Research Article |
|
Corresponding author: Sanjukta Chakravorti ( sanjukta.chakravorti@smns-bw.de ) Academic editor: Nadia Fröbisch
© 2024 Pummy Roy, Sanjukta Chakravorti, Dhurjati Prasad Sengupta.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Roy P, Chakravorti S, Sengupta DP (2024) Osteology and revised diagnosis of Cherninia denwai from the Middle Triassic Denwa Formation, Satpura Gondwana Basin, Central India. In: Witzmann F, Ruta M, Fröbisch N (Eds) The fish-to-tetrapod transition and the conquest of land by vertebrates . Fossil Record 27(3): 423-443. https://doi.org/10.3897/fr.27.135664
|
The Middle Triassic Denwa Formation located within the Satpura Gondwana basin of Central India exhibits a significant presence of temnospondyl amphibians classified under the family Mastodonsauridae. Prior investigations have documented two taxa of the Mastodonsauridae family, namely Cherninia denwai and Paracyclotosaurus crookshanki, from the Denwa Formation. These prior accounts were predominantly predicated upon two holotype skull specimens, thereby neglecting other specimens contained within the collection as well as various associated post-cranial materials. Recently, a diverse assortment of novel specimens pertaining to C. denwai has been unearthed from the Denwa Formation. Utilizing both the newly acquired specimens and previously overlooked specimens, this study presents a redescription of C. denwai. The newly discovered specimens comprise a partial skull, a mandible, clavicles, interclavicles, vertebrae, neural arches and spines, ulnae, an ilium, a femur, and a fibula, all of which are described herein for the first time. An extensive osteological analysis of the skull and mandible is conducted. It is noted that C. denwai coexists temporally with C. megarhina, and both taxa exhibit distinct synapomorphies; however, they are recognized as separate and unique species.
Capitosauridae, Gondwana, India, Middle Triassic, Temnospondyl
Temnospondyls were highly diverse amphibians having nearly 200 genera and 290 species showing high disparity and diversity. They range in size from a few centimeters to more than 6 meters (
The mastodonsaurids are the most widely distributed temnospondyls present in most of the vertebrate-bearing strata of the Triassic (
The Middle Triassic Denwa Formation of Satpura Gondwana Basin, Central India (Fig.
Two mastodonsaurids, Cherninia denwai and Paracyclotosaurus crookshanki have already been described (
A cumulative total of approximately 80 skeletal elements have now been documented and ascribed to Cherninia denwai (Suppl. material
Anatomical abbreviations: AC: Anterior coronoid; AF: Adductor fossa; AN: Angular; APV: Anterior palatal vacuity; AR: Articular; Cm: Crista muscularis; CT: Cultriform process; D: Dentary; ECT: Ectopterygoid; EO: Exoccipital; F: Frontal; FM: Foramen magnum; GF: Glenoid fossa; IJ: Insulae jugalis; IN: Internal nares; ITPV: Interpterygoid vacuity; J: Jugal; L: Lacrimal; MC: Middle coronoid; MS: Mandibular sulcus; MX: Maxilla; N: Narial; NA: Naris; O: Orbit; P: Parietal; PAL: Palatine; PAR: Prearticular; PC: Posterior coronoid; PF: Postfrontal; PMF: Posterior Meckelian foramen; PMX: Premaxilla; PNF: Pineal foramen; PO: Postorbital; POSP: Postsplenial; PP: Postparietal; PQF: Paraquadrate foramen; PRF: Prefrontal; PSP: Parasphenoid; PT: Pterygoid; PTF: Post temporal fenestra; Q: Quadrate; QB: Quadrate boss; QJ: Quadratojugal; SA: Surangular; SMX: Septomaxilla; SP: Splenial; SQ: Squamosal; ST: Supratemporal; STV: Subtemporal vacuity; T: Tabular; V: Vomers.
Institutional abbreviations: ISI: Indian Statistical Institute, Kolkata (Geological Studies Unit).
Temnospondyli von Zittel, 1887–1890
Stereospondyli von Zittel, 1887–1890
Capitosauroidea Watson, 1920
[nom. Trans. (
Mastodonsauridae Damiani, 2001
Genus: Cherninia Damiani, 2001
(= ‘Parotosuchus’ denwai Mukherjee & Sengupta, 1998).
Denwa Formation (Middle Denwa Formation).
Anisian, Middle Triassic.
Purtala village, Madhya Pradesh, Central India (22°35'38.6"N, 78°32'17.0"E).
ISI A 54, a near complete skull (Fig.
A posterior portion of skull found near Kohpani village (ISI A 207; Fig.
Claviculae of Cherninia denwai from the middle part of the Middle Triassic Denwa Formation. A–C. Left clavicle (ISI A 272) in dorsal, ventral and posterior views, respectively; D–G. Left clavicle (ISI A 273) in dorsal, ventral, lateral and posterior views respectively; H, I. Right clavicle (ISI A 274) in dorsal and ventral views respectively.
A–D. Interclaviculae of Cherninia denwai from the middle part of the Middle Triassic Denwa Formation. A, B. Interclavicle (ISI A 267) in ventral view; C, D. Interclavicle (ISI A 268) in dorsal view; E. Cleithrum (ISI A 275–280) of Cherninia denwai from the middle part of the Middle Triassic Denwa Formation.
Synapomorphies with Mastodonsauridae.
Pre-orbital part of skull (snout) elongated with orbits placed at the posterior half of the dorsal skull roof; orbital margins raised above the dorsal surface of the skull roof; posterolateral corners of the cheek anterior to the level of the posterior edge of the tabular horns; well-developed zone of intensive growth on the preorbital and cheek region of the skull; infraorbital sensory canal forms a Z-shaped loop on the lacrimal bone, the lacrimal flexure; deeply incised otic notch; occipital condyles anterior to quadrate condyles; well-developed, lappet-like tabular horns which are partly supported from below by muscular cristae from the paroccipital process; elongated preorbital projection of the jugal, extending to the lateral border of the snout; supratemporal bone excluded from the border of the otic notch; postorbital antero-laterally expanded (‘hooked’); crista muscularis of the parasphenoid levels with the posterior border of the pterygoid-parasphenoid suture; unbroken chain of teeth on the vomer-palatine-ectopterygoid series; occipital face of the pterygoid bears a tall, narrow, crest-like flange of bone, the oblique ridge of the pterygoid; posttemporal fenestra triangular in shape; mandible with an antero-posteriorly expanded symphysis; a short accessory sensory sulcus dorsal to the oral sulcus present.
Synapomorphies with Cherninia sp.
Pterygoid-parasphenoid suture short, less than the width of the corpus of the parasphenoid; occiput moderately shallow; skull margins moderately concave lateral to the orbits so that the cheek region is flared; prefenestral division of the palate (the region of the palate anterior to the interpterygoid vacuities) markedly elongated; anterior palatal vacuity paired but set in an oval depression so that the vacuities lie below the plane of the palate; elongated and broad snout so that parts of the anterior lateral margin of the skull on both sides are almost parallel to each other; skull roof with conspicuous, paired, forked ridges anterior to the orbits; anterior rim of the otic notch angular; temporal sensory canal extending posteriorly to the tips of the tabular horns; internal nares (choanae) are placed extremely far forward with respect to the interpterygoid vacuities.
Cherninia denwai can be distinguished from Cherninia megarhina, the second known species of Cherninia, by short and narrow postparietals, the presence of a septomaxilla, both anteriorly and posteriorly pointed interpterygoid vacuities, lack of parasphenoid groove, lack of occipital sensory canal, posteriorly directed and distally recurved tabular horns, the deeply concave occipital margin of the skull and the posteriorly broad otic.
Autapomorphies of Cherninia denwai
Skull margins moderately concave lateral to the orbits such that the cheek region is flared; elongated and moderately broad snout; lateral margins of the middle part of the skull anteromedially aligned. The skull roof has conspicuous, paired and forked ridges anterior to the orbits on both sides of the skull. Anterior rim of the otic notch angular (40–60 degrees), tabular horns posteriorly directed and recurved distally, postparietals antero-posteriorly compressed and narrow, deeply concave occipital margin of skull, well expressed lateral line sensory canals, septomaxilla present (
Osteology. Skull roof (Figs
Premaxillae. The anterior-most rim of the snout is formed by the premaxillae. The premaxillae suture with the maxillae laterally, with the nasals posteriorly, and form the anteromedial part of the nasal rim. In ventral view, they contact the vomers posteriorly, the maxillae laterally, and form the anterior rim of the anterior palatal vacuity. The ornamentation is made up of pits and grooves (Figs
Maxillae. The anterior one-third of the lateral skull margin is formed by the maxillae, commencing from the posterolateral rim of the nares. Septomaxillae were figured by
Nasal. The nasals are quite broad, and form a major part of the anterior skull roof medially (Figs
Lacrimal. The lacrimals are tear-drop shaped, suturing with the maxillae anterolaterally, the nasal medially, the prefrontal posteriorly, and the jugal posterolaterally (Figs
Jugal. The jugals form the majority of the cheek regions. Anteriorly, they contact the maxilla and anteromedially the lacrimal. Medially, the jugals are sutured anteriorly and in their middle part with the prefrontal and posteriorly with the postorbital. The jugal forms a narrow process and enters the orbit, thereby separating the prefrontal and the postorbital. Posteriorly, the jugals suture with the squamosal medially and the quadratojugal laterally. Pit and groove ornamentation occur in the posterior part and ridges and furrows are present in the anterior part (Figs
Prefrontal. The elongate prefrontals suture with the nasals and lacrimals anteromedially and anterolaterally, respectively (Figs
Frontal. The frontals are conspicuous, elongate bones that are anteriorly subtriangular in shape (Figs
Postfrontal. The postfrontals are pentagonal in outline and form the posteromedial margin of the orbits. Anteriorly, they suture with the frontals, posteromedially with the parietals, posteriorly with the supratemporals, and laterally with the postorbitals (Figs
Postorbital. The postorbitals are wing-like projections, contributing to the posterolateral rim of the orbits (Figs
Quadratojugals. The quadratojugals form the cheeks and the lateral-most part of the skull (Figs
Parietals. The parietals contact each other medially and resemble a trapezium in outline. They enclose the parietal (pineal) foramen along the medial suture towards the posterior half of the bone. The parietals suture with the frontals anteriorly, the postfrontals and the supratemporals laterally, and the postparietals posteriorly (Figs
Supratemporals. The supratemporals are polygonal in outline and contact the postorbitals and postfrontals anteriorly, the parietals anteromedially, and the postparietals posteromedially. The supratemporals suture with the squamosals laterally and posteriorly with the tabulars. The supratemporal does not contribute to the rim of the otic notch (Figs
Squamosals. The squamosals are located between the quadratojugals and the tabulars. They form the postero-lateral rim of the skull and almost half the anterior and lateral margin of the otic notch. The squamosals are bordered by the postorbitals and the jugals anteriorly, the supratemporals medially, and the quadratojugals laterally (Figs
Postparietals. The polygonal postparietals form the posterior concavity of the dorsal rim of the skull. The postparietals suture with the parietal anteriorly, the supratemporals anterolaterally and the tabulars laterally. They are much shorter than the parietals (Figs
Tabulars. The tabulars are elongated, polygonal in shape and have posterolaterally directed horns (Figs
Lateral Line Sulci. The lateral line sulci are present as pairs of supraorbital, infraorbital, and postorbital sulci. They are more evident laterally, especially in the posterior part of the skull, and weakly impressed medially, and again pronounced across the snout. However, all the lateral line sulci are discernible. The supraorbital sulci arise from the anterior region of the snout and traverse medially to the nares. They meander anteroposteriorly from the nasals to the prefrontals, running along the prefrontal-lacrimal suture reaching the posterior half of the frontals before terminating on the postfrontals near the orbital midline (Figs
Palate (Figs
Vomers. The vomers are elongated bones tapering posteriorly (Figs
Palatines. The palatines are crescent in shape and bear the second pair of palatal tusks. The palatines form the posterior rim of the choanae and contact the maxillae anteriorly. The palatine-maxilla sutures run posterolaterally from the choanae to the ectopterygoid and form the anterolateral rim of the interpterygoid vacuity. The palatine has a discontinuous row of teeth more or less becoming larger anteriorly (Figs
Pterygoids. The pterygoids have a bow-like structure extending between the interpterygoid vacuities and the subtemporal vacuities and form parts of their respective rims (Figs
Parasphenoid. The parasphenoid is an unpaired bone present in the middle of the palate (Figs
Ectopterygoids. The ectopterygoids are longitudinal bones. Posteromedially, the ectopterygoid sutures with the pterygoid, posteriorly with the insula jugalis, and anteriorly with the palatines (Figs
Insulae Jugalis. The insulae jugalis are triangular bones forming a point contact with the pterygoids posteriorly. Anteromedially, the insula jugalis is bound by the ectopterygoid and posteriorly forms a part of the anterior rim of the subtemporal vacuity (Figs
Quadrates. The quadrates are polygonal-shaped bone and contact the pterygoids medially and the quadratojugals laterally (Figs
Skull openings. Skull openings from the holotype ISI A 54 are listed below:
The nares are the tear-drop-shaped dorsal openings with a maximum length of 4.33 cm and maximum width 2.52 cm for the left and maximum length 4.76 cm and maximum width of 2.63 cm for the right opening. A small bone, the septomaxilla, is present at the inside of the anterolateral margin of the nares. The orbits are positioned at the posterior half of the skull with a maximum length of 5.70 cm and 5.85 cm and a maximum width of 3.76 cm and 3.30 cm respectively for left and right and they are elliptical in outline. The orbits are slightly elevated with respect to the plane of the skull roof. The pineal foramen is subcircular; its long axis is 1.68 cm and short axis is 1.03 cm, and is completely enclosed by the parietals. The otic notch is wide open posteriorly and is bounded by the squamosal and the tabular. The anterior rim of the otic notch is angular, the angles between the squamosals and the tabulars are 41 and 62 degrees in the left and right otic notch respectively. The anterior palatal vacuities are subdivided and laterally stretched with a maximum length of 2.5 cm and width of 7 cm. The left one measures 2.08 × 3.22 cm and the right one measures 1.46 × 3.49 cm. It is enclosed by the premaxillae and the vomers. The anterior palatal vacuity is bean-shaped with a constriction in between. The choanae are two slit-like cavities in the anterior part of the palate. The left and right choanae are quite deformed (taphonomically) with dimensions of 3.49 × 1.28 cm and 5.07 × 1.21 cm, respectively. The interpterygoid vacuities are the largest openings of the palate, with a ‘D’-shaped outline, they measure 28.93 × 8.08 cm and 28.91 × 9.60 cm on left and right respectively. The lateral rims have a parabolic curvature with the posterior curvature being more acute than the anterior one. The marginal rims are almost straight. The interpterygoid vacuities are enclosed by the vomers, the palatines, the pterygoids, the parasphenoid and a small portion of the ectopterygoids. The cultriform process of the parasphenoid forms most of the medial margin. The subtemporal vacuities are the posterior most vacuities in the palate. The vacuities are arch shaped with a gentle lateral convexity and a more acute medial concavity. The maximum length measured parallel to the midline is 17.30 cm, and the maximum width is 7.90 cm for the left one and 17.47 cm and 9.01 cm respectively for the right one. The subtemporal vacuities are enclosed by the pterygoids, the quadrates, the quadratojugals and the insulae jugalis. The tip of the anterior projection of the subtemporal vacuity does not reach the level of the midpoint of the interpterygoid vacuities.
Occiput (Figs
Exoccipitals. The exoccipitals project posteriorly to establish the atlas-exoccipital articulation and diverge dorsally to encompass the ventral portion of the foramen magnum. They suture with the parasphenoid anteriorly. The posterior projection of the exoccipitals lies anterior to the projection of the quadrates. The posterior contact surfaces of the exoccipitals with the atlas are sub-oval in shape and are flat and narrow.
Mandible (Fig.
Dentary. The dentary forms the dorsal and parts of the labial and lingual surface of the anterior part of the ramus (Fig.
Splenial and postsplenia
l. In labial view, the splenial and postsplenial lie ventral to the dentary with the splenial located anteriorly. The region of the posterior Meckelian foramen is broken. The ventral surface is not fully preserved (Fig.
Angular. The angular forms the remaining bone in the ventrolabial and some part of the ventrolingual surface (Fig.
Surangular. The surangular forms most of the posterodorsal part of the labial surface, including that of the postglenoid area. In labial view, the surangular sutures with the angular ventrally and with the dentary anteriorly. In lingual view, it sutures with the articular posteriorly and with the angular ventrally and anteriorly with the prearticular. In dorsal view, the surangular sutures with the dentary anteriorly; lingually it sutures with the articular and forms the lingual margin of the adductor fossa (Fig.
Coronoid series. The coronoid series consists of anterior, middle and posterior coronoid on the lingual surface of the mandible. They are placed ventral to the dentary and extend from shortly behind the symphysis to the leading edge of the adductor fossa. The anterior coronoid sutures with the splenial ventrally, the middle coronoid sutures with the postplenial and some part of the splenial and the posterior coronoid with the prearticular. No dentition is present in the coronoid series nor is there any process present in the coronoids (Fig.
Prearticular. In lingual view, the prearticular forms the posterior half of the ramus. It sutures with the postsplenial anteriorly and dorsally with the middle and posterior coronoids. The prearticular forms the lingual margin of the adductor fossa and the lingual edge of the glenoid fossa. The prearticular does not form part of the postglenoid area and it does not suture with the splenial because it is separated by the coronoid (Fig.
Articular. The articular is an endoskeletal bone that completely forms the glenoid fossa. Anterodorsally, the articular forms the posterior border of the adductor fossa. The articular is enclosed labially by the surangular and lingually by the prearticular. Ventrally, the articular is overlain by the angular. Posteriorly the articular enters the postglenoid area. The posterior extremity of the articular is not completely ossified.
Other important features of mandible (Fig.
Postcranium (Figs
The Vertebral column. The preserved vertebral elements mainly encompass the intercentra, neural arches, and neural spines (Fig.
The intercentra are wedge-shaped in lateral view and crescentic or heart-shaped in anterior and posterior views. Distinctly, two types of intercentra are present, type 1 in the anterior part and type 2 in the posterior part. The anterior intercentra are massive, quite thick, and robust. The dorsal most part is blunt. The ventrolateral surface of the intercentrum is concave with two raised rims at the anterior and posterior borders. The parapophysis is well developed. Five anterior intercentra are preserved (ISI A 209–213). The posterior intercentra are flattened ventrally and the lateral surfaces are more distinct from the ventral face. They are shallower and less ossified than the anterior ones. The parapohyses were directed more ventrally, thus their lower edges project below the ventral line with a triangular outline. There are four posterior intercentra preserved (ISI A 214–217) (Fig.
Neural arch and neural spine. Neural arch and neural spines (Fig.
Neural spines were detached from the bodies of the neural arches. They are short and stout. Eight single broken neural arches (ISI A 218–225) and two broken lateral halves of a neural arch (ISI A 226a & b) are preserved. Eight neural spines have been detected (ISI A 227–234).
No haemal arches are preserved.
Ribs. A total of 30 rib fragments and one almost complete rib are present (Fig.
The cervical ribs have two separate rib facets. The anterior thoracic rib (ISI A 235; ISI A 238–250) heads were elliptical in cross-section with a narrow extension for attachment of capitulum and tuberculum. The distal end of the anterior thoracic rib is expanded and plate-like. The posterior thoracic ribs (ISI A 251–266) are cylindrical and have elliptical proximal heads and rounded distal ends (Fig.
No caudal ribs are preserved.
Pectoral girdle. Two almost complete and three fragmented interclavicles (ISI A 267 & 268), one complete left and one fragmented left and one fragmented right clavicle (ISI A 272–274) and six fragmented cleithra (ISI A 275–280) are present. The interclavicles are large and robust and their thickness varies from 3 to 5 cm. The clavicles have a long dorsal process originating at the posterolateral corner of the clavicular blade. The dorsal process is slender and twisted. The clavicular blades are slender and spatulate (Fig.
Cleithra are slender processes having low ridges on their surfaces. A scapular crest is present at its head. The shaft’s external surface is convex. The internal facet has a concave attachment area for the clavicle and a convex attachment area for the scapula (
Forelimb. From the forelimb, only the proximal and distal heads of the ulna are preserved in the present collection (ISI A 182/3 & 4; ISI A 281–282, Fig.
Pelvic girdle. The pelvic girdle comprises only the left ilium as no other elements are preserved (Fig.
Hind limbs. From the hindlimbs, the proximal shaft of a right femur and the proximal shaft of left fibula is preserved. The tibia is not present in the collection. The proximal shaft of the right femur (Fig.
The fibula is dorsoventrally flattened, with a trapezoidal outline of the proximal head (Fig.
No digit bones were found.
Supported by the new material, an emended diagnosis and a new reconstruction of the skull of C. denwai is presented here (Fig.
The hitherto undescribed limb bones of C. denwai add to our knowledge on mastodonsaurid limb bones. This is important as stereospondyl specimens are mostly represented by skulls that are heavy and flat with better preservation potential than the long bones. The limbs of the mastodonsaurids are rarely found and are not very diverse (
The detailed osteology and the emended diagnosis of C. denwai is the first step to systematically study the huge array of temnospondyls that are present in the Anisian Denwa Formation of Central India. This detailed osteology presented here will act as a prelude to a further revised phylogenetic analysis of mastodonsaurids considering all the newer taxa and features that have been recorded so far. The emended diagnosis of Cherninia denwai presented herein reflects a future need of a detailed phylogeny of the superfamily Capitosauroidea.
The present work was carried out with the financial support from the Indian Statistical Institute, Kolkata (ISI Kolkata). The authors are grateful to the Geological Studies Unit, Indian Statistical Institute for the laboratory and financial support. We acknowledge Mr. Pushpal Kundu of Photography and Reprography Unit, ISI, Kolkata for all the photography assistance provided and preparator Mr. Lakshman Mahankur for his assistance in preparation of the specimens. We also acknowledge Mr. Swapan Aich, Mr. Ashok Saha and Mr. Sasanka Sekhar Sahu of the Transport unit of ISI, Kolkata for transport and driving assistance during field-work in the Satpura basin. The authors sincerely thank Prof. Rainer Schoch and the two anonymous peer-reviewers whose comments have significantly helped to develop the manuscript further.
List of specimens assigned as Cherninia denwai
Data type: docx
Explanation note: The data is a list of all the specimens occuring in the geology museum of the Indian Statistical Institute, Kolkat, that has now been assigned as Cherninia denwai.