cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.tjg9r5
title: Occurrence Download

description: A dataset containing 33 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "and" : [
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen)"
 ]
 }
 }
 ]
 },
 "TaxonKey is Craugastor emleni (Dunn, 1932)"
 ]
}

 The dataset includes 33 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0043515-240229165702484/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25582/data.2019-12.1896286/2366637
title: Data for EMSL Project 50076 from December 2019
DOI: 10.15468/dl.vfjwpz
title: Occurrence Download

description: A dataset containing 2103 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Chelon auratus (Risso, 1810)"
 ]
}

 The dataset includes 2103 records from 128 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0029890-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.pzgvar
title: Occurrence Download

description: A dataset listing the 1 species recorded in GBIF matching the query:
{
 "TaxonKey" : [
 "is Helianthemum piliferum Boiss."
 ]
}

 The dataset's 1 records were derived from 22 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0013394-190918142434337/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25582/data.2020-01.1938929/2366638
title: Data for EMSL Project 50076 from January 2020
DOI: 10.15468/dl.cw8jzw
title: Occurrence Download

description: A dataset containing 366 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Psammodromus occidentalis Fitze, Gonzalez-Jimena, San-Jose, San Mauro & Zardoya, 2012"
 ]
}

 The dataset includes 366 records from 7 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0043561-240229165702484/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.vaegfg
title: Occurrence Download

description: A dataset containing 148 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Diascia elongata Benth."
 ]
}

 The dataset includes 148 records from 20 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0029900-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.vs8jpi
title: Occurrence Download

description: A dataset containing 48 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-19.43816 28.92784,13.43816 28.92784,13.43816 42.07216,-19.43816 42.07216,-19.43816 28.92784))",
 "HasCoordinate is true",
 "TaxonKey is Anthyllis podocephala Boiss.",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 48 records from 7 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0013387-190918142434337/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25582/data.2020-01.1935486/2366639
title: Data for EMSL Project 50076 from January 2020
DOI: 10.15468/dl.tspvcb
title: Occurrence Download

description: A dataset containing 12 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is China",
 "TaxonKey is Abies beshanzuensis M.H.Wu"
 ]
}

 The dataset includes 12 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0039528-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.25906482
title: Additional file 1 of Determination of safety margin of nasal septum osteotomy for sphenoid sinus in cleft lip and palate patients

description: Supplementary Material 1.
DOI: 10.15468/dl.qb7q29
title: Occurrence Download

description: A dataset containing 143 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Cryptocarya thouvenotii (Danguy) Kosterm."
 ]
}

 The dataset includes 143 records from 14 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0012083-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.25906482.v1
title: Additional file 1 of Determination of safety margin of nasal septum osteotomy for sphenoid sinus in cleft lip and palate patients

description: Supplementary Material 1.
DOI: 10.15468/dl.vf98aa
title: Occurrence Download

description: A dataset containing 66 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Dillenia ingens B.L.Burtt"
 ]
}

 The dataset includes 66 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0029893-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25582/data.2020-01.1935368/2366640
title: Data for EMSL Project 50076 from January 2020
DOI: 10.15468/dl.jgkfdp
title: Occurrence Download

description: A dataset containing 1746 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "or" : [
 "BasisOfRecord is Human Observation",
 "BasisOfRecord is Specimen"
 ]
 },
 {
 "or" : [
 "Issue is Coordinate rounded",
 "Issue is Geodetic datum assumed WGS84",
 "Issue is Country derived from coordinates"
 ]
 },
 "HasCoordinate is true",
 "TaxonKey is Drosera binata Labill.",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 1746 records from 21 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0013396-190918142434337/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25582/data.2019-11.1884830/2366641
title: Data for EMSL Project 50076 from November 2019
DOI: 10.15468/dl.9wtsfj
title: Occurrence Download

description: A dataset containing 489 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Periploca aphylla Decne."
 ]
}

 The dataset includes 489 records from 44 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0043622-240229165702484/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.gmj8as
title: Occurrence Download

description: A dataset containing 1 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Dypsis plumosa Hodel, Marcus & J.Dransf."
 ]
}

 The dataset includes 1 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0029860-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.f7jxox
title: Occurrence Download

description: A dataset containing 16 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "or" : [
 "BasisOfRecord is Human Observation",
 "BasisOfRecord is Specimen"
 ]
 },
 {
 "or" : [
 "Issue is Coordinate rounded",
 "Issue is Geodetic datum assumed WGS84"
 ]
 },
 "HasCoordinate is true",
 "TaxonKey is Drosera brevicornis Lowrie",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 16 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0013400-190918142434337/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25582/data.2020-01.1934691/2366642
title: Data for EMSL Project 50076 from January 2020
DOI: 10.25582/data.2020-01.1935449/2366643
title: Data for EMSL Project 50076 from January 2020
DOI: 10.15468/dl.cqe2cz
title: Occurrence Download

description: A dataset containing 2503 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Amaurospiza moesta (Hartlaub, 1853)"
 ]
}

 The dataset includes 2503 records from 27 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0012077-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.25414113
title: Detrital or reset? <sup>40</sup>Ar/<sup>39</sup>Ar dating of mica from the Lower Jurassic Precipice Sandstone and Evergreen Formation in the Surat Basin

description: The U–Pb detrital zircon record of the Surat Basin, an important part of the Great Australian Superbasin, has already revealed important insights about sediment source terranes. However, owing to the high closure temperature of zircons, low-temperature thermal events that might have impacted the sediment are not recorded. Here, new <sup>40</sup>Ar/<sup>39</sup>Ar detrital mica ages, which record low-temperature events as a result of isotopic resetting, are paired with published U–Pb detrital zircon ages from the same samples to provide a more complete interpretation of the tectonic and thermal history of the Jurassic-age Precipice Sandstone and Evergreen Formation. The <sup>40</sup>Ar/<sup>39</sup>Ar geochronology of mica grains from five wells reveals two broad groups with distinct age populations: 1500–180 Ma and 150–45 Ma. Micas older than about 180 Ma are sourced from multiple terranes. The slight discrepancy in ages between the <sup>40</sup>Ar/<sup>39</sup>Ar and the U–Pb systems of the same samples may represent differences in closure temperature. However, some micas, such as those dating to <i>ca</i> 180 Ma, may also reflect a thermal reset event. Similarly, the younger group of micas, split into Cretaceous and Paleogene populations, reflect the impact of post-depositional thermal events on the basin. Isotopic resetting of the micas was likely the result of hydrothermal fluids migrating through reactivated faults, fractures and/or porous and permeable sediments. The origin of the fluids during the Cretaceous can be linked to an eastern subduction zone and subsequent igneous underplating resulting in uplift and denudation. The exact source of the hydrothermal fluids for the micas of Paleogene age, recorded in samples collected from the base of the Evergreen Formation, however, remains uncertain. Importantly, <sup>40</sup>Ar/<sup>39</sup>Ar dating of mica from sandstones permits the detection of post-depositional thermal events that may have implications for tracing fluid migration throughout the basin and reconstructing the Cretaceous–Paleogene tectonic history of the basin. Combining <sup>40</sup>Ar/<sup>39</sup>Ar dating of micas with U–Pb dating of zircons reveals a more complete tectonic and thermal history of the Jurassic-age Precipice Sandstone and Evergreen Formation of the Surat Basin. <sup>40</sup>Ar/<sup>39</sup>Ar dating of detrital micas reveals two broad groups with distinct age populations: 1500–180 Ma and 140–45 Ma. Ages older than <i>ca</i> 180 Ma are linked to multiple source terranes, including the Thomson and New England orogens, and the contemptuous magmatic arc. Ages younger than 150 Ma are most likely the result of post-depositional thermal resetting events, which may have implications for fluid movement throughout the basin.
DOI: 10.6084/m9.figshare.25414113.v1
title: Detrital or reset? <sup>40</sup>Ar/<sup>39</sup>Ar dating of mica from the Lower Jurassic Precipice Sandstone and Evergreen Formation in the Surat Basin

description: The U–Pb detrital zircon record of the Surat Basin, an important part of the Great Australian Superbasin, has already revealed important insights about sediment source terranes. However, owing to the high closure temperature of zircons, low-temperature thermal events that might have impacted the sediment are not recorded. Here, new <sup>40</sup>Ar/<sup>39</sup>Ar detrital mica ages, which record low-temperature events as a result of isotopic resetting, are paired with published U–Pb detrital zircon ages from the same samples to provide a more complete interpretation of the tectonic and thermal history of the Jurassic-age Precipice Sandstone and Evergreen Formation. The <sup>40</sup>Ar/<sup>39</sup>Ar geochronology of mica grains from five wells reveals two broad groups with distinct age populations: 1500–180 Ma and 150–45 Ma. Micas older than about 180 Ma are sourced from multiple terranes. The slight discrepancy in ages between the <sup>40</sup>Ar/<sup>39</sup>Ar and the U–Pb systems of the same samples may represent differences in closure temperature. However, some micas, such as those dating to <i>ca</i> 180 Ma, may also reflect a thermal reset event. Similarly, the younger group of micas, split into Cretaceous and Paleogene populations, reflect the impact of post-depositional thermal events on the basin. Isotopic resetting of the micas was likely the result of hydrothermal fluids migrating through reactivated faults, fractures and/or porous and permeable sediments. The origin of the fluids during the Cretaceous can be linked to an eastern subduction zone and subsequent igneous underplating resulting in uplift and denudation. The exact source of the hydrothermal fluids for the micas of Paleogene age, recorded in samples collected from the base of the Evergreen Formation, however, remains uncertain. Importantly, <sup>40</sup>Ar/<sup>39</sup>Ar dating of mica from sandstones permits the detection of post-depositional thermal events that may have implications for tracing fluid migration throughout the basin and reconstructing the Cretaceous–Paleogene tectonic history of the basin. Combining <sup>40</sup>Ar/<sup>39</sup>Ar dating of micas with U–Pb dating of zircons reveals a more complete tectonic and thermal history of the Jurassic-age Precipice Sandstone and Evergreen Formation of the Surat Basin. <sup>40</sup>Ar/<sup>39</sup>Ar dating of detrital micas reveals two broad groups with distinct age populations: 1500–180 Ma and 140–45 Ma. Ages older than <i>ca</i> 180 Ma are linked to multiple source terranes, including the Thomson and New England orogens, and the contemptuous magmatic arc. Ages younger than 150 Ma are most likely the result of post-depositional thermal resetting events, which may have implications for fluid movement throughout the basin.
DOI: 10.15468/dl.4mbv8z
title: Occurrence Download

description: A dataset containing 214 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "and" : [
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen)"
 ]
 }
 }
 ]
 },
 "TaxonKey is Campephilus principalis (Linnaeus, 1758)"
 ]
}

 The dataset includes 214 records from 32 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0029897-240314170635999/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.25426079
title: <i>P</i>–<i>T</i> conditions of metamorphic and hydrothermal events at Tick Hill gold deposit, Mount Isa, Queensland, Australia

description: Tick Hill gold deposit is a unique gold mineralisation style in the Mary Kathleen Fold Belt in the Mount Isa Inlier. The gold at Tick Hill is generally pure without silver and was formed during two discrete metamorphic-deformation events (D<sub>1</sub> and D<sub>3</sub>). Early gold was observed as inclusions or coarse grains hosted within D<sub>1</sub> peak-metamorphic diopside, scapolite and hornblende from the garnet–biotite–hornblende (tschemakite)–plagioclase (andesine)–quartz assemblage. Late gold is closely associated with bismuth selenide, chlorite, albite, sericite and K-feldspar, and formed during D<sub>3</sub>. The syn-D<sub>1</sub> garnet–plagioclase–hornblende–quartz–biotite assemblage was used to constrain the pressure and temperature (<i>P</i>–<i>T</i>) conditions of metamorphism and mineralisation using the garnet–plagioclase–hornblende–quartz barometer and the hornblende–plagioclase, garnet–biotite and garnet–hornblende thermometers. The results show that peak metamorphism at Tick Hill reached <i>P</i>–<i>T</i> conditions of 6.0–7.6 kbar and 720–760 °C. These <i>P</i>–<i>T</i> conditions together with gneissic and migmatisation textures recorded in different rock types at the Tick Hill area indicate that the peak metamorphism preserved in the area occurred at the amphibolite–granulite facies, compared with the amphibolite facies at the southern Mary Kathleen and Eastern Fold Belt. The D<sub>3</sub> chlorite, which formed during stage 2 to stage 4 mineralisation events, displays a wide range of compositions reflecting a gradual retrograde temperature change from ∼380 °C to ∼130 °C. The pressures during D<sub>3</sub> could not be reliably determined, but the presence of various Bi-selenides suggests that towards the waning stages of D<sub>3</sub>, the rocks may have been exhumed to a pressure less than 1 kbar. The 1790–1770 Ma D<sub>1</sub> peak metamorphism at Tick Hill reached 6–7.6 kbar and 720–760 °C. The 1525–1520 Ma D<sub>3</sub> hydrothermal mineralisation at Tick Hill Deposit occurred at temperatures between ∼380 °C and ∼130 °C. The main D<sub>3</sub> gold accumulation episodes at Tick Hill occurred at temperatures ranging from ∼380 to 160 °C.
DOI: 10.6084/m9.figshare.25762417
title: Paragenetic and geological setting of the Starra iron oxide copper–gold deposits, Mount Isa Inlier, Queensland, Australia: constraints on IOCG deposit models

description: The five Starra iron oxide copper–gold (IOCG) deposits, which are located in the Cloncurry district of the Mount Isa Inlier, NW Queensland, are hosted in a N-trending zone of deformed iron-rich metasedimentary rocks that are underlain by two mineralogically distinct mafic–intermediate meta-igneous rocks. Copper–Au mineralisation is subdivided into two stages—an early main stage that transitioned from a magnetite-dominated Cu substage comprising chalcopyrite, pyrite, biotite and chlorite, to a hematite–muscovite-bearing Cu–Au substage with chalcopyrite, bornite and rare chalcocite, as well as Au–Ag-tellurides and native Au. This second stage was followed by a subordinate but nonetheless important carbonate–quartz–barite vein stage with minor but locally high-grade Cu–Au mineralisation characterised by abundant chalcocite and bornite, minor native bismuth and wittichenite (Cu<sub>3</sub>BiS<sub>3</sub>), together with minor Au–Ag telluride minerals. Bornite in these carbonate–quartz–barite veins contains considerable amounts of Au (&gt;10 ppm), which appears to be deported either as lattice substitution in the bornite crystal structure or as homogeneously distributed Au<sup>0</sup> nanoparticles. An earlier, coarse-grained mafic intrusion was affected by early Na–Ca alteration, whereas a second mafic intrusion lacks evidence of Na–Ca alteration but was exposed to K–Fe alteration and subsequent mineralisation at Starra 222. Mushketovite (magnetite after specular hematite) is only observed in ironstone lodes proximal to the mafic–intermediate rocks. The close spatial and mineralogical associations of the mafic–intermediate bodies and the ironstone lodes point to a stronger link between magmatic activity and IOCG mineralisation than has previously been recognised at Starra. Remobilisation of gold by late-stage hydrothermal fluids aided by the relatively low fluid temperatures during the main pulse of Cu–Au mineralisation refined gold grades at Starra, making it a relatively gold-rich IOCG deposit. We show that the Cu–Au deposits of the Starra trend feature mineralogical and geochemical elements common to both Cloncurry IOCG deposits (<i>e.g.</i> abundant magnetite) and IOCG deposits of the Tennant Creek district (<i>e.g.</i> Au–Cu–Bi mineralisation; hematite–bornite–chalcocite assemblages), making them a unique and important member of this complex family of deposits. Mafic–intermediate sills below Starra ore deposits indicate a potential link between magmatic activity and IOCG mineralisation. Mushketovite associated with chalcopyrite mineralisation indicates that the mineralising fluid was initially reduced. Different radiogenic Pb isotope compositions in Cu sulfides, hematite and calcite require multiple Pb sources, which is consistent with distinct fluids.
DOI: 10.6084/m9.figshare.25762417.v1
title: Paragenetic and geological setting of the Starra iron oxide copper–gold deposits, Mount Isa Inlier, Queensland, Australia: constraints on IOCG deposit models

description: The five Starra iron oxide copper–gold (IOCG) deposits, which are located in the Cloncurry district of the Mount Isa Inlier, NW Queensland, are hosted in a N-trending zone of deformed iron-rich metasedimentary rocks that are underlain by two mineralogically distinct mafic–intermediate meta-igneous rocks. Copper–Au mineralisation is subdivided into two stages—an early main stage that transitioned from a magnetite-dominated Cu substage comprising chalcopyrite, pyrite, biotite and chlorite, to a hematite–muscovite-bearing Cu–Au substage with chalcopyrite, bornite and rare chalcocite, as well as Au–Ag-tellurides and native Au. This second stage was followed by a subordinate but nonetheless important carbonate–quartz–barite vein stage with minor but locally high-grade Cu–Au mineralisation characterised by abundant chalcocite and bornite, minor native bismuth and wittichenite (Cu<sub>3</sub>BiS<sub>3</sub>), together with minor Au–Ag telluride minerals. Bornite in these carbonate–quartz–barite veins contains considerable amounts of Au (&gt;10 ppm), which appears to be deported either as lattice substitution in the bornite crystal structure or as homogeneously distributed Au<sup>0</sup> nanoparticles. An earlier, coarse-grained mafic intrusion was affected by early Na–Ca alteration, whereas a second mafic intrusion lacks evidence of Na–Ca alteration but was exposed to K–Fe alteration and subsequent mineralisation at Starra 222. Mushketovite (magnetite after specular hematite) is only observed in ironstone lodes proximal to the mafic–intermediate rocks. The close spatial and mineralogical associations of the mafic–intermediate bodies and the ironstone lodes point to a stronger link between magmatic activity and IOCG mineralisation than has previously been recognised at Starra. Remobilisation of gold by late-stage hydrothermal fluids aided by the relatively low fluid temperatures during the main pulse of Cu–Au mineralisation refined gold grades at Starra, making it a relatively gold-rich IOCG deposit. We show that the Cu–Au deposits of the Starra trend feature mineralogical and geochemical elements common to both Cloncurry IOCG deposits (<i>e.g.</i> abundant magnetite) and IOCG deposits of the Tennant Creek district (<i>e.g.</i> Au–Cu–Bi mineralisation; hematite–bornite–chalcocite assemblages), making them a unique and important member of this complex family of deposits. Mafic–intermediate sills below Starra ore deposits indicate a potential link between magmatic activity and IOCG mineralisation. Mushketovite associated with chalcopyrite mineralisation indicates that the mineralising fluid was initially reduced. Different radiogenic Pb isotope compositions in Cu sulfides, hematite and calcite require multiple Pb sources, which is consistent with distinct fluids.