
The Barstovian North American Stage on the
geologic timescale
The geologic time scale or geological time scale (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochron ...
is the North American
faunal stage
In chronostratigraphy, a stage is a succession of rock strata laid down in a single age on the geologic timescale, which usually represents millions of years of deposition. A given stage of rock and the corresponding age of time will by conven ...
according to the
North American Land Mammal Ages
The North American land mammal ages (NALMA) establishes a geologic timescale for North American fauna beginning during the Late Cretaceous and continuing through to the present. These periods are referred to as ages or intervals (or stages when ref ...
chronology (NALMA), typically set from 16,300,000 to 13,600,000 years
BP, a period of .
Paleobiology Database, Barstovian
/ref> It is usually considered to overlap the Langhian
The Langhian is, in the ICS geologic timescale, an age or stage in the middle Miocene Epoch/Series. It spans the time between 15.97 ± 0.05 Ma and 13.65 ± 0.05 Ma (million years ago) during the Middle Miocene.GeoWhen (2007)
The Langhian was ...
and Serravallian
The Serravallian is, in the geologic timescale, an List of time periods, age or a stage (stratigraphy), stage in the middle Miocene epoch (geology), Epoch/series (stratigraphy), Series, which spans the time between 13.82 annum, Ma and 11.63 Ma (m ...
stages of the Middle Miocene
The Middle Miocene is a sub-epoch of the Miocene epoch (geology), epoch made up of two Stage (stratigraphy), stages: the Langhian and Serravallian stages. The Middle Miocene is preceded by the Early Miocene.
The sub-epoch lasted from 15.97 ± 0. ...
. The Barstovian is preceded by the Hemingfordian
The Hemingfordian on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 20,600,000 to 16,300,000 years BP. It is usually considered to overlap the lates ...
and followed by the Clarendonian
The Clarendonian North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 13,600,000 to 9,000,000 years BP, a period of .
It is us ...
NALMA stages.
The Barstovian can be further divided into the substages of:
* late Late Barstovian: Lower boundary source of the base of the Langhian (approximate)
* early Late Barstovian: Base of the Langhian (approximate)
* early/lower Barstovian: Upper boundary source: base of Clarendonian (approximate)
Correlations
The Barstovian (15.97 to 13.6 Ma) correlates with:
* SALMA
** Colloncuran (15.5-13.8 Ma)[Colloncuran]
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** earliest Laventan (13.8-11.8 Ma)[Laventan]
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* ELMA - Astaracian
The Astaracian age is a period of geologic time (), equivalent with the Middle Miocene and used more specifically with European Land Mammal Ages. It precedes the Vallesian age and follows the Orleanian age. The Astaracian overlaps the Langhian a ...
(15.97-11.608 Ma)[Astaracian]
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* Mammal Neogene Units, European Faunal Zones
** MN 5 zone (15.97-13.65 Ma)[MN 5 zone]
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* CPS[Central Paratethys Stages]
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** earliest Badenian (13.65-12.7 Ma)[Badenian]
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* New Zealand stratigraphy - Southland epoch (15.9-10.92 Ma)[Southland epoch]
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** Clifdenian (15.9-13.65 Ma)[Clifdenian]
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** earliest Lillburnian (13.65-12.7 Ma)[Lillburnian]
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* NMAC
** Shanwangian (16.9-13.65 Ma)[Shanwangian]
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** earliest Tunggurian (13.65-11.1 Ma)[Tunggurian]
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References
{{Neogene Footer
Miocene life
Miocene geochronology
Miocene animals of North America
Miocene California