cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6073/pasta/2e47c88979f85679e8f356a6a5901eb6
title: Eight Mile Lake Research Watershed, Carbon in Permafrost Experimental Heating Research (CiPEHR): Seasonal water table depth data, 2012-2022

description: The Carbon in Permafrost Experimental Heating Research (CiPEHR) project addresses the following questions: 1) Does ecosystem warming cause a net release of C from the ecosystem to the atmosphere?, 2) Does the decomposition of old C, that comprises the bulk of the soil C pool, influence ecosystem C loss?, and 3) How do winter and summer warming alone, and in combination, affect ecosystem C exchange? We are answering these questions using a combination of field and laboratory experiments to measure ecosystem carbon balance and radiocarbon isotope ratios at a warming experiment located in an upland tundra field site near Healy, Alaska in the foothills of the Alaska Range. This data includes water table depth measurements collected from winter warming and control treatment plots at CiPEHR for the ice-free period of 2012-2020.
DOI: 10.6073/pasta/2cf763b7e232218f567a5fb2fcdb2ba1
title: Eight Mile Lake Research Watershed, Thaw Gradient: Seasonal water table depth from 2004-2022

description: In this larger study, we are asking the question: Is old carbon that comprises the bulk of the soil organic matter pool released in response to thawing of permafrost? We are answering this question by using a combination of field and laboratory experiments to measure radiocarbon isotope ratios in soil organic matter, soil respiration, and dissolved organic carbon, in tundra ecosystems. The objective of these proposed measurements is to develop a mechanistic understanding of the SOM sources contributing to C losses following permafrost thawing. We are making these measurements at an established tundra field site near Healy, Alaska in the foothills of the Alaska Range. Field measurements center on a natural experiment where permafrost has been observed to warm and thaw over the past several decades. This area represents a gradient of sites each with a different degree of change due to permafrost thawing. As such, this area is unique for addressing questions at the time and spatial scales relevant for change in arctic ecosystems.
DOI: 10.6073/pasta/709d2d7f3f6002788f2762a74d0d237b
title: Eight Mile Lake Research Watershed, Carbon in Permafrost Experimental Heating and Drying Research (DryPEHR): NDVI 2011-2022

description: This drying and warming experiment addresses the following questions: 1) Does ecosystem drying, warming and permafrost thaw cause a net release or uptake of C from the ecosystem to the atmosphere?, 2) Does the decomposition of old C that comprises the bulk of the soil C pool influence ecosystem C loss? 3) How do drying and warming affect plant communities and ecosystem properties? We are answering these questions using a combined warming and drying experiment (DryPEHR), which is situated with the Carbon in Permafrost Experimental Heating Research (CiPEHR) project and located in an upland tundra field site near Healy, Alaska in the foothills of the Alaska Range. Warming treatment here refers to growing season air temperature warming (~1C) using open top chambers (OTC) combined with soil 'warming' using snow fences during the snow covered months. Drying is achieved using an automated pumping system that lowers the water table in the dry plots. Soil warming began in 2008; OTCs and drying in 2011.The Normalized Difference Vegetation Index (NDVI) was measured using a specialized handheld camera at individual plots throughout the 2011-2018 growing season.
DOI: 10.6073/pasta/cf7914a5c78d1a652377df0e5cde2069
title: Eight Mile Lake Research Watershed, Carbon in Permafrost Experimental Heating Research (CiPEHR): NDVI 2009-2022

description: The Carbon in Permafrost Experimental Heating Research (CiPEHR) project addresses the following questions: 1) Does ecosystem warming cause a net release of C from the ecosystem to the atmosphere?, 2) Does the decomposition of old C, that comprises the bulk of the soil C pool, influence ecosystem C loss?, and 3) How do winter and summer warming alone, and in combination, affect ecosystem C exchange? We are answering these questions using a combination of field and laboratory experiments to measure ecosystem carbon balance and radiocarbon isotope ratios at a warming experiment located in an upland tundra field site near Healy, Alaska in the foothills of the Alaska Range.The Normalized Difference Vegetation Index (NDVI) was measured using a specialized handheld camera at individual plots throughout the growing seasons.
DOI: 10.6073/pasta/01f9e12e457a4f1b370b4641ebe0baef
title: Eight Mile Lake Research Watershed, Thaw Gradient: NDVI 2013-2022

description: This drying and warming experiment addresses the following questions: 1) Does ecosystem drying, warming and permafrost thaw cause a net release or uptake of C from the ecosystem to the atmosphere?, 2) Does the decomposition of old C that comprises the bulk of the soil C pool influence ecosystem C loss? 3) How do drying and warming affect plant communities and ecosystem properties? We are answering these questions using a combined warming and drying experiment (DryPEHR), which is situated with the Carbon in Permafrost Experimental Heating Research (CiPEHR) project and located in an upland tundra field site near Healy, Alaska in the foothills of the Alaska Range. Warming treatment here refers to growing season air temperature warming (~1C) using open top chambers (OTC) combined with soil 'warming' using snow fences during the snow covered months. Drying is achieved using an automated pumping system that lowers the water table in the dry plots. Soil warming began in 2008; OTCs and drying in 2011.The Normalized Difference Vegetation Index (NDVI) was measured using a specialized handheld camera at individual plots throughout the 2011-2018 growing seasons.
DOI: 10.25549/usctheses-ouc113763577
title: Exploring experiences of minority-stress and alcohol use among sexual minorities using articulated thoughts in simulated situations: a proof of concept study
DOI: 10.25549/usctheses-ouc113763478
title: Externalized reasoning in language models for scalable and trustworthy AI
DOI: 10.25549/usctheses-ouc113763477
title: Document understanding based design support (DocUDS) for augmenting engineering design
DOI: 10.25549/usctheses-ouc113763529
title: Unreal engine testbed for computer vision of tall lunar tower assembly
DOI: 10.25549/usctheses-ouc113763528
title: Effects of electronic cigarettes on viability and proliferation of lung mesenchymal stem cells
DOI: 10.25549/usctheses-ouc113763098
title: Exploring the genomic landscape of giant kelp: biotechnological implications and sustainable development
DOI: 10.25549/usctheses-ouc113763620
title: Multi-modal preconditioned inference of commonsense knowledge
DOI: 10.25549/usctheses-ouc113763618
title: Silencing to belonging: the institutionalization of Black girls in public schools
DOI: 10.25549/usctheses-ouc113763615
title: Development of methods and novel crosslinkers for RNA structure and interaction studies in living cells
DOI: 10.6073/pasta/cdb948b89569ac26816cd37d1f1417d6
title: Litterfall and Hare Pellet Summary at Bonanza Creek LTER Control Plots (1985 - Present)

description: Litterfall weights and Hare Pellet counts at LTER Control Plots within the Bonanza Creek Experimental Forest and the Caribou Poker Creek Research Watershed.
DOI: 10.12770/10b71300-286b-11e0-baa5-005056987263
title: Mosaïque d'imagerie acoustique de la marge des Entrées de la Manche, campagne Sedimanche 1 (édition 1995, résolution 62.5m)

description: Mosaïque d'imagerie acoustique de la marge des Entrées de la Manche. La résolution de l'image est de 62.5 mètres.Les données ont été acquises lors de la campagne océanographique Sedimanche 1 en 1992 par sondeur multifaisceaux EM12D.
DOI: 10.12770/37b2d4a0-c487-11df-a9b6-005056987263
title: Bathy-morphologie de la marge des Entrées de la Manche - campagne Sedimanche 1 (édition 1995, résolution 200m)

description: Modèle bathymétrique (MNT) de la marge des Entrées de la Manche. Les données ont été acquises lors de la campagne océanographique Sedimanche 1 en 1992, avec le sondeur bathymétrique EM12D.Le pas de la grille est de 200m.
DOI: 10.6073/pasta/3df3761394c8a21f3e362e0483ee6618
title: Eight Mile Lake Research Watershed, Carbon in Permafrost Experimental Heating and Drying Research (DryPEHR): Weekly thaw depth data, 2011-2022

description: This drying and warming experiment addresses the following questions: 1) Does ecosystem drying, warming and permafrost thaw cause a net release or uptake of C from the ecosystem to the atmosphere?, 2) Does the decomposition of old C that comprises the bulk of the soil C pool influence ecosystem C loss? 3) How do drying and warming affect plant communities and ecosystem properties? We are answering these questions using a combined warming and drying experiment (DryPEHR), which is situated with the Carbon in Permafrost Experimental Heating Research (CiPEHR) project and located in an upland tundra field site near Healy, Alaska in the foothills of the Alaska Range. Warming treatment here refers to growing season air temperature warming (~1C) using open top chambers (OTC) combined with soil 'warming' using snow fences during the snow covered months. Drying is achieved using an automated pumping system that lowers the water table in the dry plots. Soil warming began in 2008; OTCs and drying in 2011. This data set includes weekly ground thaw measurements.
DOI: 10.6073/pasta/9ca990f8513157a6fa42183bcc485a3b
title: Eight Mile Lake Research Watershed, Carbon in Permafrost Experimental Heating Research (CiPEHR): Weekly thaw depth data, 2009-2022

description: The Carbon in Permafrost Experimental Heating Research (CiPEHR) project addresses the following questions: 1) Does ecosystem warming cause a net release of C from the ecosystem to the atmosphere?, 2) Does the decomposition of old C, that comprises the bulk of the soil C pool, influence ecosystem C loss?, and 3) How do winter and summer warming alone, and in combination, affect ecosystem C exchange? We are answering these questions using a combination of field and laboratory experiments to measure ecosystem carbon balance and radiocarbon isotope ratios at a warming experiment located in an upland tundra field site near Healy, Alaska in the foothills of the Alaska Range. This data set includes weekly thaw depth measurements collected from winter warming, summer warming, and control treatment plots at CiPEHR. Additional measurements from on-plot gas flux wells, water table monitoring wells, and off-plot locations are also reported.
DOI: 10.12770/70643254-a6b8-4511-85b6-3784b1cf0377
title: Grande vasière - golfe de Gascogne (J-F. Bourillet, 2006)

description: Contours et définition de la grande vasière dans le golfe de Gascogne, basés sur la "Carte des sédiments superficiels du plateau continental du golfe de Gascogne - partie septentrionale" (échelle 1/500 000, BRGM / Ifremer, 1986). La grande vasière au sens strict comprend les secteurs "vase &gt; 75 %", "vase &gt; 25 %" et "vase lithoclastique &lt; 25 %". La grande vasière au sens large comprend ces trois secteurs, auxquels sont ajoutés les secteurs "vase carbonatée &lt; 25%". Campagne océanographique à l'origine de cette donnée : - HILY Christian, BOURILLET Jean-François (2002) TROPHAL I cruise, RV Le Suroît, https://doi.org/10.17600/2020050 Références bibliographiques : - Bourillet Jean-Francois, Jouanneau J.M., Macher Claire, Le Hir Pierre, Naughton F (2006). "La Grande Vasière" mid-shelf mud belt : Holocene sedimentary structure, natural and anthropogenic impacts. X International Symposium on Oceanography of the Bay of Biscay, April 19-21 2006. Vigo, Galicia. Spain. https://archimer.ifremer.fr/doc/00000/6243/ - BOUYSSE P., LESUEUR P. et KLINGEBIEL A., 1986. Carte des sédiments superficiels du plateau continental du Golfe de Gascogne - Partie septentrionale. Echelle 1/500 000. coédition BRGM / Ifremer.
DOI: 10.25919/wsrz-3x80
title: Comparative transcriptomic heat stress responses data for native Australian Acacia species: supplementary data and R code

description: To improve our understanding of heat tolerance across related species from diverse climates, we cultivated a selection of Acacia species in a controlled environment, using seed sourced from wild populations that occupy a wide range of Australian climates. After four months of growth in control temperature conditions (ca 24 °C day and 18 °C night) plants were exposed to a four-day heatwave (38 °C day and 26 °C night). Heatwave responses were quantified with coupled measurements of the transcriptome (gene expression) and PHT acclimation. Samples for transcriptomics were taken across three days: one day prior to heatwave (control), at the onset of heatwave conditions (Day 1) and at the end of the heatwave (Day 4). Accompanying measurements of PHT were taken the day prior and at day four using basal chlorophyll fluorescence. This Collections includes RNA-seq metadata and cleaned expression data for data analysis (.rds file) and the associated Rmarkdown file (.Rmd file) to run analyses from our paper.
DOI: 10.6073/pasta/623bed20c4ec447a73f6c5e632f5b120
title: Eight Mile Lake Research Watershed, Thaw Gradient: half-hourly soil moisture 2010-2022

description: In this larger study, we are asking the question: Is old carbon that comprises the bulk of the soil organic matter pool released in response to thawing of permafrost? We are answering this question by using a combination of field and laboratory experiments to measure radiocarbon isotope ratios in soil organic matter, soil respiration, and dissolved organic carbon, in tundra ecosystems. The objective of these proposed measurements is to develop a mechanistic understanding of the SOM sources contributing to C losses following permafrost thawing. We are making these measurements at an established tundra field site near Healy, Alaska in the foothills of the Alaska Range. Field measurements center on a natural experiment where permafrost has been observed to warm and thaw over the past several decades. This area represents a gradient of sites each with a different degree of change due to permafrost thawing. As such, this area is unique for addressing questions at the time and spatial scales relevant for change in arctic ecosystems. This data set includes soil moisture intergrate over a 20cm soil profile at different locations within gradient of sites described.
DOI: 10.6073/pasta/b76350cd13d41bed35a04ad479a3d6dd
title: Bonanza Creek LTER: Hourly Precipitation Weighing Bucket Measurements from 2008 to Present in the Caribou-Poker Creeks Research Watershed near Fairbanks, Alaska

description: This data set includes year round precipitation values from sampling buckets filled with antifreeze to melt and prevent snow build up. While these sensors work year round, tipping bucket data seems more accurate for snow free periods.
DOI: 10.26180/24521446
title: RNAseq from P4 murine whole kidneys with Polycystic Kidney Disease

description: Snap frozen Postnatal day4 murine kidney tissues were crushed using micropestles in RLT Buffer and RNA was extracted from these tissues using QiaShredders followed by Qiagen RNAeasy Mini Kits according to manufacturer’s protocol. RNA concentration and integrity were determined by Aligent bioanalyzer. cDNA library preparation was carried out using NEB Next Ultra Directional RNA Library Prep Kit for Illumina RNA sequencing (E7420S) and sequenced on an Illumina HiSeqX10 machine in 150 bp paired end format. Sequence data was processed with Skewer adaptor trimmer and mapped with HiSat2 to the <i>Mus musculus</i> GRCm38_v90 genome assembly. The resulting Bam files are provided here.<br>Samples were from Control Cre (<b><i>Hoxb7-cre</i></b><i>)</i> mice, <i>Aurka flox/flox; Hoxb7-cre</i> (<i>Aurka</i> Knockout Out -<b>AKO</b>) mice, <i>Inpp5e flox/flox; Hoxb7-cre</i> (<i>Inpp5e</i> Knockout Out -<b>IKO</b>) mice, <i>Pkd1 flox/flox; Hoxb7-cre</i> (<i>Pkd1</i> Knockout Out -<b>PKO</b>) mice, <i>Inpp5e flox/flox; Aurka flox/flox; Hoxb7-cre</i> (<i>Inpp5e and Aurka</i><i> </i>double Knockout Out -<b>dKO-I</b>) mice, and <i>Pkd1 flox/flox; Aurka flox/flox; Hoxb7-cre</i> (<i>Pkd1 and Aurka</i><i> </i>double Knockout Out -<b>dKO-P</b>) mice.<br>Hoxb7-cre mediated deletion of floxed alleles specifically in the kidney collecting ducts.Inpp5e KO results in Polycystic Kidney Disease related to Joubert Syndrome.Pkd1 KO results in Autosomal Dominant Polycystic Kidney disease.Aurka KO had no phenotype and appeared normal.Hoxb7-cre control animals had no phenotype and appeared normal.Both Inpp5e and Aurka, and Pkd1 and Aurka double knockout mice exhibited a rescue in disease.<br>Sample labels abbreviated to groups as bolded above.<br>
DOI: 10.26180/24521446.v1
title: Bam and BAI files

description: Sequence data was processed with Skewer adaptor trimmer and mapped with HiSat2 to the <i>Mus musculus</i> GRCm38_v90 genome assembly. The resulting Bam files are provided here.
DOI: 10.34740/kaggle/dsv/6940802
title: BBC News
DOI: 10.6073/pasta/b5cd1b8e568a5eff760b45436f5d296f
title: Eight Mile Lake Research Watershed, Thaw Gradient: half-hourly soil temperature 2004-2022

description: In this larger study, we are asking the question: Is old carbon that comprises the bulk of the soil organic matter pool released in response to thawing of permafrost? We are answering this question by using a combination of field and laboratory experiments to measure radiocarbon isotope ratios in soil organic matter, soil respiration, and dissolved organic carbon, in tundra ecosystems. The objective of these proposed measurements is to develop a mechanistic understanding of the SOM sources contributing to C losses following permafrost thawing. We are making these measurements at an established tundra field site near Healy, Alaska in the foothills of the Alaska Range. Field measurements center on a natural experiment where permafrost has been observed to warm and thaw over the past several decades. This area represents a gradient of sites each with a different degree of change due to permafrost thawing. As such, this area is unique for addressing questions at the time and spatial scales relevant for change in arctic ecosystems. This data set includes soil temperature at multiple depths in the profile at different locations within gradient of sites described.
DOI: 10.34740/kaggle/dsv/6940806
title: Youtube Trending Video - Taiwan & Hong Kong
DOI: 10.5281/zenodo.10108985
title: lepidocolaptes_lacrymiger_zanfona_1.fasta.gz

description: lepidocolaptes_lacrymiger_zanfona_1.fasta.gz
DOI: 10.5281/zenodo.10108984
title: lepidocolaptes_lacrymiger_zanfona_1.fasta.gz

description: lepidocolaptes_lacrymiger_zanfona_1.fasta.gz
DOI: 10.6084/m9.figshare.24546388
title: <b>16s RNA sequencing data of gut microbiota in postmenopausal women from shanghai, china</b>

description: This study aimed to identify whether and how the gut microbiome of postmenopausal women with osteoporosis and osteopenia may differ from that of healthy individuals.Fecal samples were collected from 27 individuals with osteoporosis (OP), 44 individuals with osteopenia (ON), and 23 normal controls (NC). The composition of the gut microbial community was analyzed by 16S rRNA gene sequencing.
DOI: 10.6084/m9.figshare.24546388.v1
title: <b>16s RNA sequencing data of gut microbiota in postmenopausal women from shanghai, china</b>

description: This study aimed to identify whether and how the gut microbiome of postmenopausal women with osteoporosis and osteopenia may differ from that of healthy individuals.Fecal samples were collected from 27 individuals with osteoporosis (OP), 44 individuals with osteopenia (ON), and 23 normal controls (NC). The composition of the gut microbial community was analyzed by 16S rRNA gene sequencing.
DOI: 10.25668/4w6k-9h23
title:  Full Disk Observations from the Third-Generation Magnetograph at MWO

description: This dataset contains daily full disk maps of intensity, longitudinal magnetic field, and Doppler velocity acquired by the third-generation magnetograph at Mount Wilson Observatory‘s 150 ft. tower telescope. The telescope, spectrograph, and magnetograph are described in Howard, R.: 1974, “Studies of solar magnetic fields. I: The average field strengths“, Solar Physics, 38, issue 2, 283–299, DOI: 10.1007/BF00155067. Doppler velocity reduction is described in Ulrich et al.: 2023, ” Photospheric Velocities Measured at Mt. Wilson Show Rotational and Poleward Velocity Deviations Compose the Torsional Oscillations“, Solar Physics, 298:123, DOI: 10.1007/s11207-023-02215-5
DOI: 10.6084/m9.figshare.22304110
title: LPD Interview and Survey Data

description: <b>Aim of the research project</b>: The study aims to develop a cloud-based ‘end-user-oriented design’ (EOD) platform to facilitate real-time communication and exchange between building designers and end-users to promote sustainability and minimize abortive works in high-rise residential buildings in Hong Kong.
DOI: 10.6084/m9.figshare.22304110.v1
title: LPD Interview and Survey Data

description: <b>Aim of the research project</b>: The study aims to develop a cloud-based ‘end-user-oriented design’ (EOD) platform to facilitate real-time communication and exchange between building designers and end-users to promote sustainability and minimize abortive works in high-rise residential buildings in Hong Kong.
DOI: 10.34740/kaggle/dsv/6941091
title: WallStreetBets 2022
DOI: 10.6084/m9.figshare.24546835
title: Data for "A Forward Method for Obtaining Numerical Solution of True Total Contribution Area (TCA) for Synthetic Surface Based on Pixel De-composition and Slope Line"

description: The DEMs discretized from different synthetic surfaces. Three types of synthetic surfaces are involved in this datasets, and four sets of parameters are considered for each type of synthetic surface.
DOI: 10.6084/m9.figshare.24546835.v1
title: Data for "A Forward Method for Obtaining Numerical Solution of True Total Contribution Area (TCA) for Synthetic Surface Based on Pixel De-composition and Slope Line"

description: The DEMs discretized from different synthetic surfaces. Three types of synthetic surfaces are involved in this datasets, and four sets of parameters are considered for each type of synthetic surface.