Cidaroida Claus, 1880
publication ID |
https://doi.org/ 10.4202/app.00659.2019 |
publication LSID |
lsid:zoobank.org:pub:52C87838-856E-468B-9215-1065205FA02A |
persistent identifier |
https://treatment.plazi.org/id/03FCAB2D-FFBE-265B-FC8E-30C54D8A2FF6 |
treatment provided by |
Felipe |
scientific name |
Cidaroida Claus, 1880 |
status |
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Order Cidaroida Claus, 1880
Isolated spines and partly articulated test fragments (gen. et spp. indet.)
Fig. 30E, I, K, N View Fig .
Material.—More than 90 spines, ambulacral plates, and other ossicles (teeth, rotulae, etc.) (including PZO 12777– 12780) from Misurina Landslide bulk samples and few other remains from Lago Antorno bulk samples, Italy, Carnian, Triassic.
Remarks.—In addition to the stem group echinoid taxon, we have found well preserved and partly articulated test fragments ( Fig. 30E View Fig ) and spines (a few types; e.g., Fig. 30I, K, N View Fig ) of cidaroid echinoids (including “ Cidaris ” cf. decoratissima Wöhrmann, 1889, and “ Cidaris ” cf. flexuosa Münster, 1841) at Misurina Landslide, which represent the majority of sea urchin material from the Ladinian/Carnian Cassian Formation (see also Kier 1984; Vadet 1999a, b; Kroh 2011). However, as more than 40% of the worldwide reported Triassic echinoid “species” are spine-based taxa ( Kroh 2011), disarticulated material remain often indeterminate to species or genus level. Spines (and other ossicles) can be distinct and recognizable, but more studies combining isolated spines and test material, like ambulacral plates, are needed to validate different single species.
Regular echinoids, like in our material, are vagile benthos, moving by means of their spines over the sea floor and using their tube-feet to climb and grip hard substrata ( Smith 2004b). The proterocidarid species described and figured here is presumably a deposit feeder, using its enlarged oral tube-feet for detritus gathering (cf. Thompson and Bottjer 2019).
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