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II CLPV talk summaries: Day 2
Bom dia DMLers!
First, let me send a special shout out to Adam Yates; we missed you!
III CLPV is in Argentina in 2008, so start making plans (that goes for
the rest of you too!).
I must confess that I missed the second banquet. I was exhausted and I
had to take care of some work-related emails, so I won?t be able to
provide the skinny on the second social event. By all reports it was
also fantastic, and I was a fool (albeit a rested fool?) to have missed
it. The morning session was a symposium on Early Dinosaur Evolution,
and it had some of the most exciting talks of the conference. On to
the talks:
Day II: Thursday the 11th.
Regina Fechner examined the functional morphology of Lagerpeton. She
presented a very good morphological overview of the known remains, and
then made comparisons to facultatively bipedal lizards, from which she
concluded that Lagerpeton was likely not very erect in its stance, and
that when it engaged in bipedal locomotion it likely relied on lateral
undulation to increase hind-leg stride, again as in extant lizards that
are facultative bipeds. If I may editorialize for a moment; I?m not
prepared to say she is wrong, but I was unconvinced by her
justifications for using lizard mycology and locomotion as the primary
model. The short iliac shelf was emphasized, in conjunction with the
presumed sprawling stance (which she inferred from the non-perforated
acetabulum). I have not seen the Lagerpeton material, and she may be
correct, but as an erect-stanced biped with a non-perforated
acetabulum, I wasn?t sure I bought off on that. Also, other presumably
erect dinosaurimorphs had short iliac blades (Dilophosaurus, some
prosauropods, Herrerasaurus, etc). Hopefully she will publish some
clarifications in the proceedings volume.
Michael Benton went next with a more general talk about dinosaur
origins. He emphasized his disagreement with the Romer-based model of
the absolute competitive superiority of dinosaurs (competition with a
capital ?C?, as he clarified to me later), instead emphasizing that
changing environmental factors probably opened the door to dinosaur
radiations. He also reaffirmed his belief in a monophyletic
ornithodira, with Scleromochalus as the most primitive known member. I
want to add some comments from a discussion we had today, because I was
pleased to find out that he and I are much more in agreement on this
issue than I?d realized. My objection to the ?non-competitive? model
is that unlike the K/T event, where the non-avian dinosaurs were
literally removed from existence and could no longer compete with
mammals (allowing our subsequent radiation), the Triassic faunal
turnover did not happen as catastrophically (at least in a temporal
sense), and not all of the groups died out (at least not right away).
That is, there may well have been a series of environmental factors
that were knocking out species of dicynodonts, rynchosaurs, etc, but
over time dinosaurs proved they were more survivable, and better able
to radiate into those niches once available. In addition, once they
occupied a niche (i.e. large herbivore), they neither relinquished it
nor shared it, a feat earlier large bodied Triassic groups had proven
unable to accomplish. And, it turns out, Benton agrees with
competitive superiority in this more restricted sense of the term.
Sterling Nesbitt gave one of my favorite talks of the conference. He
showed that Shuvosaurus is not an ornithomimid (no real surprise
there), but is rather a derived suchian. And he demonstrated this
pretty convincingly, since he has a number of specimens with post
crania conveniently attached to skulls. For those of you who haven?t
seen this thing, it is insanely cool. It?s like a crocodile-line
archosaurs trying its best to be a prosauropod, complete with long
flexible neck. Even weirder, it is probably an obligate biped.
Likewise, he showed that Revueltosaurus teeth are not those of a
Triassic ornithopod, but rather come attached to a suchian skull. His
point being that there is some exceptional homoplasy in Late Triassic
archosaurs, and that identifying things as dinosaurs is tenuous from
isolated remains. Coauthor and fellow speaker Randall Irmis returns to
this point a few talks later?
But first Paul Sereno gave a talk that had two main points. One is
that he is helping to create an online database for sharing and
analyzing data matrices used in phylogenetic analyses. He showed
images of software that could show what percentage of different
matrices used the same characters, if they used disagreeing character
states, and (literally) dozens of other useful tools for trying to mine
useful comparative data from cladistic data sets. I don?t know when it
will be released (although apparently there will be a paper
forthcoming?wait for it!), but having just spent the last six months
doing phylogenetic analyses of two different groups of animals, I?m
pretty excited about the possibilities. The second part of his talk
mostly consisted of showing new, better photos of Eoraptor after
further preparation. They got it CT scanned again, and apparently this
time it clarified some internal data. Sereno still feels that both
Herrerasaurus and Eoraptor are basal theropods, not basal saurischians
as has been (cough?frequently) suggested.
Randall Irmis was up next, and picked up where Sterling left off; they
feel that a lot of North American Triassic dinosaurs aren?t and made a
pretty convincing argument for it. A (non-comprehensive) list includes
Eucoelophysis, which they feel pretty strongly is a silesaurid. Which
makes the name EU-coelophysis ironic, to say the least. Gojirosaurus
they feel is a chimera (Ken, want to comment?), made up of theropod
material and Shuvosaurus (or shuvosaur-like suchian) material. Not
surprisingly they conclude that Protoavis is a chimera, including
?coelophysoid material and non-dinosaur material?. Finally, they think
Technosaurus is a silesaurid as well.
Watch silesaurids, it seems to be raining them lately?
Max Langer gave a talk that was ostensibly on the first ornithischian
body fossils from the Triassic of Brazil. When the first slide came
up, however, it was obvious that he has a bone-bed of silesaurid-like
material as well. He has a minimum of twelve animals (he has 12 right
femurs and no left femurs in the quarry?), of differing ontogenetic
ages. He made a good case that there is more than one taxa in the bone
bed, although I wouldn?t yet rule out sexual dimorphism. None of the
specimens are articulated. He did note the similarity to Silesaurus,
but rather than concluding that his new animal(s) are not dinosaurs, he
inferred that Silesaurus is itself a basal ornithischian. I personally
have some doubts about that, but with all the new silesaurid material
coming out, we?ll hopefully have a better handle on this and it?s
bearing on ornithischian origins (if any) in the near future.
Oliver Rahut finished off the talks before the coffee break with his
analysis of saurischian diversity throughout the Mesozoic. He analyzed
Saurischia as a whole (with and without birds), and sauropods and
theropods independently (the latter with and without birds). He found
weak support consistent with sauropods (mostly) reaching peak diversity
in the Jurassic and then declining, while theropods continue to
increase in diversity throughout the Mesozoic (not surprisingly this
was more pronounced when birds were included). He cautioned, however,
that the data is very susceptible to sampling bias, and in many cases
one or two new specimens could upset the apparent diversity curves
entirely. His implied conclusion was that we need far more data before
we can safely infer macro evolutionary patterns of this sort. I would
heartily agree.
After the coffee break (and two more cups of that wonderful Brazilian
cup o? joe), Jonas Bittencourt gave a talk (in Portuguese) on
diagnosing Staurikosaurus. Happily his slides were in English, so I
caught the main gist of it. He discussed the problems with older
diagnoses, which largely included plesiomorphic characters, rendering
Staurikosaurus more or less without any diagnosable autapomorphies.
They confirmed that one suggested novel character, a strong bevel on
the anterior portion of the distal end of the pubis. He also provided
new characters from the pelvis and hind limbs. He did not find any
useful diagnostic characters in the vertebral column, and concluded
that axial evolution was more conservative during the early theropod
radiation than appendicular evolution was.
Martin Ezcurra gave a good talk on the morphology and relationships of
Zupaysaurus. He provided compelling data that Zupaysaurus is a
coelophysoid, not a basal tetanuran. He also demonstrated that
Zupaysaurus is definitely not crested, as previous reports have
suggested. Instead the skull underwent oblique crushing, leaving part
of the left lacrimals visible about the right lacrimals, giving the
appearance of a crest. Sorry to artists who have already drawn
Zupaysaurus! Also, due to the very similar distortion of the skull of
Coelophysis kayentakatae, he urged caution in interpreting it as
crested without further analysis to rule out the possibility of the
?crest? being a taphonomic artifact.
Diego Pol presented data from new specimens of Mussaurus. He found
incomplete adult and subadult specimens, and based on them was able to
refer other specimens that had been described as Plateosaurus sp. To
Mussaurus. Good thing too, as his phylogenetic analysis found that
Mussaurus is quite a bit closer to true sauropods than Plateosaurus is.
He found a paraphyletic prosauropoda. Interestingly, looking at the
ontogenetic series of Mussaurus, he found that ontogenetic trends
usually paralleled phyletic trends in phenotype; that is, Mussaurus had
a primitive ?prosauropod? set of frontals and parietals as a juvenile,
but they alter (quite extensively) during ontogeny and end up looking
very sauropod-ish. Sauropodomorph evolution seems to be crying out for
a heterochrony-based approach to understanding the early morphological
diversification of the group.
Claudia Mariscano gave an overview of the abundant dinosaurimorphs
footprints her team has found in Argentina. She feels that the
inherent difficulties in taxonomic identity (i.e. correlating with body
fossils) in intractable at this point, but does feel that the
ichnofossil record argues persuasively for an early evolution and
radiation of dinosaurs than the body fossil record shows.
Jeff Wilson gave the last talk of the morning, and demonstrated some
interesting techniques for integrating functional data from
ichnofossils with body fossils to extract timing information for the
origin certain functional traits. He scored synapomorphies from
ichnotaxa into a matrix with sauropodmorph body fossils, and then used
stratocladistics to see how the resulting tree affected the timing of
certain morphological traits. He concluded that the ichnofossils
argued that a digitigrade forelimbs evolved earlier than the body
fossils indicated (since I?ve always interpreted the prosauropod manus
as digitigrade, this wasn?t a surprise to me). He also concluded that
quadrupedality was more common basally than is often inferred, and that
the heal pad evolved further down the sauropodomorph tree than is
usually thought. That last one I found really intriguing, as it had
never occurred to me to put heal pads on prosauropod hind feet, but
some of the tracks did look convincing. I don?t know how susceptible
Jeff?s analysis technique is to the incompleteness of the fossil
record, but that seems pretty relevant. If Claudia is right that
dinosaurs diversified much earlier than though, than it?s at least
possible that the tracks Jeff are finding record that more derived
sauropodomorphs were common earlier than commonly realized. I don?t
know what kind of sensitivity analysis could be done to test this, but
it certainly would be nice to be able to combine comparative data sets
like this if it proves effective!
After lunch the talks were not on dinosaurs, and most were in
Portuguese, so I did not finish the afternoon (and have little useful
to report from the time I was there). I?ll try to get day three posted
as soon as possible.
Scott Hartman
Science Director
Wyoming Dinosaur Center
110 Carter Ranch Rd.
Thermopolis, WY 82443
(408) 483-9284
www.skeletaldrawing.com