cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.48370/ofd/ck9u2s
title: Cerylon histeroides (Fabricius, 1792), C-513

description: Coleoptera collection
DOI: 10.5281/zenodo.6358568
title: RNASeq data of isolated murine glomeruli treated with Vitamin D3 and DMSO

description: RNASeq data of isolated murine glomeruli (as described here 10.1111/bph.13667) treated with Vitamin D3 (100 nM) and DMSO (0.1%) for 6 days.
description: {"references": ["doi: 10.1111/bph.13667"]}
DOI: 10.5281/zenodo.6358567
title: RNASeq data of isolated murine glomeruli treated with Vitamin D3 and DMSO

description: RNASeq data of isolated murine glomeruli (as described here 10.1111/bph.13667) treated with Vitamin D3 (100 nM) and DMSO (0.1%) for 6 days.
description: {"references": ["doi: 10.1111/bph.13667"]}
DOI: 10.48370/ofd/bx5gkd/1vfpsj
title: Cerylon ferrugineum.tif

description: :unav
DOI: 10.48370/ofd/bx5gkd
title: Cerylon ferrugineum (Stephens, 1830), C-514

description: Coleoptera collection
DOI: 10.5519/qd.15webv5e
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (1 records)
DOI: 10.6084/m9.figshare.19137074
title: Supplementary Material for: Left Ventricular Wall Reconstruction with Autologous Vascularized Gastric Graft in a Porcine Pilot Model

description: Introduction: Surgical replacement of dysfunctional cardiac muscle with regenerative tissue is an important option to combat heart failure. But current available myocardial prostheses like a Dacron or a pericardium patch neither have a regenerative capacity nor do they actively contribute to the heart`s pump function. This study aimed to show the feasibility of utilizing a vascularized stomach patch for transmural left ventricular wall reconstruction. Methods: A left ventricular transmural myocardial defect was reconstructed by performing transdiaphragmatic autologous transplantation of a vascularized stomach segment in six Lewe minipigs. Three further animals received a conventional Dacron patch as a control treatment. The first three animals were followed up for 3 months until planned euthanasia, whereas the observation period for the remaining three animals was scheduled 6 months following surgery. Functional assessment of the grafts was carried out via cardiac magnetic resonance tomography (MRI) and angiography. Physiological remodeling was evaluated histologically and immunohistochemically after heart explanation. Results: Five out of six test animals and all control animals survived the complex surgery and completed the follow-up without clinical complications. One animal died intraoperatively due to excessive bleeding. No animal experienced a rupture of the stomach graft. Functional integration of the heterotopically transplanted stomach into the surrounding myocardium was observed. Angiography showed the development of connections between the gastric graft vasculature and the coronary system of the host cardiac tissue. Conclusions: The clinical results and the observed physiological integration of gastric grafts into the cardiac structure demonstrate the feasibility of vascularized stomach tissue as a myocardial prosthesis. The physiological remodeling indicates a regenerative potential of the graft. Above all, the connection of the gastric vessels with the coronary system constitutes a rationale for the use of vascularized and therefore viable stomach tissue for versatile tissue engineering applications.
DOI: 10.6084/m9.figshare.19367222.v1
title: Primary data from Detection and estimation of <i>Mastigimas anjosi</i> (Hemiptera: Calophyidae) populations on <i>Cedrela fissilis</i> trees

description: <i>Mastigimas anjosi</i> is an important pest of <i>Cedrela fissilis</i> in the southeastern and southern regions of Brazil. The objective of the present study was to investigate the effect of the temperature, relative humidity, rainfall and natural enemies on the flight activity of adults and the movement of <i>M. anjosi</i> nymphs, with two sampling methods, yellow sticky traps and direct collections on the leaves of <i>C. fissilis</i> trees. The sex ratio of this pest was also assessed. The number of <i>M. anjosi</i> individuals was negatively correlated with the minimum and maximum temperatures, with a population peak in late May and early June 2017. The numbers of individuals of this psyllid was positively correlated with the relative humidity and rainfall. Larvae and adults of <i>Cycloneda sanguinea</i>, <i>Hippodamia convergens</i> adults and <i>Atopozelus opsimus</i> nymphs and adults preyed upon <i>M. anjosi</i> adults and nymphs on <i>C. fissilis</i> leaves in the field. <i>Mastigimas anjosi</i> sex ratio was 0.46. Information about sampling methods of <i>M. anjosi</i> and its natural enemies is presented and can contribute to the integrated management of this pest in the field.
DOI: 10.6084/m9.figshare.19367222
title: Primary data from Detection and estimation of <i>Mastigimas anjosi</i> (Hemiptera: Calophyidae) populations on <i>Cedrela fissilis</i> trees

description: <i>Mastigimas anjosi</i> is an important pest of <i>Cedrela fissilis</i> in the southeastern and southern regions of Brazil. The objective of the present study was to investigate the effect of the temperature, relative humidity, rainfall and natural enemies on the flight activity of adults and the movement of <i>M. anjosi</i> nymphs, with two sampling methods, yellow sticky traps and direct collections on the leaves of <i>C. fissilis</i> trees. The sex ratio of this pest was also assessed. The number of <i>M. anjosi</i> individuals was negatively correlated with the minimum and maximum temperatures, with a population peak in late May and early June 2017. The numbers of individuals of this psyllid was positively correlated with the relative humidity and rainfall. Larvae and adults of <i>Cycloneda sanguinea</i>, <i>Hippodamia convergens</i> adults and <i>Atopozelus opsimus</i> nymphs and adults preyed upon <i>M. anjosi</i> adults and nymphs on <i>C. fissilis</i> leaves in the field. <i>Mastigimas anjosi</i> sex ratio was 0.46. Information about sampling methods of <i>M. anjosi</i> and its natural enemies is presented and can contribute to the integrated management of this pest in the field.
DOI: 10.6084/m9.figshare.14256333.v1
title: The Late Cretaceous magmatic arc of the south Aegean: Geodynamic implications from petrological and geochemical studies of granitoids from Anafi island (Cyclades – Greece)

description: In the Aegean region (Cyclades – Greece), a large part of the Island of Anafi consists of exhumed high-grade metamorphic sequences (amphibolites, serpentinites and metasediments) that have been intruded by Late Cretaceous intermediate and felsic granitoids. These correspond to I-type arc-related rocks, displaying calc-alkaline geochemical affinities. Variability in their petrographic features, mineral composition and geochemistry is assigned to differentiation processes that mostly involved plagioclase and/or K-feldspar, and to a lesser extent amphibole and biotite. Mineral chemistry and geochemical results suggest that the Anafi granitoids are highly comparable with the Late Cretaceous granitoid intrusive rocks from East Crete and Donousa island. The amphibole and zircon saturation thermometry yields relatively moderate temperature crystallization conditions (~790°C) for the intermediate granitoids and lower for the felsic granitoids (~630°C). Geobarometric calculations based upon the chemistry of magnesiohornblende, as well as the normative (Qz), (Ab) and (Or) contents clearly point to shallow intrusion conditions (~2.0–6.5 kbar), corresponding to an estimated depth of crystallization of ~12 ± 4 km. The thrust sheets that overly the Palaeogene flysch in Anafi (metasediments with serpentinized peridotites, amphibolites and metabasites), constitute a subducted and metamorphosed oceanic sequence. These metamorphic units likely represent a part of the Pindos – Cycladic Blueschist Unit domain that was subducted at an earlier pre-Campanian stage. In the hydrated mantle wedge, incorporation of shallow level granitoids within metamorphic units was likely facilitated via corner flow intrusion mechanisms. Following the intrusion, the granitoid rocks were exhumed in a syn-convergent setting, along with the metamorphic thrust sheets, by continuous underplating of more external units, thus, escaping penetrative ductile deformation.
DOI: 10.6084/m9.figshare.14140952
title: The Marifil Volcanic Complex at Sierra de Pailemán: implications for the Early Jurassic magmatic evolution of the Eastern North Patagonian Region

description: The Sinemurian Marifil Volcanic Complex at Sierra de Pailemán, located in the east part of the North Patagonian Region, Argentina, includes five lithofacies and three volcanic events. The volcanic activity begins with subaerial pyroclastic-fall deposits, massive lapilli tuffs with eutaxitic textures, and subaerial silicic domes’ emplacement. The upper part of the sequence is formed by pyroclastic fall deposits that pass to massive lapilli tuffs and rhyolitic lava flows. These lithofacies indicate the collapse of explosive eruption columns, coeval with small silicic domes’ emplacement, and lava-flows’ eruption. The volcanic episode at Sierra de Pailemán was generated during continuous magmatic activity because no erosional or unconformity surfaces were recognized. The Marifil Volcanic Complex’s age at Sierra de Pailemán is 191.2 ± 1.3 Ma (Sinemurian) and belongs to the V0 phase of volcanism. These rocks are high-K rhyolites, possibly produced by partial melting of the lower crust, promoted by fluids derived from a subducted plate in back-arc settings that change to an intraplate setting. The Lu-Hf isotopes suggest the possibility of magma mixing in the source and recycling or re-melting of a more evolved crust related to subduction zones. The Lower Jurassic magmatic activity in the western North Patagonian Region and the Patagonian Cordillera of Argentina and Chile correspond to continental arcs.
DOI: 10.6084/m9.figshare.14256333
title: The Late Cretaceous magmatic arc of the south Aegean: Geodynamic implications from petrological and geochemical studies of granitoids from Anafi island (Cyclades – Greece)

description: In the Aegean region (Cyclades – Greece), a large part of the Island of Anafi consists of exhumed high-grade metamorphic sequences (amphibolites, serpentinites and metasediments) that have been intruded by Late Cretaceous intermediate and felsic granitoids. These correspond to I-type arc-related rocks, displaying calc-alkaline geochemical affinities. Variability in their petrographic features, mineral composition and geochemistry is assigned to differentiation processes that mostly involved plagioclase and/or K-feldspar, and to a lesser extent amphibole and biotite. Mineral chemistry and geochemical results suggest that the Anafi granitoids are highly comparable with the Late Cretaceous granitoid intrusive rocks from East Crete and Donousa island. The amphibole and zircon saturation thermometry yields relatively moderate temperature crystallization conditions (~790°C) for the intermediate granitoids and lower for the felsic granitoids (~630°C). Geobarometric calculations based upon the chemistry of magnesiohornblende, as well as the normative (Qz), (Ab) and (Or) contents clearly point to shallow intrusion conditions (~2.0–6.5 kbar), corresponding to an estimated depth of crystallization of ~12 ± 4 km. The thrust sheets that overly the Palaeogene flysch in Anafi (metasediments with serpentinized peridotites, amphibolites and metabasites), constitute a subducted and metamorphosed oceanic sequence. These metamorphic units likely represent a part of the Pindos – Cycladic Blueschist Unit domain that was subducted at an earlier pre-Campanian stage. In the hydrated mantle wedge, incorporation of shallow level granitoids within metamorphic units was likely facilitated via corner flow intrusion mechanisms. Following the intrusion, the granitoid rocks were exhumed in a syn-convergent setting, along with the metamorphic thrust sheets, by continuous underplating of more external units, thus, escaping penetrative ductile deformation.
DOI: 10.6084/m9.figshare.14140952.v1
title: The Marifil Volcanic Complex at Sierra de Pailemán: implications for the Early Jurassic magmatic evolution of the Eastern North Patagonian Region

description: The Sinemurian Marifil Volcanic Complex at Sierra de Pailemán, located in the east part of the North Patagonian Region, Argentina, includes five lithofacies and three volcanic events. The volcanic activity begins with subaerial pyroclastic-fall deposits, massive lapilli tuffs with eutaxitic textures, and subaerial silicic domes’ emplacement. The upper part of the sequence is formed by pyroclastic fall deposits that pass to massive lapilli tuffs and rhyolitic lava flows. These lithofacies indicate the collapse of explosive eruption columns, coeval with small silicic domes’ emplacement, and lava-flows’ eruption. The volcanic episode at Sierra de Pailemán was generated during continuous magmatic activity because no erosional or unconformity surfaces were recognized. The Marifil Volcanic Complex’s age at Sierra de Pailemán is 191.2 ± 1.3 Ma (Sinemurian) and belongs to the V0 phase of volcanism. These rocks are high-K rhyolites, possibly produced by partial melting of the lower crust, promoted by fluids derived from a subducted plate in back-arc settings that change to an intraplate setting. The Lu-Hf isotopes suggest the possibility of magma mixing in the source and recycling or re-melting of a more evolved crust related to subduction zones. The Lower Jurassic magmatic activity in the western North Patagonian Region and the Patagonian Cordillera of Argentina and Chile correspond to continental arcs.
DOI: 10.6084/m9.figshare.14060522
title: Triassic magmatism in Northeast China: Implications for spatiotemporal distribution, continental crustal accretion, and geodynamic evolution

description: Triassic magmatism in Northeast (NE) China was geodynamically controlled by the Mongol–Okhotsk Ocean (MOO), Palaeo-Asian Ocean (PAO), and Palaeo-Pacific Ocean (PPO) tectonic regimes. To define the mechanisms of crustal accretion and geodynamics, the magmatic processes generated by ocean closure and plate subduction must be determined. In the present study, we assembled geochronological, geochemical, Cu (Mo)-porphyry deposit, and zircon Hf isotopic data from magmatic rocks throughout NE China. Central-NE China harbours more reworking of juvenile continental crustal material than the NE China margin. The widespread Triassic felsic magmas in NE China are primarily due to the recycling of juvenile and ancient crustal components during the tectonic evolution of the PAO. During the Triassic, NE China was subjected to a syn- to post-collisional orogenic regime accompanied by scissor-like basin closure and bidirectional subduction of the eastern PAO, before transitioning to the PPO tectonic regime in the latest Triassic. Magmatism in the Erguna and the central–northern Xing’an blocks was more affected by the MOO tectonic regime. Magmatism in the central–southern Xing’an Block, the southwestern Songliao Basin, and northern Lesser Xing’an–Zhangguangcai Range was linked to the closure of the PAO. Triassic magmatic rocks along the eastern Songliao Basin are extensional and formed during the opening of the Mudanjiang Ocean. The NE margin of Eurasia was a passive continental margin in the Late Triassic.
DOI: 10.6084/m9.figshare.14060522.v1
title: Triassic magmatism in Northeast China: Implications for spatiotemporal distribution, continental crustal accretion, and geodynamic evolution

description: Triassic magmatism in Northeast (NE) China was geodynamically controlled by the Mongol–Okhotsk Ocean (MOO), Palaeo-Asian Ocean (PAO), and Palaeo-Pacific Ocean (PPO) tectonic regimes. To define the mechanisms of crustal accretion and geodynamics, the magmatic processes generated by ocean closure and plate subduction must be determined. In the present study, we assembled geochronological, geochemical, Cu (Mo)-porphyry deposit, and zircon Hf isotopic data from magmatic rocks throughout NE China. Central-NE China harbours more reworking of juvenile continental crustal material than the NE China margin. The widespread Triassic felsic magmas in NE China are primarily due to the recycling of juvenile and ancient crustal components during the tectonic evolution of the PAO. During the Triassic, NE China was subjected to a syn- to post-collisional orogenic regime accompanied by scissor-like basin closure and bidirectional subduction of the eastern PAO, before transitioning to the PPO tectonic regime in the latest Triassic. Magmatism in the Erguna and the central–northern Xing’an blocks was more affected by the MOO tectonic regime. Magmatism in the central–southern Xing’an Block, the southwestern Songliao Basin, and northern Lesser Xing’an–Zhangguangcai Range was linked to the closure of the PAO. Triassic magmatic rocks along the eastern Songliao Basin are extensional and formed during the opening of the Mudanjiang Ocean. The NE margin of Eurasia was a passive continental margin in the Late Triassic.
DOI: 10.21227/qmm0-vg62
title: Supplementary files 

description: These files are the supplementary files of a manuscript.
DOI: 10.6084/m9.figshare.19367236
title: Additional file 1 of Emotional distress in COVID-19 patients in Maldives

description: Additional file 1.
DOI: 10.6084/m9.figshare.19367236.v1
title: Additional file 1 of Emotional distress in COVID-19 patients in Maldives

description: Additional file 1.
DOI: 10.6084/m9.figshare.19367213.v1
title: Data of Research on Wire Grasping Method Based on Deep Learning

description: Data of Research on Wire Grasping Method Based on Deep Learning
DOI: 10.6084/m9.figshare.19367213
title: Data of Research on Wire Grasping Method Based on Deep Learning

description: Data of Research on Wire Grasping Method Based on Deep Learning
DOI: 10.6084/m9.figshare.19367269
title: Additional file 1 of Decomposing compounds enables reconstruction of interaction fingerprints for structure-based drug screening

description: Additional file 1. Fragment-target binding mode conservation: The file shows for each fragment-target pair thefragment’s InChiKey, the target’s UniProt ID, the minimum TIS, the maximum TIS, and the mean TIS observed in allavailable complexes
DOI: 10.6084/m9.figshare.19367269.v1
title: Additional file 1 of Decomposing compounds enables reconstruction of interaction fingerprints for structure-based drug screening

description: Additional file 1. Fragment-target binding mode conservation: The file shows for each fragment-target pair thefragment’s InChiKey, the target’s UniProt ID, the minimum TIS, the maximum TIS, and the mean TIS observed in allavailable complexes
DOI: 10.6084/m9.figshare.19367272
title: Additional file 2 of Decomposing compounds enables reconstruction of interaction fingerprints for structure-based drug screening

description: Additional file 2. PDB test data set with original and reconstructed fingerprints: The file shows for each compound-target complex in the PDB test dataset: the complex UID (PDB:HETID:CHAIN:POS), the compound’s SMILES, the target’s UniProt ID, the MW of the compound, the origianl interactions fingerprint, the reconstructed interactions fingerprint, and the fragments used for the reconstruction (according to the defined thresholds in the pipeline).
DOI: 10.6084/m9.figshare.19367275
title: Additional file 3 of Decomposing compounds enables reconstruction of interaction fingerprints for structure-based drug screening

description: Additional file 3. ChEMBL data set with reconstructed fingerprints: The file shows for each compound-target complex in our ChEMBL dataset: the compound’s InChiKey, the target’s UniProt ID, and the reconstructed fingerprint.
DOI: 10.6084/m9.figshare.19367272.v1
title: Additional file 2 of Decomposing compounds enables reconstruction of interaction fingerprints for structure-based drug screening

description: Additional file 2. PDB test data set with original and reconstructed fingerprints: The file shows for each compound-target complex in the PDB test dataset: the complex UID (PDB:HETID:CHAIN:POS), the compound’s SMILES, the target’s UniProt ID, the MW of the compound, the origianl interactions fingerprint, the reconstructed interactions fingerprint, and the fragments used for the reconstruction (according to the defined thresholds in the pipeline).
DOI: 10.6084/m9.figshare.19367275.v1
title: Additional file 3 of Decomposing compounds enables reconstruction of interaction fingerprints for structure-based drug screening

description: Additional file 3. ChEMBL data set with reconstructed fingerprints: The file shows for each compound-target complex in our ChEMBL dataset: the compound’s InChiKey, the target’s UniProt ID, and the reconstructed fingerprint.
DOI: 10.25403/upresearchdata.26491711
title: Comparison between the Denver and Leeds laboratory flotation cells by evaluating their performance in the flotation of quartz

description: The purpose of this study was to compare the Denver and Leeds laboratory flotation cells by evaluating their performance in the flotation of quartz of four sizes (−25 μm, +25–45 μm, +45–75 μm, and +75–106 μm). This study was conducted at the Materials Science and Metallurgical Engineering laboratory of the University of Pretoria.
The impeller diameters of the Denver and Leeds cells were measured to be 0.07 m and 0.074 m, respectively. The impeller speeds of the cells were calibrated for identical flotation performance (assessed using quartz recoveries without interfering with the cell design), with the Denver cell set at 1200 rpm and the Leeds cell at 1400 rpm. The reagent regime was kept constant, using 25 g/t Flotigam EDA ether amine as a collector, no frother, and NaOH to modify the pH to 9.5. The air flow rate was kept constant at 2 L/min in each of the 3.5 L cells. Flotation kinetics tests were conducted at the optimal rotation speeds, and the results were similar. Both cells achieved similar quartz recoveries of over 70 % for the three +25 μm fractions, but only 15 % for the −25 μm fraction. An additional collector was required to improve the recovery of the −25 μm fraction significantly. These findings demonstrated the effect of particle size on flotation recovery, and the finer particles requiring more reagent due to their larger surface areas. The performance of these cells was further evaluated using dimensionless numbers and with a chemical tracer. The use of dimensionless numbers, such as Power and Reynolds numbers, allowed for a detailed analysis of the cells' hydrodynamics. Additionally, a chemical tracer (NaOH), was used to assess the mixing efficiency of the impellers. 
The Denver flotation cell exhibited superior performance compared to the Leeds cell. It managed to achieve higher recovery rates while consuming less power. This can be attributed to the effective design of its impeller and stator, which enabled it to overcome the resistance posed by the slurry, allowing it to operate at optimal levels that surpassed the capabilities of the Leeds cells. The performance of the Leeds cell was found to be inferior to that of the Denver cell, and this is attributed to several factors. One of the main reasons is the slightly larger bubble size of 3.5 mm in the Leeds cell, compared to the Denver cell's average of 2.5 mm. Therefore, the surface area available for particle attachment was still low for the Leeds cell, even at higher impeller speeds. Additionally, the power numbers for the Leeds cell were higher, averaging at 1.03 between 1000 iii and 1500 rpm in the presence of solids, while the Denver cell averaged 0.77 under the same conditions. This indicates that the Leeds cell requires more power to create the necessary flow. All this leads to deterioration in particle collection efficiency and an overall reduction in performance.