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4,489 results for “transit”

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zenodo36/100

MetForTC-Examples of phase transition plateau measurements of the new Sn miniature cells- 2023-07-27

<p>The data presents the characterization of the prototype of the Sn fixed-point mini-cell and the associated reference thermocouple type SThe cells was utilised for the experimental characterisation for drift under different thermal conditions in three zone furnaces and dry-block calibrators., which was made by TUBITAK and measured by Lab1,Lab2 and Lab3.</p>

opencc-by-4.0Jul 2023View details →
zenodo36/100

Eccentricity signal in the nannofossil time-series across the Middle Pleistocene Transition in the Northwestern Pacific Ocean

<p>Supplementary data to the paper &quot;Eccentricity signal in the nannofossil time-series across the Middle Pleistocene Transition in the Northwestern Pacific Ocean&quot; of Bordiga et al 2023 in Quaternary Science Reviews.</p>

opencc-by-4.0Jul 2023View details →
zenodo36/100

Liquid-hexatic transition for soft disks

<p>This dataset provides data files for the equation of state and equilibrium configurations of soft-disk models&nbsp;used in <a href="https://journals.aps.org/pre/abstract/10.1103/PhysRevE.108.024103">&quot;Liquid-hexatic transition for soft disks&quot; Physical Review E <strong>108</strong>, 024103 (2023) by&nbsp;Yoshihiko Nishikawa, Werner Krauth, and A. C. Maggs.</a>&nbsp;</p> <p>The following directories are included.</p> <p>- equation_of_state: This directory includes two CSV files for the equation of state plotted in the paper.&nbsp;<br> - equilibrium_configuration: This directory includes equilibrium configurations of N = 1024^2 particles of the models studied in the paper. An equilibrium configuration is stored in start.h5, a HDF5 file, together with the parameters for the simulation. By using the CUDA code available at <a href="https://github.com/jellyfysh/SoftDisks">https://github.com/jellyfysh/SoftDisks</a>, you can perform an equilibrium simulation starting from the configuration stored in start.h5.</p>

opencc-by-4.0Jul 2023View details →
zenodo36/100

Ca2+ imaging data for: A rigidity transition of MEC-2/Stomatin condensates controls neuronal mechanotransduction during touch sensing

<p>Calcium imaging data from Sanfeliu et al, NCB, 2023.</p> <p>Project contains fluorescence data to characterize the activity of the touch receptor neurons (TRNs) - which are mechanically activated upon touch &ndash; in the model organism <em>Caenorhabditis elegans</em>. The set of data includes wild-type animals as a reference and two different mutants to understand their role during touch sensation: MEC-2(R385H) and UNC-89 knock-out.</p> <p>&nbsp;</p>

opencc-by-4.0Jul 2023View details →
dryad36/100

Data from: Comparison of carbon and nitrogen accumulation rate between bog and fen phases in a pristine peatland with the fen-bog transition

<p>Long-term carbon and nitrogen dynamics in boreal peatlands are affected by both vegetation production and decomposition processes. Here, we examined the carbon accumulation rate (CAR), nitrogen accumulation rate (NAR) and δ<sup>13</sup>C, δ<sup>15</sup>N of plant residuals in a peat core dated back to ~8500 cal yr BP in a temperate peatland in Northeast China. Impacted by the tephra during 1160 and 789 cal yr BP and climate change, the peatland changed from a fen dominated by vascular plants to a bog dominated by <em>Sphagnum mosses</em>. We used the Clymo model to quantify peat addition rate and decay constant for acrotelm and catotelm layers during both bog and fen phases. Our studied peatland was dominated by <em>Sphagnum fuscum</em> during the bog phase (789 ~ -59 cal yr BP) and lower accumulation rates for the upper sections in the acrotelm layer during this phase, suggesting the dominant role of volcanic eruption in the CAR of the peat core. Both mean CAR and NAR were higher during the bog phase than during the fen phase in our study, consistent with the results of the only one similar study in the literature. Because the input rate of organic matter was considered to be lower during the bog phase, the decomposition process must have been much lower during the bog phase than during the fen phase and potentially controlled CAR and NAR. During the fen phase, CAR was also lower under higher temperature and summer insolation, conditions beneficial for decomposition. δ<sup>15</sup>N of <em>Sphagnum </em>hinted that nitrogen fixation had positive effect on nitrogen accumulation, particular in recent decades. Our study suggested that decomposition is more important for carbon and nitrogen sequestration than production in peatlands in most conditions and if future climate changes or human disturbance increase decomposition rate, carbon sequestration in peatlands will be jeopardized.</p>

opencc-zeroAug 2023View details →
zenodo36/100

Role of breakage, melt and floe size distribution on sea ice summer transition

<p>Marginal ice zones are composed of individual sea ice floes, whose breakage and melt determine its summer behavior. These processes are not well represented by global or regional climate models due to the continuum approximations used for sea ice. Here, we use a Discrete Element Model (DEM) coupled to a slab thermodynamic ocean to investigate how breakage and melt processes impact the decay of summer sea ice. The DEM is calibrated using MODIS satellite imagery and reanalysis data within the Arctic Ocean&rsquo;s Baffin Bay during June-July 2018. The sensitivity of the sea ice decay is evaluated by varying the solar heating, ice/ocean heat exchange parameter, and a prescribed floe breakage rate. For the parameter regime that best fits observations, the ratios of mass loss of resolved floes (&gt;2 km) due to breakage versus melt is 0.47, and oceanic versus solar melt is 0.46. The rate at which resolved floes lose mass is most sensitive to the breakage rate, as compared to the solar and oceanic melt parameters. The number decay of the largest floes (&gt;21 km) is controlled by breakage, while decay of smaller floes (2 - 21 km) depends strongly on lateral melt. Inferences from this exploration of parameter space may help develop more accurate parameterizations of the floe size distribution evolution in climate models.</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

Sawtooth lattice multiferroic BeCr2O4: Noncollinear magnetic structure and multiple magnetic transitions

<p>Data sets for original figures in the article &#39;Sawtooth lattice multiferroic BeCr<sub>2</sub>O<sub>4</sub>: Noncollinear magnetic structure and multiple magnetic transitions&#39; published in <a href="https://doi.org/10.1103/PhysRevMaterials.7.024422">Physical Review Materials <strong>7</strong>, 024422 (2023)</a>. The file name of each xls file corresponds to the figure number in the published article. The files can be opened using the Excel program. If there are sub-figures, or multiple frames in each figure, the data of each sub-figure is stored in separate sheets within one xls file. The files with the file extension &#39;vesta&#39; can be opened using the freely available program <a href="https://jp-minerals.org/vesta/en/">VESTA</a>.</p>

opencc-by-4.0Feb 2023View details →
zenodo36/100

LES data presented in "The role of passive cloud volumes in the transition from shallow to deep atmospheric convection"

<p>This repository contains the LES data presented&nbsp;in the manuscript entitled &quot;The role of passive&nbsp;cloud volumes&nbsp;in the transition from shallow to deep atmospheric convection&quot; by C.V. Vraciu, I.L. Kruse, J.O. Haerter, submitted to the Geophysical Research Letters.</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

Data for the publication "Sensitivity of Banner Cloud Formation to Orography and the Ambient Atmosphere: Transition From Idealized to More Realistic Scenarios"

<p>Data accompanying the paper titled:&nbsp;&quot;Sensitivity of Banner Cloud Formation to Orography and the Ambient Atmosphere: Transition From Idealized to More Realistic Scenarios&quot;</p> <p>This repository contains output statistics for thirty simulations run with the EULAG model in LES mode (Prusa et al., 2008).</p> <p>We use three distinct configurations of the model domain and its orography, ranging from highly idealized to fully realistic. The configuration with realistic orography is referred to as &ldquo;Matt_Ref&rdquo; and covers a domain of 12.8 x 9.6 x 7 km. As our intermediate configuration, we use the realistic orography from the Matterhorn summit protruding from a flat plain, referred to as &quot;Matt_Iso&quot;. As our highly idealized configuration we consider a Pyramid protruding from a flat plain, referred to as &quot;Pyr&quot;. In both configurations the model domain extends 11.6 x 9.2 x 4.5 km. The simulations of all three configurations are performed with an isotropic grid spacing of 25 m.<br> <br> Each zip-file contains the time-averaged fields of six simulations with inflow conditions of a sheared or constant wind profile with 5, 10 and 20 m/s, and neutral stratification up to the height of the mountain summit. For the &quot;Matt_Ref&quot; configuration exists two additional zip-files containing data of a neutral stratification up to 500 meter and 800 meter below the mountain summit. Moreover, for the &quot;Matt_Ref&quot; configuration exists three additional zip-files containing the time-averaged turbulent fields. For more details have a look at the paper.</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

Data and code for: The genetic architecture of a recent transition to live-bearing in marine snails

<p>This repository contains the code and VCF files needed to conduct the analyses in our MS. Each folder contains a readMe document explaining the nature of each file and&nbsp;dataset and the results and analyses that they relate to. The same anlaysis code (but not VCF files) is&nbsp;also available at&nbsp;https://github.com/seanstankowski/Littorina_reproductive_mode</p>

opencc-by-4.0Sep 2023View details →
zenodo36/100

Shape functions and Integration quadrature of nine 3D transition elements

<p>This file houses the text files and Matlab function files that contain the shape functions and integration quadrature of nine 3D transition elements. The Matlab function file also computes the Shape function gradient matrix that can be readily used for FE applications.</p>

opencc-by-4.0Sep 2023View details →
zenodo36/100

Multiple evolutionary transitions of reproductive strategies in a phylum of aquatic colonial invertebrates

<p><strong>PHYLOGENIES</strong></p> <p><strong>All_genes_alignment.nex</strong></p> <p>The concatenated mixed alignment consisting of, 13 mitochondrial protein-coding genes as amino acids, mitochondrial ribosomal RNA genes 12S+16S, and nuclear 18S+28S rRNA genes. Gene boundaries and excludes sites are indicated.</p> <p><strong>Fig_2.nex</strong></p> <p>Topology of the Bayesian phylogenetic analysis of the mixed concatenated alignment consisting of three partitions: (i) 13 mitochondrial protein-coding genes as amino acids, (ii) mitochondrial ribosomal RNA genes 12S+16S, (iii) nuclear 18S+28S rRNA genes. The analysis was performed in MrBayes5D v. 3.2.6 under the GTR+G model of nucleotide evolution (nucleotides) and the MTZOA+G model (amino acids). The analysis was run for 2.4 million generations; 1.5 million generations were discarded as burn-in.</p> <p><strong>Fig_S3</strong></p> <p>Topology of the Bayesian phylogenetic analysis of the mixed concatenated alignment consisting of three partitions: (i) 13 mitochondrial protein-coding genes (PCGs) as amino acids, (ii) mitochondrial ribosomal RNA genes 12S+16S, (iii) nuclear 18S+28S rRNA genes. The analysis was performed in p4 under the GTR+G model of nucleotide evolution (nucleotides) and the MTZOA+G+F model (amino acids). The +F model component accommodates empirical composition in the amino acid model. The analysis used three separate runs for 300,000 generations; 200,000 generations were discarded as burn-in.</p> <p><strong>Fig_S4</strong></p> <p>Topology of the maximum likelihood phylogenetic analysis of the mixed concatenated alignment consisting of three partitions: (i) 13 mitochondrial protein-coding genes as amino acids, (ii) mitochondrial ribosomal RNA genes 12S+16S, (iii) nuclear 18S+28S rRNA genes. The analysis was performed in RAxML HPC-PTHREADS-SSE3 v. 8.2.12 under the GTR+G (nucleotides) and the MTZOA+G+F models (amino acids).</p> <p><strong>Fig_S5</strong></p> <p>Topology of the Bayesian phylogenetic analysis of the 12S+16S rRNA gene partition constructed using MrBayes v. 3.2.6 under the GTR + G model. The analysis was run for 20 million generations; 10 million generations were discarded as burn-in.</p> <p><strong>Fig_S6</strong></p> <p>Topology of the maximum likelihood phylogenetic analysis of the 12S+16S rRNA gene partition constructed using RAxML HPC-PTHREADS-SSE3 v. 8.2.12 under the GTRCAT model.</p> <p><strong>Fig_S7</strong></p> <p>Topology of the Bayesian phylogenetic analysis of the 18S+28S rRNA gene partition constructed using MrBayes v. 3.2.6 under the GTR + G model. The analysis was run for 20 million generations; 10 million generations were discarded as burn-in.</p> <p><strong>Fig_S8</strong></p> <p>Topology of the maximum likelihood phylogenetic analysis of the 18S+28S rRNA gene partition constructed using RAxML HPC-PTHREADS-SSE3 v. 8.2.12 under the GTRCAT model.</p> <p><strong>Fig_S9</strong></p> <p>Topology of the Bayesian phylogenetic analysis of 13 mitochondrial protein-coding genes as amino acids constructed using MrBayes5D v. 3.2.6 under the MTZOA+G model. The analysis was run for 3.7 million generations; 2.5 million generations were discarded as burn-in.</p> <p><strong>Fig_S10</strong></p> <p>Topology of the maximum likelihood phylogenetic analysis of 13 mitochondrial protein-coding genes as amino acids constructed using RAxML HPC-PTHREADS-SSE3 v. 8.2.12 under the PROTGAMMAMTZOA model.</p> <p><strong>Fig_S11</strong></p> <p>Topology of the Bayesian phylogenetic analysis of the mixed concatenated alignment consisting of three partitions: (i) 13 mitochondrial protein-coding genes (PCGs) as amino acids, (ii) mitochondrial ribosomal RNA genes 12S+16S, (iii) nuclear 18S+28S rRNA genes. The analysis was performed in p4 under the NDCH-C2 model. The analysis used four separate runs for 300,000 generations; 200,000 generations were discarded as burn-in. The NDCH model accommodates compositional tree-heterogeneity and was used because there was a large amount of compositional heterogeneity over the sequences, especially in the PCGs and 12S+16S rRNA data partitions. This is an NDCH model with two composition vectors on each of the three data partitions.</p> <p><strong>Fig_S12</strong></p> <p>Topology of the Bayesian phylogenetic analysis of the mixed concatenated alignment consisting of three partitions: (i) 13 mitochondrial protein-coding genes as amino acids, (ii) mitochondrial ribosomal RNA genes 12S+16S, (iii) nuclear 18S+28S rRNA genes. This analysis excluded all terminals for which less than half of mitogenome genes were available, or which only had one of the two nuclear rRNA genes. The analysis was performed in MrBayes5D v. 3.2.6 under the GTR+G model of nucleotide evolution (nucleotides) and the MTZOA+G model (amino acids). The analysis was run for 350,000 generations; 125,000 generations were discarded as burn-in.</p> <p><strong>Fig_S13</strong></p> <p>Topology of the maximum likelihood phylogenetic analysis of the mixed concatenated alignment consisting of three partitions: (i) 13 mitochondrial protein-coding genes as amino acids, (ii) mitochondrial ribosomal RNA genes 12S+16S, (iii) nuclear 18S+28S rRNA genes. This analysis excluded all terminals for which less than half of mitogenome genes were available, or which only had one of the two nuclear rRNA genes. The analysis was performed in RAxML HPC-PTHREADS-SSE3 v. 8.2.12 under the GTR+G (nucleotides) and the MTZOA+G+F models (amino acids).</p> <p><strong>ANCESTRAL CHARACTER ESTIMATION:</strong></p> <p><strong>ACE.R</strong></p> <p>R script of the ancestral character estimation carried out in phytools.</p> <p><strong>Reproductive_strategy_numbers.csv</strong></p> <p>Data input file for ACE analysis (reproductive strategies coded as numbers)</p> <p><strong>Reproductive_strategies.xlsx</strong></p> <p>List of reproductive strategies per taxon with the corresponding numerical codes used in the file &#39;Reproductive_stategies_numbers.csv&#39;.</p> <p><strong>Tree.tre</strong></p> <p>Input tree for ACE analysis.</p>

opencc-by-4.0Jun 2023View details →
dryad36/100

Transit agencies want open payments but there are challenges

<p>This study explores interest in, and the challenges faced by transit agencies and operators in the adoption of open-loop payment systems. The research team focuses in particular on the ways that agencies view passenger needs in the context of adopting open payments. Challenges with cash payments, an increasingly cashless society, and the expanding offerings of digital payment options have spurred increased interest in open-loop payments among transit operators. Paying for transit with cash can require additional time at boarding, add extra steps for passengers who must pay with exact fare, and result in service inefficiencies. It presents security concerns for drivers, and administrative burdens for agencies. While the full costs of cash handling vary per agency the cost of handling and moving cash may be considerable. Pioneering transit agencies are adopting open payment systems that accept credit cards, debit cards, and smartphone/watch-based transactions. However, there is a huge diversity among transit agencies and as such, agencies face different challenges and to different degrees, when considering the adoption of open payment systems. Challenges can include financial barriers, capacity limitations, technological challenges, the duration of existing contracts, competing needs, and a number of passenger challenges such as lack of credit cards or smartphones. This study uses data collected from California transit agencies in the fall of 2022 that gathered information about agency perceptions of open-loop payments and the challenges with adopting open fare collection systems, and whether assistance programs would benefit transit agencies interested in adopting open-loop payments. Even before the pandemic prompted agencies to consider open and contactless payments, many agencies were exploring this option. Results of the present study indicate that the majority of agencies are considering or have considered implementing open payment systems, but agencies are not fully aware of the assistance available from the California Integrated Travel Program to help in the transition to digital and open payment systems. Key challenges include the cost, as well as the technical needs to implement open payments. Agencies also cited passenger familiarity with technology and ability to have a bank account as potential hurdles. This study sheds light on the challenges facing small to medium transit agencies in the transition of California's transit systems to open-loop payment systems.</p>

opencc-zeroOct 2023View details →
zenodo36/100

Data sets for "Dynamical bulk-boundary correspondence and dynamical quantum phase transitions in higher-order topological insulators"

<p>Data sets for the return rates and Loschmidt eigenvalues for the paper &quot;Dynamical bulk-boundary correspondence and dynamical quantum phase transitions in higher-order topological insulators&quot;. Included are data for both bulk calculations and finite open systems labelled OBC. Data files are named with&nbsp;the quench parameters, see the article for details.</p>

opencc-by-4.0Oct 2023View details →
zenodo36/100

TimeFISH: Long-term assessment of reef fish assemblages in a transition zone in the Southwestern Atlantic

<p>The TimeFish database provides the first public time-series dataset on reef fish assemblages in the Southwestern Atlantic (SWA), comprising 15 years of data (2007-2022) based on standardized Underwater Visual Censuses (UVCs). The rocky reefs covered by our dataset are influenced by pronounced seasonal cycles of ocean temperatures with warm tropical waters from the Brazil Current in the summer (~27&deg;C) and colder waters from the La Plata River Plume discharge and upwelling from the South Atlantic Central Water in the winter (~18&deg;C). These oceanographic conditions characterize this area as the southernmost tropical-subtropical climatic transition zone in the Atlantic Ocean. As a result, reef fish assemblages comprise both tropical and subtropical species. All records included in TimeFish were collected using UVCs, a non-destructive method that allows the estimation of fish species richness, abundance, and body size distributions. UVCs were performed through 40 m2 belt transects by scuba diving in nine locations along the southern Brazilian coast (25&deg;S &ndash; 29&deg;S). Four of these locations lie within the boundaries of the no-entry Arvoredo Marine Biological Reserve, where fishing and recreational activities are forbidden, and the remaining locations are unprotected from these activities. During each belt transect, a diver swam at a constant depth above and parallel to the reef, identifying fish species, counting the number of individuals, and estimating the total body length (Lt in cm) of all detected individuals. All fish individuals in the water column (up to 2 m above the substratum) and at the bottom were targeted. A total of 202,965 individuals belonging to 163 reef fish species and 53 families were recorded across 1,857 UVCs. All survey campaigns were funded by either public or mixed capital (private-public) sources, including seven grants from the Brazilian federal and Santa Catarina state government. Part of the data have already been used in multiple MSc and Ph.D. theses and scientific articles. TimeFISH represents an important contribution for future studies aiming to examine temporal and spatial variations of reef fish assemblages in transition zones. No copyright restrictions apply to the use of this data set, other than citing this publication.</p>

opencc-by-4.0Dec 2022View details →
zenodo36/100

Double Trouble (GJ 1132b JWST Transits NIRSpec G395H) — Supplementary Material

<p>Supplementary&nbsp;material for '<i>Double Trouble: Two Transits of the Super-Earth GJ 1132 b Observed with JWST NIRSpec G395H</i>'&nbsp;by&nbsp;May &amp; MacDonald et al., ApJL&nbsp;(2023).</p><p>This repository contains four categories of data products:</p><ol><li><strong>Data reduction reproduction</strong> — Eureka! control files (.ecf) and parameter files (.epf) alongside saved Stage 3 output for both G395H visits. These allow replication of our data reduction, light curve fitting, and transmission spectra extraction using the <a href="https://github.com/kevin218/Eureka">open-source code Eureka</a>!</li><li><strong>Transmission spectra</strong> — Reduced transmission spectra from three data reduction codes (Eureka!, FIREFLy, and ExoTiC-JEDI) for both G395H visits.</li><li><strong>Stellar spectra </strong>— Flux calibrated observed stellar spectra of GJ 1132 from each G395H visit.</li><li><strong>Retrievals</strong> — Corner plots and parameter statistics summaries from atmospheric and stellar contamination retrievals applied to both G395H visits (Eureka! reduction). The retrievals used the <a href="https://github.com/MartianColonist/POSEIDON">open-source code POSEIDON</a>.</li></ol><p>For any additional data requests or questions, please contact: ryanjmac@umich.edu</p>

opencc-by-4.0Oct 2023View details →
zenodo36/100

The origin of granitoids in Southwest Japan: Implications for the transition from Pacific to Philippine Sea plate subduction

<p>Data for the research entitled <strong>"The origin of granitoids in Southwest Japan: Implications for the transition from Pacific to Philippine Sea plate subduction" </strong>by<strong> </strong>Dao et al., submitted to JP.</p> <p><strong>Table&nbsp;S1:</strong>&nbsp;Geochemical data of plutonic rocks in Southwest Japan: (1) Ryoke belt; (2) Sanyo belt; (3) Sanin belt.</p> <p><strong>Table&nbsp;S2:</strong> Petrographic observation: (1) Modal abundances; (2) Mineral assemblages.</p> <p><strong>Table&nbsp;S3:</strong> Zircon U-Pb ages (Ma) of plutonic rocks in SW Japan from this study.</p> <p><strong>Table&nbsp;S4:</strong> Compilation of age data for Cretaceous-Paleogene igneous rocks in SW Japan.</p> <p><strong>Table&nbsp;S5:</strong> Geochemical data of plutonic rocks in SW Japan compiled by Haraguchi et al. (2018).</p> <p><strong>Table&nbsp;S6:</strong> Compilation of Sr-Nd isotope data of ~110 Ma to ~20 Ma plutonic rocks in SW Japan.</p> <p><strong>Table&nbsp;S7:</strong> CIPW normative compositions of SW-Japan granitoids from this study.</p> <p><strong>Table&nbsp;S8:</strong> End-member components used to estimate sediment contributions.</p> <p><strong>Table&nbsp;S9: </strong>Results of sediment contribution estimations.</p>

opencc-by-4.0Oct 2023View details →
ClinicalTrials.gov36/100

Advocating for Supports to Improve Service Transitions

ClinicalTrials.gov study NCT04173663. IPD Sharing: NO. Countries: 1. Publications: 6.

closedIPD-NOFeb 2026View details →
ClinicalTrials.gov36/100

Group Education Trial to Improve Transition in Type 1 Diabetes

ClinicalTrials.gov study NCT03703440. IPD Sharing: YES. Countries: 1. Publications: 13.

controlledIPD-YESFeb 2026View details →
ClinicalTrials.gov36/100

3D-Transition: Challenges and Resources of Children and Their Families During the Transition From Preschool to School

ClinicalTrials.gov study NCT04873518. IPD Sharing: YES. Countries: 1. Publications: 3.

controlledIPD-YESFeb 2026View details →

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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.

allen-brain-atlas
neuroscienceopenDocumentation, web resources, and API references are available online.
Last verified 2026-04-30Open record

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.

abode-home-cage
behavioral-neuroscienceopenThe DataShare record exposes download links for annotations, documentation, license text, and the zipped per-snippet data directory.
Last verified 2026-04-30Open record

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.

dandi-nwb
electrophysiologyopenPublished Dandiset metadata and archive endpoints are available through the production DANDI API.
Last verified 2026-04-30Open record

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.

ibl
behavioral-neuroscienceopenPublic sessions can be searched and loaded from the IBL public data server through ONE.
Last verified 2026-04-29Open record

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.

openneuro
neuroscienceopenPublished datasets are available on demand over the internet.
Last verified 2026-04-29Open record

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