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Journal articles on the topic 'Le Nain'

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Published: 4 June 2021

Last updated: 5 February 2022

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1

de Lovinfosse, Marie. "Naïn ou Naïm (Lc 7.11) : une différence révélatrice." New Testament Studies 64, no. 1 (2017): 20–32. http://dx.doi.org/10.1017/s0028688517000224.

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This study investigates spelling variants of the name of the city where Jesus raises the only son of a widow, in Lk 7.11: Nain or Naim. The study develops along three lines: textual critic, Hebraic etymology, ancient geography. The investigation eventually raises the question of the theological significance of the miracle of Nain.

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2

Dronskowski, Richard. "In2.24(NCN)3 and NaIn(NCN)2: Synthesis and Crystal Structures of New Main Group Metal Cyanamides." Zeitschrift für Naturforschung B 50, no. 8 (1995): 1245–51. http://dx.doi.org/10.1515/znb-1995-0819.

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Single crystals of In2.24(NCN)3 and NaIn(N CN)2 can be synthesized from a reaction between InBr and NaCN at 400 °C, followed by chemical transport at 400-500 °C. The X-ray crystal structure determinations of In2.24(NCN)3 (rhombohedral R3̄c, a = 606.09(4), c = 2884.4(2) pm, Z = 6) and NaIn(NCN)2 (orthorhombic Cmcm, a = 961.30(6), b = 716.84(5), c = 603.65(4) pm, Z = 4) reveal ionic layer structures built from sheets of cationic and anionic (cyanamide) motifs. While NaIn(NCN)2 contains In3+ and Na+ ions, In2.24(NCN)3 is a mixedvalence compound, incorporating a monovalent In+ ion besides trivalen

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3

Connelly, J. N., and B. Ryan. "Late Archean evolution of the Nain Province, Nain, Labrador: imprint of a collision." Canadian Journal of Earth Sciences 33, no. 9 (1996): 1325–42. http://dx.doi.org/10.1139/e96-100.

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Archean gneisses of the Nain Province in the Nain area, Labrador, comprise narrow septa between intrusions of the Mesoproterozoic Nain Plutonic Suite. This region occupies a critical position between the northern (Saglek) and southern (Hopedale) blocks of the Nain Province, which experienced distinct thermotectonic histories until the late Archean. Field and geochronological evidence are indicative of a strong late Archean thermotectonic overprint that is absent from most of the remainder of the Nain Province. Archean gneisses were intruded by granites and mafic dykes at 2578 ± 3 and [Formula:

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4

Bertrand, Anne. "frères Le Nain." Vacarme 26, no. 1 (2004): 48. http://dx.doi.org/10.3917/vaca.026.0048.

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5

Schaduw, Joshian Nicolas William. "Struktur Komunitas Dan Keberlanjutan Pengelolaan Ekosistem Mangrove Pulau-Pulau Kecil (Kasus Pada Pulau Nain Kabupaten Minahasa Utara Provinsi Sulawesi Utara)." Jurnal Ilmu Lingkungan 16, no. 2 (2018): 120. http://dx.doi.org/10.14710/jil.16.2.120-129.

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ABSTRAKKajian ini bertujuan untuk menganalisa struktur komunitas dan keberlanjutan pengelolaan ekosistem mangrove di Pulau Nain Kecamatan Wori, Kabupaten Minahasa Utara, Provinsi Sulawesi Utara. Pulau Nain adalah salah satu pulau yang masuk dalam kawasan konservasi Taman Nasional Bunaken dan memiliki kawasan budidaya rumput laut yang masih produktif. Penelitian ini menggunakan data sekunder dan primer. Data yang dibutuhkan dalam kajian ini meliputi data dimensi ekologi, sosial ekonomi, dan kelembagaan. Analisis yang digunakan dalam kajian ini adalah RAPMECS (Rapid Appraisal for Mangroves Ecosy

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6

Thaning, Kaj. "Enkens søn fra Nain." Grundtvig-Studier 41, no. 1 (1989): 32–45. http://dx.doi.org/10.7146/grs.v41i1.16017.

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The Son of the Widow from Nain.By Kaj ThaningThis article intends to elucidate the distinctions that Grundtvig made in his world of ideas in the course of the years from 1824 to 1834, first between spirit and letter, church and church-school (1826-1830), and then between natural life and Christian life (in 1832). In His "Literary Testament" (1827), Grundtvig himself admits that there was a "Chaos" in his writings, due to the youthful fervour that pervaded his literary works and his sermons in the years 1822-1824. But not until 1832 does he acknowledge that "when I speak or write as a citizen,

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7

Canning, Patricia M. "The Nain Daycare Project." Canadian Journal of Education / Revue canadienne de l'éducation 11, no. 1 (1986): 1. http://dx.doi.org/10.2307/1494611.

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8

Hordijk, Arie, and Ger Koole. "The µc-rule is not optimal in the second node of the tandem queue: a counterexample." Advances in Applied Probability 24, no. 01 (1992): 234–37. http://dx.doi.org/10.1017/s0001867800024290.

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In this note we give a counterexample which shows that the µc-rule is not optimal in the second node of the tandem queue. This counterexample contradicts the interchange argument in Nain [1] and Nain et al. [2].

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9

Hordijk, Arie, and Ger Koole. "The µc-rule is not optimal in the second node of the tandem queue: a counterexample." Advances in Applied Probability 24, no. 1 (1992): 234–37. http://dx.doi.org/10.2307/1427742.

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In this note we give a counterexample which shows that the µc-rule is not optimal in the second node of the tandem queue. This counterexample contradicts the interchange argument in Nain [1] and Nain et al. [2].

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10

Wardle, Richard J., Donald T. James, David J. Scott, and Jeremy Hall. "The southeastern Churchill Province: synthesis of a Paleoproterozoic transpressional orogen." Canadian Journal of Earth Sciences 39, no. 5 (2002): 639–63. http://dx.doi.org/10.1139/e02-004.

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The Paleoproterozoic southeastern Churchill Province (SECP) is located in the northeastern Canadian Shield of Labrador and Quebec. The SECP formed through the oblique collisions of the Archean Nain and Superior cratons with a third intervening Archean block, the core zone. The belt has a tripartite structure, comprising the Torngat Orogen (TO) formed by Nain craton core zone collision in the east, the core zone in the centre, and the New Quebec Orogen (NQO) formed by Superior craton core zone collision in the west. The SECP thus records transpressional development on the flanks of the Supe

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11

Scott, David J. "U–Pb geochronology of a Paleoproterozoic continental magmatic arc on the western margin of the Archean Nain craton, northern Labrador, Canada." Canadian Journal of Earth Sciences 32, no. 11 (1995): 1870–82. http://dx.doi.org/10.1139/e95-144.

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The Paleoproterozoic Torngat Orogen, in northernmost Labrador and northeastern Quebec, records the collision between the western margin of the Nain Province and the eastern margin of the Rae Province. Six samples from a suite of calc-alkaline plutonic rocks that intrude the Nain craton have been dated using the U–Pb method at 1895 ± 2, 1888 ± 2, [Formula: see text], 1885 ± 2 (two samples), and >1859 Ma, and support the interpretation that east-dipping subduction occurred below the Nain craton during this interval. A granitic dyke that truncates the sinistral shear fabric in the Abloviak she

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12

Martínez Andrade, Luis. "Le nain et la nature." Ecologie & politique N° 42, no. 2 (2011): 105. http://dx.doi.org/10.3917/ecopo.042.0105.

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13

Stoessel, Marleen. "Petit Bossu et Nain caché." Les Temps Modernes 641, no. 7 (2006): 105. http://dx.doi.org/10.3917/ltm.641.0105.

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14

Trevathan, W., J. Vanderkolk, and T. Miller. "National antimicrobial information network (NAIN)." American Journal of Infection Control 27, no. 2 (1999): 189. http://dx.doi.org/10.1016/s0196-6553(99)80038-8.

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15

Connelly, James N., and A. Bruce Ryan. "Age and tectonic implications of Paleoproterozoic granitoid intrusions within the Nain Province near Nain, Labrador." Canadian Journal of Earth Sciences 36, no. 5 (1999): 833–53. http://dx.doi.org/10.1139/e99-002.

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U-Pb (zircon) age determinations from three granitoid intrusions in the Nain region, formerly assigned to the well-known 1.35-1.29 Ga (Mesoproterozoic) Nain Plutonic Suite (NPS), indicate that they were emplaced, instead, during the Paleoproterozoic. Crystallization ages of 2109 ± 3 Ma for Sheet Hill granite, 2052 ± 4 Ma for Loon Island granite, and 2025 ± 7 Ma for Satok Island monzonite demonstrate a decreasing time of emplacement from north to south. Leucocratic basic rocks, superficially similar to those of the NPS, occur as inclusions within the Satok Island monzonite and are intruded by a

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16

Mizoguchi, Yoko, Kazuhiro Nakamura, Shuhei Karakawa, et al. "Clinical Characteristics in Neonates with Alloimmune Neutropenia: Significance of the Detection of Antineutrophil Antibodies." Blood 112, no. 11 (2008): 4647. http://dx.doi.org/10.1182/blood.v112.11.4647.4647.

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Abstract Neonate alloimmune neutropenia (NAIN) is caused by the transplacental transfer of maternal alloantibodies directed against antigens on the infant’s neutrophils. To date, there are scant studies about its clinical characteristics and characterization of antineutrophil antibodies though some case reports are found. In this study we analyzed 11 cases with NAIN from January 2005 to December 2007. The diagnosis of NAIN was confirmed by the transient neutropenia less than 500/μl of absolute neutrophil count (ANC), the detection of maternal antineutrophil antibody, the incompatibility of neu

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17

Li, Zhaosheng, Jinhua Ye, and Zhigang Zou. "Photocatalytic properties of MIn(WO4)2 (M = Li, Na, and K)." Journal of Materials Research 22, no. 4 (2007): 958–64. http://dx.doi.org/10.1557/jmr.2007.0111.

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MIn(WO4)2 (M = Li, Na, and K) with InO6 and WO6 octahedra were synthesized via a conventional solid-state reaction method. The photophysical and photocatalytic properties were studied. Compared with WO3, which is unable to evolve H2 from an aqueous CH3OH solution under illumination, the three materials can evolve H2 and O2 from aqueous solutions with CH3OH and AgNO3 sacrificial reagents, respectively. The activity order of photocatalytic H2 evolution is NaIn(WO4)2 > LiIn(WO4)2 > KIn(WO4)2 under irradiation (λ > 200 nm). Under irradiation (λ > 300 nm), however, LiIn(WO4)2 has a high

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18

Wiltgren, Filip. "When Nain came to Shirin’s door." Nature 557, no. 7705 (2018): 462. http://dx.doi.org/10.1038/d41586-018-05157-2.

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19

Boman, Lars. "Att skilja på bröderna Le Nain." Konsthistorisk Tidskrift/Journal of Art History 56, no. 4 (1987): 140–44. http://dx.doi.org/10.1080/00233608708604158.

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20

Bravo, Carlo Del. "I Le Nain e Pierre Charron." Artibus et Historiae 10, no. 20 (1989): 93. http://dx.doi.org/10.2307/1483355.

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21

Grønnow, Bjarne. "Archaeology of the Nain Region, Labrador." Boreas 38, no. 1 (2009): 187–88. http://dx.doi.org/10.1111/j.1502-3885.2008.00078.x.

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22

Arneth, Borros. "Neonatal Immune Incompatibilities between Newborn and Mother." Journal of Clinical Medicine 9, no. 5 (2020): 1470. http://dx.doi.org/10.3390/jcm9051470.

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Background: Incompatibilities between the mother and unborn baby can cause complications that must be identified early to initiate the appropriate treatment. For example, neonatal alloimmune thrombocytopenia (NAIT), neonatal alloimmune neutropenia (NAIN), and morbus hemolyticus neonatorum affect children worldwide. Aim: This literature review aims to depict the similarities and differences between these three disorders from a clinical and mechanistic point of view. Material and Methods: The current literature review entailed conducting a systematic search to locate articles on the three condit

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23

Kranendonk, M. J. Van, and R. J. Wardle. "Crustal-scale flexural slip folding during late tectonic amplification of an orogenic boundary perturbation in the Paleoproterozoic Torngat Orogen, northeastern Canada." Canadian Journal of Earth Sciences 34, no. 12 (1997): 1545–65. http://dx.doi.org/10.1139/e17-126.

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Large variations in metamorphic grade over short distances, disparate orientations and diverse kinematics of contemporaneous structures, and a previously unexplained, 90° counterclockwise bend in the orogenic boundary of the amphibolite- to granulite-facies northern segment of the Paleoproterozoic Torngat Orogen are shown to be the result of multiple tectonic events acting upon an orogenic boundary perturbation. The perturbation was initiated when a promontory on the Nain Province margin, composed of a 1910–1885 Ma continental magmatic arc (Burwell domain), indented the Rae Province hinterland

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24

Yu, Yang, and S. A. Morse. "40Ar/39Ar chronology of the Nain anorthosites, Canada." Canadian Journal of Earth Sciences 30, no. 6 (1993): 1166–78. http://dx.doi.org/10.1139/e93-099.

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A hornblende 40Ar/39Ar age of 1328 ± 8 Ma has been obtained from the contact aureole of the Bird Lake Massif, confirming it as one of the oldest members of the Nain plutonic suite. This age constrains the timing of the early stage magma activity of the Nain plutonic suite.Plagioclase samples from the intrusions yield either U-shaped, or staircase-shaped 40Ar/39Ar age spectra, and most of them have two isochrons of similar age but greatly different initial argon composition. Most plagioclase closure ages are >95% of either the hornblende age from a contact aureole or coexisting biotite ages,

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25

Feininger, Tomas, and Ingo Ermanovics. "Geophysical interpretation of the Torngat orogen along the North River – Nutak transect, Labrador." Canadian Journal of Earth Sciences 31, no. 4 (1994): 722–27. http://dx.doi.org/10.1139/e94-064.

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A 19.3 mGal (1 Gal = 1 cm/s2) positive Bouguer gravity anomaly and a broad aeromagnetic low coincide with the Tasiuyak domain of the early paleo-Proterozoic Torngat orogen. The domain evolved during the collision of the western margin of the Archean Nain Province with an inferred, eastward-facing, platform-to-rise, sedimentary wedge sited on a proto-continent of Churchill (Rae) Province.A density contrast of +0.065 g∙cm−3 was measured between rocks of the Tasiuyak domain and those of the flanking Lac Lomier complex of the orogen and Nain Province. Using this contrast, a two and one-half dimens

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26

Reid, Ian. "Crustal structure across the Nain – Makkovik boundary on the continental shelf off Labrador from seismic refraction data." Canadian Journal of Earth Sciences 33, no. 3 (1996): 460–71. http://dx.doi.org/10.1139/e96-036.

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A detailed seismic refraction profile was shot along the continental shelf off Labrador, across the boundary between the Archean Nain Province to the north and the Proterozoic Makkovik orogenic zone to the south. A large air-gun source was used, with five ocean-bottom seismometers as receivers. The data were analysed by forward modelling of traveltimes and amplitudes and provided a well-determined seismic velocity structure of the crust along the profile. Within the Nain province, thin postrift sediments are underlain by crust with a P-wave velocity of 6.1 km/s, which increases with depth and

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27

Cote, D., JB Dempson, M. Piersiak, et al. "Using movement, diet, and genetic analyses to understand Arctic charr responses to ecosystem change." Marine Ecology Progress Series 673 (September 2, 2021): 135–49. http://dx.doi.org/10.3354/meps13775.

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Arctic charr Salvelinus alpinus are a commercially and culturally valued species for northern Indigenous peoples. Climate shifts could have important implications for charr and those that rely on them, but studies that evaluate responses to ecosystem change and the spatial scales at which they occur are rare. We compare marine-phase habitat use, long-term diet patterns, and trends in effective population size of Arctic charr from 2 areas (Nain and Saglek) of Nunatsiavut, Labrador, Canada. Tagged charr in both areas frequently occupied estuaries but some also used other habitats that extended t

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28

Royse, K. R., and R. G. Park. "Emplacement of the Nain anorthosite: diapiric versus conduit ascent." Canadian Journal of Earth Sciences 37, no. 8 (2000): 1195–207. http://dx.doi.org/10.1139/e00-025.

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Estimation of settling velocities of large orthopyroxene megacrysts, found within anorthosite intrusions, are calculated and compared with ascent rates achieved by diapirism and conduit propagation. Calculations suggest that diapirism is far too slow to be an appropriate ascent mechanism for anorthositic crystal mush and favour conduit emplacement. The intrusions of the Nain Plutonic Suite (NPS) are located along the Abloviak shear zone, which marks the boundary between the Nain and Churchill provinces, and within the zone of juxtaposition of the Saglek and Hopedale blocks of the Nain Province

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29

Wiebe, R. A. "Proterozoic basalt dikes in the Nain anorthosite complex, Labrador." Canadian Journal of Earth Sciences 22, no. 8 (1985): 1149–57. http://dx.doi.org/10.1139/e85-117.

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Two sets of Proterozoic (between 1290 and 1042 Ma) alkali to transitional basaltic dikes occur sparsely in an area of at least 5000 km2 within the Nain anorthosite complex. Both are compositionally similar in terms of major elements, but the set that trends roughly north–south (HP dikes) contains much higher concentrations of incompatible elements than the more abundant dikes that trend roughly east-northeast–west-southwest (LP dikes). Both types have low normative clinopyroxene relative to olivine—a characteristic shared with widespread troctolitic rocks in the Nain complex. Low Mg numbers an

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30

Harvey Lemelin, Raynald, Jackie Dawson, Margaret E. Johnston, Emma J. Stewart, and Charlie Mattina. "Résilience, appartenance et tourisme à Nain, Nunatsiavut." Études/Inuit/Studies 36, no. 2 (2013): 35–58. http://dx.doi.org/10.7202/1015977ar.

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Dans le cadre de notre projet de recherche sur la vulnérabilité et la résilience du tourisme dans l’Arctique, nous avons évalué les interactions entre le changement climatique et le tourisme dans les communautés de l’Arctique canadien. Dans cet article, nous nous intéressons à la capacité d’adaptation en présentant les résultats d’entrevues menées à Nain au Nunatsiavut, dans la province de Terre-Neuve-et-Labrador. Alors que de nombreux résidents ont manifesté leur enthousiasme à propos de la nouvelle désignation de leur communauté en tant que point d’entrée du parc national du Canada des Monts

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31

RIDLEY, R. T. "On Knowing Sébastien le Nain de Tillemont." Ancient Society 23 (January 1, 1992): 233–95. http://dx.doi.org/10.2143/as.23.0.2005881.

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32

Joannin, Pascale. "L'Europe en 2025 : géant économique, nain politique ?" Géoéconomie 50, no. 3 (2009): 79. http://dx.doi.org/10.3917/geoec.050.0079.

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33

Gadbois, Jocelyn. "La mort du maudit nain de jardin." Ethnologie française 40, no. 3 (2010): 509. http://dx.doi.org/10.3917/ethn.103.0509.

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34

Knapp, Bettina L., Cho Sehui, Ch'oe Yun, and Patrick Maurus. "La petite balle lancée par un nain." World Literature Today 66, no. 3 (1992): 583. http://dx.doi.org/10.2307/40148581.

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35

Roux, Ph. "Extraction des incisives chez un lapin nain." Schweizer Archiv für Tierheilkunde 147, no. 7 (2005): 311–13. http://dx.doi.org/10.1024/0036-7281.147.7.311.

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36

El-Esawi, Mohamed, Abdullah Al-Ghamdi, Hayssam Ali, Aisha Alayafi, Jacques Witczak, and Margaret Ahmad. "Analysis of Genetic Variation and Enhancement of Salt Tolerance in French Pea (Pisum Sativum L.)." International Journal of Molecular Sciences 19, no. 8 (2018): 2433. http://dx.doi.org/10.3390/ijms19082433.

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Pisum sativum L. (field pea) is a crop of a high nutritional value and seed oil content. The characterization of pea germplasm is important to improve yield and quality. This study aimed at using fatty acid profiling and amplified fragment length polymorphism (AFLP) markers to evaluate the variation and relationships of 25 accessions of French pea. It also aimed to conduct a marker-trait associations analysis using the crude oil content as the target trait for this analysis, and to investigate whether 5-aminolevulinic acid (ALA) could enhance salt tolerance in the pea germplasm. The percentage

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37

Fortunato, Alessandro Antonio, Fabrício Ávila Rodrigues, and Kelly Juliane Teles do Nascimento. "Physiological and Biochemical Aspects of the Resistance of Banana Plants to Fusarium Wilt Potentiated by Silicon." Phytopathology® 102, no. 10 (2012): 957–66. http://dx.doi.org/10.1094/phyto-02-12-0037-r.

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Silicon amendments to soil have resulted in a decrease of diseases caused by several soilborne pathogens affecting a wide number of crops. This study evaluated the physiological and biochemical mechanisms that may have increased resistance of banana to Fusarium wilt, caused by Fusarium oxysporum f. sp. cubense, after treatment with silicon (Si) amendment. Plants from the Grand Nain (resistant to F. oxysporum f. sp. cubense) and “Maçã” (susceptible to F. oxysporum f. sp. cubense) were grown in plastic pots amended with Si at 0 or 0.39 g/kg of soil (–Si or +Si, respectively) and inoculated with

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38

Morrelli, Keri L., Betty M. Hess-Pierce, and Adel A. Kader. "Genotypic Variation in Chilling Sensitivity of Mature-green Bananas and Plantains." HortTechnology 13, no. 2 (2003): 328–32. http://dx.doi.org/10.21273/horttech.13.2.0328.

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The variation in chilling sensitivity of mature-green specialty bananas (Musa paradisiaca var. sapientum) and plantains (Musa paradisiaca var. paradisiaca) was examined using four cultivars of bananas and one plantain cultivar stored under various time and temperature combinations. Cold storage for 1 day at 5.0, 7.2, or 10.0 °C (41, 45, or 50 °F) resulted in acceptable fruit quality for up to 8 days at 20.0 °C (68 °F) for `Petite' and `Red Macabu' bananas and `Dominico Harton' plantains. `Grand Nain' and `Yangambi' bananas were considered unmarketable due to moderate to severe graying after 8

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39

Chappey, Jean-Luc. "Le nain, le médecin et le divin marquis." Annales historiques de la Révolution française, no. 374 (December 1, 2013): 53–83. http://dx.doi.org/10.4000/ahrf.12961.

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40

Kokh, A. E., N. G. Kononova, T. B. Bekker, et al. "Growth and Luminescence Properties of NaIn(WO4)2Crystal." Crystal Growth & Design 7, no. 6 (2007): 1042–43. http://dx.doi.org/10.1021/cg060502+.

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41

Carabaño Aguado, I. "Visita a la abuela: Louis Le Nain, 1640." Pediatría Atención Primaria 15, no. 60 (2013): 397–98. http://dx.doi.org/10.4321/s1139-76322013000500023.

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42

Nasekhan, Shahriar, Mehdi Soltani, and Mahmoud Setayesh Mehr. "Analysis and Typology of Fortresses Bafran City (Nain)." Parseh Journal of Archaeological Studies 2, no. 3 (2018): 101–12. http://dx.doi.org/10.30699/pjas.2.3.101.

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43

Sherafat, Shahzad, Zahra Torkzadeh, and Mohammad Ali Mackizadeh. "Sepiolite occurrence in ultramafics of the North Nain." Iranian Journal of Crystallography and Mineralogy 26, no. 1 (2018): 219–28. http://dx.doi.org/10.29252/ijcm.26.1.219.

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44

Hall, Jeremy, Richard J. Wardle, Charles F. Gower, et al. "Proterozoic orogens of the northeastern Canadian Shield: new information from the Lithoprobe ECSOOT crustal reflection seismic survey." Canadian Journal of Earth Sciences 32, no. 8 (1995): 1119–31. http://dx.doi.org/10.1139/e95-093.

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As part of the Eastern Canadian Shield Onshore–Offshore Transect (ECSOOT), Lithoprobe acquired 1250 km of deep seismic reflection data along the coast of Labrador and across Ungava Bay, to image evidence of Proterozoic crustal accretion to the Archean nuclei of the Nain and Superior provinces of the Canadian Shield. The relatively pristine Archean crust of the Nain Province has low reflectivity and generally lacks systematic reflector orientations. Reworking of Archean crust on the margins of the Makkovik Province has little effect on this weak signature. In contrast, the Archean crust in the

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45

Sachs, Ulrich J. H., Triantafyllos Chavakis, Lin Fung, et al. "Human alloantibody anti-Mart interferes with Mac-1–dependent leukocyte adhesion." Blood 104, no. 3 (2004): 727–34. http://dx.doi.org/10.1182/blood-2003-11-3809.

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AbstractThe CD11b/CD18 integrin plays a crucial role in cell-cell adhesion processes. Recently, we described a case of severe neonatal alloimmune neutropenia (NAIN) caused by an alloantibody against a variant of the CD11b subunit (Mart alloantigen). Allele-specific transfected cells allowed us to demonstrate that an H61R point mutation is directly responsible for the formation of Mart epitopes. No difference in the adhesion capability between H61 and R61 homozygous neutrophils was observed. Functional analysis showed that anti-Mart inhibited Mac-1–dependent adhesion of neutrophils and monocyti

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46

Nono, Davidson R., Farnis B. Boneka, and Grevo S. Gerung. "SIPUT GASTROPODA PADA ALGA MAKRO DI TANJUNG ARAKAN DAN PULAU NAIN, SULAWESI UTARA." JURNAL PERIKANAN DAN KELAUTAN TROPIS 9, no. 2 (2013): 45. http://dx.doi.org/10.35800/jpkt.9.2.2013.4173.

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Pengambilan sampel dilakukan di Taman Nasional Bunaken yakni Pantai Pulau Nain dan Tanjung Arakan pada bulan Februari 2012. Penelitian dimulai dengan menyusuri pantai pada pagi hingga siang hari saat air sedang surut dengan menggunakan alat snorkeling. Penelitian ini berhasil menemukan 15 jenis siput dari 9 famili dan 5 jenis alga makro dari 3 famili. Komunitas siput gastropoda di kedua stasiun penelitian memiliki nilai indeks kesamaan sebesar 63%. Sedangkan komunitas alga makro memiliki nilai indeks kesamaan sebesar 75%. Hal tersebut menyatakan bahwa siput gastropoda dan alga makro di kedua s

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47

Funck, Thomas, Annette K. Hansen, Ian D. Reid, and Keith E. Louden. "The crustal structure of the southern Nain and Makkovik provinces of Labrador derived from refraction seismic data." Canadian Journal of Earth Sciences 45, no. 4 (2008): 465–81. http://dx.doi.org/10.1139/e08-007.

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Data from a refraction seismic profile parallel to the coast of Labrador (Canada) were used to determine the crustal structure across the boundary of the Nain and Makkovik provinces, and to look for evidence for an offshore continuation of the Mesoproterozoic Nain Plutonic Suite (NPS). Seven seismometers recorded airgun shots along the 283 km long line. P- and S-wave velocity models were developed from forward and inverse modeling of travel times. The velocity model distinguishes three distinct zones. In the Saglek block of the Nain Province, the crust is divided into three layers with P-wave

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48

Fromont, P., A. Bettaieb, H. Skouri, et al. "Frequency of the polymorphonuclear neutrophil Fc gamma receptor III deficiency in the French population and its involvement in the development of neonatal alloimmune neutropenia." Blood 79, no. 8 (1992): 2131–34. http://dx.doi.org/10.1182/blood.v79.8.2131.2131.

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Abstract We report the case of a healthy woman (K.M.) who, after multiple pregnancies, developed an antibody directed against a nonpolymorphic region of the polymorphonuclear neutrophil (PMN) Fc gamma receptor III (FcRIII-CD16), which caused transient neonatal alloimmune neutropenia (NAIN). The antigenic target of the antibody was determined by an immunoprecipitation procedure and by phenotyping the mother's PMN. These latter did not react with monoclonal CD16 or polyclonal and monoclonal NA1 and NA2 antibodies, demonstrating the absence of PMN- FcRIII and, consequently, the NA-null phenotype.

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49

Fromont, P., A. Bettaieb, H. Skouri, et al. "Frequency of the polymorphonuclear neutrophil Fc gamma receptor III deficiency in the French population and its involvement in the development of neonatal alloimmune neutropenia." Blood 79, no. 8 (1992): 2131–34. http://dx.doi.org/10.1182/blood.v79.8.2131.bloodjournal7982131.

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We report the case of a healthy woman (K.M.) who, after multiple pregnancies, developed an antibody directed against a nonpolymorphic region of the polymorphonuclear neutrophil (PMN) Fc gamma receptor III (FcRIII-CD16), which caused transient neonatal alloimmune neutropenia (NAIN). The antigenic target of the antibody was determined by an immunoprecipitation procedure and by phenotyping the mother's PMN. These latter did not react with monoclonal CD16 or polyclonal and monoclonal NA1 and NA2 antibodies, demonstrating the absence of PMN- FcRIII and, consequently, the NA-null phenotype. We also

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50

Royse, K. R., S. R. Noble, J. Tarney, and A. C. Cadman. "Country-rock contamination of marginal mafic granulites bordering the Nain Plutonic Suite: implications for mobilization of Sr during high-grade contact metamorphism." Canadian Journal of Earth Sciences 36, no. 6 (1999): 985–97. http://dx.doi.org/10.1139/e99-021.

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The marginal mafic granulites that locally border the Nain Plutonic Suite (NPS) have a range of initial Nd-isotope ratios that overlap with that of the NPS anorthosites and associated Nain dykes. The similarity in Nd-isotope data suggests that gneissic Archaean country rocks have contaminated all the anorthosites, marginal mafic granulites, and dykes. Sr-isotope data for the mafic granulites and dykes support a country rock contamination scenario but preclude wholesale assimilation of rocks such as the host Archaean tonalite gneisses as the sole contaminant. Initial epsilonSr values of +10 to

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