4-(4-Hy­droxy­methyl-1H-1,2,3-triazol-1-yl)benzoic acid

In the title compound, C10H9N3O3, there is a small twist between the benzene and triazole rings [dihedral angle = 6.32 (7)°]; the carb­oxy­lic acid residue is almost coplanar with the benzene ring to which it is attached [O—C—C—C torsion angle = 1.49 (19)°]. The main deviation from coplanarity of the non-H atoms is found for the hy­droxy group which is almost perpendicular to the remaining atoms [N—C—C—O torsion angle = −75.46 (16)°]. In the crystal, the presence of O—H⋯O (between carboxyl groups) and O—H⋯N (between the hy­droxy group and the triazole ring) hydrogen bonds leads to supra­molecular chains along [03]. The chains are connected into sheets via C—H⋯O(hy­droxy) inter­actions

Musical Theatre Adapting to a Mediatized Audience Shown Through The Analysis of Dear Evan Hansen

Within this empirical study, Dear Evan Hansen has been analysed with the intention of finding how musical theatre is changing to suit a mediatized audience; an audience inhabited by digital natives. In order to achieve this, the musical’s portrayal of social media has been scrutinised through two case studies dissecting the two songs from the show, Waving through a Window and You Will Be Found. These case studies have been analysed using criteria laid out in the methodology which has then been used to interpret themes through thematic analysis. It was concluded that Dear Evan Hansen majorly favoured more negative aspects of social media and that Dear Evan Hansen has been created with a mediatized audience in mind. Thematic analysis was able to reveal these results through finding dominant features of social media through themes and recurring motifs throughout the case studies

data files for Variation and Taphonomic Implications of Composition in Modern and Fossil Malacostracan Cuticles

Data Files for Variation and Taphonomic Implications of Composition in Modern and Fossil Malacostracan Cuticles by Roy E. Plotnick and Steve McCarroll. Journal of Crustacean Biology.  https://doi.org/10.1093/jcbiol/ruad047   This data set contains major element chemical analyses (Ca, Mg, Na, P) using SEM-EDS of modern crustacean exoskeletons from Bermuda, Georgia (U.S.A.), and Lake Tanganyika, Burundi and fossils from Texas. Elemental compositions of these cuticles were determined utilizing a JEOL JSM-35CE Scanning Electron Microscope (JEOL, Tokyo, Japan) equipped with a Tracor Northern 5500 (Microscan Energy Dispersive Spectrometer (EDS) (Tracor Northern, Middleton, Wisconsin, USA), using Bence-Albee or ZAF quantitative methods.  Each data file has a name and/or an original file number. These are listed, along with the taxonomic data, in Supplemental File S4 of the paper, included here.  The ZAF analyses reported by the probe software were elemental weight percents, whereas Bence-Albee (BA) analyses were reported as normalized oxide weight percents. For consistency, the oxide values were converted to elemental values. This was a two-step process: 1) The normalization of the oxide values needed to be reversed. This required locating the original data for the total percents for each data point. The normalized data could then be converted back to the “calculated weight” for the oxide. For example: a. Normalized weight percent CaO = 50.43% b. Total non-normalized weight percent all data = 85.06% c. Original calculated (non-normalized) percent CaO = 42.90% 2) The oxide percents could then be converted to element percent using the following conversion factors: a. Ca = CaO *0.71469 b. Mg = MgO * 0.60311 c. Na = Na2O * 0.74186 d. P = P2O5 * 0.43642 ZAF: remainder of weight assumed to be oxygen BA – remainder CO2 by stochiometry Data was originally on dot matrix computer printouts. These were typed into Excel spreadsheets by Erin Conley. Original hard copies of the summary data and the point-by-point analyses are stored in Roy Plotnick’s office in 2454 SES. </p

Reinterpreting Rotherslade, Gower Peninsula: implications for Last Glacial ice limits and Quaternary stratigraphy of the British Isles

Rotherslade on the Gower Peninsula in south Wales has been viewed as a key site for the reconstruction of Quaternary depositional environments in the British Isles. Since the early 20th century, and certainly since the 1980s, the accepted view has been that Rotherslade is the most westerly location on the south Gower coast where there is in situ basal till exposed and that, logically, this location marks the position of the LGM ice limit. However, reinvestigation of the sediments and their architecture, and analysis of clast fabrics and thin sections of critical sedimentary units, show that none of the exposed sediments has properties diagnostic of subglacial deposition or deformation. We postulate here that LGM ice terminated at the western side of Swansea Bay, a few kilometres to the north-east of Rotherslade, and propose that the sedimentary sequence comprises Early to Middle Devensian periglacial sediments, overlain by a complex of Late Devensian, ice-proximal outwash fan deposits, an assemblage of paraglacial debris and, finally, periglacial mass movement deposits. The proposed repositioning of the Late Devensian ice limit and the associated new subaerial interpretation of the sediments suggest that a reassessment of sedimentary sequences (Hunts Bay, Western Slade) and landforms (Paviland Moraine) farther west on Gower, which have attained similar stratigraphical status, is now warranted