Stauroneis fuegiana Casa & Van de Vijver, 2017
publication ID |
https://doi.org/ 10.11646/phytotaxa.311.1.8 |
DOI |
https://doi.org/10.5281/zenodo.13685962 |
persistent identifier |
https://treatment.plazi.org/id/03BFC161-CC72-FFB4-9BEE-F9272E9A042E |
treatment provided by |
Felipe |
scientific name |
Stauroneis fuegiana Casa & Van de Vijver |
status |
sp. nov. |
Stauroneis fuegiana Casa & Van de Vijver sp. nov. ( Figs 1–13 View FIGURES 1–7 View FIGURES 8–13 )
LM ( Figs 1–7 View FIGURES 1–7 ): Valves rather broadly lanceolate, never linear-lanceolate with clearly convex margins, gradually tapering towards the weakly protracted, subrostrate apices. Valve dimensions (n=25): length 95–165 μm, width 17– 25 μm, length/width ratio 5.7–6.3. Axial area narrow, strictly linear, almost 1/5 of the total valve width, gradually widening until the central area. Central area forming a rectangular, only weakly wedge-shapedly widened stauros. Shortened striae only rarely present in the central area. Raphe clearly lateral. Branches straight with clearly deflected to weakly hooked ( Figs 6, 7 View FIGURES 1–7 ), droplike expanded proximal raphe endings and hooked terminal raphe fissures. Striae clearly radiate throughout the entire valve, 16–18 in 10 μm. Areolae clearly discernible in LM, 18–20 in 10 μm. Occasionally, narrow hyaline line visible at the valve face/mantle junction ( Fig. 1 View FIGURES 1–7 , arrows). SEM ( Figs 8–13 View FIGURES 8–13 ): Striae uniseriate composed of transapically elongated areolae ( Figs 9, 10 View FIGURES 8–13 ). Striae continuing uninterruptedly onto the mantle ( Fig. 10 View FIGURES 8–13 ). External proximal raphe endings clearly deflected terminating in large, droplike expanded pores ( Fig. 9 View FIGURES 8–13 ). Small silica ridge bordering the raphe ( Figs 8, 9 View FIGURES 8–13 ). Terminal raphe fissures strongly hooked, continuing onto the mantle ( Fig. 10 View FIGURES 8–13 ). Narrow silica ridge present near the central area at the valve face/mantle junction, not continuing up to the apices ( Fig. 9 View FIGURES 8–13 , arrows). Internally, stauros well-developed ( Fig. 11 View FIGURES 8–13 ). Internal proximal raphe endings terminating on the stauros ( Fig. 12 View FIGURES 8–13 ). Distal raphe endings terminating on small helictoglossae ( Fig. 13 View FIGURES 8–13 ). Stria foramina transapically elongated ( Fig. 12 View FIGURES 8–13 ).
Type:—Rancho Hambre, Tierra del Fuego, ARGENTINA: sample RH-VP4- SED, V. Casa, 21/11/2016 (holotype BR! slide no. 4480, isotype PLP! slide 325, University of Antwerp, Belgium).
Ecology and distribution:— Stauroneis fuegiana is regularly observed in the peat bogs pools of Tierra del Fuego. It is possible that the species has been identified in the past as S. phoenicenteron or S. gracilis . The species is usually found in sediment and moss samples from several shallow, dystrophic, acid to slightly acid (pH 3,6–6,8) waterbodies with low conductivity (<200 μS/cm) and DOC ranging between 5,1 to 35,1 mg/l.
Etymology:—The specific epithet fuegiana refers to the type locality in Tierra del Fuego.
V |
Royal British Columbia Museum - Herbarium |
BR |
Embrapa Agrobiology Diazothrophic Microbial Culture Collection |
PLP |
Institute of Himalayan Bioresource Technology |
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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