Science

Fossils of nearly 300 fish in limestone suggest they've been swimming in schools for 50M years


Frozen in time: Fossils of nearly 300 fish preserved in limestone suggest they’ve been swimming in schools for at least 50 million years

  • Researchers discovered fossil fish in huge group at the Green River Formation 
  • Most of the fish are facing the same direction and positioned close together
  • Simulations of the fish and water flow suggest they were swimming in formation 

A slab of limestone shale containing the impressions of nearly 300 fish has captured what’s thought to be a school that swam in unison 50 million years ago.

While many animals, from birds and fish to insects, are known to travel in formations, just when this behavior arose in the evolutionary timeline isn’t yet certain.

The fossil discovery from the Green River Formation that stretches across Colorado, Wyoming, and Utah may finally offer a glimmer of insight, suggesting it dates at least as far back as the Eocene Epoch.

Close examination of the slab revealed a staggering 259 fossilized fish, all identified as the tiny extinct species, Erismatopterus levatus. It’s unclear how exactly they died

Close examination of the slab revealed a staggering 259 fossilized fish, all identified as the tiny extinct species, Erismatopterus levatus. It’s unclear how exactly they died

Researchers from Arizona State University and the Oishi Fossils Gallery of Mizuta Memorial Museum in Japan detail the findings in a new paper published in Proceedings of the Royal Society B.

Close examination of the slab revealed a staggering 259 fossilized fish, all identified as the tiny extinct species, Erismatopterus levatus.

It’s unclear how exactly they died, but the researchers say the evidence suggests they were all in the same place at the time of the event.

And, their demise took place ‘near instantaneously.’

‘Considering that dead bodies in an assemblage of carcasses would be positioned all over the slab, the observed localized aggregation is likely to be the result of behaviour rather than an artefact of fossilization,’ the researchers note in the paper.

‘Also, the sediment is fine-grained mud, which is one criterion for an in situ rather than transported assemblage.’

The fossil discovery from the Green River Formation that stretches across Colorado, Wyoming, and Utah may finally offer a glimmer of insight to schooling behavior, suggesting it dates at least as far back as the Eocene Epoch

The fossil discovery from the Green River Formation that stretches across Colorado, Wyoming, and Utah may finally offer a glimmer of insight to schooling behavior, suggesting it dates at least as far back as the Eocene Epoch

To better understand what might have happened, the researchers simulated 1,000 possible scenarios incorporating the measurements of the fish as well as different types of water flow and spatial distribution.

And, these simulations suggest they were swimming in unison much like fish are known to do today.

Sticking together in a group (or shoaling) could have helped the small fish stay safe from predators, the researchers note.

‘Because we found evidence of approach from a distance in our fossilized group of E. levatus we can reasonably infer predator avoidance as a selective pressure leading to shoaling behaviour,’ the researchers write.

‘Consistent with this, the density within the group was higher in the safer central area, while it was lower at the edge of the group, where predators often attack.’

A slab of limestone shale containing the impressions of nearly 300 fish has captured what’s thought to be a school that swam in unison 50 million years ago. While many animals are known to travel in formations, just when this behavior arose isn’t yet certain

A slab of limestone shale containing the impressions of nearly 300 fish has captured what’s thought to be a school that swam in unison 50 million years ago. While many animals are known to travel in formations, just when this behavior arose isn’t yet certain

WHEN WERE EARTH’S ‘BIG FIVE’ EXTINCTION EVENTS?

Traditionally, scientists have referred to the ‘Big Five’ mass extinctions, including perhaps the most famous mass extinction triggered by a meteorite impact that brought about the end of the dinosaurs 66 million years ago. 

But the other major mass extinctions were caused by phenomena originating entirely on Earth, and while they are less well known, we may learn something from exploring them that could shed light on our current environmental crises.

  1. The Late Ordovician: This ancient crisis around 445m years ago saw two major waves of extinction, both caused by climate change associated with the advance and retreat of ice sheets in the southern hemisphere. This makes it the only major extinction to be linked to global cooling. 
  2. The Late Devonian: This period is now regarded as a number of ‘pulses’ of extinction spread over 20m years, beginning 380m years ago. This extinction has been linked to major climate change, possibly caused by an eruption of the volcanic Viluy Traps area in modern-day Siberia. A major eruption might have caused rapid fluctations in sea levels and reduced oxygen levels in the oceans.
  3. The Middle Permian:  Scientists have recently discovered another event 262m years ago that rivals the ‘Big Five’ in size. This event coincided with the Emeishan eruption in what’s now China, and is known to have caused simultaneous extinctions in the tropics and higher latitudes.
  4. The Late Permian: The Late Permian mass extinction around 252m years ago dwarfs all the other events, with about 96% of species becoming extinct. The extinction was triggered by a vast eruption of the Siberian Traps, a gigantic and prolonged volcanic event that covered much of modern day Siberia, which led to a cascade of environmental effects.
  5. The Late Triassic: The Late Triassic event, 201m years ago, shares a number of similarities with the Late Permian event. It was caused by another large-scale eruption, this time of the Central Atlantic Magmatic Province, which heralded the splitting of the supercontinent Pangaea and the initial opening of what would later become the Atlantic Ocean.





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