Ulnaria ulnabiseriata D.M. Williams et Bing Liu, 2017

Liu, Bing, Williams, David M. & Tan, Lin, 2017, Three new species of Ulnaria (Bacillariophyta) from the Wuling Mountains Area, China, Phytotaxa 306 (4), pp. 241-258 : 248-251

publication ID

https://doi.org/ 10.11646/phytotaxa.306.4.1

DOI

https://doi.org/10.5281/zenodo.13695822

persistent identifier

https://treatment.plazi.org/id/03B587FA-7B6D-FFA5-FF30-F89B3EA8FE0D

treatment provided by

Felipe

scientific name

Ulnaria ulnabiseriata D.M. Williams et Bing Liu
status

sp. nov.

Ulnaria ulnabiseriata D.M. Williams et Bing Liu , sp. nov. ( Figs 30–51 View FIGURES 30–36 View FIGURES 37–40 View FIGURES 41–46 View FIGURES 47–51 )

LM: Frustules rectangular in girdle view ( Fig. 36 View FIGURES 30–36 ). Valves linear-lanceolate with protracted subcapitate to rostrate poles ( Figs 30–35 View FIGURES 30–36 ). Valves with parallel sides at the centre, slightly tapering towards the poles from c. 1/3 down each half of the valve ( Figs 30–35 View FIGURES 30–36 ). Transapical axis 6–8 μm, apical axis 105–229 μm (n = 50). Sternum central, distinctive, regular, extending length of valve. Striae broad, parallel, radiating only at poles, 9–11(often 10) in 10 μm. With respect to sternum, striae mostly opposite one another, few deviating, mostly, but not always, towards the poles ( Figs 30–35 View FIGURES 30–36 , arrows). A single rimoportula at each pole, central area rectangular, c. 8×10 μm.

SEM: Frustules rectangular in girdle view, epivalve with valvocopula and three copulae ( Figs 37–40 View FIGURES 37–40 , B 8–B5 View FIGURES 3–10 ), as for hypovalve ( Figs 37–40 View FIGURES 37–40 , B 1–B View FIGURE 1 4 View FIGURES 3–10 ). Each band possessing a single row of poroids which bisects the pars interior and exterior, located at mid-line of each girdle band ( Figs 38–40 View FIGURES 37–40 ). Valve face and mantle meet almost at right angles ( Figs 37–40 View FIGURES 37–40 ). Valves with biseriate striae, situated opposite each other, equidistant until radiating at poles; striae extending to valve face-mantle junction then continued onto mantle ( Figs 37–40 View FIGURES 37–40 , 42–46 View FIGURES 41–46 ). Each stria formed from externally raised virgae with vimines, the latter having closing plates producing biseriate structure ( Figs 44–46 View FIGURES 41–46 ). Each areola (including those on mantle) covered externally by velum ( Fig. 47 View FIGURES 47–51 ). A single rimoportula present at each pole, each a pair of simple extended lips, situated close to sternum ( Figs 42–43 View FIGURES 41–46 ). Two horn-like outgrowths located on top of each ocellulimbus ( Figs 38, 40 View FIGURES 37–40 , 47 View FIGURES 47–51 ). Mantle plaques present ( Figs 38–40 View FIGURES 37–40 ). Internally, valves linear-lanceolate, with subcapitate to rostrate poles; striae biseriate almost opposite each other, near sternum becoming uniseriate ( Figs 49–51 View FIGURES 47–51 ). Rimoportulae prominent, possessing the characteristic bilabiate shape, lying close to the sternum ( Figs 49, 51 View FIGURES 47–51 ).

Type: — CHINA. Hunan: Zhangjiajie National Forestry Park, the course of Jinbian stream, at Shuirao Simen , 29°20’36” N, 110°28’13” E, 467 m a.s.l., Bing Liu , 29 th December 2015, (holotype BM! 101839, illustrated in Fig. 30 View FIGURES 30–36 ; isotype JIU! G201605 About JIU , illustrated in Fig. 35 View FIGURES 30–36 , both holotype and isotype indicated on the slide) GoogleMaps .

Etymology: —The epithet ulnabiseriata is a combination of ulna and the term ‘biseriate’ to reflect its similarity to U. ulna and its biseriate striae.

Ecology:— The following environmental parameters were measured in the field. Electric conductivity was 102.7 ± 0.8 μS/cm, pH was 8.5 ± 0.7, and water temperature was 8.7 ± 0.2 °C. Since the diatom sample was scraped off the surfaces of stones and the water electric conductivity is near 100 μS/cm, Ulnaria ulnabiseriata can be considered an epilithic diatom characteristic of moderate electrolyte content freshwaters.

BM

Bristol Museum

JIU

Jishou University

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