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Posts Tagged ‘fossilicious’

We released a publication that, for me, comes full circle with research that started my career off. Back in 1995 when I started my PhD, I thought it would be great to use biomechanical models and simulations to test how extinct dinosaurs like Tyrannosaurus rex might have moved (or not), taking Jurassic Park CGI animations (for which the goal was to look great) into a more scientific realm (for which the goal is to be “correct”, even at the cost of beauty). “It would be great”, or so I thought, haha. I set off on what has become a ~26 year journey where I tried to build the evidence needed to do so, at each step trying to convince my fairly sceptical mind that it was “good enough” science. For my PhD I mainly focused on reconstructing the hindlimb muscles and their evolution, then using very simple “stick figure”, static biomechanical models of various bipeds to test which could support fast running with their leg muscles, culminating in a 2002 Nature paper that made my early career. I since wrote a long series of papers with collaborators to build on that work, studying muscle moment arms, body/segment centre of mass, and finally a standardized “workflow” for making 3D musculoskeletal models. And gradually we worked with many species, mostly living ones, to simulate walking and running and estimate how muscles controlled observed motions and forces from experiments. This taught us how to build better models and simulations. Now, in 2021, our science has made the leap forward I long hoped for, and the key thing for me is that I believe enough of it is “good enough” for me, which long held me back. This is thus my personal perspective. We have a press release that gives the general story for public consumption; here I’ve written for more of a sciencey audience.

Skeleton of the extinct theropod Coelophysis in a running pose, viewed side-on. Image credit: Scott Hocknull, Peter Bishop, Queensland Museum.

Stomach-Churning Rating: 1/10: just digital muscles.

Earlier in 2021, we simulated tinamou birds in two papers (first one here), the second one revealing our first ever fully predictive simulations, of jumping and landing; detailed here and with a nice summary article here. That research was led by DAWNDINOS postdoc Peter Bishop and featuring new collaborators from Belgium, Dr. Antoine Falisse and Prof. Friedl De Groote. Thanks to the latter duo’s expertise, we used what is called direct collocation (optimal control) simulation; which is faster than standard “single-shooting” forward dynamic simulation. The simulations also were fully three-dimensional, although with some admitted simplifications of joints and the foot morphology; much as even most human simulations do. The great thing about predictive simulations is that, unlike tracking/inverse simulations (all of my prior simulation research), it generates new behaviours, not just explaining how experimentally observed behaviours might have been generated by neuromuscular control.

OK, so what’s this new paper really about and why do I care? We first used our tinamou model to predict how it should walk and sprint, via some basic “rules” of optimal control goals. We got good results, we felt. That is the vital phase of what can be called model “validation”, or better termed “model evaluation”; sussing out what’s good/bad about simulation outputs based on inputs. It was good enough overall to proceed with a fossil theropod dinosaur, we felt.

Computer simulation of modern tinamou bird running at maximum speed. Grey tiles = 10 cm.

And so we returned to the smallish Triassic theropod Coelophysis, asking our simulations to find optimal solutions for maximal speed running. We obtained plausible results for both, including compared against Triassic theropod footprints and our prior work using static simulations. Leg muscles acted in ways comparable with how birds use them, for example, and matching some of my prior predictions (from anatomy and simple ideas of mechanics) of how muscle function should have evolved. The hindlimbs were more upright (vertical; and stiff) as we suspect earlier theropods were; unlike the more crouched, compliant hindlimbs of birds.

TENET: Thou shalt not study extinct archosaur locomotion without looking at extant archosaurs, too!
Computer simulation of extinct theropod dinosaur Coelophysis running at maximum speed. Grey tiles = 50 cm.

We observed that the simulations did clever things with the tail, swinging it side-to-side (and up-down) with each step in 3D; and in-phase with each leg: as the leg moved backward, the tail moved toward that leg’s side. With deeper analyses of these simulations, we found that this tail swinging conserved angular momentum and thus mechanical energy; making locomotion effectively cheaper, analogous to how humans swing their arms when moving. This motion emerged just from the physics of motion (i.e., the “multi-body dynamics”); not being intrinsically linked to muscles (e.g. the big caudofemoralis longus) or other soft tissues/neural control constraints (i.e., the biology). That is a cool finding, and because Coelophysis is a fairly representative theropod in many ways (bipedal, cursorial-limb-morphology, big tail, etc.), these motions probably transfer to most other fully bipedal archosaurs with substantial tails. Curiously, these motions seem to be opposite (tail swings left when right leg swings backward) in quadrupeds and facultatively bipedal lizards, although 3D experimental data aren’t abundant for the latter. But then, it seems beavers do what Coelophysis did?

Tail swings this-a-way (by Peter Bishop)
Computer simulation of extinct theropod dinosaur Coelophysis running at maximum speed, shown from behind to exemplify tail lateral flexion (wagging). Grey tiles = 50 cm.

The tail motions, and the lovely movies that our simulations produce, are what the media would likely focus on in telling the tale of this research, but there’s much more to this study. The tinamou simulations raise some interesting questions of why certain details didn’t ideally reflect reality: e.g., the limbs were still a little too vertical, a few muscles didn’t activate at the right times vs. experimental data, the foot motions were awkward, and the forces in running tended to be high. Some of these have obvious causes, but others do not, due to the complexity of the simulations. I’d love to know more about why they happen; wrong outputs from such models can be very interesting themselves.

Computer simulation of modern tinamou bird (brown) and extinct theropod dinosaur Coelophysis (green) running at maximum speed. Grey tiles = 10 cm for tinamou, 50 cm for Coelophysis.

Speaking of wrong, in order to make our Coelophysis walk and run, we had to take two major shortcuts in modelling the leg muscles. The tinamou model had standard “Hill-type” muscles that almost everyone uses, and they’re not perfect models of muscle mechanics but they are a fair start; it also had muscle properties (capacity for force production, length change, etc.) that were based on empirical (dissection, physiology) data. Yet for our fossil, because we don’t know the lengths of the muscle fibres (active contractile parts) vs. tendons (passive stretchy bits), we adopted a simplified “muscle” model that combined both into one set of properties rather than more realistically differentiating them. It was incredibly important, then, that we try this simple muscle model with our tinamou to see how well it performed; and it did OK but still not “perfect”, and that simple muscle model might not work so well in other behaviours. That was the first major shortcut. Second, again because we don’t know the detailed architecture of the leg muscles in Coelophysis, we had to set very simple capacities for muscular force production: all muscles could only produce at most 2.15 body weights of force. This assumption worked OK when we applied it to our simulation of sprinting in the tinamou (vs. average 1.95 body weights/muscle in the real bird), so it was sufficiently justifiable for our purposes. In current work, we’re examining some alternative approaches to these two shortcuts that hopefully will improve outputs while maximising realism and objectivity.

Computer simulation of extinct theropod Coelophysis running at maximum speed, shown alongside running human (at 4 m/s) for scale and context. Image credit: Peter Bishop.

If you pay close attention, our simulations of Coelophysis output rather high leg-forces, and it’s unclear if that’s due to the simple muscle model, the simple foot modelling, or is actually realistic due to the more vertical (hence stiff) hindlimbs; or all of these. Another intriguing technical finding was that shifting the body’s centre of mass forwards slowed down the simulation’s running speed, as one might expect from basic mechanics (greater leg joint torques), but unlike some prior simulations by other teams.

Computer simulation of extinct theropod Coelophysis shown alongside running human for scale and context. Shown from above to illustrate tail wagging behaviour. Image credit: Peter Bishop.

Users of models and simulations are very familiar with catchphrases like “all models are wrong, but some are useful” or the much more cynical (or ignorant) “garbage in, garbage out”; or the very dangerous attitude that “if the mathematics is correct, then the models can’t be that wrong” (but if the biology is wrong, fuggedaboutit!). These are salutary cautionary tales and catechisms that keep us on our toes, because the visual realism that realistic-looking simulations produce can seduce you into thinking that the science is better than it is. It’s not a field that’s well-suited for those fearful of being wrong. I’ll never think these outputs are perfect; that is a crazy notion; but today I feel pretty good. This was a long time coming for me, and it is satisfying to get to this stage where we can push forwards in some new directions such as comparing simulations of different species to address bigger evolutionary questions.

The wrestling with scepticism never ends, but we can make progress while the match goes on.

from WWE… I could not resist

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The blog is back! Briefly. With dinosaurs. Back in 2005, I published a paper in which I used a “SIMM” 3D musculoskeletal biomechanical model of Tyrannosaurus rex to analyse its muscle actions and infer a relatively upright hindlimb pose. This was an outcome from my NSF-funded postdoctoral research at Stanford University, in which engineers kindly taught me how to use SIMM (handing me a loaded gun?). Part of my plan all along was to build multiple such models along a rough evolutionary sequence to revisit old questions I had with past, qualitative functional morphology papers from 2000 onwards, and see if biomechanics could quantitatively reveal more about the functional evolution of dinosaur hindlimb muscles. So I got data for modelling some extinct dinosaurs (theropods Dilophosaurus, Allosaurus, Velociraptor) and living birds (Struthio, others) and published nuggets of that but held others back…

Stomach-Churning Rating: -1/10; dinosaurs!

I handed these 3D model data off to my PhD student Vivian Allen in ~2007, charging him with the task of making more models to flesh out the phylogeny and finish what I’d started. And he sure did. He graduated, did a couple of postdocs with me, and we gradually massaged his thesis chapter on this topic into a draft paper. Easier said than done, though! That’s why 14 more years have passed.

Viv came up with some clever tools in MATLAB software code (from which he became a very competent programmer and went on to a successful career in that!) to boil complex data on muscle leverages (moment arms) across a wide range of joint motion for the hindlimbs for each taxon.

These data then were fed into further code that took the results from all models, ultimately 13 of them from an Australian freshwater crocodile to two living birds and 10 extinct dinosaurs plus close cousin Mara/Lagosuchus (Figure 1). The code expressed these leverages as changes in ancestral values along the main branch of the evolutionary tree from early (Triassic) “ruling reptile” Archosauria (represented here just by the croc as a proxy) to modern birds, and 9 main ancestral “nodes” in between. Our code tracked both how each of 35 hindlimb muscles we modelled evolved in its leverage, as well as overall “average” leverage of functional groups around the hip, knee and ankle joints.

So, back and forth we went for some 10 years playing with the models (see Video below), data and code, and the paper describing the whole thing, slowly closing in on a final version but also sometimes distracted by our other projects and Real Life Stuff like health and children, and concerns about how we conducted this study (i.e. a lot of fiddling).

Figure 1: Evolutionary tree of dinosaurs and their relatives as used in the study, showing all 13 models, species names, and names of groups along the bottom (red nodes) of the tree. Averostra and Avetheropoda were ancestral groups of theropod dinosaurs that the study inferred had particular specialisations of the hindlimb muscles. Right hindlimbs in side view. The limbs are all straightened vertically into a baseline reference posture but the study investigated variation in muscle function across a wide range of limb poses.

Then I got a new grant “DAWNDINOS” that changed the scene for me, refocusing my team’s energies onto the Triassic (and early Jurassic) and the evolutionary biomechanics of diverse archosaurs’ locomotion, assessed with both LOTS of experimental studies of living crocs and birds, and LOTS of predictive simulations of locomotion. Stay tuned for much more on that from our team, but we’ve already published some key steps here. Most notably, we developed an improved protocol for modelling and simulating our animals, as shown by Bishop et al.’s 2021 study of the early theropod Coelophysis bauri (also appearing in the current paper). Awkwardly for me, that new method rendered our old models and methods a bit obsolete (although still fine), so I pushed to publish this current paper with Viv, and brought collaborator Dr. Brandon Kilbourne on board to aid in some final stats, figures and more. That finally did it, and now we’ve published the paper in Science Advances. Deep breath.

Video: Rotating movies of 3 musculoskeletal models from this study. Models have been posed into representative limb orientations illustrating a gradual or stepwise transformation from more upright to more crouched.

Well what’s the paper about, then? We used our 13 models and processed evolutionary functional patterns to test three main questions (hypotheses) about muscle leverage, making educated guesses at what might prevail from early Archosauria to Aves:

  1. Hip extensor / flexor (i.e. femur retractor/protractor) moment arm ratios remained constant. We weren’t sure what to expect, as these antagonists both seem to change a lot on the whole lineage, so we went with this prediction.
  2. Knee flexor / extensor ratios decreased; i.e. the flexors (“hamstrings” etc.) weakened and/or extensors (equivalent of our quadriceps) strengthened their leverage. Anatomy of the knee joint and muscles around it suggests this, plus since Gatesy’s 1990-onwards studies we’ve expected archosaurs to shift from more ‘hip-based’ to more ‘knee-based’ locomotion as we get closer to avian ancestry.
  3. Hip medial (internal) long-axis rotator / abductor (i.e. pronators of the limb vs. those that draw the leg away from the body) ratios increased. This idea comes right from my paper w/Gatesy in 2000, where we surmised that archosaurs shifted from relying on hip adductors (in crocs/other quadrupeds) to abductors (in bipedal dinosaurs; like humans) to medial rotators (‘torsional control’ as in birds today) during weight support.

Moreover, we reconstructed the evolution of 35 muscles’ actions across ~250 million years, which was a new step.

Here’s a summary of what we found (Figure 2):

Figure 2: Short visualization/explanation of the study’s main insights. Pictures by palaeoartist Jaime Headden: https://qilong.wordpress.com/about/ in left side view, including “muscled” and silhouette images. Right side images include representative hip, knee and ankle muscles from the study. Changes such as the enlargement of muscles in front of the hip that straighten the knee, and reduction of the caudofemoralis longus muscle that runs from the tail to the back of the thigh, are evident.

So, overall hypothesis 1 about hip extensors/flexors ended up complicated; rejected because hip flexor leverage actually increased. Furthermore, we found that around the ancestral nodes for early theropod dinosaurs (Neotheropda through Avetheropoda; around 200 Mya), there were peaks in muscle leverage (size-normalized) that surprised us, and persisted despite many different analyses we threw at them over the years. As far as we could tell, these peaks that kept appearing for various muscles’ actions were “real” (estimates). Which meant these ancestors may have had specialised high leverage relative to both their own ancestors and descendants; the peaks got reversed in evolution. These ancestors had some other weird anatomical and functional traits, such as tightly articulated hip joints early on (which they lost later), increased body size in the later forms, more ‘macropredatory’ ecology (e.g. eating sauropods?), and a centre of mass of the body that was shifted forwards (due to big arms and heads/necks). This weirdness is a cool unexpected finding that showed up for the other hypotheses too, and it needs some more investigating. A ‘failed’ hypothesis test led to neat insights.

Figure 3. From the paper– showing our main results for changes in moment arm ratios across archosaurian ancestors. Hip extensors/flexors decreased then increased; knee flexors/extensors decreased; and hip medial rotators/abductors decreased then had a series of increases.

Hypotheses 2 and 3 found good support, on the contrary, overall (Figure 3). We seem to have been able to quantify the shifts from hip-based to knee-based, and abductor-based to medial-rotator-based, muscle actions. I find that very satisfying. Ankle weight support (extension) capacity also increased, which fits morphological changes fairly well. If you’re into archosaur limb muscle form and function, there’s a lot more food for thought in the paper.

Funnily enough, ~20 years has been sufficient time that we could have had plenty more models in this study if we’d delayed it even longer and re-re-re-analysed our data. But we had to draw the line somewhere and not infinitely revise with every new model we’ve been creating. With the current state of musculoskeletal modelling in my group, we could have more than doubled our sample size and fleshed out the most important gaps such as in the crocodile-lineage (extinct Pseudosuchia) and other Triassic forms plus elsewhere. A big challenge remains having some nice 3D-preserved early fossil birds beyond Archaeopteryx; e.g. so many nice Chinese ones are too flat (e.g. joints we need) to reliably model here. It’s something that can still be done and is worth doing, but I suspect the general trends we’ve found along the dinosaur lineage are “correct”.

What’s personally important to me about this paper is (1) how it not only bridges a huge morphofunctional gap across archosaur evolution in scientific terms, and (2) how we’ve completed a long-delayed project with stubbornness (and during a pandemic!), but also (3) how it bridges my past career from my PhD and postdoc to the present work with DAWNDINOS. We’re now forging well beyond what this new paper has done in terms of truly testing, as best we can (estimate) so far, how limb muscles of archosaurs functioned and evolved, and how these contributed to particular behaviours and performance (maybe even palaeoecology and evolutionary success/extinction?). The current paper is just simple modelling of muscle leverage, but leverage is only one (very important!) piece of muscle function and performance. With fully dynamic, anatomically integrative, physiologically and physically representative biomechanical computer simulations that predict what living and extinct archosaurs could or could not do, we can do even better. So watch for that! Hopefully it won’t all take 20 years, or 250 million.

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Our special guest post this week comes from Dr. Liz Clark of Yale University in New Haven, Connecticut, USA. She continues to bring biomechanics-fu to echinoderms– the weird marine critters like seastars and sea urchins. Including fossils, as you’ll see today! You may remember her from blog posts such as “Guest Post: Brittle Star Arms Are Weird“.

Stomach-Churning Rating: 1/10; echinoderms are inoffensive.

Imagine that you’re stuck in a cardboard box on the beach, holding a small stick. Could you use the stick to move yourself forward? What would you do? You could try digging into the sediment ahead of you to pull yourself along. You could try rowing side to side, as if you were in a rowboat. Or maybe it’s not possible and you’d give up, decide to stay put, and wave your stick in the air for help.

Believe it or not, this is a strange-but-important dilemma that some paleobiologists- like me!- have been wrestling with for generations. My research specialty is in the biomechanics of locomotion– how organisms use their bodies to get from one place to the next (through walking or swimming, for instance). We can learn a lot about an animal by studying their locomotion, such as why their body is shaped the way that it is, or what role they occupy in their ecosystem. Animal motion is a major inspiration for robotic design, and I work with engineers to apply the novel insights on animal locomotion from my research to create new kinds of devices.

Studying the biomechanics of motion in living organisms is (relatively) straightforward. We can use high-speed cameras, motion capture software, and 3D imaging tools to visualize and understand how organisms move in real-time, informing our inferences about how they perform certain tasks. Inferring locomotion in fossil organisms, on the other hand, is tricky since we can’t observe the organism’s behavior like we could if the organism were alive. Instead of being able to watch the organism move, we’re left with a snapshot of the animal frozen in place in a rock. We’re also missing a lot of physical information: locomotion in most animals requires soft tissue and hard skeletal structures, but typically with fossils, only the hard structures get preserved.

However, we can often garner some insights from living organisms to determine the locomotion strategies that fossil organisms use. Most organisms in the fossil record look at least somewhat similar to organisms alive today. If our fossil has four legs, for instance, we can study locomotion in living tetrapods (four-legged animals) to help us create a framework for deriving inferences about locomotion in our extinct tetrapod fossil animal. But for some really strange-looking animals- ones without obvious modern analogues- we’re not so lucky. For me, this is where the fun begins.

Figure 1: Stylophorans! Here are four fossilized stylophorans from the Helderberg Group of the Early Devonian (YPM 036413)

So getting back to the cardboard box and the stick. These are metaphorical examples of the different locomotion strategies that have been proposed for a group of fossil animals known as stylophorans (Figure 1). Stylophorans are extinct organisms related to sea stars and sea urchins, but with a body structure unlike any organism on the planet today. They have a large, relatively flat body called a theca (i.e., the cardboard box), and a long, thin segmented tail known as the aulacophore (i.e. the stick) (Figure 2). They’re known in the paleontological community as some of “the strangest-looking animals of all time.”

Figure 2: Stylophoran anatomy. The “theca” is the body cavity, and the “aulacophore” comprises of the proximal aulacophore, the stylocone, and the distal aulacophore.

By reconstructing stylophoran locomotion, we can unlock the mechanics of a unique system for motion and its potential applications to engineering. We can also understand more about how this organism lived and functioned in its ancient ecosystem. And, by developing a new approach to understand locomotion in stylophorans, we can apply this strategy to analyze locomotion and movement in other unusual fossil animals as well!

For years, scientists have been documenting the incredible array of stylophoran diversity in the fossil record and making their best predictions about how they would have been able to move (or not!). These predictions are based on their morphology– the structure of an organism’s body. For stylophorans, that means the shape and structure of the theca and aulacophore. There are a variety of stylophoran thecal shapes, ranging from ovoid in Enopleura to trapezoidal in Ceratocystis to almost crescent-shaped in Cortnurnocystis. There’s a similarly wide array of aulacophore morphologies as well.

Figure 3: Left: One half of the concretion within which the stylophoran fossil we analyzed is preserved. Right: The 3D digital image of the stylophoran fossil, created by micro-CT scanning the fossil specimen.

We developed a new approach using 3D imaging (Figure 3) to create a digital model of a stylophoran specimen. We used the model to test if several different locomotion strategies that had been proposed before were physically possible or impossible for a stylophoran to actually perform.

First, we used a micro-CT scanner to image a fossil stylophoran. This outputs a digital 3D picture of the stylophoran fossil that we can look at and analyze on a computer. Next, we developed a program to calculate the joint centers- the point at which one skeletal structure rotates relative to another-within the digitized stylophoran’s aulacophore (Figure 4). This created a digital marionette– a rig of our stylophoran fossil that flexes at the junctures between aulacophore segments as it would have in life. We then rotated each segment at the joint center to calculate the aulacophore’s total range of motion– a reconstruction of how far the aulacophore could flex in each direction (Figure 5).

Figure 4: A look into some of the nuts and bolts of the 3D model we created. Tri-colored axes demarcate where the joint centers are in the proximal aulacophore. 

We used this 3D range of motion model to evaluate several locomotion strategies that had been previously hypothesized for this group of stylophorans. One hypothesis suggested that these stylophorans dug their aulacophores into the substrate– sediment on the ocean floor- to pull themselves forward. Another suggested that they moved the aulacophore side to side in order to push themselves along. We found that the first hypothesis would have been impossible to conduct based on the range of motion we calculated, but the second strategy was theoretically possible! We’ll need to do more work to see how likely it was that stylophorans would have actually used this technique. Nevertheless, through this investigation, our team produced the first objective, data-driven methodology for analyzing locomotion in fossil invertebrates, which is a big step in the right direction for the study of fossil invertebrate biomechanics! Our technique can be applied to study other organisms with rigid skeletons as well, like crabs, insects, or sea stars, for instance, and we’re looking forward to seeing our technique used to uncover more interesting locomotion strategies!

Figure 5: A snapshot of the 3D model where we can observe how dorsal and ventral range of motion compare to the originally preserved orientation of the aulacophore (highlighted in green).

Do you want to know more? You can! We published a paper on this topic here!

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Ho ho ho! The vagaries of the scientific publication system today brings forth TWO open access papers on crocodylian functional anatomy, evolution and biomechanics, from my team with others’; including our DAWNDINOS project in part. Get ready to bite down on the science! I’ve loved crocodylians throughout my life– “dacadile” was among my first words, for a beloved stuffed croc toy, and “Alligators All Around” was an early favourite song (it’s still GREAT).

One of the many large adult alligators in St. Augustine, Florida.

Stomach-Churning Rating: 1/10; bones and movies of awesome behaviours.

First, I am so relieved and pleased to finally publish an experimental study I began over 17 years ago. This is my most-delayed paper ever, due to my own perfectionism, overcommitment and failures at funding it more broadly. But published is published and I’m glad to see it out. We collected a large experimental dataset from 15 species of Crocodylia at the St Augustine Alligator Farm Zoological Park (a conservation/education centre) in Florida. (No matter how you species-ify them, that’s a good chunk of diversity; roughly half or more.) This was a non-invasive study of 42 individuals ranging from 0.5 to 43 kg in body mass (hatchlings to adults). Larger adults were too dangerous or too slow to work with. It took 3 years (2002, 2004, 2005) of data collection to assemble this, with some twists and turns (including a close brush with Hurricane Katrina), and then a lot of analysis and reanalysis; and I’d do it all very differently if I did it today but that’s a moot point. So what’s the paper about?

Adorable Siamese crocodile family “cuddling”. Crocs are great parents! IIRC, that is the father shown.

Some Crocodylia (the inclusive modern name for all crocs, caimans, gharials, gators) are known to use what we call asymmetrical gaits: “mammal-like” footfall patterns in which the left and right limbs do not move as mirror images of each other. In particular, these gaits include galloping (rotary or transverse; either way a “4-beat” pattern with left-right hind- followed by right/left forefoot contacts) and bounding or half-bounding (the former being the most extreme, with left-right hind- and then forefoot contacts as synchronous pairs). Often people just say that crocs can “gallop” but this confuses/conflates the issue and omits that they can use these faster bounding gaits. Regardless, we’ve known about these gaits at least since HB Cott’s 1961 photographic documentation of them in Nile crocodiles; and more detailed studies of Australian freshwater and saltwater crocodiles in the 1970s-2000s. But very often, scientists and popular natural history accounts ascribe the asymmetrical gaits to only a few species or young individuals.

“Freshie” croc bounding in the wilds of Australia; credit Kent Vliet.

Osteolaemus dwarf African crocodile getting marked up for study.

That’s where we came in. We had access to a huge collection of captive Crocodylia and a very supportive institution (with coauthors from there as a result). I wanted to know which Crocodylia do use asymmetrical gaits, having a very strong suspicion from the literature that Alligatoroidea, the alligator and caiman lineage, don’t use them, whereas their cousins the “true crocodiles” in Crocodyloidea do. And I wanted to test how body size interacted with this ability, as prior accounts hinted that asymmetrical gaits got lost with increasing size or in adults. Finally, I was interested in what the benefits of asymmetrical gaits were– did they give those that used them marked boosts in performance, especially maximal speed? Answering that would help understand why these gaits are used.

Cuban crocodile Crocodylus rhombifer in preparation. A gorgeous but aggressive species that we handled carefully.

So we walked and ran our subjects across some platforms past video cameras and collected about 184 useful trials or strides of gait across level ground at a wide range of speeds; and a LOT of not-so-useful data (mostly subjects just sitting and pouting). We found that, yes, most Crocodyloidea we studied could bound or gallop; and no Alligatoroidea did. In the latter case, we didn’t use as large a sample of subjects as we could have, partly because it already seemed evident that alligators did not use asymmetrical gaits, and partly because those alligatoroids we did try to coax to move quickly either only used symmetrical gaits (e.g. trotting) or would only sit and fight or hiss. And we found that bigger animals moved at least relatively more slowly and less athletically, and perhaps even more slowly in absolute terms (metres/second).

Most intriguingly to me, it didn’t matter what gait alligatoroids or crocodyloids used. They all could move at roughly similar top speeds if they wanted to; less than 5 m/s or 11 mph. It’s just that crocodyloids tended to use asymmetrical gaits, especially bounding, at top speeds– but not always: some even chose to trot at their top speeds. We don’t know why, and we still don’t know why asymmetrical gaits are chosen but they likely have other benefits such as acceleration and manoeuvrability.

It’s a thrill to finally be able to share the huge dataset, including a gigantic file of videos (with some highlights shown here), with the paper, closing this study at last. It should be very useful to anyone studying Crocodylia or wanting to educate people about locomotion. I’m a bit tired of hearing that galloping is a mammalian behaviour when we know so well that many species of animals do it, or something like it. And it was absolutely thrilling to see five species of Crocodylia bound or gallop when they hadn’t been properly documented to do it before– enough anecdotes, here’s cold hard facts from video on what happens. What remains is a mystery: did Crocodylia have this ability to use asymmetrical gaits as an ancestral trait, as almost everyone assumes (and thus alligators and caimans have lost or essentially never express the ability), or did crocodiles uniquely evolve this ability more recently? I would join most scientists in wagering on the former; and there are good reasons to suspect the ability goes deeper into extinct Crocodylomorpha.

(my favourite video is below!)

Want more cool videos? Try my Youtube channel— or if you want ALL of the videos, go here!


Next, Torsten Scheyer was kind enough to invite me to join his team in studying a fossil I’ve long been fascinated by: the “giant caiman” Purussaurus mirandai, from the Miocene (~6 million years ago?) of Venezuela, in the Urumaco Formation‘s very weird biota. Purussaurus has been known of for >125 years but Torsten’s team noticed that Purussaurus (mirandai) specimens tended to add one of their trunk vertebrae to their hip girdles (sacrum; normally only two vertebrae in Crocodylia but here three), and that the shoulder and hip girdles had unusual bone morphology (straighter, more vertical relative to the body). So they asked me to help interpret these features. And here’s the paper!

Infographic by Torsten Scheyer’s team– click to emcroccen!

Three-vertebra sacrum and other traits of Purussaurus; with living caiman bones for comparison. E (bottom): inwards-facing femur head. (see paper for more info)

It became evident that, together, those odd traits conveyed a signal that the skeleton was transformed to aid in supporting the huge body against gravity. For example, I found it quite interesting how the head of the femur (thigh bone) was oriented more directly into the hip socket in multiple specimens, more like a dinosaur’s hip, and specialised for support and fore-aft motions. I used Haley O’Brien et al’s data to estimate just how big P. mirandai might have been and it came out as perhaps 3000 kg and 8 metres total length; as we’d thought, among the largest Crocodylia (and there are larger Purussaurus known, too).

Reconstruction of Purussaurus and morphology of the girdles. (see paper for more info)

The team also put a cool “evo-devo-biomechanics” spin on the study. It is well known that the regional identities of vertebrae (e.g. neck, trunk, sacrum, tail) are largely determined by Hox (homeobox) regulatory genes, early in development. So changes of vertebral identity intimate changes of genetic controls. Crocodylia don’t normally add a trunk vertebra to their sacrum, and only a few fossil crocodyliforms (extinct cousins) ever did either, but we noticed that some specimens of Crocodylia would at least partially make this transformation in pathological states (below). Hence the controls to make these changes exist and sometimes manifest in living crocs, but it’s probably not an “easy” transformation to achieve. One could speculate that under intense selection, such as that imposed by giant body size and some degree of activity on land, that transformation could more easily get permanently “fixed” in a species.

Palaeosuchus palpebrosus (Cuvier’s dwarf caiman) with pathological partial-three-vertebra-sacrum; and lots more morphology. (see paper for more info)

As a nice tie-in to the asymmetrical gait study above, we can safely infer that the giant Purussaurus wasn’t a fast animal on land, by any means. But its skeleton is consistent with it having found novel ways to maintain the ability to stand and move on land, even if slowly.

Happy holidays! Santa Jaws is watching you– be good!

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If you go into central Lausanne, Switzerland, you’re likely to pass the Palais du Remine, and if you do, I recommend you go inside. I was happy I did while visiting Lausanne for the AMAM2019 conference. A luxurious palace has been given over to house five (!) free (!) museums on science and culture. These include the canton’s (~state’s) museums of palaeontology and zoology, which I’ll showcase here (also a little of geology and archaeology museums). Tripadvisor’s reviews were good but not as glowing as I’d make mine, so I will remedy that. I’m a sucka for old-school museums, and that’s what these are. So if that sounds right for you, journey onward!

It’s nice.

As you may be expecting by now if you’ve been here before, it’s time for another museum photo blog!

Stomach-Churning Rating: 5/10 for bones, preserved organs, taxidermy aplenty, and animal developmental deformities.

Nice cathedral nearby, w/great view of the city.

Nice interior architecture. There’s lots of nice to behold.

Posters That Get You Excited 101. But you must wait. Like I did.

Quadrupedal human at Zoology museum entry.

Tomistoma, false gharial.

Not a bad collection of taxidermied Crocodylia!

Visually arresting cobra display.

I’ve never seen three Draco gliding lizards on display together!

Bipedal lizard taxidermy displays, freezing the dynamic in the static, are no easy feat.

Plenty of stuffed animals like these raptors/other large birds. Classical zoology museum style. Minimal signage. Just specimen labels, mainly.

Coelacanth!

Sperm whale jaw.

Open space with big specimens. A ~4m long great white shark included.

Second zoology hall: bones!

Gorilla standing tall next to human.

Ostrich skeleton up close, amongst the mammalz.

Cassowary skeleton.

Emu shoulder/arm bones in right side view.

Walrus skeleton in what seems like an odd pose to me, but then they are odd on land.

Alligator skeleton in repose.

Giant anteater, “knuckle-walking”.

Pangolin skeleton! And mounted digging into a nest– very well done!

Bernard Heuvelmans display, about the (in)famous cryptozoologist. This was quite a surprise to me. I’m sure I’d read his English-translated book “On the Track of Unknown Animals” as a kid, during my long stint as an avid reader of much zoology, crypto- and otherwise. He bequeathed a lot of his work to the museum.

Bernard’s handwritten CV!? With a “sea serpent” sketch.

A “sea serpent” vertebra… but if you know any anatomy, it’s not a snake’s vertebra at all but a fish’s, such as a basking shark‘s.

Are you ready for more weirdness? How about some “mutants”- congenital deformities of animals? Fascinating errors of developmental anatomy… somehow this two-headed calf survived awhile. Plenty more where that came from, as follows:

And then there’s all kinds of wonderful comparative anatomy. To be a student of this subject in Lausanne would be a lucky thing, with this museum’s collection at hand. These are valuable specimens, made with love and skill.

Jaws

Fish head anatomy. Some vertebrae on the left, too.

Developmental regions of the head: a lovely wax(?) model of an Echidna skull. A treasure.

Brains: alligator vs. pigeon.

Salamander muscles.

Pigeon muscles.

More spotted felids than you can shake a jar of catnip at.

Another pangolin!

Giant armadillo.

Petaurus: flying phalanger (a gliding marsupial).

Second zoology hall open area: left side.

Second zoology hall open area: right side.

A final hall with a more new-fangled display, on the topic of evolution and extinction. Attractive phylogeny graphic here. Birds at the “top”, of course. Poor lowly mammals!

Taxidermied giant auk- not a common sight! (Extinct)

The extinct southern pig-footed bandicoot. Also a rare sight of a whole specimen- in a Swiss museum, too.

NOW ON TO THE FOSSILS!

You’ve been very patient. Here, have a Toblerone.

Palaeo museum entry. Already there are cool things visible. Inside, we find it just like I prefer my zoo/palaeo museums (as above): stuffed with specimens and leaving plenty for you to wonder about and investigate. Not frilly; a well-stocked museum that mostly lets its specimens speak for themselves.

Sauriermuseum (Aathal) specimen of Plateosaurus: sculpt/cast. A very good, big skeleton of this common dinosaur, rearing up.

Rear view of same.

Real bones of same; vertebrae and pelvic (this is the “Frick specimen”).

Metaxytherium (current name), an ancient and large fossil dugong/seacow. Skull is in left side view. (that may help, as their skulls are odd!)

Anthracotherium upper jaw: ancient hippo-cousin.

Prolagus: the “Sardinian hare” (recently extinct; old lineage).

Potamotherium: to some an early otter-like mammal, more recently thought to be an ancient seal.

“Broke-ulum”: a walrus broke its penis bone (baculum) and was surely not pleased about it, but lived to heal— physically if not mentally. Yeesh!

Glyptodont tail club and armour.

Aepyornis elephant bird legs!

A partial/reconstructed skeleton of the dodo.

Velociraptor preparing to pounce from above. It’s too late for you!

Rhamphorhynchus fossil (2D slab) and sculpt/cast coming alive in 3D– good stuff.

Anhanguera pterosaur watches the chaos from above, fish snagged in its teeth.

Not-shabby metriorhynchid marine croc fossils, from Britain.

Lovely 3D plesiosaur bones (flippers, neck, etc.) from near RVC: Peterborough!

Mesosaur; early reptile.

The museum clearly is proud of its excellent “Mammoth of Brassus” skeleton, essentially complete.

Ice Age elk/moose, a 10,000 year old skeleton in fine shape.

Cave bear skull rawr

Purty ammonites!

Spiky ammonite!

Cretaceous sponge colony from France. I hadn’t seen something like this before, so here it is.

Trilobites, brittlestars and friends.

Well I did wander through the geology and archaeology museums too, and while I liked them I did not take so many photos. My non-human organismal bias is apparent. But check these final ones out:

Splendid cross-section of the stratigraphy of the Alps around Lausanne. I gazed at this for quite a few minutes, trying to figure out what was where in the landscape I’d seen and how old, how deformed, etc.

Slab of “dinosaur” tracks but it was not clear to me what dinosaurs/archosaurs/whatever made them. I wish my French was better. Closeup below shows two footprints superimposed.

At last, the coup de grace! What museum would be complete without a diorama!? (I love them) This one, with a goat sacrifice and early Stone Age people praying to heathen deities/spirits at an elaborate petroglyph array rocked my world. And so it makes a perfect final image. Enjoy, and conduct the proper rites.  \m/

 

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To me, there is no question that the Galerie de Paléontologie et d’Anatomie comparée of Paris’s Muséum national d’Histoire naturelle (MNHN) is the mecca of organismal anatomy, as their homepage describes. Georges Cuvier got the morphological ball rolling there and numerous luminaries were in various ways associated with it too; Buffon and Lamarck and St Hiliaire to name but a few early ones. It is easy to think of other contenders such as the NHMUK in London (i.e., Owen), Jena in Germany, the MCZ at Harvard (e.g. Romer) and so forth. But they don’t quite cut the dijon.

As today is John’s Freezer’s 7th blogoversary, and I was just at the MNHN in Paris snapping photos of their mecca, it’s time for an overdue homage to the magnificent mustard of that maison du morphologie. The exhibits have little signage and are an eclectic mix of specimens, but this adds to its appeal and eccentricity for me. I’ve chosen some of my favourite things I saw on exhibit on this visit, with a focus on things that get less attention (NO MESOZOIC DINOSAURS! sorry), are just odd, or otherwise caught my fancy. It’s a photo blog post, so I shall shut up now, much as I could gush about this place. I could live here.

Need plus-grand images? Clic!

Stomach-Churning Rating: 7/10 for some potentially disturbing anatomical images such as viscera, preserved bits, models of naughty bits etc.

Greetings. Note the stomach-churning rating above, please.

Right. We’ll get the amazing first view as one steps into the gallery done first. Mucho mecca. Anatomy fans simply must go here at least once in their life to experience it, and one cannot ever truly absorb all the history and profound, abundant details of morphology on exhibit.

Less-often-seen views from the balcony; one more below.

Indian Rhinoceros from Versailles’s royal menagerie; came to the MNHN in 1792.

Brown bear hindlimb bones.

Brown bear forelimb bones and pelvis.

Two baby polar bears; part of the extensive display of ontogeny (too often missing in other museums’ exhibits).

Asian elephant from Sri Lanka.

Lamb birth defect. Like ontogeny, pathology was a major research interest in the original MNHN days.

Wild boar birth defect.

Fabulous large Indian gharial skull + skeleton.

“Exploded” Nile crocodile skull to show major bones.

Let’s play name-all-the-fish-skull-bones, shall we?

Rare sight of a well-prepared Mola mola ocean sunfish skeleton.

Diversity of large bird eggs.

Asian musk deer (male), with tooth roots exposed.

Freaky gorilla is here to say that now the really odd specimens begin, including the squishy bits.

Freaky tamandua, to keep freaky gorilla company. Displaying salivary glands associated with the tongue/pharynx. These are examples of anatomical preparations using older analogues of plastination, such as papier-mâché modelling. I’m not completely sure how the preservation was done here.

Tamandua preserved head, showing palate/tongue/pharynx mechanism.

Chimp ears. Because.

Why not add another chimp ear?

Many-chambered ruminant stomach of a sheep.

Simpler stomach of a wolf. Not much room for Little Red Riding Hood, I’m afraid.

Expansive surface area of a hippo’s stomach; but not a multi-chambered ruminant gut.

Cervical air sacs of a Turquoise-fronted Amazon parrot.

Heart and rather complex pulmonary system of a varanid lizard.

It’s pharynx time: Keratinous spines of a sea turtle’s throat. All the better to grip squids or jellies!

Pharynx convergent evolution in a giraffe: keratinous spines to help grip food and protect the pharynx from spiny acacia thorns while it passes down the long throat.

Tongue/hyoid region of the pharynx of a varanid, showing the forked tongue mechanism.

Palaeontological awesomeness on the upper floor (the 2nd part of the gallery’s name). Here, the only Siberian woolly mammoth, I’m told, to have left Russia for permanent display like this. Frozen left side of face, here, and 2 more parts below.

Mammuthus primigenius freeze-dried lower ?left forelimb.

Skeleton that goes with the above 2 parts. It’s big.

But “big” is only relative- my large hand for scale here vs. a simply ginormous Mammuthus meridionalis; full skeleton below.

Four-tusked, moderate-sized Amebelodon elephantiform.

Naked woolly rhinoceros Coelodonta.

Extinct rhino Diaceratherium, with a pathological ankle (degenerative joint disease). I love spotting pathologies in specimens- it makes them stand out more as individuals that lived a unique life.

Glyptodont butt and thagomizer, to begin our tour of this business-end weaponry.

Eutatus leg bones, from a large fossil armadillo; Argentina. Really odd morphology; Xenarthrans are so cool.

Giant ground sloth (Megatherium) foot; ridiculously weird.

Giant ground sloth hand is full of WTF.

Metriorhynchus sea-crocodile from the Cretaceous: hind end.

Odobenocetops one-tusked whale that I still cannot get my head around, how it converged so closely on the morphology of a walrus.

Thalassocnus, the large marine sloth… few fossils are so strange to me as this one. But modern sloths swim well enough so why not, evolution says!

Rear end of the sea-sloth.

Megaladapis, the giant friggin’ lemur! Not cuddly.

A basilosaurid whale Cynthiacetus, one of the stars of the show, as the denouement of this post. Plan your visit now!

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As 2017 approaches its end, there have been a few papers I’ve been involved in that I thought I’d point out here while I have time. Our DAWNDINOS project has been taking up much of that time and you’ll see much more of that project’s work in 2018, but we just published our first paper from it! And since the other two recent papers involve a similar theme of muscles, appendages and computer models of biomechanics, they’ll feature here too.

Stomach-Churning Rating: 0/10; computer models and other abstractions.

Mussaurus patagonicus was an early sauropodomorph dinosaur from Argentina, and is now widely accepted to be a very close relative of the true (giant, quadrupedal) sauropods. Here is John Conway’s great reconstruction of it:

We have been working with Alejandro Otero and Diego Pol on Mussaurus for many years now, starting with Royal Society International Exchange funds and now supported by my ERC grant “DAWNDINOS”. It features in our grant because it is a decent example of a large sauropodomorph that was probably still bipedal and lived near the Triassic-Jurassic transition (~215mya).

In our new study, we applied one of my team’s typical methods, 3D musculoskeletal modelling, to an adult Mussaurus’s forelimbs. This is a change of topic from the hindlimbs that I’ve myopically focused on before with Tyrannosaurus and Velociraptor [in an obscure paper that I should never have published in a book! pdf link], among other critters my team has tackled (mouse, elephant [still to be finished…], ostrich, horse, Ichthyostega… dozens more to come!). But we also modelled the forelimbs of Crocodylus johnstoni (Australian “freshie”) for a key comparison with a living animal whose anatomy we actually knew, rather than reconstructed.

Mussaurus above; Crocodylus below; forelimb models in various views; muscles are red lines.

The methods for this biomechanical modelling are now standard (I learned them from their creator Prof. Scott Delp during my 2001-2003 postdoc at Stanford): scan bones, connect them with joints, add muscle paths around them, and then use the models to estimate joint ranges of motion and muscle moment arms (leverage) around joints. I have some mixed feelings about developing this approach in our 2005 paper that is now widely used by the few teams that study appendicular function in extinct animals. As a recent review paper noted and I’ve always cautioned, it has a lot of assumptions and problems and one must exercise extreme caution in its design and interpretation. Our new Mussaurus paper continues those ruminations, but I think we made some progress, too.

On to the nuts and bolts of the science (it’s a 60 page paper so this summary will omit a lot!): first, we wanted to know how the forelimb joint ranges of motion in Mussaurus compared with those in Crocodylus and whether our model of Mussaurus might be able to be placed in a quadrupedal pose, with the palms at least somewhat flat (“pronated”) on the ground. Even considering missing joint cartilage, this didn’t seem very plausible in Mussaurus unless one allowed the whole forearm to rotate around its long axis from the elbow joint, which is very speculative—but not impossible in Crocodylus, either. Furthermore, the model didn’t seem to have forelimbs fully adapted yet for a more graviportal, columnar posture. Here’s what the model’s mobility was like:

So Mussaurus, like other early sauropodomorphs such as Plateosaurus, probably wasn’t quadrupedal, and thus quadrupedalism must have evolved very close to in the Sauropoda common ancestor.

Second, we compared the muscle moment arms (individual 3D “muscle actions” for short) in different poses for all of the main forelimb muscles that extend (in various ways and extents) from the pectoral girdle to the thumb, for both animals, to see how muscle actions might differ in Crocodylus (which would be closer to the ancestral state) and Mussaurus. Did muscles transform their actions in relation to bipedalism (or reversal to quadrupedalism) in the latter? Well, it’s complicated but there are a lot of similarities and differences in how the muscles might have functioned; probably reflecting evolutionary ancestry and specialization. What I found most surprising about our results was that the forelimbs didn’t have muscles well-positioned to pronate the forearm/hand, and thus musculoskeletal modelling of those muscles reinforced the conclusions from the joints that quadrupedal locomotion was unlikely. I think that result is fairly robust to the uncertainties, but we’ll see in future work.

You like moment arms? We got moment arms! 15 figures of them, like this! And tables and explanatory text and comparisons with human data and, well, lots!

If you’re really a myology geek, you might find our other conclusions about individual muscle actions to be interesting—e.g. the scapulohumeralis seems to have been a shoulder pronator in Crocodylus vs. supinator in Mussaurus, owing to differences in humeral shape (specialization present in Mussaurus; which maybe originated in early dinosaurs?). Contrastingly, the deltoid muscles acted in the same basic way in both species; presumed to reflect evolutionary conservation. And muuuuuuch more!

Do you want to know more? You can play with our models (it takes some work in OpenSim free software but it’s do-able) by downloading them (Crocodylus; Mussaurus; also available: Tyrannosaurus, Velociraptor!). And there will be MUCH more about Mussaurus coming soon. What is awesome about this dinosaur is that we have essentially complete skeletons from tiny hatchlings (the “mouse lizard” etymology) to ~1 year old juveniles to >1000kg adults. So we can do more than arm-wave about forelimbs!

But that’s not all. Last week we published our third paper on mouse hindlimb biomechanics, using musculoskeletal modelling as well. This one was a collaboration that arose from past PhD student James Charles’s thesis: his model has been in much demand from mouse researchers, and in this case we were invited by University of Virginia biomechanical engineers to join them in using this model to test how muscle fibres (the truly muscle-y, contractile parts of “muscle-tendon units”) change length in walking mice vs. humans. It was a pleasure to re-unite in coauthorship with Prof. Silvia Blemker, who was a coauthor on that 2005 T. rex hindlimb modelling paper which set me on my current dark path.

Mouse and human legs in right side view, going through walking cycles in simulations. Too small? Click to embiggen.

We found that, because mice move their hindlimb joints through smaller arcs than humans do during walking and because human muscles have large moment arms, the hindlimb muscles of humans change length more—mouse muscles change length only about 48% of the amount that typical leg muscles do in humans! This is cool not only from an evolutionary (mouse muscles are probably closer to the ancestral mammalian state) and scaling (smaller animals may use less muscle excursions, to a point, in comparable gaits?) perspective, but it also has clinical relevance.

Simulated stride for mouse and human; with muscles either almost inactive (Act=0.05) or fully active (Act=1). Red curve goes through much bigger excursions (along y-axis) than blue curve), so humans should use bigger % of their muscle fibre lengths in walking. Too small? Click to embiggen.

My coauthors study muscular dystrophy and similar diseases that can involve muscle stiffness and similar biomechanical or neural control problems. Mice are often used as “models” (both in the sense of analogues/study systems for animal trials in developing treatments, and in the sense of computational abstractions) for human diseases. But because mouse muscles don’t work the same as human muscles, especially in regards to length changes in walking, there are concerns that overreliance on mice as human models might cause erroneous conclusions about what treatments work best to reduce muscle stiffness (or response to muscle stretching that causes progressive damage), for example. Thus either mouse model studies need some rethinking sometimes, or other models such as canines might be more effective. Regardless, it was exciting to be involved in a study that seems to deliver the goods on translating basic science to clinical relevance.

Muscle-by-muscle data; most mouse muscles go through smaller excursions; a few go through greater; some are the same as humans’.

Finally, a third recent paper of ours was led by Julia Molnar and Stephanie Pierce (of prior RVC “Team Tetrapod” affiliation), with myself and Rui Diogo. This study tied together a bunch of disparate research strands of our different teams, including musculature and its homologies, the early tetrapod fossil record, muscle reconstruction in fossils, and biomechanics. And again the focus was on forelimbs, or front-appendages anyway; but turning back the clock to the very early history of fishes, especially lobe-finned forms, and trying to piece together how the few pectoral fin muscles of those fish evolved into the many forelimb muscles of true tetrapods from >400mya to much more recent times.

Humerus in ventral view, showing muscle attachments. Extent (green) is unknown in the fossil but the muscle position is clear (arrow).

We considered the homologies for those muscles in extant forms, hypothesized by Diogo, Molnar et al., in light of the fossil record that reveals where those muscles attach(ed), using that reciprocal illumination to reconstruct how forelimb musculature evolved. This parallels almost-as-ancient (well, year 2000) work that I’d done in my PhD on reconstructing hindlimb muscle evolution in early reptiles/archosaurs/dinosaurs/birds. Along the way, we could reconstruct estimates of pectoral muscles in various representative extinct tetrapod(omorph)s.

Disparity of skeletal pectoral appendages to work with from lobe-fins to tetrapods.

Again, it’s a lengthy, detailed study (31 pages) but designed as a review and meta-analysis that introduces readers to the data and ideas and then builds on them in new ways. I feel that this was a synthesis that was badly needed to tie together disparate observations and speculations on what the many, many obvious bumps, squiggles, crests and tuberosities on fossil tetrapods/cousins “mean” in terms of soft tissues. The figures here tell the basic story; Julia, as usual, rocked it with some lovely scientific illustration! Short message: the large number of pectoral limb muscles in living tetrapods probably didn’t evolve until limbs with digits evolved, but that number might go back to the common ancestor of all tetrapods, rather than more recently. BUT there are strong hints that earlier tetrapodomorph “fishapods” had some of those novel muscles already, so it was a more stepwise/gradual pattern of evolution than a simple punctuated event or two.

Colour maps of reconstructed right fin/limb muscles in tetrapodomorph sarcopterygian (~”fishapod”) and tetrapod most recent common ancestors. Some are less ambiguous than others.

That study opens the way to do proper biomechanical studies (like the Mussaurus study) of muscle actions, functions… even locomotor dynamics (like the mouse study)– and ooh, I’ve now tied all three studies together, tidily wrapped up with a scientific bow! There you have it. I’m looking forward to sharing more new science in 2018. We have some big, big plans!

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We’d been wanting to do a family holiday in Ireland for years and so we finally did. I’d been to Dublin twice before for work visits and we wanted a more rural experience. On others’ recommendations, we started in the city of Cork. With some sleuthing and asking around, I realized that we weren’t far then from gorgeous Killarney National Park, and then it wasn’t far west from there to get to Valentia Island, where incidentally there is something amazing for palaeontology-lovers. There was no deterring me at that point from visiting what I’d only read about. I’ll mainly let the images tell the story.

Stomach-Churning Rating: 0/10; fossils and scenery. Kick back and enjoy.

Island map- it really is that simple to get around! The harbour town of Portmagee is damned adorable.

Driving in (no I am the passenger; not taking photo while at the wheel!)- excitement level = 8 and building… “Tetrapod carpark” sign ratcheted up the excitement and was amusing.

Headed to the trail; excitement level = 9…

Looking down onto the site (on the right); excitement level = 9.5; beauty level = 9.5 too!

Now, the site of what is broadly accepted by experts as a ~Middle Devonian tetrapod(omorph)’s fossil trackway(s) was originally described by Stössel in 1995. To me, that feels like a recent discovery but it is 22 years ago. The only other well-preserved, widely-accepted, probably-terrestrial, Late Devonian tetrapod(omorph) trackways are from the Genoa River site in Australia; described by Warren et al. in 1972. Those trackways even reveal some details of the fingers and toes; these do not. Other tracks are either isolated footprints of minimal scientific value/clarity, subaerial (i.e. underwater), not clearly stem-tetrapod (or now argued to be arthropod or other origin), not Devonian, or controversial for reasons I won’t get into here. The famous Zachelmie tracks in Poland are strong contenders but remain controversial to more than a few researchers in terms of who made them and in what environmental/substrate context; but their Middle Devonian age seems robustly agreed. Clack and Lucas have reviewed the relevant evidence recently. So there are essentially at least two, and arguably three, places in the world that you can visit to view tracks like these and it was a joy to go visit one set. (Easter Ross, Scotland may be a fourth site but it is reasonably disputed in age and maker)

There is a “however,” however- Falkingham and Horner showed how lungfish can produce tracks (with fins and heads together) that look like these, to some viewers (but not to others) and in some substrates (mud; not sand as at the Valentia site)– so there is still uncertainty for some tracks although the lungfish-feeding claims have also been vehemently disputed too. Without finger and toe impressions, claims of discrete tetrapod tracks are risky, and it would be wrong to say that the Valentia Island footprints are uncontroversially or 100% certainly tetrapod in origin, although they are (late-Middle) Devonian and made by some sort of animal, and very likely a tetrapodomorph at least.

Stössel et al. also published a recent update on these Valentia Island tracks with more information. I wish I’d come across that before I visited (oops!). That study reports on a total of nine(!) trackways from the area, adding to the 1995’s first one (the “Dohilla locality, Do 1”– see diagrams below), and describes them as Middle Devonian (with a radiometric dating of 385 million years old). I’m not enough of a geologist to evaluate that; prior reports had focused on Late Devonian or so.

Rippled sandstone example; preservation characteristic of the trackway area/Valentia Slate Formation. It’s an alluvial deposit (freshwater floodplain), interpreted to lie inland from the coastal marine deposits. Raindrop impressions above the plane of the tracks raise the possibilities that the tracks were made on (moist) land.

The island has plenty of signs advertising the tracks as a tourist destination but happily(?) there are no knick-knack shops stocked with plush tetrapods, or other developments at or near the site. One simply winds down a very narrow road near a radio station and old lighthouse, and parks then walks to see the tracks. No fancy crap; just AWESOME sights to take in, and some good educational information.

Explanatory plaque at the viewing area. Pretty good!

Nice image of where Valentia Island was; although the 385 My age may be exaggerated. It’s not clear how old the tracks are but “Mid-to-Late Devonian” might suffice depending on how you view the evidence. The tracks were the “oldest known” at the time of discovery and remain close to that, but challenged by the Zachelmie trackways (see references above).

Explanatory signs on the peak above the shore. Given the likely tetrapod(omorph) trackmakers like Acanthostega-style critters, the adult animal may have been able to breathe air with lungs and underwater with gills.

Enough exposition– let’s expose those tracks! (images can be clicked to enlarge)

My first close-up look at the tracks. Whoa! Small tracks are presumably hand (manus) impressions; larger ones are foot (pes). The tracks go in an alternating fashion (like a salamander’s walk) and the animal was probably going from the bottom-right toward the top-left. Moss and moisture obscured some of the prints that day, sadly. The tracks are oval, with the long axes perpendicular to the direction of travel. There are some pesky geological deformations of the trackway, faults, and other distortions. 145 footprints in total are reported from this one trackway!

Trackway as it turns to the left and gets harder to follow. John-shadow for ~scale. Frustratingly for me, a little rivulet was coming down the hill across the left side of the trackway and hiding much of the detail of the end.

Alternative view of the majority of the tracks; turned ~90 degrees from above two views.

Zoomed-in view of the tracks from head-on (opposite the view in other photos); i.e. western position looking east (ish). I added red and blue dots to roughly outline the right side of the main trackway (red) and the second one (blue), which crosses it and may have been made after it.

Even these nice trackways, viewed by an expert, take some unpacking. Here is some:

Diagram of known tracks at the site by Stössel et al. 2016.

Diagram at view site with extra tail (or body) drag trail crossing the main tracks; described later by Stössel et al. 2016.

I’m not at all a religious person and I don’t really like the term “spiritual” either, but this experience was emotional for me. Awe is certainly the best word to describe what I felt on viewing these tracks. The literature just doesn’t do them justice; nothing beats a first-person experience like this. We were lucky with excellent weather, too, and we were almost alone during the visit so there was pleasant silence in which to contemplate the tracks. I brought my copies of three papers on the trackways and, struggling with the wind, compared them with the visible tracks to understand what other scientists had seen. That amplified the experience enormously for me.

Even if they turn out to be non-tetrapod or younger or something less exciting (“sham-rock”?), it was thrilling to see the Valentia Island tracks and think about what happened ~385 million years ago when they were made by our very distant cousins, along the land-water interface of space and time.

(I also feel bad for online reviewers that were disappointed with the site- it’s hard to grasp the scientific importance and/or accept the evidence, even with the decent information available on-site. Even if people know the nice fossil record of dinosaurs, they may not know how good the fossil record of early tetrapods is and how confidently we can figure out what happened in the Devonian emergence of tetrapod(omorph)s onto land. But some visitors clearly got it.)

And, looking at the site myself, I realized how many more tracks might be buried under the cliffs of the site- the first trackway emerges from under a cliff and thus must still be preserved for some distance underground, awaiting future exposure. What more might we learn about that single animal and others that made tracks around the same time? I hope to live to find out. I feel a personal connection now to these tracks, left pondering what story they preserve– and hide. I’m glad I’m able to share my own story with you, and encourage you to make the visit yourself!

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A Confuciusornis fossil; not the one from our study but prettier (more complete).

Today almost three years of collaboration come together in a publication that is a fun departure from my normal research, but also makes sense in light of it. Professor Baoyu Jiang from Nanjing University in China has been being working on the taphonomy of the Early Cretaceous Jehol biota from northeastern China (Manchuria) for a while, and he found a lovely Confuciusornis (early bird) fossil; one of thousands of them; from the volcanic pyroclastic flow-based lake deposits there.

Although at first glance the skeletal remains of that fossil are not fabulous compared with some other Confuciusornis, what makes this one lovely is that, on peering at it with multiple microscopic and other imaging techniques, he (and me, and a China-UK collaboration that grew over the years) found striking evidence of very well-preserved fossil soft tissues. Our paper reporting on these findings has gone live in Nature Communications so I can blog about it now.

Reference: Jiang, B., Zhao, T., Regnault, S., Edwards, N.P., Kohn, S.C., Li, Z., Wogelius, R.A., Benton, M., Hutchinson, J.R. 2017. Cellular preservation of musculoskeletal specializations in the Cretaceous bird Confuciusornis. Nature Communications 8:14779. doi: 10.1038/NCOMMS14779

Stomach-Churning Rating: 3/10; gooey, but fossil gooey, except for some colourful, gastrically-tolerable histology of bird tissue.

Front view of the ankle/foot of our specimen.

Back view of the ankle/foot of our specimen.

What has been fun about this collaboration is that, for one, it fits in perfectly with my prior work. Ever since my PhD thesis I’d been wondering about odd bones in the legs of birds, including a very puzzling and very, very neglected bit of bone called the tarsal sesamoid, on the outside of the upper end of the ankle joint. Furthermore, a tunnel of tissue called the tibial cartilage sits next to that sesamoid bone, and then across the ankle joint there is a bony prominence with grooves and tunnels that vary highly among bird species; that is called the hypotarsus. These structures are all known in living birds and, to a degree, in extinct fossil cousins. Our specimen seems to reveal an earlier stage in how these little features of bird ankles originated, which we concluded to be a step along the transition to the more crouched legs that modern birds have.

This study has also challenged me to broaden my horizons as a scientist. Although this was a big collaboration and thus we had several specialists to apply supercharged technological techniques to our fossil, I had to learn something about what all that meant. My kind colleagues helped me learn more about tissue histology, scanning electron microscopy, synchrotron mapping, FTIR and mass spectrometry and more. I won’t go through all of these techniques but there are some pretty pictures sprinkled here and in the paper, and a lot more detail in the paper for those who want the gory techno-detail. Basically we threw the kitchen sink of science at the fossil to crack open some of its secrets, and what we found inside was nifty.

Scanning electron micrograph image of probable tendon or ligament fibres (arrow) in cross-section, from near the ankle joint.

We found preserved cells and other parts of connective tissues including tendons and/or ligaments, fibrocartilage (the tougher kind) and articular cartilage (the softer joint-padding kind). That’s great, although not unique, but the kitchen sink also flushed out even more reductionist data: those tissues included some organic residues, including what appear to be bits of proteins (amino acids); particularly the collagen that makes up tendons.

Fibrocartilage (“fc”) from the ankle joint region.

Hopefully we’re right, and we included as much of the data as we could manage so that others can look at our findings. The specimen is crushed into nearly two dimensions, like all Jehol biota organisms, so its anatomy was hard to interpret but we think we got it right. All of the other kitchen-sinky tools have their own nuances and pitfalls but we did our best with a superb team of experts. We’ve had to wait 125 million years to uncover this specimen and a few more years to find out if we’ve looked at the right way is no greater test of patience.

I thank my coauthors, especially Baoyu Jiang for the kind invitation to participate and the very fun experience of collaborating. I think I’ll remember this study for a long time because, for me, it takes a step beyond just describing Another Case of Jaw-Dropping Fossilization (can you hear the hipsters recounting the excitement and cynicism of the 1990s when this all was dawning? I was there and maybe now I’m one of them). By combining all of those methods we learned new things about the palaeobiology of birds and the evolution of traits within birds. Confuciusornis, not shockingly, had ankles that should have functioned in ways intermediate between those of bog-standard non-avian theropods and modern birds.

Same anatomical regions in an extant bird as in the main fossil specimen. Left distal tibiotarsus (TT; below) and proximal tarsometatarsus (TMT; above) from an adult helmeted guineafowl (Numida meleagris) after formalin fixation. (from our paper’s Supp Info)

I’m hopeful that more synthesis of molecular/cellular, imaging, biomechanical and other tools (not to mention good old palaeontology and anatomy!) can wash away some more of this mystery. And it was fun to be a part of a study that adds to overwhelming evidence that was heretical ~25 years ago: some hardy biomolecules such as collagen and keratin can survive hundreds of millions of years, not just thousands. Pioneers such as Prof. Mary Schweitzer led the original charge that made reporting on discoveries like ours much easier today.

I know how the birds fly, how the fishes swim, how animals run. But there is the Dragon. I cannot tell how it mounts on the winds through the clouds and flies through heaven. Today I have seen the Dragon.“– Confucius, ca. 500 BCE.

Let’s finish with some images of a living bird’s ankle region, by co-author and PhD student Sophie Regnault. We considered these for inclusion in the paper but they didn’t fit quite right. I love them anyway so here they are:

Patchwork of histology slide images, from a guineafowl’s ankle (as per photo above). The numbered squares correspond to zoomed-in images below. The tibiotarsus is on the proximal end (bottom left); the tarsometatarsus is on the distal end (right side); and the enigmatic tarsal sesamoid is at the top. Magnification: 20x overall.

Region 1. nice (fibro)cartilage-bone inferface at ligament insertion.

Region 2: longitudinal slice through ligaments connecting the tibiotarsus to the tarsometatarsus across the ankle joint.

Region 3: front (bottom) of the tibiotarsus/upper ankle.

Region 4: tendon fibres in longitudinal section; on the back of the tibiotarsus. Some show mineralization into ossified tendons (“metaplasia”); another curious feature of modern birds.

Region 5: muscle attachment to the back of the upper tarsometatarsus bone. Small sesamoid fragment visible.

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The early, hippo-like mammal Coryphodon. I didn’t know it had a patella but it does. From Yale Peabody Museum.

I’m not shy about my fondness for the patella (kneecap) of tetrapod vertebrates, and neither are the other members of RVC’s “Team Patella”. We’ve had a fun 3+ years studying these neglected bones, and today we’ve published a new study of them. Our attention has turned from our prior studies of bird and lepidosaur kneecaps to mammalian ones. Again, we’ve laid the groundwork for a lot of future work by focusing on (1) basic anatomy and (2) evolutionary history of these sesamoid bones, with a lot of synthesis of existing knowledge from the literature; including development and genetics. This particular paper is a sizeable monograph of the state of play in the perusal of patellae in placental and other synapsids. Here’s what we did and found, focusing mostly on bony (ossified) patellae because that allowed us to bring the fossil record better to bear on the problem.

Reference: Samuels, M., Regnault, S., Hutchinson, J.R. 2016. Evolution of the patellar sesamoid bone in mammals. PeerJ 5:e3103 https://doi.org/10.7717/peerj.3103

Stomach-Churning Rating: 1/10; bones and more bones.

The short version of the story is that mammals evolved bony kneecaps about five times, with marsupials gaining and losing them (maybe multiple times) whereas monotremes (platypus and echidna) and placentals (us and other mammals) didn’t do much once they gained them, and a couple of other fossil groups evolved patellae in apparent isolation.

Evolution of the patella in mammals: broad overview from our paper. Click to zoom in.

The marsupial case is the most fascinating one because they may have started with a fibrocartilaginous “patelloid” and then ossified that, then reduced it to a “patelloid” again and again or maybe even regained it. There needs to be a lot more study of this group to see if the standard tale that “just bandicoots and a few other oddballs have a bony patella” is true for the Metatheria (marsupials + extinct kin). And more study of the development of patellae in this group could help establish whether they truly do “regress” into fibrocartilage when they are “lost” in evolution, or if other, more flexible patterns exist, or even if some of the cases of apparent “loss” of a bony patella are actually instances of delayed ossification that only becomes evident in older adults. Our paper largely punts on these issues because of an absence of sufficient data, but we hope that it is inspiration for others to help carry the flag forward for this mystery.

The higgledy-piggledy evolution of a patella in Metatheria, including marsupials. Click to zoom in.

Some bats, too, do funky things with their kneecaps, analogous to the marsupial “patelloid” pattern, and that chiropteran pattern also is not well understood. Why do some bats such as Pteropus fruit bats “lose” their kneecaps whereas others don’t, and why do some bats and other species (e.g. various primates) seem to have an extra thing near their kneecaps often called a “suprapatella”? Kneecap geeks need to know.

The short-nosed bandicoot (marsupial) Isoodon, showing a nice bony patella as typifies this group. From Yale Peabody Museum.

Otherwise, once mammals evolved kneecaps they tended to keep them unless they lost their hindlimbs entirely (or nearly so). Witness the chunky patellae of early whales such as Pakicetus and join us in wondering why those chunks persisted. The evolutionary persistence of blocky bits of bone in the knees of various aquatic animals, especially foot-propelled diving birds, may help answer why, as the hindlimbs surely still played roles in swimming early in cetacean evolution. Ditto for sea cows (Sirenia) and other groups.

Early whale Ambulocetus, showing hefty kneecaps.

But I’m still left wondering why so many groups of land vertebrates (and aquatic ones, too) never turned parts of their knee extensor tendons into bone. We know a bit about the benefits of doing that, to add leverage to those joints that enables the knee muscles to act with dynamic gearing (becoming more forceful “low gear” or more speedy “high gear” in function). Non-avian (and most early avian/avialan) dinosaurs, crocodiles, turtles, amphibians, early mammal relatives, and almost all other known extinct lineages except for those noted above got by just fine without kneecaps, it seems, even in cases where a naïve biomechanist would expect them to be very handy, such as in giant dinosaurs.

A quoll, Dasyurus, with what is probably a fibrocartilaginous “patelloid”. From Yale Peabody Museum.

However, tendons don’t turn to bone unless the right stresses and strains are placed upon them, so maybe kneecaps are a “spandrel” or “exaptation” of sorts, to abuse Gould’s ghost, whose adaptive importance is overemphasized. Maybe that adaptive myopia overshadows a deeper ontogenetic story, of how tissues respond to their history of mechanical loading environment. It has been speculated that maybe (non-marsupial) mammals have broadly “genetically assimilated” their kneecaps, fixing them into semi-permanence in their genetic-developmental programmes, whereas in contrast the few studies of birds indicate more responsiveness and thus less assimilation/fixation. That “evo-devo-mechanics” story is what now fascinates me most and we’ve poked at this question a bit now, with some updates to come- watch this space! Regardless, whether an animal has a bony vs. more squishy soft tissue patella must have consequences for how the knee joint and muscles are loaded, so this kind of question is important.

Giant marsupial Diprotodon (at NHM London); to my knowledge, not known to have had kneecaps- why?

In the meantime, enjoy our latest contribution if it interests you. This paper came about when first author Dr. Mark Samuels emailed me in 2012, saying he’d read some of my old papers on the avian musculoskeletal system and was curious about the evolution of patellae in various lineages. Unlike many doctors and vets I’ve run into, he was deeply fascinated by the evolutionary and fossil components of patellae and how those relate to development, genetics and disorders of patellae. We got talking, found that we were kindred kneecap-spirits, and a collaboration serendipitously spun off from that, soon adding in Sophie. It was a blast!

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