| System | Series | Stage | Age (Ma) | |
|---|---|---|---|---|
| Cretaceous | Lower | Berriasian | younger | |
| Jurassic | Upper | Tithonian | 145.5–150.8 | |
| Kimmeridgian | 150.8–155.7 | |||
| Oxfordian | 155.7–161.2 | |||
| Middle | Callovian | 161.2–164.7 | ||
| Bathonian | 164.7–167.7 | |||
| Bajocian | 167.7–171.6 | |||
| Aalenian | 171.6–175.6 | |||
| Lower | Toarcian | 175.6–183.0 | ||
| Pliensbachian | 183.0–189.6 | |||
| Sinemurian | 189.6–196.5 | |||
| Hettangian | 196.5–199.6 | |||
| Triassic | Upper | Rhaetian | older | |
| Subdivision of the Jurassic system according to the IUGS, as of July 2009. | ||||
The Late Jurassic epoch of the Jurassic Period is the unit of geologic time from 161.2 ± 4.0 to 145.5 ± 4.0 million years ago, which is preserved in Upper Jurassic strata.[1] In European lithostratigraphy, the name Malm indicates rocks of Late Jurassic age. In the past this name 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.
Contents |
The Late Jurassic is divided into three ages, which correspond with the three (faunal) stages of Upper Jurassic rock:
| Tithonian | (150.8 ± 4.0 – 145.5 ± 4.0 Ma) |
| Kimmeridgian | (155.7 ± 4.0 – 150.8 ± 4.0 Ma) |
| Oxfordian | (161.2 ± 4.0 – 155.7 ± 4.0 Ma) |
Pangaea broke up into two supercontinents, Laurasia to the north, and Gondwana to the south. The result of this break-up was the spawning of the Atlantic Ocean. However, at this time, the Atlantic Ocean was relatively narrow.
This period was well known for many famous types of dinosaurs, such as the sauropods, the theropods, the thyreophorans, and the ornithopods. Other animals, such as crocodiles and the first birds, appeared in the Jurassic. Here are only a few of the many Jurassic animals:
| Jurassic period | ||
|---|---|---|
| Lower/Early Jurassic | Middle Jurassic | Upper/Late Jurassic |
|
Hettangian | Sinemurian Pliensbachian | Toarcian |
Aalenian | Bajocian Bathonian | Callovian |
Oxfordian | Kimmeridgian Tithonian |
|
|