cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.23265245.v1
title: Additional file 1 of COVID-19-associated impact and post-traumatic stress symptoms 39 days after pandemic in a sample of home-quarantined Chinese college students: the mediating effecting of past stressful events, psychological resilience, and social support

description: Additional file 1.
DOI: 10.5281/zenodo.7979517
title: Co-Occurence Keyword Network

description: A bibliometric map displaying various nodes (word items) and the links by which they are connected conceived on VOSviewer. In this publication, we focused on words indicative of deficit thinking (abnormality, behavior problem, cognitive deficit, cognitive impairment, deficit, disorder, impairment, language difficulty, problem, risk, risk factor and attention problem). This map can be viewed and explored by uploading the attached json file on app.vosviewer.com. Readers can evaluate specific nodes by using the "find" feature on the left-handside menu.
DOI: 10.5281/zenodo.7979516
title: Co-Occurence Keyword Network

description: A bibliometric map displaying various nodes (word items) and the links by which they are connected conceived on VOSviewer. In this publication, we focused on words indicative of deficit thinking (abnormality, behavior problem, cognitive deficit, cognitive impairment, deficit, disorder, impairment, language difficulty, problem, risk, risk factor and attention problem). This map can be viewed and explored by uploading the attached json file on app.vosviewer.com. Readers can evaluate specific nodes by using the "find" feature on the left-handside menu.
DOI: 10.6084/m9.figshare.23265254
title: Additional file 1 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 1: Table S1. Patterns of TLP gene duplication origins and Ka/Ks in seven grass species.
DOI: 10.6084/m9.figshare.23265254.v1
title: Additional file 1 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 1: Table S1. Patterns of TLP gene duplication origins and Ka/Ks in seven grass species.
DOI: 10.6084/m9.figshare.23265257
title: Additional file 2 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 2: Table S2. List of TLP genes in seven studied grass species.
DOI: 10.6084/m9.figshare.23265257.v1
title: Additional file 2 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 2: Table S2. List of TLP genes in seven studied grass species.
DOI: 10.6084/m9.figshare.23265263.v1
title: Additional file 4 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 4: Table S3. Basic statistical details on structural elements of all TLP genes in seven grass species.
DOI: 10.6084/m9.figshare.23265266
title: Additional file 5 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 5: Table S4. Synteny network of TLPs in seven grass species.
DOI: 10.6084/m9.figshare.23265263
title: Additional file 4 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 4: Table S3. Basic statistical details on structural elements of all TLP genes in seven grass species.
DOI: 10.6084/m9.figshare.23265266.v1
title: Additional file 5 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 5: Table S4. Synteny network of TLPs in seven grass species.
DOI: 10.6084/m9.figshare.23265269
title: Additional file 6 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 6: Table S5. Orthologous network of TLPs in seven grass species.
DOI: 10.6084/m9.figshare.23265269.v1
title: Additional file 6 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 6: Table S5. Orthologous network of TLPs in seven grass species.
DOI: 10.6084/m9.figshare.23265272
title: Additional file 7 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 7: Table S6. The cluster of TLP genes in seven grass species obtained using the MCL algorithm.
DOI: 10.6084/m9.figshare.23265272.v1
title: Additional file 7 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 7: Table S6. The cluster of TLP genes in seven grass species obtained using the MCL algorithm.
DOI: 10.6084/m9.figshare.23265275
title: Additional file 8 of Whole-genome and dispersed duplication, including transposed duplication, jointly advance the evolution of TLP genes in seven representative Poaceae lineages

description: Additional file 8: Table S7. Analysis of codon bias of TLP genes in seven grass species.
DOI: 10.15468/dl.rps9tc
title: Occurrence Download

description: A dataset containing 53105 species occurrences available in GBIF matching the query:
{
 "and" : [
 "OccurrenceStatus is Absent",
 "TaxonKey is Diogenidae"
 ]
}

 The dataset includes 53105 records from 30 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0025433-231002084531237/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.10963294
title: Supporting Software Maintenance with Dynamically Generated Document Hierarchies
DOI: 10.5281/zenodo.10963295
title: Supporting Software Maintenance with Dynamically Generated Document Hierarchies
DOI: 10.15468/dl.s4f2mz
title: Occurrence Download

description: A dataset containing 694 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Obolodiplosis robiniae (Haldeman, 1847)"
 ]
}

 The dataset includes 694 records from 16 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0017835-210914110416597/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.keacjc
title: Occurrence Download

description: A dataset containing 8174 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Machine Observation)"
 ]
 }
 },
 "TaxonKey is Zostera noltii Hornem."
 ]
}

 The dataset includes 8174 records from 151 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0025417-231002084531237/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.10963254
title: SmetSearch files
DOI: 10.5281/zenodo.10963255
title: SmetSearch files
DOI: 10.15468/dl.fxuymk
title: Occurrence Download

description: A dataset containing 269560 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Vicia cracca L."
 ]
}

 The dataset includes 269560 records from 721 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004400-171113114016250/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.9mkxxm
title: Occurrence Download

description: A dataset listing the 1040 species recorded in GBIF matching the query:
{
 "and" : [
 {
 "or" : [
 "Geometry POLYGON((100.12 21.04,100.45 21.04,100.45 21.4,100.12 21.4,100.12 21.04))",
 "Geometry POLYGON((-100.34912 21.8615,-100.87097 21.8411,-100.68146 21.30985,-100.17883 21.33032,-100.34912 21.8615))"
 ]
 },
 "HasCoordinate is true",
 "TaxonKey is Tracheophyta",
 "HasGeospatialIssue is false"
 ]
}

 The dataset's 1040 records were derived from 64 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0014872-191105090559680/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.cfn3mm
title: Occurrence Download

description: A dataset containing 251454 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Fratercula arctica (Linnaeus, 1758)"
 ]
}

 The dataset includes 251454 records from 337 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0025418-231002084531237/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.mn74j1
title: Occurrence Download

description: A dataset containing 502 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Lonchura malabarica (Linnaeus, 1758)"
 ]
}

 The dataset includes 502 records from 32 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004400-171219132708484/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.24045642
title: Three episodes of Triassic volcanism in the Eastern Kunlun Orogen, NW China: constraints for evolution of the Palaeo-Tethys Ocean

description: The Eastern Kunlun Orogenic Belt (EKOB), located north of the Qinghai-Tibetan Plateau, recorded voluminous late Palaeozoic – early Mesozoic intermediate-acid volcanic rocks. The tectonic evolution of the Palaeo-Tethys Ocean from initial subduction and final closure and post-collision extension has been hotly debated. This study examines the petrogenesis of Palaeozoic to Early Mesozoic volcanic rocks at six locations: Xiahe, Elashankou, Jirimai, Harizha, Nagengkangqieer, and Yazigounan. The investigation involves detailed field observations, petrology, zircon U-Pb geochronology, Lu-Hf isotopes, and whole-rock geochemical analysis. The rocks analysed represent three episodic volcanic events. The ca. 257–245 Ma volcanic rocks were derived from magma mixing response to the subduction. The ca. 227–220 Ma highly fractionated I-type volcanics were derived from partial melting of the ancient lower crust, with varying contribution proportions of mantle materials. The ca. 216 Ma A-type volcanic rocks derived from partial melting of the juvenile crust. In this study, using existing regional geological data and spatiotemporal distribution of the magmatic region, combined with our new data, we attempt to propose more rational models to reveal the tectonic evolution of the Palaeo-Tethys Ocean, and we recognize three significant time nodes: (1) Ca. 240 Ma marks the final closure time of the Palaeo-Tethys Ocean. (2) Ca. 230 Ma indicates the vital tectonic regime transition from compression to extension response to slab break-off and continued lithospheric delamination. (3) Ca. 216 Ma mark the beginning of the final stage of orogeny in the EKOB, and mild magmatism lasts to ca. 200 Ma in response to the mountain collapse.
DOI: 10.6084/m9.figshare.24175087
title: Late Mesozoic Tectono-stratigraphic evolution of the Hekimhan Basin and the environs (central eastern Anatolia): implications for the eastern Taurides and Gürün Curl

description: The east-west trending Taurides form a curved area in central eastern Anatolia known as the Gürün Curl. In order to understand the origin of the Gürün Curl and Tauride evolution in general, the results of a new field study of this region have been synthesized together with previously published data. We suggest that the geodynamic evolution of the area began with the likely presence of a Tethys Ocean transform fault. This fault separated the Taurides into the Akdere Sector in the west and the Munzur Sector in the east in the Late Cretaceous. During the late Santonian–early Campanian, ophiolites obducted onto the Munzur Sector, while platform sediments continued to accumulate in the Akdere Sector. This was followed by the development of an Andean-type arc-type magmatism (the Baskil Arc) during the early–middle Campanian in the Munzur Sector. Continued closure of the Tethys led to the collision of the Bitlis Massif in the south of the Munzur Sector in the Campanian. This, in turn, resulted in continental subduction and slab roll-back that was controlled by a Subduction Transform Edge Propagator (STEP) Fault that lay on the original transform fault between the Akdere and Munzur sectors. Because the subducted slab was free at its western corner, the western edge rolled back faster than in the east, leading to an asymmetrical extensional regime on the upper plate that created the late Campanian Hekimhan Basin. While these geodynamic events were taking place in the Munzur Sector, the Akdere Sector was in a platform setting. During the Palaeocene, the Late Mesozoic units of the Akdere Sector began to overthrust on the Hekimhan Basin and the ophiolites. Following the Palaeocene, all these tectonostratigraphic units were covered by Eocene sediments around the Gürün Curl of which the modern appearance was completed by the Miocene to Recent movements along the strike-slip faults.
DOI: 10.6084/m9.figshare.24175087.v1
title: Late Mesozoic Tectono-stratigraphic evolution of the Hekimhan Basin and the environs (central eastern Anatolia): implications for the eastern Taurides and Gürün Curl

description: The east-west trending Taurides form a curved area in central eastern Anatolia known as the Gürün Curl. In order to understand the origin of the Gürün Curl and Tauride evolution in general, the results of a new field study of this region have been synthesized together with previously published data. We suggest that the geodynamic evolution of the area began with the likely presence of a Tethys Ocean transform fault. This fault separated the Taurides into the Akdere Sector in the west and the Munzur Sector in the east in the Late Cretaceous. During the late Santonian–early Campanian, ophiolites obducted onto the Munzur Sector, while platform sediments continued to accumulate in the Akdere Sector. This was followed by the development of an Andean-type arc-type magmatism (the Baskil Arc) during the early–middle Campanian in the Munzur Sector. Continued closure of the Tethys led to the collision of the Bitlis Massif in the south of the Munzur Sector in the Campanian. This, in turn, resulted in continental subduction and slab roll-back that was controlled by a Subduction Transform Edge Propagator (STEP) Fault that lay on the original transform fault between the Akdere and Munzur sectors. Because the subducted slab was free at its western corner, the western edge rolled back faster than in the east, leading to an asymmetrical extensional regime on the upper plate that created the late Campanian Hekimhan Basin. While these geodynamic events were taking place in the Munzur Sector, the Akdere Sector was in a platform setting. During the Palaeocene, the Late Mesozoic units of the Akdere Sector began to overthrust on the Hekimhan Basin and the ophiolites. Following the Palaeocene, all these tectonostratigraphic units were covered by Eocene sediments around the Gürün Curl of which the modern appearance was completed by the Miocene to Recent movements along the strike-slip faults.
DOI: 10.15468/dl.zimah9
title: Occurrence Download

description: A dataset containing 3265 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Specimen",
 "HasCoordinate is true",
 "TaxonKey is Asplenium trichomanes subsp. quadrivalens D.E.Mey.",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 3265 records from 78 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031642-191105090559680/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.24045642.v1
title: Three episodes of Triassic volcanism in the Eastern Kunlun Orogen, NW China: constraints for evolution of the Palaeo-Tethys Ocean

description: The Eastern Kunlun Orogenic Belt (EKOB), located north of the Qinghai-Tibetan Plateau, recorded voluminous late Palaeozoic – early Mesozoic intermediate-acid volcanic rocks. The tectonic evolution of the Palaeo-Tethys Ocean from initial subduction and final closure and post-collision extension has been hotly debated. This study examines the petrogenesis of Palaeozoic to Early Mesozoic volcanic rocks at six locations: Xiahe, Elashankou, Jirimai, Harizha, Nagengkangqieer, and Yazigounan. The investigation involves detailed field observations, petrology, zircon U-Pb geochronology, Lu-Hf isotopes, and whole-rock geochemical analysis. The rocks analysed represent three episodic volcanic events. The ca. 257–245 Ma volcanic rocks were derived from magma mixing response to the subduction. The ca. 227–220 Ma highly fractionated I-type volcanics were derived from partial melting of the ancient lower crust, with varying contribution proportions of mantle materials. The ca. 216 Ma A-type volcanic rocks derived from partial melting of the juvenile crust. In this study, using existing regional geological data and spatiotemporal distribution of the magmatic region, combined with our new data, we attempt to propose more rational models to reveal the tectonic evolution of the Palaeo-Tethys Ocean, and we recognize three significant time nodes: (1) Ca. 240 Ma marks the final closure time of the Palaeo-Tethys Ocean. (2) Ca. 230 Ma indicates the vital tectonic regime transition from compression to extension response to slab break-off and continued lithospheric delamination. (3) Ca. 216 Ma mark the beginning of the final stage of orogeny in the EKOB, and mild magmatism lasts to ca. 200 Ma in response to the mountain collapse.
DOI: 10.6084/m9.figshare.24162708.v1
title: Neoarchaean DTTGs from the Dunhuang Block, Tarim Craton: insights into petrogenesis and crust–mantle interactions

description: Earth’s first continental crust is formed by Archaean and mainly consisted of tonalite–trondhjemite–granodiorite with a small amount of diorites (DTTGs), which has an essential role in probing early crust–mantle dynamic regime and in understanding the formation mechanism of continental crust. Here, we present zircon U‒Pb dating and Lu‒Hf isotopes, whole-rock geochemistry, and petrography on DTTGs rocks in the Dunhuang Block. Three episodes of DTTGs were emplaced circa 2.67 Ga, 2.60 Ga, and 2.50 Ga. The circa 2.67 Ga TTGs exhibit high SiO<sub>2</sub> contents (68.14–71.70 wt%), low MgO contents (0.65–1.31 wt%), and high ratios of (La/Yb)<sub>N</sub> (146 on average), with their enriched Nd-Hf isotopes [<sub>ƐHf</sub> (t) = -5.48–3.19 and <sub>ƐNd</sub> (t) = -5.77–0.53], indicating origination from partial melting of amphibolites at thickened lower crust. In contrast, the circa 2.60 Ga transitional TTGs exhibit relatively high MgO contents (2.80–3.39 wt%), flat REE (Rare earth element) patterns with moderate ratios of (La/Yb)<sub>N</sub> (20.49 on average), and dispersed Nd-Hf isotopes [<sub>ƐHf</sub> (t) = -5.48–3.19 and <sub>ƐNd</sub> (t)= −3.99–3.08]. Accordingly, circa 2.60 Ga transitional TTGs melts were produced by partial melting of the shallower crust induced by mantle-derived magma upwelling. The circa 2.50 Ga diorites exhibit low SiO<sub>2</sub> (55.72–59.11 wt%) but high MgO (3.51–4.52 wt%) contents with positive Nd-Hf isotopes [<sub>ƐHf</sub> (t) = -0.16–4.17 and <sub>ƐNd</sub> (t) = 2.00–4.45], suggesting that they originated from partial melting of mantle wedges metasomatized by fluid from subduction slabs. Combined with the detailed petrogenetic studies and crustal thickness variation, we conclude that the complex crust–mantle interaction may be an essential reason for the Neoarchaean diversity of DTTGs from the Dunhuang Block, which experienced prolonged arc accretion before Neoarchaean, followed by delamination between 2.67 and 2.60 Ga and subsequently transitioned to subduction.
DOI: 10.6084/m9.figshare.24218678
title: Tectonic slices of greenschist – epidote blueschist – epidote amphibole schist – garnet epidote amphibole schist from the Nagaland ophiolite complex, NE India: a look into their metamorphic and tectonic evolution

description: Tectonic slices of greenschist – epidote blueschist – epidote amphibole schist – garnet epidote amphibole schist are exposed in the northern part of the NOC. Metamorphic <i>P-T</i> conditions and <i>P-T</i> paths of the garnet epidote amphibole schist and epidote blueschist were determined with the help of pseudosection calculations in the MnNCKFMASHTO system using the software Perple_X. The garnet epidote amphibole schist records a pre-peak metamorphic stage at ~12 kbar and ~360°C in the lawsonite blueschist facies field. Lawsonite and glaucophane are not preserved in the rock and are attributed to progressive metamorphic reactions during prograde metamorphism. The peak metamorphic stage is constrained at ~14 kbar and ~570°C in the hornblende eclogite facies field. Post-peak metamorphism shows slight cooling and decompression from ~550°C and ~13 kbar, possibly down to ~350°C and ~7 kbar in the greenschist facies field. These three metamorphic stages reveal a clockwise metamorphic <i>P-T</i> path of evolution for the garnet epidote amphibole schist. The geotherm at metamorphic peak <i>P-T</i> condition is ~12.5°C/km, which is hotter by ~350°C compared to thermal models of mature subduction zones but shows good agreement with models of warm subduction zones. Therefore, the low geothermal gradient of ~8°C/km during the prograde metamorphism possibly reflects the subduction of cold Neo-Tethyan ocean crust when the temperature conditions of the subduction zone were still warm. The epidote blueschist shows peak metamorphism at ~10 kbar and 380°C with a clockwise <i>P-T</i> path. It indicates metamorphism at a more mature stage of subduction. Buoyancy-driven exhumation along the subduction channel due to the serpentinization of the upper mantle wedge played a vital role in the detachment and exhumation of the tectonic slivers of metamorphic rocks from different depth sections in the northern margin of the NOC.