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The Global Warming That Took Place At Permian Triassic Boundary

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Introduction
One of the most devastating weather extremes happened 250 million years ago. A massive volcanic eruption (that occurred in an area now known as Siberia) caused increase in carbon dioxide and methane levels resulting in the extreme global warming. Today, the remains of this volcanic activity are called Siberian traps. The origin of Siberian traps is considered to be a mantle plume that burst through Earth’s crust releasing large volumes of basalt lava. Radiometric dating showed this volcanic event took place approximately from 251 to 250 million years ago (Reichow et al., 2009). Siberian traps erupted over several vents releasing around 2.5 million km3 of basalt lava that covered up to 60% of Siberian craton (Fedorenko et al., …show more content…

Floating and swimming species, plankton and nekton, underwent significant extinctions. There was a large land animal and plant death, but it was not as devastating as it was for marine species. Furthermore, the recovery of ecosystem took very long time, for example there were no reefs and no coal beds for millions of years (EDIT+CITE). Seeing the extent to which global warming can affect biodiversity, it is clearly important to find main causes of it.
Lines of evidence First line of evidence is that volcanic activity from Siberian traps lead to increased amount of carbon dioxide. The eruptions of basalt lava were accompanied by large volume of CO2 (Self, Schmidt, & Mather, 2014). Accumulation of CO2 has long lasting effects on global warming due to its long lifetime. Study conducted by Archer (2005) showed that 400 km3 of flood basalt would release 2 gigatonnes (Gt, 1 Gt = 1012 kg) of carbon. Overall, Siberian traps allowed up to 11 000 Gt of carbon to be released (assuming lava volume of 2.5 million km3). The CO2 degassed during the volcanic period equals total 5000 ppm rise in atmospheric CO2 levels. The volcanism lasted around couple of hundreds of thousands of years, meaning the release of CO2 was prolonged. Thus, atmospheric CO2 was most likely doubled in levels during this eruptive period (Berner, 2002). Doubling of CO2 levels in atmosphere is could have increased the global temperature for 1.5 - 4.5 C (Houghton et al., 2001). Furthermore,

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