Conodont fossils contain data on the Kasimovian–Gzhelian Thermal Maximum, a global temperature rise of about 7.5 °C some 304 million years ago. The event was likely triggered by a modest carbon release that crossed a tipping point. In PNAS: https://ow.ly/rcjx50ZzttC
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