A New Species of Sand Racer, Psammodromus (Squamata: Lacertidae), from the Western Iberian Peninsula

A new species of lacertid lizard of the genus Psammodromus is described from the Iberian Peninsula. Genetic and recently published phenotypic data support the differentiation of Psammodromus hispanicus into three, and not as previously suggested two, distinct lineages. Age estimates, lineage allopatry, the lack of mitochondrial and nuclear haplotype sharing between lineages, ecological niche divergence, and the current biogeographic distribution, indicated that the three lineages correspond to three independent species. Here, we describe a new species, Psammodromus occidentalis sp. n., which is genetically different from the other sand racers and differentiated by the number of femoral pores, number of throat scales, snout shape, head ratio, green nuptial coloration, and number of supralabial scales below the subocular scale. We also propose to upgrade the two previously recognized subspecies, Psammodromus hispanicus hispanicus Fitzinger, 1826 from central Spain and Psammodromus hispanicus edwardsianus (Dugès, 1829) from eastern Spain, to the species level: Psammodromus hispanicus stat. nov. and Psammodromus edwardsianus stat. nov. Given that the holotype of Psammodromus hispanicus was lost, we designate a neotype. We also analysed museum specimens of P. blanci, P. microdactylus and P. algirus to describe differentiation of the Psammodromus hispanicus lineages/species from their closest relatives.

Awareness of human immunodeficiency virus screening guidelines is low in emergency departments of western Switzerland.

Background: Human immunodeficiency virus (HIV) prevalence in Switzerland is 0.4% and 30% of HIV patients are diagnosed with CD4 counts <200 cells/microliter. In 2010, the Swiss Federal Office of Public Health (SFOP) published updated guidelines regarding Physician- Initiated Counseling and Testing (PICT) for HIV. In the new guidelines, when acute HIV infection is suspected or HIV is among the differential diagnoses, an HIV test is performed without risk assessment nor prior counseling, unless the patient specifically refuses it. Counseling and verbal consent are still required when the patient asks for an HIV test or belongs to a high risk group. Whist HIV testing in the emergency departments (ED) is recommended, only 1% of patients are currently screened. Lack of awareness among physicians has been cited in the literature as the first barrier to guideline implementation. Objectives: To test if physicians working in EDs of 5 large teaching hospitals in western Switzerland, admitting 175,000 patients / year, were aware of the updated SFOP guidelines. Methods: A survey was delivered to 167 ED physicians in the summer of 2011. The survey consisted of 26 vignettes designed to test whether physicians would request an HIV test according to the new guidelines and if they knew when the PICT strategy was allowed or counseling required. Finally, physicians were asked the number of HIV tests they had requested in the previous 4 weeks, and if they were aware of the new HIV guidelines. Results are presented as mean and standard deviation, median and interquartile range (IQR), or as proportions; Student's t test was used to compare continuous variables; Results: 143 physicians returned the survey (86%); mean age was 32 ± 8 years, and median postgraduate experience of 6 years (IQR 3-12); 52% were male and 17% were attendings. The percentage of correct responses was 60 ± 13% with no difference between attendings and residents (p = 0.31); 2 of the 3 questions with the lowest scores were failure to recognize situations in which HIV testing was indicated, and the third one a failure to recognize acute HIV infection. 82% of physicians were not aware of the new guidelines. The median number of test requests was 1 (IQR 0-2, range 1-10). Conclusion: ED physicians are not aware of current HIV screening guidelines published by the SFOP, and rarely perform HIV tests. An information campaign is required if ED physicians are expected to play a significant role in the reduction of undiagnosed HIV patients.

Basin-internal derivation of hydrocarbons in the Witwatersrand Basin, South Africa: evidence from bulk and molecular δ13C data

Gold in the quartz-pebble conglomerates of the late Archean Witwatersrand Basin, South Africa, is often intimately associated with carbonaceous matter of organic/biogenic origin which occurs in the form of stratiform carbon seams and paragenetically late bitumen nodules. Both carbon forms are believed to be formed by solidification of migrating hydrocarbons. This paper presents bulk and molecular chemical and stable carbon isotope data for the carbonaceous matter, all of which are used to provide a clue to the source of the hydrocarbons. These data are compared with those from intra-basinal shales and overlying dolostone of the Transvaal Supergroup. The delta C-13 values of the extracts from the Witwatersrand carbonaceous material show small differences (up to 2.4 parts per thousand) compared to the associated insoluble organic matter. This suggests that the auriferous rocks were stained by mobile hydrocarbons produced by thermal and oxidative alteration of indigenous bitumens, a contribution from hydrocarbons derived from intra-basinal Witwatersrand shales cannot be excluded. Individual aliphatic hydrocarbons of the various carbonaceous materials were subjected to compound specific isotope analysis using on-line gas chromatography/combustion/stable isotope ratio mass spectrometry (GC/C/IRMS). The limited variability of the molecular parameters and uniform delta C-13 values of individual n-alkanes (-31.1 +/- 1.7 parts per thousand) and isoprenoids (-30.7 +/- 1.1 parts per thousand) in the Witwatersrand samples exclude the mixing of oils from different sources. Carbonaceous matter in the dolostones shows distinctly different bulk and molecular isotope characteristics and thus cannot have been the source of the hydrocarbons in the Witwatersrand deposits. All the various forms of Witwatersrand carbon appear indigenous to the Witwatersrand Basin, and the differences between them are explained by variable, in general probably short (centimeter- to meter-scale) hydrocarbon migration during diagenesis and subsequent hydrothermal infiltration. (C) 2001 Elsevier Science B.V. All rights reserved.

The Mont Collon mafic complex (Austroalpine Dent Blanche nappe) : permian evolution of the Western European mantle

Résumé: Le complexe du Mont Collon (nappe de la Dent Blanche, Austroalpin) est l'un des exemples les mieux préservés du magmatisme mafique permien des Alpes occidentales. Il est composé d'affleurements discontinus et d'une stratification magmatique en son centre (Dents de Bertol) et est composé à 95% de roches mafiques cumulatives (gabbros à olivine et/ou cpx, anorthositiques, troctolites, wehrlites et wehrlites à plagioclase) et localement de quelques gabbros pegmatitiques. Ces faciès sont recoupés par de nombreux filons acides (aphtes, pegmatites quartziques, microgranodiorites et filons anorthositiques) et mafiques tardifs (dikes mélanocrates riches en Fe et Ti). Les calculs thermométriques (équilibre olivine-augite) montrent des températures de 1070-1120 ± 6°C, tandis que le thermomètre amphibole-plagioclase indique une température de 740 ± 40°C à 0.5 GPa pour les amphiboles magmatiques tardives. La geobarométrie sur pyroxène donne des pressions moyennes de 0.3-0.6 GPa, indiquant un emplacement dans la croûte moyenne. De plus, les températures obtenues sur des amphiboles coronitiques indiquent des températures de l'ordre de 700 ± 40°C confirmant que les réactions coronitiques apparaissent dans des conditions subsolidus. Les âges concordants U/Pb sur zircons de 284.2 ± 0.6 et 282.9 ± 0.6 Ma obtenus sur un gabbro pegmatitique et une pegmatitique quartzique, sont interprétés comme des âges de cristallisation. Les datations 40Ar/39Ar sur amphiboles des filons mélanocrates donnent un âge plateau de 260.2 ± 0.7 Ma, qui est probablement très proche de l'âge de cristallisation. Ainsi, cet age 40Ar/39Ar indique un second évènement magmatique au sein du complexe. Les compositions des roches totales en éléments majeurs et traces montrent peu de variations, ainsi que le Mg# (75-80). Les éléments traces enregistrent le caractère cumulatif des roches (anomalie positive en Eu) et révèlent des anomalies négatives systématiques en Nb, Ta, Zr, Hf et Ti dans les faciès basiques. Le manque de corrélation entre éléments majeurs et traces est caractéristique d'un processus de cristallisation in situ impliquant une quantité variable de liquide interstitiel (L) entre les phases cumulus. Les distributions des éléments traces dans les minéraux sont homogènes, indiquant une rééquilibration .subsolidus entre cristaux et liquide interstitiel. Un modèle quantitatif basé sur les équations de cristallisation in situ de Langmuir reproduisent correctement les concentrations en terres rares légères des minéraux cumulatifs montrant la présence de 0 à 35% de liquide interstitiel L pour des degrés de différenciation F de 0 à 45%, par rapport au faciès les moins évolués du complexe. En outre, les valeurs de L sont bien corrélées avec les proportions modales d'amphibole interstitielle et les concentrations en éléments incompatibles des roches (Zr, Nb). Le liquide parental calculé des cumulats du Mont Collon est caractérisé par un enrichissement relatif en terres rares légères et Th, un appauvrissement en terres rares lourdes typique d'une affinité transitionnelle (T-MORB) et une forte anomalie négative en Nb-Ta. Les roches cumulatives montrent des compositions isotopiques en Nd-Sr proches de la terre globale silicatée (BSE), soit 0.6<εNdi<+3.2, 0.7045<87Sr/86Sri<0.7056. Les rapports initiaux en Pb indiquent une source dans le manteau enrichi subcontinental lithosphérique, préalablement contaminé par des sédiments océaniques. Les dikes mélanocrates Fe-Ti sont représentatifs de liquides et ont des spectres de terres rares enrichis, une anomalie positive en Nb-Ta et des εNdi de +7, des 87Sr/86Sri de 0.703 et des rapports initiaux en Pb, similaires à ceux des basaltes d'île océanique, indiquant une source asthénosphérique modérément appauvrie. Ainsi, la fusion partielle du manteau lithosphérique subcontinental est induite par l'amincissement post-orogénique et la remontée de l'asthénosphère. Les filons mélanocrates proviennent, après délamination du manteau lithosphérique, de la fusion de l'asthénosphère. Abstract The early Permian Mont Collon mafic complex (Dent Blanche nappe, Austroalpine nappe system) is one of the best preserved examples of the Permian mafic magmatism in the Western Alps. It is composed of discontinuous exposures and a well-preserved magmatic layering (the Dents de Bertol cliff) crops out in the center part of the complex. It mainly consists of cumulative mafic rocks, which represent 95 vol-% of the mafic complex (ol- and cpx-bearing gabbros and rare anorthositic layers, troctolites, wehrlites and plagioclase-wehrlites) and locally pegmatitic gabbros. All these facies are crosscut by widespread acidic (aplites, quartz-rich pegmatites, microgranodiorites) and late mafic Fe-Ti melanocratic dikes. Olivine-augite thermometric calculations yield a range of 1070-1120 ± 6°C, while amphibole-plagioclase thermometer yields a temperature of 740 ± 40°C at 0.5 GPa. Pyroxene geobarometry points to a pressure of 0.3-0.6 GPa, indicating a middle crustal level of emplacement. Moreover, temperature calculations on the Mont Conon coronitic amphiboles indicate temperatures of 700 ± 40°C, close to those calculated for magmatic amphiboles. These temperatures confirm that coronitic reactions occurred at subsolidus conditions. ID-TIMS U/Pb zircon ages of 284.2 ± 0.6 and 282.9 ± 0.6 Ma obtained on a pegmatitic gabbro and a quartz-pegmatitic dike, respectively, were interpreted as the crystallization ages of these rocks. 40Ar/39Ar dating on amphiboles from Fe-Ti melanocratic dikes yields a plateau age of 260.2 ± 0.7 Ma, which is probably very close to the crystallization age. Consequently, this 40Ar/P39Ar age indicates a second magmatic event. Whole-rock major- and trace-element compositions show little variation across the whole intrusion and Mg-number stays within a narrow range (75-80). Trace-element concentrations record the cumulative nature of the rocks (e.g. positive Eu anomaly) and reveal systematic Nb, Ta, Zr, Hf and Ti negative anomalies for all basic facies. The lack of correlation between major and trace elements is characteristic of an in situ crystallization process involving variable amounts of interstitial liquid (L) trapped between the cumulus mineral phases. LA-ICPMS measurements show that trace-element distributions in minerals are homogeneous, pointing to subsolidus re-equilibration between crystals and interstitial melts. A quantitative modeling based on Langmuir's in situ crystallization equation successfully reproduced the Rare Earth Element (REE) concentrations in cumulitic minerals. The calculated amounts of interstitial liquid L vary between 0 and 35% for degrees of differentiation F of 0 to 45%, relative to the least evolved facies of the intrusion. Furthermore, L values are well correlated with the modal proportions of interstitial amphibole and whole-rock incompatible trace-element concentrations (e.g. Zr, Nb) of the tested samples. The calculated parental melt of the Mont Collon cumulates is characterized by a relative enrichment in Light REE and Th, a depletion in Heavy REE, typical of a transitional affinity (T-MORB), and strong negative Nb-Ta anomaly. Cumulative rocks display Nd-Sr isotopic compositions close to the BSE (-0.6 < εNdi < +3.2, 0.7045 < 87Sr/86Sri < 0.7056). Initial Pb ratios point to an origin from the melting of an enriched subcontinental lithospheric mantle source, previously contaminated at the source by oceanic sediments. The contrasted alkaline Fe-Ti melanocratic dikes are representative of liquids. They display enriched fractionated REE patterns, a positive Nb-Ta anomaly and εNdi of +7, 87Sr/86Sri of 0.703 and initial Pb ratios, all reminiscent of Ocean Island Basalt-type rocks, pointing to a moderately

Etude systématique, cladistique et biogéographique des Baetidae (Ephemeroptera) de Madagascar

Les Ephéméroptères constituent un ordre très archaïque d?insectes ailés, comprenant un nombre réduit d?espèces (actuellement environ 2500 espèces). Les larves sont aquatiques; la durée de ce stade est en général d?une année. Le stade adulte est par contre extrêmement bref: de quelques heures à quelques jours. La fonction quasi unique de ce stade est la reproduction. Par sa superficie, Madagascar est la quatrième île du monde. Elle est située dans la partie occidentale de l?Océan Indien à plus de 300 km de la côte africaine. Madagascar faisait partie du super-continent Gondwana. Elle s?est séparée de l?Afrique (-165 M.a.), puis a migré vers le Sud (-125 M.a.) avant de se détacher du sous-continent indien (-65 M.a.). La connaissance des Ephéméroptères malgaches était, jusqu?à très récemment, extrêmement limitée. Grâce au programme Biodiversité et biotypologie des eaux continentales malgaches, lancé conjointement par l?ORSTOM (actuel IRD, France) et le CNRE (Madagascar), un inventaire à large échelle de la macrofaune benthique malgache a été entrepris. La systématique de plusieurs familles d?Ephéméroptères (Tricorythidae, Polymitarcyidae, Palingeniidae,?), ainsi que d?autres groupes d?invertébrés (Trichoptères, Simuliidae, macrocrustacés) a fait l?objet d?études approfondies. La présente étude consistue un des volets de ce programme. Jusqu?au milieu des années 1990, seules quatre espèces valides appartenant à trois genres différents étaient décrites de Madagascar. En 6 ans, ce ne sont pas moins de 25 articles qui sont consacrés à la systématique des Baetidae, permettant de décrire 50 espèces et 8 genres nouveaux. La faune malgache des Baetidae compte actuellement 22 genres et 54 espèces. Malgré sa taille, Madagascar possède une richesse, tant générique que spécifique équivalente à celle d?un continent. Notre connaissance des Baetidae est suffisamment avancée pour mener une étude cladistique et biogéographique. La reconstruction phylogénétique a permis de mettre en évidence cinq lignées principales à Madagascar et de préciser, pour chacune d?elles, les genres inclus et les caractères propres. La faune des Baetidae malgaches présente un taux d?endémicité très élevé: 53 des 54 espèces et un tiers des genres sont endémiques. Elle montre des affinités extrêmement fortes avec la faune africaine, puisque 90% des genres présents à Madagascar ou en Afrique ont une répartition strictement restreinte à cette région. Les autres composantes, notamment orientales et océaniennes, sont négligeables; ces régions n?ont en commun avec Madagascar qu?un nombre restreint de genres cosmopolites. Ces affinités sont en contradiction avec les données géologiques de la dislocation du Gondwana. Plusieurs explications peuvent être données pour résoudre cette contradiction. La plus vraisemblable est que le pouvoir de dispersion des Ephéméroptères, et des Baetidae en particulier, est nettement sous-estimé. L?étude des faunes des îles volcaniques récentes, telles que les Comores, démontre clairement que les Baetidae sont capables de dispersion sur une distance de plus de 300 km. Il est donc possible d?envisager une colonisation de Madagascar à partir de l?Afrique continentale postérieure à la séparation des deux plaques. Nous avons établi des scénarios retraçant l?histoire biogéographique de chacune des cinq lignées. Pour quatre d?entre elles, l?Afrique continentale est le centre d?origine. La cinquième lignée aurait une origine paléarctique; l?Afrique représenterait un centre secondaire de spéciation. Ces lignées auraient secondairement colonisé Madagascar à partir de l?Afrique continentale. Ce travail ouvre donc d?importantes perspectives. Il rend possible l?utilisation à un niveau générique, voire spécifique, des Baetidae pour des travaux de faunistique ou d?écologie, en particulier pour des études liées à la dégradation de la qualité de l?eau. Il devrait également pouvoir servir de base pour l?étude et la compréhension des phénomènes de dispersion et colonisation dans les îles et archipels de l?Ouest de l?Océan Indien.<br/><br/>Mayflies (Ephemeroptera) are among the oldest known flying insects and encompass a very small number of species (ca 2500 species). Larvae are strictly freshwater inhabitants; this stage lasts generally one year. The imaginal stage is extremely short, from few hours to few days, and is devoted almost entirely to reproduction. Madagascar is the fourth largest island in the world by area. It is situated in the western part of the Indian Ocean, at a distance of more than 300 km from the African coast. Madagascar belonged to Gondwana. It was first separated from the African plate (-165 M.y.), then moved to the South (-65 M.y.), before the break-off with the Indian plate (-65 M.y.). Knowledge of the Malagasy mayflies was until recently extremely poor. The program Biodiversity and Biotypology of Malagasy Freshwaters, jointly run by the French ORSTOM and the Malagasy CNRE, began a global survey of the freshwater macroinvertebrates. The systematics of several mayfly families (Tricorythidae, Polymitarcyidae, Palingeniidae,?), and other invertebrate groups (Caddisflies, Blackflies,?) was the subject of ground studies. Our present study is one part of this global program. Until the middle of the nineties, only four baetid species belonging to three different genera had been described from Madagascar. During the last six years, 25 papers were dedicated to the systematics of the Baetidae, allowing the description of 50 new species and 8 new genera. The Malagasy fauna encompasses now 22 genera and 54 species. Despite its size, Madagascar has the same diversity, at specific and generic level, as a continent. Our knowledge of the Baetidae is sufficient to perform a cladistic and biogeographical study. Our phylogenetic reconstruction allows us to propose five main lineages and to indicate, for each of them, the genera included and their features. The Malagasy fauna of Baetidae possesses a high level of endemicity: 53 of the 54 species and one third of the genera are endemic. It shows extremely strong affinities with the African fauna, as more than 90% of the genera present in Madagascar or in Africa have a distribution restricted to this area. Other components, especially Oriental and Oceanian, are negligible. These areas share with Madagascar only a few widespread genera. These African affinities are in contradiction with the geological events, especially the break-off history of Gondwana. Some explanations can be given to solve this contradiction. The most likely is that the dispersal power of the mayflies, especially of the Baetidae, is greatly underestimated. The study of recent volcanic islands, particularly of the Comoros, clearly demonstrates that the Baetidae are able to disperse over more than 300 km. Consequently, a colonisation by the Baetidae, of Madagascar from the continental Africa, after the break-off must be considered as possible. We have established scenarios explaining the biogeographical history of each of the five lineages. For four of them, Africa has to be regarded as the centre of origin. The fifth lineage probably has a Palearctic origin; Africa should be considered as a secondary centre of speciation. These lineages should have secondarily colonised Madagascar from continental Africa. This work opens up new perspectives. It allows the use of the Baetidae for faunistic and ecological studies, especially for problems related to water quality. It must be also considered as a first step for understanding the dispersion and colonisation of the islands of the western part of the Indian Ocean.

Spatially varying selection shapes life history clines among populations of Drosophila melanogaster from sub-Saharan Africa.

Clines in life history traits, presumably driven by spatially varying selection, are widespread. Major latitudinal clines have been observed, for example, in Drosophila melanogaster, an ancestrally tropical insect from Africa that has colonized temperate habitats on multiple continents. Yet, how geographic factors other than latitude, such as altitude or longitude, affect life history in this species remains poorly understood. Moreover, most previous work has been performed on derived European, American and Australian populations, but whether life history also varies predictably with geography in the ancestral Afro-tropical range has not been investigated systematically. Here, we have examined life history variation among populations of D. melanogaster from sub-Saharan Africa. Viability and reproductive diapause did not vary with geography, but body size increased with altitude, latitude and longitude. Early fecundity covaried positively with altitude and latitude, whereas lifespan showed the opposite trend. Examination of genetic variance-covariance matrices revealed geographic differentiation also in trade-off structure, and QST -FST analysis showed that life history differentiation among populations is likely shaped by selection. Together, our results suggest that geographic and/or climatic factors drive adaptive phenotypic differentiation among ancestral African populations and confirm the widely held notion that latitude and altitude represent parallel gradients.

Reconceptualizing Chinese state-owned entreprise in Africa : double embeddedness and localization in Ghana

Challenging the view of asymmetrical power relations between China and Africa, this thesis questions the "Chinese comparative advantages" (monolithic state power and economic advantages) of Chinese state-owned enterprises (SOEs) in Africa. It argues that the power dynamics between Chinese and African actors are dialectical and pluralistic, with localized social capital representing the true Chinese competitive advantage in Africa. Based on ethnographical fieldwork conducted in Ghana, this thesis shows that Chinese SOEs pursue their globalization in a double context - that of the deliberate "retreat" of the Chinese state, and more importantly, that of Ghanaian governance and society (characterized by political party patronage, extraversion dynamics, and worker agency). The trajectories of Chinese expatriates' expatriation/ social promotion and their SOEs' globalization/ localization are mutually influenced and reinforced. By cultivating local relationships and knowledge, a provincial Chinese SOE in Ghana can outperform a large Chinese central SOE, even if the latter has more support from the Chinese state. Moreover, the recent effort to build a "socially acceptable Chinese community" in Ghana has renewed the power dynamics between the Chinese state and the SOEs. All these observations provide for constructing a new perspective of Chinese SOEs in Africa - a "second-class" Chinese globalization - the SOEs may begin with few privileges, but promotion over time is possible. -- A contre pied des approches postulant des relations de pouvoir asymétriques entre la Chine et l'Afrique, cette thèse interroge les « avantages comparatifs chinois » (pouvoir de l'État monolithique et avantages économiques) des entreprises publiques chinoises (EPC) en Afrique. Elle soutient l'idée selon laquelle les dynamiques de pouvoir entre les acteurs chinois et africains est dialectique et pluraliste, et le capital social localisé étant le véritable avantage compétitif chinois en Afrique. S'appuyant sur un travail de terrain ethnographique au Ghana, cette thèse montre que les EPC poursuivent leur mondialisation dans un double contexte - celui de la «retraite» délibérée de l'État chinois, et, de façon plus importante, celui de la gouvernance et de la société ghanéennes (caractérisées par un clientélisme des partis politiques, une dynamique d'extraversion et le pouvoir de négociation des travailleurs). Les trajectoires d'expatriation / de promotion sociale des expatriés chinois et la mondialisation / localisation de leurs EPC s'influencent et se renforcent mutuellement. En cultivant des relations et des connaissances locales, une EPC provinciale au Ghana peut surpasser une grande EPC centrale, même si cette dernière reçoit plus de soutien de l'État chinois. En outre, les efforts récents visant à construire une «communauté chinoise socialement acceptable» au Ghana ont renouvelé la dynamique du pouvoir entre l'État chinois et les EPC. Ces observations permettent de construire une nouvelle perspective des EPC en Afrique - la globalisation chinoise de « deuxième classe » - les EPC peuvent débuter avec peu de privilèges, mais leur promotion reste possible avec le temps.

DNA barcoding of Corsican mayflies (Ephemeroptera) with implications on biogeography, systematics and biodiversity

Mayflies (Ephemeroptera) are known to generally present a high degree of insular endemism: half of the 28 species known from Corsica and Sardinia are considered as endemic. We sequenced the DNA barcode (a fragment of the mitochondrial COI gene) of 349 specimens from 50 localities in Corsica, Sardinia, continental Europe and North Africa. We reconstructed gene trees of eight genera or species groups representing the main mayfly families. Alternative topologies were built to test if our reconstructions suggested a single or multiple Corsican/Sardinian colonization event(s) in each genus or species group. A molecular clock calibrated with different evolution rates was used to try to link speciation processes with geological events. Our results confirm the high degree of endemism of Corsican and Sardinian mayflies and the close relationship between these two faunas. Moreover, we have evidence that the mayfly diversity of the two islands is highly underestimated as at least six new putative species occur on the two islands. We demonstrated that the Corsican and Sardinian mayfly fauna reveals a complex history mainly related to geological events. The Messinian Salinity Crisis, which is thought to have reduced marine barriers, thus facilitating gene flow between insular and continental populations, was detected as the most important event in the speciation of most lineages. Vicariance processes related to the split and rotation of the Corso-Sardinian microplate had a minor impact as they involved only two genera with limited dispersal and ecological range. Colonization events posterior to the Messinian Salinity Crisis had only marginal effects as we had indication of recent gene flow only in two clades. With very limited recent gene flow and a high degree of endemism, mayflies from Corsica and Sardinia present all the criteria for conservation prioritization.

Western blotting as a tool for the serodiagnosis of farmer's lung disease: validation with Lichtheimia corymbifera protein extracts.

Electrosyneresis and double diffusion are immunoprecipitation techniques commonly used in the serological diagnosis of Farmer's lung disease (FLD). These techniques are reliable but lack standardization. The aim of this study was to evaluate Western blotting for the serodiagnosis of FLD. We carried out Western blotting with an antigenic extract of Lichtheimia corymbifera, an important aetiological agent of the disease. The membranes were probed with sera from 21 patients with FLD and 21 healthy exposed controls to examine the IgG antibody responses against purified somatic antigens. Given the low prevalence of the disease, 21 patients could be considered as a relevant series. Four bands were significantly more frequently represented in membranes probed with FLD sera (bands at 27.7, 40.5, 44.0 and 50.5 kDa) than those probed with control sera. We assessed the diagnostic value of different criteria alone or in combination. The diagnostic accuracy of the test was highest with the inclusion of at least two of the following criteria: at least five bands on the strip and the presence of one band at 40.5 or 44.0 kDa. Sensitivity, specificity and positive and negative predictive values were all 81%, and the odds ratio was 18.06. Inclusion of bands of high intensity diminished rather than improved the diagnostic value of the test. We concluded that Western blotting is a valuable technique for the serodiagnosis of FLD. The industrial production of ready-to-use membranes would enable the routine use of this technique in laboratories, and provide reliable and standardized diagnostic results within a few hours.