Stauroneis thompsonii Bahls, 2012
publication ID |
https://doi.org/ 10.11646/phytotaxa.67.1.1 |
DOI |
https://doi.org/10.5281/zenodo.5067408 |
persistent identifier |
https://treatment.plazi.org/id/F67E504B-1168-F12C-4B8E-71F0FE2DFE8F |
treatment provided by |
Felipe |
scientific name |
Stauroneis thompsonii Bahls |
status |
sp. nov. |
Stauroneis thompsonii Bahls , sp. nov. ( Figs 22–24 View FIGURES 9–24 )
Type: — USA. Montana: Upper Wolverine Lake ( Fig. 25 View FIGURE 25 ), Ten Lakes Scenic Area , Kootenai National Forest , Lincoln County, 48.9705 o N, 114.9221 o W, 1890 m elevation, collected from rocks and sediment by Loren Bahls, 9 September 1990. MDC sample 108601 GoogleMaps ; holotype slide MDC P3-3-1, Figs 22–24 View FIGURES 9–24 .
Valves lanceolate with rounded, unprotracted apices. A deep pseudoseptum occupies each apex ( Fig. 24 View FIGURES 9–24 ). Valve length 88–105 µm; valve width 16.3–17.5 µm. Raphe lateral with straight proximal ends, slightly inflated. Distal raphe ends hooked to same side. Axial area narrowly lanceolate, widens gradually towards central area. Central stauros nearly rectangular and placed somewhat diagonally to apical axis. Striae radiate throughout, 17–18 in 10µm. Areolae in striae 12–15 in 10 µm.
Etymology:— Stauroneis thompsonii is named for David Thompson (1770–1857), an early 19 th Century Montana explorer and cartographer ( Jenish 2003).
Observations: — Stauroneis thompsonii was reported by Bahls (2010: 61) as S. aff. catharinae Van de Vijver & Lange-Bertalot (2004: 27) . However, it has significantly wider valves and lower stria and areola densities than S. catharinae . It is known only from the type locality, a small lake in the Galton Range in northwest Montana ( Fig. 25 View FIGURE 25 ).
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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