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Research Article
Caloneis nanyiensis sp. nov. (Bacillariophyta) from Nanyi Lake of Anhui Province, China
expand article infoYong Fang, Pan Yu§, Qing-Min You|, John Patrick Kociolek, Yue Cao#, Quan-Xi Wang, Zhi-Ping Qian
‡ Shanghai Normal University, Shanghai, China
§ Yangtze River Delta Urban Wetland Ecosystem National Field Scientific Observation and Research Station, Shanghai, China
| Shanghai Normal University, shanghai, China
¶ University of Colorado, Boulder, United States of America
# Shanghai Institute of Technology, Shanghai, China
Open Access

Abstract

A new species, Caloneis nanyiensis sp. nov., is described from Nanyi Lake, the largest lake in southern Anhui Province, China. Observations were made using a light and scanning electron microscope documenting the size, shape and ultrastructure of the new species. Caloneis nanyiensis sp. nov. has rhombic valves with acutely rounded apices. The raphe is narrow and arched. An internal axial plate covers the alveoli, leaving small marginal openings bordered by costa, thickened and raised from the valve face. The striae are slightly radiate to parallel in the central area, becoming radiate towards the apices. By comparing the new species with similar Caloneis species, C. nanyiensis sp. nov. was confirmed to be sufficiently different with respect to valve size and striae density to be recognised as new to science. The new species lives in freshwater habitats and epiphytic on Cladophora. The discovery enhances our knowledge of the diversity of freshwater diatoms in China.

Key words:

Axial area, Caloneis, girdle, raphe, rhombic valve

Introduction

Cleve and Grove initially described the genus Caloneis at the subgroup level, originally within the genus Navicula (Cleve and Grove 1891). Unfortunately, they did not provide a valid description; however, a few years later, Cleve provided a valid generic description in the Synopsis of the Naviculoid Diatoms (Cleve 1894). The type species of the genus Caloneis was indicated by Boyer (1927) to be Caloneis amphisbaena (Bory) Cleve (1894). The primary diagnostic features of this genus include valves that are linear-lanceolate to elliptical with capitate or rostrate ends. The shapes of axial and central areas are variable. Distal raphe fissures are usually distinct. The chambered striae give the appearance of one to two longitudinal lines. The striae of Caloneis are composed of fine alveoli. The outer wall of the alveoli is perforated by many rows of small, round poroids occluded by hymens and the inner wall of each alveolus typically opens to the inside of the valve by one fairly large, transapically elongate areola (Round et al. 1990). Caloneis is considered a widely distributed genus with a very broad ecological range, including freshwater, brackish and marine environments (Levkov and Williams 2014). To date, 392 taxonomically accepted species of Caloneis are listed in AlgaeBase (Guiry and Guiry 2025). After 2000, several new species have been reported from various localities from around the world (Lange-Bertalot et al. 2004; Metzeltin et al. 2005; Metzeltin and Lange-Bertalot 2007; Levkov and Williams 2014).

Traditionally, Caloneis and Pinnularia Ehrenberg have been considered distinct genera, the diagnostic features between the two genera mainly including the genus Caloneis having alveolate striae that are usually thinner and denser than those of Pinnularia (Hustedt 1935; Round et al. 1990; Mann 2001; Levkov and Williams 2014; Kulikovskiy et al. 2023). Molecular studies conducted thus far indicate that both the genus Pinnularia and the genus Caloneis are not monophyletic (Bruder et al. 2008; Souffreau et al. 2011; Kulikovskiy et al. 2023). These findings suggest that the genus Pinnularia may require further subdivision, which remains unresolved. With the in-depth study of molecular systematics, we believe that the taxonomic status of the genera Pinnularia and Caloneis will be more accurately and clearly divided.

In China, the vast majority of new Caloneis species were published before 2000, including Caloneis bacillum f. latilanceolatum Zhu and Chen (1995), Caloneis chansiensis Skvortzov (1935), C. elongata var. constricta Cheng and Chin (1980), Caloneis fasciata var. pekinensis Skvortzov (1928), Caloneis holstii var. tibetica Jao (1964), Caloneis hunanensis Chen and Zhu (Zhu and Chen 1989), Caloneis lepidula var. angustata Skvortzov (1976), Caloneis patagonica var. sinica Skvortzov (1938a), C. platycephala Cheng and Chin (1980), Caloneis schroderi var. densestriata Skvortzov (1976), Caloneis schumanniana var. biconstricta f. minor Zhu and Chen (1995), Caloneis silicula var. hankensis Skvortzov (1929), Caloneis schumanniana f. gracilis Skvortzov (1935), Caloneis silicula var. hinganica Skvortzov (1976) and Caloneis sphagnicola Skvortzov (1938b). After 2000, only one taxon has been reported in this genus: Caloneis clevei var. parallela Skvortzov ex Gololobova and Kulikovskiy (Skvortzov 2012).

During the investigation of freshwater diatom diversity in Nanyi Lake, we discovered a new species, which is described here as Caloneis nanyiensis sp. nov. The purpose of this study was to document and formally describe the species, based on both light microscope (LM) and scanning electron microscope (SEM) observations and to compare it with other morphologically similar species of the genus.

Material and methods

Diatom samples were collected from Nanyi Lake (31°01'–31°10'N, 118°50'–119°3'E), Anhui Province, China, in August 2018. The lake area is 210 km2. Nanyi Lake was formed by the differentiation of the ancient Danyang Lake. The ancient Danyang Lake system was a stagnant lake formed by long-term siltation and water accumulation in a newly-constructed fault depression. The climate of the Nanyi Lake area, as reported by the Langxi County meteorological station, belongs to the North subtropical monsoon humid climate zone. The main features are: mild climate, four distinct seasons, hot and rainy season, abundant rainfall and ample sunshine (Jia et al. 2021).

In the field, several water chemistry characteristics were recorded, including: pH, temperature, salinity, total dissolved solids (TDS) and conductivity. These parameters were measured using a YSIPro Plus multiparameter meter (YSI, Ohio, USA). In the field, collections of attached algae were scraped from the surfaces of stones using (sterilised?) toothbrushes and/or a knife and the samples were placed in a bottle, preserved with formalin (4% final concentration) and sealed.

In the laboratory, the diatom valves were cleaned of organic matter using the Microwave Accelerated Reaction System (Model MARS, CEM Corporation, USA) (Parr et al. 2004). The digestion followed a pre-programmed digestion scheme (temperature: 180 °C, ramp: 15 min, hold: 15 min) (Yu et al. 2019). After digestion, samples were alternatively centrifuged (5 minutes at 3500 rpm) and washed with distilled water (approximately five times) until the pH of the sample was approximately neutral. The cleaned material was kept in 95% ethanol. Cleaned diatom specimens were mounted on glass slides in Naphrax for light microscopy (LM) or air-dried on to coverslips and mounted on to Cu stubs for observation with a scanning electron microscope (SEM). LM studies were made with a ZEISS AXIO Imager A2 microscope fitted with DIC optics and a 1.4 numerical aperture, 100× oil immersion objective. SEM examination was conducted using a Hitachi SU-8010 (2 kV, working distance less than 6 mm). Images were compiled with Adobe Photoshop CS6. Morphological terminology follows Round et al. (1990). Both unprepared (field) samples and prepared slides of mounted material are housed in the Laboratory of Algae and Environment, Department of Biology, Shanghai Normal University (SHTU).

Results

Caloneis nanyiensis Pan Yu & Qing-Min You, sp. nov.

Figs 1, 2, 3

Type material.

Holotype. Specimen circled on slide NYH-20180801 (= Fig. 1A), deposited in the Herbarium of Shanghai Normal University (SHTU), China.

Figure 1. 

Caloneis nanyiensis sp. nov. LM ×1000 A–M thirteen valves showing a size diminution series; note that the valves rhombic and raphe narrow and arched. A Illustration of holotype specimen D illustration of isotype specimen. Scale bars: 10 µm (M).

Isotype. Specimen circled on slide 652047 (= Fig. 1D), deposited in the Herbarium of University of Colorado, Boulder, USA.

Type locality.

China. Anhui Province: Nanyi Lake, sampling site with the coordinates 31°01'N, 118°50'E. Diatom samples collected by Pan Yu, 19 August 2018.

Description.

LM (Fig. 1A–M): Valve length 14.5–28.5 μm, width 8.0–10.2 μm. Valves rhombical in shape with acutely rounded apices. Raphe narrow and arched, with slightly unilaterally bent central pores and slightly curved terminal fissures. Axial area linear-lanceolate, becoming wider at the central area. Striae are slightly radiate to parallel in the central area, becoming more radiate towards the apices, 16–18 in 10 μm.

SEM valve exterior (Fig. 2A–E): Valve face usually uneven, with slightly raised ends and a slightly concave middle (Fig. 2A, B). Central area nearly rhombic, with a width accounting for 1/4–1/3 of the valve, the striae pattern in the central area is obviously shorter. (Fig. 2A, B, E). Raphe branches arched with proximal raphe ends weakly unilaterally deflected and dilated, drop-like in shape (Fig. 2A, B, E). Distal raphe fissures hooked and continuing on to the mantle (Fig. 2C, D). Striae multiseriate, composed of 4–5 rows of small, rounded areolae, which are occluded by heavy silicified, perforated hymenes (Fig. 2D, E). Girdle with a single row of linear poroids (Fig. 2A).

Figure 2. 

Caloneis nanyiensis sp. nov. SEM views of the external valve A, B external view of an entire valve note the raphe narrow and arched C details of the apices on the external valve; note the distal raphe fissures hooked and continuing on to the mantle D details of the striae on the external valve; note the Striae multiseriate, composed of small rounded areolae and areolae are occluded by heavy silicified, perforated hymenes E showing the central area. Scale bars: 5 µm (A, B); 2 µm (C, E); 1 µm (D).

SEM valve interior (Fig. 3A–E): The raphe is filiform and slightly arched (Fig. 3A). The proximal raphe endings are deflected to the same sides (Fig. 3B, C) and curve towards a central nodule that is positioned to one side of the central area. The raphe terminates distally as an elevated helictoglossa (Fig. 3D, E). An axial plate covers the alveoli, leaving small marginal openings bordered by costae thickened and raised from the valve face (Fig. 3A, B). Striae composed of 2–4 areolae are present on the mantle (Fig. 3D, E).

Figure 3. 

Caloneis nanyiensis sp. nov. SEM views of valve interior. A Internal view of an entire valve; note the raphe is filiform and slightly arched B, C details of the proximal raphe endings which are deflected to the same side D, E details of the distal raphe ends terminating as helictoglossae and the striae are composed of 2–4 areolae on the mantle. Scale bars: 5 µm (A); 2 µm (B, C); 1 µm (D, E).

Etymology.

The new species is named after the type locality, Nanyi Lake.

Distribution and ecology.

So far, the new species has only been collected at the type locality in Nanyi Lake. The habitat of the new species is characterised by pH 8.1, water temperature 30.2 °C, TDS 0.204 g.l-1, conductivity 175.7 μs.cm-1, collected in one sample (NYH–20180801) on Cladophora. In the type sample, this new species occurred at less than 2% relative abundance, established from a total count of 400 valves. Amongst the species co-occurring with Caloneis nanyiensis sp. nov., only four species accounted for more than 5% of the assemblage: Fragilaria pararumpens Lange-Bertalot, Hofmann & Werum (Hofmann et al. 2013) (25.75%), Achnanthidium jackii Rabenhorst (Rabenhorst 1861) (18.75%), Aulacoseira granulata (Ehrenberg) Simonsen (Simonsen 1979) (11.5%) and Encyonopsis microcephala (Grunow) Krammer (Krammer 1997) (%).

Discussion

The new species described in this study possesses all the ultrastructural features of the genus Caloneis (Round et al. 1990), including having a narrow, slightly arched raphe with slightly unilaterally bent central pores and slightly curved terminal fissures, an axial plate covering the alveoli and striae parallel in the central area, becoming radiate towards the apices.

Caloneis nanyiensis sp. nov. can be compared to several species in the same genus, based on similarities in the outline and structure of the valve, including C. caribeana Metzeltin & Lange-Bertalot (Metzeltin and Lange-Bertalot 2007), C. permagna (Bailey) Cleve (Cleve 1894) and Caloneis schumanniana var. lancettula Hustedt (Hustedt 1930). The morphological characteristics of C. nanyiensis and these similar species are summarised in Table 1 to facilitate their comparison. The outline of the valves of C. nanyiensis is rhombical with acutely rounded ends, while that of C. caribeana is rhombical to rhombic-lanceolate with acutely rounded ends, C. permagna is rhombic-lanceolate with acutely rounded ends and C. schumanniana var. lancettula is narrow-lanceolate with broadly rounded ends. Additionally, the valves of C. nanyiensis are shorter (14.5–28.5 μm) than C. permagna (85–220 μm), C. caribeana (32–57 μm) and C. schumanniana var. lancettula (35–40 μm), as well as narrower (8.0–10.2 μm in C. nanyiensis) versus the breadth of valves in C. permagna (35–55 μm) and C. caribeana (14–16 μm). Furthermore, no central area was observed in the new species, but C. caribeana has a narrow fascia central area, C. permagna has an irregularly lanceolate central area and C. schumanniana var. lancettula has a transapically rectangular central area. The stria density of C. nanyiensis is higher (16–18/10 μm) than that of C. permagna (9–12/10 μm), while being lower than those of the other similar species. Individuals in the populations of C. nanyiensis examined here have a valve outline that is rhombical in shape, which, together with the slightly curved raphe, help to differentiate it from other species in the genus.

Table 1.

Comparison of morphological characteristics of Caloneis nanyiensis sp. nov. and closely-related taxa.

Species/Feature C. nanyiensis sp. nov. C. caribeana Metzeltin & Lange-Bertalot C. permagna (Bailey) Cleve C. schumanniana var. lancettula Hustedt
Valve length (μm) 14.5–28.5 32–57 85–220 35–40
Valve width (μm) 8.0–10.2 14–16 35–55 8
Valve outline Rhombical Rhombical to rhombic-lanceolate Rhombical-lanceolate Narrow-lanceolate
Valve apices Acutely round Acutely round Acutely round Broadly rounded
Axial area Linear to lanceolate Narrow, linear Irregularly lanceolate Narrow-lanceolate
Central area Absent Very narrow fascia Irregularly lanceolate Transapically rectangular
Raphe Narrow and arched Distinctly curved Straight Straight
Density of striae (10 μm) 16–18 17–20 9–12 17–20
References Current study Metzeltin and Lange-Bertalot (2007) Cleve (1894), Krammer and Lange-Bertalot (1986) Hustedt (1930), Krammer and Lange-Bertalot (1986)

We also compared our new species with the smaller valves of C. distinguenda Levkov & Williams (Levkov and Williams 2014). However, the latter taxon is characterised by elliptic-lanceolate valves being 36 μm long and 15 μm wide. Additionally, the central area in smaller specimens of C. distinguenda is distinctly separated from axial area and transversally elliptic in shape. The density of the striae in smaller specimens of C. distinguenda is lower (14–16/10 μm) than that of C. nanyiensis.

Caloneis are common in alkaline, brackish and marine habitats, species of the genus Caloneis having a broad ecological niche (Levkov and Williams 2014). For example, Caloneis is diverse in cold-water oligotrophic habitats, C. limosa prefers to inhabit alkaliphilic, oligotrophic and up to β-mesosaprobic water bodies, and C. schumanniana is classified as a planktonic-benthic, oligo-xenosaprobiontic and alkaliphilic species (Denys 1991; Stancheva et al. 2009; Levkov and Williams 2014). In the present study, Caloneis nanyiensis has only been found on Cladophora in Nanyi Lake. The water quality of Nanyi Lake reflects a moderate nutrient level. This investigation did not detect the presence of this novel species in any other location. It is postulated that this species may be a good indicator of water bodies with moderate nutrient levels. However, further ecological studies are needed to confirm this hypothesis.

Acknowledgements

We would like to thank Lixuan Zhang, Linxin Lu, Bingwei Xing and Yang Yu for help in the field and in the preparation of samples for microscopy. We extend our heartfelt gratitude to the reviewer for the invaluable guidance and support provided. The insightful recommendations have been instrumental in enhancing the quality of this manuscript and we are deeply appreciative of your professional expertise and dedication.

Additional information

Conflict of interest

The authors have declared that no competing interests exist.

Ethical statement

No ethical statement was reported.

Funding

This research was funded and supported by National Natural Science Foundation of China (No. 32100165, 32170205).

Author contributions

Formal analysis: YF, PY. Investigation: YC, QMY. Project administration: QXW, Writing – original draft: YF. Writing – review and editing: ZPQ, JPK, PY.

Author ORCIDs

Pan Yu https://orcid.org/0000-0001-7937-2381

John Patrick Kociolek https://orcid.org/0000-0001-9824-7164

Zhi-Ping Qian https://orcid.org/0009-0008-7514-8073

Data availability

All of the data that support the findings of this study are available in the main text.

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