The first <i>Otodus megalodon</i> remains from Canada and their predicted range limit

Otodus megalodon (Agassiz, 1835) is an extinct species of giant lamniform shark known from Neogene deposits around the world. Despite having been found decades ago, Canadian specimens of O. megalodon have never been formally described. Here, we identify and describe eight of these specimens, all of which were recovered by scallop dredging activities on Georges Bank, Nova Scotia. Although all these specimens are ex situ, they probably came from Miocene-aged surface deposits on Georges Bank. Similar-aged deposits on the Grand Banks of Newfoundland that have also been dredged for scallops have not yielded any O. megalodon fossils to date. However, several sites with abundant O. megalodon teeth are known from Miocene deposits along the northeast coast of the USA. We therefore cautiously interpret the Canadian specimens as occurring at or near the northern range limit of the species, and discuss the potential limiting factors of this species’ range.

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Publication Details

Journal
Canadian Journal of Earth Sciences
Published
2024-11-29
DOI
https://doi.org/10.1139/cjes-2024-0110
Citations
2
Primary Topic
Evolution and Paleontology Studies
Type
article
Field-Weighted Citation Impact
3.18

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article

The first Otodus megalodon remains from Canada and their predicted range limit

Hans C. E. Larsson, Louis-Philippe Bateman
2 citations
Canadian Journal of Earth Sciences
Evolution and Paleontology Studies
3.18
article

The first Otodus megalodon remains from Canada and their predicted range limit

Hans C. E. Larsson, Louis-Philippe Bateman
article en
2 citations

Abstract

Otodus megalodon (Agassiz, 1835) is an extinct species of giant lamniform shark known from Neogene deposits around the world. Despite having been found decades ago, Canadian specimens of O. megalodon have never been formally described. Here, we identify and describe eight of these specimens, all of which were recovered by scallop dredging activities on Georges Bank, Nova Scotia. Although all these specimens are ex situ, they probably came from Miocene-aged surface deposits on Georges Bank. Similar-aged deposits on the Grand Banks of Newfoundland that have also been dredged for scallops have not yielded any O. megalodon fossils to date. However, several sites with abundant O. megalodon teeth are known from Miocene deposits along the northeast coast of the USA. We therefore cautiously interpret the Canadian specimens as occurring at or near the northern range limit of the species, and discuss the potential limiting factors of this species’ range.

Canadian Journal of Earth SciencesVol. 62(3)
McGill University (CA)
Natural Sciences and Engineering Research Council of Canada
Openalex Percentile: Top 8%
Evolution and Paleontology Studies
3.18
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