Pinnularia valdecontroversa, Bąk & Kociolek & Lange-Bertalot & Łopato & Witkowski & Zgłobicka & Seddon, 2017
publication ID |
https://doi.org/ 10.11646/phytotaxa.311.3.1 |
DOI |
https://doi.org/10.5281/zenodo.13701745 |
persistent identifier |
https://treatment.plazi.org/id/03F3527E-FFCA-FE35-FF66-5FD5FD93FE80 |
treatment provided by |
Felipe |
scientific name |
Pinnularia valdecontroversa |
status |
sp. nov. |
Pinnularia valdecontroversa sp. nov. Lange-Bertalot, Witkowski & Bąk
Figs 157–179 View FIGURES 157–167 View FIGURES 168–173 View FIGURES 174–179
Description: —Light microscopy—Valves linear, smallest becoming weakly lanceolate. Ends variable, not protracted at all to broadly and shortly protracted with more or less bluntly rounded poles. Length 40–56 μm, breadth 7–10 μm (n=20). External raphe fissures slightly wavy ( Fig. 168 View FIGURES 168–173 —arrow) and lateral to the internal fissures. Axial area narrow, linear. Central area forming broad fascia. Striae 8–9 in 10 μm, radiate in proximal part of valve, rather strongly pronounced in broader specimens. Striae in distal part of valve becoming strongly convergent, but not different in density.
Scanning electron microscopy:—External view ( Figs 168-173 View FIGURES 168–173 ). Longitudinal bands marking the border between open and closed parts of alveoli absent. Valves asymmetrical about transapical axis because of terminal raphe fissures and length and density of distal, convergent striae. Proximal ends of raphe weakly expanded ( Fig. 168 View FIGURES 168–173 —arrowhead), neither conspicuously deflected to one side. Terminal fissures indistinctly curved and sickle-shaped ( Fig. 169 View FIGURES 168–173 —arrow), curve to opposite sides at both poles onto valve mantle ( Figs 169, 170 View FIGURES 168–173 —arrows). Subdistal striae—each one consisting of quadri- to pentaseriate areolae—become gradually shorter at one side, and become circumradiate around valve poles. On opposite side, areolae become longer and remarkably more wavy, and finally broader near axial area. Open alveola covered with porous membranes ( Fig. 173 View FIGURES 168–173 , 176 View FIGURES 174–179 —arrows). Discontinuity evident between subdistal and circumpolar striae forming gap ( Fig. 171 View FIGURES 168–173 —arrow). External raphe slit gently undulate, becoming moderately wider towards unilaterally deflected central pores. Internally, raphe fissure with intermissio at central nodule, with proximal raphe ends small, slit-shaped, bent in same direction ( Fig. 175 View FIGURES 174–179 —arrows). Internally distal raphe ends terminate with small helictoglossae ( Fig. 179 View FIGURES 174–179 —arrow).
Type: — ECUADOR. Galápagos Islands: Isabela (Albemarle) Island, Diablas wetlands, 0.95731°S, 90.98685°W, 23 July 2012, holotype (designated here):—Slide no. 20779 (species code—7877 MCCDRS) in Coll. Herbarium ( CDS) of the Charles Darwin Foundation at Galapagos, represented by Fig. 160 View FIGURES 157–167 .
Type locality: —Floating moss, at the mouth of the stream to the lagoon in the Diablas wetlands—a permanent, brackish coastal lagoon network located at sea level on the south side of Isabela Island.
Etymology: —The composite epithet in Latin means very (“valde”) and controversial (“controversus”) referring to the different structured poles of every valve.
Distribution: —As yet not observed from other regions than the type location.
Comments: —Very few Pinnularia species are characterised by asymmetry of both poles. These are Pinnularia controversa Hustedt in A. Schmidt Atlas (1934) figs 385: 16–17 from Sumatra, Indonesia. The second one is P. platycephala ( Ehrenberg 1854) P.T. Cleve (1891: 20) . Details about the distinctive characters between the three Pinnularia taxa are given in the discussion.
CDS |
Charles Darwin Research Station |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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