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The Jurassic Period was a geologic period that lasted from about 201 to 145 million years ago, forming the middle period of the Mesozoic Era. It is famous for its abundance of dinosaurs, including iconic species like Brachiosaurus, Stegosaurus, and Allosaurus. During this time, the supercontinent Pangaea began to break apart, warm climates covered much of the Earth, and the first birds evolved from small theropod dinosaurs. More Less
1795
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During a tour of the region in 1795, German naturalist Alexander von Humboldt recognized carbonate deposits within the Jura Mountains as geologically distinct from the Triassic aged Muschelkalk of southern Germany, but he erroneously concluded that they were older.
Image source: Jurassic
1799
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Following his recognition of the distinctive carbonate deposits of the Jura Mountains, Alexander von Humboldt named them Jura-Kalkstein ('Jura limestone') in 1799, providing an early label for what would later become known as the Jurassic System.
1822
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The term "Lias" had previously been used for strata of equivalent age to the Black Jurassic in England by William Conybeare and William Phillips in 1822.
1829
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In 1829, the French naturalist Alexandre Brongniart published a book entitled Tableau des terrains qui composent l'écorce du globe, ou Essai sur la structure de la partie connue de le Terre [Description of the Terrains that Constitute the Crust of the Earth or Essay on the Structure of the Known Lands of the Earth].
Image source: Alexandre Brongniart
1839
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The German geologist Leopold von Buch in 1839 established the three-fold division of the Jurassic, originally named from oldest to the youngest: the Black Jurassic, Brown Jurassic, and White Jurassic.
1842 - 1852
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The French palaeontologist Alcide d'Orbigny in papers between 1842 and 1852 divided the Jurassic into ten stages based on ammonite and other fossil assemblages in England and France, of which seven are still used, but none has retained its original definition.
1842
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The Sinemurian Stage was first defined and introduced into scientific literature by Alcide d'Orbigny in 1842.
Image source: Sinemurian
1842
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The Toarcian was named by Alcide d'Orbigny in 1842, with the original locality being Vrines quarry around 2 km northwest of Thouars.
Image source: Toarcian
1842
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The stage was named by Alcide d'Orbigny in 1842 in reference to the Kimmeridge Clay.
1843
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The Bathonian is named after the city of Bath, England, introduced by Belgian geologist d'Omalius d'Halloy in 1843, after an incomplete section of oolitic limestones in several quarries in the region.
1844
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The Oxfordian is named after the city of Oxford in England and was named by Alcide d'Orbigny in 1844 in reference to the Oxford Clay.
1852
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The Callovian is derived from the Latinized name of the village of Kellaways in Wiltshire, England, and was named by Alcide d'Orbigny in 1852, originally the base at the contact between the Forest Marble Formation and the Cornbrash Formation.
Image source: Callovian
1856 - 1858
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The German palaeontologist Albert Oppel in his studies between 1856 and 1858 altered d'Orbigny's original scheme and further subdivided the stages into biostratigraphic zones, based primarily on ammonites.
Image source: Albert Oppel
1856 - 1858
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The base of the Jurassic was previously defined as the first appearance of Psiloceras planorbis by Albert Oppel in 1856–58, but this was changed as the appearance was seen as too localised an event for an international boundary.
Image source: Hettangian
1858
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Albert Oppel in 1858 named the Pliensbachian Stage after the hamlet of Pliensbach in the community of Zell unter Aichelberg in the Swabian Alb, near Stuttgart, Germany.
Image source: Pliensbachian
1858
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The German geologist and palaeontologist Friedrich August von Quenstedt in 1858 divided the three series of von Buch in the Swabian Jura into six subdivisions defined by ammonites and other fossils.
Image source: Friedrich August von Quenstedt
1864
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The Hettangian Stage was named by Swiss palaeontologist Eugène Renevier in 1864 after Hettange-Grande in north-eastern France.
1864
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1865
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The Tithonian was introduced in scientific literature by Albert Oppel in 1865.
Image source: Tithonian
1939 - 1946
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Arkell in studies in 1939 and 1946 placed the lower boundary of the Oxfordian as the first appearance of the ammonite Quenstedtoceras mariae (then placed in the genus Vertumniceras).
1962
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Most of the modern stages of the Jurassic were formalized at the Colloque du Jurassique à Luxembourg in 1962.
1997
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The GSSP for the base of the Bajocian is located in the Murtinheira section at Cabo Mondego, Portugal; it was ratified in 1997.
2000
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The GSSP of the Sinemurian is located at a cliff face north of the hamlet of East Quantoxhead, 6 kilometres east of Watchet, Somerset, England, within the Blue Lias, and was ratified in 2000.
2000
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The GSSP for the base of the Aalenian is located at Fuentelsaz in the Iberian range near Guadalajara, Spain, and was ratified in 2000.
2005
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The GSSP for the base of the Pliensbachian is found at the Wine Haven locality in Robin Hood's Bay, Yorkshire, England, in the Redcar Mudstone Formation, and was ratified in 2005.
2009
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The GSSP for the base of the Bathonian is Ravin du Bès, Bas-Auran area, Alpes de Haute Provence, France; it was ratified in 2009.
2010
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The GSSP for the base of the Hettangian is located at the Kuhjoch Pass, Karwendel Mountains, Northern Calcareous Alps, Austria; it was ratified in 2010.
2014
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The GSSP for the base of the Toarcian is located at Peniche, Portugal, and was ratified in 2014.
2021
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The GSSP for the base of the Kimmeridgian is the Flodigarry section at Staffin Bay on the Isle of Skye, Scotland, which was ratified in 2021.
2010
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Over 1500 gigatons of Jurassic coal reserves are found in north-west China, primarily in the Turpan-Hami Basin and the Ordos Basin, making these deposits among the most significant coal resources associated with the Jurassic Period anywhere on Earth.
Image source: Coal in China
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