ArticleJournal of systematic palaeontology2017
Revision of Eocene Antarctic carpet sharks (Elasmobranchii, Orectolobiformes) from Seymour Island, Antarctic Peninsula.
Article in Journal of systematic palaeontology, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed, 13 citations in OpenAlex.
- Eocene Shark Teeth From Peninsular Antarctica: Windows to Habitat Use and Paleoceanography.Paleoceanography and paleoclimatology · 2024Article
- Probing the Ecology and Climate of the Eocene Southern Ocean With Sand Tiger SharksPaleoceanography and paleoclimatology · 2020Article
- First fossil frog from Antarctica: implications for Eocene high latitude climate conditions and Gondwanan cosmopolitanism of Australobatrachia.Scientific reports · 2020Article
- Skates and rays (Elasmobranchii, Batomorphii) from the Eocene La Meseta and Submeseta formations, Seymour Island, Antarctica.Historical biology · 2019Article
- Eocene squalomorph sharks (Chondrichthyes, Elasmobranchii) from Antarctica.Journal of South American earth sciences · 2017Article
- New Carcharhiniform Sharks (Chondrichthyes, Elasmobranchii) from the Early to Middle Eocene of Seymour Island, Antarctic Peninsula.Journal of vertebrate paleontology · 2017Article
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Authors and funding
4 authors at 2 institutions in 2 countries.
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Abstract
Seymour Island, Antarctic Peninsula, was once called the 'Rosetta Stone' of Southern Hemisphere palaeobiology, because this small island provides the most complete and richly fossiliferous Palaeogene sequence in Antarctica. Among fossil marine vertebrate remains, chondrichthyans seemingly were dominant elements in the Eocene Antarctic fish fauna. The fossiliferous sediments on Seymour Island are from the La Meseta Formation, which was originally divided into seven stratigraphical levels, TELMs 1-7 (acronym for Tertiary Eocene La Meseta) ranging from the upper Ypresian (early Eocene) to the late Priabonian (late Eocene). Bulk sampling of unconsolidated sediments from TELMs 5 and 6, which are Ypresian (early Eocene) and Lutetian (middle Eocene) in age, respectively, yielded very rich and diverse chondrichthyan assemblages including over 40 teeth of carpet sharks representing two new taxa,
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