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Figure 2 in Two new species of feather mites (Acarina: Psoroptidia) from the Oriental Magpie-Robin,Copsychus saularis (Passeriformes: Muscicapidae)
Figure 2 Dolichodectes latilobusn. sp., male: A – D details of legs, dorsal view, A – leg I, B – leg II, C – leg III, D – leg IV; E – details of opisthosoma.
Text-fig. 2. (A) Orientation of Schizocrania filosa (HALL, 1847) on articulated shells of benthic brachiopod Rafinesquina sp. (A1–A3 – on dorsal valve of articulated shells, A4 – on ventral valve of articulated shell; forward growth direction is unclear in three specimens) from Upper Ordovician, Corryville Formation, Lawrenceburg, Indiana (after www.drydredgers.org/scizo.htm). (B) Orientation of Schizocrania multistriata (REED, 1905) shells on outer face of conulariid Metaconularia imperialis test (Dobrotivá Formation, Kařízek mine, Barrandian area; after Havlíček and Vaněk 1996); preserved conulariid shell in white, suggested outline of incomplete conulariid test in grey. Arrows indicate direction of forward growth of Schizocrania specimens. in Schizocrania (Brachiopoda, Discinoidea): Taxonomy, Occurrence, Ecology And History Of The Earliest Epizoan Lingulate Brachiopod
Text-fig. 2. (A) Orientation of Schizocrania filosa (HALL, 1847) on articulated shells of benthic brachiopod Rafinesquina sp. (A1–A3 – on dorsal valve of articulated shells, A4 – on ventral valve of articulated shell; forward growth direction is unclear in three specimens) from Upper Ordovician, Corryville Formation, Lawrenceburg, Indiana (after www.drydredgers.org/scizo.htm). (B) Orientation of Schizocrania multistriata (REED, 1905) shells on outer face of conulariid Metaconularia imperialis test (Dobrotivá Formation, Kařízek mine, Barrandian area; after Havlíček and Vaněk 1996); preserved conulariid shell in white, suggested outline of incomplete conulariid test in grey. Arrows indicate direction of forward growth of Schizocrania specimens.
Text-fig. 2. Soft-tissue imprints and traces of bioerosion on Middle Ordovician cephalopods from Estonia. a: GIT 819-1, Tragoceras falcatum (SCHLOTHEIM, 1820), drag bands; b: GIT 819-1, T. falcatum, pseudosutures; c: GIT 819-2, Estonioceras sp., drag bands; d: GIT 819-3, cf. Anthoceras vaginatum (SCHLOTHEIM, 1820), drag bands; e: GIT 819-4, cf. Orthoceras regulare SCHLOTHEIM, 1820, drag bands; f: Pits on the body chamber of GIT 819-1, T. falcatum. Specimens oriented with aperture downwards. Scale bars 1 mm. in Conch Structures, Soft-Tissue Imprints And Taphonomy Of The Middle Ordovician Cephalopod Tragoceras Falcatum From Estonia
Text-fig. 2. Soft-tissue imprints and traces of bioerosion on Middle Ordovician cephalopods from Estonia. a: GIT 819-1, Tragoceras falcatum (SCHLOTHEIM, 1820), drag bands; b: GIT 819-1, T. falcatum, pseudosutures; c: GIT 819-2, Estonioceras sp., drag bands; d: GIT 819-3, cf. Anthoceras vaginatum (SCHLOTHEIM, 1820), drag bands; e: GIT 819-4, cf. Orthoceras regulare SCHLOTHEIM, 1820, drag bands; f: Pits on the body chamber of GIT 819-1, T. falcatum. Specimens oriented with aperture downwards. Scale bars 1 mm.
Text-fig. 1. Megastriae and post mortem epicoles on Tragoceras falcatum (SCHLOTHEIM, 1820). Arrows and M1–M3 indicate megastriae, bryozoan colonies are indicated by B1 and B2. a: GIT 819-1, left lateral view; b: body chamber of GIT 819-1, dorsal view; c: body chamber of GIT 819-1, left lateral view; d: GIT 819-1, right lateral view; e: PIMUZ 37299, right lateral view; f: detail of the body chamber of GIT 819-1, right lateral view, encrusted by bryozoans; g: bryozoan colony with Trypanites borings growing on an older bryozoan crust GIT 819-1. Specimens oriented with aperture downwards. Scale bars 10 mm. in Conch Structures, Soft-Tissue Imprints And Taphonomy Of The Middle Ordovician Cephalopod Tragoceras Falcatum From Estonia
Text-fig. 1. Megastriae and post mortem epicoles on Tragoceras falcatum (SCHLOTHEIM, 1820). Arrows and M1–M3 indicate megastriae, bryozoan colonies are indicated by B1 and B2. a: GIT 819-1, left lateral view; b: body chamber of GIT 819-1, dorsal view; c: body chamber of GIT 819-1, left lateral view; d: GIT 819-1, right lateral view; e: PIMUZ 37299, right lateral view; f: detail of the body chamber of GIT 819-1, right lateral view, encrusted by bryozoans; g: bryozoan colony with Trypanites borings growing on an older bryozoan crust GIT 819-1. Specimens oriented with aperture downwards. Scale bars 10 mm.
Text-fig. 34. Scanning electron microscope (SEM) images of monocolpate pollen of Mayoa portugallica from a fragmentary stamen; Torres Vedras locality, Portugal. a) Stamen fragment that yielded the pollen in this Text-figure; b–d) Pollen grains showing the distinctive perpendicular orientation of two broad bands of striae that converge at the ends of the grains. Specimen, TV44-S136663. Scale bars 150 Μm (a), 6 Μm (b, c), 3 Μm (d). in The Early Cretaceous Mesofossil Flora Of Torres Vedras (Ne Of Forte Da Forca), Portugal: A Palaeofloristic Analysis Of An Early Angiosperm Community
Text-fig. 34. Scanning electron microscope (SEM) images of monocolpate pollen of Mayoa portugallica from a fragmentary stamen; Torres Vedras locality, Portugal. a) Stamen fragment that yielded the pollen in this Text-figure; b–d) Pollen grains showing the distinctive perpendicular orientation of two broad bands of striae that converge at the ends of the grains. Specimen, TV44-S136663. Scale bars 150 Μm (a), 6 Μm (b, c), 3 Μm (d).
Figs. 36–39 in A taxonomic review of the Oriental Laccophilus javanicus species group (Coleoptera: Dytiscidae)
Figs. 36–39. Habitats: 36, E Kalimantan, Muara Ritan (type locality of Laccophilus kalimantanensis, new species); 37, China, Guangxi, Shiwandashan (locality of L. komareki, new species); 38, E Kalimantan, Sungai Wain (locality of L. mahakamensis); 39, Laos, Attapeu (locality of L. tonkinensis).
Figs. 18–35 in A taxonomic review of the Oriental Laccophilus javanicus species group (Coleoptera: Dytiscidae)
Figs. 18–35. Median lobe in lateral view: 18, Laccophilus aurofasciatus; 19, L. auropictus; 20, L. ceylonicus; 21, L. elegans; 22, L. girardi; 23, L. hendrichi, new species; 24, L. jaechi, new species; 25, L. javanicus; 26, L. kalimantanensis, new species; 27, L. komareki, new species. 28, L. mahakamensis; 29, L. mazzoldii, new species; 30, L. nusatenggaraensis, new species; 31, L. schillhammeri, new species; 32, L. stastnyi, new species; 33, L. tobaensis; 34, L. tonkinensis; 35, L. wittmeri. Scale bar = 0.5 mm.
Figs. 10–17 in A taxonomic review of the Oriental Laccophilus javanicus species group (Coleoptera: Dytiscidae)
Figs. 10–17. Habitus of Laccophilus: 10, L. mahakamensis; 11, L. mazzoldii, new species; 12, L. nusatenggaraensis, new species; 13, L. schillhammeri, new species; 14, L. stastnyi, new species; 15, L. tobaensis; 16, L. tonkinensis; 17, L. wittmeri. Scale bar = 1 mm.
Figs. 1–9 in A taxonomic review of the Oriental Laccophilus javanicus species group (Coleoptera: Dytiscidae)
Figs. 1–9. Habitus of Laccophilus: 1, L. aurofasciatus; 2, L. auropictus; 3, L. ceylonicus; 4, L. elegans; 5, L. girardi; 6, L. hendrichi, new species; 7, L. jaechi, new species; 8, L. javanicus; 9, L. komareki, new species. Scale bar = 1 mm.
Text-fig. 16. a) MNHN LBE 007, symphysis with left and right i/1 of Barytherium sp. from Dor el Talha, Libya. (a1 – superior stereo views of the symphysis, a2 – stereo distal view of right i/1 (arrow 1 shows the interstitial contact facet close to the apex caused by abrasion against the right i/2), a3 – section of right i/1 viewed from the radicular end to show the extent of the enamel cover (below the arrows 2) and the dome-shaped dentine mass on the lingual aspect (above the arrows), a4 – stereo occlusal views of right i/1 (note the orientation of the apical wear facet), a5 – stereo mesial view) (scale bar 5 cm); b–c) NHMUK M 82167b, distal stereo views of lower central incisors of Arcanotherium savagei from Dor el Talha, Libya, to show the interstitial wear facets near cervix caused by abrasion against the i/2s (b – left i/1, c – right i/1) (scale bar 10 cm). in Large Mammals From The Rupelian Of Oman - Recent Finds
Text-fig. 16. a) MNHN LBE 007, symphysis with left and right i/1 of Barytherium sp. from Dor el Talha, Libya. (a1 – superior stereo views of the symphysis, a2 – stereo distal view of right i/1 (arrow 1 shows the interstitial contact facet close to the apex caused by abrasion against the right i/2), a3 – section of right i/1 viewed from the radicular end to show the extent of the enamel cover (below the arrows 2) and the dome-shaped dentine mass on the lingual aspect (above the arrows), a4 – stereo occlusal views of right i/1 (note the orientation of the apical wear facet), a5 – stereo mesial view) (scale bar 5 cm); b–c) NHMUK M 82167b, distal stereo views of lower central incisors of Arcanotherium savagei from Dor el Talha, Libya, to show the interstitial wear facets near cervix caused by abrasion against the i/2s (b – left i/1, c – right i/1) (scale bar 10 cm).
Figs. 5–11 in A New Species of Tetralonia (Thygatina) from India, with Notes on the Oriental Fauna (Hymenoptera: Apidae)
Figs. 5–11. Holotype male of Tetralonia (Thygatina) macroceps, new species. 5. Facial view; 6. base of antenna showing scape, pedicel, and first three flagellomeres; 7. metapretarsus; 8. seventh metasomal tergum (left half is dorsal, right half is ventral); 9. seventh metasomal sternum; 10. eighth metasomal sternum; 11. genitalic capsule. Scale bars 5 1 mm (bar between mandibles for fig. 5; bar beneath distitarsus for figs. 6– 8; bar at bottom of right column for figs. 9–11).
Figs. 12–14 in A New Species of Tetralonia (Thygatina) from India, with Notes on the Oriental Fauna (Hymenoptera: Apidae)
Figs. 12–14. Photomicrographs of female of Tetralonia (Thygatina) macroceps, new species. 12. Lateral habitus; 13. dorsal habitus; 14. facial view.
Fig. 4 in A New Species of Tetralonia (Thygatina) from India, with Notes on the Oriental Fauna (Hymenoptera: Apidae)
Fig. 4. Labiomaxillary complex and detail of maxilla depicting maxillary palpus of male holotype of Tetralonia (Thygatina) macroceps, new species. Scale bars 5 1 mm.
Text-fig. 2. First upper molar variation in Progonomys husssaini from three localities in the upper part of the Nagri Formation, Potwar Plateau, Pakistan. The 12 molars are oriented with buccal side upward, each at the same 1 mm scale, making size variation apparent. a) YGSP 33187 from locality Y 450; b) 34556, c) 54131, d) 54143, e) 54151, f) 54152, all from Y 311; g) 33937, h) 33947, i) 33957, j) 33959, k) 33963, l) 33976 all from Y 259. Figures a, c, e, f, h, k are all right M1; the others are left M1. in Early Late Miocene Murine Rodents From The Upper Part Of The Nagri Formation, Siwalik Group, Pakistan, With A New Fossil Calibration Point For The Tribe Apodemurini (Apodemus/Tokudaia)
Text-fig. 2. First upper molar variation in Progonomys husssaini from three localities in the upper part of the Nagri Formation, Potwar Plateau, Pakistan. The 12 molars are oriented with buccal side upward, each at the same 1 mm scale, making size variation apparent. a) YGSP 33187 from locality Y 450; b) 34556, c) 54131, d) 54143, e) 54151, f) 54152, all from Y 311; g) 33937, h) 33947, i) 33957, j) 33959, k) 33963, l) 33976 all from Y 259. Figures a, c, e, f, h, k are all right M1; the others are left M1.
Synchrotron X-ray Diffraction Results - Measuring Bulk Crystallographic Texture from Differently-Orientated Ti-6Al-4V Samples
<p>A dataset of crystallographic texture results for both α (hexagonal close packed, hcp) and β (body-centred cubic, bcc) phases, measured from six differently orientated Ti-6Al-4V (Ti-64) samples, using two different analysis techniques of synchrotron X-ray diffraction (SXRD) data. The texture results are produced from two refinement methods for fitting intensities from SXRD pattern images; an established Rietveld refinement method using the software package <a href="http://maud.radiographema.eu">MAUD (Materials Analysis Using Diffraction)</a> and a new Fourier-based peak fitting method from the <a href="https://pypi.org/project/continuous-peak-fit/">Continuous-Peak-Fit</a> Python package. The texture results were also compared with electron backscatter diffraction (EBSD) measurements from a single sample orientation. The SXRD and EBSD textures were analysed using <a href="https://mtex-toolbox.github.io">MTEX</a> to enable a direct comparison of the pole figures, orientation distribution functions (ODFs) and numerical values for the texture indices. The SXRD texture is calculated from each of the six different sample orientations, a combination of the six sample orientations, and in a batch processing method for calculating spatially-resolved texture variation from 387 individual X-Y stage-scan SXRD measurements across one of the samples. The texture variation measured using stage-scan SXRD is directly compared with EBSD, by splitting up the EBSD map into an equivalent grid matrix using an automated script in MTEX.</p> <p><strong>Material </strong></p> <p>The Ti-64 material used in this study was pre-rolled to 87.5% reduction at 915ºC and then air-cooled to develop a characteristic texture. The run numbers from the experiment reference six different sample orientations, according to their alignment with the original rolling directions (RD – rolling direction, TD – transverse direction, ND – normal direction), and alignment with the horizontal (X) and vertical (Y) axes of the synchrotron detector.</p> <p><strong>MAUD / MTEX Analysis</strong></p> <p>The α and β phase texture for each of the six different sample orientations was calculated using MAUD, included in this <a href="https://doi.org/10.5281/zenodo.7311323">analysis dataset</a>, which produced ODFs in the form of text files. The texture files were analysed in MTEX using scripts from the <a href="https://github.com/LightForm-group/MAUD-batch-analysis">MAUD-batch-analysis</a> package, for plotting of the pole figures and ODF slices, along with calculation of pole figure maxima, ODF maxima and texture indices. The same procedure was used to analyse texture from all six orientations together; using MTEX to fit a single ODF text file. And a series of ODF text files were analysed to calculate texture variation from an X-Y stage scan of Sample 1 (103845). Two different ODF resolutions of 5º and 15º were initially used to fit the texture in MAUD, with the same ODF resolution applied to analyse the data in MTEX. However, an ODF resolution of 15° was found to reproduce the most reasonable texture strength intensity values, with the closest match to the EBSD results.</p> <p><strong>Continuous-Peak-Fit / MTEX Analysis </strong></p> <p>The lattice plane intensities for 21 α and 4 β phase peaks were extracted from the Continuous-Peak-Fit analysis, included in this <a href="https://doi.org/10.5281/zenodo.7311323">analysis dataset</a>, and saved as text files in the form of pole figures. The lattice intensity text files were analysed in MTEX using scripts from the <a href="https://github.com/LightForm-group/continuous-peak-fit-analysis">continuous-peak-fit-analysis</a> package, to plot pole figures and ODF slices, and to calculate pole figure maxima, ODF maxima and texture indices. The same procedure was used to analyse texture from all six orientations together, along with combinations of different sample orientations, by fitting combined lattice intensity text files in MTEX. And a series of lattice intensity text files were analysed to calculate texture variation from the X-Y stage scan of Sample 1 (103845). Lattice plane intensity distributions which had been normalised to a Ti-64 powder sample measurement were also analysed, to see if this had any effect on the texture intensities. Nevertheless, the powder-corrected texture was found to exactly match the raw intensity measurements. Three different ODF resolutions of 5º, 10º and 15º were initially used to fit the texture in MTEX. However, a kernel half-width of 10° was found to produce optimal data fitting, for highly accurate texture strength intensity values.</p> <p><strong>EBSD / MTEX Analysis </strong></p> <p>The indexed α-phase EBSD measurements were recorded over an area of around 100 mm<sup>2</sup>, with an equivalent sized map of β-phase orientations reconstructed from the data. Both the α and the β phase maps were analysed using the <a href="https://github.com/LightForm-group/MTEX-texture-block-analysis">MTEX-texture-block-analysis</a> package, which was used to split up the map into 387 individual square sections, with equivalent dimensions to the SXRD stage-scan measurement grid. For each of the 387 sections, MTEX was used to plot pole figures and ODF slices, and to calculate pole figure maxima, ODF maxima and texture indices.</p> <p><strong>Texture Variation Comparison</strong></p> <p>The texture values calculated from the SXRD stage scan measurements, with the two analysis methods, were used for a direct comparison with the texture variation recorded using EBSD. This analysis was recorded in the <a href="https://github.com/LightForm-group/texture-strength-comparison">texture-strength-comparison</a> package. The results show differences in texture variation across the piece depending on the method used to analyse the SXRD data. The Continuous-Peak-Fit analysis method shows the closest match with EBSD, producing clear texture intensity spikes for the different α and β lattice plane pole figure intensities, ODF maxima and texture indices, at the centre of the piece. The results were also used to develop SXRD maps showing the distribution of texture intensities across the sample.</p> <p><strong>Metadata </strong></p> <p>An accompanying YAML text file contains associated processing metadata for the SXRD and EBSD analyses, recording information about the different packages used to process the data, along with details about the different files contained within this results dataset.</p>
CommonCrawl News Articles by Political Orientation
<p><strong>Dataset description & reproduction steps</strong></p> <p>The dataset includes news articles gathered from CommonCrawl for media outlets that were selected based on their political orientation. The news articles span publication dates from 2010 to 2021. For more details, please check out our <a href="https://aclanthology.org/2022.findings-emnlp.152/">Paper</a> and <a href="https://github.com/webis-de/emnlp22-social-bias-representation-accuracy">GitHub repository</a>.</p> <p>The database file containing the news articles has two main tables, <em>article_urls</em> and <em>article_contents</em>. The tables have the following columns:</p> <p><em>article_urls</em>:</p> <ul> <li><code>uuid</code>: An ID that uniquely identifies this URL entry. This column is used as primary key for the table.</li> <li><code>url</code>: The plain text URL for the news article, as found in CommonCrawl.</li> <li><code>outlet_name</code>: The name of the news outlet that published the article.</li> </ul> <p><em>article_contents</em>:</p> <ul> <li><code>uuid</code>: An ID that uniquely identifies this content entry. This column is used as primary key for the table. The key is the same key used in the <em>article_urls</em> table to allow for cross-referencing.</li> <li><code>date</code>: The automatically extracted publishing date of the article. If it was not possible to automatically extract the date, this field remains empty.</li> <li><code>content</code>: The plain text content of the article automatically extracted from the crawled HTML document.</li> <li><code>content_preprocessed</code>: The articles content split by sentences.</li> <li><code>langauge</code>: The langauge of the article, as identified by the langdetect module (as ISO 639-1 code).</li> </ul>
IODP Expedition 350 Core orientation
<p>Core orientation data were measured downhole during advanced piston corer (APC) coring, either by Minex FlexIT or Icefield MI-5 core orientation tool. These tools measure magnetic strength and orientation, 3-axis accelerometer data, and tool temperature data.</p>
Data for: Frond orientations with independent current indicators demonstrate the reclining rheotropic mode of life of several Ediacaran rangeomorph taxa
<p>Fossils from the deep-sea Ediacaran biotas of Newfoundland are among the oldest architecturally complex soft-bodied macroorganisms on Earth. Most organisms in the Mistaken Point-type biotas of Avalonia — particularly the fractal-branching frondose Rangeomorpha — have been traditionally interpreted as living erect within the water column during life. However, due to the scarcity of documented physical sedimentological proxies associated with fossiliferous beds, Ediacaran paleocurrents have been inferred in some instances from the preferential orientation of fronds. This calls into question the relationship between frond orientation and paleocurrents. In this study, we present an integrated approach from a newly described fossiliferous surface (the "Melrose Surface" in the Fermeuse Formation at Melrose, on the southern portion of the Catalina Dome in the Discovery UNESCO Global Geopark) combining: (1) physical sedimentological evidence for paleocurrent direction in the form of climbing ripple cross lamination, and (2) a series of statistical analyses based on modified polythetic and monothetic clustering techniques reflecting the circular nature of the recorded orientation of <em>Fractofusus</em> <em>misrai</em> specimens. This study demonstrates the reclining rheotropic mode of life of the Ediacaran rangeomorph taxon <em>Fractofusus</em> <em>misrai</em> and presents preliminary inferences suggesting a similar mode of life for <em>Bradgatia</em> sp. and <em>Pectinifrons</em> <em>abyssalis</em> based on qualitative evidence. These results advocate for the consideration of an alternative conceptual hypothesis for the position of life of Ediacaran organisms in which they are interpreted as having lived reclined on the seafloor, in the position that they are preserved.</p>
Figs 16-21 in Contribution to the knowledge of Oriental Syzeuctus FÖRSTER (Hymenoptera, Ichneumonidae, Banchinae), with description of six new species
Figs 16-21: Heads from frontal: (16) Syzeuctus achterbergi nov.sp. ♀ HT; (17) S. floresiensis nov.sp. ♀ HT; (18) S. genator nov.sp. ♀ HT; (19) S. laoticus nov.sp. ♀ HT; (20) S. orientalis nov.sp. ♁ HT; (21) S. siamensis nov.sp. ♀ HT.
Figs 10-15 in Contribution to the knowledge of Oriental Syzeuctus FÖRSTER (Hymenoptera, Ichneumonidae, Banchinae), with description of six new species
Figs 10-15: Faces from frontal: (10) Syzeuctus achterbergi nov.sp. ♀ HT; (11) S. floresiensis nov.sp. ♀ HT; (12) S. genator nov.sp. ♀ HT; (13) S. laoticus nov.sp. ♀ HT; (14) S. orientalis nov.sp. ♁ HT; (15) S. siamensis nov.sp. ♀ HT.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.