Elopothrissus, SCHWARZHANS, 1981
publication ID |
https://doi.org/ 10.5070/P940361192. |
publication LSID |
lsid:zoobank.org:pub:3B70D32F-9BF0-4595-AF4B-45ADEE03B204 |
DOI |
https://doi.org/10.5281/zenodo.11474174 |
persistent identifier |
https://treatment.plazi.org/id/2B4F878B-2569-FF90-FC0A-F96AFEC9FC44 |
treatment provided by |
Felipe |
scientific name |
Elopothrissus |
status |
|
ELOPOTHRISSUS SCHWARZHANS, 1981
FIG. 5C View Figure 5
Material— one specimen, DMNH 2021-09- 03 About DMNH . About DMNH
Description and Remarks— The one elongate specimen assigned to Elopothrissus has a prominent sulcus clearly divided into an oval ostium opening anteriorly and anterodorsally, and a narrower, longer more excavated cauda. However, as noted in Schwarzhans and Stringer (2020a) there are significant changes in the H/L ratios with ontogenetic changes in size, which is caused primarily by an increase in the length of the rostrum. There is a slight postdorsal angle as well as some faint marginal crenulation. Like with many other pterothrissids, morphological maturity is only reached when specimens are more than 5 mm long, hence, smaller specimens should not be used for species definition ( Schwarzhans 2012). For this reason, DMNH 2021-09-03, which is only 1.83 mm long, is identified only to genus.
Elopothrissus carsonsloani Schwarzhans and Stringer (2020a) was reported from the Danian Clayton Formation but not the Maastrichtian Kemp Clay ( Schwarzhans and Stringer 2020a). An unidentified species of Elopothrissus was noted by Schwarzhans et al. (2018b) from the Santonian of Alabama. The genus represents an extinct pterothrissid that extends across the K-Pg extinction event and well into the Paleogene ( Schwarzhans and Stringer 2020a).
DMNH |
Delaware Museum of Natural History |
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