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The cliff forming Purbeck limestone from the Upper Jurassic at Bat's Head, Dorset, UK.
The cliff forming Purbeck limestone from the Upper Jurassic at Bat's Head, Dorset, UK. Bat's Head is a Chalk headland on the Dorset coast in southern England, located between Durdle Door to the east and White Dorset ( (or archaically, Dorsetshire) is a county in South West England on the English Channel coast The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom, the UK or Britain,is a Sovereign state located

The Late Jurassic (or Malm) Epoch of the Jurassic Period is the unit of geologic time from 161. The Jurassic is a geologic period and system that extends from about Ma (million years ago to  Ma that is from the end of the Triassic to the beginning The geologic time scale is a chronologic schema (or idealized Model) relating Stratigraphy to time that is used by Geologists and other 2 ± 4. 0 to 145. 5 ± 4. 0 million years ago, which is preserved in Upper Jurassic strata. Annum is one form of the Latin noun meaning Year, not a form normally used for derivatives in modern languages the accusative singular In Geology and related fields a stratum (plural strata) is a layer of rock or Soil with internally consistent characteristics that distinguishes [1]

Contents

Subdivisions

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

  Tithonian (150. The Tithonian is the final stage of the Late Jurassic Epoch. It spans the time between 150 8 ± 4. 0 – 145. 5 ± 4. 0 Ma)
  Kimmeridgian (155. The Kimmeridgian is a stage of the Late Jurassic Epoch. It spans the time between 155 7 ± 4. 0 – 150. 8 ± 4. 0 Ma)
  Oxfordian (161. The Oxfordian stage is the first stage of the Late Jurassic Epoch. 2 ± 4. 0 – 155. 7 ± 4. 0 Ma)

Paleogeography

Pangaea broke up into two supercontinents, Laurasia to the north, and Gondwana to the south. Pangaea, Pangæa or Pangea (pænˈdʒiːə from παν pan, meaning entire, and Γαῖα Gaea, meaning Earth in In Geology, a supercontinent is a Landmass comprising more than one Continental core or Craton. Laurasia (lɔˈreɪʃiə lɔˈreɪʒə was a Supercontinent that most recently existed as a part of the split of the Pangaean supercontinent in the late Mesozoic Gondwana (ɡɒnˈdwɑːnə originally Gondwanaland) was a southern Supercontinent that existed about 500 to 200 Ma ago The result of this break-up was the spawning of Atlantic Ocean. However, at this time, the Atlantic Ocean was relatively narrow.


Life

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 Jurrassic. Here are only a few of the many Jurrassic animals:

References

  1. ^ Owen 1987.
Jurassic period
Lower/Early Jurassic Middle Jurassic Upper/Late Jurassic
Hettangian | Sinemurian
Pliensbachian | Toarcian
Aalenian | Bajocian
Bathonian | Callovian
Oxfordian | Kimmeridgian
Tithonian
The Jurassic is a geologic period and system that extends from about Ma (million years ago to  Ma that is from the end of the Triassic to the beginning For general context see Jurassic. The Early Jurassic (in geology referred to as the Lower Jurassic, originally (and still in Europe the The Middle Jurassic, called the Dogger in the European system of classification is the second epoch of the Jurassic Period. The Hettangian is the first stage of the Early Jurassic Epoch. The Sinemurian is a stage of the Early Jurassic Epoch. It spans the time between 196 The Pliensbachian (also known as Charmouthian) is a stage of the Early Jurassic Epoch. The Toarcian Stage was the last Faunal stage of the Early Jurassic period The Aalenian (ɑːˈliːniən is a subdivision of the Middle Jurassic epoch of the Geologic timescale that extends from about 175 In the Geologic timescale, the Bajocian is an age of the Middle Jurassic epoch of the Jurassic period of the Mesozoic In the Geologic timescale the Bathonian epoch is a stage during the Middle Jurassic, of the Mesozoic era of the Phanerozoic The Callovian is a stage on the Geologic time scale occurring 164 The Oxfordian stage is the first stage of the Late Jurassic Epoch. The Kimmeridgian is a stage of the Late Jurassic Epoch. It spans the time between 155 The Tithonian is the final stage of the Late Jurassic Epoch. It spans the time between 150
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