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Lattice configurations for Cu/ Zn order-disorder transitions in Cu2ZSnS4
<p>Data on thermodynamic Cu/ Zn disorder in Cu2ZnSnS4 generated using ERIS (10.5281/zenodo.1471439).</p>
FIGURE 11 in The integration processes of the distributional patterns in the Mexican Transition Zone: Phyletic, paleogeographic and ecological factors of a case study
FIGURE 11. Graphic hypothesis of the phyletic diversification and relationships of the O. chevrolati species group in the Mexican Transition Zone. Tip names are the species complexes. The figure elucidates our ideas of the taxonomical relationships and evolution of this species group based on the male and female genitalia, external morphology and geographic distribution: 1. The ancestral line of the O. chevrolati species group must have arrived in what is now Mexico between the Eocene and the Miocene, as part of the most ancient fauna of northern origin. The ancestor of O. vespertilio early separated from the ancestral trunk (plesiomorphic genitalia characters). 2. The ancestral species of the O. hippopotamus species line and of the O. hippopotamus species complex dispersed throughout the Trans-Mexican Volcanic Belt prior to its current conformation (Miocene to Pliocene). The geomorphological evolution of this mountain system drived the processes of speciation in this complex. Its descendants adapted to the burrows of Geomyidae in the mountains. 3. Separation of the O. hippopotamus and O. brevifrons species complexes. The first evolved with the TMVB, with some expansion southwards and northwards (O. coproides reaching New Mexico and Arizona). The brevifrons species complex is found in the southeastern United States of America and north-northeastern Mexico. Both complexes are found in the mountains and associated with the protected environments of rodent nests: Geomyidae in the case of the O. hippopotamus and Neotoma species complexes, plus three species in caves in the case of the O. brevifrons species complex.
FIGURE 8 in The integration processes of the distributional patterns in the Mexican Transition Zone: Phyletic, paleogeographic and ecological factors of a case study
FIGURE 8. Onthophagus mesoamericanus, male holotype dorsal view, currently a synonym of O. cyanellus.
Transitioning from Open Strategy to Open Practice
<p>Audio from <em>Session 2: Transitioning from Open Strategy to Open Practice</em>, held Wednesday 26 June 2019 at the LIBER 2019 Annual Conference.</p> <p>Talks included:</p> <ul> <li>2.1 <a href="https://doi.org/10.5281/zenodo.3258188">Open Scholarship in Practice: Presentation of a Set of Use Cases Collected on Behalf of Knowledge Exchange</a>, Gwen Franck, Gwen Franck GCV, Belgium</li> <li>2.2 <a href="https://doi.org/10.5281/zenodo.3258190">Making Open Science transparent: the Bibliolabs project</a>, Henri Bretel, Julien Sempéré, Vincent Thébault, Université Paris-Saclay, Paris, France</li> <li>2.3 <a href="https://doi.org/10.5281/zenodo.3258192">Is This the Way to Reproducibility?</a> Patricia Herterich, University of Birmingham, United Kingdom, Rosie Higman, University of Manchester, United Kingdom, The Turing Way, Alan Turing Institute, United Kingdom</li> </ul>
Seconds-scale coherence on an optical clock transition in a tweezer array (publication data)
<p>Accompanying data for<em> Seconds-scale coherence on an optical clock transition in a tweezer array.</em></p>
Intermediate bosonic metallic state in the superconductor-insulator transition
<p>Whether a metallic ground state exists in a two-dimensional system beyond Anderson localization remains an unresolved question. Here, we study how quantum phase coherence evolves across superconductor-metal-insulator transitions via magneto-conductance quantum oscillations in nanopatterned high-temperature superconducting films. We tune the degree of phase coherence by varying the etching time of our films. Between the superconducting and insulating regimes, we detect a robust intervening anomalous metallic state characterized by saturating resistance and oscillation amplitude at low temperatures. Our measurements suggest that the anomalous metallic state is bosonic and that the saturation of phase coherence plays a prominent role in its formation.</p>
Fig. 2 in Diversity and biogeographical makeup of the dung beetle communities inhabiting two mountains in the Mexican Transition Zone
Fig. 2 Relationship between the decrease (circles and black squares) and the accumulation (circles and open squares) of genera and species with increasing elevation in Los Tuxtlas and La Chinantla
FIGURE 4 in Species richness, geographic distribution and endemism of Pinguicula (Lentibulariaceae) in the Mexican Transition Zone
FIGURE 4. Species richness and endemism distribution of Pinguicula by: A) country; B) biome; C) biogeographic province. Dark grey = total species, light grey = endemic species.
FIGURE 3 in Species richness, geographic distribution and endemism of Pinguicula (Lentibulariaceae) in the Mexican Transition Zone
FIGURE 3. Biomes with habitats of Pinguicula. A) Cave with stalactites, Tropical & Subtropical Coniferous Forest; B, I) Inselbergs, Tropical & Subtropical Coniferous Forest; C–D) Limestone rock walls, Tropical & Subtropical Moist Broadleaf Forest; E–G, L) Tropical & Subtropical Dry Broadleaf Forest; H) Ravine with a gypsum soils, Tropical & Subtropical Coniferous Forest; J–L) Tropical & Subtropical Coniferous Forest; K) Desert & Xeric Shrubland.
FIGURE 2 in Species richness, geographic distribution and endemism of Pinguicula (Lentibulariaceae) in the Mexican Transition Zone
FIGURE 2. Temperate winter and annual tropical rosettes in Pinguicula. A) P. ehlersieae; B) P. crassifolia; C, I) P. moranensis; D) P. acuminata; E) P. nivalis; F) P. michoacana; G) P. rotundiflora; H) P. kondoi; J) P. lilacina; K) P. takaki; L) P. pygmaea. A–C) epigeous rosettes, D–F) hypogeous rosettes, G–I), subhypogeous rosettes, J–L) annual rosettes. A–L) J. López.
FIGURE 6 in Species richness, geographic distribution and endemism of Pinguicula (Lentibulariaceae) in the Mexican Transition Zone
FIGURE 6. Geographical distribution of subgenera and species of Pinguicula. A) Subgenera distribution; B) Pinguicula subgenus Isoloba; C) Pinguicula subgenus Pinguicula; D) Pinguicula subgenus Temnoceras.
FIGURE 5 in Species richness, geographic distribution and endemism of Pinguicula (Lentibulariaceae) in the Mexican Transition Zone
FIGURE 5. Distribution of Pinguicula by elevation. A) Histogram frequency of the species richness distribution, in dark grey the principal class; B) boxplot distribution of Pinguicula species.
FIG. 5 in Marine Habitat Transitions and Body-Shape Evolution in Lizardfishes and Their Allies (Aulopiformes)
FIG. 5. Results of principal component analysis depicting principal component 1 and principal component 2 with eight homologous landmarks and 70 semi-landmarks. Colored polygons represent distribution by marine habitat.
FIG. 6 in Marine Habitat Transitions and Body-Shape Evolution in Lizardfishes and Their Allies (Aulopiformes)
FIG. 6. Marine habitat transitions among Aulopiformes inferred on the time-calibrated phylogeny from Davis and Fielitz (2010). Outgroups trimmed from tree to highlight Aulopiformes. Benthic continental shelf to upper slope may range from approximately 0 to 500 meters depending on region, with most continental shelves breaking at 200 m. Deep-sea pelagic includes the zones below the epipelagic starting with the mesopelagic at 200 m. Maximum-likelihood character reconstruction of habitat shown with probabilities of states represented at nodes.
FIG. 3 in Marine Habitat Transitions and Body-Shape Evolution in Lizardfishes and Their Allies (Aulopiformes)
FIG. 3. Results of principal component analysis depicting principal component 1 and principal component 2 with eight homologous landmarks and 70 semi-landmarks. Colored polygons highlight distribution of specimens within families of lizardfishes.
FIG. 2 in Marine Habitat Transitions and Body-Shape Evolution in Lizardfishes and Their Allies (Aulopiformes)
FIG. 2. Example of fixed landmark (blue circles) and sliding semi-landmark (purple circles) locations on a lizardfish (SynoduS VariegatuS illustrated). Homologous fixed landmarks follow those from McMahan et al. (2011) and include: 1, anterior insertion of the dorsal fin on body; 2, posterior insertion of the dorsal fin on the body; 3, dorsal insertion of caudal fin; 4, ventral insertion of caudal fin; 5, posterior insertion of anal fin on the body; 6, anterior insertion of anal fin on body; 7, the point at which the interopercle meets the ventral body outline; 8, anterior tip of premaxilla. Digital image by R. P. Martin.
Dataset and code for "Higher labor intensity in US automotive assembly plants after transitioning to electric vehicles"
<p>Dataset and code for the article: "<span>Higher labor intensity in US automotive assembly </span><span>plants after transitioning to electric vehicles" submitted to Nature Communications. </span></p>
FIGURE 1 in The Drosophilid Fauna (Diptera, Drosophilidae) Of The Transition Between The Pampa And Atlantic Forest Biomes In The State Of Rio Grande Do Sul, Southern Brazil: First Records
FIGURE 1: Study area: A) Map of Brazil and of the state of Rio Grande do Sul, showing the location of Cruz Alta, in the contact zone between the two biomes: Atlantic Forest (in the North) and Pampa (in the South). B) Vila Rocha, in the urban zone of Cruz Alta. C) Centro de Educação, Pesquisa e Proteção Ambiental (CEPPA), in a fragment of riparian forest within a rural zone. B and C in the same scale; arrows indicate points of collections.
Fig. 2 in Evidence of positive selection suggests possible role of aquaporins in the water-to-land transition of mudskippers
Fig. 2 Sequence alignment and structural annotation of AQP10a and AQP11b showing positively selected positions in mudskippers (indicated with triangles and olive green or purple bars, respectively). The sequences of the corresponding paralogs of D. rerio are included as reference. Upper bars denote helices and loops. Boxes denote NPA motifs
Fig. 1 in Evidence of positive selection suggests possible role of aquaporins in the water-to-land transition of mudskippers
Fig. 1 Bayesian inference cladogram of vertebrate aquaporins based on 394 aligned amino acid positions. Filled bullets on nodes denote support for both BI and ML methods of phylogenetic inference. Open bullets on nodes denote support for only one of the methods (either BI or ML). Absence of bullet on a node denotes no support for any of the methods. Aquaporin classes are indicated with colour panels and class paralogs
ScienceDex guides
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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
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.