cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.11971371.v2
title: CBD-IL-12

description: Installing collagen affinity to IL-12 improves efficacy and toxicity of IL-12.
DOI: 10.3886/e113715v1-22947
title: Replication data for: Do Risk Preferences Change? Evidence from the Great East Japan Earthquake

description: We investigate whether individuals' risk preferences change after experiencing a natural disaster, specifically, the 2011 Great East Japan Earthquake. Exploiting the panels of nationally representative surveys on risk preferences, we find that men who experienced greater intensity of the earthquake became more risk tolerant a year after the Earthquake. Interestingly, the effects on men's risk preferences are persistent even five years after the Earthquake at almost the same magnitude as those shortly after the Earthquake. Furthermore, these men gamble more, which is consistent with the direction of changes in risk preferences. We find no such pattern for women.
DOI: 10.6084/m9.figshare.11971371.v3
title: CBD-IL-12

description: Installing collagen affinity to IL-12 improves efficacy and toxicity of IL-12.
DOI: 10.14469/hpc/6949
title: 1D NMR profiles in urine

description: Nuclear Magnetic Resonance Spectroscopy of urine acquired at 600 MHz with Bruker Ascend 600 magnets and Avance III HD consoles configured to the Bruker IVDr specification (Bruker Corporation, Billerica, MA, USA). Methanol and Water intervals and the two ends of the spectrum have been removed, and all spectra aligned by the Recursive Segment-wise Peak Alignment (RSPA) algorithm
DOI: 10.5066/p9lw817k
title: Data Release for Geologic Map of Petroglyph National Monument and Vicinity, Bernalillo County, New Mexico

description: This geologic map depicts and briefly describes geologic units underlying Petroglyph National Monument and immediately adjacent areas in Bernalillo County, New Mexico. The Monument is underlain dominantly by Quaternary basalts of the Albuquerque Volcanoes volcanic field, a series of basin-filling volcanic flows and associated vents from a monogenetic volcanic highland along the eastern margin of the Llano de Albuquerque. This compilation builds on data of previously published geologic maps and reports but includes new interpretive synthesis of volcanic stratigraphy and a unified representation of Quaternary surficial deposits overlying volcanic deposits within the Monument and areas immediately adjacent. This geologic map emphasizes the distribution of Quaternary volcanic vent areas and lava flow deposits which were incompletely mapped on previous publications. Surficial deposits are simplified, but uniformly mapped and described in contrast to varying map unit distributions, names and descriptions presented in the references above. Underlying deposits of the upper Santa Fe Group are exposed in the western part of the map area and described briefly. North-trending, syn- and post-eruption faulting is well preserved in the volcanic field and reflected in the subsurface models of aeromagnetic data. These faults are dominated by dip-slip displacement and are interpreted as extensional faults of the central Albuquerque Basin of the northern Rio Grande rift. Elongate distribution of vents for most of the volcanic deposits are spatially associated with the easternmost of these faults and are interpreted to reflect eruptions from fissures paralleling the regional extensional fault trends of the rift.
DOI: 10.5281/zenodo.3706834
title: Juno Waves Detection of Dust Impacts near Jupiter

description: This is the supporting data set for the paper by the same title published in AGU JGR Space Physics. DOI 10.1029/2019JE006367 Abstract: The Juno spacecraft entered orbit at Jupiter on July 5, 2016. Since then, Juno has orbited Jupiter in high inclination orbits, crossing the ring plane near perijove 21 times. During 20 of the 21 crossings, the Waves instrument detected signals induced by dust impacts. The impact rate profiles show peaks of order 6/s around the ring plane with half width at half max ~2000-3000 km. The polarity ratio of the impact signals didn't follow the areas of the antennas exposed to dust impacts that change due to the rotation of the spacecraft, suggesting Waves detects impacts on the Juno spacecraft and not just on the Waves antennas. The impact rate profile changed during Perijove 19, when the spacecraft rotation axis was tilted to the south, increasing the area of the solar panels exposed to impacts, indicating that the detected impacts were on the spacecraft body. Grain sizes of order 1 micrometer are estimated, and the differential size distribution has a slope of -5.1. Notes on zip archive: There are subdirectories for each figure including a PDF of the figure and one or more text files with the data supporting the figure. Where the labeling in the text file is not quite complete, we've added a Fign-readme.txt file. Figures 9 and 10 are in the same directory as the two figures just have more of the same and all the data for both figures is in the same file.
DOI: 10.5281/zenodo.3706835
title: Juno Waves Detection of Dust Impacts near Jupiter

description: This is the supporting data set for the paper by the same title published in AGU JGR Space Physics. DOI 10.1029/2019JE006367 Abstract: The Juno spacecraft entered orbit at Jupiter on July 5, 2016. Since then, Juno has orbited Jupiter in high inclination orbits, crossing the ring plane near perijove 21 times. During 20 of the 21 crossings, the Waves instrument detected signals induced by dust impacts. The impact rate profiles show peaks of order 6/s around the ring plane with half width at half max ~2000-3000 km. The polarity ratio of the impact signals didn't follow the areas of the antennas exposed to dust impacts that change due to the rotation of the spacecraft, suggesting Waves detects impacts on the Juno spacecraft and not just on the Waves antennas. The impact rate profile changed during Perijove 19, when the spacecraft rotation axis was tilted to the south, increasing the area of the solar panels exposed to impacts, indicating that the detected impacts were on the spacecraft body. Grain sizes of order 1 micrometer are estimated, and the differential size distribution has a slope of -5.1. Notes on zip archive: There are subdirectories for each figure including a PDF of the figure and one or more text files with the data supporting the figure. Where the labeling in the text file is not quite complete, we've added a Fign-readme.txt file. Figures 9 and 10 are in the same directory as the two figures just have more of the same and all the data for both figures is in the same file.
DOI: 10.25345/c5hq3j
title: MassIVE MSV000085085 - 20200311_Pseudomonas_psychrophila_sp_JB418_MS2
title: P. psychrophila sp. JB418 was grown on 10% Cheese Curd Agar (CCA) for 3 days prior to extraction. For extraction, Acetonitrile was added to each culture and sonicated for 1hr, then solvent was removed and dried to afford a dry weighed extract. Extracts were then dissolved in either 100% (pooled replicates) or 90% (individual replicates) Methanol and LC-MS/MS was performed. Pooled replicate was run on a Bruker Impact II qTOF and individual biological replicates were run on a Bruker compact qTOF. Solvent B was ACN with 0.1% Formic Acid and Solvent A was water with 0.1% Formic Acid for both analyses, gradient of 10-100% B over the course of 10-12 minutes on a UPLC C18 column. File naming: JB418_alone = pooled biological replicate, JB418 followed by number = individual biological replicates, CCA = media controls and MeOH = solvent blanks.
DOI: 10.25345/c5s694
title: MassIVE MSV000085083 - XL-MS analysis of protein isolates from Flp-In 293 cells stably expressing SIN3A-HaloTag using DSSO crosslinker.
title: XL-MS analysis of protein isolates from Flp-In 293 cells stably expressing SIN3A-HaloTag using DSSO crosslinker.
DOI: 10.25919/5e693167df3cc
title: Parkes observations for project P1027 semester 2019OCTS_09

description: We propose to carry out Parkes follow-up observations of the new millisecond pulsar, J1431-6328, discovered by the Australian SKA Pathfinder (ASKAP) and Parkes Ultra-Wideband Low (UWL) receiver. The discovery demonstrated the power of identifying pulsar candidates in radio continuum images and then following up with high time resolution observations. The discovery itself is also interesting. PSR J1431-6328 has a spin period of 2.77 ms, and is likely to be in a binary system. Follow-up observations will enable us to measure the binary parameters, which will guide future multi-wavelength observations and might shed new lights on the binary evolution. The short spin period, relatively large flux density and sky location of PSR J1431-6328 also make it a promising candidate for pulsar timing arrays. The proposed observations will allow us to obtain a timing solution of this new pulsar, and are therefore essential for future timing observations.
DOI: 10.6084/m9.figshare.11971371.v4
title: CBD-IL-12

description: Installing collagen affinity to IL-12 improves efficacy and toxicity of IL-12.
DOI: 10.25573/data.11798931.v2
title: Panama Canal Meteorological Data_Flamenco

description: Data from the Panama Canal Authority (ACP) Flamenco meteorological station.<br><br>Most ACP meteorological stations provide the following parameters: air temperature, wind speed and direction, dew point, relative humidity, air pressure, solar radiation. Some stations, for some years (depending on what parameters the ACP made available that year) include interval max/min values, in addition to the interval average values.<br><br>Data have been freely provided by the Panama Canal Authority and are in the public domain.<br>Any publication using these data should credit the Panama Canal Authority.<br><br>Most data have been curated by STRI's Physical Monitoring Program.<br>All data are provided on an 'as is' basis.
DOI: 10.25345/c5nh6v
title: MassIVE MSV000085084 - Title: XL-MS analysis of protein isolates from Flp-In 293 cells stably expressing SIN3B isoform 2-HaloTag using DSSO crosslinker.
title: XL-MS analysis of protein isolates from Flp-In 293 cells stably expressing SIN3B isoform 2-HaloTag using DSSO crosslinker.
DOI: 10.25345/c5d12b
title: MassIVE MSV000085086 - 20200311_Penicillium_atramentosum_withandwithout_Pseudomonas_psychrophila_MS2
title: P. atramentosum sp. RS17 was grown alone and paired on 10% Cheese Curd Agar (CCA) for 8 days. For P. atramentosum paired with Pseudomonas psychrophila sp. JB418, P. psychrophila was inoculated next to P. atramentosum culture 5 days after initial P. atramentosum inoculation and then grown for an additional 3 days. Then cultures of P. atramentosum alone and P. atramentosum with P. psychrophila were extracted on the same day. For extraction, Acetonitrile was added to each culture and sonicated for 1hr, then solvent was removed and dried to afford a dry weighed extract. Extracts were then dissolved in either 100% (pooled replicates) or 90% (individual replicates) Methanol and LC-MS/MS was performed. Pooled replicate was run on a Bruker Impact II qTOF and individual biological replicates were run on a Bruker compact qTOF. Solvent B was ACN with 0.1% Formic Acid and Solvent A was water with 0.1% Formic Acid for both analyses, gradient of 10-100% B over the course of 10-12 minutes on a UPLC C18 column. File naming: RS17_alone = pooled biological replicate, RS17 followed by number = individual biological replicates, RS17_JB418 = pooled replicate of P. atramentosum grown with Pseudomonas psychrophila sp. JB418, RS17_JB418 followed by number = individual biological replicates. CCA = media controls and MeOH = solvent blanks.
DOI: 10.6073/pasta/73e4d60d8a96854e7243a52ae56ef815
title: MBON: Benthic percent cover in the Santa Barbara Channel

description: This study aims to quantify the percent cover of sessile species from shallow rocky reefs along the coast of Santa Barbara Channel, including the Channel Island National Park monitoring sites. BisQue (Bio-Imagery Semantic Query User Environment, a cloud-based analysis platform) was used to analyzed over 1500 images taken between 2013 and 2015 on the shallow reefs. This is the first phase of a bigger project that directs to improve the image analysis to complement or replace time-consuming in-situ surveys by divers. This data set contains percent cover and occurrence data of invertebrates, algae and fish from 22 subtidal rocky reef sites (Anacapa Landing, Arroyo Burro, Arroyo Quemado, Carpinteria, Cathedral Cove, Cuyler-Bat Rock, Diablo, Ellwood Mesa, Fry’s, Gull Island, Hazards, Isla Vista, Johnsons Lee-North, Mohawk, Naples, Pelican, Prisoners, Rhodes, Scorpion, Solimar, West-End and Cat Rock, Yellowbank). One survey image was collected at each site. Images were processed from 2015-2017 using BisQue with over 300 unique identifying tags. Data are organized in two tables (1) percent cover, (2) occurrence.
DOI: 10.25919/5e693d946a373
title: Parkes observations for project PX500 semester 2019OCTS_12

description: This proposal relates to time purchased by the Chinese Academy of Sciences for Parkes follow-up confirmation and timing of FAST discoveries. As the observing time has been purchased this proposal (and the related PX501) does not require TAC grading. The primary reason for submitting a proposal is to ensure an outreach statement and that the proposal is entered into OPAL for the data archive to access. The Chinese team have two time requests. The time scheduled for the first, relating to this proposal, will be allocated in blocks of 24 hours and the data will become available in the data archive with an 18 month embargo period. The second type of time will be scheduled in shorter blocks and the data archived with a 10 year embargo.
DOI: 10.5066/p9dybbgx
title: Database for the geologic map of the Paeroa Fault block and surrounding area, Taupo Volcanic Zone, New Zealand

description: The Taupo Volcanic Zone (TVZ), New Zealand, is the most productive area of explosive silicic volcanism in the world. Faulted early and middle Pleistocene volcanic products are generally concealed beneath voluminous, generally unfaulted, younger volcanic products. An exception is the southeast margin of the TVZ where the two parallel, northeast-trending Paeroa and Te Weta Fault blocks expose Quaternary volcanic products consisting predominantly of caldera-related, rhyolitic ignimbrites and lacustrine sediments. The Taupo-Reporoa Basin is situated along the eastern part of the map area, and its northernmost part underwent collapse to form Reporoa Caldera. The Paeroa Fault block is the largest exposed fault block within the TVZ, and it encompasses early and middle Pleistocene ignimbrites and sedimentary deposits that are buried throughout the Taupo-Reporoa Basin to the east. This map displays the volcanic and sedimentary geology of ~430 km2 of the Paeroa Fault block and the adjacent Te Weta Fault block at a scale of 1:50,000. Volcanic and sedimentary rocks are divided into the Reporoa Group, Whakamaru Group, and Huka Group (from oldest to youngest), which are overlain by relatively unfaulted late Pleistocene and Holocene surficial volcanic and sedimentary deposits. This geologic map database is accompanied by a report, which includes the formatted geologic map and explanatory text, available at https://doi.org/10.3133/ofr20201021. The authors ask that users of the geologic map database cite both the database and the report: Report: Downs, D.T., Leonard, G.S., Wilson, C.J.N., and Rowland, J.V., 2020, Geologic map of the Paeroa Fault block and surrounding area, Taupo Volcanic Zone, New Zealand: U.S. Geological Survey Open-File Report 2020-1021, https://doi.org/10.3133/ofr20201021. Database: Downs, D.T., 2020, Database for the geologic map of the Paeroa Fault block and surrounding area, Taupo Volcanic Zone, New Zealand: U.S. Geological Survey data release, https://doi.org/10.5066/P9DYBBGX.
DOI: 10.17632/2b646hgkt7.1
title: Data for: A decision support system for a capacity management problem at a container terminal

description: The capacity management problem at a container terminal seeks to balance supply (equipment assignment) and demand (arrivals of trucks) while improving customer service level and productivity indicators. In “A decision support system for a capacity management problem at a container terminal” a DSS is designed to manage traffic flows in a container terminal through proper sizing of truck appointments per time slot. In that article, the truck appointments are sized depending on the activity generated by vessels (which are usually very well anticipated). Thus, offering fewer truck appointments for busy time slots and more appointments for less busy time slots, regarding the yard resource availability. In this file are available the complete set of instances used in this paper, as well as additional instances artificially generated based on current data.
DOI: 10.7939/dvn/rh5xuv
title: Piyapong's Test Dataset 2020.03.11.1

description: test
DOI: 10.7939/dvn/rh5xuv/0qp8r9
title: 120110_parliamentnow.pdf
DOI: 10.7939/dvn/oueal1/tfrfpi
title: 120110_parliamentnow.pdf
DOI: 10.21227/t8j9-9t40
title: Graeco-Latin cubes

description: A Latin square of order q is a q×q array with elements from {0,1,...,q-1} such that each value occurs exactly once in each row and column. Two Latin squares L1 and L2 are orthogonal if (L1(x,y), L2(x,y)) = (s1,s2) has exactly one solution for each (s1,s2) from {0,1,...,q-1}×{0,1,...,q-1}. The square obtained by superimposing two orthogonal Latin squares to get entries with pairs of elements is called a Graeco-Latin square. A Latin cube of order q and is a q×q×q array with elements from {0,1,...,q-1} such that when any two coordinates are fixed, each element of {0,1,...,q-1} occurs exactly once. Two Latin cubes are orthogonal if fixing any coordinate gives a Graeco-Latin square when the cubes are superimposed. The cube obtained by superimposing two orthogonal Latin cubes is called a Graeco-Latin cube. Two standard methods to construct Graeco-Latin cubes are the following:(i) if q is a prime power larger than 3, than a q×q×q Graeco-Latin cube can be constructed as a Reed-Solomon code over the finite field GF(q);(ii) from a q'×q'×q' Graeco-Latin cube and a q''×q''×q'' Graeco-Latin cube, we can construct a q'q''×q'q''×q'q'' Graeco-Latin cube by Cartesian product.It is easy to see that with only these two constructions one cannot construct a Graeco-Latin cube of order 2p, where p is odd, or 3p, where p is not divisible by 3. In https://arxiv.org/abs/1911.12960 , there is a construction that allow to construct Graeco-Latin cubes of order 3p for some p not divisible by 3. This dataset contains examples of Graeco-Latin cubes of first few orders such that Graeco-Latin cubes of the same order cannot be constructed as a Reed-Solomon code or by Cartesian product from cubes of smaller orders.
DOI: 10.21227/xh3k-pv95
title: Graeco-Latin cubes

description: A Latin square of order q is a q×q array with elements from {0,1,...,q-1} such that each value occurs exactly once in each row and column. Two Latin squares L1 and L2 are orthogonal if (L1(x,y), L2(x,y)) = (s1,s2) has exactly one solution for each (s1,s2) from {0,1,...,q-1}×{0,1,...,q-1}. The square obtained by superimposing two orthogonal Latin squares to get entries with pairs of elements is called a Graeco-Latin square. A Latin cube of order q and is a q×q×q array with elements from {0,1,...,q-1} such that when any two coordinates are fixed, each element of {0,1,...,q-1} occurs exactly once. Two Latin cubes are orthogonal if fixing any coordinate gives a Graeco-Latin square when the cubes are superimposed. The cube obtained by superimposing two orthogonal Latin cubes is called a Graeco-Latin cube. Two standard methods to construct Graeco-Latin cubes are the following:(i) if q is a prime power larger than 3, than a q×q×q Graeco-Latin cube can be constructed as a Reed-Solomon code over the finite field GF(q);(ii) from a q'×q'×q' Graeco-Latin cube and a q''×q''×q'' Graeco-Latin cube, we can construct a q'q''×q'q''×q'q'' Graeco-Latin cube by Cartesian product.It is easy to see that with only these two constructions one cannot construct a Graeco-Latin cube of order 2p, where p is odd, or 3p, where p is not divisible by 3. In https://arxiv.org/abs/1911.12960 , there is a construction that allow to construct Graeco-Latin cubes of order 3p for some p not divisible by 3. This dataset contains examples of Graeco-Latin cubes of first few orders such that Graeco-Latin cubes of the same order cannot be constructed as a Reed-Solomon code or by Cartesian product from cubes of smaller orders.
DOI: 10.15468/4fdr5r
title: The first record of Dryadaulidae (Lepidoptera, Tineoidea) from Korea with the description of a new species, Dryadaula koreana sp. nov.

description: This dataset contains the digitized treatments in Plazi based on the original journal article Roh, Seung Jin, Shin, Young-Min, Lee, Dong-Jun, Byun, Bong-Kyu (2020): The first record of Dryadaulidae (Lepidoptera, Tineoidea) from Korea with the description of a new species, Dryadaula koreana sp. nov. Nota Lepidopterologica 43: 221-225, DOI: http://dx.doi.org/10.3897/nl.43.51564, URL: http://dx.doi.org/10.3897/nl.43.51564
DOI: 10.6073/pasta/f974ce5d26b36cc7dec2f8ac6456c903
title: Water Levels from the Shark River Slough, Everglades National Park (FCE), South Florida from October 2000 to Present

description: Water level is recorded at least hourly at SRS2, SRS3, SRS4, SRS5, and SRS6, SRS1c, and SRS1d. Water level is measured with pressure water level gauges that digitally record water height relative to the local soil surface.
DOI: 10.5281/zenodo.3706915
title: Data and analysis accompanying "A pan-plant protein complex map reveals deep conservation and novel assemblies"

description: This repository contains files, instructions to replicate, and internal scripts for the manuscript "A pan-plant protein complex map reveals deep conservation and novel assemblies" See also http://plants.proteincomplexes.org
DOI: 10.7939/dvn/o7gz27/ggcojw
title: 120110_parliamentnow.pdf
DOI: 10.25345/c5870d
title: MassIVE MSV000085087 - Identification of proteins associated with the KH-TUDOR moiety of the mitochondrial anchoring protein dAKAP1
title: Mouse MA10 Leydig cell proteins associated with purified KH-Tudor moiety from dAKAP1
DOI: 10.6073/pasta/5ebbc61168c4e0fcd0546f4f68c70a11
title: Santa Barbara Channel Marine BON: Gray Whales Count

description: This dataset documents the passage of gray whales (Eschrichtius robustus) migrating northbound since 2007, through the nearshore areas of the Santa Barbara Channel, along a corridor extending approximately 3 nautical miles (nm) from the mainland shore. The data is collected by a non-profit organization Gray Whales Count (http://www.graywhalescount.org/GWC/The_Count/The_Count.htmt), which is a research and education project. The survey is conducted at the Coal Oil Point Reserve in Goleta, California, USA. The coastline runs east-west, with northbound whales traveling west, left to right across our Point towards Point Conception. Every year, we survey 98 consecutive days from early February through mid-May. Conditions permitting, each survey-day begins at 9 AM and ends usually at 5 PM.