cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.24400/802406/87m7-8pf9
title: Cluster PEACE Summary Parameters

description: This data set contains the Cluster PEACE Summary Parameters (one minute average). The parameters are the electron density, velocity, temperature and heat flux (derived from a subset of the moment sums calculated onboard) and instrument status. Caveats At the time of writing (March 2002) the moments data provided to CSDS are being derived only from HEEA. Thus the minimum measured electron energy is typically about 34 eV opposed to 10 eV when LEEA is included. This approach is an initial response to the frequently occurring situation that the spacecraft potential does rise above 10 volts. The spacecraft potential is at times above 34 volts, in which case the moments calculations will be include measurements of both plasma and spacecraft electrons and will not accurately describe the plasma population. These cases can usually be recognised as they have particularly high density. The spacecraft potential, when uncontrolled by ASPOC, can often reach such values, particularly in thinner plasmas (e.g., magnetotail lobes, polar cap, etc.) The CSDS Quicklook plots show spacecraft potential from EFW which will further inform the interested reader about which regions characteristically have high spacecraft potential. ASPOC operations do not occur on Spacecraft 1 at all. On about 50% of the orbits there are no ASPOC operations on the other spacecraft, and operations are typically for less than 10 hours at a time when ASPOC is in use. The PEACE Team are reconsidering their approach to provision of and validation of electron moments data to the CSDS, in the light of the problems with spacecraft potential. The PEACE team will report on the outcome in a future update of this document. Please for further relevant information consult the PEACE home page (https://www.mssl.ucl.ac.uk/www_plasma/missions/cluster/).
DOI: 10.24400/802406/hpfy-mg9h
title: Cluster FGM Summary Parameters

description: This data set contains the Cluster FGM Summary Parameters (spin averaged). The parameters are a status word, the three averaged components of the magnetic field vector in the GSE coordinate system and 2 variances.
DOI: 10.24400/802406/gbts-gmsp
title: Summary parameters

description: This data set contains Cluster reference spacecraft (3) ephemeris.
DOI: 10.24400/802406/aac4-4xr7
title: Cluster EFW Summary Parameters

description: This data set contains the Cluster EFW Summary Parameters (one minute averaged). The parameters are two status parameters and six data parameters. Caveats The CSDS data are intended for event identification and are not for publication. Some obviously incorrect data have been removed in the validation process, but there may still be occasional data with poor quality in the PPDB and SPDB. Please always contact the EFW PI or the CSDS file validator (information given in the global attributes of each CDF file) for questions on data validity. The electric field E_dusk has not been corrected for offsets present due to, e.g., photoelectron asymmetries. The parameter U_probe_sc can be used as an approximate indicator of the electron density, except during periods when ASPOC is operating. Such periods have not been removed from the data. A more (less) negative value of U_probe_sc indicates lower (higher) density. The operation of WHISPER in the active mode sometimes disturbs the EFW measurements. Such disturbed data have most likely been removed in all quantities except U_probe_sc, where the disturbance is least severe.
DOI: 10.24400/802406/cde6-dnjf
title: Cluster EDI Summary Parameters

description: This data set contains the Cluster EDI Summary Parameters. Those parameters are the 3 components of the electron drift velocity and (cartesian components, GSE coordinates, corrected for spacecraft motion) and the instrument status.
DOI: 10.24400/802406/r47r-q08q
title: Cluster DWP Summary Parameters

description: This data set contains Cluster Digital Wave Processor (DWP) summary parameters (various instrument status and data status flags as well as particle correlator information).
DOI: 10.24400/802406/m5p5-c1mt
title: Cluster ASPOC Summary Parameters

description: This data set contains Cluster ASPOC (Active Spacecraft Potential Control experiment) Summary Parameters (Ion current and instrument status).
DOI: 10.5281/zenodo.6323310
title: Supplementary data to the Baseline Methodological User Needs Analysis

description: Supplementary data to the Baseline Methodological User Needs Analysis
DOI: 10.5281/zenodo.6323102
title: Salt-affected soils in Argentina

description: Maps of pH on water, electrical conductivity (dS/m), exchangeable sodium percent (%) and soils affected by salts in Argentina at different depth intervals (0-30 and 30-100 cm) at 1000 m resolution. Including the tree standard layers and error estimation using random forest. Global accuracy based on cross-validation. <strong>sp</strong> <strong>RMSE</strong> <strong>Rsquared</strong> <strong>EC (dS/m) 0-30 cm</strong> <strong>5.53</strong> <strong>0.134</strong> <strong>EC (dS/m) 30-100 cm</strong> <strong>5.77</strong> <strong>0.208</strong> <strong>pH on water 0-30 cm</strong> <strong>0.84</strong> <strong>0.456</strong> <strong>pH on water 30-100 cm</strong> <strong>0.80</strong> <strong>0.523</strong> <strong>Exchangeable sodium percent (%) 0-30 cm</strong> <strong>13.08</strong> <strong>0.169</strong> <strong>Exchangeable sodium percent (%) 30-100 cm</strong> <strong>15.40</strong> <strong>0.187</strong>
description: Rodríguez DM; Schulz GA; Tenti Vuegen LM; Angelini ME; Olmedo GF; Lavado RS. (2021) Salt-affected soils in Argentina. In: Global Soil Salinity Map - GSS map. FAO. https://www.fao.org/global-soil-partnership/gsasmap/en
DOI: 10.5281/zenodo.6323101
title: Salt-affected soils in Argentina

description: Maps of pH on water, electrical conductivity (dS/m), exchangeable sodium percent (%) and soils affected by salts in Argentina at different depth intervals (0-30 and 30-100 cm) at 1000 m resolution. Including the tree standard layers and error estimation using random forest. Global accuracy based on cross-validation. <strong>sp</strong> <strong>RMSE</strong> <strong>Rsquared</strong> <strong>EC (dS/m) 0-30 cm</strong> <strong>5.53</strong> <strong>0.134</strong> <strong>EC (dS/m) 30-100 cm</strong> <strong>5.77</strong> <strong>0.208</strong> <strong>pH on water 0-30 cm</strong> <strong>0.84</strong> <strong>0.456</strong> <strong>pH on water 30-100 cm</strong> <strong>0.80</strong> <strong>0.523</strong> <strong>Exchangeable sodium percent (%) 0-30 cm</strong> <strong>13.08</strong> <strong>0.169</strong> <strong>Exchangeable sodium percent (%) 30-100 cm</strong> <strong>15.40</strong> <strong>0.187</strong>
description: Rodríguez DM; Schulz GA; Tenti Vuegen LM; Angelini ME; Olmedo GF; Lavado RS. (2021) Salt-affected soils in Argentina. In: Global Soil Salinity Map - GSS map. FAO. https://www.fao.org/global-soil-partnership/gsasmap/en
DOI: 10.5281/zenodo.6323195
title: The Packet Number Space Debate in Multipath QUIC: Artifacts

description: The measurement data and a Jupyter notebook to reproduce the graphs in the paper.
DOI: 10.5281/zenodo.6323194
title: The Packet Number Space Debate in Multipath QUIC: Artifacts

description: The measurement data and a Jupyter notebook to reproduce the graphs in the paper.
DOI: 10.25345/c5959c89x
title: MassIVE MSV000088970 - Qtof_DDA_POS_RAW_CS_metabolomics_annotation
title: Qtof_DDA_POS_RAW_CS_metabolomics_annotation evaluation dataset
DOI: 10.5517/ccdc.csd.cc2b6tm0
title: CCDC 2151512: Experimental Crystal Structure Determination

description: Related Article: D. Schollmeyer, H. Detert|2022|IUCrData|7|x220169|doi:10.1107/S2414314622001699
DOI: 10.25747/4a1a-cj80
title: Electricity transmission system (2050) according to the Active Economy scenario from Portugal – ATTEST project
DOI: 10.5281/zenodo.5499727
title: Food web rewiring drives long-term compositional differences and late-disturbance interactions at the community level

description: <strong>Abstract</strong> Ecological communities are constantly exposed to multiple natural and anthropogenic stressors. Multivariate composition (if recovered) has been found to need significantly more time to be regained after pulsed stress compared to univariate diversity metrics and functional endpoints. However, the mechanisms driving the different recovery times of communities to single and multiple stressors remain unexplored. Here, we apply for the first time quantitative ecological network analyses to try to elucidate the mechanisms driving long-term community composition dissimilarity and late-stage stressor interactions at the community level. For this, we evaluate the effects of three stressors (two pesticides and nutrients) and their interactions in outdoor mesocosms containing a complex freshwater community. We found interactions strength reorganisation to be strongly related to compositional changes and identified post-disturbance interaction strength rewiring to be responsible for most of the observed compositional changes. Additionally, we found stressor interactions to be significant in the long term only when both interactions strength and food web architecture are reshaped by the stressors. We suggest that quantitative network analysis has the potential to unveil ecological processes that prevent long-term community recovery. <strong>Methods</strong> The dataset used in this study comes from an outdoor mesocosm experiment performed between April and July of 2019 at the facilities of the IMDEA Water Institute (Alcalá de Henares, Spain). A full factorial design was used with eight different treatments applied in a randomized fashion and three replicates per treatment. The treatments included: the insecticide chlorpyrifos (1 µg/L and absent), the herbicide diuron (18 µg/L and absent), nutrients (750 µg/L of N and 75 µg/L of P, not added), and their binary and tertiary interactions. The nutrients treatment started one month before the application of the pesticides. Since then, P and P were applied twice a week for the whole duration of the experiment. The freshwater community tested in the experiment was composed of phytoplankton, zooplankton, and macroinvertebrates, which were sampled one time before and several times after the pesticide application. However, for the purpose of this study, we focus on days -5 (initial condition), 15 (expected maximum effect) and 50 (expected recovery) relative to the pesticides’ application. Please see the "readme" sheet in the datafile for a description of the file structure and treatments abreviations.
DOI: 10.14272/nvqfhmagcydrgo-byyhnaklsa-n/chmo0000613
title: pulsed nuclear magnetic resonance spectroscopy (NMR) ()
title: InChI=1S/C26H18N2O4/c29-25(30)19-10-6-17(7-11-19)21-14-15-23(18-8-12-20(13-9-18)26(31)32)24(16-21)28-27-22-4-2-1-3-5-22/h1-16H,(H,29,30)(H,31,32)/b28-27+

description: dataset for pulsed nuclear magnetic resonance spectroscopy (NMR)
DOI: 10.34740/kaggle/dsv/3247055
title: Mahanagar Yatayat Dataset
DOI: 10.14272/nvqfhmagcydrgo-byyhnaklsa-n.1
title: C26H18N2O4
title: InChI=1S/C26H18N2O4/c29-25(30)19-10-6-17(7-11-19)21-14-15-23(18-8-12-20(13-9-18)26(31)32)24(16-21)28-27-22-4-2-1-3-5-22/h1-16H,(H,29,30)(H,31,32)/b28-27+

description: This dataset contains experimental data from a sample (InChI=1S/C26H18N2O4/c29-25(30)19-10-6-17(7-11-19)21-14-15-23(18-8-12-20(13-9-18)26(31)32)24(16-21)28-27-22-4-2-1-3-5-22/h1-16H,(H,29,30)(H,31,32)/b28-27+). The datasets from the following experiments are available: 1H NMR 13C NMR IR EA Mass Others NMR
DOI: 10.6084/m9.figshare.13622063
title: Trondhjemite leucosomes generated by partial melting of a hornblende-gabbro (Alvand plutonic complex, Hamedan, NW Iran)

description: This work describes the petrogenesis of <i>in situ</i> and in-source trondhjemite leucosomes generated by low-degree partial melting of the Jurassic Cheshmeh-Ghasaban hornblende-gabbros in the northern Alvand batholith (Hamedan, NW Iran). These leucosomes occur in a metatexite migmatite as patches, net-structures, veinlets, and dikes at scales ranging from a few millimetres to a few metres. They have high SiO<sub>2</sub> (mean ≈ 78 wt%) and Na<sub>2</sub>O (4–5 wt%) with low Al<sub>2</sub>O<sub>3</sub> (&lt;15 wt%), K<sub>2</sub>O (&lt;1.5 wt%), Sr (33–267 ppm), Eu (0.31–0.62 ppm) and heavy REE (&lt;4 ppm) contents similar to typical low-Al<sub>2</sub>O<sub>3</sub> trondhjemites. Batch-melting models indicate these leucosomes are the result of ≈1-2% partial melting of the hornblende-gabbro, whereas thermobarometric modelling constrains their petrogenesis in the field of hornblende hornfels-facies metamorphism (pressure ≈3.0–4.5 kbar and temperature ≈700-750°C). On a wider scale, our results document natural trondhjemites generated in the upper crust by amphibole-dehydration melting of a mafic source at temperature conditions close to the solidus, filling the existing gap of data in low-pressure (P
DOI: 10.6084/m9.figshare.14132128
title: Paleocene to Miocene migmatization and kinematics of the deformation at the northern boundary of the Xolapa Complex: implications for the Chortís Block-southern Mexico connection

description: The Xolapa Complex of southern Mexico preserves evidence of its connection with the Chortís Block of Central America. Orthogneisses yielded U-Pb protolith ages from 172 to 169 Ma and paramigmatites are dated at 217 Ma. El Salitre and the Amatlán granitoids show crystallization ages of 65 and 59–57 Ma, respectively. In central Xolapa, diatexites have ages from 38 to 31 Ma, and granites were dated from 30 to 29 Ma. In the southeastern Xolapa, crystallization ages of 45 Ma and 23 to 21 Ma were obtained from migmatites and anatectic granites, respectively. Previous data indicate three diachronous stages of crustal melting along the Xolapa block. Structural data reveal that the Xolapa Complex is tectonically juxtaposed against the Acatlán Complex through ductile zones. Two mylonitic foliations are predominant in the northern boundary of the Xolapa Complex: (i) a sub-vertical NW-SE foliation with subhorizontal or low-plunging stretching lineation and left-lateral kinematics; and (ii) a subhorizontal NE-SW foliation with normal plunging stretching lineation and top-to-NE kinematics. The first mylonitic event related to the sinistral eastward motion of the Chortís Block occurred between 58 and 54–50 Ma. The second event took place in central Xolapa after or synchronous with the 38–31 Ma emplacement of diatexites. This event is related to an extensional phase that uplifts the Xolapa Complex with concerning the Acatlán Complex. In the southeastern region, deformation occurred after or synchronous with the emplacement of anatectic granites dated at 23–22 Ma. Our geochronological and structural data delineated an eastward decreasing age trend of migmatization, whereas the mylonitic deformation reported through the Xolapa Complex is consistent with a diachronous migration and detachment of the Chortís Block relative to the Acatlán Complex from Paleocene to early Miocene times.
DOI: 10.6084/m9.figshare.14132128.v1
title: Paleocene to Miocene migmatization and kinematics of the deformation at the northern boundary of the Xolapa Complex: implications for the Chortís Block-southern Mexico connection

description: The Xolapa Complex of southern Mexico preserves evidence of its connection with the Chortís Block of Central America. Orthogneisses yielded U-Pb protolith ages from 172 to 169 Ma and paramigmatites are dated at 217 Ma. El Salitre and the Amatlán granitoids show crystallization ages of 65 and 59–57 Ma, respectively. In central Xolapa, diatexites have ages from 38 to 31 Ma, and granites were dated from 30 to 29 Ma. In the southeastern Xolapa, crystallization ages of 45 Ma and 23 to 21 Ma were obtained from migmatites and anatectic granites, respectively. Previous data indicate three diachronous stages of crustal melting along the Xolapa block. Structural data reveal that the Xolapa Complex is tectonically juxtaposed against the Acatlán Complex through ductile zones. Two mylonitic foliations are predominant in the northern boundary of the Xolapa Complex: (i) a sub-vertical NW-SE foliation with subhorizontal or low-plunging stretching lineation and left-lateral kinematics; and (ii) a subhorizontal NE-SW foliation with normal plunging stretching lineation and top-to-NE kinematics. The first mylonitic event related to the sinistral eastward motion of the Chortís Block occurred between 58 and 54–50 Ma. The second event took place in central Xolapa after or synchronous with the 38–31 Ma emplacement of diatexites. This event is related to an extensional phase that uplifts the Xolapa Complex with concerning the Acatlán Complex. In the southeastern region, deformation occurred after or synchronous with the emplacement of anatectic granites dated at 23–22 Ma. Our geochronological and structural data delineated an eastward decreasing age trend of migmatization, whereas the mylonitic deformation reported through the Xolapa Complex is consistent with a diachronous migration and detachment of the Chortís Block relative to the Acatlán Complex from Paleocene to early Miocene times.
DOI: 10.6084/m9.figshare.13607036
title: Late Cretaceous to Oligocene overlapping plutonic magmatism episodes in the eastern Mesa Central province of Mexico

description: Several plutonic bodies are distributed along the northern and eastern margins of the Mesa Central province, intruding mainly clastic and carbonate sedimentary sequences from the Triassic and Cretaceous. In this work, U-Pb ages in zircon and apatite have been obtained using the LA-ICPMS technique in samples from six of these plutons and some possibly related volcanic rocks. In general, intrusive rocks are porphyritic, suggesting a relatively shallow intrusion and are mostly monzogranite to quartz-monzodiorite in composition, displaying biotite and amphibole. According to the geochronological results, the plutonic rocks can be divided into two groups; a group that varies in age from Campanian-Maastrichtian limit up to Paleocene, and a second group that essentially corresponds to the Oligocene, specifically the Rupelian. Unfortunately, the geochronological data on apatites were not conclusive to establish a trajectory or cooling rate and the ages obtained in this mineral phase for several of these bodies are very similar to the age of zircons, which suggests a relatively rapid cooling, very probably associated with shallow depths of emplacement. The statistical analysis of obtained and published ages suggests two periods of significant magmatic activity that occurred essentially during the Late Cretaceous (Campanian) and during the late Eocene (Bartonian and Priabonian). Notably, the plutonic bodies, particularly those of the group of ancient granites (Paleocene-Late Cretaceous) are very far from the ancient subduction zone to which they have been associated, in addition to being spatially close to plutonic rocks of the Eocene and Oligocene. In this sense, the traditional model of magmatic migration originated by the flat subduction of the Farallon plate is not very consistent, so it will be necessary to evaluate or reconsider the geodynamic evolution associated with magmatism for this region, in view to these new data and to those that could be generated later.
DOI: 10.6084/m9.figshare.13607036.v1
title: Late Cretaceous to Oligocene overlapping plutonic magmatism episodes in the eastern Mesa Central province of Mexico

description: Several plutonic bodies are distributed along the northern and eastern margins of the Mesa Central province, intruding mainly clastic and carbonate sedimentary sequences from the Triassic and Cretaceous. In this work, U-Pb ages in zircon and apatite have been obtained using the LA-ICPMS technique in samples from six of these plutons and some possibly related volcanic rocks. In general, intrusive rocks are porphyritic, suggesting a relatively shallow intrusion and are mostly monzogranite to quartz-monzodiorite in composition, displaying biotite and amphibole. According to the geochronological results, the plutonic rocks can be divided into two groups; a group that varies in age from Campanian-Maastrichtian limit up to Paleocene, and a second group that essentially corresponds to the Oligocene, specifically the Rupelian. Unfortunately, the geochronological data on apatites were not conclusive to establish a trajectory or cooling rate and the ages obtained in this mineral phase for several of these bodies are very similar to the age of zircons, which suggests a relatively rapid cooling, very probably associated with shallow depths of emplacement. The statistical analysis of obtained and published ages suggests two periods of significant magmatic activity that occurred essentially during the Late Cretaceous (Campanian) and during the late Eocene (Bartonian and Priabonian). Notably, the plutonic bodies, particularly those of the group of ancient granites (Paleocene-Late Cretaceous) are very far from the ancient subduction zone to which they have been associated, in addition to being spatially close to plutonic rocks of the Eocene and Oligocene. In this sense, the traditional model of magmatic migration originated by the flat subduction of the Farallon plate is not very consistent, so it will be necessary to evaluate or reconsider the geodynamic evolution associated with magmatism for this region, in view to these new data and to those that could be generated later.
DOI: 10.6084/m9.figshare.13622063.v1
title: Trondhjemite leucosomes generated by partial melting of a hornblende-gabbro (Alvand plutonic complex, Hamedan, NW Iran)

description: This work describes the petrogenesis of <i>in situ</i> and in-source trondhjemite leucosomes generated by low-degree partial melting of the Jurassic Cheshmeh-Ghasaban hornblende-gabbros in the northern Alvand batholith (Hamedan, NW Iran). These leucosomes occur in a metatexite migmatite as patches, net-structures, veinlets, and dikes at scales ranging from a few millimetres to a few metres. They have high SiO<sub>2</sub> (mean ≈ 78 wt%) and Na<sub>2</sub>O (4–5 wt%) with low Al<sub>2</sub>O<sub>3</sub> (&lt;15 wt%), K<sub>2</sub>O (&lt;1.5 wt%), Sr (33–267 ppm), Eu (0.31–0.62 ppm) and heavy REE (&lt;4 ppm) contents similar to typical low-Al<sub>2</sub>O<sub>3</sub> trondhjemites. Batch-melting models indicate these leucosomes are the result of ≈1-2% partial melting of the hornblende-gabbro, whereas thermobarometric modelling constrains their petrogenesis in the field of hornblende hornfels-facies metamorphism (pressure ≈3.0–4.5 kbar and temperature ≈700-750°C). On a wider scale, our results document natural trondhjemites generated in the upper crust by amphibole-dehydration melting of a mafic source at temperature conditions close to the solidus, filling the existing gap of data in low-pressure (P