The fossil fuels powering our world are actually ancient sunlight

Photosynthesis | Energy and matter in biological systems | High school biology | Khan Academy · 10:02 · Video: Khan Academy · Watch at the source

In short: Every drop of oil and every lump of coal represents a prehistoric solar battery. Millions of years ago, plants captured light to build organic matter that eventually sank into the earth. Today, we are burning that stored history to power our modern civilization at an unprecedented speed.

Photosynthesis is the fundamental biological mechanism that sustains life on Earth by converting light energy into chemical energy. Within cyanobacteria and various green flora, such a mechanism turns minerals, carbon dioxide, plus water into organic compounds rich in energy and oxygen. Two separate stages happen during this conversion: reactions that depend on light and those that do not. This biological transformation produces sugars and released oxygen as primary outputs. The process is specifically categorized into light-dependent and light-independent reactions.

The impact of photosynthesis on our planet is profound. About 2.4 billion years ago, photosynthetic cyanobacteria triggered the Great Oxidation Event. Over a span of 600 million years, they raised atmospheric oxygen to nearly 1 percent of current levels, creating an environment that allowed for the evolution of multicellular life. Without this continuous process, most food webs would collapse, and the atmosphere would eventually lose its oxygen. If this cycle were to stop today, organic matter would quickly vanish from the planet. Only chemosynthetic bacteria could survive in such a world because they use inorganic chemical energy instead of light.

Our modern industrial society relies on a geological 'savings account' created by these ancient processes. Fossil fuels like coal, oil, and natural gas are essentially organic remains from past ages that were deposited in the Earth's crust through sedimentation. Protected from oxidation, these remains slowly converted into fuel over millions of years. We are currently consuming this multi-million-year accumulation in just a few centuries, returning carbon dioxide to the atmosphere at a rate far faster than it was originally removed. These ancient materials now serve as the primary components for manufacturing plastics and other synthetic goods. This rapid extraction means we are depleting a massive surplus of production that took millions of years to accumulate.

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