Pseudostaurosira cf. brevistriata (Grunow) Williams & Round,
publication ID |
https://doi.org/10.21826/2446-82312021v76e2021012 |
DOI |
https://doi.org/10.5281/zenodo.16415919 |
persistent identifier |
https://treatment.plazi.org/id/602387C1-FF9F-7B69-DF7A-0610FEC574E2 |
treatment provided by |
Felipe |
scientific name |
Pseudostaurosira cf. brevistriata (Grunow) Williams & Round, |
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Pseudostaurosira cf. brevistriata (Grunow) Williams & Round,
Diatom Res., 2: 276, figs. 28-31. 1988.
( Figs. 24-27 View Figure 2-40 )
Valves are lanceolate in larger specimens to elliptical in smaller specimens. Rostrate ends to rounded ends in smaller specimens. Presence of a broad lanceolate axial area and short striae found near the edge of the valve. Striae parallel to radiate in the central of the valve to slightly radiate toward the valve ends. Length: 6.2-19 μm; width: 2.9-4.3 μm; striae 12-16 in 10 μm. This taxon differs from other Pseudostaurosira Williams & Round and Staurosirella Williams & Round species by the presence of delicate and shortened marginal striae. The specimens observed are similar to those registered by Brassac et al. (2003) and Taylor et al. (2007). The study specimens are similar to the Staurosirella krammeri Morales, Chávez & Ector and Pseudostaurosira sajamaensis Morales & Ector ; however, P. brevistriata differs concerning the length and shape valve ( Morales et al. 2010, 2012). For a clear separation of these taxa, an ultra-structural analysis is required.
Material examined: BRAZIL, MATO GROSSO DO SUL: Batayporã, Garças Lake , 21.IX.2017, sediment, D.T. Ruwer (Nupélia UEM - 18071-72 , 18074 , 18076 , 18084- 97 ); Taquaruçú, Patos Lake , 23.III.2018, sediment, D.T. Ruwer (Nupélia UEM - 18119 ).
Occurrence: first citation for Upper Paraná River floodplain.
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