cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.5767002
title: burrowdensityall.dbf

description: Burrow density information from a study using drones to take aerial photographs and count the burrows from these photographs.
DOI: 10.6084/m9.figshare.5767002.v1
title: burrowdensityall.dbf

description: Burrow density information from a study using drones to take aerial photographs and count the burrows from these photographs.
DOI: 10.6084/m9.figshare.5766885
title: Plot corners

description: Coordinates of the plot corners
DOI: 10.6084/m9.figshare.5766885.v1
title: Plot corners

description: Coordinates of the plot corners
DOI: 10.6084/m9.figshare.5766882
title: Stem analysis of single trees

description: Stem analysis measurements of single trees
DOI: 10.6084/m9.figshare.5766882.v1
title: Stem analysis of single trees

description: Stem analysis measurements of single trees
DOI: 10.6084/m9.figshare.5766879
title: Stem diameter measured along the trunk

description: Stem diameter measured along the trunk
DOI: 10.6084/m9.figshare.5766879.v1
title: Stem diameter measured along the trunk

description: Stem diameter measured along the trunk
DOI: 10.6084/m9.figshare.5766876
title: Ring width from stem analysis

description: Ring width from stem analysis
DOI: 10.6084/m9.figshare.5766876.v1
title: Ring width from stem analysis

description: Ring width from stem analysis
DOI: 10.6084/m9.figshare.5766873
title: Stem disc information for stem analysis

description: Stem disc information for stem analysis
DOI: 10.6084/m9.figshare.5766873.v1
title: Stem disc information for stem analysis

description: Stem disc information for stem analysis
DOI: 10.6084/m9.figshare.5766870
title: Tree positions

description: Tree positions
DOI: 10.6084/m9.figshare.5766870.v1
title: Tree positions

description: Tree positions
DOI: 10.6084/m9.figshare.5766864
title: plot area

description: plot area
DOI: 10.6084/m9.figshare.5766777
title: Extensive and objective wine color classification with chromatic database and mathematical models

description: Theoretic conjecture and mathematical models used for classifying wines into different chromatic levels were examined, based on a comprehensive chromatic database of 237 dry red wines. Similar mathematical models were also built for 79 Chinese Cabernet Sauvignon dry red wines from different regions and vintages, which could be set as chromatic reference for other Chinese Cabernet Sauvignon dry red wines. The reliability of these models and relationships between different chromatic parameters were further validated by statistical tools. Such methodology can be adopted to build chromatic references for wines from different backgrounds, thus to classify wine color more extensively and objectively.
DOI: 10.6084/m9.figshare.5766777.v1
title: Extensive and objective wine color classification with chromatic database and mathematical models

description: Theoretic conjecture and mathematical models used for classifying wines into different chromatic levels were examined, based on a comprehensive chromatic database of 237 dry red wines. Similar mathematical models were also built for 79 Chinese Cabernet Sauvignon dry red wines from different regions and vintages, which could be set as chromatic reference for other Chinese Cabernet Sauvignon dry red wines. The reliability of these models and relationships between different chromatic parameters were further validated by statistical tools. Such methodology can be adopted to build chromatic references for wines from different backgrounds, thus to classify wine color more extensively and objectively.
DOI: 10.6084/m9.figshare.5766708
title: Dataset for Figure 3

description: Simulated and experimentally measured net charge per acceleration of an optimized MEMS piezoelectric annular accelerometer for implantable hearing devices.In both files:Column 1 - Frequency [Hz]Column 4 - Net charge per acceleration [fC/(m/s²)]
DOI: 10.6084/m9.figshare.5766657
title: replication_data.xlsx

description: Vohs ego-depletion replication data from Hagger-Chatzisarantis lab
DOI: 10.6084/m9.figshare.5766657.v1
title: replication_data.xlsx

description: Vohs ego-depletion replication data from Hagger-Chatzisarantis lab
DOI: 10.4225/03/5a5376b442289
title: Wirasinha.migec.txt.zip

description: The file contains mouse T cell receptor (TCR) sequences collected by multiplex PCR amplification of cDNA molecules followed by Illumina sequencing. Sequences were aligned to the mouse genome using MIGEC software (see doi: 10.1038/nmeth.2960 for details). Except for the header row, each row contains information about a unique TCR nucleotide sequence. Columns 1-11 contain output from MIGEC software. Columns 12-16 contain information about sample origin, detailed as follows: column 12 "sample_id" is an identifier for the sample of origin; column 13 "tcr_b" specifies the TCR beta chain status of donor mouse ("poly" = C57BL/6 inbred mouse strain); column 14 "organ" specifies organ of origin (thymus, "gut" = small intestine and spleen); column 15 "subset" specifies the T cell subset of origin ("t_p" = pre-selection thymocytes; "t_1" = wave 1 thymocytes; "t_r" = thymic T-reg; "t_4" = CD4+ naive thymocytes; "t_8" = CD8+ naive thymocytes; "g8a" = small intestinal CD8aa+ intraepithelial lymphocytes; "s_r" = splenic T-reg; "s_4" = splenic CD4+ naive T cells and "s_8" = splenic CD8+ naive T cells); column 16 is identical to column 15 except that column 16 shows whether the sample of origin was a CD25+ or CD25– fraction of a thymic or splenic T-reg population.<br>
DOI: 10.6084/m9.figshare.5766570
title: Temporary Exhibitions at Tate Modern - 2008 to 2016

description: This dataset lists all temporary exhibitions held at London's Tate Modern from 2008 to those included as part of the 2016-17 season.<br>The main source for the actual exhibitions is the Tate’s Annual Reports (http://www.tate.org.uk/about-us/tate-reports) which have a specific section listing the temporary exhibitions held at Tate Modern, as well as St.Ives, Liverpool and Tate Britain. Further information is gained for the Tate Modern website.<br>A Google Sheets version is available for comment and analysis athttps://docs.google.com/spreadsheets/d/1Nu9WrMXIW8mW3aS1JAAQAuo8ARGGw0oEJMn9tE4E5aU/edit?usp=sharing<br>
DOI: 10.6084/m9.figshare.5766567
title: Petrogenesis and tectonic implications of Triassic A-type granites in southeastern China: insights from zircon U–Pb–Hf isotopic and whole-rock geochemical compositions of the Luoguyan and Guiyantou granites in northwestern Fujian Province

description: Triassic A-type granites in eastern South China Block (SCB) are abundant in the Wuyi–Yunkai tectonic domain and provide an important opportunity to explore the early Mesozoic evolution of continental crust of the SE part of the SCB. We carried out U–Pb zircon dating, Lu–Hf isotope analyses of zircon, and whole-rock geochemical analyses for two granitic plutons, the Guiyantou (GYT) and Luoguyan (LGY) granites, from northwestern Fujian Province. LA–ICP–MS U–Pb zircon analyses yielded ages of 232 ± 4 to 231 ± 7 Ma and 221 ± 5 Ma (Middle-Late Triassic) for the GYT and LGY granites. These two granites belong to metaluminous to weakly peraluminous high K calc-alkaline A-type granite that are enriched in K, Al, light rare earth element and Rb, Th, U, and Pb, and depleted in Nb, Ta, P, and Ti. Their rare earth element patterns are highly fractionated with (La/Yb)<i><sub>N</sub></i> ratios of 2–21 and strong negative Eu anomalies (Eu/Eu* = 0.02–0.31). <i>In situ</i> Hf isotopic analysis of zircon from the GYT and LGY granites yielded <i>ε</i><sub>Hf</sub>(<i>t</i>) values ranging from –11.5 to –1.1, with corresponding two-stage Hf model ages from 1.98 to 1.33 Ga, from which it is inferred that the GYT and LGY magmas formed by partial melting of Proterozoic metasedimentary rock in the Cathaysia block. The two granites were emplaced at 232 and 221 Ma and together with Triassic A-type granites in coastal region of the SCB, which is in agreement with an extensional tectonic setting in the Middle-Late Triassic. We suggest that the Middle-Late Triassic A-type granites in eastern SCB were probably formed in an intracontinental, post-orogenic extensional regime that collision was between the SCB and an ‘unknown block’ or the eastern extension of Indochina block.
DOI: 10.6084/m9.figshare.5766558
title: Tangled up in folds: tectonic significance of superimposed folding at the core of the Central Iberian curve (West Iberia)

description: The amalgamation of Pangea during the Carboniferous produced a winding mountain belt: the Variscan orogen of West Europe. In the Iberian Peninsula, this tortuous geometry is dominated by two major structures: the Cantabrian Orocline, to the north, and the Central Iberian curve (CIC) to the south. Here, we perform a detailed structural analysis of an area within the core of the CIC. This core was intensively deformed resulting in a corrugated superimposed folding pattern. We have identified three different phases of deformation that can be linked to regional Variscan deformation phases. The main collisional event produced upright to moderately inclined cylindrical folds with an associated axial planar cleavage. These folds were subsequently folded during extensional collapse, in which a second fold system with subhorizontal axes and an intense subhorizontal cleavage formed. Finally, during the formation of the Cantabrian Orocline, a third folding event refolded the two previous fold systems. This later phase formed upright open folds with fold axis trending 100° to 130°, a crenulation cleavage and brittle–ductile transcurrent conjugated shearing. Our results show that the first and last deformation phases are close to coaxial, which does not allow the CIC to be formed as a product of vertical axis rotations, i.e. an orocline. The origin of the curvature in Central Iberia, if a single process, had to be coeval or previous to the first deformation phase.
DOI: 10.6084/m9.figshare.5766558.v1
title: Tangled up in folds: tectonic significance of superimposed folding at the core of the Central Iberian curve (West Iberia)

description: The amalgamation of Pangea during the Carboniferous produced a winding mountain belt: the Variscan orogen of West Europe. In the Iberian Peninsula, this tortuous geometry is dominated by two major structures: the Cantabrian Orocline, to the north, and the Central Iberian curve (CIC) to the south. Here, we perform a detailed structural analysis of an area within the core of the CIC. This core was intensively deformed resulting in a corrugated superimposed folding pattern. We have identified three different phases of deformation that can be linked to regional Variscan deformation phases. The main collisional event produced upright to moderately inclined cylindrical folds with an associated axial planar cleavage. These folds were subsequently folded during extensional collapse, in which a second fold system with subhorizontal axes and an intense subhorizontal cleavage formed. Finally, during the formation of the Cantabrian Orocline, a third folding event refolded the two previous fold systems. This later phase formed upright open folds with fold axis trending 100° to 130°, a crenulation cleavage and brittle–ductile transcurrent conjugated shearing. Our results show that the first and last deformation phases are close to coaxial, which does not allow the CIC to be formed as a product of vertical axis rotations, i.e. an orocline. The origin of the curvature in Central Iberia, if a single process, had to be coeval or previous to the first deformation phase.
DOI: 10.6084/m9.figshare.5766519
title: Flooding scenario for four Italian coastal plains using three relative sea level rise models

description: The coastal areas of the central Mediterranean Sea are sensitive to climate change and the consequent relative sea level rise. Both phenomena may affect densely urbanized and populated areas, causing severe damages. Our maps show the land-marine flooding projections as effects of the expected relative sea level rise for four Italian coastal plains using (i) IPCC AR5 estimations, based on the IPCC RCP 8.5 emission scenarios and (ii) the Rahmstorf 2007 model. Isostatic and tectonic data were added to the global projections to estimate the relative sea changes expected along the coastline by 2100, as well as sea-flooding. The northern Adriatic map shows the study area, extending for about 5500 km<sup>2</sup>, and is presented at a scale of 1:300,000 with two inset maps at a scale of 1:150,000. The Oristano coastal plain is about 125 km<sup>2</sup>; the map scale is at 1:60,000 with an inset map scale at 1:33,000. The Cagliari coastal study area extends for 61 km<sup>2</sup>; the map scale is at 1:60,000 with two inset maps at 1:30,000. The Taranto area extends for 4.2 km<sup>2</sup> and is represented at a scale map of 1:30,000, while the three inset maps are at a scale of 1:10,000.
DOI: 10.6084/m9.figshare.5766519.v1
title: Flooding scenario for four Italian coastal plains using three relative sea level rise models

description: The coastal areas of the central Mediterranean Sea are sensitive to climate change and the consequent relative sea level rise. Both phenomena may affect densely urbanized and populated areas, causing severe damages. Our maps show the land-marine flooding projections as effects of the expected relative sea level rise for four Italian coastal plains using (i) IPCC AR5 estimations, based on the IPCC RCP 8.5 emission scenarios and (ii) the Rahmstorf 2007 model. Isostatic and tectonic data were added to the global projections to estimate the relative sea changes expected along the coastline by 2100, as well as sea-flooding. The northern Adriatic map shows the study area, extending for about 5500 km<sup>2</sup>, and is presented at a scale of 1:300,000 with two inset maps at a scale of 1:150,000. The Oristano coastal plain is about 125 km<sup>2</sup>; the map scale is at 1:60,000 with an inset map scale at 1:33,000. The Cagliari coastal study area extends for 61 km<sup>2</sup>; the map scale is at 1:60,000 with two inset maps at 1:30,000. The Taranto area extends for 4.2 km<sup>2</sup> and is represented at a scale map of 1:30,000, while the three inset maps are at a scale of 1:10,000.
DOI: 10.6084/m9.figshare.5766471
title: Reducing CO<sub>2</sub> emissions in the EU member states: Do environmental taxes work?

description: The purpose of this paper is to investigate the impact of environmentally related taxes on carbon dioxide (CO<sub>2</sub>) emissions in the EU member states. The paper uses a dynamic panel threshold regression model to determine the nonlinear relationship between environmental taxes and CO<sub>2</sub> emissions in 15 EU member countries between 1995 and 2013. The results confirm asymmetrical relationships, in which the thresholds of the environmental taxes for total environmental taxes, energy taxes (including CO<sub>2</sub> taxes), transport taxes, and taxes on pollution and resources are 3.02%, 2.20%, 0.88%, and 0.23%, respectively. The findings reveal that, after exceeding the threshold level, the effect of environmentally related taxes (excluding transport taxes) on CO<sub>2</sub> emissions changes from insignificantly positive to significantly negative. However, the analysis shows a significant effect of transport taxes on CO<sub>2</sub> emissions neither below nor above the threshold.
DOI: 10.6084/m9.figshare.5766471.v1
title: Reducing CO<sub>2</sub> emissions in the EU member states: Do environmental taxes work?

description: The purpose of this paper is to investigate the impact of environmentally related taxes on carbon dioxide (CO<sub>2</sub>) emissions in the EU member states. The paper uses a dynamic panel threshold regression model to determine the nonlinear relationship between environmental taxes and CO<sub>2</sub> emissions in 15 EU member countries between 1995 and 2013. The results confirm asymmetrical relationships, in which the thresholds of the environmental taxes for total environmental taxes, energy taxes (including CO<sub>2</sub> taxes), transport taxes, and taxes on pollution and resources are 3.02%, 2.20%, 0.88%, and 0.23%, respectively. The findings reveal that, after exceeding the threshold level, the effect of environmentally related taxes (excluding transport taxes) on CO<sub>2</sub> emissions changes from insignificantly positive to significantly negative. However, the analysis shows a significant effect of transport taxes on CO<sub>2</sub> emissions neither below nor above the threshold.
DOI: 10.6084/m9.figshare.5766432
title: wikidata-20170928-truthy-BETA-pageRank.hdt

description: This datasets contains the PageRank scores computed over the RDF graph using PageRankRDF (https://github.com/WDAqua/PageRankRDF) of Wikidata (www.wikidata.org) in HDT format (http://www.rdfhdt.org).<br>
DOI: 10.6084/m9.figshare.5766399
title: Anion-Induced N-doping of Naphthalenediimide Polymer Semiconductor in Organic Thin Film Transistors

description: Molecular doping is an important strategy to improve the charge transport properties of organic semiconductors in various electronic devices. Compared to p-type dopants, the development of n-type dopants is especially challenging due to poor dopand stability against atmospheric conditions. In this article, we reprot the n-doping of the milestone naththalenediimide-based conjugated polymers P(NDI2OD-T2) in organic thin film transistor devices by introducing soluble anion dopants which resulted in the formation of stable radical anions in thin films, as confirmed by EPR spectroscopy. By tuning the dopant concentration via simple solution mixing, the transistor parameters could be readily controlled. <br>
DOI: 10.6084/m9.figshare.5766399.v1
title: Anion-Induced N-doping of Naphthalenediimide Polymer Semiconductor in Organic Thin Film Transistors

description: Molecular doping is an important strategy to improve the charge transport properties of organic semiconductors in various electronic devices. Compared to p-type dopants, the development of n-type dopants is especially challenging due to poor dopand stability against atmospheric conditions. In this article, we reprot the n-doping of the milestone naththalenediimide-based conjugated polymers P(NDI2OD-T2) in organic thin film transistor devices by introducing soluble anion dopants which resulted in the formation of stable radical anions in thin films, as confirmed by EPR spectroscopy. By tuning the dopant concentration via simple solution mixing, the transistor parameters could be readily controlled. <br>
DOI: 10.6084/m9.figshare.5766396
title: Datasets uploading

description: Pacific ocean
DOI: 10.6084/m9.figshare.5766396.v2
title: Datasets uploading

description: Pacific ocean
DOI: 10.6084/m9.figshare.5766396.v1
title: Datasets uploading

description: Pacific ocean
DOI: 10.6084/m9.figshare.5766384
title: sitemaps-and-depth-color-maps.zip

description: Orthophotos, Depth-Color maps and sitemaps of Tafaytour Tracksite A, divided into four sections.
DOI: 10.6084/m9.figshare.5766366
title: Photogrammetric 3D-Models (.ply) of the Tafaytour Tracksite A.

description: Photogrammetric 3D-Models (.ply) of the Tafaytour Tracksite A.
DOI: 10.6084/m9.figshare.5766366.v1
title: Photogrammetric 3D-Models (.ply) of the Tafaytour Tracksite A.

description: Photogrammetric 3D-Models (.ply) of the Tafaytour Tracksite A.
DOI: 10.6084/m9.figshare.5766348
title: photographs-for-photogrammetry.zip

description: Photographs used for 3D photogrammetric model.
DOI: 10.6084/m9.figshare.5766342
title: Dynamic cortical participation during bilateral, cyclical ankle movements: effects of Parkinson’s disease

description: Each file contains EEG signals, EMG signals, and kinematic data for one participant as MATLAB files (.mat). Each modality is stored as a structure.<br>There are two participant groups: 1) men with Parkinson's disease and 2) age- and sex-matched controls. Files with names starting with "PD" are for the first group, and files with names starting with "Ctrl" are for the second group.<br>Inside each file, EEG signals are stored in "data_eeg(i,j).file", where the index, i, indicates the task and the index, j, indicates the epoch. The signals were recorded during externally-paced (i=1) and self-paced (j=2) bilateral, anti-phasic, cyclical foot dori-/plantarflexion in the sitting position. For each task, the signals were recorded in three one-minute epochs. <br>Similalry, EMG signals and kinematic data are stored in"data_mus(i,j).file" and "data_kin(i,j).file", respectively.<br>For EEG signals, the entry at (i,j).file has the size, m-by-n, where the index, m, indicates samples and the index, n, indicates EEG channels. The EEG signals were recorded at AFz, Fz, F1, F2, F3, F4, FCz, FC1, FC2, FC3, FC4, Cz, C1, C2, C3, C4, CPz, CP1, CP2, and Pz (i.e., n=1:20) according tothe 10-10 system. The EEG signals were sampled at 1200 Hz in microvolts.<br>For EMG signals, the entry at (i,j).file has the size, m-by-n, where the index, m, indicates samples and the index, n, indicates muscle. The EMG signals were recorded from the right tibialis anterior muscle, right medial gastrocnemius muscle, left tibialis anterior muscle, and left medial gastrocnemius muscle (i.e., n=1:4). The EMG signals were sampled at 2000 Hz in volts. <br>For kinematic data, the entry at (i,j).file has the size, m-by-n, where the index, m, indicates samples and the index, n, indicates the motion-capture marker location and direction. Motion-capture markers were placed bilaterally over the EEG electrode locations, AF7 and AF8, lateral epicondyles of the femur, lateral malleoli, and second metatarsal heads. n=1:3 contain the marker coordinates for AF8 in x, y, and z coordinates, where x indicates mediolateral direction, y indicates anteroposterior direction, and z indicates superior-inferior direction. n=4:6 contain the marker coordinates for the lateral epichondyle of the right femur in x, y, and z coordinates. Similarly, n=7:9 and n=10:12 contain the marker coordinates for the right lateral malleoli and right second metatarsal heads, respectively. Similalry, n=13:24 contain the marker coordinates for AF7, the lateral epichondyle of the left femur, the left lateral malleoli, and left second metatarsal heads. The kinematic data was sampled at 100 Hz in millimeters.
DOI: 10.6084/m9.figshare.5766297
title: The 1975 Japanese diet has a stress reduction effect in mice: search for physiological effects using metabolome analysis

description: We aimed to find new physiological effects of the Japanese diet. First, to determine the key components in serum from mice fed the 1975 diet, serum from mice fed the 1960, 1975, 1990 or 2005 Japanese diet was analyzed using CE-TOFMS and LC-TOFMS. Based on these results, the key components were determined by principal component analysis. Among the identified compounds, GABA was included. Therefore, a stress reduction effect was inferred as a novel physiological effect of this diet. Next, we tested whether the 1975 diet had an actual stress reduction effect in mice. Mice were given the 1975 diet or a control diet for 4 weeks, after which they were divided into restraint stress and non-stress groups. Mice fed the 1975 diet had significantly decreased stress parameters compared with those fed the control diet. These results provide the first evidence that the 1975 Japanese diet has a stress reduction effect. In the current study, we aimed to find new physiological effects of the Japanese diet. As a result, we found that the 1975.