Luticola coloradiana, Shea, Greifenstein & Kociolek, 2022

Shea, Rachel, Greifenstein, Jeremy & Kociolek, J. P., 2022, Valve Ultrastructure and Description of a new Luticola D. G. Mann (Bacillariophyceae) species from Colorado, USA, Phytotaxa 554 (3), pp. 269-277 : 270-273

publication ID

https://doi.org/ 10.11646/phytotaxa.554.3.5

DOI

https://doi.org/10.5281/zenodo.6840213

persistent identifier

https://treatment.plazi.org/id/03F3C37F-1801-F954-D5C2-FA8DFB78E510

treatment provided by

Plazi

scientific name

Luticola coloradiana, Shea, Greifenstein & Kociolek
status

sp. nov.

Luticola coloradiana, Shea, Greifenstein & Kociolek , sp. nov. ( Figs 1–19 View FIGURES 1–8 View FIGURES 9–11 View FIGURES 12–15 View FIGURES 16–19 )

Description: In LM ( Figs 1–8 View FIGURES 1–8 ) valves are rhombic-lanceolate to rhombic in smaller specimens. Valves measure 23.0– 70.0 µm in length, 11.0–18.5 µm in breadth. Raphe branches are axial, along the apical axis. Isolated stigma near center of valve. Striae radiate outwards, non-uniform in appearance, often becoming smaller close to valve margin, 10–12 in 10 µm.

In the SEM, the valve exterior has a rugose appearance, formed by thickened ridges running longitudinally along the apical axis of the valve and by areolae being located in depressions on the valve face ( Figs 9–11 View FIGURES 9–11 ). Areola density 11–14 / 10 µm. There is an elevated ridge running around the entire margin of the valve ( Fig. 11 View FIGURES 9–11 ). The axial area is straight, expanded slightly towards the central area, rectangular in shape and without areolae, only a single, small stigma opening ( Figs 9–13 View FIGURES 9–11 View FIGURES 12–15 ). The stigma opening is smaller than the areolae. The central area may also bear numerous small depressions that do not penetrate the valve ( Fig. 13 View FIGURES 12–15 ). The areolar depressions and the smaller, more shallow ones around the central area may have small granules in and around them. The raphe is straight, with proximal ends bent to one side (opposite the stigma) and distal ends bent in the same direction, opposite the direction of the proximal ends. The raphe slit is bordered by a thin rim of silica ( Figs 9–11 View FIGURES 9–11 , 12, 14 View FIGURES 12–15 ). The mantle of the valve has a row of small poroids and a row of prominent, elongated poroids ( Fig. 15 View FIGURES 12–15 ). Girdle bands number 4–5 / valve and have a single row of poroids situated towards the valve.

The valve interior has an expanded axial area that is developed into a central area formed by a stauros that extends nearly to the margin ( Figs 16, 17 View FIGURES 16–19 ). Areolae do not appear occluded internally ( Fig. 16 View FIGURES 16–19 ). Proximal raphe ends terminate at the base of the central area ( Figs 16–18 View FIGURES 16–19 ) while the distal ends terminate in small helictoglossae ( Fig. 19 View FIGURES 16–19 ). On one side of the central area is the stigma opening. The stigma opening is simple, round, with a short, thickened collar ( Figs 16–18 View FIGURES 16–19 ). Areolae are round to dash-like in shape. The valve interior, like the exterior, appears rugose ( Figs 16, 17 View FIGURES 16–19 ). Thick siliceous ribs extend from the margin, and on the valve face there is a line of thin, fimbriate siliceous structures that are aligned with the ribs ( Figs 16, 17 View FIGURES 16–19 ).

Type: — USA. Colorado, Gunnison County. Unnamed wet meadow in Gunnison County, Colorado, USA. Latitude : 38.25025126, Longitude : -107.497408. Collection was made on August 2, 2021. Holotype Slide: JPK Collection ( COLO!) 651052 Isotypes: To be deposited at Academy of Natural Sciences (Philadelphia) and the Natural History Museum (London).

Etymology: —Named for the state of Colorado in which it occurs.

Ecology: —While no other data on the physical and chemical characteristics of the collecting site were obtained, the associated diatom flora is diverse, with unnamed species of Aulacoseira Thwaites and Encyonopsis Krammer , as well as Cavinula davisiae Bahls (2013: 15) and several species of cymbelloid diatoms being present.

COLO

University of Colorado Herbarium

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