cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.17632/c6tyt3srsg.1
title: Data1 for Measuring Differences in Protein Allosteric Graphs Constructed via Molecular Dynamics Simulations

description: Molecular Dynamics Simulation Trajectory for the manuscript "Measuring Differences in Protein Allosteric Graphs Constructed via Molecular Dynamics Simulations"

1UBQ_WT_Charmm36m_trajectory_1.tar is used for the following sections: Different trajectory frame interval (timestep), Different significance threshold, and Different distance threshold.

1UBQ_WT_Charmm36m_trajectory_1.tar, 1UBQ_WT_Charmm36m_trajectory_2.tar, and 1UBQ_WT_Charmm36m_trajectory_3.tar are used for the Independent replicate simulations section.

1UBQ_WT_Charmm36m_trajectory_1.tar, 1UBQ_WT_Charmm36_trajectory.tar, and 1UBQ_WT_Amber_trajectory.tar are used for the Different force fields section.

1UBQ_WT_Charmm36m_trajectory_1.tar, 1UBQ_I3A_Charmm36m_trajectory.tar, 1UBQ_L15S_Charmm36m_trajectory.tar, 1UBQ_K33G_Charmm36m_trajectory.tar, 1UBQ_P38Q_Charmm36m_trajectory.tar, 1UBQ_E51D_Charmm36m_trajectory.tar, and 1UBQ_V70N_Charmm36m_trajectory.tar are used for the Different mutations section.
DOI: 10.25549/inscriptifact-ouc110814257
title: Copper Scroll

description: [Text Description:] ❧ list of buried treasure ❧ [Text or Publication Number Note:] 3Q15 Copper Scroll ❧ [Excavation Description:] Found during survey of cliffs at Qumran in March 1952 by Roland de Vaux and William Reed. ❧ [Medium:] Metal ❧ [Script Note:] Jewish ❧ [Physical Object Description:] 23 oxydized copper half-cylinder segments with incised letters
DOI: 10.25549/inscriptifact-ouc110814274
title: Copper Scroll

description: [Text Description:] ❧ list of buried treasure ❧ [Text or Publication Number Note:] 3Q15 Copper Scroll ❧ [Excavation Description:] Found during survey of cliffs at Qumran in March 1952 by Roland de Vaux and William Reed. ❧ [Medium:] Metal ❧ [Script Note:] Jewish ❧ [Physical Object Description:] 23 oxydized copper half-cylinder segments with incised letters
DOI: 10.25549/inscriptifact-ouc110820456
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820409
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820569
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820561
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820406
title: Persepolis Fortification Elamite Tablet 2272.101, Fort 2272.101

description: [Text Description:] Administrative text ❧ [Text or Publication Number Note:] Fort 2272.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. ❧ [Physical Object Note:] Upper left, upper right and lower right corners broken off. Damage on obverse, reverse.
DOI: 10.5683/sp3/nfejes
title: :unav

description: :unav
DOI: 10.5683/sp3/fqnmzz
title: Forum Research Political Poll – Federal Issues (Canada) 2014

description: This survey is a Canadian federal opinion poll with general political questions as well as focus questions.
DOI: 10.5683/sp3/quaorz
title: 1996 Census of Canada, Place of Work Status by Industry (Standard Industrial Classification 1980) at the Census Tract (CT) Level [custom tabulation]

description: This dataset is a custom tabulation of the 1996 Census of Canada containing statistics on work activity and place of work status in 1995 by industry, classified by the Standard Industrial Classification of 1980, at the census tract (CT) level.
description: Statistics Canada Custom Tabulations
description: This dataset is made available under the Statistics Canada Open Licence Agreement: https://www.statcan.gc.ca/eng/reference/licence. The dataset is in Beyond 20/20 (.ivt) format. The Beyond 20/20 browser is required in order to open it. This software can be freely downloaded from the Statistics Canada website: https://www.statcan.gc.ca/eng/public/beyond20-20 (Windows only).
DOI: 10.5683/sp3/6brzff
title: 2001 Census of Canada, Shelter Costs at the Dissemination Area (DA) Level in the City of Toronto Census Subdivision (CSD) [custom tabulation]

description: This dataset is a custom tabulation of the 2001 Census of Canada containing shelter cost statistics (rent, electricity, fuel, water and other municipal services, mortgage payments, property taxes and condominium fees) for private households in non-band non-farm non-reserve occupied private dwellings in the City of Toronto.
description: Statistics Canada Custom Tabulations
description: This dataset is made available under the Statistics Canada Open Licence Agreement: https://www.statcan.gc.ca/eng/reference/licence. The dataset is in Beyond 20/20 (.ivt) format. The Beyond 20/20 browser is required in order to open it. This software can be freely downloaded from the Statistics Canada website: https://www.statcan.gc.ca/eng/public/beyond20-20 (Windows only).
DOI: 10.5683/sp3/avmwac
title: Turkey Point Flux Station 1989 Forest (TP2)
title: Meteorological and flux data from the TP89 forest.

description: &lt;p&gt;The ON-TP89 site, also known as the CA-TP2 on Global Fluxnet and ON-WPP89 in some of the Fluxnet-Canada Research Network (FCRN)/Canadian Carbon Program (CCP) publications.&lt;/p&gt; &lt;p&gt;ON-TP89 is a young planted white pine (Pinus strobusL.) forest of the Turkey Point Flux Station. It was planted in 1989 (ON-TP89) on a former agricultural land. Meteorological and flux data collection was started in summer 1989. The data documented here includes carbon, water and energy fluxes and meteorological and
soil measurements. &lt;/p&gt; &lt;p&gt;A unique aspect of Turkey Point Flux Station is its geographic location between the boreal and the broadleaf deciduous forest transition zone. It provides an excellent opportunity to investigate and quantify the strength of the carbon sink or source for planted temperate conifer forests, and its sensitivity to seasonal and annual climate variability. Also white pine is an important species in the North American landscape, because of its ability to adapt to dry enviro
nments. It grows efficiently on nutrient poor, dry, sandy soils. Generally, it is the first woody species to flourish after a disturbance such as fire or clearing and over longer time periods helps more native forest species to establish through succession. White pine trees can live for about 350–400 years and their height may reach up to 45–60 m. These characteristics make white pine a preferred plantation (afforestation) species in eastern North America.
&lt;/p&gt; &lt;p&gt;Fluxes, meteorological and soil measurement conducted at this site help us to explore carbon sequestration potential of chronosequence of planted or afforested white pine stands in southern Ontario. The main objectives are (i) to make year-round measurements of energy, water vapour and carbon dioxide (CO2) fluxes and other meteorological variables over mature, middle-aged, young and seedling white pine plantation forests (established in 1939, 1974, 1989 and 2002) (ii) to relate gross ph
otosynthesis and respiration of this stand to environmental factors (iii) determine the effects of seasonal and inter-annual climate variability on net ecosystem productivity, and to better understand the processes of
production, storage and transport of soil CO2 and (iv) use these data to further improve process-based photosynthesis and respiration models.
&lt;/p&gt;
DOI: 10.5683/sp3/i3hpbo
title: Turkey Point Flux Station 1974 Forest (TP3)

description: &lt;p&gt;The ON-TP74 site, also known as the CA-TP3 on Global Fluxnet and ON-WPP74 in some of the Fluxnet-Canada Research Network (FCRN)/Canadian Carbon Program (CCP) publications.&lt;/p&gt; &lt;p&gt;ON-TP74 is the middle-age eastern white pine (Pinus strobusL.) forest of the Turkey Point Flux Station. It was planted in 1974 (ON-TP74) on cleared oak-savannah land. Meteorological and flux data collection was started in summer 2003. The data set documented here includes carbon, water and energy fluxes and meteorol
ogical and soil measurements. &lt;/p&gt; &lt;p&gt;A unique aspect of Turkey Point Flux Station is its geographic location between the boreal and the broadleaf deciduous forest transition zone. It provides an excellent opportunity to investigate and quantify the strength of the carbon sink or source for planted temperate conifer forests, and its sensitivity to seasonal and annual climate variability. Also white pine is an important species in the North American landscape, because of its ability to adapt to
dry environments. It grows efficiently on nutrient poor, dry, sandy soils. Generally, it is the first woody species to flourish after a disturbance such as fire or clearing and over longer time periods helps more native forest species to establish through succession. White pine trees can live for about 350–400 years and their height may reach up to 45–60 m. These characteristics make white pine a preferred plantation (afforestation) species in eastern North America.
&lt;/p&gt; &lt;p&gt;Fluxes, meteorological and soil measurement conducted at this site help us to explore carbon sequestration potential of chronosequence of planted or afforested white pine stands in southern Ontario. The main objectives are (i) to make year-round measurements of energy, water vapour and carbon dioxide (CO2) fluxes and other meteorological variables over mature, middle-aged, young and seedling white pine plantation forests (established in 1939, 1974, 1989 and 2002) (ii) to relate gross ph
otosynthesis and respiration of this stand to environmental factors (iii) determine the effects of seasonal and inter-annual climate variability on net ecosystem productivity, and to better understand the pro
cesses of production, storage and transport of soil CO2 and (iv) use these data to further improve process-based photosynthesis and respiration models.
&lt;/p&gt;
DOI: 10.5683/sp3/m4amgv
title: Turkey Point Flux Station 1939 Forest (TP4)

description: &lt;p&gt;The ON-TP39 site, also known as the CA-TP4 on Global Fluxnet and ON-WPP39 in some of the Fluxnet-Canada Research Network (FCRN)/Canadian Carbon Program (CCP) publications.&lt;/p&gt; &lt;p&gt;ON-TP39 is the mature eastern white pine (Pinus strobusL.) forest of the Turkey Point Flux Station. It was planted in 1939 (ON-TP39) on cleared oak-savannah land. Meteorological data collection was started in late autumn 2001 and flux measurements were started in June 2002. The data set documented here includes carb
on, water and energy fluxes and meteorological and soil measurements.
&lt;/p&gt; &lt;p&gt;A unique aspect of Turkey Point Flux Station is its geographic location between the boreal and the broadleaf deciduous forest transition zone. It provides an excellent opportunity to investigate and quantify the strength of the carbon sink or source for planted temperate conifer forests, and its sensitivity to seasonal and annual climate variability. Also white pine is an important species in the North American landscape, because of its ability to adapt to dry environments. It grows eff
iciently on nutrient poor, dry, sandy soils. Generally, it is the first woody species to flourish after a disturbance such as fire or clearing and over longer time periods helps more native forest species to establish through succession. White pine trees can live for about 350–400 years and their height may reach up to 45–60 m. These characteristics make white pine a preferred plantation (afforestation) species in eastern North America.
&lt;/p&gt; &lt;p&gt;Fluxes, meteorological and soil measurement conducted at this site help us to explore carbon sequestration potential of chronosequence of planted or afforested white pine stands in southern Ontario. The main objectives are (i) to make year-round measurements of energy, water vapour and carbon dioxide (CO2) fluxes and other meteorological variables over mature, middle-aged, young and seedling white pine plantation forests (established in 1939, 1974, 1989 and 2002) (ii) to relate gross ph
otosynthesis and respiration of this stand to environmental factors (iii) determine the effects of seasonal and inter-annual climate variability on net ecosystem produc
tivity, and to better understand the processes of production, storage and transport of soil CO2 and (iv) use these data to further improve process-based photosynthesis and respiration models.
&lt;/p&gt;
DOI: 10.5683/sp3/isgyq9
title: Turkey Point Flux Station 2002 Forest (TP1)

description: &lt;p&gt;The ON-TP02 site, also known as the CA-TP1 on Global Fluxnet and ON-WPP02 in some of the Fluxnet-Canada Research Network (FCRN)/Canadian Carbon Program (CCP) publications.&lt;/p&gt; &lt;p&gt;ON-TP02 is a recently planted white pine (Pinus strobusL.) forest of the Turkey Point Flux Station. It was planted in 2002 (ON-TP02) on a former agricultural land. Meteorological and flux data collection was started in summer 2002. The data set documented here includes carbon, water and energy fluxes and meteorologi
cal and soil measurements. &lt;/p&gt; &lt;p&gt;A unique aspect of Turkey Point Flux Station is its geographic location between the boreal and the broadleaf deciduous forest transition zone. It provides an excellent opportunity to investigate and quantify the strength of the carbon sink or source for planted temperate conifer forests, and its sensitivity to seasonal and annual climate variability. Also white pine is an important species in the North American landscape, because of its ability to adapt to dry
environments. It grows efficiently on nutrient poor, dry, sandy soils. Generally, it is the first woody species to flourish after a disturbance such as fire or clearing and over longer time periods helps more native forest species to establish through succession. White pine trees can live for about 350–400 years and their height may reach up to 45–60 m. These characteristics make white pine a preferred plantation (afforestation) species in eastern North America.
&lt;/p&gt; &lt;p&gt;Fluxes, meteorological and soil measurement conducted at this site help us to explore carbon sequestration potential of chronosequence of planted or afforested white pine stands in southern Ontario. The main objectives are (i) to make year-round measurements of energy, water vapour and carbon dioxide (CO2) fluxes and other meteorological variables over mature, middle-aged, young and seedling white pine plantation forests (established in 1939, 1974, 1989 and 2002) (ii) to relate gross ph
otosynthesis and respiration of this stand to environmental factors (iii) determine the effects of seasonal and inter-annual climate variability on net ecosystem productivity, and to better understand the processes of production, storage and transport of soil CO2 and (iv) use these data to further improve process-based photosynthesis and respiration models.
&lt;/p&gt; &lt;p&gt;More information about the site and associated data can be found in the metadata documentation.&lt;/p&gt;
DOI: 10.5683/sp3/finmqv
title: International iSquare Study

description: During summer 2014, the Toronto-based iSquare team and eleven international collaborators launched a project to explore visual conceptions of information worldwide. Participants implemented the iSquare protocol to collect drawings of information from their classrooms. Altogether, the far flung team generated 541 "international iSquares" and is now conducting visual content analysis to characterize the drawings. Findings will be reported at conferences and in journals of information studies in 2016.
DOI: 10.5683/sp3/cblivt
title: Interdisciplinary iSquare Study

description: iSquares were collected from several Faculties across the University of Toronto in order to investigate the impact of academic cultures on visual conceptions of information.
DOI: 10.5683/sp3/elykst
title: Paleo-perspectives on environmental change in the high Arctic: the Canadian Contribution

description: Background: The snow and ice of the polar regions contain a wealth of information on the variability of the Earth's climate, past and present, and atmospheric composition. Many of the chemical compounds and aerosols found in the atmosphere find their way to the Arctic and are retained by the snow. Within large ice caps and ice sheets, annual snow layers accumulate. At depth, these layers are transformed into ice; preserving in the process much of their environmental signature. Thus, through ice core analysis, a glimpse of the pre-industrial atmosphere is offered, allowing us to place recent changes into perspective. Objectives: This project consists of three sub-projects which are closely linked in theme and method. Collectively, their aim is to document and reconstruct short and long term changes in climate and atmospheric contaminant deposition in the Canadian Arctic and neighbouring regions by analysing snow and ice cores. 1. Trends in the distribution of anthropogenic contaminants in the circumpolar region, is to conduct a pan Arctic survey of Arctic snow in order to quantify present levels and rates of accumulation of airborne contaminants. This activity is associated with the internationally approved COPOL program (IPY # 175) and with two Environment Canada-led IPY programs: (1) OASIS-CANADA: Understanding Ozone and Mercury in the Air Over the Arctic Ocean and (2) Pollutants Travelling in the Air to the Arctic. 2. Paleo-perspectives on environmental change in the High A
rctic is closely associated to the study described above. The aim is to extend the record of atmospheric mercury and trace metals by sampling snow from a deep pit and from firn cores. Also included in this study the measurement of melt features observed in the snow. 3. Greenland Ice Sheet reactions to past and present climate change is to further explore the links between trace elements, pollen assemblages, and climate - particularly during glacial, interglacial, and transitional periods. To that end, we have joined the large-scale, multi-national, ice coring program: North Greenland Eemian Ice Drilling (NEEM). Rationale: The results of the project are important to the study of long-range / transboundary dispersion of airborne contaminants in the Arctic, thus, to the health of Northerners. Also to improve our understanding of the physical processes that control the transfer of Hg and methyl mercury (MeHg) from snow to aquatic ecosystems in glacierized basins.
description: Type: Research Program: Notes: IPY-Paleoenvironmental Change, Canadian Arctic This metadata record corresponds to an IPY project. Studies completed under this research project are identified as related materials. These studies can also be retrieved using the Polar Data Catalogue.;
DOI: 10.5683/sp3/qeptpp
title: Arctic Wildlife Observatories Linking Vulnerable EcoSystems (ArcticWOLVES)

description: Extensive monitoring of the abundance, timing and success of reproduction, habitat use and diet of key wildlife species (primarily geese, small mammals, shorebirds, avian predators and mammalian predators like foxes and weasels), as well as annual plant production and arthropod diversity and abundance, was conducted at most sites from 2007 to 2009. Our results provide increasing evidence that predation plays a dominant role in the functioning of Arctic terrestrial ecosystems. At one site, less than 10% of the annual primary production was consumed by herbivores but up to 50% of the herbivore production was consumed by predators. The latter proportion also increased over the past two decades, suggesting a strengthening of top-down effects in this food web. Winter habitat quality appears to be a key factor in the population dynamics of lemmings, the primary prey of most tundra predators. Deep snow provides insulation from the cold air temperature, protection from predators and allows winter reproduction, upon which depend the periodic population irruptions of small mammals. However, deep snow is spatially uncommon in the Arctic, thus the distribution and spatial extent of good quality winter habitat may be limiting population irruptions in some regions or years. Radio-tracking of tundra predators such as snowy owls and arctic foxes revealed that they travel over very large areas and they can extensively use the marine ecosystem during winter, when terrestrial food resources are scarce. Snowy owls in particular display a remarkab
le nomadism when searching for suitable nesting sites in spring and an outstanding ability to find locally abundant lemming populations, which may contribute to the regional synchrony of lemming population dynamics. We found evidence that the strength of predation decreases with latitude. Using artificial birds¿ nests, we showed that risk of predation decreases by as much as 66% between 53 and 82 N latitude (a 3,400 km distance). We also found that soil-plant-herbivore interactions are quite sensitive to climate warming. On the one hand, earlier thaw or increasing freeze-thaw cycles will likely result in a loss of soil nutrients in some wetland ecosystems, leading to a decrease in plant production and food resource for herbivores. On the other hand, earlier and warmer springs could have a negative impact on the synchrony between the reproductive phenology of herbivores and plant growth, leading to reduced annual production.
description: Type: Research Program: Notes: IPY-ArcticWOLVES This metadata record corresponds to an IPY project. Studies completed under this research project are identified as related materials. These studies can also be retrieved using the Polar Data Catalogue.;