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Figure 5 from: Serafim-Júnior M, Perbiche-Neves G, Lansac-Toha F (2019) Environments and macrophytes as main variables controlling rotifers in a river/lake system before Porto Primavera Reservoir construction. Zoologia 36: 1-8. https://doi.org/10.3897/zoologia.36.e24191
Figure 5 Comparison of mean values of total abundance, Shannon-Wiener diversity and evenness among the sampling sites.
Effects of the electrostatic environment on superlattice Majorana nanowires (dataset)
<p><strong>Description</strong></p> <p>This repository contains the dataset required to reproduce all the figures of the article "Samuel D. Escribano, Alfredo Levy Yeyati, Yuval Oreg, and Elsa Prada,<em> Effects of the electrostatic environment on superlattice Majorana nanowires</em>, arXiv:1904.10289 (2019)".</p> <p> </p> <p><strong>Structure of the dataset</strong></p> <p>All the data is saved in Matlab file-format .mat. Their file names correspond to the figure that they plot. Together with each dataset, there is a Python script .py which plots the corresponding figure. The output of every script is the corresponding figure in PDF-format .pdf. Please, read "reedme.txt" file for further information.</p> <p><br> </p>
Data for "Individual, but not population asymmetries, are modulated by social environment and genotype in Drosophila melanogaster"
<p>Dataset and scripts for the manuscript: "Individual, but not population asymmetries, are modulated by social environment and genotype in <em>Drosophila melanogaster". </em>We upload:</p> <p>1.Data. This directory contains the raw tracking data used for the analysis and the calibration files required by Flytracker for each strain of the Drosophila Genetic Reference Panel (RAL-69, RAL-136, RAL-338, RAL-535, RAL-796).<br> The format of the dataset consists in the output of tracking the (x,y) position and related features (e.g. velocity, distance) of flies in a circular arena using the software Flytracker - http://www.vision.caltech.edu/Tools/FlyTracker/ - For each video we have a trak.mat file and a feat.mat file. For instance, for a video in which we tracked the DGRP line RAL-136 (d338), with a pair of males (mm), trial 3 (t5) we had as outputs d338mmt5joined-feat.mat and d338mmt5joined-track.mat . You can find the description of the output here: http://www.vision.caltech.edu/Tools/FlyTracker/documentation.html</p> <p>2.Load_data _and_circling_scripts. This directory contains a MATLAB file with the instructions on how to load datasets and how to compute the circling index.</p> <p>3.Heatmap. This directory contains the instructions (readme_heatmap.txt) and scripts to (a) fix a bug in the feat files ouput by Flytracker using the calibration files and the script feat_compute_revised.m (b) plot the heatmap of the position and distance between partner flies in a dyad.</p>
Spatiotemporal air environment degradation and improvement in China from 2000 to 2017
<p>The uploaded files are original data we used to analyze the PM2.5 concentration in China.</p>
Characterization of Natural Production Environment of Ogaden Cattle Breed in Wabeshebele zone of Somali Regional State in Ethiopia
<p>The objective of the study was to characterize natural production environment of Ogaden cattle breed. Questionnaire used for the study was designed using the general information developed by FAO (2012). 3 districts and 6 kebeles were purposely and 126 cattle keepers were randomly selected for data collection. The studied variables were farming, cattle breeding practice, purpose of keeping, selection criteria, feeding, health care and veterinary service, income and non-income function, and cattle production constraints. SAS version 9.2, 2008 software was used for data analysis. 30.16% were pastoral while 69.84% were agro-pastoral. Significant difference seen between districts in crop land holding, but no significant difference between districts in forage land holding. Cattle keepers prefer to keep local Ogaden cattle breed and were practicing pure breeding. Majority of them do not produce adequate pasture. They treat diseased animals by traditional method (57.94%). Male cattle were kept for socio-cultural purpose whilst female cattle were kept for milk production. None of the agro-pastoral respondents have recalled that they use draught power and manure of cattle. Cow milk in the study area has taken the first line consumed by the livestock owners and generating daily income for their family need among other livestock products making cattle the most important livestock species. Prolonged feed shortage was the first cattle production constraint. The cattle keeping society in the studied area appeared to have distinct culture and tradition of keeping and utilization cattle.</p>
Figure 11 in Scopaeus saotomensis spec. nov., a flightless rove beetle from the Island of São Tomé (Coleoptera: Staphylinidae: Paederinae: Lathrobiini) - Isolation and adaptation in a dark, humid, tropical forest environment
Figure 11. The pitfall trap (arrow) in situ at Lagoa Amélia illustrating the exact collecting spot for Scopaeus saotomensis.
Fig. 2. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 2. a – age model and AMS radiocarbon ages for Cores FC WH and CADIAC WH; b – X-Ray photograph of Core CADIAC WH and grain-size parameters.
Fig. 3 in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 3. Benthic foraminiferal fauna characteristics of Core FC WH: a – densities of the main (> 5% in at least one sample) living benthic foraminifera (ind. 50 cm–3 of wet sediment); b – species richness of the living benthic fauna; c – densities of the main (> 5% in at least one sample) dead benthic foraminiferal species (ind. 50 cm–3 of wet sediment); d – species richness of the dead benthic fauna.
Fig. 11 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 11 Microfossils from the limestone pebbles of the Aptian breccia and conglomerates outcropping in the Drumul lui Lehman section. a, b, e, f?Banatocodium sp. c Salpingoporella pygmaea (Gümbel). d?Pseudocymopolia jurassica Dragastan. g?Nipponophycus sp. h Pseudocyclamina lituus (Yokoyama). i?Everticyclamina sp. j Unidentified agglutinated foraminifer. k Gaudryina sp. l, w?Nautiloculina sp. m, n, o?Vercorsella sp. p Coscinoconus delphinensis (Arnaud-Vanneau, Boiseau & Darsac). q?Arenobulimina sp. r Pfenderina neocomiensis (Pfender). s Mohlerina basiliensis (Mohler). t, u Protopeneroplis ultragranulata (Gorbatchik). v Scythiolina camposauri (Sartoni & Crescenti). x Paracoskinolina? jourdanensis (Foury & Moullade). y Unidentified?involutinid foraminifer. a-f, m, j, o, s, t, u, sample 618; g, sample 597; h, x, sample 604; i, sample 588; k, sample 626; l, sample 613; n, sample 563; p, sample 589; q, r, sample 558; v, sample 564; w, sample 600; y, sample 594. Scale bar = 1mm (e, g, h, p); 0.5 mm (a, b, d, f, i, j, k, q, s, x, y);
Fig. 2 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 2 Geological cross-section through the northern part of Piatra Craiului Massif and Bran Pass (after Jekelius, 1938, redrawn with minor changes).
Fig. 4 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 4 Stratigraphic logs of the A Padinile Frumoase succession; and the B Drumul lui Lehman succession. Legend: 1, massive limestone; 2, marly limestone; 3, allodapic limestone; 4, breccia; 5, conglomerate; ES, erosional surface; GRPC, Gura Râului Paraconglomerates; MB, monomictic breccia; MOC, monomictic orthoconglomerate; MPC, monomictic paraconglomerate; U, unconformity. M, W, P, G, R = mudstone, wackestone, packstone, grainstone, rudstone in Dunham's (1962) limestone classification. ristic for the Berriasian-Valanginian and Barremian- Steinmann (Fig. 8n), Carpathoporella occidentalis Aptian intervals. The Berriasian-Valanginian pebbles Dragastan (Fig. 8p), Coscinophragma cribrosa (Reuss) consist of a wide range of microfacies such as fenestral (Fig. 8s), and Lithocodium aggregatum Elliott (Fig. 8r). mudstone, peloidal bioclastic packstone or peloidal The limestone fragments-bearing monomictic breccia are bioclastic packstone/grainstone. The microfollowed by monomictic conglomerates, similarly rich in paleontological assemblage contains foraminifera limestone pebbles (Fig. 3c-e). Microfacies and [Ammobaculites sp., Montsalevia salevensis (Charollais, micropaleontological analysis has shown that, similar Brönnimann & Zaninetti) (Fig. 8), Meandrospira sp., with the breccia components, the most important Protopeneroplis ultragranulata (Gorbatchik), Pfenderina microfacies and microfossils of the pebbles are character- neocomiensis (Pfender)] and dasycladalean algae.
Fig. 1 in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments
Fig. 1 Geological map of Borod Basin (redrawn after Popa, 1981). Legend: 1 Magmatic rocks; 2 Metamorphic rocks; 3 Triassic; 4 Jurassic; 5 Upper Cretaceous; 6 Miocene; 7 Quaternary; 8 Location of studied area.
Fig. 3 a, b in Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments
Fig. 3 a, b The first rudist bearing lithosome from Cioroi-Negru Brook; c, d Rudists and rudist fragments visible in this outcrop; e The second rudist-bearing lithosome; f Rudists of the second lithesome. Yellow arrows represent scale bars.
Fig. 16 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 16 Limestones from the Padina Brașoavei outcrop (Urdărița horst). a Limestones from the lower part of the succession [(the yellow arrows indicates the first brecciated level (with green-greyish matrix), while the red arrows indicate the second, black pebble bearing brecciated level]. b Well-bedded limestones from the upper part of the succession. c, d Fine laminated fenestral limestones from the lower part (c) and the upper part (d) of the succession. e The first brecciated level, with green-greyish matrix. f Black pebble-bearing level.
Fig. 2 Reefal facies. a-c in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 2 Reefal facies. a-c Coral-microbial boundstone; coral colonies are heavily encrusted by problematic microorganisms (a) or bordered by syndepositional, radiaxial-fibrous cements (b). d-h Bioclastic packstone (d, e, g-h) and bioclastic grainstone (f) internal sediment with dasycladalean algae [Steinmanniporella kapelensis (Sokač & Nikler)] (d), sponges (e), mollusks, corals, Crescentiella (f), microstalactitic (g) and microthrombolitic (h) microbial crusts.
Fig. 14 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 14 Micro-cycles within supratidal carbonates. Alternations of fractured fenestral non-fossiliferous mudstone and ostracod-bearing mudstone; horizontal, oblique and vertical cracks are present within the non-fossiliferous levels (1); fractured cavities contain vadose silt; storm deposits (2) and pond type facies (ostracod-bearing mudstone) (3).
Fig. 10 Intertidal limestones. a in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 10 Intertidal limestones. a Fine laminated peloidal grainstone; well-sorted limestones with frequent ripples (1) and horizontal or small-scale oblique laminations (2). b Subaerially exposed fenestral peloidal-bioclastic grainstone with vadose microstalactitic cement (arrowed).
Fig. 18 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 18 Main microfossils from the Cheile Dămbovicioarei Formation. a Bramkampella arabica; b Selliporella neocomiensis; c Pseudocymopolia jurassica; d Salpingoporella praturloni; e, f Haplophragmoides joukowskyi; g Montsalevia salevensis; h Scythiolina sp.; i Pseudotextulariella courtionensis; j Coscinoconus cherchiae; k Coscinoconus cf. perconigi; l Coscinoconus cf. campanellus; m Danubiella gracilima; n, o Paracoskinolina? jourdanensis; p Protopeneroplis ultragranulata; q Thaumatoporella parvovesiculifera. Scale-bar = 0.25 mm (a-c, e-q); 0.50 mm (d).
Fig. 13 Supratidal limestones. a in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 13 Supratidal limestones. a Fenestral muds with horizontal, vertical and oblique desiccation cracks. The horizontal cracks are parallel with the lamination while the upper part of the cracks is filled with vadose silt (arrow). b, c Pedogenetically modified supratidal limestones. Fractured fenestral mudstone (b, c); it contains horizontal, oblique and vertical cracks; c, detail of b; cavities are filled by micro-stalactitic and meniscus cements which from vadoid crusts (arrows 1); the lower part of the cavities contains vadose silt (arrow 2).
Fig. 1 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 1 Location of the Cheile Dâmbovicioarei within the Dâmbovicioara Area. a Location of the Dâmbovicioara zone on the Romanian map; b Location of the sampled profile on the geological map 1:50000 (redrawn from Dimitrescu et al., 1971 and Patrulius et al., 1971).
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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.