Haslea tsukamotoi Sterrenburg & Hinz, 2015

Sterrenburg, Frithjof A. S., Tiffany, Mary Ann, Hinz, Friedel, Herwig, Wulf E. & Hargraves, Paul E., 2015, Seven new species expand the morphological spectrum of Haslea. A comparison with Gyrosigma and Pleurosigma (Bacillariophyta), Phytotaxa 207 (2), pp. 143-162 : 151-152

publication ID

https://doi.org/ 10.11646/phytotaxa.207.2.1

DOI

https://doi.org/10.5281/zenodo.13637760

persistent identifier

https://treatment.plazi.org/id/6E1687D3-9271-0931-FF40-A0AC38D0FC54

treatment provided by

Felipe

scientific name

Haslea tsukamotoi Sterrenburg & Hinz
status

sp. nov.

Haslea tsukamotoi Sterrenburg & Hinz , sp. nov. ( Figs 14, 15 View FIGURES 10–20 : LM, 33–38: SEM)

Type:— “ Toque-Toque Grande Beach, Sao Sebastiao, Sao Paulo, Brazil, June, 30, 2012, leg. R. Y. Tsukamoto ”, geographic coordinates 23°83’ S, 45°51’ W. Holotype BRM ZU9 About BRM /88, slide coordinates 13.0 E, 6.1 S., isotypes in collections Sterrenburg #724 and (SP) Herbario Maria Eneyda P. K. Fidalgo, Instituto de Botanica de Sao Paulo #SP428.775. GoogleMaps

Valve ( Figs 14, 15 View FIGURES 10–20 , 33, 34 View FIGURES 33–38 ) robust, lanceolate, 40–55 μm long, 8–9.5 μm wide, with acute ends. Striae transverse slightly radiate, 16–19 in 10 μm, longitudinal finer, 18–21 in 10 μm. In LM, axial and central area so narrow that there is no visible hyaline space separating striae and raphe sternum. In SEM, the tegumental layer shows marked surface relief ( Fig. 36 View FIGURES 33–38 ). External central raphe fissure endings approximate, forming tiny “crooks” tightly curved over about 270° around a tooth-like projection ( Fig. 36 View FIGURES 33–38 and inset); apical endings undulating, terminating as retrograde hooks ( Fig. 38 View FIGURES 33–38 ). At the apex a small accessory pore perforates the solid margin of the valve ( Figs 37, 38 View FIGURES 33–38 , arrows). Basal layer: foramina apically elongated oblong, becoming about twice as wide near the margin ( Fig. 35 View FIGURES 33–38 ). The broader peripheral foramina are not reflected as wider puncta spacing in the LM, as the widening of the foramina is at the expense of the width of the longitudinal bars of the basal layer grate. Entire internal raphe fissure and internal central raphe node (which is slightly depressed in the middle) fully tilted sideways ( Fig. 35 View FIGURES 33–38 and inset).

Etymology:— Named after the collector, Dr. Ricardo Tsukamoto.

Habitat:— Wet beach.

Distribution:— Type locality only so far, fairly abundant.

Observations:— The marked difference in width of the median and the more peripheral internal foramina of the basal layer is a special feature in this new Haslea species and its internal and external raphe morphology is particularly unusual. The tightly curved “crooks” of its external central raphe endings have not yet been described in Haslea , where the fissures are generally described as almost straight or very slightly curved, as they are in H. feriarum and H. staurosigmoidea . Whilst sideways twisting of the internal raphe fissure over most of its length is considered a typical feature of Haslea species, at least its central portion is perpendicular to the valve plane in the species previously described, whereas in H. tsukamotoi the entire internal raphe system is fully sideways tilted, including the central raphe node. Saepes not satisfactorily visualized, no fragmented valves found.

H. tsukamotoi has much finer striae than H. howeana and H. nautica ; it is longer and has more markedly radiate striae than H. brittanica .

R

Departamento de Geologia, Universidad de Chile

BRM

Alfred-Wegener-Institut für Polar- und Meeresforschung

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