The image shows a reconstruction of the reptile. Credit: Marcin Ambrozik

New discoveries of fossil clawed footprints from Australia, published in Nature, push the origin of reptiles back in time by at least 35 million years and change the entire timeline for the origin of tetrapods (backboned land animals).

"I'm stunned," says Per Ahlberg of Uppsala University, who coordinated the study. "A single track-bearing slab, which one person can lift, calls into question everything we thought we knew about when modern tetrapods evolved."

The story of the origin of tetrapods began with fishes leaving the water, and ended with the descendants of these first colonists on land diversifying into the ancestors of the modern amphibians and amniotes (the group that includes reptiles, birds and mammals).

The timeline of these events has seemed clear-cut: the first tetrapods evolved during the Devonian period and the earliest members of the modern groups appeared during the following Carboniferous period. The earliest amniote fossils are from the late Carboniferous, about 320 million years old.

3D animation recreation of the reptile trackways 350 million years ago, as well as the age of the rock slabs where this discovery was found. Credit: Flinders University (Monkeystack Productions)

This led researchers to conclude that the beginning of the evolutionary radiation of the modern groups, the point on the where the ancestors of amphibians and amniotes separated (also known as the "tetrapod crown-group node"), lay in the earliest Carboniferous around 355 million years ago. The Devonian period was seen as inhabited by more primitive fish-like tetrapods and transitional "fishapods" such as Tiktaalik.

A sandstone slab from the earliest Carboniferous of Australia, approximately 355 million years old, discovered by two amateur paleontologists who co-authored the study, changes all this. It carries well-preserved footprints of long-toed feet with distinct claw impressions at the tips. These are by far the earliest clawed footprints ever discovered.

The sandstone slab from the earliest Carboniferous of Australia, approximately 355 million years old. Credit: Grzegorz Niedźwiedzk

"When I saw this specimen for the first time, I was very surprised. After just a few seconds, I noticed that there were clearly preserved claw marks," says Grzegorz Niedźwiedzki of Uppsala University, co-author of the study.

"Claws are present in all early amniotes, but almost never in other groups of tetrapods," adds Ahlberg. "The combination of the claw scratches and the shape of the feet suggests that the track maker was a primitive reptile."

If this interpretation is correct, it pushes the origin of reptiles, and thus amniotes as a whole, back by 35 million years to the earliest Carboniferous. Further support comes from new fossil reptile footprints from Poland, also presented in the study; not as old as those from Australia, but also substantially older than previous records.

This recalibration of the origin of reptiles impacts the whole timeline of tetrapod evolution. The tetrapod crown-group node must be older than the earliest amniotes, because it is a deeper branching point in the tree, but how old exactly? The authors address this problem by combining data from fossils and modern DNA.

  • Footprints of front feet (manus) are shown in yellow, hind feet (pes) in blue. Credit: Grzegorz Niedźwiedzk

  • Fully labeled image of the Australian slab, showing interpretation of the tracks. Footprints of front feet (manus) are shown in yellow, hind feet (pes) in blue. The slab carries two trackways, A and B. For each of these, the footprints are coded as follows: Am1 to Am4 means "Trackway A, manus print 1" to "Trackway A, manus print 4". Ap1 etc. means "Trackway A, pes print 1" etc.. Bm1-4 and Bp1-4 mean the same for Trackway B. Blue and yellow zig-zag lines linking prints indicate the sequence manus and pes prints in each trackway. The label "Ip" next to a white oval means "Isolated pes print", a single footprint facing the opposite direction to the trackways. Credit: Grzegorz Niedźwiedzk

"It's all about the relative length of different branches in the tree," explains Ahlberg.

"In a family tree based on DNA data from living animals, branches will have different lengths reflecting the number of genetic changes along each branch segment. This does not depend on fossils, so it's really helpful for studying phases of evolution with a poor fossil record."

Their analysis, overlaying branch lengths from DNA analyses onto the known fossil dates, indicates that the crown group node lies far back in the Devonian, roughly contemporary with Tiktaalik. This means that a diversity of advanced tetrapods existed at a time when, it has been thought, only transitional "fishapods" were dragging themselves around muddy shorelines and starting in a small way to explore the land. But perhaps that should not surprise us.

"The Australian footprint slab is about 50 cm across," says Ahlberg, "and at present it represents the entire fossil record of tetrapods from the earliest Carboniferous of Gondwana—a gigantic supercontinent comprising Africa, South America, Antarctica, Australia and India. Who knows what else lived there?"

"The most interesting discoveries are yet to come and there is still much to be found in the field. These footprints from Australia are just one example of this," says Niedźwiedzki.

More information: Earliest amniote tracks recalibrate the timeline of tetrapod evolution, Nature (2025).

Journal information: Nature

Provided by Uppsala University