Research Article |
Corresponding author: Jin-Hua Chen ( cjh_jsu@jsu.edu.cn ) Academic editor: Yasen Mutafchiev
© 2022 Ji-Yan Long, John Patrick Kociolek, David M. Williams, Bing Liu, Wen-Hui Mo, Jin-Hua Chen.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Long J-Y, Kociolek JP, Williams DM, Liu B, Mo W-H, Chen J-H (2022) Two new freshwater species of Surirella (Bacillariophyta) from the Wuling Mountains, China. PhytoKeys 201: 35-49. https://doi.org/10.3897/phytokeys.201.79626
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Two sympatric Surirella species found at the same specific locality in the Wuling Mountains of China are documented with light and scanning electron microscope. Both species are new to science and named S. wufluminensis sp. nov. and S. suiningensis sp. nov. Surirella wufluminensis has large frustules that are either clockwise or counterclockwise twisted when viewed with the light microscope, and possesses distinctive fibulae, mound-like outgrowths on the valve surface throughout, raised longitudinal ridges on both sides of the raphe, and two helictoglossa-like processes at one apex internally. Surirella suiningensis has narrowly ovate valve outline, distinctive fibulae, troughs alternating with crests from pole to pole, and two helictoglossa-like processes at one apex internally. These two species do not produce costae on the valve surface in contrast to many species in Surirella. This study provides a further two examples of the wide range of morphological diversity in the genus Surirella.
Helictoglossa-like process, new species, Surirella, twisted frustule, ultrastructure
The diatom genus Surirella
There are a few taxa in Surirella sensu stricto possesseing ‘twisted’ frustules, such as S. aquastudia (Kociolek & Q. You) Kociolek, S. xinjiangiana (Q. You & Kociolek) Kociolek, and S. dongtingensis Bing Liu & Ector (
The study site is at the course of Wu River running through Suining County, located in the Wuling Mountains of China under a sub-tropical to warm temperate type climate. At the sampling site, epilithic algae were collected from numerous submerged stones showing yellow-brown surfaces indicating the presence of diatoms. Each stone was placed on a plastic plate and its surface was brushed using a toothbrush, with the brushed-off diatom samples being washed into the plate. The diatom samples were transferred into a 100 mL sampling bottles and fixed with 70% ethanol. Two samples were collected from each site. Together with the sample collection, temperature, pH, and conductivity were measured in situ with a portable multimeter (HQ40D, HACH Company)—details are presented below in the ‘Distribution and ecology’ section of the species description.
Specimens for permanent slides were air-dried onto coverslips then mounted onto microscope slides using Naphrax. The slides were examined and specimens photographed using a Leica DM3000 light microscope (LM) at ×1000 magnification (objective NA 1.25) and a Leica MC190 HD digital camera. The holotype slides are deposited in the Natural History Museum, London, United Kingdom (
Terminology related to valve morphology follows
Order Surirellales D.G. Mann
Family Surirellaceae Kützing
Holotype
China. Hunan province: the course of Wu River, a sampling point at Changpu Town, Suining County, 26°34.59'N, 110°09.19'E, 300 m a.s.l., collected by Bing Liu, March 22, 2021.
LM
(Fig.
Surirella wufluminensis sp. nov., SEM A–C three valves in external view; note the visual discrepancies of twist degrees between them as the position of each valve relative to the observer differs D–F three valves in internal view; note the visual discrepancies of twist degrees between them. Scale bars: 20 μm.
SEM
(Figs
Surirella wufluminensis sp. nov., external view, SEM A a whole valve B middle detail from A showing the shallow depressions on the valve face correspond to the ones on the mantle (four arrows) C–E details from Fig. B showing mound-like siliceous outgrowths on the valve surface (C, D, three wavy arrows respectively), raised longitudinal ridges on both sides of the raphe (C, two arrows), slit-like external openings of areolae on both valve face and mantle (D–F) F, G apical details from A, note interrupted terminal raphe endings (see also Fig.
Surirella wufluminensis sp. nov., internal view, SEM A–C middle details from Fig.
Named after Wu River, where the species was found.
Epilithic in a mountain river with oligotrophic waters. The following environmental parameters were measured in the field. Conductivity was 99.7 ± 0.3 μS∙cm–1, pH was 7.9 ± 0.1 and water temperature was 13.2 ± 0.2 °C.
Holotype
Surirella suiningensis, sp. nov., LM. ×400 A–C three valves showing narrow-ovate outline, slightly heteropolar valves, straight valve median line, downward deflecting head and foot poles, distinctive fibulae spanning 70–80% of half valve width except near each apex where a few fibulae meet at median line. Micrograph of holotype (B). Scale bar: 50 μm.
China. Hunan Province: the course of Wu River, a sampling point at Changpu Town, Suining County, 26°34.59'N, 110°09.19'E, 300 m a.s.l., collected by Bing Liu, March 22, 2021.
LM
(Fig.
SEM
(Figs
Surirella suiningensis sp. nov., external view, SEM A one valve showing distinct continuous siliceous median ridge, downward deflecting head and foot poles (two arrows), and pattern of troughs alternating with crests B detail from A showing two troughs and one crest C, D apical details from A, note two curved terminal raphe fissures (C, two arrows) E marginal detail of A, note the recessed valve mantle with thickened base margin, no fenestrae existed, troughs on valve surface corresponding to those on the mantle (two black arrows). Scale bars: 20 μm (A); 2 μm (B–E).
Surirella suiningensis, sp. nov., internal view, SEM A one complete valve showing fibulae extending close to median line and fibulae corresponding to the sinking of mantle (i.e. troughs, six arrows) B detail from A showing only one portula between two adjacent fibulae and uniseriate striae C sinking of mantle against the fibulae (two arrows) D, E apical details from B, note the raphe continuous at one apex (D, arrow) whereas interrupted at the other apex (E, one arrow pointing at a helictoglossa-like process). Scale bars: 20 μm (A); 2 μm (B, C, E); 1 μm (D).
A–D Surirella suiningensis, sp. nov., internal view, SEM A one valve with valvocopula, note the open nature of valvocopula (arrow) B apical detail from A, note two helictoglossa-like processes (two arrows) C detail of open part of valvocopula D detail of valvocopula showing the rimmed areolae internally. Scale bars: 20 μm (A); 4 μm (B); 1 μm (C, D).
Named after Suining County of Hunan Province, where the species was found.
Epilithic in a mountain river with oligotrophic waters. Surirella suiningensis was found in the same sampling site with S. wufluminensis, for the environmental parameters, see above.
The structure of the valves in the two new species argues for their placement in the genus Surirella, in the sense of
Surirella aquastudia, S. xinjiangiana, and S. dongtingensis all have twisted frustules and all produce undulations on the valve surface from pole to pole. Previously, based on the presence of valve undulations, they would have been placed in the genus Cymatopleura. Surirella wufluminensis on the other hand, lacks undulations on its valve surface. Other similar species demonstrating valves with torsion include the former Surirella spiralis Kützing (
With regards to S. suiningensis, the ovate valve outline is reminiscent of Surirella davidsonii A.W.F. Schmidt, S. elegans Ehrenberg, S. slesvicensis Grunow (in
Surirella wufluminensis and S. suiningensis occur together in the same freshwater habitat. Their associated species comprise Pinnularia hustedtii Meister (see
This research was supported by the Natural Science Foundation of Hunan [grant number 2022JJ30473], the Scientific Research Project of the Department of Education of Hunan Province [grant number 21C0364] and the Graduate Scientific Research Innovation Project of Jishou University [grant number JGY202167].