Orthoseira variabilis Cefarelli, Guerrero & Vouilloud

Cefarelli, Adrián O., Guerrero, José M., Quartino, Liliana, Campana, Gabriela & Vouilloud, Amelia A., 2024, Orthoseira variabilis sp. nov., a new diatom from a snow patch in Potter Cove, King George Island, Antarctica, Phytotaxa 655 (1), pp. 37-53 : 39-47

publication ID

https://doi.org/ 10.11646/phytotaxa.655.1.3

DOI

https://doi.org/10.5281/zenodo.13557121

persistent identifier

https://treatment.plazi.org/id/FA39DB3E-FFFB-FFA8-ECFE-0D12FDE1FE38

treatment provided by

Felipe

scientific name

Orthoseira variabilis Cefarelli, Guerrero & Vouilloud
status

sp. nov.

Orthoseira variabilis Cefarelli, Guerrero & Vouilloud sp. nov. Figs 2–94 View FIGURES 2–14 View FIGURES 15–48 View FIGURES 49–60 View FIGURES 61–65 View FIGURES 66–78 View FIGURES 79–84 View FIGURES 85–94

Description

LM ( Figs 2–48 View FIGURES 2–14 View FIGURES 15–48 ): Frustules cylindrical in girdle view ( Figs 2–14 View FIGURES 2–14 ). Valve face flat to slightly convex, gently curving to the mantle, sometimes exhibiting both states in valves of the same frustule ( Fig. 7 View FIGURES 2–14 ). Valve mantle with a step visible in some specimens ( Figs 6, 7 View FIGURES 2–14 ). Mantle striae in parallel rows, sometimes dichotomise, continuous beyond the step up to a distinct, hyaline collum ( Figs 8, 9, 12, 14 View FIGURES 2–14 ). Girdle bands ornamented with large poroids, arranged in one row or more scattered, in irregular rows ( Figs 3, 5, 9, 11–14 View FIGURES 2–14 ). Valves disc-shaped, usually with scalloped outline when focused on the valve interior ( Figs 18, 23–30, 46–48 View FIGURES 15–48 ). Central area hyaline and small, occupying approximately ⅕ to ¼ of the total valve diameter, irregularly shaped, with 3–4 carinoportulae. Valve face striae radiating out of central area, uniseriate in the middle and becoming branched near the margin, interspersed with shorter striae that arise distant from central area. Striae composed of conspicuous, round areolae ( Figs 15–20, 22–45, 47, 48 View FIGURES 15–48 ). Marginal spines irregularly placed, present only in a few specimens ( Figs 14 View FIGURES 2–14 , 47, 48 View FIGURES 15–48 ).

SEM ( Figs 49–84 View FIGURES 49–60 View FIGURES 61–65 View FIGURES 66–78 View FIGURES 79–84 ): Externally , valve face varying from almost flat to convex ( Figs 49–54 View FIGURES 49–60 ). Carinoportulae opening surrounded by raised rims forming incomplete semicircular collars ( Figs 55, 56 View FIGURES 49–60 ). Central area ornamented with irregular silica ridges located between the carinoportulae ( Fig. 56 View FIGURES 49–60 ). Valve face striae extending to the valve face/mantle junction ( Figs 51 View FIGURES 49–60 , 61, 65 View FIGURES 61–65 ). Areola openings surrounded by distinct rims, irregularly silicified and with small spinules ( Figs 56, 57 View FIGURES 49–60 ) or forming a complete ring ( Fig. 58 View FIGURES 49–60 ), sometimes both types of areolae occurring in the same valve. When present, spines simple, solid, conical and stellate at the base ( Figs 59, 60 View FIGURES 49–60 ). Areolae more densely packed forming a sort of pore field at the valve face/mantle junction in most valves; at intervals, beneath the pore fields, mantle striae often bifurcated ( Figs 61, 65 View FIGURES 61–65 ). On the mantle portion between the step and the collum, interstriae raised and areola openings between them round to apically elongated and without raised margins ( Figs 61, 62, 64, 65 View FIGURES 61–65 ). Collum without perforations, in some specimens separated from the striated area by a circumferential smooth area ( Figs 61, 64 View FIGURES 61–65 ).

Internally, valve face flat to slightly rounded towards the mantle. Shallow caverns at the valve face/mantle junction, in number of 5 to 8 per valve ( Figs 66–70, 72 View FIGURES 66–78 ). In the areas between caverns interstriae distinctly raised and continuous from valve face to mantle ( Figs 68, 78 View FIGURES 66–78 ). Caverns rather inconspicuous in some specimens ( Fig. 71 View FIGURES 66–78 ). Carinoportula openings circular in outline, surrounded by an area of granular appearance and occluded by a silica covering ( Figs 73, 74, 77 View FIGURES 66–78 ); a rosette-like occlusion visible when the covering is detached ( Figs 73, 74 View FIGURES 66–78 ). Etched slits between the carinoportulae visible ( Figs 73, 74 View FIGURES 66–78 ), although very faintly delineated in some specimens ( Fig. 75 View FIGURES 66–78 ). Areolae occluded by stellate vela ( Figs 75, 77 View FIGURES 66–78 ), except at caverns where no areola occlusion is visible ( Figs 76, 77 View FIGURES 66–78 ). Smaller, unoccluded perforations are scattered among areola openings ( Figs 75–78 View FIGURES 66–78 ).

Cingulum consisting of at least four open and fimbriate copulae ( Figs 63, 65 View FIGURES 61–65 , 84 View FIGURES 79–84 ). Valvocopula with a thickened pars interior ( Figs 79–81 View FIGURES 79–84 ), a row of axially elongated large poroids on its advalvar margin and irregular rows of small poroids in its middle part ( Figs 62–65 View FIGURES 61–65 , 80, 81 View FIGURES 79–84 ). The rest of the copulae ligulate ( Figs 62–65 View FIGURES 61–65 , 82, 83 View FIGURES 79–84 ), with a row of small poroids in the advalvar margin and poroids scattered or arranged in somewhat irregular rows perpendicular to pervalvar axis.

Morphometric data:

Valve diameter: 11.0–36.5 μm (x = 20.0 μm, n = 154). Valve stria density: 16–24 in 10 µm (x = 19, n = 119). Valve areola density: 15–23 in 10 µm (x = 18.5, n = 100). Mantle height: 7.5–15.5 μm (x = 11.0 μm, n = 31). Mantle stria density: 18–27 in 10 µm (x = 23.5, n = 68). Mantle areola density: 20–31 in 10 µm (x = 22.5, n = 51). Valvocopula exterior width: x = 5.10 µm (n = 22). Density of valvocopula elongated poroid: 13–18 in 10 µm (x = 15.5, n = 31).

Type: — ANTARCTICA, King George Island/Isla 25 de Mayo , Potter Cove coast (62.2464° S, 58.6796° W), snow patch. LPC 13325 , February 15, 2017. (Holotype designated here, specimen positioned in England Finder D39/3, slide 13325(1)!, illustrated in Figs 24, 25 View FIGURES 15–48 ). GoogleMaps

Etymology: The specific epithet “ variabilis ” refers to the high variability in several morphological features exhibited by the new species.

Ecology and associated diatom flora: Orthoseira variabilis was found in dusty snow and associated with mosses in a circumscribed coastal area. The accompanying flora is mostly composed of taxa usually living in aerophilic environments such as several species of Chamaepinnularia Lange-Bertalot & Krammer (in Lange-Bertalot & Metzeltin 1996: 32), Humidophila (Lange-Bertalot & Werum) R.L. Lowe & al. (2014: 352) , Luticola D.G.Mann (in Round et al. 1990: 670), together with Hantzschia amphioxys (Ehrenberg) Grunow (in Cleve & Grunow 1880: 103) and Pinnularia borealis Ehrenberg (1843: 420) , among others. Marine diatom species such as Fragilariopsis curta (Van Heurck) Hustedt (1958: 160) , F. cylindrus (Grunow ex Cleve) Helmcke & Krieger (1954: 17) , Pseudogomphonema kamtschaticum (Grunow) Medlin (in Medlin & Round 1986: 216), Shionodiscus gracilis (Karsten) Alverson, Kang & Theriot (2006: 259) and S. gracilis var. expectus (VanLandingham) Alverson, Kang & Theriot (2006: 259) were also observed denoting a marine influence presumably through wind and sea spray aerosol.

Remarks: Some specimens exhibited on their valve faces patches of smooth areas ( Figs 52, 58 View FIGURES 49–60 ) that were interpreted as two layers of silica deposition, the upper one being responsible for the spiny rims and rings that surround the external areola openings.

Some initial valves and initial cells were observed ( Figs 85–94 View FIGURES 85–94 ), with clearly convex valve face ( Figs 85–87 View FIGURES 85–94 ), more irregularly arranged striae composed of rimmed areolae, an irregularly-shaped, somewhat bilobate central area, and numerous (up to eight) carinoportulae with incompletely developed collar ( Figs 88–94 View FIGURES 85–94 ). Crawford (1981) described initial valves as structurally similar to vegetative valves except that they are hemispherical in shape, without distinction between valve face and mantle, and lack spines. He illustrated in his figs 52-55 initial valves of Orthoseira sp. that also exhibit a central area with two groups of carinoportulae. Similarly, Roemer & Rosowski (1980) documented hemispherical initial valves of Orthoseira (= Melosira ) roeseana with multiple (4–10) carinoportulae which are reduced to 3–4 in vegetative valves.

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