Fordilla

''Fordilla'' is an extinct genus of early bivalves, one of two genera in the extinct family Fordillidae. The genus is known solely from Early Cambrian fossils found in North America, Greenland, Europe, the Middle East, and Asia.The Paleobiology Database ''Fordilla'' entry
accessed 4 January 2012 The genus currently contains three described species, ''Fordilla germanica'', ''Fordilla sibirica'', and the type species ''Fordilla troyensis''.

Description

''Fordilla'' are small bivalves with valves that are equal in size and suboval in shape. In size ''Fordilla'' specimens reach a total shell length of up to and a height of . The shells are compressed laterally and the back edge is slightly broadened. The rear adductor is less developed and smaller than the front adductor, while the small pedal retractor muscle scar is positioned near the front adductor scar. The valve hing is usually straight to slightly convexly curved and each valve will have at most one tooth present. The external surface of the shell occasionally show faint ribbing. The inner shell layers of ''Fordilla'' species, as with the related genus ''Pojetaia'', consist of layers of carbonate which is akin to the laminar aragonite layer found in extant monoplacophora. The structuring is similar to shell layering found in the extinct genera ''Anabarella'' and ''Watsonella'' which is thought to suggest members of the phylum Mollusca developed nacre independently several times. Due to the size and age of the fossil specimens, ''Fordilla'' are included as part of the Turkish Small shelly fauna.

Species

''F. germanica''

Described in 1994, ''F. germanica'' is the most recent valid species of ''Fordilla'' to be described. As the species etymology indicates, the species was first described from strata of the Zwetau Formation in Germany, with the type locality at Görlitz, Saxony. The species is identifiable from the other two ''Fordilla'' species by the more elongated shape of the valves, the straight dorsal edge which has a slight tilt, and by the muscle arrangement. The shells reach up to long, by wide and tall. The placement of ''F. germanica'' questioned by Geyer and Streng in 1998 who, noting the size of the specimens, moved the species to ''Pojetaia'' as ''P. germanica''. This move was rejected by subsequent authors and the species moved back to ''Fordilla'' by Elicki in 2009.

''F. sibirica''

''F. sibirica'' was named by I.N. Krasilova in 1977 based on a series of about 20 fossils from the Tyuser Formation in Northeastern Siberia. Since the species description opinions have differed on the validity of its status, with several studies synonymizing it with ''F. troyensis''. The original description cited the placement and more rounded outline of the front adductor scar along with the morphology of dorsal edge as reason for erection of the new species.

''F. troyensis''

The type species for ''Fordilla'', ''F. troyensis'' was first described by the French paleontologist Joachim Barrande in 1881. The description was based on a group of five fossils found in Cambrian sediments exposed at Troy, New York and purchased by S.W. Ford. The species has since been found in Cambrian strata of Greenland and Newfoundland in North America. Specimens have been confirmed from the island of Bornholm, Denmark. Fossils tentatively placed in ''Fordilla'' from the Browns Pond Formation of
New York and Anse Maranda Formation of Quebec have been reassigned to ''Pojetaia runnegari''.

Other fossils

Additional fossils have been attributed to the genus since its description. A fossil from North Attleboro, Massachusetts was placed in the genus by Shaler and Foerste in 1888, however this specimen was later determined to be a possible fossil of ''Heraultia''. Fossils form Hartshill, North Warwickshire, England and the lower Cambrian of Portugal have been tentatively placed into ''Fordilla'' without assignment to species. Specimens from Zaragoza, Spain were placed into ''Fordilla'' with the name ''Fordilla marini'' but the size and shape of the specimens indicates they do not belong to the genus. The cryptic genus ''Buluniella'' and species ''B. borealis'' was described in 1986 by V. Jermak from three fossils found in Northern Siberia. The two right and one left disarticulated valves known show a slightly convexity of the hinge, central umbo and lack of a row of muscle scars were used to the genus from ''Fordilla''. The less distinct umbones were suggested as reason to separate ''Buluniella'' from ''Pojetaia''. Due to the high variation in characters of Cambrian bivalve species the validity of ''Buluniella'' as a separate genus and species has been questioned several times. In 1992 Bruce Runnegar and Pojeta recommended ''Buluniella'' belonged to ''Fordilla'' and suggested the species be treated as ''Fordilla borealis''. Further examination of the fossils has resulted in both the genus and the species being currently treated as a synonym of ''P. runnegari''.

References

{{Taxonbar, from=Q5468091

Prehistoric bivalve genera
Prehistoric life of Europe
Cambrian molluscs
Fossil taxa described in 1881
Paleozoic life of Newfoundland and Labrador
Paleozoic life of Nova Scotia
Taxa named by Joachim Barrande