Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography

The last twenty million years (Maastrichtian–Santonian) of Southern Hemisphere plesiosaur history is especially well recorded in the Weddellian Province (Patagonia; Western Antarctica and New Zealand). The oldest Late Cretaceous plesiosaurs, two specimens referred to Polycotylidae indet., come from...

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Main Authors: O'Gorman, José Patricio, Otero, Rodrigo, Reguero, Marcelo, Gasparini, Zulma
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 2019
Subjects:
Online Access:http://library.arcticportal.org/2694/
http://library.arcticportal.org/2694/1/A1903004.pdf
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spelling ftarcticportal:oai:generic.eprints.org:2694 2023-12-10T09:38:59+01:00 Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography O'Gorman, José Patricio Otero, Rodrigo Reguero, Marcelo Gasparini, Zulma 2019-09 application/pdf http://library.arcticportal.org/2694/ http://library.arcticportal.org/2694/1/A1903004.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2694/1/A1903004.pdf O'Gorman, José Patricio and Otero, Rodrigo and Reguero, Marcelo and Gasparini, Zulma (2019) Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography. Advances in Polar Science, 30 (3). pp. 210-227. Fauna Terrestrial Article PeerReviewed 2019 ftarcticportal 2023-11-15T23:54:41Z The last twenty million years (Maastrichtian–Santonian) of Southern Hemisphere plesiosaur history is especially well recorded in the Weddellian Province (Patagonia; Western Antarctica and New Zealand). The oldest Late Cretaceous plesiosaurs, two specimens referred to Polycotylidae indet., come from the Santonian levels of the Santa Marta Formation, while the oldest elasmosaurids come from the lower Campanian of the same formation. In the lower Maastrichtian of the Snow Hill Island Formation the non-aristonectine elasmosaurid Vegasaurus molyi is recorded together with other non-diagnosable elasmosaurid specimens, but no aristonectines are present. Aristonectines appears in the Antarctic record in the upper Maastrichtian of the López de Bertodano Formation and are represented by Morturneria and cf. Aristonectes. The specimens from the upper Campanian previously referred to Aristonectinae indet. are referred to Elasmosauridae indet., shortening the temporal record of Aristonectinae in Antarctica. Therefore aristonectines appears in the Antarctic record in the upper Maastrichtian of the López de Bertodano Formation and are represented by Morturneria and cf. Aristonectes. The Antarctic Cretaceous elasmosaurids show a paleobiogeographic connection with South America and New Zealand (Weddellian Province). This connection is indicated by the shared presence of the Aristonectinae Kaiwhekea katiki (New Zealand) and Aristonectes (Argentina and Chile). Recent phylogenetic analysis recovered the aristonectines within the Weddellonectia clade, which includes the aristonectines and the non-aristonectines Vegasaurus molyi (Isla Vega, Antarctica); Kawanectes lafquenianum (Argentina); Morenosaurus stocki and Aphrosaurus furlongi (California). Among the Weddellonectia, the aristonectines show a relatively large body size and extremely derived features and probably occupied a trophic niche that differed from the trophic niche of other elasmosaurids. By way of contrast Kawanectes lafquenianum is an extremely small body-sized ... Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctic Antarctica Polar Science Polar Science Snow Hill Island Arctic Portal Library Antarctic The Antarctic Patagonia New Zealand Argentina Hill Island ENVELOPE(76.070,76.070,-69.395,-69.395) Snow Hill Island ENVELOPE(-57.183,-57.183,-64.466,-64.466) isla Vega ENVELOPE(-57.500,-57.500,-63.833,-63.833) Snow Hill ENVELOPE(-57.183,-57.183,-64.466,-64.466)
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
topic Fauna
Terrestrial
spellingShingle Fauna
Terrestrial
O'Gorman, José Patricio
Otero, Rodrigo
Reguero, Marcelo
Gasparini, Zulma
Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
topic_facet Fauna
Terrestrial
description The last twenty million years (Maastrichtian–Santonian) of Southern Hemisphere plesiosaur history is especially well recorded in the Weddellian Province (Patagonia; Western Antarctica and New Zealand). The oldest Late Cretaceous plesiosaurs, two specimens referred to Polycotylidae indet., come from the Santonian levels of the Santa Marta Formation, while the oldest elasmosaurids come from the lower Campanian of the same formation. In the lower Maastrichtian of the Snow Hill Island Formation the non-aristonectine elasmosaurid Vegasaurus molyi is recorded together with other non-diagnosable elasmosaurid specimens, but no aristonectines are present. Aristonectines appears in the Antarctic record in the upper Maastrichtian of the López de Bertodano Formation and are represented by Morturneria and cf. Aristonectes. The specimens from the upper Campanian previously referred to Aristonectinae indet. are referred to Elasmosauridae indet., shortening the temporal record of Aristonectinae in Antarctica. Therefore aristonectines appears in the Antarctic record in the upper Maastrichtian of the López de Bertodano Formation and are represented by Morturneria and cf. Aristonectes. The Antarctic Cretaceous elasmosaurids show a paleobiogeographic connection with South America and New Zealand (Weddellian Province). This connection is indicated by the shared presence of the Aristonectinae Kaiwhekea katiki (New Zealand) and Aristonectes (Argentina and Chile). Recent phylogenetic analysis recovered the aristonectines within the Weddellonectia clade, which includes the aristonectines and the non-aristonectines Vegasaurus molyi (Isla Vega, Antarctica); Kawanectes lafquenianum (Argentina); Morenosaurus stocki and Aphrosaurus furlongi (California). Among the Weddellonectia, the aristonectines show a relatively large body size and extremely derived features and probably occupied a trophic niche that differed from the trophic niche of other elasmosaurids. By way of contrast Kawanectes lafquenianum is an extremely small body-sized ...
format Article in Journal/Newspaper
author O'Gorman, José Patricio
Otero, Rodrigo
Reguero, Marcelo
Gasparini, Zulma
author_facet O'Gorman, José Patricio
Otero, Rodrigo
Reguero, Marcelo
Gasparini, Zulma
author_sort O'Gorman, José Patricio
title Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
title_short Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
title_full Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
title_fullStr Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
title_full_unstemmed Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
title_sort cretaceous antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography
publisher Polar Research Institute of China - PRIC
publishDate 2019
url http://library.arcticportal.org/2694/
http://library.arcticportal.org/2694/1/A1903004.pdf
long_lat ENVELOPE(76.070,76.070,-69.395,-69.395)
ENVELOPE(-57.183,-57.183,-64.466,-64.466)
ENVELOPE(-57.500,-57.500,-63.833,-63.833)
ENVELOPE(-57.183,-57.183,-64.466,-64.466)
geographic Antarctic
The Antarctic
Patagonia
New Zealand
Argentina
Hill Island
Snow Hill Island
isla Vega
Snow Hill
geographic_facet Antarctic
The Antarctic
Patagonia
New Zealand
Argentina
Hill Island
Snow Hill Island
isla Vega
Snow Hill
genre Advances in Polar Science
Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
Snow Hill Island
genre_facet Advances in Polar Science
Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
Snow Hill Island
op_relation http://library.arcticportal.org/2694/1/A1903004.pdf
O'Gorman, José Patricio and Otero, Rodrigo and Reguero, Marcelo and Gasparini, Zulma (2019) Cretaceous Antarctic plesiosaurs: stratigraphy, systematics and paleobiogeography. Advances in Polar Science, 30 (3). pp. 210-227.
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