| Nuucichthys Temporal range: Cambrian, Drumian PreꞒ Ꞓ O S D C P T J K Pg N ↓ | |
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| Holotype specimen | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Subphylum: | Vertebrata |
| Genus: | †Nuucichthys Lerosey-Aubril & Ortega-Hernández, 2024 |
| Type species | |
| Nuucichthys rhynchocephalus Lerosey-Aubril & Ortega-Hernández, 2024 | |
Nuucichthys (meaning "Núu-ci fish") is an extinct genus of stem-group vertebrates known from the Cambrian (Miaolingian series) Marjum Formation of Utah, United States. The genus contains a single species, N. rhynchocephalus, known from a single individual, representing the first Cambrian vertebrate from the Great Basin region of North America. Nuucichthys provides insights into the diversity of Cambrian vertebrates, which are more rare in Laurentian deposits. Taxonomic studies recover this genus as closely related to other Laurentian stem-vertebrates such as Metaspriggina and Emmonaspis (possible early vertebrate).
History and Research
The Nuucichthys holotype, UMNH.IP.6084, was discovered in sediments belonging to the House Range of Utah and sent to the Natural History Museum of Utah. The specimen consists of a well preserved individual that is flattened laterally. Although the exact origin of this fossil is uncertain, it most likely comes from the Ptychagnostus punctuosus biozone, located in the middle of the Marjum Formation.
The genus name, Nuucichthys, combines "Núu-ci", the name of the Ute tribe meaning "the people", with the Greek word ichthys, meaning "fish". The name refers to the type locality on lands once inhabited by the Ute people. The species name, rhynchocephalus, is derived from the Greek words rhynchos, meaning "beak" or "snout" and kephale, meaning "head", which refers to the projecting region of the front of the head observed in this species.
Description
The holotype specimen of Nuucichthys is around 32.4 millimeters (1.28 inches) long (excluding the eyes and caudal region), and is 7.9 millimeters (0.31 inches) tall. The body of this genus is fusiform in shape, and possess a caudal region lacking any evidence for a fin. The body contained around 40 myomeres that ran along its length, and seem to have shrunk in size after death. The ventral plane of this genus contains a large branchial chamber, and a set of organs which have been interpreted as the liver, and a possible intestine and anus. The caudal region of the body possesses a spiniform structure, which has also been found in animals like Yunnanozoon. By far the most distinguishing feature of this genus is its elongated cephalic region, which helps differentiate it from other Cambrian chordates. This region differentiates from the rest of the body due to the lack of noticeable myomeres, and a sudden change in elevation. This region also possesses a set of paired eyes that are distinct from the various branchial elements. The eyes themselves were well developed camera-type lenses similar to those seen in modern lampreys and Metaspriggina. Like the other known Laurentian stem-vertebrates, this genus seems to lack any sort of fins, and swam in a very different matter to other chordates at the time. This genus also lacks any form of feeding apparatus (or at least ones that would survive fossilization).
Classification
In Lerosey-Aubril & Ortega-Hernández, 2024, Nuucichthys was classified as a stem-group vertebrate within the total group vertebrata. More specifically, it was found to form a polytomy with the other Laurentian stem-vertebrates, Metaspriggina and Emmonsaspis, and was found to be closely related to the myllokunmingiids. The classification also found that the conodonts, a grouping of jawless vertebrates, formed a sister clade to the crown group vertebrates. It also found that the vetulicolians, a phylum of deuterostome animals, to be basal chordates related to tunicates and cephalochordates.
Paleoecology
Due to fins of any kind being absent in this genus, it was hypothesized by the 2024 description that Nuucichthys was not an active swimmer, and that its eyes were facing laterally to the rest of the body. This set of features suggests that it occupied a planktonektonic niche (living in the water column without swimming much). Because no feeding structures are known, and the presumed nektonic lifestyle, it is likely that this animal was likely microphagous, most likely a suspension feeder. This niche has also been suggested for its close relatives as well based on similarities in their body plans.
References
- ^ Lerosey-Aubril, R.; Ortega-Hernández, J. (2024). "A long-headed Cambrian soft-bodied vertebrate from the American Great Basin region". Royal Society Open Science. 11 (7). 240350. Bibcode:2024RSOS...1140350L. doi:10.1098/rsos.240350. PMC 11267725. PMID 39050723.
- Foster, John; Gaines, Robert (October 2016). "Taphonomy and paleoecology of the "middle" Cambrian (Series 3) formations in Utah's West Desert: Recent finds and new data". Utah Geological Association Publication. 45: 291–336.
- Cong, Pei-Yun; Hou, Xian-Guang; Aldridge, Richard J.; Purnell, Mark A.; Li, Yi-Zhen (2015). Smith, Andrew (ed.). "New data on the palaeobiology of the enigmatic yunnanozoans from the Chengjiang Biota, Lower Cambrian, China". Palaeontology. 58 (1): 45–70. doi:10.1111/pala.12117. S2CID 84567733.
- ^ Conway Morris, Simon (March 2008). "A Redescription of a Rare Chordate, Metaspriggina walcotti Simonetta and Insom, from the Burgess Shale (Middle Cambrian), British Columbia, Canada". Journal of Paleontology. 82 (2). Boulder, CO: The Paleontological Society: 424–430. Bibcode:2008JPal...82..424M. doi:10.1666/06-130.1. ISSN 0022-3360. S2CID 85619898.