The modern world gives us such ready access to nachos and ice cream that it’s easy to forget: Humans bodies require a ridiculous and—for most of Earth’s history—improbable amount of energy to stay alive.
Consider a human dropped into primordial soup 3.8 billions years ago, when life first began. They would have nothing to eat. Earth then had no plants, no animals, no oxygen even. Good luck scrounging up 1600 calories a day drinking pond- or sea water. So how did we get sources of concentrated energy (i.e. food) growing on trees and lumbering through grass? How did we end up with a planet that can support billions of energy-hungry, big-brained, warm-blooded, upright-walking humans?
In “The Energy Expansions of Evolution,” an extraordinary new essay in Nature Ecology and Evolution, Olivia Judson sets out a theory of successive energy revolutions that purports to explain how our planet came to have such a diversity of environments that support such a rich array of life, from the cyanobacteria to daisies to humans.
Judson divides the history of the life on Earth into five energetic epochs, a novel schema that you will not find in geology or biology textbooks. In order, the energetic epochs are: geochemical energy, sunlight, oxygen, flesh, and fire. Each epoch represents the unlocking of a new source of energy, coinciding with new organisms able to exploit that source and alter their planet. The previous sources of energy stay around, so environments and life on Earth become ever more diverse. Judson calls it a “step-wise construction of a life-planet system.”
In the epoch of geochemical energy 3.7 billion years ago, the first living organisms “fed” on molecules like hydrogen and methane that formed in reaction between water and rocks. They wrung energy out of chemical bonds. It was not very efficient—the biosphere’s productivity then was an estimated a thousand to a million times less than it is today.
Sunlight, of course, was shining on Earth all along. When microbes that can harness sunlight finally evolve, the productivity and diversity of the biosphere leveled up. One particular type of bacteria, called cyanobacteria, hits upon a way of harnessing the sun’s energy that makes oxygen (O2) as a byproduct, and with profound consequences: The planet gets an ozone (O3) layer that blocks UV radiation, new minerals through oxygen reactions, and an atmosphere full of highly reactive O2.
Which brings us to the epoch of oxygen. Given an opportunity, oxygen will steal electrons from anything it finds. New oxygen-resistant organisms evolve with enzymes to protect them from oxygen. They have advantages too: Because oxygen is so reactive, it makes the metabolism of these organisms much more efficient. In some conditions, organism can get 16 times as much energy out of a glucose molecule in the presence of oxygen that without.
With more energy, you can have motion and so in the epoch of flesh, highly mobile…