Scientists discover 407-million-year-old fungus in Scottish fossil, revealing ancient plant symbiosis

Symbiosis appears to have been essential to plants' survival on land.
A 407-million-year-old fossil reveals that early plants relied on fungal partners from the moment they left the ocean.
Mark

So we're looking at a fungus that lived inside a plant root 407 million years ago. How do we even know it was there?

Mimi

The fossil was preserved in Scottish rock in such fine detail that you can see the fungal structures under a microscope. The researchers used advanced imaging—confocal microscopy, fluorescence lifetime imaging, Raman spectroscopy—to distinguish the fungal tissue from the plant tissue based on their unique light signatures.

Luke

But the original biological material is carbonized. There's no DNA left. How confident are we that what they're seeing is actually fungal tissue and not just a different mineral composition that happens to look fungal?

Mimi

That's exactly why they used multiple imaging techniques together. Each one reads a different property of the material—how it fluoresces, how it scatters light, its chemical composition. When all three techniques point to the same conclusion, the confidence is high.

Mark

And this matters because?

Mimi

Because it shows that plants didn't colonize land alone. They brought fungal partners with them. This particular plant, Aglaophyton majus, was already in a symbiotic relationship with at least two different fungal species over 400 million years ago.

Luke

Is this the oldest known mycorrhizal relationship, or just the oldest one we've found in this particular fossil formation?

Mimi

It's one of the earliest known plant-fungus partnerships. The Windyfield Chert had never yielded a mycorrhiza before, so this is new for that site. But there are other ancient mycorrhizae known from elsewhere.

Mark

What does the fungus actually do for the plant?

Mimi

It extends into the soil and absorbs water and minerals like phosphorus, which it passes to the plant. The plant gives the fungus sugars in return. It's a trade.

Luke

And we know it was a trade and not parasitism because?

Mimi

Because of the arbuscule—the branching structure where the exchange happens. If the fungus were just feeding on a dead plant, you wouldn't see that structure. Its presence indicates a living, active partnership.

Mark

So what comes next for the researchers?

Mimi

They're planning to apply these same imaging techniques to other fossils from the same rock formations to understand how these symbioses evolved and spread. The real breakthrough is the technique itself—it could transform how paleontologists study ancient life across different organisms.

Luke

The technique is new to fossils, but the underlying science isn't. How much of this is genuinely novel versus applying existing lab methods to a new material?

Mimi

The novelty is in the combination and application. Using fluorescence lifetime imaging and Raman spectroscopy together on fossilized plant material to chemically identify ancient microscopic life—that's the breakthrough. It's not a new microscope; it's a new way of reading what's already there.

  • A 407-million-year-old Scottish fossil has yielded a never-before-seen fungal species, upending the assumption that early land plants were pioneering solo.
  • The challenge was acute: no DNA survives in material this ancient, leaving scientists without their most reliable tool for identifying fossilized organisms.
  • Researchers from four institutions combined confocal microscopy, fluorescence lifetime imaging, and Raman spectroscopy to read the unique light signatures fossilized tissue still emits — a workaround that bypasses the need for genetic material entirely.
  • The presence of the arbuscule — the branching nutrient-exchange structure — confirmed this was a living symbiosis, not a parasite exploiting a dead host.
  • The find is only the second fungal species known to have shared this particular plant, suggesting early ecosystems were already complex enough for plants to be selective about their partners.
  • Scientists now plan to apply these optical fingerprinting techniques across multiple ancient fossil sites, potentially transforming how paleontology reconstructs the earliest chapters of life on land.

Four hundred million years ago, before forests existed, a plant and a fungus struck a bargain in Scottish soil — and the terms of that agreement have now been read for the first time. Researchers examining a fossil from the Windyfield Chert have identified a previously unknown fungal species living inside an early land plant, offering rare evidence that life's conquest of the continents was a collaborative venture from the very beginning. The discovery reminds us that even the most foundational transitions in Earth's history were not made alone, and that partnership, not solitude, may be the deeper grammar of survival.

A fossil drawn from 407-million-year-old Scottish rock has preserved something extraordinarily rare: a functioning partnership between a plant and a fungus, intact enough to study in three dimensions. Researchers from the Natural History Museum, Cambridge's Sainsbury Laboratory, and partner institutions identified the fungus as a new species, naming it Rugososporomyces lavoisierae. It had been living inside the roots of Aglaophyton majus, an early land plant, in a mycorrhizal arrangement — the fungus mining soil for water and phosphorus, the plant repaying it in sugars produced through photosynthesis.

The fossil, sourced from the Windyfield Chert formation in Scotland, is the most detailed evidence yet that early land plants were already managing complex relationships with multiple fungal species. It is only the second fungal species known to have lived symbiotically with this plant, hinting that even ancient ecosystems had room for selectivity. The discovery reinforces a growing scientific conviction: plants did not colonize land alone. When vegetation first moved from water onto continents, it brought fungal partners with it — a dependency that resembles what we observe today in liverworts and hornworts, which still rely on fungi to access soil nutrients.

What made the identification possible was a methodological breakthrough. Because no DNA survives in material this old, the team turned to the unique light signatures that fossilized tissue continues to emit — optical fingerprints readable through confocal microscopy, fluorescence lifetime imaging, and Raman spectroscopy. These signatures allowed researchers to distinguish fungal tissue from surrounding plant material with a precision conventional microscopy cannot achieve. The presence of the arbuscule, the branching structure where nutrients are exchanged, confirmed this was a living partnership rather than a parasitic intrusion.

The implications extend well beyond this single fossil. Researchers plan to apply these imaging techniques to other specimens from the Windyfield and nearby Rhynie cherts, tracing how early symbioses evolved. The ability to identify ancient organisms by their chemical light signatures — without relying on shape or genetic material — could fundamentally reshape paleontology's capacity to reconstruct life's earliest and most consequential transitions.

A fossil pulled from Scottish rock layers 407 million years old has revealed something that rarely survives the deep past: a working partnership between a plant and a fungus, preserved in three dimensions and visible under a microscope. Researchers from the Natural History Museum and Cambridge University's Sainsbury Laboratory identified the fungus as a previously unknown species, which they named Rugososporomyces lavoisierae. It was living inside the roots of Aglaophyton majus, an early land plant, in what scientists call a mycorrhizal relationship—a mutual arrangement where the fungus extends into soil to gather water and minerals like phosphorus, which it trades to the plant in exchange for sugars the plant manufactures through photosynthesis.

This discovery matters because it shows that plants did not colonize land alone. When vegetation first moved from water onto continents, it brought fungal partners with it. The fossil, sourced from the Windyfield Chert formation in Scotland and now held at the National Museum of Scotland in Edinburgh, is the most detailed evidence yet that early land plants were already engaging in complex relationships with multiple fungal species. It is only the second fungal species known to have lived symbiotically with this particular plant, suggesting that even in those ancient ecosystems, plants were selective about their fungal companions.

What makes this finding possible is a shift in how paleontologists can read fossils. Researchers from the Natural History Museum, Cambridge's Sainsbury Laboratory, the Muséum d'Histoire Naturelle in Paris, and the Cambridge Graphene Center combined several advanced imaging techniques—confocal microscopy, fluorescence lifetime imaging microscopy, and Raman spectroscopy—to distinguish the fossilized fungal tissue from the plant tissue around it. They did this by analyzing the unique light signatures each material emits, a kind of optical fingerprint that persists even after the original biological material has turned to carbon and all DNA has vanished. Dr. Christine Strullu-Derrien, the Natural History Museum's scientific associate who co-led the study, noted that mycorrhizae are exceptionally rare in the fossil record and had never been found in the Windyfield Chert before. The presence of the arbuscule—the branching structure where the fungus and plant exchange nutrients—proved this was a living partnership, not a parasite feeding on a dead plant.

Dr. Paul Kenrick, a fossil plant expert at the museum and co-author of the study, emphasized that this symbiosis appears to have been essential to plants' survival on land. The relationship resembles what scientists observe today in liverworts and hornworts, plants that lack true roots and depend on fungal partners to access soil nutrients. The fossil evidence suggests that this dependency was not a later development but part of the original toolkit plants needed to leave the ocean.

The broader significance lies in the imaging techniques themselves. Dr. Raymond Wightman, who managed the fluorescence lifetime imaging work at the Sainsbury Laboratory, described the combined approach as opening a new window onto life's earliest chapters. By reading the light signatures of fossilized material, scientists can now distinguish between structures that look similar under conventional microscopy but differ in their fine chemical composition—a capability that could reshape how paleontologists study ancient arthropods, plants, and fungi across multiple fossil sites. Professor Schornack, who co-led the study, called this just the beginning. Researchers plan to apply these methods to other fossils from the Windyfield and nearby Rhynie cherts to trace how early symbioses evolved and how plants and fungi first learned to coexist. The technique adds a new dimension to paleontology: instead of relying on shape and structure alone, scientists can now use the optical fingerprints preserved in ancient material to identify organisms with a precision that was impossible before.

Mycorrhizas are very rare in the fossil record and have never been found in the Windyfield Chert before. The presence of the arbuscule shows that the fungus wasn't parasitizing on the plant or feeding on it after death—instead, there was a symbiotic association.
— Dr. Christine Strullu-Derrien, Natural History Museum
It's extraordinary to find such ancient evidence of a symbiotic relationship. It appears that symbioses were a necessary part of allowing plants to adapt to life on land.
— Dr. Paul Kenrick, Natural History Museum
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