Cocconeis pelta A. Schmidt

Joh, Gyeongje, 2021, Distribution of the genus Cocconeis (Bacillariophyceae) along the Seogwipo coast of Jeju Island, South Korea, Phytotaxa 528 (3), pp. 149-179 : 161-162

publication ID

https://doi.org/ 10.11646/phytotaxa.528.3.1

DOI

https://doi.org/10.5281/zenodo.5788123

persistent identifier

https://treatment.plazi.org/id/D0663914-FF86-FFE2-1B95-F8C9FDC5976E

treatment provided by

Plazi

scientific name

Cocconeis pelta A. Schmidt
status

 

16. Cocconeis pelta A. Schmidt ( Figs 20, 21 View FIGURES 3–24 )

Basionym: Schmidt 1874, p. 93, pl. 3, fig. 17.

References: Hustedt 1933, p. 361, fig. 815; Witkowski et al. 2000, p. 111, pl. 41, figs 7–10; Sar et al. 2003, p. 91, fig. 33.

Description: Valves elliptical, 15–16 μm long, 11–12 μm wide. SV: sternum slightly very broadly lanceolate to elliptical, depressed making a distinct marginal rim, irregularly punctate. Central area not developed. Transapical striae developed in the margins, radiate towards the apices, 17–18 in 10 μm. RV: raphe straight, sternum broadly elliptical like the SV. Transapical striae in the margins radiate towards the apices.

Remarks: The local specimens are smaller than the dimensions reported in referred literatures. Though the fine morphology of the three taxa seen with SEM differs, Cocconeis pelta is similar to C. peltoides Hustedt and C. fluminensis H. Peragallo & M. Peragallo in the morphology of SV under LM. Commonly, the three species have longitudinal costae in the median area of the SV, but the first species is distinguished from the second and the third taxon in that there is no striae in the inside of the longitudinal costae ( Sar et al. 2003). The first species has a similar stria density with the second, while it is distinguished from the higher density than the third.

This species has been reported from the western Baltic Sea ( Witkowski et al. 2000), European coasts in the North Atlantic and the Patagonian coasts of Argentina ( Sar et al. 2003). In South Korea, this taxon was reported firstly as the epipsammic from the Nakdong River estuary ( Joh 2012), and in this survey, very rare in small rock pools (St. 2) and salt marshes (St. 4) of the Seogwipo coast.

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