CCR5 Revisited: How Mechanisms of HIV Entry Govern AIDS Pathogenesis

The chemokine receptor CCR5 has been the focus of intensive studies since its role as a coreceptor for HIV entry was discovered in 1996. These studies lead to the development of small molecular drugs targeting CCR5, with maraviroc becoming in 2007 the first clinically approved chemokine receptor inhibitor. More recently, the apparent HIV cure in a patient transplanted with hematopoietic stem cells devoid of functional CCR5 rekindled the interest for inactivating CCR5 through gene therapy and pharmacological approaches. Fundamental research on CCR5 has also been boosted by key advances in the field of G-protein coupled receptor research, with the realization that CCR5 adopts a variety of conformations, and that only a subset of these conformations may be targeted by chemokine ligands. In addition, recent genetic and pathogenesis studies have emphasized the central role of CCR5 expression levels in determining the risk of HIV and SIV acquisition and disease progression. In this article, we propose to review the key properties of CCR5 that account for its central role in HIV pathogenesis, with a focus on mechanisms that regulate CCR5 expression, conformation, and interaction with HIV envelope glycoproteins.     

Neotrygon indica sp. nov., the Indian Ocean blue-spotted maskray (Myliobatoidei,Dasyatidae)

The blue-spotted maskray, previously N. kuhlii, consists of up to eleven lineages representing separate species. Nine of these species (N. australiae, N. bobwardi, N. caeruleopunctata, N. malaccensis, N. moluccensis, N. orientale, N. vali, N. varidens, N. westpapuensis) have already been formally described and two (Indian Ocean maskray and Ryukyu maskray) remain undescribed. Here, the Indian Ocean maskray is described as a new species, Neotrygon indica sp. nov. Specimens of the new species were generally characterized on their dorsal side by a moderately large number of small ocellated blue spots, a low number of medium-sized ocellated blue spots, the absence of large ocellated blue spots, a high number of dark speckles, a few dark spots, and a conspicuous occipital mark. The new species formed a distinct haplogroup in the tree built from concatenated nucleotide sequences at the CO1 and cytochrome b loci. A diagnosis based on colour patterns and nucleotide sequences at the CO1 and cytochrome b loci is proposed. The distribution of N. indica sp. nov. includes the Indian coast of the Bay of Bengal, the Indian coast of the Laccadives Sea, and Tanzania. Considerable sampling effort remains necessary for an in-depth investigation of the phylogeographic structure of the Indian Ocean maskray.     

The genus Opisthacanthus Peters, 1861 (Scorpiones: Hormuridae), a remarkable Gondwanian group of scorpions

New comments are proposed on the geographic distribution of genus Opisthacanthus, and the Gondwanian model is further supported. The diversity of the genus is extraordinary in Madagascar, with the same number of species as in continental Africa, but sub-Saharan Africa is home to six out of the nine groups currently recognized of Opisthacanthus. Given the affinities of the Opisthacanthus groups and their current distribution, a center of origin in Africa could be favored for these ancient scorpions. The proposed Gondwana model suggests that the Madagascar Opisthacanthus are closer to those of the New World, which is consistent with the affinities observed in morphological characters. A new species, Opisthacanthus titanus sp. n., is described from the Torotorofotsy Forest, located in Eastern Madagascar. The new species shows affinities with both Opisthacanthus madagascariensis Kraepelin, 1894 known from dry regions in the western portion of the island and Opisthacanthus lavasoa Lourenço, Wilmé & Waeber, 2016 only known from the extreme southeast of the island. The new species and O. madagascariensis have similar external morphologies but the morphometric values are markedly distinct. Moreover, O. madagascariensis is exclusively found in spiny forest thickets and open woodlands, whereas the new species was found in the humid forest of Torotorofotsy. The total number of species in Madagascar is now raised to twelve. Biogeographical scenarios are also proposed to infer the origin of the Opisthacanthus and better understand its distribution in the New World, in Africa and Madagascar.     

Preliminary Investigation of a 64-element Capacitive Micromachined Ultrasound Transducer (CMUT) Annular Array Designed for High Intensity Focused Ultrasound (HIFU)

Background

Treatment of prostate cancer using endocavitary High Intensity Focused Ultrasound (HIFU) has become more commonplace since the first treatments in the 1990s. The gold standard HIFU strategy to treat prostate cancer is the complete thermal ablation of the entire prostate gland under real-time ultrasound (US) image guidance. A more desirable treatment and the current trend, however, is towards a focal treatment but more accurate and finely tunable thermal lesions are needed along with improved US imaging guidance. In this study, Capacitive Micromachined Ultrasound Transducer (CMUT) technology is being investigated, as they have shown recent promise for US imaging and potential to be used for HIFU therapy. They offer potential advantages over current piezoelectric designs in the context of ultrasound-guided HIFU (USgHIFU) focal therapies.

Party competition and the production of nationhood in the immigration context: particularizing the universal for political gain in France and Québec

Analysing parties’ media representations in the context of France’s 2010 legal ban of Islamic facial coverings and Québec’s (rejected) Charter of Values in 2013, this paper foregrounds the neglected role that party competition plays in shaping the construction of nationhood in public debates around immigrant religious practices. Our findings show that in these debates, political parties aim to maintain their distinct identities by generating a particular universalism, in which purportedly “universal” values, such as gender equality, are imbricated with particularistic images of nationhood.     

Le Crocodilien Steneosaurus (Mesosuchia,Teleosauridae) dans le Jurassique supérieur franc-comtois (Jura,France)

Two new fossil vertebrate localities have been discovered close to each other in the Upper Jurassic (Effingen beds, Upper Oxfordian) of the Southern Jura department (France). One of the localities have yielded an incomplete skeleton of the crocodilian Steneosaurus (including a well preserved skull), as well as fish remains and an abundant invertebrate fauna. The second locality has mainly yielded various fragmentary bones of Steneosaurus. This is the first discovery of well preserved crocodilian remains in the Oxfordian of the Jura.     

Variabilité et disjonction évolutive des caractèresdans les populations de Micraster (Echinoidea,spatangoida) du Crétacé supérieur de Picardie

Morphological variation in Turonian and Coniacian Micraster (Irregular Echinoids) from Picardy is analysed in samples from 4 beds stratigraphically superimposed in the chalk cliff and numbered C2, C3, C4 and C5. The statistical study is made of 23 characters (12 quantitative and 11 qualitative).In first part, uni- and multivariate analysises, complementedby observations of populations, have enabled us to recognize M. leskei (Des Moulins) in the two lower beds and M. decipiens (Bayle) in the upper ones.The growth of M. leskei is analysed in the second part. The biometrical study (bi- and multivariate analysises) of growth processes of the C2-bed urchins (which are small) and of the C3- bed urchins (which are sometimes much bigger) shows the homology of their ontogeny and confirms the name «large M. leskei given by R.B. Stokes for the C3 urchins. The genetic or ecological origin of that variation is discussed.In the third part, the analysis (multivariate) has enabled to understand the considerable variability of M. decipiens. This species contains several morphological types: trapezoidal or heart-shaped urchins, and conical- shaped urchins. The study shows that «gibbous forms are simple variants and that the two first forms may be considered as morphs of the same species. It is possible that these forms are separate species.     

NEW JELLYFISH TAXA FROM THE UPPER JURASSIC LITHOGRAPHIC LIMESTONES OF CERIN (FRANCE): TAPHONOMY AND ECOLOGY

Abstract:  Abundant well-preserved jellyfish impressions are described from the Cerin Lagerstätte (Ain, eastern France). The enclosing sediments are lithographic limestones deposited in a Late Kimmeridgian lagoon lying on an emergent reef complex. Two new taxa of Scyphozoa are proposed: Paraurelia cerinensis gen. et sp. nov. (abundant) and Paraurelia sp. A (rare), and two new taxa of Cubozoa: Bipedalia cerinensis gen. et sp. nov. (rare) and Paracarybdea lithographica gen. et sp. nov. (very rare). Rapid covering by a microbial mat helped the preservation of the animals. Many specimens of Paraurelia cerinensis are deformed by slippage down the palaeoslope, which characterizes the margin of the lagoon. Their resultant morphology and their orientation clearly indicate the downslope direction. Tentacles of Bipedalia cerinensis and Paracarybdea lithographica are also orientated according to the palaeoslope. The jellyfish were probably dead individuals occasionally introduced into the Cerin lagoon. However, another hypothesis may be considered with reference to the model of the present-day jellyfish lakes in Palau (Caroline Islands, Western Pacific). Jellyfish could have lived in the more oxygenated upper layer of water of the Cerin lagoon that allowed pelagic life. This situation could have corresponded to short periods of easier communication between the open sea and the lagoon. Jellyfish are only found in the lower beds of the lithographic limestones and their distribution illustrates the supposed evolution of the Cerin lagoon. Initially, it was deep, mainly flooded, with possibly autochthonous jellyfish and allochthonous animals indicating clear marine influence. Later, the lagoon shallowed and its sediments often emerged with marginal marine burrows and plants indicating increasing terrestrial influence.     

ISOPOD TRACKWAYS FROM THE CRAYSSAC LAGERSTÄTTE, UPPER JURASSIC, FRANCE

Abstract:  Well-preserved arthropod trackways are described from the laminated limestones of the Crayssac Lagerstätte (south-west France, Lower Tithonian). They occur in sediments deposited in the temporary coastal mudflats of intertidal to supratidal zones. The trackways are referred to Pterichnus isopodicus isp. nov., and are interpreted as the locomotion traces of isopods. Different trackway morphotypes are recognized and clearly resulted from variations in the original consistency of the sediment. Sinuous trackways may correspond to vagrant activity on wet mud whereas numerous straight ones indicate a more rapid crawling on a soft-to-firm substratum (e.g. tidal flat during emersion). The preferred orientation of trackways indicates that isopods were crawling in a direction perpendicular to shoreline as a result of possible taxis induced by sediment wetness and/or by a migratory behaviour controlled by tidal rhythm. Unusually long emergence of the sediments may have favoured the preservation of dense networks of trackways. An isopod identity is supported by the general morphology of the tracks and the association of trackways with isopod body fossils. Archaeoniscus , which occurs abundantly in Late Jurassic deposits of England and France, was probably the trace-maker.     

Ulphaceaster sarthacensis,nouveau genre et nouvelle espèce d’échinide Archiaciidae du Cénomanien (Sarthe,France)

A new genus and a new species of the echinoid family Archiaciidae from Cenomanian deposits in Sarthe (Paris Basin, France) are described. The genus Ulphaceaster nov. gen. can be distinguished from other archiaciids by its anterior ambulacrum, which is located in a deep groove running from the peristome to the apex where the test enlarges in a tea-spoon shape. The apical rostrum is taller and more slender than for species of the close genus Claviaster. The species Uphaceaster sarthacensis sp. nov. is known from the Saint-Ulphace locality only (Sables et Grès de Lamnay Formation, La Garenne quarry), where it is found in shallow marine sandy limestones, from infralittoral deposit environments.