cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15156/bio/sh1064683.10fu
title: SH1064683.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064684.10fu
title: SH1064684.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064687.10fu
title: SH1064687.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064688.10fu
title: SH1064688.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064689.10fu
title: SH1064689.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064690.10fu
title: SH1064690.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064696.10fu
title: SH1064696.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.15156/bio/sh1064701.10fu
title: SH1064701.10FU

description: UNITE provides a unified way for delimiting, identifying, communicating, and working with DNA-based Species Hypotheses (SH). All fungal ITS sequences in the international nucleotide sequence databases are clustered to approximately the species level by applying a set of dynamic distance values (<0.5 - 3.0%). All species hypotheses are given a unique, stable name in the form of a DOI, and their taxonomic and ecological annotations are verified through distributed, web-based third-party annotation efforts. SHs are connected to a taxon name and its classification as far as possible (phylum, class, order, etc.) by taking into account identifications for all sequences in the SH. An automatically or manually designated sequence is chosen to represent each such SH. These sequences are released (https://unite.ut.ee/repository.php) for use by the scientific community in, for example, local sequence similarity searches and next-generation sequencing analysis pipelines. The system and the data are updated automatically as the number of public fungal ITS sequences grows.
DOI: 10.5281/zenodo.14231083
title: Geomag data
DOI: 10.5281/zenodo.14544557
title: Geomag data
DOI: 10.15468/dl.52eacv
title: Occurrence Download

description: A dataset containing 1070 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Pennisetum villosum Fresen.)",
 "BasisOfRecord is one of (Machine Observation, Human Observation, Observation, Literature Occurrence)",
 "HasCoordinate is true"
 ]
}

 The dataset includes 1070 records from 20 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000872-250227182430271/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.det429
title: Occurrence Download

description: A dataset containing 35395 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Brazil, Argentina)",
 "TaxonKey is Anhinga anhinga (Linnaeus, 1766)",
 "Year 1000-2024"
 ]
}

 The dataset includes 35395 records from 39 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000871-250227182430271/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.cfqpdc
title: Occurrence Download

description: A dataset containing 79 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Dioscorea birmanica Prain & Burkill"
 ]
}

 The dataset includes 79 records from 15 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000873-250227182430271/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.xuhzgn
title: Occurrence Download

description: A dataset containing 1531 species occurrences available in GBIF matching the query:
{"type":"and","predicates":[{"type":"in","key":"LICENSE","values":["CC0 1.0","CC-BY 4.0","CC0_1_0","CC_BY_4_0"],"matchCase":false},{"type":"equals","key":"MEDIA_TYPE","value":"StillImage","matchCase":false},{"type":"equals","key":"TAXON_KEY","value":"5341270","matchCase":false}]}

 The dataset includes 1531 records from 39 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000874-250227182430271/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.bxmwp7
title: Occurrence Download

description: A dataset listing the 22 species recorded in GBIF matching the query:
{
 "and" : [
 "DatasetKey is Butterfly distribution records for the UK from Butterfly Conservation, up to 2019",
 "Geometry POLYGON((-1.7 54.9,-1.6 54.9,-1.6 55,-1.7 55,-1.7 54.9))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "Year 2015-2015"
 ]
}

 The dataset's 22 records were derived from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000890-250227182400228/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.27100854
title: Clastic injectites and seismic-induced liquefaction in latest Quaternary travertine deposits (Serre di Rapolano, Italy)

description: The liquefaction and consequent injection of clastic dykes (injectites) is often associated with the occurrence of large earthquakes. Injectites are most documented in thick unconsolidated sedimentary sequences and less commonly in rocks as a result of localized clastic mud overpressure due to earthquake-induced shaking. This paper documents near-surface clastic dykes injected into Middle-Late Pleistocene travertine deposits following repeated seismic events. The novelty is that there is a clear relationship between the development of the injectites and the activity of seismogenic faults that cut the entire body of the travertine, deposited at least at 45.5 ± 8.5 ka, and the topographic surface. The clastic slurry, derived from the fluidization of silty-sandy continental deposits at the base of, or intercalated with the travertine body, was in geometric connection with the faults. When this occurred, the over-pressured slurry was injected into the fault zone, filling the fractures and assisting their development by over-pressure hydrofracturing and counteracting the frictional forces on the fault. This evidence, in addition to documenting another case of liquefaction and associated emplacement of clastic dykes, has a twofold significance: i) it records the effects of clastic dykes intruded at very shallow depths, up to the surface, within a capable fault zone; ii) it documents a polyphase injection of clastic material into travertine deposits, never before described, induced by repeated liquefaction phenomena following major seismic events, thus highlighting and reinforcing the importance of travertine for the study of active tectonics and earthquake studies.
DOI: 10.6084/m9.figshare.27100854.v1
title: Clastic injectites and seismic-induced liquefaction in latest Quaternary travertine deposits (Serre di Rapolano, Italy)

description: The liquefaction and consequent injection of clastic dykes (injectites) is often associated with the occurrence of large earthquakes. Injectites are most documented in thick unconsolidated sedimentary sequences and less commonly in rocks as a result of localized clastic mud overpressure due to earthquake-induced shaking. This paper documents near-surface clastic dykes injected into Middle-Late Pleistocene travertine deposits following repeated seismic events. The novelty is that there is a clear relationship between the development of the injectites and the activity of seismogenic faults that cut the entire body of the travertine, deposited at least at 45.5 ± 8.5 ka, and the topographic surface. The clastic slurry, derived from the fluidization of silty-sandy continental deposits at the base of, or intercalated with the travertine body, was in geometric connection with the faults. When this occurred, the over-pressured slurry was injected into the fault zone, filling the fractures and assisting their development by over-pressure hydrofracturing and counteracting the frictional forces on the fault. This evidence, in addition to documenting another case of liquefaction and associated emplacement of clastic dykes, has a twofold significance: i) it records the effects of clastic dykes intruded at very shallow depths, up to the surface, within a capable fault zone; ii) it documents a polyphase injection of clastic material into travertine deposits, never before described, induced by repeated liquefaction phenomena following major seismic events, thus highlighting and reinforcing the importance of travertine for the study of active tectonics and earthquake studies.
DOI: 10.6084/m9.figshare.27160565
title: Petrogenesis of ultramafic rocks from the Neoproterozoic Bou Azzer Ophiolite (Morocco): new insights into a long-standing geodynamic question

description: The Neoproterozoic Bou Azzer Ophiolite, located in the Pan-African orogen of the Anti-Atlas, Morocco, exposes a well-preserved mantle section of the ophiolitic sequence. Although ultramafic rocks are the most common rock types in the sequence, they have received less attention in previous studies. In this work, we investigate the petrogenesis of these ultramafic rocks in detail, including their petrology, mineralogy, and whole rock geochemistry. The mineral assemblages are mainly formed by antigorite with minor lizardite, chlorite, and accessory Cr-spinel. The only preserved primary mantle mineral is Cr-spinel, which shows unaltered cores with Cr# between 0.61 and 0.71 and alteration rims to ferrian chromite and magnetite. Whole rock analyses indicate almost total serpentinization and, locally, strong carbonation (mass loss of ignition between 11.94 and 22.20 wt%). The non-carbonated samples preserve protolith signatures, with decreased MgO/SiO<sub>2</sub> suggesting metasomatic processes related to serpentinization. Immobile trace elements compare well with fore-arc peridotites, while melting modelling indicates intense and polyphasic melting events. We propose polyphase melting in a subduction-initiation setting, with a first stage of 14–23% anhydrous melting, forming fore-arc basalts, and a second stage of 15–25% melting with 1 wt% H<sub>2</sub>O, forming boninites. The Bou Azzer ultramafic rocks represent the fore-arc region of a supra-subduction zone, challenging previous interpretations that suggested a back-arc position.
DOI: 10.6084/m9.figshare.27160565.v1
title: Petrogenesis of ultramafic rocks from the Neoproterozoic Bou Azzer Ophiolite (Morocco): new insights into a long-standing geodynamic question

description: The Neoproterozoic Bou Azzer Ophiolite, located in the Pan-African orogen of the Anti-Atlas, Morocco, exposes a well-preserved mantle section of the ophiolitic sequence. Although ultramafic rocks are the most common rock types in the sequence, they have received less attention in previous studies. In this work, we investigate the petrogenesis of these ultramafic rocks in detail, including their petrology, mineralogy, and whole rock geochemistry. The mineral assemblages are mainly formed by antigorite with minor lizardite, chlorite, and accessory Cr-spinel. The only preserved primary mantle mineral is Cr-spinel, which shows unaltered cores with Cr# between 0.61 and 0.71 and alteration rims to ferrian chromite and magnetite. Whole rock analyses indicate almost total serpentinization and, locally, strong carbonation (mass loss of ignition between 11.94 and 22.20 wt%). The non-carbonated samples preserve protolith signatures, with decreased MgO/SiO<sub>2</sub> suggesting metasomatic processes related to serpentinization. Immobile trace elements compare well with fore-arc peridotites, while melting modelling indicates intense and polyphasic melting events. We propose polyphase melting in a subduction-initiation setting, with a first stage of 14–23% anhydrous melting, forming fore-arc basalts, and a second stage of 15–25% melting with 1 wt% H<sub>2</sub>O, forming boninites. The Bou Azzer ultramafic rocks represent the fore-arc region of a supra-subduction zone, challenging previous interpretations that suggested a back-arc position.
DOI: 10.6084/m9.figshare.27084191
title: Mid-to-late Cenozoic tectonostratigraphic archives of the Qingshuihe Basin, NW China: tracing northeastward stepwise growth of the Tibetan Plateau

description: The detailed sedimentary sequence and tectonic deformation characteristics of the Qingshuihe Basin and its surrounding areas in the northeastern margin of the Tibetan Plateau have provided significant insights into the stages and intensity of lateral orogenic plateau expansion during the Mid-to-late Cenozoic. Several key unconformities and a tectonically induced river terrace have been identified, shedding light on the timing, scale, and tectonic response of the Tibetan Plateau’s growth into northwestern China. The identified unconformities include the ~ 16.5 Ma parallel unconformity (U<sub>1</sub>) between the Qingshuiying and Zhangenpu formations, the ~ 7.6 Ma slight-angular unconformity (U<sub>2</sub>) between the Zhangenpu and Ganhegou formations, the ~ 2.77–1.04 Ma slight- to high-angular unconformity (U<sub>3</sub>) between the Ganhegou and Yumen formations, and the ~ 0.135 Ma high-angular unconformity (U<sub>4</sub>) between the Yumen and Salawusu formations. A ~ 5–4 ka Holocene river terrace of the Qingshuihe River has also been identified. These unconformities and the river terrace provide evidence for a stepwise northeastward expansion model of the Tibetan Plateau. The U<sub>1</sub> disconformity signifies the outward expansion of the orogenic plateau into its northeastern margin through uplift rather than shortening, possibly subsequent to the removal of the mantle lithosphere. The angular unconformities U<sub>2</sub>, U<sub>3</sub>, and U<sub>4</sub> indicate synchronous crustal shortening across the Tibetan region and its northeastern margin, with U<sub>3</sub> representing the most intense lateral expansion of the plateau. The Holocene river terrace represents the most recent tectonic event associated with the northeastward growth of the Tibetan Plateau in the study area, shaping modern landforms and topography.
DOI: 10.6084/m9.figshare.27084191.v1
title: Mid-to-late Cenozoic tectonostratigraphic archives of the Qingshuihe Basin, NW China: tracing northeastward stepwise growth of the Tibetan Plateau

description: The detailed sedimentary sequence and tectonic deformation characteristics of the Qingshuihe Basin and its surrounding areas in the northeastern margin of the Tibetan Plateau have provided significant insights into the stages and intensity of lateral orogenic plateau expansion during the Mid-to-late Cenozoic. Several key unconformities and a tectonically induced river terrace have been identified, shedding light on the timing, scale, and tectonic response of the Tibetan Plateau’s growth into northwestern China. The identified unconformities include the ~ 16.5 Ma parallel unconformity (U<sub>1</sub>) between the Qingshuiying and Zhangenpu formations, the ~ 7.6 Ma slight-angular unconformity (U<sub>2</sub>) between the Zhangenpu and Ganhegou formations, the ~ 2.77–1.04 Ma slight- to high-angular unconformity (U<sub>3</sub>) between the Ganhegou and Yumen formations, and the ~ 0.135 Ma high-angular unconformity (U<sub>4</sub>) between the Yumen and Salawusu formations. A ~ 5–4 ka Holocene river terrace of the Qingshuihe River has also been identified. These unconformities and the river terrace provide evidence for a stepwise northeastward expansion model of the Tibetan Plateau. The U<sub>1</sub> disconformity signifies the outward expansion of the orogenic plateau into its northeastern margin through uplift rather than shortening, possibly subsequent to the removal of the mantle lithosphere. The angular unconformities U<sub>2</sub>, U<sub>3</sub>, and U<sub>4</sub> indicate synchronous crustal shortening across the Tibetan region and its northeastern margin, with U<sub>3</sub> representing the most intense lateral expansion of the plateau. The Holocene river terrace represents the most recent tectonic event associated with the northeastward growth of the Tibetan Plateau in the study area, shaping modern landforms and topography.