cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.8287781
title: Geology of the Hokusai quadrangle (H05), Mercury

description: The Hokusai (H05) quadrangle is in Mercury’s northern mid-latitudes (0–90°E, 22.5–65°N) and covers almost 5 million km<sup>2</sup>, or 6.5%, of the planet’s surface. We have used data from the MESSENGER spacecraft to make the first geological map of H05. Linework was digitized at 1:400,000-scale for final presentation at 1:3,000,000-scale, mainly using a ∼166 m/pixel monochrome basemap. Three major photogeologic units of regional extent were mapped: intercrater, intermediate, and smooth plains. Materials of craters ≥ 20 km in diameter were classified according to their degradation state. Two classification schemes were employed in parallel, one with three classes and the other with five classes, for compatibility with existing MESSENGER-era quadrangle maps and the first global geologic map. This map will provide science context and targets for the ESA-JAXA BepiColombo mission to Mercury.
DOI: 10.6084/m9.figshare.8046287
title: Geological tourist mapping of the Mount Serrone fault Geosite (Gioia dei Marsi, Central Apennines, Italy)

description: The Geological tourist map of the Mount Serrone fault Geosite (Gioia dei Marsi, Italy) has been realized for describing, in an educational perspective, the surface expression of one of the main active faults of the Central Apennines, connected with the 1915 Fucino earthquake (magnitude 7, historically, one of the strongest in Italy). The Central Apennines are a mountain range whose landscape is deeply connected to active tectonics and seismicity, as documented by recent earthquakes. In this framework, the map is a useful tool for the dissemination of the geological knowledge of the Fucino area and faults in general and for the promotion of a geological landscape through a modern, sustainable and environmentally aware tourism. The map is double-sided with simple texts and cartoons on the front outlining general info about the geosite, faults and earthquakes, how to behave in seismic areas and historical notes. The back shows the Main Map with its visual legend featuring the main geological and tectonic elements of the Mount Serrone fault Geosite and the long term history of the landscape. Through simple keywords and concepts, tectonics, faults and earthquakes are shown to be natural features that have contributed to shape the landscape of the Apennines over geological time, as well as something to be afraid and worried of, as they are connected to natural hazard and disasters. This approach is aimed at increasing people's awareness of geological processes and hazards (i.e. seismic), which with adequate knowledge and proper land management, can be lived with.
DOI: 10.6084/m9.figshare.8046287.v3
title: Geological tourist mapping of the Mount Serrone fault Geosite (Gioia dei Marsi, Central Apennines, Italy)

description: The Geological tourist map of the Mount Serrone fault Geosite (Gioia dei Marsi, Italy) has been realized for describing, in an educational perspective, the surface expression of one of the main active faults of the Central Apennines, connected with the 1915 Fucino earthquake (magnitude 7, historically, one of the strongest in Italy). The Central Apennines are a mountain range whose landscape is deeply connected to active tectonics and seismicity, as documented by recent earthquakes. In this framework, the map is a useful tool for the dissemination of the geological knowledge of the Fucino area and faults in general and for the promotion of a geological landscape through a modern, sustainable and environmentally aware tourism. The map is double-sided with simple texts and cartoons on the front outlining general info about the geosite, faults and earthquakes, how to behave in seismic areas and historical notes. The back shows the Main Map with its visual legend featuring the main geological and tectonic elements of the Mount Serrone fault Geosite and the long term history of the landscape. Through simple keywords and concepts, tectonics, faults and earthquakes are shown to be natural features that have contributed to shape the landscape of the Apennines over geological time, as well as something to be afraid and worried of, as they are connected to natural hazard and disasters. This approach is aimed at increasing people's awareness of geological processes and hazards (i.e. seismic), which with adequate knowledge and proper land management, can be lived with.
DOI: 10.6084/m9.figshare.8287781.v2
title: Geology of the Hokusai quadrangle (H05), Mercury

description: The Hokusai (H05) quadrangle is in Mercury’s northern mid-latitudes (0–90°E, 22.5–65°N) and covers almost 5 million km<sup>2</sup>, or 6.5%, of the planet’s surface. We have used data from the MESSENGER spacecraft to make the first geological map of H05. Linework was digitized at 1:400,000-scale for final presentation at 1:3,000,000-scale, mainly using a ∼166 m/pixel monochrome basemap. Three major photogeologic units of regional extent were mapped: intercrater, intermediate, and smooth plains. Materials of craters ≥ 20 km in diameter were classified according to their degradation state. Two classification schemes were employed in parallel, one with three classes and the other with five classes, for compatibility with existing MESSENGER-era quadrangle maps and the first global geologic map. This map will provide science context and targets for the ESA-JAXA BepiColombo mission to Mercury.
DOI: 10.6084/m9.figshare.16695592
title: Rat FOF Recordings During Dynamic Clicks Task

description: FOF recordings from 5 rats performing a dynamic evidence accumulation task. These recordings yielded 738 units from these 5 rats. Data was collected using unilateral electrode arrays (n=4) and bilateral tetrodes (n=1). Each rat has an accompanying behavioral dataset containing an average of 108,126 trials performing the dynamic clicks task. These trials were used to fit a previously described accumulation model to their behavior (Piet et al, 2018). The dynamic clicks task presents the animal with two streams of randomly-timed auditory clicks on the left and right side of a central fixation port. These left and right click trains are generated with at a high rate (38Hz) on one side and a low rate (2Hz) on the other. The underlying click rates alternate a rate of 1Hz and the rat is rewarded for correctly identifying the side generating the higher click rate at the end of the trial. To solve this task, rats learn to discount older evidence so that the most recently presented clicks have the greatest effect on the decision. This induces changes of mind throughout each trial, which we can predict with our behavioral model and relate to neural activity.<br>This dataset, along with the accompanying code (https://github.com/Brody-Lab/dynamic_ephys) can be used to regenerate all the results and figures in the manuscript titled Stable choice coding in FOF across model predicted changes of mind (Boyd-Meredith and Piet et al., under review; preprint here: https://www.biorxiv.org/content/10.1101/2021.05.13.444020v2).<br>Behavioral data:Each rat (H###) has behavioral data saved in a file titled data/H###.matThis contains a matlab struct called data with fields like:T - the duration of the trialleftbups - the timing of the left clicks relative to stimulus onset in each trialpokedR - boolean indicated whether the rat went to the rightward portsessid - a unique identifier for each sessiongenSwitchTimes - the timing of the state switches relative to the stimulus onset on that trial<br>Model fits:Each rat's accumulation model fits are saved in a file titled results/fit_analytical_H###.matThis contains a matlab struct with fields like:final - the best fit parameters to the accumulation modelparam_names - the names associated with each parameterauto_se - standard error derived from automatic differentiation in julia<br>Electrophysiology data:<br>Each cell has an associated file titled: data/phys/bin/phys_data_#####.matThis file contains an associated ratname and sessid as well as a struct array of length ntrials called array_data whose fields are things likestim_start - the timing (in seconds) of the stimulus start relative to the beginning of the trialspikes - the timing of the spikes on the trial<br>The easiest way to begin working with the data is to clone the accompanying git repository https://github.com/Brody-Lab/dynamic_ephys<br><br>
DOI: 10.6084/m9.figshare.8287781.v1
title: Geology of the Hokusai quadrangle (H05), Mercury

description: The Hokusai (H05) quadrangle is in Mercury’s northern mid-latitudes (0–90°E, 22.5–65°N) and covers almost 5 million km<sup>2</sup>, or 6.5%, of the planet’s surface. We have used data from the MESSENGER spacecraft to make the first geological map of H05. Linework was digitized at 1:400,000-scale for final presentation at 1:3,000,000-scale, mainly using a ∼166 m/pixel monochrome basemap. Three major photogeologic units of regional extent were mapped: intercrater, intermediate, and smooth plains. Materials of craters ≥ 20 km in diameter were classified according to their degradation state. Two classification schemes were employed in parallel, one with three classes and the other with five classes, for compatibility with existing MESSENGER-era quadrangle maps and the first global geologic map. This map will provide science context and targets for the ESA-JAXA BepiColombo mission to Mercury.
DOI: 10.6084/m9.figshare.8046287.v2
title: Geological tourist mapping of the Mount Serrone fault Geosite (Gioia dei Marsi, Central Apennines, Italy)

description: The Geological tourist map of the Mount Serrone fault Geosite (Gioia dei Marsi, Italy) has been realized for describing, in an educational perspective, the surface expression of one of the main active faults of the Central Apennines, connected with the 1915 Fucino earthquake (magnitude 7, historically, one of the strongest in Italy). The Central Apennines are a mountain range whose landscape is deeply connected to active tectonics and seismicity, as documented by recent earthquakes. In this framework, the map is a useful tool for the dissemination of the geological knowledge of the Fucino area and faults in general and for the promotion of a geological landscape through a modern, sustainable and environmentally aware tourism. The map is double-sided with simple texts and cartoons on the front outlining general info about the geosite, faults and earthquakes, how to behave in seismic areas and historical notes. The back shows the Main Map with its visual legend featuring the main geological and tectonic elements of the Mount Serrone fault Geosite and the long term history of the landscape. Through simple keywords and concepts, tectonics, faults and earthquakes are shown to be natural features that have contributed to shape the landscape of the Apennines over geological time, as well as something to be afraid and worried of, as they are connected to natural hazard and disasters. This approach is aimed at increasing people's awareness of geological processes and hazards (i.e. seismic), which with adequate knowledge and proper land management, can be lived with.
DOI: 10.34740/kaggle/dsv/2662191
title: COVID Vaccination in World (updated daily)
DOI: 10.6084/m9.figshare.14333222.v1
title: Non-linear enhancement of radiative absorption by black carbon due to particle mixing state

description: This is the full dataset shown in the figures and tables in <b><i>Non-linear enhancement of radiative absorption by black carbon due to particle mixing state.</i></b>
DOI: 10.6084/m9.figshare.16699129
title: Supplementary Material for: Serum biomarker status with a distinctive pattern in prognosis of gastroenteropancreatic neuroendocrine carcinoma

description: Medicine
DOI: 10.6084/m9.figshare.16699129.v1
title: Supplementary Material for: Serum biomarker status with a distinctive pattern in prognosis of gastroenteropancreatic neuroendocrine carcinoma

description: Medicine
DOI: 10.6084/m9.figshare.13049382
title: Landforms of the lower Hushe Valley (Central Karakoram, Pakistan)

description: This paper presents a new geomorphological map for the lower Hushe Valley (below 3400 m asl), located to the SE of the Central Karakoram in Baltistan (North Pakistan). Fieldwork and remote sensing were combined to improve understanding of the most recent surface landforms to produce a 1:50,000 scale map. Thirteen landform types associated with glacial, fluvial, gravitational and mass wasting processes were identified and mapped. Particular emphasis was made on currently dynamic processes that could pose a threat to the population. The distribution of the landforms on the valley (reworked tills, alluvial fans, rockfalls, among others) differs between the eastern and the western hillslopes, and from north to south, mainly due to bedrock types, location of geological structures and distribution of lateral tributaries. This map is the first and necessary step towards a deep assessment on geological risk related to external processes in the area.
DOI: 10.6084/m9.figshare.13049382.v1
title: Landforms of the lower Hushe Valley (Central Karakoram, Pakistan)

description: This paper presents a new geomorphological map for the lower Hushe Valley (below 3400 m asl), located to the SE of the Central Karakoram in Baltistan (North Pakistan). Fieldwork and remote sensing were combined to improve understanding of the most recent surface landforms to produce a 1:50,000 scale map. Thirteen landform types associated with glacial, fluvial, gravitational and mass wasting processes were identified and mapped. Particular emphasis was made on currently dynamic processes that could pose a threat to the population. The distribution of the landforms on the valley (reworked tills, alluvial fans, rockfalls, among others) differs between the eastern and the western hillslopes, and from north to south, mainly due to bedrock types, location of geological structures and distribution of lateral tributaries. This map is the first and necessary step towards a deep assessment on geological risk related to external processes in the area.
DOI: 10.6084/m9.figshare.13182959
title: Engineering geological mapping using airborne LiDAR datasets – an example from the Vinodol Valley, Croatia

description: This paper presents the potential of airborne LiDAR digital terrain model (DTM) for engineering geological mapping in geologically complex and forested area. The multipurpose, comprehensive engineering geological map is created for the pilot area (16.75 km<sup>2</sup>) located in the Vinodol Valley, Croatia. Eight topographic datasets were derived from 1-m DTM and visually interpreted to identify lithologies and geomorphological processes. In total, 12 engineering geological units, more than 500 landslides, and gully erosion phenomena are outlined in the pilot area. Results confirmed the greatest potential of visual interpretation of LiDAR derivatives for mapping of geomorphological processes in a large scale. On the other hand, this method allowed identification and mapping of engineering formations that are basic engineering geological units appropriate for the medium-scale engineering geological maps. The produced map represents a valuable tool for a wide range of planning and engineering purposes, as well as for geological hazard and risk assessment.
DOI: 10.6084/m9.figshare.13182959.v1
title: Engineering geological mapping using airborne LiDAR datasets – an example from the Vinodol Valley, Croatia

description: This paper presents the potential of airborne LiDAR digital terrain model (DTM) for engineering geological mapping in geologically complex and forested area. The multipurpose, comprehensive engineering geological map is created for the pilot area (16.75 km<sup>2</sup>) located in the Vinodol Valley, Croatia. Eight topographic datasets were derived from 1-m DTM and visually interpreted to identify lithologies and geomorphological processes. In total, 12 engineering geological units, more than 500 landslides, and gully erosion phenomena are outlined in the pilot area. Results confirmed the greatest potential of visual interpretation of LiDAR derivatives for mapping of geomorphological processes in a large scale. On the other hand, this method allowed identification and mapping of engineering formations that are basic engineering geological units appropriate for the medium-scale engineering geological maps. The produced map represents a valuable tool for a wide range of planning and engineering purposes, as well as for geological hazard and risk assessment.
DOI: 10.6084/m9.figshare.12287702
title: Biophysical regions of the Southern Highlands, Tanzania: regionalization in a data scarce environment with open geospatial data and statistical methods

description: Spatially explicit, evidence-based and regionally contextualized data on biophysical landscape characteristics is an essential basis for regionally sustainable landscape management schemes. In many regions of the Global South, the availability of such information is poor, especially at the subnational level, and the spatial management is often based on generic and outdated information, leading to severe threats for land sustainability. We have developed a biophysical regionalization of the Southern Highlands area of Tanzania. The map is based on open-source global datasets depicting climate, soil, topography and vegetation. Through replicable statistical and geospatial analyses, we have identified 7 regions and 18 subsections with biophysically similar and spatially distinctive environmental conditions. The regions provide spatially contextualized support for understanding and managing the landscapes of the Southern Highlands. The applications for such data sets are numerous, from screening suitability areas for e.g. afforestation schemes to evaluating the distinctiveness and vulnerability of landscapes to degradation.
DOI: 10.6084/m9.figshare.12290477
title: Physical volcanology of Tseax Volcano, British Columbia, Canada

description: Tseax volcano erupted ∼ 250 years ago in NW British Columbia, Canada producing tephra deposits and lava flows. Field mapping has defined the stratigraphy of Tseax and the lava flow morphologies. Aerial photogrammetry and bathymetry surveys were used to create a high resolution digital elevation model of the volcano to facilitate mapping and estimates of erupted material volumes. Tseax volcano (∼ 10.4 ± 0.7 × 10<sup>6</sup> m<sup>3</sup>) comprises an outer breached spatter rampart and an inner conical tephra cone. Tseax is associated with a 32 km long and 0.49 ± 0.08 km<sup>3</sup> basanite-to-tephrite lava flow field covering ∼ 36 km<sup>2</sup> and divided into 4 distinct lava flows with heterogeneous surface morphologies. We present a volcanological map of Tseax volcano at a scale of 1:22,500. This will serve as supporting information for further research on the eruptive history of Tseax volcano and the lava flow field emplacement.
DOI: 10.6084/m9.figshare.13253892
title: Ornamental stones of Piemonte (NW Italy): an updated geo-lithological map

description: The ‘Ornamental Stones of Piemonte Region’ geo-lithological map at 1:250,000 scale aims at reviewing the ornamental stone heritage of Piemonte at the regional scale. The map derives from a thorough revision of the available literature, integrated with some unpublished original data. The map shows the location of the main quarries of ornamental stones of the region, selected on the basis of their historical, cultural and architectonic relevance. A geo-lithological basemap was produced, deriving it from a basic Geological Map of Piemonte, available at the same scale. The large varieties of lithotypes of Piemonte have been resumed, in the new map, into 21 classes, which all the ornamental stones have been assigned to. The Main Map is enriched by some significant examples of using the ornamental stones in historical buildings, and it is supported by a supplementary data base containing essential information about the quarry sites and the quarried material.
DOI: 10.6084/m9.figshare.13253892.v2
title: Ornamental stones of Piemonte (NW Italy): an updated geo-lithological map

description: The ‘Ornamental Stones of Piemonte Region’ geo-lithological map at 1:250,000 scale aims at reviewing the ornamental stone heritage of Piemonte at the regional scale. The map derives from a thorough revision of the available literature, integrated with some unpublished original data. The map shows the location of the main quarries of ornamental stones of the region, selected on the basis of their historical, cultural and architectonic relevance. A geo-lithological basemap was produced, deriving it from a basic Geological Map of Piemonte, available at the same scale. The large varieties of lithotypes of Piemonte have been resumed, in the new map, into 21 classes, which all the ornamental stones have been assigned to. The Main Map is enriched by some significant examples of using the ornamental stones in historical buildings, and it is supported by a supplementary data base containing essential information about the quarry sites and the quarried material.
DOI: 10.6084/m9.figshare.12287702.v2
title: Biophysical regions of the Southern Highlands, Tanzania: regionalization in a data scarce environment with open geospatial data and statistical methods

description: Spatially explicit, evidence-based and regionally contextualized data on biophysical landscape characteristics is an essential basis for regionally sustainable landscape management schemes. In many regions of the Global South, the availability of such information is poor, especially at the subnational level, and the spatial management is often based on generic and outdated information, leading to severe threats for land sustainability. We have developed a biophysical regionalization of the Southern Highlands area of Tanzania. The map is based on open-source global datasets depicting climate, soil, topography and vegetation. Through replicable statistical and geospatial analyses, we have identified 7 regions and 18 subsections with biophysically similar and spatially distinctive environmental conditions. The regions provide spatially contextualized support for understanding and managing the landscapes of the Southern Highlands. The applications for such data sets are numerous, from screening suitability areas for e.g. afforestation schemes to evaluating the distinctiveness and vulnerability of landscapes to degradation.
DOI: 10.6084/m9.figshare.11507118
title: Volcanic evolution of the Somma-Vesuvius Complex (Italy)

description: A volcanological map of the active Somma-Vesuvius volcano is presented at the 1:20,000 scale. The map is based on 1:5000 ﬁeld mapping carried out during the Italian CARG project. Geological data are represented on a digital terrain model of the volcano. This allows a better visualisation of the main morphological, volcanic, and geological features. The legend is organised in four different panels, which depict the activity of the volcano and caldera development. The geological survey is based on recognition and description of lithostratigraphic units. The geological map highlights the volcanic evolution of the Somma-Vesuvius volcano, and it is propaedeutic for further studies aimed at improving the scientific knowledge and the volcanic hazard assessment of this world-famous volcano.
DOI: 10.6084/m9.figshare.11507118.v2
title: Volcanic evolution of the Somma-Vesuvius Complex (Italy)

description: A volcanological map of the active Somma-Vesuvius volcano is presented at the 1:20,000 scale. The map is based on 1:5000 ﬁeld mapping carried out during the Italian CARG project. Geological data are represented on a digital terrain model of the volcano. This allows a better visualisation of the main morphological, volcanic, and geological features. The legend is organised in four different panels, which depict the activity of the volcano and caldera development. The geological survey is based on recognition and description of lithostratigraphic units. The geological map highlights the volcanic evolution of the Somma-Vesuvius volcano, and it is propaedeutic for further studies aimed at improving the scientific knowledge and the volcanic hazard assessment of this world-famous volcano.