nature & planetWikipedia66–56 million years ago
The Paleocene was a greenhouse world that began with an asteroid's destruction of the dinosaurs
The Paleocene is a geological epoch that lasted from about 66 to 56 million years ago and is the first epoch of the Paleogene period. It began after the K-Pg extinction, triggered by the Chicxulub asteroid impact and possibly volcanism, which wiped out about 75 percent of species, including the non-avian dinosaurs. Global average temperatures were around 24 to 25 degrees Celsius, far warmer than today, and the planet had no permanent polar ice sheets. Mammals diversified during this time, with the earliest placental and marsupial mammals appearing, while the forests were dense and populated mostly by small creatures. The epoch ended with the Paleocene-Eocene Thermal Maximum, a sharp warming event driven by the release of thousands of gigatons of carbon.
The Paleocene shows how a single catastrophe can reset the course of life on Earth, opening space for mammals to diversify. The warming event that closed the epoch also offers a deep-time comparison for today's climate change.
The Paleocene's name comes from Ancient Greek words meaning old and new, reflecting that it was the old part of the Eocene.
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Image: Wikimedia Commons
