Kurtkrammeria salesopolensis Marquardt, A.
publication ID |
https://doi.org/ 10.11646/phytotaxa.247.1.4 |
DOI |
https://doi.org/10.5281/zenodo.13678288 |
persistent identifier |
https://treatment.plazi.org/id/39758780-FFB9-FF9F-6FC1-CEA8FC65C6E2 |
treatment provided by |
Felipe |
scientific name |
Kurtkrammeria salesopolensis Marquardt, A. |
status |
sp. nov. |
Kurtkrammeria salesopolensis Marquardt, A. Rocha & C.E.Wetzel, sp. nov. ( Figs 12–23, 15–33 View FIGURES 2–23 View FIGURES 24–31 View FIGURES 32–38 )
Valves linear-lanceolate, not or scarcely dorsiventral in the larger forms and slightly dorsiventral in the smaller ones. Length 41.6–78.7 μm. Breadth 5.3–7.4 μm. Dorsal side slightly convex. Ventral side slightly convex to straight. Valvar margins sometimes tumid in the middle region. Apices narrow, sub-rostrate, rounded, slightly curved to ventral side. Raphe filiform, slightly lateral with proximal fissures slightly expanded, curved to dorsal margin; distal raphe ends comma-shaped, sharply bent to the ventral margin. Axial area approximately 1/3 the valve breath, linear, forming a narrow longitudinal lanceolate hyaline area slightly widening to the central area. Central area variable, absent to linear lanceolate. Striae uniseriate, parallel to slightly radiate, 13–14 in 10 μm, composed of lineolate areolae visible only in the SEM, apically elongated, sometimes “Y” disposed, approximately 33 in 10 μm. Shortened striae continue around valve apices. Isolated punctum absent.
Type:— BRAZIL. São Paulo (SP), Salesópolis: Ribeirão do Campo reservoir, sediment core, 23º 38.514’ S, 45º 49.854’ W, A. C. R. Rocha & D. C. Bicudo, 13 August 2010 (holotype: SP!, slide 427990, here depicted in Figs 12–23 View FIGURES 2–23 . Isotype: BR!, slide 4431).
Etymology:—The Latin name salesopolensis refers to the municipality of Salesópolis where samples were collected.
Additional morphological data:—External raphe fissure are slightly undulate ( Fig. 32 View FIGURES 32–38 ), located approximately in the mid region of the valve. Proximal end of raphe almost straight, the enlarged proximal endings slightly curved to the dorsal side ( Figs 32–33 View FIGURES 32–38 ). Distal raphe ends are comma-shaped, first dorsally bent, then strongly hooked to the ventral side ending onto the mantle ( Figs 32, 35–36 View FIGURES 32–38 ). Axial area is linear-lanceolate ( Fig. 32 View FIGURES 32–38 ) to form a lanceolate central area, formed by very slightly shortened striae on ventral side and on dorsal side. Striae uniseriate, composed of apically-elongated areolae, sometimes “Y” disposed ( Figs 32–34, 36–38 View FIGURES 32–38 ) numbering 33 in 10 μm, radiate near the valve center, becoming parallel, then convergent near the apices. Transapically-elongated areolae, different shape and size, in shortened striae continuing around the apex ( Figs 32, 34, 37–38 View FIGURES 32–38 ), numbering 13–14 in 10 μm. Internally, struts provide structural support to the foramen, whose opening bears one very short spine at each side ( Figs 35–36 View FIGURES 32–38 ). Internal proximal raphe ends are widely separated and strongly hooked towards the dorsal margin ( Fig. 36 View FIGURES 32–38 ), and the distal endings terminate in well-developed helictoglossae that are deflected towards the ventral margin ( Fig. 35 View FIGURES 32–38 ). No isolated punctum is present.
Ecology: — Encyonema acquasedis sp. nov. and Kurtkrammeria salesopolensis sp.nov. occur in acidic environments (pH 5.2–5.6), with water temperature around 17.6–25.5 °C and electric conductivity 10.4–12.4 μS cm-1 ( Table 1). The new species were rare in samples collected from the plankton and surface sediments (relative abundance ≤ 2%). In the planktonic samples both taxa were associated with species of Kobayasiella [i. e. K. micropunctata (H. Germain 1981: 234) Lange-Bertalot (1999: 267) and K. venezuelensis Metzeltin & Lange-Bertalot (2007: 155) ], Eunotia [ Eunotia sp. , E. botuliformis F.Wild, Nörpel & Lange-Bertalot in Lange-Bertalot (1993: 29) and E. veneris ( Kützing 1844: 40) De Toni (1892: 794) ], Frustulia [ F. crassinervia (Brébisson in Smith 1853: 47) Lange-Bertalot & Krammer in Lange-Bertalot & Metzeltin (1996: 57)] and Brachysira [ B. brebissonii R.Ross in Hartley (1986: 607) and B. serians ( Brébisson 1838: 18) Round & D.G.Mann (1981: 227) ]. On benthic samples they were, associated with Brachysira brebissonii , B. serians , Eunotia botuliformis , E. bilunaris ( Ehrenberg 1832: 87) Schaarschmidt (1881: 159) , E. incisa W. Gregory (1854: 96) , Eunotia sp. , Frustulia crassinervia and Frustulia sp.
R |
Departamento de Geologia, Universidad de Chile |
BR |
Embrapa Agrobiology Diazothrophic Microbial Culture Collection |
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