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Fig. 3. A in Pliensbachian, Early Jurassic radiolarians from Mount Rettenstein in the Northern Calcareous Alps, Austria

Fig. 3. A. View of the complete Mount Rettenstein complex from the southwest. B. Position of the studied section in the Weitenhaus cirque, the oval indicates the location where the studied samples were collected. C. Schematic sketch of the structural build of Mount Rettenstein with the three main tectonic units (from Auer et al. 2006). Structural Unit I: The primary part of the Tirolic mega-unit which, in contrast to the higher structural units, stayed ( more or less) in place relative to the basis of the Upper Tirolic thrust sheet. In the Mount Rettenstein region, Permian to early Middle Triassic strata make up the succession above the Greywacke Zone basement (Ganss et al. 1954). Structural Unit II: This intermediate, rather thin sheet is mainly made up of a laterally variable mega-slide succession of the Middle Jurassic Hallstatt Mélange. It is thought to have achieved its present position in the hangingwall of a normal fault (Auer et al. 2006). Structural Unit III: The topmost Mount Rettenstein unit corresponds to the Lower to Upper Jurassic Mount Rettenstein succession sensu stricto in the sense of Auer et al. (2009). It is suggested to have been emplaced along a thrust fault (Auer et al. 2006).

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Fig. 2 in Pliensbachian, Early Jurassic radiolarians from Mount Rettenstein in the Northern Calcareous Alps, Austria

Fig. 2. Stratigraphic table with lithostratigraphic names and main tectonic events of the Jurassic of the Northern Calcareous Alps with their variations depending on the palaeogeographic position (after Gawlick et al. 2009). The different facies belts and therefore also the formations belong to depositional realms, which roughly correspond to the later formed tectonic units. The outer shelf region can only be reconstructed from blocks in Middle to Upper Jurassic mélanges and is, therefore, not completely understood in all details. The grey limestone succession from Mount Rettenstein shows characteristics of both the Scheibelberg and the Dürrnberg formations (in bold). Estimated palaeogeographic positions of the studied section are indicated. Abbreviations: Cret., Cretaceous; Fm., Formation; Lst., Limestone.

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Fig. 1. A in Pliensbachian, Early Jurassic radiolarians from Mount Rettenstein in the Northern Calcareous Alps, Austria

Fig. 1. A. Structural overview maps of the Alpine orogen, showing the situation of the central Northern Calcareous Alps. B. The middle sector of the central Northern Calcareous Alps with locations mentioned in the text indicated (modified from Frisch and Gawlick 2003). Abbreviations: Re, Mount Rettenstein; BD, Bad Dürrnberg; Te, Teltschengraben.

opencc-zeroJun 2024View details →

Dataset: ALPS Active REIT ETF (REIT) Stock Performance

This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.

opencc-zeroJun 2024View details →

Dataset: ALPS ETF Trust - Level Four Large Cap Growth Active ETF (LGRO) Stock Performance

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Plate III, Figs A.16–A.21 – Type A (French and Swiss Alps). A.16, head and pronotum of nymph (Swiss Alps); A.17, markings on tergites of nymph (Gryonne valley); A.18, markings on tergites of nymph (Sense); A.19, markings on the femora of legs, dorsal view (Gryonne Valley); A.20, sclerotized apex of extracted aedeagus of an adult ♂ (Vercors); A.21, sclerotized apex of aedeagus of Perla grandis, from Aubert 1949: 225, his Fig. 4. in Steps towards a revision of the Perla bipunctata Pictet, 1833 species complex (Plecoptera: Perlidae)

Plate III, Figs A.16–A.21 – Type A (French and Swiss Alps). A.16, head and pronotum of nymph (Swiss Alps); A.17, markings on tergites of nymph (Gryonne valley); A.18, markings on tergites of nymph (Sense); A.19, markings on the femora of legs, dorsal view (Gryonne Valley); A.20, sclerotized apex of extracted aedeagus of an adult ♂ (Vercors); A.21, sclerotized apex of aedeagus of Perla grandis, from Aubert 1949: 225, his Fig. 4.

Fig. 2 in Calliptamus italicus at 3050 m: a first evidence of dispersal across the Alps? (Orthoptera: Acrididae)

Fig. 2 – The female Calliptamus italicus (Linnaeus, 1758) observed at Punta Losetta (3050 m, Cottian Alps) on 27 Aug 2020 (body length = 28.5 mm).

Fig. 4 in Calliptamus italicus at 3050 m: a first evidence of dispersal across the Alps? (Orthoptera: Acrididae)

Fig. 4 – Landscape on the Italian slope of Punta Losetta (3050 m, Cottian Alps). The Alpine grassland in the lower part of the picture is the habitat were the female C. italicus was observed the 27 Aug 2020.

Fig. 3 – Plots representing the 23-27 Aug 2020 in Calliptamus italicus at 3050 m: a first evidence of dispersal across the Alps? (Orthoptera: Acrididae)

Fig. 3 – Plots representing the 23-27 Aug 2020 trends of the meteorological parameters considered in order to describe the weather conditions in the days just before the observation of the female Calliptamus italicus on Punta Losetta (3050 m, Cottian Alps). The trend of each parameter is better visualized with a Loess curve (blue line; grey area = 95% confi- dence interval): a, atmospheric pressure; b, precipitations; c, wind speed (solid lines) and wind gust (dotted lines); d, wind direction (origin); e, air temperature. The data collected in each weather station are reported in different colours. Sources: ARPA Piemonte and Météo France.

Fig. 1 in Calliptamus italicus at 3050 m: a first evidence of dispersal across the Alps? (Orthoptera: Acrididae)

Fig. 1 – Map of the study area (Monviso massif, Cottian Alps, France-Italy border). The yellow point identifies the locality where the female Calliptamus italicus was observed on 27 Aug 2020 (Punta Losetta, 3050 m), while the position of the weather stations considered in this short note is reported by red dots.

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

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Fig. 2 in Unexpected Echinococcus multilocularis infections in shepherd dogs and wolves in south-western Italian Alps: A new endemic area?

Fig. 2. Multiple alignment of partial mitochondrial cob (124bp) from three specimens identified as Echinococcus multilocularis analyzed in the present paper (the first three input sequences) with: (a) six E. multilocularis sequences retrieved from GenBank after comparison by Local Alignment Search Tool BLAST; (b) five sequences referred to Echinococcus granulosus (Eg, EgG1), E. ortleppi (EgG5), E. canadensis (EgG6-7) and Taenia hydatigena (Thy) retrieved from GenBank. (c) Multiple alignment of partial mitochondrial nad1 (139bp) from three specimens identified as Echinococcus ortleppi analyzed in the present paper (the first three input sequences) with sequences retrieved from GenBank belonging to other representatives of E. ortleppi, E. granulosus, E. canadensis, E. multilocularis, T. krabbei, T. ovis and T. hydatigena. Dots indicate identity with nucleotide of the first sequences listed.

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Fig. 1 in Unexpected Echinococcus multilocularis infections in shepherd dogs and wolves in south-western Italian Alps: A new endemic area?

Fig. 1. Locations of wolf (blue dots) and dog (orange dots) fecal samples positive to Echinococcus multilocularis collected during a survey on Echinococcus spp. carried out from June to November 2017 in a mountainous area in the Alps of the Imperia Province, Italy. In the map are also reported the southernmost reports of Echinococcus multilocularis (E. multilocularis) to date in Europe (France, Drs. Boué and Umhang, pers. communication; North-Eastern Italian Alps, Croatia, as in (Beck et al., 2018)). Two dog fecal samples were collected from the same pasture and are represented by a single dot (noted as 2×). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)

Fig. 3. Seasonal detection rate for E. uekii, type B in Surveillance of Eimeria species in wild Japanese rock ptarmigans, Lagopus muta japonica, and insight into parasitic seasonal life cycle at timberline regions of the Japanese Alps

Fig. 3. Seasonal detection rate for E. uekii, type B, and mixed Eimeria spp. oocyst infection in both adults and chicks in 2006 and 2007. Numbers in parentheses below months indicate the total number of fecal samples analyzed. Data for the number of chicks (23 in 2006 and 11 in 2007) were only available for August.

Fig. 1 in Surveillance of Eimeria species in wild Japanese rock ptarmigans, Lagopus muta japonica, and insight into parasitic seasonal life cycle at timberline regions of the Japanese Alps

Fig. 1. Seasonal prevalence of Eimeria spp. infection in Japanese rock ptarmigans from April to November in 2006 and 2007. (a) and (b) show the prevalence of infection in adult birds and chicks, respectively. Numbers above bars indicate the total number of fecal samples analyzed.

Fig. 2 in Surveillance of Eimeria species in wild Japanese rock ptarmigans, Lagopus muta japonica, and insight into parasitic seasonal life cycle at timberline regions of the Japanese Alps

Fig. 2. Photomicrograph of eimerian oocysts detected in the feces of Japanese rock ptarmigans; (a) E. uekii and (b) type B. The scale bar indicates 20 μm.

Fig. 6 in Surveillance of Eimeria species in wild Japanese rock ptarmigans, Lagopus muta japonica, and insight into parasitic seasonal life cycle at timberline regions of the Japanese Alps

Fig. 6. Average monthly environmental temperatures on the windward and leeward slopes of Mt. Tateyama from 2006 to 2007. The temperatures on the windward slopes were not measured in April. The table below the graph shows monthly maximum and minimum temperatures.