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1. A median fin derived from the lateral plate mesoderm and the origin of paired fins

   https://doi.org/10.1038/s41586-023-06100-w  

   Tzung, Keh-Weei; Lalonde, Robert L.; Prummel, Karin D.; Mahabaleshwar, Harsha; Moran, Hannah R.; Stundl, Jan; Cass, Amanda N.; Le, Yao; Lea, Robert; Dorey, Karel; et al (April 2023, Nature)

   Abstract The development of paired appendages was a key innovation during evolution and facilitated the aquatic to terrestrial transition of vertebrates. Largely derived from the lateral plate mesoderm (LPM), one hypothesis for the evolution of paired fins invokes derivation from unpaired median fins via a pair of lateral fin folds located between pectoral and pelvic fin territories 1 . Whilst unpaired and paired fins exhibit similar structural and molecular characteristics, no definitive evidence exists for paired lateral fin folds in larvae or adults of any extant or extinct species. As unpaired fin core components are regarded as exclusively derived from paraxial mesoderm, any transition presumes both co-option of a fin developmental programme to the LPM and bilateral duplication 2 . Here, we identify that the larval zebrafish unpaired pre-anal fin fold (PAFF) is derived from the LPM and thus may represent a developmental intermediate between median and paired fins. We trace the contribution of LPM to the PAFF in both cyclostomes and gnathostomes, supporting the notion that this is an ancient trait of vertebrates. Finally, we observe that the PAFF can be bifurcated by increasing bone morphogenetic protein signalling, generating LPM-derived paired fin folds. Our work provides evidence that lateral fin folds may have existed as embryonic anlage for elaboration to paired fins. 

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2. The element of Paaw in marsupials and the middle ear of Philander opossum (Linnaeus, 1758) (Didelphimorphia, Didelphidae)

   Wible, John R.; Shelley, Sarah L.; Belz, Carly (May 2021, Annals of Carnegie Museum)

   null (Ed.)

   A small piece of cartilage or bone, the element of Paaw, occurs in the tendon of the stapedius muscle in some extant marsupial and placental mammals. It has been nearly a century since the last comprehensive treatment of the distribution of the element of Paaw in mammals. The current report updates knowledge on this structure by synthesizing the subsequent literature and providing new observations of extant marsupials from the collections of the Section of Mammals, Carnegie Museum of Natural History, and two online resources for CT scanned data: DigiMorph.org and MorphoSource.org. We found an element of Paaw in some representatives of all seven extant marsupial orders: Didelphimorphia, Microbiotheria, Notoryctemorphia, Peramelemorphia, Paucituberculata, Dasyuromorphia, and Diprotodontia. In the first four orders, the element is substantial, longer than the long axis of the fenestra vestiuli (oval window), which holds the stapedial footplate; it is smaller than the long axis of the fenestra vestibuli in Paucituberculata and we do not have measures to report for the last two orders. In most marsupials examined, the element of Paaw contacts the petrosal behind the oval window, suggesting it functions as a sesamoid bone, increasing the lever arm of the stapedius muscle. Although there is some variability in the presence of the bone both between and within individual museum specimens, we interpret this as the result of preparation techniques rather than true variation. To place the element of Paaw in its anatomical context, we describe in detail the ear region and middle-ear auditory apparatus of the gray four-eyed opossum, Philander opossum (Linnaeus, 1758), a didelphid from Central and South America, based on a CT scanned specimen from Carnegie Museum of Natural History. It has an ossified element of Paaw with a volume greater than the stapes. Comparisons are made with petrosals of Didelphis marsupialis Linnaeus, 1758, and Monodelphis domestica (Wagner, 1842), also based on CT scanned specimens. 

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3. On the relationship between collagen- and carbonate-derived carbon isotopes with implications for the inference of carnivore dietary behavior

   https://doi.org/10.3389/fevo.2022.1031383  

   DeSantis, Larisa R.; Feranec, Robert S.; Southon, John; Cerling, Thure E.; Harris, John; Binder, Wendy J.; Cohen, Joshua E.; Farrell, Aisling B.; Lindsey, Emily L.; Meachen, Julie; et al (December 2022, Frontiers in Ecology and Evolution)

   Studies of Rancho La Brea predators have yielded disparate dietary interpretations when analyzing bone collagen vs. enamel carbonate—requiring a better understanding of the relationship between stable carbon isotopes in these tissues. Stable carbon isotope spacing between collagen and carbonate (Δ ca-co ) has also been used as a proxy for inferring the trophic level of mammals, with higher Δ ca-co values indicative of high carbohydrate consumption. To clarify the stable isotope ecology of carnivorans, past and present, we analyzed bone collagen (carbon and nitrogen) and enamel carbonate (carbon) of extinct and extant North American felids and canids, including dire wolves, sabertooth cats, coyotes, and pumas, supplementing these with data from African wild dogs and African lions. Our results reveal that Δ ca-co values are positively related to enamel carbonate values in secondary consumers and are less predictive of trophic level. Results indicate that the foraging habitat and diet of prey affects Δ ca-co in carnivores, like herbivores. Average Δ ca-co values in Pleistocene canids (8.7+/−1‰) and felids (7.0+/−0.7‰) overlap with previously documented extant herbivore Δ ca-co values suggesting that trophic level estimates may be relative to herbivore Δ ca-co values in each ecosystem and not directly comparable between disparate ecosystems. Physiological differences between felids and canids, ontogenetic dietary differences, and diagenesis at Rancho La Brea do not appear to be primary drivers of Δ ca-co offsets. Environmental influences affecting protein and fat consumption in prey and subsequently by predators, and nutrient routing to tissues may instead be driving Δ ca-co offsets in extant and extinct mammals. 

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4. Shoulder joint range of motion in fossil synapsids and the origins of mammalian locomotor diversity

   Brocklehurst, R. J. (July 2020, Journal of Vertebrate Paleontology, Program and Abstracts, 2020)

   null (Ed.)

   Extant mammals are both taxonomically and ecologically diverse, having evolved a remarkable array of locomotor ecologies (e.g., swimming, digging, and flying). Evolution of the therian-type forelimb, with a highly reduced pectoral girdle and ball-and-socket shoulder joint, has been heralded as a key innovation that enabled mammals to co-opt their forelimbs for diverse functions. The acquisition of the mammal forelimb can be traced through their forerunners, the non-mammalian synapsids (NMS), but exactly how this musculoskeletal transformation proceeded and its impact on functional diversification have not be quantitatively tested. To explore the evolution of forelimb functional diversity in synapsids, we measured shoulder joint osteological range of motion (ROM) in a range of extant amniotes (lizards, monotremes, therian mammals), and compared their patterns of joint mobility to exemplars from each of the major grades of NMS: ‘pelycosaurs’, basal therapsids, and non-mammalian cynodonts. Three-dimensional models of the shoulder girdles and humeri were digitally aligned in an anatomical ‘neutral pose’ using a semi-automated approach based on articular surface morphology. ROM was then determined for the shoulder joint using a fully automated method, where the humerus was moved in flexion-extension, adduction-abduction, and pronation-supination until bone-to-bone contact occurred. Relative degree and directionality of mobility were then compared across taxa. We find an increase in total shoulder joint ROM through synapsid evolution, suggesting that more derived NMS could perform a wider range of limb movements. However, we also see more complex trends in directionality of shoulder mobility that may be indicators of forelimb posture. Extant lepidosaurs and monotremes had the greatest ROM in abduction-adduction, whereas therians had more ROM in flexion-extension, likely related to ‘sprawling’ vs. ‘erect’ gaits. Therapsids and cynodonts both had greatest ROM in abduction-adduction, matching previous reconstructions of these taxa as sprawling to semi-erect. However, ‘pelycosaurs’ had the greatest ROM in flexion-extension, despite having abducted forelimbs, suggesting they did not move their forelimbs in same manner as modern sprawling animals. Our results demonstrate the complex nature of forelimb evolution in synapsids and provide novel insights into the functional transformation and diversification of the mammalian forelimb. Funding Sources Funding information: NSF DEB- 1757749 (S.E.P) and NSF DEB-1754502 (K.D.A). 

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5. Skull Sutures and Cranial Mechanics in the Permian Reptile Captorhinus aguti and the Evolution of the Temporal Region in Early Amniotes

   https://doi.org/10.3389/fevo.2022.841784  

   Abel, Pascal; Pommery, Yannick; Ford, David Paul; Koyabu, Daisuke; Werneburg, Ingmar (May 2022, Frontiers in Ecology and Evolution)

   While most early limbed vertebrates possessed a fully-roofed dermatocranium in their temporal skull region, temporal fenestrae and excavations evolved independently at least twice in the earliest amniotes, with several different variations in shape and position of the openings. Yet, the specific drivers behind this evolution have been only barely understood. It has been mostly explained by adaptations of the feeding apparatus as a response to new functional demands in the terrestrial realm, including a rearrangement of the jaw musculature as well as changes in strain distribution. Temporal fenestrae have been retained in most extant amniotes but have also been lost again, notably in turtles. However, even turtles do not represent an optimal analog for the condition in the ancestral amniote, highlighting the necessity to examine Paleozoic fossil material. Here, we describe in detail the sutures in the dermatocranium of the Permian reptileCaptorhinus aguti(Amniota, Captorhinidae) to illustrate bone integrity in an early non-fenestrated amniote skull. We reconstruct the jaw adductor musculature and discuss its relation to intracranial articulations and bone flexibility within the temporal region. Lastly, we examine whether the reconstructed cranial mechanics inC. aguticould be treated as a model for the ancestor of fenestrated amniotes. We show thatC. agutilikely exhibited a reduced loading in the areas at the intersection of jugal, squamosal, and postorbital, as well as at the contact between parietal and postorbital. We argue that these “weak” areas are prone for the development of temporal openings and may be treated as the possible precursors for infratemporal and supratemporal fenestrae in early amniotes. These findings provide a good basis for future studies on other non-fenestrated taxa close to the amniote base, for example diadectomorphs or other non-diapsid reptiles. 

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