Oldest sea reptile from Age of Dinosaurs found on Arctic island
For nearly 190 years, scientists have searched for the origins of ancient sea-going reptiles from the Age of Dinosaurs. Now a team of Swedish and Norwegian palaeontologists has discovered remains of the earliest known ichthyosaur or ‘fish-lizard’ on the remote Arctic island of Spitsbergen.
Ichthyosaurs were an extinct group of marine reptiles whose fossils have been recovered worldwide. They were amongst the first land living animals to adapt to life in the open sea, and evolved a ‘fish-like’ body shape similar to modern whales. Ichthyosaurs were at the top of the food chain in the oceans while dinosaurs roamed the land, and dominated marine habitats for over 160 million years.
According to the textbooks, reptiles first ventured into the open sea after the end-Permian mass extinction, which devastated marine ecosystems and paved the way for the dawn of the Age of Dinosaurs nearly 252 million years ago. As the story goes, land-based reptiles with walking legs invaded shallow coastal environments to take advantage marine predator niches that were left vacant by this cataclysmic event. Over time, these early amphibious reptiles became more efficient at swimming and eventually modified their limbs into flippers, developed a ‘fish-like’ body shape, and started giving birth to live young; thus, severing their final tie with the land by not needing to come ashore to lay eggs.
The new fossils discovered on Spitsbergen are now revising this long accepted theory.
Close to the hunting cabins on the southern shore of Ice Fjord in western Spitsbergen, Flower’s valley cuts through snow-capped mountains exposing rock layers that were once mud at the bottom of the sea around 250 million years ago. A fast-flowing river fed by snow melt has eroded away the mudstone to reveal rounded limestone boulders called concretions. These formed from limey sediments that settled around decomposing animal remains on the ancient seabed, subsequently preserving them in spectacular three-dimensional detail. Paleontologists today hunt for these concretions to examine the fossil traces of long-dead sea creatures.
During an expedition in 2014, a large number of concretions were collected from Flower’s valley and shipped back to the Natural History Museum at the University of Oslo for future study. Research conducted with The Museum of Evolution at Uppsala University has now identified bony fish and bizarre ‘crocodile-like’ amphibian bones, together with 11 articulated tail vertebrae from an ichthyosaur. Unexpectedly, these vertebrae occurred within rocks that were supposedly too old for ichthyosaurs. Also, rather than representing the textbook example of an amphibious ichthyosaur ancestor, the vertebrae are identical to those of geologically much younger larger-bodied ichthyosaurs, and even preserve internal bone microstructure showing adaptive hallmarks of fast growth, elevated metabolism and a fully oceanic lifestyle.
Geochemical testing of the surrounding rock confirmed the age of the fossils at approximately two million years after the end-Permian mass extinction. Given the estimated timescale of oceanic reptile evolution, this pushes back the origin and early diversification of ichthyosaurs to before the beginning of the Age of Dinosaurs; thereby forcing a revision of the textbook interpretation and revealing that ichthyosaurs probably first radiated into marine environments prior to the extinction event.
Excitingly, the discovery of the oldest ichthyosaur rewrites the popular vision of Age of Dinosaurs as the emergence timeframe of major reptile lineages. It now seems that at least some groups predated this landmark interval, with fossils of their most ancient ancestors still awaiting discovery in even older rocks on Spitsbergen and elsewhere in the world.
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The paper is published in the prestigious international life sciences journal Current Biology.
Kear, B.P., Engelschiøn, V.S., Hammer, Ø., Roberts, A.J. & Hurum, J.H., 2023: Earliest Triassic ichthyosaur fossils push back oceanic reptile origins. Current Biology 33(5), R1-R2.