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Middle Jurassic

Second part of the Jurassic geological period, from 174 to 161 million years ago

Middle Jurassic

Summary

Second part of the Jurassic geological period, from 174 to 161 million years ago

FieldValue
nameMiddle Jurassic
colorMiddle Jurassic
time_start174.7
time_start_uncertainty0.8
time_end161.5
time_end_uncertainty1.0
image_mapMollweide Paleographic Map of Earth, 170 Ma (Bajocian Age).png
caption_mapA map of the world 170 million years ago during the Middle Jurassic Epoch, Bajocian Age
timelineJurassic
name_formalityFormal
celestial_bodyearth
usageGlobal (ICS)
timescales_usedICS Time Scale
chrono_unitEpoch
strat_unitSeries
timespan_formalityFormal
lower_boundary_defFAD of the Ammonites Leioceras opalinum and Leioceras lineatum
lower_gssp_locationFuentelsaz, Spain
lower_gssp_coords
lower_gssp_accept_date2000
upper_boundary_defNot formally defined
upper_def_candidatesHorizon of Ammonite Cardioceras redcliffense.
  • Redcliff Point, Dorset, UK
  • Savouron, Provence, France
Middle Jurassic strata of the San Rafael Group, Colorado Plateau.

The Middle Jurassic is the second epoch of the Jurassic Period. It lasted from about 174.1 to 161.5 million years ago. Fossils of land-dwelling animals, such as dinosaurs, from the Middle Jurassic are relatively rare, but geological formations containing land animal fossils include the Forest Marble Formation in England, the Kilmaluag Formation in Scotland, the Calcaire de Caen of France, the Daohugou Beds in China, the Itat Formation in Russia, the Tiourarén Formationof Niger, and the Isalo III Formation of western Madagascar. Rocks of the Middle Jurassic were formerly (until about 1980s) in Europe called Dogger or Brown Jurassic.

Paleogeography

During the Middle Jurassic Epoch, Pangaea began to separate into Laurasia and Gondwana, and the Atlantic Ocean formed. Eastern Laurasia was tectonically active as the Cimmerian plate continued to collide with Laurasia's southern coast, completely closing the Paleo-Tethys Ocean. A subduction zone on the coast of western North America continued to create the Ancestral Rocky Mountains. Significant subduction zones were active along practically all of the continental edges surrounding Pangea, as well as in southern Tibet, southeastern Europe, and other locations, to allow the formation of fresh seabed in the proto-Atlantic Ocean. Plate tectonic activity in subduction zones caused the construction of north-south mountain ranges such as the Rocky Mountains and the Andes all along the west coast of North, Central, and South America.

Fauna

The Middle Jurassic is one of the key periods in the history of life on Earth. Many groups, including dinosaurs and mammals, diversified during this time.

Marine life

During this time, marine life (including ammonites and bivalves) flourished. Ichthyosaurs, although common, are reduced in diversity; the top marine predators, the pliosaurs, grew to the size of killer whales and larger (e.g. Pliosaurus, Liopleurodon). Plesiosaurs became common at this time, and metriorhynchids first appeared. In the Jurassic seas, a wide range of animals swam. Cartilaginous and bony fish were plentiful. Large fish and marine reptiles were plentiful.

Terrestrial life

Many of the major groups of dinosaurs emerged during the Middle Jurassic, (including cetiosaurs, brachiosaurs, megalosaurs and primitive ornithopods).

Descendants of the therapsids, the cynodonts, were still flourishing along with the dinosaurs. These included the tritylodonts and mammals. Mammals remained quite small, but were diverse and numerous in faunas from around the world. Tritylodonts were larger, and also had an almost global distribution.

Flora

Conifers were dominant in the Middle Jurassic. Other plants, such as ginkgoes, cycads, and ferns were also common.

References

References

  1. (September 2001). "The Global Boundary Stratotype Section and Point (GSSP) of the Toarcian-Aalenian Boundary (Lower-Middle Jurassic)". Episodes.
  2. Clark, James. (June 2009). "Evolutionary Transitions Among Dinosaurs: Examples from the Jurassic of China". Evolution: Education and Outreach.
  3. British Geological Survey. 2011. [https://www.researchgate.net/publication/265611781_Stratigraphical_framework_for_the_Middle_Jurassic_strata_of_Great_Britain_and_the_adjoining_continental_shelf Stratigraphic framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf: research report RR/11/06]. British Geological Survey, Keyworth, Nottingham.
  4. (24 August 2010). "Discovery of megalosaur (Dinosauria, Theropoda) in the middle Bathonian of Normandy (France) and its implications for the phylogeny of basal Tetanurae". [[Journal of Vertebrate Paleontology]].
  5. (15 January 2009). "Considerations on the age of the Tiouaren Formation (Iullemmeden Basin, Niger, Africa): Implications for Gondwanan Mesozoic terrestrial vertebrate faunas". [[Palaeogeography, Palaeoclimatology, Palaeoecology]].
  6. "How the closure of paleo-Tethys and Tethys oceans controlled the early breakup of Pangaea".
  7. Benson RBJ, Campione NE, Carrano MT, Mannion PD, Sullivan C, Upchurch P, and Evans DC. 2014. [http://journals.plos.org/plosbiology/article?id=10.1371/journal.pbio.1001853 Rates of dinosaur body mass evolution indicate 170 million years of sustained ecological innovation on the avian stem lineage]. PLoS Biology 12, no. 5: e1001853.
  8. (2015). "Evidence for a mid-Jurassic adaptive radiation in mammals". Current Biology.
  9. Kielan-Jaworowska, Z., Cifelli, R.L., and Luo, Z.-X. 2004. Mammals from the age of dinosaurs: origins evolution and structure. 630 pp. Columbia University Press, New York.
  10. Panciroli, E. 2017. [https://www.palaeontologyonline.com/articles/2017/fossil-focus-first-mammals/ The First Mammals] {{Webarchive. link. (2020-08-03 Palaeontology Online.)
  11. Kemp, T 2005. [https://www.amazon.co.uk/Origin-Evolution-Mammals-Oxford-Biology/dp/0198507615 The Origin and Evolution of Mammals]. Oxford University Press.
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