The Late Jurassic is the third epoch of the Jurassic Period, and it spans the geologic time from 161.5 ± 1.0 to 143.1 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic strata.[2]
Late/Upper Jurassic | |||||||||
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![]() A map of Earth as it appeared 155 million years ago during the Late Jurassic Epoch, Oxfordian Age | |||||||||
Chronology | |||||||||
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Etymology | |||||||||
Chronostratigraphic name | Upper Jurassic | ||||||||
Geochronological name | Late Jurassic | ||||||||
Name formality | Formal | ||||||||
Usage information | |||||||||
Celestial body | Earth | ||||||||
Regional usage | Global (ICS) | ||||||||
Time scale(s) used | ICS Time Scale | ||||||||
Definition | |||||||||
Chronological unit | Epoch | ||||||||
Stratigraphic unit | Series | ||||||||
Time span formality | Formal | ||||||||
Lower boundary definition | Not formally defined | ||||||||
Lower boundary definition candidates | Horizon of the Ammonite Cardioceras redcliffense. | ||||||||
Lower boundary GSSP candidate section(s) |
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Upper boundary definition | Not formally defined | ||||||||
Upper boundary definition candidates |
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Upper boundary GSSP candidate section(s) | None |
In European lithostratigraphy, the name "Malm" indicates rocks of Late Jurassic age.[3] In the past, Malm was also used to indicate the unit of geological time, but this usage is now discouraged to make a clear distinction between lithostratigraphic and geochronologic/chronostratigraphic units.
The Late Jurassic is divided into three ages, which correspond with the three (faunal) stages of Upper Jurassic rock:[citation needed]
Tithonian | (149.2 ±0.7 – 143.1 ± 0.8 Ma) |
Kimmeridgian | (154.8 ±0.8 – 149.2 ±0.7 Ma) |
Oxfordian | (161.5 ± 1.0 – 154.8 ±0.8 Ma) |
During the Late Jurassic Epoch, Pangaea broke up into two supercontinents, Laurasia to the north, and Gondwana to the south. The result of this break-up was the emergence of the Atlantic Ocean, which initially was relatively narrow.[citation needed]
This epoch is well known for many famous types of dinosaurs, such as the sauropods, the theropods, the thyreophorans, and the ornithopods. Other animals, such as some crocodylomorphs and the first birds, appeared in the Jurassic. Listed here are only a few of the many Jurassic animals: