Ossinodus

Ossinodus is an extinct genus of stem tetrapod. Fossils have been found from the Ducabrook Formation in Queensland, Australia dating back to the middle Visean stage of the Early Carboniferous (Mississippian).[1] It was originally placed within the family Whatcheeriidae, but the absence of an intertemporal bone as suggested by a recent reconstruction of the skull based on fragmentary material may prove it to be stemward of all whatcheeriids.[2]

Ossinodus Temporal range: Early Carboniferous, 345.3–326.4 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Scientific classification
Kingdom:	Animalia
Phylum:	Chordata
Superclass:	Tetrapoda
Family:	?Whatcheeriidae
Genus:	Ossinodus Warren and Turner, 2004
Species
O. pueri Warren and Turner, 2004 (type)

The oldest known pathological bone of a tetrapod, a fractured right radius, has been referred to Ossinodus.[3]

History and Discovery

Ossinodus is one of the first large tetrapods discovered during the time known as Romer’s Gap.[4] In 1996, initial inspection of scraps and materials postulated three possible types of tetrapods. A premaxilla with a tusk was originally attributed to a colosteid, then an ilium with a postiliac process linked it to an anthracosaur, or possibly a temnospondyl.[2] Described by Turner and Warren, all Ossinodus bones were discovered together at one site, ranging in all sizes. The recovered remains were deemed to belong in the same group O. pueri due to common ornamentation on the dermal cranial bones.[3] The specimens were found at the Drummond Basin of Queensland, Australia, in the Middle Paddock site of the Duckabrook Formation.[2]

Estimated to be about 333 million years old, the Middle Paddock site is representative of “a shallow fluviatile or lacustrine environment,” which is a large body of water with sedimentary deposits made of slits, clays, and carbonates.[5] The tetrapodal remains found here date back to Late Visean (early Carboniferous), towards the end of Romer’s Gap - a gap in the tetrapod fossil record. The excavation began in 1996 and ended in 2004, concluding with an extensive collection dis-articulated bones as well as half a skull.[2] The remains found during the time period are significant in suggesting that terrestrial tetrapods first inhabited Gondwana, and were not of small European forms.[5]

According to Warren, there were at least five specimens collected at the site, ranging in all sizes. The diversity of sizes indicated that the collection consisted of adults as well as juveniles.[2]

Description

Ossinodus are comparable in mass to modern Chinese giant salamanders. Compared to many other tetrapods of the late Devonian, it was estimated that they were 1–2 meters in length.[3] Dentition and habitat suggests that Ossinodus’ were piscivores considering habitat and teeth shape.

Skull

Ossinodus skulls are broad and heavily ornamented. Ornamentation's include deep pits and ridges all over the skull, on the parietal bones around a raised parietal foramen, as well as the jaw. The pits found on the maxilla and premaxilla are smaller and finer than those found on the skull table. Ossinodus differ from sister taxon Pederpes and Whatcheeriidae as their pits are larger than the pits on Pederpes, with Whatcheeriidae mostly lack dermal pitting.[1]  

On the outer surface of the skull, there is no apparent external sensory sulci. But upon closer inspection, the sensory canal is enclosed in the quadratojugal and only visible posteriorly along the inner surface.[1] The choana is seen on the anterior inner surface of the maxilla.[1] Orbits are small and placed anteriorly. Nostrils are located fairly low on the lateral side of the skull.[2]

The presence of an elongate supratemporal-postparietal contact played a role in eliminating anthracosaur as a possibility. As shared with other tetrapods, Ossinodus tabulars protrude slightly posteriorly and are also quite short. Sutures between the tabular-supraorbital area and squamosal suggest some motility to the posterior cheek.[1]

Dentition

Ossinodus have around 34 teeth along the maxilla as well as an inner row of teeth found on the palatine, vomer, and ectopterygoid.[2][1] The maxillary fangs are the largest teeth for Ossinodus. The teeth are distally-keeled in the shape of the head of a lance and contain grooves indicative of dentine infolds.[1] From the broken tooth, the tooth were polyplocodont - free of a pulp cavity with "ortho-dentine" folded simply and irregularly to the first degree.[6] Ossinodus teeth are also characterized as having dark dentine along the first fold.[1]

Postcranial Skeleton

Most of the postcranial skeleton, other than the neural arches, are smaller in size compared to the skull.

Some postcranial skeletal elements like the interclavicle, cleithrum, and scapulocoracoid resemble those found of genera Whatcheeriidae. Cladistically, this groups Ossinodus with Whatcheerids and Pederpes. The clavicle and interclavicle are also ornamented with deep pits, the same kind of ornamentation that decorates the dermal cranial bones. Similar to Ichthyostega and other tetrapods, their neural spines are “squared-off dorsally” with the anterior and posterior margins of the lateral faces of the intercentrum rolled outwards and enlarged pleurocentrum.[1][2] Their neural spines stand upright and the prezygapophysis are shorter than their postzygapophysis.[1]

Like most primitive tetrapods, the abductor blades of the femur protrude distally, with a groove separating it from the from the femoral head. Length and thickness depend on the size of the creature. Their tibias are broad, flat, and less waisted.[1] The humerus is covered by numerous asymmetrical pits.[7]

The most famous Ossinodus bone is the fractured radius. Along the edge of the extensor and flexor surfaces, there are prominent ridges that are found in early tetrapods. Likewise with Acanthostega, Pederpes, and Ichthyostega, the radii are shorter in length and less waisted.[1]

The ornamentation and pits found on specimen bones are sites of individual muscle attachment.[7]

Paleobiology

Paleopathology

Restoration showing placement of a fractured right radius

There is a fractured right radius of a particular specimen that shines light onto early tetrapod habitualization. A broken radius found among the Ossinodus remains in Australia suggests they must have spent a significant portion of their time on land. Through finite force analysis, the amount of force necessary to acquire the damage found on the bone is only possible from a fall of a certain height. It is unsure if Ossinodus were mainly aquatic or terrestrial, but it is safe to say that they spent time both in water and on land.[7]

Ossification along the fracture point marks one of the earliest signs of bone healing in early tetrapods.[8] The healing process produced a callus near the proximal end.[9]

Habitat

Early tetrapods were known to spend most of its time in water, with just their heads poking out.[10] However, the “axis of trabecular alignment”[7] on the fractured radius, analyzed through CT scan, lies almost parallel to the bone’s long axis. This alignment suggests that the radius was constantly remodeling as a response to supporting a heavy load. The only possible way for the radius to be under constant stress would be if the creature spent a considerable amount of time on land.[7] There are two specimens whose hind-limbs suggest aquatic locomotion, so Ossinodus could represent a pivotal transitional species. Based on a small Ossinodus femur recovered, postulated to belong to a juvenile and compared to the Horton Bluff femur, suggests that young specimens were more aquatic than older specimens.[11]

In addition to the fracture radius, the enclosed sensory canal synapomorphy is also indicative of tetrapods moving away from aquatic perceptions. These events are significant to better understand the water-to-land transition.

Paleoenvironment

The Middle Paddock site, where the Ossinodus specimen were collected, is organized as a "progradational deltaic system,"[1] meaning that there is an upper layer with sedimentary patterns exhibiting cyclic flood plains, encompassing a fluvial environment.[1] The lower layer contains alternating layers of wave-influenced siltstone, sandstone, and limestone.[1]

Uncovered at the site were also various aquatic fossils, again further suggesting that this early tetrapod coexisted with aquatic species. The aquatic fauna that were recovered at the site includes lungfish and sharks.

Classification

The closest relatives of Ossinodus are Whatcheeriidae and Pederpes. This relationship is determined through similarities in postcranial skeletal synapomorphies. However, Ossinodus separates itself from the two based on the size discrepancy between the skull bones and the limbs. While similar in skeletal features, an adult Ossinodus was typically larger than a full grown Whatcheeriidae or Pederpes.

The skull of Ossinodus is broader, shallow, and more elongated than Whatcheeriidae skulls, as Whatcheeriidae skulls have more depth due to their jugal notch.[2] The ornamentations decorated throughout the dermal cranial and skeletal bones are more apparent and take up more surfaces in Ossinodus than the other two taxa.[1]

There is strong support for Ossinodus being grouped together with Whatcheeriidae and Pederpes, as phylogenetic trees have been generated that consistently place them as a trichotomy. There is debate about whether Ossinodus is a sister taxon to Whatcheeriidae and Pederpes or if Ossinodus is perhaps the stem of the two other taxa.[1] Based on the descriptions provided by Warren and Turner, Ossinodus display more primitive features than Whatcheeriidae and Perperdes and thus could possibly be a sister taxon, older than the later two.

References

1. Warren, A.; Turner, S. (2004). "The first stem tetrapod from the Lower Carboniferous of Gondwana". Palaeontology. 47 (1): 151–184. doi:10.1111/j.0031-0239.2004.00353.x.
2. Warren, A (2007). "New data on Ossinodus pueri, a stem tetrapod from the Early Carboniferous of Australia". Journal of Vertebrate Paleontology. 27 (4): 850–862. doi:10.1671/0272-4634(2007)27[850:ndoopa]2.0.co;2.
3. Bishop, Peter J.; Walmsley, Christopher W.; Phillips, Matthew J.; Quayle, Michelle R.; Boisvert, Catherine A.; McHenry, Colin R. (2015). "Oldest Pathology in a Tetrapod Bone Illuminates the Origin of Terrestrial Vertebrates". PLOS One. 10 (5): e0125723. doi:10.1371/journal.pone.0125723. PMC 4418741. PMID 25938463.
4. Clack, Jennifer A. (March 2006). "The emergence of early tetrapods". Palaeogeography, Palaeoclimatology, Palaeoecology. 232 (2–4): 167–189. doi:10.1016/j.palaeo.2005.07.019. ISSN 0031-0182.
5. Clack, Jennifer A.A. (2012). Gaining Ground, Second Edition. Indiana University Press. ISBN 978-1-280-77261-0. OCLC 817090440.
6. Schultze, Hans-Peter (1970). Folded teeth and the monophyletic origin of Tetrapods. American Museum of Natural History. OCLC 248133835.
7. Bishop, Peter J. (2014-01-14). "The humerus ofOssinodus pueri, a stem tetrapod from the Carboniferous of Gondwana, and the early evolution of the tetrapod forelimb". Alcheringa: An Australasian Journal of Palaeontology. 38 (2): 209–238. doi:10.1080/03115518.2014.861320. ISSN 0311-5518.
8. Herbst, Eva C.; Doube, Michael; Smithson, Timothy R.; Clack, Jennifer A.; Hutchinson, John R. (September 2019). "Bony lesions in early tetrapods and the evolution of mineralized tissue repair". Paleobiology. 45 (4): 676–697. doi:10.1017/pab.2019.31. ISSN 0094-8373.
9. Warren, Anne; Ptasznik, Ron (January 2002). "The earliest fractured tetrapod bone". Alcheringa: An Australasian Journal of Palaeontology. 26 (4): 459–463. doi:10.1080/03115510208619536. ISSN 0311-5518.
10. AHLBERG, Per E. (2018-10-19). "Follow the footprints and mind the gaps: a new look at the origin of tetrapods". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 109 (1–2): 115–137. doi:10.1017/s1755691018000695. ISSN 1755-6910.
11. Anderson, Jason S.; Smithson, Tim; Mansky, Chris F.; Meyer, Taran; Clack, Jennifer (2015-04-27). "A Diverse Tetrapod Fauna at the Base of 'Romer's Gap'". PLOS One. 10 (4): e0125446. doi:10.1371/journal.pone.0125446. ISSN 1932-6203. PMC 4411152. PMID 25915639.