WONDERING what the world will look like when the heat is on?
A newly discovered micro-fossil of an organism that lived during a previous global warming is helping researchers understand how aquatic life could adapt to the warmer, lower oxygen, waters that may accompany radical environmental transformations.
Dubbed the “Magnetic Death Star”, due to its round and spiky magnetite structure, the fossil was found among sediment deposited 55 million years ago during the Paleocene-Eocene Thermal Maximum (PETM), when surging atmospheric carbon drove temperatures 9 degrees Fahrenheit higher. CalTech and McGill University workers believe the single-celled eukaryote evolved during the PETM, only to be out-competed and disappear again when conditions cooled off (Proceedings of the National Academy of Science, DOI:10.1073 / pnas.0803634105).

Since the mid 1980s, I've worked in university and industrial research, as a manager and editor in technology and environment for an international industry association, and held senior business development, strategy, and procurement posts in industry. I hold a PhD in chemical engineering from Birmingham University, an MBA from Warwick University Business School, and an MSc in Science Communication from Imperial College. In 2008, I left industry to focus full-time on my passion for science and technology, and to share that enthusiasm with others as a freelance science communicator. I live in London with my wife Erin.
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