Surirella brightwellii W. Smith. Both 1853

Surirella brightwellii W. Smith 1853 Figs 1, 2, 3 Description. LM (Fig. 1). Valve outlines ovate with broadly rounded headpole and cuneate footpole (Fig. 1). Valve dimensions (n = 102): length range 19–56 μm, width range 13–29 μm at its widest region. Costa-stria bundles (CSBs) distinct, alternating with over-fibula ribs (OFRs) from pole to pole (labelled in Fig. 1 F). CSBs parallel at the valve middle, radiate approaching two apices. Fibulae visible, short (judged by OFRs, labelled in Fig. 1 F), 5–7 in 10 μm. SEM (Figs 2, 3). Externally, raphe canal located directly on the mantle, and wall of raphe canal hyaline (Fig. 2 A, B), distal raphe endings straight, interrupted at both headpole and footpole (Fig. 2 D, E). Surface costae mostly raised, some reaching valve midline (Fig. 2 C). Each CSB composed of ca. 2–4 costae and 3–5 striae (Fig. 2 F). Outside openings of areolae slit-like or rounded (Fig. 2 D, E). Striae multiseriate, composed of ca. 2–5 rows of areolae (Fig. 2 D, E), 19–22 in 10 μm (measured at the valve margin from SEM images, n = 4). Surface siliceous warts and reticulate thickenings produced on costae and between adjacent two costae, respectively (e. g., Fig. 2 D, E). Internally, wall of raphe canal not growing conspicuously into cell cavity, leaving portulae visible (Fig. 3 A, B). Fibulae slim, short, sometimes doubled (Fig. 3 B, arrows), spanning ca. 1 / 4 of valve width, not extending to valve midline except at two valve poles. Marginal trough-like depressions present around entire raphe canal (Fig. 3 A, black dotted lines). Raphe continuous at headpole (Fig. 3 C, arrow) whereas interrupted at footpole (Fig. 3 D, two arrows). 2–5 portulae produced between two adjacent fibulae (Fig. 3 F, arrows). Inner openings of areolae rounded, not rimmed. Each mantle sinking against a fibula (Fig. 3 E, arrows). Ecology and distribution. The type localities of Surirella brightwellii are the coasts of Norfolk and Lewes (United Kingdom), and Smith stated that it was a fresh or brackish water species (Smith 1853). According to Krammer and Lange-Bertalot (1987), the syntypes designated by Hoover (1976) originate from a locality in Sussex (a brackish habitat). In this study, Surirella brightwellii was found to be a dominant species in the benthic diatom community in Lake Qinghai. At the sampling point where it was collected near the lakeshore of Lake Qinghai (36°50'34"N, 99°42'39"E, 3210 m asl.) on July 19, 2019, the conductivity was 16.3 ± 0.1 mS · cm – 1, pH was 9.14 ± 0.01, and water temperature was 15.5 ± 0.3 ° C. These data support previous findings that S. brightwellii is a brackish diatom species.

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Zenodo (CERN European Organization for Nuclear Research)
Published
2025-09-26
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https://doi.org/10.5281/zenodo.17209439
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Data Analysis with R
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article

Surirella brightwellii W. Smith. Both 1853

Zenodo (CERN European Organization for Nuclear Research)
Data Analysis with R
article

Surirella brightwellii W. Smith. Both 1853

article en

Abstract

Surirella brightwellii W. Smith 1853 Figs 1, 2, 3 Description. LM (Fig. 1). Valve outlines ovate with broadly rounded headpole and cuneate footpole (Fig. 1). Valve dimensions (n = 102): length range 19–56 μm, width range 13–29 μm at its widest region. Costa-stria bundles (CSBs) distinct, alternating with over-fibula ribs (OFRs) from pole to pole (labelled in Fig. 1 F). CSBs parallel at the valve middle, radiate approaching two apices. Fibulae visible, short (judged by OFRs, labelled in Fig. 1 F), 5–7 in 10 μm. SEM (Figs 2, 3). Externally, raphe canal located directly on the mantle, and wall of raphe canal hyaline (Fig. 2 A, B), distal raphe endings straight, interrupted at both headpole and footpole (Fig. 2 D, E). Surface costae mostly raised, some reaching valve midline (Fig. 2 C). Each CSB composed of ca. 2–4 costae and 3–5 striae (Fig. 2 F). Outside openings of areolae slit-like or rounded (Fig. 2 D, E). Striae multiseriate, composed of ca. 2–5 rows of areolae (Fig. 2 D, E), 19–22 in 10 μm (measured at the valve margin from SEM images, n = 4). Surface siliceous warts and reticulate thickenings produced on costae and between adjacent two costae, respectively (e. g., Fig. 2 D, E). Internally, wall of raphe canal not growing conspicuously into cell cavity, leaving portulae visible (Fig. 3 A, B). Fibulae slim, short, sometimes doubled (Fig. 3 B, arrows), spanning ca. 1 / 4 of valve width, not extending to valve midline except at two valve poles. Marginal trough-like depressions present around entire raphe canal (Fig. 3 A, black dotted lines). Raphe continuous at headpole (Fig. 3 C, arrow) whereas interrupted at footpole (Fig. 3 D, two arrows). 2–5 portulae produced between two adjacent fibulae (Fig. 3 F, arrows). Inner openings of areolae rounded, not rimmed. Each mantle sinking against a fibula (Fig. 3 E, arrows). Ecology and distribution. The type localities of Surirella brightwellii are the coasts of Norfolk and Lewes (United Kingdom), and Smith stated that it was a fresh or brackish water species (Smith 1853). According to Krammer and Lange-Bertalot (1987), the syntypes designated by Hoover (1976) originate from a locality in Sussex (a brackish habitat). In this study, Surirella brightwellii was found to be a dominant species in the benthic diatom community in Lake Qinghai. At the sampling point where it was collected near the lakeshore of Lake Qinghai (36°50'34"N, 99°42'39"E, 3210 m asl.) on July 19, 2019, the conductivity was 16.3 ± 0.1 mS · cm – 1, pH was 9.14 ± 0.01, and water temperature was 15.5 ± 0.3 ° C. These data support previous findings that S. brightwellii is a brackish diatom species.

Zenodo (CERN European Organization for Nuclear Research)
Jishou University (CN), Nanjing Normal University (CN), Institute of Geology and Geophysics (AZ), Institute of Geology and Geophysics (CN)
Openalex Percentile: Top 27%
Data Analysis with R
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