
How Oxygen May Have Sparked the Rise of Complex Life
Scientists dissolved 1.7-billion-year-old Australian mudstone cores and found more than 12,000 microscopic fossils, revealing a striking link between oxygen and the dawn of complex life.
How did complex life get started? That question covers the distant ancestors of everything from mushrooms to whales to us, and it is one of biology's biggest open puzzles. A new fossil discovery from northern Australia has now handed scientists a striking clue: oxygen.
In a study published in Nature, researchers Maxwell Lechte and Leigh Anne Riedman describe finding more than 12,000 microscopic fossils preserved in mudstone cores drilled decades ago in the Northern Territory. The oldest of these fossils date back 1.75 billion years. That makes them the oldest eukaryote fossils currently known anywhere on the planet.
A eukaryote is any organism made of complex cells, with a nucleus and specialised internal parts. Animals, plants, fungi and algae are all built from this kind of cell, which is quite different from the simpler cells of bacteria and archaea. The shift from simple to complex cells was, as the researchers put it, a "major evolutionary leap". It paved the way for animals and, in time, for us.
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