Temporal range: Ediacaran, around 558–555Ma
|Schematic reconstructions of P. sagitta and P. minchami|
|Phylum:||incertae sedis: Arthropoda?|
Parvancorina is a genus of shield-shaped bilaterally symmetrical fossil animal that lived in the late Ediacaran seafloor. It has some similarities with the Cambrian trilobite-like arthropods.
The specific name of the type species, P. minchami, honors Mr. H. Mincham, the private collector, who in 1957 had collected and presented a number of fine specimens of Ediacaran fossils to the South Australian Museum.
The specific name of P. sagitta from the Latin sagitta (arrow).
P. minchami fossils were first discovered in the Ediacara Member of the Rawnslay Quartzite, Flinders Ranges in South Australia. This species also known from deposites of the Verkhovka, Zimnegory and Yorga Formations in the White Sea area of the Arkhangelsk Region, Russia. Additionally, similar poorly preserved Parvancorina sp. fossils were found in Lyamtsa Formation of this Russian region.
P. sagitta is found in the Verkhovka formation on the Solza River, White Sea area of the Arkhangelsk Region, Russia.
It has a raised ridge down the central axis of symmetry. This ridge can be high in unflattened fossils. At the 'head' end of the ridge there are two quarter circle shaped raised arcs attached. In front of this are two nested semicircular lines. Teeth seem to come from the raised parts pointing into the centre spaces. These may show as raised lines.
The fossils are normally about 1 cm in each of width and length, but can be up to 2 cm.
Parvancorina has been compared with the Skania fragilis from the Burgess Shale Biota, Canada, and Primicaris larvaformis from the Chengjiang Biota, China is the Cambrian trilobite-like arthropods. However, Parvancorina growth form is unusual for an arthropod, and its apparent mode of life appears to rebut an arthropodan affinity, and P. sagitta's strong resemblance to the primitive bilateran Temnoxa.
The organisms typically lived with their "heads" parallel to the current direction, although overfolding of the fossils from all sides contradicts any form of stalked attachment to the sea floor.
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