Manidens

Extinct genus of dinosaurs

Manidens Temporal range: Middle Toarcian ~179.17–178.07 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓ ^[1]

Skull reconstruction
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Clade:	Dinosauria
Clade:	†Ornithischia
Family:	†Heterodontosauridae
Subfamily:	†Heterodontosaurinae
Genus:	†Manidens Pol et al. 2011
Type species
†Manidens condorensis Pol et al. 2011

Manidens is an extinct genus of heterodontosaurid dinosaur from the Early Jurassic of Patagonia. It is a sister taxon of the closely related Pegomastax from South Africa.^[2] Fossils have been found in the Cañadón Asfalto Formation in Chubut Province, Argentina, considered to be originally dated to the Bajocian, latter were found to be from Toarcian beds.^[3]

Etymology

The type species of Manidens, Manidens condorensis, was described in the journal Naturwissenschaften in 2011. Manidens was named in by Diego Pol, Oliver Rauhut and Marcos Becerra. The generic name is derived from Latin manus, "hand", and dens, "tooth", a reference to the hand-shaped form of the posterior lower teeth. The specific name refers to the village of Cerro Cóndor, located near to the Queso Rallado site where the specimen was found by zoologist Guillermo Rougier.^[3]

Description

The holotype specimen of Manidens, MPEF-PV 3211, consists of a partial skeleton with a skull and lower jaw, including the axial column except most of the tail; a left shoulder girdle; and the pelvis. The specimens MPEF-PV 1719, 1786, 1718, 3810, 3811, isolated posterior teeth, from the same locality and horizon as the holotype specimen are also referred to this genus.^[4] MPEF-PV 3211 consists of 11 partially articulated fragments from a single individual, with several specimens separated: the right quadrate (MPEF-PV 3211-5), right quadratojugal (MPEF-PV 3211-6), right postorbital (MPEF-PV 3211-7), a complete pelvic girdle and sacral region with six sacral vertebrae (MPEF-PV 3211-1), one cervical vertebra (MPEF-PV 3211-8), two dorsal vertebrae (MPEF-PV 3211-2 and MPEF-PV 3211-4), and a caudal vertebra (MPEF-PV 3211-3). Some bones could not be fully separated due to overlapping and were left in three blocks of associated remains (MPEF-PV 3211-9, MPEF-PV 3211-10, and MPEF-PV 3211-11).^[5]

Other specimens include partial articulated specimens, skull & associated elements as well referred isolated teeth: MPEF-PV 3809, MPEF-PV 3808, MPEF-PV 10867, MPEF-PV 1719, MPEF-PV 1786, MPEF-PV 1718, MPEF-PV 3810, MPEF-PV 3811, MPEF-PV 3812, MPEF-PV 3813, MPEF-PV 3814, MPEF-PV 3815, MPEF-PV 3816, MPEF-PV 10866.^[6]

The cervical vertebrae are shorter than the dorsal vertebrae and feature short, stout diapophyses and parapophyses, with the anterior cervical having strongly elongated, hypertrophied epipophyses, similar to those in Heterodontosaurus.^[3] Both cervical and dorsal neural spines are elongate anteroposteriorly and low. The sacrum contains six vertebrae, with their neural spines forming a continuous bony sheet over the ilium. An anterior caudal vertebra possesses a low, elongated centrum with well-developed chevron facets.^[3]

Only the left coracoid and proximal part of the scapula are preserved, displaying a prominent, hook-like posteroventral process separated from the glenoid cavity by a wide notch.^[3] The pelvic girdle is mostly intact except for the distal ends of the pubes and ischia. The ilium is low and elongated, with the preacetabular process making up about half of the bone's total length. A longitudinal ridge runs along the lateral surface of the preacetabular process, though it is less pronounced than in Heterodontosaurus. Unlike Heterodontosaurus and other basal ornithischians, where the pubic peduncle is longer than the ischial peduncle, in Manidens the pubic peduncle is subequal or slightly shorter than the ischial peduncle. As typical of ornithischians, the pubis is opisthopubic with a very slender posteroventral shaft.^[3] The prepubic process is short, extending only slightly beyond the pubic peduncle of the ilium anteriorly, and is robust. A small obturator foramen is located below the acetabulum. The ischium is more robust than the pubis, with an extensive medial suture along its shafts, which are rectangular in cross-section. There is not enough of the shaft preserved to determine the presence or absence of an obturator process.^[3]

The specimens were found in the Queso Rallado locality of the Cañadón Asfalto Formation, dating originally to the Aalenian–Early Bathonian stages, 171 ± 5 to 167 ± 4 Ma, yet where latter constrained to 179-178 million years, that is Middle-Late Toarcian.^[7]

Manidens was a relatively basal heterodontosaurid that grew to about 60 cm (2.0 ft) in length and 500 g (18 oz) in body mass, smaller than later heterodontosaurids.^[8] It has high-crowned teeth indicative of an increased adaptation to a herbivorous diet but lacks the wear facets seen in more advanced forms like Heterodontosaurus. Manidens is the sister taxon of a clade consisting of the African species Heterodontosaurus, Abrictosaurus and Lycorhinus, indicating an early radiation of the heterodontosaurids.^[3] The discovery of filamentous integumentary structures in the related Tianyulong suggests that they may also have been present in other heterodontosaurids such as Manidens.^[9]

Skull

Several Autapomorphies were identified, including postorbital has a tubercle-like thickening at the base of the jugal process, positioned between the orbit and the lowest part of the postorbital fossa, oriented dorsoventrally, jugal process of the postorbital reaches the main body of the jugal, with the jugal contributing minimally to the posterior orbit boundary. The coronoid has a triangular posterior process extending further back than the coronoid process of the dentary with the anterior foramen of the surangular featuring a wide, anteriorly developed fossa that becomes fusiform posterior to the foramen.^[5] Regarding the mandibluar fenestra & the dentition is completely closed, with a small foramen in the surangular, showing strong heterodonty between the maxillary and dentary cheek teeth, with symmetrical diamond-shaped maxillary teeth and asymmetrical diamond-shaped (hand-shaped) dentary teeth.^[5] The maxillary dentition shows crowns with sharp mesial and distal entolophs in the mid-posterior region, with a distal entoloph in the anterior teeth, cingular entolophs are located near the midsection of the lingual crown face and directed apically, paracingular fossae between the cingular entolophs and the rest of the crown and mesial/distal cingular entolophs are differently ornamented, with mesial entolophs having 2-6 denticles and distal entolophs having small serrations.^[5] Other maxillary features include obliquely oriented distal ectolophs forming a conspicuous crest on the labial face, posterior maxillary crowns having a shelf-like denticulated mesial ectoloph and a sub-cingular crest running apicobasally at the distal end of the mesial entoloph in mid-posterior crowns.^[5] Other diagnostic features are found in the postorbital Fossa, deep only at the junction between the main body and the squamosal process, without forming a pocket-like recess, the posterior exit of the quadrate foramen being wide and posterolaterally oriented and a jugal having a robust, posterodorsally oriented crest ("jugal boss").^[5]

The Revision of the Skull Osteology allowed to reinterpret it´s diagnosis:

The lateral process of the jugal, initially thought unique, varies among Heterodontosaurus specimens. Its orientation, not presence, is now considered autapomorphic for Manidens.
The postorbital process of the jugal, initially described as unique, is now known to be widely distributed among ornithischians and results from taphonomic distortion.
The absence of a mandibular fenestra at the surangular-angular-dentary contact is confirmed as an autapomorphy, though a small external opening in the surangular is present.
Additional cranial features, such as the continuation of the antorbital fossa and the enlarged forebrain facet, have been refined through CT scans and 3D reconstruction, requiring further comparison with other heterodontosaurids for confirmation.

Tooth replacement was asynchronous in Manidens, which exhibited dental replacement in a continuous anterior-to-posterior wave pattern. Furthermore, Manidens represents the first known occurrence of a heterodontosaurid with dental replacement of its caniniform teeth, which may have had distinct timing relative to its cheek dentition.^[10]

Phylogeny

Cladogram after Pol et al., 2011:^[3]

Ornithischia

Echinodon*

Manidens

	Abrictosaurus

	BMNH A100

	Heterodontosaurus

	Lycorhinus

	Eocursor

	Genasauria

*Note: Pol et al. regard Echinodon as a genus of Heterodontosauridae.

Paleoecology

The Chacritas Member hosted and hypersaline and alkaline lake similar to modern Lake Magadi in Kenya, while nearby environments where developed in a similar way to modern Waimangu Volcanic Rift Valley of New Zealand, with nearby volcanic influence of the Chon Aike Province that likely developed in a similar way to modern California volcanic fields

The holotype of Manidens comes from the Chacritas Member of the Cañadón Asfalto Formation. This member is mostly made of two major depositional settings: lacustrine and fluvial deposits, that have intervals of tuffaceous materials, suggesting this environments coevolved with volcanic activity.^[11] Palustrine littoral environments levels are seen at Cerro Cóndor and Estancia Fossati, characterized by the presence of lacustrine limestones interbedded with shales, tuffs and sandstones.^[12] The lacustrine section has been called the "Chacritas Paleolake", and seems to have been a rather saline or even hypersaline hydrologically closed pan lake, shallow in deep, with marginal zones and palustrine subenvironments made of low-energy ramp-like margins.^[13]^[14]

Fossils attributed to Manidens from Argentina indicate that this dinosaur may have been at least partially arboreal. The specimens consists of a series of bones from both hind feet and a few tail vertebrae, and are tentatively attributed to Manidens on the basis of provenance. The long toe bones indicate that the toe bones were capable of grasping; distinct anchor attachments for the muscles and tendons of the hallux indicate that its hallux was smaller than the rest of the toes but could still have grasped. Principal component analysis found that the feet of Manidens were most similar to those of tree-perching birds.^[15]

References

^ Fantasia, A.; Föllmi, K. B.; Adatte, T.; Spangenberg, J. E.; Schoene, B.; Barker, R. T.; Scasso, R. A. (2021). "Late Toarcian continental palaeoenvironmental conditions: An example from the Canadon Asfalto Formation in southern Argentina". Gondwana Research. 89 (1): 47–65. Bibcode:2021GondR..89...47F. doi:10.1016/j.gr.2020.10.001. S2CID 225120452. Retrieved 27 August 2021.
^ Sereno, Paul C. (3 October 2012). "Taxonomy, morphology, masticatory function and phylogeny of heterodontosaurid dinosaurs". ZooKeys (223): 1–225. doi:10.3897/zookeys.223.2840. PMC 3491919. PMID 23166462.
^ ^a ^b ^c ^d ^e ^f ^g ^h ⁱ Pol, D.; Rauhut, O.W.M.; Becerra, M. (2011). "A Middle Jurassic heterodontosaurid dinosaur from Patagonia and the evolution of heterodontosaurids". Naturwissenschaften. 98 (5): 369–379. Bibcode:2011NW.....98..369P. doi:10.1007/s00114-011-0780-5. PMID 21452054. S2CID 22636871.
^ Becerra, Marcos G.; Pol, Diego; Marsicano, Claudia; Rauhut, Oliver (22 May 2013). "The dentition of Manidens condorensis (Ornithischia; Heterodontosauridae) from the Jurassic Cañadón Asfalto Formation of Patagonia: morphology, heterodonty and the use of statistical methods for identifying isolated teeth". Historical Biology. 26 (4): 480–492. doi:10.1080/08912963.2013.794227. hdl:11336/5409. S2CID 84862489.
^ ^a ^b ^c ^d ^e ^f Becerra, Marcos G.; Pol, Diego; Porro, Laura B.; Paulina-Carabajal, Ariana; Rauhut, Oliver W. M. (2022-09-30). "Craniomandibular osteology of Manidens condorensis (Ornithischia: Heterodontosauridae) from the upper Lower Jurassic of Argentina". Journal of Vertebrate Paleontology. 42 (3). doi:10.1080/02724634.2023.2181087. ISSN 0272-4634.
^ Becerra, M. G. (2016). "Dinosaurios ornitisquios de la Formación Cañadón Asfalto (Jurásico temprano a medio), Chubut, Argentina: anatomía y relaciones filogenéticas" (PDF). (Doctoral Dissertation, Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales).: 1–649. Retrieved 15 October 2021.
^ Pol, D.; Gomez, K.; Holwerda, F. M.; Rauhut, O. W.; Carballido, J. L. (2022). "Sauropods from the Early Jurassic of South America and the Radiation of Eusauropoda". South American Sauropodomorph Dinosaurs. 1 (1): 131–163. doi:10.1007/978-3-030-95959-3_4. Retrieved 2 May 2022.
^ Paul, G. S. (2016). The Princeton Field Guide to Dinosaurs (2nd ed.). Princeton, New Jersey: Princeton University Press. p. 267. ISBN 9780691167664.
^ Zheng, Xiao-Ting; You, Hai-Lu; Xu, Xing; Dong, Zhi-Ming (19 March 2009). "An Early Cretaceous heterodontosaurid dinosaur with filamentous integumentary structures". Nature. 458 (7236): 333–336. Bibcode:2009Natur.458..333Z. doi:10.1038/nature07856. PMID 19295609. S2CID 4423110.
^ Becerra, Marcos G.; Pol, Diego; Whitlock, John A.; Porro, Laura B. (29 September 2020). "Tooth replacement in Manidens condorensis: baseline study to address the replacement pattern in dentitions of early ornithischians". Papers in Palaeontology. 7 (2): 1167–1193. doi:10.1002/spp2.1337. hdl:11336/143687. S2CID 224937914.
^ Cabaleri, N. G.; Benavente, C. A. (2013). "Sedimentology and paleoenvironments of the Las Chacritas carbonate paleolake, Cañadón Asfalto Formation (Jurassic), Patagonia, Argentina". Sedimentary Geology. 284 (4): 91–105. Bibcode:2013SedG..284...91C. doi:10.1016/j.sedgeo.2012.11.008. hdl:11336/182449. Retrieved 29 July 2022.
^ Cabaleri, Nora; Volkheimer, Wolfgang; Armella, Claudia; Gallego, Oscar Florencio; Monferran, Mateo Daniel; Cagnoni, Mariana; Silva Nieto, Diego; Páez, Manuhel (2010). "Humedales jurásicos y del J/K en la Cuenca Cañadón Asfalto, río Chubut medio. Argentina". 4º Simposio Argentino del Jurásico. 4 (2): 18.
^ Cabaleri, N. G.; Armella, C.; Silva Nieto, D. G. (2005). "Saline paleolake of the Cañadón Asfalto Formation (Middle-Upper Jurassic), Cerro Cóndor, Chubut province (Patagonia), Argentina". Facies. 51 (1): 350–364. doi:10.1007/s10347-004-0042-5. S2CID 129090656. Retrieved 17 August 2022.
^ Cabaleri, N.; Volkheimer, W.; Armella, C.; Gallego, O.; Silva Nieto, D.; Páez, M.; Koukharsky, M. (2010). "Estratigrafía, análisis de facies y paleoambientes de la Formación Cañadón Asfalto en el depocentro jurásico Cerro Cóndor, provincia del Chubut". Revista de la Asociación Geológica Argentina. 66 (3): 349–367. Retrieved 2022-09-05.
^ Becerra, M.C.; Pol, D.; Rauhut, O.W.M.; Cerda, I.A. (2016). "New heterodontosaurid remains from the Cañadón Asfalto Formation: cursoriality and the functional importance of the pes in small heterodontosaurids". Journal of Paleontology. 90 (3): 555–577. doi:10.1017/jpa.2016.24. S2CID 56436933.