Laosuchus

Laosuchus is an extinct genus of chroniosuchian that lived around the Permian-Triassic boundary.[1][2] It is known from the skull of a single species, Laosuchus naga.

Laosuchus
Temporal range: Late Permian-Early Triassic, 252.4–249.6 Ma
↓
Life restoration of Laosuchus naga
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Order: †Chroniosuchia
Genus: †Laosuchus
Arbez, Sidor & Steyer, 2018
Species:
†L. naga
Binomial name
†Laosuchus naga
Arbez, Sidor & Steyer, 2018

History and etymology

L. naga was found in the Luang Prabang Basin of Northern Laos, part of the Indochina block. The site was first discovered by J. B. H. Counillon in 1896 as part of the Pavie's third Mission. Counillon was tasked with mapping mineral resources for the French colonial empire. L. naga was discovered during a 2005 expedition to the area, along with remains of dicynodonts.[3][4] It was later described by Arbez, Sidor, and Steyer in 2018.[1] Its name comes from the Nāga, a snake-like deity that appears in multiple east Asian religions.

Description and phylogeny

Laosuchus naga is represented by a single skull and articulated left hemimandible designated as specimen MDS-LPQ 2005-09, stored at the Musée des Dinosaures in Savannakhet. The skull, roughly 26 centimeters in length, is similar in shape to that of crocodiles. Its long snout bore marginal labyrinthodont teeth with an average height of 9 millimeters. Its nares are similar in shape to Madygenerpeton pustulatus. Like M. pustulatus, it also has oval-shaped orbits that are raised above the skull roof, but the orbits are proportionally smaller. Its choanae are relatively long compared to other chroniosuchians.[1]

L. naga has a number of traits that make it unique among chroniosuchia. It lacks palatal tusks, bearing only small denticles on the palate. Its pineal foramen is significantly reduced with a 1mm diameter(M. pustulatus, C. dongusensis, and B. schumanni have diameters of 2mm, 2.5mm, and 3.5mm respectively[5][6][7]). A transverse flange extends from the pterygoid, contacting the maxilla. CT-scanning revealed an autapomorphic internal crest on the dorsal palate that follows the internal margin of the choanae. The parasphenoid bears a thin ventro-medial ridge, a condition also seen in Discosauriscus austriacus[8] Its tabular horn and posterior squamosal contact, closing the otic notch.[1]

There are a number of traits that L. naga share with other chroniosuchians. It bears a subtriangular fontanelle on its premaxilla, a poorly ossified braincase, a well developed pterygoid flange, and a relatively narrow parasphenoid bearing a crest between the basicranial joint.[1]

CT-scanning also revealed the presence of canals within the mandible, snout, and bones in front of the orbit. The canals in the skull roof are interpreted as being related to a lateral line system. Canals in the tip of the snout and mandible are more complex and could be neurovascular canals, which modern animals use for thermoreception, electroreception, or mechanoreception. The paleontologists who described L. naga suggest that the lateral line system was used to detect prey beneath the water surface while the neurovascular system could let it detect movement at the water surface similar to modern crocodiles.[1]

Phylogenetic relationships

The two families within chroniosuchia, Chroniosuchidae and Bystrowianidae, are differentiated primarily based on postcranial elements, such as the shape of their vertebrae and the degree of overlap between their dorsal osteoderms.[9][10] Thus, while L. naga has numerous characteristics supporting its inclusion to chroniosuchia, the lack of postcranial elements in addition to several cranial traits preclude their inclusion to either family. As a result, L. naga is classified as Chroniosuchia incertae sedis[1].

Geological context

The depositional environment that L. naga occurred in consisted of braided rivers transitioning into alluvial plains, with an input of volcanic sediment.[4] In addition to this, the presence of a lateral line system and poorly ossified braincase imply that L. naga spent much of its time in the water. According to the paleontologists who described L. naga, Its placement in nonmarine sediment provides a line of support for the scenario that the North China Block, South China Block, and Indochina block were connected like a peninsula and linked to Laurussia during the Permian and Triassic.[11]

References
  1. Arbez, Thomas; Sidor, Christian A.; Steyer, J.-Sébastien (2019-07-18). "Laosuchus naga gen. et sp. nov., a new chroniosuchian from South-East Asia (Laos) with internal structures revealed by micro-CT scan and discussion of its palaeobiology" (PDF). Journal of Systematic Palaeontology. 17 (14): 1165–1182. doi:10.1080/14772019.2018.1504827. ISSN 1477-2019. S2CID 91670454.
  2. Rossignol, Camille; Bourquin, Sylvie; Poujol, Marc; Hallot, Erwan; Dabard, Marie-Pierre; Nalpas, Thierry (2016-04-15). "The volcaniclastic series from the Luang Prabang Basin, Laos: A witness of a triassic magmatic arc?" (PDF). Journal of Asian Earth Sciences. 120: 159–183. Bibcode:2016JAESc.120..159R. doi:10.1016/j.jseaes.2016.02.001. ISSN 1367-9120.
  3. Steyer, J. Sebastien (2009). "The geological and palaeontological exploration of Laos; following in the footsteps of J. B. H. Counillon and A. Pavie". Geological Society, London, Special Publications. 315 (1): 25–32. Bibcode:2009GSLSP.315...25S. doi:10.1144/SP315.3. ISSN 0305-8719. S2CID 131670024.
  4. Bercovici, Antoine; Bourquin, Sylvie; Broutin, Jean; Steyer, Jean-Sébastien; Battail, Bernard; Véran, Monette; Vacant, Renaud; Khenthavong, Bounxou; Vongphamany, Sotsy (2012-10-22). "Permian continental paleoenvironments in Southeastern Asia: New insights from the Luang Prabang Basin (Laos)". Journal of Asian Earth Sciences. 60: 197–211. Bibcode:2012JAESc..60..197B. doi:10.1016/j.jseaes.2012.08.019. ISSN 1367-9120.
  5. Clack, J., & Klembara, J. (2009). AN ARTICULATED SPECIMEN OF CHRONIOSAURUS DONGUSENSIS AND THE MORPHOLOGY AND RELATIONSHIPS OF THE CHRONIOSUCHIDS. Patterns And Processes In Early Vertebrate Evolution, 81(81), 15-42.
  6. Schoch, Rainer R.; Voigt, Sebastian; Buchwitz, Michael (2010-11-01). "A chroniosuchid from the Triassic of Kyrgyzstan and analysis of chroniosuchian relationships". Zoological Journal of the Linnean Society. 160 (3): 515–530. doi:10.1111/j.1096-3642.2009.00613.x. ISSN 0024-4082.
  7. Witzmann, Florian; Schoch, Rainer R. (2018-07-15). "Skull and postcranium of the bystrowianid Bystrowiella schumanni from the Middle Triassic of Germany, and the position of chroniosuchians within Tetrapoda". Journal of Systematic Palaeontology. 16 (9): 711–739. doi:10.1080/14772019.2017.1336579. ISSN 1477-2019. S2CID 90784937.
  8. Klembara, Jozef (1997-03-29). "The cranial anatomy of Discosauricsus Kuhn, a seymouriamorph tetrapod from the Lower Permian of the Boskovice Furrow (Czech Republic)". Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences. 352 (1351): 257–302. doi:10.1098/rstb.1997.0021. PMC 1691931.
  9. Buchwitz, Michael; Foth, Christian; Kogan, Ilja; Voigt, Sebastian (2012). "On the use of osteoderm features in a phylogenetic approach on the internal relationships of the Chroniosuchia (Tetrapoda: Reptiliomorpha)". Palaeontology. 55 (3): 623–640. doi:10.1111/j.1475-4983.2012.01137.x. ISSN 1475-4983.
  10. Jiang, Shan; Ji, Shu-an; Mo, Jinyou (2017). "First record of Bystrowianid Chroniosuchians (Amphibia: Anthracosauromorpha) from the Middle Permian of China". Acta Geologica Sinica - English Edition. 91 (5): 1523–1529. doi:10.1111/1755-6724.13397. ISSN 1755-6724.
  11. Metcalfe, I. (2006-01-01). "Palaeozoic and Mesozoic tectonic evolution and palaeogeography of East Asian crustal fragments: The Korean Peninsula in context". Gondwana Research. Tectonic Evolution of Korean Peninsula and Adjacent Crustal Fragments in Asia. 9 (1): 24–46. Bibcode:2006GondR...9...24M. doi:10.1016/j.gr.2005.04.002. ISSN 1342-937X.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.