polarity chronozone C2n (Olduvai).
Upper boundary GSSPVrica Section, Calabria, Italy
39°02′19″N 17°08′05″E / 39.0385°N 17.1348°E / 39.0385; 17.1348
Upper GSSP ratified5 December 2011 (as base of Calabrian)
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