cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.17098878
title: New insights on the age and stratigraphy of the Cisuralian succession in the Cooper Basin, Australia, based on U–Pb CA-TIMS dating of volcanic air-fall tuffs

description: Absolute age constraints for Cisuralian units in the Cooper Basin have been hampered by poorly calibrated palynostratigraphic schemes, with implications for pan-Australian and global correlations. New U–Pb CA-TIMS (uranium–lead chemical abrasion-thermal ionisation mass spectrometry) dates acquired from volcanic air-fall tuff beds from the Patchawarra Formation combined with legacy palynological data offer new insights on the age, stratigraphy and tectonic history of the basin. Six tuffs from different regions of the Cooper Basin give dates from 284.87 to 277.36 Ma, which suggest that the Patchawarra Formation was deposited between the Artinskian and Kungurian rather than from the Sakmarian to Kungurian, as previously thought. The new dates indicate a possible unconformity at the base of the Patchawarra Formation and the underlying Tirrawarra Sandstone. They also suggest that the overlying REM succession (Roseneath Shale, Epsilon Formation and Murteree Shale) is entirely Guadalupian age rather than ranging from the Cisuralian to the Guadalupian. Consequently, existing Cisuralian and Guadalupian high-resolution spore-pollen zonations should be used with care when applied in conjunction with U–Pb CA-TIMS dates. The tuff dates in the thin Patchawarra Formation over the prominent Gidgealpa–Merrimelia–Innamincka Ridge within the Cooper Basin support the interpretation that the ridge was an area of relatively slow subsidence rather than being a positive feature during deposition. Compacted sediment accumulation rates of between 25 and ∼40 m/My for this unit are faster than for most cratonic basins, which raise questions on the tectonic setting of the Cooper Basin. The use and further acquisition of tuff dates will enhance correlations and facilitate improved paleogeographic reconstructions and our understanding of the late Paleozoic ice age.KEY POINTSSix volcanic air-fall tuff beds dated from the Cisuralian Patchawarra Formation, Cooper Basin.U–Pb CA-TIMS dates range from 284.87 to 277.36 Ma.Dates suggest deposition occurred between the Artinskian and Kungurian.New insights on basin tectonics, sedimentation rates and basin stratigraphy. Six volcanic air-fall tuff beds dated from the Cisuralian Patchawarra Formation, Cooper Basin. U–Pb CA-TIMS dates range from 284.87 to 277.36 Ma. Dates suggest deposition occurred between the Artinskian and Kungurian. New insights on basin tectonics, sedimentation rates and basin stratigraphy.
DOI: 10.6084/m9.figshare.17098878.v1
title: New insights on the age and stratigraphy of the Cisuralian succession in the Cooper Basin, Australia, based on U–Pb CA-TIMS dating of volcanic air-fall tuffs

description: Absolute age constraints for Cisuralian units in the Cooper Basin have been hampered by poorly calibrated palynostratigraphic schemes, with implications for pan-Australian and global correlations. New U–Pb CA-TIMS (uranium–lead chemical abrasion-thermal ionisation mass spectrometry) dates acquired from volcanic air-fall tuff beds from the Patchawarra Formation combined with legacy palynological data offer new insights on the age, stratigraphy and tectonic history of the basin. Six tuffs from different regions of the Cooper Basin give dates from 284.87 to 277.36 Ma, which suggest that the Patchawarra Formation was deposited between the Artinskian and Kungurian rather than from the Sakmarian to Kungurian, as previously thought. The new dates indicate a possible unconformity at the base of the Patchawarra Formation and the underlying Tirrawarra Sandstone. They also suggest that the overlying REM succession (Roseneath Shale, Epsilon Formation and Murteree Shale) is entirely Guadalupian age rather than ranging from the Cisuralian to the Guadalupian. Consequently, existing Cisuralian and Guadalupian high-resolution spore-pollen zonations should be used with care when applied in conjunction with U–Pb CA-TIMS dates. The tuff dates in the thin Patchawarra Formation over the prominent Gidgealpa–Merrimelia–Innamincka Ridge within the Cooper Basin support the interpretation that the ridge was an area of relatively slow subsidence rather than being a positive feature during deposition. Compacted sediment accumulation rates of between 25 and ∼40 m/My for this unit are faster than for most cratonic basins, which raise questions on the tectonic setting of the Cooper Basin. The use and further acquisition of tuff dates will enhance correlations and facilitate improved paleogeographic reconstructions and our understanding of the late Paleozoic ice age.KEY POINTSSix volcanic air-fall tuff beds dated from the Cisuralian Patchawarra Formation, Cooper Basin.U–Pb CA-TIMS dates range from 284.87 to 277.36 Ma.Dates suggest deposition occurred between the Artinskian and Kungurian.New insights on basin tectonics, sedimentation rates and basin stratigraphy. Six volcanic air-fall tuff beds dated from the Cisuralian Patchawarra Formation, Cooper Basin. U–Pb CA-TIMS dates range from 284.87 to 277.36 Ma. Dates suggest deposition occurred between the Artinskian and Kungurian. New insights on basin tectonics, sedimentation rates and basin stratigraphy.
DOI: 10.6084/m9.figshare.17078399
title: Mid-Phanerozoic microbialite forms and associated facies in the northern Perth Basin, Western Australia, and their relationship to the end-Permian mass extinction

description: Throughout geological history, biodiversity trends have been punctuated by sharp declines coinciding with mass extinction events. Certain organisms—known as disaster forms—flourish during the extinction aftermath from a lack of ecological competition and predation. Microbialites (in particular, stromatolites) are known to increase in environmental diversity following these biotic crises. However, it remains important to identify whether individual microbialite occurrences are a result of globally driven competition reduction or favourable local conditions. Here, we reconsider stromatolites from the northern Perth Basin of Western Australia, previously reported as Smithian (late Olenekian) in age and part of a biotic rebound following the end-Permian mass extinction and re-evaluate their paleodepositional setting and age. Detailed mapping, macro-analysis and meso-analysis of the Perth Basin locality have identified a well-preserved and diverse morphological assemblage of stromatolites that are intimately associated with a coarse siliciclastic facies. The characteristics of, and relationships between the stromatolitic and coarse siliciclastic facies support a restricted aquatic paleodepositional environment with fluvial/alluvial influences. In the Perth Basin, such depositional environments occurred most commonly during the Permian (Guadalupian to Lopingian). The robustness of previous age constraints interpreted from overlying strata (Kockatea Shale) are questioned by the identification of a depositional hiatus and onlapping relationship of the Kockatea Shale on the stromatolitic sequence. Therefore, we suggest that the mid-Phanerozoic northern Perth Basin Stromatolitic Sequence cannot be unequivocally associated with the end-Permian mass extinction and may have instead thrived owing to a favourable paleodepositional setting. The mid-Phanerozoic northern Perth Basin stromatolites are not a unique case. A compilation of reported Permian and Triassic microbialite occurrences shows that stromatolites, although most common following the end-Permian mass extinction, also occur before and after the extinction event in a range of environmental settings.KEY POINTSTen microbialite forms were described and mapped out over 30 km in the northern Perth Basin.Perth Basin Stromatolitic Sequence formed in a restricted aquatic depositional setting with fluvial and/or alluvial influences.Stromatolites from the northern Perth Basin are unlikely to be associated with the end-Permian mass. Ten microbialite forms were described and mapped out over 30 km in the northern Perth Basin. Perth Basin Stromatolitic Sequence formed in a restricted aquatic depositional setting with fluvial and/or alluvial influences. Stromatolites from the northern Perth Basin are unlikely to be associated with the end-Permian mass.
DOI: 10.6084/m9.figshare.17078399.v1
title: Mid-Phanerozoic microbialite forms and associated facies in the northern Perth Basin, Western Australia, and their relationship to the end-Permian mass extinction

description: Throughout geological history, biodiversity trends have been punctuated by sharp declines coinciding with mass extinction events. Certain organisms—known as disaster forms—flourish during the extinction aftermath from a lack of ecological competition and predation. Microbialites (in particular, stromatolites) are known to increase in environmental diversity following these biotic crises. However, it remains important to identify whether individual microbialite occurrences are a result of globally driven competition reduction or favourable local conditions. Here, we reconsider stromatolites from the northern Perth Basin of Western Australia, previously reported as Smithian (late Olenekian) in age and part of a biotic rebound following the end-Permian mass extinction and re-evaluate their paleodepositional setting and age. Detailed mapping, macro-analysis and meso-analysis of the Perth Basin locality have identified a well-preserved and diverse morphological assemblage of stromatolites that are intimately associated with a coarse siliciclastic facies. The characteristics of, and relationships between the stromatolitic and coarse siliciclastic facies support a restricted aquatic paleodepositional environment with fluvial/alluvial influences. In the Perth Basin, such depositional environments occurred most commonly during the Permian (Guadalupian to Lopingian). The robustness of previous age constraints interpreted from overlying strata (Kockatea Shale) are questioned by the identification of a depositional hiatus and onlapping relationship of the Kockatea Shale on the stromatolitic sequence. Therefore, we suggest that the mid-Phanerozoic northern Perth Basin Stromatolitic Sequence cannot be unequivocally associated with the end-Permian mass extinction and may have instead thrived owing to a favourable paleodepositional setting. The mid-Phanerozoic northern Perth Basin stromatolites are not a unique case. A compilation of reported Permian and Triassic microbialite occurrences shows that stromatolites, although most common following the end-Permian mass extinction, also occur before and after the extinction event in a range of environmental settings.KEY POINTSTen microbialite forms were described and mapped out over 30 km in the northern Perth Basin.Perth Basin Stromatolitic Sequence formed in a restricted aquatic depositional setting with fluvial and/or alluvial influences.Stromatolites from the northern Perth Basin are unlikely to be associated with the end-Permian mass. Ten microbialite forms were described and mapped out over 30 km in the northern Perth Basin. Perth Basin Stromatolitic Sequence formed in a restricted aquatic depositional setting with fluvial and/or alluvial influences. Stromatolites from the northern Perth Basin are unlikely to be associated with the end-Permian mass.
DOI: 10.6084/m9.figshare.19593835
title: Data of Handwriting Chinese Character Recognition Based on Deep Learning

description: Data of Handwriting Chinese Character Recognition Based on Deep Learning
DOI: 10.25442/hku.19446806
title: Supporting data for "Chinese language teachers' perceptions and pedagogies of intertextuality in Chinese language composition in preparing for College Entrance Exam (Gaokao) 2021"

description: The data was used to support the project entitled "Chinese language teachers' responses to intertextual practices in Chinese language composition in preparing for College Entrance Exam (<i>Gaokao</i>) 2021". There are 35 transcripts of interview data and class observations. The audio recordings of the interviews and class observations were transcribed verbatim. Each file was named by the date of conducting the interview or class observation and the identifier of the anonymous participant or the topic of the lesson.
DOI: 10.25442/hku.19446806.v1
title: Supporting data for "Chinese language teachers' perceptions and pedagogies of intertextuality in Chinese language composition in preparing for College Entrance Exam (Gaokao) 2021"

description: The data was used to support the project entitled "Chinese language teachers' responses to intertextual practices in Chinese language composition in preparing for College Entrance Exam (<i>Gaokao</i>) 2021". There are 35 transcripts of interview data and class observations. The audio recordings of the interviews and class observations were transcribed verbatim. Each file was named by the date of conducting the interview or class observation and the identifier of the anonymous participant or the topic of the lesson.
DOI: 10.25442/hku.19481603
title: Supporting data for "Designing a 5E flipped teaching approach to enhance elementary schoolers' computational thinking concepts, problem-solving and debugging skills"

description: Study One used a mixed-methods research approach to investigate student performance under different teaching approaches and their perceptions of the 5E-supported flipped classroom approach. Both quantitative and qualitative data were collected and analyzed. The quantitative data (e.g., test scores, project evaluation) can be used to indicate the student differences in learning outcomes between two instructional approaches. The qualitative data (e.g., student interviews, the instructor interview) can be used to explain the results obtained based on the quantitative data by identifying cases that describe the experiences of participants. Similar to the approach adopted in Study One, a mixed-methods research approach was also used in Study Two to examine student performance in program debugging under two different types of instructional approaches and students’ perceptions of the program debugging and the scaffolding tool that shows the systematic debugging process. This means that both quantitative and qualitative data needed to be collected and analyzed. The student performance differences in program debugging and cognitive load between the two flipped debugging training groups (i.e., the flipped debugging training approach combined with the systematic debugging process and the modeling method vs. the unassisted flipped debugging training approach) can be indicated through quantitative data (i.e., test scores in program debugging tasks and rating scores in the cognitive load questionnaire). The cases that described students’ experiences can be obtained through qualitative data (e.g., student interviews).
DOI: 10.25442/hku.19481603.v1
title: Supporting data for "Designing a 5E flipped teaching approach to enhance elementary schoolers' computational thinking concepts, problem-solving and debugging skills"

description: Study One used a mixed-methods research approach to investigate student performance under different teaching approaches and their perceptions of the 5E-supported flipped classroom approach. Both quantitative and qualitative data were collected and analyzed. The quantitative data (e.g., test scores, project evaluation) can be used to indicate the student differences in learning outcomes between two instructional approaches. The qualitative data (e.g., student interviews, the instructor interview) can be used to explain the results obtained based on the quantitative data by identifying cases that describe the experiences of participants. Similar to the approach adopted in Study One, a mixed-methods research approach was also used in Study Two to examine student performance in program debugging under two different types of instructional approaches and students’ perceptions of the program debugging and the scaffolding tool that shows the systematic debugging process. This means that both quantitative and qualitative data needed to be collected and analyzed. The student performance differences in program debugging and cognitive load between the two flipped debugging training groups (i.e., the flipped debugging training approach combined with the systematic debugging process and the modeling method vs. the unassisted flipped debugging training approach) can be indicated through quantitative data (i.e., test scores in program debugging tasks and rating scores in the cognitive load questionnaire). The cases that described students’ experiences can be obtained through qualitative data (e.g., student interviews).
DOI: 10.25442/hku.19498808
title: Supporting data for "Impact and mechanisms of ferroptosis in ovarian carcinoma"

description: This dataset is an supporting data for the PhD project "Impact and mechanisms of ferroptosis in ovarian carcinoma". This project focuses on exploration of the susceptibility of ovarian cancer cells to ferroptosis, and the synergistic anti-tumour effect of Cisplatin and ferroptosis inducers combination, as well as the molecular mechanisms of EPT1 in regulation of ferroptosis sensitivity in ovarian cancer. This dataset includes the raw and processed data of immunofluorescence, Sanger sequencing, RNA-sequencing, functional assay, quantitative-PCR and Western blotting included in the PhD thesis.<br>
DOI: 10.25442/hku.19498808.v1
title: Supporting data for "Impact and mechanisms of ferroptosis in ovarian carcinoma"

description: This dataset is an supporting data for the PhD project "Impact and mechanisms of ferroptosis in ovarian carcinoma". This project focuses on exploration of the susceptibility of ovarian cancer cells to ferroptosis, and the synergistic anti-tumour effect of Cisplatin and ferroptosis inducers combination, as well as the molecular mechanisms of EPT1 in regulation of ferroptosis sensitivity in ovarian cancer. This dataset includes the raw and processed data of immunofluorescence, Sanger sequencing, RNA-sequencing, functional assay, quantitative-PCR and Western blotting included in the PhD thesis.<br>
DOI: 10.5281/zenodo.6459080
title: 220414 NCfracset4

description: 220414 NCfracset4 TBD220310_14748_20220412
DOI: 10.5281/zenodo.6459079
title: 220414 NCfracset4

description: 220414 NCfracset4 TBD220310_14748_20220412
DOI: 10.6084/m9.figshare.19593869.v1
title: Additional file 1 of A serological biomarker of type I collagen degradation is related to a more severe, high neutrophilic, obese asthma subtype

description: Additional file 1: Table e1. Basic demographics of the PERF cohort. E-Figure1. A) Correlation betweenserum C1M level and blood neutrophils. Data were analysed using spearman’scorrelation (r = 0.214). B) Patients were stratified into highversus low percentage blood neutrophils levels based on the median. C1M wassignificantly increased in patients with high neutrophil levels (n = 122) compared to low (n = 128) (p = 0.0130). C) C1Mwas significantly increased in obese (BMI&gt;30) patients (n = 60) compared to normal-weight (BMI&lt;25) patients (n = 85) (p &lt; 0.0001). D) Obeseasthmatics with high blood neutrophils (n= 29) had a significant increase in C1M compared to normal-weight asthmaticswith low blood neutrophils (n = 39) (p &lt; 0.0001). Data arepresented as a Tukey box plot and analyzed using the Mann-Whitney test.Asterisks indicate statistically significance: *p &lt; 0.05, ****p &lt; 0.0001.
DOI: 10.6084/m9.figshare.19593869
title: Additional file 1 of A serological biomarker of type I collagen degradation is related to a more severe, high neutrophilic, obese asthma subtype

description: Additional file 1: Table e1. Basic demographics of the PERF cohort. E-Figure1. A) Correlation betweenserum C1M level and blood neutrophils. Data were analysed using spearman’scorrelation (r = 0.214). B) Patients were stratified into highversus low percentage blood neutrophils levels based on the median. C1M wassignificantly increased in patients with high neutrophil levels (n = 122) compared to low (n = 128) (p = 0.0130). C) C1Mwas significantly increased in obese (BMI&gt;30) patients (n = 60) compared to normal-weight (BMI&lt;25) patients (n = 85) (p &lt; 0.0001). D) Obeseasthmatics with high blood neutrophils (n= 29) had a significant increase in C1M compared to normal-weight asthmaticswith low blood neutrophils (n = 39) (p &lt; 0.0001). Data arepresented as a Tukey box plot and analyzed using the Mann-Whitney test.Asterisks indicate statistically significance: *p &lt; 0.05, ****p &lt; 0.0001.
DOI: 10.6084/m9.figshare.19593876.v1
title: Additional file 1 of Clinical impact of a metagenomic microbial plasma cell-free DNA next-generation sequencing assay on treatment decisions: a single-center retrospective study

description: Additional file 1. Supplementary Table 1. Raw daw compiled from retrospective record review. Records were reviewed for 80 patients who had a Karius test sent during the study period. Patient comorbidities, antibiotics courses, conventional microbiological records and clinical notes were reviewed. Clinical utility was determined via arbitration by the study authors.
DOI: 10.6084/m9.figshare.19593876
title: Additional file 1 of Clinical impact of a metagenomic microbial plasma cell-free DNA next-generation sequencing assay on treatment decisions: a single-center retrospective study

description: Additional file 1. Supplementary Table 1. Raw daw compiled from retrospective record review. Records were reviewed for 80 patients who had a Karius test sent during the study period. Patient comorbidities, antibiotics courses, conventional microbiological records and clinical notes were reviewed. Clinical utility was determined via arbitration by the study authors.
DOI: 10.6084/m9.figshare.19593885
title: Additional file 1 of The amyloid plaque proteome in early onset Alzheimer’s disease and Down syndrome

description: Additional file 1: Table S1. Total imputed dataset. Table S2. Unimputed data. Table S3. Proteins enriched in plaques in both EOAD and DS (used to generate Figs. 2 and 4). Table S4. Proteins uniquely enriched in plaques in EOAD. Table S5. Proteins uniquely enriched in DS plaques. Table S6. Chromosome 21 proteins identified in our proteomic analysis. Table S7. DS vs EOAD plaque protein differences.
DOI: 10.6084/m9.figshare.19593885.v1
title: Additional file 1 of The amyloid plaque proteome in early onset Alzheimer’s disease and Down syndrome

description: Additional file 1: Table S1. Total imputed dataset. Table S2. Unimputed data. Table S3. Proteins enriched in plaques in both EOAD and DS (used to generate Figs. 2 and 4). Table S4. Proteins uniquely enriched in plaques in EOAD. Table S5. Proteins uniquely enriched in DS plaques. Table S6. Chromosome 21 proteins identified in our proteomic analysis. Table S7. DS vs EOAD plaque protein differences.
DOI: 10.6084/m9.figshare.19593900
title: Additional file 1 of Efficiency of a novel vertebral body augmentation system (Tektona™) in non-osteoporotic spinal fractures

description: Additional file 1.
DOI: 10.6084/m9.figshare.19593900.v1
title: Additional file 1 of Efficiency of a novel vertebral body augmentation system (Tektona™) in non-osteoporotic spinal fractures

description: Additional file 1.
DOI: 10.6084/m9.figshare.19593899
title: Additional file 2 of Clinically relevant CHK1 inhibitors abrogate wild-type and Y537S mutant ERα expression and proliferation in luminal primary and metastatic breast cancer cells

description: Additional file 2. Supplementary Table 1
DOI: 10.6084/m9.figshare.19593899.v1
title: Additional file 2 of Clinically relevant CHK1 inhibitors abrogate wild-type and Y537S mutant ERα expression and proliferation in luminal primary and metastatic breast cancer cells

description: Additional file 2. Supplementary Table 1
DOI: 10.6084/m9.figshare.19593902
title: Additional file 3 of Clinically relevant CHK1 inhibitors abrogate wild-type and Y537S mutant ERα expression and proliferation in luminal primary and metastatic breast cancer cells

description: Additional file 3. Supplementary Table 2