The palaeobiogeography of South American gomphotheres

Gomphotheriid proboscideans reached South America as Late Cenozoic immigrants from North America. However, disagreements over alpha taxonomy, age dating and phylogenetic relationships have produced three competing hypotheses about this immigration: (1) a single gomphothere immigration took place soo...

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Main Author: Spencer G. Lucas
Format: Article
Language:English
Published: Springer 2013-01-01
Series:Journal of Palaeogeography
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2095383615301292
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spelling doaj-art-8b874ce00680483989927ee94c5d76072018-09-02T09:17:10ZengSpringerJournal of Palaeogeography2095-38362013-01-0121194010.3724/SP.J.1261.2013.00015The palaeobiogeography of South American gomphotheresSpencer G. LucasGomphotheriid proboscideans reached South America as Late Cenozoic immigrants from North America. However, disagreements over alpha taxonomy, age dating and phylogenetic relationships have produced three competing hypotheses about this immigration: (1) a single gomphothere immigration took place soon after the ~3 Ma closure of the Panamanian isthmus; (2) two separate gomphothere immigrations took place after closure of the isthmus; or (3) an earlier, Late Miocene (before 9 Ma) immigration brought gomphotheres into South America. A critical re-evaluation of the alpha taxonomy, age dating and phylogenetic relationships of Neotropical gomphotheres identifies two valid genera of South American gomphotheres, Cuvieronius and Notiomastodon (= “Haplomastodon”, = “Stegomastodon” from South America) and recognizes “Amahuacatherium” as an invalid genus likely based on a specimen of Notiomastodon. The oldest well-dated South American gomphothere fossil is Marplatan, ~2.5 Ma, from Argentina. The case for an age of “Amahuacatherium” older than 9 Ma is refuted by mammalian biostratigraphy and a re-evaluation of the relevant magnetostratigraphy. North American Rhynchotherium descended from Gomphotherium during the Late Hemphillian (~5–6 Ma) and gave rise to Cuvieronius in North America by the end of the Blancan (~2 Ma) time. Notiomastodon evolved from Cuvieronius in South America during the Pleistocene. The case for a close relationship between the Neotropical gomphotheres and Sinomastodon from China is rejected. Central America was not a center of endemic gomphothere evolution and merely acted as a pathway for the immigration of gomphotheres from north to south: Gomphotherium into Central America during the Miocene, Cuvieronius to Central America by Early Pleistocene time and on to South America. After closure of the Panamanian isthmus, Cuvieronius immigrated to South America, where it gave rise to Notiomastodon by Middle Pleistocene time. The South American history of gomphotheres was thus a modest evolutionary diversification from a single Plio-Pleistocene immigration.http://www.sciencedirect.com/science/article/pii/S2095383615301292gomphothereSouth AmericaCuvieroniusNotiomastodonHaplomastodonStegomastodonAmahuacatherium
institution Open Data Bank
collection Open Access Journals
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language English
format Article
author Spencer G. Lucas
spellingShingle Spencer G. Lucas
The palaeobiogeography of South American gomphotheres
Journal of Palaeogeography
gomphothere
South America
Cuvieronius
Notiomastodon
Haplomastodon
Stegomastodon
Amahuacatherium
author_facet Spencer G. Lucas
author_sort Spencer G. Lucas
title The palaeobiogeography of South American gomphotheres
title_short The palaeobiogeography of South American gomphotheres
title_full The palaeobiogeography of South American gomphotheres
title_fullStr The palaeobiogeography of South American gomphotheres
title_full_unstemmed The palaeobiogeography of South American gomphotheres
title_sort palaeobiogeography of south american gomphotheres
publisher Springer
series Journal of Palaeogeography
issn 2095-3836
publishDate 2013-01-01
description Gomphotheriid proboscideans reached South America as Late Cenozoic immigrants from North America. However, disagreements over alpha taxonomy, age dating and phylogenetic relationships have produced three competing hypotheses about this immigration: (1) a single gomphothere immigration took place soon after the ~3 Ma closure of the Panamanian isthmus; (2) two separate gomphothere immigrations took place after closure of the isthmus; or (3) an earlier, Late Miocene (before 9 Ma) immigration brought gomphotheres into South America. A critical re-evaluation of the alpha taxonomy, age dating and phylogenetic relationships of Neotropical gomphotheres identifies two valid genera of South American gomphotheres, Cuvieronius and Notiomastodon (= “Haplomastodon”, = “Stegomastodon” from South America) and recognizes “Amahuacatherium” as an invalid genus likely based on a specimen of Notiomastodon. The oldest well-dated South American gomphothere fossil is Marplatan, ~2.5 Ma, from Argentina. The case for an age of “Amahuacatherium” older than 9 Ma is refuted by mammalian biostratigraphy and a re-evaluation of the relevant magnetostratigraphy. North American Rhynchotherium descended from Gomphotherium during the Late Hemphillian (~5–6 Ma) and gave rise to Cuvieronius in North America by the end of the Blancan (~2 Ma) time. Notiomastodon evolved from Cuvieronius in South America during the Pleistocene. The case for a close relationship between the Neotropical gomphotheres and Sinomastodon from China is rejected. Central America was not a center of endemic gomphothere evolution and merely acted as a pathway for the immigration of gomphotheres from north to south: Gomphotherium into Central America during the Miocene, Cuvieronius to Central America by Early Pleistocene time and on to South America. After closure of the Panamanian isthmus, Cuvieronius immigrated to South America, where it gave rise to Notiomastodon by Middle Pleistocene time. The South American history of gomphotheres was thus a modest evolutionary diversification from a single Plio-Pleistocene immigration.
topic gomphothere
South America
Cuvieronius
Notiomastodon
Haplomastodon
Stegomastodon
Amahuacatherium
url http://www.sciencedirect.com/science/article/pii/S2095383615301292
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