Diploneis tessellata Jovanovska & Wilson & Hamilton & Stone 2023, sp. nov.
Bibliographic record
Abstract
Diploneis tessellata sp. nov. (LM Figs 132–141, SEM Figs 142–151) Valves are weakly asymmetric, broadly elliptic with convex margins and bluntly round ends (Figs 132–143). Valve length is 29.5–60.5 μm and valve width is 18.5–33.5 μm. The axial area is narrow, lanceolate, widening at the center to form an elongate and weakly asymmetric central area (Figs 133, 145, 146), 3.5–6.5 μm wide. Externally, the canal is linear to lanceolate, slightly expanded in the middle of the valve with three rows of cribrate (<9 poroids) areolae narrowing into one at the valve apices (Figs 132–141, 146, 147). Internally, a thick non-porous slightly raised silica plate encloses the longitudinal canal (Figs 148–151). Externally, the raphe is filiform, curved with simple proximal ends deflected to one side; the proximal raphe ends are positioned within expanded teardrop depressions (Figs 145, 146). The distal raphe ends are unilaterally bent to the same side and terminate at the valve face mantle junction (Figs 142, 144). Internally, the raphe is curved with simple proximal and distal ends that are slightly elevated in a depression formed by the longitudinal canal (Figs 148–151). The striae are parallel at mid-valve becoming radiate towards the valve apices, 8–9 (mostly 8) in 10 μm. Striae are uniseriate throughout (white arrow in Fig. 142). The striae are composed of round to rectangular areolae covered externally with fine pored cribra (25–45 poroids), 8–10 in 10 μm. The inter-areolar thickenings have fin-like silica ridges that are serrated with ca. 5–7 notched edges (Fig. 146). The areolae increase in size towards the valve margins (Figs 142, 143, 147). Internally, the alveoli open via a single elongated opening covered with a thin silica layer (Figs 148, 149). The valvocopula has serrated advalvar edges (Figs 148, 150). Type:— REPUBLIC OF ZAMBIA, Lake Tanganyika, Kalambo Falls Lodge, at 770 m elevation; mud, 18 m water depth, collected SCUBA diving, 8°37’25.6” S 31°11’59.7” E, H. Büscher, 1 st September 2018 (holotype designated here, circled specimen BM-108986! = Fig. 138, isotypes ANSP-GC17215!, CANA-129336!). Type material CANA-129315. Registration: http://phycobank.org/103720 Pictures of the isolated specimen:— LM micrograph on 1000× magnification (Fig. S 3t). Sequence data:— Plastid gene rbc L sequence (GenBank accession: OQ 660296) and nuclear encoded 18S (SSU rDNA) sequence (GenBank accession: OQ 629557). Etymology:— The specific epithet ‘ tessellata ’ refers to the blocky, tiled appearance of the areolae of this species. Ecology and distribution:— This species has only been observed in Lake Tanganyika along the coasts of Zambia and Tanzania in the three sub-basins, especially in Kalambo Falls Lodge, Isanga Bay, Mutondwe Island, Kalya Bay, Rukoma area, and Kiganza Bay (see Fig. 1c–f). The species is not very abundant in the alkaline, moderately mineral-rich and highly transparent waters and occurs in sandy and muddy substrates (sometimes with mollusk shells) between 10 and 33 m water depth. It can also be found on submerged rocks in the littoral areas at Jakobsen Beach, at 5 m depth on Buhingu Island, and at 20 m depth in Isanga Bay, probably due to upwelling, currents, and/or turbidity. Diploneis tessellata sp. nov. occurs together with D. salzburgeri sp. nov., D. cristata sp. nov., D. gigantea sp. nov., D. fossa sp. nov., D. cocquytiana sp. nov., D. kilhamiana sp. nov., D. tanganyikae sp. nov., and D. serrulata sp. nov. Main differential characters:— Valve shape, striae density, areolae density, external thick fin-like ornamentations evenly distributed across the valve, and poroids 25–45 per areola. Similar species:— Diploneis tenera sp. nov., D. cristata sp. nov., and D. elliptica.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.001 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.001 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.001 | 0.001 |
| Open science | 0.000 | 0.001 |
| Research integrity | 0.001 | 0.000 |
| Insufficient payload (model declined to judge) | 0.006 | 0.003 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".