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Thursday, 12 December 2013

Shedding [no] light on dinosaur predation scenes

The carcharodontosaurian Neovenator salerii stalks a pair of rebbachisaurid sauropods in Lower Cretaceous Britain, using darkness as cover. Prints of this image are available here.
Finding time for Blogging has recently become quite difficult despite no shortage of topics to cover or new paintings to post. In the interest of keeping things alive, here's a quick painting I recently finished which tackles that most traditional subject of dinosaur palaeoart: predation. This is a rare topic for my work because the ferocity, speed and armaments of theropods and their prey are subjects of so many depictions that I almost find them artistically off-putting. For all their dynamism - gaping maws, slashing claws, wrestling limbs - they've become so common that they're (whisper it quietly) a bit boring. Even the most exciting experiences become dulled if overexposed, and we may have hit that mark with dinosaur predation scenes. Not to mention that a lot of the overly-done operatics associated with dinosaur predation art really start to grate after a fashion. Theropods roaring at their prey; 'slasher poses', animals wrestling in long, drawn out battles; completely mismatched combatant species which bear little resemblance to predator/prey interactions in modern times (seriously chaps: stop drawing a dromaeosaurs attacking animals hundreds of times their size - they're not freakin' superheroes!), and so forth. So yes, for the most part, I switch off when I see depictions of dinosaur predation in favour of things which I find more conceptually interesting. Like, er... animals standing around doing nothing, lying down, walking about or perhaps, if I'm feeling adventurous, chewing a leaf.*

*Bear in mind that, in being British, I'm allergic to excitement.

My interest in dinosaur predation art was piqued recently however thanks to re-watching the excellent BBC series Planet Earth and The Life of Mammals. Both feature copious amounts of footage filmed at night using infra-red lights, revealing how many animal species are as active nocturnally as they are during the day. Many species undertake complex nocturnal activities in spite of poor night vision, and it's obvious that this brings clear advantages to species with generally higher visual acuity or those with eyes specifically adapted to work well in dim conditions. Generally speaking, this means advantage: predators.

Did the same apply to Mesozoic ecosystems? Possibly. We can currently only speculate on the day-night activity cycles of ancient animals (and no, using sclerotic rings and orbit shape to infer nocturnality as proposed by Schmitz and Motani [2011] doesn't work: see Hall et al. [2011]), but given what we know of dinosaur physiology and palaeoecology, facultative nocturnal habits for some species do not seem out of the question. Theropod dinosaurs, like modern carnivores, often have more acutely developed senses than the herbivores they likely often preyed upon, and it isn't crazy to think that some would use this to their advantage by hunting at night. We may further speculate that - like some modern carnivores - nocturnally active theropods would punch above their weight, attacking unusually big or dangerous prey because their ability to remain undetected is that much greater (see, for a famous modern example, the lions and elephants in the BBC video below).



From here, it's easy to see how I came up with the image above. It shows the carcharodontosaurian Neovenator, one of the largest theropods known from the Lower Cretaceous Wessex Formation, creeping close to a couple of rebbachisaurid sauropods (a relatively recent addition to the Wessex dinosaur fauna, but currently not represented by any name-bearing material). The Neovenator can see the sauropods with much greater clarity than they can see it, although they are not completely oblivious to its presence. I've tried to instil a sense of agitation and nervousness about them, brought on by the proximity of something which sounds and smells like trouble. Despite its ocular advantage, the Neovenator is not charging in with blazing teeth in typical palaeoart fashion, instead biding its time, keeping low and quiet, and waiting for the right moment to launch an attack. The sauropods are, after all, a bit bigger than it is (estimated as 9 m long by Mannion 2009, compared to 7.5 m for Neovenator) and a lot heavier. I don't imagine Neovenator would normally take prey as large as this, and is only taking such a chance because the night has shifted odds slightly in its favour. Still, a clumsy move would not only ruin a successful stalk but also risk injury, so caution is the best policy. Maybe the copse behind the sauropods is part of the plan too, with Neovenator driving the sauropods into a setting where they're likely to encounter unseen obstacles and pitfalls. Hopefully, the dim nature of the painting helps convey some of the uncertainty and dread that the sauropods are experiencing. Like the sauropods, we can't see much, only just enough to be sure that the rebbachisaurids are in trouble, and that the game is currently Neovenator's to lose.

I've not had the time to check thoroughly, but it does seem that images of dinosaurs in near darkness are pretty rare, and maybe that's something worth thinking about changing. Palaeoart is primarily about showing off the anatomy and form of animals but, if we're trying to create mood, we may want to take bold steps away from clearly lit subjects shown in broad daylight. There's a lot of atmosphere to be found in the unseen or the murky and, as with adding atmosphere to any visual medium, less is often more. Using extremes of lighting or visually-limiting weather conditions may obscure some details of the animals we're aiming to show, but it can tell us a lot about the biology and 'character' of a particular species. An 'extreme' environment becomes a character in its own right, and the animals have to respond to their surroundings rather than simply existing within them. I enjoyed painting these Pelorosaurus in a rainstorm (below), for instance, because the picture seems to convey how tough these animals would have to be. There's no shelter large enough for sauropod-sized animals, so they simply must have endured any awful conditions thrown at them. This isn't a great picture for saying 'this is what Pelorosaurus looked like', but we get a good sense of the hardy nature of these animals, as well as the message that their physiology is capable of sustaining them through hard times. Hopefully, the barely-seen postures and positioning of the animals in the predation scene at the top of this post convey a similar sense of character, as well as throwing some new light (or removing it, I guess) from a familiar palaeoart subject. It would be remiss of me to talk about atmospheric palaeoart without mentioning Doug Henderson's new online gallery, a site the internet has sorely needed for some time and a veritable masterclass in using environments to create moody, character-filled palaeoart.

Pelorosaurus conyberi in the rain, looking all tough and moody. For more on this image, head to this post.
So that's my brief take on dinosaur predation then: a barely discernible scene of virtually immobile, quiet animals without a single tooth, claw or roar in sight. Coming next (probably): something more substantial on a boring old ornithopod that's on the lee slope of fame.


References
  • Hall, M. I., Kirk, E. C., Kamilar, J. M., & Carrano, M. T. (2011). Comment on “Nocturnality in dinosaurs inferred from scleral ring and orbit morphology”. Science, 334(6063), 1641-1641.
  • Mannion, P. D. (2009). A rebbachisaurid sauropod from the Lower Cretaceous of the Isle of Wight, England. Cretaceous Research, 30(3), 521-526.
  • Schmitz, L., & Motani, R. (2011). Nocturnality in dinosaurs inferred from scleral ring and orbit morphology. Science, 332(6030), 705-708.

Monday, 2 December 2013

Windows into Early Cretaceous Britain: the plant debris beds of the Wessex Formation

Some parts of Lower Cretaceous Britain was subject to regular, short-lived wildfires caused by lightning strikes after long dry seasons, phenomena which played an integral role in forming the fossil-rich plant debris beds of the Wessex Formation. Here, the early tyrannosauroid Eotyrannus lengi stalks the edge of such a wildfire. Note that this Eotyrannus is based on new skeletal reconstructions presented in recent papers (e.g. Naish 2011), not the better known, original reconstruction presented by Hutt et al. (2001). Prints of this image are available.
If you're into Mesozoic reptiles, you could find yourself in much worse places than southern England. Much of the exposed geology in the southern part of the UK belongs to a unit known as the Wealden Supergroup, a series of Lower Cretaceous rocks representing ancient alluvial fans, river channels and floodplains. Many of Britain's Cretaceous dinosaurs and pterosaurs stem from Wealden deposits, along with numerous other types of fossils including armoured dinosaurs, plesiosaurs, famous sauropods and weird, burrowing amphibians.

A slumped plant debris bed in the Wessex Formation, Brighstone Bay, Isle of Wight. Image borrowed from the UK Fossil Network forums, by one only known as 'Alan'.
Fossils occur found throughout Wealden rocks but, as is often the case in palaeontology, the majority are concentrated into narrow horizons. One type of Wealden fossil bed deserves special praise and attention: the plant debris beds of the Wessex Formation. Plant debris beds are narrow, green-grey bands of pebbles, mud and plant debris which comprise only a fraction of the Wessex strata, but represent a tremendous source of its fossils. Indeed, these beds provide the majority of Britain’s Cretaceous dinosaur species as well as many other fossil species, including many rare microvertebrates. Debris bed fossils range from small, badly preserved portions of plant and isolated, broken bones, teeth and scales, to substantial chunks of very large organisms - partial or near-complete animal skeletons and 3 m long logs (below). With continental deposits relatively rare in the Lower Cretaceous, the plant debris beds represent an important window into European faunas of this time, and studies into their palaeontology are ongoing (see below).

Enormous, pyrite-riddled chunks of fossil tree trunks, like these bits of the conifer Pseudofrenelopsis, litter the beaches beneath the Wessex Formation after weathering out of plant debris horizons. The ruler in this image is 150 mm long.
The story behind the plant debris beds has intrigued scientists for decades, leading to detailed research into their formation. Because the Wessex Formation represents a complex environment - an arid floodplain dominated by enormous, meandering rivers which were bordered by wooded highlands, and subjected to long summer months with temperatures well over 30°C but short, cool and rather wet winters - several different ideas about debris bed genesis have been proposed (best summarised and explored in Sweetman and Insole 2010). Plant debris bed sediments bear characteristics of debris flows; powerful, water-saturated sediment surges which ooze across landscapes to create poorly organised pools of mud and detritus. Such flows were clearly not regular events in the Wessex palaeoenvironment. Although many plant debris beds are known, they are relatively minor components of the Wessex Formation and are randomly distributed within Wessex strata. They were not, therefore, seasonal events and must reflect particularly unusual or extreme environmental conditions. Some have suggested that intense river flooding events and bank breaches account for these deposits, but plant debris beds are not associated with river sediments in a manner predicted for breached riverbanks deposits. Because the plant remains they contain are similar to leaf-litter found in modern forests, it is likely that they originated external to the Wessex floodplain, perhaps starting on nearby upland, wooded areas, not within the river channels. Indeed, debris flows generally start on slopes when water saturated soils and sediments become too heavy and unstable to resist gravity. The slopes required to begin plastic sediment flows are not large, and the relatively low upland areas surrounding the Wessex floodplain were likely sufficiently inclined to catalyse debris flows. Topographic highs on the floodplain itself may also have done the job. Presumably, the heavy rainfalls incurred during winter seasons was the water source which saturated Wessex soils to a critically unstable level.

The secret ingredient
This is only half the story, however. Sediment flows do not start after most heavy rainfalls because precipitation is mostly absorbed by leaf litter, intercepted by plant canopies, and soils are bound by vegetation. We know that the Wessex palaeoenvironment was fairly well-vegetated, and it is likely that its plants prevented Wessex slopes from collapsing. The secret ingredient required to make a debris flow, it seems, was fire (above). A common component of all plant debris beds is the abundance (about 50%) of burnt plant material, suggesting they were only formed after fires - likely caused by lightning strikes after long, dry summers- had swept through surrounding areas. An absence of burnt tree trunks suggests Wessex wildfires were not particularly intense, their main effect being removal of canopy cover, low-level vegetation and leaf-litter. This left the environment denuded enough for rainwaters to directly interact with soils and underlying sediments. Modern wildfires raise soil temperatures to hundreds of degrees and alter their physical properties, reducing water capacity and increasing erodibility. The result is a perfect recipe for debris flows: unprotected, easily transportable soils and sediments are left exposed to heavy precipitation, which likely arrived in earnest during winter storms.

Model of plant debris bed deposition on the Wessex Formation floodplain. Based on Sweetman and Insole (2010).
The range of sediment and fossil sizes within the plant debris beds indicate that they did not travel far, maybe a few kilometres at most, but they hoovered up any organic and sedimentary material they encountered. Large sediment flows can travel relatively quickly – up to 16 kph – and carry objects weighing many tonnes. Large dinosaur carcasses and tree trunks would be carried without hesitation by flowing oozes of debris moving across the Wessex floodplain. The surges finally lost momentum when they reached depressions such as ponds, oxbow lakes, abandoned river channels or simply topographic lows, creating the thin bands of sediment we can see today in Wessex Formation cliffs. The rarity of complete animal remains suggests that few animals were killed in the transportation process, and most vertebrate fossils probably represent bones or carcasses collected en route by the debris flow. This model for plant debris bed formation is, of course, rather generalised and may not apply to all beds. Each plant debris horizon is unique and, although this model likely accounts for at least some aspects of each, each has its own characteristic depositional history. Interestingly, no other fossil horizons match the sedimentological properties of the plant debris beds, making them important to not only palaeontologists, but also sedimentologists.

It is, of course, palaeontology which benefits most from these deposits however. Ongoing examination of the debris beds fossils, largely by renowned Wealden expert Steve Sweetman, continues to reveal new discoveries. Scientists now recognise the plant debris beds as key sources of Cretaceous microfossils as well as larger, macro-scale remains. These are extracted by sieving large quantities (literally tonnes) of plant debris bed sediment, followed by many hours hunched over microscopes to analyse and identify the new finds. This hard work has certainly paid off, adding significant detail to our understanding of the Wealden palaeobiota (below). We now know that dinosaurs were only a fraction of the tetrapod fauna in these environments, with lizards, amphibians and other small animals comprising the bulk of Wessex diversity. New discoveries are still being made, and it's an exciting time to work on Wealden fossils.

How plant debris beds changed the world. A, Wessex Formation tetrapod assemblage prior to bulk sampling and detailed study of plant debris bed fossils; B, the same assemblage after. Data from Sweetman and Insole (2010).

Plant debris beds conservation
The exciting fossil content and accessible nature of many plant debris beds has made them a favourite source of fossils to hobbyists, private collectors and professionals for centuries. This interest has undoubtedly contributed to our detailed understanding of the Wealden fossil assemblage and will continue to do so in future. It is essential, however, that plant debris beds and other Wealden exposures are treated with care and responsibility. All too often, a walk along Wessex Formation exposures reveals depressing signs of geological vandalism: holes bulldozed into slumped cliffs in vain efforts to seek fossil-bearing horizons; messages carved into soft sandstones; dinosaur footprint casts with smashed toes, and even trackways with individual prints removed using power tools. Plant debris beds are often more conspicuous by the smashed rocks surrounding them than their lithological features. While some geological vandalism clearly reflects activities of bored, idle individuals, other types - and particularly that associated with debris beds – reflects the desires of eager individuals to discover and excavate fossil remains. We have to keep this in check. Over-enthusiasm not only risks damaging important specimens but also the surrounding sediments and other, less desirable fossils, both of which offer essential details on the depositional context of a fossil specimen. Remember that hammer blows do not only remove overburden, but also smash whatever lies beneath the surface.

The point here is not, of course, that Wealden fossils should be the sole remit of trained collectors, but that we should all be conscientious about our geological heritage. It is often far wiser, for instance, to alert local museum or university staff about an exciting find before collecting it, rather than risking damaging the specimen and it’s geological context by taking it immediately. If nothing else, contacting local professionals can provide sound advice on an appropriate manner to collect and preserve fossils. As with any fossil discoveries, accurate records must be made about the location and horizon of a new find and, if the specimen looks like it may be important, collectors should strongly consider accessioning their finds to a museum. Collectors who work with museums and scientists are frequently involved in the science that can follow a new discovery, helping to analyse and document the find in scientific papers and books. I can vouch from personal experience that this can happen relatively quickly. A new Wealden fossil accessioned to Dinosaur Isle (the Museum of Isle of Wight Geology under any other name) or the Natural History Museum seems to always get local palaeontologists buzzing, and several Wealden experts are well known for analysing new specimens within weeks of their arrival. If they are important, they end up being written up into technical papers, may be further featured in other palaeontological books and media, and may even end up on public view in museums.

What you'll want to understand fossils from plant debris beds, or any other part of the Wealden, for that matter.
How do you know if a fossil is 'important' enough to bring it to the attention of expert? Fossil identification guides, such as the excellent and highly comprehensive English Wealden fossils (Batten 2011) and Dinosaurs of the Isle of Wight (Martill and Naish 2001) are a useful means to gauge not only the identification of a Wealden fossil find, but also how ‘significant’ it may be. Many Wealden vertebrates are especially poorly known and new data on them is highly sought after, so it may be worth getting any well-preserved vertebrate material checked out. Doing so ensures that the window into Lower Cretaceous Britain offered by these remarkable beds remains widely open to all, which seems only right considering the importance of of these beds to British palaeontology.

References

  • Batten, D. J. (ed.) (2011). English Wealden Fossils. The Palaeontological Association, London.
  • Hutt, S., Naish, D., Martill, D. M., Barker, M. J. & Newbery, P. (2001). A preliminary account of a new tyrannosauroid theropod from the Wessex Formation (Early Cretaceous) of southern England. Cretaceous Research 22, 227-242.
  • Martill, D. M. & Naish, D. (2001). Dinosaurs of the Isle of Wight. The Palaeontological Association, London.
  • Naish, D. (2011). Theropod dinosaurs. In: Batten, D. J. (ed.) English Wealden fossils. The Palaeontological Association (London), pp. 526-559.
  • Sweetman, S. C., & Insole, A. N. (2010). The plant debris beds of the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England: their genesis and palaeontological significance. Palaeogeography, Palaeoclimatology, Palaeoecology, 292(3), 409-424.

Sunday, 10 November 2013

The retrosaur identity...revealed: I liked sauropods before they were cool

A couple of days ago, I played for time in my posting schedule by asking readers to identify the deliberately outdated reconstruction of a fossil species shown above. I'm relieved to say the event was not a complete washout, with several dozen suggestions made in the blog comment feed and on Facebook - thanks to those who made suggestions. Most proposed  that this animal is an archaic view of a marine reptile, perhaps a placodont, mosasaur, pliosaur or, best of all, Edward Cope's famous backwards Elasmosaurus. Others thought it may be an early interpretation of Basilosaurus or a Megalosaurus in its lizard-like 1820s guide.

None of these are quite on the money. I did try to leave a few hints in the image and article. The post title and keywords hinted at a reptilian identity; I mentioned that the interpretation is very, very old, and that the literature describing this animal was rather vague and open to a lot of interpretation. The marine reptiles in the top left are deliberate nods to the article describing the habits of the mystery animal, which proposed it 'might keep in check the Crocodilians and Plesiosauri'. Perhaps the biggest giveaway was the illustration caption, which read "An old, old sight, and yet somehow so young.", a quote from Moby Dick. I'm sure a lot of you have already put these hints together but, in case it's not obvious, the image above shows my rendition of Cetiosaurus as a gargantuan reptilian superpredator of Mesozoic seas, as described by Richard Owen in 1841. Of course, we also know Ceitiosaurus, the 'whale lizard', as (pretty much) the first sauropod ever named, so another way to view this is as retropalaeoart of a sauropod. Congrats to Mike Traynor, Myungkeun Ryu and Tim Morris for guessing correctly. Please treat yourselves to an extra spoonful of peas for dinner.

How is that a sauropod?
It's widely known that sauropods were once thought to be marine animals, but I'm sure some of you are wondering just how I came to reconstruct this animal in this guise, perhaps even if you are familiar with Owen's (1841) description (you can download this, for free, here). There's a lot of points to consider here, the most important of which is that this is entirely based on the very first report of a sauropod, not any later considerations. My Cetiosaurus is how it may have been imagined in 1841, perhaps after hearing the first public discussion on them (Owen's 1841 paper is actually a summary of this talk by an anonymous author, not a manuscript penned by the man himself). The illustration attempts to showcase the basic thrust of Owen's hypothetical animal along with a few nods to specific details he mentions in his description, along with some palaeoart trends of the mid-1800s.

How much of the world first met what would become sauropod dinosaurs: the title of Owen's 1841 lecture memoir. Seven pages of text, no specific names, no specimen numbers, no holotype, and no illustrations, and the beginning of a monstrously complex taxonomy which has only recently been revised into a useful format.
The first sauropods, as with many dinosaurs, were not recovered from anything like complete remains. Cetiosaurus was mostly described from caudal vertebrae and a few other bones, including limb elements and a partial shoulder girdle, and that was about all. These bones were mostly collected from Jurassic rocks of Oxfordshire, but others came from similarly-aged deposits from other locations in south east England. Owen's Cetiosaurus was subsequently represented multiple individuals without overlapping components, hampering any hope of attaining a sense its relative proportions. As such, virtually none of the iconic aspects of sauropod appearance were apparent in 1841, save for one: Cetiosaurus was clearly huge. Owen stressed how the fossils he had were much larger than those of an elephant or even Megalosaurus, and that only Iguanodon and 'full-sized whales' had bones of comparable size. Remember that many still considered Iguanodon as a lizard-like animal of tremendous length in 1841, not the more sensibly proportioned, rhinoceros-like animal we think of as the 'Victorian Iguanodon'. No size estimates for Cetiosaurus were provided in the 1841 lecture, but it's clear that Owen thought it was seriously big.

It was not only the appearance of this animal which remained enigmatic: it's affinities among Reptilia were not immediately clear. It is often reported that Owen initially considered Cetiosaurus to be a giant marine crocodile, but this is not apparent from his 1841 lecture (Taylor 2010). Cetiosaurus was compared with a number of other animals, including whales, marine reptiles, crocodiles, lizards and several genera which would later be recognised as dinosaurs. The nature of the vertebrae and the presence of a claw were sure fire signs that Cetiosaurus was of saurian origin and not, despite its size, an ancient cetacean. Owen did note that several aspects of its bone structure were reminiscent of whale bone however. We should recall here that Owen was primarily working from caudal vertebrae, which are far more whale-like in their guise than the complex, hollowed cervical vertebrae we may think of when we imagine sauropod vertebrae (below). Several favourable comparisons were made between Cetiosaurus, dinosaurs and crocodiles, but Owen refrained from allocating Cetiosaurus to a specific reptile group until 1842, when he referred it to Crocodilia (Owen 1842).

A caudal vertebra referred to Cetiosaurus by Owen in 1853, now referred to Pelorosaurus. It's not difficult to see why Owen considered vertebrae like this to be whale-like. From Wikipedia.
What of its habits? Again, there's precious little to go on here from Owen's lecture. Owen suggested the animal had to be aquatic because its bones had a cancellous texture reminiscent of cetacean bones. The size of the animal suggested it was not likely to populate small rivers and streams and probably lived in larger aquatic settings - the marine realm. On diet, it's reported that "the surpassing bulk and strength of the Cetiosaurus were probably assigned to it with carnivorous habit, that it might keep in check the Crocodilians and Plesiosauri" (Owen 1841, p. 462). Little other evidence for this predatory existence is provided, although fossils of "large conical teeth" were mentioned as possibly belonging to Cetiosaurus.

The lost world of Cetiosaurs, superpredator
By now, we're starting to emerge with a picture - vague as it is - of Owen's Cetiosaurus, c. 1841. A nondescript, gigantic, whale-like marine saurian which predated other marine reptiles is about as far as we can go but, hey, that's still pretty neat. Sadly, it seems no-one thought Owen's Cetiosaurus was worth illustrating and we can't really be sure what Owen, or any of his contemporaries, thought about its life appearance. This is a weird fact in itself, because reconstructing extinct animals was becoming quite fashionable around 1840. Maybe Cetiosaurus was just too poorly known to be professionally illustrated, or perhaps its relatively quick ushering into Crocodilia meant that, despite its size, it just wasn't exciting compared to the then newfangled dinosaurs and other more 'exotic' fossil species. But still, people must have pondered the life appearance of Cetiosaurus in 1841. It's not like a giant, whale-like killer reptile isn't sufficient fuel for the imagination. What must have Owen's lecture audience been thinking as they left his talk? The learned folks of the 1800s must have speculated and imagined ancient worlds as much as we do, and who knows what bizarre anatomies and behaviours they envisaged? Perhaps their speculations were even more elaborate than ours, their knowledge being far less constrained by data than our own.

My quick illustration here is an attempt to recapture some of this lost imaginary wonder, showing how someone in the 1840s may have imagined Owen's whale-lizard without any concept of what sauropods were actually like. Of course, given how little information we have to work with from the 1841 lecture, there's a lot of room for artistic manoeuvring here. I'll bet you could change almost every detail of this illustration and still call it Cetiosaurus c. 1841. In fact, it'd be very interesting to see what others might come up with based on the same information - I'd gladly compile a compendium of superpredator Cetiosaurus works for a blog post here if people send them in. In the meantime, I'll explain how my 1841 Cetiosaurus ended up as it did.

Material of Cetiosaurus oxonensis described by Philips (1871), the single species we now recognise within Cetiosaurus. These were the first sauropod remains which offered a significant glimpse into sauropod biology, and changed perceptions of Cetiosaurus forever. Image from Wikipedia.

Overall, my Cetiosaurus looks more like an oversized lizard than anything else, because many of the earliest renditions of fossil animals are very lizard-inspired. I guess the concept of 'reptiles' was quite restricted in the early 1800s. The tail is not shown in a crocodile-like guise because Owen noticed some differences in the cross-sectional structure of croc and Cetiosaurus caudals, but it is rather long because the caudal vertebrae of Cetiosaurus were reported as proportionally longer than those of Megalosaurus. Reflecting the fact that the tail was one part of the body we had some knowledge of in 1841, I thought this should at least look a bit sauropod-like. I tried to emphasise the 'whale' aspect of the 'whale-lizard', making the body rather bulky but keeping the limbs rather reduced, a bit like early cetaceans. In keeping with the nods towards dinosaurs and crocodiles, I decided not to make the limbs into flippers, and maintained a healthy set of claws on the end of the digits. The integument is a mix of smooth, whale-like skin and crocodilian-like scales and scutes. As is typical of early prehistoric reptile restorations, the head is generically reptilian, looking a bit like those of lizards or short-faced crocodylomorphs. Making the head small was an attempt to emphasise the bulk of the body and lean towards 'generic' reptile proportions. The prey animals are, as mentioned above, a deliberate nod towards Owen's lecture and serve to show how enormous this Cetiosaurusis meant to be.

What became of Owen's Cetiosaurus?
Unlike other early, erroneous reconstructions of dinosaurs, the idea of Cetiosaurus as a marine superpredator is barely more than a footnote in stories of dinosaur discovery, despite this interpretation remaining unquestioned for several years. Perhaps history has largely forgotten this animal because it was not widely reconstructed. With retrospect, we might argue that Gideon Mantell (1850) first put forward an argument against this reconstruction when he proposed a terrestrial existence for his then new Pelorosaurus - an animal based on the holotype for Owen's Cetiosaurus brevis*. However, Mantell also argues that Pelorosaurus is distinct from Cetiosaurus because it was a terrestrial creature: he didn't outright refute the concept of a reptilian superpredator itself. Perhaps John Phillips (1871) was the man who truly put Owen's aquatic superpredator to rest. He described much more complete Cetiosaurus remains (above) which provided a new understanding of its anatomy and relationships. Although the long neck was still not known, Phillips (1871) was able to rationalise a semi-aquatic creature with well-developed limbs, a parasagittal gait and large body size. He was also the first to propose that Cetiosaurus may have been a dinosaur. This represented a large stride towards the reality of sauropod dinosaurs, although these revelations were quickly superseded: the Bone Wars, and the American sauropod bounty they represent, were only a few short years away. The sauropod discoveries they brought rendered Owen's superpredatory marine Cetiosaurus a completely obsolete, erroneous interpretation of sauropod palaeobiology, and one that Owen was probably very happy to forget about.

*Cetiosaurus has a hella confused taxonomic history which has only recently been sorted. Over a dozen Cetiosaurus species were named for fossils across Britain by Owen and other workers, spreading Cetiosaurus across time, space and sauropod phylogeny. We now only recognise one species of Cetiosaurus, C. oxoniensis. See Upchurch and Martin (2003) for a review of this taxonomic debacle.

And that's all I've got time to say for now. I'll leave you with another image of some waterlogged sauropods, this time of a more conventional variety. The animals here are Pelorosaurus conybeari, a somphospondyl from Lower Cretaceous Britain. P. conybeari, of course, is another aspect of the Cetiosaurus story, being one species to come out of the Cetiosaurus taxonomic complex. That's a whole other article however - check out Taylor and Naish (2007) and Naish and Martill (2007) if you want to know more. Thanks again for contributing to the 'guess the retrosaur' game if you commented!

Pelorosaurus conybeari, the nomenclatural destiny of some Cetiosaurus material, in what a great Alabamian philosopher once referred to as 'big ol' fat rain'.
References
  • Owen, R. (1841). A description of a portion of the skeleton of the Cetiosaurus, a gigantic extinct saurian reptile occurring in the oolitic formations of different portions of England. Proceedings of the Geological Society of London 3, 2: 457-462.
  • Mantell, G. A. (1850). On the Pelorosaurus; An Undescribed Gigantic Terrestrial Reptile Whose Remains are Associated with Those of the Iguanodon and Other Saurians in the Strata of Tilgate Forest, in Sussex. Philosophical Transactions of the Royal Society of London, 140, 379-390.
  • Naish, D., & Martill, D. M. (2007). Dinosaurs of Great Britain and the role of the Geological Society of London in their discovery: basal Dinosauria and Saurischia. Journal of the Geological Society, 164(3), 493-510.
  • Owen, R. (1842). Report on British Fossil reptiles, Pt. II. Reports of the British Association for the Advancement of Science 11: 60–204.
  • Phillips, J. (1871). Geology of Oxford and the valley of the Thames. Clarendon Press, Oxford, 529 pp.
  • Taylor, M. P. (2010). Sauropod dinosaur research: a historical review. Geological Society, London, Special Publications, 343(1), 361-386.
  • Taylor, M. P., & Naish, D. (2007). An unusual new neosauropod dinosaur from the lower cretaceous hastings beds group of East Sussex, England. Palaeontology, 50(6), 1547-1564.
  • Upchurch, P., & Martin, J. (2003). The anatomy and taxonomy of Cetiosaurus (Saurischia, Sauropoda) from the Middle Jurassic of England. Journal of Vertebrate Paleontology, 23(1), 208-231.

Friday, 8 November 2013

Guess the retrosaur

An old, old sight, and yet somehow so young.
Finding time to blog has been more-or-less impossible of late. In the effort to keep things ticking over, I thought I'd post this quick painting as a prelude to a post I hope to have together soon. The image is, technically speaking, a piece of palaeoart, but shows a very, very dated interpretation of a fossil species. Retropalaeoart, if you will.

Question is, what is the main animal in this image? I'm not aware of any similar depictions of this taxon (which doesn't mean they don't exist, but they're probably rare) and several colleagues have already struggled to work out what this is meant to be. I'm not going to reveal the answer just yet, but feel free to leave guesses below in the comment feed. Note that the literature used to inform this reconstruction is rather vague on many anatomical details, so a fair bit of interpretation and imagination were used to put this together. That said, the identity of this animal is not that obscure, and I'm sure many readers will quickly grasp what I'm attempting to do here. The first person to guess correctly wins the satisfaction of being the first person to guess correctly.

Hopefully, the answer will be revealed in the next couple of days. Good luck!

Tuesday, 29 October 2013

Azhdarchid pterosaurs: 'terrestrial stalkers' or pelican-esque 'scoop-feeders'?

This week saw the pre-publication of a new paper by myself and Darren Naish on one of our favourite topics, azhdarchid pterosaur* feeding habits. The article is now available in proof format in the Open Access journal Acta Palaeontologica Polonica, with the final, fully typeset version following sometime next year. Darren and I are no strangers to the long-necked, frequently gigantic azhdarchids of course, having discussed azhdarchid foraging habits at length in a 2008 paper and concluding that previously proposed lifestyles - skim-feeding, sediment probing, obligate scavenging - were inconsistent with azhdarchid functional anatomy. Instead, we proposed a novel hypothesis, that azhdarchids were 'terrestrial stalkers', basically just a sexy way of saying 'they wandered around on the ground and ate whatever they could find'. Hey, half of selling an idea is a snappy name, baby.

*Surely no-one here needs to be told what an azhdarchid is? You do? Then check out this article for a primer.

Why do we think azhdarchids were 'terrestrial stalkers'? A handy infographic explaining our reasoning, from Witton and Naish (2013).  The greyed cervical vertebrae indicate the range of azhdarchid neck motion according to Averianov (2013), which we are pleased to see meeting our expectations of ground-reaching ability (see Witton and Naish 2008; Fig. 8 and caption).
We're not the only folks with opinions on azhdarchid palaeoecology of course. Although I think the terrestrial stalker idea has been generally well received, Alexander Averianov (2013) disagreed with the idea. Earlier this year, he proposed that the terrestrial stalker hypothesis is flawed for three major reasons, which can be summarised as:
  1. Azhdarchid remains are always found in ancient lake and river deposits, which indicates they were feeding there as well.
  2. Grounded azhdarchids were vulnerable to predation from theropod dinosaurs, being ill-suited to rapid takeoff or other means of quick escape.
  3. We overlooked the helical jaw joint of azhdarchids in our 2008 paper. Azhdarchids possess a skewed jaw joint which laterally displaces the mandibular rami when the jaw is opened, expanding the throat region marginally. According to Averianov (2013), this is a sign of expanding, pelican-like jaws, which permitted fish to be scooped from water in flight, which is a superior hypothesis to terrestrial stalking.
After some discussion between ourselves, Darren and I decided that we should respond formally to these points - Witton and Naish (2013) is the result. In doing so, we were able to explore some aspects of azhdarchid palaeobiology a little more, as well as put some comments into print on the way we interpret the lifestyles of fossil animals. Hopefully, a lot of the things we have to say on this will be of interest to readers here, so I thought I'd provide a quick summary.

Taphonomy is not destiny
Averanov's (2013) first 'flaw' is problematic for pretty elementary reasons. It's common knowledge that all manner of fossil terrestrial animals occur in aquatic environments because that's where the majority of continental sediments accumulate. Azhdarchids routinely occur in aquatic deposits with the likes of dinosaurs, reptiles, birds and so on, but we don't assume the latter are tied to water simply because their fossils are found in ancient rivers and lakes. Ergo, we shouldn't assume this for azhdarchids either. Taphonomy does not necessarily correlate with palaeobiology. Moreover, it's not true that all azhdarchids are found in remnants of aquatic settings: some occur in ancient deserts and ash beds. There's not much else to say on this fairly basic point (check out the paper if you want to read our full response), so we'll get onto the more interesting stuff.

Killer storks, giant pterosaurs, and the Age of MurderDeathReptiles
A number of folks have asked us about the vulnerability of grounded pterosaurs to predators, and Averianov (2013) specifically mentions the problems azhdarchids would have taking off when faced with attackers ("It is hardly probable that huge azhdarchids could take wing in one go and running for acceleration is difficult in marshland conditions” - Averianov 2013, p. 207). As we note in our new paper, palaeobehaviour is hard to discuss in a truly scientific manner and we are wary of just making bold, arm-wavy comments about ancient predator-prey interactions. There are some comments we can make, however, which do not rely on crass speculation.

Firstly, modern ideas of pterosaur takeoff (which regular pterosaurophiles will know means quadrupedal launching) suggest these animals could become airborne in seconds from a standing start (contra Averianov 2013). Thus, there is little reason to think that azhdarchids - or any other pterosaurs - would have to engage in panicked running to escape predators. Quad launches also permit greater acceleration and power than bipedal launches. This may make pterosaurs actually more adept at turning tail from predators than large modern birds, which do have to engage in a little taxiing before becoming airborne. We therefore do not envisage that grounded pterosaurs - even giant azhdarchids - would struggle to escape predators when startled.

According to some, this is pretty much what the Mesozoic looked like all the time. Background borrowed from here.
We also note that while terrestrial stalking is considered an unusual lifestyle for pterosaurs, comparable ecologies are actually pretty common among modern birds. Indeed, a lifestyle of walking around and eating stuff found on the ground seems to be the 'default' foraging strategy for many bird groups, and there's no indication that this makes them atypically vulnerable to predation. This even applies to large birds which live in predator-rich environments, where big cats, dogs, hyenas and other predatory species are real dangers. We have to ask why Mesozoic ecosystems would be any different? Is it because ancient reptiles are generally portrayed as aggressive monsters who're constantly pitched in battle (above)? Maybe, but this is almost certainly wrong. Darren communicates this very clearly in our new paper:
"...the idea of azhdarchids may have been highly vulnerable to terrestrial predation labours under several probably erroneous assumptions, including viewing theropods as unstoppable killing machines, immediately pouncing on and devouring any grounded pterosaur. In point of fact, the behaviour of living predators indicates that theropods large and small likely exploited easy prey (Hone and Rauhut 2010), ignored or avoided large or awkward prey, and were not a perpetual, 24-hour menace across all environments, worldwide." Witton and Naish 2013 (In Press)
I've discussed the over-statement of aggressive behaviour of Mesozoic animals several times before, and I'm sure I'm not alone in finding portrayal of dinosaurs as angry murder/death/kill machines irritating. It's frustrating enough when seen in popular media, but particularly irksome when it seemingly influences scientific discussions. I don't want to understate predation risks, but modern animals demonstrate that behaviours like extended bouts of foraging, resting and socialising can be performed without being ripped to pieces by passing predators. Assuming the Mesozoic operated under the same basic principles, it almost certainly wasn't the 190 million year bloodbath it's often made out to be.

A giant pterosaur compared to top theropod carnivores of giant azhdarchid-bearing Late Cretaceous ecosystems. A, Tyrannosaurus rex, representing the largest known predator in Maastrichtian North America; B, Balaur bondoc, largest predatory theropod of Maastrichtian Romania; C, Arambourgiania philadelphiae, standing in for the similarly-sized azhdarchids which lived alongside A and B, respectively; D, human sleuth for scale. From Witton and Naish (2013).

The composition of azhdarchid-bearing faunas is also of interest here (above). In some parts of time and space, enormous, 10 m wingspan azhdarchids lived alongside large predators like tyrannosaurids and spinosaurids. In others, the biggest theropods were turkey-sized. In fact, in latest Cretaceous European deposits, azhdarchids are the biggest predatory animals by a huge margin, and unlikely to be bothered by any theropods once they grew beyond a certain size. In these settings, azhdarchids weren't in perpetual trouble from theropods: they were perpetual trouble for theropods. Heck, the sheer size of an adult giant azhdarchid is impressive even alongside the very largest carnivores, and we wonder if this alone would dissuade less ambitious predators. Of course, there are plenty of small azhdarchid species which may be somewhat more easily subdued by theropods, and there are plenty of faunas were azhdarchids are not large, dominant species, but it's worth stressing that some azhdarchids lived in settings devoid of serious predator risk.

Of course, there were likely some occasions when azhdarchids were caught out by predators: would this spell instant doom for the pterosaur? Not necessarily. Again, this is hard to say with confidence, but we note that large modern storks - which resemble azhdarchids more than any other modern species - can be far more dangerous than most folks realise. These birds can inflict severe, sometimes fatal injuries with their beaks when panicked and cornered. Children are seriously wounded or even killed by marabou storks when trying to harvest soft white contour feathers from these usually calm birds (Mackay 1950). Zoo staff routinely arm themselves against attack from captive jabiru storks because attacks are so frequent and vicious (Shannon 1987). Indeed, even relatively large animals like tapirs are no match for angry jabirus. These storks are not armed with razor-sharp, hooked beaks: they deliver this damage with their simple, long, pointed bills. Whether this means azhdarchids used their jaws as similarly formidable weapons is anyone's guess, but it demonstrates that azhdarchid-like bills can be used as fearsome predator deterrents if wielded properly. Remember, of course, that some azhdarchids probably had beaks over 2 m long, 6-8 times longer than those of even the largest modern storks. An giant azhdarchid in a bad mood may be well worth avoiding.

We have some additional discussion on this point in our MS, but I think you get the gist of what we're saying. Our bottom line is not that azhdarchids could wander about Cretaceous plains without a care in the world, just that there is no reason to assume they were overtly vulnerable to predation risks. Indeed, there is evidence to quite the opposite in several cases, and there is no reason to think this is a flaw in the terrestrial stalker hypothesis.

The scoop-feeding pelican-mimic thing
This does not mean, of course, that azhdarchids had to be terrestrial stalkers just because they could walk around without being eaten immediately: water-trawling 'scoop feeding' could still be a viable alternative to terrestrial stalking. Citing the helical jaw joint of azhdarchids as evidence for a pelican-like expanding throat region, Averianov (2013)'s summation of his azhdarchid feeding hypothesis reads:
"...azhdarchids flied [sic] slowly above the water surface of large inland water bodies… looking out for fish or small fish shoals. As prey is detected, they opened the mouth, expanding the throat sac due to the spiral jaw joint, and captured fish in this scoop net, formed by the jaw rami and throat sac. Then, the head was thrown abruptly back by extension of the neck in the posterior region and prey was swallowed.” Averianov 2013, p. 209 
Although far from the first author to compare pterosaur and pelican jaws favourably, this is the first time (to my knowledge) that specifically pelican-like throat expansion has been proposed for pterosaurs and linked to a certain foraging strategy. The exact method of foraging suggested here - a mix of 'scoop' and skim-feeding - does not have a modern representative but is clearly an 'extreme' lifestyle, likely to incur considerable loading on azhdarchid skulls, jaws and neck. As with some other proposed 'extreme' azhdarchid lifestyles, like skim-feeding, we'd expect to see considerable specialisation in azhdarchid anatomy to reflect this but, unfortunately, we don't. Indeed, our assessment of this feeding mechanism suggests it is fraught with biomechanical and functional problems, in addition to failing tests offered by comparative anatomy.

Extending jaw area measurements of the brown pelican and select azhdarchid pterosaurs. Note the pelican is being rather lazy with it's jaw bowing, and yet still achieves much greater area increase than the azhdarchids. From Witton and Naish (2013).
We investigated the plausibility of 'scoop-feeding' in several ways. Firstly, we measured flexed and unflexed jaw areas of azhdarchids and pelicans to compare their range of jaw expansion (above). It turns out that azhdarchid jaws achieve pretty negligible amounts of jaw area increase even when an unrealistic amount of jaw flexion is permitted. By contrast, a bowed pelican jaw achieves an enormous area increase even when not trying very hard: we could only measure a partially bowed pelican jaw, but even this left pterosaur jaw expansion looking pretty pathetic. We utilised the same area measurements of azhdarchid jaws to calculate drag forces incurred on an azhdarchid neck during the 'scoop' phase of foraging, when the entire mandible has to be ploughed through the water. Unsurprisingly, the resultant drag forces were pretty huge, and are several hundreds times higher than the strain permissible by an azhdarchid fifth neck vertebra (hat tip to Mike Habib for suggesting using our jaw area data in this way). An azhdarchid that lowered its jaw into the water to try 'scoop feeding' would die a horrible, horrible death. This, of course, has further negative implications on the idea that azhdarchids were skim-feeders: even partial submersion of their mandibles was likely to snap their necks.

Brown pelican jaws in action. From Schreiber et al. (1975)
As if it didn't look bleak enough for 'scoop feeding', things took a turn for the worse when we compared azhdarchid and pelican jaw anatomy. Pelican mandibles and throats are amazingly freaky and specialised, and these adaptations directly relate to their manner of grabbing prey (above). Their foraging adaptations include differentially mineralised jaw bones which create distinct 'hinges' at points along the jaw; short mandibular symphyses; loosely-jointed posterior jaw bones; super-elastic throat tissues; reduction of the tongue, and skin-like beak tissues which permit jaw flexion. At least some of these features should be detectable in jaw fossils, but no indication of similar adaptations are found in azhdarchid jaws. In fact, directly opposing anatomies are seen in most instances. But what of the helical jaw joint? Isn't that functionally significant? Probably not, because helical jaw joints are far from unique to azhdarchids, being seen across all manner of archosaurs. Given the range of ecologies encapsulated by archosaurs with helical jaw joints, they're clearly of questionable, if any, significance to foraging strategies. It seems that the potential for azhdarchid jaws to perform expanding actions are limited at best, and we should stop referring to their gently-bowing mandibular rami as being 'pelican-like': they're really nothing of the sort. Indeed, the only animals we know of with even remotely pelican-like jaws are rorqual whales. I could go on (and we do in the paper), but I guess it's already clear that we don't consider 'scoop feeding' a viable alternative to terrestrial stalking at all.
Extreme lifestyles require extreme anatomies. Here's a summary of what you need to be a skim-feeding species, according to the modern skimming bird, Rynchops. From this post.
A closing point
In sum, we more-or-less go full circle in our new study, coming back to terrestrial stalking as the most likely current interpretation of azhdarchid palaeecology. Reflecting on this study, and the other studies into pterosaur palaeoecology I've been involved with (Humphries et al. 2007; Witton and Naish 2008, 2013; Witton 2012), it strikes me that proposed 'extreme' foraging methods are almost always inferred from a few anatomical characteristics rather than entire bauplans. This is certainly the case for 'scoop feeding' and skim-feeding (e.g. Kellner and Langston 1996; Martill 1997; Averianov 2013). Why do we keep doing this? It almost seems that our default assumption for pterosaurs is that they lived crazy, outlandish lives which we select evidence to verify. This is a completely backwards and unscientific way of assessing ancient animal habits. Modern animals with 'extreme' lifestyles wear their adaptations across their bodies, suggesting that we need to look at the entire picture of extinct species before we propose our palaeoecological interpretations (see details on skim-feeding adaptations, above). Folks like myself and Darren currently champion the terrestrial stalker hypothesis not because it's our 'pet idea', but because it's currently the only hypothesis which considers the entire azhdarchid bauplan (see our infographic at the top of the post), is consistent with biomechanical or functional parameters of azhdarchid anatomy and matches lifestyle predictions made through comparative anatomy. It may well not be the last word on this topic, but at least there's a foundation of science to it, which is more than can be said for a lot of proposed pterosaur lifestyles (see Witton 2013 for a review). If we're expecting to understand the palaeoecology of these animals in detail, we really have to move away from our rather basic, selective interpretations of their anatomy and provide more detailed, dedicated assessments.

I'll have to stop there for now. Be sure to check out the rest of Witton and Naish (2013) for further details on this study and, for more on pterosaur palaeoecology and azhdarchids in general, you may want to check my book (Witton 2013).

References
  • Averianov, A. O. (2013). Reconstruction of the neck of Azhdarcho lancicollis and lifestyle of azhdarchids (Pterosauria, Azhdarchidae). Paleontological Journal, 47(2), 203-209.
  • Humphries, S., Bonser, R. H., Witton, M. P., & Martill, D. M. (2007). Did pterosaurs feed by skimming? Physical modelling and anatomical evaluation of an unusual feeding method. PLoS biology, 5(8), e204.
  • Kellner, A. W., & Langston Jr, W. (1996). Cranial remains of Quetzalcoatlus (Pterosauria, Azhdarchidae) from Late Cretaceous sediments of Big Bend National Park, Texas. Journal of Vertebrate Paleontology, 16, 222-231.
  • Mackay, H. (1950). The quaint Marabou stork. Zoo Life 5, 91-92.
  • Martill, D. M. (1997). From hypothesis to fact in a flight of fancy: The responsibility of the popular scientific media. Geology Today, 13, 71-73.
  • Schreiber, R. W., Woolfenden, G. E. & Curtsinger, W. E. (1975). Prey capture by the Brown Pelican. The Auk, 92(4), 649-654.
  • Shannon, P. W. (1987) The Jabiru Stork (Jabiru mycteria) in zoo collections in the United States. Colonial Waterbirds 10, 242-250.
  • Witton, M. P. (2012). New insights into the skull of Istiodactylus latidens (Ornithocheiroidea, Pterodactyloidea). PloS One, 7(3), e33170.
  • Witton, M. P. (2013). Pterosaurs: Natural History, Evolution, Anatomy. Princeton University Press.
  • Witton, M. P., & Naish, D. (2008). A reappraisal of azhdarchid pterosaur functional morphology and paleoecology. PLoS One, 3(5), e2271.
  • Witton, M. P. & Naish, D. (2013) Azhdarchid pterosaurs: water-trawling pelican mimics or "terrestrial stalkers? Acta Palaeontologica Polonica (in press)

Monday, 14 October 2013

Marine reptiles behaving badly: freshwater(ish) Wealden plesiosaurs

Mother and calf Leptocleidus superstes, a freshwater leptocleidid plesiosaur, explore a swampy river inlet in Lower Cretaeceous Sussex. Of course, a real swampy scene should probably be drawn showing an impenetrable amount of suspended sediment and goo with, possibly, some plesiosaur-shaped silhouettes, but that would make for a lousy image. Prints of this image are available.
For various reasons, I've recently taken an interest in the plesiosaurs of the Wealden Supergroup. The latter will need no introduction to many readers here, being a very famous succession of Lower Cretaceous sediments which provide one of the best known dinosaur faunas in Europe, along with a diverse array of pterosaurs, crocodilians, amphibians, fish and, well, all sorts of things. The big deal about Wealden plesiosaurs is that they represent - gasp! - freshwater and brackish species rather than the marine variants we're more familiar with. Reading into these animals has been pretty fascinating and resulted in the generation of the following text and images presented here. My hope is that these will one day have a 'proper' home, but they'll have to sit here and wait for the meanwhile. The text below has been targeted at a fairly general audience and may not contain anything new for some readers, and doesn't contain citations. If, however, you're after more Wealden plesiosaurs (and who isn't?) with an authoritative twist, you'll want to be sure to check out this Tetrapod Zoology post and, of course, Adam Stuart Smith's Golden Trilobite Web Award winning-Plesiosaur Directory. If Mesozoic marine animals are your thing, you may also want to check out these posts on Ophthalmosaurus and the Oxford Clay fauna.

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Plesiosaurs are well-known aquatic Mesozoic reptiles characterised by their four large flippers and variably developed necks and heads. Their anatomy is completely unlike that of any other swimming animal, with barrel-shaped bodies tightly locked together by large, plate-like limb girdles which bore robust, powerfully muscled paddles. These flippers, highly modified limbs which are of no use on land, were entirely responsible for propelling plesiosaurs through water, their tails being relatively short and of apparent little assistance in underwater propulsion. This group, more correctly termed 'Plesiosauria’, has long been recognised as falling into two lineages: the pliosauroids and plesiosauroids. Some pliosauroids were super-predators like Liopleurodon and Pliosaurus, animals with likely stretched between 7 - 10 m in length with enormous skulls and jaws. These animals were likely top predators of many marine settings, hunting other large swimming vertebrates. Most pliosauroids bore relatively short necks but, in contrast, several plesiosauroid lineages – including famous species like Elasmosaurus, Cryptoclidus, and Plesiosaurus – developed long necks and small heads, ideal for foraging on relatively small fish and squid. Neck and skull proportions were once taken as a clear indicator of which group a given plesiosaur would belong to, but this idea has fallen from favour as the complexity of plesiosaur evolution has become apparent.

We mostly imagine these reptiles as sea- and ocean-going animals, making their occurrence in freshwater and brackish facies like those of the Wealden seem unexpected. Plesiosauria was a successful and adaptable group however, with a complex evolution that ran for 135 million years from the Late Triassic (c. 200 Ma) to the end Cretaceous (66 Ma) and included acclimatising to waters across the entire planet. Although plesiosaurs are undoubtedly mostly marine, they can be found in freshwater and brackish habitats throughout much of their history. Indeed, it seems that plesiosaurs invaded near-shore and freshwater habits on multiple occasions, although the catalyst of these invasions remains unknown. Did they thrive in environments free of large aquatic predators? Were they exploiting untapped niches and food sources? More data is required to answer these questions.

Skull reconstruction of Leptocleidus capensis, an Early Cretaceous leptocleidid from South Africa. The skull of L. superstes was probably pretty similar to this. Based on illustrations in Cruickshank (1997).
Wealden plesiosaur fossils are not particularly common. Most are isolated vertebrae, fragmentary limb bones and teeth, with only a handful of partial articulated skeletons and skulls known. These remains are important to palaeontologists because the Lower Cretaceous record of plesiosaurs is rather sparse, so Wealden plesiosaurs – rare as they are - provide an important window into this phase of plesiosaur evolution. Plesiosaur remains are span the entire Wealden stratigraphy and occur in both sub-basins, suggesting that they were long-term denizens of Wealden ecosystems. Three species of Wealden plesiosaur are currently recognised, each known by incomplete skeletons: Leptocleidus superstes (Upper Weald Clay Formation, East Sussex; also see the image above), Vectocleidus pastorum (Vectis Formation, Isle of Wight) and Hastanectes valdensis (Wadhurst Clay Formation, Hastings). Some fragmentary Wealden plesiosaur fossils clearly differ from these animals and likely represent additional, poorly known species.

Leptocleidus and Vectocleidus belong to a plesiosaur group known as Leptocleididae, an unusual lineage of Late Jurassic – Early Cretaceous plesiosaurs with necks of short or moderate length and relatively small skulls. This anatomy represents an ‘intermediate’ grade between the short-necked pliosauroids and long-necked plesiosauroids, which has caused some confusion about their relationships to other plesiosaurs. Some suggest they are a ‘relict’ lineage of early, generalised pliosauroids, but other proposal consider them derived plesiosaurids which abandoned long-necked morphologies in favour of a more generalised body plan. Whatever they are, it is noteworthy that all known leptocleidid fossils are known from freshwater, brackish or near-shore environments, suggesting they abandoned the more typical plesiosaur existence of life in open waters and spent much of their time in lakes, rivers and coastlines. This would make leptocleidids comparable to some modern seals (including Baikal seals, several types of ringed seal and harbour seals) and dolphins (such as the Irrawaddy dolphins; Baiji, Chinese river dolphin, and Tucuxi, Amazonian river dolphins) which have abandoned pelagic lifestyles or, at least, make considerable incursions up estuaries and rivers in search of food. Indeed, seals and river dolphins may be the best modern ecological analogues to Wealden leptocleidids. The skulls and jaws of these plesiosaurs were equipped with large jaw muscles and conical, partially serrated teeth, ideally suited to feeding on a small bodied prey. Their diet probably mostly comprised fish, supplemented by opportunistic taking of other, small swimming animals. The four-flippered propulsion system of plesiosaurs may have been ideally suited to navigating complex and tight underwater habits in pursuit of cryptic prey, permitting for excellent manoeuvrability as well as bursts of speed.

Skeletal reconstructions of mother and foetal Polycotylus latippinus, polycotylid plesiosaurs which are not a million miles away, phylogenetically speaking, from leptocleidids. Was this strategy of birthing solitary, large calves found in leptocleidids - and other plesiosaurs for that matter - as well? From O'Keefe and Chiappe 2011; image from here.
At least Leptocleidus was a fairly large animal for the Wealden waterways, attaining body lengths of around 3 m. This size may have dissuaded attacks from even the largest Wealden aquatic and semiaquatic predators, but the same cannot be said for their calves. ‘Calves’ is an appropriate word here: fossils of Late Cretaceous plesiosaurs (which happen to be closely related to leptocleidids) show that at least some plesiosaurs did not lay eggs like many other reptiles, but instead gave birth to a solitary, large and very well developed baby. This reproductive strategy is extremely similar to that of large mammals but is virtually unheard of in reptiles. Although live births are known in many modern lizards and snakes, only a few modern reptiles (various types of skinks) are known to produce a single, large and highly developed offspring. The development of such reproductive strategies in plesiosaurs is therefore rather remarkable (though we must be mindful that we do not know how common this strategy was across Plesiosauria). Both mammals and reptiles that invest heavily in a single offspring are highly social and engage in maternal care, which may indicate that adult plesiosaurs did the same. Perhaps Wealden leptocleidids protected their young from predators, warding off attacks from marauding goniopholidids crocodilians and other plesiosaurs until they were large enough to look after themselves.
Hastanectes valdensis: a possible pliosaur which, even at only 2 m long, is good reason not to paddle in Wealden waterways. Especially if you're a small crocodile.
Such predatory attempts may have been attempted by our third Wealden plesiosaur, Hastanectes (above). Some have suggested that Hastanectes is a pliosaurid rather than a leptocleidid, and closely related to the large, powerful members of this lineage with short-necks and large skulls armed with tusk-like teeth. If so, Hastanectes may represent a small (2 m long) version of these predators. Interestingly, no Hastanectes specimens currently known represent fully-grown animals, suggesting it may have grown somewhat larger. Even at 2 m in length, such a pliosaur would be keen predator of small and medium-sized swimming creatures in Wealden waters, perhaps taking not only fish but also regularly hunting other reptiles. This interpretation of Hastanectes has not gone unchallenged, however: some very recent studies have suggested it represents another Wealden leptocleidid.

A fourth, and largely mysterious type of Wealden plesiosaur is represented by very scant remains indeed. A solitary vertebra from the Hastings Group hints at the presence of a long-necked plesiosauroid within the Wealden. Exactly what sort of plesiosaur this represents however, and how it may have functioned within the Wealden palaeoecosystem, is unknown at present.

References
  • Cruickshank, A. R. I. (1997). A lower Cretaceous pliosauroid from South Africa. Annals of the South African Museum 105, 207–226.
  • O’Keefe, F. R. & Chiappe, L. M. (2011). Viviparity and K-selected life history in a Mesozoic marine plesiosaur (Reptilia, Sauropterygia). Science 333, 870-873.

Wednesday, 2 October 2013

What neck-biting Tyrannosaurus sex tells us about speculation in palaeoart

Head and neck biting sexual behaviour in Tyrannosaurus rex. A novel, brutal and undeniably speculative reconstruction for tyrannosaurs, sure, but is it the result of pure, unbridled palaeoartistic license, or is there something more to it?
It seems that "speculation" is the current word on everyone's lips in palaeoartistic circles. Thanks largely to the enormous success of All Yesterdays, and the recent unveiling of its sequel, All Your Yesterdays, palaeoartists across the internet have been buzzing with excitement over the possibilities opened by speculative leaps of logic. This is undoubtedly a Good Thing. I wrote almost a year ago about why I thought All Yesterdays and the ideas it embodied were great, and a must-see for anyone interested in vertebrate palaeontology or palaeoart. I stand by that, and am certain that many of us in the palaeoart community have be positively influenced by this project in the way we recreate extinct species. All Yesterdays revelled in speculation about prehistory, arguing that we were not being open-minded enough about our depictions of animal appearance and behaviour. The crux, as anyone reading this probably knows, is that many 'traditional' palaeoart concepts are likely erroneous by being overly conservative, and thus 'fail' at both restoring ancient life and producing convincing looking animals. In addition, All Yesterdays highlighted a number of conventions which had become tropes within palaeoart, and argued palaeoartists produce far more accurate studies of extinct life when these clichés are broken, not to mention more interesting ones. What gave All Yesterdays such a strong message was that it, for the most part, was scientifically sound, cleverly turning conventions on their head or showing us logical, plausible ancient phenomena that we'd not imagined before.

For the All Yesterdays sequel, All Your Yesterdays, we see a minority of palaeoartists reaching further than it's predecessor dared, showing some very elaborate anatomies and lifestyles which may, in my opinion, go further than reasonable inference, even enhanced with speculation, may allow. Before we get any further, I want to stress that this post is not a review of All Your Yesterdays. I enjoyed the book, and think it's well worth seeking out for a look at for some excellent and thought provoking imagery. But yes, it does contain a few images which made me question this newfound speculative approach to palaeoart. We have to bear in mind that All Your Yesterdays was crowdsourced, the result of a contest for "original, creative concepts that are at least partially in-line with our current understanding of extinct animals" from Irregular Books. This is naturally going to draw a range of knowledge bases, some of which may be more comprehensive than others, and it may be that some of the more eyebrow-raising images therein are simple mistakes. I'm not going to name names here, because I gather the artists behind All Your Yesterdays were not aware that their work was going to be showcased as a 'significant' addition to the All Yesterdays canon, but I'll hint that molluscan salinity tolerances, the nesting habits in pterosaurs, the soft-tissues of spinosaurids, hadrosaurs and thyreophorans, and the evolution of viviparity were just some things which prompted this post. It's important to stress that problematic 'overspeculations' are not confined to a few pieces in All Your Yesterdays, but a small but noticeable chunk of post-All Yesterdays palaeoartworks which, arguably, jump the palaeoart shark. It's these artworks I want to focus on here.

Getting introspective with speculation
Chiefly, some artwork inspired by All Yesterdays seems to take license for increased palaeoartistic speculation as a sign that 'anything is possible in nature', without any real consideration for how likely some possibilities are. Other pieces showcase strange anatomies for the sole purpose of contrasting with more traditional standard depictions, without considering why such reconstructions are common in the first place. These works, presented as part of a movement that I think I understand and agree with, have gone beyond the science which has to underpin any recreation of an extinct being. The question is, how much speculation we can use before our work stops being palaeoart and starts being fantasy images starring extinct species?

Detail of neck biting Tyrannosaurus. I'm sure he's got a great personality.
Of course, I'm not the first person to ponder this. Indeed, the inspiration for this post, All Your Yesterdays, muses on this same issue:
"In short, speculation in palaeoart should be seen as a sliding scale. At which point does a speculation render itself too extreme? And is it even possible to reach said extreme given the ridiculous soft tissue structures and absurd behaviours present in the modern world? It is, in fact, surprisingly difficult to come up with a speculative piece of palaeoart that is unconditionally ridiculous (at least, so long as the basic rules of anatomy, biology and physics are applied, as they are in science-based reconstructions)."
All Your Yesterdays, p. 7  

These words contrast with a few comments online. Amid the near-universal acclaim for All Yesterdays, one or two (and three, four, five) folks have made about palaeoartistic speculation running away with itself, a far cry from the suggestion that palaeoart can never, so long as basic science is followed, be too ridiculous. It seems there's some need, then, for discussion about the appropriateness of speculation in palaeoart: how it should inform our work, how far we can take it, and whether all speculations are equal. After ruminating on this for a couple of days, it seems that the best way to tackle this is by dividing palaeoartistic speculation into three categories (as with any classification of an organic, creative process, are best perhaps viewed as major points a continuum), which I'll call primary, secondary and tertiary. These distinctions effectively denote how far depicted ideas stray from actual data. We'll outline these types of speculation first, and then discuss their use below.

Primary speculations
Speculations directly based on fossil data, whereby the evidence for a behaviour, event or anatomical feature is reasonable, but details may be murky and require some imagination to restore. Gut content, pathological bones and complex track sites are good examples of evidence which can be used to inspire palaeoart using primary speculation. We may not know the entire truth behind these fossils, but we can whittle it down to a few very likely possibilities. Basic elaboration of predicted integument of an animal - making fluffy integuments long or short, altering distribution and so forth - would be an example of primary speculation on anatomy, as would adding things like wattles, skin-folds and other likely anatomical details to reconstructions. With primary speculations, we can be more-or-less entirely confident that we're displaying a degree of truth in our work.

Secondary speculations
Speculations not directly supported by fossil data, but operate within our spectrum of knowledge to maintain a degree of plausibility. This may include extrapolation of common behaviours and, to a limited extent, elaborate anatomies from closely related animals to reconstructed species. Extrapolating some behaviours from or close ecological, anatomical or biomechanical analogues may fall into this camp too. Ritualised behaviours (below), unusual ways of dying and foraging on unexpected food sources are good examples. Depicted behaviours may serve to show the function of prominent anatomies. Slightly unusual interpretations of integument and other body tissues (perhaps as responses to climate, seasons, sexual selection etc.) probably fall into this category, so long as they are consistent with the integuments known within a 'reasonable' phylogenetic bracket. In short: speculations which adorn fossil species with features so fundamental to animal existence that, even in the absence of fossil data, we can be confident they occurred in deep time.

Ritualised courting chaoyangopterid pterosaurs, Lacusovagus magnificens. Did pterosaurs do this? There's no direct fossil evidence for it, but the abundance of ritualised mating behaviour in modern animals suggests we can be relatively confident that they, and other fossil species, used complex ritualised behaviour. This undoubted speculation gains indirect support from the broad array of sociosexual devices we see on many fossil species, and hints of ancient sexual dimorphism, both of which indicate sexual behaviours were as complex and sophisticated in prehistory as they are today. Image from Witton (2013).
Tertiary speculations
Speculations operating completely outside, and sometimes contradicting, fossil data. May rely entirely on application of very specific modern animal behaviours and anatomies to fossil species, often transferring rare, sometimes highly specialised lifestyles to fossil animals. There is no particular logic or reason behind these applications: they are entirely arbitrary. In other cases, complex biologies and life histories are invented for fossil taxa. Creation of soft-tissue anatomies without, or in spite of, consideration of underlying musculoskeletal system and/or soft-tissue fossil data. Reliant on the absence of data concerning fossil species, because 'anything is possible'. Hypothetical examples of such speculations are things like lactating dinosaurs, notosuchians with trunks, an egg-laying Deinotherium, hadrosaurs with antler-like structures growing atop their crests. Jaime Headden's woolly ankylosaur, his cautionary 'mess of speculation', is a knowing graphic example of tertiary speculations gone mad.

Speculations, what are they good for?
If these are the tools of the speculative palaeoartist, what are their application? Anyone familiar with palaeoartistic practises will recognise that the former two grades of speculation are standard tenets of palaeoart. Such speculations provide our leaps of logic into prehistory and, without them, palaeoart would be an pretty limited endeavour, probably entirely formed of musculoskeletal reconstructions. It's important to recognise that such speculations were not originated by All Yesterdays, as primary and secondary speculations have always been used in palaeoart. The masterstroke of All Yesterdays was to show how primary and secondary speculations could be bolder and more imaginative than most mainstream palaeoart suggested. The result is artwork which is both interesting, unique and supported by actual data.

The image at the top of this post is the result of such an inference. It's well known that many large theropods engaged in head-biting behaviour, and some specimens of Tyrannosaurus (including BHI 3033, better known as the common T. rex museum mount 'Stan') bear particularly extensive damage to their posterior skulls. The inference made here is that Tyrannosaurus engaged in aggressive head and neck biting during copulation, a widely seen behaviour among vertebrates that can often involve substantial damage to the head and neck of the female, sometimes leading to death. I'm not the first to envision this behaviour for tyrannosaurids. Tanke and Currie (1998) suggested nuptial biting as a cause of tyrannosaurid head pathologies but suggested it was refuted by the apparent small size (50% of full size) of many tyrannosaurids with head wounds. Of course, it now seems that dinosaurs became sexually mature when only half grown (Erickson et al. 2007), so this hypothesis may be back on the table. The resultant image is a radical and speculative depiction of Tyrannosaurus behaviour, but one that has a foot firmly set in science.

Cast of the skull of Tyrannosaurus 'Stan', BHI 3033, at in the Oxford University Museum. Stan's skeleton is particularly damaged around the posterior head and neck region, with a probable tooth wound penetrating it's braincase, a smashed postorbital bar (a dorsal projection of tyrannosaur skulls which anchored neck muscles) and broken neck vertebrae. Photograph by Marc Vincent, from Love in the Time of Chasmosaurs.
The same cannot be said for tertiary speculations. Some inferences made at this level are so far removed from actual data that they have little or no evidence to support them, and thus abandon the scientific basis which should underpin any palaeoart. Others may disagree, but I think good palaeoart, like good science, is led primarily by evidence, not speculation. This most obviously impacts tertiary speculations which arise, it seems, for the sole purpose of overturning convention. "This animal is always shown like/doing this... what if it looked like/did THIS SHOCKING THING?!??" While there's nothing wrong with trying to keep palaeoart fresh, we should remind ourselves that not everything common in palaeoart is a trope or meme, or the product of unimaginative artists. Sometimes, that's just how animals were, and conventions are based in very sound evidence. Deviating from these conventions is a move away from data, which is the exact opposite of what we want to be doing here.

Other tertiary speculations apply highly unusual behaviours borrowed from modern animals, or those which are entirely made up, to fossil species for no clear reason. This can be effective on occasion, presenting a fossil species in a radical light which may make us reconsider our preconceived notions of that species, but I'm generally not a fan. Why, of all the behaviours that we can imagine or observe in in the modern day, should we chose that specific animal as a model? And do we really expect the rarest, most elaborate and weirdest behaviours to be present in specific fossil animals? Are we actually predicting that extinct animals behaved (often adorned with the same colour schemes and patterns) exactly like these aberrant modern animals? We'll score far more science points if we apply more widespread behavioural phenomena to our palaeoart. This doesn't mean we have to confine ourselves to dull behaviours like travelling and foraging, because we can also rely on primary and secondary-level speculations to give us behaviours like resting, taking care of personal hygiene, reproducing, interacting with one another and so on. Likewise, lots of interesting anatomies can be extrapolated from the fossil record itself. In sum, while we should take inspiration from modern taxa, arbitrarily 'transforming' fossil animals into ancient versions of modern species stretches credibility quite far, and is perhaps a rather unscientific approach to our work (this point echoes one made earlier, also in response to some art in All Your Yesterdays, at Laelaps).

A counterargument could be made that tertiary speculations allow us to imagine how sophisticated and complex ancient worlds were but, again, I question this. Like any guesswork, they're of questionable significance. Unknowns are unknowns. Tertiary-grade restorations are as likely to be incorrect as accurate. These depictions may fire the imagination briefly, but the flames are tiny compared to those fuelled by cool ancient behaviour derived from actual evidence. It's one thing to see a shocking piece of palaeoart, but quite another to realise that there's actually tangible evidence behind it. Rather than pondering the great unknowns of deep time when confronted with a tertiary speculation, I frequently react with the opposite approach, thinking about what we can actually deduce about a given issue, and what a more likely interpretation may be.

Why I find tertiary speculations frustrating. The fossil record is full of interesting animals with known interesting behaviours, like these burrowing Oryctodromeus, and yet they are frequently overlooked in palaeoart for entirely speculative renditions of familiar taxa. Check out this post for more on this animal and it's need for a PR campaign.
This brings us to a more pragmatic bugbear about tertiary speculations. Extremely speculative palaeoartworks are actually fairly common, at least online, while innumerable cool palaeontological topics with a significant factual basis are completely ignored. Why use art to make rather hollow points about unknown topics when there's plenty of art to be made concerning subjects we do know about? Even familiar animals have unusual, rarely-depicted behaviours which we can infer from fossils with minimal amounts of speculation (such as the tyrannosaurs above), not to mention the shedloads of fossil species which are wholly unrepresented in art (and yes, I'm well aware of the hypocrisy of saying this in a post featuring Tyrannosaurus), many of which are also known to have interesting and unusual behaviours. Heck, it's common knowledge that palaeoart is heavily biased towards a few taxa, so just showing some of these rarely seen animals would be a thought-provoking, cliché-busting achievement in itself. Is it not better, as scientific illustrators, to base our work on what we know rather than what we don't?

Which leads to...
So, yes, despite being an advocate of using speculation in palaeoart, I'm not a huge fan of the extreme and uncontrolled speculation we're seeing creeping into modern portfolios. This may sound like I'm jumping off the All Yesterdays bandwagon, but I don't think I am. Most of our best palaeoartists - including those behind All Yesterdays - use speculation of primary or secondary grade, and are more notable for avoiding clichés and artistic conventions than they are for presenting highly speculative lifestyles and anatomies in fossil species. They elaborate existing knowledge to create more convincing depictions of fossil animals, and apply detailed research of the fossil record to show us sights we've never seen before. Some of their work may seem outlandish and brash, but it's actually far more measured than it looks.

I'm sum my point up as this. While we should be using speculation to push palaeoart to its limits, we need to know both which bits we can push, and when to stop before our speculations get the better of our work. This doesn't deny us licence to make our reconstructed ancient worlds amazing and interesting and, in fact, it may make our work more striking. It's one thing to see an outlandish reconstruction of the past, but all the more poignant when we realise the weird, strange or even shocking visage before us is based on truths, and not just imagination.

References
  • Erickson, G. M., Rogers, K. C., Varricchio, D. J., Norell, M. A., & Xu, X. (2007). Growth patterns in brooding dinosaurs reveals the timing of sexual maturity in non-avian dinosaurs and genesis of the avian condition. Biology Letters, 3(5), 558-561.
  • Tanke, D. H., & Currie, P. J. (1998). Head-biting behavior in theropod dinosaurs: paleopathological evidence. Gaia, 15, 167-184.
  • Witton, M. P. (2013). Pterosaurs: Natural History, Evolution, Anatomy. Princeton University Press.