Lamprothamnium, Groves, 1916
publication ID |
https://doi.org/ 10.5252/g2014n3a3 |
DOI |
https://doi.org/10.5281/zenodo.4836366 |
persistent identifier |
https://treatment.plazi.org/id/D25987DD-FFEE-FFB7-FCED-EDE62CD08EC0 |
treatment provided by |
Felipe |
scientific name |
Lamprothamnium |
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Lamprothamnium View in CoL sp.
( Fig. 6 View FIG I-L)
DESCRIPTION
Medium-sized gyrogonites, 432-648 µm high (mean 547 µm) and 297-513 µm wide (mean 434 µm), elongate, prolate to sub-cylindrical in shape, with an isopolarity index ranging from 111-163 (mean
127). Apex lamprothamnoid, truncated, showing a marked periapical depression due to decreasing cell thickness. Ŋe base is rounded with a small basal pore (45 µm). Spiral cells flat to convex, without ornamentation. Eight to ten (frequently nine) convolutions are visible in lateral view.
REMARKS
A population from Sant Bartomeu del Grau (NE Ebro Basin) belongs to the genus Lamprothamnium according to the general sub-cylindrical shape and the apical structure ( Table 2 View TABLE ). Gyrogonites of Lamprothamnium sp. from sample CC-1 is similar in gyrogonite width and convolution number to the Lower Eocene Lamprothamnium priscum Castel & Grambast, 1969 . However, gyrogonites from the Ebro Basin are about 115 µm shorter, resulting in a more rounded morphology.Poor preservation hinders their specific attribution.
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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