Parvancorina is a genus of shield-shaped bilaterally symmetrical fossil animal that lived in the late Ediacaran seafloor. It has some superficial similarities with the Cambrian trilobite-like arthropods.
| Parvancorina ↓ | |
|---|---|
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| Schematic reconstructions of P. sagitta and P. minchami | |
| Scientific classification | |
| Kingdom: | |
| Phylum: | |
| Genus: | †Parvancorina Glaessner 1958 |
| Type species | |
| P. minchami Glaessner 1958 | |
| Species | |
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The generic name is derived from a crasis compound word from the Latin parva ancora (small anchor).
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 is the Latin word sagitta (arrow), in direct reference to the arrow-like shape.
P. minchami fossils were first discovered in the Ediacara Member of the Rawnslay Quartzite, Flinders Ranges, in South Australia.[1] This species is also known from deposits 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 the Lyamtsa Formation of this Russian region.[2] This Species is also recorded from Sursager area in Jodhpur region, Sonia Formation of Marwar Supergroup in India.[3]
P. sagitta is found in the Verkhovka formation on the Solza River, White Sea area of the Arkhangelsk Region, Russia.[4]
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.
The fossils are normally about 1 centimetre (0.39 inches) in each of width and length, but can be up to 3.0 centimetres (1.2 inches).[3]
In attempting to determine its phylogenic relationships, Parvancorina has been compared with trilobite-like arthropods, such as Skania from the Burgess Shale Biota, Canada, and Primicaris from the Chengjiang Biota, China.[5][6] However, the growth form of Parvancorina is unusual for an arthropod.[2] Furthermore, the strong resemblance of P. sagitta to the primitive mollusk-like bilateran Temnoxa[4] and similarities to parts of Kimberella[7] casts further doubt on an arthropod affinity.
Parvancorina typically lived with their "heads" parallel to the current direction.[8] Overfolding of the fossils from all sides contradicts any form of stalked attachment to the sea floor.[9] They are suggested to have been mobile and able to actively orientate their bodies towards the current direction, with smaller individuals from the Ediacara biota in Australia often found in close association with each other.[10] They have been proposed to be filter feeders, using their body ridges to direct water towards feeding structures, with deposit feeding being a possible but less likely ecology.[8]
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