Isorthoceras sp. B
publication ID |
https://doi.org/10.5852/ejt.2025.978.2801 |
publication LSID |
lsid:zoobank.org:pub:422E6F06-B4C8-4840-854C-811145D88B32 |
persistent identifier |
https://treatment.plazi.org/id/93268783-9644-7014-FD5C-FC9DFCFEFA0A |
treatment provided by |
Plazi (2025-03-07 10:46:31, last updated by GgImagineBatch 2025-03-07 11:20:26) |
scientific name |
Isorthoceras sp. B |
status |
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Fig. 12B
Material examined
ESTONIA • 1 spec.; Moe trench; Kõrgessaare Formation, Vormsi Regional Stage; GIT 878-116 View Materials .
Description
Specimen GIT 878-116 is a ca 12 mm long internal mold of parts of a mature body chamber and three phragmocone chambers with a circular conch cross section. The maximum diameter of the specimen is 10 mm at its adoral end. At the base of the body chamber the diameter is 9.8 mm and the adapicalmost chamber has a diameter of 9.6 mm (angle of expansion 2.5°). The three preserved chambers of the phragmocone decrease in length from 2.4 mm to 1.5 mm, to 0.5 mm adorally. The septal foramen is well preserved at 1.7 mm from the conch margin, where the conch cross section is 9.6 mm in diameter (RSP = 0.18), with a diameter of 1.1 mm (RSH = 0.11). The conch surface is apparently smooth, although fine details of the ornamentation are not preserved.
Remarks
This specimen can be related to I. junceum ( Hall, 1847) with respect to the mature conch size, position of the siphuncle, and general conch shape. However, because the crucial details of the conch surface are not preserved, a species level determination is not possible.
Hall J. 1847. Natural History of New York, Paleontology, Volume 1, Containing Descriptions of the Organic Remains of the Lower Division of the New-York System (equivalent of the Lower Silurian Rocks of Europe). Van Benthuysen, Albany, NY. https://doi.org/10.5962/bhl.title.39838
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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