Temporal range: Upper Cambrian
|Families and genera|
Plectronoceratids are known from the Upper Cambrian (upper Franconian – middle Trempealeauan )of China and North America (Minnesota, Wisconsin). Two families are recognized (Flower, 1964), the generally straight to endogastric Plectronoceratidae and the slightly exogastric Balkoceratidae.
Members of the Plectronocerida are characterized as follows. Shells are generally small, some even tiny, laterally compressed, curved (cyrtochonic) or straight (orthconic). Most cyrtoconic forms are endogastric, with the ventral side longitudinally concave, or the dorsal side more longitudinally convex. A few, the two know genera in Balkoceratidae are exogastrically curved, with the ventral side convex and dorsal side concave. Septa are close spaced, in some less than a milimeter. Siphuncles are ventral, and in most, proportionally large. Connecting rings are in general poorly calcified and may expand as siphonal bulbs into the chambers where not restricted by septal necks.
As with all shelled cephalopds, plectronocerids possessed a tube called a siphuncle, which allowed them to fill the chambers of their phragmocone with gas instead of water, thus controlling their buoyancy. They were not, however, adapted for jet-powered swimming.
The Plectronoceratida gave rise in the Late Cambrian (early and middle Trempealeauan) to the other three plectronoceratoid orders, the Ellesmerocerida, Protactinocerida, and Yanhecerida. The Plectronoceratidae gave rise to the other ellesmerocerid families, including the Upper Cambrian exogastric Balkoceratidea, and with remote possibility to the Discosorida. The Balkoceratidae are unrelated to later exogastric forms that first appeared in the Ordovician
Plectronocerids were probably benthic animals that crawled along the bottom in search of food or safety, facing downwards, with the shell carried above. Nothing is known of their specific soft part anatomy or to what extent tentacles, if any, had developed.
- Chen, J. Y.; Teichert, C. (1983). "Cambrian cephalopods". Geology 11 (11): 647–650. Bibcode:1983Geo....11..647J. doi:10.1130/0091-7613(1983)11<647:CC>2.0.CO;2. ISSN 0091-7613.
- Curt Teichert, 1988. Main Features of Cephalopod Evolution. The Mollusca Vol. 12 Paleontology and Neontology of Cephalopds; Academic Pres Inc.
- Flower, Rousseau H. 1964. The Nautiloid Order Ellesmeroceratida (Cephalopoda); Memoir 12, New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico
- Mutvei, H.; Zhang, Y.; Dunca, E. (2007). "Late Cambrian Plectronocerid Nautiloids and Their Role in Cephalopod Evolution". Palaeontology 50 (6): 1327–1333. doi:10.1111/j.1475-4983.2007.00708.x.
- Flower, Rousseau H. (1955). "Saltations in Nautiloid Coiling". Evolution (Society for the Study of Evolution) 9 (3): 244–260. doi:10.2307/2405647. JSTOR 2405647.
- Furnish, W.M.; Glenister, B.F. (1964). "Nautiloidea - Ellesmerocerida". Treatise on Invertebrate Paleontology K: K129 –.