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Greenlandian
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Greenlandian

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Also known as Lower Holocene, Early Holocene, Greenlandian Age, Greenlandian Stage

In the geologic time scale, the Greenlandian is the earliest age or lowest stage of the Holocene Epoch or Series, part of the Quaternary. Beginning in 11,650 BP (9701 BCE or 300 HE) and ending with the 8.2-kiloyear event (c. 8200–8300 BP, 6200–6300 BCE, 3600–3700 HE), it is the earliest of three sub-divisions of the Holocene. It was officially ratified by the International Commission on Stratigraphy in June 2018 with the later Northgrippian and Meghalayan Ages/Stages. The lower boundary of the Greenlandian Age is the GSSP sample from the North Greenland Ice Core Project in ce

Key facts

Geologic timespan.name
Greenlandian
Geologic timespan.color
Greenlandian
Geologic timespan.timeline
Holocene
Geologic timespan.name_formality
Formal
Geologic timespan.name_accept_date
14 June 2018
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
End of the Younger Dryas stadial
Geologic timespan.lower_gssp_location
NGRIP2 ice core, Greenland
Geologic timespan.lower_gssp_accept_date
14 June 2018 (as base of Greenlandian)
Geologic timespan.upper_boundary_def
8.2 kiloyear event
Geologic timespan.upper_gssp_location
NGRIP1 ice core, Greenland
Geologic timespan.upper_gssp_accept_date
14 June 2018

via Wikipedia infobox

Wikidata facts

Instance of
age
Named after
Greenland
Followed by
Northgrippian
Show 4 more facts
sRGB color hex triplet
FEECDB
start time
9701-00-00
end time
6237-00-00
Commons category
Greenlandian
Sources (3)

via Wikidata · CC0

~2 min read

Encyclopedic overview

4 sections
Contents
  • Paleofauna
  • Prehistory
  • See also
  • References

In the geologic time scale, the Greenlandian is the earliest age or lowest stage of the Holocene Epoch or Series, part of the Quaternary. Beginning in 11,650 BP (9701 BCE or 300 HE) and ending with the 8.2-kiloyear event (c. 8200–8300 BP, 6200–6300 BCE, 3600–3700 HE), it is the earliest of three sub-divisions of the Holocene. It was officially ratified by the International Commission on Stratigraphy in June 2018 with the later Northgrippian and Meghalayan Ages/Stages. The lower boundary of the Greenlandian Age is the GSSP sample from the North Greenland Ice Core Project in central Greenland (75.1000°N 42.3200°W). The Greenlandian GSSP has been correlated with the end of Younger Dryas (from near-glacial to interglacial) and a "shift in lower deuterium excess values".

thumb|Diagram of temperatures during the Holocene After the sudden rise in temperatures marking the end of the Late Pleistocene, global warming continued at a slightly more moderate pace during the Greenlandian. It was interrupted at the end of the period by the 8.2 kiloyear event, where the world experienced a relative drop in temperature. This isolated climate fluctuation was used to define the boundary between the Greenlandian and Northgrippian ages.

Excerpted from Wikipedia’s “Greenlandian” article, available under the CC BY-SA 4.0 licence.

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