Lamprothamnium, Groves, 1916

Sanjuan, Josep & Martín-Closas, Carles, 2014, Taxonomy and palaeobiogeography of charophytes from the Upper Eocene- Lower Oligocene of the Eastern Ebro Basin (Catalonia, NE Spain), Geodiversitas 36 (3), pp. 385-420 : 396-398

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
status

 

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.

TABLE 3. — Charophyte species and gyrogonite abundances of samples studied from the eastern margin of the Ebro Basin (sections of Santpedor, Maians & Rubió). Vertical position of samples does not represent their relative stratigraphic position. Abbreviations:, 1-25; ·, 26-100; l,>100.

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.

Kingdom

Plantae

Phylum

Charophyta

Class

Charophyceae

Order

Charales

Family

Characeae

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