cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.3462749
title: Analytic cognitive style, not delusional ideation, predicts data gathering in a large beads task study

description: <i>Introduction:</i> It has been proposed that deluded and delusion-prone individuals gather less evidence before forming beliefs than those who are not deluded or delusion-prone. The primary source of evidence for this “jumping to conclusions” (JTC) bias is provided by research that utilises the “beads task” data-gathering paradigm. However, the cognitive mechanisms subserving data gathering in this task are poorly understood. <i>Methods:</i> In the largest published beads task study to date (<i>n</i> = 558), we examined data gathering in the context of influential dual-process theories of reasoning. <i>Results:</i> Analytic cognitive style (the willingness or disposition to critically evaluate outputs from intuitive processing and engage in effortful analytic processing) predicted data gathering in a non-clinical sample, but delusional ideation did not. <i>Conclusion:</i> The relationship between data gathering and analytic cognitive style suggests that dual-process theories of reasoning can contribute to our understanding of the beads task. It is not clear why delusional ideation was not found to be associated with data gathering or analytic cognitive style.
DOI: 10.6084/m9.figshare.3462749.v1
title: Analytic cognitive style, not delusional ideation, predicts data gathering in a large beads task study

description: <i>Introduction:</i> It has been proposed that deluded and delusion-prone individuals gather less evidence before forming beliefs than those who are not deluded or delusion-prone. The primary source of evidence for this “jumping to conclusions” (JTC) bias is provided by research that utilises the “beads task” data-gathering paradigm. However, the cognitive mechanisms subserving data gathering in this task are poorly understood. <i>Methods:</i> In the largest published beads task study to date (<i>n</i> = 558), we examined data gathering in the context of influential dual-process theories of reasoning. <i>Results:</i> Analytic cognitive style (the willingness or disposition to critically evaluate outputs from intuitive processing and engage in effortful analytic processing) predicted data gathering in a non-clinical sample, but delusional ideation did not. <i>Conclusion:</i> The relationship between data gathering and analytic cognitive style suggests that dual-process theories of reasoning can contribute to our understanding of the beads task. It is not clear why delusional ideation was not found to be associated with data gathering or analytic cognitive style.
DOI: 10.6084/m9.figshare.3462677
title: Boninitic and tholeiitic basaltic lavas and dikes from dispersed Jurassic East Othris ophiolitic units, Greece: petrogenesis and geodynamic implications

description: Pillow lavas, massive lava flows, and sub-volcanic dikes of tholeiitic basaltic composition are found to be members of the Vrinena, Aerino, Eretria, and Velestino dispersed Middle–Upper Jurassic ophiolitic units in East Othris. The Vrinena and Eretria ophiolitic units appear to have been emplaced onto the Pelagonian continental margin during the Upper Jurassic–Lower Cretaceous, whereas the Aerino and Velestino units seem to have been finally emplaced during post-Palaeocene times. Geochemically these are divided into two groups: Group I includes subduction-related boninites and low-Ti basalts from the Vrinena and Aerino units, and Group II high-Ti basalts show spreading-type characteristics occurring in the Eretria and Velestino units. Primary magma of the Group I volcanics appears to have been formed after high partial melting degrees (~18%) of a highly depleted harzburgitic mantle source, under relatively high temperatures (mantle potential temperature ~1372°C). Petrogenetic modelling also suggests that the primary magma of the Group II volcanics were formed after lower partial melting degrees (~7%) of a moderately depleted mantle source. The petrological and geochemical data from the East Othris dispersed and diversely emplaced ophiolitic units provide evidence of a common intra-oceanic supra-subduction zone (SSZ) origin within the Pindos oceanic strand of the Western Tethys. Specifically, Group I lavas and dikes from Vrinena seem to represent the extrusive part of an almost complete fore- to island-arc ophiolitic sequence. Dikes of Aerino most likely correspond to fore-arc magmatic material that intruded within exhumed serpentinized ultramafic rocks through a subduction channel that developed close to the slab and towards the fore-arc and the accretionary prism. The Group II volcanics either corresponded to a fore-arc magmatic expression, which extruded earlier than Group I volcanics and prior to the establishment of a mature subduction zone, or represent back-arc to island-arc magmatism that was contemporaneous to the fore-arc magmatic activity during rollback subduction.
DOI: 10.6084/m9.figshare.3462677.v1
title: Boninitic and tholeiitic basaltic lavas and dikes from dispersed Jurassic East Othris ophiolitic units, Greece: petrogenesis and geodynamic implications

description: Pillow lavas, massive lava flows, and sub-volcanic dikes of tholeiitic basaltic composition are found to be members of the Vrinena, Aerino, Eretria, and Velestino dispersed Middle–Upper Jurassic ophiolitic units in East Othris. The Vrinena and Eretria ophiolitic units appear to have been emplaced onto the Pelagonian continental margin during the Upper Jurassic–Lower Cretaceous, whereas the Aerino and Velestino units seem to have been finally emplaced during post-Palaeocene times. Geochemically these are divided into two groups: Group I includes subduction-related boninites and low-Ti basalts from the Vrinena and Aerino units, and Group II high-Ti basalts show spreading-type characteristics occurring in the Eretria and Velestino units. Primary magma of the Group I volcanics appears to have been formed after high partial melting degrees (~18%) of a highly depleted harzburgitic mantle source, under relatively high temperatures (mantle potential temperature ~1372°C). Petrogenetic modelling also suggests that the primary magma of the Group II volcanics were formed after lower partial melting degrees (~7%) of a moderately depleted mantle source. The petrological and geochemical data from the East Othris dispersed and diversely emplaced ophiolitic units provide evidence of a common intra-oceanic supra-subduction zone (SSZ) origin within the Pindos oceanic strand of the Western Tethys. Specifically, Group I lavas and dikes from Vrinena seem to represent the extrusive part of an almost complete fore- to island-arc ophiolitic sequence. Dikes of Aerino most likely correspond to fore-arc magmatic material that intruded within exhumed serpentinized ultramafic rocks through a subduction channel that developed close to the slab and towards the fore-arc and the accretionary prism. The Group II volcanics either corresponded to a fore-arc magmatic expression, which extruded earlier than Group I volcanics and prior to the establishment of a mature subduction zone, or represent back-arc to island-arc magmatism that was contemporaneous to the fore-arc magmatic activity during rollback subduction.
DOI: 10.6084/m9.figshare.3462656
title: Variation in rhyolitic magma composition linked with fractionation from a common source: insights from the Rotoiti eruption, Taupo Volcanic Zone, New Zealand

description: The Taupo Volcanic Zone (TVZ), New Zealand, is a well-documented volcanic arc characterized by explosive rhyolitic magmas within a series of caldera complexes that include the Okataina Volcanic Centre (OVC). New quartz melt inclusion and volcanic glass data from the 45 ka caldera-forming Rotoiti eruption within the OVC are compared to published studies. The new data are characterized by low K<sub>2</sub>O (~1.5–3.5 wt.%), Rb (~30–70 ppm), Sr (~40–90 ppm), U (~0.5–2.5 ppm), and Ba (~300–1000 ppm) ranges that differ significantly from other OVC systems (~3.0–4.5 wt.% K<sub>2</sub>O, ~80–150 ppm Rb, and ~2.5–5.0 ppm U). Most interestingly, the Rotoiti melt inclusion data measured in this study show a decrease in Rb, Sr, and U, although the fractionation trends originate from the same source point as published OVC data. This progressive decreasing trend is interpreted as an interaction with a less enriched rhyolitic melt (represented by the low Rb, Sr, and U of glasses) during fractionation processes from a common TVZ source. The established model for TVZ rhyolites is that they are extracted from a middle or upper crustal source (‘mush’ zone) prior to eruption. Adding to this model, new melt inclusion data suggest that all TVZ rhyolites are fractionated from this common TVZ source and, prior to eruption, the Rotoiti system was rejuvenated by this source (evidenced by the low REE glasses). Exactly what triggers the common TVZ source to fractionate remains unclear, but a proposed mechanism to account for this involves the successive melting of the upper crust by upwelling mantle induced by incremental subduction.
DOI: 10.6084/m9.figshare.3462656.v1
title: Variation in rhyolitic magma composition linked with fractionation from a common source: insights from the Rotoiti eruption, Taupo Volcanic Zone, New Zealand

description: The Taupo Volcanic Zone (TVZ), New Zealand, is a well-documented volcanic arc characterized by explosive rhyolitic magmas within a series of caldera complexes that include the Okataina Volcanic Centre (OVC). New quartz melt inclusion and volcanic glass data from the 45 ka caldera-forming Rotoiti eruption within the OVC are compared to published studies. The new data are characterized by low K<sub>2</sub>O (~1.5–3.5 wt.%), Rb (~30–70 ppm), Sr (~40–90 ppm), U (~0.5–2.5 ppm), and Ba (~300–1000 ppm) ranges that differ significantly from other OVC systems (~3.0–4.5 wt.% K<sub>2</sub>O, ~80–150 ppm Rb, and ~2.5–5.0 ppm U). Most interestingly, the Rotoiti melt inclusion data measured in this study show a decrease in Rb, Sr, and U, although the fractionation trends originate from the same source point as published OVC data. This progressive decreasing trend is interpreted as an interaction with a less enriched rhyolitic melt (represented by the low Rb, Sr, and U of glasses) during fractionation processes from a common TVZ source. The established model for TVZ rhyolites is that they are extracted from a middle or upper crustal source (‘mush’ zone) prior to eruption. Adding to this model, new melt inclusion data suggest that all TVZ rhyolites are fractionated from this common TVZ source and, prior to eruption, the Rotoiti system was rejuvenated by this source (evidenced by the low REE glasses). Exactly what triggers the common TVZ source to fractionate remains unclear, but a proposed mechanism to account for this involves the successive melting of the upper crust by upwelling mantle induced by incremental subduction.
DOI: 10.6084/m9.figshare.3462641
title: U–Pb detrital zircon evidence of transcontinental sediment dispersal: provenance of Late Mississippian Wedington Sandstone member, NW Arkansas

description: U–Pb ages of detrital zircons from the Wedington Sandstone member in northwest Arkansas provide evidence for Late Mississippian westward transcontinental sediment transport from the Appalachian foreland. The Late Mississippian Wedington Sandstone member of the Fayetteville Shale is a fine- to medium-grained quartzarenite. It separates the Fayetteville Shale into informal lower and upper intervals, and was deposited as a small constructive delta complex that prograded towards the south and southeast during the Late Mississippian. As a major influx of clastic sediments, the Wedington Sandstone member records the sediment source and dispersal in the mid-continent during the Late Mississippian. A total of 559 detrital zircon grains from six Wedington samples were recovered for U–Pb detrital zircon geochronological analysis. Results show that age distributions can be subdivided into six groups: ~350–500, ~900–1350, ~1360–1500, ~1600–1800, ~1800–2300, and &gt; ~2500 Ma, and are characterized by a prominent peak for the age group of ~900–1350 Ma, a major peak at ~1600–1800 Ma, and a few other minor age clusters. Regional correlation and geological evidence from surrounding areas suggest that the transcontinental sediment dispersal started as early as the Late Mississippian. U–Pb detrital zircon age distribution suggests that the Wedington Sandstone member was likely derived from the Appalachian foreland with contributions from the Nemaha Ridge to the west where the Yavapai–Mazatzal sources were exposed during the Late Mississippian. Sediment was likely transported westward through or around the Illinois Basin, merged with mid-continent sediment, and then entered into its current location in northwest Arkansas. Transportation of this sediment from mixed sources continued along its course to the south, forming a delta on the Northern Arkansas Structural Platform.
DOI: 10.6084/m9.figshare.3462641.v1
title: U–Pb detrital zircon evidence of transcontinental sediment dispersal: provenance of Late Mississippian Wedington Sandstone member, NW Arkansas

description: U–Pb ages of detrital zircons from the Wedington Sandstone member in northwest Arkansas provide evidence for Late Mississippian westward transcontinental sediment transport from the Appalachian foreland. The Late Mississippian Wedington Sandstone member of the Fayetteville Shale is a fine- to medium-grained quartzarenite. It separates the Fayetteville Shale into informal lower and upper intervals, and was deposited as a small constructive delta complex that prograded towards the south and southeast during the Late Mississippian. As a major influx of clastic sediments, the Wedington Sandstone member records the sediment source and dispersal in the mid-continent during the Late Mississippian. A total of 559 detrital zircon grains from six Wedington samples were recovered for U–Pb detrital zircon geochronological analysis. Results show that age distributions can be subdivided into six groups: ~350–500, ~900–1350, ~1360–1500, ~1600–1800, ~1800–2300, and &gt; ~2500 Ma, and are characterized by a prominent peak for the age group of ~900–1350 Ma, a major peak at ~1600–1800 Ma, and a few other minor age clusters. Regional correlation and geological evidence from surrounding areas suggest that the transcontinental sediment dispersal started as early as the Late Mississippian. U–Pb detrital zircon age distribution suggests that the Wedington Sandstone member was likely derived from the Appalachian foreland with contributions from the Nemaha Ridge to the west where the Yavapai–Mazatzal sources were exposed during the Late Mississippian. Sediment was likely transported westward through or around the Illinois Basin, merged with mid-continent sediment, and then entered into its current location in northwest Arkansas. Transportation of this sediment from mixed sources continued along its course to the south, forming a delta on the Northern Arkansas Structural Platform.
DOI: 10.6084/m9.figshare.3462620
title: COAF, Jisc and RCUK APC data 2013-2015

description: This is the data set used for the report "Article processing charges (APCs) and subscriptions: Monitoring open access costs."<br>The data joins all existing COAF, Jisc, and RCUK APC data. The data processing steps were: <br>- De-deduplicating along DOI and title- Filling in missing data fields using CrossRef and EPMC- Using DOAJ to check if ISSN is Full OA or hybrid- Converting currency where needed based on ForEx yearly averages- Standardizing spellings, date formatting, etc.<br>One institution asked that their article-level data not be made publicly available, and therefore was excluded from this data set.
DOI: 10.6084/m9.figshare.3462617
title: Mg fluid_data for PlosOne 2016.xlsx

description: Excel file with patient´s data collected according to methodology described in the Methods Section and in the flow chart (Fig.2).
DOI: 10.6084/m9.figshare.3462617.v1
title: Mg fluid_data for PlosOne 2016.xlsx

description: Excel file with patient´s data collected according to methodology described in the Methods Section and in the flow chart (Fig.2).
DOI: 10.6084/m9.figshare.3462608
title: Dataset_Somapsyche.sav

description: Dataset belonging to publication: <br>Haverkamp GL, Torensma B, Vergouwen ACM, Honig A. Psychological distress in the hospital setting: a comparison between native Dutch and immigrant patients. <i>PLoS One</i><i>. 2015 Jun 25;10(6):e0130961</i><br>
DOI: 10.6084/m9.figshare.3462608.v1
title: Dataset_Somapsyche.sav

description: Dataset belonging to publication: <br>Haverkamp GL, Torensma B, Vergouwen ACM, Honig A. Psychological distress in the hospital setting: a comparison between native Dutch and immigrant patients. <i>PLoS One</i><i>. 2015 Jun 25;10(6):e0130961</i><br>
DOI: 10.6084/m9.figshare.3462605
title: Supplementary Material for: Power Comparisons of Methods for Joint Association Analysis of Multiple Phenotypes

description: <i>Background/Aims:</i> Genome-wide association studies (GWAS) have identified many variants that each affect multiple phenotypes, which suggests that pleiotropic effects on human complex phenotypes may be widespread. Therefore, statistical methods that can jointly analyze multiple phenotypes in GWAS may have advantages over analyzing each phenotype individually. Several statistical methods have been developed to utilize such multivariate phenotypes in genetic association studies; however, the performance of these methods under different scenarios is largely unknown. Our goal was to provide researchers with useful guidelines on selecting statistical methods for the application of real data to multiple phenotypes. <i>Methods:</i>In this study, we evaluated the performance of some of the existing methods for association studies using multiple phenotypes. These methods included the O'Brien method (OB), cross-validation method (CV), optimal weight method (OW), Trait-based Association Test that uses Extended Simes procedure (TATES), principal components of heritability (PCH), canonical correlation analysis (CCA), multivariate analysis of variance (MANOVA), and a joint model of multiple phenotypes (MultiPhen). We used simulation studies to compare the powers of these methods under a variety of scenarios, including different numbers of phenotypes, different values of between-phenotype correlation, different minor allele frequencies, and different mean and variance models. <i>Results and Conclusion:</i> Our simulation results show that there is no single method with consistently good performance among all the scenarios. Each method has its own advantages and disadvantages.
DOI: 10.6084/m9.figshare.3462605.v1
title: Supplementary Material for: Power Comparisons of Methods for Joint Association Analysis of Multiple Phenotypes

description: <i>Background/Aims:</i> Genome-wide association studies (GWAS) have identified many variants that each affect multiple phenotypes, which suggests that pleiotropic effects on human complex phenotypes may be widespread. Therefore, statistical methods that can jointly analyze multiple phenotypes in GWAS may have advantages over analyzing each phenotype individually. Several statistical methods have been developed to utilize such multivariate phenotypes in genetic association studies; however, the performance of these methods under different scenarios is largely unknown. Our goal was to provide researchers with useful guidelines on selecting statistical methods for the application of real data to multiple phenotypes. <i>Methods:</i>In this study, we evaluated the performance of some of the existing methods for association studies using multiple phenotypes. These methods included the O'Brien method (OB), cross-validation method (CV), optimal weight method (OW), Trait-based Association Test that uses Extended Simes procedure (TATES), principal components of heritability (PCH), canonical correlation analysis (CCA), multivariate analysis of variance (MANOVA), and a joint model of multiple phenotypes (MultiPhen). We used simulation studies to compare the powers of these methods under a variety of scenarios, including different numbers of phenotypes, different values of between-phenotype correlation, different minor allele frequencies, and different mean and variance models. <i>Results and Conclusion:</i> Our simulation results show that there is no single method with consistently good performance among all the scenarios. Each method has its own advantages and disadvantages.
DOI: 10.15131/shef.data.3462599
title: Interspeech 2016 - Experiment results for the paper "Combining weak tokenisers for phonotactic language recognition in a resource-constrained setting"

description: This dataset contains the test results for the experiments described in the interspeech 2016 paper "Combining weak tokenisers for phonotactic language recognition in a resource-constrained setting" DOI: 10.21437/Interspeech.2016-630.<br><br>The folders are organised in TABLE_2 / TABLE_3 and TABLE_4. In each folder, there are multiple *.detectionscore.DCF files. They are the scoring results based on different experimental conditions.<br><br>In the top directory, three csh scripts <br>gen_TABLE_2_results.csh<br>gen_TABLE_3_results.csh<br>gen_TABLE_4_results.csh<br>are included. When executed, it will automatically extract the relevant scores from the folder and displays the language recognition results as described in the paper.<br><br><br>
DOI: 10.15131/shef.data.3462599.v1
title: Interspeech 2016 - Experiment results for the paper "Combining weak tokenisers for phonotactic language recognition in a resource-constrained setting"

description: This dataset contains the test results for the experiments described in the interspeech 2016 paper "Combining weak tokenisers for phonotactic language recognition in a resource-constrained setting" DOI: 10.21437/Interspeech.2016-630.<br><br>The folders are organised in TABLE_2 / TABLE_3 and TABLE_4. In each folder, there are multiple *.detectionscore.DCF files. They are the scoring results based on different experimental conditions.<br><br>In the top directory, three csh scripts <br>gen_TABLE_2_results.csh<br>gen_TABLE_3_results.csh<br>gen_TABLE_4_results.csh<br>are included. When executed, it will automatically extract the relevant scores from the folder and displays the language recognition results as described in the paper.<br><br><br>
DOI: 10.6084/m9.figshare.3462578
title: Panshanger static 06062016 to 13062016

description: Echolocation recordings from the 6th to the 13th of June at Panshanger Park by the big Cedar tree
DOI: 10.6084/m9.figshare.3462578.v2
title: Panshanger static 06062016 to 13062016

description: Echolocation recordings from the 6th to the 13th of June at Panshanger Park by the big Cedar tree
DOI: 10.6084/m9.figshare.3462578.v1
title: Panshanger static 06062016 to 13062016

description: Echolocation recordings from the 6th to the 13th of June at Panshanger Park by the big Cedar tree
DOI: 10.6084/m9.figshare.3462575
title: Elevated Chemerin Levels in Pakistani Men: An Interrelation with Metabolic Syndrome Phenotypes

description: Table 2. Correlation of serum chemerin levels with study parameters.Fasting insulin was measured using an ELISA kit (DIA source Immuno Assay S.A., Belgium). Insulin resistance was calculated using the homeostasis model assessment of insulin resistance (HOMA-IR) index [fasting insulin (units per milliliter) x fasting glucose milligram/deciliter)/405]. The body fat percentage was measured using Diagnostic Scale BG55 (Beurer Germany) through bioelectrical impedance matching/analysis. Serum chemerin levels were measured with an enzyme immunoassay kit (Creative Diagnostics, USA,www.creative-diagnostics.com), with a sensitivity of less than 3 pg/ml, using ELISA plate reader equalizer ER 2005, (Eqiupar, Italy).<br>