Giant ground sloths made massive paleoburrows in Brazil

Dr. Buatois was featured in a new Nature article, where he commented on recent work done by the Palaeoburrows Project based at the Federal University of Rio Grande do Sul in Porto Alegre, Brazil.

In conjunction with the University of the Extreme South of Santa Catarina (UNESC) in Criciúma, Brazil, paleontologists and archaeologists have been studying a series of massive caves that have had multiple architects and inhabitants during the Pleistocene. The caves are found within a consolidated eolian sandstone unit of the early late Cretaceous Botucatu Formation (100 Ma). This makes the sandstone soft enough to burrow through and consolidated enough that the caves wouldn’t collapse.

The walls of the caves preserve large claw-like markings, as well as inscriptions and graffiti by ancient and modern humans, respectively. The large claw-like marks on the walls of the cave point to the original inhabitants of the cave, proposed to be giant ground sloths. They would construct these burrows for multiple reasons, including potentially to sharpen their claws and to seek refuge from megafaunal predators.

These would be not only the largest palaeoburrows, but the largest trace fossils known so far. From this research, a novel ichnogenera and two novel ichnospecies were named, Megaichnus minor and Megaichnus major. These palaeoburrows are so far known from Brazil and Argentina, and are attributed to giant ground sloths like Scelidotherium and Glossotherium. Work is ongoing to refine the classification scheme for palaeoburrows, conservation, and opportunities for international collaboration on future studies.

Paleoartist Renato Pereira Lopes’ reconstruction of several extinct ground sloths and armadillos and schematic representations of the dimensions of some caves found in South America. Artist credit to Renato Pereira Lopes as seen in Nature https://www.nature.com/articles/d41586-025-00216-x

Paleoartist reconstruction of extinct giant ground sloths and armadillos by Renato Pereira Lopes.

You can read the original study in Ichnos and the news feature in Nature. Listen to a Radio-Canada interview (in French) where PhD student Dmitri Ponomarenko comments on these spectacular paleoburrows here.

Written by Jack Milligan

Congrats to Dr. Brittany Laing!

We would love to congratulate Dr. Brittany Laing on her recent successful PhD defence! Her thesis focused on the behavioural evolution and ecological impact of organisms as seen through trace fossils, specifically applying theories and methodologies from mathematics & behavioural biology to trace fossil datasets in order to quantitatively examine behavioural and ecological changes through time. She also completed a master’s degree with our research group where she studied the ichnology at the Ediacaran and Cambrian GSSP in Newfoundland, Canada. She is also to thank for the Ichnoplanet website!

We are forever grateful for your contributions and wish you all the best in your future endeavours!

Written by Jack Milligan

Meet Himatiichnus mangano!

Recently, an international team of ichnologists led by Katherine A. Turk described a new ichnogenus from the late Ediacaran Huns Member of the Urusis Formation in southern Namibia. They described a series of meandering, intertwining tubes exhibiting dual lineation patterns preserved in convex relief, appearing to disappear into the sediment and reemerge on the sediment surface. The distal terminal ends of the tubes are rounded and bulbous. Modern priapulid worms have produced such structures via peristaltic probing. This is similar to the famous Ediacaran-Cambrian biostratigraphic marker trace fossil Treptichnus pedum, also attributed to priapulid worms.

Figure 2 from Turk et al., 2024 showing the holotype of Himatiichnus mangano. See paper here.

The team also noted that these new trace fossils represented the earliest occurrence of Scalidophora, and are much like those traces of worms in the Cambrian, suggesting ecological interactions typical of the Cambrian Explosion appeared earlier than previously thought (the long fuse hypothesis). The morphological evidence pointed to these trace fossils being a novel ichnogenus and ichnospecies. The team gave the trace fossils the name Himatiichnus mangano, named after our very own Dr. M. Gabriela Mángano!

We couldn’t agree more with this decision, as Dr. Mángano has not only spent her career furthering the field of ichnology from all aspects, but has also contributed greatly to research on the Ediacaran-Cambrian transition around the world. Congrats, Dr. Mangano, on this great honour and achievement!

Get the scientific paper in Royal Society Open Science here.

Written by Jack Milligan

Grasslands National Park Fieldwork 2024

Towards the end of the summer, I had the opportunity to continue fieldwork at two multitaxic Edmontosaurus quarries within the Uppermost Cretaceous Frenchman Formation in the East Block of Grasslands National Park in southern Saskatchewan under the supervision of Dr. Emily Bamforth of the Philip J. Currie Dinosaur Museum and Dr. Ryan McKellar of the Royal Saskatchewan Museum. These excavations have been ongoing and have yielded some fantastic fossil specimens and interesting geology.

We collected a limb bone (tibia) from one of our two Edmontosaurus quarries, called the “Leo” quarry. The tibia shows feeding traces as evidenced by well-defined tooth marks. During the excavation of the tibia, a shed tooth from a tyrannosaurid (Tyrannosaurus rex) was collected from the same depositional layer. This association of tooth traces on Edmontosaurus bones and T. rex teeth suggests that Leo was scavenged during subaerial exposure on a floodplain within a meandering fluvial system. Limb bones have a high likelihood of being consumed due to large locomotor muscles being present (a great food source for predators like T. rex), and thus will tend to have more tooth traces on the bone.

On an adjacent butte within the same depositional layer as the “Leo” quarry, there is a point bar deposit containing a second active quarry named the “Clifford quarry. While the Edmontosaurus in this quarry has yet to produce elements with tooth marks, teeth from T. rex and the crocodyliform Borealosuchus have shown up this past season. Adding to the mystery of this quarry, several articulated turtle skeletons have been collected from this deposit, showing no evidence of being scavenged.

Tooth marks have been a widely debated aspect of vertebrate ichnology. Recently, the category-modifier (CM) system was proposed by Wyenberg-Henzler et al., 2024, as a method to identify different morphologies of tooth marks and their associated behaviours. While not strictly defined within a traditional ichnological framework, it is the most comprehensive overview of tooth marks on bones in the literature to date. Based on the CM system, the tooth marks left on the Edmontosaurus tibia appear to be internally chattered, referring to the crescentic depression on the inside of the tooth mark. Shed carnivore teeth from both quarries suggest that the dominant predators within this ecosystem were crocodyliforms and tyrannosaurs.

Further excavation of the quarries is required, and research into the taphonomy of these two Edmontosaurus quarries is ongoing, but there are sure to be some exciting discoveries to be made in future field seasons!

Written by Jack Milligan

Eastend Summer Fieldwork 2024

Throughout this past summer, I had the opportunity to volunteer with the Saskatchewan Geologic Survey under Dr. Meagan Gilbert in my hometown of Eastend, Saskatchewan. This project aimed to characterize the stratigraphy and depositional environments of the Upper Cretaceous and lower Paleogene of southwest Saskatchewan.

Skolithos isp. in a crossbedded sandstone fluvial channel deposit in the buff facies of the Upper Ravenscrag Formation in southwestern Saskatchewan. Photo provided by Mollie Black

We went to many different geologic outcrops around the town of Eastend. A typical day consisted of taking measurements and samples (so many samples) across the section. A section was first chosen based on the extent of exposed bedrock and then measured from the lowermost exposed bedrock to the top. It wasn’t all just rocks, though! We also found many neat trace fossils and plant fossils, including many just above the KPg boundary.

A huge thank you to all landowners who allowed access to their land.

Written by Mollie Black and Dr. Meagan Gilbert