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Also known as Santonian Stage, Santonian Age

The Santonian is an age in the geologic timescale or a chronostratigraphic stage. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series. It spans the time between 85.7 ± 0.2 mya (million years ago) and 83.6 ± 0.2 mya. The Santonian is preceded by the Coniacian and is followed by the Campanian.

Key facts

Geologic timespan.name
Santonian
Geologic timespan.color
Santonian
Geologic timespan.time_start
85.7
Geologic timespan.time_start_uncertainty
0.2
Geologic timespan.time_end
83.6
Geologic timespan.time_end_uncertainty
0.2
Geologic timespan.timeline
Cretaceous
Geologic timespan.name_formality
Formal
Geologic timespan.celestial_body
earth
Geologic timespan.usage
Global (ICS)
Geologic timespan.timescales_used
ICS Time Scale
Geologic timespan.chrono_unit
Age
Geologic timespan.strat_unit
Stage
Geologic timespan.timespan_formality
Formal
Geologic timespan.lower_boundary_def
FAD of the Inoceramid Bivalve Cladoceramus undulatoplicatus
Geologic timespan.lower_gssp_location
Olazagutia, Spain
Geologic timespan.lower_gssp_accept_date
January 2013
Geologic timespan.upper_boundary_def
Base of Chron C33r

via Wikipedia infobox

Wikidata facts

Show 3 more facts
start time
86300000-0
end time
83600000-0
sRGB color hex triplet
DEE78A
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via Wikidata · CC0

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Article

6 sections
Contents
  • Stratigraphic definition
  • Subdivision
  • References
  • Notes
  • Literature
  • External links

The Santonian is an age in the geologic timescale or a chronostratigraphic stage. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series. It spans the time between 85.7 ± 0.2 mya (million years ago) and 83.6 ± 0.2 mya. The Santonian is preceded by the Coniacian and is followed by the Campanian.

==Stratigraphic definition== The Santonian Stage was established by French geologist Henri Coquand in 1857. It is named after the city of Saintes in the region of Saintonge, where the original type locality is located.

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