cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.94jxc4
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Sarda chiliensis (Cuvier, 1832)",
 "Geometry POLYGON((170 20, 170 50, 120 50, 120 20, 170 20))",
 "HasCoordinate is true"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0058467-241126133413365/datasets/export for details.
DOI: 10.7483/opendata.delphi.juyt.u0ga
title: DELPHI simulation data sh_qqps_sa94_2l_c2
DOI: 10.6084/m9.figshare.25211268
title: The geology of Sierra Calderona (SE Iberian Cordillera, Spain), a review. Results of a new 1:25.000 scale geological mapping

description: A new geological mapping of Sierra Calderona (SE Iberian Cordillera) has confirmed the widespread presence of the Muschelkalk M2 unit overlying a ubiquitous Muschelkalk M1 carbonate unit. Thus, the allocation of this range in the Levantine-Balearic Triassic Domain is not justified and a previous assignment of the entire Muschelkalk carbonate succession of this region to the M3 unit is untenable. Evidence of Permo-Triassic extensional tectonics by local unconformities separating Permian and Triassic units and a more widespread unconformity at the base of the Jurassic succession is recorded. Paleogene-Early Neogene compression-related structures associated with the formation of the NW-SE trending Sierra Calderona anticlinorium are scarce, but numerous detachment surfaces within the stratigraphic pile suggest a complex thick-skinned tectonics. The dominant tectonic grain in Sierra Calderona is a Neogene extensional structure with a preferential pattern of blocks stepping down to the coast, which is related to the opening of the Valencia Trough.
DOI: 10.6084/m9.figshare.25211268.v1
title: The geology of Sierra Calderona (SE Iberian Cordillera, Spain), a review. Results of a new 1:25.000 scale geological mapping

description: A new geological mapping of Sierra Calderona (SE Iberian Cordillera) has confirmed the widespread presence of the Muschelkalk M2 unit overlying a ubiquitous Muschelkalk M1 carbonate unit. Thus, the allocation of this range in the Levantine-Balearic Triassic Domain is not justified and a previous assignment of the entire Muschelkalk carbonate succession of this region to the M3 unit is untenable. Evidence of Permo-Triassic extensional tectonics by local unconformities separating Permian and Triassic units and a more widespread unconformity at the base of the Jurassic succession is recorded. Paleogene-Early Neogene compression-related structures associated with the formation of the NW-SE trending Sierra Calderona anticlinorium are scarce, but numerous detachment surfaces within the stratigraphic pile suggest a complex thick-skinned tectonics. The dominant tectonic grain in Sierra Calderona is a Neogene extensional structure with a preferential pattern of blocks stepping down to the coast, which is related to the opening of the Valencia Trough.
DOI: 10.6084/m9.figshare.25658115.v1
title: Geology of the basement rocks of Andorra, central Pyrenees

description: In this work we present a 1:50,000 geological map of the basement rocks of Andorra that is the harmonization of the results of two decades of field work and data analyses in the frame of the 1:25,000 Geological Map of Andorra Project by CENMA–IEA (at present AR + I, Andorra Research + Innovation). The study area lies entirely in the Axial Zone of the Pyrenees, where only late Neoproterozoic and Paleozoic rocks and Quaternary deposits crop out. The map is produced at 1:25,000 scale and Quaternary deposits have been removed, in order to obtain a continuous basement map that can be used as the basis for stratigraphical and structural works. The main results of this work are the publication of new cartographic and structural data, as well as a better understanding of the stratigraphy in this sector.
DOI: 10.7483/opendata.delphi.zxrc.dg1s
title: DELPHI simulation data sh_dswc_b94_2l_c2
DOI: 10.6084/m9.figshare.27094213
title: The geological setting of Matra ore deposit (France): insights from lithostratigraphy and polyphase deformation history

description: Arsenic sulfide mineralization in Matra mine (southern Alpine Corsica) is hosted by two tectonic units belonging to the Schistes Lustrés Complex. Country rocks include a Jurassic ophiolitic sequence and related sedimentary covers, which were metamorphosed. Geological mapping and thin section analysis were used to understand lithostratigraphy and the tectononic-metamorphic history. The polyphase deformation history includes four phases of ductile deformation during the Late Cretaceous–Early Oligocene Alpine orogeny, with associated high-pressure–low-temperature metamorphism culminating in eclogite facies. The post-Alpine phase includes an N–S extensional fault system that controls the movement of ore fluids. In the Matra area, the Santo Pietro di Tenda (ophiolitic sequence and sedimentary covers) and the Upper Castagniccia (sedimentary covers) Units crop out.They were involved in Alpine subduction registering a polyphase deformation and a peak metamorphism recorded in eclogite facies.The post-Alpine, N–S-trending normal fault of Matra hosts As-sulfide mineralization was exploited in the 1900s. In the Matra area, the Santo Pietro di Tenda (ophiolitic sequence and sedimentary covers) and the Upper Castagniccia (sedimentary covers) Units crop out. They were involved in Alpine subduction registering a polyphase deformation and a peak metamorphism recorded in eclogite facies. The post-Alpine, N–S-trending normal fault of Matra hosts As-sulfide mineralization was exploited in the 1900s.
DOI: 10.6084/m9.figshare.27094213.v1
title: The geological setting of Matra ore deposit (France): insights from lithostratigraphy and polyphase deformation history

description: Arsenic sulfide mineralization in Matra mine (southern Alpine Corsica) is hosted by two tectonic units belonging to the Schistes Lustrés Complex. Country rocks include a Jurassic ophiolitic sequence and related sedimentary covers, which were metamorphosed. Geological mapping and thin section analysis were used to understand lithostratigraphy and the tectononic-metamorphic history. The polyphase deformation history includes four phases of ductile deformation during the Late Cretaceous–Early Oligocene Alpine orogeny, with associated high-pressure–low-temperature metamorphism culminating in eclogite facies. The post-Alpine phase includes an N–S extensional fault system that controls the movement of ore fluids. In the Matra area, the Santo Pietro di Tenda (ophiolitic sequence and sedimentary covers) and the Upper Castagniccia (sedimentary covers) Units crop out.They were involved in Alpine subduction registering a polyphase deformation and a peak metamorphism recorded in eclogite facies.The post-Alpine, N–S-trending normal fault of Matra hosts As-sulfide mineralization was exploited in the 1900s. In the Matra area, the Santo Pietro di Tenda (ophiolitic sequence and sedimentary covers) and the Upper Castagniccia (sedimentary covers) Units crop out. They were involved in Alpine subduction registering a polyphase deformation and a peak metamorphism recorded in eclogite facies. The post-Alpine, N–S-trending normal fault of Matra hosts As-sulfide mineralization was exploited in the 1900s.
DOI: 10.6084/m9.figshare.27867704.v1
title: Understanding the nature of landslides through detailed geomorphological mapping on the Sumbing Volcanic Landscape, Java Island, Indonesia

description: A 1:2,500-scale geomorphological map was created to illustrate the landslide characteristics on the southern flank of the Sumbing Volcanic Landscape (SVL), Java Island, Indonesia. High-resolution LiDAR Digital Terrain Model (DTM), Global Navigation Satellite System (GNSS) data, Unmanned Aerial Vehicle (UAV)-based aerial photographs, and field surveys were integrated to enable detailed landform interpretation of post-volcanic mass wasting processes. Landslides were classified by type, activity level, and origin. Additionally, morphometric analysis, including slope and area measurements, was conducted. Through this detailed geomorphological mapping process, it reveals that most recent landslides have developed within relict landslides, which were previously overlooked. It also detects smaller, more hazardous landslides caused by human activities, in addition to those triggered by natural forces. This study represents the first large-scale geomorphological mapping effort integrating high-resolution datasets in Indonesia’s dormant volcanic landscapes. It will enhance understanding of landslide characteristics and will support disaster management strategies.
DOI: 10.7483/opendata.delphi.kbp1.a473
title: DELPHI simulation data sh_hzha03pythia6156tttt_e91.2_m40_m40_c94_2l_c2
DOI: 10.6084/m9.figshare.27867704
title: Understanding the nature of landslides through detailed geomorphological mapping on the Sumbing Volcanic Landscape, Java Island, Indonesia

description: A 1:2,500-scale geomorphological map was created to illustrate the landslide characteristics on the southern flank of the Sumbing Volcanic Landscape (SVL), Java Island, Indonesia. High-resolution LiDAR Digital Terrain Model (DTM), Global Navigation Satellite System (GNSS) data, Unmanned Aerial Vehicle (UAV)-based aerial photographs, and field surveys were integrated to enable detailed landform interpretation of post-volcanic mass wasting processes. Landslides were classified by type, activity level, and origin. Additionally, morphometric analysis, including slope and area measurements, was conducted. Through this detailed geomorphological mapping process, it reveals that most recent landslides have developed within relict landslides, which were previously overlooked. It also detects smaller, more hazardous landslides caused by human activities, in addition to those triggered by natural forces. This study represents the first large-scale geomorphological mapping effort integrating high-resolution datasets in Indonesia’s dormant volcanic landscapes. It will enhance understanding of landslide characteristics and will support disaster management strategies.
DOI: 10.6084/m9.figshare.27257681
title: The geology of the Aracruz pluton (Espírito Santo, Brazil), a Cambrian post-orogenic intrusion in the aftermath of Gondwana amalgamation

description: We present the first geological map of the Aracruz pluton (Espírito Santo, Brazil), which belongs to the late Cambrian post-orogenic suite that intruded the Nova Venécia metapelites and Ediacaran syn-orogenic S-type granites of the Araçuaí belt. Our mapping coupled with airbone magnetic and radiometric observations reveals that the pluton is not regularly zoned. It is composed of porphyric alkali feldspar granites, into which charnockite and quartz-diorite bands intruded as several pulses while the granites were a deforming crystal mush, and an undeformed central norite emplaced when most movement of the host magma had ceased. Steep-dipping concentric magmatic foliation, magmatic foliation parallel to tectonic foliation in the country rock, the noritic core, and the irregular charnockite and quartz-diorite band alignment suggest buoyancy-driven diapirism as emplacement mechanism. The Aracruz pluton is a superb example of mantle-derived post-orogenic intrusion attesting for the production of continental crust during the final stages of a Wylson cycle.
DOI: 10.6084/m9.figshare.27257681.v1
title: The geology of the Aracruz pluton (Espírito Santo, Brazil), a Cambrian post-orogenic intrusion in the aftermath of Gondwana amalgamation

description: We present the first geological map of the Aracruz pluton (Espírito Santo, Brazil), which belongs to the late Cambrian post-orogenic suite that intruded the Nova Venécia metapelites and Ediacaran syn-orogenic S-type granites of the Araçuaí belt. Our mapping coupled with airbone magnetic and radiometric observations reveals that the pluton is not regularly zoned. It is composed of porphyric alkali feldspar granites, into which charnockite and quartz-diorite bands intruded as several pulses while the granites were a deforming crystal mush, and an undeformed central norite emplaced when most movement of the host magma had ceased. Steep-dipping concentric magmatic foliation, magmatic foliation parallel to tectonic foliation in the country rock, the noritic core, and the irregular charnockite and quartz-diorite band alignment suggest buoyancy-driven diapirism as emplacement mechanism. The Aracruz pluton is a superb example of mantle-derived post-orogenic intrusion attesting for the production of continental crust during the final stages of a Wylson cycle.
DOI: 10.7483/opendata.delphi.4phc.4oo3
title: DELPHI simulation data sh_qqps_sa94_2l_b3
DOI: 10.6084/m9.figshare.27098874
title: High-resolution bathymetry coupled with 3D models of hydrothermal vents from opportunistically-acquired imagery: Aurora vent field, Arctic Ocean

description: Active venting at the Aurora hydrothermal field was first located in 2014. In July 2023, the AUV/ROV Nereid Under Ice (NUI) expanded the known size of the Aurora hydrothermal field, discovering 7 ‘black smokers’ together with associated lower-temperature flow. In this study, we present a new high-resolution bathymetric map acquired from NUI which has allowed us to identify morphological features previously undetectable from ship multibeam. All known active vents are aligned along a single 230 m-long ridge, parallel to the Gakkel Ridge strike direction and intersected by a scarp following the general trend of the Lena Trough. The new vents were measured at up to 17 m height from 3D models generated using structure-from-motion techniques applied to opportunistically acquired imaging data collected while in exploration mode. The extent of extinct sulfides present, together with the towering height of vents are consistent with a period of sustained high-temperature venting at Aurora.
DOI: 10.6084/m9.figshare.27098874.v1
title: High-resolution bathymetry coupled with 3D models of hydrothermal vents from opportunistically-acquired imagery: Aurora vent field, Arctic Ocean

description: Active venting at the Aurora hydrothermal field was first located in 2014. In July 2023, the AUV/ROV Nereid Under Ice (NUI) expanded the known size of the Aurora hydrothermal field, discovering 7 ‘black smokers’ together with associated lower-temperature flow. In this study, we present a new high-resolution bathymetric map acquired from NUI which has allowed us to identify morphological features previously undetectable from ship multibeam. All known active vents are aligned along a single 230 m-long ridge, parallel to the Gakkel Ridge strike direction and intersected by a scarp following the general trend of the Lena Trough. The new vents were measured at up to 17 m height from 3D models generated using structure-from-motion techniques applied to opportunistically acquired imaging data collected while in exploration mode. The extent of extinct sulfides present, together with the towering height of vents are consistent with a period of sustained high-temperature venting at Aurora.
DOI: 10.7483/opendata.delphi.op3l.kfo0
title: DELPHI simulation data sh_pythia5720yukatttt_e91.2_m50_c94_2l_c2
DOI: 10.7483/opendata.delphi.qc8v.91a3
title: DELPHI simulation data sh_kk2f4146qqpydcy_e91.25_c94_2l_c2
DOI: 10.6084/m9.figshare.24955538
title: Linosa island: a unique heritage of Mediterranean biodiversity

description: This publication presents a newly created map of the seafloor of Linosa, a volcanic island located in the Sicily Channel (Mediterranean Sea). The seafloor of Linosa was previously surveyed using geophysical and ground-truth data (in 2016 and 2017). Linosa is regarded as a "sentinel area" for alien species and worldwide environmental changes because of its geographical location, making it worthy of particular attention. The predominant habitats found in Linosa have been identified as three priority habitats: Posidonia oceanica meadows, rhodolith beds, and coralligenous habitats, which encompass extensive coral forests. Another crucial environmental indicator is the assemblages of benthic foraminifera, which were previously studied in this area to analyse their correlations with the topography of the seafloor. Hence, all the accessible data was gathered to create a novel comprehensive map of the seabed (at a scale of 1:15,000), with the objective of displaying and highlighting the abundant marine biodiversity of Linosa.
DOI: 10.6084/m9.figshare.24955538.v1
title: Linosa island: a unique heritage of Mediterranean biodiversity

description: This publication presents a newly created map of the seafloor of Linosa, a volcanic island located in the Sicily Channel (Mediterranean Sea). The seafloor of Linosa was previously surveyed using geophysical and ground-truth data (in 2016 and 2017). Linosa is regarded as a "sentinel area" for alien species and worldwide environmental changes because of its geographical location, making it worthy of particular attention. The predominant habitats found in Linosa have been identified as three priority habitats: Posidonia oceanica meadows, rhodolith beds, and coralligenous habitats, which encompass extensive coral forests. Another crucial environmental indicator is the assemblages of benthic foraminifera, which were previously studied in this area to analyse their correlations with the topography of the seafloor. Hence, all the accessible data was gathered to create a novel comprehensive map of the seabed (at a scale of 1:15,000), with the objective of displaying and highlighting the abundant marine biodiversity of Linosa.
DOI: 10.7483/opendata.delphi.63op.x9pp
title: DELPHI simulation data sh_ccdt_b94_2l_c2
DOI: 10.6084/m9.figshare.26348611
title: Measuring postal access and direct delivery services among Native American reservations in Montana and South Dakota

description: Over the past two decades voting by mail has increased. As the COVID-19 pandemic disrupted the 2020 political season, absentee voting increased to over 43% of all votes cast in the November Presidential Election. In recent years, many states have passed laws to limit the scope of absentee voting as necessary to curtail voter fraud. Though no evidence exists that fraud is more likely with mail-in voting, such laws have been found to have a disproportionate impact on some groups of voters more than others. This is true of many Native American communities that often rely on absentee voting. This study will utilize geospatial methods to examine postal realities for Native American on reservations in Montana and South Dakota. By illustrating where postal services are or are not located, a fuller contextual analysis of the issue can be provided. Such methods can enhance current methodologies utilized by political geographers.
DOI: 10.6084/m9.figshare.26348611.v1
title: Measuring postal access and direct delivery services among Native American reservations in Montana and South Dakota

description: Over the past two decades voting by mail has increased. As the COVID-19 pandemic disrupted the 2020 political season, absentee voting increased to over 43% of all votes cast in the November Presidential Election. In recent years, many states have passed laws to limit the scope of absentee voting as necessary to curtail voter fraud. Though no evidence exists that fraud is more likely with mail-in voting, such laws have been found to have a disproportionate impact on some groups of voters more than others. This is true of many Native American communities that often rely on absentee voting. This study will utilize geospatial methods to examine postal realities for Native American on reservations in Montana and South Dakota. By illustrating where postal services are or are not located, a fuller contextual analysis of the issue can be provided. Such methods can enhance current methodologies utilized by political geographers.
DOI: 10.6084/m9.figshare.26502265
title: Comparison of turnout in Italian parliamentary elections: a two-stage affinity propagation approach

description: This paper presents a methodology for temporal contextual analysis of electoral outcomes in the presence of redistricting. Affinity propagation is used to aggregate electoral districts, thus deriving spatial units comparable over electoral waves. The methodology is based on travel-to-work flows and socio-economic aggregated data. Comparability of clusters enables analyses of electoral trends. A map of electoral turnout variation in Italian parliamentary elections held in 2018 and 2022 illustrates the proposed approach.
DOI: 10.6084/m9.figshare.26502265.v2
title: Comparison of turnout in Italian parliamentary elections: a two-stage affinity propagation approach

description: This paper presents a methodology for temporal contextual analysis of electoral outcomes in the presence of redistricting. Affinity propagation is used to aggregate electoral districts, thus deriving spatial units comparable over electoral waves. The methodology is based on travel-to-work flows and socio-economic aggregated data. Comparability of clusters enables analyses of electoral trends. A map of electoral turnout variation in Italian parliamentary elections held in 2018 and 2022 illustrates the proposed approach.
DOI: 10.7483/opendata.delphi.jc4t.bdjz
title: DELPHI simulation data sh_hzha03pythia6156bbtt_e91.2_m70_m04_c94_2l_c2
DOI: 10.7483/opendata.delphi.pyj9.5hh7
title: DELPHI simulation data sh_hzha03pythia6156tttt_e91.2_m6_m40_c94_2l_c2
DOI: 10.7483/opendata.delphi.446e.e8tg
title: DELPHI simulation data sh_hzha03pythia6156bbtt_e91.2_m30_m06_c94_2l_c2
DOI: 10.7483/opendata.delphi.ed7r.nhb9
title: DELPHI simulation data sh_hzha03pythia6156tttt_e91.2_m6_m20_c94_2l_c2
DOI: 10.7483/opendata.delphi.oaxc.1wi9
title: DELPHI simulation data sh_qqps_s94_2l_b3
DOI: 10.7483/opendata.delphi.1eze.76az
title: DELPHI simulation data sh_hzha03pythia6156bbtt_e91.2_m60_m06_c94_2l_c2
DOI: 10.7483/opendata.delphi.ddjt.se7e
title: DELPHI simulation data sh_pythia5720yukatttt_e91.2_m30_c94_2l_c2
DOI: 10.7483/opendata.delphi.6oyk.7oyq
title: DELPHI simulation data sh_hzha03pythia6156tttt_e91.2_m60_m4_c94_2l_c2
DOI: 10.7483/opendata.delphi.szk7.ed3p
title: DELPHI simulation data sh_qqps_s94_2l_c2
DOI: 10.5281/zenodo.14597744
title: Spatial transcriptomics reveals altered communities and drivers of aberrant epithelia and pro-fibrotic fibroblasts in interstitial lung diseases

description: Interstitial lung diseases (ILD) are characterized by fibrotic scarring of the distal lung parenchyma with remarkably unfavorable prognosis. Here we generated a comprehensive portrait of diverse cell types in distal lung and investigated how their spatial organization is altered in fibrosis. 

We provide the cloupe files for each individual Visium run which can be visualized using the Loupe browser. Each file also contains additional metadata on community membership and annotated histopathological feature for each visium spot overlaid on top of the H&E stained image.
DOI: 10.5281/zenodo.14597745
title: Spatial transcriptomics reveals altered communities and drivers of aberrant epithelia and pro-fibrotic fibroblasts in interstitial lung diseases

description: Interstitial lung diseases (ILD) are characterized by fibrotic scarring of the distal lung parenchyma with remarkably unfavorable prognosis. Here we generated a comprehensive portrait of diverse cell types in distal lung and investigated how their spatial organization is altered in fibrosis. 

We provide the cloupe files for each individual Visium run which can be visualized using the Loupe browser. Each file also contains additional metadata on community membership and annotated histopathological feature for each visium spot overlaid on top of the H&E stained image.
DOI: 10.7483/opendata.delphi.qox7.soc8
title: DELPHI simulation data sh_hzha03pythia6156tttt_e91.2_m50_m6_c94_2l_c2
DOI: 10.7483/opendata.delphi.g7rz.242j
title: DELPHI simulation data sh_ccds_b94_2l_c2
DOI: 10.7483/opendata.delphi.umw0.z80p
title: DELPHI simulation data sh_hzha03pythia6156bbtt_e91.2_m40_m04_c94_2l_c2
DOI: 10.7483/opendata.delphi.kvm1.jswe
title: DELPHI simulation data sh_hzha03pythia6156bbtt_e91.2_m20_m12_c94_2l_c2