Melikeriopalla sp.

García Muro, Victoria J., Rubinstein, Claudia V. & Steemans, Philippe, 2018, Late Silurian palynomorphs from the Precordillera of San Juan, Argentina: Diversity, palaeoenvironmental and palaeogeographic significance, Acta Palaeontologica Polonica 63 (1), pp. 41-61 : 45-46

publication ID

https://doi.org/ 10.4202/app.00400.2017

DOI

https://doi.org/10.5281/zenodo.10999451

persistent identifier

https://treatment.plazi.org/id/88508783-FD4D-FF84-FC87-F8BA0F738213

treatment provided by

Felipe

scientific name

Melikeriopalla sp.
status

 

cf. Melikeriopalla sp.

Fig. 9A–F View Fig .

Material.— 14 specimens measured. Samples MPLP 1-61065 ( U47 /2, W30 /3); MPLP 3-61058 ( L33 ); MPLP 6-61061 ( M31 /3); MPLP 7-61062 (D39, D45/3, P43 /3, P50 /3); MPLP 2-60704 ( L26 /4); MPLP 3-60659 ( F38 /3, R38 /1); MPLP 4-62521 ( T40 /4, T40 /4); MPLP 6-60662 ( J25 /2). Vesicle divided into filds by muri. Homerian–Ludfordian of Argentina. Cerro La Chilca and Quebrada Ancha localities, Los Espejos Formation .

Description.— Vesicle square to sub-spherical, divided into 6–13 polygonal fields by thick muri. Each field is ornamented by a ring and/or a granum; when both are present the granum is located in the center of the ring.

Dimensions.— Vesicle 16–(23)–30 μm, fields 6–(9)–12 μm, muri high 0.3–1 μm, grana high 0.5–(1)–3 μm, grana diameter 1–(3)–5 μm, rings high 0.3–(0.5)–1 μm, rings thick 0.5–(1.5)–3 μm (14 specimens measured; number in brackets is the mean value).

Discussion.— According to the emended diagnosis of Mullins 2001), in the centre of each field a circular node beneath which a pore may or may not be present. Because of the poor preservation, the pore cannot be observed in the specimens from the Los Espejos Formation. The genus was assigned with doubts because no ring was described for Melikeriopalla .

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