145,000 research outputs found
Rhinobatos Linck 1790
No full textGenus “ Rhinobatos ” Linck, 1790 Type species Raja rhinobatos Linneaus, 1758, Recent.Published as part of Ebersole, Jun A., Cicimurri, David J. & Stringer, Gary L., 2019, Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths, pp. 1-274 in European Journal of Taxonomy 585 on page 106, DOI: 10.5852/ejt.2019.585, http://zenodo.org/record/366025
Dissertationum academicarum qvinta; exempla qvaedam epistolarum celebriora adducens. Qvam consensu ampliss:ae facult. phil. in Reg. Acad. Aboënsi, moderatore ... Daniele Achrelio, eloqv. prof. ord. Defendet Thomas Martini Anung, Aboënsis. In audit: max: ad diem 24. April. 1689.
No full textInvokaatio: I.N.J.Dedikaatio: Barthollus Festing, Nicolaus S. Kåck, Laurentius A. Krokius, Matthias Linck, Martinus Anung.Gratulaatio: Simon Tålpo, D. Achrelius, Gregorius Cl. Palicander, Matthias M. Anung, Jacob. J. Halitius, Johannes Laurenius.Painovuosi nimekkeestä.Arkit: 2 arkintunnuksetonta lehteä, F8, 2 arkintunnuksetonta lehteä
Effects of the Interaction of Varying Temperatures and Light Intensities on the Response of Flax to 2, 4-D
No full textJordan, L. S.; Dunham, R. S.; Linck, A. J.. (1960). Effects of the Interaction of Varying Temperatures and Light Intensities on the Response of Flax to 2, 4-D. Retrieved from the University Digital Conservancy, https://hdl.handle.net/11299/200813
[Report to Chief J. E. Curry, by an unknown author #1]
No full textReport to Chief J. E. Curry, by an unknown author. The report contains a list of officers who gave depositions to the United States Attorney
[Report to Chief J. E. Curry, by an unknown author #2]
No full textReport to Chief J. E. Curry, by an unknown author. The report contains a list of officers who gave depositions to the United States Attorney
Evidence for the decay B0→J/ψω and measurement of the relative branching fractions of meson decays to J/ψη and J/ψη′
No full textFirst evidence of the B 0 → J / ψ ω decay is found and the B s 0 → J / ψ η and B s 0 → J / ψ η ′ decays are studied using a dataset corresponding to an integrated luminosity of 1.0 fb -1 collected by the LHCb experiment in proton-proton collisions at a centre-of-mass energy of sqrt(s) = 7 TeV. The branching fractions of these decays are measured relative to that of the B 0 → J / ψ ρ 0 decay:frac(B (B 0 → J / ψ ω), B (B 0 → J / ψ ρ 0)) = 0.89 ± 0.19 (stat) - 0.13 + 0.07 (syst),frac(B (B s 0 → J / ψ η), B (B 0 → J / ψ ρ 0)) = 14.0 ± 1.2 (stat) - 1.5 + 1.1 (syst) - 1.0 + 1.1 (frac(f d, f s)),frac(B (B s 0 → J / ψ η ′), B (B 0 → J / ψ ρ 0)) = 12.7 ± 1.1 (stat) - 1.3 + 0.5 (syst) - 0.9 + 1.0 (frac(f d, f s)), where the last uncertainty is due to the knowledge of f d / f s, the ratio of b-quark hadronization factors that accounts for the different production rate of B 0 and B s 0 mesons. The ratio of the branching fractions of B s 0 → J / ψ η ′ and B s 0 → J / ψ η decays is measured to befrac(B (B s 0 → J / ψ η ′), B (B s 0 → J / ψ η)) = 0.90 ± 0.09 (stat) - 0.02 + 0.06 (syst)
Contributors to the September Issue/Notes
No full textNotes by Bernard F. Grainey, Leo L. Linck, Robert Sinon, James McVay, Jerry J. Killigrew, Warren A. Deahl, and Theodore P. Frericks
Measurement of the time-dependent CP asymmetry in B0 -> J/ψ KS0 decays
No full textThis Letter reports a measurement of the CP violation observables SJ/ψK0S and CJ/ψK0S in the decay channel B0→J/ψK0S performed with 1.0 fb−1 of pp collisions at s√=7 TeV collected by the LHCb experiment. The fit to the data yields SJ/ψK0S=0.73±0.07(stat)±0.04(syst) and CJ/ψK0S=0.03±0.09(stat)±0.01(syst). Both values are consistent with the current world averages and within
expectations from the Standard Model
Measurement of the ratio of prompt χ c to J / ψ production in pp collisions at √s = 7 TeV
No full textThe prompt production of charmonium χ c and J / ψ states is studied in proton-proton collisions at a centre-of-mass energy of √s = 7 TeV at the Large Hadron Collider. The χ c and J / ψ mesons are identified through their decays χ c → J / ψ γ and J / ψ → μ + μ - using 36 pb - 1 of data collected by the LHCb detector in 2010. The ratio of the prompt production cross-sections for χ c and J / ψ, σ (χ c → J / ψ γ) / σ (J / ψ), is determined as a function of the J / ψ transverse momentum in the range 2 < p T J / ψ < 15 GeV / c. The results are in excellent agreement with next-to-leading order non-relativistic expectations and show a significant discrepancy compared with the colour singlet model prediction at leading order, especially in the low p T J / ψ region
The Glacier Views of Jean-Antoine Linck – A Milestone for the Mont Blanc Glacier History from the 18th to the 19
No full textInterdisciplinary approaches are needed to reconstruct the behaviour of glaciers beyond the beginning of systematic measurements. For example, historical documents have been used to reconstruct former glacier extents successfully at different sites, including in the well-documented Mont Blanc area that became popular since the mid-18th century among artists, scientists, and travellers. Jean-Antoine Linck from Geneva is probably the artist to whom we owe the greatest number of unique glacier views. Linck’s special preference were the ice regions, which he discovered and drew with alpinistic daring and naturalistic correctness, preferably by gouache, although many pencil sketches are preserved. Linck subtly used the etching technique to create easily reproducible plates in large format, which are then hand-coloured with gouache and watercolour. This technique allowed him to create numerous reproductions of the same view, while still giving them a unique and original aspect, views that are remarkable for their serenity and silence, while offering luminous atmospheres. These illustrations introduced the realistic representation of the high mountains into the iconography of Genevese painting and thus led to a new kind of landscape painting with a permanent character. From a perspective of glacier history and although many of his artworks are not exactly dated by the author, the work of Jean-Antoine Linck is indispensable since it represents the whole development, specifically of the Mer de Glace and the Glacier des Bossons, but also other glaciers during the period from the end of the 18th century until the 19th century glacier maximum around 1820. Linck’s work has the same importance for the Mont Blanc area as that of Caspar Wolf and Samuel Birmann for the central Swiss Alps or Thomas Ender for the Austrian Alps in terms of glacier iconography. Therefore, Linck was both an artist and a glacier historian.
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Des approches interdisciplinaires sont nécessaires pour reconstruire les fluctuations des glaciers au xixe siècle, au-delà du début des mesures systématiques. Par exemple, des documents historiques ont été appliqués pour reconstituer d’anciennes étendues des glaciers sur différents sites, notamment dans la région du Mont-Blanc, qui sont très bien documentés et devenus populaires parmi les artistes, les scientifiques et les voyageurs depuis le milieu du xviiie siècle. Le Genevois Jean-Antoine Linck est probablement l’artiste à qui l’on doit le plus de vues glaciaires exceptionnelles. La préférence particulière de Linck était les régions des glaciers, qu’il a découvertes et dessinées avec une audace d’alpiniste et une exactitude de naturaliste, principalement à la gouache, bien que de nombreux croquis au crayon aient été conservés. Linck a subtilement utilisé la technique de la gravure pour créer des planches de grand format facilement reproductibles, qui ont été ensuite coloriées à la gouache et à l’aquarelle. Cette technique lui a permis de créer de nombreuses reproductions d’une même vue, tout en leur donnant un aspect unique et original. Elles sont remarquables de sérénité et de silence, tout en offrant des ambiances lumineuses. Ces illustrations introduisent la représentation réaliste de la haute montagne dans l’iconographie de la peinture genevoise et conduisent ainsi à une nouvelle forme de peinture de paysage à caractère permanent. D’un point de vue de l’histoire des glaciers, et bien que nombre de ses œuvres ne soient pas exactement datées par l’auteur, l’ouvrage de Jean-Antoine Linck est indispensable. Il représente l’ensemble de l’évolution de la mer de Glace et du glacier des Bossons, mais également d’autres glaciers, pendant la période allant de la fin du xviiie siècle jusqu’au maximum glaciaire du xixe siècle vers 1820. L’œuvre de Linck accorde au territoire du Mont-Blanc la même importance, en termes d’iconographie des glaciers, que celle de Caspar Wolf et Samuel Birmann pour les Alpes centrales suisses, ou de Thomas Ender pour les Alpes autrichiennes. Linck était donc à la fois artiste et historien des glaciers
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