July 29, 2009

Suminia, the arboreal anomodont

11:51 am

Suminia getmanovi skeletal reconstructionSkeletal reconstruction of Suminia getmanovi (sue-MIN-ee-a  get-mah-NOVE-eye), an arboreal anomodont therapsid from the Late Permian of Russia. Art by Christina Stoppa.

Paleontologists have described the earliest known animal adapted for life in the treetops, according to a paper in the Proceedings of the Royal Society B, released online today. Jörg Fröbisch, of the Field Museum, and Robert Reisz, from the University of Toronto, found several adaptations for arboreality when they examined fossil skeletons of Suminia getmanovi , a small (20 inches/50 cm) herbivore from the Late Permian of Russia.

The most striking features of the skeleton of Suminia are the relatively large hands and feet. Most of their length is taken up by long, slender fingers and toes tipped with strongly curved, laterally (side-to-side) compressed claws, which are similar in proportion and shape to some modern tree-clinging animals, including dermopterans, megabats, and lizards. The first digits on the hands and feet diverge from the remaining four digits as well, and may have been used as opposable ‘thumbs’ as the animal clung to the branches.

Suminia getmanovi PIN 2212/116 specimen 1Skeleton of Suminia getmanovi, Paleontological Institute (Moscow) specimen number 2212/116 (spec. 1) Photo by Diane Scott.

More subtle features also point toward arboreal habits. The tail of Suminia is relatively long, and the vertebrae show strong processes halfway down its length. These processes could have supported muscles that allowed Suminia to use its tail for balance or, possibly, as a prehensile grasping organ.

Suminia, at 260,000,000 years old, is the first known vertebrate with this degree of arboreal specialization. Fröbisch and Reisz note that the Late Permian Period, and the Kotel’nich locality where Suminia was found, provides some of the earliest evidence for “modern terrestrial ecosystems with large numbers of plant-eaters supporting few top predators.” While large megaherbivores fed on the greenery below, Suminia found a new way to exploit the foliage in the treetops, taking the first known step into a niche that vertebrates would return to several times over the next 260 million years.

Suminia getmanovi flesh reconstructionLife restoration of Suminia getmanovi by Christina Stoppa.

Lawless teeth

In part because of some very poorly-written articles and headlines, and in part because talking about vertebrate relationships is just plain enjoyable, it seems like a good place to put in a little bit of context regarding exactly what Suminia is related to.

Suminia is a synapsid, a group of vertebrate animals that would eventually (some 50-100 million years after Suminia) give rise to the ancestors of today’s mammals. Although some synapsids have been called “mammal-like reptiles,” (because they certainly laid eggs and might have looked something like lizards) there are no true reptiles in the synapsid group. All true reptiles—turtles, lizards, snakes, crocodiles—even dinosaurs and birds—belong to a completely separate group.

Among the synapsids, Suminia is considered a therapsid, a phrase commonly used to indicate a grade of synapsid development in between the earlier pelycosaur-grade (think Dimetrodon) and the later mammal-grade. (Although, since mammals evolved from therapsids, we’re technically therapsids too, and since therapsids evolved from pelycosaurs, we can all claim that title as well.)

Among the therapsids, Suminia is an early member of the anomodont (“lawless tooth”) lineage. Sometime during the Early/Middle Permian period, the anomodont line split off from the line of therapsids that would, by way of a whole bestiary of gorgonopsians and therocephalians and countless cynodonts, eventually lead to mammals. The closest relatives we (and all other mammals) share with Suminia would have lived before the Late Permian, around 275,000,000 years ago (give or take several million years) .

The anomodonts have no living descendants, but their roster includes the great radiation of dicynodonts that survived the end-Permian extinction, became some of the largest terrestrial herbivores of the Triassic, and might possibly have survived into the Cretaceous if the identification of an Australian fossil is correct.


Placerias hesternus, a Late Triassic anomodont from Arizona. (Illustration by me, for the day job)

Contrary to what you might have read regarding this discovery, dinosaurs did not evolve from synapsids, and while Suminia is a human relative, this potential predator of Suminia is a much closer relation.

Some images and info for this post came from this press release.

—Matt Celeskey.

November 7, 2008

Beyond Bones

10:47 am

The Beyond Bones blog at the Houston Museum of Natural Science is full of paleo-stories these days:

—Matt Celeskey.

May 22, 2008

Gerobatrachus hottoni

3:34 pm
  • Gerobatrachus hottoni
  • Gerobatrachus hottoni
    Painting by Michael Skrepnick,
    from the press release at EurekAlert.
  • New Amphibian: Gerobatrachus hottoni
  • Name means:Hotton’s Elder Frog
  • Relations: Amphibamid temnospondyl and stem-batrachian (an early offshoot on the lineage leading to frogs and salamanders)
  • Location: Texas, U.S.A.
  • Age: Early Permian, ~290,000,000 years ago
  • Size: Less than 12cm (5 inches) long
  • Info: The three groups of living amphibians (frogs, salamanders, and caecilians) most certainly had their roots in the great amphibian radiations of the Late Paleozoic Era, but the fossil record has provided few clues that help pinpoint their precise ancestry. Gerobatrachus was a small temnospondyl, part of a very successful and numerous group of amphibians in the latter part of the Paleozoic. The remains of Gerobatrachus exhibit a unique mosaic of features in its teeth, ears, limbs, and vertebrae that suggest it may have been close to the origins of both modern frogs and salamanders. Although many researchers have proposed a close relationship between all three groups of living amphibians, a phylogenetic analysis that included Gerobatrachus found that caecilians had their origins in a completely different group of Paleozoic amphibians, the lepospondyls.
  • Reference: Anderson, J. S., Reisz, R. R., Scott, D., Fröbisch, N. B., and Sumida, S. S. 2008. A stem batrachian from the Early Permian of Texas and the origin of frogs and salamanders. Nature 453, 515–518 (22 May 2008) | doi:10.1038/nature06865. The article is available for download from the Center for North American Herpetology PDF Library.
  • Web coverage:

—Matt Celeskey.

April 3, 2008

Permian Meanderings

5:10 pm

In which I play “catch-up” for a few sites overlooked in my absence (note the partially-updated blogroll to the left). Today I’ll point out some excellent posts from the past few months dealing with different aspects of the Permian:

First up, Will at The Dragon’s Tales has had a couple of great articles on two of the more charismatic groups from the latter days of the Paleozoic: the carnivorous, sabre-toothed gorgonopsians and the herbivorous, tusk-beaked dicynodonts. Plus, he notes that there are some fantastic restorations of Permian vertebrates showing up on Wikipedia.

Speaking of dicynodonts, The Lord Geekington, mentions the ubiquitous Permo-Triassic straddler Lystrosaurus in his review of aquatic habits in stem-group synapsids. At the other end (that is, the beginning) of the Permian, he also discusses the potentially piscivorous pelycosaur Ophiacodon.

Finally, I recently came across the Houston Museum of Natural Science’s Prehistoric CSI blog, whose archives are chock full of fossil finds from Seymour, Texas—a treasure trove of Early Permian vertebrates—with videos and photos, and field sketches by Dr. Robert Bakker.

—Matt Celeskey.

March 31, 2008

It came from WIPP

10:34 pm

From Will Baird I learned of this story of 253 million year-old biological material recovered from subterranean salt deposits near Carlsbad. The material was found by analyzing the contents of microscopic bubbles in salt and halide crystals from the site of the Waste Isolation Pilot Plant (WIPP), a repository for low-level radioactive waste deep beneath the southeast New Mexico desert.

According to Wikipedia, the WIPP site was chosen, in part, because the salt deposits have remained relatively stable since they precipitated from a receding Permian sea, over 250,000,000 years ago. Presumably, the same stability helped preserve the earliest direct evidence of biological life—nearly four times the age of the previous record holder: traces of protein from 68 million year-old T. rex fossils.

Cellulose microfibers
Cellulose microfibers, from the UNC News press release.

Cellulose microfibers were the most abundant biological materials found, although the article tantalizingly mentions that some evidence of ancient DNA was “observed.”

Now a quarter-billion year-old bit of biomass is pretty darn nifty, and since the research is published in April’s issue of Astrobiology it leads to some interesting ideas about the possibility of finding durable bio-molecules preserved in salt deposits on other worlds. But I think there’s far greater potential for speculation here. I mean, we’ve got Paleozoic biology in proximity to low-level radiation. Forget the atom-bomb triggered monster ants of THEM!—imagine a pickled monuran, revivified and grotesquely enlarged by the careless placement of a used radiation suit, leaping out across the desert as it attempts to satisfy 250 million years worth of salt-cured hunger…

—Matt Celeskey.