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

description: A dataset containing 10945 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Bryum pseudotriquetrum (Hedw.) G.Gaertn., B.Mey. & Scherb.",
 "HasCoordinate is true",
 "Continent is Europe",
 "HasGeospatialIssue is false",
 "Year is greater than or equal to 2000",
 "CoordinateUncertaintyInMeters is less than 10000"
 ]
}

 The dataset includes 10945 records from 104 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0011202-240216155721649/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.57934/0b01e410802dcb3f
title: Overzicht van gemeenten in verschillende gebiedsindelingen in Nederland
DOI: 10.57934/0b01e410802dd351
title: Productiestatistiek Agrarische dienstverlening
DOI: 10.15468/dl.d2sbnp
title: Occurrence Download

description: A dataset containing 407 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Spiraea tomentosa L.",
 "BasisOfRecord is one of (Specimen)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Continent is North America"
 ]
}

 The dataset includes 407 records from 20 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0167441-200613084148143/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.ez8cn8
title: Occurrence Download

description: A dataset containing 36 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Grewia baillonii R.Vig."
 ]
}

 The dataset includes 36 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0013883-240321170329656/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.hzxnr3
title: Occurrence Download

description: A dataset containing 694 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Spermacoce remota Lam.",
 "BasisOfRecord is one of (Specimen)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Continent is North America"
 ]
}

 The dataset includes 694 records from 11 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0167474-200613084148143/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.nbxlg1
title: Occurrence Download

description: A dataset containing 1241 species occurrences available in GBIF matching the query:
{
 "or" : [
 "TaxonKey is Lytocarpia myriophyllum (Linnaeus, 1758)",
 "TaxonKey is Phakellia ventilabrum (Linnaeus, 1767)"
 ]
}

 The dataset includes 1241 records from 51 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027727-190415153152247/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.kykr6x
title: Occurrence Download

description: A dataset containing 14 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Pariana ligulata Swallen"
 ]
}

 The dataset includes 14 records from 7 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0034123-240229165702484/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.7814174
title: Mesozoic–Cenozoic sedimentary rock records and applications for provenance of sediments and affiliation of the Simao Terrane, SW China

description: As the north part of Simao Terrane, Lanping Basin is located between the Sanjiang Tethys Orogen (STO) and Yangtze Block, also the junction zone between the Gondwanaland and Cathaysian old land (Pan Huaxia mainland), which includes Yangtze and Cathaysian Blocks. The aim of this study is to decipher the provenance of the sedimentary units in the Lanping Basin and affiliation of Simao Terrane by the U-Pb ages, Hf isotope of detrital zircons and whole-rock geochemistry. The whole-rock geochemistry and the mineral composition indicate that most of the Triassic–Paleocene sedimentary rocks are derived from the upper crust and exhibit recycled orogen features. The detrital zircon U-Pb ages from the North Simao Terrane are consistent with the magmatic events during Early Neoproterozoic and Permian in the Western Yangtze Block. And the detrital zircons ages from North Simao Terrane show same distribution features as the Permian–Triassic magmatic rocks, which are distributed in the Simao Terrane and along major sutures. These comparisons suggest that the clastic sediments in Lanping Basin (North Simao Terrane) are derived from Early Neoproterozoic and Permian magmatic rocks from Western Yangtze Block, Permian–Triassic magmatic rocks from Simao Terrane, along Jinshajiang, Garz-Litang and Ailaoshan Sutures. The comparison of the detrital zircon age distributions shows that Simao Terrane and Yangtze Block exhibited similarity tectonic setting in the evolution history, especially during Paleoproterozoic–Late Paleozoic. This suggests that the Simao Terrane is part of Cathaysian old land, although Simao Terrane was separated from Yangtze Block for short period during Early Paleozoic. Besides, the Hf mapping, stratigraphic succession, paleogeography and paleomagnetism in SW China support that Simao Terrane has a Cathaysian old land-affinity, rather than one involving Gondwanaland.
DOI: 10.6084/m9.figshare.7814174.v1
title: Mesozoic–Cenozoic sedimentary rock records and applications for provenance of sediments and affiliation of the Simao Terrane, SW China

description: As the north part of Simao Terrane, Lanping Basin is located between the Sanjiang Tethys Orogen (STO) and Yangtze Block, also the junction zone between the Gondwanaland and Cathaysian old land (Pan Huaxia mainland), which includes Yangtze and Cathaysian Blocks. The aim of this study is to decipher the provenance of the sedimentary units in the Lanping Basin and affiliation of Simao Terrane by the U-Pb ages, Hf isotope of detrital zircons and whole-rock geochemistry. The whole-rock geochemistry and the mineral composition indicate that most of the Triassic–Paleocene sedimentary rocks are derived from the upper crust and exhibit recycled orogen features. The detrital zircon U-Pb ages from the North Simao Terrane are consistent with the magmatic events during Early Neoproterozoic and Permian in the Western Yangtze Block. And the detrital zircons ages from North Simao Terrane show same distribution features as the Permian–Triassic magmatic rocks, which are distributed in the Simao Terrane and along major sutures. These comparisons suggest that the clastic sediments in Lanping Basin (North Simao Terrane) are derived from Early Neoproterozoic and Permian magmatic rocks from Western Yangtze Block, Permian–Triassic magmatic rocks from Simao Terrane, along Jinshajiang, Garz-Litang and Ailaoshan Sutures. The comparison of the detrital zircon age distributions shows that Simao Terrane and Yangtze Block exhibited similarity tectonic setting in the evolution history, especially during Paleoproterozoic–Late Paleozoic. This suggests that the Simao Terrane is part of Cathaysian old land, although Simao Terrane was separated from Yangtze Block for short period during Early Paleozoic. Besides, the Hf mapping, stratigraphic succession, paleogeography and paleomagnetism in SW China support that Simao Terrane has a Cathaysian old land-affinity, rather than one involving Gondwanaland.
DOI: 10.15468/dl.gjholc
title: Occurrence Download

description: A dataset containing 5183 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "TaxonKey is Asplenium marinum L.",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 5183 records from 88 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027730-180131172636756/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.9699395
title: Petrogenetic link between amphibolites and the banded iron formation of the Yishui region in the North China Craton: implications for Neoarchean plume tectonics

description: Amphibolites have a genetically close relationship with banded iron formations (BIFs) in the North China Craton (NCC). The Yishui amphibolites in the NCC occur interbedded with Algoma–type Yishui BIFs as related wall rocks. A reconstruction of the amphibolite protolith was conducted based on the results of petrologic, mineralogic, and geochemical analyses. The Yishui amphibolites consist of actinolite, ferrohornblende, albite, orthoclase, biotite, quartz, magnetite with minor pyrite, titanite, and ilmenite. Their chemical compositions are mainly SiO<sub>2</sub>, Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>, CaO, and Al<sub>2</sub>O<sub>3</sub> with subordinate TiO<sub>2</sub>, MgO, Na<sub>2</sub>O, K<sub>2</sub>O, P<sub>2</sub>O<sub>5</sub>, and MnO. The chondrite–normalized rare earth element diagram, characterized by enriched light rare earth elements (La/Yb<sub>CN</sub> = 19.51–24.05) with insignificant Eu and Ce anomalies, shows coherent trends. The primitive mantle–normalized multi–element spider diagram is enriched in large ion lithophile elements, high field strength elements, and light rare earth elements which are related to a mantle source. The results of this study, combined with previous literature data, indicate that the Yishui amphibolite protoliths had intraplate alkaline basalt affinities and were derived from an ocean island basalt–type mantle source with no contamination. The results also suggest that the basalts were primarily the product of small amounts of partial melting. Based on the results, it is considered that a mantle plume model is the most appropriate tectonic model as it better explains the amphibolite geochemical signature. Furthermore, this model can provide crucial information regarding the Archaean NCC tectonic evolution and can demonstrate the temporal and spatial relationships between the BIFs and wall rocks.
DOI: 10.6084/m9.figshare.9699395.v2
title: Petrogenetic link between amphibolites and the banded iron formation of the Yishui region in the North China Craton: implications for Neoarchean plume tectonics

description: Amphibolites have a genetically close relationship with banded iron formations (BIFs) in the North China Craton (NCC). The Yishui amphibolites in the NCC occur interbedded with Algoma–type Yishui BIFs as related wall rocks. A reconstruction of the amphibolite protolith was conducted based on the results of petrologic, mineralogic, and geochemical analyses. The Yishui amphibolites consist of actinolite, ferrohornblende, albite, orthoclase, biotite, quartz, magnetite with minor pyrite, titanite, and ilmenite. Their chemical compositions are mainly SiO<sub>2</sub>, Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>, CaO, and Al<sub>2</sub>O<sub>3</sub> with subordinate TiO<sub>2</sub>, MgO, Na<sub>2</sub>O, K<sub>2</sub>O, P<sub>2</sub>O<sub>5</sub>, and MnO. The chondrite–normalized rare earth element diagram, characterized by enriched light rare earth elements (La/Yb<sub>CN</sub> = 19.51–24.05) with insignificant Eu and Ce anomalies, shows coherent trends. The primitive mantle–normalized multi–element spider diagram is enriched in large ion lithophile elements, high field strength elements, and light rare earth elements which are related to a mantle source. The results of this study, combined with previous literature data, indicate that the Yishui amphibolite protoliths had intraplate alkaline basalt affinities and were derived from an ocean island basalt–type mantle source with no contamination. The results also suggest that the basalts were primarily the product of small amounts of partial melting. Based on the results, it is considered that a mantle plume model is the most appropriate tectonic model as it better explains the amphibolite geochemical signature. Furthermore, this model can provide crucial information regarding the Archaean NCC tectonic evolution and can demonstrate the temporal and spatial relationships between the BIFs and wall rocks.
DOI: 10.15468/dl.9qn3q2
title: Occurrence Download

description: A dataset containing 479 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Guaruba guarouba (Gmelin, 1788)"
 ]
}

 The dataset includes 479 records from 48 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0144805-230530130749713/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.9699395.v1
title: Petrogenetic link between amphibolites and the banded iron formation of the Yishui region in the North China Craton: implications for Neoarchean plume tectonics

description: Amphibolites have a genetically close relationship with banded iron formations (BIFs) in the North China Craton (NCC). The Yishui amphibolites in the NCC occur interbedded with Algoma–type Yishui BIFs as related wall rocks. A reconstruction of the amphibolite protolith was conducted based on the results of petrologic, mineralogic, and geochemical analyses. The Yishui amphibolites consist of actinolite, ferrohornblende, albite, orthoclase, biotite, quartz, magnetite with minor pyrite, titanite, and ilmenite. Their chemical compositions are mainly SiO<sub>2</sub>, Fe<sub>2</sub>O<sub>3</sub><sup>T</sup>, CaO, and Al<sub>2</sub>O<sub>3</sub> with subordinate TiO<sub>2</sub>, MgO, Na<sub>2</sub>O, K<sub>2</sub>O, P<sub>2</sub>O<sub>5</sub>, and MnO. The chondrite–normalized rare earth element diagram, characterized by enriched light rare earth elements (La/Yb<sub>CN</sub> = 19.51–24.05) with insignificant Eu and Ce anomalies, shows coherent trends. The primitive mantle–normalized multi–element spider diagram is enriched in large ion lithophile elements, high field strength elements, and light rare earth elements which are related to a mantle source. The results of this study, combined with previous literature data, indicate that the Yishui amphibolite protoliths had intraplate alkaline basalt affinities and were derived from an ocean island basalt–type mantle source with no contamination. The results also suggest that the basalts were primarily the product of small amounts of partial melting. Based on the results, it is considered that a mantle plume model is the most appropriate tectonic model as it better explains the amphibolite geochemical signature. Furthermore, this model can provide crucial information regarding the Archaean NCC tectonic evolution and can demonstrate the temporal and spatial relationships between the BIFs and wall rocks.
DOI: 10.15468/dl.kcyd6d
title: Occurrence Download

description: A dataset containing 1654 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Cicindela formosa generosa Dejean, 1831"
 ]
}

 The dataset includes 1654 records from 27 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0144664-240321170329656/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.nxxhzz
title: Occurrence Download

description: A dataset containing 5 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Astronidium constrictum J.F.Maxwell"
 ]
}

 The dataset includes 5 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0034114-240229165702484/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.7822550
title: Constraint on the eclogite age of the Sanbagawa metamorphic rocks in central Shikoku, Japan

description: To constrain the timing from the accretion to the subduction-related metamorphism of the protolith in the Sanbagawa eclogites, we performed zircon U–Pb datings and REE composition analyses on pelitic schist of the Seba eclogite-facies region in the Besshi area in central Shikoku, Japan. The detrital igneous cores of the zircons show ages from ca. 2000 to 100 Ma, and the metamorphic rims show ca. 90 Ma. These results show that the protolith was accreted at ca. 100–90 Ma, which is significantly younger than the previously reported accretion age of ca. 130 Ma of other eclogite-facies regions in this area. And, the metamorphic rim domains show HREE decrease without Eu anomalies, suggesting that they were formed at ca. 90 Ma eclogite-facies metamorphism. Our results combined with previous reports for the tectonics of the Sanbagawa metamorphic rocks suggest that there are at least two eclogite-facies units with different accretion ages in the Besshi area; ca. 130 Ma unit (Besshi unit) and ca. 100–90 Ma unit (Asemi-gawa unit), which structurally contact with each other. It is likely that the older unit was subducted into a depth of over 50 km and stagnated until the younger unit was subducted to the same depth. Probably, both units were juxtaposed at a mantle depth and began to exhume to the surface at the same timing after ca. 90 Ma. The juxtaposition and exhumation process might have relation to multi-factors such as tectonic erosion along the subduction zone, shallowing subduction angle of the hotter slab, backflow in the mantle and fluid infiltration along exhumation route.
DOI: 10.6084/m9.figshare.7822550.v2
title: Constraint on the eclogite age of the Sanbagawa metamorphic rocks in central Shikoku, Japan

description: To constrain the timing from the accretion to the subduction-related metamorphism of the protolith in the Sanbagawa eclogites, we performed zircon U–Pb datings and REE composition analyses on pelitic schist of the Seba eclogite-facies region in the Besshi area in central Shikoku, Japan. The detrital igneous cores of the zircons show ages from ca. 2000 to 100 Ma, and the metamorphic rims show ca. 90 Ma. These results show that the protolith was accreted at ca. 100–90 Ma, which is significantly younger than the previously reported accretion age of ca. 130 Ma of other eclogite-facies regions in this area. And, the metamorphic rim domains show HREE decrease without Eu anomalies, suggesting that they were formed at ca. 90 Ma eclogite-facies metamorphism. Our results combined with previous reports for the tectonics of the Sanbagawa metamorphic rocks suggest that there are at least two eclogite-facies units with different accretion ages in the Besshi area; ca. 130 Ma unit (Besshi unit) and ca. 100–90 Ma unit (Asemi-gawa unit), which structurally contact with each other. It is likely that the older unit was subducted into a depth of over 50 km and stagnated until the younger unit was subducted to the same depth. Probably, both units were juxtaposed at a mantle depth and began to exhume to the surface at the same timing after ca. 90 Ma. The juxtaposition and exhumation process might have relation to multi-factors such as tectonic erosion along the subduction zone, shallowing subduction angle of the hotter slab, backflow in the mantle and fluid infiltration along exhumation route.
DOI: 10.15468/dl.7cy88j
title: Occurrence Download

description: A dataset containing 722 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Melozone cabanisi (P.L.Sclater & Salvin, 1868)"
 ]
}

 The dataset includes 722 records from 15 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027730-180508205500799/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.utayus
title: Occurrence Download

description: A dataset containing 22951 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Linaria alpina (L.) Mill."
 ]
}

 The dataset includes 22951 records from 203 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0212073-200613084148143/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.7p7yvm
title: Occurrence Download

description: A dataset containing 7 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Astronidium glabratum J.F.Maxwell"
 ]
}

 The dataset includes 7 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0034146-240229165702484/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.wercvg
title: Occurrence Download

description: A dataset containing 10046 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "TaxonKey is Asplenium onopteris L.",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 10046 records from 74 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027731-180131172636756/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.mnk6fp
title: Occurrence Download

description: A dataset containing 287 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Astrophytum asterias (Zucc.) Lem."
 ]
}

 The dataset includes 287 records from 31 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0144666-240321170329656/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.un78kg
title: Occurrence Download

description: A dataset containing 709 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Hexasepalum teres (Walter) J.H.Kirkbr.",
 "BasisOfRecord is one of (Specimen)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Continent is North America"
 ]
}

 The dataset includes 709 records from 18 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0167447-200613084148143/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.wjfr5c
title: Occurrence Download

description: A dataset containing 54 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Astragalus moellendorffii Bunge ex Maxim."
 ]
}

 The dataset includes 54 records from 9 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0034112-240229165702484/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.beerxj
title: Occurrence Download

description: A dataset containing 5773 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "or" : [
 "BasisOfRecord is Specimen",
 "BasisOfRecord is Human Observation"
 ]
 },
 {
 "or" : [
 "Country is France",
 "Country is Spain"
 ]
 },
 "Geometry POLYGON((-0.47681 41.97437,3.80566 41.68652,1.46558 44.02222,-1.41724 43.38062,-0.47681 41.97437))",
 "HasCoordinate is true",
 "TaxonKey is Abies alba Mill.",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 5773 records from 39 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027731-190415153152247/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.