bluuebunny/crossref_metadata_2025_split huggingface dataset:
A multibeam bathymetric survey of Bay of Islands, Newfoundland: new evidence of late-glacial and Holocene geological processes
Authors: Shaw John , Batterson Martin , Christian Harold , Courtney Robert C. 
Published: September 2014

Multibeam bathymetric imagery of Ray of Islands, Newfoundland, is interpreted within the context of late-glacial and post-glacial processes- West of Humber Arm, the fiord floor is irregular and deep. Humber Arm has steep sidewalls and a flat floor. It contains glaciomarine mud. capped by a layer of red mud probably derived from the Deer Lake Basin, which was connected to the ocean ca. 12.2 ka. In the early postglacial period, sediments on the fiord sidewalls slid into deep water, forming erosional channels. Depositional lobes, stacked in many areas, overlie glaciomarine sediments in deep water. The glaciomarine and submarine slide sediments are overlain by postglacial mud that is imprinted by elongate, ovoid, and circular fluid-escape trenches, and sedimentary furrows. The natural morphology of the fiord has been modified by anthropogenic activity at Comer Brook. Effects include an apron of bark offshore from the paper mill, dredge spoil, and a sunken vessel at the mouth of Humber River. Large submarine slides, probably triggered by wharf construction at Seal Head, formed deep channels on the fiord sidewalls and overlapping depositional lobes on the fiord floor. They are morphologically similar to the lateglacial slide failures in the fund.

RÉSUMÉ
Les images bathymétriques multifaisceaux de Bay of Islands, Terre-Neuve, sont interprétées dans le contexte des processus tardiglaciaires et post-glaciaires. À I'ouest de Humber Arm. Ie fond du l’jord est irrégulier et profond. Humber Arm est doté de parois abruptes et d'un fond plat. Il renferme de la boue glaciomarine recouverte d'une couche de boue rouge provenant probablemenl du bassin du lac Deer, qui était relié à l'océan il y a environ 12.2 millies d'années avant nos jours. Au début de la période post-glaciaire, Ies sediments sur Ies parois du l’jord ont glissé a l’intérieur de I'eau profonde en formant des chenaux d'érosion. Des lobes sédimentaires s'empilant en de nombreux endroits recouvrent les sédiments glaciomarins en eaux profondes. Les sédiments de glissement glaciomarins et sous-marins sont recouverts d'une boue post-glaciaire marquée de tranchées allongées, ovoides et circulaires d'évacuation des liquides et de silions sédimentaires. L'activité anthropique a modi fié la morphologic naturelle du l’jord a Corner Brook. Les effets de cette activité comprennent un tablier d'écorce au large de la papeterie, des matériaux de dragage et un navire ayant coulé à I'embouchure dc la riviére Humber. D'importants éboulements sous-marins, probablement causés par la construction du quai de Seal Head, ont formé des chenaux profonds dans les parois du l’jord et des lobes sédimentaires qui se superposcnt sur Ic fond du l’jord Ceux-ci sont morphologiquemcnt analogues aux fractures de glissement tardiglaciaires dans le l’jord.

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A new species of stalked crinoid (Echinodermata) of possible Late Silurian age from central Newfoundland
Authors: Donovan S. K. , Dickson W. L. , Boyce W. D. , Ash J. S. 
Published: September 2014

A new fossil locality within a sequence previously assigned to the Middle Ordovician Baie D'Espoir Group in south-central Newfoundland contains fragmented crinoid columnals and brachiopods. Distinctive, pentastellate crinoid columnals, similar to those assigned to the monobathrid camerate Hexacrinites Austin and Austin by Russian authors, are named Hexacrinites? Pentastellatus n. sp. Nodal(?) columnals of this species have a circular, depressed articular facet, with a conical to bowl-like crenularium, a depressed, circular areola, a raised perilumen and a short, slender axial canal of pentagonal section. The oldest Hexacrinites sensu stricto are Late Silurian, suggesting that the fossiliferous strata have been incorrectly assigned to the Ordovician. Cross-sections of brachiopods from the same locality include an example that resembles several Early Silurian to Late Devonian pentameroid genera including Brooksina Kirk, 1922. Correlation with Late Silurian, bivalve-bearing strata SO km to the northeast would indicate that a major unconformity may occur above the fossiliferous Early and Middle Ordovician strata and the Early Ordovician ophiolite complexes.

RÉSUMÉ
Un nouvel emplacement de fossiles à I'intérieur d'une sequence auparavant attribute au groupe de l'Ordovicien moyen de Baie d'Espoir dans le centre-sud de Terre-Neuve renferme des fragments de columnales et de brachiopodes de crinoldes. Des columnales de crinoldes pentaétoilées caractéristiqucs, semblables à celles attributées à l’Hexacrinites Austin and Austin à loges monobathrides par des auteurs russes, sont baptisées nouvelle espèce pentastellatus d'Hexacrinites?. Les columnales nodales(?) de cette espèce sont pourvues d'une facette articulaire renfoncée et circulaire munie d'un crenularium allant de conique à bombé, d'une aréole circulaire renfoncie, d'un périlumen surélevé et d'un canal axial mince et court de section pentagonalc. Les plus anciens Hexacrinites, au sens strict, remontent au Silurien supérieur, ce qui permet de supposer qu'on a incorrectement attribué la strate fossilifère à l'Ordovicien. Des iéchantillons représentatifs de brachiopodes du même emplacement comprennent un exemple qui ressemble à plusieurs genres de pentaméroides datant du Silurien inférieur au Dévonien supérieur, notamment le Brooksina Kirk, 1922. Leur corrélation avec des strates renfermant des bivalves du Silurien supérieur à 50 km au nord-cst signale qu'une discordance importantc pourrait se présenter au-dessus des strates fossiliferes de l'Ordovicien inférieur ou moyen de même que des complexes d'ophiolites de l'Ordovicien inférieur.

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The Triassic-Jurassic Fundy Basin, eastern Canada: regional setting, stratigraphy and hydrocarbon potential
Authors: Wade John A. , Brown David E. , Traverse Alfred , Fensome Robert A. 
Published: September 2014

Fundy Basin, one of a series of half graben that formed along the eastern margin of North America during the Triassic/Jurassic rifting of Pangaea, lies mainly to the south of the Cobequid-Chedabucto Fault System in Nova Scotia and' beneath the Bay of Fundy. Continental red clastic rocks and basalt flows of the Triassic and Early Jurassic Newark Supergroup crop out continuously along the Bay of Fundy and Minas Basin coast of Nova Scotia and at several sites in southern New Brunswick. These units thicken beneath the waters of the bay to a present-day maximum of nearly 10 km. Proximal facies preserved along the faulted New Brunswick margin of the basin consist of upper alluvial fan and fluvial elastics which grade laterally into sheet flood deposits. Along the gently north-dipping Nova Scotia margin, facies consist of distal alluvial fan, sheet flood and playa mud flat deposits.

Facies projections suggest the probability that petroleum-generating lacustrine sequences are widespread along the basin axis. In the Wolfvilte Formation and lower part of the Blomidon Formation these may be overmature but the upper part of the Blomidon Formation and the Scots Bay Formation have the potential for appreciable quantities of hydrocarbons.

RÉSUMÉ
Le bassin dc Fundy, Pun des demi-grabens d'unc s£ric qui s'est formee le long de la marge contincntale de l'Amérique du Nord lors de la séparation triasique-jurassique de la Pangée, est principalement situé au sud du système de failles de Cobequid-Chedabucto, en Nouvelle-Écosse, ainsi qu'au-dessous de la baie de Fundy. Des écoulements de basaltes et de roches clastiques rouges continental du supcrgroupe du Trias et du Jurassiquc intérieur de Newark affleurent de fa÷on continue le long de la baie de Fundy et de la côte du bassin de Minas en Nouvelle-Écosse ainsi qu'en plusieurs endroits dans le sud du Nouveau-Brunswick. Ces unités s'épatssissent au-dessous des eaux de la baie jusqu'à un maximum actuel de près de 10 km. Les faciès proximaux conservés le long de la marge faillée néo-brunswickoise du bassin sont constitués de cônes altuviaux supérieurs et de roches déritiques fluviales qui passent latéralementà des gites d'inondation en nappes. Le long de la marge doucement inclinée vers le nord néo-écossatse, les faciès sont constitutés de cônes alluviaux distaux, de gttes d'inondation en nappes et de playas de sltkkes.

Les projections des facies permettent de supposer qu'il est probable que les séquences lacustres sont répanducs le long de l'axe du bassin. Celles-ci pourraient être immatures dans la Formation de Wolfville et la partie inférieure de la Formation de Blomidon, mats la partie supérieure de la Formation de Blomidon et la Formation de Scots Bay offrent un potentiel de quantités appréciables d'hydrocarbures.

[Traduit par la rédaction]
The holotype of Leaia silurica Matthew, 1910, Pennsylvanian, Lancaster Formation, New Brunswick
Authors: Miller Randall F. 
Published: September 2014

The conchostracan Leaia silurica Matthew, 1910 was reviewed by Copeland in 1957 and a hypotype described and deposited in the collections of the Geological Survey of Canada. Matthew's holotype has been recovered during organization of the G.F. Matthew collection at the New Brunswick Museum.

RÉSUMÉ
Le Conchostracé Leaia silurica de Matthew, 1910, a été reéxaminé par Copeland en 1957 et un hypotype a été décrit et déposé dans les collections de la Commission géologique du Canada. L'holotype de Matthew a été récuperé pendant l'organisation de la collection de G. F. Matthew au Musée du Nouveau-Brunswick.

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Thoughts on the evolution of modern oceans
Authors: Gramberg I. S. 
Published: September 2014

Explanation of the evolution of the Earth's oceans, particularly the processes involved in the generation of the oceans, are important for understanding the general appearance of our planet, and for the solution of specific problems. A comparative study of the world's oceans shows there is a single genetic series in the evolution of oceans, and that the oceans of the world are at different stages in their evolution. The Arctic Ocean, dated as Cenozoic, is noted for its small size and shallow oceanic floor, extensive but passive continental margins, limited volcanism, significant crustal thickness, and a lack of Benioff zones. The Mesozoic, Indian and Atlantic oceans have much greater dimensions and depths than the Arctic Ocean, the crust is thinner beneath them, volcanism is much more extensive, and active margins, while in the initial phase of evolution, are limited in extent. The area of the most ancient (probably Paleozoic) Pacific Ocean is equal to the sum of the rest of the three oceans; it also has the greatest oceanic depth. Beneath the Pacific, the crust is thinned and is characterized by high permeability, because of which magmatism is particularly widespread. Active continental margins arc also extensive in the Pacific. The concept of evolutionary development of the oceans enables us to predict the comparative potential of oceans with regards to their oil and gas and ore content.

RÉSUMÉ
Les explications de l'évolution des océans de la terre, particulièrement les processus impliqués dans la formation des océans, sont importants pour compréndre l'aspect général de notre planète et pour la solution de problèmes spécifiques. Une étude comparative des océans du monde montre qu'il y a une suite génétique unique dans l'évolution des océans, et que les océans du monde en sont a différents stades dans leur évolution. l'océan Arctique, datant du cénozoique, est caractérise par sa petite taille et son fond océanique peu profond, des marges continentales étendues mais passives, une petite quantité de volcanisme, une croûte épaisse, et une absence de zones de Benioff. Les océans Indien et Atlantique, mésozoiques, ont des dimensions et des profondeurs beaucoup plus grandes que celles de l'océan Arctique, la croute sous-jacente est plus mince; le volcanisme est beaucoup plus répandu, et les marges actives, dans leur phase initiate d'évolution, sont d'étendue limitée. La surface de l'océan Pacifique, le plus ancien (probablement paléozoique), est égale a la somme des trois autres océans; il a aussi la plus grande profondeur. Sous le Pacifique, la croûte est amincie et caractérisee par une grande perméabilité, en raison de laquelle le magmatisme est particulièrement repandu. Les marges continentales actives sont aussi abondantes dans le Pacifique. Le concept de l'évolution des océans nous permet de prédire le potentiel comparatif des océans en regard de leur contenu en pétrole, gaz naturel et minerai.

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A Lower Palaeozoic 'onychophoran' reinterpreted as a pelmatozoan (stalked echinoderm) column
Authors: Rhebergen Freek , Donovan Stephen K. 
Published: September 2014

Onychophorans are rare fossils, but are currently the subject of renewed research activity. However, not all 'onychophorans' have been correctly identified. The specimen described herein is preserved as a natural mould in an Upper Ordovician cobble from a Quaternary glacial deposit. The 'legs' are actually elongate tubercles, arranged in irregular circlets and showing calcite cleavage; the annulations of the body are irregularly spaced. The specimen is reinterpreted as a pelmatozoan, probably crinoid, pluricolumnal.

RÉSUMÉ
Les onychophores sont des fossiles rares, mais font préscntement L'objet d'une activité de recherche renouvelée. Toutefois, ce ne sont pas tous les «onychophores» qui ont été correctement identifiés. Le spécimen décrit ici est préservé com me un moulage naturcl dans un caillou Ordovicien supérieur provenant d'un dépôt glaciaire quaternaire. Les «pattes» sont en fait des tubercules allongés, disposes en cercles irréguliers et montrant des clivages de calcite; les annulations du corps sont irrégulierement espacées. Le specimen est réinterpreté comme un pelmatozoaire, probablement un crinoide à plusieurs tiges.

[Traduit par la rédaction]
Desire under the Elms in Dublin, The Corn Exchange production, directed by Annie Ryan
Authors: Dubost Thierry 
Published: September 2014

Abstract
In an interview with director Annie Ryan, Thierry Dubost talks about Desire under the Elms, which was staged in Smock Alley Theatre during the 2013 Dublin Theatre Festival. Annie Ryan first retraces how Corn Exchange (her theater company) came to be one of the prominent Irish theater companies. She then alludes to the situation of theater in contemporary Ireland, and provides precious information about the presence of Eugene O'Neill's work in this country, including the public reception of the play. Ryan initially mentions the influence of commedia dell'arte on the aesthetics of Corn Exchange; she then explains why she chose Desire under the Elms and how she approached O'Neill's famous play. Although the financial context forced her to make restrictive choices, her staging proved successful.
Revenants, Resurrection, and Burnt Sacrifice
Authors: Caciola Nancy Mandeville 
Published: September 2014

ABSTRACT
Shortly after the turn of the millennium, Bishop Thietmar of Merseburg incorporated several stories about the undead in his chronicle of the deeds of the Ottonian kings. His accounts feature embodied revenants (not insubstantial specters) at worship. The stories the bishop recounts likely circulated in oral form, as urban legends, for some time before he recorded them in writing. Perhaps because they featured revived bodies, Thietmar presented these stories as evidence for the Christian doctrine of Resurrection. However, the tales do not readily lend themselves to this project, not least because the revenants were presented as frightening, dangerous, and even murderous in nature. This article probes the dissonances of Thietmar's ghost stories, arguing that they represent the hybrid products of a syncretism between Slavic pagan and medieval Christian cultures.
Effect of Debarking Water from Norway Spruce (Picea abies) on the Growth of Five Species ofWood-Decaying Fungi
Authors: Edfeldt Amelie Fagerlund , Hedenström Erik , Edman Mattias , Jonsson Bengt Gunnar 
Published: September 2014

Abstract
Norway spruce (Picea abies) debarking water is an aqueous extract obtained as waste from the debarking of logs at paper mills. The debarking water contains a mixture of natural compounds that can exhibit diverse biological activities, potentially including fungicidal activity on some species of wood-decaying fungi. Thus, we investigated the growth rates of such fungi on agar plates to which debarking water extracts had been added. The experiment included five wood-decaying fungi, viz. Gloeophyllum sepiarium, Oligoporus lateritius, Ischnoderma benzoinum, Junghuhnia luteoalba, and Phlebia sp. Growth reduction was observed for all species at the highest tested concentrations of freeze-dried and ethanol-extracted debarking water, the ethyl acetate-soluble fraction and the diethyl ether-soluble fraction. However, the magnitude of the effect varied between different species and strains of individual species. The brown-rot fungi G. sepiarium and O. lateritius were generally the most sensitive species, with the growth of all tested strains being completely inhibited by the ethyl acetate-soluble fraction. These results indicate that development of antifungal wood-protecting agents from debarking water could potentially be a way to make use of a low-value industrial waste.
Detection of Mild Traumatic Brain Injury in Rodent Models Using Shear Wave Elastography
Authors: Xu Zinnia S. , Yao Anning , Chu Stephanie S. , Paun Marla K. , McClintic Abbi M. , Murphy Sean P. , Mourad Pierre D. 
Published: September 2014

ObjectivesTraumatic brain injury (TBI) can cause adverse physiologic changes in fluid content within the brain, which may lead to changes in tissue elasticity (eg, stiffness). This study evaluated the ability of ultrasonic shear wave elastography to observe these changes in the brain after TBI in vivo.MethodsMice and rats received a mild TBI or sham surgery and were imaged acutely or 24 hours after injury using shear wave elastography, and the hemispheric stiffness values were compared.ResultsStiffness values were consistent across brain hemispheres of sham TBI rodents. By 24 hours after TBI, relative brain tissue stiffness values for mice and rats each decreased ipsilaterally and increased contralaterally, both relative to each other and compared to sham TBI rodents (P < .05). The absolute tissue elasticity value increased for rats (P < .05) but not for mice.ConclusionsDifferences between intrahemispheric stiffness values of rodent brains by 24 hours after mild TBI may reflect the observed edema and hemorrhage ipsilateral to TBI and the known reduction of cerebral blood flow in both brain hemispheres. If these hypotheses hold true, ultrasonic shear wave elastography may offer a method for detecting adverse changes in fluid content within the brain after mild TBI.
Anorthite sputtering by H+ and Arq+ (q = 1–9) at solar wind velocities
Authors: Hijazi H. , Bannister M. E. , Meyer H. M. , Rouleau C. M. , Barghouty A. F. , Rickman D. L. , Meyer F. W. 
Published: September 2014

AbstractWe report sputtering measurements of anorthite‐like material, taken to be representative of soils found in the lunar highlands, impacted by singly and multicharged ions representative of the solar wind. The ions investigated include protons, as well as singly and multicharged Ar ions (as proxies for the nonreactive heavy solar wind constituents), in the charge state range +1 to +9, at fixed solar wind‐relevant impact velocities of 165 and 310 km/s (0.25 keV/amu and 0.5 keV/amu). A quartz microbalance approach (QCM) for determination of total sputtering yields was used. The goal of the measurements was to determine the sputtering contribution of the heavy, multicharged minority solar wind constituents in comparison to that due to the dominant H+ fraction. The QCM results show a yield increase of a factor of about 80 for Ar+ versus H+ sputtering and an enhancement by a factor of 1.67 between Ar9+ and Ar+, which is a clear indication of a potential sputtering effect.
Effect of scutellarin on the metabolism and pharmacokinetics of clopidogrel in rats
Authors: Chen Xinmeng , Jin Jing , Chen Yaobin , Peng Lingling , Zhong Guoping , Li Jiali , Bi Huichang , Cai Yefeng , Huang Min 
Published: September 2014

AbstractErigeron breviscapus (Vant.) Hand‐Mazz, a traditional Chinese medicine, is often co‐prescribed with clopidogrel for the treatment of ischemic vascular diseases. Scutellarin is the representative bioactive flavonoid isolated from this herb. The aim of this study was to explore the effect of scutellarin on the metabolism and pharmacokinetics of clopidogrel. The in vitro studies using rat liver microsomes showed that scutellarin significantly inhibited the metabolism of clopidogrel. The IC50 value was 2.1 µm. Ten male rats were employed to investigate the effect of scutellarin on the pharmacokinetics of clopidogrel in vivo. After pretreatment with scutellarin, there were significant increases in the AUC0–∞ (from 0.9 ± 0.4 to 1.7 ± 0.6 ng/ml h; p <0.05) and Cmax (from 0.4 ± 0.1 to 0.9 ± 0.1 ng/ml; p <0.05) of clopidogrel. The pharmacokinetic data for clopidogrel active metabolite showed significant decreases in AUC0–∞ (18.2 ± 5.6 to 11.4 ± 3.7 ng/ml h; p <0.05) and Cmax (from 8.2 ± 1.2 to 4.3 ± 0.3 ng/ml; p <0.05) after pretreatment with scutellarin. Collectively, the metabolism and pharmacokinetics of clopidogrel were significantly affected by scutellarin. This study indicated that potential herb–drug interaction between scutellarin and clopidogrel should be taken into consideration in clinical use. Copyright © 2014 John Wiley & Sons, Ltd.
Three‐year clinical outcome after infrapopliteal angioplasty for critical limb ischemia in hemodialysis patients with minor or major tissue loss
Authors: Nakano Masatsugu , Hirano Keisuke , Yamauchi Yasutaka , Iida Osamu , Soga Yoshimitsu , Kawasaki Daizo , Yamaoka Terutosh , Suematsu Nobuhiro , Suzuki Kenji 
Published: September 2014

Objectives and BackgroundAmong hemodialysis (HD)‐dependent patients with critical limb ischemia (CLI), Endovascular therapy (EVT) of isolated infrapopliteal lesions improves limb salvage. Accordingly, we sought to determine the outcomes of this group of patients based on the extent of tissue loss at baseline.MethodsFrom 2004 to 2011, 449 consecutive HD patients with CLI had ischemic wounds and underwent EVT for isolated infrapopliteal lesions. The “minor tissue loss” (MI) group was confirmed by 340 HD patients with wounds located distal to the metatarsophalangeal joints, and the “major tissue loss” (MA) group included 109 HD patients with wounds that extended beyond this point. The two groups were compared for limb salvage and amputation free survival (AFS) rates by Kaplan‐Meier analysis.ResultsThere was no significant difference in the percentage of diabetic patients (MI: 76.5 vs. MA: 75.2%). The percentage with direct flow to the wound site was lower in the MA group than in the MI group (MI: 63.5 vs. MA: 45.9%, P < 0.01). After EVT the MI group had a significantly better limb salvage rate (MI: 83.7 vs. MA: 71.2% at 3 years, P < 0.01), and AFS rate (MI: 44.1 vs. MA: 29.1% at 3 years, P < 0.01) compared to the MA group.ConclusionsEVT is an efficient treatment for HD patients with minor tissue loss, achieving >80% limb salvage rates at 3 years. However, AFS rates in all HD patients with tissue loss are <50% at 3 years, making their prognosis poor. © 2015 Wiley Periodicals, Inc.
ChemInform Abstract: Anomalous Band Gap Behavior in Mixed Sn and Pb Perovskites Enables Broadening of Absorption Spectrum in Solar Cells.
Authors: Hao Feng , Stoumpos Constantinos C. , Chang Robert P. H. , Kanatzidis Mercouri G. 
Published: September 2014

AbstractMeNH3Sn1‐xPbxI3 perovskite solid solutions are prepared by mixing stoichiometric amounts of MeNH3I and MX2 (M: Sn, Pb) in aqueous HI/H3PO2 (4:1) at 100 °C.