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The Reudemannoceratidae are the ancestral and most primitive of the
Discosorida Discosorida are an order of cephalopods that lived from the beginning of the Middle Ordovician, through the Silurian, and into the Devonian. Discosorids are unique in the structure and formation of the siphuncle, the tube that runs through an ...
, an order of cephalopods from the early
Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ...
. The Reudemannoceratidae produced generally medium-sized endogastric and almost straight shells with the
siphuncle The siphuncle is a strand of tissue passing longitudinally through the shell of a cephalopod mollusk. Only cephalopods with chambered shells have siphuncles, such as the extinct ammonites and belemnites, and the living nautiluses, cuttlefish, and ...
slightly ventral from the center.


Derivation

The Reudemannoceratidae first appeared at the beginning of the Middle Ordovician, North American Whiterock stage, (since replaced by the
ICS ICS may refer to: Computing * Image Cytometry Standard, a digital multidimensional image file format used in life sciences microscopy * Industrial control system, computer systems and networks used to control industrial plants and infrastructu ...
Dapingian), and are restricted to the lower part of that series. (the middle Ordovician). Their origin is unknown. The siphuncles in early members contain features in the early growth stages reminiscent of the siphuncular bulbs found the archaic Plectronoceratae of the
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. (Flower and Teichert 1957) but so far no unambiguous Lower Ordovician intermediaries have been found.


Characters

Reudemannoceratids are characterized by having short septal necks in the juvenile portion of the siphuncle, toward the apex of the shell, which later in life grow folded back along the back side of the septa in the characteristic fashion of the Discosorida. The connecting ring is bowed out into the camerae and is divided into the characteristic zones, the vinculum, granular zone, conchiolinous (or chitinous) zone offset by amorphous bands, and the layered bullette attached to the previous septal neck. (Flower and Teichert 1957, Teichert 1964)


Genera

The Reucenammanoceratidae contain three genera (Teichert 1964). They are ''Reudemannoceras'', ''Franklinoceras'', and ''Madiganella''. ''Reudemannoceras'' and ''Franklinoceras'', named by Flower in 1940 and 1957, are found the
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in eastern North America. ''Madiganella'', named by Teichert and Glenister in 1952, comes from central Australia. ''Reudemannoceras'' is described (Flower and Teichert 1957) as having a somewhat compressed endogastric shell, such that the width is greater than the height, with the venter slightly flattened. Sutures are closely spaced and slope forward from venter to dorsum with the obliquity increasing as growth progressed. The early part of the shell is essentially straight, but afterward expands and is notably curved. The early segments in the siphuncle (Techert 1964) are bulb shaped and the septal necks are short. In the later part of the shell she segments are expanded and septal necks become recumbent. The connecting rings are thick and have the zoning characteristic of the earlier Discosorids with well-developed bullettes. ''Franklinoceras'' (Teichert 1964) is similar to ''Reudemannocereras'', except that the shell is compressed and the sutures are straight. ''Madiganella'' has a large, slender, straight or nearly straight shell (Teichert 1964) with a siphuncle composed of broad, expanded segments and short, strongly recurved necks. Growth lines indicate a shallow hyponomic sinus.


Evolution and phylogeny

''Reudemannoceras'' gave rise to the Cyrtogomphoceratidae through ''Ulrichoceras'' (Teichert 1964) as a result of an evolutionary ventral shift of the siphuncle and the development of large, inflated bullettes. ''Ulrichoceras'' is the probable ancestor of the
Westonoceratidae Westonoceratidae are exogastric, mostly compressed, Discosorida of moderate size from the Middle Ordovician to the Lower Silurian. The siphuncle is typically close to the convexly curved outer margin of the phragmocone – the chambered part o ...
as well. ''Reudemannoceras'' is also thought to have given rise (Teichert 1964) to ''Madiganella'' by an evolutionary straightening of the shell which by the subsequent development of T-shaped constricted apertures gave rise to the
Mandaloceratidae Mandaloceratidae is a family in the nautiloid cephalopod order Discosorida, from the Middle and Upper(?) Silurian characterized by short, essentially straight shells referred to as breviconic, typically with a faintly exogastric shape produced b ...
. ''Franklinoceras'' seems to be an offshoot of ''Reudemanoceras'' with no progeny. .


Ecology and lifestyle

Reudemannoceratids probably lived on or near the sea floor. Endogastric ''Reudemannoceras'' and ''Franklinoceras'' are likely to have carried their shells high and to the back, aperture facing downward, as they probed the sea bed for prey. The more advanced and slightly later Madiganella may have been a fair swimmer, as indicated by the hyponomic sinus, and may have been an active stalker with a horizontal orientation.


References

* Flower, R.H.and Teichert, C.,1957. The Cephalopod Order Discosorida; University of Kansas Paleontological Contributions, Mollusca, Article 6. * Teichert, C.,1964. Nautiloidea -Discosorida;
Treatise on Invertebrate Paleontology The ''Treatise on Invertebrate Paleontology'' (or ''TIP'') published by the Geological Society of America and the University of Kansas Press, is a definitive multi-authored work of some 50 volumes, written by more than 300 paleontologists, and co ...
, Vol. K, (K320-k328) {{Taxonbar, from=Q7317543 Nautiloids Middle Ordovician first appearances Middle Ordovician extinctions