cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.hdpzub
title: Occurrence Download

description: A dataset containing 244532 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Cuculiformes)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Year is greater than or equal to 1980",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen)"
 ]
 }
 },
 "Geometry POLYGON((150 -60,180 -60,180 -30,150 -30,150 -60))"
 ]
}

 The dataset includes 244532 records from 48 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002179-251009101135966/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5517/cctvtwb
title: CCDC 770563: Experimental Crystal Structure Determination

description: Related Article: Amit Kumar Dutta, Suvendu Samanta, Supriya Dutta, C. Robert Lucas, Louise N. Dawe, Papu Biswas, Bibhutosh Adhikary|2016|J.Mol.Struct.|1115|207|doi:10.1016/j.molstruc.2016.02.101
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccv59s2
title: CCDC 779674: Experimental Crystal Structure Determination

description: Related Article: Hong-Ru Dong, Zhong-Lian Gao, Rong-Shan Li, Yi-Ming Hu, Heng-Shan Dong, Zhi-Xiang Xie|2014|RSC Advances|4|55827|doi:10.1039/C4RA02714K
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccv5f6m
title: CCDC 779780: Experimental Crystal Structure Determination

description: Related Article: Hong-Ru Dong, Zhong-Lian Gao, Rong-Shan Li, Yi-Ming Hu, Heng-Shan Dong, Zhi-Xiang Xie|2014|RSC Advances|4|55827|doi:10.1039/C4RA02714K
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvcg4s
title: CCDC 785575: Experimental Crystal Structure Determination

description: Related Article: Min Liu, Yu-Ping Yang, Yong-Sheng Yang, Qi-Ming Qiu, Qiong-Hua Jin, Qing-Xuan Meng, Hua Chen, Wei Yang, Yong-Cheng Dai, Li-Jun Xu|2015|Polyhedron|88|199|doi:10.1016/j.poly.2014.12.027
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvcg5t
title: CCDC 785576: Experimental Crystal Structure Determination

description: Related Article: Min Liu, Yu-Ping Yang, Yong-Sheng Yang, Qi-Ming Qiu, Qiong-Hua Jin, Qing-Xuan Meng, Hua Chen, Wei Yang, Yong-Cheng Dai, Li-Jun Xu|2015|Polyhedron|88|199|doi:10.1016/j.poly.2014.12.027
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvcg6v
title: CCDC 785577: Experimental Crystal Structure Determination

description: Related Article: Min Liu, Yu-Ping Yang, Yong-Sheng Yang, Qi-Ming Qiu, Qiong-Hua Jin, Qing-Xuan Meng, Hua Chen, Wei Yang, Yong-Cheng Dai, Li-Jun Xu|2015|Polyhedron|88|199|doi:10.1016/j.poly.2014.12.027
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvgnwt
title: CCDC 788667: Experimental Crystal Structure Determination

description: Related Article: Ramón Moreno-Corral, Herbert Höpfl, Anatoly K. Yatsimirsky, Juan Carlos Gálvez-Ruiz, Karen O. Lara|2015|Tetrahedron|71|1232|doi:10.1016/j.tet.2015.01.005
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvgnxv
title: CCDC 788668: Experimental Crystal Structure Determination

description: Related Article: Ramón Moreno-Corral, Herbert Höpfl, Anatoly K. Yatsimirsky, Juan Carlos Gálvez-Ruiz, Karen O. Lara|2015|Tetrahedron|71|1232|doi:10.1016/j.tet.2015.01.005
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvgnyw
title: CCDC 788669: Experimental Crystal Structure Determination

description: Related Article: Ramón Moreno-Corral, Herbert Höpfl, Anatoly K. Yatsimirsky, Juan Carlos Gálvez-Ruiz, Karen O. Lara|2015|Tetrahedron|71|1232|doi:10.1016/j.tet.2015.01.005
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvgnzx
title: CCDC 788670: Experimental Crystal Structure Determination

description: Related Article: Ramón Moreno-Corral, Herbert Höpfl, Anatoly K. Yatsimirsky, Juan Carlos Gálvez-Ruiz, Karen O. Lara|2015|Tetrahedron|71|1232|doi:10.1016/j.tet.2015.01.005
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvgp0z
title: CCDC 788671: Experimental Crystal Structure Determination

description: Related Article: Ramón Moreno-Corral, Herbert Höpfl, Anatoly K. Yatsimirsky, Juan Carlos Gálvez-Ruiz, Karen O. Lara|2015|Tetrahedron|71|1232|doi:10.1016/j.tet.2015.01.005
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccvgp10
title: CCDC 788672: Experimental Crystal Structure Determination

description: Related Article: Ramón Moreno-Corral, Herbert Höpfl, Anatoly K. Yatsimirsky, Juan Carlos Gálvez-Ruiz, Karen O. Lara|2015|Tetrahedron|71|1232|doi:10.1016/j.tet.2015.01.005
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.6084/m9.figshare.31045561
title: The gsmap results of sick sinus syndrome and atrial fibrillation

description: This folder contains gsMap output for the traits Atrial Fibrillation and Sick Sinus Syndrome on the MOSTA E16.5_E1S1 spatial transcriptomics sample. For each trait, there are three visualization subfolders: gsMap_plot/ (spatial maps showing where the trait-associated signal is enriched across the tissue section), GSS_plot/ (plots of Gene Specificity Score, GSS, illustrating where candidate genes are specifically expressed in space), and manhattan_plot/ (GWAS-style Manhattan/diagnostic plots summarizing genomic association signals). In addition, E16.5_E1S1.MOSTA_*_Gene_Diagnostic_Info.csv provides a gene-level diagnostic table (e.g., genes with their spatial annotation, summary GSS metrics such as median GSS, and correlation-style indicators linking spatial specificity to GWAS signal), while E16.5_E1S1.MOSTA_*_gsMap_Report.html is an integrated HTML report that brings together the key figures and summaries for quick interpretation and result review.
DOI: 10.6084/m9.figshare.31045561.v1
title: The gsmap results of sick sinus syndrome and atrial fibrillation

description: This folder contains gsMap output for the traits Atrial Fibrillation and Sick Sinus Syndrome on the MOSTA E16.5_E1S1 spatial transcriptomics sample. For each trait, there are three visualization subfolders: gsMap_plot/ (spatial maps showing where the trait-associated signal is enriched across the tissue section), GSS_plot/ (plots of Gene Specificity Score, GSS, illustrating where candidate genes are specifically expressed in space), and manhattan_plot/ (GWAS-style Manhattan/diagnostic plots summarizing genomic association signals). In addition, E16.5_E1S1.MOSTA_*_Gene_Diagnostic_Info.csv provides a gene-level diagnostic table (e.g., genes with their spatial annotation, summary GSS metrics such as median GSS, and correlation-style indicators linking spatial specificity to GWAS signal), while E16.5_E1S1.MOSTA_*_gsMap_Report.html is an integrated HTML report that brings together the key figures and summaries for quick interpretation and result review.
DOI: 10.6084/m9.figshare.30530569
title: Late Jurassic-Early Cretaceous sediment-hosted Zn-Pb mineralization in western Iran: a world-class example of passive margin mineralization

description: Iran has more than 400 Late Jurassic-Early Cretaceous sediment-hosted Zn and Pb deposits. These are valuable resources that also provide insights into the tectonic history of the northern Neo-Tethys rim in western Iran. In this review, we compiled available data for twenty-six Zn-Pb deposits in eight mineral districts in the Malayer-Esfahan Metallogenic Belt (MEMB) of western Iran to better understand this mineralization system, specifically to test if these formed on a passive margin within a Jurassic to Early Cretaceous passive margin. Basal terrigenous deposits grade upward into shallow-water carbonates, providing a favourable stratigraphic framework for mineralization. Hydrothermal circulation was driven by coeval magmatism and focused along syn-sedimentary normal faults, which acted as conduits for fluid flow. Carbon, O, S, and Pb isotope ratios indicate diverse sources for the Zn-Pb deposits: Pb from the crust, S from seawater (mediated by microbes), and host-rock sources for C and O. Hydrothermal systems involving 80–130°C brines precipitated mainly sphalerite and galena in Jurassic and Early Cretaceous carbonate and shale host rocks. We conclude that the Jurassic-Early Cretaceous Zn-Pb mineralization in western Iran occurred at a passive continental margin that was underlain by continental rift basins in a horst-graben system parallel to the Neo-Tethys Ocean.
DOI: 10.6084/m9.figshare.30530569.v1
title: Late Jurassic-Early Cretaceous sediment-hosted Zn-Pb mineralization in western Iran: a world-class example of passive margin mineralization

description: Iran has more than 400 Late Jurassic-Early Cretaceous sediment-hosted Zn and Pb deposits. These are valuable resources that also provide insights into the tectonic history of the northern Neo-Tethys rim in western Iran. In this review, we compiled available data for twenty-six Zn-Pb deposits in eight mineral districts in the Malayer-Esfahan Metallogenic Belt (MEMB) of western Iran to better understand this mineralization system, specifically to test if these formed on a passive margin within a Jurassic to Early Cretaceous passive margin. Basal terrigenous deposits grade upward into shallow-water carbonates, providing a favourable stratigraphic framework for mineralization. Hydrothermal circulation was driven by coeval magmatism and focused along syn-sedimentary normal faults, which acted as conduits for fluid flow. Carbon, O, S, and Pb isotope ratios indicate diverse sources for the Zn-Pb deposits: Pb from the crust, S from seawater (mediated by microbes), and host-rock sources for C and O. Hydrothermal systems involving 80–130°C brines precipitated mainly sphalerite and galena in Jurassic and Early Cretaceous carbonate and shale host rocks. We conclude that the Jurassic-Early Cretaceous Zn-Pb mineralization in western Iran occurred at a passive continental margin that was underlain by continental rift basins in a horst-graben system parallel to the Neo-Tethys Ocean.
DOI: 10.6084/m9.figshare.30576636.v1
title: Cenozoic flare-up in the Eastern Iran magmatic belt: the dynamic link between closure of the Neotethyan ocean and magmatic events in the Lut Block

description: In this study, we focus on the Cenozoic magmatic suites in the Lut Block, a segment of the EIMB. The investigated plutonic rocks in the Lut Block, ranging in age from 47 to 37 Ma, encompass a wide compositional range from mafic to felsic, displaying medium to high-K calc-alkaline affinities. Epsilon Nd values in the investigated rocks range between −2.8 and +2.8, and the initial Sr isotope ratios is constrained to 0.7045‒0.7065. The age-corrected Pb isotopic compositions display ratios of<sup>2 0 6</sup> Pb/<sup>2 0 4</sup> Pb between 18.01 and 18.46, <sup>2 0 7</sup> Pb/<sup>2 0 4</sup> Pb from 15.49 to 15.57, and<sup>2 0 8</sup> Pb/<sup>2 0 4</sup> Pb ranging from 38.19 to 38.47. Isotopic–incompatible trace elements modelling reveals the contribution of up to 2.5% sediment-derived melt and approximately 7% to as little as 2% assimilation of continental crust. A broader perspective on the Lut Block geochronological–isotopic data reveals a transitional shift in magmatism from the eastern (e.g. Bajestan; ~ 82 Ma) to the western (e.g. NW Gonabad, Gazu, Kajeh, and Vaghi; ~80 Ma to ~60 Ma) segments, peaking in magmatism during ~45 to ~38 Ma. This shift in magmatism may be associated with a change in the subduction mechanism of the Neo-Tethyan slab beneath Central Iran, transitioning from a low-angle dip to a higher dip following slab roll-back and the tilting of the lithospheric mantle along Eastern Iran. We hypothesize partial melting of phlogopite-bearing mantle sources metasomatized by sediment melts within the pre-collisional tectonic context, contributing to the widespread Eocene high-K magmatism throughout the Lut Block.
DOI: 10.6084/m9.figshare.30488104.v1
title: Neoarchaean granitoid complexes in the Laoling area, Jilin Province, North China Craton: transition from mantle plume to plate subduction

description: The application of zircon U-Pb geochronology, geochemistry, and Hf isotope analysis to the granitoid complex in the Laoling area of southern Jilin Province (SJP) in the northeastern part of the North China Craton can provide valuable insights into its petrogenesis and tectonic setting. The predominant rock types found in SJP granitoid complex encompass monzonitic granite, tonalite, and various other varieties. The zircon U-Pb dating results indicate that the monzonitic granite (N20HT-1–1) crystallized at 2499 ± 4.2 Ma, the tonalite (N20HT-2–1) at 2722 ± 30 Ma, and the mylonitized tonalite (PH01-14–2) at 2505 ± 15 Ma, the monzonitic granite (DA19-3) at 2563 ± 16 Ma. Through the analysis of Hf isotopes, two-stage depleted mantle model ages, and elemental geochemistry, the inference can be made that tonalite enriched with the residual magmatic zircon are originally formed by the partial melting of ~3.4 Ga basaltic crust. Besides, the magmas of the monzonitic granite and mylonitized tonalite were sourced from the partial melting of potassium-rich basaltic rocks and a small amount of metasedimentary units and TTG suite rocks within the lower crust of the Meso- to Neoarchaean (3.1–2.7 Ga) continental framework. Based on this study and previous findings, it can be concluded that there are primarily three phases of magmatic activity in SJP: During the Mid Neoarchaean period (~2.7 Ga), the basaltic crust underwent partial melting due to the tectonic influence of a mantle plume, resulting in the formation and emplacement of tonalite-trondhjemitic magma. In the Late Neoarchaean period (~2.6 Ga), a transition occurred from mantle plume to plate subduction. It was during this time that monzonitic granite began to develop, suggesting the initiation of the plate tectonic system. At the End Neoarchaean period (~2.5 Ga), a significant amount of potassium-rich granite erupted as a result of plate subduction processes. Furthermore, it is worth noting that the tectonic setting for monzonitic granite in SJP indicates a post-orogenic extensional environment, implying that felsic magmatism during this phase is associated with dynamic processes related to arc-continent collision caused by plate subduction followed by subsequent post-collision extension.
DOI: 10.6084/m9.figshare.30576636
title: Cenozoic flare-up in the Eastern Iran magmatic belt: the dynamic link between closure of the Neotethyan ocean and magmatic events in the Lut Block

description: In this study, we focus on the Cenozoic magmatic suites in the Lut Block, a segment of the EIMB. The investigated plutonic rocks in the Lut Block, ranging in age from 47 to 37 Ma, encompass a wide compositional range from mafic to felsic, displaying medium to high-K calc-alkaline affinities. Epsilon Nd values in the investigated rocks range between −2.8 and +2.8, and the initial Sr isotope ratios is constrained to 0.7045‒0.7065. The age-corrected Pb isotopic compositions display ratios of<sup>2 0 6</sup> Pb/<sup>2 0 4</sup> Pb between 18.01 and 18.46, <sup>2 0 7</sup> Pb/<sup>2 0 4</sup> Pb from 15.49 to 15.57, and<sup>2 0 8</sup> Pb/<sup>2 0 4</sup> Pb ranging from 38.19 to 38.47. Isotopic–incompatible trace elements modelling reveals the contribution of up to 2.5% sediment-derived melt and approximately 7% to as little as 2% assimilation of continental crust. A broader perspective on the Lut Block geochronological–isotopic data reveals a transitional shift in magmatism from the eastern (e.g. Bajestan; ~ 82 Ma) to the western (e.g. NW Gonabad, Gazu, Kajeh, and Vaghi; ~80 Ma to ~60 Ma) segments, peaking in magmatism during ~45 to ~38 Ma. This shift in magmatism may be associated with a change in the subduction mechanism of the Neo-Tethyan slab beneath Central Iran, transitioning from a low-angle dip to a higher dip following slab roll-back and the tilting of the lithospheric mantle along Eastern Iran. We hypothesize partial melting of phlogopite-bearing mantle sources metasomatized by sediment melts within the pre-collisional tectonic context, contributing to the widespread Eocene high-K magmatism throughout the Lut Block.
DOI: 10.6084/m9.figshare.30488104
title: Neoarchaean granitoid complexes in the Laoling area, Jilin Province, North China Craton: transition from mantle plume to plate subduction

description: The application of zircon U-Pb geochronology, geochemistry, and Hf isotope analysis to the granitoid complex in the Laoling area of southern Jilin Province (SJP) in the northeastern part of the North China Craton can provide valuable insights into its petrogenesis and tectonic setting. The predominant rock types found in SJP granitoid complex encompass monzonitic granite, tonalite, and various other varieties. The zircon U-Pb dating results indicate that the monzonitic granite (N20HT-1–1) crystallized at 2499 ± 4.2 Ma, the tonalite (N20HT-2–1) at 2722 ± 30 Ma, and the mylonitized tonalite (PH01-14–2) at 2505 ± 15 Ma, the monzonitic granite (DA19-3) at 2563 ± 16 Ma. Through the analysis of Hf isotopes, two-stage depleted mantle model ages, and elemental geochemistry, the inference can be made that tonalite enriched with the residual magmatic zircon are originally formed by the partial melting of ~3.4 Ga basaltic crust. Besides, the magmas of the monzonitic granite and mylonitized tonalite were sourced from the partial melting of potassium-rich basaltic rocks and a small amount of metasedimentary units and TTG suite rocks within the lower crust of the Meso- to Neoarchaean (3.1–2.7 Ga) continental framework. Based on this study and previous findings, it can be concluded that there are primarily three phases of magmatic activity in SJP: During the Mid Neoarchaean period (~2.7 Ga), the basaltic crust underwent partial melting due to the tectonic influence of a mantle plume, resulting in the formation and emplacement of tonalite-trondhjemitic magma. In the Late Neoarchaean period (~2.6 Ga), a transition occurred from mantle plume to plate subduction. It was during this time that monzonitic granite began to develop, suggesting the initiation of the plate tectonic system. At the End Neoarchaean period (~2.5 Ga), a significant amount of potassium-rich granite erupted as a result of plate subduction processes. Furthermore, it is worth noting that the tectonic setting for monzonitic granite in SJP indicates a post-orogenic extensional environment, implying that felsic magmatism during this phase is associated with dynamic processes related to arc-continent collision caused by plate subduction followed by subsequent post-collision extension.
DOI: 10.15468/dl.mcrm9s
title: Occurrence Download

description: A dataset containing 11624533 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Japan",
 "HasCoordinate is true",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 11624533 records from 2036 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0003253-260108223611665/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.dfdks3
title: Occurrence Download

description: A dataset containing 231944343 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Year 1850-2020",
 "TaxonKey is Plantae"
 ]
}

 The dataset includes 231944343 records from 6132 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0072472-200221144449610/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.fpzsva
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Actinopterygii",
 "Year is 1989"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0007171-250426092105405/datasets/export for details.
DOI: 10.17182/hepdata.21337.v1/t1
title: "Table 1" of "Neutron-Proton Differential-Cross-Section Measurements at 50 MeV"

description: No description provided.
description: UCD-CYC. Neutron-proton differential cross section measurements at 50 MeV.