Temporal range: Ordovician
Flower & Kummel, 1950
The Order Basslerocerida was established by Flower and Kummel (1950) for forms intermediary between the ancestral Ellesmerocerida and the more advanced Tarphycerida and Oncocerida. The order, as originally defined, contains two families, the Bassleroceratidae with thick-walled siphuncles which gave rise to the Tarphycerida, and the Graciloceratidae, derived from the former, with thin-walled siphuncles which gave rise to the Onocerida. The speculation in Flower and Kummel (1950) that the Basslerocerida, through the Graciloceratidae, might have given rise to the Barrandeocerida may account for the inclusion of the Barradeocerina in the Basslerocerida in some classifications and the extension of the order to the Devonian. The derivation of barrandeoceroids from within the Tarphycerida is however well established.
Basslerocerida has fallen into general disuse, the taxa now being included in either the Ellesmerocerida or in the derived Tarphycerida and Oncocerida, although Sheverev (2006)  continued to recognize the order. Furnish and Glenister (1964)  included the Bassleroceratidae in the Ellesmerocerida while Sweet (1964) included its derivative, the Graciloceratidae, in the Oncocerida. Flower (e.g. 1976) instead included the Bassleroceritidae in the Tarphycerida.
Nothing is known about the basslerocerid soft part anatomy, although they may be surmised to have had somewhat squid-like bodies with perhaps 8 or 10 arms.
Shells are rather small, reaching lengths of about 12 -15 cm (5 -6 in); elongate with an upward, exogastric, curvature -like a rocker -and subcircular to laterally compressed cross section. The venter on the outer curvature is commonly more sharply rounded, giving it a keel-like form, than the dorsum on the inner curvature. Septa are close spaced, the siphuncle ventral.
The siphuncle in the Bassleroceratidae is composed of thick connecting rings as found in the ancestral Ellesmerocerida and in primitive Tarphycerida. Connecting rings in the derived Graciloceratidae are thin, as found in the Oncocerida.
- R. H. Flower and B. Kummel. 1950. A Classification of the Nautiloidea. Journal of Paleontology 24(5):604-616
- A. A. Shevyrev. 2006. The Cephalopod Macrosystem: A Historical Review, the Present State of Knowledge, and Unsolved Problems: 2. Classification of Nautiloid Cephalopods. Paleontological Journal 40(1)
- Furnish W.M and Glenister, Brian F 1964, Nautiloidea -Ellesmerocerida. Treatise on Invertebrate Paleontology, Geol Soc of America and Univ Kansas Press (Teichert & Moore, Eds)
- Sweet, Walter C. 1964 Nautiloidea- Oncocerida. Treatise on Invertebrate Paleontology , Geol Soc of America and Univ Kansas Press (Teichert & Moore, Eds)
- Flower, R. H. 1976. Ordovician Cephalopod Faunas and Their Role in Correlation, in Bassett, M.C. (Ed); The Ordovician System: Proceedings of a Paleontological Association Symposium; Birmingham, Eng. 1974; Univ of Wales and Welsh Nat’l Mus Press