Halamphora submontana (Hustedt) Levkov, 2009

You, Qingmin, Kociolek, John Patrick & Wang, Quanxi, 2015, Taxonomic studies of the diatom genus Halamphora (Bacillariophyceae) from the mountainous regions of southwest China, including the description of two new species, Phytotaxa 205 (2), pp. 75-89 : 82

publication ID

https://doi.org/ 10.11646/phytotaxa.205.2.1

DOI

https://doi.org/10.5281/zenodo.13639689

persistent identifier

https://treatment.plazi.org/id/03A0F67B-F262-FF95-46AE-CDAEFE0FF7C1

treatment provided by

Felipe

scientific name

Halamphora submontana (Hustedt) Levkov
status

 

Halamphora submontana (Hustedt) Levkov ( Figs. 55–65 View FIGURES 55–65 )

Description:— Valves semi-lanceolate, dorsiventral with smoothly convex dorsal margin and slightly convex ventral margin. Valve ends protracted, narrowly rounded and deflected ventrally. Length 18.3–21.8 μm, valve breadth 3.7–4.0 μm. Externally, the raphe is weakly arched and both proximal and distal raphe ends are deflected or curved towards the dorsal margin of the valve ( Figs. 60, 62, 64 View FIGURES 55–65 ), proximal raphe ends almost not expanded ( Figs. 60, 62 View FIGURES 55–65 ). Dorsal raphe ledge present. Axial area narrow. Dorsal striae more or less interrupted in the central area ( Figs. 60, 62 View FIGURES 55–65 ). Dorsal striae beneath the raphe ledge are biseriate ( Fig. 62 View FIGURES 55–65 ). Ventral portion of the valve with a semi-elliptical central area. Striae slightly radiate throughout, 32–38/ 10 μm, difficult to resolve with LM. Internally, the proximal raphe ends terminate at a narrow central helictoglossae ( Figs. 61, 63 View FIGURES 55–65 ). Distally, internal raphe ends terminate as helictoglossae ( Fig. 65 View FIGURES 55–65 ).

Distribution and ecology:— Weixi, Yunnan, China, altitude 1929 m a.s.l., collected in mountain river.

Observations:— This species has similar valve outline with Halamphora montana and the two are difficult to distinguish in LM. Differences between them are striae density ( H. submontana has more coarse striae, 32–38/ 10 μm, while H. montana has 45–50/ 10 μm) and striae structure ( H. submontana with biseriate striae near raphe ledge, H. montana without biseriate striae). The frustules of H. submontana and H. montana are very small, and with similar outlines, so they are confused with each other. In our study, in order to avoid wrong identification, we observed the specimen in SEM first ( Fig. 74 View FIGURES 66–77 ), then examined same specimen in LM ( Fig. 70 View FIGURES 66–77 ). This method facilitates correct identification with LM.

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