cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5517/ccdc.csd.cc27zwsx
title: CCDC 2085270: Experimental Crystal Structure Determination

description: Related Article: Chiara Costabile, Annaluisa Mariconda, Marco Sirignano, Alessandra Crispini, Francesca Scarpelli, Pasquale Longo|2021|New J.Chem.|45|18509|doi:10.1039/D1NJ03444H
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: 10.21227/7b5a-g160
title: Test Dataset

description: Test Abstract
DOI: 10.6084/m9.figshare.20496354.v1
title: Lungfish terrestrial traces

description: Data from Falkingham and Horner 2016 "Trackways produced by lungfish during terrestrial locomotion" <em>Scientific Reports</em>. <br> Includes photos taken for photogrammetry over multiple runs. Only some of these appeared in the publication. <br> Paper available here: <sub>Trackways Produced by Lungfish During Terrestrial Locomotion | Scientific Reports (nature.com)</sub> <br> Please cite that paper if using these data.
DOI: 10.6084/m9.figshare.20496354
title: Lungfish terrestrial traces

description: Data from Falkingham and Horner 2016 "Trackways produced by lungfish during terrestrial locomotion" <em>Scientific Reports</em>. <br> Includes photos taken for photogrammetry over multiple runs. Only some of these appeared in the publication. <br> Paper available here: <sub>Trackways Produced by Lungfish During Terrestrial Locomotion | Scientific Reports (nature.com)</sub> <br> Please cite that paper if using these data.
DOI: 10.6084/m9.figshare.20497245
title: Original data to the paper: Effects of coenzyme Q10 supplementation on lipid profiles

description: This is the original data used by the meta-analysis entitled “Effects of coenzyme Q10 supplementation on lipid profiles in adults: a meta-analysis of randomized controlled trials”.
DOI: 10.6084/m9.figshare.20497245.v1
title: Original data to the paper: Effects of coenzyme Q10 supplementation on lipid profiles

description: This is the original data used by the meta-analysis entitled “Effects of coenzyme Q10 supplementation on lipid profiles in adults: a meta-analysis of randomized controlled trials”.
DOI: 10.6084/m9.figshare.20496195
title: Datasets and models for the Project CodeImposter

description: The datasets and models for the Project CodeImposter at: <br> https://github.com/testing-cs/CodeImposter
DOI: 10.6084/m9.figshare.20496195.v2
title: Datasets and models for the Project CodeImposter

description: The datasets and models for the Project CodeImposter at: <br> https://github.com/testing-cs/CodeImposter
DOI: 10.6084/m9.figshare.20496195.v1
title: Datasets and models for the Project CodeImposter

description: The datasets and models for the Project CodeImposter at: <br> https://github.com/testing-cs/CodeImposter
DOI: 10.6084/m9.figshare.20497263
title: PTB_Supplementary_Table_1.xlsx

description: Dataset for the paper titled " Different <em>p</em>CO2 regimes distinguish the early and late phases of Permian-Triassic mass extinction "
DOI: 10.5517/ccdc.csd.cc27kg5g
title: CCDC 2072355: Experimental Crystal Structure Determination

description: Related Article: Meng-Meng Lun, Fo-Ling Zhou, Da-Wei Fu, Qiong Ye|2022|J.Mater.Chem.C|10|11371|doi:10.1039/D2TC01063A
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/ccdc.csd.cc2897d7
title: CCDC 2094248: Experimental Crystal Structure Determination

description: Related Article: Meng-Meng Lun, Fo-Ling Zhou, Da-Wei Fu, Qiong Ye|2022|J.Mater.Chem.C|10|11371|doi:10.1039/D2TC01063A
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/ccdc.csd.cc28bhlq
title: CCDC 2095463: Experimental Crystal Structure Determination

description: Related Article: Dalia I saleh, Dalal Alhashmialameer, Samy F. Mahmoud, Safaa Eldin H. Etaiw|2022|J.Mol.Struct.|1267|133597|doi:10.1016/j.molstruc.2022.133597
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/ccdc.csd.cc27dc12
title: CCDC 2067453: Experimental Crystal Structure Determination

description: Related Article: Meng-Meng Lun, Fo-Ling Zhou, Da-Wei Fu, Qiong Ye|2022|J.Mater.Chem.C|10|11371|doi:10.1039/D2TC01063A
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/ccdc.csd.cc2bpssm
title: CCDC 2165901: Experimental Crystal Structure Determination

description: Related Article: Muhammad Saddam Hossain, Fiaz Ahmed, Stavros G. Karakalos, Mark D. Smith, Namrata Pant, Sophya Garashchuk, Andrew B. Greytak, Pablo Docampo, Linda S. Shimizu|2022|Phys.Chem.Chem.Phys.(PCCP)|24|18729|doi:10.1039/D2CP01856J
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/ccdc.csd.cc2bwq54
title: CCDC 2171586: Experimental Crystal Structure Determination

description: Related Article: Keke Han, Mengxia Zhang, Zhenhong Wei, Xing Ye, Wenjun Rao, Haina Zhang, Hu Cai|2022|Chem.Commun.|58|9254|doi:10.1039/D2CC02673B
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: 10.21227/255j-n111
title: Test instances for TSMC3198829

description: This dataset contains the test instances for the paper "A Matrix-cube-based Estimation of Distribution Algorithm for No-Wait Flow-Shop Scheduling with Sequence-Dependent Setup Times and Release Times".搜索复制
DOI: 10.57695/ecxp-je78
title: Spatiotemporal and emission characteristics of laser-induced plasmas from aluminum-zirconium composite powders
DOI: 10.34740/kaggle/dsv/4080066
title: Elon Musk Tweets
DOI: 10.5517/ccdc.csd.cc2cj4nq
title: CCDC 2190263: Experimental Crystal Structure Determination

description: Related Article: Keke Han, Mengxia Zhang, Zhenhong Wei, Xing Ye, Wenjun Rao, Haina Zhang, Hu Cai|2022|Chem.Commun.|58|9254|doi:10.1039/D2CC02673B
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: 10.18112/openneuro.ds004248.v1.0.8
title: AMSI-DatasetB
DOI: 10.5281/zenodo.6985021
title: Dendritic Spine Datasets

description: Datasets used in Argunşah, A.Ö., Erdil, E., Ghani, M.U. et al. An interactive time series image analysis software for dendritic spines. Sci Rep 12, 12405 (2022). https://doi.org/10.1038/s41598-022-16137-y 5 Datasets of Raw Data Labeled Dataset for Dendritic Feature Detector Training and Testing Trained Network for 9 Classes
description: Contact argunsah@hifo.uzh.ch for more information.
description: {"references": ["Argun\u015fah, A.\u00d6., Erdil, E., Ghani, M.U. et al. An interactive time series image analysis software for dendritic spines. Sci Rep 12, 12405 (2022). https://doi.org/10.1038/s41598-022-16137-y"]}
DOI: 10.5281/zenodo.6985022
title: Dendritic Spine Datasets

description: Datasets used in Argunşah, A.Ö., Erdil, E., Ghani, M.U. et al. An interactive time series image analysis software for dendritic spines. Sci Rep 12, 12405 (2022). https://doi.org/10.1038/s41598-022-16137-y 5 Datasets of Raw Data Labeled Dataset for Dendritic Feature Detector Training and Testing Trained Network for 9 Classes
description: Contact argunsah@hifo.uzh.ch for more information.
description: {"references": ["Argun\u015fah, A.\u00d6., Erdil, E., Ghani, M.U. et al. An interactive time series image analysis software for dendritic spines. Sci Rep 12, 12405 (2022). https://doi.org/10.1038/s41598-022-16137-y"]}
DOI: 10.5519/qd.206dano3
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (8681 records)
DOI: 10.6073/pasta/edcb50920ecc86a60745fe3a857fc7bc
title: Standard body length of Euphausia superba collected with a 2-m, 700-um net towed from surface to 120 m, collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009 - 2020.

description: Antarctic krill, Euphausia superba, are a critical food-web link between phytoplankton primary production and higher trophic levels, such as whales, penguins, and seals. Krill standard length was measured from LTER zooplankton tows along the western Antarctic Peninsula. Length data provides estimates of age-class abundance and recruitment. Climate-induced changes in krill recruitment are an important consideration in the management and modelling of krill populations.
DOI: 10.6073/pasta/6f3b29f40e3588ecd3a6c64d2dc2a1e2
title: Length of Salpa thompsoni collected with a 2-m, 700-um net towed from surface to 120 m, collected aboard Palmer LTER annual cruises off the coast of the Western Antarctic Peninsula, 2009 - 2020.

description: Salps (Salpa thompsoni) are conspicuous gelatinous zooplankton capable of rapid population increases, enabling them to respond quickly to unpredictable phytoplankton blooms common in the Antarctic. Body length was measured on salps collected from LTER zooplankton tows along the western Antarctic Peninsula. Salps have amongst the highest filtration rates of all zooplankton, and package their waste into large, fast sinking fecal pellets. These pellets provide a mechanism to export carbon fixed in the surface waters into the deep ocean. Since filtration rates and pellet size are positively related to the size of a salp, population estimates of grazing and exported carbon can be determined through length data.
DOI: 10.6084/m9.figshare.19091423.v1
title: Absence of enterotypes in the human gut microbiomes reanalyzed with non-linear dimensionality reduction methods

description: Enterotypes of the human gut microbiome have been proposed to be a powerful prognostic tool to evaluate the correlation between lifestyle, nutrition, and disease. However, the number of enterotypes suggested in the literature ranged from two to four. The growth of available metagenome data and the use of exact, non-linear methods of data analysis challenges the very concept of clusters in the multidimensional space of bacterial microbiomes. <br>We demonstrate the presence of a lower-dimensional structure in the microbiome space, with high-dimensional data concentrated near a low-dimensional non-linear submanifold, but the absence of distinct and stable clusters that could represent enterotypes. This observation is robust with regard to diverse combinations of dimensionality reduction techniques and clustering algorithms.<br><br>We used <strong>16S rRNA </strong>genotype data from the National Institutes of Health <strong>Human Microbiome Project (HMP)</strong> and <strong>American Gut Project (AGP) </strong>presented in <strong>Order, Family, and Genus taxonomic levels (O, F, and G, respectively)</strong>.These largest open-access available datasets provide a sufficient number of data points for correct estimation of the clustering partition and constructing a manifold. We used 3457 HMP samples from stool and rectum body sites downloaded from https://portal.hmpdacc.org/ and 9511 samples from AGP downloaded from https://figshare.com/ as abundance matrices.<br>All datasets were normalized by dividing the Operational Taxonomic Units (OTUs) values by the total sum of abundances for a given data sample.
DOI: 10.6084/m9.figshare.16443929
title: Neoproterozoic to Jurassic tectono-metamorphic events in the Sierra Nevada de Santa Marta Massif, Colombia: insights from zircon U-Pb geochronology and trace element geochemistry

description: The Sierra Nevada de Santa Marta Massif (SNSM) in the Northern Andes affords an insight into lower crustal section structural relations. This polymetamorphic basement comprises high-grade gneisses, which alternate with imbricate slivers of medium-to high-grade schists. New field observations coupled with LA-ICP-MS U-Pb zircon geochronology and trace element geochemistry reveal some hallmarks on the evolution of this strongly remobilized crustal section. The Proterozoic Rodinia-type basement (1100 − 880 Ma) recorded at least two separated tectono-metamorphic events (M<sub>0</sub> and M<sub>1</sub>) and was subsequently affected by a magmatic episode during the Ordovician (<b>~</b>450 Ma; M<sub>2</sub>). During the Permian, subduction of Panthalassian oceanic crust beneath Pangaea led to the installation of a magmatic-arc and probably coeval metamorphism (<b>~</b>288-266 Ma; M<sub>3</sub>). Middle-Late Triassic roll-back extension of the upper plate led to anatexis and metamorphism (M<sub>4</sub>) reaching peak conditions at ca. 239 Ma with concurrent crystallization of garnet and sillimanite, followed by a decreasing geothermal gradient at ca. 202 Ma. Early Jurassic arc build-up under a rejuvenated convergence was contemporaneous to metamorphism on an accretionary wedge (M<sub>5</sub>) at ca. 185 Ma. The SNSM Massif basement units yield metamorphic ages that compare to similar tectono-metamorphic provinces in NW-Gondwana, including the Central Cordillera of Colombia, the Guajira Peninsula, the Mérida Andes, the Perijá Range, the Santander Massif, and the Central American and Mexican terranes to the south of the Ouachita-Marathon Suture (Oaxaquia, Mixteca, and Maya blocks). Age equivalence of these events is best explained by the existence of a conjugate margin with Laurentia until the Late Triassic ~216 Ma, which preceded the inception of a Colombian marginal seaway during the break-up of western Pangaea. Furthermore, the presence of Ordovician metamorphic rocks in the SNSM Massif confirms the extent of a Famatinian arc along NW-Gondwana during the Early Palaeozoic.
DOI: 10.6084/m9.figshare.16443929.v1
title: Neoproterozoic to Jurassic tectono-metamorphic events in the Sierra Nevada de Santa Marta Massif, Colombia: insights from zircon U-Pb geochronology and trace element geochemistry

description: The Sierra Nevada de Santa Marta Massif (SNSM) in the Northern Andes affords an insight into lower crustal section structural relations. This polymetamorphic basement comprises high-grade gneisses, which alternate with imbricate slivers of medium-to high-grade schists. New field observations coupled with LA-ICP-MS U-Pb zircon geochronology and trace element geochemistry reveal some hallmarks on the evolution of this strongly remobilized crustal section. The Proterozoic Rodinia-type basement (1100 − 880 Ma) recorded at least two separated tectono-metamorphic events (M<sub>0</sub> and M<sub>1</sub>) and was subsequently affected by a magmatic episode during the Ordovician (<b>~</b>450 Ma; M<sub>2</sub>). During the Permian, subduction of Panthalassian oceanic crust beneath Pangaea led to the installation of a magmatic-arc and probably coeval metamorphism (<b>~</b>288-266 Ma; M<sub>3</sub>). Middle-Late Triassic roll-back extension of the upper plate led to anatexis and metamorphism (M<sub>4</sub>) reaching peak conditions at ca. 239 Ma with concurrent crystallization of garnet and sillimanite, followed by a decreasing geothermal gradient at ca. 202 Ma. Early Jurassic arc build-up under a rejuvenated convergence was contemporaneous to metamorphism on an accretionary wedge (M<sub>5</sub>) at ca. 185 Ma. The SNSM Massif basement units yield metamorphic ages that compare to similar tectono-metamorphic provinces in NW-Gondwana, including the Central Cordillera of Colombia, the Guajira Peninsula, the Mérida Andes, the Perijá Range, the Santander Massif, and the Central American and Mexican terranes to the south of the Ouachita-Marathon Suture (Oaxaquia, Mixteca, and Maya blocks). Age equivalence of these events is best explained by the existence of a conjugate margin with Laurentia until the Late Triassic ~216 Ma, which preceded the inception of a Colombian marginal seaway during the break-up of western Pangaea. Furthermore, the presence of Ordovician metamorphic rocks in the SNSM Massif confirms the extent of a Famatinian arc along NW-Gondwana during the Early Palaeozoic.
DOI: 10.6084/m9.figshare.16574274
title: Late Paleozoic multi-stage subduction accretion of the southwestern Central Asian Orogenic Belt: insights from the Late Carboniferous-Early Permian granites in the southern West Junggar, NW China

description: The Late Carboniferous to Early Permian tectonic evolution of the South West Junggar (SWJ), northwest China, a crucial constituent in the southwestern domain of the Central Asian Orogenic Belt (CAOB), has long been the subject of debate. Here, detailed petrographic studies, new nine LA-ICP-MS zircon U-Pb ages and forty-nine whole-rock geochemical results from six granitic plutons in the SWJ were combined with previously available data to elucidate their petrogenesis and re-decipher Late Palaeozoic tectonic evolution and accretionary process of the southwestern CAOB. The studied granites can be geochemically classified as I- and A-type granites, and the former is further subdivided into I-type and highly fractionated I-type granites. The calc-alkaline I-type amphibole-bearing granites (Group I) yield crystallization ages of ca. 317–315 Ma, and exhibit depletions in HFSEs and enrichments in LILEs with no to slight Eu anomalies and low zircon saturation temperatures, indicating that the formation of these granites may be closely related to the subduction of the Junggar oceanic slab. The Group II granite porphyries (ca. 312 Ma) contain negligible amphibole, and are characterized by evolved SiO<sub>2</sub> but low zircon saturation temperatures with sharply negative Eu, Ba, Nb, Ta, Sr, P and Ti anomalies, belonging to highly fractionated I-type granites, and were probably produced in a tectonic transition from compressional to extensional setting. In contrast, the latest Carboniferous (ca. 304–298 Ma) alkaline A-type granites (Group III) are amphibole-absent, and are similar to Group II granites in major element compositions, but exhibit higher zircon saturation temperatures, indicating that they probably resulted in a back-arc extensional setting triggered by roll-back of the subducting Junggar oceanic slab since ca. 310 Ma. In combination with regional geology and re-interpretation of previous data, a multi-stage subduction-accretion model is suggested to account for the Late Palaeozoic tectonic evolution of the southwestern CAOB. This model can plausibly interpret the differences in duration of subduction between the northern and southern domains of West Junggar and the coexistence of A-type granites with subduction-related sanukites in the SWJ during Carboniferous to Permian.
DOI: 10.6084/m9.figshare.16574274.v2
title: Late Paleozoic multi-stage subduction accretion of the southwestern Central Asian Orogenic Belt: insights from the Late Carboniferous-Early Permian granites in the southern West Junggar, NW China

description: The Late Carboniferous to Early Permian tectonic evolution of the South West Junggar (SWJ), northwest China, a crucial constituent in the southwestern domain of the Central Asian Orogenic Belt (CAOB), has long been the subject of debate. Here, detailed petrographic studies, new nine LA-ICP-MS zircon U-Pb ages and forty-nine whole-rock geochemical results from six granitic plutons in the SWJ were combined with previously available data to elucidate their petrogenesis and re-decipher Late Palaeozoic tectonic evolution and accretionary process of the southwestern CAOB. The studied granites can be geochemically classified as I- and A-type granites, and the former is further subdivided into I-type and highly fractionated I-type granites. The calc-alkaline I-type amphibole-bearing granites (Group I) yield crystallization ages of ca. 317–315 Ma, and exhibit depletions in HFSEs and enrichments in LILEs with no to slight Eu anomalies and low zircon saturation temperatures, indicating that the formation of these granites may be closely related to the subduction of the Junggar oceanic slab. The Group II granite porphyries (ca. 312 Ma) contain negligible amphibole, and are characterized by evolved SiO<sub>2</sub> but low zircon saturation temperatures with sharply negative Eu, Ba, Nb, Ta, Sr, P and Ti anomalies, belonging to highly fractionated I-type granites, and were probably produced in a tectonic transition from compressional to extensional setting. In contrast, the latest Carboniferous (ca. 304–298 Ma) alkaline A-type granites (Group III) are amphibole-absent, and are similar to Group II granites in major element compositions, but exhibit higher zircon saturation temperatures, indicating that they probably resulted in a back-arc extensional setting triggered by roll-back of the subducting Junggar oceanic slab since ca. 310 Ma. In combination with regional geology and re-interpretation of previous data, a multi-stage subduction-accretion model is suggested to account for the Late Palaeozoic tectonic evolution of the southwestern CAOB. This model can plausibly interpret the differences in duration of subduction between the northern and southern domains of West Junggar and the coexistence of A-type granites with subduction-related sanukites in the SWJ during Carboniferous to Permian.