The 'clock' that starts ticking when life ends |
When something dies, a telltale radioactive signal ticks like a natural clock. Discovering it helped us solve all sorts of natural mysteries.
There would be heaps of the stuff in sewage. Willard Libby was sure of it.
It was the mid-1940s, and the US chemist's goal was to find a radioactive form of carbon, carbon-14, in nature. He had realised that, if it were there, it would leave a slowly decaying trace in dead plants and animals – so finding out how much was left in their remains would reveal when they died.
But Libby had to prove that carbon-14 existed in the wild in concentrations that matched his estimates. Other scientists had only ever detected carbon-14 after synthesising it in a lab.
Libby reasoned that living things would deposit it in their excrement, which is why he turned to sewage. Sewage produced by the people of Baltimore, to be precise. And he found what he was looking for.
Libby didn't know it then but the idea that you could use radioactive carbon – radiocarbon – to date things would have all kinds of applications.
Since the mid-20th Century, radiocarbon dating has confirmed the age of countless ancient artefacts, helped solve missing person cases and put ivory traffickers in jail. It has even enabled scientists to understand the intricacies of Earth's climate. Radiocarbon dating is one of the keys that unlocks our world.
But how does carbon-14 come into existence in the first place? Libby understood that it was being produced constantly by cosmic rays striking nitrogen atoms in the Earth's atmosphere and changing their structure. The resulting carbon-14 atom quickly combines with oxygen to make radioactive carbon dioxide (CO2).
Back on the ground, plants absorb some of that radioactive CO2 in the air as they grow, as do the animals – including humans – that eat them. While a plant or animal is alive, it keeps replenishing its internal store of carbon-14, but when it dies, that process stops. Because radiocarbon decays at a known rate, measuring how much is left in organic material will tell you the material's age. A clock that starts ticking the moment something dies.
Once Libby confirmed there was carbon-14 in the methane gas from Baltimore sewers, he went on to detect radiocarbon in many different things, allowing him to prove how old they were – from the linen wrappings of the Dead Sea Scrolls to a piece of a ship found in the tomb of Sesostris III, an Egyptian king who lived nearly 4,000 years ago.
"This is a problem where you won't tell anybody what you're doing. It's too crazy," Libby later said. "You can't tell anybody cosmic rays can write down human history. You can't tell them that. No way. So we kept it secret."
But once he had proved it worked, he let the world know. And, in 1960, Libby won the Nobel Prize in Chemistry.
His technique works on organic material up to 50,000 years old. Older than that, and there is too little carbon-14 left. Carbon-14's gradual decay is what makes radiocarbon dating possible – but that also means you can only go back so far. Even so, radiocarbon dating is now central to our understanding of history.
"In terms of putting things in order, in terms of being able to compare between different regions in particular, and understand that pace of change, it has been really important," explains Rachel Wood, who works in one of the world's most distinguished radiocarbon dating labs, the Oxford Radiocarbon Accelerator Unit.
She and her colleagues date materials including human bones, charcoal, shells, seeds, hair, cotton, parchment and ceramics, but also stranger........