Cyclotella stipata, Frenguelli, 1942
publication ID |
https://doi.org/ 10.11646/phytotaxa.345.2.3 |
persistent identifier |
https://treatment.plazi.org/id/BC392458-894C-4977-FF71-9468FDE56C05 |
treatment provided by |
Felipe |
scientific name |
Cyclotella stipata |
status |
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Cyclotella stipata Frenguelli’s 1942 ( Figs 1–33 View FIGURES 1–14 View FIGURES 15–24 View FIGURES 25–33 )
Frenguelli described this species from mosses and attached algae in small streams located in Neuquén Province, Argentinean Patagonia. The cells were described as 33–44 μm in diameter with 12 striae in 10 μm, arranged in radial rows and delimiting a rather reduced hyaline central area ornamented with a crown of ten rounded papillae, five bigger alternating with five smaller ones. Frenguelli (1942, p. 213) named the new species as Cyclotella stipata and compared it to the presumably allied Cyclotella sevilleana Deby (1884: 49) and C. sexpunctata Deby (1884 , (?) (according to) Pelletan 1889: 20 7).
The author recorded this species in two samples from Neuquén: Series 375 (as very rare) and Series 428 (as rare). SEM analysis of the only raw sample available (Series 375), yielded no specimens of this taxon leaving the ultrastructure of the type material up to now unknown. Our LM observations of the original Frenguelli material (n= 39) ( Figs 1–14 View FIGURES 1–14 ) show round specimens, 14–69 μm in diameter, a mantle height of 22–38 μm, with 6–11 carinoportulae alternating with rimoportulae in a hyaline area at or near the center of the valve ( Figs 1–10 View FIGURES 1–14 ). Striae on the valve face are of different lengths, (10) 12–15 (16) in 10 μm, with an areola density of (10) 13–16 (18) in 10 μm. Striae on the valve mantle are arranged in longitudinal rows, parallel to the pervalvar axis, 16 in 10 μm, with 17–18 areolae in 10 μm ( Figs 11–14 View FIGURES 1–14 ). Frenguelli (1942) did not designate a type for this species ; he provided two micrographs of different specimens in valve view (Pl. XII figs 5 and 6) and a line drawing of a specimen in girdle view (fig. 2 in p. 213) but he did not refer them to a specific sample (either 375 or 428).
Specimens of C. stipata were also found in materials collected in Tierra del Fuego (n= 40), both in the Frenguelli Collection (Series 239) and in more recent samples (LPC 4682); they are illustrated with LM and SEM in Figs 15, 18, 20, 22 View FIGURES 15–24 , 25–26, 28–30, 31–33 View FIGURES 25–33 . Valves are smaller than those in Frenguelli’s original material, 17–47 μm in diameter, with 4–8 carinoportulae alternating with rimoportulae in a hyaline area at or near the center of the valve ( Figs 15, 18, 20, 22 View FIGURES 15–24 ). Scattered spines, broadly expanded at the base, are evident at the margin of the valves ( Figs 25, 26 View FIGURES 25–33 ). Striae of varying lengths are present, 12–16 in 10 μm having 12–16 areolae in 10 μm. Valves are elongated, with mantle heights ranging from 20.5–28 μm long. Frustules are 44.5–94 μm long. On the valve mantle stria number is 14–18 in 10 μm, with 15–20 areolae in 10 μm. A distinct, unornamented collum is evident ( Fig. 25 View FIGURES 25–33 ).
Specimens conforming to C. stipata from the Limay River basin (n= 36) are presented in Figs 16–17, 19, 21, 23–24 View FIGURES 15–24 and 27 View FIGURES 25–33 (LM and SEM).Valves of this population were also smaller than the type population, 17–51 μm in diameter, having striae of varying lengths, 14–19 in 10 μm. Areolae within a stria on the valve face are 14–19 in 10 μm. 4–10 carinoportulae alternate with rimoportulae and are located in a small hyaline area in the center of the valve ( Figs 16, 17, 19, 21, 23 View FIGURES 15–24 ). Valves are elongated about the valve mantle ; valve mantle height is 20.5–28 μm and frustules are 53–150 μm long about the pervalvar axis. Stria number on the mantle is 14–18 in 10 μm, and areola number is 15–19 in 10 μm. Small spines are evident around the margin of the valve when observed in girdle view ( Fig. 27 View FIGURES 25–33 ).
When examined with SEM, specimens from Tierra del Fuego and Limay River exhibited similar morphologies. The valve face is slightly concave or more or less flat, with or without numerous siliceous nodules or spinules lined up externally with the striae ( Figs 18, 19 View FIGURES 15–24 ). The transition from the valve face to the mantle is abrupt at nearly a 90-degree angle. Externally areolae appear as small, rounded pores ( Fig. 20 View FIGURES 15–24 ). The center of the valve has distinct openings of the carinoportulae ( Fig. 20 View FIGURES 15–24 , arrow), but openings of the rimoportulae are less evident ( Fig. 20 View FIGURES 15–24 , arrowhead). The mantle has fine rows of small, rounded areolae ( Figs 25–27 View FIGURES 25–33 ). Internally, areolae are unoccluded ( Fig. 28 View FIGURES 25–33 ). In the center of the valve a thickening encircles the carinoportulae, which have unoccluded openings ( Figs 22, 23 View FIGURES 15–24 , arrows). The rimoportulae are smaller, with narrow openings bordered by thin thickenings on either side ( Figs 22, 23 View FIGURES 15–24 , arrowheads). A narrow rim extends internally on the valve mantle margin ( Fig. 28 View FIGURES 25–33 ).
The cingulum may contain up to 9 open copulae. Each copula has several rows of poroids, and then a narrow or wide unornamented area. Poroids can be aligned into rows or more scattered across a copula. An elongate ligula fits into the slit or anti-ligula of the adjacent copula ( Figs 31, 33 View FIGURES 25–33 ).
Description of new taxa of Orthoseira
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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