Research Article |
Corresponding author: Brigitte Lods-Crozet ( brigitte.lods@vd.ch ) Academic editor: Patrick Rohner
© 2018 Joel Moubayed-Breil, Brigitte Lods-Crozet.
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:
Moubayed-Breil J, Lods-Crozet B (2018) On the genus Chaetocladius s. str. Kieffer, 1911 from Switzerland with descriptions of five new relic species occurring in glacial alpine springs and streams (Diptera, Chironomidae). Alpine Entomology 2: 15-34. https://doi.org/10.3897/alpento.2.22759
|
A description of the male adults of five Chaetocladius s. str. species (C. castellae sp. n., C. lencioniae sp. n., C. lodscrozetae sp. n., C. macunensis sp. n. and C. muttensis sp. n.) is provided based on material collected in some glacial alpine springs and cold streams located in the Swiss Alps (altitude 1800–2700 m). Male adult of the nearest Chaetocladius species known from Europe and neighbouring areas belong to: C. aedeagolobatus Rossaro, Magoga & Montagna, 2017; C. insolitus Caspers, 1987; C. gracilis
ChironomidaeOrthocladiinae new species glacial streams Swiss Alps conservation
Alpine freshwaters areas occurring in mountainous landscapes and high elevation are characterized by severe environment (
The Chironomidae family (Diamesinae and Orthocladiinae in particular) predominates in the high alpine ponds/lakes and stream network with a large number of species compared to the other macroinvertebrates such as other Diptera, Ephemeroptera, Plecoptera, Trichoptera, Oligochaeta (
Based on knowledge provided on the taxonomy, geographical distribution and ecology of the known Chaetocladius species from Europe and the Palaearctic Region (
Based on material collected between 1997–1998 and 2013 in high alpine springs and small cold streams located in the Swiss Alps, we here describe five new species of Chaetocladius s. str for which we discuss the taxonomic position, ecology and geographical distribution. A key to the known male adults from the catchment of the upper Rhône (including Muttbach glacier), with remarks on some related species from the Palaearctic Region are also provided.
Numerous sampling sites are located along some glacial streams and streamlets delimited by the three Alpine Swiss glacial catchments: - the Muttbach valley and the Rhône River alluvial plain “Gletschboden” in the Central Alps (46°34’12.258"N; 8°22’45.623"E); - the Macun streams and lakes in the Swiss National Park, Eastern Alps (46°43’39.678", 10°07’55.764"E).
The Mutt stream (length: 3600 m) originating from the Mutt glacier (area 0.6 km2, altitude 2582–3000 m) represents the major tributary of the upper Rhône catchment. It joins the Rhône River at the upper limit of a floodplain and contributes approximately 10 % (0.62 m3.s-1 in 1997) to the Rhône discharge (
The Rhône River alluvial plain “Gletschboden” is located in the upper catchment of the Rhône River. The major water source is the Rhône glacier (area 10.2 km2). Below the glacier snout, situated at an altitude of 2210 m, the Rhône River flows down a 400 m high granite cliff (slope 63 %) and enters an alluvial plain (length: 2000 m). During the last century, the retreat of the Rhône glacier has left valley moraine deposits and a braided channel pattern. The upper part of the Rhône is a kryal segment (
The Macun cirque site is a high alpine cirque (> 2600 m), which is located in the Eastern Alps (Swiss National Park). It was annexed to the park in 2000 and currently is an area designed for long-term monitoring of alpine water bodies (springs, streams, ponds, lakes). The region comprises more than 35 small lakes or permanent ponds and around 10 small temporary ponds scattered within two sub-basins. A north basin is fed mostly by snowmelt and groundwater, whereas the south basin is fed by glacial melt from a number of rock glaciers. Precipitation is low, typically being around 850 mm per year. Bedrock geology is crystalline (ortho-gneiss) rock. The area is above the tree line and the drainage area of each pond is characterised by a mixture of two types of land cover, rock and alpine grassland (
The sites in the Central Alps were investigated three times a year between 1996 and 1998, during the three major annual hydrological phases: in June during snowmelt, in August during ice melt and in September at low water level. The field protocols followed closely those established in the EU-project ‘AASER’ (
Ten sampling points were chosen randomly within each site. Depth, flow velocity and bed sediment composition were recorded at each of the 10 points before benthic sampling. The fauna was then collected into a 250-mm-mesh pond net at these points by kick sampling within a 30 × 30-cm area for 30 s. Adult material was collected using Malaise traps which were set up for a minimum of five days. In the Eastern Alps, during summer 2013, a supplementary survey was conducted to complete the standardized monitoring of small water bodies and streams within the Macun cirque (
All samples were preserved in 70 % Ethanol. Material of male adults were cleared of musculature in 90 % lactic acid (head, thorax, abdomen and anal segment) for about 60 to 80 minutes, which can be left overnight at room temperature without any detrimental effect or damage. The specimens were checked under a binocular microscope after 20 minutes in lactic acid to determine how the clearing was progressing. When clearing was complete the specimens were washed in two changes of 70 % Ethanol to ensure that all traces of lactic acid were removed. Compared to clearing with potassium hydroxide, or other clearing solutions, no deterioration of the typical “original” structure is reported by using lactic acid. All examined material was mounted in polyvinyl lactophenol, remaining material including paratypes were preserved in 70 % Ethanol. The eye on one side was dissected from the head, which ensures that the hairs on the inner margin of the eye are more clearly visible. Before the final slide mountings (dorsally) of the type and paratype material, the hypopygium including the IXth tergum, the anal point, the gonocoxite and the gonostylus, were viewed ventrally and laterally to examine and draw from both sides all the necessary details of the species. In particular, the ventral view of hypopygium was illustrated when anal point and tergite IX were removed. Morphological terminology and measurements largely follow
Holotype. Switzerland: Gletschboden alluvial plain, streamlet and springs located close to the upper catchment of the Rhône River, upstream to the Mutt stream confluence (station U2), altitude 1800 m, 30.IX.1998; 46°34’15.466"N, 8°22’47.054", 1 male adult, leg. B. Lods-Crozet. Environmental data of Rhône water are: crystalline water, conductivity 3.3–17.8 µS/cm; temperature 2–4 °C during late spring to late summer (June-September).
Paratypes. Switzerland: Mutt stream (Station M4), altitude 2100 m. 07.VIII.1997, 46°34’04.946"N, 8°24’17.159"E, 2 male adults, leg. B. Lods-Crozet. Environmental data of Mutt stream water are: crystalline water, conductivity: 61–183 µS/cm; temperature: 1–8 °C during late spring to late summer (June-September). In the streamlet and rheocrenes located close to station M4, conductivity ranged between 103 to 253 µS/cm; temperature 4.4. to 14.8 °C (
Holotype (mounted on 1 slide; GBIFCH 00460692) and one paratype (on slide) are deposited in the collections of the ‘Musée cantonal de Zoologie, Palais de Rumine, 6 place de la Riponne, CH-1014 Lausanne, Switzerland. Remaining paratype (on slide) is deposited in the collection of the senior author.
C. castellae sp. n. is separated from its nearest species (C. insolitus and C. muttensis sp. n.) by the following main characters: nearly similar shape of tergite IX, which bears a long nose-like dorsally projecting lamella-like structure; long triangular anal point; large inferior volsella; sinuous gonostylus. However, C. castellae sp. n. can be separated from the two previously cited species in having: palpomere 3 bearing 3–4 sensilla clavata (tubule-like) grouped in a ring; dorsal projecting lamella on tergite IX (more strongly projecting upwards), which bears 5–6 setae on ventral side; anal point long and triangular bearing 13–15 dorsal setae on its basal area and 5–6 smaller setae placed on proximal part; gonocoxite markedly swollen medially and bearing 1 row of 7–8 setae on inner dorsal margin, apex of inner dorsal margin with (or without) a distinct triangular to sub-rectangular tubercle; inferior volsella long, tongue-like, downwardly extending to distal part of gonocoxite; gonostylus nearly linear and typically sinuous.
Male imago (n = 3 male adults; Figs
Male adult of Chaetocladius spp. C. castellae sp. n.: 1, last flagellomere; 2, sensilla clavata on palpomere 3; 3, clypeus; 4, antepronotum, left side. C. muttensis sp. n.: 5, last flagellomere; 6, palpomere 3; 8, clypeus. C. insolitus: 7, apex of last flagellomere. Hypopygium of C. castellae sp. n.: 9, dorsal; 10, ventral with anal point and tergite IX removed; 11, dorsal lamellae of tergite IX; 12, anal point and tergite IX in lateral view; 13, left gonostylus in dorsal view.
Head. Eyes bare, hairs present on median part of inner eye margin. Temporals consist of 10 setae including 6 inner and 4 outer verticals. Antenna 650–660 µm long, 13-segmented; length (µm) of segments: 1, 50; 2–12, 30–35 (nearly sub-equal); last flagellomere 150–160; apex of last flagellomere (Fig.
Chaetocladius castellae sp. n. Length (µm) and proportions of legs PI, PII and PIII.
fe | ti | ta1 | ta2 | ta3 | ta4 | ta5 | LR | BV | SV | BR | |
---|---|---|---|---|---|---|---|---|---|---|---|
PI | 850 | 940 | 570 | 320 | 220 | 140 | 120 | 0.61 | 2.95 | 3.14 | 2.50 |
PII | 835 | 830 | 330 | 230 | 170 | 110 | 100 | 0.40 | 3.27 | 5.05 | 2.00 |
PIII | 940 | 950 | 550 | 280 | 220 | 120 | 100 | 0.58 | 3.38 | 3.43 | 2.40 |
Hypopygium in dorsal, ventral and lateral view as in Figs
Male adult of Chaetocladius spp. C. castellae sp. n. (paratype-1): 14–15, gonocoxite, lateral and dorsal; 16, gonostylus in dorsal view. C. castellae sp. n. (paratype-2): 17, hypopygium in dorsal view; 18, dorsal lamellae of tergite IX. C. insolitus: 19, gonostylus in dorsal view; 20, anal point and tergite IX in lateral view; 21, dorsal lamellae of tergite IX.
C. castellae sp. n. keys near C. insolitus and C. muttensis sp. n. based on the following resembling characters: presence of dorsal long projecting lamella-like structure; long triangular anal point; large inferior volsella; sinuous gonostylus. However, C. castellae sp. n. can be separated from the two previously cited species by the following main differentiating features: dorsal lamella-like structure on tergite IX is more strongly projecting and bearing setae on ventral side (Figs
The new species is named castellae in honour to our colleague Dr. Emmanuel Castella, who worked closely together with B. Lods-Crozet on the AASER project (AASER: Alpine and Arctic of Streams Ecosystem Research) during three years (from 1996 to 1998). He is currently senior research scientist at the University of Geneva and at the head of a research group, which focuses on aquatic invertebrate ecology.
Crenophilous species inhabiting cold mountain springs and cold streams with crystalline to calcareous water. Emergence: from July to early September.
Only known from its type locality: Central Swiss Alps.
Holotype. Switzerland: Mutt stream (station M4), altitude 2100 m, 09.VIII.1997; 46°34’04.946"N, 8°24’17.159"E, 1 male adult, leg. B. Lods-Crozet. Environmental data of Mutt stream water are: crystalline/calcareous water, conductivity 61–183 µS/cm; temperature: 1–8 °C during late spring to late summer (June-September). In the streamlet and rheocrenes located near station M4, conductivity ranged between 103 to 253 µS/cm; temperature 4.4. to 14.8 °C (
Paratype. 1 male adult, same locality and data as for holotype.
Holotype (mounted on 1 slide; GBIFCH 00460691) is deposited in the collections of the ‘Musée cantonal de Zoologie, Palais de Rumine, 6 place de la Riponne, CH-1014 Lausanne, Switzerland. The single paratype is deposited in the collection of the senior author.
C. lencioniae sp. n. keys near the following two species: C. gracilis, based on the shape of both tergite IX and the anal point; C. antipovae, based on the shape of the inferior volsella. However, C. lencioniae sp. n. can be distinguished in having: tergite IX semi-circular; sternite IX typically circle-like in shape; anal point markedly pointed apically and bearing setae on proximal part; virga faint, consists of 2 long teeth; gonostylus massively spherical to bulb-shaped, anterior margin swollen medially, ending in 3 characteristic small teeth comb-like placed close to the base of megaseta, posterior margin rounded, projecting downwards and terminating in a pointed sclerotized apical tooth; crista dorsalis large tooth-like, sclerotized and spherical, smooth with rounded apex, placed pre-apically close to megaseta (clearly visible in dorsal and ventral view).
Male imago (n = 2 male adults; Figs
Male adult of Chaetocladius lencioniae sp. n.: 22, last flagellomere and preceding segment; 23, clypeus; 24, scutellum. Hypoygium: 25–26, dorsal (25) and ventral (26) with anal point and tergite IX removed; 27, virga; 28, anal point and tergite IX in lateral view; 29, left gonostylus, dorsal; 30, right gonostylus, ventral; 31, gonocoxite and gonostylus in lateral view.
Head. Eyes bare, hairs on inner eye margin absent. Temporals consist of 9–10 uniserial setae including 7–8 inner and 2 outer verticals. Antenna 1370 µm long, 12-segmented; last flagellomere (Fig.
Chaetocladius lencioniae sp. n. Length (µm) and proportions of legs PI, PII and PIII.
fe | ti | ta1 | ta2 | ta3 | ta4 | ta5 | LR | BV | SV | BR | |
---|---|---|---|---|---|---|---|---|---|---|---|
PI | 810 | 1020 | 710 | 430 | 260 | 165 | 140 | 0.70 | 2.55 | 2.58 | 3.10 |
PII | 840 | 850 | 390 | 230 | 150 | 85 | 100 | 0.46 | 3.68 | 4.33 | 2.75 |
PIII | 910 | 1060 | 560 | 315 | 240 | 100 | 125 | 0.43 | 3.24 | 3.52 | 3.40 |
Hypopygium in dorsal, ventral and lateral view as in Figs
C. lencioniae sp. n. keys near C. gracilis, based on the shape of both tergite IX and the anal point (
The new species is named lencioniae in honour of our colleague Dr. Valeria Lencioni from the Museum of Trento (Italy), who is active as curator ‘Conservatore’ and hydrobiologist in contributing to preserve the biological and ecological quality of water and environment in Trento and surrounding areas.
High mountain springs and cold streams with crystalline to calcareous water. Emergence: from July to early September.
C. lencioniae sp. n. is only known from its type locality. It can be considered as a typical biogeographic representative of high mountain rheocrenes and cold streams delimited by some Swiss Alpine glaciers.
Holotype. Switzerland: Gletschboden alluvial plain, streamlet and springs located close to the upper catchment of the Rhône River, upstream of the Mutt stream confluence (station U2), altitude 1800 m, 08.IX.1998, 46°34’15.466"N, 8°22’47.054", 1 male adult, leg. B. Lods-Crozet. Environmental data of Rhône water are: crystalline water, conductivity 3.3–17.8 µS/cm; temperature 2–4 °C during late spring to late summer (June-September).
Paratypes (all leg. B. Lods-Crozet). Switzerland. 1 male adult, same locality and data as for holotype. 2 male adults, Gletschboden, upstream, altitude 1800 m, 30.IX.1999. 1 male adult, Mutt stream (station M4), altitude 2100 m, 07.VIII.1997, Swiss coordinates: 2’674’059, 1’157’904. Environmental data of Mutt stream water are: crystalline/calcareous water; conductivity: 61–183 µS/cm; temperature: 1–8 °C during late spring to late summer (June-September). In the streamlet and rheocrenes located near the station M4, conductivity ranged between 103 to 253 µS/cm; temperature 4.4. to 14.8 °C (
Holotype (mounted on 1 slide; GBIFCH 00460693) and 1 male paratype (on 1 slide; GBIFCH 00460694) are deposited in the collections of the ‘Musée cantonal de Zoologie, Palais de Rumine, 6 place de la Riponne, CH-1014 Lausanne, Switzerland. Remaining paratypes are deposited in the collection of the senior author.
The nearest species to C. lodscrozetae sp. n. are C. dissipatus, C. holmgreni, C. egorych and C. aedeagolobatus Rossaro, Magoga & Montagna, 2017 from which it can be separated in having: clypeus half diamond-like, with V-shaped posterior side, bearing 6 setae placed in 2 rows; palpomere 4 distinctly truncate apically, sensilla clavata present on segment 3 including 5 sparsely distributed and 3 (tubule-like) grouped on a ring placed distally; ultimate flagellomere 465–475 µm long, distinctly clubbed, AR about 1; tergite IX broad and semi-circular with 16–22 dorsal setae placed on its posterior part; anal point long, triangle-like, nearly parallel-sided and distinctly thin between base and apex, dorsally bearing a characteristic massive lamella-like orally directed structure which is markedly visible in lateral view, lamella is cup-like in dorsal view, composed of 2 well separate margins, inner margin linear and bare, outer margin markedly undulated and bearing 7–8 dorsolateral setae, inside area bare; virga typical inversed V-shaped, composed of 6–7 posteriorly directed spines; gonocoxite broad basally and narrowed distally, abruptly tapering before apex; inferior volsella extending from base of gonocoxite to its distal part, consist of 2 lobes (dorsal lobe markedly projecting medially and beak-like in shape, distal part distinctly swollen and pouch-like in shape; ventral lobe swollen basally and tapering distally, ending nearly at tip of gonocoxite, inner ventral margin bearing about 11 strong setae; gonostylus half bulb-shaped ending with a distinct hyaline rounded distal area, anterior side with orally directed small setae, posterior margin markedly rounded bearing a double inner apical margin, anterior margin varies from straight to convex, crista dorsalis low and indistinct.
Male imago (n = 4 male adults; Figs
Male adult of Chaetocladius lodscrozetae sp. n.: 32–33, palpomeres 3–4 with sensilla clavata on palpomere 3; 34, last flagellomere; 35, clypeus; 36–37, hypopygium, dorsal (36) and ventral (37) with anal point and tergite IX removed; 38, virga, two aspects; 39, ventral view of inferior volsella; 40, anal point and tergite IX in lateral view; 41, left gonocoxite in lateral view; 42–44, gonostylus, lateral (42), dorsal (43) and dorso-lateral (44).
Head. Eyes bare, hairs present anterior part of inner eye margin. Temporals consist of 11–12 setae including 7–8 uniserial inner and 4 outer verticals. Antenna 915–920 µm long, 13-segmented; ultimate flagellomere 465–475 µm long, distinctly clubbed distally and bearing a dense brush of curved sensilla chaetica apically, apex (Fig.
Chaetocladius lodscrozetae sp. n. Length (µm) and proportions of legs PI, PII and PIII.
fe | ti | ta1 | ta2 | ta3 | ta4 | ta5 | LR | BV | SV | BR | |
---|---|---|---|---|---|---|---|---|---|---|---|
PI | 790 | 885 | 560 | 320 | 240 | 150 | 110 | 3.63 | 2.73 | 2.99 | 2.20 |
PII | 820 | 830 | 370 | 230 | 180 | 110 | 100 | 3.45 | 3.26 | 4.46 | 2.90 |
PIII | 890 | 980 | 585 | 325 | 260 | 145 | 110 | 3.60 | 3.43 | 3.20 | 2.30 |
Hypopygium in dorsal, ventral and lateral view as in Figs
C. lodscrozetae sp. n. keys close to C. dissipatus, C. holmgreni, C. egorych and C. aedeagolobatus from which it can be separated in having: sensilla clavata present on palpomere 3 including 5 sparsely distributed and 3 grouped on a characteristic ring placed distally; tergite IX broad and nearly semi-circular with 10–11 setae on its posterior area, presence of a characteristic massive rounded prominence extending from the median area to base of anal point; anal point elongated and parallel-sided which is distinctly thicker on its proximal half; virga inversed V-shaped, composed of 6–7 posteriorly directed spines; gonocoxite broad basally and narrowed distally, abruptly tapering before apex; inferior volsella extending from base of gonocoxite to its distal part, consist of a large lobe which is pouch-like in shape, inner margin terminating in a hyaline nose-like lobe which is bare and bent downwards; gonostylus nearly semi-circular, distal part of posterior margin hyaline and bare, anterior side with orally directed small setae, anterior margin varies from straight to convex.
The new species is named lodscrozetae in honour of Dr. Brigitte Lods-Crozet from the Cantonal Museum of Zoology of Lausanne (Switzerland), who is still active as researcher and hydrobiologist in contributing to preserve the biological and ecological quality of water and environment in Switzerland.
Glacial springs and cold mountain streams with crystalline to calcareous water. Emergence: from July to early September.
C. lodscrozetae sp. n. is only known from rheocrenes and lotic habitats delimited by the Gletschboden floodplain, the Mutt stream and streamlet, Swiss Alps, altitude 1800–2100 m.
Holotype. Switzerland: Macun cirque, streamlet and rheocrenes, left shore of Immez Lake, alt. 2616 m, 27.VII.2013; 46°43’39.678", 10°07’55.764"E, 1 male adult, leg. B. Lods-Crozet. Environmental data from inlet of Immez Lake: crystalline water, conductivity 5.9 µS/cm; temperature 11.6 °C, pH 6.7 (
Paratypes. 3 male adults, same locality and data as for holotype.
Holotype (mounted on 1 slide; GBIFCH 00460690) is deposited in the collections of the ‘Musée cantonal de Zoologie, Palais de Rumine, 6 place de la Riponne, CH-1014 Lausanne, Switzerland. Paratypes are deposited in the collection of the senior author.
Based on the unusual and unique shape of the inferior volsella, C. macunensis sp. n. can be easily separated from other members of the Chaetocladius genus by the following characters: clypeus semi-circular bearing 7 setae placed in 1 row along an arc line; antenna and ultimate flagellomere relatively short (respectively 600–660 and 130–200 µm long), apex distinctly clubbed and bearing 1 pre-apical seta, AR markedly low (0.25–0.35); tergite IX sub-triangular and lacking dorsal setae; anal point triangular, uniformly narrowed, apex rounded, base with 6 setae inserted dorsolaterally (3 on each side); virga horseshoe-shaped, median tooth sinuous and S-like in shape; gonocoxite markedly swollen medially and distally, inner dorsal margin without stout setae, inner ventral margin swollen medially; inferior volsella consists of 1 single large and typical lobe, which bears numerous strong stout setae on its inner margin; gonostylus elongated and nearly linear, anterior side covered with setae, posterior margin nearly straight.
Male imago (n = 2 male adults; Figs
Male adult of Chaetocladius macunensis sp. n.: 45, palpomeres 2–3; 46, last flagellomere and the two preceding segments; 47, clypeus; 48, head, thorax and first abdominal segment; 49, antepronotum, left side; 50, tarsomeres 2–4 of PIII; 51, anal point and tergite IX in lateral view; 52–53, hypopygium, dorsal (52) and ventral with anal point and tergite IX removed (53); 54, virga; 55, left gonostylus, dorsal; 56, right gonostylus, lateral; 57, anal point, gonocoxite and gonostylus in lateral view.
Head, thorax and tergite I as in Fig.
Chaetocladius macunensis sp. n. Length (µm) and proportions of legs PI, PII and PIII.
fe | ti | ta1 | ta2 | ta3 | ta4 | ta5 | LR | BV | SV | BR | |
---|---|---|---|---|---|---|---|---|---|---|---|
PI | 550 | 650 | 410 | 290 | 210 | 120 | 100 | 0.63 | 2.24 | 2.93 | 2.40 |
PII | 675 | 655 | 290 | 160 | 140 | 91 | 82 | 0.44 | 3.42 | 3.24 | 2.10 |
PIII | 725 | 775 | 420 | 220 | 190 | 120 | 98 | 0.54 | 3.06 | 3.57 | 2.30 |
Hypopygium in dorsal, ventral and lateral view as in Figs
C. macunensis sp. n. can be easily separated from its nearest species (C. tenuistylus, sensu
The new species is named macunensis after the Swiss Alpine cirque of Macun, which was annexed to the Swiss National Park in 2000 (canton of Graubunden).
C. macunensis sp. n. is apparently confined to cold glacial streams and the inflow section of lakes delimited by the Macun cirque where water is typically crystalline. Emergence is recorded from July to early September.
A typical biogeographic representative of Alpine high mountain springs and glacial streams located in the eastern Swiss Alps area. Currently, C. macunensis sp. n. is only known from the Macun cirque.
Holotype. Switzerland: upper basin of the Mutt glacial stream (station M5), altitude 1800 m, 03.VIII.1997, 46°34’12.347"N, 8°22’51.363", 1 male adult, leg. B. Lods-Crozet. Environmental data of Mutt stream water are: crystalline to calcareous water, conductivity 61–183 µS/cm; temperature: 1–8 °C during late spring to late summer (June-September).
Paratype. Switzerland: upper basin of Mutt stream (station M4), altitude 2100 m, 09.VIII.1997, 46°34’04.946"N, 8°24’17.159"E, 1 male adult, leg. B. Lods-Crozet. Environmental data of Mutt stream water are: crystalline to calcareous water, conductivity 61–183 µS/cm; temperature: 1–8 °C during late spring to late summer (June-September). In the streamlet and springs located close to station M4, conductivity ranged between 103 to 253 µS/cm; temperature 4.4 to 14.8 °C (
Holotype (mounted on 1 slide; GBIFCH 00460695) is deposited in the collections of the ‘Musée cantonal de Zoologie, Palais de Rumine, 6 place de la Riponne, CH-1014 Lausanne, Switzerland. The single paratype is deposited in the collection of the senior author.
C. muttensis sp. n. can be separated from its nearest species (C. insolitus and C. castellae sp. n.) by the following characters: tergite IX bearing a characteristic dorsal lamella-structure which is bare and slightly projecting close to the dorsal side of tergite IX; anal point triangular, widely broad at base and bearing 6 setae at base (3 on each side); virga faint but present, consists of 3 long spines; inferior volsella tongue-like with distal outer margin well separated from inner margin of gonocoxite; inner margin of gonocoxite not swollen medially and lacking row of strong setae; gonostylus gradually narrowing distally, anterior area with a characteristic undulate line placed distally and reaching base of megaseta, posterior margin with a typical lob-like expansion placed medially and directed downwards.
Male imago (n = 2 male adults; Figs
Head. Eyes bare, hairs absent on median part of inner eye margin. Temporals consist of 8 setae including 5 inner and 3 outer verticals. Antenna 575–585 µm long, 13-segmented; last flagellomere (Fig.
Chaetocladius muttensis sp. n. Length (µm) and proportions of legs PI, PII and PIII.
fe | ti | ta1 | ta2 | ta3 | ta4 | ta5 | LR | BV | SV | BR | |
---|---|---|---|---|---|---|---|---|---|---|---|
PI | 840 | 895 | 550 | 310 | 205 | 120 | 100 | 0.62 | 3.11 | 3.15 | 1.50 |
PII | 815 | 790 | 370 | 215 | 160 | 105 | 95 | 0.47 | 3.45 | 4.34 | 2.20 |
PIII | 890 | 925 | 520 | 290 | 210 | 115 | 95 | 0.56 | 3.29 | 3.49 | 3.25 |
Hypopygium in dorsal, ventral and lateral view as in Figs
Male adult of Chaetocladius muttensis sp. n. 58–59, hypopygium, dorsal (58) and ventral with anal point and tergite IX removed (59); 60–61, virga, two aspects; 62, tergite IX and anal point in lateral view; 63, right gonostylus, lateral; 64, left gonostylus, distal part (dorsal); 65, anal point, gonocoxite, tergite IX and gonostylus in lateral view.
C. muttensis sp. n. keys near C. insolitus and C. castellae sp. n. from which it can be separated in having: tergite IX with a characteristic dorsal cup-like lamella-structure, bare and slightly projecting (Fig.
The new species is named muttensis after the Swiss Alpine glacial Mutt stream, which is located in the upper basin of the Rhône River in the central Swiss Alps.
C. muttensis sp. n. only occurs in the Mutt glacial stream where larvae are apparently confined to the lotic part of springs and the rhithral (crystalline to calcareous water). Emergence from July to early August. Associated species found in the same locality include: C. laminatus Brundin, 1947; C. cf. longivirgatus Stur & Spies, 2011; C. suecicus (Kieffer, 1916); Heleniella helvetica.
C. muttensis sp. n. is only known from its type locality, which is delimited by the upper basin of the Mutt glacial stream.
1 | Tergite IX with a dorsal lamella structure located on median area (Figs |
2 |
– | Tergite IX without such dorsal lamella structure | 3 |
2 | Gonostylus gradually narrowing distally, anterior area with a typical undulate line extended from median part to base of megaseta, posterior margin rounded and bearing a characteristic lobe-like expansion directed downwards (Figs |
C. muttensis sp. n. |
– | Gonostylus linearly elongated, both anterior and posterior margin sinuous (Figs |
C. castellae sp. n. |
3 | Gonostylus bulbous and spherical (Figs |
4 |
– | Gonostylus not as above, slender, semi-circular with rounded posterior margin (Figs |
5 |
4 | Inferior volsella (Figs |
C. lencioniae sp. n. |
5 | Tergite IX bearing a dorsal elevated massive hump, located distally (Figs |
C. lodscrozetae sp. n. |
– | Tergite IX without such elevated dorsal hump (Fig. |
C. macunensi sp. n. |
The nearest Chaetocladius species to the five diagnosed and described species include: C. insolitus for C. castellae sp. n.; C. gracilis and C. antipovae for C. lencioniae sp. n.; C. dissipatus, C. holmgreni, C. egorych and C. aedeagolobatus for C. lodscrozetae sp. n. Based on some specific characters found in the male adult of C. macunensis sp. n (shape of anal point, inferior volsella and virga), this new species can be placed near C. tenuistylus Brundin, 1947 (sensu
Worldwide there are actually about 79 known Chaetocladius species, which include the hitherto listed 69 species by
Currently, only seven Chaetocladius species are known from Switzerland: C. coppai Moubayed-Breil, 2017; C. laminatus Brundin, 1947; C. cf. longivirgatus Stur & Spies, 2011; C. melaleucus (Meigen, 1818); C. perennis (Meigen, 1830); C. piger (Goetghebuer, 1913); C. suecicus (Kieffer, 1916). Consequently, the description here of the five new Chaetocladius species increases the total number in the genus to 12 known valid species for this country.
Geographical distribution of the five new described species is currently restricted to the two Alpine Swiss glacial catchments (Figs
It is of interest to note that none of the new described species in the present work is identical to any of those described recently from southern side of the Alps (
The presence of the five new species in some high mountain Alpine ranges of Switzerland highlights the importance of some cold glacial enclaves, considered as hotspots of endemism, in the preservation and persistence of autochthonous and sensitive alpine relic species. Such species are considered as relevant biogeographically representative and their loss would be biologically indicative of the global warming and climate change.
Special thanks are due to our colleagues Patrick Ashe (Dublin) and Martin Spies (ZSM, Munich) for their constructive comments and suggestions, which markedly improved the manuscript. The authors express their thanks to Michel Sartori (Musée cantonal de Zoologie, Lausanne) for his kind assistance as well to Jade and Marie-Helene Breil-Moubayed for achieving the measurements of the leg ratios.