Showing posts with label Therapsida. Show all posts
Showing posts with label Therapsida. Show all posts

Saturday, December 21, 2024

[Paleontology • 2024] Early–middle Permian Mediterranean gorgonopsian suggests an equatorial origin of therapsids

a gorgonopsian from the island of Mallorca, western Mediterranean

in Matamales-Andreu, Kammerer, Angielczyk, Simões, Mujal, Galobart et Fortuny, 2024.  
Reconstruction by Henry Sutherland Sharpe

Abstract
Therapsids were a dominant component of middle–late Permian terrestrial ecosystems worldwide, eventually giving rise to mammals during the early Mesozoic. However, little is currently known about the time and place of origin of Therapsida. Here we describe a definitive therapsid from the lower–?middle Permian palaeotropics, a partial skeleton of a gorgonopsian from the island of Mallorca, western Mediterranean. This specimen represents, to our knowledge, the oldest gorgonopsian record worldwide, and possibly the oldest known therapsid. Using emerging relaxed clock models, we provide a quantitative timeline for the origin and early diversification of therapsids, indicating a long ghost lineage leading to the evolutionary radiation of all major therapsid clades within less than 10 Myr, in the aftermath of Olson’s Extinction. Our findings place this unambiguous early therapsid in an ancient summer wet biome of equatorial Pangaea, thus suggesting that the group originated in tropical rather than temperate regions.

Systematic palaeontology
Synapsida Osborn, 190313
Therapsida Broom, 190514

Gorgonopsia Seeley, 189415
Gorgonopsia indet.

Most relevant elements of DA21/17-01-01 and silhouette showing their positions


 Life reconstruction of the gorgonopsian from Mallorca in a floodplain setting.
Reconstruction by Henry Sutherland Sharpe


 Rafel Matamales-Andreu, Christian F. Kammerer, Kenneth D. Angielczyk, Tiago R. Simões, Eudald Mujal, Àngel Galobart and Josep Fortuny. 2024. Early–middle Permian Mediterranean gorgonopsian suggests an equatorial origin of therapsids. Nature Communications. 15: 10346. DOI: doi.org/10.1038/s41467-024-54425-5  

Thursday, July 25, 2024

[Paleontology • 2024] Jurassic Fossil Juvenile reveals prolonged Life History in early Mammals



in Panciroli, Benson, Fernandez, Fraser, Humpage, Luo, Newham et Walsh, 2024.

Abstract
Living mammal groups exhibit rapid juvenile growth with a cessation of growth in adulthood. Understanding the emergence of this pattern in the earliest mammaliaforms (mammals and their closest extinct relatives) is hindered by a paucity of fossils representing juvenile individuals. We report exceptionally complete juvenile and adult specimens of the Middle Jurassic docodontan Krusatodon, providing anatomical data and insights into the life history of early diverging mammaliaforms. We used synchrotron X-ray micro-computed tomography imaging of cementum growth increments in the teeth to provide evidence of pace of life in a Mesozoic mammaliaform. The adult was about 7 years and the juvenile 7 to 24 months of age at death and in the process of replacing its deciduous dentition with its final, adult generation. When analysed against a dataset of life history parameters for extant mammals5, the relative sequence of adult tooth eruption was already established in Krusatodon and in the range observed in extant mammals but this development was prolonged, taking place during a longer period as part of a significantly longer maximum lifespan than extant mammals of comparable adult body mass (156 g or less). Our findings suggest that early diverging mammaliaforms did not experience the same life histories as extant small-bodied mammals and the fundamental shift to faster growth over a shorter lifespan may not have taken place in mammaliaforms until during or after the Middle Jurassic.




Krusatodon 

 
Elsa Panciroli, Roger B. J. Benson, Vincent Fernandez, Nicholas C. Fraser, Matt Humpage, Zhe-Xi Luo, Elis Newham and Stig Walsh. 2024. Jurassic Fossil Juvenile reveals prolonged Life History in early Mammals. Nature. DOI: doi.org/10.1038/s41586-024-07733-1

Friday, February 9, 2024

[Paleontology • 2024] Riojanodon nenoi • A New early-diverging probainognathian cynodont and A Revision of the Occurrence of cf. Aleodon from the Chañares Formation, northwestern Argentina: New clues on the Faunistic Composition of the latest Middle–?earliest Late Triassic Tarjadia Assemblage Zone


Riojanodon nenoi
 Martinelli, Ezcurra, Fiorelli, Escobar, Hechenleitner, von Baczko, Taborda & Desojo, 2024

 DOI: 10.1002/ar.25388  
 
Abstract
The Chañares Formation (Ischigualasto-Villa Unión Basin) is worldwide known by its exquisitely preserved fossil record of latest Middle-to-early Late Triassic tetrapods, including erpetosuchids, “rauisuchians,” proterochampsids, gracilisuchids, dinosauromorphs, pterosauromorphs, kannemeyeriiform dicynodonts, and traversodontid, chiniquodontid and probainognathid cynodonts, coming from the Tarjadia (bottom) and Massetognathus-Chanaresuchus (top) Assemblage Zones of its lower member. Regarding cynodonts, most of its profuse knowledge comes from the traditional layers discovered by Alfred Romer and his team in the 1960s that are now enclosed in the Massetognathus-Chanaresuchus Assemblage Zone (AZ). In this contribution we focus our study on the probainognathian cynodonts discovered in levels of the Tarjadia Assemblage Zone. We describe a new chiniquodontid cynodont with transversely broad postcanine teeth (Riojanodon nenoi gen. et sp. nov.) which is related to the genus Aleodon. In addition, the specimen CRILAR-Pv 567 previously referred to cf. Aleodon is here described, compared, and included in a phylogenetic analysis. It is considered as an indeterminate Aleodontinae nov., a clade here proposed to included chiniquodontids with transversely broad upper and lower postcanines, by having a cuspidated sectorial labial margin and a lingual platform that is twice broader than a lingual cingulum. Cromptodon mamiferoides, from the Cerro de Las Cabras Formation (Cuyo Basin), was also included in the phylogenetic analysis and recovered as an Aleodontinae. The new cynodont and the record of Aleodontinae indet. reinforce the faunal differentiation between the Tarjadia and Massetognathus-Chanaresuchus Assemblage Zones, in the lower member of the Chañares Formation, and inform on the diverse chiniquodontid clade with both sectorial and transversely broad postcanine teeth.

Keywords: Chiniquodontidae, Cynodontia, Probainognathia, South America, taxonomy

 

Riojanodon nenoi gen. et sp. nov.


 

Agustín G. Martinelli, Martín D. Ezcurra, Lucas E. Fiorelli, Juan Escobar, E. Martín Hechenleitner, M. Belén von Baczko, Jeremías R. A. Taborda and Julia B. Desojo. 2024. A New early-diverging probainognathian cynodont and A Revision of the Occurrence of cf. Aleodon from the Chañares Formation, northwestern Argentina: New clues on the Faunistic Composition of the latest Middle–?earliest Late Triassic Tarjadia Assemblage Zone. The Anatomical Record.  DOI: 10.1002/ar.25388

Wednesday, February 7, 2024

[Paleontology • 2024] Paratraversodon franciscaensis • Skull Anatomy and Paleoneurology of A New traversodontid (Therapsida: Cynodontia) from the Middle-Late Triassic of Brazil

 
 Paratraversodon franciscaensis
Kerber, Roese-Miron, Medina, da Roberto-da-Silva, Cabreira & Pretto, 2024

 
Abstract
Traversodontidae, a clade of gomphodont cynodonts, thrived during the Middle and Late Triassic, displaying a wide geographical distribution. During fieldwork in 2009, a new specimen was discovered in Ladinian/early Carnian stratigraphic layers in southern Brazil. Here, we describe this specimen and propose a new taxon closely related to Traversodon stahleckeri (Traversodontinae) but displaying a unique combination of traits (e.g., presence of a poorly developed suborbital process, mesiodistal length of the paracanine fossa similar to the length of the canine, short diastema between the fourth incisor and the upper canine, and coronoid process not entirely covering the distalmost lower postcanine). Furthermore, the endocranial anatomy of the new taxon was examined. The reconstruction of the cranial endocast revealed paleoneurological features consistent with non-Gomphodontosuchinae traversodontids. These features include the presence of a pineal body (but the absence of an open parietal foramen). These recent findings contribute significantly to our understanding of the evolutionary history and cranial anatomy of Middle-Late Triassic traversodontids, shedding light on the diversity and adaptations of non-mammaliaform cynodonts.

Keywords: Dinodontosaurus Assemblage Zone, Ladinian/Carnian, phylogeny, Traversodontidae




 Paratraversodon franciscaensis


Leonardo Kerber, Lívia Roese-Miron, Thais G. M. Medina, Lúcio da Roberto-da-Silva, Sérgio F. Cabreira and Flávio A. Pretto. 2024. Skull Anatomy and Paleoneurology of A New traversodontid from the Middle-Late Triassic of Brazil. The Anatomical Record. DOI: 10.1002/ar.25385


Tuesday, May 30, 2023

[Paleontology • 2023] Santagnathus mariensis • Old Fossil findings in the Upper Triassic Rocks of southern Brazil improve Diversity of traversodontid Cynodonts (Therapsida: Cynodontia)


 Santagnathus mariensis
Schmitt, Martinelli, Kaiuca, Schultz & Soares, 2023


Abstract
In this contribution we describe a new genus and species of gomphodontosuchine cynodont from the Late Triassic Hyperodapedon Assemblage Zone (AZ) of the Santa Maria Supersequence of southern Brazil, based on material collected 20 years ago. The new taxon, Santagnathus mariensis gen. et sp. nov., is based on numerous cranial and postcranial remains, which altogether provide data on several parts of the skeleton. Santagnathus mariensis is closely related to Siriusgnathus niemeyerorum and Exaeretodon spp. and expands the knowledge about gomphodontosuchine cynodonts. Morphologically, the new species has a skull bauplan particularly similar to S. niemeyerorum and E. riograndensis, differing from them by a unique combination of traits such as three upper incisors, the absence of a descending process in the jugal, a more posterior position of the postorbital bar and a preorbital region larger than the temporal one. The new traversodontid was found associated with the rhynchosaur Hyperodapedon sp., corroborating the assignment of the cynodont fossils to the Hyperodapedon AZ. We also provide comments on the status of the Argentine traversodontid cynodont Proexaeretodon vincei, typically considered a junior synonym of Exaeretodon argentinus, and here accepted as a valid taxon.

Keywords: Eucynodontia, Late Triassic, Santa Maria Supersequence, Traversodontidae



 Santagnathus mariensis gen. et sp. nov.

 

Maurício Rodrigo Schmitt, Agustín Guillermo Martinelli, João Felipe Leal Kaiuca, Cesar Leandro Schultz, Marina Bento Soares. 2023. Old Fossil findings in the Upper Triassic Rocks of southern Brazil improve Diversity of traversodontid Cynodonts (Therapsida, Cynodontia). The Anatomical Record. 

Wednesday, August 24, 2022

[Paleontology • 2022] Taphonomy of Drought afflicted Tetrapods in the Early Triassic Karoo Basin, South Africa


Mummified skin on spreadeagled Lystrosaurus 

in Smith, Botha & Viglietti, 2022. 

Highlights: 
• Outcrop containing hundreds of Early Triassic tetrapod fossils interpreted as evidence of drought.
• Clusters of articulated skeletons interpreted as drought-induced aggregations.
• Mummified skin on spreadeagled Lystrosaurus suggest rapid desiccation after death by starvation.
• Bone histology confirms that all the Lystrosaurus were juveniles or early sub-adult.
• Bonebeds of juvenile Lystrosaurus are interpreted as sheet-washed behavioural aggregations.

Abstract
The sedimentology and taphonomy of in-situ fossils from earliest Triassic strata (Induan) in the southern Karoo Basin of South Africa is presented as evidence for episodes of drought-induced mass death of the resident tetrapods. Abundant skeletons are preserved in a 2 m-thick tabular silty-sandstone capping a multi-storeyed low-sinuosity channel sandstone interpreted as a wide shallow channel that became progressively abandoned, with more ephemeral flow regime than in the underlying channels and subjected to intermittent flows of low-density sediment-laden floodwaters. Stratigraphic and planimetric distribution of 170 in-situ tetrapod fossils shows several clusters of up to eight closely-spaced articulated Lystrosaurus skeletons preserved in prone and spread-eagled body position. These are interpreted as drought-stricken carcasses that collapsed and died of starvation in and alongside dried-up water sources. Two of the specimens display an unusual micritic envelope with a distinctive pustular texture interpreted as permineralised mummified skin indicative of rapid desiccation after death. Bonebeds of disarticulated bones of multiple juvenile Lystrosaurus occur in shallow depressions within the rubified mudstones. Layering of different skeletal elements suggests some hydraulic sorting but the initial aggregation was likely a behavioural response to drought. Osteohistology of spread-eagled Lystrosaurus (L. declivis and L. murrayi species) skeletons show that they represent early juvenile stage which is in accordance with previous findings that throughout Pangaea Early Triassic Lystrosaurus died relatively young due to environmental stressors. Our results support the hyperthermal hypothesis that ~252 Mya increased continental aridity, already a consequence of the coalescence of Pangaea, was critically intensified by volcanogenic greenhouse gasses from the Siberian traps. We propose that in the aftermath of the End-Permian mass extinction event, a succession of climatic drying episodes orchestrated a series of fully-functioning terrestrial ecosystems that were markedly different to those of the pre-extinction, and likely had a profound and lasting influence on the evolution of tetrapods.

Keywords: Early Triassic, Katberg Formation, Lystrosaurus, Drought accumulations, Bonebeds, Mummified skin


Roger M.H. Smith, Jennifer Botha and Pia A. Viglietti. 2022. Taphonomy of Drought afflicted Tetrapods in the Early Triassic Karoo Basin, South Africa. Palaeogeography, Palaeoclimatology, Palaeoecology. In Press, 111207. DOI: 10.1016/j.palaeo.2022.111207 

Thursday, May 27, 2021

[PaleoMammalogy • 2021] Mammaliaform Extinctions as A Driver of the Morphological Radiation of Cenozoic Mammals


 large Gobiconodon outcompeted the ancestors of modern mammals in the time of dinosaurs.

in Brocklehurst, Panciroli, Benevento & Benson, 2021. 
Illustration: Corbin Rainbolt.  twitter.com/CorbinRainbolt

Highlights
• The therian mammal radiation is usually associated with extinctions among dinosaurs
• Mesozoic therians show greater morphological constraint than their close relatives
• The release of this constraint occurred later than the extinction of the dinosaurs
• The therian radiation was in part driven by extinctions among other mammaliaforms

Summary
Adaptive radiations are hypothesized as a generating mechanism for much of the morphological diversity of extant species. The Cenozoic radiation of placental mammals, the foundational example of this concept, gave rise to much of the morphological disparity of extant mammals, and is generally attributed to relaxed evolutionary constraints following the extinction of non-avian dinosaurs. However, study of this and other radiations has focused on variation in evolutionary rates, leaving the extent to which relaxation of constraints enabled the origin of novel phenotypes less well characterized. We evaluate constraints on morphological evolution among mammaliaforms (mammals and their closest relatives) using a new method that quantifies the capacity of evolutionary change to generate phenotypic novelty. We find that Mesozoic crown-group therians, which include the ancestors of placental mammals, were significantly more constrained than other mammaliaforms. Relaxation of these constraints occurred in the mid-Paleocene, post-dating the extinction of non-avian dinosaurs at the K/Pg boundary, instead coinciding with important environmental shifts and with declining ecomorphological diversity in non-theriimorph mammaliaforms. This relaxation occurred even in small-bodied Cenozoic mammals weighing <100 g, which are unlikely to have competed with dinosaurs. Instead, our findings support a more complex model whereby Mesozoic crown therian evolution was in part constrained by co-occurrence with disparate mammaliaforms, as well as by the presence of dinosaurs, within-lineage incumbency effects, and environmental factors. Our results demonstrate that variation in evolutionary constraints can occur independently of variation in evolutionary rate, and that both make important contributions to the understanding of adaptive radiations.

Keywords: adaptive radiation, constraint, mammal, Mesozoic, K/Pg mass extinction


Early lineages of mammal like this large Gobiconodon from Mongolia outcompeted the ancestors of modern mammals in the time of dinosaurs.
Illustration: Corbin Rainbolt.

 
Neil Brocklehurst, Elsa Panciroli, Gemma Louise Benevento and Roger B.J. Benson. 2021. Mammaliaform Extinctions as A Driver of the Morphological Radiation of Cenozoic Mammals. Current Biology. DOI: 10.1016/j.cub.2021.04.044

In brief: Brocklehurst et al. report that Mesozoic therians evolved under greater morphological constraint than contemporary mammaliaforms. This constraint was released later than the extinction of non-avian dinosaurs, including in therians less than 100 g. They suggest the therian radiation was in part driven by extinctions among non-therian mammaliaforms.

Mammals in the time of dinosaurs held each other back

Sunday, May 16, 2021

[Paleontology • 2021] Niche Partitioning shaped Herbivore Macroevolution through the early Mesozoic



in Singh, Elsler, Stubbs, ... et Benton, 2021. 

Abstract
The Triassic (252–201 Ma) marks a major punctuation in Earth history, when ecosystems rebuilt themselves following the devastating Permian-Triassic mass extinction. Herbivory evolved independently several times as ecosystems comprising diverse assemblages of therapsids, parareptiles and archosauromorphs rose and fell, leading to a world dominated by dinosaurs. It was assumed that dinosaurs prevailed either through long-term competitive replacement of the incumbent clades or rapidly and opportunistically following one or more extinction events. Here we use functional morphology and ecology to explore herbivore morphospace through the Triassic and Early Jurassic. We identify five main herbivore guilds (ingestion generalists, prehension specialists, durophagous specialists, shearing pulpers, and heavy oral processors), and find that herbivore clades generally avoided competition by almost exclusively occupying different guilds. Major ecosystem remodelling was triggered multiple times by external environmental challenges, and previously dominant herbivores were marginalised by newly emerging forms. Dinosaur dominance was a mix of opportunity following disaster, combined with competitive advantage in their new world.








 
Suresh A. Singh, Armin Elsler, Thomas L. Stubbs, Russell Bond, Emily J. Rayfield and Michael J. Benton. 2021. Niche Partitioning shaped Herbivore Macroevolution through the early Mesozoic. Nature Communications. 12: 2796. DOI: 10.1038/s41467-021-23169-x

Tuesday, December 8, 2020

[Paleontology • 2020] Agudotherium gassenae • A New Prozostrodontian Cynodont (Eucynodontia, Probainognathia) from the Upper Triassic of Southern Brazil


Agudotherium gassenae   
Stefanello, Kerber, Martinelli & Dias-Da-Silva, 2020

 
ABSTRACT
Probainognathian cynodonts are well represented in the fossil record from the Middle and Upper Triassic of South America, especially in Brazil and Argentina. In this contribution, we describe a new genus and species of non-mammaliaform prozostrodontian cynodont from southern Brazil. The new taxon comes from the Niemeyer Site, a locality in which the traversodontid cynodont Siriusgnathus niemeyerorum is numerically dominant, whereas probainognathians and other tetrapods are comparatively scarce. The fauna from the Niemeyer Site was putatively assigned to the Riograndia Assemblage Zone (Norian age) recently, although none of the index fossils for that biozone (e.g., Riograndia, Clevosaurus, Jachaleria) have so far been discovered at this locality. The new cynodont taxon is based on a left lower jaw with the canine and six (pc2–pc7) well-preserved postcanines (CAPPA/UFSM 0262, holotype), and a second referred specimen (CAPPA/UFSM 0208, paratype), which includes a right lower jaw with incisors, canine, and seven (pc1–pc7) postcanines, with pc6–pc7 being the best preserved. These specimens have a robust dentary, a long and dorsoventrally tall Meckelian groove, unserrated canines, and unserrated, sectorial postcanine teeth with posteriorly inclined cusps and a poorly developed lingual cingulum. This combination of features is unknown in other Carnian and Norian non-mammaliaform cynodonts. The new taxon contributes to our knowledge of the evolutionary radiation of small prozostrodonts that occurred in western Gondwana during the Late Triassic and led to the emergence of several important cynodont groups, including Mammaliaformes.



SYSTEMATIC PALEONTOLOGY 

THERAPSIDA Broom, 1905 
CYNODONTIA Owen, 1861 
EUCYNODONTIA Kemp, 1982 
PROBAINOGNATHIA Hopson, 1990 

PROZOSTRODONTIA Liu and Olsen, 2010 

Agudotherium gassenae, gen. et sp. nov.

Etymology—Agudo,’ in reference to the municipality of Agudo (state of Rio Grande do Sul, Brazil) where the specimens were found. The suffix ‘therium’ (from the Greek ‘thērion’) means ‘beast,’ and is often used for mammals and closely related forms. The specific epithet honors Mrs. Valserina Maria Bulegon Gassen, former mayor of the city of São João do Polesine (State of Rio Grande do Sul, Brazil), for her valuable contribution in the creation of CAPPA/UFSM.


Micheli Stefanello, Leonardo Kerber, Agustin G. Martinelli and Sérgio Dias-Da-Silva. 2020. A New Prozostrodontian Cynodont (Eucynodontia, Probainognathia) from the Upper Triassic of Southern Brazil. Journal of Vertebrate Paleontology. 40(3)e1782415. DOI: 10.1080/02724634.2020.1782415  

Thursday, July 4, 2019

[Paleontology • 2019] Vetusodon elikhulu • A New Large Cynodont from the Late Permian (Lopingian) of the South African Karoo Basin and its Phylogenetic Significance


Vetusodon elikhulu
Abdala, Gaetano, Smith & Rubidge, 2019

DOI: 10.1093/zoolinnean/zlz004 
Artwork by Gabriel Lio.  twitter.com/GabrielLuisLio

Abstract
The Karoo Basin of South Africa has the best global record of Lopingian (Late Permian) non-mammaliaform cynodonts, currently represented by five species. We describe Vetusodon elikhulu gen. et sp. nov., documented by four specimens from the Daptocephalus Assemblage Zone. With a basal skull length of ~18 cm, it is the largest Lopingian cynodont and is also larger than Induan representatives of the group. Vetusodon elikhulu has a cranial morphology that departs notably from that previously documented for Permo-Triassic cynodonts. It features a short and extremely wide snout, resembling that of the contemporaneous therocephalian Moschorhinus, and has large incisors and canines that contrast with the small unicusped postcanines, suggesting a more important role of the anterior dentition for feeding. The dentary is extremely long and robust, with the posterior margin located closer to the craniomandibular joint than in other Lopingian and Induan cynodonts (e.g. Thrinaxodon). The secondary palate morphology of V. elikhulu is unique, being short and incomplete and with the posterior portion of the maxilla partly covering the vomer. A phylogenetic analysis suggests that V. elikhulu is the sister taxon of Eucynodontia and thus the most derived of the Lopingian to Induan cynodonts yet discovered.

Keywords: anatomy, Changhsingian, epicynodont, Gondwana, phylogeny



Life reconstructions of Vetusodon elikhulu. 
Artwork by Gabriel Lio.  

Life reconstructions of Vetusodon elikhulu.
 Artwork by Gabriel Lio. 

Vetusodon elikhulu gen. et sp. nov.


Fernando Abdala, Leandro C. Gaetano, Roger M. H. Smith and Bruce S Rubidge. 2019. A New Large Cynodont from the Late Permian (Lopingian) of the South African Karoo Basin and its Phylogenetic Significance. Zoological Journal of the Linnean Society. zlz004. DOI: 10.1093/zoolinnean/zlz004
Vetusodon elikhulu: when the old has something modern conicet.gov.ar/vetusodon-elikhulu-when-the-old-has-something-modern


Friday, May 31, 2019

[Paleontology • 2019] Ufudocyclops mukanelai • A New Kannemeyeriiform Dicynodont from Subzone C of the Cynognathus Assemblage Zone, Triassic of South Africa, with Implications for Biostratigraphic Correlation with other African Triassic Faunas


Ufudocyclops mukanelai
Kammerer, Viglietti, Hancox, Butler & Choiniere, 2019

ABSTRACT
A new taxon of kannemeyeriiform dicynodont, Ufudocyclops mukanelai, is described based on a well-preserved skull from Subzone C of the Cynognathus Assemblage Zone, which are the youngest strata (probably Middle Triassic) of the Beaufort Group (uppermost Burgersdorp Formation) in South Africa. Ufudocyclops mukanelai is diagnosed by its autapomorphic intertemporal morphology: the intertemporal bar in this taxon is ‘X’-shaped—broad anteriorly and posteriorly but distinctly ‘pinched’ at mid-length and bears a deep, triangular depression immediately behind the enormous pineal foramen. The new kannemeyeriiform can also be diagnosed by the presence of a laterally expanded jugal plate beneath the orbit, and highly discrete, ovoid nasal bosses separated by a broad, unornamented median portion of the premaxilla and the nasals. Two partial dicynodont skulls from this subzone, previously identified as specimens of the otherwise Tanzanian taxon Angonisaurus, are also referable to U. mukanelai. Removal of these specimens from the hypodigm of Angonisaurus eliminates a crucial point of correlation between Cynognathus Subzone C and the Manda Beds of Tanzania and suggests that Subzone C preserves a distinct, endemic fauna, not just a southern extension of the better-known Middle–Late Triassic tetrapod faunas from Tanzania and Zambia. Inclusion of Ufudocyclops in a phylogenetic analysis of anomodonts recovers it as an early stahleckeriid, the first record of this clade from the Cynognathus Assemblage Zone.

FIGURE 4. Ufudocyclops mukanelai, gen. et sp. nov., BP/1/8208, holotype, photograph and interpretive drawing in right lateral view. Gray indicates matrix; dotted lines indicate missing bone.

 Abbreviations: af, fossa for M. adductor mandibulae externus lateralis; cp, caniniform process of maxilla; fo, fenestra ovalis; fr, frontal; j, jugal; la, lacrimal; mx, maxilla; na, nasal; pa, parietal; pmx, premaxilla; po, postorbital; pr?, prootic; prf, prefrontal; pt, pterygoid; q, quadrate; smx, septomaxilla; sq, squamosal. Scale bar equals 5 cm.


FIGURE 10. Ufudocyclops and Angonisaurus compared.
A, B, holotype of Ufudocyclops mukanelai (BP/1/8208) in A, dorsal and B, right lateral views.
C, D, holotype of Angonisaurus cruickshanki (NHMUK PV R9732) in C, dorsal and D, left lateral views; D is mirrored for comparative purposes. Scale bars equal 5 cm.


SYSTEMATIC PALEONTOLOGY

 SYNAPSIDA Osborn, 1903 
THERAPSIDA Broom, 1905 
ANOMODONTIA Owen, 1860 

DICYNODONTIA Owen, 1860 
KANNEMEYERIIFORMES Maisch, 2001 
STAHLECKERIIDAE Lehman, 1961 

UFUDOCYCLOPS MUKANELAI, gen. et sp. nov.

Etymology— From the Xhosa ufudo, meaning tortoise (in reference to the toothless, tortoise-like beak), and the Ancient Greek cyclops, a one-eyed mythological giant (in reference to the enormous opening for the pineal eye on the dorsal midline of the skull). Species named in honor of Mr. Pepson Mukanela, in recognition of his many years working in the preparatory laboratory of the Evolutionary Studies Institute (and its predecessor, the Bernard Price Institute for Palaeontological Research) and in particular his skillful preparation of BP/1/8208.


Christian F. Kammerer, Pia A. Viglietti, P. John Hancox, Richard J. Butler and Jonah N. Choiniere. 2019. A New Kannemeyeriiform Dicynodont (Ufudocyclops mukanelai, gen. et sp. nov.) from Subzone C of the Cynognathus Assemblage Zone, Triassic of South Africa, with Implications for Biostratigraphic Correlation with other African Triassic Faunas. Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2019.1596921 

Thursday, May 16, 2019

[Paleontology • 2019] The Postcranial Anatomy of Brasilodon quadrangularis and the Acquisition of Mammaliaform Traits Among Non-mammaliaform Cynodonts


Brasilodon quadrangularis 
Bonaparte, Martinelli, Schultz & Rubert, 2003

 from the Riograndia Assemblage Zone of the Candelária Sequence, Santa Maria Supersequence (Brazil).
  Illustration: Jorge Blanco. 

in Guignard, Martinelli & Soares, 2019. 

Abstract
Brasilodon quadrangularis (Cynodontia, Probainognathia) is an iconic non-mammaliaform cynodont from the Late Triassic of Brazil (Riograndia Assemblage Zone, Candelária Sequence), being considered as the sister taxon of Mammaliaformes. Although its phylogenetic position is very important, several aspects of its postcranial anatomy remain unclear or unstudied. Here, we present a detailed description of the postcranial elements referred to Brasilodon, including previously mentioned specimens and new ones, which add relevant information about its postcranial morphology and provide a new insight into the anatomical transition between advanced non-mammaliaform cynodonts and early mammaliaforms. Functional and ecological implications are also investigated, based on the postcranial morphology and muscular reconstructions. The postcranium of Brasilodon differs from most non-mammaliaform cynodonts and presents similarities with tritylodontids, early mammaliaforms and extant therians, such as a ventrally oriented scapular glenoid facet, a distinct and ossified greater humeral tubercle, lack of ectepicondylar foramen, olecranon process, hemispherical humeral and femoral heads and a prominent intertrochanteric crest. The humeral torsion, the length of the deltopectoral crest, the large bicipital groove and the well-developed lesser tubercle, indicate that the forelimb of Brasilodon was hold in a semi-sprawling position, with well-developed adductor muscles to maintain the body off the ground. The short femoral neck and the strong medial projection of the femoral head indicate the femur was held in a more erect posture than in basal non-mammaliaform cynodonts. The anterodorsally projected iliac blade with reduced postacetabular process, reduction of the anterior part of the pubis, medially located lesser trochanter indicate a basically mammalian pattern of pelvic musculature, able to swing the femur in a nearly parasagittal plane.

Fig 13. Paleoartistic reconstruction of Brasilodon quadrangularis (left) and Riograndia guaibensis (right), two abundant probainognathian cynodonts from the Riograndia Assemblage Zone of the Candelária Sequence, Santa Maria Supersequence (Brazil), which exhibits different morphologies in skull, dentition and locomotor apparatus.
 Illustration: Jorge Blanco.

Conclusion: 
The postcranium of Brasilodon quadrangularis differs from other non-mammaliaform cynodonts and is similar to early mammaliaforms and extant therians (e.g., hemispherical humeral and femoral head, distinct greater tubercle of the humerus, circular acetabulum, salient intertrochanteric crest of the femur). The morphology of the ulnar condyle of the humerus and olecranon process of the ulna suggests more abilities for extension and flexion of the elbow, a necessary component for a parasagittal locomotion. However, the humeral torsion, the length of the deltopectoral crest, the large bicipital groove and the well-developed lesser tubercle, indicate that the forelimb of B. quadrangularis was hold in a semi-sprawling position, with well-developed adductor muscles to maintain the body off the ground. The short femoral neck and the strong medial projection of the femoral head indicate the femur was held in a more erect posture than in basal non-mammaliaform cynodonts. The anterodorsally projected iliac blade with reduced postacetabular process, enlarged obturator foramen, reduction of the anterior part of the pubis, prominent and distinctive greater trochanter, medially located lesser trochanter, narrow intertrochanteric fossa represent a further continuation of trends that indicates a basically mammalian pattern of pelvic musculature, able to swing the femur in a nearly parasagittal plane.

Although fossorial or semifossorial habits appear to have been common in derived non-mammaliaform probainognathians (i.e., Riograndia, Irajatherium and Kayentatherium), the postcranial study of B. quadrangularis shows more generalized adaptations and highlights that distinctive ecological strategies (Fig 13) were developed among small-sized non-mammaliaform cynodonts.


 Morgan L. Guignard, Agustin G. Martinelli and Marina B. Soares. 2019. The Postcranial Anatomy of Brasilodon quadrangularis and the Acquisition of Mammaliaform Traits Among Non-mammaliaform Cynodonts.  PLoS ONE. 14(5): e0216672. DOI: 10.1371/journal.pone.0216672