cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.24439295.v1
title: Additional file 1 of Anti-atherosclerotic effects of naringenin and quercetin from Folium Artemisiae argyi by attenuating Interleukin-1 beta (IL-1β)/ matrix metalloproteinase 9 (MMP9): network pharmacology-based analysis and validation

description: Supplementary Material 1
DOI: 10.6084/m9.figshare.26632120
title: Additional file 4 of Anti-atherosclerotic effects of naringenin and quercetin from Folium Artemisiae argyi by attenuating Interleukin-1 beta (IL-1β)/ matrix metalloproteinase 9 (MMP9): network pharmacology-based analysis and validation

description: Supplementary Material 4
DOI: 10.6084/m9.figshare.26632120.v1
title: Additional file 4 of Anti-atherosclerotic effects of naringenin and quercetin from Folium Artemisiae argyi by attenuating Interleukin-1 beta (IL-1β)/ matrix metalloproteinase 9 (MMP9): network pharmacology-based analysis and validation

description: Supplementary Material 4
DOI: 10.1594/pangaea.52698
title: (Table 1) Cadmium and uranium of sediment core MD88-769
DOI: 10.1594/pangaea.320677
title: Water temperature real-time profiles from cruise GACA93 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.111922
title: Basic hydrographic, nutrient and carbon/nitrogen chemistries at station AT_II-119/4_13-1
DOI: 10.1594/pangaea.320261
title: Water temperature real-time profiles from cruise NZBI90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.15468/dl.m9avdn
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((147.394825 -33.907605, 147.394825 -33.909851, 147.399317 -33.909851, 147.399317 -33.914343, 147.401562 -33.914343, 147.401562 -33.907605, 147.394825 -33.907605))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069929-240626123714530/datasets/export for details.
DOI: 10.1594/pangaea.66448
title: Magnetic profile from the 8th Dec 2001 during cruise ANT-XIX/2 in the South Atlantic
DOI: 10.1594/pangaea.419293
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1992
DOI: 10.1594/pangaea.663654
title: Oceanography at CTD/bottle station IFREMER_0494
DOI: 10.1594/pangaea.111993
title: Basic hydrographic, nutrient and carbon/nitrogen chemistries at station AT_II-119/5_35-2
DOI: 10.1594/pangaea.476168
title: Hydrochemistry measured on water bottle samples at station NAtl_1957_DS_47N/3518-2

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.745110
title: (Table A1) CaCO3 contents and Sr/Ca ratios in ODP Leg 130, 138 and 154

description: Strontium/calcium (Sr/Ca) ratios in bulk and foraminiferal calcite have been used to constrain the history of Sr/Ca in the oceans and to evaluate calcite diagenetic alteration. However bulk Sr/Ca records also may be influenced by differences in Sr uptake and/or in the diagenetic susceptibility of different calcium carbonate sedimentary components. We present data on the sediment size fraction and calcium carbonate distribution in bulk samples, Sr/Ca in a range of sedimentary size components, and Sr/Ca in bulk sediments. Ocean Drilling Program samples from sites on Ontong Java Plateau and Ceara Rise (in the western equatorial Pacific and Atlantic, respectively) and from sites in the eastern equatorial Pacific were selected to represent progressive stages in the diagenetic pathway from the sea floor through a range of burial depths equivalent to sediment ages of ~5.6, ~9.4, and ~37.1 Ma. Samples were subdivided by size to produce a unique data set of size-specific Sr/Ca ratios. Fine fraction (&lt;45 ?m) Sr/Ca ratios are higher than those of all corresponding coarse fractions, indicating that fine nannofossil-dominated calcite has a Sr partition coefficient 1.3–1.5 times greater than that of coarse foraminifera-dominated calcite. Thus, absolute values of bulk Sr/Ca in contemporaneous samples reflect, in part, the ratio of fine to coarse calcite sedimentary components. Sr/Ca values in fine and coarse components also behave differently in their response to pre-burial dissolution and to recrystallization at depth. Coarse size components are sensitive to bottom water carbonate ion undersaturation, and they lose original Sr/Ca differences among contemporary samples over not, vert, similar10 my. In contrast, fine components recrystallize faster in more deeply buried samples. Interpretation of the historical Sr/Ca record is complicated by post-depositional diagenetic artifacts, and thus our data do not provide clear evidence of specific temporal changes in oceanic Sr/Ca ratios over the past 10 million years. This paper represents the first systematic attempt to examine trends in calcite Sr/Ca as a function of sediment size fraction and age.
description: Depth, sediment = mbsf
description: Supplement to: Andreasen, Gretchen Hampt; Delaney, Margaret Lois (2000): Bulk calcite size fraction distribution and Sr/Ca composition for deep-sea sediments at selected age horizons. Marine Geology, 169(1-2), 185-205
DOI: 10.1594/pangaea.424371
title: Hourly fast delivery sea level from coastal tide gauge station Ponta_Delgada in 2001
DOI: 10.1594/pangaea.816144
title: (Table 15) Organic C, organic N, and CaCO3 concentrations of sediments from DSDP Sites 70-506 to 70-509
DOI: 10.1594/pangaea.420252
title: Hourly delayed mode sea level from coastal tide gauge station Miami in 1985
DOI: 10.1594/pangaea.112277
title: Physical oceanography from CTD station EN198_8-2
DOI: 10.1594/pangaea.221046
title: Mineral composition of the less than 2 µm fraction from Hole 66-493A
DOI: 10.6084/m9.figshare.24439324
title: Additional file 1 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 1
DOI: 10.6084/m9.figshare.24439324.v1
title: Additional file 1 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 1
DOI: 10.6084/m9.figshare.24439505.v1
title: Additional file 2 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 2
DOI: 10.6084/m9.figshare.26632264
title: Additional file 3 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 3
DOI: 10.6084/m9.figshare.26632264.v1
title: Additional file 3 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 3
DOI: 10.6084/m9.figshare.26632270
title: Additional file 4 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 4
DOI: 10.6084/m9.figshare.26632270.v1
title: Additional file 4 of Evaluating understandability and actionability of online education materials for home-care patients with COVID-19 in Japan

description: Supplementary Material 4
DOI: 10.1594/pangaea.772173
title: (Table 1) Basement penetration, recovery, and lithology of crustal DSDP holes in the North Atlantic Ocean

description: Oceanic crustal drilling by R. V. Glomar Challenger at 15 sites in the North Atlantic has led to a complex picture of the upper half kilometer of the crust. Elements of the picture include the absence of the source for linear magnetic anomalies, marked episodicity of volcanic activity, ubiquitous low temperature alteration and evidence for large scale tectonic disturbance. Comparison sections in the Pacific and much deeper crustal drilling are needed to attack problems arising from the North Atlantic results.
description: Depth gives the basement penetration.
description: Supplement to: Hall, J Michael; Robinson, Paul T (1979): Deep crustal drilling in the North Atlantic Ocean. Science, 204(4393), 573-586
DOI: 10.1594/pangaea.805563
title: Total flux, particulate carbon and nitrogen from surface-tethered sediment traps at time series station BATS in 2007
DOI: 10.1594/pangaea.112309
title: Physical oceanography from CTD station AT_II-119/4_12-2
DOI: 10.1594/pangaea.915450
title: Pore-water salinity measurements in surface sediments (2017) within BEFmate experimental islands and saltmarsh enclosed plots at different elevation levels, Spiekeroog, Germany, 2017-01 to 2017-11

description: Data presented here were collected between January 2017 to November 2017 within the BEFmate project (Biodiversity - Ecosystem Functioning across marine and terrestrial ecosystems, https://uol.de/icbm/verbundprojekte/abgeschlossene-projekte/befmate/) of the Universities of Oldenburg and Göttingen and the Nationalpark Niedersächsisches Wattenmeer. Experimental islands and saltmarsh enclosed plots were created in the back barrier tidal flat and in the saltmarsh zone of the island of Spiekeroog.Sediment samples for the determination of pore-water salinity in soil were taken bi-/monthly in surface sediments (0-3 cm depth). Samples were measured in the laboratory within two month after sampling according to DIN ISO 11265:1997-06.Post-processing of measured data was done using MATLAB (R2018a). Quality control was performed by quality check algorithms:QC = 4 (bad data) - do not use this data-point.QC = 3 (questionable data) - likely bad data-point.QC = 2 (probably good data) - likely good data-point.QC = 1 (good data) - certainly good data-point.QC = 0 (unknown data) - no data point available.Further data sets will be added regularly.
description: Pore-water salinity measurements in surface sediments
DOI: 10.1594/pangaea.832181
title: Stable isotope ratios of planktonic foraminifera from North Atlantic surface sediments

description: We measured the oxygen isotopic composition of the deep-dwelling foraminiferal species G. inflata, G. truncatulinoides dextral and sinistral, and P. obliquiloculata in 29 modern core tops raised from the North Atlantic Ocean. We compared calculated isotopic temperatures with atlas temperatures and defined ecological models for each species. G. inflata and G. truncatulinoides live preferentially at the base of the seasonal thermocline. Under temperature stress, i.e., when the base of the seasonal thermocline is warmer than 16°C, G. inflata and G. truncatulinoides live deeper in the main thermocline. P. obliquiloculata inhabits the seasonal thermocline in warm regions. We tested our model using 10 cores along the Mauritanian upwelling and show that the comparison of d18O variations registered by the surficial species G. ruber and G. bulloides and the deep-dwelling species G. inflata evidences significant glacial-interglacial shifts of the Mauritanian upwelling cells.
description: Supplement to: Cléroux, Caroline; Cortijo, Elsa; Duplessy, Jean-Claude; Zahn, Rainer (2007): Deep-dwelling foraminifera as thermocline temperature recorders. Geochemistry, Geophysics, Geosystems, 8(4), Q04N11
DOI: 10.1594/pangaea.476499
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_6N_37W/14

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.426938
title: Daily sea level from coastal tide gauge station Dakar-D in 1989 (Research quality database)
DOI: 10.1594/pangaea.322513
title: Water temperature real-time profiles from cruise 4154900 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322298
title: Water temperature and salinity real-time profiles from cruise CGDG95 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.476853
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_OC_51W/248

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.742948
title: Benthic foraminifera abundance in ODP Leg 155 holes

description: The general Pleistocene architecture of the Amazon Fan has been reconstructed using sediment recovered by Ocean Drilling Program Leg 155. Huge regional mass-transport deposits (MTDs) make up a significant component of the Amazon Fan. These deposits each cover an area over 15,000 km**2 (approximately the size of Jamaica), reach a maximum thickness of 200 m, and consist of ~5000 Gt of sediment. Benthic foraminiferal fauna analysis and sedimentology indicate that the MTDs originated on the continental slope, which is at least 200 km laterally and 1500 m above their present position. Each mass-failure event was formed by the catastrophic failure of the continental slope and has been dated and correlated with climate-induced changes in sea level. Studies of the benthic foraminiferal assemblages in the Amazon Fan has been essential to our reconstruction of the origin and cause of these failures. The MTDs contain rare shelf (Quinqueloculina cf. stalkeri, Brizalina aenariensis, Q. lamarckiana, and Pseudononion atlanticum) and dominant upper-middle bathyal species (cassidulinids and buliminids). We conclude that the MTD originated between 200 and 600 m water depth, approximately the same zone in which gas hydrates occur. We suggest that the glacial MTDs referred to as Deep Eastern MTD (35–37 ka) and Unit R MTD (41–45 ka) correlate with rapid drops in sea level which destabilized continental slope gas-hydrate reservoirs causing catastrophic slope failure. An alternative explanation is required for the deglacial MTDs referred to as Western and Eastern Debris Flows (13–14 ka) which occurred as sea level rose rapidly during the Bølling-Allerød period. We suggest that the deglaciation of the Andes and the consequent enhanced sediment supply coupled with a shift of the depo-centre to the continental shelf, caused over-burdening and thus slope failure. Evidence for a 2 per mil negative d13C shift in both planktonic foraminifera and organic matter coeval with these failures suggest that whatever the cause, there was a large release of methane hydrate associated with each failure.
description: Supplement to: Maslin, Mark; Vilela, Naja; Mikkelsen, Naja; Grootes, Pieter Meiert (2005): Causes of catastrophic sediment failures of the Amazon Fan. Quaternary Science Reviews, 24(20-21), 2180-2193
DOI: 10.1594/pangaea.112515
title: Pigment concentrations measured on water bottle samples at station AT_II-119/4_19-1
DOI: 10.1594/pangaea.915442
title: Pore-water salinity measurements in surface sediments (2014-2015) within BEFmate experimental islands and saltmarsh enclosed plots at different elevation levels, Spiekeroog, Germany, 2014-10 to 2015-12

description: Data presented here were collected between October 2014 to December 2015 within the BEFmate project (Biodiversity - Ecosystem Functioning across marine and terrestrial ecosystems, https://uol.de/icbm/verbundprojekte/abgeschlossene-projekte/befmate/) of the Universities of Oldenburg and Göttingen and the Nationalpark Niedersächsisches Wattenmeer. Experimental islands and saltmarsh enclosed plots were created in the back barrier tidal flat and in the saltmarsh zone of the island of Spiekeroog.Sediment samples for the determination of pore-water salinity in soil were taken bi-/monthly in surface sediments (0-3 cm depth). Samples were measured in the laboratory within two month after sampling according to DIN ISO 11265:1997-06.Post-processing of measured data was done using MATLAB (R2018a). Quality control was performed by quality check algorithms:QC = 4 (bad data) - do not use this data-point.QC = 3 (questionable data) - likely bad data-point.QC = 2 (probably good data) - likely good data-point.QC = 1 (good data) - certainly good data-point.QC = 0 (unknown data) - no data point available.Further data sets will be added regularly.
description: Pore-water salinity measurements in surface sediments
DOI: 10.1594/pangaea.426511
title: Daily sea level from coastal tide gauge station Charleston in 1949 (Research quality database)
DOI: 10.1594/pangaea.716924
title: Radiosonde PS73/29536 during POLARSTERN cruise ANT-XXV/1 on 2008-11-05 11:00h

description: Height of tropopause 11049 m, precipitable water content 1.3667 cm
DOI: 10.1594/pangaea.423021
title: Hourly fast delivery sea level from coastal tide gauge station Dakar-E in 1997
DOI: 10.15468/dl.eyj7w6
title: Occurrence Download

description: A dataset containing 47368 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is Europe",
 "Country is Norway",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 "TaxonKey is Lyrurus tetrix (Linnaeus, 1758)",
 "Year 1970-2024"
 ]
}

 The dataset includes 47368 records from 25 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069930-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.380089
title: Radiosonde PS23/09320 during POLARSTERN cruise ANT-X/8 on 1993-02-14 20:53h

description: Height of tropopause 10589 m, precipitable water content 1.5283 cm
DOI: 10.1594/pangaea.357304
title: Water temperature XBT profiles from cruise DBFR96 (SCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.15468/dl.y3fzjt
title: Occurrence Download

description: A dataset containing 23 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "MULTIPOLYGON (((148.160642 -33.909851, 148.162888 -33.909851, 148.162888 -33.907605, 148.160642 -33.907605, 148.160642 -33.909851)), ((148.160642 -33.909851, 148.158397 -33.909851, 148.158397 -33.916588, 148.160642 -33.916588, 148.160642 -33.909851)))"
 ]
}

 The dataset includes 23 records from 4 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069931-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.111923
title: Basic hydrographic, nutrient and carbon/nitrogen chemistries at station AT_II-119/4_13-10
DOI: 10.1594/pangaea.58516
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2500-2
DOI: 10.6084/m9.figshare.26763310
title: GWAS of IOP

description: GWAS of corneal-compensated IOP (IOPcc) (n=97,644) in the UK Biobank cohort.
DOI: 10.6084/m9.figshare.26763310.v1
title: GWAS of IOP

description: GWAS of corneal-compensated IOP (IOPcc) (n=97,644) in the UK Biobank cohort.
DOI: 10.1594/pangaea.757168
title: Hydrochemistry measured on water bottle samples during Mikhail Lomonosov cruise ML38
DOI: 10.1594/pangaea.326020
title: Water temperature XBT profiles from cruise FNWC94 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.712153
title: (Appendix 1) 87Sr/86Sr ratios of planktonic foraminifera from DSDP Hole 86-577A

description: 87Sr/86Sr values for standards equal 0.710265 for NBS 987, and 0.709175 for seawater samples from the North Atlantic and Central Pacific. Ratios are fractionation corrected to an 86Sr/S8Sr ratio of 0.1194. All samples have been assigned a minimum uncertainty of +/- 22 * 10**-6, equivalent to the variability of repeated analyses of NBS 987
DOI: 10.1594/pangaea.112570
title: Absolute number of siliceous skeletons in sediment core M8_008-3, Ibero-Moroccan shelf (Table 5)
DOI: 10.1594/pangaea.68592
title: Clay mineralogy of ODP Hole 108-659A
DOI: 10.1594/pangaea.920168
title: Continuous water level observations at station BEFmate_I3low (2017-12)
DOI: 10.1594/pangaea.920304
title: Continuous water level observations at station BEFmate_I4low (2017-07)
DOI: 10.1594/pangaea.920272
title: Continuous water level observations at station BEFmate_I3low (2018-02)
DOI: 10.1594/pangaea.920277
title: Continuous water level observations at station BEFmate_I3low (2018-07)
DOI: 10.1594/pangaea.920284
title: Continuous water level observations at station BEFmate_I3upp (2017-04)
DOI: 10.1594/pangaea.476858
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_OC_51W/253

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.758900
title: (Table 1) Carbonate concentration of sediments from ODP Leg 164

description: Sediment cores recovered during ODP drilling operations are commonly scanned using a Minolta CM-2002 spectrophotometer to obtain spectral data. Core processing procedures aboard the JOIDES Resolution require that these spectral data be measured on wet cores. However, the effects of changing water content on the spectra of marine sediments is unknown. We examined the effects of changing water content on visible light (VIS) diffuse refiectance spectra for core samples composed of clay to foraminiferal ooze. The spectra of dry powdered samples were measured, then the samples were completely saturated (~35% water content) and spectra were measured at set time intervals as the samples progressively dried. The fully saturated samples were appreciably darker than the initial dry samples. The samples continued to darken during the initial phases of drying until the water content had decreased from 35% to ~20%. As the water content continued to decrease below 20%, the samples became progressively lighter and attained spectral values similar to the fully saturated samples at water contents of ~ 17%. Samples continued to lighten until they were totally dry; however, values never became as light as those of the dry samples prior to initial wetting. Changes in refiectance with decreasing water content are not uniform across the VIS. If the water content is greater than 5%, the refiectance decrease relative to a dry sample is greater at the red end of the spectrum. However, at water contents of less than 5%, the spectral curves of the wet and dry sediments are similar in shape, but the wet sediments are still darker. Comparison of these data with data obtained from similar saturation experiments using a coarse-grained beach sand suggest that the initial darkening of the saturated carbonate sediments apparently results frorn changing of the physical properties of the sediment; decreasing the water content apparently rearranges the grains. These studies suggest that maximum information will be obtained when spectral measurements are taken on samples that are allowed to dry as much as possible.
description: Supplement to: Balsam, William L; Deaton, Bobby C; Damuth, John E (1998): The effects of water content on diffuse reflectance spectrophotometry studies of deep-sea sediment cores. Marine Geology, 149(1-4), 177-189
DOI: 10.1594/pangaea.476875
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_OC_51W/270

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.920313
title: Continuous water level observations at station BEFmate_I4low (2018-04)
DOI: 10.6084/m9.figshare.24447629
title: Additional file 2 of Inflammatory response-based prognostication and personalized therapy decisions in clear cell renal cell cancer to aid precision oncology

description: Additional file 2. The clinical information of TCGA-KIRC, E-MATB-1980, and ICGC datasets.