cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.1011451
title: As table 2 but for precipitation responses to the surface temperature changes (d<em>P</em>/d<em>T</em>)

description: <b>Table 3.</b> As table 2 but for precipitation responses to the surface temperature changes (d<em>P</em>/d<em>T</em>). <strong>Abstract</strong> Global warming is expected to enhance fluxes of fresh water between the surface and atmosphere, causing wet regions to become wetter and dry regions drier, with serious implications for water resource management. Defining the wet and dry regions as the upper 30% and lower 70% of the precipitation totals across the tropics (30° S–30° N) each month we combine observations and climate model simulations to understand changes in the wet and dry regions over the period 1850–2100. Observed decreases in precipitation over dry tropical land (1950–2010) are also simulated by coupled atmosphere–ocean climate models (−0.3%/decade) with trends projected to continue into the 21st century. Discrepancies between observations and simulations over wet land regions since 1950 exist, relating to decadal fluctuations in El Niño southern oscillation, the timing of which is not represented by the coupled simulations. When atmosphere-only simulations are instead driven by observed sea surface temperature they are able to adequately represent this variability over land. Global distributions of precipitation trends are dominated by spatial changes in atmospheric circulation. However, the tendency for already wet regions to become wetter (precipitation increases with warming by 3% K<sup>−1</sup> over wet tropical oceans) and the driest regions drier (precipitation decreases of −2% K<sup>−1</sup> over dry tropical land regions) emerges over the 21st century in response to the substantial surface warming.
DOI: 10.6084/m9.figshare.1011451.v1
title: As table 2 but for precipitation responses to the surface temperature changes (d<em>P</em>/d<em>T</em>)

description: <b>Table 3.</b> As table 2 but for precipitation responses to the surface temperature changes (d<em>P</em>/d<em>T</em>). <strong>Abstract</strong> Global warming is expected to enhance fluxes of fresh water between the surface and atmosphere, causing wet regions to become wetter and dry regions drier, with serious implications for water resource management. Defining the wet and dry regions as the upper 30% and lower 70% of the precipitation totals across the tropics (30° S–30° N) each month we combine observations and climate model simulations to understand changes in the wet and dry regions over the period 1850–2100. Observed decreases in precipitation over dry tropical land (1950–2010) are also simulated by coupled atmosphere–ocean climate models (−0.3%/decade) with trends projected to continue into the 21st century. Discrepancies between observations and simulations over wet land regions since 1950 exist, relating to decadal fluctuations in El Niño southern oscillation, the timing of which is not represented by the coupled simulations. When atmosphere-only simulations are instead driven by observed sea surface temperature they are able to adequately represent this variability over land. Global distributions of precipitation trends are dominated by spatial changes in atmospheric circulation. However, the tendency for already wet regions to become wetter (precipitation increases with warming by 3% K<sup>−1</sup> over wet tropical oceans) and the driest regions drier (precipitation decreases of −2% K<sup>−1</sup> over dry tropical land regions) emerges over the 21st century in response to the substantial surface warming.
DOI: 10.6084/m9.figshare.1011449
title: Observed and simulated data sets and their properties

description: <b>Table 1.</b> Observed and simulated data sets and their properties. Ticks indicate the data set is used in the corresponding analysis. <strong>Abstract</strong> Global warming is expected to enhance fluxes of fresh water between the surface and atmosphere, causing wet regions to become wetter and dry regions drier, with serious implications for water resource management. Defining the wet and dry regions as the upper 30% and lower 70% of the precipitation totals across the tropics (30° S–30° N) each month we combine observations and climate model simulations to understand changes in the wet and dry regions over the period 1850–2100. Observed decreases in precipitation over dry tropical land (1950–2010) are also simulated by coupled atmosphere–ocean climate models (−0.3%/decade) with trends projected to continue into the 21st century. Discrepancies between observations and simulations over wet land regions since 1950 exist, relating to decadal fluctuations in El Niño southern oscillation, the timing of which is not represented by the coupled simulations. When atmosphere-only simulations are instead driven by observed sea surface temperature they are able to adequately represent this variability over land. Global distributions of precipitation trends are dominated by spatial changes in atmospheric circulation. However, the tendency for already wet regions to become wetter (precipitation increases with warming by 3% K<sup>−1</sup> over wet tropical oceans) and the driest regions drier (precipitation decreases of −2% K<sup>−1</sup> over dry tropical land regions) emerges over the 21st century in response to the substantial surface warming.
DOI: 10.6084/m9.figshare.1011450
title: Precipitation trend for different data sets over various time periods

description: <b>Table 2.</b> Precipitation trend for different data sets over various time periods. Statistically significant values at the 95% confidence level are marked bold. Δ<em>m</em> denotes the 95% confidence range. Trends from composite model runs are calculated from ensemble means. <strong>Abstract</strong> Global warming is expected to enhance fluxes of fresh water between the surface and atmosphere, causing wet regions to become wetter and dry regions drier, with serious implications for water resource management. Defining the wet and dry regions as the upper 30% and lower 70% of the precipitation totals across the tropics (30° S–30° N) each month we combine observations and climate model simulations to understand changes in the wet and dry regions over the period 1850–2100. Observed decreases in precipitation over dry tropical land (1950–2010) are also simulated by coupled atmosphere–ocean climate models (−0.3%/decade) with trends projected to continue into the 21st century. Discrepancies between observations and simulations over wet land regions since 1950 exist, relating to decadal fluctuations in El Niño southern oscillation, the timing of which is not represented by the coupled simulations. When atmosphere-only simulations are instead driven by observed sea surface temperature they are able to adequately represent this variability over land. Global distributions of precipitation trends are dominated by spatial changes in atmospheric circulation. However, the tendency for already wet regions to become wetter (precipitation increases with warming by 3% K<sup>−1</sup> over wet tropical oceans) and the driest regions drier (precipitation decreases of −2% K<sup>−1</sup> over dry tropical land regions) emerges over the 21st century in response to the substantial surface warming.
DOI: 10.6084/m9.figshare.1011449.v1
title: Observed and simulated data sets and their properties

description: <b>Table 1.</b> Observed and simulated data sets and their properties. Ticks indicate the data set is used in the corresponding analysis. <strong>Abstract</strong> Global warming is expected to enhance fluxes of fresh water between the surface and atmosphere, causing wet regions to become wetter and dry regions drier, with serious implications for water resource management. Defining the wet and dry regions as the upper 30% and lower 70% of the precipitation totals across the tropics (30° S–30° N) each month we combine observations and climate model simulations to understand changes in the wet and dry regions over the period 1850–2100. Observed decreases in precipitation over dry tropical land (1950–2010) are also simulated by coupled atmosphere–ocean climate models (−0.3%/decade) with trends projected to continue into the 21st century. Discrepancies between observations and simulations over wet land regions since 1950 exist, relating to decadal fluctuations in El Niño southern oscillation, the timing of which is not represented by the coupled simulations. When atmosphere-only simulations are instead driven by observed sea surface temperature they are able to adequately represent this variability over land. Global distributions of precipitation trends are dominated by spatial changes in atmospheric circulation. However, the tendency for already wet regions to become wetter (precipitation increases with warming by 3% K<sup>−1</sup> over wet tropical oceans) and the driest regions drier (precipitation decreases of −2% K<sup>−1</sup> over dry tropical land regions) emerges over the 21st century in response to the substantial surface warming.
DOI: 10.6084/m9.figshare.1011450.v1
title: Precipitation trend for different data sets over various time periods

description: <b>Table 2.</b> Precipitation trend for different data sets over various time periods. Statistically significant values at the 95% confidence level are marked bold. Δ<em>m</em> denotes the 95% confidence range. Trends from composite model runs are calculated from ensemble means. <strong>Abstract</strong> Global warming is expected to enhance fluxes of fresh water between the surface and atmosphere, causing wet regions to become wetter and dry regions drier, with serious implications for water resource management. Defining the wet and dry regions as the upper 30% and lower 70% of the precipitation totals across the tropics (30° S–30° N) each month we combine observations and climate model simulations to understand changes in the wet and dry regions over the period 1850–2100. Observed decreases in precipitation over dry tropical land (1950–2010) are also simulated by coupled atmosphere–ocean climate models (−0.3%/decade) with trends projected to continue into the 21st century. Discrepancies between observations and simulations over wet land regions since 1950 exist, relating to decadal fluctuations in El Niño southern oscillation, the timing of which is not represented by the coupled simulations. When atmosphere-only simulations are instead driven by observed sea surface temperature they are able to adequately represent this variability over land. Global distributions of precipitation trends are dominated by spatial changes in atmospheric circulation. However, the tendency for already wet regions to become wetter (precipitation increases with warming by 3% K<sup>−1</sup> over wet tropical oceans) and the driest regions drier (precipitation decreases of −2% K<sup>−1</sup> over dry tropical land regions) emerges over the 21st century in response to the substantial surface warming.
DOI: 10.6084/m9.figshare.1011438
title: Scombroid Fishes Provide Novel Insights into the Trait/Rate Associations of Molecular Evolution

description: The study of which life history traits primarily affect molecular evolutionary rates is often confounded by the covariance of these traits. Scombroid fishes (billfishes, tunas, barracudas, and their relatives) are unusual in that their mass-specific metabolic rate is positively associated with body size. This study exploits this atypical pattern of trait variation, which allows for direct tests of whether mass-specific metabolic rate or body size is the more important factor of molecular evolutionary rates. We inferred a phylogeny for scombroids from a supermatrix of molecular and morphological characters and used new phylogenetic comparative approaches to assess the associations of body size and mass-specific metabolic rate with substitution rate. As predicted by the body size hypothesis, there is a negative correlation between body size and substitution rate. However, unexpectedly, we also find a negative association between mass-specific metabolic and substitution rates. These relationships are supported by analyses of the total molecular data, separate mitochondrial and nuclear genes, and individual loci, and they are robust to phylogenetic uncertainty. The molecular evolutionary rates of scombroids are primarily tied to body size. This study demonstrates that groups with novel patterns of trait variation can be particularly informative for identifying which life history traits are the primary factors of molecular evolutionary rates.
DOI: 10.6084/m9.figshare.1011438.v1
title: Scombroid Fishes Provide Novel Insights into the Trait/Rate Associations of Molecular Evolution

description: The study of which life history traits primarily affect molecular evolutionary rates is often confounded by the covariance of these traits. Scombroid fishes (billfishes, tunas, barracudas, and their relatives) are unusual in that their mass-specific metabolic rate is positively associated with body size. This study exploits this atypical pattern of trait variation, which allows for direct tests of whether mass-specific metabolic rate or body size is the more important factor of molecular evolutionary rates. We inferred a phylogeny for scombroids from a supermatrix of molecular and morphological characters and used new phylogenetic comparative approaches to assess the associations of body size and mass-specific metabolic rate with substitution rate. As predicted by the body size hypothesis, there is a negative correlation between body size and substitution rate. However, unexpectedly, we also find a negative association between mass-specific metabolic and substitution rates. These relationships are supported by analyses of the total molecular data, separate mitochondrial and nuclear genes, and individual loci, and they are robust to phylogenetic uncertainty. The molecular evolutionary rates of scombroids are primarily tied to body size. This study demonstrates that groups with novel patterns of trait variation can be particularly informative for identifying which life history traits are the primary factors of molecular evolutionary rates.
DOI: 10.6084/m9.figshare.1011379
title: Examples of sparql queries to browse the library of eligibility criteria

description: File contains example of sparql queries that can be used to browse the library of structured eligibility criteria available at [1]. The queries can be executed at this endpoint [2], for example using yasgui [3].
DOI: 10.6084/m9.figshare.1010377
title: Biofuel production (2011)

description: <b>Table 1.</b> Biofuel production (2011). Source: [11]. <strong>Abstract</strong> The perspective by Haberl <em>et al</em> (2013 <em>Environ. Res. Lett.</em> <strong>8</strong> 031004) entitled 'Bioenergy: how much can we expect for 2050?' is timely and valuable. It deals with an important subject since contrasting views on the subject make it very difficult for policy makers to adopt policies that would allow 'production and consumption of energy at sustainable levels', in the words of the authors. It is therefore very important to sort out from the abundant literature on the issue which are the facts and which are the biases and preferences.
DOI: 10.6084/m9.figshare.1011379.v1
title: Examples of sparql queries to browse the library of eligibility criteria

description: File contains example of sparql queries that can be used to browse the library of structured eligibility criteria available at [1]. The queries can be executed at this endpoint [2], for example using yasgui [3].
DOI: 10.6084/m9.figshare.1010377.v1
title: Biofuel production (2011)

description: <b>Table 1.</b> Biofuel production (2011). Source: [11]. <strong>Abstract</strong> The perspective by Haberl <em>et al</em> (2013 <em>Environ. Res. Lett.</em> <strong>8</strong> 031004) entitled 'Bioenergy: how much can we expect for 2050?' is timely and valuable. It deals with an important subject since contrasting views on the subject make it very difficult for policy makers to adopt policies that would allow 'production and consumption of energy at sustainable levels', in the words of the authors. It is therefore very important to sort out from the abundant literature on the issue which are the facts and which are the biases and preferences.
DOI: 10.6084/m9.figshare.1010196
title: Serology data

description: Two asexual malaria vaccine candidates (MSP3 and GLURP) were tested in this study on plasma samples obtained from blood collected on a monthly basis during the first six months of follow up and quaterly thereafter.
DOI: 10.6084/m9.figshare.1010195
title: Monthly follow up data

description: Children were visited at home 1) to collect blood samples for malaria serology and 2) to the detect the first malaria infection.
DOI: 10.6084/m9.figshare.1010195.v1
title: Monthly follow up data

description: Children were visited at home 1) to collect blood samples for malaria serology and 2) to the detect the first malaria infection.
DOI: 10.6084/m9.figshare.1010196.v1
title: Serology data

description: Two asexual malaria vaccine candidates (MSP3 and GLURP) were tested in this study on plasma samples obtained from blood collected on a monthly basis during the first six months of follow up and quaterly thereafter.
DOI: 10.6084/m9.figshare.1010194
title: Active case detection data

description: Children were visited at home weekly by fieldworkers to check their health status and collect blood smears for parasitology in case of fever or history of fever in the past 24 hours.
DOI: 10.6084/m9.figshare.1010192
title: Homesteads coordinates

description: Study participants homesteads coordinates were recorded using a GPS device (eTrex Summit® HC).
DOI: 10.6084/m9.figshare.1010193
title: Passive case detection data

description: The caregivers were encouraged to bring their children to the nearest healthcare facility should the child feel unwell. A blood smear was collected in case of fever or histrory of fever in the past 24 hours.
DOI: 10.6084/m9.figshare.1010194.v1
title: Active case detection data

description: Children were visited at home weekly by fieldworkers to check their health status and collect blood smears for parasitology in case of fever or history of fever in the past 24 hours.
DOI: 10.6084/m9.figshare.1010192.v1
title: Homesteads coordinates

description: Study participants homesteads coordinates were recorded using a GPS device (eTrex Summit® HC).
DOI: 10.6084/m9.figshare.1010193.v1
title: Passive case detection data

description: The caregivers were encouraged to bring their children to the nearest healthcare facility should the child feel unwell. A blood smear was collected in case of fever or histrory of fever in the past 24 hours.
DOI: 10.6084/m9.figshare.1010188
title: The Andean tarantulas <i>Euathlus</i> Ausserer, 1875, <i>Paraphysa</i> Simon, 1892 and <i>Phrixotrichus</i> Simon, 1889 (Araneae: Theraphosidae): phylogenetic analysis, genera redefinition and new species descriptions

description: Based on a phylogenetic analysis we revised the Chilean tarantula genera <i>Euathlus</i> and <i>Paraphysa</i>. As results of our analyses, within a wider context of South American lineages, <i>Paraphysa</i> is synonymous of <i>Euathlus</i>, and <i>Phrixotrichus</i> is resurrected. <i>Euathlus</i> and <i>Phrixotrichus</i> are sister genera, supported by their shared palpal organ morphology, especially at the ventral position of the distal prolateral inferior keel, also by spermathecal receptacles with a lateral chamber, and tarsal claws without teeth. Both genera are redefined based on cladistic results, and some of their constituent species are transferred. We describe four new species, and for the first time present the spermathecae of <i>Euathlus</i><i>parvulus</i> comb. nov. All species described for both genera are diagnosed and keyed. <i>Euathlus</i> now includes: <i>Euathlus</i><i>antai</i> Perafán and Pérez-Miles sp. nov., <i>Euathlus</i><i>atacama</i> Perafán and Pérez-Miles sp. nov., <i>Euathlus</i><i>condorito</i> Perafán and Pérez-Miles sp. nov., <i>Euathlus</i><i>manicata</i> (Simon 1892) comb. nov., <i>Euathlus</i><i>parvulus</i> (Pocock, 1903) comb. nov. and <i>Euathlus</i><i>truculentus</i> L. Koch, 1875. <i>Phrixotrichus</i> now comprises: <i>Phrixotrichus</i><i>jara</i> Perafán and Pérez-Miles sp. nov., <i>Phrixotrichus</i><i>scrofa</i> (Molina, 1788) comb. nov. and <i>Phrixotrichus</i><i>vulpinus</i> (Karsch, 1880) comb. nov. Furthermore, <i>Paraphysa riparia</i> Schmidt and Bolle, 2008 is synonymized with <i>Eupalaestrus weijenberghi</i> (Thorell, 1894), <i>Paraphysa pulcherrimaklaasi</i> Schmidt, 1991 is transferred to <i>Maraca</i> Pérez-Miles, 2006 and <i>Paraphysa peruviana</i> Schmidt, 2007 is considered a <i>nomen dubium.</i>http://zoobank.org/urn:lsid:zoobank.org:pub:62B49343-DCF0-4AFE-8154-19F9D50E9AA0
DOI: 10.6084/m9.figshare.1010191
title: Baseline visit data

description: Health, socio-demographic, parasitological and serologycal data were recorded for each participant at the baseline/screening visit.
DOI: 10.6084/m9.figshare.1010177
title: Cognitive reflection test. Dataset of 2019 responses with all the items.

description: This additional dataset contains all the items, not just the overall value on each test. This allows additional analyses not reported in the original article: Campitelli, G., & Gerrans, P. (2014). What does the cognitive reflection test measure? A mathematical modelling approach. Memory and Cognition, 42, 434-447.
DOI: 10.6084/m9.figshare.1010176
title: Cognitive reflection test. Dataset of 2019 participants.

description: This is the dataset used in the article: Campitelli, G., & Gerrans, P. (2014). What does the cognitive reflection test measure? A mathematical modelling approach. Memory and Cognition, 42, 434-447.
DOI: 10.6084/m9.figshare.1010191.v1
title: Baseline visit data

description: Health, socio-demographic, parasitological and serologycal data were recorded for each participant at the baseline/screening visit.
DOI: 10.6084/m9.figshare.1010188.v2
title: The Andean tarantulas <i>Euathlus</i> Ausserer, 1875, <i>Paraphysa</i> Simon, 1892 and <i>Phrixotrichus</i> Simon, 1889 (Araneae: Theraphosidae): phylogenetic analysis, genera redefinition and new species descriptions

description: Based on a phylogenetic analysis we revised the Chilean tarantula genera <i>Euathlus</i> and <i>Paraphysa</i>. As results of our analyses, within a wider context of South American lineages, <i>Paraphysa</i> is synonymous of <i>Euathlus</i>, and <i>Phrixotrichus</i> is resurrected. <i>Euathlus</i> and <i>Phrixotrichus</i> are sister genera, supported by their shared palpal organ morphology, especially at the ventral position of the distal prolateral inferior keel, also by spermathecal receptacles with a lateral chamber, and tarsal claws without teeth. Both genera are redefined based on cladistic results, and some of their constituent species are transferred. We describe four new species, and for the first time present the spermathecae of <i>Euathlus</i><i>parvulus</i> comb. nov. All species described for both genera are diagnosed and keyed. <i>Euathlus</i> now includes: <i>Euathlus</i><i>antai</i> Perafán and Pérez-Miles sp. nov., <i>Euathlus</i><i>atacama</i> Perafán and Pérez-Miles sp. nov., <i>Euathlus</i><i>condorito</i> Perafán and Pérez-Miles sp. nov., <i>Euathlus</i><i>manicata</i> (Simon 1892) comb. nov., <i>Euathlus</i><i>parvulus</i> (Pocock, 1903) comb. nov. and <i>Euathlus</i><i>truculentus</i> L. Koch, 1875. <i>Phrixotrichus</i> now comprises: <i>Phrixotrichus</i><i>jara</i> Perafán and Pérez-Miles sp. nov., <i>Phrixotrichus</i><i>scrofa</i> (Molina, 1788) comb. nov. and <i>Phrixotrichus</i><i>vulpinus</i> (Karsch, 1880) comb. nov. Furthermore, <i>Paraphysa riparia</i> Schmidt and Bolle, 2008 is synonymized with <i>Eupalaestrus weijenberghi</i> (Thorell, 1894), <i>Paraphysa pulcherrimaklaasi</i> Schmidt, 1991 is transferred to <i>Maraca</i> Pérez-Miles, 2006 and <i>Paraphysa peruviana</i> Schmidt, 2007 is considered a <i>nomen dubium.</i>http://zoobank.org/urn:lsid:zoobank.org:pub:62B49343-DCF0-4AFE-8154-19F9D50E9AA0