Cristispira caballasensis, DeVries, 2019
publication ID |
https://doi.org/ 10.1080/00222933.2018.1524032 |
DOI |
https://doi.org/10.5281/zenodo.3671276 |
persistent identifier |
https://treatment.plazi.org/id/03BB2338-E36E-E21D-FE6D-A34B5E88F973 |
treatment provided by |
Valdenar |
scientific name |
Cristispira caballasensis |
status |
sp. nov. |
Cristispira caballasensis sp. nov.
( Figure 5 View Figure 5 (i))
Diagnosis
Hypercampanulate; three strong keeled spiral cords on anterior two-thirds of spire whorls; finely spirally threaded interspaces.
Description
Shell small; pleural angle about 12°. Whorls hypercampanulate, sutural area deeply concave. Protoconch unknown, number of whorls in spire cannot be estimated. Spiral cords keeled; spiral formula dCBAr; primary cords about equally strong. Spacing formula C14B45A67; n = 1). Interspaces with microscopic spiral threads. Lateral growth line orthocline; posterior inflexion absent, anterior inflexion barely discernible. Lateral sinus moderately deep, apex close to spiral cord B. Base and aperture not preserved. Allmon formula?-1-M-B-OR.
Remarks
The elements of the spiral sculpture of Cristispira caballasensis sp. nov., evident even from the partial single specimen available, are nearly identical with those of two Peruvian species, the Late Cretaceous C. prechira (Olsson, 1944) and the middle Eocene C. paracasensis (Rivera, 1957) : three keeled primary spiral cords, a deeply con- cave sutural area, wide concave interspaces with microscopic spiral threads, and in some specimens a secondary spiral cord or thread near the posterior suture. The spacing formula for C. caballasensis (C14B45A67; n = 1) does differ from that of the younger C. paracasensis (C35B58A72; n = 8; DeVries 2007) but is the same as that for the older C. prechira (C14B40A69; n = 1). The strength of the anteriormost primary spiral cord of C. caballasensis , however, is like that of C. paracasensis , i.e. much stronger than the anteriormost primary spiral cord of C. prechira .
Material
UWBM 107605 , holotype, B8769 (type locality), L (5.1), W (4.4).
Occurrence
Lower Paleogene, Cuenca Member, Caballas Formation, East Pisco Basin, southern Peru.
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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