cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.1308551.v2
title: 2014 07 01-02 Time-Lapse Sequence Images 6500-7500

description: 1-2 July 2014 - Partial sequence of Reconyx HC600 HyperFire trail camera images using both the motion sensor and time-lapse to trigger the camera. The total sequence includes 14,546 images covering the period 11:15 AM Eastern Standard Time on 1 July 2014 through 12:27 PM Eastern Standard Time on 2 July 2014. The intention was for a long-term observation (about 10 days) however the motion sensor triggered on moving branches and in consequence the memory card was full in a little more than one day. The time lapse sequence turns off after sunset to conserve battery and memory space and resumes before sunrise. The first 2000 images happen to also document finding and casting a large (approximately 14" long by 5" wide) footprint nearly on center in the scene. During the time-lapse sequence known animals such as deer are visible moving through the scene. No other human activity is observed. An unknown animal appears in image 6891. GPS coordinates of the camera are latitude N 40 deg 09.038 min longitude W 074 deg 08.894 min. The camera is attached 20 feet above the ground in a medium sized tree at the western edge of the cleared area underneath the power transmission lines and with a view across that cleared area at an approximate orientation of 42 deg magnetic. NOTE: Images 6965, 7065, 7165, 7265, 7365, and 7465 are missing. They were most likely deleted inadvertently while initially screening the images. They are missing from both working folders and back-up copies of the 1-2July 2014 data.<br>Project order 24a<br>
DOI: 10.6084/m9.figshare.1308551.v1
title: 1-2 July 2014 Time-Lapse Sequence Images 6500-7500

description: 1-2 July 2014 - Partial sequence of Reconyx HC600 HyperFire trail camera images using both the motion sensor and time-lapse to trigger the camera. The total sequence includes 14,546 images covering the period 11:15 AM Eastern Standard Time on 1 July 2014 through 12:27 PM Eastern Standard Time on 2 July 2014. The intention was for a long-term observation (about 10 days) however the motion sensor triggered on moving branches and in consequence the memory card was full in a little more than one day. The time lapse sequence turns off after sunset to conserve battery and memory space and resumes before sunrise. The first 2000 images happen to also document finding and casting a large (approximately 14" long by 5" wide) footprint nearly on center in the scene. During the time-lapse sequence known animals such as deer are visible moving through the scene. No other human activity is observed. An unknown animal appears in image 6891. GPS coordinates of the camera are latitude N 40 deg 09.038 min longitude W 074 deg 08.894 min. The camera is attached 20 feet above the ground in a medium sized tree at the western edge of the cleared area underneath the power transmission lines and with a view across that cleared area at an approximate orientation of 42 deg magnetic. NOTE: Images 6965, 7065, 7165, 7265, 7365, and 7465 are missing. They were most likely deleted inadvertently while initially screening the images. They are missing from both working folders and back-up copies of the 1-2July 2014 data.
DOI: 10.6084/m9.figshare.1308698.v6
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308698.v7
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308525
title: 2014 07 01-02 Time-Lapse Sequence Images 0001-1000

description: 1-2 July 2014 - Partial sequence of Reconyx HC600 HyperFire trail camera images using both the motion sensor and time-lapse to trigger the camera. The total sequence includes 14,546 images covering the period 11:15 AM Eastern Standard Time on 1 July 2014 through 12:27 PM Eastern Standard Time on 2 July 2014. The intention was for a long-term observation (about 10 days) however the motion sensor triggered on moving branches and in consequence the memory card was full in a little more than one day. The time lapse sequence turns off after sunset to conserve battery and memory space and resumes before sunrise. The first 2000 images happen to also document finding and casting a large (approximately 14" long by 5" wide) footprint nearly on center in the scene. During the time-lapse sequence known animals such as deer are visible moving through the scene. No other human activity is observed. An unknown animal appears in image 6891. GPS coordinates of the camera are latitude N 40 deg 09.038 min longitude W 074 deg 08.894 min. The camera is attached 20 feet above the ground in a medium sized tree at the western edge of the cleared area underneath the power transmission lines and with a view across that cleared area at an approximate orientation of 42 deg magnetic.<br>Project order 22a<br>
DOI: 10.6084/m9.figshare.1308517
title: Simulated dataset for I = 0.48% and RR = 6

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 6 for a base incidence of 0.48 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308698.v8
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308517.v1
title: Simulated dataset for I = 0.48% and RR = 6

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 6 for a base incidence of 0.48 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308525.v2
title: 2014 07 01-02 Time-Lapse Sequence Images 0001-1000

description: 1-2 July 2014 - Partial sequence of Reconyx HC600 HyperFire trail camera images using both the motion sensor and time-lapse to trigger the camera. The total sequence includes 14,546 images covering the period 11:15 AM Eastern Standard Time on 1 July 2014 through 12:27 PM Eastern Standard Time on 2 July 2014. The intention was for a long-term observation (about 10 days) however the motion sensor triggered on moving branches and in consequence the memory card was full in a little more than one day. The time lapse sequence turns off after sunset to conserve battery and memory space and resumes before sunrise. The first 2000 images happen to also document finding and casting a large (approximately 14" long by 5" wide) footprint nearly on center in the scene. During the time-lapse sequence known animals such as deer are visible moving through the scene. No other human activity is observed. An unknown animal appears in image 6891. GPS coordinates of the camera are latitude N 40 deg 09.038 min longitude W 074 deg 08.894 min. The camera is attached 20 feet above the ground in a medium sized tree at the western edge of the cleared area underneath the power transmission lines and with a view across that cleared area at an approximate orientation of 42 deg magnetic.<br>Project order 22a<br>
DOI: 10.6084/m9.figshare.1308525.v1
title: 1-2 July 2014 Time-Lapse Sequence Images 0001-1000

description: 1-2 July 2014 - Partial sequence of Reconyx HC600 HyperFire trail camera images using both the motion sensor and time-lapse to trigger the camera. The total sequence includes 14,546 images covering the period 11:15 AM Eastern Standard Time on 1 July 2014 through 12:27 PM Eastern Standard Time on 2 July 2014. The intention was for a long-term observation (about 10 days) however the motion sensor triggered on moving branches and in consequence the memory card was full in a little more than one day. The time lapse sequence turns off after sunset to conserve battery and memory space and resumes before sunrise. The first 2000 images happen to also document finding and casting a large (approximately 14" long by 5" wide) footprint nearly on center in the scene. During the time-lapse sequence known animals such as deer are visible moving through the scene. No other human activity is observed. An unknown animal appears in image 6891. GPS coordinates of the camera are latitude N 40 deg 09.038 min longitude W 074 deg 08.894 min. The camera is attached 20 feet above the ground in a medium sized tree at the western edge of the cleared area underneath the power transmission lines and with a view across that cleared area at an approximate orientation of 42 deg magnetic.
DOI: 10.6084/m9.figshare.1308698.v9
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308500
title: Simulated dataset for I = 2.26 % and RR = 6

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 6 for a base incidence of 2.26 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308501
title: Simulated dataset for I = 0.48 % and RR = 3

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 3 for a base incidence of 0.48 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308501.v1
title: Simulated dataset for I = 0.48 % and RR = 3

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 3 for a base incidence of 0.48 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308698.v10
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308494
title: Simulated dataset for I = 2.26 % and RR = 3

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 3 for a base incidence of 2.26 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308497
title: U-PB zircon tuff geochronology from the Karoo Basin, South Africa: implications of zircon recycling on stratigraphic age controls

description: Along the &gt;650 km long southern margin of the Karoo Basin in South Africa, we traversed four evenly spaced stratigraphic transects and collected 22 samples of volcanic, air-fall tuffs thought to be distal deposits derived from the Permian–Triassic Southern Gondwanan volcanic arc. We present 469 new U-Pb zircon ages determined by sensitive high-resolution ion microprobe reverse geometry (SHRIMP-RG) at the Stanford–USGS Microanalytical Center in order to constrain the maximum depositional ages for the southern Karoo Basin strata. Weighted means of these youngest coherent zircon populations were selected to maximize the number of analyses while minimizing the mean square weighted deviation (MSWD) to increase the robustness and decrease the influence of Pb-loss and inheritance in determining the maximum depositional age. Maximum depositional ages for the marine Ecca Group range from 250 to 274 Ma, whereas in the conformably overlying terrestrial Beaufort Group maximum depositional ages ranged from 257 to 452 Ma. Across the southern Karoo Basin, the Ecca Group tuffs produce maximum depositional ages that young upward; however, the Beaufort Group tuffs yield maximum depositional ages that are geochronologically out of sequence. Furthermore, maximum depositional ages of the Beaufort Group tuffs are consistently older than ash ages within the underlying marine strata. Our results are supported by previously published U-Pb tuff zircon geochronology in the Karoo Basin and demonstrate that the presence of out-of-sequence, older tuff ages are repeatable in Beaufort Group tuffs along the southern margin of the basin. We propose that tuffs in the Karoo Basin are correlative with tuffs in southern South America, and that the age spectra of these tuffs were influenced by magmatic crustal recycling. We use these data to highlight the complexity of U-Pb zircon datasets from tuffs, address the use of U-Pb zircon ages to provide absolute age controls, and discuss the implications of these new age controls on the Permian-Triassic Karoo strata.
DOI: 10.6084/m9.figshare.1308698.v11
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308494.v1
title: Simulated dataset for I = 2.26 % and RR = 3

description: A collection of 221 datasets in R format (rda), each corresponding to 1000 simulations of one cluster with a relative risk of 3 for a base incidence of 2.26 % births per year. Each dataset is a table of 221 000 rows and 6 columns.<br>The rows contain: -the coordinates (longitude and latitude) of a SU, the observed number of cases, -the size of the at-risk population (i.e., the number of live births), -the expected number of cases in the specified SU assuming an inhomogeneous Poisson process for the cases distribution and -an indicator for the simulation ranging from 1 to 1000.
DOI: 10.6084/m9.figshare.1308497.v1
title: U-PB zircon tuff geochronology from the Karoo Basin, South Africa: implications of zircon recycling on stratigraphic age controls

description: Along the &gt;650 km long southern margin of the Karoo Basin in South Africa, we traversed four evenly spaced stratigraphic transects and collected 22 samples of volcanic, air-fall tuffs thought to be distal deposits derived from the Permian–Triassic Southern Gondwanan volcanic arc. We present 469 new U-Pb zircon ages determined by sensitive high-resolution ion microprobe reverse geometry (SHRIMP-RG) at the Stanford–USGS Microanalytical Center in order to constrain the maximum depositional ages for the southern Karoo Basin strata. Weighted means of these youngest coherent zircon populations were selected to maximize the number of analyses while minimizing the mean square weighted deviation (MSWD) to increase the robustness and decrease the influence of Pb-loss and inheritance in determining the maximum depositional age. Maximum depositional ages for the marine Ecca Group range from 250 to 274 Ma, whereas in the conformably overlying terrestrial Beaufort Group maximum depositional ages ranged from 257 to 452 Ma. Across the southern Karoo Basin, the Ecca Group tuffs produce maximum depositional ages that young upward; however, the Beaufort Group tuffs yield maximum depositional ages that are geochronologically out of sequence. Furthermore, maximum depositional ages of the Beaufort Group tuffs are consistently older than ash ages within the underlying marine strata. Our results are supported by previously published U-Pb tuff zircon geochronology in the Karoo Basin and demonstrate that the presence of out-of-sequence, older tuff ages are repeatable in Beaufort Group tuffs along the southern margin of the basin. We propose that tuffs in the Karoo Basin are correlative with tuffs in southern South America, and that the age spectra of these tuffs were influenced by magmatic crustal recycling. We use these data to highlight the complexity of U-Pb zircon datasets from tuffs, address the use of U-Pb zircon ages to provide absolute age controls, and discuss the implications of these new age controls on the Permian-Triassic Karoo strata.
DOI: 10.6084/m9.figshare.1308698.v12
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308492
title: of Late presentation to HIV/AIDS Care in Southern Tigray zone, Northern Ethiopiaof Late presentation to HIV/AIDS Care in Southern Tigray zone, Northern Ethiopia

description: This data set contains variables that was collected by the research team to identify the potential risk facters for lately seeking care
DOI: 10.6084/m9.figshare.1308497.v3
title: U-PB zircon tuff geochronology from the Karoo Basin, South Africa: implications of zircon recycling on stratigraphic age controls

description: Along the &gt;650 km long southern margin of the Karoo Basin in South Africa, we traversed four evenly spaced stratigraphic transects and collected 22 samples of volcanic, air-fall tuffs thought to be distal deposits derived from the Permian–Triassic Southern Gondwanan volcanic arc. We present 469 new U-Pb zircon ages determined by sensitive high-resolution ion microprobe reverse geometry (SHRIMP-RG) at the Stanford–USGS Microanalytical Center in order to constrain the maximum depositional ages for the southern Karoo Basin strata. Weighted means of these youngest coherent zircon populations were selected to maximize the number of analyses while minimizing the mean square weighted deviation (MSWD) to increase the robustness and decrease the influence of Pb-loss and inheritance in determining the maximum depositional age. Maximum depositional ages for the marine Ecca Group range from 250 to 274 Ma, whereas in the conformably overlying terrestrial Beaufort Group maximum depositional ages ranged from 257 to 452 Ma. Across the southern Karoo Basin, the Ecca Group tuffs produce maximum depositional ages that young upward; however, the Beaufort Group tuffs yield maximum depositional ages that are geochronologically out of sequence. Furthermore, maximum depositional ages of the Beaufort Group tuffs are consistently older than ash ages within the underlying marine strata. Our results are supported by previously published U-Pb tuff zircon geochronology in the Karoo Basin and demonstrate that the presence of out-of-sequence, older tuff ages are repeatable in Beaufort Group tuffs along the southern margin of the basin. We propose that tuffs in the Karoo Basin are correlative with tuffs in southern South America, and that the age spectra of these tuffs were influenced by magmatic crustal recycling. We use these data to highlight the complexity of U-Pb zircon datasets from tuffs, address the use of U-Pb zircon ages to provide absolute age controls, and discuss the implications of these new age controls on the Permian-Triassic Karoo strata.
DOI: 10.6084/m9.figshare.1308698.v13
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308492.v1
title: of Late presentation to HIV/AIDS Care in Southern Tigray zone, Northern Ethiopiaof Late presentation to HIV/AIDS Care in Southern Tigray zone, Northern Ethiopia

description: This data set contains variables that was collected by the research team to identify the potential risk facters for lately seeking care
DOI: 10.6084/m9.figshare.1308497.v2
title: U-PB zircon tuff geochronology from the Karoo Basin, South Africa: implications of zircon recycling on stratigraphic age controls

description: Along the &gt;650 km long southern margin of the Karoo Basin in South Africa, we traversed four evenly spaced stratigraphic transects and collected 22 samples of volcanic, air-fall tuffs thought to be distal deposits derived from the Permian–Triassic Southern Gondwanan volcanic arc. We present 469 new U-Pb zircon ages determined by sensitive high-resolution ion microprobe reverse geometry (SHRIMP-RG) at the Stanford–USGS Microanalytical Center in order to constrain the maximum depositional ages for the southern Karoo Basin strata. Weighted means of these youngest coherent zircon populations were selected to maximize the number of analyses while minimizing the mean square weighted deviation (MSWD) to increase the robustness and decrease the influence of Pb-loss and inheritance in determining the maximum depositional age. Maximum depositional ages for the marine Ecca Group range from 250 to 274 Ma, whereas in the conformably overlying terrestrial Beaufort Group maximum depositional ages ranged from 257 to 452 Ma. Across the southern Karoo Basin, the Ecca Group tuffs produce maximum depositional ages that young upward; however, the Beaufort Group tuffs yield maximum depositional ages that are geochronologically out of sequence. Furthermore, maximum depositional ages of the Beaufort Group tuffs are consistently older than ash ages within the underlying marine strata. Our results are supported by previously published U-Pb tuff zircon geochronology in the Karoo Basin and demonstrate that the presence of out-of-sequence, older tuff ages are repeatable in Beaufort Group tuffs along the southern margin of the basin. We propose that tuffs in the Karoo Basin are correlative with tuffs in southern South America, and that the age spectra of these tuffs were influenced by magmatic crustal recycling. We use these data to highlight the complexity of U-Pb zircon datasets from tuffs, address the use of U-Pb zircon ages to provide absolute age controls, and discuss the implications of these new age controls on the Permian-Triassic Karoo strata.
DOI: 10.6084/m9.figshare.1308698.v14
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"
DOI: 10.6084/m9.figshare.1308698.v15
title: raw fMRI data set (Boly et al.)

description: raw fMRI data set obtained in "Stimulus set meaningfulness and neurophysiological differentiation: a functional magnetic resonance imaging study"