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Spinisinella zagorseki
Taxonomy
Spinisinella zagorseki was named by Di Martino and Taylor (2012). Its type specimen is NMP O-6751 and is a 3D body fossil. Its type locality is Kaňk (Počta collection), which is in a Cenomanian/Turonian carbonate limestone in Czechia. It is the type species of Spinisinella.
Synonymy list
Year | Name and author |
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2012 | Spinisinella zagorseki Di Martino and Taylor p. 6 figs. 9-12 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Spinisinella zagorseki Di Martino and Taylor 2012
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Diagnosis
Reference | Diagnosis | |
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E. Di Martino and P. D. Taylor 2012 | Colony encrusting, multiserial, unilaminar. Autozooids small, distinct, oval, slightly longer than broad, separated by deep furrows. Gymnocyst narrow. Cryptocyst extensively developed, depressed, flat and granular; mural rim salient, together with distal rim of opesia forming pear-shaped border around the cryptocyst and opesia; opesiules lacking. Opesia trifoliate, longer than wide, a pair of rounded indentations present in the proximal third. Oral spines present. Ovicell cribrate, ooecium represented by a pair of spine bases arranged parallel to the long axis of the zooid and bordering a depression on the proximal gymnocyst of the distal zooid. Avicularia and ancestrula not observed. |
Measurements
No measurements are available
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Source: o = order, c = class, uc = unranked clade | |||||
References: Nesnidal et al. 2013, Smith et al. 2006 |
Age range: base of the Late/Upper Cenomanian to the top of the Early/Lower Turonian or 100.50000 to 89.80000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Late/Upper Cenomanian - Early/Lower Turonian | Czechia | Spinisinella zagorseki (type locality: 213659) |