cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25549/inscriptifact-ouc110597239
title: Persepolis Fortification Aramaic Text 372, PFAT 372

description: [Text Description:] Administrative text with illegible seal. ❧ [Text or Publication Number Note:] PFAT 372, Bowman 372 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription. Illegible seal impressions on obverse, reverse.
DOI: 10.25549/inscriptifact-ouc110597272
title: Persepolis Fortification Aramaic Text 373, PFAT 373

description: [Text Description:] Administrative text with seals PFS 1098; PFS 0017. ❧ [Text or Publication Number Note:] PFAT 373, Bowman 373 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription.Seal impressions PFS 1098 on obverse, upper edge, reverse, bottom edge; PFS 0017 on flat edge.
DOI: 10.25549/inscriptifact-ouc110597236
title: Persepolis Fortification Aramaic Text 372, PFAT 372

description: [Text Description:] Administrative text with illegible seal. ❧ [Text or Publication Number Note:] PFAT 372, Bowman 372 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription. Illegible seal impressions on obverse, reverse.
DOI: 10.25549/inscriptifact-ouc110597265
title: Persepolis Fortification Aramaic Text 373, PFAT 373

description: [Text Description:] Administrative text with seals PFS 1098; PFS 0017. ❧ [Text or Publication Number Note:] PFAT 373, Bowman 373 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription.Seal impressions PFS 1098 on obverse, upper edge, reverse, bottom edge; PFS 0017 on flat edge.
DOI: 10.25549/inscriptifact-ouc110597235
title: Persepolis Fortification Aramaic Text 372, PFAT 372

description: [Text Description:] Administrative text with illegible seal. ❧ [Text or Publication Number Note:] PFAT 372, Bowman 372 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription. Illegible seal impressions on obverse, reverse.
DOI: 10.25549/inscriptifact-ouc110597251
title: Persepolis Fortification Aramaic Text 373, PFAT 373

description: [Text Description:] Administrative text with seals PFS 1098; PFS 0017. ❧ [Text or Publication Number Note:] PFAT 373, Bowman 373 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription.Seal impressions PFS 1098 on obverse, upper edge, reverse, bottom edge; PFS 0017 on flat edge.
DOI: 10.25549/inscriptifact-ouc110597223
title: Persepolis Fortification Aramaic Text 372, PFAT 372

description: [Text Description:] Administrative text with illegible seal. ❧ [Text or Publication Number Note:] PFAT 372, Bowman 372 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription. Illegible seal impressions on obverse, reverse.
DOI: 10.25549/inscriptifact-ouc110600189
title: Persepolis Fortification Anepigraphic Tablet 2156.101, PFAnep 2156.101

description: [Text Description:] Administrative text with seals PFUTS 0018* ❧ [Text or Publication Number Note:] PFAnep 2156.101, PFUT 2156-101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impression PFUTS 0018* on obverse, upper edge, reverse, bottom edge, flat edge. ❧ [Physical Object Note:] Damage on round edge.
DOI: 10.25549/inscriptifact-ouc110601139
title: Persepolis Fortification Aramaic Text 428, PFAT 428

description: [Text Description:] Administrative text with seals PFATS 0044 ❧ [Text or Publication Number Note:] PFAT 428, Bowman 428 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Aramaic ❧ [Physical Object Description:] Clay tablet with ink inscription. Seal impression PFATS 0044 on obverse, reverse, flat edge.
DOI: 10.15468/dl.8w8wtm
title: Occurrence Download

description: A dataset containing 1859765888 species occurrences available in GBIF matching the query:
{
 "Year" : [
 "1992-2022"
 ]
}

 The dataset includes 1859765888 records from 36039 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0105314-220831081235567/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.vr4g9x
title: Occurrence Download

description: A dataset containing 5710 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Specimen",
 "OccurrenceStatus is Present",
 "TaxonKey is Schlegeliaceae"
 ]
}

 The dataset includes 5710 records from 173 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015361-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.5bzmws
title: Occurrence Download

description: A dataset containing 331 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Argentina, Chile)",
 "TaxonKey is Schinus montana (Phil.) Engl."
 ]
}

 The dataset includes 331 records from 30 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015365-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.9mw37b
title: Occurrence Download

description: A dataset containing 937 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Specimen",
 "OccurrenceStatus is Present",
 "TaxonKey is Sciadopityaceae"
 ]
}

 The dataset includes 937 records from 168 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015363-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.f6prmk
title: Occurrence Download

description: A dataset containing 11065 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Specimen",
 "OccurrenceStatus is Present",
 "TaxonKey is Schoepfiaceae"
 ]
}

 The dataset includes 11065 records from 354 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015362-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.8y3em3
title: Occurrence Download

description: A dataset containing 129466 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Rattus fuscipes (Waterhouse, 1839)"
 ]
}

 The dataset includes 129466 records from 56 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015357-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.qkx2k7
title: Occurrence Download

description: A dataset containing 582171 species occurrences available in GBIF matching the query:
{
 "DatasetKey" : [
 "is Insect Species Occurrence Data from Multiple Projects Worldwide with Focus on Bees and Wasps in North America"
 ]
}

 The dataset includes 582171 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015364-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.3wmr5r
title: Occurrence Download

description: A dataset containing 262 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Chile, Argentina)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Schinus montana (Phil.) Engl."
 ]
}

 The dataset includes 262 records from 19 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015368-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15151/esrf-es-2110593915
title: The Israeli BAG

description: This Summary will only portray a very limited scope of the BAG proposal due to its size and more information will be available in the Global Summary. We plan establish a comprehensive structural narrative for the assembly and entry of viruses from the Bunyavirales family using X-ray crystallography, biophysics, biochemistry, and molecular virology. Using X-ray crystallography to obtain the 3D structure of GN and GC in different conformations and from different bunyavituses. We will pursue a structure of GN or GC bound to a neutralizing antibody to obtain new data for vaccine design. In the SAXS arena, we plan to continue the study on MT (microtubules) and expand the experiments with different nucleotide type and concentrations, (GTP, GDP, GMPCPP, and GMPPCP, GTP-gammaS). We will perform at selected points SEC-SAXS experiments in the presence of full-length tau (4RL). Our preliminary data revealed that 4RL promote MT assembly at 36C and of single tubulin rings at low temperatures.
DOI: 10.6084/m9.figshare.28529610
title: Geochemical, U–Pb geochronological, and Hf isotopic characterisation and geological significance of late Caledonian granites in Gushan area of Dagelegou, East Kunlun, China

description: The East Kunlun orogenic belt, located in the northeastern part of the Qinghai–Tibet Plateau, is distinguished by the widespread distribution of Phanerozoic granites. However, the late evolution of the proto-Tethys remains controversial. In this study, detailed field observations, petrography, geochemistry, zircon U–Pb age, and Hf isotope analyses were performed on the Gushan granites (alkali-feldspar granite and syenogranite) from the Dagele area. This research establishes the formation age and petrogenesis of the granites and discusses the late Caledonian tectonic background of the East Kunlun Orogenic Belt. The laser ablation inductively coupled plasma mass spectrometry zircon data indicate that the Gushan granites range in age from 423 to 422 Ma, assigning them to the late Silurian. Geochemical analyses reveal that the Gushan granites exhibit high K<sub>2</sub>O, FeO/MgO, 1000Ga/Al, and w(Zr + Nb + Ce + Y) values, low Al<sub>2</sub>O<sub>3</sub> and CaO, enrichment in LILE and REE, and pronounced depletion in Sr, Ba, and Eu. The zircon saturation temperatures for syenogranite range from 814 to 847 °C (average temperature 830 °C), while those for alkali-feldspar granite range from 794–849 °C (average temperature 820 °C), categorising them as A2-type granite of the high potassium calc-alkaline series. The εHf<sub>(t)</sub> values range from −0.2 to 2.6, predominantly positive, as demonstrated by the Hf isotope analysis of zircon. A two-stage model age (t<sub>DM2</sub>) spans 1262–1080 Ma, suggesting the granite source is primarily a newly formed basaltic crust with contamination from an ancient silicon–aluminium crust. Tectonic discrimination diagrams of trace elements and their characteristic ratios indicate that the Gushan granites formed during the post-orogenic extension stage of the late Silurian East Kunlun orogenic cycle. Accordingly, it is proposed that the latest closure of the Proto-Tethys Ocean occurred no later than the late Silurian, as opposed to the Early Devonian. The age of the Gushan syenogranite in the Dagelegou area of the East Kunlun is 419.0 ± 5.6 Ma and that of the alkali-feldspar granite 423 ± 5.2 Ma. The Gushan granites have typical A-type granite characteristics and belong to A2 type. The high Rb/Sr and Rb/Nb ratios, and zircon εHf<sub>(t)</sub> values suggest that the source area of the granites is a new basaltic crust with an ancient aluminosilicate crustal contamination. In this area, the closure time for the Proto-Tethys Ocean is late Silurian.
DOI: 10.6084/m9.figshare.28529610.v1
title: Geochemical, U–Pb geochronological, and Hf isotopic characterisation and geological significance of late Caledonian granites in Gushan area of Dagelegou, East Kunlun, China

description: The East Kunlun orogenic belt, located in the northeastern part of the Qinghai–Tibet Plateau, is distinguished by the widespread distribution of Phanerozoic granites. However, the late evolution of the proto-Tethys remains controversial. In this study, detailed field observations, petrography, geochemistry, zircon U–Pb age, and Hf isotope analyses were performed on the Gushan granites (alkali-feldspar granite and syenogranite) from the Dagele area. This research establishes the formation age and petrogenesis of the granites and discusses the late Caledonian tectonic background of the East Kunlun Orogenic Belt. The laser ablation inductively coupled plasma mass spectrometry zircon data indicate that the Gushan granites range in age from 423 to 422 Ma, assigning them to the late Silurian. Geochemical analyses reveal that the Gushan granites exhibit high K<sub>2</sub>O, FeO/MgO, 1000Ga/Al, and w(Zr + Nb + Ce + Y) values, low Al<sub>2</sub>O<sub>3</sub> and CaO, enrichment in LILE and REE, and pronounced depletion in Sr, Ba, and Eu. The zircon saturation temperatures for syenogranite range from 814 to 847 °C (average temperature 830 °C), while those for alkali-feldspar granite range from 794–849 °C (average temperature 820 °C), categorising them as A2-type granite of the high potassium calc-alkaline series. The εHf<sub>(t)</sub> values range from −0.2 to 2.6, predominantly positive, as demonstrated by the Hf isotope analysis of zircon. A two-stage model age (t<sub>DM2</sub>) spans 1262–1080 Ma, suggesting the granite source is primarily a newly formed basaltic crust with contamination from an ancient silicon–aluminium crust. Tectonic discrimination diagrams of trace elements and their characteristic ratios indicate that the Gushan granites formed during the post-orogenic extension stage of the late Silurian East Kunlun orogenic cycle. Accordingly, it is proposed that the latest closure of the Proto-Tethys Ocean occurred no later than the late Silurian, as opposed to the Early Devonian. The age of the Gushan syenogranite in the Dagelegou area of the East Kunlun is 419.0 ± 5.6 Ma and that of the alkali-feldspar granite 423 ± 5.2 Ma. The Gushan granites have typical A-type granite characteristics and belong to A2 type. The high Rb/Sr and Rb/Nb ratios, and zircon εHf<sub>(t)</sub> values suggest that the source area of the granites is a new basaltic crust with an ancient aluminosilicate crustal contamination. In this area, the closure time for the Proto-Tethys Ocean is late Silurian.
DOI: 10.6084/m9.figshare.28719807
title: Occurrence and petrogenesis of diverse S-type granites in an extensional tectonic setting: a case study from the Wongwibinda Complex, eastern Australia

description: The high-temperature–low-pressure (HTLP) Wongwibinda Metamorphic Complex (WMC) hosts four distinct types of early Permian S-type granitoids belonging, or related, to the Hillgrove Supersuite. We use field relationships, age data and petrogenetic modelling to determine the petrogenesis of these granitoid types. Biotite-only bearing granitoids are the most voluminous (∼50% of the WMC area). A newly characterised second type (&lt;1% of the WMC), here defined as the Wongwibinda monzogranite, has nearly equal proportions of muscovite and biotite, and a distinct chemical signature. The third and fourth types (&lt;1% of the WMC) include pegmatite dykes and a garnet-bearing leucogranite. THERMOCALC modelling of water-fluxed and dehydration partial melting of local metasedimentary rock compositions indicates that the biotite-only granitoids are consistent with crustal melts produced by 30–40% dehydration partial melting of accretionary complex metasedimentary rocks at 6–9 kbar, with an admixture of ∼30% mafic magma. In contrast, the Wongwibinda monzogranite is a nearly pure S-type granite with its composition influenced by assimilated migmatite xenoliths. One viable model for its geochemistry involves a mix of 45% water-fluxed 5–10% partial melt of metasedimentary rocks at 3–6 kbar, 65% assimilated local migmatites and inclusion of 10% residual biotite following the extraction of 20% haplogranite melt, although alternative scenarios are plausible. The leucogranite can be modelled through both dehydration and water-fluxed melting of metasedimentary rocks at 3–6 kbar, while the pegmatite composition is consistent with 5% water-fluxed or dehydration partial melts at 3 kbar. It is plausible that the pegmatites, leucogranite and Wongwibinda monzogranite formed coevally with peak metamorphism in the complex. In contrast, the emplacement of the biotite-only Hillgrove Supersuite plutons occurred in the later stages of thermal perturbation, as melts from the deep crust ascended <i>via</i> the Wongwibinda Shear Zone. Small volumes of two-mica Wongwibinda monzogranite type granitoids are commonly associated with HTLP metamorphism in extensional tectonic settings. Four granitoid types are recognised within the WMC. One is newly named and described. Petrogenetic modelling and isotope data indicate that three are pure S-types formed from local metasedimentary rocks. The most voluminous plutons are concluded to be a mix of S-type melts with minor mafic magma.
DOI: 10.6084/m9.figshare.28571042
title: Mixed volcanic and hydrothermal origin of siliceous rocks in a volcanic lake in the Santanghu Basin, NW China

description: The siliceous rock is formed by authigenic quartz and records crucial geological information on the basin’s paleogeography, paleoclimate and paleotectonics. The siliceous rocks in the Lucaogou Formation are widely developed in tight oil reservoirs composed of fine-grained sedimentary rocks and occur as lamina, lenses and bands. However, there is little research on the siliceous rocks in this area, and the understanding of their formation mechanism and processes is still lacking. Two types of siliceous rocks were selected for petrological, mineralogical, <i>in situ</i> major, and trace, and silicon isotopic analysis to explore their source and origin. The siliceous lenses consist of anhedral microcrystalline quartz distributed in tuffaceous shales with a soft-deformation sedimentary structure, indicating a syn-depositional origin. The siliceous phenocrysts, which are composed of quartz, dolomite and smectite, are sand-sized, angular and irregular-shaped occurring in tuffaceous dolostones with a porphyritic texture and normal graded bedding suggesting an origin of the subaqueous explosion as pyroclastic flow. The siliceous lenses show positive Eu anomalies (Eu/Eu* = 1.29–1.65) and a wide range in δ<sup>30</sup>Si values (–0.81 to −0.06‰ deviation from the NBS28 standard), indicating chemical precipitation of hydrothermal fluids. At the same time, the siliceous phenocrysts have a narrow spread in δ<sup>30</sup>Si values (0.30–0.69‰) with weak positive Eu anomalies (Eu/Eu* = 0.84–1.42) and weak negative Ce anomalies (Ce/Ce* = 0.87–1.02), which are interpreted as hydrothermal metasomatism. A high-pH alkaline lake environment with high temperatures and pressures brought by mantle-derived magmatic fluids are the controlling factors for the formation of siliceous rocks. The genetic model of siliceous rocks in the Lucaogou Formation provides an alternative interpretation of the origin of siliceous rocks in the study area and lays a good foundation for reconstructing the basin’s paleoenvironment. The siliceous rocks in the Lucaogou Formation have a mixed volcanic and hydrothermal origin. The siliceous rocks are formed by a high-pH alkaline lake environment and local high temperatures and pressures from mantle-derived magmatic fluids. The depositional mechanism of the siliceous rocks provides crucial information for reconstructing the paleoenvironment of the whole basin.
DOI: 10.6084/m9.figshare.28571042.v1
title: Mixed volcanic and hydrothermal origin of siliceous rocks in a volcanic lake in the Santanghu Basin, NW China

description: The siliceous rock is formed by authigenic quartz and records crucial geological information on the basin’s paleogeography, paleoclimate and paleotectonics. The siliceous rocks in the Lucaogou Formation are widely developed in tight oil reservoirs composed of fine-grained sedimentary rocks and occur as lamina, lenses and bands. However, there is little research on the siliceous rocks in this area, and the understanding of their formation mechanism and processes is still lacking. Two types of siliceous rocks were selected for petrological, mineralogical, <i>in situ</i> major, and trace, and silicon isotopic analysis to explore their source and origin. The siliceous lenses consist of anhedral microcrystalline quartz distributed in tuffaceous shales with a soft-deformation sedimentary structure, indicating a syn-depositional origin. The siliceous phenocrysts, which are composed of quartz, dolomite and smectite, are sand-sized, angular and irregular-shaped occurring in tuffaceous dolostones with a porphyritic texture and normal graded bedding suggesting an origin of the subaqueous explosion as pyroclastic flow. The siliceous lenses show positive Eu anomalies (Eu/Eu* = 1.29–1.65) and a wide range in δ<sup>30</sup>Si values (–0.81 to −0.06‰ deviation from the NBS28 standard), indicating chemical precipitation of hydrothermal fluids. At the same time, the siliceous phenocrysts have a narrow spread in δ<sup>30</sup>Si values (0.30–0.69‰) with weak positive Eu anomalies (Eu/Eu* = 0.84–1.42) and weak negative Ce anomalies (Ce/Ce* = 0.87–1.02), which are interpreted as hydrothermal metasomatism. A high-pH alkaline lake environment with high temperatures and pressures brought by mantle-derived magmatic fluids are the controlling factors for the formation of siliceous rocks. The genetic model of siliceous rocks in the Lucaogou Formation provides an alternative interpretation of the origin of siliceous rocks in the study area and lays a good foundation for reconstructing the basin’s paleoenvironment. The siliceous rocks in the Lucaogou Formation have a mixed volcanic and hydrothermal origin. The siliceous rocks are formed by a high-pH alkaline lake environment and local high temperatures and pressures from mantle-derived magmatic fluids. The depositional mechanism of the siliceous rocks provides crucial information for reconstructing the paleoenvironment of the whole basin.