Adlafia sinensis Bing Liu & D.M. Williams, 2017

Liu, Bing, Williams, David M. & Ou, Yongda, 2017, Adlafia sinensis sp. nov. (Bacillariophyceae) from the Wuling Mountains Area, China, with reference to the structure of its girdle bands, Phytotaxa 298 (1), pp. 43-54 : 47

publication ID

https://doi.org/ 10.11646/phytotaxa.298.1.4

DOI

https://doi.org/10.5281/zenodo.13689506

persistent identifier

https://treatment.plazi.org/id/823887E6-844F-FFD0-FF68-FEE98A08FA6B

treatment provided by

Felipe

scientific name

Adlafia sinensis Bing Liu & D.M. Williams
status

sp. nov.

Adlafia sinensis Bing Liu & D.M. Williams sp. nov. ( Figs 2–50 View FIGURES 2–35 View FIGURES 36–39 View FIGURES 40–42 View FIGURES 43–46 View FIGURES 47–50 )

LM: Valves lanceolate with rostrate to subcapitate apices ( Figs 2–35 View FIGURES 2–35 ), dimensions (n = 50): 11.0–17.0 μm long, 3.4– 4.2 μm broad.Axial area linear throughout valve’s entire length, central area almost non-existent ( Figs 2–35 View FIGURES 2–35 ). External central raphe endings discernible, opposite each other (e.g. Figs 27–35 View FIGURES 2–35 ). Striae dense, uncountable.

SEM: Valves lanceolate with rostrate to subcapitate apices ( Figs 36–38 View FIGURES 36–39 ). Axial area linear gently widening at central area ( Figs 36–38 View FIGURES 36–39 ). Raphe with terminal fissures hooked towards secondary side; both fissures with slightly expanded central raphe endings bent towards primary side ( Figs 36–38 View FIGURES 36–39 ). Striae uniseriate, radiate, becoming abruptly convergent approaching apices, continuing onto mantle (e.g. Figs 41 View FIGURES 40–42 , 47–50 View FIGURES 47–50 ). A few shortened striae present on each side of central valve ( Figs 36–38 View FIGURES 36–39 ). Stria density 32–36 (often 34) per 10 μm. Areolae round, occluded by hymenes outside ( Figs 36–38 View FIGURES 36–39 ). Internally, both proximal raphe endings deflected towards primary side of valve and distal raphe endings terminating in small helictoglossae ( Fig. 39 View FIGURES 36–39 ).

Frustule and girdle views: Frustules in girdle view rectangular composed of epivalve, hypovalve and valvocopula ( Figs 40–42 View FIGURES 40–42 , EV, VC and HV respectively). Striae continuing onto deep mantle, c. 5–7 striae on mantle not continuous from valve ( Fig. 41 View FIGURES 40–42 , arrowheads; Figs 47–50 View FIGURES 47–50 , arrows). Stria density on mantle 37–40 per 10 μm due to c. 5–7 striae more than valve face. Mantle becomes abruptly narrow close to apex where 4–6 rows of areolae merge into one row distal to terminal raphe fissures ( Fig. 41 View FIGURES 40–42 , Fig. 43 View FIGURES 43–46 , curved arrow). Valvocopula connects epivalve and hypovalve ( Figs 40–41 View FIGURES 40–42 , 43–46 View FIGURES 43–46 ). Two rows of poroids on valvocopula ( Fig. 38 View FIGURES 36–39 , arrow; Fig. 41 View FIGURES 40–42 , VC; Fig. 47 View FIGURES 47–50 , arrow), but in complete frustules, deep mantle covers one of two rows of valvocopula poroids located on pars interior of valvocopula, and only one row of poroids on pars exterior visible ( Fig. 40 View FIGURES 40–42 , VC). Valvocopula composed of at least two parts that connect epivalve and hypovalve into a complete frustule; beneath the apices one part turns towards epivalve, the other turns towards hypovalve; both terminal ends of each part insert into the alternate part at inflection points of each ( Figs 43–44, 46 View FIGURES 43–46 , arrows). Valvocopula open due to its two parts not being fused at inflection points ( Figs 43–44, 46 View FIGURES 43–46 , arrows). Two segmental bands occur only beneath apices ( Figs 44 View FIGURES 43–46 , B 2, B3 View FIGURES 2–35 ).

Type: — CHINA. Hunan: Zhangjiajie National Forestry Park, the course of Jinbian brook, at Laomowang , 29°19’ 38” N, 110°26’32” E, 482 m a.s.l., Bing Liu , 29 th December 2015, (holotype JIU! G201607 About JIU = Fig. 29 View FIGURES 2–35 ; isotype BM! 101860 = Fig. 17 View FIGURES 2–35 ) GoogleMaps .

Etymology: —Named after China, the country where the species was found.

Ecology:— The following environmental parameters were measured in the field. 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 conductivity is near 100 μS/cm, Adlafia sinensis can be considered an epilithic diatom characteristic of moderate electrolyte content in freshwaters.

JIU

Jishou University

BM

Bristol Museum

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