(geology) Part of or the underlying stage of the Valanginian at the base of the Cretaceous.
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(geology) Part of or the underlying stage of the Valanginian at the base of the Cretaceous.
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| 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. | ||||
In the geologic timescale, the Berriasian is an age or stage of the Early or Lower Creteceous. It is the oldest or lowest subdivision in the entire Cretaceous. It spanned between 145.5 ± 4.0 Ma and 140.2 ± 3.0 Ma (million years ago). The Berriasian succeeds the Tithonian (part of the Jurassic) and precedes the Valanginian.[1]
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The Berriasian stage was introduced in scientific literature by Henri Coquand in 1869. It is named after the village of Berrias in the Ardèche region of France. The English Wealden Group is of Berriasian age and in the past the name Wealden was also used to address rocks of the lowest Cretaceous.
The base of the Berriasian (also the base of the Cretaceous system) is at the first appearance of fossils of ammonite species Berriasella jacobi. A global reference profile (a GSSP) for the Berriasian had in 2009 not yet been established. A section in Austria has been proposed for ratification.
The top of the Berriasian stage (the base of the Valanginian) is at the first appearance of calpionellid species Calpionellites darderi in the stratigraphic column. This is just a little below the first appearance of ammonite species Thurmanniceras pertransiens.
In the Tethys domain, the Berriasian contains four ammonite biozones, from top to bottom:
| Birds of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Crocodylomorphs of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Mammals of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Durlston Bay, Dorset, England | ||||
| Durlston Bay, Dorset, England; Spain | ||||
| Portugal | ||||
| Durlston Bay, Dorset, England | ||||
| Portugal | ||||
| Ornithischians of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Swanage, England | A bipedal herbivore, it was around 0.6 meters (2 ft) long. Unlike most ornithischians, Echinodon had one or two caniniform teeth in each maxilla. | |||
| Kirkwood Formation, Cape Province, South Africa | A 4 meters long, 1.8 meters high stegosaurid with a skull similar to Kentrosaurus | |||
| Isle of Wight, England; Niger, Africa | A dryosaurid | |||
| Pterosaurs of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Sauropods of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| †Thalattosuchians of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| From Kimmeridgian to Valanginian | Austria, England, Germany, Portugal and Switzerland | |||
| Attested since Toarcian | England, France, Germany, Switzerland and Morocco | |||
| †Non-avian theropods of the Berriasian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| Neocomian (geology) | |
| Portlandian (geology) | |
| Early Cretaceous |
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