Ammonicrinus kerdreoletensis Le Menn and Jaouen, 2003
publication ID |
https://doi.org/ 10.4202/app.2010.0020 |
publication LSID |
lsid:zoobank.org:pub:B872F974-253A-4060-B8F7-C1EC01CECAE3 |
persistent identifier |
https://treatment.plazi.org/id/9D1C87EB-FFE9-FFA8-6421-C8F19C8EFA21 |
treatment provided by |
Felipe |
scientific name |
Ammonicrinus kerdreoletensis Le Menn and Jaouen, 2003 |
status |
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Ammonicrinus kerdreoletensis Le Menn and Jaouen, 2003
Figs. 6, 11 View Fig , 15A View Fig .
2003 Ammonicrinus kerdreoletensis Le Menn and Jaouen, 2003: 207 , 210–211, fig. 4A–C.
Holotype: LPB−1073. The type locality is Coupe de Kerdréolet , niveau
K2, L'Hôpital−Camfrout, Département Finistère (Brittany, France); and the stratigraphy is Kerdréolet Formation, Emsian (Lower Devonian).
Material.— Type material and new material no. GIK−2121 ( Fig. 11 View Fig ).
doi:10.4202/app.2010.0020
Description.— Ammonicrinus kerdreoletensis has a subspherical crown with a relatively large cup in comparison to the narrow width of the mesistele; the cup is not covered laterally by the mesistele and is clearly visible in lateral view ( Fig. 11 View Fig ); the cup ossicles are unsculptured(?). The mesistele is very long and composed of numerous columnals (“exposed runner−type”) that have nearly uncurved to slightly concave external flanks and thin cross sections ( Fig. 11 View Fig ), LCEE of the mesistele regularly arranged and very short ( Fig. 15A View Fig ), several columnals of the mesistele have very short and blunt lateral expansions on both lateral edges of the exterior flanks; connection between mesi− and dististele obviously distinguished by a narrow triangular columnal, which follows distally after the rapid narrowing of the columnals of the distal−most mesistele; dististele and attachment unknown; shape of coiled stem narrow discoidal; mesi− and dististele obviously covered by echinoid spine−tubercles, which presumably bear articulated spines (not preserved).
Discussion.—The numerous columnals of the mesistele of Ammonicrinus kerdreoletensis , the very short lateral expansions of the mesistele and the huge rounded crown clearly separates this species from all other ammonicrinids.
As stated above, the cup of A. kerdreoletensis is laterally not covered by the LCEE. That possibly implies feeding in the current ( Fig. 6) and negates the internal, respectively pumping proposal assumed for the younger ammonicrinids described herein. Furthermore, the new recovered material indicates that the stem of A. kerdreoletensis tapers toward the crown, which was obviously elevated up from the substrate into a possible low velocity current for feeding. Therefore, A. kerdreoletensis can be designated a morphological progenitor of the younger and encased ammonicrinids.
Stratigraphic and geographic range.—Emsian (Kerdréolet Formation) of the Coupe de Kerdréolet, niveau K2, L'Hôpital−Camfrout, Département Finistère (Brittany, France) and lower Eifelian of Vireux−Molhain (southern Ardennes, northern France).
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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Ammonicrinus kerdreoletensis Le Menn and Jaouen, 2003
Bohatý, Jan 2011 |
Ammonicrinus kerdreoletensis
Le Menn, J. & Jaouen, P. A. 2003: 207 |