Orthoseira johansenii R.L.Lowe & Kociolek, 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 : 46-48

publication ID

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

DOI

https://doi.org/10.5281/zenodo.5078793

persistent identifier

https://treatment.plazi.org/id/820B746D-FF9A-FF9A-B4FF-F9B35DB9FB86

treatment provided by

Felipe

scientific name

Orthoseira johansenii R.L.Lowe & Kociolek
status

sp. nov.

Orthoseira johansenii R.L.Lowe & Kociolek sp. nov. ( Figs 34–52 View FIGURES 34–41 View FIGURES 42–47 View FIGURES 48–52 )

Frustules cylindrical in girdle view, usually occurring singly or in short chains of 2–4 cells. Valves disc-shaped, 24–65 µm in diameter, mantle 11–13 µm deep. Valve surface flat, forming a nearly right angle with the mantle. Mantle striae uniseriate, 18–21/ 10 µm. Areolae on the valve face small, round, irregularly-scattered and rarely forming straight continuous striae restricted to the outer 2/3 of the valve face with the remaining surface forming an hyaline area pitted and containing carinoportulae. Carinoportulae relatively large, numbering 1–3. Marginal spines are usually straight but can but forked. Spines number 2–4/ 10 µm. No caverns or internal undulations present. Internal valves wanting. Copulae open, numbering 5–7/cell.

Type: — Pua Po’o lave tube, Volcanoes National Park, Hawai’i, slide no. BISH-755092 (Holotype, Bishop Museum of Natural History, Honolulu ), ANSP-20040 ( Isotype Academy of Natural Sciences , JPK-COLO 4195 ( Isotype Kociolek Collection , University of Colorado, Boulder ).

Etymology:— the specific epithet johansenii refers to our friend and colleague Dr. Jeffrey Johansen, John Carroll University (Cleveland, USA).

Observations:— In the SEM, the valve face is flat ( Fig. 42 View FIGURES 42–47 ) to weakly domed/concave ( Fig. 43 View FIGURES 42–47 ). Hyaline central area smooth ( Figs 42, 43 View FIGURES 42–47 ) and may be reduced due to irregularly-placed areolae ( Fig. 42 View FIGURES 42–47 ). Areolae in defined striae near the margin becoming irregularly spaced towards the valve centre ( Figs 42, 45 View FIGURES 42–47 ), small and poroid, sometimes surrounded by a slightly raised rim ( Figs 44, 45 View FIGURES 42–47 ). No difference in areolae structure or size between valve face and mantle ( Fig. 42 View FIGURES 42–47 ). Areolae on the mantle always arranged in parallel striae ( Figs 45, 46 View FIGURES 42–47 ). External marginal pore fields between spines absent ( Fig. 45 View FIGURES 42–47 ). Carinoportulae distinct in the central area, often surrounded by raised rosettes or fine ridges ( Fig. 44 View FIGURES 42–47 ), each with a pronounced (sometimes even conical) silica collar ( Fig. 44 View FIGURES 42–47 ). Valve face/mantle junction abrupt with rounded edge ( Fig. 45 View FIGURES 42–47 ). Ring of large linking spines may be present ( Figs 45, 46 View FIGURES 42–47 ), but in this species more frequently encountered are stout siliceous thickenings ( Figs 45, 46 View FIGURES 42–47 ). Linked spines plate-like, bifurcated or with a quite complex shape ( Figs 45, 46 View FIGURES 42–47 ). On the mantle small, irregular thickenings visible between the areolae ( Fig. 45 View FIGURES 42–47 ). Internally, valve face flat, smooth ( Figs 48, 49 View FIGURES 48–52 ). Areolae appearing as small rounded poroids ( Fig. 48 View FIGURES 48–52 ), with a velum ( Figs 50, 51 View FIGURES 48–52 ). Carinoportulae unoccluded, with small, simple and rounded internal openings ( Figs48, 49, 52 View FIGURES 48–52 ). No other processes are present on the valve interior. Copulae open, with very small poroids scattered or organized into one straight row and others scattered, parallel to the pervalvar axis ( Figs 47 View FIGURES 42–47 ). Sometimes copulae ornamentation is but a few poroids ( Fig. 47 View FIGURES 42–47 ).

Ecology:— The internal surface of this lava tube was damp, with soil, bryophytes and exposed lava representing the primary microhabitats. Present along with O. johansenii were Nupela sp. , Melosira sp. Kobayasiella sp. Diadesmis biceps G.A.Arnott ex Grunow in Van Heurck 1880: 14 /31b, Nitzschia hantzschiana Rabenh. (1860: 40) and Pinnularia divergentissima (Grunow in Van Heurck 1880: 6 /32) Cleve 1895: 77. Of these diatoms, O. johansenii was the least abundant taxon.

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