| Priscansermarinus Temporal range: Middle Cambrian (Wuliuan), ~ | |
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| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| Superclass: | Multicrustacea |
| Family: | † Priscansermarinidae Newman, 2004 |
| Genus: | † Priscansermarinus Collins & Rudkin, 1981 |
| Species: | †P. barnetti |
| Binomial name | |
| †Priscansermarinus barnetti Collins & Rudkin, 1981 | |
Priscansermarinus barnetti is an organism known from the Middle Cambrian Burgess Shale which was originally interpreted as a species of lepadomorph barnacle. [2] [1] Four specimens of P. barnetti are known from the Greater Phyllopod bed. [3] A reflective area originally interpreted as external plates has been reinterpreted as a more complex structure inside the body; Derek Briggs, a leading authority on the arthropods of the Burgess Shale, has questioned its assignment as a barnacle or even an arthropod. [4] The World Register of Marine Species places Priscansermarinus in Multicrustacea without assigning a class or order. [5]
The genus name, Priscansermarinus, is a combination of the Latin priscus ("of ancient times"), anser ("goose"), and marinus ("sea"). It roughly translates to "sea goose", referring to the lepadomorph barnacles it was originally assigned to. [1]
The sole species, P. barnetti, is named after Robert Barnett, a member of the Royal Ontario Museum’s 1975 inaugural Burgess Shale expedition, where 62 specimens were discovered in a slab buried beneath scree. [1]