Chaetoceros coloradensis Li & Kociolek, 2016

Li, Jing, Kociolek, J. Patrick & Gao, Yahui, 2016, Chaetoceros coloradensis sp. nov. (Bacillariophyta, Chaetocerotaceae), a new inland species from Little Gaynor Lake, Colorado, North America, Phytotaxa 255 (3), pp. 199-213 : 202-205

publication ID

https://doi.org/ 10.11646/phytotaxa.255.3.2

persistent identifier

https://treatment.plazi.org/id/921287A7-FFB2-FFEC-30D1-64F9AF42F8A4

treatment provided by

Felipe

scientific name

Chaetoceros coloradensis Li & Kociolek
status

sp. nov.

Chaetoceros coloradensis Li & Kociolek , sp. nov. ( Figs 2–5 View FIGURES 2–8 , 9–17 View FIGURES 9–13 View FIGURES 14–17 , 27–35 View FIGURES 27–35 )

Cells solitary, rectangular in girdle view, one chloroplast per valve, Cells 3.0–9.5 μm in the apical axis, 2.4–8.1 μm in the transapical axis, and 2.0–9.0 μm in the pervalvar axis. Valves elliptical, sometimes nearly circular, lacking processes. Valve surface flat. An anastomosing pattern of siliceous ribs on valve face. Girdle bands delicate, weak costae on the bands. Setae thin, hollow, not fused, and closed at the end. Spiral rows of rectangular pores and tiny spines on setae. Pores smaller at the base of setae. Setae offset 30 to 45° between setae on opposite valves. Resting spores heavily silicified, smooth on the surface. Primary valve convex. Secondary valve with variable morphology, usually with a chimney-like protrusion, sometimes with almost the same apical length as the primary valve. Puncta randomly distributed on the mantle of the secondary valve. A siliceous annulus is present on the mantle of secondary valve.

Type: — UNITED STATES. Colorado: Boulder County, Little Gaynor Lake (40.12° N, 105.12° W), May 3 rd 2012. (holotype: COLO!, individual on slide JPK 9560, Kociolek Collection, here illustrated as Fig. 4 View FIGURES 2–8 . Isotype: AU!, slide MMDL 120503).

Etymology: —Named for the state where the species was collected.

Observations: —Over 100 vegetative cells have been measured. Frustules are solitary, delicate, containing only one chloroplast ( Figs 2–3 View FIGURES 2–8 ). The cells are rectangular in girdle view ( Figs 3–5 View FIGURES 2–8 ), sometimes nearly square ( Fig. 3 View FIGURES 2–8 ). Valve surfaces are flat ( Figs 3–5 View FIGURES 2–8 ), an anastomosing pattern of narrow ribs can be found on the valve face ( Fig. 9 View FIGURES 9–13 ). No processes are present on the valve ( Fig. 9 View FIGURES 9–13 ). Cells are 3.0–9.5 μm in the apical axis, 2.4–8.1 μm in the transapical axis, and 2.0–9.0 μm in the pervalvar axis. Very weak siliceous costae are ornamented on girdle bands ( Fig. 10 View FIGURES 9–13 ). Setae are thin, 3–4 times longer than apical axis. Setae on opposite valves have different orientation, with a 30–45° difference between these on opposite valves ( Fig. 2 View FIGURES 2–8 ). Spiral rows of rectangular pores, spiral rows of minute spines on setae ( Fig. 13 View FIGURES 9–13 ), and the pores, are smaller at the base of the setae ( Fig. 11 View FIGURES 9–13 ). Setae are closed at the end tip ( Fig. 12 View FIGURES 9–13 ).

Nearly 300 resting spores have been measured. Resting spores are smooth, and form inside of vegetative cells ( Fig. 5 View FIGURES 2–8 ). Apical length of primary valve is 2.4–13.8 μm, width of the primary valve is 2.6–10.0 μm, height of primary valve is 3.6–6.2 μm. Length of secondary valve is 1.0–6.0 μm. Spore height ranges from 4.8 to 11.0 μm. The shape of resting spores is highly variable ( Figs 27–35 View FIGURES 27–35 ). The primary valve is convex, sometimes concave at the center ( Fig. 28 View FIGURES 27–35 ). The secondary valve sometimes has a chimney-like protrusion ( Fig. 15 View FIGURES 14–17 ). The secondary valve is not always substantially narrow when compared with the apical length of the primary valve ( Figs 16 View FIGURES 14–17 , 27, 33 View FIGURES 27–35 ). In addition, the secondary valve can be narrow and long ( Fig. 34 View FIGURES 27–35 ). The margin of the secondary valve is flat ( Fig. 29 View FIGURES 27–35 ) or concave ( Fig. 30 View FIGURES 27–35 ). Additionally, the secondary valve can be trapezoidal ( Fig. 29 View FIGURES 27–35 ) or inverted trapezoidal ( Figs 28, 32 View FIGURES 27–35 ) in shape. The secondary valve mantle might be elongated ( Figs 17 View FIGURES 14–17 , 33, 35 View FIGURES 27–35 ), or even be separated from the primary valve ( Fig. 32 View FIGURES 27–35 ). The primary and secondary valves can also be similar to one another ( Fig. 31 View FIGURES 27–35 ). There is a siliceous annulus at the margin of the secondary valve mantle ( Fig. 15 View FIGURES 14–17 ). Puncta are randomly distributed on the secondary valve mantle ( Figs 15 View FIGURES 14–17 , 27 View FIGURES 27–35 ).

Phylogenetic analyses: —The ML and MrB for LSU have the same topologies ( Fig. 24 View FIGURE 24 ). In these trees, all solitary Chaetoceros species, including C. coloradensis , fall into clade V with high support (96% ML/100% MrB). Within the clade V, C. coloradensis clusters with C. muelleri (strain GSL5) and C. gracilis F. Schütt (1895: 42) with high support (100% ML/ 100% MrB); while inside the small clade formed by these three species, C. muelleri clusters with C. gracilis and forms a smaller clade (ML 80%/99% MrB), which suggests that C. muelleri is more closely related to C. gracilis in the LSU analysis.

For SSU, the ML and MrB analyses also have the same topologies ( Fig. 25 View FIGURE 25 ). However, members of the section Simplicia do not fall into a single clade in the SSU analyses, indicating that the section Simplicia is not monophyletic. Although most Simplicia taxa are in clade IV (62% ML/87% MrB), two strains of C. muelleri , two strains of C. calcitrans f. pumilus Takano (1968: 3) and two strains of C. calcitrans ( Paulsen 1905: 6) Takano (1968: 1) fall outside of this clade. These two strains of C. muelleri form clade I with C. decipiens ( Cleve 1873: 11) and C. cf. lorenzianus Grunow (1863: 157) with high support (100% ML/100% MrB). The four strains of C. calcitrans and C. calcitrans f. pumilus form clade II with high support (100% ML/100% MrB). Chaetoceros coloradensis falls into clade IV and forms a sister clade with the strain of C. muelleri collected from Great Salt Lake, but the support is low (60% ML/63% MrB).

The ML and MrB analyses generated the same topologies for the phylogenetic tree of LSU+SSU ( Fig. 26 View FIGURE 26 ). Solitary Chaetoceros species fall into clade V with high support (98% ML/100% MrB). Chaetoceros coloradensis forms a small clade with C. muelleri (strain GSL5) and C. gracilis with high support (100% ML & MrB). Inside this small clade, C. coloradensis forms a clade with C. muelleri (strain GSL5) (88% ML and 100% MrB).

The analyses of LSU, SSU and LSU+SSU provide high support that the position of C. coloradensis is close to C. muelleri (strain GSL5) isolated from Great Salt Lake. The molecular analyses also indicate C. coloradensis is one member of the clade composed by solitary Chaetoceros taxa.

COLO

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