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Jurassic




The Jurassic period is a major unit of the Geologic Timescale that extends from about 200 Ma (million years ago) at the end of the Triassic to 146 Ma at the beginning of the Cretaceous . As with other geologic periods, the rock beds that define the start and end of the period are well identified, but the exact dates are uncertain by 5 - 10 million years. The Jurassic constitutes the middle period of the Mesozoic era, also known as the Age of Dinosaur s. The start of the period is marked by the major Triassic-Jurassic Extinction Event .

The Jurassic was named by Alexandre Brogniart for the extensive marine Limestone exposures of the Jura Mountains in the region where Germany , France and Switzerland meet.


DIVISIONS

The Jurassic period of time is usually broken into Early , Middle , and Late subdivisions, also known as ''Lias'', ''Dogger'' and ''Malm''. The corresponding terms for the rocks are Lower, Middle, and Upper Jurassic. The Faunal Stage s from youngest to oldest are:


PALEOGEOGRAPHY

During the early Jurassic, the Supercontinent Pangea broke up into North America , Eurasia and Gondwana . Still, the early Atlantic and Tethyan Oceans were relatively narrow. In the Late Jurassic, the southern continent, Gondwana, started to break up and as the Tethys closed the Neotethys basin appeared. Climates were warm with no evidence of Glaciation . As in the Triassic, apparently there was no land near either pole, and no extensive ice caps existed. The geological record of the Jurassic is well exposed in western Europe , where marine sequences are found along the coasts. A shallow sea ( Epicontinental Sea ) called the Sundance Sea was present in parts of the northern plains of the United States and Canada . Most Jurassic exposures in North America are continental. Important Jurassic exposures are also found in Russia , India , South America , Japan , Australasia , and the United Kingdom .


AQUATIC AND MARINE ANIMALS

During the Jurassic, the "highest" life forms living in the seas were Fish and marine Reptile s. The latter include Ichthyosaur s, Plesiosaur s, and marine Crocodiles of the families Teleosauridae and Metriorhynchidae .

In the Invertebrate world, several new groups appeared, such as:

Ammonite s (shelled Cephalopod s) were particularly common and diverse, forming 62 Biozones .


TERRESTRIAL ANIMALS

On land, large Archosaur ian reptiles remained dominant. Great plant-eating dinosaurs ( Sauropod s) roamed the land, feeding on Prairie s of Fern s and palm-like Cycad s and Bennettitales . They were preyed upon by large Theropod s (Ceratosaurs, Megalosaurs, and Allosaurs). All these belong to the "lizard hipped" or Saurischia n branch of the dinosaurs.

During the Late Jurassic the first Birds Evolved from small Coelurosaur dinosaurs. Ornithischia n dinosaurs were less predominant than saurischian dinosaurs, although some like Stegosaur s and small Ornithopod s played important roles as small and medium-to-large (but not sauropod large) herbivores. In the air, Pterosaur s were common, filling many ecological roles now taken by birds.


PLANTS

The arid conditions that had characterized much of the Triassic steadily eased during the following period, especially at higher latitudes; the warm, humid climate allowed lush jungles to cover much of the landscape (Haines 2000). Flowering Plants had not evolved yet, and Conifers dominated the landscape, as they had during the Triassic, and in fact were the most diverse group of trees, and constituted the greatest majority of large trees. Extant Conifer families that flourished during the Jurassic included the Araucariaceae , Cephalotaxaceae , Pinaceae , Podocarpaceae , Taxaceae , and Taxodiaceae (Behrensmeyer ''et al'', 1992, p.349). The extinct Mesozoic Conifer family Cheirolepidiaceae dominated low latitude vegetation, as did the shrubby Bennettitales (Behrensmeyer ''et al.'', 1992, p.352). Cycad s were also common, as were Ginkgo s and Tree Ferns in the forest; smaller Ferns were probably the dominant undergrowth. Caytoniaceous Seed Ferns were another group of important plants during this time, and are thought to have been shrub to small-tree in size (Behrensmeyer ''et al.'', 1992, p.353). Ginkgo-like plants were particularly common in the mid- to high northern lattitudes. In the Southern Hemisphere, Podocarps were especially successful (Haines 2000), while Ginkgos and Czekanowskiales were rare (Behrensmeyer ''et al.'', 1992, p.352).


POPULAR CULTURE

Though the movie '' Jurassic Park '' brought the word "Jurassic" to household usage, many of the creatures featured in that film would more likely be found in the Cretaceous period.


REFERENCES

  • , Chicago and London, ISBN 0226041549 (cloth), ISBN 0226041557 (paper)

  • Haines, Tim (2000) ''Walking with Dinosaurs: A Natural History'', New York: Dorling Kindersley Publishing, Inc., p. 65. ISBN 0563384492

  • Kazlev, M. Alan (2002) Paleos website Accessed Jan. 8, 2006

  • Ogg, Jim; June, 2004, ''Overview of Global Boundary Stratotype Sections and Points (GSSP's)'' http://www.stratigraphy.org/gssp.htm Accessed April 30, 2006.