cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.12254489.v1
title: Influence of winter feeding on colony development and the antioxidant system of the honey bee, <i>Apis mellifera</i>

description: The effects of supplementary feeding (artificial diet cake + sucrose syrup supplemented with vitamin C) for different periods (feeding for 12, 15 and 18 weeks) on colony development, protein content and antioxidant system in newly emerged workers were investigated from October to March for two consecutive beekeeping seasons. Sugar syrup was used as the control. The results revealed that there was a marked increase in colony growth parameters (sealed brood areas and adult bee population sizes) in colonies provided with supplemental diet for different periods compared to control colonies. Moreover, colonies fed longest (feeding for 18 weeks) recorded significantly higher sealed brood areas and adult bee population sizes in comparison to other treatment groups. Also, activities of superoxide dismutase (SOD) and catalase (CAT) enzymes together with levels of glutathione (GSH) and lipid peroxidation (LPO) were measured in newly emerged honey bee workers sampled from colonies fed supplemental diet for different periods and control group. There was a clear improvement in the antioxidant system in bee colonies that were provided with supplemental diet for 18 weeks compared to other treatments and control ones. This suggests that honey bee workers supplemented with artificial feeding during the winter season possess mechanisms that reduce their oxidative stress. Together, our results suggest that supplemental winter feeding for 18 weeks (from 1 November to 11 March) has the potential to improve colony development and health during overwintering, a period of elevated colony losses.
DOI: 10.21227/ej8z-mq69
title: Result For Paraphrase Generation

description: Including Code & Result of the paper "Unsupervised Paraphrasing via Sentence Reconstruction and Back-translation"
DOI: 10.21227/xtgj-vj53
title: Result For Paraphrase Generation

description: Including Code & Result of the paper "Unsupervised Paraphrasing via Sentence Reconstruction and Back-translation"
DOI: 10.6084/m9.figshare.12957254
title: Shapefile.zip

description: This contain shapefile of land use 2013 and 2019 and also the suitability with spatial plan.<br>
DOI: 10.5281/zenodo.4024252
title: Experiment: Prominent anchor time of French FID

description: This is the data set of a forced-choice experiment concerning the temporal anchoring of free indirect discourse events in French. The experiment confirms the findings of a previous corpus study.
description: The work was supported by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) as part of the Collaborative Research Center 1252 Prominence in Language, Project-ID 281511265, which is gratefully acknowledged. I want to thank Barbara Zeyer and David Wick for practical assistance, Fahime Same for help with the experimental setup and Clémentine Raffy and Marine Espinat for input concerning the experimental items. I thank all of the participants in the study.
DOI: 10.5281/zenodo.4024251
title: Experiment: Prominent anchor time of French FID

description: This is the data set of a forced-choice experiment concerning the temporal anchoring of free indirect discourse events in French. The experiment confirms the findings of a previous corpus study.
description: The work was supported by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) as part of the Collaborative Research Center 1252 Prominence in Language, Project-ID 281511265, which is gratefully acknowledged. I want to thank Barbara Zeyer and David Wick for practical assistance, Fahime Same for help with the experimental setup and Clémentine Raffy and Marine Espinat for input concerning the experimental items. I thank all of the participants in the study.
DOI: 10.25392/leicester.data.12937583.v1
title: Raw data for Choudhury et al., 2020

description: This excel spreadsheet contains the data for the Choudhury et al., 2020 research article.<br>Choudhury et al., J. Physiol 598.11 pp2199-2222, 2020DOI: 10.1113/JP279668
DOI: 10.25392/leicester.data.12937583
title: Raw data for Choudhury et al., 2020

description: This excel spreadsheet contains the data for the Choudhury et al., 2020 research article.<br>Choudhury et al., J. Physiol 598.11 pp2199-2222, 2020DOI: 10.1113/JP279668
DOI: 10.25392/leicester.data.12937523
title: Summary Data for Choudhury et al., 2020

description: This is the summary data and statistics for the research paper published in the Journals of Physiology: Choudhury et al., J Physiol 598.11 pp 2199–2222. 2020.DOI: 10.1113/JP279668
DOI: 10.25392/leicester.data.12937523.v1
title: Summary Data for Choudhury et al., 2020

description: This is the summary data and statistics for the research paper published in the Journals of Physiology: Choudhury et al., J Physiol 598.11 pp 2199–2222. 2020.DOI: 10.1113/JP279668
DOI: 10.21227/q1yh-wd43
title: Key parameters of the sensor test experimental data

description: In order to test the performance of the proposed sensor, the measurement error of the original sensor is tested.In addition, error test, stability test and repeatability test are carried out for the optimized sensor model.
DOI: 10.21227/thw7-m249
title: Key parameters of the sensor test experimental data

description: In order to test the performance of the proposed sensor, the measurement error of the original sensor is tested.In addition, error test, stability test and repeatability test are carried out for the optimized sensor model.
DOI: 10.6084/m9.figshare.11687064.v2
title: Example Dataset for BIDS Manager

description: This folder contains data from a fictional participants that you can use to test BIDS Manager (https://github.com/Dynamap/BIDS_Manager).
DOI: 10.5281/zenodo.4030412
title: Replication package for: "What Would You Do with $500? Spending Responses to Gains, Losses, News and Loans"

description: The package contains all the code and data necessary to reproduce the tables and figures in Fuster, Kaplan and Zafar, "What Would You Do with $500? Spending Responses to Gains, Losses, News and Loans", Review of Economic Studies.
DOI: 10.6084/m9.figshare.12957341.v1
title: Figure2

description: Fluence to Ambient dose equivalent conversion coefficients from the Fluka database<br>
DOI: 10.6084/m9.figshare.12957389.v1
title: Dataset on concentrations of different elements in deionized and ultrapure water

description: This dataset describes the concentrations of elements in deionized and ultrapure water detected using the technique of inductively coupled plasma mass spectrometry (ICP-MS). Instrument used was Agilent 7500a ICP-MS calibrated by Merck multi-element ICP calibration standard.
DOI: 10.6084/m9.figshare.12957389
title: Dataset on concentrations of different elements in deionized and ultrapure water

description: This dataset describes the concentrations of elements in deionized and ultrapure water detected using the technique of inductively coupled plasma mass spectrometry (ICP-MS). Instrument used was Agilent 7500a ICP-MS calibrated by Merck multi-element ICP calibration standard.
DOI: 10.18112/openneuro.ds003148.v1.0.0
title: Neuroimaging evidence for network sampling theory of human intelligence
DOI: 10.6084/m9.figshare.12957422
title: Supplementary material for "Meta-analysis shows the evidence for context-dependent mating behaviour is inconsistent or weak across animals"

description: Supplementary data, methods and results for: Dougherty, LR (2020). Meta-analysis shows the evidence for context-dependent mating behaviour is inconsistent or weak across animals. Ecology Letters.<br>Contains:- Supplementary methods- List of studies included in the meta-analysis- List of studies excluded after reading full-texts- Supplementary results<br>- Excel file with six datasets: with and without directionless effect sizes for three behaviours (sexual signalling, responsiveness, choosiness). - TRE files for the six phylogenies - R code for the three behaviours
DOI: 10.6084/m9.figshare.12957422.v1
title: Supplementary material for "Meta-analysis shows the evidence for context-dependent mating behaviour is inconsistent or weak across animals"

description: Supplementary data, methods and results for: Dougherty, LR (2020). Meta-analysis shows the evidence for context-dependent mating behaviour is inconsistent or weak across animals. Ecology Letters.<br>Contains:- Supplementary methods- List of studies included in the meta-analysis- List of studies excluded after reading full-texts- Supplementary results<br>- Excel file with six datasets: with and without directionless effect sizes for three behaviours (sexual signalling, responsiveness, choosiness). - TRE files for the six phylogenies - R code for the three behaviours
DOI: 10.15161/oar.it/30703
title: CovidStat project data

description: This record contains the daily updated data of the CovidStat project. CovidStat is a project carried out by the CovidStat Working Group at INFN, whose creation was promoted within the Italian National Institute of Nuclear Physics with the aim of making a statistical analysis of the data provided daily by the Civil Protection on the spread of the pandemic in Italy. CovidStat data can interactively be browsed at https://covid19.infn.it.
description: The software to process this Root TTree is in the related identifier. Be sure to use the right corresponding version, based on the data in which Root TTree was generated.
DOI: 10.5525/gla.researchdata.1029
title: Seeing around corners: cells solve mazes and respond at a distance using attractant breakdown
DOI: 10.6084/m9.figshare.11768610.v1
title: The Dunedin Volcanic Group and a revised model for Zealandia's alkaline intraplate volcanism

description: The intraplate rocks of the Dunedin Volcanic Group (DVG) in New Zealand’s South Island erupted in two discrete areas between 25 and 21 Ma before becoming distributed over &gt; 7,800 km<sup>2</sup> until ∼9 Ma. Although most eruptive centres were of small volume and mainly vented alkaline basanite, the largest centre–the 16–11 Ma composite Dunedin Volcano–discharged basanite and basalt through to trachyte and phonolite. DVG components were mainly derived from mantle sources with <sup>87</sup>Sr/<sup>86</sup>Sr = ∼0.7029, <sup>143</sup>Nd/<sup>144</sup>Nd = ∼0.5129, <sup>206</sup>Pb/<sup>204</sup>Pb = ∼20.0, <sup>207</sup>Pb/<sup>204</sup>Pb = ∼15.65, <sup>208</sup>Pb/<sup>204</sup>Pb = 39.5 and εHf = +3.5 to + 10.1 that extended to anomalously light δ<sup>26</sup>Mg (−0.47). Exceptions are some potassic basalts in NW of the field with elevated <sup>207</sup>Pb/<sup>204</sup>Pb and more radiogenic Sr. The DVG Sr-Nd-Pb isotopes mostly overlap with metasomatised anhydrous mantle peridotite xenoliths but have less radiogenic Hf, meaning that equivalent anhydrous mantle rock-types cannot be the sole magma sources. Although there is debate regarding whether DVG was derived from the lithospheric or asthenospheric mantle, intermittent melting of a middle lithospheric mantle metasomatised by hydrous asthenosphere-derived melts could account for: (1) the widely distributed magmatism for ∼16 Myr during which time Otago lithosphere shifted NW ∼ 870 km over the asthenosphere; (2) the small chemical range of the least evolved magmas; (3) the Sr-Nd-Pb-Hf isotopic range; and (4) an absence of lower lithosphere mantle xenoliths. This process could account for other occurrences of isotopically restricted Zealandia alkaline intraplate volcanism.
DOI: 10.6084/m9.figshare.11768610
title: The Dunedin Volcanic Group and a revised model for Zealandia's alkaline intraplate volcanism

description: The intraplate rocks of the Dunedin Volcanic Group (DVG) in New Zealand’s South Island erupted in two discrete areas between 25 and 21 Ma before becoming distributed over &gt; 7,800 km<sup>2</sup> until ∼9 Ma. Although most eruptive centres were of small volume and mainly vented alkaline basanite, the largest centre–the 16–11 Ma composite Dunedin Volcano–discharged basanite and basalt through to trachyte and phonolite. DVG components were mainly derived from mantle sources with <sup>87</sup>Sr/<sup>86</sup>Sr = ∼0.7029, <sup>143</sup>Nd/<sup>144</sup>Nd = ∼0.5129, <sup>206</sup>Pb/<sup>204</sup>Pb = ∼20.0, <sup>207</sup>Pb/<sup>204</sup>Pb = ∼15.65, <sup>208</sup>Pb/<sup>204</sup>Pb = 39.5 and εHf = +3.5 to + 10.1 that extended to anomalously light δ<sup>26</sup>Mg (−0.47). Exceptions are some potassic basalts in NW of the field with elevated <sup>207</sup>Pb/<sup>204</sup>Pb and more radiogenic Sr. The DVG Sr-Nd-Pb isotopes mostly overlap with metasomatised anhydrous mantle peridotite xenoliths but have less radiogenic Hf, meaning that equivalent anhydrous mantle rock-types cannot be the sole magma sources. Although there is debate regarding whether DVG was derived from the lithospheric or asthenospheric mantle, intermittent melting of a middle lithospheric mantle metasomatised by hydrous asthenosphere-derived melts could account for: (1) the widely distributed magmatism for ∼16 Myr during which time Otago lithosphere shifted NW ∼ 870 km over the asthenosphere; (2) the small chemical range of the least evolved magmas; (3) the Sr-Nd-Pb-Hf isotopic range; and (4) an absence of lower lithosphere mantle xenoliths. This process could account for other occurrences of isotopically restricted Zealandia alkaline intraplate volcanism.
DOI: 10.6084/m9.figshare.12433766
title: Influence of host magma alkalinity on trachytic melts formed during incongruent orthopyroxene dissolution in mantle xenoliths

description: Spectacular reactions textures developed during the non-isochemical breakdown of orthopyroxene and spinel in peridotite mantle xenoliths in intraplate alkaline basalts from the Auckland Volcanic Field and the Dunedin Volcano in New Zealand, and Jeju Island in South Korea. Mantle orthopyroxene is replaced by symplectitic intergrowths of silica-rich glass and olivine (± clinopyroxene ± orthopyroxene) with individual minerals showing large diffusion gradients at their margins proximal to the host melt. The glasses are basaltic to trachytic and formed by incongruent melting of orthopyroxene and subsequent re-equilibration by diffusion and mixing during changing boundary conditions with the host magma. Although the glass composition is strongly dependent on the alkalinity of the host magma, the distance to the reacting contact and the respective phase assemblage that develops in the reaction zone (melt + ol ± clinopyroxene ± orthopyroxene), the most evolved melts converge at trachytic composition. Diffusion-driven Fe enrichment for mantle olivine indicates residence timescales within the host magma on the order of weeks to several months.
DOI: 10.6084/m9.figshare.12433766.v1
title: Influence of host magma alkalinity on trachytic melts formed during incongruent orthopyroxene dissolution in mantle xenoliths

description: Spectacular reactions textures developed during the non-isochemical breakdown of orthopyroxene and spinel in peridotite mantle xenoliths in intraplate alkaline basalts from the Auckland Volcanic Field and the Dunedin Volcano in New Zealand, and Jeju Island in South Korea. Mantle orthopyroxene is replaced by symplectitic intergrowths of silica-rich glass and olivine (± clinopyroxene ± orthopyroxene) with individual minerals showing large diffusion gradients at their margins proximal to the host melt. The glasses are basaltic to trachytic and formed by incongruent melting of orthopyroxene and subsequent re-equilibration by diffusion and mixing during changing boundary conditions with the host magma. Although the glass composition is strongly dependent on the alkalinity of the host magma, the distance to the reacting contact and the respective phase assemblage that develops in the reaction zone (melt + ol ± clinopyroxene ± orthopyroxene), the most evolved melts converge at trachytic composition. Diffusion-driven Fe enrichment for mantle olivine indicates residence timescales within the host magma on the order of weeks to several months.
DOI: 10.6084/m9.figshare.10115939
title: Petrology and petrogenesis of an intraplate alkaline lamprophyre-phonolite-carbonatite association in the Alpine Dyke Swarm, New Zealand

description: The Alpine Dyke Swarm (ADS), intruding Haast Schist in the Southern Alps, New Zealand, comprises dykes, sills and diatremes of alkaline and ultramafic lamprophyres, phonolites and carbonatites. Intrusion peaked at ∼25 Ma during inception of dextral transtensional displacement on the Alpine Fault plate boundary. In a chamber beneath Haast River, magmas evolved by fractional crystallisation from primitive lamprophyres to phonolites, and then by liquid immiscibility to carbonatite magmas. Carbonatitic magmas coexisted with a highly sodic fluid that metasomatised adjacent quartzofeldspathic schist to aegirine-albite fenites. Carbonatites fractionated from Ca- to Fe-rich and, under late-stage, hydrothermal conditions, to Ba-Sr-REE–rich varieties. Some lamprophyres rose directly from a highly refractory spinel- or possibly garnet-spinel peridotite mantle that had been extensively metasomatised prior to the low-degree partial melting event and Cr-diopside series nodule entrainment. Al-augite series nodules give ages similar to host lamprophyres and are interpreted as deep-seated cognate cumulates. Compared to the broadly coeval basaltic-basanitic magmas of the Dunedin Volcanic Group (DVG) of East Otago, ADS magmas are enriched in volatiles, LILE, and HFSE (including REE). DVG magmas were derived from a less metasomatised mantle source, and, although undergoing extensive fractionation, failed to achieve the extreme alkali enrichment necessary for silicate melt-carbonatite immiscibility.
DOI: 10.6084/m9.figshare.10115939.v1
title: Petrology and petrogenesis of an intraplate alkaline lamprophyre-phonolite-carbonatite association in the Alpine Dyke Swarm, New Zealand

description: The Alpine Dyke Swarm (ADS), intruding Haast Schist in the Southern Alps, New Zealand, comprises dykes, sills and diatremes of alkaline and ultramafic lamprophyres, phonolites and carbonatites. Intrusion peaked at ∼25 Ma during inception of dextral transtensional displacement on the Alpine Fault plate boundary. In a chamber beneath Haast River, magmas evolved by fractional crystallisation from primitive lamprophyres to phonolites, and then by liquid immiscibility to carbonatite magmas. Carbonatitic magmas coexisted with a highly sodic fluid that metasomatised adjacent quartzofeldspathic schist to aegirine-albite fenites. Carbonatites fractionated from Ca- to Fe-rich and, under late-stage, hydrothermal conditions, to Ba-Sr-REE–rich varieties. Some lamprophyres rose directly from a highly refractory spinel- or possibly garnet-spinel peridotite mantle that had been extensively metasomatised prior to the low-degree partial melting event and Cr-diopside series nodule entrainment. Al-augite series nodules give ages similar to host lamprophyres and are interpreted as deep-seated cognate cumulates. Compared to the broadly coeval basaltic-basanitic magmas of the Dunedin Volcanic Group (DVG) of East Otago, ADS magmas are enriched in volatiles, LILE, and HFSE (including REE). DVG magmas were derived from a less metasomatised mantle source, and, although undergoing extensive fractionation, failed to achieve the extreme alkali enrichment necessary for silicate melt-carbonatite immiscibility.
DOI: 10.6084/m9.figshare.12854676
title: Volcanoes buried in Te Riu-a-Māui/Zealandia sedimentary basins

description: Many volcanoes are buried within Te Riu-a-Māui/Zealandia sedimentary basins. Based on a large collection of seismic reflection and drillhole data, this paper outlines the morphology, location and age of over 400 volcanoes buried and preserved in offshore New Zealand basins. We discuss the relationships of these volcanoes to the timing and locations of the main tectonic events that shaped Zealandia in the last 105 Myr. Late Cretaceous volcanism mainly formed large (&gt;20 km<sup>3</sup>) composite cones and volcanic complexes that erupted along rift faults related to the break-up of Zealandia from south-eastern Gondwana. Cenozoic intraplate volcanic activity was widespread, typically forming clusters of scattered small-volume (&lt;1 km<sup>3</sup>) craters and cones. In contrast, large Cenozoic volcanic complexes, composite cones and shield volcanoes erupted along linear arcs associated with subduction along the Pacific-Australian plate boundary. In detail, the presence of pre-existing structures and types of host rocks also influence the passage of magma in the shallow (&lt;5 km) crust and the location of eruptive centres, regardless the tectonic setting of eruption. Insights from this work demonstrate the value of characterising volcanoes buried in sedimentary basins for improved understanding of the interplay between volcanism and plate tectonics in Zealandia and further afield.
DOI: 10.6084/m9.figshare.12854676.v2
title: Volcanoes buried in Te Riu-a-Māui/Zealandia sedimentary basins

description: Many volcanoes are buried within Te Riu-a-Māui/Zealandia sedimentary basins. Based on a large collection of seismic reflection and drillhole data, this paper outlines the morphology, location and age of over 400 volcanoes buried and preserved in offshore New Zealand basins. We discuss the relationships of these volcanoes to the timing and locations of the main tectonic events that shaped Zealandia in the last 105 Myr. Late Cretaceous volcanism mainly formed large (&gt;20 km<sup>3</sup>) composite cones and volcanic complexes that erupted along rift faults related to the break-up of Zealandia from south-eastern Gondwana. Cenozoic intraplate volcanic activity was widespread, typically forming clusters of scattered small-volume (&lt;1 km<sup>3</sup>) craters and cones. In contrast, large Cenozoic volcanic complexes, composite cones and shield volcanoes erupted along linear arcs associated with subduction along the Pacific-Australian plate boundary. In detail, the presence of pre-existing structures and types of host rocks also influence the passage of magma in the shallow (&lt;5 km) crust and the location of eruptive centres, regardless the tectonic setting of eruption. Insights from this work demonstrate the value of characterising volcanoes buried in sedimentary basins for improved understanding of the interplay between volcanism and plate tectonics in Zealandia and further afield.
DOI: 10.6084/m9.figshare.12854676.v1
title: Volcanoes buried in Te Riu-a-Māui/Zealandia sedimentary basins

description: Many volcanoes are buried within Te Riu-a-Māui/Zealandia sedimentary basins. Based on a large collection of seismic reflection and drillhole data, this paper outlines the morphology, location and age of over 400 volcanoes buried and preserved in offshore New Zealand basins. We discuss the relationships of these volcanoes to the timing and locations of the main tectonic events that shaped Zealandia in the last 105 Myr. Late Cretaceous volcanism mainly formed large (&gt;20 km<sup>3</sup>) composite cones and volcanic complexes that erupted along rift faults related to the break-up of Zealandia from south-eastern Gondwana. Cenozoic intraplate volcanic activity was widespread, typically forming clusters of scattered small-volume (&lt;1 km<sup>3</sup>) craters and cones. In contrast, large Cenozoic volcanic complexes, composite cones and shield volcanoes erupted along linear arcs associated with subduction along the Pacific-Australian plate boundary. In detail, the presence of pre-existing structures and types of host rocks also influence the passage of magma in the shallow (&lt;5 km) crust and the location of eruptive centres, regardless the tectonic setting of eruption. Insights from this work demonstrate the value of characterising volcanoes buried in sedimentary basins for improved understanding of the interplay between volcanism and plate tectonics in Zealandia and further afield.