Chubutinectes

Photographs from the excavation of the Chubutinectes type specimen

The Chubutinectes holotype specimen, MPEF-PV 5232, was discovered in 2009 within sediments of the La Colonia Formation on the Somún Curá plateau in Chubut Province, Argentina. The disarticulated specimen consists of cervical, pectoral, dorsal, sacral, and caudal vertebral centra and neural arches, various ribs, partial pectoral and pelvic girdles, fore- and hind-limb elements, and about 350 gastroliths.[1]

In 2023, O'Gorman et al. described Chubutinectes carmeloi as a new genus and species of elasmosaurid plesiosaur based on these fossil remains. The generic name, "Chubutinectes", combines a reference to the Argentinean province "Chubut", where the holotype was found, with the Greek word "nectes", meaning "swimmer". The specific name, "carmeloi", honors Carmelo Muñoz, the discoverer of the holotype.[1]

The holotype of Chubutinectes is an osteologically immature specimen with a dorsal region measuring 1.4 m (4.6 ft) long, indicating that it was larger than an adult Kawanectes from the same formation. This size difference may result from their environmental difference, as Kawanectes lived in estuaries, while Chubutinectes lived in marine habitats.[1]

O'Gorman et al. (2023) recovered Chubutinectes as a member of the elasmosaurid clade Weddellonectia, as the sister taxon to the clade containing Aphrosaurus and Hydrotherosaurus. The results of their phylogenetic analyses are shown in the cladogram below:[1]

Elasmosauridae

Eromangasaurus Wapuskanectes Speeton Clay plesiosaurian Callawayasaurus Libonectes Jucha Fluvionectes Thalassomedon Tuarangisaurus Cardiocorax Zarafasaura Terminonatator Nakonanectes Albertonectes Elasmosaurus Styxosaurus spp. Futabasaurus Chubutinectes Aphrosaurus Hydrotherosaurus Morenosaurus Vegasaurus Kawanectes MLP-99-XII-1-5 (Aristonectinae indet.)[2] Wunyelfia Morturneria Aristonectes spp. Kaiwhekea

Chubutinectes was discovered in layers of the La Colonia Formation, which dates to the upper Maastrichtian. Based on the presence of nanofossils of Micula spp., the rock layers are younger than around 67.3 million years old. The fellow elasmosaurid Kawanectes was also found in this formation, as well as the remains of indeterminate elasmosaurids.[1] Dinosaur fossils, including those of Carnotaurus and indeterminate abelisaurids, ankylosaurs, hadrosauroids, and somphospondylans, have also been found.[3] Other fossils animals include mammals and turtles.[4]