The climate change Earth is experiencing today is similar to that during a period of rapid and intense global warming it experienced some 56 million years ago. Understanding the similarities can help scientists evaluate what is happening in today’s warming world, according to Ellen Thomas, Harold T. Stearns Professor of Integrative Sciences, Emerita. Key to that understanding is figuring out how much oxygen was dissolved in large swaths of the oceans during that period of rapid warming, called the Paleocene-Eocene Thermal Maximum or PETM, when average temperatures increased by 5-8o Celsius or 9-14o Fahrenheit in a few thousand years, Thomas…