The links between large igneous provinces, continental break
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TitleThe links between large igneous provinces, continental break-up and environmental change: Evidence reviewed from AntarcticaAbstractEarth history is punctuated by events during which large volumes of predominantly mafic magmas were generated and emplaced by processes that are generally accepted as being, unrelated to ʼnormal Ìsea-floor spreading and subduction processes. These events form large igneous provinces (LIPs) which are best preserved in the Mesozoic and Cenozoic where they occur as continental and ocean basin flood basalts, giant radiating dyke swarms, volcanic rifted margins, oceanic plateaus, submarine ridges, and seamount chains. The Mesozoic history of Antarctica is no exception in that a number of different igneous provinces were emplaced during the initial break-up and continued disintegration of Gondwana, leading to the isolation of Antarctica in a polar position. The link between the emplacement of the igneous rocks and continental break-up processes remains controversial. The environmental impact of large igneous province formation on the Earth System is equally debated. Large igneous province eruptions are coeval with, and may drive environmental and climatic effects including global warming, oceanic anoxia and/or increased oceanic fertilisation, calcification crises, mass extinction and release of gas hydrates. This review explores the links between the emplacement of large igneous provinces in Antarctica, the isolation of Antarctica from other Gondwana continents, and possibly related environmental and climatic changes during the Mesozoic and Cenozoic. Copyright 2013 The Royal Society of Edinburgh.AcknowledgementsWe are very grateful to the ISAES organisers for supporting and providing the opportunity to present this review. We are also very grateful to our numerous colleagues that we have worked with on this topic over the years and to the reviewers (Stephen Self, Andrew Kerr and Kathryn Goodenough) for their thorough and detailed reviews that have much improved the manuscript.
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1st AuthorStorey, B.AuthorStorey, B.Vaughan, A.Riley, T.Year2013JournalEarth and Environmental Science Transactions of the Royal Society of EdinburghVolume104Number1Pages17-30DOI10.1017/S175569101300011XURLhttps://www.scopus.com/inward/recor.....f8269b81639b2be9eb406f31eKeywordsclimate changecontinental breakupdike swarmemplacementenvironmental changeflood basaltGondwanalarge igneous provincerift zoneseafloor spreadingsubduction zone, Antarctica, rank3Author Keywordsclimate changeEarth SystemGondwana break-upmafic magmasupercontinent
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TypeArticleCitationStorey, B., Vaughan, A. and Riley, T. (2013) The links between large igneous provinces, continental break-up and environmental change: Evidence reviewed from Antarctica. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 104(1): 17-30 doi:10.1017/S175569101300011X IdentifierStorey2013bRelevancerank3
Riley, T., The links between large igneous provinces, continental break, [Storey2013b]. Antarctica NZ, accessed 16/04/2026, https://adam.antarcticanz.govt.nz/nodes/view/63788, 10.1017/S175569101300011X





