Neidium fogedii Bahls, 2013
publication ID |
https://doi.org/ 10.11646/phytotaxa.82.1.2 |
persistent identifier |
https://treatment.plazi.org/id/03F2878E-FFC8-F86D-46F6-FF0C639FFCDD |
treatment provided by |
Felipe |
scientific name |
Neidium fogedii Bahls |
status |
stat. nov., nom. nov. |
Neidium fogedii Bahls , stat. nov., nom. nov. ( Figs 60–65 View FIGURES 52–68 )
Replaced Synonym: — Neidium kozlowi var. densestriata Foged (1981: 135 , pl. XXV, fig. 11).
Holotype: —USA, Alaska: Brooks Range , Desperation Lake, freshwater, 68.3333 o N, 158.7500 o W, coll. C. Holmquist, 30 July 1969. Slide No. 13/1969, Foged Collection, Natural History Museum of Denmark (C), Copenhagen. GoogleMaps
Vouchers: — USA, Colorado: Gunnison County, Mexican Cut Preserve, Upper Pond #56, 39.0247 o N, 107.0675 o W, elev. 3458 m, coll. M. Penton, 7 July 2012. MDC sample 494301; MDC slides 41-40 ( Figs 60- 65 View FIGURES 52–68 ), 124-34. MONTU GoogleMaps !
Etymology:—This species is named after Niels Foged. The new name is necessary because the name N. densestriatum is already occupied.
Observations:— Foged (1981) described valves of this taxon as 37 µm long by 9 µm wide with 18–20 striae in 10 µm. Specimens recently collected from a pond in Colorado ( Figs 60–65 View FIGURES 52–68 ) are 33–55 µm long by 9.3–11.1 µm wide with 17–18 striae in 10 µm. Neidium fogedii has a higher stria density and narrower central area than Neidium inconstans ( Figs 52–55 View FIGURES 52–68 ).
Distribution and Ecology: —To date this taxon has been collected only from the type locality and from a high elevation pond in Colorado. It appears to be a North American endemic. The type locality registered a pH of 7.3 and specific conductance of 27 µS/cm ( Foged 1981). The pond in Colorado had a pH of 7.2 and specific conductance of 102 µS/cm (M. Penton, unpublished data).
MONTU |
University of Montana |
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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