Behold, NHMUK R5161: the extraordinary holotype of Scolosaurus cutleri. This is truly one of the most amazing dinosaur fossils that has been collected from Alberta, and is one of the best preserved ankylosaurs in the world. And the best part is that it is on display for everyone to enjoy in the galleries of the Natural History Museum in London.
(Many thanks to Angelica Torices for snapping this photo for me! NHMUK R5161 is beautiful to look at, but difficult to photograph well, and I’m afraid most of my photos from my visit in 2009, while useful to me, are not necessarily that nice to look at.)
Most of the time, when you’re looking at a drawing or model of Euoplocephalus, what you’re really mostly looking at is NHMUK R5161. This specimen preserves a large amount of intact skin, which means that the free-floating osteoderms are, for the most part, in their correct life positions. Osteoderms form in the dermis of the skin, and so osteoderms are usually found as isolated elements, or scattered around disarticulated or associated skeletons. Because NHMUK R5161 is so complete, it has formed the basis for most restorations of Euoplocephalus.
Yup, all of these are kind of Scolosaurus. Especially the pink one. Perhaps somewhat embarassingly, this does not represent my complete collection of ankylosaur ‘scientific models’.
However, you may have noticed something important: Scolosaurus lacks a skull and tail club. So, how could I figure out if Scolosaurus was the same as Euoplocephalus, if I couldn’t look at the patterns of cranial ornamentation? If you remember back to part 2 of this series, I said that the morphology of the first cervical half ring was useful for diagnosing Euoplocephalus.
The first cervical half ring of NHMUK R5161 has some important differences when compared to CMN 0210, UALVP 31, or AMNH 5406. In NHMUK R5161, the two medial osteoderms (closest to the midline) are round and lack keels, instead having a centrally located bump. Even in specimens of Euoplocephalus that have relatively flat medial osteoderms on the cervical half rings, like AMNH 5404, the medial osteoderms always have a keel and are more oval than circular. This suggested that Scolosaurus was distinct from Euoplocephalus and Anodontosaurus, even though it didn’t have a head or tail club. (I largely agree with Penkalski and Blows’ (2013) assessment that Scolosaurus is a valid taxon, but for somewhat different reasons than what they present in their paper.)
(A quick note about tail clubs and Scolosaurus – many artists have reconstructed this animal with a short tail and spiked tail club. The tail of NHMUK R5161 is broken at about the midpoint of the tail, probably just in front of where the tail club would have started. The skin is kind of sloughed out in this area, which has led many to erroneously interpret Nopcsa’s figures and drawings as showing the knob of bone at the end of the tail. The ‘spikes’ on the tail club are really just osteoderms present at about the midpoint of the tail – no ankylosaurs had spikes on their tail clubs.)
The collection of NHMUK R5161 is one of the more interesting stories of palaeontological collecting in Alberta. The specimen was discovered and primarily excavated by William Edward Cutler in 1914, working for the Calgary Syndicate for Prehistoric Research (an excellent name for an organization that is, sadly, defunct). During excavation, the ankylosaur block collapsed on Cutler, no doubt causing grievous injuries. One of the Sternbergs finished the excavation, and the specimen was shipped to London.
NHMUK R5161 is significant, beyond being so complete, because it may derive from the Oldman Formation of Dinosaur Provincial Park, rather than the Dinosaur Park Formation. The quarry is somewhere across the river from Happy Jack’s, the University of Alberta’s field camp since 2008. However, the precise locality of the quarry is somewhat up for debate, and Oldman Formation sediments crop out in this area. Next week I’ll be heading to Dinosaur Provincial Park, and one of the goals is to check out some of the potential quarry locations with our crew from the UofA, as well as Darren Tanke from the Tyrrell Museum, who has been investigating the NHMUK R5161 quarry for some time. It’s important to know whether or not Scolosaurus comes from the Oldman or Dinosaur Park formation, so we can know whether or not Scolosaurus lived at the same time as Euoplocephalus. We will also be on the lookout for any leftover material…like the skull and tail club.
For a long time I was bitterly disappointed that there was no skull known for Scolosaurus. Could some of the isolated skulls I was referring to Euoplocephalus instead belong to Scolosaurus? Or was the skull of Scolosaurus noticeably different from Euoplocephalus? I despaired that I wouldn’t have an answer to that question unless we miraculously collected another Scolosaurus from Dinosaur Park during my thesis. In the meantime, I was trying to figure out the identities of “Euoplocephalus” specimens from the Two Medicine Formation of Montana, which seemed very different from the Albertan specimens. These skulls had much longer and pointier squamosal horns with a ‘backswept’ appearance compared to Euoplocephalus and Anodontosaurus. I thought perhaps that the Two Medicine ankylosaurids might represent a new species of ankylosaurid (as did others – Penkalski named Oohkotokia earlier this year based on MOR 433, which has this unusual squamosal horn morphology).
From left to right, the first cervical half rings of AMNH 5337, TMP 2001.42.9, USNM 7943, and NHMUK R5161. The top row shows the half rings in anterior or posterior view, and the bottom row shows the rings in dorsal view. NHMUK R5161 is in dorsal view. Modified from Arbour and Currie (2013).
One day I was flipping through my photos of the Two Medicine Formation specimens when I realized that the morphology of the first cervical half ring of TMP 2001.42.9, the only specimen that had a half ring and skull, matched that of NHMUK R5161. Both had flat medial osteoderms with a central bump, rather than a keel. And indeed, another isolated half ring from the Two Medicine formation had this morphology as well. Scolosaurus was present in Montana!
I’ll just take a moment here to address Oohkotokia: while I agree with Penkalski (2013) that the Two Medicine Formation ankylosaurid differs from Euoplocephalus, I do not think it differs sufficiently from Scolosaurus for these to be considered separate species. Perhaps one day in the future we’ll find another Scolosaurus from Dinosaur Park that has flat medial osteoderms on the cervical half ring, but a skull with different squamosal horns compared to the Two Medicine skulls. If that happens, then I think you could make the case that Oohkotokia is valid. Until then, Oohkotokia is a junior synonym of Scolosaurus.
With the referral of the Two Medicine ankylosaur material to Scolosaurus, Scolosaurus now had a head! TMP 2001.42.9 even has a tail club, so we know that Scolosaurus had a round tail club knob. With the in situ osteoderms and skin impressions of NHMUK R5161, Scolosaurus is now one of the best understood ankylosaurids in the world. Now, if we could just figure out for certain exactly where it was collected from…
Next time: wrapping up loose ends, and figuring out what it all means.
Arbour VM, Currie PJ. 2013. Euoplocephalus tutus and the diversity of ankylosaurid dinosaurs from the Late Cretaceous of Alberta, Canada, and Montana, USA. PLOS ONE 8:e62421.
Nopcsa BF. 1928. Palaeontological notes on reptiles. V. On the skull of the Upper Cretaceous dinosaur Euoplocephalus. Geologica Hungarica, Series Palaeontologica 1:1-84.
Penkalski P, Blows WT. 2013. Scolosaurus cutleri (Ornithischia: Ankylosauria) from the Upper Cretaceous Dinosaur Park Formation of Alberta, Canada. Canadian Journal of Earth Sciences 50:171-182.
Penkalski P. 2013. A new ankylosaurid from the Late Cretaceous Two Medicine Formation of Montana, USA. Acta Palaeontologica Polonica, in press.