A new small-sized penguin from the late Eocene of Seymour Island with additional material of Mesetaornis polaris

• Published in: GFF
• Main Authors: Jadwiszczak, Piotr, Reguero, Marcelo, Mörs, Thomas
• Format: Article in Journal/Newspaper
• Language: English
• Published: Naturhistoriska riksmuseet, Enheten för paleobiologi 2021
• Subjects: Paleontology; Geology; Paleogene; Antarctic Peninsula; Submeseta Formation; early Sphenisciformes; Marambiornopsis; Mesetaornis; Other Earth and Related Environmental Sciences; Annan geovetenskap och miljövetenskap; Antarctic; The Antarctic; Seymour; Seymour Island; Antarc*; Antarctica; Swedish Polar Research Secretariat
• Online Access: http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-4289; https://doi.org/10.1080/11035897.2021.1900385

Here, we report on two tarsometatarsi assignable to relatively small-sized Eocene Antarctic penguins, housed in the palaeozoological collections of Naturhistoriska riksmuseet, Stockholm. The Priabonian fossils were collected by museum staff during two joined Argentinean and Swedish expeditions from the Submeseta Formation on Seymour Island, Antarctic Peninsula. One specimen represents a new early sphenisciform, Marambiornopsis sobrali gen. et sp. nov., the sixth small-sized tarsometatarsus-based penguin species known from the Antarctic Eocene. Micro-CT scanning revealed the presence of quite large and essentially empty metatarsal medullary cavities. The second fossil can unequivocally be assigned to Mesetaornis polaris. The specimen represents only the second record of this species and supposedly a relatively young bird. Micro-CT scanning showed that in M. polaris the metatarsal medullary cavities are less developed than in M. sobrali – the cortical and trabecular bone tissues left rather little room for significant hollow spaces. Both specimens also differ in overall density of their trabecular networks. We thank the Argentinean Antarctic Institute (IAA-DNA), the Argentinean Air Force and the Swedish Polar Research Secretariat (SPFS) for logistical support in Antarctica and Jonas Hagström (NRM) for assistance in the field. We thank Vivi Vajda (NRM) for making the CT scanning possible, Ashley Kruger (NRM) for the CT-scanning. Financial support through SYNTHESYS funding made available by the European Community – Research Infrastructure Action under the FP6 Structuring the European Research Area Programme, project SE-TAF-4399 to PJ; from the Consejo Nacional de lnvestigaciones Cientificas y Tecnicas (CONICET grant PIP 0462) and from the Argentinean National Agency for Promotion of Science and Technology (ANPCyT grant PICTO 0093/2010) to MR; from the Swedish Research Council (VR Grant 2009-4447) and from the Carl Tryggers Foundation (CTS grant 20:300) to TM is gratefully acknowledged.