Influence of the initial condition in equilibrium last-passage percolation models

In this paper we consider an equilibrium last-passage percolation model on an environment given by a compound two-dimensional Poisson process. We prove an L-2-formula relating the initial measure with the last-passage percolation time. This formula turns out to be a useful tool to analyze the fluctuations of the last-passage times along non-characteristic directions.

A PHASE TRANSITION FOR COMPETITION INTERFACES

We study the competition interface between two growing clusters in a growth model associated to last-passage percolation. When the initial unoccupied set is approximately a cone, we show that this interface has an asymptotic direction with probability 1. The behavior of this direction depends on the angle theta of the cone: for theta >= 180 degrees, the direction is deterministic, while for theta < 180 degrees, it is random, and its distribution can be given explicitly in certain cases. We also obtain partial results on the fluctuations of the interface around its asymptotic direction. The evolution of the competition interface in the growth model can be mapped onto the path of a second-class particle in the totally asymmetric simple exclusion process; from the existence of the limiting direction for the interface, we obtain a new and rather natural proof of the strong law of large numbers (with perhaps a random limit) for the position of the second-class particle at large times.

Isolation, culture et caractérisation phénotypique de cellules musculaires lisses endobronchiques équines.

Le muscle lisse endobronchique est l’un des acteurs principaux de l’asthme. La description de ces caractéristiques phénotypiques reste cependant très elliptique, notamment à cause de la difficulté inhérente à l’échantillonnage. Le cheval offre un large champ d’investigation en raison de sa taille et un modèle d’asthme pertinent en regard de la similitude entre asthme et souffle. La technique de culture et de caractérisation du muscle lisse a été mise au point à partir de muscle lisse trachéal. Ce modèle a ensuite été transposé et réalisé à partir de biopsies endobronchiques chez le cheval. Les cellules du muscle lisse ont été isolées, mises en culture puis caractérisées par immunofluorescence, cytométrie de flux et immunobuvardage. Le maintien du phénotype contractile en culture restant un défi dans l’établissement d’un modèle d’asthme réaliste. Suite à l’isolement des cellules musculaires lisses à partir de muscle lisse trachéal équin et leur mise en culture en présence de 10% de FBS pendant 7 passages, 96.4% des cellules expriment l’α-smooth muscle-actine (α-sm-actine), tandis que 83.8% et 77% expriment la desmine et la myosine respectivement. Les cellules musculaires lisses issues de biopsies endobronchiques expriment après 7 passages à 84% l’α-sm-actine, à 57% la desmine et 69% la myosine. Ces résultats ont été obtenus par immunofluorescence et immunobuvardage. Le pourcentage de cellules exprimant les protéines d’intérêt, tout comme l’intensité moyenne de fluorescence ne présentent pas de variation significative ni entre le 4ième et le 7ième passage, ni avec la caractérisation initiale, lors du premier passage. Cette étude suggère qu’il est possible de maintenir le phénotype contractile en culture sur plastique en présence de 10% de FBS, et que les biopsies endobronchiques sont un support d’étude valable pour de futures investigations concernant le rôle du muscle lisse et ses caractéristiques.

The last voyage of Capt. Sir John Ross ... to the Arctic regions for the discovery of a north west passage : performed in the years 1829-30-31-32 and 33 : to which is prefixed an abridgement of the former voyages of Captns. Ross, Parry & other celebrated navigators to the northern latitudes : compiled from authentic information and original documents transmitted by an officer attached to the last expedition ; illustrated by engravings from drawings taken on the spot /

"On the position of the north magnetic pole. (Supplement)": 44 p. at end.

Melancholy shipwreck, and remarkable instance of the interposition of Divine Providence, in the preservation of the lives of 12 unfortunate persons, who were shipwrecked on the 3d of December last, 1833, on their passage from Portsmouth, Eng. to Bombay, and after being 17 days in an open boat, subsisting on an allowance of half a biscuit to each per day, were providentially picked up by an English homeward bound whaleman.

Mode of access: Internet.

Detection of high-velocity material from the wind-wind collision zone of Eta Carinae across the 2009.0 periastron passage

We report near-infrared spectroscopic observations of the Eta Carinae massive binary system during 2008-2009 using the CRIRES spectrograph mounted on the 8m UT 1 Very Large Telescope (VLT Antu). We detect a strong, broad absorption wing in He I lambda 10833 extending up to -1900 km s(-1) across the 2009.0 spectroscopic event. Analysis of archival Hubble Space Telescope/Space Telescope Imaging Spectrograph ultraviolet and optical data identifies a similar high-velocity absorption (up to -2100 km s(-1)) in the ultraviolet resonance lines of Si IV lambda lambda 1394, 1403 across the 2003.5 event. Ultraviolet resonance lines from low-ionization species, such as Si II lambda lambda 1527, 1533 and CII lambda lambda 1334, 1335, show absorption only up to -1200 km s(-1), indicating that the absorption with velocities -1200 to -2100 km s(-1) originates in a region markedly more rapidly moving and more ionized than the nominal wind of the primary star. Seeing-limited observations obtained at the 1.6m OPD/LNA telescope during the last four spectroscopic cycles of Eta Carinae (1989-2009) also show high-velocity absorption in He I lambda 10833 during periastron. Based on the large OPD/LNA dataset, we determine that material with velocities more negative than -900 km s(-1) is present in the phase range 0.976 <= phi <= 1.023 of the spectroscopic cycle, but absent in spectra taken at phi <= 0.947 and phi >= 1.049. Therefore, we constrain the duration of the high-velocity absorption to be 95 to 206 days (or 0.047 to 0.102 in phase). We propose that the high-velocity absorption component originates in shocked gas in the wind-wind collision zone, at distances of 15 to 45 AU in the line-of-sight to the primary star. With the aid of three-dimensional hydrodynamical simulations of the wind-wind collision zone, we find that the dense high-velocity gas is along the line-of-sight to the primary star only if the binary system is oriented in the sky such that the companion is behind the primary star during periastron, corresponding to a longitude of periastron of omega similar to 240 degrees-270 degrees. We study a possible tilt of the orbital plane relative to the Homunculus equatorial plane and conclude that our data are broadly consistent with orbital inclinations in the range i = 40 degrees-60 degrees.

Perception d’effort et de mise en charge et asymétrie motrice lors du passage assis à debout chez le sujet hémiparétique

L’asymétrie de mise en charge (MEC) lors du passage assis à debout (PAD) chez les personnes hémiparétiques est une observation clinique connue mais peu expliquée. Ce projet visait donc le développement de connaissances sur les facteurs explicatifs de l’asymétrie de MEC chez cette clientèle en s’intéressant plus spécifiquement au lien entre la distribution des efforts aux genoux lors du PAD et l’asymétrie de MEC observée ainsi qu’à la perception de ces deux éléments lors de cette tâche. Ainsi, les objectifs généraux étaient de : 1) déterminer si l’exécution spontanée asymétrique du PAD des sujets hémiparétiques est expliquée par une distribution des efforts symétriques aux genoux en quantifiant ces efforts par le Taux d’utilisation musculaire électromyographique (TUMEMG) et, 2) déterminer si les individus hémiparétiques sont conscients des stratégies motrices qu’ils utilisent en évaluant leurs perceptions de MEC et d’efforts aux genoux durant le PAD. La première étude a évalué la capacité des personnes hémiparétiques à percevoir leur distribution de MEC aux membres inférieurs lors du PAD. Par rapport aux participants sains, leur distribution de MEC fut davantage asymétrique et leurs erreurs de perception plus élevées. La deuxième étude a quantifié la distribution des efforts aux genoux chez les sujets sains et hémiparétiques lors du PAD spontané. Les deux groupes ont montré une association entre leur distribution de MEC et leur distribution d’effort. Toutefois, la relation était plus faible chez les patients. Le classement des participants hémiparétiques en sous-groupes selon leur degré d’asymétrie de force maximale des extenseurs des genoux (faible, modéré, sévère) a révélé une similarité des efforts aux genoux parétique et non parétique chez le groupe ayant une atteinte sévère. La troisième étude a déterminé si la perception de la distribution des efforts aux genoux des sujets hémiparétiques était reliée à leur distribution réelle d’effort mesurée lors de PAD exécutés dans différentes positions de pieds. En plus d’être incapables de percevoir les changements de distribution d’effort induits par les différentes positions de pieds, leurs erreurs de perception d’effort furent plus élevées que celles de MEC. Par le biais du test fonctionnel assis-debout de cinq répétitions, la dernière étude a déterminé l’influence du nombre de répétitions du PAD sur les distributions de MEC et d’efforts aux genoux chez les sujets sains et hémiparétiques. Contrairement aux contrôles, les distributions des sujets hémiparétiques furent plus asymétriques à la première répétition du test fonctionnel que lors de l’exécution spontanée unique du PAD. En somme, les résultats de cette thèse ont démontré que la distribution des efforts aux genoux doit être considérée parmi les facteurs explicatifs de l’asymétrie de MEC des individus hémiparétiques lors du PAD et qu’il y a un besoin de mieux documenter la perception des personnes hémiparétiques lorsqu’elles exécutent des tâches fonctionnelles.

Abrupt changes in high-latitude nutrient supply to the Atlantic during the last glacial cycle

The supply of nutrients to the low-latitude thermocline is largely controlled by intermediate-depth waters formed at the surface in the high southern latitudes. Silicic acid is an essential macronutrient for diatoms, which are responsible for a significant portion of marine carbon export production. Changes in ocean circulation, such as those observed during the last deglaciation, would influence the nutrient composition of the thermocline and, therefore, the relative abundance of diatoms in the low latitudes. Here we present the first record of the silicic acid content of the Atlantic over the last glacial cycle. Our results show that at intermediate depths of the South Atlantic, the silicic acid concentration was the same at the Last Glacial Maximum (LGM) as it is today, overprinted by high silicic acid pulses that coincided with abrupt changes in ocean and atmospheric circulation during Heinrich Stadials and the Younger Dryas. We suggest these pulses were caused by changes in intermediate water formation resulting from shifts in the subpolar hydrological cycle, with fundamental implications for the nutrient supply to the Atlantic.

(Table 3) Sedimentation rates of stage 1 and last glacial maximum from different Holes during cruises of RRS Discovery in 1984-1985 and 1987-1988, and RRS James Clark Ross in 1992-1993

Within the Scotia Sea, the axis of the Antarctic Circumpolar Current (ACC) is geographically confined, and sediments therefore contain a record of palaeo-flow speed uncomplicated by ACC axis migration. We outline Holocene and Last Glacial Maximum (LGM) current-controlled sedimentation using data from 3.5-kHz profiles, cores and current meter moorings. Geophysical surveys show areas of erosion and deposition controlled by Neogene basement topography. Deposition occurs in mounded sediment drifts or flatter areas, where 500-1000 m of sediment overlies acoustic basement. 3.5-kHz profiles show parallel, continuous sub-bottom reflectors with highest sedimentation rates in the centre of the drifts, and reflectors converging towards marginal zones of non-deposition. Locally, on the flanks of continental blocks (e.g. South Georgia), downslope processes are dominant. The absence of mudwaves on the sediment drifts may result from the unsteadiness of ACC flow. A core transect from the ACC axis south to the boundary with the Weddell Gyre shows a southward decrease in biogenic content, controlled by the Polar Front and the spring sea-ice edge. Both these features lay farther north at LGM. The cores have been dated by relative abundance of the radiolarian Cycladophora davisiana, and by changes in the biogenic Ba content, a palaeoproductivity indicator. Sedimentation rates range from 3 to 17 cm/ka. The grain size of Holocene sediments shows a coarsening trend from south to north, consistent with strongest bottom-current flow near the ACC axis, though interpretation is complicated by the presence of biogenic grains. Year-long current meter records indicate mean speeds from 7 cm/s in the south to 12 cm/s in the north, with benthic storm frequency increasing northwards. LGM sediments are predominantly terrigenous and show a clearer northward-coarsening trend, with well-sorted silts in the northern Scotia Sea. Assuming a constant terrigenous source, this implies stronger ACC flow at the LGM, contrasting with weaker Weddell Gyre flow deduced from earlier work.

Holocene sedimentation rates in the Northwest Passage

Palynological, geochemical, and physical records were used to document Holocene paleoceanographic changes in marine sediment core from Dease Strait in the western part of the main axis of the Northwest Passage (core 2005-804-006 PC latitude 68°59.552'N, longitude 106°34.413'W). Quantitative estimates of past sea surface conditions were inferred from the modern analog technique applied to dinoflagellate cyst assemblages. The chronology of core 2005-804-006 PC is based on a combined use of the paleomagnetic secular variation records and the CALS7K.2 time-varying spherical harmonic model of the geomagnetic field. The age-depth model indicates that the core spans the last ~7700 cal years B.P., with a sedimentation rate of 61 cm/ka. The reconstructed sea surface parameters were compared with those from Barrow Strait and Lancaster Sound (cores 2005-804-004 PC and 2004-804-009 PC, respectively), which allowed us to draw a millennial-scale Holocene sea ice history along the main axis of the Northwest Passage (MANWP). Overall, our data are in good agreement with previous studies based on bowhead whale remains. However, dinoflagellate sea surface based reconstructions suggest several new features. The presence of dinoflagellate cysts in the three cores for most of the Holocene indicates that the MANWP was partially ice-free over the last 10,000 years. This suggests that the recent warming observed in the MANWP could be part of the natural climate variability at the millennial time scale, whereas anthropogenic forcing could have accelerated the warming over the past decades. We associate Holocene climate variability in the MANWP with a large-scale atmospheric pattern, such as the Arctic Oscillation, which may have operated since the early Holocene. In addition to a large-scale pattern, more local conditions such as coastal current, tidal effects, or ice cap proximity may have played a role on the regional sea ice cover. These findings highlight the need to further develop regional investigations in the Arctic to provide realistic boundary conditions for climatic simulations.

Age models, sedimentology and geochemistry from sediment cores in Drake Passage throughflow

The Drake Passage (DP) is the major geographic constriction for the Antarctic Circumpolar Current (ACC) and exerts a strong control on the exchange of physical, chemical, and biological properties between the Atlantic, Pacific, and Indian Ocean basins. Resolving changes in the flow of circumpolar water masses through this gateway is, therefore, crucial for advancing our understanding of the Southern Ocean's role in global ocean and climate variability. Here, we reconstruct changes in DP throughflow dynamics over the past 65,000 y based on grain size and geochemical properties of sediment records from the southernmost continental margin of South America. Combined with published sediment records from the Scotia Sea, we argue for a considerable total reduction of DP transport and reveal an up to ~40% decrease in flow speed along the northernmost ACC pathway entering the DP during glacial times. Superimposed on this long-term decrease are high-amplitude, millennial-scale variations, which parallel Southern Ocean and Antarctic temperature patterns. The glacial intervals of strong weakening of the ACC entering the DP imply an enhanced export of northern ACC surface and intermediate waters into the South Pacific Gyre and reduced Pacific-Atlantic exchange through the DP ("cold water route"). We conclude that changes in DP throughflow play a critical role for the global meridional overturning circulation and interbasin exchange in the Southern Ocean, most likely regulated by variations in the westerly wind field and changes in Antarctic sea ice extent.

Diatom isotope data from ODP Hole 178-1098A for the last deglaciation (12.2-12.8 ka BP)

Understanding the response of the Antarctic ice sheets during the rapid climatic change that accompanied the last deglaciation has implications for establishing the susceptibility of these regions to future 21st Century warming. A unique diatom d18O record derived from a high-resolution deglacial seasonally laminated core section off the west Antarctic Peninsula (WAP) is presented here. By extracting and analysing single species samples from individual laminae, season-specific isotope records were separately generated to show changes in glacial discharge to the coastal margin during spring and summer months. As well as documenting significant intra-annual seasonal variability during the deglaciation, with increased discharge occurring in summer relative to spring, further intra-seasonal variations are apparent between individual taxa linked to the environment that individual diatom species live in. Whilst deglacial d18O are typically lower than those for the Holocene, indicating glacial discharge to the core site peaked at this time, inter-annual and inter-seasonal alternations in excess of 3 per mil suggest significant variability in the magnitude of these inputs. These deglacial variations in glacial discharge are considerably greater than those seen in the modern day water column and would have altered both the supply of oceanic warmth to the WAP as well as regional marine/atmospheric interactions. In constraining changes in glacial discharge over the last deglaciation, the records provide a future framework for investigating links between annually resolved records of glacial dynamics and ocean/climate variability along the WAP.

Last Instar Larvae And Pupae Of Ourocnemis Archytas And Anteros Formosus (lepidoptera: Riodinidae), With A Summary Of Known Host Plants For The Tribe Helicopini.

Last instar larvae and pupae of Ourocnemis archytas (Lepidoptera: Riodinidae) are described for the first time and compared with those of Anteros formosus, which are also described in detail. Last instars of both species present body covered with long white plumose setae, a row of orange balloon setae on the prothoracic shield, and clusters of perforated cupola organs (PCOs) near the spiracles; differences are the black cephalic capsule, the placement and format of balloon setae cluster, and the presence of enlarged black tips on some plumose setae. Pupae of O. archytas resemble that of Anteros, covered with the last instar setae and with no balloon setae. Characteristics of the immature stages of these two genera could be useful to establish the still unresolved relationship between them. A summary of the host plants of Helicopini is presented, showing a polyphagous pattern for Anteros, recorded in 21 host plant families, which contrasts with the specialized diet observed in Helicopis and Sarota.