Fordilla
The Early Cambrian fossils Fordilla and Pojetaia are regarded as bivalves.[2][3][4][5] Their inner shell layers were constituted of layers of carbonate akin to the laminar aragonite layer in extant monoplacophora.[6]
References
- ^ Charles Doolittle Walcott (1886). Second contribution to the studies on the Cambrian faunas of North America. 30 of Geological Survey bulletin. Govt. Print. Off.,. pp. 369. http://books.google.com/books?id=wikrAAAAYAAJ.
- ^ Pojeta, J. (2000). "Cambran Pelecypoda (Mollusca)". American Malacological Bulletin 15: 157–166.
- ^ Schneider, J.A. (November 2001). "Bivalve systematics during the 20th century". Journal of Paleontology 75 (6): 1119–1127. doi:10.1666/0022-3360(2001)075<1119:BSDTC>2.0.CO;2. http://findarticles.com/p/articles/mi_qa3790/is_200111/ai_n9001371/pg_3. Retrieved 2008-10-05.
- ^ Gubanov, A.P., Kouchinsky, A.V. and Peel, J.S.. "The first evolutionary-adaptive lineage within fossil molluscs". Lethaia 32 (2): 155–157.
- ^ Gubanov, A.P., and Peel, J.S. (2003). "The early Cambrian helcionelloid mollusc Anabarella Vostokova". Palaeontology 46 (5): 1073–1087. doi:10.1111/1475-4983.00334.
- ^ Vendrasco, M.J.; Checa, A.G.; Kouchinsky, A.V. (2011). "Shell microstructure of the early bivalve Pojetaia and the independent origin of nacre within the Mollusca". Palaeontology: no–no. doi:10.1111/j.1475-4983.2011.01056.x. edit