(geology) Lower Cretaceous geologic age, between Hauterivian and Aptian.
| Sci-Tech Dictionary: Barremian |
(geology) Lower Cretaceous geologic age, between Hauterivian and Aptian.
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| Wikipedia: Barremian |
| System | Series | Stage | Age (Ma) | |
|---|---|---|---|---|
| Paleogene | Paleocene | Danian | younger | |
| Cretaceous | Upper | Maastrichtian | 65.5–70.6 | |
| Campanian | 70.6–83.5 | |||
| Santonian | 83.5–85.8 | |||
| Coniacian | 85.8–89.3 | |||
| Turonian | 89.3–93.5 | |||
| Cenomanian | 93.5–99.6 | |||
| Lower | Albian | 99.6–112.0 | ||
| Aptian | 112.0–125.0 | |||
| Barremian | 125.0–130.0 | |||
| Hauterivian | 130.0–136.4 | |||
| Valanginian | 136.4–140.2 | |||
| Berriasian | 140.2–145.5 | |||
| Jurassic | Upper | Tithonian | older | |
| Subdivision of the Cretaceous system according to the IUGS, as of July 2009. | ||||
The Barremian is an age in the geologic timescale (or a chronostratigraphic stage) between 130.0 ± 1.5 Ma (million years ago) and 125.0 ± 1.0 Ma). It is a subdivision of the Early Cretaceous epoch (or Lower Cretaceous series). It is preceded by the Hauterivian and followed by the Aptian stage.[1]
The Barremian falls in the Gallic epoch, a subdivision of the Cretaceous that is no longer used by the ICS. It overlaps the lower part of the Urgonian stage, which is sometimes used in western European stratigraphy. In North America, the late Coahulian and the early Comanchean correspond to the Barremian. In New Zealand, it falls within the Mokoiwian, and in Japan it corresponds to the late Aritan.[1]
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The original type locality for the Barremian stage is in the vicinity of the village of Barrême, Alpes-de-Haute-Provence, France. Henry Coquand defined the stage and named it in 1873.
The base of the Barremian is determined by the first appearance of the ammonites Spitidiscus hugii and Spitidiscus vandeckii. The end of the Barremian is determined by the geomagnetic reversal at the start of the M0r chronozone, which is biologically near the first appearance of the ammonite Paradeshayesites oglanlensis.
The Barremian is often subdivided into two substages or subages, Lower/Early and Upper/Late Barremian.
In the Tethys domain, the Barremian stage contains eleven ammonite biozones:
Much knowledge about the Barremian fauna—especially regarding birds, mammals and pterosaurs—derived from the famous Yixiang Formation of China, part of which dates from this stage.
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| Neocoleoids of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
|
Maioteuthis |
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|
Neololigosepia |
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| Belemnites of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Nautiloids of the Bajocian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
|
Eucymatoceras |
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|
Pseudaturoidea |
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| Cerapoda of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| China | ||||
| Czech Republic | ||||
| Japan | ||||
| England, Portugal | ||||
| China | ||||
| Utah, USA | ||||
| Europe, Africa | ||||
| South Dakota, USA | ||||
| Belgium, Germany, England | ||||
| Europe, Africa, Asia, North America | ||||
| Gansu, China | ||||
| Liaoning, China | ||||
| China, Mongolia, Russia, possibly Thailand | ||||
| Marginocephalia of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Germany | ||||
| Liaoning, China | ||||
| Liaoning, China | ||||
| China, Mongolia, Russia, possibly Thailand | ||||
| Marginocephalia of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Utah, USA | ||||
| Aragón, Spain | ||||
| Neuquén, Argentina | ||||
| Croatia | ||||
| Isle of Wight, England | ||||
| Isle of Wight, England | ||||
| Neuquén, Argentina | ||||
| Theropods of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Japan | ||||
| Liaoning, China | ||||
|
"Proornis" |
North Korea | |||
| Isle of Wight, England | ||||
| Liaoning, China | ||||
| Liaoning, China | ||||
| Liaoning, China | ||||
| Liaoning, China | ||||
| Liaoning, China | ||||
| Utah, USA | ||||
| Cuenca, Spain | ||||
| Cuenca, Spain | ||||
| Gobi Desert, Mongolia | ||||
| Liaoning, China | ||||
| Niger, Africa | ||||
| Liaoning, China | ||||
| Liaoning, China | ||||
| Cuenca, Spain | ||||
| Liaoning, China | ||||
| England, Spain, Portugal | ||||
| China | ||||
| Isle of Wight, England | ||||
| China, Mongolia | ||||
| Isle of Wight, England | ||||
| Liaoning, China | ||||
| Thyreophora of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Liaoning, China | ||||
| Utah, USA | ||||
| South Dakota, USA | ||||
| England | ||||
| Gansu, China | ||||
| England | ||||
| Sussex, England | ||||
| Mammals of the Barremian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| several species from Hauterivian to Albian | Spain, Mongolia |
Skeleton of the primitive mammal Eomaia
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This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| Aptian (geology) | |
| Hauterivian (geology) | |
| Neocomian (geology) |
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