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The Samebito (鮫人, shark man) is a creature that appears in "The Gratitude of the Samebito", a short story by Lafcadio Hearn. It is described as a shark-like humanoid with inky black skin, emerald green eyes, a face like a demon 's and a beard like a dragon 's.
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The word "leiomano" is derived from the Hawaiian language and may originate from lei o manō, meaning "a shark's lei." [2] The weapon resembles a thick ping-pong paddle inset with shark teeth, typically from the tiger shark. These teeth are placed into grooves in the club and sewn into place.
This is a typical Cladodont tooth, of a shark called Glikmanius. Cladodont (from Latin cladus, meaning branch and Greek Odon, meaning tooth) is the term for a common category of early Devonian shark known primarily for its "multi-cusped" tooth consisting of one long blade surrounded by many short, fork-like tines, designed to catch food that was swallowed whole, instead of being used to saw ...
The snaggletooth shark, or fossil shark (Hemipristis elongata), is a species of weasel shark in the family Hemigaleidae, and the only extant member of the genus Hemipristis. It is found in the Indo-West Pacific, including the Red Sea, from southeast Africa to the Philippines, north to China, and south to Australia, at depths from 1 to 130 meters.
Carcharodon (meaning "jagged/sharp tooth" in Ancient Greek) [2] is a genus of sharks within the family Lamnidae, colloquially called the "white sharks." The only extant member is the great white shark (Carcharodon carcharias). Extinct species include C. hubbelli and C. hastalis. [3]
A māripi is a type of knife consisting of carved wood with shark teeth embedded in it. It was traditionally made by Māori, the indigenous people of New Zealand. It was used for cutting meat, and not generally as a weapon. [1]
Fossil tooth of Hemipristis serra Several Hemipristis serra teeth from two different locations in the U.S., housed in a large ryker display. Sharks portal; Hemipristis serra is an extinct species of weasel shark which existed during the Miocene epoch. It was described by Louis Agassiz in 1843. [1]