Fluminicola warnerensis, Hershler & Liu & Frest & Johannes, 2007

Hershler, Robert, Liu, Hsiu-Ping, Frest, Terrence J. & Johannes, Edward J., 2007, Extensive diversification of pebblesnails (Lithoglyphidae: Fluminicola) in the upper Sacramento River basin, northwestern USA, Zoological Journal of the Linnean Society 149 (3), pp. 371-422 : 388-393

publication ID

https://doi.org/ 10.1111/j.1096-3642.2007.00243.x

DOI

https://doi.org/10.5281/zenodo.10544941

persistent identifier

https://treatment.plazi.org/id/03BC4773-0B44-F704-4093-F9041B92FF72

treatment provided by

Felipe

scientific name

Fluminicola warnerensis
status

sp. nov.

FLUMINICOLA WARNERENSIS SP. NOV. (WARNER

PEBBLESNAIL)

Type material: Holotype ( Fig. 10A View Figure 10 ), USNM 1020652 About USNM , Parsnip Springs, south of South Warner Road (FS64, also designated as 39NO1) in wet, open meadow, Modoc National Forest , Lassen County, California

(729680 E, 4559760 N, 1957 m), 18 September 2001, TF, EJ . Paratypes (from same lot), USNM 1020653 About USNM .

Referred material: CALIFORNIA. Lassen County: USNM 1020655 About USNM , spring brook in sedge meadow on east side of Blue Lake just east of Blue Lake Campground access road, c. 0.16 km east of lake, Modoc National Forest (728375 E, 4558240 N, 1853 m), 17 September 2001 TF, EJ.— USNM 1020656 About USNM , spring creek to Blue Lake on west side of FS64, c. 0.81 km south-east of Blue Lake Campground, Modoc National Forest (729020 E, 4557760 N, 1894 m), 18 June 1994 TF, EJ. – USNM 883557 About USNM , USNM 883561 About USNM , spring tributary to Blue Lake (729770 E, 4557577 N, 1830 m), 2 June 1993 DS. – USNM 883559 About USNM , spring tributary to large meadow, Harvey Creek drainage, Jess Valley (725112 E, 4563474 N), 2 June 1993 DS. – USNM 883564 About USNM , stream tributary to south end of Blue Lake (728489 E, 4558041 N, 1830 m), 1 July 2003 DS. Modoc County: USNM 1020654 About USNM , Soup Spring just north of Soup Spring Campground, Modoc National Forest (728000 E, 4576530 N, 2067 m), 17 September 2001 TF, EJ. – USNM 1020789 About USNM , Soup Creek on north side of FS40N24 crossing, Modoc National Forest (726000 E, 4574760 N, 1702 m), 17 September 2001 TF, EJ. – USNM 1020657 About USNM , springs south-east of Hilton on south side of Hilton Road, 0.48 km west of Hilton Creek (689280 E, 4567560 N, 1769 m), 18 September 2001, TF, EJ. – USNM 1020658 About USNM , head spring of Rush Creek west of FS40N18, north-west end of Manzanita Ridge, Modoc National Forest (682590 E, 4573530 N, 1903 m), 20 July 2002 TF, EJ. – USNM 1020659 About USNM , Miller Spring run, 0.32 km south of FS41N11, Miller Gulch, Modoc National Forest (664700 E, 4577150 N, 1586 m), 22 September 2001 TF, EJ. – USNM 1020790 About USNM , springs in gulch east of Miller Gulch, 0.48 km on road off (south of) FS41N12, Modoc National Forest (667260 E, 4576920 N, 1513 m), 22 September 2001, TF, EJ .

Diagnosis: Differs from similar F. turbiniformis in its larger size (SH, SW, P = 0; data for latter given below), darker body pigment, less prominent sperm storage area in the coiled oviduct, complete overlap of the seminal receptacle by the albumen gland, broader bursa copulatrix, absence of a seminal receptacle duct, and frequent occurrence of a papilla-like capsule gland opening. Distinguished from geographically proximal F. erosus and F. lunsfordensis (both described below) by its more elongate shell, more convex shell whorls, single basal cusp of the central radular tooth, and enlarged large central cusp of the lateral radular tooth. Also differs from the former in its larger size and from the latter by its weakly angled adapical portion of the aperture.

Description: Shell ( Fig. 10A–K View Figure 10 ; Table 4) turbiniform to ovate-conic, rarely having eroded spire; height, 2.40–4.68 mm; whorls, 3.5–4.0. Protoconch 1.4 whorls, diameter approximately 0.70 mm. Teleoconch whorls medium to weakly convex, sometimes wider below, narrowly shouldered. Last 0.125 whorl rarely disjunct. Aperture broad, angled above. Parietal lip complete, slightly disjunct and thickened in larger specimens. Columellar lip usually medium width and overlapping part of umbilical region, sometimes narrow. Outer lip usually thin, prosocline. Shell anomphalous or narrowly rimate, umbilical region sometimes excavated. Periostracum tan, light brown, or red. Last 0.5 whorl of operculum very weakly frilled ( Fig. 10L View Figure 10 ). Central radular tooth approximately 53 µm wide, cutting edge convex, lateral cusps four (one tooth having three); central cusp pointed; basal cusps one; basal tongue Vshaped, equal to lateral margin ( Fig. 10O View Figure 10 ). Lateral tooth face broadly rectangular; central cusp rounded, lateral cusps two (inner), three to five (outer); outer wing flexed, medium length ( Fig. 10N View Figure 10 ). Inner marginal teeth having 20–26 cusps ( Fig. 10M, N View Figure 10 ). Outer marginal teeth having 24–38 cusps; basal wing rectangular ( Fig. 10M View Figure 10 ). Head-foot dark brown, almost black. Ctenidium connected to pericardium by short, efferent branchial vessel; ctenidial filaments approximately 17, without pleats. Osphradium elongate, positioned opposite middle of ctenidium. Female reproductive anatomy shown in Figure 6B View Figure 6 . Bursa copulatrix horizontal, pyriform or triangular, duct short. Seminal receptacle medium-sized, overlapped by albumen gland. Albumen gland having pronounced rectal furrow. Capsule gland a little longer than albumen gland. Genital aperture a short slit, usually forming a small papilla. Penis medium-sized, narrow, coiled, distal end pointed ( Fig. 7B View Figure 7 ). Base and medial section grey, pigment concentrated along penial duct. Penial duct near centrally positioned, weakly undulating in proximal section.

Distribution: Distributed within the drainage of the south fork of the Pit River, and along the Pit River just above Big Valley (upper Pit River basin) ( Fig. 9 View Figure 9 ).

Etymology: The species name refers to the type locality area in the Warner Mountains, north-eastern California.

Remarks: Populations allocated to F. warnerensis vary somewhat in shell form ( Fig. 10A–K View Figure 10 ). Nonetheless they share diagnostic morphological features, are little divergent genetically (0–0.6% for COI, 0–0.3% for cytb), and were consistently depicted as a well-supported monophyletic group ( Figs 2–4 View Figure 2 View Figure 3 View Figure 4 ), justifying recognition as a single species. In all of the phylogenetic analyses, F. warnerensis was depicted as most closely related to F. turbiniformis , with moderate to strong bootstrap support (75–100%). Haplotypes of these two species differ by 2.3–2.6% ( COI) and 3.6–3.9% (cytb).

This species was referred to as Fluminicola n. sp. 13 by Frest & Johannes (1995a).

FLUMINICOLA LUNSFORDENSIS SP. NOV. ( LUNSFORD

TF

Department of Mineral Resources

EJ

Ein Yabrud collection catalogue entries at The Hebrew University

COI

University of Coimbra Botany Department

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