cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.1183513
title: Early Cretaceous arc magmatism and high-sulphidation epithermal porphyry Cu–Au mineralization in Yanbian area, Northeast China: the Duhuangling example

description: Yanbian area (Northeast China) is part of the Western Pacific porphyry–epithermal gold–copper metallogenic belt. Here, we present the results of a detailed study of Early Cretaceous mineralization-associated magmatic events in this region and, based on the results, identify the geological setting and mineralizing processes involved in mineral deposit formation. We focus on the timing and geodynamic mechanisms of hydrothermal alteration and metallogenesis of the Duhuangling high-sulphidation epithermal gold deposit, located ~15 km NW of the large Xiaoxinancha gold-rich porphyry copper deposit. New data are presented for zircon U–Pb, fluid inclusion Ar–Ar, whole-rock geochemical, and <i>in situ</i> zircon Hf isotopes for igneous rocks of the Duhuangling deposit, and the data – integrated with results of previous research – reveal that Yanbian area epithermal and porphyry Cu–Au deposits are associated with two stages of Early Cretaceous intermediate-felsic magmatism (116–118 and 112–109 Ma), with the later stage of magmatism more closely associated with mineral deposit formation. Our new data constrain the timing of formation of high-sulphidation epithermal gold deposits to 108–106 Ma and the timing of formation of gold-rich porphyry copper deposits to 111–109 Ma. The two stages of magmatism are associated with magmas derived from different sources, with the first-stage magmas potentially derived from partial melting of a depleted mantle wedge that had been metasomatized by subducted slab-derived fluids or melts; these first magmas are also mixed with material derived from the underplated lower crust. Second-stage magmas were probably generated by partial melting of subducting oceanic slab and some oceanic sediments and the interaction of these magmas with melts derived from the overlying lower crust. Most mineralization in the study area is associated with Cu- and Au-rich post-magmatic hydrothermal fluids that were generated during fractionation of hydrous, sulphur-rich, and high oxygen fugacity adakite-like/adakitic mixed magmas. The formation of both igneous rocks and mineral deposits in the study area occurred in a tectonic setting dominated by Late–Early Cretaceous subduction of the Izanagi or Pacific Plate beneath eastern Asia, indicating that the formation of epithermal and porphyry Cu–Au deposits in the Yanbian area involved subduction-derived fluids, melt modification, partial melting, magma mixing, and crystal fractionation.
DOI: 10.6084/m9.figshare.1183522
title: Condition of Close Tree Pairs

description: A dataset looking at the distance between trees, diameter at breast height, and conditions of pairs of trees in close proximity to each other in Danby woodlot on campus at York University.<br><br>Researchers walked from the outskirts of a woodlot and collected data from the first sighted tree and it's closest pair. Distance between trees were measured by transect measuring tape, from the closest edge of each pair of trees. Diameter of each tree was also measured by transect measuring tape held at a tangent at a height of approximately 110cm. Distance and diameter were both measured in centimeters (converted from meters) while the condition of the trees were simply eyed. Researchers repeated this ten times for ten pairs of trees, each time moving in a straight line deeper into the woodlot. The outskirts of the woodlots are more clear, and trees are a fair distance apart, whereas further in the trees grow more densely packed. This can be seen in the dataset which was recorded on paper at the time.
DOI: 10.6084/m9.figshare.1184101.v4
title: SGR 1900+14, RXTE Data

description: The SGR 1900+14 burst data set, including Standard 1 files, averaged periodograms and some posterior samples
DOI: 10.6084/m9.figshare.1183526.v1
title: Population Distribution and Condition of Trees at Danby Woods

description: Measuring tape was to only tool for this experiment; in addition, to a data sheet as shown in Wood-Distance excel sheet. The tape was used to measure the distance between a pair of adult trees. This process was applied for ten pairs of trees. Each pair was given a number and each tree in that pair was given either letters (a or b). After recording the distance, the circumference of each tree (a and b) was recorded by picturing the tree trunk as a circle and we are acquired to measure half of the exterior surface of that circle at a breast height of an individual. From the circumference, we were able to obtain on dbh (diameter at breast height) of each tree by using the OnlineConversion.com*. Further, the conditions of the sampled trees were recorded as 1 dead, 2 living, 3 healthy and big (explained more in the metadata). This research was done at York University in Danby Woods. The data was collected during the fall season of 2014. The measurements took 25 minutes for 10 pairs of trees. *The OnlineConversion.com: http://www.onlineconversion.com/circlesolve.htm Or by using this equation: (Circumference*0.3183)
DOI: 10.6084/m9.figshare.1183522.v1
title: Condition of Close Tree Pairs

description: A dataset looking at the distance between trees, diameter at breast height, and conditions of pairs of trees in close proximity to each other in Danby woodlot on campus at York University.<br><br>Researchers walked from the outskirts of a woodlot and collected data from the first sighted tree and it's closest pair. Distance between trees were measured by transect measuring tape, from the closest edge of each pair of trees. Diameter of each tree was also measured by transect measuring tape held at a tangent at a height of approximately 110cm. Distance and diameter were both measured in centimeters (converted from meters) while the condition of the trees were simply eyed. Researchers repeated this ten times for ten pairs of trees, each time moving in a straight line deeper into the woodlot. The outskirts of the woodlots are more clear, and trees are a fair distance apart, whereas further in the trees grow more densely packed. This can be seen in the dataset which was recorded on paper at the time.
DOI: 10.6084/m9.figshare.1183513.v2
title: Early Cretaceous arc magmatism and high-sulphidation epithermal porphyry Cu–Au mineralization in Yanbian area, Northeast China: the Duhuangling example

description: Yanbian area (Northeast China) is part of the Western Pacific porphyry–epithermal gold–copper metallogenic belt. Here, we present the results of a detailed study of Early Cretaceous mineralization-associated magmatic events in this region and, based on the results, identify the geological setting and mineralizing processes involved in mineral deposit formation. We focus on the timing and geodynamic mechanisms of hydrothermal alteration and metallogenesis of the Duhuangling high-sulphidation epithermal gold deposit, located ~15 km NW of the large Xiaoxinancha gold-rich porphyry copper deposit. New data are presented for zircon U–Pb, fluid inclusion Ar–Ar, whole-rock geochemical, and <i>in situ</i> zircon Hf isotopes for igneous rocks of the Duhuangling deposit, and the data – integrated with results of previous research – reveal that Yanbian area epithermal and porphyry Cu–Au deposits are associated with two stages of Early Cretaceous intermediate-felsic magmatism (116–118 and 112–109 Ma), with the later stage of magmatism more closely associated with mineral deposit formation. Our new data constrain the timing of formation of high-sulphidation epithermal gold deposits to 108–106 Ma and the timing of formation of gold-rich porphyry copper deposits to 111–109 Ma. The two stages of magmatism are associated with magmas derived from different sources, with the first-stage magmas potentially derived from partial melting of a depleted mantle wedge that had been metasomatized by subducted slab-derived fluids or melts; these first magmas are also mixed with material derived from the underplated lower crust. Second-stage magmas were probably generated by partial melting of subducting oceanic slab and some oceanic sediments and the interaction of these magmas with melts derived from the overlying lower crust. Most mineralization in the study area is associated with Cu- and Au-rich post-magmatic hydrothermal fluids that were generated during fractionation of hydrous, sulphur-rich, and high oxygen fugacity adakite-like/adakitic mixed magmas. The formation of both igneous rocks and mineral deposits in the study area occurred in a tectonic setting dominated by Late–Early Cretaceous subduction of the Izanagi or Pacific Plate beneath eastern Asia, indicating that the formation of epithermal and porphyry Cu–Au deposits in the Yanbian area involved subduction-derived fluids, melt modification, partial melting, magma mixing, and crystal fractionation.
DOI: 10.6084/m9.figshare.1183512.v5
title: Chessboard Dataset 25x

description: These are z-projections of ribbons imaged at 25x magnification for DAPI and YFP to serve as guides for subsequent higher-magnification imaging of desired subregions.
DOI: 10.6084/m9.figshare.1183513.v1
title: Early Cretaceous arc magmatism and high-sulphidation epithermal porphyry Cu–Au mineralization in Yanbian area, Northeast China: the Duhuangling example

description: Yanbian area (Northeast China) is part of the Western Pacific porphyry–epithermal gold–copper metallogenic belt. Here, we present the results of a detailed study of Early Cretaceous mineralization-associated magmatic events in this region and, based on the results, identify the geological setting and mineralizing processes involved in mineral deposit formation. We focus on the timing and geodynamic mechanisms of hydrothermal alteration and metallogenesis of the Duhuangling high-sulphidation epithermal gold deposit, located ~15 km NW of the large Xiaoxinancha gold-rich porphyry copper deposit. New data are presented for zircon U–Pb, fluid inclusion Ar–Ar, whole-rock geochemical, and <i>in situ</i> zircon Hf isotopes for igneous rocks of the Duhuangling deposit, and the data – integrated with results of previous research – reveal that Yanbian area epithermal and porphyry Cu–Au deposits are associated with two stages of Early Cretaceous intermediate-felsic magmatism (116–118 and 112–109 Ma), with the later stage of magmatism more closely associated with mineral deposit formation. Our new data constrain the timing of formation of high-sulphidation epithermal gold deposits to 108–106 Ma and the timing of formation of gold-rich porphyry copper deposits to 111–109 Ma. The two stages of magmatism are associated with magmas derived from different sources, with the first-stage magmas potentially derived from partial melting of a depleted mantle wedge that had been metasomatized by subducted slab-derived fluids or melts; these first magmas are also mixed with material derived from the underplated lower crust. Second-stage magmas were probably generated by partial melting of subducting oceanic slab and some oceanic sediments and the interaction of these magmas with melts derived from the overlying lower crust. Most mineralization in the study area is associated with Cu- and Au-rich post-magmatic hydrothermal fluids that were generated during fractionation of hydrous, sulphur-rich, and high oxygen fugacity adakite-like/adakitic mixed magmas. The formation of both igneous rocks and mineral deposits in the study area occurred in a tectonic setting dominated by Late–Early Cretaceous subduction of the Izanagi or Pacific Plate beneath eastern Asia, indicating that the formation of epithermal and porphyry Cu–Au deposits in the Yanbian area involved subduction-derived fluids, melt modification, partial melting, magma mixing, and crystal fractionation.
DOI: 10.6084/m9.figshare.1183526.v2
title: Population Distribution and Condition of Trees at Danby Woods

description: Measuring tape was to only tool for this experiment; in addition, to a data sheet as shown in Wood-Distance excel sheet. The tape was used to measure the distance between a pair of adult trees. This process was applied for ten pairs of trees. Each pair was given a number and each tree in that pair was given either letters (a or b). After recording the distance, the circumference of each tree (a and b) was recorded by picturing the tree trunk as a circle and we are acquired to measure half of the exterior surface of that circle at a breast height of an individual. From the circumference, we were able to obtain on dbh (diameter at breast height) of each tree by using the OnlineConversion.com*. Further, the conditions of the sampled trees were recorded as 1 dead, 2 living, 3 healthy and big (explained more in the metadata). This research was done at York University in Danby Woods. The data was collected during the fall season of 2014. The measurements took 25 minutes for 10 pairs of trees. *The OnlineConversion.com: http://www.onlineconversion.com/circlesolve.htm Or by using this equation: (Circumference*0.3183)
DOI: 10.6084/m9.figshare.1183476
title: Stability, metastability and spectroscopic constants of electronic states of NH<sup>−</sup> and CH<sup>−</sup>

description: Highly correlated <i>ab initio</i> methods were used in order to calculate potential energy curves (PECs) of the bound electronic states of CH<sup>−</sup> and NH<sup>−</sup> anions and the long-range parts of their excited states. The spin–orbit interaction between electronic states has been calculated for the cases in which the couplings were assumed to be responsible for perturbations. The spectroscopic constants of bound states were calculated from the PECs and compared with previous theoretical and/or available experimental values. Also, from the ground states of CH/CH<sup>−</sup> and NH/NH<sup>−</sup>, the adiabatic electron affinities were given and discussed.
DOI: 10.6084/m9.figshare.1183468
title: Eyetracking Magic Video Stimuli Summaries

description: These figures display timelines of each of the magic videos used in our misdirection research. They are drawn from stills and illustrated by Allison Friebertshauser.
DOI: 10.6084/m9.figshare.1183468.v1
title: Eyetracking Magic Video Stimuli Summaries

description: These figures display timelines of each of the magic videos used in our misdirection research. They are drawn from stills and illustrated by Allison Friebertshauser.
DOI: 10.6084/m9.figshare.1183448
title: Land use and surface water withdrawal effects on fish and macroinvertebrate assemblages in the Susquehanna River basin, USA

description: Water withdrawals in the Susquehanna River basin, USA, are increasing due to burgeoning shale gas extraction activities. In order to determine if flow alteration resulting from shale gas industry surface water withdrawals impacts fish and macroinvertebrate assemblages in lotic habitats, data were collected upstream and downstream of 12 withdrawal and three reference sites in headwater, cold water, and large warm water streams. Watershed size ranged from 4 to 517 km<sup>2</sup> and average daily withdrawals ranged from 0.05 to 1.4 million liters. Analysis of withdrawal data indicated that approved withdrawals far exceeded actual withdrawals across all stream types. The largest withdrawals relative to stream size were from headwater streams, where on average 6.8% of average daily flow was withdrawn daily. Fish and macroinvertebrate assemblage similarity at study sites depended largely on stream sampled, rather than position upstream or downstream of withdrawals. Regression techniques were employed to determine if catchment-level variables or withdrawal metrics best described variation in fish and macroinvertebrate metrics shown to be sensitive to flow alteration. The catchment-level variables were responsible for the majority of observed variation in fish metrics. Macroinvertebrate models performed poorly, indicating that the stream sampled or variables not included in the analyses were responsible for the majority of variation. Overall, evidence suggests impacts of shale gas withdrawals within the Susquehanna basin are limited at the present state of flow alteration. Potential reasons include protective measures such as pass-by flow restrictions, which require withdrawals to cease when flows drop below a predetermined low flow threshold, maximum instantaneous and daily withdrawal limits, and recent initiation of withdrawals (1–3 years of operation).
DOI: 10.6084/m9.figshare.1183476.v1
title: Stability, metastability and spectroscopic constants of electronic states of NH<sup>−</sup> and CH<sup>−</sup>

description: Highly correlated <i>ab initio</i> methods were used in order to calculate potential energy curves (PECs) of the bound electronic states of CH<sup>−</sup> and NH<sup>−</sup> anions and the long-range parts of their excited states. The spin–orbit interaction between electronic states has been calculated for the cases in which the couplings were assumed to be responsible for perturbations. The spectroscopic constants of bound states were calculated from the PECs and compared with previous theoretical and/or available experimental values. Also, from the ground states of CH/CH<sup>−</sup> and NH/NH<sup>−</sup>, the adiabatic electron affinities were given and discussed.
DOI: 10.6084/m9.figshare.1183434
title: Analysis of occludin trafficking, demonstrating continuous endocytosis, degradation, recycling and biosynthetic secretory trafficking

description: occludin recycling during epithelial polarisation
DOI: 10.6084/m9.figshare.1183448.v2
title: Land use and surface water withdrawal effects on fish and macroinvertebrate assemblages in the Susquehanna River basin, USA

description: Water withdrawals in the Susquehanna River basin, USA, are increasing due to burgeoning shale gas extraction activities. In order to determine if flow alteration resulting from shale gas industry surface water withdrawals impacts fish and macroinvertebrate assemblages in lotic habitats, data were collected upstream and downstream of 12 withdrawal and three reference sites in headwater, cold water, and large warm water streams. Watershed size ranged from 4 to 517 km<sup>2</sup> and average daily withdrawals ranged from 0.05 to 1.4 million liters. Analysis of withdrawal data indicated that approved withdrawals far exceeded actual withdrawals across all stream types. The largest withdrawals relative to stream size were from headwater streams, where on average 6.8% of average daily flow was withdrawn daily. Fish and macroinvertebrate assemblage similarity at study sites depended largely on stream sampled, rather than position upstream or downstream of withdrawals. Regression techniques were employed to determine if catchment-level variables or withdrawal metrics best described variation in fish and macroinvertebrate metrics shown to be sensitive to flow alteration. The catchment-level variables were responsible for the majority of observed variation in fish metrics. Macroinvertebrate models performed poorly, indicating that the stream sampled or variables not included in the analyses were responsible for the majority of variation. Overall, evidence suggests impacts of shale gas withdrawals within the Susquehanna basin are limited at the present state of flow alteration. Potential reasons include protective measures such as pass-by flow restrictions, which require withdrawals to cease when flows drop below a predetermined low flow threshold, maximum instantaneous and daily withdrawal limits, and recent initiation of withdrawals (1–3 years of operation).
DOI: 10.6084/m9.figshare.1183476.v3
title: Stability, metastability and spectroscopic constants of electronic states of NH<sup>−</sup> and CH<sup>−</sup>

description: Highly correlated <i>ab initio</i> methods were used in order to calculate potential energy curves (PECs) of the bound electronic states of CH<sup>−</sup> and NH<sup>−</sup> anions and the long-range parts of their excited states. The spin–orbit interaction between electronic states has been calculated for the cases in which the couplings were assumed to be responsible for perturbations. The spectroscopic constants of bound states were calculated from the PECs and compared with previous theoretical and/or available experimental values. Also, from the ground states of CH/CH<sup>−</sup> and NH/NH<sup>−</sup>, the adiabatic electron affinities were given and discussed.
DOI: 10.6084/m9.figshare.1183476.v2
title: Stability, metastability and spectroscopic constants of electronic states of NH<sup>−</sup> and CH<sup>−</sup>

description: Highly correlated <i>ab initio</i> methods were used in order to calculate potential energy curves (PECs) of the bound electronic states of CH<sup>−</sup> and NH<sup>−</sup> anions and the long-range parts of their excited states. The spin–orbit interaction between electronic states has been calculated for the cases in which the couplings were assumed to be responsible for perturbations. The spectroscopic constants of bound states were calculated from the PECs and compared with previous theoretical and/or available experimental values. Also, from the ground states of CH/CH<sup>−</sup> and NH/NH<sup>−</sup>, the adiabatic electron affinities were given and discussed.
DOI: 10.6084/m9.figshare.1183448.v1
title: Land use and surface water withdrawal effects on fish and macroinvertebrate assemblages in the Susquehanna River basin, USA

description: Water withdrawals in the Susquehanna River basin, USA, are increasing due to burgeoning shale gas extraction activities. In order to determine if flow alteration resulting from shale gas industry surface water withdrawals impacts fish and macroinvertebrate assemblages in lotic habitats, data were collected upstream and downstream of 12 withdrawal and three reference sites in headwater, cold water, and large warm water streams. Watershed size ranged from 4 to 517 km<sup>2</sup> and average daily withdrawals ranged from 0.05 to 1.4 million liters. Analysis of withdrawal data indicated that approved withdrawals far exceeded actual withdrawals across all stream types. The largest withdrawals relative to stream size were from headwater streams, where on average 6.8% of average daily flow was withdrawn daily. Fish and macroinvertebrate assemblage similarity at study sites depended largely on stream sampled, rather than position upstream or downstream of withdrawals. Regression techniques were employed to determine if catchment-level variables or withdrawal metrics best described variation in fish and macroinvertebrate metrics shown to be sensitive to flow alteration. The catchment-level variables were responsible for the majority of observed variation in fish metrics. Macroinvertebrate models performed poorly, indicating that the stream sampled or variables not included in the analyses were responsible for the majority of variation. Overall, evidence suggests impacts of shale gas withdrawals within the Susquehanna basin are limited at the present state of flow alteration. Potential reasons include protective measures such as pass-by flow restrictions, which require withdrawals to cease when flows drop below a predetermined low flow threshold, maximum instantaneous and daily withdrawal limits, and recent initiation of withdrawals (1–3 years of operation).
DOI: 10.6084/m9.figshare.1183434.v2
title: Analysis of occludin trafficking, demonstrating continuous endocytosis, degradation, recycling and biosynthetic secretory trafficking

description: occludin recycling during epithelial polarisation
DOI: 10.6084/m9.figshare.1183435.v1
title: R scripts for ms "Fitness costs in spatially structured environments"

description: R scripts to rerun the simulations and plot the figures of manuscript on "Fitness costs in spatially structured environments".
DOI: 10.6084/m9.figshare.1183434.v1
title: occludin recycling during epithelial polarisation

description: occludin recycling during epithelial polarisation