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This supercontinent-triggered superplume mechanism for continental break-up is examined in light of the Mesozoic fragmentation of Pangaea\u2013Gondwana. We summarize the evidence for a superplume event that occurred between 227 and 183 Ma ago, during the Late Triassic\u2013Early Jurassic break-up of Pangaea\u2013Gondwana. The evidence reviewed includes flood magmatism, kimberlite emplacement, plate reorganization and tectonism (including ophiolite obduction events), reversal rate frequency of the geomagnetic field, marine anoxia, deposition of carbon-rich sediments, including oil source rocks and coal, the carbon isotope record, major mass extinctions, and global sea levels. This Late Triassic\u2013Early Jurassic superplume event was comparable in scale with those in the late Proterozoic (\n            <jats:italic>c<\/jats:italic>\n            . 800 Ma) and during Cretaceous times (\n            <jats:italic>c<\/jats:italic>\n            . 120\u201380 Ma). Similar to the mid-Cretaceous event, an extended phase of plume magmatism is implicated, with two oceanic and three continental large igneous provinces being emplaced.\n          <\/jats:p>","DOI":"10.1144\/0016-76492005-109","type":"journal-article","created":{"date-parts":[[2007,2,22]],"date-time":"2007-02-22T23:08:18Z","timestamp":1172185698000},"page":"383-392","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":25,"title":["A new supercontinent self-destruct mechanism: evidence from the Late Triassic\u2013Early Jurassic"],"prefix":"10.1144","volume":"164","author":[{"given":"ALAN P.M.","family":"VAUGHAN","sequence":"first","affiliation":[{"name":"1British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK (e-mail: a.vaughan@bas.ac.uk)"}]},{"given":"BRYAN C.","family":"STOREY","sequence":"additional","affiliation":[{"name":"2Gateway Antarctica, University of Canterbury, Private Bag 4800, Christchurch, New Zealand"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,6]]},"reference":[{"key":"e_1_3_2_1_1","doi-asserted-by":"publisher","DOI":"10.1144\/jgs.157.1.55"},{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1038\/297391a0"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.1130\/0091-7613(1994)022<0039:SOS>2.3.CO;2"},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0031-9201(02)00009-2"},{"key":"e_1_3_2_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0009-2541(98)00096-5"},{"key":"e_1_3_2_6_1","doi-asserted-by":"publisher","DOI":"10.1666\/0094-8373(2004)030<0522:OEAMDO>2.0.CO;2"},{"key":"e_1_3_2_7_1","doi-asserted-by":"crossref","unstructured":"Barnes C.R. 2004. 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