Article 63P0D Major Volcanic Events Linked to the Slowing of Tectonic Plates

Major Volcanic Events Linked to the Slowing of Tectonic Plates

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Major volcanic events linked to the slowing of tectonic plates:

In the past history of Earth there have been times when magma from the molten mantle has flowed out into, or over, the solid crust of the planet. In the cases where these major volcanic events have led to excessive accumulations of lava, the resulting formations have been termed Large Igneous Provinces (LIPs). Some LIPs have an aerial extent of a few million km2 and involve volumes of igneous rock totaling up to a million km3. Such phenomena clearly had major impacts on the geology, structure and natural environments where they occurred.

[...] In the new study, led by scientists in the School of Natural Sciences at Trinity College Dublin, chemical data was obtained from ancient mudstone deposits in Wales by drilling a borehole down to a depth of 1.5 km. Analysis of the chemical markers enabled the researchers to link two key events that occurred around 183 million years ago, during the Toarcian stage at the end of the Early Jurassic Period.

The team discovered that this time period coincides directly with the occurrence of the major volcanic activity that gave rise to the Karoo and Ferrar LIP's which covered parts of what are today southern Africa and Antarctica with lava. This time was also characterized by increased concentrations of greenhouse gases, by some of the most severe climatic and environmental changes ever, and by the Pliensbachian-Toarcian extinction event that affected the world's fauna and flora.

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