Endocerida
Endocerida Temporal range:
| |
---|---|
The massive endocerid Cameroceras (middle) alongside other nautiloids | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Mollusca |
Class: | Cephalopoda |
Subclass: | Nautiloidea |
Superorder: | †Endoceratoidea |
Order: | †Endocerida Teichert, 1933 |
Families | |
† Cyrtendoceratidae |
Endocerida is an extinct
Morphology
Endocerids had a relatively small
Body size
Endocerids reached enormous body sizes. The largest confirmed specimen, belonging to Endoceras giganteum, is 3 metres (9.8 ft) long as preserved, but is missing a substantial portion of its aboral end.[3][4] The reconstructed length of the shell is nearly 6 metres (20 ft).[3][4] An alleged endocerid specimen 30 feet (9.1 m) long is unconfirmed.[3]
Ecology
The mode of life of endocerids is debated.[5] Endocerids may have been the apex predators of the Ordovician, probably living close to the sea floor, and preying on trilobites, molluscs, brachiopods and other bottom-dwelling organisms.[1] They were probably not active nektonic swimmers, but rather crawled over the floor of epicontinental seas or lay there in ambush.[citation needed] Although there is study that supports filter feeding ecology,[5] according to hydrostatic properties, it is not likely and still supports benthic predators.[6]
Reproduction
Endocerids laid relatively large eggs, and hatched at a relatively large body size.
Diversity
Endocerids were among some half a dozen cephalopod orders that appeared in the Lower Ordovician. They reached their greatest diversity during the Lower to Mid-Ordovician, but were already in decline by the middle of this period with most genera becoming extinct by the end of the Sandbian (late Ordovician), while some rare hangers on lasted into the Silurian.[2] In any case, the endocerid lineage became completely extinct relatively early on in cephalopod history.
Classification
Evolution
Endocerids evolved from the earlier ellesmerocerids, most likely from a genus similar to Pachendoceras. This ellesmerocerid gave rise to Proendoceras, the earliest representative of the Proterocameroceratidae and hence of the Endocerida. Endocerids evolved from ellesmerocerids by reduction of siphuncle diaphragms and the development of endocones. In the early part of the mid-Lower Ordovician, the Endocerida quickly diversified into many different families. In true endocerids, there was a trend of overall increasing size, eventually resulting in massive orthoconic genera such as Endoceras and Cameroceras. In another lineage (now known as Bisonocerida), the siphuncle grew more complex, resulting in genera such as Chihlioceras and Allotrioceras.
Taxonomy
Citing its diversity, Curt Teichert (1964) placed the Endocerida in its own subclass called the Endoceroidea or Endoceratoidea (which some Russian paleontologists ranked as a
Flower (1958) divided the Endocerida into two suborders, the Proterocamerocerina and the Endocerina. As he defined the two suborders, Proterocamerocerina included the Proterocameroceratidae, Manchuroceratidae, and Emmonsoceratidae, while Endocerina included the Piloceratidae and Endoceratidae. Endocerid classification since then has relied on a dichotomy between short-shelled forms with complex endocones and long-shelled forms with simple endocones.
Endocerid relationships have been difficult to establish both within the order and relative to other nautiloids. Their generally orthoconic shell shape and dorsomyarian muscle scars are similar to the subclass
Restudy of piloceratid-like families with complex endocones has suggested that Endocerida in its broadest form is polyphyletic, with piloceratid-like and proterocameroceratid-like members having independent origins from ellesmerocerids. In light of this issue, the numerous piloceratid-like families were placed within a new order, Bisonocerida.[10] Bisonocerida may still be related to endocerids within Endoceratoidea.[9]
See also
References
- ^ a b Kröger, Björn; Yun-Bai, Zhang (2008). "Pulsed cephalopod diversification during the Ordovician". Palaeogeography, Palaeoclimatology, Palaeoecology. 273 (1–2): 174–183. .
- ^ S2CID 83608661.
- ^ a b c Teichert, Curt; Kummel, Bernhard (1960). "Size of endoceroid cephalopods". Breviora. 128.
- ^ a b Klug, Christian; De Baets, Kenneth; Kröger, Björn; Bell, Mark A.; Korn, Dieter; Payne, Jonathan L. (2015). "Normal giants? Temporal and latitudinal shifts of Palaeozoic marine invertebrate gigantism and global change". Lethaia. 48 (2): 267–288. .
- ^ a b c
Mironenko, Aleksandr A. (2018). "Endocerids: suspension feeding nautiloids?". Historical Biology. 32 (2): 1–9. S2CID 89799876.
- S2CID 181794320.
- ^ a b
Laptikhovsky, Vladimir; Nikolaeva, Svetlana; Rogov, Mikhail (2018). "Cephalopod embryonic shells as a tool to reconstruct reproductive strategies in extinct taxa". Biological Reviews. 93 (1): 270–83. PMID 28560755.
- S2CID 133647555.
- ^ S2CID 248158390.
- ISSN 0016-6995.
Further reading
- Clarke, J.M. 1897. The Lower Silurian Cephalopoda of Minnesota. In: E.O. Ulrich, J.M. Clarke, W.H. Scofield & N.H. Winchell The Geology of Minnesota. Vol. III, Part II, of the final report. Paleontology. Harrison & Smith, Minneapolis. pp. 761–812.
- Flower, 1955, Status of Endoceroid Classification; Jour. Paleon. V 29. n.3 May 1955,pp 327–370; figs, plts.
- Flower,1958, Some Chazyan and Mohawkian Endoceratida; Jour. Paleon V32, n.3,pp 433–468; figs, plts.
- Flower, 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.
- Teichert, C. 1964, Endoceratoidea, in the Treatise on Invertebrate Paleontology, Part-K (Nautiloidea; Geol Soc of America and University of Kansas Press; pp K160–K188; figs.
- Neale Monks and Philip Palmer. Ammonites. Smithsonian Institution Press, Washington D.C. 2002.