Afrocymbella symmetrica, Stone & Wilson & Jovanovska, 2022
publication ID |
https://doi.org/ 10.11646/phytotaxa.556.1.3 |
DOI |
https://doi.org/10.5281/zenodo.6952080 |
persistent identifier |
https://treatment.plazi.org/id/03AC87E9-455A-FFA6-FF28-FF5BFB580E89 |
treatment provided by |
Plazi |
scientific name |
Afrocymbella symmetrica |
status |
sp. nov. |
Afrocymbella symmetrica sp. nov. (LM Figs 2–23 View FIGURES 2–23 , SEM Figs 24–31 View FIGURES 24–27 View FIGURES 28–31 )
Description:— Valve length 34–49 μm, valve breadth 7.5–9.5 μm. Length to breadth ratio: 5.8. Valves distinctly dorsiventral, slightly heteropolar, semirhomboid-lanceolate ( Figs 2–31 View FIGURES 2–23 View FIGURES 24–27 View FIGURES 28–31 ). Dorsal margin distinctly arched; ventral margin with wide gibbous center portion, typically 1/3 length of valve, otherwise weakly convex ( Figs 24, 26 View FIGURES 24–27 ). Valve apices acutely rounded and slightly protracted, with headpole and footpole nearly symmetrical, often only differentiated by APF and slightly greater breadth in footpole ( Figs 25, 26 View FIGURES 24–27 ). Internally, each column of the APF poroids partially surrounded by knobby jointed ridge of silica ( Fig. 29 View FIGURES 28–31 ). From inside, valve apices with small to indistinguishable pseudosepta ( Figs 29, 31 View FIGURES 28–31 ). Axial area narrow, curved, ventrally displaced ( Fig. 24 View FIGURES 24–27 ). Central area small, asymmetric and diamond-shaped, notably wider on dorsal side ( Figs 2–24 View FIGURES 2–23 View FIGURES 24–27 ). Distinct single stigmoid present on dorsal side of central nodule; externally slightly elongated ( Fig. 27 View FIGURES 24–27 ), internally forming antler-like intermissio ( Fig. 30 View FIGURES 28–31 ). Raphe slightly sinusoidal ( Figs 24, 25 View FIGURES 24–27 ). External proximal raphe ends slightly expanded into small pores, deflected towards the dorsal (primary) margin ( Fig. 27 View FIGURES 24–27 ). External distal raphe terminal fissures ventrally deflected ( Figs 25, 26 View FIGURES 24–27 ). Internal proximal raphe ends covered by nodular or flap-like development from primary side of valve ( Figs 28, 30 View FIGURES 28–31 ). Internal distal raphe terminal fissures bisect the APF and terminate into small lobed helictoglossa at some distance from valve apices (white arrow in Fig. 29 View FIGURES 28–31 ). Striae almost parallel in the middle, strongly radiate towards the apices, and continue uninterrupted onto valve mantle. Stria density in middle portion 15–17 in 10 μm dorsally, often slightly coarser ventrally (15–16 in 10 μm) and increasing slightly (17–18 in 10 μm) towards valve apices. Areolae elongate slits, becoming smaller and nearly circular at edge of valve mantle, 26–30 in 10 μm. Internally, areolae ellipsoid without velum ( Figs 28, 30, 31 View FIGURES 28–31 ).
Type:— UNITED REPUBLIC OF TANZANIA. Lake Tanganyika central basin, core NPO4-KH1-1K, Drive 4; mud, sampled at 43–44 cm (estimated to be ~ 50 ka), 6°35’27.0” S 30°06’00.0” E, J. R.Stone, 30th March 2019 (holotype designated here, circled specimen ANS-GC17192! = Fig. 9 View FIGURES 2–23 , isotypes circled specimens ANS-GC17193!, BM-101977!). Cleaned type materials: ANS-GCM 33025 GoogleMaps .
Registration:https://zoobank.org/NomenclaturalActs/2d7a7068-a78b-425f-a9e6-5d41e121a43b
Etymology:— The specific epithet ‘ symmetrica ’ refers to the symmetrical outline that characterizes this species.
Distribution:— Afrocymbella symmetrica sp. nov. was first observed in sediment assemblages from Lake Tanganyika, dating back to about 60–50 ka from the core NPO4-KH1-1K (4K, Fig. 1 View FIGURE 1 ) and was not observed in the more recent sediments from this core. Initially, we thought it may have been putatively extinct, but have subsequently observed living specimen from modern samples in Tanzania collected in shallow water near Kigoma.
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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