Gyrosigma rostratum Bing Liu, D.M. Williams and Bangqin Huang, 2015

Liu, Bing, Williams, David M. & Huang, Bangqin, 2015, Gyrosigma rostratum sp. nov. (Bacillariophyta) from the low intertidal zone, Xiamen Bay, southern China, Phytotaxa 203 (3), pp. 254-262 : 256-259

publication ID

https://doi.org/ 10.11646/phytotaxa.203.3.4

DOI

https://doi.org/10.5281/zenodo.13638884

persistent identifier

https://treatment.plazi.org/id/4555A913-FFE8-FF8D-13E3-EC78FF21FD4B

treatment provided by

Felipe

scientific name

Gyrosigma rostratum Bing Liu, D.M. Williams and Bangqin Huang
status

sp. nov.

Gyrosigma rostratum Bing Liu, D.M. Williams and Bangqin Huang , sp. nov. ( Figs. 2–20 View FIGURES 2–11 View FIGURES 12–16 View FIGURES 17–20 )

Type: — CHINA. Fujian: Xiamen Bay, Yefeng Village, the low intertidal zone, 24º 26’ 49.9” N, 118º 10’ 11.4” E, 0 m a.s.l., Bing Liu , 7 July 2013 (holotype JIU! G201501 About JIU = Fig. 3, 7.4 View FIGURES 2–11 mm south by 16.5 mm east from the benchmark cross on the slide; isotype CL201301 = Fig. 4, 3.1 View FIGURES 2–11 mm south by 14.9 mm east from the benchmark cross on the slide) GoogleMaps .

Cells solitary, usually lying in valve view. Each cell with two large plate-like chloroplasts, one against each side of girdle ( Fig. 2 View FIGURES 2–11 ). Valves lanceolate with protracted rostrate apices, symmetrical to both apical and transapical axis, not sigmoid ( Figs. 3–11 View FIGURES 2–11 ), apical and transapical axes 57–93 μm and 16–21 μm, respectively. Valve face flat, slightly twisted along raphe-sternum ( Figs. 3–11 View FIGURES 2–11 ). Conopeum (a lunate flap of silica, approximately 0.8–1.1 μm wide by 4.4–4.8 μm long) covers the axial area, with two rows of areolae near each terminal end ( Figs. 3–4 View FIGURES 2–11 , 13–14 View FIGURES 12–16 ). Raphe straight, rotates either clockwise ( Figs. 3–6 View FIGURES 2–11 , 12 View FIGURES 12–16 ) or anticlockwise ( Figs. 7–11 View FIGURES 2–11 , 13 View FIGURES 12–16 ), both at an angle of approximately two degrees in relation to apical axis ( Figs. 3–13 View FIGURES 2–11 View FIGURES 12–16 ). Central area small, round, non-rotated ( Figs. 3–11 View FIGURES 2–11 , 15–16 View FIGURES 12–16 ). Externally, proximal raphe fissures turn in same direction, close to each other ( Figs. 15–16 View FIGURES 12–16 ), while terminal raphe fissures curve in opposite directions with deeply grooved endings ( Fig. 14 View FIGURES 12–16 ). Proximal raphe fissures of the two types of valves (i.e. epitheca and hypotheca, not from the same frustule) superimposed one above the other ( Figs. 12–13, 15–16 View FIGURES 12–16 ). Internally, central bars of silica either lunate ( Fig. 18 View FIGURES 17–20 ) or both bars divided into two independent entities ( Figs. 17, 20 View FIGURES 17–20 ); proximal raphe endings T-shaped lying in flat nodule, at poles end in bulky and raised helictoglossa ( Fig. 19 View FIGURES 17–20 ). Internally, prominent axial costa more marked on one side, merging with one central bar at center ( Figs. 19–20 View FIGURES 17–20 ). Transapical striae (20–21 in 10 μm) parallel throughout valve, longitudinal striae (21–22 in 10 μm) parallel from pole to pole. The striae consist of rounded to quadrangular areolae that open externally by apically elongated slits ( Figs. 14, 16 View FIGURES 12–16 ) and are internally occluded by hymens (not shown in this paper). Rounded pores are located on the mantle ( Figs. 14, 16 View FIGURES 12–16 ). Distal to terminal raphe ending, five apical pores occur, continuous with the marginal row of round pores on one side of apex and discontinuous with it on the other side ( Figs. 14 View FIGURES 12–16 , 19 View FIGURES 17–20 ).

Etymology: —From the Latin adjective rostratus, referring to the protracted, not inflated valve apices with parallel sides.

Ecology and distribution: —In our 32 sampling sites, G. rostratum was only found among the three low intertidal zones in Huizhan Center, Yefeng Village, and Zengcuo Village respectively (not in the other 29 sampling sites). The specimens of G. rostratum are infrequent in all the samples from these three sampling sites, with the highest frequency in the sample from the low intertidal zone from Yefeng village. From Table 1 it is clear that G. rostratum is epipsammic and lives in marine habitats. The associated diatom flora in all three sites was dominated by Cocconeiopsis kantsinensis (Giffen) Witkowski, Lange-Bertalot and Metzeltin (2000: 173 ; basionym: Navicula kantsinesis Giffen 1967: 269 ).

Observations: —In his monograph on Pleurosigma, Peragallo divided the genus 11 sub-divisions based on the striae orientation ( Peragallo 1891: 3–4). Peragallo’s classification has since been revised but a consequence of the older sub-divisions would have placed Gyrosigma rostratum (transapical striae 20–21 in 10 μm vs. longitudinal striae 21–22 in 10 μm) in Peragallo’s sub-division Acuminati as the densities of the transapical and longitudinal striae are approximately equal. Gyrosigma rostratum differs from other species placed in that sub-division by Peragallo because of its symmetrical valve and straight (not sigmoid) raphe with a raphe angle of approximately two degrees in relation to the apical axis. Following Reid’s recent re-assessment of the genera Gyrosigma and Pleurosigma , many of Peragallo’s sub-divisions are in need of revision ( Reid 2012). Nevertheless, G. rostratum , using available evidence, should rightly be considered a species of Gyrosigma .

Gyrosigma rostratum bears some resemblance to G. fogedii Stidolph (1994: 215) but can be distinguished from the latter by its rostrate, rather than spathulate, apices and the single row of striae, rather than the dichotomous/intercalary striae opposite the central valve area. Taking into account the valve outline, G. rostratum resembles Pleurosigma cuspidatum (Cleve) H. Peragallo (1891: 12 ; basionym: P. lanceolatum var. cuspidatum Cleve 1881: 5 ) that also has a raphe of a similar orientation to G. rostratum (see Cardinal et al. 1986). At any rate, G. rostratum is readily identified by its fairly straight valve outline in LM, its identity being confirmed by its lunate flaps of silica at terminal ends in SEM.

JIU

Jishou University

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