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Perisphinctes (Arisphinctes) chloroolithicus
Taxonomy
Ammonites chloroolithicus was named by Guembel (1865).
It was recombined as Perisphinctes chloroolithicus by Waagen (1875); it was recombined as Perisphinctes (Perisphinctes) chloroolithicus by Schlegelmilch (1994); it was recombined as Perisphinctes (Arisphinctes) chloroolithicus by Pandey et al. (2012).
It was recombined as Perisphinctes chloroolithicus by Waagen (1875); it was recombined as Perisphinctes (Perisphinctes) chloroolithicus by Schlegelmilch (1994); it was recombined as Perisphinctes (Arisphinctes) chloroolithicus by Pandey et al. (2012).
Sister species lacking formal opinion data
P. africanus, P. andium, P. mairei-matheyi, P. malinowskae, P. panderi, P. polygyratus, P. praestenocyclus, P. progeron, P. quadratus, P. scythicus, P. siemiradzkii, P. eucostatus, P. quadratus, P. pickeringius, P. buckmani, P. buckmanni, P. luciaeformis, P. crassissimus, P. A, P. B, P. anguiculus, P. patturatensis, P. siemirazkii, P. roedereri, P. alatus, P. andelotensis, P. densecostatus, P. pumilus, P. dorsoplanus, P. dacquei, P. polygyratus
Synonymy list
Year | Name and author |
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1875 | Perisphinctes chloroolithicus Waagen p. 198 |
1994 | Perisphinctes (Perisphinctes) chloroolithicus Schlegelmilch p. 61 figs. Pl 20, fig 2 |
2012 | Perisphinctes (Arisphinctes) chloroolithicus Pandey et al. |
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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.
†Perisphinctes (Arisphinctes) chloroolithicus Guembel 1865
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Diagnosis
Reference | Diagnosis | |
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D.K. Pandey et al. 2012 | Shells small to moderately large, incomplete, septate till end, evolute, compressed. Whorl section subquadrate to subtabulate in outline, lanks lat, merging smoothly into rounded venter (Fig. 15A-D). Ornamentation consists of gradually varicostate, sharp, prorsiradiate primary ribs, very ine in nucleus and moderately coarse in middle whorls. Primaries generally bifurcate into iner secondary ribs at ventrolateral region. Bifurcation occasionally also seen in umbilicus. Secondary ribs cross the venter with slight forward-directed convexity. Ribs originate rursiradiately at umbilical suture (Fig. 15E, F). Ribbing density is moderate to dense. Umbilical wall short, distinct, and steep. Constrictions present, at least one per whorl. |
Measurements
No measurements are available
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Source: o = order, c = class | |||||
References: Kiessling 2003, Kiessling 2004 |
Age range: Middle Oxfordian or 161.20000 to 155.70000 Ma
Collections (6 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Early/Lower Oxfordian | France | Perisphinctes chloroolithicus (12286 12287) | |
Middle Oxfordian | Germany | Perisphinctes chloroolithicus (62304) | |
Middle Oxfordian | France | Perisphinctes chloroolithicus (12288 12291) | |
Middle Oxfordian | United Kingdom | Perisphinctes chloroolithicus (86019) |