SHENZHEN, May 30, 2026 — infopulsetoday.com —The question of how life on Earth got started has long frustrated scientists.
They know the raw ingredients were present: water, carbon compounds, energy from volcanoes and lightning. But something was missing — a bridge between simple chemistry and the complex molecules that living things need. Professor Yongdong Jin of Shenzhen University thinks he has found that bridge.
His Nanozyme Hypothesis, announced May 30, points to mineral nanoparticles as the missing link. Tiny bits of metal, metal oxides, and sulfides — produced naturally by the heat and pressure around volcanoes, hydrothermal vents, and hot springs — could have acted as primitive catalysts.
They behaved like enzymes, speeding up chemical reactions that otherwise would have taken far too long.
This is not a small idea. Origin-of-life research has been stuck for decades.
Competing models — the primordial soup, the RNA world, metabolism-first theories — all have strengths and all have gaps. What none of them could explain is how the first organic molecules formed in sufficient quantity and complexity to lead to life. Jin’s hypothesis offers an answer.
Nanozymes could have concentrated molecules, kept fragile compounds safe from ultraviolet radiation, and turned environmental energy into useful chemical forms.
They did not just speed things up — they created conditions where life could emerge. The theory is simple at its core.
Anyone who has seen rust forming knows that minerals interact with their surroundings.
Jin’s insight was to ask what those interactions might have looked like on the early Earth, before life existed. The answer: mineral nanoparticles with enzyme-like properties, scattered across the planet’s surface, working as tiny chemical factories.
If experiments back this up, the implications go far beyond Earth.
The same conditions that produced these nanoparticles here — volcanoes, hot springs, hydrothermal vents — exist on other worlds. Mars shows evidence of all three. The icy moons of Jupiter and Saturn have subsurface oceans and hydrothermal activity.
The Nanozyme Hypothesis gives scientists something concrete to look for in those places. The hypothesis also offers a way to test competing origin-of-life models.
If mineral nanoparticles can bridge the gap between them, it may resolve debates that have divided the field for decades.
Researchers can now design experiments to see whether these nanozymes actually work the way Jin predicts. This is early-stage science.
The hypothesis needs experimental support before it becomes accepted theory. But it has one thing that many origin-of-life proposals lack: a clear mechanism that can be tested in a laboratory. You can take mineral nanoparticles, put them in conditions that mimic the early Earth, and watch what happens.
Professor Jin has not claimed to have solved the mystery of life’s origins.
He has proposed a mechanism that fits the available evidence and makes testable predictions. That is how science moves forward — not with grand pronouncements, but with ideas that can be checked against reality.
The search for life’s origins has been going on for more than a century.
Each new hypothesis narrows the possibilities. The Nanozyme Hypothesis may turn out to be wrong.
But it gives researchers a new direction to explore, and that alone makes it significant.
