Showing posts with label Ontogeny. Show all posts
Showing posts with label Ontogeny. Show all posts

Wednesday, August 13, 2025

[PaleoMammalogy • 2025] Janjucetus dullardi • An Immature Toothed Mysticete from the Oligocene of Australia and insights into mammalodontid (Mysticeti: Mammalodontidae) Morphology, Systematics, and Ontogeny

 

Janjucetus dullardi 
Duncan, Rule, Park, Evans, Adams & Fitzgerald, 2025


Abstract
Mammalodontids are a clade of toothed mysticetes known only from the Chattian of south-eastern Australia and New Zealand. Despite three named species (Janjucetus hunderi, Mammalodon colliveri, and Mammalodon hakataramea), the majority of mammalodontid material, largely represented by isolated teeth and ear bones found within the Torquay Basin (Victoria, Australia), remains undescribed. Here we describe a new species of mammalodontid, Janjucetus dullardi sp. nov., from the Jan Juc Marl. The holotype was found stratigraphically lower than M. colliveri and has morphology consistent with an immature stage of growth, plus near-unworn dental morphology. We identify a correlation between occipital condyle breadth and bizygomatic width and propose equations that permit us to estimate bizygomatic width and, subsequently, a body size estimate similar to the smallest known toothed mysticetes of ∼2.05–2.18 m. Phylogenetic analysis recovers J. dullardi as sister to J. hunderi within a monophyletic mammalodontid clade in all analyses. It also provides support for Mammalodontidae within Mysticeti, sister to an Aetiocetidae + Chaeomysticeti clade. Finally, revised diagnoses of Mammalodon and Janjucetus incorporating newly recogniszed tympanic and periotic characters permit the identification of isolated ear bones and inference of ontogenetic variation within Janjucetus.

Australia, Cetacea, Janjucetus, Mammalodon, Mammalodontidae, Mysticeti, Oligocene, ontogeny, phylogeny




Artist’s reconstruction of the complete skull of Janjucetus dullardi.
Parts preserved in the fossil are white and light grey.
 Art by Ruairidh Duncan


Janjucetus dullardi sp. nov. 

Etymology: The species name dullardi honours Mr Ross Dullard, who discovered the holotype.

Type locality, horizon, and age: The holotype of Janjucetus dullardi (NMV P256471) was discovered near the town of Jan Juc in the lowest beds of the exposed onshore Jan Juc Marl at Half Moon Bay, southwest of Bird Rock (Fig. 2) at approximately 38°21′03″S, 144°18′02″E (precise locality details are available on request). The lithology of this cliff face describes a neritic, inner mid-shelf environment, which coarsens upwards, and with relatively low abundance of infauna (Li et al. 1999, McLaren et al. 2009). The type of J. dullardi was found near the base of this outcrop, exposed beneath a wave-eroded overhang, slightly above the level of the tidal beach sands (Fig. 1). The lithology of this horizon [unit 1 and 2 of Reeckmann (1979)] is one of a silty, sandy grey marl, interspersed with bedding planes of coarse silts to fine sandstones and rich in glauconite. A horizon ∼3 m above the fossil-producing layer was aged to 24.67 Mya using strontium isotope ratios (Korasidis et al. 2018). The top of the Bells Headland outcrop, interpreted as ∼2 m stratigraphically lower than the base of the Bird Rock outcrop, was aged to 26.05 Mya at a point correlated to ∼2.5 m below the horizon containing NMV P256471 using the same methodology (Korasidis et al. 2018). We therefore give an estimated age of this specimen of between 24.67 and 26.05 Mya (middle Chattian).

Diagnosis: We interpret J. dullardi as a mammalodontid on the basis of: the presence of an involucral concavity on the medial surface of the tympanic bulla ventral to the involucral ridge; a dorsomedially extended and anteroposteriorly wide crista transversa, which reaches to the level of the rim of the internal acoustic meatus medially (also seen in Salishicetus and Coronodon); and the presence of apicobasal ridges on both the buccal and lingual surfaces of the tooth crowns (also seen in Morawanocetus, ­Coronodon, and Llanocetus).

This specimen shares the following features with J. hunderi to the exclusion of Mammalodon: an obliquely truncated rather than squared anterior margin of the tympanic bulla; an inner posterior prominence of the tympanic bulla mediolaterally broader than the outer posterior prominence at the widest point of the bulla; periotic body and posterior process greatly exceed the posterior margin of the fenestra rotunda; anteroposterior and dorsoventral diameters of the anterior process of the periotic are subequal to one another; and the mandibular posterior postcanine teeth lack a distal accessory shelf near the base of the crown.
...

Janjucetus dullardi calf and mother swimming through the shallow seas, 25 million years ago.
Art by Ruairidh Duncan

 
Ruairidh J Duncan, James P Rule, Travis Park, Alistair R Evans, Justin W Adams and Erich M G Fitzgerald. 2025. An Immature Toothed Mysticete from the Oligocene of Australia and insights into mammalodontid (Cetacea: Mysticeti) Morphology, Systematics, and Ontogeny. Zoological Journal of the Linnean Society. 204(4); zlaf090. DOI: doi.org/10.1093/zoolinnean/zlaf090 [12 August 2025] 
https://theconversation.com/a-cornucopia-of-tiny-bizarre-whales-used-to-live-in-australian-waters-heres-one-of-them-262806

Wednesday, March 12, 2025

[Paleontology • 2025] Darwinopterus camposi • A New Species of Darwinopterus (Pterosauria: Wukongopteridae) from western Liaoning provides some new information on the Ontogeny of this clade

 

Darwinopterus camposi
Cheng, Jiang, Bantim, Sayão, Saraiva, Meng, Kellner & Wang, 2025
 

Abstract
The Wukongopteridae is an important pterosaur clade from the Yanliao Biota, combining features of basal and derived pterosaurs. So far, the Wukongopteridae consists of five species divided into three genera: Wukongopterus lii, Darwinopterus modularis, Darwinopterus linglongtaensis, Darwinopterus robustodens, and Kunpengopterus sinensis. Here we report a new species, Darwinopterus camposi sp. nov., based on an almost complete skeleton (IVPP V 17957). The new species is referred to Darwinopterus due to the presence of an elongated posterior region of the skull and the bony premaxillary crest that starts about the anterior margin of the nasoantorbital fenestra. It differs from all other wukongopterids by having the dorsal margin of the premaxillary crest straight, without an extensive dorsal projection and presenting a smooth lateral surface. Furthermore, D. camposi sp. nov. has eighteen and fourteen teeth on each side of the upper and lower jaws, respectively, and the fourth phalanx of the wing finger shorter than the first. IVPP V 17957 shows some fused postcranial bones, like the extensor tendon process to the first wing finger phalanx, but also has unfused premaxilla and frontal, which provides further information about wukongopterid ontogeny.

Key words: Pterosauria; Wukongopteridae; ontogeny; Yanliao Biota; Middle-Late Jurassic; China



SYSTEMATIC PALEONTOLOGY
Pterosauria Kaup 1834
Wukongopteridae Wang, Kellner, Jiang and Meng 2009

Darwinopterus Lü, Unwin, Jin, Liu and Ji 2010

Darwinopterus camposi sp. nov.

 Holotype: Almost complete skeleton lacking the distal end of the tail and hindlimbs, housed at the Institute of Vertebrate Paleontology and Paleoanthropology, Beijing, under the number IVPP V 17957 (Figs. 1-Fig. 4).

Etymology: In honor to Dr. Diogenes de Almeida Campos, an important geologist and vertebrate paleontologist who has contributed to pterosaur research and the cooperation between Brazilian and Chinese paleontologists.
 


Cheng, X.; Jiang, S.; Bantim, R. A. M.; Sayão, J. M.; Saraiva, A. Á. F.; Meng, X.; Kellner, A. W. A.; Wang, X. 2025. A New Species of Darwinopterus (Wukongopteridae, Pterosauria) from western Liaoning provides some new information on the Ontogeny of this clade. Anais da Academia Brasileira de Ciências. 97 (Suppl. 1). e20240707. DOI: doi.org/10.1590/0001-3765202520240707

Wednesday, October 9, 2024

[Paleontology • 2024] Ardetosaurus viator • A New diplodocine Sauropod from the Morrison Formation, Wyoming, USA


 Ardetosaurus viator
van der Linden, Tschopp, Sookias, Wallaard, Holwerda & Schulp, 2024

 DOI: 10.26879/1380 
  Life reconstruction by Ole Zant. x.com/TheBioBob

ABSTRACT
The Morrison Formation of the western United States is well-known for its high diversity of sauropod dinosaurs. The Howe-Stephens Quarry in northern Wyoming is one of several quarries which has yielded several associated to completely articulated dinosaur specimens, among which a semi-articulated diplodocid specimen, MAB011899, which was excavated in 1993. This diplodocid specimen is represented by posterior cervical, dorsal, sacral, and anterior caudal vertebrae, multiple thoracic ribs, two chevrons, a left coracoid, a left ilium, both pubes and ischia, a left femur, a left tibia, and a left fibula. Through comparative anatomy, we interpret this specimen as a new species of diplodocine sauropod, Ardetosaurus viator gen. et sp. nov. Unambiguous autapomorphies include paired accessory laminae in the spinoprezygapophyseal fossae of posterior cervical and anterior dorsal vertebrae, bifurcating anterior centrodiapophyseal laminae in the anterior dorsal vertebrae, fossae present in the centropostzygapophyseal laminae of the second dorsal vertebra, a low vertebral height/centrum length ratio of the posterior dorsal vertebrae and reduced to absent centroprezygapophyseal laminae in the anterior caudal vertebrae. Local autapomorphic features include single centroprezygapophyseal laminae in the posterior cervical vertebrae and a highly elliptical cross-section of the femoral midshaft. Ardetosaurus viator is the first skeletally mature sauropod specimen described from the Howe-Stephens Quarry. This specimen provides insight into serial variation of vertebral laminae and laminar transitions. Finally, the peculiar morphology of the—often not preserved—first chevron is described in detail, and its possible use in studying sexual dimorphism in sauropods is discussed.

Keywords: sauropod; new genus; new species; Morrison Formation; Diplodocinae; Wyoming




  Skeletal reconstruction of  Ardetosaurus viator MAB011899. Skeletal reconstruction indicating preserved bones (white), excavated bones but subsequently lost (light gray) and not preserved (dark gray). Unknown elements are based on other diplodocines.
Scale bar equals 1 m. Reconstruction by Ole Zant.

SYSTEMATIC PALEONTOLOGY
DINOSAURIA Owen, 1842
SAUROPODA Marsh, 1878
EUSAUROPODA Upchurch, 1995
NEOSAUROPODA Bonaparte, 1986

DIPLODOCOIDEA Marsh, 1884
FLAGELLICAUDATA Harris and Dodson, 2004

DIPLODOCIDAE Marsh, 1884
DIPLODOCINAE Marsh, 1884

ARDETOSAURUS gen. nov.
 
Ardetosaurus viator gen. et sp. nov.
 
Holotype. MAB011899: two cervical vertebrae, 10 dorsal vertebrae, sacrum, five caudal vertebrae, eight dorsal ribs, two chevrons, a left coracoid, a left ilium, both pubes, both ischia, a left femur, a left tibia, and a partial left fibula.

Diagnosis. Ardetosaurus viator is diagnosed by the combination of the following autapomorphies: 1) the presence of distinct, paired accessory laminae in the spinoprezygapophyseal fossae (SPRF) in the posterior cervical and anterior dorsal vertebrae, 2) anteroventrally bifurcating anterior centrodiapophyseal laminae (ACDLs) in the anterior dorsal vertebrae, 3) the presence of centropostzygapophyseal lamina fossae (CPOL-f) in the second dorsal vertebra, 4) a vertebral height/centrum length ratio of <2.5 of the posterior dorsal vertebrae, and 5) reduced or absent centroprezygapophyseal laminae (CPRLs) in the anterior-most caudal vertebrae. Ardetosaurus viator differs from all other diplodocines by having unbifurcated CPRLs in the posterior cervical vertebrae and a highly elliptical femoral cross-section. Ardetosaurus viator differs from Amphicoelias Cope, 1878, in lacking the rounded, lateral projections of the neural spine tip and the thin neural spine base in the dorsal vertebrae; from Barosaurus Marsh, 1890, by having tall cervical neural spines, single midline keels, narrower prezygapophyseal rami in the cervical vertebrae, ten dorsal vertebrae, the presence of ...


Etymology. ‘Ardeto’ is an inflection of Latin ārdēre, meaning ‘to burn.’ It refers to the history of some of the elements, which were either fully destroyed in a fire, or still show burn scars from the fire. ‘saurus, ’ Latinized form of the Greek σαῦρος (saúros), meaning lizard or reptile. ‘viator’ is Latin for traveler, referring to the journey of the specimen from the USA, via Switzerland and Germany, to the Netherlands.

Locality and horizon. Ardetosaurus viator comes from the Howe-Stephens Quarry of northern Wyoming, USA. The quarry is dated, based on magnetostratigraphy and correlation with other sections in the Morrison basin (Maidment and Muxworthy, 2019; Maidment, personal communication, 2022) at 150.44 to 149.21 million years old, placing it in the Kimmeridgian Stage of the Upper Jurassic.


 Quarry map of Ardetosaurus viator MAB011899. Excavation map of the Howe-Stephens Quarry, indicating the major finds from 1992-2000. Individual dinosaurs are color coded, and MAB011899 is coded with dark blue, and named ‘Diplodocus Brösmeli’ herein. The red crosses indicate the missing/lost cervical vertebrae. Note the relatively similar color for ‘Brösmeli’ and ‘David’ (SMA 0086), but their significant separation in the quarry.
 Figure is courtesy of the SMA. Quarry sections equal 1 by 0.5 m.


  Life reconstruction of  Ardetosaurus viator MAB011899.
Illustration by Ole Zant.

The skeleton of Brösmeli is on display in the Oertijdmuseum.


Tom T.P. van der Linden, Emanuel Tschopp, Roland B. Sookias, Jonathan J.W. Wallaard, Femke M. Holwerda, and Anne S. Schulp. 2024. A New diplodocine Sauropod from the Morrison Formation, Wyoming, USA. Palaeontologia Electronica. 27(3): a50. DOI: doi.org/10.26879/1380
palaeo-electronica.org/content/2024/5327-new-diplodocine-sauropod

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

Monday, December 11, 2023

[Paleontology • 2023] Exceptionally preserved Stomach Contents of A Young tyrannosaurid reveal An Ontogenetic Dietary Shift in an iconic Extinct Predator


Gorgosaurus libratus feeding on Citipes elegans.

in Therrien, Zelenitsky, Tanaka, Voris, ... et Kobayashi, 2023.

Illustration by Julius Csotonyi 
 
Abstract
Tyrannosaurids were large carnivorous dinosaurs that underwent major changes in skull robusticity and body proportions as they grew, suggesting that they occupied different ecological niches during their life span. Although adults commonly fed on dinosaurian megaherbivores, the diet of juvenile tyrannosaurids is largely unknown. Here, we describe a remarkable specimen of a juvenile Gorgosaurus libratus that preserves the articulated hindlimbs of two yearling caenagnathid dinosaurs inside its abdominal cavity. The prey were selectively dismembered and consumed in two separate feeding events. This predator-prey association provides direct evidence of an ontogenetic dietary shift in tyrannosaurids. Juvenile individuals may have hunted small and young dinosaurs until they reached a size when, to satisfy energy requirements, they transitioned to feeding on dinosaurian megaherbivores. Tyrannosaurids occupied both mesopredator and apex predator roles during their life span, a factor that may have been key to their evolutionary success.



Juvenile Gorgosaurus TMP 2009.12.14 preserving stomach contents.
Photographs of specimen in (A) right lateral view and (B) left anterolateral view. (C) Interpretive illustration of specimen in right lateral view. Skeleton consists of a nearly complete skull, the left side of the body and limbs, and a nearly complete pelvis. Red rectangle delineates location of stomach contents. (D) Histological photomicrograph of tibia showing the presence of five lines of arrested growths and two annuli (marked by asterisks), indicating that the individual was between 5 and 7 years old.
Scale bars, 50 cm (A) to (C) and 1 mm (D).

  


Juvenile Citipes remains preserved as stomach contents.
(A) Diagram illustrating relative body sizes of predator and prey and skeletal elements preserved in TMP 2009.12.14. Scale bar, 50 cm.
Histological photomicrographs of (B) posterior Citipes individual (metatarsal II) and (C) anterior Citipes individual (tibia), showing highly vascularized woven bone with reticular and longitudinally oriented vascular canals and lacking growth lines, indicative of young individuals that are less than 1 year old. Scale bars, 500 μm.

Gorgosaurus libratus feeding on Citipes elegans.
Illustration by Julius Csotonyi 


 Francois Therrien, Darla K. Zelenitsky, Kohei Tanaka, Jared T. Voris, Gregory M. Erickson, Philip J. Currie, Christopher L. Debuhr, and Yoshitsugu Kobayashi. 2023. Exceptionally preserved Stomach Contents of A Young tyrannosaurid reveal An Ontogenetic Dietary Shift in an iconic Extinct Predator. SCIENCE ADVANCES. 9, 49. DOI: 10.1126/sciadv.adi0505

 


Tuesday, November 21, 2023

[PaleoMammalogy • 2023] New Skeletons of the Ancient Dolphin Xenorophus sloanii and Xenorophus simplicidens sp. nov. (Cetacea: Odontoceti) from the Oligocene of South Carolina and the Ontogeny, Functional Anatomy, Asymmetry, Pathology, and Evolution of the Earliest Odontoceti


Xenorophus simplicidens 
Boessenecker & Geisler, 2023


Abstract
The early diverging, dolphin-sized, cetacean clade Xenorophidae are a short-lived radiation of toothed whales (Odontoceti) that independently evolved two features long thought to be odontocete synapomorphies: the craniofacial and cochlear morphology underlying echolocation and retrograde cranial telescoping (i.e., posterior migration of the viscerocranium). This family was based on Xenorophus sloanii, which, for the past century, has been known only by a partial skull lacking a braincase and tympanoperiotics, collected around 1900 from the Ashley Formation (28–29 Ma, Rupelian) near Ladson, South Carolina. A large collection of new skulls and skeletons (ChM PV 5022, 7677; CCNHM 104, 168, 1077, 5995) from the Ashley Formation considerably expands the hypodigm for this species, now the best known of any stem odontocete and permitting evaluation of intraspecific variation and ontogenetic changes. This collection reveals that the holotype (USNM 11049) is a juvenile. Xenorophus sloanii is a relatively large odontocete (70–74 cm CBL; BZW = 29–31 cm; estimated body length 2.6–3 m) with a moderately long rostrum (RPI = 2.5), marked heterodonty, limited polydonty (13–14 teeth), prominent sagittal crest and intertemporal constriction, and drastically larger brain size than basilosaurid archaeocetes (EQ = 2.9). Dental morphology, thickened cementum, a dorsoventrally robust rostrum, and thick rugose enamel suggest raptorial feeding; oral pathology indicates traumatic tooth loss associated with mechanically risky predation attempts. Ontogenetic changes include increased palatal vomer exposure; fusion of the nasofrontal, occipito-parietal, and median frontal sutures; anterior lengthening of the nasals; elaboration of the nuchal crests; and blunting and thickening of the antorbital process. The consistent deviation of the rostrum 2–5° to the left and asymmetry of the palate, dentition, neurocranium, mandibles, and vertebrae in multiple specimens of Xenorophus sloanii suggest novel adaptations for directional hearing driven by the asymmetrically oriented pan bones of the mandibles. A second collection consisting of a skeleton and several skulls from the overlying Chandler Bridge Formation (24–23 Ma, Chattian) represents a new species, Xenorophus simplicidens n. sp., differing from Xenorophus sloanii in possessing shorter nasals, anteroposteriorly shorter supraorbital processes of the frontal, and teeth with fewer accessory cusps and less rugose enamel. Phylogenetic analysis supports monophyly of Xenorophus, with specimens of Xenorophus simplicidens nested within paraphyletic X. sloanii; in concert with stratigraphic data, these results support the interpretation of these species as part of an anagenetic lineage. New clade names are provided for the sister taxon to Xenorophidae (Ambyloccipita), and the odontocete clade excluding Xenorophidae, AshleycetusMirocetus, and Simocetidae (Stegoceti). Analyses of tooth size, body size, temporal fossa length, orbit morphology, and the rostral proportion index, prompted by well-preserved remains of Xenorophus, provide insight into the early evolution of Odontoceti.

Keywords: Xenorophidae; Odontoceti; Cetacea; Oligocene; asymmetry

 Geographic and geologic context of Xenorophus fossils from South Carolina.
(A) Map of South Carolina. (B) Simplified geologic map of Oligocene rocks within the Charleston Embayment. (C) Stratigraphic column of the Ashley and Chandler Bridge formations of South Carolina, showing stratigraphic position of age determinations (stars) and silhouettes of the xenorophid assemblage known from each stratum. Modified from Boessenecker et al. ([2023]: Figure 1).

  Systematic Paleontology
Mammalia Linneaus,1758 
Cetacea Brisson, 1762 
Odontoceti Flower, 1867 
Xenorophidae Uhen, 2008 

Xenorophus Kellogg, 1923 





Xenorophus simplicidens sp. nov.
Xenorophus n. sp. Sanders, 1996 
Xenorophus sp. Sanders and Geisler, 2015 

Holotype: CCNHM 8720, a partial skeleton including a nearly complete but crushed skull, right mandible, nearly complete upper and lower dentition, five cervical vertebrae, eight or nine thoracic vertebrae, nine or ten lumbar vertebrae, and at least six ribs, collected in 2017 by Dean Rogers, Everett White, and Joshua Basak from Bed 2 of the Chandler Bridge Formation in the vicinity of North Charleston, Charleston County, South Carolina.

Diagnosis of Species: A large xenorophid dolphin, with approximate adult condylobasal length of 68–74 cm and bizygomatic width of 27–30.8 cm and differing from Xenorophus sloanii in possessing anteroposteriorly shorter nasals (16–19% of bizygomatic width vs. 22–29% in X. sloanii), nasal process of premaxilla lacking lateral overhanging crest adjacent to bony nares in adult specimens, right antorbital fossa longer than left (left longer than right in X. sloanii), rounded anterior margin of bony nares, anteroposteriorly shorter supraorbital process (distance from antorbital notch to posterior edge of supraorbital process 34% of bizygomatic width vs. 43% in X. sloanii), slightly narrower nasals with posterior end narrower than bony nares, left and right palatines separated by an anteroposteriorly long median triangular exposure of maxilla, paroccipital processes not extending posterior to occipital condyles, longer median furrow on the tympanic bulla (except ChM PV 4266), fewer teeth with accessory denticles (only on PC 7–9, as opposed to PC 5–9 in X. sloanii), fewer accessory denticles per tooth (three distal cusps vs. five in X. sloanii; one–three mesial cusps vs. three–four in X. sloanii), widespread striated enamel throughout dentition and nodular enamel only present on PC7–9 and less rugose than in X. sloanii (nodular enamel on PC5–9).


Etymology: simplicidenssimplex + dens—meaning simple teeth in Latin, referring to the reduced cingula and smoother enamel of this species. This name was coined by Albert Sanders and conveyed to the second author prior to his passing.

 Locality and Age: All specimens of Xenorophus simplicidens were collected from the upper Oligocene Chandler Bridge Formation in the Charleston Embayment, ranging in age from 24.7 to 23.5 Ma. 



 Robert W. Boessenecker and Jonathan H. Geisler. 2023. New Skeletons of the Ancient Dolphin Xenorophus sloanii and Xenorophus simplicidens sp. nov. (Mammalia, Cetacea) from the Oligocene of South Carolina and the Ontogeny, Functional Anatomy, Asymmetry, Pathology, and Evolution of the Earliest Odontoceti. Diversity. 15(11), 1154. DOI: 10.3390/d15111154
(This article belongs to the Special Issue Evolution of Crown Cetacea)

Tuesday, October 17, 2023

[Paleontology • 2023] Evaluating Growth in Macrospondylus bollensis (Crocodylomorpha: Teleosauroidea) in the Toarcian Posidonia Shale, Germany


Macrospondylus bollensis  Jäger, 1828

in Johnson, Amson & Maxwell, 2023.

Abstract
The study of how organisms grow is a fundamental aspect of palaeontology. Growth in teleosauroids is poorly understood and little studied, especially in an ontogenetic sense. We investigate growth rates of the most common and abundant teleosauroid, Macrospondylus bollensis, in which a large sample of multiple body sizes is available from the Posidonienschiefer Formation (Posidonia Shale) of southwestern Germany. We perform linear regression analyses on 62 specimens of Macrospondylus (16 juveniles, 7 subadults and 39 adults) using 21 cranial and postcranial measurements. Our results show that juvenile, subadult and adult individuals have near-isometric or isometric growth throughout much of the body. Notably, we find that in Macrospondylus: (1) the femur grows at a faster rate than the skull and hindlimb zeugopodium; (2) the forelimb and hindlimb grow at the same rate; and (3) there is distinct ontogenetic signal in the growth of the orbit and supratemporal fenestra. We also find that limb scaling in Macrospondylus is somewhat comparable to that seen in the extant gavialids Gavialis gangeticus and Tomistoma schlegelii. Last, we examine evolutionary allometry in skull length relative to body size in Crocodylomorpha using femoral length as a proxy, which shows a near-isometric trend. Non-thalattosuchian crocodylomorphs (with the exception of one pholidosaurid and one dryosaurid taxon) are differentiated from thalattosuchians due to their shorter skulls, as previously suggested, but the scaling relationship with femur length remains unchanged.

Keywords: Teleosauroidea, Crocodylomorpha, evolutionary allometry, ontogenetic allometry, Macrospondylus bollensis, Posidonia Shale Formation



 
Michela M. Johnson, Eli Amson and Erin E. Maxwell. 2023. Evaluating Growth in Macrospondylus bollensis (Crocodylomorpha, Teleosauroidea) in the Toarcian Posidonia Shale, Germany. Papers in Palaeontology. DOI: 10.1002/spp2.1529
  phys.org/news/2023-10-size-growth-marine-crocodiles-jurassic.html

Tuesday, February 28, 2023

[Paleontology • 2023] Cribroconcha honggulelengensis • Allometry in Late Devonian Podocopa Ostracods (Crustacea) and its implications for Ostracod Ontogeny


Cribroconcha honggulelengensis Song & Crasquin, 2017
in the Upper Devonian Hongguleleng Formation 
of western Junggar, NW China

in Song, Huang & Qie, 2023. 

 Abstract
Podocopa ostracods have abounded in various marine and non-marine habitats since the early Palaeozoic and left a diverse fossil record in strata worldwide. This is particularly useful for stratigraphic correlation and palaeoenvironmental and palaeogeographical reconstructions. However, despite being the most numerous ostracods during the Palaeozoic, their origins, evolution, ontogeny and phylogeny remain poorly defined. This paper represents the first study of morphological variation in Devonian Platycopida ostracods (an order of Podocopa) using a geometric morphometric approach. Our results identify substantial shape variation in Cribroconcha honggulelengensis Song & Crasquin from the Upper Devonian Hongguleleng Formation of western Junggar, northwest China, demonstrating a remarkable change in juveniles between stages A-3 and A-2. Using linear regressions between principal component scores from right lateral view and carapace length, we demonstrate allometric growth patterns for this species. The body plan of C. honggulelengensis developed along an ontological variable: from an ovate outline with rare pores to an oblong outline with dense and large pores. Environmental factors should play an important role in shape determination during ontogeny of C. honggulelengensis.


Ecological reconstruction and life mode interpretation of Cribroconcha honggulelengensis Song & Crasquin, 2017 in the Upper Devonian Hongguleleng Formation of western Junggar, NW China

  
Junjun Song, Bing Huang and Wenkun Qie. 2023. Allometry in Late Devonian Podocopa Ostracods (Crustacea) and its implications for Ostracod Ontogeny. Papers in Palaeontology. DOI: 10.1002/spp2.1480

Study on ontogeny of Platycopida ostracods in Late Devonian reveals the mystery of Paleozoic ostracod evolution
https://phys.org/news/2023-02-reveals-mystery-paleozoic-ostracod-evolution.html

Monday, November 28, 2022

[Paleontology • 2022] The Ontogenetic Growth of Anhangueridae (Pterosauria: Pterodactyloidea) Premaxillary Crests as revealed by A Crestless Anhanguera Specimen


Anhanguera sp. 

in Duque, Pinheiro et Barreto, 2022. 
Digital painting by Matheus Fernandes Gadelha.

ABSTRACT
The Anhangueridae are a clade of toothed pterodactyloid pterosaurs, known from their characteristic anteriorly expanded premaxillae and conspicuous rostral sagittal premaxillary and dentary crests. Most known anhanguerids come from the Lower Cretaceous Romualdo Formation within the Araripe Basin of northeast Brazil. With four currently valid genera and several specimens referred to the clade, anhanguerids are the most abundant and diverse tetrapod group in the Romualdo Formation. However, some studies suggest this diversity may be overestimated, as many taxa have been diagnosed based on subtle differences in their premaxillary crests, a structure argued to be either ontogenetically variable or sexually dimorphic. Here we describe an anterior fragment of a gracile pterosaur rostrum that possesses the single diagnostic feature of Anhanguera (fifth and sixth pairs of dental alveoli smaller than the fourth and seventh), but lacks a sagittal crest. The affinities of the new fossil among other toothed pterosaurs were tested through both cladistic and geometric morphometric approaches, which allow referral of the new specimen to Anhanguera. The absence of a crest in the new specimen of Anhanguera suggests that this structure varies in terms of ontogeny and/or sex, and that perhaps it was influenced by sexual selection.

 Artistic reconstruction based on specimen DGEO-CTG-UFPE 8283.
A, skull of a young individual; B, reconstructed skull of an ontogenetically advanced individual.
Scale bar equals 100 mm. 
Digital painting by Matheus Fernandes Gadelha.


Rudah Ruano C. Duque, Felipe L. Pinheiro and Alcina Magnólia Franca Barreto. 2022. The Ontogenetic Growth of Anhangueridae (Pterosauria, Pterodactyloidea) Premaxillary Crests as revealed by A Crestless Anhanguera Specimen. Journal of Vertebrate Paleontology. 42(1);  e2116984. DOI: 10.1080/02724634.2022.2116984