229 research outputs found
Drassodex simoni Herve, Roberts & Murphy 2009
Drassodex simoni Hervé, Roberts & Murphy, 2009 MATERIAL. — La Méa, rocky lands, 2409 m, 02.VII.2017, Isaia & Mammola leg., 2 ♀, coll. MI; Chapeau de Gendarme, rocky lands, 2661 m, 02.VII.2017, Isaia & Mammola leg., 1 ♀, coll. MI. CHOROTYPE. — ALPW. MACROHABITAT. — Rocky lands. NOTE. — Endemic of the Maritime Alps. This species occurs in high alpine habitats, such as screes and alpine prairies. This species has recently been described by Hervé et al. (2009) from material collected in the French Maritime Alps (Mercantour National Park)Published as part of Milano, Filippo, Mammola, Stefano, Rollard, Christine, Leccia, Marie-France & Isaia, Marco, 2019, An inventory of the spider species of Barcelonnette (France), with taxonomic notes on Piniphantes agnellus n. comb. (Araneae, Linyphiidae), pp. 29-58 in Zoosystema 41 (4) on page 36, DOI: 10.5252/zoosystema2019v41a4, http://zenodo.org/record/371848
Cellule staminali mesenchimali per la prevenzione dell’ototossicità indotta dal cisplatino
Psammoecus simoni Grouvelle 1892
Psammoecus simoni Grouvelle, 1892 (Fig. 11) Psammoecus simonis Grouvelle, 1892: 287. Psammoecus simoni – Grouvelle 1908c: 476.— Pal 1985. Material examined Lectotype ♂, by present designation: ‘ Antipolo | E. Simon’, ‘TYPE’ [red label], ‘MUSEUM PARIS | 1917 | Coll. GROUVELLE’ [yellow label], ‘ Psammoecus | Simoni | ty. A. Grouv’ [Grouvelle’s hand] (MNHN). Paralectotype 1 spm with identical data as lectotype (MNHN). Other material 5 spms ‘COLL: MUS. CONGO | Madagascar: Maroansetra | (à la lumière) II/ IV-1950 | J. Vadon’ (MRAC). 1spm ‘COLL. MUS. TERVUREN | N.E. Madagascar: | Ambodivoangy 1959 | J. Vadon’ (MRAC). Differential diagnosis Ps. simoni differs by its short oval habitus and the short, stout parameres that are fused with the basal piece from all other African Psammoecus. The wide-based pronotal teeth resemble Ps. luchti sp. nov., it differs by the elytral striae being considerably wider than interstices, elytra being shorter, darkened basis of elytra, parameres short, stout and fused with basal piece. Redescription BODY. Oval, total length 2.13-3.00 mm (Fig. 11A). Surface yellowish-brown, sometimes reddish-brown, elytra with brown or blackish-brown maculae: humeral swelling, a transverse band in the middle of the elytra, the elytral suture along the posterior two thirds and the elytral apex are dark. Base of antennae yellowish or reddish brown, 6 th to 10 th antennomere darkened, 11 th antennomere yellowish-white, some specimens with light apex of 10 th antennomere. HEAD. Broad, temples narrowed immediately behind eyes; width 0.64-0.71 mm, length 0.33-0.44 mm, 1.67-1.73 times as wide as long. Eyes protuberant, rounded, 0.17-0.20 mm long, distance of inner margins 0.38-0.45 mm. Puncturation on vertex coarse, density of punctures variable, pubescence composed of long, semierect setae, directed anteriorly; microsculpture absent. Longitudinal impressions on vertex very shallow, attaining the middle of the eyes, sometimes shorter. Antennae as in Fig. 11B, 1.17-1.40 mm long, stout, antennomere proportions of lectotype as follows: 2.9: 1.3: 1.8: 1.5: 1.8: 1.6: 1.4: 1.0:1.2: 1.4: 2.8. PRONOTUM. Broad; width 0.62-0.74 mm, length 0.48-0.56 mm, 1.22-1.35 times as wide as long. Surface smooth, without impressions. Anterior angles with distinct groups of small teeth; lateral margins with four distinct teeth; tooth I very small, tooth II a little larger, teeth III and IV largest. Posterior group of teeth consisting of a larger anterior tooth and a very small, almost obtuse posterior tooth. Puncturation coarser than on vertex, punctures sometimes adjoining. Pubescence as on vertex; microsculpture absent. ELYTRA. Oval, short, length 1.35-1.70 mm, combined width 1.00- 1.23 mm, 1.27-1.43 times as long as their combined width. Rows of punctures on disc wider than interstices. Pubescence consists of long, semierect setae. Microsculpture absent. PARAMERES. Short, stout, fused with basal piece; with distinct pattern of three large setae (Fig. 11 C). Remarks In his original description, Grouvelle (1892) spells the name ‘simonis’. However, on the labels that Grouvelle added to the syntypes as well as in a later paper (Grouvelle, 1908c), he spells the name ‘simoni’. Pal (1985) also uses the latter spelling. Hence the present author considers ‘simonis’ to be a misprint and proposes to spell the name in accordance with Grouvelle (1908c) and Pal (1985).Published as part of Karner, Michael, 2012, A revision of African Psammoecus (Coleoptera, Silvanidae) and descriptions of two new species from the collection of the Musée royal de l'Afrique centrale, pp. 1-31 in European Journal of Taxonomy 17 on pages 24-26, DOI: 10.5852/ejt.2012.17, http://zenodo.org/record/385784
Construyendo la ópera nacional: A Marília de Itamaracá de L. V. De-Simoni
Luiz Vicente De Simoni (1782-1881) was an Italian physician who went to Rio de Janeiro in 1817, and was constantly involved in the musical and theatrical scene of the city. He is the author of Marília de Itamaracá (1854, music by Adolpho Maersch), considered by some authors as the first “Brazilian” opera. The subject is historical and narrates some episodes of the 17th century war against the Dutch. One of his main concerns was the use of Brazilian and Portuguese themes in operas, in order to invent something “national”. As part of a broader movement, the idea was to explore Brazilian people, landscape and traditions as the main subject for operas that should be sung in Portuguese. The movement was related to a broader political project sponsored by the government and the Emperor, aimed at the revision of Brazilian history and the construction of a new cultural identity for the country. The purpose of this paper is to examine some aspects of the libretto of Marília de Itamaracá and the ideas discussed in its preface, showing the contradictions and tensions involved in the creation of a “national” identity through operas
Optofluidic Flow Cytometer with In-Plane Spherical Mirror for Signal Enhancement
Statistical analysis of the properties of single microparticles, such as cells, bacteria or plastic slivers, has attracted increasing interest in recent years. In this regard, field flow cytometry is considered the gold standard technique, but commercially available instruments are bulky, expensive, and not suitable for use in point-of-care (PoC) testing. Microfluidic flow cytometers, on the other hand, are small, cheap and can be used for on-site analyses. However, in order to detect small particles, they require complex geometries and the aid of external optical components. To overcome these limitations, here, we present an opto-fluidic flow cytometer with an integrated 3D in-plane spherical mirror for enhanced optical signal collection. As a result, the signal-to-noise ratio is increased by a factor of six, enabling the detection of particle sizes down to 1.5 µm. The proposed optofluidic detection scheme enables the simultaneous collection of particle fluorescence and scattering using a single optical fiber, which is crucial to easily distinguishing particle populations with different optical properties. The devices have been fully characterized using fluorescent polystyrene beads of different sizes. As a proof of concept for potential real-world applications, signals from fluorescent HEK cells and Escherichia coli bacteria were analyzed
Landslide prediction, monitoring and early warning: a concise review of state-of-the-art
Landslide is one of the repeated geological hazards during rainy season, which causes fatalities, damage to property and economic losses in Korea. Landslides are responsible for at least 17% of all fatalities from natural hazards worldwide, and nearly 25% of annual casualties caused by natural hazards in Korea. Due to global climate change, the frequency of landslide occurrence has been increased and subsequently, the losses and damages associated with landslides also have been increased. Therefore, accurate prediction of landslide occurrence, and monitoring and early warning for ground movements are very important tasks to reduce the damages and losses caused by landslides. Various studies on landslide prediction and reduction in landslide damage have been performed and consequently, much of the recent progress has been in these areas. In particular, the application of information and geospatial technologies such as remote sensing and geographic information systems (GIS) has greatly contributed to landslide hazard assessment studies over recent years. In this paper, the recent advances and the state-of-the-art in the essential components of the landslide hazard assessment, such as landslide susceptibility analysis, runout modeling, landslide monitoring and early warning, were reviewed. Especially, this paper focused on the evaluation of the landslide susceptibility using probabilistic approach and physically based method, runout evaluation using volume based model and dynamic model, in situ ground based monitoring techniques, remote sensing techniques for landslide monitoring, and landslide early warning using rainfall and physical thresholds
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