Showing posts with label geology. Show all posts
Showing posts with label geology. Show all posts

Wednesday, March 9, 2016

Ankylosaurs by the sea

Ankylosaurs, like probably most other dinosaurs, were landlubbing, terrestrial animals without obvious aquatic adaptations. And yet, surprisingly, their fossils are found in marine sedimentary environments more often than most other dinosaurs (except hadrosaurs). Some, like Aletopelta, wound up in shallow or lagoonal environments - Aletopelta's carcass became a reef! - but some, like the Suncor nodosaurid, wound up far away from shore.

Aletopelta! See if you can spot the oyster marks, invertebrates, and shark teeth around the pelvis and legs.

I wanted to look into this phenomenon in a bit more detail than it had been investigated previously, and with my work on ankylosaurid phylogenetics and biogeography published last year the time was right to dive into marine ankylosaurs. I added in more taxa into my ankylosaurid character matrix to check whether there were any secret ankylosaurids hiding in the taxa I didn't previously include. 


Surprisingly, Hylaeosaurus popped out as a basal ankylosaurid in this analysis, an intriguing result that I think needs further investigation but could be really interesting. Mostly everything else that should be a nodosaurid was a nodosaurid, and I got surprisingly good resolution in the Nodosauridae, but take the interrelationships there with a tiny grain of salt given that I didn't make any new characters for this analysis and the existing character set is geared towards ankylosaurids.

Next up, I downloaded a dataset of all the ankylosaur occurrences in the Paleobiology Database and went through each entry (more than 500!) to verify whether or not the specimens were ankylosaurids, nodosaurids, or if we couldn't tell for sure, and their depositional environment. With that data in hand, we wanted to know what the geographic distribution of ankylosaur marine occurrences looked like, and here it is:


Lots of ankylosaurs in the northern hemisphere, not so many in the southern hemisphere. More than half of marine ankylosaurs occur in North America, which is perhaps unsurprising given that North America had a bad habit of being underwater for a lot of the Cretaceous. When we exclude indeterminate occurrences, we get an ankylosaurid-nodosaurid marine-terrestrial split that looks like this:


In North America and Asia, the distribution of ankylosaurs in different environments is statistically significant, but it isn't in Europe (and remember, Hylaeosaurus hasn't previously been found as an ankylosaurid so there might not even be ankylosaurids in Europe).

Although there are nodosaurids and ankylosaurids in Asia, I don't think they overlapped very much in time - nodosaurids disappear from the Asian fossil record around the time that ankylosaurids appear. North America is unique in that it is the only place where we find both clades of ankylosaurs overlapping for significant chunks of time, so I wanted to know whether or not the significant marine-terrestrial dichotomy holds up in different time intervals within North America. We decided to divide up the dataset by the ebb and flow of the Western Interior Seaway, or, transgressive-regressive cycles. There were several major cycles well known to sequence stratigraphers and other geologists, and it seemed like a logical way to look at how the seaway influenced marine occurrences in ankylosaurs. How does that data look?


Like this! Unsurprisingly, a huge number of ankylosaur occurrences are clustered at the end of the Cretaceous, largely because of the Dinosaur Park Formation and its well-documented dinosaur fauna. But focus on the marine occurrences and an interesting pattern emerges - while the number of terrestrial occurrences fluctuates widely, the number of marine occurrences stays relatively steady. We think this reflects the absence of terrestrial outcrops for a chunk of the mid Cretaceous when sea levels were at their very highest - in other words, although there's a greater proportion of marine occurrences in the middle, they don't really increase in absolute terms and the proportion is being driven by the drop in terrestrial occurrences.


And here's what it looks like when we exclude indeterminate ankylosaurs. Unfortunately, this is the point at which we lose statistical power for most of the data, which means we can't really interpret most of the results with any confidence. Plus, there is a good chunk of time in the mid Cretaceous in which there are no ankylosaurids known at all, which probably represents a regional extinction for this group of dinosaurs. BUT, one time bin shows a significant difference between depositional environment and clade - the Kiowa-Skull Creek cycle in the Albian-Cenomanian.

What does it all mean? For one thing, breaking down the global ankylosaur dataset still yields enough statistical power for some analyses to be useful and give us more insight into biogeographic patterns...up to a point. Secondly, there really does seem to be something about nodosaurids that makes them wind up in marine environments more often than ankylosaurids. And this begs the question: why don't ankylosaurids like the beach? Given that ankylosaurids disappear from North America right around the time that sea levels rose to their highest point, could rising sea levels have led to the extinction of North American ankylosaurids? Did sea levels need to drop substantially before the inland, somewhat desert-dwelling Asian ankylosaurids migrated back into North America in the latest Cretaceous? Did ankylosaurids avoid the European archipelago because they didn't like to get their feet wet? I don't have definite answers yet, but I find this pattern terribly interesting and I'm sure this isn't the last we'll be looking at this weird split in environmental preferences between ankylosaurids and nodosaurids.

The paper is free until April 22! Get your PDF while it's still hot! Arbour VM, Zanno LE, Gates T. 2016. Ankylosaurian dinosaur palaeoenvironmental associations were influenced by extirpation, sea-level fluctuation, and geodispersal. Palaeogeography, Palaeoclimatology, Palaeoecology 449:289-299.

Saturday, November 7, 2015

Fortunate Son

Elsewhere in the Mesozoic, parts of the field crew were working away at Cretaceous dinosaurs in the Mussentuchit Member of the Cedar Mountain Formation. In may we worked at Crystal Geyser Quarry, which is in the Yellow Cat Member of the same formation and is about 125 million years old, in a part of the Cretaceous called the Barremian. In contrast, the Mussentuchit Member is about 98 million years old, or Cenomanian in age. The Cedar Mountain Formation is a giant unit of rock, and the dinosaur faunas changed dramatically throughout!

The dinosaur fauna of the Mussentuchit is still poorly known, and we still don't know very much about the dinosaurs of the 'middle' Cretaceous compared to the Jurassic (like the Morrison Formation) or the Late Cretaceous (like my previous fieldwork in Alberta and Mongolia). There are still many new dinosaurs to be discovered here! This quarry has produced a new small iguanodontian, nicknamed Fortunate Son for the time being while we prepare its bones and until it is formally described.

The views from this quarry are terrible. Just awful.

The Fortunate Son quarry was about a 30-40 minute hike from camp and generally a very pleasant place to work. However, when the weather looks like this, you're probably going to get wet.

This particular thunderstorm was threatening us for a long time, but when the sky opened up it was worse than expected and an almost instantaneous drenching. Here we are hiding from the lightning! For extra bonus fun, we had to walk over the highest hill in the vicinity in order to return to camp, so we had to wait this one out for a long time until we thought it was safe. When we finally tried heading home, the slick wet mud made us very slow, and the lightning started again by the time we got to the top of the hill. GOOD TIMES. Lindsay also posted about our stormy weather at the Expedition Live blog!

  
Camp wasn't much drier!

Later that day, a second thunderstorm rolled through, throwing hail onto us like I haven't experienced before. Grape-sized hail came down for at least 15 minutes straight, so we figured we may as well try to get some free ice for our drinks.

Haviv made the best of the bad weather with some mud sculpting!

We also spent some time prospecting for new localities, although I didn't find anything particularly exciting. The strata here are much more deformed than what I'm used to, making for some steep hiking! The red rocks towards the bottom are Jurassic Morrison Formation, and the buff coloured rocks above are largely the Ruby Ranch Member of the Cedar Mountain Formation, with Mussentuchit Member rocks closer to the top.

Here's a kind of ok 180-panorama from the highest point I climbed to one day. Click to embiggen!

Next time, we meet a Decepticon.

Monday, October 19, 2015

Wading With Dinosaurs

It's that time of year again! Time to talk palaeontology with a 1000 of my closest friends in a convention centre somewhere far, far away! That's right, it's the annual meeting of the Society of Vertebrate Paleontology, this time in Dallas, Texas. This year I tried out an SVP meeting field trip for the first time. We chased dinosaurs and their friends through the mid Cretaceous near Dallas!

First stop - Jones Ranch

While the morning was still cool, we ventured out to the Jones Ranch quarry, where the remains of several Sauroposeidon were excavated. Originally called Paluxysaurus, these bones belonged to several large sauropods from the Twin Mountains Formation, which is about 113 million years old or so. I was pretty impressed by the size of the quarry - I'm standing maybe 5 feet in front of one of the quarry walls, and looking towards the other.


Second stop - Dinosaur Valley State Park and the Paluxy River/Glen Rose trackways!

Dinosaur Valley State Park is one of those iconic dinosaur places that I'm sure is on many palaeontologist's bucket lists. If you've visited the American Museum of Natural History, you will probably have seen some of the trackways cut out of this very river - a piece of the tracksite was taken back to New York for display and hangs out underneath the Apatosaurus (Brontosaurus? Now I forget which specimens are which!). 

 The trackways are in the Albian aged Glen Rose Formation, and the rocks represent a lagoon or shallow marine environment. I guess dinosaurs liked the occasional day at the beach, as well! There are two kinds of trackmakers here, and here's one of them - a large theropod, probably something like Acrocanthosaurus.

And here's the other trackmaker, a large sauropod, possibly something like Sauroposeidon. In case that one is hard to make out, the hind foot print is about a foot to the left of that person's shoe, and is the large smooth depression with a series of vertical shadows at the front - those are the claw marks from a sauropod's hind foot. The front feet made totally different tracks, which look kind of like crescents or half-moons.

Intrepid field trip leader James Farlow heads into the river to sweep of a larger track surface. Most of the trackways are submerged, and you can see some of them in the foreground in this picture - look for the alternating big teardrop or circle shapes!

Most of us waded in and took turns sweeping slime out of the footprints and standing in them. 

The cool water felt pretty good on a hot Texas afternoon!

 
And this post wouldn't be complete without mentioning the great opportunity to see a different era of palaeontological history, in the form of original Sinclair World's Fair dinosaur statues!


Third stop - Arlington Archosaur Site


The Arlington Archosaur Site is a huge quarry in the Cenomanian Woodbine Formation that is located in an active housing development site - pretty soon, this will be part of some lucky people's backyards! It's a neat parallel to the Danek Bonebed in Edmonton, which is also located right within the city. Many volunteers have contributed thousands of hours to help excavate the remains of crocodilians, the early hadrosaur Protohadros, and more. This site has only been worked for a few years, so expect lots of discoveries and publications to come. Find some ankylosaurs, guys!

 The AAS volunteers had cold beverages and dinosaur trackway cookies waiting for us! Y'all are too nice. What a great way to end the day.


Many many thanks to the field trip leaders Chris Noto, Thomas Adams, and James Farlow for taking us on this romp through the mid Cretaceous - it was a great mix of classic sites and new discoveries, and a great start to the conference!

Friday, May 16, 2014

Many animals have skeletons besides dinosaurs.

I was reminded of an old post on this blog today when someone brought up the all too common question of "Is that real?" in museums. In 2011 I had visited the Smithsonian natural history museum for some of my Euoplocephalus research, and spent a day browsing the galleries and shamelessly eavesdropping on people's conversations. I was dismayed by the number of people saying things like "What's that!" and then walking away without finding out, or saying "Look, a T. rex!" to things that were patently not T. rex. In the comments on that post, there was some discussion of the fact that visitors to museums often mistake any skeleton as a dinosaur skeleton.

Anyway, that in turn reminded me of a photo I took in the Nova Scotia Museum of Natural History's marine gallery a while ago:


Despite being surrounded by all manner of marine specimens, including a fleshed out model of a sei whale up above, the museum has to explicitly say that a pilot whale is not a dinosaur. In fairness, the museum (sadly!) does not have any dinosaur skeletons, what with Halifax being located on top of the Cambrian-Ordovician Meguma Terrane, and with the Fundy Geological Museum fulfilling the role of the dinosaur-having museum in Nova Scotia.

What lessons can we learn from this?
1. Museum people: put a dinosaur in your museum. There's no excuse not to have one.
2. Everybody else: many animals have skeletons besides dinosaurs.
3. ????




*Bonus! Sable Island is a super neat place that not many people have heard about outside of the maritime provinces - you can read more about it at their National Park page!

Sunday, December 1, 2013

Paleo201 comes to an end

The first offering of Paleo201, Dinosaurs in the Fossil Record, essentially comes to an end today with the final field trip of the semester. The students will have their exam later in December.

Even though it is a lot of work to be involved in the creation of a new course, I think Paleo201 is a great addition to the University of Alberta's paleontology offerings. Using the Dino101 content on Coursera, and pitched at an essentially first-year level (despite its 200 designation) for students from all faculties, Paleo201 is what's called a blended learning course. We rely on the Dino101 course videos to deliver the base lecture content for the course, which means we typically only meet once per week for an in-class lesson. These lessons have included research talks by grad students in our labs on topics relevant to each week's lesson. However, we also tried to break away from the lecture format for at least some of the in class lessons, to take advantage of some of the resources available on campus. One week we learned the basics of the rock cycle and general Canadian geology using the Department of Earth and Atmospheric Sciences Geoscience Garden, an installation of rocks from around Canada arranged in a particular fashion for students to learn basic mapping skills. And last week we did tours of the Paleontology Museum and our prep labs, including sneak peeks of some cool up and coming research projects. FUN FACT: Our Dunkleosteus skull cast was ranked higher than the dinosaur specimens in my highly scientific 'what did you find most interesting' poll. Blindingly obvious take-home message for instructors: Students like new things and surprises, and dinosaurs are not necessarily the be-all and end-all!

But the highlights, in my opinion, are the three field trips to Jurassic Forest, Dry Island Buffalo Jump Provincial Park, and the Royal Tyrrell Museum.

Jurassic Forest is a tourist attraction outside of Edmonton that features animatronic dinosaurs set outside in a forest. Although I had some comments that this was an odd place to take students on a university field trip, I actually think it worked really well as a way to ease students into some of the topics covered in the first couple of lessons – basic dinosaur anatomy, diversity, diet, etc. And because a lot of the signage and interpretive material at the forest has been put together by graduates of the UofA's BSc program in Paleontology, the educational content is accurate, up to date, and nicely presented.


Many of the students told me that our trip to Dry Island was the first time they had really gone hiking, so I think that speaks to the value of having a course like this one. We hiked the students around the badlands and out to the Albertosaurus bonebed, stopping to discuss  geology, look for fossils (but not collect any, as we didn't have permits this time), and talk about how we interpret bonebeds and make inferences about dinosaur behaviour. Everyone was SO EXCITED to find little bits and fragments of bones. A couple of the students told me they returned the next weekend with their families because they had enjoyed the field trip so much! Blindingly obvious take-home message for instructors: Students like to go outside! And while videos and online stuff and lectures are perfectly fine, doing 'real' things with real fossils and real locations etc. etc. can never fully replace the online experience. Also I got artists and history students and linguistics majors and such to like rocks, so there.


And today we headed down to the Tyrrell Museum, which is a bit of a long day trip from Edmonton, since Drumheller is a little more than 3 hours away – but we were helped along by some dino documentaries. As always, the museum is an amazing resource, and it was super fun to see the students putting together many of the different concepts learned this semester. There were many good questions and enthusiastic discussions about the things we were seeing. And of course, having Phil there to talk to the students about the history of the museum and some of his personal experiences in collecting many of the fossils on display is pretty cool!


Because this is partly an online course, one of the things I've tried to incorporate into the field trips is discussion of the field trip in the course discussion forums. Each time the students have had to take a picture of themselves with a backdrop of choice (favourite dinosaur at Jurassic Forest, favourite scenic view at Dry Island, favourite display at the Tyrrell) and tell us something about it. This worked really well and it is also a fun way to get some feedback about what people are twigging onto as interesting in the course. Fun fact: Not everyone's favourite dinosaur/etc. was T. rex! There is hope for the world!



This is the last course for which I will ever be a teaching assistant, as my grad school days are wrapping up in a few weeks. This course was lots of fun to teach, hopefully has been fun to take, and I hope future students and instructors have as much fun as I did!

Saturday, June 1, 2013

Dinosaur Provincial Park fieldwork 2013

Last week I returned to Happy Jack's at Dinosaur Provincial Park for a brief stint of fieldwork. This has been the University of Alberta's base camp since 2008, and the area has been very productive for us.


Just north of our campground is the old homestead Old Mexico Ranch, where Happy Jack lived from 1903 to 1942.


A few weeks before we arrived in camp, a huge fire burnt away most of the sage bushes and other scrub at ground level. You can see scorch marks on the cottonwood trees in this photo. Windy days meant we all got pretty dirty from blowing ash.


We have a pretty nice setup in camp - two large canvas tents are our supply tent and kitchen tent (and also work as a shelter during rainy days). A fire pit and grill are available for cooking when there aren't fire bans, and the river is our bathtub (although a bit silty). 


We headed across the river from Happy Jack's to check out some possible locations for the Scolosaurus quarry. I was very grateful to be out with Darren Tanke, who has been researching the location of the quarry for quite some time, and Phil Currie. Both of them know Dinosaur Provincial Park like the back of their hands (well, their own hands). 


We weren't able to pinpoint the exact location of the quarry just yet, but tantalizing clues continue to be unearthed. I am hopeful that one day we will be able to relocate the quarry and determine once and for all if Scolosaurus is from the Oldman or Dinosaur Park formation.


The area around Happy Jack's, on the north side of the Red Deer River, has steeper badlands compared to the 'core' area of Dinosaur Provincial Park where the camping and visitor facilities are located. This means there's slightly less accessible exposure and you have to do a lot of climbing. But, it also meant it had been prospected much less for several decades until we began working there in 2008. We've found several interesting and scientifically significant specimens over the last few years that are still undergoing preparation and awaiting publication, but I'm looking forward to sharing them here once they're published!


Traversing the steep slopes sometimes requires more courage than I think I am naturally equipped with, but I enjoy the challenge of navigating around this landscape. You have to watch out for sinkholes and steep dropoffs. Ironstone pebbles and dry bentonite can roll under your feet and cause you to fall and slide, so you have to be relatively surefooted. 


The bentonite is surprisingly sharp on your hands when it's dry, and it isn't pleasant to put your hands on it while climbing. (But still preferable to sticking your hand on a cactus, which I stupidly did a couple of times when I started to slide. Ouch!) When it rains, the bentonite swells up and becomes incredibly greasy. It's impossible to get your footing, and it gloms on to your boots. When it rains it is too treacherous for us to go hiking, but even as the bentonite is drying it can be very slippery.


But the rewards of hiking around this terrain are well, well worth it. It is almost impossible to walk around Dinosaur Provincial Park without finding at least some bone. The trick is finding stuff that is worth collecting - the volume of bone is so high that we cannot possibly collect all of it, so we need to be somewhat choosy in what we bring back to the university. (No hadrosaur caudal centra allowed, unless they are pathological!) The bones in this picture are the weathered remains of a hadrosaur. They were too far gone to collect, but we recorded their location with a GPS. We keep a database of uncollected dinosaur skeletons in the park, for understanding relative dinosaur diversity geographically and stratigraphically.


I was happy to find this nicely preserved ?fibula on the second day of fieldwork. Just a little piece of one end was showing, but it was obviously still going into the ground, so I decided to pick a little bit at it. I'm glad I did!


On my last afternoon in the park, we spent an hour or so prospecting in the marine Bearpaw Formation, which overlies the terrestrial Dinosaur Park Formation. I don't usually spend a lot of time looking in the Bearpaw, so this was neat for me. The Bearpaw is usually a dark grey shale, but at this spot in the prairie it is weathering out a bit reddish. You can see a couple of white chert nodules in the bottom left corner - these often had chunks of large ammonites, or sometimes clams or bryozoans!

Saturday, September 29, 2012

Ultimate ROM

This summer, the Royal Ontario Museum unveiled a brand-new exhibit all about the dinosaurs of Gondwana. When Pangaea rifted apart during the Triassic, it split into two continents - Laurasia, represented by the modern northern continents of North America, Europe, and Asia, and Gondwana, represented by the modern southern continents of South America, Africa, Australia, and Antarctica, plus India, Madagascar, and New Zealand. The dinosaurs and other extinct terrestrial vertebrates of Gondwana differed from their northern neighbours, and we don't often see them in exhibitions in North America.
 
Ultimate Dinosaurs: Giants of Gondwana features lots of interesting and sometimes obscure dinosaurs, some really great artwork, and some neat technological things (of which I am sometimes skeptical, but can wholeheartedly endorse here).
 
 
 
After a brief but informative introduction to plate tectonics, we're introduced to some of the earliest dinosaurs, like Herrerasaurus, Eoraptor, and the early ornithischian Pisanosaurus. In an exhibit that is definitely dominated by saurischian dinosaurs, it was neat to see this little fellow! Take note of the beautiful murals in the background, painted by Canadian palaeoartist Julius Csotonyi.
 
 
 
Ah, Cryolophosaurus. My second favourite dinosaur from Antarctica! ;)
This restoration of Cryolophosaurus definitely seems to have a more Dilophosaurus-y look to the skull, perhaps a result of recent phylogenetic analyses recovering a close relationship between the Antarctic taxon and other early, crested theropods.
 
 
 
As we move into the Cretaceous, the dinosaurs are arranged by geographic area on platforms. First off are African dinosaurs, including Malawisaurus, Nigersaurus, Carcharodontosaurus, and (shown here), Suchomimus.
 
 
 
I was super excited to see a mounted skeleton of Ouranosaurus, a bizarre sail-backed iguanodontian.
 
 
 
Ok, hands-down my favourite critter featured in this exhibition was one of the smaller skeletons, and not a dinosaur! I am sorry, dinosaur colleagues! But his adorable stubby tail and marvelous coat of osteoderms stole my heart. This is Simosuchus, a herbivorous crocodilian from Madagascar.
 
 
 
 I'll perhaps also add that the Madagascar 'pod' of Majungasaurus, Rapetosaurus, Masiakasaurus, and Rahonavis was probably my favourite part of the exhibition, just because I've never seen any of these taxa as mounted skeletons before, and because they're just so, so weird. Also, Majungasaurus just wants a hug, WHY DON'T YOU LOVE ME, RAPETOSAURUS?
 
 
 
I was very fortunate to get to see a lot of Patagonian dinosaurs last November during my visit to Argentina, but I'd never seen Austroraptor before. He is BIG! This 'pod' also features Buitreraptor, Carnotaurus, and Amargasaurus.
 
 
 
 
Although the dinosaurs are the main attraction, the main take-home messages of the exhibition are 1) continents move and 2) evolution happens. The dinosaurs are just the vehicle for delivering an exhibit that is actually all about the effects of plate tectonics on evolution, and I think that's awesome. Palaeogeography is prominently featured throughout the exhibition, and there's even an interactive team puzzle where you reassemble the continents into Gondwana. However, one of the most incredible things in the exhibit were the two giant Blakey palaeomap globes, animated to show the drifting of the continents. As you enter the exhibit, Pangaea breaks apart, and as you leave, the continents assemble into their current positions, and then keep going into the future! The video projections are staggeringly beautiful.
 
Honestly, I think this is one of the best dinosaur exhibits I have seen. It is bright, colourful, up to date, and packed with really good information not just about dinosaurs, but about broader themes in geology and evolution as well. Ultimate Dinosaurs is at the ROM for a limited time (I think until the end of 2012) and then it (hopefully!) goes on tour. GO SEE IT!

Friday, June 8, 2012

Thoughts on Tarbosaurus, Part 2

In my last post I talked about the role of museums in conserving fossil resources, with regards to the recent news about the Tarbosaurus auction. I wanted to address some of the other frequent comments I have seen on blogs and news articles. So, we’re now on to:

Comment 2: How do we know the tyrannosaur came from Mongolia? (and the related question, which I’ve decided to lump with this one: Why does the auction company, and subsequent news stories, refer to the specimen as Tyrannosaurus bataar while palaeontologists call it Tarbosaurus?


The first thing we need to address with these questions is the concept of ‘species’. In high school, most of us will have learned that a species is defined as a group of interbreeding individuals that can produce fertile offspring. This is called the Biological Species Concept. What many people may not know is that this is just one of many species concepts. Palaeontologists can’t go back in time to check on which dinosaurs were interbreeding, so the biological species concept can’t really be used in palaeontology. Instead, we generally use the Morphological Species Concept, which essentially boils down to ‘a species is a group of individuals that look like each other and not like others’.

Much of the arguing and debate in palaeontology results from the problems associated with the morphological species concept, and that is because individuals from the same species can look different from each other, and individuals from different species can look similar to each other. Biologists working on still living (‘extant’) animals need to worry about three main sources of morphological variation:
1.      Changes that occur during growth: An older individual of the same species can look different from a younger one.
2.      Sexual dimorphism: Males and females of the same species may look different.
3.      Normal individual variation: Individuals within a species can look different from each other because of normal variation resulting from small genetic differences and environmental differences. As an example, think about all the different dog breeds there are today. All dogs can interbreed (theoretically, although surely a Great Dane crossed with a Chihuahua must be pushing the limits of what is practical...) and produce fertile offspring, and belong to the same species, Canis familiaris. On top of that, all dogs are descended from domesticated grey wolves, and so many scientists regard them as a subset of the species Canis lupus. In taxonomic terms, this is called a subspecies, and we would write it as Canis lupus familiaris.



Palaeontologists need to add one more source of variation because we work with fossils, and that is:
4.     Changes that occur during fossilization (‘taphonomy’): Most fossils preserve only the skeleton, and so information from soft tissues like colour, integument, and muscles is lost. Skeletons become disarticulated, and individual bones get broken. All of this reduces the amount of information we have to work with. Finally, the remaining bones can become squished and distorted because of the extreme forces that occur as rocks form.

 Disarticulated Argali sheep skeleton in Mongolia, 2010.


Finally, it is important to remember that the natural world doesn’t always fit into discrete categories, and that the concept of species, genus, etc. is something that humans have created to help sort living things into workable categories. How many differences do two populations need to have in order to call them different species? How many differences until we split things into different genera? There isn’t really an answer to those questions, and so deciding on what are ‘species-level’ differences vs. ‘genus-level’ differences is the source of much debate.

But that’s ok, because that is a big part of what is fun about taxonomy and palaeontology!

So, moving on to Tyrannosaurus rex vs. Tyrannosaurus bataar vs. Tarbosaurus bataar. Tarbosaurus bataar and Tyrannosaurus rex have several morphological differences in the skull, but these are not necessarily obvious if you’re not accustomed to anatomical terminology or used to looking at skulls. Nevertheless, they are present, and there is an excellent, free to access paper in Acta Palaeontologica Polonica that you can go download right now to see for yourself. In a nutshell, the skull of Tarbosaurus is narrower than Tyrannosaurus when you look at it front on, and the nasal bones (the bones along the top of the snout) are domed near the front of the eyes. Additionally, the arms of Tarbosaurus are proportionately even shorter relative to the rest of the body than those of Tyrannosaurus, which are already pretty short.

Tarbosaurus bataar partial skull at the Palaeontological Institute in Moscow.


Tyrannosaurus rex skull at the Royal Tyrrell Museum in Drumheller, Alberta.



It’s pretty clear that Tarbosaurus bataar and Tyrannosaurus rex represent different species, because these differences are geographically separated. Small-armed, narrow-skull tyrannosaurs are only found in Mongolia, and longer-armed, wider-skull tyrannosaurs are found only in North America. You could make an argument that perhaps the differences are insufficient to warrant having two genera, in which case the genus Tyrannosaurus has priority over Tarbosaurus because it was named first. However, most palaeontologists accept both the genus Tarbosaurus and the genus Tyrannosaurus as being valid. So why did the auction house consistently call their skeleton Tyrannosaurus bataar? I can’t say for sure, but I suspect it is because Tyrannosaurus is much more a household name than Tarbosaurus, and this makes the skeleton more recognizable and interesting. It’s easier to tell someone your skeleton is a Tyrannosaurus than to do what I’ve just done here and explain how there is a similar, but different, tyrannosaur in Mongolia called Tarbosaurus.

So, we can look for anatomical features in the skull and skeleton that indicate whether or not the tyrannosaur was a Tarbosaurus or a Tyrannosaurus. But how do we know that the skeleton came from Mongolia? Well, much like certain animals today are found only in certain places, some dinosaurs were found only in some places and not others. Tarbosaurus has so far only been recovered from the Nemegt Formation, a set of rocks that are only known in the Gobi Desert of Mongolia. If the skeleton is shown to be a Tarbosaurus, and not some other species of tyrannosaur, then the conclusion we must come to without any additional information is that the specimen comes from Mongolia. We can also use the colour and preservation of the bones to identify where the skeleton came from, because different rock units will produce differently coloured fossils (in Alberta, dinosaur bones are often brown or black, and in Mongolia, they are often white or reddish).

If for some reason there was good evidence that the skeleton did not, in fact, come from Mongolia, that would only make the specimen more scientifically important, as it would extend the geographic or stratigraphic range of the genus Tarbosaurus and would give us important new information about that genus.


I had originally hoped to post this second part much sooner, and so much has transpired since my original Tarbosaurus post. I’m particularly pleased to see that a delegation of Mongolians and palaeontologists examined the auctioned Tarbosaurus this week as part of the investigation into the specimen. You can read their report at the Painter Law Firm's website. I also highly recommend this article at the Guardian by palaeontologist Dave Hone, and many thanks to Brian Switek at Dinosaur Tracking for his kind words about my first post in this series.

Literature!