A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?

During the Jurassic two main marine pathways might act as dispersion routes for vertebrates and invertebrates between Laurasia and Gondwana: the Caribbean Seaway (between North and South America) and the Trans-Erythraean Seaway (splitting Africa from India, Madagascar). The former has proven to be o...

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Publicado: 2018
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_16310683_v17_n3_p158_OGorman
http://hdl.handle.net/20.500.12110/paper_16310683_v17_n3_p158_OGorman
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spelling paper:paper_16310683_v17_n3_p158_OGorman2023-06-08T16:25:35Z A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway? Ameghino Formation Plesiosauria Tithonian Trans-Erythraean Seaway dispersal fauna Gondwana invertebrate Jurassic marine environment Tethys Tithonian type specimen vertebrate Africa Antarctic Peninsula Antarctica Atlantic Ocean Caribbean Sea India Madagascar North America South America West Antarctica Invertebrata Plesiosauria Vertebrata During the Jurassic two main marine pathways might act as dispersion routes for vertebrates and invertebrates between Laurasia and Gondwana: the Caribbean Seaway (between North and South America) and the Trans-Erythraean Seaway (splitting Africa from India, Madagascar). The former has proven to be of relevance as a dispersion route for marine vertebrates and invertebrates between the Tethys and Pacific margin of Gondwana. Nevertheless, little is known about the role of the Trans-Erythraean Seaway as a vertebrate dispersion pathway. The Trans-Erythraean Seaway divides the eastern and western South of Gondwana landmasses in the so-called break-up of Gondwana and connects the Tethys Sea with the Palaeo-Pacific. We describe a newly recovered plesiosaur specimen from the Ameghino (= Nordensköld) Formation, Antarctic Peninsula, the first Jurassic plesiosaur from Antarctica. We discuss the importance of this record regarding the hypothesis of marine vertebrate dispersion through the Trans-Erythraean Seaway. © 2017 Académie des sciences 2018 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_16310683_v17_n3_p158_OGorman http://hdl.handle.net/20.500.12110/paper_16310683_v17_n3_p158_OGorman
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Ameghino Formation
Plesiosauria
Tithonian
Trans-Erythraean Seaway
dispersal
fauna
Gondwana
invertebrate
Jurassic
marine environment
Tethys
Tithonian
type specimen
vertebrate
Africa
Antarctic Peninsula
Antarctica
Atlantic Ocean
Caribbean Sea
India
Madagascar
North America
South America
West Antarctica
Invertebrata
Plesiosauria
Vertebrata
spellingShingle Ameghino Formation
Plesiosauria
Tithonian
Trans-Erythraean Seaway
dispersal
fauna
Gondwana
invertebrate
Jurassic
marine environment
Tethys
Tithonian
type specimen
vertebrate
Africa
Antarctic Peninsula
Antarctica
Atlantic Ocean
Caribbean Sea
India
Madagascar
North America
South America
West Antarctica
Invertebrata
Plesiosauria
Vertebrata
A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?
topic_facet Ameghino Formation
Plesiosauria
Tithonian
Trans-Erythraean Seaway
dispersal
fauna
Gondwana
invertebrate
Jurassic
marine environment
Tethys
Tithonian
type specimen
vertebrate
Africa
Antarctic Peninsula
Antarctica
Atlantic Ocean
Caribbean Sea
India
Madagascar
North America
South America
West Antarctica
Invertebrata
Plesiosauria
Vertebrata
description During the Jurassic two main marine pathways might act as dispersion routes for vertebrates and invertebrates between Laurasia and Gondwana: the Caribbean Seaway (between North and South America) and the Trans-Erythraean Seaway (splitting Africa from India, Madagascar). The former has proven to be of relevance as a dispersion route for marine vertebrates and invertebrates between the Tethys and Pacific margin of Gondwana. Nevertheless, little is known about the role of the Trans-Erythraean Seaway as a vertebrate dispersion pathway. The Trans-Erythraean Seaway divides the eastern and western South of Gondwana landmasses in the so-called break-up of Gondwana and connects the Tethys Sea with the Palaeo-Pacific. We describe a newly recovered plesiosaur specimen from the Ameghino (= Nordensköld) Formation, Antarctic Peninsula, the first Jurassic plesiosaur from Antarctica. We discuss the importance of this record regarding the hypothesis of marine vertebrate dispersion through the Trans-Erythraean Seaway. © 2017 Académie des sciences
title A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?
title_short A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?
title_full A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?
title_fullStr A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?
title_full_unstemmed A Late Jurassic plesiosaur in Antarctica: Evidence of the dispersion of marine fauna through the Trans-Erythraean Seaway?
title_sort late jurassic plesiosaur in antarctica: evidence of the dispersion of marine fauna through the trans-erythraean seaway?
publishDate 2018
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_16310683_v17_n3_p158_OGorman
http://hdl.handle.net/20.500.12110/paper_16310683_v17_n3_p158_OGorman
_version_ 1768543201679900672