cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.10839098
title: Asaia spp. accelerate development of the yellow fever mosquito, Aedes aegypti, via interactions with the vertically transmitted larval microbiome

description: Background: Aedes aegypti mosquitoes are the primary vectors of yellow fever, dengue, chikungunya and Zika virus. Control programs primarily rely on insecticide application, which encounter challenges related to efficacy and resistance evolution. Alternative strategies, such as the sterile insect technique, highly depend on efficient mass-rearing of healthy insects prior to mass release. Based on effects seen in other mosquito species, we tested the hypothesis that acetic acid bacteria of the Asaia genus are mutualists for developing Ae. aegypti larvae. We tested for beneficial interactions across three Asaia species and whether Asaia inoculation benefited both axenic and conventionally reared larvae. To better understand the underlying mechanisms, we characterized the larval microbiome using culture-based methods and 16S rRNA gene amplicon sequencing.

Results: Even though Asaia bacteria were transient members of the gut community in conventionally reared insects, two Asaia species accelerated larval development relative to controls. Despite their transient nature, the two mutualist Asaia species had lasting impacts on the larval microbiome, mostly by altering the relative abundance of the most dominant bacteria genera Klebsiella and Pseudomonas and other minor components. Axenic larvae that were inoculated with Asaia were dominated by this group, but always exhibited slower development than conventionally reared insects.

Conclusions: These results reveal Asaia as a poor mutualist for Ae. aegypti, with its positive effect on the host mediated by interactions with other bacteria. A practical application of Asaia for improving mass-rearing efficiency results from the acceleration of development time to pupation by a day.
DOI: 10.14473/csda/w2xli6/8avttw
title: D_CSDA00150.pdf

description: Dotazník CSDA00150
DOI: 10.14473/csda/w2xli6/icieoi
title: Data_JM_volby 2012_1.tab

description: Data CSDA00150
DOI: 10.14473/csda/w2xli6/nvwvkl
title: TI_CSDA00150.pdf

description: Technická informace CSDA00151
DOI: 10.14473/csda/w2xli6/nhocee
title: OM_CSDA00150-162.pdf

description: Ostatní materiály CSDA00150-162
DOI: 10.17632/w4xxkf7brg.1
title: Psychometric Validation of the Chinese Versions of EQ-5D-Y-3L and EQ-TIPS In Children and Adolescents with COVID-19

description: The entire data for total sample
DOI: 10.17632/yf7s47rcth.1
title: Causes of conflicts in standardization alliances related to the Belt and Road Initiative

description: This dataset is associated with the article "Causes of conflicts in standardization alliances related to the Belt and Road Initiative".
DOI: 10.17632/k5r7ch8db7.1
title: Cell Cycle Arrest

description: Biological activity data
DOI: 10.17632/nbtsxftm77.1
title: Laying Performance and Egg Quality Traits of Vanaraja Birds as Influenced by Dietary Supplementation of Turmeric Powder

description: ABSTRACT: The present study was conducted to use turmeric powder as an alternative to antibiotics properties. The current study was designed to determine laying performance, albumin index, yolk index, haugh unit, and yolk cholesterol as influenced by different levels of turmeric powder dietary 
supplementation. The experimental birds were randomly divided into four treatment groups designated as T1, T2, T3 and T4 with thirty (30) chicks in each group having five replicates of six (6) birds each. They were 
subjected to four dietary levels of turmeric powder containing 0%, 0.5%, 0.75%, and 1.5%, respectively, for a period of 365 days. The overall level of statistical significance was defined as p&lt;0.05. The significance 
of the result was evaluated using an analysis of variance (ANOVA) in the computer software WASP. Dietary supplementation with turmeric powder improved laying performance and enhanced egg quality traits. Yolk index and albumen index increased (p&lt;0.05) while yolk cholesterol decreased with the increase in the level of turmeric powder. On the basis of the above findings, supplementation of turmeric powder at 0.75 per cent of feed can be recommended under Nagaland's agro-climatic conditions.
CONCLUSIONS
Turmeric powder supplementation at the rate of 0.75 resulted in better performance in egg production and egg quality traits of Vanaraja birds as compared to the control group. Therefore, on the basis of the above 
findings, the use of turmeric powder as a feed additive at the rate of 0.75 in poultry diets may be advocated for better production performance and for producing betterquality eggs.
DOI: 10.17632/973whj3m8d.1
title: Shelf life of shrimp coated with gelatin

description: This study aimed to assess the shelf life of Pacific white shrimp coated with gelatin extracted from Nile tilapia concerning microbial degradation, pH levels, total volatile bases nitrogen (TVB-N), trimethylamine nitrogen (TMA-N), and thiobarbituric acid-reactive substances (TBARS) assessed at intervals of 30 days (T0, T30, T60, T90, T120, T150 and T180 days).
DOI: 10.17632/9k4xmb46k6.1
title: High oxygen concentration in shallow seawater during a transient mid-Proterozoic oxygenation event revealed by iodine content in water-column precipitated calcite

description: Carbonate I/(Ca+Mg) ratio has been used as a proxy to track shallow-seawater oxygen levels through Earth’s history. However, due to potential loss of iodine during diagenetic transformation (e.g., dolomitization) and homogenization of iodine in carbonate minerals formed in the redox-stratified water column or porewater, bulk-rock carbonate I/(Ca+Mg) values―and thus the oxygen levels in Precambrian shallow seawater―could have been significantly underestimated. Here, we report a mineralogy-based sequential dissolution method to obtain I/(Ca+Mg) values from water-column precipitated calcites in mid-Proterozoic dolomitic limestones from North China. Petrographic observations indicate that these dolomitic limestones consist of both calcite precipitated from the water column and dolomite that formed in porewater. 
Using dilute acid (0.1% v/v and 0.03% v/v nitric acid) for stepwise carbonate dissolution showed progressive decrease in I/(Ca+Mg) values and increase in Mg/Ca molar ratios. Comparison of the data obtained from the dissolution steps, using 0.03% v/v nitric acid to dissolve 5% of dolomitic limestones most effectively captured the I/(Ca+Mg) values of the initial water-column precipitated calcites, which are significantly higher than those of the corresponding bulk-rock. Application of this method to the ~1.57 Ga oxygenation event suggests initial I/(Ca+Mg) ratios up to ~11 μmol/mol. These I/(Ca+Mg) values indicate that shallow seawater O2 levels, which may have exceeded 125 μM, could have been underestimated by previous bulk-rock analyses that indicated I/(Ca+Mg) up to 4.1 μmol/mol, corresponding to O2 levels > 20 μM. These results suggest that fluctuating O2 concentrations in mid-Proterozoic (1.8–0.8 Ga) shallow seawater were likely high enough to support the respiratory requirements of eukaryotes including animals, at least during transient oxygenation events.
This data set contains the duplicate tests of iodine in dolostone standard GSR-12, and major elements in JDo-1 (Table S1 and S2). The data set also shows the detailed dissolution data of a stepwise dissolution protocol (Table S3 and S4), and its application on the ~1.57-Ga Gaoyuzhuang Formation samples (Table S5). We use dilute nitric acid to partially dissolve the dolomitic limestone samples to acquire the I/(Ca+Mg) values from water-column precipitated carbonate mud. The results show significantly high I/(Ca+Mg) values than those acquired with bulk-rock dissolution methods.
DOI: 10.17632/9k4xmb46k6.2
title: High oxygen concentration in shallow seawater during a transient mid-Proterozoic oxygenation event revealed by iodine content in water-column precipitated calcite

description: Carbonate I/(Ca+Mg) ratio has been used as a proxy to track shallow-seawater oxygen levels through Earth’s history. However, due to potential loss of iodine during diagenetic transformation (e.g., dolomitization) and homogenization of iodine in carbonate minerals formed in the redox-stratified water column or porewater, bulk-rock carbonate I/(Ca+Mg) values―and thus the oxygen levels in Precambrian shallow seawater―could have been significantly underestimated. Here, we report a mineralogy-based sequential dissolution method to obtain I/(Ca+Mg) values from water-column precipitated calcites in mid-Proterozoic dolomitic limestones from North China. Petrographic observations indicate that these dolomitic limestones consist of both calcite precipitated from the water column and dolomite that formed in porewater. 
Using dilute acid (0.1% v/v and 0.03% v/v nitric acid) for stepwise carbonate dissolution showed progressive decrease in I/(Ca+Mg) values and increase in Mg/Ca molar ratios. Comparison of the data obtained from the dissolution steps, using 0.03% v/v nitric acid to dissolve 5% of dolomitic limestones most effectively captured the I/(Ca+Mg) values of the initial water-column precipitated calcites, which are significantly higher than those of the corresponding bulk-rock. Application of this method to the ~1.57 Ga oxygenation event suggests initial I/(Ca+Mg) ratios up to ~11 μmol/mol. These I/(Ca+Mg) values indicate that shallow seawater O2 levels, which may have exceeded 125 μM, could have been underestimated by previous bulk-rock analyses that indicated I/(Ca+Mg) up to 4.1 μmol/mol, corresponding to O2 levels > 20 μM. These results suggest that fluctuating O2 concentrations in mid-Proterozoic (1.8–0.8 Ga) shallow seawater were likely high enough to support the respiratory requirements of eukaryotes including animals, at least during transient oxygenation events.
This data set contains the duplicate tests of iodine in dolostone standard GSR-12, and major elements in JDo-1 (Table S1 and S2). The data set also shows the detailed dissolution data of a stepwise dissolution protocol (Table S3 and S4), and its application on the ~1.57-Ga Gaoyuzhuang Formation samples (Table S5). We use dilute nitric acid to partially dissolve the dolomitic limestone samples to acquire the I/(Ca+Mg) values from water-column precipitated carbonate mud. The results show significantly high I/(Ca+Mg) values than those acquired with bulk-rock dissolution methods.
DOI: 10.17632/9k4xmb46k6.3
title: High oxygen concentration in shallow seawater during a transient mid-Proterozoic oxygenation event revealed by iodine content in water-column precipitated calcite

description: Carbonate I/(Ca+Mg) ratio has been used as a proxy to track shallow-seawater oxygen levels through Earth’s history. However, due to potential loss of iodine during diagenetic transformation (e.g., dolomitization) and homogenization of iodine in carbonate minerals formed in the redox-stratified water column or porewater, bulk-rock carbonate I/(Ca+Mg) values―and thus the oxygen levels in Precambrian shallow seawater―could have been significantly underestimated. Here, we report a mineralogy-based sequential dissolution method to obtain I/(Ca+Mg) values from water-column precipitated calcites in mid-Proterozoic dolomitic limestones from North China. Petrographic observations indicate that these dolomitic limestones consist of both calcite precipitated from the water column and dolomite that formed in porewater. 
Using dilute acid (0.1% v/v and 0.03% v/v nitric acid) for stepwise carbonate dissolution showed progressive decrease in I/(Ca+Mg) values and increase in Mg/Ca molar ratios. Comparison of the data obtained from the dissolution steps, using 0.03% v/v nitric acid to dissolve 5% of dolomitic limestones most effectively captured the I/(Ca+Mg) values of the initial water-column precipitated calcites, which are significantly higher than those of the corresponding bulk-rock. Application of this method to the ~1.57 Ga oxygenation event suggests initial I/(Ca+Mg) ratios up to ~11 μmol/mol. These I/(Ca+Mg) values indicate that shallow seawater O2 levels, which may have exceeded 125 μM, could have been underestimated by previous bulk-rock analyses that indicated I/(Ca+Mg) up to 4.1 μmol/mol, corresponding to O2 levels > 20 μM. These results suggest that fluctuating O2 concentrations in mid-Proterozoic (1.8–0.8 Ga) shallow seawater were likely high enough to support the respiratory requirements of eukaryotes including animals, at least during transient oxygenation events.
This data set contains the duplicate tests of iodine in dolostone standard GSR-12, and major elements in JDo-1 (Table S1 and S2). The data set also shows the detailed dissolution data of a stepwise dissolution protocol (Table S3 and S4), and its application on the ~1.57-Ga Gaoyuzhuang Formation samples (Table S5). We use dilute nitric acid to partially dissolve the dolomitic limestone samples to acquire the I/(Ca+Mg) values from water-column precipitated carbonate mud. The results show significantly high I/(Ca+Mg) values than those acquired with bulk-rock dissolution methods.
DOI: 10.17632/9k4xmb46k6.4
title: Mineralogy-based stepwise dissolution of dolomitic limestone reveals high iodine content in water-column precipitated calcite and well-oxygenated shallow seawater during the ~1.57 Ga oxygenation event

description: Carbonate I/(Ca+Mg) has been used as a proxy to track shallow-seawater oxygen levels through Earth’s history. However, due to diagenetic alteration and homogenization of iodine in carbonates formed in a redox-stratified water column or in porewater, bulk-rock I/(Ca+Mg) values―and thus the oxygen levels in Precambrian shallow seawater―could have been significantly underestimated. Here, we report a mineralogy-based sequential dissolution method using dilute nitric acid (0.03% v/v) to obtain I/(Ca+Mg) values of water-column precipitated calcite during the ~1.57 Ga oxygenation event in North China. The results show that at the peak of the oxygenation event, the I/(Ca+Mg) ratios of primary calcites are up to ~11 μmol/mol, which are significantly higher than the bulk-rock I/(Ca+Mg) values (up to ~4 μmol/mol). The new data imply that local shallow seawater O2 concentrations at ~1.57 Ga were higher than previously estimated and sufficient to support the respiratory needs of eukaryotes including animals. The delay of complex eukaryote and ecosystem evolution during the mid-Proterozoic (1.8–0.8 Ga) was not due to the lack of local oxic niches for eukaryotes but a consequence of temporal and spatial redox instability in shallow-marine environments.
This data set contains the duplicate tests of iodine in dolostone standard GSR-12, and major elements in JDo-1 (Table S1 and S2). The data set also shows the detailed dissolution data of a stepwise dissolution protocol (Table S3 and S4), and its application on the ~1.57-Ga Gaoyuzhuang Formation samples (Table S5). We use dilute nitric acid to partially dissolve the dolomitic limestone samples to acquire the I/(Ca+Mg) values from water-column precipitated carbonate mud. The results show significantly high I/(Ca+Mg) values than those acquired with bulk-rock dissolution methods.
DOI: 10.17632/vd5jy5w52m.1
title: Electrical muscular stimulation on shoulder instability: is it beneficial?

description: Objective: 
The aim of the study to collect relevant studies that examined the effects of Electrical Muscular Stimulation (EMS) on Shoulder Instability.
Background: 
The Shoulder instability is described as emerging when there are indications of shoulder laxity. The most common cause of primary shoulder dislocation in athletes is glenohumeral subluxation and dislocation. Roughly ninety-five percent of the first cases of shoulder dislocation result from an abrupt twisting motion, a forceful blow, or landing on an outstretched arm.
Methods: 
The review was carried out by searching scientifically recognized medical databases, including PubMed, Scopus, Pedro Database, ICTRP Database and WILEY Online Library. Date restrictions were not applied.
Results:
The studies that were included demonstrated that patients with Functional Posterior Shoulder Instability who received NMES-enhanced physical therapy had a significantly better main outcome. At the 3-month follow-up, the frequency of instability episodes improved significantly in the NMES-enhanced physical therapy group, and shoulder subluxation was significantly lower in position-triggered ES than in passive ES.
Conclusion:
The posterior shoulder instability was significantly and clinically alleviated by electrical muscle stimulation. On the other hand, position-triggered electrical stimulation (ES) might be more effective than passive ES for treating poststroke shoulder subluxation.
DOI: 10.17632/hmn3b4c6c4.1
title: Dataset of student internship experience, competence, psychological capital and employability’s vocational student (Original data)

description: This data is the original data collected through a survey conducted on student internship experience, competence, psychological capital, and employability of vocational students in Aceh Province. Data were collected by simple random sampling through surveys and questionnaires from August to December 2022. The data collected included 266 vocational students who had participated in internship programmes in industries and businesses. The goal of the survey was to collect information on the internship experiences of vocational students and schools in Aceh Province as it relates to employability through psychological capital and competencies. This dataset can be useful for policymakers and practitioners of vocational education institutions as well as a broad reference for improving learning both in schools and in industry. In addition, this dataset can also be a broad reference for other researchers who are interested in understanding students' experiences of internships and employability from different perspectives. Thus, this dataset has great potential to be used in various analyses and research related to vocational education and improving students' employability in Aceh.
DOI: 10.17632/bsf2ykpkzz.1
title: Organizational Change Capacity

description: The International Journal of Human Resource Management
Research Data Organizational Change Capacity on Organizational Alignment and Performance: Moderator Effects of Organizational Inertia.
DOI: 10.5281/zenodo.8262688
title: Global Cenozoic paleogeography and paleo-dynamic topography

description: This repository contains the data and files supporting the research paper titled: "Impact of mantle convection and dynamic topography on the Cenozoic paleogeography of Central Eurasia and the West Siberian Seaway", EPSL 2024. It contains global paleogeography for every millionth year of the Cenozoic and paleo-Dynamic topography from 100 - 0 Ma. 

### Contents ###

- Paleogeography:

  - This folder contains NetCDF files representing global paleogeographic reconstruction for each millionth year of the Cenozoic era. There is also a folder with global plots for each time step.

 

- Paleo-Dynamic_Topography:

- This folder contains NetCDF files from the paleo-dynamic topography models in 1 Myr time interval for the last 100 million years distributed in subfolders containing data computed in different reference frames i.e. paleomagnetic/pmag , mantle and dynamic topography in the reference frame of simplified individual plates where plate motions are from Torsvik et al. 2019 (as for both pmag and mantle), and we distinguish the plates using  present-day plate boundaries. Within these subfolders you find the dynamic topography based on various tomography models:

        - SMEAN2: Dynamic topography results based on the SMEAN2 tomography model (preferred).

        - Tx2019Slab: Dynamic topography results based on the Tx2019Slab tomography model (preferred).

        - S40RTS: Dynamic topography results based on the S40RTS tomography model.

        - SEMUCB-WM1: Dynamic topography results based on the SEMUCB-WM1 tomography model.
DOI: 10.5281/zenodo.8262689
title: Global Cenozoic paleogeography and paleo-dynamic topography

description: This repository contains the data and files supporting the research paper titled: "Impact of mantle convection and dynamic topography on the Cenozoic paleogeography of Central Eurasia and the West Siberian Seaway", EPSL 2024. It contains global paleogeography for every millionth year of the Cenozoic and paleo-Dynamic topography from 100 - 0 Ma. 

### Contents ###

- Paleogeography:

  - This folder contains NetCDF files representing global paleogeographic reconstruction for each millionth year of the Cenozoic era. There is also a folder with global plots for each time step.

 

- Paleo-Dynamic_Topography:

- This folder contains NetCDF files from the paleo-dynamic topography models in 1 Myr time interval for the last 100 million years distributed in subfolders containing data computed in different reference frames i.e. paleomagnetic/pmag , mantle and dynamic topography in the reference frame of simplified individual plates where plate motions are from Torsvik et al. 2019 (as for both pmag and mantle), and we distinguish the plates using  present-day plate boundaries. Within these subfolders you find the dynamic topography based on various tomography models:

        - SMEAN2: Dynamic topography results based on the SMEAN2 tomography model (preferred).

        - Tx2019Slab: Dynamic topography results based on the Tx2019Slab tomography model (preferred).

        - S40RTS: Dynamic topography results based on the S40RTS tomography model.

        - SEMUCB-WM1: Dynamic topography results based on the SEMUCB-WM1 tomography model.
DOI: 10.60580/novasbe.25416628
title: Replication package for: Spending a Windfall

description: We study the effect of the discovery of precious metals in America from 1500 to 1810 on international trade. Around 1500, there was a simultaneous discovery of precious metals and new trading routes. We construct a counterfactual of new routes but no precious metals. The discovery of precious metals increased the stock of precious metals more than tenfold. We show that Euro-Asian trade at its peak increased up to 20 times compared with the counterfactual. Our simulations match the observed price dynamics. We find that precious metals were at least as important as the new routes.
DOI: 10.60580/novasbe.25416628.v1
title: Replication package for: Spending a Windfall

description: We study the effect of the discovery of precious metals in America from 1500 to 1810 on international trade. Around 1500, there was a simultaneous discovery of precious metals and new trading routes. We construct a counterfactual of new routes but no precious metals. The discovery of precious metals increased the stock of precious metals more than tenfold. We show that Euro-Asian trade at its peak increased up to 20 times compared with the counterfactual. Our simulations match the observed price dynamics. We find that precious metals were at least as important as the new routes.
DOI: 10.17632/2cfsg7mb6p.1
title: Sm-PMN-PT Piezoelectric Ceramics Performance Database

description: This database stores research data from related papers
DOI: 10.17632/rdmpmhdzvs.1
title: Advancing Environmental Impact Assessments

description: This data delves into the application of machine learning (ML) to revolutionize Environmental Impact Assessments (EIA) within China
DOI: 10.18112/openneuro.ds003846.v2.0.2
title: Prediction Error
DOI: 10.17632/42vgccdwx9.1
title: Inter- and intra-mineral Li isotope fractionation during granitic magma differentiation

description: Li isotopic compositions (‰) of whole rocks (WR), plagioclase (Pl), K-feldspar (Kfs), quartz (Qtz), amphibole (Amp), clinopyroxene (Cpx), and biotite (Bt) from the Tagong pluton and geostandards during analysis. Li contents (ppm) of whole rocks (WR), plagioclase (Pl), K-feldspar (Kfs), quartz (Qtz), amphibole (Amp), clinopyroxene (Cpx), and biotite (Bt) from the Tagong pluton. Major element compositions (wt.%) of biotite, K-feldspar, plagioclase, clinopyroxene, and amphibole from the Tagong pluton. Trace element compositions (ppm) of biotite, plagioclase, amphibole and clinopyroxene from the Tagong pluton.