Dinosaur snack, Sinobaatar, enters the LRT

Several specimens
of tiny (mouse-sized Sinobaatar created this generic chimaera  (Figs 1 –3) with close affinities to chipmunk-sized Rugosodon.

Figure 1. Sinobaatar in situ. DGS colors and reconstuctions added here.

Figure 1. Sinobaatar in situ. DGS colors and reconstuctions added here.

The canine might be missing or absent.
The premolars and molars are shaped like those in Rugosodon. As in rodents, the jugal is not exposed laterally.

Figure 2. Skull of Sinobaatar from two specimens. DGS colors added here.

Figure 2. Skull of Sinobaatar from two specimens. DGS colors added here. This skull is compressed and torsioned. See Rugosodon for in vivo shapes.

This clade of multituberculates
nests between extant tree shrews + aye-ayes (Daubentonia) and extant rodents in the LRT.

Figure 3. An old chart of multituberculate skulls to scale. Sinobaatar added here.

Figure 3. An old chart of multituberculate skulls to scale. Sinobaatar added here.

Sinobaatar lingyuanensis
(Hu and Wang 2002, Early Cretaceous) is a small multituberculate close to Rugosodon (Fig 4). Several specimens are known. One mandible was found inside the belly of the theropod we looked at yesterday, GMV2124. So small size did not protect all Mesozoic mammals.

Rugosodon eurasiaticus (Yuan et al. 2013, Late Jurassic, the size of a chimpmunk) is the oldest multituberculate and it is represented by a complete skeleton. Teeth and ankle evidence indicate it was an omnivore and arboreal.

Figure 4. Rugosodon eurasiaticus (Yuan et al. 2013, Late Jurassic, the size of a chimpmunk) is the oldest multituberculate and it is represented by a complete skeleton. Teeth and ankle evidence indicate it was an omnivore and arboreal.

Traditionally
multituberculates are considered pre-monotremes = pre-mammals due to the primitive structure of the posterior mandible bones. This is a reversal in this placental based on the sliding jaw joint interfering with normal ontogenetic development of the tiny middle ear bones otherwise transformed during phylogeny and ontogeny from posterior jaw bones.

References
Hu Y Wang YQ 2002. Sinobaatar gen nov: First multituberculate from the Jehol Biota of Liaoning, Northeast China. Chinese Science Bulletin 47(11): 933–938.

wiki/Rugosodon
wiki/Xianshou
wiki/Sinobaatar

Early Cretaceous NGMC 2124 = GMV 2124 enters the LRT with Aorun

Cau 2024 reported,
“A specimen referred to Sinosauropteryx by Currie & Chen (2001), NGMC 2124 (Fig 1), differs in several features from the former and represents a distinct taxon (Longrich, 2002).

This 1m long specimen also has short feathery filaments on the back and base of the neck, but nothing on the tail, except at the base. So feathers were not for display in this case. They seemed to form a short, trim pelage.

Phylogenetically this was an early appearance of any feathers,
but chronologically fully feathered Archaeopteryx was older and more derived. So this specimen was unchanged from a much earlier radiation with regard to pelage.

Figure 1. GMN 2124 aka NGMC 2124 in situ. Colors and reconstructions added here. Note the short metatarsal 3. This is not seen in other theropods. This morphology largely prevents flexion and extension of the proximal pedal phalanges.

Figure 1. GMN 2124 aka NGMC 2124 in situ. Colors and reconstructions added here. Note the short metatarsal 3. This is not seen in other theropods. This morphology largely prevents flexion and extension of the proximal pedal phalanges. The black lines indicate PILs in distal phalanges are continuous for flexion and extension there.  This specimen is 1m long.

Cau 2024 also reported,
“Another, yet unnamed Jehol Biota “compsognathid” (NGMC 2124, originally referred
to Sinosauropteryx), has been placed among the earliest branches of Tyrannosauroidea.”

The large reptile tree (LRT, 2319 taxa) largely confirms this nesting, but nests this taxon a little further outside, more primitive.

BTW, Ji and Ji 1997b originally described this specimen, naming it another Sinosauropteryx. The name needs to change, but that does not mean it is ‘unnamed.’

Afterward 1997 several authors (see below) continued to name this specimen Sinosauropteryx prima, even though it does not nest with the much smaller holotype (in the LRT) and differs in many ways, confirming the assessment of Cau 2024.

Does anyone else know of another specimen
in which metatarsal 3 is shorter than mt2 and mt4 in theropods? I had a hard time trying to  figure this out, but both metatarsal sets share this odd-to-unique pattern. So it’s not an artifact of jumbled taphonomy. Such a morphology would have prevented flexion and extension of the proximal pedal phalanges. However more distally the medial set of parallel interphalangeal lines (PILs) is continuous across all three digits. So this novel morphology works for GMV 2124. It’s just different. Have others noted this before?

Two small Mesozoic cynodont jaws were described inside the gut
of GMV 2124 by Hurum  et al in 2006 highlighted here (Fig 2). Sinobaatar is an Early Cretaceous placental mutiturberculate (close to extant tree shrews). Zhangeotheriumi s an Earliest Cretaceous pre-mammal cynodont close to Maotherium and Yanaconodon in the LRT.

Figure 1. Stomach contents of NGMC2124 include jaw elements from two small Jurassic mammals.

Figure 2. Stomach contents of NGMC2124 include jaw elements from two small Jurassic mammals, described by Hurum, Luo and Kielan-Jaworska 2006,

A kind reader or two asked for Coelurus to be added to the LRT.
Unfortunately, not enough is currently known to make that happen. It needs skull, foot  and pelvis data that is currently lacking. Hopefully this much more complete taxon, NGMC 2124, will suffice.

References
Cau A 2024.
A Unified Framework for Predatory Dinosaur Macroevolution. Bollettino della Società Paleontologica Italiana, 63(1): 1-19.
Currie PJ and Chen PJ 2001.
Anatomy of Sinosauropteryx prima from Liaoning, northeastern China. Canadian Journal of Earth Sciences, 38: 705-727.
Hurum JH, Luo Z-X and Kielan-Jaworowska 2006. Were mammals originally venomous? Acta Palaeontologica. Polonica 51 (1): 1–11.
Ji Q and Ji,S-A1997b. Advances in the study of the avian Sinosauropteryx prima. Chinese Geology, 242: 30–32 (in Chinese).

wiki/Sinosauropteryx

 

Ptychodus body fossil publicity

From theguardian.com
“Fossil experts say they have gained unprecedented insights into a type of enormous prehistoric shark, after finding complete skeletons of the creatures. The specimens, discovered in small quarries in north-eastern Mexico within the last decade, belong to Ptychodus – a creature that roamed the seas from around 105m to 75m years ago.

Figure 1. Ptychodus illustration from theguardian.com website. Note the pavement teeth.

Figure 1. Ptychodus illustration from theguardian.com website. Note the pavement teeth.

“Ptychodus fossils had turned up before but with its bones made of cartilage, which does not mineralise well, many were isolated teeth, which were huge and unusual. As a result, it was difficult to pin down exactly what Ptychodus looked like and where it sat on the evolutionary family tree.”

“The team say the plethora of features preserved within the specimens, including its fin skeletal anatomy, enabled them to carry out a fresh analysis of where Ptychodus sits on the evolutionary family tree. The results reveal it was a kind of mackerel shark – a group that includes the extinct gigantic shark megalodon and the great white shark that inhabits oceans today.”

The large reptile tree (LRT, 2318 taxa) recovered the same results.

Figure 2. Ptychodus fossil from theguardian.com. This one is different from the one stolen and recovered.

Figure 2. Ptychodus fossil from theguardian.com. This one is different from the one stolen and recovered.

“Taken together, the team say the findings suggest Ptychodus hunted prey in open water, with its meals probably comprising sea turtles and ammonites rather than creatures such as clams that dwelled on the sea floor, as had previously been thought.”

“new fossils suggest it had a maximum length of about 9.7 metres”

The link in the publicity to the Royal Society paper
has a flaw. Perhaps that will be repaired soon. A link from Wikipedia is shown below. The paper is currently behind a paywall.

References
Vullo R et al (11 coauthors 2024. Exceptionally preserved shark fossils from Mexico elucidate the long-standing enigma of the Cretaceous elasmobranch Ptychodus. Proceedings of the Royal Society B: Biological Sciences 291.
https://doi.org/10.1098/rspb.2024.0262

Publicity
theguardian.com

Singing came before talking in the human lineage

Which came first: singing or talking?
Several links on Google indicate: singing.

If true, and I think there’s good evidence for this,
then take a look at how primate singing began in this YouTube video of gibbons expressing their emotions, individually, much as birds do.

Gibbons sing. Humans sing.
Gorillas sing to themselves in contentment when eating. That was recently discovered. Chimps sing when they get excited, joining in with a chorus of other chimps. That has been known for a long time.

Earlier
here, here and here we looked at the overlooked gibbon-human more direct connection. On the other ape branch, in the LRT gibbon ancestors were also basal to the orangutan > Australopithecus > chimp > gorilla clade. So singing goes back, back, back.

South American howler monkeys howl by convergence.

It might be argued
that we humans sing now for the same reason(s) gibbons likely sang millions of years ago as they do today. Note the young singers in the second YouTube video (directly above) are all breeding age males. Their audience is largely made up of breeding age females. Breeding occasionally takes place between the two, but most of the audience members go home to their parents, appreciating the singing and songs as a performance.

Talking is so important to human interactions.
Talking leads to writing, books lead to newspapers, radio, television and the Internet. Talking leads to trade, cooperation, heirarchy, technology, and travel. Thanks to singing gibbons and siamangs ten million years ago, talking, writing and the rest eventually became possible in the human lineage.

References
Several links on Google

 

A 3.8m Sinosauropteryx on Facebook

Currie and Chen 2001 reported,
“The [smaller] specimens of Sinosauropteryx prima [Fig 1] show skull and orbit proportions, and bone texture typical of immature stages.”

In the LRT juveniles are phylogenetically recovered when these relatively small taxa nest conspicuously among relatively larger-to-much larger taxa. Since extant archosaurs change proportions during ontogenetic growth, similar changes should also be expected in fossil archosaurs. A changing morphology for a single taxon is a taxonomic nightmare. That is why juveniles are generally avoided.

By contrast, pterosaurs and other other lepidosaurs more closely retain adult proportions throughout their growth cycle.That makes ontogeny and phylogeny easier to separate.

Phylogenetic miniaturization is enabled when sexual maturity arrives earlier and earlier. Small precocious parents give rise to small precocious hatchlings in cycle after cycle. Neotony takes over. After several generations immature bone texture will appear in fossils of small, neotonous, yet sexually mature and gravid parents reproducing at a faster rate.

Figure 1. A 3.8m long 'Sinosauropteryx' from the FB page of Andrea Cau here compared to smaller specimens of Sinosauropteryx and details for both.

Figure 1. A 3.8m long ‘Sinosauropteryx’ from the FB page of Andrea Cau here compared to smaller specimens of Sinosauropteryx and details for both. Note the manual and pedal difference here. Otherwise the large and small specimens score so closely that they nest together in the LRT.

On his Facebook page,
Andrea Cau published a photo of an undescribed 3.8m long Sinosauropteryx. After testing in the LRT this specimen indeed nests with the smaller specimens. According to Cau’s caption: “This is the so-far-undescribed “largest Sinosauropteryx”, an amazing 3.8 m long (!) specimen housed in a Chinese museum and claimed to be a Sinosauropteryx. Although not yet included in my matrix, this specimen confirms the hypothesis developed in my latest paper that “compsognathids” are not adult morphs of small size, but juvenile semaphoronts of larger tetanurans. This specimen would surely improve the systematic placement of the Jehol Biota “compys”.

Sinosauropteryx 3.8m specimen
(not yet described; Early Cretaceous, Yixian Formation). The hand and foot are distinct from the holotype (Fig 1). The tail is relatively shorter. The hind limb is relatively longer, more typical of theropod proportions. The premaxilla is robust with hyper-robust premaxillary teeth. The anterior dentary tooth is a fang. Otherwise, scores in the LRT are very similar.

Figure 2. The 3.8 Sinosauropteryx specimen compared to related taxa, including Aorun, Compsognathus and the holoype Sinosauropteryx.

Figure 2. The 3.8 Sinosauropteryx specimen compared to related taxa, including Aorun, Compsognathus and the holoype Sinosauropteryx.

Here’s a pair of questions for all you lumpers and splitters out there:
At what point do you ascribe ontogeny to similar, yet distinct fossil archosaurs?
At what do you ascribe phylogeny to similar, yet distinct fossil archosaurs?

Let’s remember, juvenile flamingos have short legs and juvenile alligators have a shorter rostrum than adults do. In Sinosauropteryx the torso and tail length vary. So do the phalangeal proportions. The skull is nearly the same except for the gracile-robust difference. The two small skulls (Fig 1) also show individual differences.

The LRT currently tests several juveniles among the two thousand adults.. Small taxa often accumulate as examples of phylogenetic miniaturization at the bases of new clades. Traditionally these tiny adults have been omitted from analyses –  if they are pterosaurs – but not omitted if they are mammals.

In the LRT ontogeny-phylogeny problems are handled by specimen numbers or other identifiers (like ‘3.8m’). So no special coding is necessary.

Currie and Chen 2001 reported on the smaller specimens.
“Sinosauropteryx prima has a number of characters that were poorly preserved in known specimens of the closely related Compsognathus longipes from Europe. These include the longest tail known for any theropod and a three-fingered hand dominated by the first digit, which is longer and thicker than either of the bones of the forearm.” (Fig 1).

“Sinosauropteryx is comparable in size and morphology to known specimens of Compsognathus (Bidar et al. 1972; Ostrom 1978) from Europe. Sinosauropteryx and Compsognathus share a suite of characters that indicate close relationship.” (Fig 2).

Figure 4. From 2023, the theropod subset of the LRT.

Figure 3. From 2023, the theropod subset of the LRT.

Sinosauropteryx prima (smaller specimens)
(Ji and Ji 1996; Currie and Chen 2001, Early Cretaceous, Yixian Formation, Fig 1) is considered to have very primitive feathers. The rostrum is relatively short. The dorsal vertebrae are robust. The tail is quite long and gracile. The humerus is short and robust. The elbow (ulna) and manual digit 1 are both robust. The hind limbs are relatively shorter and robust.

Figure 4. Portion of a cladogram from Cau 2024 SuppData (SOM). Second frame indicates clades in the LRT. One of these two is a little shuffled due to taxon excluion and other factors. Cau includes many taxa known from scraps that do not appear in the LRT.

Figure 4. Portion of a cladogram from Cau 2024 SuppData (SOM). Second frame indicates clades in the LRT. One of these two is a little shuffled due to taxon excluion and other factors. Cau includes many taxa known from scraps that do not appear in the LRT.

Cau reported on his phylogenetic analysis:
“A detailed description of the result of the phylogenetic analysis based on the OSP data set is beyond the aims of this contribution. Here, I briefly mention the most significant
elements of the topology reconstructed, and discuss in detail the affinities of the compsognathid-like OTUs. The analysis found 10000 shortest trees.”

That’s a huge number when only one shortest tree is the goal. Systematists try to model actual evolutionary events and this should lead to a single tree. In my experience omitting scrappy taxa helps facilitate resolution. Cau includes scrappy taxa. There’s a time and place for that This might not be that time and place as Cau concurs in the next paragraph.

“The reduced consensus tree after the pruning of the less stable “wildcard” OTUs is well-resolved and supports the monophyly of successively less inclusive subgroups of the avian totalgroup e.g., Dinosauria, Saurischia, Theropoda, Averostra, Tetanurae, Neotetanurae,
Coelurosauria, Maniraptoriformes, Maniraptora, Paraves and Avialae. Most of the “wilcards” [sic] are taxa known uniquely for immature semaphoronts and thus
could not be directly compared to the majority of OTUs (which are known uniquely for mature semaphoronts).”

As mentioned yesterday, Cau’s outgroups (Fig 4) were traditional and cherry-picked, not the result of testing with the inclusion of pertinent taxa. Missing is a long list of poposaurs and basal bipedal crocodylomorphs. These are both proximal outgroups to the Dinosauria in the LRT. Unrelated taxa (e.g. the bipedal proterochampsid Lagerpeton) are not appropriate here. As a result, Cau did not find a basal split in the Dinosauria separating Theropoda from Phytodinosauria, as in the LRT.

Cau provided no reconstructions with DGS colors (Fig 1) for readers to see how scores were rendered. So scoring may also be an issue. Cau did not recognize phylogenetic miniaturization and neotony as a method used by nature to accelerate reproduction and introduce new morphologies in smaller taxa.

Cau’s analysis found
Aorun (Fig 2) an early diverging member of the Allosauroidea. That is confirmed by the LRT (Fig 3) where that divergence made Aorun basal to a long list of descendant theropods, including compsognathids and their descendants on one branch. Podokesaurus, Ornitholestes and their descendants, including birds, are at the base of the other branch following Aorun.

Here’s a TED Talk YouTube video featuring Jack Horner
on shape-shifting dinosaurs. Like I said, these can be taxonomic nightmares.

Bottom line:
The large and small Sinosauropteryx specimens (Fig 1) do nest together in the LRT. They have nearly identical skulls, except for the increase in robust characters in the large one. The torso and tail have different proportions. The feet have longer toes on one vs the other. The hands are very different. If those differences are acceptable to you as part of the growing-process (allometry), then meet the Sinosauropteryx family. If not acceptable, and you understand the process of phylogenetic miniaturization, then the small and large specimens are more distant cousins, different species. Even so, no other taxa are closer to either one than they are to each other in the LRT.

Cau needed to test a larger number of more complete taxa and omit (at least until later) the many scrappy taxa that score too few traits to be useful on this topic.

References
Cau A 2024. A Unified Framework for Predatory Dinosaur Macroevolution. Bollettino della Società Paleontologica Italiana, 63(1): 1-19.
Currie PJ and Chen PJ 2001.
Anatomy of Sinosauropteryx prima from Liaoning, northeastern China. Canadian Journal of Earth Sciences, 38: 705-727.
Ji Q and Ji S-A 1996. On the Discovery of the earliest fossil bird in China (Sinosauropteryx gen. nov.) and the origin of birds. Chinese Geology 233:30-33.

wiki/Sinosauropteryx

Theropod macroevolution: Cau 2024

Cau 2024 abstract:
“Known since the 19th Century, the compsognathids are among the smallest predatory dinosaurs, and include the first feathered non-avian species found.”

Which genus is not specified. A name drop would be appropriate here. We can guess that genus is Sinosauropteryx prima. In the LRT Sinosauropteryx is a small theropod nesting with Juravenator basal to Oviraptoridae + Theizinosauria.

Defining the Compsognathidae is key. In the large reptile tree (LRT, 2318 taxa, subset figure 2) the holotype of Compsognathus (Fig 1) nests as a basal member of the Ornithomimosauria. Outgroup taxa include the larger CNJ79 specimen also referred to Compsognathus (Fig 1). In the LRT phylogenetically miniaturized taxa often nest at the base of new clades as these two do. In the LRT the Compsognathidae include these two species, their last common ancsestor, Aorun, and all their descendants. That’s a long list that includes Ornitholestes, Tyrannosaurus and penguins.

The Cau 2024 cladogram (his figure 4-a) nests “Compsognathus specimens” deep within “Megalosauroidea” far from his “Ornithomimosauria + Therizinosauria”. 543 taxa and 1944 characters were tested. Cau also nests Ornithischia and Sauropodomorpha outside Herrerasauria. Outgroup taxa were not labeled, but were based on Cau 2018.

Earlier we looked at Cau 2018 in a four-part series. In that paper outgroup taxa included the LRT theropod, Marasuchus, two proterochampsids known from scraps (Dromomeron and Lagerpeton) and Teleocrater, a long-necked quadruped. By contrast, according to the LRT Cau’s dinosaur outgroup should have been the basal bipedal members of the Crocoylomorpha, then Poposauria.

“Traditionally, compsognathids have been considered small and unspecialized coelurosaurs, closer to birds than large-bodied forms like allosauroids and megalosaurids.”

Sounds like Cau is about to blast ‘tradition’. Cau is also keeping things vague here. A definition (see above) would have been appropriate for readers, but theropod experts may know this definition/list already.

“Yet, all known compsognathids are based on skeletally-immature specimens, and this challenges the accuracy of their traditional phyletic placement.”

This is the first time I’ve heard this asserted. Am I the last to know?
(For an answer, see below.)
At this time perhaps a list of compsognathids is warranted. Perhaps theropod experts know this list, so Cau assumes they know this list.

“Despite the role of heterochrony in dinosaur evolution is widely recognized, the impact of ontogenetic-biased miscodings in shaping theropod phylogenetics is mostly underestimated.”

Is it underestimated? Fewer assertions and more citations would be helpful.

“Herein, I show that the standard framework of theropod macroevolution is biased by a series of coding artifacts which violate semaphoront equality prescribed by phylogenetic systematics.”

An unfamiliar term ‘semaphoront’ pushed me to the dictionary.

semaphoront: biology, rare) An organism as seen in a specific time, as the object of identification or basis for systematics.

From Sharma et al 2017:A new practice in systematics, “semaphoront” coding, treats developmental stages as terminals. We submit that this approach is antithetical to cladistic practice and constitutes a gross misunderstanding of Hennig’s original idea. We contend that treating ontogenetic stages as terminals both violates tenets of phylogenetic systematics and oversimplifies the complexity of developmental processes. We contend that the application of semaphoront coding to any palaeontological question requires invoking multiple, unjustified assumptions, and ultimately will not yield a possible phylogenetic solution.”
Figure 1. The large (from Peyer 2006) and small Compsognathus specimens to scale. Several different traits nest these next to one another, but at the bases of two sister clades. Note the differences in the forelimb and skull reconstructions here. There may be an external mandibular fenestra. Hard to tell with the medial view and shifting bones.

Figure 1. The large (from Peyer 2006) and small Compsognathus specimens to scale. Several different traits nest these next to one another, but at the bases of two sister clades. Note the differences in the forelimb and skull reconstructions here. There may be an external mandibular fenestra. Hard to tell with the medial view and shifting bones.

Cau 2024 abstract continues:
“I introduce “Ontogenetic State Partitioning” (OSP), a novel coding protocol which integrates ontogenetic and morphological variation under a total evidence approach, and apply it to a densely sampled data set focusing on Mesozoic theropods.”

Good! Hope this works as well as standard trait-based analysis.

“The phylogenetic analysis dismissed “Compsognathidae” from being a natural group: its members are identified as juvenile morphs nested among several non-maniraptoriform tetanuran lineages.”

Cau 2018, 2024, provides a competing analysis to the LRT. This deep into the abstract Cau still has not listed any compsognathids, not even the two Compsognathus species, which the LRT found to constitute (along with the LCA, Aorun), a natural group.

We also remember the warnings of Sharma et al 2017 (see above).

“Conservatism in the immature body plan and greater disparity among large-sized adults differentiate the predatory communities dominated by non-coelurosaurian species (e.g., the so called “triumvirates”) from the maniraptoriform-tyrannosaurid faunas (herein named “tyrannies”).

“Triumvirates” usually refer to three of something. What are the three somethings?
Googling this term takes you first to three giant theropod skeletal models.

‘Tyrannies”? Is this a new trend in renaming clades?
Again, am I the last to know this trend?


Added not quite a day later:
Cau’s text reports, “The term “tyranny” used here (and inspired by the analogous “triumvirate” sensu Sereno & Brusatte, 2008) equates to “tyrant-dominated fauna” of Holtz (2021).

Hopefully that helps readers familiar with theropods. It still seems vague = poorly defined for Early Cretaceous taxa.


“This clade-specific differentiation among the communities is confirmed by an analysis of the predatory guild structures including all growth stages: triumvirates and tyrannies result as particular cases along a continuum of communities regulated mainly by alternative contributions of the small-and medium-sized classes.”

An unfamiliar term ‘guild structures’ pushed me to the dictionary, again. A guild structure is tripartite: 1. apprentice, 2. journeyman and 3. master.
Triumvirate is different, referring to three ruling men sharing power.

“The oldest tyrannies (early Late Cretaceous in age) cluster among non-tyranny communities, supporting the hypothesis that tyrannosaurid-dominated faunas acquired their peculiar structure only after the extinction of the non-coelurosaurian components.”

In the LRT the basalmost members of the tyrnannosaurus clade are Fukuiraptor, Tianyuraptor and Huaxiagnathus. All three are indeed Early Cretaceous. The latter is considered a traditional compsognathid. I don’t know if Cau intends his ‘oldest tyrannies’ to mean these three taxa.

It’s always better to be specific, not suprageneric, whenever possible.

“The macroevolutionary trajectory that led the maniraptoriforms to realize the avian-like biology may have precluded them from occupying hypercarnivorous large-bodied niches:”

Aren’t all theropods more or less ‘avian-like’? Among maniraptoriforms, isn’t Utahraptor among the ‘hypercarnivorous large-bodied’? I would add the terror bird, Phorusrhacos, to that list. If not, where is the large-bodied lower limit in size? Cau assumes readers know this. Some readers (= I) don’t know this.

“this bauplan constraint would have favored the tyrannosauroids in opportunistically assuming the apex predatory roles in Late Cretaceous Asiamerica but not elsewhere.”

Cau wrote about compsognathids as juveniles in this abstract. That’s a paper in itself. Now Cau is on the opposite end of the theropod continuum: apex predators. Hopefully Cau will tie this all in together with a discussion on hatchling tyrannosaurs, which were likely the size and shape of the larger Compsognathus species (CNJ79, Fig 1), which Cau appears to be considering a juvenile, if I’m reading this abstract correctly.

“The large-scale structure of the Cenozoic radiation of birds is coherent with the framework introduced herein.”

The “radiation of birds”? Evidently Cau is going to tie this topic in with immature compsognathids and apex predatior tyrannosaurs. We’ll see…

 

Figure 4. From 2023, the theropod subset of the LRT.

Figure 2. From 2023, the theropod subset of the LRT. Note how many small theropods are located at the bases of theropod clades that produced giant members. That’s phylogenetic miniaturization.

Wikipedia reports,
“Some authors have proposed that Compsognathidae is not a monophyletic group, and at least some compsognathids represent juvenile specimens of larger tetanuran theropods, such as carnosaurs and tyrannosaurs.”

Two of those three authors were Andrea Cau (2021, 2024). The multi-author third paper included, “the juvenile theropod dinosaurs Sciurumimus and Juravenator’ in the headline. The LRT nested these two taxa with relatively small taxa (Ornitholestes and Sinosauropteryx respectively), not with much larger =  ontogenetically older taxa.

Small does not automatically = young.

If there is something of value in the text of Cau 2024,
I will be happy to shed some light on that in future posts when I have time to read it. Let me know if I missed anything pertinent. Otherwise, in the abstract to this paper Cau is following a method Sharma et al warned others not to follow (see above).

References
Cau A 2018. The assembly of the avian body plan: a 160-milliony ear long process. Bollettino della Società Paleontologica Italiana, 57: 1-25.
Cau A 2024.
A Unified Framework for Predatory Dinosaur Macroevolution. Bollettino della Società Paleontologica Italiana, 63(1): 1-19.
Sharma PP, Clouse RM and Wheeler WC 2017. Henning’s semaphront concept and the use of ontogenetic stages in phylogenetic reconstruction. Cladistics 33(1):93–108.

wiki/Compsognathidae

Cau 2018: Evolution of the avian body plan – part 4

The next hurdle in the fish subset of the LRT: the humpback transition

Several extinct fish
have a buffalo-like hump in their back (Fig 1). We’ll look at two today and more later.

Figure 1. Middle Devonian Cheiracanthus compared to Late Jurassic Thaiichthys. These two humpbacked fish share several other traits despite their chronological separation.

Figure 1. Middle Devonian Cheiracanthus compared to Late Jurassic Thaiichthys. These two humpbacked fish share several other traits despite their chronological separation.

Cheiracanthus (Middle Devonian)
(Fig 1) is a humpback spiny shark. The mandible is about as long as the skull.

Thaiichthys (Late Jurassic)
(Fig 1) shortens the jaw line and increases the hump size as the fins turn from spines to rays with a robust leading edge ray.

The overall proportions
and skull details indicate homology rather than convergence. The LRT now nests these two together. This could change as studies continue.

 

Ticinolepis crassidens revisited, again.

More revisions.
This is how it goes when you try to reconstruct a fish skull, like Ticinolepis crassidens, that has seen a bit of facial bone dislocation and tessalation (Fig 1).

DGS (= coloring the bones) is helpful
because it avoids freehand, avoids arrows and abbreviations, is replicable by other workers, and brings out errors if elements don’t fit they way do in tentatively related taxa. It’s a learning tool currently enjoying wider use in µCT scans.

This is what it means to ‘manipulate in Photoshop’, a practice the Wikipedia author meant to imply something other than an attempt at precision reconstruction without a pencil and paper.

Figure 2. The skull of Ticinolepis crassidens (MCSN 8072) in situ from López-Arbarello 2016, traced and reconstructed using DGS methods.

Figure 1. The skull of Ticinolepis crassidens (MCSN 8072) in situ from López-Arbarello 2016, traced and reconstructed using DGS methods. Identifying scattered skull bones is the first step. It helps to occlude the teeth with each other as a given. Then start rebuilding.

Ticinoelpis crassidens now nests far apart
from Ticinolepis longaeva (Fig 4) which lacks builbous palatine teeth and has many other distinct traits. So the two are not congeneric. I know of (= tested in the LRT) no other fish with such palatine teeth and other traits.

Figure 2. Narcetes from Fujiwara et al 2021. Compare to Prohalecites in figure 3.

Figure 2. Narcetes from Fujiwara et al 2021. This is relative of the herring, Clupea.

Ticinoelpis crassidens
(López-Arbarell, Bürgin, Furrer and Stockar 2016, PIMUZ T 273, Triassic, 240 mya) this species has large, bulbous, crushing palatine teeth. Extant Narcetes (Fig 2) from Arctic waters is relative in the LRT.

Ticinolepis longaev (Fig 4) is closer to Robustichthys.

Figure 3. This specimen, wrongly attributed to Pholidophorus, is also close to Ticinolepis crassidents and is similar in age/antiquity.

Figure 3. This specimen, wrongly attributed to Pholidophorus, is also close to Ticinolepis crassidents and is similar in age/antiquity. Still looking for a museum number on this specimen in the herring family.

Apologies for earlier mistakes on this taxon.
It takes time to get to know certain specimens and fish in general.

Figure 4. Ticinolepis longaeva shares more traits with Robustichthys.

Figure 4. Ticinolepis longaeva shares more traits with Robustichthys.

The original authors, López-Arbarello, Bürgin, Furrer and Stockar 2016,
reported, “The anatomy of this fish shows a mosaic of halecomorph and ginglymodian characters and, thus, the new taxon probably represents a basal holostean.” 

The authors did not attempt a DGS reconstruction or phylogenetic analysis

The authors concluded,
“Among them
[= more than a hundred specimens], it was not possible to identify 37 specimens beyond the generic level, but the remaining fishes were classified in two new species: T. longaeva (48 specimens) and T. crassidens (20 specimens).

Even among fish experts, It takes time to get to know certain specimens and fish in general. Please report any observable errors if corrections are warranted.

References
López-Arbarello A, Bürgin T, Furrer H and Stockar R 2016. New holostean fishes (Actinopterygii: Neopterygii) from the Middle Triassic of the Monte San Giorgio (Canton Ticino, Switzerland). PeerJ 4(e2234):1-61.

wiki/Ticinolepis

Thalattosuchia 2024

Young et al 2024
took a deep dive into the marine crocodylomorphs: the clade Thalattosuchia (Fig 1).  They wrote, ” Thalattosuchia are composed of two clades: Teleosauroidea and
Metriorhynchoidea. Both clades are present in the early Toarcian (Early Jurassic) of Western Europe. Teleosauroids have often been considered ‘marine gavialids’ and have particularly been compared to
Gavialis gangeticus.”

According to Wikipedia,
“The exact phylogenetic position of Thalattosuchia is uncertain, with them either being interpreted as members of Neosuchia alongside other aquatic crocodylomorphs, or more basal members of Crocodylomorpha, with the similarities to neosuchians being as a result of convergent evolution.”

The authors undertook
a comprehensive presentation of the literature, which goes back to 1814. The citations you seek are here if they are anywhere. The photographs are large and professionally shot.

The team created a Crocodylomorph SuperMatrix.
They note their iteration “has the largest number of changes compared to any previous version of this dataset.”

Figure 2. Several Jurassic sea crocs, apparently derived from Late Triassic Dyoplax.

Figure 1. Several Jurassic sea crocs, apparently derived from Late Triassic gavialids.

From the abstract
“As we cannot reliably discriminate between the positional hypotheses for Thalattosuchia within Crocodylomorpha, the clades’ origins are as much of a mystery today as they were over a century ago.”

From the text
“The first phylogenetic definition of Thalattosuchia was proposed by Young and Andrade (2009). They followed the post-Ginsburg definition of Thalattosuchia (=Teleosauridae + Metriorhynchidae). Their definition was: the most inclusive clade consisting of Teleosaurus cadomensis (Lamouroux, 1820) and Metriorhynchus geoffroyii von Meyer, 1832, but not Pholidosaurus schaumburgensis von Meyer, 1841, Goniopholis crassidens Owen, 1842, or Dyrosaurus phosphaticus (Thomas, 1893). They chose the type species of the type genera of Metriorhynchidae and Teleosauridae as the internal specifiers, and selected a goniopholidid, a pholidosaurid, and a dyrosaurid as external specifiers.”

“Curiously, the four major differing phylogenetic positions recovered for Thalattosuchia [1] (sister-taxon to Crocodyliformes, [2] outside Metasuchia, [3] sister-taxon to Neosuchia, or [4] within a neosuchian longirostrine clade alongside Dyrosauridae) do mirror, to some extent, the varying historic ergotaxonomies for Thalattosuchia.”

In the large reptile tree (LRT, 2318 taxa,Fig 3) four thalattosuchians are tested:Teleosaurus (2 specimens (Fig 1), Dakosaurus and Metriorhynchus (Fig 1). Proximal outgroup taxa include Pelagosaurus, Dyrosaurus.

The outgroup to that clade in the LRT includes Gavialis, Alligatorellus and Dyoplax.

Abbreviaitons
The team used the abbreviation MPC. That appears to mean “minimum phylogenetic coverage.” Not sure how that differs from MPT = “most parsimonious tree”.

Figure 3. Subset of the LRT focusing on Crocodylomorpha. The new nestings represent just the latest of a changing hypothesis of interrelationships.

Figure 2. Subset of the LRT focusing on Crocodylomorpha in 2023. The new nestings represent just the latest of a changing hypothesis of interrelationships.

Outgroup taxa
The team cherry-picked Gracilisuchus, and the rauisuchians Batrachotomus and Postosuchus, as outgroup taxa, with Gracilisuchus at the base. While not likely to affect their multiple outcomes with their focus on Thalattosuchia, the LRT nests Gracilisuchus within the Crocodylomorpha – after testing 2300+ competing candidate taxa.

Figure 1. Ten basal bipedal crocodylomorphs descending from a sister to Decuriasuchus.

Figure 3. Ten basal bipedal crocodylomorphs descending from a sister to Decuriasuchus from 2014.

The other two outgroup taxa
are indeed tested outgroup taxa in the LRT, but are not proximal to the Crocodylomorpha, which is the sister clade of the Dinosauria, together comprising the clade Archosauria. No other clades are members of the Archosauria in the LRT. The proximal outgroup clade in the LRT is the Poposauria and Turfanosuchus (not mentioned in the text, Fig 4) is at its base. Likewise, the basal dinosaur, Herrerasaurus (not mentioned in the text, Fig 4), might also have been included among the short list of outgroup taxa in Young et al 2024.

Figure 1. Teleoctrater compared to related taxa in the LRT.

Figure 4. Teleoctrater compared to related taxa in the LRT. Hete Turfanosuchus is a phylogenetically miniaturized taxon at the base of the Poposauria + Archosauria.

As everyone in paleontology should know,
basal crocodylomorphs and basal dinosaurs were both bipedal (Fig 3). That fact seems to have been overlooked by Young et al 2024 when they included those two more distantly related quadrupedal rauisuchians.

Lesson here: Don’t cherry-pick outgroup taxa and hope no one will notice. The LRT has been online for 13 years to provide outgroup taxa for any vertebrate clade you want to focus on. Even so, build your own LRT so you’ll understand hypothetical interrelationships from firsthand experience, not borrowing based on trust. or cherry-picking based on a guess, tradition or rumor.

Characters in Young et al 2024
“885 phenotypic characters (671 craniomandibular and dental characters, 197 postcranial characters, 14 soft-tissue characters, and three behavioural characters.”

That is several times more than the LRT, which uses 238 characters. That bump in character number is likely necessary to lump and split species and specimens. By contrast, the LRT tests the widest possible gamut of chordate taxa seeking to ascertain more generic and suprageneric interrelatiionships.

Results in Young et al 2024
The team reported the shortest tree length recovered  was 185 MPCs. The team published 9 similar cladograms (their figures 4–12). Several included suprageneric taxa. Seemingly (= only guessing here) every known thalattosuchian was tested.

Not every crocodylomorph was tested.
That wasn’t necessary, given the focus of this study, but it would have avoided the problem of cherry-picking academically-approved, but erroneous, outgroup taxa that might have effected tree topology in more derived taxa.

Who knows how a possible ‘butterfly affect’ effects cladograms, so try to not cherry-pick ingroup or outgroup taxa. Test a wide gamut of taxa to find out.
Taxon exclusion continues to be the number one problem in paleontology in 2024.
The LRT is online to help. No credit or citation is necessary.

References
Young MT et al (12 co-authors) 2024. The history, systematics, and nomenclature of Thalattosuchia (Archosauria: Crocodylomorpha). Zoological Journal of the Linnean Society, 2024, XX, 1–71 https://doi.org/10.1093/zoolinnean/zlad165

wiki/Thalattosuchia

Novel spiny shark-to-bony fish transition series

Slogging through the process
of modeling actual evolutionary events with trait analysis, the LRT appears to present a novel hypothesis of interrelationships linking certain spiny sharks, Early Devonian 3cm long Mesacanthus and Early Devonian, 5.2cm Triazeugacanthus (Fig 1) with that clade of basal bony fish derived from placoderms.

Of course, this hypothesis needs testing by independent workers.
At present, this hypothesis of very fragile.

Figure 1. Two spiny sharks, Mesacanthus and Triazeugacanthus, now appear to be basal to Triassic bony fish close to Amia, the extant bowfin, illustrated here in phylogenetic order.

Figure 1. Two spiny sharks, Mesacanthus and Triazeugacanthus, now appear to be basal to Triassic bony fish close to Amia, the extant bowfin, illustrated here in phylogenetic order.

Nothing is ever settled here,
but revisiting and revising Triazeugacanthus based on a new Bauplan, seems to be shedding new light on this novel hypothesis of interrelationships.

Note the origin of
more less similar fin rays in both the pectoral and pelvic fins from the more primitive morphology in which the leading edge of a pectoral and pelvic fin were both spines. In the transitional taxon, Hulettia (Fig 1), the leading edge ray is more robust than the other rays.

If you want to remind me that catfish have a similar pectoral fin with a robust leading ray, you are correct. In the LRT catfish are closely related to this series of taxa.

Triazeugacanthus affinis
(Miles 1966; Chevrinais, Sire and Cloutier 2017, Early Devonian; 380 mya; up to 5.2cm) is a small acanthodian basal to ray-fin fish not in the clade that produced tetrapods. That clade includes Prohalecites and Hulettia at its base.

References
Chevrinais M, Sire, J-Y and Cloutier R 2017. From body scale ontogeny to species ontogeny: Histological and morphological assessment of the Late Devonian acanthodian Triazeugacanthus affinis from Miguasha, Canada. PLOS ONE. 12 (4): e0174655. Bibcode:2017PLoSO..1274655C. doi:10.1371/journal.pone.0174655
Miles RS 1966. The acanthodian fishes of the Devonian Plattenkalk of the Paffrath. Trough in the Rhineland. Arkiv för Zoologica (Stockholm)18: 147–194.

wiki/Mesacanthus
wiki/Triazeugacanthus
wiki/Hulettia