Cladida Moore and Laudon, 1943

Głuchowski, Edward, Casier, Jean-Georges & Olempska, Ewa, 2006, Crinoid and ostracod succession within the Early-Middle Frasnian interval in the Wietrznia quarry, Holy Cross Mountains, Poland, Acta Palaeontologica Polonica 51 (4), pp. 695-706 : 699

publication ID

https://doi.org/ 10.5281/zenodo.13748684

persistent identifier

https://treatment.plazi.org/id/B318330E-9C49-FFC0-0535-E9CB60D9FAFD

treatment provided by

Felipe

scientific name

Cladida Moore and Laudon, 1943
status

 

Order Cladida Moore and Laudon, 1943 Family Cupressocrinitidae Roemer, 1854

Cupressocrinites sp. ( Fig. 3E View Fig ).—The columnals are small, rounded triangular with smooth and slightly convex latus. The articular facet is flat and bordered by a narrow crenularium composed of thick culmina. The lumen is large, trilobate with distinct constrictions in the middle part of the lobes. The columnals are similar to those of Givetian Cupressocrinites inflatus Schultze, 1867 reported from the Loogh Formation of the Eifel Mountains, Germany ( Schultze 1867), and the Portilla Formation of León, Spain ( Breimer 1962), Laskowa Góra Beds and Kowala Formation of the Holy Cross Mountains ( Głuchowski 1993), as well Givetian Cupressocrinites sampelayoi ( Almela and Revilla, 1950) reported from the Portilla Formation ( Almela and Revilla 1950; Breimer 1962) and Laskowa Góra Beds ( Głuchowski 1993), but differ in having more triangular outline and thicker culmina. Le Menn (1988) described similar triangular, rounded columnals with a trilobate axial canal and thin culmina from Frasnian Beaulieu Formation of Boulonnais, France as Trilobocrinus boloniensis Le Menn, 1988 but they may belong to Cupressocrinites .

Order

Cladida

Loc

Cladida Moore and Laudon, 1943

Głuchowski, Edward, Casier, Jean-Georges & Olempska, Ewa 2006
2006
Loc

Trilobocrinus boloniensis

Le Menn 1988
1988
Loc

Cupressocrinites inflatus

Schultze 1867
1867
Loc

Cupressocrinites

Goldfuss 1831
1831
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