Late Jurassic (163.5 +/-1.0 Ma)
Back to Jurassic (201.4 +/-0.2 Ma)Representation and status
- Color CMYK
- 30 / 0 / 0 / 0
- Color RGB
- R: 179 G: 227 B: 238
- Rank
- chronostratigraphic Epoch
- Validity
- Unit is in Use
- Status
- valid formal name
Nomenclature
- Deutsch
- Später Jura
- Français
- Jurassique tardif
- Italiano
- Giurassico tardo
- English
- Late Jurassic (163.5 +/-1.0 Ma)
- Historical Variants
-
Néojurassique (Lugeon 1910: incl. Callovien), Série néojurassique (Revil 1911), Malm [sic], fini-jurassique (Detraz 1989)
Hierarchy and sequence
- Units at roof
Age
- Age at top
-
- Tithonian
- Age at base
-
- Oxfordian
-
Tithonian (152.1 +/-0.9 Ma)
- Name Origin
-
Named derived from the Greek mythology: Tithon was the son of Laomedon of Troy, who fell in love with Eos, Greek goddess of the dawn (thus prefiguring the Cretaceous system).
- Rank
- chronostratigraphic Stage
- Status
- valid formal name
- Nomenclatorial Remarks
- <p>The Berriasella jacobi Zone, previously placed at the end of the Tithonian, is now considered as defining the start of the Berriasian.</p>
- In short
-
Last stage of the Jurassic.
- Age
- Tithonian
-
Kimmeridgian (157.3 +/-1.0 Ma)
- Name Origin
-
Named after the town of Kimmeridge on the Dorset coast (UK). The Kimmeridge Clay Formation is the main oil source rock in the North Sea petroleum province.
- Rank
- chronostratigraphic Stage
- Status
- valid formal name
- Age
- Kimmeridgian
-
Oxfordian (163.5 +/-1.0 Ma)
- Name Origin
-
Named after the city of Oxford (UK).
- Rank
- chronostratigraphic Stage
- Status
- valid formal name
- In short
-
First stage of the Late Jurassic.
- Age
- Oxfordian