Caloneis quilinensis Frenguelli, 1937

Sunesen, Ines, Tardivo Kubis, Jonas A. & Sar, Eugenia A., 2017, A re-investigation of three Frenguelli’s Caloneis taxa (Pinnulariaceae, Bacillariophyta) from Argentina, Phytotaxa 305 (3), pp. 165-178 : 172

publication ID

https://doi.org/ 10.11646/phytotaxa.305.3.4

persistent identifier

https://treatment.plazi.org/id/987D9873-E31E-C35D-FF21-F92D74D2FD34

treatment provided by

Felipe

scientific name

Caloneis quilinensis Frenguelli
status

 

Caloneis quilinensis Frenguelli (slides of series #310 and associated unmounted material) ( Figs 16–54 View FIGURES 16–28 View FIGURES 29–36 View FIGURES 37–49 View FIGURES 50–54 , Table 1)

Specimens observed were slightly shorter and narrower and had a higher stria density than those described in the protologue of Frenguelli in Frenguelli & Cordini (1937: 96) ( Table 1). They all have rectangular frustules, with rounded, obliquely reinforced corners, almost always lying in girdle view, 8–18 μm in depth (n = 49) ( Figs 16–25 View FIGURES 16–28 , 37, 42 View FIGURES 37–49 ). The valves are linear-elliptic to linear-panduriform with a triundulated margin; the central undulation is slightly narrower than the distal undulations and the apices are cuneate to broadly apiculate ( Figs 29–36 View FIGURES 29–36 , 50, 51 View FIGURES 50–54 ). Valve length 39–81 μm (n = 95), valve width 7.5–16.0 μm (n = 25). The valve face is flat, narrow, gently depressed in the central area and slightly raised toward the poles ( Figs 38, 39 View FIGURES 37–49 , 50, 51 View FIGURES 50–54 ), merging gently into a deep mantle. The valve mantle, with a curved proximal region and a vertical distal region, is deep, much shallower near the apices, and mostly unperforated ( Figs 26–28 View FIGURES 16–28 , 40, 48, 49 View FIGURES 37–49 , 52 View FIGURES 50–54 ). The overlap between the valve mantles forms the figure of a clepsydra ( Figs 18, 19 View FIGURES 16–28 ). The central nodule is elliptical, asymmetric ( Figs 32, 35 View FIGURES 29–36 , 53 View FIGURES 50–54 ). The axial area is fusiform-lanceolate, narrow near the apices and gradually widening toward the central area ( Figs 31, 32 View FIGURES 29–36 ). The central area is large, forming an asymmetrical, broad fascia ( Figs 29–36 View FIGURES 29–36 , 45 View FIGURES 37–49 ). The raphe is filiform, with slightly curved branches deflected in the same direction as the central fissures. The central external raphe fissures are dug out on the central area and end in drop-like pores ( Figs 30–32 View FIGURES 29–36 , 38, 39, 41, 44 View FIGURES 37–49 ). The terminal external raphe fissures are deflected in the same direction as a continuous arch to one side of the apex ( Figs 30, 31 View FIGURES 29–36 , 38, 39, 46 View FIGURES 37–49 ), and finish close to the margin of the mantle ( Figs 38, 39, 46, 48, 49 View FIGURES 37–49 , 52 View FIGURES 50–54 arrowheads). Internally, the raphe is seen as continuous at the central area, slightly undulate near a subtle, asymmetrical, central nodule ( Figs 50, 51, 53 View FIGURES 50–54 ), and end distally in small helictoglossae ( Fig. 54 View FIGURES 50–54 , arrowhead). Pseudosepta surrounding both poles are very short ( Figs 50, 54 View FIGURES 50–54 , arrows). The striae are alveolate, continuing shortly onto the mantle ( Figs 43, 45, 49 View FIGURES 37–49 ). Each stria has an outer areolate layer, multiseriate (3–4 poroids rows) ( Figs 43, 45–47, 49 View FIGURES 37–49 ) and an inner ingrowth of silica opening by an elliptical aperture ( Figs 50, 51, 53, 54 View FIGURES 50–54 ). These apertures are aligned and located at the junction of valve face and mantle ( Figs 50, 51 View FIGURES 50–54 ). The girdle is composed of two bands. The valvocopulae is open at one pole ( Figs 39, 41, 42, 46–48 View FIGURES 37–49 ), with one row of elongate poroids in the pars exterior ( Figs 45, 46 View FIGURES 37–49 ). The copula is wide, segmental, unstructured, occupying the gap left at the pole that close the full circumference of the valve mantle ( Figs 39, 42, 47 View FIGURES 37–49 , arrows).

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF