cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.25036366
title: Basin provenance and its control on mineralisation within the Early Devonian Cobar Basin, western Lachlan Orogen, eastern Australia

description: The Cobar Basin, in central New South Wales, is an Early Devonian extensional basin that formed in the western Lachlan Orogen. The basin was filled with shallow- to deep-water sequences of the Cobar Supergroup and hosts small to large polymetallic deposits. Detrital zircon geochronology and whole-rock geochemical data collected from the Amphitheatre Group of the Cobar Supergroup provide constraints on the history of basin fill and illustrate the dynamic interplay between basin provenance and mineralisation, corresponding to the evolving tectonic regime. Data reveal provenance dissimilarity between the southern and northern parts of the basin. In the south, units of the Amphitheatre Group received abundant detritus from <i>ca</i> 430–410 Ma magmatic rocks situated to the southwest and southeast of the basin. By contrast, the northern successions were predominately sourced from recycled Ordovician basement found to the northwest, north, northeast of the basin, along with contributions associated with the Macquarie Arc. This spatial provenance variation, however, is less significant in the younger formations: the northern and southern sequences both exhibit an increase in older recycled detritus upwards with time. This reflects a progressive modification of basin paleogeography, during the transition from rift phase to sag phase. The rift-phase basin geography is characterised by fault-restricted deposition with predominant sediments derived from local proximal sources. The subsequent sag-phase subsidence exhibits a uniform depositional system with more homogenised basin input. This provenance variation is coeval with the stratigraphically controlled mineralisation features within the Amphitheatre Group successions, implying a provenance influence on mineralisation. Data suggest the different sediment source regions have produced distinct detrital mineral compositions between the major mineral-hosting and mineral-barren formations. The enrichment of some detrital minerals in the mineral-hosting units, such as feldspar, muscovite, Ti-minerals (and carbonate), is suggested to be an important factor for mineralisation in the basin. Detrital zircon geochronology and whole-rock geochemistry illustrate the history of basin fill for the Cobar Basin. Spatial and temporal variation of basin provenance reflects a modification of basin geography, corresponding to the evolving tectonic regimes. The change in basin source regions is one of key controls on the mineralisation within the Cobar Basin.
DOI: 10.6084/m9.figshare.25036366.v1
title: Basin provenance and its control on mineralisation within the Early Devonian Cobar Basin, western Lachlan Orogen, eastern Australia

description: The Cobar Basin, in central New South Wales, is an Early Devonian extensional basin that formed in the western Lachlan Orogen. The basin was filled with shallow- to deep-water sequences of the Cobar Supergroup and hosts small to large polymetallic deposits. Detrital zircon geochronology and whole-rock geochemical data collected from the Amphitheatre Group of the Cobar Supergroup provide constraints on the history of basin fill and illustrate the dynamic interplay between basin provenance and mineralisation, corresponding to the evolving tectonic regime. Data reveal provenance dissimilarity between the southern and northern parts of the basin. In the south, units of the Amphitheatre Group received abundant detritus from <i>ca</i> 430–410 Ma magmatic rocks situated to the southwest and southeast of the basin. By contrast, the northern successions were predominately sourced from recycled Ordovician basement found to the northwest, north, northeast of the basin, along with contributions associated with the Macquarie Arc. This spatial provenance variation, however, is less significant in the younger formations: the northern and southern sequences both exhibit an increase in older recycled detritus upwards with time. This reflects a progressive modification of basin paleogeography, during the transition from rift phase to sag phase. The rift-phase basin geography is characterised by fault-restricted deposition with predominant sediments derived from local proximal sources. The subsequent sag-phase subsidence exhibits a uniform depositional system with more homogenised basin input. This provenance variation is coeval with the stratigraphically controlled mineralisation features within the Amphitheatre Group successions, implying a provenance influence on mineralisation. Data suggest the different sediment source regions have produced distinct detrital mineral compositions between the major mineral-hosting and mineral-barren formations. The enrichment of some detrital minerals in the mineral-hosting units, such as feldspar, muscovite, Ti-minerals (and carbonate), is suggested to be an important factor for mineralisation in the basin. Detrital zircon geochronology and whole-rock geochemistry illustrate the history of basin fill for the Cobar Basin. Spatial and temporal variation of basin provenance reflects a modification of basin geography, corresponding to the evolving tectonic regimes. The change in basin source regions is one of key controls on the mineralisation within the Cobar Basin.
DOI: 10.6084/m9.figshare.24891668
title: Geology of the Mutis Complex, Miomaffo, West Timor

description: Mesozoic forearc assemblages are widespread across Indonesia, and these are also exposed in the overthrust terranes on Timor. The oldest rocks in the allochthonous Mutis Complex, West Timor are Mesozoic basaltic volcaniclastic rocks and melange containing blocks of normal mid-ocean ridge basalt (N-MORB) basalt (194 ± 5 Ma), amphibolite (metamorphism at 184 ± 6 Ma), garnet and actinolite-bearing schists, arkosic sandstone and volcanogenic sedimentary rocks. Based on the large component of Jurassic material, these rocks were probably derived from the Woyla terrane. The eastern part of the Miomaffo massif is complexly deformed with a dominant foliation overprinted by several fold and fault events including late normal cataclastic zones. This sequence is intruded by calc-alkaline andesitic dykes (possibly in the Eocene). The Central Sector of the massif is a block of high-strain greenschist facies rocks where the primary texture can no longer be recognised, but the bulk composition is the same as the volcaniclastic rocks in the east. Further west is an amphibolite facies metamorphic province. Amphibolite from the Western Sector have the same N-MORB composition as the basalt in the east, but the gneissic rocks have a higher proportion of arc-sourced protoliths. The peak metamorphic conditions were 650 °C and 0.9 GPa. This metamorphic event occurred at 37 Ma, reflecting subduction on the southeast margin of Sundaland, whereas the low-grade Mesozoic metamorphism of the Eastern Sector of the massif occurred in the accretionary prism along the Woyla Arc. The Mutis Complex at Miomaffo demonstrates the complex geological history of Mesozoic rocks in eastern Indonesia. The Miomaffo massif demonstrates the strong oceanic character of the Banda terrane. The anomalous Eocene metamorphic age of rocks ‘unconformably overlain’ by Cretaceous sediments is resolved.
DOI: 10.6084/m9.figshare.24733484
title: Shoshonitic pluton and an associated base-metal deposit in the Tarom–Hashtjin metallogenic zone, NW Iran: implication for tectono-magmatic evolution and metallogenic considerations

description: Petrological, geochemical and zircon U–Pb and Hf isotope studies were carried out on the Hajseyran pluton, along the Tarom–Hashtjin metallogenic zone, as part of the Alborz–Azerbaijan magmatic belt, which is located in the central part of the Alpine–Himalayan orogenic belt. The Hajseyran pluton, which is made up of syenite, monzonite, quartz-monzonite and granite, yields a zircon U–Pb age of 39.20 ± 0.56 Ma (for a quartz-monzonite sample) with shoshonitic features. Enrichment in large ion lithophile elements, depletion in high-field-strength elements and negative anomalies of Nb, Ta and Ti in Chomalou samples suggest a subduction-related arc magmatic setting. The Chomalou epithermal Pb–Zn–Cu deposit occurs close to the Hajseyran pluton with the quartz–base metal sulfide veins predominantly hosted by Eocene volcanic rocks. The ore-forming processes include chalcopyrite and sphalerite–galena formation, with the latter the major mineralisation in this region. Microthermometric results from the liquid–vapour fluid-inclusion assemblages show that the homogenisation temperatures in the first-stage quartz range from 230 to 310 °C, in the sphalerite and second-stage quartz from 161 to 293 °C and in the late-stage quartz from 175 to 262 °C. The salinities of fluids decrease from early-stage quartz to late-stage quartz. The calculated stable isotope values of ore–fluid components (δ<sup>18</sup>O<sub>water</sub> = +3.28‰ to −3.68‰; δ<sup>34</sup>S<sub>H2S</sub> = +5.5‰ to +7.8‰) show that magmatic fluids have played a significant role during mineralisation. The Chomalou deposit is interpreted as a volcanic-hosted intermediate-sulfidation type of epithermal mineralisation formed through shallow-level emplacement of the Hajseyran pluton, which formed <i>via</i> partial melting of phlogopite–amphibole-bearing sub-continental lithospheric mantle. The Neotethyan slab roll-back and concomitant asthenospheric upwelling led to the decompression melting of metasomatised sub-continental lithospheric mantle and the formation of several K-rich plutons and associated epithermal deposits in the Alborz–Azerbaijan magmatic belt. The late Eocene Hajseyran pluton shows a shoshonitic, arc-related signature. The Chomalou Pb–Zn–Cu deposit is an intermediate-sulfidation style of epithermal mineralisation. Fluid inclusion and stable isotope data suggest the evolution of ore-fluid system from magmatic to meteoric. Decompression melting of metasomatised sub-continental lithospheric mantle <i>via</i> slab roll-back led to the formation of Hajseyran pluton.
DOI: 10.5281/zenodo.10694979
title: Review of WorldFAIR Agricultural Plant-Pollinator Data Pilot: Max Rünzel, Drew Robinson. 2023. HiveTracks WorldFAIR Test Data.

description: Abstract

Life on Earth is sustained by complex interactions between organisms and their environment. These biotic interactions can be captured in datasets and published digitally. We describe a review process of such an openly accessible digital interactions dataset of known origin, and discuss their outcome. The dataset under review (aka globalbioticinteractions/hivetracks2023) has size 84.2KiB and contains 1 interaction with 1 unique type of association (e.g., pollinatedBy) between 1 primary taxon (e.g., Trifolium repens) and 1 associated taxon (e.g., Apis mellifera ligustica). The report includes detailed summaries of interactions data as well as a taxonomic review from multiple catalogs.

Please note that the pilot contributors have opted to provide open access to their metadata and review. Their data is available on request. 




filename
description


index.pdf
data review report as pdf


index.docx
data review report as docx


index.md
data review report as markdown


index.html
data review report as html


eml.xml
metadata as expressed in Ecological Metadata Language
description: WorldFAIR has received funding from the European Commission’s WIDERA coordination and support programme under the Grant Agreement no. 101058393. The content of this document does not represent the opinion of the European Commission, and the European Commission is not responsible for any use that might be made of such content.
DOI: 10.5281/zenodo.10694980
title: Review of WorldFAIR Agricultural Plant-Pollinator Data Pilot: Max Rünzel, Drew Robinson. 2023. HiveTracks WorldFAIR Test Data.

description: Abstract

Life on Earth is sustained by complex interactions between organisms and their environment. These biotic interactions can be captured in datasets and published digitally. We describe a review process of such an openly accessible digital interactions dataset of known origin, and discuss their outcome. The dataset under review (aka globalbioticinteractions/hivetracks2023) has size 84.2KiB and contains 1 interaction with 1 unique type of association (e.g., pollinatedBy) between 1 primary taxon (e.g., Trifolium repens) and 1 associated taxon (e.g., Apis mellifera ligustica). The report includes detailed summaries of interactions data as well as a taxonomic review from multiple catalogs.

Please note that the pilot contributors have opted to provide open access to their metadata and review. Their data is available on request. 




filename
description


index.pdf
data review report as pdf


index.docx
data review report as docx


index.md
data review report as markdown


index.html
data review report as html


eml.xml
metadata as expressed in Ecological Metadata Language
description: WorldFAIR has received funding from the European Commission’s WIDERA coordination and support programme under the Grant Agreement no. 101058393. The content of this document does not represent the opinion of the European Commission, and the European Commission is not responsible for any use that might be made of such content.
DOI: 10.6084/m9.figshare.24862782
title: MGHKFastq_Plate1_COI_ARMS

description: Fastq files for COI metabarcoding of samples (sessile scrapings, motile &lt;100 microns, motile 100-500 microns) collected from Autonomous Reef Monitoring Structures (ARMS13-ARMS54) deployed within Hong Kong nearshore marine environments.Data associated with publication: McIlroy SE, I Guibert, A Archana, WY Chung, E Duffy, R Gotama, J Hui, N Knowlton, M Leray, C Meyer, G Panagiotou, G Paulay,, B Russell, PD Thompson, DM Baker (accepted) Life goes on: spatial heterogeneity promotes biodiversity in an urbanized coastal marine ecosystem. <i>Global Change Biology</i>
DOI: 10.6084/m9.figshare.24862782.v1
title: MGHKFastq_Plate1_COI_ARMS

description: Fastq files for COI metabarcoding of samples (sessile scrapings, motile &lt;100 microns, motile 100-500 microns) collected from Autonomous Reef Monitoring Structures (ARMS13-ARMS54) deployed within Hong Kong nearshore marine environments.Data associated with publication: McIlroy SE, I Guibert, A Archana, WY Chung, E Duffy, R Gotama, J Hui, N Knowlton, M Leray, C Meyer, G Panagiotou, G Paulay,, B Russell, PD Thompson, DM Baker (accepted) Life goes on: spatial heterogeneity promotes biodiversity in an urbanized coastal marine ecosystem. <i>Global Change Biology</i>
DOI: 10.6084/m9.figshare.24862863
title: MGHKFastq_Plate2_COI_ARMS

description: Fastq files for COI metabarcoding of samples (sessile scrapings, motile &lt;100 microns, motile 100-500 microns) collected from Autonomous Reef Monitoring Structures (ARMS13-ARMS54) deployed within Hong Kong nearshore marine environments.Data associated with publication: McIlroy SE, I Guibert, A Archana, WY Chung, E Duffy, R Gotama, J Hui, N Knowlton, M Leray, C Meyer, G Panagiotou, G Paulay,, B Russell, PD Thompson, DM Baker (accepted) Life goes on: spatial heterogeneity promotes biodiversity in an urbanized coastal marine ecosystem. Global Change Biology
DOI: 10.6084/m9.figshare.24862863.v1
title: MGHKFastq_Plate2_COI_ARMS

description: Fastq files for COI metabarcoding of samples (sessile scrapings, motile &lt;100 microns, motile 100-500 microns) collected from Autonomous Reef Monitoring Structures (ARMS13-ARMS54) deployed within Hong Kong nearshore marine environments.Data associated with publication: McIlroy SE, I Guibert, A Archana, WY Chung, E Duffy, R Gotama, J Hui, N Knowlton, M Leray, C Meyer, G Panagiotou, G Paulay,, B Russell, PD Thompson, DM Baker (accepted) Life goes on: spatial heterogeneity promotes biodiversity in an urbanized coastal marine ecosystem. Global Change Biology
DOI: 10.18739/a2416t169
title: Davis Strait hydrographic mooring Level 2 data: temperature, salinity, and velocity measurements from the Davis Strait Observing System moorings, 2004 to 2022

description: The Davis Strait observing system was established in 2004 to advance understanding of the role of Arctic – sub-Arctic interactions in the climate system by collecting sustained measurements of physical, chemical and biological variability at one of the primary gateways that connect the Arctic and subpolar oceans. Efforts began as a collaboration between researchers at the University of Washington’s Applied Physics Laboratory and the Canadian Department of Fisheries and Ocean’s Bedford Institute of Oceanography, but has grown to include researchers from the Greenland Institute of Natural Resources, Greenland Climate Institute, Danish Technological University, University of Alberta and University of Colorado, Boulder. The project is a component of the NSF Arctic Observing and Atlantic Meridional Overturning Networks, and the international Arctic-Subarctic Ocean Flux (ASOF) program, Global Ocean Ship-Based Hydrographic Investigations Program (GO-SHIP), Global Ocean Acidification Observing Network (GOA-ON), Arctic Monitoring Assessment Programme (AMAP) and OceanSITES system.
 A mooring array spanning the entire Davis Strait has been in place nearly continuously since September 2004 as part of the Davis Strait observing system, collecting year-round measurements of temperature, salinity and velocity extending to the sea surface/ice-ocean interface. The mooring typically included 14 moorings, 4 on each shelf and 6 in the center of the strait, that are recovered and data offloaded each autumn. Exact mooring location, instrumentation, and deployment duration varied slightly over time.
 This dataset consists of Level 2 data from the Davis Strait mooring array. Each file contains data from a single sensor (e.g., MicroCAT temperature and salinity measurements or ADCP velocity measurements) at one mooring site collected during a single deployment (typically one year long). Files also include quality control flags.
 More details about the project can be found at https://iop.apl.washington.edu/project.php?id=davis.
DOI: 10.25919/wfte-7b76
title: Parkes observations for project P630 semester 2009APRS_20

description: We propose to carry out the most ambitious and comprehensive all-sky survey for pulsars and transient sources to date. Using the 20cm multibeam and a new digital filterbank array this survey will create a petabyte digital record of the sky that can be data mined in the future and used to search for relativistic binary and millisecond pulsars, RRATs, and extragalactic radio bursts. The survey should discover 100s of new millisecond and normal pulsars and help define the lower limit to pulsar periods, test theories of relativistic gravity, find transients and provide pulsars for gravitational wave detection. With all the hardware in place, and our first new pulsar discovery made, we request a substantial time allocation this semester.
DOI: 10.18739/a2086372j
title: Winter open-water zone remote sensing (2017-2023) and field (2023) data from the Yukon and Kuskokwim rivers and their tributaries in western Alaska

description: Timing and completeness of freeze-up on northern rivers impacts safe winter travel and may indicate responses to climate change. Open-water zones (OWZs) within ice-covered rivers are hazardous partly because their unpredictability and are suggested to be increasing in extent and persistence due to groundwater upwelling, higher winter discharge, and permafrost degradation. To better understand the distribution, variability, and mechanisms of winter OWZs, we selected nine study reaches totaling 400 kilometers (km) of the Yukon and Kuskokwim rivers and their tributaries for remote sensing analysis and field studies in western Alaska, USA. We identified 51 OWZs from late November optical imagery along these reaches ranging from 60 meters (m) to 9 km in length, inventoried their persistence over six years, and at a subset measured ice thickness, under-ice water depth and velocity, water-column and river-bed physico-chemistry. Concurrently, we investigated if and to what extent sediment was entrained in river ice at these same sites. These locations corresponding to observed OWZs were quantified by size, classified by hydrogeomophic location, and tracked for consistency during the preceding five years in the early (late November) and late (late February or early March) winter periods. A subset of these OWZ were visited in March of 2023 to collect additional field data on snow, ice, and physico-chemistry including ice sediment concentration. This research is part of the Fresh Eyes on Ice and Sediment Ice Learning on the Tanana (SILT) projects.
DOI: 10.34740/kaggle/dsv/7681720
title: WallStreetBets 2022
DOI: 10.6084/m9.figshare.25270276.v3
title: AgingMouseBrain

description: UCSC track hub
DOI: 10.5519/qd.nrktvo3y
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (12948 records)
DOI: 10.48668/g23xxx/0g3wqg
title: wvs_translate_updated_v5.tab

description: Country names consolidation
DOI: 10.48668/g23xxx/heq6lm
title: WVS Data prep RR.R

description: Data preparation
DOI: 10.48668/g23xxx/ika489
title: WVS Analysis RR.R

description: Data analysis
DOI: 10.48668/g23xxx/km8olm
title: VDEM_Polarization.tab

description: Country-level polarization data
DOI: 10.48668/g23xxx/s38le7
title: Country_Variables_27_NEW.tab

description: Data for control variables
DOI: 10.48668/g23xxx
title: R Scripts and data to reproduce results for Social media use and political engagement in polarized times. Examining the contextual roles of issue and affective polarization in developed democracies

description: R scripts and data to reproduce data analyses. Note that data for the V-DEM file "V-Dem-CY-Full+Others-v12.sav" and WVS file "WVS_Cross-National_Wave_7_csv_v5_0.csv" must be downloaded directly from their respective websites.
DOI: 10.48668/g23xxx/v1nk4x
title: ReadMe.txt

description: :unav
DOI: 10.5517/ccdc.csd.cc2f6lr0
title: CCDC 2240672: Experimental Crystal Structure Determination

description: Related Article: Ryo Sumitani, Yosuke Nakazono, Rio Soga, Tomoyuki Mochida|2024|J.Mol.Liq.|397|124163|doi:10.1016/j.molliq.2024.124163
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.cc2fc5tt
title: CCDC 2245076: Experimental Crystal Structure Determination

description: Related Article: Rachel T. Smith, Kelly M. Walsh, Qianni Jiang, Jiun-Haw Chu, Daniel R. Gamelin|2024|Chem.Mater.|36|1571|doi:10.1021/acs.chemmater.3c02824
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.cc2fflyf
title: CCDC 2247405: Experimental Crystal Structure Determination

description: Related Article: Ryo Sumitani, Yosuke Nakazono, Rio Soga, Tomoyuki Mochida|2024|J.Mol.Liq.|397|124163|doi:10.1016/j.molliq.2024.124163
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.