cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.13275323.v2
title: Short Term Mortality Fluctuations series at the Human Mortality Database

description: The COVID-19 pandemic has revealed substantial coverage and quality gaps in existing international and national statistical monitoring systems. It is striking that obtaining timely, accurate, and comparable across countries data in order to adequately respond to unexpected epidemiological threats is very challenging. The most robust and reliable approach to quantify the mortality burden due to short-term risk factors is based on estimating weekly excess deaths. This approach is more reliable than monitoring deaths with COVID-19 diagnosis or calculating incidence or fatality rates affected by numerous problems such as testing coverage and comparability of diagnostic approaches. In response to the newly emerging data challenges, a new data resource on weekly mortality has been established. The Short-term Mortality Fluctuations (STMF, available at www.mortality.org) data series is the first international database providing open-access harmonized, uniform, and fully documented data on weekly all-cause mortality. The STMF online vizualisation tool provides an opportunity to perform a quick assessment of the excess weekly mortality in one or several countries by means of an interactive graphical interface.
DOI: 10.6084/m9.figshare.14251025
title: A predictive model for maceral discrimination by means of Raman spectra on dispersed organic matter: a case study from the Carpathian Fold-and-Thrust Belt (Ukraine)

description: Excel file report results from spectra fitting divided for maceral type
DOI: 10.6084/m9.figshare.14251025.v1
title: A predictive model for maceral discrimination by means of Raman spectra on dispersed organic matter: a case study from the Carpathian Fold-and-Thrust Belt (Ukraine)

description: Excel file report results from spectra fitting divided for maceral type
DOI: 10.6084/m9.figshare.14525484
title: Data For: Lipid bound phosphorus in the seston of Lake Erie and its tributaries and its use as an indicator of algal P-limitation

description: Physical, chemical, and biological parameters measured in offshore areas and tributaries of Lake Erie.
DOI: 10.6084/m9.figshare.14525484.v1
title: Data For: Lipid bound phosphorus in the seston of Lake Erie and its tributaries and its use as an indicator of algal P-limitation

description: Physical, chemical, and biological parameters measured in offshore areas and tributaries of Lake Erie.
DOI: 10.6084/m9.figshare.14473344.v1
title: Mechanomics RT-DC Set 02 - Carcinoma

description: Entry is a part of <b>Mechanomics</b> collection (10.6084/m9.figshare.c.5399826) that contains data supporting findings presented in the following manuscript:<i>Urbanska, M., Ge, Y.</i> et al., 2021 bioRxiv<b><i>De novo identification of universal cell mechanics regulators</i></b>https://doi.org/10.1101/2021.04.26.441418<br>This dataset contains mechanical measurement of six carcinoma cell lines obtained from RIKEN institute:<br>• ECC4 (RCB0982) - intestine - small-cell carcinoma• TGBC18TKB (RCB0982) - intestine - adenocarcinoma• WA-hT (RCB2279) - lung - small-cell carcinoma• EBC-1 (RCB1965) - lung - squamous cell carcinoma• A549 (RCB0098) - lung - adenocarcinoma• ECC10 (RCB0983) - stomach - small-cell carcinoma• MKN45 (RCB1001) - stomach - adenocarcinoma• MKN1 (RCB1003) - stomach - adenocarcinoma.<br>Measurements were performed using real-time deformability cytometry (RT-DC).<br><b>_rtdc.zip</b> - contains data acquired during the measurments in '*.rtdc' format<b>_tsv.zip</b> - contains extended data in a '*.tsv' format<b>_glmm.zip</b> - contains result summaries of statistical analysis comparing Young's moduli of the different cell types using generalised linear mixed effects models<br>
DOI: 10.6084/m9.figshare.8797586
title: On the behaviour of molecular interactions of ionic liquids with organic solvent from <i>T</i> = (298.15 to 323.15) K at 0.1 MPa

description: Density, speed of sound and viscosity values are measured for different binary mixture concentrations of ([Bmim][NTf<sub>2</sub>] + aniline) and ([Bmim][Pf<sub>6</sub>] + aniline) systems at temperatures from <i>T</i> = (298.15 to 323.15) K. VTF equation is used to fit the experimental viscosity values. The excess values of – molar volume, isentropic compressibility, molar Gibbs free energy of activation and speed of sound have been calculated. R-K equation is utilised to evaluate coefficients and standard deviations. The assumptions on the behaviour of molecular interactions from the analysis of excess parameters are supported by the spectroscopic studies.
DOI: 10.6084/m9.figshare.8797586.v1
title: On the behaviour of molecular interactions of ionic liquids with organic solvent from <i>T</i> = (298.15 to 323.15) K at 0.1 MPa

description: Density, speed of sound and viscosity values are measured for different binary mixture concentrations of ([Bmim][NTf<sub>2</sub>] + aniline) and ([Bmim][Pf<sub>6</sub>] + aniline) systems at temperatures from <i>T</i> = (298.15 to 323.15) K. VTF equation is used to fit the experimental viscosity values. The excess values of – molar volume, isentropic compressibility, molar Gibbs free energy of activation and speed of sound have been calculated. R-K equation is utilised to evaluate coefficients and standard deviations. The assumptions on the behaviour of molecular interactions from the analysis of excess parameters are supported by the spectroscopic studies.
DOI: 10.6084/m9.figshare.14525538
title: Lifestyle information from YouTube influencers: A comment analysis

description: Information about comments on 223 female influencer lifestyle channels. Data from paper: Lifestyle information from YouTube influencers: A comment analysis
DOI: 10.6084/m9.figshare.14525556
title: claustrum_axial_0.h5

description: claustrum axial weights 0
DOI: 10.6084/m9.figshare.14525556.v1
title: claustrum_axial_0.h5

description: claustrum axial weights 0
DOI: 10.6084/m9.figshare.14525541
title: claustrum_coronal_2.h5

description: claustrum coronal weights 2<br>
DOI: 10.6084/m9.figshare.14525541.v1
title: claustrum_coronal_2.h5

description: claustrum coronal weights 2<br>
DOI: 10.6084/m9.figshare.14525547
title: claustrum_axial_2.h5

description: claustrum axial weights 2<br>
DOI: 10.6084/m9.figshare.14525547.v1
title: claustrum_axial_2.h5

description: claustrum axial weights 2<br>
DOI: 10.6084/m9.figshare.14525544
title: claustrum_axial_1.h5

description: claustrum axial weights 1
DOI: 10.6084/m9.figshare.14525544.v1
title: claustrum_axial_1.h5

description: claustrum axial weights 1
DOI: 10.6084/m9.figshare.14525553.v1
title: claustrum_coronal_1.h5

description: claustrum coronal weights 1<br>
DOI: 10.6084/m9.figshare.14525553
title: claustrum_coronal_1.h5

description: claustrum coronal weights 1<br>
DOI: 10.5281/zenodo.4732330
title: Validation of C3S v202012 vs C3S v201912 vs ERA5-Land v20190904

description: QA4SM validation of soil moisture data: C3S v202012 vs C3S v201912 vs ERA5-Land v20190904. URL: https://qa4sm.eu/result/cf26befd-d356-4636-97d9-83438a586995/. Produced on QA4SM (https://qa4sm.eu)
DOI: 10.5281/zenodo.4732329
title: Validation of C3S v202012 vs C3S v201912 vs ERA5-Land v20190904

description: QA4SM validation of soil moisture data: C3S v202012 vs C3S v201912 vs ERA5-Land v20190904. URL: https://qa4sm.eu/result/cf26befd-d356-4636-97d9-83438a586995/. Produced on QA4SM (https://qa4sm.eu)
DOI: 10.6084/m9.figshare.14525550
title: claustrum_coronal_0.h5

description: claustrum coronal weights 0<br>
DOI: 10.6084/m9.figshare.14525550.v1
title: claustrum_coronal_0.h5

description: claustrum coronal weights 0<br>
DOI: 10.6084/m9.figshare.14046101
title: Connaissance et attitude des ménages_Palu_RDC.xlsx

description: these data ware collected from households in DRC. They describe, knowledge of antimalarials and bahaviour towards suspected malaria
DOI: 10.6084/m9.figshare.14046101.v1
title: Connaissance et attitude des ménages_Palu_RDC.xlsx

description: these data ware collected from households in DRC. They describe, knowledge of antimalarials and bahaviour towards suspected malaria
DOI: 10.5281/zenodo.4732274
title: TAMUoic2019 Database P21 Kernel Extension

description: The P21 kernel extension of the TAMUoic2019 database (https://doi.org/10.5281/zenodo.4718022), which is a database of the single-scattering properties of oriented ice crystals (OIC). The two major oriented particles, horizontally oriented plates (HOP) and columns (HOC), are considered in the database.
description: {"references": ["Saito, M., and P. Yang (2019), Oriented ice crystals: A single-scattering property database for applications to lidar and optical phenomenon simulations, J. Atmos. Sci., 76, 2635\u20132652."]}
DOI: 10.7910/dvn/bvfqi0
title: Replication Data for: "Rethinking Women's Interests: An Inductive and Intersectional Approach to Defining Women's Policy Priorities"

description: Replication data
DOI: 10.6084/m9.figshare.11889678
title: Evolution of the Jurassic Comallo volcanic sedimentary complex in the western North Patagonian Massif, Rio Negro province, Argentina

description: Here we define the Comallo volcanic sedimentary complex of the western North Patagonian Massif. It is composed by two members that include 9 lithofacies and 7 facies associations. The lower member is represented by massive and stratified lapilli tuffs, lithic and tuffaceous breccias, coherent andesite-dacite lava-flows, andesitic breccias, and massive crystalline limestones. The upper member consists of red conglomerates, parallel and cross-stratification sandstones, and mudstones. The lower member is interpreted as having been deposited by dilute and dense pyroclastic currents, block and ash deposits and lava-flow, and hypersaline lacustrine environments. The upper member is considered to have been deposited in fluviatile environments. A new U-Pb age of 192.0 ± 3.0 Ma (Sinemurian) was obtained for this complex. It is coeval with several volcanic sedimentary units that crop out along the western North Patagonian Massif, the Neuquén basin and the Extraandean Chubut in pull-apart or rift depocentres. The movements of the NW-SE strike-slip faults that border the northern and southern limits of the Comallo depocentre made possible the development of a pull-apart basin as well as the volcanism and the fluvial system. This and other coeval units were deposited in similar environmental conditions along the North Patagonian Massif, the Neuquén basin and the extraandean Chubut, indicating a similar tectonomagmatic setting, in a tensional rear-arc during Lower Jurassic times.
DOI: 10.6084/m9.figshare.11889702.v1
title: Late Neoproterozoic mafic sills in the Suizhou area of the South Qinling block: constraints for the tectonic evolution of the northern margin of the Yangtze craton

description: Late Neoproterozoic gabbroic-diabasic sills are widely distributed in the eastern part of the South Qinling block. Here, a comprehensive geochronological and geochemical study of these mafic sills has been conducted. LA-ICP-MS zircon U-Pb results indicate that the gabbroic-diabasic sills were formed at 632 ± 2 Ma. The sills consist mainly of tholeiitic basaltic rocks with relatively low TiO<sub>2</sub> contents (0.81–1.07 wt.%) and high Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>/MgO ratios. These rocks display relatively flat to moderate light rare earth elements (LREE) enrichment patterns and positive Eu anomalies (Eu/Eu* = 1.15–1.41). On the primitive mantle normalized spider diagram, the samples show E-MORB-like geochemical features. All of the studied samples display similar Sm-Nd isotopic compositions with negative ε<sub>Nd</sub> (t) values ranging from −6.2 to −5.5. Most clinopyroxenes from the mafic sills have relatively low Al/Ti ratios similar to those of typical rift-related cumulates. Therefore, Whole-rock and mineral geochemical features of the studied samples suggest that the mafic sills might have been derived from partial melting of a metasomatised subcontinental lithospheric mantle source in a continental rift setting. It can be advocated that the break-up of the Rodinia supercontinent in the northern part of the Yangtze craton might have been a long-lasting process. By comparison of the coherent Neoproterozoic magmatic events in the northern Yangtze craton and the Tarim block, it can be suggested that the Yangtze craton might have been adjacent to the Tarim block in the reconstruction model of the Rodinia supercontinent.
DOI: 10.6084/m9.figshare.11889678.v1
title: Evolution of the Jurassic Comallo volcanic sedimentary complex in the western North Patagonian Massif, Rio Negro province, Argentina

description: Here we define the Comallo volcanic sedimentary complex of the western North Patagonian Massif. It is composed by two members that include 9 lithofacies and 7 facies associations. The lower member is represented by massive and stratified lapilli tuffs, lithic and tuffaceous breccias, coherent andesite-dacite lava-flows, andesitic breccias, and massive crystalline limestones. The upper member consists of red conglomerates, parallel and cross-stratification sandstones, and mudstones. The lower member is interpreted as having been deposited by dilute and dense pyroclastic currents, block and ash deposits and lava-flow, and hypersaline lacustrine environments. The upper member is considered to have been deposited in fluviatile environments. A new U-Pb age of 192.0 ± 3.0 Ma (Sinemurian) was obtained for this complex. It is coeval with several volcanic sedimentary units that crop out along the western North Patagonian Massif, the Neuquén basin and the Extraandean Chubut in pull-apart or rift depocentres. The movements of the NW-SE strike-slip faults that border the northern and southern limits of the Comallo depocentre made possible the development of a pull-apart basin as well as the volcanism and the fluvial system. This and other coeval units were deposited in similar environmental conditions along the North Patagonian Massif, the Neuquén basin and the extraandean Chubut, indicating a similar tectonomagmatic setting, in a tensional rear-arc during Lower Jurassic times.
DOI: 10.6084/m9.figshare.11889690
title: Petrogenesis and tectonic regime of two types of Neoarchaean amphibolites in the northern margin of the North China Craton

description: The Neoarchaean crustal evolutionary processes of the North China Craton (NCC) provide a window to understanding the crust–mantle interaction in the Early Earth. The Jiefangyingzi amphibolites are located in the Bainaimiao arc belt, along the northern margin of the NCC. LA–ICP–MS U–Pb isotopic data reveal that the Type 1 amphibolites were formed at ~2562 Ma, and the Type 2 amphibolites were formed at ~2504 Ma, but were subsequently subjected to metamorphism at ~1889 Ma. Lu–Hf isotopic data of the Type 1 amphibolite show positive ε<sub>Hf</sub>(t) values (+1.2–+6.0) and T<sub>DM</sub> from 2612 Ma to 2791 Ma, suggesting a significant episode of 2.6–2.8 Ga crustal growth within the study area. Geochemically, the Type 1 amphibolites show high SiO<sub>2</sub> contents (53.37%–55.19%), moderate LREE–enriched patterns (La/Sm)<sub>N</sub> = 2.42–3.15 and HREE–depleted patterns (Gd/Yb)<sub>N</sub> = 1.86–2.64, with negative Nb anomalies, which are similar to IAB–like rocks, suggesting that they were derived from partial melting of arc–related depleted mantle with intense subduction–related fluids metasomatism. The Type 2 amphibolites have lower SiO<sub>2</sub> contents from 44.28% to 50.77%, and show LREE–depleted REE patterns ((La/Sm)<sub>N</sub> = 0.67–1.02), nearly unfractionated HREE patterns ((Gd/Yb)<sub>N</sub> = 0.89–1.77), with negative Nb, Th and positive Sr, Zr anomalies, which are close to N–MORB–like rocks, indicating that they were generated from partial melting of depleted mantle with slight fluid metasomatism. The geochronological, Lu–Hf isotopic and geochemical features show that the IAB–like rocks were formed in an intra–oceanic arc environment, coincide with the significant ~2.5–2.6 Ga episode of crustal growth in the NCC; The slightly younger MORB–like rocks reflect the spreading of the oceanic crust might last until ~2.5 Ga in the central zone.
DOI: 10.6084/m9.figshare.11889702
title: Late Neoproterozoic mafic sills in the Suizhou area of the South Qinling block: constraints for the tectonic evolution of the northern margin of the Yangtze craton

description: Late Neoproterozoic gabbroic-diabasic sills are widely distributed in the eastern part of the South Qinling block. Here, a comprehensive geochronological and geochemical study of these mafic sills has been conducted. LA-ICP-MS zircon U-Pb results indicate that the gabbroic-diabasic sills were formed at 632 ± 2 Ma. The sills consist mainly of tholeiitic basaltic rocks with relatively low TiO<sub>2</sub> contents (0.81–1.07 wt.%) and high Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>/MgO ratios. These rocks display relatively flat to moderate light rare earth elements (LREE) enrichment patterns and positive Eu anomalies (Eu/Eu* = 1.15–1.41). On the primitive mantle normalized spider diagram, the samples show E-MORB-like geochemical features. All of the studied samples display similar Sm-Nd isotopic compositions with negative ε<sub>Nd</sub> (t) values ranging from −6.2 to −5.5. Most clinopyroxenes from the mafic sills have relatively low Al/Ti ratios similar to those of typical rift-related cumulates. Therefore, Whole-rock and mineral geochemical features of the studied samples suggest that the mafic sills might have been derived from partial melting of a metasomatised subcontinental lithospheric mantle source in a continental rift setting. It can be advocated that the break-up of the Rodinia supercontinent in the northern part of the Yangtze craton might have been a long-lasting process. By comparison of the coherent Neoproterozoic magmatic events in the northern Yangtze craton and the Tarim block, it can be suggested that the Yangtze craton might have been adjacent to the Tarim block in the reconstruction model of the Rodinia supercontinent.
DOI: 10.6084/m9.figshare.11926257
title: Evidence for Early Tonian (Ca. 1000-940 Ma) continental rifting in southern Borborema Province (NE Brazil): tectonic inheritance and shear zone nucleation during assembly of West Gondwana

description: The factors controlling the inception of continental-scale transcurrent shear zones are still under debate. In order to a better understanding of the origin and evolution of the 400 km long West Pernambuco shear zone (WPSZ), we undertook a structural, geochronological and geochemical study in an area around its eastern termination. The WPSZ is one of the most expressive strike-slip shear zones in the Borborema Province of NE Brazil, which resulted from orogenic processes associated with the assembly of western Gondwana in the Late Neoproterozoic. Previous studies have shown that 1000–940 Ma-old granitic orthogneisses are located immediately to the south of the western and central portions of the WPSZ. Based on LA-ICP-MS U-Pb zircon dating, we show that rocks with similar ages (995–956 Ma) also occur to the East. The geochemical characteristics of this magmatism and the alignment of the bodies along a narrow, less than 40 km-wide belt point to emplacement in a continental rift-related setting. The WPSZ thus follows the trend of a pre-existing rheological discontinuity, which induced strain localization during the post-collisional stage of the Brasiliano-Pan-African orogeny.
DOI: 10.6084/m9.figshare.11956191
title: Disequilibrium crystallization and rapid crystal growth: a case study of orbicular granitoids of magmatic origin

description: Archaean orbicular granitoids from western Australia were investigated to better understand crystal growth processes. The orbicules are dioritic to tonalitic spheroids dispersed in a granitic host magma. Most orbicules have at least two to three concentric bands composed of elongate and radially oriented hornblendes with interstitial plagioclase. Each band consists of a hornblende-rich outer layer and a plagioclase-rich inner layer. Doublet band thicknesses increase, crystal number density decreases, and grain size increases from rim to core, suggesting crystallization was more rapid on the rims than in the core. Despite these radial differences, mineral mode and bulk composition of each band are similar, indicating limited crystal-melt segregation during crystallization. These observations lead us to suggest that the orbicules represent slowly quenched blobs of hot dioritic to tonalitic liquids injected into a cooler granitic magma. The oscillatory bands in the orbicules can be explained by rapid, disequilibrium crystallization (supercooling). In particular, a linear correlation between bandwidth and radial distance from orbicule rim can be explained by transport-limited crystallization, wherein crystallization timescales are shorter than chemical diffusion timescales. The slope of this linear relationship corresponds to the square root of the ratio between effective chemical diffusivity in the growth medium and thermal diffusivity, resulting in effective chemical diffusivities of 3 <b>× </b>10<sup>−8</sup> m<sup>2</sup>/s. These high effective diffusivities require static diffusion through a free volatile phase (fluid) and/or a strong advective/convective component in the fluid. Regardless of the mechanisms, these effective diffusivities can be used to estimate growth rates of ~10<sup>−6</sup> m/s or 0.4 cm/hr. Our results indicate that crystals can grow rapidly, possibly facilitated by fluids and dynamic conditions. These rapid growth rates suggest that centimetre or larger crystals, such as in porphyritic and pegmatitic systems, can conceivably grow within days.
DOI: 10.6084/m9.figshare.11889690.v1
title: Petrogenesis and tectonic regime of two types of Neoarchaean amphibolites in the northern margin of the North China Craton

description: The Neoarchaean crustal evolutionary processes of the North China Craton (NCC) provide a window to understanding the crust–mantle interaction in the Early Earth. The Jiefangyingzi amphibolites are located in the Bainaimiao arc belt, along the northern margin of the NCC. LA–ICP–MS U–Pb isotopic data reveal that the Type 1 amphibolites were formed at ~2562 Ma, and the Type 2 amphibolites were formed at ~2504 Ma, but were subsequently subjected to metamorphism at ~1889 Ma. Lu–Hf isotopic data of the Type 1 amphibolite show positive ε<sub>Hf</sub>(t) values (+1.2–+6.0) and T<sub>DM</sub> from 2612 Ma to 2791 Ma, suggesting a significant episode of 2.6–2.8 Ga crustal growth within the study area. Geochemically, the Type 1 amphibolites show high SiO<sub>2</sub> contents (53.37%–55.19%), moderate LREE–enriched patterns (La/Sm)<sub>N</sub> = 2.42–3.15 and HREE–depleted patterns (Gd/Yb)<sub>N</sub> = 1.86–2.64, with negative Nb anomalies, which are similar to IAB–like rocks, suggesting that they were derived from partial melting of arc–related depleted mantle with intense subduction–related fluids metasomatism. The Type 2 amphibolites have lower SiO<sub>2</sub> contents from 44.28% to 50.77%, and show LREE–depleted REE patterns ((La/Sm)<sub>N</sub> = 0.67–1.02), nearly unfractionated HREE patterns ((Gd/Yb)<sub>N</sub> = 0.89–1.77), with negative Nb, Th and positive Sr, Zr anomalies, which are close to N–MORB–like rocks, indicating that they were generated from partial melting of depleted mantle with slight fluid metasomatism. The geochronological, Lu–Hf isotopic and geochemical features show that the IAB–like rocks were formed in an intra–oceanic arc environment, coincide with the significant ~2.5–2.6 Ga episode of crustal growth in the NCC; The slightly younger MORB–like rocks reflect the spreading of the oceanic crust might last until ~2.5 Ga in the central zone.