Triassic Megapredator’s Last Meal Was a Massive Marine Reptile

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Fossil Ichthyosaur Guizhouichthyosaurus Stomach

Closeup of the stomach area of a fossil ichthyosaur, Guizhouichthyosaurus, showing part of the body of another large marine reptile. The ichthyosaur had swallowed its prey shortly before it died and was fossilized. This is the oldest known direct evidence of megapredation, or a large animal eating another large animal. Credit: Da-Yong Jiang, et al.

Some 240 million years ago, a dolphinlike ichthyosaur ripped to pieces and swallowed another marine reptile only a little smaller than itself. Then it almost immediately died and was fossilized, preserving the first evidence of megapredation, or a large animal preying on another large animal. The fossil, discovered in 2010 in southwestern China, is described in a paper published on August 20, 2020 in the journal iScience.

The ichthyosaurs were a group of marine reptiles that appeared in the oceans after the Permian mass extinction, about 250 million years ago. They had fishlike bodies similar to modern tuna, but breathed air like dolphins and whales. Like modern orcas or great white sharks, they may have been apex predators of their ecosystems, but until recently there has been little direct evidence of this.

When a specimen of the ichthyosaur Guizhouichthyosaurus was discovered in Guizhou province, China, in 2010, researchers noticed a large bulge of other bones within the animal’s abdomen. On examination, they identified the smaller bones as belonging to another marine reptile, Xinpusaurus xingyiensis, which belonged to a group called thalattosaurs. Xinpusaurus was more lizardlike in appearance than an ichthyosaur, with four paddling limbs.

Ichthyosaur's Last Meal

The stomach of this 240-million year old fossil ichthyosaur contains the mid-section of another marine reptile that in life would have been only slight smaller. It’s the first direct evidence of ancient megapredation — one large animal eating another. Credit: Da-Yong Jiang, et al, iScience

“We have never found articulated remains of a large reptile in the stomach of gigantic predators from the age of dinosaurs, such as marine reptiles and dinosaurs,” said Ryosuke Motani, professor of earth and planetary sciences at the University of California, Davis, and co-author on the paper. “We always guessed from tooth shape and jaw design that these predators must have fed on large prey but now we have direct evidence that they did.”

The Guizhouichthyosaurus was almost 5 meters (15 feet) long, while the researchers calculate its prey was about 4 meters (12 feet) long, although thalattosaurs had skinnier bodies than ichythosaurs. The predator’s last meal appears to be the middle section of the thalattosaur, from its front to back limbs. Interestingly, a fossil of what appears to be the tail section of the animal was found nearby.

Predators that feed on large animals are often assumed to have large teeth adapted for slicing up prey. Guizhouichthyosaurus had relatively small, peglike teeth, which were thought to be adapted for grasping soft prey such as the squidlike animals abundant in the oceans at the time. However, it’s clear that you don’t need slicing teeth to be a megapredator, Motani said. Guizhouichthyosaurus probably used its teeth to grip the prey, perhaps breaking the spine with the force of its bite, then ripped or tore the prey apart. Modern apex predators such as orcas, leopard seals and crocodiles use a similar strategy.

Read Massive Reptile Discovered in the Belly of a Triassic Megapredator for more on this research.

Reference: “Evidence Supporting Predation of 4-m Marine Reptile by Triassic Megapredator” by Da-Yong Jiang, Ryosuke Motani, Andrea Tintori, Olivier Rieppel, Cheng Ji, Min Zhou, Xue Wang, Hao Lu and Zhi-Guang Li, 20 August 2020, iScience.
DOI: 10.1016/j.isci.2020.101347

Co-authors on the study: Da-Yong Jiang, Min Zhou, Xue Wang and Hao Lu, Peking University, China; Andrea Tintori, Università degli Studi di Milano, Italy; Olivier Rieppel, The Field Museum, Chicago; Cheng Ji, Nanjing Institute of Geology and Palaeontology, China; and Zhi-Guang Li, The Geoscience Museum, Hebei GEO University, China. Funding was provided by the National Natural Science Foundation of China, the Ministry of Science and Technology, and the National Geographic Society.





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