Lessons from Earth’s deep past: climate change and ocean acidification 200 million years ago

Understanding ongoing climate change is a major scientific challenge. Climate events in the deep history of Earth can inform us about the possible extremes of greenhouse conditions, rates and magnitude of long-term climate change, and their consequences to the ocean and the biosphere. The end of the Triassic period was a time of greenhouse warming, driven by volcanic emission of CO2 and other gases from eruptions in the Central Atlantic Magmatic Province. The end-Triassic mass extinction is the biotic response to rapid environmental changes triggered by volcanism. Ocean acidification was likely a major factor driving the selective extinction of calcifying marine organisms.

Pálfy J., Kocsis T. A., Kovács Z. & Karancz S., 2019. Lessons from Earth’s deep past: climate change and ocean acidification 200 million years ago. In: Palocz-Andresen M., Szalay D., Gosztom A., Sípos L. & Taligás T. (Eds.), International Climate Protection, pp 13-19. Springer, Cham. Chapter (subscription required).

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