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Fig. 5 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 5 Camera lucida drawings of Triassic orthoceratoid genera (not to scale) in comparison with Michelinoceras. Phattalungoceras is not shown here, as the only specimen is too poorly preserved to confidently reconstruct its internal structures, although it appears to resemble Pseudotemperoceras. A Michelinoceras michelini, after Barrande (1870; pl. 381; fig. 14); B Trematoceras elegans, after Schindewolf (1933; fig. 5); C Paratrematoceras shevyrevi, after Schastlivceva (1988 pl. 1, fig. 3); D Pseudotemperoceras nyalamense, after Chen (1981; text-fig. 2); E Pseudotemperoceras pulchrum, after Schastlivceva (1988; pl. 1, fig. 5c)

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Fig. 6 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 6 Comparison of embryonic shells of selected orthoceratoids. A Trematoceras cf. politum (= T. elegans), Late Triassic, Carnian, after Schindewolf (1933; fig. 5). B Michelinoceras michelini, late Silurian, Ludlow, after Ristedt (1968; fig. 3.1b); C Pseudorthoceras knoxense, Carboniferous, Serpukhovian, after Kröger & Mapes (Kröger & Mapes, 2004; fig. 5.9)

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Fig. 7 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 7 Simplified time-scaled phylogeny demonstrating possible relationships of the Trematoceratidae to other orthoceratoids and coleoids. Note that Orthoceras and Michelinoceras are more closely related to coleoids than they are to trematoceratids under this concept. Several groups are omitted here for clarity (e.g., Nautilida, Ammonoida). The questionable Zhuravlevia is here excluded

Fig. 7 in First description of Onchocerca jakutensis (Nematoda: Filarioidea) in red deer (Cervus elaphus) in Switzerland

Fig. 7. Microfilaria showing transverse annulation and irregular shape of swollen anterior end (magnitude of annulation and swelling might be exaggerated by artefact of fixation).

Fig. 5 in First description of Onchocerca jakutensis (Nematoda: Filarioidea) in red deer (Cervus elaphus) in Switzerland

Fig. 5. External cuticular annulation (A) of O. jakutensis female with interruption over lateral field.

Fig. 4. a and b in First description of Onchocerca jakutensis (Nematoda: Filarioidea) in red deer (Cervus elaphus) in Switzerland

Fig. 4. a and b: Posterior end of O. jakutensis male with 5 pairs of pericloacal papillae without unpaired precloacal papilla.

Fig. 3. O in First description of Onchocerca jakutensis (Nematoda: Filarioidea) in red deer (Cervus elaphus) in Switzerland

Fig. 3. O. jakutensis male and female (bars: 100 Mm): a. Tail of male with five pairs of pericloacal and two pair of closely spaced terminal papillae. b. Tail of another male with more distantly spaced papillae on tail end. Left spicule protruding. c. Spicules in ventral view. d. Head end of male. e. Head end of female with vulva. f. Posterior end of female with conical tail in ventral view, annulations indicated on sides. g. Microfilaria with terminal distribution of nuclei.

Fig. 1 in First description of Onchocerca jakutensis (Nematoda: Filarioidea) in red deer (Cervus elaphus) in Switzerland

Fig. 1. Subcutaneous nodule in red deer skin with partly freed O. jakutensis female (stained with methylene blue). (For interpretation of the references to colour in this figure legend, the reader is referred to the web version of this article.)

opencc-by-4.0Sep 2022View details →

Fig. 4 in The first Jurassic coelacanth from Switzerland

Fig. 4 Skeleton of Libys callolepis sp. nov. on the counterpart (holotype, NMBE 5034072). A Photos with osteological details: 1, articular head of the scapulocoracoid. 2, Scales on the flank immediately beneath the first anterior dorsal fin. 3, Scales of the lateral line showing the ornamental pattern with the larger central tubercles (white arrowheads point, showed only on one scale). 4, Scales on the ventral flank from the pelvic to the anal fin. 5, Axial mesomere (white arrowhead) surrounded by some fin rays of the anal fin. 6, Axial mesomeres (white arrowhead) partially covered by sediment in the pelvic fin. B Semi-interpretative line drawing of the specimen

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Fig. 3 in The first Jurassic coelacanth from Switzerland

Fig. 3 Skeleton of Libys callolepis sp. nov. on the part (holotype, NMBE 5034073). A Photos with osteological details: 1, denticles on the proximal fin rays of the caudal fin. 2, Postparietal shield with the otic sensory canal opening as a deep groove crossed by pillars (white arrowhead). 3, Posterior parietal and the supraorbitals with their pillars (white arrowhead). 4, Consolidated snout with the anterior opening for the rostral organ (white arrowhead). 5, Teeth on the prearticular. B Semi-interpretative line drawing of the specimen

Fig. 5 in A new pachypleurosaur from the Early Ladinian Prosanto Formation in the Eastern Alps of Switzerland

Fig. 5 Details of forelimbs and girdle elements of Prosantosaurus scheffoldi gen et spec. nov. from the upper Prosanto Formation (Early Ladinian, Middle Triassic) of Ducanfurgga locality no. 4, southwest of Davos, Canton of Grisons, south-eastern Switzerland. A Both forearms and anterior trunk region in dorsal view (PIMUZ A/III 1240). B Left forearm in ventral view (PIMUZ A/III 1275). C Right forearm in dorsal view (PIMUZ A/III 668). D Shoulder girdle in ventral view (PIMUZ A/III 4566). E Right scapula in ventral view (PIMUZ A/III 1275). F Partially disarticulated pelvic girdle in ventral view (PIMUZ A/III 1197). G Pelvic girdle in ventral view (PIMUZ A/III 4566). H Left pelvic girdle in ventral view (PIMUZ A/III 1275)

Fig. 3 in A new pachypleurosaur from the Early Ladinian Prosanto Formation in the Eastern Alps of Switzerland

Fig. 3 Ventral skull morphology and dentition of Prosantosaurus scheffoldi gen et spec. nov. from the upper Prosanto Formation (Early Ladinian, Middle Triassic) of Ducanfurgga locality no. 4, southwest of Davos, Canton of Grisons, south-eastern Switzerland. A Detail of the skull in ventral view of specimen PIMUZ A/III 4566. B Detail of skull in ventral view of specimen PIMUZ A/III 1275. Note that the posterior pterygoid region is displaced. C Detail of lower jaws, skull and dentition in ventral view of specimen PIMUZ A/III 1197. D Skull of PIMUZ A/III 1490 providing details of tooth morphology and replacement pattern. E Outline sketch of skull PIMUZ A/III 1490. See Additional file 1: Figs. S8, S13 for interpretative and labelled sketches of the skulls of PIMUZ A/III 1275 and PIMUZ A/III 1197

Fig. 2 in A new pachypleurosaur from the Early Ladinian Prosanto Formation in the Eastern Alps of Switzerland

Fig. 2 Holotype specimen (PIMUZ A/III 1274) of Prosantosaurus scheffoldi gen. et spec. nov. from the upper Prosanto Formation (Early Ladinian, Middle Triassic) of Ducanfurgga locality no. 4, southwest of Davos, Canton of Grisons, south-eastern Switzerland. A Nearly complete specimen as prepared in dorsal view. The posterior part of the tail was lost prior to burial. Both forearms are not visible but lie below the trunk region, pointing in an anteromedial direction (see Additional file 1: Fig. S3A). B Detail of skull and anterior neck region. C Outline sketch of skull sutures. D Detail of shoulder girdle (claviculae, scapulae) and anterior dorsal vertebrae and ribs. E Detail of right humerus. F Detail of posterior dorsal vertebrae and ribs, sacral vertebrae and ribs, and anterior caudal vertebrae and ribs. G Detail of left ilium and hindlimb. ar articular; as astragalus; bo basioccipital; cal calcaneus; cl clavicula; co coracoid; d dentary; en external naris; eo exoccipital; fe femur; fi fibula; fr frontal; hu humerus; il ilium; in internal naris; is ischium; j jugal; mx maxilla; na naris; o orbit; pa parietal; pl palatine; pmx premaxilla; pof postfrontal; po postorbital; prf prefrontal; pt pterygoid; pu pubis; q quadrate; qj quadratojugal; ti tibia; sacr sacral rib; sc scapula; so supraoccipital; sp splenial; sq squamosal; su surangular; utf upper temporal fenestra; v vomer

Fig. 1 A in A new pachypleurosaur from the Early Ladinian Prosanto Formation in the Eastern Alps of Switzerland

Fig. 1 A Schematic palaeogeographic map of the Germanic and Alpine Triassic (Middle Triassic) exhibiting European pachypleurosaur occurrences and their stratigraphy. Map is based on Ziegler (2005: fig. 6), Furrer (2019: fig. 129) and references therein. I–VI, Germanic Basin localities; VII–XIII, Alpine Triassic localities. I—Pachypleurosauria indet., Iberian Peninsula (Anisian: Aiguafreda; Ladinian: Mont-ral-Alcover; Carnian: Vilanueva de la Sal); II—Neusticosaurus sp., Lorraine region, France (Ladinian); III—Anarosaurus heterodontus, Winterswijk, The Netherlands (Early to Middle Anisian); IV—Anarosaurus pumilio, Magdeburg, eastern/central Germany (Middle Anisian); V—Neusticosaurus pusillus, Hoheneck, southern Germany (Early Ladinian); VI—Dactylosaurus gracilis, Gogolin, Poland (Early Anisian); VII—Neusticosaurus toeplitschi, Northern Calcareous Alps, Austria (Early Ladinian); VIII—Prosantosaurus scheffoldi nov. gen. et sp., Ducan area, SE-Switzerland (Early Ladinian); IX—Neusticosaurus toeplitschi, Gailtal Alps, Austria (Early Ladinian); X—Odoiporosaurus teruzzii, Besano, Monte San Giorgio area, Italy (Late Anisian); Serpianosaurus mirigiolensis, Monte San Giorgio area, Italy/Switzerland (latest Anisian-earliest Ladinian); Neusticosaurus pusillus, N. peyeri and N. edwardsii, Monte San Giorgio, northern Italy/southern Switzerland (Early Ladinian); XI—Neusticosaurus pusillus, Valtravaglia, Varese, Italy (Early Ladinian); XII—Pachypleurosauria indet. aff. Serpianosaurus/ Neusticosaurus, West Carpathian Alps, Slovakia (Middle to Late Anisian) and Pachypleurosauria indet., Velika Planina, Slovenia (Early–Middle Anisian). Ba Barcelona; Be Berlin; Bs Basel; Bu Budapest; Fr Frankfurt a. M.; Ha Hamburg; Kr Krakow; Ly Lyon; Mr Marseille; Mu Munich; Pr Prague; Wa Warsaw; BG Burgundian Gate; SMG Silesian–Moravian Gate; ECG Eastern Carpathian Gate. B Localities and stratigraphic position of the Alpine pachypleurosaurs in Switzerland. B1 Map showing the Ducanfurgga locality relative to the UNESCO World Heritage vertebrate site of Monte San Giorgio with the pachypleurosaur-bearing beds indicated. B2 Correlation of the Middle Triassic section at Ducanfurgga (Upper Austroalpine Silvretta Nappe, south-eastern Switzerland) with that of Monte San Giorgio (southern Alps, southern Switzerland; modified from Scheyer et al., 2017). B3 Schematic succession of five nearly complete specimens and the disarticulated one found in the upper Prosanto Formation near Ducanfurgga. The numbers refer to bed numbers progressing from older to younger layers

opencc-by-4.0Jul 2019View details →

ENERGISE Living Lab Country Report - Switzerland

In Switzerland, the two ENERGISE Living Labs (ELLs) took place in the City and Canton of Geneva, in the French-speaking region of the country. The first Living Lab (ELL1) included 20 households with diverse profiles, from one- and two-person households to families with two or three children, and with participants of all age groups. A large majority of them lived in multi-family houses or larger apartment buildings, reflecting the housing situation in Switzerland. The second Living Lab (ELL2) was organised in a community of place, a housing cooperative located in the Geneva city center. The participants' profile was also varied in terms of age group and type of households.

opencc-by-4.0Aug 2019View details →

Supporting data: The seasonal origins of streamwater in Switzerland

These data support the analysis conducted in "The seasonal origins of streamwater in Switzerland", accepted for publication in Geophysical Research Letters (<a href="https://doi.org/10.1029/2019GL084552">https://doi.org/10.1029/2019GL084552</a>) by Scott T. Allen, Jana von Freyberg, Markus Weiler, Gregory R. Goldsmith, James W. Kirchner. Information on the study sites, sampling procedures, and analysis can be found in the main text and supporting information files. Here we provide the data used: Data Table S1. Annual precipitation and discharge isotope values, precipitation sine fit parameters, and typical isotope ratios of summer and winter precipitation.  Data Table S2. Streamwater grab sample SOIq values with matched daily discharge rates. See the Methods section for further details.

Fig. 5 a in Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland)

Fig. 5 a to p (scale bar: 250 µm): a random section of Terquemella sp., "Urgonien jaune", Upper Hauterivian, sample 107; b random section of Terquemella sp., "Urgonien jaune", Upper Hauterivian, sample 128; c subtransverse section of Deloffrella hauteriviana, " Pierre jaune", Lower Hauterivian, sample 171; d section of a lateral of Rajkaella minima, Vions Fm, Upper Berriasian, sample 287; e section of a lateral of Rajkaella minima, Pierre Châtel Formation, Middle Berriasian, sample 312; f subtransverse section of Salpingoporella steinhauseri, Pierre Châtel Formation, Middle Berriasian, sample 307; g oblique section of Salpingoporella steinhauseri, Pierre Châtel Formation, Middle Berriasian, sample 307; h tangential section of Salpingoporella steinhauseri, Pierre Châtel Formation, Middle Berriasian, sample 307; i oblique section of a verticil of Actinoporella sp. (note: the corona structure is visible), Pierre Châtel Formation, Middle Berriasian, sample 301; j oblique section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 310; k subaxial section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 310; l oblique section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 310; m subtransverse section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 309; n oblique section of Clypeina aff. parasolkani (two fertile verticils visible), transition Vions - Pierre Châtel formations, Middle-Upper Berriasian, sample 291.8; o subaxial section of Clypeina aff. parasolkani (three fertile verticils visible), transition Vions - Pierre Châtel formations, Middle-Upper Berriasian, sample 291.8; p oblique section of Otternstella lemmensis, Pierre Châtel Formation, Middle Berriasian, sample 317

Fig. 3 a in Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland)

Fig. 3 a to l (scale bar: 500 µm): a oblique section of Zergabriella embergeri, Chambotte Fm, Upper Berriasian, sample 253; b oblique section of Triploporella? praturloni, "Calcaires roux", Lower Valanginian, sample 241; c oblique section of Triploporella? praturloni, "Calcaires roux", Lower Valanginian, sample 241.60; d tangential section of Zergabriella embergeri, Vions Fm, Upper Berriasian, sample 258; e transverse section of Zergabriella embergeri, Chambotte Fm, Upper Berriasian, sample 253; f oblique section of a verticil of Selliporella neocomiensis, transition Vions - Pierre Châtel formations, Middle-Upper Berriasian, sample 291.80; g oblique section of Falsolikanella danilovae, "Urgonien jaune", Upper Hauterivian, sample 116; h subaxial section of a verticil of Falsolikanella danilovae, "Urgonien jaune", Upper Hauterivian, sample 107; i oblique section of Dissocladella intercedens "Calcaires roux", Lower Valanginian, sample 241.60; j tangential section of a verticil of Clypeina sulcata, Pierre Châtel Formation, Middle Berriasian, sample 317; k oblique section of a verticil of Clypeina sulcata, Pierre Châtel Formation, Middle Berriasian, sample 317; l random sections of verticils of Clypeina sulcata, Pierre Châtel

Fig. 6 a in Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland)

Fig. 6 a to o (scale bar: 250 µm): a oblique section of Salpingoporella annulata, Pierre Châtel Formation, Middle Berriasian, sample 317; b oblique section of Salpingoporella annulata, Pierre Châtel Formation, Middle Berriasian, sample 317; c subtransverse section of Salpingoporella annulata, Pierre Châtel Formation, Middle Berriasian, sample 317; d oblique section of Falsolikanella campanensis, Vions Fm, Upper Berriasian, sample 270; e deep tangential section of Pseudoactinoporella fragilis, "Urgonien jaune", Upper Hauterivian, sample 101; f oblique section of Pseudoactinoporella fragilis, "Urgonien jaune", Upper Hauterivian, sample 107; g oblique section of Conradella bakalovae, "Urgonien jaune", Upper Hauterivian, sample 134; h oblique section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 309; i oblique section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 293; j oblique section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 293; k subaxial section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 309; l subtransverse section of a verticil of Clypeina parasolkani, Pierre Châtel Formation, Middle Berriasian, sample 309; m deep tangential section of Deloffrella quercifoliipora, Vions Fm, Upper Berriasian, sample 271; n random section of Cymopolia sp. or Neomeris sp., "Urgonien jaune", Upper Hauterivian, sample 115; o oblique section of Angioporella fouryae, "Urgonien jaune", Upper Hauterivian, sample 129

Fig. 7 a in Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland)

Fig. 7 a to o (scale bar: 250 µm): a tangential to oblique section of Salpingoporella muehlbergii, "Urgonien blanc", Upper Hauterivian, sample 42; b transverse section of Salpingoporella muehlbergii, "Urgonien blanc", Upper Hauterivian, sample 42; c oblique section of Salpingoporella muehlbergii, "Urgonien blanc", Upper Hauterivian, sample 42; d oblique section of Salpingoporella genevensis, "Urgonien blanc", Upper Hauterivian, sample 40; e oblique section of Suppiluliumaella sp., "Urgonien jaune", Upper Hauterivian, sample 96; f oblique section of Suppiluliumaella sp., "Urgonien jaune", Upper Hauterivian, sample 96; g oblique section of Suppiluliumaella sp., "Urgonien jaune", Upper Hauterivian, sample 96; h oblique section of a verticil of Falsolikanella danilovae, "Urgonien jaune", Upper Hauterivian, sample 116; i transverse section of Salpingoporella melitae, "Urgonien blanc", Upper Hauterivian, sample 42; j oblique section of Cylindroporella sp., "Urgonien blanc", Upper Hauterivian, sample 71; k oblique section of Salpingoporella heraldica, "Urgonien jaune", Upper Hauterivian, sample 115; l oblique section of Angioporella fouryae, "Urgonien jaune", Upper Hauterivian, sample 115; m subtransverse section of Suppiluliumaella sp., "Urgonien jaune", Upper Hauterivian, sample 96; n tangential section of a sterile verticil of Angioporella fouryae, "Urgonien jaune", Upper Hauterivian, sample 115; o tangential section of a verticil of Pseudoclypeina sp., "Urgonien blanc", Upper Hauterivian, sample 72; p to u (scale bar: 500 µm): p oblique section of Deloffrella hauteriviana, "Urgonien blanc", Upper Hauterivian, sample 37.85; q subtransverse section of Dissocladella? sp., "Urgonien blanc", Upper Hauterivian, sample 90; r oblique section of Deloffrella hauteriviana, "Urgonien blanc", Upper Hauterivian, sample 37.85; s axial section of Oroseina sp., "Urgonien jaune", Upper Hauterivian, sample 114; t random section of Oroseina sp., "Urgonien jaune", Upper Hauterivian, sample 112; u tangential section of Oroseina sp., "Urgonien jaune", Upper Hauterivian, sample 112.