cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.27300351
title: Genetic types, metallogenic and geodynamic models of Pb-Zn deposits in the Jiao-Liao-Ji Belt, NE China

description: Jiao-Liao-Ji Belt (JLJB) is a famous Pb–Zn polymetallic metallogenic belt in China, situated on the Northeastern margin of North China Craton (NCC). Recently, we conducted geochronological, elemental, zircon Hf isotopic studies on the metallogenic magmatites of Ji’ an Pb–Zn deposit in the east of JLJB, summarizing the fluid inclusions, geological, geochemical, and chronological data of the regional Pb–Zn deposits. Three categories of Pb–Zn deposits have been identified: skarn (Type-I), sedimentary hydrothermal-reformed (Type-II), and sedimentary superimposed-hydrothermal (Type-III) types. Type-I ore bodies occurred in the outer contact zone between Mesozoic granites and Paleozoic carbonate rocks. The ore-forming fluids belong to a H<sub>2</sub>O–NaCl±CO<sub>2</sub>±CH<sub>4</sub> system with medium–high temperature and medium salinity, which originated from magmatic water, similar to the magmatic origin of ore-forming materials. Type-II deposits mainly occurred in Paleoproterozoic marbles and schists, formed by a hydrothermal fluid system consisting of H<sub>2</sub>O–NaCl±CO<sub>2</sub> with medium to low temperature and salinity levels. The source of fluids is characterized by mixing of magmatic and meteoric waters, while the ore-forming minerals are of crustal and orogenic origins. Type-III deposits were found in Paleoproterozoic dolomitic marbles. The ore-forming fluids are characterized by a H<sub>2</sub>O–NaCl composition, exhibiting low temperature and medium salinity. The ore-forming materials are believed to originate from magma and stratum sources. The majority of the metallogenic intrusive rocks associated with Pb–Zn deposits are classified as type-I granites with high-K calc-alkaline and quasi-peraluminous characteristics, and they were formed during the Mesozoic. Late Jurassic and Early Cretaceous magmas predominantly originate from the lower crust, whereas Triassic magmas are sourced from the mantle. The metallogenic environments are influenced by the geodynamic settings associated with the collision between the Yangtze Plate and NCC during the Triassic period, and the subduction of the Palaeo-Pacific Plate beneath the Eurasian Plate during the Early Cretaceous period.
DOI: 10.6084/m9.figshare.27300351.v1
title: Genetic types, metallogenic and geodynamic models of Pb-Zn deposits in the Jiao-Liao-Ji Belt, NE China

description: Jiao-Liao-Ji Belt (JLJB) is a famous Pb–Zn polymetallic metallogenic belt in China, situated on the Northeastern margin of North China Craton (NCC). Recently, we conducted geochronological, elemental, zircon Hf isotopic studies on the metallogenic magmatites of Ji’ an Pb–Zn deposit in the east of JLJB, summarizing the fluid inclusions, geological, geochemical, and chronological data of the regional Pb–Zn deposits. Three categories of Pb–Zn deposits have been identified: skarn (Type-I), sedimentary hydrothermal-reformed (Type-II), and sedimentary superimposed-hydrothermal (Type-III) types. Type-I ore bodies occurred in the outer contact zone between Mesozoic granites and Paleozoic carbonate rocks. The ore-forming fluids belong to a H<sub>2</sub>O–NaCl±CO<sub>2</sub>±CH<sub>4</sub> system with medium–high temperature and medium salinity, which originated from magmatic water, similar to the magmatic origin of ore-forming materials. Type-II deposits mainly occurred in Paleoproterozoic marbles and schists, formed by a hydrothermal fluid system consisting of H<sub>2</sub>O–NaCl±CO<sub>2</sub> with medium to low temperature and salinity levels. The source of fluids is characterized by mixing of magmatic and meteoric waters, while the ore-forming minerals are of crustal and orogenic origins. Type-III deposits were found in Paleoproterozoic dolomitic marbles. The ore-forming fluids are characterized by a H<sub>2</sub>O–NaCl composition, exhibiting low temperature and medium salinity. The ore-forming materials are believed to originate from magma and stratum sources. The majority of the metallogenic intrusive rocks associated with Pb–Zn deposits are classified as type-I granites with high-K calc-alkaline and quasi-peraluminous characteristics, and they were formed during the Mesozoic. Late Jurassic and Early Cretaceous magmas predominantly originate from the lower crust, whereas Triassic magmas are sourced from the mantle. The metallogenic environments are influenced by the geodynamic settings associated with the collision between the Yangtze Plate and NCC during the Triassic period, and the subduction of the Palaeo-Pacific Plate beneath the Eurasian Plate during the Early Cretaceous period.
DOI: 10.3535/p8r-nq6-5e9
title: Gastropoda Cuvier, 1795

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.6084/m9.figshare.26207834.v1
title: Focus Group Audio Transcription.pdf

description: Background: There is existing literature on the mental health struggles of foster children, but less information about the mental health of foster parents. Very little has been studied regarding how foster care impacts a foster parent’s ability to participate in their leisure occupations. Objectives: This study aimed to explore foster parent perceptions of the impact fostering has on their mental health and leisure participation. Method: An audio-recorded focus group with seven (n=7) participants was conducted. The focus group transcript was coded, and codes were analyzed to create themes. Results: Five themes emerged: mental, physical, and emotional health, time and energy, change in routines, support, and new experiences Conclusion: Findings indicate that foster parents experience multiple barriers to participation in leisure occupations, including poor mental and physical health, exhaustion, different interests of the foster child, and time. <br>
DOI: 10.6084/m9.figshare.27266514
title: Magmatic and metamorphic evolution of the Late Cretaceous Muslim Bagh Ophiolite, western Pakistan: implications for ridge subduction after subduction initiation

description: The magmatic and metamorphic evolutions of the Muslim Bagh Ophiolite (MBO) can help understand the relationship among supra-subduction ophiolite, subduction initiation, and the spreading centre in the forearc. Here, we investigated the whole-rock chemistry, mineral composition, P–T conditions, and K–Ar ages of the MBO and its associated units. The whole-rock and magmatic clinopyroxene compositions indicate that the MBO amphibolites and tholeiitic basalts of the underlying Bagh Complex originated in a supra-subduction setting and mid-ocean ridges, respectively. Late Cretaceous oceanic island basalts found in the Bagh Complex and the Bibai Formation occurred in oceans and near the passive continental margin of western India, respectively. Metamorphic Mg-hornblendes in the MBO amphibolites record low-P/T type upper amphibolite-facies metamorphism (2.4–2.9 kbar, 612–690 °C), indicating a &gt; 50 ºC/km geothermal gradient. The K–Ar hornblende and plagioclase ages suggest contemporaneous low-P/T type metamorphism at ca. 78–71 Ma in the MBO formed in a forearc and tholeiitic ridge-related magmatism of ca. 78–77 Ma in the Bagh Complex, indicating a spreading ridge was active during the subduction. Our results, combined with plate kinematic reconstructions of the Neotethys Ocean in the previous studies, suggest that the abnormally high geothermal gradient in the MBO could be due to orthogonal ridge subduction near the triple junction after the ca. 80 Ma subduction initiation in the forearc. It is also likely that the geothermal gradient in the MBO dropped from &gt;50 °C/km at 78–71 Ma, through 35–45 °C/km, to &lt;25 °C/km at approximately 65 Ma due to gradual steepening of the subducting slab, followed by the obduction of the MBO during the Paleocene to Eocene period.
DOI: 10.6084/m9.figshare.27266514.v1
title: Magmatic and metamorphic evolution of the late cretaceous Muslim Bagh Ophiolite, western Pakistan: implications for ridge subduction after subduction initiation

description: The magmatic and metamorphic evolutions of the Muslim Bagh Ophiolite (MBO) can help understand the relationship among supra-subduction ophiolite, subduction initiation, and the spreading centre in the forearc. Here, we investigated the whole-rock chemistry, mineral composition, P–T conditions, and K–Ar ages of the MBO and its associated units. The whole-rock and magmatic clinopyroxene compositions indicate that the MBO amphibolites and tholeiitic basalts of the underlying Bagh Complex originated in a supra-subduction setting and mid-ocean ridges, respectively. Late Cretaceous oceanic island basalts found in the Bagh Complex and the Bibai Formation occurred in oceans and near the passive continental margin of western India, respectively. Metamorphic Mg-hornblendes in the MBO amphibolites record low-P/T type upper amphibolite-facies metamorphism (2.4–2.9 kbar, 612–690 °C), indicating a &gt; 50 ºC/km geothermal gradient. The K–Ar hornblende and plagioclase ages suggest contemporaneous low-P/T type metamorphism at ca. 78–71 Ma in the MBO formed in a forearc and tholeiitic ridge-related magmatism of ca. 78–77 Ma in the Bagh Complex, indicating a spreading ridge was active during the subduction. Our results, combined with plate kinematic reconstructions of the Neotethys Ocean in the previous studies, suggest that the abnormally high geothermal gradient in the MBO could be due to orthogonal ridge subduction near the triple junction after the ca. 80 Ma subduction initiation in the forearc. It is also likely that the geothermal gradient in the MBO dropped from &gt;50 °C/km at 78–71 Ma, through 35–45 °C/km, to &lt;25 °C/km at approximately 65 Ma due to gradual steepening of the subducting slab, followed by the obduction of the MBO during the Paleocene to Eocene period.
DOI: 10.6084/m9.figshare.27266514.v2
title: Magmatic and metamorphic evolution of the Late Cretaceous Muslim Bagh Ophiolite, western Pakistan: implications for ridge subduction after subduction initiation

description: The magmatic and metamorphic evolutions of the Muslim Bagh Ophiolite (MBO) can help understand the relationship among supra-subduction ophiolite, subduction initiation, and the spreading centre in the forearc. Here, we investigated the whole-rock chemistry, mineral composition, P–T conditions, and K–Ar ages of the MBO and its associated units. The whole-rock and magmatic clinopyroxene compositions indicate that the MBO amphibolites and tholeiitic basalts of the underlying Bagh Complex originated in a supra-subduction setting and mid-ocean ridges, respectively. Late Cretaceous oceanic island basalts found in the Bagh Complex and the Bibai Formation occurred in oceans and near the passive continental margin of western India, respectively. Metamorphic Mg-hornblendes in the MBO amphibolites record low-P/T type upper amphibolite-facies metamorphism (2.4–2.9 kbar, 612–690 °C), indicating a &gt; 50 ºC/km geothermal gradient. The K–Ar hornblende and plagioclase ages suggest contemporaneous low-P/T type metamorphism at ca. 78–71 Ma in the MBO formed in a forearc and tholeiitic ridge-related magmatism of ca. 78–77 Ma in the Bagh Complex, indicating a spreading ridge was active during the subduction. Our results, combined with plate kinematic reconstructions of the Neotethys Ocean in the previous studies, suggest that the abnormally high geothermal gradient in the MBO could be due to orthogonal ridge subduction near the triple junction after the ca. 80 Ma subduction initiation in the forearc. It is also likely that the geothermal gradient in the MBO dropped from &gt;50 °C/km at 78–71 Ma, through 35–45 °C/km, to &lt;25 °C/km at approximately 65 Ma due to gradual steepening of the subducting slab, followed by the obduction of the MBO during the Paleocene to Eocene period.
DOI: 10.3535/9cq-0t4-d2w
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/r9r-r18-5dg
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/8p6-y5t-4sf
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/ncm-90j-qph
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/pvl-rcf-9f2
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/vfh-fn8-2xz
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.6084/m9.figshare.7064516.v1
title: Scripts Directory

description: Scripts used to produce results for this manuscript. View the README.md for more information.
DOI: 10.3535/hlm-gds-08d
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/vee-lde-tn9
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.6084/m9.figshare.26509378.v2
title: Data from '<b>Should we really predict the response of wild endotherms to climate change based on thermal responses measured in captivity?</b>'

description: To provide a data-supported commentary on the publication by Beaman et al. 2024 (https://doi.org/10.1098/rspb.2023.1887), data was recovered from Figures from this study, as well as from other sources related to the thermal biology of dovekies (<i>Alle alle</i>).
DOI: 10.3535/psl-grw-kqe
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.6084/m9.figshare.6809618.v1
title: Dataset S1. Nucleotide Alignments of primate, rodent and bat NTCP

description: PRANK alignments of orthologous nucleotide sequences of NTCP from 27 primate (1,047 bp), 18 rodent (1,029 bp) and 21 bat (1,005 bp) species retrieved from public databases and newly sequenced in this study. Corresponding Accession Numbers are found in the Manuscript Table S1.
DOI: 10.3535/9d7-h3q-70h
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/zkc-ezw-pn6
title: Cephalopoda Cuvier, 1795

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.17632/xngcbynbyd
title: MiIsoGra: Simple Un-directed Graphs That Might Be Isomorphic

description: Thousands of undirected simple graph pairs with different number of nodes and different degree sequences are given. These graph pairs have been tested for isomorphism. The non-isomorphic graph pairs with identical degree sequences have also been given.
DOI: 10.3535/ny5-yrf-rxt
title: Conularia sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/v1m-p8l-ghr
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.17632/jsn8c49wpy
title: The PPR domain of mitochondrial RNA polymerase is a ribonuclease required for mtDNA replication 

description: Unprocessed imaging data.
DOI: 10.3535/bxk-e77-ak0
title: Brachiopoda Duméril, 1805

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/lys-w78-s7s
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.25403/upresearchdata.11763420.v1
title: Non-invasive monitoring of adrenocortical function in female domestic pigs using saliva and faeces as hormone sample matrices

description: Faecal glucocorticoid metabolite and salivary glucocorticoid concentrations in female pigs after ACTH challenge
DOI: 10.3535/5yj-3gr-pb2
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/714-1e4-5fr
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/zt1-tcq-3x0
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/6e2-fbt-9ff
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/hg8-nwa-vft
title: Brachiopoda Duméril, 1805

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.6084/m9.figshare.13554509.v1
title: Supplement, data and code "The Link between Regional Temperature and Regional Incomes: Econometric Evidence with Sub-National Data"

description: This fileset contains the supplement, the data and the replication code for the paper "The Link between Regional Temperature and Regional Incomes: Econometric Evidence with Sub-National Data".<br><br>Abstract: We present a micro-based approach to evaluate the effect of water- and health-related development projects which complements established evaluation methods. We collect information from 1.8 million individuals from DHS clusters (Demographic and Health Surveys) in 38 developing economies between 1986 and 2017. By geocodes, we combine cluster information with over 14,000 sub-national projects from the World Bank. We then investigate the impact of the projects employing fixed effects estimation techniques. Our findings indicate that the time to gather water and child mortality tend to decrease when projects are realized. The quality of drinking water and sanitation facilities are also positively affected by projects. Our data allows us to account for cluster heterogeneity, which is an important extension to the cross-country literature. Various robustness checks support our findings.
DOI: 10.6084/m9.figshare.21947219.v1
title: Raw data

description: Contrast-enhanced ultrasound for the diagnosis of acute pyelonephritis in pediatric patients with urinary tract infection: a feasibility study
DOI: 10.6084/m9.figshare.5043214.v1
title: main time stepping code and the data it generates

description: main time stepping code and the data it generates
DOI: 10.3535/m09-vmx-nvw
title: Brachiopoda Duméril, 1805

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/y0r-7vp-hqq
title: †Obolus Eichwald, 1829

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.17632/xh545yt88t
title: Data for: Why Do Multinational Firms Hold So Much Cash? Further Evidence on the Precautionary Motive

description: A full sample data-set is provided.
DOI: 10.17632/z2njptskdj
title: Data and supplementary data for "A diamond gammavoltaic cell utilising surface conductivity and its response to different photon interaction mechanisms".

description: These data show measurements of the composition and capabilities of a novel diamond gammavoltaic cell (DGV). A full description of the main data and methods used to acquire them can be found in the main article manuscript. In no less detail, the same information is presented in a supplementary information manuscript, for those data which are presented for supplementary figures here. The data presented in these MS Excel files are colour-coded, and labelled with the figures the data appear in. Data that do not appear in the figures are coded grey, and their uncertainties pale grey. These may be either data that do not have physical meaning, such as the power data in the power-voltage figures which are negative, or may be data presented as stages of a manipulation, such as in the digitisation, smoothing and plotting of the data from Fornalski 2018 (DOI: 10.1088/2399-6528/aab408). Plotted data all have axes and series numbers indicated, but for visual ease are also colour-coded: abscissa data in blue, abscissa uncertainties in pale blue, ordinate data in green, and ordinate uncertainties in pale green. Each figure is also supplied as a TIF files alongside the data, for ease of comparison. Contributors who produced data, by sub/figure: Fig3: GRM Fig4: GRM, TC, CH, PGM Fig5: GRM, TC, CH, PGM FigS1: MC, GRM FigS2: MC, GRM FigS3: TC, GRM FigS4: GRM, TC, CH, PGM
DOI: 10.3535/vqv-a35-8qg
title: Rock Crystal

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/yzx-9ak-jbn
title: Conichnus conicus Männil

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.6084/m9.figshare.19969314.v1
title: Family expenditures on healthcare plans in Brazil and household budget commitment: an analysis of the Brazilian Household Budgets Survey (2017/2018)

description: According to studies using previous editions of the Household Budgets Survey (POF) in Brazil, paying for a healthcare plan increases the percentage of income spent on health and fails to reduce the probability of incurring excessive health expenditures. The study’s objective was to describe relations between expenditures on healthcare plans, income, and age groups, highlighting the effect of having a plan on the probability of committing more than 40% of income on health-related expenditures. An analysis of the POF 2017/2018 determined the commitment of per capita household income for payers of plans by age group and type of plan and logistic regression for factors associated with committing more than 40% of income to health-related expenditures. In 12 months, 22.1 million Brazilians spent BRL 78.1 billion on private medical insurance. The share of income spent on individual plans increases consistently with age, from 4.5% of per capita household income (at &lt; 19 years) to 10.6% of this income (at 79 years or older). The probability of committing more than 40% of income to health expenditures decreases with income, increases with age, and is higher for those paying for health plans. Spending on healthcare plans alone exceeds 40% of per capita household income for 5.6% of Brazilians 60 years or older who pay for individual plans and for 4% of those who pay for company plans. Persons in the oldest age groups and in the lowest income brackets show the highest likelihood of spending more than 40% of their income on healthcare. A revision of the plans’ adjustment by age is an alternative for attempting to mitigate this problem.
DOI: 10.6084/m9.figshare.918663.v4
title: Phylogenetics of <i>Panthera</i>, including <i>Panthera atrox</i>, based on craniodental characters

description: The phylogenetic position of <i>Panthera atrox</i> within Felidae is still controversial despite many morphological and molecular studies addressing its relationships. This is in part due to the lack of consensus on a tree for <i>Panthera.</i> These inconsistencies suggest the need for further analysis and perhaps even different methodology to better understand pantherine evolution. Morphologic characters from the skull and dentary were analysed within <i>Panthera</i> to elucidate pantherine phylogeny. Extant taxa included <i>Panthera leo</i> (African lion), <i>Panthera tigris</i> (tiger), <i>Panthera onca</i> (jaguar), <i>Panthera pardus</i> (leopard), <i>Uncia uncia</i> (snow leopard) and <i>Neofelis nebulosa</i> (clouded leopard). Four outgroups were used: <i>Crocuta crocuta</i> (spotted hyena), <i>Metailurus</i> spp., <i>Proailurus lemanensis</i> and <i>Pseudaelurus validus</i>. Our study found a clade containing <i>Panthera leo</i>, <i>Panthera tigris</i> and <i>Panthera atrox</i>, suggesting that <i>Panthera atrox</i> is more closely related to the African lion and the tiger than the jaguar, in contrast to what has been recently proposed. Moreover, gross morphological similarities between <i>Panthera atrox</i> and <i>Panthera onca</i> are more likely the result of convergent hunting styles and/or prey selection, rather than phylogenetic affinity.