Fabanychus

Fabanychus
Temporal range: Late Triassic (mid-Norian), ~215–209 Ma
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Neodiapsida
Clade: Drepanosauromorpha
Genus: Fabanychus
Sodano et al., 2025
Species:
F. monos
Binomial name
Fabanychus monos
Sodano et al., 2025

Fabanychus (lit.'bean claw') is an extinct genus of drepanosauromorph reptiles known from the Late Triassic (Norian age) of the United States. The genus contains a single species, Fabanychus monos, known from several isolated hand claws found in outcrops assigned to the Revueltian teilzone in the Chinle Formation of Arizona and Cooper Canyon Formation of Texas. The shape and curvature of the claws of Fabanychus are similar to those of the contemporary drepanosauromorph Ancistronychus, and indicate it likely had a fossorial ecology, meaning it was well-adapted to digging.

Discovery and naming

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The Fabanychus fossil material was discovered in multiple localities in Arizona and Texas, all of which can be referred to the Revueltian local teilzone, a biochronological unit identified by the tetrapod fossils found there. The holotype specimen—accessioned as PEFO 50566—and five additional specimens identified as paratypes were found in outcrops of the Chinle Formation (Sonsela Member, Bowman locality) in Petrified Forest National Park (PEFO) of Navajo County, Arizona, US. Another specimen from the DMNH 2018-05 (Green Layer) locality of the same member of the Chinle Formation was also identified as belonging to the same species, as was one collected from the Cooper Canyon Formation (middle unit, Headquarters Site) in Garza County, Texas. All eight specimens represent isolated unguals (claws) from the second digit of the hand.[1]

In 2025, Megan P. Sodano and colleagues described Fabanychus monos as a new genus and species of drepanosauromorph reptiles based on these fossil remains. The generic name, Fabanychus, combines the Latin word faba, meaning 'bean' with the Greek word nychus, meaning 'claw', referencing the beanlike shape of the animal's enlarged hand claws. The specific name, monos, is a Greek word meaning 'alone', referencing the discovery of all eight specimens in isolation. Sodano and colleagues histologically sectioned two of the paratype claws to observe the internal structure.[1]

Description and classification

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Speculative life restoration of the related Drepanosaurus, which may have had an arboreal lifestyle

Fabanychus is one of multiple drepanosauromorphs from the southwestern United States known only from hypertrophied second manual unguals (hand claws); others include Ancistronychus,[2] Skybalonyx,[3] and Unguinychus,[4] all of which can be distinguished by distinct morphologies of their claws. Of these genera, Fabanychus is most similar to Ancistronychus, sharing a similar curvature and arrangement of foramina (small holes), tuberosities (bumps), and lack of cortical bone (hard outer layer) on the dorsal (top) and distal (toward the tip) surfaces of the claw. The claws of Skybalonyx and Unguinychus exhibit a flatter morphology with a more shallow curve, while those of Drepanosaurus—known from more complete remains—are much more robust and strongly curved.[1] Avicranium,[5] Dolabrosaurus,[6] and Drepanosaurus are also known from the southwest United States geographic region, albeit from more complete cranial or postcranial remains.[7]

Paleobiology

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The inner (63.6°) and outer (166.5°) curvature of the claws are intermediate between Ancistronychus and Skybalonyx, which are recognized as likely having a fossorial or subterranean (digging or underground) ecology. Drepanosaurus, with its strongly hooked claws, is interpreted as having an arboreal to semi-arboreal (climbing in trees) ecology.[1]

See also

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References

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  1. ^ a b c d Sodano, Megan P.; Kligman, Ben T.; Marsh, Adam D.; Pritchard, Adam C.; Stocker, Michelle R.; Parker, William G.; Gonçalves, Gabriel S.; Nesbitt, Sterling J. (2025-10-23). "Gross anatomy and histological analysis of manual unguals of Drepanosauromorpha (Sauropsida: Diapsida) and description of a new taxon from the Sonsela Member of the Chinle Formation (Late Triassic) of the southwestern United States". The Anatomical Record. doi:10.1002/ar.70057. ISSN 1932-8486.
  2. ^ Gonçalves, Gabriel S.; Sidor, Christian A. (2019-12-15). "A new drepanosauromorph, Ancistronychus paradoxus n. gen. et sp., from the Chinle Formation of Petrified Forest National Park, Arizona, USA". PaleoBios. 36: ucmp_paleobios_46203. doi:10.5070/P9361046203. ISSN 0031-0298. S2CID 210142302.
  3. ^ Jenkins, Xaver A.; Pritchard, Adam C.; Marsh, Adam D.; Kligman, Ben T.; Sidor, Christian A.; Reed, Kaye E. (2020-10-08). "Using manual ungual morphology to predict substrate use in the Drepanosauromorpha and the description of a new species". Journal of Vertebrate Paleontology. 40 (5) e1810058. Bibcode:2020JVPal..40E0058J. doi:10.1080/02724634.2020.1810058.
  4. ^ Pugh, Isaac; Nesbitt, Sterling J.; Heckert, Andrew B.; Lauer, René; Lauer, Bruce (2024-07-04). "A new drepanosauromorph (Diapsida) from East–Central New Mexico and diversity of drepanosaur morphology and ecology at the Upper Triassic Homestead Site at Garita Creek (Triassic: mid-Norian)". Journal of Vertebrate Paleontology. 43 (6). doi:10.1080/02724634.2024.2363202. ISSN 0272-4634.
  5. ^ Pritchard, Adam C.; Nesbitt, Sterling J. (2017-10-01). "A bird-like skull in a Triassic diapsid reptile increases heterogeneity of the morphological and phylogenetic radiation of Diapsida". Royal Society Open Science. 4 (10) 170499. Bibcode:2017RSOS....470499P. doi:10.1098/rsos.170499. ISSN 2054-5703. PMC 5666248. PMID 29134065.
  6. ^ Berman, David S.; Reisz, Robert R. (1992). "Dolabrosaurus aquatilis, a small lepidosauromorph reptile from the Upper Triassic Chinle Formation of North-Central New Mexico". Journal of Paleontology. 66 (6): 1001–1009. Bibcode:1992JPal...66.1001B. doi:10.1017/S0022336000020928. JSTOR 1305953. S2CID 130221236.
  7. ^ Pritchard, Adam C.; Turner, Alan H.; Irmis, Randall B.; Nesbitt, Sterling J.; Smith, Nathan D. (2016-10-24). "Extreme modification of the tetrapod forelimb in a Triassic diapsid reptile". Current Biology. 26 (20): 2779–2786. doi:10.1016/j.cub.2016.07.084.