Gyrosigma tenuissimum var. gundulae Hargraves & Sterrenburg, 2014
publication ID |
https://doi.org/ 10.11646/phytotaxa.172.2.2 |
DOI |
https://doi.org/10.5281/zenodo.5151177 |
persistent identifier |
https://treatment.plazi.org/id/03F987BC-650D-FFC3-FF18-B006FBD2FCB5 |
treatment provided by |
Felipe |
scientific name |
Gyrosigma tenuissimum var. gundulae Hargraves & Sterrenburg |
status |
var. nov. |
Gyrosigma tenuissimum var. gundulae Hargraves & Sterrenburg var. nov. ( Figs 28–36 View FIGURES 28–36 )
As the species, but valves larger and more robust.
Type:— USA. Indian River Lagoon, Florida ( BRM ZU 8 About BRM /74! holotype = fig. 28, coordinates 6.7 East, 10.0 South; collection Sterrenburg #721, isotype; collection Hargraves, isotype) GoogleMaps .
As G. tenuissimum , with comparable striation ( Fig. 28, 30 View FIGURES 28–36 ) but much more robust and larger: 159–190 µm long and 9.5–11 µm wide. With respect to G. tenuissimum var. tenuissimum , valve much broader at apices ( Figs 32, 34 View FIGURES 28–36 ), with presence of small accessory apical pore ( Fig. 32 View FIGURES 28–36 , arrow). Externally, central raphe fissures ( Figs 33 View FIGURES 28–36 ) identical to G. tenuissimum var. tenuissimum . Some external areolar fissures of adjacent rows show tendency to fuse, forming the letter V ( Fig. 33 View FIGURES 28–36 ), as in G. tenuissimum . Internal raphe fissures show sideways twisting ( Fig. 35 View FIGURES 28–36 ).
Central bars around internal central raphe node markedly variable in their degree of silification but are often vestigial, reduced to 4 small “knobs” of silica ( Figs 35 and 36 View FIGURES 28–36 ). The extreme resolution of the special LM technique used reveals that one central bar (the lower in Fig. 30 View FIGURES 28–36 ) may also consist of a continuous sharp ridge, the other (upper in Fig. 30 View FIGURES 28–36 ) being reduced to two separate “knobs”, which matches the aspect seen in Fig. 7 of G. tenuissimum var. tenuissimum .
Etymology:— The epithet refers to the long-term support of the first author’s diatom studies by his spouse.
Habitat:—Found at temperatures of 21.9–30.5° C and salinities of 26.2–38.9 PSU; typical spring and summer conditions. The Indian River Lagoon is quite shallow ( Hargraves & Hanisak, 2011), so that the presence of this taxon in plankton samples is not by itself indicative of a planktonic habitat.
Distribution:—Subtropical Indian River Lagoon, East coast of Florida: widespread (but rare).
Observations:— The vestigial central bars (4 “knobs”) match the situation in a specimen from the Adriatic illustrated in Höbel & Sterrenburg (2011: Fig. 12) that conforms to G. tenuissimum . The central bars are highly variable in shape in both G. tenuissimum and the variety described here. Deposition of silica is a quantitative process and marked variation in the solidity of the central bars is common in the genus. Probably the basic shape in the taxa discussed is as in Fig. 7 and 30 View FIGURES 28–36 , reduction leading to the aspect as in Figs 35 and 36 View FIGURES 28–36 .
BRM |
Alfred-Wegener-Institut für Polar- und Meeresforschung |
V |
Royal British Columbia Museum - Herbarium |
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