cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.28397201.v1
title: The Triassic tectonic transition of the Northwestern margin of Ordos Basin, North China Craton

description: The Northwestern margin of Ordos Basin (NWOB), which contains the Helanshan Tectonic Belt (HTB) and Northwestern margin of Ordos Basin Thrust Belt (NWOBTB), is situated in the northwest of the North China Craton (NCC). The Triassic sedimentary-tectonic transition of the NWOB provides crucial insights for revealing the tectonic evolution of the NCC. In this study, we have utilized a comprehensive dataset including the palaeocurrent orientations, sandstone modal composition, U-Pb age analysis of detrital zircons, and balanced cross-sections restorations, to clarify the Triassic sedimentary-tectonic evolution of NWOB. The southeast-directed palaeocurrent indicates the sediments were primarily derived from northwest. The composition of clastic material suggests diverse sources, including magmatic arc and continental blocks. Detrital zircons extracted from four sandstones yield five major LA-ICP-MS U-Pb age groups: 2600–2500 Ma, 2300–2200 Ma, 2000–1800 Ma, 500–400 Ma and 390–230 Ma. A comparison of these U-Pb age groups from the Triassic strata in the NWOBTB with the magmatic records in the Alxa Massif, the Qilian Orogenic Belt, and detrital zircons from pre-Triassic strata in the HTB reveals that the Triassic detritus in the NWOBTB was predominantly originated from the Alxa Massif. Furthermore, the absence of detrital zircons in NWOBTB that originated from the HTB suggests the HTB had not been uplifted until the Mid-Late Triassic and remained in a steady sedimentary environment with NWOBTB during this period. In addition, the E-W treading shortening structures, along with the angular unconformity between the Jurassic and the Upper Triassic in the HTB, indicate a phase of extensive N-S shortening occurred in the HTB in the end of the Triassic. Balanced cross-section restorations demonstrate the southern HTB experienced 27% shortening, while the middle HTB underwent 15% shortening. In contrast, the Jurassic strata are in parallel-unconformity with the Triassic strata in the NWOBTB. This suggests the NWOBTB was not significantly effected by the end Triassic N-S shortening deformation. These distinct deformations between the HTB and NWOBTB imply that there was a phase of dextral strike-slip displacement between the two regions in the end of the Triassic, which is related to the closure of Paleo Tethys Ocean.
DOI: 10.6084/m9.figshare.28416078
title: Precambrian history of the Altun microcontinent: review and synthesis

description: Microcontinents in orogenic belts possess valuable records of orogenic process and provide insights for the reconstruction of supercontinents. The Central Altun terrane is an ancient block preserved in the Altun Orogen, located on the northwestern margin of the Qinghai-Tibet Plateau and the southeastern margin of the Tarim Craton. In this contribution, relevant published data and unpublished geological mapping reports are compiled, reviewed and synthesized, and an overview of the Precambrian history of the Central Altun terrane and its periphery is presented, including their formation, evolution, and tectonic processes. These data suggest that the Central Altun terrane, sandwiched by two Paleozoic ophiolite mélange belts, was a microcontinent comprising of Neoproterozoic clastic rocks, carbonate rocks and granitoids before it collided with Tarim craton in early Paleozoic. The geochronological data show the possible existence of Paleoproterozoic and Mesoproterozoic crystalline basement beneath the surface of the Altun Microcontinent. The Neoproterozoic geological records in the Altun orogen indicate that the northern and southern margins of the Altun Microcontinent were broken up simultaneously and are consistent with the supercontinent cycle, possibly triggered by a mantle plume that resulted in the break-up of the Rodinia supercontinent. Collectively, the geochronological data on both sides of the Altun Microcontinent suggest that it was not evolved independently until the break-up of the Rodinia supercontinent and may belong to Laurentia before that.
DOI: 10.6084/m9.figshare.28416078.v1
title: Precambrian history of the Altun microcontinent: review and synthesis

description: Microcontinents in orogenic belts possess valuable records of orogenic process and provide insights for the reconstruction of supercontinents. The Central Altun terrane is an ancient block preserved in the Altun Orogen, located on the northwestern margin of the Qinghai-Tibet Plateau and the southeastern margin of the Tarim Craton. In this contribution, relevant published data and unpublished geological mapping reports are compiled, reviewed and synthesized, and an overview of the Precambrian history of the Central Altun terrane and its periphery is presented, including their formation, evolution, and tectonic processes. These data suggest that the Central Altun terrane, sandwiched by two Paleozoic ophiolite mélange belts, was a microcontinent comprising of Neoproterozoic clastic rocks, carbonate rocks and granitoids before it collided with Tarim craton in early Paleozoic. The geochronological data show the possible existence of Paleoproterozoic and Mesoproterozoic crystalline basement beneath the surface of the Altun Microcontinent. The Neoproterozoic geological records in the Altun orogen indicate that the northern and southern margins of the Altun Microcontinent were broken up simultaneously and are consistent with the supercontinent cycle, possibly triggered by a mantle plume that resulted in the break-up of the Rodinia supercontinent. Collectively, the geochronological data on both sides of the Altun Microcontinent suggest that it was not evolved independently until the break-up of the Rodinia supercontinent and may belong to Laurentia before that.
DOI: 10.6084/m9.figshare.28374745
title: Triassic contractional deformation and sedimentary response in the Helanshan fold–thrust belt, Northwest China: evidence from growth strata

description: The Helanshan fold – thrust belt is located between the Alxa and Ordos blocks and has been a deformation area of tectonic activity since the Mesozoic. During the Mesozoic tectonic deformation, the Jurassic WNW – ESE-trending contraction transformed the Triassic NNE – SSW shortening. Field mapping and structural analysis reveal that the Middle Triassic Zhifang Formation in the northern wing of the Rujigou overturned anticline is characteristic of a growth strata, which is in response to SSW-NNE contraction. Detrital zircon U – Pb age spectra of the Middle Triassic Zhifang Formation show that the Triassic sedimentary materials originated from the North China Craton to the north, the Alxa block to the north, the Qilian orogenic belt to the south, and the Qinling orogenic belt to the south. The youngest age at the bottom of the growth strata is 282 ± 11 Ma, and the youngest age at the top is 291 ± 12 Ma, indicating that the strata maximum depositional age was later than the Permian, revealing that the youngest detrital zircon of the Middle Triassic Zhifang Formation is derived from the Rujigou overturned anticline, reflecting the characteristics of the reverse sedimentary sequence of detrital zircon and suggesting an interaction between structure and deposition. We propose that with the closure of the Paleo-Tethys Ocean, under the far-field response to the collision between the North China Craton and South China Craton, the Helanshan fold – thrust belt expanded northward and formed a northward protruding tectonic node that controlled the sedimentary process of the Triassic foreland basin.
DOI: 10.6084/m9.figshare.28374745.v1
title: Triassic contractional deformation and sedimentary response in the Helanshan fold–thrust belt, Northwest China: evidence from growth strata

description: The Helanshan fold – thrust belt is located between the Alxa and Ordos blocks and has been a deformation area of tectonic activity since the Mesozoic. During the Mesozoic tectonic deformation, the Jurassic WNW – ESE-trending contraction transformed the Triassic NNE – SSW shortening. Field mapping and structural analysis reveal that the Middle Triassic Zhifang Formation in the northern wing of the Rujigou overturned anticline is characteristic of a growth strata, which is in response to SSW-NNE contraction. Detrital zircon U – Pb age spectra of the Middle Triassic Zhifang Formation show that the Triassic sedimentary materials originated from the North China Craton to the north, the Alxa block to the north, the Qilian orogenic belt to the south, and the Qinling orogenic belt to the south. The youngest age at the bottom of the growth strata is 282 ± 11 Ma, and the youngest age at the top is 291 ± 12 Ma, indicating that the strata maximum depositional age was later than the Permian, revealing that the youngest detrital zircon of the Middle Triassic Zhifang Formation is derived from the Rujigou overturned anticline, reflecting the characteristics of the reverse sedimentary sequence of detrital zircon and suggesting an interaction between structure and deposition. We propose that with the closure of the Paleo-Tethys Ocean, under the far-field response to the collision between the North China Craton and South China Craton, the Helanshan fold – thrust belt expanded northward and formed a northward protruding tectonic node that controlled the sedimentary process of the Triassic foreland basin.
DOI: 10.48420/29126585
title: Widening Participation from the Ground Up: Early Intervention in Primary Education to Improve Healthcare Opportunities

description: Access to medical careers has historically been limited for individuals from disadvantaged backgrounds. While widening participation (WP) efforts have primarily focused on secondary education, early career aspirations often develop between the ages of 9 and 11, making primary school interventions crucial. However, the impact of early healthcare exposure on children from WP backgrounds remains underexplored. To address this gap, we implemented a healthcare career intervention for Key Stage 2 (KS2) children from deprived communities, identified using the Index of Multiple Deprivation (IMD) and POLAR4. The intervention consisted of three interactive sessions covering heart anatomy and function, CPR training, and healthcare role-play scenarios. Pre- and post-intervention questionnaires were used to assess changes in knowledge, skills, and career aspirations. Ethnicity was classified using standardised demographic categories. Our findings demonstrated significant improvements in children's knowledge of heart function (p&lt;0.001), CPR (p&lt;0.001), and healthcare roles (p&lt;0.001), as assessed by Likert-scale questionnaires. Career aspirations also increased, with the percentage of children considering a healthcare career rising from 37% pre-intervention to 49% post-intervention (p&lt;0.05). Learning CPR and other healthcare skills at an early age is valuable for all children but may be particularly impactful for those in disadvantaged communities, who often face greater health inequalities. The workshops also provided medical students with practical experience in engaging with children, highlighting potential benefits for broader healthcare student involvement. Despite aligning with the curriculum, school engagement proved challenging, underscoring the need for government-backed initiatives to integrate healthcare workshops into primary education. Introducing structured healthcare education at an early stage may help address inequalities in career access while equipping children with essential life-saving skills.
DOI: 10.15468/dl.seuc9r
title: Occurrence Download

description: A dataset containing 3 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Aotus jorgehernandezi Defler & Bueno, 2007"
 ]
}

 The dataset includes 3 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015532-250515123054153/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.29136590
title: <b>Data for sulfur isotopes from the lunar farside reveal</b><b> a global evaporation signiture following the gaint impact</b>

description: Table S1. Mineral composition of clinopyroxene and plagioclase in CE-6 basalt and crustal clasts.Table 2. Mineral abundance of CE-6 basalt clasts, NWA 12008 and NWA 14526 analysed by TIMA.Table S3. Composition of sulfide in Chang'e-6 basalt clasts, highland clasts and breccias.Table S4. δ34SV-CDT value of troilites in CE-6 basalt clasts, breccias and highland clasts, and lunar meteorites NWA 14526 and NWA 12008.Table S5. 34SV-CDT value of reference materials.
DOI: 10.34740/kaggle/dsv/11922370
title: Bitcoin BTC, 7 Exchanges, 1m Full Historical Data
DOI: 10.5281/zenodo.14726443
title: Confocal fluorescence microscopy images of dentinal porosity at the dentin-enamel junction UM_0003_C2_DEJ

description: Confocal image stacks were acquired with a Leica TCS SP8 microscope, using a 40x/1.3NA oil immersion lens. A wavelength of 561 nm (LED laser DPSS 561) was used to excite Rhodamine B fluorescence which was collected in a range of 567-636 nm with a hybrid detector. The acquisitions were performed on the polished surface of crown dentin up to 900 µm from the DEJ in the direction of the pulp (cf Fig.1a-b). The scanning was performed using 26-52 µW laser power with a linear increase in depth to compensate for scattering and absorption with a pixel dwell time of 300 ns and a line average of 3 acquisitions. The scan consisted of a mosaic of 5 overlapping stacks of 205.5×205.5 µm2 images with a pixel size of 100 nm, collected over 20.65 µm in depth with 350 nm sampling, forming a 934.4×205.5×20.65 µm3 volume. The resulting experimental dataset was thus 2055×9344×59 voxels in shape with 100×100×350 nm3 voxel size.

ROI1 and ROI2 from the paper corresponds the rectangular regions defined by coordinates: [(X:500,Y:6000), (X:1500,Y:1500)] and [(X:500,Y:500), (X:1500,Y:1500)], i.e. 1000 x 1000 pixels,

Note that images in the paper are mirrored vertically, i.e. upside-down.
DOI: 10.5281/zenodo.14726444
title: Confocal fluorescence microscopy images of dentinal porosity at the dentin-enamel junction UM_0001_C1_2_DEJ

description: Confocal image stacks were acquired with a Leica TCS SP8 microscope, using a 40x/1.3NA oil immersion lens. A wavelength of 561 nm (LED laser DPSS 561) was used to excite Rhodamine B fluorescence which was collected in a range of 567-636 nm with a hybrid detector. The acquisitions were performed on the polished surface of crown dentin up to 900 µm from the DEJ in the direction of the pulp (cf Fig.1a-b). The scanning was performed using 26-52 µW laser power with a linear increase in depth to compensate for scattering and absorption with a pixel dwell time of 300 ns and a line average of 3 acquisitions. The scan consisted of a mosaic of 5 overlapping stacks of 205.5×205.5 µm2 images with a pixel size of 100 nm, collected over 20.65 µm in depth with 350 nm sampling, forming a 934.4×205.5×20.65 µm3 volume. The resulting experimental dataset was thus 2055×9344×59 voxels in shape with 100×100×350 nm3 voxel size.
DOI: 10.5281/zenodo.15496458
title: Confocal fluorescence microscopy images of dentinal porosity at the dentin-enamel junction UM_0003_C2_DEJ

description: Confocal image stacks were acquired with a Leica TCS SP8 microscope, using a 40x/1.3NA oil immersion lens. A wavelength of 561 nm (LED laser DPSS 561) was used to excite Rhodamine B fluorescence which was collected in a range of 567-636 nm with a hybrid detector. The acquisitions were performed on the polished surface of crown dentin up to 900 µm from the DEJ in the direction of the pulp (cf Fig.1a-b). The scanning was performed using 26-52 µW laser power with a linear increase in depth to compensate for scattering and absorption with a pixel dwell time of 300 ns and a line average of 3 acquisitions. The scan consisted of a mosaic of 5 overlapping stacks of 205.5×205.5 µm2 images with a pixel size of 100 nm, collected over 20.65 µm in depth with 350 nm sampling, forming a 934.4×205.5×20.65 µm3 volume. The resulting experimental dataset was thus 2055×9344×59 voxels in shape with 100×100×350 nm3 voxel size.

ROI1 and ROI2 from the paper corresponds the rectangular regions defined by coordinates: [(X:500,Y:6000), (X:1500,Y:1500)] and [(X:500,Y:500), (X:1500,Y:1500)], i.e. 1000 x 1000 pixels,

Note that images in the paper are mirrored vertically, i.e. upside-down.
DOI: 10.21227/cz94-2d92
title: "Calibration of the Detector for Registration  of High-Power Microwave Radiation"

description: "A method of measuring the effective surface area of antennas at short ranges using a reference antenna in the form of an open end of a waveguide with a flange is proposed and realized. For a reference antenna in the form of a pyramidal horn, a technique for measuring its effective area is proposed, taking into account the position of the antenna phase center in the frequency band. Receiving antennas in the form of the open end of the waveguide in the frequency range of 8\u201310 GHz with effective area from 3.5 to 0.3 cm2 are created. Detectors of powerful microwave pulses for generation frequencies of 8\u201312 GHz were created. The detectors are calibrated at the frequency of 9.4 GHz."
DOI: 10.5281/zenodo.15496549
title: Coyotes in Ohio - Limits on Hunting

description: The context, methods, and wider output of this project can be find in the published report here: http://dx.doi.org/10.13140/RG.2.2.28929.12643/1
DOI: 10.5281/zenodo.15490755
title: NOAA Ocean Exploration Gap Analysis Results

description: The NOAA Ocean Exploration Gap Analysis (EGA) is a tool to establish a spatial coverage baseline for ocean exploration data holdings, support the monitoring of exploration and characterization progress on previously unexplored ocean areas, and aid in the identification of priority areas for future expeditions and data collection efforts.

This data package consists of output files in several formats described in the DATA_README containing the H3 Geo (h3geo.org/) hexagon addresses/polygons/centroids and corresponding exploration scores for each grid cell and observation type, as well as a copy of the PostGIS database. Users can work off of the data package results directly or clone the repository, run the analysis, and create their own results.

For more details on the methodology, see the repository at github.com/NOAA-OceanExploration/ExplorationGapAnalysis/
DOI: 10.5281/zenodo.15490756
title: NOAA Ocean Exploration Gap Analysis Results

description: The NOAA Ocean Exploration Gap Analysis (EGA) is a tool to establish a spatial coverage baseline for ocean exploration data holdings, support the monitoring of exploration and characterization progress on previously unexplored ocean areas, and aid in the identification of priority areas for future expeditions and data collection efforts.

This data package consists of output files in several formats described in the DATA_README containing the H3 Geo (h3geo.org/) hexagon addresses/polygons/centroids and corresponding exploration scores for each grid cell and observation type, as well as a copy of the PostGIS database. Users can work off of the data package results directly or clone the repository, run the analysis, and create their own results.

For more details on the methodology, see the repository at github.com/NOAA-OceanExploration/ExplorationGapAnalysis/
DOI: 10.5281/zenodo.15497040
title: The mixed Candida albicans - Staphylococcus aureus biofilm is reduced by light-activated nanocomposite with phloxine B
DOI: 10.5281/zenodo.15497041
title: The mixed Candida albicans - Staphylococcus aureus biofilm is reduced by light-activated nanocomposite with phloxine B
DOI: 10.15468/dl.s8kjby
title: Occurrence Download

description: A dataset containing 140434 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Türkiye",
 {
 "or" : [
 "Geometry POLYGON((16.85277 31.74421,53.14723 31.74421,53.14723 46.25579,16.85277 46.25579,16.85277 31.74421))",
 "Geometry POLYGON((38.05693 39.33428,38.50379 39.33428,38.50379 39.61512,38.05693 39.61512,38.05693 39.33428))"
 ]
 },
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Plantae",
 "Year 1777-2025"
 ]
}

 The dataset includes 140434 records from 234 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015538-250515123054153/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.uk5swe
title: Occurrence Download

description: A dataset containing 25789 species occurrences available in GBIF matching the query:
{
 "DatasetKey" : [
 "is Explore Your Shore"
 ]
}

 The dataset includes 25789 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015541-250515123054153/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.77xxcr
title: Occurrence Download

description: A dataset containing 1398 species occurrences available in GBIF matching the query:
{
 "and" : [
 "DatasetKey is iNaturalist Research-grade Observations",
 "TaxonKey is Acropora palmata (Lamarck, 1816)"
 ]
}

 The dataset includes 1398 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015539-250515123054153/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.29135555
title: All data.xlsx

description: The data set was originated from a research project aiming at testing the applicability of the K-bicarbonate method for lime requirement of aquaculture ponds in the Mekong delta of Vietnam.
DOI: 10.15468/dl.v752z5
title: Occurrence Download

description: A dataset containing 115 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Aotus brumbacki Hershkovitz, 1983"
 ]
}

 The dataset includes 115 records from 18 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015542-250515123054153/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25824/redu/ykfgl0
title: Replication data for: Efeitos de íon-comum e múltiplos eletrólitos na solvatação de proteínas por líquidos iônicos

description: (i) a dataset containing input and output files for a molecular dynamics simulation of the ionic liquid BMIMCl at 1.0 mol/L in the presence of the protein Ubiquitin, illustrating one replica representative of the simulations performed in the thesis; (ii) input models used to run the molecular dynamics simulations with the OPLS-VSIL force field and the GROMACS software;
DOI: 10.15129/1f1c7b31-8be2-4434-b786-f21d9bf8f236
title: Data for: "Stability properties of the first-in-class anti-cancer IgE antibody drug, MOv18 IgE"

description: This dataset contains data in excel file format which was created for the purpose of plotting figures within the paper and supplementary of "Frit-Inlet Asymmetric Flow Field-Flow Fractionation for the Analysis of Lipid Nanoparticle-Protein Interactions".
DOI: 10.15468/dl.ysjhpd
title: Occurrence Download

description: A dataset containing 1571 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Stylosanthes scabra Vogel",
 "HasCoordinate is true",
 "BasisOfRecord is one of (Human Observation, Living Specimen, Occurrence evidence)"
 ]
}

 The dataset includes 1571 records from 12 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015507-250515123054153/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.