Orthoseira verleyenii Van de Vijver, 2013

Lowe, Rex L., Kociolek, J. Patrick & Vijver, Bart Van De, 2013, Two new Orthoseira species (Bacillariophyceae) from lava tubes on Île Amsterdam and Big Island (Hawai ΄ i), Phytotaxa 111 (1), pp. 39-52 : 41-44

publication ID

https://doi.org/ 10.11646/phytotaxa.111.1.3

DOI

https://doi.org/10.5281/zenodo.5078789

persistent identifier

https://treatment.plazi.org/id/820B746D-FF9F-FF96-B4FF-F9ED5B09FE7D

treatment provided by

Felipe

scientific name

Orthoseira verleyenii Van de Vijver
status

sp. nov.

Orthoseira verleyenii Van de Vijver sp. nov. ( Figs 1–33 View FIGURES 1–5 View FIGURES 6–15 View FIGURES 16–22 View FIGURES 23–27 View FIGURES 28–33 )

Cells cylindrical forming long chains. Frustules in girdle view 45–95 µm long. Diameter 17–70 µm. Mantle height 15–25 µm. Central area forming a small hyaline zone (max. 1/3 of the total valve diameter). Marginal spines bifurcating, irregularly positioned on the valve face/mantle margin. Areolae on the valve face dispersed or arranged in radiate striae, 15–18 in 10 µm. On the mantle, striae parallel, distinctly areolated, 19–25 in 10 µm. Carinoportulae 1–6, usually 2.

Type: — Île Amsterdam, Grand Tunnel, sample AMS-W33 (37°48’47.1”S, 77°33’42.6” E, Leg. B. Van de Vijver , coll. date 04/12/2007), slide no. BR-4309 (holotype BR), slide PLP-224 (isotype University of Antwerp, Belgium) GoogleMaps .

Etymology: —The specific epithet verleyenii refers to my colleague and friend Dr. Elie Verleyen (University of Ghent, Belgium) in recognition of his important contribution to the (paleo-) ecology and biodiversity of Antarctic algae.

Observations:—LM ( Figs 1–15 View FIGURES 1–5 View FIGURES 6–15 ): Cells cylindrical in girdle view ( Figs 1–2 View FIGURES 1–5 ), attached with linking spines ( Figs 3–5 View FIGURES 1–5 ), usually forming large chains, up to 8–10 valves. Cells 45–95 µm, mantle height ca. 15–25 µm. Valves disc-shaped ( Figs 6–9 View FIGURES 6–15 ), diameter 17–70 µm. Valve surface flat, forming a right angle with valve mantle. Striae on the mantle composed of uniseriate areolae, 19–25 in 10 µm. Valve face areolae small, radiate, irregularly scattered, rarely forming continuous series, occupying almost 2/3 of the total valve face surface, with remaining surface forming an irregular, small central hyaline area. Towards the valve centre, areolae more scattered, 15–18 areolae in 10 µm, irrespective of valve size. Central area with 1–6 carinoportulae ( Figs 10–15 View FIGURES 6–15 ) (for 100 valves, 48 % with only two, 23 % with three, 24 % with four and only 1–3% with one, five or six carinoportulae). No relationship noted between number of carinoportulae and valve diameter. Distinct ring of marginal linking spines at the valve face/mantle junction. No caverns or internal undulations present. Internal valves absent. Copulae number variable, between 5-7. ( Figs 1–2 View FIGURES 1–5 ). SEM ( Figs 16–33 View FIGURES 16–22 View FIGURES 23–27 View FIGURES 28–33 ): Valve face flat ( Figs 16, 19 View FIGURES 16–22 ) to weakly domed ( Fig. 17 View FIGURES 16–22 ). Hyaline central area smooth ( Figs 16, 18 View FIGURES 16–22 ) or even absent due to irregular scattering of areolae ( Fig. 17 View FIGURES 16–22 ). Areolae irregularly placed ( Figs 17, 19 View FIGURES 16–22 ) or in radiating series ( Fig. 16 View FIGURES 16–22 ), small and poroid, sometimes surrounded by a slightly raised rim ( Fig. 18 View FIGURES 16–22 ). No difference in areolae structure or size between valve face and mantle ( Figs 16, 18 View FIGURES 16–22 ). Areolae on the mantle always arranged in parallel striae. External marginal pore fields between spines absent ( Figs 16–18 View FIGURES 16–22 ). Carinoportulae well distinguishable in the central area, often surrounded by slightly raised, fine ridges ( Figs 18–21 View FIGURES 16–22 ), each with a double, pronounced (sometimes even conical) silica collar ( Figs 20–22 View FIGURES 16–22 ). Valve face/mantle junction abrupt with rounded edge ( Fig. 18 View FIGURES 16–22 ). Ring of large linking spines present ( Figs 16–19 View FIGURES 16–22 , 30–33 View FIGURES 28–33 ), regularly scattered along the entire valve edge. Spines either simple siliceous thickenings ( Figs 18–19 View FIGURES 16–22 ) or plate-like structures extending from the mantle ( Figs 17 View FIGURES 16–22 , 30–31 View FIGURES 28–33 ). Linked spines plate-like, bifurcated ( Fig. 17 View FIGURES 16–22 ) or with quite complex shape ( Fig. 31 View FIGURES 28–33 ). On the mantle small, irregular thickenings visible between the areolae ( Figs 32–33 View FIGURES 28–33 ). Some valves possessing a regular thickened line going around the entire valve ( Fig. 32 View FIGURES 28–33 ). Internally, valve face flat, smooth ( Figs 23–24 View FIGURES 23–27 ). Areolae appearing as small rounded poroids ( Figs 23–24 View FIGURES 23–27 ), without a velum ( Fig. 24 View FIGURES 23–27 ). Near the mantle, areolae organised in sometimes dichotomised rows with occasional short rows of areolae inserted between regular rows ( Fig. 24 View FIGURES 23–27 ). Lower part of the valve mantle near the cingulum without areolae, forming a hyaline zone ( Fig. 24 View FIGURES 23–27 ). Carinoportulae unoccluded, with small, simple rounded to slit-like external pits in comparison to the larger internal openings ( Figs. 25–27 View FIGURES 23–27 ). Inside small granules sometimes present ( Fig. 25 View FIGURES 23–27 ). Central to the carinoportulae, irregular slits usually present ( Figs 25–26 View FIGURES 23–27 ) though sometimes absent ( Fig. 27 View FIGURES 23–27 ).

Copulae open, with very small poroids scattered or organized into rows parallel to the pervalvar axis ( Figs 28-29 View FIGURES 28–33 ). Sometimes copulae unornamented ( Fig. 30 View FIGURES 28–33 ).

Ecology: — So far, Orthoseira verleyenii has only been found in lava tube samples on Ile Amsterdam ( southern Indian Ocean ). At the type locality, the species is not rare, occurring with a relative abundance of more than 5 %. Due to their large size, specimens were easily observed. The type locality is a small puddle in a cave that is part of a collapsed lava tunnel running from the lower Venus Crater towards the coast at an altitude of 220 m. The puddle is fed by water dripping from the ceiling of the cave. The bottom of the cave, surrounding the puddle is covered by mosses and liverworts. PH of the puddle was 5.8 with a specific conductance value of 239 µS/cm. No macro-vegetation was observed in the puddle .

Apart from Orthoseira verleyenii , the sample is dominated by Planothidium lanceolatum (Brébisson ex Kützing 1846: 247) Lange-Bertalot (1999: 287) , Karayevia oblongella ( Østrup 1902: 252) Aboal in Aboal, Alvarez-Cobelas, Cambra & Ector (2003: 159), Diadesmis crozetikerguelensis Le Cohu & Van de Vijver (2002: 124) , Eunotia muscicola Krasske (1939: 366) var. muscicola and an unidentified Melosira species.

BR

Embrapa Agrobiology Diazothrophic Microbial Culture Collection

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