cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.14272/fotkyaajkylffn-uhfffaoysa-n.1
title: decane-1,10-diol
title: InChI=1S/C10H22O2/c11-9-7-5-3-1-2-4-6-8-10-12/h11-12H,1-10H2

description: This is a physical chemical entity[CHEBI_24431] associated with a molecule[CHEBI_25367].
 The molecule[CHEBI_25367] can be described by the following structural desciptors[cheminf_000085]:
 InChI descriptor[cheminf_000113]: InChI=1S/C10H22O2/c11-9-7-5-3-1-2-4-6-8-10-12/h11-12H,1-10H2, and canonical SMILES descriptor[cheminf_000007]: OCCCCCCCCCCO, and by the IUPAC name[cheminf_000107]: decane-1,10-diol.
 
 The physical chemical entity[CHEBI_24431] has a component solvent[CHEBI_46787] which is described by the canonical SMILES descriptor[cheminf_000007]:
 
 The physical chemical entity[CHEBI_24431] has the following Sample ID as registered in the research data repository chemotion (www.chemotion-repository.net, https://doi.org/10.25504/FAIRsharing.iagXcR): CRS-43216

 The physical chemical entity[CHEBI_24431] can be described by the physical descriptors [CHEMINF_000025]:
 Melting point descriptor[CHEMINF_000256]: 
 Boiling point descriptor[CHEMINF_000257]: 
 Refractive index descriptor[CHEMINF_000253]:

 The physical chemical entity[CHEBI_24431] can be further described by the following assays[OBI:0000070][CHMO:0001133]:
 
 CHMO:0001148 | 1H--13C heteronuclear multiple bond coherence (13C-1H HMBC)
 
 CHMO:0000596 | distortionless enhancement with polarization transfer (DEPT)
 
 CHMO:0000596 | distortionless enhancement with polarization transfer (DEPT)
 
 CHMO:0000599 | correlation spectroscopy (COSY)
 
 CHMO:0000593 | 1H nuclear magnetic resonance spectroscopy (1H NMR)
 
 CHMO:0001146 | 1H--13C heteronuclear single quantum coherence (1H-13C HSQC)
 
 CHMO:0000595 | 13C nuclear magnetic resonance spectroscopy (13C NMR)
 
 The physical chemical entity[CHEBI_24431] was deposited to the Molecule Archive of the Karlsruhe Insitute of Technology (KIT) with the following Sample ID: 

 Used ontologies:
 CHEBI - Chemical Entities of Biological Interest
 CHEMINF - chemical information ontology (information entities about chemical entities)
 CHMO - Chemical Methods Ontology
 OBI - Ontology for Biomedical Investigations
DOI: 10.14272/fotkyaajkylffn-uhfffaoysa-n/chmo0001148
title: 1H--13C heteronuclear multiple bond coherence (13C-1H HMBC) (decane-1,10-diol)
title: InChI=1S/C10H22O2/c11-9-7-5-3-1-2-4-6-8-10-12/h11-12H,1-10H2

description: dataset for 1H--13C heteronuclear multiple bond coherence (13C-1H HMBC)
DOI: 10.15468/dl.cn7343
title: Occurrence Download

description: A dataset containing 765 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((149.247609 -35.908612, 149.247609 -35.917595, 149.243118 -35.917595, 149.243118 -35.919841, 149.254347 -35.919841, 149.254347 -35.908612, 149.247609 -35.908612))"
 ]
}

 The dataset includes 765 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0053885-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.26509417
title: Source Data Extended Data Figures 7a and 7d

description: This file contains the source data for Extended Data Figures 7a and 7d.<b>a,</b> Mean plots describing genome-wide insulation score around TADs in the unchanged, lost, and gained TADs in GSK343 vs DMSO condition.<b>d,</b> Mean plots describing genome-wide insulation score around TADs in the unchanged, lost and gained TADs in X5050 vs DMSO condition.<br>
DOI: 10.6084/m9.figshare.26509417.v1
title: Source Data Extended Data Figures 7a and 7d

description: This file contains the source data for Extended Data Figures 7a and 7d.<b>a,</b> Mean plots describing genome-wide insulation score around TADs in the unchanged, lost, and gained TADs in GSK343 vs DMSO condition.<b>d,</b> Mean plots describing genome-wide insulation score around TADs in the unchanged, lost and gained TADs in X5050 vs DMSO condition.<br>
DOI: 10.6084/m9.figshare.25323984
title: Effects of long-term application of inorganic fertilizer and organic amendments on the amounts of fractionated soil organic carbon and their determining factors in paddy fields

description: To investigate how the long-term application of inorganic fertilizer and organic amendments affects the accumulation of organic matter in physico-chemically fractionated components in paddy soils and how the accumulation is determined by soil properties and anthropogenic carbon input, we studied the effect of variable management of inorganic fertilizer and organic amendments for &gt; 50 years on the amounts of accumulated soil organic carbon (SOC) in fractionated components in three paddy fields. SOC was fractionated into four components based on their physical and chemical properties: (1) light fraction (LF) derived from plant residues, (2) heavy fraction (HF) containing stable aggregates, (3) oxidizable fraction (OxF) and (4) non-oxidizable fraction (NOxF) forming organo-mineral complexes with fine-textured minerals. On average, the amount and percentage of accumulated C in the four fractions were as follows: OxF (6.63 gC kg<sup>−1</sup><sub>soil</sub>, 46%) &gt; NOxF (5.32, 35) &gt; LF (1.68, 12) &gt; HF (1.12, 7.2), suggesting about 80% of SOC was in fine, stable fractions. The amount of accumulated C in all fractions increased slightly with the application of inorganic fertilizer, while it increased considerably with the use of organic amendments. In addition, the application of fertilizers and amendments raised the proportion of C content in LF and HF, which are labile and related to soil fertility. Stepwise multiple regression analysis using two principal component analysis scores of soil properties and anthropogenic C input further revealed that the labile fractions (LF and HF) were more strongly determined by the management of fertilizers and amendments, while the stable fractions (OxF and NOxF) were more strongly determined by soil-specific properties, mainly the amorphous nature of the soil. These results indicate that the use of certain amounts of organic amendments would be recommended to carry out rational management to improve soil fertility and C sequestration in paddy fields, with the application of amorphous minerals as an additional option.
DOI: 10.6084/m9.figshare.25323984.v2
title: Effects of long-term application of inorganic fertilizer and organic amendments on the amounts of fractionated soil organic carbon and their determining factors in paddy fields

description: To investigate how the long-term application of inorganic fertilizer and organic amendments affects the accumulation of organic matter in physico-chemically fractionated components in paddy soils and how the accumulation is determined by soil properties and anthropogenic carbon input, we studied the effect of variable management of inorganic fertilizer and organic amendments for &gt; 50 years on the amounts of accumulated soil organic carbon (SOC) in fractionated components in three paddy fields. SOC was fractionated into four components based on their physical and chemical properties: (1) light fraction (LF) derived from plant residues, (2) heavy fraction (HF) containing stable aggregates, (3) oxidizable fraction (OxF) and (4) non-oxidizable fraction (NOxF) forming organo-mineral complexes with fine-textured minerals. On average, the amount and percentage of accumulated C in the four fractions were as follows: OxF (6.63 gC kg<sup>−1</sup><sub>soil</sub>, 46%) &gt; NOxF (5.32, 35) &gt; LF (1.68, 12) &gt; HF (1.12, 7.2), suggesting about 80% of SOC was in fine, stable fractions. The amount of accumulated C in all fractions increased slightly with the application of inorganic fertilizer, while it increased considerably with the use of organic amendments. In addition, the application of fertilizers and amendments raised the proportion of C content in LF and HF, which are labile and related to soil fertility. Stepwise multiple regression analysis using two principal component analysis scores of soil properties and anthropogenic C input further revealed that the labile fractions (LF and HF) were more strongly determined by the management of fertilizers and amendments, while the stable fractions (OxF and NOxF) were more strongly determined by soil-specific properties, mainly the amorphous nature of the soil. These results indicate that the use of certain amounts of organic amendments would be recommended to carry out rational management to improve soil fertility and C sequestration in paddy fields, with the application of amorphous minerals as an additional option.
DOI: 10.6084/m9.figshare.25245244
title: Variability of soil characteristics around an active volcano, Mt. Mayon in the Philippines with special reference to the distance and direction from the crater

description: This study investigated soil characteristics around Mt. Mayon, an active stratovolcano in the Philippines, which might depend on the meteorological condition and distribution of volcanic material deposition varying with distance and direction from the crater. Soil profiles were prepared at four and six sites in different directions, on a circle of 6 km and 15 km away from the crater, respectively. Soil profile morphology was described and the soil samples collected from each horizon were analyzed for physicochemical properties including total element, oxalate, and dithionite-citrate extractable Si, Al, and Fe, and phosphate adsorption coefficient, as well as clay mineralogical composition by XRD analysis. In general, regarding the distance, the soils showed less weathered status at 6 km and moderately weathered status at 15 km. In terms of direction, the soils at 6 km were moist and shallow in the northeast and southeast sites but dry and deep in the northwest and southwest sites. Meanwhile, despite all being deep, the soils at 15 km were moist in the northeast and east sites and dry in the other sites. While all soils showed less acidic nature and high levels of basic cations irrespective of distance and direction, phosphate adsorption coefficient was varied widely depending on the contents of oxalate-extractable Al and dithionite-citrate extractable Fe, for which the soils containing the higher amount of the oxalate-extractable Al showed the higher values of the coefficient. Consequently, the soils at 6 km were classified into Aquandic Humudepts (northeast), Vitrandic Eutrudepts (southeast and southwest), and Typic Udivitrands (northwest) while the soils at 15 km were Vitrandic Eutrudepts (northeast), Duric Epiaquands (east), and Typic Hapludalfs (southeast, southwest, northwest, and San Miguel Island). Such differences in soil formation and characteristics around Mt. Mayon seemed to be ascribable to the different geographical setting such as decrease in the supply of new volcanic material depending on the distance from the crater and the impacts of precipitation and typhoons, of which amount and intensity are higher in the east side than the west side because of the east side facing to the Pacific Ocean.
DOI: 10.6084/m9.figshare.25245244.v1
title: Variability of soil characteristics around an active volcano, Mt. Mayon in the Philippines with special reference to the distance and direction from the crater

description: This study investigated soil characteristics around Mt. Mayon, an active stratovolcano in the Philippines, which might depend on the meteorological condition and distribution of volcanic material deposition varying with distance and direction from the crater. Soil profiles were prepared at four and six sites in different directions, on a circle of 6 km and 15 km away from the crater, respectively. Soil profile morphology was described and the soil samples collected from each horizon were analyzed for physicochemical properties including total element, oxalate, and dithionite-citrate extractable Si, Al, and Fe, and phosphate adsorption coefficient, as well as clay mineralogical composition by XRD analysis. In general, regarding the distance, the soils showed less weathered status at 6 km and moderately weathered status at 15 km. In terms of direction, the soils at 6 km were moist and shallow in the northeast and southeast sites but dry and deep in the northwest and southwest sites. Meanwhile, despite all being deep, the soils at 15 km were moist in the northeast and east sites and dry in the other sites. While all soils showed less acidic nature and high levels of basic cations irrespective of distance and direction, phosphate adsorption coefficient was varied widely depending on the contents of oxalate-extractable Al and dithionite-citrate extractable Fe, for which the soils containing the higher amount of the oxalate-extractable Al showed the higher values of the coefficient. Consequently, the soils at 6 km were classified into Aquandic Humudepts (northeast), Vitrandic Eutrudepts (southeast and southwest), and Typic Udivitrands (northwest) while the soils at 15 km were Vitrandic Eutrudepts (northeast), Duric Epiaquands (east), and Typic Hapludalfs (southeast, southwest, northwest, and San Miguel Island). Such differences in soil formation and characteristics around Mt. Mayon seemed to be ascribable to the different geographical setting such as decrease in the supply of new volcanic material depending on the distance from the crater and the impacts of precipitation and typhoons, of which amount and intensity are higher in the east side than the west side because of the east side facing to the Pacific Ocean.
DOI: 10.6084/m9.figshare.25323984.v1
title: Effects of long-term application of inorganic fertilizer and organic amendments on the amounts of fractionated soil organic carbon and their determining factors in paddy fields

description: To investigate how the long-term application of inorganic fertilizer and organic amendments affects the accumulation of organic matter in physico-chemically fractionated components in paddy soils and how the accumulation is determined by soil properties and anthropogenic carbon input, we studied the effect of variable management of inorganic fertilizer and organic amendments for &gt; 50 years on the amounts of accumulated soil organic carbon (SOC) in fractionated components in three paddy fields. SOC was fractionated into four components based on their physical and chemical properties: (1) light fraction (LF) derived from plant residues, (2) heavy fraction (HF) containing stable aggregates, (3) oxidizable fraction (OxF) and (4) non-oxidizable fraction (NOxF) forming organo-mineral complexes with fine-textured minerals. On average, the amount and percentage of accumulated C in the four fractions were as follows: OxF (6.63 gC kg<sup>−1</sup><sub>soil</sub>, 46%) &gt; NOxF (5.32, 35) &gt; LF (1.68, 12) &gt; HF (1.12, 7.2), suggesting about 80% of SOC was in fine, stable fractions. The amount of accumulated C in all fractions increased slightly with the application of inorganic fertilizer, while it increased considerably with the use of organic amendments. In addition, the application of fertilizers and amendments raised the proportion of C content in LF and HF, which are labile and related to soil fertility. Stepwise multiple regression analysis using two principal component analysis scores of soil properties and anthropogenic C input further revealed that the labile fractions (LF and HF) were more strongly determined by the management of fertilizers and amendments, while the stable fractions (OxF and NOxF) were more strongly determined by soil-specific properties, mainly the amorphous nature of the soil. These results indicate that the use of certain amounts of organic amendments would be recommended to carry out rational management to improve soil fertility and C sequestration in paddy fields, with the application of amorphous minerals as an additional option.
DOI: 10.15468/dl.p6z4ee
title: Occurrence Download

description: A dataset listing the 90 species recorded in GBIF matching the query:
{
 "DatasetKey" : [
 "is Peces laguna El Tinije"
 ]
}

 The dataset's 90 records were derived from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0053877-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.25ujqz
title: Occurrence Download

description: A dataset containing 1461 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((147.379104 -35.895137, 147.379104 -35.910858, 147.372367 -35.910858, 147.372367 -35.919841, 147.354401 -35.919841, 147.354401 -35.926579, 147.370121 -35.926579, 147.370121 -35.93107, 147.376859 -35.93107, 147.376859 -35.933316, 147.388088 -35.933316, 147.388088 -35.935562, 147.399317 -35.935562, 147.399317 -35.93107, 147.392579 -35.93107, 147.392579 -35.924333, 147.394825 -35.924333, 147.394825 -35.917595, 147.399317 -35.917595, 147.399317 -35.91535, 147.394825 -35.91535, 147.394825 -35.908612, 147.403808 -35.908612, 147.403808 -35.910858, 147.4083 -35.910858, 147.4083 -35.91535, 147.415037 -35.91535, 147.415037 -35.917595, 147.417283 -35.917595, 147.417283 -35.919841, 147.421775 -35.919841, 147.421775 -35.901875, 147.406054 -35.901875, 147.406054 -35.895137, 147.379104 -35.895137))"
 ]
}

 The dataset includes 1461 records from 13 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0053886-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.26509426
title: Source Data Extended Data Figures 8a and 8c

description: This file contains the source data for Extended Data Figures 8a and 8c.<b>a,</b> Mean plots showing global H3K27me3 levels around TSS in K562 cells (left) and THP1 cells (right) treated with DMSO or GR for 24 h.<b>c,</b> Mean plots depicting genome-wide insulation score around TADs in the unchanged, lost and gained TADs in GR vs DMSO condition.
DOI: 10.6084/m9.figshare.26509426.v1
title: Source Data Extended Data Figures 8a and 8c

description: This file contains the source data for Extended Data Figures 8a and 8c.<b>a,</b> Mean plots showing global H3K27me3 levels around TSS in K562 cells (left) and THP1 cells (right) treated with DMSO or GR for 24 h.<b>c,</b> Mean plots depicting genome-wide insulation score around TADs in the unchanged, lost and gained TADs in GR vs DMSO condition.
DOI: 10.14272/dekpyxudjrabnk-uhfffaoysa-n/chmo0001148
title: 1H--13C heteronuclear multiple bond coherence (13C-1H HMBC) (dimethyl 5-aminobenzene-1,3-dicarboxylate)
title: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3

description: dataset for 1H--13C heteronuclear multiple bond coherence (13C-1H HMBC)
DOI: 10.14272/dekpyxudjrabnk-uhfffaoysa-n/chmo0000593
title: 1H nuclear magnetic resonance spectroscopy (1H NMR) (dimethyl 5-aminobenzene-1,3-dicarboxylate)
title: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3

description: dataset for 1H nuclear magnetic resonance spectroscopy (1H NMR)
DOI: 10.14272/dekpyxudjrabnk-uhfffaoysa-n/chmo0000595
title: 13C nuclear magnetic resonance spectroscopy (13C NMR) (dimethyl 5-aminobenzene-1,3-dicarboxylate)
title: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3

description: dataset for 13C nuclear magnetic resonance spectroscopy (13C NMR)
DOI: 10.14272/dekpyxudjrabnk-uhfffaoysa-n/chmo0001150
title: 1H--1H correlation spectroscopy (1H-1H COSY) (dimethyl 5-aminobenzene-1,3-dicarboxylate)
title: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3

description: dataset for 1H--1H correlation spectroscopy (1H-1H COSY)
DOI: 10.14272/dekpyxudjrabnk-uhfffaoysa-n.1
title: dimethyl 5-aminobenzene-1,3-dicarboxylate
title: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3

description: This is a physical chemical entity[CHEBI_24431] associated with a molecule[CHEBI_25367].
 The molecule[CHEBI_25367] can be described by the following structural desciptors[cheminf_000085]:
 InChI descriptor[cheminf_000113]: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3, and canonical SMILES descriptor[cheminf_000007]: COC(=O)c1cc(N)cc(c1)C(=O)OC, and by the IUPAC name[cheminf_000107]: dimethyl 5-aminobenzene-1,3-dicarboxylate.
 
 The physical chemical entity[CHEBI_24431] has a component solvent[CHEBI_46787] which is described by the canonical SMILES descriptor[cheminf_000007]:
 
 The physical chemical entity[CHEBI_24431] has the following Sample ID as registered in the research data repository chemotion (www.chemotion-repository.net, https://doi.org/10.25504/FAIRsharing.iagXcR): CRS-42254

 The physical chemical entity[CHEBI_24431] can be described by the physical descriptors [CHEMINF_000025]:
 Melting point descriptor[CHEMINF_000256]: 
 Boiling point descriptor[CHEMINF_000257]: 
 Refractive index descriptor[CHEMINF_000253]:

 The physical chemical entity[CHEBI_24431] can be further described by the following assays[OBI:0000070][CHMO:0001133]:
 
 CHMO:0000593 | 1H nuclear magnetic resonance spectroscopy (1H NMR)
 
 CHMO:0000595 | 13C nuclear magnetic resonance spectroscopy (13C NMR)
 
 CHMO:0001150 | 1H--1H correlation spectroscopy (1H-1H COSY)
 
 CHMO:0001146 | 1H--13C heteronuclear single quantum coherence (1H-13C HSQC)
 
 CHMO:0001148 | 1H--13C heteronuclear multiple bond coherence (13C-1H HMBC)
 
 The physical chemical entity[CHEBI_24431] was deposited to the Molecule Archive of the Karlsruhe Insitute of Technology (KIT) with the following Sample ID: 

 Used ontologies:
 CHEBI - Chemical Entities of Biological Interest
 CHEMINF - chemical information ontology (information entities about chemical entities)
 CHMO - Chemical Methods Ontology
 OBI - Ontology for Biomedical Investigations
DOI: 10.14272/dekpyxudjrabnk-uhfffaoysa-n/chmo0001146
title: 1H--13C heteronuclear single quantum coherence (1H-13C HSQC) (dimethyl 5-aminobenzene-1,3-dicarboxylate)
title: InChI=1S/C10H11NO4/c1-14-9(12)6-3-7(10(13)15-2)5-8(11)4-6/h3-5H,11H2,1-2H3

description: dataset for 1H--13C heteronuclear single quantum coherence (1H-13C HSQC)
DOI: 10.15468/dl.bdzjn6
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((147.630634 -35.919841, 147.630634 -35.924333, 147.63288 -35.924333, 147.63288 -35.919841, 147.630634 -35.919841))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0053888-240626123714530/datasets/export for details.
DOI: 10.6084/m9.figshare.26509438
title: Source Data Extended Data Figure 10c

description: This file contains the source data for Extended Data Figure 10c.<b>c,</b> Screenshots of ATAC-seq signal tracks at the promoters and gene body regions of CTCF (top) and TOP2A (bottom) in K562 cells treated with DMSO or GR for 72 h.
DOI: 10.6084/m9.figshare.26509438.v1
title: Source Data Extended Data Figure 10c

description: This file contains the source data for Extended Data Figure 10c.<b>c,</b> Screenshots of ATAC-seq signal tracks at the promoters and gene body regions of CTCF (top) and TOP2A (bottom) in K562 cells treated with DMSO or GR for 72 h.
DOI: 10.15468/dl.8s9z4n
title: Occurrence Download

description: A dataset containing 30271 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is Europe",
 "TaxonKey is Aedes albopictus (Skuse, 1894)"
 ]
}

 The dataset includes 30271 records from 118 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0053889-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.brd4n9
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((147.21067 -35.924333, 147.21067 -35.928824, 147.212915 -35.928824, 147.212915 -35.924333, 147.21067 -35.924333))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0053891-240626123714530/datasets/export for details.