Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection

The biogeographic hypothesis more accepted today is that Antarctica (West Antarctica) and southern South America (Magellan region, Patagonia) were connected by a long and narrow causeway (Weddellian Isthmus) between the Antarctic Peninsula and South America since the Late Cretaceous (Campanian) unti...

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Autores principales: Reguero, M.A., Gelfo, J.N., López, G.M., Bond, M., Abello, A., Santillana, S.N., Marenssi, S.A.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_09218181_v123_n_p400_Reguero
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spelling todo:paper_09218181_v123_n_p400_Reguero2023-10-03T15:45:42Z Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection Reguero, M.A. Gelfo, J.N. López, G.M. Bond, M. Abello, A. Santillana, S.N. Marenssi, S.A. Early Paleogene Land connection South America South American and Antarctic native ungulate West Antarctica Antarctic Peninsula Gondwana breakups Paleogene Seafloor spreading South America South American and Antarctic native ungulate Southern south america West antarctica Bridges Astrapotheria Litopterna Ungulata Vertebrata Weddellia The biogeographic hypothesis more accepted today is that Antarctica (West Antarctica) and southern South America (Magellan region, Patagonia) were connected by a long and narrow causeway (Weddellian Isthmus) between the Antarctic Peninsula and South America since the Late Cretaceous (Campanian) until the Early Paleogene allowing terrestrial vertebrates to colonize new frontiers using this land bridge. Stratigraphically calibrated phylogenies including large, terrestrial native ungulates Litopterna and Astrapotheria taxa reveal long ghost lineages that extended into the Late Paleocene and provide evidence for the minimum times at which these "native ungulates" were present both on Antarctica and South America. Based on these results we estimate that the Weddellian Isthmus was functional as a land bridge until the Late Paleocene. Our data place the disconnection between Antarctica and South America in the Late Paleocene, indicating that the terrestrial faunistic isolation (Simpson's "splendid isolation") in South America begun at the end of the Paleocene (~ 56 to 57 m.y.). This faunistic isolation is documented to have occurred at least 25. Ma before the existence of deep-water circulation conditions in Drake Passage (~ 30 m.y.) based on the onset of seafloor spreading in the west Scotia Sea region. We hypothesize that in the early stages of extension (Late Paleocene, ~ 55 m.y.) a wide and relatively shallow epicontinental sea developed between the Antarctic Peninsula and South America drowning the Weddellian Isthmus and preventing the faunal interchange for obligate cursorial terrestrial forms. © 2014 Elsevier B.V. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_09218181_v123_n_p400_Reguero
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Early Paleogene
Land connection
South America
South American and Antarctic native ungulate
West Antarctica
Antarctic Peninsula
Gondwana breakups
Paleogene
Seafloor spreading
South America
South American and Antarctic native ungulate
Southern south america
West antarctica
Bridges
Astrapotheria
Litopterna
Ungulata
Vertebrata
Weddellia
spellingShingle Early Paleogene
Land connection
South America
South American and Antarctic native ungulate
West Antarctica
Antarctic Peninsula
Gondwana breakups
Paleogene
Seafloor spreading
South America
South American and Antarctic native ungulate
Southern south america
West antarctica
Bridges
Astrapotheria
Litopterna
Ungulata
Vertebrata
Weddellia
Reguero, M.A.
Gelfo, J.N.
López, G.M.
Bond, M.
Abello, A.
Santillana, S.N.
Marenssi, S.A.
Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection
topic_facet Early Paleogene
Land connection
South America
South American and Antarctic native ungulate
West Antarctica
Antarctic Peninsula
Gondwana breakups
Paleogene
Seafloor spreading
South America
South American and Antarctic native ungulate
Southern south america
West antarctica
Bridges
Astrapotheria
Litopterna
Ungulata
Vertebrata
Weddellia
description The biogeographic hypothesis more accepted today is that Antarctica (West Antarctica) and southern South America (Magellan region, Patagonia) were connected by a long and narrow causeway (Weddellian Isthmus) between the Antarctic Peninsula and South America since the Late Cretaceous (Campanian) until the Early Paleogene allowing terrestrial vertebrates to colonize new frontiers using this land bridge. Stratigraphically calibrated phylogenies including large, terrestrial native ungulates Litopterna and Astrapotheria taxa reveal long ghost lineages that extended into the Late Paleocene and provide evidence for the minimum times at which these "native ungulates" were present both on Antarctica and South America. Based on these results we estimate that the Weddellian Isthmus was functional as a land bridge until the Late Paleocene. Our data place the disconnection between Antarctica and South America in the Late Paleocene, indicating that the terrestrial faunistic isolation (Simpson's "splendid isolation") in South America begun at the end of the Paleocene (~ 56 to 57 m.y.). This faunistic isolation is documented to have occurred at least 25. Ma before the existence of deep-water circulation conditions in Drake Passage (~ 30 m.y.) based on the onset of seafloor spreading in the west Scotia Sea region. We hypothesize that in the early stages of extension (Late Paleocene, ~ 55 m.y.) a wide and relatively shallow epicontinental sea developed between the Antarctic Peninsula and South America drowning the Weddellian Isthmus and preventing the faunal interchange for obligate cursorial terrestrial forms. © 2014 Elsevier B.V.
format JOUR
author Reguero, M.A.
Gelfo, J.N.
López, G.M.
Bond, M.
Abello, A.
Santillana, S.N.
Marenssi, S.A.
author_facet Reguero, M.A.
Gelfo, J.N.
López, G.M.
Bond, M.
Abello, A.
Santillana, S.N.
Marenssi, S.A.
author_sort Reguero, M.A.
title Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection
title_short Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection
title_full Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection
title_fullStr Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection
title_full_unstemmed Final Gondwana breakup: The Paleogene South American native ungulates and the demise of the South America-Antarctica land connection
title_sort final gondwana breakup: the paleogene south american native ungulates and the demise of the south america-antarctica land connection
url http://hdl.handle.net/20.500.12110/paper_09218181_v123_n_p400_Reguero
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