Rhoicosphenia kloseri E.W. Thomas & R. Ligowski, 2016
publication ID |
https://doi.org/ 10.11646/phytotaxa.265.1.4 |
DOI |
https://doi.org/10.5281/zenodo.13670638 |
persistent identifier |
https://treatment.plazi.org/id/039BB059-E605-9B16-FF0E-FA80FF374C9B |
treatment provided by |
Felipe |
scientific name |
Rhoicosphenia kloseri E.W. Thomas & R. Ligowski |
status |
sp. nov. |
Rhoicosphenia kloseri E.W. Thomas & R. Ligowski , sp. nov. ( Figs 1–104 View FIGURES 1–8 View FIGURES 9–34 View FIGURES 35–60 View FIGURES 61–66 View FIGURES 67–84 View FIGURES 85–104 )
Frustules flexed in girdle view. Valves isopolar in valve view, linear with rounded apices, 9–27 μm long, 2.7–3.8 μm wide. Frustules heterovalvate, one valve concave with long raphe branches (R-valve), one valve convex with shortened raphe branches (D-valve). R-valve raphe straight, proximal raphe ends expanded externally, distal raphe ends curved in same direction externally, ending in helictoglossae internally. Axial area narrow, central area expanded laterally to margins. Striae strongly radiate at center of the valve and radiate throughout, 11–13 in 10 μm, composed of round areolae, 20 in 10 μm. D-valve raphe 1.0–2.5 μm long at each pole, external proximal ends straight, not inflated externally, external distal ends straight, terminating in helictoglossae internally. Striae parallel throughout, 9–13 in 10 μm, composed of round areolae, 20 in 10 μm. Both valves with short pseudoseptum at each apex. R-valve with condensed areolae at each pole, 3 per 1 μm. LM observations, living cells ( Figs 1–2 View FIGURES 1–8 ): in unprepared slides, the living cells detached from the substrate are commonly visible in girdle view. Cells contain one lobed chloroplast. Cleaned frustules ( Figs 3–60 View FIGURES 1–8 View FIGURES 9–34 View FIGURES 35–60 ), girdle view ( Figs 3–8 View FIGURES 1–8 ): frustules are bent and very slightly wedge shaped. Bending is uniform and has the shape of the arc of a circle. Polar pseudosepta stretch up to 1/4 on the concave valve length and usually up to 1/5 of on the convex dorsal valve. One row of pores (14 – 17 in 10 μm) is present on the epicingulum and hypocingulum. Concave (R-valve) ( Figs 9–34 View FIGURES 9–34 ): valve shape differs as the length of the valve increases. Striae close to the central area are irregular and less dense than striae close to the poles. In the central area of the valve there usually are no striae. However, on some valves longer than 20 μm, striae are present in the central area ( Figs 25, 26, 28, 31, 33, 34 View FIGURES 9–34 ). Convex valve (D-valve) ( Figs 35–60 View FIGURES 35–60 ): axial area very narrow. Striae can be irregular both in the middle of valve ( Figs 36, 40, 41, 43, 44, 52 View FIGURES 35–60 ) and near the central raphe ending ( Figs 39, 43, 53, 54, 57 View FIGURES 35–60 ). SEM observations, girdle view Figs 61–66 View FIGURES 61–66 : at the poles of both valves the striae are more closely spaced than in the central part of the valves. The row of pores on the cingulum on concave valve is more or less straight and the pores at the poles are elongated, whereas the row of pores on the cingulum at the R-valve is curved, and the pores at the poles are also elongated. On frustules of different length, the number of more closely spaced striae at the poles is more or less equal (5–6), while the number of remaining striae vary from 3 ( Fig. 61 View FIGURES 61–66 ) to 15 ( Fig. 65 View FIGURES 61–66 ). Concave valve, external view ( Figs 67–77 View FIGURES 67–84 ): the striae are radiate along the valve forming a narrow axial area. Striae are composed of round areolae; there is only one row of areolae along the axial area and they are elongated. The raphe slits terminate in the central area as drop shaped pores. As the raphe approaches the apices, it bends and then another small branch abruptly hooks back towards the center of the valve. The central area is expanded to the valve mantle with the exception of larger cells, in which shorter striae are located in the central area ( Figs 73, 74, 76 View FIGURES 67–84 ). Concave valve, internal view ( Figs 78–84 View FIGURES 67–84 ): arms of the slits are located asymmetrically. The internal central raphe endings are hooked in the same direction. Convex valve, external view ( Figs 85–94 View FIGURES 85–104 ): axial area is narrow. Striae are parallel and irregular over the length of the valve. The central raphe endings are drop shaped. The raphe slits end at the poles in a curved terminal fissure. Convex valve, internal view ( Figs 95–104 View FIGURES 85–104 ): proximal raphe endings are hooked in the same direction. One valve was found without a pseudoseptum ( Figs 102–104 View FIGURES 85–104 ) which allows for the documentation of the raphe terminating in helictoglossae.
Type:— SOUTH SHETLAND ISLANDS. King George Island: Potter Cove (62.14 o S, 58.46 o W), epiphytic on G. confluens . Sample BRM R 1272 (holotype: BRM! Zu10/68, illustrated in Fig. 29 View FIGURES 9–34 ).
Etymology:— Named in honor of Dr. Heinz Klöser, naturalist, ecologist, marine diatomist, and friend.
Taxonomic remarks and differential diagnosis:— Rhoicosphenia kloseri is most easily distinguished from the other isopolar Rhoicosphenia by its narrow valves, 2.7–3.8 μm in width. At its longest, R. kloseri that we observed and documented are 27 μm with a width of 3.8 μm. At its smallest, the type of R. adolfii is 21 μm with a width of 4.5 μm. This means that the smallest R. adolfii is wider than R. kloseri of comparable size, a key feature in demonstrating how narrow the valves of R. kloseri are when compared to other isopolar Rhoicosphenia . A comparison of the morphometric features of R. kloseri to the other isopolar Rhoicosphenia taxa, R. genuflexa , R. adolfii , and R. pullus , is presented in Table 1.
Distribution:— Known from various localities in the South Shetland Islands from epiphytes on Georgiella confluens . Rhoicosphenia kloseri is found also on the seabed in shallow sublittoral at depths ranging from 2 to 25 meters.
BRM |
Alfred-Wegener-Institut für Polar- und Meeresforschung |
R |
Departamento de Geologia, Universidad de Chile |
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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