Lophophaena sp. E

Trubovitz, Sarah, Renaudie, Johan, Lazarus, David & Noble, Paula, 2022, Late Neogene Lophophaenidae (Nassellaria, Radiolaria) from the eastern equatorial Pacific, Zootaxa 5160 (1), pp. 1-158 : 70

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.10551572

persistent identifier

https://treatment.plazi.org/id/03C96F50-FFD6-FFBD-75DF-E5E5FA9DC700

treatment provided by

Plazi

scientific name

Lophophaena sp. E
status

 

Lophophaena sp. E group

Plate 37, Figs. 1A View FIGURE 1 – 3C View FIGURE 3 .

Remarks. These three specimens almost certainly belong to different species, but as we only observed three specimens with this very distinct morphology we are placing them together in one group until more specimens are found.All three have an unusually short and widely-flared thorax with teeth, and a proportionally large cephalis. This overall morphology is similar to a specimen figured by Popofsky (1913) as Lampromitra circumtexta, Popofsky, 1913 , pl. 32, fig. 1, text-fig. 53. However, none of our specimens appear to be conspecific with Popofsky’s. One specimen observed from sample 6H3, 31–32cm (Pliocene) differs from Popofsky’s illustrated specimen in that pores on the thorax decrease significantly in size before the segment terminates in several prominent teeth. Our specimen also may have more pronounced shoulder humps, though it is difficult to tell whether this character was present on Popofsky’s specimen due to the nature of the illustration. The overall morphology, shape of the cephalis, and size dimensions are very similar to Popofsky’s specimen, however. A much smaller specimen was found in our Pleistocene EEP sample (3H 2, 103–106cm). It shares several characteristics with our Pliocene specimen, including a large, thorny cephalis with a short, wide thorax that terminates in multiple long teeth, which is a highly unusual morphology for lophophaenids. A third specimen with similar characteristics to our other two was observed in sample 10H2, 91–93cm, although we do not consider any of them to be conspecific. Until additional material is studied, we include them here as a loose species group.

Material examined. 3 specimens form samples 321-1337A-10H-2, 91–94cm (Early Pliocene), 321-1337A-6H-3, 29–32cm (Late Pliocene), and 321-1337A-3H- 2, 103–106cm (Middle Pleistocene).

Range. Pliocene– Pleistocene, EEP ( Table 1 View TABLE 1 ). Range and morphological concept is not well constrained.

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF