cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.12854114
title: Paleoproterozoic S-type granites in the Lengshui complex, South China: Implications for the tectonic evolution of the Yangtze Block

description: Paleoproterozoic granitoids provide crucial constraints on the tectonic evolution of the Yangtze Block, South China, and its reconstructed position in the Columbia supercontinent. Here, we report zircon U–Pb age and Hf–isotope data coupled with whole-rock geochemistry for monzogranites from the Lengshui complex (LSC) of the Zhongxiang Terrane in the northern Yangtze Block. Zircon U–Pb dating yields crystallization ages of 2039 ± 36 Ma and 1950 ± 16 Ma for two monzogranite samples, respectively. Both samples show S-type granite affinities. The older S-type granites in the LSC are interpreted to record a subduction-related tectonic setting, whereas the younger ones are related to a syn-collisional setting. This scenario reflects a critical geodynamic transition during the assembly of the Columbia supercontinent at ca. 2.04–1.95 Ga within the Yangtze Block. The two granites have similar zircon Hf isotope ratios with ε<sub>Hf</sub>(t) values of −17.11 to −9.69 and T<sub>DM2</sub> ages of ca. 3.67–3.22 Ga, suggesting that the monzogranites could have been generated by partial melting of Archaean crustal materials in the Zhongxiang Terrane. Widespread Paleoproterozoic magmatism and metamorphism in the Yangtze Block indicate a change in tectonic regime from ca. 2.15–2.04 Ga subduction to ca. 2.0–1.93 Ga collision followed by ca. 1.87–1.82 Ga post-collisional extension. Based on the similarity of ages and rock types with other blocks in the Columbia supercontinent, our results support that the Yangtze Block may be placed near Laurentia in the Columbia supercontinent.
DOI: 10.6084/m9.figshare.12854114.v1
title: Paleoproterozoic S-type granites in the Lengshui complex, South China: Implications for the tectonic evolution of the Yangtze Block

description: Paleoproterozoic granitoids provide crucial constraints on the tectonic evolution of the Yangtze Block, South China, and its reconstructed position in the Columbia supercontinent. Here, we report zircon U–Pb age and Hf–isotope data coupled with whole-rock geochemistry for monzogranites from the Lengshui complex (LSC) of the Zhongxiang Terrane in the northern Yangtze Block. Zircon U–Pb dating yields crystallization ages of 2039 ± 36 Ma and 1950 ± 16 Ma for two monzogranite samples, respectively. Both samples show S-type granite affinities. The older S-type granites in the LSC are interpreted to record a subduction-related tectonic setting, whereas the younger ones are related to a syn-collisional setting. This scenario reflects a critical geodynamic transition during the assembly of the Columbia supercontinent at ca. 2.04–1.95 Ga within the Yangtze Block. The two granites have similar zircon Hf isotope ratios with ε<sub>Hf</sub>(t) values of −17.11 to −9.69 and T<sub>DM2</sub> ages of ca. 3.67–3.22 Ga, suggesting that the monzogranites could have been generated by partial melting of Archaean crustal materials in the Zhongxiang Terrane. Widespread Paleoproterozoic magmatism and metamorphism in the Yangtze Block indicate a change in tectonic regime from ca. 2.15–2.04 Ga subduction to ca. 2.0–1.93 Ga collision followed by ca. 1.87–1.82 Ga post-collisional extension. Based on the similarity of ages and rock types with other blocks in the Columbia supercontinent, our results support that the Yangtze Block may be placed near Laurentia in the Columbia supercontinent.
DOI: 10.6084/m9.figshare.20194140
title: Additional file 5 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 5. Table S8. Monthly precipitation (mm) at several sites reported within the wintering areas of both subspecies.
DOI: 10.6084/m9.figshare.20194134
title: Additional file 4 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 4. Table S7. List of random samples and monthly precipitation (mm) during the breeding season.
DOI: 10.6084/m9.figshare.20194134.v1
title: Additional file 4 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 4. Table S7. List of random samples and monthly precipitation (mm) during the breeding season.
DOI: 10.6084/m9.figshare.20194140.v1
title: Additional file 5 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 5. Table S8. Monthly precipitation (mm) at several sites reported within the wintering areas of both subspecies.
DOI: 10.6084/m9.figshare.20194146
title: Additional file 6 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 6. Table S9. List of random samples and monthly precipitation (mm) during the wintering season.
DOI: 10.6084/m9.figshare.12854123
title: Geochronology and geochemistry of early Carboniferous basalts from Baogutu Formation in West Junggar, Northwest China: evidence for a back-arc extension

description: Early Carboniferous magmatism of the southern West Junggar (SWJ) region is essential for understanding the accretionary processes and crustal growth in the southwestern segment of the Central Asian Orogenic Belt. A comprehensive study of geochronological, geochemical, and Sr-Nd-Pb-Hf isotopic compositions was carried out in this study for basalts from the Baogutu Formation in Sulushuoke region, aiming to provide constraints on the Early Carboniferous tectonic evolution of the SWJ, NW China. LA-ICP-MS zircon U-Pb dating of four basalt samples yielded crystallization ages ranging from 339 Ma to 347 Ma, indicating the presence of early Carboniferous volcanic rocks in West Junggar. The studied tholeiitic basalts are geochemically characterized by nearly flat REE patterns, enriched large iron lithosphere elements (e.g. K) and depleted high field strength elements (e.g. Nb, Ta, Zr, Hf) relative to those in N-MORB, resembling those of modern Mariana Trough back-arc basin basalts. In addition, they have high positive εNd(t) values (+5.86 to +6.59) with initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios in the range of 0.704783–0.705315 and variable εHf(t) values (+3.99 to +15.6). The rocks cover restricted ranges in initial Pb isotope ratios with (<sup>206</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> from 17.529 to 18.289, (<sup>207</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> from 15.509 to 15.627, and (<sup>208</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> from 37.628 to 38.397. These signatures indicate that the tholeiitic basalts were derived from 10% to 20% partial melting of a spinel-lherzolitic N-MORB-like depleted mantle source modified by fluids released from the subducted lithosphere in a back-arc extensional setting. From our new data presented in this study and in conjunction with those from previous works, we, therefore, suggest that a back-arc basin related to the northwestward subduction of the Junggar oceanic crust was developed in the Hatu-Baogutu region during the early Carboniferous time.
DOI: 10.6084/m9.figshare.20194146.v1
title: Additional file 6 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 6. Table S9. List of random samples and monthly precipitation (mm) during the wintering season.
DOI: 10.6084/m9.figshare.12854123.v1
title: Geochronology and geochemistry of early Carboniferous basalts from Baogutu Formation in West Junggar, Northwest China: evidence for a back-arc extension

description: Early Carboniferous magmatism of the southern West Junggar (SWJ) region is essential for understanding the accretionary processes and crustal growth in the southwestern segment of the Central Asian Orogenic Belt. A comprehensive study of geochronological, geochemical, and Sr-Nd-Pb-Hf isotopic compositions was carried out in this study for basalts from the Baogutu Formation in Sulushuoke region, aiming to provide constraints on the Early Carboniferous tectonic evolution of the SWJ, NW China. LA-ICP-MS zircon U-Pb dating of four basalt samples yielded crystallization ages ranging from 339 Ma to 347 Ma, indicating the presence of early Carboniferous volcanic rocks in West Junggar. The studied tholeiitic basalts are geochemically characterized by nearly flat REE patterns, enriched large iron lithosphere elements (e.g. K) and depleted high field strength elements (e.g. Nb, Ta, Zr, Hf) relative to those in N-MORB, resembling those of modern Mariana Trough back-arc basin basalts. In addition, they have high positive εNd(t) values (+5.86 to +6.59) with initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios in the range of 0.704783–0.705315 and variable εHf(t) values (+3.99 to +15.6). The rocks cover restricted ranges in initial Pb isotope ratios with (<sup>206</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> from 17.529 to 18.289, (<sup>207</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> from 15.509 to 15.627, and (<sup>208</sup>Pb/<sup>204</sup>Pb)<sub>i</sub> from 37.628 to 38.397. These signatures indicate that the tholeiitic basalts were derived from 10% to 20% partial melting of a spinel-lherzolitic N-MORB-like depleted mantle source modified by fluids released from the subducted lithosphere in a back-arc extensional setting. From our new data presented in this study and in conjunction with those from previous works, we, therefore, suggest that a back-arc basin related to the northwestward subduction of the Junggar oceanic crust was developed in the Hatu-Baogutu region during the early Carboniferous time.
DOI: 10.6084/m9.figshare.12854126
title: The Cryogenian Nanhuan System (South China) during the interglacial-glacial transition: geochemistry, sedimentary provenance, and tectonic setting

description: Samples of the Nanhuan System during the interglacial-glacial transition in the Shennongjia area, northern Yangtze block, were analysed via major and trace elements, clay mineralogy, and sulphur isotopes to infer provenance, paleoweathering intensity of the source rocks, tectonic setting, and marine chemistry. The magmatogenic sedimentary rocks are typical of acidic igneous sources, whereas the remaining samples show a sedimentary trend. The tectonic discrimination of a passive continental margin was determined via major element diagram. The samples showing subduction-affinity geochemistry may represent provenance virtually entirely comprising old recycled material. Low chemical index of alteration values and high illite contents of the sedimentary deposits reveal that the basin is characterized by physical erosion owing to the combined effects of tectonic movement and long-term cool and dry climatic conditions. Extreme δ<sup>34</sup>S enrichment in the Datangpo Formation indicates that this Cryogenian formation was a restricted rift basin with limited exchange with the open ocean. The δ<sup>34</sup>S<sub>sulfide</sub> and illite values increase rapidly at the end of the Sturtian glaciation followed by a sharp decline at the end of inter-glacial silt deposition. Low oceanic sulphate concentrations and intense bacterial reduction of sulphate may account for the <sup>34</sup>S enrichment in this restricted deep-water basin.
DOI: 10.6084/m9.figshare.20194119
title: Additional file 2 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 2. Table S6. Migration phenology of each individual in this study.
DOI: 10.6084/m9.figshare.20194119.v1
title: Additional file 2 of A 30,000-km journey by Apus apus pekinensis tracks arid lands between northern China and south-western Africa

description: Additional file 2. Table S6. Migration phenology of each individual in this study.
DOI: 10.6084/m9.figshare.12854126.v1
title: The Cryogenian Nanhuan System (South China) during the interglacial-glacial transition: geochemistry, sedimentary provenance, and tectonic setting

description: Samples of the Nanhuan System during the interglacial-glacial transition in the Shennongjia area, northern Yangtze block, were analysed via major and trace elements, clay mineralogy, and sulphur isotopes to infer provenance, paleoweathering intensity of the source rocks, tectonic setting, and marine chemistry. The magmatogenic sedimentary rocks are typical of acidic igneous sources, whereas the remaining samples show a sedimentary trend. The tectonic discrimination of a passive continental margin was determined via major element diagram. The samples showing subduction-affinity geochemistry may represent provenance virtually entirely comprising old recycled material. Low chemical index of alteration values and high illite contents of the sedimentary deposits reveal that the basin is characterized by physical erosion owing to the combined effects of tectonic movement and long-term cool and dry climatic conditions. Extreme δ<sup>34</sup>S enrichment in the Datangpo Formation indicates that this Cryogenian formation was a restricted rift basin with limited exchange with the open ocean. The δ<sup>34</sup>S<sub>sulfide</sub> and illite values increase rapidly at the end of the Sturtian glaciation followed by a sharp decline at the end of inter-glacial silt deposition. Low oceanic sulphate concentrations and intense bacterial reduction of sulphate may account for the <sup>34</sup>S enrichment in this restricted deep-water basin.
DOI: 10.6084/m9.figshare.12854129
title: Mesozoic intracontinental deformation of the Alxa Block in the middle part of Central Asian Orogenic Belt: A review

description: Intracontinental deformation is an inseparable element of the evolutionary history of orogenic belts. It can reactivate and intensely modify the structures of previous orogenic belts due to remote effects of plate margin orogenesis. As an important part of the Phanerozoic Central Asian Orogenic Belt (CAOB), the Alxa Block and its vicinity experienced multistage intracontinental deformation during the Mesozoic and Cenozoic and became a representative region to study remote effects from plate margins. Both the previous structures of the CAOB and continuous accretion to the Eurasian continent from different directions controlled and affected the Mesozoic evolution of the Alxa Block. However, mantle loading can’t pertinently explain the geological phenomena alone. In the Late Triassic, the Alxa Block was deformed by large-scale left-lateral shearing along largely northeast-southwest-trending faults and rotated anticlockwise caused by the collision between the North China Craton and Yangtze Craton and the northward movement of the North China Craton. In the Late Jurassic, the low-angle westward subduction of the Paleo-Pacific Ocean beneath the Eurasian Plate, the closure of the Mongol-Okhotsk Ocean to the north and/or the Lhasa-Qiangtang collision to the south combined to deform the Alxa Block from different directions, forming contraction structures with various strikes and invert previous extensional basins. In the Late Cretaceous, the Eurasian Plate experienced oblique collision along its southeastern margin and the subduction of the Neo-Tethys along its southern boundary, an intraplate sinistral transpressional megashear system developed along the eastern Alxa Block, and the uplift of mountain ranges along the basin margins. The multistage Mesozoic intracontinental deformation of the Alxa Block supports the view that they are driven by stresses generated at plate boundaries largely, and controlled by previous complicated orogenic structures in the upper crust.
DOI: 10.6084/m9.figshare.12854129.v1
title: Mesozoic intracontinental deformation of the Alxa Block in the middle part of Central Asian Orogenic Belt: A review

description: Intracontinental deformation is an inseparable element of the evolutionary history of orogenic belts. It can reactivate and intensely modify the structures of previous orogenic belts due to remote effects of plate margin orogenesis. As an important part of the Phanerozoic Central Asian Orogenic Belt (CAOB), the Alxa Block and its vicinity experienced multistage intracontinental deformation during the Mesozoic and Cenozoic and became a representative region to study remote effects from plate margins. Both the previous structures of the CAOB and continuous accretion to the Eurasian continent from different directions controlled and affected the Mesozoic evolution of the Alxa Block. However, mantle loading can’t pertinently explain the geological phenomena alone. In the Late Triassic, the Alxa Block was deformed by large-scale left-lateral shearing along largely northeast-southwest-trending faults and rotated anticlockwise caused by the collision between the North China Craton and Yangtze Craton and the northward movement of the North China Craton. In the Late Jurassic, the low-angle westward subduction of the Paleo-Pacific Ocean beneath the Eurasian Plate, the closure of the Mongol-Okhotsk Ocean to the north and/or the Lhasa-Qiangtang collision to the south combined to deform the Alxa Block from different directions, forming contraction structures with various strikes and invert previous extensional basins. In the Late Cretaceous, the Eurasian Plate experienced oblique collision along its southeastern margin and the subduction of the Neo-Tethys along its southern boundary, an intraplate sinistral transpressional megashear system developed along the eastern Alxa Block, and the uplift of mountain ranges along the basin margins. The multistage Mesozoic intracontinental deformation of the Alxa Block supports the view that they are driven by stresses generated at plate boundaries largely, and controlled by previous complicated orogenic structures in the upper crust.
DOI: 10.6084/m9.figshare.19669879
title: Additional file 5 of Proton pump inhibitors induce changes in the gut microbiome composition of systemic lupus erythematosus patients

description: Additional file 5.
DOI: 10.6084/m9.figshare.19669879.v1
title: Additional file 5 of Proton pump inhibitors induce changes in the gut microbiome composition of systemic lupus erythematosus patients

description: Additional file 5.
DOI: 10.6084/m9.figshare.19669871
title: Additional file 3 of Identification of ARF family in blueberry and its potential involvement of fruit development and pH stress response

description: Additional file 3: Table S3. Primers used in the study
DOI: 10.6084/m9.figshare.19669871.v1
title: Additional file 3 of Identification of ARF family in blueberry and its potential involvement of fruit development and pH stress response

description: Additional file 3: Table S3. Primers used in the study
DOI: 10.6084/m9.figshare.19669880
title: Additional file 6 of Identification of ARF family in blueberry and its potential involvement of fruit development and pH stress response

description: Additional file 6. Raw data for qRT-PCR investigation during fruit development.
DOI: 10.6084/m9.figshare.19669880.v1
title: Additional file 6 of Identification of ARF family in blueberry and its potential involvement of fruit development and pH stress response

description: Additional file 6. Raw data for qRT-PCR investigation during fruit development.
DOI: 10.6084/m9.figshare.19669898.v1
title: Additional file 1 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 1: Supplementary Table 1. DEGs_of_4_datasets.
DOI: 10.6084/m9.figshare.19669901.v1
title: Additional file 2 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 2: Supplementary Table 2. IDs_of_samples_with_taxol_treatment.
DOI: 10.6084/m9.figshare.19669904
title: Additional file 3 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 3: Supplementary Table 3. Taxol_IC50_and_RIPK2_expression.
DOI: 10.6084/m9.figshare.19669907
title: Additional file 4 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 4: Supplementary Table 4. Genes_co-expressed_with_RIPK2.
DOI: 10.6084/m9.figshare.19669907.v1
title: Additional file 4 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 4: Supplementary Table 4. Genes_co-expressed_with_RIPK2.
DOI: 10.6084/m9.figshare.19669901
title: Additional file 2 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 2: Supplementary Table 2. IDs_of_samples_with_taxol_treatment.
DOI: 10.6084/m9.figshare.19669904.v1
title: Additional file 3 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 3: Supplementary Table 3. Taxol_IC50_and_RIPK2_expression.
DOI: 10.6084/m9.figshare.19669910
title: Additional file 5 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 5: Supplementary Table 5. GO,KEGG_and_PPI_analysis.
DOI: 10.6084/m9.figshare.19669910.v1
title: Additional file 5 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 5: Supplementary Table 5. GO,KEGG_and_PPI_analysis.
DOI: 10.6084/m9.figshare.19669913
title: Additional file 6 of High expression of RIPK2 is associated with Taxol resistance in serous ovarian cancer

description: Additional file 6: Supplementary Table 6. Relationship_of_CNA_with_RIPK2.
DOI: 10.15156/bio/sh1307579.09fu
title: SH1307579.09FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1307580.09fu
title: SH1307580.09FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.