Chilomycterus dzonotensis
| Chilomycterus dzonotensis Temporal range:
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|---|---|
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Actinopterygii |
| Order: | Tetraodontiformes |
| Family: | Diodontidae |
| Genus: | Chilomycterus |
| Species: | †C. dzonotensis
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| Binomial name | |
| †Chilomycterus dzonotensis Cantalice et. al., 2025
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Chilomycterus dzonotensis is an extinct species of burrfish that inhabited the waters around the Yucatan Peninsula during the Neogene period.[1] The species name derives from d'zonot, the Mayan word for "sinkhole" (eventually translated into the Spanish and English cenote).[2]
Distribution
[edit]Fossils of C. dzonotensis are known from the Carrillo Puerto Formation, dating to the boundary between the Late Miocene and Early Pliocene. As suggested by the species name, these fossils were recovered via cave diving within cenotes (the "X-Nabuy" Cenote), at a depth of about 40 to 50 metres (130 to 160 ft) below the surface.[2]
References
[edit]- ^ "PBDB Taxon". paleobiodb.org. Retrieved 2025-02-24.
- ^ a b Cantalice, Kleyton M.; Salgado-Garrido, Hugo E.; Sosa-Rodríguez, Erick; Vilchis-Zapata, Kay; González-Barba, Gerardo; on behalf of the Underwater Archaeological Atlas project (6 February 2025). Schubert, Michael (ed.). "Underwater paleontology inside cenotes reveals the Miocene-Pliocene fish diversity in the Yucatan Peninsula, southeast Mexico". PLOS ONE. 20 (2): e0315382. Bibcode:2025PLoSO..2015382C. doi:10.1371/journal.pone.0315382. ISSN 1932-6203. PMC 11801553. PMID 39913453.
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