Ceratocyrtis sp. I
publication ID |
https://doi.org/ 10.11646/zootaxa.5160.1.1 |
publication LSID |
lsid:zoobank.org:pub:A9179C79-EE43-44E4-8723-919505500049 |
DOI |
https://doi.org/10.5281/zenodo.10551452 |
persistent identifier |
https://treatment.plazi.org/id/03C96F50-FFB7-FFDC-75DF-E4EFFD6AC1D8 |
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Plazi |
scientific name |
Ceratocyrtis sp. I |
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Ceratocyrtis sp. I group
Plate. 14, Figs. 3A View FIGURE 3 – 6B View FIGURE 6 .
Ceratocyrtis sp 7 cf, Trubovitz et al., 2020, supplementary data 7.
Remarks. This species group is unique for its relatively heavily silicified cephalis, and long, thin thorax with semiirregular pores that remain similar in size throughout the length of the thorax. It differs from C. cucullaris (Pl. 10, Fig. 1 View FIGURE 1 ) in that the thorax does not flare as widely outward, and it has a relatively thin thorax wall. It differs from C. histricosus (Pl. 10, Figs. 2–3 View FIGURE 2 View FIGURE 3 ) in that it generally grows a much longer thorax, and the pores on the thorax do not substantially increase in size toward the bottom. We list this as a species group rather than a single species because the simple morphology and lack of constraint in morphological variability make it difficult to determine whether this is one species or multiple.
Material examined. 10 specimens observed from Late Miocene samples 321-1337D-23H- 6, 134–137cm, 321- 1337A-18H-6, 77–80cm, and 321-1337A-16H- 6, 121–124cm.
Range. Late Miocene in the EEP ( Table 1 View TABLE 1 ).
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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