The Gold Story, part one: a metal from dying stars

The Gold Story

The first entry in The Gold Story, our long history of gold from its arrival in the universe to the sovereign vaults of today. Every factual claim in this series is drawn from published, checkable sources, linked as we go.

Forged in dying stars

Gold cannot be made by ordinary stars. The furnace that fuses hydrogen into helium, and on through carbon and oxygen towards iron, stops there: beyond iron, fusion costs more energy than it releases. The heaviest elements need something far more violent. The leading explanation is the rapid neutron capture process, in which atomic nuclei are bombarded with neutrons so quickly that they swell and decay into heavy elements, including gold and platinum.

In 2017 astronomers watched it happen. Gravitational wave event GW170817 recorded two neutron stars colliding in a galaxy 130 million light years away, and the explosion that followed, kilonova AT 2017gfo, glowed with exactly the light expected from freshly made heavy elements decaying. The merger ejected several hundred Earth-masses of new material, and modelling published in Nature concluded that such mergers are a dominant source of these elements in the universe (Kasen et al. 2017; Pian et al. 2017).

Honesty note, because this series deals in checkable facts: gold itself has never been directly identified in a kilonova spectrum. Only strontium, yttrium and tellurium have individual detections; gold is inferred as part of the same family of elements. And the debate is live: a peer-reviewed analysis by Siegel (2019) argues that rare giant supernovae called collapsars may actually dominate the galaxy’s production. Science holds both candidates on the table. Either way, every ring in our cabinets began in an event that outshone a galaxy.

A late delivery to Earth

When the Earth formed and melted, almost all of its gold should have sunk with the iron into the core, where it remains forever beyond reach. The gold we can actually mine is best explained by what geochemists call the late veneer: a rain of metal-rich meteorites that arrived after the core had already closed, salting the young crust and mantle with precious metals. Tungsten isotope evidence for this was published in Nature in 2011 (see also Kleine 2011). In other words, the gold on your hand did not just come from space. It came from space twice.

Three billion years of concentration

Once delivered, gold had to be gathered into veins rich enough to mine. The principal deposit class, orogenic gold, forms kilometres down where mountain-building squeezes hot fluids along great faults, and it has been forming for more than three billion years (Goldfarb, Groves & Gardoll 2001). Every nugget is the end of a pipeline that runs from colliding stars, through falling meteorites, to the slow grinding of continents.

Why it matters to what we sell

Scarcity is not a marketing line. It is written into physics. In the next entry we will count what humanity has actually managed to gather in six thousand years of trying, and what the world’s surveyors say is left in the ground. The numbers surprise almost everyone.