(A shorter version was first published on Blogcritics)
The early evolution of life on Earth is a subject I’ve always found fascinating, but it’s a couple of decades since I last revisited the subject in any depth, and having read Oxygen: A Four Billion Year History by Donald E Canfield I now know that pretty well everything I’ve ever read or been taught on the subject was wrong. The idea that gradually algae spread around the earth, pumping out oxygen in a steady-growing stream, well it simply isn’t true.
It’s not surprising my teachers were so wrong, for as I read in Oxygen, a big breakthrough in understanding early life on Earth came in only 1999, when a colleague and friend of the author, James Farquahar, found some highly unexpected results on a study of sulfur isotopes, in Archaen rocks aged from 2.3-2.4 billion years ago. That led to the conclusion that at this time there’d been interaction between UV light and sulfur dioxide gas from volcanoes. Today, that’s absorbed by ozone, of course from oxygen. Further studies on the form some molybdenum takes in rocks of this age from some parts of the world, however, show that in some places there was free oxygen – what’s come to be known as a “whiff” of oxygen.
What was happening was that by around 2.5 billion years ago, the production of oxygen by photosynthesis more or less balanced the consumption of it by volcanic gases. Sometimes the balance shifted one way, so the oxygen disappeared, sometimes the cyanobacteria were beating the volcanoes.
It was between 2.3 and 2.4 billion years ago that “the great oxidation event” (GOE) changed that. Quite what caused it is still up for grabs. Canfield has a favourite, not evolution of cyanobacteria but a less active mantle, as it gradually cooled, cutting the production of reducing gases. Seems entirely plausible to this interested amateur.
But the GOE wasn’t entirely even – it was Canfield suggests concentrated in the atmosphere, the oceans remaining anoxic and rich in sulfide, with more sulfur being weathered from the land through oxidative weathering of sulfides. This is now known as the “Canfield Ocean” – yes after the author, we’re in seriously expert hands here.
Related to that is the likelihood that for much of the Earth’s “middle ages” atmospheric oxygen levels were much lower than today’s. (Any time machine travellers would need to take oxygen cylinders.) The author’s theory is just 10% of today’s levels, others suggest 40-50%.
read more