Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)

Abstract Perinatal specimens give valuable information about the first stages of vertebrate ontogeny. Here, the morphology and palaeohistology of an aristonectine perinatal specimen from Seymour Island (Isla Marambio), López de Bertodano Formation are analysed. The palaeohistological analysis shows...

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Published in:Antarctic Science
Main Authors: O’Gorman, José P., Talevi, Marianella, Fernández, Marta S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2016
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102016000365
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102016000365
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spelling crcambridgeupr:10.1017/s0954102016000365 2024-04-28T08:03:26+00:00 Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae) O’Gorman, José P. Talevi, Marianella Fernández, Marta S. 2016 http://dx.doi.org/10.1017/s0954102016000365 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102016000365 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 29, issue 1, page 61-72 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2016 crcambridgeupr https://doi.org/10.1017/s0954102016000365 2024-04-02T06:55:10Z Abstract Perinatal specimens give valuable information about the first stages of vertebrate ontogeny. Here, the morphology and palaeohistology of an aristonectine perinatal specimen from Seymour Island (Isla Marambio), López de Bertodano Formation are analysed. The palaeohistological analysis shows incomplete endochondral ossification (retention of a calcified cartilaginous core in the medullary region), predominance of primary bone tissue without secondary remodelling, lack of primary or secondary osteons and of growth marks in the cortical bone, and open vascular spaces not surrounded by a thin coat of lamellar bone tissue. General lines of morphological changes were inferred from comparing the fossil with an adult aristonectine specimen indicating i) a tendency of relatively high and broad posterior cervicals to decrease during ontogeny, ii) a decrease of relative size of the dorsolateral process and an increase of the glenoid ramus and iii) the existence of two separate stages in propodial growth divided into an initial elongation followed by a distal expansion. The presence of a perinatal specimen in the James Ross Archipelago indicates that the region was used as a breeding area by the aristonectines during the last part of the Cretaceous. Article in Journal/Newspaper Antarctic Science Ross Archipelago Seymour Island Cambridge University Press Antarctic Science 29 1 61 72
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
O’Gorman, José P.
Talevi, Marianella
Fernández, Marta S.
Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Abstract Perinatal specimens give valuable information about the first stages of vertebrate ontogeny. Here, the morphology and palaeohistology of an aristonectine perinatal specimen from Seymour Island (Isla Marambio), López de Bertodano Formation are analysed. The palaeohistological analysis shows incomplete endochondral ossification (retention of a calcified cartilaginous core in the medullary region), predominance of primary bone tissue without secondary remodelling, lack of primary or secondary osteons and of growth marks in the cortical bone, and open vascular spaces not surrounded by a thin coat of lamellar bone tissue. General lines of morphological changes were inferred from comparing the fossil with an adult aristonectine specimen indicating i) a tendency of relatively high and broad posterior cervicals to decrease during ontogeny, ii) a decrease of relative size of the dorsolateral process and an increase of the glenoid ramus and iii) the existence of two separate stages in propodial growth divided into an initial elongation followed by a distal expansion. The presence of a perinatal specimen in the James Ross Archipelago indicates that the region was used as a breeding area by the aristonectines during the last part of the Cretaceous.
format Article in Journal/Newspaper
author O’Gorman, José P.
Talevi, Marianella
Fernández, Marta S.
author_facet O’Gorman, José P.
Talevi, Marianella
Fernández, Marta S.
author_sort O’Gorman, José P.
title Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)
title_short Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)
title_full Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)
title_fullStr Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)
title_full_unstemmed Osteology of a perinatal aristonectine (Plesiosauria; Elasmosauridae)
title_sort osteology of a perinatal aristonectine (plesiosauria; elasmosauridae)
publisher Cambridge University Press (CUP)
publishDate 2016
url http://dx.doi.org/10.1017/s0954102016000365
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102016000365
genre Antarctic Science
Ross Archipelago
Seymour Island
genre_facet Antarctic Science
Ross Archipelago
Seymour Island
op_source Antarctic Science
volume 29, issue 1, page 61-72
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102016000365
container_title Antarctic Science
container_volume 29
container_issue 1
container_start_page 61
op_container_end_page 72
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