In 2014, an unlikely discovery was made in the Judith River Formation of Montana: a massive Ankylosaurid, perhaps the best preserved of its type ever found in North America. The specimen’s axial skeleton remains largely intact, articulated from the iconic clubbed tail to the end of the cervical vertebra. Even more spectacular is that this skeleton (TE-072) has a majority of its skin, soft tissue and armor keratin preserved The skeleton is approximately 21 feet long, making it one of the largest Ankylosaurids found in N. America.

The Ankylosaurs are members of an unusual group of armored dinosaurs that existed during the Late Cretaceous epoch. They are relatively rare in the fossil record and are generally described from isolated bones and partial skeletons. Nicknamed “Sherman” after the formidable WWII tank of the same name, TE-072 represents one of the finest and best preserved specimens of Ankylosaurid yet to be discovered. This 78 million-year-old fossil shows exceptional preservation of the articulated skeleton and includes fine preservation of soft tissue and intact armor plates. Its exceptional condition along with an unusually large size, makes “Sherman” a truly remarkable specimen for research and exhibition.

A – Dorsal vertebrae (ventral side)
B – Dorsal ribs (slight disarticulation)
C – Cervical vertebra (disarticulated
D – Dorsal ribs (distal ends)
E – Right ilium
F – Sacral vertebra

The Judith River Formation comprises a vast expanse of sediment laid down during the Campanian age between 80 and 75 million years ago. The Campanian is the penultimate age of the Late Cretaceous epoch, before the extinction event which abruptly concluded the age of dinosaurs around 65.5 million years ago.

TE-072 was discovered in the summer of 2014 on a private ranch in north central Montana, in the heart of the Upper Judith River Formation. The Judith River Formation is part of the Judith River Group, which is a series of Campanian Age sedimentary formations, running from the southern regions of Alberta and Saskatchewan, Canada into northern and central Montana in the United States. This group is known for the excellent preservation of its diverse flora and fauna.

TE-072 was discovered in a channel lag deposit, which was being excavated for a disarticulated Gorgosaurus liberatus specimen (TE-036). Nearly all of the articulated specimen was preserved in a siderite concretion formed from ultra-fine silt/sandstone. Contained within this concretion are numerous exquisite plant fossils, which exhibit the detailed preservation of which this matrix is capable. The unlikely discovery of “Sherman”, nearly 30ft from the edge of the exposure and beneath 40 feet of overburden, means none of the fossil had weathered or had been exposed to the elements. This rare occurance is ideal for fossil collection, as the specimen remains intact with minimal deterioration to the fossil material and scientific data.

The specimen TE-072 was recovered in two oversized blocks, one containing the tail and one containing the body and head, to maintain the integrity of the site and prevent damage to soft tissue and preserved materials valuable to science. The main block weighed a total of 21 tons after it had been safely prepared for extraction.

“Sherman” is estimated to be between a 90-95% complete specimen. Due to the abundance of delicate soft-tissue preservation, the majority of the specimen has not been exposed from the matrix. This preserves the scientific integrity of the specimen until further detailed research can be conducted. “Sherman” was preserved ventral side up with an axial skeleton fully articulated from the club through the end of the cervical series.

The osteograph shows currently exposed elements including the ventral side of the articulated dorsals, articulated caudal and tail club, several disarticulated dorsal ribs and cervical vertebra, and partially articulated ischium and sacral vertebra. Several intact osteoderms of various sizes including armor scutes have also been exposed. The skull was disarticulated from the cervical vertebra and has been fully prepared to assist in species identification.

The method of preservation and location at the time of discovery has preserved TE-072 as an exceptional museum- quality specimen. Most notable is the abundance of soft-tissue preservation in conjunction with a nearly complete articulated axial skeleton. The bones are well protected by the matrix and show excellent surface texture and detail. The patina of the fossil is medium to light brown, which is consistent with fossils found in the Judith River Formation. There is no sign of “pyrite disease” or other mineral issues that would represent a problem with future preservation of the fossils.

Order: Ornithiscia
Family: Ankylosauridae
Subfamily: Ankylosaurinae
Genus: Euoplocephalus/ Ankylosaurus
Species: sp?

With limited examples of the North American Anylosauridae available, TE-072 will allow for a breadth of new information about this unusual family. Articulated bone position, skin texture, preserved keratin structures, and possible muscle layers and orientation are preserved and may support or provide new information about Ankylosaurid morphology. In preliminary taxonomic comparisons with Euoplocephalus tutus, several skull horns and armored elements suggest inconsistencies from the described species E. tutus and may lead to the establishment of a second species within this monotypic genus.

In preliminary studies of TE-072, the specimen appears to be one of the best preserved examples of Ankylosaurid from North America. Skin preservation appears on nearly every exposed area of the specimen. The preserved skin layer sits around 3 inches above the fossil bone, suggesting mummification and the preservation of soft tissue elements preserved within. Thick layers of tiny osteoderms (average of 1cm), estimated in the thousands, lay embedded between the outer skin and fossil bone, further supporting evidence of subcutaneous soft tissue preservation. Exposure of soft tissue has been minimized, but several areas are known areas of soft tissue preservation. Several of the major lateral osteoderms on the dorsal side of the tail still retain evidence of their keratin coverings.

A.  Caudal area with keratin over the lateral osteoderms and skin preservation on dorsal side of the caudal series
B.  Keratin over the large lateral osteoderms by the left shoulder
C. Skin layer and soft tissue area from the belly to the ischium.

– Partially prepared, nearly complete articulated skeleton contained in two field jackets
– Fully prepared skull and dentaries
– Quarry maps
– Inventory lists of all collected material
– Field and labratory photos
– Field and labratory notes
– GPS location data
– Legal documentation including, signed lease agreement and Federal certification letter from appropriate agency if applicable.

For all information concerning TE-072 or any specimens from our catalog please contact us at

info@theropodaexpeditions.com

For General information or interest in our full project catalog please visit  us at:

www.theropodaexpeditions.com

All documentation and materials will be transferred to buyer at the time of purchase.

Documentation, materials, photographs, maps, legal documents, GPS data are available for inspection upon request.