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Gradual warming prior to the end-Permian mass extinction

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Gradual warming prior to the end-Permian mass extinction

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Summary: A study using oxygen isotope ratios from late Permian ostracods in north-western Iran found that the ambient seawater temperature began to rise at least 300 kyr prior to the main extinction event. It is suggested that the gradual warming of approximately 12 degrees C was responsible for the initial environmental degradation that eventually led to the global end-Permian mass extinction.

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