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Grouping behavior in a Triassic marine apex predator

Abstract:
Marine tetrapods occupy important roles in modern marine ecosystems and often gather in large aggregations driven by patchy prey distribution, 1 ,2 social or reproductive behaviors, 3 ,4 or oceanographic factors. 5 Here, we show that similar grouping behaviors evolved in an early marine tetrapod lineage, documented by dozens of specimens of the giant ichthyosaur Shonisaurus in the Luning Formation in West Union Canyon, Nevada, USA. 6 ,7 A concentration of at least seven skeletons closely preserved on a single bedding plane received the bulk of previous attention. However, many more specimens are preserved across ∼106 square meters and ∼200 stratigraphic meters of outcrop representing an estimated >105–6 years. Unlike other marine-tetrapod-rich deposits, this assemblage is essentially monotaxic; other vertebrate fossils are exceptionally scarce. Large individuals are disproportionately abundant, with the exception of multiple neonatal or embryonic specimens, indicating an unusual demographic composition apparently lacking intermediate-sized juveniles or subadults. Combined with geological evidence, our data suggest that dense aggregations of Shonisaurus inhabited this moderately deep, low-diversity, tropical marine environment for millennia during the latest Carnian Stage of the Late Triassic Period (237–227 Ma). Thus, philopatric grouping behavior in marine tetrapods, potentially linked to reproductive activity, has an antiquity of at least 230 million years.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.cub.2022.11.005

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
et al.


Publisher:
Cell Press
Journal:
Current Biology More from this journal
Volume:
32
Issue:
24
Pages:
5398-5405.E3
Publication date:
2022-12-19
Acceptance date:
2022-11-02
DOI:
EISSN:
1879-0445
ISSN:
0960-9822


Language:
English
Keywords:
Pubs id:
1298979
Local pid:
pubs:1298979
Deposit date:
2022-11-04

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