We all know that the dinosaurs were wiped out by a massive meteor strike, 65 million years ago. We know where it struck: off the Yucatan peninsula, forming the Chixculub crater. What I didn’t know was that the impact was so fierce that the site was burning hot for millions of years afterward.
The collision was intense enough to cause deformation far beneath the surface. Subterranean effects reached 35 km (almost 22 miles) down, and included the melting an immense amount of rock. Exposure to seawater made that rock porous. As hot water seeped into the pores, a hydrothermal system formed. The hot water gushing into an isolated region of the freezing depths could have attracted microorganisms and possibly other life forms that were otherwise struggling to survive.
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Traces of argon found inside a rock are indicative of potassium decay. Since the gas will also escape from molten rock, this provides a measure of when the rock solidified. How much time has passed since that rock melted can be determined from potassium-argon dating, which involves measuring the amount potassium-40 isotope present relative to the argon-40 it decays into. Levels of argon meant the hydrothermal system stayed heated from 66 million years ago, when the asteroid first hit, to 58 million years ago.With 8 million years of heat and nutrients, life had more than enough time to colonize the hydrothermal system in the Chixculub crater. Pickersgill also ran computer simulations of hydrothermal activity in that location. Results suggested that cooling to 90° C (194° F) took between 1.5 and 2.3 million years after the impact at depths of one kilometer. Cooling to below 50° C (122° F) took up to 5 million years, still enough heat for colonies of microbes to thrive. After 6 million years, significantly less hot water was flowing, and by 8 million years, the flow had ceased. These results matched the rock age found by isotope analysis.
The impact had consequences for millions of years — it killed the world and set a pot to simmer for long ages afterwards.











