Fossils of Antarctica Codexery

Heptranchias howelli

Extinct sevengill shark known from fossil teeth across multiple continents.

Heptranchias howelli, commonly known as the sevengill shark, is an extinct species of nektonic carnivore belonging to the genus Heptranchias. It existed from approximately 37.2 to 20.43 million years ago, spanning the Eocene and Miocene epochs. Its fossil teeth have been found in Europe, North America, South America, and Antarctica, providing insight into the distribution of ancient sharks.

Quick Facts

Genus
Heptranchias
Species
howelli

Facts from the source article.

Lore & Background

The largest tooth found at Trelde Næs measured 17.5 mm mesio-distally, 8.5 mm apico-basally, and 4.5 mm labio-lingually, with root heights ranging from 3 to 5 mm. Fossils of this species have been discovered in Eocene deposits of the La Meseta Formation in Antarctica, as well as in Canada (British Columbia), the United States (New Jersey, Oregon, Washington), and Miocene deposits of the Uitpa Formation in Colombia.

Reader's Guide

Heptranchias howelli is significant as an extinct representative of the sevengill shark lineage, providing evidence of the genus's wide geographic distribution during the Eocene and Miocene. Its fossil teeth, found across Europe, North America, South America, and Antarctica, indicate that these sharks inhabited diverse marine environments. The detailed descriptions of tooth morphology—such as the sigmoid cusp, serrations, and cusplet patterns—help paleontologists distinguish this species from related forms and track evolutionary changes within Heptranchias. The discovery of teeth in Denmark and Colombia, along with specimens from the United States and Canada, underscores the species' broad range. The largest tooth from Trelde Næs, measuring 17.5 mm, offers a glimpse into the size of these ancient sharks. Although the fossil record is limited to teeth, these remains are crucial for understanding the paleoecology and biogeography of extinct sharks. The species' existence from 37.2 to 20.43 Ma places it within a period of significant climatic and oceanic change, making it a valuable subject for studies of ancient marine life.

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