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Late Jurassic

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(Redirected from Malm (geology)) Third epoch of the Jurassic Period
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Late/Upper Jurassic
161.5 ± 1.0 – ~145.0 Ma PreꞒ O S D C P T J K Pg N
A map of Earth as it appeared 155 million years ago during the Late Jurassic Epoch, Oxfordian Age
Chronology
−205 —–−200 —–−195 —–−190 —–−185 —–−180 —–−175 —–−170 —–−165 —–−160 —–−155 —–−150 —–−145 —–−140 —MesozoicTJurassicKLate TEarlyMiddleLateEarly KHettangianSinemurianPliensbachianToarcianAalenianBajocianBathonianCallovianOxfordianKimmeridgianTithonian   
Triassic–Jurassic extinction event
Subdivision of the Jurassic according to the ICS, as of 2024.
Vertical axis scale: Millions of years ago
Etymology
Chronostratigraphic nameUpper Jurassic
Geochronological nameLate Jurassic
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitEpoch
Stratigraphic unitSeries
Time span formalityFormal
Lower boundary definitionNot formally defined
Lower boundary definition candidatesHorizon of the Ammonite Cardioceras redcliffense.
Lower boundary GSSP candidate section(s)
Upper boundary definitionNot formally defined
Upper boundary definition candidates
Upper boundary GSSP candidate section(s)None

The Late Jurassic is the third epoch of the Jurassic Period, and it spans the geologic time from 161.5 ± 1.0 to 145.0 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic strata.

In European lithostratigraphy, the name "Malm" indicates rocks of Late Jurassic age. 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.

Subdivisions

The Late Jurassic is divided into three ages, which correspond with the three (faunal) stages of Upper Jurassic rock:

  Tithonian (149.2 ±0.7 – 145.0 ± 0.8 Ma)
  Kimmeridgian (154.8 ±0.8 – 149.2 ±0.7 Ma)
  Oxfordian (161.5 ± 1.0 – 154.8 ±0.8 Ma)

Paleogeography

This section needs expansion. You can help by adding to it. (May 2008)

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 spawning of the Atlantic Ocean. However, at this time, the Atlantic Ocean was relatively narrow.

Life forms of the epoch

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:

References

  1. "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. December 2024. Retrieved January 1, 2025.
  2. Owen 1987.
  3. Gradstein, F.M.; Ogg, J.G.; Schmitz, M.D.; Ogg, G.M., eds. (2012). The Geologic Timescale 2012 (volume 1). Elsevier. p. 744. ISBN 978-0-44-459390-0.
Jurassic Period
Lower/Early JurassicMiddle JurassicUpper/Late Jurassic
Geological history of Earth
Cenozoic Era
(present–66.0 Ma)
Quaternary (present–2.58 Ma)
Neogene (2.58–23.0 Ma)
Paleogene (23.0–66.0 Ma)
Mesozoic Era
(66.0–252 Ma)
Cretaceous (66.0–145 Ma)
Jurassic (145–201 Ma)
Triassic (201–252 Ma)
Paleozoic Era
(252–539 Ma)
Permian (252–299 Ma)
Carboniferous (299–359 Ma)
Devonian (359–419 Ma)
Silurian (419–444 Ma)
Ordovician (444–485 Ma)
Cambrian (485–539 Ma)
Proterozoic Eon
(539 Ma–2.5 Ga)
Neoproterozoic (539 Ma–1 Ga)
Mesoproterozoic (1–1.6 Ga)
Paleoproterozoic (1.6–2.5 Ga)
Archean Eon (2.5–4 Ga)
Hadean Eon (4–4.6 Ga) 
ka = kiloannum (thousand years ago); Ma = megaannum (million years ago); Ga = gigaannum (billion years ago).
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