Waptia
Sign in to saveWaptia is an extinct genus of marine arthropod from the Middle Cambrian of North America. It grew to a length of , and had a large bivalved carapace and a segmented body terminating into a pair of tail flaps. It was an active swimmer and likely a predator of soft-bodied prey. It is also one of the oldest animals with direct evidence of brood care. Waptia fieldensis is the only species classified under the genus Waptia, and is known from the Burgess Shale Lagerstätte of British Columbia, Canada. Specimens of Waptia are also known from the Spence Shale of Utah, United States.
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Vinony's link graph records 50 inbound references to Waptia, and connects out to arthropod leg, Cambrian and Charles Doolittle Walcott.
It sits within the topics Burgess Shale fossils, Cambrian arthropods and Cambrian arthropods of North America.
Vinony links it to 10 Wikipedia language editions.
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Encyclopedic overview
8 sectionsContents
- Description
- Discovery
- Taphonomy
- Taxonomy
- Ecology
- See also
- References
- External links
Waptia is an extinct genus of marine arthropod from the Middle Cambrian of North America. It grew to a length of , and had a large bivalved carapace and a segmented body terminating into a pair of tail flaps. It was an active swimmer and likely a predator of soft-bodied prey. It is also one of the oldest animals with direct evidence of brood care. Waptia fieldensis is the only species classified under the genus Waptia, and is known from the Burgess Shale Lagerstätte of British Columbia, Canada. Specimens of Waptia are also known from the Spence Shale of Utah, United States.
Based on the number of individuals, Waptia fieldensis is the third most abundant arthropod from the Burgess Shale Formation, with thousands of specimens collected. It was among the first fossils found by the American paleontologist Charles D. Walcott in 1909. He described it in 1912 and named it after two mountains near the discovery site – Wapta Mountain and Mount Field.
Excerpted from Wikipedia’s “Waptia” article, available under the CC BY-SA 4.0 licence.