Lenisicaris is a Cambrian anomalocaridid radiodont, known from the Maotianshan Shales of China and the Kinzers Formation of Pennsylvania.[1]
| Lenisicaris Temporal range: Cambrian Stage 3 to Cambrian Stage 4
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| A reconstruction of L. lupata's frontal appendage | |
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| A fossil of L. pennsylvanica | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| Order: | †Radiodonta |
| Family: | †Anomalocarididae |
| Genus: | †Lenisicaris Wu et al, 2021 |
| Type species | |
| †Lenisicaris lupata Wu et al., 2021
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| Other species | |
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| Synonyms | |
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Discovery and naming
editIn 1929, American paleontologist Charles E. Resser described a poorly preserved arthropod fossil from the Kinzers Formation. He thought this specimen represents a new species of Anomalocaris, so he named it as Anomalocaris pennsylvanica,[2] which makes it the second radiodont species ever described.[3] Numerous specimens have later been referred to this species, but the majority of them were subsequently assigned to different taxa of radiodonts.[3][4] Only three specimens were now confidently included within this species.[3]
L. pennsylvanica was long thought to be a species of Anomalocaris, until a 2021 study assigned it to the genus Lenisicaris on the basis of frontal appendage morphology similar to that of the type species, L. lupata. The genus Lenisicaris derives from the combination of the word "lenis", meaning "smooth" from the non-spinose endites, and "caris", meaning "shrimp". The specific name of L. lupata derives from the combination of the word "lupus" and "fanga", meaning large sharp wolf tooth, based on the shape of the endites resembling wolf fangs.[1]
Description
editLenisicaris is only known from frontal appendages, though these specimens have several distinguishing traits, most noticeably the lack of auxiliary spines.[5] The type species L. lupata has smaller, triangular endites, closely resembling those of Anomalocaris.[1] The other species L. pennsylvanica (formerly described as a species of Anomalocaris[2]) has larger and more rectangular endites, with those on odd-numbered podomeres being smaller.[1]
References
edit- ^ a b c d Wu, Yu; Ma, Jiaxin; Lin, Weiliang; Sun, Ao; Zhang, Xingliang; Fu, Dongjing (1 May 2021). "New anomalocaridids (Panarthropoda: Radiodonta) from the lower Cambrian Chengjiang Lagerstätte: Biostratigraphic and paleobiogeographic implications". Palaeogeography, Palaeoclimatology, Palaeoecology. 569. Bibcode:2021PPP...56910333W. doi:10.1016/j.palaeo.2021.110333. S2CID 233565727.
- ^ a b Resser, Charles E. (1929). "New Lower and Middle Cambrian Crustacea" (PDF). Proceedings of the United States National Museum. 76 (2806): 1–18. doi:10.5479/si.00963801.76-2806.1.
- ^ a b c Pates, Stephen; Daley, Allison C. (2019). "The Kinzers Formation (Pennsylvania, USA): the most diverse assemblage of Cambrian Stage 4 radiodonts". Geological Magazine. 156 (7): 1233–1246. Bibcode:2019GeoM..156.1233P. doi:10.1017/S0016756818000547. S2CID 134299859.
- ^ Pates S, Daley AC, Edgecombe GD, Cong P, Lieberman BS (2019). "Systematics, preservation and biogeography of radiodonts from the southern Great Basin, USA, during the upper Dyeran (Cambrian Series 2, Stage 4)". Papers in Palaeontology. 7: 235–262. doi:10.1002/spp2.1277. ISSN 2056-2799. S2CID 204260554.
- ^ Potin, Gaëtan J.-M.; Daley, Allison C. (2023). "The significance of Anomalocaris and other Radiodonta for understanding paleoecology and evolution during the Cambrian explosion". Frontiers in Earth Science. 11. Bibcode:2023FrEaS..1160285P. doi:10.3389/feart.2023.1160285. ISSN 2296-6463.