Volborthella
Volborthella is an animal of uncertain classification, whose fossils pre-date. It has been considered for a period a cephalopod. However discoveries of more detailed fossils showed that Volborthella’s small, conical shell was not secreted but built from grains of the mineral silicon dioxide, and that it was not divided into a series of compartments by septa as those of fossil shelled cephalopods and the living Nautilus are. This illusion was a result of the laminated texture of the organisms' tests. Therefore, Volborthella
Volborthella is widespread, and a useful biostratigraphic indicator; it has been found in North America, Greenland, Spitsbergen, and northeastern Europe, and is restricted to Lower Cambrian rocks, appearing before the trilobites and co-existing with them for some time.
Volborthella has been described as a 'failed attempt in mineralisation'; it constructed its wall by agglutinating grains of sediment, much like some foraminifera, and declined in conjunction with the origin of truly-biomineralising organisms. However, its similarity to Salterella, which contained embedded sediment grains in its mineralised wall, suggests a possible biological relationship - Salterella may have begun to mineralise its agglutinated wall. Some Volborthella specimens do show taphonomic hints that some form of lightly mineralised sheath may have enclosed its agglutinated shell.
A 2025 study suggested that agmatans including Volborthella represent a group of cnidarians.